{"meta":{"query_hash":"ba133cb3e4e0","filters":{"venue":"Geophysical Research Letters"},"cohort_total":2724,"direct_labels_cover":2,"predictions_cover":2724,"exported":2724,"export_cap":100000,"truncated":false,"label_status":"direct model label, unvalidated","prediction_status":"machine_predicted_unvalidated (Codex and Gemma teacher distillation)","score_status":"score_only:v0-immature-baseline","snapshot":{"source":"OpenAlex, pinned release, all 482 partitions","release":"2026-06-24","frame_built":"2026-07-12"},"permalink":"https://metacan.xera.ac/q/ba133cb3e4e0","api":"https://metacan.xera.ac/api/v1/cohort?venue=Geophysical+Research+Letters"},"results":[{"id":"W1480015928","doi":"10.1029/2007gl030780","title":"Recent volume loss of British Columbian glaciers, Canada","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":179,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Northern British Columbia","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Shuttle Radar Topography Mission; Glacier; Geology; Digital elevation model; Physical geography; Elevation (ballistics); Glacier mass balance; Thinning; Oceanography; Climatology; Geomorphology; Geography; Remote sensing","score_opus":0.026731860125983043,"score_gpt":0.25782684142388257,"score_spread":0.23109498129789952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1480015928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9751772,0.0022267234,0.0001517797,0.00054659165,0.000028778713,0.000012668739,0.014980712,0.000048021757,0.006827325],"genre_scores_gemma":[0.98817444,0.0010525112,0.00018058819,0.00009409004,0.000008775422,0.000008359946,0.0077692205,0.000012571351,0.0026995067],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995789,0.000014515536,0.000021066111,0.00009359212,0.00017187995,0.00012007156],"domain_scores_gemma":[0.998005,0.000055445555,0.00030826582,0.000058507412,0.0013454639,0.0002273311],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034532777,0.00033206693,0.00028177953,0.0020881232,0.0016918645,0.0018023899,0.00084909354,0.00035652358,0.0020514354],"category_scores_gemma":[0.001762165,0.00020489041,0.00021217809,0.0048130266,0.00056139665,0.0005599113,0.00056492264,0.0004657557,0.00032549788],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015040705,0.000028524653,0.95534027,0.000094359246,0.00014333367,0.0001840146,0.00096377404,0.0021981718,0.00082593394,0.00033785996,0.008118772,0.031614486],"study_design_scores_gemma":[0.000003677176,0.000004236531,0.9949197,0.00002250274,0.0000140684715,0.00004406171,0.00031616577,0.00043493402,0.00012730544,0.000018006654,0.0040866556,0.000008656511],"about_ca_topic_score_codex":0.99480385,"about_ca_topic_score_gemma":0.9976273,"teacher_disagreement_score":0.028674522,"about_ca_system_score_codex":0.028674522,"about_ca_system_score_gemma":0.013844026,"threshold_uncertainty_score":0.20804918},"labels":[],"label_agreement":null},{"id":"W1482297813","doi":"10.1029/2010gl043773","title":"Does the ocean impact the atmospheric response to stratospheric ozone depletion?","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Stratosphere; Ozone depletion; Environmental science; Atmosphere (unit); Atmospheric sciences; Troposphere; Ozone layer; Climatology; Ozone; Atmospheric model; Climate model; Atmospheric models; Atmospheric chemistry; Climate change; Meteorology; Geology; Oceanography; Geography","score_opus":0.01519911999834174,"score_gpt":0.29079354687350295,"score_spread":0.2755944268751612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1482297813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941837,0.0008558828,0.0003274412,0.0011055231,0.000052267525,0.0000034106504,0.00018817018,0.000019809571,0.0032636735],"genre_scores_gemma":[0.99887663,0.0005868439,0.00006183261,0.00009701369,0.000015261616,9.86235e-7,0.00005109099,0.0000069850853,0.00030338802],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998592,0.00004277312,0.000006584064,0.000016484817,0.000011675826,0.000063275074],"domain_scores_gemma":[0.99954504,0.00025317475,0.000080995334,0.000032673368,0.000033224955,0.000054867356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027731934,0.00041951373,0.00040386213,0.00019241968,0.00033120663,0.0012023464,0.00025031465,0.0009399345,0.0025305192],"category_scores_gemma":[0.0010234996,0.0002419584,0.000563272,0.00026921567,0.00046787964,0.00087681133,0.000985542,0.0004691343,0.0002820701],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025211968,0.00032960591,0.7114321,0.0005320874,0.0014459525,0.0014603505,0.0004050145,0.12914583,0.11098175,0.005815755,0.0018552195,0.03407515],"study_design_scores_gemma":[0.00022586787,0.0003897596,0.8659431,0.0000783893,0.0012126274,0.00018318169,0.0017722717,0.10522053,0.013806397,0.00616794,0.004915982,0.00008409094],"about_ca_topic_score_codex":0.011176239,"about_ca_topic_score_gemma":0.012626851,"teacher_disagreement_score":0.011176239,"about_ca_system_score_codex":0.000434535,"about_ca_system_score_gemma":0.00041867877,"threshold_uncertainty_score":0.02222234},"labels":[],"label_agreement":null},{"id":"W1482907538","doi":"10.1029/2011gl050079","title":"Airborne electromagnetic imaging of discontinuous permafrost","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":210,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Geology; Groundwater; Wetland; Arctic; Climate change; Earth science; Tundra; Hydrogeology; Physical geography; Thermokarst; Hydrology (agriculture); Environmental science; Oceanography; Ecology; Geography","score_opus":0.05705400704851837,"score_gpt":0.2824105469603205,"score_spread":0.2253565399118021,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1482907538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.989499,0.00023674061,0.0045409743,0.00008644103,0.000011785914,0.000008378364,0.0006374708,0.00007734644,0.004901788],"genre_scores_gemma":[0.9922426,0.00015517026,0.0064957766,0.00004957681,0.000014538946,0.000004488159,0.0003774232,0.000008713419,0.0006517429],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999652,0.0000048515685,0.0000010570077,0.0000095283785,0.000010288946,0.00000913225],"domain_scores_gemma":[0.99992216,0.000015774765,0.000013409489,0.00000811814,0.000030112595,0.0000104252995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007690761,0.000086348504,0.000049946575,0.0004305265,0.00013384344,0.0001677119,0.00010983184,0.00015795429,0.0007578983],"category_scores_gemma":[0.00014632297,0.00006343103,0.0000513605,0.00032239838,0.00007559869,0.00011366342,0.00013901418,0.000120714314,0.00017168104],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026711094,0.000109039465,0.32164183,0.0001535859,0.00007378711,0.0011656693,0.0008236463,0.002121588,0.54217124,0.0007406845,0.0034190523,0.12731265],"study_design_scores_gemma":[0.000013926273,0.000086852815,0.96645766,0.000024057073,0.0000341624,0.0015747003,0.0007932001,0.0063290806,0.019064268,0.000343152,0.0052628336,0.000016091317],"about_ca_topic_score_codex":0.0026336473,"about_ca_topic_score_gemma":0.010512294,"teacher_disagreement_score":0.0026336473,"about_ca_system_score_codex":0.00007633164,"about_ca_system_score_gemma":0.000095503485,"threshold_uncertainty_score":0.0052366257},"labels":[],"label_agreement":null},{"id":"W1486784739","doi":"10.1029/2011gl048025","title":"Rise of the Ellsworth mountains and parts of the East Antarctic coast observed with GPS","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Peninsula; Oceanography; Holocene; Ice shelf; East coast; Ice sheet; Climatology; Physical geography; Sea ice; Geography; Cryosphere; Archaeology","score_opus":0.07224211409627868,"score_gpt":0.257903721495206,"score_spread":0.18566160739892734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1486784739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927288,0.00016083638,0.00017244086,0.00002998806,0.000007040758,0.000007443796,0.0034597528,0.000011798115,0.003421982],"genre_scores_gemma":[0.9916448,0.00028809215,0.0006664584,0.000026162992,0.000011246931,0.000017428412,0.005691078,0.000006805604,0.0016479996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999162,0.000010684319,0.000008477485,0.000019144944,0.000024593473,0.000020974894],"domain_scores_gemma":[0.9996525,0.00003585046,0.00014266933,0.000039521878,0.00008233038,0.000047178637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018435762,0.00019413688,0.00014736726,0.0010660955,0.00035875218,0.000745502,0.00031360748,0.00014290363,0.0015021617],"category_scores_gemma":[0.00072408636,0.00012444743,0.00012365537,0.0015686078,0.00019630014,0.00022380354,0.00045949794,0.00013983328,0.00031386712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038255374,0.000008283939,0.9918064,0.000014376182,0.000036454927,0.000093173694,0.00024524837,0.00084904785,0.00047370157,0.00009428747,0.0008584194,0.0054824976],"study_design_scores_gemma":[0.0000027911565,0.0000063595926,0.99759537,0.000009547517,0.000007141314,0.000027254402,0.00019554647,0.00039777323,0.000088888024,0.000014003285,0.0016536444,0.000001768793],"about_ca_topic_score_codex":0.16574062,"about_ca_topic_score_gemma":0.44936678,"teacher_disagreement_score":0.16574062,"about_ca_system_score_codex":0.0005572373,"about_ca_system_score_gemma":0.0006467224,"threshold_uncertainty_score":0.32955176},"labels":[],"label_agreement":null},{"id":"W1486817810","doi":"10.1029/2012gl054017","title":"A new look at Greenland flow distortion and its impact on barrier flow, tip jets and coastal oceanography","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Advection; Oceanography; Climatology","score_opus":0.017882742143125567,"score_gpt":0.2707759942011678,"score_spread":0.25289325205804225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1486817810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9561852,0.010031649,0.0066491375,0.00368167,0.00011100936,0.000021448433,0.00044305477,0.00008926379,0.022787571],"genre_scores_gemma":[0.989495,0.0033129656,0.0037492411,0.00041091975,0.00010028232,0.0000055982564,0.00019069192,0.00003096562,0.0027044318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999894,0.000027402733,0.0000067574915,0.000016534517,0.000025859043,0.000029422656],"domain_scores_gemma":[0.99931276,0.000257784,0.00015912524,0.00007314949,0.00008362399,0.00011347153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043123856,0.00024982088,0.00035903257,0.0019646036,0.000391806,0.001770753,0.00026623256,0.00031844128,0.0015844414],"category_scores_gemma":[0.0010018082,0.000121586985,0.00031081607,0.0016737811,0.0019229632,0.0016070596,0.00084574055,0.00054994394,0.00010599286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023127516,0.000050473354,0.8024697,0.00017710814,0.00015705927,0.004053174,0.005656216,0.004859828,0.017017558,0.029127667,0.0026249369,0.13357502],"study_design_scores_gemma":[0.0000039700317,0.00007626925,0.96952415,0.00006947242,0.00002984335,0.0011010658,0.0030666417,0.0021924558,0.00082388474,0.0072648316,0.015816722,0.00003070737],"about_ca_topic_score_codex":0.047623735,"about_ca_topic_score_gemma":0.10312487,"teacher_disagreement_score":0.047623735,"about_ca_system_score_codex":0.0014889132,"about_ca_system_score_gemma":0.0007341407,"threshold_uncertainty_score":0.094693065},"labels":[],"label_agreement":null},{"id":"W1488491466","doi":"10.1002/2014gl061627","title":"Biases in southern hemisphere climate trends induced by coarsely specifying the temporal resolution of stratospheric ozone","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"NOAA Research; Natural Sciences and Engineering Research Council of Canada; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; National Oceanic and Atmospheric Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Ozone; Atmospheric sciences; Southern Hemisphere; Climatology; Ozone layer; Northern Hemisphere; Environmental science; Ozone depletion; Troposphere; Tropospheric ozone; Coupled model intercomparison project; Climate model; Atmosphere (unit); Stratosphere; Climate change; Meteorology; Geology; Geography","score_opus":0.05477626446008499,"score_gpt":0.2915468639570252,"score_spread":0.23677059949694024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1488491466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954015,0.00006475983,0.003501406,0.00005769204,0.000012660806,0.000004607902,0.00042731952,0.000044285138,0.0004856397],"genre_scores_gemma":[0.9985384,0.000024907524,0.0010584693,0.000021854124,0.0000045853835,0.0000035349126,0.00027332237,0.000007967614,0.00006703279],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99939215,0.00030200588,0.00006269442,0.00009727124,0.0001003514,0.0000455513],"domain_scores_gemma":[0.9963749,0.0018689788,0.0006194569,0.00080291677,0.00027656072,0.000057304576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023755378,0.00016560714,0.0001609735,0.00022954369,0.00012730049,0.0005331917,0.0002590303,0.00023664835,0.00046016154],"category_scores_gemma":[0.007293026,0.00013707517,0.00023580306,0.0004159436,0.00018787033,0.00030926985,0.00028946152,0.00025827714,0.000080380734],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010011019,0.000088481,0.77310866,0.00007100656,0.00042568016,0.00009161893,0.00039011324,0.17083843,0.032850094,0.002451388,0.0007305317,0.017952789],"study_design_scores_gemma":[0.0000944808,0.00013361362,0.8254622,0.00003082233,0.0001480238,0.0000705097,0.00024014951,0.15099645,0.019280365,0.0018098442,0.0016895817,0.000043910797],"about_ca_topic_score_codex":0.016507758,"about_ca_topic_score_gemma":0.020358218,"teacher_disagreement_score":0.016507758,"about_ca_system_score_codex":0.00043510308,"about_ca_system_score_gemma":0.00037562658,"threshold_uncertainty_score":0.032823324},"labels":[],"label_agreement":null},{"id":"W1488932768","doi":"10.1029/2009gl041644","title":"Measurements and predictions of subsidence induced by soil consolidation using persistent scatterer InSAR and a hyperbolic model","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Office of Naval Research; National Aeronautics and Space Administration","keywords":"Interferometric synthetic aperture radar; Geology; Consolidation (business); Subsidence; Interferometry; Geodesy; Geotechnical engineering; Synthetic aperture radar; Remote sensing; Geomorphology; Physics","score_opus":0.06602337745194566,"score_gpt":0.30565941303252997,"score_spread":0.23963603558058433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1488932768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910205,0.000024258197,0.008497945,0.000010884524,0.0000021590638,0.000006194721,0.00006062054,0.00008368698,0.0002938422],"genre_scores_gemma":[0.9978124,0.000020370251,0.0019862296,0.0000016122904,6.0193537e-7,0.0000030628007,0.00008348824,0.000003924142,0.00008827169],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999217,0.000013759394,0.0000049094706,0.000020894948,0.000022485054,0.00001627713],"domain_scores_gemma":[0.99979633,0.00006070759,0.000048039135,0.000037284444,0.000037255475,0.000020349278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028625276,0.00036737375,0.00016134721,0.00033707474,0.00007550028,0.00022594696,0.00025534118,0.00023315365,0.00025652442],"category_scores_gemma":[0.0005248201,0.00022701651,0.00017192462,0.00024282573,0.00025241982,0.000370106,0.00016463427,0.0001856802,0.0001218888],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005723715,0.0002232433,0.2065045,0.000065605345,0.000053511427,0.00021718371,0.00018595104,0.6559097,0.07752253,0.00054570177,0.00033396273,0.05786569],"study_design_scores_gemma":[0.000018971265,0.0001579895,0.057732943,0.0000028823424,0.000010022308,0.000035545927,0.000036165246,0.93564653,0.006164337,0.000081943945,0.000102926206,0.000009739426],"about_ca_topic_score_codex":0.005556526,"about_ca_topic_score_gemma":0.0071060676,"teacher_disagreement_score":0.005556526,"about_ca_system_score_codex":0.0004543839,"about_ca_system_score_gemma":0.00019757668,"threshold_uncertainty_score":0.011048377},"labels":[],"label_agreement":null},{"id":"W1489776005","doi":"10.1002/2013gl058442","title":"F region dusk ion temperature spikes at the equatorward edge of the high‐latitude convection pattern","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Science Foundation","keywords":"Dusk; Plasmasphere; Convection; Physics; Geophysics; Ion; Daytime; Latitude; Radar; Earth's magnetic field; Plasma; Atmospheric sciences; Local time; Geology; Astrophysics; Magnetosphere; Meteorology; Astronomy; Magnetic field","score_opus":0.012413857804950496,"score_gpt":0.25056201948330853,"score_spread":0.23814816167835803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1489776005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985581,0.000056519926,0.0003150619,0.00001579011,0.0000067891697,0.0000029596479,0.00010659052,0.000019577186,0.0009186452],"genre_scores_gemma":[0.999619,0.00001748547,0.00014757918,0.000005374787,0.0000038203593,0.0000012963828,0.00009102953,0.0000028463483,0.00011153128],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999691,0.0000020650555,0.0000015278956,0.000010018469,0.0000075768908,0.00000961741],"domain_scores_gemma":[0.999881,0.0000170797,0.000038852515,0.000013907936,0.000023614915,0.000025546819],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006801634,0.000095416275,0.00014335757,0.00030085605,0.00018264295,0.00022919553,0.0000984635,0.00012552757,0.0004644169],"category_scores_gemma":[0.00020959252,0.00007537425,0.00010266437,0.00019790887,0.00015805809,0.000112375135,0.00018296017,0.00022463409,0.000094786374],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011321552,0.00005505276,0.48270416,0.000084359475,0.0000955938,0.0011165901,0.0011598337,0.0019192217,0.48817238,0.00044589015,0.00090036134,0.02221426],"study_design_scores_gemma":[0.000007668088,0.000050929757,0.9833377,0.0000049542996,0.000012400943,0.00033126835,0.00010548866,0.0012796544,0.0140473405,0.00006320028,0.00075297593,0.000006372668],"about_ca_topic_score_codex":0.0031691138,"about_ca_topic_score_gemma":0.005130968,"teacher_disagreement_score":0.0031691138,"about_ca_system_score_codex":0.00017593554,"about_ca_system_score_gemma":0.00009268414,"threshold_uncertainty_score":0.0063013434},"labels":[],"label_agreement":null},{"id":"W1490491137","doi":"10.1029/2011gl050411","title":"A novel approach for micro‐scale characterization and modeling of geomaterials incorporating actual material heterogeneity","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Characterization (materials science); Finite element method; Indentation; Materials science; Fracture (geology); Material properties; Ultimate tensile strength; Scale (ratio); Modulus; Composite material; Structural engineering; Physics; Engineering","score_opus":0.08268212335752126,"score_gpt":0.28066778596013386,"score_spread":0.1979856626026126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1490491137","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.012880245,0.000051559662,0.98565984,0.000026029482,0.0000109503535,0.000037332586,0.000053056858,0.0002690706,0.0010118043],"genre_scores_gemma":[0.305761,0.00016772076,0.6925058,0.000032394433,0.000013904624,0.00023407734,0.0001447815,0.000050187457,0.0010901841],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998511,0.00001443286,0.000007847819,0.00003577479,0.00007949012,0.000011295396],"domain_scores_gemma":[0.9997936,0.000049161103,0.000031473668,0.00007977299,0.00003736372,0.000008665591],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022253385,0.00043337303,0.00040763684,0.000430259,0.00022195453,0.00043560006,0.0006992765,0.0005691761,0.0005813188],"category_scores_gemma":[0.00041483878,0.0003722292,0.00047649315,0.00030237663,0.00040167035,0.00059532846,0.0005175393,0.00037465256,0.00020103561],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000024338673,0.00009484342,0.0017665834,0.00018717993,0.00005506728,0.0002566628,0.00010728735,0.538568,0.36862513,0.021578768,0.00068141415,0.06805469],"study_design_scores_gemma":[0.0000037883233,0.00003453895,0.00060794957,0.0000045607308,0.000008155543,0.000109224486,0.000012229313,0.97649914,0.017485997,0.002245286,0.0029779817,0.00001118081],"about_ca_topic_score_codex":0.00094391505,"about_ca_topic_score_gemma":0.0015885335,"teacher_disagreement_score":0.00094391505,"about_ca_system_score_codex":0.00034550772,"about_ca_system_score_gemma":0.00048594867,"threshold_uncertainty_score":0.0025069118},"labels":[],"label_agreement":null},{"id":"W1491695496","doi":"10.1029/2011gl049674","title":"Implications of changing El Niño patterns for biological dynamics in the equatorial Pacific Ocean","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Sea surface temperature; Anomaly (physics); Oceanography; Climatology; Environmental science; Satellite; Primary production; La Niña; Pacific ocean; Chlorophyll a; Annual cycle; Ecosystem; Geology; Atmospheric sciences; El Niño Southern Oscillation; Biology; Ecology; Physics","score_opus":0.07877660617518338,"score_gpt":0.2943668171452826,"score_spread":0.21559021097009923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1491695496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9826805,0.0022916119,0.00028687427,0.004278997,0.00023282334,0.00002056175,0.0013186681,0.000023345558,0.008866523],"genre_scores_gemma":[0.99707663,0.0016814476,0.00009466961,0.00036140828,0.000069028065,0.000006519487,0.00036266557,0.000006121029,0.00034150388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978465,0.000056676574,0.000022316844,0.000045968834,0.000026093076,0.00006432301],"domain_scores_gemma":[0.999263,0.00012236103,0.0002963995,0.000040388346,0.00010025292,0.00017756168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006640026,0.00023594992,0.00013939421,0.0005076736,0.00040858748,0.0012031713,0.0003494371,0.0004241756,0.0023736774],"category_scores_gemma":[0.0022059996,0.00011077183,0.00029442247,0.0009151851,0.0005717943,0.0007657511,0.00044409835,0.00039247386,0.00020034329],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023524702,0.00006259292,0.9794127,0.00008802435,0.0001261231,0.00046417434,0.0002559934,0.0012488653,0.0024938353,0.00076338614,0.0010734274,0.013775571],"study_design_scores_gemma":[0.000012193068,0.000017794422,0.9974903,0.000018497167,0.00001755226,0.000029156019,0.00062909385,0.00048760066,0.000117013,0.00031808915,0.00085767685,0.0000050574617],"about_ca_topic_score_codex":0.037260026,"about_ca_topic_score_gemma":0.033178493,"teacher_disagreement_score":0.037260026,"about_ca_system_score_codex":0.000835579,"about_ca_system_score_gemma":0.00068993197,"threshold_uncertainty_score":0.07408631},"labels":[],"label_agreement":null},{"id":"W1492152512","doi":"10.1029/2012gl051689","title":"Joint horizontal‐vertical anisotropic scaling, isobaric and isoheight wind statistics from aircraft data","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Wind and Air Flow Studies","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Scaling; Physics; Transverse plane; Horizontal and vertical; Spectral line; Isobaric process; Turbulence; Isobar; Stratification (seeds); Meteorology; Statistical physics; Geodesy; Geology; Geometry; Mathematics; Thermodynamics; Nuclear physics; Quantum mechanics","score_opus":0.05373869356190511,"score_gpt":0.3030447486705874,"score_spread":0.24930605510868228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1492152512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974496,0.000019746756,0.0012068045,0.000008258369,0.0000027408532,0.000004471281,0.00034378708,0.000031653817,0.0009329345],"genre_scores_gemma":[0.9991819,0.000010285202,0.00035434408,0.0000010072565,0.0000019611389,0.0000028075892,0.00039316106,0.0000041133135,0.000050435912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998715,0.000018663484,0.000014132424,0.000026476144,0.00004688207,0.000022375067],"domain_scores_gemma":[0.9995177,0.000087322085,0.00012264343,0.00007715118,0.00013478869,0.000060472164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029463193,0.00016748546,0.000114704,0.0010038777,0.00016259495,0.00037483545,0.000104686136,0.00008982698,0.0005318416],"category_scores_gemma":[0.0011875882,0.000083271574,0.00016442924,0.00068632775,0.00018686414,0.00031353094,0.00025433724,0.0001527647,0.00016581902],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013509515,0.00005148812,0.93302876,0.000028254144,0.000053984822,0.00011523123,0.00031408286,0.012671986,0.0230215,0.0012816805,0.000629283,0.028668528],"study_design_scores_gemma":[0.0000049718274,0.000028980963,0.98086995,0.000003098061,0.00000985785,0.00004449292,0.00006156711,0.016770441,0.0016247331,0.00025754102,0.00031519457,0.000009017923],"about_ca_topic_score_codex":0.0038826559,"about_ca_topic_score_gemma":0.0045033903,"teacher_disagreement_score":0.0038826559,"about_ca_system_score_codex":0.00013412976,"about_ca_system_score_gemma":0.00012474207,"threshold_uncertainty_score":0.007720113},"labels":[],"label_agreement":null},{"id":"W1492961050","doi":"10.1029/2009gl041972","title":"Gulf Stream thermal fronts detected by synthetic aperture radar","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Geology; Synthetic aperture radar; Gulf Stream; Remote sensing; Thermal; Geophysics; Meteorology; Oceanography; Geography","score_opus":0.010257440764257943,"score_gpt":0.23586945398418274,"score_spread":0.2256120132199248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1492961050","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940749,0.00013597282,0.0035708824,0.000036348305,0.000010855412,0.000010162214,0.00022337477,0.0000543373,0.0018831913],"genre_scores_gemma":[0.9913823,0.0001747686,0.0074159484,0.000030307672,0.000017816046,0.00000648735,0.00045396033,0.0000050849676,0.0005134292],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999956,0.0000048560973,0.0000021649362,0.0000079018155,0.000020162814,0.000008879397],"domain_scores_gemma":[0.99986625,0.000019820176,0.00003632464,0.000011572458,0.000047531263,0.000018441484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012781694,0.0001847576,0.000080655,0.00071053597,0.00007407024,0.00022754332,0.000062972256,0.00011960758,0.00038518646],"category_scores_gemma":[0.00029110681,0.000109742534,0.00009343148,0.000239028,0.000106293875,0.00020148061,0.00015180472,0.00012613868,0.00011162381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009929353,0.00015124053,0.41535783,0.00016763326,0.00007568141,0.0005531252,0.00041222703,0.016036611,0.4092539,0.0011201027,0.0024347005,0.15344417],"study_design_scores_gemma":[0.00006667018,0.00020575302,0.8261495,0.00003850604,0.000047190333,0.0005800059,0.00020004649,0.11334706,0.055156637,0.00060883706,0.0035640385,0.000035728266],"about_ca_topic_score_codex":0.0018727286,"about_ca_topic_score_gemma":0.0027091727,"teacher_disagreement_score":0.0018727286,"about_ca_system_score_codex":0.00014053464,"about_ca_system_score_gemma":0.000099580255,"threshold_uncertainty_score":0.0037236214},"labels":[],"label_agreement":null},{"id":"W1493509693","doi":"10.1002/2014gl062768","title":"Long‐term change of CO<sub>2</sub> latitudinal distribution in the upper troposphere","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministry of Education, India; Ministry of Education, Culture, Sports, Science and Technology; York University","keywords":"Troposphere; Southern Hemisphere; Northern Hemisphere; Climatology; Biosphere; Environmental science; Latitude; Atmospheric sciences; Biosphere model; Geology","score_opus":0.03763950247508062,"score_gpt":0.2913888288483181,"score_spread":0.2537493263732375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1493509693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924374,0.000045274395,0.00008326442,0.000013966996,0.0000019822605,7.816084e-7,0.00041456378,0.000004065597,0.000192355],"genre_scores_gemma":[0.9994036,0.000025594936,0.000055352433,0.000005610164,0.000002790427,0.0000014964511,0.00041728414,0.0000013291776,0.000086960856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999416,0.0000087192275,0.000004392598,0.000017230732,0.0000105312165,0.000017509821],"domain_scores_gemma":[0.9997507,0.000025521767,0.00009208719,0.000019194345,0.00007335287,0.000039139515],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022262344,0.00012841861,0.00015373323,0.0003656001,0.00016140816,0.0002922623,0.00009197933,0.00013822403,0.0005877418],"category_scores_gemma":[0.00032747377,0.00009465937,0.00019044873,0.0005303998,0.00012259507,0.00019263686,0.00016378939,0.00015768851,0.00014760703],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000103460305,0.00002055466,0.9844603,0.0000143514235,0.00011233477,0.00008409651,0.00010717873,0.0012961308,0.010214824,0.00005127487,0.00026180362,0.0032735788],"study_design_scores_gemma":[3.4720796e-7,0.0000044238623,0.99923325,6.916661e-7,0.0000053634876,0.000008881071,0.000016715461,0.00040161225,0.00022444011,0.0000029570176,0.000100369034,9.981796e-7],"about_ca_topic_score_codex":0.029266968,"about_ca_topic_score_gemma":0.05108944,"teacher_disagreement_score":0.029266968,"about_ca_system_score_codex":0.0003338849,"about_ca_system_score_gemma":0.00016732056,"threshold_uncertainty_score":0.058193207},"labels":[],"label_agreement":null},{"id":"W1494783053","doi":"10.1029/2004gl019447","title":"Solar influence on the O(<sup>1</sup><i>D</i>) dayglow emission rate: Global‐scale measurements by WINDII on UARS","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Solar zenith angle; Thermosphere; Zenith; Atmospheric sciences; Airglow; Physics; Ionosphere; Irradiance; Scale height; Environmental science; Astrophysics; Astronomy; Optics","score_opus":0.018190562996191883,"score_gpt":0.2790137471348716,"score_spread":0.2608231841386797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1494783053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99816257,0.00016907102,0.00022682274,0.0000228027,0.0000037365874,0.000005515408,0.00041693274,0.000015143184,0.0009775365],"genre_scores_gemma":[0.99884486,0.00011893029,0.00031079352,0.000014113741,0.0000074228146,0.000004505571,0.00058833376,0.000005591574,0.0001054628],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999356,0.0000103014645,0.0000038313497,0.000018696142,0.000018177037,0.000013444307],"domain_scores_gemma":[0.9998958,0.000018973858,0.0000345921,0.000010802353,0.000025081277,0.000014791083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001440041,0.00022500791,0.00018695397,0.0002486695,0.00026658966,0.00034984408,0.00013554055,0.00020310932,0.00037259384],"category_scores_gemma":[0.000340668,0.00012628958,0.00016967798,0.00031734534,0.00013235625,0.00020686835,0.00018811086,0.0002288745,0.00011100699],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037886633,0.000055857097,0.8969768,0.000052887768,0.00015438077,0.00016722672,0.00022123854,0.003035087,0.08008583,0.00024486444,0.0005410016,0.018086007],"study_design_scores_gemma":[0.0000052844075,0.000019233958,0.9969112,0.000002497861,0.000012311223,0.00002737978,0.000028729935,0.00067732536,0.0018615285,0.000018202723,0.00043323048,0.000003142029],"about_ca_topic_score_codex":0.012193352,"about_ca_topic_score_gemma":0.019113837,"teacher_disagreement_score":0.012193352,"about_ca_system_score_codex":0.0003381878,"about_ca_system_score_gemma":0.000100607074,"threshold_uncertainty_score":0.024244785},"labels":[],"label_agreement":null},{"id":"W1495016338","doi":"10.1002/2013gl058553","title":"First common volume ground‐based and space measurements of the mesospheric front in noctilucent clouds","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Athabasca University","funders":"","keywords":"Thermosphere; Depth sounding; Mesosphere; Mesopause; Altitude (triangle); Airglow; Geology; Atmosphere (unit); Atmospheric sciences; Meteor (satellite); Satellite; Front (military); Observatory; Environmental science; Ionosphere; Meteorology; Geophysics; Physics; Stratosphere; Astronomy","score_opus":0.021778327914210197,"score_gpt":0.26254178399895456,"score_spread":0.24076345608474436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1495016338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947566,0.00018463431,0.00082154723,0.000021760228,0.000017688715,0.00002285316,0.0014245823,0.00007899962,0.002671497],"genre_scores_gemma":[0.9962723,0.0000575692,0.0012342678,0.000015016477,0.000013837772,0.000013513303,0.0020733147,0.000015402711,0.00030461774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998734,0.000006977667,0.0000032893656,0.000027427868,0.000052631054,0.000036201196],"domain_scores_gemma":[0.9997582,0.000021329197,0.000046396057,0.00003042107,0.00008099963,0.00006263668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014287925,0.00030404056,0.00023854055,0.0008925811,0.000553024,0.00040261514,0.00039096916,0.00026212508,0.0008752438],"category_scores_gemma":[0.00024880967,0.00012256888,0.00019574654,0.00054174307,0.00025407184,0.00032707065,0.000554887,0.0003597262,0.00021498058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012437154,0.0002044361,0.68394387,0.00014062379,0.00014262077,0.0010887553,0.0010520093,0.002205997,0.26506668,0.00020461614,0.0016376826,0.043068916],"study_design_scores_gemma":[0.000019955745,0.00009694423,0.9884377,0.00001304197,0.000018971828,0.00015526032,0.0001955554,0.0012746275,0.007346705,0.000055718512,0.0023756982,0.000009712491],"about_ca_topic_score_codex":0.016036414,"about_ca_topic_score_gemma":0.035910785,"teacher_disagreement_score":0.016036414,"about_ca_system_score_codex":0.00038908087,"about_ca_system_score_gemma":0.00026332692,"threshold_uncertainty_score":0.03188616},"labels":[],"label_agreement":null},{"id":"W1496193094","doi":"10.1002/grl.50717","title":"Analysis of satellite remote sensing observations of low ozone events in the tropical upper troposphere and links with convection","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Waterloo; University of Saskatchewan; Dalhousie University","funders":"","keywords":"Microwave Limb Sounder; Troposphere; Ozone; Satellite; Atmospheric sciences; Convection; Environmental science; Chemical transport model; Tropospheric ozone; Climatology; Total Ozone Mapping Spectrometer; Geology; Ozone layer; Stratosphere; Meteorology; Physics","score_opus":0.026049476786946645,"score_gpt":0.2640636542061589,"score_spread":0.23801417741921227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1496193094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995677,0.000022435417,0.000060263843,0.000010829738,8.558686e-7,0.0000017050874,0.00021607651,0.0000029408325,0.0001172568],"genre_scores_gemma":[0.9992632,0.000028091772,0.00015137381,0.0000044157673,0.0000027728413,0.0000028802426,0.0004896504,9.072356e-7,0.00005671475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999946,0.000009777629,0.0000046348587,0.000012225977,0.000013891262,0.000013412533],"domain_scores_gemma":[0.9996985,0.000075525626,0.00011144509,0.000017394499,0.00003460048,0.00006266055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023284838,0.0001215274,0.00010563345,0.00071136723,0.00014563325,0.00023872146,0.000100873454,0.00011563088,0.00052676746],"category_scores_gemma":[0.00053046126,0.00009513064,0.00017070603,0.0005433891,0.00010147983,0.00014124384,0.00016521393,0.00010039547,0.000060633534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013194607,0.000055498283,0.9811678,0.000024790961,0.00007968898,0.00006722649,0.00010988597,0.0015928756,0.009420832,0.00006937465,0.00019249757,0.00708759],"study_design_scores_gemma":[0.0000059018716,0.000027498247,0.996229,0.0000029001685,0.000015278436,0.000027303699,0.000058555775,0.0031079333,0.00039483365,0.00001732281,0.000111504785,0.0000019151819],"about_ca_topic_score_codex":0.017365148,"about_ca_topic_score_gemma":0.020852964,"teacher_disagreement_score":0.017365148,"about_ca_system_score_codex":0.00021221048,"about_ca_system_score_gemma":0.00018422319,"threshold_uncertainty_score":0.034528136},"labels":[],"label_agreement":null},{"id":"W1498564333","doi":"10.1029/2010gl045416","title":"Upstream Pc3‐4 waves: Experimental evidence of propagation to the nightside plasmapause/plasmatrough","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Physics; Plasmasphere; Geophysics; Magnetosphere; Magnetohydrodynamics; Field line; Computational physics; Magnetohydrodynamic drive; Wave propagation; Magnetic field; Shock wave; Longitudinal wave; Interplanetary magnetic field; Solar wind; Mechanics; Optics","score_opus":0.023552261638447477,"score_gpt":0.31649259656169554,"score_spread":0.29294033492324806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1498564333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945754,0.00019233658,0.001890449,0.0000363536,0.000012524266,0.00000727924,0.00006763559,0.000027550537,0.003190414],"genre_scores_gemma":[0.998315,0.00010135254,0.0010421734,0.000020864676,0.0000146516295,0.0000050405824,0.00008891991,0.0000065105373,0.000405561],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995196,0.0000061853757,0.0000018682537,0.0000129661485,0.0000131756,0.000013721991],"domain_scores_gemma":[0.9997063,0.00007986506,0.000058958365,0.000053717795,0.000063150204,0.000037887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001050249,0.00011779018,0.000081574224,0.0001994121,0.00028667363,0.00021396241,0.00023940367,0.00024064218,0.0016794956],"category_scores_gemma":[0.00030995824,0.000085049716,0.000045138597,0.0001798945,0.0003404344,0.00022392819,0.00026735585,0.0003382136,0.00017853531],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007378712,0.00006572267,0.04073692,0.00007732414,0.000019603627,0.00044450402,0.00038717862,0.00009018787,0.93495166,0.00059517694,0.00030322082,0.021590652],"study_design_scores_gemma":[0.000067646535,0.0008000094,0.5596342,0.000023105633,0.000052645504,0.0014468186,0.00045910652,0.001982807,0.4276487,0.0010883921,0.0067741284,0.000022378841],"about_ca_topic_score_codex":0.0006791516,"about_ca_topic_score_gemma":0.0006877774,"teacher_disagreement_score":0.0016794956,"about_ca_system_score_codex":0.00010176919,"about_ca_system_score_gemma":0.00007258624,"threshold_uncertainty_score":0.0056185126},"labels":[],"label_agreement":null},{"id":"W1499019742","doi":"10.1002/2014gl059989","title":"Effects of westerly wind bursts on El Niño: A new perspective","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"","keywords":"Downwelling; Geology; Climatology; Atmosphere (unit); Atmospheric sciences; Westerlies; Oceanography; Physics; Meteorology; Upwelling","score_opus":0.022346390365117975,"score_gpt":0.31441463171605594,"score_spread":0.29206824135093795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1499019742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92372376,0.011153449,0.010505483,0.010713031,0.0011293477,0.000024344428,0.0013687502,0.00014861603,0.041233197],"genre_scores_gemma":[0.98869145,0.006286998,0.0008097659,0.0004997056,0.0014413586,0.0000054183633,0.00017198148,0.00006176165,0.0020316318],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983704,0.000050843522,0.000012337526,0.000041271876,0.000027402662,0.000031059222],"domain_scores_gemma":[0.9983864,0.00089554995,0.00032772525,0.00013263781,0.00013605284,0.000121677],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008698659,0.00064050953,0.0007013415,0.0005642895,0.00036195392,0.0021082577,0.0005599828,0.000789278,0.003504296],"category_scores_gemma":[0.0020474896,0.00031894413,0.0006793976,0.00041310952,0.0008502351,0.0026134094,0.0010966454,0.001273625,0.00019636062],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029997728,0.000995516,0.3851047,0.0007852572,0.0015355293,0.0028137693,0.001917218,0.26122054,0.029299583,0.13513619,0.010331574,0.16786045],"study_design_scores_gemma":[0.00032969343,0.00089483574,0.61135364,0.00033389835,0.00090480543,0.0004654249,0.0016828072,0.23354945,0.004150907,0.105705634,0.040357396,0.00027151333],"about_ca_topic_score_codex":0.007345319,"about_ca_topic_score_gemma":0.008720881,"teacher_disagreement_score":0.007345319,"about_ca_system_score_codex":0.0005155433,"about_ca_system_score_gemma":0.0003257506,"threshold_uncertainty_score":0.014605105},"labels":[],"label_agreement":null},{"id":"W1499471208","doi":"10.1029/2009gl037242","title":"Frequency of cool summers in interior North America over the past three centuries","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg; Research Manitoba; Natural Resources Canada; Canadian Forest Service","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Winnipeg","keywords":"Mars Exploration Program; Secular variation; Dendrochronology; Environmental science; Pinus <genus>; Term (time); Climatology; Physical geography; Geology; Atmospheric sciences; Geography; Archaeology; Physics; Geophysics; Astronomy","score_opus":0.028932795470068766,"score_gpt":0.28844226501424963,"score_spread":0.25950946954418086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1499471208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903643,0.00017862579,0.000072492236,0.000019365594,0.0000034478337,8.9669845e-7,0.00026238343,0.0000040462123,0.00042231358],"genre_scores_gemma":[0.9993622,0.000099630444,0.00009712047,0.000008751619,0.0000069802477,0.0000020607065,0.0002901443,0.000001724858,0.00013126573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994445,0.000009255936,0.0000040822647,0.000022988783,0.000008715246,0.000010554311],"domain_scores_gemma":[0.99953866,0.00007956281,0.00022940643,0.000025526579,0.00007164323,0.000055312787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023208438,0.0000679403,0.000103561986,0.0005281795,0.00022797288,0.0002464238,0.00009073013,0.00009228419,0.00068316696],"category_scores_gemma":[0.0004967125,0.000055108245,0.00006550098,0.0005031109,0.00016965016,0.00015221116,0.00025033348,0.00017472,0.000048454567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058843376,0.000008130037,0.9897871,0.000028841878,0.00004013386,0.000039814964,0.0007339524,0.00023497945,0.0019230772,0.00007040099,0.00026699385,0.006807775],"study_design_scores_gemma":[4.136255e-7,0.0000029769592,0.99955314,0.0000015628965,0.0000030393794,0.000018072613,0.000081232545,0.000055978315,0.000026858203,0.000005666612,0.0002503599,7.4540117e-7],"about_ca_topic_score_codex":0.014781574,"about_ca_topic_score_gemma":0.048307266,"teacher_disagreement_score":0.9852184,"about_ca_system_score_codex":0.00019324265,"about_ca_system_score_gemma":0.00013430086,"threshold_uncertainty_score":0.02939105},"labels":[],"label_agreement":null},{"id":"W1500079129","doi":"10.1029/2012gl052395","title":"Satellite‐based estimates of reduced CO and CO<sub>2</sub> emissions due to traffic restrictions during the 2008 Beijing Olympics","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Connaught Fund; National Aeronautics and Space Administration","keywords":"Beijing; Environmental science; Air quality index; Meteorology; Troposphere; Weather Research and Forecasting Model; Carbon monoxide; Satellite; Air pollution; Greenhouse gas; Atmospheric sciences; Climatology; China; Geography; Geology; Chemistry","score_opus":0.030080824973584275,"score_gpt":0.2896113055437326,"score_spread":0.2595304805701483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1500079129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99659014,0.000056841196,0.0007190381,0.000082585706,0.0000074493114,0.000007152689,0.00093407463,0.0000437388,0.0015589126],"genre_scores_gemma":[0.99824214,0.000043103533,0.00031462358,0.000012607057,0.0000049554947,0.000009490847,0.0010229867,0.0000052791584,0.00034482926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990344,0.000011407253,0.0000072440207,0.000023713503,0.00003454578,0.000019624924],"domain_scores_gemma":[0.9998654,0.000012847164,0.000053286487,0.0000109190005,0.00004158624,0.000015920661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013591847,0.00035438733,0.00014249135,0.00038994366,0.00019880592,0.00033123663,0.00022883371,0.0003583856,0.0007572774],"category_scores_gemma":[0.00034985325,0.00018341764,0.00021299212,0.0004063137,0.00018920058,0.00030522872,0.00022557695,0.0002502211,0.00015657007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021934607,0.000094341725,0.88864875,0.00009475903,0.0002282568,0.0002679714,0.00015044512,0.068651736,0.024563465,0.00049619155,0.0020339158,0.014550769],"study_design_scores_gemma":[0.000012038375,0.000032714335,0.9728204,0.0000048080833,0.00003784358,0.00002642603,0.00007074482,0.02165761,0.0038631388,0.0000942042,0.0013698451,0.000010246744],"about_ca_topic_score_codex":0.04855286,"about_ca_topic_score_gemma":0.06587682,"teacher_disagreement_score":0.04855286,"about_ca_system_score_codex":0.0008641878,"about_ca_system_score_gemma":0.00033399474,"threshold_uncertainty_score":0.09654051},"labels":[],"label_agreement":null},{"id":"W1500733121","doi":"10.1029/2012gl053320","title":"Global <i>M</i><sub>2</sub> internal tide and its seasonal variability from high resolution ocean circulation and tide modeling","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; University of Victoria","funders":"Deutsche Forschungsgemeinschaft; Deutsches Klimarechenzentrum","keywords":"Internal tide; Baroclinity; Barotropic fluid; Climatology; Altimeter; Forcing (mathematics); Internal wave; Geology; Ocean current; Ocean surface topography; Sea-surface height; Drifter; Wind stress; Environmental science; Oceanography; Sea surface temperature; Geodesy; Lagrangian; Physics","score_opus":0.021066410638641318,"score_gpt":0.24828652438073692,"score_spread":0.2272201137420956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1500733121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.966088,0.00018436887,0.02176578,0.00030350563,0.00002602743,0.000022411705,0.0019081724,0.00041289203,0.009288725],"genre_scores_gemma":[0.9922415,0.00015810912,0.0052268025,0.000026231668,0.000009712236,0.000022899074,0.0014401842,0.000057906956,0.0008165984],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999944,0.000019488616,0.0000029217858,0.000010908586,0.000012373137,0.000010258825],"domain_scores_gemma":[0.9998882,0.0000454728,0.000017623806,0.000019512037,0.000016760094,0.000012326149],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017234481,0.000386332,0.00026433283,0.00017925806,0.00016930483,0.0006462627,0.00032656433,0.0004376355,0.0010982937],"category_scores_gemma":[0.00053337193,0.00028080578,0.0004259341,0.00043452712,0.00027368384,0.00043900366,0.00033563076,0.00038784381,0.00016452711],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003025,0.000022222759,0.009504167,0.000025653138,0.000038885388,0.000044432785,0.000022734901,0.9832683,0.0018743859,0.0011330458,0.0006197673,0.003416132],"study_design_scores_gemma":[0.000022259921,0.000021099806,0.0081801675,0.0000058025184,0.000021951586,0.000013743371,0.0000150665,0.98971176,0.0005189906,0.00067193154,0.0008083385,0.000008925209],"about_ca_topic_score_codex":0.017452424,"about_ca_topic_score_gemma":0.017886275,"teacher_disagreement_score":0.017452424,"about_ca_system_score_codex":0.00054038485,"about_ca_system_score_gemma":0.0005156624,"threshold_uncertainty_score":0.034701645},"labels":[],"label_agreement":null},{"id":"W1505059248","doi":"10.1002/2015gl064522","title":"Stability and properties of liquid CO<sub>2</sub> at high pressure and high temperature: Implications for electrical conductivities in Earth's lower mantle","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Western Canada Research Grid","keywords":"Mantle (geology); Oxygen; Materials science; Delocalized electron; Chemical physics; Ionic bonding; Thermodynamics; Metal; Chemistry; Ion; Geology; Geophysics; Physics; Metallurgy","score_opus":0.04542808469584391,"score_gpt":0.2680440962217054,"score_spread":0.22261601152586147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505059248","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99783,0.00023729405,0.00055183354,0.00006976852,0.0000031977142,0.0000024443416,0.00006916077,0.000023762865,0.0012124475],"genre_scores_gemma":[0.9997894,0.000035520403,0.000061045816,0.000003355119,0.0000011431745,0.0000011229755,0.000037021957,0.0000027279839,0.000068690795],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994636,0.000005809205,0.0000022549912,0.00000969028,0.000020404103,0.000015489853],"domain_scores_gemma":[0.9999182,0.00002891225,0.000020214342,0.000009179225,0.000016336886,0.0000070278948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011407353,0.00019249713,0.00016574393,0.00023403829,0.0002487352,0.0005036677,0.00031793438,0.00026824643,0.0012439508],"category_scores_gemma":[0.00032564005,0.00011809789,0.00014283007,0.00021888538,0.0006004588,0.00037272155,0.0003014334,0.00021199328,0.00013328598],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082746777,0.00014792745,0.030768365,0.00044257127,0.00009940883,0.00074472633,0.00041373292,0.05914922,0.88431585,0.012348274,0.0005932608,0.010149201],"study_design_scores_gemma":[0.00011441594,0.00050894346,0.052099485,0.000034137563,0.000089857676,0.00046062752,0.000559754,0.36571214,0.5698726,0.007923627,0.0025520448,0.00007233176],"about_ca_topic_score_codex":0.0014262674,"about_ca_topic_score_gemma":0.00061777537,"teacher_disagreement_score":0.0014262674,"about_ca_system_score_codex":0.00032883717,"about_ca_system_score_gemma":0.00019120309,"threshold_uncertainty_score":0.0041614175},"labels":[],"label_agreement":null},{"id":"W1505080555","doi":"10.1029/2010gl044296","title":"Coriolis forces influence the secondary circulation of gravity currents flowing in large‐scale sinuous submarine channel systems","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Natural Environment Research Council; University of Leeds","keywords":"Centrifugal force; Secondary circulation; Geology; Circulation (fluid dynamics); Mechanics; Physics; Throughflow; Channel (broadcasting); Turbidity current; RADIUS; Vortex; Flow (mathematics); Geomorphology","score_opus":0.021782203475387073,"score_gpt":0.274791508685571,"score_spread":0.25300930521018394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505080555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99898607,0.000026660653,0.00019079121,0.000016929323,0.0000021055876,0.0000021209546,0.0000147808105,0.000011651821,0.00074879616],"genre_scores_gemma":[0.9998468,0.000016264554,0.00006679,0.000002338178,0.0000014581544,0.0000010042951,0.0000068298123,0.0000023046011,0.00005614304],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999224,0.0000148220615,0.000004265872,0.000015146579,0.000012397981,0.000030954972],"domain_scores_gemma":[0.99964285,0.000102915605,0.00008445464,0.000020737594,0.00004400083,0.000105084655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013602583,0.00021308941,0.00025449417,0.00035911234,0.0004412006,0.0006739599,0.00012963502,0.0001287445,0.00094579655],"category_scores_gemma":[0.0006299282,0.00018577317,0.00016607836,0.00019493223,0.00061516603,0.00022943472,0.0003900331,0.00017852425,0.00009902347],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011445398,0.00015211635,0.41804317,0.000112475056,0.00011698433,0.0006403519,0.0014300119,0.027523892,0.51419175,0.0032706507,0.0008347643,0.03253923],"study_design_scores_gemma":[0.000084642335,0.00022411747,0.9282306,0.000010754663,0.000059121554,0.00013372893,0.0005210537,0.057401367,0.011283423,0.0012092605,0.0007958425,0.0000461224],"about_ca_topic_score_codex":0.013274462,"about_ca_topic_score_gemma":0.014066305,"teacher_disagreement_score":0.013274462,"about_ca_system_score_codex":0.00055445824,"about_ca_system_score_gemma":0.0005172389,"threshold_uncertainty_score":0.026394367},"labels":[],"label_agreement":null},{"id":"W1505201697","doi":"10.1029/2010gl043706","title":"Eastern boreal North American wildfire risk of the past 7000 years: A model‐data comparison","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec en Abitibi-Témiscamingue; Canadian Forest Service","funders":"Centre National de la Recherche Scientifique","keywords":"Climatology; Boreal; Environmental science; Taiga; Fire regime; Physical geography; Holocene; Climate change; Precipitation; Paleoclimatology; Geology; Geography; Meteorology; Oceanography; Ecosystem; Archaeology","score_opus":0.02482871405567791,"score_gpt":0.2968306799312224,"score_spread":0.2720019658755445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505201697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976417,0.00006158647,0.00037353233,0.000029045594,0.0000034630123,0.00000252597,0.0010091352,0.0000551745,0.00082395785],"genre_scores_gemma":[0.99758255,0.000041367155,0.00044235188,0.00000803093,0.000002209932,0.000004478864,0.0017524787,0.000013190844,0.00015323018],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998648,0.000038979553,0.0000091907,0.000052366555,0.000017681577,0.00001699284],"domain_scores_gemma":[0.9997168,0.00010229773,0.00005640389,0.00003977554,0.000052667798,0.000032084867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005661122,0.00034577117,0.0002617138,0.00044017093,0.00021739388,0.0005488877,0.00044085959,0.00030508035,0.0010943803],"category_scores_gemma":[0.00070739386,0.00019215437,0.00047289702,0.00051949103,0.00021625252,0.00043614957,0.00019717694,0.0001900471,0.00016780132],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071118993,0.00018033534,0.5500233,0.000058950263,0.00038459068,0.00014956215,0.0001978165,0.43005645,0.0010216848,0.0006996423,0.0018191612,0.014697282],"study_design_scores_gemma":[0.00009030146,0.00023219449,0.5311244,0.000018581486,0.00012105816,0.000285148,0.00034314816,0.46354923,0.00094186596,0.0006465598,0.0025838555,0.00006360109],"about_ca_topic_score_codex":0.06238498,"about_ca_topic_score_gemma":0.07977453,"teacher_disagreement_score":0.93761504,"about_ca_system_score_codex":0.00064840936,"about_ca_system_score_gemma":0.0003659945,"threshold_uncertainty_score":0.12404376},"labels":[],"label_agreement":null},{"id":"W1505774726","doi":"10.1029/2011gl047936","title":"Turbulent nitrate fluxes in the Amundsen Gulf during ice‐covered conditions","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; GDG Environnement; Université de Sherbrooke; Fisheries and Oceans Canada; Université du Québec à Rimouski","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Eddy diffusion; Thermal diffusivity; Nitrate; Flux (metallurgy); Atmospheric sciences; Turbulence; Oceanography; Environmental science; Geology; Meteorology; Chemistry; Physics; Thermodynamics","score_opus":0.046032353141673664,"score_gpt":0.275291457554278,"score_spread":0.2292591044126043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1505774726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998068,0.00001783544,0.000008088658,0.0000057503353,0.0000012072708,3.7905588e-7,0.00006112243,9.1618267e-7,0.00009780499],"genre_scores_gemma":[0.9994659,0.00004026358,0.00006150194,0.00000830581,0.0000019469926,0.000003072854,0.0003258986,0.0000018292066,0.00009142183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.000014070701,0.00001544919,0.000034019107,0.000024745183,0.000026545755],"domain_scores_gemma":[0.99985445,0.000029825533,0.000045201687,0.000007683799,0.00003312455,0.000029688239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026902504,0.0003590536,0.00032138874,0.00054347486,0.00044119766,0.00059197855,0.00016380235,0.0003533897,0.000246215],"category_scores_gemma":[0.0005154445,0.00028315812,0.00020423002,0.00052983814,0.0003588469,0.00040565536,0.0005191883,0.00021697662,0.000069605885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011612503,0.00010234368,0.911712,0.000051696217,0.00013834782,0.0008030114,0.0017207884,0.0038500186,0.07142011,0.00017361181,0.0003039277,0.008562951],"study_design_scores_gemma":[0.00001780768,0.000085716616,0.9954385,0.000009011334,0.00001338637,0.000064673855,0.00034791292,0.0019495657,0.001684306,0.000036511745,0.00034149666,0.000011000118],"about_ca_topic_score_codex":0.028172707,"about_ca_topic_score_gemma":0.044215754,"teacher_disagreement_score":0.028172707,"about_ca_system_score_codex":0.0010069784,"about_ca_system_score_gemma":0.00038241182,"threshold_uncertainty_score":0.05601746},"labels":[],"label_agreement":null},{"id":"W1506217675","doi":"10.1002/grl.50275","title":"Deep‐sea nutrient loss inferred from the marine dissolved N<sub>2</sub>/Ar ratio","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Abyssal zone; Benthic zone; Oceanography; Denitrification; Subarctic climate; Environmental science; Deep sea; Geology; Water mass; Nutrient; Nitrogen; Ecology; Chemistry","score_opus":0.017955116696096337,"score_gpt":0.23466411636342877,"score_spread":0.21670899966733242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1506217675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984211,0.0000761127,0.00032235996,0.000014676935,0.0000018950258,0.0000013369792,0.00036835598,0.000021279473,0.0007728679],"genre_scores_gemma":[0.9991399,0.000050110604,0.00023548304,0.0000070237375,0.0000015379699,0.0000019998113,0.00039199612,0.0000041803446,0.00016771567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993014,0.00000792558,0.0000064030396,0.000018334427,0.000027045176,0.000010102411],"domain_scores_gemma":[0.9998074,0.000040019087,0.000056719993,0.000018936194,0.000050993178,0.000025952113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018828241,0.00033104056,0.00020330714,0.00053211366,0.00015632884,0.00045612437,0.00021336958,0.00022646069,0.00044520592],"category_scores_gemma":[0.0005221101,0.00024125143,0.00015099139,0.00042539058,0.00022725691,0.00036782984,0.00031539993,0.00022673055,0.00019925094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047522885,0.000027572878,0.93877035,0.000045553123,0.00007234108,0.00012237288,0.00008725859,0.0045444346,0.048954006,0.00012636062,0.00015478309,0.0066197473],"study_design_scores_gemma":[0.000012909142,0.00004839892,0.9810992,0.0000052770706,0.000022017655,0.000055231838,0.00006526359,0.0094890455,0.008651413,0.00013080939,0.0004116599,0.00000875735],"about_ca_topic_score_codex":0.02546545,"about_ca_topic_score_gemma":0.023512457,"teacher_disagreement_score":0.02546545,"about_ca_system_score_codex":0.00063356454,"about_ca_system_score_gemma":0.00020479764,"threshold_uncertainty_score":0.050634444},"labels":[],"label_agreement":null},{"id":"W1507407018","doi":"10.1029/2012gl053761","title":"Relation of substorm pre‐onset arc to large‐scale field‐aligned current distribution","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Substorm; Arc (geometry); Geology; Geophysics; Physics; Magnetic field; Magnetosphere; Geometry","score_opus":0.015004807484402605,"score_gpt":0.30804704599578525,"score_spread":0.29304223851138267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1507407018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99747306,0.000068730944,0.0003867718,0.00001882513,0.0000033574743,0.0000074849713,0.00019747458,0.000061171384,0.0017831955],"genre_scores_gemma":[0.9991806,0.000032095715,0.00023154404,0.000006193904,0.000007500717,0.000004821353,0.00025630076,0.00000763577,0.00027324763],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994993,0.0000030696253,0.0000032057094,0.000017351811,0.000010454922,0.00001596201],"domain_scores_gemma":[0.9994831,0.00008367199,0.000168292,0.000031420925,0.00015732112,0.00007622971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006559918,0.00007596609,0.00013211163,0.0006514231,0.00018401621,0.00033493797,0.000113605995,0.00013067643,0.0018386198],"category_scores_gemma":[0.00055562897,0.00009948344,0.00007890557,0.0003743953,0.0001518292,0.00024016564,0.0001924173,0.00018716925,0.00020991072],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018539597,0.000036843725,0.8822504,0.000031997264,0.000027922511,0.0002673269,0.00027769327,0.0006272621,0.103594944,0.00017716286,0.0003635087,0.012159667],"study_design_scores_gemma":[0.0000015452404,0.000008967921,0.99813074,0.0000011700429,0.0000024125716,0.00007647482,0.000035460766,0.00029401388,0.001239791,0.000018255536,0.00018964776,0.0000015117024],"about_ca_topic_score_codex":0.006716185,"about_ca_topic_score_gemma":0.011362089,"teacher_disagreement_score":0.006716185,"about_ca_system_score_codex":0.00029059744,"about_ca_system_score_gemma":0.00012742108,"threshold_uncertainty_score":0.013354182},"labels":[],"label_agreement":null},{"id":"W1507410518","doi":"10.1029/2003gl019299","title":"Comparison of the Odin/OSIRIS stratospheric ozone profiles with coincident POAM III and ozonesonde measurements","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; Trent University; University of Saskatchewan","funders":"National Research Council Canada; Centre National d’Etudes Spatiales; Smithsonian Astrophysical Observatory; Tekes; Canadian Space Agency; Smithsonian Institution","keywords":"Osiris; Radiance; Ozone; Environmental science; Atmospheric sciences; Stratosphere; Ozone layer; Meteorology; Remote sensing; Geography; Geology","score_opus":0.0620825123990722,"score_gpt":0.3130518181324546,"score_spread":0.2509693057333824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1507410518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99757594,0.000029564113,0.00070625567,0.00000917232,0.0000048275206,0.0000063385132,0.0010225424,0.000021101054,0.00062428275],"genre_scores_gemma":[0.99450785,0.000032676435,0.0007143281,0.000008132791,0.000008150122,0.000011205691,0.004441057,0.000010969896,0.00026573596],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966395,0.000067650755,0.000030995856,0.000083957246,0.00010287068,0.000050603514],"domain_scores_gemma":[0.9991115,0.00021735425,0.00024290459,0.00010102842,0.00027032534,0.00005693492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071876333,0.00020273145,0.00018525189,0.0008085334,0.0002164324,0.00041346037,0.00017133009,0.00014684153,0.00055325305],"category_scores_gemma":[0.0021337944,0.0001326834,0.00018166043,0.0011138789,0.00012544954,0.0002755853,0.00041070682,0.00016330315,0.00020476876],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082086714,0.00010902192,0.9495887,0.000043450127,0.00022743628,0.00012354275,0.0002567319,0.0067342846,0.015355604,0.0002806051,0.0010522496,0.02540743],"study_design_scores_gemma":[0.00001086586,0.00008566817,0.9941684,0.0000027313733,0.000025597936,0.00004569387,0.00011555232,0.0031659703,0.0015121822,0.000048232578,0.0008131482,0.0000060243565],"about_ca_topic_score_codex":0.0064533465,"about_ca_topic_score_gemma":0.0070460318,"teacher_disagreement_score":0.0064533465,"about_ca_system_score_codex":0.00021988797,"about_ca_system_score_gemma":0.00021135651,"threshold_uncertainty_score":0.012831569},"labels":[],"label_agreement":null},{"id":"W1507506485","doi":"10.1002/2015gl064541","title":"The impact of stored solar heat on Arctic sea ice growth","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Mixed layer; Environmental science; Atmospheric sciences; Entrainment (biomusicology); Sea ice thickness; Sea ice growth processes; Arctic ice pack; Temperature salinity diagrams; Geology; Salinity; Oceanography; Climatology","score_opus":0.03751032916307117,"score_gpt":0.3012954725899036,"score_spread":0.2637851434268324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1507506485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998845,0.00013071646,0.000088353096,0.000020792106,0.0000045527295,0.0000011733349,0.00020657973,0.000005397948,0.00069734635],"genre_scores_gemma":[0.99959177,0.000049255774,0.00003480275,0.000005598867,0.000002780708,0.0000014704567,0.00013693215,0.00000398994,0.0001735451],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999329,0.00001043507,0.0000044798617,0.0000131616725,0.000018686127,0.00002022324],"domain_scores_gemma":[0.99966264,0.00012798468,0.000041734766,0.000027062939,0.000087849985,0.00005279086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029867204,0.00021039482,0.00019021316,0.00022114613,0.00033152822,0.00060079375,0.00018804792,0.00017670993,0.00089840917],"category_scores_gemma":[0.00063922093,0.00012084999,0.00018867436,0.00017121772,0.00023837233,0.00029616203,0.0003132008,0.00020792709,0.00012357922],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018693898,0.00011395458,0.6708386,0.00017118701,0.00020105978,0.00058592734,0.0003477081,0.027525239,0.26569608,0.0006972973,0.000541467,0.03141207],"study_design_scores_gemma":[0.000010933523,0.000106697276,0.97010124,0.000009806675,0.000025187197,0.000078016594,0.0001562611,0.008117403,0.02072236,0.00013216709,0.0005304723,0.000009408601],"about_ca_topic_score_codex":0.017172154,"about_ca_topic_score_gemma":0.023821857,"teacher_disagreement_score":0.017172154,"about_ca_system_score_codex":0.0007423688,"about_ca_system_score_gemma":0.0003463969,"threshold_uncertainty_score":0.0341444},"labels":[],"label_agreement":null},{"id":"W1508495092","doi":"10.1029/2002gl016820","title":"Transport of forest fire smoke above the tropopause by supercell convection","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":275,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Canadian Forest Service; Goddard Space Flight Center; National Oceanic and Atmospheric Administration","keywords":"Troposphere; Tropopause; Stratosphere; Atmospheric sciences; Taiga; Environmental science; Boreal; Climatology; Smoke; Convection; Geology; Meteorology; Geography","score_opus":0.024554808456619125,"score_gpt":0.2624393305264677,"score_spread":0.23788452206984856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1508495092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972314,0.0002674324,0.00048000077,0.00011030745,0.000013187797,0.000005466531,0.00007270617,0.00003330061,0.0017861826],"genre_scores_gemma":[0.9994342,0.00010009907,0.00017781767,0.000009245735,0.0000053951803,0.0000011356392,0.000041915915,0.0000023692126,0.00022796883],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.0000037000218,0.0000015397062,0.0000065991103,0.000007794837,0.000028214465],"domain_scores_gemma":[0.99990463,0.000014284671,0.000020734778,0.000013687753,0.000018084213,0.000028475702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008051545,0.00018197717,0.00012511505,0.00028029247,0.00053814054,0.00059976475,0.0001703353,0.00017508374,0.0013080525],"category_scores_gemma":[0.00022493457,0.000108348664,0.00020011188,0.00016452302,0.00016097641,0.00030273086,0.0004581063,0.00021539461,0.0001519797],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012680759,0.00015535575,0.4063247,0.00011632546,0.00013882307,0.0019330566,0.0010141873,0.020186266,0.51625913,0.010523431,0.0027170547,0.039363466],"study_design_scores_gemma":[0.00036312934,0.000701333,0.5370248,0.000058367077,0.00018303977,0.0013558198,0.0023299174,0.25691682,0.1785238,0.009634652,0.012808421,0.00009978],"about_ca_topic_score_codex":0.033479147,"about_ca_topic_score_gemma":0.015101418,"teacher_disagreement_score":0.033479147,"about_ca_system_score_codex":0.0005601403,"about_ca_system_score_gemma":0.0004669591,"threshold_uncertainty_score":0.06656855},"labels":[],"label_agreement":null},{"id":"W1509587216","doi":"10.1029/2011gl050405","title":"Changes in seasonal land precipitation during the latter twentieth‐century","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Climatology; Precipitation; Environmental science; Boreal; Latitude; Forcing (mathematics); Climate model; Climate change; Atmospheric sciences; Meteorology; Geology; Geography","score_opus":0.03599985523483132,"score_gpt":0.30214541460105065,"score_spread":0.2661455593662193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1509587216","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99347126,0.0003158672,0.0006739262,0.00022613636,0.000024623387,0.000005083528,0.0039037867,0.00005935331,0.0013198785],"genre_scores_gemma":[0.995713,0.00042883292,0.00044493485,0.000031615946,0.000013305005,0.000007629791,0.002909834,0.000009238468,0.00044164583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999902,0.000011615905,0.000008891542,0.000036704158,0.000019984956,0.00002068308],"domain_scores_gemma":[0.999821,0.00002397607,0.00008396835,0.000021702777,0.000031904212,0.000017360333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025540302,0.00018492239,0.00013016592,0.0004555805,0.00022855615,0.0006353983,0.00021346277,0.00020905363,0.0009136913],"category_scores_gemma":[0.0009770832,0.00010907857,0.00025013904,0.0011690942,0.00014279195,0.00041206426,0.0003672284,0.00029350794,0.00009640292],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024434336,0.00007024658,0.889357,0.00012524144,0.00042180036,0.0002673892,0.00025836396,0.06802728,0.004915989,0.0018893037,0.0032438706,0.031179136],"study_design_scores_gemma":[0.000032437427,0.00004192994,0.96048194,0.000019461297,0.000095942705,0.00015671308,0.0001286942,0.029379755,0.0017085272,0.00047227356,0.0074642557,0.000018044542],"about_ca_topic_score_codex":0.034744747,"about_ca_topic_score_gemma":0.048622303,"teacher_disagreement_score":0.034744747,"about_ca_system_score_codex":0.0006455449,"about_ca_system_score_gemma":0.00028217526,"threshold_uncertainty_score":0.069085},"labels":[],"label_agreement":null},{"id":"W1510071287","doi":"10.1029/2011gl049675","title":"Monitoring the F-region peak electron density using HF backscatter interferometry","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Interferometry; Backscatter (email); Electron density; Remote sensing; Electron; Geology; Optics; Environmental science; Physics; Geodesy; Nuclear physics; Telecommunications; Computer science","score_opus":0.055042078200625295,"score_gpt":0.30863741375411335,"score_spread":0.25359533555348807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1510071287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95167845,0.0006007248,0.043755997,0.0000569936,0.000021896427,0.00003458624,0.0010619316,0.0003918598,0.0023976432],"genre_scores_gemma":[0.9357837,0.0003368228,0.062337145,0.000033298107,0.000040558803,0.000022392482,0.0010373101,0.000035531044,0.00037329952],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99988306,0.000019031011,0.000005507737,0.000030799838,0.00004484984,0.000016826807],"domain_scores_gemma":[0.9997422,0.00007035533,0.00006710606,0.000024191035,0.000075221185,0.000020988851],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002919081,0.0003537295,0.00023111147,0.00091733143,0.00022477379,0.00024205136,0.00038097615,0.0003393689,0.00040562733],"category_scores_gemma":[0.0006435304,0.000117992306,0.00011048869,0.0005198365,0.00013839957,0.0005303015,0.00029510033,0.0001529256,0.00018414645],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063332863,0.00019063866,0.3901542,0.00014499588,0.00012716888,0.00026438455,0.000231739,0.010313119,0.4546315,0.00050357607,0.0017703627,0.14103493],"study_design_scores_gemma":[0.00007672386,0.00045071446,0.64240694,0.000029551655,0.000108006636,0.0008621735,0.00015731038,0.17162848,0.18071666,0.00062516454,0.0028591796,0.00007904934],"about_ca_topic_score_codex":0.0018788663,"about_ca_topic_score_gemma":0.0052562407,"teacher_disagreement_score":0.0018788663,"about_ca_system_score_codex":0.00011559724,"about_ca_system_score_gemma":0.00012719432,"threshold_uncertainty_score":0.0037358403},"labels":[],"label_agreement":null},{"id":"W1510600477","doi":"10.1002/grl.50704","title":"Relative changes in CO emissions over megacities based on observations from space","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Megacity; Environmental science; Troposphere; Atmospheric sciences; Air pollution; Meteorology; Emission inventory; Pollutant; Air pollutants; Pollution; Air quality index; Geography; Geology","score_opus":0.05704461944620923,"score_gpt":0.2894995772549972,"score_spread":0.23245495780878797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1510600477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947907,0.00015980184,0.0016182415,0.0000307981,0.0000069532093,0.000008647923,0.0019844968,0.000072046954,0.0013283336],"genre_scores_gemma":[0.9959246,0.000115872965,0.0015228229,0.0000059194786,0.000008313102,0.000016920341,0.0022135729,0.000011940081,0.00018008288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997677,0.00003347403,0.000013868508,0.00007788084,0.00008054645,0.00002648999],"domain_scores_gemma":[0.99936646,0.00012810204,0.00027788198,0.00007692807,0.00012145914,0.000029086434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023146055,0.00030606065,0.00019220258,0.0019719377,0.00016949332,0.00048626654,0.0002694373,0.00024390889,0.00045283505],"category_scores_gemma":[0.0010191144,0.00012364522,0.00023459166,0.002783653,0.00017323498,0.00044012477,0.00049198227,0.00023321655,0.00014547032],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016273913,0.00003962746,0.95508796,0.0000631884,0.00026473374,0.00013018571,0.00018715464,0.012178031,0.007447594,0.00018677075,0.00054688525,0.023705225],"study_design_scores_gemma":[0.0000037485809,0.00001930262,0.99101675,0.0000049447585,0.00003306466,0.000045545843,0.000109776745,0.0062319846,0.0018845679,0.000039236806,0.00060233,0.00000867569],"about_ca_topic_score_codex":0.031788506,"about_ca_topic_score_gemma":0.051156443,"teacher_disagreement_score":0.031788506,"about_ca_system_score_codex":0.0005282034,"about_ca_system_score_gemma":0.00018158181,"threshold_uncertainty_score":0.06320691},"labels":[],"label_agreement":null},{"id":"W1511645316","doi":"10.1029/2003gl018106","title":"Stress change near the Kunlun fault before and after the Ms 8.1 Kunlun earthquake","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Geology; Seismology; Intraplate earthquake; Fault (geology); Principal stress; Stress field; Magnitude (astronomy); Stress (linguistics); Interplate earthquake; Tectonics; Petrology; Shear (geology)","score_opus":0.03568725444292759,"score_gpt":0.27342106029181346,"score_spread":0.23773380584888587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1511645316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996679,0.00002498993,0.000009536144,0.000012974931,0.0000025183488,0.0000010812046,0.000040805113,0.0000015113659,0.00023879998],"genre_scores_gemma":[0.9995074,0.000027964998,0.000016439366,0.000009455994,0.000003798355,0.000002532785,0.00015900163,7.602385e-7,0.0002725717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998963,0.0000074621303,0.000006270819,0.00002403566,0.000027954595,0.000037869922],"domain_scores_gemma":[0.9997228,0.000015864016,0.00009367945,0.000013953798,0.000075303135,0.00007837668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012393856,0.00019469911,0.00032584934,0.0006083168,0.00062834786,0.0004311446,0.00024433783,0.0004563422,0.0008437037],"category_scores_gemma":[0.0004110989,0.00021145165,0.00016822762,0.0005831148,0.00045613563,0.00031792375,0.00032480722,0.0002739112,0.00016829935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013410961,0.00024402988,0.7758832,0.0001281657,0.000094533396,0.0031346357,0.0055792555,0.0016356875,0.19232175,0.00027526915,0.00083364703,0.018528817],"study_design_scores_gemma":[0.0000056194326,0.00008197545,0.99817955,0.0000034867103,0.0000045953784,0.000057620415,0.0003115156,0.00015813211,0.00095552864,0.000017427783,0.00021825457,0.000006300781],"about_ca_topic_score_codex":0.01695269,"about_ca_topic_score_gemma":0.029160049,"teacher_disagreement_score":0.01695269,"about_ca_system_score_codex":0.00090725266,"about_ca_system_score_gemma":0.00036293504,"threshold_uncertainty_score":0.033708036},"labels":[],"label_agreement":null},{"id":"W1511742916","doi":"10.1029/2011gl048305","title":"Deep-sea observations and modeling of the 2004 Sumatra tsunami in Drake Passage","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Tide gauge; Geology; Amplitude; Tsunami wave; Seismology; Dispersion (optics); Indian ocean; Wind wave; Arrival time; Geodesy; Sea level; Oceanography; Physics","score_opus":0.11595570887898105,"score_gpt":0.28280554396478474,"score_spread":0.1668498350858037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1511742916","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841547,0.000030591753,0.0005870615,0.00005330572,0.000006670173,0.0000073333226,0.00031418342,0.000036041838,0.0005494377],"genre_scores_gemma":[0.99910563,0.000023144794,0.00037445524,0.0000067021615,0.000002465091,0.0000062097156,0.00024324626,0.0000066443245,0.00023136861],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992037,0.000018887,0.0000074250765,0.000027383967,0.000010336873,0.000015577178],"domain_scores_gemma":[0.99980944,0.000051736526,0.000043228556,0.000022926613,0.000036163547,0.000036497826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018605574,0.00061305834,0.00029543444,0.0003600068,0.00045103967,0.00072390697,0.00061670906,0.00076631835,0.0008771189],"category_scores_gemma":[0.0007775309,0.00041675562,0.00041360856,0.00035278217,0.00038593425,0.00051439024,0.00038799952,0.0004819106,0.00019914951],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016852254,0.00009630656,0.06606921,0.000027411294,0.000072564195,0.00032270228,0.00011329195,0.9258993,0.0039667664,0.00031136844,0.00035940125,0.002593092],"study_design_scores_gemma":[0.000039050978,0.00006819704,0.043136287,0.0000059196136,0.000025693185,0.00004060454,0.0000829607,0.95560896,0.0006040172,0.00014316071,0.00022643743,0.00001869688],"about_ca_topic_score_codex":0.07435295,"about_ca_topic_score_gemma":0.051172126,"teacher_disagreement_score":0.07435295,"about_ca_system_score_codex":0.0016268921,"about_ca_system_score_gemma":0.00052259327,"threshold_uncertainty_score":0.14784032},"labels":[],"label_agreement":null},{"id":"W1512105388","doi":"10.1029/2012gl052127","title":"Scales of variability of black carbon plumes over the Pacific Ocean","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Clarendon Fund; Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Plume; Environmental science; Atmospheric sciences; Climatology; Panache; Geology; Spatial variability; Range (aeronautics); Meteorology; Geography","score_opus":0.022813478979941924,"score_gpt":0.2660669626651579,"score_spread":0.24325348368521596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512105388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994112,0.000031388656,0.00015283035,0.000010399144,6.219816e-7,0.0000016251478,0.000095784104,0.000009731545,0.00028641074],"genre_scores_gemma":[0.9996153,0.000022563278,0.00013686411,0.0000019382146,0.0000014548266,0.0000017801567,0.00017745243,0.000003027421,0.000039520746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.0000045889346,0.0000019245867,0.000014393177,0.000015820211,0.000011082881],"domain_scores_gemma":[0.99980015,0.0000650576,0.0000535283,0.000013096748,0.000039098362,0.000029170573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013747113,0.00013630057,0.00009427642,0.00056211755,0.00018781533,0.0002719121,0.0001225239,0.00013638247,0.0002526683],"category_scores_gemma":[0.0005237587,0.00012853842,0.00019462654,0.00031779349,0.00020449737,0.00026578392,0.00022777688,0.00012836474,0.00003105947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025607998,0.00007177533,0.89748883,0.00004499534,0.00019549597,0.00036330894,0.00049289525,0.015257118,0.068271674,0.0003527373,0.00033548425,0.016869595],"study_design_scores_gemma":[0.0000034541322,0.00001401545,0.99183005,0.000001924888,0.000011364138,0.000027345723,0.00004611131,0.0068479027,0.0010655216,0.00004721611,0.000099984914,0.000005138016],"about_ca_topic_score_codex":0.01646562,"about_ca_topic_score_gemma":0.012166243,"teacher_disagreement_score":0.01646562,"about_ca_system_score_codex":0.00039006304,"about_ca_system_score_gemma":0.00015678609,"threshold_uncertainty_score":0.03273952},"labels":[],"label_agreement":null},{"id":"W1512192239","doi":"10.1029/2012gl051288","title":"Retrievals of sea surface temperature fronts from SAR imagery","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Geology; Synthetic aperture radar; Remote sensing; Curl (programming language); Sea surface temperature; Wind stress; Altimeter; Gaussian; Divergence (linguistics); Image resolution; Wind speed; Meteorology; Geodesy; Climatology; Computer science; Oceanography; Geography; Artificial intelligence; Physics","score_opus":0.029195058132730597,"score_gpt":0.27824014696947685,"score_spread":0.24904508883674625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512192239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85733134,0.00046850514,0.13701652,0.00009320826,0.00004744314,0.000042206015,0.0011874243,0.0007247014,0.003088789],"genre_scores_gemma":[0.8997225,0.00041303536,0.09609095,0.0000283858,0.00007020275,0.000026323018,0.0022542977,0.0000549683,0.0013392011],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9999615,0.000003071119,0.0000021250632,0.000008158548,0.000017449358,0.000007732347],"domain_scores_gemma":[0.9999019,0.000014444926,0.000022848231,0.000012026126,0.000037328336,0.000011415918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011869592,0.0003703386,0.0001877609,0.0009478443,0.000113844464,0.00044280125,0.00014110048,0.0001758599,0.0005541333],"category_scores_gemma":[0.0003470532,0.00021554992,0.00022957631,0.0005232206,0.000121655874,0.00034187097,0.00018465916,0.0002265983,0.00029927574],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048485651,0.00015576639,0.050822925,0.00018544894,0.00009743764,0.00024596616,0.00018263182,0.07296189,0.39723018,0.0014510948,0.001816064,0.4743658],"study_design_scores_gemma":[0.000049404887,0.00015410337,0.15943427,0.000030843752,0.000060316157,0.00025803052,0.00007237414,0.74892217,0.0861551,0.0013247876,0.0034873877,0.000051296684],"about_ca_topic_score_codex":0.0025563256,"about_ca_topic_score_gemma":0.0043472336,"teacher_disagreement_score":0.0025563256,"about_ca_system_score_codex":0.00020169378,"about_ca_system_score_gemma":0.00022199644,"threshold_uncertainty_score":0.0050829053},"labels":[],"label_agreement":null},{"id":"W1512462330","doi":"10.1029/2011gl047599","title":"A 5200-year record of freshwater availability for regions in western North America fed by high-elevation runoff","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; University of Waterloo; Wilfrid Laurier University","funders":"","keywords":"Glacier; Surface runoff; Hydrology (agriculture); Climate change; Physical geography; Period (music); Holocene; Meltwater; Environmental change; Elevation (ballistics); Freshwater ecosystem; Snow; Geology; Ecosystem; Environmental science; Oceanography; Geography; Ecology; Geomorphology","score_opus":0.056521257624811305,"score_gpt":0.2827913678405976,"score_spread":0.2262701102157863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1512462330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9762329,0.00093683397,0.0003312383,0.0011331899,0.00003074971,0.000014432786,0.010313388,0.00004643657,0.010960875],"genre_scores_gemma":[0.9915657,0.0006626377,0.0003570453,0.00021643637,0.00003196376,0.000007696862,0.0039731297,0.000007781013,0.0031776475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999685,0.0000029116711,0.0000020412253,0.000010113441,0.000008445432,0.0000079466445],"domain_scores_gemma":[0.9997799,0.000008047099,0.00007071105,0.000009621019,0.00008255269,0.00004916057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000781957,0.000088024644,0.00006123045,0.00039883194,0.00038219732,0.00023114694,0.00014364904,0.00014937007,0.003542428],"category_scores_gemma":[0.0002400013,0.000054763634,0.000038981,0.000833091,0.00019606951,0.00022890136,0.00023620133,0.00014604071,0.00033719078],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000071399474,0.000043503125,0.9249505,0.00012782196,0.00006305965,0.00024723602,0.0018845076,0.00017538284,0.013712478,0.00032610673,0.018970344,0.03942771],"study_design_scores_gemma":[4.5479328e-7,0.0000048604225,0.99469584,0.0000040676473,0.0000029970192,0.000039263894,0.00025921932,0.000025062092,0.00009798357,0.000015883485,0.004852894,0.0000015587422],"about_ca_topic_score_codex":0.24961248,"about_ca_topic_score_gemma":0.68073976,"teacher_disagreement_score":0.24961248,"about_ca_system_score_codex":0.00047820222,"about_ca_system_score_gemma":0.00047256178,"threshold_uncertainty_score":0.49631917},"labels":[],"label_agreement":null},{"id":"W1513300606","doi":"10.1002/2013gl057919","title":"Are scale‐invariant stress orientations related to seismicity rates near the San Andreas fault?","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"San andreas fault; Geology; Induced seismicity; Scaling; Scale invariance; Amplitude; Seismology; Slip (aerodynamics); Magnitude (astronomy); Nonlinear system; Fault (geology); Invariant (physics); Orientation (vector space); Stress (linguistics); Geodesy; Geometry; Physics; Statistics; Mathematics; Optics","score_opus":0.031127840373387713,"score_gpt":0.29293070098900315,"score_spread":0.2618028606156154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1513300606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970054,0.00014042752,0.0015332411,0.00013220572,0.000006137361,0.0000039369456,0.00007996315,0.000022752276,0.0010760204],"genre_scores_gemma":[0.99965835,0.000064055224,0.00011961113,0.000010007268,0.000005790774,0.0000015254964,0.000030244448,0.0000037733753,0.00010652535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.000034567503,0.000015272852,0.00007144986,0.000028898377,0.000048213114],"domain_scores_gemma":[0.9979425,0.0003411145,0.0012101185,0.00018296212,0.00015437577,0.00016884605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035785176,0.00018659618,0.0002449053,0.00077193585,0.00015562995,0.00066184346,0.00026366432,0.00038877947,0.0012278851],"category_scores_gemma":[0.0032030998,0.00033827196,0.00017170787,0.00087017,0.0010713362,0.00087649806,0.00025069917,0.0002804507,0.0003326693],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001394238,0.00005085178,0.9496561,0.000050661984,0.000111007386,0.00025615707,0.0004065176,0.004172907,0.024615424,0.0018063607,0.00026114777,0.018473404],"study_design_scores_gemma":[0.0000036492795,0.000015369316,0.9955089,0.0000037352925,0.000007809892,0.00008802803,0.00013571559,0.0029038172,0.0006291779,0.0005800878,0.00011038157,0.000013311529],"about_ca_topic_score_codex":0.0055131186,"about_ca_topic_score_gemma":0.005308457,"teacher_disagreement_score":0.0055131186,"about_ca_system_score_codex":0.00035008398,"about_ca_system_score_gemma":0.0001737738,"threshold_uncertainty_score":0.010962069},"labels":[],"label_agreement":null},{"id":"W1513454981","doi":"10.1002/grl.50234","title":"Persistent sensitivity of Asian aerosol to emissions of nitrogen oxides","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Universitatea \"Lucian Blaga\" din Sibiu; National Oceanic and Atmospheric Administration; U.S. Environmental Protection Agency; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; Nitrate; Ammonium; Trace gas; Chemical transport model; Environmental chemistry; Atmospheric sciences; Population; Sulfur dioxide; NOx; Reactive nitrogen; Ammonia; Nitrogen; Nitrogen dioxide; Nitrogen oxide; Chemistry; Meteorology; Inorganic chemistry; Geography; Combustion; Physics","score_opus":0.028959902947839435,"score_gpt":0.26882683153017234,"score_spread":0.2398669285823329,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1513454981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982582,0.00002208212,0.0004528415,0.00007391038,0.000007365141,0.000004185236,0.00014377382,0.000034379686,0.0010031434],"genre_scores_gemma":[0.9995547,0.000018998162,0.00016579939,0.000015731057,0.0000020990387,0.0000024217343,0.00010949675,0.0000055850765,0.00012509657],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998672,0.000030333127,0.000010003014,0.0000361106,0.000017878107,0.00003841033],"domain_scores_gemma":[0.9995739,0.00016361279,0.00007918304,0.00004694702,0.00008311023,0.00005325084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004532114,0.0005745148,0.0003112158,0.00021344569,0.00036122004,0.0006723061,0.00050945237,0.0005868048,0.0006591424],"category_scores_gemma":[0.0010889475,0.0002908089,0.00077794923,0.0002947418,0.00042644885,0.0005416759,0.00059732795,0.00065959425,0.00007986203],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000357032,0.00016200637,0.12760653,0.00005377879,0.00026792026,0.0004785359,0.00015329682,0.8371472,0.02896926,0.0017394652,0.00042070338,0.0026443435],"study_design_scores_gemma":[0.000062201194,0.00012884772,0.038400553,0.00000692677,0.000090139736,0.000055802113,0.00015207303,0.9512869,0.008762047,0.000667712,0.00034752148,0.000039181417],"about_ca_topic_score_codex":0.077149086,"about_ca_topic_score_gemma":0.020443833,"teacher_disagreement_score":0.077149086,"about_ca_system_score_codex":0.0010329629,"about_ca_system_score_gemma":0.00083200657,"threshold_uncertainty_score":0.15340006},"labels":[],"label_agreement":null},{"id":"W1513807882","doi":"10.1029/2008gl036220","title":"Temperature and concentration feedbacks in the carbon cycle","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Positive feedback; Carbon fibers; Atmosphere (unit); Environmental science; Carbon cycle; Greenhouse gas; Negative feedback; Atmospheric sciences; Carbon dioxide; Flux (metallurgy); Coupled model intercomparison project; Range (aeronautics); Global warming; Climate change; Chemistry; Materials science; Meteorology; Climate model; Physics; Geology; Oceanography; Ecosystem","score_opus":0.008413838488422445,"score_gpt":0.2532355797008087,"score_spread":0.24482174121238623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1513807882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94447714,0.00094064174,0.035574935,0.0013578222,0.000111110654,0.000046047866,0.0002834289,0.0004137551,0.016795155],"genre_scores_gemma":[0.9974795,0.00021796969,0.0013505004,0.000033483044,0.00001502398,0.000011781654,0.000024333149,0.000027588827,0.0008398188],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981636,0.00006435468,0.0000075127223,0.000031025957,0.000045115466,0.000035598176],"domain_scores_gemma":[0.9994056,0.00037240135,0.00008299011,0.000027154416,0.00008087591,0.000030886764],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041874443,0.00047803245,0.00029643916,0.00040981703,0.000537799,0.0010335727,0.00034159143,0.00075180124,0.002584073],"category_scores_gemma":[0.002558402,0.0004446312,0.00056559907,0.00031603203,0.0007118728,0.0014951605,0.0005667398,0.00051980605,0.00017343431],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002393242,0.00007993279,0.012534312,0.000111117595,0.0000716923,0.00016339851,0.00014203484,0.8968816,0.03609428,0.039280888,0.0007747474,0.0136266565],"study_design_scores_gemma":[0.00005334298,0.0000753516,0.009108658,0.0000106403995,0.000036933223,0.000046986388,0.000042715958,0.96209234,0.005248171,0.022119004,0.001125779,0.00004012965],"about_ca_topic_score_codex":0.0075454162,"about_ca_topic_score_gemma":0.004419096,"teacher_disagreement_score":0.0075454162,"about_ca_system_score_codex":0.001520714,"about_ca_system_score_gemma":0.00056628976,"threshold_uncertainty_score":0.015002966},"labels":[],"label_agreement":null},{"id":"W1514205744","doi":"10.1029/2005gl023552","title":"Ratio of the Greenland to global temperature change: Comparison of observations and climate modeling results","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Greenland ice sheet; Climatology; Global warming; North Atlantic oscillation; Climate change; Global temperature; Environmental science; Future sea level; Global change; Temperature record; Groenlandia; GCM transcription factors; General Circulation Model; Sea surface temperature; Atlantic multidecadal oscillation; Ice sheet; Geology; Cryosphere; Oceanography; Sea ice; Ice stream","score_opus":0.12608338188798135,"score_gpt":0.3638307174965161,"score_spread":0.23774733560853473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1514205744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98954433,0.00073431944,0.0026847254,0.00015743458,0.0000138472615,0.000007817355,0.003565319,0.00035921668,0.0029329825],"genre_scores_gemma":[0.9971776,0.00018028967,0.0007853925,0.000022304594,0.000008255667,0.000006491595,0.0016387345,0.000045479243,0.00013550067],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997348,0.00008273828,0.000017327908,0.00008918542,0.000054310374,0.00002159823],"domain_scores_gemma":[0.99948716,0.00021526974,0.00012239128,0.00007801031,0.00007865912,0.000018484541],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006423861,0.00035489045,0.00021579054,0.00079421065,0.000084389605,0.00040255144,0.00023486852,0.00027433172,0.00072599476],"category_scores_gemma":[0.0012806052,0.00013024526,0.00047867882,0.0012798079,0.0001430783,0.00050139,0.00019205401,0.00015367269,0.0002640583],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059209694,0.00008453711,0.79467785,0.0002756591,0.00092068786,0.00021920359,0.00030499155,0.11726085,0.012600872,0.0011848526,0.002960214,0.06891822],"study_design_scores_gemma":[0.000023020651,0.000032932912,0.9284273,0.000024016601,0.00010353314,0.00010811538,0.00011753063,0.06276799,0.0048642415,0.00047789872,0.003025852,0.000027670685],"about_ca_topic_score_codex":0.01896166,"about_ca_topic_score_gemma":0.018542342,"teacher_disagreement_score":0.01896166,"about_ca_system_score_codex":0.0006899001,"about_ca_system_score_gemma":0.00023488843,"threshold_uncertainty_score":0.03770262},"labels":[],"label_agreement":null},{"id":"W1514229750","doi":"10.1002/grl.50303","title":"Lower tropospheric ozone at northern midlatitudes: Changing seasonal cycle","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Park Service; European Commission","keywords":"Middle latitudes; Environmental science; Atmospheric sciences; Troposphere; Climatology; Annual cycle; Abundance (ecology); Tropospheric ozone; Latitude; Climate change; Ozone depletion; Stratosphere; Geology; Oceanography; Ecology; Biology","score_opus":0.01734333670412752,"score_gpt":0.2545088996867434,"score_spread":0.23716556298261587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1514229750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99726474,0.00030356128,0.0001997351,0.00021831402,0.000009971908,0.0000035678452,0.0004980249,0.000024127266,0.0014779622],"genre_scores_gemma":[0.9993742,0.000102245125,0.00007667854,0.000024688587,0.000005695562,0.0000016286886,0.00022096638,0.0000027797398,0.00019122918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999966,0.000005458282,0.0000017980049,0.0000106095085,0.000006494078,0.00000970987],"domain_scores_gemma":[0.99984443,0.000024217285,0.000043330616,0.000013852057,0.00003824949,0.000035814555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016923637,0.00009138178,0.00020242296,0.00029060603,0.00017626162,0.00032851347,0.00015599144,0.00022076437,0.0009856231],"category_scores_gemma":[0.00033781512,0.000088001645,0.00015119812,0.00042789732,0.00016383233,0.00022220756,0.00017922114,0.00015417069,0.00015982123],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036605916,0.0000639284,0.9386988,0.000062094026,0.0000968317,0.00022026364,0.0004961635,0.0030954527,0.036846258,0.00063329807,0.0015080177,0.017912885],"study_design_scores_gemma":[0.0000027026072,0.000011654289,0.997209,0.0000031156846,0.000008189055,0.000025271018,0.00005149543,0.0015299914,0.00043461352,0.00009022934,0.0006305698,0.0000031547963],"about_ca_topic_score_codex":0.01962201,"about_ca_topic_score_gemma":0.029845279,"teacher_disagreement_score":0.01962201,"about_ca_system_score_codex":0.00035675155,"about_ca_system_score_gemma":0.00018110043,"threshold_uncertainty_score":0.03901559},"labels":[],"label_agreement":null},{"id":"W1516486789","doi":"10.1029/2007gl032324","title":"Urban heat island in the subsurface","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":191,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Urban heat island; Environmental science; Climate change; Work (physics); Climatology; Subsurface flow; Current (fluid); Geology; Meteorology; Groundwater; Geography; Oceanography","score_opus":0.02698459601855709,"score_gpt":0.3008962738650093,"score_spread":0.2739116778464522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1516486789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99729663,0.00042232155,0.00035157066,0.00014409551,0.000006492778,0.0000017143501,0.000053526564,0.000009292665,0.0017143168],"genre_scores_gemma":[0.99972206,0.00008911175,0.000050886374,0.0000061647224,0.0000028927109,5.6547987e-7,0.00001607723,0.0000012455653,0.00011097279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999442,0.000017638586,0.0000013022252,0.000007827955,0.000006855838,0.000022055423],"domain_scores_gemma":[0.99989915,0.000017865961,0.000033846845,0.000011719845,0.000022523864,0.000014899438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006270189,0.00009751964,0.00014205507,0.00015364558,0.00015109566,0.0003812074,0.000054265558,0.000099722034,0.0010608854],"category_scores_gemma":[0.0002470724,0.000048832953,0.00008453409,0.00031695986,0.00028381572,0.00024096269,0.00036790472,0.00013667527,0.00008413472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056453544,0.00013391601,0.8318597,0.00022603791,0.00014838751,0.0009869405,0.0023545495,0.0071907113,0.054391704,0.007874701,0.002189403,0.09207935],"study_design_scores_gemma":[0.000005906592,0.00011943739,0.9854401,0.00002585228,0.0000464445,0.00025125913,0.0024275435,0.001848048,0.0024096332,0.0036807628,0.0037341567,0.000010762907],"about_ca_topic_score_codex":0.00478269,"about_ca_topic_score_gemma":0.008151208,"teacher_disagreement_score":0.00478269,"about_ca_system_score_codex":0.00015813406,"about_ca_system_score_gemma":0.0001887924,"threshold_uncertainty_score":0.009509683},"labels":[],"label_agreement":null},{"id":"W1517380424","doi":"10.1029/2004gl021128","title":"Evidence of vertical transport of carbon monoxide from Measurements of Pollution in the Troposphere (MOPITT)","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Troposphere; Atmospheric sciences; Plume; Environmental science; Carbon monoxide; Convection; Panache; Latitude; Climatology; Mixing ratio; Deep convection; Monsoon; Pollution; Geology; Meteorology; Chemistry; Geography","score_opus":0.063245105495117,"score_gpt":0.2881748223670255,"score_spread":0.22492971687190852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1517380424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975968,0.0001591753,0.00045730596,0.00004017974,0.00000539038,0.00000575143,0.0010354628,0.000038169623,0.0006618502],"genre_scores_gemma":[0.9973562,0.000110363864,0.00082937453,0.0000144104315,0.000006383403,0.0000060961297,0.0015389858,0.0000055292458,0.00013272036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984384,0.000012690558,0.00000865666,0.000039036397,0.00006611444,0.000029541625],"domain_scores_gemma":[0.99974483,0.000037017126,0.00009525131,0.00002198486,0.00007871978,0.00002211395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011287787,0.0002537709,0.00013252332,0.00051724334,0.00024378939,0.0003103592,0.00016186095,0.00033114853,0.00030993755],"category_scores_gemma":[0.0004863785,0.00018144873,0.00011081345,0.0008306709,0.00014105543,0.00023591369,0.00028252765,0.000258933,0.00009728233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037644876,0.00008063849,0.68115485,0.0001367076,0.00016927291,0.00066858705,0.00028188768,0.0013202124,0.2979293,0.00019399406,0.0006457983,0.01704233],"study_design_scores_gemma":[0.000008792307,0.0000728977,0.9729476,0.0000069568932,0.000027772028,0.0002542447,0.00004644601,0.0022029015,0.023335349,0.000041481748,0.0010468353,0.000008733533],"about_ca_topic_score_codex":0.0122130895,"about_ca_topic_score_gemma":0.016924446,"teacher_disagreement_score":0.0122130895,"about_ca_system_score_codex":0.00024949454,"about_ca_system_score_gemma":0.00018872366,"threshold_uncertainty_score":0.024284005},"labels":[],"label_agreement":null},{"id":"W1517433839","doi":"10.1029/2003gl019088","title":"A coupled sheet‐conduit mechanism for jökulhlaup propagation","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; European Commission; Háskóli Íslands; Landsvirkjun; National Science Foundation","keywords":"Electrical conduit; Flood myth; Geology; Glacier; Hydrology (agriculture); Geomorphology; Greenland ice sheet; Archaeology; Geotechnical engineering; Geography","score_opus":0.05855874063187926,"score_gpt":0.2968276585996325,"score_spread":0.23826891796775324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1517433839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89015925,0.00041487836,0.097285286,0.000551892,0.00012179234,0.000047939306,0.00012793326,0.00075082434,0.010540112],"genre_scores_gemma":[0.9949032,0.00012424243,0.0030164062,0.000026108155,0.000019483574,0.00002210987,0.000025604106,0.00001772361,0.001845061],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999608,0.000005643716,0.000002539028,0.000013985554,0.0000066899456,0.0000104276905],"domain_scores_gemma":[0.9998394,0.000047375222,0.000034808356,0.000020813839,0.000020843318,0.0000367027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013768574,0.00020854796,0.0001757791,0.00021549239,0.00050672743,0.00077866646,0.0005987004,0.000493033,0.0016872999],"category_scores_gemma":[0.00046156428,0.00029376076,0.00026531148,0.00010879395,0.00046076946,0.0007610828,0.00037649824,0.00028997447,0.0002262518],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050750666,0.00013223109,0.031508077,0.0002129122,0.00019696017,0.0034634338,0.0017551208,0.3934456,0.23734498,0.28946403,0.006857347,0.035111785],"study_design_scores_gemma":[0.000059948896,0.000121130935,0.0069748634,0.0000160405,0.00004928045,0.00032897296,0.00013297149,0.95843583,0.00520288,0.026112646,0.0025132494,0.000052123552],"about_ca_topic_score_codex":0.0041367155,"about_ca_topic_score_gemma":0.002698724,"teacher_disagreement_score":0.0041367155,"about_ca_system_score_codex":0.0006133529,"about_ca_system_score_gemma":0.00043260137,"threshold_uncertainty_score":0.008225262},"labels":[],"label_agreement":null},{"id":"W1517894914","doi":"10.1029/2007gl029536","title":"An evaluation of deep soil configurations in the CLM3 for improved representation of permafrost","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":184,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Advanced Research; National Science Foundation","keywords":"Permafrost; Layer (electronics); Slab; Active layer; Geology; Soil science; Soil horizon; Environmental science; Atmospheric sciences; Soil water; Geophysics; Materials science","score_opus":0.1349032467963563,"score_gpt":0.40012743420343255,"score_spread":0.26522418740707626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1517894914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9904744,0.00012337376,0.005571665,0.00011750467,0.000024410248,0.000032400283,0.0010995271,0.0007857599,0.0017709314],"genre_scores_gemma":[0.9898134,0.000045041714,0.009007115,0.000027100172,0.00000432748,0.000020180472,0.0008211402,0.00009818005,0.00016353223],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996954,0.0001279973,0.000020393421,0.00004862025,0.00004809548,0.00005941991],"domain_scores_gemma":[0.9987594,0.0006082746,0.00006667513,0.00021007439,0.00021218654,0.00014344777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009987768,0.0010011237,0.0006242242,0.00034095455,0.0004160348,0.00067106547,0.0014028744,0.0009116755,0.0015404512],"category_scores_gemma":[0.0029811745,0.00040376492,0.00058808166,0.00068427506,0.0003356556,0.0008584899,0.0006366953,0.00061865355,0.00021962269],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006326778,0.00017500183,0.01388823,0.000065342916,0.0000892317,0.00015244729,0.000055825232,0.9668024,0.0064384677,0.0007007451,0.0005665313,0.010433128],"study_design_scores_gemma":[0.00016013591,0.00018009957,0.0040452364,0.000009985641,0.000028229138,0.000022475859,0.000059966613,0.9915814,0.0031771644,0.0002721298,0.00044048595,0.000022658363],"about_ca_topic_score_codex":0.030938331,"about_ca_topic_score_gemma":0.025877787,"teacher_disagreement_score":0.030938331,"about_ca_system_score_codex":0.0008155552,"about_ca_system_score_gemma":0.0008976887,"threshold_uncertainty_score":0.061516464},"labels":[],"label_agreement":null},{"id":"W1518414747","doi":"10.1029/2012gl053695","title":"Long‐term variation of atmospheric methyl iodide and its link to global environmental change","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Pacific decadal oscillation; Climatology; Climate change; Sea surface temperature; Global warming; Methyl iodide; Pacific ocean; Atmospheric sciences; Oceanography; Geology; Chemistry","score_opus":0.039489808671260444,"score_gpt":0.2854514239665844,"score_spread":0.24596161529532395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1518414747","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985203,0.0002877794,0.00022824245,0.00005837473,0.0000065580134,0.0000024609442,0.00036476954,0.000012937512,0.00051862624],"genre_scores_gemma":[0.99930024,0.00013755809,0.00014787074,0.000017650673,0.000008161531,0.0000033646384,0.0002533364,0.0000023970726,0.00012931903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999318,0.000009388504,0.00000572207,0.000021593423,0.000014607136,0.0000167657],"domain_scores_gemma":[0.999634,0.00007666476,0.00014477302,0.000028409415,0.00008190996,0.000034251763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023596971,0.00012915026,0.00013625548,0.0004328235,0.00017103644,0.00029664554,0.00011915168,0.00032107238,0.0004505966],"category_scores_gemma":[0.0005418468,0.00010120576,0.00013344546,0.00065894733,0.0001943154,0.00030628717,0.00026203864,0.00020602548,0.00009750169],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015887778,0.000053794764,0.9526267,0.000047533194,0.00014933744,0.00011955269,0.00024019959,0.0015734724,0.03390512,0.00010991004,0.00022062751,0.010794832],"study_design_scores_gemma":[0.0000013268187,0.000023194316,0.9979907,0.0000025415673,0.00001380278,0.00002418281,0.00005419164,0.00052528805,0.0009944049,0.000043981552,0.00032173004,0.000004592223],"about_ca_topic_score_codex":0.009485766,"about_ca_topic_score_gemma":0.0116899675,"teacher_disagreement_score":0.009485766,"about_ca_system_score_codex":0.00035035575,"about_ca_system_score_gemma":0.00014780648,"threshold_uncertainty_score":0.018861115},"labels":[],"label_agreement":null},{"id":"W1518686455","doi":"10.1002/2014gl059274","title":"The Atlantic Multidecadal Oscillation as a dominant factor of oceanic influence on climate","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Atlantic multidecadal oscillation; Climatology; Coupled model intercomparison project; Environmental science; Radiative forcing; Climate model; North Atlantic oscillation; Atmospheric sciences; Aerosol; Forcing (mathematics); Mean radiant temperature; Oscillation (cell signaling); Global warming; Variance (accounting); Climate change; Meteorology; Geography; Geology; Chemistry","score_opus":0.02620880831236253,"score_gpt":0.3102930175111395,"score_spread":0.28408420919877697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1518686455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933711,0.001031782,0.0011666233,0.0006668605,0.00009601444,0.0000049312484,0.00055517117,0.000034778604,0.003072591],"genre_scores_gemma":[0.9988285,0.0002839509,0.00019694118,0.000034563873,0.000038916358,0.0000019836355,0.00016709464,0.000011923637,0.0004362012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998839,0.000048636794,0.000006139211,0.000023413071,0.000018645747,0.000019205108],"domain_scores_gemma":[0.9996551,0.0001237542,0.000066241424,0.000030476764,0.00006254648,0.0000617637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004869639,0.00027303852,0.00019099137,0.0002549454,0.00020444141,0.00063724135,0.00013266467,0.00014990928,0.0014970881],"category_scores_gemma":[0.0010071635,0.000107140026,0.00057397207,0.00036106302,0.000117649426,0.00028377215,0.00041580817,0.0003596127,0.00016254101],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000250022,0.000059635608,0.9394266,0.00007043927,0.0005356755,0.0001752046,0.000115621195,0.014039981,0.0073625506,0.002214899,0.0028687073,0.032880723],"study_design_scores_gemma":[0.000013065783,0.00002881827,0.9579141,0.00002074479,0.00022571503,0.000036313057,0.000092106566,0.038392395,0.00049460103,0.00063045276,0.002142121,0.000009544246],"about_ca_topic_score_codex":0.020218646,"about_ca_topic_score_gemma":0.022593535,"teacher_disagreement_score":0.020218646,"about_ca_system_score_codex":0.00031784072,"about_ca_system_score_gemma":0.00045267757,"threshold_uncertainty_score":0.040201902},"labels":[],"label_agreement":null},{"id":"W1519564052","doi":"10.1029/2011gl050219","title":"Winter sea‐ice melt in the Canada Basin, Arctic Ocean","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Research Foundation","keywords":"Sea ice; Environmental science; Halocline; Climatology; Arctic ice pack; Drift ice; Antarctic sea ice; Sea ice thickness; Geology; Atmospheric sciences; Oceanography","score_opus":0.021662430456036795,"score_gpt":0.2563968576948163,"score_spread":0.2347344272387795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1519564052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99211496,0.0013431404,0.00004524265,0.00039071424,0.000015323962,0.000005923309,0.0024244492,0.000015361566,0.0036447847],"genre_scores_gemma":[0.99638283,0.0007261552,0.00008720857,0.00004016044,0.000006643821,0.0000033708377,0.0013394381,0.0000071446098,0.0014070343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986804,0.000004759165,0.000005576979,0.000020921065,0.000050995834,0.000049671347],"domain_scores_gemma":[0.9996995,0.00001175657,0.00003886584,0.000006087211,0.00016199169,0.00008186775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021060296,0.000168133,0.0001791955,0.0011939376,0.0020321163,0.0013486762,0.00033550043,0.00023901547,0.0014165395],"category_scores_gemma":[0.0007343748,0.00015074066,0.00019004349,0.0021619608,0.0005266829,0.00036924996,0.00044834826,0.00023280976,0.00013873281],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002061925,0.000026774154,0.9739986,0.000060567207,0.00008750838,0.00020724663,0.0008870865,0.0019925782,0.0019377599,0.00082670135,0.003296767,0.016472088],"study_design_scores_gemma":[0.000005701004,0.000004758327,0.9959902,0.00001614735,0.000015498501,0.00002135406,0.0005375585,0.0005284054,0.00013575815,0.00007155228,0.0026676022,0.000005334413],"about_ca_topic_score_codex":0.99385506,"about_ca_topic_score_gemma":0.9975364,"teacher_disagreement_score":0.022540918,"about_ca_system_score_codex":0.022540918,"about_ca_system_score_gemma":0.019867083,"threshold_uncertainty_score":0.16354656},"labels":[],"label_agreement":null},{"id":"W1519582367","doi":"10.1002/grl.50745","title":"Impact thermochronology and the age of Haughton impact structure, Canada","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ames Research Center; National Aeronautics and Space Administration","keywords":"Thermochronology; Impact structure; Systematics; Geochronology; Radiogenic nuclide; Zircon; Geology; Yield (engineering); Earth science; Geochemistry; Physics; Astrobiology; Thermodynamics","score_opus":0.01726160689092038,"score_gpt":0.2835962981244937,"score_spread":0.26633469123357334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1519582367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9157441,0.0032836597,0.0015140298,0.0006296896,0.000056708206,0.00007417788,0.009736621,0.00018334862,0.06877764],"genre_scores_gemma":[0.98764265,0.00074437173,0.00054705667,0.000041160936,0.000004690925,0.000008747812,0.0017041032,0.000031837477,0.009275349],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99963164,0.000009534999,0.000009650854,0.000051071176,0.00017563012,0.0001224279],"domain_scores_gemma":[0.998825,0.000034123794,0.000083720864,0.000032115942,0.0009129628,0.00011208904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032680354,0.00032265793,0.00024043852,0.0032289727,0.0029049185,0.0012125965,0.00065617485,0.00022077892,0.0041579334],"category_scores_gemma":[0.001128525,0.0002190902,0.00020253129,0.0034294883,0.00083552406,0.00042209585,0.0006622154,0.00038982992,0.0003984561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006090414,0.00004033557,0.8595942,0.00016047695,0.00018928436,0.00059828395,0.005131471,0.006114307,0.014830381,0.013147281,0.011988512,0.087596506],"study_design_scores_gemma":[0.0000071749564,0.000015619577,0.970303,0.00003972662,0.000024998986,0.000111960464,0.0011848185,0.0009088954,0.0027298725,0.0002712022,0.024381539,0.000021193553],"about_ca_topic_score_codex":0.9938453,"about_ca_topic_score_gemma":0.99783665,"teacher_disagreement_score":0.03993587,"about_ca_system_score_codex":0.03993587,"about_ca_system_score_gemma":0.01927322,"threshold_uncertainty_score":0.28975642},"labels":[],"label_agreement":null},{"id":"W1519949070","doi":"10.1002/grl.50193","title":"CryoSat‐2 estimates of Arctic sea ice thickness and volume","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":854,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Environment Research Council; Deutsches Zentrum für Luft- und Raumfahrt; Alberta Ingenuity; Sight Research UK; European Space Agency; National Aeronautics and Space Administration; National Science Foundation","keywords":"Climatology; Data assimilation; Arctic; Arctic ice pack; Volume (thermodynamics); Sea ice; Geology; The arctic; Satellite; Environmental science; Oceanography; Physical geography; Meteorology; Geography","score_opus":0.018874035893861874,"score_gpt":0.25959518244776475,"score_spread":0.24072114655390286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1519949070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.929931,0.00045022173,0.007791749,0.00013172046,0.000075965574,0.000037503687,0.03991839,0.0005514189,0.021112058],"genre_scores_gemma":[0.94517964,0.0004212916,0.0062144836,0.000049490216,0.00005147862,0.0000738612,0.045410797,0.00010832589,0.0024906343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985194,0.000015968986,0.000013482303,0.00003236455,0.00006590277,0.000020374488],"domain_scores_gemma":[0.9995906,0.000061092425,0.00014817136,0.000044247845,0.00013459685,0.00002132684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033920494,0.00047361245,0.00018617694,0.0013144885,0.00017083646,0.0005147188,0.00025958903,0.0001547135,0.0017723392],"category_scores_gemma":[0.0008221717,0.00014616693,0.0004135443,0.001193713,0.00014064001,0.00045420788,0.0003108466,0.00020070253,0.0006026358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017988872,0.00009277079,0.829297,0.0001326458,0.0003700281,0.00013057138,0.00040353596,0.08750496,0.007886908,0.0014602308,0.013752363,0.058789063],"study_design_scores_gemma":[0.000018621608,0.000038449176,0.9493549,0.000030455045,0.000043551056,0.00011430673,0.00017054797,0.027006764,0.0036516027,0.000727004,0.018813077,0.000030787483],"about_ca_topic_score_codex":0.02714719,"about_ca_topic_score_gemma":0.041060425,"teacher_disagreement_score":0.02714719,"about_ca_system_score_codex":0.00061894284,"about_ca_system_score_gemma":0.00032385948,"threshold_uncertainty_score":0.053978384},"labels":[],"label_agreement":null},{"id":"W1519971169","doi":"10.1029/2012gl053097","title":"Spatial distribution of air‐sea heat fluxes over the sub‐polar North Atlantic Ocean","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"North Atlantic Deep Water; Climatology; Thermohaline circulation; Environmental science; Sensible heat; Arctic sea ice decline; Ocean current; Heat flux; Geology; Sea surface temperature; Sea ice; Oceanography; Cryosphere; Atmospheric sciences; Sea ice thickness; Heat transfer","score_opus":0.024783912553810083,"score_gpt":0.27832304492759813,"score_spread":0.25353913237378806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1519971169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99826044,0.000103108934,0.000098032826,0.000037813297,0.0000042273573,0.0000022365202,0.000629866,0.000010899821,0.0008531857],"genre_scores_gemma":[0.9989938,0.00011238255,0.00011014563,0.000008640125,0.0000079291685,0.000004632755,0.00051516213,0.0000026627076,0.00024460634],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999435,0.0000061041387,0.0000047614944,0.000019263653,0.000011243924,0.000015185343],"domain_scores_gemma":[0.9997695,0.00004960553,0.00007264603,0.000013415294,0.00005521103,0.000039591356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096614676,0.0001119958,0.00014870697,0.0005880461,0.00018434497,0.0003545462,0.0000888545,0.00013017748,0.00097113044],"category_scores_gemma":[0.00024791717,0.00008427461,0.00014830666,0.0005664409,0.00017083026,0.0001681415,0.00020821934,0.000099109246,0.00015339849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013327117,0.000026746156,0.9712261,0.000031888772,0.00009355308,0.00018716477,0.00040023203,0.0024939838,0.011695401,0.0002552259,0.0007663596,0.012690009],"study_design_scores_gemma":[0.0000029067494,0.0000057981697,0.9983077,0.0000032788885,0.000008782781,0.000020894193,0.00012495932,0.00096068805,0.00019144037,0.00003169903,0.000338485,0.0000033624763],"about_ca_topic_score_codex":0.03803584,"about_ca_topic_score_gemma":0.050702162,"teacher_disagreement_score":0.03803584,"about_ca_system_score_codex":0.00025993603,"about_ca_system_score_gemma":0.000266772,"threshold_uncertainty_score":0.07562888},"labels":[],"label_agreement":null},{"id":"W1520194505","doi":"10.1029/2009gl038659","title":"Emissions of ozone‐depleting halocarbons from China","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Montreal Protocol; China; Ozone; Environmental science; Ozone layer; Ozone depletion; Environmental protection; Meteorology; Atmospheric sciences; Natural resource economics; Geography; Economics","score_opus":0.026041840015266493,"score_gpt":0.2866721345870921,"score_spread":0.2606302945718256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1520194505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954834,0.00024204054,0.00010810867,0.0001281849,0.0000064648557,0.000010612655,0.0015972558,0.000012559765,0.002411359],"genre_scores_gemma":[0.9945696,0.00049017626,0.00016470617,0.000073871226,0.000009048833,0.00001282407,0.0023719103,0.000004725092,0.002303172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.0000076085907,0.000008728211,0.000019367908,0.000053385655,0.000025821699],"domain_scores_gemma":[0.9998983,0.000013320143,0.000023137214,0.000009250505,0.000040278854,0.000015706702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021262445,0.00047584932,0.00020424675,0.0009111093,0.0006212424,0.00047153851,0.00019440602,0.0002271211,0.00074288045],"category_scores_gemma":[0.00015823497,0.0001353307,0.00038513873,0.0014502503,0.00012135531,0.00019585164,0.00040964378,0.0001534235,0.000108212276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070570986,0.00019005811,0.7768487,0.00082417135,0.0006985625,0.003561658,0.0015482642,0.041110624,0.08286954,0.0026881036,0.010506476,0.07844808],"study_design_scores_gemma":[0.000031071457,0.00006853113,0.97884387,0.000011395188,0.000083549465,0.00010942693,0.00020638457,0.0057819234,0.0070996354,0.00027858294,0.0074528493,0.00003267422],"about_ca_topic_score_codex":0.22938316,"about_ca_topic_score_gemma":0.25269634,"teacher_disagreement_score":0.22938316,"about_ca_system_score_codex":0.0022213652,"about_ca_system_score_gemma":0.0019335183,"threshold_uncertainty_score":0.45609605},"labels":[],"label_agreement":null},{"id":"W1520412144","doi":"10.1029/2004gl019883","title":"Power‐law scaling behavior of crustal density and gravity","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Crust; Scaling; Power law; Isotropy; Scaling law; Geophysics; Surface gravity; Scale invariance; Spectral density; Seismology; Geodesy; Spectral line; Physics; Geometry; Optics; Astronomy","score_opus":0.03289562889738861,"score_gpt":0.3130348497211805,"score_spread":0.2801392208237919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1520412144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9119316,0.00033638923,0.078833684,0.0002689595,0.000019735295,0.000041380546,0.00029823673,0.00048294428,0.007786955],"genre_scores_gemma":[0.99607736,0.00010981108,0.0032010605,0.000024526498,0.000014533493,0.00001573878,0.00011721757,0.000024593066,0.0004152095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998307,0.000026771233,0.0000060240186,0.000060256883,0.000054153028,0.000022063943],"domain_scores_gemma":[0.9983051,0.0008183036,0.00029619728,0.00032145134,0.00020579949,0.000053137817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003093713,0.00020116752,0.0001380295,0.0005510064,0.00012722245,0.00038816675,0.00030222823,0.00024156607,0.0013550364],"category_scores_gemma":[0.007081144,0.00018715461,0.00016026194,0.0003618285,0.0007714505,0.00091714994,0.00025784952,0.00029366696,0.00034402896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029890408,0.00024655214,0.33104783,0.00028284857,0.00025396055,0.0019751193,0.0021530816,0.23712315,0.16225873,0.08915175,0.0073225508,0.16788553],"study_design_scores_gemma":[0.000029256575,0.00011328298,0.30717066,0.000024154833,0.000032603846,0.0013513139,0.00023733154,0.61268336,0.013477882,0.061602753,0.0031889093,0.00008854526],"about_ca_topic_score_codex":0.0017778837,"about_ca_topic_score_gemma":0.0007418564,"teacher_disagreement_score":0.0017778837,"about_ca_system_score_codex":0.00026786586,"about_ca_system_score_gemma":0.00012096066,"threshold_uncertainty_score":0.004532993},"labels":[],"label_agreement":null},{"id":"W1522874890","doi":"10.1029/2012gl052712","title":"Glacier volume‐area relation for high‐order mechanics and transient glacier states","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Glacier; Geology; Glacier ice accumulation; Accumulation zone; Surge; Tidewater glacier cycle; Meltwater; Glacier morphology; Glacier mass balance; Climatology; Rock glacier; Geomorphology; Physical geography; Cryosphere; Geography; Ice stream; Sea ice","score_opus":0.04291021986236452,"score_gpt":0.275490568419052,"score_spread":0.2325803485566875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1522874890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96987534,0.00022586861,0.024831101,0.00016041828,0.000012610764,0.000017084378,0.00018603861,0.00009751645,0.004594128],"genre_scores_gemma":[0.99807537,0.000059318183,0.0014397518,0.000008566076,0.000004255232,0.00001623388,0.000091287155,0.000017012442,0.00028821133],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987483,0.000026558142,0.000008768083,0.00004086996,0.000024542365,0.000024303115],"domain_scores_gemma":[0.9981287,0.0010693268,0.00029886098,0.00030577328,0.00011204444,0.00008522965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073279033,0.00015584796,0.00020542055,0.00072395836,0.00048460258,0.0007436405,0.00044520016,0.0004224569,0.0019662217],"category_scores_gemma":[0.004834461,0.00017295638,0.0004988708,0.0004669235,0.00092048553,0.0009416694,0.0003714669,0.0005490321,0.00017001711],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048715196,0.00003562418,0.044190966,0.000040170475,0.0000348023,0.00013589497,0.0004729422,0.8842797,0.004437905,0.056649964,0.0007724594,0.008900875],"study_design_scores_gemma":[0.000010855344,0.000034102373,0.029944085,0.000012547813,0.000012345716,0.00011959541,0.000067066605,0.9380066,0.00082985393,0.030147646,0.0007942008,0.000021059333],"about_ca_topic_score_codex":0.0034070604,"about_ca_topic_score_gemma":0.003253858,"teacher_disagreement_score":0.0034070604,"about_ca_system_score_codex":0.00076980883,"about_ca_system_score_gemma":0.0003323396,"threshold_uncertainty_score":0.006774485},"labels":[],"label_agreement":null},{"id":"W1524633450","doi":"10.1029/2012gl054306","title":"Isentropic constraints by midlatitude surface warming on the Arctic midtroposphere","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Middle latitudes; Climatology; Global warming; Arctic; Environmental science; Climate model; Atmospheric sciences; Eddy; Latitude; Climate change; Geology; Meteorology; Oceanography; Geography","score_opus":0.04201345078052596,"score_gpt":0.30392399937151066,"score_spread":0.2619105485909847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1524633450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98815453,0.00021190193,0.0011752582,0.00030352193,0.000011095288,0.0000020948132,0.00017232125,0.000018688095,0.009950596],"genre_scores_gemma":[0.99965644,0.00006707305,0.00006334646,0.00001297325,0.000005135707,9.655378e-7,0.000038657938,0.000004224147,0.00015118749],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993753,0.000021654341,0.0000032484936,0.000008850741,0.000009594982,0.000019207786],"domain_scores_gemma":[0.99958915,0.00016933333,0.00007589474,0.00003647082,0.000060589526,0.00006865378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024318974,0.00018386992,0.00017210258,0.00024507302,0.00029997705,0.00074154156,0.0001772582,0.0002465234,0.0036795032],"category_scores_gemma":[0.0012629138,0.00015824885,0.00025605035,0.00015090259,0.00035875474,0.00056804315,0.00059961586,0.00033937622,0.00021517252],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007787931,0.00014319594,0.32510483,0.00014516865,0.0001980651,0.0009210439,0.00047915647,0.5260962,0.05782002,0.0694871,0.002013557,0.016812783],"study_design_scores_gemma":[0.00012100769,0.00014510305,0.48508006,0.000071714996,0.00007274486,0.00016906398,0.00053362385,0.45246503,0.0055380813,0.050955046,0.0048051206,0.000043408414],"about_ca_topic_score_codex":0.0060407473,"about_ca_topic_score_gemma":0.006437746,"teacher_disagreement_score":0.0060407473,"about_ca_system_score_codex":0.00038202395,"about_ca_system_score_gemma":0.000299055,"threshold_uncertainty_score":0.012309194},"labels":[],"label_agreement":null},{"id":"W1525270929","doi":"10.1002/grl.50176","title":"The effect of pre‐existing craters on the initial development of explosive volcanic eruptions: An experimental investigation","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Natural Sciences and Engineering Research Council of Canada; University at Buffalo; Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Impact crater; Ejecta; Volcano; Geology; Explosive material; Explosive eruption; Shaped charge; Projectile; Seismology; Jet (fluid); Petrology; Geophysics; Pyroclastic rock; Astrobiology; Mechanics; Materials science; Physics; Astrophysics","score_opus":0.0745960457517762,"score_gpt":0.3322116818077724,"score_spread":0.2576156360559962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1525270929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99861205,0.00014548074,0.0007651254,0.0000103651955,0.000009015182,0.000031606563,0.00007952142,0.000013294142,0.00033351852],"genre_scores_gemma":[0.99606687,0.00027363206,0.0023679254,0.000028373335,0.000011688809,0.00007608691,0.00016212024,0.000021522026,0.0009919761],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996871,0.000041843436,0.00003953685,0.00008642588,0.00005392191,0.00009128323],"domain_scores_gemma":[0.9984403,0.00080977805,0.00021452378,0.00028644784,0.000074379845,0.00017460647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033378467,0.00035217646,0.00027124924,0.0002473003,0.0002053066,0.0004304814,0.00031298056,0.00034431278,0.0024305892],"category_scores_gemma":[0.0011657942,0.00025703365,0.00020843289,0.0001509023,0.0006697397,0.00036904056,0.00064449984,0.0007378377,0.00015066333],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067639723,0.0005971599,0.0013558582,0.00004378692,0.000009417765,0.000083752435,0.00007556696,0.00026848642,0.99412787,0.00010925939,0.000021465941,0.002630945],"study_design_scores_gemma":[0.00016630563,0.010542725,0.032286767,0.00001822488,0.000058026417,0.00038706843,0.00020816058,0.0044474914,0.9507194,0.0002061353,0.0009322769,0.000027438165],"about_ca_topic_score_codex":0.00062796054,"about_ca_topic_score_gemma":0.0006530785,"teacher_disagreement_score":0.0024305892,"about_ca_system_score_codex":0.00025579758,"about_ca_system_score_gemma":0.00015539359,"threshold_uncertainty_score":0.008131146},"labels":[],"label_agreement":null},{"id":"W1529157380","doi":"10.1002/2015gl064580","title":"Inverted barometer contributions to recent sea level changes along the northeast coast of North America","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Barometer; Tide gauge; Sea level; Climatology; Geology; Oceanography; Atmospheric pressure; Sea level rise; Environmental science; Climate change; Geography; Meteorology","score_opus":0.1218107831732647,"score_gpt":0.31319041108402623,"score_spread":0.19137962791076152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1529157380","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99844104,0.000097148,0.00018522507,0.000065769294,0.000012707873,0.0000018100594,0.00033830138,0.000016155345,0.00084171334],"genre_scores_gemma":[0.9989813,0.00008806919,0.00015442318,0.000011122646,0.000013502254,0.000001981774,0.00053720456,0.0000052259666,0.0002071734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998888,0.000024110694,0.0000075027842,0.000029775485,0.00003415766,0.0000156425],"domain_scores_gemma":[0.99940777,0.00015098046,0.00014399707,0.000052156058,0.00019253396,0.000052568932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038913803,0.0001815593,0.00012602156,0.00056786375,0.00017511997,0.00048351526,0.00020224357,0.00011417082,0.0007225381],"category_scores_gemma":[0.0015928139,0.0001405321,0.00014509795,0.0008485285,0.00020114392,0.0002825252,0.0004235071,0.00024597428,0.00008406976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055687553,0.000011919043,0.98191476,0.000015134278,0.00006149296,0.000075144686,0.00027481467,0.001688292,0.0023835553,0.00011970002,0.00036510534,0.013034358],"study_design_scores_gemma":[0.000001329226,0.0000047528024,0.9977126,0.0000024179838,0.0000074352397,0.000009628111,0.00005752545,0.0017213026,0.000077758625,0.000024265832,0.0003781914,0.0000028192687],"about_ca_topic_score_codex":0.09089744,"about_ca_topic_score_gemma":0.13928764,"teacher_disagreement_score":0.90910256,"about_ca_system_score_codex":0.00046127487,"about_ca_system_score_gemma":0.0003913133,"threshold_uncertainty_score":0.18073672},"labels":[],"label_agreement":null},{"id":"W1529196992","doi":"10.1002/2014gl060604","title":"Electric currents of a substorm current wedge on 24 February 2010","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"National Aeronautics and Space Administration","keywords":"Substorm; Electrojet; Ionosphere; Geophysics; Ampere; Physics; Magnetosphere; Current (fluid); Wedge (geometry); Geology; Earth's magnetic field; Magnetic field","score_opus":0.022988014707059964,"score_gpt":0.29864171160801745,"score_spread":0.2756536969009575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1529196992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99591297,0.000035648394,0.00032490335,0.00005261216,0.000010712658,0.000007174635,0.00047800053,0.00007268584,0.0031053254],"genre_scores_gemma":[0.99845624,0.000011261697,0.00020928706,0.000017329612,0.000006687663,0.000003528223,0.0007588193,0.0000117403815,0.00052515976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.0000051568804,0.0000029337043,0.000019145817,0.000026235919,0.000020939891],"domain_scores_gemma":[0.9997776,0.000017703504,0.00003705744,0.000028341346,0.00008471069,0.00005449648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013187814,0.00012766018,0.0002473029,0.000417805,0.0004195027,0.00044994807,0.00023477203,0.00029594556,0.0012682357],"category_scores_gemma":[0.00042422753,0.0000678938,0.00010012834,0.00036280564,0.00023368176,0.0002388346,0.0004016037,0.000356589,0.00027677996],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013074809,0.00029050326,0.66522205,0.00007890866,0.00008788521,0.0043341676,0.0014647841,0.0056589227,0.23884423,0.0024451595,0.007269206,0.07299672],"study_design_scores_gemma":[0.000012900659,0.000078660094,0.98086977,0.000009922552,0.000013358367,0.00025129184,0.00023801206,0.004732882,0.00873278,0.00035963504,0.00468693,0.000013785956],"about_ca_topic_score_codex":0.007326342,"about_ca_topic_score_gemma":0.012386071,"teacher_disagreement_score":0.007326342,"about_ca_system_score_codex":0.0005876334,"about_ca_system_score_gemma":0.00016626867,"threshold_uncertainty_score":0.014567375},"labels":[],"label_agreement":null},{"id":"W1530760391","doi":"10.1029/2010gl044852","title":"Geostatistical inversion of seismic and ground‐penetrating radar reflection images: What can we actually resolve?","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Ground-penetrating radar; Geology; Inversion (geology); Reflection (computer programming); Radar; Seismic inversion; Seismology; Geophysics; Remote sensing; Geodesy; Geometry; Azimuth; Computer science; Mathematics","score_opus":0.032298459757026894,"score_gpt":0.3283649321543277,"score_spread":0.29606647239730083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1530760391","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14097819,0.010409148,0.8246481,0.02000252,0.00022690203,0.0000368064,0.00025753753,0.0007252163,0.002715544],"genre_scores_gemma":[0.83370996,0.011253307,0.15136163,0.0013748022,0.00067687273,0.000056738154,0.00030366547,0.00012415228,0.0011389046],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99928695,0.0003588419,0.00003849648,0.000055395507,0.00018713038,0.00007326111],"domain_scores_gemma":[0.99455243,0.0035380104,0.00074209727,0.0005336012,0.0004741717,0.00015979251],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0044503147,0.0006698278,0.0009281178,0.0007491458,0.00017172753,0.0016015406,0.0011896244,0.0015171784,0.0005684304],"category_scores_gemma":[0.026232587,0.00052509934,0.0003943656,0.0012681234,0.0019828272,0.0040831957,0.0010354592,0.0010228982,0.00047523985],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029334275,0.00027746396,0.028996639,0.0011857268,0.00037350054,0.0004974904,0.0006157698,0.15772033,0.018916652,0.12862064,0.009523604,0.6529789],"study_design_scores_gemma":[0.00006224146,0.000077124765,0.0073807063,0.00018193116,0.00006204819,0.00039837038,0.0006229764,0.75219876,0.0055529885,0.22828658,0.0050965324,0.00007971637],"about_ca_topic_score_codex":0.0027854883,"about_ca_topic_score_gemma":0.0021691984,"teacher_disagreement_score":0.0044503147,"about_ca_system_score_codex":0.00035314707,"about_ca_system_score_gemma":0.0014947626,"threshold_uncertainty_score":0.023535848},"labels":[],"label_agreement":null},{"id":"W1531040956","doi":"10.1002/2015gl064671","title":"Controls on <sup>231</sup>Pa and <sup>230</sup>Th in the Arctic Ocean","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"FP7 People: Marie-Curie Actions; Natural Sciences and Engineering Research Council of Canada","keywords":"Arctic; Sedimentary rock; Geology; Structural basin; Canada Basin; Oceanography; Scavenging; Glacial period; The arctic; Water column; Sedimentary basin; Paleontology; Chemistry","score_opus":0.05033053657860836,"score_gpt":0.2994631269745838,"score_spread":0.24913259039597546,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1531040956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995812,0.000084212224,0.0013628078,0.00009403355,0.000012433487,0.0000026966961,0.00012707798,0.000034615252,0.0024700405],"genre_scores_gemma":[0.99966776,0.000032064236,0.000089752444,0.000010500095,0.0000027288147,0.0000013416213,0.000032000517,0.000006622372,0.00015724248],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989915,0.000029498158,0.0000069349508,0.000025069789,0.000014712377,0.000024692417],"domain_scores_gemma":[0.9996942,0.000121994985,0.000049254435,0.000027945214,0.00005584645,0.000050795938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028655806,0.0003987873,0.00022313067,0.00018091266,0.0003110669,0.0007852094,0.00023398073,0.00027738095,0.0013881286],"category_scores_gemma":[0.00072867447,0.0002386839,0.00034395469,0.000100269746,0.00046566382,0.00038684424,0.00039508997,0.00026578948,0.00014849684],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090150425,0.00009993136,0.12425317,0.00014253997,0.00028548003,0.00083162764,0.0002572196,0.48729104,0.3632033,0.013114958,0.0008610216,0.008758302],"study_design_scores_gemma":[0.00013610175,0.0002603431,0.20008871,0.00002082686,0.00020404301,0.00017510109,0.0004730056,0.7446987,0.044035938,0.0071499757,0.0026645204,0.00009277156],"about_ca_topic_score_codex":0.02061707,"about_ca_topic_score_gemma":0.010162139,"teacher_disagreement_score":0.02061707,"about_ca_system_score_codex":0.0008808144,"about_ca_system_score_gemma":0.00053417706,"threshold_uncertainty_score":0.040994108},"labels":[],"label_agreement":null},{"id":"W1532917172","doi":"10.1029/2009gl041752","title":"A dynamo model for axisymmetrizing Saturn's magnetic field","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Dynamo; Dynamo theory; Differential rotation; Physics; Mercury's magnetic field; Magnetic field; Solar dynamo; Saturn; Magnetic dipole; Dipole; Equator; Dipole model of the Earth's magnetic field; Rotational symmetry; Field (mathematics); Classical mechanics; Geophysics; Mechanics; L-shell; Earth's magnetic field; Astrophysics; Planet; Astronomy; Latitude; Interplanetary magnetic field; Quantum mechanics","score_opus":0.02272826829909863,"score_gpt":0.30966250227513337,"score_spread":0.28693423397603474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1532917172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7030647,0.0011115952,0.21511263,0.0032981718,0.00032017252,0.00015384925,0.0010622187,0.0004225266,0.0754541],"genre_scores_gemma":[0.9811817,0.00028617078,0.006233326,0.00011013429,0.000051438947,0.00012461844,0.00016718336,0.000053490385,0.011791939],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993575,0.000015901145,0.0000032683693,0.00001600376,0.000013925127,0.000015237085],"domain_scores_gemma":[0.9998623,0.000035370434,0.000029765244,0.000012139424,0.000024725816,0.000035677713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022577039,0.00035047097,0.00047102576,0.0003111523,0.0006492841,0.0008296821,0.0007072082,0.0011442264,0.0023388392],"category_scores_gemma":[0.0005142375,0.0003197241,0.00045833908,0.00024024856,0.001074166,0.0009893036,0.0007244076,0.00050302816,0.00028435333],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012245319,0.000038596627,0.0012604668,0.00005678625,0.00003419224,0.00032991148,0.00019681454,0.8450194,0.011955681,0.13835901,0.00098842,0.0016382891],"study_design_scores_gemma":[0.00006037464,0.000018410117,0.00029301923,0.000003358876,0.0000059118447,0.000032734937,0.000029159237,0.98505497,0.0002621602,0.013168397,0.0010620385,0.00000946854],"about_ca_topic_score_codex":0.010699026,"about_ca_topic_score_gemma":0.0044247634,"teacher_disagreement_score":0.010699026,"about_ca_system_score_codex":0.0010799813,"about_ca_system_score_gemma":0.0009256984,"threshold_uncertainty_score":0.021273494},"labels":[],"label_agreement":null},{"id":"W1532997732","doi":"10.1029/2010gl043965","title":"Geodynamic models of Archean continental collision and the formation of mantle lithosphere keels","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Imbrication; Geology; Underplating; Lithosphere; Mantle (geology); Crust; Craton; Transition zone; Continental crust; Archean; Collision zone; Petrology; Crustal recycling; Geophysics; Mantle convection; Geochemistry; Seismology; Tectonics","score_opus":0.01813682859017436,"score_gpt":0.2579912510572722,"score_spread":0.23985442246709787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1532997732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96532947,0.000513737,0.01884281,0.0009411199,0.00006957145,0.00002800345,0.00047027125,0.00017058007,0.013634296],"genre_scores_gemma":[0.9955166,0.00024639317,0.0014517052,0.000036914465,0.000019675625,0.000029573985,0.00013365026,0.000033415785,0.002532006],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999293,0.000027624215,0.000004066645,0.0000126248615,0.000011008312,0.00001542614],"domain_scores_gemma":[0.9997875,0.00007933369,0.000041489202,0.000021453694,0.00002910868,0.000041163818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028290044,0.00045503912,0.0004906167,0.0004583627,0.00058782584,0.0010401143,0.0009765928,0.0010489958,0.0020579796],"category_scores_gemma":[0.001253529,0.000507311,0.00052460184,0.00046577392,0.000956236,0.00092160434,0.0008487882,0.0005407543,0.00017512013],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026826918,0.000009482426,0.0013678283,0.00000618489,0.000014152886,0.0000321263,0.000029861732,0.9932094,0.0003906515,0.0044097253,0.000107847314,0.00039593622],"study_design_scores_gemma":[0.00002152853,0.000008513859,0.0008845953,0.0000024077963,0.000005903286,0.000007806195,0.000029690622,0.99571157,0.000083031744,0.0029937034,0.000246218,0.0000049746836],"about_ca_topic_score_codex":0.033992674,"about_ca_topic_score_gemma":0.013590062,"teacher_disagreement_score":0.033992674,"about_ca_system_score_codex":0.0015056066,"about_ca_system_score_gemma":0.0008605636,"threshold_uncertainty_score":0.06758964},"labels":[],"label_agreement":null},{"id":"W1534239563","doi":"10.1002/2015gl063930","title":"Real‐time estimation of Arctic sea ice thickness through maximum covariance analysis","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Initialization; Sea ice; Climatology; Covariance; Data assimilation; Arctic ice pack; Environmental science; Arctic; Meteorology; Geology; Statistics; Oceanography; Computer science; Mathematics; Geography","score_opus":0.03652281724398879,"score_gpt":0.300015867905522,"score_spread":0.26349305066153317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1534239563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7545287,0.00013426063,0.23924819,0.0002873022,0.000047889545,0.000038849324,0.0011205777,0.0017533371,0.0028408587],"genre_scores_gemma":[0.9543813,0.000033502245,0.044247504,0.000023233588,0.000015695448,0.000023660308,0.000823773,0.00008262678,0.00036871035],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997265,0.000111330715,0.000014405388,0.0000588265,0.000063692016,0.000025281111],"domain_scores_gemma":[0.9988445,0.00050681137,0.00017659602,0.00015749314,0.00027669812,0.00003787232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001168689,0.00034998704,0.00027656,0.0006500844,0.00027056996,0.00043048855,0.0004190169,0.00025082208,0.0006989877],"category_scores_gemma":[0.004116127,0.00029895408,0.00042904072,0.00061596156,0.00020068743,0.0006015475,0.00033262838,0.0005216716,0.00027123527],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028967467,0.00016838888,0.13326354,0.000057297333,0.00023494594,0.00006310453,0.00010428656,0.72585666,0.020634655,0.0020767006,0.002604145,0.11464666],"study_design_scores_gemma":[0.000010947728,0.000011436045,0.021088604,0.000004171612,0.0000063535213,0.0000069976973,0.0000064736146,0.9758322,0.0024622935,0.00029689205,0.00026219076,0.000011426908],"about_ca_topic_score_codex":0.04963247,"about_ca_topic_score_gemma":0.065253995,"teacher_disagreement_score":0.04963247,"about_ca_system_score_codex":0.0006510643,"about_ca_system_score_gemma":0.001105355,"threshold_uncertainty_score":0.09868711},"labels":[],"label_agreement":null},{"id":"W1534738398","doi":"10.1029/2010gl044771","title":"Twentieth century warming in deep waters of the Gulf of St. Lawrence: A unique feature of the last millennium","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"","keywords":"Oceanography; Water mass; Benthic zone; Estuary; Global warming; Climate change; Deep water; Geology; Little ice age; Isotopes of oxygen; Environmental science; Climatology; Physical geography; Geography; Geochemistry","score_opus":0.01586106220676416,"score_gpt":0.26699535025923904,"score_spread":0.2511342880524749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1534738398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99842715,0.0003930087,0.00006518455,0.000119404925,0.0000058459054,6.894177e-7,0.00017677475,0.0000041389844,0.000807807],"genre_scores_gemma":[0.99886143,0.00045215918,0.00010647678,0.000043513217,0.0000041941557,8.864446e-7,0.0001525969,0.0000012646009,0.00037747514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997354,0.0000023616324,0.0000020185284,0.000008102808,0.0000070216643,0.000006893107],"domain_scores_gemma":[0.99990237,0.000005023512,0.00004267205,0.0000062827576,0.00003354022,0.000010188064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009650758,0.00007531081,0.00007344825,0.00037264975,0.00029680453,0.00034253224,0.00009232794,0.00013412963,0.00043958388],"category_scores_gemma":[0.00025492278,0.000052888896,0.00006488557,0.00045265985,0.00030601953,0.00023175491,0.00025367417,0.0001444439,0.00006472212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006393166,0.000010227006,0.9634916,0.00004375968,0.000032769578,0.00007819762,0.0006768563,0.00026537577,0.015439484,0.00025355534,0.00026473246,0.019379482],"study_design_scores_gemma":[5.193919e-7,0.000006550471,0.99798274,0.000004591573,0.000005682546,0.000025863032,0.0001512997,0.000057463316,0.00055881304,0.00003186126,0.0011728546,0.0000017381867],"about_ca_topic_score_codex":0.0770595,"about_ca_topic_score_gemma":0.22367482,"teacher_disagreement_score":0.9229405,"about_ca_system_score_codex":0.00067125453,"about_ca_system_score_gemma":0.0003940826,"threshold_uncertainty_score":0.15322196},"labels":[],"label_agreement":null},{"id":"W1536258309","doi":"10.1029/2003gl017192","title":"Sensitivity study of the spectral dispersion of the cloud droplet size distribution on the indirect aerosol effect","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":133,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Cloud albedo; Aerosol; Atmospheric sciences; Dispersion (optics); Albedo (alchemy); Liquid water content; Environmental science; Scaling; Atmosphere (unit); Cloud computing; Meteorology; Computational physics; Cloud cover; Physics; Optics; Mathematics","score_opus":0.013683548602339089,"score_gpt":0.25839411950570806,"score_spread":0.24471057090336898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1536258309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932679,0.00012400393,0.005288947,0.00005063004,0.000017708642,0.00003515143,0.00027576167,0.00008358252,0.0008562213],"genre_scores_gemma":[0.9988772,0.000036431822,0.0008308082,0.00001971123,0.000005088264,0.0000064528367,0.00014516203,0.000011363055,0.00006771734],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993611,0.00027040497,0.000030079113,0.0001397904,0.00012361615,0.0000750033],"domain_scores_gemma":[0.9900149,0.008595383,0.00027286037,0.0005845191,0.00041478546,0.000117570635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014568911,0.0006600243,0.0004214116,0.0006051303,0.00029888682,0.00046935596,0.00046035947,0.0007928178,0.000752394],"category_scores_gemma":[0.0076936777,0.00029882498,0.00086296664,0.00046900712,0.00039819867,0.0004907439,0.0006486656,0.0004538638,0.00007453682],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086247094,0.00020898179,0.07772691,0.00014261993,0.0007059986,0.00050624,0.00011408799,0.8438936,0.06536604,0.00065072963,0.00030558417,0.009516709],"study_design_scores_gemma":[0.00012347843,0.00078554725,0.15392478,0.000032897307,0.00046262014,0.00041288542,0.0001353938,0.7742309,0.06815231,0.0007365626,0.00087507523,0.00012764784],"about_ca_topic_score_codex":0.019701447,"about_ca_topic_score_gemma":0.0060454304,"teacher_disagreement_score":0.019701447,"about_ca_system_score_codex":0.00074222416,"about_ca_system_score_gemma":0.00029408414,"threshold_uncertainty_score":0.039173543},"labels":[],"label_agreement":null},{"id":"W1537080486","doi":"10.1002/2015gl064988","title":"Imprints of impulse‐excited hydromagnetic waves on electrons in the Van Allen radiation belts","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Physics; Magnetosphere; Van Allen radiation belt; Van Allen Probes; Electron; Impulse (physics); Electromagnetic radiation; Excited state; Computational physics; Atomic physics; Energy flux; Resonance (particle physics); Radiation; Geophysics; Quantum electrodynamics; Plasma; Classical mechanics; Optics; Astronomy; Nuclear physics","score_opus":0.02126068980466993,"score_gpt":0.3001593264710361,"score_spread":0.27889863666636616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1537080486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991059,0.000052327705,0.00010026373,0.0000126507275,0.0000012340096,7.6219976e-7,0.000021225092,0.0000047120448,0.0007008644],"genre_scores_gemma":[0.99983704,0.000015421658,0.00002981469,0.0000024943804,0.0000012897099,4.759006e-7,0.00002339258,0.0000016375512,0.00008846616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995196,0.0000067561627,0.0000022009883,0.000013610818,0.000011195303,0.000014376932],"domain_scores_gemma":[0.9997316,0.00007408134,0.00009891892,0.000025606121,0.000028720659,0.000041086292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011257012,0.00008044124,0.0001324378,0.0005448475,0.00018727458,0.0005521354,0.00018114534,0.00015620323,0.0010214546],"category_scores_gemma":[0.00050677144,0.00010609216,0.00007834296,0.00027559476,0.0004004104,0.00031105205,0.0004256601,0.00022641169,0.00008623593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011393541,0.00008532972,0.5332196,0.00009065638,0.000119668366,0.0009756467,0.0043499777,0.0023454532,0.41358486,0.0063146525,0.00039036048,0.037384477],"study_design_scores_gemma":[0.0000057167554,0.00004282622,0.99323684,0.000009694121,0.000010266958,0.00008457495,0.0005343406,0.001005199,0.003905524,0.0005481722,0.00060957245,0.000007368163],"about_ca_topic_score_codex":0.002460403,"about_ca_topic_score_gemma":0.0025868965,"teacher_disagreement_score":0.002460403,"about_ca_system_score_codex":0.00022768482,"about_ca_system_score_gemma":0.00006478282,"threshold_uncertainty_score":0.0048921704},"labels":[],"label_agreement":null},{"id":"W1538635073","doi":"10.1029/2012gl051472","title":"Observations of Mercury's northern cusp region with MESSENGER's Magnetometer","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Magnetosphere; Physics; Solar wind; Geophysics; Interplanetary magnetic field; Magnetometer; Cusp (singularity); Magnetopause; Mercury's magnetic field; Magnetic field; Astrophysics; Atmospheric sciences; Geometry","score_opus":0.06952945845979602,"score_gpt":0.2956006150147204,"score_spread":0.22607115655492438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1538635073","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913442,0.00012643282,0.00044429293,0.00017107095,0.00001254759,0.000009526913,0.0015681818,0.00012834427,0.006195425],"genre_scores_gemma":[0.9968798,0.00006965118,0.0009751605,0.00003492302,0.000017539676,0.0000065311,0.0008097358,0.0000089953055,0.0011974775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.0000036717029,0.0000014272306,0.000011682989,0.000038894304,0.00001538645],"domain_scores_gemma":[0.99985933,0.000014597653,0.000043264823,0.000012396276,0.00003375653,0.000036647954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009447559,0.00011614949,0.00010802792,0.00047706283,0.0002993782,0.00015342131,0.00010934446,0.00016352207,0.0008908304],"category_scores_gemma":[0.00024286626,0.00007880947,0.00010227937,0.0003250492,0.00011970811,0.000120820725,0.00038686843,0.00019186821,0.00022851386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006308479,0.00007826246,0.6455895,0.0001333391,0.00008700454,0.0006600553,0.0017866726,0.0004251339,0.27858326,0.0009228219,0.008750507,0.062352624],"study_design_scores_gemma":[0.00002434487,0.00010924462,0.9766177,0.000011391488,0.000025182517,0.0003327556,0.00013423651,0.0006090303,0.012172332,0.00019595253,0.009754579,0.000013301575],"about_ca_topic_score_codex":0.005344414,"about_ca_topic_score_gemma":0.012996032,"teacher_disagreement_score":0.005344414,"about_ca_system_score_codex":0.00025777088,"about_ca_system_score_gemma":0.00016240437,"threshold_uncertainty_score":0.010626614},"labels":[],"label_agreement":null},{"id":"W1538984895","doi":"10.1029/2004gl021286","title":"Feeding methane vents and gas hydrate deposits at south Hydrate Ridge","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":245,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"United States Science Support Program; Pennsylvania State University; National Science Foundation","keywords":"Clathrate hydrate; Geology; Methane; Ridge; Seafloor spreading; Petrology; Turbidite; Geomorphology; Hydrate; Geochemistry; Sediment; Paleontology; Chemistry","score_opus":0.026799603773247166,"score_gpt":0.27781323827683035,"score_spread":0.25101363450358316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1538984895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995714,0.000013343423,0.000021003625,0.000009894367,2.901833e-7,3.724361e-7,0.000057833695,0.000006288127,0.00031957342],"genre_scores_gemma":[0.9997255,0.000013406941,0.000028199247,0.0000018799792,5.5279827e-7,6.5636215e-7,0.000080611215,0.0000010720066,0.00014803585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995303,0.0000037071454,0.0000037762304,0.000015503554,0.000011514485,0.000012327866],"domain_scores_gemma":[0.999858,0.000021163549,0.000052774092,0.000012188791,0.000021120299,0.00003473207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008043088,0.00014841248,0.0001055221,0.0006364363,0.0003782133,0.00025341235,0.00017125903,0.00017923515,0.0010520272],"category_scores_gemma":[0.00033275745,0.0002173139,0.00010011087,0.0003334259,0.000517447,0.00019260067,0.0005047847,0.00010964599,0.00012694276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002510898,0.000009640441,0.94037104,0.000031559517,0.00003239416,0.0005704342,0.0015003027,0.00076824205,0.051921304,0.00020998095,0.00013559495,0.0041984697],"study_design_scores_gemma":[0.0000023527703,0.000010610042,0.9979165,0.0000015519586,0.000004861561,0.00006383169,0.00023760063,0.00022338252,0.0013518487,0.000033780438,0.00015142794,0.000002298023],"about_ca_topic_score_codex":0.026062652,"about_ca_topic_score_gemma":0.053612657,"teacher_disagreement_score":0.026062652,"about_ca_system_score_codex":0.00050298497,"about_ca_system_score_gemma":0.00024814208,"threshold_uncertainty_score":0.051821947},"labels":[],"label_agreement":null},{"id":"W1539115379","doi":"10.1029/2001gl014394","title":"Improved mapping functions for atmospheric refraction correction in SLR","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"GNSS positioning and interference","field":"Engineering","cited_by":152,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Radiosonde; Elevation (ballistics); Ray tracing (physics); Remote sensing; Geodesy; Elevation angle; Atmospheric refraction; Data set; Satellite; Satellite laser ranging; Geology; Lidar; Refraction; Meteorology; Laser ranging; Optics; Physics; Laser; Computer science; Geometry; Mathematics","score_opus":0.0390548298331476,"score_gpt":0.2766028583128544,"score_spread":0.23754802847970682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1539115379","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021647342,0.000113618225,0.97604525,0.000048352395,0.000039281214,0.000015825204,0.000088642555,0.0012745626,0.00072716293],"genre_scores_gemma":[0.27303627,0.0002485633,0.7225574,0.000059881713,0.00009686919,0.00015473837,0.0004885047,0.00053717004,0.002820555],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996045,0.00012950505,0.000017000979,0.000053282594,0.00015637315,0.000039389073],"domain_scores_gemma":[0.999019,0.00034005224,0.00010431516,0.0002126903,0.00030133914,0.000022643217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010563144,0.0010796362,0.00044958066,0.0008954398,0.0002705888,0.00045952288,0.0010216774,0.0006327137,0.0013853373],"category_scores_gemma":[0.004443542,0.0002739838,0.00064813544,0.000749143,0.0002493849,0.0011262306,0.00045191785,0.0008132976,0.00092604064],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000108896915,0.000056089233,0.0028081378,0.000056394314,0.00005012854,0.000097146694,0.00012663384,0.77216697,0.013323212,0.021543257,0.0023786477,0.18728445],"study_design_scores_gemma":[0.0000053504914,0.0000113471,0.00044130403,0.000002979531,0.0000042994125,0.000017978195,0.0000037599339,0.9940826,0.0017327808,0.0020723832,0.0016151101,0.000010143161],"about_ca_topic_score_codex":0.0069104973,"about_ca_topic_score_gemma":0.0044827806,"teacher_disagreement_score":0.0069104973,"about_ca_system_score_codex":0.00051986997,"about_ca_system_score_gemma":0.0005171884,"threshold_uncertainty_score":0.01374054},"labels":[],"label_agreement":null},{"id":"W1539758185","doi":"10.1002/2015gl064700","title":"Using patchy pulsating aurora to remote sense magnetospheric convection","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Convection; Physics; Geophysics; Convection cell; Geology; Radar; Azimuth; Magnetosphere; Mechanics; Plasma; Combined forced and natural convection; Astronomy; Computer science; Natural convection","score_opus":0.06533171286103201,"score_gpt":0.34170251725821066,"score_spread":0.27637080439717865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1539758185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9857875,0.00028211312,0.011607972,0.000035572542,0.000020381067,0.000020129313,0.0003157246,0.00013323285,0.0017975144],"genre_scores_gemma":[0.9892211,0.000094005285,0.0103291,0.000011135136,0.000019906794,0.0000072647854,0.00015696809,0.000012977783,0.00014756393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993277,0.000012564248,0.000003334943,0.000033490734,0.000006955797,0.0000109029825],"domain_scores_gemma":[0.9997812,0.000071364906,0.000051066054,0.00004072941,0.00001935242,0.00003642798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002091326,0.00019320413,0.00016947491,0.0007862655,0.0001359002,0.00046405953,0.00011873814,0.00016194617,0.0006369611],"category_scores_gemma":[0.00057326246,0.00010192147,0.00016881943,0.00061375817,0.00017281213,0.0004327047,0.0002969902,0.00018597025,0.00014576038],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080224907,0.00009345856,0.41442817,0.00015108923,0.00018853726,0.00030246115,0.0007045328,0.012335076,0.32229766,0.0006988771,0.0007068054,0.247291],"study_design_scores_gemma":[0.000036112295,0.00022313681,0.928326,0.000035418278,0.000070734786,0.00038667629,0.00032895847,0.052727982,0.014980884,0.0009201889,0.0019334552,0.000030390464],"about_ca_topic_score_codex":0.0018956177,"about_ca_topic_score_gemma":0.0034202554,"teacher_disagreement_score":0.0018956177,"about_ca_system_score_codex":0.000103894025,"about_ca_system_score_gemma":0.000088137946,"threshold_uncertainty_score":0.0037691593},"labels":[],"label_agreement":null},{"id":"W1540501767","doi":"10.1029/2010gl046484","title":"Using multiple RADARSAT InSAR pairs to estimate a full three-dimensional solution for glacial ice movement","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agency for Natural Resources and Energy; Canadian Space Agency; Natural Resources Canada; U.S. Geological Survey","keywords":"Geology; Geodesy; Interferometric synthetic aperture radar; Azimuth; Glacier; Displacement (psychology); Synthetic aperture radar; Terrain; Latitude; Remote sensing; Geomorphology; Optics; Geography; Physics; Cartography","score_opus":0.14093802293454852,"score_gpt":0.3283803785155722,"score_spread":0.1874423555810237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1540501767","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.41148213,0.00081587967,0.5749685,0.00022585131,0.00011740289,0.00012797696,0.0033019579,0.0028016486,0.006158577],"genre_scores_gemma":[0.48959732,0.0003167563,0.50281584,0.000101136895,0.00006165358,0.00008508616,0.0043434747,0.00011912237,0.002559563],"study_design_codex":"design_other","study_design_gemma":"not_applicable","domain_scores_codex":[0.9999124,0.000010065803,0.0000036278282,0.000023371753,0.00003896294,0.000011670002],"domain_scores_gemma":[0.99989164,0.000014982567,0.000024089777,0.000021149894,0.00003848581,0.00000961196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002316345,0.0009840858,0.00033210745,0.0009628554,0.0004260123,0.00061193726,0.00052869174,0.0004146081,0.001433892],"category_scores_gemma":[0.00066784257,0.00040316317,0.0003442972,0.001112637,0.00018532573,0.00041700443,0.0004126028,0.00038984092,0.00086548436],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001520482,0.00018004223,0.045657136,0.00015872013,0.0004356088,0.00032011353,0.0003029845,0.31289294,0.0768074,0.0024992218,0.007979367,0.5526145],"study_design_scores_gemma":[0.00005232555,0.00009038459,0.060739644,0.000029071804,0.00012517937,0.00025524665,0.00016515738,0.91813207,0.011427481,0.0019610326,0.0069635827,0.000058865433],"about_ca_topic_score_codex":0.030120827,"about_ca_topic_score_gemma":0.07309439,"teacher_disagreement_score":0.030120827,"about_ca_system_score_codex":0.00036154044,"about_ca_system_score_gemma":0.0010618455,"threshold_uncertainty_score":0.059890985},"labels":[],"label_agreement":null},{"id":"W1540555244","doi":"10.1029/2008gl036141","title":"Spatiotemporal patterns of changes in maximum and minimum temperatures in multi‐model simulations","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Longwave; Cloud cover; Climatology; Atmospheric sciences; Shortwave radiation; Latitude; Shortwave; Atmosphere (unit); Diurnal cycle; Outgoing longwave radiation; Climate model; Water vapor; Radiative transfer; Climate change; Radiation; Meteorology; Geography; Convection; Geology; Cloud computing","score_opus":0.06193084669610673,"score_gpt":0.3386738163674456,"score_spread":0.2767429696713389,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1540555244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966515,0.00009901097,0.0010601562,0.00014510404,0.00001138175,0.000008834266,0.0010009112,0.00010427378,0.0009188108],"genre_scores_gemma":[0.9978744,0.000052226387,0.0006717061,0.000019975172,0.000004534174,0.000014682054,0.0012115296,0.000021132964,0.00012991964],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99966836,0.00009590675,0.00003268959,0.000099762714,0.000045416476,0.000057889745],"domain_scores_gemma":[0.99868757,0.0006467746,0.00020414765,0.00016973377,0.00015686556,0.00013480589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011083948,0.00041872184,0.0004597987,0.0007340994,0.00039156555,0.000822339,0.00076307484,0.0007759864,0.0009486828],"category_scores_gemma":[0.003996668,0.00046418337,0.000799715,0.0008250275,0.00034375078,0.00071746274,0.000575306,0.0005873213,0.00013266645],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039547283,0.00014253228,0.13388485,0.00006521921,0.00034035154,0.00017494727,0.00016643893,0.85398245,0.004051442,0.0012787373,0.0015142302,0.004003315],"study_design_scores_gemma":[0.00009212986,0.00007678631,0.055792358,0.000016345928,0.000058508776,0.00004094102,0.000119984914,0.94065773,0.0016830371,0.0005411531,0.0008861184,0.000034847206],"about_ca_topic_score_codex":0.018822167,"about_ca_topic_score_gemma":0.014733182,"teacher_disagreement_score":0.018822167,"about_ca_system_score_codex":0.00083425915,"about_ca_system_score_gemma":0.00047422957,"threshold_uncertainty_score":0.03742522},"labels":[],"label_agreement":null},{"id":"W1540963639","doi":"10.1029/2012gl052876","title":"On the sunrise oscillation of the F region in the equatorial ionosphere","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Sunrise; Ionosonde; Ionosphere; Sunset; Altitude (triangle); Physics; Atmospheric sciences; Morning; F region; Jump; Geodesy; Geology; Plasma; Meteorology; Geophysics; Astronomy; Electron density; Geometry; Nuclear physics","score_opus":0.03033998226719907,"score_gpt":0.2902897575530681,"score_spread":0.259949775285869,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1540963639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993357,0.00069011934,0.00095244823,0.00012424435,0.000014484571,0.0000038213607,0.00015304865,0.000023492716,0.0046813013],"genre_scores_gemma":[0.9991304,0.0003048787,0.00016902207,0.000018968034,0.000022787903,0.0000012805078,0.00006837058,0.000007487576,0.000276743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999972,0.0000058964956,0.0000010493234,0.000008408837,0.0000050583367,0.000007603072],"domain_scores_gemma":[0.999819,0.00007468428,0.000046565074,0.0000128052,0.000021598815,0.000025341895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011022981,0.00011020542,0.00010180928,0.0003272578,0.00017266226,0.00027786693,0.00009801674,0.00016917702,0.001094936],"category_scores_gemma":[0.0005704233,0.00006937528,0.00009114211,0.00022499205,0.00022047156,0.0002710484,0.00017728374,0.000113653885,0.0001566988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020488878,0.00008780802,0.7168878,0.00036135607,0.00016212619,0.0016891665,0.0026750606,0.009039522,0.14216296,0.010802663,0.0037562351,0.110326484],"study_design_scores_gemma":[0.000016563352,0.0000750451,0.9909546,0.000019512956,0.000022603952,0.00016788101,0.00024135014,0.0042230105,0.0014730768,0.0008341733,0.0019600466,0.000012191359],"about_ca_topic_score_codex":0.0021866374,"about_ca_topic_score_gemma":0.0029268365,"teacher_disagreement_score":0.0021866374,"about_ca_system_score_codex":0.0001777453,"about_ca_system_score_gemma":0.000077365345,"threshold_uncertainty_score":0.004347861},"labels":[],"label_agreement":null},{"id":"W1541130000","doi":"10.1029/2011gl049899","title":"Global CO<sub>2</sub>fluxes inferred from surface air-sample measurements and from TCCON retrievals of the CO<sub>2</sub>total column","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":114,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Inversion (geology); Environmental science; Northern Hemisphere; Atmospheric sciences; Southern Hemisphere; Meteorology; Climatology; Geology; Structural basin","score_opus":0.036983564638812125,"score_gpt":0.263944733772303,"score_spread":0.22696116913349085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1541130000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934429,0.00007574411,0.0014151476,0.00003183013,0.000009088307,0.000010552168,0.002455056,0.00006647015,0.0024931277],"genre_scores_gemma":[0.99112856,0.00005446807,0.0030942885,0.000025573825,0.0000136630015,0.0000113314345,0.005354845,0.00002944026,0.00028771517],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998697,0.000011126042,0.0000057275397,0.0000462303,0.000033496064,0.00003371174],"domain_scores_gemma":[0.9996427,0.000053961292,0.00009584156,0.000056426557,0.00011978082,0.000031331918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002755249,0.00059636607,0.00025808366,0.00096726976,0.00024010017,0.000500298,0.00024270144,0.0003713727,0.0006706592],"category_scores_gemma":[0.00071474933,0.00021154218,0.00028831797,0.0012410602,0.0002990228,0.00047809238,0.00041690603,0.00021105826,0.00014337071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007144208,0.00011010197,0.869935,0.00012036247,0.00029286838,0.00019303127,0.00026344895,0.034661356,0.05430095,0.0007407666,0.0015003807,0.037167426],"study_design_scores_gemma":[0.000031275802,0.000055074208,0.95403063,0.000016931135,0.00011642432,0.00008831572,0.00011555477,0.031736936,0.011625025,0.00019934072,0.001956933,0.00002756368],"about_ca_topic_score_codex":0.04624276,"about_ca_topic_score_gemma":0.092111625,"teacher_disagreement_score":0.04624276,"about_ca_system_score_codex":0.00069316634,"about_ca_system_score_gemma":0.00050277985,"threshold_uncertainty_score":0.0919472},"labels":[],"label_agreement":null},{"id":"W1542235505","doi":"10.1029/2011gl049508","title":"Skillful predictions of decadal trends in global mean surface temperature","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Environmental science; El Niño Southern Oscillation; Volcano; Mean radiant temperature; Greenhouse gas; Surface air temperature; Atmospheric sciences; Climate change; Geology; Oceanography","score_opus":0.04227159966343597,"score_gpt":0.3149873100526206,"score_spread":0.27271571038918463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542235505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9554171,0.000086313,0.04110803,0.00021703927,0.000036520985,0.000016751601,0.00093427143,0.0003865024,0.0017974459],"genre_scores_gemma":[0.99382555,0.000040452822,0.005356643,0.000019331945,0.00001659079,0.000006791259,0.0005183962,0.000021311691,0.00019490898],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998883,0.00003149061,0.000009370885,0.000037485363,0.000020180416,0.000013169245],"domain_scores_gemma":[0.99903846,0.0004064673,0.0001739128,0.00019560219,0.00013743,0.000048242284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078809395,0.00044571736,0.0001925129,0.00028185046,0.00019044928,0.000506167,0.0003319014,0.00037961683,0.0005673346],"category_scores_gemma":[0.005656657,0.00022600192,0.00019229863,0.0002204165,0.00022794961,0.0007412512,0.00031461156,0.00041938754,0.00013662704],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000797414,0.000027871141,0.041900326,0.000017011016,0.000050986575,0.000029807417,0.000032495664,0.9436874,0.0032938125,0.0010299238,0.00045538502,0.009395188],"study_design_scores_gemma":[0.00001516531,0.00002420961,0.018714853,0.0000051089214,0.000014399048,0.000015332795,0.00000867108,0.9782357,0.0016484772,0.0010399637,0.00026962103,0.00000850236],"about_ca_topic_score_codex":0.010498216,"about_ca_topic_score_gemma":0.010008519,"teacher_disagreement_score":0.010498216,"about_ca_system_score_codex":0.0003441039,"about_ca_system_score_gemma":0.00048039522,"threshold_uncertainty_score":0.020874262},"labels":[],"label_agreement":null},{"id":"W1542261836","doi":"10.1002/grl.50599","title":"The location of old groundwater in hydrogeologic basins and layered aquifer systems","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Aquifer; Groundwater; Geology; Hydrogeology; Groundwater recharge; Groundwater flow; Groundwater discharge; Groundwater model; Permeability (electromagnetism); Hydraulic conductivity; Structural basin; Hydrology (agriculture); Soil science; Geomorphology; Geotechnical engineering; Soil water","score_opus":0.023651661968600968,"score_gpt":0.26265382766337164,"score_spread":0.23900216569477067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542261836","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965031,0.0000921814,0.0025938412,0.000019372366,0.000001283895,0.000002598855,0.00009157498,0.000022763077,0.000673149],"genre_scores_gemma":[0.9995265,0.000034535264,0.00035126798,0.0000023641699,3.61399e-7,0.0000013905199,0.000022103892,0.0000015931552,0.000059823087],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.000010819777,0.000003692995,0.000014488903,0.000006962866,0.000018797087],"domain_scores_gemma":[0.99985385,0.00003802276,0.00006006137,0.000013674428,0.0000132895675,0.00002107693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012807046,0.00009790726,0.00013015936,0.00037813163,0.00029167495,0.0007489192,0.00023670927,0.00024307777,0.0006916216],"category_scores_gemma":[0.00049546297,0.0001693082,0.0001479455,0.0005177305,0.0008844357,0.00058627146,0.00054827303,0.000117009906,0.000042205855],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002287486,0.000063436535,0.41368064,0.000114925475,0.000063944746,0.0004829807,0.0008490815,0.49620643,0.04828843,0.022796314,0.00037170094,0.016853435],"study_design_scores_gemma":[0.00005796389,0.00016345124,0.42879504,0.00006204335,0.00006400593,0.00031628582,0.0008423484,0.53153193,0.013413586,0.02183696,0.0028285768,0.000087904395],"about_ca_topic_score_codex":0.006794052,"about_ca_topic_score_gemma":0.005458431,"teacher_disagreement_score":0.006794052,"about_ca_system_score_codex":0.0007946876,"about_ca_system_score_gemma":0.00034027442,"threshold_uncertainty_score":0.013509035},"labels":[],"label_agreement":null},{"id":"W1542450125","doi":"10.1029/2004gl020389","title":"Variability of atmospheric winds and waves in the Arctic polar mesosphere during a stratospheric sudden warming","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Sudden stratospheric warming; Stratosphere; Mesopause; Atmospheric sciences; Polar night; Climatology; Environmental science; Mesosphere; Polar vortex; Amplitude; Zonal and meridional; Polar; Arctic; Geology; Physics; Oceanography","score_opus":0.009989774624822376,"score_gpt":0.26022786977982354,"score_spread":0.2502380951550012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1542450125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997671,0.00001431134,0.000018085726,0.0000063805046,0.0000014087092,0.0000010518564,0.00008117125,0.0000020261416,0.00010845983],"genre_scores_gemma":[0.999509,0.000025388796,0.000058869482,0.0000060728034,0.0000036384056,0.0000020841865,0.00030335638,0.000001007791,0.00009056345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.000005603783,0.0000023637792,0.0000106432635,0.000018032857,0.000017591641],"domain_scores_gemma":[0.9998331,0.00001942517,0.000046758105,0.000011154234,0.00004784111,0.000041803753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014018586,0.00015917077,0.00011916235,0.0003486375,0.00034357945,0.00034211093,0.00010144364,0.00018007917,0.00020029172],"category_scores_gemma":[0.00033920896,0.00011182378,0.000102091115,0.00034019497,0.0002105355,0.000114402734,0.00016162747,0.0001645296,0.000060073133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002574226,0.000048684447,0.9670848,0.000010741849,0.000072807685,0.00020878411,0.0004976362,0.000716485,0.026456721,0.00005167188,0.00022525183,0.0043689427],"study_design_scores_gemma":[0.0000018986669,0.00001831538,0.9992859,8.0431505e-7,0.000005810175,0.000020545927,0.000055769466,0.00021862071,0.00028450147,0.000004565072,0.00010188607,0.0000014592431],"about_ca_topic_score_codex":0.071523674,"about_ca_topic_score_gemma":0.14254516,"teacher_disagreement_score":0.071523674,"about_ca_system_score_codex":0.0005819369,"about_ca_system_score_gemma":0.00037908123,"threshold_uncertainty_score":0.14221472},"labels":[],"label_agreement":null},{"id":"W1543562910","doi":"10.1002/2013gl057706","title":"The role of vertical eddy flux in Southern Ocean heat uptake","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Isopycnal; Eddy; Heat flux; Eddy covariance; Geology; Wind stress; Climatology; Atmospheric sciences; Ocean heat content; Flux (metallurgy); Eddy diffusion; Ocean current; Turbulence; Meteorology; Mechanics; Heat transfer; Physics; Materials science","score_opus":0.013053026528446079,"score_gpt":0.23858227146941033,"score_spread":0.22552924494096424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1543562910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960115,0.00020306697,0.0017796431,0.00022986376,0.00001552096,0.000004388786,0.00012734927,0.000059733185,0.0015689644],"genre_scores_gemma":[0.9995753,0.000059415433,0.00013931961,0.000008263176,0.00000290631,0.0000021642813,0.00002444006,0.000012522848,0.00017574689],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998839,0.000041437444,0.000007971406,0.000021349177,0.000013055245,0.000032258096],"domain_scores_gemma":[0.9995752,0.00020212315,0.00006867862,0.000051734365,0.00003819735,0.000064010506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045011065,0.0005247871,0.0003579649,0.00025872324,0.00036508325,0.0010072436,0.0004107667,0.00069904065,0.0010729944],"category_scores_gemma":[0.0015642592,0.00041489792,0.0005893812,0.00026970843,0.0007285581,0.0010269833,0.00084180734,0.0003622076,0.00011427767],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005957589,0.00011039081,0.086290985,0.00011216194,0.00014963235,0.0003867353,0.00017624813,0.8302761,0.06510795,0.008902563,0.00036157493,0.0075299093],"study_design_scores_gemma":[0.00012361872,0.0001683973,0.058863904,0.000019901567,0.00006466761,0.000090913905,0.000100675716,0.9301629,0.005953024,0.003875351,0.0005240338,0.000052636704],"about_ca_topic_score_codex":0.011168422,"about_ca_topic_score_gemma":0.006517171,"teacher_disagreement_score":0.011168422,"about_ca_system_score_codex":0.0009307775,"about_ca_system_score_gemma":0.00080560177,"threshold_uncertainty_score":0.022206843},"labels":[],"label_agreement":null},{"id":"W1546980190","doi":"10.1029/2009gl037400","title":"Observations of northern latitude ground‐surface and surface‐air temperatures","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"","keywords":"Borehole; Snow cover; Latitude; Snow; Climatology; Environmental science; Period (music); Proxy (statistics); Climate change; Surface air temperature; Atmospheric sciences; Geology; Physical geography; Geography; Geodesy; Geomorphology","score_opus":0.08368074021052252,"score_gpt":0.3099426131119779,"score_spread":0.22626187290145539,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1546980190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9866838,0.00014007108,0.0007243077,0.00004694698,0.0000074132436,0.000014261451,0.0044376845,0.000058915935,0.007886626],"genre_scores_gemma":[0.9939977,0.00014815378,0.0011768386,0.00001690725,0.000003802472,0.000010823095,0.0028452773,0.000009124056,0.0017913989],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986887,0.0000071694626,0.0000048210954,0.000026619044,0.00005684809,0.00003571723],"domain_scores_gemma":[0.9995684,0.000028755514,0.00008977777,0.000028551607,0.00022825618,0.000056251723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012737988,0.00015164082,0.00013729245,0.00048324937,0.00061614334,0.00036992523,0.00022515644,0.00011298738,0.0014338183],"category_scores_gemma":[0.0005433021,0.00009627981,0.000092384034,0.0010976143,0.00024209847,0.0001968696,0.00022807984,0.0002031618,0.00025091082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013234417,0.000022762726,0.93670034,0.00006356844,0.000053963213,0.00008412788,0.0015497566,0.0007911892,0.029695414,0.00019804089,0.0015168105,0.029191699],"study_design_scores_gemma":[0.0000010420792,0.000004652498,0.9981035,0.0000024511962,0.0000037485331,0.000017788287,0.00014235306,0.00013539064,0.000548226,0.000010275444,0.0010276042,0.0000029077876],"about_ca_topic_score_codex":0.78027916,"about_ca_topic_score_gemma":0.9479555,"teacher_disagreement_score":0.78027916,"about_ca_system_score_codex":0.0014324739,"about_ca_system_score_gemma":0.001569655,"threshold_uncertainty_score":0.4420296},"labels":[],"label_agreement":null},{"id":"W1547652159","doi":"10.1029/2011gl047120","title":"Drivers of past and future Southern Ocean change: Stratospheric ozone versus greenhouse gas impacts","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Greenhouse gas; Environmental science; Ozone layer; Climatology; Ozone depletion; Atmospheric sciences; Ozone; Climate change; Atmosphere (unit); Climate model; Circumpolar star; Stratosphere; Meteorology; Oceanography; Geology; Geography","score_opus":0.047945266219597306,"score_gpt":0.2516322609604747,"score_spread":0.2036869947408774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1547652159","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98649406,0.0012202438,0.0036042333,0.0016452145,0.00004508038,0.000015715004,0.0013754076,0.000051650368,0.005548457],"genre_scores_gemma":[0.998058,0.00054898736,0.00041884894,0.00005582368,0.000029969817,0.000006508576,0.00029545004,0.000012138013,0.0005742194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999236,0.000018085795,0.0000042586666,0.000022360427,0.00001074864,0.000020892896],"domain_scores_gemma":[0.9997055,0.000101633676,0.000107310836,0.000012388271,0.000024131597,0.000049082617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030199203,0.00037901438,0.00028943422,0.00050011463,0.0002990929,0.0011602389,0.00047224478,0.0010041241,0.0022781834],"category_scores_gemma":[0.0011112092,0.00026552862,0.00061333535,0.0006899741,0.0004735662,0.0011051354,0.00080812984,0.000451285,0.00013000579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035517302,0.00011641971,0.49283653,0.00032871854,0.00052995724,0.00038592215,0.0003738152,0.436007,0.009324851,0.039422214,0.0021415048,0.018177904],"study_design_scores_gemma":[0.00012336734,0.00020276038,0.4241041,0.000072142924,0.00037894427,0.00018648201,0.0007014894,0.53664154,0.0028702386,0.026740212,0.007876591,0.00010213037],"about_ca_topic_score_codex":0.027818704,"about_ca_topic_score_gemma":0.024461595,"teacher_disagreement_score":0.027818704,"about_ca_system_score_codex":0.0009210149,"about_ca_system_score_gemma":0.00075905514,"threshold_uncertainty_score":0.055313587},"labels":[],"label_agreement":null},{"id":"W1547681715","doi":"10.1002/grl.50268","title":"Further observations of a decreasing atmospheric CO<sub>2</sub> uptake capacity in the Canada Basin (Arctic Ocean) due to sea ice loss","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Fisheries and Oceans Canada; McGill University; University of British Columbia; University of Manitoba","funders":"Division of Arctic Sciences; Social Sciences and Humanities Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; University of Manitoba; ArcticNet; Canada Research Chairs; Canadian Institutes of Health Research","keywords":"Sink (geography); Sea ice; Arctic; Arctic ice pack; Environmental science; Atmospheric sciences; Climatology; Cryosphere; Structural basin; Antarctic sea ice; Canada Basin; Geology; Oceanography; Geomorphology; Geography","score_opus":0.03272453564372045,"score_gpt":0.2373118541188599,"score_spread":0.20458731847513945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1547681715","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989359,0.000032204287,0.00009513412,0.000033559605,0.0000011580089,0.0000027431213,0.00045908685,0.0000087827775,0.00043142625],"genre_scores_gemma":[0.99941874,0.00002171518,0.00008775254,0.000015972346,6.492167e-7,0.0000019485205,0.00029061988,0.0000021514272,0.00016049462],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999485,0.000003732906,0.0000016695831,0.000009180973,0.000017679988,0.000019257888],"domain_scores_gemma":[0.9998343,0.000023755072,0.000027427528,0.000008938993,0.00006714304,0.000038452457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012006032,0.0001898171,0.00016482198,0.00021694724,0.00058344804,0.00045276448,0.000255634,0.0002481033,0.000758231],"category_scores_gemma":[0.00029522862,0.00009818111,0.00018464914,0.0003763341,0.00027747458,0.0001502089,0.00019669115,0.00030929432,0.000073884636],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038024658,0.00004982487,0.9347281,0.00004036419,0.00006703581,0.00029302892,0.00036283242,0.0021987727,0.056378447,0.00011462261,0.0005962244,0.004790444],"study_design_scores_gemma":[0.0000026607088,0.000011779005,0.9962457,0.0000016041498,0.000008318787,0.000027129965,0.00012084959,0.0014926719,0.0017239199,0.000015052752,0.00034802657,0.000002348645],"about_ca_topic_score_codex":0.81055844,"about_ca_topic_score_gemma":0.81651986,"teacher_disagreement_score":0.18944156,"about_ca_system_score_codex":0.0022985078,"about_ca_system_score_gemma":0.0016990167,"threshold_uncertainty_score":0.38111442},"labels":[],"label_agreement":null},{"id":"W1548063599","doi":"10.1029/2009gl041408","title":"A GCM‐based analysis of circulation controls on <i>δ</i><sup>18</sup>O in the southwest Yukon, Canada: Implications for climate reconstructions in the region","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Toronto","funders":"","keywords":"Paleoclimatology; Precipitation; Climatology; GCM transcription factors; Geology; Atmospheric circulation; General Circulation Model; Glacial period; Climate change; Period (music); Atmospheric sciences; Geography; Meteorology; Oceanography; Geomorphology","score_opus":0.05151946062659332,"score_gpt":0.3087934168365991,"score_spread":0.2572739562100058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1548063599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990632,0.000052277985,0.00006852335,0.00005170496,0.0000016657871,0.0000030244562,0.0004710853,0.000009018653,0.00027946266],"genre_scores_gemma":[0.9991653,0.000047858968,0.00019004995,0.0000115617195,0.0000011279797,0.000002127482,0.00047505464,0.0000036967012,0.00010331279],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000012110325,0.0000063870025,0.000025181997,0.000011271348,0.00002201538],"domain_scores_gemma":[0.99974674,0.00004634759,0.00003681434,0.000019557077,0.000103174265,0.000047340614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022561113,0.00016472676,0.00016021045,0.00041702387,0.0005134032,0.00059041014,0.0003069613,0.00019453061,0.0006474155],"category_scores_gemma":[0.00074188155,0.00015718426,0.0002523652,0.00084449153,0.00031601152,0.00020532969,0.00026354595,0.00017611598,0.00005396017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016567783,0.000019359995,0.97890806,0.0000315215,0.00014988685,0.00010743246,0.0002452219,0.009430959,0.0044853035,0.00045892806,0.0004616611,0.0055360436],"study_design_scores_gemma":[0.000020296244,0.000009782477,0.98414165,0.000008830267,0.000059611666,0.000024831503,0.00027239465,0.014156832,0.00048564552,0.00009040529,0.00071940967,0.000010282439],"about_ca_topic_score_codex":0.9071808,"about_ca_topic_score_gemma":0.9067384,"teacher_disagreement_score":0.092819214,"about_ca_system_score_codex":0.0048669185,"about_ca_system_score_gemma":0.0045687133,"threshold_uncertainty_score":0.18673164},"labels":[],"label_agreement":null},{"id":"W1548985879","doi":"10.1002/2013gl058731","title":"Can regional climate engineering save the summer Arctic sea ice?","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Arctic geoengineering; Sea ice; Environmental science; Arctic; Climatology; Arctic ice pack; Shortwave radiation; Arctic sea ice decline; Ice-albedo feedback; Arctic dipole anomaly; Climate model; Albedo (alchemy); Climate change; Geology; Oceanography; Drift ice; Radiation","score_opus":0.026480625940847213,"score_gpt":0.25397879746473084,"score_spread":0.22749817152388363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1548985879","genre_codex":"commentary","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19420901,0.045739528,0.029812602,0.42745718,0.0088634845,0.00009861087,0.0011926508,0.0013713796,0.2912555],"genre_scores_gemma":[0.92851895,0.018867647,0.008364523,0.020754423,0.001601016,0.000057391866,0.00024810943,0.00025698665,0.021330886],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995005,0.00022304217,0.000013971332,0.000055942757,0.00004923268,0.0001573905],"domain_scores_gemma":[0.9991365,0.00020895165,0.00014849554,0.00013073292,0.00015198527,0.00022330185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017108928,0.00042673756,0.00027358913,0.0002695637,0.00046490142,0.0020652658,0.00080487935,0.001609715,0.012829122],"category_scores_gemma":[0.0035798384,0.00012099804,0.00066064164,0.00040345365,0.00063840515,0.0029370736,0.001003882,0.00084630924,0.0014737641],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014518143,0.0007318423,0.0137757575,0.0012270375,0.00041226947,0.00047960778,0.000599326,0.054338213,0.0054803127,0.18361072,0.13099356,0.60689956],"study_design_scores_gemma":[0.00040831603,0.001053237,0.03173371,0.0010142631,0.0006152026,0.00056287425,0.0048543834,0.01913777,0.0073898905,0.28045085,0.6525784,0.00020107365],"about_ca_topic_score_codex":0.004856938,"about_ca_topic_score_gemma":0.008799311,"teacher_disagreement_score":0.012829122,"about_ca_system_score_codex":0.0008305645,"about_ca_system_score_gemma":0.0023094204,"threshold_uncertainty_score":0.04291767},"labels":[],"label_agreement":null},{"id":"W1549121058","doi":"10.1029/2012gl053025","title":"Deep mesoscale eddies in the Canada Basin, Arctic Ocean","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Eddy; Geology; Ocean gyre; Anticyclone; Mooring; Oceanography; Arctic; Canada Basin; Outflow; Climatology; Mesoscale meteorology; Structural basin; Boundary current; Oceanic basin; Ocean current; Meteorology; Subtropics; Geography; Paleontology; Turbulence","score_opus":0.019387836710250125,"score_gpt":0.25095945577624384,"score_spread":0.23157161906599372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1549121058","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997617,0.00019394199,0.00021940841,0.00003895179,0.000003238752,0.0000064463557,0.0009357842,0.000009924597,0.0009753563],"genre_scores_gemma":[0.9985446,0.00018972078,0.0002701936,0.000009850355,0.0000021328399,0.0000033281194,0.0006513613,0.000001654834,0.00032725465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999677,0.0000011935092,0.0000013391625,0.0000071235377,0.000006943725,0.000015710999],"domain_scores_gemma":[0.9999049,0.000009579016,0.000020565813,0.0000042234637,0.0000269416,0.000033796397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058039943,0.00017731264,0.000097919954,0.0004782966,0.0005460121,0.0003922115,0.00014873789,0.00012880775,0.00037408833],"category_scores_gemma":[0.00020573987,0.00010534636,0.00013963661,0.0007855753,0.00019100502,0.00010827151,0.00027651753,0.00011810533,0.00003306093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095169984,0.000028464241,0.96170515,0.000045411438,0.00009141469,0.0003955513,0.0005865837,0.008342928,0.010367127,0.0008555784,0.0011906383,0.016295902],"study_design_scores_gemma":[0.0000027122053,0.000003939077,0.99524176,0.000007788773,0.000009884834,0.000028219169,0.00019172297,0.0031832927,0.00023541746,0.00006353305,0.0010265755,0.0000052455575],"about_ca_topic_score_codex":0.8222081,"about_ca_topic_score_gemma":0.90290785,"teacher_disagreement_score":0.1777919,"about_ca_system_score_codex":0.0022734823,"about_ca_system_score_gemma":0.001653887,"threshold_uncertainty_score":0.35767788},"labels":[],"label_agreement":null},{"id":"W1549217243","doi":"10.1002/2014gl061401","title":"Constraints on the secular variation of Mercury's magnetic field from the combined analysis of MESSENGER and Mariner 10 data","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Carnegie Institution of Washington; Johns Hopkins University; National Aeronautics and Space Administration","keywords":"Secular variation; Equator; Mercury (programming language); Dipole; Magnetometer; Magnetic dip; Geodesy; Spacecraft; Magnetic field; Physics; Multipole expansion; Geophysics; Dynamo; Magnetic dipole; Geology; Latitude; Astronomy","score_opus":0.024371676856628874,"score_gpt":0.2825946276504499,"score_spread":0.258222950793821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1549217243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99726,0.00009864867,0.0007199329,0.00003718383,0.00000513853,0.000003508664,0.0005922958,0.00003949145,0.0012438985],"genre_scores_gemma":[0.9971637,0.00006861867,0.0010171931,0.0000136744675,0.000009890096,0.00000482467,0.0015317929,0.000019253182,0.00017106123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966455,0.00008475801,0.000018618312,0.00008155771,0.0000854261,0.00006511022],"domain_scores_gemma":[0.9990596,0.00028286566,0.0002315023,0.00014655184,0.00016391519,0.00011551576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00073175546,0.00034478892,0.0004617018,0.0014822221,0.00023632299,0.0005660032,0.0002143565,0.000178768,0.0006761785],"category_scores_gemma":[0.0016046307,0.00018340086,0.0003905549,0.0015883966,0.0002452039,0.0002430022,0.0006255872,0.00028921076,0.00029947638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041868677,0.000033070362,0.8835964,0.000054702665,0.00032922265,0.0003698984,0.00046809803,0.0026914119,0.08610562,0.00033578303,0.00068207993,0.024915135],"study_design_scores_gemma":[0.000010102389,0.00003396902,0.9932597,0.0000066574644,0.00006244034,0.00008085746,0.00008088693,0.0027565125,0.0025279904,0.00006485688,0.0011042908,0.000011736581],"about_ca_topic_score_codex":0.011284067,"about_ca_topic_score_gemma":0.036976784,"teacher_disagreement_score":0.011284067,"about_ca_system_score_codex":0.00040429799,"about_ca_system_score_gemma":0.000488663,"threshold_uncertainty_score":0.022436738},"labels":[],"label_agreement":null},{"id":"W1550470625","doi":"10.1002/grl.50640","title":"The role of the geothermal heat flux in driving the abyssal ocean circulation","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Abyssal zone; Geology; Seabed; Stratification (seeds); Ocean current; Geothermal heating; Buoyancy; Flux (metallurgy); Antarctic Bottom Water; Oceanography; Heat flux; Ocean heat content; Circulation (fluid dynamics); Geothermal gradient; Geophysics; Climatology; Bottom water; Geothermal energy; Mechanics; Heat transfer","score_opus":0.010171872719547833,"score_gpt":0.228904941763456,"score_spread":0.21873306904390816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1550470625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973093,0.00009481667,0.0011189472,0.00008524785,0.000009718907,0.0000033247281,0.00011143074,0.000024651938,0.0012424918],"genre_scores_gemma":[0.99942243,0.000079479,0.00031883115,0.000008344256,0.000004854756,0.0000017930046,0.00004138918,0.000008702011,0.00011425434],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999485,0.000012779809,0.0000037744815,0.000012224353,0.000010256308,0.000012381998],"domain_scores_gemma":[0.99987173,0.000050714534,0.000019476933,0.000015232986,0.000021203961,0.000021679965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015513273,0.00034085722,0.00019913944,0.00023719184,0.00036365644,0.0006857223,0.0002535049,0.00024189564,0.0010119823],"category_scores_gemma":[0.0008510014,0.00020294882,0.0003997899,0.00023360555,0.00038938888,0.00055893767,0.00046342757,0.0003146545,0.00012445051],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049611065,0.00010584798,0.29325143,0.00026420716,0.00024615487,0.00059969537,0.00032146313,0.51674926,0.16124746,0.005758325,0.00046441564,0.020495636],"study_design_scores_gemma":[0.00010942484,0.00016048343,0.30236408,0.0000269699,0.00009402608,0.00016506357,0.00025118867,0.6783176,0.015609331,0.0016232932,0.0012250029,0.000053478583],"about_ca_topic_score_codex":0.029452566,"about_ca_topic_score_gemma":0.020015439,"teacher_disagreement_score":0.029452566,"about_ca_system_score_codex":0.0005966366,"about_ca_system_score_gemma":0.000629383,"threshold_uncertainty_score":0.05856228},"labels":[],"label_agreement":null},{"id":"W1550642787","doi":"10.1002/2015gl064707","title":"Accurately specifying storm‐time ULF wave radial diffusion in the radiation belts","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"FP7 Space; Natural Sciences and Engineering Research Council of Canada; European Commission; European Social Fund; National Aeronautics and Space Administration","keywords":"Van Allen radiation belt; Physics; Magnetometer; Computational physics; Wave power; Solar wind; Diffusion; Van Allen Probes; Storm; Geophysics; Power (physics); Acceleration; Magnetosphere; Meteorology; Classical mechanics; Magnetic field; Quantum mechanics","score_opus":0.05894105446061106,"score_gpt":0.31613065236065657,"score_spread":0.25718959790004553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1550642787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92486817,0.00010157978,0.072266996,0.00013780492,0.000011387114,0.000019390907,0.00075030176,0.00021605042,0.0016282809],"genre_scores_gemma":[0.99706787,0.000024375497,0.0025454776,0.000009577423,0.0000035223932,0.000007259458,0.00024745605,0.000019295536,0.00007506721],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9996501,0.00012527974,0.000042112744,0.00007243018,0.00006397308,0.00004611377],"domain_scores_gemma":[0.9964886,0.0019737293,0.00077185984,0.0004474571,0.00024624733,0.000072108276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022545368,0.00039055024,0.00030655417,0.00054057804,0.00025378302,0.0010884244,0.0005779317,0.0007498122,0.00060092943],"category_scores_gemma":[0.010933527,0.00030868014,0.00035989512,0.0005116043,0.0004667117,0.001703543,0.00045848792,0.00049975864,0.00015537551],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013346992,0.000046940637,0.15627891,0.000054076798,0.00006567938,0.00016316173,0.00014680068,0.80802596,0.011137711,0.01258121,0.00039134044,0.0109747555],"study_design_scores_gemma":[0.00003063066,0.000040554693,0.06334348,0.000017724926,0.000016733535,0.00010897929,0.00009866401,0.9242218,0.0047769095,0.0061958036,0.0011100157,0.00003872008],"about_ca_topic_score_codex":0.007470049,"about_ca_topic_score_gemma":0.0032450813,"teacher_disagreement_score":0.007470049,"about_ca_system_score_codex":0.00071245275,"about_ca_system_score_gemma":0.00044232555,"threshold_uncertainty_score":0.01485312},"labels":[],"label_agreement":null},{"id":"W1551107186","doi":"10.1029/2010gl046038","title":"Methane and environmental change during the Paleocene-Eocene thermal maximum (PETM): Modeling the PETM onset as a two-stage event","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Carbon cycle; Methane; Atmosphere (unit); Isotopes of carbon; Stage (stratigraphy); Excursion; Geology; Atmospheric sciences; Climatology; Environmental science; Global warming; Carbon fibers; Climate change; δ13C; Carbon dioxide in Earth's atmosphere; Oceanography; Paleontology; Stable isotope ratio; Total organic carbon; Ecosystem; Meteorology; Chemistry; Environmental chemistry; Ecology","score_opus":0.036799143455052245,"score_gpt":0.2678576449719722,"score_spread":0.23105850151691992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1551107186","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98878235,0.00016274999,0.0052837264,0.00046858768,0.00003211793,0.00003782692,0.0011696484,0.00012062978,0.0039424095],"genre_scores_gemma":[0.99747676,0.00007310692,0.0014133661,0.000025936666,0.0000141093105,0.00004258762,0.00031311638,0.000020865078,0.00062005944],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999913,0.000030510655,0.000004092415,0.000021456262,0.000008263595,0.000022761684],"domain_scores_gemma":[0.9998441,0.000063715794,0.000026264624,0.000011750155,0.000014041035,0.000040166386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034877995,0.00048001847,0.00036234994,0.00030940818,0.0004740052,0.00067292654,0.00085020636,0.001793039,0.001876415],"category_scores_gemma":[0.0010297883,0.00047523057,0.0006594104,0.00041632503,0.000511635,0.00076207635,0.00060958957,0.0006437715,0.00014215967],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026674403,0.000086763794,0.019842299,0.000033423697,0.00008335609,0.00012763246,0.00007074232,0.97227955,0.001991136,0.0031678502,0.0005131824,0.0015374476],"study_design_scores_gemma":[0.0000812125,0.00006319481,0.008379302,0.000005139214,0.000025897236,0.000015917847,0.000026304733,0.98986596,0.0003054767,0.0007678819,0.0004509599,0.000012854844],"about_ca_topic_score_codex":0.03472536,"about_ca_topic_score_gemma":0.021772861,"teacher_disagreement_score":0.03472536,"about_ca_system_score_codex":0.0014117131,"about_ca_system_score_gemma":0.000681262,"threshold_uncertainty_score":0.0690465},"labels":[],"label_agreement":null},{"id":"W1552038478","doi":"10.1002/2013gl057776","title":"Contributions to twentieth century total column ozone change from halocarbons, tropospheric ozone precursors, and climate change","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Canadian Space Agency; Scheme for Promotion of Academic and Research Collaboration; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Ozone; Tropospheric ozone; Atmospheric sciences; Ozone layer; Ozone depletion; Climatology; Environmental science; Northern Hemisphere; Southern Hemisphere; Troposphere; Climate change; Boreal; Meteorology; Oceanography; Geology; Geography","score_opus":0.026746068490112802,"score_gpt":0.2775698765781407,"score_spread":0.2508238080880279,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1552038478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99587196,0.00037544972,0.0009099537,0.00035591048,0.000027834492,0.000004859973,0.0005526904,0.000029237865,0.0018721998],"genre_scores_gemma":[0.99808335,0.00046997226,0.00027607515,0.000039168786,0.000011799529,0.000005664419,0.00036722943,0.000010255157,0.0007364814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999304,0.000013357561,0.000002935311,0.000013491013,0.000013566658,0.000026252092],"domain_scores_gemma":[0.99986005,0.00004319003,0.00003112511,0.000011865043,0.00002311692,0.000030688767],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021341922,0.00030698616,0.00016098715,0.00031443796,0.0003269812,0.0004978286,0.0002660968,0.0004937158,0.0016326731],"category_scores_gemma":[0.0008078641,0.00026417035,0.00058417645,0.0003982744,0.00018059812,0.00041030877,0.0006115381,0.0004105099,0.00011459609],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069058454,0.00017301997,0.47081232,0.00022475487,0.00079570396,0.0007442994,0.00035455645,0.4628362,0.03312307,0.00952288,0.0015317533,0.019190878],"study_design_scores_gemma":[0.00024195379,0.00030412557,0.5891434,0.000047669935,0.000617385,0.00041908838,0.00035651808,0.37732655,0.012181146,0.0051031294,0.014152809,0.000106288084],"about_ca_topic_score_codex":0.032652635,"about_ca_topic_score_gemma":0.029958855,"teacher_disagreement_score":0.032652635,"about_ca_system_score_codex":0.0008920999,"about_ca_system_score_gemma":0.00056787423,"threshold_uncertainty_score":0.064925194},"labels":[],"label_agreement":null},{"id":"W1552550877","doi":"10.1002/grl.50624","title":"Sea‐state‐dependent wind work on the oceanic general circulation","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Wind stress; Climatology; Ocean current; Hindcast; Sea state; Geostrophic current; Geostrophic wind; Geology; Wind wave; Environmental science; Wind speed; Latitude; Sea-surface height; Wind shear; Storm; Atmospheric sciences; Sea surface temperature; Oceanography; Geodesy","score_opus":0.02654581244323654,"score_gpt":0.24887548050781924,"score_spread":0.2223296680645827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1552550877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99677473,0.000087562286,0.00036313228,0.00004323806,0.000009300689,0.0000027573237,0.001311712,0.000018024304,0.0013895751],"genre_scores_gemma":[0.99687296,0.00008901725,0.00014423333,0.000008289383,0.000007147565,0.000002738626,0.0023926818,0.000010714827,0.00047222862],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999729,0.000078899124,0.000019199295,0.00006811215,0.000066338296,0.000038481674],"domain_scores_gemma":[0.9989581,0.0004390775,0.00015505857,0.00016955871,0.00020108807,0.00007706079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046544307,0.0003006998,0.00021777373,0.00065310404,0.0001786937,0.0004854961,0.0001753482,0.00016931903,0.001671643],"category_scores_gemma":[0.0020582539,0.00017679132,0.00044912577,0.00086022046,0.00019937636,0.00045186357,0.00036709142,0.00020974327,0.00031567697],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032878196,0.000118203374,0.8546973,0.00008306325,0.00044695352,0.00022244739,0.00014923351,0.10579912,0.010200511,0.00059689704,0.0018511157,0.025506336],"study_design_scores_gemma":[0.000008935105,0.000043157863,0.9721121,0.000008920034,0.000032900378,0.00003322733,0.000060444014,0.02579599,0.0009581461,0.00015155,0.0007803522,0.0000142502595],"about_ca_topic_score_codex":0.006811863,"about_ca_topic_score_gemma":0.012882573,"teacher_disagreement_score":0.006811863,"about_ca_system_score_codex":0.00021252148,"about_ca_system_score_gemma":0.00018779474,"threshold_uncertainty_score":0.01354444},"labels":[],"label_agreement":null},{"id":"W1553168446","doi":"10.1029/2012gl053576","title":"Seasonal forecasts of Arctic sea ice initialized with observations of ice thickness","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Sea ice; Climatology; Arctic ice pack; Sea ice thickness; Arctic; Geology; Sea ice concentration; Environmental science; Drift ice; Oceanography","score_opus":0.06022622814675546,"score_gpt":0.29115738217861215,"score_spread":0.23093115403185668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1553168446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8727204,0.00032627987,0.037396625,0.00036362026,0.0005372373,0.00018181282,0.06810088,0.0022713947,0.018101698],"genre_scores_gemma":[0.8953168,0.00034890673,0.03591893,0.00007014049,0.000078161676,0.00017192349,0.062448148,0.00017062968,0.0054764743],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989533,0.00001981463,0.000006401748,0.000029617056,0.00003224653,0.000016505455],"domain_scores_gemma":[0.99951386,0.000053823027,0.000061915904,0.000054102366,0.0002571674,0.000059065806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043640097,0.00036463264,0.0002356736,0.00038957543,0.00022541784,0.00034397223,0.00036819858,0.00024949596,0.001878555],"category_scores_gemma":[0.0009320044,0.00022028203,0.00023120578,0.0003923811,0.000084978456,0.00022671111,0.00015779576,0.0004244367,0.00049752684],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073294516,0.0003030024,0.15516753,0.00018004126,0.00022815437,0.00020020206,0.0002477334,0.6841755,0.017089311,0.0036145172,0.07178644,0.06627458],"study_design_scores_gemma":[0.00021549547,0.00014430971,0.16946481,0.000052933625,0.00007875917,0.00006209679,0.0001449124,0.7878992,0.0074561005,0.0015057967,0.03289969,0.00007599846],"about_ca_topic_score_codex":0.038176145,"about_ca_topic_score_gemma":0.060508974,"teacher_disagreement_score":0.038176145,"about_ca_system_score_codex":0.00049892213,"about_ca_system_score_gemma":0.0007392953,"threshold_uncertainty_score":0.075907886},"labels":[],"label_agreement":null},{"id":"W1554829979","doi":"10.1002/2014gl060080","title":"Derivation of paleolongitude from the geometric parametrization of apparent polar wander path: Implication for absolute plate motion reconstruction","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Compute Canada","keywords":"Apparent polar wander; Paleomagnetism; Geology; Geodesy; Reference frame; Polar wander; Rotation (mathematics); Great circle; Geometry; Paleontology; Mathematics; Frame (networking); Computer science","score_opus":0.025249945423659426,"score_gpt":0.28354145129487773,"score_spread":0.2582915058712183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1554829979","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.119389884,0.00022341263,0.8747932,0.00014213979,0.000043672106,0.00002177914,0.0002167412,0.00056996034,0.0045992085],"genre_scores_gemma":[0.7786508,0.000308531,0.21815763,0.00003468123,0.000024217958,0.000050674334,0.00042425806,0.00025308866,0.0020960537],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999012,0.00003169079,0.0000058681194,0.0000343368,0.000020387972,0.000006516288],"domain_scores_gemma":[0.9998615,0.000034246164,0.000026048212,0.00004026735,0.000028740145,0.000009176122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002995078,0.0004313989,0.00014763504,0.0006991716,0.00021088186,0.00046048957,0.00048139863,0.00029922154,0.0019920052],"category_scores_gemma":[0.0015816566,0.00019127238,0.00028482464,0.0006221831,0.00036271504,0.00053465314,0.000385169,0.0004280409,0.00055954134],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059893413,0.000036256588,0.03758773,0.00014139322,0.000072474766,0.00031908596,0.00044148634,0.6472973,0.039440755,0.07937547,0.0014256125,0.19380255],"study_design_scores_gemma":[0.000015250277,0.000033379496,0.014696431,0.00004301011,0.00001793263,0.00025335644,0.00011320659,0.9465751,0.008186781,0.02170966,0.008316338,0.000039559265],"about_ca_topic_score_codex":0.004236837,"about_ca_topic_score_gemma":0.003734485,"teacher_disagreement_score":0.004236837,"about_ca_system_score_codex":0.0003372295,"about_ca_system_score_gemma":0.0005308737,"threshold_uncertainty_score":0.008424401},"labels":[],"label_agreement":null},{"id":"W1555222693","doi":"10.1029/2010gl044125","title":"THEMIS observations of the spatial extent and pressure‐pulse excitation of field line resonances","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Magnetosphere; Physics; Amplitude; Field line; Electric field; Magnetic field; Excitation; Field (mathematics); Line (geometry); Equator; Computational physics; Excited state; Geophysics; Optics; Atomic physics; Astronomy; Mathematics; Geometry; Quantum mechanics","score_opus":0.020692985249938844,"score_gpt":0.2869378185301874,"score_spread":0.26624483328024856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1555222693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882144,0.00015428217,0.0015865887,0.00008087166,0.000012739816,0.000008854683,0.00029921674,0.000065950786,0.009577123],"genre_scores_gemma":[0.99851733,0.00004545569,0.0007003247,0.000013966111,0.00001883343,0.000005145701,0.00019523001,0.0000057263696,0.0004979528],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999959,0.0000037900131,9.712946e-7,0.000012215181,0.0000129784,0.000011081933],"domain_scores_gemma":[0.9998926,0.00002262313,0.00003820463,0.000012231855,0.00001716954,0.000017115117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000105077794,0.00015389794,0.000109177636,0.00046305664,0.0003068729,0.00017001094,0.00015078996,0.00022435455,0.0006569924],"category_scores_gemma":[0.000202727,0.00007767345,0.00008833761,0.0004344756,0.00014597236,0.00018179559,0.0002836891,0.0002473043,0.00010507549],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010870087,0.00013677934,0.25139216,0.00014717014,0.000086490785,0.0024897235,0.0014856245,0.002889025,0.6547318,0.002873059,0.0023980115,0.08028318],"study_design_scores_gemma":[0.000037805847,0.00036271848,0.9192551,0.000021923854,0.000045786543,0.0012817039,0.0005943887,0.0055599893,0.06510884,0.0006352599,0.007074186,0.00002230158],"about_ca_topic_score_codex":0.0009851162,"about_ca_topic_score_gemma":0.0022343593,"teacher_disagreement_score":0.0009851162,"about_ca_system_score_codex":0.00014968218,"about_ca_system_score_gemma":0.000058219157,"threshold_uncertainty_score":0.0021978617},"labels":[],"label_agreement":null},{"id":"W1557427700","doi":"10.1002/grl.50504","title":"Paleofire reconstruction based on an ensemble‐member strategy applied to sedimentary charcoal","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Université du Québec en Abitibi-Témiscamingue; Université du Québec à Montréal","funders":"Canadian Forest Service; Centre National de la Recherche Scientifique; Fonds de recherche du Québec – Nature et technologies; Max-Planck-Gesellschaft; Agence Nationale de la Recherche; Biodiversa+; Université du Québec à Chicoutimi; Natural Sciences and Engineering Research Council of Canada; Université du Québec à Montréal","keywords":"Charcoal; Char; Smoothing; Fire regime; Environmental science; Biome; Taiga; Sedimentary rock; Computer science; Geology; Statistics; Mathematics; Coal; Paleontology; Chemistry; Archaeology; Forestry; Geography; Ecology","score_opus":0.0413266802728866,"score_gpt":0.2943387104066323,"score_spread":0.2530120301337457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1557427700","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2390782,0.00006441692,0.7591618,0.00006846155,0.00002094273,0.000023553686,0.000117555915,0.0006728215,0.00079229445],"genre_scores_gemma":[0.7816344,0.000053688513,0.21699074,0.000033420118,0.000029528133,0.000046890425,0.0004812256,0.00012223219,0.00060786743],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99974364,0.00009484328,0.000013701299,0.00005671145,0.000052034946,0.00003895562],"domain_scores_gemma":[0.9981341,0.00074565376,0.00014173712,0.00032964736,0.0005281498,0.00012076937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020464337,0.000479448,0.0007077074,0.0010550221,0.0006548046,0.000996554,0.00088136556,0.000865322,0.0008876874],"category_scores_gemma":[0.003866354,0.00034919134,0.0008179013,0.0007245209,0.00034165755,0.0006456929,0.0007418416,0.0006205409,0.0002675397],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021337732,0.000093075345,0.016872866,0.000030094285,0.00019956785,0.00013814989,0.00021664829,0.8441489,0.010466853,0.004144384,0.00059120724,0.12288487],"study_design_scores_gemma":[0.0000019999854,0.000005054145,0.0008099498,0.0000018062316,0.0000052051105,0.000007044247,0.0000063200014,0.9980118,0.00063816056,0.00042779668,0.000080622754,0.000004289299],"about_ca_topic_score_codex":0.007831161,"about_ca_topic_score_gemma":0.0070703835,"teacher_disagreement_score":0.007831161,"about_ca_system_score_codex":0.0003724761,"about_ca_system_score_gemma":0.0007335222,"threshold_uncertainty_score":0.015571177},"labels":[],"label_agreement":null},{"id":"W1557552867","doi":"10.1029/2006gl028685","title":"Carbon‐cycle feedbacks increase the likelihood of a warmer future","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Alberta Energy; University of Calgary; Concordia University","funders":"University of Victoria","keywords":"Environmental science; Global warming; Carbon cycle; Climate change; Climatology; Greenhouse gas; Carbon fibers; Atmospheric sciences; Albedo (alchemy); Coupled model intercomparison project; Climate model; Ecosystem; Ecology; Computer science; Biology","score_opus":0.007684300992552111,"score_gpt":0.25338037598398955,"score_spread":0.24569607499143745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1557552867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92421746,0.00081116514,0.0648389,0.0015368494,0.000061230225,0.000035787893,0.00029650467,0.00027153638,0.007930553],"genre_scores_gemma":[0.99786323,0.00015769398,0.0016260673,0.000058922284,0.000018970573,0.0000074618583,0.00003055073,0.000009086265,0.00022819778],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99931586,0.0002454204,0.000043450847,0.00013756732,0.00016779735,0.000089875684],"domain_scores_gemma":[0.9917853,0.0060820756,0.0013920455,0.00021730611,0.0002732954,0.00024995612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021022493,0.00049017987,0.000489834,0.0007591195,0.00055406516,0.0013303979,0.00038557552,0.001458157,0.0036067753],"category_scores_gemma":[0.011722429,0.0004976464,0.0006379851,0.00036043418,0.00080698245,0.0027290285,0.001193564,0.00095053937,0.00018660347],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007094386,0.00007077482,0.09984958,0.00032430573,0.0004003593,0.00055197417,0.00026130068,0.8138694,0.012301512,0.035961088,0.0010932393,0.034607105],"study_design_scores_gemma":[0.0000853913,0.00027578298,0.08453073,0.00007276582,0.0003389212,0.00069624896,0.00025152267,0.74349695,0.0060788905,0.1590011,0.0049836105,0.00018806747],"about_ca_topic_score_codex":0.0014438397,"about_ca_topic_score_gemma":0.0024243272,"teacher_disagreement_score":0.0036067753,"about_ca_system_score_codex":0.000654274,"about_ca_system_score_gemma":0.00031487324,"threshold_uncertainty_score":0.012065828},"labels":[],"label_agreement":null},{"id":"W1557761653","doi":"10.1002/2014gl062898","title":"Interhemispheric air temperature phase relationships in the nonlinear Dansgaard‐Oeschger oscillation","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Climatology; Northern Hemisphere; Southern Hemisphere; Thermocline; Thermohaline circulation; Zonal and meridional; Sea surface temperature; North Atlantic Deep Water; Oceanography","score_opus":0.08269962878677506,"score_gpt":0.33857243895509853,"score_spread":0.2558728101683235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1557761653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983902,0.0000773522,0.00041592325,0.00003866446,0.0000052077194,0.0000026127962,0.00012700183,0.000008006403,0.000934995],"genre_scores_gemma":[0.99965405,0.000024307994,0.00010176675,0.000004000255,0.0000021163337,0.0000012365439,0.000057634308,0.0000023493421,0.00015237698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999634,0.000007910145,0.0000023443122,0.00001248319,0.00000736334,0.000006453677],"domain_scores_gemma":[0.999762,0.000096006974,0.000061817154,0.000017492108,0.000036308906,0.000026275722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020111211,0.00012707272,0.000126124,0.00023322945,0.00019094658,0.000387367,0.00008689781,0.00016004205,0.0010607733],"category_scores_gemma":[0.0012402312,0.00010112299,0.00008384695,0.00026017107,0.00021229342,0.00027490722,0.00023279978,0.00017127978,0.00013180159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091467466,0.0000567737,0.88193876,0.000062395535,0.00011070558,0.0002491436,0.00074518996,0.02946941,0.057892703,0.005042515,0.0008957118,0.02262199],"study_design_scores_gemma":[0.00002722673,0.00003469609,0.96933055,0.000005373198,0.000016162656,0.00004729142,0.00008415225,0.026435962,0.0013064331,0.0014539346,0.0012473202,0.000010996314],"about_ca_topic_score_codex":0.009538761,"about_ca_topic_score_gemma":0.010910753,"teacher_disagreement_score":0.009538761,"about_ca_system_score_codex":0.00042073324,"about_ca_system_score_gemma":0.00023012485,"threshold_uncertainty_score":0.018966496},"labels":[],"label_agreement":null},{"id":"W1558526850","doi":"10.1002/2015gl064508","title":"Observed platelet ice distributions in Antarctic sea ice: An index for ocean‐ice shelf heat flux","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Ministry of Science and Innovation, New Zealand; Foundation for Research, Science and Technology; National Institute of Water and Atmospheric Research","keywords":"Ice shelf; Sea ice; Antarctic sea ice; Geology; Cryosphere; Sea ice thickness; Arctic ice pack; Drift ice; Oceanography; Iceberg; Fast ice; Climatology; Ice sheet","score_opus":0.10129863422314819,"score_gpt":0.3182353687008926,"score_spread":0.2169367344777444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558526850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99732375,0.0000444778,0.00022486546,0.0000069153075,0.0000021748197,0.000002086527,0.0017484805,0.000016578033,0.00063065527],"genre_scores_gemma":[0.99853086,0.000023859127,0.00019756959,0.000002443659,0.000003087337,0.0000037748714,0.001158787,0.0000037890425,0.00007572016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.000007137126,0.000004353021,0.000013188545,0.00001415934,0.000008358514],"domain_scores_gemma":[0.9997278,0.00007109576,0.000094810406,0.000029264786,0.000047871574,0.000029116823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009945243,0.00016502578,0.000105877196,0.0010382185,0.0001293165,0.00036685506,0.00009626374,0.00012436272,0.0007094807],"category_scores_gemma":[0.00040609567,0.000080234466,0.00012459372,0.0009652366,0.00013131235,0.00019238445,0.00023711495,0.00012302566,0.00018812505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007394918,0.000009380438,0.9873748,0.000015672285,0.000043087013,0.000031838434,0.00009720269,0.0014119089,0.0053027235,0.00006177335,0.00030183938,0.0052758204],"study_design_scores_gemma":[0.0000019229315,0.000009937281,0.9969715,0.0000020335574,0.0000067448377,0.000040944193,0.00005984301,0.0016986587,0.0008329646,0.000032091004,0.00034083347,0.0000024029468],"about_ca_topic_score_codex":0.0029003653,"about_ca_topic_score_gemma":0.0046154987,"teacher_disagreement_score":0.0029003653,"about_ca_system_score_codex":0.0001605893,"about_ca_system_score_gemma":0.000058720194,"threshold_uncertainty_score":0.005766988},"labels":[],"label_agreement":null},{"id":"W1558662600","doi":"10.1002/grl.50901","title":"Van Allen Probes observation of localized drift resonance between poloidal mode ultra‐low frequency waves and 60 keV electrons","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":152,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Physics; Magnetosphere; Electron; Ultra low frequency; Atomic physics; Resonance (particle physics); Amplitude; Van Allen Probes; Oscillation (cell signaling); Computational physics; Van Allen radiation belt; Plasma; Nuclear physics; Optics","score_opus":0.015744007988670494,"score_gpt":0.2757124145491314,"score_spread":0.25996840656046094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558662600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955244,0.00011207602,0.00051467674,0.000055614146,0.0000072782964,0.0000061218716,0.00017228171,0.000029804922,0.003577674],"genre_scores_gemma":[0.9978219,0.00006357547,0.00080540136,0.000029285282,0.000006989125,0.000006788397,0.0002725533,0.000006824793,0.0009866691],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999397,0.0000044360304,0.0000011946292,0.000016085916,0.000018032284,0.000020552821],"domain_scores_gemma":[0.9999304,0.000015338317,0.000021314323,0.000006858058,0.000011910797,0.000014158701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007750669,0.00014199033,0.000099524055,0.00041354843,0.00023758634,0.00020933009,0.0002464891,0.00022630682,0.0007222721],"category_scores_gemma":[0.0001505064,0.00011038201,0.00008702336,0.0001786913,0.00011799614,0.00019700744,0.00029068222,0.00022598683,0.000097574615],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006121052,0.00009837603,0.12930553,0.000076278295,0.00012107581,0.0013179475,0.0010455674,0.0030997344,0.82817644,0.0011909632,0.0017796297,0.03317638],"study_design_scores_gemma":[0.000060310605,0.0006089512,0.8801091,0.000040058072,0.000098586694,0.00078404805,0.0007399346,0.0113717485,0.09345002,0.0006678247,0.012016145,0.00005328624],"about_ca_topic_score_codex":0.006372806,"about_ca_topic_score_gemma":0.014254786,"teacher_disagreement_score":0.006372806,"about_ca_system_score_codex":0.00021053408,"about_ca_system_score_gemma":0.000109459725,"threshold_uncertainty_score":0.012671411},"labels":[],"label_agreement":null},{"id":"W1558800605","doi":"10.1002/2015gl064622","title":"Interception effects on stable isotope driven streamwater transit time estimates","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; University of Saskatchewan","funders":"Deutsche Forschungsgemeinschaft","keywords":"Throughfall; TRACER; Interception; Isotope; Environmental science; STREAMS; Hydrology (agriculture); Stable isotope ratio; Watershed; Precipitation; Atmospheric sciences; Geology; Meteorology; Soil water; Soil science","score_opus":0.025901120583185167,"score_gpt":0.28750176550226136,"score_spread":0.2616006449190762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1558800605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99413717,0.000053235362,0.005266965,0.000013531013,0.0000046988885,0.000007911228,0.00019191313,0.000108174674,0.00021637628],"genre_scores_gemma":[0.99837637,0.000018376724,0.0013355769,0.0000055640626,0.0000013662708,0.0000055514843,0.00017963866,0.000023312718,0.00005423963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99944574,0.00024149027,0.000045721306,0.00013616525,0.00007647376,0.00005438702],"domain_scores_gemma":[0.99610966,0.0028159919,0.00038381197,0.00030658112,0.00030965413,0.000074267744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020893845,0.00038140133,0.0002700625,0.00042795768,0.00027584712,0.00051419827,0.00031720835,0.00026793944,0.00054632727],"category_scores_gemma":[0.008092961,0.00027199637,0.00035419382,0.00048827607,0.00028781837,0.00043863896,0.00036032702,0.00028114917,0.000075651486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012359305,0.00009555646,0.61233646,0.00012539655,0.00031506128,0.0002052973,0.00040066132,0.27968293,0.079708114,0.00049925776,0.0002718614,0.025123376],"study_design_scores_gemma":[0.0000653157,0.00031456174,0.32823533,0.00002550674,0.00014165434,0.000101380516,0.00011638874,0.60496455,0.06476215,0.00032456403,0.00089568866,0.00005289875],"about_ca_topic_score_codex":0.019921819,"about_ca_topic_score_gemma":0.0148509545,"teacher_disagreement_score":0.019921819,"about_ca_system_score_codex":0.0007344392,"about_ca_system_score_gemma":0.0003595587,"threshold_uncertainty_score":0.039611697},"labels":[],"label_agreement":null},{"id":"W1561092974","doi":"10.1029/2012gl051947","title":"Influence of sediment deposition on deep lithospheric tectonics","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Subduction; Crust; Mantle (geology); Collision zone; Oceanic crust; Eclogitization; Continental crust; Geophysics; Petrology; Tectonics; Geochemistry; Seismology","score_opus":0.01915967040441487,"score_gpt":0.2595437572822386,"score_spread":0.24038408687782373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1561092974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971048,0.00015111326,0.0011656,0.00006521148,0.000010437251,0.0000048823426,0.000070824484,0.000030654417,0.0013964123],"genre_scores_gemma":[0.9996166,0.00006036665,0.00017053547,0.0000040245027,0.0000013126195,0.0000015860401,0.00002264533,0.0000048935262,0.000117987765],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978966,0.000067525696,0.000022812008,0.000038898866,0.00003529125,0.000045877445],"domain_scores_gemma":[0.9994055,0.00027775002,0.00008386872,0.0001030316,0.000050130762,0.0000796689],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042958115,0.00073967513,0.00051224447,0.00041025112,0.0005663019,0.0011593264,0.00029117038,0.00046543885,0.0014404064],"category_scores_gemma":[0.0018957162,0.0003509739,0.00050295837,0.00044027838,0.0011190936,0.00048399737,0.0011197781,0.00036249936,0.000146057],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006333422,0.000086744505,0.047599886,0.0001354198,0.00012887156,0.00042294062,0.00013270193,0.8520695,0.08805108,0.0037446797,0.000101882135,0.0068929833],"study_design_scores_gemma":[0.00028716557,0.0007131621,0.11891825,0.00004561428,0.0002007465,0.00016210903,0.00020561372,0.83632547,0.037358567,0.0045119594,0.0011734106,0.00009788344],"about_ca_topic_score_codex":0.007139151,"about_ca_topic_score_gemma":0.003408915,"teacher_disagreement_score":0.007139151,"about_ca_system_score_codex":0.000990506,"about_ca_system_score_gemma":0.0005690191,"threshold_uncertainty_score":0.014195204},"labels":[],"label_agreement":null},{"id":"W1562571311","doi":"10.1029/2005gl024251","title":"Amplitude and frequency of temperature extremes over the North Atlantic region","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Amplitude; Extreme value theory; Environmental science; Forcing (mathematics); Spatial distribution; Magnitude (astronomy); Intensity (physics); Atmospheric sciences; Climate change; Geology; Oceanography; Physics; Statistics","score_opus":0.02970280101270228,"score_gpt":0.2757910243227369,"score_spread":0.2460882233100346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1562571311","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99898416,0.00010221749,0.000085227155,0.0000357179,0.0000017680708,7.352296e-7,0.0001836591,0.000005823597,0.0006006421],"genre_scores_gemma":[0.99968815,0.00004431843,0.00003486029,0.0000035780095,0.000004679832,9.413858e-7,0.00016567104,9.259799e-7,0.000056796904],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998803,0.000019634037,0.000013549895,0.000035015175,0.000034246415,0.00001719199],"domain_scores_gemma":[0.99937385,0.00018460242,0.00024719335,0.000044414654,0.00010712026,0.00004287346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024434764,0.00005933623,0.00014036684,0.0005643766,0.00015691323,0.0003479757,0.00009706254,0.00016956622,0.00043703063],"category_scores_gemma":[0.0012122985,0.00007012783,0.00013985221,0.0005485182,0.00022341296,0.000201693,0.00022395018,0.00015351613,0.00008395135],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009555743,0.0000101198575,0.98339486,0.000018990268,0.0000802843,0.00010908579,0.00031981204,0.002417013,0.0043112664,0.00017003855,0.0002817485,0.008791342],"study_design_scores_gemma":[0.0000011651763,0.000006411282,0.9988368,0.000001781045,0.0000058906944,0.000039939998,0.000056055524,0.0007427372,0.00007870891,0.00004460471,0.00018359908,0.0000023179966],"about_ca_topic_score_codex":0.0077661714,"about_ca_topic_score_gemma":0.011424805,"teacher_disagreement_score":0.0077661714,"about_ca_system_score_codex":0.00023204542,"about_ca_system_score_gemma":0.00011577949,"threshold_uncertainty_score":0.0154418945},"labels":[],"label_agreement":null},{"id":"W1565092696","doi":"10.1029/2012gl053409","title":"The impact of the El Niño‐Southern Oscillation on maximum temperature extremes","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"El Niño Southern Oscillation; Climatology; Environmental science; Southern oscillation; Multivariate ENSO index; Climate change; Climate model; Maximum temperature; Magnitude (astronomy); Pacific decadal oscillation; Extreme value theory; La Niña; Atmospheric sciences; Geology; Physics; Oceanography","score_opus":0.04072380938546565,"score_gpt":0.3287104684313346,"score_spread":0.28798665904586895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1565092696","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99091095,0.00035020715,0.00084048155,0.00041161472,0.000048060378,0.0000046379823,0.00086397666,0.00006176385,0.0065084132],"genre_scores_gemma":[0.99915326,0.00016506934,0.00013291919,0.000026439116,0.000011165715,0.000002874235,0.00033383997,0.000011335365,0.00016304108],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99964166,0.00012377047,0.00002793602,0.00006452299,0.000069870664,0.00007233624],"domain_scores_gemma":[0.99916184,0.0004504661,0.00014091298,0.00007560741,0.000085865744,0.00008530273],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071944384,0.00030443387,0.00032428742,0.00027794403,0.0004872427,0.0013592578,0.0003847837,0.0005458299,0.0016713939],"category_scores_gemma":[0.0037407922,0.0003428331,0.0004945839,0.00048797968,0.00036201035,0.0011187083,0.00085480814,0.0006173219,0.00018895073],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007047072,0.00019804409,0.33935416,0.00018370365,0.00042055783,0.00041619426,0.0002135005,0.6262895,0.0077024517,0.005579938,0.00270204,0.016235195],"study_design_scores_gemma":[0.0001032283,0.00022339285,0.48401755,0.00006413406,0.00013128469,0.00014564412,0.00036182828,0.50383216,0.0035863454,0.0036101572,0.003860952,0.00006329796],"about_ca_topic_score_codex":0.020252287,"about_ca_topic_score_gemma":0.02427514,"teacher_disagreement_score":0.020252287,"about_ca_system_score_codex":0.00080706395,"about_ca_system_score_gemma":0.0006503859,"threshold_uncertainty_score":0.04026884},"labels":[],"label_agreement":null},{"id":"W1566220736","doi":"10.1002/2014gl062345","title":"Hemispheric asymmetry of the structure of dayside auroral oval","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Fundamental Research Funds for the Central Universities; Chinese Arctic and Antarctic Administration; National Natural Science Foundation of China","keywords":"Asymmetry; Ionosphere; Solar wind; Geology; Northern Hemisphere; Interplanetary magnetic field; Magnetosheath; Atmospheric sciences; Geophysics; Physics; Magnetopause; Magnetic field","score_opus":0.008990336312961492,"score_gpt":0.2633697504384116,"score_spread":0.2543794141254501,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1566220736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926963,0.00016218206,0.0011834217,0.00003170766,0.00000953746,0.0000068460627,0.00078540447,0.000048944315,0.005075629],"genre_scores_gemma":[0.9990206,0.000049718165,0.00018558957,0.000004595397,0.000010442336,0.0000030988829,0.0004141989,0.000013840208,0.00029797436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989426,0.000014442172,0.000008588194,0.000027660759,0.000029415787,0.000025627585],"domain_scores_gemma":[0.99936455,0.00012510379,0.00019823964,0.000044103923,0.00018456478,0.00008344326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017956684,0.00011235179,0.00013252269,0.0010518237,0.0001490488,0.0005842597,0.00009964827,0.00011419347,0.0020763406],"category_scores_gemma":[0.000638032,0.000085524676,0.00012604585,0.00059719133,0.00021192335,0.0002902953,0.00029116566,0.00013115956,0.0003026945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009424754,0.00003672856,0.77495503,0.0001226086,0.00018412771,0.00048659593,0.00087536674,0.0033488218,0.15098731,0.002600597,0.0023613274,0.06309894],"study_design_scores_gemma":[0.000005019442,0.000018770592,0.9946108,0.0000052116197,0.000015537198,0.00012497765,0.00012890332,0.0013052812,0.0021648547,0.00029474197,0.0013169817,0.00000882991],"about_ca_topic_score_codex":0.001403473,"about_ca_topic_score_gemma":0.0017768178,"teacher_disagreement_score":0.0020763406,"about_ca_system_score_codex":0.00016336405,"about_ca_system_score_gemma":0.00010309799,"threshold_uncertainty_score":0.0069460273},"labels":[],"label_agreement":null},{"id":"W1567677637","doi":"10.1029/2012gl054118","title":"Direct ventilation of the North Pacific did not reach the deep ocean during the last deglaciation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Deglaciation; Subarctic climate; Geology; Oceanography; Deep water; Circumpolar deep water; Deep sea; Stadial; Pacific ocean; Holocene; North Atlantic Deep Water","score_opus":0.02534310176922355,"score_gpt":0.2605486903595229,"score_spread":0.23520558859029933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1567677637","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991008,0.0001523888,0.000045296896,0.000022346821,0.0000026873083,0.00000143351,0.00010061169,0.0000042120023,0.0005701946],"genre_scores_gemma":[0.9996245,0.00006890612,0.000035796573,0.000009763976,0.000004051101,0.0000016051357,0.00008615673,0.0000019816243,0.00016728698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.0000032605403,0.0000037042905,0.000019861582,0.00001070641,0.000016007365],"domain_scores_gemma":[0.9997633,0.000033536002,0.000072180614,0.000016105303,0.00006191187,0.00005302364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013269162,0.00022610472,0.00023482417,0.00033503503,0.0005749204,0.00047890446,0.00020935845,0.00027044924,0.0010410888],"category_scores_gemma":[0.00035574203,0.0001857932,0.0001645908,0.00035304492,0.00048137543,0.00034378897,0.0005269641,0.00036051238,0.00015198055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043860587,0.000018431687,0.8723573,0.00008607823,0.00008454643,0.0004715471,0.0008281064,0.00019438514,0.117206156,0.000098002645,0.000114502094,0.0081022885],"study_design_scores_gemma":[0.0000014462958,0.0000177568,0.9985379,0.0000024842,0.000006943948,0.00003114582,0.000095433905,0.00003069218,0.0011223308,0.000008338604,0.00014433802,0.0000011402907],"about_ca_topic_score_codex":0.012836159,"about_ca_topic_score_gemma":0.0246061,"teacher_disagreement_score":0.012836159,"about_ca_system_score_codex":0.00057652243,"about_ca_system_score_gemma":0.00027998426,"threshold_uncertainty_score":0.025522888},"labels":[],"label_agreement":null},{"id":"W1568959237","doi":"10.1002/grl.50182","title":"Relative sea level variations in the Chukchi region ‐ Arctic Ocean ‐ since the late Eocene","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Arctic; Paleontology; Oceanography; Canada Basin; Structural basin; Sea level","score_opus":0.09038691027215438,"score_gpt":0.27523377538698013,"score_spread":0.18484686511482573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1568959237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986798,0.00010870773,0.000044041186,0.000022508671,0.0000034590005,0.000001038705,0.00039553936,0.0000053907897,0.0007395416],"genre_scores_gemma":[0.9992055,0.000056846253,0.0000504833,0.0000048177676,0.0000020084958,0.0000015097451,0.00039360518,0.0000023539787,0.00028293498],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999459,0.0000046096698,0.000004862842,0.000013990307,0.000009770479,0.000020895533],"domain_scores_gemma":[0.9997054,0.000020143692,0.0000754158,0.000012324236,0.00014292228,0.000043745247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010863689,0.00013571192,0.00008537939,0.0008182688,0.00029410236,0.0003926067,0.000120440774,0.00012709151,0.0007315703],"category_scores_gemma":[0.000330594,0.00009521795,0.00007597109,0.0012112077,0.0002559952,0.00016742031,0.0002477317,0.0001343348,0.00011308849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000097219614,0.000014394205,0.9766401,0.00006232626,0.0000668199,0.0001870206,0.00090609613,0.00094280794,0.006506898,0.00021010735,0.0005344346,0.013831828],"study_design_scores_gemma":[7.64937e-7,0.0000049714085,0.9986229,0.0000045351994,0.0000057449065,0.000024493267,0.00013511027,0.0002652275,0.00019736652,0.0000063700722,0.0007300156,0.0000024823842],"about_ca_topic_score_codex":0.12641059,"about_ca_topic_score_gemma":0.24759395,"teacher_disagreement_score":0.12641059,"about_ca_system_score_codex":0.0008584138,"about_ca_system_score_gemma":0.0005554492,"threshold_uncertainty_score":0.25134963},"labels":[],"label_agreement":null},{"id":"W1570025454","doi":"10.1029/2010gl046016","title":"Evidence of liquid dependent ice nucleation in high-latitude stratiform clouds from surface remote sensors","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":287,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Ice nucleus; Sea ice growth processes; Sea ice; Geology; Arctic ice pack; Microwave radiometer; Atmospheric sciences; Arctic; Sea ice thickness; Sea ice concentration; Nucleation; Lidar; Antarctic sea ice; Supersaturation; Environmental science; Climatology; Radiometer; Remote sensing; Oceanography; Physics","score_opus":0.054583927252895306,"score_gpt":0.29660463644366647,"score_spread":0.24202070919077118,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1570025454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972691,0.00024176906,0.0009857317,0.000023066497,0.0000032243513,0.0000069141574,0.00023315317,0.000018494105,0.0012185118],"genre_scores_gemma":[0.99934775,0.000046420646,0.00021728438,0.000008136078,0.0000037410096,0.0000019397148,0.00027406277,0.0000016730414,0.00009910771],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998915,0.000008505813,0.0000059315853,0.000023354021,0.000039953087,0.00003067867],"domain_scores_gemma":[0.99929345,0.00019960522,0.00022741237,0.00004099187,0.00016598811,0.00007261137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019793794,0.00011195117,0.00010949522,0.00043157575,0.00045171846,0.0003243094,0.0003670809,0.0002461927,0.00092131423],"category_scores_gemma":[0.00051318324,0.00012310183,0.00008160519,0.00038824795,0.00036708915,0.00024453105,0.00020404899,0.00018996812,0.0001241014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005185956,0.000113247996,0.7682486,0.000118398,0.00006150684,0.00039062975,0.00034744327,0.00077061827,0.21945222,0.00026013676,0.00034509614,0.009373523],"study_design_scores_gemma":[0.000013553404,0.00012697122,0.9650707,0.000014698281,0.000029050938,0.00029668715,0.00015392425,0.0020571055,0.031642374,0.00007789737,0.00051041803,0.0000065431877],"about_ca_topic_score_codex":0.019964948,"about_ca_topic_score_gemma":0.03581748,"teacher_disagreement_score":0.019964948,"about_ca_system_score_codex":0.00033520567,"about_ca_system_score_gemma":0.00023061795,"threshold_uncertainty_score":0.03969747},"labels":[],"label_agreement":null},{"id":"W1571745720","doi":"10.1002/grl.50101","title":"Energetics of weakening and recovery of the Atlantic overturning in a climate change simulation","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Pycnocline; Energetics; Geology; Buoyancy; Thermohaline circulation; Forcing (mathematics); Oceanography; Climate change; Climatology; Ocean current; Shutdown of thermohaline circulation; North Atlantic Deep Water; Physics","score_opus":0.02988056520677093,"score_gpt":0.26157631476294224,"score_spread":0.2316957495561713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1571745720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99445516,0.0000345036,0.001122611,0.0001855765,0.000020590567,0.00002352703,0.0005096129,0.000060314782,0.0035881593],"genre_scores_gemma":[0.99882513,0.000019808454,0.00046255876,0.00003162187,0.000005234806,0.00002001103,0.00027791745,0.000014544734,0.0003431279],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999782,0.00008439006,0.000011744609,0.000028702529,0.000031153628,0.00006202242],"domain_scores_gemma":[0.999318,0.00028983114,0.00007992026,0.00006467309,0.00009019771,0.00015738787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006314309,0.00039905388,0.0006633928,0.00059322425,0.0006973207,0.0010361874,0.0007358866,0.0012257752,0.0021004824],"category_scores_gemma":[0.0021979108,0.0003492378,0.0006711339,0.00052340137,0.0008187762,0.00045891927,0.0007256544,0.000818277,0.00014970516],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023835449,0.00009703453,0.013067814,0.000015340696,0.000057245845,0.00018395769,0.000037958704,0.9829191,0.0010412465,0.0011449289,0.00033766305,0.0008593123],"study_design_scores_gemma":[0.000109786524,0.00009595679,0.008434733,0.0000048332518,0.00002443024,0.000019510764,0.000048618196,0.9903133,0.00034257403,0.0003472514,0.00024252877,0.000016434771],"about_ca_topic_score_codex":0.03978492,"about_ca_topic_score_gemma":0.017332291,"teacher_disagreement_score":0.03978492,"about_ca_system_score_codex":0.0010706766,"about_ca_system_score_gemma":0.0010712576,"threshold_uncertainty_score":0.07910669},"labels":[],"label_agreement":null},{"id":"W1576011138","doi":"10.1029/2004gl019638","title":"Experimental and modeling study of fluid pressure‐driven fractures in Darley Dale sandstone","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Acoustic emission; Geology; Fluid pressure; Mechanics; Fracture (geology); Fluid dynamics; Internal pressure; Phase (matter); Flow (mathematics); Geotechnical engineering; Materials science; Physics; Composite material","score_opus":0.03529694930113253,"score_gpt":0.324922666735688,"score_spread":0.28962571743455545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1576011138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934787,0.000006716534,0.00049618696,0.0000026999194,3.7923397e-7,0.0000040164773,0.000026944343,0.00000634603,0.00010884583],"genre_scores_gemma":[0.9989191,0.000009578447,0.0009250145,0.0000012972505,4.0170775e-7,0.0000072249873,0.000042215244,0.0000012537688,0.00009400599],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99984384,0.000012529891,0.0000068208215,0.000045704248,0.000067046734,0.000024049397],"domain_scores_gemma":[0.9997378,0.00008352522,0.00004943173,0.000036360907,0.00006581604,0.000027018501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018861463,0.00018798518,0.00020613002,0.00026839328,0.00035600987,0.00019285738,0.0004592319,0.00026587644,0.0002638806],"category_scores_gemma":[0.00047701623,0.00021331322,0.00012839143,0.00023020318,0.00046989182,0.00017078401,0.0003058556,0.00022366573,0.000055843797],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048011472,0.00021736459,0.12450732,0.00008018374,0.000027997086,0.0008565123,0.00071860926,0.025849007,0.8344776,0.0003583282,0.00007490008,0.012352153],"study_design_scores_gemma":[0.00006998608,0.0009916137,0.4927341,0.0000087188555,0.000031743413,0.0005877014,0.0005144667,0.13060634,0.37285137,0.00024742918,0.00130828,0.00004828508],"about_ca_topic_score_codex":0.009660307,"about_ca_topic_score_gemma":0.013877736,"teacher_disagreement_score":0.009660307,"about_ca_system_score_codex":0.00042115818,"about_ca_system_score_gemma":0.00027406114,"threshold_uncertainty_score":0.019208133},"labels":[],"label_agreement":null},{"id":"W1578573232","doi":"10.1029/2003gl019393","title":"Nonlinear interaction among internal wave beams generated by tidal flow over supercritical topography","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Supercritical fluid; Internal wave; Nonlinear system; Supercritical flow; Geology; Internal tide; Flow (mathematics); Harmonic; Internal flow; Mechanics; Optics; Physics; Acoustics","score_opus":0.018147561347999146,"score_gpt":0.26647369739934407,"score_spread":0.24832613605134493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1578573232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9596027,0.00007647627,0.024488699,0.000050664472,0.000022996968,0.00003472889,0.00004555619,0.000074257776,0.015604017],"genre_scores_gemma":[0.9955254,0.000052231157,0.0018818717,0.000014869263,0.000006316659,0.000014812437,0.000037058846,0.000016458665,0.0024508974],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992335,0.000005923944,0.0000020164146,0.000008568523,0.000029220755,0.000030890063],"domain_scores_gemma":[0.9997423,0.00008453589,0.000048078433,0.000027294702,0.00004485777,0.0000529531],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010293149,0.00025170005,0.0001865149,0.0003278111,0.00039475036,0.00044270017,0.0002414659,0.00020186193,0.004287593],"category_scores_gemma":[0.00040488114,0.00020728279,0.00025198652,0.00029270875,0.0004779072,0.0003298787,0.0004832075,0.00029689423,0.00038452112],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027278715,0.00014210693,0.02104026,0.00018575272,0.00013147193,0.000863345,0.0010459254,0.08378203,0.8073547,0.024978468,0.0014663006,0.05873694],"study_design_scores_gemma":[0.00009512991,0.00018040404,0.0481457,0.00002125094,0.00007297794,0.00040469618,0.00045580324,0.7797812,0.15716101,0.01058706,0.003009838,0.00008491334],"about_ca_topic_score_codex":0.001381539,"about_ca_topic_score_gemma":0.0023340785,"teacher_disagreement_score":0.004287593,"about_ca_system_score_codex":0.00025559403,"about_ca_system_score_gemma":0.000277855,"threshold_uncertainty_score":0.0143434405},"labels":[],"label_agreement":null},{"id":"W1582258667","doi":"10.1029/2012gl053054","title":"Argon supersaturation indicates low decadal‐scale vertical mixing in the ocean thermocline","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Thermocline; Mixing (physics); Photic zone; Supersaturation; Oceanography; Geology; New production; Atmospheric sciences; Environmental science; Nutrient; Chemistry; Physics","score_opus":0.02490134419486747,"score_gpt":0.2694136734571021,"score_spread":0.24451232926223462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1582258667","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99901116,0.000042420404,0.00038091917,0.000012287487,0.0000027514084,0.0000013816123,0.00009992158,0.000014522048,0.00043460017],"genre_scores_gemma":[0.9997004,0.000013675929,0.00012886006,0.0000054640655,0.0000012625961,0.0000020079333,0.00007116044,0.0000020040306,0.0000751984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999449,0.000007595981,0.000005112995,0.00001756162,0.000013082092,0.000011687567],"domain_scores_gemma":[0.9997217,0.00006857905,0.000100976715,0.00002703678,0.000038102742,0.00004355356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016223072,0.00013929457,0.00012529282,0.00032075602,0.00020185171,0.00031132234,0.00012054523,0.00021147948,0.000749505],"category_scores_gemma":[0.0003968927,0.00016135706,0.00014311023,0.00023224465,0.0002759847,0.00026924777,0.00032665307,0.00034723704,0.00009902951],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033358578,0.000031576958,0.6164254,0.000035889647,0.000056817982,0.00009752376,0.00033160637,0.00088069163,0.37684417,0.00027456248,0.0000913436,0.0045968024],"study_design_scores_gemma":[0.000003765829,0.000049589984,0.9715057,0.0000021746157,0.000014180221,0.00008059795,0.000097152304,0.0019797704,0.025937488,0.00011596137,0.0002069918,0.0000065759327],"about_ca_topic_score_codex":0.0026713058,"about_ca_topic_score_gemma":0.0031387303,"teacher_disagreement_score":0.0026713058,"about_ca_system_score_codex":0.0001710001,"about_ca_system_score_gemma":0.00009463933,"threshold_uncertainty_score":0.005311489},"labels":[],"label_agreement":null},{"id":"W1585345649","doi":"10.1029/2010gl042678","title":"Microburst precipitation of energetic electrons associated with chorus wave generation","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Microburst; Chorus; Electron; Electron precipitation; Van Allen radiation belt; Physics; Precipitation; Atmosphere (unit); Atmospheric sciences; Computational physics; Meteorology; Magnetosphere; Nuclear physics; Plasma; Wind shear","score_opus":0.015259267536629862,"score_gpt":0.26195222891046643,"score_spread":0.24669296137383656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1585345649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99275196,0.00004936607,0.0039224387,0.00010089846,0.000018450322,0.00002273369,0.000114260234,0.00007083836,0.0029490662],"genre_scores_gemma":[0.99889636,0.000027411497,0.00068477,0.000012230231,0.0000045972843,0.000013628763,0.00008739431,0.000013876098,0.0002595616],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000010646989,0.0000030599936,0.000008139883,0.00001412174,0.000022998394],"domain_scores_gemma":[0.99973565,0.000093613584,0.00005773678,0.000024354744,0.000031393363,0.000057306974],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015017067,0.00024269636,0.00031079358,0.00024535894,0.00043696893,0.0003472511,0.0004285874,0.00045737476,0.0013612236],"category_scores_gemma":[0.0010549458,0.00022132162,0.00035490195,0.00021879627,0.0004515262,0.00041300556,0.00047805387,0.00040257772,0.00007590251],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032739274,0.00014632089,0.033205673,0.00007301229,0.00009349322,0.0007278708,0.00020996932,0.94567347,0.010287547,0.004875443,0.00086827663,0.0035115676],"study_design_scores_gemma":[0.000068226494,0.000048291095,0.008738545,0.00000432913,0.000012442292,0.00005137551,0.00005237871,0.9881137,0.0018531246,0.0007516942,0.0002951701,0.000010609765],"about_ca_topic_score_codex":0.0110292835,"about_ca_topic_score_gemma":0.004294184,"teacher_disagreement_score":0.0110292835,"about_ca_system_score_codex":0.00045999425,"about_ca_system_score_gemma":0.00051745836,"threshold_uncertainty_score":0.021930158},"labels":[],"label_agreement":null},{"id":"W1586209620","doi":"10.1002/grl.50220","title":"Tremors along the Queen Charlotte Margin triggered by large teleseismic earthquakes","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Seismology; Geology; Epicenter; Rayleigh wave; Thrust fault; Amplitude; Tectonics; Fault (geology); Queen (butterfly); Geodesy; Surface wave","score_opus":0.02306543395290682,"score_gpt":0.25863779705872986,"score_spread":0.23557236310582302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1586209620","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99804485,0.0001535445,0.000060249204,0.000024184812,0.0000023390892,0.000018303488,0.0005956477,0.000008124479,0.0010926636],"genre_scores_gemma":[0.99856925,0.00010137758,0.000109716224,0.000017743545,0.0000025702018,0.000007527842,0.0004391517,0.0000024733683,0.00075007585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971956,0.000018451023,0.000013582386,0.000055818255,0.00013178689,0.000060775223],"domain_scores_gemma":[0.99847883,0.00013657923,0.00048293106,0.00006283744,0.0005575284,0.0002813218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015333867,0.00019434745,0.000204875,0.0021995406,0.0010416891,0.0006182607,0.0004047023,0.00025859821,0.0009274278],"category_scores_gemma":[0.0008245776,0.00012868264,0.00013085773,0.002073797,0.00047260206,0.00012878698,0.000523907,0.00016181899,0.00016850005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014044676,0.000031804553,0.97263217,0.000063905856,0.000046369893,0.00066227716,0.0009966074,0.00031201792,0.012376701,0.000069096604,0.00067858474,0.01199002],"study_design_scores_gemma":[0.0000022591153,0.000016271062,0.9985636,0.000007001447,0.0000047721414,0.00007392847,0.00030784533,0.000101233054,0.00033783508,0.000004799732,0.00057652977,0.0000039975766],"about_ca_topic_score_codex":0.78992695,"about_ca_topic_score_gemma":0.92433673,"teacher_disagreement_score":0.78992695,"about_ca_system_score_codex":0.003215003,"about_ca_system_score_gemma":0.004217504,"threshold_uncertainty_score":0.42262042},"labels":[],"label_agreement":null},{"id":"W1588975770","doi":"10.1029/2012gl052462","title":"Ocean circulation promotes methane release from gas hydrate outcrops at the NEPTUNE Canada Barkley Canyon node","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of Victoria","funders":"","keywords":"Geology; Clathrate hydrate; Canyon; Methane; Outcrop; Seafloor spreading; Petroleum seep; Benthic zone; Submarine canyon; Continental shelf; Submarine pipeline; Sediment; Oceanography; Hydrate; Geomorphology","score_opus":0.022568681673258872,"score_gpt":0.25895149636051806,"score_spread":0.2363828146872592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1588975770","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990089,0.000026794598,0.000012241131,0.000015936192,0.0000014547916,0.0000026541911,0.000079115634,0.0000041430153,0.0008487497],"genre_scores_gemma":[0.9982343,0.000041437943,0.000047896614,0.000017306473,6.628392e-7,0.000004283746,0.00015068142,0.000003141279,0.0015001834],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999422,0.0000023568537,0.0000011294953,0.00001540724,0.000011704176,0.000027282043],"domain_scores_gemma":[0.999752,0.000019514853,0.000028557204,0.000007181078,0.000067111454,0.00012561673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000049586884,0.00017497176,0.00016933226,0.00026979845,0.0010916736,0.00050162256,0.00029586937,0.000260116,0.002035676],"category_scores_gemma":[0.00023618086,0.00022242336,0.00010820423,0.00026379107,0.0003509491,0.00012016261,0.00054019794,0.00032087593,0.00019879494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009754766,0.00012207715,0.5954233,0.000109773355,0.000076462886,0.0018155165,0.0026498672,0.0015789953,0.38423702,0.0002519302,0.0022753477,0.010484226],"study_design_scores_gemma":[0.0000073810743,0.000040908766,0.9937596,0.000008127253,0.00001183596,0.00003365057,0.0010644323,0.00056153914,0.0038568354,0.000013330366,0.000636427,0.0000059647346],"about_ca_topic_score_codex":0.710935,"about_ca_topic_score_gemma":0.89281446,"teacher_disagreement_score":0.710935,"about_ca_system_score_codex":0.002846547,"about_ca_system_score_gemma":0.002039438,"threshold_uncertainty_score":0.58153474},"labels":[],"label_agreement":null},{"id":"W1590550131","doi":"10.1002/2014gl062759","title":"Recent changes in the freshwater composition east of Greenland","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Seventh Framework Programme; Centre National d’Etudes Spatiales; European Commission; National Science Foundation","keywords":"Oceanography; Hydrography; Salinity; Arctic; Geology; Water mass; Meteoric water; Brine; Structural basin; Groundwater","score_opus":0.060299471219764034,"score_gpt":0.2862494739857352,"score_spread":0.22595000276597116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1590550131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974661,0.00019734669,0.00008569983,0.00014746173,0.00000672369,0.0000029602115,0.0011549646,0.000011252408,0.0009275198],"genre_scores_gemma":[0.99784184,0.00014529814,0.00018787416,0.000078203855,0.000004437523,0.0000030245294,0.0009518244,0.0000049711834,0.0007825781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988484,0.000009173702,0.000008513167,0.000033781962,0.000019732393,0.00004395774],"domain_scores_gemma":[0.9996939,0.000017552473,0.00010006141,0.000012675107,0.000110815046,0.000064999644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022661319,0.00018795113,0.00017451472,0.0009870186,0.00035755883,0.0006568744,0.00022351522,0.00017954869,0.0008222425],"category_scores_gemma":[0.00038326986,0.000100513855,0.00017982128,0.0014173844,0.000357321,0.00041057914,0.0005762398,0.00016054827,0.000115242845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014529357,0.000018775605,0.9713426,0.000058604674,0.00012192789,0.00029782747,0.0010467718,0.000901158,0.0055471854,0.0003261328,0.0009899022,0.019203832],"study_design_scores_gemma":[5.997877e-7,0.0000036083763,0.9986512,0.0000057393245,0.0000043458263,0.000021292313,0.00018804053,0.000113399765,0.00013729789,0.000017022288,0.00085557543,0.0000017946084],"about_ca_topic_score_codex":0.2957531,"about_ca_topic_score_gemma":0.57321066,"teacher_disagreement_score":0.2957531,"about_ca_system_score_codex":0.0029402117,"about_ca_system_score_gemma":0.0014142334,"threshold_uncertainty_score":0.58806324},"labels":[],"label_agreement":null},{"id":"W1591289697","doi":"10.1029/2010gl045565","title":"Mapping permeability over the surface of the Earth","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":418,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"U.S. Geological Survey; Deutsche Forschungsgemeinschaft","keywords":"Geology; Earth (classical element); Permeability (electromagnetism); Geophysics; Earth surface; Astrobiology; Physics; Chemistry","score_opus":0.07459426117986286,"score_gpt":0.298815131438858,"score_spread":0.22422087025899518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1591289697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9289821,0.0009946064,0.052372556,0.00013809722,0.000010986643,0.000022999924,0.004134662,0.00076227775,0.012581808],"genre_scores_gemma":[0.9901419,0.0004014103,0.0079359235,0.000010940346,0.000009499474,0.000008592312,0.0010234528,0.000038431215,0.0004298966],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.000006640673,0.0000019223314,0.00001936353,0.000015895714,0.000007333939],"domain_scores_gemma":[0.999897,0.000031409843,0.000026209991,0.000015029558,0.00001962579,0.000010663368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010120142,0.00017551715,0.00012153459,0.0008508713,0.00018972465,0.00036849445,0.00016829051,0.00015318084,0.0010478696],"category_scores_gemma":[0.00052418496,0.00009724551,0.000094629046,0.0010056692,0.0001657234,0.0006741269,0.00036435865,0.00013014818,0.0002140532],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002994334,0.00009913867,0.28009507,0.0003890697,0.00014237815,0.00044634892,0.0006615875,0.19670825,0.21260692,0.007862007,0.0052390643,0.29545072],"study_design_scores_gemma":[0.000018767525,0.00011623859,0.6501959,0.00006180707,0.00007893741,0.000892814,0.0003659272,0.27125672,0.046985254,0.013331581,0.016615845,0.00008022509],"about_ca_topic_score_codex":0.0042412183,"about_ca_topic_score_gemma":0.0039552175,"teacher_disagreement_score":0.0042412183,"about_ca_system_score_codex":0.00019390749,"about_ca_system_score_gemma":0.0001533473,"threshold_uncertainty_score":0.008433104},"labels":[],"label_agreement":null},{"id":"W1591602797","doi":"10.1029/2011gl047953","title":"Improved Os-isotope stratigraphy of the Arctic Ocean","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":135,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Stratigraphy; Paleontology; Coring; Ridge; Marine isotope stage; Arctic; Tectonics; Oceanography; Interglacial; Quaternary; Drilling","score_opus":0.06348893583393374,"score_gpt":0.25454937991205273,"score_spread":0.191060444078119,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1591602797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9688649,0.004755309,0.011106342,0.0001778492,0.000109498375,0.000009311418,0.002397411,0.00018304746,0.012396289],"genre_scores_gemma":[0.98212713,0.0024049208,0.010181454,0.0000511533,0.00008037212,0.0000048227,0.0021531314,0.00004309705,0.0029540309],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.000005538604,0.0000052540518,0.000020382395,0.000014337276,0.0000075322064],"domain_scores_gemma":[0.9999063,0.0000041499175,0.000019812202,0.000007796754,0.000055197626,0.0000067202996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019871989,0.0003131623,0.00013354907,0.001085993,0.00022545502,0.0003548255,0.0001702387,0.0001286099,0.00067991484],"category_scores_gemma":[0.00017768565,0.000091756985,0.00006072467,0.0010195635,0.00014859486,0.00025840866,0.00021888246,0.00015469402,0.00023503898],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044292284,0.000030977444,0.2902763,0.00027348424,0.000072980685,0.00028494085,0.00055768364,0.0042198687,0.52492887,0.0028000418,0.0014923449,0.17461957],"study_design_scores_gemma":[0.000012218642,0.00014936218,0.803423,0.00009097134,0.000105256826,0.00049608905,0.0003218158,0.009744125,0.1179227,0.0010321625,0.066659965,0.00004229447],"about_ca_topic_score_codex":0.019810356,"about_ca_topic_score_gemma":0.042664308,"teacher_disagreement_score":0.019810356,"about_ca_system_score_codex":0.0004038575,"about_ca_system_score_gemma":0.00031832108,"threshold_uncertainty_score":0.039390087},"labels":[],"label_agreement":null},{"id":"W1591980695","doi":"10.1029/2010gl044255","title":"Comparing variability and trends in observed and modelled global‐mean surface temperature","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Climatology; Volcano; Mean radiant temperature; Forcing (mathematics); Environmental science; Global temperature; Global warming; Natural (archaeology); Surface air temperature; Southern oscillation; Climate model; Atmospheric temperature; Explosive material; Climate change; Atmospheric sciences; Series (stratigraphy); Oscillation (cell signaling); Geology; El Niño Southern Oscillation; Geography","score_opus":0.06147836533785864,"score_gpt":0.31290606712481345,"score_spread":0.25142770178695484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1591980695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977907,0.00007241703,0.0007223984,0.00009686442,0.000009647928,0.000001672129,0.00060450385,0.000023297842,0.00067850464],"genre_scores_gemma":[0.9984414,0.000046127247,0.00022965472,0.000011246676,0.000007989597,0.000003398676,0.0011764714,0.000007425798,0.000076258395],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997346,0.000078643636,0.000023059923,0.00008440393,0.000048170492,0.00003115806],"domain_scores_gemma":[0.9987587,0.00073549396,0.00017947177,0.00015218156,0.00014604538,0.000028133903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00079724105,0.00012694095,0.00010797674,0.00043913932,0.000111225585,0.00050927856,0.00026141354,0.0003139641,0.0004256928],"category_scores_gemma":[0.0037621863,0.00011260576,0.00035604637,0.00070354925,0.00022428289,0.00064865354,0.00023075279,0.00035108664,0.00009209992],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004051855,0.00013381327,0.8772394,0.000103353,0.00078254915,0.000114930845,0.00037427712,0.09253001,0.00708869,0.0014454619,0.0011733206,0.018609015],"study_design_scores_gemma":[0.000030942694,0.000088734894,0.91312486,0.000016738066,0.0000873921,0.00007604381,0.00019203183,0.0815066,0.002695919,0.00066168234,0.0014922994,0.000026772668],"about_ca_topic_score_codex":0.006891364,"about_ca_topic_score_gemma":0.009311191,"teacher_disagreement_score":0.006891364,"about_ca_system_score_codex":0.00047025856,"about_ca_system_score_gemma":0.00021692223,"threshold_uncertainty_score":0.013702512},"labels":[],"label_agreement":null},{"id":"W1592226826","doi":"10.1029/2009gl042143","title":"Thermospheric density enhancements in the dayside cusp region during strong B<sub>Y</sub> conditions","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Air Force Office of Scientific Research; Multidisciplinary University Research Initiative; University of Texas at Dallas; University of Alberta; University of Texas at San Antonio; Science and Technology Facilities Council; Johns Hopkins University; University of Michigan; National Aeronautics and Space Administration; National Science Foundation","keywords":"Thermosphere; Cusp (singularity); Ionosphere; Latitude; Physics; Atmospheric sciences; Geophysics; Computational physics; Astronomy; Geometry","score_opus":0.014705621018447055,"score_gpt":0.2799854803887677,"score_spread":0.2652798593703206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1592226826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886215,0.000022633378,0.00020047138,0.000054943986,0.0000032857445,0.000002259739,0.00007715869,0.000023315653,0.00075374515],"genre_scores_gemma":[0.99976426,0.000010401667,0.00010782104,0.0000057531624,0.0000016694457,0.0000016978313,0.000052223397,0.0000034456366,0.00005266377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997675,0.0000045387246,0.0000012433057,0.0000056748186,0.0000036226438,0.0000082350525],"domain_scores_gemma":[0.99992275,0.000021507918,0.000018747305,0.0000071983914,0.00001077655,0.000019114565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011124967,0.00015638446,0.00014615354,0.00013086174,0.00025026526,0.00024702036,0.00017995283,0.00022973855,0.0008567231],"category_scores_gemma":[0.00035645033,0.00016122541,0.00019867519,0.00012775345,0.00022864397,0.00022328476,0.0002868341,0.0002453868,0.00006740082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011312743,0.00020334398,0.5642063,0.00009525225,0.00021034095,0.001755944,0.00069569674,0.29551744,0.114938065,0.0031037338,0.0035652812,0.014577258],"study_design_scores_gemma":[0.00008768268,0.00011139489,0.55733454,0.000009524017,0.00003532189,0.00016301226,0.0002254597,0.43408546,0.0063894386,0.000694849,0.00084393006,0.00001943774],"about_ca_topic_score_codex":0.014779644,"about_ca_topic_score_gemma":0.014129772,"teacher_disagreement_score":0.014779644,"about_ca_system_score_codex":0.00038640102,"about_ca_system_score_gemma":0.00020437357,"threshold_uncertainty_score":0.029387236},"labels":[],"label_agreement":null},{"id":"W1593331112","doi":"10.1029/2012gl052512","title":"Evidence for El Niño–Southern Oscillation (ENSO) influence on Arctic CO interannual variability through biomass burning emissions","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Environmental science; Boreal; Climatology; Biomass burning; Arctic; El Niño Southern Oscillation; Atmospheric sciences; The arctic; Biomass (ecology); Arctic oscillation; Precipitation; Oceanography; Meteorology; Geography; Northern Hemisphere; Aerosol; Geology","score_opus":0.05644506256581935,"score_gpt":0.355653685281938,"score_spread":0.2992086227161187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1593331112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977921,0.000092543385,0.00017758139,0.00008553715,0.000008054849,0.0000015159848,0.00013054918,0.000011552352,0.0017005069],"genre_scores_gemma":[0.9996425,0.00006576297,0.000050911887,0.00001236602,0.00000441415,8.2637195e-7,0.00011723002,0.0000035961577,0.00010241399],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984777,0.00005735611,0.000012759732,0.000030080133,0.000023740808,0.000028326473],"domain_scores_gemma":[0.9987907,0.0006221002,0.00022329524,0.0000768982,0.0001372766,0.00014986588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006744543,0.00020444355,0.00016657812,0.00030075596,0.0002830785,0.00053600245,0.00018123603,0.0001474686,0.0014725912],"category_scores_gemma":[0.0014996942,0.00021453295,0.00039388993,0.00027087994,0.000337321,0.00027744498,0.00039736874,0.00018337743,0.00011200583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006550915,0.00012821464,0.95247614,0.00006679556,0.00031721083,0.00024239518,0.00015628432,0.029716702,0.007982338,0.0010477111,0.00055326876,0.006657873],"study_design_scores_gemma":[0.00003994796,0.00007701214,0.9545969,0.000013413906,0.000102876984,0.00004794432,0.00016033588,0.0428943,0.000994336,0.00034723134,0.0007148457,0.000010870353],"about_ca_topic_score_codex":0.030263674,"about_ca_topic_score_gemma":0.03729427,"teacher_disagreement_score":0.030263674,"about_ca_system_score_codex":0.00038554316,"about_ca_system_score_gemma":0.00046792242,"threshold_uncertainty_score":0.060175},"labels":[],"label_agreement":null},{"id":"W1593617336","doi":"10.1029/2001gl013785","title":"Does the braking of the fast plasma flow trigger a substorm?: A study of the August 14, 1996, event","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Optometric Education Trust Fund","funders":"","keywords":"Substorm; Physics; Geosynchronous orbit; Geophysics; Satellite; Magnetic field; Plasma; Local time; Flux (metallurgy); Plasma sheet; Event (particle physics); Flow (mathematics); Magnetosphere; Astrophysics; Mechanics; Astronomy; Materials science","score_opus":0.017366277621743087,"score_gpt":0.2641842996682898,"score_spread":0.24681802204654674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1593617336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99965274,0.00003114036,0.00002606802,0.000020758815,0.0000012900477,0.0000037553364,0.000035802397,0.0000018158651,0.00022667747],"genre_scores_gemma":[0.9996718,0.000043070686,0.00003825938,0.00001808985,0.000008336808,0.000003022578,0.00011813097,0.0000014961305,0.00009784028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999355,0.000012578311,0.0000049744835,0.000011792071,0.000009278788,0.000025780899],"domain_scores_gemma":[0.9996972,0.000061556835,0.000106539046,0.000026801965,0.000038303944,0.000069690795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021881566,0.00012887592,0.00021102566,0.00026132906,0.0005071899,0.00049951766,0.0001694009,0.0003306198,0.0006688254],"category_scores_gemma":[0.0006840664,0.000102400576,0.0001368996,0.00027029304,0.0003379459,0.0002655367,0.00032448256,0.00027350985,0.00015074036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011203922,0.00019997299,0.95727473,0.000044639113,0.00009523529,0.0043754475,0.0021698023,0.00031854058,0.023476636,0.00028911405,0.00047996722,0.010155524],"study_design_scores_gemma":[0.000019031986,0.00016462212,0.99739516,0.0000037083346,0.000017809636,0.0005287631,0.00064492226,0.0003160484,0.0004514989,0.00006546917,0.0003900329,0.000003050262],"about_ca_topic_score_codex":0.011153103,"about_ca_topic_score_gemma":0.015829813,"teacher_disagreement_score":0.011153103,"about_ca_system_score_codex":0.00037095006,"about_ca_system_score_gemma":0.00017047163,"threshold_uncertainty_score":0.022176385},"labels":[],"label_agreement":null},{"id":"W1594169643","doi":"10.1029/2011gl050196","title":"Linkages between the cold summer mesopause and thermospheric zonal mean circulation","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Toronto","funders":"Office of Naval Research; National Center for Atmospheric Research; National Aeronautics and Space Administration","keywords":"Mesopause; Thermosphere; Atmospheric sciences; Climatology; Stratosphere; Mesosphere; Environmental science; Atmospheric circulation; Atmosphere (unit); Atmospheric tide; Northern Hemisphere; General Circulation Model; Ionosphere; Meteorology; Geology; Physics; Climate change; Geophysics","score_opus":0.045238743538052024,"score_gpt":0.28740554250080713,"score_spread":0.24216679896275511,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1594169643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980636,0.00005486431,0.00034553668,0.000070286245,0.000005632525,0.0000029047808,0.00046343956,0.00004708874,0.000946696],"genre_scores_gemma":[0.9991773,0.00002999965,0.00016766148,0.000011139947,0.0000051885954,0.0000028129202,0.00041213442,0.000008115668,0.00018556169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999478,0.000009986167,0.0000022078198,0.000014255702,0.0000064729124,0.000019213736],"domain_scores_gemma":[0.99977225,0.000075939635,0.000046340552,0.000027962113,0.000023712473,0.000053751573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013286267,0.0001959045,0.000180286,0.00019977408,0.00026968066,0.00044745358,0.000149892,0.00016411924,0.0017134479],"category_scores_gemma":[0.0005924979,0.00016729935,0.00024258324,0.000277072,0.00016297477,0.00024571596,0.00033830033,0.00024225134,0.00007760624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004937054,0.00007630634,0.92496395,0.0000469641,0.00029257574,0.00019719785,0.00022879562,0.035560485,0.023416966,0.0013528746,0.0016319023,0.011738318],"study_design_scores_gemma":[0.000015327212,0.000044527947,0.9790132,0.0000031399932,0.00003232379,0.000027574697,0.000049053342,0.019123662,0.0007716527,0.00029262487,0.0006171664,0.000009791993],"about_ca_topic_score_codex":0.04195967,"about_ca_topic_score_gemma":0.06378895,"teacher_disagreement_score":0.04195967,"about_ca_system_score_codex":0.00029416825,"about_ca_system_score_gemma":0.00033239127,"threshold_uncertainty_score":0.083430886},"labels":[],"label_agreement":null},{"id":"W1597111655","doi":"10.1029/2012gl054199","title":"Human influence on extratropical Southern Hemisphere summer precipitation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"British Antarctic Survey; Office of Science; Sight Research UK; National Oceanic and Atmospheric Administration; Natural Environment Research Council; U.S. Department of Energy","keywords":"Extratropical cyclone; Southern Hemisphere; Climatology; Precipitation; Environmental science; Northern Hemisphere; Atmospheric sciences; Latitude; Stratification (seeds); Climate change; Oceanography; Geology; Meteorology; Geography","score_opus":0.059268969326151485,"score_gpt":0.3428366387686428,"score_spread":0.2835676694424913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1597111655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983876,0.000075073796,0.00009616178,0.00006235356,0.0000045748297,0.0000011796637,0.0003010186,0.000011282681,0.0010609247],"genre_scores_gemma":[0.99956363,0.00008135302,0.000040079598,0.0000078282965,0.0000030811364,9.975131e-7,0.00013192551,0.0000023643142,0.00016861691],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993503,0.000024172223,0.0000036871577,0.0000119697925,0.000010128458,0.000014991908],"domain_scores_gemma":[0.99980646,0.000060150694,0.000036092915,0.000019660072,0.000037083755,0.000040565305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016587833,0.00014062808,0.00013300769,0.00020215737,0.0001743434,0.00034009476,0.000113774135,0.00013927238,0.0016067941],"category_scores_gemma":[0.00059827376,0.000084872285,0.00024539194,0.00039721007,0.00020451589,0.00017167939,0.00026687782,0.00012242649,0.00011401112],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025038788,0.000058671318,0.87974185,0.000059574344,0.00018152098,0.00030531123,0.00028189586,0.096062064,0.003683473,0.0008242947,0.001367106,0.017183784],"study_design_scores_gemma":[0.00001842032,0.00002834867,0.96363574,0.000008331212,0.000033431195,0.000048463233,0.00019805053,0.034051802,0.0004972119,0.00032940545,0.0011417038,0.000009052254],"about_ca_topic_score_codex":0.07948124,"about_ca_topic_score_gemma":0.11967756,"teacher_disagreement_score":0.07948124,"about_ca_system_score_codex":0.00056869484,"about_ca_system_score_gemma":0.00049844297,"threshold_uncertainty_score":0.15803725},"labels":[],"label_agreement":null},{"id":"W1597301243","doi":"10.1029/2003gl018999","title":"How efficient is cloud droplet formation of organic aerosols?","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Toronto; Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Supersaturation; Aerosol; Nucleation; Ammonium sulfate; Adipic acid; Cloud condensation nuclei; Sulfate; Chemistry; Environmental chemistry; Chemical engineering; Atmospheric sciences; Organic chemistry; Physics","score_opus":0.02319565825111435,"score_gpt":0.2525585631164108,"score_spread":0.22936290486529642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1597301243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9776179,0.0041485857,0.009856669,0.0002860997,0.00007867045,0.000058493417,0.00024460416,0.00011498386,0.0075939777],"genre_scores_gemma":[0.99629754,0.0010630223,0.0014327766,0.000037957358,0.000018121718,0.000008345532,0.0001435711,0.000017573453,0.000980998],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99950886,0.000057516296,0.000021433443,0.00010711909,0.00015056995,0.00015449086],"domain_scores_gemma":[0.99971133,0.00009458623,0.00006274854,0.000041474254,0.000047054247,0.000042716987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004210564,0.00031250616,0.00035804542,0.00029740672,0.00019920098,0.0008972731,0.00039327482,0.0004245696,0.001310363],"category_scores_gemma":[0.0009474209,0.00021189787,0.00035938493,0.00020886854,0.00033704308,0.0013400288,0.00035855302,0.00021967925,0.00047337572],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023141758,0.000082006445,0.014542791,0.00024944174,0.00008742928,0.0002859185,0.00006377544,0.0062035834,0.94828886,0.00424343,0.00028936358,0.025432035],"study_design_scores_gemma":[0.00003850789,0.00031479483,0.019260548,0.000016419177,0.00006606801,0.00043779606,0.00014371033,0.018846352,0.95349234,0.002036369,0.005321625,0.00002548692],"about_ca_topic_score_codex":0.0021039485,"about_ca_topic_score_gemma":0.0013312661,"teacher_disagreement_score":0.0021039485,"about_ca_system_score_codex":0.00064844923,"about_ca_system_score_gemma":0.00026393772,"threshold_uncertainty_score":0.0047048926},"labels":[],"label_agreement":null},{"id":"W1597405737","doi":"10.1029/2010gl045321","title":"Interannual to decadal variability of outflow from the Labrador Sea","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung, Wissenschaft und Forschung; Bundesministerium für Bildung und Forschung","keywords":"Geology; Current (fluid); Current meter; Outflow; Water mass; Oceanography; Advection; Boundary current; Water column; Climatology; Deep convection; Submarine pipeline; Convection; Environmental science; Ocean current; Meteorology; Geography","score_opus":0.015919149491156314,"score_gpt":0.27096909830105287,"score_spread":0.25504994880989657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1597405737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814487,0.00008631568,0.00006716799,0.000027106431,0.0000067232045,0.0000016930696,0.00093677634,0.000024302612,0.00070503383],"genre_scores_gemma":[0.99792236,0.00007537253,0.000059652335,0.000017433016,0.000007478815,0.000003734256,0.0014531707,0.000007413866,0.00045340808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986947,0.000019477706,0.0000148131385,0.000042802618,0.000016837947,0.000036686688],"domain_scores_gemma":[0.9996557,0.00005476835,0.00013932405,0.00003998719,0.00006825125,0.000041874617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035172654,0.00019895022,0.00017632163,0.00070853106,0.00017343016,0.0006466749,0.0001875977,0.00018340068,0.0010603837],"category_scores_gemma":[0.0005404596,0.00008184975,0.00018321628,0.00064041466,0.00012442381,0.00026064576,0.0003462074,0.00018689033,0.00037378975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023551438,0.000038915186,0.98255324,0.000021760206,0.00012873925,0.00007590004,0.00019897771,0.0006415809,0.0027874096,0.000058471338,0.0007402578,0.012519173],"study_design_scores_gemma":[0.0000019958466,0.000012266803,0.9989849,0.0000029342111,0.000012367129,0.000025381121,0.00006038036,0.00021469545,0.00025980826,0.000007820796,0.00041451014,0.0000028855154],"about_ca_topic_score_codex":0.015679257,"about_ca_topic_score_gemma":0.020350732,"teacher_disagreement_score":0.015679257,"about_ca_system_score_codex":0.0004006636,"about_ca_system_score_gemma":0.00018879978,"threshold_uncertainty_score":0.03117603},"labels":[],"label_agreement":null},{"id":"W1599301092","doi":"10.1002/2014gl059696","title":"Multidecadal modulations of the low‐frequency climate variability in the wintertime North Pacific since 1950","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Extratropical cyclone; Subarctic climate; Anticyclone; Sea surface temperature; Subtropics; Environmental science; Spatial variability; Geology; Oceanography; Atmospheric sciences","score_opus":0.026384212411946,"score_gpt":0.28475986582525387,"score_spread":0.25837565341330787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1599301092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99874985,0.00010534924,0.0001399524,0.00007837197,0.0000074477766,0.0000013869769,0.00030055174,0.000008622123,0.00060838513],"genre_scores_gemma":[0.99957067,0.000037716323,0.000040576007,0.0000065419877,0.000004490718,0.0000014898883,0.00021349096,0.00000136583,0.00012369656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999701,0.0000041364397,0.0000020497337,0.000011845047,0.000004719621,0.0000071772897],"domain_scores_gemma":[0.9998635,0.000030061823,0.00003983984,0.0000121583125,0.000030765917,0.000023636065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017315487,0.00008558065,0.00008807687,0.00039269484,0.0002203648,0.00041287448,0.000101171114,0.0001168878,0.0007023601],"category_scores_gemma":[0.00043271357,0.000077244826,0.00012865369,0.00041378188,0.0001624764,0.00017644138,0.0002671184,0.00021224305,0.00006381228],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000107161606,0.0000434643,0.967581,0.00002796624,0.00010972474,0.0001315108,0.00043049938,0.0056058643,0.0085918065,0.0004804184,0.0010911768,0.015799565],"study_design_scores_gemma":[0.000002371454,0.000009813537,0.9969511,0.0000031057368,0.000011183495,0.000014954413,0.000043694923,0.0020577786,0.00018450666,0.000058284546,0.0006603749,0.000002606814],"about_ca_topic_score_codex":0.020738835,"about_ca_topic_score_gemma":0.026449736,"teacher_disagreement_score":0.020738835,"about_ca_system_score_codex":0.0005116043,"about_ca_system_score_gemma":0.00015880223,"threshold_uncertainty_score":0.04123628},"labels":[],"label_agreement":null},{"id":"W1599730348","doi":"10.1002/grl.50156","title":"Surface response to stratospheric aerosol changes in a coupled atmosphere–ocean model","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Stratosphere; Precipitation; Climate model; Atmosphere (unit); Climatology; Sulfate aerosol; Atmospheric model; Global warming; Climate change; Meteorology; Geology; Geography; Oceanography","score_opus":0.0404333818989959,"score_gpt":0.2998175914321489,"score_spread":0.259384209533153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1599730348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940771,0.000082850165,0.0011582496,0.0003124336,0.000048574246,0.000023440567,0.0010129971,0.00016887077,0.0031155217],"genre_scores_gemma":[0.9978903,0.00005093565,0.00064447464,0.000075027594,0.0000107705955,0.00002476187,0.0007000144,0.000023080425,0.0005805952],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981624,0.000060712737,0.000010432489,0.000043961394,0.000021339285,0.000047321424],"domain_scores_gemma":[0.9994974,0.00024780698,0.000044430442,0.000036107605,0.000083584426,0.00009060967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048696945,0.0008550623,0.0008080281,0.00045696253,0.0006710197,0.0011937034,0.0012523488,0.0017121809,0.0022337714],"category_scores_gemma":[0.0014571034,0.0005810565,0.0011472376,0.0005140055,0.0006576486,0.00068612007,0.0008160026,0.00094292266,0.0002075769],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018230824,0.000094417424,0.009009984,0.000023906729,0.00015379458,0.00007759547,0.000025507454,0.9878457,0.0012891277,0.00033075447,0.00036661196,0.00060030055],"study_design_scores_gemma":[0.00012758594,0.00008868022,0.00427379,0.0000035427495,0.00005523895,0.0000065268237,0.000030070096,0.9946228,0.0003839724,0.00020544067,0.00018603734,0.000016272497],"about_ca_topic_score_codex":0.105987996,"about_ca_topic_score_gemma":0.045894206,"teacher_disagreement_score":0.105987996,"about_ca_system_score_codex":0.0014411535,"about_ca_system_score_gemma":0.0013459995,"threshold_uncertainty_score":0.21074218},"labels":[],"label_agreement":null},{"id":"W1601006326","doi":"10.1029/2011gl046870","title":"Release of multiple bubbles from cohesive sediments","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Office of Naval Research; Killam Trusts; Dalhousie University","keywords":"Geology; Mineralogy; Geophysics","score_opus":0.04471645532396936,"score_gpt":0.27685906654132514,"score_spread":0.23214261121735577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1601006326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98967147,0.00038747973,0.008825342,0.000095108066,0.00003106403,0.000014701763,0.00010916304,0.00009069781,0.00077505445],"genre_scores_gemma":[0.99879056,0.00008528072,0.0008070382,0.0000063884827,0.000006350681,0.0000051797265,0.0000583124,0.0000060908706,0.00023478168],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991024,0.0000063052016,0.0000054466473,0.000029641658,0.000026904874,0.000021342432],"domain_scores_gemma":[0.9997775,0.00007304154,0.00007069458,0.000018355857,0.00002776419,0.000032664673],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018213775,0.00031113243,0.00023094626,0.00031664243,0.00031021927,0.00034882536,0.00037816176,0.00023199942,0.0012077717],"category_scores_gemma":[0.0006969875,0.0002172298,0.00017135557,0.00013405713,0.0003316006,0.00069411926,0.00037777043,0.00032213755,0.00012277675],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006423109,0.00016478,0.08700375,0.00041002512,0.00013178766,0.0032799835,0.00042240194,0.043258455,0.8296049,0.0044987183,0.0011023307,0.029480543],"study_design_scores_gemma":[0.00008108709,0.0007003566,0.09082925,0.00004356373,0.00012069031,0.0011894939,0.0003443305,0.33155185,0.5691691,0.0027465427,0.003161619,0.00006215888],"about_ca_topic_score_codex":0.0021397136,"about_ca_topic_score_gemma":0.0028312895,"teacher_disagreement_score":0.0021397136,"about_ca_system_score_codex":0.00041914635,"about_ca_system_score_gemma":0.0001744159,"threshold_uncertainty_score":0.0042544603},"labels":[],"label_agreement":null},{"id":"W1601447128","doi":"10.1029/2010gl043219","title":"Deepest mantle viscosity: Constraints from Earth rotation anomalies","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mantle (geology); Post-glacial rebound; Geophysics; Earth's rotation; Polar; Inner core; Viscosity; Geodesy; Glacial period; Physics; Paleontology; Thermodynamics","score_opus":0.02250874900743095,"score_gpt":0.27123000836453703,"score_spread":0.2487212593571061,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1601447128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9862059,0.0023035153,0.0037605253,0.00027434627,0.00000865699,0.0000036524339,0.0004022992,0.00006107294,0.0069798967],"genre_scores_gemma":[0.9986808,0.00042835745,0.00057847396,0.000013064407,0.000010544623,0.0000021062715,0.00015030481,0.000011555606,0.00012460278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999161,0.000013697834,0.000005715784,0.000018419798,0.000021994163,0.000023983976],"domain_scores_gemma":[0.99905187,0.00047021575,0.0002487046,0.000075070166,0.000065246364,0.000088883266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002738856,0.00040989538,0.00034135918,0.0008733548,0.00021850629,0.0012804796,0.00033292308,0.0002562345,0.0012748229],"category_scores_gemma":[0.0024121809,0.00031694476,0.00017788025,0.00041271883,0.00039988858,0.0009778258,0.0008390705,0.00071551604,0.0001773928],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017625601,0.00014910719,0.446402,0.0004142151,0.00017044271,0.001017216,0.001170895,0.024402373,0.33004895,0.04895897,0.0015931599,0.14391008],"study_design_scores_gemma":[0.00009740992,0.00021237704,0.8236595,0.0001791704,0.00015592774,0.0006608881,0.00039306207,0.07624599,0.041327313,0.0498474,0.0070935246,0.00012740915],"about_ca_topic_score_codex":0.0024174592,"about_ca_topic_score_gemma":0.0026087316,"teacher_disagreement_score":0.0024174592,"about_ca_system_score_codex":0.00026037925,"about_ca_system_score_gemma":0.00022059542,"threshold_uncertainty_score":0.004806757},"labels":[],"label_agreement":null},{"id":"W1601934020","doi":"10.1029/2010gl044629","title":"Volcanic ash fuels anomalous plankton bloom in subarctic northeast Pacific","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":303,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; University of Victoria","funders":"National Oceanic and Atmospheric Administration","keywords":"Iron fertilization; Subarctic climate; Volcanic ash; Bloom; Oceanography; Volcano; Geology; Phytoplankton; Plankton; Algal bloom; Environmental science; Dominance (genetics); Nutrient; Geochemistry; Ecology; Chemistry","score_opus":0.016699874912526648,"score_gpt":0.24454493865328913,"score_spread":0.2278450637407625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1601934020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953055,0.000107749176,0.000016981896,0.000012591311,0.0000014213412,7.1302867e-7,0.00007026153,0.0000029591192,0.00025671837],"genre_scores_gemma":[0.9994785,0.00017072377,0.000051997395,0.000009045603,0.0000026994176,0.0000010158114,0.00010213192,8.9504266e-7,0.00018283525],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997675,0.000002470405,0.0000018543371,0.0000052980236,0.0000068463387,0.0000068291165],"domain_scores_gemma":[0.99984133,0.000017323144,0.000071145354,0.000008359416,0.000025559062,0.000036246398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000099875535,0.00010638635,0.00014056507,0.000370993,0.00024394681,0.0002525503,0.000078345496,0.00012018528,0.0005012825],"category_scores_gemma":[0.00019713765,0.00010668848,0.00007112052,0.00025933472,0.00014635897,0.00014943747,0.00019616357,0.00010829702,0.0000768442],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015702982,0.000024496643,0.9297219,0.000031070103,0.000035261815,0.0009169879,0.00024015084,0.00019500323,0.065460324,0.000031948886,0.00014682561,0.0030389803],"study_design_scores_gemma":[0.000001103344,0.000011393307,0.99820685,0.000002108543,0.000007620519,0.00008970363,0.00011288813,0.000092766306,0.0013373994,0.00001239139,0.00012478346,9.286747e-7],"about_ca_topic_score_codex":0.018069021,"about_ca_topic_score_gemma":0.04659879,"teacher_disagreement_score":0.018069021,"about_ca_system_score_codex":0.00038863125,"about_ca_system_score_gemma":0.0002152429,"threshold_uncertainty_score":0.035927713},"labels":[],"label_agreement":null},{"id":"W1602293203","doi":"10.1029/2007gl030285","title":"North Atlantic climate and deep‐ocean flow speed changes during the last 230 years","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"North Atlantic oscillation; Geology; Oceanography; North Atlantic Deep Water; Hydrography; Ridge; Climatology; Thermohaline circulation; Deep sea; Atlantic multidecadal oscillation; Gulf Stream; Range (aeronautics); Mid-Atlantic Ridge; Period (music); Paleontology","score_opus":0.023428278807660723,"score_gpt":0.2691870011689664,"score_spread":0.24575872236130566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1602293203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992335,0.000089305,0.000012312653,0.000027913004,0.0000032699947,4.8248205e-7,0.00042494215,0.000002550461,0.00020575273],"genre_scores_gemma":[0.99886453,0.00010874599,0.000029872428,0.0000149687185,0.000006454484,0.0000014201775,0.0007896236,0.0000012631801,0.00018318495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999397,0.0000062971662,0.000005102213,0.000018726878,0.000011416134,0.000018670347],"domain_scores_gemma":[0.99974006,0.000027000173,0.00012216916,0.000018663522,0.000041836796,0.000050284125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019068658,0.00009347944,0.00012735378,0.0003379461,0.00017410351,0.00034451656,0.00009937611,0.00017963327,0.00077728013],"category_scores_gemma":[0.00052054453,0.00009371524,0.00016171734,0.00038057216,0.00017259362,0.00022225334,0.00023762282,0.00019721568,0.00016856466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008261963,0.000015239895,0.994335,0.000009741569,0.00007088781,0.00005834855,0.0001304116,0.0002598826,0.0008485382,0.00004583334,0.00025520232,0.0038882326],"study_design_scores_gemma":[0.0000011282887,0.0000070466754,0.9996458,9.467893e-7,0.000005941058,0.000018538534,0.000029891202,0.00006566023,0.000028937086,0.000006668948,0.00018844605,0.000001003603],"about_ca_topic_score_codex":0.0301718,"about_ca_topic_score_gemma":0.073009126,"teacher_disagreement_score":0.0301718,"about_ca_system_score_codex":0.0004012796,"about_ca_system_score_gemma":0.00021150507,"threshold_uncertainty_score":0.059992373},"labels":[],"label_agreement":null},{"id":"W1603372043","doi":"10.1002/2015gl064363","title":"Low‐frequency earthquakes at the southern Cascadia margin","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; University of British Columbia","funders":"","keywords":"Geology; Seismology; San andreas fault; Episodic tremor and slip; Slip (aerodynamics); Fault (geology); Subduction; Tectonics","score_opus":0.05600191853403335,"score_gpt":0.2834310451376872,"score_spread":0.22742912660365383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1603372043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919134,0.000017146702,0.000044269294,0.000019520823,9.675842e-7,0.0000022532672,0.00026040676,0.000015916394,0.0004482354],"genre_scores_gemma":[0.9994004,0.000010861829,0.00006402483,0.0000021968053,0.0000012373812,0.0000021893472,0.00037416458,0.0000018913316,0.00014309426],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985945,0.000021479887,0.000008749981,0.00004957022,0.000037120433,0.000023718296],"domain_scores_gemma":[0.99944276,0.00007695214,0.00015488056,0.000065015374,0.00010888129,0.00015146412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024604207,0.00021379498,0.00016706024,0.0009907405,0.00046934944,0.00048409335,0.00022170009,0.00018776002,0.001077881],"category_scores_gemma":[0.0012823843,0.000113694856,0.00012680993,0.00071840966,0.00020720156,0.00013978129,0.0003559347,0.00014290745,0.00015729415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014655356,0.000035378944,0.9829914,0.000020067471,0.000042996733,0.00020010227,0.00035295502,0.0027495036,0.005918426,0.000060251667,0.00032774967,0.007154582],"study_design_scores_gemma":[0.0000054028637,0.000010850186,0.99855775,0.000002567448,0.00000700683,0.000014498302,0.00010152754,0.0010002736,0.00013485883,0.000015263598,0.00014727804,0.0000027303977],"about_ca_topic_score_codex":0.10073173,"about_ca_topic_score_gemma":0.18486105,"teacher_disagreement_score":0.10073173,"about_ca_system_score_codex":0.00084482593,"about_ca_system_score_gemma":0.00041058232,"threshold_uncertainty_score":0.2002908},"labels":[],"label_agreement":null},{"id":"W1604308019","doi":"10.1029/2002gl014989","title":"A marine source of methyl nitrate","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Seawater; Nitrate; Water column; Atmosphere (unit); Nitrite; Nitrogen; Oceanography; Environmental science; New production; Environmental chemistry; Atmospheric sciences; Phytoplankton; Chemistry; Geology; Meteorology; Nutrient; Physics","score_opus":0.03988300653202145,"score_gpt":0.2586316012907019,"score_spread":0.21874859475868044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1604308019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93736553,0.0059853545,0.0047385367,0.00087304384,0.00023519021,0.000044569224,0.0015373786,0.00017318569,0.049047206],"genre_scores_gemma":[0.9884753,0.0020274564,0.0024188594,0.00012548303,0.000041815492,0.000008925339,0.00045208348,0.000014206747,0.006435794],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.0000046000905,0.000002971824,0.000019400472,0.000020334855,0.000018443865],"domain_scores_gemma":[0.999915,0.000008263856,0.000013887123,0.000009421748,0.000028805263,0.000024464598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000670157,0.0004196683,0.00019277669,0.00031299575,0.000450672,0.00029242338,0.00027268214,0.0003617254,0.0027743105],"category_scores_gemma":[0.00016311018,0.00013837634,0.0001855264,0.00024342703,0.00013344876,0.00016861867,0.000777263,0.0002533493,0.0007181499],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023466109,0.000020722428,0.041616764,0.00040370395,0.000033217326,0.0019834086,0.00017633139,0.00033644226,0.9182891,0.0013204961,0.0007712853,0.034813844],"study_design_scores_gemma":[0.000060191403,0.0009045746,0.3191181,0.000344093,0.00021346626,0.003682323,0.0013971751,0.0034561048,0.56969994,0.0028254725,0.098233916,0.00006460447],"about_ca_topic_score_codex":0.00595314,"about_ca_topic_score_gemma":0.00754351,"teacher_disagreement_score":0.00595314,"about_ca_system_score_codex":0.00041330804,"about_ca_system_score_gemma":0.00034416086,"threshold_uncertainty_score":0.011836946},"labels":[],"label_agreement":null},{"id":"W1605490487","doi":"10.1029/2012gl051103","title":"Biological response to the 1997–98 and 2009–10 El Niño events in the equatorial Pacific Ocean","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Jet Propulsion Laboratory; National Oceanic and Atmospheric Administration; Canada Excellence Research Chairs, Government of Canada; Lamont-Doherty Earth Observatory, Columbia University; California Institute of Technology; National Aeronautics and Space Administration","keywords":"Advection; Pacific ocean; Oceanography; Pacific decadal oscillation; Environmental science; Climatology; Phytoplankton; Chlorophyll a; North Pacific High; Geology; Atmospheric sciences; Biology; Nutrient","score_opus":0.044867690601633696,"score_gpt":0.29131928484727393,"score_spread":0.24645159424564023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1605490487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936014,0.000050049526,0.000012327103,0.00006497801,0.0000072558582,0.000002512134,0.0001286944,0.000001503349,0.0003724908],"genre_scores_gemma":[0.99912196,0.00013427097,0.00002300383,0.0000769855,0.000011216797,0.00001057991,0.0004558659,0.0000011921394,0.00016479238],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998808,0.000018868177,0.000010882616,0.00002813083,0.00002467191,0.000036674963],"domain_scores_gemma":[0.9995419,0.000071165436,0.00019459602,0.000025522813,0.000074295924,0.00009248535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003716812,0.00021654158,0.00016159772,0.00033610564,0.0002899294,0.00043463282,0.00022416511,0.00038063765,0.00067619525],"category_scores_gemma":[0.00093493675,0.00012895644,0.00021816134,0.00035065328,0.0003582653,0.00030019018,0.00061336113,0.00041076358,0.00008006113],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078300445,0.00027633327,0.96199536,0.000077816236,0.00024991122,0.00023790839,0.0005099713,0.0019495223,0.024889212,0.0001740857,0.00049459946,0.008362284],"study_design_scores_gemma":[0.0000045171555,0.000033614964,0.99933916,0.000002943746,0.000007866671,0.000009616247,0.00014043806,0.00014276887,0.00019924215,0.000015577256,0.000102219696,0.0000020833195],"about_ca_topic_score_codex":0.021204522,"about_ca_topic_score_gemma":0.021564577,"teacher_disagreement_score":0.021204522,"about_ca_system_score_codex":0.0007848866,"about_ca_system_score_gemma":0.0003803045,"threshold_uncertainty_score":0.04216224},"labels":[],"label_agreement":null},{"id":"W1607112949","doi":"10.1002/2014gl061253","title":"A ULF wave driver of ring current energization","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Ring current; Physics; Van Allen radiation belt; Current (fluid); Ion; Van Allen Probes; Diffusion; Ring (chemistry); Electron; Resonance (particle physics); Atomic physics; Computational physics; Magnetosphere; Plasma; Nuclear physics; Chemistry; Quantum mechanics","score_opus":0.01895577061986191,"score_gpt":0.2856453401645749,"score_spread":0.26668956954471296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607112949","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9502224,0.00033397684,0.040552557,0.00033930282,0.000047234593,0.000018278137,0.00019015276,0.00024309382,0.008052969],"genre_scores_gemma":[0.99859244,0.000053344054,0.0006307013,0.00001116031,0.000011353976,0.0000023984421,0.00003290032,0.000012189138,0.000653581],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999517,0.0000067204764,0.0000020632165,0.000015447835,0.000008009172,0.000016054706],"domain_scores_gemma":[0.9998053,0.000050082992,0.000052148247,0.000028424201,0.000038097496,0.000025932017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015564139,0.0002081832,0.00016136369,0.00031044826,0.00016726027,0.0005699521,0.00029431356,0.00030212768,0.0016360912],"category_scores_gemma":[0.0008566701,0.00013711712,0.00018950245,0.00017435022,0.00025372254,0.0006133772,0.00036702753,0.0002790103,0.000244425],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005996937,0.00014433224,0.16116253,0.00025079714,0.00016467123,0.001492799,0.00064511615,0.23165113,0.4694796,0.06729021,0.003010052,0.06410909],"study_design_scores_gemma":[0.0000211459,0.00010578992,0.08150455,0.000015382635,0.00004197667,0.000405883,0.00017611663,0.8843085,0.02125804,0.009841305,0.0022801284,0.000041196858],"about_ca_topic_score_codex":0.0018427918,"about_ca_topic_score_gemma":0.00068919006,"teacher_disagreement_score":0.0018427918,"about_ca_system_score_codex":0.00036341973,"about_ca_system_score_gemma":0.00015327742,"threshold_uncertainty_score":0.005473256},"labels":[],"label_agreement":null},{"id":"W1607153631","doi":"10.1002/grl.50257","title":"Broadband array observations of the 300 km seismic discontinuity","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Center for High Performance Computing","keywords":"Geology; Seismic array; Discontinuity (linguistics); Classification of discontinuities; Mantle (geology); Seismology; Subduction; Eclogite; Basalt; Seismic wave; Stishovite; Geophysics; Transition zone; Crust; Petrology; Tectonics; Quartz; Paleontology","score_opus":0.03768964053772479,"score_gpt":0.2654500818033348,"score_spread":0.22776044126561001,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607153631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99352705,0.000042503292,0.0027870063,0.000033090044,0.0000039650595,0.0000033239505,0.00071477535,0.00009237974,0.0027960779],"genre_scores_gemma":[0.9973839,0.000021590678,0.0017134647,0.000010051999,0.000003844756,0.000004167151,0.00053553435,0.0000047661856,0.00032281043],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999695,0.0000030313456,0.0000011655945,0.0000122623005,0.000007661603,0.0000063512434],"domain_scores_gemma":[0.9999063,0.000023820123,0.000020962048,0.00000968253,0.00001819513,0.000020967407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000062854546,0.00005907922,0.00008264929,0.00030632105,0.00008452289,0.00014779829,0.000093168055,0.00018050791,0.0014073411],"category_scores_gemma":[0.0002735127,0.000086972665,0.0000551115,0.00028367422,0.000064685155,0.00013807742,0.0001474603,0.00017458445,0.0002914134],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003479725,0.00013522405,0.21925071,0.00007106811,0.00006448955,0.00019844696,0.00026908907,0.009922707,0.6976862,0.001310567,0.0020355375,0.06870798],"study_design_scores_gemma":[0.000026603362,0.00010929661,0.95608735,0.000012290898,0.000035784095,0.00017584278,0.000116925505,0.025607042,0.0151388915,0.00043141327,0.0022392797,0.000019391957],"about_ca_topic_score_codex":0.0019786723,"about_ca_topic_score_gemma":0.0038460135,"teacher_disagreement_score":0.0019786723,"about_ca_system_score_codex":0.0001225974,"about_ca_system_score_gemma":0.00006904206,"threshold_uncertainty_score":0.0047080517},"labels":[],"label_agreement":null},{"id":"W1607405879","doi":"10.1029/2010gl045473","title":"Transport driven by eddy momentum fluxes in the Gulf Stream Extension region","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Gulf Stream; Ocean gyre; Oceanography; Geology; Ocean current; Momentum (technical analysis); Climatology; Eddy; Environmental science; Meteorology; Geography; Subtropics; Turbulence","score_opus":0.019242897177001603,"score_gpt":0.25851116247127753,"score_spread":0.23926826529427592,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607405879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988708,0.000048093632,0.00026327829,0.00006333629,0.0000063825823,0.00000247216,0.00011024081,0.000021659356,0.000613668],"genre_scores_gemma":[0.99921286,0.00008568027,0.00020983131,0.000010632977,0.0000029754945,0.0000029058604,0.00013994986,0.000007540363,0.00032769202],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995804,0.000011349581,0.0000034781503,0.000010603113,0.000004587907,0.000012064813],"domain_scores_gemma":[0.999866,0.00003395344,0.000035173176,0.000011782809,0.000029635345,0.00002343354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017276665,0.00034877594,0.0002379509,0.00023494691,0.0003277683,0.00077300397,0.0002865736,0.00046081012,0.00059491245],"category_scores_gemma":[0.0005109975,0.0003080607,0.0004244486,0.0003024839,0.00026626783,0.00041441843,0.00040692207,0.0002839475,0.000082195234],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020910458,0.00009712783,0.19704673,0.00003297691,0.00011673448,0.0004389171,0.00013584277,0.7820222,0.012962648,0.0019566256,0.0006578958,0.0043231845],"study_design_scores_gemma":[0.00008543906,0.000059920087,0.0952648,0.000016071079,0.000051361672,0.000052478183,0.00009427022,0.90144455,0.0015086725,0.00073844136,0.000654219,0.000029688179],"about_ca_topic_score_codex":0.12843639,"about_ca_topic_score_gemma":0.05843453,"teacher_disagreement_score":0.12843639,"about_ca_system_score_codex":0.0013635241,"about_ca_system_score_gemma":0.0010801813,"threshold_uncertainty_score":0.2553776},"labels":[],"label_agreement":null},{"id":"W1607987656","doi":"10.1029/2011gl046728","title":"Observation of the 2009 Samoa tsunami by the NEPTUNE-Canada cabled observatory: Test data for an operational regional tsunami forecast model","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Fisheries and Oceans Canada","funders":"","keywords":"Geology; Observatory; Tide gauge; Oceanography; Seismology; Neptune; Seafloor spreading; Meteorology; Climatology; Sea level; Geography","score_opus":0.22859173342666525,"score_gpt":0.2978615471840376,"score_spread":0.06926981375737237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1607987656","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953851,0.000033191536,0.0012172716,0.00006948071,0.000010357174,0.000032190754,0.002272437,0.00014195169,0.000838],"genre_scores_gemma":[0.9945703,0.00003107033,0.0023041503,0.000009383335,0.000004620364,0.000014679089,0.0028476615,0.0000148087165,0.0002033095],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988425,0.000015062441,0.0000061330807,0.000035081095,0.000035468292,0.000023961265],"domain_scores_gemma":[0.9996213,0.000052193373,0.00003942965,0.000051565286,0.00015399558,0.00008149477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030894275,0.00043822854,0.00015442831,0.00026362008,0.00044966102,0.000471284,0.0008891014,0.00024486703,0.0006120481],"category_scores_gemma":[0.0009878083,0.00019386293,0.00022090378,0.00046182898,0.00031409282,0.00032250906,0.0003059807,0.00031658928,0.00012918156],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006726337,0.0002770858,0.4135109,0.000046798108,0.00013042564,0.00026267767,0.00026738047,0.54799753,0.007536453,0.0005884385,0.004310048,0.024399592],"study_design_scores_gemma":[0.0001307894,0.00009420793,0.13530731,0.000011226365,0.00004299543,0.000034267865,0.00014158114,0.8603284,0.0028202243,0.000099342025,0.0009572481,0.00003246292],"about_ca_topic_score_codex":0.7417264,"about_ca_topic_score_gemma":0.6452903,"teacher_disagreement_score":0.2582736,"about_ca_system_score_codex":0.0036291853,"about_ca_system_score_gemma":0.0029200383,"threshold_uncertainty_score":0.5195892},"labels":[],"label_agreement":null},{"id":"W1608879395","doi":"10.1029/2011gl047439","title":"Aqueous OH oxidation of ambient organic aerosol and cloud water organics: Formation of highly oxidized products","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":146,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Glyoxal; Aqueous solution; Aerosol; Chemistry; Environmental chemistry; Mass spectrometry; Organic chemistry; Chromatography","score_opus":0.03008538520637435,"score_gpt":0.23421051668855694,"score_spread":0.2041251314821826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1608879395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97999567,0.004023142,0.012689991,0.00005788169,0.000059083788,0.000053741995,0.00051724986,0.000057024652,0.0025461752],"genre_scores_gemma":[0.99257034,0.0013557784,0.0043387557,0.00005014161,0.000047589896,0.000012837801,0.00039257697,0.00000944726,0.0012225793],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998658,0.00000997134,0.0000057882758,0.0000457489,0.000052753418,0.000019851115],"domain_scores_gemma":[0.9999167,0.000014458978,0.000029813425,0.000005825398,0.000022921857,0.000010305023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015361496,0.0005017775,0.00015306973,0.00028251257,0.00014593979,0.00029229294,0.0002016705,0.0002730544,0.00089205406],"category_scores_gemma":[0.00017376187,0.00009868552,0.00012327085,0.00015950395,0.00019035669,0.00033073427,0.00025677326,0.00020135748,0.00018735671],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059846236,0.000016798263,0.0029609373,0.00007825194,0.000012466408,0.000085046,0.000018024073,0.000113363036,0.99209315,0.00012936641,0.00006328055,0.0043694265],"study_design_scores_gemma":[0.000006778065,0.00021143735,0.012861704,0.000005843999,0.000019704396,0.00025888457,0.00004208462,0.0015255316,0.9823997,0.0002030081,0.0024599356,0.0000054303227],"about_ca_topic_score_codex":0.0007721614,"about_ca_topic_score_gemma":0.00097339816,"teacher_disagreement_score":0.00089205406,"about_ca_system_score_codex":0.00019727623,"about_ca_system_score_gemma":0.00010414409,"threshold_uncertainty_score":0.0029841661},"labels":[],"label_agreement":null},{"id":"W1609047602","doi":"10.1029/2003gl017144","title":"Ground surface temperatures in Canada: Spatial and temporal variability","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Homogeneous; Spatial variability; Climatology; Geology; Environmental science; Atmospheric sciences; Physics","score_opus":0.04313467718384508,"score_gpt":0.27495848562701436,"score_spread":0.23182380844316927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1609047602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99299026,0.0005691733,0.00023565537,0.00016855124,0.000006144949,0.0000056424137,0.004641689,0.000029103925,0.0013537662],"genre_scores_gemma":[0.99596006,0.0002838327,0.00017789446,0.000026384972,0.0000029437413,0.000003821842,0.00300075,0.0000061845353,0.00053804996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975353,0.000012736185,0.000011153942,0.000056711415,0.0000943701,0.00007146408],"domain_scores_gemma":[0.9988501,0.00009151271,0.00016295898,0.000043889853,0.00074250344,0.00010898643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025213696,0.0001651481,0.00019254998,0.0012402222,0.0007377839,0.00077485293,0.00046257203,0.0002114097,0.00076240103],"category_scores_gemma":[0.001060503,0.00013693342,0.00017657921,0.0030555935,0.00040568804,0.00019896275,0.00040206837,0.00028282896,0.00014110733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006912256,0.000011919532,0.9804185,0.000023641942,0.0000732731,0.0000563067,0.00052992825,0.0010494171,0.00085512345,0.00013569325,0.0012575999,0.015519463],"study_design_scores_gemma":[0.0000015224412,0.0000027889034,0.9978181,0.0000065649615,0.000008847627,0.000022024129,0.00023879473,0.00072979607,0.00010011846,0.000022018416,0.0010440968,0.000005186066],"about_ca_topic_score_codex":0.98454475,"about_ca_topic_score_gemma":0.98972064,"teacher_disagreement_score":0.015455246,"about_ca_system_score_codex":0.008611126,"about_ca_system_score_gemma":0.0057740784,"threshold_uncertainty_score":0.062478423},"labels":[],"label_agreement":null},{"id":"W1609952363","doi":"10.1029/2012gl052647","title":"Statistical adjustment of decadal predictions in a changing climate","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Initialization; Climatology; Forcing (mathematics); Environmental science; Residual; Climate model; Climate change; Climate system; General Circulation Model; Econometrics; Meteorology; Computer science; Geology; Mathematics; Geography","score_opus":0.046523274976322866,"score_gpt":0.33715590256680184,"score_spread":0.290632627590479,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1609952363","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45845732,0.0001837313,0.53302336,0.00029725197,0.0002196425,0.00006211133,0.00100995,0.0026330145,0.0041136947],"genre_scores_gemma":[0.9167584,0.000105735606,0.07979141,0.00005381157,0.000044822453,0.000063376334,0.0014878311,0.00037651823,0.0013181051],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994419,0.00015385756,0.000040216986,0.00018905467,0.00013982451,0.000034959656],"domain_scores_gemma":[0.99786514,0.000713313,0.000347636,0.00047930007,0.0005510999,0.000043524862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019069376,0.00023416373,0.0001698133,0.0005529931,0.00023042496,0.0005726173,0.00033245562,0.00014604711,0.0009127493],"category_scores_gemma":[0.009220136,0.00022465487,0.00027240202,0.00085101847,0.00018826338,0.00046037958,0.00048464673,0.00066614593,0.0002814866],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029901712,0.00008304522,0.12069146,0.00006541715,0.00038339672,0.00011140395,0.00029695395,0.4619885,0.014277395,0.0111443,0.0049138144,0.3857453],"study_design_scores_gemma":[0.000013948917,0.00006670573,0.08117874,0.000009854647,0.000039251845,0.00003791434,0.00007806295,0.89913523,0.0074680024,0.0061415583,0.0057932455,0.000037418667],"about_ca_topic_score_codex":0.004863859,"about_ca_topic_score_gemma":0.0069267973,"teacher_disagreement_score":0.004863859,"about_ca_system_score_codex":0.00040869034,"about_ca_system_score_gemma":0.0007587073,"threshold_uncertainty_score":0.010084927},"labels":[],"label_agreement":null},{"id":"W1610202149","doi":"10.1029/2005gl023317","title":"Initial uptake of ozone on Saharan dust at atmospheric relative humidities","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Atmospheric sciences; Environmental science; Ozone; Atmospheric dust; Relative humidity; Mineral dust; Meteorology; Aerosol; Geology; Physics","score_opus":0.042268907496383006,"score_gpt":0.2930505170991742,"score_spread":0.25078160960279117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1610202149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983315,0.00047963267,0.00045940015,0.000008226185,0.0000037064426,0.000005357385,0.00012865881,0.000014322429,0.00056922383],"genre_scores_gemma":[0.9986172,0.00031403446,0.00029994288,0.0000101368,0.0000052099067,0.000008112271,0.00029341134,0.000009117549,0.00044286344],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99986076,0.000016789965,0.0000059215686,0.000035334506,0.00003551586,0.00004559153],"domain_scores_gemma":[0.9998672,0.000050484992,0.000014841372,0.000010937112,0.00003723471,0.000019307921],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015412673,0.00035901836,0.00038278877,0.00029752016,0.00023459927,0.00032659422,0.00023028243,0.00022037154,0.001146858],"category_scores_gemma":[0.00026586402,0.00017705296,0.0002971174,0.00019462041,0.00016550989,0.00022956995,0.00024770547,0.00032001716,0.0002366057],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032046225,0.000015898617,0.0039207563,0.00008437031,0.00003441573,0.00007930507,0.00010979873,0.00037976273,0.9928899,0.000044053835,0.00002512998,0.0020962222],"study_design_scores_gemma":[0.000017657978,0.0004996959,0.06564332,0.000008996169,0.00005195886,0.00008965802,0.00019656871,0.0022662648,0.93029773,0.000056989455,0.00085714844,0.000014000324],"about_ca_topic_score_codex":0.00399756,"about_ca_topic_score_gemma":0.0026681938,"teacher_disagreement_score":0.00399756,"about_ca_system_score_codex":0.00033908384,"about_ca_system_score_gemma":0.000112683,"threshold_uncertainty_score":0.007948577},"labels":[],"label_agreement":null},{"id":"W1611003009","doi":"10.1029/2012gl051790","title":"Post‐fire changes in net shortwave radiation along a latitudinal gradient in boreal North America","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Albedo (alchemy); Shortwave radiation; Boreal; Environmental science; Taiga; Shortwave; Climatology; Fire regime; Vegetation (pathology); Atmospheric sciences; Ecosystem; Geography; Geology; Ecology; Radiation; Radiative transfer; Forestry","score_opus":0.018179723006258048,"score_gpt":0.27380704798585315,"score_spread":0.2556273249795951,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1611003009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994117,0.00007970032,0.000044321136,0.000016862143,0.0000031896154,0.0000028787701,0.00017240588,0.00000538632,0.00026357718],"genre_scores_gemma":[0.9995109,0.000058028414,0.00008812494,0.000014122411,0.0000029743928,0.0000039602687,0.0002249815,0.0000014052582,0.00009548509],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998555,0.000017985085,0.000010701872,0.000051317675,0.000030313427,0.000034207213],"domain_scores_gemma":[0.99947745,0.000058144964,0.00016238287,0.000025126938,0.00015268837,0.00012412481],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032400773,0.00021436326,0.0001907997,0.0006046376,0.00041774724,0.00043841402,0.00022160013,0.00015989851,0.00043990038],"category_scores_gemma":[0.0004233295,0.00013098982,0.00022686289,0.0005700733,0.00028912723,0.00023260056,0.00019212416,0.00015518392,0.000057124744],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007008498,0.000024998717,0.99402267,0.000009506177,0.000040969262,0.00003187113,0.00019739993,0.00024334852,0.0033433584,0.000021588196,0.00013240006,0.0018617716],"study_design_scores_gemma":[0.0000010051233,0.000004426121,0.99977475,6.941508e-7,0.0000026110329,0.000007977746,0.000060677106,0.0000736562,0.00002351593,0.0000025947763,0.00004702803,0.0000010247561],"about_ca_topic_score_codex":0.35100836,"about_ca_topic_score_gemma":0.55680466,"teacher_disagreement_score":0.64899164,"about_ca_system_score_codex":0.001064882,"about_ca_system_score_gemma":0.00071143,"threshold_uncertainty_score":0.6979305},"labels":[],"label_agreement":null},{"id":"W1611826328","doi":"10.1029/2012gl052905","title":"Predicting vegetation‐stabilized dune field morphology","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Lethbridge","funders":"Ministry of Economy, Trade and Industry; Western Canada Research Grid; Compute Canada; Alberta Innovates; Cenovus Energy; National Aeronautics and Space Administration","keywords":"Deposition (geology); Vegetation (pathology); Geology; Aeolian processes; Sedimentary depositional environment; Sand dune stabilization; Flux (metallurgy); Morphology (biology); Geomorphology; Erosion; Transverse plane; Hydrology (agriculture); Atmospheric sciences; Paleontology; Sediment; Materials science; Geotechnical engineering","score_opus":0.03134333994447041,"score_gpt":0.30256105536407696,"score_spread":0.27121771541960654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1611826328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998439,0.000013857594,0.0011219552,0.000019851166,0.0000019265628,0.0000038425555,0.00009524236,0.00003152592,0.00027280717],"genre_scores_gemma":[0.9992323,0.0000083443465,0.0005992052,0.0000024589815,9.5131304e-7,0.00000228219,0.00008532926,0.0000030302724,0.00006606827],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000013301958,0.000002937946,0.000020460984,0.000006481515,0.000018960387],"domain_scores_gemma":[0.99956363,0.00019422166,0.00006042658,0.000038359245,0.000062406354,0.00008093051],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017973642,0.00025757507,0.0002520317,0.00046473194,0.00019441232,0.0007363079,0.00034122088,0.0006884066,0.00068423623],"category_scores_gemma":[0.001563534,0.00031792588,0.00026268023,0.0003019546,0.00022358088,0.00042989803,0.00025083858,0.00017655245,0.00009258397],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005937787,0.000057992933,0.098749764,0.000013824538,0.000036838723,0.00008611602,0.000035033485,0.894035,0.00269444,0.0001990613,0.00017342973,0.0038591318],"study_design_scores_gemma":[0.000009118846,0.000008954828,0.014798294,0.0000010891282,0.000003265399,0.0000074479813,0.000015474136,0.9848497,0.00019196603,0.00007369368,0.000037543905,0.000003545],"about_ca_topic_score_codex":0.032805253,"about_ca_topic_score_gemma":0.023756875,"teacher_disagreement_score":0.032805253,"about_ca_system_score_codex":0.00071896403,"about_ca_system_score_gemma":0.00046876128,"threshold_uncertainty_score":0.06522864},"labels":[],"label_agreement":null},{"id":"W1612553446","doi":"10.1029/2007gl030822","title":"Automatic detection and characterization of seismic tremors in northern Cascadia","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Seismology; Waveform; Seismogram; Geology; Event (particle physics); Notice; Chart; Algorithm; Computer science; Telecommunications; Law; Statistics","score_opus":0.02141531044344082,"score_gpt":0.26229063598191094,"score_spread":0.24087532553847013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1612553446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5959849,0.00022743377,0.38233444,0.00022126178,0.000023684943,0.00013745723,0.0014269844,0.013927548,0.0057163406],"genre_scores_gemma":[0.8616818,0.0001050099,0.1324921,0.000030019351,0.000018744739,0.000072190356,0.002910566,0.0002113847,0.0024782126],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99963343,0.00003988328,0.00003106279,0.00014080065,0.00011320471,0.00004160932],"domain_scores_gemma":[0.99901235,0.00019270259,0.0001654626,0.00012831559,0.0004173446,0.00008391692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041924906,0.0005755062,0.00040086076,0.0027970728,0.000399404,0.00072784885,0.0006132252,0.0003200907,0.0012024111],"category_scores_gemma":[0.0018889684,0.00021681677,0.00019359803,0.0009526777,0.0003107355,0.0003764821,0.0005134441,0.00024211487,0.00052602735],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038399076,0.000114586,0.11523961,0.00016617082,0.000078197736,0.00034542626,0.00047405876,0.048227835,0.08112244,0.0012941922,0.0058642915,0.74668926],"study_design_scores_gemma":[0.000093573166,0.00016608107,0.2599201,0.000020915388,0.00006682872,0.00044019928,0.0003335344,0.6807354,0.04812407,0.0023155243,0.0077072447,0.00007650698],"about_ca_topic_score_codex":0.018288102,"about_ca_topic_score_gemma":0.024344053,"teacher_disagreement_score":0.018288102,"about_ca_system_score_codex":0.0005383352,"about_ca_system_score_gemma":0.0009792281,"threshold_uncertainty_score":0.036363304},"labels":[],"label_agreement":null},{"id":"W1612660228","doi":"10.1029/2003gl016977","title":"Viscous magnetization, archaeology and Bayesian statistics of small samples from Israel and England","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; York University","keywords":"Geology; Power law; Pelagic zone; Exponent; Bayesian probability; Statistics; Archaeology; Paleontology; Mathematics; Geography; Oceanography","score_opus":0.019793697065316772,"score_gpt":0.267291458150372,"score_spread":0.2474977610850552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1612660228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998862,0.00006112882,0.0005229314,0.000009845803,7.345581e-7,0.000005509769,0.000117128104,0.0000036436734,0.00041712605],"genre_scores_gemma":[0.9988772,0.000028982391,0.00040664285,0.000005888315,0.0000024940045,0.000010650674,0.0003908379,0.0000036027072,0.00027367022],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990621,0.0004158302,0.00008705234,0.00025249872,0.000108866196,0.00007369628],"domain_scores_gemma":[0.9950375,0.0030391554,0.0006337621,0.00052440807,0.00057339104,0.00019169551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001942097,0.00014095914,0.00032411094,0.0018725556,0.00043960233,0.00072928995,0.0005139244,0.0003163256,0.00092864764],"category_scores_gemma":[0.009255298,0.0002257835,0.00016946456,0.0010051869,0.0010480384,0.0002760226,0.00073244964,0.00019019104,0.0001929087],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033881798,0.00004120407,0.9672664,0.00004399162,0.00015439941,0.000377333,0.0059376797,0.0029026123,0.0038928203,0.0012566759,0.00027818626,0.017509937],"study_design_scores_gemma":[0.00001712181,0.000067488676,0.9916374,0.00001480718,0.000028341548,0.00029856336,0.0016396286,0.003988923,0.0006269253,0.0005128208,0.0011495166,0.000018532399],"about_ca_topic_score_codex":0.027852802,"about_ca_topic_score_gemma":0.039194964,"teacher_disagreement_score":0.027852802,"about_ca_system_score_codex":0.00069216394,"about_ca_system_score_gemma":0.0002219592,"threshold_uncertainty_score":0.055381358},"labels":[],"label_agreement":null},{"id":"W1612991129","doi":"10.1002/2013gl058187","title":"Realistic initiation and dynamics of the Madden‐Julian Oscillation in a coarse resolution aquaplanet GCM","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"New York University Abu Dhabi; University of Victoria","keywords":"Madden–Julian oscillation; Climatology; Rossby wave; Ocean gyre; Convection; Geology; GCM transcription factors; Equator; Environmental science; Meteorology; Physics; Climate change; General Circulation Model; Oceanography; Geodesy","score_opus":0.034048864284916665,"score_gpt":0.28510011066662716,"score_spread":0.2510512463817105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1612991129","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933931,0.000043198514,0.0028541954,0.0001928227,0.000017944698,0.000022442084,0.0007119457,0.00020222375,0.002562071],"genre_scores_gemma":[0.99616843,0.000027400454,0.0029243464,0.000031558488,0.0000055086684,0.000023192293,0.00035887648,0.000024180192,0.00043652838],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991465,0.000018871697,0.0000053785457,0.000028263174,0.000013237034,0.000019579848],"domain_scores_gemma":[0.9998054,0.000072255,0.000028143304,0.000034130684,0.000026039896,0.00003416504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018281021,0.00036891093,0.00043113148,0.00024764927,0.0005184917,0.0007607826,0.0011352639,0.00093837385,0.0017686952],"category_scores_gemma":[0.0007887997,0.0003399693,0.0004311376,0.00041269464,0.00065164105,0.00054461724,0.0004283748,0.00073995156,0.00012630718],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076073426,0.000048703383,0.0048855552,0.000011559862,0.000027068403,0.0000869769,0.00003917052,0.9911265,0.0015466535,0.0011612048,0.00027784312,0.0007127777],"study_design_scores_gemma":[0.00004664213,0.000014150872,0.0021558711,0.0000020842501,0.000009374792,0.000007445332,0.000018570447,0.9968683,0.0003490735,0.00033776253,0.00018235378,0.000008377815],"about_ca_topic_score_codex":0.08162593,"about_ca_topic_score_gemma":0.028112775,"teacher_disagreement_score":0.08162593,"about_ca_system_score_codex":0.0016251814,"about_ca_system_score_gemma":0.0011066594,"threshold_uncertainty_score":0.16230166},"labels":[],"label_agreement":null},{"id":"W1613961603","doi":"10.1029/2009gl042045","title":"Northern Rocky Mountain streamflow records: Global warming trends, human impacts or natural variability?","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Regina","funders":"","keywords":"Streamflow; Climatology; Environmental science; Pacific decadal oscillation; Dryness; Proxy (statistics); Climate change; El Niño Southern Oscillation; Hydrology (agriculture); Geology; Geography; Drainage basin; Oceanography","score_opus":0.018289922857567725,"score_gpt":0.31429481511060575,"score_spread":0.29600489225303805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1613961603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939511,0.0012728347,0.0002527353,0.0010065871,0.000014492474,0.000005883196,0.00074977067,0.000027595017,0.0027190268],"genre_scores_gemma":[0.9983492,0.00041725117,0.00016707723,0.00011774492,0.000035995683,0.0000028075779,0.0005419351,0.000004687875,0.00036347128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985397,0.0000563268,0.000008785695,0.000029686638,0.000026070784,0.000025086352],"domain_scores_gemma":[0.9993678,0.00017181416,0.0002218848,0.00008206599,0.00010356814,0.000052980027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090845156,0.00010118955,0.00018324074,0.00036510345,0.00017602615,0.0006049728,0.00027709495,0.00018740103,0.0012026838],"category_scores_gemma":[0.0018595939,0.000069510366,0.00015355946,0.0010525921,0.00058259506,0.0005180926,0.0001426175,0.00015805266,0.0001228401],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039266743,0.000014668235,0.9849974,0.000036375208,0.00009868344,0.000055461976,0.0002818792,0.00046310195,0.00037848065,0.00031315535,0.00071675685,0.012604741],"study_design_scores_gemma":[0.0000015180145,0.0000063746143,0.99836713,0.0000080326945,0.00001486138,0.000016312308,0.000209173,0.00045070684,0.000053709315,0.00007167537,0.0007984506,0.000002013837],"about_ca_topic_score_codex":0.106524624,"about_ca_topic_score_gemma":0.19530025,"teacher_disagreement_score":0.89347535,"about_ca_system_score_codex":0.0006105527,"about_ca_system_score_gemma":0.0005730322,"threshold_uncertainty_score":0.21180916},"labels":[],"label_agreement":null},{"id":"W1615868986","doi":"10.1002/grl.50214","title":"Irreversible mass loss of Canadian Arctic Archipelago glaciers","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Seventh Framework Programme; Chinese Academy of Agricultural Sciences; National Collegiate Athletic Association","keywords":"Meltwater; Glacier; Glacier mass balance; Snow; Arctic; Glacier ice accumulation; Climatology; Tundra; Environmental science; Cryosphere; Geology; Archipelago; Atmospheric sciences; Physical geography; Ice stream; Sea ice; Geomorphology; Oceanography; Geography","score_opus":0.04008988299010842,"score_gpt":0.25587086410651466,"score_spread":0.21578098111640626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1615868986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99698097,0.00008427908,0.00024626774,0.00007661275,0.0000055602295,0.000005370688,0.0010911633,0.00004214684,0.00146751],"genre_scores_gemma":[0.99911696,0.000027339402,0.000067819754,0.000010648345,0.0000011766231,0.000002332586,0.0005131411,0.000004059139,0.00025637535],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998292,0.000013974273,0.000006535696,0.00004148037,0.000038873626,0.000069948044],"domain_scores_gemma":[0.9998171,0.000025150557,0.000022826081,0.00002835436,0.00007136026,0.000035180652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026709063,0.0004960203,0.0002513969,0.00048886356,0.0009971182,0.00088075397,0.00075830397,0.00034904372,0.0012675951],"category_scores_gemma":[0.0009016649,0.00017954629,0.00047624134,0.0006621529,0.000429117,0.00039436805,0.00041381738,0.00031595485,0.00009573517],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029148808,0.00009911361,0.38051835,0.00004937958,0.0003036983,0.00020978486,0.00013139036,0.5954737,0.0069669625,0.0016226798,0.0019000361,0.012433345],"study_design_scores_gemma":[0.00006576675,0.000071076494,0.51036453,0.000016078639,0.00011080113,0.000065523025,0.00024316995,0.480637,0.0044979667,0.0009511554,0.0029239955,0.000052845066],"about_ca_topic_score_codex":0.8538477,"about_ca_topic_score_gemma":0.784482,"teacher_disagreement_score":0.14615232,"about_ca_system_score_codex":0.0069279913,"about_ca_system_score_gemma":0.0037938827,"threshold_uncertainty_score":0.29402602},"labels":[],"label_agreement":null},{"id":"W1616547970","doi":"10.1029/2005gl023157","title":"Are some domes the ghosts of basins?","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Structural basin; Sedimentary basin; Crust; Back-stripping; Tectonic subsidence; Inversion (geology); Seismology; Sedimentary rock; Petrology; Extensional definition; Subsidence; Pull apart basin; Tectonics; Geomorphology; Geophysics; Sedimentary basin analysis; Paleontology","score_opus":0.04742984873729317,"score_gpt":0.300427536602767,"score_spread":0.25299768786547383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1616547970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87460756,0.003878298,0.015064141,0.014828238,0.00028500217,0.000054574597,0.000758606,0.0002720223,0.09025155],"genre_scores_gemma":[0.989833,0.000442087,0.0026960862,0.00067732844,0.00004851664,0.000010881138,0.000095434705,0.000042039053,0.0061547863],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.99969363,0.000092287395,0.00001436494,0.0000761049,0.000042565403,0.00008101502],"domain_scores_gemma":[0.9992059,0.00012046286,0.00011994562,0.00029822293,0.000104456325,0.00015108217],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005041956,0.00014321835,0.00029895292,0.0005152293,0.0016099524,0.0023068748,0.0003218241,0.0006979396,0.005284842],"category_scores_gemma":[0.0023077684,0.00028237147,0.00018822248,0.0005940167,0.0042547267,0.0036171768,0.0015249882,0.00049166894,0.0007514549],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059334026,0.000042179763,0.18747413,0.0003068441,0.00013749492,0.0022809952,0.03043667,0.0012886893,0.009900994,0.5917014,0.02081687,0.15502037],"study_design_scores_gemma":[0.000072607196,0.00009329459,0.23099898,0.0002240323,0.00008845152,0.0055211317,0.03641065,0.0027175716,0.0042917947,0.29692447,0.42256725,0.00008981333],"about_ca_topic_score_codex":0.0026737358,"about_ca_topic_score_gemma":0.006650468,"teacher_disagreement_score":0.005284842,"about_ca_system_score_codex":0.00049624685,"about_ca_system_score_gemma":0.00050592533,"threshold_uncertainty_score":0.017679572},"labels":[],"label_agreement":null},{"id":"W1617694494","doi":"10.1029/2005gl023410","title":"Defining climatological seasons using radially constrained clustering","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Contiguity; Cluster analysis; Boundary (topology); Cluster (spacecraft); Set (abstract data type); Data set; Climatology; Meteorology; Environmental science; Computer science; Mathematics; Statistics; Geology; Geography","score_opus":0.06690639911992695,"score_gpt":0.3379142127655082,"score_spread":0.27100781364558124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1617694494","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007754295,0.000099275225,0.9898634,0.000059817292,0.000024453724,0.000081279766,0.00043039274,0.0003750805,0.0013120538],"genre_scores_gemma":[0.10085077,0.00020864677,0.89460003,0.000068661706,0.000040435873,0.0003442245,0.0017027801,0.00030210704,0.0018823042],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99887294,0.00039174748,0.00008427362,0.00029699615,0.00023832945,0.00011563877],"domain_scores_gemma":[0.9981476,0.00049961323,0.00033247506,0.0002482462,0.0006844982,0.00008761802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018500305,0.0007025506,0.0005559259,0.0018102645,0.0009941856,0.0015693846,0.0015920822,0.0006406912,0.001880354],"category_scores_gemma":[0.0057704058,0.00046755595,0.00086267566,0.0026284957,0.00045183062,0.0011586624,0.0012354555,0.0011308651,0.0010198263],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021169687,0.00012978504,0.020590551,0.00027191412,0.00020186101,0.00024279756,0.0013529484,0.34341726,0.012610113,0.10890054,0.0188438,0.49322668],"study_design_scores_gemma":[0.000022775272,0.00003621557,0.009516056,0.00007092937,0.000026869273,0.00017134544,0.00036510333,0.9135942,0.0029546677,0.05097819,0.022129323,0.00013433074],"about_ca_topic_score_codex":0.027845843,"about_ca_topic_score_gemma":0.032044012,"teacher_disagreement_score":0.027845843,"about_ca_system_score_codex":0.000856178,"about_ca_system_score_gemma":0.0024766899,"threshold_uncertainty_score":0.05536747},"labels":[],"label_agreement":null},{"id":"W1617728669","doi":"10.1029/2012gl051537","title":"Northern Bering Sea tip jets","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Cape; Geology; Oceanography; Climatology; Range (aeronautics); Boreal; Geography; Paleontology","score_opus":0.03481641220210826,"score_gpt":0.28071185000345544,"score_spread":0.24589543780134718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1617728669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9839648,0.00055007765,0.00040824048,0.00007734459,0.00003841882,0.000007176954,0.0011713773,0.000059759746,0.013722621],"genre_scores_gemma":[0.994747,0.0003848436,0.00036714922,0.00003363281,0.00002386805,0.0000049686846,0.0013385501,0.000011166648,0.003088876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999262,0.0000052817895,0.000005507712,0.000026141208,0.000015413358,0.000021487263],"domain_scores_gemma":[0.9998447,0.00001455429,0.000050962655,0.000014465715,0.000047288304,0.00002798735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001176878,0.00028842903,0.0003296979,0.0004030283,0.0005476664,0.00068604527,0.00014431008,0.00017746742,0.0034413813],"category_scores_gemma":[0.0003695472,0.00008863472,0.000114404036,0.00049699575,0.00017338023,0.0002762506,0.00041725574,0.00023866615,0.000773908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050139416,0.00004820832,0.86054975,0.00024546965,0.00008399979,0.0029736976,0.0014109372,0.005277355,0.05223191,0.001038062,0.0060621966,0.06957697],"study_design_scores_gemma":[0.0000071866907,0.000031082334,0.99327093,0.000019997577,0.000012863756,0.00027705234,0.00022269064,0.0011970858,0.0011102129,0.00015609807,0.0036887683,0.00000602873],"about_ca_topic_score_codex":0.014505514,"about_ca_topic_score_gemma":0.01513743,"teacher_disagreement_score":0.014505514,"about_ca_system_score_codex":0.00041113418,"about_ca_system_score_gemma":0.00022014683,"threshold_uncertainty_score":0.028842151},"labels":[],"label_agreement":null},{"id":"W1617981396","doi":"10.1002/grl.50231","title":"Tropical American‐Atlantic forcing of austral summertime variability in the southern annular mode","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Extratropical cyclone; Forcing (mathematics); Climatology; Anomaly (physics); Environmental science; Eddy; Atmospheric circulation; Atmospheric sciences; Tropical Atlantic; Geology; Geography; Meteorology; Sea surface temperature; Physics","score_opus":0.03450583123444092,"score_gpt":0.3088690257547689,"score_spread":0.274363194520328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1617981396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99902725,0.000016304157,0.00006534052,0.000026958802,0.0000023601897,9.4988326e-7,0.0000875323,0.000008971586,0.00076425786],"genre_scores_gemma":[0.9998305,0.000020362455,0.0000368123,0.0000031977331,0.0000017619051,8.504041e-7,0.00003871577,9.1360596e-7,0.00006691885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997425,0.000006348422,0.0000019982256,0.0000047364188,0.0000053938147,0.0000072384905],"domain_scores_gemma":[0.9998535,0.00003207019,0.0000373938,0.000011005725,0.00002674199,0.00003931631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016509047,0.0001288371,0.000086889195,0.00014991943,0.00015913026,0.00024267366,0.00007815611,0.00006035726,0.0009643969],"category_scores_gemma":[0.00032667862,0.00007312133,0.00013558981,0.00015330898,0.000119093864,0.000095631156,0.00022076881,0.00010459892,0.00007215711],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008190638,0.00016365098,0.8174919,0.00009988027,0.00016600838,0.0004927542,0.0005049292,0.033179637,0.122206375,0.002293904,0.0015949226,0.02098707],"study_design_scores_gemma":[0.000036411588,0.000075155935,0.97673404,0.000007797936,0.00003283101,0.000060105256,0.00011677037,0.020242726,0.0014905804,0.0003164823,0.0008807614,0.0000064474457],"about_ca_topic_score_codex":0.022481367,"about_ca_topic_score_gemma":0.031317312,"teacher_disagreement_score":0.022481367,"about_ca_system_score_codex":0.00032514744,"about_ca_system_score_gemma":0.00026550886,"threshold_uncertainty_score":0.04470104},"labels":[],"label_agreement":null},{"id":"W1620475694","doi":"10.1029/2007gl030637","title":"Impact of a modified convective scheme on the Madden‐Julian Oscillation and El Niño–Southern Oscillation in a coupled climate model","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Madden–Julian oscillation; Climatology; Oscillation (cell signaling); Convection; GCM transcription factors; Southern oscillation; Climate model; El Niño Southern Oscillation; General Circulation Model; Atmosphere (unit); Forcing (mathematics); Environmental science; Atmospheric sciences; Meteorology; Geology; Physics; Climate change; Chemistry","score_opus":0.053950491820667405,"score_gpt":0.3442758944430507,"score_spread":0.29032540262238327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1620475694","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98444843,0.0003573157,0.009396122,0.00045202184,0.0001670325,0.00007479024,0.0003061651,0.00033759486,0.004460632],"genre_scores_gemma":[0.99626946,0.000074394586,0.0028877454,0.000075915945,0.000025845731,0.000030329373,0.00010563543,0.00003216811,0.0004984846],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99963295,0.00017363933,0.000028893997,0.00005174678,0.000047398375,0.00006538431],"domain_scores_gemma":[0.99846554,0.00081745966,0.00021424644,0.00012935353,0.00016663774,0.00020682863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001028859,0.00092567987,0.00074655743,0.00028411677,0.0007369719,0.001403967,0.0011473539,0.0012645941,0.0017528681],"category_scores_gemma":[0.004291599,0.0005298258,0.0006024388,0.00022821536,0.0010071814,0.0010423096,0.0013824445,0.00074540364,0.0001397986],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035235303,0.000093023555,0.0060651368,0.000026194544,0.00008536647,0.000089814035,0.000045103185,0.98630816,0.0021419763,0.0022185964,0.00034328815,0.00223105],"study_design_scores_gemma":[0.00009451876,0.00007429284,0.00091358577,0.0000039388296,0.000026329517,0.000005107608,0.000009978157,0.9982572,0.00025379052,0.0002443178,0.00010853145,0.000008490608],"about_ca_topic_score_codex":0.037716262,"about_ca_topic_score_gemma":0.015249202,"teacher_disagreement_score":0.037716262,"about_ca_system_score_codex":0.0009784889,"about_ca_system_score_gemma":0.0012942848,"threshold_uncertainty_score":0.07499349},"labels":[],"label_agreement":null},{"id":"W1621911916","doi":"10.1029/2007gl031656","title":"Lengthening plus shortening of river‐to‐lake connection times in the Mackenzie River Delta respectively via two global change mechanisms along the arctic coast","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Delta; River delta; Geology; Arctic; Connection (principal bundle); Hydrology (agriculture); Oceanography; Physical geography; Climatology; Environmental science; Geography; Geotechnical engineering; Geometry","score_opus":0.07842277515336575,"score_gpt":0.3257614930210156,"score_spread":0.24733871786764983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1621911916","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986374,0.00013007467,0.000097738295,0.000080654594,0.000005447335,0.000002789969,0.00008373979,0.00000597687,0.00095622946],"genre_scores_gemma":[0.99902356,0.00014935486,0.00016657988,0.0000385203,0.000010372196,0.0000050444633,0.00010996543,0.0000030296133,0.0004936964],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988914,0.000014988989,0.000015490476,0.000034292018,0.000016654869,0.000029372159],"domain_scores_gemma":[0.9993724,0.000049192022,0.0003030917,0.000060465685,0.00008475344,0.00013014299],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003651478,0.0001562156,0.00014366067,0.00058515026,0.00051765644,0.0007210648,0.00015226356,0.00020347451,0.0013212903],"category_scores_gemma":[0.0010334994,0.00012668701,0.00019467443,0.00042260878,0.00047023527,0.00042525353,0.00045513368,0.00029288573,0.00010368046],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041850616,0.000058271246,0.9364565,0.00007315573,0.00011773942,0.0002647155,0.00088064896,0.0023752458,0.014605614,0.0016901463,0.00069360057,0.04236587],"study_design_scores_gemma":[0.000004531344,0.000033113614,0.99802125,0.0000043682444,0.000018459896,0.000058410915,0.00014647507,0.00025586813,0.0004738125,0.00012715433,0.0008519102,0.0000046301257],"about_ca_topic_score_codex":0.011720638,"about_ca_topic_score_gemma":0.034700636,"teacher_disagreement_score":0.98827934,"about_ca_system_score_codex":0.00095016044,"about_ca_system_score_gemma":0.0006128279,"threshold_uncertainty_score":0.02330482},"labels":[],"label_agreement":null},{"id":"W1623751028","doi":"10.1029/2007gl030550","title":"Impacts of peat and vegetation on permafrost degradation under climate warming","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Permafrost; Peat; Environmental science; Climate change; Vegetation (pathology); Global warming; Climatology; Climate model; Land cover; Physical geography; Land use; Geology; Ecology; Geography; Oceanography","score_opus":0.06750696112007651,"score_gpt":0.33006367150286925,"score_spread":0.2625567103827927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1623751028","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979108,0.000050727085,0.00021165595,0.00006634946,0.000005860964,0.0000074589193,0.00036982461,0.000024458139,0.0013529874],"genre_scores_gemma":[0.9991999,0.000038149923,0.00023389082,0.000014931236,0.0000015951854,0.0000058438277,0.00021587181,0.000005848634,0.00028393272],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998652,0.000032117765,0.0000049906403,0.000019922338,0.000015939466,0.000061834144],"domain_scores_gemma":[0.99964213,0.00014010535,0.000040990806,0.000018674584,0.000060831568,0.00009734578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033504688,0.0004004349,0.00036819174,0.0003702256,0.0007988993,0.00073061616,0.0007514875,0.0007514979,0.0016472905],"category_scores_gemma":[0.0010454875,0.0003212705,0.0007121782,0.00050715293,0.0007555334,0.00038295632,0.00041930503,0.00048547966,0.00008854568],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023897423,0.000078986974,0.046874896,0.00002897975,0.000067598005,0.00015585285,0.000052538344,0.9488324,0.0011938496,0.0007475484,0.00031651033,0.001411916],"study_design_scores_gemma":[0.00017791837,0.00012273318,0.044913445,0.000014776765,0.00006832798,0.000052557723,0.00022171035,0.9525257,0.0008536344,0.00046400898,0.00055917905,0.000025985573],"about_ca_topic_score_codex":0.57461965,"about_ca_topic_score_gemma":0.5651188,"teacher_disagreement_score":0.57461965,"about_ca_system_score_codex":0.004202733,"about_ca_system_score_gemma":0.0032348328,"threshold_uncertainty_score":0.855771},"labels":[],"label_agreement":null},{"id":"W1623908870","doi":"10.1029/2010gl046012","title":"Quantifying stratospheric ozone trends: Complications due to stratospheric cooling","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Environment and Climate Change Canada","funders":"","keywords":"Ozone layer; Environmental science; Ozone; Atmospheric sciences; Stratosphere; Ozone depletion; Climatology; Meteorology; Astrobiology; Geology; Physics","score_opus":0.11215023651753923,"score_gpt":0.3233796621243339,"score_spread":0.21122942560679464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1623908870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.64759386,0.016136153,0.31143764,0.0029660303,0.00055365457,0.00037448894,0.0078841355,0.00083589903,0.012218178],"genre_scores_gemma":[0.9576511,0.0027667466,0.035161857,0.00070500345,0.0004142036,0.00019664268,0.002108633,0.00025375283,0.0007421142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9969459,0.0016039415,0.0002320233,0.0005469184,0.00046638915,0.00020492276],"domain_scores_gemma":[0.991478,0.0048085405,0.0017378515,0.0011997278,0.0006938507,0.00008206419],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009542155,0.0005979522,0.00070387486,0.0017827826,0.0007854586,0.0010649632,0.0008281277,0.0007255199,0.00057354773],"category_scores_gemma":[0.025083128,0.00040537413,0.000649032,0.0044673258,0.0007800842,0.0018025485,0.0016188733,0.0008147128,0.0002058309],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004724362,0.000044316857,0.7278491,0.0010872085,0.0011466632,0.0006018227,0.001949913,0.023553465,0.018272975,0.017436182,0.0055749654,0.20201097],"study_design_scores_gemma":[0.00002679116,0.00024254089,0.8830691,0.0003452926,0.0004933849,0.0012668048,0.00085180026,0.04008774,0.018211843,0.028649257,0.0266745,0.000080915415],"about_ca_topic_score_codex":0.009601931,"about_ca_topic_score_gemma":0.0077729314,"teacher_disagreement_score":0.009601931,"about_ca_system_score_codex":0.0005787553,"about_ca_system_score_gemma":0.00053225545,"threshold_uncertainty_score":0.050464332},"labels":[],"label_agreement":null},{"id":"W1624413182","doi":"10.1029/2003gl019212","title":"The role of midlatitude storms on air‐sea exchange of CO<sub>2</sub>","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"","keywords":"Middle latitudes; Fugacity; Storm; Environmental science; Upwelling; Climatology; Atmospheric sciences; Sea surface temperature; Oceanography; Storm surge; Geology; Chemistry","score_opus":0.022432742832983837,"score_gpt":0.2738505894965945,"score_spread":0.25141784666361067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1624413182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980844,0.0001932633,0.000101936756,0.00010834267,0.000008596868,0.000001878951,0.00005106269,0.0000076092724,0.0014429332],"genre_scores_gemma":[0.99956375,0.00015868248,0.00004597284,0.000014857879,0.00000825293,0.0000010647657,0.000026069927,0.0000021343753,0.0001792622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.000011153423,0.0000018009383,0.0000040098253,0.000003735608,0.000016757425],"domain_scores_gemma":[0.9998049,0.00009722282,0.00003462863,0.000006162347,0.00001586886,0.000041144638],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012452198,0.00021643507,0.00011703692,0.00013488083,0.00023442398,0.00042640945,0.00011095525,0.00022567742,0.0011951574],"category_scores_gemma":[0.00038352938,0.000106343956,0.00015999109,0.000080342885,0.0002594267,0.00025966132,0.00022516158,0.00015447292,0.00010072649],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003300873,0.00044493843,0.6286345,0.00036237668,0.00028258687,0.0029502301,0.0010081361,0.10336129,0.18854763,0.013424377,0.0042478717,0.0534352],"study_design_scores_gemma":[0.00011867026,0.00032959844,0.8602881,0.00002697761,0.00011589318,0.0001892331,0.0007373687,0.12171694,0.0128772855,0.0020328516,0.0015430204,0.000024078536],"about_ca_topic_score_codex":0.011180783,"about_ca_topic_score_gemma":0.010541225,"teacher_disagreement_score":0.011180783,"about_ca_system_score_codex":0.00040692868,"about_ca_system_score_gemma":0.00024563915,"threshold_uncertainty_score":0.0222314},"labels":[],"label_agreement":null},{"id":"W1626722022","doi":"10.1029/2011gl050478","title":"Severe 2011 ozone depletion assessed with 11 years of ozone, NO<sub>2</sub>, and OClO measurements at 80°N","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; University of Waterloo; Environment and Climate Change Canada; University of Toronto","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Research and Innovation Foundation; University of Toronto; Government of Canada; Nova Scotia Research Innovation Trust; Sight Research UK; Canadian Foundation for Climate and Atmospheric Sciences; Ontario Innovation Trust","keywords":"Ozone; Ozone depletion; Ozone layer; Atmospheric sciences; Environmental science; Polar vortex; Arctic; Stratosphere; Climatology; Meteorology; Physics; Geology; Oceanography","score_opus":0.038775859387364116,"score_gpt":0.26198826821650323,"score_spread":0.22321240882913912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1626722022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99840325,0.00004608429,0.00007834336,0.00003802184,0.000004729537,0.000004558613,0.00087211665,0.0000088130655,0.0005439819],"genre_scores_gemma":[0.9958762,0.000101708894,0.00021111847,0.000052141444,0.000010088799,0.0000109940875,0.0033230186,0.0000045578154,0.00041018327],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998313,0.0000139722115,0.000012775643,0.000045219353,0.000043456184,0.000053169086],"domain_scores_gemma":[0.99968505,0.00003191716,0.00010831004,0.000040686286,0.00007868572,0.000055364908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042010678,0.00044131203,0.00040188272,0.00032151715,0.0007669904,0.00073587644,0.00027097267,0.00056498614,0.00041491154],"category_scores_gemma":[0.00042435175,0.0002819655,0.00031334002,0.0005648973,0.00036509425,0.0005826717,0.0005949926,0.00047272936,0.000112819536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009996215,0.00026930476,0.94347817,0.00009123526,0.00038023686,0.00039521788,0.00034221236,0.004660497,0.040912487,0.00014687257,0.001468685,0.0068553593],"study_design_scores_gemma":[0.000005595713,0.000056757155,0.9958259,0.000003435823,0.00003330916,0.00003309596,0.00009596766,0.0006330113,0.0026719903,0.0000117535565,0.00062307046,0.0000061432506],"about_ca_topic_score_codex":0.076148406,"about_ca_topic_score_gemma":0.17085738,"teacher_disagreement_score":0.076148406,"about_ca_system_score_codex":0.0012496903,"about_ca_system_score_gemma":0.0007946373,"threshold_uncertainty_score":0.15141034},"labels":[],"label_agreement":null},{"id":"W1627710482","doi":"10.1029/2010gl042440","title":"Mystery of ice multiplication in warm‐based precipitating shallow cumulus clouds","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Clear ice; Ice crystals; Supercooling; Atmospheric sciences; Geology; Sea ice growth processes; Ice cloud; Ice nucleus; Sea ice; Climatology; Meteorology; Sea ice thickness; Arctic ice pack; Physics; Antarctic sea ice; Optics; Radiative transfer; Thermodynamics","score_opus":0.025202703804189736,"score_gpt":0.31056152627896594,"score_spread":0.2853588224747762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1627710482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882804,0.0030520575,0.004141861,0.0009499735,0.00007606615,0.00001288784,0.000054307406,0.00007754216,0.0033548917],"genre_scores_gemma":[0.9992716,0.00040485567,0.0002016673,0.000013461247,0.000033318975,0.0000021712551,0.000008228342,0.0000022547292,0.00006242841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998783,0.000025100793,0.000008073845,0.000027158556,0.000027664802,0.000033675078],"domain_scores_gemma":[0.9995968,0.00016156065,0.00009300114,0.00004886693,0.000028520359,0.00007144108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003317388,0.0001833026,0.00037374216,0.00026991087,0.0006178342,0.00088946876,0.00069548894,0.0005703334,0.00064166985],"category_scores_gemma":[0.001146651,0.00028645233,0.0002760055,0.00014023973,0.0017187529,0.0019617297,0.00061820087,0.0005475056,0.00008815493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017992913,0.0003606926,0.32161498,0.000979474,0.00046903893,0.007805936,0.0021732561,0.16474643,0.18345183,0.1980181,0.005552208,0.11302868],"study_design_scores_gemma":[0.00024956974,0.00048356233,0.24077445,0.00014452409,0.00019824579,0.004329125,0.002132918,0.5361619,0.02890076,0.17534438,0.0110357,0.00024485865],"about_ca_topic_score_codex":0.002465009,"about_ca_topic_score_gemma":0.0011969637,"teacher_disagreement_score":0.002465009,"about_ca_system_score_codex":0.00045771082,"about_ca_system_score_gemma":0.00042128164,"threshold_uncertainty_score":0.0049013495},"labels":[],"label_agreement":null},{"id":"W1627798039","doi":"10.1029/2005gl023060","title":"Correction of atmospheric dynamical seasonal forecasts using the leading ocean‐forced spatial patterns","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geopotential height; Climatology; Forecast skill; General Circulation Model; GCM transcription factors; Geopotential; Ensemble average; North Atlantic oscillation; Singular value decomposition; Environmental science; Meteorology; Ensemble forecasting; Econometrics; Mathematics; Geography; Climate change; Geology; Precipitation; Oceanography","score_opus":0.0366265734294305,"score_gpt":0.3074671099422481,"score_spread":0.2708405365128176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1627798039","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.20264222,0.0002689434,0.78995967,0.00064329826,0.00061665225,0.00005214138,0.0007098853,0.0029216243,0.0021855324],"genre_scores_gemma":[0.7913342,0.0003008426,0.204005,0.00009587314,0.00016863609,0.000054440836,0.0011205975,0.00041027274,0.0025100945],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99958915,0.00009682372,0.000031362553,0.00006210893,0.00019096448,0.00002953962],"domain_scores_gemma":[0.99804187,0.00048926746,0.00033238722,0.00037916593,0.0006970082,0.00006029081],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010353753,0.00044507053,0.00029648014,0.0006884925,0.00030664596,0.0005702105,0.0004749378,0.0003214375,0.0007457401],"category_scores_gemma":[0.008357201,0.00034267904,0.0003551514,0.0007061912,0.00018718638,0.00060092116,0.00046885718,0.00078976364,0.00032893877],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112673115,0.000056701978,0.019026473,0.00005444589,0.00018593139,0.00009662659,0.00008318999,0.6532823,0.014395508,0.005493287,0.0052295276,0.30198333],"study_design_scores_gemma":[0.000013927801,0.000016152913,0.0046832943,0.0000042995853,0.000011188005,0.000024380517,0.000008187536,0.98836935,0.004227684,0.0014281496,0.0011986488,0.000014823734],"about_ca_topic_score_codex":0.014458421,"about_ca_topic_score_gemma":0.020753078,"teacher_disagreement_score":0.014458421,"about_ca_system_score_codex":0.00035461935,"about_ca_system_score_gemma":0.0013077086,"threshold_uncertainty_score":0.028748512},"labels":[],"label_agreement":null},{"id":"W1628231082","doi":"10.1029/2010gl043478","title":"Reorganization of ice sheet flow patterns in Arctic Canada and the mid‐Pleistocene transition","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Glacial period; Ice sheet; Deglaciation; Pleistocene; Interglacial; Arctic; Ice stream; Oceanography; Erosion; Bedrock; Glacier; Physical geography; Ice-sheet model; Paleontology; Geomorphology; Arctic ice pack; Cryosphere; Sea ice; Antarctic sea ice; Geography","score_opus":0.011785372695715775,"score_gpt":0.236232279682432,"score_spread":0.2244469069867162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1628231082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764663,0.000335158,0.00006498735,0.00011603115,0.0000030645735,0.0000044892186,0.00033558914,0.000010483475,0.0014835424],"genre_scores_gemma":[0.9988741,0.00020763774,0.000091718575,0.000021236263,0.0000014383496,0.0000026628634,0.0002733556,0.0000035778419,0.0005242152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998615,0.000008397426,0.0000045824836,0.000028346589,0.00003462329,0.00006267154],"domain_scores_gemma":[0.99957424,0.000024128913,0.00005680018,0.000011233171,0.00023189251,0.00010168616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018902405,0.00011068515,0.00013908991,0.001589539,0.00158491,0.0010057411,0.00032902972,0.00021592142,0.0011654634],"category_scores_gemma":[0.00093833054,0.00015263948,0.00014476918,0.0014055135,0.0008284568,0.00021954397,0.0003926737,0.00021635459,0.00009313403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013033293,0.000016293132,0.96693635,0.000031847576,0.000056020494,0.00018778023,0.0031941228,0.0011237394,0.005303537,0.00066967943,0.0006684039,0.021681966],"study_design_scores_gemma":[0.0000012311128,0.0000029369762,0.9979771,0.0000058099085,0.00000402426,0.000017816506,0.000715131,0.00022008583,0.00010177514,0.000031177588,0.00091975345,0.0000032058751],"about_ca_topic_score_codex":0.98202896,"about_ca_topic_score_gemma":0.99342704,"teacher_disagreement_score":0.017971039,"about_ca_system_score_codex":0.015478231,"about_ca_system_score_gemma":0.012055976,"threshold_uncertainty_score":0.11230296},"labels":[],"label_agreement":null},{"id":"W1630296365","doi":"10.1029/2009gl041861","title":"Variability of Indian summer monsoon in a new upper tropospheric humidity data set","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Environment Research Council; National Aeronautics and Space Administration; Langley Research Center; Department for Environment, Food and Rural Affairs, UK Government; Sight Research UK; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Monsoon; Troposphere; Climatology; Humidity; Subsidence; Atmospheric sciences; Environmental science; Monsoon of South Asia; Convection; Relative humidity; East Asian Monsoon; Geology; Meteorology; Geography; Structural basin","score_opus":0.08850986255795931,"score_gpt":0.35512128941605026,"score_spread":0.2666114268580909,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1630296365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9739647,0.00006424596,0.0010991722,0.00011948112,0.0000604618,0.00003229288,0.023161992,0.00022445073,0.0012731478],"genre_scores_gemma":[0.913433,0.00009933467,0.0029082508,0.000041683426,0.00006632696,0.000083386294,0.08287937,0.000049450566,0.0004391374],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999337,0.00010111446,0.00007271557,0.00014741265,0.00022819443,0.00011350134],"domain_scores_gemma":[0.99772257,0.00039782963,0.000353075,0.0006484148,0.0005799847,0.00029807404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095280743,0.00040762578,0.00049500697,0.0011599421,0.0003739275,0.00085960224,0.00063083146,0.00032629544,0.0005079308],"category_scores_gemma":[0.0015594303,0.00021958753,0.0005497241,0.0015079984,0.00033214258,0.0005144285,0.0007818927,0.0008239449,0.0002450536],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017675575,0.001581269,0.812386,0.00030070418,0.0010095068,0.001158925,0.0011338365,0.07216034,0.036862224,0.0013566844,0.018767208,0.051515814],"study_design_scores_gemma":[0.00008635213,0.000101972066,0.9427891,0.0000152236935,0.00011578334,0.0002862636,0.00023064925,0.037626687,0.006891381,0.00015750619,0.0116147585,0.00008435918],"about_ca_topic_score_codex":0.030683184,"about_ca_topic_score_gemma":0.038469084,"teacher_disagreement_score":0.030683184,"about_ca_system_score_codex":0.0006695648,"about_ca_system_score_gemma":0.00059852697,"threshold_uncertainty_score":0.06100917},"labels":[],"label_agreement":null},{"id":"W1632683774","doi":"10.1029/2011gl048542","title":"Turbulence transition in stratified atmospheric and oceanic shear flows: Reynolds and Prandtl number controls upon the mechanism","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fluid Dynamics and Turbulent Flows","field":"Engineering","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Compute Canada","keywords":"Prandtl number; Turbulence; Instability; Reynolds number; Convective instability; Mechanics; Physics; Turbulent Prandtl number; Shear (geology); Stagnation point; Geology; Convection; Classical mechanics; Meteorology; Heat transfer; Nusselt number","score_opus":0.01690590424870568,"score_gpt":0.23791534752644303,"score_spread":0.22100944327773736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1632683774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97764903,0.0007146022,0.018568479,0.00022396668,0.000026562366,0.000027753542,0.00008627359,0.00016119258,0.002542126],"genre_scores_gemma":[0.9983632,0.00014444055,0.0011477765,0.00000792275,0.000009980883,0.000008826127,0.000021936477,0.0000068675567,0.00028910307],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991035,0.000012571542,0.000005771655,0.000018582228,0.000026150019,0.000026627715],"domain_scores_gemma":[0.9998385,0.000038500577,0.000053377826,0.000019569097,0.000023591088,0.000026412197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016297212,0.0002071048,0.00019364493,0.00040529243,0.0004233727,0.0006368503,0.00028773688,0.00022790853,0.00065191713],"category_scores_gemma":[0.0006468759,0.00011134306,0.00019919661,0.00017139217,0.0007525614,0.0004251131,0.00042474773,0.00033898072,0.00016053388],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078208634,0.00012913332,0.046927977,0.00022656906,0.00002719273,0.00082008034,0.0012579699,0.021741731,0.8129408,0.0811065,0.0009901803,0.033049796],"study_design_scores_gemma":[0.00018513358,0.000868361,0.20053604,0.000073275856,0.00005540634,0.0013666258,0.0005959765,0.25811714,0.46064597,0.071302086,0.0060999016,0.00015411315],"about_ca_topic_score_codex":0.00073266355,"about_ca_topic_score_gemma":0.0005279054,"teacher_disagreement_score":0.00073266355,"about_ca_system_score_codex":0.00035936045,"about_ca_system_score_gemma":0.00033241944,"threshold_uncertainty_score":0.0026073456},"labels":[],"label_agreement":null},{"id":"W1633273390","doi":"10.1029/2008gl033354","title":"Organic iron (III) complexing ligands during an iron enrichment experiment in the western subarctic North Pacific","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Subarctic climate; Ligand (biochemistry); Genetic algorithm; Environmental chemistry; Chemistry; Iron fertilization; Dilution; Bioavailability; Bloom; Nutrient; Phytoplankton; Biology; Ecology; Receptor; Organic chemistry","score_opus":0.03784123107702348,"score_gpt":0.266956055592106,"score_spread":0.22911482451508253,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1633273390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998555,0.000011975565,0.00002382891,0.000007602237,6.069804e-7,0.0000034873524,0.000013130892,0.000001128887,0.00008268241],"genre_scores_gemma":[0.998855,0.00006451466,0.0003870215,0.000043935885,0.0000028974296,0.000012884191,0.00007736187,0.000002998561,0.00055341364],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.000009416364,0.0000028756494,0.000020592805,0.000013566783,0.000015850002],"domain_scores_gemma":[0.9998373,0.00003192887,0.000038096976,0.000008592472,0.000036467914,0.00004757787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016564471,0.00021507057,0.00029145312,0.00013367036,0.0005532314,0.00028980226,0.00019268185,0.00024714472,0.00030463684],"category_scores_gemma":[0.00019476262,0.00020924708,0.00009531843,0.00013429395,0.00033381078,0.00013509257,0.00022912999,0.0003984819,0.000055147306],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010800193,0.00021082906,0.056528203,0.00006475343,0.00004915763,0.00037389362,0.00061649334,0.0003613248,0.93773335,0.000022046168,0.00007028751,0.002889674],"study_design_scores_gemma":[0.00010140893,0.0016035963,0.79457104,0.000010520839,0.000099883604,0.0001660429,0.0012530212,0.0016563684,0.19934952,0.000035811176,0.0011325664,0.000020291305],"about_ca_topic_score_codex":0.04683875,"about_ca_topic_score_gemma":0.10309139,"teacher_disagreement_score":0.04683875,"about_ca_system_score_codex":0.000706713,"about_ca_system_score_gemma":0.00049848837,"threshold_uncertainty_score":0.09313226},"labels":[],"label_agreement":null},{"id":"W1633959171","doi":"10.1029/2011gl047705","title":"Sharp thermal transition in the forearc mantle wedge as a consequence of nonlinear mantle wedge flow","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Forearc; Mantle wedge; Wedge (geometry); Geology; Transition zone; Mantle (geology); Geophysics; Thermal; Nonlinear system; Seismology; Petrology; Subduction; Physics; Tectonics; Thermodynamics; Optics","score_opus":0.05410277053972061,"score_gpt":0.28188915725148095,"score_spread":0.22778638671176032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1633959171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966397,0.000118495045,0.0006302227,0.00013015798,0.000016791912,0.0000067494907,0.00024791257,0.0001295052,0.0020805106],"genre_scores_gemma":[0.99925023,0.00003966593,0.00010847377,0.000022202265,0.0000032986466,0.0000021090045,0.00010422612,0.00001147839,0.0004582463],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999776,0.000001855163,0.0000014858907,0.000005780814,0.0000044780754,0.000008777786],"domain_scores_gemma":[0.99991596,0.000016460961,0.000018131941,0.00001637344,0.000009103499,0.000024058334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006999895,0.00008184944,0.00015975785,0.00019775137,0.00019865851,0.0003310393,0.00026181337,0.000339159,0.004575254],"category_scores_gemma":[0.0003180126,0.00015829473,0.00014527391,0.0001595683,0.0006352415,0.0001663164,0.00053030223,0.00056606205,0.00039644953],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028833277,0.00014280336,0.06376547,0.00021448242,0.00006925079,0.00400867,0.0005411078,0.007585897,0.8963097,0.0054092826,0.0024212813,0.016648853],"study_design_scores_gemma":[0.00035776754,0.0003298289,0.9053946,0.00003055801,0.00006457321,0.0015793348,0.00044220526,0.014917853,0.070380315,0.004405636,0.002052717,0.000044567005],"about_ca_topic_score_codex":0.0023940816,"about_ca_topic_score_gemma":0.0020572452,"teacher_disagreement_score":0.004575254,"about_ca_system_score_codex":0.00027978307,"about_ca_system_score_gemma":0.00014838106,"threshold_uncertainty_score":0.0153057575},"labels":[],"label_agreement":null},{"id":"W1634245572","doi":"10.1029/2010gl042652","title":"Synoptic airborne thickness surveys reveal state of Arctic sea ice cover","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Climatology; Sea ice; Arctic; Snow cover; Arctic ice pack; Sea ice concentration; Cryosphere; Environmental science; Geology; The arctic; Cover (algebra); Remote sensing; Sea ice thickness; Oceanography; Physical geography; Meteorology; Atmospheric sciences; Snow; Geography; Geomorphology","score_opus":0.019473877733898755,"score_gpt":0.26783509225656843,"score_spread":0.24836121452266968,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1634245572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909933,0.00007021968,0.0003769645,0.00001392468,0.0000046071023,0.000009657035,0.0067646275,0.00002891911,0.0017377161],"genre_scores_gemma":[0.99105,0.00012916239,0.0011958396,0.000012990672,0.000010153509,0.000015932723,0.007025428,0.000008068369,0.0005524375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000018949831,0.000016027792,0.000027723849,0.000030020656,0.000018875502],"domain_scores_gemma":[0.9993249,0.00010639014,0.0002693752,0.00006160584,0.00018955658,0.000048183738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028629752,0.00022053675,0.00010176026,0.0011098894,0.00018755137,0.00033689034,0.00011033949,0.00012982529,0.0010143598],"category_scores_gemma":[0.0006841456,0.00010497733,0.000093800176,0.0010253487,0.00011095895,0.00033936164,0.00031553645,0.00009444694,0.0002921793],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066882385,0.000027335258,0.98386544,0.00003107109,0.000047434674,0.000042201023,0.00025193987,0.00077124557,0.002991783,0.00006216628,0.0009647522,0.010877749],"study_design_scores_gemma":[0.0000016960798,0.000016814458,0.997721,0.0000038073642,0.0000069371163,0.000024771556,0.00020647602,0.0006247592,0.000465533,0.00001996517,0.00090596464,0.0000022768877],"about_ca_topic_score_codex":0.011711319,"about_ca_topic_score_gemma":0.03113784,"teacher_disagreement_score":0.011711319,"about_ca_system_score_codex":0.0001790394,"about_ca_system_score_gemma":0.00015294236,"threshold_uncertainty_score":0.023286343},"labels":[],"label_agreement":null},{"id":"W1635365782","doi":"10.1002/grl.50672","title":"Controls on recent Alaskan lake changes identified from water isotopes and remote sensing","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Innovates","funders":"","keywords":"Permafrost; Snowmelt; Precipitation; Environmental science; Hydrology (agriculture); Surface water; Groundwater; Wetland; Snow; Water balance; Water cycle; Period (music); Geology; Physical geography; Oceanography; Ecology; Geomorphology; Geography","score_opus":0.062276511246701347,"score_gpt":0.28822030845355723,"score_spread":0.22594379720685587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1635365782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99893993,0.000074819414,0.00007346497,0.000023002953,0.0000020979678,0.0000019548909,0.00018776512,0.0000053659087,0.00069146475],"genre_scores_gemma":[0.9996983,0.000036486043,0.00004927686,0.00000517047,0.0000022199818,0.0000011843515,0.000107158296,9.446491e-7,0.000099315264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998857,0.000018192464,0.000013304105,0.000038479382,0.000023047249,0.000021293501],"domain_scores_gemma":[0.99954873,0.000072064024,0.00023623859,0.000029978764,0.00006611717,0.00004681654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029614594,0.00011491474,0.00008905859,0.00068163837,0.00022671996,0.00047499393,0.00009955908,0.00013040843,0.00073643663],"category_scores_gemma":[0.00066688785,0.00009874229,0.00012476539,0.00048256168,0.00028662774,0.00030997922,0.00021964176,0.00010178452,0.00006642026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044657627,0.000013740773,0.9927043,0.0000072775697,0.00004247628,0.000054900753,0.00020777938,0.00024970766,0.0025730114,0.000085340165,0.000082773324,0.0039341445],"study_design_scores_gemma":[4.63377e-7,0.000005189787,0.9995153,0.0000011147663,0.0000051782526,0.000012719387,0.00007313474,0.0001681718,0.000095092575,0.00002114266,0.000101325095,0.0000012402717],"about_ca_topic_score_codex":0.02345588,"about_ca_topic_score_gemma":0.07112919,"teacher_disagreement_score":0.02345588,"about_ca_system_score_codex":0.00037778934,"about_ca_system_score_gemma":0.00017822541,"threshold_uncertainty_score":0.046638727},"labels":[],"label_agreement":null},{"id":"W1636999165","doi":"10.1029/2011gl047493","title":"Water vapor intrusions into the High Arctic during winter","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; Dalhousie University","funders":"","keywords":"Downwelling; Arctic; Environmental science; Longwave; Water vapor; Atmospheric sciences; Lidar; Climatology; Arctic geoengineering; Radiative transfer; Upwelling; Meteorology; Geology; Remote sensing; Arctic ice pack; Oceanography; Geography; Sea ice thickness; Physics","score_opus":0.026124294847818304,"score_gpt":0.24838169633513016,"score_spread":0.22225740148731185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1636999165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99927396,0.00005493734,0.000051622985,0.000019417454,0.00000398863,0.0000019595172,0.0001431208,0.000012020773,0.0004390122],"genre_scores_gemma":[0.9993517,0.00005401034,0.000069565926,0.000008186014,0.000007831498,0.0000019386796,0.0003526003,0.0000033327474,0.00015076884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.00000550978,0.000002578833,0.000015815009,0.000021843494,0.000021801061],"domain_scores_gemma":[0.9998858,0.000012620664,0.00003194723,0.0000064101305,0.0000374107,0.000025780846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013503552,0.00021633829,0.00022379671,0.00036544522,0.00067235186,0.0005276179,0.00019266478,0.00024673602,0.00037198712],"category_scores_gemma":[0.00024008988,0.00013531637,0.00013810612,0.0005179968,0.00032283636,0.00021784456,0.000343061,0.00024339384,0.00008773469],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007792558,0.00014726128,0.892383,0.00007350726,0.00015360242,0.0008263588,0.0012270381,0.0023994336,0.0842879,0.00020570216,0.0010451416,0.016471792],"study_design_scores_gemma":[0.000004349176,0.000045944715,0.99549145,0.000004586615,0.00001622945,0.00007302114,0.00021816704,0.0011117529,0.0022642436,0.000021455508,0.00074364705,0.0000053282192],"about_ca_topic_score_codex":0.106307335,"about_ca_topic_score_gemma":0.168581,"teacher_disagreement_score":0.8936927,"about_ca_system_score_codex":0.0008402802,"about_ca_system_score_gemma":0.00045647664,"threshold_uncertainty_score":0.21137708},"labels":[],"label_agreement":null},{"id":"W1637296903","doi":"10.1002/2014gl060662","title":"Simulation of monsoon intraseasonal oscillations in a coarse‐resolution aquaplanet GCM","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Climatology; Madden–Julian oscillation; Monsoon; Intertropical Convergence Zone; Convection; Rossby wave; GCM transcription factors; Seesaw molecular geometry; Geology; Atmospheric sciences; Zonal and meridional; Trough (economics); Environmental science; General Circulation Model; Precipitation; Oceanography; Meteorology; Physics; Climate change","score_opus":0.04415484784857567,"score_gpt":0.3182795791728986,"score_spread":0.27412473132432297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1637296903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940614,0.000027993308,0.0020948092,0.00011321775,0.00001996469,0.00003064648,0.00060984935,0.00032299492,0.0027191807],"genre_scores_gemma":[0.99582773,0.00001560993,0.003096911,0.00003214569,0.0000032257426,0.00003289771,0.0004208195,0.000025363262,0.0005453366],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999889,0.000029961699,0.0000059966956,0.000027047521,0.000021839463,0.000026211083],"domain_scores_gemma":[0.9996123,0.0001703543,0.000031080977,0.000051388142,0.00006800393,0.000066848115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030489106,0.0004892183,0.00046860467,0.00030330548,0.0005835026,0.0006248439,0.0015426236,0.0010280204,0.002890532],"category_scores_gemma":[0.0008152914,0.0003586754,0.00043101417,0.0005575694,0.00068454375,0.00045688977,0.00046285675,0.00091576553,0.00020291227],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017412001,0.00013460175,0.0066947327,0.000015590766,0.000045379875,0.00010862774,0.00004945624,0.9884466,0.0015469469,0.00050963275,0.0005164448,0.0017579327],"study_design_scores_gemma":[0.00007180278,0.000034787885,0.001986924,0.0000018139799,0.000007555223,0.0000058838677,0.00002660367,0.99693453,0.00054801354,0.00015797614,0.00021642465,0.0000075477187],"about_ca_topic_score_codex":0.084326714,"about_ca_topic_score_gemma":0.03876097,"teacher_disagreement_score":0.084326714,"about_ca_system_score_codex":0.0014361023,"about_ca_system_score_gemma":0.0011321154,"threshold_uncertainty_score":0.16767174},"labels":[],"label_agreement":null},{"id":"W1637748895","doi":"10.1029/2012gl052815","title":"The impact of model fidelity on seasonal predictive skill","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Environmental science; Forecast skill; Cyclostationary process; Fidelity; Forcing (mathematics); GCM transcription factors; Meteorology; Climate model; Statistics; Climate change; Computer science; General Circulation Model; Mathematics","score_opus":0.05348547046849572,"score_gpt":0.360703001193278,"score_spread":0.30721753072478225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1637748895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9698093,0.0002581239,0.02676889,0.00035336398,0.000049850223,0.00003898583,0.0003956134,0.00020347397,0.0021224648],"genre_scores_gemma":[0.9976828,0.000043809014,0.0019927314,0.00002096712,0.000006501719,0.000009510675,0.00012886222,0.000024674178,0.00008999122],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99845433,0.00063627324,0.00015396197,0.00026317604,0.00031298536,0.00017910202],"domain_scores_gemma":[0.9797902,0.0143355755,0.0012746325,0.0033666189,0.00092978776,0.0003031483],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0056453524,0.00052659126,0.00059732515,0.00034485222,0.00041842196,0.0011579947,0.0007482867,0.0007696244,0.0007321478],"category_scores_gemma":[0.03031944,0.000343238,0.00066004286,0.0003870396,0.00071634026,0.001695985,0.0010255338,0.001168959,0.000090173016],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006296049,0.00015221669,0.06906387,0.0001201496,0.00030935492,0.00017784245,0.00013267958,0.89634687,0.012368452,0.0020877377,0.0003663051,0.018244954],"study_design_scores_gemma":[0.00003680665,0.0003527144,0.029294198,0.000025013953,0.00006938024,0.00007458477,0.00006633549,0.9577598,0.010506205,0.0013549956,0.0004249297,0.00003508473],"about_ca_topic_score_codex":0.010121436,"about_ca_topic_score_gemma":0.007190553,"teacher_disagreement_score":0.010121436,"about_ca_system_score_codex":0.0006506882,"about_ca_system_score_gemma":0.0006939142,"threshold_uncertainty_score":0.029855847},"labels":[],"label_agreement":null},{"id":"W1638313377","doi":"10.1029/2011gl047011","title":"The impact of surface temperature variability on the climate change response in the Northern Hemisphere polar vortex","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Northern Hemisphere; Stratosphere; Climatology; Environmental science; Forcing (mathematics); Atmospheric sciences; Southern Hemisphere; Polar vortex; Greenhouse gas; Atmosphere (unit); Climate model; Sea surface temperature; Latitude; Climate change; Geology; Meteorology; Oceanography; Geography","score_opus":0.045191593267361094,"score_gpt":0.29345883364169595,"score_spread":0.24826724037433484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1638313377","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989285,0.00005949897,0.00017779329,0.000073206415,0.000008758022,0.0000021968278,0.00011303979,0.0000137565985,0.00062322133],"genre_scores_gemma":[0.9997458,0.000023858105,0.000044821274,0.0000092553055,0.0000060087505,0.0000014409233,0.00011063863,0.000005018153,0.00005322618],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998683,0.00005645915,0.000006296849,0.000022722625,0.000012448088,0.00003379587],"domain_scores_gemma":[0.9995153,0.00028316095,0.00006900276,0.000043552704,0.00004002808,0.000049023463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000440769,0.00028452094,0.00026907763,0.0002186163,0.00039252755,0.00069483666,0.00017602078,0.00040855104,0.0010717303],"category_scores_gemma":[0.0018958513,0.00015788304,0.00027233266,0.00023276382,0.00042081665,0.00039555202,0.00032859523,0.0002654028,0.000099425604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017180247,0.00026113275,0.4928347,0.00014049074,0.00039401336,0.00056827004,0.00027811885,0.4054538,0.07969683,0.002162511,0.0021604106,0.014331692],"study_design_scores_gemma":[0.000158589,0.00044673527,0.66209435,0.000016025417,0.00011154235,0.00015450925,0.0002507977,0.32589912,0.008387574,0.0013061658,0.001135433,0.000039192448],"about_ca_topic_score_codex":0.0062502795,"about_ca_topic_score_gemma":0.0046210573,"teacher_disagreement_score":0.0062502795,"about_ca_system_score_codex":0.00026410588,"about_ca_system_score_gemma":0.00021686267,"threshold_uncertainty_score":0.012427807},"labels":[],"label_agreement":null},{"id":"W1640184946","doi":"10.1002/2014gl060677","title":"Erosion dynamics following localized permafrost slope disturbances","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; ArcticNet","keywords":"Disturbance (geology); Channelized; Erosion; Geology; Permafrost; Sediment; Bank erosion; Channel (broadcasting); Geomorphology; Hydrology (agriculture); Environmental science; Oceanography; Geotechnical engineering","score_opus":0.04117175602107481,"score_gpt":0.29674654731538264,"score_spread":0.2555747912943078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1640184946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99988115,0.0000090101685,0.000018243549,0.0000015902665,1.8901629e-7,7.094025e-7,0.000025243318,8.4300206e-7,0.00006291825],"genre_scores_gemma":[0.99987125,0.000005503367,0.000012884294,0.0000018385165,3.9877588e-7,0.0000012472179,0.00005992933,2.6570612e-7,0.000046757705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999336,0.000010023303,0.0000037932293,0.00002143842,0.000011835977,0.000019367815],"domain_scores_gemma":[0.99976724,0.00003707717,0.00009888377,0.000013491051,0.0000357826,0.000047493755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015602981,0.00011023358,0.00021323004,0.00033205838,0.0002584055,0.00035124065,0.00014249611,0.00024160015,0.0006497381],"category_scores_gemma":[0.00042992076,0.00007773971,0.00013633995,0.00033118075,0.00026301955,0.00016232186,0.00027097628,0.00016480406,0.000091299735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004875146,0.00015300169,0.9462,0.000029116598,0.000065917455,0.0004879046,0.00060271274,0.003085917,0.042218875,0.000064431144,0.00010751502,0.006497151],"study_design_scores_gemma":[0.0000021281396,0.00006730672,0.9987766,0.0000011902359,0.0000033173949,0.00003501634,0.00009379103,0.0006171319,0.00034764758,0.0000132434725,0.000040802457,0.0000016702207],"about_ca_topic_score_codex":0.007244147,"about_ca_topic_score_gemma":0.011180492,"teacher_disagreement_score":0.007244147,"about_ca_system_score_codex":0.00040403174,"about_ca_system_score_gemma":0.00011438124,"threshold_uncertainty_score":0.014403939},"labels":[],"label_agreement":null},{"id":"W1640341850","doi":"10.1029/2012gl051045","title":"The Atlantic and summer Pacific waters variability in the Arctic Ocean from 1997 to 2008","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Arctic; Canada Basin; Water mass; Context (archaeology); Climatology; Structural basin; Environmental science; Arctic ice pack; Arctic sea ice decline; Arctic dipole anomaly; Period (music); North Atlantic Deep Water; Circumpolar deep water; Thermohaline circulation; Geology; Drift ice","score_opus":0.02545272857215383,"score_gpt":0.26408888844691997,"score_spread":0.23863615987476614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1640341850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99679285,0.00017202759,0.00005217107,0.000034436012,0.000006864645,0.0000031114364,0.002042362,0.000005255902,0.0008908666],"genre_scores_gemma":[0.99508685,0.00024819642,0.00016980317,0.000015936226,0.000011534915,0.00000795147,0.0039628386,0.00000451019,0.0004924573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998853,0.00000762293,0.00000942544,0.000031768628,0.000033944805,0.00003190377],"domain_scores_gemma":[0.9996319,0.00002341148,0.0000926821,0.000014768209,0.00019035896,0.000046855905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002879029,0.00018070405,0.00018611553,0.0008643929,0.00034357372,0.0004582688,0.00015194043,0.00013623924,0.0003482945],"category_scores_gemma":[0.00047155583,0.000095073876,0.00021096048,0.001561023,0.00015506693,0.00017598235,0.00029118985,0.00016747937,0.000098389166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000143918,0.00001674765,0.9895559,0.000034907098,0.00009327549,0.000091070906,0.00042479992,0.00032891738,0.0015653603,0.00005926317,0.0005991788,0.0070866123],"study_design_scores_gemma":[0.0000010204666,0.000004828383,0.99910825,0.0000042234333,0.000013182334,0.00001589035,0.00008970187,0.0001071403,0.00007851623,0.000003866293,0.0005722188,0.0000012930343],"about_ca_topic_score_codex":0.27624935,"about_ca_topic_score_gemma":0.3821298,"teacher_disagreement_score":0.27624935,"about_ca_system_score_codex":0.0009772386,"about_ca_system_score_gemma":0.00094593037,"threshold_uncertainty_score":0.5492828},"labels":[],"label_agreement":null},{"id":"W1640914291","doi":"10.1029/2003gl019340","title":"The shape of auroral backscatter spectra","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Backscatter (email); Autocorrelation; Doppler effect; Physics; Spectral shape analysis; Exponential function; Scattering; Spectral line; Fourier transform; Computational physics; Exponential decay; Gaussian; Radar; Optics; Mathematics; Mathematical analysis; Statistics","score_opus":0.0555132952376232,"score_gpt":0.30244024602688696,"score_spread":0.24692695078926374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1640914291","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98094636,0.000166817,0.01188944,0.00010199915,0.00001190504,0.00000852418,0.00020970563,0.00021249145,0.006452785],"genre_scores_gemma":[0.9985562,0.00006128525,0.00075771613,0.0000100086845,0.0000049614005,0.0000026856158,0.00015264543,0.00004663635,0.0004078641],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.00001102116,0.0000030550827,0.000020623354,0.000026227994,0.000017245235],"domain_scores_gemma":[0.99944085,0.00017880788,0.00008062747,0.00006515571,0.00019250691,0.00004198741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025633836,0.00015703161,0.00016009074,0.00049404014,0.00018125073,0.00047611608,0.00015917791,0.00033406098,0.0014131846],"category_scores_gemma":[0.0014163048,0.00018599383,0.00022531126,0.00025289485,0.00034420285,0.00042975706,0.000205582,0.00030489572,0.00034112067],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001212498,0.00013705814,0.19272223,0.00023569279,0.00015528948,0.002111386,0.0016188341,0.15740368,0.512646,0.019001106,0.0037606298,0.108995505],"study_design_scores_gemma":[0.000060385006,0.00028087888,0.45711508,0.000045160505,0.00006568165,0.003968395,0.0005753436,0.45926714,0.059670035,0.013511425,0.0053036637,0.00013687913],"about_ca_topic_score_codex":0.0008796314,"about_ca_topic_score_gemma":0.0005564134,"teacher_disagreement_score":0.0014131846,"about_ca_system_score_codex":0.00022316024,"about_ca_system_score_gemma":0.00014807026,"threshold_uncertainty_score":0.004727602},"labels":[],"label_agreement":null},{"id":"W1644074212","doi":"10.1029/2001gl014289","title":"Heterogeneous nucleation of ice in (NH<sub>4</sub>)<sub>2</sub>SO<sub>4</sub>‐H<sub>2</sub>O particles with mineral dust immersions","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":190,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Ice nucleus; Kaolinite; Nucleation; Montmorillonite; Mineral; Mineralogy; Homogeneous; Aqueous solution; Materials science; Analytical Chemistry (journal); Chemistry; Thermodynamics; Environmental chemistry; Physics; Physical chemistry","score_opus":0.023917945922447323,"score_gpt":0.2366617621145353,"score_spread":0.212743816192088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1644074212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985623,0.00009498062,0.0009733382,0.000004512207,0.0000026367757,0.000008789856,0.000021582056,0.0000058489272,0.00032609992],"genre_scores_gemma":[0.99835724,0.00007335997,0.0011722298,0.000007588862,0.0000036915917,0.000009277722,0.000046317266,0.000004833477,0.0003253928],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998988,0.000009036454,0.000004257432,0.000027571026,0.000027812239,0.000032550393],"domain_scores_gemma":[0.99986875,0.000049942508,0.000028025124,0.000008636813,0.000027389813,0.000017189135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014906842,0.00023275272,0.00013175572,0.00013962995,0.00014824628,0.00018305283,0.0001903752,0.00015702682,0.00041590372],"category_scores_gemma":[0.0001808347,0.00014206576,0.00022174152,0.000053213742,0.0003103382,0.00017711139,0.00021265689,0.00019004314,0.000045273184],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004226564,0.0000085747815,0.001105799,0.000013141246,0.000006345771,0.00003444627,0.00002994143,0.00024231533,0.9980603,0.000024089495,0.0000063040425,0.00042654027],"study_design_scores_gemma":[0.0000071961513,0.000108225686,0.010195068,0.0000017713372,0.000009282976,0.000056391447,0.00004301633,0.0025036014,0.9868348,0.00004169437,0.00019539961,0.0000035288679],"about_ca_topic_score_codex":0.0030525315,"about_ca_topic_score_gemma":0.003412949,"teacher_disagreement_score":0.0030525315,"about_ca_system_score_codex":0.00031702663,"about_ca_system_score_gemma":0.00009753024,"threshold_uncertainty_score":0.006069541},"labels":[],"label_agreement":null},{"id":"W1644665235","doi":"10.1002/2013gl057837","title":"Nighttime vertical plasma drifts and the occurrence of sunrise undulation at the dip equator: A study using Jicamarca incoherent backscatter radar measurements","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Sunrise; Sunset; Geology; Equator; Equinox; Ionosphere; Solstice; F region; Atmospheric sciences; Magnetic dip; Altitude (triangle); Morning; Geodesy; Latitude; Geophysics; Physics; Astronomy; Geometry","score_opus":0.041759751574505115,"score_gpt":0.3046050652405625,"score_spread":0.2628453136660574,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1644665235","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943405,0.000060081402,0.000044520893,0.0000036842491,0.0000020759962,0.0000026541484,0.00017994666,0.000002661603,0.0002703056],"genre_scores_gemma":[0.99918,0.00007677126,0.00011824706,0.0000051882043,0.00000482186,0.0000037634388,0.0004483885,0.000002359547,0.00016059836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000014060837,0.00000731028,0.000026190957,0.000026104924,0.00001767534],"domain_scores_gemma":[0.9996537,0.000057435715,0.00011407846,0.000033421096,0.00007933101,0.00006201723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016354313,0.00018634778,0.00020127745,0.00060323684,0.00024762683,0.00036301947,0.00015827375,0.00022156464,0.00046195908],"category_scores_gemma":[0.00040280726,0.00012231739,0.00013814773,0.00069489627,0.00017020981,0.00014761112,0.00018296053,0.00015947872,0.0001465415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025011005,0.00007848476,0.9822871,0.000031554533,0.00006703804,0.00020662289,0.00049371977,0.00013103923,0.010645391,0.000026232803,0.00012135779,0.005661376],"study_design_scores_gemma":[0.0000012128032,0.000025192845,0.9994468,0.0000010111245,0.0000050675844,0.000046250778,0.0000749243,0.000094864234,0.00021429977,0.0000020768068,0.00008691105,0.0000014260637],"about_ca_topic_score_codex":0.011605651,"about_ca_topic_score_gemma":0.014754495,"teacher_disagreement_score":0.011605651,"about_ca_system_score_codex":0.00021619191,"about_ca_system_score_gemma":0.0001478661,"threshold_uncertainty_score":0.023076177},"labels":[],"label_agreement":null},{"id":"W1644901782","doi":"10.1029/2007gl031584","title":"On the Pacific Decadal Oscillation and the Atlantic Multidecadal Oscillation: Might they be related?","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":139,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Pacific decadal oscillation; Atlantic multidecadal oscillation; Oscillation (cell signaling); Climatology; Geology; Sea surface temperature; Structural basin; Environmental science; Forcing (mathematics); Oceanography; Chemistry","score_opus":0.03293621513711283,"score_gpt":0.2928946095798604,"score_spread":0.2599583944427476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1644901782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6194789,0.13274726,0.008447413,0.11084596,0.0049107075,0.00010314435,0.0016488546,0.00015558198,0.12166208],"genre_scores_gemma":[0.93618983,0.037917852,0.001379311,0.009897885,0.0046798885,0.00007865866,0.0005093979,0.00004980546,0.009297316],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995254,0.0001803005,0.000024657356,0.00010947214,0.0000693463,0.00009074278],"domain_scores_gemma":[0.9947259,0.0023432046,0.0015542901,0.00043027592,0.0005601603,0.00038622538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016728481,0.00035680187,0.00068261736,0.001098785,0.00055864523,0.0019166378,0.00056164304,0.001703453,0.010771349],"category_scores_gemma":[0.0112717375,0.0003237018,0.0004433936,0.002922566,0.002091553,0.0040357616,0.0013996416,0.0012454328,0.0011832329],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018254714,0.00028859117,0.36949363,0.00095891,0.00062770874,0.0022774434,0.0039961995,0.0036154508,0.0025739444,0.3060295,0.026363991,0.28194916],"study_design_scores_gemma":[0.00013434191,0.00023085265,0.73419315,0.0009953417,0.00024609032,0.0013336035,0.0037256307,0.004481458,0.00038008587,0.18293087,0.07123337,0.000115247734],"about_ca_topic_score_codex":0.003223483,"about_ca_topic_score_gemma":0.0028534187,"teacher_disagreement_score":0.010771349,"about_ca_system_score_codex":0.00058565324,"about_ca_system_score_gemma":0.0005193457,"threshold_uncertainty_score":0.03603381},"labels":[],"label_agreement":null},{"id":"W1645815967","doi":"10.1029/2008gl033573","title":"Impact of the stratosphere on tropospheric climate change","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Scheme for Promotion of Academic and Research Collaboration; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Stratosphere; Atmospheric sciences; Orographic lift; Climatology; Environmental science; Troposphere; Atmospheric circulation; Atmospheric model; Climate model; Orography; Atmospheric models; Meteorology; Climate change; Geology; Physics; Atmosphere (unit); Precipitation","score_opus":0.07502199912536266,"score_gpt":0.3332474461143889,"score_spread":0.2582254469890262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1645815967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964371,0.00030899205,0.0005176195,0.0003899274,0.00003661815,0.0000026349608,0.00040988822,0.00006062832,0.0018366446],"genre_scores_gemma":[0.99943393,0.00012678733,0.00008890436,0.00004360011,0.000007649689,0.0000014013041,0.00017020018,0.0000085320635,0.000119054464],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998209,0.000066307395,0.0000071086965,0.00002609024,0.00002299708,0.000056612673],"domain_scores_gemma":[0.99975926,0.00008804779,0.000030399295,0.000039434944,0.000033263335,0.00004961794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033341828,0.0005102129,0.00027381486,0.00015664233,0.0002647942,0.0007939734,0.00023808499,0.00050561,0.0018575513],"category_scores_gemma":[0.00082487,0.00018749898,0.0005408471,0.00018708379,0.0004354473,0.0005764793,0.00062703027,0.0002654547,0.00015608323],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020801234,0.00015101956,0.27554488,0.0002625319,0.0014720982,0.000716189,0.0002550894,0.5441524,0.12962233,0.005382889,0.0030480342,0.03731256],"study_design_scores_gemma":[0.0002336428,0.0005435664,0.7142421,0.00004069814,0.0008482403,0.0002118143,0.00037186343,0.24821047,0.024506764,0.0051645236,0.0055584707,0.000067802524],"about_ca_topic_score_codex":0.013337712,"about_ca_topic_score_gemma":0.010422129,"teacher_disagreement_score":0.013337712,"about_ca_system_score_codex":0.0005150879,"about_ca_system_score_gemma":0.00042765366,"threshold_uncertainty_score":0.026520133},"labels":[],"label_agreement":null},{"id":"W1646338516","doi":"10.1029/2010gl044018","title":"CO<sub>2</sub> fluxes at northern fens and bogs have opposite responses to inter‐annual fluctuations in water table","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Lethbridge; Trent University","funders":"U.S. Department of Energy","keywords":"Eddy covariance; Bog; Environmental science; Peat; Boreal; Ecosystem; Ecosystem respiration; Water table; Atmospheric sciences; Temperate climate; Ecohydrology; Hydrology (agriculture); Ecology; Sphagnum; Physical geography; Climatology; Geography; Geology; Biology; Groundwater","score_opus":0.013423053849460471,"score_gpt":0.2797368769244641,"score_spread":0.2663138230750036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1646338516","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997497,0.000015151085,0.000028639914,0.000003650461,5.178486e-7,6.6791534e-7,0.00004422422,0.0000018500712,0.00015561076],"genre_scores_gemma":[0.9997173,0.000012580423,0.00006500254,0.000004451141,6.513521e-7,0.000001526573,0.00011806718,0.0000013852257,0.0000790879],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998853,0.000017789478,0.0000056692525,0.00002875174,0.00002126997,0.000041213218],"domain_scores_gemma":[0.99960095,0.000057729438,0.00010284232,0.000022527714,0.000118782875,0.00009721338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020102621,0.00012997889,0.00024072616,0.00040791577,0.00044445685,0.0004145684,0.000121876365,0.00017969118,0.00041943233],"category_scores_gemma":[0.0005047226,0.0001573516,0.00010645739,0.0002969214,0.00034787256,0.00022651881,0.00022745525,0.000104563616,0.00007702842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029911436,0.000033589124,0.9735702,0.000018046663,0.000062811545,0.000081242404,0.00058951933,0.00039794797,0.019620469,0.00005637015,0.0001060726,0.0051646875],"study_design_scores_gemma":[9.4335707e-7,0.000004898665,0.9994703,8.0116513e-7,0.0000023729615,0.000016792534,0.00012421074,0.0001034598,0.00022595243,0.0000073136703,0.000041619078,0.0000014020957],"about_ca_topic_score_codex":0.16050795,"about_ca_topic_score_gemma":0.41333213,"teacher_disagreement_score":0.16050795,"about_ca_system_score_codex":0.0005982327,"about_ca_system_score_gemma":0.0004888417,"threshold_uncertainty_score":0.31914735},"labels":[],"label_agreement":null},{"id":"W1646541019","doi":"10.1029/2012gl053929","title":"Source location of falling tone chorus","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Japan Society for the Promotion of Science; Centre National de la Recherche Scientifique; Centre National d’Etudes Spatiales; National Aeronautics and Space Administration","keywords":"Chorus; Falling (accident); Equator; Tone (literature); Physics; Latitude; Geology; Geophysics; Astronomy; Psychology","score_opus":0.020357882917578746,"score_gpt":0.30826967770157915,"score_spread":0.2879117947840004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1646541019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833693,0.00026038144,0.0066465056,0.000083458006,0.000032061704,0.000031885305,0.00027782773,0.00016216231,0.00913637],"genre_scores_gemma":[0.9984004,0.000046095494,0.00088027917,0.0000057456755,0.000009062115,0.0000051155075,0.00010174667,0.000019900664,0.00053161493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998616,0.000021068352,0.0000071361424,0.000039720377,0.00003710345,0.000033378157],"domain_scores_gemma":[0.99949265,0.00014539866,0.00012617538,0.000049307,0.00010559755,0.00008084169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013301555,0.00022655335,0.00018768196,0.0010495345,0.00044525872,0.00039564457,0.00015951111,0.00015095295,0.0022705593],"category_scores_gemma":[0.0009690427,0.00014363574,0.0001934307,0.0006120136,0.00040712152,0.00030449076,0.0005249027,0.00030138256,0.00022497316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001641539,0.00005625953,0.5312585,0.0003598588,0.00019007822,0.00979954,0.00411261,0.0032210194,0.29844108,0.0077879536,0.0030143326,0.14011714],"study_design_scores_gemma":[0.00004186161,0.00012477704,0.9450681,0.000043876913,0.00011395108,0.0025983523,0.0015069327,0.011514827,0.03312714,0.0020310848,0.0037752804,0.00005373354],"about_ca_topic_score_codex":0.0045388844,"about_ca_topic_score_gemma":0.0031064556,"teacher_disagreement_score":0.0045388844,"about_ca_system_score_codex":0.00018532856,"about_ca_system_score_gemma":0.00018977729,"threshold_uncertainty_score":0.009024978},"labels":[],"label_agreement":null},{"id":"W1647067242","doi":"10.1029/2005gl024446","title":"Scaling of fracture energies: The rationalization of different laboratory measurements","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Wilson Centre; University of Toronto","funders":"","keywords":"Scaling; Geology; Seismology; Fracture (geology); Scaling law; Geophysics; Geotechnical engineering; Geometry; Mathematics","score_opus":0.03960597596709549,"score_gpt":0.2778945243546335,"score_spread":0.23828854838753805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1647067242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8780354,0.001946002,0.108735554,0.00056114857,0.00012182014,0.00011554485,0.00048662367,0.0004960779,0.00950185],"genre_scores_gemma":[0.9926924,0.00025816928,0.006561452,0.00008029243,0.000024700192,0.0000758295,0.00012309387,0.000023505763,0.00016047472],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993656,0.00015200867,0.00003682889,0.00023767307,0.00015199228,0.000055865905],"domain_scores_gemma":[0.99757737,0.0010917286,0.00036297957,0.00066519383,0.00021902549,0.00008371379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014687987,0.0005428536,0.00032293674,0.0008042602,0.00032781236,0.00071919226,0.0010324912,0.0008343795,0.0010631026],"category_scores_gemma":[0.005188765,0.0003413593,0.0003457247,0.00039412113,0.0018544613,0.0011821802,0.0008322495,0.0010244303,0.00021426885],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008993698,0.0008213566,0.06274951,0.00038914703,0.00018883501,0.0009631834,0.000478231,0.030876178,0.7989986,0.053853143,0.0021219845,0.04766048],"study_design_scores_gemma":[0.0001137107,0.0015309008,0.13905333,0.0000751389,0.00011581021,0.0011901202,0.00042180732,0.20632504,0.59736645,0.04842282,0.005165517,0.00021937361],"about_ca_topic_score_codex":0.00039598945,"about_ca_topic_score_gemma":0.00023665513,"teacher_disagreement_score":0.0014687987,"about_ca_system_score_codex":0.0005147284,"about_ca_system_score_gemma":0.00012902016,"threshold_uncertainty_score":0.0077677965},"labels":[],"label_agreement":null},{"id":"W1647484032","doi":"10.1029/2002gl015836","title":"Detecting anthropogenic influence with a multi‐model ensemble","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Department for Environment, Food and Rural Affairs, UK Government; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Aerosol; Environmental science; Greenhouse gas; Scaling; Consistency (knowledge bases); Atmospheric sciences; Climatology; Meteorology; Mathematics; Geology; Physics","score_opus":0.06858393138657572,"score_gpt":0.3178076818658301,"score_spread":0.24922375047925438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1647484032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81053066,0.00030797353,0.18487017,0.00022926243,0.00010921307,0.000049175225,0.0005095841,0.0014835089,0.0019104319],"genre_scores_gemma":[0.95911336,0.00008253939,0.03990863,0.000030185189,0.000031520725,0.000036031972,0.00050592324,0.00007569488,0.0002160995],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99946874,0.0001839056,0.000035538455,0.00013962957,0.000117396245,0.000054877197],"domain_scores_gemma":[0.99871206,0.00047925988,0.00018831187,0.00035595588,0.0002148207,0.000049638533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001565838,0.00073537655,0.0008668916,0.00066627417,0.00040507768,0.0007726063,0.0005112713,0.00041792067,0.0005094009],"category_scores_gemma":[0.0029087632,0.0003354088,0.0010927587,0.00065232214,0.00015676681,0.001148291,0.00079921953,0.0007927298,0.00012277019],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035822898,0.00019926317,0.08719755,0.00007097166,0.0012407941,0.00009001226,0.00012639549,0.7659684,0.020317543,0.0011153937,0.00091062405,0.12240486],"study_design_scores_gemma":[0.000014737885,0.00006834143,0.014434778,0.0000044505937,0.000102613085,0.00001598428,0.000015744934,0.9800062,0.0041875504,0.00060682965,0.00051664293,0.000026169542],"about_ca_topic_score_codex":0.00704224,"about_ca_topic_score_gemma":0.009763211,"teacher_disagreement_score":0.00704224,"about_ca_system_score_codex":0.0003785493,"about_ca_system_score_gemma":0.0005664566,"threshold_uncertainty_score":0.014002502},"labels":[],"label_agreement":null},{"id":"W1648074782","doi":"10.1029/2009gl041780","title":"Depolarized radar return for breaking wave measurement and hurricane wind retrieval","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Breaking wave; Radar; Wind speed; Wind wave; Physics; Scattering; Dissipation; Meteorology; Computational physics; Atmospheric sciences; Geology; Environmental science; Wave propagation; Optics; Aerospace engineering","score_opus":0.04883675546433281,"score_gpt":0.2774457857182247,"score_spread":0.2286090302538919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1648074782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8719632,0.0005352864,0.12293974,0.00012041274,0.0000318519,0.00003574245,0.0004982879,0.00043818704,0.0034372609],"genre_scores_gemma":[0.95081985,0.00020585924,0.04806675,0.0000302413,0.000018762179,0.000016289565,0.00039418123,0.000026836293,0.00042115283],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998062,0.000076414806,0.00000709663,0.000027071836,0.00005645172,0.000026638352],"domain_scores_gemma":[0.9997341,0.00009993144,0.000039966762,0.000049136383,0.000051731346,0.00002520516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004146761,0.00029163132,0.00019935583,0.0005745761,0.000098737204,0.00030815616,0.0001954008,0.00021732818,0.0008305914],"category_scores_gemma":[0.0011012768,0.00017279912,0.000119392,0.0004605047,0.000114050155,0.0002815467,0.0003299869,0.0003025433,0.00036655916],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073716836,0.00017681633,0.056195922,0.00011956623,0.000078700985,0.00026732916,0.00010617245,0.022785366,0.6193818,0.004218478,0.0013755239,0.29455724],"study_design_scores_gemma":[0.0000757247,0.0005444751,0.20820841,0.000032577147,0.00008666113,0.0009370254,0.00019819451,0.58559185,0.19546248,0.0035365163,0.0052227206,0.00010334647],"about_ca_topic_score_codex":0.0005889197,"about_ca_topic_score_gemma":0.00095692003,"teacher_disagreement_score":0.0008305914,"about_ca_system_score_codex":0.00008971501,"about_ca_system_score_gemma":0.00011841477,"threshold_uncertainty_score":0.0027785897},"labels":[],"label_agreement":null},{"id":"W1648755393","doi":"10.1029/2002gl014855","title":"Modeling CFC inventories and formation rates of Labrador Sea Water","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"North Atlantic oscillation; Chlorofluorocarbon; Climatology; Environmental science; Lag; Atmospheric sciences; Oceanography; Geology; Meteorology; Geography","score_opus":0.03958550781850841,"score_gpt":0.26870700636883293,"score_spread":0.22912149855032451,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1648755393","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98199743,0.00008309492,0.011947276,0.00015654022,0.000010648724,0.000030056495,0.002317948,0.0002996335,0.0031574334],"genre_scores_gemma":[0.99390703,0.00005933112,0.004099117,0.000018076496,0.000004604074,0.000032575324,0.0012099388,0.000026630343,0.0006425988],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982256,0.000036734156,0.0000128424845,0.000056667162,0.000032696535,0.00003853111],"domain_scores_gemma":[0.9994373,0.00016833274,0.00014006074,0.000077575976,0.0001311772,0.00004552886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047155784,0.00036042408,0.0002466866,0.00048163687,0.00031599434,0.00071902166,0.00093165465,0.000514028,0.00082919444],"category_scores_gemma":[0.0016615458,0.00047957277,0.00053950015,0.0007205018,0.00032115565,0.00076681946,0.00037295735,0.00045175225,0.00014666465],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059316426,0.000025360334,0.045849998,0.000014215089,0.000050907798,0.000036183443,0.000038206035,0.94737965,0.0010495159,0.0011954444,0.00029545827,0.0040057646],"study_design_scores_gemma":[0.000024152945,0.000012755279,0.009750752,0.0000027550573,0.000013708281,0.000011845203,0.000015288973,0.98845553,0.00080870104,0.00035390267,0.00053864555,0.000012001495],"about_ca_topic_score_codex":0.18578945,"about_ca_topic_score_gemma":0.11576292,"teacher_disagreement_score":0.18578945,"about_ca_system_score_codex":0.0027981035,"about_ca_system_score_gemma":0.0013851376,"threshold_uncertainty_score":0.36941612},"labels":[],"label_agreement":null},{"id":"W1648875851","doi":"10.1029/2009gl042359","title":"Coincident reflection images of the Gulf Stream from seismic and hydrographic data","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"","keywords":"Bathythermograph; Hydrography; Geology; Reflection (computer programming); Sampling (signal processing); Seismology; Remote sensing; Oceanography; Computer science","score_opus":0.030743217916954675,"score_gpt":0.28986583646649466,"score_spread":0.25912261854954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1648875851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99437934,0.00008522865,0.0009877014,0.000028626677,0.000007740154,0.000015243293,0.00093507086,0.00011288959,0.0034481778],"genre_scores_gemma":[0.99139917,0.00016340948,0.006027803,0.000019777197,0.000013665585,0.000008772337,0.0015424112,0.000022817423,0.0008022574],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999232,0.000007983901,0.0000055342434,0.000016735527,0.000032044183,0.000014487644],"domain_scores_gemma":[0.999881,0.000017787179,0.000032331925,0.000016052454,0.00003162871,0.000021252765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013871257,0.00012739799,0.00009890192,0.0009878447,0.000121980534,0.00020411417,0.00016788389,0.00019135392,0.002302074],"category_scores_gemma":[0.00042409977,0.00011134921,0.000108472,0.0007585555,0.00010723088,0.00017186053,0.0002715903,0.00014155652,0.00029001952],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001650697,0.00044769119,0.1684377,0.00039424864,0.0001329769,0.0018274277,0.0010566298,0.009390886,0.5760178,0.001139347,0.003406128,0.2360984],"study_design_scores_gemma":[0.00006826412,0.00030338898,0.9481387,0.000039229206,0.000052831376,0.0011985336,0.0005275359,0.016840542,0.029473485,0.00015528806,0.0031838755,0.000018290362],"about_ca_topic_score_codex":0.0040068855,"about_ca_topic_score_gemma":0.009835282,"teacher_disagreement_score":0.0040068855,"about_ca_system_score_codex":0.00015541879,"about_ca_system_score_gemma":0.00022673619,"threshold_uncertainty_score":0.007967114},"labels":[],"label_agreement":null},{"id":"W1649740783","doi":"10.1029/2011gl048115","title":"Theoretical constraints on pure vapor-pressure driven condensation of organics to ultrafine particles","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Nucleation; Volatility (finance); Condensation; Saturation (graph theory); Range (aeronautics); Gas phase; Materials science; Ultrafine particle; Vapor pressure; Chemical engineering; Chemical physics; Thermodynamics; Chemistry; Nanotechnology; Organic chemistry; Physics; Composite material","score_opus":0.03724300064987859,"score_gpt":0.2694734692323992,"score_spread":0.23223046858252058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1649740783","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3583743,0.005261243,0.21891232,0.011986082,0.0010189565,0.0003164169,0.00393695,0.0006968039,0.3994969],"genre_scores_gemma":[0.9762567,0.0021251203,0.009991892,0.00052857073,0.00062190165,0.00040660775,0.001014339,0.000138767,0.008916077],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9994554,0.000087557215,0.00001724819,0.00009243873,0.0002063229,0.00014095801],"domain_scores_gemma":[0.9957178,0.0030830454,0.00032331044,0.00032249163,0.00035831615,0.00019489479],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014919427,0.0011325959,0.00095134793,0.00084789575,0.0015376697,0.001400127,0.0026009677,0.0018164028,0.01358987],"category_scores_gemma":[0.006932182,0.00063940225,0.00065940403,0.0003661989,0.0019411156,0.0034614375,0.0017069165,0.0010325547,0.0019017943],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000079444835,0.00006844727,0.0012879856,0.00053323543,0.00002417564,0.00030385677,0.00008684903,0.13654186,0.0064420598,0.846849,0.003387092,0.004395995],"study_design_scores_gemma":[0.000084881074,0.000054785574,0.0012461081,0.00005893373,0.000017827639,0.00015886193,0.00005474912,0.5564239,0.0030507892,0.43567732,0.0031174782,0.00005433342],"about_ca_topic_score_codex":0.0025967727,"about_ca_topic_score_gemma":0.0013347638,"teacher_disagreement_score":0.01358987,"about_ca_system_score_codex":0.0015869144,"about_ca_system_score_gemma":0.0010218843,"threshold_uncertainty_score":0.04546261},"labels":[],"label_agreement":null},{"id":"W1653702621","doi":"10.1029/2009gl042030","title":"Sustained rapid shrinkage of Yukon glaciers since the 1957–1958 International Geophysical Year","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Office of Polar Programs; U.S. Geological Survey","keywords":"Glacier; Precipitation; Geology; Climatology; Water equivalent; Sea level; Physical geography; Environmental science; Oceanography; Snow; Geomorphology; Meteorology; Geography","score_opus":0.02488073552605034,"score_gpt":0.27987183701363383,"score_spread":0.25499110148758347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1653702621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99720025,0.00020794319,0.00009406088,0.00008483701,0.0000062235017,0.0000025469371,0.00038287003,0.000012761189,0.0020084693],"genre_scores_gemma":[0.9991154,0.0000988013,0.0000598193,0.000013970384,0.0000024871044,0.0000014026701,0.00030011113,0.0000024485664,0.0004055619],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.000005076929,0.000007829591,0.000025931395,0.000019911531,0.00003411795],"domain_scores_gemma":[0.99968076,0.000014164254,0.00010650367,0.000034199868,0.00012974117,0.000034543424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018194108,0.00018886264,0.00014240795,0.00045081077,0.0005751232,0.0005735097,0.000254169,0.0001578948,0.00094056915],"category_scores_gemma":[0.00071504776,0.00009452082,0.00014433857,0.00081452343,0.0006297313,0.00041136687,0.00054207025,0.00022793352,0.00016295488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007935435,0.000010542708,0.96086854,0.000036487214,0.000054885488,0.00017802141,0.0008420102,0.000837958,0.0056391726,0.0004638117,0.00094014406,0.030049024],"study_design_scores_gemma":[0.0000011539906,0.000007574876,0.9972959,0.0000038166604,0.000008624518,0.000056116558,0.00025194182,0.00014911321,0.00027687976,0.00003873932,0.0019075255,0.0000026497182],"about_ca_topic_score_codex":0.22989234,"about_ca_topic_score_gemma":0.43701583,"teacher_disagreement_score":0.7701076,"about_ca_system_score_codex":0.0019462579,"about_ca_system_score_gemma":0.0014103552,"threshold_uncertainty_score":0.45710844},"labels":[],"label_agreement":null},{"id":"W1655224201","doi":"10.1029/2008gl037020","title":"Mountain glaciers and ice caps around Antarctica make a large sea‐level rise contribution","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":181,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Future sea level; Glacier; Sea level rise; Ice caps; Peninsula; Sea level; Climate change; Global warming; Climatology; Ice sheet; Antarctic ice sheet; Environmental science; Geology; Global change; Atmospheric sciences; Ice stream; Oceanography; Physical geography; Sea ice; Cryosphere; Geography","score_opus":0.039418844196503836,"score_gpt":0.2969090002303865,"score_spread":0.2574901560338827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1655224201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96448296,0.0031102027,0.0032802827,0.0009990521,0.00016150414,0.000025289892,0.0072176377,0.00038539906,0.020337654],"genre_scores_gemma":[0.99254614,0.0011485823,0.0009509078,0.00007849371,0.00005969625,0.000008491432,0.0026821126,0.000035359513,0.00249018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.0000094335755,0.000004467177,0.000012477248,0.000033907912,0.000019511175],"domain_scores_gemma":[0.9998907,0.000013818906,0.000039354312,0.000009323342,0.000034713437,0.000012115388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010687411,0.00042324234,0.0002441234,0.0006035253,0.00027447144,0.00081703387,0.00019326237,0.0002025392,0.0030809946],"category_scores_gemma":[0.00033662884,0.00019277778,0.00040917352,0.0012517913,0.00018650174,0.0003534853,0.0004767601,0.0003345349,0.00055720384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001932433,0.00004856568,0.7566132,0.0002852801,0.0007108779,0.0005745076,0.00047180834,0.056610066,0.009532713,0.004449978,0.010888772,0.15962107],"study_design_scores_gemma":[0.000036243895,0.00006645991,0.90168273,0.00006388803,0.00023299329,0.0005577781,0.00056982896,0.018489936,0.002952484,0.0020377648,0.07327577,0.000034110388],"about_ca_topic_score_codex":0.01693882,"about_ca_topic_score_gemma":0.018342335,"teacher_disagreement_score":0.01693882,"about_ca_system_score_codex":0.000354023,"about_ca_system_score_gemma":0.00041058447,"threshold_uncertainty_score":0.03368044},"labels":[],"label_agreement":null},{"id":"W1656460106","doi":"10.1029/2003gl016929","title":"Nonlinear acceleration of dispersive effects in field line resonances","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plasma Diagnostics and Applications","field":"Engineering","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Nonlinear system; Physics; Computational physics; Acceleration; Dispersion (optics); Alfvén wave; Dipole; Perpendicular; Field line; Magnetic field; Field (mathematics); Geophysics; Mechanics; Classical mechanics; Optics; Geometry; Magnetohydrodynamics","score_opus":0.0215127472768493,"score_gpt":0.3005288754108525,"score_spread":0.27901612813400317,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1656460106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93752205,0.00010535494,0.055924896,0.000092587245,0.000011195927,0.000016516125,0.000030860014,0.00020857435,0.0060879565],"genre_scores_gemma":[0.99240017,0.000048363592,0.0065641073,0.0000066467505,0.000004337424,0.0000068676495,0.00001534548,0.000024008774,0.0009300556],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999634,0.000008621647,0.0000010816501,0.000006441976,0.000013738202,0.0000067631504],"domain_scores_gemma":[0.9998085,0.00009054413,0.000045486653,0.000019269484,0.000020644038,0.00001559559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096099575,0.00021221371,0.000102043996,0.00013345666,0.00021067185,0.00025069967,0.0001948633,0.00024919736,0.000786279],"category_scores_gemma":[0.00053346576,0.00016520119,0.00013308597,0.00007703885,0.0003930632,0.00031642933,0.000377626,0.00022967701,0.00016994093],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025792935,0.00008442467,0.009821524,0.000087800065,0.000027867474,0.0005598138,0.0006127823,0.4705662,0.4774446,0.016553305,0.0004776629,0.02350609],"study_design_scores_gemma":[0.0000135557775,0.000039271803,0.0018470843,0.0000034939542,0.0000029185705,0.00010301972,0.000032538315,0.9806476,0.015344258,0.001394479,0.0005604451,0.000011216055],"about_ca_topic_score_codex":0.0010906128,"about_ca_topic_score_gemma":0.00085819175,"teacher_disagreement_score":0.0010906128,"about_ca_system_score_codex":0.00022352971,"about_ca_system_score_gemma":0.000116812145,"threshold_uncertainty_score":0.002630353},"labels":[],"label_agreement":null},{"id":"W1656703508","doi":"10.1029/2004gl019438","title":"Shear‐wave splitting observations in the lower Great Lakes region: Evidence for regional anisotropic domains and keel‐modified asthenospheric flow","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; Western University","funders":"","keywords":"Shear wave splitting; Geology; Lithosphere; Seismic anisotropy; Seismology; Rift; Geophysics; Keel; Asthenosphere; Anisotropy; Mantle (geology); Tectonics; Crust; Shear (geology); Seismometer; Geodesy; Petrology; Physics","score_opus":0.13849138688641938,"score_gpt":0.3107166644583459,"score_spread":0.17222527757192652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1656703508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999866,0.000008310688,0.000015864607,0.0000045132833,1.0007763e-7,3.5390167e-7,0.00002611833,0.0000014096777,0.000077375575],"genre_scores_gemma":[0.9997131,0.00001955698,0.00008535542,0.0000023717482,0.0000012714233,0.0000016803975,0.000108264554,0.0000010017131,0.00006721158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999542,0.0000074919703,0.000003293612,0.000009476719,0.000011368669,0.000014090985],"domain_scores_gemma":[0.9998573,0.000025289752,0.000053960983,0.000011269856,0.000022535512,0.00002957805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008268484,0.0001155342,0.00009338116,0.0005370695,0.0002065607,0.00028809372,0.00010168732,0.00011854468,0.00029790902],"category_scores_gemma":[0.0003019627,0.00014710303,0.00006708648,0.0005233722,0.00031128107,0.00018293959,0.00024695863,0.00009990745,0.0000608007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017902478,0.0000205772,0.9171246,0.00002230458,0.00004635145,0.00024189387,0.0015499325,0.0006510299,0.07248539,0.00009765067,0.00013077374,0.007450398],"study_design_scores_gemma":[0.000003567342,0.000007891837,0.9986877,9.708278e-7,0.000004976157,0.00003228425,0.00009069181,0.0003822864,0.000694396,0.000012232667,0.00008100532,0.0000020709433],"about_ca_topic_score_codex":0.027725317,"about_ca_topic_score_gemma":0.059478763,"teacher_disagreement_score":0.027725317,"about_ca_system_score_codex":0.00021918652,"about_ca_system_score_gemma":0.00020859709,"threshold_uncertainty_score":0.05512786},"labels":[],"label_agreement":null},{"id":"W1656843456","doi":"10.1029/2007gl030689","title":"Mobilization pathways of organic carbon from permafrost to arctic rivers in a changing climate","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":304,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Permafrost; Dissolved organic carbon; Total organic carbon; Soil carbon; Arctic; Environmental science; Subarctic climate; Hydrology (agriculture); Leaching (pedology); Geology; Oceanography; Environmental chemistry; Soil water; Soil science; Chemistry","score_opus":0.04957383520562827,"score_gpt":0.28782465820331465,"score_spread":0.23825082299768638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1656843456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99734855,0.00064326223,0.00035614448,0.000115602,0.0000038906733,0.0000046083414,0.00010329759,0.000014049482,0.0014105198],"genre_scores_gemma":[0.9968786,0.0010426062,0.00082507177,0.00008052921,0.0000067195183,0.000010342744,0.00023466593,0.000007978104,0.0009134045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999161,0.000014932806,0.0000056363106,0.000024890398,0.000013261742,0.000025231322],"domain_scores_gemma":[0.99986446,0.000023769908,0.000047464364,0.000006852833,0.000030613868,0.000026798449],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021934207,0.00019022152,0.00017011247,0.00065463234,0.0008255832,0.00076737354,0.00016402412,0.00021576892,0.0008766764],"category_scores_gemma":[0.00021023299,0.00023468182,0.00014548976,0.00042079296,0.0003575522,0.00040535058,0.0004116567,0.0001979787,0.00014144952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006521493,0.00011363001,0.6342137,0.0002565419,0.00017573399,0.0008668221,0.0018556624,0.0022440352,0.29353184,0.0029307941,0.00052372593,0.06263551],"study_design_scores_gemma":[0.0000141195815,0.00008116553,0.9810847,0.00003404314,0.00004649805,0.00024821993,0.00148284,0.0019152372,0.009521829,0.0010593672,0.0044905846,0.00002138848],"about_ca_topic_score_codex":0.01141983,"about_ca_topic_score_gemma":0.030952014,"teacher_disagreement_score":0.01141983,"about_ca_system_score_codex":0.0008312279,"about_ca_system_score_gemma":0.0009676979,"threshold_uncertainty_score":0.022706747},"labels":[],"label_agreement":null},{"id":"W1658122803","doi":"10.1029/2011gl049784","title":"Arctic winter 2010/2011 at the brink of an ozone hole","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ozone depletion; Ozone; Stratosphere; Atmospheric sciences; Polar vortex; Environmental science; Ozone layer; Arctic; Montreal Protocol; Climatology; Meteorology; Geology; Oceanography; Physics","score_opus":0.05455259238799963,"score_gpt":0.27655275574708255,"score_spread":0.2220001633590829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1658122803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9753283,0.0008211019,0.00081805943,0.0016386478,0.00069286785,0.00002206956,0.00903646,0.00015966262,0.011482742],"genre_scores_gemma":[0.9847093,0.00042856723,0.0010823386,0.0005477988,0.00019674067,0.000016602015,0.00726328,0.00005016009,0.0057052756],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998976,0.000010122836,0.0000039424735,0.000023685994,0.000029763567,0.000034818386],"domain_scores_gemma":[0.99987125,0.0000045663473,0.000020798707,0.000010721931,0.000045708897,0.000047013596],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003744608,0.00031003953,0.0002503576,0.00038470572,0.001652756,0.0008781867,0.0001800347,0.00060206425,0.001293227],"category_scores_gemma":[0.00024971418,0.00011663894,0.00022379757,0.0003875936,0.00020471508,0.0003111333,0.00062666106,0.00047889326,0.00039902763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0039674914,0.00047368367,0.7214791,0.0005823176,0.0006055777,0.0033661115,0.0027146775,0.014310497,0.07333383,0.00696017,0.10339736,0.06880924],"study_design_scores_gemma":[0.000049312086,0.00016039741,0.92654204,0.00006350981,0.000094121715,0.00014876114,0.00090470834,0.0028914094,0.0050793383,0.00049408,0.06354016,0.000032072265],"about_ca_topic_score_codex":0.15495136,"about_ca_topic_score_gemma":0.36423022,"teacher_disagreement_score":0.15495136,"about_ca_system_score_codex":0.0015748342,"about_ca_system_score_gemma":0.0014667301,"threshold_uncertainty_score":0.3080989},"labels":[],"label_agreement":null},{"id":"W1658326591","doi":"10.1029/2005gl024693","title":"Simulation and inversion of borehole temperature profiles in surrogate climates: Spatial distribution and surface coupling","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":163,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Borehole; Inversion (geology); Geology; Thermal conduction; Perturbation (astronomy); Climatology; Geophysics; Geomorphology; Physics; Geotechnical engineering; Structural basin; Thermodynamics","score_opus":0.03735630839740782,"score_gpt":0.294669310172661,"score_spread":0.2573130017752532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1658326591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98635453,0.00002349059,0.012269597,0.0001006436,0.00001711792,0.000019407507,0.0003389082,0.00019136886,0.000684886],"genre_scores_gemma":[0.99749327,0.000011328452,0.0021793703,0.0000061073556,0.0000023200923,0.000011907949,0.00018595696,0.000008524751,0.00010122819],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997942,0.0000826038,0.000012263892,0.000034330704,0.000029212828,0.00004742108],"domain_scores_gemma":[0.99884844,0.0006980437,0.00011529305,0.00010332082,0.00013347265,0.00010147675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008905457,0.0005025338,0.00038894592,0.00030961,0.00032485617,0.00052679935,0.0007791485,0.0009818587,0.0007103186],"category_scores_gemma":[0.00292257,0.0003609259,0.0004930226,0.0004957816,0.00070668233,0.0007700957,0.0005505636,0.0006630645,0.000062265426],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013079189,0.00006355138,0.004598769,0.000009021336,0.000014179093,0.00004491656,0.00003185359,0.9921405,0.0012291232,0.0005509804,0.00009155038,0.001094866],"study_design_scores_gemma":[0.000024681125,0.00002433693,0.0008073897,6.3549766e-7,0.0000025588263,0.000004283369,0.00000853375,0.9985006,0.00046187235,0.00013467105,0.000026414918,0.0000040555437],"about_ca_topic_score_codex":0.020488564,"about_ca_topic_score_gemma":0.01092816,"teacher_disagreement_score":0.020488564,"about_ca_system_score_codex":0.0006230064,"about_ca_system_score_gemma":0.00083260215,"threshold_uncertainty_score":0.040738583},"labels":[],"label_agreement":null},{"id":"W1659081628","doi":"10.1029/2001gl014386","title":"Substorm onset times as derived from geomagnetic indices","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; University of Saskatchewan","funders":"","keywords":"Substorm; Ionosphere; Magnetosphere; Earth's magnetic field; Atmospheric sciences; Physics; Geomagnetic storm; Climatology; Geophysics; Geology; Magnetic field","score_opus":0.017785541744054435,"score_gpt":0.2676280149619172,"score_spread":0.24984247321786274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1659081628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95945567,0.0005367913,0.029554116,0.000036937847,0.000031665204,0.000050591967,0.0018976196,0.00032806164,0.008108604],"genre_scores_gemma":[0.99291915,0.00016611225,0.005214656,0.000006731634,0.000014764363,0.000021471495,0.0011171063,0.000028432958,0.00051162543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990356,0.000009397447,0.000013465574,0.000023965156,0.000028811608,0.000020738255],"domain_scores_gemma":[0.9992778,0.0001899655,0.00024802555,0.000055576125,0.00014637415,0.00008232966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028516454,0.0001994758,0.00014567174,0.0011063752,0.00015776567,0.0003931239,0.00011418105,0.0001228709,0.0010197258],"category_scores_gemma":[0.0016807993,0.00011196793,0.000117348696,0.0006959846,0.0001319233,0.00044883834,0.0002722304,0.00027300388,0.00028040688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077218685,0.000048303347,0.6280096,0.00026004665,0.00009244189,0.0004531027,0.0006934584,0.009261551,0.16905606,0.0074425717,0.0024135455,0.18149708],"study_design_scores_gemma":[0.000019161067,0.000099323726,0.94060796,0.000022282875,0.00004331971,0.00061865075,0.00012120427,0.028906377,0.02133236,0.0021991467,0.0059972554,0.000032994514],"about_ca_topic_score_codex":0.0011393429,"about_ca_topic_score_gemma":0.0023648422,"teacher_disagreement_score":0.0011393429,"about_ca_system_score_codex":0.00022003015,"about_ca_system_score_gemma":0.00014444182,"threshold_uncertainty_score":0.003411293},"labels":[],"label_agreement":null},{"id":"W1659589290","doi":"10.1029/2010gl044413","title":"Sodium ion exosphere of Mercury during MESSENGER flybys","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Exosphere; Planet; Solar wind; Mercury (programming language); Astrobiology; Spacecraft; Physics; Geophysics; Ion; Magnetic field; Astronomy","score_opus":0.022137008642150846,"score_gpt":0.2855318189879002,"score_spread":0.26339481034574935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1659589290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99973994,0.000009509114,0.000018658111,0.000009597615,6.000054e-7,6.4314855e-7,0.00003575645,0.0000033259919,0.00018181965],"genre_scores_gemma":[0.9996612,0.000010554935,0.00003397269,0.0000043929917,0.0000012600086,0.0000010505009,0.0001239457,0.0000013371763,0.00016233622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999795,0.000002215295,5.4251853e-7,0.000004929958,0.0000060199127,0.0000068020895],"domain_scores_gemma":[0.9999411,0.000010757197,0.000015735743,0.0000051329966,0.000010015457,0.000017223492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006542139,0.00013310005,0.00016782868,0.00019367246,0.00026065324,0.00022181998,0.00012362022,0.000252193,0.00043936816],"category_scores_gemma":[0.00022862239,0.00008801087,0.00011131386,0.00011857996,0.00013923255,0.00016186389,0.00032565245,0.00017464723,0.0000766417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026723603,0.0001434767,0.61411685,0.000053503813,0.000178561,0.0015108351,0.001970633,0.006478285,0.35596478,0.00045287848,0.0009827648,0.015475146],"study_design_scores_gemma":[0.000023118975,0.00018208327,0.9886395,0.0000063272155,0.000022189348,0.000110134286,0.0002934926,0.0040708557,0.0059331404,0.00006803033,0.000639441,0.000011762589],"about_ca_topic_score_codex":0.015045681,"about_ca_topic_score_gemma":0.028519668,"teacher_disagreement_score":0.015045681,"about_ca_system_score_codex":0.00049611065,"about_ca_system_score_gemma":0.00016932079,"threshold_uncertainty_score":0.029916167},"labels":[],"label_agreement":null},{"id":"W1659598892","doi":"10.1029/2010gl043985","title":"Biophysical feedbacks between the Pleistocene megafauna extinction and climate: The first human‐induced global warming?","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Beringia; Megafauna; Extinction (optical mineralogy); Pleistocene; Herbivore; Climate change; Global warming; Ecology; Environmental science; Physical geography; Geology; Geography; Biology; Paleontology","score_opus":0.03496911554982369,"score_gpt":0.31041727729708174,"score_spread":0.27544816174725806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1659598892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933727,0.00075334014,0.0005526802,0.0026160923,0.00007786065,0.000010831329,0.00030859487,0.00010011712,0.0022079828],"genre_scores_gemma":[0.9990896,0.00023574171,0.000103119135,0.00016283987,0.000031776424,0.0000033458969,0.00005192915,0.00000846807,0.00031310297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999186,0.000023452882,0.0000042141314,0.000019848832,0.0000073108545,0.000026714873],"domain_scores_gemma":[0.99964726,0.00009423902,0.00008090804,0.000023530542,0.000046263147,0.00010776053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003883083,0.00037058792,0.00038975655,0.0003452407,0.00046643752,0.001266281,0.00027367103,0.0010275807,0.0050294446],"category_scores_gemma":[0.0016198917,0.00045671733,0.00034290698,0.00021758217,0.000454482,0.00076540967,0.0006576286,0.00056248927,0.0002829344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007849713,0.0005546382,0.8587438,0.00039110225,0.0007528807,0.00096832385,0.0010118101,0.04325152,0.038471222,0.0066911243,0.006200823,0.042177707],"study_design_scores_gemma":[0.000068483794,0.00012153935,0.9629311,0.000035733454,0.00021290904,0.00017650762,0.0006722989,0.0274483,0.0011552632,0.0040955795,0.0030308363,0.000051501487],"about_ca_topic_score_codex":0.009959167,"about_ca_topic_score_gemma":0.014889813,"teacher_disagreement_score":0.009959167,"about_ca_system_score_codex":0.00080528366,"about_ca_system_score_gemma":0.0004054758,"threshold_uncertainty_score":0.019802392},"labels":[],"label_agreement":null},{"id":"W1659833838","doi":"10.1029/2010gl042793","title":"Twentieth century bipolar seesaw of the Arctic and Antarctic surface air temperatures","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Seesaw molecular geometry; Arctic; Climatology; Arctic geoengineering; Environmental science; Arctic vegetation; North Atlantic oscillation; Arctic dipole anomaly; Arctic oscillation; Atlantic multidecadal oscillation; Arctic ecology; Climate change; Global warming; Oceanography; Arctic ice pack; Geology; Tundra; Northern Hemisphere; Antarctic sea ice","score_opus":0.016278936628568944,"score_gpt":0.2732692924483728,"score_spread":0.25699035581980384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1659833838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9848555,0.0011432101,0.0010453708,0.0006789101,0.000066055385,0.000006864191,0.0008224102,0.000025083922,0.011356553],"genre_scores_gemma":[0.9976203,0.0005913869,0.00029597856,0.0000676144,0.000025151245,0.0000043641003,0.00032164317,0.0000042218107,0.001069455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.0000056863105,0.000003802471,0.00001881989,0.000010053023,0.00001215865],"domain_scores_gemma":[0.9998272,0.00001611632,0.00007203036,0.000014642706,0.000052531297,0.000017532111],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018041911,0.00008266316,0.0000489702,0.00046247285,0.00019208257,0.00058419065,0.00008877581,0.00017511129,0.00090060587],"category_scores_gemma":[0.00076752494,0.000061701474,0.00008720021,0.00055799127,0.00026973337,0.0003652744,0.00037856068,0.00018939769,0.00012354857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046351174,0.000030340567,0.8869196,0.00011114324,0.00013532575,0.00042201293,0.0017547796,0.002411165,0.016148007,0.020085968,0.0030015688,0.068516634],"study_design_scores_gemma":[0.000003846488,0.000027093758,0.9867539,0.000013146793,0.000016290109,0.0001484581,0.00024779793,0.00071246555,0.0008050616,0.0013925002,0.009873628,0.0000057591556],"about_ca_topic_score_codex":0.0056823823,"about_ca_topic_score_gemma":0.01026695,"teacher_disagreement_score":0.0056823823,"about_ca_system_score_codex":0.00035138833,"about_ca_system_score_gemma":0.00023778374,"threshold_uncertainty_score":0.011298597},"labels":[],"label_agreement":null},{"id":"W1660021593","doi":"10.1029/2009gl038802","title":"A large‐aperture sodium fluorescence lidar with very high resolution for mesopause dynamics and adaptive optics studies","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Mesopause; Thermosphere; Lidar; Mesosphere; Spectral density; Turbulence; Physics; Gravity wave; Intermittency; Optics; Atmospheric sciences; Computational physics; Geophysics; Meteorology; Wave propagation; Ionosphere","score_opus":0.017078993609182063,"score_gpt":0.28388620543423265,"score_spread":0.26680721182505057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1660021593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9038667,0.00057292037,0.08269082,0.0009381966,0.00010131421,0.00017519754,0.00063364574,0.0004580221,0.01056315],"genre_scores_gemma":[0.90841436,0.00011367974,0.087750286,0.00016008434,0.00004927455,0.00007733765,0.00031593218,0.000033234664,0.0030857963],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99974364,0.00003848037,0.0000050439075,0.00005724276,0.00011382909,0.000041841577],"domain_scores_gemma":[0.9997726,0.000046592184,0.000019338158,0.000028845552,0.00007579778,0.0000568386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005017995,0.00019753598,0.00025786427,0.00037835538,0.00058758946,0.000235167,0.0005642169,0.00044149254,0.001051947],"category_scores_gemma":[0.0003149447,0.0002020094,0.00022839951,0.00031326863,0.0002997155,0.0007141617,0.0005611417,0.00034834212,0.0001812217],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018853725,0.00015612574,0.009440619,0.000046555822,0.000020061907,0.00022944904,0.00025113055,0.001311673,0.9551061,0.0021665206,0.00104379,0.03003946],"study_design_scores_gemma":[0.00052161055,0.0033112124,0.11136028,0.00008643016,0.00012383018,0.0052786786,0.00077303645,0.22104163,0.5911201,0.0063844346,0.059675775,0.00032305266],"about_ca_topic_score_codex":0.0020948697,"about_ca_topic_score_gemma":0.0044036824,"teacher_disagreement_score":0.0020948697,"about_ca_system_score_codex":0.0003945647,"about_ca_system_score_gemma":0.000571621,"threshold_uncertainty_score":0.0041653514},"labels":[],"label_agreement":null},{"id":"W1660805619","doi":"10.1029/2011gl048270","title":"Forearc extension and slow rollback of the Calabrian Arc from GPS measurements","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Geology; Subduction; Forearc; Seismology; Reference frame; Geodesy; Foreland basin; Trench; Arc (geometry); Wedge (geometry); Global Positioning System; Tectonics; Geometry; Frame (networking)","score_opus":0.11975863308516788,"score_gpt":0.27659058052849655,"score_spread":0.15683194744332868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1660805619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97451615,0.0015379034,0.0044248067,0.00013467224,0.000031496467,0.000044773406,0.0071193227,0.00022332904,0.011967551],"genre_scores_gemma":[0.98889685,0.0004389573,0.0037780772,0.00001810496,0.000020142068,0.000016198612,0.0060075363,0.000020026951,0.0008042534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998227,0.000022109198,0.000010874234,0.000067311186,0.00005287141,0.000024125015],"domain_scores_gemma":[0.99967265,0.000041131665,0.00009508397,0.000045842866,0.00012156044,0.000023745886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025675955,0.0003416792,0.00014498246,0.0016406267,0.00021902399,0.0005925388,0.0003007904,0.00019038282,0.0018254165],"category_scores_gemma":[0.0014935012,0.0001306829,0.00011136834,0.001925223,0.0001636467,0.00018648253,0.00040167055,0.00028641985,0.00041113005],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012965906,0.000015690655,0.87437385,0.000084063795,0.000051990723,0.000113220034,0.0007081036,0.0040052924,0.005651657,0.00028181286,0.0019871313,0.11259753],"study_design_scores_gemma":[0.00000575352,0.000013640346,0.9953151,0.0000147086985,0.00000967535,0.000035780897,0.00009688504,0.001200275,0.00022092453,0.000053904696,0.0030297185,0.0000036186188],"about_ca_topic_score_codex":0.14188479,"about_ca_topic_score_gemma":0.23149994,"teacher_disagreement_score":0.14188479,"about_ca_system_score_codex":0.0006512291,"about_ca_system_score_gemma":0.0003347107,"threshold_uncertainty_score":0.2821179},"labels":[],"label_agreement":null},{"id":"W1660905893","doi":"10.1029/2010gl045453","title":"Observations of internal wave packets propagating along-shelf in northern Monterey Bay","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Gordon and Betty Moore Foundation; David and Lucile Packard Foundation","keywords":"Thermocline; Geology; Bay; Internal wave; Oceanography; Upwelling; Isopycnal; Amplitude; Wave packet; Continental shelf; Physics","score_opus":0.07843884967458603,"score_gpt":0.2666170506952908,"score_spread":0.18817820102070476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1660905893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99940777,0.00002368889,0.00003359714,0.00000888825,0.0000011164761,0.0000028896566,0.00011967458,0.0000044543613,0.00039804215],"genre_scores_gemma":[0.9990841,0.00006197651,0.00019775864,0.000013076714,0.0000018782357,0.000004313896,0.0002087477,0.0000014912664,0.00042661332],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994373,0.0000036898844,0.0000041028966,0.000013547201,0.000021266587,0.0000137009565],"domain_scores_gemma":[0.99968076,0.000025358408,0.000102919126,0.00001671979,0.000088900706,0.00008530635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011943776,0.0001309887,0.00012576839,0.0003273489,0.0003601237,0.00030862217,0.00016425122,0.00014904412,0.00040046673],"category_scores_gemma":[0.00034774156,0.00016228363,0.00008716363,0.00034181133,0.00025016314,0.00014642863,0.00035948603,0.00017813368,0.00008917943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017653836,0.000046668836,0.95624655,0.000041871117,0.00003569819,0.0002753011,0.0023953535,0.00028688856,0.028639583,0.000045206594,0.000467424,0.0113428645],"study_design_scores_gemma":[0.0000017922005,0.000012827429,0.99929154,0.000003044969,0.0000049469713,0.00001751216,0.00014728523,0.000121935955,0.00024509794,0.0000024407095,0.00014987827,0.0000017522076],"about_ca_topic_score_codex":0.21327443,"about_ca_topic_score_gemma":0.4625766,"teacher_disagreement_score":0.21327443,"about_ca_system_score_codex":0.00096172537,"about_ca_system_score_gemma":0.0005596952,"threshold_uncertainty_score":0.42406607},"labels":[],"label_agreement":null},{"id":"W1661375993","doi":"10.1029/2010gl044317","title":"Lidar measurements of clouds in the planetary boundary layer on Mars","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency; University of Arizona; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Lidar; Mars Exploration Program; Atmospheric sciences; Environmental science; Planetary boundary layer; Cloud physics; Liquid water content; Atmosphere of Mars; Boundary layer; Liquid water; Meteorology; Geology; Astrobiology; Remote sensing; Cloud computing; Physics; Martian","score_opus":0.044964255850712016,"score_gpt":0.3029329167165012,"score_spread":0.2579686608657892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1661375993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938168,0.00026106884,0.0012283331,0.000071028255,0.0000126797195,0.000015626722,0.0015530844,0.00008205898,0.002959329],"genre_scores_gemma":[0.9947708,0.00012877438,0.0031071363,0.000036428566,0.00001459942,0.000015143485,0.0013311103,0.000009872462,0.00058617967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985623,0.000019649204,0.0000060020316,0.000032189597,0.000055173918,0.000030742052],"domain_scores_gemma":[0.9998092,0.000028833792,0.00003761378,0.000015739834,0.000069731446,0.00003884128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022615345,0.00014314285,0.00015569052,0.00076811836,0.00036986865,0.0003839369,0.00029640694,0.00036686892,0.0007840224],"category_scores_gemma":[0.00043254532,0.00014717935,0.00011839433,0.0006081554,0.00006537399,0.0003584529,0.00036213978,0.00033334075,0.0001799386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005531776,0.00029352645,0.5227631,0.00019262506,0.00021607493,0.00046836582,0.0015601135,0.010534335,0.38605386,0.0011926658,0.004916827,0.07125532],"study_design_scores_gemma":[0.00011821709,0.0002595222,0.9091966,0.00006240145,0.00008899425,0.00034249126,0.0005720367,0.030971356,0.046070818,0.0004006816,0.011866625,0.000050236074],"about_ca_topic_score_codex":0.0037794597,"about_ca_topic_score_gemma":0.004375622,"teacher_disagreement_score":0.0037794597,"about_ca_system_score_codex":0.00020065146,"about_ca_system_score_gemma":0.00011824968,"threshold_uncertainty_score":0.0075149536},"labels":[],"label_agreement":null},{"id":"W1661505871","doi":"10.1029/2005gl023643","title":"Enhanced vertical propagation of storm‐induced near‐inertial energy in an eddying ocean channel model","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Mesoscale meteorology; Inertial wave; Storm; Geology; Eddy; Anticyclone; Inertial frame of reference; Storm track; Climatology; Meteorology; Oceanography; Turbulence; Physics; Wave propagation","score_opus":0.03350987017202957,"score_gpt":0.2792134175760214,"score_spread":0.24570354740399186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1661505871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98432803,0.00014163226,0.008624745,0.0004007325,0.00003727631,0.00002423981,0.0007453364,0.00018478515,0.0055132178],"genre_scores_gemma":[0.99544394,0.00012752211,0.0015155497,0.000028637625,0.000019365143,0.000025098434,0.0003052167,0.00003932866,0.0024953124],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990535,0.000026584295,0.0000043345553,0.000020328394,0.000011961244,0.000031479678],"domain_scores_gemma":[0.9994174,0.0002550318,0.00009991599,0.00003182197,0.00007435273,0.000121421086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032215012,0.00060075364,0.0006508472,0.0003719621,0.0007056153,0.0011432944,0.0011263448,0.0015672536,0.0020442428],"category_scores_gemma":[0.0009047458,0.00049582106,0.0005614404,0.0004771797,0.0008466165,0.000856244,0.0007333317,0.0008325244,0.0001489819],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096642514,0.000051614246,0.0027537153,0.000013465085,0.000019717392,0.000065351946,0.000030950312,0.9923408,0.0011498379,0.0027103457,0.00023211274,0.00053543516],"study_design_scores_gemma":[0.000025934576,0.000014336127,0.000420355,0.0000013420535,0.000005956539,0.000002956024,0.000008284067,0.99912995,0.00008778751,0.00024147406,0.00005652102,0.0000050906096],"about_ca_topic_score_codex":0.0734238,"about_ca_topic_score_gemma":0.03532674,"teacher_disagreement_score":0.0734238,"about_ca_system_score_codex":0.0013210418,"about_ca_system_score_gemma":0.0014897918,"threshold_uncertainty_score":0.14599288},"labels":[],"label_agreement":null},{"id":"W1661733002","doi":"10.1029/2012gl051832","title":"The spatial extent of source influences on modeled column concentrations of short‐lived species","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Dalhousie University","funders":"","keywords":"Column (typography); Environmental science; Sulfur dioxide; Atmospheric sciences; Nitrogen dioxide; Satellite; Meteorology; Geology; Chemistry; Computer science; Physics","score_opus":0.04748715631314364,"score_gpt":0.28794027578420367,"score_spread":0.24045311947106002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1661733002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99131525,0.000104858416,0.005524605,0.00012587932,0.00001267751,0.000008561588,0.00079961703,0.00017288924,0.0019357101],"genre_scores_gemma":[0.9985403,0.0000417454,0.0008597026,0.00001602014,0.0000034751938,0.0000054484053,0.00034683652,0.00001987561,0.00016666771],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999915,0.000015016204,0.0000057207626,0.000028929893,0.000015167021,0.000020135163],"domain_scores_gemma":[0.99971646,0.00014354182,0.00003177766,0.000041980886,0.000045964036,0.000020124562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027867718,0.00032905166,0.00023879157,0.00018827253,0.00031166413,0.0004850751,0.0004971687,0.00040685572,0.0009229617],"category_scores_gemma":[0.00065445737,0.00024011481,0.00068247394,0.00024180251,0.00025816538,0.00069093873,0.00040615044,0.00053166266,0.00010020169],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016289673,0.000098904704,0.08573241,0.000068887835,0.00016617008,0.000104982726,0.00006683406,0.8717381,0.03274484,0.0015087619,0.00044621038,0.00716103],"study_design_scores_gemma":[0.000039778137,0.000036069705,0.04629862,0.000012006624,0.0000528485,0.00001804785,0.00005332592,0.9414862,0.010818176,0.00071420777,0.00044587205,0.000024820056],"about_ca_topic_score_codex":0.03469304,"about_ca_topic_score_gemma":0.032098092,"teacher_disagreement_score":0.03469304,"about_ca_system_score_codex":0.00062717404,"about_ca_system_score_gemma":0.0007001444,"threshold_uncertainty_score":0.068982184},"labels":[],"label_agreement":null},{"id":"W1661959973","doi":"10.1029/2011gl050726","title":"On the information content of surface meteorology for downward atmospheric long‐wave radiation synthesis","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Meteorology; A priori and a posteriori; Cloud cover; Climatology; Variable (mathematics); Atmospheric sciences; Representation (politics); State variable; Empirical modelling; Cloud computing; Computer science; Mathematics; Geography; Geology; Physics","score_opus":0.09195660826690286,"score_gpt":0.2845689450269772,"score_spread":0.19261233676007436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1661959973","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1884472,0.0017200932,0.7899473,0.0029642235,0.00016324046,0.0001893283,0.0022367411,0.00054016715,0.013791838],"genre_scores_gemma":[0.89198685,0.002223844,0.101591825,0.00034642706,0.00023947342,0.00027706884,0.0015985075,0.00020439227,0.0015316431],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99895704,0.0005225516,0.00008875082,0.000108943015,0.0002365946,0.000086055945],"domain_scores_gemma":[0.9654746,0.030729922,0.00075638323,0.001668849,0.0011861674,0.00018405617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004806864,0.0005948764,0.00070642005,0.0012428684,0.000502404,0.0018511756,0.0006479785,0.0007436047,0.0035752484],"category_scores_gemma":[0.039140802,0.00030572937,0.00063462334,0.0012766861,0.001193185,0.0035527723,0.0013355127,0.0010913241,0.0004368434],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029301524,0.00008930394,0.010589738,0.00049866724,0.0000998809,0.00025744957,0.00015517713,0.67981255,0.0070941453,0.20059164,0.0023164707,0.098202005],"study_design_scores_gemma":[0.000015824642,0.000048993043,0.002400753,0.00011224697,0.000032094955,0.00007105639,0.00003754582,0.9301593,0.002709849,0.06341034,0.0009830357,0.000019086869],"about_ca_topic_score_codex":0.0031448265,"about_ca_topic_score_gemma":0.0018841199,"teacher_disagreement_score":0.004806864,"about_ca_system_score_codex":0.0008220714,"about_ca_system_score_gemma":0.0012790669,"threshold_uncertainty_score":0.02542144},"labels":[],"label_agreement":null},{"id":"W1662350274","doi":"10.1029/2001gl014022","title":"Noctilucent clouds, PMSE and 5‐day planetary waves: A case study","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Vetenskapsrådet","keywords":"Mesosphere; Atmospheric sciences; Atmosphere (unit); Altitude (triangle); Polar; Climatology; Mesopause; Environmental science; Geology; Meteorology; Stratosphere; Physics; Astronomy","score_opus":0.026914360450914068,"score_gpt":0.28401614378954854,"score_spread":0.2571017833386345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1662350274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984896,0.00030141303,0.00031285797,0.00006499483,0.0000032881671,0.000006916621,0.00011240717,0.000005133089,0.00070317386],"genre_scores_gemma":[0.9982496,0.0004280239,0.0005497933,0.000013758596,0.000016414468,0.000007187978,0.00025962546,0.0000035303399,0.00047197693],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981993,0.00006207081,0.000012048603,0.00002117655,0.00003660505,0.00004823092],"domain_scores_gemma":[0.9992884,0.00044261583,0.0001225365,0.000054835014,0.000041322026,0.000050262028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003305518,0.00029825376,0.00018338581,0.00046627637,0.00042817008,0.0004616329,0.00025163888,0.00048150096,0.0006142506],"category_scores_gemma":[0.0013149976,0.00015977919,0.00043393002,0.00088554877,0.00036016267,0.0003533222,0.00047133,0.00025090243,0.00008574525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006432301,0.00036042632,0.9109713,0.00016045503,0.00021513317,0.03071795,0.0010866622,0.019961149,0.002466221,0.0017870835,0.0017472173,0.029883286],"study_design_scores_gemma":[0.000051769966,0.00038789964,0.9331865,0.0000359405,0.00012017803,0.016748566,0.0022589401,0.039259005,0.001619301,0.000963285,0.005329706,0.000038948656],"about_ca_topic_score_codex":0.0177594,"about_ca_topic_score_gemma":0.021865124,"teacher_disagreement_score":0.0177594,"about_ca_system_score_codex":0.00035434426,"about_ca_system_score_gemma":0.00018881491,"threshold_uncertainty_score":0.035312057},"labels":[],"label_agreement":null},{"id":"W1663757402","doi":"10.1029/2001gl013854","title":"Limitations in DGPS positioning accuracies at low latitudes during solar maximum","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"TEC; Global Positioning System; Geodesy; Latitude; Anomaly (physics); Differential GPS; Residual; Ionosphere; Remote sensing; Precise Point Positioning; Solar maximum; Environmental science; Geology; Meteorology; Solar cycle; Geography; GNSS applications; Mathematics; Computer science; Physics; Geophysics","score_opus":0.04720093667879527,"score_gpt":0.2781840975004847,"score_spread":0.2309831608216894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1663757402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7492626,0.003110623,0.20282425,0.001899494,0.0004947552,0.000095358235,0.009232122,0.0043410114,0.028739948],"genre_scores_gemma":[0.9556138,0.0011536368,0.037403084,0.00015753976,0.00015092279,0.00006062149,0.0035105192,0.00015501941,0.0017949353],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9980385,0.00057670625,0.00014640723,0.0003178278,0.0007943657,0.00012620381],"domain_scores_gemma":[0.99511117,0.0021823237,0.0003708061,0.001074886,0.0011981194,0.00006269792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023943593,0.0004753973,0.0004157426,0.0008451234,0.0003539795,0.00090401905,0.00068919465,0.0003444438,0.0016318167],"category_scores_gemma":[0.011155422,0.00032523795,0.00027941758,0.001999907,0.00029192618,0.00054937677,0.0006370009,0.00045633918,0.0018432015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062546425,0.000035154964,0.12578341,0.0010407751,0.000236134,0.00025516617,0.0016902497,0.060211092,0.03551614,0.0030992446,0.011093102,0.7604141],"study_design_scores_gemma":[0.0001214709,0.00034772616,0.6867127,0.0005367767,0.00047180973,0.0036924877,0.0028976144,0.10638301,0.06817779,0.009086941,0.12137476,0.00019691096],"about_ca_topic_score_codex":0.009900732,"about_ca_topic_score_gemma":0.010893327,"teacher_disagreement_score":0.009900732,"about_ca_system_score_codex":0.0004392704,"about_ca_system_score_gemma":0.00029831604,"threshold_uncertainty_score":0.019686162},"labels":[],"label_agreement":null},{"id":"W1665063918","doi":"10.1029/2011gl047563","title":"Major influence of tropical volcanic eruptions on the stratospheric aerosol layer during the last decade","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":469,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Canadian Space Agency; Freie Universität Berlin; Université de Versailles Saint-Quentin-en-Yvelines; Université de Lille; Langley Research Center; National Aeronautics and Space Administration","keywords":"Stratosphere; Aerosol; Volcano; Atmospheric sciences; Vulcanian eruption; Environmental science; Climatology; Latitude; Satellite; Troposphere; Total Ozone Mapping Spectrometer; Sulfate aerosol; Lidar; Ozone layer; Atmosphere (unit); Geology; Meteorology; Remote sensing; Geography; Physics","score_opus":0.03898847376554177,"score_gpt":0.2701389654330194,"score_spread":0.23115049166747764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1665063918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9918887,0.005252515,0.00006555169,0.00017679643,0.000034037563,0.000004604339,0.0010237478,0.00001106988,0.0015430242],"genre_scores_gemma":[0.99751425,0.0014228836,0.00004923536,0.000051029772,0.00007323591,0.0000017862852,0.00063093216,0.0000033142383,0.00025324468],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988663,0.000015564208,0.000013273398,0.00003538172,0.000019917827,0.000029284933],"domain_scores_gemma":[0.99949074,0.0000663125,0.0002398696,0.000024687512,0.00008032664,0.00009804578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002896448,0.00017796917,0.00017387193,0.0005646656,0.0002647942,0.00054608256,0.00016738568,0.0002786389,0.0014334877],"category_scores_gemma":[0.00057963625,0.00006979133,0.00013859436,0.0006946507,0.00018915493,0.00021739845,0.00029230688,0.00016901111,0.00020345839],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029920213,0.000033566026,0.97273004,0.000111618516,0.00012294475,0.0003070796,0.00024756422,0.0002566534,0.0067651263,0.000120883284,0.00055697066,0.018448435],"study_design_scores_gemma":[0.0000018374291,0.000027946344,0.9989741,0.0000063874627,0.000020327096,0.0000723122,0.000050976098,0.000037488968,0.00020376286,0.0000052021605,0.00059855176,0.0000011673809],"about_ca_topic_score_codex":0.007516043,"about_ca_topic_score_gemma":0.012738428,"teacher_disagreement_score":0.007516043,"about_ca_system_score_codex":0.00035443736,"about_ca_system_score_gemma":0.00026839788,"threshold_uncertainty_score":0.014944613},"labels":[],"label_agreement":null},{"id":"W1667593643","doi":"10.1029/2003gl018520","title":"A significant abiotic pathway for the formation of <i>unknown</i> nitrogen in nature","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada; Canadian Light Source (Canada); University of Saskatchewan","funders":"","keywords":"Abiotic component; Nitrogen; Chemistry; Abiotic stress; Ecosystem; Sugar; Abiogenesis; Amino acid; Maillard reaction; Organic chemistry; Environmental chemistry; Astrobiology; Ecology; Biology; Biochemistry","score_opus":0.021649254712748155,"score_gpt":0.26191195920506927,"score_spread":0.24026270449232112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1667593643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9480874,0.011317581,0.025159646,0.0007143129,0.00018265119,0.00005413972,0.0006386733,0.00011699401,0.0137286065],"genre_scores_gemma":[0.98973024,0.0024604937,0.005179634,0.00013133304,0.000036495338,0.000016459797,0.00038023014,0.000010473924,0.0020546962],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991786,0.000013283487,0.0000030824929,0.000033005057,0.000018728253,0.000014080263],"domain_scores_gemma":[0.99988186,0.00002920954,0.000044030825,0.000014549184,0.00001619935,0.000014121067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017032947,0.00026666466,0.00011790379,0.00012942789,0.0003145804,0.0003845979,0.00025765735,0.0002602671,0.0013970042],"category_scores_gemma":[0.00017616048,0.000089961126,0.00015077788,0.00013866654,0.0004871085,0.0004316484,0.00028802178,0.0003247156,0.00037607658],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020058198,0.00002515762,0.014049476,0.0005261589,0.00002453611,0.0003270619,0.00006845349,0.00025318025,0.9673527,0.004084809,0.00023425552,0.01285365],"study_design_scores_gemma":[0.0000128293095,0.0005968636,0.032876786,0.00005746951,0.000051216328,0.0009412433,0.00028733388,0.001190758,0.9360609,0.0040318607,0.023866817,0.000025945099],"about_ca_topic_score_codex":0.0005718646,"about_ca_topic_score_gemma":0.0011183535,"teacher_disagreement_score":0.0013970042,"about_ca_system_score_codex":0.00030434915,"about_ca_system_score_gemma":0.00039689496,"threshold_uncertainty_score":0.004673481},"labels":[],"label_agreement":null},{"id":"W1669889489","doi":"10.1029/2003gl019089","title":"The northern hemisphere stratospheric vortex during the 2002–03 winter: Subsidence, chlorine activation and ozone loss observed by the Odin Sub‐Millimetre Radiometer","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Office of International Science and Engineering; Centre National d’Etudes Spatiales","keywords":"Ozone; Polar vortex; Atmospheric sciences; Stratosphere; Radiometer; Northern Hemisphere; Environmental science; Ozone layer; Subsidence; Arctic; Ozone depletion; Microwave Limb Sounder; Geology; Meteorology; Physics; Oceanography; Remote sensing","score_opus":0.02266323439159192,"score_gpt":0.2426231474239807,"score_spread":0.21995991303238877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1669889489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924684,0.00004739566,0.00005166847,0.000018376477,0.0000031646575,0.0000026991931,0.00023136247,0.000010690331,0.00038771427],"genre_scores_gemma":[0.99881893,0.000051340307,0.0001226985,0.000025645379,0.000009196597,0.0000048353154,0.00072438247,0.000004186916,0.00023880436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999559,0.0000046152145,0.0000025573927,0.000010154387,0.000012595852,0.000014157415],"domain_scores_gemma":[0.9998828,0.000010435611,0.000045874367,0.000009332092,0.000022723218,0.000028706627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011289724,0.0001902186,0.00021241332,0.00027846443,0.00031340096,0.0003719846,0.00011949313,0.00026950898,0.00038955727],"category_scores_gemma":[0.00021772725,0.00008160379,0.00009959735,0.0002449555,0.00013553488,0.00018341694,0.00022445958,0.0001647007,0.00011494083],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00079012563,0.00012751448,0.93651193,0.000049192815,0.0000780384,0.0005583002,0.0009533217,0.0007940874,0.043726046,0.00008105545,0.0012910896,0.015039321],"study_design_scores_gemma":[0.000006183714,0.000040202543,0.9981192,0.0000020872235,0.0000083249715,0.000053621417,0.00007455659,0.00037705997,0.0007328633,0.000007643212,0.0005762787,0.0000019855286],"about_ca_topic_score_codex":0.021502914,"about_ca_topic_score_gemma":0.0384461,"teacher_disagreement_score":0.021502914,"about_ca_system_score_codex":0.00038040112,"about_ca_system_score_gemma":0.00018374638,"threshold_uncertainty_score":0.042755485},"labels":[],"label_agreement":null},{"id":"W1673079646","doi":"10.1002/grl.50183","title":"Implications of Arctic sea ice changes for North Atlantic deep convection and the meridional overturning circulation in CCSM4‐CMIP5 simulations","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Shutdown of thermohaline circulation; Forcing (mathematics); Geology; Thermohaline circulation; Climatology; Sea ice; Arctic ice pack; North Atlantic Deep Water; Arctic; Convection; Oceanography; Arctic geoengineering; Deep convection; Environmental science; Drift ice; Meteorology; Geography","score_opus":0.025740769338591086,"score_gpt":0.269148871618207,"score_spread":0.2434081022796159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1673079646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99224913,0.00015762015,0.0006995475,0.00049960235,0.0001085121,0.000019427374,0.0027365903,0.00013718156,0.0033924459],"genre_scores_gemma":[0.9980367,0.00008698987,0.00033817065,0.000056104232,0.000015689904,0.000015236151,0.0010147955,0.000023964847,0.00041241726],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997359,0.00010577647,0.000017054857,0.000043885477,0.000032372147,0.0000650087],"domain_scores_gemma":[0.99942905,0.0002372617,0.000053654116,0.000046457728,0.000108796354,0.00012485239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010274936,0.0010085694,0.0005017419,0.00049259304,0.0007570934,0.0013112013,0.0008656428,0.0013364804,0.0019724502],"category_scores_gemma":[0.0025266176,0.00047017273,0.0012128333,0.00065826345,0.0006582506,0.00067909044,0.0005282281,0.0009582654,0.00024011779],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030131408,0.00010632521,0.027038595,0.000051510775,0.00017740203,0.0002058775,0.000044316766,0.9656532,0.0019498739,0.0013205427,0.0015423734,0.0016087312],"study_design_scores_gemma":[0.00021280198,0.00013227398,0.02646361,0.00003026827,0.00011923114,0.000024246528,0.00011713976,0.96925575,0.0018254218,0.00062618795,0.0011427861,0.000050231018],"about_ca_topic_score_codex":0.17296034,"about_ca_topic_score_gemma":0.074596435,"teacher_disagreement_score":0.17296034,"about_ca_system_score_codex":0.0022645753,"about_ca_system_score_gemma":0.0022554144,"threshold_uncertainty_score":0.34390718},"labels":[],"label_agreement":null},{"id":"W1673471330","doi":"10.1029/2010gl045237","title":"Quality of reanalysis data during stratospheric vortex weakening and intensification events","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Troposphere; Climatology; Polar vortex; Northern Hemisphere; Stratosphere; Atmospheric sciences; Southern Hemisphere; Vortex; Meteorology; Geology; Physics","score_opus":0.07188885167087934,"score_gpt":0.34116882200926396,"score_spread":0.26927997033838463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1673471330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884531,0.0006264893,0.002295798,0.00012880917,0.00004967969,0.000036481317,0.0067198738,0.00014440659,0.0015453623],"genre_scores_gemma":[0.9892162,0.00018619116,0.0014967239,0.000028784476,0.000026124768,0.000015916807,0.008635579,0.00003504098,0.0003593811],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9964104,0.0012408056,0.00067599345,0.00078035425,0.00066256744,0.0002298703],"domain_scores_gemma":[0.9810246,0.0073185535,0.0046837,0.0025092354,0.0038808761,0.00058291917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0069419146,0.00038395173,0.00060048257,0.002241638,0.0003737737,0.0017357004,0.0005375246,0.0005031041,0.0007735485],"category_scores_gemma":[0.02226854,0.0003234152,0.0007015698,0.0026277807,0.00041072184,0.0012055103,0.0007345445,0.00034627278,0.00033417472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006534633,0.000053970653,0.95738256,0.00007649423,0.00057341956,0.000099643396,0.00042768367,0.010444002,0.002758129,0.00017502274,0.0007471825,0.026608378],"study_design_scores_gemma":[0.000031737694,0.00010791171,0.9862877,0.000034944307,0.00015877385,0.00008432472,0.00035266744,0.009684738,0.0017310553,0.00011457983,0.0013745012,0.000037054273],"about_ca_topic_score_codex":0.02438589,"about_ca_topic_score_gemma":0.031305272,"teacher_disagreement_score":0.02438589,"about_ca_system_score_codex":0.0005187933,"about_ca_system_score_gemma":0.00059281365,"threshold_uncertainty_score":0.0484879},"labels":[],"label_agreement":null},{"id":"W1674104847","doi":"10.1029/2010gl044927","title":"Estimating seismic moment magnitude (<i>M</i><sub><i>w</i></sub>) of tremor bursts in northern Cascadia: Implications for the “seismic efficiency” of episodic tremor and slip","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of Toronto; Geological Survey of Canada","funders":"U.S. Geological Survey","keywords":"Seismogram; Seismology; Geology; Amplitude; Slip (aerodynamics); Magnitude (astronomy); Seismic moment; Moment magnitude scale; Episodic tremor and slip; Consistency (knowledge bases); Seismic wave; Geodesy; Subduction; Physics; Tectonics; Mathematics; Geometry","score_opus":0.024850585016031282,"score_gpt":0.2801703168840403,"score_spread":0.25531973186800905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1674104847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98455334,0.000080929225,0.013983584,0.000053336655,0.000002775041,0.000010137386,0.00024036347,0.0001509787,0.0009245084],"genre_scores_gemma":[0.9939744,0.000060333707,0.0055308966,0.0000032276803,0.0000049919163,0.000009032591,0.00022006733,0.000010554631,0.00018651543],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.000017614446,0.000007926184,0.000034709472,0.000026678339,0.000010697904],"domain_scores_gemma":[0.9993692,0.00015707624,0.00023560403,0.00007223174,0.000096030955,0.00006987987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030439644,0.00045711632,0.00015451682,0.0012292584,0.00018688357,0.00023883756,0.00033519542,0.00021333153,0.00042266538],"category_scores_gemma":[0.0018942353,0.0002539718,0.00014061252,0.0005921729,0.0002391577,0.00025445997,0.00033495683,0.00018684562,0.00015967271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018456277,0.000043538854,0.8244593,0.00009286756,0.00010810348,0.0001616767,0.00053302635,0.030342456,0.04197702,0.00024129766,0.00029526578,0.10156098],"study_design_scores_gemma":[0.00001638699,0.000092207476,0.92471945,0.000009799109,0.000043049396,0.00013118892,0.0001929123,0.06559404,0.008250784,0.0003138391,0.00060372666,0.000032619275],"about_ca_topic_score_codex":0.012358866,"about_ca_topic_score_gemma":0.023761278,"teacher_disagreement_score":0.012358866,"about_ca_system_score_codex":0.00045235208,"about_ca_system_score_gemma":0.0003622786,"threshold_uncertainty_score":0.024573863},"labels":[],"label_agreement":null},{"id":"W1675512008","doi":"10.1029/2012gl053387","title":"Spring snow cover extent reductions in the 2008–2012 period exceeding climate model projections","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":442,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos; Environment and Climate Change Canada","funders":"","keywords":"Northern Hemisphere; Climatology; Snow; Coupled model intercomparison project; Environmental science; Snow cover; Spring (device); Arctic; Climate model; Period (music); Climate change; Physical geography; Meteorology; Geology; Oceanography; Geography","score_opus":0.09126757674276756,"score_gpt":0.31838288450783275,"score_spread":0.2271153077650652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1675512008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993079,0.00009882096,0.00042695802,0.00033222334,0.000025307296,0.0000049753908,0.0040688864,0.000097725744,0.0018659434],"genre_scores_gemma":[0.994769,0.000045933528,0.0001895043,0.000036873374,0.000009458583,0.0000059398176,0.004604616,0.000009623747,0.0003290766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985397,0.000023456578,0.000012738412,0.000051500465,0.000028072829,0.000030188434],"domain_scores_gemma":[0.9997143,0.00004873644,0.00008374772,0.000025941876,0.00009108492,0.000036157868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048663843,0.00021864612,0.00016325162,0.0002746701,0.00021155429,0.0004806597,0.00021878521,0.00032104852,0.0012788379],"category_scores_gemma":[0.0011752772,0.00015941243,0.0003410251,0.00038243883,0.0001183862,0.00043417973,0.0002789595,0.0003316866,0.00022208429],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006998573,0.00012625038,0.9209692,0.00007794048,0.00026775297,0.00018166295,0.00023311017,0.04868438,0.0024247752,0.00071442407,0.009402376,0.01621845],"study_design_scores_gemma":[0.000017378952,0.000048710044,0.9565257,0.000010929048,0.00004439941,0.000059764177,0.00013874372,0.03886598,0.00084290846,0.00016413683,0.0032685963,0.000012768459],"about_ca_topic_score_codex":0.047536884,"about_ca_topic_score_gemma":0.068069145,"teacher_disagreement_score":0.047536884,"about_ca_system_score_codex":0.0007887479,"about_ca_system_score_gemma":0.0005471509,"threshold_uncertainty_score":0.09452039},"labels":[],"label_agreement":null},{"id":"W1677251393","doi":"10.1002/2013gl057454","title":"Disentangling Mie and attenuation effects in rain using a K<sub><i>a</i></sub>‐W dual‐wavelength Doppler spectral ratio technique","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Precipitation Measurement and Analysis","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Attenuation; Wavelength; Doppler effect; Rayleigh scattering; Optics; Doppler radar; Spectral line; Radar; Physics; Remote sensing; Computational physics; Geology","score_opus":0.03300929471892686,"score_gpt":0.2753014721440528,"score_spread":0.24229217742512596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1677251393","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.70611805,0.00083815044,0.2895718,0.000090223126,0.00003787728,0.000052723128,0.00019469952,0.0004980273,0.0025984815],"genre_scores_gemma":[0.86249703,0.00048018526,0.1362568,0.000040205727,0.000053001153,0.000032182008,0.00015670137,0.000052815674,0.00043113227],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998629,0.000024989153,0.000008687318,0.00003578712,0.000045165958,0.000022468468],"domain_scores_gemma":[0.9995975,0.00016126507,0.00009590909,0.000049352446,0.0000722273,0.000023790522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032949206,0.00037408833,0.0002864354,0.0007954244,0.00018394392,0.00046062085,0.0003259963,0.00024256864,0.0005811609],"category_scores_gemma":[0.0010727175,0.00024055823,0.00020717629,0.0005119777,0.00022648426,0.0011130717,0.00046067836,0.0003921367,0.00027926924],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005023976,0.0001628536,0.038316358,0.00013938005,0.000089676876,0.00017006243,0.00017955407,0.006458035,0.7357868,0.0019663987,0.0002738412,0.21595468],"study_design_scores_gemma":[0.00012669172,0.00058843545,0.12025014,0.00003687903,0.0002526387,0.0015774734,0.0002538717,0.31429788,0.5549954,0.0035989326,0.00390469,0.00011687606],"about_ca_topic_score_codex":0.00058198627,"about_ca_topic_score_gemma":0.0013014773,"teacher_disagreement_score":0.0007954244,"about_ca_system_score_codex":0.00010638351,"about_ca_system_score_gemma":0.00018255155,"threshold_uncertainty_score":0.0019442439},"labels":[],"label_agreement":null},{"id":"W1677923143","doi":"10.1029/2010gl045459","title":"Deepening of the nutricline and chlorophyll maximum in the Canada Basin interior, 2003–2009","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":234,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Photic zone; Upwelling; Oceanography; Deep chlorophyll maximum; Stratification (seeds); Ocean gyre; New production; Mixed layer; Canada Basin; Nitrate; Geology; Halocline; Environmental science; Arctic; Chlorophyll a; Phytoplankton; Nutrient; Salinity; Chemistry; Subtropics; Ecology","score_opus":0.01250953196842929,"score_gpt":0.24020222118533863,"score_spread":0.22769268921690933,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1677923143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9752607,0.0016306759,0.00012385106,0.0009834815,0.000042551077,0.000021635355,0.01368099,0.00004851396,0.008207604],"genre_scores_gemma":[0.98971725,0.0006807187,0.0002801334,0.00020618075,0.000010244489,0.000010148715,0.005559577,0.000013202105,0.00352257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979323,0.0000040065433,0.000007771748,0.000041192172,0.00007700343,0.000076862634],"domain_scores_gemma":[0.99891436,0.000019647345,0.00010543967,0.00002398162,0.0006954421,0.00024121576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002513715,0.0002864567,0.0003248915,0.001362982,0.0022988368,0.0015394753,0.0006064464,0.00042091435,0.00163396],"category_scores_gemma":[0.0007897565,0.00023613693,0.00029760215,0.0021745532,0.000685445,0.0003298702,0.00067479187,0.00056570576,0.00020631464],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002524348,0.000051992163,0.9638378,0.00010561061,0.00014683907,0.0002551553,0.0015706931,0.00065657124,0.0033105973,0.00054546195,0.010092026,0.019174887],"study_design_scores_gemma":[0.0000028473758,0.000003302957,0.99628276,0.000013056299,0.000009608382,0.000017654915,0.00034772983,0.0001512755,0.000121938996,0.00001247604,0.0030321681,0.0000051133693],"about_ca_topic_score_codex":0.9962108,"about_ca_topic_score_gemma":0.99870837,"teacher_disagreement_score":0.034207877,"about_ca_system_score_codex":0.034207877,"about_ca_system_score_gemma":0.03366526,"threshold_uncertainty_score":0.24819672},"labels":[],"label_agreement":null},{"id":"W1680373685","doi":"10.1029/2011gl047793","title":"The Kamikatsura event in the Gold Hill loess, Alaska","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Loess; Geology; Event (particle physics); Earth science; Physical geography; Geomorphology; Geography","score_opus":0.0578192269896234,"score_gpt":0.29735666536340877,"score_spread":0.23953743837378538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1680373685","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986572,0.0000833117,0.000018697223,0.000019258716,0.0000022905836,0.0000019383153,0.00007513153,0.0000015163632,0.001140563],"genre_scores_gemma":[0.99909437,0.00010169212,0.000046212514,0.000008697694,0.0000029254709,0.000002134224,0.00011478269,5.151609e-7,0.0006286337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996114,0.000005065668,0.0000032073385,0.000015149362,0.0000063229254,0.000009085981],"domain_scores_gemma":[0.9999286,0.0000067430087,0.00002365192,0.0000034489353,0.000013572173,0.000023961185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013662875,0.00006504119,0.00005439986,0.0004550059,0.0007667865,0.00038954034,0.0001515366,0.00021478758,0.0012916389],"category_scores_gemma":[0.00022063412,0.00006367138,0.000045316465,0.00044537612,0.00032728055,0.0002673612,0.00046405883,0.00010608852,0.00012398831],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076353936,0.000025170788,0.98136395,0.00004120224,0.000019828658,0.00094483094,0.0034363877,0.00013555806,0.0052740043,0.0001764271,0.00024652432,0.008259692],"study_design_scores_gemma":[0.0000010281009,0.000010063275,0.9980495,0.0000081245935,0.000004603763,0.00006666943,0.0012676909,0.00004102084,0.000112726186,0.000021277274,0.00041610142,0.0000012615418],"about_ca_topic_score_codex":0.10499031,"about_ca_topic_score_gemma":0.25953135,"teacher_disagreement_score":0.10499031,"about_ca_system_score_codex":0.00046230337,"about_ca_system_score_gemma":0.0003593772,"threshold_uncertainty_score":0.20875835},"labels":[],"label_agreement":null},{"id":"W1681747307","doi":"10.1029/2004gl019922","title":"Electrodynamics of a flux transfer event: Experimental test of the Southwood model","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Poynting vector; Physics; Flux (metallurgy); Ionosphere; Meteorology; Flow (mathematics); Convection; Current (fluid); Mechanics; Computational physics; Geophysics; Atmospheric sciences; Magnetic field; Materials science","score_opus":0.011836905205752075,"score_gpt":0.2723067162166046,"score_spread":0.26046981101085254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1681747307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966273,0.0000189297,0.0018685646,0.00004148767,0.000007073775,0.000018294477,0.000026368882,0.000020728065,0.0013712056],"genre_scores_gemma":[0.99903595,0.000023890989,0.0006081107,0.0000085688425,0.0000039387987,0.000011833373,0.000033465676,0.0000063785383,0.00026792657],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998822,0.000029357227,0.0000062532804,0.000033520133,0.00002610065,0.000022640766],"domain_scores_gemma":[0.99933475,0.00038538215,0.00008531205,0.00010728025,0.000042433374,0.000044875378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004491474,0.00018602735,0.00019640687,0.00016745734,0.00027093032,0.00039466325,0.00047663398,0.00038191726,0.002336403],"category_scores_gemma":[0.0023563425,0.00015092417,0.00014986141,0.000104063394,0.00047870638,0.0008768766,0.00051092834,0.00047433854,0.00022492792],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.012881754,0.0020609617,0.055409808,0.0002798889,0.00010687264,0.0014719325,0.0032070754,0.04485606,0.80137575,0.025804043,0.0015177613,0.051028073],"study_design_scores_gemma":[0.0008695823,0.004668358,0.07799931,0.0000439197,0.00008138942,0.000660001,0.0008147014,0.6956583,0.2033659,0.012167651,0.0035967403,0.000074127325],"about_ca_topic_score_codex":0.00069897773,"about_ca_topic_score_gemma":0.00022824822,"teacher_disagreement_score":0.002336403,"about_ca_system_score_codex":0.0002704887,"about_ca_system_score_gemma":0.00013043493,"threshold_uncertainty_score":0.007816076},"labels":[],"label_agreement":null},{"id":"W1682899846","doi":"10.1029/2010gl043989","title":"Non‐stormtime injection of energetic particles into the slot‐region between Earth's inner and outer electron radiation belts as observed by STSAT‐1 and NOAA‐POES","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Substorm; Van Allen radiation belt; Geomagnetic storm; Electron; Van Allen Probes; Earth's magnetic field; Storm; Physics; Radiation; Geophysics; Satellite; Atmospheric sciences; Geology; Meteorology; Magnetic field; Magnetosphere; Astronomy; Nuclear physics; Plasma","score_opus":0.01074505759156795,"score_gpt":0.25770714501497016,"score_spread":0.2469620874234022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1682899846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99881965,0.00004089292,0.00016770363,0.000014258003,0.0000045578186,0.0000032621226,0.00007784045,0.000012427621,0.0008594413],"genre_scores_gemma":[0.99938655,0.000025827045,0.00014440394,0.00001111263,0.000004718001,0.000003510865,0.00015478281,0.0000025116444,0.00026647098],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999523,0.0000043420987,0.000002324362,0.0000115731,0.000013800055,0.00001565918],"domain_scores_gemma":[0.9997905,0.000032355394,0.00008035924,0.000022186128,0.00003389388,0.000040822186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012336916,0.00010925398,0.00016826195,0.00025368333,0.0002390335,0.00027648432,0.00015888993,0.00021326706,0.00060765847],"category_scores_gemma":[0.0002863434,0.00012770717,0.00009389674,0.00021619789,0.00021927955,0.00027202672,0.00031484742,0.0002475624,0.00010758999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011960013,0.00011692584,0.6761821,0.000062143925,0.00011296175,0.001223418,0.0011334753,0.0008786759,0.30394143,0.0006311912,0.00082735624,0.013694311],"study_design_scores_gemma":[0.00002864874,0.00015333811,0.98874795,0.0000057457146,0.0000205749,0.00027988764,0.0001770876,0.0010157747,0.008398006,0.00007545476,0.0010916003,0.0000059451104],"about_ca_topic_score_codex":0.0027141802,"about_ca_topic_score_gemma":0.006896633,"teacher_disagreement_score":0.0027141802,"about_ca_system_score_codex":0.00021225822,"about_ca_system_score_gemma":0.00014327257,"threshold_uncertainty_score":0.0053967237},"labels":[],"label_agreement":null},{"id":"W1696170708","doi":"10.1029/2009gl041417","title":"Giant impact stratification of the Martian core","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Stratification (seeds); Dynamo; Martian; Mars Exploration Program; Geology; Shock wave; Thermal stratification; Inner core; Geophysics; Mantle (geology); Atmospheric sciences; Mechanics; Astrobiology; Physics; Climatology; Magnetic field","score_opus":0.04482475234239547,"score_gpt":0.3307804222274718,"score_spread":0.2859556698850763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1696170708","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967552,0.00011592249,0.0004455399,0.000022799231,0.000004475977,0.0000041391204,0.00002703858,0.000013040198,0.002611847],"genre_scores_gemma":[0.99966085,0.00005241617,0.000071611285,0.000004015219,0.0000016987827,0.0000013603035,0.000022801803,0.000004273298,0.0001809822],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999714,0.0000021561486,7.618916e-7,0.0000034943084,0.0000055911682,0.00001665438],"domain_scores_gemma":[0.99992037,0.000012834778,0.000025539493,0.0000053877966,0.0000096366975,0.000026293372],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006690058,0.00022429145,0.00014380361,0.00023770348,0.0002955105,0.0002607606,0.00016452193,0.00013151974,0.0013522814],"category_scores_gemma":[0.00030606706,0.000121685334,0.00025056966,0.000120410805,0.00019879019,0.00021609526,0.0005195185,0.0001901167,0.00013473582],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010349795,0.00024327864,0.19694236,0.00027506132,0.00022653562,0.0025560567,0.00054646627,0.36916682,0.37446195,0.017368456,0.0011719345,0.03600611],"study_design_scores_gemma":[0.00011800241,0.0010018522,0.4228625,0.000031075637,0.00015770737,0.0006791236,0.0003926712,0.50074947,0.06511783,0.0052402723,0.0035924749,0.000056963712],"about_ca_topic_score_codex":0.0057807066,"about_ca_topic_score_gemma":0.0045099105,"teacher_disagreement_score":0.0057807066,"about_ca_system_score_codex":0.00062869804,"about_ca_system_score_gemma":0.00029063373,"threshold_uncertainty_score":0.0114941},"labels":[],"label_agreement":null},{"id":"W1705051723","doi":"10.1029/2010gl045283","title":"Response of mantle heat flux to plate evolution","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fluid Dynamics and Turbulent Flows","field":"Engineering","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Heat flux; Convection; Mantle (geology); Mantle convection; Mechanics; Geophysics; Geology; Plate tectonics; Rayleigh number; Heat transfer; Natural convection; Geometry; Physics; Mathematics","score_opus":0.012871035306978267,"score_gpt":0.2674940455276559,"score_spread":0.2546230102206776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1705051723","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984047,0.000037994057,0.00060887245,0.000022057091,0.0000030940912,0.0000030976107,0.000049990853,0.000049059483,0.0008211426],"genre_scores_gemma":[0.9994611,0.000022907087,0.0002600997,0.000004534403,0.0000012241657,0.00000265191,0.00006717157,0.000016017762,0.0001643366],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988353,0.000024884459,0.0000050468943,0.000025901987,0.000026199164,0.000034457047],"domain_scores_gemma":[0.99955386,0.00025977407,0.000042423373,0.000042714903,0.00005540386,0.000045775734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018604154,0.0004381168,0.0003366489,0.0003898714,0.00022164703,0.00064938964,0.00035434347,0.0004019109,0.0010924471],"category_scores_gemma":[0.0016691269,0.00030863247,0.00046627678,0.00026281277,0.000675035,0.0002883075,0.00048144933,0.0004009614,0.00013485459],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009856703,0.00012050494,0.055233438,0.00010614371,0.00013134076,0.0003979522,0.00015799297,0.6266011,0.30667233,0.0010286286,0.00021278167,0.008352071],"study_design_scores_gemma":[0.000095048876,0.00038934965,0.076858595,0.000013350515,0.00006632311,0.00014894847,0.00014786306,0.79477465,0.12638824,0.000613514,0.00045377205,0.000050294926],"about_ca_topic_score_codex":0.003916899,"about_ca_topic_score_gemma":0.0013053156,"teacher_disagreement_score":0.003916899,"about_ca_system_score_codex":0.00049393775,"about_ca_system_score_gemma":0.00026599687,"threshold_uncertainty_score":0.0077881813},"labels":[],"label_agreement":null},{"id":"W1709829657","doi":"10.1002/2015gl064626","title":"Potential positive feedback between Greenland Ice Sheet melt and Baffin Bay heat content on the west Greenland shelf","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Oceanography; Meltwater; Geology; Bay; Greenland ice sheet; Fjord; Ice sheet; Iceberg; Sea ice; Arctic ice pack; Ice shelf; Archipelago; Glacier; Future sea level; Arctic; Antarctic sea ice; Cryosphere; Climatology; Geomorphology","score_opus":0.07983566508900852,"score_gpt":0.27919129696739764,"score_spread":0.19935563187838912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1709829657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995925,0.000007715368,0.000016490056,0.000043236614,0.0000015674569,0.0000021558315,0.00005072958,0.0000038207722,0.0002817938],"genre_scores_gemma":[0.9998049,0.000007485403,0.000030742438,0.000017322564,8.4192953e-7,0.0000025701545,0.000041796873,0.0000011503523,0.000093219336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998988,0.000029557903,0.000005510966,0.000021220758,0.000013592713,0.00003140253],"domain_scores_gemma":[0.99961674,0.00015532883,0.000051404837,0.000026231397,0.00006381178,0.00008651934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033374998,0.0002706329,0.00024722886,0.00027649247,0.00045400098,0.00075927324,0.00028582654,0.00039162138,0.002356941],"category_scores_gemma":[0.0008097987,0.00016226893,0.00023978378,0.00018389939,0.0006264458,0.0003391603,0.00039295867,0.00020886816,0.00010675321],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015656044,0.0004427099,0.84600073,0.000083835606,0.00019303006,0.00058684044,0.0005698981,0.02269804,0.11765176,0.0006173264,0.0008944107,0.008695835],"study_design_scores_gemma":[0.00008008923,0.00017661495,0.9794891,0.000007704329,0.00005245997,0.000017771357,0.000552145,0.01587336,0.0032248439,0.00015629992,0.00035622666,0.000013346014],"about_ca_topic_score_codex":0.119767584,"about_ca_topic_score_gemma":0.14061472,"teacher_disagreement_score":0.8802324,"about_ca_system_score_codex":0.0017824594,"about_ca_system_score_gemma":0.0007297763,"threshold_uncertainty_score":0.23814088},"labels":[],"label_agreement":null},{"id":"W1713659348","doi":"10.1029/2005gl022941","title":"Primary productivity control of simulated carbon cycle–climate feedbacks","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of Calgary","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Carbon cycle; Environmental science; Climate change; Climate model; Climatology; Productivity; Carbon fibers; Transient climate simulation; Atmospheric sciences; Vegetation (pathology); Ecosystem; Ecology; Computer science; Geology","score_opus":0.00857193055125468,"score_gpt":0.24732143303195497,"score_spread":0.2387495024807003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1713659348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936033,0.00009371222,0.002664574,0.00017181484,0.000026881642,0.000009751729,0.00059967645,0.00019435075,0.0026358836],"genre_scores_gemma":[0.9994784,0.000019993548,0.00019931723,0.000010354509,0.0000023725643,0.0000061436544,0.00016216542,0.000017163264,0.000104173894],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981064,0.00005599802,0.000010503731,0.00004825886,0.000026737527,0.000047972568],"domain_scores_gemma":[0.9991941,0.00044385984,0.00006170061,0.00006958674,0.0001397785,0.00009104873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005076477,0.0004974946,0.00038724017,0.00030473675,0.00040904712,0.00078573625,0.0006013546,0.000582408,0.0014335798],"category_scores_gemma":[0.0028356588,0.00027202285,0.00038556743,0.00035046382,0.0004639618,0.00053398364,0.00047553508,0.0005354967,0.00014516755],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014864384,0.0000551274,0.012472543,0.00003868686,0.00005877265,0.000046349913,0.000040945724,0.9741082,0.009149773,0.001010687,0.00042481627,0.0024455255],"study_design_scores_gemma":[0.000062283165,0.000031461455,0.0070028817,0.000004299301,0.000018385865,0.00001243081,0.000015969454,0.98934877,0.0025323145,0.00068330346,0.00027511193,0.000012858424],"about_ca_topic_score_codex":0.016812464,"about_ca_topic_score_gemma":0.010563015,"teacher_disagreement_score":0.016812464,"about_ca_system_score_codex":0.0010659335,"about_ca_system_score_gemma":0.00088337116,"threshold_uncertainty_score":0.033429205},"labels":[],"label_agreement":null},{"id":"W1714710418","doi":"10.1029/2005gl023293","title":"Variations of the mean winds and diurnal tides in the mesosphere and lower thermosphere observed by WINDII from 1992 to 1996","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"National Research Council Canada; Canadian Space Agency; Smithsonian Astrophysical Observatory; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Thermosphere; Northern Hemisphere; Atmospheric sciences; Mesosphere; Southern Hemisphere; Diurnal temperature variation; Latitude; Atmospheric tide; Altitude (triangle); Diurnal cycle; Climatology; Environmental science; Geology; Ionosphere; Stratosphere; Geodesy","score_opus":0.015834776015534173,"score_gpt":0.2604556521093822,"score_spread":0.24462087609384803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1714710418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983481,0.000060886403,0.000030176994,0.000019707028,0.0000032823564,0.0000044642643,0.0012036777,0.000006566707,0.00032305994],"genre_scores_gemma":[0.99279857,0.00015730577,0.00019380038,0.000021472593,0.000014298934,0.000023061239,0.0059053497,0.0000052758483,0.0008808718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998423,0.0000124458875,0.000018848801,0.00004768708,0.000033447584,0.000045178684],"domain_scores_gemma":[0.99926096,0.00004076268,0.0003897671,0.000046412144,0.00013745918,0.00012464568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003104752,0.00043970734,0.00030789393,0.0007524116,0.00032591462,0.0005755539,0.00025531003,0.00033462455,0.00073360436],"category_scores_gemma":[0.0008460025,0.00019998943,0.00021025944,0.0009119022,0.00012747041,0.00027777607,0.00028106317,0.00029364735,0.00029616908],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035184494,0.000054235188,0.98523766,0.00002340211,0.000078330275,0.00018836296,0.00030477095,0.00036988605,0.0068258136,0.000028740596,0.00044542778,0.006091401],"study_design_scores_gemma":[0.0000050267463,0.00002742136,0.9990538,0.0000036046706,0.0000063387383,0.00004681108,0.000048953323,0.00010180025,0.0002283657,0.0000034375544,0.0004725038,0.0000019615309],"about_ca_topic_score_codex":0.023017574,"about_ca_topic_score_gemma":0.04420821,"teacher_disagreement_score":0.023017574,"about_ca_system_score_codex":0.0007697509,"about_ca_system_score_gemma":0.00023988118,"threshold_uncertainty_score":0.045767188},"labels":[],"label_agreement":null},{"id":"W1730000284","doi":"10.1002/2015gl064540","title":"Phytoplankton biomass cycles in the North Atlantic subpolar gyre: A similar mechanism for two different blooms in the Labrador Sea","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Oceanography; Bloom; Phytoplankton; Spring bloom; Biomass (ecology); Mixed layer; Environmental science; Algal bloom; Irradiance; Front (military); Chlorophyll a; Climatology; Subtropics; Geology; Ecology; Biology; Nutrient; Physics","score_opus":0.043064303120054354,"score_gpt":0.27822749904743427,"score_spread":0.23516319592737991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1730000284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986615,0.000101789505,0.000098141354,0.0000480227,0.000002715759,0.000007881297,0.00014516973,0.000028444749,0.0009062001],"genre_scores_gemma":[0.9991404,0.000040143055,0.00012698252,0.000023795523,0.000002611445,0.0000074139016,0.0001906477,0.000005171978,0.0004627908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990964,0.000012638213,0.000007831209,0.000024836292,0.000012597168,0.000032426447],"domain_scores_gemma":[0.9996747,0.000028089298,0.000103187,0.000032840624,0.00007317305,0.000087992325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020260834,0.00025159592,0.00031340003,0.0010942708,0.00039771953,0.0007577629,0.00025769297,0.00028943835,0.00083529047],"category_scores_gemma":[0.0004154993,0.0002685763,0.00041668612,0.00037981773,0.0003584932,0.00023867366,0.00047469046,0.00013153354,0.00022538862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007037887,0.00010786611,0.8994229,0.00005604511,0.00014387819,0.00026293594,0.00093577703,0.0013723095,0.08291575,0.0008331722,0.0005096653,0.01273585],"study_design_scores_gemma":[0.000014549782,0.000031391613,0.9979729,0.0000031831225,0.00001537684,0.000027771064,0.00012011164,0.00073055556,0.0007729738,0.00006283627,0.00024052989,0.000007757968],"about_ca_topic_score_codex":0.03779819,"about_ca_topic_score_gemma":0.046639554,"teacher_disagreement_score":0.03779819,"about_ca_system_score_codex":0.0009979003,"about_ca_system_score_gemma":0.0003583381,"threshold_uncertainty_score":0.07515639},"labels":[],"label_agreement":null},{"id":"W1732620039","doi":"10.1029/2010gl045136","title":"Thermal response of the mantle following the formation of a “super‐plate”","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Hotspot (geology); Geology; Supercontinent; Mantle (geology); Subduction; Mantle convection; Plate tectonics; Mantle wedge; Geophysics; Continental margin; Mantle plume; Earth science; Paleontology; Tectonics; Lithosphere; Craton","score_opus":0.021685788742083573,"score_gpt":0.2701038513500971,"score_spread":0.24841806260801355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1732620039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991211,0.000036999256,0.00028600093,0.00001569984,0.0000019849815,0.0000010699148,0.000016833337,0.000010220582,0.000510029],"genre_scores_gemma":[0.9997602,0.000014089258,0.00009334032,0.0000057020943,9.0108534e-7,8.363486e-7,0.000027034392,0.0000029147313,0.00009491807],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999751,0.0000026824976,9.170012e-7,0.000006497569,0.0000052763135,0.000009579506],"domain_scores_gemma":[0.9999335,0.000019139048,0.000010894198,0.000009381825,0.000013002736,0.00001409623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000066288456,0.00011225637,0.00013677683,0.00017990461,0.00016842569,0.00029608383,0.00016850005,0.00017036227,0.0013287296],"category_scores_gemma":[0.0002332112,0.00014208771,0.00018851971,0.00011990095,0.00035789135,0.00021409811,0.0004391389,0.0003486897,0.00013605191],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059985276,0.00003413156,0.049427003,0.000048454876,0.00005629082,0.00037816947,0.00026078825,0.014297953,0.9279568,0.00083042035,0.00014401822,0.00596606],"study_design_scores_gemma":[0.000043021813,0.0004507212,0.6722379,0.000012441386,0.00008121443,0.00046890904,0.0007238135,0.08353689,0.23908195,0.0018272995,0.001486688,0.000049200025],"about_ca_topic_score_codex":0.002292051,"about_ca_topic_score_gemma":0.0016977077,"teacher_disagreement_score":0.002292051,"about_ca_system_score_codex":0.00023530402,"about_ca_system_score_gemma":0.00011124161,"threshold_uncertainty_score":0.004557371},"labels":[],"label_agreement":null},{"id":"W1738365655","doi":"10.1029/2002gl014998","title":"Crustal structure of the Chicxulub Impact crater imaged with magnetotelluric exploration","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Impact crater; Geology; Magnetotellurics; Electrical resistivity and conductivity; Sedimentary rock; Crust; Impact structure; Porosity; Geophysics; Hydrothermal circulation; Petrology; Mineralogy; Seismology; Geochemistry; Geotechnical engineering; Astrobiology","score_opus":0.036938500566631526,"score_gpt":0.28311027226048285,"score_spread":0.24617177169385132,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1738365655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965928,0.000116160445,0.00015066494,0.000021045445,0.0000011464684,0.0000045299703,0.00020890642,0.000018503026,0.002886105],"genre_scores_gemma":[0.9990307,0.000060002312,0.000310225,0.000010895037,0.0000015819105,0.0000036287624,0.00017607695,0.0000040797136,0.00040284186],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996054,0.0000023317295,0.000002000221,0.000009344789,0.0000126583855,0.000013126835],"domain_scores_gemma":[0.9999101,0.000010956332,0.000021173515,0.000009510242,0.00002383794,0.000024347219],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006384722,0.00015421023,0.00013002922,0.0009600103,0.00032996613,0.00031795682,0.00013886197,0.00025457767,0.0014317347],"category_scores_gemma":[0.00020267018,0.00019935469,0.000068902424,0.00050551246,0.00019163602,0.000097335695,0.0004727082,0.00015829051,0.00014445587],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005849027,0.000060034476,0.27274215,0.0002008223,0.000085762826,0.0035433406,0.001359225,0.0038143594,0.681606,0.00084448815,0.0015740169,0.033584967],"study_design_scores_gemma":[0.000009737258,0.000033751032,0.9929987,0.000029630773,0.000011821926,0.00056254974,0.00018790178,0.0013723193,0.0040009255,0.000020973148,0.0007630204,0.000008667462],"about_ca_topic_score_codex":0.018459275,"about_ca_topic_score_gemma":0.035769854,"teacher_disagreement_score":0.018459275,"about_ca_system_score_codex":0.00031327875,"about_ca_system_score_gemma":0.00022692954,"threshold_uncertainty_score":0.036703646},"labels":[],"label_agreement":null},{"id":"W1738705487","doi":"10.1029/2009gl042071","title":"Changes in equatorial atmospheric zonal circulations in recent decades","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Walker circulation; Climatology; Atmospheric circulation; Precipitation; Atmospheric sciences; Environmental science; Circulation (fluid dynamics); General Circulation Model; Geology; Oceanography; Sea surface temperature; Meteorology; Climate change; Geography; Physics","score_opus":0.05101126179854963,"score_gpt":0.3310216239315691,"score_spread":0.28001036213301944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1738705487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9604431,0.005344217,0.00073401496,0.0009844413,0.00024908475,0.000016472817,0.02176434,0.000078185236,0.010386028],"genre_scores_gemma":[0.9815538,0.002715855,0.00048448046,0.00025944927,0.00016360795,0.000020672307,0.012040735,0.000013153459,0.0027482002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997869,0.000026404388,0.000034507804,0.00005904595,0.000042787942,0.00005033662],"domain_scores_gemma":[0.9989135,0.00013390694,0.00046774145,0.000055702345,0.00034410306,0.00008493609],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006581741,0.00015418568,0.00017250114,0.0009941269,0.0002592257,0.0008067026,0.00021834696,0.00037365593,0.0022545464],"category_scores_gemma":[0.0023887996,0.00011252675,0.00035415211,0.0023160449,0.00011449199,0.000601811,0.0002990379,0.00043762592,0.00046415222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016468043,0.000043271546,0.96492654,0.00015655192,0.00047424732,0.00007970438,0.00032803725,0.0016336227,0.0013802181,0.0014330045,0.004788532,0.024591647],"study_design_scores_gemma":[0.0000041654844,0.000019042327,0.9881486,0.000018885275,0.000044607903,0.000086851556,0.000080934326,0.00036927598,0.00018287705,0.00006743916,0.010969438,0.000007855118],"about_ca_topic_score_codex":0.03059472,"about_ca_topic_score_gemma":0.038340114,"teacher_disagreement_score":0.03059472,"about_ca_system_score_codex":0.0008019036,"about_ca_system_score_gemma":0.00046132915,"threshold_uncertainty_score":0.060833275},"labels":[],"label_agreement":null},{"id":"W1742193183","doi":"10.1029/2012gl052810","title":"Observed and simulated changes in the Southern Hemisphere surface westerly wind‐stress","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":368,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Coupled model intercomparison project; Westerlies; Climatology; Southern Hemisphere; Climate model; Northern Hemisphere; Environmental science; Wind stress; Atmospheric sciences; Forcing (mathematics); Annual cycle; Climate change; Geology; Oceanography","score_opus":0.07740268282935805,"score_gpt":0.3067204459688865,"score_spread":0.22931776313952842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1742193183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99644035,0.00004291304,0.0004158422,0.00006045525,0.000016951755,0.0000058232663,0.0021496727,0.00005645118,0.00081148423],"genre_scores_gemma":[0.99746084,0.00005230675,0.00035699154,0.000012794017,0.0000069290663,0.000011806133,0.0018997369,0.000009627618,0.00018889022],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998952,0.000026852333,0.0000090904705,0.000030813197,0.000015897498,0.000022219221],"domain_scores_gemma":[0.9996873,0.00011939907,0.00006115466,0.00003605445,0.00006347481,0.000032649237],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041170148,0.00033823826,0.00018355831,0.00021843943,0.00016015592,0.00043101126,0.00034607522,0.00045859301,0.0014320087],"category_scores_gemma":[0.0009136442,0.00016480956,0.0004145421,0.000497131,0.00019884991,0.00042381548,0.00015638281,0.00030634733,0.00017881216],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049319677,0.00028801215,0.22372967,0.00010599943,0.00037211904,0.000118378965,0.000111874884,0.754097,0.006434781,0.0009144622,0.0032574467,0.010077059],"study_design_scores_gemma":[0.0003045027,0.00026637578,0.26608178,0.000020900927,0.0001366268,0.000058228583,0.00012398201,0.72533447,0.0048300615,0.0007053414,0.0020796582,0.00005801828],"about_ca_topic_score_codex":0.023916893,"about_ca_topic_score_gemma":0.02920943,"teacher_disagreement_score":0.023916893,"about_ca_system_score_codex":0.0006065178,"about_ca_system_score_gemma":0.00044253812,"threshold_uncertainty_score":0.047555387},"labels":[],"label_agreement":null},{"id":"W1742644122","doi":"10.1002/grl.50625","title":"The open ocean energy decay of three recent trans‐Pacific tsunamis","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; North Pacific Marine Science Organization","funders":"Russian Foundation for Basic Research","keywords":"Seismology; Geology; Pacific ocean; Range (aeronautics); Period (music); Oceanography; Physics","score_opus":0.04956692538873289,"score_gpt":0.2825790430352771,"score_spread":0.2330121176465442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1742644122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991716,0.000040705316,0.000055426313,0.000022007402,0.0000037586046,0.0000013227418,0.00019405645,0.000003102661,0.00050787616],"genre_scores_gemma":[0.99916387,0.00007073452,0.000053047777,0.0000070809197,0.000004444716,0.0000027001793,0.00046934863,0.000002313108,0.0002265301],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999627,0.000001972519,0.000004099001,0.000010057634,0.000009324493,0.00001188667],"domain_scores_gemma":[0.9996896,0.000042160136,0.0001042467,0.000019695302,0.0000851301,0.00005928072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010320354,0.00018382628,0.000087065695,0.0004469131,0.00026691623,0.0004987096,0.00012641755,0.00020527116,0.00087004696],"category_scores_gemma":[0.0006766075,0.000119277975,0.00016797021,0.0005347583,0.00024269104,0.0003940394,0.000675191,0.00031792742,0.00011404177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048480948,0.00008264156,0.94665945,0.00006567932,0.0001521875,0.00036988384,0.0005780218,0.0020676248,0.024285775,0.0003409979,0.00044742462,0.024465488],"study_design_scores_gemma":[0.0000040542086,0.000022922964,0.99814427,0.0000036734853,0.000012965365,0.000031547555,0.00015100876,0.0006151038,0.0006073883,0.00004142093,0.0003602511,0.0000053334734],"about_ca_topic_score_codex":0.02264208,"about_ca_topic_score_gemma":0.03732503,"teacher_disagreement_score":0.02264208,"about_ca_system_score_codex":0.00048027112,"about_ca_system_score_gemma":0.00027609392,"threshold_uncertainty_score":0.04502058},"labels":[],"label_agreement":null},{"id":"W1746170873","doi":"10.1029/2012gl054231","title":"Carbonate dissolution rates at the deep ocean floor","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Carbonate; Geology; Dissolution; Oceanography; Deep sea; Earth science; Materials science; Chemistry; Metallurgy","score_opus":0.031152094142697123,"score_gpt":0.29690158700017405,"score_spread":0.26574949285747695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1746170873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99788684,0.00013893608,0.00052422023,0.000023003391,0.0000026485968,0.0000040096957,0.00037367077,0.000015792595,0.0010308805],"genre_scores_gemma":[0.9989712,0.00009784418,0.00025719035,0.000008407122,8.470365e-7,0.0000031832117,0.00027798172,0.000005790603,0.00037745238],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998919,0.0000070972646,0.0000068519757,0.000027261865,0.000042484167,0.000024542689],"domain_scores_gemma":[0.99973065,0.000073806594,0.000046883913,0.000025084692,0.00008985033,0.000033719945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001835366,0.00022133427,0.0001913023,0.0002051913,0.00013670523,0.00034114753,0.00021592574,0.0001969156,0.001013446],"category_scores_gemma":[0.0007737384,0.0002080586,0.00021198438,0.00020352281,0.00018768053,0.00028183032,0.00034446694,0.00039314883,0.00020511913],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066567486,0.000037036203,0.089248635,0.00016400623,0.000039117203,0.00010580417,0.00028904472,0.007224755,0.88466805,0.0005920928,0.00015338683,0.01681243],"study_design_scores_gemma":[0.000049526934,0.0005898509,0.3284433,0.00001860302,0.000043390897,0.00011939048,0.00041402207,0.023712417,0.6438547,0.00046253708,0.0022492446,0.00004308444],"about_ca_topic_score_codex":0.01467551,"about_ca_topic_score_gemma":0.010171361,"teacher_disagreement_score":0.01467551,"about_ca_system_score_codex":0.00059132016,"about_ca_system_score_gemma":0.00024784982,"threshold_uncertainty_score":0.02918017},"labels":[],"label_agreement":null},{"id":"W1749774267","doi":"10.1002/2013gl058581","title":"Spatial localization and ducting of EMIC waves: Van Allen Probes and ground‐based observations","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Van Allen Probes; Plasmasphere; Physics; Geophysics; Van Allen radiation belt; Elliptical polarization; Magnetometer; Polarization (electrochemistry); Earth's magnetic field; Computational physics; Ionosphere; Magnetosphere; Geology; Geodesy; Astrophysics; Magnetic field; Optics; Linear polarization","score_opus":0.023784059769343738,"score_gpt":0.2744956841875738,"score_spread":0.2507116244182301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1749774267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913872,0.000115129646,0.0015645273,0.00005788806,0.00000782839,0.000018121842,0.0013462324,0.00006196171,0.00544118],"genre_scores_gemma":[0.9961372,0.000045905865,0.0017955416,0.000018382625,0.000005212157,0.00000996895,0.0015011507,0.000010523376,0.00047606684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998673,0.000020636908,0.000003472155,0.000044765293,0.000033991393,0.000029797684],"domain_scores_gemma":[0.9998703,0.00002144729,0.000031429678,0.0000131671,0.000040091894,0.000023589993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016677375,0.0001372948,0.00012029914,0.00060290546,0.00019457645,0.00040668048,0.00035687943,0.00022205825,0.0006184982],"category_scores_gemma":[0.00033163032,0.00013727398,0.00008881307,0.0007013649,0.00014692415,0.00029059357,0.00026775966,0.00024723972,0.0001340584],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042851115,0.0001420297,0.7767298,0.00007128059,0.000144056,0.00027941435,0.0013551652,0.005970349,0.15171047,0.0011436923,0.0024647815,0.059560537],"study_design_scores_gemma":[0.000023142351,0.000082540326,0.977825,0.000017253313,0.00002504897,0.00009326261,0.00040225335,0.009965935,0.0072845654,0.00014368653,0.004123877,0.0000133802705],"about_ca_topic_score_codex":0.041068275,"about_ca_topic_score_gemma":0.09882084,"teacher_disagreement_score":0.041068275,"about_ca_system_score_codex":0.00039459535,"about_ca_system_score_gemma":0.00028273943,"threshold_uncertainty_score":0.08165848},"labels":[],"label_agreement":null},{"id":"W1766139619","doi":"10.1029/2010gl045052","title":"Importance of location for describing typical and extreme wind speed behavior","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Wind speed; Environmental science; Meteorology; Wind power; Climate change; Climatology; Global wind patterns; Percentile; Extreme value theory; Atmospheric sciences; Geography; Geology; Oceanography; Statistics; Mathematics; Ecology","score_opus":0.11505582955195186,"score_gpt":0.331855137415424,"score_spread":0.21679930786347212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1766139619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8828453,0.0007970788,0.1068376,0.00018721941,0.00005921396,0.000096310185,0.0018090523,0.0005159837,0.006852272],"genre_scores_gemma":[0.990948,0.00012572017,0.007988639,0.000014209224,0.000024679794,0.000026986467,0.0005997065,0.00003106639,0.00024093849],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993505,0.00027400497,0.00008329936,0.00014628447,0.00008772847,0.000058257574],"domain_scores_gemma":[0.99492705,0.002812646,0.001045249,0.00072001567,0.00034354563,0.00015144153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001251284,0.00049757614,0.00045493263,0.0011859698,0.00025367294,0.0010170523,0.0005016357,0.0005637589,0.0012424423],"category_scores_gemma":[0.007726199,0.00018494761,0.00040847354,0.0013086973,0.00045461443,0.0017436991,0.0005920234,0.000418421,0.0006620829],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041186897,0.00008470032,0.8132791,0.00018516065,0.00017582027,0.00038056631,0.00041951076,0.107337475,0.0044564735,0.0031829472,0.0008355812,0.069250785],"study_design_scores_gemma":[0.00003214536,0.00034041965,0.6382112,0.00009868699,0.00012557278,0.0013843887,0.0010592442,0.34307197,0.0019315426,0.009264642,0.0043469057,0.00013342535],"about_ca_topic_score_codex":0.0025645006,"about_ca_topic_score_gemma":0.002695615,"teacher_disagreement_score":0.0025645006,"about_ca_system_score_codex":0.00017888003,"about_ca_system_score_gemma":0.00020283913,"threshold_uncertainty_score":0.0066174865},"labels":[],"label_agreement":null},{"id":"W1767738953","doi":"10.1002/2015gl064838","title":"Assessment of thermal change in cold avalanching glaciers in relation to climate warming","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Glacier; Climate change; Geology; Firn; Climatology; Temperate climate; Global warming; Glacier mass balance; Physical geography; Glacier morphology; Surge; Rock glacier; Environmental science; Geomorphology; Cryosphere; Ice stream; Oceanography; Geography; Sea ice","score_opus":0.10341746794805441,"score_gpt":0.35271136007190174,"score_spread":0.24929389212384734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1767738953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875,0.00007122388,0.0002646546,0.000025507312,0.0000026518287,0.00000555047,0.0003521409,0.000017832328,0.0005104662],"genre_scores_gemma":[0.99954516,0.000019740519,0.00009846135,0.0000052311357,0.0000023509465,0.0000031043862,0.00023105157,0.000001753107,0.00009317308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000028156956,0.000004883272,0.000025579806,0.000019094095,0.000019244053],"domain_scores_gemma":[0.9996451,0.000094004004,0.00008375621,0.00002958884,0.00008881923,0.000058716512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003807429,0.00030263275,0.00016867238,0.00076316285,0.0003065162,0.0006116737,0.0001629165,0.0003744506,0.0009563294],"category_scores_gemma":[0.00052565796,0.000093459734,0.00036982188,0.0006436813,0.00019385792,0.0003065562,0.00025098975,0.00026102253,0.00011584022],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004866207,0.00007218824,0.9382747,0.000036191268,0.00014308833,0.0001100078,0.00010449693,0.043631885,0.009711086,0.00015478281,0.00019876745,0.0070763645],"study_design_scores_gemma":[0.0000060728503,0.00010025322,0.98103344,0.000003610226,0.000022385673,0.000031269763,0.000118462114,0.017451823,0.0008871946,0.000095859556,0.00024136005,0.000008222485],"about_ca_topic_score_codex":0.026942411,"about_ca_topic_score_gemma":0.019664828,"teacher_disagreement_score":0.026942411,"about_ca_system_score_codex":0.00082406786,"about_ca_system_score_gemma":0.00018013499,"threshold_uncertainty_score":0.053571165},"labels":[],"label_agreement":null},{"id":"W1768487093","doi":"10.1002/grl.50285","title":"Detecting human influence on extreme temperatures in China","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China","keywords":"Forcing (mathematics); Environmental science; Climatology; Greenhouse gas; Atmospheric sciences; Radiative forcing; Solar irradiance; Solar variation; Natural (archaeology); Climate change; Geology","score_opus":0.04411968517716412,"score_gpt":0.313305635667714,"score_spread":0.2691859504905499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1768487093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99910945,0.000031052015,0.00042181733,0.000030250163,0.0000032448131,0.0000019666356,0.0001480567,0.000015142264,0.00023904747],"genre_scores_gemma":[0.99975544,0.000012113923,0.00008574723,0.0000025965899,0.0000019250122,0.0000011824826,0.00011443617,0.0000010331477,0.000025509868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998111,0.000052380474,0.000009788542,0.000062529456,0.000026933063,0.00003729072],"domain_scores_gemma":[0.9996457,0.00010274654,0.00008881371,0.00004341941,0.000071726936,0.00004757692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005426865,0.0003377517,0.00027472642,0.0005345519,0.00022049385,0.00049131166,0.0002844702,0.00019958768,0.0004928274],"category_scores_gemma":[0.0010630332,0.00016293887,0.00039892073,0.0006432278,0.0003771017,0.00034630095,0.00039456057,0.00014538865,0.00004585376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028737372,0.00005511801,0.81664735,0.00005050061,0.0002137043,0.00021869331,0.00019530654,0.16615899,0.0033693286,0.000609391,0.0005018875,0.011692455],"study_design_scores_gemma":[0.000031641615,0.00003966269,0.7656743,0.000011082903,0.00006465288,0.000036108606,0.00013782056,0.2319372,0.0012532476,0.00035926764,0.00043216778,0.000022902961],"about_ca_topic_score_codex":0.039843008,"about_ca_topic_score_gemma":0.035928883,"teacher_disagreement_score":0.039843008,"about_ca_system_score_codex":0.000773773,"about_ca_system_score_gemma":0.0006054626,"threshold_uncertainty_score":0.0792222},"labels":[],"label_agreement":null},{"id":"W1769631967","doi":"10.1029/2011gl048325","title":"Spatial reorganization in the equatorial divergence in the Eastern Tropical Pacific during the last 150 kyr","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences; Canadian Institute for Advanced Research","keywords":"Geology; Divergence (linguistics); Climatology; Oceanography; Geography","score_opus":0.042987735511857326,"score_gpt":0.2649953962528988,"score_spread":0.22200766074104147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1769631967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865353,0.000338548,0.00006930477,0.000048710874,0.0000032808064,0.0000024951967,0.00023697632,0.000004160861,0.00064281805],"genre_scores_gemma":[0.9991961,0.00019173541,0.00010872992,0.000018713932,0.0000074878612,0.000004000055,0.00035041774,0.0000023505647,0.00012043675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991214,0.000010519985,0.000007720912,0.00004176318,0.000010274045,0.000017537397],"domain_scores_gemma":[0.99961406,0.000040524785,0.00018567876,0.000021686496,0.00008661165,0.000051474264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000257294,0.00010644683,0.00014929689,0.00096619996,0.0004012748,0.00054710003,0.00018793716,0.00018034775,0.00095127866],"category_scores_gemma":[0.00066281174,0.00012478894,0.00012593724,0.0012687318,0.0004187929,0.00028110523,0.0005381146,0.00015987732,0.00010000524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000095261676,0.00000982105,0.9791412,0.000050781375,0.000081084894,0.0001534439,0.001384899,0.00017581998,0.010346836,0.00015278696,0.00020432015,0.0082038585],"study_design_scores_gemma":[9.248675e-7,0.000002927831,0.9995161,0.000002935542,0.0000047624835,0.000025079908,0.00013279132,0.0000359894,0.000055706932,0.000008436066,0.00021343918,0.0000010334384],"about_ca_topic_score_codex":0.031846512,"about_ca_topic_score_gemma":0.067060865,"teacher_disagreement_score":0.031846512,"about_ca_system_score_codex":0.00042191142,"about_ca_system_score_gemma":0.0003449199,"threshold_uncertainty_score":0.063322306},"labels":[],"label_agreement":null},{"id":"W1770103121","doi":"10.1002/2014gl060787","title":"Modeling cross L shell impacts of magnetopause shadowing and ULF wave radial diffusion in the Van Allen belts","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science and Technology Facilities Council; European Commission; Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Alberta Innovates; FP7 Space; National Aeronautics and Space Administration","keywords":"Van Allen radiation belt; Magnetopause; Plasmasphere; Van Allen Probes; Physics; Geophysics; Magnetosphere; Computational physics; Geomagnetic storm; Space weather; Flux (metallurgy); Diffusion; Geomagnetically induced current; Solar wind; Plasma","score_opus":0.019075311062163446,"score_gpt":0.28915459549784256,"score_spread":0.27007928443567913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1770103121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99011517,0.000061800594,0.005051903,0.00015338653,0.00001452918,0.000012514309,0.0001154587,0.00009389341,0.004381269],"genre_scores_gemma":[0.9987023,0.000025997104,0.0006938925,0.000017965436,0.0000042913657,0.000006401883,0.000038116417,0.000016248478,0.00049472897],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999198,0.0000239459,0.0000032447886,0.00001093703,0.000009824528,0.000032292068],"domain_scores_gemma":[0.9996903,0.00013180602,0.00005587841,0.000026666372,0.00003765862,0.000057660975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034363449,0.00042436202,0.0004196839,0.00033537953,0.00037247236,0.0008077456,0.00092069997,0.0009222053,0.0013364442],"category_scores_gemma":[0.0011779021,0.00028704887,0.0005856496,0.00027123606,0.0005344735,0.0006005684,0.00065202935,0.00047446176,0.00011875252],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060206134,0.000035249523,0.004612554,0.0000070058973,0.000016635968,0.00009606006,0.00003791696,0.99124473,0.0019316906,0.0010849964,0.000095492105,0.00077750045],"study_design_scores_gemma":[0.000022110467,0.00001607801,0.0009690988,0.0000015322698,0.0000039646916,0.0000076192196,0.000018732888,0.9984403,0.00026041284,0.0001649654,0.00009107709,0.0000040286513],"about_ca_topic_score_codex":0.05113431,"about_ca_topic_score_gemma":0.014011997,"teacher_disagreement_score":0.05113431,"about_ca_system_score_codex":0.0012105383,"about_ca_system_score_gemma":0.00066402473,"threshold_uncertainty_score":0.101673365},"labels":[],"label_agreement":null},{"id":"W1770659215","doi":"10.1029/2012gl050890","title":"The Arctic Ocean warms from below","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Office of Polar Programs; Fisheries and Oceans Canada","keywords":"Geothermal gradient; Geology; Structural basin; Convection; Geothermal heating; Heat flux; Heat transfer; Water column; Arctic; Canada Basin; Deep water; Flux (metallurgy); The arctic; Petrology; Geomorphology; Geothermal energy; Oceanography; Geophysics; Meteorology; Mechanics; Materials science","score_opus":0.03842939123386859,"score_gpt":0.294887002116648,"score_spread":0.2564576108827794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1770659215","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89625365,0.008686057,0.0027035193,0.0009667637,0.0002891608,0.00002521171,0.0060292645,0.0005011765,0.084545195],"genre_scores_gemma":[0.9833165,0.0028707131,0.0010565,0.00023319697,0.00006683862,0.0000068987906,0.0023852955,0.000037012473,0.010027029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994385,0.000004863917,0.000002419115,0.000016419715,0.000013982516,0.000018556959],"domain_scores_gemma":[0.99990964,0.000006098009,0.000020407968,0.000007593671,0.000034555025,0.000021669313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008325625,0.00024902445,0.00013115568,0.0003145315,0.0006921626,0.0008541039,0.00009671312,0.00013559149,0.0030006177],"category_scores_gemma":[0.00014292203,0.0000734982,0.00013442425,0.0004263243,0.00017876511,0.00026113802,0.0004825336,0.0002236459,0.0015088143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047699115,0.000074790434,0.46967253,0.00053846213,0.00025384367,0.0009770902,0.0027116947,0.0016973722,0.07835497,0.0059816027,0.020764088,0.41849658],"study_design_scores_gemma":[0.000006695919,0.00005570514,0.8278209,0.0001015843,0.000045504592,0.00028757827,0.0009083959,0.0002728214,0.0039308155,0.0004425429,0.16610613,0.000021310983],"about_ca_topic_score_codex":0.061331727,"about_ca_topic_score_gemma":0.11178629,"teacher_disagreement_score":0.061331727,"about_ca_system_score_codex":0.0007601521,"about_ca_system_score_gemma":0.0008777823,"threshold_uncertainty_score":0.121949434},"labels":[],"label_agreement":null},{"id":"W1773518713","doi":"10.1002/grl.51010","title":"Attributing intensification of precipitation extremes to human influence","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":351,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria; Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Precipitation; Coupled model intercomparison project; Environmental science; Climatology; Northern Hemisphere; Southern Hemisphere; Atmospheric sciences; Climate model; Climate change; Mean radiant temperature; Meteorology; Geography; Geology; Oceanography","score_opus":0.07356488872650761,"score_gpt":0.3441001417048041,"score_spread":0.27053525297829645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1773518713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998953,0.00011080169,0.00025369655,0.00004336438,0.000002032925,7.5924527e-7,0.000045275083,0.000005219328,0.00058577064],"genre_scores_gemma":[0.99982977,0.000046646197,0.000047153444,0.000005159643,0.0000063207744,3.5032642e-7,0.000034735694,5.2880057e-7,0.000029379014],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999793,0.00006291348,0.000010336542,0.000066163426,0.000034685327,0.000032911677],"domain_scores_gemma":[0.9990951,0.0002596823,0.00038391628,0.00011437464,0.000085451735,0.0000616475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039430583,0.000098181285,0.000118479824,0.00052235,0.00013431188,0.00035211066,0.00012188623,0.00013887906,0.0006054487],"category_scores_gemma":[0.0017098937,0.00011812132,0.00014195175,0.00038869958,0.00040202946,0.00022262151,0.00053507526,0.00021521846,0.000045941477],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006624364,0.000006526575,0.9901426,0.0000096721815,0.00005387008,0.00005209887,0.00015547799,0.0019309105,0.0008570852,0.00013572727,0.000078090416,0.006511658],"study_design_scores_gemma":[0.0000011136402,0.000008451981,0.99786586,0.0000031680759,0.000007907068,0.000053930966,0.00007951605,0.0014702281,0.00015113504,0.00013588104,0.00022054515,0.0000023562143],"about_ca_topic_score_codex":0.00780189,"about_ca_topic_score_gemma":0.012437184,"teacher_disagreement_score":0.00780189,"about_ca_system_score_codex":0.00033586397,"about_ca_system_score_gemma":0.00012406768,"threshold_uncertainty_score":0.015512943},"labels":[],"label_agreement":null},{"id":"W1782129337","doi":"10.1029/2003gl019113","title":"Polar cap index comparisons with AMIE cross polar cap potential, electric field, and polar cap area","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Michigan; Canadian Space Agency; National Science Foundation","keywords":"Polar; Ionosphere; Electric field; Polar cap; Conventional PCI; Latitude; Atmospheric sciences; Physics; Geodesy; Geophysics; Computational physics; Geology; Astronomy","score_opus":0.011163506267731275,"score_gpt":0.2734929390590481,"score_spread":0.2623294327913168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1782129337","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8810293,0.00081513706,0.04938837,0.00036319657,0.000092626244,0.000072324685,0.0042843325,0.001459937,0.062494677],"genre_scores_gemma":[0.98955256,0.0001838882,0.0069708056,0.00003342653,0.00004123636,0.000025341587,0.0021235105,0.00008635969,0.0009828339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978393,0.000040102354,0.00001636789,0.000059439964,0.00008127301,0.000018928056],"domain_scores_gemma":[0.9991053,0.00024932396,0.00014745172,0.00012312453,0.0003304761,0.000044328084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069758884,0.0003395045,0.00030178105,0.0011131719,0.00027170117,0.0010791457,0.00026739767,0.00025431687,0.0018129349],"category_scores_gemma":[0.0029839068,0.00016056419,0.0003018438,0.0017264796,0.00026961384,0.0012233317,0.00064139557,0.00033979642,0.000460544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003586616,0.00007300773,0.52446926,0.00018050933,0.00036251495,0.000264017,0.0004383347,0.32494566,0.018773232,0.011063057,0.0069988933,0.11207279],"study_design_scores_gemma":[0.000053074105,0.00009377329,0.61067194,0.000032939,0.00008500862,0.0002475746,0.00029913848,0.35596913,0.014416627,0.004942311,0.013112356,0.00007620328],"about_ca_topic_score_codex":0.008020594,"about_ca_topic_score_gemma":0.006142183,"teacher_disagreement_score":0.008020594,"about_ca_system_score_codex":0.00040953662,"about_ca_system_score_gemma":0.00028564644,"threshold_uncertainty_score":0.015947819},"labels":[],"label_agreement":null},{"id":"W1784670537","doi":"10.1029/2009gl041375","title":"Pan‐Arctic sunphotometry during the ARCTAS‐A campaign of April 2008","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Environment and Climate Change Canada; York University; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; U.S. Department of Energy; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Environmental science; Aerosol; Arctic; Climatology; Smoke; The arctic; Atmospheric sciences; Meteorology; Geology; Geography; Oceanography","score_opus":0.013102204459532474,"score_gpt":0.2721381171064066,"score_spread":0.25903591264687414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1784670537","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98065096,0.0002275194,0.0006610098,0.000036445585,0.0000466244,0.000022381746,0.013659271,0.00012003205,0.004575811],"genre_scores_gemma":[0.9722845,0.0003460007,0.003468205,0.00003360227,0.00006255636,0.000034264005,0.02088751,0.000043469186,0.0028398533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998586,0.000021816506,0.0000065983227,0.000043004686,0.000048756076,0.000021259486],"domain_scores_gemma":[0.9998412,0.000012837459,0.000030620307,0.000017015711,0.000071746574,0.000026497319],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002671831,0.00030448727,0.000214277,0.00056585437,0.0003455555,0.00029627132,0.00012309889,0.00013937494,0.0008221235],"category_scores_gemma":[0.00015919445,0.000108752145,0.00012542192,0.0005014409,0.00008545563,0.00015958915,0.00020613414,0.0001241677,0.00023504684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026931898,0.00026973264,0.8490156,0.00028979406,0.0004347885,0.0005444319,0.0014630614,0.006927434,0.06374974,0.00064011704,0.013210501,0.060761567],"study_design_scores_gemma":[0.00003811577,0.00007513364,0.9819296,0.00001218926,0.00005047391,0.00007525692,0.0001322035,0.0021494487,0.004977854,0.00003757447,0.010509334,0.000012790435],"about_ca_topic_score_codex":0.06059264,"about_ca_topic_score_gemma":0.14263216,"teacher_disagreement_score":0.06059264,"about_ca_system_score_codex":0.00039493424,"about_ca_system_score_gemma":0.00042176966,"threshold_uncertainty_score":0.12047994},"labels":[],"label_agreement":null},{"id":"W1794191941","doi":"10.1002/2015gl063198","title":"Multiple carriers of Q noble gases in primitive meteorites","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Meteorite; Chondrite; Noble gas; Phase (matter); Noble metal; Solar System; Carbonaceous chondrite; Gas phase; Parent body","score_opus":0.05342942811869127,"score_gpt":0.3152283635988373,"score_spread":0.26179893548014604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1794191941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99954706,0.00008087856,0.00016284516,0.00000473487,9.846387e-7,0.0000016284205,0.0000186638,0.000006491605,0.00017667658],"genre_scores_gemma":[0.9996886,0.000022947115,0.00011399186,0.0000021916126,0.0000014231423,7.6024793e-7,0.00002980762,0.0000023170082,0.00013785243],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.0000044147982,0.0000033170709,0.000025820973,0.000013007247,0.000014452834],"domain_scores_gemma":[0.9999018,0.000017636892,0.000027985425,0.0000088295,0.000021990303,0.00002183131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010556367,0.00015826756,0.00016457887,0.0005654335,0.00034687706,0.0004820564,0.00020448897,0.0002192028,0.00043816818],"category_scores_gemma":[0.00016218044,0.00016727383,0.00010374593,0.00022241913,0.0004297333,0.00029715674,0.00030463564,0.00017605552,0.00008484712],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004740132,0.00002136984,0.06114756,0.000041309224,0.000025367997,0.00060233276,0.00031158314,0.00034535123,0.93320066,0.00062775466,0.00003936626,0.0031632527],"study_design_scores_gemma":[0.00007508006,0.00095064053,0.5090896,0.000015810825,0.00008627326,0.0017783914,0.0010370021,0.008820092,0.47338417,0.001271718,0.0034600343,0.000031309282],"about_ca_topic_score_codex":0.002774147,"about_ca_topic_score_gemma":0.0019042477,"teacher_disagreement_score":0.002774147,"about_ca_system_score_codex":0.0003299916,"about_ca_system_score_gemma":0.00015634061,"threshold_uncertainty_score":0.005515933},"labels":[],"label_agreement":null},{"id":"W1800977649","doi":"10.1029/2011gl050355","title":"Net carbon accumulation of a high‐latitude permafrost palsa mire similar to permafrost‐free peatlands","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ste. Anne's Hospital; University of Guelph; McGill University","funders":"Vetenskapsrådet; Sweden-America Foundation; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Permafrost; Subarctic climate; Mire; Peat; Environmental science; Climate change; Boreal; Ecosystem; Physical geography; Geology; Ecology; Oceanography; Geography","score_opus":0.11735516468679943,"score_gpt":0.3501217347213294,"score_spread":0.23276657003452997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1800977649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99896884,0.00002614354,0.00007347425,0.000006408437,8.80413e-7,0.0000011838848,0.00022792073,0.000007309889,0.00068788993],"genre_scores_gemma":[0.9991135,0.00003515985,0.00020402038,0.000006116804,0.0000016011924,0.0000047119097,0.0003890729,0.0000030996796,0.0002427527],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999703,0.0000043003483,0.0000020370092,0.000010974163,0.0000053116137,0.0000070048745],"domain_scores_gemma":[0.99989736,0.000020034058,0.000032158616,0.000009756839,0.000018390352,0.000022332946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014643001,0.00019032093,0.00015722713,0.00048263505,0.0002820236,0.00042805538,0.00014520534,0.00012508524,0.0013531562],"category_scores_gemma":[0.0001521109,0.00011640606,0.00011795327,0.00026819555,0.00021947408,0.0003124993,0.00021826307,0.000110863126,0.00018482386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042118263,0.000050572366,0.8505363,0.00007450626,0.00009930999,0.00033878305,0.00037921607,0.001427017,0.13433903,0.00030557165,0.00020868136,0.011819848],"study_design_scores_gemma":[0.000003167947,0.000030085117,0.9962469,0.0000034418972,0.000011087654,0.00007576805,0.00012460389,0.0007149997,0.0022940054,0.000042629123,0.00044958285,0.0000036732847],"about_ca_topic_score_codex":0.0041812533,"about_ca_topic_score_gemma":0.010432206,"teacher_disagreement_score":0.0041812533,"about_ca_system_score_codex":0.0002948666,"about_ca_system_score_gemma":0.00015557624,"threshold_uncertainty_score":0.008313835},"labels":[],"label_agreement":null},{"id":"W1806024449","doi":"10.1029/2009gl038671","title":"Ozone hole and Southern Hemisphere climate change","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":242,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Ozone depletion; Stratosphere; Tropopause; Hadley cell; Climatology; Environmental science; Climate change; Greenhouse gas; Atmospheric sciences; Ozone layer; Polar vortex; Climate model; Jet stream; Atmospheric circulation; Global warming; Northern Hemisphere; Forcing (mathematics); Southern Hemisphere; General Circulation Model; Geology; Jet (fluid)","score_opus":0.038204297867627336,"score_gpt":0.28354177916021384,"score_spread":0.2453374812925865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1806024449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9002825,0.029180812,0.0013161905,0.018003464,0.0003869591,0.000020164462,0.0039359783,0.00012425105,0.04674964],"genre_scores_gemma":[0.99362093,0.0037795503,0.00013532108,0.00032830553,0.000077535435,0.0000037589903,0.0004562829,0.0000056547537,0.001592564],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999362,0.000016042686,0.0000021009216,0.000009848075,0.000010576673,0.00002516289],"domain_scores_gemma":[0.999814,0.000028480237,0.00007595614,0.000010328245,0.000028302995,0.000043036573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032549293,0.00011738026,0.00013677121,0.00037369962,0.00023680407,0.0007851705,0.00017910411,0.00035926627,0.0046000998],"category_scores_gemma":[0.0005377149,0.000046967656,0.00017870375,0.0006654169,0.00025889993,0.00048269215,0.00046324826,0.000352066,0.00018104483],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008950458,0.00013360487,0.71871823,0.00037267036,0.000530247,0.0008306653,0.001119565,0.010007641,0.005846933,0.07862435,0.041899756,0.14102133],"study_design_scores_gemma":[0.00004642621,0.00006545783,0.91971266,0.00006727984,0.00007655081,0.00010665168,0.00084782165,0.0027119438,0.00043735153,0.031060213,0.044849325,0.000018325996],"about_ca_topic_score_codex":0.037757352,"about_ca_topic_score_gemma":0.038812876,"teacher_disagreement_score":0.037757352,"about_ca_system_score_codex":0.0006498509,"about_ca_system_score_gemma":0.0004925008,"threshold_uncertainty_score":0.07507515},"labels":[],"label_agreement":null},{"id":"W1809108046","doi":"10.1002/grl.50260","title":"Dense bottom layers in the Scotia Sea, Southern Ocean: Creation, lifespan, and destruction","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Oceanography; Stratification (seeds); Nova scotia; Ridge; Bottom water; Circumpolar deep water; Deep sea; Thermohaline circulation; Mixed layer; Water column; Climatology; Paleontology; North Atlantic Deep Water","score_opus":0.015873782474726653,"score_gpt":0.24904352880287411,"score_spread":0.23316974632814746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1809108046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942744,0.000076909586,0.00002129769,0.0000064415995,7.0428615e-7,0.000001921047,0.00015729437,0.0000010635449,0.00030694908],"genre_scores_gemma":[0.99972576,0.000036229834,0.00002586949,0.000001954273,5.113378e-7,8.1455187e-7,0.000073909345,3.268401e-7,0.00013465241],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999503,0.0000048333377,0.0000043620867,0.0000085457,0.000010434276,0.000021404458],"domain_scores_gemma":[0.9994772,0.000067214176,0.000213494,0.000033499047,0.00008345227,0.00012522748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022275421,0.000110506386,0.00008151225,0.0006549572,0.0003036654,0.0003971828,0.000105253785,0.00008296499,0.00066888396],"category_scores_gemma":[0.0006692363,0.00010201949,0.0000774114,0.00038605975,0.0002568734,0.00013989717,0.00042743664,0.000095940166,0.000073269795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114654315,0.000006432576,0.98798263,0.000015286936,0.000021087624,0.00014321283,0.00030669686,0.00024791303,0.007645302,0.0001077205,0.000052592186,0.0033564344],"study_design_scores_gemma":[9.034118e-7,0.000010729054,0.99939966,0.0000023912442,0.0000028961276,0.00003109906,0.00014185513,0.00009891738,0.0001762302,0.000020838223,0.00011327033,0.0000011316054],"about_ca_topic_score_codex":0.11751733,"about_ca_topic_score_gemma":0.2021519,"teacher_disagreement_score":0.11751733,"about_ca_system_score_codex":0.00077364553,"about_ca_system_score_gemma":0.0004271822,"threshold_uncertainty_score":0.2336666},"labels":[],"label_agreement":null},{"id":"W1809829952","doi":"10.1029/2008gl033520","title":"An improved bathymetric portrayal of the Arctic Ocean: Implications for ocean modeling and geological, geophysical and oceanographic analyses","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":520,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Oceanic and Atmospheric Administration; Stockholms Universitet; Vetenskapsrådet; Knut och Alice Wallenbergs Stiftelse; Polarforskningssekretariatet","keywords":"Stereographic projection; Bathymetry; Bathymetric chart; Geology; Arctic; Seafloor spreading; The arctic; Oceanography; Seabed; Ocean surface topography; Geophysics","score_opus":0.06780791780277477,"score_gpt":0.3289461450252304,"score_spread":0.2611382272224556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1809829952","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22485685,0.002545402,0.72720766,0.0018338817,0.0005816861,0.00006700717,0.01038828,0.0017794018,0.030739725],"genre_scores_gemma":[0.60063714,0.0033368885,0.3890237,0.00012641668,0.00017773407,0.000039504648,0.0038272997,0.0002630645,0.0025683062],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998709,0.00003823628,0.000011652136,0.000016438886,0.000051245053,0.000011528911],"domain_scores_gemma":[0.99947447,0.00010533644,0.000083784806,0.00011071636,0.00018422035,0.00004155904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048053905,0.00029443848,0.00026036834,0.0010088865,0.00024847634,0.0015844316,0.00036024163,0.00021464385,0.0016399341],"category_scores_gemma":[0.0019879634,0.00013738057,0.000192579,0.0016552442,0.00046148666,0.0011553884,0.0006493079,0.00045676174,0.0002522644],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019619364,0.000051568244,0.08024787,0.00031737253,0.00009616739,0.00033169158,0.0007338016,0.3606051,0.029079966,0.09731448,0.016338255,0.41468754],"study_design_scores_gemma":[0.00004201706,0.00008189282,0.1522728,0.0002958302,0.0001222726,0.0006379863,0.0017623114,0.6057652,0.011878898,0.058870263,0.16803762,0.00023294779],"about_ca_topic_score_codex":0.025137318,"about_ca_topic_score_gemma":0.03925804,"teacher_disagreement_score":0.025137318,"about_ca_system_score_codex":0.0003936632,"about_ca_system_score_gemma":0.0007248054,"threshold_uncertainty_score":0.04998195},"labels":[],"label_agreement":null},{"id":"W1814429163","doi":"10.1029/2010gl042831","title":"Arctic organic aerosol measurements show particles from mixed combustion in spring haze and from frost flowers in winter","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Aerosol; Haze; Environmental science; Sea salt; Atmospheric sciences; Air mass (solar energy); Arctic; Environmental chemistry; Organic matter; Oceanography; Geology; Chemistry; Meteorology; Geography","score_opus":0.03600757045345334,"score_gpt":0.25676325713912357,"score_spread":0.22075568668567022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1814429163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778324,0.00011853103,0.00015350411,0.00001134272,0.000009279571,0.0000035315422,0.0008106447,0.000018079676,0.0010917899],"genre_scores_gemma":[0.99721885,0.00008498954,0.00043792799,0.000019854191,0.000009551289,0.0000051989214,0.0014749916,0.000008511976,0.00074019877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000002170905,0.0000033775036,0.00001832824,0.000023749333,0.000014505275],"domain_scores_gemma":[0.99991846,0.000009976527,0.000016653452,0.0000036880601,0.00002301938,0.000028182023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093935254,0.00032673968,0.00015997553,0.0005057657,0.00056522933,0.00032751777,0.00014259969,0.00024749656,0.00083493313],"category_scores_gemma":[0.00010520612,0.00015420331,0.00022600881,0.00030007516,0.00011734399,0.00011843723,0.00019065349,0.00020243127,0.00017590568],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008707619,0.000103522005,0.6861895,0.00008466926,0.00018984132,0.0008615674,0.00065238297,0.00073622074,0.29433236,0.00011295668,0.0010640809,0.014802186],"study_design_scores_gemma":[0.0000026005096,0.000024578585,0.9946273,0.0000031873476,0.000013292196,0.000067810994,0.00009270086,0.00027202422,0.004492552,0.000010320686,0.0003905153,0.000003041858],"about_ca_topic_score_codex":0.044011015,"about_ca_topic_score_gemma":0.09584359,"teacher_disagreement_score":0.044011015,"about_ca_system_score_codex":0.0003466113,"about_ca_system_score_gemma":0.00017352792,"threshold_uncertainty_score":0.08750969},"labels":[],"label_agreement":null},{"id":"W1819371092","doi":"10.1002/2015gl063987","title":"Surface motions and intraplate continental deformation in Alaska driven by mantle flow","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"American Chemical Society Petroleum Research Fund; National Science Foundation","keywords":"Geology; Lithosphere; Geodynamics; Plate tectonics; Mantle (geology); Intraplate earthquake; Convergent boundary; Mantle convection; Geophysics; Subduction; North American Plate; Seismology; Oceanic crust; Tectonics","score_opus":0.027150973851457837,"score_gpt":0.25385904842666585,"score_spread":0.226708074575208,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1819371092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995327,0.000011732579,0.00016089929,0.0000063510615,6.739152e-7,3.1253833e-7,0.00001835159,0.0000033312124,0.00026567024],"genre_scores_gemma":[0.9998331,0.000009096435,0.00007085355,9.877444e-7,4.1212635e-7,2.3011555e-7,0.000019191317,6.7751563e-7,0.000065577085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997866,0.0000041671606,0.0000021457909,0.000006630385,0.000003878099,0.0000044115436],"domain_scores_gemma":[0.9999484,0.000012066504,0.0000137428315,0.0000052752616,0.000009470673,0.00001111542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009866614,0.00012230934,0.00010737987,0.00036554557,0.0002532474,0.00037624603,0.00012594601,0.00014984369,0.00075775926],"category_scores_gemma":[0.000296105,0.00011520945,0.00013273781,0.00022429274,0.0002468426,0.00021841067,0.00027876193,0.00014092958,0.000079040976],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025637317,0.000058021094,0.8763316,0.000023518734,0.00010361348,0.00035557523,0.00051272195,0.063017845,0.048351843,0.0012329414,0.000101437756,0.009654441],"study_design_scores_gemma":[0.000010245232,0.000044567096,0.9322003,0.000008235503,0.000027200898,0.00006923362,0.00047213837,0.06364649,0.002492161,0.0007704849,0.00024635784,0.000012570367],"about_ca_topic_score_codex":0.037231214,"about_ca_topic_score_gemma":0.047511518,"teacher_disagreement_score":0.037231214,"about_ca_system_score_codex":0.00034021813,"about_ca_system_score_gemma":0.00019167586,"threshold_uncertainty_score":0.07402897},"labels":[],"label_agreement":null},{"id":"W1819426174","doi":"10.1029/2011gl047339","title":"Does earlier snowmelt lead to greater CO <sub>2</sub> sequestration in two low Arctic tundra ecosystems?","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Trent University; Carleton University","funders":"","keywords":"Tundra; Snowmelt; Environmental science; Arctic; Ecosystem; Snow; Growing season; Overwintering; Terrestrial ecosystem; Atmospheric sciences; Eddy covariance; Climatology; Physical geography; Ecology; Geography; Biology; Geology","score_opus":0.07801018911059408,"score_gpt":0.3103538521150217,"score_spread":0.2323436630044276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1819426174","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997842,0.000043608525,0.000021020522,0.000016488422,8.383667e-7,8.040456e-7,0.000047393165,0.0000016450812,0.00008405114],"genre_scores_gemma":[0.9997304,0.00002608437,0.000052967418,0.000015733745,8.8902823e-7,9.870064e-7,0.00010763176,0.0000011514827,0.000064149404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983287,0.000045035915,0.000009095296,0.000038215287,0.0000120958475,0.00006269647],"domain_scores_gemma":[0.999481,0.00008843195,0.00015888739,0.000030869654,0.00007437356,0.00016638651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005896127,0.00024126226,0.00028544798,0.000584079,0.0006468922,0.0009529954,0.00035535172,0.00034089296,0.00066775345],"category_scores_gemma":[0.0006340526,0.00017633072,0.00035995446,0.0005181316,0.0005864107,0.00032655313,0.00032028544,0.00018057729,0.00007003453],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044652677,0.000056748537,0.9829594,0.000022980144,0.00017315356,0.00015564656,0.00028926396,0.00033409838,0.01335079,0.00008470737,0.00006353771,0.0020631228],"study_design_scores_gemma":[0.0000035544135,0.000024276766,0.9985677,0.0000019212807,0.000023190514,0.000027663158,0.0003192665,0.0005633825,0.00036044588,0.00003154406,0.000074085045,0.0000028898446],"about_ca_topic_score_codex":0.18934442,"about_ca_topic_score_gemma":0.31674707,"teacher_disagreement_score":0.18934442,"about_ca_system_score_codex":0.0018696444,"about_ca_system_score_gemma":0.001080554,"threshold_uncertainty_score":0.37648457},"labels":[],"label_agreement":null},{"id":"W1820622915","doi":"10.1029/2003gl018619","title":"Cold‐water coral mounds: Evidence for early Holocene climate change and slope failure","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Holocene; Coral; Oceanography; Before Present; Population; Physical geography; Last Glacial Maximum; Deglaciation; Period (music); Glacial period; Paleontology; Geography","score_opus":0.11431318475966153,"score_gpt":0.3341062425096149,"score_spread":0.2197930577499534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1820622915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936897,0.000047116522,0.000031136868,0.0000456713,0.0000018085032,0.0000011342888,0.000096122465,0.000003324247,0.0004047911],"genre_scores_gemma":[0.99973303,0.000026224017,0.000025493368,0.0000092568025,0.0000040455056,0.0000010778538,0.00012745944,0.0000013074897,0.00007209752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998878,0.000020176212,0.000009803587,0.000022734775,0.000019707926,0.000039847077],"domain_scores_gemma":[0.9981875,0.00022064737,0.0009181786,0.0001463562,0.00021161673,0.00031581568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031672968,0.00013255201,0.00017595215,0.00085538055,0.00033855956,0.00052314927,0.0002923091,0.00037432552,0.0021135563],"category_scores_gemma":[0.001767315,0.0001891986,0.00016580179,0.0007949788,0.00061971374,0.00028054244,0.00035764222,0.0003952544,0.00022092358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057652454,0.000013567865,0.99732685,0.0000034028753,0.000014153789,0.00008071515,0.00011061921,0.00004526669,0.0007365543,0.000027042277,0.000061816616,0.0015224488],"study_design_scores_gemma":[0.0000013366782,0.000011606536,0.9996568,8.245732e-7,0.0000026290438,0.00008147327,0.00006541955,0.000051850322,0.000042783227,0.000013717549,0.00007051966,0.0000010156477],"about_ca_topic_score_codex":0.010932042,"about_ca_topic_score_gemma":0.025528917,"teacher_disagreement_score":0.010932042,"about_ca_system_score_codex":0.00030398607,"about_ca_system_score_gemma":0.00021790148,"threshold_uncertainty_score":0.0217368},"labels":[],"label_agreement":null},{"id":"W1821731599","doi":"10.1002/2013gl058486","title":"Last Glacial Maximum ice sheet impacts on North Atlantic climate variability: The importance of the sea ice lid","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Ice sheet; Climatology; Sea ice; Last Glacial Maximum; Arctic ice pack; Ice-sheet model; Oceanography; Glacial period; Lead (geology); Antarctic sea ice; Holocene; Geomorphology","score_opus":0.022876447814725153,"score_gpt":0.27077978590361196,"score_spread":0.24790333808888682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1821731599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99871755,0.000032628017,0.00008644959,0.00007253285,0.000008190078,0.0000025495115,0.00013348035,0.000008429599,0.0009381473],"genre_scores_gemma":[0.99968374,0.000018801778,0.000060536226,0.000021972786,0.0000021327353,0.0000024034896,0.00008886215,0.0000031092018,0.00011849321],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998913,0.000048834685,0.000006962729,0.000015863692,0.000011450318,0.00002561837],"domain_scores_gemma":[0.9997502,0.000113900314,0.00003209662,0.000026103053,0.000029509689,0.0000482345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005807531,0.00024706958,0.00022295333,0.00014930301,0.00026483712,0.0007758238,0.00027203295,0.0003296712,0.0013709089],"category_scores_gemma":[0.0010176828,0.00015757864,0.0003976816,0.00012342246,0.0003080187,0.0003028394,0.00041653818,0.0003044008,0.0000824201],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028777097,0.00059830054,0.48453572,0.00016277406,0.00071255176,0.00042867524,0.00016598456,0.4515316,0.040333934,0.0024920928,0.0021466413,0.014014],"study_design_scores_gemma":[0.00039666452,0.0006599362,0.49352974,0.000034654044,0.00031640904,0.00004989902,0.0003471183,0.4906403,0.012012797,0.0007716628,0.0012033178,0.00003738975],"about_ca_topic_score_codex":0.026532885,"about_ca_topic_score_gemma":0.026982917,"teacher_disagreement_score":0.026532885,"about_ca_system_score_codex":0.00080480386,"about_ca_system_score_gemma":0.00050607993,"threshold_uncertainty_score":0.052756906},"labels":[],"label_agreement":null},{"id":"W1822045618","doi":"10.1002/grl.50261","title":"Geochemical profile of a layered outcrop in the Atacama analogue using laser‐induced breakdown spectroscopy: Implications for Curiosity investigations in Gale","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Laser-induced spectroscopy and plasma","field":"Engineering","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Space Agency","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Outcrop; Laser-induced breakdown spectroscopy; Geology; Mars Exploration Program; Impact crater; Raman spectroscopy; Spectroscopy; Exploration of Mars; Astrobiology; Remote sensing; Laser; Geochemistry; Optics; Physics","score_opus":0.06243886900128445,"score_gpt":0.3323274280573838,"score_spread":0.2698885590560993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1822045618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986885,0.000050001774,0.00018201981,0.000013414139,9.24583e-7,0.0000069725893,0.000106210304,0.00000910151,0.00094283326],"genre_scores_gemma":[0.9987984,0.000042145617,0.00038683257,0.000014762202,0.0000012618467,0.000007946775,0.000097722455,0.000006400082,0.0006445237],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999176,0.0000061010187,0.000002780962,0.000024895042,0.000029311852,0.000019282581],"domain_scores_gemma":[0.9998381,0.0000309505,0.000032333126,0.000012263156,0.000060180144,0.000026209122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015129434,0.00018675906,0.0002540149,0.0015042116,0.0008788564,0.00072442903,0.000366742,0.00028582162,0.0012654581],"category_scores_gemma":[0.00027682455,0.00014622087,0.00012294603,0.0008018902,0.00064866,0.00025183544,0.0006101572,0.0002845608,0.00020091124],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041875296,0.0001304222,0.48147196,0.00020333682,0.00007978413,0.0022335558,0.0051721516,0.0012134417,0.4889271,0.0003050125,0.00024194585,0.019602489],"study_design_scores_gemma":[0.00000971227,0.00008148645,0.9754876,0.000018257511,0.000019047773,0.0003457701,0.003378204,0.00074071565,0.017784009,0.000103528815,0.002018789,0.000012888393],"about_ca_topic_score_codex":0.015072826,"about_ca_topic_score_gemma":0.029445456,"teacher_disagreement_score":0.015072826,"about_ca_system_score_codex":0.0006529503,"about_ca_system_score_gemma":0.0002844621,"threshold_uncertainty_score":0.029970169},"labels":[],"label_agreement":null},{"id":"W1824026236","doi":"10.1029/2011gl050205","title":"Is the climate response to CO<sub>2</sub> emissions path dependent?","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Simon Fraser University","funders":"","keywords":"Environmental science; Climate change; Climatology; Atmospheric sciences; Cumulative effects; Greenhouse gas; Climate model; Representative Concentration Pathways; Precipitation; Range (aeronautics); GCM transcription factors; Meteorology; General Circulation Model; Oceanography; Geology; Geography; Ecology","score_opus":0.020379879787246934,"score_gpt":0.2918632980857059,"score_spread":0.27148341829845896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1824026236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99078965,0.00039548022,0.004340747,0.00095208583,0.000028201002,0.000017848255,0.00067266694,0.000092904804,0.002710267],"genre_scores_gemma":[0.9989316,0.00020981467,0.00033521574,0.00012756986,0.000008729264,0.0000060120506,0.00013630965,0.000014295916,0.00023037655],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984455,0.000045588225,0.0000051193615,0.00005700762,0.000014008834,0.000033660777],"domain_scores_gemma":[0.9993901,0.00023162349,0.0001742691,0.00007416176,0.00007761909,0.000052142303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037213977,0.00024941462,0.00030325603,0.00018349967,0.00020067078,0.0005805854,0.00038927438,0.00075639103,0.0017313558],"category_scores_gemma":[0.0014921834,0.00031042725,0.0004965383,0.0003314426,0.00054453884,0.00073690905,0.00032788268,0.00034454052,0.00029562716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014163094,0.00026217208,0.54978067,0.00043046087,0.0010256702,0.00065478735,0.00028908183,0.2388322,0.15966316,0.005823175,0.0026594654,0.039162908],"study_design_scores_gemma":[0.000057670277,0.0002328061,0.8016889,0.00002237601,0.00024080786,0.00023584232,0.00033988967,0.17514482,0.011231511,0.00804403,0.0026823892,0.00007896874],"about_ca_topic_score_codex":0.003949494,"about_ca_topic_score_gemma":0.0043700123,"teacher_disagreement_score":0.003949494,"about_ca_system_score_codex":0.00041876716,"about_ca_system_score_gemma":0.00027241526,"threshold_uncertainty_score":0.007853031},"labels":[],"label_agreement":null},{"id":"W1825150210","doi":"10.1029/2012gl054259","title":"The great Arctic cyclone of August 2012","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":293,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Climatology; Storm; Cyclone (programming language); Polar vortex; Arctic dipole anomaly; Arctic sea ice decline; Arctic geoengineering; Extratropical cyclone; Siberian High; Arctic ice pack; Environmental science; Storm surge; Oceanography; Geology; Geography; Stratosphere; East Asia; China; Antarctic sea ice","score_opus":0.028440315490849983,"score_gpt":0.27737967418097476,"score_spread":0.24893935869012476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1825150210","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.69726324,0.009007453,0.0008474757,0.013166385,0.0053381617,0.000084671265,0.009989624,0.0002861267,0.2640169],"genre_scores_gemma":[0.97555554,0.0028058107,0.00037806405,0.0020115217,0.0016413665,0.000021323383,0.0026000587,0.000032929343,0.014953324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997712,0.000037128553,0.000011882423,0.00003719674,0.00005877636,0.00008379722],"domain_scores_gemma":[0.9996158,0.000028428058,0.000093563176,0.000036801168,0.00011733807,0.000108067725],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003196558,0.0001923298,0.000106930886,0.00054169423,0.0009858129,0.0010065458,0.00009866003,0.00034402456,0.0032165805],"category_scores_gemma":[0.0010117461,0.00007875899,0.0001137288,0.00055599585,0.00033114347,0.00037663447,0.0006840742,0.00052025955,0.00050653407],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005184656,0.000048417554,0.4466143,0.00033515366,0.00012457512,0.0028715248,0.0044808094,0.00064482895,0.0043637976,0.01649862,0.39305878,0.1304407],"study_design_scores_gemma":[0.000012912604,0.000038949132,0.6458558,0.00016393521,0.000010633476,0.0009215633,0.0010919279,0.00013518576,0.0002329155,0.000888965,0.35063234,0.000014852258],"about_ca_topic_score_codex":0.017921431,"about_ca_topic_score_gemma":0.050207876,"teacher_disagreement_score":0.017921431,"about_ca_system_score_codex":0.0006946245,"about_ca_system_score_gemma":0.0006623517,"threshold_uncertainty_score":0.03563422},"labels":[],"label_agreement":null},{"id":"W1826752627","doi":"10.1002/grl.50132","title":"Historical changes in Australian temperature extremes as inferred from extreme value distribution analysis","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Extreme value theory; Generalized extreme value distribution; Percentile; Extreme heat; Climatology; Environmental science; Extreme Cold; Return period; Climate change; Atmospheric sciences; Statistics; Mathematics; Geology; Geography; Oceanography","score_opus":0.062215191581552365,"score_gpt":0.3036578148815462,"score_spread":0.24144262329999383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1826752627","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99630874,0.000042267544,0.0019259778,0.000030498803,0.0000024461306,0.0000036360095,0.00022115288,0.000011333403,0.0014539096],"genre_scores_gemma":[0.99919456,0.000029308318,0.00043141632,0.000004053601,0.0000014546637,0.0000028670772,0.00017125178,0.0000019809838,0.00016305078],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997373,0.000084458115,0.000018938801,0.000050624512,0.00007869179,0.000029925457],"domain_scores_gemma":[0.9991497,0.00018854535,0.00023823277,0.000091026704,0.0002791222,0.00005345278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007122301,0.00009261382,0.0001475613,0.0009959665,0.00022123555,0.00040046655,0.00019516751,0.00018987703,0.0006124262],"category_scores_gemma":[0.0026729018,0.00012373674,0.00016586838,0.0011274967,0.00029105743,0.00038335047,0.00041028706,0.00026198992,0.00013551665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112910966,0.00003389022,0.9300471,0.00004622478,0.00011484437,0.0003115622,0.0010560347,0.029018804,0.0058253217,0.0021562737,0.0006283794,0.030648613],"study_design_scores_gemma":[9.2514995e-7,0.000026931644,0.9829501,0.000005620297,0.000009637241,0.00006930389,0.00011259499,0.015080849,0.00040223534,0.00039587013,0.00093870383,0.000007278638],"about_ca_topic_score_codex":0.012709758,"about_ca_topic_score_gemma":0.016971167,"teacher_disagreement_score":0.012709758,"about_ca_system_score_codex":0.00057916803,"about_ca_system_score_gemma":0.00017164338,"threshold_uncertainty_score":0.025271595},"labels":[],"label_agreement":null},{"id":"W1826953724","doi":"10.1002/grl.50363","title":"How does Arctic summer wind modulate sea ice‐ocean heat balance in the Canada Basin?","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Arctic ice pack; Drift ice; Sea ice thickness; Climatology; Antarctic sea ice; Upwelling; Geology; Environmental science; Arctic sea ice decline; Cryosphere; Canada Basin; Oceanography; Heat flux; Arctic; Sea ice concentration; Fast ice; Heat transfer","score_opus":0.015823306976828048,"score_gpt":0.23108928322964115,"score_spread":0.2152659762528131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1826953724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736565,0.00028032187,0.000100990575,0.00028578745,0.000010471412,0.000003738136,0.0002570242,0.000007887429,0.0016882499],"genre_scores_gemma":[0.9991565,0.00023865508,0.00005326902,0.000023489178,0.000002443232,9.984694e-7,0.00007981115,0.0000039057118,0.00044092792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.00001053424,0.0000021426968,0.00001042222,0.000009747894,0.000033257693],"domain_scores_gemma":[0.9998491,0.000022838898,0.000016233615,0.000005789858,0.000059166534,0.000046915902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018855388,0.00017397574,0.00019472491,0.00021733338,0.00077648455,0.0010091902,0.00025078884,0.00029760756,0.00089739665],"category_scores_gemma":[0.00058419374,0.00016070236,0.00019171846,0.00033979674,0.00034931235,0.0003002961,0.0002493397,0.00015342378,0.0001005781],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042423393,0.00007366339,0.92551583,0.00008093196,0.00020710302,0.00043049036,0.00084521563,0.03211804,0.016597746,0.0019587195,0.0021415416,0.01960654],"study_design_scores_gemma":[0.000019057428,0.000023853067,0.97187763,0.000020360818,0.0000674404,0.000029888417,0.001217367,0.023807606,0.00070367224,0.00045735957,0.0017538321,0.000021866648],"about_ca_topic_score_codex":0.9160907,"about_ca_topic_score_gemma":0.9496831,"teacher_disagreement_score":0.08390927,"about_ca_system_score_codex":0.004466501,"about_ca_system_score_gemma":0.005075012,"threshold_uncertainty_score":0.16880679},"labels":[],"label_agreement":null},{"id":"W1827973530","doi":"10.1002/grl.50635","title":"Direct auroral precipitation from the magnetotail during substorms","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Aeronautics and Space Administration","keywords":"Substorm; Electron precipitation; Electron; Physics; Precipitation; Earth's magnetic field; Geophysics; Atmospheric sciences; Pitch angle; Magnetosphere; Computational physics; Magnetic field; Meteorology","score_opus":0.013513999251724581,"score_gpt":0.2569067695013643,"score_spread":0.24339277024963973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1827973530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992262,0.00002680191,0.0002815764,0.000021165308,0.0000025815107,0.000002638325,0.00005527367,0.000024922183,0.00035880844],"genre_scores_gemma":[0.9998103,0.000012985111,0.000052953365,0.0000034555262,0.0000026356636,0.0000013201281,0.000062544204,0.0000034667821,0.000050468592],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995315,0.000009825765,0.0000031144205,0.00000909339,0.0000090410995,0.00001571519],"domain_scores_gemma":[0.99980694,0.000057687394,0.00006255962,0.000016766036,0.000022733067,0.00003330435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015797415,0.00018818496,0.00020007927,0.00019840353,0.00027951112,0.00033822714,0.00014614435,0.00021920909,0.0009910846],"category_scores_gemma":[0.0006406356,0.00011060665,0.00028430021,0.00016324228,0.00021307378,0.00018590005,0.0003282314,0.00018999094,0.00008954261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005477393,0.000098185665,0.89471334,0.00006110556,0.00020959404,0.0010348142,0.00033861992,0.0640179,0.029587353,0.000527682,0.00058848405,0.008275226],"study_design_scores_gemma":[0.00010765206,0.00019728224,0.883987,0.000012754277,0.00007386846,0.00029508804,0.00026208005,0.10699351,0.0066859326,0.0004746752,0.0008948545,0.000015223281],"about_ca_topic_score_codex":0.0061766356,"about_ca_topic_score_gemma":0.0067970105,"teacher_disagreement_score":0.0061766356,"about_ca_system_score_codex":0.0004279758,"about_ca_system_score_gemma":0.00015330447,"threshold_uncertainty_score":0.012281418},"labels":[],"label_agreement":null},{"id":"W1829353783","doi":"10.1002/grl.50500","title":"Attribution of observed sea level pressure trends to greenhouse gas, aerosol, and ozone changes","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"British Antarctic Survey; Climate Program Office; Biological and Environmental Research; Department for Environment, Food and Rural Affairs, UK Government; Office of Science; National Oceanic and Atmospheric Administration; Met Office; U.S. Department of Energy","keywords":"Greenhouse gas; Aerosol; Environmental science; Ozone; Atmospheric sciences; Climatology; Latitude; Climate change; Atmospheric circulation; General Circulation Model; Meteorology; Oceanography; Geography; Geology","score_opus":0.1244773833554507,"score_gpt":0.3119480560347402,"score_spread":0.1874706726792895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1829353783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99860626,0.000025592719,0.00032884226,0.000052917447,0.000004748615,0.000002907189,0.00049526815,0.000026768479,0.0004565954],"genre_scores_gemma":[0.9994442,0.00001902763,0.00010891001,0.00000432536,0.0000025358825,0.0000024496644,0.00035451382,0.000004594343,0.000059436537],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987304,0.000036226673,0.000008950309,0.000039839197,0.000015734011,0.000026188674],"domain_scores_gemma":[0.9995555,0.00018348273,0.000092574584,0.000056071254,0.00006167721,0.00005058326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042766,0.00022315365,0.00021378114,0.00038813933,0.0002081709,0.0006352191,0.00024570964,0.0002949546,0.0011484693],"category_scores_gemma":[0.0013024645,0.00019577547,0.0005713753,0.00055382046,0.00030195777,0.00030745566,0.00036988765,0.00026786077,0.000120016026],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017488118,0.00007069694,0.85928094,0.000033480108,0.00027691512,0.00008299487,0.00007412962,0.1321348,0.0032986202,0.00055546704,0.00047117245,0.0035458268],"study_design_scores_gemma":[0.000066180626,0.00009002822,0.73057216,0.000011127655,0.00007606461,0.000036324596,0.00014902362,0.26559013,0.0018854857,0.00086418685,0.0006321232,0.000027188591],"about_ca_topic_score_codex":0.032742433,"about_ca_topic_score_gemma":0.025150105,"teacher_disagreement_score":0.032742433,"about_ca_system_score_codex":0.0006690287,"about_ca_system_score_gemma":0.0004254342,"threshold_uncertainty_score":0.06510371},"labels":[],"label_agreement":null},{"id":"W1829662551","doi":"10.1002/2015gl065863","title":"The origin of Mauna Loa's Nīnole Hills: Evidence of rift zone reorganization","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Bouguer anomaly; Rift; Gravity anomaly; Rift zone; Volcano; Mass wasting; Seafloor spreading; Seismology; Geomorphology; Landslide; Paleontology; Tectonics","score_opus":0.04185027170289194,"score_gpt":0.3180095394227467,"score_spread":0.2761592677198547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1829662551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924797,0.000058573805,0.000047626705,0.000019199997,7.686857e-7,0.0000038635158,0.00003198567,0.000004546689,0.0005855077],"genre_scores_gemma":[0.9997695,0.000027627018,0.00006801164,0.000005956948,0.0000026832329,0.0000016798066,0.000050660048,5.686819e-7,0.000073220544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999194,0.000008820532,0.000006090223,0.00001965738,0.000018754663,0.000027332517],"domain_scores_gemma":[0.9995536,0.000049864437,0.00021455786,0.00003408914,0.00006304669,0.00008482501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000181745,0.0001223406,0.00016846824,0.000860817,0.0002893724,0.00042249402,0.0002290699,0.00023072549,0.00078856194],"category_scores_gemma":[0.0006011022,0.00013216518,0.00009110387,0.00051101745,0.00070301536,0.00024117071,0.00034899963,0.00016956104,0.000122053025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006190381,0.000015610261,0.97591156,0.000017885533,0.000020474168,0.0007106006,0.0007548378,0.00018848894,0.01681687,0.000112090434,0.000065122455,0.005324633],"study_design_scores_gemma":[0.0000014496405,0.000010560435,0.9993383,0.0000016488009,0.0000025091724,0.00011848707,0.00014738235,0.00007632021,0.00016923096,0.000011460969,0.00012121572,0.0000012676165],"about_ca_topic_score_codex":0.011171081,"about_ca_topic_score_gemma":0.02812875,"teacher_disagreement_score":0.011171081,"about_ca_system_score_codex":0.00035229785,"about_ca_system_score_gemma":0.00024695558,"threshold_uncertainty_score":0.022212088},"labels":[],"label_agreement":null},{"id":"W1830788433","doi":"10.1002/2014gl060478","title":"Return periods of global climate fluctuations and the pause","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Climatology; Environmental science; Return period; Forcing (mathematics); Radiative forcing; Scaling; General Circulation Model; Event (particle physics); Amplitude; Climate model; Global warming; Climate change; Atmospheric sciences; Series (stratigraphy); Period (music); Geography; Mathematics; Geology; Physics","score_opus":0.010376571652959889,"score_gpt":0.26704995131874754,"score_spread":0.2566733796657876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1830788433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940891,0.00021266266,0.0036608838,0.00016543242,0.000016415384,0.000005017982,0.00028034367,0.000094299394,0.0014756985],"genre_scores_gemma":[0.99974364,0.000021142409,0.00008634946,0.0000048691154,0.0000069972916,0.0000013105247,0.00008756167,0.000006023253,0.000042120224],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998092,0.00004648063,0.000017172659,0.000060848408,0.000037039288,0.000029230265],"domain_scores_gemma":[0.99566096,0.0021263633,0.001376511,0.0003887459,0.00017148665,0.0002759488],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012218026,0.00020009415,0.00020362336,0.00094277586,0.00026173252,0.0009103913,0.00028026119,0.00039408036,0.0014992066],"category_scores_gemma":[0.007305533,0.00019112545,0.00038713033,0.00051055447,0.000709182,0.0006808096,0.00058814726,0.0005772254,0.00015023383],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009220477,0.000046969275,0.906084,0.0000917696,0.000315306,0.00085988693,0.0007698257,0.03881779,0.0061516115,0.018331524,0.0016381566,0.025971118],"study_design_scores_gemma":[0.000027033393,0.00018617054,0.919001,0.00003578004,0.00009854081,0.00097028393,0.00043455654,0.05640745,0.0023928182,0.017324967,0.0030674126,0.00005393919],"about_ca_topic_score_codex":0.000742453,"about_ca_topic_score_gemma":0.0005883421,"teacher_disagreement_score":0.0014992066,"about_ca_system_score_codex":0.0002689099,"about_ca_system_score_gemma":0.00010055873,"threshold_uncertainty_score":0.0064616203},"labels":[],"label_agreement":null},{"id":"W1830853164","doi":"10.1029/2010gl042417","title":"Reorganization of the ocean overturning in a colder climate","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Thermohaline circulation; Stratification (seeds); Oceanography; Northern Hemisphere; Climate change; Climate model; Geology; Environmental science; Ocean heat content; High latitude; Southern Hemisphere; Ocean current; Latitude","score_opus":0.0120476664067321,"score_gpt":0.24927877496379414,"score_spread":0.23723110855706203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1830853164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970951,0.000035892164,0.0011300435,0.000125006,0.000011771882,0.000004743835,0.00008554745,0.000046197958,0.0014656801],"genre_scores_gemma":[0.9992237,0.000036463225,0.00028141704,0.000024014775,0.0000073979854,0.0000047190993,0.00005869546,0.000022388846,0.00034129003],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990237,0.000027421707,0.0000044458125,0.000028584771,0.0000062309873,0.000031020456],"domain_scores_gemma":[0.9996902,0.00006594465,0.00007061611,0.00005839064,0.00002981375,0.000085019485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027229087,0.00036384683,0.00046587028,0.0002573171,0.00044876433,0.0010326575,0.0004913604,0.00068455614,0.0026668934],"category_scores_gemma":[0.0008791638,0.0002711559,0.00085093244,0.00021631521,0.00063085975,0.0005867693,0.0006111192,0.0005203146,0.00018418349],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037271605,0.00021571624,0.04403239,0.000049937862,0.00015054896,0.0004622763,0.00016892873,0.9154347,0.029927809,0.0048509156,0.00057142926,0.003762673],"study_design_scores_gemma":[0.00012631044,0.00012706422,0.07346309,0.00000715336,0.000053071344,0.00006562511,0.00010364994,0.9223655,0.0009736923,0.0022632924,0.00041931853,0.0000322407],"about_ca_topic_score_codex":0.012513711,"about_ca_topic_score_gemma":0.007067582,"teacher_disagreement_score":0.012513711,"about_ca_system_score_codex":0.0007596995,"about_ca_system_score_gemma":0.0004347115,"threshold_uncertainty_score":0.02488172},"labels":[],"label_agreement":null},{"id":"W1833212134","doi":"10.1002/grl.50439","title":"Nutrient enrichment of the subarctic Pacific Ocean pycnocline","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Pycnocline; Subarctic climate; Oceanography; Nutrient; Environmental science; Thermohaline circulation; Stratification (seeds); New production; Nitrate; Geology; Ecology; Biology; Phytoplankton","score_opus":0.018161852765915795,"score_gpt":0.2639144921590501,"score_spread":0.2457526393931343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1833212134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99774086,0.0003200663,0.00005363791,0.00012561092,0.000006311263,0.0000021778842,0.00067081704,0.000015226755,0.00106536],"genre_scores_gemma":[0.99927765,0.00018240513,0.00007018944,0.000024628614,0.0000032149119,0.0000022365798,0.00028197674,0.0000038941266,0.00015391239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992657,0.000010525827,0.00000642619,0.000025588777,0.000013794305,0.00001709728],"domain_scores_gemma":[0.99970645,0.000023118022,0.00010992869,0.000020780331,0.0000849933,0.00005476862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023568417,0.00022840212,0.00017289372,0.0005011021,0.00034032794,0.00055298995,0.00018137677,0.00014957061,0.0010065689],"category_scores_gemma":[0.0005274284,0.0001134804,0.0001635637,0.0005966915,0.00031974973,0.00033981,0.0006560151,0.00024028635,0.000112540285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013715049,0.00001454898,0.9778365,0.000108379674,0.0001115199,0.00024787473,0.000251991,0.001184778,0.014213392,0.00012702796,0.00043709384,0.0053297477],"study_design_scores_gemma":[0.0000025023642,0.0000054014586,0.99864274,0.000006333291,0.000010691491,0.000019876607,0.00011686153,0.00024020129,0.00041857804,0.000020463229,0.0005148112,0.0000015480439],"about_ca_topic_score_codex":0.10401909,"about_ca_topic_score_gemma":0.122465335,"teacher_disagreement_score":0.10401909,"about_ca_system_score_codex":0.0010383589,"about_ca_system_score_gemma":0.0008476276,"threshold_uncertainty_score":0.20682728},"labels":[],"label_agreement":null},{"id":"W1833367443","doi":"10.1002/2015gl065311","title":"Revisiting the evidence of increasing springtime ozone mixing ratios in the free troposphere over western North America","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; Ames Research Center; National Aeronautics and Space Administration","keywords":"Hindcast; Climatology; Environmental science; Ozone; Atmospheric sciences; Troposphere; Tropospheric ozone; Meteorology; Geography; Geology","score_opus":0.05265911496326058,"score_gpt":0.305825482646508,"score_spread":0.2531663676832474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1833367443","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911946,0.00008841025,0.0001451578,0.00006682472,0.0000040177088,0.0000014924759,0.00025190468,0.000013472464,0.00030915826],"genre_scores_gemma":[0.99930036,0.00007106253,0.00021185428,0.000027331542,0.0000046584237,0.0000020463146,0.00028457993,0.0000038752396,0.0000941967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.000010172596,0.0000046231908,0.000024069133,0.000011487027,0.000012218424],"domain_scores_gemma":[0.9998068,0.000048600497,0.000052063555,0.000026490468,0.000037268517,0.000028773897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002136611,0.00018958886,0.00014450203,0.00039398967,0.00025761878,0.00038364858,0.00025982724,0.00027215955,0.0006831142],"category_scores_gemma":[0.00048667038,0.00015498459,0.0002862465,0.00045667685,0.00022390002,0.00042831828,0.00028755315,0.00022658835,0.000068652334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013636862,0.00007019722,0.9536477,0.00005943816,0.00019246578,0.00014774285,0.00051209854,0.0030268596,0.03241518,0.00019233221,0.00057675736,0.009022962],"study_design_scores_gemma":[0.0000036233519,0.000013037642,0.99674135,0.0000042651764,0.000020820708,0.000013861699,0.00008937133,0.001875707,0.0008227759,0.000036247322,0.00037608386,0.0000028790764],"about_ca_topic_score_codex":0.08598672,"about_ca_topic_score_gemma":0.1301905,"teacher_disagreement_score":0.08598672,"about_ca_system_score_codex":0.00040790837,"about_ca_system_score_gemma":0.00042092014,"threshold_uncertainty_score":0.17097247},"labels":[],"label_agreement":null},{"id":"W1835396178","doi":"10.1029/2012gl051570","title":"Decadal variability and a recent amplification of the summer Beaufort Sea High","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Arctic sea ice decline; Beaufort sea; Beaufort scale; Climatology; Arctic; Arctic ice pack; Arctic geoengineering; Sea ice; Cyclogenesis; Oceanography; Environmental science; Troposphere; The arctic; Arctic dipole anomaly; Cyclone (programming language); Geology; Antarctic sea ice","score_opus":0.036959311879371154,"score_gpt":0.28603633177025645,"score_spread":0.2490770198908853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1835396178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965899,0.00041890304,0.00022391642,0.00033658632,0.000033894325,0.000001531783,0.0004665671,0.000019373427,0.0019093445],"genre_scores_gemma":[0.9990037,0.00011112426,0.00008242365,0.000053361342,0.00004803439,0.0000012634237,0.00038908672,0.000002821329,0.00030834752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999002,0.00001262577,0.000006848178,0.00003821458,0.000018924466,0.000023132561],"domain_scores_gemma":[0.9992399,0.00009651107,0.00032001233,0.00006469981,0.00018754158,0.00009148191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039776516,0.000100800666,0.000106685024,0.00049263856,0.00020402875,0.00059913937,0.0001201893,0.00022199623,0.00086480385],"category_scores_gemma":[0.0006881501,0.00007673977,0.00014780492,0.00072229624,0.00021779681,0.00019926271,0.0002347042,0.00031315125,0.00012593676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022219625,0.000037735103,0.9648523,0.0000521756,0.0001876806,0.00021501523,0.00077601755,0.00062218733,0.0072261468,0.000581589,0.0020713822,0.023155602],"study_design_scores_gemma":[9.48198e-7,0.000009183229,0.9985129,0.0000014724206,0.000005642751,0.000031381205,0.000038389553,0.00009601944,0.00009350854,0.000017097598,0.0011916253,0.0000017157339],"about_ca_topic_score_codex":0.007547773,"about_ca_topic_score_gemma":0.0126027195,"teacher_disagreement_score":0.007547773,"about_ca_system_score_codex":0.00023997223,"about_ca_system_score_gemma":0.00011988459,"threshold_uncertainty_score":0.015007675},"labels":[],"label_agreement":null},{"id":"W1839128451","doi":"10.1002/grl.50187","title":"Linkages between lake shrinkage/expansion and sublacustrine permafrost distribution determined from remote sensing of interior Alaska, USA","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Strategic Environmental Research and Development Program; U.S. Geological Survey","keywords":"Permafrost; Aquifer; Geology; Groundwater; Hydrology (agriculture); Groundwater flow; Spatial distribution; Surface water; Physical geography; Geomorphology; Environmental science; Remote sensing; Oceanography; Geography","score_opus":0.04900228098511408,"score_gpt":0.2916341716610621,"score_spread":0.242631890675948,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1839128451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994037,0.000019271825,0.00003933166,0.0000042810652,4.4918164e-7,7.875132e-7,0.00029013227,0.00000318401,0.00023882775],"genre_scores_gemma":[0.99952054,0.000016470387,0.000048854672,0.0000020048167,6.919685e-7,0.000001537771,0.00034517143,5.424009e-7,0.00006404725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.000009973354,0.000009249769,0.000024256906,0.000011902746,0.0000102990725],"domain_scores_gemma":[0.9995859,0.0001064293,0.00014220778,0.00002899535,0.00008988017,0.000046649366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019099283,0.00010723948,0.000100540994,0.00085329486,0.00024814822,0.00034784005,0.000120755416,0.00012563067,0.00085546565],"category_scores_gemma":[0.0005395046,0.00009553245,0.00010638189,0.00074367627,0.00014291318,0.00023084432,0.00027004498,0.00009770143,0.0000799194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019328856,0.0000062171534,0.9971545,0.000004967418,0.000022454304,0.00002342153,0.000116439245,0.0002796719,0.0006928534,0.000013260782,0.000051612777,0.0016153214],"study_design_scores_gemma":[4.823179e-7,0.0000035994585,0.9994299,0.0000018785524,0.0000054799725,0.0000110931405,0.00012788315,0.0002951961,0.00006404865,0.00000652152,0.000053188764,7.297771e-7],"about_ca_topic_score_codex":0.056989405,"about_ca_topic_score_gemma":0.13909265,"teacher_disagreement_score":0.056989405,"about_ca_system_score_codex":0.00026781097,"about_ca_system_score_gemma":0.00018894674,"threshold_uncertainty_score":0.113315344},"labels":[],"label_agreement":null},{"id":"W1839339604","doi":"10.1029/2009gl040990","title":"Ice streaming in the Laurentide Ice Sheet: A first comparison between data‐calibrated numerical model output and geological evidence","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ice sheet; Deglaciation; Ice-sheet model; Geology; Ice stream; STREAMS; Ice divide; Cryosphere; Climatology; Glacial period; Sea ice; Oceanography; Geomorphology; Computer science","score_opus":0.1971122135038439,"score_gpt":0.3509093478499808,"score_spread":0.1537971343461369,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1839339604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99777263,0.000046274956,0.0006447392,0.000038226193,0.0000032449927,0.0000059848758,0.00030295362,0.000040842726,0.0011450874],"genre_scores_gemma":[0.998237,0.000039951734,0.0011900123,0.000007634665,0.000002943532,0.000005636599,0.00041883357,0.000011823616,0.00008599153],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999846,0.000046243884,0.0000145198865,0.00004114307,0.000036691283,0.000015303418],"domain_scores_gemma":[0.99905735,0.0004408404,0.00013417321,0.00012629121,0.00019956489,0.000041716146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008392852,0.00034951587,0.00025264858,0.0004421618,0.00030011177,0.00084245,0.00047012637,0.00035558606,0.0005115011],"category_scores_gemma":[0.002599041,0.00018049621,0.00029140283,0.00045657743,0.00040029213,0.00058837404,0.0003324369,0.00024305504,0.00009098927],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028100752,0.00012390235,0.227898,0.00006372305,0.00011854729,0.00023876701,0.00027681666,0.75269514,0.0035526834,0.0009352056,0.0005209489,0.013295293],"study_design_scores_gemma":[0.000040530384,0.000108299144,0.098641336,0.000024762876,0.000032552452,0.00006493497,0.00015920111,0.8952529,0.0041688285,0.0005017874,0.0009727724,0.000032082084],"about_ca_topic_score_codex":0.02590651,"about_ca_topic_score_gemma":0.025181938,"teacher_disagreement_score":0.02590651,"about_ca_system_score_codex":0.001159903,"about_ca_system_score_gemma":0.00064422813,"threshold_uncertainty_score":0.051511407},"labels":[],"label_agreement":null},{"id":"W1839605824","doi":"10.1002/2015gl064610","title":"A new physics‐based modeling approach for tsunami‐ionosphere coupling","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Jet Propulsion Laboratory; California Institute of Technology","keywords":"Ionosphere; TEC; Thermosphere; Total electron content; Physics; Perturbation (astronomy); Geophysics; Atmosphere (unit); Gravity wave; Wavelength; Gravitational wave; Wave propagation; Meteorology; Geodesy; Geology; Astronomy; Optics","score_opus":0.06336380829164426,"score_gpt":0.3192856161475453,"score_spread":0.255921807855901,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1839605824","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.19058342,0.0003680962,0.7757307,0.00096667674,0.00027453323,0.00017131453,0.0011928022,0.0014365854,0.029275699],"genre_scores_gemma":[0.93183917,0.00030974153,0.061411045,0.00016861777,0.0001276891,0.0002556722,0.0004643477,0.00022438534,0.005199339],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989414,0.000028067881,0.0000075868356,0.00002444599,0.000027181968,0.00001849168],"domain_scores_gemma":[0.9997936,0.00007521071,0.00002742296,0.000031228203,0.000051142717,0.000021405593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027507028,0.00069256284,0.0005245471,0.00047445408,0.0007237607,0.0009945083,0.0016514851,0.0011953294,0.00260734],"category_scores_gemma":[0.00074931997,0.00054537045,0.0010145545,0.00053131237,0.0005105722,0.0013832544,0.0010448194,0.0012005566,0.00026368696],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000051771935,0.000019306715,0.00048697426,0.0000067711308,0.000023712924,0.000029838784,0.000020630852,0.991956,0.00076097785,0.005175958,0.00019615736,0.0013185185],"study_design_scores_gemma":[0.0000041764683,0.0000026654889,0.00009751716,8.256142e-7,0.0000031486247,0.000002989696,0.000002475682,0.9983954,0.00005894162,0.0011517126,0.00027749073,0.00000272602],"about_ca_topic_score_codex":0.028630586,"about_ca_topic_score_gemma":0.015270856,"teacher_disagreement_score":0.028630586,"about_ca_system_score_codex":0.0009436592,"about_ca_system_score_gemma":0.0013818055,"threshold_uncertainty_score":0.05692786},"labels":[],"label_agreement":null},{"id":"W1840015033","doi":"10.1002/2015gl064314","title":"Inability of stratospheric sulfate aerosol injections to preserve the West Antarctic Ice Sheet","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Environmental science; Sulfate aerosol; Future sea level; Cryosphere; Climatology; Greenhouse gas; Antarctic ice sheet; Ice sheet; Aerosol; Ice shelf; Global warming; Atmospheric sciences; Climate change; Stratosphere; Oceanography; Geology; Sea ice; Meteorology; Geography","score_opus":0.07498647456206536,"score_gpt":0.3090786655195217,"score_spread":0.23409219095745631,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1840015033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99813807,0.000028121114,0.0010226284,0.00002829827,0.000007465964,0.0000051014495,0.00006285458,0.000025102432,0.0006823184],"genre_scores_gemma":[0.99942386,0.000023257391,0.00039503005,0.000009929382,0.0000011229783,0.000003004303,0.000025248068,0.0000037003813,0.00011487717],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999627,0.0000071794407,0.0000027619196,0.000008641002,0.0000079159345,0.000010825869],"domain_scores_gemma":[0.9999256,0.000016864797,0.000020210888,0.000015518897,0.000008746497,0.000013039812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001307648,0.00025295393,0.00017408343,0.000078551064,0.00017605872,0.000417207,0.0002943989,0.00023036412,0.00047344298],"category_scores_gemma":[0.00026130464,0.00014667919,0.00034038536,0.00006667118,0.00022907209,0.00023588062,0.00026327523,0.00023935389,0.000052357216],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065093284,0.00026636818,0.054933257,0.00012325722,0.00036351904,0.00023775485,0.00006680768,0.5965961,0.33135957,0.0021468354,0.00036883395,0.012886692],"study_design_scores_gemma":[0.00023058009,0.0009417743,0.048439026,0.000010671355,0.00017744355,0.00008669783,0.00010161593,0.8320072,0.115323074,0.0012349339,0.0014140323,0.000032853884],"about_ca_topic_score_codex":0.009277799,"about_ca_topic_score_gemma":0.0077817803,"teacher_disagreement_score":0.009277799,"about_ca_system_score_codex":0.00034254446,"about_ca_system_score_gemma":0.0005545621,"threshold_uncertainty_score":0.018447578},"labels":[],"label_agreement":null},{"id":"W1842943593","doi":"10.1029/2012gl052798","title":"Reduction in field‐aligned currents preceding and local to auroral substorm onset","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Calgary; Alberta Innovates; National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Substorm; Ionosphere; Magnetosphere; Geophysics; Physics; Field line; Field (mathematics); Coupling (piping); Atmospheric sciences; Magnetic field","score_opus":0.022489347161753395,"score_gpt":0.3198093328340689,"score_spread":0.29731998567231555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1842943593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973761,0.00010636195,0.00021755231,0.00003263728,0.000006592953,0.0000063419347,0.00024847718,0.000036960922,0.0019690047],"genre_scores_gemma":[0.99909663,0.000039283776,0.00010064792,0.000011099134,0.0000092761675,0.0000042751003,0.00027146502,0.0000050862614,0.00046226132],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.0000024658493,0.0000019083252,0.000010786114,0.000009025407,0.00002232515],"domain_scores_gemma":[0.99975306,0.00002652322,0.00008109072,0.000016652984,0.000057096524,0.0000655874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000054910895,0.000101533835,0.0002045972,0.00047664216,0.000261898,0.00038762114,0.00011022981,0.00022801831,0.0020665044],"category_scores_gemma":[0.0003488378,0.00006933229,0.00013294631,0.00030414725,0.00025397787,0.00023198925,0.00032675275,0.00036644368,0.00023189613],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010067957,0.00010097009,0.4379841,0.00011459865,0.00007658593,0.0015397717,0.0013038295,0.0010094987,0.5325376,0.00049367466,0.0010359798,0.022796651],"study_design_scores_gemma":[0.0000025031645,0.000039917748,0.9961511,0.0000030136769,0.0000049747778,0.00012929787,0.000129824,0.00018933462,0.002893584,0.000033477543,0.0004202155,0.0000027556432],"about_ca_topic_score_codex":0.006095817,"about_ca_topic_score_gemma":0.009343074,"teacher_disagreement_score":0.006095817,"about_ca_system_score_codex":0.00031293876,"about_ca_system_score_gemma":0.0001078005,"threshold_uncertainty_score":0.012120664},"labels":[],"label_agreement":null},{"id":"W1844967195","doi":"10.1029/2009gl041821","title":"Active shoreline of Ontario Lacus, Titan: A morphological study of the lake and its surroundings","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"European Space Agency; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Shore; Geology; Alluvium; Littoral zone; Synthetic aperture radar; Titan (rocket family); Geomorphology; Oceanography; Remote sensing; Astrobiology","score_opus":0.043706934825059905,"score_gpt":0.30204854371742806,"score_spread":0.2583416088923682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1844967195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99816483,0.000052595267,0.000026133239,0.000014053915,5.260454e-7,0.0000059629256,0.00021303458,0.0000021863946,0.0015206606],"genre_scores_gemma":[0.9978738,0.000077418794,0.00018584474,0.000009803976,0.0000010762587,0.000008684989,0.00035226712,0.0000027504416,0.0014883793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.000002622839,0.0000021741903,0.000011524578,0.000017202452,0.000017605074],"domain_scores_gemma":[0.9998878,0.0000062068298,0.000025653291,0.0000054514303,0.000042812142,0.000032136693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000046063833,0.000110399895,0.00012004601,0.0007927853,0.0015705797,0.00048172043,0.00018917225,0.00014394891,0.0009900465],"category_scores_gemma":[0.00016171085,0.00012327862,0.000100163095,0.0011326062,0.0005589858,0.00014638493,0.00049258413,0.00008223255,0.0001781899],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016977145,0.000024142772,0.94698924,0.000071830385,0.000025830323,0.00092210365,0.010969661,0.00013978957,0.02107942,0.0002433026,0.0006896476,0.018675292],"study_design_scores_gemma":[8.503354e-7,0.000010246058,0.9977324,0.0000026658383,0.0000028276559,0.000099275494,0.0010495922,0.00005032899,0.0000915114,0.000004905257,0.0009536775,0.0000016821571],"about_ca_topic_score_codex":0.78284305,"about_ca_topic_score_gemma":0.9467322,"teacher_disagreement_score":0.78284305,"about_ca_system_score_codex":0.0029683812,"about_ca_system_score_gemma":0.0019832747,"threshold_uncertainty_score":0.43687165},"labels":[],"label_agreement":null},{"id":"W1845672550","doi":"10.1002/grl.50509","title":"Geometrical effects of a subducted seamount on stopping megathrust ruptures","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Seamount; Geology; Subduction; Seismology; Fault gouge; Fault (geology); Tectonics; Oceanography","score_opus":0.028396758658262918,"score_gpt":0.275926717459429,"score_spread":0.24752995880116607,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1845672550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977375,0.00002693779,0.0008065515,0.000032288066,0.0000066563694,0.0000070255005,0.000052390864,0.000033481232,0.0012970426],"genre_scores_gemma":[0.9993993,0.000014597965,0.0003786556,0.0000067216465,0.0000010903282,0.0000033695512,0.000028456996,0.0000053396498,0.00016253704],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998739,0.000030582698,0.000008954996,0.000018860635,0.000020711115,0.000047009595],"domain_scores_gemma":[0.9996105,0.00013329466,0.00008317353,0.00004772329,0.000050190272,0.00007517306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029572414,0.00039501066,0.00038374987,0.0003893781,0.0004645198,0.0007099887,0.00084978476,0.0008501277,0.0024078658],"category_scores_gemma":[0.0015495886,0.00031764596,0.00051320577,0.00029398798,0.00083489454,0.00035108984,0.0006810192,0.00030421626,0.00012468724],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021212154,0.0000548871,0.014714208,0.000031800588,0.000050045335,0.00038941726,0.00007739289,0.97552615,0.006325262,0.0008321337,0.00007949795,0.0017071416],"study_design_scores_gemma":[0.00009749293,0.00038759934,0.01063621,0.00001646014,0.000056732402,0.0000969228,0.0001327246,0.9845195,0.0034152262,0.00029589527,0.0003200596,0.000025210866],"about_ca_topic_score_codex":0.015096374,"about_ca_topic_score_gemma":0.008406874,"teacher_disagreement_score":0.015096374,"about_ca_system_score_codex":0.0008511908,"about_ca_system_score_gemma":0.00068236823,"threshold_uncertainty_score":0.030017018},"labels":[],"label_agreement":null},{"id":"W1849307842","doi":"10.1002/2014gl061861","title":"On Mars too expect macroweather","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Science and Technology Facilities Council","keywords":"Mars Exploration Program; Martian; Atmosphere of Mars; Planet; Astrobiology; Terrestrial planet; Spectral line; Venus; Flux (metallurgy); Physics; Solar System; Atmospheric sciences; Environmental science; Solar wind; Geology; Geophysics; Astronomy; Plasma","score_opus":0.030912102755914918,"score_gpt":0.29978594224516475,"score_spread":0.2688738394892498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1849307842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856559,0.00017956638,0.003651531,0.00041203923,0.00004296937,0.0000060268385,0.00054194365,0.00019285432,0.00931712],"genre_scores_gemma":[0.9980996,0.00006570074,0.0007747526,0.000063657244,0.000011561941,0.000002645675,0.00023137713,0.000035826193,0.0007148615],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993706,0.000006111229,0.0000018362962,0.000022310032,0.000014581269,0.000018246154],"domain_scores_gemma":[0.9997969,0.00003826223,0.000052834068,0.00003786334,0.000044450706,0.000029688796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008770742,0.00021617934,0.00012960933,0.0003097984,0.00029897346,0.0007299529,0.000100619065,0.0002410955,0.0042950953],"category_scores_gemma":[0.00046938483,0.00009137211,0.00012583449,0.00029895437,0.00021496521,0.00059320865,0.00029258544,0.0003494541,0.00078540616],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041126527,0.00009371716,0.50950664,0.00024413505,0.00020685949,0.000548719,0.0011279081,0.011238894,0.25243083,0.0076794066,0.008717498,0.20779411],"study_design_scores_gemma":[0.000009557873,0.00007206461,0.9527902,0.000018231025,0.00002546084,0.0002931211,0.0007985522,0.0069517344,0.014553323,0.0047477563,0.019717602,0.00002237206],"about_ca_topic_score_codex":0.00074412394,"about_ca_topic_score_gemma":0.0011924407,"teacher_disagreement_score":0.0042950953,"about_ca_system_score_codex":0.0001085378,"about_ca_system_score_gemma":0.00006429029,"threshold_uncertainty_score":0.0143684745},"labels":[],"label_agreement":null},{"id":"W1849866310","doi":"10.1029/2007gl030627","title":"Model‐measurement comparison of mesospheric temperature inversions, and a simple theory for their occurrence","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"TD Bank Group; University of Toronto; Western University","funders":"","keywords":"Lapse rate; Amplitude; Lidar; Adiabatic process; Rayleigh scattering; Atmospheric sciences; Inversion (geology); Environmental science; Atmospheric temperature; Atmosphere (unit); Computational physics; Physics; Geology; Meteorology; Optics; Thermodynamics","score_opus":0.04715711060454775,"score_gpt":0.3287980891249427,"score_spread":0.28164097852039494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1849866310","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86770594,0.00032631573,0.12079596,0.00031405682,0.00007327812,0.0002078911,0.0027737352,0.0014781372,0.0063246377],"genre_scores_gemma":[0.99320257,0.000037366728,0.005521552,0.0000142522995,0.0000043386012,0.000028053486,0.0010324711,0.0000447814,0.00011457676],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995722,0.00006328636,0.00002579467,0.00014188394,0.0001578332,0.000038961534],"domain_scores_gemma":[0.999191,0.00020039782,0.00014325145,0.00022579171,0.00020856565,0.000030933476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010808484,0.0005093553,0.0002491912,0.0005124977,0.000342159,0.00046751602,0.0006880971,0.00030631226,0.0005166585],"category_scores_gemma":[0.0024395415,0.00020114412,0.0004952828,0.00058384245,0.00033411323,0.0006519277,0.0004745373,0.00040343002,0.00013565317],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078836683,0.00035571755,0.36416137,0.0003745756,0.00066094624,0.00021698611,0.00049207837,0.37700605,0.12893903,0.0047870427,0.004061965,0.11815589],"study_design_scores_gemma":[0.00006763024,0.00020975509,0.26575047,0.000016296057,0.00007835015,0.00016131451,0.00012309388,0.70642,0.023656024,0.0015255053,0.001927479,0.00006414543],"about_ca_topic_score_codex":0.02226537,"about_ca_topic_score_gemma":0.036196195,"teacher_disagreement_score":0.02226537,"about_ca_system_score_codex":0.0014358322,"about_ca_system_score_gemma":0.0009005505,"threshold_uncertainty_score":0.04427153},"labels":[],"label_agreement":null},{"id":"W1850401716","doi":"10.1002/2014gl060610","title":"The Siding Spring cometary encounter with Mars: A natural experiment for the Martian atmosphere?","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Mars Exploration Program; Atmosphere of Mars; Astrobiology; Martian; Atmosphere (unit); Atmospheric sciences; Physics; Population; Extinction (optical mineralogy); Environmental science; Comet; Meteorology; Optics","score_opus":0.023551017859789178,"score_gpt":0.28450442486543326,"score_spread":0.26095340700564407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1850401716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954333,0.00003578952,0.00014899037,0.0010076886,0.000060360002,0.0000411881,0.00026474043,0.000022092641,0.002985707],"genre_scores_gemma":[0.9957218,0.000036107383,0.000319119,0.00036366103,0.000041900203,0.00004438498,0.00036866922,0.0000076198676,0.003096803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997751,0.00009243074,0.0000043649343,0.000039352355,0.000035970756,0.00005265771],"domain_scores_gemma":[0.9994497,0.000078617544,0.00006125223,0.00009814933,0.000045190154,0.00026713184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077424693,0.00014215046,0.00022431156,0.00015052951,0.002024939,0.0006070064,0.0002940191,0.0005094325,0.0032413895],"category_scores_gemma":[0.0006361279,0.000104014674,0.00020294303,0.00010332397,0.0007939961,0.0003861032,0.0005134847,0.00065420853,0.00038705286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.019042132,0.014738576,0.7317912,0.00016376693,0.00036501588,0.0025083667,0.007938875,0.00089336705,0.12330863,0.008861241,0.03375239,0.05663643],"study_design_scores_gemma":[0.00059599424,0.008847198,0.9417813,0.00002441463,0.000076842334,0.00047082588,0.0054972493,0.001982009,0.00948461,0.0019326776,0.02924835,0.00005860448],"about_ca_topic_score_codex":0.012378251,"about_ca_topic_score_gemma":0.03156533,"teacher_disagreement_score":0.012378251,"about_ca_system_score_codex":0.00067191117,"about_ca_system_score_gemma":0.00046139734,"threshold_uncertainty_score":0.024612367},"labels":[],"label_agreement":null},{"id":"W1855875207","doi":"10.1002/2014gl062400","title":"Increases in plasma sheet temperature with solar wind driving during substorm growth phases","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Science and Technology Facilities Council; U.S. Geological Survey; National Aeronautics and Space Administration; Austrian Science Fund; Goddard Space Flight Center; Sight Research UK; Florida Institute of Technology; Natural Environment Research Council; Alberta Agricultural Research Institute","keywords":"Substorm; Plasma sheet; Solar wind; Magnetopause; Plasma; Adiabatic process; Physics; Astrophysics; Flux (metallurgy); Magnetic reconnection; Geophysics; Atmospheric sciences; Magnetosphere; Materials science; Thermodynamics","score_opus":0.0066813936855758226,"score_gpt":0.23823946477987099,"score_spread":0.23155807109429516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1855875207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819094,0.00007916455,0.00023781676,0.000024313355,0.0000025976199,0.0000023481061,0.0005714778,0.000026519032,0.00086482323],"genre_scores_gemma":[0.9985858,0.000037024245,0.00012500011,0.000006299553,0.000006256386,0.0000040481923,0.0010128719,0.000006328191,0.00021632033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.0000054227753,0.0000035853366,0.00001529295,0.0000141298615,0.000012059246],"domain_scores_gemma":[0.9995801,0.000096139105,0.00016407084,0.000038879807,0.00006144564,0.00005932456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101330035,0.0001477501,0.00013018491,0.00041407073,0.0002898125,0.00043840276,0.00013239057,0.00016376564,0.0013738412],"category_scores_gemma":[0.00048641698,0.00009581884,0.0001853738,0.00039506322,0.00017905972,0.00023800987,0.00026566003,0.00023828508,0.00018777754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026323972,0.000024618737,0.930926,0.000040405866,0.00010675367,0.00020831564,0.00027860035,0.0018299718,0.057123773,0.00022942665,0.0007128565,0.008256038],"study_design_scores_gemma":[0.0000019263405,0.000011317229,0.9975376,0.0000012810917,0.000005228995,0.00007419504,0.000036179437,0.00066285185,0.0012522696,0.000038712027,0.00037688555,0.000001591713],"about_ca_topic_score_codex":0.0031563954,"about_ca_topic_score_gemma":0.0052503697,"teacher_disagreement_score":0.0031563954,"about_ca_system_score_codex":0.00018851379,"about_ca_system_score_gemma":0.000091606,"threshold_uncertainty_score":0.006276071},"labels":[],"label_agreement":null},{"id":"W1857132413","doi":"10.1002/2015gl064547","title":"Interannual variability of the Madden‐Julian Oscillation and its impact on the North Atlantic Oscillation in the boreal winter","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment Canada; National Oceanic and Atmospheric Administration","keywords":"Madden–Julian oscillation; Climatology; Teleconnection; Boreal; Extratropical cyclone; Forcing (mathematics); Empirical orthogonal functions; Indian ocean; Environmental science; North Atlantic oscillation; Oscillation (cell signaling); Convection; Geology; El Niño Southern Oscillation; Oceanography; Geography; Meteorology","score_opus":0.048745071510107235,"score_gpt":0.32274441798719616,"score_spread":0.2739993464770889,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1857132413","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984529,0.0001437909,0.00011760228,0.00006134001,0.000011514582,0.0000016744424,0.00017389444,0.000013092442,0.0010242122],"genre_scores_gemma":[0.9997546,0.000036436984,0.000041875646,0.000006680292,0.0000072852145,8.8005066e-7,0.00009129235,0.0000020417738,0.000058940637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990976,0.000022049131,0.000007293506,0.000016439915,0.000024020908,0.000020357604],"domain_scores_gemma":[0.99971193,0.0000655492,0.000087493616,0.00001817304,0.000057084377,0.000059724665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031526582,0.00015406076,0.00016716126,0.00030958463,0.00026384613,0.000536121,0.000120837765,0.00014077069,0.00056951935],"category_scores_gemma":[0.00064653344,0.000073757285,0.00024466653,0.0002803625,0.00018165195,0.00018752455,0.0002466424,0.00012763997,0.000076639946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025815572,0.00006538084,0.9693749,0.000023680452,0.00017845178,0.00019222379,0.0001927966,0.0037687924,0.013634433,0.00055205,0.0005821026,0.011177025],"study_design_scores_gemma":[0.0000050203557,0.000024524134,0.9970209,0.0000021609007,0.000013592502,0.000025403899,0.00004833477,0.00230819,0.000114881426,0.00006650279,0.00036712637,0.0000032634573],"about_ca_topic_score_codex":0.017196072,"about_ca_topic_score_gemma":0.022611095,"teacher_disagreement_score":0.017196072,"about_ca_system_score_codex":0.00034847468,"about_ca_system_score_gemma":0.00021716312,"threshold_uncertainty_score":0.034191906},"labels":[],"label_agreement":null},{"id":"W1857261600","doi":"10.1029/2007gl031317","title":"Self‐consistent wave‐particle interactions in dispersive scale long‐period field‐line‐resonances","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Physics; Electron; Computational physics; Landau damping; Plasma; Particle acceleration; Waves in plasmas; Atomic physics; Magnetic field; Geophysics","score_opus":0.0201625025623563,"score_gpt":0.3108115829779937,"score_spread":0.2906490804156374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1857261600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94817567,0.00014559661,0.03742002,0.0004538815,0.000061546394,0.000055906035,0.0001807435,0.00028508418,0.013221529],"genre_scores_gemma":[0.9911505,0.000058815516,0.005778892,0.000065137,0.000015175158,0.000077995806,0.000119773285,0.00008681417,0.0026469873],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998559,0.000040969513,0.0000067901406,0.000016746852,0.00003503493,0.000044580866],"domain_scores_gemma":[0.9993524,0.00029057814,0.000098369725,0.000050645674,0.000095796,0.000112249654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005983171,0.00039866182,0.0008103545,0.0004902579,0.0011855746,0.0011035547,0.00097341806,0.0011716494,0.0025920812],"category_scores_gemma":[0.0014716038,0.00063428504,0.00052838016,0.00040772758,0.0014250679,0.0009920814,0.0010654188,0.00064040825,0.00025296383],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077240315,0.000041099946,0.0011277552,0.000022816872,0.000024667203,0.00012902448,0.00008424232,0.9863694,0.0015338733,0.009402025,0.00036424975,0.0008235189],"study_design_scores_gemma":[0.000041274357,0.00001212254,0.00020607759,0.0000017898918,0.0000025653644,0.0000057177535,0.000028268501,0.997951,0.00019160187,0.001421233,0.00013268292,0.000005686762],"about_ca_topic_score_codex":0.012014615,"about_ca_topic_score_gemma":0.008608435,"teacher_disagreement_score":0.012014615,"about_ca_system_score_codex":0.0011867208,"about_ca_system_score_gemma":0.0010451698,"threshold_uncertainty_score":0.023889363},"labels":[],"label_agreement":null},{"id":"W1858207246","doi":"10.1002/2013gl058558","title":"Glacier velocities and dynamic ice discharge from the Queen Elizabeth Islands, Nunavut, Canada","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; University of Ottawa; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; Canadian Space Agency; Sight Research UK; ArcticNet; University of Ottawa","keywords":"Glacier; Surge; Arctic; Archipelago; Climatology; Geology; Ice stream; Glacier ice accumulation; Groenlandia; Arctic ice pack; Physical geography; Oceanography; Cryosphere; Antarctic sea ice; Sea ice; Ice sheet; Geography; Geomorphology","score_opus":0.017446725239959,"score_gpt":0.23949649389404717,"score_spread":0.22204976865408818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1858207246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9858726,0.0005158294,0.00015251212,0.0002334429,0.00001718111,0.000029918558,0.0066504683,0.000024929182,0.0065031913],"genre_scores_gemma":[0.99127734,0.00041312436,0.0004045066,0.00006588672,0.00000457673,0.000019405516,0.0030956166,0.000015339376,0.0047041206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998203,0.00001056032,0.0000092297805,0.00004038113,0.000060830807,0.000058795336],"domain_scores_gemma":[0.99876785,0.00007626347,0.00009660901,0.0000368136,0.0007799264,0.00024251164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002752421,0.000253738,0.00017663698,0.00093600893,0.0018711578,0.0010811044,0.00079966325,0.00018816954,0.0022823915],"category_scores_gemma":[0.00096065894,0.00020597264,0.000165691,0.001699833,0.0005068018,0.00026637246,0.00063155184,0.00042205924,0.0003089681],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014598634,0.00003076916,0.9796379,0.000050294868,0.000060371116,0.00019416871,0.0018018888,0.0010355803,0.0014288302,0.00030371893,0.0039739707,0.011336471],"study_design_scores_gemma":[0.0000047779404,0.000006715837,0.995265,0.000031542015,0.00000984037,0.00003190442,0.0017462379,0.00048373584,0.0002444885,0.000028064112,0.0021344211,0.000013256497],"about_ca_topic_score_codex":0.99641246,"about_ca_topic_score_gemma":0.99885476,"teacher_disagreement_score":0.01841186,"about_ca_system_score_codex":0.01841186,"about_ca_system_score_gemma":0.017041698,"threshold_uncertainty_score":0.13358802},"labels":[],"label_agreement":null},{"id":"W1860473002","doi":"10.1029/2007gl030471","title":"Strong dependence of cubic ice formation on droplet ammonium to sulfate ratio","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; University of Leeds; Sight Research UK; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Tropopause; Troposphere; Ammonium sulfate; Aqueous solution; Ice nucleus; Ice crystals; Ammonium; Ice cloud; Ozone; Phase (matter); Sulfate; Atmospheric sciences; Materials science; Chemistry; Geology; Meteorology; Nucleation; Physics; Satellite; Physical chemistry; Chromatography; Organic chemistry","score_opus":0.034981759418876525,"score_gpt":0.29812977417230024,"score_spread":0.2631480147534237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1860473002","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996274,0.0003892669,0.0010835241,0.000054507855,0.00001215685,0.000013986058,0.00029845873,0.000063494466,0.0018106918],"genre_scores_gemma":[0.9987447,0.0001585219,0.00048423302,0.00001675014,0.000005433123,0.000007850498,0.00019178848,0.00001296185,0.00037763792],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989367,0.0000069511416,0.0000063843313,0.000029841098,0.00003555258,0.000027571303],"domain_scores_gemma":[0.999635,0.0001537922,0.00007841824,0.00002549668,0.00007083789,0.000036560636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000094481446,0.0002218604,0.00020034787,0.00012399943,0.00010951559,0.0002640014,0.00016723921,0.00014688956,0.0014372057],"category_scores_gemma":[0.00044295573,0.00012252669,0.00014080142,0.00008648414,0.00022529837,0.00023409877,0.00020603176,0.00038376616,0.00025373243],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007866429,0.000009179677,0.002600026,0.000029767187,0.0000065114655,0.000060779814,0.000023138908,0.00028333883,0.99549556,0.00005145055,0.000039890794,0.0013216581],"study_design_scores_gemma":[0.0000065850722,0.000117176576,0.016780434,0.0000021420947,0.000006807459,0.00009402571,0.000021291182,0.0030089822,0.97963744,0.000052957046,0.00026581192,0.0000064466726],"about_ca_topic_score_codex":0.0014917374,"about_ca_topic_score_gemma":0.001191335,"teacher_disagreement_score":0.0014917374,"about_ca_system_score_codex":0.0001870324,"about_ca_system_score_gemma":0.00014180428,"threshold_uncertainty_score":0.004807949},"labels":[],"label_agreement":null},{"id":"W1860521957","doi":"10.1002/2014gl060840","title":"Characteristics of the O<sup>+</sup>(<sup>2</sup>P–<sup>2</sup>D) 732.0 and 733.0 nm airglow emissions observed with WINDII and simulated with the C‐IAM","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Airglow; Solar zenith angle; Zenith; Thermosphere; Atmosphere (unit); Photoelectric effect; Physics; Atmospheric sciences; Aeronomy; Twilight; Atomic physics; Flux (metallurgy); Photoionization; Mesosphere; Ionosphere; Environmental science; Ionization; Optics; Meteorology; Stratosphere; Materials science; Astronomy; Ion","score_opus":0.013390904275452292,"score_gpt":0.242008231210858,"score_spread":0.2286173269354057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1860521957","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979528,0.000027110444,0.000690797,0.000016145954,0.0000025774439,0.0000037019288,0.00030025316,0.000059100243,0.0009472926],"genre_scores_gemma":[0.9993162,0.000010670334,0.00020089962,0.0000041632566,0.0000012362037,0.000002750669,0.00033515776,0.000012592489,0.00011643723],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999653,0.000003502351,0.00000119778,0.00001000535,0.000010234633,0.000009687442],"domain_scores_gemma":[0.99990857,0.000034643548,0.0000126464465,0.0000063540133,0.000022217504,0.000015568172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010356919,0.0001964125,0.000107073734,0.00017191035,0.000154889,0.00021784166,0.0001584752,0.00022440075,0.000770157],"category_scores_gemma":[0.00019247932,0.00011968334,0.00018348393,0.00022126632,0.00011084749,0.00015125048,0.00009173389,0.00018207368,0.00012813984],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017128852,0.00019061065,0.5631293,0.0001003247,0.00017948134,0.0007961827,0.00039913584,0.094316006,0.3055762,0.0007934755,0.0017893692,0.031017054],"study_design_scores_gemma":[0.00006241558,0.000121854646,0.86390764,0.000007317089,0.00003705902,0.00013915867,0.0001390467,0.10816044,0.026193175,0.00014853523,0.0010601551,0.000023199635],"about_ca_topic_score_codex":0.0069302316,"about_ca_topic_score_gemma":0.008993988,"teacher_disagreement_score":0.0069302316,"about_ca_system_score_codex":0.00025403165,"about_ca_system_score_gemma":0.000084015905,"threshold_uncertainty_score":0.013779759},"labels":[],"label_agreement":null},{"id":"W1860838469","doi":"10.1002/grl.50399","title":"Impact of the high topography of Madagascar on the structure of the Findlater Jet","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Intertropical Convergence Zone; Equator; Jet (fluid); Eddy; Boreal; Climatology; Jet stream; Monsoon; Oceanography; Atmospheric sciences; Latitude; Turbulence; Geography; Physics; Meteorology; Paleontology; Geodesy; Mechanics","score_opus":0.013219510184193215,"score_gpt":0.24371210032281304,"score_spread":0.23049259013861984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1860838469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998379,0.0000464945,0.00003771306,0.00004765068,0.0000023712003,0.0000022662452,0.000087455315,0.0000061425644,0.0013908695],"genre_scores_gemma":[0.99981374,0.00003047157,0.000034685385,0.0000072871744,0.0000012829499,0.0000011224644,0.000052524527,0.0000013986771,0.00005740329],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999547,0.0000073630513,0.0000024769533,0.000009299962,0.000008064126,0.00001799488],"domain_scores_gemma":[0.9998167,0.00004655071,0.00007238658,0.000012598954,0.000020063415,0.000031746644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000071125876,0.00012958188,0.00011639363,0.00036168384,0.000431891,0.00082796125,0.000103013386,0.00011586729,0.0013106238],"category_scores_gemma":[0.00037980016,0.000060354207,0.00009690689,0.00041549752,0.0003385178,0.00018762275,0.00036291324,0.0001916947,0.00005457564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021028254,0.000049565544,0.9476805,0.000055494264,0.00006155486,0.0022265997,0.0009724038,0.0037609579,0.025960337,0.00062691746,0.00052703737,0.017868433],"study_design_scores_gemma":[0.000004434061,0.000019376494,0.9964625,0.000006776531,0.000010641953,0.00009397768,0.00054465554,0.0018344343,0.0004892293,0.000030654366,0.00049798674,0.000005383912],"about_ca_topic_score_codex":0.03607938,"about_ca_topic_score_gemma":0.046554066,"teacher_disagreement_score":0.03607938,"about_ca_system_score_codex":0.0004263643,"about_ca_system_score_gemma":0.00025402533,"threshold_uncertainty_score":0.07173872},"labels":[],"label_agreement":null},{"id":"W1863178690","doi":"10.1002/2013gl058635","title":"Vulnerability of shallow subarctic lakes to evaporate and desiccate when snowmelt runoff is low","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; Brock University; Wilfrid Laurier University; Université Laval; Center for Northern Studies","funders":"","keywords":"Snowmelt; Subarctic climate; Tundra; Surface runoff; Environmental science; Snow; Hydrology (agriculture); Meltwater; Physical geography; Permafrost; Arctic; Geology; Ecology; Oceanography; Geography; Geomorphology","score_opus":0.07323285884720032,"score_gpt":0.3078873663834862,"score_spread":0.23465450753628586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1863178690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998287,0.000017421653,0.000014489673,0.000006254449,1.9004223e-7,5.4429495e-7,0.00003731062,0.0000012351485,0.00009371144],"genre_scores_gemma":[0.99986196,0.000015781474,0.000020794705,0.0000047904373,5.0077523e-7,6.099589e-7,0.0000543786,4.660501e-7,0.00004061962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999292,0.0000088937095,0.0000040069162,0.00001737414,0.000009091315,0.00003143174],"domain_scores_gemma":[0.99976546,0.000027776938,0.00010228105,0.000012158674,0.000040479932,0.000051850915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013165663,0.00013342651,0.0001902567,0.000477445,0.00041457388,0.00054798357,0.00014917678,0.00015241056,0.00072176807],"category_scores_gemma":[0.0003460543,0.000108632856,0.000114822185,0.0005081863,0.00033617968,0.0002406727,0.0004875877,0.00012598264,0.00007136591],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004136062,0.0000070365672,0.9953601,0.000005684144,0.000022474858,0.000039941242,0.00021186948,0.00016722943,0.0030760476,0.000016112717,0.00003063783,0.0010214768],"study_design_scores_gemma":[6.1928085e-7,0.0000056532426,0.999395,0.000001026951,0.0000035731452,0.000013970178,0.00028777862,0.00014819267,0.000101464706,0.000011449886,0.000030327305,7.7949045e-7],"about_ca_topic_score_codex":0.05883355,"about_ca_topic_score_gemma":0.16289052,"teacher_disagreement_score":0.05883355,"about_ca_system_score_codex":0.00063058024,"about_ca_system_score_gemma":0.00031845068,"threshold_uncertainty_score":0.11698216},"labels":[],"label_agreement":null},{"id":"W1863393092","doi":"10.1002/grl.50191","title":"Arctic climate warming and sea ice declines lead to increased storm surge activity","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University; Brock University; Aboriginal Affairs Northern Dev Canada; Carleton University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Aboriginal Affairs and Northern Development Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Storm surge; Environmental science; Climate change; Global warming; Arctic; Storm; Surge; Climatology; Coastal flood; Sea ice; Lead (geology); Arctic ice pack; Oceanography; Geology; Sea level rise; Geography; Meteorology","score_opus":0.029045855042499256,"score_gpt":0.28207992391331316,"score_spread":0.2530340688708139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1863393092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652314,0.0001448792,0.00010653574,0.00013078601,0.000012695033,0.0000035164892,0.0003000095,0.00001362308,0.0027648583],"genre_scores_gemma":[0.9991904,0.000114782335,0.000053237214,0.000043631742,0.000007802892,0.000002147689,0.00016775788,0.000002447471,0.0004177302],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990404,0.000022227448,0.00000610469,0.00002075643,0.000015645588,0.000031283973],"domain_scores_gemma":[0.9995968,0.000073283125,0.00016167779,0.000027849006,0.00006589764,0.00007450038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022585846,0.00011471395,0.00012332424,0.00027346058,0.00028747693,0.00055026193,0.00009064572,0.0001571928,0.002545461],"category_scores_gemma":[0.0007708887,0.000067055655,0.00019077078,0.00025373074,0.00022550812,0.00013319793,0.00028859242,0.00021332827,0.00020495999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003503242,0.00006978403,0.98026204,0.000041544125,0.00012453477,0.0002189045,0.00012315268,0.0010395847,0.0093255155,0.0001673976,0.0009902144,0.00728696],"study_design_scores_gemma":[0.0000027335925,0.00003198139,0.9982704,0.000004969151,0.000014571799,0.00003035162,0.00017335865,0.0002653082,0.0006047339,0.000055740373,0.00054458814,0.000001250499],"about_ca_topic_score_codex":0.030092813,"about_ca_topic_score_gemma":0.060863778,"teacher_disagreement_score":0.030092813,"about_ca_system_score_codex":0.00038287728,"about_ca_system_score_gemma":0.00041658065,"threshold_uncertainty_score":0.059835315},"labels":[],"label_agreement":null},{"id":"W1864122870","doi":"10.1002/2015gl063365","title":"Toward an internal gravity wave spectrum in global ocean models","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Office of Naval Research; Stennis Space Center; Centre National de la Recherche Scientifique; University of Michigan; U.S. Department of Defense; National Science Foundation","keywords":"Internal wave; Kinetic energy; Gravity wave; Physics; Spectral line; Dispersion (optics); Computational physics; Nonlinear system; Wind wave; Gravitational wave; Inertial frame of reference; Wave propagation; Mechanics; Geophysics; Geology; Classical mechanics; Optics; Astrophysics","score_opus":0.0809921211353771,"score_gpt":0.3008728186191071,"score_spread":0.21988069748373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1864122870","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.78734577,0.00022408822,0.19955748,0.0007696237,0.000054945984,0.000035917667,0.00034074057,0.0007350923,0.010936394],"genre_scores_gemma":[0.98496014,0.00009826659,0.014146309,0.000034258872,0.000013301944,0.00002132373,0.00012228146,0.00008629468,0.00051790907],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998733,0.00006053373,0.000006102674,0.000014711717,0.000033221033,0.000012163661],"domain_scores_gemma":[0.99964476,0.00012054634,0.000046248293,0.000070936534,0.00009018883,0.00002736256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007094794,0.00038792353,0.00028704942,0.00041438386,0.00024549398,0.0008502914,0.000452243,0.00036564074,0.0005836085],"category_scores_gemma":[0.0023674977,0.0003837455,0.00031398205,0.00032601497,0.00040810788,0.0010204955,0.0007560192,0.00064357155,0.00013325014],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022734584,0.000031059382,0.0074938075,0.000012701011,0.00002714455,0.000027479822,0.00006173292,0.9744805,0.001951373,0.008378906,0.000415438,0.007097106],"study_design_scores_gemma":[0.0000067232054,0.00000533512,0.00080018793,0.0000044341195,0.0000030059773,0.0000028714687,0.000010735078,0.9964491,0.00022845516,0.0023286075,0.00015776753,0.0000028081683],"about_ca_topic_score_codex":0.008475063,"about_ca_topic_score_gemma":0.005123795,"teacher_disagreement_score":0.008475063,"about_ca_system_score_codex":0.0004869263,"about_ca_system_score_gemma":0.00037269757,"threshold_uncertainty_score":0.016851485},"labels":[],"label_agreement":null},{"id":"W1864504472","doi":"10.1029/2004gl019502","title":"Sensitivity of Asian dust storm to natural and anthropogenic factors","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Desertification; Precipitation; Storm; Dust storm; Environmental science; Natural (archaeology); China; Vegetation (pathology); Chine; Physical geography; Spring (device); Asian Dust; Climatology; Atmospheric sciences; Geology; Geography; Meteorology; Aerosol; Oceanography; Ecology","score_opus":0.018228818335962897,"score_gpt":0.2900949140003002,"score_spread":0.2718660956643373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1864504472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99888605,0.000041603915,0.00008678677,0.000027507085,0.0000024744338,0.000002697686,0.00019443552,0.000006858295,0.0007515352],"genre_scores_gemma":[0.9996325,0.00004187656,0.00003079934,0.000008855486,0.0000020521002,0.0000017721853,0.00017892319,0.0000018886884,0.0001013855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999813,0.00004529518,0.000017749557,0.0000395696,0.000028209515,0.00005611673],"domain_scores_gemma":[0.9991708,0.00020683186,0.00021145945,0.00008711572,0.0002188788,0.00010491429],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040478024,0.00020568827,0.00023296585,0.0002798068,0.0002551436,0.0007424385,0.00018408711,0.00018666915,0.0007620059],"category_scores_gemma":[0.00081530656,0.00011317458,0.00029268558,0.00048411108,0.00022811942,0.00030151993,0.00039432614,0.0001845604,0.0001465707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003686871,0.000036774407,0.9794836,0.00003390063,0.00018112376,0.00034202333,0.0002807299,0.0062723956,0.008622862,0.00018985444,0.00025321447,0.003934733],"study_design_scores_gemma":[0.000009462979,0.00005052419,0.99109125,0.0000031944062,0.00004351078,0.0001331473,0.00052924844,0.0046047135,0.0030507264,0.00009471399,0.00037974832,0.000009718599],"about_ca_topic_score_codex":0.024607267,"about_ca_topic_score_gemma":0.017430516,"teacher_disagreement_score":0.024607267,"about_ca_system_score_codex":0.00053116505,"about_ca_system_score_gemma":0.00036004884,"threshold_uncertainty_score":0.048928082},"labels":[],"label_agreement":null},{"id":"W1866038626","doi":"10.1002/2015gl064477","title":"Yardang evolution from maturity to demise","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Compute Canada; Western Canada Research Grid; Lancaster University; University of Calgary","keywords":"Aeolian processes; Geology; Denudation; Erosion; Sediment; Bedform; Substrate (aquarium); Geomorphology; Earth science; Oceanography; Sediment transport; Paleontology","score_opus":0.04840937410802958,"score_gpt":0.3033712401759602,"score_spread":0.2549618660679306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1866038626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954308,0.00008131018,0.0015636304,0.00003171968,0.0000013122441,0.0000033512326,0.00024362054,0.000031569783,0.0026125952],"genre_scores_gemma":[0.9990771,0.000030508792,0.0003415181,0.0000038120447,4.7503394e-7,0.0000027034077,0.00013041806,0.0000053885387,0.00040803503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992716,0.000013205577,0.0000030387746,0.000026250407,0.000008707917,0.000021663413],"domain_scores_gemma":[0.99964404,0.00008881821,0.00009756549,0.000046239173,0.000038403217,0.000084872496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026255706,0.00015410513,0.00014799503,0.00038771908,0.0002754172,0.00075738644,0.0003402973,0.00033541903,0.0028876637],"category_scores_gemma":[0.0011203901,0.00015736619,0.0002682352,0.00025420124,0.00037117465,0.00046570576,0.000573416,0.0003225678,0.00035363878],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004317925,0.00007956279,0.72092927,0.00011286615,0.00016215105,0.0007852776,0.0008339433,0.16313379,0.041434426,0.029667187,0.0009786452,0.041451134],"study_design_scores_gemma":[0.000025874197,0.00035930064,0.78381026,0.00006207992,0.000067348505,0.0010900375,0.0007509071,0.186082,0.0051790806,0.014705066,0.0078108646,0.000057154768],"about_ca_topic_score_codex":0.0032335154,"about_ca_topic_score_gemma":0.005718557,"teacher_disagreement_score":0.0032335154,"about_ca_system_score_codex":0.0006272574,"about_ca_system_score_gemma":0.00015385378,"threshold_uncertainty_score":0.009660184},"labels":[],"label_agreement":null},{"id":"W1866976455","doi":"10.1029/2012gl054315","title":"Toward quantifying discrete groundwater discharge from frozen seepage faces using thermal infrared images","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"École de Technologie Supérieure; Université du Québec à Montréal; McGill University","funders":"","keywords":"Geology; Groundwater; Infrared; Thermal; Hydrology (agriculture); Environmental science; Geomorphology; Geotechnical engineering; Meteorology","score_opus":0.08855495707474824,"score_gpt":0.3308190893183681,"score_spread":0.24226413224361987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1866976455","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96915,0.00010360806,0.029849973,0.000009096349,0.000003935229,0.000037565384,0.00017502287,0.00005788366,0.00061293907],"genre_scores_gemma":[0.96813744,0.00013330716,0.031329025,0.000009088543,0.0000027403921,0.00004171935,0.000119591416,0.000009634183,0.00021741829],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.000014493691,0.000004289953,0.00003845102,0.000032639306,0.000013871665],"domain_scores_gemma":[0.9998722,0.000036213518,0.000037596245,0.000012823969,0.00002604027,0.000015251353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021631252,0.00024397168,0.000184502,0.0004045667,0.00014517184,0.00034689574,0.00025148512,0.00020879449,0.00046827114],"category_scores_gemma":[0.00038616758,0.00017994082,0.0001259178,0.0002745481,0.00035452354,0.0003382147,0.00028599962,0.00027610315,0.0000691159],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001469135,0.000052075648,0.011738271,0.000047472517,0.0000073124675,0.00003270963,0.000075059186,0.0035340001,0.9765602,0.00016933927,0.000022778951,0.00761381],"study_design_scores_gemma":[0.00003429921,0.00082230923,0.16143046,0.000027764585,0.00006287952,0.00022980156,0.0003044655,0.07756941,0.75822747,0.0005868088,0.00065857935,0.00004570091],"about_ca_topic_score_codex":0.0015451103,"about_ca_topic_score_gemma":0.002501767,"teacher_disagreement_score":0.0015451103,"about_ca_system_score_codex":0.00023099867,"about_ca_system_score_gemma":0.00016773253,"threshold_uncertainty_score":0.0030722618},"labels":[],"label_agreement":null},{"id":"W1867260020","doi":"10.1002/2015gl065142","title":"Variations in grain size and viscosity based on vacancy diffusion in minerals, seismic tomography, and geodynamically inferred mantle rheology","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Geology; Grain size; Rheology; Viscosity; Seismic tomography; Arrhenius equation; Diffusion creep; Mineralogy; Geophysics; Thermodynamics; Materials science; Grain boundary; Physics; Microstructure; Activation energy; Chemistry; Composite material","score_opus":0.020162965224324418,"score_gpt":0.26829727936257997,"score_spread":0.24813431413825554,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1867260020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964347,0.00005842672,0.003088184,0.00001884699,0.0000017137115,0.0000023142863,0.00008274261,0.000038824684,0.00027423608],"genre_scores_gemma":[0.9992619,0.000016486569,0.0006584114,0.0000017952093,0.0000011549971,9.2113817e-7,0.000035382178,0.0000041077155,0.000019728828],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999429,0.000009941525,0.0000037842028,0.000018989092,0.000016367076,0.000007969406],"domain_scores_gemma":[0.9994684,0.00023597192,0.00016886668,0.0000441075,0.000045245986,0.000037420054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024064838,0.00018201933,0.0001526453,0.0010706114,0.00011415929,0.0005596221,0.00023373768,0.00021736984,0.00045490655],"category_scores_gemma":[0.0016039977,0.00023389462,0.00014915559,0.00045373273,0.0003377971,0.00064979977,0.0003427854,0.00019503078,0.00007848196],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058130146,0.00006382123,0.40374577,0.00007447396,0.00013733948,0.00026515563,0.00025837115,0.035355072,0.5348967,0.0016008166,0.00016853119,0.022852702],"study_design_scores_gemma":[0.000026747535,0.000066584995,0.68592066,0.000011502425,0.00005477686,0.00023725553,0.00010617323,0.2612088,0.050837394,0.0012465105,0.00023808805,0.000045559616],"about_ca_topic_score_codex":0.0023171802,"about_ca_topic_score_gemma":0.002807574,"teacher_disagreement_score":0.0023171802,"about_ca_system_score_codex":0.00024808836,"about_ca_system_score_gemma":0.000078394514,"threshold_uncertainty_score":0.0046073794},"labels":[],"label_agreement":null},{"id":"W1868050845","doi":"10.1002/grl.50098","title":"Recent changes in pan‐Arctic melt onset from satellite passive microwave measurements","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos; Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; University of East Anglia","keywords":"Satellite; Snow; Arctic; Environmental science; Climatology; Brightness temperature; Microwave; Radar; Remote sensing; Geology; Atmospheric sciences; Meteorology; Oceanography; Geography","score_opus":0.09093919681231329,"score_gpt":0.28851659454172185,"score_spread":0.19757739772940858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1868050845","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99128574,0.0007157449,0.0012938563,0.00007012193,0.000029028042,0.000008016309,0.004739788,0.00007043372,0.001787256],"genre_scores_gemma":[0.9859801,0.00069032435,0.0021175935,0.000033214787,0.00006327023,0.000012533965,0.010612482,0.000018452942,0.00047217845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999163,0.000009242401,0.00000875198,0.000029867344,0.0000251006,0.000010684402],"domain_scores_gemma":[0.9996793,0.000035063935,0.00009362348,0.000017483857,0.0001500709,0.000024464944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004195935,0.00022135413,0.00015323854,0.00087954174,0.00013558089,0.00038566097,0.00010413733,0.00015388003,0.00041250192],"category_scores_gemma":[0.00061266264,0.000084724714,0.00018497513,0.0010075805,0.00006400853,0.00028585267,0.00020654533,0.00016144663,0.00016051765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037549416,0.000040621475,0.91866475,0.00015664163,0.00018315305,0.00011457644,0.00024993523,0.002828483,0.025294207,0.00012864533,0.0014716284,0.050491877],"study_design_scores_gemma":[0.0000036113258,0.000017669647,0.9930193,0.0000108597205,0.000033890752,0.00003094402,0.000036534755,0.0023636227,0.0019988269,0.000022769278,0.002458006,0.0000039754377],"about_ca_topic_score_codex":0.012997996,"about_ca_topic_score_gemma":0.02498572,"teacher_disagreement_score":0.012997996,"about_ca_system_score_codex":0.00030263362,"about_ca_system_score_gemma":0.0001512019,"threshold_uncertainty_score":0.025844634},"labels":[],"label_agreement":null},{"id":"W1873576635","doi":"10.1002/grl.50483","title":"Abyssal connections of Antarctic Bottom Water in a Southern Ocean State Estimate","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Antarctic Climate and Ecosystems Cooperative Research Centre; Australian Research Council; National Science Foundation","keywords":"Antarctic Bottom Water; Abyssal zone; Circumpolar deep water; Geology; Oceanography; Subtropics; Circumpolar star; Antarctic Intermediate Water; Abyssal plain; Bottom water; Weddell Sea Bottom Water; Oceanic basin; Temperature salinity diagrams; Salinity; Climatology; Structural basin; North Atlantic Deep Water; Thermohaline circulation; Paleontology; Ice shelf; Sea ice","score_opus":0.017487659002047712,"score_gpt":0.261658907367531,"score_spread":0.2441712483654833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1873576635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99033207,0.00007956621,0.0020395017,0.00021528595,0.000012629862,0.0000067177066,0.0019049565,0.00005605817,0.0053531425],"genre_scores_gemma":[0.9975674,0.00005260029,0.0006139167,0.0000079566935,0.0000028677907,0.0000029705268,0.0010720884,0.0000044289054,0.0006758777],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999918,0.000020899895,0.000008996798,0.000022653974,0.000019565783,0.0000099492145],"domain_scores_gemma":[0.9995766,0.00014113195,0.000089485315,0.00004073455,0.00012449376,0.000027449007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029285697,0.00008374994,0.00010319281,0.0006420332,0.00018368874,0.0008303156,0.00011101811,0.00012544345,0.0019323161],"category_scores_gemma":[0.0018241345,0.00011646023,0.00017248782,0.00071280834,0.00016182777,0.0003440244,0.0006288976,0.00023015162,0.00016502074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012578815,0.00001993601,0.9110923,0.00002273561,0.000100821,0.00008926285,0.00025977133,0.058440804,0.00087070477,0.007461947,0.00078415463,0.020731803],"study_design_scores_gemma":[0.000021478036,0.00004287935,0.7739232,0.000025284106,0.000050307182,0.00004797201,0.0006209141,0.21222423,0.0008937084,0.004480582,0.0076474906,0.000021933842],"about_ca_topic_score_codex":0.050869074,"about_ca_topic_score_gemma":0.042265132,"teacher_disagreement_score":0.050869074,"about_ca_system_score_codex":0.0005258168,"about_ca_system_score_gemma":0.00036055085,"threshold_uncertainty_score":0.10114598},"labels":[],"label_agreement":null},{"id":"W1878965460","doi":"10.1029/2012gl051574","title":"Storm‐induced upwelling of high <i>p</i>CO<sub>2</sub> waters onto the continental shelf of the western Arctic Ocean and implications for carbonate mineral saturation states","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Oceanography; Upwelling; Geology; Continental shelf; Sea ice; Arctic sea ice decline; Arctic; Aragonite; Arctic geoengineering; Ekman transport; Arctic ice pack; Climatology; Antarctic sea ice; Geochemistry","score_opus":0.02093216914503174,"score_gpt":0.2601537440938494,"score_spread":0.23922157494881766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1878965460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99910885,0.00005617939,0.000028552391,0.000063136664,0.000007449935,0.0000021621408,0.00009488391,0.0000035711034,0.0006352308],"genre_scores_gemma":[0.99950445,0.000071441835,0.000030586478,0.000044503908,0.000008468032,0.000002228332,0.00013585402,0.0000012550826,0.00020127404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999936,0.000008854425,0.0000039555653,0.000013369821,0.000013447466,0.000024360552],"domain_scores_gemma":[0.99979347,0.000013518426,0.00007786249,0.000010489236,0.000046085297,0.00005855304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015732236,0.00017650129,0.00014410533,0.00022536347,0.0004932015,0.0005907569,0.00012530488,0.0002489829,0.00071783137],"category_scores_gemma":[0.0001919859,0.00015625417,0.0002836112,0.00027826912,0.00032786798,0.00016694685,0.00022894522,0.0001783888,0.000099777964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006387886,0.00008072977,0.89721715,0.000042901804,0.0001131738,0.0009357903,0.00061424676,0.001225668,0.09138703,0.0001666766,0.0009444818,0.0066333436],"study_design_scores_gemma":[0.0000021695382,0.00002275916,0.99913484,0.0000013066077,0.0000045632496,0.000022135326,0.00012972856,0.00020205318,0.00032724362,0.000013094713,0.00013804215,0.0000020840619],"about_ca_topic_score_codex":0.09390429,"about_ca_topic_score_gemma":0.1127691,"teacher_disagreement_score":0.09390429,"about_ca_system_score_codex":0.0010636958,"about_ca_system_score_gemma":0.0006835245,"threshold_uncertainty_score":0.18671542},"labels":[],"label_agreement":null},{"id":"W1879898335","doi":"10.1002/2015gl065245","title":"Observations of coincident EMIC wave activity and duskside energetic electron precipitation on 18–19 January 2013","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Natural Environment Research Council; Sight Research UK; Dartmouth College; National Aeronautics and Space Administration","keywords":"Electron precipitation; Physics; Van Allen radiation belt; Substorm; Geophysics; Magnetosphere; Astrophysics; Van Allen Probes; Electron; Emic and etic; Precipitation; Computational physics; Atmospheric sciences; Meteorology; Magnetic field; Nuclear physics","score_opus":0.05351721538147047,"score_gpt":0.313430081626218,"score_spread":0.2599128662447475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1879898335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978654,0.00007726989,0.00020129998,0.000026116306,0.000010977475,0.000008333942,0.00053209043,0.00001926401,0.0012593962],"genre_scores_gemma":[0.9979079,0.00010008775,0.00032891234,0.00001779352,0.000029342824,0.00000992823,0.0010873487,0.0000073651895,0.0005114206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987936,0.000012926761,0.000011023994,0.000025984566,0.000041334362,0.000029381621],"domain_scores_gemma":[0.99961495,0.00003170702,0.00017036531,0.0000311036,0.00009472181,0.00005706812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021327479,0.00017592548,0.00028733857,0.00075505406,0.00046357448,0.0004424563,0.00018802534,0.00021958207,0.0008461068],"category_scores_gemma":[0.0004910605,0.00011986893,0.00015407265,0.00049949315,0.00020682557,0.00018370678,0.00070587563,0.00029342488,0.00017056984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006758681,0.00008640248,0.94507676,0.000047327223,0.00009755834,0.00055049575,0.0008688504,0.0004698125,0.037220497,0.00015682977,0.0008929469,0.0138567155],"study_design_scores_gemma":[0.0000071565164,0.00004877582,0.99672216,0.000005652218,0.00001134624,0.00010329367,0.00010952321,0.0001843294,0.0016019193,0.000013358789,0.0011896933,0.0000027188885],"about_ca_topic_score_codex":0.009821125,"about_ca_topic_score_gemma":0.028591972,"teacher_disagreement_score":0.009821125,"about_ca_system_score_codex":0.00034050838,"about_ca_system_score_gemma":0.00023794657,"threshold_uncertainty_score":0.019527912},"labels":[],"label_agreement":null},{"id":"W1880216166","doi":"10.1002/2015gl063699","title":"Real‐time imaging of density ducts between the plasmasphere and ionosphere","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Theoretical Astrophysics; University of Toronto","funders":"Australian Research Council; U.S. Air Force; Ministero dello Sviluppo Economico; Victoria University; Smithsonian Astrophysical Observatory; Astronomy Australia Limited; Victoria University of Wellington; Nvidia; Australian National University; Commonwealth Scientific and Industrial Research Organisation; Air Force Office of Scientific Research; Australian Government; Curtin University of Technology; Smithsonian Institution; Harvard University; Australia-India Strategic Research Fund; National Science Foundation","keywords":"Plasmasphere; Ionosphere; Geophysics; Physics; Geology; Magnetosphere; Plasma; Earth's magnetic field; Magnetic field","score_opus":0.02031711412390262,"score_gpt":0.2809748850065999,"score_spread":0.26065777088269726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1880216166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98459446,0.00023067012,0.013134298,0.000053700147,0.000011570478,0.000009959339,0.00019767552,0.0001268374,0.0016408067],"genre_scores_gemma":[0.98681366,0.00010972371,0.012192192,0.000022912032,0.000014426108,0.000007908505,0.00016412318,0.000021267626,0.0006536558],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999726,0.0000024343572,6.8262136e-7,0.0000093000035,0.0000072409985,0.0000077233235],"domain_scores_gemma":[0.9999293,0.000014749293,0.000020509808,0.000007733484,0.000012174592,0.000015518985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000063147854,0.00009713161,0.00007936424,0.00034190336,0.00011332436,0.00024209592,0.00016229245,0.00020480859,0.0007151101],"category_scores_gemma":[0.00011961728,0.000101622274,0.000046819412,0.00021356884,0.00013545644,0.00026374502,0.00021905806,0.00018541394,0.00014852572],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000083859086,0.000015756774,0.0092831245,0.000023871044,0.000009258938,0.00015954809,0.00010468949,0.00029797928,0.9789211,0.00019256427,0.00022464745,0.010683639],"study_design_scores_gemma":[0.00005426696,0.00040512788,0.514977,0.00004290991,0.00005875474,0.003545193,0.00077106,0.030487029,0.44015443,0.0008549568,0.008603678,0.00004563504],"about_ca_topic_score_codex":0.000360628,"about_ca_topic_score_gemma":0.0006717165,"teacher_disagreement_score":0.0007151101,"about_ca_system_score_codex":0.00008627205,"about_ca_system_score_gemma":0.00008229445,"threshold_uncertainty_score":0.002392292},"labels":[],"label_agreement":null},{"id":"W1882246716","doi":"10.1029/2010gl045520","title":"Rain impacts on CO<sub>2</sub> exchange in the western equatorial Pacific Ocean","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Dalhousie University","funders":"","keywords":"Environmental science; Pacific ocean; Carbon cycle; Sink (geography); Atmosphere (unit); Carbon sink; Oceanography; Precipitation; Climatology; Atmospheric sciences; Carbon dioxide; Ocean heat content; Carbon flux; Ocean current; Geology; Meteorology; Climate change; Geography; Chemistry; Ecosystem","score_opus":0.01835972182259931,"score_gpt":0.2753957125971514,"score_spread":0.2570359907745521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1882246716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993075,0.000052981628,0.000031817017,0.00004878342,0.000002675777,0.0000020648704,0.00011049768,0.000004318603,0.0004393469],"genre_scores_gemma":[0.9994665,0.00013688079,0.000047294678,0.000039639075,0.000006076374,0.0000025103345,0.00012416276,0.0000032692728,0.00017367747],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994755,0.000011692615,0.0000048023658,0.000008936699,0.000009626424,0.000017344559],"domain_scores_gemma":[0.9998491,0.000034923174,0.000050002385,0.0000116945075,0.00002649356,0.000027704178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014426385,0.00018900675,0.00017566833,0.000122049074,0.00031588168,0.0004248607,0.00009375055,0.00019958196,0.0009496793],"category_scores_gemma":[0.00042499052,0.00012912933,0.00017529605,0.00020271522,0.00036929996,0.000309874,0.00047681032,0.00020387689,0.00009890881],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010963903,0.0001269854,0.86669576,0.00010019205,0.00019865441,0.0009465746,0.00038683586,0.0043402426,0.11152333,0.00026158942,0.00059530995,0.01372806],"study_design_scores_gemma":[0.0000135556875,0.000035194993,0.9964127,0.0000022487932,0.000028919128,0.000040647537,0.00013152268,0.00095939037,0.0020702071,0.00006108166,0.00024094712,0.0000037245484],"about_ca_topic_score_codex":0.023804454,"about_ca_topic_score_gemma":0.022500651,"teacher_disagreement_score":0.023804454,"about_ca_system_score_codex":0.00031106215,"about_ca_system_score_gemma":0.00032048367,"threshold_uncertainty_score":0.04733181},"labels":[],"label_agreement":null},{"id":"W1882535646","doi":"10.1029/2010gl046146","title":"Quantifying spatial and seasonal variability in atmospheric ammonia with in situ and space-based observations","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Spatial variability; Atmospheric sciences; Biogeochemical cycle; Mixing ratio; Climatology; Satellite; Troposphere; Atmosphere (unit); In situ; Meteorology; Geology; Geography; Physics; Chemistry","score_opus":0.04339688231231001,"score_gpt":0.25996341466930756,"score_spread":0.21656653235699755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1882535646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736637,0.0000523239,0.001362401,0.00001596725,0.0000029820837,0.000007283347,0.0004535606,0.000040440023,0.00069863047],"genre_scores_gemma":[0.99565756,0.00005822436,0.003213131,0.000010692622,0.0000067224405,0.000011380956,0.0008009817,0.000010201852,0.00023109978],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998493,0.000022682812,0.000006518374,0.00005668365,0.000039886643,0.000024858064],"domain_scores_gemma":[0.999749,0.000071634124,0.00008150807,0.000022408884,0.000056459256,0.000018896086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021445421,0.00020964727,0.00018178034,0.0006740848,0.00024331588,0.00036307727,0.0003230285,0.0002333558,0.0004005794],"category_scores_gemma":[0.000468327,0.00015204956,0.00016189167,0.0011023502,0.0001305616,0.00034354554,0.00022258266,0.00014540528,0.00007617523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003156166,0.00017505468,0.7275762,0.000115395414,0.00021061083,0.00026009086,0.0004621794,0.0082231,0.23608154,0.000098921366,0.00047188808,0.02600928],"study_design_scores_gemma":[0.000011484936,0.00006521071,0.9639221,0.0000063766506,0.000056808567,0.00008024237,0.0003120764,0.019008223,0.015753673,0.00005790427,0.00071020774,0.000015623576],"about_ca_topic_score_codex":0.041469295,"about_ca_topic_score_gemma":0.10184008,"teacher_disagreement_score":0.041469295,"about_ca_system_score_codex":0.0004084944,"about_ca_system_score_gemma":0.00026328652,"threshold_uncertainty_score":0.08245587},"labels":[],"label_agreement":null},{"id":"W1885577679","doi":"10.1002/2015gl063148","title":"Lifetimes and emissions of SO<sub>2</sub> from point sources estimated from OMI","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":254,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Earth Sciences Division","keywords":"Ozone Monitoring Instrument; Environmental science; Satellite; Sulfur dioxide; Ozone; Wind speed; Atmospheric sciences; Principal component analysis; Meteorology; Point (geometry); Point source; Computational physics; Remote sensing; Physics; Statistics; Mathematics; Geology; Optics; Chemistry","score_opus":0.04004534711940174,"score_gpt":0.27734900374754434,"score_spread":0.2373036566281426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1885577679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903132,0.00012693371,0.008097563,0.00002228067,0.0000040815416,0.000010376179,0.0007198664,0.00010450278,0.0006012515],"genre_scores_gemma":[0.99280447,0.00007182401,0.005779445,0.000004034462,0.000005928398,0.00001363592,0.0010832854,0.000014932573,0.00022247783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998956,0.00001800427,0.000004784827,0.000028586948,0.000043677817,0.00000937943],"domain_scores_gemma":[0.9997274,0.000066299115,0.00007447267,0.000027427868,0.0000916088,0.000012720194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002590676,0.00024112563,0.00016816235,0.00076548225,0.00014137468,0.00020318912,0.0002260797,0.00021088465,0.00031060696],"category_scores_gemma":[0.0006115448,0.00014996805,0.00022046674,0.00049314386,0.0000907117,0.00031649874,0.00019073732,0.00020319474,0.00011765379],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047281405,0.00009746876,0.69129556,0.00018216683,0.00027561907,0.00017993947,0.000394103,0.051262602,0.18834795,0.000831984,0.0008840231,0.06577592],"study_design_scores_gemma":[0.000024987297,0.00014781748,0.78251296,0.000022012886,0.000116896015,0.00018825756,0.00018723305,0.12179727,0.091139674,0.00073831953,0.0030721803,0.000052396128],"about_ca_topic_score_codex":0.004906295,"about_ca_topic_score_gemma":0.008376781,"teacher_disagreement_score":0.004906295,"about_ca_system_score_codex":0.0003730411,"about_ca_system_score_gemma":0.00015031279,"threshold_uncertainty_score":0.009755492},"labels":[],"label_agreement":null},{"id":"W1887050604","doi":"10.1029/2010gl043654","title":"Waveform inversion for S‐wave structure in the lowermost mantle beneath the Arctic: Implications for mineralogy and chemical composition","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Geology; Core–mantle boundary; Mantle (geology); Geophysics; Arctic; Transition zone; Shear velocity; Mineralogy; Meteorology; Oceanography; Physics","score_opus":0.028031918948686108,"score_gpt":0.2831888192608133,"score_spread":0.2551569003121272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1887050604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98816746,0.000044952067,0.009162651,0.00009852417,0.000008801385,0.000009137436,0.0005768518,0.00024768527,0.0016839344],"genre_scores_gemma":[0.98619425,0.0000658772,0.012171173,0.000014405563,0.000008254773,0.0000051109987,0.0010463912,0.000054183725,0.00044040915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000006392368,0.0000031202258,0.000010375639,0.000021968832,0.000021472617],"domain_scores_gemma":[0.99985397,0.000029189008,0.000019323139,0.000011064105,0.00006637292,0.000020093672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002359553,0.0003038467,0.00016086454,0.0007779125,0.0003878588,0.0005481223,0.00026581433,0.00021103815,0.0010155675],"category_scores_gemma":[0.00089985837,0.00013847904,0.00031607298,0.000729585,0.00011330512,0.00027347176,0.00023343255,0.00025562008,0.00026305116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065432885,0.00022982481,0.37586278,0.00009200784,0.00016781021,0.00031552158,0.00052593276,0.081456326,0.34188622,0.0015515297,0.0014409699,0.19581674],"study_design_scores_gemma":[0.00010396563,0.00007917823,0.3450294,0.000021491504,0.00009169013,0.00011915989,0.00048827118,0.58538264,0.06504022,0.0009218485,0.002666661,0.000055401022],"about_ca_topic_score_codex":0.07867034,"about_ca_topic_score_gemma":0.09290465,"teacher_disagreement_score":0.07867034,"about_ca_system_score_codex":0.00027464158,"about_ca_system_score_gemma":0.001064378,"threshold_uncertainty_score":0.15642482},"labels":[],"label_agreement":null},{"id":"W1889123826","doi":"10.1002/grl.50238","title":"Quantifying Northern Hemisphere freshwater ice","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Impact; University of Victoria","funders":"","keywords":"Cryosphere; Ice sheet; Northern Hemisphere; Climatology; Snow; Glacier; Antarctic sea ice; Sea ice; Arctic ice pack; Ice-sheet model; Greenland ice sheet; Physical geography; Geology; Environmental science; Oceanography; Geography; Geomorphology","score_opus":0.07107021997923446,"score_gpt":0.29431231650541606,"score_spread":0.2232420965261816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1889123826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9730505,0.0007541862,0.0017594167,0.00010137323,0.000010328803,0.00001101374,0.016289357,0.00008248458,0.007941397],"genre_scores_gemma":[0.98859626,0.00028867368,0.0012619081,0.000014334982,0.000009559726,0.000012792047,0.009241972,0.00001079221,0.0005638144],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998654,0.000021623273,0.000007105617,0.00004761543,0.00003458178,0.000023586323],"domain_scores_gemma":[0.99969184,0.000039512313,0.00011972047,0.00002399349,0.00008647321,0.000038397146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030276753,0.00018896314,0.00017333974,0.0011806424,0.00015664876,0.00047038056,0.00015406501,0.00009626842,0.0011157421],"category_scores_gemma":[0.00066839525,0.00007661035,0.00021576378,0.0013988981,0.0001315383,0.000331852,0.00030525608,0.00008593532,0.000144157],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007158883,0.000011550668,0.9358707,0.00008326163,0.000120717894,0.000096740136,0.0004248905,0.01947854,0.0016850369,0.000982872,0.004544455,0.03662976],"study_design_scores_gemma":[0.0000037995928,0.000010493403,0.9850552,0.000017408043,0.00002015707,0.00005358609,0.00017634041,0.0067775296,0.0007073817,0.0002883865,0.0068820966,0.0000076228007],"about_ca_topic_score_codex":0.051288366,"about_ca_topic_score_gemma":0.09738715,"teacher_disagreement_score":0.051288366,"about_ca_system_score_codex":0.0008492578,"about_ca_system_score_gemma":0.00049551565,"threshold_uncertainty_score":0.10197967},"labels":[],"label_agreement":null},{"id":"W1889819234","doi":"10.1029/2010gl043995","title":"Summertime trans‐Pacific transport of Asian dust","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Outflow; Lidar; Atmosphere (unit); Asian Dust; Storm; Geology; Mineral dust; Altitude (triangle); Anomaly (physics); Environmental science; Atmospheric sciences; Aeolian processes; Dust storm; Climatology; Oceanography; Meteorology; Aerosol; Geomorphology; Geography; Remote sensing","score_opus":0.016889186776487583,"score_gpt":0.2730968929384584,"score_spread":0.2562077061619708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1889819234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99640095,0.00026587516,0.00023121058,0.00007635816,0.000015544512,0.000004421853,0.00032157032,0.000023973647,0.0026600733],"genre_scores_gemma":[0.9981918,0.0002605256,0.00030643103,0.000023793502,0.0000075575836,0.0000045744387,0.0004156776,0.0000057458938,0.00078396976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.0000032809419,0.000003957254,0.000018703331,0.000012615987,0.000018135515],"domain_scores_gemma":[0.99987435,0.000007169379,0.00002863491,0.000008172148,0.000054834687,0.000026798383],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011762822,0.0003140946,0.00015585108,0.00035049536,0.0006132761,0.0006010257,0.00017390559,0.00014909318,0.0012527185],"category_scores_gemma":[0.00013701766,0.00013170774,0.00021794553,0.00050459005,0.00010791694,0.0003458043,0.000535671,0.0003080936,0.00020187964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027417298,0.00007127711,0.91190296,0.00015226315,0.0002111039,0.001545993,0.002985421,0.00093410455,0.04171821,0.00038309698,0.0014338591,0.038387634],"study_design_scores_gemma":[0.000012882195,0.000075203796,0.9838912,0.000028028859,0.00008691257,0.0005094028,0.002700103,0.0021887475,0.0054739933,0.00009724079,0.004922834,0.000013453576],"about_ca_topic_score_codex":0.05286845,"about_ca_topic_score_gemma":0.073864006,"teacher_disagreement_score":0.05286845,"about_ca_system_score_codex":0.0005042494,"about_ca_system_score_gemma":0.00046494088,"threshold_uncertainty_score":0.105121434},"labels":[],"label_agreement":null},{"id":"W1890793174","doi":"10.1029/2008gl035997","title":"Effects of sulfuric acid and ammonium sulfate coatings on the ice nucleation properties of kaolinite particles","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal; University of British Columbia","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ice nucleus; Efflorescence; Kaolinite; Nucleation; Relative humidity; Sulfuric acid; Materials science; Ammonium sulfate; Mineralogy; Clear ice; Ammonium; Chemical engineering; Geology; Chemistry; Arctic ice pack; Meteorology; Climatology; Metallurgy; Antarctic sea ice; Sea ice; Physics; Organic chemistry","score_opus":0.026964959770035,"score_gpt":0.24518136046609243,"score_spread":0.21821640069605744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1890793174","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99921787,0.00015314858,0.00014974306,0.0000063768716,0.000007741406,0.000007128767,0.000043575303,0.000007105499,0.0004072949],"genre_scores_gemma":[0.9988961,0.00014642603,0.00044286653,0.000011970033,0.0000048731513,0.00000614038,0.00007032877,0.000009161547,0.0004119556],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99983084,0.000015622272,0.000015580152,0.00002921128,0.00005379267,0.00005492462],"domain_scores_gemma":[0.99963236,0.00013587465,0.0000674506,0.000022895723,0.00008223244,0.000059213933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001906493,0.00033192005,0.00026487448,0.00018768375,0.0002501343,0.0004346715,0.00022110628,0.00022155153,0.0007135053],"category_scores_gemma":[0.00046985128,0.00028267584,0.000310148,0.00008348959,0.00029424034,0.00018024957,0.0001771384,0.00022687284,0.00010428014],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020367137,0.000013844093,0.0007127841,0.000030383158,0.000009969863,0.000028686585,0.00002531995,0.00016032594,0.99822944,0.000012454011,0.000011985738,0.00056115683],"study_design_scores_gemma":[0.000011153661,0.00024231579,0.010227696,0.0000026365888,0.000017967883,0.000033170534,0.000033322725,0.0007099875,0.98847884,0.0000075911566,0.00022895703,0.000006345807],"about_ca_topic_score_codex":0.003572464,"about_ca_topic_score_gemma":0.0046837274,"teacher_disagreement_score":0.003572464,"about_ca_system_score_codex":0.00032219006,"about_ca_system_score_gemma":0.00019751092,"threshold_uncertainty_score":0.007103324},"labels":[],"label_agreement":null},{"id":"W1891215053","doi":"10.1029/2012gl053608","title":"Topographic characterization of lunar complex craters","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; University of British Columbia","funders":"","keywords":"Impact crater; Geology; Orbiter; Altimeter; Terrain; Lunar craters; Astrobiology; Far side of the Moon; Geomorphology; Remote sensing; Geophysics; Geography","score_opus":0.061488277265933484,"score_gpt":0.310564607447245,"score_spread":0.24907633018131153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1891215053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979006,0.00012482084,0.0004956881,0.0000063470916,9.234237e-7,0.0000086973,0.0007536399,0.000023857967,0.00068545004],"genre_scores_gemma":[0.99837995,0.000044138364,0.000809296,0.000002908188,0.0000019559764,0.000003044632,0.0006334624,0.000005276968,0.000120093835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999907,0.000006203469,0.000010041109,0.000029367027,0.000029559895,0.000017822707],"domain_scores_gemma":[0.9994037,0.00011021026,0.00016915907,0.000065135275,0.00018014757,0.00007160065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114967355,0.0001547982,0.00017768751,0.0021247326,0.00024608686,0.0006223782,0.0001828266,0.00009628054,0.0010474978],"category_scores_gemma":[0.00065483485,0.00012412199,0.00017054706,0.0018554466,0.00020184228,0.00023657412,0.00037108993,0.0001333938,0.0001502887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005551121,0.000014431374,0.965739,0.000046241657,0.000042554002,0.00012300722,0.00024709053,0.0028347513,0.00794494,0.000072809344,0.00023517021,0.022644518],"study_design_scores_gemma":[0.0000016408586,0.000008473689,0.9977411,0.0000028559418,0.00000474437,0.00007066182,0.00007055058,0.001435237,0.00038665647,0.0000128738375,0.00026243864,0.0000028431475],"about_ca_topic_score_codex":0.020845264,"about_ca_topic_score_gemma":0.045866955,"teacher_disagreement_score":0.020845264,"about_ca_system_score_codex":0.00025393453,"about_ca_system_score_gemma":0.00015047268,"threshold_uncertainty_score":0.041447878},"labels":[],"label_agreement":null},{"id":"W1891800431","doi":"10.1002/2015gl063455","title":"Hydraulic fracturing and the Crooked Lake Sequences: Insights gleaned from regional seismic networks","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Western University","funders":"","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Seismometer; Sequence (biology); Paleontology","score_opus":0.05631406258949844,"score_gpt":0.27134961307717137,"score_spread":0.21503555048767292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1891800431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980292,0.00006778967,0.00028552004,0.000028430804,0.0000013920484,0.0000071186437,0.00051817147,0.000010449797,0.0010519343],"genre_scores_gemma":[0.998727,0.00004053925,0.00030928125,0.000004825363,0.0000017224028,0.00000228827,0.00067555846,0.000003065579,0.00023568088],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999107,0.000008707673,0.000006094713,0.000019396133,0.000024146706,0.000030906056],"domain_scores_gemma":[0.99955386,0.000056149445,0.0001090054,0.000026300584,0.00019360968,0.000061020022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013525627,0.0001378819,0.00013789203,0.0018800203,0.0003836579,0.00046859868,0.00026577403,0.00018355042,0.0008619432],"category_scores_gemma":[0.0012217491,0.000067670284,0.00010254236,0.0020445727,0.00034477576,0.00017590332,0.0004381523,0.00013111504,0.00011387074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016587818,0.00003987072,0.9435165,0.000068299254,0.00007301241,0.00054471404,0.0015408621,0.0075949496,0.013553939,0.0006208683,0.0008352903,0.031445943],"study_design_scores_gemma":[0.0000030484973,0.000012573008,0.99326247,0.0000108886825,0.0000118588905,0.00006151997,0.0010195639,0.0043577747,0.00038417344,0.00006505387,0.0008045091,0.0000066690295],"about_ca_topic_score_codex":0.60510963,"about_ca_topic_score_gemma":0.8081914,"teacher_disagreement_score":0.60510963,"about_ca_system_score_codex":0.0010976682,"about_ca_system_score_gemma":0.001334284,"threshold_uncertainty_score":0.7944319},"labels":[],"label_agreement":null},{"id":"W1892627350","doi":"10.1029/2011gl047282","title":"GRACE era secular trends in Earth rotation parameters: A global scale impact of the global warming process?","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Secular variation; Global warming; Climatology; Scale (ratio); Earth's rotation; Environmental science; Earth (classical element); Climate change; Geology; Earth science; Geodesy; Geophysics; Geography; Physics; Oceanography","score_opus":0.05830580100536031,"score_gpt":0.32300806007873206,"score_spread":0.26470225907337175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1892627350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7171151,0.04428649,0.02262874,0.046765193,0.0037805631,0.000091961614,0.06893068,0.001874134,0.09452718],"genre_scores_gemma":[0.95975304,0.013956913,0.005224131,0.0015439144,0.0013831228,0.000019748413,0.011700399,0.00029703657,0.0061216606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977154,0.000046565347,0.000011543102,0.000050009905,0.00008425609,0.000036121575],"domain_scores_gemma":[0.99914885,0.00008689276,0.00043383078,0.00010066039,0.00016181525,0.00006787983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076875946,0.00066092785,0.00027019694,0.0010687327,0.00017163683,0.0008764543,0.0002950156,0.00041644147,0.006062517],"category_scores_gemma":[0.0021267748,0.00011863696,0.00017640437,0.0035049303,0.00047677237,0.0016852379,0.00062561466,0.0006357242,0.0014724587],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052336213,0.00006048185,0.5785178,0.0004187648,0.00030861233,0.00046669386,0.00032313133,0.009550961,0.0058513954,0.023114588,0.09321718,0.28764713],"study_design_scores_gemma":[0.000013781011,0.000119645505,0.89505476,0.00010125983,0.00010828426,0.00031024328,0.00038016916,0.0069762855,0.0022577075,0.008346391,0.08628148,0.000049922204],"about_ca_topic_score_codex":0.007860425,"about_ca_topic_score_gemma":0.020826736,"teacher_disagreement_score":0.007860425,"about_ca_system_score_codex":0.00043209485,"about_ca_system_score_gemma":0.00045252068,"threshold_uncertainty_score":0.020281136},"labels":[],"label_agreement":null},{"id":"W1893342066","doi":"10.1029/2001gl014069","title":"Prospects for decadal prediction of the North Atlantic Oscillation (NAO)","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences; Innovative Research Group Project of the National Natural Science Foundation of China","keywords":"North Atlantic oscillation; Thermohaline circulation; Climatology; Atlantic multidecadal oscillation; Index (typography); Range (aeronautics); Environmental science; Atlantic hurricane; Gulf Stream; Geology; Tropical cyclone","score_opus":0.05220836023778696,"score_gpt":0.28077345766580986,"score_spread":0.2285650974280229,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1893342066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.54558176,0.008424578,0.38476852,0.031634968,0.0014467717,0.000044383953,0.002448993,0.0022453493,0.023404676],"genre_scores_gemma":[0.9741029,0.0011694023,0.021425761,0.0006038195,0.00021037189,0.000039723604,0.0008579935,0.000060536207,0.0015294746],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997625,0.00010340452,0.000011338545,0.00006820856,0.000031672018,0.000022934719],"domain_scores_gemma":[0.9972295,0.0014562244,0.00032041184,0.00039765198,0.0003544889,0.00024171613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003182526,0.00053205126,0.00047192976,0.00027876647,0.00044423068,0.0012493208,0.0006241537,0.0010110587,0.0021100473],"category_scores_gemma":[0.0072493716,0.00033341735,0.00038307827,0.00041800115,0.0005486003,0.0019435633,0.00091218116,0.0015817191,0.0003579792],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010548885,0.00016658827,0.055586386,0.00011807347,0.00019617706,0.0002037805,0.00015365664,0.7560935,0.0047759963,0.10037404,0.0074806893,0.07379629],"study_design_scores_gemma":[0.00006230151,0.00008548642,0.011572127,0.00004698685,0.00003592345,0.000045639303,0.00012575724,0.8173822,0.0010721587,0.16158554,0.00793177,0.000054152704],"about_ca_topic_score_codex":0.003438047,"about_ca_topic_score_gemma":0.0029540593,"teacher_disagreement_score":0.003438047,"about_ca_system_score_codex":0.00052436936,"about_ca_system_score_gemma":0.0007155965,"threshold_uncertainty_score":0.01683104},"labels":[],"label_agreement":null},{"id":"W1893479363","doi":"10.1029/2010gl043963","title":"Aged black carbon identified in marine dissolved organic carbon","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":206,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Dissolved organic carbon; Total organic carbon; Radiocarbon dating; Deposition (geology); Environmental science; Carbon fibers; Carbon black; Sedimentary rock; Environmental chemistry; Organic matter; Geology; Oceanography; Chemistry; Sediment; Geochemistry; Paleontology","score_opus":0.018318949634779612,"score_gpt":0.25984441316801915,"score_spread":0.24152546353323953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1893479363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99234116,0.0011494533,0.0011898029,0.000020787627,0.000032314812,0.000012842305,0.0014794194,0.000026145311,0.0037480837],"genre_scores_gemma":[0.99280614,0.00056075916,0.0032231107,0.00007662026,0.00002138841,0.00001463868,0.0010437736,0.00001160229,0.0022419095],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999037,0.000006325765,0.000005131385,0.000029863719,0.000029591272,0.00002538652],"domain_scores_gemma":[0.9997435,0.000025639196,0.00007821299,0.000016426071,0.00008322491,0.000053071966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011655089,0.00024132573,0.00009771941,0.0014805264,0.00032692443,0.00041851873,0.00017586643,0.0003237777,0.0014728592],"category_scores_gemma":[0.00031288687,0.00010832625,0.00008345162,0.0008834002,0.00024083085,0.00028918072,0.00028259365,0.00015730661,0.0003059667],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039734843,0.00003888938,0.2286331,0.000112841364,0.00006283785,0.0006417663,0.00018834042,0.00015431046,0.74594986,0.0007719608,0.0003224401,0.022726346],"study_design_scores_gemma":[0.000011302512,0.00015584345,0.78990436,0.000032946704,0.0000452597,0.0012336794,0.00024108241,0.00076229917,0.19521724,0.00051083625,0.011864886,0.000020366477],"about_ca_topic_score_codex":0.002884203,"about_ca_topic_score_gemma":0.0040987497,"teacher_disagreement_score":0.002884203,"about_ca_system_score_codex":0.0002981349,"about_ca_system_score_gemma":0.00017200841,"threshold_uncertainty_score":0.005734861},"labels":[],"label_agreement":null},{"id":"W1893936119","doi":"10.1002/grl.50459","title":"Aerosol effect on climate extremes in Europe under different future scenarios","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Deutsche Forschungsgemeinschaft","keywords":"Aerosol; Environmental science; Greenhouse gas; Precipitation; Climatology; Atmospheric sciences; Climate change; Climate model; Global warming; Daytime; Current (fluid); Meteorology; Geography; Geology","score_opus":0.021514109413173697,"score_gpt":0.26221002928904047,"score_spread":0.24069591987586678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1893936119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99668026,0.000135015,0.00060606893,0.00017246939,0.000025324502,0.000008409251,0.0008431476,0.000050304116,0.0014791028],"genre_scores_gemma":[0.99892163,0.0000680055,0.0002249529,0.00002672945,0.0000076112556,0.000008573494,0.0006240967,0.0000073195542,0.00011113611],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996063,0.00017246856,0.000021665177,0.000074986296,0.000035836772,0.00008868384],"domain_scores_gemma":[0.9995142,0.00022124512,0.00007809564,0.000043118227,0.00007802156,0.00006534164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010760429,0.00059350475,0.0005242744,0.00042165833,0.0003665043,0.0011238031,0.000453941,0.0015368009,0.0010563823],"category_scores_gemma":[0.0012950198,0.00029202053,0.0012855442,0.00052693795,0.00038781852,0.000754088,0.00047168465,0.0004825557,0.00012542993],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007143356,0.00014141088,0.07701613,0.0000817407,0.00054807763,0.00045394895,0.000059889753,0.9101442,0.005316849,0.0015536308,0.0009129872,0.0030568135],"study_design_scores_gemma":[0.0005236044,0.0010242289,0.23371698,0.000068873574,0.000495641,0.00025118727,0.0004777312,0.74941385,0.007858202,0.0023388201,0.0036633005,0.00016761059],"about_ca_topic_score_codex":0.010955728,"about_ca_topic_score_gemma":0.0059540714,"teacher_disagreement_score":0.010955728,"about_ca_system_score_codex":0.00086505903,"about_ca_system_score_gemma":0.00034537088,"threshold_uncertainty_score":0.021783888},"labels":[],"label_agreement":null},{"id":"W1894581224","doi":"10.1002/2014gl062695","title":"Anisotropic core ion temperatures associated with strong zonal flows and upflows","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Anisotropy; Ion; Electric field; Physics; Atomic physics; Core (optical fiber); Field (mathematics); Acceleration; Computational physics; Geophysics; Classical mechanics; Optics","score_opus":0.029482179144724778,"score_gpt":0.2870020354666666,"score_spread":0.2575198563219418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1894581224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99898976,0.000022344466,0.00018859953,0.000012391108,0.0000023444854,0.0000014265295,0.000038848586,0.000015050273,0.00072924024],"genre_scores_gemma":[0.99977475,0.000011469366,0.000087189575,0.0000030990907,0.000003780735,6.9822875e-7,0.000035857272,0.0000025538584,0.00008057445],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999602,0.0000032809066,0.0000022116637,0.000007760771,0.0000097710845,0.00001668992],"domain_scores_gemma":[0.99976045,0.000035692552,0.00011041859,0.000019488996,0.00002443137,0.000049603048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006224067,0.00013590617,0.00010658842,0.0004268859,0.0001624352,0.00032308546,0.000070807946,0.000093612885,0.0008669664],"category_scores_gemma":[0.0003003485,0.00013137347,0.00008658374,0.00017884355,0.00027432258,0.00015884524,0.00032815913,0.00016554588,0.00007543306],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068220915,0.00004346873,0.516944,0.000046874713,0.000042727806,0.0010679885,0.00062288204,0.0015815059,0.46778038,0.0011599474,0.00057221646,0.009455819],"study_design_scores_gemma":[0.000013152557,0.000027294034,0.9844928,0.0000037586624,0.000011267963,0.0003585253,0.0001143339,0.0020250906,0.012146883,0.00028606234,0.00051325804,0.000007600908],"about_ca_topic_score_codex":0.0014166664,"about_ca_topic_score_gemma":0.0018688979,"teacher_disagreement_score":0.0014166664,"about_ca_system_score_codex":0.00015710275,"about_ca_system_score_gemma":0.00007064594,"threshold_uncertainty_score":0.002900362},"labels":[],"label_agreement":null},{"id":"W1894872574","doi":"10.1002/2013gl057467","title":"Reversing climate warming by artificial atmospheric carbon‐dioxide removal: Can a Holocene‐like climate be restored?","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Holocene; Environmental science; Carbon dioxide; Reversing; Carbon dioxide in Earth's atmosphere; Climatology; Climate change; Atmospheric carbon cycle; Atmospheric sciences; Precipitation; Geology; Carbon sequestration; Oceanography; Meteorology; Ecology; Geography; Materials science","score_opus":0.017450260168808192,"score_gpt":0.25514189157003836,"score_spread":0.23769163140123017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1894872574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736375,0.00009408545,0.0010335746,0.00024876028,0.000049162205,0.000012454478,0.00009376943,0.000056250796,0.0010482932],"genre_scores_gemma":[0.99935395,0.00005256565,0.00034787806,0.000036921545,0.0000035250225,0.000005876738,0.00004312509,0.000008682134,0.00014747688],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999244,0.000017258013,0.000005526065,0.000011942745,0.000010577991,0.00003023202],"domain_scores_gemma":[0.99979395,0.00007356629,0.000038148257,0.000046373658,0.000011945115,0.000036118872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033525552,0.00030384178,0.0002987757,0.0001112572,0.00033380822,0.00045602175,0.0005354553,0.00049139175,0.0012964174],"category_scores_gemma":[0.0010570483,0.00015102321,0.0006012033,0.00011014827,0.0006451879,0.0005746911,0.00038461204,0.0006263416,0.000090248286],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003488694,0.0009105572,0.04425108,0.00060884823,0.0007614676,0.0012364254,0.0004943582,0.5636627,0.34815493,0.011944049,0.0022445787,0.022242391],"study_design_scores_gemma":[0.0014953179,0.0027594217,0.08494721,0.00004205808,0.000579203,0.000433204,0.0010522937,0.70917314,0.17207173,0.014769678,0.012470255,0.00020648103],"about_ca_topic_score_codex":0.005035292,"about_ca_topic_score_gemma":0.00529105,"teacher_disagreement_score":0.005035292,"about_ca_system_score_codex":0.0004920102,"about_ca_system_score_gemma":0.00044663754,"threshold_uncertainty_score":0.010011971},"labels":[],"label_agreement":null},{"id":"W1895339151","doi":"10.1002/grl.50960","title":"A new type of Doppler velocity fluctuations in HF ground scatter from the polar cap","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Doppler effect; Ionosphere; Physics; Polar; Noon; Geophysics; Line-of-sight; Computational physics; Geology; Astrophysics; Atmospheric sciences; Astronomy","score_opus":0.02311341652798264,"score_gpt":0.2908709637398187,"score_spread":0.26775754721183603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1895339151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927181,0.00034901936,0.0033669125,0.000055464563,0.00004298307,0.000013711943,0.00039307974,0.00011384053,0.0029469193],"genre_scores_gemma":[0.9986696,0.000060118295,0.00056940445,0.000020112197,0.000040423958,0.000005706471,0.00022119671,0.000011191219,0.0004021302],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.0000046843593,0.0000021355984,0.000015951302,0.00001813203,0.000021048534],"domain_scores_gemma":[0.9996791,0.00007290506,0.00010078808,0.000043511765,0.000057475147,0.00004629017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009217496,0.0002006989,0.00012785802,0.0007777183,0.0002131333,0.00039123627,0.00016206528,0.00022977887,0.0011811312],"category_scores_gemma":[0.00039017087,0.00009973021,0.000107271284,0.000592294,0.00021951445,0.00017129838,0.0002057681,0.00024211232,0.00019622456],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007194458,0.00011943743,0.2681575,0.00010966583,0.00010023771,0.002340322,0.00085941417,0.0021648353,0.6762673,0.0009989097,0.0018546551,0.04630823],"study_design_scores_gemma":[0.000017532282,0.00024891098,0.9522331,0.000015539174,0.00003719926,0.0013106252,0.00018451594,0.004395954,0.037922915,0.0003601546,0.0032394913,0.000034050383],"about_ca_topic_score_codex":0.0012305053,"about_ca_topic_score_gemma":0.0013724602,"teacher_disagreement_score":0.0012305053,"about_ca_system_score_codex":0.00012293372,"about_ca_system_score_gemma":0.00008464767,"threshold_uncertainty_score":0.0039512515},"labels":[],"label_agreement":null},{"id":"W1897345630","doi":"10.1002/grl.50271","title":"Transition of Pi2 ULF wave polarization structure from the ionosphere to the ground","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Magnetometer; Ionosphere; Substorm; Geophysics; Polarization (electrochemistry); Earth's magnetic field; Physics; Radar; Geology; Remote sensing; Magnetosphere; Magnetic field; Computer science; Telecommunications; Chemistry","score_opus":0.012574010714367784,"score_gpt":0.24778587092408835,"score_spread":0.23521186020972057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1897345630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986665,0.00009536534,0.009179273,0.00006441638,0.000010647,0.000006752707,0.00022222666,0.00012980848,0.0036264209],"genre_scores_gemma":[0.9983853,0.00003929214,0.0011293421,0.000010906561,0.0000064580786,0.0000031482568,0.00014464156,0.0000115125285,0.0002694812],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995613,0.00000529653,0.0000010600781,0.000013593635,0.0000091295915,0.000014692576],"domain_scores_gemma":[0.9998964,0.00002192276,0.000026222575,0.000017044391,0.00002310154,0.000015270743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000089084584,0.00015844408,0.00008134957,0.00045571756,0.00013363965,0.00037617894,0.00015427539,0.00020252471,0.001353383],"category_scores_gemma":[0.00029630805,0.0000916705,0.00008171468,0.00046212145,0.00024859057,0.00035154852,0.0002424854,0.00029829438,0.00017991698],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008062739,0.00008886457,0.19150238,0.0000951837,0.00005373865,0.00049285596,0.0008253548,0.0041903304,0.680237,0.0026824174,0.0013676637,0.117657945],"study_design_scores_gemma":[0.000026525699,0.0001767841,0.8801686,0.00001300665,0.000026825091,0.0007320422,0.00038229785,0.02731834,0.086754866,0.001464511,0.0029030966,0.000033036045],"about_ca_topic_score_codex":0.00070325227,"about_ca_topic_score_gemma":0.0006004382,"teacher_disagreement_score":0.001353383,"about_ca_system_score_codex":0.00011003677,"about_ca_system_score_gemma":0.00008087751,"threshold_uncertainty_score":0.004527509},"labels":[],"label_agreement":null},{"id":"W1897521382","doi":"10.1002/2015gl066003","title":"The 2014–2015 eruption of Fogo volcano: Geodetic modeling of Sentinel‐1 TOPS interferometry","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency; Natural Environment Research Council; Sociedad Española de Oncología Médica; Sight Research UK","keywords":"TOPS; Geology; Volcano; Seismology; Lava; Synthetic aperture radar; Geodesy; Interferometric synthetic aperture radar; Geodetic datum; Volcanology; Interferometry; Lateral eruption; Magma; Remote sensing; Azimuth; Explosive eruption","score_opus":0.040704056105490584,"score_gpt":0.31853946408189526,"score_spread":0.27783540797640466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1897521382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948378,0.000088345165,0.002924873,0.00020745667,0.000020035122,0.000018712188,0.0005104948,0.0000846797,0.0013076039],"genre_scores_gemma":[0.9982152,0.000032780015,0.0011934519,0.000017713384,0.0000081942235,0.00000717428,0.00031811366,0.000011315374,0.00019594059],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999881,0.000027561964,0.0000059758668,0.000033591517,0.000017599463,0.000034206292],"domain_scores_gemma":[0.99981827,0.00006727226,0.000033681823,0.000016991467,0.00003568485,0.000028172239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005494166,0.0004824203,0.0003431732,0.0004360209,0.00044518363,0.0007377969,0.000696097,0.00084854953,0.0006657626],"category_scores_gemma":[0.00072982564,0.00036729217,0.00067755894,0.00031850688,0.0005282593,0.00043866047,0.00037610094,0.00041785437,0.00009998808],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007959111,0.00012594555,0.04513906,0.000019220939,0.000092605704,0.00011519417,0.000039334718,0.94715863,0.0019175305,0.0008551479,0.0007493983,0.0037084187],"study_design_scores_gemma":[0.000009943411,0.000011115773,0.008221714,0.000002739617,0.000009250961,0.000010737241,0.000014905477,0.99133754,0.00014201726,0.000101956764,0.00013153593,0.0000065315485],"about_ca_topic_score_codex":0.100405544,"about_ca_topic_score_gemma":0.057810847,"teacher_disagreement_score":0.100405544,"about_ca_system_score_codex":0.0010525866,"about_ca_system_score_gemma":0.0010233033,"threshold_uncertainty_score":0.19964224},"labels":[],"label_agreement":null},{"id":"W1898833506","doi":"10.1029/2010gl043934","title":"The role of poleward energy transport in Arctic temperature evolution","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Troposphere; Arctic; Climatology; Environmental science; Energy transport; Atmospheric sciences; The arctic; Global warming; Zonal and meridional; Climate change; Geology; Oceanography; Physics","score_opus":0.010158123849665848,"score_gpt":0.25640150092722575,"score_spread":0.2462433770775599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1898833506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99773324,0.00046141527,0.00072987773,0.00005987543,0.000009216198,0.0000012871557,0.00009526493,0.00001268006,0.0008971534],"genre_scores_gemma":[0.99932337,0.0002637095,0.00018221805,0.000010670064,0.000007785234,0.0000011153273,0.00007382474,0.0000055882697,0.00013190662],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999472,0.000012922868,0.0000046981913,0.000014805547,0.000008095875,0.000012280107],"domain_scores_gemma":[0.9998115,0.00004147172,0.000076814285,0.000017137801,0.000039856845,0.000013396233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019026994,0.00017044319,0.00015859916,0.00042302455,0.0002497175,0.00061646727,0.00011052473,0.00021812432,0.0006978355],"category_scores_gemma":[0.0007644551,0.00014257155,0.00019290943,0.00036583756,0.00020969847,0.0004972893,0.00024250505,0.00021952303,0.00012623481],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048599436,0.000048664948,0.8443965,0.00009141672,0.00017009581,0.00042432558,0.00068938,0.03603236,0.07757796,0.0034152784,0.0003883697,0.036279596],"study_design_scores_gemma":[0.000006119851,0.000047384292,0.9751339,0.000017634395,0.000044672557,0.0001364049,0.00016488251,0.017729629,0.003889226,0.0012627293,0.0015483291,0.000019095312],"about_ca_topic_score_codex":0.008493728,"about_ca_topic_score_gemma":0.007205908,"teacher_disagreement_score":0.008493728,"about_ca_system_score_codex":0.0003368086,"about_ca_system_score_gemma":0.00020773667,"threshold_uncertainty_score":0.016888559},"labels":[],"label_agreement":null},{"id":"W1901177346","doi":"10.1002/grl.50821","title":"Long‐periodic strong radar echoes in the summer polar <i>D</i> region correlated with oscillations of high‐speed solar wind streams","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Polar; Magnetosphere; Solar wind; Atmospheric sciences; Physics; Ionosphere; Earth's magnetic field; Polar cap; Local time; Astrophysics; Geology; Geophysics; Plasma; Astronomy; Magnetic field","score_opus":0.014825384361037855,"score_gpt":0.2543151553454555,"score_spread":0.23948977098441765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1901177346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942636,0.0000457988,0.000100315025,0.000014908663,0.0000049113364,0.0000016794286,0.00008937516,0.0000071703917,0.00030950518],"genre_scores_gemma":[0.9994312,0.00003481914,0.00013898252,0.000011795558,0.000013099958,0.0000022117313,0.0002692356,0.0000016109021,0.00009715294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999578,0.0000048622787,0.000003166819,0.000010505798,0.000010254741,0.000013324518],"domain_scores_gemma":[0.9996468,0.000042953485,0.00018230343,0.00002050546,0.000040116203,0.00006729351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012960116,0.00012404047,0.00010290861,0.000266244,0.00015960178,0.00018241009,0.000077358636,0.00017607198,0.00047897044],"category_scores_gemma":[0.00028809262,0.0000722591,0.00007364477,0.00023621395,0.00016714883,0.00013879314,0.00019820065,0.00016250242,0.00010375048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039521532,0.00006816148,0.9191632,0.000047300473,0.00005971601,0.0004783538,0.00038679613,0.0004190044,0.06595288,0.00006824077,0.00077050395,0.012190638],"study_design_scores_gemma":[0.0000029876896,0.000055679135,0.9984792,0.0000018184927,0.000005064112,0.00013323042,0.000062306484,0.000137585,0.0007771854,0.000010535791,0.00033247418,0.000002056015],"about_ca_topic_score_codex":0.0009852861,"about_ca_topic_score_gemma":0.0029320228,"teacher_disagreement_score":0.0009852861,"about_ca_system_score_codex":0.00009290535,"about_ca_system_score_gemma":0.00006642831,"threshold_uncertainty_score":0.0019590855},"labels":[],"label_agreement":null},{"id":"W1901858764","doi":"10.1002/2015gl063783","title":"Growth in stratospheric chlorine from short‐lived chemicals not controlled by the Montreal Protocol","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Chlorine; Montreal Protocol; Phosgene; Hydrogen chloride; Dichloromethane; Ozone layer; Chloroform; Chemistry; Chloride; Stratosphere; Environmental chemistry; Troposphere; Environmental science; Atmospheric sciences; Ozone; Organic chemistry; Physics; Solvent","score_opus":0.047437943811482274,"score_gpt":0.3048990356002434,"score_spread":0.25746109178876114,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1901858764","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7990385,0.0025767067,0.108042456,0.0026166362,0.00028948032,0.0011774733,0.021631666,0.0019884612,0.0626385],"genre_scores_gemma":[0.96840626,0.00058781425,0.01647271,0.00029562262,0.000012327857,0.00033428028,0.0026978657,0.000065715125,0.011127454],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99928087,0.00011191348,0.000027575647,0.0001535881,0.00028904006,0.00013713233],"domain_scores_gemma":[0.9992913,0.00008880143,0.00016170423,0.000107731394,0.00028704162,0.00006334827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013862349,0.0005596048,0.00017939346,0.0005174512,0.0006396964,0.00086583867,0.0013939092,0.0005875472,0.0036834893],"category_scores_gemma":[0.0011220083,0.00021766932,0.0006755476,0.00046986094,0.00047205572,0.0007455034,0.0005440465,0.00052997604,0.00055437285],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008928829,0.00033199403,0.16414833,0.00077074335,0.0004427062,0.0004530517,0.0003290883,0.18931536,0.48583603,0.056098327,0.028741173,0.07264036],"study_design_scores_gemma":[0.00022270145,0.0014716979,0.16592395,0.00015048656,0.0003100499,0.00020948795,0.00032696303,0.22344702,0.40721554,0.010331316,0.18997166,0.00041918192],"about_ca_topic_score_codex":0.39458993,"about_ca_topic_score_gemma":0.45583764,"teacher_disagreement_score":0.39458993,"about_ca_system_score_codex":0.008734776,"about_ca_system_score_gemma":0.0085355975,"threshold_uncertainty_score":0.7845863},"labels":[],"label_agreement":null},{"id":"W1903237231","doi":"10.1029/2012gl053716","title":"Experimental craters formed by single and multiple buried explosions and implications for volcanic craters with emphasis on maars","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Impact crater; Ejecta; Geology; Volcano; Maar; Explosive material; Explosive eruption; Seismology; Geophysics; Astrobiology; Pyroclastic rock","score_opus":0.06689322472392299,"score_gpt":0.30724980048755207,"score_spread":0.24035657576362907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1903237231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938774,0.00005963087,0.00027622253,0.0000068505456,0.000003311463,0.00001667442,0.00004599417,0.0000049845007,0.00019845912],"genre_scores_gemma":[0.9977633,0.0000898646,0.0013799313,0.000014590617,0.000006705027,0.000049008988,0.00012737776,0.000007687262,0.0005615445],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99957293,0.000062343875,0.00005942685,0.000091626105,0.000081789185,0.00013185568],"domain_scores_gemma":[0.99892694,0.00051107304,0.00014185498,0.00020341115,0.00007329607,0.00014339782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036575313,0.00044259257,0.00030719256,0.00040814915,0.0003894384,0.0003203444,0.00036267182,0.00050935237,0.002586857],"category_scores_gemma":[0.00080119324,0.00028814838,0.0004282911,0.00021389489,0.0007488514,0.0003073736,0.00079813803,0.0008115612,0.000118534175],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027228235,0.0014365215,0.011187807,0.00009138869,0.00005191844,0.00035408625,0.0002320129,0.0025833615,0.9763188,0.00022130676,0.00004878156,0.0047512595],"study_design_scores_gemma":[0.0005412683,0.03544158,0.10094013,0.000039532548,0.0001982302,0.0017738958,0.0008591631,0.008124884,0.85056037,0.00039493377,0.0010753104,0.000050788974],"about_ca_topic_score_codex":0.0009034395,"about_ca_topic_score_gemma":0.0014507731,"teacher_disagreement_score":0.002586857,"about_ca_system_score_codex":0.00020415604,"about_ca_system_score_gemma":0.00012427926,"threshold_uncertainty_score":0.008653939},"labels":[],"label_agreement":null},{"id":"W1903891751","doi":"10.1002/2014gl060213","title":"Laboratory chamber measurements of the longwave extinction spectra and complex refractive indices of African and Asian mineral dusts","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Toronto; Centre National d’Etudes Spatiales","keywords":"Longwave; Mineral dust; Extinction (optical mineralogy); Particle-size distribution; Environmental science; Atmospheric sciences; Radiative transfer; Asian Dust; Particle (ecology); Particle size; Range (aeronautics); Aerosol; Mineralogy; Materials science; Chemistry; Geology; Physics; Optics; Meteorology","score_opus":0.031821677335439814,"score_gpt":0.2798729614333008,"score_spread":0.248051284097861,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1903891751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971103,0.00005295405,0.0022354024,0.000004022537,0.0000048557113,0.000009031307,0.00008855863,0.000013774357,0.00048122095],"genre_scores_gemma":[0.9981336,0.000053957676,0.0013229665,0.000010439633,0.00000611306,0.000017447652,0.00016455654,0.000005751365,0.00028522007],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998579,0.000029734498,0.0000070004003,0.00004442477,0.000042299955,0.000018615096],"domain_scores_gemma":[0.99977607,0.000070409995,0.00005943796,0.000029172765,0.00004541899,0.000019470684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022318792,0.00027063212,0.00012288919,0.00014243783,0.0002633282,0.000368084,0.00018712677,0.00013695823,0.0006707125],"category_scores_gemma":[0.00028742212,0.000091810114,0.00013985408,0.000114453476,0.00021864218,0.00020625329,0.00015547052,0.00017556938,0.0001545855],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018835126,0.0001910681,0.068334185,0.00003664119,0.000061012215,0.000064157706,0.00023029721,0.00058243005,0.9257427,0.000104515515,0.00006901554,0.0043955976],"study_design_scores_gemma":[0.000041375384,0.00083579496,0.28428403,0.000009502617,0.00009733277,0.0003044376,0.00030946973,0.003747435,0.7089599,0.00009619946,0.0012944343,0.000020032878],"about_ca_topic_score_codex":0.0015955264,"about_ca_topic_score_gemma":0.0017177787,"teacher_disagreement_score":0.0015955264,"about_ca_system_score_codex":0.00017522319,"about_ca_system_score_gemma":0.00011158401,"threshold_uncertainty_score":0.0031723976},"labels":[],"label_agreement":null},{"id":"W1904185185","doi":"10.1029/2011gl048204","title":"Temperature signature of high latitude Atlantic boundary currents revealed by marine mammal‐borne sensor and Argo data","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Office of Polar Programs; Fisheries and Oceans Canada; Natural Environment Research Council; Sight Research UK; Society for Marine Mammalogy","keywords":"Argo; Marine mammal; Oceanography; Sea surface temperature; Latitude; Geology; Boundary current; Climatology; Ocean current; Fishery; Geodesy; Biology","score_opus":0.030557537941940008,"score_gpt":0.2643136560479343,"score_spread":0.23375611810599428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1904185185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925403,0.00004906289,0.00047401135,0.00003632637,0.000014471807,0.000009824198,0.0055725966,0.000041702122,0.0012618143],"genre_scores_gemma":[0.9792392,0.000053045587,0.001967703,0.000023214954,0.00001855711,0.000017169821,0.01816861,0.000018587556,0.00049374235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999757,0.000035148023,0.000018023162,0.00007323277,0.00007035879,0.000046327386],"domain_scores_gemma":[0.9995245,0.00006950779,0.00011529034,0.00006654439,0.00013173679,0.00009231772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000385919,0.00020381798,0.00028138436,0.00062864256,0.00019817211,0.0004142699,0.000193697,0.00022302539,0.00056272437],"category_scores_gemma":[0.00060873496,0.00011449571,0.00025569226,0.0006349177,0.00014169764,0.0003118698,0.000403521,0.0001997798,0.00028708117],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043088358,0.00013924162,0.9430299,0.0000511793,0.000108477994,0.0001753325,0.00020267788,0.004222452,0.03272876,0.00019515521,0.0019218834,0.016794026],"study_design_scores_gemma":[0.000011231928,0.00003808132,0.99362636,0.0000046619575,0.000015614909,0.000050976174,0.000071139366,0.0035278243,0.001605055,0.000026603737,0.0010140198,0.000008330065],"about_ca_topic_score_codex":0.013944272,"about_ca_topic_score_gemma":0.03334112,"teacher_disagreement_score":0.013944272,"about_ca_system_score_codex":0.0002617088,"about_ca_system_score_gemma":0.00027489936,"threshold_uncertainty_score":0.027726233},"labels":[],"label_agreement":null},{"id":"W1907162398","doi":"10.1002/2015gl064377","title":"Isolated cases of remote dynamic triggering in Canada detected using cataloged earthquakes combined with a matched‐filter approach","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Waveform; Shock (circulatory); Filter (signal processing); Statistical analysis; Statistics","score_opus":0.05271104119515374,"score_gpt":0.2657852839870638,"score_spread":0.21307424279191006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1907162398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995148,0.00010871781,0.00071419234,0.00003170925,0.0000034056175,0.000025395017,0.0018037474,0.000052265455,0.0021126065],"genre_scores_gemma":[0.99754506,0.00006327099,0.0005397587,0.000012678816,0.0000021197118,0.0000049427067,0.0012286686,0.000004609061,0.0005988055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997017,0.000011681024,0.000015447094,0.00005338151,0.00011501118,0.00010271732],"domain_scores_gemma":[0.9990115,0.000120665,0.00027212562,0.00007636272,0.00031376298,0.00020545235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024426263,0.000233838,0.00020585465,0.0021384107,0.0010178379,0.00068536727,0.00055531267,0.00020599738,0.002114381],"category_scores_gemma":[0.001320081,0.00015076781,0.00022703383,0.0026786227,0.00035007193,0.00015990568,0.00055981125,0.00017425217,0.0001677103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015345846,0.00003210798,0.97123295,0.0000294374,0.00009709447,0.00057652424,0.00028009422,0.0009913496,0.004396097,0.0001299062,0.0007387921,0.021342246],"study_design_scores_gemma":[0.000004995145,0.000019232975,0.99700576,0.0000056298077,0.0000264463,0.00013667968,0.00037427628,0.0011687159,0.00065648305,0.000020557836,0.0005753346,0.0000058704436],"about_ca_topic_score_codex":0.91168433,"about_ca_topic_score_gemma":0.96618193,"teacher_disagreement_score":0.088315666,"about_ca_system_score_codex":0.0029904323,"about_ca_system_score_gemma":0.004451026,"threshold_uncertainty_score":0.17767149},"labels":[],"label_agreement":null},{"id":"W1908004599","doi":"10.1002/2015gl065320","title":"Trends and variability in rain‐on‐snow events","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":198,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University of Washington; Joint Institute for the Study of the Atmosphere and Ocean; National Aeronautics and Space Administration; Goddard Space Flight Center; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"North Atlantic oscillation; Arctic oscillation; Climatology; Snow; Snow cover; Climate change; Physical geography; Geography; Environmental science; Geology; Oceanography; Northern Hemisphere; Meteorology","score_opus":0.07155460878297268,"score_gpt":0.34232036401153443,"score_spread":0.2707657552285617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1908004599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99620557,0.00011892514,0.0002929242,0.000040194634,0.000006824267,0.0000040943282,0.0023134155,0.000027578437,0.0009904235],"genre_scores_gemma":[0.9971312,0.00006033837,0.00020090476,0.000007176283,0.000010257928,0.0000043894142,0.0023802295,0.0000072001667,0.00019837827],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984217,0.000025663207,0.000021292493,0.00005332938,0.000037997594,0.000019470303],"domain_scores_gemma":[0.9991035,0.00021825876,0.00033351785,0.000068918045,0.00022092507,0.00005488006],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049155595,0.00014329457,0.00012752147,0.000876752,0.00013800962,0.0005321354,0.00017368469,0.00014800108,0.0006950695],"category_scores_gemma":[0.0011737635,0.00009565004,0.00022742209,0.0009456064,0.00013170799,0.00037665438,0.00023967109,0.00020696581,0.00016059651],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008125811,0.000014736039,0.9913395,0.000017898961,0.00012358213,0.000030788087,0.000198354,0.000885913,0.0014810374,0.00012430079,0.00034011138,0.0053625014],"study_design_scores_gemma":[0.000002516354,0.0000114135755,0.99712,0.0000039917745,0.000014030974,0.000020224013,0.00006541156,0.0016621319,0.00028788467,0.00003989672,0.0007696754,0.0000029505304],"about_ca_topic_score_codex":0.008336047,"about_ca_topic_score_gemma":0.0126795955,"teacher_disagreement_score":0.008336047,"about_ca_system_score_codex":0.00018687804,"about_ca_system_score_gemma":0.00014088013,"threshold_uncertainty_score":0.016575038},"labels":[],"label_agreement":null},{"id":"W1908615695","doi":"10.1029/2012gl053047","title":"Linking the 8.2 ka event and its freshwater forcing in the Labrador Sea","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Geology; Glacial period; Seawater; Continental shelf; Thermohaline circulation; Forcing (mathematics); Climatology; Paleontology","score_opus":0.04441958450328678,"score_gpt":0.30500165562798126,"score_spread":0.2605820711246945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1908615695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858344,0.000028902585,0.000033872588,0.00010525036,0.0000061471046,0.0000022129723,0.00015626973,0.000015905314,0.0010680385],"genre_scores_gemma":[0.99956125,0.000021313059,0.000043884298,0.000032868295,0.000008505363,0.0000031657744,0.00016915366,0.000004877596,0.00015501388],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999137,0.000009821958,0.000006969808,0.000021831986,0.000010586153,0.000037070367],"domain_scores_gemma":[0.9997451,0.000020746424,0.000105746476,0.0000295872,0.00004892459,0.0000498426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019235567,0.00024898455,0.00029147035,0.00053320115,0.0004969226,0.0006984866,0.00029158598,0.00043200818,0.0012261921],"category_scores_gemma":[0.0008161923,0.00018238834,0.00023913673,0.00044569274,0.0004172225,0.0003271327,0.0008560006,0.00035904231,0.00018809455],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00089583284,0.00011044845,0.94254255,0.000052877378,0.00015372978,0.00073240773,0.0006719567,0.0021814853,0.037546206,0.0006710284,0.00087110046,0.013570398],"study_design_scores_gemma":[0.000012239416,0.00002564419,0.9981462,0.0000041472017,0.000015266578,0.000034933288,0.00011780341,0.0003746828,0.0005743134,0.00007889127,0.0006087423,0.0000070977703],"about_ca_topic_score_codex":0.04543756,"about_ca_topic_score_gemma":0.062636845,"teacher_disagreement_score":0.04543756,"about_ca_system_score_codex":0.0012880224,"about_ca_system_score_gemma":0.0005771767,"threshold_uncertainty_score":0.09034622},"labels":[],"label_agreement":null},{"id":"W1909035556","doi":"10.1002/2015gl065331","title":"First satellite imaging of auroral pulsations by the Fast Auroral Imager on e‐<scp>POP</scp>","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Johns Hopkins University; National Aeronautics and Space Administration; Canadian Space Agency; University of Calgary; National Science Foundation","keywords":"Substorm; Satellite; Bulge; Physics; Polar; Latitude; Ionosphere; Outflow; Astrophysics; Geophysics; Remote sensing; Astronomy; Magnetosphere; Geology; Stars; Meteorology; Magnetic field","score_opus":0.022824500470353667,"score_gpt":0.28979659521782425,"score_spread":0.2669720947474706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1909035556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98641926,0.0003354653,0.0021396582,0.000107246466,0.00003070199,0.000025415322,0.0013785481,0.00014457226,0.009419256],"genre_scores_gemma":[0.99038774,0.0001906402,0.005442407,0.00006176374,0.00003580698,0.000015506559,0.0018705081,0.00005030435,0.0019453665],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999368,0.000006400085,0.0000024623118,0.000012429519,0.000026706444,0.0000151177765],"domain_scores_gemma":[0.9998374,0.000019313147,0.00002750423,0.000024716854,0.00005702053,0.000034025536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016474012,0.00018097943,0.0001614103,0.0007376497,0.00032687894,0.0003588731,0.00017972973,0.00022583497,0.0013083216],"category_scores_gemma":[0.00023899703,0.00013849753,0.00015287558,0.00048409402,0.00021946443,0.00025689692,0.0004923905,0.0003262261,0.00021033062],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007609046,0.000104358514,0.260162,0.00020530693,0.00024724743,0.0034462642,0.00092459115,0.0015716535,0.64581823,0.0005774081,0.0056035593,0.08057851],"study_design_scores_gemma":[0.000029480992,0.00023705761,0.92797714,0.000035565274,0.00006527328,0.002232493,0.0004304755,0.002811121,0.05282581,0.00017369162,0.013156725,0.000025186699],"about_ca_topic_score_codex":0.002049693,"about_ca_topic_score_gemma":0.005975244,"teacher_disagreement_score":0.002049693,"about_ca_system_score_codex":0.00019161153,"about_ca_system_score_gemma":0.00014121529,"threshold_uncertainty_score":0.004376769},"labels":[],"label_agreement":null},{"id":"W1909403247","doi":"10.1002/grl.50701","title":"Dependence of abrupt Atlantic meridional ocean circulation changes on climate background states","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Last Glacial Maximum; Glacial period; Geology; Holocene; Thermohaline circulation; Interglacial; Oceanography; Advection; Zonal and meridional; North Atlantic Deep Water; Ocean current; Geomorphology","score_opus":0.047875076038496896,"score_gpt":0.30275652494268146,"score_spread":0.25488144890418457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1909403247","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992304,0.000012151031,0.000090896036,0.000032690008,0.0000036286533,0.00000221467,0.000120665994,0.000009492075,0.0004978975],"genre_scores_gemma":[0.99979514,0.0000076047145,0.00003249393,0.00000747453,9.597105e-7,0.0000015659369,0.00009021229,0.000002436338,0.00006205447],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992836,0.000016097687,0.00000393809,0.000016599515,0.000005537608,0.000029516184],"domain_scores_gemma":[0.9996722,0.00015484152,0.000044358734,0.000029626943,0.000023243458,0.000075858494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002677617,0.00023174232,0.00018697303,0.00018565045,0.0002257891,0.00051858096,0.0001685976,0.00028315998,0.0022965304],"category_scores_gemma":[0.00091680797,0.00013941017,0.0003185102,0.00012879312,0.0002656081,0.00025336476,0.00028944304,0.00041775478,0.00014673095],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017666369,0.00054051995,0.57230693,0.00008217289,0.00043925713,0.00047184437,0.00012633504,0.36062,0.04981677,0.002494336,0.0015401952,0.009794986],"study_design_scores_gemma":[0.00023304128,0.0005761428,0.5806941,0.000016239537,0.00009641075,0.000055622513,0.0002044772,0.41101632,0.005732274,0.00068364845,0.0006557532,0.000035941717],"about_ca_topic_score_codex":0.011169301,"about_ca_topic_score_gemma":0.009738407,"teacher_disagreement_score":0.011169301,"about_ca_system_score_codex":0.00037483743,"about_ca_system_score_gemma":0.0002724672,"threshold_uncertainty_score":0.022208631},"labels":[],"label_agreement":null},{"id":"W1910062242","doi":"10.1002/2014gl062107","title":"Trend and interannual variability in southeast Greenland Sea Ice: Impacts on coastal Greenland climate variability","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; European Centre for Medium-Range Weather Forecasts; Universität Hamburg; Strong; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Oceanography; Fjord; Climatology; Future sea level; Sea ice; Arctic ice pack; Antarctic sea ice; Cryosphere; Glacier; Iceberg; North Atlantic oscillation; Greenland ice sheet; Ice sheet; Geomorphology","score_opus":0.015770347721535335,"score_gpt":0.2693455641127898,"score_spread":0.25357521639125447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1910062242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99900085,0.000047702557,0.000023413131,0.00010098477,0.0000025706115,7.525837e-7,0.00030350767,0.000004327274,0.000515871],"genre_scores_gemma":[0.99952245,0.000032907665,0.000024738305,0.000024858587,0.0000022071627,8.5844897e-7,0.00023034427,0.0000015059841,0.00015996986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.0000063410503,0.000004036337,0.000011295998,0.000010358863,0.000021546857],"domain_scores_gemma":[0.9997329,0.00003068516,0.000106252555,0.000020348996,0.000064960484,0.000044824803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023831916,0.00009936209,0.00009449433,0.0005642884,0.00020741129,0.00053298136,0.00015120477,0.00016154566,0.0007980806],"category_scores_gemma":[0.0004437858,0.00003922181,0.00012436663,0.0007482914,0.0002478971,0.00026409456,0.00032023966,0.00011650378,0.000088166016],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003821524,0.000013572734,0.9919629,0.000008197768,0.00003332503,0.00011163035,0.00022112762,0.00064480933,0.0015964909,0.00013405891,0.00032181735,0.0049138553],"study_design_scores_gemma":[5.399036e-7,0.0000040844193,0.9991936,0.0000023171579,0.000002634219,0.00001100335,0.000150386,0.00028052912,0.00005331293,0.00001934883,0.00028135837,8.8101757e-7],"about_ca_topic_score_codex":0.118509464,"about_ca_topic_score_gemma":0.2426926,"teacher_disagreement_score":0.118509464,"about_ca_system_score_codex":0.0012025326,"about_ca_system_score_gemma":0.00054343574,"threshold_uncertainty_score":0.23563933},"labels":[],"label_agreement":null},{"id":"W1912262825","doi":"10.1029/2003gl019300","title":"Modeling evidence for recent warming of the Arctic soil thermal regime","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Active layer; Arctic; Climate change; Environmental science; Global warming; Geology; Structural basin; Physical geography; Climatology; Drainage basin; Hydrology (agriculture); Atmospheric sciences; Oceanography; Geomorphology; Layer (electronics); Geography","score_opus":0.19839004280802713,"score_gpt":0.35389837111266564,"score_spread":0.1555083283046385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1912262825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99641234,0.00007809376,0.0007747177,0.00014422416,0.000011076135,0.000004300448,0.00045421463,0.00005507703,0.0020659338],"genre_scores_gemma":[0.9989447,0.00006679882,0.00045145594,0.000013428627,0.0000054526085,0.00000537193,0.00030793785,0.000006161333,0.00019864831],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992263,0.000025024729,0.0000048823244,0.00002174074,0.000009086706,0.00001665295],"domain_scores_gemma":[0.9996753,0.00014392177,0.000057930843,0.000022451402,0.00006339818,0.000036999867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032179223,0.00025748936,0.00020009624,0.0002877259,0.0002574123,0.00052160944,0.0005143895,0.00054761703,0.0015248357],"category_scores_gemma":[0.00093647774,0.00022208726,0.00039224682,0.0004742142,0.0002043917,0.0003816621,0.00026020975,0.0003084198,0.00013705085],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017646488,0.00008636515,0.10378037,0.00006047312,0.00012867768,0.000126095,0.00009083027,0.8868645,0.002338062,0.001224954,0.0006257733,0.004497585],"study_design_scores_gemma":[0.00006349451,0.0000623112,0.04654182,0.0000129178625,0.00006402888,0.000029359828,0.00006167941,0.9509448,0.0006349566,0.0005183798,0.001051783,0.000014497193],"about_ca_topic_score_codex":0.04572486,"about_ca_topic_score_gemma":0.049626295,"teacher_disagreement_score":0.04572486,"about_ca_system_score_codex":0.00086673384,"about_ca_system_score_gemma":0.0006222563,"threshold_uncertainty_score":0.09091747},"labels":[],"label_agreement":null},{"id":"W1912647720","doi":"10.1029/2010gl044878","title":"Changing spring air‐temperature gradients along large northern rivers: Implications for severity of river‐ice floods","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact; University of Victoria; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Spring (device); Climate change; Flood myth; Arctic; Flooding (psychology); Hydrology (agriculture); Current (fluid); Climatology; Physical geography; Air temperature; Atmospheric sciences; Geology; Oceanography; Geography","score_opus":0.016215800553779913,"score_gpt":0.27323937941502796,"score_spread":0.25702357886124805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1912647720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991093,0.000052971223,0.000082831735,0.000043370004,0.0000017958118,0.0000016417647,0.00012650355,0.000005233564,0.00057624636],"genre_scores_gemma":[0.99960226,0.000047058496,0.00010020531,0.000009610837,0.0000034486252,0.000002228159,0.00012154806,0.0000023297252,0.00011127061],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998857,0.00003194089,0.0000104118035,0.000034226647,0.000015350772,0.000022414853],"domain_scores_gemma":[0.9996574,0.00009028325,0.00012045019,0.00001728959,0.000057126024,0.00005746316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003876753,0.0001325146,0.00017264727,0.00042161893,0.00028923174,0.00055950554,0.00015049952,0.0001812077,0.0005437197],"category_scores_gemma":[0.000631442,0.00011114129,0.00023885828,0.00044698702,0.00031869093,0.00029601582,0.0002333885,0.00018296036,0.000076321085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009876424,0.000019345114,0.99044025,0.0000117618265,0.000036211986,0.000046810244,0.00016681071,0.0018565962,0.0040646745,0.00009368243,0.00011420308,0.0030509012],"study_design_scores_gemma":[9.1868725e-7,0.00000886181,0.99897444,0.0000015027459,0.000005598778,0.00001221757,0.00013245243,0.00058925623,0.00015166815,0.00002705148,0.00009409596,0.000002008696],"about_ca_topic_score_codex":0.026195778,"about_ca_topic_score_gemma":0.04905802,"teacher_disagreement_score":0.026195778,"about_ca_system_score_codex":0.00056573434,"about_ca_system_score_gemma":0.0004421791,"threshold_uncertainty_score":0.05208659},"labels":[],"label_agreement":null},{"id":"W1912786102","doi":"10.1029/2011gl049846","title":"Absolute gravity calibration of GPS velocities and glacial isostatic adjustment in mid-continent North America","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Geodesy; Post-glacial rebound; Global Positioning System; Geology; Geodetic datum; Reference frame; Satellite geodesy; Tectonic uplift; Glacial period; Geomorphology; Seismology; Tectonics; Frame (networking)","score_opus":0.053510119945985736,"score_gpt":0.26296177047474356,"score_spread":0.20945165052875783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1912786102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936254,0.00038113675,0.0009680325,0.00007445458,0.000014920726,0.000009504472,0.0017909994,0.00007423727,0.003061321],"genre_scores_gemma":[0.9966493,0.00009897753,0.0011021716,0.000014328422,0.0000055298337,0.000006340778,0.0018623116,0.00000962744,0.00025142456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979395,0.000038231225,0.000018232897,0.000064324595,0.00005529822,0.000030021714],"domain_scores_gemma":[0.9993574,0.000051583593,0.00020928385,0.000071361465,0.0002754111,0.00003491519],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003922158,0.00024654577,0.00015782255,0.0013282367,0.00028274726,0.0004379007,0.00036218276,0.00017593117,0.0007509986],"category_scores_gemma":[0.0015840544,0.000104016755,0.00012734115,0.0019155117,0.00023925099,0.00034671108,0.00035307187,0.0001613469,0.00017029406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035637335,0.000020190068,0.9706663,0.000022239616,0.00003646356,0.00006622158,0.00026796118,0.004383043,0.0018540033,0.00022697997,0.0011607325,0.021260202],"study_design_scores_gemma":[0.0000010970936,0.0000056926256,0.99769753,0.000003538895,0.0000028429477,0.000018340603,0.00006497293,0.0012620444,0.00014131349,0.00002166691,0.00077880797,0.0000022304382],"about_ca_topic_score_codex":0.18091692,"about_ca_topic_score_gemma":0.26058927,"teacher_disagreement_score":0.18091692,"about_ca_system_score_codex":0.0008963908,"about_ca_system_score_gemma":0.00048503582,"threshold_uncertainty_score":0.35972768},"labels":[],"label_agreement":null},{"id":"W1913840600","doi":"10.1002/grl.50166","title":"Biogeochemical carbon coupling influences global precipitation in geoengineering experiments","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Office of Science; University of Victoria; U.S. Department of Energy","keywords":"Biogeochemical cycle; Environmental science; Carbon cycle; Atmospheric sciences; Precipitation; Coupled model intercomparison project; Primary production; Climate change; Carbon fibers; Climatology; Climate model; Ecosystem; Environmental chemistry; Chemistry; Meteorology; Ecology; Geology; Oceanography; Materials science; Physics","score_opus":0.03505220495507627,"score_gpt":0.3125371769829084,"score_spread":0.2774849720278321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1913840600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992367,0.000015753072,0.0003359753,0.000029863842,0.0000033806152,0.0000042444403,0.00004869713,0.000011123262,0.00031431022],"genre_scores_gemma":[0.9996865,0.000018731778,0.00014924274,0.000023003158,0.0000014946137,0.00000640562,0.000051807725,0.000004104377,0.000058770765],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997844,0.00010149099,0.000013551062,0.000043849454,0.000028931907,0.000027695149],"domain_scores_gemma":[0.99933666,0.0003522799,0.0001262569,0.000076793105,0.00002974653,0.000078213685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004769428,0.00025059882,0.00022799397,0.00016203083,0.00016001504,0.0005002951,0.0003007095,0.0003248828,0.00056882174],"category_scores_gemma":[0.00089870923,0.00011883691,0.00020975266,0.0002391276,0.0004595711,0.00037730666,0.00038375685,0.0005004735,0.00004885643],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025125297,0.0012515481,0.10119915,0.00010952415,0.00034409628,0.0003557374,0.0002661261,0.09598352,0.783726,0.0034541273,0.00054934015,0.010248296],"study_design_scores_gemma":[0.0005603852,0.0037358801,0.4680206,0.000014868249,0.00029884104,0.00014156332,0.0003351083,0.21755545,0.30080566,0.0061791493,0.002250723,0.000101845464],"about_ca_topic_score_codex":0.0018925284,"about_ca_topic_score_gemma":0.0019711412,"teacher_disagreement_score":0.0018925284,"about_ca_system_score_codex":0.000526891,"about_ca_system_score_gemma":0.000203082,"threshold_uncertainty_score":0.003822863},"labels":[],"label_agreement":null},{"id":"W1915543731","doi":"10.1002/2015gl064892","title":"A solar escalator on Mars: Self‐lifting of dust layers by radiative heating","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency; University of Arizona; Jet Propulsion Laboratory; Belgian Federal Science Policy Office; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Atmospheric sciences; Dust storm; Radiative transfer; Environmental science; Lidar; Atmosphere (unit); Advection; Aerosol; Geology; Astrobiology; Meteorology; Physics; Remote sensing","score_opus":0.04568512907755409,"score_gpt":0.30704883163464214,"score_spread":0.2613637025570881,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1915543731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99659926,0.000032593234,0.0015274228,0.00007206397,0.000007839,0.000008043293,0.000045509947,0.000106485975,0.0016008115],"genre_scores_gemma":[0.99951136,0.000010713851,0.0002805517,0.000006701431,0.000002302923,0.0000017339282,0.000016510512,0.0000052486234,0.0001648824],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995315,0.000008984826,0.00000187442,0.000012714867,0.0000074562163,0.00001569494],"domain_scores_gemma":[0.99991083,0.000017685628,0.000016137847,0.000022543813,0.00000947901,0.000023269678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014214964,0.00021578722,0.00015164254,0.00018810728,0.0003587156,0.00046940517,0.00033901824,0.00036150558,0.0013499014],"category_scores_gemma":[0.00022164703,0.00018780299,0.00041694217,0.00008630355,0.00021769422,0.00029438877,0.00044561754,0.00026385896,0.00013225444],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085559377,0.00039196617,0.42527878,0.00007530596,0.00034530394,0.0026877227,0.00067167013,0.2402667,0.28076264,0.0082241325,0.003165371,0.037274756],"study_design_scores_gemma":[0.000129851,0.00032337656,0.24267721,0.000013302829,0.000066182016,0.00045445847,0.00020223713,0.7329227,0.018643592,0.0024306118,0.0020896818,0.00004681364],"about_ca_topic_score_codex":0.0039441027,"about_ca_topic_score_gemma":0.0018255945,"teacher_disagreement_score":0.0039441027,"about_ca_system_score_codex":0.00032206753,"about_ca_system_score_gemma":0.00011831374,"threshold_uncertainty_score":0.007842302},"labels":[],"label_agreement":null},{"id":"W1917629280","doi":"10.1029/2011gl050299","title":"Real barchan dune collisions and ejections","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Lethbridge","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates; Google","keywords":"Geology; Geomorphology; Turbulence; Wake; Meteorology; Mechanics; Physics","score_opus":0.054371108720700154,"score_gpt":0.2929821504720477,"score_spread":0.2386110417513475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1917629280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981993,0.000050382994,0.00033383752,0.00005870253,0.000008209845,0.0000065827317,0.000054515465,0.000010984625,0.0012775492],"genre_scores_gemma":[0.99960846,0.000010212869,0.00018534741,0.000009469928,0.000003901714,0.0000029044338,0.0000379258,0.0000011398641,0.00014061276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979144,0.000036011195,0.0000114891645,0.000048713853,0.000054414762,0.000057943274],"domain_scores_gemma":[0.9993523,0.00021571394,0.0002080865,0.00007112995,0.000055912064,0.000096871336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002706164,0.00015015979,0.00019272999,0.00037517026,0.0009110369,0.0005634967,0.00037921732,0.00058208196,0.0033180884],"category_scores_gemma":[0.0015277279,0.00020199709,0.000085303385,0.00027954121,0.0005494831,0.0005214787,0.0011903889,0.00035933236,0.00019526988],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095422147,0.00017433976,0.9306719,0.00020891066,0.00015264958,0.005167503,0.0066793575,0.0026098606,0.02067351,0.004162364,0.0022942082,0.026251309],"study_design_scores_gemma":[0.000041618965,0.00020020703,0.9783972,0.000040166662,0.000033958306,0.0018025371,0.004420558,0.0074083,0.0021667667,0.0012175697,0.004242469,0.000028808441],"about_ca_topic_score_codex":0.0017504259,"about_ca_topic_score_gemma":0.0041642445,"teacher_disagreement_score":0.0033180884,"about_ca_system_score_codex":0.00033770953,"about_ca_system_score_gemma":0.00016510385,"threshold_uncertainty_score":0.011100173},"labels":[],"label_agreement":null},{"id":"W1917916713","doi":"10.1029/2007gl029894","title":"Mineralogic constraints on sulfur‐rich soils from Pancam spectra at Gusev crater, Mars","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg","funders":"","keywords":"Jarosite; Mars Exploration Program; Impact crater; Soil water; Geology; Sulfur; Sulfate; Mineralogy; Geochemistry; Astrobiology; Chemistry; Soil science; Physics","score_opus":0.04215463173283306,"score_gpt":0.2989374576354868,"score_spread":0.2567828259026537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1917916713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998582,0.00004511167,0.0002591992,0.000022310396,8.969216e-7,0.0000032995856,0.00050634006,0.00005423953,0.0005264714],"genre_scores_gemma":[0.9980884,0.000035080993,0.0010282601,0.000005706654,0.0000022543782,0.0000023712494,0.0007411007,0.00001392991,0.00008285141],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988997,0.000016733533,0.0000053779722,0.000034290017,0.00003208718,0.000021572328],"domain_scores_gemma":[0.9998317,0.000032378095,0.00003475379,0.000022069918,0.000049641032,0.00002951992],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018838585,0.00042935743,0.00026337215,0.0015345212,0.00035833108,0.00044988975,0.00034302782,0.00030121885,0.0010520001],"category_scores_gemma":[0.0005058342,0.00039266623,0.00019812581,0.0010112388,0.0002405275,0.0002583264,0.00042091354,0.00015149874,0.00025030487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001196604,0.0001464836,0.7315989,0.0001949483,0.00018582556,0.0010092756,0.00094812305,0.03497754,0.16458192,0.00050359045,0.0035241193,0.06113269],"study_design_scores_gemma":[0.000052355597,0.000054169417,0.95091707,0.000014615319,0.00004033684,0.00024824386,0.0003337052,0.04127965,0.0056159184,0.00019744555,0.0012292425,0.00001729055],"about_ca_topic_score_codex":0.037366737,"about_ca_topic_score_gemma":0.11144806,"teacher_disagreement_score":0.037366737,"about_ca_system_score_codex":0.00034630115,"about_ca_system_score_gemma":0.00025796116,"threshold_uncertainty_score":0.0742985},"labels":[],"label_agreement":null},{"id":"W1918270636","doi":"10.1002/2014gl059575","title":"Reconstruction of Pacific Ocean bottom water salinity during the Last Glacial Maximum","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"National Science Foundation","keywords":"Last Glacial Maximum; Oceanography; Salinity; Geology; Latitude; Circumpolar deep water; Seawater; Water mass; Glacial period; Bottom water; Climatology; North Atlantic Deep Water; Holocene; Thermohaline circulation; Geomorphology","score_opus":0.020732148033031476,"score_gpt":0.25668227259014265,"score_spread":0.23595012455711117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918270636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99832207,0.000047251066,0.00035322653,0.00003376994,0.0000034085622,0.0000028351583,0.0005635032,0.000026019023,0.0006478547],"genre_scores_gemma":[0.99884003,0.000033322598,0.00031953,0.0000072672096,0.0000018746188,0.0000032284574,0.0006948769,0.00000436071,0.000095532],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999428,0.000010233855,0.0000035999458,0.000019077832,0.000013663546,0.000010611428],"domain_scores_gemma":[0.999838,0.000019136325,0.00002872237,0.000016294174,0.00006105763,0.00003683112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002717872,0.00029548767,0.00019866212,0.000887164,0.0003011855,0.00048687344,0.00022976157,0.00028465633,0.00052323105],"category_scores_gemma":[0.00057657214,0.00026324234,0.0003400863,0.0007991902,0.00022823428,0.00023731105,0.00041178116,0.0002798735,0.00018960601],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017639337,0.000023082148,0.9708501,0.000025357358,0.00012077123,0.00014800516,0.00017017998,0.0065514753,0.012208937,0.00012572421,0.0003310931,0.009268838],"study_design_scores_gemma":[0.000007011788,0.000017584884,0.99386793,0.000006339076,0.000016082042,0.000035893558,0.00007525323,0.0049279802,0.0007112464,0.000041598756,0.00028674112,0.0000063828875],"about_ca_topic_score_codex":0.038452674,"about_ca_topic_score_gemma":0.029204357,"teacher_disagreement_score":0.038452674,"about_ca_system_score_codex":0.0005561191,"about_ca_system_score_gemma":0.00041751214,"threshold_uncertainty_score":0.07645774},"labels":[],"label_agreement":null},{"id":"W1918626762","doi":"10.1029/2012gl052219","title":"The International Bathymetric Chart of the Arctic Ocean (IBCAO) Version 3.0","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":1183,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of New Brunswick; Canadian Hydrographic Service","funders":"","keywords":"Bathymetry; Bathymetric chart; Arctic; The arctic; Oceanography; Navy; Seafloor spreading; Marine geology; Geology; Range (aeronautics); Climatology; Geography; Archaeology; Engineering","score_opus":0.023024637509741788,"score_gpt":0.27557726892503975,"score_spread":0.252552631415298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918626762","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.046603862,0.0046526557,0.10433325,0.0010344037,0.0032030556,0.0015852366,0.6097381,0.005316845,0.22353256],"genre_scores_gemma":[0.09870983,0.0045418567,0.21226476,0.0006269738,0.00035442875,0.0020378625,0.6510454,0.0025483803,0.02787056],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9990701,0.00013691894,0.00011316195,0.00009679384,0.00045851883,0.00012453266],"domain_scores_gemma":[0.99810034,0.00009424623,0.00025720743,0.00022597198,0.0011823532,0.00013983471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015133892,0.0008498508,0.00053067616,0.0038493618,0.0006373367,0.0012261174,0.00068035815,0.00031264353,0.008437565],"category_scores_gemma":[0.0028734035,0.0003073836,0.0004673338,0.007711247,0.0004143497,0.0008300668,0.0011904581,0.0011082771,0.0038343444],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047308457,0.000063634965,0.05934907,0.0010299411,0.00009774819,0.0003384425,0.0010291046,0.007100527,0.010474566,0.024856491,0.6104584,0.284729],"study_design_scores_gemma":[0.000036580466,0.000024925333,0.06605411,0.00017497595,0.000021208012,0.00015335235,0.0003391824,0.0017133162,0.0012019913,0.0019149192,0.928309,0.000056400866],"about_ca_topic_score_codex":0.1333107,"about_ca_topic_score_gemma":0.109062865,"teacher_disagreement_score":0.1333107,"about_ca_system_score_codex":0.0010477947,"about_ca_system_score_gemma":0.0053696134,"threshold_uncertainty_score":0.26506948},"labels":[],"label_agreement":null},{"id":"W1918781448","doi":"10.1002/2015gl065402","title":"The Iquique earthquake sequence of April 2014: Bayesian modeling accounting for prediction uncertainty","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Southern California Earthquake Center","keywords":"Aftershock; Geology; Foreshock; Seismology; Subduction; Slip (aerodynamics); Geodetic datum; Seismic gap; Trench; Shock (circulatory); Geodesy; Tectonics; Induced seismicity","score_opus":0.08324452757035668,"score_gpt":0.3137374505010344,"score_spread":0.23049292293067775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1918781448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7066272,0.0005305554,0.2838349,0.0018086625,0.000053467447,0.00008850546,0.00089322584,0.00029994853,0.0058635743],"genre_scores_gemma":[0.986541,0.00017542968,0.010544977,0.000074437114,0.00005618471,0.00005656686,0.00033889338,0.000028748605,0.0021838034],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995647,0.00020684199,0.000018356413,0.000096638425,0.000053315696,0.000060136037],"domain_scores_gemma":[0.9965868,0.0025967695,0.00037739018,0.00010058158,0.00023339664,0.000104942985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002957609,0.0005879407,0.0008543664,0.0007599486,0.0005894846,0.0012838978,0.0013645646,0.0012729076,0.0014932937],"category_scores_gemma":[0.007608515,0.0007755473,0.0008236176,0.00053831673,0.0006624792,0.0012517049,0.0007578373,0.0010665541,0.00020359734],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056813904,0.00003275199,0.0055932184,0.000013471135,0.000047412697,0.000047100606,0.00005146001,0.9806029,0.00019873906,0.0068731494,0.00039139605,0.006091425],"study_design_scores_gemma":[0.0000046421824,0.0000054497555,0.0006667041,0.00000255133,0.000005594379,0.000003496786,0.000004969892,0.99744654,0.000019047491,0.0017743097,0.00006226063,0.0000044417807],"about_ca_topic_score_codex":0.062112853,"about_ca_topic_score_gemma":0.039218098,"teacher_disagreement_score":0.062112853,"about_ca_system_score_codex":0.0013590332,"about_ca_system_score_gemma":0.001094153,"threshold_uncertainty_score":0.12350267},"labels":[],"label_agreement":null},{"id":"W1920375935","doi":"10.1002/2013gl057282","title":"Sea surface temperature and sea ice variability in the subpolar North Atlantic from explosive volcanism of the late thirteenth century","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Aurora College; Makivik Corporation","funders":"","keywords":"Volcanism; Geology; Oceanography; Explosive material; Sea surface temperature; Climatology; Archaeology; Paleontology; Geography; Tectonics","score_opus":0.01690369535849771,"score_gpt":0.23988893501935452,"score_spread":0.22298523966085682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1920375935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996848,0.000022771754,0.000034381665,0.000011269567,0.0000014297837,4.4490253e-7,0.000126681,0.0000022341605,0.00011597826],"genre_scores_gemma":[0.99959356,0.000030074349,0.00003671296,0.0000050766635,0.00000194138,9.786743e-7,0.00026316821,0.0000012144305,0.00006731258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995923,0.000006459346,0.0000026457528,0.00001383449,0.000006998594,0.00001078415],"domain_scores_gemma":[0.9998661,0.000023595294,0.000041919073,0.000013810267,0.00002661557,0.000027913127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024549608,0.00012518045,0.00013443398,0.0003205723,0.0001769939,0.0005696823,0.00012894193,0.00017885478,0.00054115057],"category_scores_gemma":[0.00043165352,0.00010257923,0.00030112808,0.00038503428,0.00021150387,0.0001958339,0.0003534403,0.0002380698,0.00008028207],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014069809,0.000023303346,0.9863934,0.000012021554,0.00011407822,0.00013425302,0.00011791583,0.0045986967,0.0050682067,0.0001015932,0.00010919669,0.0031865814],"study_design_scores_gemma":[0.0000024918154,0.0000123671425,0.9975133,0.0000027401659,0.000012931701,0.000019298726,0.00007226805,0.001912688,0.0002973421,0.000024396528,0.0001271415,0.000003043614],"about_ca_topic_score_codex":0.027028626,"about_ca_topic_score_gemma":0.038204074,"teacher_disagreement_score":0.027028626,"about_ca_system_score_codex":0.00049462117,"about_ca_system_score_gemma":0.00029779572,"threshold_uncertainty_score":0.053742588},"labels":[],"label_agreement":null},{"id":"W1920490671","doi":"10.1002/2015gl064696","title":"Increasing carbon dioxide concentration in the upper atmosphere observed by SABER","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Goddard Space Flight Center; Ministerio de Ciencia e Innovación; University of Waterloo; Langley Research Center; National Aeronautics and Space Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Mesopause; Atmosphere (unit); Atmospheric sciences; Troposphere; Environmental science; Thermosphere; Carbon dioxide; Northern Hemisphere; Mesosphere; Depth sounding; Climatology; Carbon dioxide in Earth's atmosphere; Ozone; Atmospheric chemistry; Stratosphere; Southern Hemisphere; Geology; Meteorology; Ionosphere; Physics; Chemistry","score_opus":0.031051688352538135,"score_gpt":0.26535080375152115,"score_spread":0.23429911539898302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1920490671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99744177,0.00006840811,0.00025720298,0.000017001514,0.0000039627744,0.0000025969478,0.00067606964,0.00008724483,0.0014457633],"genre_scores_gemma":[0.99888223,0.00003611596,0.00029754973,0.00001237892,0.000004978512,0.0000032360226,0.00053553336,0.0000066560287,0.0002213812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997751,0.000018942445,0.00001195403,0.000056927493,0.00008864284,0.000048382113],"domain_scores_gemma":[0.9996172,0.00008307453,0.00010087511,0.000039651597,0.00008820378,0.000070971255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003125014,0.00032942143,0.00043737463,0.001431593,0.0002791561,0.0005947987,0.00024760843,0.00039021234,0.00087930536],"category_scores_gemma":[0.0006538991,0.00022370818,0.00029661358,0.0009522443,0.0002543074,0.00042485647,0.0005039618,0.00036676205,0.00026091727],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069781754,0.00012924826,0.76084554,0.000118216754,0.00020430249,0.00040347525,0.00071159535,0.003905516,0.20947923,0.00023320423,0.00061467267,0.022657163],"study_design_scores_gemma":[0.0000046020773,0.00004548576,0.9901938,0.0000034698237,0.000019267747,0.000058891193,0.00006494591,0.0020208696,0.006960825,0.00003986553,0.00057749054,0.000010546764],"about_ca_topic_score_codex":0.010227071,"about_ca_topic_score_gemma":0.007605243,"teacher_disagreement_score":0.010227071,"about_ca_system_score_codex":0.0003427609,"about_ca_system_score_gemma":0.0002012884,"threshold_uncertainty_score":0.020335138},"labels":[],"label_agreement":null},{"id":"W1921635979","doi":"10.1002/2015gl064291","title":"Radiative flux and forcing parameterization error in aerosol‐free clear skies","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Shortwave; Longwave; Forcing (mathematics); Radiative forcing; Environmental science; Cloud forcing; Atmospheric sciences; Aerosol; Climatology; Climate model; Radiative transfer; Meteorology; Climate change; Physics","score_opus":0.03553387051246367,"score_gpt":0.28747209615245606,"score_spread":0.2519382256399924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1921635979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99045396,0.00015165847,0.006921551,0.000072408155,0.000020734684,0.000009634186,0.001062387,0.0003158634,0.0009917241],"genre_scores_gemma":[0.9980787,0.000032375898,0.0010205865,0.0000091125285,0.0000035776086,0.0000055045452,0.00071230374,0.00003554681,0.00010219879],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99908495,0.00030234465,0.00010814958,0.00020974864,0.00018963637,0.0001051918],"domain_scores_gemma":[0.9960685,0.0019912648,0.00044987607,0.0008524753,0.00058738614,0.000050434253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027181595,0.00056208565,0.00041239872,0.0006918741,0.0003041052,0.0008383005,0.0006422548,0.00055250444,0.00042207594],"category_scores_gemma":[0.0076659364,0.00030943356,0.0006338523,0.0006799644,0.0004640465,0.00090586033,0.0005358247,0.00035076815,0.00019374299],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030756768,0.00005117888,0.1499015,0.00006455613,0.00025624532,0.00007712922,0.00008581259,0.827895,0.0061036055,0.0012434142,0.0005566129,0.013457296],"study_design_scores_gemma":[0.00011376157,0.00014293262,0.2416935,0.000048802136,0.00016406071,0.000105625346,0.00010259501,0.73247844,0.022327699,0.0013503312,0.0013801424,0.00009220744],"about_ca_topic_score_codex":0.034506354,"about_ca_topic_score_gemma":0.017234433,"teacher_disagreement_score":0.034506354,"about_ca_system_score_codex":0.00086659513,"about_ca_system_score_gemma":0.0006052488,"threshold_uncertainty_score":0.068611026},"labels":[],"label_agreement":null},{"id":"W1924264378","doi":"10.1029/2012gl052234","title":"Boundary‐layer turbulence characteristics during aeolian saltation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University","funders":"","keywords":"Boundary layer; Turbulence; Reynolds stress; Mechanics; Wind tunnel; Anemometer; Geology; Airflow; Wind speed; Turbulence kinetic energy; Meteorology; Aeolian processes; Physics; Geomorphology; Thermodynamics","score_opus":0.03118368143083095,"score_gpt":0.29319121308672724,"score_spread":0.2620075316558963,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1924264378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999816,0.000016080703,0.000036019737,0.0000030869148,7.8935125e-7,0.0000011047644,0.000019606316,0.0000025531747,0.000104649174],"genre_scores_gemma":[0.999767,0.000011719035,0.00003418491,0.0000037192383,5.212089e-7,0.0000019688443,0.000073985815,0.0000014154152,0.00010550924],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000045951106,0.0000037932357,0.000010809076,0.00001107925,0.000012465529],"domain_scores_gemma":[0.99987876,0.000018842104,0.000030668805,0.000005911699,0.00003623949,0.000029640527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106603075,0.00012965123,0.00022926,0.00035959124,0.00028795341,0.00027803917,0.00008605274,0.00020143528,0.0005507392],"category_scores_gemma":[0.00021516267,0.00010728019,0.00011466168,0.00015772144,0.00025001078,0.00018138645,0.0002642197,0.00018411888,0.00012415869],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011364676,0.000114739145,0.20616524,0.00004461498,0.000034072047,0.00045206698,0.0010262366,0.0015063151,0.7810426,0.00017905471,0.00013836565,0.008160309],"study_design_scores_gemma":[0.000015620284,0.00016786568,0.9750334,0.000005133834,0.000009811255,0.0000792744,0.000222938,0.003609165,0.020601036,0.000029928075,0.00021032918,0.000015448672],"about_ca_topic_score_codex":0.0079011405,"about_ca_topic_score_gemma":0.0050560534,"teacher_disagreement_score":0.0079011405,"about_ca_system_score_codex":0.00032249032,"about_ca_system_score_gemma":0.00010792949,"threshold_uncertainty_score":0.015710294},"labels":[],"label_agreement":null},{"id":"W1930277386","doi":"10.1029/2006gl025919","title":"Boreal ecosystems sequestered more carbon in warmer years","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Toronto","funders":"","keywords":"Environmental science; Ecosystem; Atmospheric sciences; Boreal; Troposphere; Boreal ecosystem; Ecosystem respiration; Eddy covariance; Flux (metallurgy); Carbon cycle; Planetary boundary layer; Photosynthesis; Boundary layer; Climatology; Oceanography; Ecology; Geology; Chemistry; Biology; Physics; Botany","score_opus":0.013055705418977694,"score_gpt":0.26020440561069114,"score_spread":0.24714870019171345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930277386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996226,0.00007387819,0.000028934921,0.000014379311,0.0000023421792,4.821707e-7,0.000072998264,0.0000046945524,0.00017966657],"genre_scores_gemma":[0.99955124,0.00004892294,0.00006085209,0.00003088767,0.000006477705,0.0000012939456,0.00019065535,0.0000020773011,0.00010757029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987435,0.000009530666,0.000010782423,0.00004609193,0.000017332213,0.000041991283],"domain_scores_gemma":[0.99963164,0.000030737287,0.00018154268,0.000040491195,0.000041836367,0.000073756295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003360781,0.00021565951,0.0004265554,0.0005014918,0.00065491785,0.00076108094,0.00021045521,0.0003260299,0.0007844637],"category_scores_gemma":[0.0004506694,0.00017394041,0.00027152558,0.00029682773,0.00038949098,0.000551257,0.00038693222,0.00027384592,0.000070944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00087995315,0.00009816693,0.8887475,0.00008641665,0.00040996654,0.00043720508,0.0006659607,0.0011878489,0.09514786,0.000382829,0.00044151637,0.011514777],"study_design_scores_gemma":[0.0000037610682,0.00002023878,0.9990526,0.0000014372996,0.000014649372,0.000060067978,0.000057193425,0.00008016839,0.00043887997,0.000023599781,0.00024385881,0.0000034419331],"about_ca_topic_score_codex":0.024566922,"about_ca_topic_score_gemma":0.054165643,"teacher_disagreement_score":0.024566922,"about_ca_system_score_codex":0.00074491574,"about_ca_system_score_gemma":0.00027362694,"threshold_uncertainty_score":0.048847854},"labels":[],"label_agreement":null},{"id":"W1930607044","doi":"10.1002/grl.50734","title":"Distribution of natural halocarbons in marine boundary air over the Arctic Ocean","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"JST-Mirai Program; National Oceanic and Atmospheric Administration","keywords":"Dimethyl sulfide; Bromoform; Arctic; Environmental science; Arctic geoengineering; Methyl iodide; Oceanography; Atmospheric sciences; Dimethylsulfoniopropionate; Atmosphere (unit); Troposphere; Bromide; Environmental chemistry; Climatology; Chemistry; Meteorology; Arctic ice pack; Geology; Geography; Phytoplankton","score_opus":0.011967768315333235,"score_gpt":0.24539459433586347,"score_spread":0.23342682602053022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930607044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993175,0.00013806252,0.000036337784,0.0000045966926,0.0000016250852,0.000001260056,0.0001999135,0.0000020392079,0.00029862113],"genre_scores_gemma":[0.99904746,0.00021326794,0.00013927951,0.00000858043,0.000005614506,0.0000035386379,0.00044049817,0.0000018815407,0.0001398856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.000014328435,0.0000067072565,0.000021056274,0.000027580669,0.000023318686],"domain_scores_gemma":[0.99979633,0.000025353891,0.000049817594,0.000007985499,0.00008061308,0.000039913983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013315298,0.00013612873,0.000121117395,0.0007734782,0.00037581782,0.00030806303,0.00010813367,0.00015405238,0.00019983409],"category_scores_gemma":[0.00017657349,0.00008686426,0.00015487689,0.00043403657,0.00018484361,0.00011000887,0.00018184968,0.000088706925,0.00009247394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029943642,0.00002201433,0.9358533,0.000036441965,0.000071230046,0.0001181293,0.000360946,0.00036700178,0.057075042,0.000048300462,0.00010895104,0.005639244],"study_design_scores_gemma":[0.0000020144932,0.000030929663,0.9979898,0.0000041934422,0.00000947821,0.000054384032,0.00017851558,0.00014094486,0.0013253128,0.000009854708,0.00025140878,0.0000031134264],"about_ca_topic_score_codex":0.04378324,"about_ca_topic_score_gemma":0.055047873,"teacher_disagreement_score":0.04378324,"about_ca_system_score_codex":0.00040575457,"about_ca_system_score_gemma":0.00034344092,"threshold_uncertainty_score":0.087056816},"labels":[],"label_agreement":null},{"id":"W1930871163","doi":"10.1002/2013gl058055","title":"Systematic land climate and evapotranspiration biases in CMIP5 simulations","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":290,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Goddard Space Flight Center; University of East Anglia","keywords":"Coupled model intercomparison project; Evapotranspiration; Environmental science; Climatology; Precipitation; Water cycle; Climate model; Population; Ensemble average; Amazon rainforest; Climate change; Atmospheric sciences; Geography; Meteorology; Geology","score_opus":0.061798852287842244,"score_gpt":0.3255628621495614,"score_spread":0.26376400986171916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1930871163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938182,0.00020834687,0.002291133,0.0001964486,0.000035184767,0.000026773669,0.0019159423,0.0001487597,0.0013592636],"genre_scores_gemma":[0.9974439,0.000067347806,0.0013542762,0.0000388247,0.000008505483,0.000019934914,0.0009531594,0.00003412181,0.00007982031],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994299,0.00024196478,0.000056548342,0.000103118444,0.00007417787,0.00009422787],"domain_scores_gemma":[0.99855703,0.00066916365,0.00020959043,0.00018749671,0.000291111,0.00008553744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019465606,0.0007431425,0.00035643353,0.0004506501,0.00039699225,0.00062445155,0.0007085141,0.0008332188,0.0006078595],"category_scores_gemma":[0.0053244643,0.0003177259,0.00050698855,0.00083806005,0.00033898768,0.00085124513,0.0005214777,0.00044179944,0.00011187413],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025886975,0.0001045717,0.1200573,0.000119891934,0.00020906872,0.00012851994,0.00013027644,0.8658856,0.0039955843,0.0015398401,0.0017211658,0.005849358],"study_design_scores_gemma":[0.00014094057,0.00009782006,0.0534032,0.000063933316,0.00009965659,0.000038692848,0.000100864396,0.9374568,0.0060710907,0.0014288911,0.0010466041,0.000051474108],"about_ca_topic_score_codex":0.033625472,"about_ca_topic_score_gemma":0.022918414,"teacher_disagreement_score":0.033625472,"about_ca_system_score_codex":0.001062359,"about_ca_system_score_gemma":0.0010059936,"threshold_uncertainty_score":0.06685954},"labels":[],"label_agreement":null},{"id":"W1932688471","doi":"10.1029/2012gl052922","title":"Small‐scale methane dispersion modelling for possible plume sources on the surface of Mars","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Winnipeg; University of Toronto","funders":"","keywords":"Mars Exploration Program; Atmosphere of Mars; Methane; Plume; Martian; Environmental science; Atmosphere (unit); Astrobiology; Geology; Martian surface; Atmospheric sciences; Atmospheric methane; Meteorology; Physics","score_opus":0.09079624159444585,"score_gpt":0.30122004412563047,"score_spread":0.21042380253118462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1932688471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873045,0.00013736256,0.011071745,0.00013749389,0.00000481408,0.000018500688,0.00014527541,0.00010927399,0.0010710802],"genre_scores_gemma":[0.9968129,0.00005116785,0.002610698,0.0000048335123,0.000003545884,0.000011096915,0.000110069,0.0000148085,0.00038100514],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999466,0.000017398765,0.0000029510968,0.000011107962,0.000008400425,0.000013611499],"domain_scores_gemma":[0.9996582,0.00021650616,0.000043187407,0.0000163036,0.00003620929,0.000029589371],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031313545,0.00049361086,0.00026508368,0.0006445466,0.0004415763,0.0006894758,0.00055320025,0.00088712975,0.0007406779],"category_scores_gemma":[0.00096969836,0.00029617897,0.0007605093,0.0003444407,0.00026162324,0.00045293913,0.0003641352,0.00040700645,0.000100495075],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006539501,0.000029194545,0.007289573,0.000011130652,0.000020999385,0.00006163862,0.00005192379,0.9879517,0.0018306262,0.0005699323,0.0000939581,0.0020240415],"study_design_scores_gemma":[0.000006633683,0.000008112317,0.0013055406,0.0000017140061,0.000002837103,0.0000050052563,0.000013994854,0.99828774,0.00017099341,0.00013275695,0.000060802184,0.000003927517],"about_ca_topic_score_codex":0.04864614,"about_ca_topic_score_gemma":0.02158497,"teacher_disagreement_score":0.04864614,"about_ca_system_score_codex":0.0007241509,"about_ca_system_score_gemma":0.0004692269,"threshold_uncertainty_score":0.096726},"labels":[],"label_agreement":null},{"id":"W1932951172","doi":"10.1029/2011gl048277","title":"The free librations of Mercury and the size of its inner core","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Inner core; Libration (molecule); Mantle (geology); Outer core; Core–mantle boundary; Physics; Mercury (programming language); Geophysics; Geology; Geodesy; Geometry","score_opus":0.04521265243572541,"score_gpt":0.27907925919050675,"score_spread":0.23386660675478133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1932951172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9658229,0.0025941718,0.016409937,0.00030760886,0.00004694518,0.000009431278,0.0007785789,0.00019700114,0.013833426],"genre_scores_gemma":[0.9974687,0.00025953347,0.0012399681,0.000016517548,0.000016999491,0.000005527939,0.0003062625,0.00003495495,0.00065154553],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993956,0.000008202822,0.000003406955,0.000028787788,0.00000920882,0.000010801426],"domain_scores_gemma":[0.99969256,0.00008723173,0.00010556892,0.00004448313,0.000034780114,0.000035372897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018441564,0.00017721106,0.00015653216,0.00048607442,0.00034694388,0.00040192754,0.0004135922,0.0003271589,0.0021715704],"category_scores_gemma":[0.0013186114,0.00024537765,0.00017527415,0.00026031322,0.0003513048,0.0005603427,0.00053382025,0.00022626949,0.00039109177],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018520097,0.000086247645,0.43626192,0.0008835263,0.0005175441,0.0006679442,0.0009488115,0.07028259,0.2764754,0.040453207,0.008719196,0.1628517],"study_design_scores_gemma":[0.00005579463,0.00025587637,0.80909276,0.00007721527,0.0002478013,0.00124781,0.00023051124,0.074397095,0.07059854,0.023606151,0.020043233,0.00014715665],"about_ca_topic_score_codex":0.0014719372,"about_ca_topic_score_gemma":0.0018526202,"teacher_disagreement_score":0.0021715704,"about_ca_system_score_codex":0.00042046703,"about_ca_system_score_gemma":0.00013767602,"threshold_uncertainty_score":0.0072646737},"labels":[],"label_agreement":null},{"id":"W1938867268","doi":"10.1029/2009gl041523","title":"Simulating observed boundary layer clouds on Mars","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Mars Exploration Program; Water vapor; Diurnal cycle; Atmospheric sciences; Planetary boundary layer; Precipitation; Environmental science; Daytime; Lidar; Boundary layer; Water cycle; Geology; Meteorology; Astrobiology; Physics; Remote sensing; Mechanics","score_opus":0.07753703298538495,"score_gpt":0.32906521773605374,"score_spread":0.2515281847506688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1938867268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9892586,0.00011853622,0.0057774596,0.00020432255,0.000057259018,0.00006342355,0.001135911,0.00045284315,0.002931586],"genre_scores_gemma":[0.9938892,0.000051700452,0.004624176,0.00003730718,0.000015386397,0.000057124562,0.00071145874,0.00003954232,0.0005740305],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997758,0.00006862529,0.000011688666,0.00004200909,0.000040075454,0.00006184655],"domain_scores_gemma":[0.9992791,0.00031584373,0.000060861577,0.00006744856,0.00012122206,0.00015552771],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047221413,0.0006872428,0.00075941323,0.00047068708,0.00089732744,0.0009564128,0.0016465936,0.0016659471,0.0026318128],"category_scores_gemma":[0.0013797284,0.0004993351,0.0009543093,0.0005845797,0.0005360837,0.00069364347,0.0006277936,0.0009988577,0.0001888313],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011032729,0.00008698449,0.0049218666,0.000022847975,0.000037076836,0.00009866067,0.00004210244,0.9912395,0.0013157711,0.00054567994,0.00034807756,0.001231172],"study_design_scores_gemma":[0.00004837582,0.000027340055,0.0011146874,0.000001812007,0.000006477917,0.00000710855,0.000017292361,0.9981646,0.00033054204,0.000102275946,0.00017390243,0.000005510965],"about_ca_topic_score_codex":0.04320461,"about_ca_topic_score_gemma":0.017830767,"teacher_disagreement_score":0.04320461,"about_ca_system_score_codex":0.001720544,"about_ca_system_score_gemma":0.0010699665,"threshold_uncertainty_score":0.08590627},"labels":[],"label_agreement":null},{"id":"W1940303797","doi":"10.1002/2015gl065727","title":"Iron supply and demand in an Antarctic shelf ecosystem","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Oceanography; Environmental science; Photic zone; Phytoplankton; Circumpolar star; Lead (geology); Productivity; New production; Marine ecosystem; Ecosystem; Continental shelf; Primary productivity; Satellite; Sea ice; Iron fertilization; Geology; Climatology; Ecology","score_opus":0.035037410656386915,"score_gpt":0.27377619289495647,"score_spread":0.23873878223856956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1940303797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924064,0.000015956954,0.00007924902,0.000043902033,8.4387887e-7,0.0000010969184,0.00019569551,0.0000026328937,0.00041995617],"genre_scores_gemma":[0.999445,0.000027573758,0.00016399329,0.000013560887,0.0000017848679,0.0000022291558,0.00018373945,0.0000018986198,0.00016008518],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999423,0.000015636102,0.000004822599,0.000012625386,0.000013998745,0.000010742139],"domain_scores_gemma":[0.9997402,0.000083295454,0.000043824522,0.00001832762,0.000061024006,0.000053269756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002158074,0.00018638032,0.00019677314,0.00052773516,0.00036615733,0.0008641042,0.00024060707,0.00036635585,0.0009916088],"category_scores_gemma":[0.000669914,0.0002172592,0.00021476566,0.0007037676,0.0002680309,0.0005141635,0.00037381877,0.000148432,0.00015399334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019429339,0.00005482639,0.93540937,0.000055815257,0.0001665972,0.00055257685,0.0003996158,0.041663904,0.011830105,0.0010561186,0.00059297914,0.008023742],"study_design_scores_gemma":[0.000026585189,0.00006392069,0.85895026,0.000012967761,0.000054271815,0.00018877261,0.0010919439,0.13554193,0.0012297587,0.0015827253,0.0012328005,0.000023949373],"about_ca_topic_score_codex":0.02928758,"about_ca_topic_score_gemma":0.04100168,"teacher_disagreement_score":0.02928758,"about_ca_system_score_codex":0.0010885784,"about_ca_system_score_gemma":0.0005552841,"threshold_uncertainty_score":0.058234215},"labels":[],"label_agreement":null},{"id":"W1941403918","doi":"10.1002/2015gl063216","title":"Modification of turbulent dissipation rates by a deep Southern Ocean eddy","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Mesoscale meteorology; Geology; Dissipation; Baroclinity; Eddy diffusion; Internal wave; Stratification (seeds); Geophysics; Turbulence; Mechanics; Hydrography; Geostrophic wind; Turbulence kinetic energy; Meteorology; Atmospheric sciences; Climatology; Physics; Oceanography","score_opus":0.04063557357420058,"score_gpt":0.2930537431088168,"score_spread":0.25241816953461627,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1941403918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99975926,0.000009907596,0.00009402074,0.0000037444456,3.7535932e-7,3.804147e-7,0.000020496916,0.0000042515962,0.00010765734],"genre_scores_gemma":[0.99986243,0.000005620769,0.00005015134,0.0000016492755,4.995453e-7,4.607516e-7,0.0000310278,0.0000012364856,0.000046961068],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995553,0.0000064912233,0.0000032379803,0.00001187118,0.000012809844,0.000010130416],"domain_scores_gemma":[0.99979836,0.000058447884,0.000058962218,0.000025249485,0.000024654186,0.000034354103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015363107,0.00014108286,0.00011988426,0.0001915392,0.000093318675,0.0002906922,0.000064608896,0.00009405231,0.00039094954],"category_scores_gemma":[0.0004960532,0.00015251873,0.000114565504,0.00012140046,0.00019260947,0.00014122552,0.00022382702,0.00010683152,0.000056736626],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048915297,0.000049192684,0.42020178,0.00003213398,0.00006448361,0.00013838003,0.00022055276,0.004520652,0.56517404,0.00032512954,0.000080804086,0.008703636],"study_design_scores_gemma":[0.000010786824,0.00010653942,0.979349,0.0000025537547,0.000013666482,0.000033562468,0.00004883283,0.0066991607,0.013520725,0.00006952767,0.00014032912,0.0000054021752],"about_ca_topic_score_codex":0.0018345532,"about_ca_topic_score_gemma":0.0018533998,"teacher_disagreement_score":0.0018345532,"about_ca_system_score_codex":0.00019452858,"about_ca_system_score_gemma":0.00008230213,"threshold_uncertainty_score":0.0036478043},"labels":[],"label_agreement":null},{"id":"W1941837589","doi":"10.1029/2012gl053283","title":"Understanding Atlantic multi‐decadal variability prediction skill","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Conselho Nacional de Desenvolvimento Científico e Tecnológico","keywords":"Ocean gyre; Initialization; Forcing (mathematics); Climatology; Environmental science; Forecast skill; Radiative forcing; Subtropics; Oceanography; Geology; Climate change; Computer science","score_opus":0.15213566499721606,"score_gpt":0.3383035241867617,"score_spread":0.18616785918954562,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1941837589","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99478793,0.00007709758,0.0032923608,0.00012207111,0.000007596026,0.0000043065643,0.00028066785,0.000051038252,0.0013769504],"genre_scores_gemma":[0.9990477,0.0000276825,0.00060365564,0.000009603711,0.0000034067937,0.0000016664413,0.00020340664,0.0000046332125,0.0000981706],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998909,0.000021480257,0.000010750258,0.00003862175,0.000019796222,0.000018438246],"domain_scores_gemma":[0.9981552,0.0010997762,0.0002553038,0.00016567748,0.0002550843,0.00006891188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084383995,0.00017904861,0.00013319806,0.00029993616,0.00009543211,0.00082216895,0.00018691922,0.0003006106,0.0005995138],"category_scores_gemma":[0.005821842,0.0001323777,0.00019354839,0.0002100056,0.0001270611,0.0010473342,0.00036812402,0.00037603301,0.00010846963],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021044389,0.000068075155,0.77514046,0.000040366172,0.00012425728,0.000082090664,0.0003745477,0.16510232,0.009152097,0.002411385,0.000783206,0.046510726],"study_design_scores_gemma":[0.000011471675,0.000049545935,0.5272504,0.000014515474,0.000034107677,0.000025217078,0.00013929546,0.46764258,0.0031014327,0.0012465704,0.00046552648,0.000019366787],"about_ca_topic_score_codex":0.0131933885,"about_ca_topic_score_gemma":0.011751001,"teacher_disagreement_score":0.0131933885,"about_ca_system_score_codex":0.0003729286,"about_ca_system_score_gemma":0.00032421696,"threshold_uncertainty_score":0.026233196},"labels":[],"label_agreement":null},{"id":"W1942549508","doi":"10.1002/grl.50306","title":"Extreme storms and changes in particulate and dissolved organic carbon in runoff: Entering uncharted waters?","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":137,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Science and Technology Facilities Council; National Science Foundation","keywords":"Environmental science; Dissolved organic carbon; Biota; Surface runoff; Particulates; Aquatic ecosystem; Storm; Ecosystem; Precipitation; Hydrology (agriculture); Particulate organic carbon; Climate change; Environmental chemistry; Oceanography; Ecology; Geology; Phytoplankton; Meteorology; Geography; Chemistry; Biology","score_opus":0.024879272855228226,"score_gpt":0.24449972482946197,"score_spread":0.21962045197423374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1942549508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996755,0.000030001185,0.000032151507,0.000021811846,0.0000010870274,0.0000011485877,0.000055003355,0.0000012726491,0.00018210919],"genre_scores_gemma":[0.9996755,0.000045999117,0.00005076206,0.000015120501,0.0000071851864,0.0000010553409,0.00009991987,0.0000011848556,0.000103312625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998889,0.000018001918,0.000007947793,0.000020843176,0.000024758801,0.000039454277],"domain_scores_gemma":[0.99973947,0.00004448306,0.00010091546,0.0000096113135,0.000041378786,0.000064108404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023013998,0.00012942406,0.00026079244,0.00018344038,0.00033496253,0.00079291494,0.00011030268,0.00027080558,0.0006343748],"category_scores_gemma":[0.0005079069,0.000114638395,0.00013288713,0.00030548402,0.00036165572,0.00040759312,0.00031444547,0.0002723711,0.00008386222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044522778,0.00008142261,0.974609,0.000017711762,0.000033346816,0.00045128053,0.0002293427,0.0005402591,0.020115549,0.00010587413,0.00011801587,0.0032528813],"study_design_scores_gemma":[0.0000053968124,0.00008882786,0.99718446,0.0000030827212,0.0000067865903,0.000098092976,0.00042348777,0.00041339744,0.0013928814,0.000096775846,0.00028320547,0.0000034958605],"about_ca_topic_score_codex":0.004228432,"about_ca_topic_score_gemma":0.0073420065,"teacher_disagreement_score":0.004228432,"about_ca_system_score_codex":0.00038765755,"about_ca_system_score_gemma":0.00022540925,"threshold_uncertainty_score":0.008407652},"labels":[],"label_agreement":null},{"id":"W1943471202","doi":"10.1002/2014gl061047","title":"Recent Arctic Ocean sea ice loss triggers novel fall phytoplankton blooms","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":397,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski; Université Laval","funders":"National Oceanic and Atmospheric Administration; Canada Research Chairs; ArcticNet; Canada Excellence Research Chairs, Government of Canada; National Aeronautics and Space Administration","keywords":"Arctic; Oceanography; Environmental science; Phytoplankton; Sea ice; Marine ecosystem; Stratification (seeds); Arctic geoengineering; Arctic sea ice decline; Arctic ice pack; Ecosystem; Drift ice; Geology; Nutrient; Ecology; Biology","score_opus":0.024783195981215506,"score_gpt":0.26309439326293427,"score_spread":0.23831119728171876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1943471202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979856,0.00020072187,0.00021940537,0.000101556696,0.000032542845,0.000007671126,0.0005312487,0.000029332688,0.00089175784],"genre_scores_gemma":[0.9976362,0.00012495797,0.00022157724,0.00010973002,0.000028167698,0.000013677581,0.0010753558,0.000006709814,0.00078361895],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999206,0.0000054829143,0.000004869476,0.00001884555,0.000020342572,0.000029817436],"domain_scores_gemma":[0.9997701,0.000031849784,0.000060206356,0.000018910798,0.000043524444,0.000075459175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001863732,0.00017753054,0.00035991173,0.00033579674,0.00041259493,0.00062867766,0.000116040435,0.00031787134,0.0018029681],"category_scores_gemma":[0.00026860062,0.00011163627,0.00018519361,0.00023015733,0.00021552507,0.00012187927,0.00040222247,0.0004328982,0.0004157539],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0037066685,0.0003883244,0.48130512,0.00012958214,0.000095402735,0.0017514073,0.0005221443,0.00040645915,0.4937804,0.00022592697,0.002779767,0.014908871],"study_design_scores_gemma":[0.000013463413,0.00018918613,0.98637563,0.0000076217298,0.00001074378,0.00039755576,0.0002801189,0.00047327625,0.010541299,0.0001324088,0.0015720328,0.000006774021],"about_ca_topic_score_codex":0.003437256,"about_ca_topic_score_gemma":0.006058564,"teacher_disagreement_score":0.003437256,"about_ca_system_score_codex":0.0003772653,"about_ca_system_score_gemma":0.00020913238,"threshold_uncertainty_score":0.006834507},"labels":[],"label_agreement":null},{"id":"W1944168514","doi":"10.1029/2007gl031074","title":"Warming and salinification of intermediate and deep waters in the Irminger Sea and Iceland Basin in 1997–2006","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Structural basin; Geology; Salinity; Climatology; Water mass; Environmental science; Paleontology","score_opus":0.01903554059246946,"score_gpt":0.27122615042459514,"score_spread":0.25219060983212566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1944168514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99917644,0.000080448786,0.000012402906,0.000018646278,0.0000019045066,0.0000013211445,0.00040796818,0.0000027867031,0.00029819083],"genre_scores_gemma":[0.99794656,0.00011402112,0.0000782146,0.000029249553,0.0000063863904,0.0000049199257,0.0015605476,0.0000020735033,0.0002580308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999101,0.00000901594,0.000012651013,0.000028284101,0.00001461019,0.000025231775],"domain_scores_gemma":[0.99973804,0.000019574616,0.00013243577,0.000020545544,0.00005075313,0.000038639275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037761792,0.00021212873,0.0001867512,0.0007871902,0.00026772547,0.00042801196,0.00019662442,0.00019712937,0.00057430915],"category_scores_gemma":[0.00041911096,0.00008475235,0.0002161406,0.0008481956,0.00022748562,0.00030526947,0.0004281952,0.00016440306,0.000103067134],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024474223,0.000029694933,0.9854534,0.000045624398,0.00010210472,0.00016932875,0.0006013651,0.00091725355,0.0032531994,0.000096390584,0.00047852943,0.008608463],"study_design_scores_gemma":[0.0000010971927,0.0000109181365,0.99917054,0.0000034971554,0.000008360766,0.000018336772,0.00010640496,0.00009050422,0.00020308372,0.0000052006085,0.00038034192,0.0000018795163],"about_ca_topic_score_codex":0.035874445,"about_ca_topic_score_gemma":0.06419076,"teacher_disagreement_score":0.035874445,"about_ca_system_score_codex":0.00086115993,"about_ca_system_score_gemma":0.00050878635,"threshold_uncertainty_score":0.07133126},"labels":[],"label_agreement":null},{"id":"W1944846275","doi":"10.1002/2015gl064106","title":"The isotopic composition of the Laurentide Ice Sheet and fossil groundwater","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Saskatchewan","funders":"","keywords":"Ice sheet; Meltwater; Geology; Groundwater; Greenland ice sheet; Glacial period; Ice-sheet model; Pleistocene; Hydrology (agriculture); Ice stream; Geomorphology; Cryosphere; Climatology; Sea ice; Paleontology","score_opus":0.052735489909850365,"score_gpt":0.2808102120646206,"score_spread":0.22807472215477023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1944846275","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979857,0.00012811075,0.000056739722,0.000015527658,0.000002328159,8.969897e-7,0.00034969568,0.000004351922,0.0014567007],"genre_scores_gemma":[0.99897975,0.00009602293,0.00013663863,0.000010362231,0.0000024550754,0.000001476113,0.00032532157,0.0000023864447,0.00044548744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999577,0.0000037135533,0.0000022989425,0.000015198627,0.000011550437,0.000009594653],"domain_scores_gemma":[0.99991167,0.000012854106,0.00003095018,0.000003877995,0.000027011014,0.0000135896735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009772062,0.00012909116,0.00008734327,0.0006220005,0.00022758826,0.000405344,0.00010685251,0.0000824653,0.00062253955],"category_scores_gemma":[0.0002132073,0.00006772309,0.00006683095,0.00039081916,0.00020976606,0.0002142472,0.00021111341,0.000065910695,0.00008442993],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019455291,0.000017588103,0.9348757,0.000043543634,0.000040164115,0.00015365529,0.00034985208,0.0012613864,0.044686455,0.00026680986,0.00028897624,0.017821305],"study_design_scores_gemma":[0.0000036119714,0.000022662918,0.99070215,0.000012289659,0.000010421428,0.00007596338,0.00027832607,0.0016991032,0.0051234905,0.00007484111,0.001990792,0.0000062864506],"about_ca_topic_score_codex":0.046607297,"about_ca_topic_score_gemma":0.09432103,"teacher_disagreement_score":0.046607297,"about_ca_system_score_codex":0.00094941247,"about_ca_system_score_gemma":0.00029085606,"threshold_uncertainty_score":0.09267199},"labels":[],"label_agreement":null},{"id":"W1944913231","doi":"10.1029/2010gl043733","title":"Widespread Amazon forest tree mortality from a single cross‐basin squall line event","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Squall line; Storm; Environmental science; Amazon rainforest; Precipitation; Climate change; Climatology; Deforestation (computer science); Atmospheric sciences; Geography; Meteorology; Geology; Ecology; Oceanography; Biology","score_opus":0.04576777939013737,"score_gpt":0.33265463896291103,"score_spread":0.28688685957277366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1944913231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995927,0.00002486221,0.000097304954,0.000015546788,0.0000012165137,0.000002074509,0.0000436191,0.0000055920527,0.00021709921],"genre_scores_gemma":[0.9998808,0.000013628151,0.000027933484,0.000005459144,0.0000015451357,6.1492733e-7,0.000033478744,4.626706e-7,0.000036134243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999223,0.000012543548,0.0000064762544,0.000022322174,0.000017177503,0.000019246037],"domain_scores_gemma":[0.9996263,0.00004727622,0.00019017824,0.000036095185,0.00004097058,0.000059195394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015415026,0.00014664745,0.00014675963,0.00016603088,0.00022446559,0.00015933553,0.00012010258,0.0001501117,0.0007831461],"category_scores_gemma":[0.00043207116,0.000042186744,0.00012303716,0.00008582205,0.00013748293,0.00014439873,0.00025675516,0.00014439611,0.00009492738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026558788,0.00007387076,0.9360931,0.000030669118,0.00010904664,0.000462663,0.00023882801,0.0009925804,0.046729196,0.000078706435,0.00023434988,0.014691544],"study_design_scores_gemma":[0.0000045022557,0.00014474001,0.9966517,0.0000029582627,0.000014273616,0.00029024124,0.00007972444,0.000984679,0.0016416468,0.000054533044,0.00012798126,0.0000031232196],"about_ca_topic_score_codex":0.0039199963,"about_ca_topic_score_gemma":0.010082127,"teacher_disagreement_score":0.0039199963,"about_ca_system_score_codex":0.0002239929,"about_ca_system_score_gemma":0.000096171905,"threshold_uncertainty_score":0.0077943206},"labels":[],"label_agreement":null},{"id":"W1945829080","doi":"10.1029/2012gl052261","title":"Quantifying the relevance of atmospheric blocking for co‐located temperature extremes in the Northern Hemisphere on (sub‐)daily time scales","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":421,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Blocking (statistics); Northern Hemisphere; Climatology; Atmospheric sciences; Atmospheric circulation; Forcing (mathematics); Latitude; Atmospheric temperature; Middle latitudes; Geology","score_opus":0.05230203701326302,"score_gpt":0.31757831708067935,"score_spread":0.2652762800674163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1945829080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975587,0.00020959086,0.0011594892,0.00003199824,0.000005536363,0.0000035224907,0.00013671831,0.000012014454,0.0008823575],"genre_scores_gemma":[0.99960476,0.000056805813,0.00017679228,0.000002815877,0.00000771558,0.0000012188253,0.00010907064,0.0000032115263,0.000037500402],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998418,0.00005912938,0.000009688187,0.000035139507,0.000022259666,0.000031960393],"domain_scores_gemma":[0.9978787,0.0012690981,0.0005339983,0.00013303426,0.000074046286,0.00011125792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052682444,0.00017009203,0.00023045177,0.00026746775,0.00024697464,0.00049042475,0.00018497973,0.00024699725,0.00073410396],"category_scores_gemma":[0.0025365248,0.000088547706,0.00029840507,0.0006163183,0.00022704879,0.0005502011,0.00030679425,0.00027053666,0.000067179506],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004018134,0.000046099132,0.9342385,0.00007607091,0.00023469821,0.0001872532,0.00022199599,0.03746881,0.013976019,0.00086136523,0.00024770707,0.012039748],"study_design_scores_gemma":[0.0000047762856,0.000041043313,0.9755781,0.0000042668744,0.00006480752,0.00004984119,0.00009694438,0.022571048,0.0007355352,0.00053965155,0.0003042438,0.0000096539125],"about_ca_topic_score_codex":0.009726519,"about_ca_topic_score_gemma":0.01330532,"teacher_disagreement_score":0.009726519,"about_ca_system_score_codex":0.00028989263,"about_ca_system_score_gemma":0.00026003888,"threshold_uncertainty_score":0.0193398},"labels":[],"label_agreement":null},{"id":"W1946951480","doi":"10.1029/2011gl047633","title":"Infrasonic detection of a near-Earth object impact over Indonesia on 8 October 2009","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Infrasound; Explosive material; Seismology; Geology; Range (aeronautics); Environmental science; Meteorology; Physics; Geography; Acoustics; Aerospace engineering","score_opus":0.03321586680856149,"score_gpt":0.28513204841183337,"score_spread":0.2519161816032719,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1946951480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975988,0.000030340545,0.00026255715,0.000022417078,0.0000053834347,0.000005229785,0.00045826664,0.000017363594,0.001599597],"genre_scores_gemma":[0.9984763,0.000028592363,0.00020742208,0.000007322818,0.000009008405,0.0000025902127,0.0009118532,0.0000044842104,0.00035239026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998963,0.0000061345354,0.0000058074625,0.000020850386,0.000037509268,0.00003329659],"domain_scores_gemma":[0.99976987,0.000025738087,0.000096194235,0.00001613534,0.00004143367,0.00005055321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009239073,0.0002358948,0.000170081,0.00077258673,0.00028149868,0.00030203033,0.0002482786,0.00024658127,0.0011688443],"category_scores_gemma":[0.0003288243,0.000080841724,0.00009993145,0.0005999334,0.00018855638,0.0001976104,0.00044132528,0.0002782659,0.00027822904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000612858,0.00017452748,0.9012963,0.00007265105,0.00010071047,0.0041708928,0.00047946314,0.003235674,0.050529093,0.0003462502,0.0015099117,0.037471745],"study_design_scores_gemma":[0.000003909593,0.000065965905,0.99417555,0.000005470259,0.000020306674,0.00046420618,0.00018249796,0.0021786743,0.0022393994,0.000036866917,0.00061938097,0.00000775735],"about_ca_topic_score_codex":0.0061139804,"about_ca_topic_score_gemma":0.013214209,"teacher_disagreement_score":0.0061139804,"about_ca_system_score_codex":0.00020202962,"about_ca_system_score_gemma":0.0001256514,"threshold_uncertainty_score":0.012156785},"labels":[],"label_agreement":null},{"id":"W1948003952","doi":"10.1029/2011gl050226","title":"Improved constraints on 21st‐century warming derived using 160 years of temperature observations","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Greenhouse gas; Climatology; Climate change; Global warming; Atmospheric sciences; Climate model; Representative Concentration Pathways; Geology","score_opus":0.1002542700162763,"score_gpt":0.3099562303529074,"score_spread":0.20970196033663113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948003952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8104542,0.0037765098,0.14668956,0.00092102366,0.0003547229,0.000036274552,0.011745824,0.0005745201,0.025447255],"genre_scores_gemma":[0.9765529,0.0006340019,0.014567928,0.00015922754,0.00006872951,0.0000441438,0.0070187827,0.00015077819,0.0008035543],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9993505,0.00018151307,0.00006151877,0.00022512181,0.000103096,0.00007839652],"domain_scores_gemma":[0.9977628,0.0009112837,0.00035280397,0.0004915555,0.00040373715,0.00007792817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021790317,0.000964832,0.00065567385,0.0010821378,0.00065556105,0.0011881635,0.0007634516,0.000588251,0.002781905],"category_scores_gemma":[0.006342401,0.0005301825,0.0013554352,0.001425264,0.00037910434,0.0020518075,0.0012443732,0.00092673575,0.0004895362],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004180202,0.00008593867,0.12980717,0.0003437763,0.0012731801,0.00013841329,0.00017708394,0.8008457,0.008774451,0.016920578,0.0028538231,0.03836183],"study_design_scores_gemma":[0.00015184862,0.00015737368,0.33559018,0.00030485494,0.00040072863,0.00014174057,0.00030280117,0.5703592,0.015829142,0.039557222,0.03683635,0.0003685396],"about_ca_topic_score_codex":0.038846117,"about_ca_topic_score_gemma":0.053426493,"teacher_disagreement_score":0.038846117,"about_ca_system_score_codex":0.001421816,"about_ca_system_score_gemma":0.0014152378,"threshold_uncertainty_score":0.07723999},"labels":[],"label_agreement":null},{"id":"W1948827418","doi":"10.1029/2011gl047735","title":"Distribution and trends in Arctic sea ice age through spring 2011","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":678,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Arctic ice pack; Arctic sea ice decline; Oceanography; Antarctic sea ice; Drift ice; Arctic; Cryosphere; Fast ice; Climatology; Canada Basin; Geology; Environmental science; Physical geography; Geography","score_opus":0.04902695545921107,"score_gpt":0.27890893100423675,"score_spread":0.22988197554502568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1948827418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9737613,0.0014535417,0.00022989685,0.00024431653,0.000040557847,0.000010991932,0.019607993,0.00005590565,0.004595581],"genre_scores_gemma":[0.9724568,0.0013240636,0.0006173384,0.00010565545,0.000049907623,0.000025800287,0.02239605,0.000021909329,0.0030023442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998055,0.000022460623,0.0000325956,0.00005568789,0.000038678198,0.000045053326],"domain_scores_gemma":[0.99868137,0.0001281975,0.00045453815,0.00005873374,0.00049985806,0.0001772978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043210658,0.000168004,0.00013974316,0.0019909372,0.0003101344,0.00044699214,0.00023823805,0.00021918108,0.0015799542],"category_scores_gemma":[0.0012835206,0.00010428669,0.00024488452,0.0015486431,0.00010744399,0.0003830129,0.0002962911,0.00026085085,0.00080786645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013100514,0.000021182352,0.98323476,0.000050761944,0.000059434802,0.00004562351,0.00025834318,0.00017080441,0.00065597094,0.00010307709,0.002371812,0.012897361],"study_design_scores_gemma":[0.0000012298672,0.000022649916,0.9976312,0.000012928088,0.000006155585,0.00007789589,0.000112024485,0.00013391295,0.00007640631,0.000011249742,0.0019111079,0.000003122466],"about_ca_topic_score_codex":0.029310284,"about_ca_topic_score_gemma":0.06616883,"teacher_disagreement_score":0.029310284,"about_ca_system_score_codex":0.00041233207,"about_ca_system_score_gemma":0.00040043375,"threshold_uncertainty_score":0.058279335},"labels":[],"label_agreement":null},{"id":"W1949314878","doi":"10.1002/grl.50310","title":"Eroding dynamic topography","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Institute for Advanced Research","keywords":"Subaerial; Geology; Ocean surface topography; Mantle (geology); Downwelling; Sedimentary rock; Upwelling; Geomorphology; Fluvial; Geophysics; Paleontology; Structural basin; Oceanography","score_opus":0.0306353516950081,"score_gpt":0.2825138250641117,"score_spread":0.25187847336910363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1949314878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920427,0.00009293337,0.0033101074,0.000064599255,0.0000056354224,0.0000037374687,0.000080558246,0.00005152935,0.0043482147],"genre_scores_gemma":[0.9984856,0.000062503525,0.00036431014,0.000011196309,0.000003935818,0.0000013892785,0.00004752896,0.000009686936,0.0010139268],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999399,0.0000047295625,0.000003159715,0.000017478127,0.000011929612,0.00002276104],"domain_scores_gemma":[0.9997638,0.000031925123,0.000069200505,0.00006117287,0.000054887634,0.000018921213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000072257026,0.0001380682,0.0001283913,0.00034161226,0.00012649545,0.00048413512,0.00017385418,0.00018570924,0.0016956822],"category_scores_gemma":[0.0005541896,0.00012863333,0.00009930696,0.0003465609,0.0002814152,0.00034138077,0.00046280955,0.00020377875,0.00021842628],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021643985,0.000056628956,0.29992732,0.00008531022,0.00008241154,0.0013790634,0.0010624788,0.011937983,0.5241436,0.0075314017,0.0015172388,0.15206018],"study_design_scores_gemma":[0.000015458165,0.00008817013,0.96330285,0.00001259681,0.000031791144,0.0011553229,0.0004431805,0.0115349535,0.015107734,0.0017278116,0.00655926,0.000020979443],"about_ca_topic_score_codex":0.0025280952,"about_ca_topic_score_gemma":0.0026249853,"teacher_disagreement_score":0.0025280952,"about_ca_system_score_codex":0.00022802329,"about_ca_system_score_gemma":0.00013167082,"threshold_uncertainty_score":0.0056726336},"labels":[],"label_agreement":null},{"id":"W1949554075","doi":"10.1002/2015gl065018","title":"Mantle‐driven uplift of Hangai Dome: New seismic constraints from adjoint tomography","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Upwelling; Mantle (geology); Seismic tomography; Lithosphere; Seismology; Geophysics; Mantle wedge; Partial melting; Crust; Petrology; Tectonics","score_opus":0.04950039734614027,"score_gpt":0.28427260187511155,"score_spread":0.2347722045289713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1949554075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99659973,0.00006020071,0.0019064975,0.00007176826,0.0000030653573,0.0000031630846,0.00019471408,0.000024268878,0.0011365769],"genre_scores_gemma":[0.9994437,0.000023649314,0.0003593412,0.0000052873884,0.0000028720065,0.0000012838358,0.00009870801,0.000002177556,0.00006295337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.000007533081,0.0000033720205,0.00001237566,0.000008287464,0.000011177407],"domain_scores_gemma":[0.99976987,0.00006342057,0.000058824513,0.000034275305,0.000043830423,0.000029764195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015171501,0.00018732119,0.0001285551,0.0007680942,0.00017293345,0.0006127888,0.00017162063,0.00023088395,0.0008735283],"category_scores_gemma":[0.0007667475,0.00016108788,0.00010048961,0.00060618634,0.00031383778,0.00032607777,0.0005511128,0.00019154705,0.00008285091],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029466674,0.000050179886,0.78172696,0.000092535185,0.000080308455,0.0012800691,0.001081405,0.0077302735,0.16162834,0.0031639219,0.0003717241,0.042499695],"study_design_scores_gemma":[0.000017057126,0.00002804908,0.95946395,0.000018194014,0.00003665809,0.0002905894,0.00060218386,0.0332926,0.003918608,0.0013339191,0.00097514346,0.000022956045],"about_ca_topic_score_codex":0.004629217,"about_ca_topic_score_gemma":0.008300979,"teacher_disagreement_score":0.004629217,"about_ca_system_score_codex":0.00015866784,"about_ca_system_score_gemma":0.00017035594,"threshold_uncertainty_score":0.0092045665},"labels":[],"label_agreement":null},{"id":"W1949897725","doi":"10.1029/2009gl041849","title":"Frost‐ring chronologies as dendroclimatic proxies of boreal environments","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Frost (temperature); Boreal; Taiga; Climate change; Growing season; Dendrochronology; Woodland; Climatology; Environmental science; Chronology; Physical geography; Black spruce; Geology; Geography; Ecology; Forestry; Biology; Meteorology; Paleontology","score_opus":0.030795769129376337,"score_gpt":0.29471211142452197,"score_spread":0.26391634229514566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1949897725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864586,0.00024276353,0.009604781,0.00001194491,0.000018265282,0.000044972694,0.0016480179,0.00016667432,0.001804012],"genre_scores_gemma":[0.98987913,0.000058547124,0.009014606,0.0000034387647,0.000008662261,0.000022673888,0.0008562502,0.000024438355,0.00013225469],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998343,0.00006061224,0.000014205595,0.000047001682,0.00002211629,0.000021724893],"domain_scores_gemma":[0.999358,0.00018978845,0.00018992188,0.00008911218,0.000092891525,0.00008033497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009185064,0.00032773704,0.00014927013,0.0013593024,0.0002512953,0.0005385664,0.00013270478,0.00012985179,0.00056871143],"category_scores_gemma":[0.0013193343,0.0001681803,0.00019191434,0.0009957227,0.00011994075,0.0003424991,0.00019874945,0.00020593475,0.00011195938],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003433566,0.000047806105,0.92337656,0.00006266029,0.0001457757,0.00008189654,0.0004410542,0.016150234,0.02124612,0.00076867134,0.00059644505,0.03673939],"study_design_scores_gemma":[0.000011296052,0.000051507395,0.98548836,0.000005921794,0.000027096556,0.00008725805,0.000108546046,0.011468335,0.0011478286,0.00017624696,0.0014151572,0.000012514937],"about_ca_topic_score_codex":0.0074052606,"about_ca_topic_score_gemma":0.029786538,"teacher_disagreement_score":0.0074052606,"about_ca_system_score_codex":0.00021416407,"about_ca_system_score_gemma":0.00018411853,"threshold_uncertainty_score":0.014724314},"labels":[],"label_agreement":null},{"id":"W1950127861","doi":"10.1029/2011gl046789","title":"Seasonal cycle of emissions of CO inferred from MOPITT profiles of CO: Sensitivity to pyroconvection and profile retrieval assumptions","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Environmental science; Troposphere; Atmospheric sciences; Biomass burning; Range (aeronautics); Climatology; Mixing ratio; Seasonality; Meteorology; Aerosol; Geography; Geology; Statistics","score_opus":0.028860815662255474,"score_gpt":0.2896236669965237,"score_spread":0.26076285133426824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1950127861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935088,0.000109327644,0.0034326145,0.00009714496,0.00000938758,0.000019673806,0.0017578278,0.000095523654,0.0009697104],"genre_scores_gemma":[0.9959662,0.0000513009,0.0019061033,0.000022494442,0.0000063428397,0.00000883359,0.0019399117,0.000028668832,0.00007028512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970883,0.00006037222,0.000023560286,0.00010475338,0.000067412475,0.00003497046],"domain_scores_gemma":[0.99867946,0.0005517556,0.00026601696,0.00022470969,0.00023010436,0.00004800795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000878609,0.00035811914,0.00022350585,0.00034017873,0.00030355743,0.00049933436,0.0005124745,0.0004802592,0.0003444461],"category_scores_gemma":[0.0039280835,0.0003517324,0.00037243436,0.0005172949,0.00025871338,0.0005953645,0.0003055181,0.00042792733,0.00011858493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005370712,0.00012745261,0.68447405,0.000101830614,0.0002950478,0.00021700197,0.00011327777,0.27258813,0.020115728,0.00042610808,0.0014248026,0.019579533],"study_design_scores_gemma":[0.000029959278,0.000049340637,0.5951709,0.000021964503,0.000050708702,0.000120190096,0.00003303658,0.39246285,0.011037597,0.00023204372,0.0007557895,0.000035610992],"about_ca_topic_score_codex":0.04325338,"about_ca_topic_score_gemma":0.0395446,"teacher_disagreement_score":0.04325338,"about_ca_system_score_codex":0.0007024799,"about_ca_system_score_gemma":0.00034090027,"threshold_uncertainty_score":0.086003244},"labels":[],"label_agreement":null},{"id":"W1950915280","doi":"10.1029/2012gl051002","title":"Summer thermal structure and anticyclonic circulation of Lake Erie","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; Center for Sponsored Coastal Ocean Research; National Water Research Institute","keywords":"Thermocline; Anticyclone; Geology; Oceanography; Ocean gyre; Hypolimnion; Ekman transport; Hydraulic jump; Potential vorticity; Climatology; Upwelling; Vorticity; Subtropics; Flow (mathematics); Fishery; Vortex; Geography","score_opus":0.025482677743183725,"score_gpt":0.289901606289041,"score_spread":0.26441892854585725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1950915280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99901116,0.00004847067,0.000020595084,0.000028013666,8.920767e-7,8.7547335e-7,0.00010772061,0.00000683768,0.00077550334],"genre_scores_gemma":[0.99920577,0.00005633378,0.000043237407,0.000017293849,0.0000039135325,0.0000028498966,0.00022320468,0.0000054290667,0.00044194004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.000008022587,0.0000040665404,0.0000143121215,0.00000867274,0.000025770592],"domain_scores_gemma":[0.9999145,0.0000062734275,0.00002892447,0.000005079146,0.000025031566,0.000020133617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009458132,0.00011127619,0.00020284012,0.0005613589,0.00027693543,0.00036063182,0.00010573372,0.00017145151,0.0011868163],"category_scores_gemma":[0.00019756178,0.00016202897,0.00012855252,0.0005047527,0.00019821235,0.0002436151,0.00041407172,0.00013120096,0.00023648977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053956825,0.0000665169,0.9486871,0.00005381886,0.000115253366,0.00031217662,0.0022484583,0.0008082656,0.03270895,0.00023883718,0.001219953,0.013001034],"study_design_scores_gemma":[0.0000033244007,0.000012532417,0.99913687,0.000002203275,0.0000047012613,0.0000184393,0.00015537142,0.00021580508,0.000084060026,0.000012075018,0.00035262774,0.000002088509],"about_ca_topic_score_codex":0.023956576,"about_ca_topic_score_gemma":0.05558629,"teacher_disagreement_score":0.023956576,"about_ca_system_score_codex":0.0005134847,"about_ca_system_score_gemma":0.00026873918,"threshold_uncertainty_score":0.047634244},"labels":[],"label_agreement":null},{"id":"W1951032585","doi":"10.1002/2014gl061677","title":"Steady‐state field‐aligned currents at Mercury","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Carnegie Institution of Washington; Johns Hopkins University; National Aeronautics and Space Administration","keywords":"Geophysics; Physics; Magnetic field; Magnetopause; Dusk; Electric field; Current density; Current (fluid); Planet; Conductance; Atmospheric sciences; Magnetosphere; Geology; Astrophysics; Astronomy; Condensed matter physics","score_opus":0.03415318353392833,"score_gpt":0.3122790516516707,"score_spread":0.27812586811774237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1951032585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962257,0.000031904503,0.00033675527,0.00005165886,0.000003572302,0.0000036978454,0.0002955857,0.000110062516,0.0029409335],"genre_scores_gemma":[0.99933213,0.00001176748,0.00012813382,0.0000051870347,0.0000026605398,0.0000020673683,0.00018233174,0.0000054248153,0.00033036456],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999565,0.0000035241185,0.0000012636809,0.000013091578,0.00001189432,0.000013713354],"domain_scores_gemma":[0.99991167,0.0000099731105,0.0000128279735,0.000009272869,0.00003641033,0.000019819074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008035736,0.00010581936,0.00014909302,0.0003072869,0.00038533667,0.00038377405,0.0002775066,0.00018290384,0.0018018099],"category_scores_gemma":[0.00029339353,0.00008856088,0.00011955388,0.00027282175,0.00030156135,0.0003167928,0.00031685954,0.00016347281,0.00029170554],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019262818,0.00043804233,0.26745194,0.0001829513,0.00022959954,0.0013806974,0.0022354715,0.026467517,0.64095,0.007524037,0.005271154,0.045942247],"study_design_scores_gemma":[0.00021858154,0.0009162877,0.77033114,0.000030492687,0.0001022713,0.00042522434,0.0010647167,0.08279488,0.13061681,0.0051199817,0.008301307,0.00007826664],"about_ca_topic_score_codex":0.007206952,"about_ca_topic_score_gemma":0.0043849736,"teacher_disagreement_score":0.007206952,"about_ca_system_score_codex":0.0007330362,"about_ca_system_score_gemma":0.00029346376,"threshold_uncertainty_score":0.01432997},"labels":[],"label_agreement":null},{"id":"W1951078582","doi":"10.1029/2011gl050691","title":"The Wrangel Island Polynya in early summer: Trends and relationships to other polynyas and the Beaufort Sea High","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Climatology; Sea ice; Oceanography; Beaufort scale; Environmental science; Geology; Arctic ice pack; Beaufort sea; Arctic sea ice decline; Drift ice","score_opus":0.03138140128613356,"score_gpt":0.2732197065038697,"score_spread":0.2418383052177361,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1951078582","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971385,0.0007089446,0.000020398335,0.00022016278,0.000010139053,0.0000037411357,0.00040648936,0.0000038225635,0.0014879175],"genre_scores_gemma":[0.9979634,0.00063516514,0.000058599573,0.000060994378,0.00002274592,0.0000046968016,0.00042390972,0.0000028708178,0.0008277024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000010838343,0.000007772068,0.000028384693,0.000017094024,0.000032851985],"domain_scores_gemma":[0.99903774,0.00005932744,0.00038825805,0.000028206141,0.00015710083,0.00032940943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015784346,0.0001541407,0.00013142772,0.000701658,0.00050376373,0.0006520859,0.00025760135,0.00028251525,0.0017137986],"category_scores_gemma":[0.0005192816,0.000080333535,0.00016546002,0.001179893,0.00031548835,0.00042929972,0.00036641065,0.0004185185,0.00020398381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021050953,0.000010516211,0.9968451,0.000014745534,0.000021721129,0.000070032605,0.00046050033,0.000020613732,0.00030087357,0.000018856714,0.00016292589,0.0020530997],"study_design_scores_gemma":[1.9590028e-7,0.000004327624,0.99943906,0.0000027014846,0.0000016069729,0.00002324759,0.00030992914,0.000013883967,0.00000774041,0.0000019506372,0.00019491103,5.305429e-7],"about_ca_topic_score_codex":0.13056175,"about_ca_topic_score_gemma":0.3015184,"teacher_disagreement_score":0.13056175,"about_ca_system_score_codex":0.00056686735,"about_ca_system_score_gemma":0.0005324051,"threshold_uncertainty_score":0.25960362},"labels":[],"label_agreement":null},{"id":"W1952214568","doi":"10.1029/2010gl044301","title":"Has the ozone hole contributed to increased Antarctic sea ice extent?","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":154,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Ozone depletion; Sea ice; Southern Hemisphere; Cryosphere; Oceanography; Climatology; Environmental science; Northern Hemisphere; Antarctic sea ice; Arctic ice pack; Atmospheric sciences; Ozone layer; Ekman transport; Geology; Stratosphere; Upwelling","score_opus":0.023788997476404533,"score_gpt":0.2712880496055963,"score_spread":0.2474990521291918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1952214568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98431903,0.004949032,0.00047652712,0.005037968,0.00024856627,0.000012767032,0.00041641315,0.000026750984,0.004512998],"genre_scores_gemma":[0.99665076,0.0020280892,0.00012563233,0.00036360582,0.00010671697,0.0000031921268,0.000102166414,0.0000079228175,0.0006119553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998535,0.000036580943,0.000007875562,0.00002812558,0.000013253985,0.000060713493],"domain_scores_gemma":[0.99962056,0.00009513453,0.00011767033,0.000036254638,0.000045136843,0.000085248845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080169545,0.000331236,0.00040097465,0.0002951898,0.00031550365,0.001282116,0.00038081474,0.0011261672,0.0031002641],"category_scores_gemma":[0.0012066943,0.00021494858,0.00067026267,0.0003691229,0.00052500854,0.0012583475,0.000720947,0.0004901189,0.00025282567],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012926089,0.00021240997,0.89843273,0.00063224835,0.0009876908,0.0016184167,0.00054875395,0.014318338,0.015430447,0.013886489,0.003090619,0.04954916],"study_design_scores_gemma":[0.00011697953,0.00025167674,0.96684873,0.00009357818,0.0004315001,0.00042425786,0.001142051,0.009583479,0.0024388847,0.0068840934,0.011742579,0.0000421424],"about_ca_topic_score_codex":0.016074907,"about_ca_topic_score_gemma":0.010419405,"teacher_disagreement_score":0.016074907,"about_ca_system_score_codex":0.0007600826,"about_ca_system_score_gemma":0.0005855994,"threshold_uncertainty_score":0.031962633},"labels":[],"label_agreement":null},{"id":"W1952393191","doi":"10.1002/2014gl062741","title":"Internally generated decadal cold events in the northern North Atlantic and their possible implications for the demise of the Norse settlements in Greenland","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Climatology; North Atlantic Deep Water; North Atlantic oscillation; Oceanography; Thermohaline circulation; Geology; Demise; Forcing (mathematics); Atlantic multidecadal oscillation; Advection; Climate change; Gulf Stream; Subtropics","score_opus":0.06145735681616938,"score_gpt":0.3125185681157311,"score_spread":0.2510612112995617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1952393191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995357,0.000025344743,0.00009735472,0.000043375603,0.0000021815606,0.0000010456029,0.00006345223,0.0000052720234,0.00022624753],"genre_scores_gemma":[0.9998771,0.000010740026,0.000025543162,0.000004330627,9.771637e-7,5.737108e-7,0.000043860295,0.0000011150889,0.00003573419],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995244,0.000009869419,0.0000036469553,0.000013352801,0.000006950801,0.000013761602],"domain_scores_gemma":[0.9998186,0.000034089462,0.000057795172,0.000024666422,0.000029439016,0.000035360863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003148087,0.00013175132,0.00019414669,0.00036623605,0.00025780158,0.00054063014,0.00018505946,0.00021198316,0.00069471024],"category_scores_gemma":[0.00068467524,0.00007236605,0.00019067695,0.00024260565,0.0004438148,0.00018579708,0.0004758942,0.00017360969,0.000049103237],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001962963,0.00005143929,0.9452207,0.00002516854,0.00014755092,0.0005050656,0.0004759392,0.027251963,0.015277487,0.001295256,0.00030331925,0.00924974],"study_design_scores_gemma":[0.000009523202,0.00001953259,0.9822397,0.0000055317487,0.000020447853,0.000033457603,0.00024834587,0.016303968,0.00043827976,0.0002945405,0.00037965563,0.0000070635706],"about_ca_topic_score_codex":0.031247899,"about_ca_topic_score_gemma":0.04540224,"teacher_disagreement_score":0.031247899,"about_ca_system_score_codex":0.00086459913,"about_ca_system_score_gemma":0.0003720201,"threshold_uncertainty_score":0.06213206},"labels":[],"label_agreement":null},{"id":"W1957552617","doi":"10.1029/2012gl053033","title":"Cross‐regional prediction of long‐term trajectory of stream water DOC response to climate change","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":164,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; McMaster University; University of Saskatchewan; Trent University","funders":"Northern Research Station; Leverhulme Trust; U.S. Department of Agriculture","keywords":"STREAMS; Drainage basin; Environmental science; Dissolved organic carbon; Climate change; Hydrology (agriculture); Surface water; Latitude; Range (aeronautics); Physical geography; Geology; Oceanography; Geography","score_opus":0.04927638734360459,"score_gpt":0.31605785661345626,"score_spread":0.2667814692698517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1957552617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976418,0.00016659398,0.0015495537,0.000042855605,0.000003994884,0.0000026190996,0.00031378012,0.000025898838,0.00025283784],"genre_scores_gemma":[0.99888104,0.00006121055,0.00055805064,0.0000056075833,0.0000026870887,0.0000031976197,0.0004182782,0.0000063237803,0.000063606785],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983335,0.0000509286,0.000010048569,0.00006900793,0.000013328807,0.000023294719],"domain_scores_gemma":[0.999258,0.0002852871,0.00013433589,0.00010438827,0.00015364027,0.00006430721],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011200742,0.00017689097,0.00026458877,0.0005339147,0.0001623765,0.0005566701,0.00022380525,0.0002848871,0.00048863806],"category_scores_gemma":[0.0018228734,0.00018100307,0.0004973118,0.0005798073,0.00019007048,0.00040061795,0.00038409227,0.00021179003,0.00017396628],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014372195,0.000022802265,0.94474125,0.000023271901,0.0003145268,0.000059849455,0.00007542411,0.04135738,0.005219165,0.00019121621,0.00019406024,0.007657371],"study_design_scores_gemma":[0.000006668806,0.000033472974,0.9191188,0.00000488711,0.00005302463,0.000028682547,0.00008032162,0.0791873,0.00083559944,0.00025626353,0.00038561434,0.000009470306],"about_ca_topic_score_codex":0.018142112,"about_ca_topic_score_gemma":0.019632818,"teacher_disagreement_score":0.018142112,"about_ca_system_score_codex":0.0005176863,"about_ca_system_score_gemma":0.0002745104,"threshold_uncertainty_score":0.03607303},"labels":[],"label_agreement":null},{"id":"W1958797316","doi":"10.1002/grl.50899","title":"Tomographic image of melt storage beneath Askja Volcano, Iceland using local microseismicity","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Met Office; Natural Environment Research Council; Research Councils UK; Sight Research UK","keywords":"Geology; Sill; Volcano; Seismology; Magma; Magma chamber; Anomaly (physics); Caldera; Microseism; Petrology; Geophysics","score_opus":0.030791998918483044,"score_gpt":0.2742944400470217,"score_spread":0.24350244112853864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1958797316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99138016,0.00006371195,0.00075511076,0.00004701065,0.0000046712944,0.000026761425,0.0037235597,0.00013005346,0.003868885],"genre_scores_gemma":[0.9948355,0.00007665719,0.00212975,0.000013428394,0.000011582592,0.000015714992,0.0023796847,0.000018783698,0.0005188948],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999789,0.0000013099933,0.000001270852,0.000006002075,0.0000050656427,0.000007484357],"domain_scores_gemma":[0.99993443,0.000008008698,0.0000158069,0.000005575733,0.000016717047,0.000019390267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000053152624,0.00017468154,0.00010470401,0.0010255373,0.00020994795,0.0003733117,0.00016050373,0.00016566462,0.0013514381],"category_scores_gemma":[0.000095919946,0.000119606324,0.0001857891,0.0006183715,0.00015648917,0.00013208014,0.00020618958,0.00012018528,0.00019366542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007590632,0.00025966,0.7167055,0.0002705014,0.00020376944,0.0015374146,0.0020122528,0.038331848,0.15395357,0.00096485106,0.006126157,0.07887547],"study_design_scores_gemma":[0.000016031343,0.000022448467,0.9842367,0.000015633042,0.000026542559,0.000120114055,0.0002625166,0.0125989,0.0017417907,0.000042924687,0.0009097952,0.0000066985926],"about_ca_topic_score_codex":0.038196005,"about_ca_topic_score_gemma":0.07616756,"teacher_disagreement_score":0.038196005,"about_ca_system_score_codex":0.00039300814,"about_ca_system_score_gemma":0.0004039532,"threshold_uncertainty_score":0.075947344},"labels":[],"label_agreement":null},{"id":"W1958988077","doi":"10.1002/2015gl064744","title":"The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM)","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Climatology; Salinity; Environmental science; Oceanography; Ozone; Ocean current; Sea surface temperature; General Circulation Model; Wind stress; Atmospheric sciences; Climate model; Climate change; Ozone depletion; Geology; Meteorology; Geography; Stratosphere","score_opus":0.05455086434610953,"score_gpt":0.30822378747238144,"score_spread":0.25367292312627193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1958988077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905175,0.000024614921,0.000060688937,0.000055882243,0.000005290035,0.000005202203,0.0005156256,0.000015633563,0.00026530854],"genre_scores_gemma":[0.99867934,0.000033379412,0.00014076033,0.000018607981,0.0000074002332,0.000006923136,0.0009782647,0.000009816196,0.00012564528],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99972063,0.00009220815,0.000019751593,0.00006546155,0.000030261364,0.00007165198],"domain_scores_gemma":[0.99902713,0.00031381668,0.000159501,0.00018876547,0.00014143516,0.00016933693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010569446,0.0006360836,0.0005893141,0.0004184842,0.00054493034,0.00095536455,0.000894905,0.00094024884,0.0013511723],"category_scores_gemma":[0.0015493849,0.0004187809,0.0014356879,0.00095983053,0.00048343046,0.00076197693,0.0007368859,0.0006782209,0.00020542213],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020259446,0.0011414549,0.70736843,0.00019524303,0.0015245714,0.0007446299,0.00040033006,0.2605233,0.01597143,0.0013801006,0.0026061893,0.0061183483],"study_design_scores_gemma":[0.0007188674,0.00053960975,0.7017515,0.0000215626,0.00041093057,0.00007144193,0.00034638427,0.2876723,0.0064367866,0.00027098888,0.0016539961,0.00010548288],"about_ca_topic_score_codex":0.094566286,"about_ca_topic_score_gemma":0.048692856,"teacher_disagreement_score":0.094566286,"about_ca_system_score_codex":0.0011231728,"about_ca_system_score_gemma":0.00073760323,"threshold_uncertainty_score":0.18803167},"labels":[],"label_agreement":null},{"id":"W1959726294","doi":"10.1029/2010gl044366","title":"Formation of cratonic mantle keels by arc accretion: Evidence from S receiver functions","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Geology; Lithosphere; Craton; Classification of discontinuities; Mantle (geology); Asthenosphere; Plate tectonics; Geophysics; Tectonics; Accretion (finance); Seismology","score_opus":0.03426834005363012,"score_gpt":0.28260075100410753,"score_spread":0.24833241095047742,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1959726294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986356,0.00003552597,0.00024179438,0.0000134515385,2.9471025e-7,7.6160853e-7,0.00002527133,0.000009149737,0.001038206],"genre_scores_gemma":[0.9993845,0.000033119813,0.00020052,0.0000034496043,7.7341775e-7,5.5420253e-7,0.000061859384,0.0000027355318,0.00031251484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.0000070614806,0.0000031537554,0.00001863322,0.000020633846,0.000029428506],"domain_scores_gemma":[0.99961215,0.00008881309,0.000094749725,0.00004839633,0.00011071029,0.000045238852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013365776,0.00016989865,0.000118518685,0.00066417916,0.00041592456,0.0006268979,0.00029667892,0.00022996384,0.0008800656],"category_scores_gemma":[0.00072593696,0.00020653017,0.000083107436,0.0006507846,0.0006303486,0.00026948686,0.00040835325,0.0001950795,0.00014903815],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039697357,0.0000248779,0.81596255,0.00004239856,0.00004472674,0.0008091794,0.0017856265,0.0013204524,0.13981673,0.0016853999,0.00022366401,0.037887525],"study_design_scores_gemma":[0.000010100021,0.000044766737,0.9832472,0.000007586211,0.000019877436,0.00036977354,0.000492986,0.0024562571,0.012297377,0.00024722907,0.0007971045,0.000009717635],"about_ca_topic_score_codex":0.043875672,"about_ca_topic_score_gemma":0.049518257,"teacher_disagreement_score":0.043875672,"about_ca_system_score_codex":0.00045698063,"about_ca_system_score_gemma":0.0003315921,"threshold_uncertainty_score":0.08724058},"labels":[],"label_agreement":null},{"id":"W1959728552","doi":"10.1002/2013gl058096","title":"Breaking the oceanic lithosphere of a subducting slab: The 2013 Khash, Iran earthquake","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geology; Subduction; Seismology; Lithosphere; Slab; Mantle (geology); Episodic tremor and slip; Interplate earthquake; Oceanic crust; Crust; Mantle wedge; Geophysics; Tectonics","score_opus":0.045208588890498225,"score_gpt":0.2762157134620481,"score_spread":0.23100712457154987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1959728552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993406,0.00003172151,0.00004998954,0.000061335384,0.0000042176925,0.0000032381809,0.00004151648,0.0000032791554,0.0004641708],"genre_scores_gemma":[0.99976,0.00003270141,0.000043733206,0.000012846299,0.0000062823656,0.0000011055433,0.000060839728,4.6804243e-7,0.00008214175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999474,0.0000039477723,0.000003751206,0.000009447355,0.000015251249,0.000020189596],"domain_scores_gemma":[0.9998807,0.000008322763,0.00005120408,0.000009138161,0.000028023398,0.000022601102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014261642,0.00015660365,0.0001749454,0.00033155698,0.00046124365,0.0003178574,0.00018663568,0.00024814537,0.00046065619],"category_scores_gemma":[0.0003374099,0.000111274705,0.0001374014,0.00037047488,0.00047514925,0.00025524237,0.00048213135,0.00019951919,0.000113543174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042982356,0.00009619505,0.94641316,0.000057673147,0.00008651426,0.0021157977,0.0018715358,0.0024531751,0.020266982,0.00059410016,0.0014222614,0.024192639],"study_design_scores_gemma":[0.000011272106,0.00005394387,0.99684805,0.0000059385725,0.000017342354,0.0002155994,0.00082566397,0.00077709847,0.0005816889,0.00016499317,0.00049210247,0.0000062446347],"about_ca_topic_score_codex":0.012037029,"about_ca_topic_score_gemma":0.015413223,"teacher_disagreement_score":0.012037029,"about_ca_system_score_codex":0.0006040777,"about_ca_system_score_gemma":0.0005178282,"threshold_uncertainty_score":0.023933947},"labels":[],"label_agreement":null},{"id":"W1959961340","doi":"10.1002/2015gl065101","title":"The low‐degree shape of Mercury","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Lomonosov Moscow State University; Moscow State University of Geodesy and Cartography; Russian Science Foundation; Carnegie Institution of Washington; Natural Sciences and Engineering Research Council of Canada; Johns Hopkins University; National Aeronautics and Space Administration","keywords":"Mercury (programming language); Geoid; Planet; Geodesy; Spacecraft; Geology; Latitude; Altimeter; Southern Hemisphere; Oblate spheroid; Northern Hemisphere; Polar; Geophysics; Physics; Astrobiology; Atmospheric sciences; Astronomy; Climatology","score_opus":0.09530307383002155,"score_gpt":0.32647684061099747,"score_spread":0.2311737667809759,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1959961340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9781188,0.00007323436,0.0037185026,0.000112852285,0.000010235193,0.0000031704612,0.00035106228,0.00018800994,0.017424017],"genre_scores_gemma":[0.99793375,0.000018202307,0.00043692597,0.000012664816,0.0000048416287,0.00000120767,0.00022425492,0.000030084342,0.0013380062],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991167,0.000006217369,0.0000024818098,0.000025905903,0.00003710559,0.000016655786],"domain_scores_gemma":[0.9998023,0.000018939889,0.00004876574,0.000028525705,0.00007530654,0.000026135775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000053304804,0.0001264923,0.00014289274,0.000555346,0.00048354684,0.00053250405,0.00020886517,0.00011772157,0.0034437075],"category_scores_gemma":[0.000351241,0.00010308876,0.00009678351,0.0005700592,0.0004191192,0.00018989097,0.00045526554,0.000188337,0.0006826355],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043929776,0.00002738007,0.41429195,0.00011173077,0.000086446526,0.0006528,0.0014302643,0.0056884037,0.45903754,0.0068651964,0.0045407973,0.10682819],"study_design_scores_gemma":[0.000014064304,0.00009581108,0.91614825,0.000009499148,0.000033252527,0.001023979,0.0006578701,0.007852231,0.05650879,0.0028770599,0.01473276,0.00004630087],"about_ca_topic_score_codex":0.0038604944,"about_ca_topic_score_gemma":0.0041128034,"teacher_disagreement_score":0.0038604944,"about_ca_system_score_codex":0.00027528568,"about_ca_system_score_gemma":0.00018120027,"threshold_uncertainty_score":0.011520386},"labels":[],"label_agreement":null},{"id":"W1960195134","doi":"10.1029/2010gl045106","title":"Extremely low long‐term erosion rates around the Gamburtsev Mountains in interior East Antarctica","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Geology; Denudation; Glacial period; Paleontology; Erosion; Glacier; Geomorphology; Cretaceous; Antarctic ice sheet; Rift; Gondwana; Tectonics; Oceanography; Cryosphere; Sea ice","score_opus":0.040075574042392786,"score_gpt":0.314912937828003,"score_spread":0.2748373637856102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1960195134","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989742,0.0003317757,0.000018169225,0.000025743419,0.0000022210409,0.0000018660602,0.00011412439,0.0000050974713,0.00052668795],"genre_scores_gemma":[0.99932647,0.00020038216,0.00006670561,0.0000098159835,0.0000054061047,0.0000030608965,0.00021575177,0.0000027436258,0.00016978617],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999131,0.0000128964875,0.000006594474,0.000019954592,0.000017961198,0.00002950158],"domain_scores_gemma":[0.99984086,0.000017818775,0.00006443806,0.000014813336,0.000027178576,0.00003480804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002091649,0.00020612785,0.00029760983,0.001301817,0.00065461174,0.00085659616,0.00023588222,0.00021815178,0.00082746707],"category_scores_gemma":[0.0004689224,0.0001570415,0.00010303873,0.0015382782,0.000524124,0.00030632163,0.00063578144,0.00015467928,0.00021777353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011943006,0.000016152268,0.9739469,0.000060048744,0.00008403275,0.0005136334,0.0019996108,0.00032600816,0.0061047007,0.00010639068,0.00033737387,0.016385624],"study_design_scores_gemma":[0.0000018852325,0.0000060781053,0.9990945,0.000006789876,0.0000063957123,0.00005901631,0.0003393922,0.000043512624,0.000052936757,0.000015126174,0.0003728045,0.0000015885274],"about_ca_topic_score_codex":0.030866558,"about_ca_topic_score_gemma":0.092242084,"teacher_disagreement_score":0.030866558,"about_ca_system_score_codex":0.00043457953,"about_ca_system_score_gemma":0.00036811628,"threshold_uncertainty_score":0.06137377},"labels":[],"label_agreement":null},{"id":"W1961184383","doi":"10.1002/2015gl063733","title":"Inverting interpolated receiver functions with surface wave dispersion and gravity: Application to the western U.S. and adjacent Canada and Mexico","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Laboratory Directed Research and Development; Northwestern University; National Science Foundation","keywords":"Receiver function; Geology; Interpolation (computer graphics); Geodesy; Smoothing; Azimuth; Dispersion (optics); Surface wave; Rayleigh wave; Seismology; Geophysics; Mathematical analysis; Geometry; Physics; Mathematics; Optics; Classical mechanics","score_opus":0.02568855382191007,"score_gpt":0.24262774911567467,"score_spread":0.2169391952937646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1961184383","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97762007,0.000049234663,0.019354494,0.00010132217,0.000010839656,0.000017858742,0.00031585444,0.0006470019,0.0018832744],"genre_scores_gemma":[0.9805853,0.000033103694,0.018465292,0.0000072028065,0.0000038074822,0.000007582453,0.00022311488,0.000031993994,0.000642524],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989235,0.000022700842,0.000004789564,0.000020398333,0.000034073906,0.00002567884],"domain_scores_gemma":[0.999681,0.00011702476,0.00003111651,0.00003306607,0.00012151023,0.00001631254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003527344,0.00034413,0.00015985461,0.0004479331,0.0005911489,0.0004922009,0.00060677016,0.0002870776,0.00090560224],"category_scores_gemma":[0.0019183333,0.0002562697,0.00031845522,0.0009672854,0.00025560058,0.00022435581,0.00028499903,0.00039098813,0.00009796498],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019774494,0.00011162781,0.17643252,0.000026694192,0.00010456672,0.0005310007,0.00027372208,0.73873514,0.006088276,0.0015538967,0.0011125196,0.074832246],"study_design_scores_gemma":[0.000035947396,0.000016800472,0.03310708,0.00000605304,0.000020495574,0.000034556822,0.000113249334,0.9635247,0.0020268783,0.00028876157,0.00081112917,0.0000143518655],"about_ca_topic_score_codex":0.8170129,"about_ca_topic_score_gemma":0.7523419,"teacher_disagreement_score":0.1829871,"about_ca_system_score_codex":0.0023008788,"about_ca_system_score_gemma":0.0031592562,"threshold_uncertainty_score":0.36812943},"labels":[],"label_agreement":null},{"id":"W1961316012","doi":"10.1002/2013gl057973","title":"Measuring water accumulation rates using GRACE data in areas experiencing glacial isostatic adjustment: The Nelson River basin","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Environment and Climate Change Canada; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; National Oceanic and Atmospheric Administration; Deutsches Zentrum für Luft- und Raumfahrt; Manitoba Hydro","keywords":"Post-glacial rebound; Geology; Drainage basin; Anomaly (physics); Geodesy; Structural basin; Glacial period; Global Positioning System; Geomorphology; Water level; Hydrology (agriculture); Geotechnical engineering; Cartography; Geography","score_opus":0.20917639550227732,"score_gpt":0.3443263510029731,"score_spread":0.13514995550069578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1961316012","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99833715,0.000012205329,0.00013048602,0.000010548517,0.000001042876,0.0000039440392,0.0007197787,0.000012657472,0.000772169],"genre_scores_gemma":[0.99867296,0.0000289542,0.00045239844,0.0000033440292,0.0000011863162,0.0000063245616,0.00064037537,0.000005168439,0.00018934606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998704,0.000016846665,0.000011551621,0.000031608142,0.000043793712,0.000025770494],"domain_scores_gemma":[0.9996263,0.00004596427,0.000087833556,0.000042654534,0.00013404543,0.000063252555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021671694,0.00015871474,0.00016951142,0.0009537616,0.00043663188,0.00055349804,0.0002388503,0.00013170787,0.0003723135],"category_scores_gemma":[0.0010973236,0.00011431451,0.00012446297,0.001659507,0.00027356044,0.00034499756,0.00038455447,0.00015739993,0.00010551023],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017091943,0.000038997656,0.9812019,0.000011345459,0.00003711018,0.00007698485,0.00057997,0.0025771996,0.0048175845,0.00015066694,0.00036763216,0.009969671],"study_design_scores_gemma":[0.000006077679,0.000011067363,0.9954798,0.0000026135933,0.000009864708,0.000021821828,0.00030301884,0.0025253557,0.0010443124,0.00003480646,0.00055429887,0.0000070313763],"about_ca_topic_score_codex":0.53553027,"about_ca_topic_score_gemma":0.7431993,"teacher_disagreement_score":0.46446973,"about_ca_system_score_codex":0.0017099394,"about_ca_system_score_gemma":0.0015553248,"threshold_uncertainty_score":0.93441015},"labels":[],"label_agreement":null},{"id":"W1962315276","doi":"10.1002/2013gl059099","title":"Recent and future trends in synthetic greenhouse gas radiative forcing","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":162,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; Sight Research UK; Natural Environment Research Council; Australian Government; Commonwealth Scientific and Industrial Research Organisation; Department for Environment, Food and Rural Affairs, UK Government; National Aeronautics and Space Administration","keywords":"Radiative forcing; Greenhouse gas; Environmental science; Forcing (mathematics); Atmospheric sciences; Radiative transfer; Greenhouse effect; Climatology; Global warming; Climate change; Meteorology; Aerosol; Physics","score_opus":0.012509231354372277,"score_gpt":0.25695219520902046,"score_spread":0.2444429638546482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1962315276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8458683,0.04091459,0.016807538,0.017859757,0.00076249795,0.00005234283,0.027110523,0.0011312669,0.049493216],"genre_scores_gemma":[0.97276616,0.009427787,0.0060401913,0.0006310552,0.00030773834,0.000028130511,0.00932882,0.000071700866,0.0013984358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970955,0.000043213277,0.00001947775,0.000086813765,0.00009397949,0.0000469111],"domain_scores_gemma":[0.99911886,0.00014726794,0.00016330359,0.00006690566,0.00043622192,0.000067342946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012124163,0.00050886953,0.0002273347,0.0008864373,0.00023719954,0.0009875599,0.00050813303,0.00066069426,0.002239765],"category_scores_gemma":[0.0015071931,0.00016047343,0.00045277874,0.0013963106,0.0004216209,0.001250615,0.0003564833,0.0004794357,0.00048199718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018599218,0.00028525575,0.4308452,0.0028047396,0.000769025,0.0006073761,0.00090230757,0.0917626,0.04727347,0.038617447,0.037934557,0.34633812],"study_design_scores_gemma":[0.000058247428,0.0002933589,0.6006742,0.0003455927,0.00016953015,0.0007678578,0.0007081202,0.050286237,0.021096416,0.009166921,0.31622466,0.00020882304],"about_ca_topic_score_codex":0.022252293,"about_ca_topic_score_gemma":0.01723999,"teacher_disagreement_score":0.022252293,"about_ca_system_score_codex":0.0022673167,"about_ca_system_score_gemma":0.0007142975,"threshold_uncertainty_score":0.04424554},"labels":[],"label_agreement":null},{"id":"W1962354521","doi":"10.1002/grl.50511","title":"Compressional and shear‐wave velocity structure of the continent‐ocean transition zone at the eastern Grand Banks, Newfoundland","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seafloor spreading; Continental crust; Continental margin; Mantle (geology); Seismology; Rift; Crust; Seismometer; Oceanic crust; Transition zone; Continental shelf; Seismic refraction; Geophysics; Subduction; Tectonics; Oceanography","score_opus":0.019204507735248528,"score_gpt":0.22698320309387598,"score_spread":0.20777869535862745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1962354521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99807286,0.00009635754,0.0000691495,0.00007940076,0.0000017809324,0.0000026117737,0.00056016765,0.000015263655,0.0011024907],"genre_scores_gemma":[0.9989605,0.000059508253,0.00008275119,0.000012015548,8.2399254e-7,0.0000019819124,0.0003893823,0.0000027538729,0.0004902362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991345,0.000005814384,0.0000046239707,0.000023652376,0.000012677723,0.000039728726],"domain_scores_gemma":[0.99966156,0.00003665112,0.000093137816,0.000027040207,0.00011102736,0.00007048698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015312652,0.00021116454,0.00012413312,0.0007192365,0.0006107777,0.00062804675,0.00041157275,0.00018032316,0.0020015065],"category_scores_gemma":[0.00048281127,0.00019372269,0.00015656141,0.00077401084,0.0005427221,0.00030965105,0.0004953308,0.00023047683,0.00018694648],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000730442,0.000018783827,0.9784627,0.000028666072,0.000051153755,0.0002496343,0.0006996335,0.00407538,0.0024887614,0.00030032208,0.0014476537,0.012104295],"study_design_scores_gemma":[0.0000034528598,0.0000052760806,0.99760973,0.000009164707,0.000007650335,0.000018210787,0.0002473472,0.001481588,0.0001196741,0.0000127377525,0.00048067034,0.000004380077],"about_ca_topic_score_codex":0.9634575,"about_ca_topic_score_gemma":0.9803285,"teacher_disagreement_score":0.036542475,"about_ca_system_score_codex":0.006310234,"about_ca_system_score_gemma":0.0034505464,"threshold_uncertainty_score":0.073515296},"labels":[],"label_agreement":null},{"id":"W1963608744","doi":"10.1029/2008gl035263","title":"Neural network analysis of crosshole tomographic images: The seismic signature of gas hydrate bearing sediments in the Mackenzie Delta (NW Canada)","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Bundesministerium für Bildung und Forschung","keywords":"Geology; Attenuation; Anisotropy; Clathrate hydrate; Mineralogy; Seismic attribute; Seismology; Tomography; Hydrate","score_opus":0.022791317100994773,"score_gpt":0.2596457728857986,"score_spread":0.23685445578480382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963608744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99827373,0.000025317935,0.0009625463,0.0000250894,0.0000015692276,0.0000056869035,0.00016009196,0.0000308399,0.00051501254],"genre_scores_gemma":[0.99825245,0.000035759305,0.0011496253,0.0000041860903,9.802624e-7,0.0000032441637,0.00020442293,0.0000029449789,0.00034645773],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999949,0.000003750178,0.000002123003,0.00001285401,0.000016623271,0.000015721285],"domain_scores_gemma":[0.99989486,0.000016270284,0.000018508048,0.0000049861173,0.000052671756,0.000012768586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009450045,0.0002208006,0.00009675039,0.0007794336,0.00019668591,0.00025928378,0.00026486235,0.00015485326,0.00037788585],"category_scores_gemma":[0.00045724073,0.00011147925,0.000102870756,0.0007442392,0.00026686766,0.00012431624,0.0001676422,0.00010545772,0.00005858249],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000656412,0.00024189318,0.453189,0.00017676181,0.00017027734,0.001257832,0.0009221336,0.15221204,0.2121934,0.0009967324,0.002058658,0.17592488],"study_design_scores_gemma":[0.000016500502,0.000035196506,0.6639274,0.000008700214,0.000030049718,0.00013851824,0.0003721502,0.32002485,0.014652379,0.0001755951,0.0005974103,0.00002137989],"about_ca_topic_score_codex":0.46364507,"about_ca_topic_score_gemma":0.5684698,"teacher_disagreement_score":0.5363549,"about_ca_system_score_codex":0.0014566121,"about_ca_system_score_gemma":0.0008645946,"threshold_uncertainty_score":0.9218927},"labels":[],"label_agreement":null},{"id":"W1963613810","doi":"10.1029/2004gl022293","title":"Evidence for melt lubrication during large earthquakes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lubrication; Slip (aerodynamics); Geology; Melting point; Materials science; Mechanics; Thermodynamics; Composite material; Physics","score_opus":0.09911029649065599,"score_gpt":0.3434663241904369,"score_spread":0.24435602769978088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963613810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996051,0.0001221515,0.00007813075,0.000009516884,0.0000011136997,0.0000011617658,0.000025824958,0.000008342017,0.00014867815],"genre_scores_gemma":[0.9998209,0.00003103335,0.000034749002,0.000003459612,0.000001047896,9.233593e-7,0.00005042737,0.0000017632934,0.000055702556],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9997366,0.000030232657,0.000025967727,0.000044022247,0.000086710206,0.000076366494],"domain_scores_gemma":[0.99889636,0.00018921148,0.0004786099,0.00013432006,0.00020557368,0.000095972435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026459456,0.00020522595,0.0003878309,0.0006505517,0.00031557947,0.0004948739,0.00027165635,0.00051479245,0.00096174784],"category_scores_gemma":[0.0016129507,0.00031350466,0.00019074278,0.00041442676,0.0008396711,0.00031011342,0.000582582,0.00021446403,0.00017842998],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002301061,0.00008671244,0.23671107,0.00023431302,0.000080256956,0.0010085317,0.0014550304,0.0011888145,0.74853826,0.0002830398,0.00014123978,0.00797164],"study_design_scores_gemma":[0.000067623034,0.001021875,0.8673529,0.000016219055,0.000055428784,0.0010979298,0.0004427365,0.0020301796,0.126416,0.0002155094,0.0012576301,0.000025956982],"about_ca_topic_score_codex":0.0023751876,"about_ca_topic_score_gemma":0.0030407754,"teacher_disagreement_score":0.0023751876,"about_ca_system_score_codex":0.00034087442,"about_ca_system_score_gemma":0.00011623979,"threshold_uncertainty_score":0.0047227144},"labels":[],"label_agreement":null},{"id":"W1963772074","doi":"10.1029/2005gl022803","title":"Photoproduction of carbon monoxide in first‐year sea ice in Franklin Bay, southeastern Beaufort Sea","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Sea ice; Oceanography; Arctic ice pack; Bay; Beaufort sea; Seawater; Colored dissolved organic matter; Arctic; Sea ice thickness; Environmental science; Dissolved organic carbon; Geology; Organic matter; Atmospheric sciences; Chemistry; Phytoplankton","score_opus":0.018265345497958673,"score_gpt":0.25345147811809643,"score_spread":0.23518613262013777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963772074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996977,0.00006012339,0.00001159399,0.00001423813,0.0000012082722,8.6566615e-7,0.000077583754,0.0000019430347,0.00013482093],"genre_scores_gemma":[0.9993099,0.0000717432,0.00006856852,0.000015214745,0.0000017365026,0.0000026551731,0.00030008054,0.000001251356,0.00022868734],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999124,0.000006516075,0.0000033549493,0.000025556636,0.000024948456,0.000027229607],"domain_scores_gemma":[0.9998323,0.000018913148,0.000047527017,0.000006414906,0.000048614664,0.00004617847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012073054,0.00024305735,0.00020664895,0.00052039477,0.00079660927,0.00051813654,0.00034859014,0.0003087702,0.0003755331],"category_scores_gemma":[0.0001675492,0.00025645838,0.00022207921,0.0003904942,0.00043634814,0.00027857439,0.00032843897,0.00022637953,0.00010858935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049698586,0.00005806833,0.8685897,0.000054610162,0.00006113686,0.0006868442,0.001453103,0.0008242119,0.1220456,0.000054983706,0.0004006556,0.005274111],"study_design_scores_gemma":[0.000003882879,0.000027845454,0.9977246,0.0000017327097,0.0000057763104,0.000051857805,0.00026702782,0.0002544059,0.00148169,0.000005442906,0.00017254987,0.000003131189],"about_ca_topic_score_codex":0.43434286,"about_ca_topic_score_gemma":0.5500888,"teacher_disagreement_score":0.43434286,"about_ca_system_score_codex":0.0023834126,"about_ca_system_score_gemma":0.00082605844,"threshold_uncertainty_score":0.8636294},"labels":[],"label_agreement":null},{"id":"W1963956511","doi":"10.1002/2014gl061700","title":"Interacting components of the top‐of‐atmosphere energy balance affect changes in regional surface temperature","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Energy balance; Atmosphere (unit); Environmental science; Radiative transfer; Atmospheric sciences; Energy transport; Energy budget; Balance (ability); Climatology; Meteorology; Physics; Geology; Thermodynamics","score_opus":0.0316746555188592,"score_gpt":0.2908540709021639,"score_spread":0.2591794153833047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1963956511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99174225,0.00009126559,0.002825341,0.00030726736,0.000024757048,0.000010735685,0.0002299014,0.000088326895,0.0046802238],"genre_scores_gemma":[0.99957436,0.000024632262,0.0001741884,0.000014930963,0.0000039032593,0.0000025467393,0.00003489833,0.000011467865,0.00015896073],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99975306,0.000081795035,0.000012662278,0.00006445183,0.00003510607,0.000052853567],"domain_scores_gemma":[0.99966955,0.00015155903,0.000045287037,0.000028717368,0.000044955057,0.000060025566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003732088,0.0004091848,0.00036574464,0.00032713864,0.00035697233,0.0013331065,0.0004527977,0.0005296695,0.0021293578],"category_scores_gemma":[0.0011702435,0.00038689902,0.0007118481,0.00028308254,0.0004108194,0.00090779224,0.00080734934,0.0005586418,0.0002344879],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009895493,0.00025642794,0.16274904,0.0001249264,0.0010770387,0.00029521206,0.00022522271,0.68637794,0.12704498,0.0068743383,0.0015003363,0.012485013],"study_design_scores_gemma":[0.00017216743,0.0002200296,0.25517172,0.000015307594,0.00048070934,0.00008456024,0.00025781424,0.72571635,0.012736978,0.0037380743,0.0013276108,0.00007878086],"about_ca_topic_score_codex":0.0115652615,"about_ca_topic_score_gemma":0.007050627,"teacher_disagreement_score":0.0115652615,"about_ca_system_score_codex":0.00083565665,"about_ca_system_score_gemma":0.0005185706,"threshold_uncertainty_score":0.02299589},"labels":[],"label_agreement":null},{"id":"W1964173628","doi":"10.1029/2004gl020075","title":"Downscaling daily extreme temperatures with genetic programming","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Downscaling; Context (archaeology); Scale (ratio); Genetic programming; Environmental science; Computer science; Statistical model; Climatology; Meteorology; Climate change; Machine learning; Geology; Ecology; Geography; Biology","score_opus":0.042546450133563965,"score_gpt":0.2909065955735153,"score_spread":0.24836014543995133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964173628","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.29650056,0.00013853697,0.6983585,0.0002247712,0.0000712228,0.00007310682,0.0001974999,0.0011842967,0.0032515167],"genre_scores_gemma":[0.7783439,0.0000752547,0.2202912,0.00007841926,0.000025862959,0.00010047112,0.00030234084,0.00015953147,0.00062294496],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982905,0.00005699972,0.000007301825,0.00004423051,0.000040501665,0.000021950971],"domain_scores_gemma":[0.9995977,0.00020470409,0.0000465422,0.000038264934,0.00009699673,0.000015788622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005417609,0.00049830927,0.00044218477,0.00036461666,0.0003363002,0.00043920797,0.00065130356,0.00055560435,0.00066585396],"category_scores_gemma":[0.0022116401,0.0003380463,0.00052171835,0.0005238109,0.00029525845,0.00041770225,0.00040956962,0.0009429348,0.00011296993],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015965601,0.000016158281,0.0009150537,0.0000066651137,0.000020620473,0.000016337342,0.0000129101045,0.9832902,0.0009850349,0.0008973648,0.00018903625,0.013634573],"study_design_scores_gemma":[0.0000050907006,0.00000651408,0.00020590743,0.0000012873613,0.000003836928,0.0000035721966,0.0000032420548,0.9983535,0.0005212079,0.0007661779,0.00012713954,0.000002572731],"about_ca_topic_score_codex":0.012272991,"about_ca_topic_score_gemma":0.012064112,"teacher_disagreement_score":0.012272991,"about_ca_system_score_codex":0.0005390214,"about_ca_system_score_gemma":0.00092190824,"threshold_uncertainty_score":0.024403095},"labels":[],"label_agreement":null},{"id":"W1964201649","doi":"10.1029/2005gl023642","title":"A regional index of northeast Pacific variability based on satellite altimeter data","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Sea-surface height; Climatology; Pacific decadal oscillation; Sea surface temperature; Altimeter; La Niña; Principal component analysis; Satellite; Environmental science; Geology; Oceanography; El Niño Southern Oscillation; Remote sensing","score_opus":0.07911672303946507,"score_gpt":0.32426901573285233,"score_spread":0.24515229269338726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964201649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9344141,0.00068879034,0.029790422,0.00015806938,0.00004143606,0.00007434006,0.021864258,0.0007736895,0.012194891],"genre_scores_gemma":[0.9851871,0.00021703701,0.0064435657,0.000024040777,0.000038437174,0.000039583316,0.0072279605,0.000038491096,0.0007839456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99969757,0.000041629177,0.000041015133,0.00008513061,0.00010670248,0.00002801207],"domain_scores_gemma":[0.99860007,0.00027311358,0.00050416536,0.0001415328,0.00041375382,0.00006729675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00065882487,0.00026788836,0.00022107676,0.0019463208,0.00014990714,0.0006348965,0.00022463879,0.00013530953,0.0010087144],"category_scores_gemma":[0.0020115662,0.00007255191,0.00023424077,0.0029732622,0.00016205446,0.0005037921,0.00039873636,0.00025149377,0.0002873161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010847661,0.000030088067,0.91439223,0.00005621422,0.00028760044,0.00007632064,0.000108238724,0.02314755,0.004354193,0.000852571,0.0022067216,0.0543798],"study_design_scores_gemma":[0.0000057026577,0.000049558046,0.96295077,0.000010387971,0.000050850213,0.00012397414,0.000099294484,0.031056492,0.0018158484,0.00039704464,0.0034222573,0.000017739289],"about_ca_topic_score_codex":0.0069732727,"about_ca_topic_score_gemma":0.009316578,"teacher_disagreement_score":0.0069732727,"about_ca_system_score_codex":0.00042450425,"about_ca_system_score_gemma":0.00028530677,"threshold_uncertainty_score":0.013865352},"labels":[],"label_agreement":null},{"id":"W1964297347","doi":"10.1029/2008gl035822","title":"Increasing winter baseflow and mean annual streamflow from possible permafrost thawing in the Northwest Territories, Canada","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":317,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Regina","funders":"","keywords":"Baseflow; Streamflow; Permafrost; Environmental science; Climatology; Context (archaeology); Climate change; Hydrology (agriculture); Water cycle; Geology; Drainage basin; Oceanography; Geography","score_opus":0.028557436483015904,"score_gpt":0.26665473995709393,"score_spread":0.23809730347407804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964297347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993923,0.00040172326,0.00009393872,0.0002232312,0.000006527639,0.000007803647,0.0024037913,0.000008376596,0.0029315692],"genre_scores_gemma":[0.99716383,0.0003130904,0.00016336872,0.00003316433,0.00000296892,0.0000033128656,0.0010287935,0.0000030261606,0.0012883985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998086,0.000014583596,0.000009115639,0.00003281979,0.00006913335,0.00006578926],"domain_scores_gemma":[0.99929285,0.000049954648,0.000107137515,0.000024331026,0.00034510548,0.00018059717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026424642,0.00011300785,0.00014528152,0.0006312843,0.001341434,0.00077133364,0.00040998193,0.00015031279,0.0015289314],"category_scores_gemma":[0.0010408132,0.00012291918,0.00016177286,0.0012535092,0.00040582768,0.0002502588,0.00029777474,0.00021121892,0.00010114816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053693802,0.000011664721,0.9902305,0.000014577481,0.00003912933,0.000115911054,0.00029183534,0.000329787,0.00043712722,0.00015705604,0.0008484821,0.007470311],"study_design_scores_gemma":[0.0000015384521,0.0000025500126,0.99877006,0.0000055892356,0.0000063134007,0.000026819045,0.0003390056,0.00021438823,0.0000725478,0.000017663668,0.0005409736,0.0000025666177],"about_ca_topic_score_codex":0.993818,"about_ca_topic_score_gemma":0.99801695,"teacher_disagreement_score":0.010966081,"about_ca_system_score_codex":0.010966081,"about_ca_system_score_gemma":0.013858963,"threshold_uncertainty_score":0.07956481},"labels":[],"label_agreement":null},{"id":"W1964414172","doi":"10.1002/2014gl062231","title":"Observed and simulated changes in Antarctic sea ice extent over the past 50 years","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Center for Neuroscience and Regenerative Medicine","keywords":"Geology; Climatology; Sea ice; Oceanography; Environmental science","score_opus":0.033262890494223284,"score_gpt":0.2664467400035269,"score_spread":0.23318384950930363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964414172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99767226,0.000046106397,0.00043379673,0.000031382577,0.000008493817,0.0000050919107,0.0010726056,0.000033000164,0.00069733907],"genre_scores_gemma":[0.99797934,0.000040454037,0.00043078032,0.0000113887545,0.0000030337692,0.000012466181,0.0013407498,0.0000041429516,0.00017765588],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998393,0.00003551852,0.0000185684,0.000059633072,0.000016742342,0.00003025705],"domain_scores_gemma":[0.9995485,0.00020763511,0.00009755895,0.000041265197,0.00006568972,0.000039380106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005348707,0.00036215567,0.00020898967,0.00037594576,0.0002351004,0.00038207183,0.0004395881,0.00053154636,0.0011306739],"category_scores_gemma":[0.0012209906,0.00021265406,0.0005198172,0.0005906808,0.00032868888,0.0004313442,0.00023949682,0.0002921347,0.00015745757],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024281527,0.00010546966,0.11588657,0.000040078674,0.00016358566,0.00009407884,0.000060554696,0.877656,0.0010464017,0.0003094714,0.00048292617,0.003912098],"study_design_scores_gemma":[0.00016015045,0.00032803597,0.16831596,0.000024924158,0.00011995642,0.00009357793,0.00014227745,0.82729423,0.001794049,0.00034845297,0.0013361403,0.000042213123],"about_ca_topic_score_codex":0.032827456,"about_ca_topic_score_gemma":0.03430249,"teacher_disagreement_score":0.032827456,"about_ca_system_score_codex":0.00079755834,"about_ca_system_score_gemma":0.0004363897,"threshold_uncertainty_score":0.06527281},"labels":[],"label_agreement":null},{"id":"W1964442347","doi":"10.1029/2001gl014476","title":"A comparison of mesospheric temperatures from the Canadian Middle Atmosphere Model and HALOE observations: Zonal mean and signature of the solar diurnal tide","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Solstice; Equinox; Atmosphere (unit); Sunset; Mesosphere; Atmospheric sciences; Sunrise; Environmental science; Atmospheric model; Stratopause; Occultation; Climatology; Geology; Meteorology; Stratosphere; Geography; Ionosphere; Physics; Latitude; Astronomy","score_opus":0.07321813796389556,"score_gpt":0.27057348237551804,"score_spread":0.19735534441162247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964442347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831014,0.00045170932,0.0016156906,0.00023679018,0.00003436343,0.000025706086,0.007692952,0.0002647459,0.006576671],"genre_scores_gemma":[0.9910595,0.00017120344,0.0017972218,0.00002788063,0.0000057740563,0.000011235234,0.0062328596,0.000030374647,0.0006639487],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997962,0.000015219436,0.000006469197,0.00003864709,0.00009026178,0.000053330386],"domain_scores_gemma":[0.99967647,0.000023018441,0.000019441084,0.000018806877,0.000222323,0.00003987313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035167154,0.00031604708,0.00015439547,0.0005557924,0.0007457703,0.0008323499,0.000570661,0.00022005342,0.001052568],"category_scores_gemma":[0.000924937,0.00016211258,0.0002914709,0.000980217,0.0001369628,0.0003460932,0.00035334646,0.0002610121,0.00016211272],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011959241,0.000105911946,0.8140371,0.00017982995,0.0005136425,0.00022915474,0.0006813349,0.06240666,0.020029714,0.0024524594,0.009534117,0.088634156],"study_design_scores_gemma":[0.00003718033,0.000027571537,0.94439965,0.000022255213,0.00006701669,0.000026746171,0.00021180986,0.04355156,0.0032890383,0.00017324618,0.008156391,0.000037597296],"about_ca_topic_score_codex":0.93585885,"about_ca_topic_score_gemma":0.96754575,"teacher_disagreement_score":0.93585885,"about_ca_system_score_codex":0.0055925553,"about_ca_system_score_gemma":0.0057880506,"threshold_uncertainty_score":0.12903774},"labels":[],"label_agreement":null},{"id":"W1964719424","doi":"10.1029/2005gl023693","title":"Recent primary production increases in arctic lakes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":188,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Arctic; Oceanography; Sediment; Context (archaeology); Environmental science; Chlorophyll a; Primary producers; Geology; Physical geography; Phytoplankton; Ecology; Geography; Geomorphology; Paleontology; Nutrient; Biology","score_opus":0.035931507858093674,"score_gpt":0.29197572360386415,"score_spread":0.25604421574577046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964719424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997244,0.0011123754,0.00010740861,0.00014501151,0.000011913332,0.0000015693919,0.0004675965,0.00000826452,0.0009017999],"genre_scores_gemma":[0.99806803,0.00078983145,0.000113085225,0.00003440813,0.000034324457,0.000003086318,0.00056213886,0.0000021488618,0.0003930341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998907,0.000009553309,0.0000075107873,0.00003477918,0.000031751206,0.000025793048],"domain_scores_gemma":[0.999356,0.00004171174,0.0001827764,0.000023922767,0.00030371026,0.00009201432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003900959,0.00018082764,0.00015023956,0.0006607468,0.00065710675,0.0006971622,0.00015598013,0.00031188558,0.0008797848],"category_scores_gemma":[0.00095897174,0.00017313688,0.00012530382,0.00072453223,0.00036129303,0.00043306162,0.00032225918,0.00024523804,0.00021239449],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028286874,0.000034415272,0.96480286,0.00007499029,0.00009473894,0.00021556758,0.0007899353,0.0004536448,0.016307471,0.00023388484,0.0005867222,0.01612294],"study_design_scores_gemma":[0.000001948846,0.000016256088,0.99830806,0.0000026816442,0.000008998524,0.00008890302,0.00008836811,0.00008419223,0.0004075917,0.000023035256,0.00096738467,0.0000024195444],"about_ca_topic_score_codex":0.07937936,"about_ca_topic_score_gemma":0.124555945,"teacher_disagreement_score":0.07937936,"about_ca_system_score_codex":0.0014722722,"about_ca_system_score_gemma":0.0006218321,"threshold_uncertainty_score":0.15783465},"labels":[],"label_agreement":null},{"id":"W1964909389","doi":"10.1029/2008gl034470","title":"A millennial‐scale record of Arctic Ocean sea ice variability and the demise of the Ellesmere Island ice shelves","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":108,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact; Geological Survey of Canada; Natural Resources Canada; University of Alberta","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; University of Ottawa","keywords":"Sea ice; Oceanography; Geology; Arctic ice pack; Ice shelf; Antarctic sea ice; Cryosphere; Iceberg; Arctic sea ice decline; Arctic; Fjord; Climatology; Physical geography; Geography","score_opus":0.016112858640651363,"score_gpt":0.23775154512222008,"score_spread":0.2216386864815687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964909389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99671704,0.00060517533,0.00016455808,0.00009625335,0.000009354161,0.0000024304245,0.0010713146,0.000008962585,0.0013249796],"genre_scores_gemma":[0.9974241,0.00050996244,0.0002951031,0.000045903445,0.000015449514,0.0000032767675,0.0012535418,0.0000035355608,0.00044914696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999645,0.000003788592,0.0000031835127,0.000011157083,0.0000067395667,0.000010601887],"domain_scores_gemma":[0.99974483,0.000030434536,0.00011651072,0.000025926543,0.000052410327,0.000029764187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023431939,0.000088174595,0.0000739528,0.0005034882,0.00019561911,0.0004644372,0.000103865605,0.00017085095,0.00090875285],"category_scores_gemma":[0.0005650295,0.000083217434,0.00006191408,0.0005827872,0.00021721321,0.00042647467,0.00044100525,0.00021972743,0.00018519218],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040764357,0.000015423611,0.9749493,0.00002548262,0.00003990764,0.000104132865,0.0005318066,0.00029760838,0.003095725,0.00018251153,0.0009728116,0.019744605],"study_design_scores_gemma":[5.3481176e-7,0.0000044914473,0.9983267,0.0000046171613,0.000004508068,0.000031408315,0.000090920075,0.00006156415,0.000169545,0.000012641102,0.0012918327,0.0000011862941],"about_ca_topic_score_codex":0.01289058,"about_ca_topic_score_gemma":0.04021958,"teacher_disagreement_score":0.01289058,"about_ca_system_score_codex":0.00025539793,"about_ca_system_score_gemma":0.00018361607,"threshold_uncertainty_score":0.02563107},"labels":[],"label_agreement":null},{"id":"W1964920345","doi":"10.1029/2004gl021112","title":"The effect of vertical measurement resolution on the correlation structure of a ground penetrating radar reflection image","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Radar; Geology; Remote sensing; Ground-penetrating radar; Reflection (computer programming); Radar imaging; Resolution (logic); Range (aeronautics); Horizontal and vertical; Image resolution; Radar horizon; Geodesy; Optics; Continuous-wave radar; Physics; Materials science; Computer science","score_opus":0.03644449384364897,"score_gpt":0.3233812261642073,"score_spread":0.28693673232055833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1964920345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6342964,0.0026471203,0.35629496,0.00046499827,0.000096591335,0.00006422072,0.0005528815,0.00082015456,0.004762738],"genre_scores_gemma":[0.9475573,0.0006960813,0.050661262,0.00007390935,0.000031945194,0.000028604481,0.00038340504,0.0001349356,0.00043265586],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9978217,0.0006986638,0.00016819661,0.00035883655,0.00074007077,0.00021249091],"domain_scores_gemma":[0.9588589,0.03355458,0.0016122009,0.0023781068,0.003353882,0.00024230119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004945416,0.0005231191,0.00032359626,0.00066231325,0.00027523658,0.0007930743,0.00029446316,0.0005823378,0.0008877098],"category_scores_gemma":[0.03117635,0.00066907814,0.00034490318,0.0008780842,0.0005779981,0.0011595996,0.0008252516,0.000697804,0.00032068542],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016935174,0.00015387891,0.08465561,0.0007372806,0.00038865276,0.000814165,0.0007539223,0.171755,0.4480292,0.0047001927,0.0014604011,0.2848582],"study_design_scores_gemma":[0.000080166385,0.0009109352,0.23645385,0.00015011163,0.00046552267,0.0017935402,0.0003647132,0.3806221,0.37159467,0.0038965899,0.0034673603,0.00020039905],"about_ca_topic_score_codex":0.0014566324,"about_ca_topic_score_gemma":0.0013275665,"teacher_disagreement_score":0.004945416,"about_ca_system_score_codex":0.00043280763,"about_ca_system_score_gemma":0.0003910394,"threshold_uncertainty_score":0.02615416},"labels":[],"label_agreement":null},{"id":"W1965073820","doi":"10.1029/2005gl022750","title":"Observations of premonitory acoustic emission and slip nucleation during a stick slip experiment in smooth faulted Westerly granite","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Nucleation; Slip (aerodynamics); Acoustic emission; Fault plane; Instability; Geology; Amplitude; Seismology; Waveform; Fault (geology); Acoustics; Mechanics; Physics; Optics","score_opus":0.045302379854108725,"score_gpt":0.29285757180455846,"score_spread":0.24755519195044973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965073820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99962914,0.000024894409,0.00019568087,0.000002405555,8.9972394e-7,0.000003524803,0.00002511846,0.000006875517,0.0001113632],"genre_scores_gemma":[0.9994949,0.0000307293,0.00022029025,0.0000047256726,0.000002387571,0.0000065837808,0.00008409962,0.0000025837373,0.0001535308],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999157,0.000009284623,0.0000035770872,0.000020180585,0.000025780413,0.00002548604],"domain_scores_gemma":[0.99976724,0.00006273326,0.000043846238,0.000018170162,0.00003474873,0.000073176336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001315605,0.00015926064,0.00024637821,0.0002945137,0.00019593177,0.00016614853,0.00015397382,0.00021380783,0.000521931],"category_scores_gemma":[0.00029897603,0.00014447351,0.00010641375,0.00014090686,0.00027166982,0.00008972647,0.00023910619,0.00028381732,0.00011938391],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037270327,0.000044880133,0.013683302,0.000020372656,0.000010520613,0.00020305204,0.00013415955,0.00016805792,0.9831457,0.00002643361,0.00002850609,0.002162225],"study_design_scores_gemma":[0.00004161013,0.0016970416,0.6834238,0.000007532778,0.000025364861,0.00031297267,0.0002352705,0.0030343665,0.31066224,0.00006598749,0.00047484855,0.000018891566],"about_ca_topic_score_codex":0.0014316973,"about_ca_topic_score_gemma":0.0031641736,"teacher_disagreement_score":0.0014316973,"about_ca_system_score_codex":0.00020024895,"about_ca_system_score_gemma":0.0000820387,"threshold_uncertainty_score":0.0028467178},"labels":[],"label_agreement":null},{"id":"W1965170232","doi":"10.1029/2004gl020840","title":"Effects of time averaging on climate regimes","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Institute for Advanced Research; University of Victoria","funders":"Canadian Institute for Advanced Research","keywords":"Extratropical cyclone; Climatology; Climate model; Environmental science; Climate change; Northern Hemisphere; Atmospheric sciences; Atmosphere (unit); Gaussian; Residence time (fluid dynamics); Statistical physics; Meteorology; Geology; Physics","score_opus":0.018220121409214442,"score_gpt":0.28637607509667273,"score_spread":0.2681559536874583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965170232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91925156,0.0015036665,0.073444344,0.00039920883,0.00018982375,0.000024290046,0.00035619934,0.00050913636,0.004321807],"genre_scores_gemma":[0.9959623,0.00032690054,0.0032442496,0.000046690046,0.00006501946,0.000011968682,0.0001191598,0.00010764185,0.0001159701],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9989723,0.0003631164,0.000109834335,0.00021246182,0.00019428585,0.00014808467],"domain_scores_gemma":[0.98147774,0.014219059,0.0014910791,0.0019384178,0.00048095244,0.00039273742],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00356102,0.00045217833,0.00041767056,0.0005824035,0.00056143804,0.0007690269,0.00038579392,0.00042249603,0.0009730745],"category_scores_gemma":[0.021921007,0.00018437959,0.00093149085,0.0010110085,0.00073664123,0.0019936508,0.0008237895,0.0007345771,0.00007591989],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012704384,0.00014235286,0.07250237,0.00036111948,0.000997832,0.0009381165,0.00071074447,0.69863397,0.091054104,0.028766168,0.0012948836,0.10332788],"study_design_scores_gemma":[0.00005745842,0.00034487218,0.1365982,0.000055032557,0.0006163763,0.0004832063,0.00019210338,0.7986052,0.029066026,0.03061247,0.0031886478,0.00018043483],"about_ca_topic_score_codex":0.0022165785,"about_ca_topic_score_gemma":0.0016956369,"teacher_disagreement_score":0.00356102,"about_ca_system_score_codex":0.00046501047,"about_ca_system_score_gemma":0.00034145502,"threshold_uncertainty_score":0.018832684},"labels":[],"label_agreement":null},{"id":"W1965190544","doi":"10.1029/2006gl025676","title":"Spatial patterns of ground heat gain in the Northern Hemisphere","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Northern Hemisphere; Heat flux; Energy balance; Latent heat; Sensible heat; Environmental science; Flux (metallurgy); Climatology; Thermal; Geology; Atmospheric sciences; Heat transfer; Geophysics; Meteorology; Physics; Materials science; Mechanics; Thermodynamics","score_opus":0.027470310369764838,"score_gpt":0.2782843778769449,"score_spread":0.25081406750718005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965190544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988961,0.000056999077,0.000042402775,0.000021671725,8.90068e-7,6.178288e-7,0.00025360443,0.000012142773,0.000715523],"genre_scores_gemma":[0.99947983,0.000032152206,0.00003630541,0.0000062573727,0.0000027455785,0.0000013467218,0.00028230803,0.0000020170892,0.00015709408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999422,0.0000074467894,0.0000024514297,0.000018693183,0.000010354286,0.000018850236],"domain_scores_gemma":[0.99982363,0.000032908505,0.00006796565,0.000018674895,0.000032834872,0.00002405203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013435389,0.00007277858,0.000121717836,0.0004064555,0.00012151443,0.0003787431,0.000089034045,0.00013479107,0.0011483972],"category_scores_gemma":[0.0004234526,0.000067524794,0.00010891716,0.00051417283,0.00018538442,0.00016722216,0.00015909734,0.00009015358,0.00017904163],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032400776,0.000029883611,0.9565604,0.0000359952,0.00009718703,0.00015153793,0.00117081,0.0029239005,0.017684614,0.00029656474,0.0011384947,0.019586695],"study_design_scores_gemma":[0.0000014940478,0.0000046801533,0.9992631,0.0000011789002,0.0000038448875,0.000016625849,0.00006548928,0.00027793727,0.00014132523,0.000018545652,0.00020427523,0.0000014760699],"about_ca_topic_score_codex":0.021209164,"about_ca_topic_score_gemma":0.032407347,"teacher_disagreement_score":0.021209164,"about_ca_system_score_codex":0.0003248983,"about_ca_system_score_gemma":0.000104067454,"threshold_uncertainty_score":0.04217142},"labels":[],"label_agreement":null},{"id":"W1965626242","doi":"10.1029/2004gl022296","title":"Change in ozone trends at southern high latitudes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ozone; Montreal Protocol; Environmental science; Ozone layer; Polar vortex; Ozone depletion; Atmospheric sciences; Climatology; Latitude; Satellite; Stratosphere; High latitude; Meteorology; Geology; Geography; Physics","score_opus":0.04918902248705134,"score_gpt":0.3016785793027746,"score_spread":0.25248955681572327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965626242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987708,0.000101007165,0.000023123295,0.000024325878,0.0000021001206,9.123139e-7,0.00049575005,0.000005937517,0.0005760209],"genre_scores_gemma":[0.9985915,0.00011595997,0.000045647826,0.000014353044,0.0000054370057,0.0000018793284,0.0009480376,0.0000012655994,0.00027588796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.000008916473,0.0000050308654,0.00001742858,0.000016881151,0.000019175443],"domain_scores_gemma":[0.9996985,0.000041131978,0.00012696502,0.000016950997,0.00006716036,0.000049235907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020637171,0.000115785224,0.00014448633,0.0006744527,0.0002038069,0.00045861353,0.00006728812,0.00021965831,0.0011524349],"category_scores_gemma":[0.00036650777,0.000078185025,0.00020411788,0.00092141825,0.00012928752,0.00017153296,0.00018356147,0.00014022463,0.00026611204],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001775605,0.00003058093,0.9866291,0.000034080043,0.00008932852,0.000079889214,0.00038289372,0.00066020514,0.006379527,0.00013361749,0.00038075552,0.0050224657],"study_design_scores_gemma":[0.0000013263211,0.000025681891,0.99936956,0.0000017539377,0.0000083118,0.000014949431,0.00006434857,0.000078651516,0.00012097261,0.000008328034,0.00030516143,0.0000010985003],"about_ca_topic_score_codex":0.017523533,"about_ca_topic_score_gemma":0.02813454,"teacher_disagreement_score":0.017523533,"about_ca_system_score_codex":0.00027916435,"about_ca_system_score_gemma":0.00015689526,"threshold_uncertainty_score":0.034843087},"labels":[],"label_agreement":null},{"id":"W1965632437","doi":"10.1029/2007gl032388","title":"Stabilizing climate requires near‐zero emissions","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Global Energy and Sustainability Research","field":"Energy","cited_by":605,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"","keywords":"Greenhouse gas; Environmental science; Atmosphere (unit); Climate change; Climate model; Global warming; Atmospheric sciences; Runaway climate change; Climatology; Climate commitment; Global temperature; Greenhouse effect; Effects of global warming; Meteorology; Geology; Geography","score_opus":0.05821922129309021,"score_gpt":0.3499205722666138,"score_spread":0.2917013509735236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965632437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93778145,0.0002948231,0.047942895,0.0010527194,0.00006095768,0.00001979221,0.00028696898,0.00014447511,0.012416003],"genre_scores_gemma":[0.99799407,0.00010613908,0.0013321167,0.00004138418,0.000009403576,0.000012356265,0.00003627824,0.000010015382,0.0004583313],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997849,0.000076999786,0.000009460549,0.0000397699,0.000032063163,0.000056928486],"domain_scores_gemma":[0.99956614,0.00020633987,0.00008265492,0.000057566678,0.000037210964,0.00005006142],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043716436,0.00038921536,0.00052018295,0.00016294338,0.0004862932,0.0010207186,0.00044458988,0.00096438214,0.0021495721],"category_scores_gemma":[0.00172327,0.00022640004,0.00063617394,0.0001446523,0.0008146515,0.0015509172,0.0010801381,0.00078412774,0.00015648021],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012696318,0.00002408142,0.005539398,0.000070707385,0.000056954832,0.0001691128,0.000089522844,0.9397371,0.008965366,0.041926395,0.00034915312,0.0029452126],"study_design_scores_gemma":[0.000095153286,0.00016044665,0.007238974,0.000019086421,0.000074701275,0.00015907739,0.00018444397,0.92000073,0.0026885127,0.06721274,0.0021136808,0.000052556104],"about_ca_topic_score_codex":0.0042129946,"about_ca_topic_score_gemma":0.0028514888,"teacher_disagreement_score":0.0042129946,"about_ca_system_score_codex":0.0006057586,"about_ca_system_score_gemma":0.0007676621,"threshold_uncertainty_score":0.008376956},"labels":[],"label_agreement":null},{"id":"W1965710373","doi":"10.1029/2003gl018978","title":"Annual cycles of sea ice and phytoplankton in Cape Bathurst polynya, southeastern Beaufort Sea, Canadian Arctic","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":170,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Sea ice; Phytoplankton; Arctic; Environmental science; Arctic sea ice decline; Bloom; Cape; SeaWiFS; Arctic ice pack; Stratification (seeds); Geology; Climatology; Antarctic sea ice; Geography; Nutrient; Ecology","score_opus":0.014807108382900988,"score_gpt":0.246672713224145,"score_spread":0.23186560484124402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965710373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962943,0.0005798088,0.000039013765,0.00013102122,0.000006334241,0.000010158586,0.0019607365,0.000008534552,0.00097014033],"genre_scores_gemma":[0.9966628,0.00040996444,0.00017250537,0.000051156683,0.000004700424,0.000009219085,0.0018255027,0.0000040241835,0.0008599052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977344,0.000016999376,0.000015182876,0.000037950005,0.00007894328,0.00007757032],"domain_scores_gemma":[0.99872905,0.00008218078,0.00021699915,0.000033598026,0.0006875054,0.00025060147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037590397,0.00023828869,0.00021791602,0.0016708568,0.0014631706,0.00076427707,0.0005404825,0.00028104548,0.00081859325],"category_scores_gemma":[0.0014273347,0.0002234594,0.00022797525,0.0025075732,0.00058081344,0.0003079943,0.00039955918,0.00020109657,0.00011755163],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001071142,0.000016025208,0.98991185,0.000037803304,0.00007829546,0.00013604421,0.000961475,0.0006495087,0.0011514683,0.000095160925,0.0011905587,0.005664594],"study_design_scores_gemma":[0.000002337321,0.0000036546005,0.9989648,0.0000060975713,0.000007309567,0.000018447325,0.00022063142,0.00016587261,0.000041933443,0.000006180177,0.00055886654,0.000003885593],"about_ca_topic_score_codex":0.9938234,"about_ca_topic_score_gemma":0.99793845,"teacher_disagreement_score":0.01420325,"about_ca_system_score_codex":0.01420325,"about_ca_system_score_gemma":0.009065698,"threshold_uncertainty_score":0.10305226},"labels":[],"label_agreement":null},{"id":"W1965780718","doi":"10.1029/2006gl027775","title":"Differences in geomagnetic storms driven by magnetic clouds and ICME sheath regions","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Ring current; Substorm; Geomagnetic storm; Physics; Geophysics; Magnetosphere; Storm; Earth's magnetic field; Magnetic cloud; Solar wind; Electrojet; Coronal mass ejection; Interplanetary spaceflight; Plasma sheet; Interplanetary magnetic field; Atmospheric sciences; Magnetic field; Geology; Meteorology","score_opus":0.01475194054156352,"score_gpt":0.2704310207818011,"score_spread":0.25567908024023756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965780718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99939656,0.00002767081,0.000032395314,0.0000031524346,9.750312e-7,0.000001972115,0.000090673384,0.0000030663998,0.0004435412],"genre_scores_gemma":[0.99949455,0.000021308488,0.000029467277,0.0000024967098,0.0000020126554,0.0000017460839,0.00023686848,0.0000018127091,0.00020975921],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999027,0.000008447856,0.000008867229,0.000016973807,0.000023407641,0.000039628325],"domain_scores_gemma":[0.9993273,0.000119688455,0.00026119335,0.0000413989,0.000084476065,0.00016591379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001604826,0.000108517204,0.00016673845,0.0007208298,0.00022159315,0.00033260428,0.00009321906,0.00013345436,0.0009400321],"category_scores_gemma":[0.0007522441,0.00007291466,0.00014362478,0.0003330012,0.00017590015,0.00016786916,0.00031220837,0.000103370774,0.00018044647],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007257983,0.00004288074,0.941962,0.000023402737,0.00007586841,0.0003599712,0.0007070392,0.000692167,0.044788215,0.00027963385,0.00018567486,0.010157221],"study_design_scores_gemma":[0.0000027765254,0.000059401995,0.99843854,0.0000010136663,0.0000065710233,0.0001386702,0.00011583103,0.00019777396,0.00074504915,0.000021769092,0.000269973,0.0000027039273],"about_ca_topic_score_codex":0.0015364292,"about_ca_topic_score_gemma":0.0029110196,"teacher_disagreement_score":0.0015364292,"about_ca_system_score_codex":0.00022273789,"about_ca_system_score_gemma":0.00010819019,"threshold_uncertainty_score":0.0031446815},"labels":[],"label_agreement":null},{"id":"W1965818384","doi":"10.1029/2006gl028009","title":"Thermochemical structure and dynamics of the African superplume","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":214,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Buoyancy; Mantle (geology); Plume; Convection; Geology; Geophysics; Core–mantle boundary; Mechanics; Physics; Meteorology","score_opus":0.013356883081099127,"score_gpt":0.25344316541233064,"score_spread":0.24008628233123153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965818384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98820424,0.00022803522,0.007813785,0.00011064807,0.0000035898313,0.000007451815,0.00019574075,0.000066475535,0.0033700166],"genre_scores_gemma":[0.99753153,0.00013788321,0.0018649815,0.000008499895,0.0000025897443,0.000008173537,0.00011103809,0.000013719987,0.00032156208],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999972,0.0000044587337,0.0000011027113,0.00000695227,0.000006428995,0.000009120971],"domain_scores_gemma":[0.9999536,0.0000075173803,0.000013041484,0.0000088713505,0.000006843236,0.000010244181],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004517895,0.00028525974,0.00016591977,0.00036229083,0.0003472281,0.00076030433,0.00060028,0.00041677727,0.0011446412],"category_scores_gemma":[0.00019537081,0.00033734672,0.0004438178,0.0003290206,0.00038830144,0.0005525426,0.00057705736,0.00026744787,0.00019809126],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002488626,0.000044534772,0.05297704,0.000091784495,0.0001015525,0.0010019699,0.00062284333,0.8114599,0.10278876,0.011071673,0.0005138823,0.019077174],"study_design_scores_gemma":[0.000028752032,0.00004274165,0.054236986,0.000016142694,0.000023309967,0.00038976382,0.00012616233,0.93411577,0.00478069,0.0028894655,0.0033042617,0.000046006477],"about_ca_topic_score_codex":0.017337587,"about_ca_topic_score_gemma":0.010205302,"teacher_disagreement_score":0.017337587,"about_ca_system_score_codex":0.0006614241,"about_ca_system_score_gemma":0.000474216,"threshold_uncertainty_score":0.03447336},"labels":[],"label_agreement":null},{"id":"W1965858414","doi":"10.1029/2008gl035863","title":"Atmospheric complexity or scale by scale simplicity?","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"","keywords":"Radiance; Cascade; Simplicity; Scale (ratio); Satellite; Meteorology; Atmospheric wave; Remote sensing; Microwave; Radar; Nonlinear system; Physics; Environmental science; Wave propagation; Geology; Gravity wave; Optics; Computer science; Astronomy; Telecommunications","score_opus":0.09585003029803876,"score_gpt":0.3086315547541306,"score_spread":0.21278152445609186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965858414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.52126276,0.0027520978,0.4055275,0.021347152,0.000793948,0.00013074533,0.00027818032,0.00090008194,0.04700757],"genre_scores_gemma":[0.97887385,0.0009039286,0.015665594,0.00062349334,0.00038512703,0.00003881456,0.000048797778,0.000094529234,0.003365912],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996662,0.00008368939,0.000015715745,0.000079651545,0.00009734293,0.00005732349],"domain_scores_gemma":[0.99804074,0.000819897,0.00038619188,0.0004875214,0.00011950678,0.0001462408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000919036,0.00032449,0.0006673447,0.00025907796,0.00043698767,0.0010662097,0.0007746081,0.0007567223,0.0036448196],"category_scores_gemma":[0.0065302444,0.00029787183,0.0007996149,0.00025536236,0.0019460327,0.0064530377,0.0013392173,0.0013626232,0.00036214996],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013280708,0.00006317328,0.018816024,0.0002762638,0.00028357533,0.00056954665,0.00095183204,0.14555424,0.0068027936,0.76941335,0.0057827635,0.051353615],"study_design_scores_gemma":[0.000040412047,0.000072289615,0.012946812,0.00004598541,0.00006388199,0.00021759653,0.00031691205,0.3542717,0.0010992119,0.6188156,0.012056344,0.000053203785],"about_ca_topic_score_codex":0.0022121747,"about_ca_topic_score_gemma":0.0015328571,"teacher_disagreement_score":0.0036448196,"about_ca_system_score_codex":0.0005422601,"about_ca_system_score_gemma":0.00046237168,"threshold_uncertainty_score":0.012193143},"labels":[],"label_agreement":null},{"id":"W1965990157","doi":"10.1029/2002gl016224","title":"Impact of deep‐ocean carbon sequestration on atmospheric CO<sub>2</sub> and on surface‐water chemistry","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Carbon sequestration; Environmental science; Supersaturation; Mixed layer; Atmospheric sciences; Carbon fibers; Carbon cycle; Atmospheric carbon cycle; Carbon dioxide; Environmental chemistry; Climatology; Chemistry; Geology; Materials science; Ecosystem","score_opus":0.017899455450036572,"score_gpt":0.2768517743234862,"score_spread":0.2589523188734496,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1965990157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961027,0.00017893375,0.0008684478,0.00016657685,0.000012540689,0.000006182084,0.0002845789,0.000042990894,0.002336989],"genre_scores_gemma":[0.99946815,0.00008162462,0.00016998246,0.00002495869,0.0000014963849,0.0000028946804,0.000072692244,0.0000029952212,0.00017511456],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998311,0.00006253799,0.0000066317084,0.00001815151,0.000020822044,0.000060615806],"domain_scores_gemma":[0.999419,0.00035554584,0.000074740514,0.000035576835,0.00005185762,0.000063433574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037498484,0.00066014606,0.0003946627,0.0001980516,0.0002447559,0.00046651333,0.0002628075,0.00064249284,0.0023922385],"category_scores_gemma":[0.0010708036,0.00031666446,0.0004997958,0.00019541907,0.00044131055,0.0005578564,0.0006996445,0.0002848985,0.0001518127],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026742998,0.00016381938,0.0743133,0.0002781564,0.0003370771,0.0007575506,0.000055094213,0.80600566,0.09820946,0.0036199219,0.00055404904,0.013031634],"study_design_scores_gemma":[0.00040281814,0.0017029414,0.123137616,0.000056244913,0.00056766503,0.00025384827,0.00044433962,0.76210433,0.10141086,0.007071941,0.00274848,0.00009894787],"about_ca_topic_score_codex":0.011636569,"about_ca_topic_score_gemma":0.012064862,"teacher_disagreement_score":0.011636569,"about_ca_system_score_codex":0.0008974574,"about_ca_system_score_gemma":0.0010016111,"threshold_uncertainty_score":0.023137629},"labels":[],"label_agreement":null},{"id":"W1966175738","doi":"10.1029/2006gl027692","title":"Modelling deep seasonal temperature changes in the Labrador Sea","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Advection; Isopycnal; Mooring; Geology; Oceanography; Hydrography; Climatology; Continental shelf; Sea surface temperature; Mixed layer","score_opus":0.020340653945056603,"score_gpt":0.24539331148163207,"score_spread":0.22505265753657547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966175738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887522,0.000099206154,0.007850735,0.0001144551,0.000016851147,0.000011810355,0.0006648969,0.0002577449,0.0022320917],"genre_scores_gemma":[0.99708,0.00006876942,0.0015312034,0.000016379747,0.0000055875316,0.000015020956,0.00036051328,0.000022493092,0.0009000734],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999366,0.000013068466,0.000003949838,0.000018214396,0.0000063265397,0.000021859238],"domain_scores_gemma":[0.99991024,0.000023390747,0.000023598044,0.000012367009,0.000013945796,0.000016427306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014566422,0.00049649103,0.00041464742,0.0002202409,0.00028100368,0.0008197079,0.0006518445,0.0005417872,0.00086633716],"category_scores_gemma":[0.0004405983,0.0002878222,0.0005114517,0.0003371104,0.00027371096,0.00046726878,0.00043450727,0.00037315636,0.00016282906],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009003084,0.00002756172,0.012881333,0.000016044612,0.000048808888,0.00006014324,0.00003955062,0.97991127,0.0021499305,0.0004921256,0.000333033,0.003950155],"study_design_scores_gemma":[0.000020248604,0.00003067975,0.0057081175,0.0000032716637,0.000013501618,0.00000941873,0.0000258851,0.9930462,0.0004797699,0.00015512186,0.0004976257,0.000010078241],"about_ca_topic_score_codex":0.10988822,"about_ca_topic_score_gemma":0.072695814,"teacher_disagreement_score":0.10988822,"about_ca_system_score_codex":0.0012013871,"about_ca_system_score_gemma":0.00074881496,"threshold_uncertainty_score":0.21849722},"labels":[],"label_agreement":null},{"id":"W1966341729","doi":"10.1029/2001gl014357","title":"A glaciation indirect aerosol effect caused by soot aerosols","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":316,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Atmospheric sciences; Glacial period; Soot; Environmental science; Ice nucleus; Precipitation; Climatology; Geology; Meteorology; Chemistry; Geomorphology; Physics","score_opus":0.026993888049965376,"score_gpt":0.2620583779774981,"score_spread":0.2350644899275327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966341729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.983982,0.0012983662,0.0012430698,0.00031204117,0.00006830223,0.000027579443,0.0005420619,0.00024812244,0.0122784665],"genre_scores_gemma":[0.99746597,0.0005249134,0.00025435982,0.00009826029,0.0000609627,0.0000064200185,0.00022653327,0.000019494812,0.0013430354],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999833,0.000026541991,0.000007159544,0.00003004927,0.000048866917,0.00005442932],"domain_scores_gemma":[0.9995758,0.00012638711,0.00011579499,0.000046896457,0.000058444235,0.00007672905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016379985,0.0006117675,0.0004600155,0.00037233197,0.00038900782,0.00046424998,0.0002378606,0.00047892227,0.0069470084],"category_scores_gemma":[0.0004725701,0.00023362026,0.0005827714,0.0003390979,0.00046662072,0.00035329524,0.000887857,0.00040912864,0.00046031404],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020604653,0.00023256661,0.40711784,0.0010889051,0.000969457,0.0031992632,0.0004326174,0.017744767,0.5145393,0.0037665337,0.0024875763,0.04636067],"study_design_scores_gemma":[0.00007916761,0.00042182094,0.96363574,0.00001790329,0.0002919832,0.0005928964,0.00010913113,0.0028005496,0.02882961,0.00089243427,0.0023072863,0.00002154996],"about_ca_topic_score_codex":0.003778451,"about_ca_topic_score_gemma":0.004450608,"teacher_disagreement_score":0.0069470084,"about_ca_system_score_codex":0.0004985102,"about_ca_system_score_gemma":0.00025308662,"threshold_uncertainty_score":0.02324009},"labels":[],"label_agreement":null},{"id":"W1966391652","doi":"10.1029/2009gl037525","title":"Rapid change in freshwater content of the Arctic Ocean","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":254,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs","keywords":"Thermohaline circulation; Oceanography; Ocean gyre; Hydrography; Shutdown of thermohaline circulation; Ridge; Arctic; Climatology; Arctic dipole anomaly; Geology; Arctic sea ice decline; Oceanic basin; Circumpolar deep water; Lead (geology); Environmental science; North Atlantic Deep Water; Arctic ice pack; Structural basin; Antarctic sea ice; Fishery","score_opus":0.06325676295803265,"score_gpt":0.2747809293654265,"score_spread":0.21152416640739383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966391652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99644345,0.00070804683,0.00011398661,0.00004374508,0.000010222015,0.0000020229274,0.00071948435,0.000010979556,0.0019480335],"genre_scores_gemma":[0.99825126,0.00057446887,0.00017239334,0.000025818183,0.00001159182,0.0000024387314,0.00054841954,0.0000037232237,0.00040996907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.0000047892486,0.0000037932714,0.000019163774,0.000020897403,0.000013380435],"domain_scores_gemma":[0.99991083,0.0000052171836,0.000021677773,0.0000040823807,0.000041609277,0.000016507189],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000975122,0.00014613697,0.00013056683,0.00064513227,0.00029743876,0.00037461182,0.0000963713,0.00010536556,0.0007016363],"category_scores_gemma":[0.00019034544,0.00008322759,0.000126641,0.0005505043,0.00016662941,0.00028625113,0.00023201291,0.000114186834,0.00020087886],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003854293,0.00003338499,0.6835741,0.00014364369,0.00017140854,0.00024314795,0.00044469573,0.001551707,0.25784507,0.0004941071,0.0007063587,0.054406926],"study_design_scores_gemma":[0.0000018698116,0.000033006938,0.99376315,0.000006033052,0.000010518589,0.00008372649,0.00009456435,0.00022881334,0.0040198243,0.00006980669,0.0016837112,0.000004935533],"about_ca_topic_score_codex":0.023599941,"about_ca_topic_score_gemma":0.020785123,"teacher_disagreement_score":0.023599941,"about_ca_system_score_codex":0.0006409547,"about_ca_system_score_gemma":0.00031074378,"threshold_uncertainty_score":0.046925187},"labels":[],"label_agreement":null},{"id":"W1966462928","doi":"10.1029/2006gl028756","title":"Response of the Atlantic meridional overturning circulation to increasing atmospheric CO<sub>2</sub>: Sensitivity to mean climate state","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; University of Victoria","funders":"Canada Research Chairs; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Climatology; Environmental science; Climate model; Atmospheric sciences; Transient (computer programming); Climate change; Greenhouse gas; Zonal and meridional; Snow; Atmospheric circulation; Climate sensitivity; Climate state; Global warming; Geology; Oceanography; Effects of global warming","score_opus":0.023905637495475487,"score_gpt":0.2946914932698859,"score_spread":0.27078585577441044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966462928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999321,0.000015649324,0.00022338929,0.00003240077,0.000006217075,0.0000042832635,0.000110547226,0.000015394335,0.00027110215],"genre_scores_gemma":[0.99966383,0.00002167465,0.00011811752,0.000016821177,0.0000017699573,0.000006022841,0.0000967452,0.0000046139194,0.00007045623],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993753,0.000016384041,0.0000052713476,0.000016091955,0.0000071166955,0.000017632547],"domain_scores_gemma":[0.99951124,0.00024763486,0.00006157879,0.0000650733,0.000040982544,0.00007350327],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023985053,0.0002722797,0.00021438082,0.000095502124,0.00015433277,0.00034117387,0.00023690525,0.0002707018,0.00084623264],"category_scores_gemma":[0.0008653904,0.00014995574,0.00029473365,0.00009806349,0.00027349056,0.00019756611,0.00027358835,0.00046850558,0.00007401199],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026119782,0.0004951191,0.12219986,0.00016350963,0.00032968484,0.00020890056,0.00015196753,0.14178556,0.7210027,0.0008014227,0.0006888432,0.009560504],"study_design_scores_gemma":[0.00030697064,0.0025705707,0.37452894,0.000023314831,0.00028440575,0.00014612835,0.00020295635,0.43811476,0.18164171,0.0010538102,0.0010455286,0.000080870625],"about_ca_topic_score_codex":0.0054532327,"about_ca_topic_score_gemma":0.0038482994,"teacher_disagreement_score":0.0054532327,"about_ca_system_score_codex":0.00038640012,"about_ca_system_score_gemma":0.00019110632,"threshold_uncertainty_score":0.010842979},"labels":[],"label_agreement":null},{"id":"W1966654773","doi":"10.1029/2004gl020191","title":"Inertial currents estimated from surface trajectories of ARGO floats","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Argo; Inertial wave; Inertial frame of reference; Geodesy; Amplitude; Geology; Meteorology; Physics; Climatology; Optics","score_opus":0.04103241572897103,"score_gpt":0.2976723265235348,"score_spread":0.2566399107945638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966654773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9215866,0.0003483511,0.07241097,0.00007229552,0.00006220821,0.00003592522,0.0011767659,0.000262965,0.004043995],"genre_scores_gemma":[0.9691477,0.00016434642,0.028260564,0.000011061506,0.000033877073,0.000020639576,0.0012897638,0.000044147688,0.0010280424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000017359154,0.0000065519102,0.000028058648,0.000039841747,0.000019799721],"domain_scores_gemma":[0.9996804,0.00005866357,0.000077696146,0.000022801423,0.00013843401,0.000021935592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021347376,0.00029890647,0.00018895286,0.0010123425,0.00014822453,0.000384354,0.00012270968,0.00014866842,0.0006838718],"category_scores_gemma":[0.001343788,0.00015679328,0.00014385574,0.0005364257,0.00010159321,0.0005002217,0.0002091625,0.0002217149,0.00035863882],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003100696,0.00007066337,0.44208044,0.00015799259,0.00018754348,0.00024491324,0.00060811127,0.13154353,0.09332362,0.003271715,0.0030425813,0.32515877],"study_design_scores_gemma":[0.0000377772,0.00012091183,0.4553972,0.00004743323,0.000056910972,0.00013386949,0.00016524496,0.5231009,0.012794561,0.0013120755,0.0067805666,0.000052610056],"about_ca_topic_score_codex":0.006713323,"about_ca_topic_score_gemma":0.0077665383,"teacher_disagreement_score":0.006713323,"about_ca_system_score_codex":0.00021708941,"about_ca_system_score_gemma":0.00021254134,"threshold_uncertainty_score":0.01334852},"labels":[],"label_agreement":null},{"id":"W1966668178","doi":"10.1029/2006gl028542","title":"Meridional ozone gradients in the African upper troposphere","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique","keywords":"Intertropical Convergence Zone; Hadley cell; Troposphere; Ozone; Atmospheric sciences; Zonal and meridional; Climatology; Environmental science; Tropospheric ozone; Relative humidity; Equator; Latitude; Geology; Meteorology; Climate change; General Circulation Model; Geography; Precipitation","score_opus":0.02672708845634862,"score_gpt":0.2888224917908975,"score_spread":0.26209540333454884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1966668178","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998912,0.00016586256,0.000044866913,0.00004659076,0.0000023101136,0.0000023983566,0.0002929395,0.000004767928,0.0005283482],"genre_scores_gemma":[0.9995105,0.00009235103,0.00010331656,0.00000737711,0.0000036834278,0.000002277003,0.00019394148,0.0000014128758,0.0000851172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999933,0.00001148126,0.0000035622415,0.000013745254,0.000009861944,0.00002828545],"domain_scores_gemma":[0.99983203,0.00002022363,0.000075135096,0.000011502348,0.000037984057,0.000023154886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012196495,0.00011026576,0.0001252147,0.00066127564,0.0003046705,0.0004041602,0.00008742001,0.00012369924,0.00063871127],"category_scores_gemma":[0.0004393177,0.00010326122,0.00006921946,0.0008334792,0.000104884086,0.00020645869,0.00024089447,0.00017986141,0.00007848173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001382164,0.000025289315,0.97323674,0.00003067215,0.000055942877,0.00018456107,0.0005930902,0.0009150636,0.010537115,0.0002644923,0.0006763981,0.013342436],"study_design_scores_gemma":[0.00000336036,0.0000052196788,0.99852186,0.0000049637856,0.0000053544736,0.00002360804,0.000107512606,0.00027722088,0.00026757678,0.000019424966,0.00076156144,0.0000023595085],"about_ca_topic_score_codex":0.02829763,"about_ca_topic_score_gemma":0.049698252,"teacher_disagreement_score":0.02829763,"about_ca_system_score_codex":0.00036165345,"about_ca_system_score_gemma":0.00020675341,"threshold_uncertainty_score":0.05626583},"labels":[],"label_agreement":null},{"id":"W1967307131","doi":"10.1029/2008gl036831","title":"Utilizing chromophoric dissolved organic matter measurements to derive export and reactivity of dissolved organic carbon exported to the Arctic Ocean: A case study of the Yukon River, Alaska","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":237,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Colored dissolved organic matter; Environmental science; Arctic; Biogeochemical cycle; Terrigenous sediment; Organic matter; Oceanography; Total organic carbon; Hydrology (agriculture); Environmental chemistry; Nutrient; Geology; Ecology; Chemistry; Sediment","score_opus":0.03991083763448623,"score_gpt":0.2691473604613638,"score_spread":0.22923652282687756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967307131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948186,0.000026250555,0.00023347848,0.0000054392385,5.351192e-7,0.0000031915554,0.000022773515,0.0000024367782,0.00022410942],"genre_scores_gemma":[0.9984794,0.00006007521,0.0012700318,0.0000044585922,8.3213894e-7,0.000002989275,0.000044118013,0.0000027132367,0.00013530685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997992,0.000048758153,0.000021051754,0.00006108467,0.0000453197,0.000024621006],"domain_scores_gemma":[0.9996032,0.00017543044,0.000050703136,0.000035885667,0.00010698422,0.000027888895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006634545,0.00034387733,0.0002256826,0.000497993,0.0012131319,0.000879039,0.00028822452,0.00038555992,0.00015429172],"category_scores_gemma":[0.0008318726,0.00015608844,0.0002820932,0.0007577946,0.00049118197,0.0003582501,0.00041850776,0.00022827694,0.000041010764],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013312702,0.0001351822,0.9504113,0.000061774816,0.00013098649,0.0023882424,0.0021382712,0.004408086,0.024417216,0.00018849538,0.000057461584,0.015529833],"study_design_scores_gemma":[0.000018345676,0.00025439024,0.9568565,0.000023906923,0.00018151224,0.0011404573,0.005606158,0.015003422,0.019732533,0.00034118886,0.0007926821,0.000048994447],"about_ca_topic_score_codex":0.12285842,"about_ca_topic_score_gemma":0.21113467,"teacher_disagreement_score":0.12285842,"about_ca_system_score_codex":0.001002012,"about_ca_system_score_gemma":0.0006473292,"threshold_uncertainty_score":0.2442866},"labels":[],"label_agreement":null},{"id":"W1967899845","doi":"10.1029/2009gl039647","title":"Estimating ocean climatologies for short periods: A simple technique for removing the effect of eddies from temperature and salinity profiles","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Argo; Climatology; Altimeter; Mesoscale meteorology; Temperature salinity diagrams; Environmental science; Sea surface temperature; Salinity; Sea-surface height; Satellite altimetry; Satellite; Gulf Stream; Geology; Oceanography; Remote sensing","score_opus":0.02003535159733023,"score_gpt":0.30602935109837776,"score_spread":0.28599399950104754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1967899845","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.33335906,0.0004624715,0.6589557,0.00018990022,0.00014245539,0.00010479128,0.0030397398,0.0019364272,0.0018094538],"genre_scores_gemma":[0.51773727,0.00039816057,0.47469932,0.00005803338,0.00010460394,0.000117200136,0.003672977,0.00034164122,0.002870752],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998584,0.000016460468,0.000013392276,0.00004145722,0.000056393157,0.00001390404],"domain_scores_gemma":[0.9995035,0.00013127175,0.00011592528,0.00013360807,0.00009154917,0.000024149027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005553116,0.000592265,0.0004909011,0.00091550907,0.00030308406,0.00036292343,0.0003791282,0.00029501028,0.001115494],"category_scores_gemma":[0.0015775274,0.000286407,0.00045882037,0.0010154379,0.00014433416,0.0005068654,0.0003975203,0.00048219776,0.00049307244],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023641864,0.00021722695,0.08482601,0.00035867788,0.0006243539,0.00024406973,0.000418539,0.030174265,0.14381577,0.0016682019,0.0042582736,0.73315823],"study_design_scores_gemma":[0.00013348526,0.00032472762,0.64315826,0.000054564705,0.00037120102,0.0005428979,0.00017817605,0.24917519,0.08031709,0.0035517584,0.021970399,0.00022226645],"about_ca_topic_score_codex":0.0047444548,"about_ca_topic_score_gemma":0.0140287,"teacher_disagreement_score":0.0047444548,"about_ca_system_score_codex":0.00014862037,"about_ca_system_score_gemma":0.00044826476,"threshold_uncertainty_score":0.009433627},"labels":[],"label_agreement":null},{"id":"W1968021118","doi":"10.1029/2009gl040448","title":"Laboratory studies of products of N<sub>2</sub>O<sub>5</sub> uptake on Cl<sup>−</sup> containing substrates","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":166,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Chloride; Chlorine; Chemistry; Mass spectrometry; Inorganic chemistry; Analytical Chemistry (journal); Spectroscopy; Organic chemistry; Chromatography","score_opus":0.03980884959175117,"score_gpt":0.2852038547205955,"score_spread":0.24539500512884432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968021118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977864,0.00012781293,0.0014415556,0.000012434827,0.000004708749,0.000020275162,0.00011171361,0.000025865022,0.00046907092],"genre_scores_gemma":[0.9970312,0.00017929518,0.0015813701,0.000024977482,0.0000059161966,0.000033240656,0.00025628973,0.000014253527,0.0008735092],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998053,0.00003619369,0.000009102778,0.000057148536,0.00006110561,0.000031233783],"domain_scores_gemma":[0.99974245,0.00008012886,0.00007952402,0.000019240557,0.000056047145,0.00002268902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025204924,0.0004929488,0.00021742705,0.00011163775,0.00019743995,0.0002874416,0.0003110915,0.00037493056,0.00066776015],"category_scores_gemma":[0.000509365,0.000129202,0.00018272117,0.00008924408,0.00025312643,0.00020250039,0.0002165713,0.0002671846,0.00023928728],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010596041,0.000019972033,0.0010652492,0.000023034983,0.0000057907314,0.000051702973,0.00003056363,0.00013406537,0.9978098,0.000027362128,0.000020960992,0.0007054871],"study_design_scores_gemma":[0.0000073292986,0.00040360403,0.0023526922,0.0000016036096,0.0000061954297,0.00006381651,0.000030536794,0.00043779312,0.99643457,0.000014629235,0.0002437341,0.0000035237902],"about_ca_topic_score_codex":0.0013412545,"about_ca_topic_score_gemma":0.0012255149,"teacher_disagreement_score":0.0013412545,"about_ca_system_score_codex":0.00037677202,"about_ca_system_score_gemma":0.00017087978,"threshold_uncertainty_score":0.0027337074},"labels":[],"label_agreement":null},{"id":"W1968091164","doi":"10.1029/2005gl024031","title":"Future tropospheric ozone simulated with a climate‐chemistry‐biosphere model","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Biosphere; Biosphere model; Environmental science; Tropospheric ozone; Atmospheric sciences; Ozone; Troposphere; Climate model; Atmospheric chemistry; Climatology; Climate change; Meteorology; Geology; Oceanography; Geography; Ecology","score_opus":0.015704473130137744,"score_gpt":0.2545692647308519,"score_spread":0.23886479160071417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968091164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96389514,0.0002912585,0.006464737,0.00091189536,0.00014358897,0.00010232289,0.016235385,0.00057027716,0.011385351],"genre_scores_gemma":[0.98480934,0.00022057616,0.0039836396,0.00010490959,0.000032775213,0.00012351308,0.008439095,0.00007140294,0.0022147358],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998697,0.00004037192,0.000006066467,0.0000311085,0.000020499609,0.000032198324],"domain_scores_gemma":[0.99957925,0.0001401401,0.00004698275,0.000040802737,0.00009425759,0.00009865872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051058683,0.00073173206,0.0006170051,0.00036500077,0.00066874566,0.00081888307,0.0011612871,0.001420767,0.0027602096],"category_scores_gemma":[0.0010255529,0.00048504118,0.0005918937,0.0010508382,0.00040730083,0.0012246514,0.0004962324,0.0010883646,0.00046806876],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031955022,0.0001714448,0.009779835,0.000053513082,0.00012970727,0.0001102404,0.00003978936,0.9803649,0.0011719825,0.002958526,0.0029035478,0.00199697],"study_design_scores_gemma":[0.00028381357,0.00008809735,0.0048692785,0.0000051267953,0.000048258407,0.000017353785,0.000032901185,0.9905715,0.0005989397,0.0012454366,0.0022199766,0.000019272893],"about_ca_topic_score_codex":0.0671791,"about_ca_topic_score_gemma":0.035425033,"teacher_disagreement_score":0.0671791,"about_ca_system_score_codex":0.0017361788,"about_ca_system_score_gemma":0.0012101163,"threshold_uncertainty_score":0.1335761},"labels":[],"label_agreement":null},{"id":"W1968406968","doi":"10.1029/2005gl024778","title":"Evolution of high‐latitude snow mass derived from the GRACE gravimetry mission (2002–2004)","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Snow; Latitude; Geology; Water equivalent; Climatology; Environmental science; Satellite; Atmospheric sciences; Geodesy; Geomorphology","score_opus":0.030611502407686585,"score_gpt":0.26431768488772406,"score_spread":0.23370618248003747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968406968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99769586,0.0000489248,0.00022760294,0.00004821441,0.0000046710757,0.0000029426772,0.0010420139,0.000047649148,0.0008821943],"genre_scores_gemma":[0.9976775,0.000018912657,0.00032852235,0.000011205549,0.0000023911953,0.0000032403975,0.0016865954,0.000009937285,0.0002617163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.0000117028,0.0000045817947,0.000026469856,0.000014432988,0.000020045616],"domain_scores_gemma":[0.99971455,0.00004708681,0.000076339034,0.00003160644,0.00009824063,0.000032172855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002498025,0.00022660285,0.00017012494,0.00050046085,0.00023270438,0.00045763125,0.0002098857,0.0003854173,0.0007988445],"category_scores_gemma":[0.0007033609,0.00015027408,0.00021727558,0.00063502416,0.00018472801,0.00028670562,0.00022398222,0.0002211206,0.00024227763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071420055,0.00012321668,0.9209532,0.00004796285,0.0002344458,0.00037098536,0.00049232086,0.025579933,0.031380966,0.0007691736,0.0037763624,0.015557358],"study_design_scores_gemma":[0.000015874115,0.000044219123,0.97940093,0.000004154293,0.000025946438,0.00008498427,0.00007843542,0.016506558,0.0023403084,0.00010546931,0.001382019,0.0000111392],"about_ca_topic_score_codex":0.020391507,"about_ca_topic_score_gemma":0.025231352,"teacher_disagreement_score":0.020391507,"about_ca_system_score_codex":0.0006307921,"about_ca_system_score_gemma":0.00022528163,"threshold_uncertainty_score":0.040545583},"labels":[],"label_agreement":null},{"id":"W1968706437","doi":"10.1029/2001gl012877","title":"Global temperature change and its uncertainties since 1861","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":368,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Environmental science; Climatology; Sea surface temperature; Global temperature; Global change; Climate change; Global warming; Climate model; Meteorology; Atmospheric sciences; Geology; Physics","score_opus":0.06973761275559937,"score_gpt":0.3239289756083655,"score_spread":0.2541913628527661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968706437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84487325,0.04659574,0.020687548,0.010843493,0.001116804,0.000030729145,0.019945184,0.00035811984,0.055548977],"genre_scores_gemma":[0.9888629,0.0061957445,0.001743613,0.00016157686,0.00046069126,0.000012074498,0.0018828777,0.000051650906,0.00062888855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99914336,0.00024121744,0.00006077994,0.00024086045,0.00024715945,0.00006666655],"domain_scores_gemma":[0.99794227,0.00069962704,0.00059090514,0.000269914,0.00043805264,0.00005930162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014576335,0.0005259394,0.00035486725,0.0017862916,0.0005299771,0.0013469614,0.00037757095,0.00047816275,0.0011376159],"category_scores_gemma":[0.008184887,0.00019917687,0.00055466045,0.0054743164,0.0013004334,0.0020033543,0.000989108,0.000819148,0.00029368067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034644376,0.000032199958,0.50379956,0.0006214828,0.001017995,0.0003109129,0.0026011658,0.1969914,0.0011011536,0.059702434,0.009742561,0.22373278],"study_design_scores_gemma":[0.000013736602,0.00009309364,0.751404,0.0003690006,0.00023907957,0.00052051456,0.0008010121,0.036429286,0.0015101318,0.054290053,0.15420903,0.000121120574],"about_ca_topic_score_codex":0.021673748,"about_ca_topic_score_gemma":0.01648997,"teacher_disagreement_score":0.021673748,"about_ca_system_score_codex":0.0020914935,"about_ca_system_score_gemma":0.00041774166,"threshold_uncertainty_score":0.04309517},"labels":[],"label_agreement":null},{"id":"W1968841004","doi":"10.1029/2006gl026772","title":"Impacts on phytoplankton biomass and productivity in the Pacific Northwest during the warm ocean conditions of 2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"San Francisco State University","keywords":"Upwelling; Phytoplankton; Productivity; Oceanography; Biomass (ecology); Environmental science; Hydrography; Trophic level; La Niña; Chlorophyll a; Geology; Nutrient; Climatology; Ecology; Biology","score_opus":0.01455704073067865,"score_gpt":0.246035131857313,"score_spread":0.23147809112663434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968841004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992167,0.000066431334,0.000019721465,0.000046385485,0.0000030046458,9.951053e-7,0.00019989829,0.0000026553585,0.00044414532],"genre_scores_gemma":[0.99892586,0.00013289224,0.000063770116,0.000042750886,0.0000035227833,0.0000024231417,0.0003346424,0.0000019619847,0.00049202924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999335,0.000008782498,0.000004983904,0.000010322055,0.000017030254,0.000025318368],"domain_scores_gemma":[0.999701,0.000020502388,0.00012162129,0.000011737779,0.000060668237,0.00008437905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019438303,0.0001792355,0.00016504907,0.0002687018,0.0005836992,0.00055322825,0.00014506033,0.00021063931,0.0007546332],"category_scores_gemma":[0.00044526914,0.0001212555,0.00013897377,0.00027301512,0.00017909848,0.00024868632,0.00046111463,0.00021041268,0.00007511164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006496618,0.00010490492,0.96972275,0.00005714874,0.00012219154,0.00068513607,0.0005634378,0.0015856002,0.011133883,0.00016292275,0.0008983045,0.014314019],"study_design_scores_gemma":[0.0000030062631,0.000033658103,0.99858165,0.000004181345,0.000009884825,0.000035245546,0.00032898376,0.00011851167,0.00044054963,0.000016781203,0.0004251297,0.0000024771734],"about_ca_topic_score_codex":0.1359584,"about_ca_topic_score_gemma":0.31875673,"teacher_disagreement_score":0.1359584,"about_ca_system_score_codex":0.0013119589,"about_ca_system_score_gemma":0.0006343733,"threshold_uncertainty_score":0.27033406},"labels":[],"label_agreement":null},{"id":"W1968973672","doi":"10.1029/2006gl027028","title":"An increasing CO<sub>2</sub> sink in the Arctic Ocean due to sea‐ice loss","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic sea ice decline; Sea ice; Oceanography; Arctic geoengineering; Arctic ice pack; Arctic; Environmental science; Sink (geography); Seawater; Cryosphere; Arctic dipole anomaly; Canada Basin; Antarctic sea ice; Geology; Continental shelf; Sea ice thickness; Climatology; Geography","score_opus":0.015543299976784242,"score_gpt":0.2649013788726334,"score_spread":0.24935807889584913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1968973672","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652773,0.0006369646,0.0006120753,0.00018902529,0.00001589928,0.000002288622,0.0004577694,0.00004707442,0.001511078],"genre_scores_gemma":[0.9979674,0.00057076867,0.00030390237,0.00007182866,0.000014266776,0.0000033670858,0.0004812425,0.000012305839,0.0005748447],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999565,0.0000044940716,0.000003138343,0.000009465026,0.000012565673,0.000013905312],"domain_scores_gemma":[0.9998654,0.000020197976,0.000042543455,0.000008142358,0.000038767746,0.000024904568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015553947,0.00023048936,0.00019168611,0.0005607402,0.00027589974,0.0005875763,0.00013976436,0.00038475636,0.00086759654],"category_scores_gemma":[0.00030485267,0.00016351772,0.00013616377,0.00043301744,0.00022011659,0.00052035484,0.00020894763,0.0001936381,0.00033220055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00080752576,0.00008961143,0.7579651,0.00018111177,0.00016528532,0.0008302848,0.00018201023,0.0075503625,0.19633815,0.0014991192,0.0014404712,0.03295098],"study_design_scores_gemma":[0.000011873976,0.00006326597,0.9764582,0.00000946916,0.00005570252,0.0005019747,0.00014661445,0.0064806347,0.012968101,0.0006660342,0.0026254859,0.000012552654],"about_ca_topic_score_codex":0.011924529,"about_ca_topic_score_gemma":0.011571771,"teacher_disagreement_score":0.011924529,"about_ca_system_score_codex":0.0005924942,"about_ca_system_score_gemma":0.00028699797,"threshold_uncertainty_score":0.02371025},"labels":[],"label_agreement":null},{"id":"W1969034680","doi":"10.1029/2002gl015597","title":"Thermoremanence and stable memory of single‐domain hematites","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Iron oxide chemistry and applications","field":"Energy","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Demagnetizing field; Magnetism; Thermoremanent magnetization; Condensed matter physics; Hematite; Rock magnetism; Remanence; Materials science; Magnetization; Grain size; Single domain; Single crystal; Magnetic domain; Nuclear magnetic resonance; Magnetic field; Physics; Metallurgy","score_opus":0.04745089091199729,"score_gpt":0.28431631986784806,"score_spread":0.23686542895585078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969034680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951255,0.000051204956,0.00023196159,0.000004279152,0.000001466608,0.0000018366408,0.000033195494,0.000010353983,0.00015327061],"genre_scores_gemma":[0.99943167,0.000019938137,0.00025322766,0.0000016815386,0.0000011272876,0.0000019862932,0.00006994198,0.0000041708195,0.00021640139],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999387,0.0000043640707,0.0000036277331,0.000018463359,0.000020038366,0.000014880884],"domain_scores_gemma":[0.99983156,0.000025161311,0.000043948527,0.000024210876,0.00005280129,0.000022228698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000081071164,0.00014113143,0.0001392441,0.00022521289,0.00018941358,0.00018120735,0.00021027429,0.00011749863,0.000614807],"category_scores_gemma":[0.0002643205,0.00009612276,0.00008068692,0.000119973796,0.00027529616,0.00015210596,0.00013654382,0.00019008355,0.00006383803],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009684724,0.000012075826,0.0022702797,0.000024990073,0.000008223846,0.000043758966,0.00004821223,0.00018561298,0.99505866,0.000024363571,0.0000154719,0.0022115596],"study_design_scores_gemma":[0.000009359325,0.0002483816,0.035717823,0.000003389293,0.00002111936,0.00019210583,0.00006137863,0.0020770442,0.9612849,0.000033080927,0.00034341883,0.000008144009],"about_ca_topic_score_codex":0.0009026453,"about_ca_topic_score_gemma":0.0015299115,"teacher_disagreement_score":0.0009026453,"about_ca_system_score_codex":0.00016265557,"about_ca_system_score_gemma":0.000082783066,"threshold_uncertainty_score":0.0020566583},"labels":[],"label_agreement":null},{"id":"W1969078569","doi":"10.1029/1999gl010761","title":"A continuous view of the dawn‐dusk polar cap","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Dusk; Polar; Polar cap; Noon; Airglow; Daytime; Field line; Brightness; Magnetosphere; Latitude; Earth's magnetic field; Geophysics; Physics; Geology; Atmospheric sciences; Astronomy; Magnetic field","score_opus":0.011557066560288869,"score_gpt":0.2698846773341135,"score_spread":0.2583276107738246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969078569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8634522,0.0020297202,0.0061933943,0.00024125751,0.00029890405,0.000046820507,0.0069665094,0.0005522134,0.120218985],"genre_scores_gemma":[0.9835068,0.0007208088,0.002475009,0.00007264909,0.000104242616,0.000011816274,0.0023921134,0.00006925979,0.0106473025],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999713,0.0000020725058,8.3458247e-7,0.000007836547,0.000007952595,0.000010053645],"domain_scores_gemma":[0.99988556,0.000012830207,0.000014502249,0.000012909617,0.000030017536,0.000044137985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060504095,0.0001489336,0.00009443416,0.0008145052,0.00037442762,0.0006355264,0.00010301682,0.00021216413,0.006020953],"category_scores_gemma":[0.00014892111,0.00009886025,0.00008262754,0.000513208,0.0001578686,0.00020384093,0.00036491815,0.00039938895,0.00090692384],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002035396,0.00014970452,0.34544706,0.00038727844,0.00015651716,0.0026745133,0.0044542267,0.0020999801,0.4330661,0.003499658,0.026663497,0.17936611],"study_design_scores_gemma":[0.000010423408,0.00010197057,0.94785887,0.000045004243,0.00002186911,0.0010325781,0.000581528,0.0008666039,0.007603069,0.00018167248,0.041680805,0.000015539914],"about_ca_topic_score_codex":0.0074504986,"about_ca_topic_score_gemma":0.01786615,"teacher_disagreement_score":0.0074504986,"about_ca_system_score_codex":0.0001416409,"about_ca_system_score_gemma":0.00016843001,"threshold_uncertainty_score":0.020142138},"labels":[],"label_agreement":null},{"id":"W1969148653","doi":"10.1029/2002gl015406","title":"Thermal models of the Middle America Trench at the Nicoya Peninsula, Costa Rica","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":139,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Forearc; Subduction; Trench; Induced seismicity; Accretionary wedge; Seismology; Hypocenter; Hydrothermal circulation; Seafloor spreading; Thermal; Prism; Petrology; Geophysics; Tectonics; Meteorology","score_opus":0.08314370147969984,"score_gpt":0.26145007152154826,"score_spread":0.1783063700418484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969148653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9647948,0.00036453878,0.003706665,0.00034049532,0.000017423976,0.00004651217,0.0015106109,0.0002196498,0.02899939],"genre_scores_gemma":[0.9959552,0.000152558,0.00080301194,0.00002330756,0.0000069678513,0.00005167223,0.00029219026,0.000029657755,0.0026853369],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992716,0.000024062252,0.0000030118647,0.00001846531,0.000008495383,0.000018878556],"domain_scores_gemma":[0.99987614,0.000036480425,0.000020165859,0.000013864009,0.00003259734,0.00002086003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013713399,0.000488439,0.00030385857,0.0005235932,0.00066578167,0.0009219654,0.0009910818,0.0006934091,0.0031176081],"category_scores_gemma":[0.0006953643,0.00030645804,0.00041651315,0.0006194424,0.00056586135,0.00038191964,0.0005660863,0.00025320367,0.00025395027],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033949484,0.00001318799,0.0056133983,0.000012675764,0.00002232734,0.00006239432,0.00008749806,0.99093866,0.00042826936,0.0014653769,0.00032318558,0.0009989392],"study_design_scores_gemma":[0.00003910521,0.000015251688,0.007135964,0.000009792258,0.000017464981,0.000022779475,0.00014041505,0.99020445,0.00015033007,0.0007787245,0.0014710012,0.000014771141],"about_ca_topic_score_codex":0.31973606,"about_ca_topic_score_gemma":0.21218784,"teacher_disagreement_score":0.31973606,"about_ca_system_score_codex":0.0032063595,"about_ca_system_score_gemma":0.0010539417,"threshold_uncertainty_score":0.63575},"labels":[],"label_agreement":null},{"id":"W1969195669","doi":"10.1029/2009gl039581","title":"Dispersion inversion of electromagnetic pulse propagation within freezing and thawing soil waveguides","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical Methods and Applications","field":"Engineering","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Ground-penetrating radar; Dispersion (optics); Radar; Soil science; Atmospheric sciences; Optics; Physics","score_opus":0.023667286673642204,"score_gpt":0.29054850184717784,"score_spread":0.26688121517353564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969195669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79725903,0.00008540647,0.20113194,0.000027859662,0.000007265215,0.000012633779,0.000112161964,0.00020668794,0.0011571085],"genre_scores_gemma":[0.9233175,0.00016464494,0.075288504,0.0000070951182,0.0000057219545,0.00001599059,0.00017394418,0.000027629894,0.0009989855],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999541,0.000007847361,0.0000022177096,0.0000096866315,0.00001933466,0.000006774287],"domain_scores_gemma":[0.9998292,0.00008085873,0.000032149706,0.000017383969,0.00003093417,0.0000093966055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014506308,0.00024973895,0.00009870106,0.00033927785,0.00010091829,0.00022665686,0.00019711547,0.00017623254,0.00030266593],"category_scores_gemma":[0.0005669392,0.00015682408,0.00010794051,0.0003020908,0.00018819123,0.00034496005,0.00021933159,0.00029643887,0.0000851139],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002890268,0.00008170284,0.010431573,0.00008195271,0.000044317097,0.0002487063,0.00043457965,0.12616087,0.716929,0.004830081,0.00025483963,0.14021328],"study_design_scores_gemma":[0.000025498617,0.00007431232,0.009397574,0.000012041696,0.000015603606,0.00012787421,0.00009718264,0.809708,0.17832765,0.0012344929,0.00095304317,0.00002677007],"about_ca_topic_score_codex":0.0023462444,"about_ca_topic_score_gemma":0.0028591335,"teacher_disagreement_score":0.0023462444,"about_ca_system_score_codex":0.00018862831,"about_ca_system_score_gemma":0.00029091485,"threshold_uncertainty_score":0.0046651363},"labels":[],"label_agreement":null},{"id":"W1969436019","doi":"10.1029/2004gl020206","title":"Impact of an adiabatic correction technique on the simulation of CFC‐12 in a model of the North Atlantic Ocean","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Hydrography; Boundary current; Geology; Adiabatic process; Climatology; Current (fluid); Momentum (technical analysis); Convection; Boundary (topology); Deep sea; Deep convection; Ocean current; Continental shelf; Oceanography; Geodesy; Meteorology; Physics; Mathematics","score_opus":0.028889105141069668,"score_gpt":0.2844391651642709,"score_spread":0.25555006002320124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969436019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97942895,0.00012402388,0.014178879,0.0002789159,0.00012267039,0.00007734734,0.00025024093,0.0008182415,0.0047207363],"genre_scores_gemma":[0.9901059,0.000053890493,0.0089951595,0.00005694348,0.000020581125,0.00003447679,0.00013574219,0.00008707373,0.000510296],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999767,0.000094663235,0.00001619922,0.000027831897,0.000045621087,0.000048591515],"domain_scores_gemma":[0.9984366,0.0009240503,0.00016709187,0.00011760463,0.00022327548,0.00013132187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008266392,0.0007464493,0.0005808846,0.00030634907,0.00080248615,0.0008477124,0.0011737032,0.0009074485,0.0011476896],"category_scores_gemma":[0.0041086082,0.00045761027,0.000617559,0.00045965367,0.000653002,0.00050613465,0.00065619487,0.00090593623,0.000116719726],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024652574,0.00012675277,0.008257822,0.000032369815,0.00007613704,0.0001331823,0.000053323063,0.9804566,0.0037449186,0.0009827861,0.0003074641,0.0055821664],"study_design_scores_gemma":[0.000053702683,0.00007080579,0.0008447124,0.0000023763462,0.000021622162,0.000009847671,0.000013449264,0.99756634,0.0011684021,0.00008051655,0.00016091728,0.0000073686747],"about_ca_topic_score_codex":0.06524402,"about_ca_topic_score_gemma":0.027209258,"teacher_disagreement_score":0.06524402,"about_ca_system_score_codex":0.0008491101,"about_ca_system_score_gemma":0.0019575022,"threshold_uncertainty_score":0.1297285},"labels":[],"label_agreement":null},{"id":"W1969622405","doi":"10.1029/2009gl037163","title":"Influence of stratospheric quasi‐biennial oscillation on tropical cyclone tracks in the western North Pacific","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Quasi-biennial oscillation; Typhoon; Tropical cyclone; Climatology; Environmental science; China sea; Stratosphere; Geology; Atmospheric sciences; Oceanography","score_opus":0.02602259730358129,"score_gpt":0.2847969849431218,"score_spread":0.25877438763954047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1969622405","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930596,0.000108964756,0.00003893303,0.0000271413,0.0000052593987,0.0000017427767,0.000079651545,0.0000032840207,0.00042908918],"genre_scores_gemma":[0.99967825,0.0000973117,0.000025688796,0.000011136946,0.000009053703,0.0000011985798,0.00008697563,0.0000017043752,0.00008880448],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998666,0.000048665595,0.000011307922,0.000022895629,0.000023223027,0.00002727686],"domain_scores_gemma":[0.9987942,0.00046273263,0.00032566095,0.00006715243,0.0001401079,0.00021008913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002968719,0.00014962709,0.00014757537,0.00036153456,0.0002387358,0.0004909568,0.000075114716,0.00015246811,0.00067811523],"category_scores_gemma":[0.0014842001,0.00009869041,0.00017600098,0.00033784268,0.0002315729,0.00022400229,0.00022979816,0.00015170936,0.00009239135],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000279849,0.00003087357,0.9864086,0.000016328979,0.00010373835,0.000205819,0.00009810197,0.0008231998,0.005344764,0.00004484895,0.0001602897,0.006483693],"study_design_scores_gemma":[0.0000026129167,0.00001978802,0.99935085,0.0000014130623,0.000014162564,0.000019692536,0.00003847464,0.00040765415,0.00007345428,0.0000065307195,0.00006423137,0.0000011544436],"about_ca_topic_score_codex":0.014255698,"about_ca_topic_score_gemma":0.031771824,"teacher_disagreement_score":0.014255698,"about_ca_system_score_codex":0.00022275145,"about_ca_system_score_gemma":0.00023463776,"threshold_uncertainty_score":0.028345466},"labels":[],"label_agreement":null},{"id":"W1970006538","doi":"10.1029/2002gl015120","title":"Simulation of the last glacial inception and rapid ice sheet growth in the McGill Paleoclimate Model","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Ice sheet; Geology; Ice-sheet model; Milankovitch cycles; Paleoclimatology; Cryosphere; Climatology; Sea ice; Ice stream; Greenland ice sheet; Glacial period; Meltwater; Antarctic sea ice; Oceanography; Climate change; Geomorphology","score_opus":0.052518110800427904,"score_gpt":0.2871482098602403,"score_spread":0.2346300990598124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970006538","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98580825,0.000115725576,0.0037281613,0.00044181524,0.00003649846,0.000038387025,0.0021445188,0.0001409543,0.007545723],"genre_scores_gemma":[0.99486166,0.00006171624,0.0023582035,0.0000704798,0.000007866891,0.000046748435,0.0010553235,0.0000274779,0.0015104755],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989915,0.000025811549,0.000003183924,0.00001967585,0.000014444225,0.00003769905],"domain_scores_gemma":[0.9996213,0.00013264718,0.00004740004,0.000018173958,0.00006134641,0.000119042714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002946519,0.0005028994,0.0003576995,0.00030504633,0.00046274072,0.00067468546,0.0018457763,0.0008684071,0.0034140798],"category_scores_gemma":[0.0010278671,0.00033547037,0.00045780576,0.00045268377,0.0006607034,0.00035684305,0.00064974587,0.0007360819,0.00019107443],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019075256,0.00004542153,0.0055695693,0.00001776493,0.000045430974,0.000099964585,0.000038974224,0.9891444,0.0014997921,0.0013942851,0.00072013057,0.001233503],"study_design_scores_gemma":[0.000096066695,0.000041085194,0.00314383,0.00000444041,0.00002184219,0.000008304223,0.000021273596,0.99559754,0.00032740095,0.0002578507,0.0004670948,0.000013190522],"about_ca_topic_score_codex":0.3946231,"about_ca_topic_score_gemma":0.3157199,"teacher_disagreement_score":0.3946231,"about_ca_system_score_codex":0.0029758983,"about_ca_system_score_gemma":0.0026470316,"threshold_uncertainty_score":0.7846523},"labels":[],"label_agreement":null},{"id":"W1970232808","doi":"10.1029/2006gl026815","title":"Will Greenland melting halt the thermohaline circulation?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":142,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung; Deutsches Klimarechenzentrum","keywords":"Meltwater; Greenland ice sheet; Thermohaline circulation; Shutdown of thermohaline circulation; Climatology; Geology; Future sea level; Ridge; Ice sheet; Oceanography; Climate change; Ocean current; Environmental science; Glacier; Arctic ice pack; North Atlantic Deep Water; Sea ice; Antarctic sea ice; Geomorphology; Paleontology","score_opus":0.04044983542220476,"score_gpt":0.2811249626227443,"score_spread":0.24067512720053952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970232808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9299879,0.0017547313,0.00050946855,0.034682084,0.00023951588,0.000010058495,0.00059216365,0.00006194298,0.032162216],"genre_scores_gemma":[0.9961738,0.00043629392,0.00012086046,0.0018930861,0.00003662335,0.0000023366842,0.00007100238,0.000007813178,0.0012581556],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987113,0.000020147532,0.0000028426223,0.00001509156,0.000011919727,0.000078830024],"domain_scores_gemma":[0.99976605,0.000044983713,0.00007218996,0.000031232077,0.000035370336,0.000050061357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007001274,0.00016562418,0.00016773204,0.00013513096,0.0004712269,0.0009706092,0.00028101812,0.00070394226,0.0036868702],"category_scores_gemma":[0.0013249158,0.00006338701,0.00020005887,0.0002486086,0.0008204823,0.0012618564,0.0005561082,0.00045901636,0.0003807017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023334986,0.0002295722,0.53796095,0.0003519642,0.0004415359,0.0020176456,0.0030099612,0.02000959,0.027155073,0.14050414,0.04212623,0.22385989],"study_design_scores_gemma":[0.00015819834,0.00040618333,0.7213766,0.00021396398,0.0002403765,0.00031453726,0.007406547,0.010669213,0.013435899,0.117745034,0.12796356,0.00006986255],"about_ca_topic_score_codex":0.029870978,"about_ca_topic_score_gemma":0.030807355,"teacher_disagreement_score":0.029870978,"about_ca_system_score_codex":0.0018343751,"about_ca_system_score_gemma":0.0011612528,"threshold_uncertainty_score":0.05939424},"labels":[],"label_agreement":null},{"id":"W1970271121","doi":"10.1029/2007gl032722","title":"Observation of isolated high‐speed auroral streamers and their interpretation as optical signatures of Alfvén waves generated by bursty bulk flows","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan; University of Calgary; Canadian Space Agency","funders":"","keywords":"Low latitude; Geology; Physics; Sky; Geophysics; Latitude; Night sky; Event (particle physics); Astrophysics; Ionosphere; Astronomy","score_opus":0.013959349818129518,"score_gpt":0.258496495865402,"score_spread":0.2445371460472725,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970271121","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978607,0.00012265705,0.00025218094,0.000019672796,0.000004931857,0.000006985398,0.00013191091,0.000022647719,0.0015783282],"genre_scores_gemma":[0.99888414,0.00009859406,0.00048931874,0.000009749658,0.000024982317,0.0000041851854,0.00017857896,0.0000040112536,0.00030638458],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997187,0.0000013367106,8.696235e-7,0.000007469822,0.0000070176698,0.000011404595],"domain_scores_gemma":[0.99988973,0.000013051088,0.000042421165,0.000009267988,0.000015188668,0.000030323603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000059496073,0.0001487952,0.00011411955,0.0006403533,0.00035714696,0.00035178452,0.00016755254,0.00017709873,0.00055318],"category_scores_gemma":[0.00013143549,0.000092047594,0.000076314755,0.0002820908,0.00027513612,0.00016489303,0.00024444246,0.00022768375,0.00008831615],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007123466,0.0001204751,0.4239792,0.000091403504,0.0000785566,0.0027370837,0.001129145,0.000583119,0.5272377,0.00097384537,0.0016543187,0.04070272],"study_design_scores_gemma":[0.000028983857,0.00009007173,0.97723854,0.000007826265,0.000026551517,0.0009980415,0.00025898547,0.0012827059,0.01837303,0.00015503728,0.0015311595,0.000009070456],"about_ca_topic_score_codex":0.0041495212,"about_ca_topic_score_gemma":0.007979659,"teacher_disagreement_score":0.0041495212,"about_ca_system_score_codex":0.00026777727,"about_ca_system_score_gemma":0.00012303294,"threshold_uncertainty_score":0.008250773},"labels":[],"label_agreement":null},{"id":"W1970431911","doi":"10.1029/2004gl022098","title":"A high time resolution study of boundary layer ozone chemistry and dynamics over the Arctic Ocean near Alert, Nunavut","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Troposphere; Radiosonde; Boundary layer; Atmospheric sciences; Arctic; Ozone; Environmental science; Planetary boundary layer; Climatology; Ozone depletion; Synoptic scale meteorology; Sea ice; Meteorology; Geology; Stratosphere; Oceanography; Geography; Physics","score_opus":0.01376105893046776,"score_gpt":0.250078605323847,"score_spread":0.23631754639337926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970431911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988061,0.00014285803,0.000120972676,0.000030667707,0.000010086764,0.000009271967,0.0003059799,0.000007488751,0.00056655274],"genre_scores_gemma":[0.99832577,0.000094789735,0.00031844943,0.000033134773,0.000005050617,0.000009541177,0.0006128806,0.00000496946,0.00059544167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999169,0.0000073502993,0.000002374923,0.000024886214,0.00002220117,0.00002631124],"domain_scores_gemma":[0.99985516,0.000018124116,0.00001854967,0.00000940099,0.000054940203,0.000043712014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017260267,0.00021333864,0.0001807723,0.0004037809,0.0010573051,0.00048355488,0.00037542678,0.00024196737,0.00046761904],"category_scores_gemma":[0.00028406802,0.00021470485,0.00014983183,0.00041855482,0.0003090379,0.00018740693,0.00032002662,0.00024795783,0.000103674334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061639136,0.00020613786,0.91451865,0.00007537086,0.00017088241,0.00093692465,0.0025416934,0.0032961809,0.06061183,0.00025726695,0.0012417232,0.015526944],"study_design_scores_gemma":[0.000022155145,0.00004622878,0.9941075,0.000011576864,0.000023463963,0.00007604108,0.0006596887,0.0023490745,0.0012524853,0.00004046692,0.0013990004,0.000012325412],"about_ca_topic_score_codex":0.81907344,"about_ca_topic_score_gemma":0.889237,"teacher_disagreement_score":0.18092656,"about_ca_system_score_codex":0.0020220994,"about_ca_system_score_gemma":0.0016008537,"threshold_uncertainty_score":0.3639841},"labels":[],"label_agreement":null},{"id":"W1970640511","doi":"10.1029/2005gl023908","title":"Decadal variability in the Arctic Ocean shown in hydrochemical data","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Geology; Silicate; Oceanography; Climatology; Outflow; The arctic; Boundary current; Oceanic basin; Structural basin; Ocean current; Environmental science; Geomorphology","score_opus":0.04105556209156311,"score_gpt":0.3012557221664531,"score_spread":0.26020016007489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1970640511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942174,0.00037169753,0.0010067732,0.000092999246,0.00002910526,0.0000035452692,0.0022353062,0.00005191459,0.001991092],"genre_scores_gemma":[0.997867,0.00011532924,0.0002873041,0.00001177567,0.000012244644,0.0000041105573,0.0014889549,0.0000066911457,0.00020663487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997509,0.000058644044,0.000028138176,0.00008768899,0.00004261951,0.000032010867],"domain_scores_gemma":[0.9983392,0.0005467254,0.00046729422,0.00021837173,0.0003289494,0.000099462704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007684379,0.00010971617,0.00013451425,0.0012844255,0.00018263841,0.00061208016,0.000087090186,0.00027227894,0.00073244784],"category_scores_gemma":[0.002611635,0.0000972596,0.00013111153,0.0014538441,0.00013744831,0.00031309365,0.0003634014,0.00026786563,0.00021311299],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017577982,0.000027278837,0.9606522,0.00003978882,0.00022330163,0.00013947442,0.00043327716,0.0044095186,0.0058037173,0.00095677626,0.0015448908,0.025594104],"study_design_scores_gemma":[0.0000021015185,0.000017379445,0.9933143,0.000008104554,0.000024089128,0.00012074085,0.00010743892,0.0036624882,0.00046820802,0.00020726425,0.0020573803,0.000010569735],"about_ca_topic_score_codex":0.0022107814,"about_ca_topic_score_gemma":0.0032907578,"teacher_disagreement_score":0.0022107814,"about_ca_system_score_codex":0.00017668061,"about_ca_system_score_gemma":0.00008103476,"threshold_uncertainty_score":0.0043958426},"labels":[],"label_agreement":null},{"id":"W1971080811","doi":"10.1029/2001gl014002","title":"Carbon dioxide in soil profiles: Production and temperature dependence","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Soil respiration; Environmental science; Carbon dioxide; Flux (metallurgy); Respiration; Vegetation (pathology); Atmospheric sciences; Soil carbon; Carbon cycle; Soil science; Soil water; Ecosystem; Chemistry; Ecology; Geology; Biology","score_opus":0.013843320133895349,"score_gpt":0.23825321833746416,"score_spread":0.2244098982035688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971080811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99606955,0.00055628817,0.0021230085,0.000032257736,0.0000031902164,0.000008989511,0.0004810693,0.000021961288,0.00070362526],"genre_scores_gemma":[0.9991547,0.00014529824,0.0003427848,0.0000045648553,0.0000032507644,0.00000370963,0.00023627926,0.000004325167,0.00010508944],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999261,0.000015124565,0.0000041323656,0.000024709241,0.000017890467,0.000011959941],"domain_scores_gemma":[0.9995858,0.00016476215,0.00011788807,0.00003210818,0.00006976835,0.000029678733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027562998,0.00021182798,0.00016708858,0.00027134782,0.00008694664,0.00035540812,0.0001330021,0.00021877479,0.00039303605],"category_scores_gemma":[0.0009889548,0.00018945242,0.00013324786,0.00036833918,0.00016868202,0.00038411334,0.00019207616,0.00016012859,0.00010708293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063860876,0.00004463251,0.4872054,0.00014537704,0.00013534512,0.00019475559,0.00024200456,0.0055328878,0.48619884,0.0003025741,0.00012069308,0.019238826],"study_design_scores_gemma":[0.000004091334,0.000052618234,0.97301346,0.0000051061215,0.000021252554,0.0001535871,0.000032488337,0.007748696,0.018619359,0.00012337763,0.0002185279,0.0000073828464],"about_ca_topic_score_codex":0.004287646,"about_ca_topic_score_gemma":0.005585625,"teacher_disagreement_score":0.004287646,"about_ca_system_score_codex":0.00018955179,"about_ca_system_score_gemma":0.000097413686,"threshold_uncertainty_score":0.008525431},"labels":[],"label_agreement":null},{"id":"W1971192624","doi":"10.1029/2005gl023860","title":"Predominance of industrial Pb in recent snow (1994–2004) and ice (1842–1996) from Devon Island, Arctic Canada","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Snow; Arctic; Environmental science; Physical geography; The arctic; Radiogenic nuclide; Atmospheric sciences; Climatology; Oceanography; Geology; Geography; Geochemistry; Geomorphology","score_opus":0.03147599959439628,"score_gpt":0.27383244421450614,"score_spread":0.24235644462010986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971192624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967991,0.000403168,0.000043813936,0.000029722201,0.0000045377665,0.0000071484124,0.0014065955,0.0000033380984,0.0013026448],"genre_scores_gemma":[0.9947009,0.00065768184,0.00016376196,0.000029921697,0.000007718503,0.000007166825,0.0027285502,0.0000062368085,0.0016980362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973434,0.00001043253,0.000012409771,0.000049666218,0.00009155232,0.00010167685],"domain_scores_gemma":[0.99937683,0.000030927727,0.0000937556,0.000013177004,0.0003711616,0.000114244336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002458826,0.00038304046,0.00029935766,0.0023108898,0.0018600684,0.0010934492,0.0004917941,0.0002417785,0.00075874524],"category_scores_gemma":[0.00044432998,0.00023329617,0.00019720364,0.0030902808,0.0006030403,0.0002160178,0.00046400973,0.00020336607,0.00014775433],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014185577,0.000015239548,0.98566324,0.00004450118,0.00005465888,0.0004176847,0.0012775691,0.00011940533,0.004733105,0.0000383162,0.00035661415,0.007137849],"study_design_scores_gemma":[0.0000020894397,0.000008020012,0.9972102,0.000008277097,0.000010310429,0.00008375803,0.0006496914,0.00006687976,0.0005116746,0.0000049824994,0.0014413153,0.0000028016402],"about_ca_topic_score_codex":0.9650069,"about_ca_topic_score_gemma":0.989486,"teacher_disagreement_score":0.034993112,"about_ca_system_score_codex":0.0066603925,"about_ca_system_score_gemma":0.0046972125,"threshold_uncertainty_score":0.07039833},"labels":[],"label_agreement":null},{"id":"W1971548140","doi":"10.1002/2014gl060239","title":"Response of the high‐resolution Chinese loess grain size record to the 50°N integrated winter insolation during the last 500,000 years","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Scholarship Council; National Natural Science Foundation of China; University of Alberta; National Science Foundation","keywords":"Insolation; Climatology; Loess; Climate change; Environmental science; Annual cycle; Volume (thermodynamics); Physical geography; Ice sheet; Grain size; Ice age; Atmospheric sciences; Geology; Geography; Oceanography; Glacial period; Paleontology; Geomorphology","score_opus":0.013141190814471763,"score_gpt":0.2615330065044596,"score_spread":0.24839181568998783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971548140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99827445,0.00008174591,0.00033192767,0.000029590316,0.0000063955963,0.0000025761117,0.00066395506,0.000035269364,0.000573974],"genre_scores_gemma":[0.9989851,0.000021548058,0.00010429858,0.000013841393,0.000004310171,0.0000029297548,0.0007408386,0.000005316618,0.000121830344],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998692,0.000013228887,0.000012225226,0.000057092704,0.000022230259,0.000025879865],"domain_scores_gemma":[0.9995216,0.000075389435,0.00008790514,0.0001190263,0.0001373979,0.000058720798],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052808534,0.00016550736,0.00019407894,0.0007315679,0.0003088114,0.0005924123,0.00033797507,0.00028735882,0.0010616144],"category_scores_gemma":[0.00093534036,0.00013826792,0.00032776236,0.00069612317,0.0002621346,0.00038679485,0.0004120519,0.00014408225,0.00019332631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113999966,0.000022912116,0.9775349,0.000028046343,0.00018700583,0.0001127988,0.00022282635,0.0049073976,0.0072088134,0.0001688368,0.00057733624,0.008915141],"study_design_scores_gemma":[0.0000034780878,0.0000047687217,0.9951786,0.0000027993635,0.00001892652,0.000018967681,0.000034464018,0.0039396966,0.0003818288,0.00002308209,0.00038905107,0.0000043676323],"about_ca_topic_score_codex":0.03353233,"about_ca_topic_score_gemma":0.0388946,"teacher_disagreement_score":0.03353233,"about_ca_system_score_codex":0.00049547764,"about_ca_system_score_gemma":0.00028234939,"threshold_uncertainty_score":0.06667429},"labels":[],"label_agreement":null},{"id":"W1971901315","doi":"10.1029/2006gl027183","title":"A biological origin for climate signals in corals—Trace element “vital effects” are ubiquitous in Scleractinian coral skeletons","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Université du Québec à Montréal","funders":"","keywords":"Coral; Porites; Reef; Oceanography; Geology; Zooxanthellae; Coral reef; Scleractinia; Ecology; Cnidaria; Biology; Paleontology; Symbiosis","score_opus":0.04484557018887884,"score_gpt":0.32856610978587936,"score_spread":0.2837205395970005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971901315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782157,0.0003138235,0.0005289117,0.00006406393,0.0000027228741,0.0000024830124,0.0001109699,0.000022765495,0.0011327276],"genre_scores_gemma":[0.9995147,0.00007354483,0.0002187786,0.000016892225,0.000002758414,0.0000017374632,0.00004540889,0.000004672697,0.00012156662],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99986494,0.000025635194,0.000010347919,0.00003784707,0.000036233083,0.000024936426],"domain_scores_gemma":[0.99918014,0.00013684889,0.0003641912,0.00006885067,0.00013667515,0.00011326631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024442593,0.0001798885,0.00019595906,0.0007167216,0.00028685434,0.00036677608,0.00018190518,0.00023417846,0.000721969],"category_scores_gemma":[0.0010150248,0.00018081436,0.00012750179,0.0005199108,0.00062021596,0.00021990223,0.00051977875,0.00018315585,0.000106768275],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041049856,0.00001245769,0.4206912,0.00011041003,0.000055939418,0.00024811077,0.00044398342,0.00026459884,0.56562513,0.0005462845,0.00008764725,0.011503751],"study_design_scores_gemma":[0.0000052736827,0.000061339095,0.98626584,0.0000046150963,0.000021275897,0.0003301203,0.0001762676,0.00026693652,0.01213495,0.00027322402,0.00045398818,0.000006173149],"about_ca_topic_score_codex":0.0018036796,"about_ca_topic_score_gemma":0.0040477603,"teacher_disagreement_score":0.0018036796,"about_ca_system_score_codex":0.00023390332,"about_ca_system_score_gemma":0.00017728914,"threshold_uncertainty_score":0.0035864115},"labels":[],"label_agreement":null},{"id":"W1971967577","doi":"10.1029/2009gl040006","title":"Bottom pressure signals at the TAG deep‐sea hydrothermal field: Evidence for short‐period, flow‐induced ground deformation","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Woods Hole Oceanographic Institution","keywords":"Hydrothermal circulation; Geology; Seafloor spreading; Ridge; Amplitude; Seabed; Permeability (electromagnetism); Mineralogy; Geophysics; Seismology; Petrology; Oceanography; Paleontology; Optics; Physics; Chemistry","score_opus":0.07334681407200014,"score_gpt":0.32774433680996645,"score_spread":0.25439752273796634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1971967577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99932075,0.000028216014,0.00016214,0.00001140589,0.0000028129593,0.000001689527,0.00016248968,0.000008715783,0.00030178652],"genre_scores_gemma":[0.9995173,0.000016933316,0.00013107868,0.0000090542835,0.0000040822606,0.0000020319776,0.00019912493,0.00000188484,0.00011858449],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000028327506,0.0000028508161,0.0000102510985,0.000011120778,0.000015764985],"domain_scores_gemma":[0.9998286,0.000023692064,0.00005316671,0.000009536048,0.00003335001,0.00005159856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000079550555,0.00013898888,0.00014392241,0.00042054456,0.00019606575,0.0002469824,0.00015403389,0.0002419261,0.0006376769],"category_scores_gemma":[0.00029006542,0.00015813074,0.00009819936,0.0004105539,0.00023529596,0.00016814054,0.00018672344,0.0001613552,0.00013882821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046976286,0.0000757952,0.61766285,0.000047028527,0.00004820088,0.00038263667,0.00038256918,0.00032075334,0.37048194,0.00009232139,0.00030521097,0.009730994],"study_design_scores_gemma":[0.000004921938,0.000030191097,0.9972518,0.0000010355308,0.000005842912,0.000073853895,0.000042389092,0.00034493243,0.0021576995,0.000008522427,0.00007580536,0.0000028999527],"about_ca_topic_score_codex":0.0069262297,"about_ca_topic_score_gemma":0.013181622,"teacher_disagreement_score":0.0069262297,"about_ca_system_score_codex":0.00021300877,"about_ca_system_score_gemma":0.00015656723,"threshold_uncertainty_score":0.013771832},"labels":[],"label_agreement":null},{"id":"W1972020394","doi":"10.1002/2014gl059269","title":"Crustal structure beneath SE Tibet from joint analysis of receiver functions and Rayleigh wave dispersion","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Natural Science Foundation of China","keywords":"Geology; Crust; Seismology; Receiver function; Rayleigh wave; Block (permutation group theory); Dispersion (optics); Joint (building); Seismic array; Flow (mathematics); Anisotropy; Lithosphere; Geophysics; Surface wave; Tectonics; Geometry; Optics","score_opus":0.03013242095378375,"score_gpt":0.2545158118885318,"score_spread":0.22438339093474804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972020394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99871826,0.000038296148,0.00067028764,0.000007083406,8.372605e-7,0.0000012540894,0.00008860751,0.00001385004,0.0004615322],"genre_scores_gemma":[0.99958414,0.000011738051,0.00015631328,0.0000010083446,8.0745446e-7,5.8261634e-7,0.00016073044,0.0000017705894,0.000082780345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999455,0.0000088325305,0.0000040382774,0.000013015274,0.000013484606,0.000015127729],"domain_scores_gemma":[0.9998512,0.000028899369,0.00003484128,0.000010554223,0.00004429561,0.000030188525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021305164,0.00029528464,0.00017739905,0.0014172373,0.00021804759,0.00051239243,0.000136338,0.00013192608,0.00088635867],"category_scores_gemma":[0.0003769991,0.00015155769,0.00020321063,0.0011764718,0.0001902645,0.00019135227,0.000328284,0.00013998375,0.00014440836],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041831777,0.000047045225,0.7681099,0.00007002288,0.00017366798,0.00079067773,0.00048768305,0.018206734,0.15945812,0.00051544234,0.00023019605,0.05149216],"study_design_scores_gemma":[0.0000141442615,0.000053436626,0.9691862,0.000009154248,0.000032665277,0.0000981988,0.00013119016,0.0284028,0.0017415569,0.00013487833,0.0001837924,0.000011994786],"about_ca_topic_score_codex":0.01223995,"about_ca_topic_score_gemma":0.015846245,"teacher_disagreement_score":0.01223995,"about_ca_system_score_codex":0.00017013907,"about_ca_system_score_gemma":0.00023773452,"threshold_uncertainty_score":0.02433741},"labels":[],"label_agreement":null},{"id":"W1972105879","doi":"10.1029/2000gl011830","title":"Seasonal transition in gravity wave activity during the springtime stratospheric vortex breakdown","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Stratosphere; Polar vortex; Anticyclone; Atmospheric sciences; Vortex; Gravity wave; Orographic lift; Sudden stratospheric warming; Environmental science; Climatology; Breaking wave; Gravitational wave; Geology; Physics; Meteorology; Wave propagation; Precipitation","score_opus":0.010656685456911941,"score_gpt":0.2531805139067559,"score_spread":0.24252382844984394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972105879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992238,0.000056698398,0.0000669113,0.000018948023,0.0000050481362,0.000004274604,0.00020335386,0.000008323088,0.0004126793],"genre_scores_gemma":[0.9988943,0.000039425937,0.000043884764,0.000018591763,0.000005762388,0.0000065014247,0.00066275237,0.000003309121,0.00032553644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.0000059097492,0.0000033931528,0.000013327075,0.000012159346,0.00002726024],"domain_scores_gemma":[0.99959606,0.00007356724,0.000084477666,0.000016877062,0.00006847025,0.00016050933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015798018,0.00013229139,0.0002676458,0.0005350633,0.00027974357,0.0004905823,0.000114769864,0.0002620339,0.00101567],"category_scores_gemma":[0.00061921985,0.00012625202,0.00012883611,0.00030378904,0.00024447954,0.00019274102,0.00026192647,0.00040232638,0.0002936619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038362695,0.00033400534,0.83117336,0.00007098933,0.00010875012,0.0006878886,0.0015147547,0.00052668434,0.13957147,0.00029204553,0.0011616364,0.020722086],"study_design_scores_gemma":[0.0000060243806,0.00015333359,0.997976,0.000003494597,0.0000061442092,0.000056754972,0.00019132785,0.00014873399,0.0011197935,0.000027448548,0.00030763427,0.000003349372],"about_ca_topic_score_codex":0.0046250685,"about_ca_topic_score_gemma":0.008551346,"teacher_disagreement_score":0.0046250685,"about_ca_system_score_codex":0.00024234556,"about_ca_system_score_gemma":0.00014024095,"threshold_uncertainty_score":0.009196341},"labels":[],"label_agreement":null},{"id":"W1972313145","doi":"10.1029/2008gl034723","title":"Imaging compaction band propagation in Diemelstadt sandstone using acoustic emission locations","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Compaction; Geology; Acoustic emission; Bedding; Deformation bands; Amplitude; Seismology; Deformation (meteorology); Overburden pressure; Mineralogy; Cracking; Geotechnical engineering; Materials science; Optics; Composite material; Physics","score_opus":0.05246167117458835,"score_gpt":0.3158843793882749,"score_spread":0.2634227082136866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972313145","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99882644,0.000015379912,0.00079551886,0.000002889243,7.676627e-7,0.0000023712248,0.000032472875,0.000015270341,0.000308897],"genre_scores_gemma":[0.9984902,0.000018354578,0.0011514195,0.0000024010071,9.00564e-7,0.0000027896908,0.00004460535,0.000003161417,0.0002861752],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994206,0.00000478967,0.0000030542008,0.000014615089,0.000020151845,0.000015233361],"domain_scores_gemma":[0.99984527,0.00003901985,0.00003491265,0.00001623818,0.000036893893,0.00002753686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009649534,0.00019542112,0.00010447083,0.0005614196,0.00014501745,0.00015499508,0.00014582349,0.0002173199,0.00086902786],"category_scores_gemma":[0.0001994549,0.00014611732,0.00006752898,0.00028742786,0.00027046524,0.00012316124,0.00022998666,0.00015650499,0.00015277066],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018912306,0.000027122436,0.025779372,0.000027201753,0.000009026463,0.00024825023,0.00023033458,0.00090267777,0.9650633,0.000037186488,0.00002585665,0.007460588],"study_design_scores_gemma":[0.000018310086,0.0003976096,0.718914,0.000013553799,0.00002877305,0.0005265184,0.0003662557,0.009317501,0.2697634,0.000045589255,0.0005875149,0.0000210103],"about_ca_topic_score_codex":0.0026685596,"about_ca_topic_score_gemma":0.007436791,"teacher_disagreement_score":0.0026685596,"about_ca_system_score_codex":0.00009450812,"about_ca_system_score_gemma":0.000085252716,"threshold_uncertainty_score":0.005306065},"labels":[],"label_agreement":null},{"id":"W1972588305","doi":"10.1029/2000gl003768","title":"Mesospheric and lower thermospheric manifestations of a stratospheric warming event over Eureka, Canada (80°N)","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Stratosphere; Sudden stratospheric warming; Polar vortex; Airglow; Environmental science; Atmospheric sciences; Mesosphere; Thermosphere; Climatology; Lidar; Atmosphere (unit); Stratopause; Meteorology; Ionosphere; Geology; Physics; Remote sensing","score_opus":0.013723652894043667,"score_gpt":0.25347413771804167,"score_spread":0.239750484823998,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1972588305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946946,0.000021196116,0.000010166013,0.000014227685,6.6774146e-7,0.0000017497439,0.00020442305,0.0000022722347,0.00027584968],"genre_scores_gemma":[0.9993529,0.00003832001,0.000039376384,0.000008324695,0.0000010465677,0.0000017420676,0.00038927063,0.0000011078431,0.00016793709],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991,0.000006381258,0.0000025327756,0.000013639639,0.000018825645,0.000048696824],"domain_scores_gemma":[0.99987733,0.000012055915,0.000020133368,0.000008322275,0.000047028323,0.000035074027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014221513,0.00019943948,0.00014524856,0.00025742358,0.00064781425,0.00049690175,0.00021870866,0.00018956843,0.00051124574],"category_scores_gemma":[0.00027620004,0.00011125264,0.00015429068,0.0004133082,0.00029504768,0.00017003689,0.00029951523,0.00019095768,0.000054851967],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046032234,0.00010164856,0.9607764,0.000040783794,0.00015242297,0.0007417498,0.0011781031,0.009655297,0.015886119,0.00028575878,0.0008505692,0.009870875],"study_design_scores_gemma":[0.000006031492,0.000009682907,0.9973471,0.0000026800856,0.000012199436,0.000026495149,0.00021733159,0.0013366631,0.0005766531,0.000018883797,0.00044175662,0.000004339915],"about_ca_topic_score_codex":0.8803036,"about_ca_topic_score_gemma":0.9327574,"teacher_disagreement_score":0.11969638,"about_ca_system_score_codex":0.0033850041,"about_ca_system_score_gemma":0.0018797447,"threshold_uncertainty_score":0.24080253},"labels":[],"label_agreement":null},{"id":"W1973026421","doi":"10.1029/2004gl020089","title":"Carbon kinetic isotope effects in the gas‐phase reactions of aromatic hydrocarbons with the OH radical at 296 ± 4 K","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Benzene; Ethylbenzene; Toluene; Kinetic isotope effect; Chemistry; Radical; Combustion; Carbon fibers; Isotope-ratio mass spectrometry; Isotope; Isotopes of carbon; Analytical Chemistry (journal); Mass spectrometry; Photochemistry; Physical chemistry; Organic chemistry; Deuterium; Total organic carbon; Materials science; Chromatography","score_opus":0.015595823962561513,"score_gpt":0.26076162292739546,"score_spread":0.24516579896483395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973026421","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909651,0.00169487,0.0031633493,0.00009020136,0.00006237254,0.000017816585,0.00081511174,0.00016712083,0.0030240268],"genre_scores_gemma":[0.99768686,0.0004524787,0.0006256969,0.000015991676,0.0000073472634,0.000007847016,0.0003433251,0.000028267086,0.0008320564],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997204,0.000030797233,0.000012278458,0.00005618425,0.000116341434,0.000064006985],"domain_scores_gemma":[0.99965584,0.0001422211,0.000039682334,0.000033420907,0.000108917906,0.000019958288],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034730378,0.00046869428,0.00037552416,0.000549013,0.0005476554,0.00051267387,0.0007298009,0.00042971814,0.001981086],"category_scores_gemma":[0.0008885472,0.0003105199,0.00031842518,0.00052160746,0.00058417895,0.00081724016,0.0002630479,0.00076020573,0.0007815239],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000765469,0.000026583637,0.002306492,0.00014622034,0.000030037549,0.00015299869,0.00015316076,0.00088685594,0.99237204,0.000341189,0.00015493497,0.0026640638],"study_design_scores_gemma":[0.000025003537,0.00015176024,0.011293014,0.0000070505944,0.00001818035,0.0001679466,0.00008960125,0.0028890031,0.98391783,0.00022653825,0.0011793165,0.000034698453],"about_ca_topic_score_codex":0.0025800585,"about_ca_topic_score_gemma":0.0022320685,"teacher_disagreement_score":0.0025800585,"about_ca_system_score_codex":0.00060658285,"about_ca_system_score_gemma":0.00018928683,"threshold_uncertainty_score":0.006627381},"labels":[],"label_agreement":null},{"id":"W1973289087","doi":"10.1029/2008gl034270","title":"Global distributions of carbonyl sulfide in the upper troposphere and stratosphere","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Stratosphere; Troposphere; Atmospheric sciences; Carbonyl sulfide; Occultation; Equator; Mixing ratio; Environmental science; Dimethyl sulfide; Latitude; Climatology; Altitude (triangle); Atmospheric chemistry; Ozone; Meteorology; Geology; Chemistry; Physics","score_opus":0.02381315346354159,"score_gpt":0.2760202326901283,"score_spread":0.25220707922658675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973289087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99894863,0.00011711626,0.000051102954,0.00001247967,9.223066e-7,0.0000010150521,0.00043981217,0.000009126927,0.0004199029],"genre_scores_gemma":[0.99858665,0.00013860881,0.00013241415,0.000009824556,0.000004401677,0.0000021970461,0.00093540695,0.0000033378335,0.00018727568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997497,0.0000020228285,0.0000012284647,0.000008765374,0.0000042894158,0.000008713732],"domain_scores_gemma":[0.99988675,0.000012432361,0.000042392807,0.000008443993,0.000024243172,0.000025753814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006619471,0.00021678183,0.00014377538,0.000701946,0.00016953163,0.000263901,0.000067527304,0.00015050697,0.0007208807],"category_scores_gemma":[0.00010983089,0.00009931151,0.0001357017,0.0004516177,0.00017710548,0.00022583603,0.00025715376,0.000095404816,0.00012383756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022222058,0.000029370694,0.9223688,0.000030900752,0.00009932065,0.00011411891,0.00041257366,0.0012520949,0.062120896,0.00009101737,0.0003701697,0.012888448],"study_design_scores_gemma":[0.0000019439155,0.00003963737,0.9981975,0.0000015155813,0.0000119073475,0.000050915245,0.00004746117,0.00016573143,0.001105396,0.000017729597,0.00035795703,0.0000022785139],"about_ca_topic_score_codex":0.0071350494,"about_ca_topic_score_gemma":0.008340864,"teacher_disagreement_score":0.0071350494,"about_ca_system_score_codex":0.00020641736,"about_ca_system_score_gemma":0.00012259085,"threshold_uncertainty_score":0.014187038},"labels":[],"label_agreement":null},{"id":"W1973294409","doi":"10.1002/2014gl060212","title":"A new health check of the ozone layer at global and regional scales","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"European Organization for the Exploitation of Meteorological Satellites","keywords":"Climatology; Ozone layer; Environmental science; Montreal Protocol; Ozone; Middle latitudes; Climate change; Multivariate statistics; Term (time); Tropics; Atmospheric sciences; Geography; Meteorology; Geology; Oceanography; Statistics","score_opus":0.03938287971272174,"score_gpt":0.3020110149994967,"score_spread":0.2626281352867749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973294409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.949917,0.0045297537,0.025010262,0.0022881927,0.00032045925,0.00007880549,0.0073087527,0.00047744575,0.010069278],"genre_scores_gemma":[0.994238,0.00031268006,0.003692536,0.00015319404,0.00013027398,0.000012695647,0.0008546371,0.00002397354,0.00058196904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99960333,0.00011834207,0.000022531807,0.00011899847,0.00008727861,0.000049629503],"domain_scores_gemma":[0.99820054,0.00026974603,0.00053689315,0.0003002624,0.0005234637,0.00016909052],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014512533,0.0002951273,0.00027875637,0.0013964276,0.0005402144,0.0011754099,0.00047638465,0.0003668682,0.0014472187],"category_scores_gemma":[0.0020445678,0.000103256,0.00034395553,0.00095726614,0.0005578176,0.0013382629,0.0010149718,0.0007517575,0.00016087606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007167577,0.00019852894,0.8297494,0.00018782078,0.0006126534,0.0002548676,0.00047313503,0.0055634924,0.043722767,0.0048798546,0.0054356274,0.10820511],"study_design_scores_gemma":[0.000014452118,0.0002835199,0.97070134,0.000035427536,0.00021142214,0.00012518109,0.0005470679,0.0056468723,0.012368593,0.001687475,0.008341005,0.00003755468],"about_ca_topic_score_codex":0.021728175,"about_ca_topic_score_gemma":0.02602817,"teacher_disagreement_score":0.021728175,"about_ca_system_score_codex":0.0005821643,"about_ca_system_score_gemma":0.00079639367,"threshold_uncertainty_score":0.043203413},"labels":[],"label_agreement":null},{"id":"W1973478069","doi":"10.1029/2006gl025753","title":"A pan‐arctic evaluation of changes in river discharge during the latter half of the 20th century","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":389,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Division of Arctic Sciences; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Arctic; Environmental science; The arctic; Geology; Discharge; Oceanography; Climatology; Physical geography; Hydrology (agriculture); Geography; Drainage basin; Geotechnical engineering","score_opus":0.057592630655547365,"score_gpt":0.3015627877359965,"score_spread":0.2439701570804491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973478069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986133,0.002012987,0.0007420402,0.00014443618,0.000036511177,0.0000101693495,0.0026736949,0.000019087089,0.008228156],"genre_scores_gemma":[0.9922465,0.0025105963,0.00093642727,0.000054649976,0.000054082768,0.000015173234,0.0025662587,0.00000950312,0.0016067325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981946,0.000039104787,0.000025036921,0.000035456454,0.00005512687,0.000025814365],"domain_scores_gemma":[0.99943036,0.000053998003,0.00017194981,0.000021694961,0.00027059324,0.00005139957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00064613525,0.00017214032,0.00016638586,0.0015107068,0.00035009382,0.00066430547,0.0000736907,0.00014526212,0.00069170137],"category_scores_gemma":[0.0009501808,0.000061383216,0.00019324668,0.0021114603,0.00018626447,0.00037874185,0.0003455092,0.00016639348,0.00010762652],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043150064,0.000036435704,0.93769443,0.0001352236,0.00019362534,0.00019733093,0.0008626561,0.0013780867,0.0024706475,0.0007241021,0.00079889654,0.055077083],"study_design_scores_gemma":[0.000002382169,0.00005216941,0.994194,0.0000101733995,0.000025763076,0.00013959128,0.00022248432,0.00022754761,0.00046614592,0.00005380091,0.0046020993,0.000003834346],"about_ca_topic_score_codex":0.018786563,"about_ca_topic_score_gemma":0.032321736,"teacher_disagreement_score":0.018786563,"about_ca_system_score_codex":0.0005124381,"about_ca_system_score_gemma":0.00044942982,"threshold_uncertainty_score":0.03735441},"labels":[],"label_agreement":null},{"id":"W1973625983","doi":"10.1029/2007gl030850","title":"Determination of substorm onset timing and location using the THEMIS ground based observatories","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Substorm; Electrojet; Magnetometer; Longitude; Latitude; Magnetosphere; Geology; Physics; Geodesy; Geophysics; Arc (geometry); Sky; Satellite; Noon; Meteorology; Atmospheric sciences; Magnetic field; Astronomy; Earth's magnetic field","score_opus":0.043349867679220305,"score_gpt":0.31883509451208847,"score_spread":0.27548522683286814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973625983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9664773,0.00031593605,0.011958473,0.000095398645,0.00003480071,0.00008621829,0.0077848374,0.0007651076,0.012482084],"genre_scores_gemma":[0.974411,0.00018471346,0.016622975,0.00003207192,0.000032151478,0.00005829403,0.0069251335,0.00006772385,0.0016659056],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988914,0.000011158318,0.000010748609,0.000031750576,0.000029112636,0.000028120816],"domain_scores_gemma":[0.99953055,0.00003518613,0.00019011488,0.00005301656,0.0001301987,0.000060822345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024183914,0.00018374654,0.00021622858,0.0012251028,0.00028733118,0.00042293945,0.00019318296,0.00017830054,0.001572567],"category_scores_gemma":[0.0005944443,0.000106847314,0.00013381727,0.0013738314,0.000103729806,0.00028626504,0.00033768057,0.00026786077,0.0003283895],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003607622,0.000049710317,0.7531491,0.0001190432,0.000054959386,0.00033157112,0.00064134866,0.0013319668,0.1586469,0.0009766229,0.0040983805,0.08023959],"study_design_scores_gemma":[0.000012001855,0.000041271986,0.98089474,0.0000135311875,0.000016975278,0.00014207196,0.00014085251,0.002260202,0.011332892,0.00015341921,0.0049839932,0.000007924335],"about_ca_topic_score_codex":0.013524704,"about_ca_topic_score_gemma":0.04333636,"teacher_disagreement_score":0.013524704,"about_ca_system_score_codex":0.00042708716,"about_ca_system_score_gemma":0.00028018854,"threshold_uncertainty_score":0.026892006},"labels":[],"label_agreement":null},{"id":"W1973907743","doi":"10.1029/2002gl016719","title":"The Dufek and Forrestal intrusions, Antarctica: A centre for Ferrar Large Igneous Province dike emplacement?","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dike; Geology; Sill; Doming; Mantle plume; Imbrication; Plume; Large igneous province; Igneous rock; Gondwana; Impact crater; Seismology; Geomorphology; Paleontology; Geophysics; Geochemistry; Tectonics; Magmatism; Lithosphere","score_opus":0.02518584439878035,"score_gpt":0.2921641502989215,"score_spread":0.26697830590014116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973907743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99272585,0.000945537,0.00006044884,0.000594372,0.000021402431,0.000013871434,0.00022066293,0.000008586512,0.005409332],"genre_scores_gemma":[0.9975163,0.0005861804,0.00019385583,0.00008639816,0.000020012709,0.000004264326,0.00018099755,0.0000029204073,0.0014092146],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992085,0.0000051932593,0.0000032400426,0.000012689188,0.0000104337005,0.000047508525],"domain_scores_gemma":[0.999821,0.000011378434,0.00007648001,0.000019642253,0.000035693494,0.000035902252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013049152,0.00019966553,0.00016620322,0.0004903626,0.0011507,0.000833463,0.0002418101,0.00047699828,0.002889636],"category_scores_gemma":[0.0004170189,0.00012993117,0.00014686253,0.0006177359,0.0005444776,0.00063476764,0.00047049153,0.00027441987,0.0003904488],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026736927,0.00002282428,0.9475184,0.000081315105,0.000035295554,0.002653387,0.0019318812,0.00006938416,0.007948441,0.0006232651,0.0012321868,0.037616238],"study_design_scores_gemma":[0.000008434665,0.000025228417,0.9901764,0.00001934068,0.000015722511,0.0010618685,0.0017572589,0.000052532374,0.0003841447,0.00006629994,0.006427715,0.0000050545545],"about_ca_topic_score_codex":0.10420425,"about_ca_topic_score_gemma":0.27590337,"teacher_disagreement_score":0.10420425,"about_ca_system_score_codex":0.0009209368,"about_ca_system_score_gemma":0.0010563823,"threshold_uncertainty_score":0.2071954},"labels":[],"label_agreement":null},{"id":"W1973925446","doi":"10.1029/2000gl012822","title":"Azimuth‐time‐intensity striations of quasiperiodic radar echoes from the midlatitude E region ionosphere","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National de la Recherche Scientifique","keywords":"Striation; Azimuth; Geology; Ionosphere; Quasiperiodic function; Middle latitudes; Radar; Geodesy; Geophysics; Incoherent scatter; F region; Doppler effect; Physics; Optics; Atmospheric sciences; Astronomy","score_opus":0.0217842791703921,"score_gpt":0.2760101207416425,"score_spread":0.2542258415712504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1973925446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739885,0.00008196674,0.0012147131,0.000012709496,0.000006213893,0.000004417304,0.00015152169,0.00003578455,0.0010939181],"genre_scores_gemma":[0.9986941,0.000046844507,0.0007382812,0.0000052910364,0.000006375894,0.0000025335978,0.00024352015,0.0000090778185,0.00025396916],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999659,0.00000427492,0.0000018209919,0.000007671401,0.000012310415,0.000008089459],"domain_scores_gemma":[0.99979097,0.000055950477,0.000061869076,0.000017578439,0.000036140194,0.000037504997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009876884,0.0000956931,0.000075479475,0.0005339111,0.00006726226,0.0001614899,0.00008146322,0.0000902223,0.00085694034],"category_scores_gemma":[0.00035690854,0.00008295605,0.00007517448,0.000291038,0.000083840474,0.000116492665,0.00012613085,0.00012009731,0.0001449095],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000489654,0.00008953739,0.22824776,0.00012820454,0.00007593543,0.00068221544,0.00069743796,0.002721277,0.6987053,0.00042834895,0.0008857345,0.06684846],"study_design_scores_gemma":[0.000007197657,0.00008592966,0.98572993,0.000004497723,0.000011252873,0.00033706523,0.00008055011,0.0035529379,0.00936863,0.000060547114,0.0007526165,0.000008838092],"about_ca_topic_score_codex":0.0006720735,"about_ca_topic_score_gemma":0.001036853,"teacher_disagreement_score":0.00085694034,"about_ca_system_score_codex":0.000073052746,"about_ca_system_score_gemma":0.0000485831,"threshold_uncertainty_score":0.002866745},"labels":[],"label_agreement":null},{"id":"W1974186354","doi":"10.1029/2005gl025181","title":"Inflation model of Uzon caldera, Kamchatka, constrained by satellite radar interferometry observations","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; California Institute of Technology; Jet Propulsion Laboratory; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Caldera; Geology; Interferometric synthetic aperture radar; Volcano; Deformation (meteorology); Magma; Seismology; Geodesy; Magma chamber; Synthetic aperture radar; Interferometry; Satellite; Remote sensing","score_opus":0.02906924825000049,"score_gpt":0.27162506183025253,"score_spread":0.24255581358025205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974186354","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99515355,0.00007166809,0.0028169616,0.000078698555,0.0000048779584,0.000011288481,0.00018226523,0.000030055598,0.0016506148],"genre_scores_gemma":[0.99924636,0.000033255947,0.00032486796,0.0000067841956,0.0000023364685,0.0000068914455,0.00015190561,0.000008926259,0.00021875594],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991167,0.000012484651,0.0000059532795,0.00003154389,0.000008834843,0.000029528786],"domain_scores_gemma":[0.9998785,0.000029331259,0.00003687851,0.000012199041,0.000019624697,0.00002345984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012948616,0.00040419836,0.0003553751,0.00039518354,0.00040777674,0.00086195994,0.00056746684,0.00069250213,0.0008483592],"category_scores_gemma":[0.0006624493,0.00046755685,0.00035937876,0.00027603234,0.00054461206,0.0005969617,0.00052875647,0.00037161013,0.00013361442],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002526221,0.000055349257,0.107135944,0.00003955516,0.00009507867,0.0009781237,0.00020897177,0.8703569,0.010508102,0.0064631696,0.0004415981,0.0034645235],"study_design_scores_gemma":[0.0000647854,0.000033252374,0.050617486,0.0000082570505,0.00004484379,0.0001094908,0.00010554509,0.94632596,0.0006963479,0.0015303016,0.0004439813,0.000019715626],"about_ca_topic_score_codex":0.054963548,"about_ca_topic_score_gemma":0.026635818,"teacher_disagreement_score":0.054963548,"about_ca_system_score_codex":0.0011834657,"about_ca_system_score_gemma":0.0008830261,"threshold_uncertainty_score":0.10928726},"labels":[],"label_agreement":null},{"id":"W1974323811","doi":"10.1029/2001gl014188","title":"Sunphotometric observations of the 2001 Asian dust storm over Canada and the U.S.","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"Plume; Dust storm; Storm; Climatology; Asian Dust; Environmental science; Aerosol; Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.034113194280365196,"score_gpt":0.2525050242366044,"score_spread":0.21839182995623924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974323811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99047184,0.00012023058,0.00022650747,0.00004061311,0.0000069447783,0.000014829746,0.0058820555,0.00006022997,0.003176722],"genre_scores_gemma":[0.988897,0.00026821438,0.0010201298,0.00003574722,0.000007876428,0.00000840377,0.008026667,0.000011416567,0.0017243781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999032,0.0000026330895,0.000002775443,0.000014670237,0.00005081654,0.000026019432],"domain_scores_gemma":[0.9997707,0.000010796924,0.00002603713,0.000008393494,0.00013743214,0.00004674939],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008692748,0.00017807781,0.00013206767,0.00060286757,0.0006665181,0.00037700718,0.00016804486,0.00013110042,0.0007184891],"category_scores_gemma":[0.00019121495,0.00010278231,0.00009369201,0.001079844,0.00019351573,0.00014800209,0.00022169099,0.00015687835,0.00010395954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044517388,0.000121715144,0.9093408,0.00010646427,0.0001144118,0.00037017209,0.0016428403,0.004695939,0.019471401,0.00043559566,0.009682434,0.05357295],"study_design_scores_gemma":[0.000013104006,0.000017608865,0.99296606,0.00000646472,0.000017198938,0.000047786954,0.00032603118,0.0016469755,0.0013612016,0.000038495204,0.0035509558,0.000008205682],"about_ca_topic_score_codex":0.9225971,"about_ca_topic_score_gemma":0.9801697,"teacher_disagreement_score":0.07740289,"about_ca_system_score_codex":0.0035445576,"about_ca_system_score_gemma":0.0035135078,"threshold_uncertainty_score":0.15571743},"labels":[],"label_agreement":null},{"id":"W1974493306","doi":"10.1029/2000gl011585","title":"The Assessment of Marine Gas Hydrates Through Electrical Remote Sounding: Hydrate Without a BSR?","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Clathrate hydrate; Geology; Sediment; Hydrate; Submarine pipeline; Electrical resistivity and conductivity; Mineralogy; Drilling; Petrology; Geomorphology; Oceanography; Materials science","score_opus":0.024743033859714936,"score_gpt":0.3247299881811693,"score_spread":0.2999869543214544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1974493306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920399,0.00017526171,0.0060653538,0.0000524411,0.0000043610466,0.000007484913,0.00007264641,0.000062994164,0.0015196268],"genre_scores_gemma":[0.9978344,0.00007290612,0.001770597,0.0000058499336,0.0000029527089,0.0000023268608,0.000035838264,0.0000036401225,0.00027152334],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999448,0.0000099088775,0.0000020972084,0.000013826852,0.000023502822,0.0000058557407],"domain_scores_gemma":[0.99993324,0.000015735408,0.000017165343,0.000008343856,0.000016923668,0.000008630362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014723832,0.0001838929,0.00015655036,0.00037888702,0.000119571436,0.00018427694,0.00019140648,0.00025659436,0.00053178816],"category_scores_gemma":[0.00033747748,0.00008057359,0.00007764902,0.00017278132,0.00029112265,0.0004267797,0.00027894406,0.00010879291,0.00011903039],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007443002,0.00007777287,0.19245002,0.00024398798,0.00004932901,0.0006717494,0.00034269036,0.011166233,0.6940378,0.0009688212,0.00021862026,0.099028654],"study_design_scores_gemma":[0.000057092813,0.0014003904,0.6270773,0.00003908704,0.000107018815,0.0010971453,0.0012942529,0.097636975,0.2655609,0.0021438338,0.003506854,0.0000791812],"about_ca_topic_score_codex":0.0018763926,"about_ca_topic_score_gemma":0.0037777082,"teacher_disagreement_score":0.0018763926,"about_ca_system_score_codex":0.00009407033,"about_ca_system_score_gemma":0.00007453796,"threshold_uncertainty_score":0.0037310123},"labels":[],"label_agreement":null},{"id":"W1975203671","doi":"10.1029/2003gl019003","title":"A barotropic inverse tidal model for the Arctic Ocean","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":325,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Barotropic fluid; Tide gauge; Bathymetry; Arctic; Geology; Oceanography; Archipelago; Bay; Tidal Model; Climatology; Altimeter; Geodesy; Sea level","score_opus":0.038275002675494094,"score_gpt":0.2743587836709611,"score_spread":0.236083780995467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975203671","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07623215,0.00073359895,0.88170016,0.00039147874,0.0003593557,0.00014630542,0.006823537,0.003719135,0.029894372],"genre_scores_gemma":[0.5837326,0.001579885,0.3700731,0.00020680434,0.00041018357,0.0006988179,0.008348339,0.00087442336,0.034075867],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999341,0.000010554554,0.0000040615287,0.000016150447,0.000025998408,0.000009200176],"domain_scores_gemma":[0.9999248,0.000013081129,0.000010664326,0.000012032388,0.000028409251,0.000011124915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016885437,0.00046469603,0.00037647778,0.00022512057,0.0004628669,0.0006651059,0.0011510826,0.0006516783,0.002698376],"category_scores_gemma":[0.0003583478,0.00038790097,0.00054960465,0.00041453974,0.0001983082,0.00058394263,0.00054046523,0.000571957,0.0016795732],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002171734,0.000023232875,0.0015741393,0.000032021857,0.000034444456,0.000054985525,0.00004678985,0.96423876,0.0026731724,0.012436356,0.0028301922,0.0160342],"study_design_scores_gemma":[0.000009448184,0.000008789274,0.00031338917,0.000002798701,0.000008741642,0.000018579942,0.0000037906166,0.9888898,0.00025280277,0.0022073437,0.008277238,0.0000072225685],"about_ca_topic_score_codex":0.02614295,"about_ca_topic_score_gemma":0.024906665,"teacher_disagreement_score":0.02614295,"about_ca_system_score_codex":0.00045774574,"about_ca_system_score_gemma":0.0011177469,"threshold_uncertainty_score":0.05198157},"labels":[],"label_agreement":null},{"id":"W1975270494","doi":"10.1029/2006gl026231","title":"Carbon monoxide (CO) maximum over the Zagros mountains in the Middle East: Signature of mountain venting?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Troposphere; Daytime; Climatology; Atmospheric sciences; Environmental science; Geology; Carbon monoxide; Ozone; Meteorology; Geography","score_opus":0.030480618352225586,"score_gpt":0.2612652197895924,"score_spread":0.2307846014373668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975270494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99963784,0.00007474769,0.000025316824,0.0000170539,0.0000020842365,8.996528e-7,0.000043728778,0.000004012868,0.00019438432],"genre_scores_gemma":[0.99981743,0.00003744626,0.000041070158,0.0000065965596,0.0000073873744,5.6947874e-7,0.000051855983,6.5779426e-7,0.000036964782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996495,0.0000024083972,0.0000026000039,0.000008976881,0.000005536248,0.000015498548],"domain_scores_gemma":[0.99991953,0.000006769352,0.00004347577,0.000008031922,0.000008938033,0.000013233034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000610085,0.000106824904,0.0001564641,0.00031522795,0.00030330723,0.0003366192,0.00016351287,0.00022279311,0.00041351296],"category_scores_gemma":[0.000107076085,0.00008607786,0.00010651141,0.00038033008,0.00018379543,0.00017487934,0.00021840629,0.00011782759,0.0000769834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031375073,0.000044652137,0.9640119,0.000041683492,0.000051484316,0.0012694089,0.00044787786,0.00020271125,0.024780037,0.000075385746,0.00022388436,0.008537279],"study_design_scores_gemma":[0.0000038499147,0.000021026728,0.9988784,0.000001992251,0.0000081204,0.00016005762,0.00012550193,0.00012236387,0.00047486232,0.00001215732,0.00018998902,0.0000016255862],"about_ca_topic_score_codex":0.009050383,"about_ca_topic_score_gemma":0.016203243,"teacher_disagreement_score":0.009050383,"about_ca_system_score_codex":0.00015921828,"about_ca_system_score_gemma":0.00011640338,"threshold_uncertainty_score":0.017995358},"labels":[],"label_agreement":null},{"id":"W1975302322","doi":"10.1029/2008gl033428","title":"Spatial and temporal variation of sediment yield in the landscape: Example of Huanghe (Yellow River)","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Tributary; Sediment; Structural basin; Erosion; Hydrology (agriculture); Geology; Floodplain; Loess; Loess plateau; Sedimentary budget; Drainage basin; Spatial variability; Sedimentary rock; Yield (engineering); Sediment transport; Physical geography; Geomorphology; Soil science; Geography","score_opus":0.06861532657610098,"score_gpt":0.26820381786391917,"score_spread":0.1995884912878182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975302322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99952304,0.000012739128,0.00007191368,0.000010573,4.988264e-7,9.691014e-7,0.000117316886,0.000007039691,0.00025598743],"genre_scores_gemma":[0.99963903,0.0000104208775,0.000089561414,0.0000010095285,7.14781e-7,0.0000012292145,0.00013047723,0.0000012459501,0.00012637462],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.0000056800427,0.000002138618,0.000012510695,0.0000053741055,0.000013873681],"domain_scores_gemma":[0.9998012,0.00004213301,0.00004375612,0.000018463936,0.00004798589,0.000046457564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011365659,0.00009175262,0.00010357512,0.0005763018,0.00020647426,0.00022935926,0.00015875303,0.00015127486,0.0010171613],"category_scores_gemma":[0.00038179586,0.00008303036,0.00012410068,0.00090345327,0.0001992764,0.00015869779,0.00025972247,0.00010072246,0.00006555134],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026131078,0.00007902617,0.9411256,0.00005238331,0.00011830863,0.0014522246,0.0015320916,0.01494361,0.016331023,0.001021334,0.00097134296,0.022111777],"study_design_scores_gemma":[0.0000039241113,0.000016489957,0.98979974,0.0000018627575,0.000015899335,0.00007785907,0.0002441323,0.009305088,0.00022848333,0.000061939776,0.00023918145,0.0000055470823],"about_ca_topic_score_codex":0.047351554,"about_ca_topic_score_gemma":0.070066154,"teacher_disagreement_score":0.047351554,"about_ca_system_score_codex":0.0003434568,"about_ca_system_score_gemma":0.00014391226,"threshold_uncertainty_score":0.094151855},"labels":[],"label_agreement":null},{"id":"W1975450477","doi":"10.1029/2006gl026113","title":"Temporal fluctuations of microseismic noise in Yellowstone's Upper Geyser Basin from a continuous gravity observation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geoscience BC; North Pacific Marine Science Organization","funders":"Japan Society for the Promotion of Science; National Aeronautics and Space Administration; National Science Foundation","keywords":"Microseism; Geology; Noise (video); Seismology; Structural basin; Amplitude; Seismic noise; Caldera; Geodesy; Geophysics; Geomorphology; Volcano; Physics","score_opus":0.02271755063273904,"score_gpt":0.2647540738245521,"score_spread":0.2420365231918131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975450477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998005,0.000007017926,0.00003513306,0.0000051463617,2.9012637e-7,0.0000010004755,0.000058316607,0.0000026718226,0.000089987814],"genre_scores_gemma":[0.99966943,0.000008712499,0.00006656235,0.0000024249591,0.0000014778591,0.0000015952425,0.00017340008,0.0000010063131,0.00007543604],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999018,0.000008278182,0.0000068349045,0.000029404144,0.00002978976,0.0000239184],"domain_scores_gemma":[0.99976546,0.000035131565,0.000076103184,0.000022646263,0.000051284136,0.000049375525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018040571,0.00014245196,0.00016143061,0.0005490983,0.00018212506,0.00025765758,0.00016371833,0.00020394803,0.00035626112],"category_scores_gemma":[0.0006110071,0.00010545723,0.00008461837,0.0005572734,0.00027562655,0.00015577427,0.00047995694,0.00012551415,0.000079185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014777374,0.00002144882,0.9729004,0.000013740263,0.000032302418,0.00025462566,0.0010256802,0.0009488791,0.018732088,0.00006863242,0.00013384155,0.005720572],"study_design_scores_gemma":[0.000001326823,0.0000069574085,0.9992482,7.461779e-7,0.0000021638207,0.000016629518,0.000048408205,0.0004430279,0.0001545866,0.0000050970802,0.00007174041,0.0000011497577],"about_ca_topic_score_codex":0.031494748,"about_ca_topic_score_gemma":0.06453345,"teacher_disagreement_score":0.031494748,"about_ca_system_score_codex":0.00043062193,"about_ca_system_score_gemma":0.0001983063,"threshold_uncertainty_score":0.062622845},"labels":[],"label_agreement":null},{"id":"W1975590034","doi":"10.1029/2007gl030947","title":"Abrupt environmental change in Canada’s northernmost lake inferred from fossil diatom and pigment stratigraphy","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Canadian Obesity Network; University of Toronto; Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; ArcticNet","keywords":"Diatom; Arctic; Sedimentary rock; Paleolimnology; Geology; Oceanography; Sediment; Climate change; Environmental change; Latitude; Physical geography; Paleontology; Geography","score_opus":0.0301007341941279,"score_gpt":0.2635743997158754,"score_spread":0.23347366552174748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975590034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99863017,0.00011533558,0.000025210198,0.00006265354,0.0000020421007,0.0000032357614,0.00033733764,0.000003965498,0.000820082],"genre_scores_gemma":[0.9993279,0.00008960145,0.00006633945,0.000021820486,0.0000015035471,0.0000020494099,0.00027343153,0.0000018476952,0.00021549976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998746,0.000005750791,0.000005028506,0.000025397017,0.000031403328,0.00005787999],"domain_scores_gemma":[0.99962676,0.000024917485,0.000062025145,0.000010086776,0.00017910826,0.00009715897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014157663,0.00014384367,0.00018224458,0.0010415526,0.0016694171,0.0011010896,0.0003678446,0.00032712801,0.0008616204],"category_scores_gemma":[0.00064851384,0.00024602353,0.00013373028,0.0017777493,0.00088400225,0.00030969564,0.00065395294,0.00029465414,0.00009427669],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000079150755,0.000014724805,0.9888819,0.000022877935,0.00003571941,0.00020413278,0.0013721011,0.00046415694,0.0028321252,0.00017250958,0.00044672695,0.0054738726],"study_design_scores_gemma":[0.0000010681229,0.0000021090202,0.99882895,0.000004121919,0.000004281747,0.000017474349,0.0005333489,0.00017087057,0.00007117758,0.000014582845,0.00034916284,0.000002947995],"about_ca_topic_score_codex":0.9629491,"about_ca_topic_score_gemma":0.9886634,"teacher_disagreement_score":0.037050903,"about_ca_system_score_codex":0.012077163,"about_ca_system_score_gemma":0.0071794237,"threshold_uncertainty_score":0.0876264},"labels":[],"label_agreement":null},{"id":"W1975898009","doi":"10.1029/2007gl033057","title":"Nitrous oxide emissions from tropical hydroelectric reservoirs","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hydro-Québec","funders":"","keywords":"Environmental science; Nitrous oxide; Tropical rainforest; Hydrology (agriculture); Greenhouse gas; Hydroelectricity; Tropical climate; Tropics; Flooding (psychology); Ecosystem; Atmospheric sciences; Rainforest; Oceanography; Ecology; Geology","score_opus":0.021056167208696113,"score_gpt":0.25784685680086983,"score_spread":0.23679068959217373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1975898009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99168783,0.003505103,0.0006297503,0.00006828046,0.000009991781,0.0000055140667,0.0010860581,0.000024203588,0.0029832995],"genre_scores_gemma":[0.9925841,0.0051481146,0.00047830635,0.000025187275,0.00001944107,0.000009004848,0.0008861416,0.0000072165926,0.0008426003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.000010179453,0.000006011407,0.000018820876,0.0000310697,0.000013151287],"domain_scores_gemma":[0.9998622,0.000032574797,0.000051989085,0.0000070105257,0.000037080088,0.000009121484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011913327,0.00027351896,0.00012050753,0.00067238044,0.00024136322,0.0003125389,0.00010254686,0.00010573675,0.00038217075],"category_scores_gemma":[0.00019062168,0.0000747597,0.00015237874,0.0009445038,0.00009228692,0.00030210434,0.00023662938,0.00010018468,0.000050815877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062545185,0.00007304592,0.6465293,0.0012319009,0.00041504932,0.0013110195,0.0012400487,0.007925552,0.23314473,0.00078271044,0.001487346,0.1052338],"study_design_scores_gemma":[0.000016072436,0.00017797225,0.90841985,0.000107770764,0.00025300146,0.0005025839,0.0004493113,0.0026875767,0.06416722,0.00048765168,0.022689473,0.000041506086],"about_ca_topic_score_codex":0.013823263,"about_ca_topic_score_gemma":0.02900366,"teacher_disagreement_score":0.013823263,"about_ca_system_score_codex":0.0005150042,"about_ca_system_score_gemma":0.00018884624,"threshold_uncertainty_score":0.027485609},"labels":[],"label_agreement":null},{"id":"W1976021042","doi":"10.1029/2006gl027644","title":"Discontinuities in the late 1960's in different atmospheric data products","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Met Office; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Classification of discontinuities; Troposphere; Climatology; Precipitation; Environmental science; Atmosphere (unit); Atmospheric sciences; Atmospheric circulation; Geology; Meteorology; Geography; Mathematics","score_opus":0.054783547144329474,"score_gpt":0.3023813947771598,"score_spread":0.24759784763283033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976021042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888487,0.0009380117,0.0020261835,0.0001018455,0.000023552706,0.000013922588,0.0043354966,0.00008668148,0.003625678],"genre_scores_gemma":[0.9932233,0.00024248475,0.0015836002,0.00001251909,0.000013321496,0.000011915659,0.0043286183,0.000015854768,0.0005683429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995672,0.00005542008,0.000052179603,0.000102459904,0.00011982455,0.000102828366],"domain_scores_gemma":[0.9971757,0.0011197521,0.0007229615,0.00019057517,0.0006571092,0.00013380228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014483291,0.00018851271,0.00019349378,0.0027011891,0.0003741115,0.0009699136,0.00014064806,0.0002938154,0.00095763785],"category_scores_gemma":[0.0043480573,0.00019968342,0.00027882308,0.0040955315,0.00021621933,0.000685654,0.0005068383,0.00057716214,0.00022850864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053016056,0.00007556355,0.91866744,0.00010741927,0.00010282463,0.00058362924,0.0016659911,0.0048485817,0.0077487165,0.003299333,0.002175986,0.06019422],"study_design_scores_gemma":[0.0000060302373,0.000028168692,0.9917065,0.000023256343,0.00002130149,0.00009239321,0.00021817922,0.0016187895,0.0010351571,0.00029862777,0.0049407193,0.000010943181],"about_ca_topic_score_codex":0.014014758,"about_ca_topic_score_gemma":0.013141564,"teacher_disagreement_score":0.014014758,"about_ca_system_score_codex":0.000774413,"about_ca_system_score_gemma":0.00023282331,"threshold_uncertainty_score":0.027866364},"labels":[],"label_agreement":null},{"id":"W1976031057","doi":"10.1029/2008gl033794","title":"Simultaneous THEMIS in situ and auroral observations of a small substorm","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University; University of Alberta; Canadian Space Agency; University of Calgary","funders":"Science and Technology Facilities Council","keywords":"Substorm; Front (military); Geophysics; Geology; Physics; Field line; Arc (geometry); Magnetic field; Astrophysics; Magnetosphere; Meteorology; Geometry","score_opus":0.0376701249378852,"score_gpt":0.27543869196248705,"score_spread":0.23776856702460186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976031057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99358314,0.000061771854,0.00048006664,0.00006476142,0.000020493771,0.000013919088,0.0014023188,0.000103455204,0.004270017],"genre_scores_gemma":[0.9958448,0.00005566813,0.0010464431,0.000033202374,0.00004627306,0.000015845306,0.0024225384,0.000015701647,0.0005195991],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990666,0.000005843234,0.0000049053624,0.00002723184,0.000028059801,0.00002736477],"domain_scores_gemma":[0.99976975,0.000022999546,0.00005377636,0.000028960469,0.000059562593,0.00006489947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000183742,0.00019486142,0.0002905567,0.0007672643,0.0006785283,0.00045549995,0.00029407378,0.00036649086,0.000691246],"category_scores_gemma":[0.00024132388,0.00016012615,0.00019111998,0.0006278148,0.00017439478,0.00027162657,0.00042563662,0.00034415562,0.00013702564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011790564,0.00052242656,0.60840815,0.00013026231,0.0001586845,0.00132816,0.0018518998,0.0030041088,0.3366779,0.0008360009,0.007464491,0.03843884],"study_design_scores_gemma":[0.00003598183,0.00012042205,0.981122,0.000013001329,0.000051406,0.0003091519,0.0003172012,0.002896074,0.011101405,0.00010822426,0.0039127804,0.000012407764],"about_ca_topic_score_codex":0.008277244,"about_ca_topic_score_gemma":0.035215776,"teacher_disagreement_score":0.008277244,"about_ca_system_score_codex":0.0005216982,"about_ca_system_score_gemma":0.00027613342,"threshold_uncertainty_score":0.016458094},"labels":[],"label_agreement":null},{"id":"W1976133708","doi":"10.1029/2008gl034888","title":"Severe hail frequency over Ontario, Canada: Recent trend and variability","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Precipitable water; Climatology; Environmental science; Meteorology; Lag; Severe weather; Atmospheric sciences; Convective storm detection; Convection; Precipitation; Geography; Geology; Storm","score_opus":0.05108032801221818,"score_gpt":0.25988264449677256,"score_spread":0.20880231648455438,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976133708","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98413783,0.0010354224,0.0003272725,0.0006865142,0.000019973042,0.00001453634,0.009622726,0.000034526063,0.0041212016],"genre_scores_gemma":[0.9937429,0.00054650666,0.00017713504,0.00006230941,0.000010672059,0.000005992166,0.0032240066,0.000007460907,0.0022231275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996433,0.000012738983,0.00002243078,0.0000627645,0.000154318,0.00010444447],"domain_scores_gemma":[0.99697876,0.00014501774,0.00064381474,0.00007218649,0.0016974362,0.00046285437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034453443,0.00018993008,0.00025371986,0.0012766741,0.0010299829,0.0010945195,0.0007683654,0.00028123282,0.0016892691],"category_scores_gemma":[0.0013085708,0.00019121604,0.00028669933,0.003821364,0.0006246292,0.00035443922,0.0005317952,0.00040671573,0.00019408875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009292062,0.000014444772,0.9840965,0.00006380649,0.000114351555,0.00010578352,0.0010248354,0.00083441753,0.00073457777,0.0002145847,0.0023643654,0.010339497],"study_design_scores_gemma":[0.000002047513,0.000006018664,0.9970822,0.000008126246,0.000010974069,0.000023396706,0.0004482731,0.00045201715,0.000066398956,0.000013585016,0.0018798931,0.000007095372],"about_ca_topic_score_codex":0.99423003,"about_ca_topic_score_gemma":0.9972566,"teacher_disagreement_score":0.01642881,"about_ca_system_score_codex":0.01642881,"about_ca_system_score_gemma":0.015843963,"threshold_uncertainty_score":0.11919993},"labels":[],"label_agreement":null},{"id":"W1976217903","doi":"10.1029/2009gl037422","title":"Os‐isotope insights into major environmental changes of the Arctic Ocean during the Cenozoic","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Cenozoic; Sedimentary rock; Chronology; Paleontology; Ridge; Radiogenic nuclide; Arctic; Phanerozoic; Oceanography; Structural basin; Mantle (geology)","score_opus":0.0219487674881151,"score_gpt":0.22996018601949691,"score_spread":0.2080114185313818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976217903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969151,0.00055657694,0.0002473686,0.00003790146,0.0000073379683,8.4736666e-7,0.00018514563,0.000005091881,0.0020446444],"genre_scores_gemma":[0.9984163,0.00046732384,0.0002217226,0.000014339843,0.0000064889873,0.0000010045217,0.00018052378,0.0000057310567,0.0006864615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999802,0.0000028475886,0.0000017295957,0.000005705563,0.0000033708668,0.000006068601],"domain_scores_gemma":[0.99996424,0.000003865209,0.000010750041,0.0000024563608,0.000012148422,0.0000065453496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012754009,0.00016693922,0.00007808973,0.0006004814,0.00024148455,0.00044331522,0.00006471983,0.000093027076,0.0005586676],"category_scores_gemma":[0.00013472592,0.00009692224,0.00007773155,0.00050564884,0.00016194124,0.00019358474,0.00020305664,0.00010024795,0.000066577406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050145655,0.000030703817,0.808463,0.00009280667,0.00008244815,0.00034442736,0.0015619766,0.0016418318,0.14742959,0.002188032,0.000286254,0.037377514],"study_design_scores_gemma":[0.0000028619725,0.00003114053,0.9906489,0.000011810158,0.000022539512,0.00006991247,0.0005088063,0.00059122214,0.004101354,0.00025070002,0.0037564836,0.0000042695065],"about_ca_topic_score_codex":0.017406123,"about_ca_topic_score_gemma":0.055597655,"teacher_disagreement_score":0.017406123,"about_ca_system_score_codex":0.0004582808,"about_ca_system_score_gemma":0.00029892958,"threshold_uncertainty_score":0.034609616},"labels":[],"label_agreement":null},{"id":"W1976338719","doi":"10.1029/2009gl038669","title":"Solar eclipse‐induced E‐region plasma irregularities observed by the Gadanki radar","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Solar eclipse; Plasma; Eclipse; Ionosphere; Sunset; Radar; Physics; Instability; Ion; Geophysics; Atmospheric sciences; Computational physics; Astrophysics; Geology; Astronomy; Mechanics; Aerospace engineering","score_opus":0.035030278425724336,"score_gpt":0.27486496245363584,"score_spread":0.2398346840279115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976338719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911886,0.00004326941,0.00011063656,0.000010208605,0.0000021234246,0.0000025554077,0.000045461562,0.000005328325,0.0006615202],"genre_scores_gemma":[0.9996326,0.000034567034,0.0001457111,0.000007195966,0.000003186562,0.0000017149702,0.0000801666,0.0000014888925,0.000093427974],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.0000036194426,0.00000131793,0.000008911784,0.0000071335553,0.000011774611],"domain_scores_gemma":[0.99990106,0.000020336625,0.000032153548,0.000010215118,0.000014135539,0.000021987038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010429883,0.00011447792,0.00013450118,0.00025050683,0.00015560251,0.00019877711,0.00009487101,0.00016041346,0.00023466257],"category_scores_gemma":[0.00022708297,0.00007210195,0.0000704458,0.00016521031,0.00013293364,0.00011293396,0.00025426425,0.00018734243,0.00007227143],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012025421,0.0001031132,0.46041027,0.00009643278,0.00009188123,0.0020352323,0.00086411944,0.0013782808,0.513384,0.00035397583,0.0005634146,0.019516835],"study_design_scores_gemma":[0.00003043887,0.00018929479,0.98010075,0.000007791551,0.00003034308,0.00056003884,0.00023082642,0.002342014,0.01503841,0.000072966846,0.0013872494,0.0000098710525],"about_ca_topic_score_codex":0.0009294775,"about_ca_topic_score_gemma":0.0016152128,"teacher_disagreement_score":0.0009294775,"about_ca_system_score_codex":0.000117983756,"about_ca_system_score_gemma":0.0000581447,"threshold_uncertainty_score":0.0018481016},"labels":[],"label_agreement":null},{"id":"W1976601254","doi":"10.1029/2006gl029063","title":"Magnetic phases in hemo‐ilmenite: Insight from low‐velocity and high‐field Mössbauer spectroscopy","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Iron oxide chemistry and applications","field":"Energy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ilmenite; Hematite; Mössbauer spectroscopy; Ferrimagnetism; Stoichiometry; Materials science; Analytical Chemistry (journal); Mineralogy; Spectroscopy; Geology; Crystallography; Chemistry; Magnetic field; Environmental chemistry; Magnetization; Physics; Physical chemistry","score_opus":0.018387815808102073,"score_gpt":0.30754608163426644,"score_spread":0.2891582658261644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976601254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990313,0.0001543611,0.00027640775,0.000018038354,6.746554e-7,0.0000023395617,0.00004731797,0.000006398474,0.0004631414],"genre_scores_gemma":[0.9989911,0.000077352415,0.00031889268,0.0000083628365,8.5029325e-7,0.0000012689453,0.000078382756,0.000002005837,0.00052181596],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99996877,0.000002912466,9.4080445e-7,0.0000069061684,0.0000082065035,0.000012252659],"domain_scores_gemma":[0.9999242,0.000012216166,0.000015939722,0.000005104738,0.00002978662,0.000012718889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000076590186,0.00014472942,0.0000674475,0.00034984192,0.00020738521,0.00030362344,0.00018601476,0.00017470052,0.0005270271],"category_scores_gemma":[0.00016523474,0.00012073296,0.000054249984,0.00015633676,0.00035880296,0.00017351468,0.00007763858,0.00012314104,0.00008311481],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017487646,0.00003109192,0.03616488,0.00005376246,0.000008827113,0.0001944094,0.00031010824,0.00033451454,0.95817286,0.00031901157,0.00004963847,0.004185971],"study_design_scores_gemma":[0.000033818887,0.00019924727,0.54423,0.000020971987,0.000027461858,0.00092134695,0.00067230023,0.005211537,0.4438219,0.00043611755,0.0044045667,0.000020781397],"about_ca_topic_score_codex":0.051664818,"about_ca_topic_score_gemma":0.13559969,"teacher_disagreement_score":0.051664818,"about_ca_system_score_codex":0.0008385046,"about_ca_system_score_gemma":0.00032268898,"threshold_uncertainty_score":0.10272819},"labels":[],"label_agreement":null},{"id":"W1976714714","doi":"10.1029/2001gl013023","title":"Retention of dissolved iron and Fe<i><sup>II</sup></i> in an iron induced Southern Ocean phytoplankton bloom","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":145,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bloom; Phytoplankton; Nitrate; Environmental chemistry; Chemistry; Algal bloom; Ligand (biochemistry); Nutrient; Oceanography; Geology","score_opus":0.03056226044812439,"score_gpt":0.2588686453565336,"score_spread":0.2283063849084092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976714714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997924,0.000020222096,0.000048336922,0.000007196423,9.096225e-7,8.4141004e-7,0.000034849,0.0000033366027,0.00009184895],"genre_scores_gemma":[0.99898905,0.000029310531,0.00022049775,0.000018176568,0.0000020035197,0.000004352544,0.00020300635,0.0000043511577,0.0005291971],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999641,0.0000054202023,0.0000025917134,0.0000101383785,0.000007890102,0.000009860192],"domain_scores_gemma":[0.99987495,0.000026974498,0.000025990674,0.000013079416,0.000020391404,0.000038667313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013730855,0.00011355963,0.0002147931,0.0001225059,0.0001680418,0.0002453744,0.000096720585,0.00022766658,0.00041537415],"category_scores_gemma":[0.0002089265,0.00014613627,0.00009292361,0.00010731252,0.00027136825,0.00014370165,0.00016732328,0.00035959794,0.000118624965],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008688864,0.000042343272,0.031969905,0.00001945072,0.0000117710015,0.00010719465,0.000111161826,0.0001100637,0.9649734,0.000041492218,0.000036404876,0.0017081338],"study_design_scores_gemma":[0.00005686872,0.0011937516,0.7551629,0.0000059809627,0.000033828797,0.00022522947,0.0002640619,0.0016234176,0.24048963,0.00013407419,0.00079345255,0.000016763503],"about_ca_topic_score_codex":0.0019558903,"about_ca_topic_score_gemma":0.0031069638,"teacher_disagreement_score":0.0019558903,"about_ca_system_score_codex":0.00031246204,"about_ca_system_score_gemma":0.00017449041,"threshold_uncertainty_score":0.0038889647},"labels":[],"label_agreement":null},{"id":"W1976815994","doi":"10.1029/2008gl035201","title":"Whistler waves associated with magnetic reconnection","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Whistler; Physics; Electron; Pitch angle; Magnetic reconnection; Computational physics; Magnetic field; Field line; Geophysics; Anisotropy; Optics","score_opus":0.02298555658356854,"score_gpt":0.26079889297017356,"score_spread":0.237813336386605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1976815994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920657,0.000054491295,0.0034910068,0.00015974788,0.000030340832,0.000019890607,0.00006610724,0.00012698116,0.0039857123],"genre_scores_gemma":[0.99810946,0.000035342116,0.0010398048,0.00002351138,0.0000074761733,0.00001893731,0.000082775055,0.00002919708,0.00065341505],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998939,0.000020248968,0.0000037731238,0.000013410376,0.000021690974,0.000046963396],"domain_scores_gemma":[0.99952817,0.00018082344,0.000072039446,0.000041635936,0.00005740479,0.00011988549],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002507403,0.00033348633,0.0006165816,0.00027261584,0.0008323217,0.0008990368,0.0006040461,0.00089428585,0.0025890456],"category_scores_gemma":[0.0014816005,0.00034699414,0.000437269,0.00037448437,0.00077044073,0.00064086955,0.000603693,0.0008360222,0.0001534017],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016563266,0.00010902599,0.00747066,0.000045541732,0.000058837497,0.0006741202,0.00025706732,0.97691524,0.0055379374,0.0050538913,0.0010251298,0.0026869522],"study_design_scores_gemma":[0.000086280845,0.000033270444,0.0017763252,0.0000023797515,0.0000106275775,0.000028567792,0.00005000886,0.99626154,0.00070728903,0.0008456531,0.00018918235,0.0000088490715],"about_ca_topic_score_codex":0.013563342,"about_ca_topic_score_gemma":0.0053726905,"teacher_disagreement_score":0.013563342,"about_ca_system_score_codex":0.00067249185,"about_ca_system_score_gemma":0.0008303931,"threshold_uncertainty_score":0.026968777},"labels":[],"label_agreement":null},{"id":"W1977230097","doi":"10.1029/2005gl023922","title":"Assessing the impact of changes in climate and CO<sub>2</sub> on potential carbon sequestration in agricultural soils","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Biological and Environmental Research; Office of Science","keywords":"Carbon sequestration; Environmental science; Soil carbon; Soil water; Tillage; Carbon cycle; Carbon fibers; Climate change; Atmospheric carbon cycle; Greenhouse gas; Soil science; Atmospheric sciences; Carbon dioxide; Environmental chemistry; Agronomy; Chemistry; Geology; Ecology; Ecosystem; Oceanography","score_opus":0.03477474659659239,"score_gpt":0.32653060291016234,"score_spread":0.29175585631356993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977230097","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99811757,0.00010167664,0.00046480558,0.00007399375,0.0000034796044,0.000008938346,0.00023025558,0.000011365213,0.0009879583],"genre_scores_gemma":[0.99909484,0.00015270011,0.00036356846,0.000018458757,0.0000021187857,0.0000033439044,0.00015123331,0.0000029196165,0.00021082645],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989414,0.000041360287,0.000004604853,0.00001459333,0.000018425388,0.000026749427],"domain_scores_gemma":[0.99953496,0.000297516,0.000050851675,0.000016530248,0.00005713042,0.000043077525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003711959,0.00040168336,0.00019052411,0.00017182171,0.0002352753,0.0005431481,0.00026570942,0.0005876138,0.0012599408],"category_scores_gemma":[0.0011993091,0.00018621494,0.0003202592,0.00027712216,0.00027378483,0.00065973884,0.00024168126,0.00022740626,0.0000943097],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061801064,0.00019627447,0.23766313,0.00018747189,0.00025174153,0.00033643108,0.000058061574,0.72587574,0.02152265,0.0014202463,0.00047013082,0.011400138],"study_design_scores_gemma":[0.00008784757,0.0005178943,0.250371,0.00001871164,0.0002082981,0.00010222139,0.00028420732,0.73058045,0.014766848,0.001806555,0.0012164825,0.000039480467],"about_ca_topic_score_codex":0.12571749,"about_ca_topic_score_gemma":0.1610199,"teacher_disagreement_score":0.12571749,"about_ca_system_score_codex":0.0020098458,"about_ca_system_score_gemma":0.0014376115,"threshold_uncertainty_score":0.24997145},"labels":[],"label_agreement":null},{"id":"W1977449139","doi":"10.1029/2007gl031076","title":"Fluid‐induced rupture experiment on Fontainebleau sandstone: Premonitory activity, rupture propagation, and aftershocks","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Aftershock; Fault plane; Differential stress; Acoustic emission; Pore water pressure; Nucleation; Overburden pressure; Permeability (electromagnetism); Porosity; Geotechnical engineering; Mineralogy; Composite material; Seismology; Fault (geology); Materials science; Deformation (meteorology)","score_opus":0.02986361660801322,"score_gpt":0.30676501321506566,"score_spread":0.27690139660705243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1977449139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997937,0.000008304533,0.000072784685,0.0000022732472,8.9188876e-7,0.000003647719,0.000025051082,0.000004124233,0.000089230576],"genre_scores_gemma":[0.9994733,0.000015123354,0.00016416489,0.0000024333876,0.0000012371162,0.0000051616908,0.000058466005,0.0000011990085,0.0002789087],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999119,0.000007532043,0.0000059507097,0.000024678937,0.000026430567,0.000023415649],"domain_scores_gemma":[0.99981683,0.000035767625,0.000041022176,0.000019342204,0.00004704508,0.00003998803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014420829,0.00024012053,0.00038554778,0.00032398396,0.00034433513,0.00020185365,0.00035426626,0.00036183852,0.0008353402],"category_scores_gemma":[0.00027050907,0.00016394672,0.00018320038,0.00025152517,0.0003515413,0.00017353703,0.00036185712,0.00027934008,0.000116447794],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014183641,0.00022691757,0.016231189,0.000038487444,0.00002125659,0.00045414318,0.00026410905,0.0023445978,0.9754916,0.000054125012,0.000032633016,0.0034226123],"study_design_scores_gemma":[0.00015252143,0.0053387713,0.28675285,0.00001059263,0.000050312156,0.00028148256,0.00032503958,0.021540605,0.68444973,0.00009657903,0.0009635635,0.00003784608],"about_ca_topic_score_codex":0.006447809,"about_ca_topic_score_gemma":0.0078111608,"teacher_disagreement_score":0.006447809,"about_ca_system_score_codex":0.00032673968,"about_ca_system_score_gemma":0.00019043092,"threshold_uncertainty_score":0.012820601},"labels":[],"label_agreement":null},{"id":"W1978013062","doi":"10.1029/2005gl024360","title":"Modification of the dichotomy boundary on Mars by Amazonian mid‐latitude regional glaciation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":135,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Geology; Glacial period; Amazonian; Mars Exploration Program; Landform; Paleontology; Geomorphology; Geophysics; Astrobiology; Physics; Amazon rainforest","score_opus":0.028979008621547578,"score_gpt":0.2870259042541215,"score_spread":0.25804689563257394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978013062","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991015,0.000057032987,0.00007913293,0.000027725051,0.0000015136923,0.0000012610675,0.000039737486,0.000009807468,0.00068223366],"genre_scores_gemma":[0.9997892,0.00001810628,0.000085906955,0.000005727477,0.0000011801544,9.786959e-7,0.000049462567,0.000002546764,0.000046798203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999132,0.000014138893,0.0000036946028,0.000022769702,0.000021691556,0.0000245368],"domain_scores_gemma":[0.9998362,0.000015492196,0.00007051631,0.000017626657,0.000027863967,0.00003224026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009125847,0.000059766575,0.000174864,0.0003497317,0.00060822314,0.00061059906,0.00016402444,0.00020947326,0.0008332323],"category_scores_gemma":[0.00053768005,0.00008946972,0.00009361842,0.00026270252,0.0004644983,0.0002781545,0.00070564053,0.00022624792,0.000105644634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076149503,0.00005507982,0.8294542,0.000057325764,0.00006813903,0.0010545526,0.0034440737,0.0016657813,0.1250827,0.0017550467,0.0006171661,0.03598441],"study_design_scores_gemma":[0.000011379921,0.000031012223,0.9962584,0.0000075097696,0.00000597426,0.00022289781,0.0005453313,0.00072328653,0.00083813386,0.00017733227,0.0011738208,0.0000049238342],"about_ca_topic_score_codex":0.006625569,"about_ca_topic_score_gemma":0.0093655465,"teacher_disagreement_score":0.006625569,"about_ca_system_score_codex":0.0004135583,"about_ca_system_score_gemma":0.00014413391,"threshold_uncertainty_score":0.013173997},"labels":[],"label_agreement":null},{"id":"W1978764969","doi":"10.1029/2008gl036125","title":"Climate‐driven shifts in quantity and seasonality of river discharge over the past 1000 years from the hydrographic apex of North America","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Wilfrid Laurier University","funders":"BC Hydro; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Government of Ontario","keywords":"Glacier; Meltwater; Hydrography; Climate change; Snow; Surface runoff; Physical geography; Little ice age; Geology; Range (aeronautics); Discharge; Climatology; Precipitation; Streamflow; Environmental science; Oceanography; Geography; Drainage basin; Ecology; Geomorphology","score_opus":0.03742543922537828,"score_gpt":0.26725862891175506,"score_spread":0.22983318968637678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978764969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989454,0.00008064532,0.000066674635,0.00007857713,0.0000025925547,0.0000012208321,0.00040799138,0.0000055187697,0.0004112648],"genre_scores_gemma":[0.9992544,0.000106008425,0.000059059093,0.000027054672,0.0000048012525,0.0000021809842,0.00038240576,0.0000014923231,0.00016262337],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000010816388,0.000004873264,0.000024210918,0.000009120863,0.000009853074],"domain_scores_gemma":[0.9997689,0.000040006635,0.000115686,0.000019179912,0.000030353063,0.000025775744],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012259495,0.00008320093,0.00007277511,0.00034699996,0.00016016816,0.0003436556,0.0001118578,0.000121256184,0.0009129125],"category_scores_gemma":[0.00056630274,0.000087862536,0.000097830736,0.00056267105,0.00024321058,0.0002813999,0.00021493527,0.00016294199,0.00008643484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040353752,0.000021633145,0.98888373,0.000015390515,0.00004404155,0.000030690386,0.00021345528,0.00047441066,0.0033657504,0.000082495506,0.00031288195,0.0065152016],"study_design_scores_gemma":[4.448366e-7,0.000004242817,0.99948716,8.911214e-7,0.0000028577438,0.000011834237,0.00005010016,0.0001462526,0.000079735,0.000012606865,0.00020285496,0.0000010376391],"about_ca_topic_score_codex":0.020435104,"about_ca_topic_score_gemma":0.05052974,"teacher_disagreement_score":0.020435104,"about_ca_system_score_codex":0.00043776506,"about_ca_system_score_gemma":0.00014733129,"threshold_uncertainty_score":0.040632308},"labels":[],"label_agreement":null},{"id":"W1978846551","doi":"10.1029/2006gl026634","title":"Perturbation of ground surface temperature reconstructions by groundwater flow?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Advection; Groundwater; Perturbation (astronomy); Groundwater flow; Environmental science; Thermal conduction; Heat flow; Flow (mathematics); Geology; Meteorology; Hydrology (agriculture); Climatology; Mechanics; Thermal; Thermodynamics; Physics; Geotechnical engineering; Aquifer","score_opus":0.013686770719504512,"score_gpt":0.25138369481226464,"score_spread":0.2376969240927601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978846551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9815345,0.00030005947,0.0155216595,0.0004273014,0.00003237701,0.0000076216415,0.00052892015,0.00018797361,0.00145956],"genre_scores_gemma":[0.99773884,0.00007506001,0.0018627862,0.000023330182,0.0000056581453,0.000001850039,0.00019010503,0.000018657987,0.00008364218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978465,0.000089511275,0.000011432906,0.000055333843,0.000025196485,0.000033945824],"domain_scores_gemma":[0.99980515,0.000055753924,0.00005063852,0.00005556279,0.000022444769,0.000010537424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056531205,0.00017611463,0.00020479082,0.00029352028,0.000121805024,0.00064695417,0.00024170431,0.00039977484,0.0006784995],"category_scores_gemma":[0.0023703396,0.00018483514,0.0002133531,0.0004815198,0.00040003043,0.0006222127,0.00029918132,0.0002558444,0.00017494256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007440213,0.00012090699,0.557641,0.00016683064,0.00043118405,0.00050566456,0.00038898698,0.18320139,0.098830946,0.009656826,0.0019584692,0.14635374],"study_design_scores_gemma":[0.000056644094,0.00014916745,0.50023824,0.00007225218,0.000102904385,0.00043579977,0.00035402254,0.4458857,0.03513564,0.011116364,0.0063800653,0.00007322178],"about_ca_topic_score_codex":0.0055080885,"about_ca_topic_score_gemma":0.0045292727,"teacher_disagreement_score":0.0055080885,"about_ca_system_score_codex":0.0003814108,"about_ca_system_score_gemma":0.00022307706,"threshold_uncertainty_score":0.010952055},"labels":[],"label_agreement":null},{"id":"W1978959432","doi":"10.1029/2004gl020159","title":"Heat flow in the Nipigon arm of the Keweenawan rift, northwestern Ontario, Canada","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique","keywords":"Geology; Mafic; Sill; Rift; Archean; Crust; Geomorphology; Oceanography; Geochemistry","score_opus":0.019675966287851218,"score_gpt":0.22275007794178953,"score_spread":0.2030741116539383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1978959432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935098,0.00023995781,0.00005525518,0.00015466637,0.0000036272202,0.000013585709,0.0008796196,0.000009407772,0.005133921],"genre_scores_gemma":[0.99523973,0.00030824158,0.00019122078,0.000028960332,0.000002346439,0.000010907237,0.00050082314,0.0000053855833,0.003712259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989116,0.0000033030042,0.0000039751244,0.000022818764,0.00003996172,0.000038854057],"domain_scores_gemma":[0.9997733,0.000013050603,0.000027574664,0.0000054461198,0.00012491338,0.000055708195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000071677736,0.00014273722,0.00013471952,0.0005514015,0.0017681321,0.0008460166,0.00025361901,0.00017884166,0.0015884534],"category_scores_gemma":[0.00042890784,0.00016505868,0.000117669624,0.0010209676,0.00059901725,0.00021208992,0.00051218027,0.00024081525,0.00014098562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018432716,0.000032274664,0.9634849,0.000099037854,0.00004585134,0.00054792105,0.004943438,0.0014661546,0.006092455,0.0007586724,0.0022530896,0.0200919],"study_design_scores_gemma":[0.000008084318,0.0000064448454,0.9946572,0.000016550288,0.0000066933776,0.000032466527,0.0013693724,0.00046487246,0.00020653826,0.00005060511,0.0031737303,0.000007314021],"about_ca_topic_score_codex":0.99140257,"about_ca_topic_score_gemma":0.9984969,"teacher_disagreement_score":0.017643033,"about_ca_system_score_codex":0.017643033,"about_ca_system_score_gemma":0.013906622,"threshold_uncertainty_score":0.1280098},"labels":[],"label_agreement":null},{"id":"W1979155994","doi":"10.1029/2007gl030845","title":"On the resonance and influence of the tides in Ungava Bay and Hudson Strait","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Université du Québec à Rimouski","funders":"","keywords":"Bay; Forcing (mathematics); Oceanography; Structural basin; Geology; Climatology; Disturbance (geology); Geomorphology","score_opus":0.016256260681321806,"score_gpt":0.2554204528698358,"score_spread":0.23916419218851398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979155994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989642,0.000035266814,0.000013850901,0.000052876974,0.000004442472,0.0000011363701,0.000043659154,0.0000022457855,0.0008822546],"genre_scores_gemma":[0.99969065,0.000027474582,0.000016191727,0.000015402895,0.0000026573177,0.0000010000671,0.000043586195,0.0000014832532,0.00020147808],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999088,0.0000198444,0.0000041363,0.000015335147,0.000011651256,0.000040130126],"domain_scores_gemma":[0.99954957,0.00014005537,0.00007129152,0.000018572866,0.00007838582,0.00014214049],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018219698,0.00011290811,0.00017761842,0.0005320249,0.00049627287,0.00073933334,0.00019290962,0.00017085535,0.0016034602],"category_scores_gemma":[0.001231556,0.00016808091,0.00009288985,0.00055449124,0.0007520997,0.00023530671,0.00068000815,0.00024996977,0.0001740924],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005270174,0.000057748544,0.9690701,0.000030808093,0.0000580554,0.00075989903,0.0039144075,0.0022003963,0.008027634,0.0006751737,0.0011534623,0.013525308],"study_design_scores_gemma":[0.0000068784293,0.000020088712,0.9966307,0.0000082617225,0.000008917799,0.00003094197,0.0018560464,0.0007973508,0.00011727554,0.000045716093,0.00047308265,0.0000046780788],"about_ca_topic_score_codex":0.25909117,"about_ca_topic_score_gemma":0.35109657,"teacher_disagreement_score":0.74090886,"about_ca_system_score_codex":0.0012082953,"about_ca_system_score_gemma":0.0006689487,"threshold_uncertainty_score":0.51516616},"labels":[],"label_agreement":null},{"id":"W1979261544","doi":"10.1029/2001gl014277","title":"Tidal stress/strain and acoustic emission activity at the Underground Research Laboratory, Canada","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Akaike information criterion; Environmental science; Geology; Atmospheric sciences; Statistics; Seismology; Geodesy; Mathematics","score_opus":0.07161750273467339,"score_gpt":0.2947846569472121,"score_spread":0.22316715421253874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979261544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974367,0.00008596955,0.00016243487,0.00011827795,0.000002025224,0.000009330497,0.0010766296,0.000010313075,0.0010982711],"genre_scores_gemma":[0.9978842,0.00010654887,0.00018186125,0.000014421195,0.0000016923839,0.000004425683,0.0009004524,0.0000049258906,0.00090140343],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99951243,0.000041591393,0.000013583445,0.0000585535,0.00023062485,0.00014318443],"domain_scores_gemma":[0.99792176,0.00024245876,0.00049150817,0.00006382557,0.0009342756,0.0003460879],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041871046,0.00023954749,0.00021946801,0.0007257914,0.0012188095,0.000810884,0.00073183107,0.00023192466,0.0015259876],"category_scores_gemma":[0.0023482845,0.00018657696,0.00015376972,0.0014740791,0.0007108316,0.00026245843,0.00043289302,0.0003904529,0.0002784453],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012953415,0.00006189232,0.989785,0.000014588457,0.0000544693,0.0001207915,0.0005977611,0.0019766248,0.0010569472,0.00026234204,0.0010920505,0.004848064],"study_design_scores_gemma":[0.000006528968,0.00002743581,0.9951982,0.0000063869516,0.000011614949,0.000029441599,0.00077448314,0.0029793764,0.00029272263,0.000048804595,0.00061253546,0.000012530951],"about_ca_topic_score_codex":0.98668915,"about_ca_topic_score_gemma":0.9931248,"teacher_disagreement_score":0.014768525,"about_ca_system_score_codex":0.014768525,"about_ca_system_score_gemma":0.011100144,"threshold_uncertainty_score":0.107153654},"labels":[],"label_agreement":null},{"id":"W1979569300","doi":"10.1029/2003gl017526","title":"Wind‐driven shelf/basin exchange on an Arctic shelf: The joint roles of ice cover extent and shelf‐break bathymetry","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"North Pacific Marine Science Organization","funders":"","keywords":"Ice shelf; Sea ice; Upwelling; Oceanography; Iceberg; Geology; Arctic ice pack; Hydrography; Bathymetry; Antarctic sea ice; Arctic sea ice decline; Climatology; Cryosphere; Arctic; Arctic geoengineering; Drift ice; Environmental science","score_opus":0.025750632559036677,"score_gpt":0.26112856254926964,"score_spread":0.23537792999023296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979569300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99931824,0.000044027292,0.000079046375,0.000020621681,0.0000014410051,6.599705e-7,0.000048585964,0.000002135213,0.0004853757],"genre_scores_gemma":[0.99965215,0.000080249716,0.000052226853,0.000003072779,0.0000026731873,6.786009e-7,0.000056423967,0.0000012160733,0.00015129545],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999977,0.0000071035574,0.000001275647,0.0000031820712,0.000003458806,0.0000079362],"domain_scores_gemma":[0.9999192,0.000020110452,0.000016239987,0.0000042806114,0.000016456872,0.000023756726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016978027,0.00011759806,0.00008829459,0.00015654603,0.00022237904,0.00045668296,0.00009573043,0.00010550772,0.00081366976],"category_scores_gemma":[0.00031280334,0.000120749304,0.00011061972,0.00016448663,0.00016094264,0.00025111568,0.00017541258,0.00007402843,0.000088548295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00083786016,0.000118210686,0.83132136,0.00008309898,0.00019202079,0.0006755471,0.0005357658,0.0717393,0.049982477,0.0069941403,0.0014562194,0.036064006],"study_design_scores_gemma":[0.000029886154,0.000054610082,0.9174472,0.000010478498,0.000050225462,0.000101094105,0.00025146257,0.0776778,0.0018111448,0.0016117467,0.0009403378,0.0000139540125],"about_ca_topic_score_codex":0.023161253,"about_ca_topic_score_gemma":0.04551824,"teacher_disagreement_score":0.023161253,"about_ca_system_score_codex":0.00035560314,"about_ca_system_score_gemma":0.00029006955,"threshold_uncertainty_score":0.046052873},"labels":[],"label_agreement":null},{"id":"W1979585634","doi":"10.1029/2003gl017592","title":"Gyrophase‐restricted 100 keV–2 MeV ion beams near the foreshock boundary","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"National Aeronautics and Space Administration","keywords":"Foreshock; Physics; Gyroradius; Ion; Solar wind; Atomic physics; Range (aeronautics); Earth radius; Nuclear physics; Plasma; Magnetosphere; Aftershock; Materials science; Geology","score_opus":0.02060168755884901,"score_gpt":0.29729889395941395,"score_spread":0.27669720640056494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979585634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938,0.0004405502,0.001244142,0.00004524711,0.000008524413,0.000012607519,0.00024427977,0.00004435249,0.0041603292],"genre_scores_gemma":[0.9974049,0.00017982174,0.0012097631,0.000035551213,0.000008875352,0.000013937227,0.0003947162,0.000010781261,0.00074168306],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.0000053617073,0.0000013449278,0.0000131748075,0.00001645041,0.000026103988],"domain_scores_gemma":[0.9997943,0.000057308753,0.000058128295,0.00001950907,0.00003987882,0.000030759118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012640489,0.00024175383,0.00019457086,0.00026546736,0.00037227376,0.00025816192,0.00025533972,0.00022773149,0.001709849],"category_scores_gemma":[0.00028999796,0.0001320022,0.00013559911,0.00030259235,0.00024204052,0.00024966418,0.00035518725,0.00029184436,0.00023645573],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001994733,0.00009761385,0.14126837,0.00026647805,0.00013146494,0.0026160828,0.0015997345,0.003104861,0.82522094,0.0011498558,0.0011990791,0.021350786],"study_design_scores_gemma":[0.00010832628,0.0009161277,0.7703244,0.00008879477,0.00013130327,0.002185147,0.0009349894,0.003499743,0.20317492,0.0009484304,0.017620824,0.00006691366],"about_ca_topic_score_codex":0.0022173559,"about_ca_topic_score_gemma":0.006216097,"teacher_disagreement_score":0.0022173559,"about_ca_system_score_codex":0.00021049155,"about_ca_system_score_gemma":0.00015900967,"threshold_uncertainty_score":0.0057200193},"labels":[],"label_agreement":null},{"id":"W1979676158","doi":"10.1029/2006gl028223","title":"Cloud fraction parameterization as a function of mean cloud water content and its variance using in‐situ observations","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Cure Cancer Australia Foundation; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Cloud fraction; Liquid water content; Standard deviation; Environmental science; Cloud cover; Scale (ratio); Cloud computing; Latitude; Atmospheric sciences; Meteorology; Statistics; Mathematics; Physics; Geology; Geodesy; Computer science","score_opus":0.1312769283127994,"score_gpt":0.3066191085612141,"score_spread":0.1753421802484147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979676158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824572,0.00005755448,0.016677607,0.000020996662,0.0000050322737,0.000009092166,0.0002517242,0.00012610643,0.0003946349],"genre_scores_gemma":[0.9971934,0.000023301356,0.0025117358,0.0000034343846,0.0000026172559,0.000004395733,0.0001987387,0.000013948897,0.000048521513],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999287,0.000017107102,0.000005432896,0.000024718593,0.000011359221,0.00001269161],"domain_scores_gemma":[0.9996481,0.00017109406,0.000067049594,0.00005710354,0.00004109109,0.000015446767],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025411788,0.0005089799,0.00025040202,0.0005608727,0.00016797276,0.0004937292,0.00029292286,0.00027255606,0.0002758784],"category_scores_gemma":[0.0010722098,0.0002134253,0.0004081906,0.00046071527,0.00011221623,0.00045841973,0.00012571923,0.00021052887,0.000058685488],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028337692,0.00015945746,0.24701723,0.00009592009,0.00024272146,0.00016545552,0.00012733466,0.62343353,0.08517921,0.0004292699,0.00033923896,0.042527243],"study_design_scores_gemma":[0.000016927124,0.00005041423,0.15291928,0.000008202051,0.000058337926,0.00007809232,0.000054117423,0.825076,0.02103103,0.00027216843,0.00040973056,0.000025648145],"about_ca_topic_score_codex":0.012098915,"about_ca_topic_score_gemma":0.009470506,"teacher_disagreement_score":0.012098915,"about_ca_system_score_codex":0.00052263885,"about_ca_system_score_gemma":0.0001974117,"threshold_uncertainty_score":0.024056971},"labels":[],"label_agreement":null},{"id":"W1979829362","doi":"10.1029/2001gl014502","title":"Hindcasting the NAO using diabatic forcing of a simple AGCM","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Dalhousie University","funders":"","keywords":"Hindcast; Climatology; Diabatic; Forcing (mathematics); Environmental science; Tropical cyclone; Atmospheric sciences; Latitude; Meteorology; Geology; Geography; Physics","score_opus":0.12361066845002476,"score_gpt":0.3329990441350825,"score_spread":0.20938837568505775,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1979829362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9584263,0.00007161022,0.03118011,0.0002527697,0.00029354446,0.00008314095,0.004923281,0.0010953783,0.0036739772],"genre_scores_gemma":[0.98012024,0.00005878402,0.016472563,0.000044670607,0.000036230358,0.000054359847,0.0023728071,0.000064504624,0.00077576813],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998963,0.000025433732,0.000007827445,0.00003332137,0.000020149386,0.000016977907],"domain_scores_gemma":[0.9996094,0.000088591885,0.000041031388,0.00010343869,0.000097887,0.00005976025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000451036,0.00043075805,0.00044028193,0.0003110372,0.00045886324,0.00052258384,0.000663896,0.0005157865,0.0016059031],"category_scores_gemma":[0.0013541476,0.00032105678,0.0004409567,0.0006168058,0.00027238304,0.00038753485,0.00040943906,0.00081445475,0.00023168398],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029417814,0.00016071495,0.020775855,0.00006251467,0.00013875176,0.00008932398,0.000057156114,0.95240456,0.010055563,0.0019216773,0.0018444116,0.012195345],"study_design_scores_gemma":[0.00012396906,0.000048259673,0.006764006,0.0000027042772,0.00002246793,0.0000120913755,0.000008784432,0.98966926,0.001988468,0.00048171135,0.0008620476,0.000016153099],"about_ca_topic_score_codex":0.030260254,"about_ca_topic_score_gemma":0.02619351,"teacher_disagreement_score":0.030260254,"about_ca_system_score_codex":0.00056059484,"about_ca_system_score_gemma":0.0009898008,"threshold_uncertainty_score":0.060168266},"labels":[],"label_agreement":null},{"id":"W1980407359","doi":"10.1029/1999gl011218","title":"Seasonal variations of HCN over northern Japan measured by ground‐based infrared solar spectroscopy","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Mixing ratio; Troposphere; Infrared; Fourier transform infrared spectroscopy; Infrared spectroscopy; Seasonality; Spectral line; Analytical Chemistry (journal); Spectroscopy; Atmospheric sciences; Chemistry; Environmental science; Physics; Optics; Environmental chemistry","score_opus":0.019104382163472877,"score_gpt":0.2633164363961349,"score_spread":0.244212054232662,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980407359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994862,0.0000755268,0.00004542843,0.0000059358003,0.0000011679638,0.0000012321927,0.00012900126,0.000004135282,0.00025123288],"genre_scores_gemma":[0.99889094,0.00011856398,0.00017962191,0.00000650389,0.0000036778285,0.000004339923,0.00045011338,0.0000024884555,0.00034380401],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993837,0.0000043008013,0.0000042152037,0.000021727092,0.000017988837,0.000013461035],"domain_scores_gemma":[0.99980026,0.00001578881,0.000053146297,0.000010394248,0.00008823869,0.000032186264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014800843,0.00021104378,0.00019170693,0.00044910132,0.0002819018,0.00025081585,0.0001557563,0.000165437,0.00038375007],"category_scores_gemma":[0.00018810711,0.00013584034,0.000094275616,0.00075018493,0.00015928966,0.000214535,0.00016537218,0.00011355682,0.00008459175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023750956,0.00004139683,0.94485694,0.00006710985,0.00010286915,0.00040997466,0.00087739027,0.00096974836,0.039072108,0.000036540132,0.0003373675,0.012991075],"study_design_scores_gemma":[0.0000021681105,0.000013062117,0.9983821,0.0000016591264,0.000012998828,0.00003563308,0.0001419271,0.00035060107,0.00074996636,0.000005392082,0.00030194846,0.000002513472],"about_ca_topic_score_codex":0.04602986,"about_ca_topic_score_gemma":0.10440777,"teacher_disagreement_score":0.04602986,"about_ca_system_score_codex":0.0006386352,"about_ca_system_score_gemma":0.00019497648,"threshold_uncertainty_score":0.091523886},"labels":[],"label_agreement":null},{"id":"W1980470069","doi":"10.1029/2004gl021538","title":"Ecosystem dynamics and export production in the central and eastern equatorial Pacific: A modeling study of impact of ENSO","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Biogeochemical cycle; Phytoplankton; Oceanography; Environmental science; New production; Ecosystem; Zooplankton; Climatology; Nutrient; Geology; Ecology; Biology","score_opus":0.033388076835004735,"score_gpt":0.2834927500311637,"score_spread":0.250104673196159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980470069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730337,0.00007430103,0.0005201741,0.00013949936,0.0000071315208,0.000007902386,0.00025394926,0.000026613765,0.0016670336],"genre_scores_gemma":[0.9982299,0.000109619235,0.00058085937,0.000029407938,0.000009432873,0.000019570678,0.0002266458,0.000014112102,0.000780489],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992263,0.00002588621,0.0000043563623,0.000018580153,0.000006999045,0.00002140411],"domain_scores_gemma":[0.9996408,0.00017741296,0.00005807156,0.000020807007,0.000037049722,0.00006581951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041826305,0.00067812135,0.0004909442,0.00032865413,0.0006341273,0.0011082153,0.0007809905,0.0013127996,0.0018070749],"category_scores_gemma":[0.0009310955,0.00047889948,0.00081326463,0.0005119609,0.0005138612,0.0010085554,0.0005284862,0.0006136926,0.00012794705],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022676421,0.00020097784,0.026934985,0.000032338914,0.00011586092,0.00020054533,0.000082074366,0.96816707,0.0009252513,0.0011472174,0.0004938581,0.0014730506],"study_design_scores_gemma":[0.000090947586,0.00006176593,0.008405376,0.0000048866623,0.0000363053,0.000024347832,0.000076219774,0.9905371,0.00015337697,0.00034509625,0.00025625032,0.000008394243],"about_ca_topic_score_codex":0.08100106,"about_ca_topic_score_gemma":0.044164844,"teacher_disagreement_score":0.08100106,"about_ca_system_score_codex":0.0013985443,"about_ca_system_score_gemma":0.0010066441,"threshold_uncertainty_score":0.16105914},"labels":[],"label_agreement":null},{"id":"W1980546382","doi":"10.1029/2009gl037248","title":"Early Eocene Arctic climate sensitivity to pCO<sub>2</sub> and basin geography","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Arctic; Climatology; Arctic dipole anomaly; Environmental science; Arctic geoengineering; Climate model; The arctic; Canada Basin; Structural basin; Climate change; Arctic sea ice decline; Oceanography; Greenhouse gas; Global warming; Geology; Sea ice; Atmospheric sciences; Arctic ice pack; Drift ice; Geomorphology","score_opus":0.018815541142105655,"score_gpt":0.2657377273651927,"score_spread":0.24692218622308704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980546382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974853,0.00007401131,0.00054763455,0.00006930765,0.0000064906694,0.0000037731925,0.00049835077,0.000015835742,0.001299375],"genre_scores_gemma":[0.99910825,0.000050996172,0.00031801529,0.000018872885,0.0000035277403,0.0000045711076,0.00033901256,0.000006818066,0.00015000864],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998933,0.00003736684,0.000005874445,0.000029217561,0.0000147917235,0.00001944339],"domain_scores_gemma":[0.99961686,0.00014704486,0.000044740893,0.000080094425,0.00006977677,0.00004141658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045042226,0.00023498901,0.0001970356,0.00018807284,0.0002718745,0.00037146776,0.00019378863,0.00018225223,0.0012086999],"category_scores_gemma":[0.0011396507,0.00015066564,0.00030870573,0.00025285676,0.0002966294,0.00032661387,0.00025377527,0.0003494086,0.00009830636],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016405958,0.0003283467,0.54900074,0.000124028,0.00044117606,0.0002044259,0.00035212774,0.3250264,0.098658316,0.0038658602,0.0021590753,0.018199034],"study_design_scores_gemma":[0.00014467753,0.00024229087,0.7378323,0.000017936813,0.00015847647,0.00009877241,0.00015977609,0.22503676,0.029614534,0.0023499487,0.0042954376,0.000049071157],"about_ca_topic_score_codex":0.03638392,"about_ca_topic_score_gemma":0.03052099,"teacher_disagreement_score":0.03638392,"about_ca_system_score_codex":0.0007435396,"about_ca_system_score_gemma":0.0002193268,"threshold_uncertainty_score":0.0723443},"labels":[],"label_agreement":null},{"id":"W1980610108","doi":"10.1029/2006gl029139","title":"Anomalous 20th century tree growth, Mackenzie Delta, Northwest Territories, Canada","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Aboriginal Affairs Northern Dev Canada; Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Dendrochronology; Delta; Divergence (linguistics); Geography; Physical geography; Precipitation; Dendroclimatology; Climatology; Offset (computer science); Geology; Archaeology; Meteorology","score_opus":0.018583846247617043,"score_gpt":0.25774355623734724,"score_spread":0.23915970998973018,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980610108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98760533,0.00083126826,0.00012138091,0.0003490762,0.0000093599265,0.000010157799,0.006087889,0.00001941067,0.0049660997],"genre_scores_gemma":[0.9929792,0.0010237715,0.00034225642,0.000047825884,0.000003425315,0.000007444999,0.0019723994,0.00000922623,0.0036143383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990416,0.000004907877,0.000005051081,0.000023459164,0.000030821408,0.000031636922],"domain_scores_gemma":[0.9995384,0.00002333242,0.00007722911,0.000018386485,0.000262157,0.00008047938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017644491,0.00010834609,0.00009611066,0.00097352976,0.0013707634,0.000574151,0.00032034592,0.00011187156,0.0014982817],"category_scores_gemma":[0.000657222,0.00007335515,0.00006306426,0.0018124277,0.00030795264,0.0002491026,0.00036459893,0.00021404076,0.00012312402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061184815,0.000016031581,0.9613146,0.00003920233,0.00003772054,0.000216681,0.0026803194,0.00046557514,0.0013143389,0.0008588636,0.0041768244,0.028818656],"study_design_scores_gemma":[0.0000012784403,0.0000021025178,0.9940785,0.00001148567,0.000004871458,0.00004502989,0.0012228958,0.00017617678,0.00010968586,0.000042630476,0.0043012016,0.000004180068],"about_ca_topic_score_codex":0.9897031,"about_ca_topic_score_gemma":0.9984522,"teacher_disagreement_score":0.010296881,"about_ca_system_score_codex":0.01000286,"about_ca_system_score_gemma":0.0080192285,"threshold_uncertainty_score":0.072576225},"labels":[],"label_agreement":null},{"id":"W1980744485","doi":"10.1029/2001gl013674","title":"Magnetoclimatology and paleoprecipitation: evidence from a north‐south transect through the Chinese Loess Plateau","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Transect; Loess; Geology; Interglacial; Loess plateau; Physical geography; Isotopes of oxygen; Plateau (mathematics); Precipitation; Climatology; Geomorphology; Oceanography; Glacial period; Geography; Soil science; Geochemistry","score_opus":0.06028010812901025,"score_gpt":0.2979354770345853,"score_spread":0.23765536890557504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980744485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997645,0.00002624058,0.00001797875,0.00000831575,3.8110153e-7,6.862359e-7,0.000029741223,9.110661e-7,0.00015134017],"genre_scores_gemma":[0.99965155,0.000033780714,0.000048275393,0.000007050621,0.0000020031855,0.0000029998134,0.00014338926,8.0368295e-7,0.00011013041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990594,0.000018740322,0.000007850921,0.000030392273,0.000017304252,0.000019726336],"domain_scores_gemma":[0.99938345,0.00008759918,0.00020339256,0.000044507815,0.00017136322,0.000109708766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020780879,0.0001937138,0.00012814265,0.0007837154,0.0005850485,0.00029354406,0.00023605974,0.00022317408,0.00037439493],"category_scores_gemma":[0.0005431183,0.0001843418,0.00011423561,0.0006882938,0.0005594904,0.0002155526,0.00043638432,0.00015454718,0.00007940527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009403324,0.000013839486,0.9802729,0.000021896676,0.00003909633,0.00020191459,0.002315989,0.0000662948,0.01428397,0.00003738554,0.000053269163,0.0025994342],"study_design_scores_gemma":[0.0000020835316,0.000013021924,0.99939704,0.0000015190373,0.000006746157,0.000052160027,0.0002274826,0.00004010534,0.0001752416,0.0000052912574,0.00007766131,0.0000016193865],"about_ca_topic_score_codex":0.04273659,"about_ca_topic_score_gemma":0.11218359,"teacher_disagreement_score":0.04273659,"about_ca_system_score_codex":0.00038298444,"about_ca_system_score_gemma":0.00039559347,"threshold_uncertainty_score":0.08497566},"labels":[],"label_agreement":null},{"id":"W1980874154","doi":"10.1029/2008gl033268","title":"Remote sensing of hydrologic recharge in the Peace‐Athabasca Delta, Canada","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Flood Risk Assessment and Management","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Groundwater recharge; Wetland; Hydrology (agriculture); Floodplain; Delta; Environmental science; Water level; Hydrological modelling; Geology; Groundwater; Climatology; Aquifer; Ecology; Geography","score_opus":0.036281535238757524,"score_gpt":0.2862392450680941,"score_spread":0.2499577098293366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980874154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928053,0.00012062743,0.00022551823,0.00023042501,0.000004734715,0.000017557171,0.0039853663,0.000058038964,0.002552485],"genre_scores_gemma":[0.9971336,0.000097191,0.00049306895,0.000022642656,0.0000021201292,0.0000067376477,0.0015503566,0.0000043346186,0.00068994885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998665,0.000011287331,0.000005896531,0.00002059401,0.000058117417,0.00003757603],"domain_scores_gemma":[0.99962413,0.000039573973,0.0000469759,0.000014406937,0.00019377717,0.000081204234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001658565,0.00015244311,0.00013133214,0.00080878305,0.0009247864,0.0006055075,0.00034157548,0.00012569598,0.0010163961],"category_scores_gemma":[0.00076475425,0.00008589337,0.00009587157,0.0015900537,0.00026876995,0.00017749296,0.00028134574,0.00017632332,0.00008282658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001663879,0.00014744721,0.92519665,0.00006578745,0.00008961959,0.00031836284,0.0009930865,0.00808121,0.0068276953,0.0010204018,0.007637554,0.049455915],"study_design_scores_gemma":[0.000023152717,0.000008510134,0.9847816,0.000019617568,0.000016335818,0.000035498917,0.0011391235,0.009652761,0.00071364414,0.00012475508,0.0034686,0.000016573238],"about_ca_topic_score_codex":0.9855311,"about_ca_topic_score_gemma":0.9929395,"teacher_disagreement_score":0.014468908,"about_ca_system_score_codex":0.0068930974,"about_ca_system_score_gemma":0.0072103203,"threshold_uncertainty_score":0.050013185},"labels":[],"label_agreement":null},{"id":"W1980913577","doi":"10.1029/2005gl025297","title":"An empirical model for the altitude of the OH nightglow emission","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Airglow; Altitude (triangle); Latitude; Atmospheric sciences; Environmental science; Physics; Mathematics; Astronomy; Geometry","score_opus":0.046580229268508126,"score_gpt":0.3318983163790729,"score_spread":0.2853180871105648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980913577","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.39060092,0.00060087146,0.5957201,0.0005074158,0.00010754144,0.00016483202,0.0018570184,0.0021889436,0.008252278],"genre_scores_gemma":[0.950215,0.000574125,0.03704441,0.000086960266,0.00006407738,0.00025814964,0.0020321354,0.00024028274,0.009484977],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997627,0.000034406552,0.000011486008,0.00010429231,0.00005251443,0.000034635126],"domain_scores_gemma":[0.99935335,0.00023638755,0.00015200782,0.00007517774,0.00015732365,0.000025730407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006602939,0.00059498893,0.00035538,0.0007097077,0.00025391008,0.00076187565,0.001304913,0.0007723354,0.0025269792],"category_scores_gemma":[0.0022901294,0.00035103425,0.0005519539,0.0008328116,0.0002773733,0.0012232582,0.00031709645,0.0009320888,0.002296737],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000114919436,0.00028333146,0.06919883,0.00020089284,0.00021812847,0.0003022284,0.00037186273,0.80703247,0.0147148715,0.016629763,0.004319037,0.08661369],"study_design_scores_gemma":[0.00001094771,0.00004672246,0.013910557,0.000012650393,0.000021553897,0.00017695641,0.000032734173,0.9791764,0.00076282176,0.0034627074,0.0023694474,0.00001654397],"about_ca_topic_score_codex":0.0051423525,"about_ca_topic_score_gemma":0.00376204,"teacher_disagreement_score":0.0051423525,"about_ca_system_score_codex":0.0005791881,"about_ca_system_score_gemma":0.0005646147,"threshold_uncertainty_score":0.010224879},"labels":[],"label_agreement":null},{"id":"W1980943103","doi":"10.1029/2009gl038778","title":"Routing of western Canadian Plains runoff during the 8.2 ka cold event","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Bay; Geology; Surface runoff; Foraminifera; Oceanography; Ice sheet; Climatology; Routing (electronic design automation)","score_opus":0.0249615464729325,"score_gpt":0.284027477278151,"score_spread":0.25906593080521845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1980943103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988066,0.000021515956,0.000069315596,0.00005340253,0.0000024901399,0.0000037827656,0.00030106507,0.000019428631,0.0007223233],"genre_scores_gemma":[0.999292,0.00003103906,0.00010302775,0.000011797977,9.522976e-7,0.0000024084939,0.000299322,0.0000032506655,0.00025611575],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999502,0.000002752839,0.0000020324624,0.000014165842,0.000010940085,0.000019929808],"domain_scores_gemma":[0.9998964,0.000007801341,0.000020154885,0.000006093708,0.00004104004,0.000028529506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000089874105,0.00018338337,0.00013149166,0.00041751354,0.00076257985,0.0006010223,0.0003147796,0.0002329823,0.00071614364],"category_scores_gemma":[0.00041864184,0.0001730943,0.00019017707,0.0003511678,0.00034097178,0.00016261527,0.00029142425,0.00022369559,0.00005656931],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028185765,0.000061422536,0.907036,0.000043632925,0.00014984357,0.0004877537,0.00060681184,0.04793869,0.027256748,0.0010419812,0.0018174415,0.013277907],"study_design_scores_gemma":[0.000020765607,0.000021372372,0.96432906,0.000007731876,0.00004050136,0.000044916847,0.000354634,0.031804763,0.0015977185,0.00014856138,0.001603691,0.000026378399],"about_ca_topic_score_codex":0.90477765,"about_ca_topic_score_gemma":0.93115556,"teacher_disagreement_score":0.095222354,"about_ca_system_score_codex":0.006249291,"about_ca_system_score_gemma":0.0038038546,"threshold_uncertainty_score":0.19156623},"labels":[],"label_agreement":null},{"id":"W1981131979","doi":"10.1029/2005gl024079","title":"A 10‐year integrated atmospheric water vapor record using precision filter radiometers at two high‐alpine sites","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"GNSS positioning and interference","field":"Engineering","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Radiometer; Microwave radiometer; Atmospheric sciences; Global Positioning System; Troposphere; Latitude; Meteorology; Climatology; Remote sensing; Geodesy; Geology; Geography","score_opus":0.0354021434253358,"score_gpt":0.2917038746252792,"score_spread":0.2563017311999434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981131979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980319,0.00003785046,0.00026862443,0.000010508799,0.0000017385192,0.000004127706,0.0010208715,0.000024049306,0.00060038693],"genre_scores_gemma":[0.9950264,0.00005748761,0.00061377924,0.0000080965865,0.0000071527807,0.00000801616,0.00380236,0.000004467362,0.00047237807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.0000056292583,0.0000034728946,0.000020052425,0.00003160305,0.000018215644],"domain_scores_gemma":[0.9997949,0.000027348095,0.000044085482,0.000017930322,0.00007905354,0.000036763802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017717591,0.00020824693,0.00018022725,0.00056253857,0.00045564648,0.00036958244,0.00015129535,0.00022382893,0.0006211468],"category_scores_gemma":[0.00019961318,0.0001240801,0.000142599,0.00054592645,0.00016294587,0.00023044563,0.00017502531,0.00018193171,0.0001448291],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045291265,0.00012765951,0.93093675,0.000053175867,0.00014490889,0.00036998664,0.0006501089,0.0017357066,0.0415087,0.00011219347,0.0008146148,0.02309328],"study_design_scores_gemma":[0.000012387959,0.00007272314,0.99648404,0.000002268758,0.000018625124,0.000057326324,0.000060233346,0.00076895126,0.0015096354,0.000009996186,0.0009989077,0.000004940078],"about_ca_topic_score_codex":0.036618166,"about_ca_topic_score_gemma":0.07413394,"teacher_disagreement_score":0.036618166,"about_ca_system_score_codex":0.0003601091,"about_ca_system_score_gemma":0.000269792,"threshold_uncertainty_score":0.072810054},"labels":[],"label_agreement":null},{"id":"W1981261468","doi":"10.1029/2009gl039090","title":"Response of the eastern North Atlantic subpolar gyre to the North Atlantic Oscillation","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Oceanography; Geology; Salinity; North Atlantic oscillation; Anomaly (physics); Anticyclone; Climatology; Subtropics; North Atlantic Deep Water; Thermohaline circulation; Physics; Fishery; Biology","score_opus":0.03426786624664742,"score_gpt":0.28702320720864927,"score_spread":0.25275534096200186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981261468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909747,0.000020668369,0.00011627992,0.0000664262,0.0000109923385,0.0000041001986,0.0000710584,0.000011769587,0.0006012289],"genre_scores_gemma":[0.999653,0.000023005172,0.000052996358,0.00002298982,0.0000030287479,0.000002910311,0.00006624956,0.000002395041,0.00017354578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989116,0.000040655224,0.000008565339,0.000023503893,0.0000143979005,0.00002168812],"domain_scores_gemma":[0.9995757,0.0001356008,0.00007730547,0.00006889948,0.000054379572,0.00008814284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027466856,0.00019354653,0.00024493007,0.00009374652,0.00018888676,0.0005357665,0.00013009917,0.00032039903,0.0011999615],"category_scores_gemma":[0.0016298441,0.00013831751,0.00016400896,0.00008089023,0.000279449,0.00023416955,0.00034197216,0.00025392752,0.00021083179],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00293829,0.0004648063,0.44984618,0.00012701938,0.0004837367,0.0005802814,0.0006391758,0.26946405,0.25039303,0.0023705382,0.0023278557,0.020365026],"study_design_scores_gemma":[0.0002664048,0.0007262769,0.70993507,0.000014802517,0.000098502125,0.000120853976,0.0004562789,0.27405372,0.010975458,0.0013458227,0.0019546312,0.00005217119],"about_ca_topic_score_codex":0.007364745,"about_ca_topic_score_gemma":0.0060847187,"teacher_disagreement_score":0.007364745,"about_ca_system_score_codex":0.00034403865,"about_ca_system_score_gemma":0.0001863183,"threshold_uncertainty_score":0.014643788},"labels":[],"label_agreement":null},{"id":"W1981273289","doi":"10.1029/2001gl014392","title":"Towards evaluating the viscosity of the Earth's outer core: An experimental high pressure study of liquid Fe‐S (8.5 wt.% S)","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Viscosity; Outer core; Inner core; Thermodynamics; Materials science; Isothermal process; Synchrotron; Volume (thermodynamics); Core (optical fiber); Temperature dependence of liquid viscosity; Analytical Chemistry (journal); Chemistry; Relative viscosity; Composite material; Physics; Optics; Chromatography","score_opus":0.0956084923520528,"score_gpt":0.3482173937585056,"score_spread":0.25260890140645276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981273289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980578,0.00013716554,0.0012792235,0.000014281122,0.0000017507385,0.0000036344745,0.00005060877,0.000019554767,0.00043598955],"genre_scores_gemma":[0.9977775,0.0001704667,0.0016512441,0.000012211849,0.000004679796,0.000005605177,0.00010162261,0.00001532577,0.00026136092],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999527,0.0000066496027,0.0000029228927,0.000010768264,0.000016349857,0.000010610775],"domain_scores_gemma":[0.99987113,0.000039944236,0.00003426613,0.00001050652,0.000030036346,0.000014117332],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016423744,0.0003028602,0.0002367086,0.0003213878,0.00020644866,0.00042595484,0.00025770869,0.00032447826,0.000665643],"category_scores_gemma":[0.0003512125,0.00019373634,0.0001245082,0.00017909882,0.00053208193,0.0004574574,0.0002873646,0.00039778813,0.00010364764],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056484605,0.000005860536,0.0012790149,0.000032710333,0.0000048299626,0.00004284335,0.000048422007,0.00016028737,0.99755055,0.00008576374,0.00001076852,0.00072241534],"study_design_scores_gemma":[0.000013317972,0.00014303485,0.021692133,0.000009076578,0.000013219083,0.00012564218,0.0000638319,0.002488699,0.9746097,0.00009559994,0.00073980837,0.0000058761166],"about_ca_topic_score_codex":0.0010667488,"about_ca_topic_score_gemma":0.00075650966,"teacher_disagreement_score":0.0010667488,"about_ca_system_score_codex":0.00015500512,"about_ca_system_score_gemma":0.00008949114,"threshold_uncertainty_score":0.00222677},"labels":[],"label_agreement":null},{"id":"W1981451556","doi":"10.1029/2002gl015488","title":"Lightning activity during the 1999 Superior derecho","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Lightning and Electromagnetic Phenomena","field":"Physics and Astronomy","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lightning (connector); Lightning detection; Derecho; Storm; Geography; Severe weather; Meteorology; Environmental science; Physical geography; Climatology; Geology; Thunderstorm","score_opus":0.025533294094784213,"score_gpt":0.27512785978478577,"score_spread":0.24959456569000155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981451556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988306,0.00015772325,0.00009413479,0.00020150057,0.00003270953,0.000011585907,0.000690467,0.000030701543,0.010475014],"genre_scores_gemma":[0.9972554,0.00014674298,0.00010456847,0.00006752317,0.00003632306,0.000004202298,0.0008687918,0.000004796851,0.0015116198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981004,0.0000138640435,0.000010852186,0.000030834002,0.00009507654,0.000039303693],"domain_scores_gemma":[0.99956185,0.000052293602,0.00007597124,0.000028007571,0.00019793473,0.00008390793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002895352,0.00011520132,0.00013390841,0.0002989498,0.0006909888,0.0005446058,0.00012338058,0.00026024945,0.001231444],"category_scores_gemma":[0.00089954195,0.00005069463,0.000046549805,0.0003112882,0.00027392898,0.00021931005,0.00045924354,0.00020467056,0.00022978302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069331523,0.00013012157,0.87999594,0.00012023963,0.000058760736,0.0030694269,0.0064095925,0.0022916,0.021567184,0.0015522653,0.019468544,0.06464294],"study_design_scores_gemma":[0.00002095557,0.00012748806,0.9702631,0.000032218755,0.00001214943,0.0003718958,0.002165699,0.0012030513,0.0015850434,0.00018703805,0.024019336,0.000011935228],"about_ca_topic_score_codex":0.07686806,"about_ca_topic_score_gemma":0.22018518,"teacher_disagreement_score":0.07686806,"about_ca_system_score_codex":0.0015011958,"about_ca_system_score_gemma":0.0006489525,"threshold_uncertainty_score":0.15284127},"labels":[],"label_agreement":null},{"id":"W1981613926","doi":"10.1029/2000gl003811","title":"Fast tailward stream observed in the distant tail associated with substorm: A multi‐instrument study","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency","keywords":"Substorm; Plasma sheet; Physics; Plasma; Geophysics; Electric field; Event (particle physics); Astrophysics; Magnetosphere; Nuclear physics","score_opus":0.03268247058071914,"score_gpt":0.27869031248898696,"score_spread":0.24600784190826783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981613926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994143,0.000034421893,0.00023219528,0.000007371238,0.000001760908,0.0000044951403,0.0000527203,0.000009125627,0.00024359909],"genre_scores_gemma":[0.99935347,0.000026823147,0.0002537387,0.000012540801,0.000014160589,0.0000033160518,0.00018904585,0.0000037479804,0.00014309792],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999442,0.0000050704834,0.0000025159407,0.000014227604,0.000010224593,0.000023724853],"domain_scores_gemma":[0.99980396,0.00002585225,0.00005758207,0.00002143008,0.00003567049,0.000055585137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014290391,0.00017076706,0.00020412431,0.0005520694,0.0003709046,0.0002923777,0.00017414054,0.00030048884,0.0004971133],"category_scores_gemma":[0.00028144635,0.00011195544,0.00017385883,0.0002526187,0.000191089,0.00019892122,0.0003770117,0.00024552768,0.00011543334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057404273,0.00013431915,0.9002503,0.000028402668,0.00006252202,0.0048531424,0.0006518592,0.00031142237,0.08144786,0.00012301793,0.00031068092,0.011252349],"study_design_scores_gemma":[0.000012569414,0.0002814921,0.9927371,0.000004755367,0.000019586516,0.0023474398,0.00015451925,0.0009724881,0.0028925566,0.000052286872,0.000517493,0.0000076012584],"about_ca_topic_score_codex":0.002469304,"about_ca_topic_score_gemma":0.003250087,"teacher_disagreement_score":0.002469304,"about_ca_system_score_codex":0.00015933675,"about_ca_system_score_gemma":0.000096073265,"threshold_uncertainty_score":0.004909873},"labels":[],"label_agreement":null},{"id":"W1981831844","doi":"10.1002/2014gl061887","title":"Laboratory experiments of forced plumes in a density‐stratified crossflow and implications for volcanic plumes","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Plume; Dimensionless quantity; Volcano; Panache; Geology; Atmospheric sciences; Wind speed; Geophysics; Meteorology; Environmental science; Mechanics; Physics; Seismology; Oceanography","score_opus":0.052008815836471094,"score_gpt":0.32571714115769157,"score_spread":0.27370832532122047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981831844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99848,0.000025868221,0.0012364953,0.000019898838,0.000008349548,0.000018365827,0.00006688208,0.000024169987,0.0001200303],"genre_scores_gemma":[0.99855155,0.000023707631,0.0012163958,0.000008344016,0.000003123565,0.000023496212,0.000065348344,0.0000035795492,0.0001043933],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999869,0.000028415388,0.000012530422,0.000025971785,0.00003131983,0.000032716955],"domain_scores_gemma":[0.9992505,0.00030439525,0.00015192578,0.00009009412,0.00008921909,0.00011385945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036170398,0.00027904246,0.00021967506,0.00023756213,0.00031931043,0.0003461523,0.00041596976,0.00026671527,0.00061631424],"category_scores_gemma":[0.0009281072,0.0001304067,0.0003560866,0.00012722112,0.00044024142,0.00030179488,0.00051445374,0.00056406367,0.000044445896],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010609189,0.0017008894,0.01575753,0.0001125065,0.000080485166,0.00031144233,0.0002657651,0.057686817,0.9166957,0.0013144909,0.00024727095,0.0047661015],"study_design_scores_gemma":[0.00042250357,0.007954458,0.022407373,0.000023825269,0.00006452693,0.00013839616,0.00019097488,0.48008958,0.48704895,0.0011036915,0.00048283362,0.00007286994],"about_ca_topic_score_codex":0.0023545967,"about_ca_topic_score_gemma":0.0014923448,"teacher_disagreement_score":0.0023545967,"about_ca_system_score_codex":0.00036899257,"about_ca_system_score_gemma":0.0002299452,"threshold_uncertainty_score":0.0046818256},"labels":[],"label_agreement":null},{"id":"W1981927376","doi":"10.1029/2007gl032739","title":"Effects of atmospheric vorticity on the seasonal hydrographic cycle over the eastern Siberian shelf","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Arctic Sciences; Office of Polar Programs; Natural Sciences and Engineering Research Council of Canada; International Arctic Research Center, University of Alaska, Fairbanks; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Hydrography; Oceanography; Climatology; Salinity; Potential vorticity; Environmental science; Vorticity; Anticyclone; Geology; Geography; Meteorology; Vortex","score_opus":0.014681340493081214,"score_gpt":0.23728428226995413,"score_spread":0.22260294177687293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1981927376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850994,0.00015933315,0.000049195096,0.00009572803,0.000016715634,0.0000017523037,0.0002852076,0.000011030893,0.00087114953],"genre_scores_gemma":[0.999501,0.00009008904,0.000016225766,0.000011465668,0.000007859396,0.0000011952297,0.00022657758,0.0000035379899,0.00014199973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998604,0.00003651769,0.0000195352,0.000023324648,0.000025169213,0.000035048055],"domain_scores_gemma":[0.99941885,0.00016888489,0.00012314167,0.000055083554,0.00010993459,0.0001240598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004566906,0.00025533047,0.00028296272,0.00039610045,0.0005517748,0.0010595844,0.00013192456,0.00019276878,0.0020101403],"category_scores_gemma":[0.0013931103,0.00016922169,0.0003112686,0.0005087376,0.00032327833,0.0003622546,0.0006127394,0.0002516576,0.00022777278],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059969915,0.00009012064,0.9633762,0.00004238719,0.0002841469,0.0003955424,0.00023720542,0.014187522,0.0069897794,0.000498798,0.0009565484,0.0123420665],"study_design_scores_gemma":[0.000008360724,0.000029015622,0.9946733,0.000005506888,0.000028549166,0.000017992703,0.00008070125,0.00467588,0.00020204629,0.00008604681,0.00018787866,0.0000047192384],"about_ca_topic_score_codex":0.039585315,"about_ca_topic_score_gemma":0.03407845,"teacher_disagreement_score":0.039585315,"about_ca_system_score_codex":0.0007264609,"about_ca_system_score_gemma":0.000586029,"threshold_uncertainty_score":0.07870984},"labels":[],"label_agreement":null},{"id":"W1982277006","doi":"10.1029/2009gl039743","title":"How islands cause phytoplankton to bloom in their wakes","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Bloom; Phytoplankton; Oceanography; Environmental science; Algal bloom; Geology; Biology; Ecology; Nutrient","score_opus":0.027950838290709608,"score_gpt":0.2676656635374604,"score_spread":0.2397148252467508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982277006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987596,0.0000142096505,0.00047910356,0.00003082976,0.000007650568,0.0000028471113,0.000011623733,0.000014739993,0.0006793141],"genre_scores_gemma":[0.9996755,0.000013954908,0.0001411194,0.0000059387366,0.0000014908875,0.0000013774326,0.0000111105865,0.000002470907,0.00014709965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999685,0.0000071409636,0.0000016406307,0.000005865829,0.0000048385727,0.000011896617],"domain_scores_gemma":[0.9998549,0.00003606999,0.00003272339,0.000013469787,0.000018491906,0.000044281966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008655938,0.00009145849,0.000119522076,0.00008085422,0.00020702956,0.0003831789,0.00009779912,0.00019942579,0.0007191042],"category_scores_gemma":[0.0005870084,0.00015025934,0.00014511483,0.000041915897,0.00021027931,0.00021310119,0.00029592073,0.00014115674,0.00011237728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009041879,0.0002265618,0.48666072,0.00013189782,0.00021567268,0.002058996,0.000923078,0.22819236,0.25039524,0.007916249,0.0024061783,0.019968936],"study_design_scores_gemma":[0.00010741559,0.00054396986,0.38165814,0.00002326324,0.00015222984,0.00031791936,0.001426201,0.5915557,0.017472144,0.0038327926,0.0028605734,0.000049627623],"about_ca_topic_score_codex":0.0027406616,"about_ca_topic_score_gemma":0.0034403591,"teacher_disagreement_score":0.0027406616,"about_ca_system_score_codex":0.00021741794,"about_ca_system_score_gemma":0.00018677258,"threshold_uncertainty_score":0.005449474},"labels":[],"label_agreement":null},{"id":"W1982350179","doi":"10.1029/2003gl017775","title":"On the relationship between stomatal characters and atmospheric CO<sub>2</sub>","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"U.S. Department of Agriculture; U.S. Department of Energy","keywords":"Stomatal density; Atmospheric sciences; Environmental science; Climate change; Evapotranspiration; Biology; Ecology; Botany; Geology; Photosynthesis","score_opus":0.03009769378497386,"score_gpt":0.2680584224786405,"score_spread":0.23796072869366663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982350179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948114,0.000071023074,0.00015065224,0.000014858565,0.0000015931664,0.000003667651,0.00006877001,0.0000032366013,0.0002050004],"genre_scores_gemma":[0.9989767,0.00009738104,0.00030224762,0.000044570304,0.0000047606577,0.000008830085,0.00021997876,0.000004548751,0.00034110315],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000021904483,0.000006672047,0.000027307042,0.000013947525,0.000016226231],"domain_scores_gemma":[0.99931896,0.0003427114,0.00013458851,0.00007023044,0.000052552132,0.000080979946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002531764,0.00022927138,0.00019459333,0.00017267394,0.00015624048,0.00018416927,0.00021916209,0.00028413357,0.0013124725],"category_scores_gemma":[0.00042816316,0.0001866953,0.0001364038,0.00015982946,0.00040445066,0.0002857764,0.00028939833,0.00040477348,0.00024063577],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010001085,0.00013425748,0.07466797,0.00008363517,0.00005654842,0.0002424971,0.00034166605,0.0006305226,0.9129322,0.00008107846,0.00012511846,0.009704349],"study_design_scores_gemma":[0.000015394759,0.00071152236,0.9397074,0.000005149428,0.00004574171,0.00024001529,0.00019831547,0.0017904396,0.05663086,0.00011097236,0.0005293145,0.000014881406],"about_ca_topic_score_codex":0.001251234,"about_ca_topic_score_gemma":0.0031996043,"teacher_disagreement_score":0.0013124725,"about_ca_system_score_codex":0.00018381543,"about_ca_system_score_gemma":0.00008573478,"threshold_uncertainty_score":0.004390657},"labels":[],"label_agreement":null},{"id":"W1982407096","doi":"10.1029/2007gl031967","title":"Probing the sources of ambient seismic noise near the coasts of southern Italy","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Ambient noise level; Seismology; Seismic noise; Subduction; Microseism; Noise (video); Oceanography; Tectonics; Sound (geography)","score_opus":0.023880531624309732,"score_gpt":0.2626384491496545,"score_spread":0.23875791752534478,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982407096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909604,0.00006146745,0.00014309326,0.00002417819,0.0000020221937,0.0000021301628,0.00008624178,0.000006258526,0.000578424],"genre_scores_gemma":[0.99917907,0.00006797122,0.00022067812,0.000008688466,0.000010371675,0.0000051323827,0.000318915,0.0000031517334,0.0001861116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998555,0.000022519444,0.000007654144,0.00004678752,0.00003360027,0.000033944474],"domain_scores_gemma":[0.99959606,0.000059993512,0.0002005787,0.00003188034,0.0000793132,0.00003213277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018075523,0.00019340136,0.00018494038,0.00069647725,0.00016605778,0.00040890407,0.00017905408,0.00019789304,0.0004137821],"category_scores_gemma":[0.0009932691,0.00011225883,0.000100127574,0.0009549582,0.00023844508,0.00019343678,0.0004357539,0.00015137644,0.00012088226],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001122558,0.000023440773,0.9737936,0.00002586075,0.00003604507,0.00029037104,0.001017965,0.0010607028,0.007026176,0.00007979114,0.00027448343,0.01625924],"study_design_scores_gemma":[0.0000026370426,0.000010488777,0.9992655,0.0000023985144,0.0000043087744,0.000030686144,0.00008983568,0.0002877018,0.000060619368,0.000011035281,0.0002333901,0.0000014664566],"about_ca_topic_score_codex":0.020992802,"about_ca_topic_score_gemma":0.044554718,"teacher_disagreement_score":0.020992802,"about_ca_system_score_codex":0.00030883588,"about_ca_system_score_gemma":0.00021048772,"threshold_uncertainty_score":0.041741252},"labels":[],"label_agreement":null},{"id":"W1982798809","doi":"10.1002/grl.50111","title":"Correction to “Linking the 8.2 ka event and its freshwater forcing in the Labrador Sea”","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Forcing (mathematics); Geology; Event (particle physics); Oceanography; Seawater; Climatology; Physics; Astrophysics","score_opus":0.03015257498872357,"score_gpt":0.2884338335891007,"score_spread":0.2582812586003771,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1982798809","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012723543,0.0015256358,0.0036425116,0.034361888,0.90842617,0.00008992719,0.034455378,0.004715696,0.011510405],"genre_scores_gemma":[0.10556085,0.009837415,0.05025501,0.06814198,0.32322484,0.0009106433,0.1232899,0.021293538,0.2974858],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9977069,0.00026939492,0.00026959335,0.00040706218,0.001013573,0.00033337355],"domain_scores_gemma":[0.9846303,0.0014370619,0.0010303686,0.001547677,0.010295784,0.0010588799],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014482961,0.0025245596,0.002096246,0.0052280705,0.0033615287,0.0038297703,0.0041563543,0.0036897578,0.11843159],"category_scores_gemma":[0.02042719,0.0014926831,0.0021510115,0.006179344,0.0017096675,0.0040751877,0.0027680527,0.008416729,0.045688912],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004994511,0.0000058690293,0.00018540001,0.00009052615,0.000011816744,0.00004592536,0.000028429384,0.00007551584,0.00014000601,0.0003990487,0.9954964,0.0034711855],"study_design_scores_gemma":[0.00008082969,0.000014940087,0.0061677494,0.00016745586,0.000038815437,0.0001443557,0.0000883965,0.00031496762,0.00055448606,0.00073503965,0.99164575,0.000047113514],"about_ca_topic_score_codex":0.06155745,"about_ca_topic_score_gemma":0.07716646,"teacher_disagreement_score":0.11843159,"about_ca_system_score_codex":0.0032379355,"about_ca_system_score_gemma":0.004808589,"threshold_uncertainty_score":0.39619315},"labels":[],"label_agreement":null},{"id":"W1983559033","doi":"10.1002/2014gl059965","title":"A laboratory acoustic emission experiment under in situ conditions","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Acoustic emission; Induced seismicity; Geology; Excavation; Seismology; Geophone; Quartz; Prism; Geotechnical engineering; Acoustics; Physics; Optics","score_opus":0.027673529475999794,"score_gpt":0.3133845585345244,"score_spread":0.28571102905852463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983559033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99428695,0.000026995844,0.004433753,0.000025756592,0.00000922449,0.00003195644,0.000116583615,0.00007479811,0.0009939678],"genre_scores_gemma":[0.99462444,0.000051780156,0.003961188,0.000053356063,0.000010010575,0.000052252708,0.00017905183,0.00002352592,0.0010443315],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99952126,0.00007532142,0.000016048207,0.0001234591,0.0001646934,0.000099267185],"domain_scores_gemma":[0.9994179,0.00015326634,0.00007906353,0.000070426875,0.00022559092,0.000053760716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004466414,0.0004242247,0.0003768318,0.00026392186,0.00059912854,0.0003168266,0.0007481463,0.00053320493,0.0011883948],"category_scores_gemma":[0.00059184426,0.00019471509,0.00019130195,0.00031297814,0.0006743415,0.00028148017,0.00051335816,0.00055952533,0.00028989097],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002831814,0.0003355017,0.008192468,0.00004866241,0.000023234707,0.00022630132,0.0004634613,0.00089545955,0.98500293,0.000047174577,0.00011846552,0.004363081],"study_design_scores_gemma":[0.00022994255,0.003983038,0.1080191,0.000026546748,0.00012829698,0.0005879595,0.001945384,0.008266682,0.8720182,0.00013249599,0.0045996862,0.00006264687],"about_ca_topic_score_codex":0.02082468,"about_ca_topic_score_gemma":0.040246006,"teacher_disagreement_score":0.02082468,"about_ca_system_score_codex":0.0005432107,"about_ca_system_score_gemma":0.00062668737,"threshold_uncertainty_score":0.04140693},"labels":[],"label_agreement":null},{"id":"W1983605515","doi":"10.1029/2012gl054675","title":"A high‐resolution study of tides in the Delaware Bay: Past conditions and future scenarios","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Oceanic and Atmospheric Administration","keywords":"Bay; Post-glacial rebound; Geology; Oceanography; Sea level; Shore; Glacial period; Tidal range; Sea level rise; Last Glacial Maximum; Estuary; Geomorphology; Holocene; Climate change","score_opus":0.0335562294472095,"score_gpt":0.3028062044004617,"score_spread":0.2692499749532522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983605515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899954,0.0000366037,0.00013197951,0.00004400133,0.0000019248116,0.0000033496112,0.00044483482,0.000008821466,0.0003289856],"genre_scores_gemma":[0.99883896,0.00004763323,0.00031960214,0.00000950144,0.0000018826664,0.000004700379,0.00058645365,0.0000019785853,0.00018929158],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992955,0.000016263992,0.0000049902956,0.000021516824,0.000013223605,0.000014469316],"domain_scores_gemma":[0.9997172,0.00007833514,0.0000642899,0.000036518548,0.00005715773,0.000046505702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002780959,0.00014457564,0.0001600999,0.000383998,0.0003101057,0.0006885237,0.0004021905,0.00026013906,0.0005260665],"category_scores_gemma":[0.0005433451,0.00021475193,0.00032146138,0.0006765011,0.00021215888,0.00037615365,0.0002858012,0.00028179112,0.000072074385],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001894728,0.00015150568,0.90406615,0.000042614734,0.00022985628,0.00043321727,0.00033488905,0.08046595,0.0020491488,0.0003707034,0.0009902276,0.010676361],"study_design_scores_gemma":[0.000039290233,0.00007805432,0.9072933,0.000018143232,0.000080593105,0.0001174875,0.0007092728,0.08900603,0.00053192925,0.00011822323,0.0019782144,0.000029482111],"about_ca_topic_score_codex":0.3049103,"about_ca_topic_score_gemma":0.46719438,"teacher_disagreement_score":0.3049103,"about_ca_system_score_codex":0.0016477909,"about_ca_system_score_gemma":0.00074178434,"threshold_uncertainty_score":0.606271},"labels":[],"label_agreement":null},{"id":"W1983619700","doi":"10.1029/2009gl040224","title":"Recent tectonic plate decelerations driven by mantle convection","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Mantle convection; Plate tectonics; Mantle (geology); Geophysics; Convection; Post-glacial rebound; Geodetic datum; Buoyancy; Ocean surface topography; Gravity anomaly; Tectonics; Geodesy; Seismology; Lithosphere; Sea level; Mechanics; Physics","score_opus":0.029148150436334667,"score_gpt":0.27024621240238167,"score_spread":0.241098061966047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983619700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942047,0.00020137298,0.0031891277,0.000099831464,0.000006355833,0.0000029092885,0.00016890938,0.00013899368,0.00198779],"genre_scores_gemma":[0.998776,0.00012943536,0.00058782654,0.000006296734,0.000003869337,0.0000017416002,0.00016769728,0.000013019009,0.00031414375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997675,0.0000029324783,0.0000013997178,0.00000830901,0.000005225196,0.000005350516],"domain_scores_gemma":[0.99988186,0.000017246666,0.000039102077,0.000020963294,0.000024914718,0.000015909814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016879031,0.00028679802,0.0001165938,0.0004238504,0.00019468389,0.00035374923,0.00025265652,0.0002038349,0.0011363984],"category_scores_gemma":[0.0006693623,0.00019953649,0.00025275748,0.00024358815,0.00026856092,0.00030745566,0.00031267005,0.00024657184,0.00013208039],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047221457,0.000050952647,0.45259795,0.00014580069,0.00020049415,0.00059628027,0.0005807812,0.42833385,0.063485615,0.013087969,0.0012507805,0.03919726],"study_design_scores_gemma":[0.000064703374,0.00014562315,0.45372382,0.000021196942,0.00009465068,0.0005230166,0.00011100306,0.5213059,0.012601882,0.006438966,0.004926203,0.00004308579],"about_ca_topic_score_codex":0.008866564,"about_ca_topic_score_gemma":0.007240167,"teacher_disagreement_score":0.008866564,"about_ca_system_score_codex":0.00059995684,"about_ca_system_score_gemma":0.00020254885,"threshold_uncertainty_score":0.017629921},"labels":[],"label_agreement":null},{"id":"W1983952469","doi":"10.1029/2008gl035430","title":"Phase coherence analysis of a field line resonance and solar wind oscillation","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Magnetosphere; Solar wind; Physics; Oscillation (cell signaling); Computational physics; Coherence (philosophical gambling strategy); Amplitude; Magnetopause; Field line; Geophysics; Phase (matter); Plasma; Optics","score_opus":0.024616837766683528,"score_gpt":0.3133868641978379,"score_spread":0.28877002643115435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1983952469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9191338,0.000066812485,0.079290725,0.000035567395,0.000006822761,0.000008998112,0.00007202167,0.00006400061,0.0013211651],"genre_scores_gemma":[0.99579215,0.000022242952,0.0039475127,0.0000040694285,0.0000041627277,0.0000040607642,0.000060271934,0.0000069755456,0.00015850809],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993837,0.000012444924,0.0000025268016,0.000014427885,0.00002320986,0.000009006261],"domain_scores_gemma":[0.99968696,0.00017497127,0.00006768271,0.000019675015,0.00003828609,0.000012429745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017122214,0.00008244549,0.00006168177,0.000378262,0.000082273495,0.0001497637,0.00007781788,0.00011006249,0.00064975925],"category_scores_gemma":[0.0012686967,0.000063289226,0.000060658167,0.00027587684,0.0001612085,0.00021950838,0.00012501059,0.00012070292,0.00005240742],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075061625,0.00013258979,0.05506063,0.00012065912,0.000113538845,0.00054431846,0.0005351778,0.16292672,0.5722671,0.033167128,0.0010467906,0.1733347],"study_design_scores_gemma":[0.000028287282,0.00017210176,0.0949378,0.000006333357,0.000022583194,0.00026581238,0.00010827029,0.8535418,0.043793365,0.0057539605,0.0013491898,0.000020435727],"about_ca_topic_score_codex":0.0007761192,"about_ca_topic_score_gemma":0.0005084366,"teacher_disagreement_score":0.0007761192,"about_ca_system_score_codex":0.00010256221,"about_ca_system_score_gemma":0.00009272958,"threshold_uncertainty_score":0.0021736026},"labels":[],"label_agreement":null},{"id":"W1984320821","doi":"10.1029/2006gl027774","title":"Deglaciating the snowball Earth: Sensitivity to surface albedo","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Albedo (alchemy); Snowball Earth; Deglaciation; Forcing (mathematics); Snow; Earth system science; Geology; Climatology; Environmental science; Climate model; Atmospheric sciences; Climate change; Glacial period; Geomorphology; Oceanography","score_opus":0.030494609978622526,"score_gpt":0.2871638411138207,"score_spread":0.2566692311351982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984320821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989623,0.00005470943,0.0004940778,0.000033302815,0.0000025180404,0.0000034703883,0.00010679426,0.00001724159,0.00032561916],"genre_scores_gemma":[0.9996464,0.00005065801,0.00015960535,0.000010250082,8.7604514e-7,0.0000010923268,0.000087024135,0.0000045924207,0.000039413088],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987113,0.000033836986,0.0000073039987,0.000024847157,0.000022839315,0.0000399796],"domain_scores_gemma":[0.99915075,0.00046894915,0.00014528199,0.00008894429,0.000067345936,0.00007872907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048730706,0.0002823074,0.00027077072,0.00025145322,0.00020218745,0.0005930778,0.00024350619,0.0003885327,0.0005446863],"category_scores_gemma":[0.0024961436,0.00023489112,0.00043968047,0.0003936688,0.00039618654,0.00042971445,0.00050265784,0.0003766117,0.000056497716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00092504115,0.00007846033,0.46168908,0.00016484266,0.0003208399,0.00050422276,0.00023097135,0.40535048,0.12112177,0.00077180925,0.0003835555,0.008458855],"study_design_scores_gemma":[0.00006169108,0.00031013697,0.65390843,0.000021966547,0.00014034176,0.00029923077,0.0003490319,0.3038118,0.03898814,0.0012633663,0.0007942005,0.000051708626],"about_ca_topic_score_codex":0.021612434,"about_ca_topic_score_gemma":0.016146887,"teacher_disagreement_score":0.021612434,"about_ca_system_score_codex":0.0004974863,"about_ca_system_score_gemma":0.00023144708,"threshold_uncertainty_score":0.04297328},"labels":[],"label_agreement":null},{"id":"W1984505848","doi":"10.1029/2003gl017645","title":"Validation of imaging Doppler interferometer winds using meteor radar","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Meteor (satellite); Radar; Remote sensing; Geology; Interferometry; Meteoroid; Doppler effect; Observatory; Doppler radar; Geodesy; Meteorology; Physics; Computer science; Telecommunications; Optics; Astronomy","score_opus":0.02624638637561325,"score_gpt":0.3066283310119974,"score_spread":0.2803819446363841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984505848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879816,0.00014508917,0.0072608613,0.000052207397,0.000055829572,0.000048267884,0.0009698826,0.00016642822,0.0033199259],"genre_scores_gemma":[0.9902554,0.000061261584,0.008321439,0.00003397412,0.0000126061905,0.00002084744,0.0010314023,0.000016668188,0.00024638933],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99917525,0.0001957432,0.000098713506,0.00018819574,0.00026017317,0.000081898834],"domain_scores_gemma":[0.9983309,0.00024674166,0.0003054635,0.0003465932,0.0006729763,0.00009723292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00149807,0.00026154864,0.00027275126,0.00044017806,0.0002732333,0.0006946943,0.00048179063,0.0002514235,0.00034776563],"category_scores_gemma":[0.0038320466,0.00016854296,0.000140982,0.00052957336,0.00019289803,0.000632148,0.0006048137,0.0003295596,0.00027121074],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010295237,0.00014340754,0.8708044,0.00012492434,0.000109750414,0.00016470789,0.0003961237,0.0057940376,0.056164455,0.00066282874,0.00080940046,0.063796334],"study_design_scores_gemma":[0.00023639797,0.0011475101,0.8862712,0.000077563636,0.00009719256,0.0005419224,0.00053907785,0.046833217,0.05720777,0.00035473803,0.006639522,0.00005402049],"about_ca_topic_score_codex":0.003132728,"about_ca_topic_score_gemma":0.004058366,"teacher_disagreement_score":0.003132728,"about_ca_system_score_codex":0.00021010675,"about_ca_system_score_gemma":0.0003296561,"threshold_uncertainty_score":0.007922649},"labels":[],"label_agreement":null},{"id":"W1984510328","doi":"10.1029/2006gl026913","title":"Interannual variability of newly formed Labrador Sea Water from 1994 to 2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Geology; Environmental science; Climatology","score_opus":0.012441875341231336,"score_gpt":0.2488336204522214,"score_spread":0.23639174511099006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984510328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966732,0.00018131569,0.00007889958,0.000018978242,0.000004390203,0.00000603578,0.002436923,0.000030692412,0.00056942547],"genre_scores_gemma":[0.9949639,0.00012737434,0.00013792694,0.00001333619,0.000008043438,0.000008993185,0.0043543233,0.0000043871437,0.00038179342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982697,0.000012739478,0.000023394688,0.000055654684,0.000036527683,0.00004479517],"domain_scores_gemma":[0.9993917,0.00004040788,0.0003175987,0.000041489668,0.00015141493,0.000057407848],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032619626,0.00023939363,0.0002562868,0.0014831737,0.00022361733,0.00060260994,0.00032056376,0.00016735567,0.0006178321],"category_scores_gemma":[0.00053393963,0.00009667726,0.0002296374,0.0013818522,0.00015361146,0.00032245927,0.00037402767,0.000118875665,0.0002303606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016662224,0.000032650423,0.9822833,0.000049936785,0.00012995327,0.000081717386,0.00022080114,0.0005319859,0.0018954896,0.000038457518,0.0005963095,0.013972846],"study_design_scores_gemma":[0.0000012741315,0.000017339618,0.9989385,0.0000036989227,0.000010336487,0.0000260887,0.000060353952,0.00014090433,0.0002739521,0.000002357247,0.0005226917,0.000002560928],"about_ca_topic_score_codex":0.043265607,"about_ca_topic_score_gemma":0.08386394,"teacher_disagreement_score":0.043265607,"about_ca_system_score_codex":0.0011334756,"about_ca_system_score_gemma":0.00031877236,"threshold_uncertainty_score":0.08602756},"labels":[],"label_agreement":null},{"id":"W1984560390","doi":"10.1029/2003gl017346","title":"Investigating the geoelectrical response of hydrocarbon contamination undergoing biodegradation","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; University of Waterloo","funders":"","keywords":"Contamination; Weathering; Biodegradation; Geology; Conductivity; Soil science; Hydrocarbon; Environmental chemistry; Water table; Soil water; Groundwater; Environmental science; Mineralogy; Geotechnical engineering; Geomorphology; Chemistry; Ecology","score_opus":0.04415461969416919,"score_gpt":0.3032335513552576,"score_spread":0.2590789316610884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984560390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986998,0.0000257484,0.0010300843,0.000012243764,5.577738e-7,0.0000020022499,0.000028904682,0.00000956157,0.00019112657],"genre_scores_gemma":[0.9994696,0.00003592189,0.0003065498,0.00000401822,4.9309904e-7,0.0000015651374,0.000049889062,0.000001596074,0.00013034257],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995553,0.0000074495742,0.0000020615485,0.000008374735,0.000014625241,0.0000119388005],"domain_scores_gemma":[0.9999021,0.000036197333,0.000024352365,0.0000064835704,0.000023130244,0.0000077197665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000079334044,0.00011253384,0.0000961786,0.00017321318,0.00007181101,0.00020898788,0.000094194744,0.00016127493,0.00028559443],"category_scores_gemma":[0.00032277944,0.000057468096,0.000075628974,0.00023269594,0.00012441231,0.00016761295,0.00014273178,0.00011969829,0.00008159391],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021841892,0.000034131033,0.033275194,0.00003747331,0.000010661676,0.00019780664,0.00009091251,0.0030845143,0.9563983,0.00011138067,0.000033336382,0.006507729],"study_design_scores_gemma":[0.000017698956,0.0005260835,0.11773678,0.0000052062182,0.000019361423,0.00057052914,0.00040075395,0.060372353,0.81891465,0.0005741201,0.00084878574,0.000013641887],"about_ca_topic_score_codex":0.0009690953,"about_ca_topic_score_gemma":0.00083836477,"teacher_disagreement_score":0.0009690953,"about_ca_system_score_codex":0.0001448494,"about_ca_system_score_gemma":0.00008011031,"threshold_uncertainty_score":0.0019269586},"labels":[],"label_agreement":null},{"id":"W1984828365","doi":"10.1029/2002gl016516","title":"On the response of Southern Ocean water‐masses to atmospheric meridional moisture advection","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Australian Research Council","keywords":"Advection; Zonal and meridional; Climatology; Moisture; Stratification (seeds); Water mass; Environmental science; Atmospheric sciences; Geology; Salinity; Oceanography; Meteorology; Geography","score_opus":0.023255354985108827,"score_gpt":0.2707606522326577,"score_spread":0.24750529724754888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1984828365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99855477,0.00003039193,0.0007233305,0.00006998065,0.0000049720506,0.0000075691546,0.00009307553,0.000025476658,0.0004904892],"genre_scores_gemma":[0.9996568,0.000030798914,0.00014226451,0.000011866999,0.0000021281307,0.000003983113,0.00005422282,0.0000051850393,0.00009269317],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998629,0.00004894445,0.0000064887536,0.000027587079,0.000015428825,0.00003873723],"domain_scores_gemma":[0.9991129,0.000557457,0.00011989032,0.00006321162,0.00007027451,0.000076211654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000518469,0.0005197206,0.00036425985,0.00023567988,0.0002550716,0.0006153596,0.0003317533,0.00055681734,0.0007599327],"category_scores_gemma":[0.0023902252,0.00029994018,0.00054693944,0.00022715531,0.0004973173,0.0004379122,0.00062550406,0.00042781697,0.00008519656],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008270381,0.00015187748,0.085276484,0.00007051006,0.0002378351,0.00023272928,0.0001076914,0.8678688,0.0400827,0.0010533045,0.00029966992,0.0037913453],"study_design_scores_gemma":[0.00010759542,0.0004263114,0.04711603,0.0000057639127,0.00007648797,0.000029076196,0.000069349415,0.9458156,0.0054051117,0.0007318987,0.00018628199,0.000030568925],"about_ca_topic_score_codex":0.017364612,"about_ca_topic_score_gemma":0.009177073,"teacher_disagreement_score":0.017364612,"about_ca_system_score_codex":0.00042940938,"about_ca_system_score_gemma":0.0003169514,"threshold_uncertainty_score":0.034527123},"labels":[],"label_agreement":null},{"id":"W1985526802","doi":"10.1029/2006gl026510","title":"Greenland warming of 1920–1930 and 1995–2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Global warming; Climatology; Environmental science; Groenlandia; Climate change; Greenland ice sheet; Current (fluid); Physical geography; Geology; Oceanography; Geography; Glacier; Ice sheet","score_opus":0.03235515261328663,"score_gpt":0.2952815329384858,"score_spread":0.26292638032519916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985526802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868151,0.0005781642,0.00022335968,0.00023033582,0.000035373305,0.000007315625,0.0066257245,0.000035320383,0.0054492857],"genre_scores_gemma":[0.99372685,0.00026416965,0.00022452632,0.00008509422,0.000023639795,0.000010190881,0.0051026866,0.0000069171174,0.0005557862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.0000059434547,0.0000051863663,0.000024444738,0.00001560769,0.000028440756],"domain_scores_gemma":[0.99979955,0.000018906145,0.00007413627,0.000019237215,0.00005500378,0.000033215318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037299775,0.00021940375,0.00016508748,0.0012782941,0.00034090906,0.0003850471,0.00023791185,0.00026753763,0.0012577447],"category_scores_gemma":[0.0006064056,0.0000881324,0.00030509869,0.0011926463,0.00026799846,0.00043780138,0.00043410197,0.0002773807,0.00017795117],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065402593,0.000096118754,0.93434757,0.00014310336,0.00033827446,0.0003952239,0.0011340916,0.0075646313,0.0046161143,0.0031124083,0.006971408,0.04062689],"study_design_scores_gemma":[0.0000039277597,0.000010231883,0.9963387,0.000009025318,0.000017310414,0.000023960654,0.00006115091,0.00036329756,0.00021621858,0.000100388774,0.0028514287,0.000004371361],"about_ca_topic_score_codex":0.13410643,"about_ca_topic_score_gemma":0.23966306,"teacher_disagreement_score":0.13410643,"about_ca_system_score_codex":0.0019195626,"about_ca_system_score_gemma":0.00054165785,"threshold_uncertainty_score":0.2666517},"labels":[],"label_agreement":null},{"id":"W1985856626","doi":"10.1029/2006gl026705","title":"Impact of floods versus routing events on the thermohaline circulation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Thermohaline circulation; Shutdown of thermohaline circulation; Younger Dryas; Atlantic multidecadal oscillation; Climatology; Geology; Deglaciation; Abrupt climate change; Northern Hemisphere; Oceanography; Climate change; North Atlantic Deep Water; Global warming; Holocene; Effects of global warming","score_opus":0.058725043129941576,"score_gpt":0.34018769639934854,"score_spread":0.28146265326940695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1985856626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99791986,0.000047782996,0.00036213588,0.00018715081,0.000011903956,0.0000039199413,0.0001395884,0.000021535841,0.0013061152],"genre_scores_gemma":[0.9995128,0.000055209017,0.000095473806,0.00002927845,0.000005117233,0.0000029670834,0.000057198,0.0000058791575,0.0002361087],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998441,0.000058954683,0.0000057324255,0.000027521493,0.000012765892,0.000050911323],"domain_scores_gemma":[0.99949634,0.00030125832,0.00006261902,0.000022544462,0.000025467505,0.0000916474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003509061,0.00036396028,0.00032740977,0.0002034419,0.0005343003,0.0012157595,0.0003400688,0.00096146704,0.0023935144],"category_scores_gemma":[0.0013344925,0.0003137235,0.00067933835,0.00018599915,0.00081995124,0.00085036876,0.000711026,0.0006728275,0.00008465364],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067624066,0.00018006831,0.050281778,0.00003453008,0.00016486661,0.000286394,0.000091501235,0.9307364,0.010374443,0.0036430294,0.0005721151,0.002958669],"study_design_scores_gemma":[0.0002130204,0.0003929705,0.03820613,0.0000072223143,0.00014983655,0.0000611487,0.00016834693,0.9561743,0.0022727519,0.0019213039,0.0003915561,0.000041339074],"about_ca_topic_score_codex":0.026323736,"about_ca_topic_score_gemma":0.01661251,"teacher_disagreement_score":0.026323736,"about_ca_system_score_codex":0.0011415466,"about_ca_system_score_gemma":0.000687046,"threshold_uncertainty_score":0.052341044},"labels":[],"label_agreement":null},{"id":"W1986223085","doi":"10.1029/2004gl021155","title":"Reply to comment by R. Blender and K. Fraedrich on “Volcanic forcing improves atmosphere–ocean coupled general circulation model scaling performance”","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Forcing (mathematics); Atmosphere (unit); Volcano; Noise (video); Physics; White (mutation); Meteorology; Climatology; Seismology; Computer science; Chemistry","score_opus":0.029589488752395143,"score_gpt":0.28390661838644504,"score_spread":0.2543171296340499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986223085","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00025875316,0.001268205,0.00025800607,0.9776487,0.019698383,0.0000073162487,0.000266043,0.000074799806,0.0005198502],"genre_scores_gemma":[0.0039033925,0.001013771,0.00029735878,0.9635443,0.028733304,0.000043067626,0.00013464161,0.00010525814,0.0022249557],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99566466,0.00082371704,0.00066979084,0.0010430947,0.0014256795,0.0003730896],"domain_scores_gemma":[0.98062366,0.008887789,0.0020261358,0.0008947448,0.0064163464,0.0011513364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007134604,0.0015177433,0.0019038889,0.0011675017,0.0030031907,0.0031301156,0.004903639,0.031928968,0.00790228],"category_scores_gemma":[0.04299803,0.0010468608,0.001836483,0.00154781,0.004007696,0.007164715,0.0031784442,0.040900655,0.008574635],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042143573,0.000010305737,0.00022583413,0.000060973678,0.0000148242625,0.000078722995,0.00015865656,0.00007860057,0.00012321661,0.0013660726,0.9947973,0.0030435014],"study_design_scores_gemma":[0.00016305226,0.00008887498,0.0045397184,0.0005507062,0.00006270872,0.00047635063,0.0007876267,0.0010305854,0.0012177029,0.014792797,0.9760208,0.0002691004],"about_ca_topic_score_codex":0.014682668,"about_ca_topic_score_gemma":0.00886178,"teacher_disagreement_score":0.031928968,"about_ca_system_score_codex":0.0038228743,"about_ca_system_score_gemma":0.003286005,"threshold_uncertainty_score":0.037731826},"labels":[],"label_agreement":null},{"id":"W1986676657","doi":"10.1029/2006gl026278","title":"An examination of advection in the northeast Pacific Ocean, 2001–2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; University of Alberta","funders":"National Oceanic and Atmospheric Administration","keywords":"Advection; Argo; Climatology; Ocean gyre; Environmental science; Geology; Eddy; Oceanography; Subtropics; Meteorology; Geography; Turbulence","score_opus":0.017818468031764755,"score_gpt":0.2576117383461541,"score_spread":0.23979327031438932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986676657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977863,0.00010436603,0.00015283789,0.00006029785,0.000005104605,0.000003021271,0.0007539436,0.000009164136,0.0011248552],"genre_scores_gemma":[0.997131,0.00012846955,0.00027648913,0.000019697949,0.00000448974,0.0000053435992,0.0017581005,0.0000032391597,0.0006731856],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993193,0.000008040153,0.000010976316,0.00001996717,0.00001910461,0.000010076143],"domain_scores_gemma":[0.9992092,0.00017124237,0.00032650793,0.000056208137,0.00018935905,0.00004741259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033907706,0.00015602013,0.00008923303,0.0006055944,0.00026107903,0.0005034183,0.00015150178,0.0002307453,0.0006111099],"category_scores_gemma":[0.0014388785,0.00013928369,0.00022385134,0.0009205727,0.00011592155,0.00042183782,0.00026526774,0.00025202305,0.000110901405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000197153,0.00004564303,0.9770558,0.00005526817,0.00011728301,0.00014168567,0.0007414692,0.0040534805,0.0025912605,0.00038977686,0.00075773604,0.013853467],"study_design_scores_gemma":[0.000002398761,0.000018055594,0.9966595,0.000006857681,0.000010541291,0.00005115603,0.00013913914,0.0017436903,0.00024137806,0.000039537365,0.0010841718,0.0000034954833],"about_ca_topic_score_codex":0.028304243,"about_ca_topic_score_gemma":0.03777617,"teacher_disagreement_score":0.028304243,"about_ca_system_score_codex":0.0005068308,"about_ca_system_score_gemma":0.00027703185,"threshold_uncertainty_score":0.056279004},"labels":[],"label_agreement":null},{"id":"W1986898856","doi":"10.1029/2001gl014556","title":"Daily maximum and minimum temperature trends in a climate model","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Environmental science; Forcing (mathematics); Climatology; Greenhouse gas; Atmospheric sciences; Climate change; Climate model; Global warming; Diurnal temperature variation; Cloud cover; Radiative forcing; Range (aeronautics); Geology; Cloud computing","score_opus":0.04684187529435717,"score_gpt":0.3004598879245743,"score_spread":0.2536180126302171,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1986898856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9338671,0.00032892812,0.0094379345,0.0008030863,0.0001317197,0.000052328865,0.03580993,0.001081345,0.018487608],"genre_scores_gemma":[0.9794668,0.00018050677,0.0033418704,0.00007309831,0.00003035803,0.00006552552,0.014248179,0.000090908135,0.0025027578],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988186,0.000033362634,0.000008856142,0.000045897734,0.000015272037,0.0000148286435],"domain_scores_gemma":[0.9997547,0.00006680614,0.00003228606,0.000045947298,0.00006787191,0.000032362233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003007703,0.00030818465,0.000327431,0.00027356044,0.0003194484,0.00082178006,0.00079077575,0.00071197737,0.003631745],"category_scores_gemma":[0.00086094905,0.00030528253,0.0005204458,0.00079647073,0.00019744181,0.00064930297,0.00025238228,0.0005410974,0.00081634824],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021486873,0.00007657874,0.014307756,0.000055675308,0.0001763275,0.000042984568,0.00006364787,0.97091055,0.001500095,0.0033246467,0.0054844194,0.0038424004],"study_design_scores_gemma":[0.00015531303,0.000075622534,0.020935902,0.000010132947,0.000073065494,0.000027098327,0.000033085533,0.96719944,0.0007953935,0.002274368,0.008387164,0.000033314383],"about_ca_topic_score_codex":0.031728532,"about_ca_topic_score_gemma":0.024067318,"teacher_disagreement_score":0.031728532,"about_ca_system_score_codex":0.0010219159,"about_ca_system_score_gemma":0.0006343494,"threshold_uncertainty_score":0.0630877},"labels":[],"label_agreement":null},{"id":"W1987642525","doi":"10.1029/2004gl020426","title":"“Great Salinity Anomalies” in a coupled climate model","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"HadCM3; Climatology; Ocean gyre; Climate change; Salinity; Geology; Climate model; Global warming; Oceanography; Environmental science; General Circulation Model","score_opus":0.035617852055665276,"score_gpt":0.29056128482013105,"score_spread":0.2549434327644658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1987642525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9655209,0.00019721809,0.013701809,0.0010731866,0.00016108296,0.000046442707,0.0031226105,0.0005409141,0.01563573],"genre_scores_gemma":[0.99369955,0.00008595914,0.0032025,0.00013128959,0.000024484454,0.000048395148,0.000880214,0.000044124503,0.0018834787],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998448,0.000051013227,0.000009939809,0.00004634586,0.000019233372,0.000028797718],"domain_scores_gemma":[0.9996561,0.00012357246,0.000038671642,0.000037023303,0.00006886232,0.00007576993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003624271,0.00046249558,0.0005125319,0.0003077111,0.00052017753,0.0011865163,0.0008892243,0.0012400226,0.0020581323],"category_scores_gemma":[0.0014179568,0.00051592645,0.00068396016,0.00056522695,0.000577075,0.00086023484,0.00089837576,0.00082244555,0.00023584849],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006267812,0.000019978868,0.0025114417,0.000009240474,0.0000498111,0.00003412293,0.000017380386,0.9938864,0.0003995042,0.0017942322,0.00052729156,0.00068792404],"study_design_scores_gemma":[0.00005981429,0.000016331993,0.0014472037,0.000002434703,0.00002003117,0.000005314691,0.000010531543,0.9968989,0.000095264,0.0010891241,0.00034346592,0.00001158557],"about_ca_topic_score_codex":0.080853924,"about_ca_topic_score_gemma":0.046472218,"teacher_disagreement_score":0.080853924,"about_ca_system_score_codex":0.001594713,"about_ca_system_score_gemma":0.0012644707,"threshold_uncertainty_score":0.16076666},"labels":[],"label_agreement":null},{"id":"W1988264930","doi":"10.1029/2000gl003745","title":"Eastward convection jet at the poleward boundary of the nightside auroral oval","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Convection; Geology; Geophysics; Convection cell; Jet stream; Substorm; Jet (fluid); Plasma; Physics; Magnetosphere; Meteorology; Combined forced and natural convection; Mechanics","score_opus":0.013389415447690463,"score_gpt":0.27042414532493936,"score_spread":0.2570347298772489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988264930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986149,0.000058194095,0.00013508627,0.000015025297,0.000005357894,0.0000014503343,0.000070178285,0.000009292392,0.0010905558],"genre_scores_gemma":[0.9994885,0.000034356428,0.0000729964,0.00000838088,0.0000047989433,7.1027586e-7,0.00008514691,0.0000013592663,0.00030387336],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997735,0.0000019476324,0.0000012330535,0.000005024838,0.000004995467,0.000009510936],"domain_scores_gemma":[0.9998336,0.00001823534,0.00005084422,0.000010130427,0.000029772735,0.000057275545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000044219123,0.000043561464,0.000085065694,0.00016907282,0.0001513939,0.00031748973,0.0000346437,0.00006222667,0.0010886748],"category_scores_gemma":[0.000190211,0.00004215883,0.000043560798,0.00011885119,0.00014709293,0.00009178639,0.00013480894,0.00011143058,0.00012928987],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008810939,0.000040347517,0.7917054,0.00004880775,0.000041998777,0.0018938658,0.0007599606,0.0011630285,0.17519885,0.0012383474,0.001525208,0.025503088],"study_design_scores_gemma":[0.000009114409,0.000029657294,0.99555993,0.000004505991,0.000003971483,0.00028222607,0.00016141261,0.00054376863,0.0021907706,0.00008002462,0.001131142,0.0000034985296],"about_ca_topic_score_codex":0.0067352913,"about_ca_topic_score_gemma":0.008604123,"teacher_disagreement_score":0.0067352913,"about_ca_system_score_codex":0.00014565173,"about_ca_system_score_gemma":0.00021199913,"threshold_uncertainty_score":0.01339221},"labels":[],"label_agreement":null},{"id":"W1988281801","doi":"10.1029/2007gl032433","title":"Increasing rates of retrogressive thaw slump activity in the Mackenzie Delta region, N.W.T., Canada","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":351,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Aboriginal Affairs Northern Dev Canada; University of British Columbia","funders":"","keywords":"Slump; Slumping; Permafrost; Thermokarst; Global warming; Climate change; Physical geography; Environmental science; Ecosystem; Delta; Terrain; Geology; Hydrology (agriculture); Climatology; Oceanography; Ecology; Geomorphology; Geography; Archaeology","score_opus":0.09554282164283909,"score_gpt":0.31144234167431695,"score_spread":0.21589952003147786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988281801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985812,0.00024825765,0.00003447152,0.00010066692,0.000002174424,0.0000043375753,0.00043068855,0.0000055527667,0.00059265865],"genre_scores_gemma":[0.99843496,0.0003948993,0.00014231657,0.000031560416,0.0000025074878,0.0000036821882,0.00031278803,0.0000017886878,0.00067547074],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991715,0.0000060196003,0.0000063812668,0.000021005882,0.000023395123,0.000026073298],"domain_scores_gemma":[0.9996762,0.00002222427,0.000102794766,0.000012069134,0.00012496024,0.000061688654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013773328,0.00009589973,0.000082058024,0.0009863193,0.0008076009,0.00046596176,0.00028445013,0.0001329822,0.0006848495],"category_scores_gemma":[0.00041369157,0.0001153474,0.00009422026,0.0010049428,0.00036898904,0.00024087518,0.00028946594,0.00021312822,0.000062045765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041451578,0.000009437585,0.9875995,0.000029286095,0.000031825948,0.000118022406,0.0006856324,0.00018766416,0.0014512375,0.00006480844,0.00052916404,0.009251944],"study_design_scores_gemma":[0.0000010588166,0.000002387391,0.99898714,0.000005066191,0.0000035820945,0.000025063648,0.00034919532,0.00010017661,0.00008483824,0.000005877983,0.00043387682,0.0000018376617],"about_ca_topic_score_codex":0.9488902,"about_ca_topic_score_gemma":0.98980135,"teacher_disagreement_score":0.05110979,"about_ca_system_score_codex":0.0056453017,"about_ca_system_score_gemma":0.003072148,"threshold_uncertainty_score":0.10282153},"labels":[],"label_agreement":null},{"id":"W1988443063","doi":"10.1029/2002gl015925","title":"Shear stress at the base of shield lithosphere","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Mantle (geology); Geology; Asthenosphere; Lithosphere; Geophysics; Mantle convection; Anisotropy; Plate tectonics; Stress field; Shield; Shear stress; Seismology; Seismic anisotropy; Tectonics; Mechanics; Petrology; Finite element method; Physics","score_opus":0.039415240848969295,"score_gpt":0.2670615508102298,"score_spread":0.2276463099612605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988443063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99108815,0.00028335565,0.00030737763,0.000080790946,0.000006307586,0.000002572077,0.0005893062,0.000050467068,0.0075916303],"genre_scores_gemma":[0.9992077,0.00009922355,0.000100755344,0.0000070733126,0.0000036238885,6.6848213e-7,0.00018658629,0.0000045458382,0.0003899525],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999063,0.0000030065873,0.0000023005834,0.000016803626,0.000037406437,0.000034140772],"domain_scores_gemma":[0.9998241,0.000012938158,0.000027600743,0.00001216035,0.00007285648,0.00005029732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009378792,0.0003384818,0.00028642477,0.0012040307,0.0006533341,0.00085811125,0.00029844177,0.0002919721,0.001658505],"category_scores_gemma":[0.00037079852,0.00023607977,0.00014713699,0.00067936524,0.00078379386,0.00023010554,0.00042970036,0.00027826565,0.00040592384],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062156783,0.000031516065,0.38572887,0.00012531545,0.00008837222,0.0006305263,0.0015946392,0.009413096,0.56135964,0.007370085,0.0011718224,0.031864617],"study_design_scores_gemma":[0.000010717774,0.00003610511,0.9776928,0.000015863276,0.00001875865,0.0001085434,0.00036710023,0.0021953362,0.017060615,0.0010123356,0.0014501308,0.000031655785],"about_ca_topic_score_codex":0.19663,"about_ca_topic_score_gemma":0.1375963,"teacher_disagreement_score":0.19663,"about_ca_system_score_codex":0.001776214,"about_ca_system_score_gemma":0.0009467085,"threshold_uncertainty_score":0.39097095},"labels":[],"label_agreement":null},{"id":"W1988606067","doi":"10.1029/2007gl030905","title":"Long term fate of anthropogenic carbon","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Environmental science; Atmosphere (unit); Atmospheric sciences; Perturbation (astronomy); Atmosphere of Earth; Term (time); Carbon dioxide; Atmospheric carbon cycle; Climatology; Meteorology; Carbon sequestration; Chemistry; Physics; Geology","score_opus":0.033447368238403115,"score_gpt":0.31990370202932394,"score_spread":0.28645633379092084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1988606067","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963972,0.00010245066,0.00093054964,0.00026560377,0.000020524432,0.000007425656,0.00038971493,0.00003548351,0.0018510955],"genre_scores_gemma":[0.9992306,0.00004514644,0.00015362274,0.000016876878,0.0000031958725,0.0000065091485,0.0001918494,0.0000059937756,0.00034621268],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987185,0.000044391596,0.000005590196,0.0000224312,0.000020515963,0.00003519338],"domain_scores_gemma":[0.99933296,0.0003056276,0.00007737814,0.00006705064,0.00013689463,0.00008004756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005712308,0.0004112445,0.00027255868,0.00023980481,0.00050729554,0.000868386,0.00049173454,0.0010895582,0.0019119022],"category_scores_gemma":[0.001918,0.00026001557,0.00049133366,0.0002934053,0.00049715425,0.0008262572,0.0005877894,0.00054507866,0.00017227531],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004813197,0.0001976557,0.07328051,0.00008486752,0.00024259998,0.0005475296,0.000098506745,0.8975483,0.013992756,0.005893629,0.0011518237,0.0064805127],"study_design_scores_gemma":[0.00006648853,0.00030784908,0.04582194,0.000013172433,0.000056809018,0.000094753814,0.00015894177,0.94392174,0.004299043,0.0039000036,0.0013125547,0.000046705052],"about_ca_topic_score_codex":0.008658991,"about_ca_topic_score_gemma":0.0056704995,"teacher_disagreement_score":0.008658991,"about_ca_system_score_codex":0.0011167363,"about_ca_system_score_gemma":0.0005964558,"threshold_uncertainty_score":0.017217219},"labels":[],"label_agreement":null},{"id":"W1989020994","doi":"10.1029/2007gl030808","title":"Future regional Arctic sea ice declines","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Sea ice; Arctic; Climatology; Arctic ice pack; Bay; Climate change; Oceanography; Climate model; Environmental science; Geology; Physical geography; Geography","score_opus":0.03088210802417794,"score_gpt":0.2947144215328102,"score_spread":0.26383231350863223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989020994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85719603,0.014906175,0.005450703,0.015898151,0.00048809443,0.000038262137,0.009777062,0.00039347578,0.09585207],"genre_scores_gemma":[0.984365,0.003960283,0.0013342845,0.0013095919,0.00023820346,0.00004404737,0.004566424,0.000039292234,0.0041428837],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995253,0.00011253632,0.000034212324,0.00012861124,0.000080056394,0.000119256605],"domain_scores_gemma":[0.998654,0.00017265823,0.00038532921,0.00010073659,0.00056210154,0.0001250053],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022021134,0.00040941307,0.0003322642,0.0007154949,0.00048921176,0.0012653141,0.0005531133,0.0007040882,0.0074024214],"category_scores_gemma":[0.003025589,0.00012415762,0.0006253461,0.000766955,0.00035384062,0.0016305657,0.00069162453,0.0007893088,0.0014357222],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072880083,0.00016259216,0.6991003,0.0005887073,0.00050581014,0.0007878856,0.0015653465,0.030229459,0.004234426,0.019750783,0.04571327,0.19663267],"study_design_scores_gemma":[0.00005224639,0.00046962622,0.8447157,0.00035235708,0.000269894,0.0012579858,0.002337691,0.013772747,0.0022244044,0.0093003465,0.12519391,0.000053012503],"about_ca_topic_score_codex":0.01013797,"about_ca_topic_score_gemma":0.014733174,"teacher_disagreement_score":0.01013797,"about_ca_system_score_codex":0.0011230819,"about_ca_system_score_gemma":0.0007432381,"threshold_uncertainty_score":0.024763584},"labels":[],"label_agreement":null},{"id":"W1989084221","doi":"10.1029/2005gl023344","title":"Response of the ocean, climate and terrestrial carbon cycle to Holocene freshwater discharge after 8 kyr BP","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Meltwater; Geology; Climatology; Holocene; Oceanography; Thermohaline circulation; Carbon cycle; Paleoclimatology; Northern Hemisphere; Radiative forcing; North Atlantic Deep Water; Sea ice; Ice sheet; Climate change; Environmental science; Glacial period; Paleontology","score_opus":0.018539684357621843,"score_gpt":0.27613330455018176,"score_spread":0.25759362019255994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989084221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99717605,0.000052515614,0.00018717548,0.00018900925,0.000023942948,0.0000064023925,0.0011506291,0.000082915125,0.0011313931],"genre_scores_gemma":[0.99791235,0.000037362544,0.00015958487,0.000049449583,0.0000056450713,0.000010476051,0.0013740477,0.000022262524,0.0004287945],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99988973,0.000020529444,0.000005374341,0.00003248002,0.000010836276,0.000041079864],"domain_scores_gemma":[0.9997639,0.000057094425,0.00002627978,0.0000187168,0.00004007093,0.000093868686],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025173798,0.0006057838,0.00041065138,0.00023509233,0.00044130802,0.0007398472,0.00086740387,0.0009983273,0.0028321014],"category_scores_gemma":[0.0011106736,0.00038894833,0.000568635,0.00028621673,0.00045932186,0.00044694077,0.00051813823,0.0009215719,0.0003094787],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018819899,0.00023510428,0.17896093,0.00010551811,0.0005257523,0.0008638963,0.00015724372,0.78446287,0.020596828,0.001600455,0.004530479,0.00607891],"study_design_scores_gemma":[0.00043328688,0.00033888654,0.24512887,0.0000331127,0.00015138999,0.00012486667,0.00017986358,0.745606,0.0049375435,0.0008666093,0.0021187037,0.000080873644],"about_ca_topic_score_codex":0.104709655,"about_ca_topic_score_gemma":0.06204837,"teacher_disagreement_score":0.104709655,"about_ca_system_score_codex":0.002112593,"about_ca_system_score_gemma":0.000917727,"threshold_uncertainty_score":0.20820034},"labels":[],"label_agreement":null},{"id":"W1989235867","doi":"10.1002/2014gl062767","title":"InSAR imaging of displacement on flexural‐slip faults triggered by the 2013 <i>Mw</i> 6.6 Lake Grassmere earthquake, central New Zealand","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"New Zealand Government","keywords":"Slip (aerodynamics); Geology; Interferometric synthetic aperture radar; Seismology; Episodic tremor and slip; Epicenter; Flexural strength; Synthetic aperture radar; Subduction; Tectonics; Remote sensing","score_opus":0.04101361224465221,"score_gpt":0.2871871244287047,"score_spread":0.24617351218405248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989235867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976356,0.000043212553,0.0001339833,0.000035595163,0.0000049606383,0.0000073249535,0.00067120156,0.000019179603,0.0014489247],"genre_scores_gemma":[0.9982856,0.00007061515,0.0004337566,0.00001679435,0.000004804445,0.000004411456,0.00061874243,0.000004966673,0.0005604046],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994385,0.0000027699075,0.000003120659,0.000012424262,0.000021078426,0.000016805603],"domain_scores_gemma":[0.9998325,0.00000954727,0.00006186386,0.000011123528,0.00004554648,0.00003936186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012210669,0.0002050769,0.00016861994,0.0006783712,0.0003552237,0.0004078547,0.00020800345,0.0002190002,0.0010897851],"category_scores_gemma":[0.00030167145,0.00022481901,0.000107796805,0.00056256703,0.0003292305,0.00024911185,0.00037515792,0.00020621651,0.00021012158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078985107,0.00016778988,0.72829694,0.00013305705,0.000112566755,0.001348575,0.0017635663,0.0037241015,0.2254984,0.00025793587,0.003520779,0.03438638],"study_design_scores_gemma":[0.000012117486,0.000022836331,0.99664956,0.00000556491,0.000013896767,0.000059113754,0.00019394136,0.0012537024,0.0012342108,0.000016370444,0.0005324697,0.0000062190984],"about_ca_topic_score_codex":0.13687602,"about_ca_topic_score_gemma":0.27976263,"teacher_disagreement_score":0.13687602,"about_ca_system_score_codex":0.0006145627,"about_ca_system_score_gemma":0.00037918641,"threshold_uncertainty_score":0.27215862},"labels":[],"label_agreement":null},{"id":"W1989364707","doi":"10.1029/2004gl020876","title":"Detecting the effect of climate change on Canadian forest fires","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":766,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Forest Service; Pacific Institute for Climate Solutions; University of Victoria","funders":"","keywords":"Environmental science; Climate change; Greenhouse gas; Ecosystem; Aerosol; Atmospheric sciences; Sulfate aerosol; Global warming; Forest ecology; Greenhouse effect; Carbon dioxide; Terrestrial ecosystem; Climatology; Ecology; Meteorology; Geography; Geology","score_opus":0.018974234079017584,"score_gpt":0.27726071256160395,"score_spread":0.25828647848258635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989364707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941209,0.00014621744,0.00075318565,0.00014754663,0.00001029226,0.000008882473,0.0022949537,0.00008263366,0.002435352],"genre_scores_gemma":[0.99744785,0.000111704794,0.0008483162,0.00002562273,0.0000040028776,0.0000029280543,0.0012367093,0.000008052637,0.00031487131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974805,0.000029377035,0.000008552564,0.000057621426,0.00008017456,0.00007611573],"domain_scores_gemma":[0.9993586,0.00014846609,0.00008210226,0.000035354777,0.00027100145,0.00010445536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046526807,0.0004195937,0.00023877768,0.000573436,0.00098964,0.0009754262,0.00040572614,0.00042244725,0.0010335221],"category_scores_gemma":[0.0021890367,0.0002384178,0.00038583679,0.0009116143,0.00029953665,0.00031425396,0.00046070997,0.00038484548,0.0001065297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025956138,0.000058594633,0.9263071,0.000045762852,0.00023886978,0.000061859355,0.00012600621,0.052495617,0.004075418,0.00049263984,0.0013182053,0.014520339],"study_design_scores_gemma":[0.000023778663,0.00002666006,0.912951,0.000013148842,0.00008816622,0.000029861496,0.00027096443,0.082677186,0.0021597533,0.00027492142,0.0014532985,0.00003124391],"about_ca_topic_score_codex":0.97128737,"about_ca_topic_score_gemma":0.98198706,"teacher_disagreement_score":0.02871263,"about_ca_system_score_codex":0.008365026,"about_ca_system_score_gemma":0.0065202997,"threshold_uncertainty_score":0.060692728},"labels":[],"label_agreement":null},{"id":"W1989416203","doi":"10.1029/2008gl035680","title":"Evidence of the cloud lifetime effect from wildfire‐induced thunderstorms","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Cloud condensation nuclei; Thunderstorm; Cirrus; Atmospheric sciences; Environmental science; Convection; Effective radius; Aerosol; Cloud computing; Ice crystals; Meteorology; Climate change; Cloud physics; Smoke; RADIUS; Condensation; Climatology; Geology; Geography; Physics; Astrophysics","score_opus":0.04721253339305635,"score_gpt":0.29440247673605996,"score_spread":0.2471899433430036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1989416203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955336,0.00028852903,0.0003713036,0.000057698708,0.0000057752513,0.00001211646,0.00022333379,0.000013493408,0.0034940795],"genre_scores_gemma":[0.99925905,0.00015513322,0.00014029027,0.000017149205,0.0000068613667,0.0000017961939,0.00010079321,0.0000036577487,0.00031518628],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997876,0.000036154346,0.000007471594,0.000024665236,0.00007543575,0.00006861851],"domain_scores_gemma":[0.9964695,0.0016406456,0.00071779324,0.00026606338,0.0006488037,0.0002571167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061950734,0.00019964993,0.00014446814,0.00038619313,0.0007223375,0.00043929697,0.00032768206,0.0003126486,0.001801593],"category_scores_gemma":[0.0023197543,0.000107429034,0.00020904547,0.0003745447,0.0006163133,0.00025691112,0.00032481004,0.0003461168,0.00010357325],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009571439,0.00020402484,0.93413407,0.00015014566,0.00017844817,0.0011085912,0.0006520065,0.006382718,0.023100277,0.0008151947,0.00071231736,0.031605028],"study_design_scores_gemma":[0.000013486199,0.0002239977,0.9913863,0.000012330371,0.000064993255,0.0004027263,0.00032950568,0.0018843208,0.004422016,0.0002022009,0.0010457159,0.000012499511],"about_ca_topic_score_codex":0.17164044,"about_ca_topic_score_gemma":0.28013715,"teacher_disagreement_score":0.17164044,"about_ca_system_score_codex":0.0014272749,"about_ca_system_score_gemma":0.0007902002,"threshold_uncertainty_score":0.34128278},"labels":[],"label_agreement":null},{"id":"W1990277017","doi":"10.1002/2014gl060630","title":"Seismic evidence for rotating mantle flow around subducting slab edge associated with oceanic microplate capture","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Geology; Subduction; Slab; Seismology; Mantle (geology); Slab window; Buoyancy; Mantle wedge; Geophysics; Oceanic crust; Transition zone; Plate tectonics; Shear wave splitting; Clockwise; Tectonics; Geometry; Mechanics; Physics","score_opus":0.04839631582163823,"score_gpt":0.29123385269863616,"score_spread":0.24283753687699794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990277017","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992423,0.00002855215,0.00016631061,0.000016824239,0.0000011021378,0.0000014583142,0.00006466128,0.000011359512,0.0004674456],"genre_scores_gemma":[0.99968946,0.000017688559,0.00009334548,0.000005945518,0.0000025021743,0.0000015956,0.00008656145,0.0000017337395,0.00010122587],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999286,0.000008521442,0.0000047843646,0.000022871163,0.000015899788,0.000019352725],"domain_scores_gemma":[0.9995357,0.00004419409,0.00020265715,0.000051185973,0.00007618829,0.00009011485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015859932,0.0001934624,0.00015289643,0.00095477764,0.0002731307,0.00034199058,0.00028871238,0.00027000767,0.0014998277],"category_scores_gemma":[0.00045936828,0.00022199984,0.00011964055,0.0005908864,0.0004263001,0.00018984498,0.0005191143,0.00017935825,0.00016784179],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025240463,0.00003849935,0.8468571,0.00002662061,0.000041330724,0.00043688517,0.00072854577,0.00030703947,0.14592448,0.00015425123,0.0001131699,0.005119597],"study_design_scores_gemma":[0.0000023381479,0.000017515866,0.99821705,0.000002303086,0.000005926567,0.00007822923,0.0001711105,0.00022755121,0.0011759665,0.00003102857,0.00006794879,0.0000029457453],"about_ca_topic_score_codex":0.0052196006,"about_ca_topic_score_gemma":0.0058109807,"teacher_disagreement_score":0.0052196006,"about_ca_system_score_codex":0.00017381442,"about_ca_system_score_gemma":0.00013775231,"threshold_uncertainty_score":0.01037848},"labels":[],"label_agreement":null},{"id":"W1990520590","doi":"10.1029/2008gl035338","title":"Structure of Titan's low altitude ionized layer from the Relaxation Probe onboard HUYGENS","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Royal Military College of Canada","funders":"","keywords":"Ionosphere; Titan (rocket family); Electron; Ion; Ionization; Atmosphere of Titan; Physics; Altitude (triangle); Atmosphere (unit); Computational physics; Atmospheric sciences; Atomic physics; Geophysics; Meteorology; Astrobiology","score_opus":0.028144875285039058,"score_gpt":0.2767821854900879,"score_spread":0.2486373102050488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990520590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953957,0.00016390198,0.0009252566,0.00010541171,0.0000063141074,0.0000046858295,0.00028788362,0.0000738407,0.0030369519],"genre_scores_gemma":[0.99808335,0.000045710178,0.00090672675,0.00003632643,0.0000050490967,0.0000027319286,0.0002838625,0.0000149912275,0.00062127196],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999671,0.0000030752217,8.4507656e-7,0.00000951131,0.000009550485,0.0000098963865],"domain_scores_gemma":[0.999925,0.00001657064,0.000015593778,0.0000065733925,0.00002180277,0.000014345619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009085531,0.00011178348,0.00011275006,0.00038039297,0.00027285947,0.00040401865,0.00030841833,0.0002010404,0.0011855226],"category_scores_gemma":[0.00023299898,0.000104933504,0.00008153495,0.00031685262,0.00023554015,0.00026961765,0.0002906085,0.00022544536,0.00019171006],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004892584,0.00007880034,0.08593952,0.0000846327,0.00005475325,0.00088568166,0.0011888741,0.002193072,0.8827578,0.0018514981,0.0012152159,0.023260973],"study_design_scores_gemma":[0.00004821713,0.00015108699,0.8900738,0.00002106354,0.00005612939,0.00046238524,0.00048836286,0.025446933,0.078280725,0.0006353621,0.0042954297,0.00004038351],"about_ca_topic_score_codex":0.0073118783,"about_ca_topic_score_gemma":0.0063128034,"teacher_disagreement_score":0.0073118783,"about_ca_system_score_codex":0.0003548916,"about_ca_system_score_gemma":0.00018189441,"threshold_uncertainty_score":0.014538646},"labels":[],"label_agreement":null},{"id":"W1990557554","doi":"10.1029/1999gl011025","title":"Cl and Br atom concentrations during a surface boundary layer ozone depletion event in the Canadian High Arctic","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Bromine; Halogen; Mixing ratio; Hydrocarbon; Chemistry; Ozone depletion; Ozone; Atom (system on chip); Analytical Chemistry (journal); Mercury (programming language); Environmental chemistry; Physical chemistry; Organic chemistry","score_opus":0.019744277369721557,"score_gpt":0.2575834011166209,"score_spread":0.23783912374689936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990557554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851006,0.000086873326,0.00006744468,0.000044291704,0.000005132479,0.0000102490585,0.0004476814,0.000009113398,0.0008190127],"genre_scores_gemma":[0.99779737,0.000106238665,0.00023819024,0.00004314362,0.000004255443,0.000008901797,0.00073539634,0.000004649239,0.0010618927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973446,0.000012657045,0.0000067053434,0.00005672824,0.00011202666,0.00007742356],"domain_scores_gemma":[0.99955803,0.000030464738,0.000040773983,0.000008824613,0.00026346245,0.0000984169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026862367,0.00041309002,0.0003877379,0.00089946226,0.0030285013,0.0009393973,0.00071200484,0.0005701173,0.0006266888],"category_scores_gemma":[0.0005333697,0.00033358872,0.00021195081,0.00089331326,0.00058114674,0.0002590861,0.0003857533,0.0004152245,0.000092318165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001130417,0.00021726558,0.9137097,0.00010174694,0.00019809931,0.0007909511,0.0043328437,0.0014334633,0.06308256,0.00017968558,0.0012790321,0.013544127],"study_design_scores_gemma":[0.000012705913,0.000055796772,0.9941257,0.000008221207,0.000032059885,0.000042403844,0.0008874396,0.0010628921,0.0026315732,0.000020615475,0.0011018348,0.000018823197],"about_ca_topic_score_codex":0.9770213,"about_ca_topic_score_gemma":0.989175,"teacher_disagreement_score":0.022978723,"about_ca_system_score_codex":0.012248599,"about_ca_system_score_gemma":0.006906248,"threshold_uncertainty_score":0.08887029},"labels":[],"label_agreement":null},{"id":"W1990724596","doi":"10.1029/2009gl037617","title":"Stratospheric ozone during the Last Glacial Maximum","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Stratosphere; Atmospheric sciences; Environmental science; Ozone layer; Ozone; Atmosphere (unit); Climatology; Troposphere; Ozone depletion; Middle latitudes; Geology; Meteorology; Geography","score_opus":0.019679423905451895,"score_gpt":0.26515337793681987,"score_spread":0.24547395403136796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1990724596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970637,0.0001607776,0.0001138401,0.0001682454,0.000014475435,0.0000023958212,0.0005323624,0.00003441805,0.0019097448],"genre_scores_gemma":[0.99920386,0.00007018171,0.000046543213,0.000025865333,0.0000047670565,0.000003236997,0.00040158784,0.000006162185,0.00023786927],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993587,0.00001920521,0.000001792231,0.000011352988,0.0000059995964,0.000025773092],"domain_scores_gemma":[0.9999143,0.000025210904,0.000015621416,0.000008355515,0.000010408836,0.00002615182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023421284,0.0002973163,0.00029434948,0.00022799135,0.00040633924,0.00067640113,0.00029206398,0.0006806484,0.0013160902],"category_scores_gemma":[0.0005340277,0.0002237393,0.0006066712,0.0003956636,0.00025337416,0.00030995437,0.00036189993,0.00037221858,0.00014499326],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001127743,0.00018067994,0.40481058,0.00019937877,0.00082720676,0.0007853253,0.00042069843,0.5557186,0.017047454,0.004684097,0.005364506,0.0088337045],"study_design_scores_gemma":[0.00045654597,0.00039792404,0.72943366,0.00006985573,0.00042658378,0.00020589387,0.00044736775,0.257404,0.003411437,0.002364132,0.0053167115,0.000065965665],"about_ca_topic_score_codex":0.04761618,"about_ca_topic_score_gemma":0.030819999,"teacher_disagreement_score":0.04761618,"about_ca_system_score_codex":0.0009771037,"about_ca_system_score_gemma":0.0005551187,"threshold_uncertainty_score":0.094678044},"labels":[],"label_agreement":null},{"id":"W1991121218","doi":"10.1029/2003gl017586","title":"Distribution of the Pacific/North America motion in the Queen Charlotte Islands‐S. Alaska plate boundary zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Pacific Plate; Seismology; North American Plate; Plate tectonics; Sinistral and dextral; Transform fault; Tectonics; Subduction; Oceanography","score_opus":0.020973258896008862,"score_gpt":0.24964086480731607,"score_spread":0.2286676059113072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991121218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99839145,0.00014686924,0.00003078899,0.000017315122,0.0000011884524,0.0000017752291,0.00020080045,0.0000045665565,0.0012051687],"genre_scores_gemma":[0.9992099,0.000102924816,0.00007101104,0.0000048132697,0.0000011636478,0.0000027426597,0.0002548038,0.0000012451443,0.00035142305],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998903,0.000012663969,0.0000099229665,0.000034208537,0.000024962068,0.000028016562],"domain_scores_gemma":[0.9993303,0.00007852214,0.00019881445,0.000042328185,0.0002184368,0.00013158037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018974383,0.00009976208,0.00011678162,0.0012788001,0.0006566294,0.00061374943,0.0002043385,0.0001681601,0.0011049465],"category_scores_gemma":[0.00081603206,0.00013296913,0.00008921422,0.001011246,0.00045500524,0.00017438346,0.000411552,0.00011688924,0.0001704791],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013112627,0.000009366691,0.9821562,0.000027507904,0.00003483834,0.00020901648,0.0015005977,0.0011408132,0.0031394842,0.00018145436,0.00045016775,0.011019307],"study_design_scores_gemma":[0.0000031150887,0.000008879175,0.99825984,0.0000106145635,0.0000070263773,0.00005603618,0.00045746434,0.00048329134,0.00014120959,0.000015793104,0.0005510093,0.0000057991083],"about_ca_topic_score_codex":0.614911,"about_ca_topic_score_gemma":0.77607244,"teacher_disagreement_score":0.38508898,"about_ca_system_score_codex":0.0017691347,"about_ca_system_score_gemma":0.0009735711,"threshold_uncertainty_score":0.7747137},"labels":[],"label_agreement":null},{"id":"W1991170456","doi":"10.1029/2007gl031304","title":"Younger Dryas: A data to model comparison to constrain the strength of the overturning circulation","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Younger Dryas; Geology; Radiocarbon dating; Oceanography; Foraminifera; Climatology; Thermohaline circulation; Stadial; Ocean current; Varve; Benthic zone; Climate change; Holocene; Paleontology","score_opus":0.12329840702306129,"score_gpt":0.36548594750791363,"score_spread":0.24218754048485236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991170456","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98693997,0.000054656088,0.001546761,0.00011213503,0.000022581484,0.00005170886,0.008833614,0.0002454541,0.0021931597],"genre_scores_gemma":[0.98796964,0.00005392232,0.0024758952,0.000036173984,0.000010240386,0.00008020332,0.0087267775,0.00012726201,0.0005198203],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998467,0.000045705336,0.000010361159,0.000049764025,0.000018021874,0.00002950235],"domain_scores_gemma":[0.9991831,0.0003308216,0.00013576323,0.00011064937,0.00013705002,0.000102453756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009611113,0.0005844741,0.000515292,0.0004680233,0.00045035782,0.0005692542,0.0009629573,0.00042747735,0.00161025],"category_scores_gemma":[0.0017007062,0.00028171882,0.0007272644,0.0005819158,0.00022266271,0.0005098665,0.0003732101,0.00047078962,0.00025633568],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017255355,0.00048371992,0.1694946,0.00016292086,0.0005552645,0.00019908513,0.00024661975,0.7986029,0.0062610065,0.0017398902,0.0047501014,0.015778363],"study_design_scores_gemma":[0.001079193,0.00030946598,0.13418369,0.00002500532,0.00017394734,0.000067855646,0.00016239718,0.85178024,0.0051167086,0.0007379212,0.006308345,0.00005521314],"about_ca_topic_score_codex":0.10376058,"about_ca_topic_score_gemma":0.07256683,"teacher_disagreement_score":0.10376058,"about_ca_system_score_codex":0.0014945057,"about_ca_system_score_gemma":0.0010648597,"threshold_uncertainty_score":0.20631325},"labels":[],"label_agreement":null},{"id":"W1991296426","doi":"10.1002/2014gl060595","title":"Spatiotemporal analysis and interpretation of 1993–2013 ground deformation at Campi Flegrei, Italy, observed by advanced DInSAR","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Natural Resources Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Caldera; Volcano; Seismology; Geodesy; Subsidence; Interferometric synthetic aperture radar; Deformation (meteorology); Synthetic aperture radar; Remote sensing; Geomorphology; Structural basin","score_opus":0.014300225060125913,"score_gpt":0.26465939281690853,"score_spread":0.25035916775678263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991296426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950041,0.00009981516,0.00063270336,0.00008529782,0.000007894482,0.000015193101,0.0019772048,0.00008484972,0.0020928953],"genre_scores_gemma":[0.99649954,0.000045595792,0.0009126149,0.000010992327,0.000008601784,0.0000075441376,0.0022056268,0.00000731507,0.00030225242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999081,0.000009944165,0.0000042823153,0.000031815198,0.000021086276,0.000024703213],"domain_scores_gemma":[0.9998399,0.00002173032,0.000045058227,0.000029099907,0.000036858037,0.000027352506],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028618018,0.00032383914,0.0001637986,0.0011058379,0.00020263926,0.00040852284,0.0002645411,0.000273336,0.00070016476],"category_scores_gemma":[0.00034935583,0.00011478234,0.00023999259,0.000815872,0.00024135725,0.000199284,0.00025819516,0.00018916558,0.00018667609],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005758191,0.00040682114,0.7742426,0.00021168559,0.00034606902,0.0014429558,0.0009306592,0.07997789,0.041423872,0.0009832814,0.009978842,0.08947959],"study_design_scores_gemma":[0.000012992498,0.000029014262,0.97795576,0.000011989186,0.000020098394,0.00008521083,0.000092596085,0.019193318,0.0008633589,0.00003927576,0.0016837716,0.000012660628],"about_ca_topic_score_codex":0.06153053,"about_ca_topic_score_gemma":0.0992857,"teacher_disagreement_score":0.06153053,"about_ca_system_score_codex":0.00086833665,"about_ca_system_score_gemma":0.00036204554,"threshold_uncertainty_score":0.12234479},"labels":[],"label_agreement":null},{"id":"W1991373191","doi":"10.1029/2004gl021189","title":"The spectrum of waves and turbulence at the tropopause","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; Dalhousie University","funders":"","keywords":"Turbulence; Turbulence kinetic energy; Wavelength; Tropopause; Physics; Kinetic energy; Equipartition theorem; Altitude (triangle); Gravity wave; Atmospheric sciences; Wave turbulence; Spectral line; Gravitational wave; Troposphere; Computational physics; Meteorology; Geology; Optics; Astrophysics; Classical mechanics; Geometry; Astronomy; Magnetic field","score_opus":0.01385861705243659,"score_gpt":0.27087341347531224,"score_spread":0.25701479642287567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991373191","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989097,0.000055071978,0.00011555374,0.000014021427,0.0000012328524,0.0000012810285,0.000059796836,0.0000021664773,0.0008411806],"genre_scores_gemma":[0.99951303,0.000044692668,0.00008890682,0.0000042893967,0.0000021158576,0.000001092527,0.000100504614,0.0000014598686,0.00024380375],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997437,0.000003010436,9.951934e-7,0.000004856853,0.000007508265,0.000009339234],"domain_scores_gemma":[0.99993336,0.000011781962,0.000015135655,0.0000040518653,0.000013962169,0.000021772823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061241255,0.000075114214,0.00006189513,0.00032282222,0.00013225985,0.0001896655,0.000061141465,0.00010476293,0.0007361552],"category_scores_gemma":[0.00016868266,0.000089621295,0.000047421312,0.00021510113,0.00014236219,0.00013718173,0.0001655009,0.00012493944,0.00011557245],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006895189,0.000067508416,0.46940288,0.00006096708,0.000040924297,0.00108493,0.0011715775,0.0009727513,0.5002048,0.0016652666,0.0005818199,0.024057036],"study_design_scores_gemma":[0.000005412266,0.00003721874,0.99527705,0.000003851805,0.0000032607488,0.00019457606,0.00012853763,0.0006335554,0.003249104,0.00014052702,0.00032248508,0.0000044542935],"about_ca_topic_score_codex":0.0027229022,"about_ca_topic_score_gemma":0.0042998227,"teacher_disagreement_score":0.0027229022,"about_ca_system_score_codex":0.00015133862,"about_ca_system_score_gemma":0.000066069784,"threshold_uncertainty_score":0.0054141283},"labels":[],"label_agreement":null},{"id":"W1991431973","doi":"10.1029/2007gl030903","title":"Energy exchange rate for the equatorial electrojet: Test of the model of two‐stream processes that includes thermal corrections","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Energy exchange; Electrojet; Thermal; Environmental science; Geophysics; Atmospheric sciences; Energy (signal processing); Geology; Meteorology; Physics","score_opus":0.030310582679584308,"score_gpt":0.30203872453773833,"score_spread":0.271728141858154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991431973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98395455,0.00029686734,0.012622796,0.0002122443,0.000038306283,0.000014669106,0.00006230332,0.00008119021,0.0027169497],"genre_scores_gemma":[0.99844754,0.00011562415,0.00066965655,0.000012111339,0.000010409051,0.0000063627917,0.000038223203,0.0000191803,0.00068088586],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983656,0.000033303524,0.0000092116925,0.000040497333,0.000036747915,0.000043734388],"domain_scores_gemma":[0.99767214,0.0015890619,0.00028650547,0.0002489775,0.00012980711,0.00007356273],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012530443,0.0004877095,0.00051883777,0.0005746594,0.00031792955,0.0007587449,0.00097050064,0.00068337505,0.0023274878],"category_scores_gemma":[0.0046768654,0.00036085103,0.0006714697,0.0004298997,0.0007447288,0.0016453745,0.0007589379,0.0006005641,0.0003279546],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038021088,0.00061251834,0.11193118,0.000326333,0.00027794615,0.0017537592,0.00065818836,0.6491223,0.04806921,0.13834232,0.0016171094,0.043487076],"study_design_scores_gemma":[0.00015491794,0.00013086718,0.015247582,0.000005759501,0.000035394427,0.00027790054,0.000049138795,0.96918386,0.0057970206,0.008776369,0.00031075752,0.000030477006],"about_ca_topic_score_codex":0.002517848,"about_ca_topic_score_gemma":0.0003918968,"teacher_disagreement_score":0.002517848,"about_ca_system_score_codex":0.0005838464,"about_ca_system_score_gemma":0.00034810594,"threshold_uncertainty_score":0.007786274},"labels":[],"label_agreement":null},{"id":"W1991448376","doi":"10.1029/2009gl037681","title":"Sea ice conditions and melt season duration variability within the Canadian Arctic Archipelago: 1979–2008","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Arctic; Archipelago; Sea ice; Arctic ice pack; Climatology; Oceanography; Arctic sea ice decline; Environmental science; Geology; Antarctic sea ice","score_opus":0.018125597236430747,"score_gpt":0.2614747578640724,"score_spread":0.24334916062764167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991448376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943809,0.00027067884,0.000036658857,0.000046940633,0.0000047934536,0.0000074469385,0.0041378313,0.0000063075254,0.0011085403],"genre_scores_gemma":[0.994132,0.00028577377,0.0001242903,0.000022162476,0.0000052219734,0.000008605098,0.004675714,0.0000027729725,0.000743495],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998312,0.0000051924667,0.000009909576,0.00003469052,0.000067521745,0.00005142646],"domain_scores_gemma":[0.9992176,0.0000376892,0.00011485533,0.000018160348,0.00048542337,0.0001262544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025357405,0.00023130611,0.0002115091,0.0016440457,0.0011349343,0.000622988,0.00045695886,0.0002136943,0.0007809422],"category_scores_gemma":[0.00075079355,0.00014121865,0.00026295212,0.0025490485,0.00034315456,0.0002467807,0.00030186423,0.0002796897,0.00012610284],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000098404016,0.000017494502,0.99225396,0.000021573698,0.00007100562,0.000058087662,0.00038277873,0.00023219094,0.00087460637,0.000043406188,0.00076450175,0.005182035],"study_design_scores_gemma":[6.1550367e-7,0.000003924377,0.9992586,0.00000299092,0.0000073052697,0.000014378202,0.00013203501,0.00008352134,0.000058761576,0.000002352497,0.0004335213,0.000002096173],"about_ca_topic_score_codex":0.97190136,"about_ca_topic_score_gemma":0.99000823,"teacher_disagreement_score":0.028098643,"about_ca_system_score_codex":0.006486554,"about_ca_system_score_gemma":0.005622539,"threshold_uncertainty_score":0.05652821},"labels":[],"label_agreement":null},{"id":"W1991862329","doi":"10.1029/2004gl021157","title":"Ebullition of methane‐containing gas bubbles from near‐surface <i>Sphagnum</i> peat","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Peat; Bog; Sphagnum; Methane; Atmosphere (unit); Environmental chemistry; Wetland; Environmental science; Hydrology (agriculture); Geology; Soil science; Chemistry; Ecology; Physics","score_opus":0.024475136469173722,"score_gpt":0.2873925762121681,"score_spread":0.2629174397429944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991862329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958056,0.000042475156,0.00026041674,0.000002889492,0.0000014557282,0.0000024279345,0.000022708313,0.000004923162,0.00008217612],"genre_scores_gemma":[0.998061,0.000070705304,0.0014677856,0.00000794734,0.0000029216008,0.0000070734613,0.000120971235,0.0000075198577,0.0002540411],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998666,0.000018455601,0.000008797586,0.000037519385,0.000033182874,0.000035416324],"domain_scores_gemma":[0.9997004,0.00010205206,0.00007305305,0.00002149108,0.000045997498,0.000056948436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029923182,0.00021364604,0.00026937333,0.00021289039,0.00022387289,0.00027146915,0.00018101912,0.00020131162,0.00022293291],"category_scores_gemma":[0.0006230352,0.00015953073,0.00015283449,0.00010250277,0.00031576757,0.00029669222,0.00031678766,0.00026137315,0.00006917696],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025830648,0.000023437962,0.035020076,0.00004807406,0.000017341405,0.00011073522,0.00021271638,0.0006372439,0.95950514,0.000028397286,0.000016481972,0.0041220067],"study_design_scores_gemma":[0.00001885121,0.00041707832,0.37257618,0.000021682119,0.000039550836,0.0002630894,0.000286139,0.009562285,0.61600024,0.00013041096,0.00065740896,0.000027027743],"about_ca_topic_score_codex":0.0027995887,"about_ca_topic_score_gemma":0.0034982534,"teacher_disagreement_score":0.0027995887,"about_ca_system_score_codex":0.00018014906,"about_ca_system_score_gemma":0.00014168372,"threshold_uncertainty_score":0.0055665374},"labels":[],"label_agreement":null},{"id":"W1991870655","doi":"10.1029/2004gl020040","title":"On the relationship between Tibetan snow cover, the Tibetan plateau monsoon and the Indian summer monsoon","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Monsoon; Plateau (mathematics); Climatology; East Asian Monsoon; Snow cover; Snow; Monsoon of South Asia; Physical geography; Geology; Geography; Meteorology","score_opus":0.08547123988394227,"score_gpt":0.32013891089750107,"score_spread":0.2346676710135588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1991870655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968466,0.00064742926,0.00022881584,0.00017756477,0.000005665564,0.0000020635368,0.00010470789,0.0000043805267,0.0019826521],"genre_scores_gemma":[0.99921274,0.0003405034,0.000086454675,0.000018067649,0.000020258267,0.0000010863947,0.00008825355,0.0000015153327,0.00023109547],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998801,0.000050629085,0.000005337192,0.000013366115,0.000016018306,0.000034637276],"domain_scores_gemma":[0.99928135,0.00040001312,0.00016899519,0.000022538388,0.00005591972,0.000071199494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000511073,0.00016465281,0.00014822325,0.00075313606,0.00033602313,0.0007834216,0.00018688463,0.00019806952,0.0013444743],"category_scores_gemma":[0.00145946,0.0001036856,0.00017091662,0.0015673984,0.0005151429,0.00032779144,0.0002918132,0.00019649285,0.00012780975],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002658492,0.000026236772,0.97913396,0.00003814582,0.00014357486,0.0004969863,0.00031583535,0.005187015,0.002147709,0.0016262556,0.00022464682,0.010393712],"study_design_scores_gemma":[0.000006418214,0.00005659694,0.99060565,0.000011625177,0.0000317846,0.000080267055,0.0003793806,0.0069071143,0.0001104426,0.0013796883,0.00042395154,0.00000703555],"about_ca_topic_score_codex":0.022997444,"about_ca_topic_score_gemma":0.03719095,"teacher_disagreement_score":0.022997444,"about_ca_system_score_codex":0.0003628076,"about_ca_system_score_gemma":0.00045474878,"threshold_uncertainty_score":0.045727134},"labels":[],"label_agreement":null},{"id":"W1992383389","doi":"10.1029/2007gl031252","title":"Viscous relaxation on early Mars: A study of ancient impact basins","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Martian; Mars Exploration Program; Geology; Martian surface; Geophysics; Lithosphere; Planet; Astrobiology; Tectonics; Paleontology; Physics","score_opus":0.0416610710592363,"score_gpt":0.34354006390883013,"score_spread":0.30187899284959385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992383389","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960095,0.000075192846,0.00006646062,0.0000096989315,3.3394795e-7,0.0000011150256,0.00001646565,0.0000024204126,0.00022739885],"genre_scores_gemma":[0.9996111,0.00009912654,0.00012906227,0.000004874482,0.0000028906084,0.000001850748,0.000062748775,0.000002398557,0.000085990745],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999448,0.00001273878,0.0000037331488,0.000012077639,0.00000954938,0.000017104783],"domain_scores_gemma":[0.99984777,0.00003558558,0.00004549191,0.000017687213,0.0000179157,0.000035531324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015484559,0.00016314424,0.00021506831,0.0008901351,0.00055478147,0.0004339193,0.00030375924,0.00027313043,0.00061369],"category_scores_gemma":[0.000618775,0.00018265356,0.00024747485,0.00078521535,0.00040594762,0.00031191294,0.0004618862,0.0002493913,0.000094609015],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005261076,0.00038292797,0.84719604,0.00022816595,0.0003762176,0.0026397498,0.0049774237,0.016228514,0.06826732,0.0018671828,0.0006102626,0.0567],"study_design_scores_gemma":[0.000008615195,0.000078463825,0.99124616,0.0000072808098,0.000027059283,0.00034289472,0.0004165281,0.0058689797,0.00080028985,0.00027295412,0.00092090527,0.000009792001],"about_ca_topic_score_codex":0.004244845,"about_ca_topic_score_gemma":0.0032535938,"teacher_disagreement_score":0.004244845,"about_ca_system_score_codex":0.0003045799,"about_ca_system_score_gemma":0.00010859971,"threshold_uncertainty_score":0.008440256},"labels":[],"label_agreement":null},{"id":"W1992660544","doi":"10.1029/2009gl041282","title":"El Niño stills winter winds across the southern Canadian Prairies","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Queen's University; Carleton University; Geological Survey of Canada","funders":"","keywords":"Environmental science; Climatology; Wind speed; Prevailing winds; Atmospheric sciences; Wind power; Global wind patterns; Wind direction; Meteorology; Geology; Geography","score_opus":0.0322713154940034,"score_gpt":0.32368721381622567,"score_spread":0.29141589832222226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992660544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9659681,0.0012742997,0.0003744,0.0011973992,0.000036755308,0.00006741247,0.00846297,0.0000760697,0.022542588],"genre_scores_gemma":[0.9928067,0.0006390259,0.00045658014,0.00010154017,0.0000070264728,0.0000145802815,0.0019859388,0.000010115583,0.003978493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995302,0.000029915263,0.000017359853,0.00008617646,0.0001943484,0.00014202745],"domain_scores_gemma":[0.9991328,0.00003094501,0.000093117495,0.0000338082,0.00058781396,0.00012150291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043457377,0.00020392842,0.00020649316,0.0009715535,0.0019783804,0.0009754628,0.0005954303,0.00017949443,0.0021461055],"category_scores_gemma":[0.00116079,0.00024111943,0.00019718465,0.0023422353,0.00048513085,0.0004030433,0.0005780543,0.00034228462,0.00019592542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017227366,0.00007243905,0.9180363,0.00011337443,0.000288059,0.00028651103,0.0015850681,0.004364932,0.0023377326,0.0018576746,0.015453067,0.05543257],"study_design_scores_gemma":[0.000008889775,0.0000056391855,0.9932175,0.000014094504,0.000016802313,0.000020639936,0.00050106004,0.00075613015,0.00005575686,0.00008284503,0.0053103305,0.000010305762],"about_ca_topic_score_codex":0.9937283,"about_ca_topic_score_gemma":0.9980039,"teacher_disagreement_score":0.01091833,"about_ca_system_score_codex":0.01091833,"about_ca_system_score_gemma":0.015755594,"threshold_uncertainty_score":0.07921845},"labels":[],"label_agreement":null},{"id":"W1992796439","doi":"10.1029/2003gl018206","title":"Sources of Asian dust and role of climate change versus desertification in Asian dust emission","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":564,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Desertification; Asian Dust; Dust storm; Environmental science; Storm; China; Precipitation; Atmospheric dust; Climate change; Atmospheric sciences; Climatology; Physical geography; Geography; Aerosol; Meteorology; Geology; Oceanography","score_opus":0.04220615380582602,"score_gpt":0.2927766334634806,"score_spread":0.25057047965765455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1992796439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965019,0.00011181426,0.00056415243,0.00016859025,0.000009537871,0.0000070914593,0.00025428535,0.000020727832,0.0023618233],"genre_scores_gemma":[0.9990349,0.00012978277,0.00018003094,0.000020860216,0.0000040701702,0.0000053895287,0.00015799781,0.0000095312325,0.00045761393],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.000028782182,0.0000044395756,0.000012126531,0.000006886294,0.000022691065],"domain_scores_gemma":[0.9997304,0.00011378211,0.00004440361,0.000011915731,0.000030918465,0.000068618836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040854228,0.0005054252,0.0003196409,0.00027630935,0.0004279701,0.00082935166,0.0004159971,0.00061582477,0.0020160587],"category_scores_gemma":[0.00077017717,0.00027993086,0.0006192635,0.00047265005,0.0003763789,0.00067368406,0.0005197535,0.00044306912,0.00015009109],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002462819,0.00007781063,0.077029325,0.000046238434,0.000092951814,0.0003215558,0.00011102268,0.9152724,0.0018184516,0.0020305575,0.0004716808,0.0024817463],"study_design_scores_gemma":[0.0001574694,0.00010253191,0.035141766,0.000016167565,0.000077213415,0.00008282076,0.00037324155,0.9607983,0.0010440396,0.0012372121,0.0009454059,0.000023763963],"about_ca_topic_score_codex":0.05197702,"about_ca_topic_score_gemma":0.0397875,"teacher_disagreement_score":0.05197702,"about_ca_system_score_codex":0.000930215,"about_ca_system_score_gemma":0.0006863094,"threshold_uncertainty_score":0.10334891},"labels":[],"label_agreement":null},{"id":"W1993056149","doi":"10.1029/2004gl020166","title":"Evidence of continuing methylchloroform emissions from the United States","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Montreal Protocol; Troposphere; Atmospheric sciences; Abundance (ecology); Meteorology; Ozone; Geography; Ozone layer; Geology; Ecology","score_opus":0.05690827786251709,"score_gpt":0.31203331312273597,"score_spread":0.2551250352602189,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993056149","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968183,0.00035681005,0.00013180959,0.00023035247,0.00000757431,0.0000044441717,0.0006077001,0.000015106386,0.0018277911],"genre_scores_gemma":[0.99789244,0.0003000083,0.0002594786,0.0001474934,0.0000067072892,0.000004120227,0.0010539325,0.000004080431,0.00033172788],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978393,0.000028188848,0.000018965351,0.00004896061,0.00007485121,0.00004517497],"domain_scores_gemma":[0.9991142,0.00010933676,0.00030438832,0.00004735675,0.00033263455,0.000091937945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032898955,0.00016493266,0.00015813918,0.0006246816,0.0005582729,0.000622563,0.00019558851,0.0004486651,0.0008899261],"category_scores_gemma":[0.00083781773,0.0001932235,0.00013007647,0.0006847431,0.0002655296,0.00036397018,0.0005407357,0.00041975573,0.000112054346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015119494,0.00008359754,0.9636492,0.00006503409,0.000069078465,0.00020049686,0.0007252016,0.00043362303,0.017166013,0.00014903469,0.0011999218,0.01610764],"study_design_scores_gemma":[0.0000036442975,0.00005384056,0.99343514,0.000018484427,0.000021575455,0.00009208798,0.00033558308,0.00043694634,0.002972441,0.000041989653,0.0025804236,0.000007923108],"about_ca_topic_score_codex":0.09879053,"about_ca_topic_score_gemma":0.230546,"teacher_disagreement_score":0.09879053,"about_ca_system_score_codex":0.0009419871,"about_ca_system_score_gemma":0.00078935735,"threshold_uncertainty_score":0.19643098},"labels":[],"label_agreement":null},{"id":"W1993133049","doi":"10.1029/1999gl010928","title":"Convective boundary layer evolution to 4 km asl over High‐alpine terrain: Airborne lidar observations in the Alps","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council","keywords":"Lidar; Troposphere; Atmospheric sciences; Tropopause; Climatology; Convective Boundary Layer; Convection; Boundary layer; Geology; Orography; Latitude; Aerosol; Planetary boundary layer; Environmental science; Meteorology; Precipitation; Geography; Remote sensing","score_opus":0.0271229314653146,"score_gpt":0.29184933670951474,"score_spread":0.26472640524420016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993133049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994722,0.000056926478,0.00008310565,0.0000132134855,0.000001383698,0.000001512069,0.00006143795,0.000014872453,0.00029540967],"genre_scores_gemma":[0.99956125,0.000027340919,0.00019901161,0.0000064023016,0.0000041202507,0.0000020044508,0.00012801003,0.0000014705855,0.00007043193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999621,0.0000063337284,0.000002123997,0.000008294225,0.000009723824,0.000011376425],"domain_scores_gemma":[0.9998759,0.000019122148,0.000036063146,0.000008057472,0.000039194925,0.000021618796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018658106,0.000118934404,0.00015038892,0.00054841285,0.0003123465,0.0003905767,0.00019298929,0.00027314216,0.00042875475],"category_scores_gemma":[0.00028782577,0.00009971499,0.000117787036,0.0003327305,0.00012659705,0.00022081996,0.00017476515,0.00017752156,0.00008400213],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003809006,0.000185843,0.8403207,0.00008764658,0.000104036444,0.0004555126,0.0011059651,0.0038504396,0.12351989,0.00028754654,0.0005253516,0.029176295],"study_design_scores_gemma":[0.000030395142,0.00006279835,0.9899895,0.000010779216,0.000022927667,0.0000817114,0.00020903899,0.006080739,0.0026410567,0.000082139006,0.0007801765,0.000008726512],"about_ca_topic_score_codex":0.0102439355,"about_ca_topic_score_gemma":0.00896332,"teacher_disagreement_score":0.0102439355,"about_ca_system_score_codex":0.00025741378,"about_ca_system_score_gemma":0.00014270483,"threshold_uncertainty_score":0.020368576},"labels":[],"label_agreement":null},{"id":"W1993370861","doi":"10.1029/2002gl016098","title":"Radiative forcing of climate by historical land cover change","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Radiative forcing; Land cover; Forcing (mathematics); Environmental science; Climatology; Climate model; Climate change; Vegetation (pathology); Atmospheric sciences; Land use; Range (aeronautics); Geology; Ecology","score_opus":0.05781587707354278,"score_gpt":0.3060292628969756,"score_spread":0.2482133858234328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993370861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952518,0.000078404795,0.0010621845,0.00020277433,0.00001761387,0.0000031766997,0.00033388313,0.000058816804,0.0029914195],"genre_scores_gemma":[0.99946123,0.0000568086,0.00014457775,0.0000112925845,0.000009994166,0.0000042232655,0.00014227156,0.0000097804505,0.00015982846],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988544,0.000047564008,0.00000483509,0.000017208316,0.000014782469,0.000030145711],"domain_scores_gemma":[0.9997335,0.00013534728,0.000034882323,0.00003445621,0.000037877875,0.000023910998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000379714,0.00027108792,0.00017083777,0.00030411594,0.00036948238,0.000541528,0.00032928484,0.0005009341,0.0014314825],"category_scores_gemma":[0.0015121857,0.0002706915,0.0004478835,0.00039870327,0.0003823123,0.0003906467,0.00028622357,0.0003299768,0.00016420675],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018793094,0.000096649565,0.10733858,0.000057809153,0.0001201105,0.0002647722,0.0001575649,0.86111504,0.013058024,0.006624522,0.001633076,0.009345923],"study_design_scores_gemma":[0.00007733007,0.00009621607,0.13416846,0.000012533052,0.00007527465,0.00018741106,0.00011316779,0.8558501,0.002658372,0.0045233895,0.002205471,0.00003225977],"about_ca_topic_score_codex":0.006714655,"about_ca_topic_score_gemma":0.0042899656,"teacher_disagreement_score":0.006714655,"about_ca_system_score_codex":0.00080626644,"about_ca_system_score_gemma":0.0002722849,"threshold_uncertainty_score":0.013351142},"labels":[],"label_agreement":null},{"id":"W1993618349","doi":"10.1029/2009gl037351","title":"Termite mounds as hot spots of nitrous oxide emissions in South‐Sudanian savanna of Burkina Faso (West Africa)","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Insect and Arachnid Ecology and Behavior","field":"Biochemistry, Genetics and Molecular Biology","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Nitrous oxide; Ecosystem; Methane; Wet season; Environmental science; Dry season; Tropics; Ecology; Agroforestry; Biology","score_opus":0.024250329085984606,"score_gpt":0.3155066988652474,"score_spread":0.2912563697792628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993618349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998129,0.00007031978,0.00001309644,0.0000083949935,5.2510103e-7,0.0000017700085,0.000016004115,6.1460304e-7,0.00007654433],"genre_scores_gemma":[0.99973124,0.00007979282,0.00006153727,0.0000051373404,0.0000012025625,0.0000028884424,0.000026067904,3.3402495e-7,0.000091764894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000013695218,0.0000034243235,0.000013130955,0.000007835111,0.000025146757],"domain_scores_gemma":[0.99983466,0.00001771916,0.00007746492,0.00000575853,0.00002115248,0.00004329409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015843092,0.00019926197,0.00013033049,0.00057714235,0.0008149201,0.0005561647,0.00018551933,0.00023279645,0.00049229286],"category_scores_gemma":[0.00028704203,0.0001520832,0.00007520108,0.00045493236,0.0003883733,0.0002820182,0.00041658324,0.00014609545,0.000046296664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027863425,0.000056540117,0.9622497,0.000041427927,0.000030822168,0.0012829162,0.0040690233,0.00008119321,0.023522094,0.00006338174,0.00008026458,0.008243974],"study_design_scores_gemma":[0.0000037253365,0.000039749655,0.9959233,0.0000091823,0.000009200559,0.00030227215,0.003003946,0.00009828672,0.0003307088,0.0000246453,0.0002510847,0.0000039230827],"about_ca_topic_score_codex":0.032083437,"about_ca_topic_score_gemma":0.10329453,"teacher_disagreement_score":0.032083437,"about_ca_system_score_codex":0.00050083065,"about_ca_system_score_gemma":0.0002944062,"threshold_uncertainty_score":0.06379342},"labels":[],"label_agreement":null},{"id":"W1993636872","doi":"10.1029/2006gl025805","title":"Latitudinal dependence of noctilucent cloud growth","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Tekes; Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales","keywords":"Atmospheric sciences; Latitude; Zonal and meridional; Water vapor; Environmental science; Particle (ecology); Supersaturation; Physics; Meteorology; Geology; Astronomy","score_opus":0.026887499551476374,"score_gpt":0.274730958434797,"score_spread":0.24784345888332063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993636872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814844,0.00013287127,0.00012047523,0.000016809892,0.0000023058085,0.0000017710975,0.00037477477,0.000011462737,0.001191193],"genre_scores_gemma":[0.9987985,0.000073721385,0.0001014618,0.0000088727975,0.0000029407115,0.0000025447505,0.0006069983,0.0000060730954,0.0003988369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999931,0.000009161737,0.0000051368334,0.000028514634,0.000010236722,0.000016014186],"domain_scores_gemma":[0.9992895,0.00013632195,0.00020034038,0.0000603389,0.00024115427,0.000072381954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017480266,0.00012796377,0.0000948455,0.0004479886,0.00015246913,0.00026610921,0.00008676847,0.00012357885,0.00093407306],"category_scores_gemma":[0.00046718083,0.00009624273,0.000108963075,0.00025122415,0.000110405905,0.00015157026,0.0001926677,0.000121765195,0.00022426022],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019787457,0.000019686051,0.92938083,0.000033239055,0.000038648468,0.00013144407,0.00026051555,0.0015176425,0.06012223,0.000141662,0.00033443174,0.007821838],"study_design_scores_gemma":[9.676515e-7,0.000009256297,0.9977592,0.0000015059003,0.0000025592124,0.000029119636,0.000039802886,0.00052046025,0.0012674417,0.0000062498425,0.0003616012,0.0000017318183],"about_ca_topic_score_codex":0.0092899045,"about_ca_topic_score_gemma":0.017301537,"teacher_disagreement_score":0.0092899045,"about_ca_system_score_codex":0.00024515527,"about_ca_system_score_gemma":0.00009329492,"threshold_uncertainty_score":0.018471658},"labels":[],"label_agreement":null},{"id":"W1993936612","doi":"10.1029/2005gl023013","title":"Shape and composition of PMC particles derived from satellite remote sensing measurements","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Waterloo","funders":"","keywords":"Satellite; Spectrograph; Remote sensing; Spectrometer; Polar; Infrared; Physics; Atmospheric sciences; Environmental science; Spectral line; Materials science; Optics; Geology; Astronomy","score_opus":0.06260539717247407,"score_gpt":0.29006590566111734,"score_spread":0.22746050848864327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993936612","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99750406,0.000060146882,0.0006508566,0.0000068402687,0.000003802415,0.0000075440407,0.0007300602,0.000016977558,0.0010196994],"genre_scores_gemma":[0.99745387,0.000033134645,0.0007193964,0.000007503545,0.0000038183866,0.000004609118,0.0016370051,0.000009457134,0.000131306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988925,0.000006216673,0.0000063029115,0.00003630664,0.00004991496,0.000011953171],"domain_scores_gemma":[0.9998124,0.000027760394,0.00004033774,0.000021565576,0.00007871774,0.000019266252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013057915,0.00012036581,0.00013842716,0.0006351861,0.00017062628,0.00032170909,0.00015625433,0.00018161073,0.00047034555],"category_scores_gemma":[0.0005118469,0.00011536666,0.00017671243,0.00047909716,0.0001242005,0.0002145755,0.00015749587,0.000119630626,0.00021140891],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005768306,0.00006263801,0.74459165,0.000059371712,0.000083911385,0.00030276453,0.00018487472,0.004563865,0.221437,0.00036838165,0.0008618106,0.026906872],"study_design_scores_gemma":[0.000008296044,0.000032046988,0.9774596,0.0000029766466,0.000013284556,0.00020702052,0.000071739785,0.009527237,0.011864315,0.00009868982,0.0007070783,0.000007748134],"about_ca_topic_score_codex":0.006002039,"about_ca_topic_score_gemma":0.004660794,"teacher_disagreement_score":0.006002039,"about_ca_system_score_codex":0.00030446376,"about_ca_system_score_gemma":0.00009834686,"threshold_uncertainty_score":0.011934221},"labels":[],"label_agreement":null},{"id":"W1993985472","doi":"10.1029/2006gl028907","title":"Wind work in a model of the northwest Atlantic Ocean","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Wind stress; Sink (geography); Forcing (mathematics); Work (physics); Wind speed; Meteorology; Ocean current; Wind power; Kinetic energy; Environmental science; Geology; Climatology; Atmospheric sciences; Physics; Engineering; Geography","score_opus":0.025692772838498145,"score_gpt":0.2576228946057779,"score_spread":0.23193012176727978,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1993985472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96365076,0.0004250433,0.017291399,0.00071165914,0.00011580317,0.00003724026,0.0013954701,0.00017897978,0.01619365],"genre_scores_gemma":[0.9913492,0.00028691077,0.0032707814,0.000057133704,0.000029618279,0.000051751693,0.00055715884,0.000048085207,0.004349325],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999006,0.000027821734,0.000008703401,0.000025559162,0.00001850399,0.000018817516],"domain_scores_gemma":[0.999767,0.00007720539,0.000047337468,0.000025515614,0.00004363053,0.00003935263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020967047,0.00039710785,0.00049464754,0.0002468339,0.0006269251,0.0011908584,0.000848434,0.0012042021,0.0022733286],"category_scores_gemma":[0.00082172715,0.0004222317,0.00074165856,0.00057232863,0.0004753486,0.00079108746,0.000542016,0.0005651698,0.00028484038],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057231908,0.00003052817,0.0027188126,0.000015285856,0.00001829062,0.00006615121,0.000023116507,0.99288094,0.0007828687,0.0019378441,0.00024687086,0.0012220786],"study_design_scores_gemma":[0.00005191513,0.000023941284,0.0018075063,0.0000042589304,0.000008482651,0.000013750356,0.00001812162,0.9966742,0.00009903023,0.0008059075,0.00048363738,0.000009247757],"about_ca_topic_score_codex":0.061835326,"about_ca_topic_score_gemma":0.031944852,"teacher_disagreement_score":0.061835326,"about_ca_system_score_codex":0.001138289,"about_ca_system_score_gemma":0.0010726558,"threshold_uncertainty_score":0.12295079},"labels":[],"label_agreement":null},{"id":"W1994660837","doi":"10.1029/2002gl016579","title":"Crustal loading near Great Salt Lake, Utah","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"California Institute of Technology; U.S. Geological Survey; National Aeronautics and Space Administration; Smithsonian Institution; National Science Foundation","keywords":"Amplitude; Salt lake; Geology; Global Positioning System; Precipitation; Elevation (ballistics); Geodesy; Climatology; Meteorology; Geomorphology; Geometry; Geography","score_opus":0.05906411771350186,"score_gpt":0.28930420587042094,"score_spread":0.23024008815691907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994660837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9922845,0.00009113496,0.00019187618,0.00016510894,0.000003735564,0.000008933557,0.0013101813,0.00010308917,0.0058415164],"genre_scores_gemma":[0.99573743,0.000068291025,0.00043173687,0.000033652424,0.000004215728,0.000009238369,0.0012054897,0.000009930587,0.002499911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990606,0.000005504231,0.000004279894,0.0000279148,0.000040827254,0.000015315522],"domain_scores_gemma":[0.9998739,0.00000839633,0.000030806605,0.000012294476,0.000049229515,0.00002546306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009074968,0.00014318981,0.000106402884,0.0004879543,0.000737,0.00049124705,0.00041310652,0.0002000251,0.0027447087],"category_scores_gemma":[0.00054036896,0.00012625924,0.00006769688,0.0006562596,0.00032897765,0.00030809533,0.001124781,0.000101975915,0.00034851336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010235417,0.000038496528,0.91643894,0.00008460498,0.00009344533,0.00070525776,0.002490145,0.008730928,0.014347488,0.0010195776,0.008271978,0.04767687],"study_design_scores_gemma":[0.000010908176,0.000011901553,0.98992574,0.000009358292,0.0000112159505,0.000054069442,0.0002860186,0.0032933196,0.0008372898,0.0002346104,0.005315496,0.0000100433335],"about_ca_topic_score_codex":0.23536628,"about_ca_topic_score_gemma":0.50295377,"teacher_disagreement_score":0.23536628,"about_ca_system_score_codex":0.001732816,"about_ca_system_score_gemma":0.0008937322,"threshold_uncertainty_score":0.4679926},"labels":[],"label_agreement":null},{"id":"W1994691247","doi":"10.1002/2014gl062366","title":"Observed multivariable signals of late 20th and early 21st century volcanic activity","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Volcano; Troposphere; Climatology; Vulcanian eruption; Environmental science; Water vapor; Atmospheric sciences; Geology; Global warming; Climate change; Meteorology; Geography; Seismology; Oceanography","score_opus":0.05297498966023854,"score_gpt":0.2907605598722973,"score_spread":0.2377855702120588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994691247","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962435,0.000048976126,0.0022063546,0.00003691113,0.0000060951274,0.000003692118,0.0006124377,0.00003770208,0.00080431293],"genre_scores_gemma":[0.9993856,0.000014438046,0.00020623197,0.0000033544611,0.0000072591642,0.0000010356376,0.00028914757,0.0000013592106,0.00009165193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990904,0.000016858343,0.0000045412967,0.000032683212,0.00001729335,0.000019585585],"domain_scores_gemma":[0.9994962,0.00023375322,0.0001347051,0.00003712217,0.00005461431,0.00004357423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028554516,0.00016268506,0.00013366526,0.00046205596,0.00008227396,0.00039495365,0.00011070878,0.00012500367,0.0016876287],"category_scores_gemma":[0.0011504276,0.000070375434,0.00013213619,0.00043895663,0.00011153412,0.00019327416,0.00028563774,0.00018842788,0.00012941334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028833174,0.000113907576,0.8843056,0.00006164892,0.000265995,0.00025142892,0.0001449823,0.027621558,0.03453723,0.0013079612,0.00077414466,0.050327174],"study_design_scores_gemma":[0.0000045890442,0.00004454704,0.96458024,0.0000025924637,0.000019666764,0.00004680044,0.00003549737,0.0331996,0.0013394186,0.0003727474,0.00034542408,0.000008896231],"about_ca_topic_score_codex":0.002074028,"about_ca_topic_score_gemma":0.0020807309,"teacher_disagreement_score":0.002074028,"about_ca_system_score_codex":0.00013275263,"about_ca_system_score_gemma":0.00009293203,"threshold_uncertainty_score":0.0056456327},"labels":[],"label_agreement":null},{"id":"W1994876543","doi":"10.1002/2014gl060369","title":"Evidence of Arctic sea ice thinning from direct observations","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; York University","funders":"","keywords":"Thinning; Sea ice; Arctic ice pack; Geology; Antarctic sea ice; Cryosphere; Climatology; Melt pond; Arctic; Oceanography; Environmental science; Geography","score_opus":0.07607666510202632,"score_gpt":0.29727338580771356,"score_spread":0.22119672070568724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994876543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913726,0.0004145547,0.00037127745,0.000039740396,0.000019657246,0.000009031771,0.00252684,0.000020206633,0.0052262163],"genre_scores_gemma":[0.99557143,0.00031057486,0.00051973277,0.000049129863,0.000034424666,0.000013319629,0.0029286593,0.0000064085148,0.0005663072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996376,0.000060076447,0.00003558502,0.00009893226,0.00012634178,0.000041437354],"domain_scores_gemma":[0.9978865,0.0003453289,0.00080534053,0.00015963643,0.000692358,0.000110819965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076226227,0.00023209589,0.00018837795,0.0007672431,0.00024749324,0.00063764537,0.00023089715,0.00023645618,0.0012881721],"category_scores_gemma":[0.001362958,0.0001942665,0.00015232964,0.00072903524,0.00022767202,0.00028936742,0.000432114,0.00026356353,0.00043910628],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014708363,0.000022609029,0.9853507,0.00006174533,0.000079487145,0.00008810012,0.00018230341,0.00022062208,0.006278678,0.000027119295,0.0005340534,0.007007458],"study_design_scores_gemma":[0.000002067747,0.000018885234,0.9985404,0.000013315506,0.000008978441,0.000051315903,0.00007977275,0.00014901948,0.0006131369,0.000010078504,0.00051039783,0.0000026549408],"about_ca_topic_score_codex":0.011837197,"about_ca_topic_score_gemma":0.022257606,"teacher_disagreement_score":0.011837197,"about_ca_system_score_codex":0.00023557476,"about_ca_system_score_gemma":0.00019833354,"threshold_uncertainty_score":0.023536563},"labels":[],"label_agreement":null},{"id":"W1994893415","doi":"10.1029/2004gl019747","title":"Subpolar Mode Water formation traced by neodymium isotopic composition","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subarctic climate; Ocean gyre; Water mass; Oceanography; Salinity; Geology; Mode water; TRACER; Circumpolar deep water; Current (fluid); North Atlantic Deep Water; Formation water; Deep water; Ecology","score_opus":0.022699301347474467,"score_gpt":0.2832604065113525,"score_spread":0.26056110516387804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994893415","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993511,0.00003579726,0.00006770632,0.000004983738,6.5609373e-7,0.0000012225598,0.000061682236,0.000004319084,0.00047253084],"genre_scores_gemma":[0.99908614,0.0000931334,0.00018830391,0.000009105481,7.9021606e-7,0.0000028420109,0.00013696185,0.000003262685,0.0004794021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999865,0.000001163572,6.1128634e-7,0.0000048453,0.0000027765927,0.0000041483313],"domain_scores_gemma":[0.9999443,0.0000050319177,0.000016970289,0.0000034354778,0.00001357987,0.000016651786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004080969,0.00009579929,0.000098348646,0.0004220852,0.00013852988,0.00023255196,0.00006208737,0.00009538908,0.00065365166],"category_scores_gemma":[0.00008302133,0.00013865688,0.000049899587,0.00024183777,0.00017281296,0.00015792462,0.00020554673,0.00009478746,0.00016546239],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029796668,0.000018037508,0.5734393,0.000017131237,0.00001953814,0.00018756372,0.0004888107,0.0002057394,0.411984,0.00020198376,0.00012281201,0.013017145],"study_design_scores_gemma":[0.0000033529948,0.000033881137,0.9869294,0.0000026344553,0.000007932313,0.000054867007,0.0002136393,0.000513366,0.011669753,0.00006012352,0.0005088041,0.000002189362],"about_ca_topic_score_codex":0.0077506877,"about_ca_topic_score_gemma":0.0131924255,"teacher_disagreement_score":0.0077506877,"about_ca_system_score_codex":0.00026320017,"about_ca_system_score_gemma":0.00010364171,"threshold_uncertainty_score":0.015411139},"labels":[],"label_agreement":null},{"id":"W1994937395","doi":"10.1029/2001gl013632","title":"Importance of wind‐driven sea ice motion for the formation of Antarctic Intermediate Water in a global climate model","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; International Arctic Research Center, University of Alaska, Fairbanks","keywords":"Geology; Antarctic Intermediate Water; Oceanography; Sea ice; Antarctic sea ice; Arctic ice pack; Fast ice; Wind stress; Salinity; Climatology; Thermohaline circulation","score_opus":0.02609171091510749,"score_gpt":0.2837481117930441,"score_spread":0.2576564008779366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1994937395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833635,0.00017388286,0.0069344416,0.00052676245,0.00005175905,0.000030474388,0.00080551195,0.00014992898,0.00796361],"genre_scores_gemma":[0.9983487,0.00008137465,0.00077629025,0.00003173851,0.000007765893,0.00001848149,0.00023516937,0.000032736945,0.00046777423],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993324,0.000024992152,0.000004038101,0.000011495331,0.000008221997,0.000017983908],"domain_scores_gemma":[0.9997665,0.00009852178,0.000029790419,0.000015698524,0.000031275427,0.000058196067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002638361,0.0005327871,0.00044727794,0.00028389366,0.00064522907,0.00088778674,0.00056783314,0.0008222646,0.0013683399],"category_scores_gemma":[0.0012233107,0.00034149,0.0005547461,0.00036119577,0.0005564359,0.00074798736,0.0005959694,0.00056660967,0.00012351629],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044164834,0.00001802855,0.0061615086,0.000011689098,0.000019884563,0.00006641178,0.000023708864,0.99047893,0.0006446404,0.0015452803,0.0002556617,0.00073008356],"study_design_scores_gemma":[0.000038582602,0.000033215816,0.0023575565,0.0000047308904,0.000017852866,0.000012755303,0.00002717073,0.9961986,0.00019763366,0.00078216894,0.00031991824,0.000009881758],"about_ca_topic_score_codex":0.03622797,"about_ca_topic_score_gemma":0.021591522,"teacher_disagreement_score":0.03622797,"about_ca_system_score_codex":0.00092866004,"about_ca_system_score_gemma":0.0010449233,"threshold_uncertainty_score":0.07203418},"labels":[],"label_agreement":null},{"id":"W1995238254","doi":"10.1029/2000gl012611","title":"New constraints on Laurentide postglacial rebound from absolute gravity measurements","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Resources Canada; National Oceanic and Atmospheric Administration; Manitoba Hydro","keywords":"Geology; Ice sheet; Mantle (geology); Bay; Homogeneous; Post-glacial rebound; Oceanography; Geodesy; Geophysics; Climatology; Physics","score_opus":0.08233221373171455,"score_gpt":0.32086430193604076,"score_spread":0.2385320882043262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995238254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98179674,0.0008522739,0.0010720931,0.00019377437,0.000012309009,0.0000060344155,0.00083336985,0.00006914478,0.015164178],"genre_scores_gemma":[0.9972283,0.00020805,0.0005281576,0.00005173571,0.000010108781,0.00000797068,0.001147882,0.000014641043,0.00080299436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997514,0.000027560467,0.000021263633,0.00009559136,0.000046918474,0.00005732351],"domain_scores_gemma":[0.9989662,0.00030444798,0.0002703698,0.00012194951,0.00024469476,0.000092343274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006498007,0.00041644624,0.0004528603,0.0011407716,0.0007327198,0.0017939617,0.00047121054,0.00034593538,0.0031265097],"category_scores_gemma":[0.002406961,0.00029746996,0.00014656791,0.00085855165,0.0005208339,0.00092950766,0.0010229299,0.00038994534,0.0005620535],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058349496,0.0000576319,0.9120541,0.00017737693,0.000101952595,0.00057187985,0.0022256966,0.0025613667,0.038053695,0.002625741,0.0018470784,0.039139997],"study_design_scores_gemma":[0.000012358042,0.00003994494,0.9875388,0.000059827595,0.000024239018,0.00017644733,0.00081097026,0.0024889673,0.0025776697,0.00058798614,0.005660038,0.000022674883],"about_ca_topic_score_codex":0.037890237,"about_ca_topic_score_gemma":0.16082218,"teacher_disagreement_score":0.037890237,"about_ca_system_score_codex":0.0007076012,"about_ca_system_score_gemma":0.00053961156,"threshold_uncertainty_score":0.07533938},"labels":[],"label_agreement":null},{"id":"W1995538647","doi":"10.1029/2004gl020671","title":"What drives heat transport in the Atlantic: Sensitivity to mechanical energy supply and buoyancy forcing in the Southern Ocean","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Buoyancy; Forcing (mathematics); Sensitivity (control systems); Environmental science; Oceanography; Climatology; Geology; Mechanics; Physics; Engineering","score_opus":0.015588428182456286,"score_gpt":0.24490004115090097,"score_spread":0.22931161296844468,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1995538647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977308,0.000060287195,0.00043223597,0.00053886446,0.000018507397,0.0000059718823,0.0002028613,0.000039687133,0.00097079633],"genre_scores_gemma":[0.9996916,0.00003813857,0.00008297492,0.000029821385,0.000005078299,0.0000016750336,0.00007048427,0.0000083223085,0.00007190365],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991643,0.000028612365,0.00000606095,0.000016048276,0.000010626723,0.000022206876],"domain_scores_gemma":[0.9995171,0.00021160215,0.00007311178,0.000045268902,0.000057199828,0.0000956971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037984052,0.00030828663,0.00032011664,0.00021983325,0.00038274462,0.00084707286,0.00033647305,0.00092759344,0.0013058505],"category_scores_gemma":[0.002130558,0.0003676372,0.0005790946,0.00025703167,0.00048467764,0.00054967724,0.0004018195,0.00050641864,0.0001674773],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069735124,0.00021401992,0.35355708,0.0001680666,0.00034015073,0.00061270007,0.00029707572,0.5322087,0.10042606,0.0039038495,0.0018067812,0.0057681785],"study_design_scores_gemma":[0.00019268946,0.00014899576,0.20448053,0.000025518286,0.00011178173,0.00007837864,0.00025250268,0.78542674,0.005163111,0.0033724543,0.0006741706,0.00007312133],"about_ca_topic_score_codex":0.026661774,"about_ca_topic_score_gemma":0.0154892225,"teacher_disagreement_score":0.026661774,"about_ca_system_score_codex":0.0008092429,"about_ca_system_score_gemma":0.0005064954,"threshold_uncertainty_score":0.053013206},"labels":[],"label_agreement":null},{"id":"W1996136195","doi":"10.1029/2002gl015255","title":"The Sudbury Structure: A circular impact crater?","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McMaster University","funders":"","keywords":"Impact crater; Geology; Meteorite; Impact structure; Igneous rock; Paleomagnetism; Thrust fault; Geochemistry; Petrology; Seismology; Geophysics; Geomorphology; Tectonics; Astrobiology","score_opus":0.03784012562697973,"score_gpt":0.2987144250455928,"score_spread":0.26087429941861306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996136195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9251263,0.0065206164,0.0021521645,0.0020583812,0.00033613722,0.00011015121,0.00064754154,0.00012398897,0.06292474],"genre_scores_gemma":[0.9907046,0.000899403,0.000946093,0.00018166906,0.0000673197,0.000006084545,0.00021631422,0.000009601379,0.0069689676],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.0000064259966,0.0000044661506,0.000032194,0.000024607723,0.000047294547],"domain_scores_gemma":[0.99990606,0.000007488545,0.00003480729,0.000010915696,0.000014467472,0.00002624587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000820743,0.00019475685,0.00014654778,0.0005812501,0.0011671714,0.0012969774,0.00027919043,0.0006544309,0.00924869],"category_scores_gemma":[0.0004196107,0.00029055006,0.00011767141,0.0007575257,0.0016248154,0.00046835685,0.0007649318,0.00028924,0.0008738617],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015647729,0.000110044086,0.48185053,0.0005376179,0.000095968426,0.057454955,0.005179439,0.0018098564,0.03688234,0.04919733,0.026300404,0.33901674],"study_design_scores_gemma":[0.00011287386,0.00034465693,0.7462202,0.00028464085,0.00007519171,0.08240379,0.005452389,0.0030490712,0.003603773,0.003930294,0.15444756,0.00007550155],"about_ca_topic_score_codex":0.074986205,"about_ca_topic_score_gemma":0.15758604,"teacher_disagreement_score":0.9250138,"about_ca_system_score_codex":0.0013100104,"about_ca_system_score_gemma":0.001005743,"threshold_uncertainty_score":0.14909953},"labels":[],"label_agreement":null},{"id":"W1996493171","doi":"10.1029/2007gl031932","title":"Empirical transfer functions: Application to determination of outermost core velocity structure using <i>SmKS</i> phases","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Waveform; Seismogram; Deconvolution; Transfer function; Core (optical fiber); Geology; Gaussian; Stack (abstract data type); Computational physics; Physics; Optics; Computer science; Seismology","score_opus":0.06250673636538946,"score_gpt":0.3485920917965348,"score_spread":0.2860853554311453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996493171","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2056868,0.000092481736,0.78858435,0.00010212729,0.000023840277,0.000034265955,0.00025093104,0.0031551071,0.0020701045],"genre_scores_gemma":[0.6821092,0.00017485303,0.31570625,0.000032506225,0.00003164213,0.00005550322,0.00047982298,0.0005599402,0.0008503152],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99987555,0.000028344715,0.000009462653,0.000029275281,0.000035779383,0.000021594886],"domain_scores_gemma":[0.9993687,0.00025800278,0.00011559812,0.000114651615,0.000118226315,0.000024947807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009394841,0.0005966685,0.00018484943,0.0010084987,0.00027222233,0.00051053864,0.00052063266,0.00044659775,0.0016223792],"category_scores_gemma":[0.004535757,0.000301891,0.00038308045,0.0009970037,0.0003130196,0.0008255584,0.0004855273,0.0005461661,0.0006015604],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023792894,0.00014072779,0.032028943,0.00013540954,0.00008864408,0.00018364469,0.00046233035,0.33017528,0.048905917,0.010848678,0.0015492323,0.5752432],"study_design_scores_gemma":[0.00001913436,0.00005223389,0.011376292,0.000013214631,0.00001591865,0.00011839065,0.00005883218,0.96294457,0.018518535,0.00486794,0.0019831064,0.000031745996],"about_ca_topic_score_codex":0.0021817144,"about_ca_topic_score_gemma":0.001850942,"teacher_disagreement_score":0.0021817144,"about_ca_system_score_codex":0.00041409166,"about_ca_system_score_gemma":0.0005753228,"threshold_uncertainty_score":0.00542742},"labels":[],"label_agreement":null},{"id":"W1996744758","doi":"10.1029/2007gl032971","title":"Atmospheric conditions associated with oceanic convection in the south‐east Labrador Sea","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Centers for Disease Control and Prevention","keywords":"Climatology; Forcing (mathematics); Deep convection; Convection; Synoptic scale meteorology; Geology; Atmospheric convection; Oceanography; North Atlantic oscillation; Atmospheric sciences; Meteorology; Geography; Troposphere","score_opus":0.03946864200431307,"score_gpt":0.2762556331150572,"score_spread":0.2367869911107441,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996744758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934894,0.00002739336,0.00002774927,0.000028939805,0.0000014642786,0.0000014633684,0.00009871306,0.0000073888154,0.00045793352],"genre_scores_gemma":[0.9997172,0.000024847619,0.000034543365,0.0000075683965,0.000002901956,0.000001452636,0.0001472026,0.0000021396722,0.000062221356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998852,0.000025356847,0.000012058425,0.000017765708,0.000016974045,0.00004268337],"domain_scores_gemma":[0.99974376,0.00003639936,0.00012717473,0.000027550193,0.00003013092,0.00003495128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017556318,0.00014410945,0.00020440925,0.00047769994,0.00034288983,0.0006964978,0.00014728226,0.00018995725,0.0007156156],"category_scores_gemma":[0.00055635447,0.00012840905,0.0001947372,0.00044050356,0.00034888272,0.00026982493,0.00041714034,0.0001634164,0.00013718735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017388807,0.000034943445,0.98586833,0.000020015263,0.000050934523,0.00018644369,0.000172874,0.0025221165,0.0065072947,0.00021160775,0.00039259804,0.0038588513],"study_design_scores_gemma":[0.000010598045,0.000026850608,0.99739873,0.0000035535113,0.000015954236,0.000046880035,0.0001652716,0.0013793508,0.0006029398,0.0000588647,0.00028503724,0.0000060940715],"about_ca_topic_score_codex":0.033506952,"about_ca_topic_score_gemma":0.0420837,"teacher_disagreement_score":0.033506952,"about_ca_system_score_codex":0.0006447745,"about_ca_system_score_gemma":0.0003016154,"threshold_uncertainty_score":0.06662387},"labels":[],"label_agreement":null},{"id":"W1996834935","doi":"10.1029/1999gl011070","title":"Can deglaciation trigger earthquakes in N. America?","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Deglaciation; Geology; Margin (machine learning); Glacial period; Seismology; Lithosphere; Instability; Magnitude (astronomy); Last Glacial Maximum; Fault (geology); Geomorphology; Tectonics","score_opus":0.030603843144565084,"score_gpt":0.27916720653163657,"score_spread":0.2485633633870715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1996834935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784863,0.00013258585,0.00012845833,0.0002077744,0.0000068658496,0.0000025124045,0.00015794873,0.000013487704,0.0015016602],"genre_scores_gemma":[0.9995702,0.00009504177,0.00007046159,0.000017395203,0.0000035014948,0.0000014420255,0.00008739432,0.000002157622,0.00015235852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996805,0.000005644242,0.0000018089801,0.000010484427,0.0000027916678,0.000011323941],"domain_scores_gemma":[0.99984026,0.00003677901,0.000058130358,0.000009872859,0.000020631724,0.000034243738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012405963,0.00014756495,0.00010612282,0.0002150306,0.00022056134,0.00040966878,0.00016745686,0.0003246998,0.00086648617],"category_scores_gemma":[0.0008952445,0.0001384162,0.00014724562,0.0002666189,0.00023663887,0.00039080478,0.0003154709,0.00012141979,0.00010434141],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021964299,0.00003826857,0.9624546,0.00005371686,0.000053020456,0.0007078538,0.0006250343,0.016825274,0.0034767904,0.0010934359,0.0013124372,0.013139908],"study_design_scores_gemma":[0.000027112108,0.000048457867,0.96745515,0.000018019646,0.000038112066,0.00022658623,0.0007666892,0.027892046,0.0003935374,0.0013245023,0.001798062,0.000011709192],"about_ca_topic_score_codex":0.060443096,"about_ca_topic_score_gemma":0.10503234,"teacher_disagreement_score":0.9395569,"about_ca_system_score_codex":0.00060975086,"about_ca_system_score_gemma":0.00036839643,"threshold_uncertainty_score":0.120182574},"labels":[],"label_agreement":null},{"id":"W1997146064","doi":"10.1029/2005gl022462","title":"Contrasting trends in North Atlantic deep‐water formation in the Labrador Sea and Nordic Seas during the Holocene","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Belgian Federal Science Policy Office; Fonds De La Recherche Scientifique - FNRS","keywords":"North Atlantic Deep Water; Oceanography; Holocene; Geology; Atlantic Equatorial mode; Arctic; Sea ice; Thermohaline circulation; Surface water; Climatology; Water mass; Forcing (mathematics); Circumpolar deep water; Environmental science","score_opus":0.022554361187778024,"score_gpt":0.2656315286233125,"score_spread":0.24307716743553448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997146064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995454,0.000020837546,0.00003231435,0.00003831303,0.0000033140263,0.0000016919224,0.0001494685,0.0000123291775,0.00019620526],"genre_scores_gemma":[0.99937624,0.000027065948,0.00007038217,0.000015219225,0.0000016987706,0.000004488937,0.00035707533,0.000004386034,0.0001435595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998795,0.000029148361,0.000010779012,0.000029325302,0.000009837238,0.000041441806],"domain_scores_gemma":[0.9997539,0.00006635299,0.000046338508,0.00002715937,0.000031478812,0.00007477733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037706344,0.00041756607,0.00038866643,0.0002050847,0.00042645147,0.000923339,0.00040281282,0.0007344668,0.0008442907],"category_scores_gemma":[0.00095097686,0.00035625702,0.00070033193,0.00026436057,0.00047379063,0.0003873214,0.00042165408,0.00040022345,0.00012690766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027645733,0.00048172707,0.644483,0.0001275863,0.0006874103,0.00059502205,0.00045311032,0.3219071,0.017779604,0.0016520142,0.0019392397,0.007129609],"study_design_scores_gemma":[0.00059776445,0.00078403053,0.7305963,0.000031057738,0.0003099325,0.00009197042,0.0007354322,0.2605459,0.00424927,0.00037608854,0.0016036592,0.00007857409],"about_ca_topic_score_codex":0.09423946,"about_ca_topic_score_gemma":0.094163015,"teacher_disagreement_score":0.09423946,"about_ca_system_score_codex":0.001185547,"about_ca_system_score_gemma":0.000692383,"threshold_uncertainty_score":0.18738186},"labels":[],"label_agreement":null},{"id":"W1997164308","doi":"10.1029/2003gl017731","title":"Self‐potential, soil CO<sub>2</sub> flux, and temperature on Masaya volcano, Nicaragua","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université de Montréal","funders":"National Aeronautics and Space Administration","keywords":"Volcano; Flux (metallurgy); Geology; Soil gas; Table (database); Mineralogy; Soil water; Soil science; Geomorphology; Atmospheric sciences; Petrology; Geochemistry; Chemistry","score_opus":0.013523824352300042,"score_gpt":0.24643620600110647,"score_spread":0.23291238164880643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997164308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996691,0.000024238336,0.000022759366,0.000008773731,4.662669e-7,0.0000012151943,0.000041551084,0.0000026937803,0.00022916892],"genre_scores_gemma":[0.9996797,0.000035363533,0.000060647966,0.0000035632927,0.0000016558669,0.000005514837,0.000113597445,0.0000015832038,0.00009838317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992204,0.000016327245,0.0000047466715,0.000025023875,0.000011852049,0.000020030731],"domain_scores_gemma":[0.99976975,0.000048307535,0.00007766797,0.000021983775,0.000058154645,0.000024139894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012781938,0.00023583273,0.00022264657,0.00051783264,0.00039339103,0.0003396693,0.00037045864,0.00022559501,0.0003937786],"category_scores_gemma":[0.000487885,0.00015684769,0.00014178955,0.00053504005,0.00041719503,0.00021677543,0.0005517159,0.00012435182,0.000088056964],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021249095,0.000025860223,0.9749315,0.00003301906,0.00008000605,0.00040703418,0.0012527782,0.0021219056,0.015928436,0.00007878213,0.00012989646,0.0047982126],"study_design_scores_gemma":[0.0000027776816,0.000014909597,0.99752444,0.000003543843,0.000011871107,0.000042369393,0.00032548557,0.001309241,0.0005589953,0.000016730393,0.00018583142,0.000003807486],"about_ca_topic_score_codex":0.12018037,"about_ca_topic_score_gemma":0.16998105,"teacher_disagreement_score":0.12018037,"about_ca_system_score_codex":0.0010931435,"about_ca_system_score_gemma":0.0002757769,"threshold_uncertainty_score":0.2389617},"labels":[],"label_agreement":null},{"id":"W1997411679","doi":"10.1029/2000gl012369","title":"Sea‐level change and true polar wander during the Late Cretaceous","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Cretaceous; Geology; Paleomagnetism; Sea level; Paleontology; Polar; Apparent polar wander; Earth's rotation; Geodesy; Oceanography","score_opus":0.09508848105943771,"score_gpt":0.2761666590557154,"score_spread":0.1810781779962777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997411679","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99910575,0.0001119907,0.00005121512,0.000021319445,0.0000014045748,7.1264543e-7,0.00011129693,0.0000041755875,0.00059212634],"genre_scores_gemma":[0.9995944,0.00007044073,0.000057600428,0.0000058159335,0.0000026125667,9.411018e-7,0.000156684,0.0000012044409,0.000110376764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.0000068917725,0.0000036842382,0.00001218398,0.000010476767,0.0000132304685],"domain_scores_gemma":[0.99958485,0.000081787424,0.00019807449,0.000025410782,0.00006484639,0.000045116423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016730493,0.000100667436,0.00007642691,0.00079053047,0.00022684797,0.00028585922,0.00013494657,0.00015270876,0.0007395599],"category_scores_gemma":[0.001015898,0.00007690804,0.00005982377,0.0007775601,0.00044822242,0.0002561573,0.00022484707,0.00012936756,0.00009177352],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020437899,0.0000121043595,0.9746431,0.00002405532,0.000034558263,0.00042745424,0.0011414225,0.00066238054,0.0037953395,0.00042191357,0.00028197787,0.018351393],"study_design_scores_gemma":[0.0000020182317,0.000009957266,0.99943477,0.0000015299814,0.0000029309897,0.000063241336,0.00007927681,0.00012305431,0.000061568084,0.00006282242,0.00015746556,0.0000014445802],"about_ca_topic_score_codex":0.03197886,"about_ca_topic_score_gemma":0.07168359,"teacher_disagreement_score":0.03197886,"about_ca_system_score_codex":0.00042844977,"about_ca_system_score_gemma":0.00019483338,"threshold_uncertainty_score":0.0635854},"labels":[],"label_agreement":null},{"id":"W1997724502","doi":"10.1029/2002gl015243","title":"Freshening of the Labrador Sea surface waters in the 1990s: Another great salinity anomaly?","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Anomaly (physics); Oceanography; Geology; Salinity; Climatology","score_opus":0.0386094652440352,"score_gpt":0.2530067355441354,"score_spread":0.2143972703001002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1997724502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99709046,0.00033271065,0.000041587547,0.000716742,0.000007679955,0.0000022746156,0.00035295569,0.000014717759,0.001440844],"genre_scores_gemma":[0.99885297,0.0003430318,0.000052085463,0.00009587541,0.000016119451,8.7032544e-7,0.00035834758,0.000003056113,0.0002776804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.0000041422018,0.000005761165,0.000014699758,0.000008317998,0.000022005543],"domain_scores_gemma":[0.9997826,0.000010020117,0.000108907516,0.000015792988,0.000035067525,0.00004756093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021654429,0.00018922961,0.00024778603,0.0006120481,0.00027681506,0.00081150397,0.00022459682,0.00035878073,0.0013230174],"category_scores_gemma":[0.00049336697,0.00010414856,0.00035319204,0.0009054267,0.00039666388,0.00065428304,0.00051802467,0.0002750784,0.00017231275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024011539,0.000045051816,0.9694772,0.00006962373,0.000071609065,0.0003889697,0.0005732398,0.0008118268,0.0048533566,0.00077286887,0.0012764401,0.021419607],"study_design_scores_gemma":[0.0000052530017,0.000018518573,0.9978811,0.000009003035,0.000012924053,0.000054513268,0.00021750851,0.0002453089,0.0002849845,0.00009596334,0.0011716008,0.0000032296887],"about_ca_topic_score_codex":0.07769883,"about_ca_topic_score_gemma":0.14834505,"teacher_disagreement_score":0.9223012,"about_ca_system_score_codex":0.0012004165,"about_ca_system_score_gemma":0.00060226314,"threshold_uncertainty_score":0.15449315},"labels":[],"label_agreement":null},{"id":"W1998460057","doi":"10.1029/2008gl034154","title":"One‐decade trend analysis of stratospheric BrO over Harestua (60°N) and Lauder (45°S) reveals a decline","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Stratosphere; Bromine; Montreal Protocol; Troposphere; Environmental science; Ozone layer; Atmospheric sciences; Chlorofluorocarbon; Climatology; Trend analysis; Meteorology; Geography; Chemistry; Physics; Mathematics; Geology","score_opus":0.043510492065534916,"score_gpt":0.30128202861241965,"score_spread":0.2577715365468847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998460057","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997027,0.0001937879,0.00027634506,0.00004594183,0.00000558959,0.0000051564234,0.0012568216,0.000023003371,0.0011664592],"genre_scores_gemma":[0.99672097,0.0001429306,0.00035795817,0.000016610586,0.000003967561,0.0000060000557,0.0017192991,0.000004452935,0.0010277738],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999274,0.000006355496,0.0000042812794,0.000022474183,0.000014837722,0.000024632527],"domain_scores_gemma":[0.9995413,0.000053575306,0.00014556682,0.000030627416,0.00019509018,0.000033929857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021259912,0.00012675214,0.00013192356,0.0009263672,0.00018814746,0.0003316047,0.00015582329,0.0001349288,0.00075963006],"category_scores_gemma":[0.00041334587,0.00007961332,0.0001781668,0.0009034377,0.000103558625,0.00017675795,0.00018875067,0.0001402047,0.00014344782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014519335,0.000021148579,0.9685376,0.00004165596,0.00013287591,0.00012012561,0.00047853577,0.00062223664,0.010609559,0.00012503601,0.0006326107,0.018533412],"study_design_scores_gemma":[7.849578e-7,0.000019459334,0.9982168,0.0000021188628,0.000010235598,0.000021416823,0.00009541087,0.00015400536,0.00055851066,0.0000035832668,0.0009157937,0.0000018012867],"about_ca_topic_score_codex":0.12870586,"about_ca_topic_score_gemma":0.25492805,"teacher_disagreement_score":0.12870586,"about_ca_system_score_codex":0.00052222755,"about_ca_system_score_gemma":0.0004400958,"threshold_uncertainty_score":0.25591344},"labels":[],"label_agreement":null},{"id":"W1998480042","doi":"10.1029/2001gl013619","title":"The global magnetic field of Mars and implications for crustal evolution","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":282,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Association of Canadian Universities for Research in Astronomy","keywords":"Mars Exploration Program; Geology; Geophysics; Magnetization; Dynamo; Mantle (geology); Magnetic field; Astrobiology; Earth science; Physics","score_opus":0.028236484026521166,"score_gpt":0.32696032788112345,"score_spread":0.29872384385460227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998480042","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9417166,0.03217903,0.000695683,0.004183437,0.00004600936,0.0000038310777,0.00087575655,0.000035035504,0.020264618],"genre_scores_gemma":[0.9949287,0.0041028014,0.00019354447,0.0000829842,0.000054976303,0.0000015548175,0.0001839437,0.0000048407646,0.00044649045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999534,0.000011825369,0.0000023090313,0.000011998768,0.000007860944,0.0000126272125],"domain_scores_gemma":[0.99984264,0.000027134183,0.000044317923,0.00001077061,0.000039776445,0.00003528602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020900523,0.00018783163,0.00013435632,0.0009821412,0.00028524204,0.0009763309,0.00016899065,0.00027828105,0.0018922674],"category_scores_gemma":[0.0007466844,0.00008545057,0.000115528586,0.0010440303,0.00075938465,0.0007669408,0.00045781708,0.00031371092,0.00015722758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000464043,0.00003550296,0.5731799,0.0004534837,0.00022220059,0.0007192649,0.0021665397,0.006859972,0.015295002,0.034174956,0.0050533446,0.36137572],"study_design_scores_gemma":[0.000011732728,0.000050527928,0.9651932,0.00006478837,0.000033106637,0.00031025667,0.0007975892,0.000682688,0.00034203174,0.014762181,0.017737813,0.000014209415],"about_ca_topic_score_codex":0.0052975966,"about_ca_topic_score_gemma":0.0044348114,"teacher_disagreement_score":0.0052975966,"about_ca_system_score_codex":0.00078735343,"about_ca_system_score_gemma":0.00016573729,"threshold_uncertainty_score":0.010533512},"labels":[],"label_agreement":null},{"id":"W1998857608","doi":"10.1029/1999gl002353","title":"Basin scale estimates of sea surface nitrate and new production from remotely sensed sea surface temperature and chlorophyll","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Sea surface temperature; Structural basin; Environmental science; Nitrate; Phytoplankton; Oceanography; Chlorophyll a; Scale (ratio); Geology; Sea-surface height; Remote sensing; Climatology; Nutrient; Geomorphology; Geography; Ecology","score_opus":0.019962156486980142,"score_gpt":0.24066965387841324,"score_spread":0.2207074973914331,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1998857608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9642312,0.0014278557,0.02737416,0.00009288594,0.000017119313,0.00001959225,0.0013409778,0.00014471647,0.005351437],"genre_scores_gemma":[0.9795089,0.0007553938,0.017756378,0.000022746226,0.00001882812,0.000027591264,0.0011556754,0.000022439946,0.00073199644],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991894,0.000013607993,0.0000054097177,0.000033907185,0.00002293026,0.0000053389012],"domain_scores_gemma":[0.99974483,0.00008534502,0.000082420476,0.000023815777,0.000047645888,0.000015847882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025086847,0.00021294357,0.00017031874,0.0005504949,0.00012214582,0.00026901273,0.00014205222,0.00015773934,0.00059870526],"category_scores_gemma":[0.00080182264,0.00014233384,0.00014460858,0.00053046906,0.00015699868,0.0005878066,0.00035237242,0.00017237372,0.00015172368],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001527158,0.00012288977,0.6531273,0.0002589554,0.00034628305,0.00014242729,0.00028125645,0.05333612,0.09434419,0.0015441529,0.0017729804,0.1945707],"study_design_scores_gemma":[0.00001403766,0.000047770507,0.9336686,0.000020662714,0.000044201443,0.00011195402,0.000107551314,0.055853605,0.005836115,0.0016122784,0.0026600491,0.000023293056],"about_ca_topic_score_codex":0.004122817,"about_ca_topic_score_gemma":0.0113989785,"teacher_disagreement_score":0.004122817,"about_ca_system_score_codex":0.00021164409,"about_ca_system_score_gemma":0.00016357431,"threshold_uncertainty_score":0.008197665},"labels":[],"label_agreement":null},{"id":"W1999186212","doi":"10.1029/2003gl019405","title":"Electrical resistivity structure at the SAFOD site from magnetotelluric exploration","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Magnetotellurics; Geology; San andreas fault; Electrical resistivity and conductivity; Inversion (geology); Seismology; Electrical resistivity tomography; Geophysics; Petrology; Fault (geology); Tectonics","score_opus":0.034297020814609475,"score_gpt":0.2868371543259711,"score_spread":0.2525401335113616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999186212","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960556,0.000022224023,0.00021932798,0.00004337266,0.0000034314212,0.000003410034,0.0026064913,0.000025594923,0.001020489],"genre_scores_gemma":[0.98790354,0.000031654163,0.0008881605,0.000013641225,0.000009403953,0.0000058985306,0.01043624,0.000006694169,0.0007047385],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999137,0.000010795276,0.0000045340425,0.000022548864,0.00003064111,0.000017736129],"domain_scores_gemma":[0.9997485,0.00003094348,0.000047030473,0.000032275915,0.00010368055,0.000037529124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018044871,0.0001293419,0.00019205804,0.00068749493,0.00017902147,0.00021205412,0.00018745285,0.00020012545,0.0010559784],"category_scores_gemma":[0.00043072028,0.00008840074,0.00009916795,0.0007743989,0.00016111291,0.00018457942,0.00026261815,0.00016491693,0.00021843775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030302003,0.00015716141,0.9352303,0.000050136277,0.00006150563,0.0004825027,0.0003998633,0.0056522535,0.01598863,0.0005101824,0.004270674,0.03689371],"study_design_scores_gemma":[0.00002592911,0.000033532946,0.9919722,0.0000052865603,0.00000947374,0.00010902362,0.000096627075,0.0048880926,0.0008328789,0.000110722845,0.0019092701,0.00000690102],"about_ca_topic_score_codex":0.016327593,"about_ca_topic_score_gemma":0.04334961,"teacher_disagreement_score":0.016327593,"about_ca_system_score_codex":0.00026084116,"about_ca_system_score_gemma":0.00029554515,"threshold_uncertainty_score":0.0324651},"labels":[],"label_agreement":null},{"id":"W1999196794","doi":"10.1002/2014gl061838","title":"Substrate size and heterogeneity control anomalous transport in small streams","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Leading Edge Endowment Fund; National Science Foundation","keywords":"STREAMS; Hyporheic zone; Substrate (aquarium); Fluvial; Scaling; Biogeochemical cycle; Sediment transport; Hydrology (agriculture); Environmental science; Soil science; Sediment; Stream power; Benthic zone; Geology; Chemistry; Geomorphology; Environmental chemistry; Geotechnical engineering; Geometry","score_opus":0.016094550372186683,"score_gpt":0.2491576194507502,"score_spread":0.23306306907856353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999196794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997812,0.000010412949,0.00014955297,0.0000013597356,2.6020248e-7,0.000002143592,0.000011305565,0.000001954989,0.000041814583],"genre_scores_gemma":[0.99969935,0.000011746707,0.00020907554,0.0000020610341,4.2880023e-7,0.0000031549207,0.000028146545,0.0000014265723,0.000044591743],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99985385,0.000038316008,0.000014258725,0.00004658464,0.000023403238,0.000023519182],"domain_scores_gemma":[0.9994475,0.0002681223,0.0001272558,0.000031155498,0.000053347896,0.000072572715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035680138,0.00014921647,0.00024582562,0.00027038556,0.00030660914,0.00074816524,0.00019273716,0.0001516427,0.00042024037],"category_scores_gemma":[0.0007589155,0.00014978868,0.0001348447,0.00018385678,0.00041351904,0.00037453344,0.00029477637,0.00018481204,0.000034917535],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012178305,0.00020344557,0.29586142,0.000052787753,0.000057479374,0.00020546812,0.0002746134,0.005568927,0.69037455,0.00044921722,0.00006297127,0.0056712506],"study_design_scores_gemma":[0.00007720098,0.00076632755,0.85300314,0.000010383243,0.00005800467,0.00015195593,0.0003857898,0.041926105,0.102571435,0.0006614667,0.00036049337,0.000027695118],"about_ca_topic_score_codex":0.004047837,"about_ca_topic_score_gemma":0.0058534583,"teacher_disagreement_score":0.004047837,"about_ca_system_score_codex":0.00051684026,"about_ca_system_score_gemma":0.00025266685,"threshold_uncertainty_score":0.008048534},"labels":[],"label_agreement":null},{"id":"W1999204832","doi":"10.1029/2004gl020563","title":"High‐resolution gravity survey: Investigation of subsurface structures at Poás volcano, Costa Rica","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Environment Research Council; National Aeronautics and Space Administration","keywords":"Geology; Volcano; Impact crater; Bouguer anomaly; Digital elevation model; Magma; Terrain; Seismology; Geodesy; Elevation (ballistics); Intrusion; Magma chamber; Gravity anomaly; Caldera; Remote sensing; Geochemistry; Paleontology; Geometry; Cartography; Astrobiology","score_opus":0.03722160486719091,"score_gpt":0.2724111657657762,"score_spread":0.23518956089858528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999204832","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99742585,0.00012419342,0.00028164647,0.0000820521,9.85277e-7,0.00002285634,0.00030478495,0.00002612672,0.0017314007],"genre_scores_gemma":[0.99856216,0.0000948936,0.00070383016,0.000013524394,0.00000220071,0.000007569687,0.00025658854,0.000003441694,0.00035593263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999273,0.000016348971,0.0000037914365,0.000012482644,0.00002271712,0.000017344588],"domain_scores_gemma":[0.9998776,0.000014864898,0.00002811891,0.000019557661,0.00004211072,0.000017764216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001576314,0.00015771844,0.0001157382,0.0008190489,0.00032626963,0.0002689345,0.000241265,0.00023689665,0.0003175863],"category_scores_gemma":[0.00041757245,0.000111433124,0.000109474764,0.0010838065,0.0002617028,0.00020308435,0.0003921294,0.00011789896,0.00010309544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005578879,0.00008385775,0.9444112,0.000070813505,0.00005286542,0.00090841315,0.0019857942,0.0034635146,0.016298598,0.00034567202,0.0008535656,0.031469863],"study_design_scores_gemma":[0.0000026830091,0.000012385326,0.9964024,0.000003454626,0.0000043518107,0.000109071625,0.00037939945,0.0020344171,0.00024997618,0.000022716127,0.00077657733,0.0000025725612],"about_ca_topic_score_codex":0.12093072,"about_ca_topic_score_gemma":0.20677991,"teacher_disagreement_score":0.12093072,"about_ca_system_score_codex":0.000540509,"about_ca_system_score_gemma":0.00051574677,"threshold_uncertainty_score":0.24045366},"labels":[],"label_agreement":null},{"id":"W1999344872","doi":"10.1029/2003gl018982","title":"Ground‐based measurements of halogen oxides at the Hudson Bay by active longpath DOAS and passive MAX‐DOAS","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Meteorological and Oceanographic Society","funders":"","keywords":"Differential optical absorption spectroscopy; Bay; Ozone depletion; Ozone; Halogen; Environmental science; Atmospheric sciences; Bromine; Latitude; Absorption (acoustics); Meteorology; Chemistry; Geology; Oceanography; Optics; Physics; Geodesy","score_opus":0.02540239717951665,"score_gpt":0.26615661499225346,"score_spread":0.24075421781273681,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999344872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983911,0.000052755448,0.00027189023,0.000013530191,0.0000046056816,0.000009513516,0.0005196983,0.000021507478,0.00071529055],"genre_scores_gemma":[0.9967603,0.00008758407,0.001389423,0.000027377593,0.000006834178,0.000016521268,0.000802585,0.0000046898463,0.00090455817],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998938,0.0000088521265,0.0000037464322,0.000033762648,0.000036886253,0.000023071098],"domain_scores_gemma":[0.9998104,0.000018986882,0.000040014856,0.000012249784,0.00007311071,0.000045323923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017779837,0.0003662722,0.00017696335,0.0004953704,0.0003593546,0.00028236123,0.00028167854,0.00013239689,0.0005648722],"category_scores_gemma":[0.00021872348,0.00020295811,0.00009885459,0.0005167646,0.00023397358,0.00020901319,0.000360157,0.0002083677,0.00009975285],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039372474,0.00010973433,0.89965683,0.000045451896,0.00006406719,0.00013337682,0.00051541725,0.0003947455,0.08301595,0.00007352987,0.0004935434,0.015103638],"study_design_scores_gemma":[0.000018704863,0.000117918295,0.9927654,0.0000027641818,0.000019032917,0.00003281438,0.0002196092,0.0005544159,0.005539838,0.000017254799,0.00070749596,0.0000046883347],"about_ca_topic_score_codex":0.13395005,"about_ca_topic_score_gemma":0.2828708,"teacher_disagreement_score":0.86604995,"about_ca_system_score_codex":0.00081439415,"about_ca_system_score_gemma":0.0006045359,"threshold_uncertainty_score":0.26634073},"labels":[],"label_agreement":null},{"id":"W1999504515","doi":"10.1029/2009gl040777","title":"Longitudinally propagating arc wave in the pre‐onset optical aurora","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Space Agency; University of Calgary","funders":"","keywords":"Arc (geometry); Geology; Meteorology; Seismology; Optics; Physics; Engineering","score_opus":0.025717205905604744,"score_gpt":0.30355197498656344,"score_spread":0.2778347690809587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999504515","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974872,0.00010083964,0.0004360452,0.000025338213,0.000005136001,0.0000055866262,0.000092154245,0.000028018185,0.0018196824],"genre_scores_gemma":[0.9989115,0.000060592174,0.0005456147,0.000010820658,0.000013479117,0.000005301786,0.0001627961,0.000004561325,0.00028525622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996376,0.000003141531,0.0000015862928,0.000009226,0.000010321472,0.000011904734],"domain_scores_gemma":[0.99974316,0.000030533443,0.00011309983,0.000025157024,0.000046958063,0.000041025025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007614575,0.00010138426,0.000068435926,0.00047726367,0.0002438661,0.0002750249,0.0001505176,0.0001379983,0.00076886243],"category_scores_gemma":[0.00032216334,0.0000836544,0.00007858058,0.00030945655,0.00018972339,0.00027135012,0.00029828644,0.00021687051,0.00014572925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067353866,0.00009949472,0.75339663,0.00015375605,0.000049488313,0.0010991353,0.0011483959,0.0005853812,0.1669875,0.0012525781,0.0011171807,0.073436946],"study_design_scores_gemma":[0.000012771465,0.00011890364,0.99111056,0.000011666696,0.000018914698,0.00041369148,0.00020719925,0.00094672444,0.004855168,0.00019523613,0.0021028533,0.000006213455],"about_ca_topic_score_codex":0.0023411377,"about_ca_topic_score_gemma":0.0045533227,"teacher_disagreement_score":0.0023411377,"about_ca_system_score_codex":0.00017153473,"about_ca_system_score_gemma":0.0001172534,"threshold_uncertainty_score":0.004655063},"labels":[],"label_agreement":null},{"id":"W1999727510","doi":"10.1029/2002gl015816","title":"A new method for the quantitative identification of the composition, size and density of stratospheric aerosols from high resolution IR satellite measurements","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Aerosol; Environmental science; Satellite; Remote sensing; Trace gas; Atmospheric sciences; Atmosphere of Earth; Atmospheric composition; Stratosphere; Atmosphere (unit); Meteorology; Geology; Physics","score_opus":0.07421840928056286,"score_gpt":0.31867752038875824,"score_spread":0.24445911110819538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999727510","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.017825192,0.0034826796,0.9727687,0.00020136482,0.0005586217,0.00016711299,0.00075118337,0.0017833071,0.0024618062],"genre_scores_gemma":[0.0713014,0.0020075792,0.9198867,0.00023994649,0.00028044,0.00048512095,0.00048865547,0.00018635317,0.0051238327],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988096,0.0001514704,0.000041025,0.0002787038,0.00066561735,0.00005364116],"domain_scores_gemma":[0.99886334,0.0003559563,0.00015332071,0.00025108544,0.00031299863,0.00006319512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012002867,0.0006487815,0.00061811105,0.0027576971,0.0005372149,0.0006908249,0.0007751634,0.0007637612,0.0022249678],"category_scores_gemma":[0.0017870333,0.00062021625,0.0005538215,0.0012781243,0.0006468629,0.0014863302,0.0008530904,0.0014529902,0.0016421466],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013835337,0.00010005729,0.0035172456,0.00037928406,0.00013398215,0.00018519501,0.0001183846,0.0012322097,0.75514984,0.003945702,0.0035733632,0.23152636],"study_design_scores_gemma":[0.00015478043,0.00091960497,0.028819613,0.00008860085,0.00036670468,0.0059269248,0.0001233876,0.07383328,0.75543404,0.006701888,0.1272613,0.00036980506],"about_ca_topic_score_codex":0.0010137493,"about_ca_topic_score_gemma":0.0018647957,"teacher_disagreement_score":0.0027576971,"about_ca_system_score_codex":0.0003764898,"about_ca_system_score_gemma":0.0004985986,"threshold_uncertainty_score":0.007443309},"labels":[],"label_agreement":null},{"id":"W1999989774","doi":"10.1029/2005gl024926","title":"Comparisons of remote sensing retrievals and in situ measurements of aerosol fine mode fraction during ACE‐Asia","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"University of Maryland, Baltimore County; National Aeronautics and Space Administration","keywords":"Aerosol; Environmental science; In situ; Remote sensing; Mode (computer interface); Atmospheric sciences; Range (aeronautics); Meteorology; Materials science; Geology; Physics; Computer science","score_opus":0.03767587791021277,"score_gpt":0.3070740245932438,"score_spread":0.269398146683031,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W1999989774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981779,0.000035026034,0.00034338317,0.0000070787232,0.000005747113,0.000004269645,0.00047772046,0.000029349112,0.0009196459],"genre_scores_gemma":[0.9981439,0.000035786186,0.0006320856,0.000010601423,0.0000065376234,0.0000062648755,0.0009523981,0.000008435354,0.00020409763],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998853,0.000007756557,0.000008861334,0.000040703555,0.000032850774,0.00002445419],"domain_scores_gemma":[0.99964714,0.00009471148,0.00006845247,0.00003741326,0.00011634346,0.00003606435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003106422,0.00035696043,0.0003058349,0.00043590638,0.00023858903,0.00035556604,0.00028421675,0.00025082208,0.0004856634],"category_scores_gemma":[0.00054884166,0.00018317925,0.0002211069,0.00027874627,0.0001320722,0.00031067213,0.00013267416,0.00018600553,0.00010427327],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018848393,0.00044236417,0.528726,0.00019572153,0.00038428392,0.00035944206,0.0007585474,0.0075644557,0.42686665,0.00019356412,0.000766253,0.031857908],"study_design_scores_gemma":[0.000025913918,0.00012387718,0.95792645,0.0000059685794,0.000068846326,0.00011391864,0.00011901864,0.006068816,0.034969576,0.000032545955,0.00053048733,0.000014535074],"about_ca_topic_score_codex":0.016319387,"about_ca_topic_score_gemma":0.021388326,"teacher_disagreement_score":0.016319387,"about_ca_system_score_codex":0.00033795077,"about_ca_system_score_gemma":0.00014391281,"threshold_uncertainty_score":0.03244883},"labels":[],"label_agreement":null},{"id":"W2000042998","doi":"10.1029/2001gl012838","title":"Observations of an intense anticyclonic warm eddy in the Newfoundland Basin","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique","keywords":"Anticyclone; Eddy; Geology; Thermohaline circulation; Oceanography; Hydrography; Temperature salinity diagrams; Climatology; Dynamic height; Hydrographic survey; Boundary current; Anomaly (physics); Structural basin; Latitude; Sea-surface height; Ocean current; Salinity; Sea surface temperature; Meteorology; Geography; Geodesy; Turbulence; Geomorphology","score_opus":0.0555470792982066,"score_gpt":0.29910308870925273,"score_spread":0.24355600941104613,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000042998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989712,0.00009294347,0.000025782454,0.000055658722,0.0000026524513,0.0000032145056,0.000262038,0.0000045189217,0.0005819291],"genre_scores_gemma":[0.9983248,0.00020948214,0.00011591309,0.00005262387,0.000007193841,0.0000068574755,0.0004794952,0.0000021510082,0.0008014912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987495,0.0000074236837,0.000008003434,0.000024788462,0.00002940874,0.000055339842],"domain_scores_gemma":[0.99951637,0.000044905362,0.00017276316,0.000024352,0.0001216733,0.00011996115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020580951,0.0001507638,0.00015683648,0.0006305273,0.0008026758,0.00065602234,0.0002292812,0.00024833163,0.00057251],"category_scores_gemma":[0.0005675134,0.00016718628,0.0000790795,0.00055723917,0.00041205407,0.00026586908,0.00051639753,0.00024002099,0.00009005133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091466456,0.000048722643,0.98024166,0.000031742427,0.000054885917,0.00050002424,0.0011660788,0.0003275368,0.006307473,0.00005315902,0.0014378651,0.009739354],"study_design_scores_gemma":[0.0000012878068,0.000005017834,0.99932194,0.0000032443922,0.0000037374468,0.000024414996,0.00011891778,0.000050793344,0.00006721194,0.0000013406866,0.00040088236,0.000001374918],"about_ca_topic_score_codex":0.74072164,"about_ca_topic_score_gemma":0.91890776,"teacher_disagreement_score":0.25927836,"about_ca_system_score_codex":0.0033256016,"about_ca_system_score_gemma":0.0013188218,"threshold_uncertainty_score":0.52161056},"labels":[],"label_agreement":null},{"id":"W2000398211","doi":"10.1029/2005gl025035","title":"A structural study of an interior layered deposit in southwestern Candor Chasma, Valles Marineris, Mars, using high resolution stereo camera data from Mars Express","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"3M (Canada); Brock University","funders":"","keywords":"Mars Exploration Program; Geology; Sedimentary depositional environment; Lithology; High resolution; Fault (geology); Basement; Geomorphology; Paleontology; Astrobiology; Remote sensing; Structural basin; Archaeology; Physics; Geography","score_opus":0.067184043252572,"score_gpt":0.3155958209661949,"score_spread":0.24841177771362288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000398211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987614,0.0000526743,0.00008095422,0.000006399424,8.841979e-7,0.0000063673724,0.00030190367,0.00000668479,0.0007827063],"genre_scores_gemma":[0.99858665,0.00005770398,0.0006159683,0.0000053258013,0.0000027472825,0.0000034742814,0.00045953793,0.0000036271044,0.00026493453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999019,0.0000043502187,0.0000048542465,0.000024926623,0.00004251998,0.0000214303],"domain_scores_gemma":[0.9997516,0.000019682931,0.00007212389,0.000024197907,0.000074229705,0.00005811135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010138611,0.00017381838,0.00015297196,0.0016202296,0.000701665,0.00051311555,0.00031151652,0.00024143896,0.0008155039],"category_scores_gemma":[0.00035875046,0.00022855659,0.0001501333,0.0012457168,0.00041517607,0.00015056311,0.00039798403,0.00016494839,0.00018233585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016943974,0.00005983532,0.93187124,0.00007107701,0.000074250616,0.00093313656,0.0013268591,0.0005420236,0.040128216,0.00007851947,0.0003321247,0.024413237],"study_design_scores_gemma":[0.0000015829459,0.000012103897,0.999108,0.0000027816668,0.0000043763634,0.0001306863,0.00012243904,0.00017847087,0.00022913249,0.00000195716,0.0002069783,0.0000014208854],"about_ca_topic_score_codex":0.11902046,"about_ca_topic_score_gemma":0.32605872,"teacher_disagreement_score":0.11902046,"about_ca_system_score_codex":0.0005289309,"about_ca_system_score_gemma":0.00048975786,"threshold_uncertainty_score":0.23665535},"labels":[],"label_agreement":null},{"id":"W2000438450","doi":"10.1029/2001gl013173","title":"Observational evidence for the role of denitrification in Arctic stratospheric ozone loss","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Denitrification; Stratosphere; Environmental science; Ozone; Atmospheric sciences; Arctic; Climatology; Ozone depletion; Polar vortex; Ozone layer; Meteorology; Oceanography; Chemistry; Nitrogen; Geology; Geography","score_opus":0.1160117114263365,"score_gpt":0.33976241642880106,"score_spread":0.22375070500246458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000438450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99857724,0.00026081494,0.00021983503,0.00009521113,0.0000026930868,0.0000018460203,0.000111879905,0.0000044528633,0.00072594424],"genre_scores_gemma":[0.9995245,0.00015912966,0.000073183684,0.000014178323,0.000004739027,8.9132556e-7,0.00016647278,8.91113e-7,0.000056112254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981314,0.00005355253,0.000020553709,0.000037328155,0.00004059851,0.00003482972],"domain_scores_gemma":[0.9981589,0.0005811568,0.000607549,0.00014554278,0.0003761164,0.00013072275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009887122,0.00014197516,0.0001213279,0.00028927834,0.00029035483,0.00043162145,0.00017002749,0.00024869345,0.00041127647],"category_scores_gemma":[0.0020230024,0.00016000055,0.00012601328,0.00025885995,0.00029285724,0.00023639305,0.00035146959,0.00023242718,0.000066044966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020516984,0.000027486129,0.9871459,0.000029229017,0.00006793617,0.000053776337,0.0002461362,0.00068058056,0.0070236567,0.00014547388,0.00010725435,0.004267345],"study_design_scores_gemma":[0.0000020079947,0.000014475815,0.9986505,0.000004371186,0.000010818264,0.000022296228,0.000072648705,0.0005408397,0.00037024263,0.000042759202,0.00026757017,0.0000014990915],"about_ca_topic_score_codex":0.027065141,"about_ca_topic_score_gemma":0.033101786,"teacher_disagreement_score":0.027065141,"about_ca_system_score_codex":0.0003235981,"about_ca_system_score_gemma":0.00027297216,"threshold_uncertainty_score":0.053815186},"labels":[],"label_agreement":null},{"id":"W2000713434","doi":"10.1029/2008gl035757","title":"Interaction between kinetic ballooning perturbation and thin current sheet: Quasi‐electrostatic field, local onset, and global characteristics","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Canadian Space Agency","funders":"","keywords":"Ballooning; Substorm; Physics; Perturbation (astronomy); Current sheet; Current (fluid); Plasma sheet; Kinetic energy; Mechanics; Plasma; Classical mechanics; Magnetosphere; Magnetohydrodynamics","score_opus":0.018095769352250986,"score_gpt":0.29806814426405887,"score_spread":0.2799723749118079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000713434","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990978,0.00003900686,0.00025415665,0.000012288589,0.0000018266227,0.0000028013492,0.000017562916,0.0000104080555,0.0005641511],"genre_scores_gemma":[0.9997738,0.000011534633,0.00011368542,0.0000038598428,0.0000043908053,0.0000014171726,0.000025236852,0.0000011228049,0.00006494239],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996114,0.0000046306695,0.0000016018618,0.000007098521,0.0000114883305,0.000014174078],"domain_scores_gemma":[0.99975556,0.000047228972,0.00010490594,0.000021400085,0.000023581528,0.00004738489],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008224329,0.00011509416,0.00017732549,0.00033238746,0.00021590681,0.00025051998,0.00013096946,0.0001850254,0.00053424557],"category_scores_gemma":[0.0003002546,0.00008241853,0.00010332889,0.00023568417,0.00024141386,0.00019437766,0.00029927774,0.00021119374,0.000067578454],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010635438,0.00012541743,0.49306688,0.0000766915,0.00012611199,0.0043641683,0.001038374,0.0032472857,0.4748278,0.0009766163,0.0005138641,0.020573292],"study_design_scores_gemma":[0.000018794277,0.00027061347,0.9769645,0.0000067882957,0.000037647373,0.0011663891,0.0003285205,0.0072240024,0.013189466,0.00025538277,0.00052360224,0.000014194244],"about_ca_topic_score_codex":0.0009669979,"about_ca_topic_score_gemma":0.0011662563,"teacher_disagreement_score":0.0009669979,"about_ca_system_score_codex":0.0001486806,"about_ca_system_score_gemma":0.00005243466,"threshold_uncertainty_score":0.0019227862},"labels":[],"label_agreement":null},{"id":"W2000785775","doi":"10.1029/2001gl013827","title":"A coupled atmospheric‐hydrological modeling study of the 1996 Ha! Ha! River basin flash flood in Québec, Canada","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Compute Canada; McGill University","funders":"","keywords":"Hydrograph; Flash flood; Hydrology (agriculture); Routing (electronic design automation); Flood myth; Drainage basin; Precipitation; Environmental science; Structural basin; Flood forecasting; Geology; Hydrological modelling; Rain gauge; Meteorology; Climatology; Geomorphology; Geography; Cartography","score_opus":0.02706574374916787,"score_gpt":0.24353380797041757,"score_spread":0.2164680642212497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000785775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99424183,0.000119646946,0.0003197765,0.00042839252,0.000013647382,0.000047591635,0.0027233458,0.00006189574,0.0020439697],"genre_scores_gemma":[0.99492586,0.00014098463,0.0007400358,0.000081595106,0.000007941166,0.00003735842,0.002019396,0.000021596974,0.00202518],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999818,0.00003486319,0.000008380662,0.000044760272,0.000029725912,0.00006434448],"domain_scores_gemma":[0.99955124,0.00008445366,0.00003711267,0.000025032425,0.00020219987,0.0001000313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003755827,0.00047572915,0.00032639096,0.00046671723,0.0015419605,0.0010734812,0.0014467108,0.0008564533,0.0025968195],"category_scores_gemma":[0.0010201834,0.00038033695,0.00040951473,0.0011372388,0.00055163674,0.0006570425,0.00042092736,0.0006554058,0.0002772625],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005679602,0.0012045862,0.38132012,0.00016351874,0.00064870116,0.0013713235,0.0014741464,0.5570103,0.004685122,0.0037443072,0.021765696,0.026044289],"study_design_scores_gemma":[0.00031628466,0.00009959107,0.25788325,0.00004186202,0.00016640728,0.000058839873,0.0017052606,0.73088443,0.0009477185,0.00043630385,0.007334112,0.00012584233],"about_ca_topic_score_codex":0.99447674,"about_ca_topic_score_gemma":0.9935469,"teacher_disagreement_score":0.02979902,"about_ca_system_score_codex":0.02979902,"about_ca_system_score_gemma":0.01221572,"threshold_uncertainty_score":0.21620804},"labels":[],"label_agreement":null},{"id":"W2000833069","doi":"10.1029/2007gl031124","title":"Low temperature dependence of electrical resistivity: Implications for near surface geophysical monitoring","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":258,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Petrophysics; Electrical resistivity and conductivity; Saturation (graph theory); Conductivity; Geophysics; Electrical resistivity tomography; Atmospheric temperature range; Soil science; Materials science; Mineralogy; Geology; Thermodynamics; Porosity; Chemistry; Physics; Composite material","score_opus":0.041212556900311496,"score_gpt":0.34048353298530604,"score_spread":0.29927097608499453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000833069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6627089,0.013843198,0.29370916,0.008965988,0.00058725034,0.000092446535,0.0016582642,0.0017956105,0.016639275],"genre_scores_gemma":[0.9707912,0.003443073,0.023311019,0.00027894264,0.00016145116,0.00002814849,0.00025697326,0.00008395401,0.0016452085],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9996276,0.00011803711,0.000019260155,0.00010901698,0.00009507324,0.00003098323],"domain_scores_gemma":[0.99791235,0.0008759124,0.00038541245,0.00031096567,0.0004262538,0.000089130896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096380396,0.00038722635,0.00050885935,0.0005905193,0.0002442894,0.0010930835,0.0008480376,0.0010861363,0.0010906237],"category_scores_gemma":[0.0049535176,0.00024954093,0.0001911218,0.0010386632,0.0007371433,0.0019353284,0.00051746826,0.0009733972,0.0004903252],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053062587,0.0004256483,0.2094733,0.0009956345,0.000090152425,0.0013225912,0.0006716137,0.093427956,0.43533385,0.020917699,0.006204831,0.2306061],"study_design_scores_gemma":[0.0000557472,0.0006644891,0.20340006,0.0002767497,0.00013849454,0.003187398,0.0013644915,0.50485265,0.2008958,0.06311491,0.021782355,0.00026688774],"about_ca_topic_score_codex":0.0021133309,"about_ca_topic_score_gemma":0.0018273062,"teacher_disagreement_score":0.0021133309,"about_ca_system_score_codex":0.00038552296,"about_ca_system_score_gemma":0.0002464501,"threshold_uncertainty_score":0.005097151},"labels":[],"label_agreement":null},{"id":"W2000927013","doi":"10.1029/2007gl029756","title":"Uptake of NO<sub>3</sub> on soot and pyrene surfaces","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Soot; Pyrene; Methane; Atmosphere (unit); Hexane; Chemistry; Environmental chemistry; Organic chemistry; Combustion; Thermodynamics; Physics","score_opus":0.02606122034359168,"score_gpt":0.26931768105125603,"score_spread":0.24325646070766435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2000927013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986903,0.00013773068,0.00054758496,0.000013505699,0.000005427141,0.000008201853,0.00007325669,0.000011078718,0.00051282614],"genre_scores_gemma":[0.99806803,0.00015402134,0.0007801474,0.00001014717,0.0000026222683,0.0000065653653,0.00011464203,0.00000776968,0.0008560905],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998266,0.00002187466,0.000005715725,0.00004337061,0.000054376884,0.000048126712],"domain_scores_gemma":[0.9998043,0.00009336403,0.00003106395,0.000014245216,0.000039096107,0.000017950957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017949632,0.00029217842,0.00027017377,0.00013246103,0.00025384835,0.00032920513,0.0002419494,0.00028636304,0.00084954716],"category_scores_gemma":[0.00041066197,0.00014623246,0.00025857872,0.0000811746,0.00024259108,0.00026980537,0.00019417389,0.00021244673,0.00019385626],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008757448,0.0000073925194,0.00087823556,0.000028719674,0.000005057864,0.000030662333,0.000027036793,0.00017465967,0.99793327,0.000047641355,0.000013483188,0.00076623895],"study_design_scores_gemma":[0.0000030120093,0.00011659482,0.00565645,0.0000021971553,0.000008105565,0.000037890648,0.00004041771,0.002235301,0.9915662,0.000028201583,0.00030101518,0.00000468604],"about_ca_topic_score_codex":0.007528552,"about_ca_topic_score_gemma":0.0050349166,"teacher_disagreement_score":0.007528552,"about_ca_system_score_codex":0.0005316227,"about_ca_system_score_gemma":0.00024181978,"threshold_uncertainty_score":0.014969468},"labels":[],"label_agreement":null},{"id":"W2001147321","doi":"10.1029/2009gl040150","title":"On the formation of high‐latitude soil carbon stocks: Effects of cryoturbation and insulation by organic matter in a land surface model","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":201,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"Agence Nationale de la Recherche; Natural Environment Research Council; Sight Research UK; Impact Fund","keywords":"Permafrost; Soil carbon; Environmental science; Carbon fibers; Soil water; Soil organic matter; Soil science; Carbon cycle; Carbon sequestration; Geology; Atmospheric sciences; Carbon dioxide; Materials science; Ecosystem; Ecology; Oceanography","score_opus":0.021813543058270424,"score_gpt":0.2538951783996425,"score_spread":0.23208163534137205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001147321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9743492,0.00023603716,0.014309968,0.0008346978,0.00005070025,0.00003094761,0.00057803496,0.00019068079,0.009419627],"genre_scores_gemma":[0.99644756,0.00012042477,0.001332736,0.000084131556,0.000014909972,0.000041178744,0.00017854017,0.00005538443,0.0017250143],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985874,0.00004612331,0.000006891323,0.000026122547,0.000017081305,0.000045028748],"domain_scores_gemma":[0.9992686,0.00030677594,0.00010368752,0.000049730934,0.00008772512,0.00018353575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042770072,0.0007322053,0.00092030136,0.00050378963,0.0008915849,0.0014600744,0.0012718872,0.0019986036,0.0024133998],"category_scores_gemma":[0.0015574804,0.0005372308,0.0011180759,0.0005004875,0.0013419318,0.0012540694,0.0011512169,0.00093824154,0.0002362412],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000644978,0.000028639812,0.002337896,0.000014499825,0.00002472471,0.00006984824,0.000017906412,0.9926076,0.0013951529,0.002868586,0.00013273134,0.0004380105],"study_design_scores_gemma":[0.000057063695,0.000026424299,0.0010760005,0.0000031026634,0.000017013286,0.000007648425,0.00001821741,0.9972904,0.00021515126,0.001163175,0.00011507983,0.0000107347705],"about_ca_topic_score_codex":0.049546834,"about_ca_topic_score_gemma":0.017703034,"teacher_disagreement_score":0.049546834,"about_ca_system_score_codex":0.0017394198,"about_ca_system_score_gemma":0.0015690081,"threshold_uncertainty_score":0.09851688},"labels":[],"label_agreement":null},{"id":"W2001393574","doi":"10.1029/2006gl026794","title":"Cloudless aerosol forcing efficiency in the UV region from AERONET and WOUDC databases","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Air Canada","funders":"","keywords":"AERONET; Aerosol; Environmental science; Forcing (mathematics); Atmospheric sciences; Climatology; Meteorology; Geography; Physics; Geology","score_opus":0.0325110527788559,"score_gpt":0.28497900282738153,"score_spread":0.2524679500485256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001393574","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3628686,0.00089067017,0.0035178966,0.00004801972,0.000021571812,0.00019155222,0.6218774,0.0013466983,0.009237675],"genre_scores_gemma":[0.2663957,0.00044292843,0.008800044,0.000030160147,0.000020004836,0.00023082821,0.72263765,0.00015111385,0.0012915577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990243,0.00006989227,0.00020431972,0.00021382282,0.00039859416,0.00008900515],"domain_scores_gemma":[0.9983076,0.00035015942,0.0003822672,0.00033924798,0.000526841,0.00009394199],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000921932,0.00057033665,0.00067068567,0.0065462636,0.00031420033,0.0011172551,0.0008588654,0.0003959553,0.0031124789],"category_scores_gemma":[0.0034271,0.00017384822,0.00056510005,0.0068071033,0.00010758896,0.00078322494,0.00055626937,0.00021517456,0.0014866302],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097113044,0.00019725376,0.76214814,0.0017175615,0.0013946214,0.00059508445,0.00029891395,0.03873769,0.009514384,0.0014209647,0.059097968,0.12390632],"study_design_scores_gemma":[0.00019389617,0.000054835797,0.8966597,0.00011045677,0.00032188516,0.0003799285,0.00015837587,0.03358904,0.008188963,0.00072466454,0.059542883,0.00007541447],"about_ca_topic_score_codex":0.04675982,"about_ca_topic_score_gemma":0.0500649,"teacher_disagreement_score":0.04675982,"about_ca_system_score_codex":0.00079853315,"about_ca_system_score_gemma":0.0007107831,"threshold_uncertainty_score":0.09297526},"labels":[],"label_agreement":null},{"id":"W2001586852","doi":"10.1029/2008gl034352","title":"Extreme longitudinal disturbances in the mesosphere and thermosphere observed with the Wind Imaging Interferometer on UARS","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Thermosphere; Mesosphere; Interferometry; Atmospheric sciences; Atmospheric tide; Geology; Geophysics; Ionosphere; Environmental science; Physics; Remote sensing; Meteorology; Astronomy; Stratosphere","score_opus":0.049038657022840326,"score_gpt":0.268895754164369,"score_spread":0.21985709714152868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001586852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904066,0.000035521673,0.00010984322,0.00001630559,0.000004350594,0.000004647917,0.0003310891,0.000016103364,0.00044151634],"genre_scores_gemma":[0.99897087,0.000029744378,0.00023321272,0.0000095068735,0.000008469325,0.000004039223,0.0006477424,0.000002315155,0.00009405103],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987376,0.000015843065,0.000009558587,0.000020183856,0.00004400692,0.000036626054],"domain_scores_gemma":[0.9996075,0.000030073765,0.00016886393,0.000042901404,0.00006155149,0.00008904625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000226742,0.00015641071,0.0001669924,0.0006834011,0.0002766077,0.00023703405,0.00014431958,0.00021149118,0.00036872583],"category_scores_gemma":[0.00045890262,0.00009648164,0.00014464084,0.0005627576,0.00017071661,0.00017008164,0.00027055343,0.00021948243,0.00009726685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023037587,0.00008332624,0.9643751,0.00001559169,0.00008381879,0.0005894316,0.0003538774,0.0007687644,0.021252051,0.00011198868,0.00085780886,0.011277804],"study_design_scores_gemma":[0.000004058301,0.000030397576,0.99837273,0.00000153038,0.000004986557,0.00009435685,0.00004600669,0.0004233427,0.00062566117,0.000011335825,0.00038314093,0.0000024317978],"about_ca_topic_score_codex":0.00802413,"about_ca_topic_score_gemma":0.017036876,"teacher_disagreement_score":0.00802413,"about_ca_system_score_codex":0.00024885402,"about_ca_system_score_gemma":0.00016001916,"threshold_uncertainty_score":0.015954852},"labels":[],"label_agreement":null},{"id":"W2001802061","doi":"10.1029/1999gl011069","title":"Low mantle heat flow at the edge of the North American Continent, Voisey Bay, Labrador","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National de la Recherche Scientifique","keywords":"Geology; Mantle (geology); Bay; Archean; Shield; Heat flow; Crust; Rift; Geochemistry; Oceanography; Drilling; Geomorphology; Structural basin; Petrology; Thermal; Geography; Meteorology","score_opus":0.014567158739539825,"score_gpt":0.2341049703768699,"score_spread":0.21953781163733008,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001802061","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997214,0.000118962,0.00003896831,0.00006736889,0.0000018965292,0.0000027199837,0.0005036186,0.000012530481,0.0020399606],"genre_scores_gemma":[0.99824715,0.00008979721,0.00014077108,0.00001694984,0.0000018778186,0.0000031925351,0.0005595152,0.0000060684984,0.0009346008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999858,0.000009056783,0.0000041776557,0.000038684804,0.000027546826,0.000062535975],"domain_scores_gemma":[0.9998275,0.00001331455,0.000030072611,0.000009931233,0.00008298002,0.0000362746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012775115,0.00016466521,0.00023037227,0.0011275918,0.001579961,0.0010108352,0.0005269872,0.00018880448,0.0012430027],"category_scores_gemma":[0.00042362948,0.00016422413,0.00013134153,0.0010499351,0.00069799385,0.0003333954,0.00058016053,0.00020079347,0.00018125316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018922494,0.000026921141,0.9621389,0.00005499748,0.00008409396,0.00034926436,0.003395507,0.00063815207,0.0145588955,0.00056039763,0.001253808,0.01674981],"study_design_scores_gemma":[0.000004842959,0.000006797379,0.99740845,0.000008833274,0.000010935321,0.00003639501,0.00082923734,0.0001452569,0.0005207997,0.000027249296,0.0009961479,0.000005112521],"about_ca_topic_score_codex":0.8900243,"about_ca_topic_score_gemma":0.9565159,"teacher_disagreement_score":0.109975696,"about_ca_system_score_codex":0.004306113,"about_ca_system_score_gemma":0.0031425026,"threshold_uncertainty_score":0.22124666},"labels":[],"label_agreement":null},{"id":"W2001843910","doi":"10.1002/2014gl062960","title":"Rapid disappearance of perennial ice on Canada's most northern lake","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; Université de Montréal; Université Laval; Center for Northern Studies","funders":"","keywords":"Perennial plant; Geology; Advection; Melt pond; Shelf ice; Arctic ice pack; Cryosphere; Physical geography; Climatology; Sea ice; Ice shelf; Oceanography; Geography","score_opus":0.03033098816293212,"score_gpt":0.2569177804610248,"score_spread":0.2265867922980927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001843910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968541,0.00019013238,0.00006472865,0.00015922298,0.0000043377695,0.0000047423673,0.0005486395,0.00001499869,0.0021590113],"genre_scores_gemma":[0.9987386,0.00009090893,0.00007839965,0.00002998402,0.0000019723375,0.0000019153742,0.00039064503,0.000002405157,0.00066501234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.000005051518,0.0000059420017,0.000026803256,0.00009007928,0.00007037374],"domain_scores_gemma":[0.999419,0.000025556112,0.000101863785,0.000015380949,0.00030338028,0.00013493962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021754713,0.00013156339,0.00022394164,0.00094229315,0.0019236708,0.0011504671,0.00041096527,0.0002142431,0.0010207132],"category_scores_gemma":[0.0006093848,0.00014915588,0.00012090578,0.0010152961,0.00073299074,0.00036185663,0.0005325952,0.00032119057,0.00008901911],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024271388,0.000032712323,0.9470702,0.000113088245,0.00007755189,0.00045185047,0.0030678003,0.0008924773,0.012801936,0.0005007359,0.0040790257,0.03066982],"study_design_scores_gemma":[0.0000016339143,0.0000057117495,0.99713314,0.000008737264,0.0000053219965,0.000033930206,0.0005754281,0.00033920386,0.00048110372,0.000019459945,0.001392058,0.0000042676093],"about_ca_topic_score_codex":0.93193996,"about_ca_topic_score_gemma":0.98234355,"teacher_disagreement_score":0.06806004,"about_ca_system_score_codex":0.008939446,"about_ca_system_score_gemma":0.007927355,"threshold_uncertainty_score":0.13692164},"labels":[],"label_agreement":null},{"id":"W2001844234","doi":"10.1029/2004gl021466","title":"Nonmigrating tides in equinox temperature fields from the Extended Canadian Middle Atmosphere Model (CMAM)","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University; University of New Brunswick","funders":"","keywords":"Equinox; Atmospheric tide; Atmosphere (unit); Atmospheric sciences; Airglow; Amplitude; Mesosphere; Geology; Convection; Solstice; Tidal Waves; Troposphere; Geophysics; Atmospheric model; Superposition principle; Climatology; Thermosphere; Ionosphere; Physics; Meteorology; Stratosphere; Geodesy; Latitude; Oceanography","score_opus":0.02185355343635844,"score_gpt":0.27120671209010677,"score_spread":0.24935315865374832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001844234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9548472,0.0003999414,0.005017648,0.0006539985,0.0001483402,0.00007447343,0.028154455,0.0011731939,0.009530857],"genre_scores_gemma":[0.9683796,0.00019379958,0.004120895,0.00008697136,0.000022173434,0.000045533696,0.024799002,0.00018862325,0.0021633797],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981934,0.000025634074,0.000007457039,0.00003883971,0.000060265622,0.000048376965],"domain_scores_gemma":[0.9995567,0.000068607966,0.00003132776,0.000035859746,0.00023394778,0.000073572475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040560568,0.0006140554,0.00033931198,0.0004510528,0.001161656,0.000948296,0.0017346548,0.00057627686,0.002568915],"category_scores_gemma":[0.0015246281,0.00040014368,0.00062453636,0.0010275691,0.000373177,0.000507623,0.00043971173,0.00085441116,0.00043239136],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005370428,0.0001646869,0.06884812,0.000112759604,0.00036417058,0.00015989991,0.00018558002,0.88750315,0.0038599693,0.0032784042,0.015922261,0.01906395],"study_design_scores_gemma":[0.0002681598,0.000052585492,0.10146709,0.000024386964,0.00010400278,0.00004614338,0.00010081612,0.8840731,0.0017579282,0.00091697223,0.011083568,0.000105194114],"about_ca_topic_score_codex":0.92647445,"about_ca_topic_score_gemma":0.93996966,"teacher_disagreement_score":0.92647445,"about_ca_system_score_codex":0.0056700376,"about_ca_system_score_gemma":0.0061111217,"threshold_uncertainty_score":0.14791703},"labels":[],"label_agreement":null},{"id":"W2001897470","doi":"10.1029/2005gl025321","title":"Model investigation of the Slope Water, north of the Gulf Stream","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"Los Alamos National Laboratory; Centre National d’Etudes Spatiales","keywords":"Gulf Stream; Geology; Oceanography; Environmental science","score_opus":0.025145432944255836,"score_gpt":0.23206557991909546,"score_spread":0.20692014697483962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2001897470","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99721247,0.000029485804,0.0005202199,0.00008691911,0.000008207206,0.000011301678,0.00074269495,0.000036913432,0.001351708],"genre_scores_gemma":[0.9975599,0.000035003683,0.0006618683,0.000026825563,0.000004947416,0.0000204991,0.0011932352,0.00001554666,0.00048214346],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990416,0.000025565592,0.0000063544458,0.000030828378,0.000014655066,0.00001852005],"domain_scores_gemma":[0.999648,0.00014935988,0.00004677665,0.00004088345,0.00006358034,0.000051267303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031091212,0.0004777184,0.0004980811,0.0003734747,0.0005338081,0.00073842675,0.0008086024,0.0012272566,0.001592572],"category_scores_gemma":[0.001055395,0.00042639012,0.0006227701,0.00043623103,0.0007063309,0.0005187362,0.0003862353,0.00072321395,0.00016696643],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016442203,0.0001341073,0.025040848,0.000026069287,0.0000837491,0.00013135262,0.000050734765,0.9705557,0.001941075,0.00043759696,0.00038638906,0.0010480175],"study_design_scores_gemma":[0.000106204774,0.00008968577,0.014469423,0.0000055045807,0.00003209846,0.000023748595,0.000055559158,0.984063,0.0006266733,0.00017610284,0.00033976094,0.000012184678],"about_ca_topic_score_codex":0.069945455,"about_ca_topic_score_gemma":0.050462566,"teacher_disagreement_score":0.069945455,"about_ca_system_score_codex":0.0012809345,"about_ca_system_score_gemma":0.00092478504,"threshold_uncertainty_score":0.13907665},"labels":[],"label_agreement":null},{"id":"W2002056853","doi":"10.1029/2000gl012828","title":"Correction to “Subevent structure of large earthquakes—A ground‐motion perspective”","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Sensor Technology","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":false,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Citation; Ground motion; Perspective (graphical); Library science; State (computer science); Common ground; History; Art history; Geology; Computer science; Sociology; Artificial intelligence; Seismology; Algorithm","score_opus":0.014737577347503432,"score_gpt":0.2834845942743611,"score_spread":0.2687470169268577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002056853","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.007489928,0.0037126183,0.03264128,0.061274566,0.8808615,0.00008224527,0.0048503056,0.0048118723,0.004275672],"genre_scores_gemma":[0.29268202,0.012129613,0.064965434,0.05836383,0.38579628,0.00039840574,0.016632123,0.0072859796,0.16174625],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9987978,0.00025078488,0.00024596546,0.00021992615,0.00034892393,0.00013658259],"domain_scores_gemma":[0.97801876,0.0030812162,0.001605427,0.003110006,0.0131948935,0.0009896538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017318554,0.001440945,0.0012487033,0.0024943312,0.0013728903,0.0016988702,0.002943977,0.0034184144,0.029599797],"category_scores_gemma":[0.04248862,0.0008512642,0.0011175307,0.003219834,0.0007615598,0.0014936237,0.001502058,0.0045435834,0.01225538],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026019497,0.000016263457,0.0015528464,0.0003529144,0.00009155443,0.0005343626,0.000104929044,0.0013237945,0.0007692893,0.002725603,0.9287534,0.06351498],"study_design_scores_gemma":[0.00031310102,0.000104075036,0.025499873,0.00032028827,0.0003625823,0.0014847915,0.00037423428,0.01335555,0.0036990645,0.010258568,0.94408727,0.00014071487],"about_ca_topic_score_codex":0.015006872,"about_ca_topic_score_gemma":0.029445628,"teacher_disagreement_score":0.029599797,"about_ca_system_score_codex":0.0010065334,"about_ca_system_score_gemma":0.002532077,"threshold_uncertainty_score":0.09902114},"labels":[],"label_agreement":null},{"id":"W2002180428","doi":"10.1029/2006gl028389","title":"Influence of atmospheric transport on the inter‐annual variation of the CO<sub>2</sub> seasonal cycle downward zero‐crossing","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Northern Hemisphere; Climatology; Atmospheric sciences; Seasonality; Latitude; Southern Hemisphere; Atmospheric circulation; Chemical transport model; Annual cycle; Flux (metallurgy); Proxy (statistics); Troposphere; Geography; Geology","score_opus":0.008458632582059332,"score_gpt":0.2472595408228455,"score_spread":0.23880090824078617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002180428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99795806,0.00006250548,0.00086132414,0.0000930877,0.000018183575,0.0000035963521,0.00018100589,0.00005020718,0.0007719454],"genre_scores_gemma":[0.99952507,0.000042862164,0.00015206091,0.000008887394,0.000003449339,0.0000018706683,0.00013834875,0.000011640088,0.00011584214],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991477,0.000029790659,0.000005431992,0.000020193425,0.000011091148,0.000018730338],"domain_scores_gemma":[0.99963844,0.00016339053,0.000068040026,0.000036221696,0.000052864445,0.000040972987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033114885,0.00040794298,0.0001974311,0.00021489615,0.00026376086,0.0006903908,0.00020631464,0.0003205604,0.0005946579],"category_scores_gemma":[0.0011412639,0.00022049784,0.00046233734,0.00027293336,0.00027038556,0.00031292503,0.0002572592,0.0003555123,0.00008843733],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074484467,0.00011857961,0.26159298,0.00006034493,0.0003166115,0.00053826853,0.000120706034,0.6691959,0.053811908,0.0018214938,0.0011508891,0.010527506],"study_design_scores_gemma":[0.000061304505,0.00009548503,0.17853928,0.000008055708,0.000106329724,0.00007654299,0.00005773455,0.8141614,0.0057310723,0.0004047977,0.0007219273,0.00003605549],"about_ca_topic_score_codex":0.04798858,"about_ca_topic_score_gemma":0.022488065,"teacher_disagreement_score":0.04798858,"about_ca_system_score_codex":0.00076963723,"about_ca_system_score_gemma":0.0004720971,"threshold_uncertainty_score":0.09541851},"labels":[],"label_agreement":null},{"id":"W2002238045","doi":"10.1029/2008gl033690","title":"Singular value decomposition analyses of tropical tropospheric ozone determined from TOMS","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Tropospheric ozone; Troposphere; Environmental science; Atmospheric sciences; Ozone; Total Ozone Mapping Spectrometer; Depth sounding; Microwave Limb Sounder; Climatology; Satellite; Advanced Microwave Sounding Unit; Ozone Monitoring Instrument; Meteorology; Ozone layer; Geography; Geology","score_opus":0.04966824456449638,"score_gpt":0.3291269563033729,"score_spread":0.27945871173887654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002238045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9859694,0.00007825116,0.012758405,0.000026617272,0.0000073894394,0.000007174703,0.00043685889,0.0000811375,0.00063468615],"genre_scores_gemma":[0.9881136,0.000050279956,0.010422285,0.000005479019,0.0000076047318,0.000005473859,0.0011214633,0.000013647679,0.00026004485],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998982,0.000023206558,0.0000072825997,0.000018517363,0.00003139353,0.00002148072],"domain_scores_gemma":[0.999694,0.00007602572,0.00006401506,0.000035277375,0.00010876584,0.000021910048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027996692,0.00021910065,0.000119140306,0.0007812924,0.00009809622,0.00024649946,0.000069496455,0.00007392135,0.0006249639],"category_scores_gemma":[0.0010662347,0.000058405833,0.00023788147,0.0004940354,0.00011441964,0.00013012311,0.00016764154,0.00013756777,0.00011584752],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014306572,0.00022689061,0.2521761,0.00017745342,0.00037874092,0.00031529466,0.0004414236,0.04225155,0.35081357,0.0032132124,0.002727048,0.34584808],"study_design_scores_gemma":[0.000034254725,0.00026981893,0.6132104,0.000016134312,0.00011317775,0.00025729183,0.0003709724,0.3277237,0.053627897,0.00234855,0.0019855937,0.000042134834],"about_ca_topic_score_codex":0.0039756387,"about_ca_topic_score_gemma":0.0040638666,"teacher_disagreement_score":0.0039756387,"about_ca_system_score_codex":0.0001387762,"about_ca_system_score_gemma":0.00015017139,"threshold_uncertainty_score":0.007905006},"labels":[],"label_agreement":null},{"id":"W2002412751","doi":"10.1029/2001gl013080","title":"Mechanism and duration of banding in Mississippi Valley‐type sphalerite","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Theoretical and Computational Physics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Ottawa","funders":"","keywords":"Sphalerite; Dissolution; Galena; Geology; Mineralogy; Sequence (biology); Geochemistry; Chemistry; Pyrite","score_opus":0.027778737253163086,"score_gpt":0.30988659459720536,"score_spread":0.28210785734404226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002412751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905229,0.00006307883,0.0073700855,0.00012586461,0.000004480928,0.0000073251513,0.00010462813,0.000054546832,0.0017471273],"genre_scores_gemma":[0.9990282,0.000024770256,0.0005381961,0.0000054227057,0.0000010941027,0.0000054894163,0.000025426778,0.0000062595873,0.00036517077],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999671,0.0000046924547,0.0000014889391,0.000013262799,0.0000041654203,0.000009309926],"domain_scores_gemma":[0.9998424,0.000043489086,0.000043762342,0.000018660628,0.000021311247,0.00003028919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001415379,0.000212863,0.00020995554,0.00023244048,0.00039872856,0.00043642006,0.0007031645,0.0006021136,0.0013523645],"category_scores_gemma":[0.0004948963,0.00032165082,0.0003184422,0.0001445008,0.00047210616,0.00046395735,0.00032080803,0.00026541267,0.000108103566],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011150728,0.000051788586,0.02220553,0.000031529944,0.00003464555,0.00020853072,0.00013859264,0.94543004,0.018551674,0.010024067,0.0003030885,0.0029089882],"study_design_scores_gemma":[0.000015374724,0.00001795137,0.004420149,0.000001796208,0.000007192305,0.000039941042,0.000022762211,0.99173075,0.0014054882,0.0022056666,0.00012548802,0.0000075730427],"about_ca_topic_score_codex":0.018478278,"about_ca_topic_score_gemma":0.009999357,"teacher_disagreement_score":0.018478278,"about_ca_system_score_codex":0.0011511325,"about_ca_system_score_gemma":0.00043333002,"threshold_uncertainty_score":0.036741436},"labels":[],"label_agreement":null},{"id":"W2002488857","doi":"10.1029/2004gl020536","title":"An assessment of the statistical significance of the total ozone changes simulated with global chemical transport model MEZON","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ozone; Environmental science; Statistical significance; Montreal Protocol; Statistical analysis; Statistical model; Atmospheric sciences; Atmosphere (unit); Sensitivity (control systems); Chemical transport model; Meteorology; Statistics; Ozone layer; Mathematics; Physics","score_opus":0.023245133956997895,"score_gpt":0.3130567329800998,"score_spread":0.2898115990231019,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002488857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971865,0.00006115959,0.0015510867,0.00014227911,0.000014190692,0.000009967864,0.00053745124,0.000056790115,0.00044069352],"genre_scores_gemma":[0.9981658,0.000026332378,0.00082668604,0.000019836236,0.000007744024,0.0000080276295,0.00082761527,0.000019932073,0.00009799278],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994019,0.0002569709,0.000026903277,0.00014673089,0.000113255475,0.000054151693],"domain_scores_gemma":[0.9968567,0.0021160212,0.0003300296,0.00027887974,0.0003273948,0.000091001086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018934375,0.00037436245,0.00035043978,0.00040711666,0.00025239744,0.000600719,0.00054022676,0.0004570246,0.0006042885],"category_scores_gemma":[0.008059041,0.0002068072,0.00054704165,0.00051166816,0.00054586504,0.00052634836,0.0005699834,0.0005982775,0.000069875496],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022196984,0.00014068288,0.28104135,0.00010118851,0.0006798281,0.00023615085,0.00011532376,0.6920163,0.010234634,0.002092016,0.00089786964,0.010225035],"study_design_scores_gemma":[0.00026476645,0.00036597508,0.20876576,0.000011412103,0.00012204842,0.000036641668,0.00014421581,0.7825893,0.00595409,0.00084035296,0.0008713689,0.000034118693],"about_ca_topic_score_codex":0.02541348,"about_ca_topic_score_gemma":0.010355815,"teacher_disagreement_score":0.02541348,"about_ca_system_score_codex":0.0006754353,"about_ca_system_score_gemma":0.0005593307,"threshold_uncertainty_score":0.05053115},"labels":[],"label_agreement":null},{"id":"W2002649050","doi":"10.1029/2003gl017859","title":"The use of ATSR active fire counts for estimating relative patterns of biomass burning – a study from the boreal forest region","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Forest Service","funders":"","keywords":"Environmental science; Taiga; Boreal; Radiometer; Satellite; Smoke; Fire regime; Atmospheric sciences; Biomass (ecology); Fire detection; Meteorology; Remote sensing; Physical geography; Ecology; Geography; Forestry; Geology; Oceanography; Ecosystem","score_opus":0.057434197186861505,"score_gpt":0.3123110374214067,"score_spread":0.2548768402345452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002649050","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883384,0.000060870556,0.0006338259,0.000010754102,0.0000043340747,0.000010787135,0.0001269495,0.000010588122,0.0003080961],"genre_scores_gemma":[0.9954287,0.00009234804,0.0037084944,0.000013565373,0.000013913804,0.000012637435,0.00055035396,0.000010278689,0.00016970298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99918073,0.000348097,0.00008107012,0.00016188476,0.00017055933,0.000057571815],"domain_scores_gemma":[0.99610436,0.0013054286,0.00093752146,0.0004836175,0.0009807345,0.00018836152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022818076,0.0006899185,0.00037483993,0.00074693176,0.0004427776,0.0005483922,0.0004563446,0.00034106217,0.00021797005],"category_scores_gemma":[0.003826635,0.00024674,0.00057366287,0.00070144207,0.00033505357,0.0007596887,0.0002643908,0.00034220357,0.000117702824],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045191674,0.00020228687,0.94954026,0.00004397591,0.000148301,0.000101684614,0.00037922207,0.0037585013,0.010563201,0.000074646625,0.0001447249,0.034591198],"study_design_scores_gemma":[0.00001485659,0.00061395695,0.98887235,0.000007088213,0.000082105245,0.00029125504,0.00018853699,0.0060939556,0.0033234558,0.000035501987,0.00045480006,0.000022218144],"about_ca_topic_score_codex":0.04010831,"about_ca_topic_score_gemma":0.08036049,"teacher_disagreement_score":0.04010831,"about_ca_system_score_codex":0.00033099987,"about_ca_system_score_gemma":0.0002999802,"threshold_uncertainty_score":0.07974976},"labels":[],"label_agreement":null},{"id":"W2002678855","doi":"10.1029/2006gl027166","title":"Tomographic evidence for the Eurasian lithosphere subducting beneath south Taiwan","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Lithosphere; Eurasian Plate; Seismology; Plate tectonics; Collision zone; Seismic tomography; Crust; Convergent boundary; Slab window; Oceanic crust; Tectonics; Geophysics; Mantle (geology)","score_opus":0.0846416965720218,"score_gpt":0.3179592711327981,"score_spread":0.2333175745607763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002678855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998021,0.00008604863,0.00031602243,0.000055938584,0.0000015206494,0.000004159277,0.00012483544,0.000016626287,0.001373831],"genre_scores_gemma":[0.9989785,0.00007455029,0.0005380928,0.00000794467,0.0000025389954,0.0000027056735,0.00019374234,0.000002970306,0.00019906466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99998236,0.0000015477173,0.0000019989486,0.0000059118156,0.000003984554,0.000004163549],"domain_scores_gemma":[0.9998809,0.000017153627,0.000043694054,0.000015118416,0.000022720811,0.000020298916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005153369,0.00012146507,0.00007489242,0.0004981682,0.00015011655,0.0002961561,0.00016064031,0.00017847591,0.0011668119],"category_scores_gemma":[0.00021226775,0.00015267848,0.00009862598,0.00047781033,0.00018307377,0.00017546244,0.00027735558,0.00015709002,0.00013162513],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030987474,0.000039591214,0.767632,0.00016379816,0.000071018854,0.0030010054,0.0016343686,0.0031495078,0.19404538,0.00069371524,0.00061238545,0.028647402],"study_design_scores_gemma":[0.000028349454,0.000036303096,0.9873338,0.000029348217,0.000052599768,0.0012601644,0.0006097274,0.00496718,0.004147435,0.00021359522,0.001312197,0.0000093783665],"about_ca_topic_score_codex":0.00758639,"about_ca_topic_score_gemma":0.010919752,"teacher_disagreement_score":0.00758639,"about_ca_system_score_codex":0.0001512068,"about_ca_system_score_gemma":0.00025372664,"threshold_uncertainty_score":0.0150844455},"labels":[],"label_agreement":null},{"id":"W2002727626","doi":"10.1029/2005gl024164","title":"Past and future changes in biogenic volatile organic compound emissions simulated with a global dynamic vegetation model","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":189,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Environmental science; Isoprene; Biosphere; Northern Hemisphere; Climate change; Last Glacial Maximum; Atmospheric sciences; Vegetation (pathology); Ecosystem; Climatology; Tropics; Volatile organic compound; Trace gas; Holocene; Geology; Ecology; Oceanography; Chemistry","score_opus":0.01416509508956286,"score_gpt":0.26412055447528715,"score_spread":0.24995545938572428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002727626","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99489,0.00006172299,0.001656415,0.00018753682,0.000020110583,0.00001267899,0.0015224761,0.00009411229,0.0015549274],"genre_scores_gemma":[0.9968177,0.000060493316,0.0012615095,0.0000311224,0.0000069939265,0.000019494872,0.0014327414,0.000022753395,0.000347117],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998586,0.00004153218,0.000007919445,0.00004356019,0.000014772897,0.000033577602],"domain_scores_gemma":[0.9994216,0.0002856053,0.000071985756,0.000038912072,0.00008400007,0.00009799039],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005310676,0.00070015376,0.00052864844,0.00050911185,0.0004788705,0.0008406138,0.00093014154,0.0011766959,0.0014701042],"category_scores_gemma":[0.0013507735,0.0004386122,0.0008038331,0.00086697796,0.00057454297,0.00092000194,0.00046990055,0.00074543775,0.0001626756],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010424765,0.000050514915,0.008204097,0.000012205575,0.00005607218,0.000048134738,0.00001681514,0.9894135,0.0005992148,0.00045058032,0.00025877389,0.00078582234],"study_design_scores_gemma":[0.00006675727,0.000036001682,0.0035637761,0.0000026926355,0.000022563661,0.000009266954,0.000019696803,0.9955812,0.00019096705,0.00028641563,0.00020851911,0.000012089292],"about_ca_topic_score_codex":0.07398394,"about_ca_topic_score_gemma":0.040448215,"teacher_disagreement_score":0.07398394,"about_ca_system_score_codex":0.0016561783,"about_ca_system_score_gemma":0.0007940778,"threshold_uncertainty_score":0.14710659},"labels":[],"label_agreement":null},{"id":"W2002867293","doi":"10.1029/2006gl027356","title":"Evidence for coeval Late Triassic terrestrial impacts from the Rochechouart (France) meteorite crater","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Paleomagnetism; Meteorite; Impact crater; Breccia; Apparent polar wander; Natural remanent magnetization; Tectonics; Polar wander","score_opus":0.0910777599243602,"score_gpt":0.3375122619092823,"score_spread":0.24643450198492212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2002867293","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962289,0.0005733291,0.00009413125,0.00009869763,0.000011542604,0.000003366449,0.00018034056,0.0000132556515,0.0027963957],"genre_scores_gemma":[0.99865484,0.00020281598,0.0000829651,0.00003396391,0.000011903605,0.0000021740827,0.00036050152,0.000004119653,0.00064664916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997948,0.000015292217,0.000012834672,0.000039921917,0.00006417495,0.00007305458],"domain_scores_gemma":[0.99889994,0.0001359464,0.0003827648,0.000067345856,0.00030464126,0.00020943898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028378487,0.000250078,0.00024794933,0.001567426,0.0007443453,0.0008545768,0.00026519338,0.00052097935,0.002104338],"category_scores_gemma":[0.0010329098,0.00024905722,0.00013171854,0.0010003971,0.0007446387,0.00030409914,0.0006214834,0.0003336784,0.00033377224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001889328,0.000027037488,0.9642138,0.000038263453,0.000070413116,0.0008988638,0.0009935405,0.00014894122,0.020883555,0.0003341873,0.0003518303,0.011850641],"study_design_scores_gemma":[0.000002511496,0.000012635059,0.9988557,0.0000037669063,0.000004214416,0.0003306123,0.00008865199,0.000020947115,0.0002250977,0.000009322045,0.00044453016,0.0000019194574],"about_ca_topic_score_codex":0.07266927,"about_ca_topic_score_gemma":0.18960251,"teacher_disagreement_score":0.07266927,"about_ca_system_score_codex":0.0009413482,"about_ca_system_score_gemma":0.00054968457,"threshold_uncertainty_score":0.14449257},"labels":[],"label_agreement":null},{"id":"W2003078807","doi":"10.1029/2003gl017553","title":"Scalings for large turbulent flow structures in gravel‐bed rivers","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Turbulence; Amplitude; Geology; Flow (mathematics); Bursting; Mechanics; Scale (ratio); Meteorology; Physics; Optics","score_opus":0.02085739782729191,"score_gpt":0.2901100119593434,"score_spread":0.2692526141320515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003078807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98004526,0.00021332377,0.018446563,0.00006092746,0.000007127005,0.000018280714,0.000046185043,0.000094258365,0.0010681184],"genre_scores_gemma":[0.99833834,0.000061572086,0.0014267146,0.0000041221115,0.000008996472,0.000007268292,0.00003615596,0.000011253454,0.00010548082],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998902,0.000015628237,0.000009655403,0.00003490553,0.000032022625,0.000017494784],"domain_scores_gemma":[0.9983639,0.00079604884,0.00043290952,0.00014466107,0.00011684472,0.00014568919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042241465,0.00019097934,0.00013789951,0.0011371126,0.0003193293,0.0007352757,0.00021947554,0.0002379838,0.0006405007],"category_scores_gemma":[0.0045369263,0.00028429314,0.00021880087,0.00030308837,0.0006601423,0.00060097326,0.00026809634,0.00034421124,0.00007859407],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007580976,0.0003741541,0.18293072,0.00034148278,0.00017349585,0.0020381878,0.004361835,0.3712565,0.24511556,0.08585402,0.0013521578,0.10544382],"study_design_scores_gemma":[0.000052555624,0.00018142717,0.21692088,0.000035946585,0.0000376796,0.000614983,0.00028480342,0.74439186,0.008137231,0.028261779,0.000994246,0.00008654989],"about_ca_topic_score_codex":0.0012302211,"about_ca_topic_score_gemma":0.0009210715,"teacher_disagreement_score":0.0012302211,"about_ca_system_score_codex":0.00045948586,"about_ca_system_score_gemma":0.00012738511,"threshold_uncertainty_score":0.0033338666},"labels":[],"label_agreement":null},{"id":"W2003467344","doi":"10.1029/2005gl023099","title":"Thermal conditions for PMC existence derived from Odin/OSIRIS and TIMED/SABER data","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Tekes; Centre National d’Etudes Spatiales","keywords":"Depth sounding; Physics; Brightness; Atmosphere (unit); Spectrograph; Infrared; Atmospheric sciences; Radiometer; Radiometry; Environmental science; Astrophysics; Geology; Astronomy; Meteorology; Optics","score_opus":0.04649350652558139,"score_gpt":0.33107153338098244,"score_spread":0.28457802685540107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003467344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977709,0.00004418398,0.00073823566,0.000012423303,0.0000036882097,0.000008407004,0.0007074228,0.000034885066,0.00067988015],"genre_scores_gemma":[0.9984218,0.000016838934,0.0004907507,0.0000036479703,0.0000048261245,0.0000045467787,0.0009961856,0.000009957358,0.00005137616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99967563,0.000054257776,0.000035884437,0.00009418698,0.00006972267,0.000070324015],"domain_scores_gemma":[0.99901533,0.00021731613,0.0003510693,0.00008242869,0.00024259233,0.0000912902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006719634,0.00020263849,0.00025062007,0.0010085098,0.00037961086,0.00046533372,0.00023188732,0.00019384592,0.0007456097],"category_scores_gemma":[0.0013569735,0.0001851569,0.00024432573,0.0009162827,0.00022853108,0.0004433002,0.00032275147,0.00018870567,0.00016302512],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046791486,0.000048674334,0.9742192,0.000041652904,0.000070617396,0.00021002952,0.00018218956,0.00535552,0.012618277,0.00030092598,0.00034708885,0.0061377864],"study_design_scores_gemma":[0.000016824528,0.000030941235,0.9850743,0.0000066055286,0.000027821774,0.00010065646,0.00012635604,0.011351583,0.0027366655,0.00009284031,0.00042714525,0.0000083273],"about_ca_topic_score_codex":0.0063322573,"about_ca_topic_score_gemma":0.009134989,"teacher_disagreement_score":0.0063322573,"about_ca_system_score_codex":0.0004394167,"about_ca_system_score_gemma":0.0002526659,"threshold_uncertainty_score":0.012590766},"labels":[],"label_agreement":null},{"id":"W2003628460","doi":"10.1029/2000gl012279","title":"The mechanism of solution of aluminum oxide in MgSiO<sub>3</sub> perovskite","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ferroelectric and Piezoelectric Materials","field":"Materials Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Perovskite (structure); Octahedron; Octahedral symmetry; Materials science; Oxide; Range (aeronautics); Spectral line; Mineralogy; Crystallography; Nuclear magnetic resonance; Crystal structure; Chemistry; Physics; Ion; Metallurgy","score_opus":0.02711604850205504,"score_gpt":0.28695196920427196,"score_spread":0.25983592070221695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003628460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864912,0.0011592376,0.007297915,0.00066783,0.00005842085,0.00007306974,0.00020272545,0.0002066789,0.0038428747],"genre_scores_gemma":[0.9947082,0.00038978687,0.0021905114,0.00008835464,0.000012307985,0.0000329067,0.000087711625,0.000014372857,0.0024757832],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999256,0.00000862893,0.0000034806656,0.000019755473,0.000023819357,0.00001864025],"domain_scores_gemma":[0.999941,0.00001813665,0.000017074388,0.0000048307493,0.000010716167,0.0000082135575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001108719,0.0001928951,0.00016763547,0.00014792054,0.00034684298,0.00034805518,0.0005314912,0.00036731493,0.002083857],"category_scores_gemma":[0.00017564958,0.00017057244,0.0001932163,0.000058141595,0.00037087296,0.00037181054,0.00027716128,0.000308865,0.00045131968],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093651724,0.000020782407,0.0003804754,0.00011325236,0.0000074080754,0.0001308525,0.000076098244,0.0003762029,0.99469346,0.001499815,0.0001620708,0.0024460235],"study_design_scores_gemma":[0.000044847387,0.00007702289,0.0005671263,0.0000041946064,0.000005661415,0.00010877113,0.00004567552,0.0031608518,0.99375397,0.00051188096,0.0017140022,0.0000060218795],"about_ca_topic_score_codex":0.0006897762,"about_ca_topic_score_gemma":0.0004766592,"teacher_disagreement_score":0.002083857,"about_ca_system_score_codex":0.00034225904,"about_ca_system_score_gemma":0.000234502,"threshold_uncertainty_score":0.00697124},"labels":[],"label_agreement":null},{"id":"W2003713232","doi":"10.1029/2009gl041087","title":"Rugged lava flows on the Moon revealed by Earth‐based radar","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lava; Geology; Earth (classical element); Astrobiology; Radar; Geophysics; Remote sensing; Meteorology; Geodesy; Volcano; Seismology; Aerospace engineering; Geography","score_opus":0.03224932866961577,"score_gpt":0.28640276119908264,"score_spread":0.25415343252946687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003713232","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990233,0.000095940704,0.00017592644,0.000013365595,0.0000014210345,0.0000011987237,0.00005898268,0.000015580594,0.0006142867],"genre_scores_gemma":[0.99944156,0.000058052898,0.00025212317,0.000009547141,0.0000054180678,8.846178e-7,0.0001023939,0.0000019617082,0.00012806233],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.0000076206607,0.0000025012016,0.000013154268,0.000012522932,0.000019827965],"domain_scores_gemma":[0.99978095,0.000036001275,0.00006299888,0.000019782306,0.00003454642,0.000065670734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012684803,0.00007396662,0.0001026911,0.00063291396,0.00010932318,0.00030401215,0.000090057176,0.00018234522,0.0006822099],"category_scores_gemma":[0.00046854487,0.000088841785,0.00005048925,0.00019424112,0.00014452533,0.00017733901,0.00021689017,0.00013240294,0.00017349698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029311722,0.00006512763,0.5635548,0.00004246662,0.000056565084,0.0010863729,0.0007661387,0.00036118837,0.38927075,0.00029144617,0.00068558374,0.043526337],"study_design_scores_gemma":[0.000004641624,0.00004880283,0.993353,0.0000051733577,0.00001454377,0.0008511933,0.00017053659,0.0008419288,0.0040451814,0.000062252904,0.0005981533,0.000004500305],"about_ca_topic_score_codex":0.0010452718,"about_ca_topic_score_gemma":0.0016625894,"teacher_disagreement_score":0.0010452718,"about_ca_system_score_codex":0.0000818841,"about_ca_system_score_gemma":0.000054378746,"threshold_uncertainty_score":0.0022822022},"labels":[],"label_agreement":null},{"id":"W2003876112","doi":"10.1029/2008gl035666","title":"Estimation of phytoplankton loss rate by remote sensing","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"Canadian Space Agency; National Centre for Earth Observation; Natural Environment Research Council; Sight Research UK","keywords":"Phytoplankton; Biomass (ecology); Environmental science; Bloom; Spring bloom; Growth rate; Photosynthesis; Atmospheric sciences; Range (aeronautics); Mathematics; Biology; Ecology; Nutrient; Physics; Botany; Materials science","score_opus":0.0272400055747413,"score_gpt":0.2643959213682404,"score_spread":0.23715591579349912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2003876112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.53080696,0.00062009896,0.4630029,0.000053443153,0.000038407412,0.00016367895,0.0010656747,0.0016293467,0.002619453],"genre_scores_gemma":[0.812183,0.00035624506,0.18374696,0.000023110153,0.000025005505,0.00018378839,0.0015419365,0.00016025142,0.0017796775],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996766,0.000047636095,0.000017711965,0.00008378745,0.00015366991,0.000020681808],"domain_scores_gemma":[0.9992982,0.0002162155,0.00019777592,0.00012015065,0.00014350517,0.000024074401],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010936658,0.00065044477,0.0004524366,0.0017050448,0.00020654926,0.0003388489,0.0005166262,0.00029481234,0.0006238222],"category_scores_gemma":[0.002056932,0.00028590174,0.00038162887,0.0008896497,0.00014855292,0.0005814989,0.00039172595,0.00029935935,0.00035993097],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005967251,0.0002153909,0.17584755,0.00044047442,0.00026870178,0.0002411431,0.0003305498,0.1608707,0.17963943,0.0018953633,0.0014355266,0.47821835],"study_design_scores_gemma":[0.000026715488,0.00024285475,0.19458383,0.000037459842,0.00006227148,0.00047075585,0.00006256089,0.76722157,0.03288981,0.0014344946,0.002873428,0.00009423503],"about_ca_topic_score_codex":0.0026549618,"about_ca_topic_score_gemma":0.0021574537,"teacher_disagreement_score":0.0026549618,"about_ca_system_score_codex":0.00036413418,"about_ca_system_score_gemma":0.0002514331,"threshold_uncertainty_score":0.005783975},"labels":[],"label_agreement":null},{"id":"W2004142130","doi":"10.1029/2006gl025975","title":"Oxygen minimum zone expansion in the eastern tropical North Pacific during deglaciation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Deglaciation; Oxygen minimum zone; Oceanography; Geology; Southern Hemisphere; Northern Hemisphere; Last Glacial Maximum; Climate change; Quaternary; Climatology; Upwelling; Holocene; Paleontology","score_opus":0.02474189657833586,"score_gpt":0.26123677110887894,"score_spread":0.23649487453054308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004142130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99922407,0.00008065435,0.00001805929,0.000024143334,0.0000018217611,9.6596e-7,0.00004800235,0.000002343184,0.00059981743],"genre_scores_gemma":[0.99947804,0.00013225635,0.000037262085,0.0000148816625,0.000004876716,0.0000019270933,0.00011669265,0.0000013987143,0.00021267583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999547,0.0000035631174,0.0000031030588,0.000014468397,0.000007634081,0.000016514465],"domain_scores_gemma":[0.999876,0.000010497567,0.0000575664,0.000006000485,0.000019491139,0.00003038183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011564344,0.00010704495,0.00010395527,0.0004179153,0.00032766582,0.0004150247,0.000112902184,0.0001294616,0.00071810023],"category_scores_gemma":[0.00032191252,0.0001137839,0.00008165533,0.00037031545,0.00026041898,0.00020289583,0.00037917032,0.00015768927,0.000058254147],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016553258,0.000015533353,0.9733555,0.000030730207,0.000030207422,0.00018973192,0.0009359247,0.0002142396,0.013938383,0.00013163418,0.00023682429,0.010755777],"study_design_scores_gemma":[0.0000017198536,0.0000069374705,0.9993462,0.0000018306104,0.0000031045586,0.000025822477,0.00012273798,0.000035565186,0.00012991684,0.000008648614,0.00031692436,7.0441297e-7],"about_ca_topic_score_codex":0.028226154,"about_ca_topic_score_gemma":0.05588686,"teacher_disagreement_score":0.028226154,"about_ca_system_score_codex":0.0005234964,"about_ca_system_score_gemma":0.00033832388,"threshold_uncertainty_score":0.056123734},"labels":[],"label_agreement":null},{"id":"W2004291496","doi":"10.1029/2004gl021521","title":"Observations of mesospheric ozone depletion during the October 28, 2003 solar proton event by OSIRIS","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Tekes; Centre National d’Etudes Spatiales","keywords":"Stratosphere; Atmospheric sciences; Ozone depletion; Ozone; Environmental science; Osiris; Mesosphere; Tropopause; Atmosphere (unit); Polar; Latitude; Ozone layer; Meteorology; Physics; Astronomy","score_opus":0.02675257639678424,"score_gpt":0.2719657827483425,"score_spread":0.24521320635155824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004291496","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946656,0.00008149514,0.00020667144,0.000049866987,0.0000069058337,0.000012762643,0.0035357468,0.00006663656,0.0013744178],"genre_scores_gemma":[0.9898123,0.00017750119,0.0016536295,0.000050322804,0.00001443583,0.0000157407,0.0075272215,0.000010796348,0.0007380523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991345,0.000009354709,0.000007848712,0.000018900422,0.000033338245,0.000017011456],"domain_scores_gemma":[0.99975175,0.000017774215,0.00009737466,0.000025037518,0.000059825103,0.000048188045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003463807,0.00018978381,0.00021100213,0.00050399906,0.00031367238,0.00024493216,0.00017754661,0.0002523623,0.000569391],"category_scores_gemma":[0.0003271177,0.00017838964,0.0001112868,0.00046962244,0.000098229895,0.00025397012,0.0003000912,0.0003052849,0.0001589598],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000789833,0.00025251394,0.9225138,0.000094163755,0.00018147647,0.00025517662,0.00078032824,0.0016389805,0.047324575,0.00020280799,0.005772555,0.020193797],"study_design_scores_gemma":[0.000019874684,0.000039850656,0.9933744,0.0000046320442,0.000020065476,0.000053154658,0.00012186941,0.0012774282,0.0029474292,0.00003694106,0.0020980923,0.000006287803],"about_ca_topic_score_codex":0.012547608,"about_ca_topic_score_gemma":0.044550695,"teacher_disagreement_score":0.012547608,"about_ca_system_score_codex":0.00025830374,"about_ca_system_score_gemma":0.00019502017,"threshold_uncertainty_score":0.024949133},"labels":[],"label_agreement":null},{"id":"W2004329181","doi":"10.1029/2009gl039896","title":"Decadal changes in ecological provinces of the Northwest Atlantic Ocean revealed by satellite observations","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Climate change; Satellite; Ecosystem; Oceanography; Period (music); Environmental science; Geography; Climatology; Biomass (ecology); Sea surface temperature; Physical geography; Ecology; Geology","score_opus":0.03129341414519536,"score_gpt":0.2549317533058036,"score_spread":0.2236383391606082,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2004329181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883205,0.00008029337,0.00017456022,0.000030486717,0.0000031879904,0.0000014926401,0.0005455385,0.00000648406,0.00032588423],"genre_scores_gemma":[0.9984823,0.00009005294,0.00041042254,0.00001039719,0.0000029540063,0.0000034795485,0.0008681704,0.0000027840208,0.00012940668],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987304,0.00002906961,0.00001601535,0.00003052917,0.000023622273,0.00002776838],"domain_scores_gemma":[0.9989543,0.0001963265,0.00041260596,0.00011477842,0.00022369654,0.0000982683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005461861,0.00007933866,0.00014780942,0.0007492004,0.00023673454,0.0005169888,0.00013933003,0.00013793279,0.0004480172],"category_scores_gemma":[0.001714631,0.00012234946,0.00016200518,0.0012617434,0.00021800185,0.00028736485,0.00036878823,0.000266756,0.000087276494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008326015,0.0000109418415,0.98935026,0.000017255763,0.000049974657,0.000026993212,0.00026972304,0.00072513014,0.0020328374,0.00009182152,0.00019460001,0.007147168],"study_design_scores_gemma":[0.0000013789983,0.0000047259955,0.9988752,0.0000031649774,0.0000064245287,0.000011190054,0.00013917864,0.00054465776,0.000073612675,0.000027005515,0.00031113427,0.0000021933824],"about_ca_topic_score_codex":0.07552309,"about_ca_topic_score_gemma":0.14555192,"teacher_disagreement_score":0.07552309,"about_ca_system_score_codex":0.0004893792,"about_ca_system_score_gemma":0.0004010159,"threshold_uncertainty_score":0.15016699},"labels":[],"label_agreement":null},{"id":"W2005831348","doi":"10.1029/2007gl032527","title":"Spatial variability in annual sea level variations around the Korean peninsula","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Peninsula; Climatology; Sea level; Oceanography; Amplitude; Geology; Environmental science; Atmospheric sciences; Geography","score_opus":0.08111271771509185,"score_gpt":0.2926967296912171,"score_spread":0.21158401197612522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2005831348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983741,0.000111045854,0.00005782086,0.000030272875,0.0000035816379,0.0000022371034,0.00079867814,0.0000065820072,0.0006156311],"genre_scores_gemma":[0.99887604,0.0000911783,0.00005621394,0.0000098284345,0.0000039188653,0.0000032263083,0.0007755767,0.0000024543406,0.00018161509],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.000012188594,0.000014984065,0.000045391665,0.000015628138,0.000021251913],"domain_scores_gemma":[0.9993425,0.00007157442,0.00024178653,0.000053608805,0.00019263709,0.00009781794],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002606895,0.00014331384,0.00011274478,0.0008494731,0.0001601057,0.0004926893,0.00017838743,0.00010015746,0.00091883686],"category_scores_gemma":[0.00045246808,0.00014432563,0.00018411888,0.0014924656,0.00018149214,0.0002867972,0.0003519427,0.0001216176,0.00024514357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007103828,0.000011214331,0.9901585,0.000023240334,0.000121287805,0.00013232962,0.000242026,0.0006958172,0.002137486,0.000098999204,0.00047489855,0.0058333],"study_design_scores_gemma":[0.0000013651575,0.000005308588,0.9991347,0.0000029932685,0.000012268679,0.00003366313,0.00015362367,0.00026272048,0.000057312467,0.0000115608045,0.00032129994,0.000003055235],"about_ca_topic_score_codex":0.02039034,"about_ca_topic_score_gemma":0.023954626,"teacher_disagreement_score":0.02039034,"about_ca_system_score_codex":0.00029290357,"about_ca_system_score_gemma":0.00025848037,"threshold_uncertainty_score":0.040543318},"labels":[],"label_agreement":null},{"id":"W2006305975","doi":"10.1029/2006gl026568","title":"Impact of 3‐D Earth structure on Fennoscandian glacial isostatic adjustment: Implications for space‐geodetic estimates of present‐day crustal deformations","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Geodetic datum; Lithosphere; Geodesy; Mantle (geology); Glacial period; Geophysics; Earth model; Global Positioning System; Seismology; Geomorphology; Tectonics","score_opus":0.02620846353106203,"score_gpt":0.3118804405375901,"score_spread":0.2856719770065281,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006305975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9697899,0.0003184106,0.024999904,0.00043666767,0.00003695986,0.000015482165,0.0006806078,0.00024881418,0.0034731575],"genre_scores_gemma":[0.99569833,0.00010920587,0.003687565,0.00003943792,0.0000051861252,0.000006520249,0.00018863469,0.00003220902,0.00023283256],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999747,0.00009302344,0.000019963914,0.000057244753,0.000050507573,0.000032136548],"domain_scores_gemma":[0.99923444,0.00041430225,0.000086744796,0.000097307566,0.00011900845,0.000048202586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096994184,0.0004508054,0.0003611782,0.00044911267,0.00051918754,0.0012523725,0.0007041341,0.0005502661,0.0009187379],"category_scores_gemma":[0.0039507044,0.0002943694,0.0005593405,0.0008219644,0.0007966449,0.00076997065,0.0006257938,0.0004154718,0.00013117694],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000120320554,0.000025090769,0.12466085,0.000046266206,0.000113490176,0.00012744938,0.00012930945,0.8465448,0.0033034459,0.0026224018,0.00023326727,0.022073278],"study_design_scores_gemma":[0.000021546026,0.000027945509,0.09013614,0.000024010304,0.00003652757,0.00006286199,0.0000901896,0.9055504,0.0016955411,0.0013957733,0.0009210127,0.00003807311],"about_ca_topic_score_codex":0.21950269,"about_ca_topic_score_gemma":0.19373827,"teacher_disagreement_score":0.21950269,"about_ca_system_score_codex":0.0018016077,"about_ca_system_score_gemma":0.0025164078,"threshold_uncertainty_score":0.43645006},"labels":[],"label_agreement":null},{"id":"W2006331539","doi":"10.1029/2008gl033672","title":"Ionospheric localisation and expansion of long‐period Pi1 pulsations at substorm onset","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency; University of Alberta; National Aeronautics and Space Administration","keywords":"Substorm; Geophysics; Ionosphere; Physics; Magnetometer; Epicenter; Geology; Geodesy; Magnetosphere; Seismology; Magnetic field","score_opus":0.022658354127541774,"score_gpt":0.2749098324635408,"score_spread":0.25225147833599904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2006331539","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985831,0.000065259046,0.0002193902,0.000014446112,0.0000019027223,0.0000040147324,0.00014507584,0.000014523359,0.00095236296],"genre_scores_gemma":[0.99934083,0.000046607256,0.00015357595,0.0000064147675,0.000005091519,0.0000035139603,0.000285898,0.0000031568466,0.00015486535],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995506,0.000004215097,0.0000017410042,0.00001128634,0.000008605443,0.000019122348],"domain_scores_gemma":[0.9997558,0.00004619568,0.000109342094,0.000018332383,0.000037060414,0.000033373195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104639636,0.00012989723,0.00015396999,0.0004573288,0.00020182265,0.00028422836,0.00011075916,0.00018508274,0.0010187965],"category_scores_gemma":[0.00046809646,0.000064780346,0.00009378792,0.00044348385,0.00018527397,0.00024066328,0.00035517642,0.00023172353,0.00017167792],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006446189,0.00006760584,0.8319526,0.00007720153,0.000047996906,0.0008058824,0.0009633686,0.0021255503,0.13195288,0.00047786723,0.00060841494,0.030275933],"study_design_scores_gemma":[0.0000035920068,0.000037978745,0.9970499,0.000003186773,0.0000049398955,0.00011089318,0.0000816317,0.00048175128,0.001840241,0.000038275117,0.0003450215,0.000002397269],"about_ca_topic_score_codex":0.0031943726,"about_ca_topic_score_gemma":0.005144019,"teacher_disagreement_score":0.0031943726,"about_ca_system_score_codex":0.00023599603,"about_ca_system_score_gemma":0.000080478065,"threshold_uncertainty_score":0.0063515306},"labels":[],"label_agreement":null},{"id":"W2007039016","doi":"10.1029/2004gl020882","title":"Anomalous topography in the western Atlantic caused by edge‐driven convection","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Ocean surface topography; Convection; Lithosphere; Geophysics; Convection cell; Subsidence; Mantle convection; Plate tectonics; Climatology; Seismology; Geomorphology; Tectonics; Meteorology; Natural convection","score_opus":0.028833407324239682,"score_gpt":0.2732160692958878,"score_spread":0.24438266197164815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007039016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998134,0.0000045912384,0.00006133304,0.0000026010532,6.5587665e-7,5.4461174e-7,0.000009207447,0.0000042096312,0.00010339913],"genre_scores_gemma":[0.9998635,0.0000053030803,0.00007520414,0.0000025278657,6.0865057e-7,6.0171567e-7,0.0000205934,7.387076e-7,0.000030828505],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999677,0.0000051478696,0.0000020813761,0.000006170414,0.000006894079,0.000012042364],"domain_scores_gemma":[0.99985814,0.000024766161,0.000044924018,0.000024311545,0.00001895392,0.000028909824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004760191,0.00009024855,0.0000941872,0.00008927754,0.00012965259,0.00013716708,0.000071646646,0.00011421536,0.00042928028],"category_scores_gemma":[0.00030620862,0.00008751451,0.00008787075,0.00007529731,0.00022480956,0.000078799174,0.00017398204,0.00012370171,0.00004328687],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005849204,0.000106396736,0.20691295,0.000030389185,0.000041597108,0.00065189326,0.00018186137,0.0108703915,0.77360636,0.00041198742,0.00019238674,0.006408888],"study_design_scores_gemma":[0.000088700275,0.00039195488,0.8921644,0.0000055061255,0.000041824387,0.0004440545,0.00014558189,0.0645808,0.041435033,0.00031544265,0.0003677962,0.000018811033],"about_ca_topic_score_codex":0.002899115,"about_ca_topic_score_gemma":0.0043535186,"teacher_disagreement_score":0.002899115,"about_ca_system_score_codex":0.00016147019,"about_ca_system_score_gemma":0.000080398524,"threshold_uncertainty_score":0.0057644844},"labels":[],"label_agreement":null},{"id":"W2007408843","doi":"10.1029/2007gl030419","title":"Irminger Water variability in the West Greenland Current","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Oceanography; Salinity; Current (fluid); Geology; Climatology; Cape; Groenlandia; Lag; Sea level; Environmental science; Geography; Ice sheet","score_opus":0.03201721586861789,"score_gpt":0.2976124369524008,"score_spread":0.2655952210837829,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007408843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924636,0.000043592092,0.000034566794,0.00002089251,0.0000012894974,0.0000010591277,0.00011631933,0.0000047256513,0.0005311133],"genre_scores_gemma":[0.99929345,0.00004334434,0.00007241366,0.000021287628,0.0000019265167,0.0000012442418,0.00024745485,0.0000017918177,0.0003170863],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995506,0.0000027051226,0.0000026328999,0.000015642803,0.000009161494,0.000014831313],"domain_scores_gemma":[0.99989796,0.0000050239073,0.00004847813,0.0000068137015,0.000025078414,0.000016646154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001245209,0.000099953664,0.000094710376,0.0005692415,0.00018998858,0.00036483954,0.00012772555,0.00014598113,0.0005699649],"category_scores_gemma":[0.00023729092,0.000046247904,0.000087687185,0.0005392951,0.00018592486,0.00031159224,0.00025196993,0.000101046455,0.000092763716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043358006,0.000028163644,0.97891414,0.000013770783,0.000052029405,0.00020048326,0.0007936273,0.001157872,0.0055016726,0.00020973691,0.00052534963,0.01255972],"study_design_scores_gemma":[5.623869e-7,0.0000071910395,0.99898726,0.0000028835334,0.0000045686365,0.0000135995415,0.00008070863,0.00023441396,0.00010678735,0.00001300729,0.0005475253,0.0000013726303],"about_ca_topic_score_codex":0.12061956,"about_ca_topic_score_gemma":0.2949574,"teacher_disagreement_score":0.12061956,"about_ca_system_score_codex":0.0011630888,"about_ca_system_score_gemma":0.00030914755,"threshold_uncertainty_score":0.23983496},"labels":[],"label_agreement":null},{"id":"W2007426147","doi":"10.1029/2000gl012067","title":"Cloud optical depths and TOA fluxes: Comparison between satellite and surface retrievals from multiple platforms","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Natural Resources Canada","funders":"Centre National d’Etudes Spatiales; Langley Research Center; U.S. Department of Energy","keywords":"Radiative transfer; Environmental science; Remote sensing; Inversion (geology); Shortwave; Cloud computing; Satellite; Broadband; Meteorology; Atmospheric radiative transfer codes; Cloud top; Cloud fraction; Flux (metallurgy); Cloud cover; Computer science; Geology; Physics; Optics; Telecommunications; Materials science; Astronomy","score_opus":0.04181469243076415,"score_gpt":0.30951975065682213,"score_spread":0.267705058226058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007426147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944746,0.0002867936,0.0025217978,0.0000390641,0.000014974478,0.000030528623,0.0011260754,0.00011947368,0.0013867342],"genre_scores_gemma":[0.9892813,0.00023752563,0.0077007865,0.000015679234,0.00002312741,0.000025549612,0.0022534183,0.000046270372,0.00041631484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994986,0.00008009351,0.00003387261,0.00011980274,0.0001998933,0.0000677043],"domain_scores_gemma":[0.9987431,0.0004055096,0.00022743676,0.00016545082,0.0003774396,0.00008110883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012709287,0.0005617389,0.000496341,0.0016317555,0.00031586393,0.0009764517,0.00044246326,0.0007530162,0.0007046289],"category_scores_gemma":[0.0034041665,0.0003699749,0.00046257622,0.0016988833,0.00018447948,0.0013270406,0.00056906196,0.00023825417,0.00034099142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031354877,0.0005733067,0.62347704,0.00046010662,0.0011260628,0.00036188844,0.00066644646,0.060766,0.12657891,0.0009824241,0.001195642,0.18067673],"study_design_scores_gemma":[0.0003370539,0.00079768436,0.810763,0.000063799016,0.00044891963,0.00034676556,0.00039582897,0.14844874,0.03572925,0.0007251974,0.0018478605,0.00009589094],"about_ca_topic_score_codex":0.00860551,"about_ca_topic_score_gemma":0.010177936,"teacher_disagreement_score":0.00860551,"about_ca_system_score_codex":0.00053450785,"about_ca_system_score_gemma":0.00031636722,"threshold_uncertainty_score":0.017110825},"labels":[],"label_agreement":null},{"id":"W2007570030","doi":"10.1029/2009gl041239","title":"Impact of sudden Arctic sea‐ice loss on stratospheric polar ozone recovery","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of Toronto; Environment and Climate Change Canada","funders":"Scheme for Promotion of Academic and Research Collaboration; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Climatology; Sea ice; Arctic; Arctic geoengineering; Ozone depletion; Polar vortex; Polar night; Environmental science; Atmospheric sciences; Stratosphere; Ozone layer; Polar; Arctic sea ice decline; Northern Hemisphere; Ozone; Arctic ice pack; Radiative forcing; Troposphere; Geology; Oceanography; Climate change; Meteorology; Sea ice thickness; Physics","score_opus":0.023900322761437796,"score_gpt":0.2984372304034875,"score_spread":0.27453690764204974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007570030","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988643,0.000031915293,0.00023387738,0.00012384502,0.000014987341,0.0000071788013,0.00013505018,0.00002795932,0.0005609913],"genre_scores_gemma":[0.9997068,0.000023585144,0.000071829556,0.000024548866,0.0000032873752,0.000003650506,0.00008453926,0.0000041271314,0.00007760326],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979764,0.00005762753,0.000008731485,0.000029918901,0.000020044557,0.00008612038],"domain_scores_gemma":[0.9994448,0.00027763014,0.000097829165,0.000038923365,0.00004660201,0.000094265044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005445819,0.0006069006,0.00041091413,0.00023692581,0.00057054026,0.0007184723,0.00048882485,0.000990005,0.001306412],"category_scores_gemma":[0.002157188,0.00025880884,0.00086130237,0.00020252202,0.0005960035,0.00046336287,0.0007765827,0.00074109295,0.0001125566],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011951677,0.0002976137,0.057628978,0.000065518616,0.000345541,0.0007882373,0.00008551344,0.9199426,0.015455633,0.0008754885,0.0006030785,0.0027165401],"study_design_scores_gemma":[0.00036351,0.001544496,0.081902325,0.000016742297,0.00020869725,0.00014533848,0.0004058899,0.9026391,0.011275285,0.00085702457,0.00058079755,0.000060776714],"about_ca_topic_score_codex":0.024415234,"about_ca_topic_score_gemma":0.009660553,"teacher_disagreement_score":0.024415234,"about_ca_system_score_codex":0.0007203354,"about_ca_system_score_gemma":0.0005130566,"threshold_uncertainty_score":0.048546195},"labels":[],"label_agreement":null},{"id":"W2007578351","doi":"10.1029/2001gl012973","title":"A unique stratospheric warming event in November 2000","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Stratosphere; Sudden stratospheric warming; Polar vortex; Atmospheric sciences; Arctic oscillation; Climatology; Environmental science; Polar; Global warming; Northern Hemisphere; Climate change; Geology; Physics; Oceanography","score_opus":0.029360837976627314,"score_gpt":0.29517346678012607,"score_spread":0.26581262880349876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007578351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9644465,0.00089302793,0.0009401627,0.002066744,0.0010360985,0.00015487407,0.0045495327,0.00015431883,0.025758646],"genre_scores_gemma":[0.9903582,0.0004379176,0.0003706467,0.00072759256,0.00054990174,0.000036970992,0.004125996,0.000014490909,0.0033782301],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981695,0.000017430804,0.000009590887,0.000032273478,0.000055192537,0.00006859874],"domain_scores_gemma":[0.99968565,0.000025427355,0.00006364296,0.00002250995,0.000081241145,0.00012157211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028294115,0.00037024944,0.00028776212,0.00047961276,0.0016228333,0.00085807435,0.0001344845,0.0007100266,0.0010123083],"category_scores_gemma":[0.0006141148,0.00011402852,0.0001300581,0.00045018233,0.0003194258,0.00034010332,0.001081891,0.00062590034,0.00024919712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0029173265,0.0003491977,0.8050897,0.00052047084,0.00024480486,0.011425325,0.0060038115,0.0022197429,0.04183153,0.002908476,0.05087413,0.07561548],"study_design_scores_gemma":[0.00002203052,0.00015843438,0.9677036,0.000029243507,0.000031148113,0.00090302987,0.000670128,0.0003328548,0.0015895586,0.00015915371,0.028381469,0.000019379591],"about_ca_topic_score_codex":0.027966311,"about_ca_topic_score_gemma":0.09915563,"teacher_disagreement_score":0.027966311,"about_ca_system_score_codex":0.0008561845,"about_ca_system_score_gemma":0.00065435044,"threshold_uncertainty_score":0.05560708},"labels":[],"label_agreement":null},{"id":"W2007871900","doi":"10.1029/2005gl023774","title":"Global budget of water isotopes inferred from polar ice sheets","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Cryosphere; Ice sheet; Ice core; Geology; δ18O; Sea ice; Ice stream; Ice shelf; Antarctic sea ice; Antarctic ice sheet; Polar; Ice divide; Oceanography; Climatology; Stable isotope ratio","score_opus":0.032102374733337526,"score_gpt":0.28454903673590415,"score_spread":0.2524466620025666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007871900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970797,0.00016328141,0.00046025586,0.00009062059,0.0000061753426,0.0000027591695,0.0013356421,0.00005285908,0.00080878707],"genre_scores_gemma":[0.9966192,0.00024970627,0.00071929157,0.000031617485,0.000007358843,0.0000064431756,0.002063328,0.000019489189,0.00028355207],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999521,0.000009803262,0.0000037653126,0.000017606857,0.000007906556,0.000008864368],"domain_scores_gemma":[0.99986446,0.000027471186,0.000032966556,0.00002024984,0.000034636465,0.000020108124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002382844,0.00050889666,0.0002082908,0.0005986668,0.00016222885,0.00051252946,0.00020624345,0.000305974,0.0007226139],"category_scores_gemma":[0.00038876504,0.000301965,0.00030893716,0.00060374476,0.0002874235,0.00045361166,0.0003279074,0.00017188136,0.00020867785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00068649976,0.00009848901,0.7753041,0.00015841181,0.0006964476,0.00028045912,0.00017381865,0.089628145,0.09901431,0.0019785094,0.0011340055,0.030846719],"study_design_scores_gemma":[0.000111365014,0.0001473762,0.9088179,0.00003644092,0.00031651714,0.00014121975,0.000110008696,0.07053168,0.013629797,0.0016552387,0.0044622864,0.00004016488],"about_ca_topic_score_codex":0.012424686,"about_ca_topic_score_gemma":0.007790135,"teacher_disagreement_score":0.012424686,"about_ca_system_score_codex":0.00082880387,"about_ca_system_score_gemma":0.00041324995,"threshold_uncertainty_score":0.024704695},"labels":[],"label_agreement":null},{"id":"W2007914817","doi":"10.1029/2009gl038775","title":"Sea‐ice production over the Laptev Sea shelf inferred from historical summer‐to‐winter hydrographic observations of 1960s–1990s","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Arctic Sciences; Office of Polar Programs; Natural Sciences and Engineering Research Council of Canada; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Hydrography; Oceanography; Climatology; Geology; Sea ice; Environmental science","score_opus":0.04669789133623438,"score_gpt":0.27765958664273016,"score_spread":0.2309616953064958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007914817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99671483,0.00017371395,0.00007425456,0.000020306126,0.000002057595,0.000002256217,0.0018843743,0.000010064377,0.0011182397],"genre_scores_gemma":[0.9945651,0.00018741586,0.00011530511,0.0000074140457,0.0000049566884,0.0000060242724,0.0048037614,0.0000035842138,0.0003063569],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999523,0.0000061414758,0.000005039075,0.000014169669,0.000008344239,0.000014058636],"domain_scores_gemma":[0.9998518,0.00002775942,0.00004961023,0.000012254638,0.00003231766,0.000026284799],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017079557,0.00020157994,0.000116860494,0.0012048332,0.00016608107,0.00047977513,0.00015229623,0.000091708,0.001067131],"category_scores_gemma":[0.00048638773,0.00012843097,0.00018536144,0.00083192723,0.00014809525,0.0002474312,0.00040798675,0.00012512114,0.0002498966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077209676,0.000017478975,0.98028505,0.000051709132,0.00007931899,0.0002058909,0.00020898269,0.0041704425,0.0022124858,0.00023166781,0.0006900478,0.011769747],"study_design_scores_gemma":[0.000006676915,0.000018625527,0.9960828,0.000019607296,0.000015250035,0.00006820163,0.00007067029,0.0017711014,0.00037614803,0.000051724746,0.0015167183,0.000002569199],"about_ca_topic_score_codex":0.033169713,"about_ca_topic_score_gemma":0.04340149,"teacher_disagreement_score":0.033169713,"about_ca_system_score_codex":0.0006255371,"about_ca_system_score_gemma":0.00036272526,"threshold_uncertainty_score":0.065953314},"labels":[],"label_agreement":null},{"id":"W2007925375","doi":"10.1029/2000gl011476","title":"Along strike variations in the electrical structure of the San Andreas Fault at Parkfield, California","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":127,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"San andreas fault; Magnetotellurics; Geology; Seismology; Electrical resistivity and conductivity; Wedge (geometry); Fault (geology); Geometry; Electrical engineering","score_opus":0.015368915814369045,"score_gpt":0.25563539425697207,"score_spread":0.24026647844260302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2007925375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990343,0.00002052732,0.00003826631,0.000018728326,0.0000012136018,0.0000011822497,0.00011692864,0.0000068538593,0.0007621165],"genre_scores_gemma":[0.999226,0.000031377243,0.00010254574,0.0000053098015,0.0000018943265,0.0000011334876,0.00016853905,0.0000014083199,0.0004618078],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992764,0.0000036076415,0.00000243497,0.000025582483,0.000025997868,0.00001481814],"domain_scores_gemma":[0.9997538,0.000023211725,0.000071510236,0.000013297403,0.00010271797,0.000035512672],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008647211,0.000078351026,0.00007322572,0.0005271547,0.0002733391,0.00026473813,0.00014002074,0.00013750927,0.0007402488],"category_scores_gemma":[0.00037619885,0.00008621324,0.000027139275,0.00032436906,0.00021262039,0.0001829586,0.00016917444,0.00013505161,0.00008127978],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019140271,0.00008483356,0.9478123,0.000024697161,0.00003477859,0.00028455022,0.00092847826,0.001380828,0.027813967,0.00023438047,0.0010336092,0.020176228],"study_design_scores_gemma":[0.0000036474344,0.000014284506,0.99874276,0.000001990448,0.0000031940472,0.000030769465,0.00010514875,0.00029376353,0.0004610576,0.000009597355,0.00033187002,0.0000020634063],"about_ca_topic_score_codex":0.06495648,"about_ca_topic_score_gemma":0.20743056,"teacher_disagreement_score":0.06495648,"about_ca_system_score_codex":0.0005296299,"about_ca_system_score_gemma":0.00027418425,"threshold_uncertainty_score":0.12915677},"labels":[],"label_agreement":null},{"id":"W2008125660","doi":"10.1029/2008gl035725","title":"Human influence on Arctic sea ice detectable from early 1990s onwards","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Sea ice; Arctic; Arctic ice pack; Oceanography; The arctic; Climatology; Arctic sea ice decline; Environmental science; Geology; Antarctic sea ice","score_opus":0.028762762202016415,"score_gpt":0.2700085551115013,"score_spread":0.2412457929094849,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008125660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987703,0.0001757206,0.00019709392,0.00003739192,0.0000046391674,0.0000012349358,0.00019011219,0.000010292296,0.0006132129],"genre_scores_gemma":[0.99950826,0.000099388,0.00010822152,0.000005073738,0.0000045129514,7.709389e-7,0.00020246206,0.0000013457523,0.0000700492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991655,0.000014549827,0.0000063816774,0.000021645672,0.000014678522,0.00002617663],"domain_scores_gemma":[0.99943,0.00012941133,0.00020109503,0.000042233612,0.00012111891,0.000076050164],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030002452,0.00023816468,0.00021255168,0.0005527889,0.00019687954,0.00039534955,0.00010657186,0.00015908717,0.0007757339],"category_scores_gemma":[0.0012147785,0.00012592164,0.0002659654,0.0004408665,0.00026867923,0.00021557604,0.0003194529,0.00014914364,0.000077500845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030417086,0.000037706,0.9682693,0.00004192339,0.00008256997,0.00012137648,0.00013938101,0.0072967643,0.004946522,0.00019135141,0.00025462222,0.018314155],"study_design_scores_gemma":[0.0000041373523,0.000032441163,0.99444604,0.000012307934,0.000021526015,0.00004611421,0.000064408996,0.00429892,0.00061814074,0.00009929428,0.00035252466,0.0000040866325],"about_ca_topic_score_codex":0.02497854,"about_ca_topic_score_gemma":0.046156473,"teacher_disagreement_score":0.02497854,"about_ca_system_score_codex":0.00036766016,"about_ca_system_score_gemma":0.00042530807,"threshold_uncertainty_score":0.049666286},"labels":[],"label_agreement":null},{"id":"W2008408468","doi":"10.1029/2008gl036682","title":"The interchange cycle: A fundamental mode of magnetic flux circulation for northward interplanetary magnetic field","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Interplanetary magnetic field; Physics; Dipole; Flux (metallurgy); Magnetic flux; Magnetic field; Ionosphere; Geophysics; Solar wind; Materials science","score_opus":0.014771678171154603,"score_gpt":0.2930771064696801,"score_spread":0.2783054282985255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008408468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7166322,0.0024196128,0.14776237,0.000611626,0.00033169673,0.00014152893,0.0012478568,0.0012832856,0.12956984],"genre_scores_gemma":[0.9800822,0.00047501703,0.010717004,0.000088055545,0.00011732932,0.000038896505,0.00033394826,0.00012276182,0.008024801],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998925,0.000011929443,0.0000053431813,0.00002837906,0.00003779152,0.000024077763],"domain_scores_gemma":[0.9998405,0.000018412717,0.000042928186,0.000035595163,0.000039693674,0.000022879838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011146692,0.00017906126,0.00017077196,0.00041753045,0.00057891826,0.0008254553,0.00033614234,0.00031210895,0.0032271591],"category_scores_gemma":[0.00048755962,0.000074486656,0.000121682446,0.00041144708,0.0005542202,0.00070294907,0.0003564393,0.00027019694,0.0005835028],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005487967,0.00012298198,0.053144652,0.00026080213,0.00003711427,0.0011913099,0.0031199658,0.0058645825,0.17602365,0.36263344,0.024134533,0.3729182],"study_design_scores_gemma":[0.00014392224,0.00044399628,0.2011152,0.0001237954,0.00007039799,0.009402758,0.001916971,0.08413938,0.096928544,0.19120675,0.41427577,0.00023248834],"about_ca_topic_score_codex":0.0010744982,"about_ca_topic_score_gemma":0.0013874017,"teacher_disagreement_score":0.0032271591,"about_ca_system_score_codex":0.00031723344,"about_ca_system_score_gemma":0.00026877047,"threshold_uncertainty_score":0.010795891},"labels":[],"label_agreement":null},{"id":"W2008865901","doi":"10.1029/2006gl026671","title":"Measurements of the vapor pressure of cubic ice and their implications for atmospheric ice clouds","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration; National Science Foundation","keywords":"Ice crystals; Cirrus; Water vapor; Vapor pressure; Vapour pressure of water; Sublimation (psychology); Atmosphere (unit); Atmospheric sciences; Clear ice; Hexagonal crystal system; Materials science; Atmospheric pressure; Environmental science; Meteorology; Thermodynamics; Geology; Chemistry; Physics; Arctic ice pack; Crystallography; Sea ice","score_opus":0.041488830058951445,"score_gpt":0.27831002730360055,"score_spread":0.23682119724464912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2008865901","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99129194,0.00083880406,0.002118896,0.00015368193,0.00003113356,0.000014508915,0.0006145407,0.00007559878,0.0048609655],"genre_scores_gemma":[0.9987452,0.00024908938,0.00065382186,0.000018969151,0.000020508118,0.0000053302556,0.00016520095,0.000008050541,0.00013379428],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989617,0.000010602881,0.0000038645994,0.000028334245,0.00003794124,0.0000231281],"domain_scores_gemma":[0.99976796,0.00008519525,0.00005853212,0.000017949686,0.00004374323,0.000026689919],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014949546,0.00022833594,0.00013833994,0.0003196214,0.00044840772,0.00035490276,0.00038768115,0.0002428827,0.00057606265],"category_scores_gemma":[0.00047658425,0.00017937568,0.00009679321,0.00047710445,0.00030848625,0.00030678342,0.0002199496,0.0004739553,0.00010720267],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003407773,0.00019067053,0.25979128,0.00031244848,0.00006534989,0.0003903106,0.000724794,0.0018033059,0.7075193,0.000928838,0.0013067136,0.026626188],"study_design_scores_gemma":[0.000019260839,0.00022631131,0.62946546,0.000021022666,0.00004355707,0.00050409866,0.000394908,0.009363983,0.35643488,0.0006499851,0.0028447045,0.00003185324],"about_ca_topic_score_codex":0.007983809,"about_ca_topic_score_gemma":0.0072380695,"teacher_disagreement_score":0.007983809,"about_ca_system_score_codex":0.00031179073,"about_ca_system_score_gemma":0.000230647,"threshold_uncertainty_score":0.015874684},"labels":[],"label_agreement":null},{"id":"W2009048518","doi":"10.1029/1999gl010811","title":"Match observations in the Arctic winter 1996/97: High stratospheric ozone loss rates correlate with low temperatures deep inside the polar vortex","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Bundesministerium für Bildung und Forschung; European Commission","keywords":"Polar vortex; Ozone; Stratosphere; Vortex; Atmospheric sciences; Ozone layer; Ozone depletion; Environmental science; Arctic; Climatology; Polar; Meteorology; Geology; Oceanography; Physics","score_opus":0.017978024474169553,"score_gpt":0.24825308428277337,"score_spread":0.23027505980860383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009048518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988009,0.00008082103,0.00016684529,0.0000104366745,0.0000059615886,0.0000029740918,0.00054904557,0.000010861319,0.00037212932],"genre_scores_gemma":[0.99761885,0.00013209936,0.00035187765,0.000013177202,0.000011716962,0.000008175515,0.0015580287,0.000005848709,0.00030001614],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998977,0.000011410887,0.000007563687,0.00002190442,0.000034110926,0.000027362907],"domain_scores_gemma":[0.9998357,0.000017224766,0.00006813313,0.000014118045,0.000037367965,0.000027301781],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002705163,0.00024120428,0.00027297734,0.000468011,0.0004721923,0.00050573656,0.000119501114,0.00021993219,0.0002863644],"category_scores_gemma":[0.00033253452,0.00013798896,0.00014103443,0.00054554985,0.00017194364,0.00017421396,0.00029719385,0.00016323013,0.00013862304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011206223,0.00008548871,0.9512341,0.000060995604,0.00017441493,0.00031643786,0.0005737345,0.00089497125,0.03233786,0.00010815426,0.0007919106,0.012301251],"study_design_scores_gemma":[0.000008305514,0.00006569265,0.99476033,0.000004171613,0.0000252386,0.00009154412,0.00013375102,0.0005359398,0.0035935827,0.000023237653,0.00075402635,0.0000041268913],"about_ca_topic_score_codex":0.029977754,"about_ca_topic_score_gemma":0.04903394,"teacher_disagreement_score":0.029977754,"about_ca_system_score_codex":0.00036930805,"about_ca_system_score_gemma":0.00025184962,"threshold_uncertainty_score":0.059606493},"labels":[],"label_agreement":null},{"id":"W2009314922","doi":"10.1029/2003gl017497","title":"Substorm associated changes in the high‐latitude ionospheric convection","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; Western University","funders":"","keywords":"Substorm; Convection; Geophysics; Geology; Ionosphere; Polar; Magnetometer; Latitude; Atmospheric sciences; Magnetosphere; Physics; Geodesy; Meteorology; Magnetic field","score_opus":0.01848171483501091,"score_gpt":0.2765158746047927,"score_spread":0.2580341597697818,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009314922","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994342,0.00004900256,0.00012640537,0.0000057960165,0.0000014174385,0.000003463915,0.00006903671,0.000005845499,0.00030483006],"genre_scores_gemma":[0.9997719,0.00002120706,0.000037943435,0.00000433501,0.0000019455524,0.000001858528,0.00009005186,8.25762e-7,0.00006993043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999616,0.0000046537284,0.0000020054717,0.000010042404,0.0000075831663,0.000014071054],"domain_scores_gemma":[0.99984527,0.000023080385,0.00004487484,0.000014398008,0.00004199158,0.000030506291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087076565,0.00010371151,0.00012639741,0.00019005545,0.00014359083,0.00019384407,0.00007626325,0.00012659354,0.00063642836],"category_scores_gemma":[0.00034087477,0.000059473205,0.00007223643,0.00014858792,0.00017149777,0.000092354356,0.00014316209,0.00012122162,0.000088397785],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007581222,0.000044724537,0.5055785,0.000051635503,0.00006798002,0.00030182945,0.00076718454,0.00091741624,0.47644752,0.00017191592,0.00024406871,0.014649037],"study_design_scores_gemma":[0.000003979652,0.000061372135,0.9938075,0.0000012799763,0.000007677463,0.00006457755,0.00006911846,0.00034981951,0.005439843,0.00001780762,0.00017501578,0.0000021706435],"about_ca_topic_score_codex":0.00618895,"about_ca_topic_score_gemma":0.0073115914,"teacher_disagreement_score":0.00618895,"about_ca_system_score_codex":0.0001973321,"about_ca_system_score_gemma":0.00010103393,"threshold_uncertainty_score":0.012305856},"labels":[],"label_agreement":null},{"id":"W2009527236","doi":"10.1029/2006gl028477","title":"Postseismic deformation following the 1991 Racha, Georgia, earthquake","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Aftershock; Geology; Seismology; Crust; Deformation (meteorology); Seismic moment; Tsunami earthquake; Geodesy; Moment (physics); Thrust; Geophysics; Fault (geology); Oceanography","score_opus":0.029511904896875933,"score_gpt":0.2860385575895907,"score_spread":0.25652665269271474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009527236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909425,0.000014618262,0.000020024821,0.000027675818,0.0000014810089,0.000002374803,0.00018435517,0.0000047348917,0.0006504963],"genre_scores_gemma":[0.9992836,0.000018617642,0.000029416977,0.000010442266,0.0000013889071,0.0000019809752,0.00034141383,0.0000014518661,0.00031159798],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.0000066617235,0.0000033144463,0.000016878827,0.000016609842,0.000021344733],"domain_scores_gemma":[0.9997813,0.000018432462,0.000084262945,0.000021947537,0.000056836496,0.000037168396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000083286825,0.00013925898,0.000119834425,0.00029447582,0.00030404722,0.00026447274,0.00019867896,0.0003591113,0.0007095034],"category_scores_gemma":[0.0006394159,0.000111051464,0.00007669865,0.00025297637,0.00021388795,0.00014949731,0.00029354967,0.00022271919,0.00029437896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005173267,0.00013659016,0.9292929,0.000055171357,0.00006514006,0.0008767865,0.0011285617,0.0068236482,0.03681471,0.000410047,0.002858341,0.021020833],"study_design_scores_gemma":[0.0000022688002,0.000023307077,0.9989423,0.0000018126547,0.0000025772283,0.00003376892,0.00005975272,0.0005573063,0.00014211782,0.000011851587,0.00022091513,0.0000020136333],"about_ca_topic_score_codex":0.07229655,"about_ca_topic_score_gemma":0.17837028,"teacher_disagreement_score":0.07229655,"about_ca_system_score_codex":0.000884536,"about_ca_system_score_gemma":0.00036063505,"threshold_uncertainty_score":0.1437515},"labels":[],"label_agreement":null},{"id":"W2009623812","doi":"10.1029/2009gl039225","title":"Evolution of shallow groundwater flow systems in areas of degrading permafrost","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":236,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Permafrost; Groundwater; Groundwater flow; Hydrogeology; Aquifer; Water table; Hydrology (agriculture); Geology; Groundwater discharge; Current (fluid); STREAMS; Environmental science; Flow (mathematics); Arctic; Subsurface flow; Groundwater model; Oceanography; Geotechnical engineering","score_opus":0.056741112222974927,"score_gpt":0.2914650201931205,"score_spread":0.23472390797014556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009623812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997389,0.000011421082,0.00006257356,0.00000767629,1.8875345e-7,6.263135e-7,0.00003876746,0.000003785051,0.00013613325],"genre_scores_gemma":[0.99976677,0.000011670616,0.000098741904,0.0000028788702,2.6764158e-7,7.2865083e-7,0.000055079297,8.5668995e-7,0.00006305015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996746,0.0000063678003,0.0000022989234,0.000010038441,0.0000037030647,0.000010144767],"domain_scores_gemma":[0.99988604,0.000020657004,0.00003449856,0.0000068750937,0.000018684006,0.000033305078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000977855,0.000057492547,0.00010755716,0.00045412628,0.00023221473,0.00032862404,0.00011162977,0.00022045203,0.000865604],"category_scores_gemma":[0.0003872446,0.00009820142,0.000118143165,0.00033084562,0.00027584896,0.0001810117,0.00021550103,0.0001272409,0.000066962486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049489515,0.00008095608,0.8487056,0.000049244627,0.00005390668,0.00045314585,0.0012113987,0.019457294,0.10499216,0.0012550956,0.00030453296,0.022941764],"study_design_scores_gemma":[0.000007281978,0.000060874634,0.985537,0.0000033812612,0.000007845534,0.00013890438,0.0002785629,0.011558318,0.0017704872,0.00039088924,0.00023679323,0.000009545307],"about_ca_topic_score_codex":0.007694144,"about_ca_topic_score_gemma":0.00941773,"teacher_disagreement_score":0.007694144,"about_ca_system_score_codex":0.0004930999,"about_ca_system_score_gemma":0.00019782323,"threshold_uncertainty_score":0.015298724},"labels":[],"label_agreement":null},{"id":"W2009732327","doi":"10.1029/2000gl011524","title":"Tropical convective outflow and near surface equivalent potential temperatures","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Goddard Space Flight Center","keywords":"Outflow; Convection; Troposphere; Atmospheric sciences; Potential temperature; Environmental science; Free convective layer; Sky; Climatology; Geology; Meteorology; Physics","score_opus":0.024499679415315414,"score_gpt":0.2951365464757004,"score_spread":0.27063686706038503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009732327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99598444,0.00014135851,0.0016143634,0.000034506473,0.0000026042862,0.000001050406,0.00026074777,0.000020180842,0.0019407616],"genre_scores_gemma":[0.9996166,0.00005358788,0.000086695254,0.0000028955355,0.0000035590026,5.775374e-7,0.00011544676,0.0000036683023,0.00011684928],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.000011285234,0.0000023147195,0.000008854292,0.0000069613357,0.00001636208],"domain_scores_gemma":[0.9994911,0.00022995492,0.00015274639,0.000023546349,0.00002029224,0.000082393104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016811409,0.0001301159,0.000073503674,0.00023360757,0.000103134276,0.0003486646,0.00007613209,0.00008912945,0.0010321249],"category_scores_gemma":[0.0009294938,0.000066114284,0.0001366797,0.00025464103,0.0002600017,0.00031166623,0.0002891956,0.00015725833,0.00008966557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078281836,0.00005677062,0.7245745,0.000083958446,0.00014194462,0.00058921723,0.00041969935,0.19007514,0.035125844,0.027413458,0.00078941305,0.019947283],"study_design_scores_gemma":[0.00002706938,0.00006886504,0.8614924,0.000014279315,0.000036965248,0.0005125389,0.000114229246,0.12280857,0.0047305254,0.008806059,0.0013691289,0.000019422887],"about_ca_topic_score_codex":0.0024882583,"about_ca_topic_score_gemma":0.001272138,"teacher_disagreement_score":0.0024882583,"about_ca_system_score_codex":0.00017599342,"about_ca_system_score_gemma":0.00008156411,"threshold_uncertainty_score":0.004947543},"labels":[],"label_agreement":null},{"id":"W2009869185","doi":"10.1029/2005gl022388","title":"Initial validation comparisons for the Atmospheric Chemistry Experiment (ACE‐FTS)","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Satellite; Ozone; Atmospheric sciences; Environmental science; Northern Hemisphere; Aerosol; Southern Hemisphere; Remote sensing; Latitude; Atmospheric sounding; Atmospheric chemistry; Meteorology; Climatology; Geology; Geodesy; Physics; Astronomy","score_opus":0.052221119386646225,"score_gpt":0.33590269629874303,"score_spread":0.28368157691209683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009869185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8649927,0.0019861767,0.06707538,0.0012221393,0.00095970824,0.0013668919,0.032584786,0.0015165948,0.028295659],"genre_scores_gemma":[0.8907486,0.00051055104,0.053325318,0.00070430315,0.00014892354,0.00081545336,0.048032288,0.00046469798,0.0052499357],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99109393,0.0025807912,0.0005665074,0.0012529567,0.0038968823,0.00060898694],"domain_scores_gemma":[0.9697099,0.0073789246,0.0014947469,0.0044989674,0.016336253,0.0005812177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.026857248,0.0011591497,0.0005811839,0.0014862728,0.0012863709,0.0016268665,0.0020574392,0.0018598771,0.0018917631],"category_scores_gemma":[0.027457362,0.00049488805,0.0010194445,0.0014094105,0.00054661115,0.0021192944,0.001700448,0.0011954267,0.0009513117],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008428235,0.0037009018,0.5335465,0.00076889136,0.0015992005,0.0007335298,0.001463347,0.08366099,0.113410555,0.009678749,0.04876041,0.19424877],"study_design_scores_gemma":[0.0009151207,0.0027363454,0.66163045,0.00035380118,0.00048654372,0.00048296052,0.00073699513,0.09776761,0.15813035,0.003546618,0.07295776,0.00025545515],"about_ca_topic_score_codex":0.015645316,"about_ca_topic_score_gemma":0.012643203,"teacher_disagreement_score":0.026857248,"about_ca_system_score_codex":0.0023332194,"about_ca_system_score_gemma":0.0015627027,"threshold_uncertainty_score":0.14203638},"labels":[],"label_agreement":null},{"id":"W2009963997","doi":"10.1029/2008gl036308","title":"Sensitivity of the subpolar Atlantic climate to local winds","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"North Atlantic Deep Water; Thermohaline circulation; Oceanography; Shutdown of thermohaline circulation; Climatology; Atlantic Equatorial mode; Geology; Wind stress; Gulf Stream; Atlantic multidecadal oscillation; Tropical Atlantic; North Atlantic oscillation; Arctic; Sea surface temperature","score_opus":0.016209572120618784,"score_gpt":0.25944218625856846,"score_spread":0.24323261413794967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2009963997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981501,0.00008045264,0.000087354754,0.00005821374,0.000007457735,0.0000047539884,0.00035155943,0.000010762781,0.0012493073],"genre_scores_gemma":[0.99947983,0.0000553997,0.000020234253,0.000022609802,0.000003955662,0.0000016344485,0.00027376614,0.0000035201112,0.0001390504],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987125,0.000030024265,0.000007783778,0.00003806326,0.000015712541,0.000037142894],"domain_scores_gemma":[0.9992723,0.00023752624,0.00014197888,0.00010127139,0.00010549918,0.00014144155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029841444,0.00013852592,0.00028000213,0.000251063,0.00020979847,0.00078887836,0.00012505398,0.00030334134,0.001568026],"category_scores_gemma":[0.0012464831,0.00016291122,0.00022598683,0.000286175,0.00016785157,0.0002473286,0.00033032242,0.00028590774,0.00031841092],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052687817,0.00007745837,0.93523574,0.000041049963,0.0002993727,0.00033719782,0.00021375786,0.02851966,0.026333591,0.00032020104,0.0009524049,0.0071426076],"study_design_scores_gemma":[0.000011772337,0.000038408474,0.99193805,0.000005105296,0.000023801582,0.000043792712,0.00014834055,0.006592222,0.00071760104,0.00013939917,0.0003319011,0.000009638974],"about_ca_topic_score_codex":0.021743855,"about_ca_topic_score_gemma":0.018760838,"teacher_disagreement_score":0.021743855,"about_ca_system_score_codex":0.00035957908,"about_ca_system_score_gemma":0.00017688744,"threshold_uncertainty_score":0.043234587},"labels":[],"label_agreement":null},{"id":"W2010235654","doi":"10.1029/2007gl031385","title":"An RCM projection of soil thermal and moisture regimes for North American permafrost zones","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Ouranos; Université du Québec à Montréal","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Permafrost; Water content; Environmental science; Moisture; Climate change; Hydrology (agriculture); Geology; Climatology; Atmospheric sciences; Soil science; Meteorology; Geography; Geotechnical engineering","score_opus":0.04640771048041154,"score_gpt":0.31913010302667943,"score_spread":0.2727223925462679,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010235654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.76965576,0.0028543263,0.010374405,0.002378806,0.00024592457,0.00016495581,0.12031686,0.0017079546,0.09230107],"genre_scores_gemma":[0.9513956,0.0017275496,0.010713656,0.00011953536,0.00002805039,0.0001628957,0.02836614,0.00007791322,0.0074086906],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984014,0.00002132785,0.000004418212,0.000023266302,0.00007096692,0.000039944065],"domain_scores_gemma":[0.99973506,0.000009541906,0.0000134547945,0.000011608518,0.00020404492,0.000026313304],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025593492,0.0005626182,0.00021057705,0.0010881305,0.00064460584,0.0005499594,0.000634869,0.00036342046,0.003504774],"category_scores_gemma":[0.00043822662,0.00023301385,0.0005403643,0.0015564427,0.00016407091,0.00025302463,0.0003014087,0.00045321335,0.00065155537],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038132694,0.00011105453,0.09222569,0.00037690054,0.00033982523,0.0003576446,0.0002930027,0.7330911,0.0049005984,0.008033214,0.07402068,0.085868835],"study_design_scores_gemma":[0.00020102836,0.00006410734,0.46585262,0.00018188091,0.00020357482,0.00016767309,0.00054420193,0.35085627,0.004569511,0.0038314979,0.17330353,0.00022409658],"about_ca_topic_score_codex":0.9169432,"about_ca_topic_score_gemma":0.91434014,"teacher_disagreement_score":0.9169432,"about_ca_system_score_codex":0.008382665,"about_ca_system_score_gemma":0.0078081456,"threshold_uncertainty_score":0.16709185},"labels":[],"label_agreement":null},{"id":"W2010408594","doi":"10.1029/2009gl041269","title":"Attribution of anthropogenic influence on seasonal sea level pressure","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Department for Environment, Food and Rural Affairs, UK Government; U.S. Department of Energy","keywords":"Latitude; Climatology; Northern Hemisphere; Southern Hemisphere; Subtropics; Middle latitudes; Boreal; Environmental science; Tropics; High latitude; Atmospheric sciences; Sea level; Geology; Oceanography; Ecology","score_opus":0.07703776003485426,"score_gpt":0.31926309685725535,"score_spread":0.2422253368224011,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010408594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99646986,0.00005140453,0.00044814905,0.00008873626,0.000013070538,0.0000028486577,0.0002985641,0.000023629753,0.0026037053],"genre_scores_gemma":[0.99960214,0.00003166008,0.0000545156,0.0000068922755,0.0000096543245,0.0000013938329,0.00020009978,0.0000058230216,0.000087875254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996643,0.00009390456,0.000029309122,0.0000731734,0.00007274515,0.00006656735],"domain_scores_gemma":[0.9979413,0.00054277485,0.00064757705,0.00024917582,0.0004283453,0.00019086395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004886895,0.00018681106,0.00015741945,0.0006538311,0.00022150867,0.00067399006,0.00020999358,0.0001266172,0.0012720489],"category_scores_gemma":[0.0027831818,0.0001075589,0.0002812253,0.0008251274,0.0004695945,0.00027936697,0.00076211157,0.0002302686,0.0001258652],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000636263,0.000014612865,0.9906103,0.000014134088,0.00006912381,0.00007059453,0.000116184536,0.0011371974,0.0014627771,0.00021451281,0.00011518224,0.006111796],"study_design_scores_gemma":[0.0000017459193,0.000016184169,0.9969748,0.0000033595115,0.000010763958,0.000025107227,0.00011194886,0.0022008896,0.000249637,0.00008604349,0.00031523986,0.000004223991],"about_ca_topic_score_codex":0.0076954826,"about_ca_topic_score_gemma":0.011414749,"teacher_disagreement_score":0.0076954826,"about_ca_system_score_codex":0.0003959619,"about_ca_system_score_gemma":0.00028894178,"threshold_uncertainty_score":0.015301406},"labels":[],"label_agreement":null},{"id":"W2010423728","doi":"10.1029/2000gl900007","title":"Correction to “Anomalous temperatures in central Scotia Sea sediments—bottom water variation or pore water circulation in old ocean crust”","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Oceanography; Citation; Nova scotia; History; Library science; Geophysics; Computer science","score_opus":0.012860710063018827,"score_gpt":0.2545938778407331,"score_spread":0.24173316777771428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010423728","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0003843506,0.0014213347,0.0008278025,0.030957097,0.96414995,0.000023732335,0.00083836116,0.00041086614,0.0009864544],"genre_scores_gemma":[0.038998272,0.0099531505,0.005115199,0.14866903,0.68102604,0.00030256173,0.004433211,0.00157771,0.10992475],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9966491,0.0005412754,0.0006586137,0.0005907419,0.001124405,0.00043592489],"domain_scores_gemma":[0.97989684,0.004781776,0.0017263378,0.0017951911,0.010313768,0.0014860759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002904714,0.0027460272,0.0027353845,0.0038528664,0.0031142563,0.0034390583,0.0034281458,0.00793293,0.021850279],"category_scores_gemma":[0.03809662,0.0013518088,0.0021266018,0.002992877,0.002579287,0.0019640182,0.00260134,0.010255414,0.0153107885],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011402893,0.000011237746,0.00025540675,0.00030286596,0.000037373444,0.0003683338,0.000054952696,0.000101481266,0.00022004527,0.00067931757,0.9918967,0.0059583304],"study_design_scores_gemma":[0.00017476077,0.00004981859,0.0059881485,0.0003029824,0.00009368822,0.0008506469,0.00015126505,0.00064203434,0.0009984155,0.0016255487,0.98905444,0.00006826833],"about_ca_topic_score_codex":0.023372544,"about_ca_topic_score_gemma":0.023303822,"teacher_disagreement_score":0.023372544,"about_ca_system_score_codex":0.0029353872,"about_ca_system_score_gemma":0.0039526033,"threshold_uncertainty_score":0.073096514},"labels":[],"label_agreement":null},{"id":"W2010652876","doi":"10.1029/1999gl011233","title":"The Extended Canadian Middle Atmosphere Model","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Thermosphere; Atmosphere (unit); Mesosphere; Gravity wave; Orographic lift; Atmospheric sciences; Atmospheric models; Atmospheric model; Middle latitudes; Drag; Environmental science; Satellite; Geology; Climatology; Meteorology; Gravitational wave; Stratosphere; Physics; Ionosphere; Geophysics; Mechanics","score_opus":0.019573223649171884,"score_gpt":0.26779691452658205,"score_spread":0.24822369087741017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010652876","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2964217,0.0060920604,0.09671096,0.0058648204,0.001022464,0.00075592985,0.17848831,0.0075531597,0.40709054],"genre_scores_gemma":[0.8690662,0.0019145143,0.047178846,0.00048467942,0.00007615444,0.00034612353,0.03941093,0.0008045442,0.04071814],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969256,0.000040138897,0.0000086078935,0.000050575632,0.00011199729,0.00009619275],"domain_scores_gemma":[0.9994019,0.000036056124,0.000019013076,0.000034303266,0.0004009783,0.00010768847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038694587,0.00080096006,0.00051872333,0.0007511542,0.0022394378,0.0023854305,0.0027279076,0.00060760725,0.015098111],"category_scores_gemma":[0.0011810894,0.00031670762,0.0007709769,0.0015702889,0.00039746767,0.0012635227,0.0009558844,0.0010196053,0.0016393227],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032095308,0.00006518332,0.018883603,0.00017365334,0.00032891793,0.00022634718,0.0002524825,0.80719286,0.0018028484,0.051874783,0.07851621,0.040362235],"study_design_scores_gemma":[0.00016968501,0.000029470839,0.012745307,0.000078437646,0.00016114603,0.00005217555,0.00022493424,0.7967789,0.0008858169,0.009935885,0.1787964,0.00014185936],"about_ca_topic_score_codex":0.96734035,"about_ca_topic_score_gemma":0.95475924,"teacher_disagreement_score":0.96734035,"about_ca_system_score_codex":0.013307098,"about_ca_system_score_gemma":0.01905741,"threshold_uncertainty_score":0.09655017},"labels":[],"label_agreement":null},{"id":"W2010915548","doi":"10.1029/2008gl035625","title":"Scale‐free and scale‐dependent modes of energy release dynamics in the nighttime magnetosphere","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Magnetosphere; Scaling; Physics; Dissipation; Power law; Polar; Latitude; Plasma sheet; Universality (dynamical systems); Range (aeronautics); Turbulence; Atmospheric sciences; Plasma; Electron precipitation; Computational physics; Statistical physics; Meteorology; Astronomy; Statistics; Materials science; Geometry; Mathematics","score_opus":0.011169003616251763,"score_gpt":0.2447013128298561,"score_spread":0.23353230921360435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2010915548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962639,0.00005166286,0.003211325,0.000012771306,0.0000011811499,0.00000184287,0.000054039043,0.000011763437,0.0003914038],"genre_scores_gemma":[0.99959284,0.000020861538,0.00026757145,0.000001159405,0.000002909134,0.0000015434479,0.00003407221,0.0000021678145,0.00007700908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999813,0.0000024561873,8.782194e-7,0.0000063870525,0.0000037466386,0.000005294593],"domain_scores_gemma":[0.99990106,0.000023525161,0.000036470134,0.0000133590565,0.000010396297,0.000015196027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000051514526,0.00007485108,0.00007514474,0.0003526253,0.00010853273,0.00023265932,0.00009823148,0.000066234934,0.0003417906],"category_scores_gemma":[0.00027904194,0.00007275714,0.000107296146,0.00017654758,0.0001749539,0.00019525479,0.00013180083,0.000084083076,0.000044360655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007440535,0.00012394211,0.4645548,0.000100538266,0.00018370726,0.0015217736,0.0013804047,0.049137454,0.40887204,0.013649476,0.0009809067,0.058750957],"study_design_scores_gemma":[0.000011145831,0.000050694573,0.85932773,0.0000036500262,0.00002248833,0.0004125512,0.00015477015,0.13128877,0.0059809135,0.0023520452,0.0003756006,0.0000196039],"about_ca_topic_score_codex":0.0007904047,"about_ca_topic_score_gemma":0.000888946,"teacher_disagreement_score":0.0007904047,"about_ca_system_score_codex":0.00009810951,"about_ca_system_score_gemma":0.00005260294,"threshold_uncertainty_score":0.0015716553},"labels":[],"label_agreement":null},{"id":"W2011216096","doi":"10.1029/2001gl014119","title":"Magnetotelluric imaging of the creeping segment of the San Andreas Fault near Hollister","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Magnetotellurics; Geology; San andreas fault; Seismology; Induced seismicity; Fault (geology); Inversion (geology); Tectonics; Geophysics; Electrical resistivity and conductivity","score_opus":0.03996333278326362,"score_gpt":0.2796255227985332,"score_spread":0.2396621900152696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011216096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99836975,0.00005224947,0.00033946167,0.000041931853,0.0000016716369,0.000002596926,0.00013649139,0.000039757568,0.0010161062],"genre_scores_gemma":[0.9982712,0.00005949215,0.00092035445,0.0000075052762,0.0000064184337,0.0000016659784,0.000196333,0.0000032719777,0.00053367467],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999702,0.0000029152047,0.0000011616071,0.000009253155,0.000010403354,0.0000060302455],"domain_scores_gemma":[0.9999403,0.0000064587803,0.00002068036,0.0000047545277,0.00001663234,0.0000112257385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006780095,0.00010671963,0.0000802477,0.00038839143,0.00020039812,0.00016074817,0.00013796147,0.00012773616,0.0003793428],"category_scores_gemma":[0.00016878113,0.00008475235,0.000040851588,0.00024929098,0.00012592523,0.000121806304,0.00011504972,0.000095815456,0.00007488628],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040462363,0.00025404108,0.39435282,0.00012422915,0.00007079248,0.0007543244,0.0010535507,0.007265033,0.5338782,0.0005848116,0.0020288634,0.059228756],"study_design_scores_gemma":[0.000026652671,0.00007522884,0.96849525,0.000010884436,0.00002632149,0.0002316774,0.0002268361,0.012932599,0.016157227,0.00007628137,0.0017293355,0.00001163107],"about_ca_topic_score_codex":0.018660873,"about_ca_topic_score_gemma":0.069305114,"teacher_disagreement_score":0.018660873,"about_ca_system_score_codex":0.00024399074,"about_ca_system_score_gemma":0.00019387716,"threshold_uncertainty_score":0.037104487},"labels":[],"label_agreement":null},{"id":"W2011243969","doi":"10.1002/2013gl058456","title":"Radiative forcing at high concentrations of well‐mixed greenhouse gases","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Western Canada Research Grid; Compute Canada; University of Victoria","keywords":"Radiative forcing; Greenhouse gas; Forcing (mathematics); Tropopause; Atmospheric sciences; Environmental science; Climatology; Climate sensitivity; Radiative transfer; Climate change; Climate model; Range (aeronautics); Cloud forcing; Troposphere; Physics; Materials science; Geology","score_opus":0.015168526051040451,"score_gpt":0.2494782514578019,"score_spread":0.23430972540676143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011243969","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9158743,0.0003657122,0.05363882,0.00067564694,0.00012974981,0.000058149086,0.0013041625,0.00091357325,0.027039917],"genre_scores_gemma":[0.98998964,0.00018436671,0.008176166,0.0000769399,0.000038323014,0.000054687633,0.0004186478,0.00011260743,0.0009484454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997632,0.00007507142,0.0000116256515,0.000035043806,0.000072389,0.000042671076],"domain_scores_gemma":[0.99935144,0.000277127,0.00008611693,0.000105581115,0.00013674019,0.000042930846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003812463,0.0007091525,0.0007218571,0.00034217516,0.00063322805,0.0010029844,0.001101758,0.0008256237,0.0018704819],"category_scores_gemma":[0.0020634965,0.00054780295,0.0009429205,0.0006201108,0.0006486106,0.0009447437,0.00064196315,0.00091523875,0.00019604107],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036983292,0.000024330686,0.0016689377,0.000035966794,0.000033066703,0.00011839316,0.000034660417,0.9889404,0.004698297,0.00189747,0.0003884145,0.0021231298],"study_design_scores_gemma":[0.00008552626,0.00002744136,0.003987928,0.000006816716,0.000035003734,0.000033976547,0.000023882425,0.9889538,0.0042387214,0.0018399132,0.0007388831,0.00002808228],"about_ca_topic_score_codex":0.020329181,"about_ca_topic_score_gemma":0.01444701,"teacher_disagreement_score":0.020329181,"about_ca_system_score_codex":0.0011246095,"about_ca_system_score_gemma":0.0009724467,"threshold_uncertainty_score":0.040421724},"labels":[],"label_agreement":null},{"id":"W2011273066","doi":"10.1029/2005gl025496","title":"Temporal variance of lower mesospheric ozone over Switzerland during winter 2000/2001","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"GLS Industries (Canada)","funders":"North Dakota Soybean Council","keywords":"Stratosphere; Atmospheric sciences; Mesosphere; Environmental science; Ozone; Altitude (triangle); Radiometer; Gravity wave; Ozone layer; Climatology; Mixing ratio; Daytime; Meteorology; Gravitational wave; Physics; Geology; Remote sensing; Mathematics","score_opus":0.0157949595918482,"score_gpt":0.2567909455150138,"score_spread":0.2409959859231656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011273066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99883634,0.00005578554,0.00005025386,0.00002363012,0.0000031930733,0.0000015209515,0.00071276835,0.000011754376,0.00030486655],"genre_scores_gemma":[0.9985266,0.000027698765,0.00003087237,0.000005708707,0.000005288832,0.0000028367697,0.0012435535,0.0000024155663,0.00015510796],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999088,0.000009264657,0.000005413311,0.000027010961,0.000022196627,0.000027419477],"domain_scores_gemma":[0.9996811,0.00006503957,0.00012130751,0.000021705227,0.00005717464,0.000053628097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022440909,0.00025770892,0.0001544691,0.0006707774,0.0002673798,0.00054684014,0.00011952755,0.00032097232,0.0007401409],"category_scores_gemma":[0.00042416446,0.00011333981,0.00014879023,0.0005843711,0.00015917791,0.00019735393,0.00018047864,0.00021790106,0.00019652114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006642047,0.000069594214,0.97437245,0.000048564674,0.00016678027,0.00033942994,0.0005871438,0.002288441,0.012190705,0.00016024226,0.0011815677,0.007930899],"study_design_scores_gemma":[0.0000024400454,0.000014920072,0.99905866,0.0000016797412,0.000007660204,0.000024782494,0.000031561074,0.00046030091,0.0002042118,0.000005959256,0.00018535572,0.0000025667914],"about_ca_topic_score_codex":0.02553294,"about_ca_topic_score_gemma":0.04106619,"teacher_disagreement_score":0.02553294,"about_ca_system_score_codex":0.00050176366,"about_ca_system_score_gemma":0.00016305187,"threshold_uncertainty_score":0.050768614},"labels":[],"label_agreement":null},{"id":"W2011557819","doi":"10.1029/2002gl016723","title":"Long‐term decrease of cadmium concentrations in the Canadian Arctic air","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Trent University; Health Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Health Canada","keywords":"Cadmium; Arctic; Environmental science; Particulates; Environmental chemistry; Ferrous; Air pollution; The arctic; Atmospheric sciences; Oceanography; Chemistry; Geology","score_opus":0.043506415604917886,"score_gpt":0.32874187799027305,"score_spread":0.28523546238535513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011557819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99633455,0.00050439953,0.000119516684,0.00018263317,0.000013759336,0.0000064313176,0.0009975947,0.0000127864105,0.0018283803],"genre_scores_gemma":[0.9969758,0.00030215184,0.00014436174,0.00007111323,0.0000059576346,0.000006024028,0.0008432267,0.0000027816423,0.0016485441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996165,0.0000151967015,0.000010756751,0.000081456936,0.00017329502,0.0001028715],"domain_scores_gemma":[0.9987966,0.00003700516,0.00008229284,0.000027876009,0.00092620956,0.0001300608],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037863824,0.00035218635,0.00036479297,0.000688202,0.0020912196,0.00087276835,0.0005875514,0.0005439957,0.0006821176],"category_scores_gemma":[0.00080627686,0.0002412666,0.0001892197,0.0011514067,0.0006403893,0.00026137018,0.00043704,0.0004651749,0.0001871466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067467976,0.00010618693,0.93528056,0.00009586897,0.00022458345,0.00030302882,0.0013181055,0.00085771,0.03551525,0.00016538377,0.0021537694,0.023304857],"study_design_scores_gemma":[0.0000034053232,0.00002470205,0.9964503,0.000005482541,0.000024791827,0.000035666,0.00026029567,0.00011790883,0.0012859072,0.000009113534,0.0017750622,0.0000074472005],"about_ca_topic_score_codex":0.9527701,"about_ca_topic_score_gemma":0.96872777,"teacher_disagreement_score":0.047229886,"about_ca_system_score_codex":0.010439627,"about_ca_system_score_gemma":0.008546908,"threshold_uncertainty_score":0.095016},"labels":[],"label_agreement":null},{"id":"W2011569431","doi":"10.1029/2007gl032997","title":"Salmon‐driven bed load transport and bed morphology in mountain streams","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Skeena Fisheries Commission; University of British Columbia","funders":"","keywords":"Bed load; STREAMS; Sediment transport; Hydrology (agriculture); Sediment; River morphology; Environmental science; Channel (broadcasting); Alluvium; Bedform; Stream bed; Ecosystem; Geology; Drainage basin; Ecology; Geomorphology; Geography; Biology; Geotechnical engineering","score_opus":0.022677715989697658,"score_gpt":0.27662357197582166,"score_spread":0.253945855986124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011569431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995726,0.000024712617,0.000065098706,0.0000063703264,5.2127257e-7,0.0000017225184,0.00014868948,0.0000049579608,0.00017535848],"genre_scores_gemma":[0.99934834,0.000027607666,0.000080649916,0.0000030349452,7.8580644e-7,0.0000029728599,0.00031426293,0.000002276186,0.00022005975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984384,0.000036948593,0.000013194053,0.000029090505,0.00003634881,0.000040481984],"domain_scores_gemma":[0.99955934,0.00008136719,0.00014299057,0.000023678162,0.000117111325,0.000075486954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002741377,0.00010383095,0.00015832386,0.00083633175,0.00048115134,0.0006938762,0.00020073354,0.00016614569,0.0010812485],"category_scores_gemma":[0.0008982581,0.00019100322,0.0001322538,0.0013121008,0.00036433036,0.00018822963,0.0002838858,0.00014298706,0.00015513747],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048958125,0.000010982228,0.9945904,0.000008710879,0.000030404184,0.0000643691,0.00032218298,0.00047394296,0.0008273003,0.000030163983,0.00012365333,0.0034689838],"study_design_scores_gemma":[0.0000014468702,0.0000061780925,0.9994129,0.0000014964506,0.0000031289944,0.000015456748,0.00013703409,0.0003196248,0.00002959729,0.000008569395,0.000062475716,0.0000021590463],"about_ca_topic_score_codex":0.2687159,"about_ca_topic_score_gemma":0.5405135,"teacher_disagreement_score":0.2687159,"about_ca_system_score_codex":0.0010406044,"about_ca_system_score_gemma":0.00068408495,"threshold_uncertainty_score":0.53430355},"labels":[],"label_agreement":null},{"id":"W2011665680","doi":"10.1029/2008gl036331","title":"Crustal structure beneath the Florida‐to‐Edmonton broadband seismometer array","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismometer; Seismology; Rift; Orogeny; Crust; Proterozoic; Paleozoic; Metamorphism; Lithosphere; Tectonics; Petrology; Geophysics; Geochemistry","score_opus":0.021472977991427354,"score_gpt":0.2733097236939273,"score_spread":0.2518367457025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011665680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950021,0.00008299135,0.0007201081,0.000028874525,0.0000018133494,0.0000036397773,0.0012661405,0.000036511687,0.0028578],"genre_scores_gemma":[0.9943784,0.00006496227,0.0012453293,0.000008387135,0.0000020715904,0.0000042377324,0.0012663954,0.00000613994,0.003024116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997616,0.0000013149362,6.766104e-7,0.0000068857667,0.000005898567,0.0000090708445],"domain_scores_gemma":[0.9999374,0.0000058689698,0.000013150038,0.0000037723526,0.000031127103,0.000008663434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057424546,0.00027110006,0.000060360824,0.0005969546,0.00016688573,0.00020387027,0.00011661971,0.00009310055,0.0033093274],"category_scores_gemma":[0.00015790097,0.00012034676,0.00007683247,0.0004135092,0.0000650273,0.00015340082,0.0001895554,0.00009057374,0.0002264661],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000401629,0.000031724143,0.5443071,0.000067220826,0.00014904051,0.00031459815,0.00087738945,0.009502707,0.2827503,0.0015074797,0.0036309047,0.15645988],"study_design_scores_gemma":[0.000004562074,0.000018972745,0.9919504,0.000005754465,0.000018208886,0.000055090055,0.00008591297,0.0030170355,0.0032320796,0.0000708289,0.0015351974,0.000005926977],"about_ca_topic_score_codex":0.13526341,"about_ca_topic_score_gemma":0.28078523,"teacher_disagreement_score":0.86473656,"about_ca_system_score_codex":0.00056224375,"about_ca_system_score_gemma":0.0003668077,"threshold_uncertainty_score":0.2689522},"labels":[],"label_agreement":null},{"id":"W2011768812","doi":"10.1029/2002gl016802","title":"Nucleation of gas hydrate in marine environments","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Nucleation; Clathrate hydrate; Hydrate; Extrapolation; Geology; Supercooling; Seafloor spreading; Porosity; Thermodynamics; Materials science; Mineralogy; Chemistry; Geophysics; Geotechnical engineering; Physics","score_opus":0.019790456528357876,"score_gpt":0.26812809580497304,"score_spread":0.24833763927661517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011768812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97068465,0.0019707284,0.018302891,0.00009516991,0.000025430621,0.000020679958,0.00019212074,0.00013579572,0.008572472],"genre_scores_gemma":[0.99714357,0.0007381585,0.0012011218,0.000005157646,0.0000046907453,0.000011911632,0.00011479326,0.000009129256,0.00077156874],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994934,0.000008559313,0.0000026185417,0.0000132569485,0.000012170668,0.000014005267],"domain_scores_gemma":[0.9999522,0.000026097647,0.0000062427544,0.00000337321,0.000005755039,0.000006390401],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011861536,0.00025403962,0.00021314385,0.00022307558,0.00028759867,0.00031541343,0.00023021044,0.00022398114,0.00054868107],"category_scores_gemma":[0.00029647336,0.00022928274,0.0002237374,0.0001119358,0.0003303007,0.00029296055,0.00050069485,0.0001635818,0.00011547253],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034404718,0.000054608532,0.013831704,0.0004741023,0.000050412244,0.0014047703,0.0004524843,0.20065387,0.731139,0.032935094,0.0006708562,0.017989064],"study_design_scores_gemma":[0.00004873449,0.0002253373,0.02191702,0.00003562864,0.000029109353,0.0005716931,0.00032968126,0.50248903,0.45432448,0.013535469,0.006446947,0.00004694829],"about_ca_topic_score_codex":0.0062573147,"about_ca_topic_score_gemma":0.0032252914,"teacher_disagreement_score":0.0062573147,"about_ca_system_score_codex":0.00068314356,"about_ca_system_score_gemma":0.00016526389,"threshold_uncertainty_score":0.012441814},"labels":[],"label_agreement":null},{"id":"W2011769532","doi":"10.1002/2014gl060613","title":"Rapid subsurface warming and circulation changes of Antarctic coastal waters by poleward shifting winds","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":244,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Oceanography; Climatology; Advection; Geology; Global wind patterns; Forcing (mathematics); Environmental science; Shore; Global warming; Peninsula; Climate change; Atmospheric sciences; Geography","score_opus":0.03712210483947338,"score_gpt":0.26312272821078486,"score_spread":0.2260006233713115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2011769532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903727,0.000015794165,0.00018599187,0.00004914233,0.000008233148,0.000002326442,0.00010558659,0.000016973776,0.00057880627],"genre_scores_gemma":[0.9997187,0.000023201263,0.000086209475,0.000011428566,0.0000025897334,0.000001943743,0.00006398821,0.0000031805453,0.000088655586],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999621,0.000011002491,0.0000024298042,0.0000073634287,0.0000056420017,0.000011599478],"domain_scores_gemma":[0.9999336,0.00001415313,0.000016831254,0.000007928729,0.000010458121,0.000016957341],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008391334,0.00032411498,0.00015044183,0.00015825534,0.00017504217,0.00044312424,0.00015472558,0.0003720827,0.0019052603],"category_scores_gemma":[0.00020941035,0.00013739578,0.00044807504,0.00020764499,0.00023370069,0.000229748,0.00027517363,0.00027346108,0.00013506951],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057498395,0.00022057559,0.293781,0.00010807514,0.0003373944,0.0011204365,0.0001721097,0.6013201,0.088900976,0.0012755422,0.0018460625,0.010342677],"study_design_scores_gemma":[0.00027697423,0.00039647456,0.4687867,0.000023070865,0.00014347702,0.0002013558,0.00039913875,0.51625735,0.010420481,0.0011575575,0.0018899868,0.00004747266],"about_ca_topic_score_codex":0.011237257,"about_ca_topic_score_gemma":0.0076928185,"teacher_disagreement_score":0.011237257,"about_ca_system_score_codex":0.00047000288,"about_ca_system_score_gemma":0.0002816471,"threshold_uncertainty_score":0.022343695},"labels":[],"label_agreement":null},{"id":"W2012252613","doi":"10.1029/2004gl021951","title":"Response of thermohaline circulation and thermal structure to removal of ice sheets and high atmospheric CO<sub>2</sub> concentration","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Thermohaline circulation; Geology; Convection; Shutdown of thermohaline circulation; North Atlantic Deep Water; Salinity; Climatology; Atmospheric sciences; Oceanography; Precipitation; Environmental science; Meteorology","score_opus":0.011378565584090743,"score_gpt":0.2598665439093129,"score_spread":0.24848797832522215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012252613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990289,0.000023989336,0.00024964276,0.00006455814,0.00000842943,0.000003984151,0.000088412955,0.000023232555,0.0005087814],"genre_scores_gemma":[0.9995939,0.00002299607,0.00009756414,0.00001661553,0.0000029793785,0.0000037436264,0.0000944483,0.0000046794175,0.00016310971],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999517,0.00000843485,0.000002546066,0.000010267273,0.000005966426,0.000021103613],"domain_scores_gemma":[0.99983084,0.000050135503,0.00003280074,0.000014132025,0.000020222566,0.00005187439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010279828,0.00032322377,0.00025552337,0.000117379815,0.00023357326,0.0003551043,0.00029648014,0.0005201694,0.0010115206],"category_scores_gemma":[0.0006098386,0.00023395843,0.0004689843,0.00008727633,0.0003639908,0.0003012892,0.00036909318,0.0004447785,0.000088692635],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021327578,0.00047610028,0.1274676,0.0001397193,0.0005362428,0.0007230884,0.00017690579,0.6025666,0.25526193,0.0013639469,0.0014197357,0.007735418],"study_design_scores_gemma":[0.00017246537,0.00041196693,0.18477848,0.0000066785205,0.00012369738,0.000107894484,0.00016255557,0.80033857,0.012833423,0.00058721687,0.00043587302,0.000041105664],"about_ca_topic_score_codex":0.012419457,"about_ca_topic_score_gemma":0.008030464,"teacher_disagreement_score":0.012419457,"about_ca_system_score_codex":0.00048910873,"about_ca_system_score_gemma":0.00038259488,"threshold_uncertainty_score":0.024694324},"labels":[],"label_agreement":null},{"id":"W2012276975","doi":"10.1029/2000gl012069","title":"The preferred structure of variability of the northern hemisphere atmospheric circulation","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of British Columbia","funders":"","keywords":"Extratropical cyclone; Northern Hemisphere; Geopotential height; Climatology; Atmospheric circulation; Arctic oscillation; Troposphere; Atmospheric sciences; Environmental science; Principal component analysis; Geopotential; Southern Hemisphere; Geology; Meteorology; Geography; Mathematics; Precipitation","score_opus":0.024146444011017624,"score_gpt":0.2751206522834006,"score_spread":0.250974208272383,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012276975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97616845,0.00023437168,0.02016628,0.00014016517,0.0000060692614,0.000011019336,0.00024754816,0.000052667107,0.0029734096],"genre_scores_gemma":[0.99742967,0.00008124387,0.0021153807,0.0000064255855,0.0000072048906,0.000007534534,0.0001554163,0.000010167252,0.0001868975],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998355,0.000054461234,0.0000078352605,0.000046034434,0.000027112417,0.0000291063],"domain_scores_gemma":[0.99953985,0.0001450294,0.00010324995,0.000064943975,0.000108761524,0.000038121692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037100873,0.00011752597,0.00009284938,0.00041671432,0.0002465234,0.00075984903,0.00011365551,0.00014012987,0.00072180654],"category_scores_gemma":[0.0020605705,0.00015753508,0.00017529538,0.00039659144,0.00053413404,0.00042661902,0.0003128472,0.00029069913,0.00011951513],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008916059,0.00012808408,0.42683083,0.0003730819,0.0004010987,0.0005830944,0.0049297726,0.117085665,0.14785303,0.117655344,0.004310774,0.1789576],"study_design_scores_gemma":[0.000027748501,0.00012846156,0.7284312,0.000036910056,0.00006299178,0.00038844006,0.00059221,0.19841765,0.004274581,0.06544967,0.002117249,0.00007287737],"about_ca_topic_score_codex":0.0024435401,"about_ca_topic_score_gemma":0.003655542,"teacher_disagreement_score":0.0024435401,"about_ca_system_score_codex":0.00038313525,"about_ca_system_score_gemma":0.00040025474,"threshold_uncertainty_score":0.0048586726},"labels":[],"label_agreement":null},{"id":"W2012303460","doi":"10.1029/2006gl028371","title":"Effect of Alpine glaciation on thermochronometer age‐elevation profiles","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Elevation (ballistics); Glacial period; Erosion; Physical geography; Zircon; Sea level; Geomorphology; Paleontology; Oceanography; Geography","score_opus":0.026755856485730867,"score_gpt":0.3189007668168423,"score_spread":0.29214491033111145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012303460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99743646,0.00010748868,0.00065592816,0.000053367432,0.0000037314057,0.0000046062523,0.0004772914,0.00012497335,0.0011361749],"genre_scores_gemma":[0.9982774,0.000056007408,0.000741937,0.000022398679,0.0000012765614,0.0000038790777,0.0006142228,0.000041793523,0.00024104126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995358,0.00016004569,0.00003344451,0.00009448416,0.000106991596,0.00006925931],"domain_scores_gemma":[0.99904627,0.00032247018,0.00016611283,0.00017666302,0.00021579086,0.00007269712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008907689,0.00045124718,0.00042053353,0.00048444438,0.0006052476,0.0011154154,0.0003543747,0.00037116723,0.0010723022],"category_scores_gemma":[0.0033793128,0.0003624603,0.0004990601,0.001071662,0.00035607503,0.00031130124,0.0005792094,0.00046735167,0.00026845394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011278575,0.00007179474,0.81136554,0.000055591117,0.00041702564,0.00016874366,0.00038278356,0.12104081,0.036929853,0.00036038816,0.0005392769,0.027540173],"study_design_scores_gemma":[0.000056344477,0.00008385437,0.9313072,0.0000150084325,0.00013944024,0.00009130056,0.00011124919,0.059006248,0.0076728417,0.000101751684,0.0013914832,0.000023351831],"about_ca_topic_score_codex":0.13817036,"about_ca_topic_score_gemma":0.18397482,"teacher_disagreement_score":0.13817036,"about_ca_system_score_codex":0.0013493771,"about_ca_system_score_gemma":0.00079408055,"threshold_uncertainty_score":0.27473223},"labels":[],"label_agreement":null},{"id":"W2012405885","doi":"10.1029/2006gl027981","title":"Geological and oceanographic perspectives on event bed formation during Hurricane Katrina","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Storm; Shore; Geology; Landfall; Tropical cyclone; Deposition (geology); Oceanography; Marine transgression; Hurricane katrina; Storm surge; Atlantic hurricane; Overwash; Geomorphology; Barrier island; Sediment; Natural disaster; Structural basin","score_opus":0.01892323086005573,"score_gpt":0.2657844701140394,"score_spread":0.24686123925398365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012405885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992926,0.0004392616,0.00007551318,0.000285432,0.000006658967,0.000002851882,0.00039822125,0.000005431595,0.0058607217],"genre_scores_gemma":[0.99871624,0.00045422037,0.00010942724,0.000020266727,0.000016314103,0.0000016991794,0.00025538934,0.0000024647838,0.00042409156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992156,0.000026109694,0.000008214276,0.000012357611,0.000011500591,0.000020315158],"domain_scores_gemma":[0.99948776,0.00010009593,0.00019895883,0.00002081517,0.00011166083,0.00008072866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002151758,0.0000865513,0.00006230379,0.002375912,0.0006515113,0.0009860134,0.00016413035,0.00016864279,0.0020908436],"category_scores_gemma":[0.0008475803,0.000153181,0.00006860777,0.0017841682,0.0007670091,0.0004278086,0.00057335454,0.00017417641,0.00014168251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089762485,0.000016161202,0.9799018,0.00004155017,0.000022282366,0.00046685225,0.0029259857,0.00060595083,0.0017382344,0.0014762324,0.00047077527,0.01224442],"study_design_scores_gemma":[9.4348775e-7,0.000006479301,0.9971028,0.000006439028,0.0000031410716,0.00006399886,0.0014325704,0.00008985368,0.00007316334,0.00006784731,0.0011502653,0.000002484162],"about_ca_topic_score_codex":0.06719969,"about_ca_topic_score_gemma":0.20719685,"teacher_disagreement_score":0.06719969,"about_ca_system_score_codex":0.001245657,"about_ca_system_score_gemma":0.00041601993,"threshold_uncertainty_score":0.1336171},"labels":[],"label_agreement":null},{"id":"W2012578583","doi":"10.1002/2014gl060059","title":"Effects of particle mixtures and nozzle geometry on entrainment into volcanic jets","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Particle Dynamics in Fluid Flows","field":"Engineering","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Entrainment (biomusicology); Plume; Geology; Mechanics; Turbulence; Eddy; Volcano; Inflow; Jet (fluid); Explosive eruption; Particle (ecology); Atmospheric sciences; Geometry; Pyroclastic rock; Meteorology; Physics; Seismology","score_opus":0.00977561340627868,"score_gpt":0.26812340035766535,"score_spread":0.25834778695138666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012578583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931496,0.0012166735,0.0023445524,0.00014190706,0.000077452256,0.00001763069,0.000083566985,0.00009753548,0.0028711595],"genre_scores_gemma":[0.9978802,0.00033856955,0.00035116536,0.000035717312,0.000025032388,0.000004048925,0.000043553842,0.00004418444,0.001277608],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996902,0.000051351577,0.000020824114,0.000085868385,0.00007867878,0.00007309307],"domain_scores_gemma":[0.99912626,0.0005319284,0.00012788124,0.00003514454,0.0000946124,0.000084165025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005511945,0.0003599754,0.000718524,0.00025219395,0.00049549295,0.0016326607,0.00037319478,0.00064849126,0.005239604],"category_scores_gemma":[0.0020496568,0.00035964543,0.00031103753,0.00016855742,0.00046188006,0.0009613896,0.00069778174,0.000566896,0.00060599775],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002131765,0.00013288413,0.002910718,0.00018091589,0.000052228494,0.0003609362,0.00012063048,0.013420675,0.9699795,0.00042305645,0.00022996192,0.0100566065],"study_design_scores_gemma":[0.00008000116,0.0006335014,0.013251647,0.00001692161,0.000082154285,0.00013908953,0.00013798727,0.024959533,0.9594814,0.00022161614,0.00096275756,0.000033442953],"about_ca_topic_score_codex":0.00081773795,"about_ca_topic_score_gemma":0.0006947069,"teacher_disagreement_score":0.005239604,"about_ca_system_score_codex":0.0004041762,"about_ca_system_score_gemma":0.00021606332,"threshold_uncertainty_score":0.017528236},"labels":[],"label_agreement":null},{"id":"W2012622165","doi":"10.1029/2008gl034415","title":"Characterizing an “uncharacteristic” ETS event in northern Cascadia","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Geology; Seismology; Episodic tremor and slip; Borehole; Slip (aerodynamics); Paleontology; Tectonics","score_opus":0.05274247804368247,"score_gpt":0.29322576233397835,"score_spread":0.24048328429029586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012622165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993967,0.000010140031,0.000093641305,0.0000160045,8.105594e-7,0.0000021644807,0.00009298109,0.000007399633,0.0003801192],"genre_scores_gemma":[0.9996176,0.000016122438,0.000062614265,0.0000027692363,0.00000150318,0.0000018695821,0.00019395986,0.0000017357721,0.00010175178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998745,0.00001488203,0.000015334095,0.00004617615,0.000025922685,0.000023169896],"domain_scores_gemma":[0.99959177,0.000052389416,0.00010753003,0.00005849011,0.000074468466,0.000115374656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020222351,0.00023642124,0.00022277738,0.0007109955,0.00059480837,0.00034182874,0.0003319533,0.00030426498,0.00066215196],"category_scores_gemma":[0.0007724378,0.00018692295,0.00029808065,0.00068477175,0.00059502356,0.00027860916,0.0005081098,0.000191666,0.00010577052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015822731,0.00004530816,0.9675878,0.000038339535,0.00005813867,0.0012363401,0.0010017178,0.010535965,0.013906521,0.00022251937,0.00021883378,0.0049902285],"study_design_scores_gemma":[0.000003731274,0.000017179189,0.99659306,0.0000017498005,0.000010525108,0.00007799821,0.00020040375,0.002627486,0.00024857136,0.000053971387,0.00015997935,0.0000053037766],"about_ca_topic_score_codex":0.084529154,"about_ca_topic_score_gemma":0.17425437,"teacher_disagreement_score":0.084529154,"about_ca_system_score_codex":0.0011807171,"about_ca_system_score_gemma":0.00053626567,"threshold_uncertainty_score":0.16807431},"labels":[],"label_agreement":null},{"id":"W2012695634","doi":"10.1029/2005gl025612","title":"Kinetic aspects of foreshock cavities","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Foreshock; Physics; Geophysics; Bow shock (aerodynamics); Interplanetary magnetic field; Solar wind; Shock (circulatory); Kinetic energy; Interplanetary spaceflight; Magnetosphere; Magnetic field; Computational physics; Shock wave; Mechanics; Geology; Seismology; Classical mechanics; Aftershock","score_opus":0.011925323333958215,"score_gpt":0.26661991374046384,"score_spread":0.2546945904065056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2012695634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950335,0.00025163146,0.0026111314,0.000020911484,0.0000068646095,0.000005910602,0.00006542811,0.000037934045,0.001966711],"genre_scores_gemma":[0.99898857,0.000057374516,0.00058661535,0.0000041163394,0.0000033664257,0.0000019691565,0.00004786511,0.000006527188,0.00030360033],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999131,0.000007255097,0.0000019780384,0.000017244047,0.000016561597,0.000043769698],"domain_scores_gemma":[0.9996673,0.00008214047,0.000104380255,0.000046261597,0.000048885388,0.000051104278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013265367,0.0001522351,0.00011805488,0.00023705912,0.00033768005,0.00041641272,0.00020161552,0.0001747665,0.0010534885],"category_scores_gemma":[0.00047655654,0.00014817463,0.000120015335,0.000110551184,0.00037656463,0.00046038773,0.0003416204,0.00025826658,0.00012678115],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008719698,0.000042424457,0.05331479,0.00014929892,0.000030155601,0.0018242549,0.0011073194,0.019390127,0.8948139,0.008543911,0.00035118972,0.019560706],"study_design_scores_gemma":[0.0000907271,0.00076845475,0.39549473,0.000098851815,0.00009466625,0.004402545,0.002483901,0.065535404,0.5026115,0.008368174,0.019870488,0.00018062434],"about_ca_topic_score_codex":0.00089462975,"about_ca_topic_score_gemma":0.0008829121,"teacher_disagreement_score":0.0010534885,"about_ca_system_score_codex":0.00012468023,"about_ca_system_score_gemma":0.00011253299,"threshold_uncertainty_score":0.0035242438},"labels":[],"label_agreement":null},{"id":"W2013135688","doi":"10.1029/2004gl019552","title":"MLT cooling during stratospheric warming events","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Airglow; Thermosphere; Atmospheric sciences; Environmental science; Zonal and meridional; Climatology; Latitude; GCM transcription factors; Bay; High latitude; Stratosphere; Mesosphere; General Circulation Model; Climate change; Ionosphere; Geology; Oceanography","score_opus":0.015303618479180063,"score_gpt":0.28429750133365495,"score_spread":0.2689938828544749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013135688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99856526,0.000038509716,0.00006211322,0.000023758228,0.0000044582184,0.000004885527,0.0003863827,0.000019774012,0.00089493085],"genre_scores_gemma":[0.998928,0.000019695395,0.000031984913,0.000016220623,0.00001056608,0.0000048893394,0.0007486491,0.000004856493,0.00023515685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000047611843,0.0000025572378,0.000016097603,0.000010647479,0.000024810965],"domain_scores_gemma":[0.9998442,0.00002261604,0.00004536308,0.000015582797,0.000037619295,0.00003445444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011233432,0.00013453042,0.00018109457,0.00031435583,0.00029046615,0.0002807739,0.000102148086,0.00022776994,0.0014566628],"category_scores_gemma":[0.00042885184,0.00007251415,0.00012672786,0.00022712175,0.0001339102,0.00020276818,0.00031444844,0.0002521485,0.00020832875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026697891,0.00014532171,0.78699255,0.00012730437,0.00014874224,0.0007535594,0.0013336799,0.0027126898,0.16884099,0.00035198542,0.0040663383,0.03185702],"study_design_scores_gemma":[0.0000051834627,0.000037333855,0.9972078,0.0000026878297,0.000006054311,0.000041159612,0.00006152882,0.00028854085,0.0017882563,0.00001675449,0.0005424982,0.0000020516807],"about_ca_topic_score_codex":0.006876961,"about_ca_topic_score_gemma":0.009870674,"teacher_disagreement_score":0.006876961,"about_ca_system_score_codex":0.0003037184,"about_ca_system_score_gemma":0.00011574736,"threshold_uncertainty_score":0.013673902},"labels":[],"label_agreement":null},{"id":"W2013234742","doi":"10.1029/2005gl024768","title":"Variability of Nares Strait ice flux","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Arctic ice pack; Geology; Sea ice thickness; Antarctic sea ice; Flux (metallurgy); Drift ice; Oceanography; Climatology; Fast ice; Context (archaeology); Atmospheric sciences","score_opus":0.02435554438001724,"score_gpt":0.28169531966840916,"score_spread":0.2573397752883919,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013234742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902818,0.00014954932,0.0001865943,0.00006361018,0.000011334308,0.000006113455,0.0049208896,0.000023533566,0.0043565496],"genre_scores_gemma":[0.98053783,0.00025729966,0.00046297756,0.00003808048,0.000012157285,0.000019713621,0.014759796,0.000017276976,0.0038949826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983096,0.000012844859,0.000017279885,0.00006399429,0.00004814299,0.000026743859],"domain_scores_gemma":[0.9994697,0.000041751755,0.00012346322,0.00004836715,0.0002710579,0.000045702353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039157431,0.00020805997,0.00021890414,0.0009875566,0.00028315998,0.00046386558,0.00016661195,0.00013335311,0.00073939364],"category_scores_gemma":[0.000780134,0.00009534479,0.00021704036,0.00056365924,0.00013093337,0.00032128458,0.00038915788,0.00018786297,0.00029336082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000162692,0.00003083757,0.97387266,0.000051205272,0.00015814869,0.00016998767,0.0009230298,0.0020170754,0.005420487,0.00044017608,0.0019690176,0.014784731],"study_design_scores_gemma":[0.000001895453,0.000007895024,0.9949881,0.000007830239,0.000008869862,0.000033419423,0.00009460942,0.0005661757,0.00041258527,0.00001693748,0.003856672,0.000005022448],"about_ca_topic_score_codex":0.14906257,"about_ca_topic_score_gemma":0.3120519,"teacher_disagreement_score":0.14906257,"about_ca_system_score_codex":0.0011275203,"about_ca_system_score_gemma":0.00043012903,"threshold_uncertainty_score":0.29638988},"labels":[],"label_agreement":null},{"id":"W2013238982","doi":"10.1029/2008gl036675","title":"Confirmation of quasi‐perpendicular shock reformation in two‐dimensional hybrid simulations","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Natural Resources Canada","funders":"","keywords":"Whistler; Physics; Shock (circulatory); Amplitude; Perpendicular; Bow shock (aerodynamics); Shock wave; Geophysics; Plasma; Mechanics; Nuclear physics; Optics; Geometry","score_opus":0.014546718903862492,"score_gpt":0.3089501664639031,"score_spread":0.2944034475600406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013238982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98921543,0.00004716854,0.005223747,0.00014756141,0.000027935432,0.000033525397,0.00032247408,0.00023104147,0.0047511933],"genre_scores_gemma":[0.9961733,0.000027316626,0.0030481007,0.000043792443,0.000008244869,0.000042970165,0.00023546441,0.000037440877,0.0003834209],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981004,0.00003299662,0.000013462569,0.000030215679,0.000047740195,0.00006556719],"domain_scores_gemma":[0.99925107,0.00031922583,0.00009914756,0.00009662984,0.00010552421,0.00012841653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034411444,0.00052346126,0.0006310537,0.0004547195,0.0005004675,0.0011108133,0.0008306666,0.0010218472,0.0023063526],"category_scores_gemma":[0.0016714146,0.00032502343,0.0005625144,0.00035218807,0.0006884561,0.0005884879,0.00084319775,0.0008315084,0.00014232812],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031675314,0.00025545649,0.014653861,0.0000725151,0.00012571651,0.00035036693,0.00025803893,0.96640766,0.009607753,0.004656372,0.0006411925,0.0026542887],"study_design_scores_gemma":[0.00004382294,0.00005626934,0.002062941,0.0000033949384,0.0000064354726,0.000018207678,0.000038971837,0.996406,0.0008377766,0.00037467113,0.00014207992,0.000009387395],"about_ca_topic_score_codex":0.008387827,"about_ca_topic_score_gemma":0.0048850463,"teacher_disagreement_score":0.008387827,"about_ca_system_score_codex":0.0005366773,"about_ca_system_score_gemma":0.0006460478,"threshold_uncertainty_score":0.016678035},"labels":[],"label_agreement":null},{"id":"W2013318732","doi":"10.1029/2008gl034289","title":"Stratospheric winter climate response to ENSO in three chemistry‐climate models","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"El Niño Southern Oscillation; Climatology; Environmental science; Atmospheric sciences; Climate model; Climate change; Multivariate ENSO index; Atmospheric chemistry; Meteorology; Southern oscillation; Geology; Oceanography; Ozone; Geography","score_opus":0.04129301785977881,"score_gpt":0.28078218702036895,"score_spread":0.23948916916059013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013318732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99530184,0.000107605454,0.0012829915,0.00023298991,0.000027815004,0.000029458513,0.0007633776,0.00013570431,0.0021182608],"genre_scores_gemma":[0.99780625,0.00008411229,0.0009812223,0.00006059045,0.000012413592,0.000039483624,0.000679773,0.000025252559,0.00031093945],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997924,0.00007105562,0.00001382079,0.000040897237,0.000026027816,0.000055823602],"domain_scores_gemma":[0.9991841,0.0003319818,0.00010926216,0.00007198952,0.000117071715,0.00018562366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007010751,0.00090582535,0.00060594635,0.00038377315,0.00070375984,0.0011289674,0.001029517,0.0012861817,0.0009428913],"category_scores_gemma":[0.0017801455,0.0004997072,0.0010931294,0.00042877274,0.0005716553,0.0006400214,0.00067649106,0.0008391744,0.00012624601],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004220894,0.00013426182,0.02029024,0.00003310734,0.00022374165,0.000070724156,0.00007100326,0.9732405,0.002403265,0.00087458827,0.00043379405,0.0018026261],"study_design_scores_gemma":[0.00035489324,0.00020785467,0.0143778045,0.000007791216,0.000117976815,0.000022831688,0.00004982331,0.98231,0.0013326347,0.0006440241,0.00053206424,0.000042339976],"about_ca_topic_score_codex":0.052474845,"about_ca_topic_score_gemma":0.024861794,"teacher_disagreement_score":0.052474845,"about_ca_system_score_codex":0.0016514803,"about_ca_system_score_gemma":0.0009102716,"threshold_uncertainty_score":0.104338825},"labels":[],"label_agreement":null},{"id":"W2013328420","doi":"10.1029/2006gl027734","title":"Autonomous underwater vehicle (AUV) mapping reveals coral mound distribution, morphology, and oceanography in deep water of the Straits of Florida","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":164,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Quest University Canada","funders":"","keywords":"Bathymetry; Seafloor spreading; Geology; Oceanography; Coral; Underwater; Current (fluid)","score_opus":0.01673608237886045,"score_gpt":0.24109130247515329,"score_spread":0.22435522009629283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013328420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990995,0.000054928114,0.00021898409,0.000020765261,6.421104e-7,0.0000019806291,0.000093443356,0.000008475571,0.0005013602],"genre_scores_gemma":[0.9987379,0.00005559093,0.00082436384,0.0000123045265,0.0000011042478,0.000002813172,0.00013222912,0.0000018741196,0.00023185012],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999641,0.0000053527965,0.0000011561979,0.000008854362,0.000010134368,0.0000103769935],"domain_scores_gemma":[0.9999167,0.000014362076,0.000022000177,0.000005988118,0.000022593964,0.000018248635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006862328,0.000095220676,0.000073691626,0.0005499004,0.00026543898,0.0001754979,0.00010366682,0.00013015005,0.00039086852],"category_scores_gemma":[0.00024979704,0.0000868159,0.00004928352,0.0003006949,0.0001476169,0.00021988942,0.00025303088,0.00009283982,0.00005408443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007509328,0.000042651725,0.86569786,0.000045992118,0.000033252032,0.00021075743,0.0011113569,0.0008161816,0.06443343,0.00017253438,0.0007951304,0.06656576],"study_design_scores_gemma":[0.0000021677704,0.000037684036,0.99629956,0.0000052290693,0.000007195232,0.0001253619,0.00052293943,0.0013520448,0.00090973655,0.00004263142,0.00069087464,0.0000045443594],"about_ca_topic_score_codex":0.060568202,"about_ca_topic_score_gemma":0.15594654,"teacher_disagreement_score":0.060568202,"about_ca_system_score_codex":0.00021636739,"about_ca_system_score_gemma":0.00018605395,"threshold_uncertainty_score":0.12043136},"labels":[],"label_agreement":null},{"id":"W2013356945","doi":"10.1002/2014gl061112","title":"Cloud partitioning of isocyanic acid (HNCO) and evidence of secondary source of HNCO in ambient air","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Environment and Climate Change Canada; University of Toronto","funders":"University of Toronto; California Institute of Technology","keywords":"Isocyanic acid; Environmental science; Chemistry; Physics; Astrobiology; Organic chemistry","score_opus":0.02671764276783253,"score_gpt":0.2742483639849893,"score_spread":0.24753072121715677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013356945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99810165,0.000071324495,0.00035624907,0.000026396385,0.000007988334,0.000021883934,0.00021907833,0.000011792196,0.0011837357],"genre_scores_gemma":[0.9990533,0.00004574029,0.00035435052,0.000031300246,0.000009198298,0.0000075508883,0.00017864669,0.0000036788929,0.00031626906],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99985254,0.000010384309,0.0000038343205,0.000043402186,0.000059721504,0.000030176876],"domain_scores_gemma":[0.9998149,0.000023493092,0.000026948634,0.000010176609,0.00009135421,0.000033192082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013861709,0.00022039801,0.00018940239,0.00047015146,0.0006760806,0.00036016112,0.0002615938,0.00033110625,0.0011535436],"category_scores_gemma":[0.00013405035,0.000099769975,0.00012448053,0.00020969305,0.00035307166,0.00022114548,0.0001961877,0.0002855386,0.00016958595],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072845514,0.0002687715,0.16214162,0.000060583345,0.00003441456,0.00035059842,0.00013757909,0.00035309873,0.83051854,0.0001582739,0.0004381193,0.004809785],"study_design_scores_gemma":[0.00006940088,0.00064704445,0.7420748,0.000013000404,0.000026546331,0.0002275713,0.000395031,0.0043037883,0.2507641,0.00016071364,0.0013026027,0.000015321932],"about_ca_topic_score_codex":0.051995914,"about_ca_topic_score_gemma":0.040678874,"teacher_disagreement_score":0.051995914,"about_ca_system_score_codex":0.0006092187,"about_ca_system_score_gemma":0.00041125354,"threshold_uncertainty_score":0.10338652},"labels":[],"label_agreement":null},{"id":"W2013693023","doi":"10.1029/2006gl026090","title":"Timescale dependency of spatial patterns in the variability of the Northern Hemisphere winter SLP field","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of East Anglia; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Northern Hemisphere; North Atlantic oscillation; Arctic oscillation; Climatology; Arctic; Spatial variability; Common spatial pattern; Pacific decadal oscillation; Spatial ecology; Geology; Southern Hemisphere; Oceanography; Sea surface temperature","score_opus":0.016487700196557018,"score_gpt":0.2690846035299723,"score_spread":0.2525969033334153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013693023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99688417,0.00007623828,0.0010787785,0.000049678834,0.000004845595,0.0000032635949,0.00020417117,0.000020177431,0.0016785407],"genre_scores_gemma":[0.99943775,0.000040518873,0.00017762203,0.0000059925433,0.0000045222314,0.000002488218,0.00015719446,0.0000041137864,0.00016979294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995196,0.0000074360964,0.0000042750275,0.000016880607,0.000008525104,0.0000108891845],"domain_scores_gemma":[0.9994073,0.0002359935,0.0001512193,0.00005608219,0.0000995505,0.000049832415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021781631,0.00007459043,0.00008409029,0.0004900939,0.00010369984,0.00028586932,0.00006881837,0.00013231662,0.0010509443],"category_scores_gemma":[0.0015073034,0.00010558602,0.00012476015,0.00032183915,0.00017957317,0.00018435394,0.00017920576,0.00015137586,0.00012921407],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005197687,0.00006597495,0.8076979,0.000112306814,0.00019750484,0.000446342,0.00097568135,0.02251816,0.10169122,0.002970429,0.0014467888,0.061357953],"study_design_scores_gemma":[0.000005100629,0.000017949505,0.98964,0.0000042038773,0.000010364271,0.00006904775,0.00008962009,0.008803341,0.00078797835,0.0003161735,0.00025082135,0.000005383106],"about_ca_topic_score_codex":0.003527256,"about_ca_topic_score_gemma":0.0027819553,"teacher_disagreement_score":0.003527256,"about_ca_system_score_codex":0.00014142822,"about_ca_system_score_gemma":0.00010162053,"threshold_uncertainty_score":0.00701344},"labels":[],"label_agreement":null},{"id":"W2013737680","doi":"10.1029/2005gl025065","title":"Satellite observation of chlorophyll and nutrients increase induced by Typhoon Megi in the Japan/East Sea","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Canadian Space Agency; Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Typhoon; Environmental science; Upwelling; Chlorophyll a; Nutrient; Sea surface temperature; Phytoplankton; Oceanography; Satellite; Climatology; Geology; Chemistry","score_opus":0.035108016556386554,"score_gpt":0.26597368431783136,"score_spread":0.2308656677614448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013737680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978167,0.000017312765,0.000023424347,0.000011701327,0.0000019442027,0.0000015158166,0.00006703643,0.000002591772,0.00009290016],"genre_scores_gemma":[0.99947065,0.000038081915,0.00009198049,0.00002422754,0.00000530525,0.000005143113,0.00027539604,0.0000015640499,0.0000876512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995625,0.000006022397,0.0000035233882,0.00001037428,0.000009643212,0.000014155705],"domain_scores_gemma":[0.9997658,0.00002300055,0.00009648187,0.000013300126,0.000039467486,0.000061853956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013634645,0.00016150236,0.00017668246,0.0002798324,0.00016106975,0.00016562434,0.00008471315,0.00019687766,0.00030140037],"category_scores_gemma":[0.00023350668,0.00013839507,0.00015089913,0.00029239664,0.00022950539,0.00013431188,0.00023925169,0.0002388772,0.00005892482],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00079574174,0.00009781841,0.84345025,0.000074076874,0.0001452093,0.0005281345,0.00059468794,0.0010232327,0.14714062,0.000058156245,0.00048373913,0.005608308],"study_design_scores_gemma":[0.000007502312,0.00004288153,0.99868435,0.0000012868072,0.000010489887,0.000024180674,0.00008408769,0.00025740993,0.000795998,0.000007223799,0.000082617385,0.0000019722813],"about_ca_topic_score_codex":0.007883738,"about_ca_topic_score_gemma":0.01583285,"teacher_disagreement_score":0.007883738,"about_ca_system_score_codex":0.00030225358,"about_ca_system_score_gemma":0.0001737864,"threshold_uncertainty_score":0.015675664},"labels":[],"label_agreement":null},{"id":"W2013798846","doi":"10.1029/2007gl031958","title":"Solar modulation of the Northern Hemisphere winter trends and its implications with increasing CO<sub>2</sub>","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of Toronto","funders":"Japan Society for the Promotion of Science; Ministerio de Educación, Cultura y Deporte; National Oceanic and Atmospheric Administration; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Troposphere; Polar vortex; Northern Hemisphere; Climatology; Arctic oscillation; Atmospheric sciences; Environmental science; North Atlantic oscillation; Stratosphere; Atmosphere (unit); Sudden stratospheric warming; Polar; Arctic; Southern Hemisphere; Geology; Oceanography; Meteorology; Geography; Physics","score_opus":0.014992563004828454,"score_gpt":0.24346788533528885,"score_spread":0.2284753223304604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2013798846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970822,0.00019771597,0.00026726924,0.0000751091,0.0000064854166,0.000002648092,0.0002241187,0.00001964,0.002124812],"genre_scores_gemma":[0.9995407,0.00007611424,0.000078237106,0.000007342897,0.0000067735727,0.0000012779124,0.00008840351,0.000003837108,0.00019732781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997985,0.0000051304746,0.000001443222,0.000004535571,0.0000037556338,0.000005277466],"domain_scores_gemma":[0.9998417,0.000048087062,0.000060265418,0.000011999877,0.000023477727,0.00001437817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010497563,0.00009743896,0.00007074376,0.00021046243,0.000082609105,0.00028298568,0.000066694,0.000106633765,0.0012855362],"category_scores_gemma":[0.00041554729,0.000062207975,0.00012929356,0.00035113737,0.00012658401,0.0001311683,0.00010745936,0.00008485998,0.00012668593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039481642,0.000041555166,0.9154497,0.00007327473,0.00011489823,0.00028280317,0.00019710843,0.011744352,0.045861345,0.0010156443,0.00075481925,0.02406974],"study_design_scores_gemma":[0.0000051135926,0.00003190362,0.99201435,0.0000029610055,0.000019520285,0.000054442455,0.00004349647,0.0057743667,0.0013824567,0.00015549065,0.0005124866,0.0000033459728],"about_ca_topic_score_codex":0.0055633183,"about_ca_topic_score_gemma":0.0068870964,"teacher_disagreement_score":0.0055633183,"about_ca_system_score_codex":0.00018270967,"about_ca_system_score_gemma":0.00010488767,"threshold_uncertainty_score":0.011061847},"labels":[],"label_agreement":null},{"id":"W2014030031","doi":"10.1029/2008gl033469","title":"Magnetospheric quasi‐static response to the dynamic magnetosheath: A THEMIS case study","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Magnetosheath; Magnetopause; Magnetosphere; Physics; Geophysics; Dynamic pressure; Solar wind; Magnetohydrodynamics; Magnetic field; Magnetosphere of Saturn; Mechanics","score_opus":0.022825899461678307,"score_gpt":0.30821813002186776,"score_spread":0.2853922305601895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014030031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909383,0.0002010152,0.0011589997,0.00014986882,0.000010557332,0.000014059022,0.00026635293,0.00003674722,0.0072241696],"genre_scores_gemma":[0.9988802,0.00008238658,0.00029179567,0.000006085315,0.000011128989,0.000004741884,0.00010496803,0.0000037251077,0.00061506615],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998642,0.00003123574,0.0000055531764,0.000017689172,0.000023445591,0.000057740734],"domain_scores_gemma":[0.9996136,0.00018786523,0.00007026207,0.00004048884,0.000044824243,0.000042993204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029316146,0.00038274247,0.00028448322,0.00039759005,0.0007364363,0.0006736359,0.00042675855,0.0006297133,0.0009783729],"category_scores_gemma":[0.00076896645,0.00010932203,0.000377524,0.00079202384,0.0003838359,0.0003140467,0.00048019766,0.00023618064,0.00011046034],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023397517,0.000541352,0.38807964,0.0006436919,0.00045942853,0.028075252,0.0022473882,0.45911872,0.034695316,0.032412294,0.007788643,0.043598372],"study_design_scores_gemma":[0.00029023533,0.0015468018,0.39095062,0.00007465078,0.0004425149,0.008659754,0.006209045,0.5401014,0.02074281,0.008544873,0.022297325,0.0001399127],"about_ca_topic_score_codex":0.013917063,"about_ca_topic_score_gemma":0.010875344,"teacher_disagreement_score":0.013917063,"about_ca_system_score_codex":0.00060085877,"about_ca_system_score_gemma":0.00022016361,"threshold_uncertainty_score":0.027672112},"labels":[],"label_agreement":null},{"id":"W2014042014","doi":"10.1002/2015gl063306","title":"Causes and impacts of the 2014 warm anomaly in the NE Pacific","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1198,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Anomaly (physics); Advection; Sea surface temperature; Oceanography; Climatology; Boreal; Environmental science; Pacific decadal oscillation; Atmosphere (unit); Geology; Atmospheric sciences; Geography; Meteorology","score_opus":0.06099073454429709,"score_gpt":0.3189841471190794,"score_spread":0.2579934125747823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014042014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99697554,0.00020186682,0.00008903262,0.00044516224,0.00001959179,0.0000055047367,0.00036998736,0.000011886795,0.0018814846],"genre_scores_gemma":[0.9993729,0.00018808493,0.000048896254,0.000040405197,0.000018145665,0.0000025895733,0.00015265813,0.000002225694,0.00017423402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998716,0.000021862132,0.000011546073,0.000030377092,0.000026758698,0.00003782145],"domain_scores_gemma":[0.9995252,0.00004112532,0.0002574228,0.000026368843,0.000064867076,0.00008508753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002951833,0.00015150828,0.00014193794,0.0004875949,0.0005009682,0.0006017797,0.00022162845,0.0003688742,0.0008267428],"category_scores_gemma":[0.0006563941,0.00015369072,0.0003147433,0.0004326521,0.00056067685,0.0003172879,0.0007995714,0.00043802534,0.000058937076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006449337,0.00003316034,0.9898369,0.000030110508,0.00011011046,0.00039704406,0.00021551819,0.0015249081,0.0022054135,0.00043109048,0.00078361656,0.0043677306],"study_design_scores_gemma":[0.0000033580925,0.00001773286,0.99675995,0.0000114239665,0.000024274865,0.00009568337,0.000426417,0.0010075335,0.00037810317,0.00014864004,0.0011208903,0.0000059574527],"about_ca_topic_score_codex":0.057128865,"about_ca_topic_score_gemma":0.102025546,"teacher_disagreement_score":0.057128865,"about_ca_system_score_codex":0.0009678399,"about_ca_system_score_gemma":0.0007780783,"threshold_uncertainty_score":0.113592684},"labels":[],"label_agreement":null},{"id":"W2014329278","doi":"10.1029/2008gl034245","title":"Fracture propagation propensity in relation to snow slab avalanche release: Validating the Propagation Saw Test","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Snowpack; Snow; Slab; Fracture (geology); Fracture mechanics; Geology; Geotechnical engineering; Materials science; Composite material; Geophysics; Geomorphology","score_opus":0.060218092343297974,"score_gpt":0.28035562092389177,"score_spread":0.2201375285805938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014329278","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920913,0.000025045601,0.0067530777,0.000016784797,0.000007231868,0.000019540203,0.0005364979,0.000106094114,0.00044448426],"genre_scores_gemma":[0.9965431,0.00001540819,0.0025501207,0.0000066122393,0.0000045173765,0.000014506467,0.00074922235,0.000013641503,0.000102918704],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994599,0.00012589371,0.000050521347,0.00014204047,0.00015629848,0.00006528297],"domain_scores_gemma":[0.99092484,0.005724521,0.0012985514,0.00069660007,0.001042395,0.00031312223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020425636,0.0005053477,0.00026615948,0.0010730609,0.00027088227,0.0004573975,0.0006274819,0.00046699654,0.0009446528],"category_scores_gemma":[0.0085072955,0.00021975591,0.00054911664,0.00084908906,0.00049317844,0.0008992806,0.00057144667,0.0006161815,0.0002961883],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008078279,0.00033773162,0.88732076,0.00005863343,0.00016729128,0.0002559997,0.00017458429,0.0669467,0.016040461,0.00030883835,0.0005656647,0.027015543],"study_design_scores_gemma":[0.000044436667,0.0013068682,0.5187876,0.0000118113885,0.0000525054,0.000301446,0.00016075403,0.4583153,0.019776,0.0007625672,0.0004432876,0.000037383044],"about_ca_topic_score_codex":0.0062415726,"about_ca_topic_score_gemma":0.006367319,"teacher_disagreement_score":0.0062415726,"about_ca_system_score_codex":0.00033013133,"about_ca_system_score_gemma":0.00037326218,"threshold_uncertainty_score":0.012410462},"labels":[],"label_agreement":null},{"id":"W2014401730","doi":"10.1029/2002gl015757","title":"On the relationship between Dasuopu Snow Accumulation and the Asian Summer Monsoon","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Snow; Ice core; Climatology; Monsoon; Glacier; Hadley cell; East Asian Monsoon; Cryosphere; Proxy (statistics); Geology; Atmospheric circulation; Atmospheric sciences; Environmental science; Climate change; Sea ice; General Circulation Model; Oceanography; Geomorphology","score_opus":0.22310670428685814,"score_gpt":0.3647021329341353,"score_spread":0.14159542864727714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014401730","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998304,0.00012475596,0.00006856728,0.00017498285,0.0000035154671,0.0000013217708,0.000066150256,0.0000036975923,0.0012529365],"genre_scores_gemma":[0.999701,0.00009039722,0.000024866918,0.000010854625,0.000010815484,9.975779e-7,0.00004645313,0.0000010865308,0.00011355914],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998888,0.00004361288,0.0000069318107,0.000017757844,0.000015259404,0.00002761135],"domain_scores_gemma":[0.997285,0.0016157601,0.00060280063,0.00005853115,0.00017917313,0.0002587448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042012264,0.00014324635,0.00013987142,0.0005993596,0.0004333418,0.00088341994,0.00020627669,0.00027861845,0.0018568035],"category_scores_gemma":[0.0028263626,0.00014354414,0.0001167578,0.0011187131,0.00039387096,0.00037106447,0.0004678649,0.0003050184,0.00019305167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027468437,0.000045325105,0.987183,0.000023435909,0.00007417904,0.00043549566,0.00048800468,0.0015182892,0.0016809065,0.0010445095,0.00030199985,0.006930269],"study_design_scores_gemma":[0.0000071246996,0.00004832728,0.9943124,0.0000101191345,0.000033892353,0.00012509647,0.00044514536,0.003931987,0.00023063926,0.0004400138,0.0004087968,0.000006426779],"about_ca_topic_score_codex":0.009199177,"about_ca_topic_score_gemma":0.01274718,"teacher_disagreement_score":0.009199177,"about_ca_system_score_codex":0.00035696692,"about_ca_system_score_gemma":0.00034269816,"threshold_uncertainty_score":0.018291235},"labels":[],"label_agreement":null},{"id":"W2014539233","doi":"10.1029/2007gl029261","title":"Dry snow slab shear fracture speeds","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Snow; Slab; Geology; Shear (geology); Dissipation; Shear modulus; Geotechnical engineering; Shear velocity; Fracture mechanics; Mechanics; Geophysics; Materials science; Geomorphology; Composite material; Petrology; Physics","score_opus":0.016679517067158534,"score_gpt":0.2976814465164808,"score_spread":0.2810019294493223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014539233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9889684,0.00018294569,0.0067336443,0.000017253347,0.000007866846,0.000013121399,0.0012211258,0.00011103934,0.0027445639],"genre_scores_gemma":[0.99721766,0.000096351854,0.0015959922,0.000004673206,0.0000024138772,0.000007931619,0.00055513676,0.000012075258,0.00050786545],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991786,0.0000061433907,0.0000044809267,0.000024814904,0.000033008208,0.000013654584],"domain_scores_gemma":[0.9997974,0.00005787166,0.000048045054,0.000016312993,0.000059816648,0.000020559466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015569512,0.00027210324,0.00011616655,0.00066175323,0.00018624139,0.000293548,0.00023331908,0.00013401418,0.0028989192],"category_scores_gemma":[0.00061080797,0.00012415987,0.00015482861,0.00041363126,0.00023269105,0.00031367893,0.0002653426,0.00025448544,0.00038127953],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014073341,0.00010139465,0.3885227,0.00054489454,0.000275156,0.0003335712,0.0012200917,0.035891898,0.457254,0.0024388505,0.0015724327,0.11043773],"study_design_scores_gemma":[0.00003758822,0.0003084823,0.77483594,0.000048019014,0.000081436454,0.00046416608,0.000635073,0.029408257,0.18777236,0.0014463178,0.0049032234,0.000059177673],"about_ca_topic_score_codex":0.0046674525,"about_ca_topic_score_gemma":0.00710442,"teacher_disagreement_score":0.0046674525,"about_ca_system_score_codex":0.0003086466,"about_ca_system_score_gemma":0.00015762281,"threshold_uncertainty_score":0.009697914},"labels":[],"label_agreement":null},{"id":"W2014855181","doi":"10.1029/2004gl022082","title":"Impact of freshwater from the Canadian Arctic Archipelago on Labrador Sea Water formation","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"","keywords":"Oceanography; Archipelago; Arctic; Geology; The arctic; Water mass","score_opus":0.021721629952658774,"score_gpt":0.26395827926061605,"score_spread":0.24223664930795727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014855181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932273,0.00014479151,0.00019008163,0.0003380531,0.000020776408,0.000007837238,0.0007071444,0.00006312155,0.005301009],"genre_scores_gemma":[0.99784434,0.00021187915,0.0001670531,0.000077443394,0.000004338635,0.0000068841523,0.0005457755,0.000023863038,0.0011183977],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999742,0.00003679623,0.000012248911,0.0000403021,0.00004508407,0.00012354185],"domain_scores_gemma":[0.99957556,0.000073917916,0.000039753988,0.000025748304,0.00010836058,0.00017665044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002754151,0.0008025568,0.0006112372,0.000499975,0.0022572456,0.0023459676,0.00087617914,0.00085977383,0.0027582769],"category_scores_gemma":[0.0017017607,0.00043446315,0.0011567224,0.00070092146,0.00086823944,0.0007249401,0.0014241616,0.0007299943,0.00019417389],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010825384,0.00015379333,0.13399157,0.00011787808,0.0003874562,0.0008289438,0.00026167466,0.83702487,0.010890621,0.0039744307,0.0024374623,0.008848853],"study_design_scores_gemma":[0.0007406006,0.00063925155,0.37006506,0.000104955885,0.0008049385,0.00031435414,0.0021384892,0.6023043,0.008373237,0.0018791301,0.012304706,0.00033098657],"about_ca_topic_score_codex":0.90583205,"about_ca_topic_score_gemma":0.87418085,"teacher_disagreement_score":0.09416795,"about_ca_system_score_codex":0.0154530015,"about_ca_system_score_gemma":0.012262885,"threshold_uncertainty_score":0.18944502},"labels":[],"label_agreement":null},{"id":"W2014933081","doi":"10.1029/2005gl025145","title":"Crustal velocity structure across the southern Korean Peninsula from seismic refraction survey","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Geology; Crust; Peninsula; Seismology; Transect; Seismic refraction; Discontinuity (linguistics); Basin and Range Province; Mantle (geology); Cretaceous; Geophysics; Paleontology; Tectonics","score_opus":0.02485958721636855,"score_gpt":0.28145761248997825,"score_spread":0.2565980252736097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2014933081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997661,0.00006579781,0.00009104099,0.000013785817,0.0000011667117,0.000004816587,0.0016108532,0.0000088739325,0.0005426596],"genre_scores_gemma":[0.9958072,0.00009813824,0.00033173978,0.0000052100227,0.0000011761986,0.000005531567,0.0034653565,0.00000321543,0.00028251996],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999398,0.0000054980155,0.000009479827,0.00001973792,0.000014205686,0.000011258959],"domain_scores_gemma":[0.99970657,0.000015388385,0.0000840637,0.00002609039,0.00012316751,0.000044698507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001867067,0.00034590915,0.00013482771,0.0013188457,0.00020198378,0.000310865,0.00020168396,0.000110728535,0.00093286566],"category_scores_gemma":[0.00031956076,0.00019789152,0.00019355191,0.0012846262,0.000091269954,0.00026790623,0.0003856338,0.00013609666,0.00019046181],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077668825,0.000020560687,0.97919476,0.000034183162,0.00007964372,0.00029664044,0.00048266895,0.0013236826,0.0053960015,0.0000991479,0.00051398465,0.012481148],"study_design_scores_gemma":[0.0000030515196,0.000010372717,0.99809664,0.0000062742106,0.000017211509,0.00005786552,0.0002216886,0.00076884276,0.00027849025,0.000012649886,0.00052233506,0.0000046461078],"about_ca_topic_score_codex":0.07395444,"about_ca_topic_score_gemma":0.13804321,"teacher_disagreement_score":0.07395444,"about_ca_system_score_codex":0.0005538666,"about_ca_system_score_gemma":0.00040668223,"threshold_uncertainty_score":0.14704794},"labels":[],"label_agreement":null},{"id":"W2015117702","doi":"10.1029/2001gl014170","title":"Geotail observations of magnetospheric midtail during an extended period of strongly northward interplanetary magnetic field","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Magnetosphere; Physics; Interplanetary magnetic field; Geophysics; Earth's magnetic field; Solar wind; Interplanetary spaceflight; Plasma; Ionosphere; Substorm; Geomagnetic storm; Astrophysics; Magnetic field","score_opus":0.023764148120420076,"score_gpt":0.2600439169855737,"score_spread":0.23627976886515364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015117702","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964064,0.00006722882,0.00036174137,0.000036634345,0.000006514316,0.00000416576,0.00070151844,0.00006875651,0.002347058],"genre_scores_gemma":[0.9978461,0.00004172442,0.00046609118,0.000026655182,0.000009223951,0.0000036389747,0.001115147,0.000009208395,0.00048212428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999682,0.0000022953345,0.0000012101169,0.000009877294,0.000009691148,0.0000087726485],"domain_scores_gemma":[0.99984586,0.000018351915,0.00003765988,0.000022447912,0.00003683724,0.00003884441],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011022823,0.00012835262,0.00014013481,0.00022353398,0.00022369112,0.00019977923,0.00014316729,0.00031766592,0.0009027077],"category_scores_gemma":[0.000256224,0.00011647956,0.000099160956,0.00019540882,0.00012250333,0.00021382718,0.00031795073,0.00020484549,0.00027780255],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011018777,0.00008702104,0.5687204,0.00009521757,0.00007949764,0.0014471792,0.001095901,0.0011152299,0.4087559,0.00054569845,0.0024614707,0.0144945],"study_design_scores_gemma":[0.0000369716,0.00017639593,0.98664784,0.000008545644,0.000013547871,0.00044157167,0.00012442326,0.0013692252,0.007678947,0.00015261878,0.0033412955,0.0000085950105],"about_ca_topic_score_codex":0.0021389998,"about_ca_topic_score_gemma":0.005648287,"teacher_disagreement_score":0.0021389998,"about_ca_system_score_codex":0.00013877699,"about_ca_system_score_gemma":0.000075862285,"threshold_uncertainty_score":0.00425303},"labels":[],"label_agreement":null},{"id":"W2015128350","doi":"10.1029/2006gl026651","title":"Testing the silica leakage hypothesis with sedimentary opal records from the eastern equatorial Pacific over the last 150 kyrs","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; Woods Hole Oceanographic Institution","keywords":"Geology; Oceanography; Glacial period; Biogenic silica; Upwelling; Sedimentary rock; Southern Hemisphere; Diatom; Climatology; Paleontology","score_opus":0.04393521723640182,"score_gpt":0.2556871945388384,"score_spread":0.2117519773024366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015128350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969316,0.00002786253,0.00008044288,0.0000076224533,7.5759806e-7,0.0000013567287,0.000027271293,0.0000024253036,0.00015923014],"genre_scores_gemma":[0.9996985,0.000019574216,0.00011843237,0.000011296386,0.0000031771224,0.000002160197,0.00012109739,0.0000017290887,0.000023895254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99964285,0.00007710317,0.000039053495,0.000094898045,0.000054362532,0.00009170105],"domain_scores_gemma":[0.99858993,0.00035532762,0.0005287428,0.00015343232,0.00018729648,0.00018528344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011343866,0.00027910553,0.0002897998,0.00067132356,0.0004157628,0.0006950281,0.00031896663,0.0002949754,0.00034487783],"category_scores_gemma":[0.002540774,0.00034013446,0.00027489278,0.00051170524,0.00066894555,0.00066366384,0.0010180596,0.00029345087,0.00010249358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018495035,0.000025062483,0.98930746,0.000012186937,0.00009419353,0.00010444624,0.00019126385,0.00049621565,0.0075719585,0.00005397382,0.00001650938,0.0019417143],"study_design_scores_gemma":[0.000010848534,0.000054220996,0.99671507,0.0000044964695,0.000029903955,0.000057061025,0.00016642701,0.0017277052,0.0010567401,0.0000810587,0.00009176259,0.000004727059],"about_ca_topic_score_codex":0.006730648,"about_ca_topic_score_gemma":0.009328758,"teacher_disagreement_score":0.006730648,"about_ca_system_score_codex":0.0004578295,"about_ca_system_score_gemma":0.00031228518,"threshold_uncertainty_score":0.013382912},"labels":[],"label_agreement":null},{"id":"W2015144391","doi":"10.1029/2003gl018722","title":"Is there observational support for an El Niño‐like pattern of future global warming?","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Meteorological and Oceanographic Society","funders":"","keywords":"Paleoclimatology; Climatology; Radiative forcing; Forcing (mathematics); Greenhouse gas; Environmental science; Atmospheric sciences; Radiative transfer; Climate model; Observational study; Global warming; Climate change; Geology; Oceanography; Physics; Mathematics","score_opus":0.07461541394849759,"score_gpt":0.35115240888208227,"score_spread":0.2765369949335847,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015144391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7906761,0.011568861,0.013425491,0.11136848,0.0011416705,0.000039656352,0.010564987,0.00032107663,0.060893696],"genre_scores_gemma":[0.9858305,0.003474971,0.001534285,0.0057384265,0.00055365526,0.00001833506,0.0022003772,0.00002384663,0.0006257176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9993616,0.00016929736,0.000069649665,0.00024203777,0.00010532895,0.00005213425],"domain_scores_gemma":[0.9839522,0.00742646,0.004558467,0.0018691486,0.0017411086,0.0004524988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033346922,0.00020832795,0.00029462605,0.00055381045,0.00044031467,0.0012847908,0.00074646843,0.001216451,0.008277095],"category_scores_gemma":[0.017360406,0.00023035226,0.00035538338,0.0011051075,0.0021971716,0.0026689477,0.0008281845,0.0008342818,0.00093548425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006906984,0.00030669261,0.8900293,0.0010753404,0.0008678671,0.00027518583,0.0010650959,0.0030029276,0.003213043,0.026918007,0.012083457,0.060472302],"study_design_scores_gemma":[0.00010306061,0.0001287517,0.9035347,0.00027656252,0.00018334207,0.00032823996,0.002850273,0.0043771695,0.0008881373,0.049209863,0.038047865,0.00007198242],"about_ca_topic_score_codex":0.0066330675,"about_ca_topic_score_gemma":0.007822462,"teacher_disagreement_score":0.008277095,"about_ca_system_score_codex":0.0005404722,"about_ca_system_score_gemma":0.0005936926,"threshold_uncertainty_score":0.027689636},"labels":[],"label_agreement":null},{"id":"W2015255530","doi":"10.1029/2003gl016917","title":"Satellite based retrieval of aerosol optical thickness: The effect of sun and satellite geometry","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Nadir; Remote sensing; Satellite; Aerosol; Pixel; Multispectral image; AERONET; Scattering; Near-infrared spectroscopy; Optics; Environmental science; Physics; Meteorology; Geology; Astronomy","score_opus":0.013584302830715662,"score_gpt":0.2737179429944709,"score_spread":0.26013364016375523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015255530","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99127835,0.00027637396,0.006513723,0.000023060757,0.000016176398,0.000016585347,0.00064413616,0.00017942386,0.0010520992],"genre_scores_gemma":[0.9903617,0.00013348635,0.0084762145,0.00000863035,0.000004889214,0.000005916282,0.0006862439,0.000043420365,0.00027956697],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984133,0.00002708854,0.000009134098,0.000032479224,0.00007036714,0.000019586387],"domain_scores_gemma":[0.9997211,0.000092473,0.000043777112,0.00004018612,0.00008638548,0.000016036209],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002939375,0.00030159726,0.00036620794,0.00040992995,0.00016511582,0.0004835759,0.00027142465,0.00023861676,0.00055618904],"category_scores_gemma":[0.0010335594,0.00022986498,0.00033588367,0.00051643123,0.00013050708,0.0005058795,0.00020897432,0.00015624822,0.00019053556],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008063226,0.00021379608,0.24451801,0.00030127662,0.00061314943,0.00031756124,0.00013812825,0.28835335,0.35642102,0.00042797544,0.0010423675,0.10684707],"study_design_scores_gemma":[0.000087324115,0.0002210996,0.41226408,0.000023417435,0.00019011306,0.00047697156,0.000090595386,0.4489111,0.13611636,0.00023364197,0.0013241417,0.000061193365],"about_ca_topic_score_codex":0.011126271,"about_ca_topic_score_gemma":0.014258619,"teacher_disagreement_score":0.011126271,"about_ca_system_score_codex":0.00039380393,"about_ca_system_score_gemma":0.00032484595,"threshold_uncertainty_score":0.022123039},"labels":[],"label_agreement":null},{"id":"W2015302898","doi":"10.1029/2008gl033733","title":"Occurrence of weak, sub‐micron, tropospheric aerosol events at high Arctic latitudes","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; Environment and Climate Change Canada; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Fonds Québécois de la Recherche sur la Nature et les Technologies; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Aerosol; Lidar; Environmental science; Troposphere; Arctic; Climatology; Atmospheric sciences; Observatory; Remote sensing; The arctic; Latitude; Meteorology; Geology; Geography; Oceanography; Astronomy; Physics","score_opus":0.023146818904169215,"score_gpt":0.2700265299739376,"score_spread":0.2468797110697684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015302898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994659,0.000044439083,0.00004332677,0.00000670617,0.0000018375904,0.0000011056737,0.00009789096,0.0000023668192,0.0003365989],"genre_scores_gemma":[0.999542,0.000046610454,0.000095078154,0.0000053113495,0.0000035210687,9.765877e-7,0.00015878331,8.4417206e-7,0.00014683949],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.0000058596042,0.000004582977,0.000016232547,0.000019713125,0.000018737916],"domain_scores_gemma":[0.99973506,0.000043555596,0.000064642416,0.000016117847,0.000085065156,0.000055524353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001449131,0.0001082228,0.0001236773,0.0004256579,0.00044266577,0.0003840789,0.0001119485,0.00016376893,0.00026045722],"category_scores_gemma":[0.00033668932,0.00008728116,0.000072092604,0.0002694329,0.00019599398,0.0001364215,0.0001972198,0.0001327525,0.00006860319],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008628653,0.000018486087,0.9854553,0.000016857155,0.00002351593,0.00014734255,0.00031112292,0.00023845797,0.008348125,0.00003600115,0.00013510356,0.005183597],"study_design_scores_gemma":[8.503871e-7,0.000009948553,0.9990337,0.0000018170663,0.000005841485,0.000036274912,0.00010604193,0.00017439845,0.00046639878,0.0000046683367,0.00015863584,0.0000014979172],"about_ca_topic_score_codex":0.13043329,"about_ca_topic_score_gemma":0.28859395,"teacher_disagreement_score":0.13043329,"about_ca_system_score_codex":0.00038275594,"about_ca_system_score_gemma":0.00037721242,"threshold_uncertainty_score":0.25934815},"labels":[],"label_agreement":null},{"id":"W2015307847","doi":"10.1029/2009gl038385","title":"Recent changes in the Greenland–Scotland overflow‐derived water transport inferred from hydrographic observations in the southern Irminger Sea","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique; Russian Foundation for Basic Research","keywords":"Hydrography; Oceanography; Baroclinity; Boundary current; Geology; Water mass; Groenlandia; Climatology; Current (fluid); Ocean current; Ice sheet","score_opus":0.046716535323549066,"score_gpt":0.2599743713481024,"score_spread":0.21325783602455334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015307847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995347,0.000049151986,0.000017395796,0.00001972823,0.0000021389676,0.000001011767,0.00019483604,0.0000028234426,0.00017824442],"genre_scores_gemma":[0.99930084,0.000060887283,0.000060795664,0.00001659003,0.0000039249544,0.0000012696753,0.0004464991,0.0000012439177,0.00010801595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999348,0.0000070302776,0.000006790469,0.000017343313,0.00001408973,0.000020010633],"domain_scores_gemma":[0.99965036,0.000026826101,0.00017974134,0.000021842228,0.000067046996,0.000054122247],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029795675,0.0001936551,0.00012082037,0.0007174012,0.00015724153,0.00045257184,0.0001570951,0.00016298455,0.00040516918],"category_scores_gemma":[0.0008239069,0.00010407728,0.00014212375,0.0008464612,0.00029358687,0.00030581857,0.00035184136,0.00014221283,0.000077868805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009127902,0.000019261479,0.9859373,0.000023985798,0.00009801415,0.00017930326,0.0005273115,0.0006223415,0.003901921,0.000077966375,0.00032113152,0.008200134],"study_design_scores_gemma":[0.0000010767619,0.0000067777405,0.9995635,0.0000017427723,0.0000052389905,0.000009982005,0.00003873793,0.00010802261,0.00006151997,0.0000041040953,0.00019751681,0.0000017117488],"about_ca_topic_score_codex":0.10415994,"about_ca_topic_score_gemma":0.2307691,"teacher_disagreement_score":0.10415994,"about_ca_system_score_codex":0.0012628933,"about_ca_system_score_gemma":0.0004424774,"threshold_uncertainty_score":0.20710737},"labels":[],"label_agreement":null},{"id":"W2015312486","doi":"10.1029/1999gl012157","title":"Subevent structure of large earthquakes—A ground‐motion perspective","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Performance and Analysis","field":"Engineering","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Seismology; Geology; Slip (aerodynamics); Ground motion; Strong ground motion; Source model; Fault (geology); Geodesy; Physics; Computational physics","score_opus":0.016190929270570132,"score_gpt":0.2928943327437796,"score_spread":0.27670340347320943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015312486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9681217,0.0003427513,0.026436957,0.00022254555,0.0000147923965,0.000019377394,0.00027092043,0.00014473226,0.0044263094],"genre_scores_gemma":[0.99859816,0.00008454696,0.0009166255,0.000008112921,0.000008743111,0.000003432273,0.00009542365,0.000013410891,0.00027150454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992144,0.000016743157,0.000005014901,0.000018972665,0.000019067404,0.00001872464],"domain_scores_gemma":[0.9993267,0.0002836897,0.00015646826,0.000069448986,0.00006575285,0.00009801061],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025144604,0.00023548851,0.00025128547,0.00091738557,0.00020565788,0.0007471378,0.0003955373,0.00035006195,0.001756463],"category_scores_gemma":[0.0015123752,0.00016587706,0.00022776713,0.00049984205,0.0004059488,0.00086465024,0.0004324377,0.00035704143,0.0002191343],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026707046,0.00019886988,0.19335829,0.00009667339,0.00009034313,0.00085205055,0.00041218312,0.7059752,0.015487651,0.02860966,0.0009882377,0.053663794],"study_design_scores_gemma":[0.000021292068,0.00024801542,0.20126949,0.000018394776,0.00003559424,0.00020181325,0.0002140728,0.77643776,0.0024223435,0.017391445,0.0017136174,0.00002610217],"about_ca_topic_score_codex":0.0024199456,"about_ca_topic_score_gemma":0.0023427512,"teacher_disagreement_score":0.0024199456,"about_ca_system_score_codex":0.00030628018,"about_ca_system_score_gemma":0.00017028578,"threshold_uncertainty_score":0.005875945},"labels":[],"label_agreement":null},{"id":"W2015316283","doi":"10.1029/2005gl024066","title":"Oldest reliable terrestrial <sup>40</sup>Ar‐<sup>39</sup>Ar age from pyrite crystals at Isua west Greenland","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pyrite; Geology; Radiogenic nuclide; Geochemistry; Sedimentary rock; Metamorphic rock; Hadean; Banded iron formation; Volcanic rock; Archean; Crust; Isotopes of argon; Precambrian; Metasomatism; Mineral; Mineralogy; Volcano; Argon; Chemistry; Mantle (geology)","score_opus":0.03117615748618204,"score_gpt":0.2597748428704288,"score_spread":0.22859868538424674,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015316283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99621296,0.00016074188,0.00029569044,0.000014872226,0.0000031962063,0.000005696756,0.0004182824,0.00002307983,0.0028655147],"genre_scores_gemma":[0.9977168,0.000111505295,0.00080360565,0.000013971827,0.0000024229753,0.00000337821,0.00058234046,0.000015797254,0.0007502736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998871,0.0000068141603,0.0000085340525,0.000035666282,0.000033699696,0.000028138706],"domain_scores_gemma":[0.9997851,0.000018727338,0.000047778034,0.00003439896,0.00009373757,0.000020291745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019151383,0.00015350267,0.00018035446,0.00091452006,0.00044314665,0.00047107332,0.00027377962,0.00017118556,0.0006517097],"category_scores_gemma":[0.000228196,0.0001290252,0.000105359926,0.0006006025,0.00037710206,0.0002243907,0.00031264653,0.00013921967,0.0002874114],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028614054,0.000039497314,0.5742444,0.00010164594,0.00008087492,0.0008493205,0.0012363717,0.0005891852,0.37928954,0.0004900325,0.00037446606,0.04241863],"study_design_scores_gemma":[0.000004609187,0.000039898834,0.97255117,0.000010173916,0.00002871107,0.00021764224,0.00026604894,0.0003549087,0.023082219,0.000079513135,0.0033587602,0.0000062107083],"about_ca_topic_score_codex":0.029456908,"about_ca_topic_score_gemma":0.095419765,"teacher_disagreement_score":0.029456908,"about_ca_system_score_codex":0.00045633505,"about_ca_system_score_gemma":0.00041783665,"threshold_uncertainty_score":0.05857092},"labels":[],"label_agreement":null},{"id":"W2015434783","doi":"10.1029/2003gl019334","title":"Propagation of the “Great Salinity Anomaly” of the 1990s around the northern North Atlantic","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":206,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Geology; Subarctic climate; Oceanography; Advection; Trough (economics); Shetland; Anomaly (physics); Structural basin; Channel (broadcasting); Climatology; Subtropics; Paleontology; Fishery","score_opus":0.021968385482176115,"score_gpt":0.2435986007787798,"score_spread":0.22163021529660368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015434783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913345,0.00023284642,0.00031222543,0.00016487429,0.000019426612,0.00000949656,0.0030691558,0.00003895249,0.0048186574],"genre_scores_gemma":[0.99604034,0.0003591059,0.00032237987,0.000027604514,0.000011590217,0.000006533259,0.002595937,0.0000036224646,0.00063281984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994195,0.000005299659,0.000006395097,0.000017102973,0.000013973398,0.000015256562],"domain_scores_gemma":[0.9994281,0.000049005303,0.00030915262,0.000021421514,0.00013089461,0.00006134298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022563632,0.00013255695,0.000077357385,0.0007432027,0.00020610387,0.00036537123,0.00010188804,0.00015943112,0.00075502857],"category_scores_gemma":[0.0010782887,0.00006971144,0.0001376591,0.0008192718,0.00018286338,0.00020028636,0.0003468422,0.000188494,0.00010855643],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001593206,0.000028667875,0.95194954,0.00007119212,0.00009066584,0.00019959015,0.0008224497,0.0054084808,0.0029782,0.0012927084,0.0037173452,0.033281863],"study_design_scores_gemma":[0.000004375519,0.000016410597,0.9962484,0.000016227501,0.000009612982,0.00004104139,0.000076278644,0.001030169,0.00014274898,0.0000683232,0.0023427203,0.000003679384],"about_ca_topic_score_codex":0.21963216,"about_ca_topic_score_gemma":0.30669385,"teacher_disagreement_score":0.21963216,"about_ca_system_score_codex":0.0011881324,"about_ca_system_score_gemma":0.00079980533,"threshold_uncertainty_score":0.4367075},"labels":[],"label_agreement":null},{"id":"W2015626848","doi":"10.1029/2007gl030764","title":"Relationship between the <i>Q</i> factor and inherent optical properties: Relevance to ocean‐colour inversion algorithms","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Dalhousie University","funders":"Canadian Space Agency; Natural Environment Research Council; Sight Research UK","keywords":"Radiance; Zenith; Solar zenith angle; Remote sensing; Irradiance; Ocean color; Inversion (geology); Satellite; Environmental science; Upwelling; Algorithm; Geology; Physics; Optics; Computer science","score_opus":0.07874043487167527,"score_gpt":0.29217937098672336,"score_spread":0.2134389361150481,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2015626848","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06934808,0.0007789962,0.9265971,0.00035708252,0.00005621531,0.00003075604,0.000069400354,0.00046353665,0.0022987854],"genre_scores_gemma":[0.7145622,0.00079104427,0.28267747,0.00012940553,0.000110526285,0.000049507875,0.000118542914,0.0002950907,0.0012661802],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996176,0.00012961362,0.000029366089,0.00007609258,0.000118718825,0.000028646018],"domain_scores_gemma":[0.9937603,0.004576625,0.00039997138,0.00044224414,0.00074414886,0.00007668922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018207056,0.00045714766,0.00039283768,0.0004961338,0.00024045158,0.0010585181,0.0005314816,0.00077182625,0.0011152719],"category_scores_gemma":[0.017818436,0.00031678553,0.0002186336,0.00066369417,0.00083207234,0.0018561487,0.0006128346,0.0007521517,0.00042542283],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033541574,0.0001430875,0.034869518,0.0003002804,0.00018327874,0.00021033503,0.00022427554,0.43648636,0.06272383,0.06645759,0.004045741,0.39402035],"study_design_scores_gemma":[0.000027871181,0.000034693097,0.006454993,0.000021092254,0.000019521549,0.00016504306,0.000025349402,0.9518788,0.010232991,0.029909667,0.0011822873,0.000047647587],"about_ca_topic_score_codex":0.0023579774,"about_ca_topic_score_gemma":0.0016428839,"teacher_disagreement_score":0.0023579774,"about_ca_system_score_codex":0.0003905242,"about_ca_system_score_gemma":0.00043583807,"threshold_uncertainty_score":0.009628892},"labels":[],"label_agreement":null},{"id":"W2016102970","doi":"10.1029/2008gl034619","title":"CO<sub>2</sub> efflux from Amazonian headwater streams represents a significant fate for deep soil respiration","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":248,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"STREAMS; Amazonian; Soil water; Groundwater; Environmental science; Soil gas; Hydrology (agriculture); Dissolved organic carbon; Atmosphere (unit); Soil respiration; Environmental chemistry; Carbon dioxide; Surface water; Carbon cycle; Soil science; Geology; Ecology; Chemistry; Ecosystem; Amazon rainforest; Environmental engineering","score_opus":0.040307641442715966,"score_gpt":0.27443228980152534,"score_spread":0.23412464835880936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016102970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999331,0.000093058814,0.0001382354,0.000037379603,0.0000013425694,0.0000024913047,0.00011347663,0.0000055579485,0.00027752624],"genre_scores_gemma":[0.99936444,0.000090834736,0.00013652604,0.000017017479,0.0000033802444,0.000001907741,0.00014293555,0.0000041488956,0.00023886598],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999616,0.000003915701,0.0000030148942,0.000010719833,0.000008456229,0.000012256334],"domain_scores_gemma":[0.99992776,0.000011097693,0.000023467259,0.00000452608,0.000020955702,0.000012160149],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007094799,0.0001790435,0.00014391857,0.0001946169,0.00037459022,0.00055103295,0.0001343503,0.00014626927,0.0008801893],"category_scores_gemma":[0.00020626214,0.00012347272,0.00006298631,0.00024666803,0.00020499165,0.00036749756,0.00020654847,0.00019699127,0.000082774386],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044785748,0.000049980576,0.41875598,0.0001270036,0.000042339638,0.00039400483,0.00049595005,0.00046846003,0.5570858,0.0003151609,0.00023203848,0.02158531],"study_design_scores_gemma":[0.000025060222,0.00012146894,0.9323373,0.000011455234,0.000042444586,0.0002462094,0.0005440572,0.004451774,0.0599051,0.0003026473,0.0020007878,0.000011741681],"about_ca_topic_score_codex":0.026641693,"about_ca_topic_score_gemma":0.04282858,"teacher_disagreement_score":0.026641693,"about_ca_system_score_codex":0.0004932663,"about_ca_system_score_gemma":0.00028412812,"threshold_uncertainty_score":0.05297327},"labels":[],"label_agreement":null},{"id":"W2016257799","doi":"10.1029/2005gl022983","title":"Near‐Earth breakup triggered by the earthward traveling burst flow","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Breakup; Physics; Magnetic field; Convection; Geophysics; Plasma sheet; Plasma; Nonlinear system; Leading edge; Computational physics; Mechanics; Magnetosphere","score_opus":0.014377898717572331,"score_gpt":0.27055791224878173,"score_spread":0.2561800135312094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016257799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916372,0.000051756655,0.005092624,0.00007982295,0.000016516695,0.00001033677,0.00016102828,0.00012882458,0.0028219973],"genre_scores_gemma":[0.9989569,0.00002521438,0.00052365556,0.0000058321634,0.0000036129488,0.00000654175,0.00009141241,0.00000968229,0.0003771467],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999713,0.0000057323236,0.0000010834126,0.0000051474567,0.000005030273,0.000011800367],"domain_scores_gemma":[0.9998826,0.000050350853,0.000021291036,0.000008648108,0.0000128199445,0.000024196092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093926115,0.00027192326,0.00032742787,0.00022899981,0.00027741797,0.00040013154,0.00037561957,0.0003980569,0.0021538916],"category_scores_gemma":[0.00044248396,0.000132792,0.00029854223,0.00014284969,0.00032019996,0.00032243988,0.00028107924,0.00046366843,0.00012638862],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031215226,0.00008538302,0.012563317,0.000050694016,0.00005685029,0.00078017416,0.00012744487,0.96776205,0.009320452,0.0039624386,0.00078276475,0.0041962336],"study_design_scores_gemma":[0.000014493647,0.00003241138,0.002419577,0.0000016163272,0.000007958179,0.000029587458,0.000035600293,0.9960575,0.0007250197,0.00052097975,0.0001501375,0.000005068609],"about_ca_topic_score_codex":0.0065341615,"about_ca_topic_score_gemma":0.0024882264,"teacher_disagreement_score":0.0065341615,"about_ca_system_score_codex":0.0002933113,"about_ca_system_score_gemma":0.00021701635,"threshold_uncertainty_score":0.012992263},"labels":[],"label_agreement":null},{"id":"W2016334707","doi":"10.1002/2013gl058934","title":"Passive margin subduction and the dynamics of collisional orogenesis","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Subduction; Lithosphere; Continental margin; Passive margin; Mantle (geology); Continental crust; Geophysics; Crust; Seismology; Tectonics; Rift","score_opus":0.014499303382516794,"score_gpt":0.2368459952752611,"score_spread":0.2223466918927443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016334707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942064,0.000016240652,0.00022103355,0.000008244511,4.8118227e-7,9.5315715e-7,0.000013842503,0.0000041288713,0.00031448505],"genre_scores_gemma":[0.9998808,0.000012680562,0.00006006889,0.0000011330919,1.8758857e-7,6.2851177e-7,0.000011654518,0.0000012770275,0.00003141844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.000011952295,0.0000039178085,0.000012606525,0.0000054612215,0.0000138243695],"domain_scores_gemma":[0.99981767,0.00005383148,0.00006473887,0.000023975625,0.000012901616,0.00002700371],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001706969,0.00017985968,0.00014515303,0.0002850542,0.0001909666,0.00056068326,0.00023871576,0.0001701863,0.00071146485],"category_scores_gemma":[0.0010281883,0.00017513048,0.00015301778,0.00021218011,0.0005982045,0.00038662157,0.0005191002,0.00016308296,0.00006483584],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006594831,0.0001012881,0.47035298,0.00007154939,0.00013713364,0.0005171561,0.0005629282,0.43077618,0.07963137,0.0070470865,0.00013076203,0.010012057],"study_design_scores_gemma":[0.00011532841,0.00033366913,0.41445267,0.000029251056,0.0000946634,0.00022935838,0.00081566325,0.56639755,0.013196544,0.0033908046,0.0009033324,0.000041176514],"about_ca_topic_score_codex":0.0032910455,"about_ca_topic_score_gemma":0.002828184,"teacher_disagreement_score":0.0032910455,"about_ca_system_score_codex":0.00042262409,"about_ca_system_score_gemma":0.00017710633,"threshold_uncertainty_score":0.0065437555},"labels":[],"label_agreement":null},{"id":"W2016342684","doi":"10.1029/2000gl012410","title":"Dependence of multiple climate states on ocean mixing parameters","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Thermohaline circulation; Mixing (physics); Climatology; Ocean current; Geology; Lead (geology); Diffusion; Precipitation; Climate model; Atmosphere (unit); Circulation (fluid dynamics); North Atlantic Deep Water; Climate change; Atmospheric sciences; Environmental science; Oceanography; Meteorology; Mechanics; Physics; Thermodynamics","score_opus":0.04828721089257715,"score_gpt":0.3065999827100261,"score_spread":0.25831277181744894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016342684","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973859,0.00005385508,0.001788157,0.000053747794,0.0000015584671,0.0000026409432,0.000082659135,0.000031720727,0.00059969374],"genre_scores_gemma":[0.9997129,0.000012152992,0.00017814209,0.0000023270009,7.0792277e-7,0.0000011388227,0.000049142698,0.0000054585503,0.000037979353],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999796,0.000057683952,0.000020583684,0.00006044506,0.000027060767,0.00003827756],"domain_scores_gemma":[0.9944062,0.004075801,0.00067981635,0.0004525708,0.00019132576,0.00019424866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00087634067,0.0002744366,0.00028170808,0.00059907115,0.0003823989,0.0010688116,0.00021127673,0.00039163517,0.0010660406],"category_scores_gemma":[0.007711434,0.00036624182,0.00041337917,0.00023829733,0.0005969108,0.0009241288,0.0007479335,0.00051523524,0.00011952721],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063085184,0.00006726686,0.64977866,0.000093309325,0.00050874887,0.00052772166,0.0004280387,0.28263187,0.043342654,0.00774946,0.00031460848,0.013926744],"study_design_scores_gemma":[0.000036478737,0.00016517653,0.31085894,0.000029624325,0.00012929038,0.00032438876,0.00016755816,0.6639286,0.016183356,0.0077322214,0.00036318626,0.00008111568],"about_ca_topic_score_codex":0.0017142768,"about_ca_topic_score_gemma":0.0021375308,"teacher_disagreement_score":0.0017142768,"about_ca_system_score_codex":0.00032410785,"about_ca_system_score_gemma":0.00015305309,"threshold_uncertainty_score":0.004634559},"labels":[],"label_agreement":null},{"id":"W2016492658","doi":"10.1029/2001gl014109","title":"Effects of nonlinear rheology on degree 2 harmonic deformation in a spherical self‐gravitating earth","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Rheology; Mantle (geology); Geology; Nonlinear system; Geophysics; Post-glacial rebound; Spherical harmonics; Physics; Glacial period; Thermodynamics","score_opus":0.03232915629991261,"score_gpt":0.26804558854252797,"score_spread":0.23571643224261535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016492658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969171,0.000039705094,0.0015977862,0.000053942873,0.0000051982806,0.000005204342,0.000038744587,0.00006094269,0.0012812543],"genre_scores_gemma":[0.999271,0.00004221759,0.00037611733,0.000007413287,0.0000016525811,0.000002466233,0.00002421009,0.000018316785,0.00025660032],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990976,0.000024662226,0.0000064096052,0.000010624261,0.000023332854,0.000025091962],"domain_scores_gemma":[0.9992471,0.0004399868,0.00009199086,0.00010064619,0.000054836095,0.00006559399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002261543,0.00037678296,0.00033826486,0.00034396208,0.00033101693,0.0006474772,0.00028117574,0.00050618703,0.0010658482],"category_scores_gemma":[0.001805076,0.0002954519,0.0005229481,0.00029005963,0.00088416936,0.00042920889,0.00067312474,0.0003454076,0.00013167509],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030788034,0.000070420596,0.010371756,0.000071421586,0.00004348694,0.00033182005,0.00019353433,0.934241,0.04797061,0.001683804,0.00013744831,0.004576674],"study_design_scores_gemma":[0.000025304353,0.000104743885,0.006099138,0.0000064681135,0.000018009408,0.00005539876,0.00003592158,0.98288065,0.0102847405,0.00031585363,0.00015301838,0.00002086062],"about_ca_topic_score_codex":0.006778818,"about_ca_topic_score_gemma":0.0037902815,"teacher_disagreement_score":0.006778818,"about_ca_system_score_codex":0.00045525102,"about_ca_system_score_gemma":0.0003440321,"threshold_uncertainty_score":0.013478696},"labels":[],"label_agreement":null},{"id":"W2016507588","doi":"10.1029/2008gl033532","title":"Mixing across the Arctic Ocean: Microstructure observations during the Beringia 2005 Expedition","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Core Research for Evolutional Science and Technology; Polarforskningssekretariatet; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Beringia; Arctic; Mixing (physics); The arctic; Oceanography; Geology; Climatology; Physics","score_opus":0.04302506758200594,"score_gpt":0.2888059028811027,"score_spread":0.24578083529909675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016507588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99922454,0.000056570163,0.000048427417,0.000013227684,0.0000032008338,0.0000024519163,0.0002430688,0.000004510874,0.00040404126],"genre_scores_gemma":[0.9986223,0.0000987403,0.0002720681,0.000015883908,0.000008498452,0.0000042812117,0.0005482808,0.000005705221,0.00042431196],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989283,0.000011570877,0.0000067678543,0.000032383225,0.000026903148,0.00002948419],"domain_scores_gemma":[0.99980396,0.000013477335,0.000060113613,0.0000094338275,0.00006740025,0.000045625693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029579943,0.00028488412,0.0002715784,0.0005014215,0.0008340509,0.0005325521,0.00015304652,0.0002380648,0.00035360508],"category_scores_gemma":[0.00036513025,0.00021544842,0.00014726359,0.00039865915,0.00025663033,0.00028543847,0.00042582914,0.00027386888,0.00015542368],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004947483,0.00006752995,0.95929646,0.000027964968,0.00010124402,0.0002544612,0.002489989,0.00041422615,0.027301695,0.000069968155,0.00054693705,0.008934843],"study_design_scores_gemma":[0.000002139025,0.000023496661,0.999005,0.0000028461848,0.0000064790015,0.000020182713,0.00014261853,0.00012178468,0.00034161206,0.0000039000206,0.00032769918,0.0000021920823],"about_ca_topic_score_codex":0.12088856,"about_ca_topic_score_gemma":0.24297635,"teacher_disagreement_score":0.12088856,"about_ca_system_score_codex":0.0011256636,"about_ca_system_score_gemma":0.00045357615,"threshold_uncertainty_score":0.2403698},"labels":[],"label_agreement":null},{"id":"W2016792977","doi":"10.1029/2000gl011802","title":"Further evidence of ice thinning in the Arctic Ocean","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":192,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council","keywords":"Arctic ice pack; Geology; Arctic; The arctic; Thinning; Oceanography; Sea ice; Climatology; Canada Basin; Arctic sea ice decline; Arctic dipole anomaly; Antarctic sea ice; Geography","score_opus":0.03830843509338509,"score_gpt":0.29674893586454704,"score_spread":0.25844050077116193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016792977","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99881303,0.00015859687,0.000053624106,0.000011305868,0.0000028148033,0.0000010443656,0.0001389713,0.00000212934,0.0008183062],"genre_scores_gemma":[0.9987785,0.0001747289,0.000100149664,0.000012712799,0.0000056643976,0.0000024210058,0.0004960552,0.0000018211277,0.0004279292],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999137,0.000011971044,0.0000095877185,0.000019889361,0.000019217756,0.000025672753],"domain_scores_gemma":[0.99949956,0.000066479806,0.00016795516,0.000038316757,0.00015250272,0.00007508411],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028786037,0.00012981848,0.000169043,0.000689603,0.00045056507,0.0004661159,0.0001010823,0.00023470173,0.00092450355],"category_scores_gemma":[0.0006476933,0.000104478204,0.00015597387,0.0006580587,0.00022292399,0.00019049413,0.0002444497,0.00023243472,0.00016873382],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007066024,0.00006308302,0.8550686,0.000059252023,0.00005818783,0.0005701655,0.0004702007,0.00033781413,0.13333268,0.00016409134,0.00020360068,0.0089657],"study_design_scores_gemma":[0.000001969907,0.000034590314,0.9964953,0.000005174215,0.000006739135,0.00018042854,0.0000611919,0.000092630115,0.0025878886,0.00001937347,0.00051297323,0.0000017882221],"about_ca_topic_score_codex":0.006120924,"about_ca_topic_score_gemma":0.009225038,"teacher_disagreement_score":0.006120924,"about_ca_system_score_codex":0.0002134817,"about_ca_system_score_gemma":0.00025553943,"threshold_uncertainty_score":0.012170613},"labels":[],"label_agreement":null},{"id":"W2016961897","doi":"10.1029/2009gl039429","title":"On the availability of uncoated mineral dust ice nuclei in cold cloud regions","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Ice nucleus; Atmospheric sciences; Environmental science; Mineral dust; Relative humidity; Clear ice; Saturation (graph theory); Liquid water; Nucleation; Sea ice growth processes; Mineral; Liquid water content; Homogeneous; Ice cloud; Geology; Arctic ice pack; Aerosol; Meteorology; Materials science; Climatology; Cloud computing; Sea ice thickness; Antarctic sea ice; Physics; Earth science; Sea ice; Thermodynamics","score_opus":0.02850881705845159,"score_gpt":0.2823977466553896,"score_spread":0.253888929596938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016961897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992698,0.00003507221,0.00026860155,0.0000053651165,7.5329393e-7,0.0000014525772,0.000033554756,0.0000051462985,0.0003802051],"genre_scores_gemma":[0.99975437,0.000017949204,0.00013242291,0.0000011051852,4.315076e-7,7.737822e-7,0.000044022105,0.000003066462,0.000045890352],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.0000080974,0.0000016615238,0.000012232494,0.0000081092085,0.000015569834],"domain_scores_gemma":[0.9997689,0.00013305957,0.000032628934,0.00001370179,0.0000349331,0.000016718459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015888584,0.00023246619,0.00019260691,0.00024021465,0.00025867243,0.00029821537,0.00034715794,0.00021017967,0.0009211123],"category_scores_gemma":[0.0006042407,0.0001585411,0.0002657606,0.00015576802,0.00022866971,0.00045964555,0.00017841058,0.000118374344,0.000086096494],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007939858,0.00013413795,0.24254711,0.00015315601,0.00015169164,0.0008112027,0.0002264177,0.6230254,0.12108798,0.001398048,0.00017239084,0.009498453],"study_design_scores_gemma":[0.00007565906,0.00018989856,0.1969695,0.000016402792,0.00010214123,0.00011430651,0.00035808596,0.75138336,0.049901556,0.00043663732,0.00042561328,0.000026895099],"about_ca_topic_score_codex":0.018993028,"about_ca_topic_score_gemma":0.013559854,"teacher_disagreement_score":0.018993028,"about_ca_system_score_codex":0.00061368564,"about_ca_system_score_gemma":0.00025213746,"threshold_uncertainty_score":0.037764966},"labels":[],"label_agreement":null},{"id":"W2016973289","doi":"10.1029/2006gl027668","title":"Recycling the lid: Effects of subduction and stirring on boundary layer dynamics in bottom‐heated planetary mantle convection","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Geology; Mantle (geology); Subduction; Mantle convection; Geophysics; Mantle wedge; Mantle plume; Transition zone; Lithosphere; Plate tectonics; Plume; Downwelling; Boundary layer; Convection; Upwelling; Venus; Tectonics; Mechanics; Astrobiology; Thermodynamics; Seismology; Oceanography","score_opus":0.014331118567103516,"score_gpt":0.2530985269157111,"score_spread":0.2387674083486076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2016973289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979407,0.00013128556,0.0005778959,0.00007219415,0.000011880264,0.000006332606,0.000050487626,0.00004906101,0.0011601241],"genre_scores_gemma":[0.99944454,0.000045468358,0.00025154246,0.000016801345,0.0000023373198,0.0000037121642,0.000027267633,0.000012922274,0.00019541354],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993587,0.000014567756,0.000004884736,0.000010710513,0.000008288022,0.000025629997],"domain_scores_gemma":[0.9996649,0.000113126574,0.000068342015,0.000030336247,0.000026251555,0.000097146185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022060215,0.000302827,0.0003267456,0.00034863933,0.00047459156,0.0011078898,0.0003886242,0.0005637436,0.0013417521],"category_scores_gemma":[0.0016712658,0.00030499746,0.00039924143,0.00016467023,0.0007173872,0.0006341506,0.0007884537,0.00048750918,0.00016692776],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026481275,0.000788853,0.08136085,0.00027924398,0.00016192949,0.0011588113,0.00058356056,0.6402926,0.2506194,0.0057892706,0.0008972782,0.0154201295],"study_design_scores_gemma":[0.00024769193,0.00033541973,0.026492614,0.000029403951,0.00006719478,0.00007136392,0.00019586796,0.9522731,0.018765759,0.0008969512,0.00058061775,0.00004391068],"about_ca_topic_score_codex":0.00838337,"about_ca_topic_score_gemma":0.0034048287,"teacher_disagreement_score":0.00838337,"about_ca_system_score_codex":0.00065534585,"about_ca_system_score_gemma":0.00053765165,"threshold_uncertainty_score":0.016669154},"labels":[],"label_agreement":null},{"id":"W2017259013","doi":"10.1029/2008gl034586","title":"Rheological stratification of the lithosphere: A direct inference based upon the geodetically observed pattern of the glacial isostatic adjustment of the North American continent","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Post-glacial rebound; Geology; Lithosphere; Glacial period; Stratification (seeds); Deglaciation; Ice sheet; Rheology; Last Glacial Maximum; Geodesy; Geophysics; Climatology; Paleontology; Geomorphology; Tectonics","score_opus":0.05862973166974873,"score_gpt":0.272594135574942,"score_spread":0.21396440390519328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017259013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9753493,0.0032851659,0.0131173935,0.0006579248,0.000025585116,0.000010106239,0.00012281886,0.00009474636,0.007336959],"genre_scores_gemma":[0.9963755,0.0012009713,0.001949603,0.00003847543,0.000020881915,0.0000025101888,0.00008590045,0.0000063978746,0.00031969993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.000013358125,0.0000027384337,0.000014532309,0.000010014959,0.0000058888],"domain_scores_gemma":[0.99980325,0.000051092025,0.00006511491,0.000034227385,0.00002956365,0.000016771843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030300114,0.00015847823,0.00009413673,0.00060888584,0.00020742316,0.0008635004,0.0002757091,0.0001846081,0.0005770169],"category_scores_gemma":[0.00092946243,0.0000980074,0.00011700644,0.00042411918,0.0013450147,0.0007302441,0.00048685068,0.00033145174,0.00014842139],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003034321,0.00005971053,0.78037524,0.00027052723,0.000100821555,0.0006879808,0.0016624687,0.014858448,0.022900345,0.030098446,0.0015449519,0.14713758],"study_design_scores_gemma":[0.000024942756,0.00017714268,0.8733271,0.00011203552,0.00013232698,0.0007824156,0.0014608391,0.073610865,0.00742666,0.030629102,0.0122592375,0.000057361034],"about_ca_topic_score_codex":0.008335451,"about_ca_topic_score_gemma":0.014260402,"teacher_disagreement_score":0.008335451,"about_ca_system_score_codex":0.00048813623,"about_ca_system_score_gemma":0.0004289903,"threshold_uncertainty_score":0.016573846},"labels":[],"label_agreement":null},{"id":"W2017302039","doi":"10.1029/2008gl035152","title":"Dynamic ocean topography for the northeast Pacific and its continental margins","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Ocean surface topography; Altimeter; Geoid; Geology; Tide gauge; Sea-surface height; Satellite; Dynamic height; Climatology; Continental shelf; Oceanography; Geodesy; Sea level; Geophysics; Hydrography","score_opus":0.04054182933104244,"score_gpt":0.2670404169695141,"score_spread":0.22649858763847164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017302039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910623,0.00023690781,0.0026435542,0.000061027757,0.0000038063424,0.000006704643,0.0010894205,0.000049309267,0.0048469305],"genre_scores_gemma":[0.9975089,0.00013166461,0.0010808216,0.0000052520586,0.0000017944833,0.000002758255,0.0008261318,0.000008370776,0.00043421696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999682,0.0000026254172,0.0000022152212,0.000011337601,0.000011359073,0.0000042235943],"domain_scores_gemma":[0.9999343,0.00000617699,0.00001805218,0.000009808476,0.00002173405,0.0000099879],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056042038,0.00010258568,0.00005944038,0.00043202259,0.00015570864,0.00042168685,0.00010661476,0.000090824135,0.0008296845],"category_scores_gemma":[0.00028747585,0.00009596506,0.00012178005,0.00060468575,0.00011322035,0.00030777827,0.00031938168,0.000091292764,0.00011531155],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055253255,0.000014955152,0.81663865,0.000041057287,0.000068689325,0.00027603575,0.00017536421,0.087197915,0.0060348525,0.0015207919,0.0013321693,0.08664426],"study_design_scores_gemma":[0.0000048920647,0.0000144843325,0.9549884,0.000010882873,0.00001585348,0.00013496383,0.00011098,0.041043207,0.0005191404,0.00046635207,0.0026808593,0.000009901072],"about_ca_topic_score_codex":0.059226684,"about_ca_topic_score_gemma":0.07192646,"teacher_disagreement_score":0.059226684,"about_ca_system_score_codex":0.00030398637,"about_ca_system_score_gemma":0.00042201317,"threshold_uncertainty_score":0.11776394},"labels":[],"label_agreement":null},{"id":"W2017464670","doi":"10.1029/2006gl027740","title":"A study of aspect angle effects in the <i>E</i>‐region irregularity velocity using multi‐point electric field measurements","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Electric field; Point (geometry); Field (mathematics); Geology; Geophysics; Physics; Geodesy; Optics; Computational physics; Geometry; Mathematics","score_opus":0.042387930289510524,"score_gpt":0.30920516836609124,"score_spread":0.2668172380765807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017464670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99494064,0.000109758905,0.003790344,0.00000799382,0.000003787677,0.000007890667,0.00009069582,0.00003460443,0.0010142925],"genre_scores_gemma":[0.9990325,0.000053232656,0.0007594499,0.0000025541758,0.0000029417592,0.0000018614127,0.00007509407,0.0000067853252,0.000065650354],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998765,0.000025584884,0.0000075892494,0.00003465727,0.0000363604,0.000019202878],"domain_scores_gemma":[0.9985139,0.0007678658,0.000383947,0.00010836572,0.0001800349,0.0000458908],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002790127,0.0001915067,0.00012712265,0.00041392745,0.00009799572,0.00028792926,0.00012478394,0.00014779957,0.00023903165],"category_scores_gemma":[0.0017251595,0.00012496971,0.00012614949,0.0005266701,0.00013279403,0.00027454653,0.0001148512,0.00014253348,0.000079825484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00088768965,0.00011259106,0.54283834,0.00011476323,0.000088959896,0.000441843,0.0002800106,0.018726876,0.36770877,0.00045029938,0.00020600151,0.06814388],"study_design_scores_gemma":[0.000013012281,0.0003802383,0.91393864,0.000010819737,0.00003506852,0.0005470476,0.000068711925,0.027643017,0.05646389,0.000081890386,0.0007964222,0.000021071142],"about_ca_topic_score_codex":0.0009669827,"about_ca_topic_score_gemma":0.00097443233,"teacher_disagreement_score":0.0009669827,"about_ca_system_score_codex":0.000106293664,"about_ca_system_score_gemma":0.00006633127,"threshold_uncertainty_score":0.001922667},"labels":[],"label_agreement":null},{"id":"W2017484112","doi":"10.1029/2006gl028959","title":"Changes in the pool of Labrador Sea Water in the subpolar North Atlantic","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Baroclinity; North Atlantic Deep Water; North Atlantic oscillation; Oceanography; Climatology; Geology; Water mass; Circumpolar deep water; Subtropics; Thermohaline circulation; Fishery","score_opus":0.034192813752676264,"score_gpt":0.2884736071981351,"score_spread":0.25428079344545884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017484112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991353,0.000078765246,0.000020669662,0.000020136604,0.0000010078562,0.000001397083,0.00038135325,0.000003249347,0.00035822947],"genre_scores_gemma":[0.99897027,0.00007412424,0.000047150756,0.000015061595,0.0000027324065,0.0000037829489,0.00068111595,0.0000016996116,0.00020405941],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999157,0.000008609857,0.000009025746,0.00002901565,0.000014360761,0.000023250717],"domain_scores_gemma":[0.99957794,0.000029393726,0.00021472499,0.000031391617,0.00007869966,0.00006792634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018873536,0.00013163504,0.00017555765,0.00078798993,0.00029518807,0.0006438623,0.0002722174,0.00017847845,0.0007909864],"category_scores_gemma":[0.00042281972,0.00011781962,0.00017422925,0.00079045555,0.00025141874,0.0004345433,0.00034997085,0.00013019869,0.00026576998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012791267,0.00001664262,0.98893726,0.000014821109,0.000042226486,0.000046870442,0.00031235567,0.000111448106,0.004858089,0.00005373989,0.00014134913,0.005337226],"study_design_scores_gemma":[0.000001225057,0.000009018151,0.9993563,0.0000020173056,0.0000045697584,0.000014052065,0.0000783567,0.000083099585,0.00022484119,0.0000071998734,0.00021766912,0.0000016013603],"about_ca_topic_score_codex":0.065635286,"about_ca_topic_score_gemma":0.108302034,"teacher_disagreement_score":0.065635286,"about_ca_system_score_codex":0.0009393234,"about_ca_system_score_gemma":0.000385214,"threshold_uncertainty_score":0.13050652},"labels":[],"label_agreement":null},{"id":"W2017881067","doi":"10.1029/2001gl012959","title":"Wide‐angle reflectivity across the Torngat Orogen, NE Canada","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Transect; Reflection (computer programming); Reflectivity; Seismology; Refraction; Optics; Oceanography","score_opus":0.04834963795337511,"score_gpt":0.3119233835186255,"score_spread":0.2635737455652504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2017881067","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9678518,0.0008950118,0.00042056074,0.00034591547,0.000012883402,0.00005619141,0.008535252,0.00006794027,0.021814404],"genre_scores_gemma":[0.9822253,0.0008581454,0.0009132215,0.00010788105,0.0000037339287,0.000020599358,0.003949143,0.000030025156,0.011891773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997154,0.00001074751,0.00000735118,0.000040844818,0.00010077578,0.00012472938],"domain_scores_gemma":[0.9996779,0.000010229252,0.00002617138,0.000008023674,0.00022128283,0.000056297227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013381791,0.000252891,0.00019397183,0.0009272171,0.0014331288,0.0007471186,0.00045619544,0.00016158061,0.0025609597],"category_scores_gemma":[0.00037035445,0.00021641856,0.00012810086,0.0020385678,0.00034044086,0.00017295622,0.0004341361,0.00022663458,0.00040589503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059871806,0.00006782485,0.8618299,0.00032340584,0.00023341033,0.0016472578,0.004936957,0.0028611484,0.02070908,0.0017079083,0.017480599,0.08760384],"study_design_scores_gemma":[0.00001551865,0.000017380164,0.9805024,0.000047317233,0.00003711281,0.00020326265,0.0021451213,0.00080836186,0.0011729845,0.000048967613,0.014980797,0.000020743091],"about_ca_topic_score_codex":0.99326706,"about_ca_topic_score_gemma":0.9983536,"teacher_disagreement_score":0.012288163,"about_ca_system_score_codex":0.012288163,"about_ca_system_score_gemma":0.018375287,"threshold_uncertainty_score":0.08915734},"labels":[],"label_agreement":null},{"id":"W2018045227","doi":"10.1029/2009gl039533","title":"Annual push moraines as climate proxy","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Northern British Columbia","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Glacier; Moraine; Glacier mass balance; Climatology; Precipitation; Climate change; Proxy (statistics); Physical geography; Tidewater glacier cycle; Geology; Paleoclimatology; Environmental science; Geography; Meteorology; Oceanography","score_opus":0.034453744976421806,"score_gpt":0.3059326136034208,"score_spread":0.271478868626999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018045227","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963128,0.00023463026,0.000353674,0.00003319919,0.000002717388,0.0000036592478,0.0015233207,0.00002360238,0.0015123188],"genre_scores_gemma":[0.99728787,0.00012626895,0.0006067037,0.0000061375017,0.0000026809053,0.000004550082,0.0015814116,0.0000052466708,0.00037911168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999021,0.000014693366,0.0000037930267,0.000025044508,0.000022246917,0.00003202227],"domain_scores_gemma":[0.9995604,0.000047626516,0.00014582902,0.000054443033,0.000114519295,0.00007717714],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018653908,0.00012594085,0.00013868955,0.0009107565,0.00048367126,0.0006686377,0.00020960892,0.0000952233,0.0008780592],"category_scores_gemma":[0.00074792997,0.000096842785,0.000096938966,0.0012546668,0.00021857816,0.00016037491,0.00034438225,0.00020333505,0.00018041825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046504014,0.000011649133,0.97825706,0.000017277274,0.000067288296,0.00011256178,0.00044940374,0.0048158565,0.0009091357,0.00046512933,0.0009965149,0.013851622],"study_design_scores_gemma":[0.0000028083853,0.000005740027,0.9891606,0.000014849813,0.000014634346,0.00005674125,0.00042894436,0.0059046065,0.000202066,0.000118777265,0.0040820152,0.000008096519],"about_ca_topic_score_codex":0.5494101,"about_ca_topic_score_gemma":0.83702064,"teacher_disagreement_score":0.5494101,"about_ca_system_score_codex":0.0015970477,"about_ca_system_score_gemma":0.0015636382,"threshold_uncertainty_score":0.906487},"labels":[],"label_agreement":null},{"id":"W2018334591","doi":"10.1029/2004gl021812","title":"On the role of atmospheric chemistry in the global CO<sub>2</sub>budget","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Carbon cycle; Atmosphere (unit); Carbon fibers; Combustion; Biomass (ecology); Deposition (geology); Environmental science; Fossil fuel; Environmental chemistry; Vegetation (pathology); Atmospheric sciences; Chemistry; Materials science; Meteorology; Geology; Paleontology; Oceanography; Physical chemistry; Physics; Ecology","score_opus":0.007307486638470389,"score_gpt":0.24334324708351093,"score_spread":0.23603576044504054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018334591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9779643,0.00032111592,0.014490471,0.00055455574,0.000029009505,0.000037411173,0.00079177326,0.00015164868,0.005659706],"genre_scores_gemma":[0.99648225,0.00022961889,0.002440413,0.000034057914,0.000008034476,0.000021721155,0.00016257391,0.000035989346,0.00058513356],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999393,0.000027657363,0.000002417794,0.000009548854,0.000009219152,0.000011949644],"domain_scores_gemma":[0.99975437,0.0001703759,0.000019485979,0.000012477498,0.000025472937,0.000017739345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003273876,0.00060482987,0.00032876947,0.000259223,0.00038691305,0.00066042703,0.00036851043,0.0006624401,0.0016212194],"category_scores_gemma":[0.00088307494,0.00031093584,0.00041100115,0.00046017626,0.0004553849,0.00067885104,0.0004654801,0.00031491678,0.00013599354],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008051143,0.000019125257,0.006067645,0.000023984787,0.000027491666,0.000044887838,0.0000149083235,0.98658806,0.0024053266,0.0016385291,0.00015736638,0.0029321874],"study_design_scores_gemma":[0.000020119453,0.00001968167,0.0023001079,0.0000026662142,0.000013645348,0.0000063554453,0.0000138308515,0.996154,0.0004973865,0.00069903204,0.00026735553,0.000005792325],"about_ca_topic_score_codex":0.047397926,"about_ca_topic_score_gemma":0.021620397,"teacher_disagreement_score":0.047397926,"about_ca_system_score_codex":0.0011004888,"about_ca_system_score_gemma":0.00083746057,"threshold_uncertainty_score":0.09424406},"labels":[],"label_agreement":null},{"id":"W2018517736","doi":"10.1029/2005gl023533","title":"Nonlinear atmospheric variability in the winter northeast Pacific associated with the Madden‐Julian oscillation","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Madden–Julian oscillation; Climatology; Precipitation; Oscillation (cell signaling); Environmental science; Atmospheric sciences; Latitude; Nonlinear system; Pacific decadal oscillation; Geology; Antarctic oscillation; El Niño Southern Oscillation; Meteorology; Geography; Convection; Physics","score_opus":0.023961023907618867,"score_gpt":0.2742708654563054,"score_spread":0.2503098415486865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018517736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866307,0.000055150398,0.00021746938,0.00006732006,0.0000046541163,0.0000028264417,0.0000927289,0.000009009111,0.00088774815],"genre_scores_gemma":[0.99964416,0.000031169653,0.00008162475,0.0000059237364,0.0000055620712,0.0000014365428,0.00010747938,0.0000016604762,0.000120923134],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994576,0.000011679887,0.0000038217177,0.000012510845,0.000014775228,0.00001141568],"domain_scores_gemma":[0.9997527,0.00007249427,0.00009008561,0.000017143939,0.000040164174,0.0000274446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001906684,0.00012002278,0.0001066536,0.00022110394,0.0002576043,0.00035339597,0.00009303257,0.00011592531,0.0005572514],"category_scores_gemma":[0.0011317563,0.00010574845,0.00014129719,0.00034766813,0.00022729808,0.00016114704,0.0003505661,0.00020924868,0.000063710075],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002549125,0.000049720722,0.9543408,0.00004181805,0.000116714575,0.00045312353,0.0004732475,0.015327802,0.014213208,0.0014135891,0.0008421918,0.012472775],"study_design_scores_gemma":[0.000006942464,0.000012627146,0.98437035,0.0000036272213,0.000011897409,0.000061827486,0.00005250044,0.014565193,0.00024728852,0.00034116293,0.00032144104,0.000005197276],"about_ca_topic_score_codex":0.017512288,"about_ca_topic_score_gemma":0.017992456,"teacher_disagreement_score":0.017512288,"about_ca_system_score_codex":0.00039618544,"about_ca_system_score_gemma":0.00023000596,"threshold_uncertainty_score":0.034820735},"labels":[],"label_agreement":null},{"id":"W2018553921","doi":"10.1029/2001gl013712","title":"The influence of continental surface area on the assembly time for supercontinents","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Supercontinent; Geology; Mantle (geology); Geophysics; Geodesy; Paleontology; Tectonics; Craton","score_opus":0.03452787916867365,"score_gpt":0.26484538228545107,"score_spread":0.23031750311677743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018553921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99640924,0.000051179533,0.0028692817,0.00004090479,0.0000036433642,0.0000028904649,0.000038257636,0.000029812612,0.0005547171],"genre_scores_gemma":[0.9990823,0.000032797794,0.00062981015,0.000004342113,0.0000012867418,0.0000044286144,0.00006273741,0.0000176461,0.00016454009],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998807,0.000025266932,0.0000053625067,0.000031837943,0.000021392905,0.000035556663],"domain_scores_gemma":[0.99801433,0.0012304095,0.00025464824,0.0001776074,0.00011888797,0.00020417351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056014775,0.0002488972,0.0002454205,0.00044076968,0.00066037575,0.0007349793,0.000434702,0.00033379073,0.0012356585],"category_scores_gemma":[0.005585347,0.00028310466,0.00041777967,0.0003273074,0.0006149972,0.0006289548,0.0006145487,0.0004925111,0.000113105314],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036520997,0.000056726913,0.076947205,0.000040065985,0.00007894319,0.00024997554,0.00022164924,0.88312507,0.026582615,0.005141151,0.00021564534,0.0069757705],"study_design_scores_gemma":[0.000029581055,0.00017015937,0.024718279,0.000007557133,0.000053071602,0.000104383915,0.00010647773,0.9620225,0.010419351,0.0018161881,0.0005216519,0.00003074057],"about_ca_topic_score_codex":0.006984756,"about_ca_topic_score_gemma":0.0035701462,"teacher_disagreement_score":0.006984756,"about_ca_system_score_codex":0.0006771729,"about_ca_system_score_gemma":0.0003911412,"threshold_uncertainty_score":0.01388824},"labels":[],"label_agreement":null},{"id":"W2018665108","doi":"10.1029/2002gl016197","title":"Variability of sea‐ice draft off Hokkaido in the Sea of Okhotsk revealed by a moored ice‐profiling sonar in winter of 1999","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"ASL Environmental Sciences (Canada)","funders":"","keywords":"Sea ice; Geology; Oceanography; Climatology; Arctic ice pack; Antarctic sea ice","score_opus":0.018442779136345958,"score_gpt":0.2683984464084261,"score_spread":0.24995566727208013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018665108","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978215,0.000014608445,0.000019823576,0.0000037843918,0.00000121654,0.0000011263255,0.00007958022,0.0000014191469,0.000096332755],"genre_scores_gemma":[0.99938023,0.00003143645,0.00008868551,0.000005825539,0.0000020933273,0.0000038774047,0.00037550685,0.0000013797862,0.00011087254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991786,0.000005616242,0.000010072426,0.000020795513,0.000016593913,0.00002904503],"domain_scores_gemma":[0.99962974,0.000041019786,0.00011002502,0.000019450206,0.00010718774,0.00009266688],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019923136,0.00024791717,0.00024126064,0.00047064447,0.00046254383,0.000535474,0.00020381373,0.00027515762,0.00026681728],"category_scores_gemma":[0.00045309044,0.00019672849,0.00016454232,0.00046734494,0.00042547676,0.0003173006,0.00038399635,0.0001745405,0.00009094859],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003043802,0.000046328394,0.9765686,0.000036149886,0.00009447892,0.0004238774,0.0017433172,0.0007958924,0.014505258,0.000035094323,0.00018376292,0.0052627707],"study_design_scores_gemma":[0.0000018297944,0.000017669652,0.99918276,0.000002429263,0.000011145725,0.000027178203,0.00028513698,0.0002069164,0.00017487633,0.0000029448631,0.00008436917,0.0000027465376],"about_ca_topic_score_codex":0.07635135,"about_ca_topic_score_gemma":0.15869114,"teacher_disagreement_score":0.07635135,"about_ca_system_score_codex":0.0007602992,"about_ca_system_score_gemma":0.0004763535,"threshold_uncertainty_score":0.15181386},"labels":[],"label_agreement":null},{"id":"W2018693596","doi":"10.1029/2003gl018542","title":"Nonstationary impact of ENSO on Euro‐Atlantic winter climate","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Climatology; Extratropical cyclone; Teleconnection; Tropics; Forcing (mathematics); El Niño Southern Oscillation; Environmental science; Southern oscillation; Tropical Atlantic; Climate change; Atmospheric sciences; Geology; Oceanography; Sea surface temperature","score_opus":0.04077208401518674,"score_gpt":0.34374965321857337,"score_spread":0.30297756920338664,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018693596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99628323,0.00009794948,0.00075370073,0.00037541497,0.000040835235,0.0000055263004,0.00042497393,0.000057177298,0.0019611889],"genre_scores_gemma":[0.99952114,0.000051936666,0.000049460432,0.00003362169,0.000014708639,0.0000019663657,0.0001953344,0.000009963854,0.00012198921],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966955,0.000088944485,0.000032579857,0.000092464616,0.000048579826,0.000067838235],"domain_scores_gemma":[0.9977477,0.0010864533,0.0005185607,0.00027573897,0.00020192262,0.00016955721],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014465303,0.00034780838,0.00029033353,0.00036913098,0.00044988032,0.000999735,0.0003064224,0.00060809444,0.0015687458],"category_scores_gemma":[0.006609961,0.00023848553,0.0004442258,0.00046120537,0.0005209655,0.00094780006,0.00077450153,0.00051039265,0.00020991631],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017461521,0.0002193697,0.6892152,0.00012850789,0.00078186835,0.00086209585,0.00037619617,0.25180802,0.023508694,0.0077940524,0.002378706,0.021181136],"study_design_scores_gemma":[0.000057772377,0.00013120478,0.80567807,0.000021273407,0.00010777306,0.00009522929,0.000110904075,0.18877862,0.0019252198,0.0021409187,0.0009126645,0.000040282415],"about_ca_topic_score_codex":0.010780031,"about_ca_topic_score_gemma":0.011178611,"teacher_disagreement_score":0.010780031,"about_ca_system_score_codex":0.0007274096,"about_ca_system_score_gemma":0.00042588782,"threshold_uncertainty_score":0.021434605},"labels":[],"label_agreement":null},{"id":"W2018763204","doi":"10.1029/2006gl028811","title":"Coralline alga reveals first marine record of subarctic North Pacific climate change","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal plant biology","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Subarctic climate; Oceanography; Teleconnection; Pacific decadal oscillation; Geology; Climate change; Crustose; Climatology; Marine ecosystem; El Niño Southern Oscillation; Sea surface temperature; Ecosystem; Ecology; Reef","score_opus":0.05035426599012259,"score_gpt":0.2777427884855382,"score_spread":0.22738852249541558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018763204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99380964,0.0005551504,0.000117143936,0.00010995024,0.000008848347,0.0000037358575,0.0023088898,0.000027759797,0.0030588272],"genre_scores_gemma":[0.9970408,0.0004997818,0.00033183378,0.00003664631,0.000014780616,0.000004441342,0.0016493452,0.000008462471,0.00041389072],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999472,0.0000043258415,0.0000051687352,0.000016417294,0.000012804239,0.000014222179],"domain_scores_gemma":[0.9996152,0.000018434674,0.00015379665,0.000046823676,0.00010625098,0.00005940976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013919831,0.00015879315,0.0001450321,0.001149362,0.00037659678,0.00062216056,0.00011681414,0.00014699338,0.0011466438],"category_scores_gemma":[0.0004123647,0.00010121889,0.00008718583,0.0011159622,0.00019472362,0.00029481036,0.00053190876,0.00022255063,0.00021442253],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028123604,0.000014247294,0.9801736,0.000031349082,0.00004062266,0.00008598177,0.00023833812,0.00017573516,0.0033090098,0.00010704962,0.00073646154,0.015059405],"study_design_scores_gemma":[3.5486798e-7,0.0000026611042,0.998836,0.000002673107,0.000005011818,0.000029947503,0.000058540998,0.000039649825,0.00011248648,0.000009988058,0.0009017505,9.4195855e-7],"about_ca_topic_score_codex":0.0359111,"about_ca_topic_score_gemma":0.09699511,"teacher_disagreement_score":0.0359111,"about_ca_system_score_codex":0.00035256345,"about_ca_system_score_gemma":0.00045479625,"threshold_uncertainty_score":0.07140416},"labels":[],"label_agreement":null},{"id":"W2018880304","doi":"10.1029/2007gl033063","title":"Current broadening as a mechanism for anticyclogenesis at the Northwest Corner of the North Atlantic Current","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Naval Research Laboratory; National Science Foundation","keywords":"Eddy; Current (fluid); Geology; Oceanography; Front (military); Boundary current; Vortex; Subduction; Flow (mathematics); Ocean current; Climatology; Meteorology; Paleontology; Mechanics; Turbulence; Physics; Tectonics","score_opus":0.03952160633892153,"score_gpt":0.2797017156899934,"score_spread":0.24018010935107187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018880304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99061346,0.00037773122,0.0036019103,0.0001811434,0.000024584397,0.000018830824,0.00003461755,0.00012407335,0.0050236895],"genre_scores_gemma":[0.9989359,0.000098175435,0.00042212027,0.00001647583,0.000012308704,0.000003910521,0.000013209884,0.000009990419,0.00048784603],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999205,0.000010916551,0.0000040524124,0.000014849681,0.000017690289,0.000032074513],"domain_scores_gemma":[0.9997596,0.00003917396,0.000072205614,0.00003950821,0.00003473286,0.00005477634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017785127,0.00015672721,0.00030617448,0.00058987434,0.000401109,0.0005669503,0.0003888621,0.0003010325,0.0016671235],"category_scores_gemma":[0.0004828739,0.00023736649,0.00020802586,0.00019463248,0.00042727287,0.0005333852,0.0006763973,0.0003620982,0.00017694125],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075670093,0.00031478624,0.20841219,0.00018760713,0.00012487655,0.0037912158,0.001729778,0.059444193,0.5968068,0.055595875,0.0025989579,0.070236996],"study_design_scores_gemma":[0.00018390453,0.00029939378,0.5945592,0.00011296885,0.00012457234,0.0014527617,0.0012536782,0.34009147,0.037869494,0.016609836,0.007337835,0.0001049831],"about_ca_topic_score_codex":0.005569579,"about_ca_topic_score_gemma":0.0054693185,"teacher_disagreement_score":0.005569579,"about_ca_system_score_codex":0.0006348103,"about_ca_system_score_gemma":0.0002617959,"threshold_uncertainty_score":0.011074305},"labels":[],"label_agreement":null},{"id":"W2018980692","doi":"10.1029/2005gl022415","title":"Trends of HF, HCl, CCl<sub>2</sub>F<sub>2</sub>, CCl<sub>3</sub>F, CHClF<sub>2</sub> (HCFC‐22), and SF<sub>6</sub> in the lower stratosphere from Atmospheric Chemistry Experiment (ACE) and Atmospheric Trace Molecule Spectroscopy (ATMOS) measurements near 30°N latitude","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University; University of Waterloo","funders":"","keywords":"Stratosphere; Atmospheric sciences; Occultation; Altitude (triangle); Atmospheric chemistry; Environmental science; Mixing ratio; Trace gas; Analytical Chemistry (journal); Ozone; Chemistry; Meteorology; Physics; Astrophysics; Environmental chemistry","score_opus":0.018666614157022227,"score_gpt":0.2553516247243764,"score_spread":0.23668501056735416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018980692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99498934,0.00011784684,0.0002041554,0.00003960066,0.0000046873793,0.000007213357,0.0031978998,0.000041847143,0.0013973241],"genre_scores_gemma":[0.9946681,0.00009787055,0.00034880533,0.00003540096,0.000005989406,0.000012399017,0.0038804302,0.000004965884,0.00094603363],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999455,0.0000037007521,0.0000035443668,0.000019034922,0.000011380469,0.00001688071],"domain_scores_gemma":[0.9996927,0.00004287193,0.00008994783,0.000014434853,0.00012639238,0.00003360489],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009680963,0.00020435233,0.00011556485,0.000720928,0.00016508103,0.00022915009,0.00018819123,0.0002787694,0.0009579727],"category_scores_gemma":[0.0002361133,0.00009935452,0.00013177306,0.00067539443,0.00012089286,0.00018223432,0.00010269423,0.00021488528,0.00016787428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004628849,0.00009007016,0.90750986,0.00011217989,0.0001378287,0.00018447106,0.0004490205,0.0021897082,0.072559364,0.000292259,0.0023904897,0.013621873],"study_design_scores_gemma":[0.0000023888356,0.000031162006,0.995552,0.0000021974706,0.00001317051,0.00002073295,0.00007043985,0.00050715794,0.0029728988,0.000009557848,0.0008150416,0.0000030961094],"about_ca_topic_score_codex":0.09514111,"about_ca_topic_score_gemma":0.13678609,"teacher_disagreement_score":0.09514111,"about_ca_system_score_codex":0.00084245455,"about_ca_system_score_gemma":0.00027553883,"threshold_uncertainty_score":0.18917465},"labels":[],"label_agreement":null},{"id":"W2018987657","doi":"10.1029/2000gl011581","title":"The lognormal distribution as a reference for reporting aerosol optical depth statistics; Empirical tests using multi‐year, multi‐site AERONET Sunphotometer data","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":209,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"AERONET; Log-normal distribution; Aerosol; Statistics; Environmental science; Meteorology; Mathematics; Geography","score_opus":0.17986106485943712,"score_gpt":0.4230865685575935,"score_spread":0.2432255036981564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2018987657","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14405717,0.0017165217,0.8217145,0.0011927715,0.0006602002,0.00065470126,0.007308681,0.0022860072,0.020409415],"genre_scores_gemma":[0.70265347,0.0017359403,0.2812726,0.00089607184,0.00023664511,0.0012058953,0.0067793885,0.0004790334,0.0047410154],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.98117524,0.008291394,0.002351611,0.0015259874,0.006208726,0.00044697756],"domain_scores_gemma":[0.89569026,0.061309647,0.0111441575,0.013141926,0.018064506,0.0006493895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.023397652,0.0007198255,0.0007610378,0.003949468,0.0010176441,0.0021203787,0.0022913858,0.0013681477,0.004046428],"category_scores_gemma":[0.13653316,0.0002918655,0.00070108316,0.004984249,0.0014655015,0.0034835304,0.0011110154,0.0017313673,0.0011378233],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012058519,0.00090274867,0.30952173,0.001180357,0.0007068477,0.0016423649,0.0020227428,0.13151778,0.013483903,0.15706123,0.05215892,0.32859552],"study_design_scores_gemma":[0.00027682158,0.0029448303,0.19770007,0.0015065953,0.00042420012,0.0066396673,0.0035657126,0.47536972,0.040577486,0.14427556,0.12610409,0.0006152629],"about_ca_topic_score_codex":0.009985432,"about_ca_topic_score_gemma":0.009372137,"teacher_disagreement_score":0.023397652,"about_ca_system_score_codex":0.0016222425,"about_ca_system_score_gemma":0.002315861,"threshold_uncertainty_score":0.12374008},"labels":[],"label_agreement":null},{"id":"W2019074087","doi":"10.1029/2008gl036467","title":"A decade of dust: Asian dust and springtime aerosol load in the U.S. Pacific Northwest","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Asian Dust; Environmental science; SeaWiFS; Atmospheric sciences; Precipitation; Climatology; Mineral dust; Meteorology; Geography; Geology; Chemistry","score_opus":0.020234401714234254,"score_gpt":0.262836278173726,"score_spread":0.24260187645949177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019074087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99812025,0.00018359777,0.00014974085,0.000100342084,0.0000061931046,0.0000013481259,0.0007762092,0.0000128545935,0.0006493792],"genre_scores_gemma":[0.99781334,0.00018767701,0.0003022272,0.000035377245,0.000007830942,0.0000021482704,0.0013172379,0.0000070514416,0.0003270259],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994767,0.0000063009174,0.000005348789,0.00001989349,0.0000125891565,0.000008180857],"domain_scores_gemma":[0.99977404,0.000035041983,0.00006150593,0.000017669252,0.00006044362,0.000051335617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032514246,0.00015029043,0.0001501426,0.0004807619,0.00024800608,0.00062048086,0.00017879733,0.0002691741,0.00057065557],"category_scores_gemma":[0.00054389745,0.00011823784,0.00016489021,0.00082718016,0.000119678894,0.0005630801,0.00025458712,0.00023723097,0.00012368425],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008910184,0.000027093816,0.98095465,0.000022981441,0.00006825365,0.00013404145,0.00025273475,0.0029192574,0.0013951358,0.00013068812,0.00070947735,0.013296607],"study_design_scores_gemma":[0.000004780898,0.000012218048,0.9927509,0.000012579494,0.000026331803,0.000055614175,0.00029793073,0.004936112,0.0006511363,0.00009193061,0.0011556458,0.000004917508],"about_ca_topic_score_codex":0.11410217,"about_ca_topic_score_gemma":0.16691132,"teacher_disagreement_score":0.11410217,"about_ca_system_score_codex":0.0005597768,"about_ca_system_score_gemma":0.0004832775,"threshold_uncertainty_score":0.22687608},"labels":[],"label_agreement":null},{"id":"W2019090568","doi":"10.1029/2009gl038462","title":"Coupled chemistry climate model simulations of stratospheric temperatures and their trends for the recent past","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; York University","funders":"Economic and Social Research Council; European Centre for Medium-Range Weather Forecasts; Natural Environment Research Council; Sight Research UK","keywords":"Radiosonde; Stratosphere; Climatology; Environmental science; Troposphere; Atmospheric sciences; Climate model; Volcano; Range (aeronautics); Meteorology; Climate change; Geology; Geography","score_opus":0.030123363427633325,"score_gpt":0.29127810441158825,"score_spread":0.2611547409839549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019090568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873568,0.00022888392,0.0043008868,0.00047946922,0.00006261636,0.00003055079,0.003172597,0.00023043348,0.0041377023],"genre_scores_gemma":[0.9949523,0.00014938622,0.0019671875,0.00005443856,0.000017470973,0.000050598017,0.0016074551,0.000033965727,0.0011673403],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998493,0.00004114101,0.000010456721,0.000048092843,0.00002160359,0.000029349989],"domain_scores_gemma":[0.99951744,0.00022717871,0.00006520055,0.000036740425,0.000089462694,0.000064039785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00069841766,0.00063991675,0.0005157278,0.0005129143,0.00058374985,0.00075931085,0.0010531272,0.0011125416,0.0021567775],"category_scores_gemma":[0.0015465999,0.0005745871,0.0008750148,0.0011261641,0.00041924886,0.0009906797,0.00044306894,0.00070877216,0.0002683334],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096856136,0.00003936117,0.004559716,0.000016418991,0.00005910818,0.000017460618,0.000021920016,0.9925464,0.00050819165,0.00064206036,0.00033148134,0.0011609907],"study_design_scores_gemma":[0.00008123809,0.0000380659,0.0042872117,0.0000026215998,0.00003962023,0.000007624712,0.000017460363,0.99417937,0.0003432868,0.0005990958,0.00038846923,0.000015812531],"about_ca_topic_score_codex":0.07928153,"about_ca_topic_score_gemma":0.0521337,"teacher_disagreement_score":0.07928153,"about_ca_system_score_codex":0.0020832126,"about_ca_system_score_gemma":0.0012966675,"threshold_uncertainty_score":0.15764016},"labels":[],"label_agreement":null},{"id":"W2019139653","doi":"10.1029/2006gl029016","title":"Recent trends in Arctic Ocean mass distribution revealed by GRACE","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Anticyclone; Arctic; Climatology; Oceanography; Geology; The arctic; Structural basin; Canada Basin; Water mass; Spatial distribution; Environmental science; Geomorphology; Remote sensing","score_opus":0.02098681413918662,"score_gpt":0.29850737292349755,"score_spread":0.2775205587843109,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019139653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958533,0.00027857858,0.00022554172,0.00028306086,0.000017245526,0.0000021043302,0.0015393047,0.000026691145,0.0017742373],"genre_scores_gemma":[0.9966106,0.0003791029,0.0002927313,0.00005144446,0.000041419335,0.000003318969,0.0021431902,0.000006471373,0.00047178814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000008784831,0.000011566587,0.000022049688,0.000022606144,0.000020959089],"domain_scores_gemma":[0.9993704,0.00005065943,0.00025397155,0.000037087557,0.00022923987,0.00005865779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030982762,0.00011225422,0.00010935081,0.0008335487,0.00018480765,0.0004131558,0.00013894554,0.00023439022,0.00073193153],"category_scores_gemma":[0.00096286356,0.00007955071,0.00011628414,0.0010374903,0.0001908108,0.00036251816,0.00022536048,0.0002409,0.0002216331],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003421094,0.00003788718,0.96878237,0.000037567148,0.00008164369,0.00010784956,0.00039423158,0.0007207594,0.0067997267,0.00043545713,0.0012565755,0.021003662],"study_design_scores_gemma":[0.0000029296252,0.00004096182,0.9944981,0.000004759339,0.00001958077,0.00009568025,0.00013816681,0.00056491175,0.0010828576,0.00007192274,0.0034746462,0.000005511728],"about_ca_topic_score_codex":0.009294641,"about_ca_topic_score_gemma":0.015583779,"teacher_disagreement_score":0.009294641,"about_ca_system_score_codex":0.00036029454,"about_ca_system_score_gemma":0.00017351701,"threshold_uncertainty_score":0.018481076},"labels":[],"label_agreement":null},{"id":"W2019412579","doi":"10.1029/2006gl026916","title":"Estimating drift velocity of polar cap patches with all‐sky airglow imager at Resolute Bay, Canada","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Airglow; Polar; Sky; Latitude; Geodesy; Physics; Geology; Magnitude (astronomy); Bay; Drift velocity; Atmospheric sciences; Astrophysics; Astronomy; Plasma","score_opus":0.008848991188378496,"score_gpt":0.242696928726447,"score_spread":0.23384793753806848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2019412579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98957705,0.0002761526,0.0030674129,0.000033534005,0.000016093565,0.000050041817,0.0035999303,0.0003678502,0.0030119347],"genre_scores_gemma":[0.98441166,0.0001781582,0.009219524,0.000013455251,0.000009754702,0.000018029617,0.004389325,0.00006390604,0.0016961846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998666,0.000004479146,0.0000026040782,0.00003073378,0.0000559138,0.00003967647],"domain_scores_gemma":[0.99968874,0.00001770512,0.000032283624,0.000022494654,0.00018168936,0.000057002704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016279337,0.00038337422,0.00032585463,0.0017136894,0.00052929483,0.000518101,0.0005605232,0.00021274653,0.0013259781],"category_scores_gemma":[0.0004970602,0.0002343585,0.000177507,0.0010553045,0.00014322996,0.00020466726,0.00028475214,0.000242068,0.0004399979],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007714941,0.00014111897,0.70432806,0.00014528025,0.00027472893,0.0005362203,0.00080781674,0.010675336,0.16664906,0.00040157602,0.0087706335,0.106498696],"study_design_scores_gemma":[0.00002064408,0.00001964692,0.96539956,0.0000103730445,0.000030203795,0.00007826233,0.00016426978,0.02410825,0.008481025,0.000033330456,0.0016365495,0.00001791879],"about_ca_topic_score_codex":0.6998454,"about_ca_topic_score_gemma":0.8381559,"teacher_disagreement_score":0.30015463,"about_ca_system_score_codex":0.0015680067,"about_ca_system_score_gemma":0.001643444,"threshold_uncertainty_score":0.6038446},"labels":[],"label_agreement":null},{"id":"W2020340643","doi":"10.1029/2006gl027029","title":"Rise and decline of active chlorine in the stratosphere","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research; National Aeronautics and Space Administration","keywords":"Stratosphere; Chlorofluorocarbon; Montreal Protocol; Chlorine; Ozone layer; Troposphere; Environmental science; Atmospheric sciences; Ozone; Ozone depletion; Methane; Climatology; Meteorology; Chemistry; Geography; Geology","score_opus":0.02272263270379454,"score_gpt":0.28100867801872437,"score_spread":0.2582860453149298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020340643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967399,0.0005552064,0.00012265921,0.00018680263,0.0000073178535,0.0000031346449,0.00042266163,0.00001813675,0.00194412],"genre_scores_gemma":[0.99875486,0.00015274528,0.00008755594,0.000051099574,0.000009127541,0.0000023422917,0.000327824,0.0000025890681,0.0006117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989533,0.000007861889,0.0000062037752,0.000032547894,0.000024361607,0.000033743872],"domain_scores_gemma":[0.99957937,0.000032608372,0.00010049673,0.000026629665,0.00019374372,0.000067165805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023926469,0.000112064816,0.00012792923,0.0006234742,0.00029215866,0.00063739135,0.00020100838,0.00044323684,0.0008207385],"category_scores_gemma":[0.0006389621,0.00010734362,0.00014813649,0.00046829818,0.0002797449,0.0004366831,0.00029835443,0.00041027827,0.00016874894],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036427032,0.000055193155,0.9359075,0.000053740536,0.00007735405,0.0003312376,0.00088129216,0.00036334153,0.037203837,0.0005932739,0.00093863124,0.023230407],"study_design_scores_gemma":[0.000002365083,0.00004071375,0.996648,0.0000041235626,0.000009445718,0.00006124782,0.00016221715,0.00012215784,0.0015026769,0.00004011558,0.0014035297,0.0000034841307],"about_ca_topic_score_codex":0.030084783,"about_ca_topic_score_gemma":0.019308845,"teacher_disagreement_score":0.030084783,"about_ca_system_score_codex":0.00079576444,"about_ca_system_score_gemma":0.00047016918,"threshold_uncertainty_score":0.05981934},"labels":[],"label_agreement":null},{"id":"W2020351800","doi":"10.1029/2006gl028540","title":"Ventilation of the Upper Labrador Sea Water, 2003–2005","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Dartmouth College","keywords":"Hydrography; Geology; Salinity; Water mass; Oceanography; Structural basin; Climatology; Potential temperature; Geomorphology","score_opus":0.01818154664448269,"score_gpt":0.2632038761544616,"score_spread":0.24502232950997893,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020351800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934471,0.0003764898,0.000117795425,0.00008842525,0.0000069860835,0.000008720462,0.003615619,0.000050973107,0.0022877788],"genre_scores_gemma":[0.9942987,0.00016390787,0.000219936,0.00006342262,0.0000072206794,0.000012683158,0.003951655,0.000010895468,0.0012715338],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975914,0.000022975932,0.00002631306,0.0000664247,0.00004966115,0.00007545569],"domain_scores_gemma":[0.9997774,0.000013624207,0.00009763855,0.000016867956,0.000064627464,0.000029903034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030107785,0.0003490364,0.0002241292,0.0006181449,0.00038114437,0.0010923829,0.000374529,0.00017343496,0.0009909968],"category_scores_gemma":[0.0005756782,0.000114268405,0.00022666961,0.0011657259,0.0001983326,0.00047666396,0.00045708037,0.00020732528,0.00032334184],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010412056,0.000104844104,0.8991866,0.00025777816,0.00025021794,0.00038193105,0.0014582624,0.0029622768,0.009827022,0.00026628142,0.005717643,0.07854598],"study_design_scores_gemma":[0.000005470723,0.000032064607,0.9930952,0.000011267668,0.000015810525,0.000046813195,0.00031117722,0.0005847538,0.0019260639,0.0000127749445,0.0039509903,0.000007632735],"about_ca_topic_score_codex":0.22701934,"about_ca_topic_score_gemma":0.31984717,"teacher_disagreement_score":0.7729807,"about_ca_system_score_codex":0.0028927813,"about_ca_system_score_gemma":0.0010189853,"threshold_uncertainty_score":0.45139587},"labels":[],"label_agreement":null},{"id":"W2020359576","doi":"10.1029/2003gl017022","title":"Lithospheric thickness inferred from Australian post‐glacial sea‐level change: The influence of a ductile crustal zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Lithosphere; Geology; Crust; Glacial period; Post-glacial rebound; Sea level; Geophysics; Seismology; Geomorphology; Oceanography; Tectonics","score_opus":0.07378921795161288,"score_gpt":0.3029481083420827,"score_spread":0.22915889039046983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020359576","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99893564,0.00003572625,0.00033612832,0.00008650343,0.000002164514,0.0000017464095,0.000062494015,0.000016293772,0.00052336405],"genre_scores_gemma":[0.9997818,0.000020280284,0.000087739376,0.0000068578106,7.6724143e-7,0.0000010356185,0.000036541853,0.0000022519532,0.0000627562],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99983835,0.000055899367,0.000011280116,0.000033320484,0.000024692092,0.000036433466],"domain_scores_gemma":[0.99943334,0.00022139671,0.00010017624,0.00006804307,0.000102239566,0.000074723845],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062946934,0.00033293833,0.00025411398,0.00039224923,0.0003765718,0.0009760565,0.0007570606,0.0007070731,0.0007470335],"category_scores_gemma":[0.003228029,0.00055812445,0.00046293862,0.0003550429,0.00065251236,0.00049372355,0.0008018891,0.00042325587,0.00013943888],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023230528,0.000053360094,0.30418584,0.00006298104,0.00012905849,0.0002649653,0.00034217667,0.68143255,0.006656131,0.001321344,0.00024193183,0.0050773565],"study_design_scores_gemma":[0.00006588358,0.00011960859,0.21266854,0.000021353517,0.00007465409,0.00006194859,0.00019173883,0.78388673,0.0017398882,0.0008040191,0.00033410997,0.00003150132],"about_ca_topic_score_codex":0.080173224,"about_ca_topic_score_gemma":0.040011305,"teacher_disagreement_score":0.080173224,"about_ca_system_score_codex":0.001411393,"about_ca_system_score_gemma":0.0007414246,"threshold_uncertainty_score":0.1594131},"labels":[],"label_agreement":null},{"id":"W2020616811","doi":"10.1029/2003gl019060","title":"Can aerosols spin down the water cycle in a warmer and moister world?","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":258,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Environmental science; Atmospheric sciences; Longwave; Radiative forcing; Aerosol; Climatology; Water cycle; Greenhouse gas; Climate model; Sensible heat; Atmosphere (unit); Forcing (mathematics); Liquid water path; Precipitation; Radiative transfer; Climate change; Meteorology; Physics; Geology","score_opus":0.015962085957645564,"score_gpt":0.27751859298728404,"score_spread":0.26155650702963845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2020616811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9269028,0.013008671,0.000800843,0.047123946,0.0011522395,0.000011078838,0.00045106577,0.000052062944,0.010497235],"genre_scores_gemma":[0.99382424,0.0024559528,0.00012814942,0.002558987,0.00041521128,0.000002530165,0.000048019156,0.0000092103355,0.0005576884],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986875,0.000026592246,0.0000062103704,0.00003399241,0.000017440052,0.00004703052],"domain_scores_gemma":[0.9996284,0.00006302917,0.00012004167,0.000037771057,0.000040748826,0.00010995397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042401103,0.00018366176,0.00031116948,0.00032094354,0.0005852152,0.001610963,0.00022658361,0.0009649359,0.002060198],"category_scores_gemma":[0.001892988,0.00015881799,0.0002587013,0.00044799648,0.0014592564,0.003657903,0.0007280178,0.0006517253,0.00031258244],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001076498,0.00016970799,0.7473041,0.00049112015,0.00086904864,0.0015131932,0.004171652,0.003057473,0.015796717,0.050493173,0.019080637,0.15597671],"study_design_scores_gemma":[0.00012234808,0.00018216654,0.8620702,0.00015417147,0.00027314873,0.0002915364,0.0061827768,0.0025112408,0.002248665,0.086270995,0.039608873,0.00008378609],"about_ca_topic_score_codex":0.0078288345,"about_ca_topic_score_gemma":0.013970823,"teacher_disagreement_score":0.0078288345,"about_ca_system_score_codex":0.00053114427,"about_ca_system_score_gemma":0.0003639735,"threshold_uncertainty_score":0.015566528},"labels":[],"label_agreement":null},{"id":"W2021042766","doi":"10.1029/2009gl037246","title":"Sensitivity of climate to dynamically‐consistent zonal asymmetries in ozone","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Ozone; Atmospheric sciences; Stratosphere; Environmental science; Climatology; Ozone layer; Geopotential height; Atmospheric model; Radiative transfer; Atmosphere (unit); Ozone depletion; Meteorology; Geology; Physics; Precipitation","score_opus":0.022600355641330547,"score_gpt":0.2870525165178027,"score_spread":0.26445216087647216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021042766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971386,0.00006460939,0.0009766992,0.00016429846,0.000027150189,0.000012622158,0.0003770112,0.00006892262,0.0011701543],"genre_scores_gemma":[0.99952734,0.000035118435,0.00016601951,0.000027817501,0.0000032710593,0.0000052385603,0.00016630889,0.00001357927,0.000055382734],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99967885,0.00011492577,0.000021603346,0.00006773149,0.00003609223,0.0000808344],"domain_scores_gemma":[0.9986552,0.0007116374,0.00015704651,0.00019166306,0.00016424073,0.00012012763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008451737,0.0003983019,0.00042743504,0.0002840412,0.00054726563,0.0010180838,0.0005564841,0.0008088478,0.0008268227],"category_scores_gemma":[0.0055312156,0.00039498904,0.0006451661,0.0003421321,0.00062281964,0.0006338116,0.0007366349,0.0007293212,0.0000844772],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004882728,0.000098751385,0.07973635,0.00006072957,0.0003251524,0.00015274069,0.0001132,0.8937779,0.020050593,0.0017823805,0.00054962636,0.0028642488],"study_design_scores_gemma":[0.00020431586,0.00017103885,0.07637375,0.000017156659,0.00013090325,0.000047937545,0.00012435844,0.91097724,0.009812443,0.0012410401,0.0008279426,0.00007193005],"about_ca_topic_score_codex":0.06667074,"about_ca_topic_score_gemma":0.028219828,"teacher_disagreement_score":0.06667074,"about_ca_system_score_codex":0.0015044807,"about_ca_system_score_gemma":0.00096290954,"threshold_uncertainty_score":0.13256538},"labels":[],"label_agreement":null},{"id":"W2021694292","doi":"10.1002/2014gl060329","title":"High manganese concentrations in rocks at Gale crater, Mars","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Brock University; University of Guelph","funders":"Centre National d’Etudes Spatiales; National Aeronautics and Space Administration","keywords":"Manganese; Mars Exploration Program; Oxidizing agent; Geology; Redox; Martian; Impact crater; Martian surface; FERRIC IRON; Basalt; Astrobiology; Geochemistry; Mineralogy; Chemistry; Inorganic chemistry; Ferrous","score_opus":0.025188501013244765,"score_gpt":0.2823886449581984,"score_spread":0.2572001439449536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021694292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999057,0.00011747744,0.00004114673,0.000029646686,0.000003513297,0.0000033302908,0.00018545867,0.000013583912,0.000548925],"genre_scores_gemma":[0.9994624,0.00005510466,0.00007609354,0.00000854347,0.0000060069156,0.0000020239909,0.0001350991,0.000003079679,0.0002516283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998826,0.000011244622,0.0000058239557,0.00003621424,0.000038750706,0.000025408826],"domain_scores_gemma":[0.9998847,0.000013871057,0.000029217115,0.0000068705426,0.000036358866,0.000028984412],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011400991,0.00037528097,0.00029549358,0.0023127,0.0011273399,0.00097518455,0.0004266792,0.0006390008,0.0011166029],"category_scores_gemma":[0.0002219522,0.0002561246,0.00020673625,0.0005658034,0.0006013182,0.00028525837,0.0006789594,0.00023867845,0.0002398366],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053025986,0.00005907885,0.8994536,0.00010569082,0.00020695213,0.0016151107,0.0019372549,0.00081956596,0.08671002,0.00019429991,0.00044290573,0.007925331],"study_design_scores_gemma":[0.000009742069,0.00004466278,0.99645364,0.00000789301,0.000013115,0.00021307073,0.000549507,0.0003177119,0.0015791577,0.00002878914,0.00077755103,0.000005060374],"about_ca_topic_score_codex":0.031526368,"about_ca_topic_score_gemma":0.035570092,"teacher_disagreement_score":0.031526368,"about_ca_system_score_codex":0.0007470837,"about_ca_system_score_gemma":0.00031589495,"threshold_uncertainty_score":0.06268573},"labels":[],"label_agreement":null},{"id":"W2021861597","doi":"10.1029/2004gl020093","title":"Long‐range transport of Siberian biomass burning emissions and impact on surface ozone in western North America","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":322,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Office of Naval Research; National Aeronautics and Space Administration; Harvard University; National Science Foundation","keywords":"Environmental science; Biomass burning; Air quality index; Ozone; Range (aeronautics); Atmospheric sciences; Aerosol; Climatology; Pollutant; Chemical transport model; Air pollution; Biomass (ecology); Meteorology; Geography; Oceanography; Geology","score_opus":0.023699484574839964,"score_gpt":0.28628901148675423,"score_spread":0.2625895269119143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2021861597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996728,0.00005347581,0.000019823507,0.000039340783,0.0000017998876,5.649836e-7,0.000056236087,0.000002705378,0.00015334284],"genre_scores_gemma":[0.9995414,0.000080604674,0.000041125593,0.00001437525,0.0000019477009,0.0000015422679,0.00016101397,0.0000013568657,0.00015679169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.000012568497,0.000003610601,0.000010053896,0.000007253984,0.000016164577],"domain_scores_gemma":[0.9998211,0.000035587822,0.000042410164,0.0000120152035,0.000033834003,0.000055033463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023739954,0.00021220036,0.00020061435,0.00029626087,0.00046753167,0.0005110481,0.000168913,0.00025364853,0.0010074923],"category_scores_gemma":[0.00041319497,0.00015417347,0.00023987936,0.00032162998,0.00017346755,0.00029568071,0.00049762195,0.0002390305,0.000115492796],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019300418,0.000082072234,0.9781994,0.000017860499,0.00014892177,0.00063266343,0.00029194276,0.009227665,0.005236081,0.00012306585,0.0002897239,0.0055573937],"study_design_scores_gemma":[0.000007229944,0.000027064021,0.99267334,0.00000813487,0.000031349304,0.000033913242,0.0002047162,0.00649882,0.0002934181,0.00006413754,0.00015328573,0.000004513325],"about_ca_topic_score_codex":0.13101381,"about_ca_topic_score_gemma":0.13175392,"teacher_disagreement_score":0.8689862,"about_ca_system_score_codex":0.0010949861,"about_ca_system_score_gemma":0.00055989076,"threshold_uncertainty_score":0.26050246},"labels":[],"label_agreement":null},{"id":"W2022103410","doi":"10.1029/2004gl021733","title":"Relative location of excavation induced microseismicity at the Underground Research Laboratory (AECL, Canada) using surveyed reference events","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Hypocenter; Geology; Excavation; Seismology; Context (archaeology); Relocation; Coalescence (physics); Induced seismicity; Magnitude (astronomy); Mining engineering; Geotechnical engineering; Computer science","score_opus":0.11474614684392669,"score_gpt":0.34369003324780245,"score_spread":0.22894388640387575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022103410","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941005,0.00007070064,0.0021616824,0.000020743057,0.0000033045596,0.000016968477,0.0008000217,0.00014864141,0.002677351],"genre_scores_gemma":[0.99766433,0.000030727686,0.0014312217,0.0000027438603,8.735505e-7,0.00000620362,0.00036310244,0.0000087044,0.0004921632],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974924,0.000011300235,0.0000068661598,0.000048272326,0.00011869008,0.00006554358],"domain_scores_gemma":[0.99950814,0.00003070103,0.00010776484,0.000037470116,0.00026329988,0.00005267157],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017970405,0.00016238997,0.00013927014,0.0014539466,0.00043940332,0.0004591365,0.0004983152,0.00027227998,0.0009703786],"category_scores_gemma":[0.0010139308,0.00010466058,0.00008706611,0.0012510855,0.0003258562,0.00021517498,0.0004577047,0.00022277035,0.00025063177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005916705,0.00016267784,0.73821986,0.00019054949,0.00005534085,0.0011401828,0.0034788956,0.023043552,0.11394804,0.0014666356,0.002480504,0.11522203],"study_design_scores_gemma":[0.00001626585,0.000089353816,0.96715105,0.000017968976,0.00001643052,0.00023487302,0.000822675,0.013855171,0.015431065,0.00009375101,0.0022430283,0.0000284135],"about_ca_topic_score_codex":0.2394727,"about_ca_topic_score_gemma":0.47989583,"teacher_disagreement_score":0.7605273,"about_ca_system_score_codex":0.0014164236,"about_ca_system_score_gemma":0.0014145687,"threshold_uncertainty_score":0.4761576},"labels":[],"label_agreement":null},{"id":"W2022331802","doi":"10.1029/1999gl011234","title":"Increased carbon sequestration by a boreal deciduous forest in years with a warm spring","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":338,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Forest Service; University of British Columbia","funders":"","keywords":"Carbon sequestration; Deciduous; Spring (device); Taiga; Environmental science; Boreal; Ecosystem; Carbon cycle; Carbon fibers; Photosynthesis; Boreal ecosystem; Atmospheric sciences; Forestry; Ecology; Carbon dioxide; Geology; Geography; Biology; Botany","score_opus":0.009468868262212958,"score_gpt":0.2382862293449051,"score_spread":0.22881736108269213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022331802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997242,0.000033614575,0.000012452954,0.000019864705,0.0000017803609,4.449018e-7,0.000038513183,0.0000016838171,0.00016730925],"genre_scores_gemma":[0.99966514,0.00004802514,0.00003484769,0.000020452811,0.0000018323582,7.957742e-7,0.00008157207,6.662373e-7,0.00014666472],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993443,0.000009140848,0.0000036315498,0.000014160945,0.0000066872944,0.000032015065],"domain_scores_gemma":[0.9998481,0.000013532244,0.00003385119,0.0000106465795,0.00002242421,0.0000713684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017578462,0.0001557398,0.00017070863,0.00017196249,0.00039704086,0.00038784015,0.00020219729,0.00023313452,0.0005698571],"category_scores_gemma":[0.00022655747,0.00007636782,0.00012593111,0.00022328158,0.00027242565,0.00017690363,0.0002525857,0.00017361382,0.00005207071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012176322,0.00016512258,0.86540216,0.0000467767,0.0001833136,0.00064905215,0.00034258206,0.0022569527,0.11346703,0.00034460414,0.0005825928,0.015342194],"study_design_scores_gemma":[0.000016900012,0.000042255735,0.99796057,0.0000029031044,0.000023243703,0.00008987636,0.0001856267,0.00043161976,0.0007802729,0.000062739324,0.0003986926,0.0000054378365],"about_ca_topic_score_codex":0.19565728,"about_ca_topic_score_gemma":0.5912991,"teacher_disagreement_score":0.19565728,"about_ca_system_score_codex":0.001733698,"about_ca_system_score_gemma":0.0015157892,"threshold_uncertainty_score":0.38903683},"labels":[],"label_agreement":null},{"id":"W2022440867","doi":"10.1029/2002gl016739","title":"Seasonal persistence of midlatitude total ozone anomalies","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Middle latitudes; Northern Hemisphere; Southern Hemisphere; Predictability; Climatology; Atmospheric sciences; Seasonality; Ozone; Ozone depletion; Environmental science; Latitude; Stratosphere; Geology; Meteorology; Geography; Biology","score_opus":0.038622402857150843,"score_gpt":0.27198146662035516,"score_spread":0.2333590637632043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022440867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989497,0.00007027717,0.00010001267,0.000031412543,0.0000025808233,0.0000011139124,0.00030028608,0.000011440191,0.00053331547],"genre_scores_gemma":[0.99942136,0.000022737588,0.000030713123,0.0000055396804,0.0000030051465,0.0000010800899,0.00038414792,0.0000018168026,0.00012963971],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999145,0.000006614929,0.0000073995566,0.000028993294,0.00001612449,0.000026331662],"domain_scores_gemma":[0.9993337,0.00012573479,0.00019858356,0.000073967014,0.0001620322,0.00010596296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024433274,0.0000604058,0.00016665262,0.00056912214,0.00020889267,0.00043382525,0.00014394808,0.0001634195,0.001206326],"category_scores_gemma":[0.0009696901,0.000113457674,0.00012633813,0.0004605396,0.00014125071,0.00021120442,0.00022045455,0.0002303066,0.0002151842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016860868,0.00003439818,0.98022735,0.000016356153,0.000045160097,0.00009961725,0.00030408578,0.0004616434,0.009317169,0.00024105136,0.00036948995,0.008715179],"study_design_scores_gemma":[0.0000014851421,0.000013125365,0.9989354,0.0000019143215,0.0000054757465,0.000040041272,0.000051101648,0.0003511366,0.00027767153,0.000047141737,0.00027352624,0.0000020118612],"about_ca_topic_score_codex":0.009291775,"about_ca_topic_score_gemma":0.013150071,"teacher_disagreement_score":0.009291775,"about_ca_system_score_codex":0.0002275186,"about_ca_system_score_gemma":0.00017811006,"threshold_uncertainty_score":0.018475354},"labels":[],"label_agreement":null},{"id":"W2022585183","doi":"10.1029/2000gl011978","title":"A regional study of shear wave splitting above the Cascadia Subduction Zone: Margin‐parallel crustal stress","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Shear wave splitting; Shear (geology); Anisotropy; Borehole; Geophysics; Petrology; Tectonics; Geotechnical engineering","score_opus":0.06462835755179935,"score_gpt":0.2963087153510412,"score_spread":0.23168035779924184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022585183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969745,0.000016985396,0.000021084046,0.000004623902,2.602487e-7,0.0000013374136,0.000059918744,0.0000014557012,0.00019683319],"genre_scores_gemma":[0.9995276,0.00003975295,0.000064456835,0.0000021971564,0.0000010774257,0.0000025849945,0.00016626864,0.0000011607154,0.00019498558],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999112,0.000008696649,0.0000043395435,0.00003119291,0.000015560094,0.000028992172],"domain_scores_gemma":[0.99964416,0.000032060358,0.00009936645,0.000035730118,0.00010493207,0.00008362668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011413511,0.00024410337,0.00016630878,0.00070661906,0.0004177329,0.0003024173,0.00014509546,0.0001500626,0.00059953897],"category_scores_gemma":[0.0004708857,0.00020461359,0.0001404674,0.0008711499,0.00028490368,0.00018747181,0.00029377308,0.00016603229,0.00016067844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022513304,0.000045831606,0.9642713,0.000022988506,0.00007315095,0.0004389528,0.001664584,0.00033979263,0.025031544,0.00005920623,0.00013895732,0.007688493],"study_design_scores_gemma":[0.0000016251007,0.000015187694,0.999246,0.0000012261195,0.0000075681846,0.00007518307,0.00023797732,0.00007276618,0.00021762248,0.0000046695695,0.000118560885,0.0000017131123],"about_ca_topic_score_codex":0.12039479,"about_ca_topic_score_gemma":0.22788145,"teacher_disagreement_score":0.12039479,"about_ca_system_score_codex":0.00069980416,"about_ca_system_score_gemma":0.00045116243,"threshold_uncertainty_score":0.23938805},"labels":[],"label_agreement":null},{"id":"W2022703777","doi":"10.1029/2002gl015822","title":"Tropical links of the Arctic Oscillation","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; McGill University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Forcing (mathematics); Extratropical cyclone; Climatology; Diabatic; Environmental science; Atmospheric sciences; Arctic oscillation; Oscillation (cell signaling); Tropics; The arctic; Madden–Julian oscillation; Meteorology; Geology; Geography; Northern Hemisphere; Physics; Chemistry; Oceanography; Convection; Biology","score_opus":0.05614987675443547,"score_gpt":0.29493693193441445,"score_spread":0.23878705517997897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022703777","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89246523,0.0011873019,0.015740473,0.0007110651,0.00016961193,0.000057738765,0.01294639,0.00045588723,0.07626642],"genre_scores_gemma":[0.9901951,0.0006094619,0.0035234406,0.000061011353,0.000029628634,0.00003453996,0.0026123053,0.000068044836,0.0028664374],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999248,0.00001851817,0.00000454236,0.000019841043,0.000015765721,0.000016620872],"domain_scores_gemma":[0.9998528,0.00003401149,0.000034358527,0.000022737511,0.00002925597,0.00002689735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014691422,0.00018182037,0.00020929398,0.00026660113,0.0003362282,0.00089619745,0.0002668259,0.00019274121,0.0042406064],"category_scores_gemma":[0.00072755764,0.00014640503,0.00024150641,0.0006390657,0.0001384463,0.00049316435,0.0005329748,0.0003711223,0.0003534142],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051132846,0.00013259074,0.22581038,0.00025081905,0.00033963288,0.00047633395,0.0004896832,0.599348,0.009722279,0.075879574,0.017566657,0.06947279],"study_design_scores_gemma":[0.0002261807,0.00012125612,0.16739151,0.00006205057,0.00020203812,0.00028995602,0.0002727798,0.7415081,0.002767504,0.026757421,0.060335156,0.00006601615],"about_ca_topic_score_codex":0.015075374,"about_ca_topic_score_gemma":0.01620868,"teacher_disagreement_score":0.015075374,"about_ca_system_score_codex":0.0003565229,"about_ca_system_score_gemma":0.0006643672,"threshold_uncertainty_score":0.029975295},"labels":[],"label_agreement":null},{"id":"W2022766712","doi":"10.1029/2004gl022007","title":"The effect of ocean mixing parametrisation on the enhanced CO<sub>2</sub> response of the Southern Hemisphere midlatitude jet","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Middle latitudes; Southern Hemisphere; Climatology; Troposphere; Environmental science; Northern Hemisphere; Jet (fluid); Atmospheric sciences; Climate model; Mixing (physics); Jet stream; Geology; Climate change; Physics; Oceanography; Mechanics","score_opus":0.01963198214520813,"score_gpt":0.2871378720603253,"score_spread":0.2675058899151172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022766712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960334,0.000112048656,0.0019061764,0.00018792877,0.000027364098,0.000011328131,0.00014338021,0.00009578346,0.0014826251],"genre_scores_gemma":[0.9988182,0.000055672233,0.0007861731,0.000043166223,0.0000070034057,0.000010220105,0.00008083277,0.000027117188,0.00017140961],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99977213,0.000105987914,0.000023823151,0.00003556328,0.00002648475,0.000036081794],"domain_scores_gemma":[0.99837863,0.0010272906,0.00018842627,0.0002669599,0.00007377436,0.00006493177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007117046,0.00059787586,0.00032127264,0.0002342372,0.0002821403,0.0009574267,0.00052445085,0.00068000134,0.0014221179],"category_scores_gemma":[0.003853626,0.0003642682,0.000604313,0.00032854822,0.00048692402,0.00078867876,0.0006773143,0.0010991049,0.00013089592],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012991237,0.00018856487,0.057907324,0.00012550603,0.00030997046,0.00028633073,0.00021282048,0.87202793,0.05737329,0.0017376951,0.00047545697,0.00805601],"study_design_scores_gemma":[0.00043655752,0.0006752188,0.06160687,0.0000413172,0.0003424273,0.00010770103,0.0002308778,0.8923045,0.04184203,0.00078792265,0.001549364,0.00007512092],"about_ca_topic_score_codex":0.010719612,"about_ca_topic_score_gemma":0.007766182,"teacher_disagreement_score":0.010719612,"about_ca_system_score_codex":0.00042840012,"about_ca_system_score_gemma":0.00031210124,"threshold_uncertainty_score":0.021314383},"labels":[],"label_agreement":null},{"id":"W2022853824","doi":"10.1029/2007gl032122","title":"Do stable atmospheric layers exist?","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"National Oceanic and Atmospheric Administration","keywords":"Scaling; Hierarchy; Stability (learning theory); Statistical physics; Fractal; Atmospheric instability; Idealization; Convection; Atmospheric dynamics; Physics; Theoretical physics; Mechanics; Meteorology; Classical mechanics; Mathematics; Mathematical analysis; Computer science; Atmosphere (unit); Geometry","score_opus":0.06525509134806311,"score_gpt":0.3126413737687815,"score_spread":0.24738628242071836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2022853824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81860524,0.016118353,0.051052522,0.011702299,0.00044453252,0.00003828329,0.0008244057,0.00028813703,0.10092629],"genre_scores_gemma":[0.9944424,0.0012211853,0.0024206047,0.00034474724,0.00016072251,0.000012849435,0.00012181814,0.000021319349,0.0012542715],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9994936,0.00010304667,0.000031180214,0.00017033001,0.00008639622,0.000115459414],"domain_scores_gemma":[0.99685895,0.0015683807,0.00054361305,0.00035046606,0.0002935673,0.00038497092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013005642,0.00021562271,0.00044748667,0.00076357025,0.0009952944,0.0024456843,0.00048822927,0.0013109997,0.004837883],"category_scores_gemma":[0.0069258953,0.00033522004,0.00033230727,0.0006152499,0.0029043467,0.005982065,0.0012875666,0.0007756552,0.0006667338],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000194303,0.000031629683,0.024886776,0.0003019261,0.000072888644,0.0002790792,0.0015951751,0.0018887029,0.0035399063,0.91845304,0.004374627,0.04438192],"study_design_scores_gemma":[0.000032060823,0.000034098666,0.017802967,0.00006994678,0.000037927195,0.00024464354,0.0012619253,0.005495542,0.0010218583,0.95709383,0.016875986,0.00002929649],"about_ca_topic_score_codex":0.0009433707,"about_ca_topic_score_gemma":0.0006349776,"teacher_disagreement_score":0.004837883,"about_ca_system_score_codex":0.0005776211,"about_ca_system_score_gemma":0.00028464818,"threshold_uncertainty_score":0.01618427},"labels":[],"label_agreement":null},{"id":"W2023026126","doi":"10.1029/1999gl002399","title":"Multi‐year meanders and eddies in the Alaskan Stream as observed by TOPEX/Poseidon altimeter","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Eddy; Altimeter; Gulf Stream; Geology; Anticyclone; Satellite altimetry; Meander (mathematics); Sea-surface height; Oceanography; Current (fluid); Climatology; Geodesy; Geography; Meteorology","score_opus":0.035898677833551336,"score_gpt":0.2697397103123236,"score_spread":0.23384103247877225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023026126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953604,0.000054442484,0.000036468224,0.0000058028745,0.000002462266,8.7565024e-7,0.00016577684,0.0000032901569,0.00019478929],"genre_scores_gemma":[0.99898535,0.00010432198,0.00021474468,0.0000060624716,0.0000050718713,0.0000030418707,0.0004348433,0.0000010215095,0.00024548106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995124,0.0000047242784,0.00000468009,0.000017955426,0.00001090982,0.000010454297],"domain_scores_gemma":[0.99981564,0.00002958342,0.000058103265,0.000009159894,0.000033045584,0.000054614055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019968094,0.00016348528,0.00010693732,0.0005436051,0.0003071378,0.00029456115,0.000094963514,0.00018617391,0.00043274488],"category_scores_gemma":[0.0002833874,0.0001296877,0.00009833711,0.00030108876,0.00014262837,0.00029779857,0.00027651543,0.00013630031,0.00007473276],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008586921,0.000031126146,0.98907954,0.000010553439,0.000023313118,0.0001787969,0.00027079863,0.00051715213,0.0035065054,0.00003532097,0.00020795308,0.0060530496],"study_design_scores_gemma":[0.0000022419226,0.00002308011,0.99832505,0.0000035128803,0.00000872018,0.000084737556,0.00015728622,0.00075802347,0.00038206854,0.000010405442,0.00024217604,0.0000025552285],"about_ca_topic_score_codex":0.014050509,"about_ca_topic_score_gemma":0.035830174,"teacher_disagreement_score":0.014050509,"about_ca_system_score_codex":0.0003127884,"about_ca_system_score_gemma":0.0001410417,"threshold_uncertainty_score":0.027937472},"labels":[],"label_agreement":null},{"id":"W2023092140","doi":"10.1029/2001gl013947","title":"Mantle flow modeling of the anomalous subsidence of the Silurian Baltic Basin","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Mantle (geology); Baltica; Geophysics; Foreland basin; Mantle convection; Trench; Mantle wedge; Slab; Structural basin; Petrology; Seismology; Paleontology; Ordovician; Tectonics","score_opus":0.04138469514694683,"score_gpt":0.23690491054754317,"score_spread":0.19552021540059633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023092140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951592,0.000079419115,0.0014101386,0.0001638257,0.0000089725545,0.0000060965526,0.00016125581,0.00007130546,0.002939699],"genre_scores_gemma":[0.99869066,0.00004606446,0.00059773034,0.0000148712725,0.000004893943,0.0000059572712,0.00012444702,0.0000122233405,0.000503158],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999645,0.0000107117085,0.000002110206,0.000007997796,0.0000043163845,0.000010322483],"domain_scores_gemma":[0.99990034,0.000037490216,0.000014810234,0.000007494954,0.000020401647,0.000019469355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017878164,0.00031233698,0.0002315866,0.0003604122,0.00039159355,0.00069476647,0.0006082936,0.0005336969,0.0016600024],"category_scores_gemma":[0.00061169756,0.00027393523,0.00031262895,0.00029621006,0.0004302106,0.00026713824,0.00033572214,0.00026750957,0.00009221399],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004556255,0.000027442782,0.0093496675,0.000010823065,0.000030724845,0.000068074776,0.00005198942,0.98612136,0.0013447043,0.0009517116,0.00017734006,0.0018206884],"study_design_scores_gemma":[0.000028659051,0.000011021927,0.0038431108,0.0000022987085,0.0000082666065,0.0000050965145,0.000019074902,0.9954621,0.00013523402,0.00029597664,0.00018564682,0.0000035573973],"about_ca_topic_score_codex":0.12419436,"about_ca_topic_score_gemma":0.08115546,"teacher_disagreement_score":0.12419436,"about_ca_system_score_codex":0.0012437665,"about_ca_system_score_gemma":0.0009429264,"threshold_uncertainty_score":0.24694294},"labels":[],"label_agreement":null},{"id":"W2023092830","doi":"10.1029/2006gl026704","title":"Accelerated melting of Himalayan snow and ice triggers pronounced changes in a valley peatland from northern India","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Peat; Snow; Monsoon; Physical geography; Glacial period; Snow line; Plateau (mathematics); Permafrost; Precipitation; Snowmelt; Climate change; Environmental science; Surface runoff; Geology; Climatology; Ecology; Geography; Oceanography; Geomorphology","score_opus":0.034372453156266025,"score_gpt":0.2777659713278368,"score_spread":0.2433935181715708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023092830","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997538,0.000011711316,0.000010555379,0.0000063240686,5.0044935e-7,4.849509e-7,0.000025110214,0.0000025783822,0.0001890208],"genre_scores_gemma":[0.99983215,0.000017182865,0.000019282623,0.0000048397683,0.0000011561887,7.113635e-7,0.00006228634,7.2050017e-7,0.00006160262],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995303,0.0000058690393,0.00000290518,0.000011555242,0.000008847342,0.00001787001],"domain_scores_gemma":[0.99988425,0.000017915243,0.00003232691,0.00001205655,0.000017191762,0.000036292124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007255898,0.000090286936,0.00010365515,0.00040882494,0.0004939109,0.0005735163,0.00013657924,0.00011587149,0.000499095],"category_scores_gemma":[0.00020377019,0.00009454922,0.00008393935,0.00041035473,0.00029280782,0.00014787076,0.0003394333,0.00015196462,0.00008130374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019332135,0.00004414996,0.92680043,0.00004269805,0.000048612546,0.0012956085,0.0027256662,0.00046813808,0.060801905,0.00015937038,0.00020266068,0.0072175353],"study_design_scores_gemma":[0.0000011193857,0.000010055025,0.99865216,0.0000013792387,0.000004682451,0.00013069161,0.00043067563,0.00010801988,0.000519325,0.000018823906,0.00012135461,0.000001702077],"about_ca_topic_score_codex":0.016689984,"about_ca_topic_score_gemma":0.031628266,"teacher_disagreement_score":0.016689984,"about_ca_system_score_codex":0.00033142173,"about_ca_system_score_gemma":0.00025806448,"threshold_uncertainty_score":0.03318566},"labels":[],"label_agreement":null},{"id":"W2023348588","doi":"10.1029/2009gl040389","title":"Measurement of crack‐face friction in collapsed weak snow layers","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"European Commission; University of Calgary","keywords":"Snowpack; Snow; Mechanics; Frictional coefficient; Debris; Shear (geology); Materials science; Friction coefficient; Drop (telecommunication); Coefficient of friction; Dynamical friction; Geotechnical engineering; Plane (geometry); Geology; Composite material; Geometry; Physics; Mathematics","score_opus":0.05961388843014044,"score_gpt":0.29069311798123176,"score_spread":0.23107922955109134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023348588","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99933016,0.0000487701,0.0004877257,0.0000015156119,0.0000012761758,0.0000036866145,0.0000304361,0.0000048336024,0.00009153364],"genre_scores_gemma":[0.9992787,0.00002853476,0.0004873551,0.0000026243226,0.0000013567769,0.0000030561944,0.00007626625,0.0000019303359,0.00012031113],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998753,0.00000859944,0.000005988898,0.000022518665,0.000042198586,0.000045361852],"domain_scores_gemma":[0.99963903,0.000085739295,0.00008349101,0.000029494704,0.00007295152,0.00008931203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014632869,0.0001620469,0.0002738172,0.00049032335,0.0003674002,0.000252345,0.00023583342,0.0002079971,0.0008724017],"category_scores_gemma":[0.00068442535,0.00018160293,0.00015213004,0.00018607508,0.00023310227,0.00027515605,0.00038560107,0.0002844846,0.00017075699],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005135536,0.000050171027,0.057574674,0.00006818179,0.000032040567,0.00020198747,0.00041847044,0.00069087546,0.9325535,0.00006499192,0.00004985214,0.00778162],"study_design_scores_gemma":[0.000031635776,0.0012732373,0.6908612,0.000021267428,0.000042624295,0.0005848588,0.00049215,0.014306425,0.29132023,0.00011841111,0.0009082809,0.000039641913],"about_ca_topic_score_codex":0.0026071426,"about_ca_topic_score_gemma":0.0029220602,"teacher_disagreement_score":0.0026071426,"about_ca_system_score_codex":0.00017862198,"about_ca_system_score_gemma":0.0001357835,"threshold_uncertainty_score":0.005183995},"labels":[],"label_agreement":null},{"id":"W2023368487","doi":"10.1029/2000gl011404","title":"Ozone destruction and production rates between spring and autumn in the Arctic stratosphere","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Stratosphere; Ozone; Atmospheric sciences; Arctic; Ozone depletion; Environmental science; Spring (device); The arctic; Climatology; Meteorology; Geography; Oceanography; Geology; Physics","score_opus":0.02923530005689135,"score_gpt":0.27910758318842716,"score_spread":0.2498722831315358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2023368487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996314,0.00005346019,0.00006552385,0.0000069274097,7.516832e-7,5.050491e-7,0.00011090876,0.0000055346018,0.00012499384],"genre_scores_gemma":[0.9991203,0.00004942424,0.00006865811,0.0000040897244,0.0000016155557,0.0000020686675,0.00049591286,0.0000027243414,0.00025517686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.00000781389,0.0000026986318,0.000013122694,0.0000096051,0.000020341833],"domain_scores_gemma":[0.9997392,0.00008642042,0.00007000267,0.000016205504,0.000040902858,0.000047243968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002518633,0.00018372116,0.0001265571,0.0003904451,0.00021610082,0.00032119668,0.00013298677,0.00020902336,0.0003976562],"category_scores_gemma":[0.00046034032,0.00014886899,0.00016211427,0.00020265009,0.00012773176,0.00016604006,0.00013700472,0.00018544115,0.00011147723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090708374,0.000064084365,0.9513794,0.000024648498,0.00009054727,0.00013840373,0.0005222899,0.002019384,0.037003953,0.000110968445,0.00020929136,0.007530043],"study_design_scores_gemma":[0.000003934803,0.00004005198,0.9971207,0.0000015530563,0.000011622601,0.00004508287,0.000062610176,0.0010564275,0.0014714479,0.000019099249,0.00016470245,0.0000026701891],"about_ca_topic_score_codex":0.012253694,"about_ca_topic_score_gemma":0.014055254,"teacher_disagreement_score":0.012253694,"about_ca_system_score_codex":0.00034027942,"about_ca_system_score_gemma":0.00012141945,"threshold_uncertainty_score":0.02436477},"labels":[],"label_agreement":null},{"id":"W2024060325","doi":"10.1002/2014gl059940","title":"What causes the location of the air‐sea turbulent heat flux maximum over the Labrador Sea?","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Seventh Framework Programme; Natural Sciences and Engineering Research Council of Canada; European Commission; National Oceanic and Atmospheric Administration; Sight Research UK; National Aeronautics and Space Administration; National Science Foundation","keywords":"Heat flux; Geology; Climatology; Convection; Flux (metallurgy); Buoyancy; Sea ice; Atmospheric sciences; Oceanography; Heat transfer; Meteorology; Geography; Mechanics","score_opus":0.017102044396840946,"score_gpt":0.25280526588728863,"score_spread":0.2357032214904477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024060325","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988777,0.000087446366,0.00004555265,0.00011821512,0.0000041648045,0.0000019510294,0.00011458895,0.000007105208,0.0007432417],"genre_scores_gemma":[0.9997938,0.00003058267,0.000020519157,0.00001019553,0.000006448523,8.960416e-7,0.00004824332,0.0000020161995,0.00008721503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998698,0.000025111214,0.00000810625,0.0000277631,0.000011067722,0.00005814006],"domain_scores_gemma":[0.99951863,0.00008127469,0.00023495416,0.000023677447,0.00007638648,0.00006507136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020237666,0.00012223193,0.00022287511,0.00070621475,0.00044694293,0.0007950603,0.00024665322,0.00030845864,0.0019301194],"category_scores_gemma":[0.000802306,0.00010639569,0.0002424045,0.0007066399,0.00041820187,0.00032885093,0.00035060887,0.00019656874,0.000211888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014196149,0.00002544443,0.99084795,0.000021192673,0.000051477058,0.00026950476,0.00017179079,0.0007895268,0.003261341,0.00013003845,0.00031378938,0.0039759846],"study_design_scores_gemma":[0.0000026760433,0.000011762167,0.9985304,0.000006168423,0.000012924079,0.000030249272,0.00046224898,0.00040120215,0.00031335687,0.000034868965,0.0001905433,0.0000036065567],"about_ca_topic_score_codex":0.05624633,"about_ca_topic_score_gemma":0.06657197,"teacher_disagreement_score":0.94375366,"about_ca_system_score_codex":0.00082947145,"about_ca_system_score_gemma":0.00042007194,"threshold_uncertainty_score":0.11183792},"labels":[],"label_agreement":null},{"id":"W2024212629","doi":"10.1029/2005gl024779","title":"Inertial Alfvén waves and acceleration of electrons in nonuniform magnetic fields","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Physics; Acceleration; Electron; Magnetic field; Computational physics; Alfvén wave; Particle acceleration; Pulse (music); Field line; Classical mechanics; Optics; Magnetohydrodynamics; Quantum mechanics","score_opus":0.009690657444722129,"score_gpt":0.26403718461309167,"score_spread":0.25434652716836953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024212629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941208,0.00004558505,0.00319261,0.000094368064,0.00001308134,0.000011855358,0.000048691727,0.000042252537,0.0024307193],"genre_scores_gemma":[0.99877924,0.000039768336,0.0006305938,0.000016430557,0.000007210953,0.000011095502,0.00003651179,0.000013478156,0.00046570555],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994826,0.000012667553,0.0000023597265,0.000005110312,0.0000105586905,0.000020989155],"domain_scores_gemma":[0.99965847,0.00016511061,0.000060735754,0.000026947859,0.000034363093,0.000054423817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023178187,0.00028626586,0.00029316175,0.00022214549,0.00045090512,0.00046572377,0.00048043093,0.00054091413,0.0011850902],"category_scores_gemma":[0.0013267505,0.00023404522,0.000244931,0.00025020968,0.0006785008,0.0004856016,0.00041526076,0.0003761551,0.000094951014],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018051734,0.000077891615,0.005889759,0.000029449737,0.00003347477,0.00026222394,0.00011155342,0.9791589,0.006508976,0.0058943224,0.00026522108,0.0015878241],"study_design_scores_gemma":[0.00006181202,0.00003704106,0.0015524622,0.0000022813383,0.000005927632,0.0000130282915,0.000032623437,0.99640274,0.0009302851,0.00081508415,0.00014132836,0.0000053457607],"about_ca_topic_score_codex":0.0060740924,"about_ca_topic_score_gemma":0.00315475,"teacher_disagreement_score":0.0060740924,"about_ca_system_score_codex":0.00045380043,"about_ca_system_score_gemma":0.000394472,"threshold_uncertainty_score":0.01207751},"labels":[],"label_agreement":null},{"id":"W2024295140","doi":"10.1029/2007gl029515","title":"Density structure and buoyancy of the oceanic lithosphere revisited","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"European Social Fund","keywords":"Geology; Mantle (geology); Lithosphere; Geophysics; Subduction; Buoyancy; Thermal; Adiabatic process; Oceanic crust; Layering; Density contrast; Crust; Compressibility; Tectonics; Seismology; Thermodynamics; Physics","score_opus":0.015404382521860837,"score_gpt":0.26230391350980337,"score_spread":0.24689953098794254,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024295140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972556,0.00037914157,0.0007979957,0.00005718875,0.00000364697,0.0000016008112,0.00005823467,0.000010923181,0.001435607],"genre_scores_gemma":[0.99941766,0.00013342954,0.00020637357,0.0000042378556,0.000004683762,9.116345e-7,0.000051621053,0.0000029415467,0.0001782528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995863,0.000005632413,0.0000020776406,0.000009072658,0.000013464968,0.0000112049365],"domain_scores_gemma":[0.9998803,0.000023064207,0.000041973995,0.000010067227,0.00002673011,0.00001791577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014014443,0.0001518179,0.00014854215,0.000638097,0.0001426277,0.00048138257,0.00024119738,0.0001402883,0.0007458083],"category_scores_gemma":[0.00061735656,0.00015056826,0.00012569562,0.0003584023,0.00047164146,0.00032307438,0.00041858494,0.00019538478,0.00011757753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047741208,0.000033999295,0.6677404,0.0001196588,0.00014210185,0.0005078721,0.0016217952,0.017432569,0.22036582,0.023863541,0.00050407887,0.067190655],"study_design_scores_gemma":[0.000019965237,0.000104096245,0.91428673,0.000033660683,0.000047674275,0.0003599591,0.00046599208,0.058958936,0.017908752,0.00586381,0.0019175072,0.000033046133],"about_ca_topic_score_codex":0.006788845,"about_ca_topic_score_gemma":0.0034340774,"teacher_disagreement_score":0.006788845,"about_ca_system_score_codex":0.0003531673,"about_ca_system_score_gemma":0.0001754059,"threshold_uncertainty_score":0.013498664},"labels":[],"label_agreement":null},{"id":"W2024311828","doi":"10.1029/2007gl032459","title":"Unexpected rapid decrease in phase velocity of submeter Farley‐Buneman waves with altitude","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Altitude (triangle); Radar; Physics; Electrojet; Atmospheric sciences; Meteorology; Geodesy; Geology; Geophysics; Magnetic field","score_opus":0.02292564979462562,"score_gpt":0.2921090961008197,"score_spread":0.26918344630619406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024311828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782145,0.00009545097,0.00057371875,0.000026991,0.0000060618213,0.0000031133109,0.00006781862,0.00002396242,0.0013815134],"genre_scores_gemma":[0.9994659,0.00003258689,0.00023483716,0.000008417448,0.0000043960595,0.0000020525292,0.00006438294,0.0000035306257,0.00018397773],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996305,0.0000030798758,0.0000012296338,0.000010558988,0.000011490774,0.000010733228],"domain_scores_gemma":[0.9998628,0.000039542596,0.00003556467,0.000017411548,0.00002878871,0.000015843525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007867701,0.00009719285,0.00009729087,0.00029314496,0.00012615684,0.00022457626,0.0001299924,0.00016937198,0.0006381338],"category_scores_gemma":[0.00031635366,0.0001157849,0.000065054344,0.00020461185,0.00014064631,0.00014806617,0.00013331688,0.0002759884,0.00010596334],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040356594,0.000042702304,0.1939481,0.000076696975,0.000042675398,0.00069035514,0.00052222476,0.0011330735,0.7736698,0.0006241912,0.00047937102,0.02836722],"study_design_scores_gemma":[0.00001488635,0.00010493567,0.95582587,0.000006447422,0.000014586412,0.0003767565,0.00008349383,0.0018706885,0.040493395,0.00016278814,0.0010365609,0.000009477938],"about_ca_topic_score_codex":0.0009814149,"about_ca_topic_score_gemma":0.0010100997,"teacher_disagreement_score":0.0009814149,"about_ca_system_score_codex":0.00010972685,"about_ca_system_score_gemma":0.000053937893,"threshold_uncertainty_score":0.0021347404},"labels":[],"label_agreement":null},{"id":"W2024392701","doi":"10.1029/1999gl003692","title":"SuperDARN observations of medium‐scale gravity wave pairs generated by Joule heating in the auroral zone","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Joule heating; Geophysics; Electric field; Ionosphere; Physics; Joule effect; Gravity wave; Gravitational wave; Perturbation (astronomy); Computational physics; Geology; Astrophysics","score_opus":0.029331796203228434,"score_gpt":0.2791120559991227,"score_spread":0.24978025979589427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024392701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977482,0.00018147579,0.0003791377,0.00004389976,0.000010665322,0.000006261328,0.0002261065,0.0000260734,0.0013780567],"genre_scores_gemma":[0.9979361,0.000120190285,0.0011636135,0.000028529268,0.000018469396,0.0000071605054,0.00047220552,0.00000583391,0.00024792983],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.0000066416587,0.0000029736211,0.000015750002,0.000026537415,0.000013866374],"domain_scores_gemma":[0.9998061,0.00002537037,0.000049741455,0.00002517063,0.000029363278,0.000064382504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024218504,0.00017345068,0.0001622482,0.0004773879,0.00022477077,0.00016216638,0.00019647111,0.00022950057,0.00059246283],"category_scores_gemma":[0.00035017158,0.00014588844,0.00014358576,0.00028862077,0.0001708687,0.00020583993,0.00050540623,0.00031458246,0.00010036196],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001664862,0.00019718462,0.26302746,0.00018988125,0.00016685203,0.0015125254,0.0012443872,0.002342033,0.689348,0.0010077782,0.0020205122,0.037278492],"study_design_scores_gemma":[0.00005709631,0.00014704626,0.9869708,0.000008202051,0.000037862508,0.00036546486,0.00010257684,0.0019955006,0.008079212,0.000138699,0.0020846012,0.0000129560185],"about_ca_topic_score_codex":0.0020640956,"about_ca_topic_score_gemma":0.0047907615,"teacher_disagreement_score":0.0020640956,"about_ca_system_score_codex":0.00019986248,"about_ca_system_score_gemma":0.00010185696,"threshold_uncertainty_score":0.004104197},"labels":[],"label_agreement":null},{"id":"W2024612359","doi":"10.1029/2004gl021528","title":"The summer northern annular mode and abnormal summer weather in 2003","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Empirical orthogonal functions; Jet stream; Northern Hemisphere; Arctic oscillation; Forcing (mathematics); Period (music); Atmospheric circulation; Environmental science; Polar vortex; Mode (computer interface); North Atlantic oscillation; Anomaly (physics); Geography; Jet (fluid); Geology; Stratosphere","score_opus":0.03407873241837865,"score_gpt":0.3104999683804677,"score_spread":0.276421235962089,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024612359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99507684,0.0001991886,0.00023338397,0.00012858106,0.00002552947,0.000005379831,0.0010191781,0.000023182065,0.0032888616],"genre_scores_gemma":[0.9988268,0.00006108617,0.00012069792,0.00001707082,0.000017865872,0.000004225442,0.00066159654,0.000004059624,0.0002865716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998869,0.00001640313,0.000011409545,0.000025651849,0.000027117636,0.000032442815],"domain_scores_gemma":[0.99958414,0.000044123295,0.00018099815,0.000024499315,0.00008260504,0.00008360554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031252077,0.00013128994,0.0001671246,0.0003633363,0.0002879482,0.0005828847,0.000110202265,0.00018619701,0.0006742043],"category_scores_gemma":[0.00076695683,0.00007308828,0.000101984566,0.00063938333,0.00014859656,0.0002539333,0.00024518027,0.00018498905,0.00014099167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006934847,0.000063300016,0.9534622,0.000060383383,0.00004834648,0.0006516134,0.0018156196,0.0018913706,0.004230341,0.0012796086,0.006936478,0.028867409],"study_design_scores_gemma":[0.0000070512037,0.000027366834,0.99321127,0.000012073886,0.0000070334127,0.000220087,0.0002917473,0.0014666906,0.00024296073,0.00023926083,0.0042691594,0.0000052333426],"about_ca_topic_score_codex":0.021996574,"about_ca_topic_score_gemma":0.036410652,"teacher_disagreement_score":0.021996574,"about_ca_system_score_codex":0.00062868395,"about_ca_system_score_gemma":0.00031640372,"threshold_uncertainty_score":0.043737113},"labels":[],"label_agreement":null},{"id":"W2024883634","doi":"10.1029/2001gl013567","title":"Evolution of subducting mantle lithosphere at a continental plate boundary","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Lithosphere; Mantle (geology); Convergent boundary; Collision zone; Plate tectonics; Geophysics; Crustal recycling; Mantle convection; Mantle wedge; Continental crust; Seismology; Oceanic crust; Tectonics","score_opus":0.023973757964524157,"score_gpt":0.2710516885031785,"score_spread":0.24707793053865434,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2024883634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99713874,0.00011376325,0.00029869983,0.000045389166,0.0000016166813,0.0000023708217,0.00005722045,0.000020247824,0.0023219902],"genre_scores_gemma":[0.9991352,0.00007754121,0.00030186863,0.000008579416,0.000001114421,0.00000177456,0.00009720636,0.000007366214,0.00036930505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995136,0.000011335345,0.0000034026993,0.00001148789,0.000008712921,0.0000136015715],"domain_scores_gemma":[0.99984896,0.000024677902,0.000031720494,0.000021908494,0.000026047315,0.000046663245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018217682,0.0001893056,0.0001941365,0.00078824186,0.000600906,0.0012943305,0.00034819273,0.0006831569,0.0016192317],"category_scores_gemma":[0.0008010303,0.00033073302,0.00026058563,0.0005257159,0.00073432823,0.00041164906,0.001022077,0.0002750068,0.00036905098],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008480279,0.00011985758,0.4311616,0.00013337369,0.00029139745,0.0023698725,0.002855762,0.3030555,0.19085072,0.039584335,0.00078188424,0.02794766],"study_design_scores_gemma":[0.00011839418,0.00027377062,0.7457471,0.000086491986,0.00011788222,0.000743448,0.0016631724,0.21774548,0.014739882,0.0133327525,0.0053327247,0.000098910714],"about_ca_topic_score_codex":0.007455645,"about_ca_topic_score_gemma":0.0038143836,"teacher_disagreement_score":0.007455645,"about_ca_system_score_codex":0.0010911329,"about_ca_system_score_gemma":0.00029820087,"threshold_uncertainty_score":0.01482451},"labels":[],"label_agreement":null},{"id":"W2025124163","doi":"10.1029/2001gl014011","title":"Ocean‐Atmosphere Feedback: Using the non‐stationarity in the climate system","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Atmosphere (unit); Environmental science; Climate system; Climate model; Climatology; Atmospheric model; Bridging (networking); Climate change; Ecosystem; Cloud feedback; Meteorology; Atmospheric sciences; Climate sensitivity; Computer science; Geology; Oceanography; Geography; Ecology","score_opus":0.06358269548342739,"score_gpt":0.308477578474616,"score_spread":0.2448948829911886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025124163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.66352916,0.003037077,0.31791517,0.004252458,0.00027015203,0.000041860145,0.000293247,0.00040760185,0.010253234],"genre_scores_gemma":[0.98106456,0.0008075166,0.017449738,0.000109215005,0.00010448835,0.000017651992,0.00004408344,0.000043270305,0.00035961182],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9994074,0.00033473218,0.00002954769,0.000073983334,0.00011287471,0.00004146295],"domain_scores_gemma":[0.995138,0.0036804094,0.00051640294,0.0004023549,0.00015999444,0.00010283967],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024813546,0.00038601688,0.00054213486,0.00067423645,0.0006066082,0.0014644092,0.00053341006,0.00053779257,0.00061089237],"category_scores_gemma":[0.011134623,0.00028100316,0.00042978147,0.00079198455,0.0014886155,0.0033812404,0.0015985332,0.001283537,0.00010307637],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038182133,0.00009854009,0.07103825,0.00027604034,0.00041543384,0.0005593932,0.0012292856,0.50838536,0.010971277,0.24994664,0.0018493286,0.15484862],"study_design_scores_gemma":[0.000028038154,0.00007649144,0.020584393,0.000033846605,0.00008181873,0.00012181368,0.00014910882,0.7045849,0.0020899854,0.27004454,0.0021336295,0.00007151877],"about_ca_topic_score_codex":0.0072033843,"about_ca_topic_score_gemma":0.005305329,"teacher_disagreement_score":0.0072033843,"about_ca_system_score_codex":0.0007919223,"about_ca_system_score_gemma":0.0009380704,"threshold_uncertainty_score":0.014322877},"labels":[],"label_agreement":null},{"id":"W2025194223","doi":"10.1029/2003gl017446","title":"Anomalous subarctic influence in the southern California Current during 2002","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Subarctic climate; Current (fluid); Pycnocline; Oceanography; Water mass; Geology; Plankton; Salinity; Bedrock; Submarine pipeline; Environmental science; Geomorphology","score_opus":0.01967933595241521,"score_gpt":0.2580571598755773,"score_spread":0.2383778239231621,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025194223","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975847,0.00022005217,0.000016219092,0.000092411356,0.000009122405,0.0000022576971,0.00025681136,0.0000055506125,0.0018128232],"genre_scores_gemma":[0.99844474,0.00025300658,0.000036505542,0.000032294163,0.000012413637,0.0000023254413,0.00046093698,0.0000028306895,0.0007550662],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999198,0.000005644561,0.0000058479263,0.000025792395,0.000021795526,0.000021132242],"domain_scores_gemma":[0.9994791,0.000029438734,0.00022850193,0.00002032374,0.00014884936,0.00009382477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014132952,0.000098396675,0.00013529096,0.0005357685,0.00044047646,0.0007356114,0.00015231351,0.00015941197,0.00080331165],"category_scores_gemma":[0.00063589384,0.00009071135,0.000049450788,0.00056246517,0.00020853325,0.00018282015,0.0003517418,0.00020846547,0.000072022856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012495507,0.00003251191,0.9868298,0.000028367833,0.000036605197,0.00020354798,0.0011356628,0.00023558628,0.0017839897,0.00015147506,0.0012486824,0.0081888065],"study_design_scores_gemma":[0.0000015168206,0.0000040744335,0.9983127,0.0000033406113,0.000004793847,0.000024200624,0.00023539356,0.000046407913,0.000050112398,0.0000075400967,0.0013086584,0.0000013533663],"about_ca_topic_score_codex":0.1870124,"about_ca_topic_score_gemma":0.44559494,"teacher_disagreement_score":0.1870124,"about_ca_system_score_codex":0.0012818286,"about_ca_system_score_gemma":0.00055403856,"threshold_uncertainty_score":0.37184775},"labels":[],"label_agreement":null},{"id":"W2025343504","doi":"10.1029/2009gl040423","title":"Evidence of O<sub>2</sub> consumption in underway seawater lines: Implications for air‐sea O<sub>2</sub> and CO<sub>2</sub> fluxes","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Seawater; Environmental science; Environmental chemistry; Oceanography; Atmospheric sciences; Chemistry; Geology","score_opus":0.04802419175176881,"score_gpt":0.30214221790229556,"score_spread":0.25411802615052675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025343504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99935776,0.000019594714,0.00017077837,0.00001797553,0.000001474759,0.0000019346003,0.000056932935,0.000005963178,0.00036760472],"genre_scores_gemma":[0.99920005,0.000034082674,0.0002576055,0.000018287557,0.0000027022786,0.0000048844063,0.00013542786,0.0000061224987,0.00034075684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988925,0.000011488327,0.000009639339,0.00003741754,0.00003223963,0.00001995408],"domain_scores_gemma":[0.99942076,0.00004734057,0.0002794702,0.000066515095,0.00012895628,0.00005693332],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017423455,0.00030465366,0.00021072448,0.00027408075,0.0005123575,0.00040628697,0.0002794674,0.00044847184,0.00087737007],"category_scores_gemma":[0.00052799605,0.0002928427,0.00019371805,0.00042496802,0.00066726585,0.00057040324,0.00053729175,0.00036691225,0.00015903241],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021678228,0.000027432076,0.77016145,0.000039041603,0.000040843865,0.0003715714,0.00056450197,0.00025056626,0.2235022,0.00006235641,0.0000861039,0.0046770414],"study_design_scores_gemma":[0.0000043643618,0.00013201819,0.9867756,0.0000031272955,0.000021588156,0.00016483605,0.0005465264,0.00019403547,0.011601359,0.000048808317,0.00050125114,0.0000065633276],"about_ca_topic_score_codex":0.0072908583,"about_ca_topic_score_gemma":0.012848007,"teacher_disagreement_score":0.0072908583,"about_ca_system_score_codex":0.00024707522,"about_ca_system_score_gemma":0.0002052404,"threshold_uncertainty_score":0.014496863},"labels":[],"label_agreement":null},{"id":"W2025436147","doi":"10.1029/2007gl030396","title":"Lake Agassiz Final drainage event in the northwest North Atlantic","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Université du Québec à Montréal","funders":"","keywords":"Geology; Thermohaline circulation; North Atlantic Deep Water; Shutdown of thermohaline circulation; Oceanography; Ice sheet; Gulf Stream; Glacial period; Quaternary; North Atlantic oscillation; Atlantic multidecadal oscillation; Climatology; Paleontology","score_opus":0.041709808644629684,"score_gpt":0.3069687014609408,"score_spread":0.2652588928163111,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025436147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972595,0.00007572046,0.000027348759,0.00009857913,0.000009563034,0.00000205924,0.0005312673,0.000012378886,0.0019835876],"genre_scores_gemma":[0.9985348,0.000059239126,0.00006142156,0.00003266576,0.00001091781,0.000003318319,0.0008717875,0.0000019665827,0.000423913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.0000035042717,0.0000025171164,0.000012647247,0.000009804691,0.000020663547],"domain_scores_gemma":[0.9998883,0.00000828615,0.00004990516,0.000006527113,0.000029096736,0.000017863042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109165674,0.00008466139,0.00012411714,0.0004541029,0.00038401943,0.00041981897,0.00012918266,0.00024526304,0.0010188294],"category_scores_gemma":[0.00025978984,0.00005664586,0.00007494007,0.0003652554,0.00019967754,0.00018329595,0.00044403254,0.00020055295,0.000118558026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008885055,0.000059156268,0.9567096,0.00005000506,0.00007534391,0.00062708464,0.0012522052,0.00071749446,0.016685126,0.00047853426,0.0031978192,0.019258963],"study_design_scores_gemma":[0.0000044859894,0.0000066354924,0.9984267,0.0000034914901,0.0000050723424,0.000024179117,0.000093537834,0.00012724893,0.00015341162,0.000018130164,0.0011352856,0.0000018902784],"about_ca_topic_score_codex":0.06175333,"about_ca_topic_score_gemma":0.21346475,"teacher_disagreement_score":0.06175333,"about_ca_system_score_codex":0.0010449213,"about_ca_system_score_gemma":0.0004998589,"threshold_uncertainty_score":0.12278777},"labels":[],"label_agreement":null},{"id":"W2025812132","doi":"10.1002/2015gl063147","title":"Evaluation of the inertial dissipation method within boundary layers using numerical simulations","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fluid Dynamics and Turbulent Flows","field":"Engineering","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Dissipation; Turbulence; Mechanics; Physics; Turbulence kinetic energy; Boundary layer; Inertial frame of reference; Computation; Spectral line; Kinetic energy; Convection; Logarithm; Computational physics; Classical mechanics; Mathematical analysis; Mathematics; Thermodynamics; Algorithm","score_opus":0.09679808177892282,"score_gpt":0.38154571788219405,"score_spread":0.28474763610327125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2025812132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8326434,0.0006975327,0.15915845,0.00026131523,0.00014250234,0.0001677113,0.00016400886,0.0006193252,0.006145771],"genre_scores_gemma":[0.97022724,0.00008487534,0.029212702,0.000017550246,0.0000125424285,0.000056745732,0.000045039957,0.000059082467,0.00028426846],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993383,0.00024693247,0.000049991668,0.000042191212,0.00025539126,0.000067119196],"domain_scores_gemma":[0.9942899,0.00366221,0.00046808447,0.00052722293,0.0009027931,0.00014974402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022058664,0.00067526824,0.00079344737,0.00087949727,0.0006629419,0.0009320342,0.0008062003,0.0008860662,0.0006314104],"category_scores_gemma":[0.008619821,0.00028016395,0.00041550287,0.0005981267,0.0007550497,0.0007390653,0.0006301383,0.0007322898,0.00013063321],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002583331,0.00019849028,0.007418933,0.00011887682,0.000055578246,0.00012026594,0.00014359904,0.95041263,0.018522665,0.004234193,0.00023541515,0.018280918],"study_design_scores_gemma":[0.000010804433,0.000050225182,0.0004973493,0.000011399289,0.0000046248542,0.0000054995294,0.000006263457,0.99594516,0.0031732942,0.00015667189,0.00013144255,0.0000072228554],"about_ca_topic_score_codex":0.005309354,"about_ca_topic_score_gemma":0.0019876438,"teacher_disagreement_score":0.005309354,"about_ca_system_score_codex":0.00062474655,"about_ca_system_score_gemma":0.0005061219,"threshold_uncertainty_score":0.011665881},"labels":[],"label_agreement":null},{"id":"W2026087292","doi":"10.1029/2007gl031765","title":"Channelized bottom melting and stability of floating ice shelves","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":234,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Arctic Sciences; European Space Agency; California Institute of Technology; National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Ice shelf; Geology; Oceanography; Sea ice; Antarctic sea ice; Arctic ice pack; Ice stream; Ice sheet; Fast ice; Iceberg; Channelized; Ice divide; Drilling; Melt pond; Geomorphology; Cryosphere","score_opus":0.08143620546543238,"score_gpt":0.2935033573471982,"score_spread":0.21206715188176578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026087292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998708,0.000014839131,0.0000074976847,0.0000011548227,2.0792687e-7,1.5002213e-7,0.00003592014,4.859651e-7,0.00006888387],"genre_scores_gemma":[0.9998248,0.000009934739,0.000011221337,0.0000017567895,2.5220118e-7,2.7808457e-7,0.00008806372,6.5372416e-7,0.00006300633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996436,0.0000018353625,0.0000013017461,0.00000792728,0.0000058912674,0.000018698483],"domain_scores_gemma":[0.9998939,0.0000100713105,0.000040372972,0.000006862276,0.000017139362,0.00003159144],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000065988366,0.00007257102,0.00009897032,0.0003153362,0.00021332847,0.00033607232,0.00010332939,0.00009692602,0.00064985396],"category_scores_gemma":[0.00023529436,0.00008367562,0.000086208136,0.00017788196,0.00025857848,0.0001595137,0.00026390122,0.00010886265,0.00007922208],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004578063,0.00003747024,0.9507583,0.000012085941,0.00006790836,0.00017867563,0.00022995459,0.0013025583,0.039391965,0.00013676014,0.00013010029,0.0072963787],"study_design_scores_gemma":[0.0000015833011,0.000019167475,0.99854434,0.0000013158389,0.0000049364216,0.000032532575,0.00009123698,0.0002689,0.000941715,0.000029803274,0.00006270883,0.0000017804232],"about_ca_topic_score_codex":0.021030271,"about_ca_topic_score_gemma":0.03443367,"teacher_disagreement_score":0.021030271,"about_ca_system_score_codex":0.00050050137,"about_ca_system_score_gemma":0.00019316933,"threshold_uncertainty_score":0.041815758},"labels":[],"label_agreement":null},{"id":"W2026147422","doi":"10.1029/2001gl014649","title":"Estimates of heat flow in the deep mantle based on the power requirements for the geodynamo","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":222,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Mantle (geology); Dynamo theory; Buoyancy; Convection; Geophysics; Inner core; Geology; Thermal; Mantle convection; Dynamo; Mechanics; Earth's internal heat budget; Heat generation; Convective heat transfer; Thermodynamics; Magnetic field; Physics","score_opus":0.038269901558631456,"score_gpt":0.3041303064398028,"score_spread":0.26586040488117135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026147422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89281464,0.0048300344,0.09191995,0.00031768225,0.00006642583,0.000032821637,0.0006263358,0.000277544,0.009114618],"genre_scores_gemma":[0.9858833,0.001103714,0.011837171,0.000024893936,0.000020957817,0.000018529177,0.0003571216,0.00005085395,0.0007034707],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986506,0.000026712272,0.000008549634,0.0000346909,0.000047174224,0.000017694569],"domain_scores_gemma":[0.9995197,0.0002428528,0.00008793104,0.000059113492,0.0000705515,0.000019828885],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051808194,0.0004755199,0.00023573045,0.00079585466,0.0002477239,0.0005145307,0.00034200607,0.00037496877,0.0008419256],"category_scores_gemma":[0.0015520797,0.00031353245,0.00024623284,0.00039425018,0.0005161045,0.00072558667,0.0005180422,0.0006224218,0.0004131896],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007056546,0.00003943121,0.07042727,0.0003378098,0.000090945774,0.00017984505,0.0004940759,0.025287207,0.8239517,0.017598074,0.0006143516,0.06027364],"study_design_scores_gemma":[0.000070335445,0.00030509708,0.2998167,0.00008794891,0.00011615989,0.00077845814,0.0001682051,0.07380603,0.58006865,0.025382467,0.019274358,0.00012551318],"about_ca_topic_score_codex":0.0014382079,"about_ca_topic_score_gemma":0.0016254311,"teacher_disagreement_score":0.0014382079,"about_ca_system_score_codex":0.000604154,"about_ca_system_score_gemma":0.00020953397,"threshold_uncertainty_score":0.004383445},"labels":[],"label_agreement":null},{"id":"W2026242197","doi":"10.1029/2007gl031981","title":"Inconsistency between atmospheric dynamics and temperatures during the exceptional 2006/2007 fall/winter and recent warming in Europe","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"Agence Nationale de la Recherche","keywords":"Climatology; Atmospheric circulation; Anomaly (physics); Environmental science; Atmospheric sciences; Atmospheric dynamics; Climate change; Atmospheric temperature; Meteorology; Geography; Geology; Atmosphere (unit); Oceanography","score_opus":0.02243208329359908,"score_gpt":0.28803230206248726,"score_spread":0.2656002187688882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026242197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998538,0.00012673892,0.00016234446,0.0001212615,0.000009840488,0.0000013677254,0.00028692457,0.000010878122,0.0007426747],"genre_scores_gemma":[0.99926573,0.00005874368,0.00010132569,0.000036540405,0.000015720017,0.0000012067394,0.00046895686,0.0000041242174,0.00004768477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998356,0.000023285043,0.000021849317,0.000058571593,0.000029767341,0.00003091883],"domain_scores_gemma":[0.9994837,0.000090052956,0.00019865429,0.00005825517,0.000106801104,0.000062541134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005941834,0.00012636307,0.0002638703,0.00045570693,0.00029155874,0.00072636013,0.00024978444,0.0004171163,0.00061272574],"category_scores_gemma":[0.0010104361,0.00012872192,0.0002143187,0.0006545737,0.000392374,0.00040736492,0.00040438835,0.00030863218,0.00012331718],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027389423,0.0000465508,0.98550886,0.000033024888,0.00013291818,0.00008615694,0.0002914193,0.0013771997,0.00403465,0.00035192582,0.0008001847,0.007063178],"study_design_scores_gemma":[0.0000039292477,0.000013305715,0.9986953,0.0000035851347,0.000012382081,0.000034034994,0.00007389382,0.00044021252,0.00019704812,0.00008885798,0.00043374448,0.0000036942752],"about_ca_topic_score_codex":0.008425725,"about_ca_topic_score_gemma":0.011219386,"teacher_disagreement_score":0.008425725,"about_ca_system_score_codex":0.00035543914,"about_ca_system_score_gemma":0.00023107577,"threshold_uncertainty_score":0.016753316},"labels":[],"label_agreement":null},{"id":"W2026354693","doi":"10.1029/1999gl011178","title":"Emissions of methyl chloroform (CH <sub>3</sub> CCl <sub>3</sub> ) from biomass burning and the tropospheric methyl chloroform budget","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Chloroform; Biomass (ecology); Carbon monoxide; Biomass burning; Environmental chemistry; Environmental science; Troposphere; Carbon dioxide; Methyl iodide; Atmosphere (unit); Chemistry; Atmospheric sciences; Meteorology; Organic chemistry; Agronomy; Aerosol; Physics","score_opus":0.016063257794160613,"score_gpt":0.2507665085656989,"score_spread":0.23470325077153825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026354693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99385685,0.0023019703,0.000744036,0.00013238216,0.0000052741534,0.000007608084,0.00076650135,0.000016298174,0.0021690123],"genre_scores_gemma":[0.9962364,0.0019647684,0.00059420674,0.000039273396,0.000008298339,0.000009226881,0.0005739563,0.000009628325,0.0005643928],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990845,0.00001692241,0.000004464058,0.00001788935,0.000032343294,0.000020069621],"domain_scores_gemma":[0.99990666,0.000034516088,0.000023954515,0.000004919736,0.000020006026,0.000009916336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019675495,0.00026401095,0.00013446962,0.00051611435,0.00024682118,0.00044865438,0.00015128091,0.00037404214,0.0011747921],"category_scores_gemma":[0.00031287552,0.00013096734,0.00014794366,0.0006897427,0.00019642485,0.0004625747,0.0002200954,0.00013990035,0.00029016915],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017187494,0.00012780965,0.28665206,0.00036468415,0.00017122534,0.00059120846,0.00014033396,0.0117645785,0.6535666,0.002490148,0.0007257553,0.04168678],"study_design_scores_gemma":[0.00005738928,0.00029709507,0.8157247,0.00005435752,0.00012927756,0.00036640256,0.00025911757,0.014438216,0.15973401,0.0020639936,0.006838581,0.000036995752],"about_ca_topic_score_codex":0.008290202,"about_ca_topic_score_gemma":0.011397108,"teacher_disagreement_score":0.008290202,"about_ca_system_score_codex":0.0006533587,"about_ca_system_score_gemma":0.00025609945,"threshold_uncertainty_score":0.016483903},"labels":[],"label_agreement":null},{"id":"W2026517599","doi":"10.1029/2000gl011777","title":"Variability in the Deep Western Boundary Current in the equatorial Atlantic at 44°W","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Equator; Hydrography; North Atlantic Deep Water; Oceanography; Tropical Atlantic; Geology; Climatology; Current (fluid); Boundary current; Range (aeronautics); Lag; Ocean current; Deep water; Sea surface temperature; Latitude; Geodesy","score_opus":0.03504756136913698,"score_gpt":0.29867313401842094,"score_spread":0.26362557264928393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2026517599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956745,0.00002476992,0.000031438052,0.000010486544,0.0000011057607,0.0000018520057,0.00008015649,0.0000017021949,0.00028101227],"genre_scores_gemma":[0.99948657,0.00003275866,0.000069106274,0.0000063358866,0.0000032049297,0.0000025645354,0.0002423984,0.0000012819871,0.00015586904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.000011576328,0.000005962695,0.00001763848,0.000021853626,0.000021851543],"domain_scores_gemma":[0.99965096,0.000038382834,0.000149695,0.000022056547,0.0000904383,0.00004842947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020112937,0.00008298683,0.00015061766,0.0005602786,0.00022230443,0.00038443133,0.00011705176,0.00015090604,0.0003733729],"category_scores_gemma":[0.0008463395,0.000119831,0.00009621299,0.00043851224,0.00026052428,0.00021599101,0.00029084025,0.00011569097,0.00008699581],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006783189,0.000018315981,0.9824867,0.000007905685,0.000032905376,0.000096186035,0.00046651132,0.00014493383,0.011358957,0.00008880953,0.00009720594,0.005133752],"study_design_scores_gemma":[0.0000016695938,0.0000115484345,0.99948585,0.0000012927756,0.0000035512753,0.000022408498,0.000057736717,0.00010542848,0.00011819237,0.000009536044,0.00018133747,0.0000013516941],"about_ca_topic_score_codex":0.035583895,"about_ca_topic_score_gemma":0.078108735,"teacher_disagreement_score":0.035583895,"about_ca_system_score_codex":0.00045538688,"about_ca_system_score_gemma":0.00020156534,"threshold_uncertainty_score":0.070753515},"labels":[],"label_agreement":null},{"id":"W2027397158","doi":"10.1029/2006gl027316","title":"Observations of non‐volcanic tremor during the northern Cascadia slow‐slip event in February 2002","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Episodic tremor and slip; Subduction; Geology; Seismology; Volcano; Slip (aerodynamics); Tectonics","score_opus":0.03110222833571543,"score_gpt":0.26142540855377966,"score_spread":0.23032318021806422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027397158","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649966,0.00006835476,0.00006558079,0.00006411496,0.0000065527174,0.000008282155,0.00073519914,0.000041347048,0.002510887],"genre_scores_gemma":[0.9967699,0.00008096234,0.00011824646,0.000024997193,0.00001472656,0.0000123445925,0.0015007982,0.000008310213,0.0014696516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978787,0.000019742996,0.00001551315,0.00005482508,0.00007918745,0.000042986798],"domain_scores_gemma":[0.9992865,0.00004989439,0.00017832255,0.00007019494,0.00021155193,0.00020358259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022000227,0.00033238746,0.0002579459,0.00097400387,0.0006013027,0.00048685554,0.0003518553,0.0004074348,0.0011866022],"category_scores_gemma":[0.0009450966,0.00024407591,0.0001326385,0.0007328776,0.00028465118,0.00021870575,0.0005662107,0.00025693563,0.00036331618],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003021113,0.00008191231,0.9591712,0.00008297126,0.000074980446,0.0010508379,0.003088075,0.0004934979,0.021331985,0.000065256754,0.0028058111,0.011451361],"study_design_scores_gemma":[0.0000053767167,0.00001738921,0.99878377,0.000002967822,0.000005217176,0.000058486658,0.00014719706,0.000099598044,0.00020541098,0.0000051253396,0.0006668668,0.0000025912327],"about_ca_topic_score_codex":0.08261554,"about_ca_topic_score_gemma":0.2389088,"teacher_disagreement_score":0.08261554,"about_ca_system_score_codex":0.0009847386,"about_ca_system_score_gemma":0.00043770205,"threshold_uncertainty_score":0.16426933},"labels":[],"label_agreement":null},{"id":"W2027419649","doi":"10.1029/2003gl018571","title":"Simulation of extratropical Hurricane Gustav using a coupled atmosphere‐ocean‐sea spray model","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Bedford Institute of Oceanography","funders":"","keywords":"Extratropical cyclone; Entrainment (biomusicology); Environmental science; Sea spray; Storm; Atmospheric sciences; Sea surface temperature; Mesoscale meteorology; Climatology; Heat flux; Mass flux; Meteorology; Geology; Heat transfer; Aerosol; Oceanography; Mechanics; Physics","score_opus":0.05692687857066954,"score_gpt":0.3219976464789615,"score_spread":0.265070767908292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027419649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962286,0.000034515655,0.0009434138,0.00010603076,0.000017205823,0.000021956732,0.0002844808,0.00006677787,0.0022970114],"genre_scores_gemma":[0.99754757,0.00003624846,0.0013187745,0.000024408768,0.0000050844133,0.00002215416,0.00031412116,0.000013728715,0.0007178554],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999002,0.000021022703,0.00000531743,0.000013805787,0.000022129498,0.00003743894],"domain_scores_gemma":[0.9997191,0.00008713668,0.000033149772,0.000016271288,0.000059686663,0.00008466479],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019084592,0.00054241804,0.0005216798,0.00034652968,0.00043607014,0.00044302247,0.00080769055,0.00080795574,0.00200555],"category_scores_gemma":[0.00067187974,0.00028770315,0.00045873385,0.00037918915,0.00044712404,0.00029691603,0.0007608892,0.00062564923,0.000098407276],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017526148,0.00010173389,0.010526063,0.000021190071,0.000037438618,0.00022824357,0.000059943763,0.9823585,0.0035012388,0.0011743086,0.0004294361,0.0013867194],"study_design_scores_gemma":[0.00008472882,0.0000669749,0.0036597515,0.0000022664708,0.000009380499,0.000012535222,0.000047960573,0.99524313,0.00051970483,0.00017430166,0.00017191238,0.000007338583],"about_ca_topic_score_codex":0.070506,"about_ca_topic_score_gemma":0.038500853,"teacher_disagreement_score":0.070506,"about_ca_system_score_codex":0.00091911096,"about_ca_system_score_gemma":0.00105307,"threshold_uncertainty_score":0.14019126},"labels":[],"label_agreement":null},{"id":"W2027433621","doi":"10.1029/2006gl026340","title":"Modifications of a land surface scheme for improved simulation of ground freeze‐thaw in northern environments","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Environmental science; Frost (temperature); Peat; Permafrost; Soil science; Water content; Vegetation (pathology); Hydrology (agriculture); Groundwater; Meteorology; Geology; Ecology; Geotechnical engineering","score_opus":0.06853022517014773,"score_gpt":0.30863205212081185,"score_spread":0.24010182695066412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027433621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84962916,0.00008406792,0.14226906,0.00014707177,0.00009735249,0.00019343248,0.00037262248,0.0013229394,0.0058842483],"genre_scores_gemma":[0.9553728,0.000027894743,0.043305766,0.00002426303,0.000009575192,0.00010323383,0.00021496683,0.0000673991,0.0008741445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998944,0.000037964444,0.000008357181,0.000015347143,0.00002407751,0.000019826823],"domain_scores_gemma":[0.9996735,0.00012484219,0.000047500347,0.000042455205,0.00007490099,0.00003676228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005196651,0.00045947274,0.00040677935,0.00021702876,0.00032587172,0.00046667363,0.00090328837,0.0006678502,0.0013481259],"category_scores_gemma":[0.0012030366,0.00024690497,0.000498319,0.0002910011,0.00034306393,0.00034971404,0.0005462101,0.00055445294,0.00016073498],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004154458,0.000042348707,0.0019872854,0.000010121564,0.000010549744,0.000028844324,0.00002243938,0.99109143,0.001914535,0.0007071283,0.00011608531,0.00402768],"study_design_scores_gemma":[0.000007848628,0.0000092080945,0.00017969708,5.814863e-7,0.0000012698987,0.0000016914834,0.0000022849133,0.9994709,0.00018633578,0.000047686965,0.00009109149,0.0000014968687],"about_ca_topic_score_codex":0.020716993,"about_ca_topic_score_gemma":0.014385939,"teacher_disagreement_score":0.020716993,"about_ca_system_score_codex":0.00065042585,"about_ca_system_score_gemma":0.0009763393,"threshold_uncertainty_score":0.04119283},"labels":[],"label_agreement":null},{"id":"W2027469749","doi":"10.1029/2005gl024057","title":"Bias corrections of long‐term (1973–2004) daily precipitation data over the northern regions","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":310,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Precipitation; Snow; Environmental science; Climatology; Atmospheric sciences; Latitude; Arctic; Meteorology; Geography; Geology; Oceanography; Geodesy","score_opus":0.07601246924893018,"score_gpt":0.3165493399341646,"score_spread":0.24053687068523444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2027469749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91303664,0.00070214376,0.072771996,0.00015105298,0.00020653485,0.0002730819,0.0081857685,0.0011042649,0.003568551],"genre_scores_gemma":[0.91167796,0.00032152265,0.07498492,0.00009073928,0.00007833368,0.0004243271,0.008537534,0.00041171283,0.0034728919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9990846,0.00018231441,0.00014352541,0.00021995722,0.00027597285,0.00009365046],"domain_scores_gemma":[0.9974674,0.00041257273,0.00043019568,0.00038466917,0.0012671085,0.00003810452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024429348,0.00038940966,0.00031057082,0.0011089921,0.00046458666,0.00044104876,0.00043594174,0.0002099836,0.0008015851],"category_scores_gemma":[0.0053642294,0.00018749987,0.000679092,0.0024838296,0.00016410799,0.00030121827,0.00037757077,0.00033721118,0.0003798409],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036137266,0.00011474004,0.6767108,0.0002654619,0.0006322286,0.00013700615,0.0006312815,0.031582553,0.026025005,0.0011819113,0.005364399,0.2569932],"study_design_scores_gemma":[0.000054645927,0.000109013345,0.9452035,0.000025350966,0.0001204814,0.00008363119,0.00010644287,0.023573639,0.014547885,0.00042189966,0.015712643,0.000040870258],"about_ca_topic_score_codex":0.032905407,"about_ca_topic_score_gemma":0.06605241,"teacher_disagreement_score":0.032905407,"about_ca_system_score_codex":0.00090136303,"about_ca_system_score_gemma":0.0013743861,"threshold_uncertainty_score":0.06542772},"labels":[],"label_agreement":null},{"id":"W2028522241","doi":"10.1029/2009gl038852","title":"Observational evidence of an intensifying hydrological cycle in northern Canada","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":204,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Northern British Columbia","funders":"","keywords":"Bay; Climatology; Streamflow; Arctic; Annual cycle; Period (music); Environmental science; Water cycle; Discharge; Physical geography; Oceanography; Geology; Geography; Drainage basin","score_opus":0.11370919250692824,"score_gpt":0.31955395778823753,"score_spread":0.2058447652813093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028522241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950864,0.00022367778,0.00006972527,0.00025356503,0.000004284008,0.0000056024305,0.001673519,0.000014210321,0.0026689775],"genre_scores_gemma":[0.99827397,0.0002095494,0.00009171636,0.000050142866,0.0000033830927,0.0000023119035,0.00083862216,0.0000030100898,0.00052736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981517,0.000009606194,0.000009065743,0.000040234387,0.00006999877,0.000055977558],"domain_scores_gemma":[0.9988518,0.000074815376,0.00019198471,0.000047264326,0.00064255245,0.00019169236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027734975,0.00012503026,0.00017797222,0.0007872548,0.0011396366,0.00092093897,0.0003250126,0.00019993434,0.0014500115],"category_scores_gemma":[0.0011913686,0.00013789558,0.00012678321,0.0020638038,0.00058621255,0.00022354252,0.0004144915,0.00027748544,0.000083730694],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006554862,0.000021030892,0.9825865,0.000038119415,0.000047899717,0.00013907035,0.0013033034,0.000627163,0.0020738225,0.00027593027,0.0019716953,0.010849936],"study_design_scores_gemma":[0.0000013941844,0.0000025065183,0.99793184,0.000006020519,0.000006737057,0.000021039343,0.00033193055,0.00020293913,0.000080809186,0.000011322091,0.0013997547,0.0000037577267],"about_ca_topic_score_codex":0.98983127,"about_ca_topic_score_gemma":0.9959014,"teacher_disagreement_score":0.013914524,"about_ca_system_score_codex":0.013914524,"about_ca_system_score_gemma":0.01269818,"threshold_uncertainty_score":0.10095739},"labels":[],"label_agreement":null},{"id":"W2028554965","doi":"10.1029/2003gl018134","title":"UV induced mass‐independent sulfur isotope fractionation in stratospheric volcanic sulfate","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":205,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institut Polaire Français Paul Emile Victor; Polar Knowledge Canada; Fondazione Internazionale Premio Balzan; National Science Foundation","keywords":"Volcano; Stratosphere; Sulfate; Volcanic Gases; Ozone depletion; Sulfate aerosol; Plume; Geology; Sulfur; Mass-independent fractionation; Atmospheric sciences; Geochemistry; Isotope fractionation; Chemistry; Fractionation; Meteorology; Physics","score_opus":0.03494668488138185,"score_gpt":0.2848585210660106,"score_spread":0.24991183618462876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028554965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992993,0.00013703761,0.000115741765,0.000012589058,0.0000044528456,0.0000024389878,0.000069316004,0.000013356415,0.00034576326],"genre_scores_gemma":[0.99908006,0.00008633387,0.0001070079,0.000014154676,0.000004741277,0.0000029995283,0.0001452242,0.0000044639764,0.00055503193],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999664,0.0000053264,0.000001252485,0.000007745537,0.000008927258,0.000010235112],"domain_scores_gemma":[0.99992967,0.00001402171,0.0000150942005,0.000010281735,0.000015975818,0.000014911577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069853384,0.00015882586,0.000098119046,0.000234974,0.00011288248,0.0001688658,0.000098601806,0.00019874756,0.0012345138],"category_scores_gemma":[0.00011264217,0.0001189258,0.0001398997,0.00011598325,0.00021418223,0.00009068212,0.00012491847,0.00016470933,0.00015431421],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037036272,0.000020998421,0.0050516585,0.000015058505,0.000011238293,0.00005208879,0.000042523,0.000044642497,0.9925109,0.00004063773,0.000043182135,0.0017967112],"study_design_scores_gemma":[0.000033285178,0.0004956194,0.28153104,0.000003976588,0.000028655772,0.000236251,0.00008241469,0.0007172943,0.715972,0.00011756408,0.00077400333,0.000007883615],"about_ca_topic_score_codex":0.0013906526,"about_ca_topic_score_gemma":0.0012014855,"teacher_disagreement_score":0.0013906526,"about_ca_system_score_codex":0.00019964727,"about_ca_system_score_gemma":0.00008543925,"threshold_uncertainty_score":0.004129827},"labels":[],"label_agreement":null},{"id":"W2028635687","doi":"10.1029/2003gl017754","title":"The influence of phase boundary deflection on velocity anomalies of stagnant slabs in the transition zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Subduction; Slab; Transition zone; Slab window; Discontinuity (linguistics); Geophysics; Deflection (physics); Mantle wedge; Mantle (geology); Seismic tomography; Seismology; Mantle convection; Mechanics; Physics; Tectonics; Oceanic crust; Optics","score_opus":0.02662603596190203,"score_gpt":0.299776902851212,"score_spread":0.27315086688930995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028635687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99955064,0.000024668536,0.00025367358,0.000012272358,7.5108005e-7,5.4984105e-7,0.000014713562,0.000013153202,0.00012968629],"genre_scores_gemma":[0.99987304,0.000014193212,0.00006254848,0.0000013247968,5.8105763e-7,3.396035e-7,0.0000213419,0.0000033469878,0.000023283139],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995816,0.000008676222,0.0000026180103,0.000008122466,0.0000080753825,0.000014331381],"domain_scores_gemma":[0.9997888,0.000076183605,0.000050584793,0.000017345908,0.00002320426,0.000043917487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010843239,0.00013952254,0.00012858219,0.000287971,0.00017915912,0.00038227043,0.00013075472,0.00014637977,0.0005250871],"category_scores_gemma":[0.0009919093,0.00015660396,0.00012981391,0.00015907062,0.00036860388,0.00019875079,0.00034343405,0.0002324491,0.00007214363],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012954612,0.00006590087,0.22200786,0.00004922984,0.00006890773,0.0005519554,0.00046787798,0.069746755,0.6916636,0.001430545,0.00015340162,0.012498422],"study_design_scores_gemma":[0.00011843409,0.00031080542,0.7280951,0.000015310185,0.00006917093,0.0002963337,0.00031154047,0.17704694,0.09177643,0.0013539905,0.0005655625,0.000040407267],"about_ca_topic_score_codex":0.005294467,"about_ca_topic_score_gemma":0.0029725966,"teacher_disagreement_score":0.005294467,"about_ca_system_score_codex":0.00034199317,"about_ca_system_score_gemma":0.00022431412,"threshold_uncertainty_score":0.010527313},"labels":[],"label_agreement":null},{"id":"W2028754750","doi":"10.1002/2014gl061027","title":"Long‐term sea level trends: Natural or anthropogenic?","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Complex Systems and Time Series Analysis","field":"Economics, Econometrics and Finance","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique; University of Toronto; Centre National d’Etudes Spatiales; Agence Nationale de la Recherche","keywords":"Sea level; Detrended fluctuation analysis; Term (time); Natural (archaeology); Climatology; Period (music); Environmental science; Geology; Oceanography; Mathematics","score_opus":0.10043669683718585,"score_gpt":0.3202148026234015,"score_spread":0.21977810578621565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028754750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99031454,0.001304833,0.0022644484,0.0009705289,0.00004039754,0.0000033465783,0.0009925017,0.000026199783,0.004083281],"genre_scores_gemma":[0.9990921,0.00034078016,0.00014807106,0.000023734066,0.000035947007,9.343642e-7,0.00022878232,0.0000023005784,0.00012734637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998679,0.00003316492,0.000017427868,0.000029543859,0.000038677477,0.000013299149],"domain_scores_gemma":[0.99811745,0.0004428897,0.0009840975,0.00012771605,0.00025033482,0.00007748137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039666615,0.00009119288,0.00013711254,0.0008848319,0.00014013454,0.0009123738,0.0001395465,0.00013277389,0.0011466411],"category_scores_gemma":[0.0023470605,0.000045859273,0.00009058014,0.002397764,0.0004704155,0.00065253937,0.0002832264,0.00019205877,0.00013616613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070438415,0.00001991479,0.96318144,0.000090449714,0.00009666588,0.00013375291,0.00024334798,0.0019085672,0.001018542,0.0042082225,0.0008662558,0.028162533],"study_design_scores_gemma":[0.0000016427267,0.000033920605,0.9860532,0.000039371596,0.000030334748,0.00011004561,0.00047597833,0.007125316,0.0005153151,0.0028824182,0.0027237341,0.000008729054],"about_ca_topic_score_codex":0.0030635654,"about_ca_topic_score_gemma":0.005429806,"teacher_disagreement_score":0.0030635654,"about_ca_system_score_codex":0.00033545372,"about_ca_system_score_gemma":0.0001829649,"threshold_uncertainty_score":0.0060914755},"labels":[],"label_agreement":null},{"id":"W2028767031","doi":"10.1002/2013gl059116","title":"Seismic anisotropy of the Archean crust in the Minnesota River Valley, Superior Province","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Rhodes University; University of Minnesota; National Science Foundation","keywords":"Geology; Crust; Layering; Seismic anisotropy; Anisotropy; Gneiss; Mantle (geology); Archean; Lithosphere; Geophysics; Shear (geology); Seismology; Shear wave splitting; Shear zone; Petrology; Geochemistry; Metamorphic rock; Tectonics","score_opus":0.02319170673660253,"score_gpt":0.25793319657962865,"score_spread":0.23474148984302612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028767031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972928,0.00012954349,0.000045140172,0.000041586904,0.0000014162791,0.0000019789563,0.00059959205,0.000008375662,0.001879435],"genre_scores_gemma":[0.99924016,0.000047678004,0.00006470889,0.0000045048096,9.680838e-7,6.7384406e-7,0.00024233494,0.0000011529997,0.0003978206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.000005875515,0.0000048520756,0.000028087352,0.000018896524,0.000015501844],"domain_scores_gemma":[0.9998331,0.00001328511,0.000033708548,0.000009709682,0.00007405467,0.000036065863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013527121,0.000115000024,0.00008885542,0.0009882748,0.00044651577,0.00054978934,0.00018733852,0.00011515442,0.001178845],"category_scores_gemma":[0.00035831195,0.00013710406,0.0000776468,0.0008941989,0.00025863247,0.00011334456,0.00037404496,0.00009838335,0.00013751649],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046930913,0.000010337797,0.9851719,0.000018663573,0.000040346007,0.000109804634,0.0007901264,0.00074598426,0.0048469473,0.00024691934,0.00040356882,0.007568515],"study_design_scores_gemma":[0.0000016089402,0.0000029881753,0.9988244,0.0000043333393,0.0000039190745,0.000014040769,0.00022105215,0.00033187846,0.00010067118,0.000013695636,0.00048001023,0.0000013472769],"about_ca_topic_score_codex":0.6951072,"about_ca_topic_score_gemma":0.8670208,"teacher_disagreement_score":0.6951072,"about_ca_system_score_codex":0.0019380649,"about_ca_system_score_gemma":0.0010487834,"threshold_uncertainty_score":0.6133767},"labels":[],"label_agreement":null},{"id":"W2028833876","doi":"10.1029/2007gl029359","title":"Is isotropic turbulence relevant in the atmosphere?","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"National Oceanic and Atmospheric Administration","keywords":"Isotropy; Anisotropy; Scaling; Turbulence; Atmosphere (unit); Physics; Geophysics; Statistical physics; Meteorology; Computational physics; Optics; Geometry; Mathematics","score_opus":0.042657928147838566,"score_gpt":0.3239370483651401,"score_spread":0.2812791202173015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2028833876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7150131,0.059471343,0.042706963,0.076021984,0.0032170431,0.000022667386,0.00070750446,0.0002735065,0.102565795],"genre_scores_gemma":[0.988727,0.0074689696,0.0008463132,0.0011463603,0.0009247285,0.000004594388,0.00008144858,0.000018773719,0.0007817625],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99960417,0.00011223544,0.000016966245,0.00007126054,0.000094339266,0.00010105202],"domain_scores_gemma":[0.9991598,0.00038851678,0.00016017785,0.00011460108,0.0000891916,0.00008763898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007471474,0.00021965621,0.00057596224,0.00048495148,0.0006739583,0.002810057,0.0003440921,0.0010706057,0.0012826945],"category_scores_gemma":[0.0037881883,0.0002442109,0.00038912837,0.0008196579,0.0025035013,0.0034363873,0.0009000101,0.0011702813,0.00035374807],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001536167,0.00005114507,0.025073603,0.00039543508,0.00009583686,0.0008255833,0.00075015635,0.008090076,0.0046838364,0.9115145,0.010264404,0.03810171],"study_design_scores_gemma":[0.000013748415,0.000015536916,0.012077446,0.000064828026,0.00002366983,0.00016051781,0.00049003516,0.006915947,0.000367134,0.97121406,0.008632037,0.000025037642],"about_ca_topic_score_codex":0.00260597,"about_ca_topic_score_gemma":0.0018680984,"teacher_disagreement_score":0.002810057,"about_ca_system_score_codex":0.0005429092,"about_ca_system_score_gemma":0.00055825216,"threshold_uncertainty_score":0.0051816106},"labels":[],"label_agreement":null},{"id":"W2029247260","doi":"10.1029/2008gl034458","title":"Multipoint observations of magnetospheric compression‐related EMIC Pc1 waves by THEMIS and CARISMA","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":169,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center; Canadian Space Agency; University of Alberta","keywords":"Emic and etic; Physics; Solar wind; Geophysics; Computational physics; Astrophysics; Van Allen Probes; Magnetosphere; Plasma; Van Allen radiation belt; Nuclear physics","score_opus":0.024060581000858703,"score_gpt":0.26514973830510236,"score_spread":0.24108915730424366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029247260","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9917706,0.00011942972,0.00027373293,0.000081892606,0.0000113919505,0.000013528508,0.0005430661,0.00005892527,0.007127426],"genre_scores_gemma":[0.99676895,0.00007696168,0.0011346265,0.000029232067,0.0000302906,0.000015136253,0.0010398255,0.00001043913,0.00089451653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981767,0.000013864757,0.0000042614492,0.000044721124,0.00007319524,0.000046249414],"domain_scores_gemma":[0.9996942,0.000024345582,0.000068452304,0.000038779963,0.000084906795,0.00008942179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031563998,0.00031962595,0.0002960508,0.0010706084,0.0008161623,0.000462291,0.000373151,0.00034312808,0.00065783167],"category_scores_gemma":[0.0004041446,0.0002621006,0.00020933589,0.00089448446,0.00020601526,0.00028696406,0.0007631152,0.0005702567,0.00018977621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013594662,0.00026068083,0.6673828,0.00011616604,0.0003490724,0.0009995218,0.0029321727,0.0016751762,0.24646802,0.0013993063,0.0056298575,0.071427725],"study_design_scores_gemma":[0.000029215294,0.00009446466,0.9889443,0.0000091317825,0.000039259823,0.00017313955,0.0002772314,0.0011205612,0.004627648,0.000069691014,0.0046034446,0.000011955428],"about_ca_topic_score_codex":0.011762845,"about_ca_topic_score_gemma":0.045848344,"teacher_disagreement_score":0.011762845,"about_ca_system_score_codex":0.0006472826,"about_ca_system_score_gemma":0.0003464793,"threshold_uncertainty_score":0.023388803},"labels":[],"label_agreement":null},{"id":"W2029300460","doi":"10.1029/2004gl021962","title":"Comment on “The 2003 North American electrical blackout: An accidental experiment in atmospheric chemistry” by L. T. Marufu et al.","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Lightning and Electromagnetic Phenomena","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Blackout; Meteorology; Environmental science; Atmospheric chemistry; Lightning (connector); Accidental; Atmospheric sciences; Atmospheric electricity; Geology; Physics; Ozone; Thermodynamics","score_opus":0.011420059910705561,"score_gpt":0.2922357035050326,"score_spread":0.28081564359432704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029300460","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00089492707,0.0016416904,0.00034690707,0.92712015,0.06667457,0.000052984225,0.0004987859,0.00023194637,0.002538053],"genre_scores_gemma":[0.003556388,0.0010309104,0.00034530598,0.95087934,0.03956688,0.00007056636,0.00011367821,0.00007183378,0.004365047],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9969068,0.0005311301,0.00041618114,0.0007081464,0.0011124166,0.00032530574],"domain_scores_gemma":[0.9908664,0.004137318,0.000772466,0.00053418876,0.0028552627,0.0008342757],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0048560095,0.001568837,0.0014579959,0.00081577594,0.0033232109,0.0022024906,0.0038535914,0.03500863,0.0073319594],"category_scores_gemma":[0.018096976,0.00076521677,0.0014738496,0.00097562047,0.0031880795,0.003863349,0.0016458867,0.02982297,0.008319055],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006493322,0.000023644856,0.00034503473,0.000049805923,0.000010936007,0.00031499367,0.00012036144,0.000034141583,0.00017205617,0.00057022535,0.9951782,0.0031156058],"study_design_scores_gemma":[0.00009405178,0.00009183987,0.0027639454,0.00028981038,0.000031740215,0.00074575725,0.0006279418,0.00028460528,0.0007597853,0.0024519295,0.9917672,0.00009153235],"about_ca_topic_score_codex":0.01704209,"about_ca_topic_score_gemma":0.018686628,"teacher_disagreement_score":0.03500863,"about_ca_system_score_codex":0.0030371132,"about_ca_system_score_gemma":0.0041566305,"threshold_uncertainty_score":0.033885837},"labels":[],"label_agreement":null},{"id":"W2029356185","doi":"10.1029/2000gl011790","title":"Deformation of Earth's inner core by electromagnetic forces","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Inner core; Hydrostatic equilibrium; Lorentz force; Deformation (meteorology); Anisotropy; Core (optical fiber); Physics; Geology; Mechanics; Flow (mathematics); Classical mechanics; Lorentz transformation; Body force; Outer core; Geophysics; Magnetic field; Optics","score_opus":0.013755604689787895,"score_gpt":0.27227510098964613,"score_spread":0.25851949629985826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029356185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99100643,0.00019636675,0.0029143563,0.00009256771,0.000008599962,0.000002958567,0.00001846454,0.000024465578,0.0057357284],"genre_scores_gemma":[0.9991184,0.00011146149,0.00041204292,0.00001181608,0.0000046605433,0.0000012336603,0.000016444978,0.0000041706817,0.000319834],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99996114,0.000004788921,0.0000020485234,0.000006831479,0.000010593603,0.000014664037],"domain_scores_gemma":[0.9999306,0.00001190099,0.000023007588,0.000010046308,0.000010120834,0.000014271766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011578059,0.00017237225,0.000199148,0.00023830871,0.0003398557,0.00053082465,0.00014567381,0.00015501252,0.0006970841],"category_scores_gemma":[0.00031235247,0.0001199555,0.00018574447,0.00011267246,0.0005091907,0.0003032757,0.00047361362,0.00016171455,0.00017774006],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020798123,0.00005771273,0.03274937,0.0001021025,0.000037914288,0.0006883114,0.0003657146,0.021730354,0.87508994,0.04541851,0.00042714513,0.023124916],"study_design_scores_gemma":[0.00018674898,0.0005479396,0.52066857,0.000036619524,0.00008908738,0.0018893968,0.00063097005,0.14260648,0.26099914,0.060272127,0.0119781345,0.00009480346],"about_ca_topic_score_codex":0.0011816015,"about_ca_topic_score_gemma":0.00078717223,"teacher_disagreement_score":0.0011816015,"about_ca_system_score_codex":0.00031071357,"about_ca_system_score_gemma":0.00021967338,"threshold_uncertainty_score":0.0023494363},"labels":[],"label_agreement":null},{"id":"W2029362687","doi":"10.1029/2004gl021500","title":"Bedrock response to Llanquihue Holocene and present‐day glaciation in southernmost South America","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Aeronautics and Space Administration","keywords":"Geology; Bedrock; Post-glacial rebound; Holocene; Glacier; Glacial period; Mantle (geology); Physical geography; Geophysics; Earth science; Geodesy; Geomorphology; Paleontology","score_opus":0.024954157310305876,"score_gpt":0.289799457687775,"score_spread":0.2648453003774691,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029362687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993191,0.00006870936,0.000011819265,0.00006781136,0.0000014146772,8.500518e-7,0.00018305887,0.0000035375076,0.00034373446],"genre_scores_gemma":[0.99940634,0.000048328493,0.000018592124,0.00002471645,0.0000017199865,0.0000017018265,0.00027002348,0.0000014631511,0.00022705902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999948,0.000011466443,0.0000034376928,0.000011882825,0.00000767936,0.00001753336],"domain_scores_gemma":[0.99980325,0.000032651904,0.0000582067,0.000007900931,0.00004609885,0.00005190235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013227171,0.00010260075,0.00009729365,0.00047536218,0.0002817516,0.00034757637,0.00020070253,0.00025032015,0.00160618],"category_scores_gemma":[0.00050603,0.000092734794,0.00010860696,0.00046308732,0.00030233344,0.00020587917,0.00032355307,0.00017473234,0.0001302326],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000065764856,0.000021535381,0.9930397,0.000017326127,0.000026862755,0.00007774894,0.0006346546,0.00042071388,0.0012884148,0.00007838168,0.00048686514,0.00384204],"study_design_scores_gemma":[0.0000013918624,0.000003244366,0.9993949,0.000002430029,0.0000026713271,0.000010268751,0.00024596142,0.0001340828,0.000029085124,0.000013272388,0.00016192101,7.930291e-7],"about_ca_topic_score_codex":0.2221252,"about_ca_topic_score_gemma":0.49932232,"teacher_disagreement_score":0.2221252,"about_ca_system_score_codex":0.0009410532,"about_ca_system_score_gemma":0.00036991938,"threshold_uncertainty_score":0.44166458},"labels":[],"label_agreement":null},{"id":"W2029472371","doi":"10.1029/1999gl011243","title":"Capabilities of 3‐D wavelet transforms to detect plume‐like structures from seismic tomography","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Plume; Geology; Wavelet; Noise (video); Gaussian; Seismology; Computational physics; Physics; Meteorology; Computer science","score_opus":0.01649307748162653,"score_gpt":0.253898235840237,"score_spread":0.23740515835861048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2029472371","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22851646,0.00025357297,0.7684452,0.00021291412,0.00002755141,0.000040397354,0.0002157189,0.00071416836,0.0015740928],"genre_scores_gemma":[0.6334871,0.00059728674,0.36460605,0.00006692366,0.000045537585,0.0000624565,0.0005269426,0.00014676712,0.0004609885],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99975246,0.00007640865,0.000017525317,0.00002412592,0.0000984261,0.000031025567],"domain_scores_gemma":[0.99854374,0.00094274024,0.00012515324,0.0001670317,0.00017035178,0.00005108629],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014480264,0.00053148204,0.00026774025,0.0010480069,0.00014680078,0.0007425829,0.00033587008,0.000490961,0.00050116377],"category_scores_gemma":[0.0058648493,0.000342299,0.00044666862,0.0007726479,0.0004669689,0.0008613434,0.00092167465,0.0006844658,0.0003204125],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005399001,0.00016081205,0.0089240195,0.00022111056,0.00012499839,0.00034748358,0.00045360313,0.28193307,0.31743005,0.013014043,0.0011866057,0.37566423],"study_design_scores_gemma":[0.000036183275,0.00010025646,0.0051909992,0.00001702731,0.000030463214,0.00025429108,0.00005851355,0.9336398,0.05127116,0.008009958,0.0013373261,0.00005395402],"about_ca_topic_score_codex":0.0005699407,"about_ca_topic_score_gemma":0.0006375821,"teacher_disagreement_score":0.0014480264,"about_ca_system_score_codex":0.00013708013,"about_ca_system_score_gemma":0.0003058349,"threshold_uncertainty_score":0.007657945},"labels":[],"label_agreement":null},{"id":"W2030032594","doi":"10.1029/2005gl024186","title":"A Tibetan Taylor Cap and a halo of stratospheric ozone over the Himalaya","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Troposphere; Plateau (mathematics); Stratosphere; Atmospheric sciences; Ozone; Climatology; Sink (geography); Environmental science; Halo; Latitude; Ozone depletion; Northern Hemisphere; Geology; Geography; Meteorology; Astrophysics; Physics","score_opus":0.023025961636743465,"score_gpt":0.27431398583150435,"score_spread":0.2512880241947609,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030032594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983948,0.00020644371,0.000047126698,0.00004816874,0.0000031435884,0.0000016871808,0.000050517247,0.000005851974,0.0012422786],"genre_scores_gemma":[0.9997323,0.000057056535,0.000025897429,0.000016046914,0.000006762645,5.8566155e-7,0.000040275314,6.017727e-7,0.000120448414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999498,0.00000777524,0.000002057267,0.0000078923595,0.000011412656,0.000021003543],"domain_scores_gemma":[0.9998847,0.000013735602,0.000037199443,0.000009051447,0.000011922311,0.000043312775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087152,0.00011029163,0.000117675234,0.00057340314,0.00075652014,0.0006673253,0.00012538821,0.00015209262,0.0013067985],"category_scores_gemma":[0.00020503173,0.000121473764,0.000107647036,0.00064925564,0.0005680413,0.0002254058,0.0004206965,0.00013941576,0.000117701486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007806739,0.000059033395,0.90242374,0.00010739175,0.00015501623,0.0057589086,0.0035835938,0.00092666387,0.06905012,0.0014288542,0.0007900012,0.014935993],"study_design_scores_gemma":[0.0000070503534,0.00003174622,0.997276,0.0000065937124,0.000011385788,0.00058613514,0.00072217354,0.00016749301,0.00056872616,0.00016947399,0.00044751161,0.0000056565345],"about_ca_topic_score_codex":0.014741844,"about_ca_topic_score_gemma":0.018815238,"teacher_disagreement_score":0.014741844,"about_ca_system_score_codex":0.00037360558,"about_ca_system_score_gemma":0.00029966893,"threshold_uncertainty_score":0.029312074},"labels":[],"label_agreement":null},{"id":"W2030043506","doi":"10.1029/2006gl026122","title":"Earthquake recurrence as a record breaking process","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Perimeter Institute","funders":"","keywords":"Scaling; Induced seismicity; Magnitude (astronomy); Point process; Observer (physics); Scaling law; Statistical physics; Geology; Computer science; Seismology; Mathematics; Physics; Statistics; Geometry","score_opus":0.03510357604512188,"score_gpt":0.304952378250072,"score_spread":0.2698488022049501,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030043506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6470691,0.0018708792,0.31138018,0.0018095997,0.00011821647,0.0000662774,0.0011738833,0.00056456774,0.035947267],"genre_scores_gemma":[0.98389727,0.0006281578,0.010986455,0.00005367558,0.0001276046,0.000040659634,0.00030606898,0.00005634957,0.003903742],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994603,0.00010347169,0.00005111192,0.00019793783,0.00013363289,0.000053516018],"domain_scores_gemma":[0.99553573,0.0017080616,0.0013394792,0.0006766385,0.00043049504,0.0003096239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014370778,0.00026385268,0.00028877324,0.0013211797,0.00052124064,0.0020253623,0.0007354737,0.00066403364,0.0038968746],"category_scores_gemma":[0.008817383,0.00025066093,0.0003750433,0.0011695008,0.0012832694,0.0045528146,0.00095230644,0.0011240591,0.0004350784],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008314947,0.000033856526,0.0123216305,0.00009943075,0.000042313597,0.00025824463,0.0008666316,0.031334307,0.00531768,0.90915346,0.0013808213,0.039108578],"study_design_scores_gemma":[0.000041771484,0.00013022708,0.025483474,0.000045915694,0.00007744081,0.000487011,0.0002677793,0.23642845,0.0012926229,0.72578317,0.009904949,0.00005711309],"about_ca_topic_score_codex":0.0017993117,"about_ca_topic_score_gemma":0.00073578145,"teacher_disagreement_score":0.0038968746,"about_ca_system_score_codex":0.00064597576,"about_ca_system_score_gemma":0.0002877498,"threshold_uncertainty_score":0.013036311},"labels":[],"label_agreement":null},{"id":"W2030187298","doi":"10.1029/2007gl032876","title":"Biogenic silica concentration as a high‐resolution, quantitative temperature proxy at Hallet Lake, south‐central Alaska","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Proxy (statistics); Climate change; Paleoclimatology; Context (archaeology); Climatology; Biogenic silica; Geology; Sediment; High resolution; Temperature record; Environmental science; Physical geography; Oceanography; Geography; Geomorphology","score_opus":0.033543094612704445,"score_gpt":0.2834839807823934,"score_spread":0.24994088616968896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030187298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997069,0.00001576982,0.00010070864,0.0000051835887,6.8654333e-7,5.3181435e-7,0.000049751467,0.000007637891,0.00011272402],"genre_scores_gemma":[0.9995763,0.0000133528065,0.00023547378,0.0000017723899,7.1058963e-7,0.0000011840501,0.00008849446,0.0000015832243,0.000081166436],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999317,0.00001286258,0.0000079181655,0.000028971514,0.000011095981,0.000007567782],"domain_scores_gemma":[0.99984264,0.00003131028,0.00005475169,0.000015461152,0.000029834255,0.00002600823],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000278302,0.00015644293,0.000106607644,0.00055961625,0.0005562121,0.0005442771,0.00022571358,0.00021795447,0.00039302648],"category_scores_gemma":[0.00050518324,0.00020028753,0.00012192832,0.00045357793,0.00032484936,0.00039110653,0.00040305848,0.00017013647,0.000059309583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014686464,0.000031207113,0.9638365,0.000023417155,0.000091632486,0.00014908015,0.0007339928,0.007251655,0.020561643,0.000109987304,0.00012787913,0.0069361576],"study_design_scores_gemma":[0.000010208549,0.000022397731,0.98271585,0.000008995295,0.000032380725,0.00005365113,0.0005702006,0.012396417,0.0037950184,0.00009331534,0.00028743863,0.000014182726],"about_ca_topic_score_codex":0.045942407,"about_ca_topic_score_gemma":0.12714088,"teacher_disagreement_score":0.045942407,"about_ca_system_score_codex":0.0007241312,"about_ca_system_score_gemma":0.0003229755,"threshold_uncertainty_score":0.09134996},"labels":[],"label_agreement":null},{"id":"W2030466742","doi":"10.1029/2006gl027149","title":"Anomalously warm July 2005 in the northern California Current: Historical context and the significance of cumulative wind stress","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Upwelling; Hydrography; Oceanography; Wind stress; Context (archaeology); Climatology; Submarine pipeline; Current (fluid); Geology; Sea surface temperature; Environmental science","score_opus":0.019760307121679182,"score_gpt":0.2525500675760389,"score_spread":0.2327897604543597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030466742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984812,0.0005016952,0.00003672404,0.00009012759,0.000011949552,0.0000012100357,0.00021684189,0.000003974371,0.000656326],"genre_scores_gemma":[0.99935037,0.00026413822,0.00003098341,0.000011025813,0.000016203636,9.3542167e-7,0.00020124437,0.000001430036,0.00012364006],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998702,0.000013271761,0.0000103778775,0.000050233102,0.00002397382,0.000032027816],"domain_scores_gemma":[0.9990758,0.00010480072,0.00038097144,0.00006178556,0.00019402895,0.00018257518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038242625,0.00011542739,0.00015878225,0.000891946,0.0006364189,0.00084466895,0.00024396725,0.00030643027,0.0008451786],"category_scores_gemma":[0.0010065684,0.00015829156,0.00011365865,0.0010157102,0.00043206787,0.0004173838,0.00030419798,0.0003204189,0.000085199965],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033543252,0.000014660768,0.9951324,0.000012466995,0.00003440574,0.000044148914,0.00033614392,0.00014367247,0.0002856685,0.000096110765,0.00031900188,0.003547749],"study_design_scores_gemma":[5.6963813e-7,0.0000046568857,0.9994442,0.0000035672977,0.0000062479667,0.000018873146,0.00011854392,0.00006399089,0.000027897519,0.0000108748145,0.00029905717,0.0000015326816],"about_ca_topic_score_codex":0.067568965,"about_ca_topic_score_gemma":0.23653607,"teacher_disagreement_score":0.067568965,"about_ca_system_score_codex":0.000882447,"about_ca_system_score_gemma":0.00036605855,"threshold_uncertainty_score":0.13435131},"labels":[],"label_agreement":null},{"id":"W2030559577","doi":"10.1029/2006gl026638","title":"A simulation of a lake effect snowstorm with a cloud resolving numerical model","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Winter storm; Meteorology; Snow; Convection; Environmental science; Convective storm detection; Climatology; Geology; Storm; Severe weather; Computer simulation; Atmospheric sciences; Geography; Computer science; Simulation","score_opus":0.03203431815150895,"score_gpt":0.28465398297675776,"score_spread":0.2526196648252488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2030559577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98419327,0.00008739422,0.0035580567,0.0004756878,0.000047217145,0.000065386055,0.0010729292,0.00017718905,0.010322995],"genre_scores_gemma":[0.9937937,0.000050722872,0.004059847,0.000066842294,0.00001016152,0.000049881088,0.000613681,0.000025080111,0.0013300927],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985635,0.0000344295,0.0000073349397,0.000024304405,0.000027612587,0.000049831797],"domain_scores_gemma":[0.9993,0.00032445812,0.00006266784,0.000035196877,0.00009918466,0.00017840695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026384438,0.00043139147,0.0005145317,0.00035803605,0.00075731997,0.00087919435,0.0010818606,0.0014524333,0.0030401726],"category_scores_gemma":[0.0013089528,0.00032690231,0.00046943047,0.0006095161,0.0006923124,0.000583425,0.00069631764,0.00084109814,0.00018294743],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018300125,0.00017161759,0.005553683,0.00002511663,0.000028397128,0.0002319288,0.00006859138,0.9889187,0.0010918769,0.0016797824,0.00074901426,0.0012982698],"study_design_scores_gemma":[0.000056282704,0.00003344701,0.001054139,0.0000028374484,0.0000059218264,0.0000077936475,0.000039303235,0.9982236,0.00017829979,0.0001863444,0.00020659973,0.000005317381],"about_ca_topic_score_codex":0.055851195,"about_ca_topic_score_gemma":0.03548231,"teacher_disagreement_score":0.055851195,"about_ca_system_score_codex":0.0010583481,"about_ca_system_score_gemma":0.0012060364,"threshold_uncertainty_score":0.111052215},"labels":[],"label_agreement":null},{"id":"W2031216054","doi":"10.1029/2003gl019306","title":"Tharsis as a consequence of Mars' dichotomy and layered mantle","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Tharsis; Geology; Martian; Mars Exploration Program; Volcano; Upwelling; Mantle (geology); Astrobiology; Earth science; Geophysics; Martian surface; Mantle plume; Hesperian; Lithosphere; Tectonics; Paleontology","score_opus":0.034197976998285765,"score_gpt":0.30914578806849385,"score_spread":0.2749478110702081,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031216054","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904424,0.0001794791,0.00010726696,0.000026761378,0.0000040940727,0.000002168353,0.00003555176,0.000008647767,0.00059177633],"genre_scores_gemma":[0.99970907,0.000061686216,0.00004424068,0.000010005925,0.0000026685636,0.0000013713682,0.000037543716,8.335762e-7,0.00013263998],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999471,0.000010537464,0.000002107446,0.0000133165495,0.000008822653,0.000018086048],"domain_scores_gemma":[0.9999089,0.00001270124,0.00003536581,0.000015898688,0.0000045807647,0.000022544285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000072356386,0.00017719416,0.00011626473,0.00013410572,0.00023249343,0.000501288,0.00013043193,0.00021797442,0.0011869124],"category_scores_gemma":[0.00018916612,0.000072531795,0.00014494611,0.00013614196,0.00048866624,0.00018326014,0.00037205624,0.00034402683,0.00008013224],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011199573,0.00007095778,0.048303902,0.000057635592,0.000054512,0.0020324793,0.00030986554,0.0005851193,0.93670547,0.0020969242,0.00021490447,0.00844826],"study_design_scores_gemma":[0.00010611702,0.0009790182,0.87568146,0.000013719465,0.000093256866,0.00609804,0.0007692082,0.0021972393,0.10671913,0.002549518,0.004765078,0.000028220078],"about_ca_topic_score_codex":0.0011320582,"about_ca_topic_score_gemma":0.0008325736,"teacher_disagreement_score":0.0011869124,"about_ca_system_score_codex":0.00023970378,"about_ca_system_score_gemma":0.000089505134,"threshold_uncertainty_score":0.003970623},"labels":[],"label_agreement":null},{"id":"W2031515918","doi":"10.1029/1999gl011326","title":"Microbial degradation is a key elimination pathway of hexachlorocyclohexanes from the Arctic Ocean","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Toxic Organic Pollutants Impact","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Arctic; Environmental science; Microbial biodegradation; Environmental chemistry; Degradation (telecommunications); The arctic; Surface water; Oceanography; Chemistry; Environmental engineering; Geology; Microorganism; Bacteria","score_opus":0.019844705180416717,"score_gpt":0.2654474771717008,"score_spread":0.24560277199128408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031515918","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954319,0.0006854011,0.002475178,0.000023172517,0.000004671765,0.000008878221,0.00031216975,0.000025342979,0.0010332838],"genre_scores_gemma":[0.9956999,0.0010098588,0.0019903998,0.000009834553,0.000002131932,0.000006111889,0.00059184094,0.00000912143,0.00068079133],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998635,0.000013668485,0.000007993724,0.000034252505,0.000047595542,0.000032985197],"domain_scores_gemma":[0.99988127,0.000017877368,0.000026976855,0.000006416052,0.000056513807,0.000010937411],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001924452,0.0005341524,0.00023756821,0.00022078436,0.00033935872,0.0006388336,0.00009929967,0.00016593165,0.00045487276],"category_scores_gemma":[0.00024557777,0.00017711832,0.0003677219,0.00024943933,0.00016051765,0.00021859944,0.00018744374,0.0002343815,0.00018645533],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00079920166,0.000057915422,0.14177696,0.0003487691,0.00017772031,0.00033446617,0.00019337112,0.022868881,0.80073524,0.00051453186,0.00024688474,0.03194593],"study_design_scores_gemma":[0.000023278086,0.00063995324,0.2744798,0.000043070417,0.0002035899,0.0005076504,0.00049457746,0.043182433,0.67456836,0.0004476653,0.005366499,0.000043158037],"about_ca_topic_score_codex":0.040920217,"about_ca_topic_score_gemma":0.024009041,"teacher_disagreement_score":0.040920217,"about_ca_system_score_codex":0.0007727554,"about_ca_system_score_gemma":0.00059082836,"threshold_uncertainty_score":0.081364095},"labels":[],"label_agreement":null},{"id":"W2031578087","doi":"10.1029/2009gl037160","title":"Spatiotemporal gravity changes on volcanoes: Assessing the importance of topography","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministerio de Ciencia e Innovación","keywords":"Geology; Volcano; Deformation (meteorology); Gravity anomaly; Seismology; Mass movement; Magma; Geophysics; Geodesy; Gravity current; Landslide","score_opus":0.052555781480583263,"score_gpt":0.3283430005099931,"score_spread":0.27578721902940984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031578087","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991578,0.00004071865,0.00055862754,0.000012672516,0.00000102411,0.000002562558,0.00005588807,0.000012642701,0.00015800114],"genre_scores_gemma":[0.9996805,0.000028564205,0.0002247782,0.0000011516953,0.0000019729873,0.0000010135276,0.000037775837,0.000001766358,0.000022443342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998988,0.000023812405,0.000010323271,0.00002291996,0.000025401048,0.000018715898],"domain_scores_gemma":[0.9994241,0.0002335349,0.00017111952,0.00005544333,0.00006390301,0.00005200433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033779241,0.00019681685,0.00017938578,0.0008593705,0.00012615202,0.00030189415,0.00025876393,0.00031180232,0.0004197091],"category_scores_gemma":[0.0021435583,0.00009603398,0.00024389282,0.00053513516,0.00033289264,0.0005493386,0.00041955808,0.00011331302,0.00005949998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004731838,0.0001559728,0.7946145,0.00013465407,0.0002042332,0.00074007065,0.00034187917,0.10945323,0.05728023,0.0012030222,0.00023137312,0.035167575],"study_design_scores_gemma":[0.000016914335,0.000188682,0.7838143,0.00000884238,0.00005134333,0.0002063156,0.00023730002,0.21149053,0.0034434304,0.00037566468,0.0001503984,0.000016172606],"about_ca_topic_score_codex":0.004868431,"about_ca_topic_score_gemma":0.003996985,"teacher_disagreement_score":0.004868431,"about_ca_system_score_codex":0.000299951,"about_ca_system_score_gemma":0.00012912895,"threshold_uncertainty_score":0.009680152},"labels":[],"label_agreement":null},{"id":"W2031605732","doi":"10.1029/2003gl017406","title":"Tropical/Extratropical forcing of the AO/NAO: A corrigendum","year":2003,"lang":"en","type":"erratum","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Dalhousie University","funders":"","keywords":"Extratropical cyclone; Forcing (mathematics); Climatology; Environmental science; Tropics; The arctic; Atmospheric sciences; Geology; Oceanography; Biology","score_opus":0.053564422680091865,"score_gpt":0.30381234800172446,"score_spread":0.2502479253216326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031605732","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0008577771,0.0048584677,0.0025497247,0.023699993,0.9624242,0.00003909248,0.0008822031,0.00051604514,0.004172458],"genre_scores_gemma":[0.065491065,0.035449635,0.020518282,0.15761936,0.42532882,0.0005885643,0.005054547,0.0044814493,0.2854683],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99862003,0.000233214,0.00025755665,0.00035882855,0.0004367095,0.00009368791],"domain_scores_gemma":[0.99215347,0.0014493994,0.00038493887,0.0010481641,0.0047064084,0.0002576013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018791355,0.0023542698,0.001634394,0.0022888058,0.0019659803,0.0033432788,0.0024363361,0.0026403742,0.01454125],"category_scores_gemma":[0.019068506,0.0008617891,0.0014771768,0.002412354,0.001841963,0.001726072,0.0017361564,0.004715687,0.012451564],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009580669,0.000030427665,0.00072474725,0.0004372874,0.000047390222,0.00057125895,0.00004977824,0.0005040611,0.0003293572,0.002044491,0.97011423,0.025051236],"study_design_scores_gemma":[0.000072701754,0.000105789215,0.0055346023,0.00050859974,0.00013705346,0.0010171257,0.00015232585,0.002553148,0.001732491,0.004300654,0.98375815,0.00012732546],"about_ca_topic_score_codex":0.04109002,"about_ca_topic_score_gemma":0.03911213,"teacher_disagreement_score":0.04109002,"about_ca_system_score_codex":0.0033257045,"about_ca_system_score_gemma":0.0023777832,"threshold_uncertainty_score":0.081701696},"labels":[],"label_agreement":null},{"id":"W2031696126","doi":"10.1029/2007gl029482","title":"Formation and spreading of Eurasian source oxygen‐rich halocline water into the Canadian Basin in the Arctic Ocean","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Halocline; Ocean gyre; Geology; Oceanography; Canada Basin; Structural basin; Ridge; Arctic; Potential vorticity; Plateau (mathematics); Climatology; Geomorphology; Paleontology; Geography; Vorticity; Salinity","score_opus":0.04533089116941866,"score_gpt":0.28787857898509256,"score_spread":0.2425476878156739,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031696126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730766,0.00030002985,0.000057931156,0.0000719961,0.0000025353072,0.00000523437,0.00034234874,0.000005684299,0.0019066212],"genre_scores_gemma":[0.99878746,0.00028796293,0.00015521316,0.000019492918,0.0000012239183,0.000002669604,0.000235161,0.0000028067486,0.00050799764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982613,0.0000103361945,0.0000063871644,0.0000410093,0.00005340364,0.00006269043],"domain_scores_gemma":[0.9993849,0.000027238248,0.000099049874,0.000017092923,0.00037140638,0.00010029115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002707475,0.00018640341,0.00016035856,0.0014827782,0.0015839112,0.0009217743,0.00033053602,0.00015165035,0.00055688823],"category_scores_gemma":[0.0006462236,0.00013118057,0.0001848138,0.0017305855,0.0005118352,0.0002634663,0.0006007516,0.000168587,0.000054112857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009652823,0.000010904185,0.97475344,0.000033844353,0.000051529074,0.00016365774,0.0023180125,0.00045211572,0.0043966044,0.00031196207,0.0005113151,0.016900036],"study_design_scores_gemma":[0.000001856315,0.000005305835,0.99765044,0.000009017983,0.00000965041,0.000029923029,0.0008508107,0.00021878371,0.00021200896,0.000013616996,0.0009934397,0.0000052256282],"about_ca_topic_score_codex":0.977711,"about_ca_topic_score_gemma":0.99283797,"teacher_disagreement_score":0.977711,"about_ca_system_score_codex":0.007608141,"about_ca_system_score_gemma":0.010510796,"threshold_uncertainty_score":0.055201232},"labels":[],"label_agreement":null},{"id":"W2031902169","doi":"10.1029/2006gl026906","title":"Decadal variability of subpolar gyre transport and its reverberation in the North Atlantic overturning","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":276,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Oceanography; Boundary current; Climatology; Hydrography; Geology; Hindcast; North Atlantic oscillation; Sea-surface height; North Atlantic Deep Water; Thermohaline circulation; Shutdown of thermohaline circulation; Ocean current; Gulf Stream; Current (fluid); Subtropics; Sea surface temperature","score_opus":0.015240927260467142,"score_gpt":0.2405807775486628,"score_spread":0.22533985028819567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031902169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994336,0.000032267595,0.00015215272,0.000039259383,0.000003749775,7.516635e-7,0.00007997015,0.000015182028,0.00024311942],"genre_scores_gemma":[0.9997378,0.00001918795,0.000051839594,0.000006880594,0.0000015180257,8.2457547e-7,0.00009560492,0.0000031687985,0.00008321832],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999567,0.000010182519,0.0000030772376,0.0000151788545,0.0000055540713,0.00000923023],"domain_scores_gemma":[0.999816,0.000050787305,0.00004457683,0.000028633322,0.000028388666,0.000031697615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022294035,0.00013758273,0.00017156189,0.00020700136,0.00016401663,0.00053965446,0.00012610247,0.0002296917,0.00061157456],"category_scores_gemma":[0.0008180029,0.00014483849,0.00018910265,0.00017018351,0.0001706105,0.00025204444,0.00024150229,0.00026190624,0.00011826366],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052506983,0.00013486992,0.8698023,0.00003643386,0.00026467512,0.0003280524,0.0005347801,0.08752519,0.02296399,0.0014737243,0.0012832746,0.0151277445],"study_design_scores_gemma":[0.000029552351,0.00008225593,0.8626863,0.0000074639006,0.00006266773,0.00007786973,0.00018759207,0.13319196,0.0022208712,0.0004268562,0.0010038472,0.000022843105],"about_ca_topic_score_codex":0.010759685,"about_ca_topic_score_gemma":0.01129442,"teacher_disagreement_score":0.010759685,"about_ca_system_score_codex":0.0003186733,"about_ca_system_score_gemma":0.00015874092,"threshold_uncertainty_score":0.021394134},"labels":[],"label_agreement":null},{"id":"W2031962675","doi":"10.1029/2006gl025953","title":"Oceanic deep water formation as a sink of persistent organic pollutants","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Environmental science; Sink (geography); Surface water; Total organic carbon; Deep sea; Deep ocean water; Deep water; Water column; Thermohaline circulation; Settling; Pollutant; North Atlantic Deep Water; Salinity; Environmental chemistry; Geology; Chemistry","score_opus":0.01618430369403181,"score_gpt":0.23034919424715705,"score_spread":0.21416489055312524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2031962675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946202,0.0006765386,0.0021041732,0.00009017044,0.000012719921,0.000011230003,0.0004977147,0.000055033,0.0019322601],"genre_scores_gemma":[0.9956701,0.0007771638,0.0013130046,0.00004964484,0.0000049346872,0.000007539569,0.00063962815,0.000025665024,0.0015123115],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989486,0.000008680945,0.0000058330816,0.000035887377,0.00002545874,0.000029171251],"domain_scores_gemma":[0.9998759,0.000016296019,0.00003534091,0.0000106870775,0.00003475446,0.00002705524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014707989,0.00041129015,0.00031632712,0.00046456454,0.00023727915,0.00075477565,0.0001956579,0.00028469783,0.0008348142],"category_scores_gemma":[0.00018355042,0.00023379251,0.00026328853,0.00052052864,0.00018429733,0.000529538,0.0007839384,0.00025091297,0.0003071211],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029715974,0.000039957096,0.21885297,0.0003214891,0.00009402647,0.00034420853,0.0002967925,0.0036207265,0.74372566,0.0012410436,0.0004774632,0.030688468],"study_design_scores_gemma":[0.000094020965,0.00056777144,0.7767373,0.000055326975,0.00030423162,0.0003820602,0.0014124824,0.02188284,0.16999455,0.0025371092,0.025973346,0.000059002858],"about_ca_topic_score_codex":0.012391846,"about_ca_topic_score_gemma":0.010877725,"teacher_disagreement_score":0.012391846,"about_ca_system_score_codex":0.00077204726,"about_ca_system_score_gemma":0.00061556336,"threshold_uncertainty_score":0.024639428},"labels":[],"label_agreement":null},{"id":"W2032076428","doi":"10.1029/2009gl041158","title":"Evidence for significant photochemical production of carbon monoxide by particles in coastal and oligotrophic marine waters","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Colored dissolved organic matter; Particulates; Seawater; Biogeochemical cycle; Environmental chemistry; Dissolved organic carbon; Environmental science; Carbon monoxide; Photic zone; Oceanography; Chemistry; Phytoplankton; Geology","score_opus":0.043405693542917366,"score_gpt":0.2811100312785518,"score_spread":0.2377043377356344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032076428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992574,0.00016159669,0.0001153968,0.000013374082,0.0000026067316,0.0000031925279,0.00007336074,0.000003307484,0.0003697446],"genre_scores_gemma":[0.9991697,0.0001558831,0.00022318088,0.000016298056,0.000003853782,0.0000047992435,0.00020324087,0.0000016984842,0.00022144681],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99987817,0.000008387689,0.000011742602,0.000039035654,0.00004431764,0.000018302519],"domain_scores_gemma":[0.99974674,0.000054317967,0.00006742249,0.000020316624,0.000052038235,0.000059138423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012674018,0.0003222841,0.00019351,0.00034223584,0.00043123052,0.0004555102,0.00017112779,0.00038558914,0.000540819],"category_scores_gemma":[0.00021002503,0.00029726073,0.00022392819,0.00024147051,0.00046157683,0.00018789306,0.0004379022,0.000252212,0.00011988059],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000257919,0.00003652485,0.19802041,0.000076657525,0.0000419954,0.00022191259,0.00027274844,0.00009289503,0.7982709,0.0000475863,0.000043195178,0.0026173317],"study_design_scores_gemma":[0.0000206841,0.00040920888,0.9001713,0.000009059287,0.0000627395,0.0005910427,0.00042116965,0.00022457914,0.097376436,0.000051510495,0.0006536514,0.000008640649],"about_ca_topic_score_codex":0.0050466903,"about_ca_topic_score_gemma":0.0061125467,"teacher_disagreement_score":0.0050466903,"about_ca_system_score_codex":0.00029411356,"about_ca_system_score_gemma":0.00021247934,"threshold_uncertainty_score":0.010034621},"labels":[],"label_agreement":null},{"id":"W2032329011","doi":"10.1029/2001gl014592","title":"Properties of near surface marine sediments from wavelet correlation analysis","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Geology; Wavelet; Dispersion (optics); Porosity; Cross-correlation; Fourier transform; Mineralogy; Geophysics; Physics; Geotechnical engineering; Optics; Statistics; Mathematics","score_opus":0.04402210971936056,"score_gpt":0.25331452703754215,"score_spread":0.2092924173181816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032329011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81254244,0.0005084723,0.18283412,0.00007405101,0.000031395502,0.000021729284,0.00034353422,0.000242301,0.0034019083],"genre_scores_gemma":[0.9800637,0.0004494079,0.018185614,0.000014935855,0.000028283868,0.000009754482,0.0004938094,0.00006464605,0.0006899305],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998554,0.000021327853,0.000006457924,0.000021043865,0.000077873556,0.00001796148],"domain_scores_gemma":[0.9996112,0.00011833069,0.00007472624,0.000046438552,0.00012934374,0.00002004728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031954248,0.000312897,0.00026093546,0.0008948169,0.00013664385,0.0005639789,0.00014221974,0.00020206663,0.0008297548],"category_scores_gemma":[0.0018940027,0.00019828779,0.00019757441,0.0011518691,0.0002990564,0.00070388656,0.0003890362,0.00034066406,0.00030780173],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000272422,0.00006733677,0.026991257,0.00028658562,0.000106738175,0.0008763325,0.00026906957,0.0946603,0.6545061,0.006492825,0.0013892528,0.21408182],"study_design_scores_gemma":[0.000024211102,0.00021262465,0.10249036,0.000045018067,0.00013214308,0.0011961894,0.00020928649,0.74050033,0.14321804,0.008140638,0.0037126562,0.00011842959],"about_ca_topic_score_codex":0.00084116706,"about_ca_topic_score_gemma":0.00083419355,"teacher_disagreement_score":0.0008948169,"about_ca_system_score_codex":0.000100682795,"about_ca_system_score_gemma":0.00021443683,"threshold_uncertainty_score":0.0027757883},"labels":[],"label_agreement":null},{"id":"W2032448857","doi":"10.1029/2005gl023714","title":"Long‐term tracking of climate change by underground temperatures","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; National Science Foundation","keywords":"Borehole; Geothermal gradient; Snow; Environmental science; Geology; Climate change; Geothermal energy; Term (time); Energy balance; Climatology; Atmospheric sciences; Geophysics; Geomorphology; Physics","score_opus":0.08895932455133491,"score_gpt":0.3331398689163927,"score_spread":0.24418054436505776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032448857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977634,0.00006460198,0.00093221216,0.0000458389,0.0000051283087,0.0000016361449,0.00037256195,0.000037308724,0.00077729713],"genre_scores_gemma":[0.9993156,0.000025053127,0.0002830709,0.000004768972,0.0000039671986,0.0000015810131,0.0002638242,0.0000044745093,0.000097717406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998894,0.000020134494,0.000009265414,0.00003296068,0.000022973358,0.00002524704],"domain_scores_gemma":[0.99925536,0.000119901815,0.00028157895,0.00011033617,0.00017778552,0.000055061202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026244367,0.000105382125,0.00012613626,0.0005519394,0.00021745337,0.00038309454,0.00017494489,0.0001828381,0.0006086717],"category_scores_gemma":[0.0011907263,0.00011101472,0.0001186821,0.0007316223,0.0002122724,0.0005437886,0.00032554695,0.00020133599,0.00014477856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010070264,0.000028624945,0.96140194,0.000016625567,0.000052322324,0.00007015343,0.00038852534,0.0012596147,0.017606255,0.0004170881,0.00039235104,0.018265836],"study_design_scores_gemma":[0.0000020347636,0.000023173452,0.99536103,0.0000037784373,0.000013370325,0.00005143506,0.000112617396,0.0022828807,0.0013587265,0.00017514016,0.00060914306,0.000006605322],"about_ca_topic_score_codex":0.0044789645,"about_ca_topic_score_gemma":0.009976451,"teacher_disagreement_score":0.0044789645,"about_ca_system_score_codex":0.00022961943,"about_ca_system_score_gemma":0.000111443434,"threshold_uncertainty_score":0.008905768},"labels":[],"label_agreement":null},{"id":"W2032915125","doi":"10.1029/2006gl027247","title":"Southern Ocean warming due to human influence","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Office of Science; Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"Effects of global warming on oceans; Climatology; Environmental science; Global warming; Climate change; Oceanography; Geology","score_opus":0.03063340333535365,"score_gpt":0.30729993802038563,"score_spread":0.276666534685032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2032915125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9822353,0.0009401083,0.0010132296,0.0008329553,0.000055150125,0.0000025962668,0.0006770994,0.00007684371,0.01416667],"genre_scores_gemma":[0.9989222,0.00035672344,0.00007233866,0.000043001466,0.000023972207,0.0000014018427,0.00013166144,0.0000036580504,0.000445183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.000014430791,0.0000021993953,0.000011676318,0.000009454038,0.000019032375],"domain_scores_gemma":[0.99982053,0.000062502506,0.000056031266,0.000021003952,0.000019797924,0.0000201552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111204376,0.0001959443,0.00011996625,0.00030392114,0.00018100842,0.00046066384,0.00008599975,0.00019561556,0.003570119],"category_scores_gemma":[0.00057654385,0.000092929105,0.0004059867,0.00037913327,0.00027117116,0.00024067108,0.0006271997,0.00022042953,0.00020754324],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060449285,0.0000617015,0.7196192,0.00026285043,0.0004664419,0.00131998,0.00068540656,0.1807635,0.011597711,0.016955998,0.008182428,0.059480168],"study_design_scores_gemma":[0.000046659272,0.000113076596,0.91214025,0.000052751762,0.00020049013,0.00061340566,0.00047597545,0.05106477,0.002938403,0.019820886,0.0124989,0.000034515764],"about_ca_topic_score_codex":0.0068679983,"about_ca_topic_score_gemma":0.0059063663,"teacher_disagreement_score":0.0068679983,"about_ca_system_score_codex":0.00044438735,"about_ca_system_score_gemma":0.00019822048,"threshold_uncertainty_score":0.01365608},"labels":[],"label_agreement":null},{"id":"W2033123210","doi":"10.1029/2000gl012231","title":"Impact of rotational Raman scattering in the O<sub>2</sub><i>A</i> band","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; York University","funders":"Universität Heidelberg; Trent University; York University; National Aeronautics and Space Administration","keywords":"Zenith; Radiance; Nadir; Radiative transfer; Scattering; Raman scattering; Solar zenith angle; Optics; X-ray Raman scattering; Computational physics; Diffuse sky radiation; Atmospheric radiative transfer codes; Physics; Satellite; Spectral resolution; Raman spectroscopy; Materials science; Spectral line; Astronomy","score_opus":0.023320298562134384,"score_gpt":0.28984011747813326,"score_spread":0.26651981891599885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033123210","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9854165,0.00031933,0.0061961915,0.00011116704,0.000027094038,0.000015487043,0.00019543665,0.0002605833,0.007458248],"genre_scores_gemma":[0.998376,0.00013673092,0.0009908335,0.000026953896,0.000005160988,0.000004516639,0.00009985891,0.000042180505,0.0003177495],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9996216,0.00008466614,0.000013091563,0.000075874625,0.00012713543,0.00007753163],"domain_scores_gemma":[0.998816,0.00074552663,0.00011769971,0.00009419442,0.00015761516,0.00006893147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047268905,0.0007097986,0.0002885129,0.00027810733,0.00044095755,0.00051995,0.00031781103,0.0002845163,0.002953753],"category_scores_gemma":[0.0012123615,0.00031223157,0.00055925554,0.00023363119,0.0004898634,0.0006369177,0.0005997834,0.0003793323,0.0003576098],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022152439,0.0003280192,0.118934594,0.00024723436,0.00028388752,0.00064637366,0.00027395858,0.21065912,0.61183697,0.0048610847,0.0010855016,0.04862805],"study_design_scores_gemma":[0.00021382638,0.0010355486,0.22164862,0.000052275973,0.00032948324,0.0005304935,0.00053611473,0.33299464,0.43676472,0.0035150563,0.0022019537,0.00017724159],"about_ca_topic_score_codex":0.007920496,"about_ca_topic_score_gemma":0.0045955013,"teacher_disagreement_score":0.007920496,"about_ca_system_score_codex":0.0003821283,"about_ca_system_score_gemma":0.00033565256,"threshold_uncertainty_score":0.015748799},"labels":[],"label_agreement":null},{"id":"W2033206183","doi":"10.1029/2007gl030611","title":"A long distance measurement of radioxenon in Yellowknife, Canada, in late October 2006","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Radioactive contamination and transfer","field":"Environmental Science","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Health Canada","funders":"","keywords":"Geology; Geodesy; Seismology; Geophysics","score_opus":0.021233454051880225,"score_gpt":0.2703770079715416,"score_spread":0.2491435539196614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033206183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923252,0.00020849485,0.00043985006,0.00010783025,0.000011329351,0.000034700726,0.0016379617,0.000032012347,0.0052025663],"genre_scores_gemma":[0.9920691,0.00029142876,0.0011841785,0.0000696841,0.000003986216,0.000016962103,0.0011692082,0.000014100081,0.0051813414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996879,0.000008493707,0.000006884734,0.000061400715,0.00015238649,0.00008284635],"domain_scores_gemma":[0.99949753,0.000013631517,0.00004068944,0.000009271132,0.00035235813,0.00008658694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016227203,0.00038969726,0.00027699803,0.00082302094,0.0026341658,0.0006745784,0.0005889497,0.00034749517,0.0007818778],"category_scores_gemma":[0.0004084142,0.0002829827,0.00012304467,0.0013339688,0.0005150597,0.0002790023,0.00058232894,0.0005536993,0.00022469641],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045869482,0.00013510899,0.86770946,0.00010243379,0.000099273144,0.0021524422,0.0061111907,0.0014067137,0.09605523,0.00047743268,0.002821893,0.022470176],"study_design_scores_gemma":[0.000015923655,0.00006737227,0.98224014,0.000021925516,0.000020660778,0.00023379634,0.0027619586,0.00096139516,0.0071816957,0.00002819954,0.0064387145,0.000028203816],"about_ca_topic_score_codex":0.9721921,"about_ca_topic_score_gemma":0.9924987,"teacher_disagreement_score":0.027807891,"about_ca_system_score_codex":0.010227106,"about_ca_system_score_gemma":0.011122717,"threshold_uncertainty_score":0.07420313},"labels":[],"label_agreement":null},{"id":"W2033301437","doi":"10.1029/2004gl020446","title":"Nonlinear complex principal component analysis of the tropical Pacific interannual wind variability","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Principal component analysis; Climatology; Nonlinear system; Multivariate statistics; Mode (computer interface); Asymmetry; Environmental science; Divergence (linguistics); Atmospheric sciences; Meteorology; Geology; Mathematics; Statistics; Geography; Physics; Computer science","score_opus":0.041890564654752625,"score_gpt":0.30242366486000133,"score_spread":0.2605331002052487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033301437","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36835814,0.0014849862,0.62250656,0.0005629514,0.00013838714,0.000074732554,0.0010598389,0.0003619537,0.005452424],"genre_scores_gemma":[0.93167007,0.0011754549,0.062332608,0.000030906383,0.00008261407,0.000060556955,0.0009953823,0.00007987286,0.0035726344],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998211,0.000052252322,0.000008145368,0.00003874119,0.000062965795,0.00001684431],"domain_scores_gemma":[0.9994055,0.00022914629,0.00007470431,0.00005373401,0.00021771803,0.00001926868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005318264,0.0003961569,0.00017795645,0.0006662336,0.00020166991,0.0004947428,0.00016703554,0.00014350007,0.0007697509],"category_scores_gemma":[0.0024572075,0.0000983765,0.0002846148,0.00087676244,0.0002510034,0.0005211629,0.00024315657,0.00037568744,0.0001600915],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031013333,0.00008111782,0.032583166,0.00017032368,0.00023282805,0.00022453681,0.00021885464,0.41088656,0.026286017,0.025952073,0.00651156,0.49654293],"study_design_scores_gemma":[0.0000057235357,0.000015444384,0.038114913,0.0000075208923,0.000023154606,0.000034788558,0.00002503643,0.9539702,0.001490498,0.0043957974,0.0018991972,0.000017710738],"about_ca_topic_score_codex":0.007892044,"about_ca_topic_score_gemma":0.0063968645,"teacher_disagreement_score":0.007892044,"about_ca_system_score_codex":0.00031259167,"about_ca_system_score_gemma":0.0005721186,"threshold_uncertainty_score":0.015692234},"labels":[],"label_agreement":null},{"id":"W2033423182","doi":"10.1029/2006gl026050","title":"Subsurface temperatures during the last millennium: Model and observation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministerio de Economía y Competitividad; St. Francis Xavier University","keywords":"Forcing (mathematics); Climatology; Borehole; GCM transcription factors; General Circulation Model; Natural (archaeology); Geology; Environmental science; Climate change; Climate model; Atmospheric sciences; Oceanography","score_opus":0.02959099480744181,"score_gpt":0.2661759330507517,"score_spread":0.2365849382433099,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033423182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9747645,0.000079131096,0.002343209,0.00021233506,0.00001630922,0.000023077357,0.02054067,0.00025052184,0.0017702169],"genre_scores_gemma":[0.98736423,0.0000735717,0.0015101167,0.000024255934,0.000008147757,0.000047017948,0.010581264,0.000029845298,0.00036154664],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998609,0.000030458044,0.000009455388,0.00005955666,0.000017042128,0.000022629381],"domain_scores_gemma":[0.9996613,0.00010033736,0.00005932893,0.00006255087,0.00007800656,0.000038352715],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004972855,0.00033202735,0.00030424906,0.00033443127,0.00022321261,0.00066415255,0.00078664767,0.00070962444,0.0013390719],"category_scores_gemma":[0.0013037228,0.00034268052,0.0005310362,0.000865324,0.00025615122,0.00063120795,0.00034308012,0.0005331407,0.00030791917],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040618313,0.00014816943,0.23690066,0.00006181365,0.00026666696,0.00008645268,0.00010578483,0.749249,0.0011588917,0.0014699402,0.0037990024,0.006347523],"study_design_scores_gemma":[0.00030107022,0.00009299906,0.12312883,0.000019577816,0.00011990659,0.00006168979,0.00006408938,0.87075996,0.0013733632,0.0010881099,0.0029395965,0.0000507593],"about_ca_topic_score_codex":0.074855424,"about_ca_topic_score_gemma":0.034856517,"teacher_disagreement_score":0.074855424,"about_ca_system_score_codex":0.0011021165,"about_ca_system_score_gemma":0.0009042697,"threshold_uncertainty_score":0.14883941},"labels":[],"label_agreement":null},{"id":"W2033442581","doi":"10.1029/2006gl028999","title":"Spreading of the Labrador Sea Water to the Irminger and Iceland basins","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Geology; Oceanography; Water mass; Climatology","score_opus":0.018835774035068927,"score_gpt":0.25986926580438985,"score_spread":0.24103349176932093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033442581","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958318,0.00023648032,0.000055278884,0.00009556263,0.000004817481,0.000008578626,0.0002035895,0.000014513527,0.0035492657],"genre_scores_gemma":[0.99763584,0.0003271293,0.00022255263,0.00007207704,0.000016496324,0.000007859886,0.00051573635,0.0000071809695,0.0011951538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999094,0.000009268658,0.0000056447343,0.000027380507,0.000018139952,0.00003022825],"domain_scores_gemma":[0.99970204,0.000016416965,0.00013628723,0.000023307035,0.00006284252,0.00005902878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018141791,0.00023427517,0.00018972936,0.000971286,0.00054150657,0.0008120346,0.0003058929,0.00014607733,0.0014321608],"category_scores_gemma":[0.00055804383,0.00008972596,0.00014704974,0.0007484775,0.0005112489,0.00034944076,0.00064786983,0.00021646685,0.00021270636],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002188695,0.000052788764,0.91068804,0.00007363807,0.00006735617,0.00034137396,0.0018028758,0.0008210198,0.008392239,0.0006064042,0.0016810044,0.0752544],"study_design_scores_gemma":[0.0000033653846,0.000026893807,0.9964192,0.000011535222,0.000007929986,0.00004207535,0.0003553392,0.00016918231,0.0004730535,0.00002586081,0.0024614134,0.0000041163853],"about_ca_topic_score_codex":0.09222428,"about_ca_topic_score_gemma":0.13357577,"teacher_disagreement_score":0.9077757,"about_ca_system_score_codex":0.001226851,"about_ca_system_score_gemma":0.00086140615,"threshold_uncertainty_score":0.18337494},"labels":[],"label_agreement":null},{"id":"W2033459048","doi":"10.1029/1999gl010929","title":"Size distribution and estimated optical properties of carbonate, water soluble organic carbon, and sulfate in aerosols at a remote high altitude site in western China","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Total organic carbon; Altitude (triangle); Aerosol; Sulfate; Carbonate; Carbon fibers; Chemical composition; Analytical Chemistry (journal); Mineralogy; Mass concentration (chemistry); Chemistry; Atmospheric sciences; Environmental chemistry; Physics; Materials science; Meteorology; Mathematics; Physical chemistry","score_opus":0.016323054433835103,"score_gpt":0.23562982794707407,"score_spread":0.21930677351323896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033459048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99968207,0.000008528202,0.0000639728,0.0000046230944,5.9241336e-7,0.0000030626195,0.00007873045,0.0000048062307,0.0001536804],"genre_scores_gemma":[0.99934906,0.000016662661,0.00018298843,0.0000057053126,0.0000027975625,0.000006715017,0.0002528783,0.0000015798752,0.00018166937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998871,0.000007909405,0.000009429088,0.000038100767,0.00003538177,0.000022072132],"domain_scores_gemma":[0.9998307,0.000020218358,0.000033074113,0.000010538397,0.00005721025,0.000048229507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002332746,0.00033350984,0.00020755848,0.0008629383,0.00051875843,0.00036504827,0.00045841536,0.0002772218,0.00039760294],"category_scores_gemma":[0.00021995274,0.00024807843,0.00033056468,0.0005455275,0.00031842064,0.00027343162,0.00029753323,0.00013134553,0.00010760558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006086129,0.00006622946,0.96012527,0.000021329348,0.000055659795,0.00032512686,0.00040587157,0.001972583,0.032545384,0.000060898677,0.00011635,0.0042442996],"study_design_scores_gemma":[0.000004568993,0.0000124919625,0.99659294,9.0949675e-7,0.0000092415985,0.00003441217,0.00009293644,0.002438302,0.00075080956,0.000008731723,0.0000499127,0.000004732682],"about_ca_topic_score_codex":0.102053106,"about_ca_topic_score_gemma":0.0985267,"teacher_disagreement_score":0.102053106,"about_ca_system_score_codex":0.0008153749,"about_ca_system_score_gemma":0.00051494135,"threshold_uncertainty_score":0.20291817},"labels":[],"label_agreement":null},{"id":"W2033672883","doi":"10.1029/2009gl037488","title":"Sensitivity of ocean acidification to geoengineered climate stabilization","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"Canadian Foundation for Climate and Atmospheric Sciences; University of Victoria","keywords":"Aragonite; Ocean acidification; Climate change; Saturation (graph theory); Environmental science; Biosphere; Climate sensitivity; Carbon dioxide; Carbon cycle; Global warming; Ocean chemistry; Global change; Climate model; Atmospheric sciences; Climatology; Oceanography; Geology; Seawater; Ecology; Ecosystem; Mineralogy; Calcite; Biology","score_opus":0.036206071146000496,"score_gpt":0.3020649809945296,"score_spread":0.2658589098485291,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2033672883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976786,0.00009877162,0.00083770166,0.00021200624,0.000017626166,0.0000060091033,0.00018470417,0.00004008295,0.0009244813],"genre_scores_gemma":[0.9997198,0.00004037884,0.00008132113,0.000019907344,0.0000015569561,0.0000019364697,0.000064040956,0.0000025595502,0.00006844883],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998498,0.000044852368,0.000010545817,0.00003355154,0.00002010388,0.000041133455],"domain_scores_gemma":[0.9992091,0.0003956724,0.00014600344,0.000093028924,0.000082112376,0.00007411984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042107084,0.00033300373,0.00027556217,0.0002042861,0.00020483808,0.00070067606,0.00030543425,0.0007705648,0.00087164016],"category_scores_gemma":[0.0020311514,0.000214729,0.00052288605,0.00023199036,0.00040409146,0.0004735764,0.00086713734,0.0005725853,0.000072011244],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061180047,0.000136244,0.060058277,0.00008539342,0.0002767792,0.00031326228,0.000058450416,0.8665287,0.06627022,0.0015056279,0.0005077347,0.003647456],"study_design_scores_gemma":[0.00017314876,0.00054164726,0.1211682,0.0000147075125,0.00014464375,0.00011917342,0.0001733672,0.83643174,0.03591036,0.0039685075,0.0012488517,0.00010568545],"about_ca_topic_score_codex":0.009784563,"about_ca_topic_score_gemma":0.0048492714,"teacher_disagreement_score":0.009784563,"about_ca_system_score_codex":0.0007914837,"about_ca_system_score_gemma":0.00042140594,"threshold_uncertainty_score":0.019455194},"labels":[],"label_agreement":null},{"id":"W2034091857","doi":"10.1029/2007gl032316","title":"Comment on “Abrupt environmental change in Canada's northernmost lake inferred from fossil diatom and pigment stratigraphy” by Dermot Antoniades et al.","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa","funders":"","keywords":"Arctic; Geology; Stratigraphy; Paleolimnology; Diatom; Climate change; Oceanography; Environmental change; Latitude; Physical geography; Global warming; The arctic; Paleoclimatology; Paleontology; Geography","score_opus":0.0353299474872797,"score_gpt":0.26464274218102946,"score_spread":0.22931279469374977,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034091857","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0015242401,0.0013066563,0.0004099709,0.92928207,0.061923582,0.000033148,0.00069423433,0.00017963766,0.004646458],"genre_scores_gemma":[0.009473017,0.0009009018,0.0005192654,0.944378,0.035121925,0.000045188885,0.00018352325,0.00008290822,0.009295243],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99710804,0.0003075183,0.0003723968,0.0005334134,0.001312354,0.00036630107],"domain_scores_gemma":[0.9851199,0.0046372064,0.0010966463,0.0005954989,0.0073295026,0.0012213694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0032599387,0.0010566984,0.0010036563,0.0011810592,0.0040541915,0.0025940125,0.003897284,0.020810183,0.0056603057],"category_scores_gemma":[0.020126663,0.00076779304,0.0010702896,0.0013823109,0.004818658,0.0026336247,0.0018490324,0.020564483,0.006221985],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035327357,0.000007695726,0.000734387,0.000044803983,0.000009354009,0.00023145422,0.00027017374,0.00006110776,0.00022613314,0.000735303,0.9952769,0.0023672767],"study_design_scores_gemma":[0.00005762403,0.000044885684,0.009911643,0.00034112713,0.00004269206,0.00068484386,0.001853518,0.00044301344,0.0011585582,0.003773417,0.98153883,0.00014977714],"about_ca_topic_score_codex":0.13459721,"about_ca_topic_score_gemma":0.14931147,"teacher_disagreement_score":0.8654028,"about_ca_system_score_codex":0.0055447035,"about_ca_system_score_gemma":0.0067112814,"threshold_uncertainty_score":0.26762754},"labels":[],"label_agreement":null},{"id":"W2034129653","doi":"10.1029/2007gl032303","title":"Tundra lake changes from 1978 to 2001 on the Tuktoyaktuk Peninsula, western Canadian Arctic","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":140,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Thermokarst; Tundra; Peninsula; Precipitation; Physical geography; Permafrost; Arctic; Climate change; Climatology; Environmental science; Period (music); Geology; Geography; Oceanography; Meteorology; Archaeology","score_opus":0.1250430605008354,"score_gpt":0.29822490098088533,"score_spread":0.17318184048004992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034129653","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99073315,0.00043862517,0.00006721661,0.00009895507,0.000012471315,0.000012233166,0.0071268342,0.000025687204,0.0014846518],"genre_scores_gemma":[0.9937448,0.0003057891,0.00016157996,0.00003252221,0.0000052752243,0.0000123395885,0.004412946,0.0000068580666,0.0013179341],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997532,0.0000115069915,0.00001541169,0.000050226456,0.0000744731,0.00009517373],"domain_scores_gemma":[0.99930716,0.000025213049,0.00012949617,0.000015659676,0.00042995872,0.000092530936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020425628,0.00028223742,0.000236633,0.0018055504,0.0011331685,0.00078413857,0.00041469524,0.00026422023,0.0014869884],"category_scores_gemma":[0.0007391583,0.00018653195,0.00024216634,0.0026141477,0.0003536983,0.00028921134,0.00049322756,0.00026217083,0.0001932362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019275001,0.000027002965,0.97540504,0.000090174675,0.00013795258,0.0003009201,0.0010376375,0.00091782503,0.0029399965,0.00010254982,0.0035026327,0.015345587],"study_design_scores_gemma":[0.0000015037086,0.0000024325295,0.9986292,0.000007434906,0.000012128304,0.00002513417,0.0002487538,0.00017693198,0.00009244232,0.0000026067307,0.0007984142,0.0000029670741],"about_ca_topic_score_codex":0.97579145,"about_ca_topic_score_gemma":0.9931452,"teacher_disagreement_score":0.024208546,"about_ca_system_score_codex":0.009581967,"about_ca_system_score_gemma":0.0051417127,"threshold_uncertainty_score":0.06952238},"labels":[],"label_agreement":null},{"id":"W2034614564","doi":"10.1029/2004gl020263","title":"Stochastic modeling of climatic variability in dendrochronology","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"St. Francis Xavier University","keywords":"Dendrochronology; Climatic variability; Climatology; Range (aeronautics); Series (stratigraphy); Dendroclimatology; Environmental science; Gaussian; Time series; Climate change; Scaling; Statistical physics; Geology; Statistics; Mathematics; Physics","score_opus":0.04838424834666457,"score_gpt":0.31252168956169585,"score_spread":0.2641374412150313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034614564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.55016315,0.0008016796,0.441937,0.0013231563,0.00007240479,0.000025271069,0.00051103154,0.0002635029,0.0049027526],"genre_scores_gemma":[0.995401,0.00023826082,0.0029936105,0.000027489179,0.00003011039,0.000016731869,0.0001142132,0.000022374348,0.0011561727],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99965096,0.00015391396,0.000018993127,0.00006603609,0.0000536991,0.00005640932],"domain_scores_gemma":[0.99879223,0.0007234443,0.00025008444,0.000066015244,0.000085628846,0.000082665945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001215253,0.00031240756,0.0003949909,0.0004155001,0.00041670477,0.0009872899,0.00082479016,0.0006797017,0.0005944669],"category_scores_gemma":[0.003747049,0.00031327578,0.0004145512,0.0005633128,0.00094246154,0.000990768,0.0005769809,0.00064323883,0.00008751535],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014221716,0.000007606704,0.0019897379,0.00000892408,0.000022318702,0.00003407268,0.00003849253,0.9522371,0.00043328555,0.043683104,0.00021755988,0.0013134754],"study_design_scores_gemma":[0.0000025411466,0.000003282967,0.0005161735,0.0000014135979,0.0000022695472,0.0000053356057,0.000006032602,0.98619115,0.000033777265,0.013051868,0.00018261907,0.0000035036298],"about_ca_topic_score_codex":0.013615777,"about_ca_topic_score_gemma":0.01057183,"teacher_disagreement_score":0.013615777,"about_ca_system_score_codex":0.0011758987,"about_ca_system_score_gemma":0.0006291979,"threshold_uncertainty_score":0.027073085},"labels":[],"label_agreement":null},{"id":"W2034998917","doi":"10.1029/2009gl038187","title":"Heave of a surficial rock layer due to pressures generated by injected fluids","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Caprock; Cabin pressurization; Geology; Rotational symmetry; Layer (electronics); Geotechnical engineering; Surface layer; Geomechanics; Mechanics; Materials science; Composite material","score_opus":0.03203806752502076,"score_gpt":0.33130453120641273,"score_spread":0.299266463681392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2034998917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9503209,0.0005235969,0.042790554,0.00045491254,0.00010886517,0.00003943945,0.00008830904,0.00011137681,0.005562044],"genre_scores_gemma":[0.99612755,0.00020262806,0.00079811306,0.000023893312,0.000021154578,0.000007671236,0.000022440572,0.000016802052,0.0027797518],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998915,0.000019011162,0.000006371423,0.000016771039,0.000028351793,0.000038034603],"domain_scores_gemma":[0.9997143,0.000120597964,0.000054323613,0.000022764001,0.000031010662,0.000056965033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036050187,0.00039515927,0.00040217128,0.00035394894,0.00048423873,0.0009650821,0.00034913907,0.0007663151,0.0014617933],"category_scores_gemma":[0.0010406446,0.00032641244,0.00045440512,0.00013281124,0.001223887,0.0007583542,0.0015168209,0.0006418754,0.00011487398],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013322076,0.00011247671,0.019528564,0.00043325793,0.00019202304,0.006975169,0.0010216733,0.48868173,0.41386026,0.026672147,0.00091195287,0.04027858],"study_design_scores_gemma":[0.00022797135,0.0007360058,0.03353407,0.000050200833,0.000097809236,0.0014302584,0.0010679424,0.8731435,0.0735017,0.013747114,0.0023149722,0.00014847852],"about_ca_topic_score_codex":0.0011700523,"about_ca_topic_score_gemma":0.000534793,"teacher_disagreement_score":0.0014617933,"about_ca_system_score_codex":0.00041646176,"about_ca_system_score_gemma":0.00025658507,"threshold_uncertainty_score":0.0048902035},"labels":[],"label_agreement":null},{"id":"W2035041359","doi":"10.1002/2014gl060402","title":"Resonant ocean current responses driven by coastal winds near the critical latitude","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ontario Tech University; Vancouver Island University","funders":"National Research Foundation","keywords":"Latitude; Wind stress; Current (fluid); Sea breeze; Atmospheric sciences; Ekman transport; Climatology; Geology; Amplitude; Inertial wave; Environmental science; Oceanography; Physics; Geodesy; Upwelling; Wave propagation","score_opus":0.024070536642136122,"score_gpt":0.2985935832341515,"score_spread":0.27452304659201543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035041359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899226,0.00000800745,0.0005523073,0.000005013893,0.0000011961808,0.0000017793984,0.000020032156,0.000015103885,0.00040436152],"genre_scores_gemma":[0.99987817,0.0000039513966,0.000061421655,0.0000014274793,4.7426823e-7,7.788579e-7,0.00001546626,0.000001321824,0.000036981233],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999967,0.0000042429438,0.000001427952,0.000008376236,0.000007224211,0.000011702938],"domain_scores_gemma":[0.99983644,0.000053694213,0.000028117753,0.000013344569,0.000041144758,0.000027220998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000771645,0.00011335073,0.00012553463,0.00016942417,0.000095444484,0.0001537325,0.000082097,0.00013018255,0.00071013585],"category_scores_gemma":[0.00047869474,0.00008278654,0.00008789321,0.00007997307,0.00013941589,0.00014747071,0.00017365968,0.00013615364,0.00010276428],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006775031,0.000110582165,0.22223163,0.000088066394,0.00004640879,0.0005869142,0.00047179716,0.022209316,0.73314804,0.0007668892,0.0005053999,0.019157534],"study_design_scores_gemma":[0.000033905228,0.0001825489,0.87702113,0.000012118694,0.000018037164,0.00024162015,0.0003481152,0.08677538,0.034492858,0.00053532154,0.00031516785,0.00002378008],"about_ca_topic_score_codex":0.0016597828,"about_ca_topic_score_gemma":0.0011435226,"teacher_disagreement_score":0.0016597828,"about_ca_system_score_codex":0.00017846806,"about_ca_system_score_gemma":0.00007364855,"threshold_uncertainty_score":0.0033003092},"labels":[],"label_agreement":null},{"id":"W2035101449","doi":"10.1029/2004gl020825","title":"Derivation of polarization from Odin/OSIRIS limb spectra","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; York University","funders":"Tekes; Centre National d’Etudes Spatiales","keywords":"Osiris; Radiance; Polarization (electrochemistry); Radiative transfer; Physics; Linear polarization; Differential optical absorption spectroscopy; Spectral line; Polar; Optics; Remote sensing; Geology; Absorption (acoustics); Astronomy; Chemistry; Laser","score_opus":0.028791477158513875,"score_gpt":0.2720688809754004,"score_spread":0.2432774038168865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035101449","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.041841477,0.00013260012,0.9418608,0.000078805344,0.00014624653,0.00010039526,0.0022847415,0.0019664997,0.011588477],"genre_scores_gemma":[0.3359188,0.0007531697,0.64886135,0.000121052144,0.000090008594,0.00025994948,0.0059472206,0.0009621513,0.0070861992],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99969554,0.00003124775,0.000012300843,0.00005023937,0.00017846208,0.000032262447],"domain_scores_gemma":[0.99964297,0.000033641765,0.000024605142,0.000058383986,0.00022975859,0.000010677895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000498367,0.0005146585,0.00020459312,0.00081568037,0.00036779986,0.000590063,0.00047321964,0.00021598504,0.0022712597],"category_scores_gemma":[0.0015025596,0.00034685739,0.0003863493,0.00066251145,0.0001723034,0.0005772799,0.00060697866,0.00093237346,0.0024348951],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012052518,0.00011902858,0.017522318,0.0002536009,0.00008286316,0.00035535745,0.00044770632,0.08379848,0.17909367,0.03494486,0.012958452,0.6703032],"study_design_scores_gemma":[0.00004712407,0.000087697204,0.03441921,0.00009428684,0.00006811645,0.00063330267,0.00022932734,0.65975744,0.17065734,0.041796464,0.092055544,0.00015413343],"about_ca_topic_score_codex":0.0020850375,"about_ca_topic_score_gemma":0.0020853737,"teacher_disagreement_score":0.0022712597,"about_ca_system_score_codex":0.00024412107,"about_ca_system_score_gemma":0.0005742219,"threshold_uncertainty_score":0.0075981617},"labels":[],"label_agreement":null},{"id":"W2035244633","doi":"10.1029/2008gl033565","title":"Influence of the enhanced mixing within the Southern Ocean fronts on the overturning circulation","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"University of Victoria","keywords":"Upwelling; Geology; Abyssal zone; Oceanography; Antarctic Bottom Water; Mixing (physics); Climatology; Circumpolar deep water; Thermohaline circulation; Shutdown of thermohaline circulation; Lead (geology); Ocean current; North Atlantic Deep Water; Water column; Current (fluid); Geomorphology","score_opus":0.02371826949209366,"score_gpt":0.2399851611870865,"score_spread":0.21626689169499283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035244633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835986,0.00003480501,0.00051800493,0.000054640106,0.000006624546,0.0000043348487,0.000028697612,0.000018863173,0.0009741219],"genre_scores_gemma":[0.9995875,0.00003300611,0.00019171761,0.0000071132545,0.0000050927365,0.0000016075348,0.000017981736,0.0000047074514,0.00015126374],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988735,0.00003835147,0.000005374497,0.000016423894,0.000015729946,0.000036744943],"domain_scores_gemma":[0.999742,0.00009357009,0.00004523554,0.000028064787,0.000024185723,0.00006692965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028469865,0.00065386324,0.000318069,0.00025013453,0.0004374078,0.000951121,0.0002740337,0.00045626936,0.0014187307],"category_scores_gemma":[0.0010239463,0.00027850826,0.0007431095,0.00017179745,0.00046194304,0.0004702718,0.000926783,0.00044691158,0.00008858876],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078811793,0.00031398505,0.11038594,0.00006638876,0.0002888369,0.0009964516,0.00017109145,0.7648168,0.10542936,0.0036331373,0.00030468573,0.012805223],"study_design_scores_gemma":[0.00023097993,0.00043666942,0.11462735,0.000010763966,0.0002200275,0.00012311789,0.0001135659,0.87359476,0.009169575,0.0009904926,0.00044715375,0.000035568763],"about_ca_topic_score_codex":0.01918531,"about_ca_topic_score_gemma":0.008930102,"teacher_disagreement_score":0.01918531,"about_ca_system_score_codex":0.00062366645,"about_ca_system_score_gemma":0.00048592986,"threshold_uncertainty_score":0.03814727},"labels":[],"label_agreement":null},{"id":"W2035511167","doi":"10.1029/2005gl025016","title":"Evidence for atmospheric control of sea‐ice motion through Nares Strait","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Science Foundation","keywords":"Geology; Arctic ice pack; Sea ice; Antarctic sea ice; Drift ice; Oceanography; Climatology; Wind stress; Sea ice thickness; Fast ice; Atmospheric pressure; Atmospheric sciences","score_opus":0.046923154956567535,"score_gpt":0.3032356605982435,"score_spread":0.25631250564167596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035511167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782854,0.00008393082,0.00024333183,0.00009100697,0.000006154719,0.0000029530747,0.0001641505,0.000016802744,0.0015630625],"genre_scores_gemma":[0.9994992,0.00005734125,0.00007706452,0.000009899438,0.000005473907,0.0000014936085,0.00017985029,0.0000032961377,0.00016628516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985635,0.000025307338,0.000010978051,0.00004758236,0.000023674156,0.000036110447],"domain_scores_gemma":[0.99934894,0.00017694623,0.00018222549,0.00007273558,0.0001163539,0.00010272064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034877995,0.00021863029,0.00016970451,0.00033898331,0.0002651777,0.00070083863,0.00020033144,0.0001336784,0.0011821081],"category_scores_gemma":[0.000862609,0.00020034844,0.00031232266,0.00031203253,0.00041705824,0.00024581485,0.00034288052,0.0001825357,0.0001264665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042453269,0.00006549678,0.94698244,0.000054951422,0.00025875441,0.00018441763,0.00041302765,0.0065307044,0.034854647,0.0010200675,0.00047109716,0.008739874],"study_design_scores_gemma":[0.000024757726,0.00003360455,0.9921489,0.000006149505,0.00004006518,0.000026240228,0.00009479725,0.005769515,0.0012497328,0.000102053345,0.00049595867,0.00000815585],"about_ca_topic_score_codex":0.07385206,"about_ca_topic_score_gemma":0.105313495,"teacher_disagreement_score":0.07385206,"about_ca_system_score_codex":0.00066418864,"about_ca_system_score_gemma":0.0005522902,"threshold_uncertainty_score":0.14684439},"labels":[],"label_agreement":null},{"id":"W2035538442","doi":"10.1029/2007gl030685","title":"Double jeopardy: Concurrent arrival of the 2004 Sumatra tsunami and storm‐generated waves on the Atlantic coast of the United States and Canada","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada","funders":"National Oceanic and Atmospheric Administration; Russian Foundation for Basic Research","keywords":"Tide gauge; Nova scotia; Geology; Storm; Oceanography; Shore; Submarine pipeline; Arrival time; East coast; Seismology; Climatology; Sea level","score_opus":0.03387425765395936,"score_gpt":0.262020335632289,"score_spread":0.22814607797832964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035538442","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782383,0.00016905008,0.000023404129,0.00020348148,0.000012931349,0.00000600441,0.00038748863,0.0000043846876,0.0013694251],"genre_scores_gemma":[0.99858296,0.00020835607,0.000051343257,0.00007115136,0.0000067598653,0.0000042210754,0.00040345755,0.000002456943,0.00066925446],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99964964,0.000023535176,0.000021987715,0.00004722253,0.00012865335,0.00012886898],"domain_scores_gemma":[0.9981717,0.0001256648,0.00041534394,0.00008808278,0.0008314023,0.00036775926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027641313,0.00020074063,0.0002287024,0.0013570505,0.0016610902,0.0011798441,0.00036306432,0.00033036145,0.001097836],"category_scores_gemma":[0.0019315381,0.00020563239,0.00014191169,0.0018284651,0.00064664596,0.00042134066,0.00154046,0.0006156619,0.00013573573],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119391436,0.000024850051,0.9847246,0.000018163564,0.00008068528,0.0008541277,0.0017453326,0.000169255,0.0008775887,0.000084980646,0.0014063665,0.009894784],"study_design_scores_gemma":[0.0000024015496,0.000010598216,0.9949181,0.000009120886,0.000019006711,0.0001488552,0.003317747,0.00014735562,0.00014132328,0.000022934912,0.0012538086,0.000008867919],"about_ca_topic_score_codex":0.8957279,"about_ca_topic_score_gemma":0.96438617,"teacher_disagreement_score":0.10427213,"about_ca_system_score_codex":0.005892166,"about_ca_system_score_gemma":0.0054954686,"threshold_uncertainty_score":0.20977235},"labels":[],"label_agreement":null},{"id":"W2035552631","doi":"10.1029/2006gl026767","title":"Ocean warming and freshening in the northern Gulf of Alaska","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Office of Naval Research; North Pacific Research Board; Exxon Valdez Oil Spill Trustee Council; Canadian Institute for Advanced Research; National Oceanic and Atmospheric Administration; Old Dominion University; National Science Foundation","keywords":"Oceanography; Stratification (seeds); Geology; Arctic; Glacial period; Water column; Environmental science; Ocean current; Climatology","score_opus":0.01673494222363565,"score_gpt":0.25016059406418867,"score_spread":0.23342565184055303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035552631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99600023,0.0006620035,0.00001471241,0.00011059403,0.000008997145,0.0000017427777,0.00012655396,0.0000033628019,0.003071756],"genre_scores_gemma":[0.998273,0.0007076712,0.00002816386,0.000034899993,0.00001005001,0.0000016553167,0.0001412764,0.0000014915342,0.00080179976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.000007918544,0.0000048212974,0.000010306368,0.0000073160218,0.000010301287],"domain_scores_gemma":[0.9998914,0.000015081824,0.000041920932,0.000008101933,0.000018032188,0.00002538892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021577303,0.00007676158,0.00009991364,0.00065214833,0.00061524374,0.000618256,0.00007460438,0.00020051147,0.002266952],"category_scores_gemma":[0.0004102149,0.00006646588,0.00018491833,0.0005077977,0.00034584964,0.00040491164,0.00044649496,0.00016807609,0.00010534666],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005041572,0.00006035155,0.95436275,0.000118809956,0.000100259094,0.0011415635,0.0035181202,0.0017370175,0.006966901,0.0009123825,0.00081309956,0.029764606],"study_design_scores_gemma":[0.0000034007248,0.00002106579,0.99635065,0.000012310368,0.000017351827,0.0000863624,0.0011048728,0.0000705443,0.00017841335,0.00025309136,0.0018979557,0.0000039292227],"about_ca_topic_score_codex":0.04917258,"about_ca_topic_score_gemma":0.07834662,"teacher_disagreement_score":0.04917258,"about_ca_system_score_codex":0.00093113986,"about_ca_system_score_gemma":0.00036006756,"threshold_uncertainty_score":0.09777272},"labels":[],"label_agreement":null},{"id":"W2035867147","doi":"10.1029/1999gl011332","title":"A modified pool permutation procedure for short regional climate model simulations nested within analyzed fields","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"demographic modeling and climate adaptation","field":"Decision Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Precipitation; Climate model; Climatology; Environmental science; Nested set model; General Circulation Model; Meteorology; Climate change; Geography; Geology; Computer science","score_opus":0.23264500044660266,"score_gpt":0.44849904084573794,"score_spread":0.21585404039913528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2035867147","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.010283176,0.000019614574,0.98514414,0.00005835115,0.00011013514,0.0010822461,0.0006677544,0.0018292806,0.00080527423],"genre_scores_gemma":[0.0662635,0.00002951996,0.9239239,0.00007892428,0.00006444321,0.005958213,0.0012939223,0.00079982274,0.0015877442],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.98945856,0.007408878,0.0007754018,0.0012090284,0.0008242023,0.00032387846],"domain_scores_gemma":[0.9581922,0.02126651,0.0013798682,0.015935918,0.002783901,0.00044156983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.018524341,0.000983977,0.0016160097,0.001728017,0.00141125,0.0012988867,0.0028762987,0.00088241545,0.018637536],"category_scores_gemma":[0.090483904,0.00079010386,0.0026226083,0.0021361662,0.0012613541,0.0014991881,0.002853823,0.0026699712,0.0028081909],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022059965,0.0007087267,0.0138634695,0.0007296156,0.0022971954,0.0011351366,0.0017255653,0.08581468,0.01965378,0.16094545,0.031069044,0.67985135],"study_design_scores_gemma":[0.0007775774,0.001222635,0.009475932,0.00011277581,0.00039032177,0.000392013,0.00033140666,0.7840444,0.018245198,0.14107801,0.043664135,0.0002656034],"about_ca_topic_score_codex":0.0052793953,"about_ca_topic_score_gemma":0.0071010897,"teacher_disagreement_score":0.018637536,"about_ca_system_score_codex":0.0007664275,"about_ca_system_score_gemma":0.0028949908,"threshold_uncertainty_score":0.09796721},"labels":[],"label_agreement":null},{"id":"W2036036726","doi":"10.1029/2000gl012568","title":"Ice nucleation in NH<sub>4</sub>HSO<sub>4</sub>, NH<sub>4</sub>NO<sub>3</sub>, and H<sub>2</sub>SO<sub>4</sub> aqueous particles: Implications for cirrus cloud formation","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Supercooling; Nucleation; Aqueous solution; Ice nucleus; Cirrus; Sulfate; Aerosol; Ammonium sulfate; Materials science; Analytical Chemistry (journal); Chemistry; Thermodynamics; Physical chemistry; Meteorology; Chromatography; Organic chemistry; Physics","score_opus":0.026116470266734523,"score_gpt":0.2637809443040667,"score_spread":0.23766447403733215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036036726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899143,0.00015743024,0.0002874469,0.000009041325,0.0000043903915,0.000005191421,0.000042093507,0.000003976034,0.0004989346],"genre_scores_gemma":[0.99902236,0.00015602043,0.00040889767,0.0000067003116,0.0000038129342,0.0000047087583,0.00009731058,0.0000021907597,0.0002979686],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996173,0.00000409793,0.0000021209903,0.000008375442,0.000011211214,0.000012487967],"domain_scores_gemma":[0.9999361,0.000017786651,0.000014094466,0.0000026691184,0.000017348695,0.000011916228],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012891194,0.00022077702,0.00012945135,0.00017730823,0.0001627451,0.0002559598,0.00013309433,0.00013279592,0.00050603575],"category_scores_gemma":[0.00019673319,0.00012855203,0.00013993573,0.000055899585,0.00023202463,0.00020112112,0.00013490449,0.00013792819,0.00006322853],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010785689,0.000010619388,0.005377012,0.000028529561,0.000006822761,0.000047081405,0.000025889009,0.00063054456,0.9927729,0.000077591554,0.000019265608,0.00089583197],"study_design_scores_gemma":[0.00002245561,0.00025184068,0.082030654,0.0000073954684,0.000022862829,0.00011902491,0.00008146386,0.011750726,0.90494484,0.00020712237,0.0005541666,0.0000074801324],"about_ca_topic_score_codex":0.0031325135,"about_ca_topic_score_gemma":0.002924654,"teacher_disagreement_score":0.0031325135,"about_ca_system_score_codex":0.00032044825,"about_ca_system_score_gemma":0.00011942559,"threshold_uncertainty_score":0.006228566},"labels":[],"label_agreement":null},{"id":"W2036222581","doi":"10.1029/2006gl028238","title":"Fracture energy applicable to dry snow slab avalanche release","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Slab; Snow; Fracture (geology); Geology; Ultimate tensile strength; Geotechnical engineering; Materials science; Composite material; Geophysics; Geomorphology","score_opus":0.011343893046830547,"score_gpt":0.2771406200571888,"score_spread":0.2657967270103583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036222581","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.43852028,0.01205732,0.4741577,0.0005675234,0.00027940064,0.00018517836,0.0016744754,0.00030924767,0.07224894],"genre_scores_gemma":[0.9664946,0.0036331704,0.016235054,0.000120336554,0.00008574253,0.00012852847,0.000451215,0.0000906477,0.012760629],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99985397,0.000016422013,0.000012069266,0.000026793823,0.000065374945,0.000025470763],"domain_scores_gemma":[0.9997795,0.00012247005,0.000030070105,0.000019878424,0.00004163517,0.0000065705435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023822261,0.0004106919,0.0003389269,0.0010853796,0.00023543193,0.0004597387,0.00070626056,0.00052516494,0.0045145797],"category_scores_gemma":[0.00090501225,0.00020836969,0.00037222193,0.0006378386,0.00040484875,0.00052097964,0.00062413735,0.00048755915,0.0006469492],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021715536,0.00012286607,0.017125301,0.0006108398,0.0001363458,0.0015336445,0.00029694245,0.65803695,0.08222479,0.111013494,0.0022887376,0.12639293],"study_design_scores_gemma":[0.000033068656,0.00015914123,0.04065312,0.00025752044,0.000059305206,0.0020695752,0.0002879799,0.8245824,0.022666924,0.08798475,0.021162331,0.00008391521],"about_ca_topic_score_codex":0.0024166119,"about_ca_topic_score_gemma":0.0025771104,"teacher_disagreement_score":0.0045145797,"about_ca_system_score_codex":0.00046772734,"about_ca_system_score_gemma":0.0002261416,"threshold_uncertainty_score":0.015102744},"labels":[],"label_agreement":null},{"id":"W2036264045","doi":"10.1029/2004gl021080","title":"Anisotropy of the flexural response of the lithosphere in the Canadian Shield","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Lithosphere; Shield; Geology; Anisotropy; Flexural strength; Geophysics; Seismology; Petrology; Tectonics; Physics; Materials science; Optics; Composite material","score_opus":0.02634217695026945,"score_gpt":0.2710980626453812,"score_spread":0.24475588569511178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036264045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981135,0.00006293191,0.00006710973,0.00003211591,8.6908085e-7,0.0000015528838,0.00026081092,0.000008544478,0.0014526127],"genre_scores_gemma":[0.9996026,0.00004006389,0.000041356234,0.0000035708929,4.7506177e-7,5.1868034e-7,0.00012720213,0.0000019826077,0.00018216451],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990904,0.0000028329168,0.0000018524019,0.000015981172,0.00002180785,0.00004844068],"domain_scores_gemma":[0.99983096,0.000015291664,0.000020925158,0.000008677079,0.00008807359,0.000036013098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008055062,0.0002445574,0.00012249258,0.0009315365,0.0009362364,0.0005734092,0.00020882972,0.00014819809,0.0014989553],"category_scores_gemma":[0.00036649243,0.00017478432,0.00012720135,0.0009503207,0.0005684149,0.00012928087,0.00031615587,0.00016700577,0.00011897036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036784855,0.000029216155,0.85908514,0.000060919756,0.0001206026,0.0005201506,0.0016137682,0.014182752,0.0953145,0.0016344202,0.0015334056,0.025537254],"study_design_scores_gemma":[0.0000025571353,0.000002883214,0.9970036,0.0000026427774,0.00000685619,0.000035632067,0.00017156795,0.0017391274,0.0006339778,0.000049826616,0.0003406964,0.000010519509],"about_ca_topic_score_codex":0.95740646,"about_ca_topic_score_gemma":0.97482896,"teacher_disagreement_score":0.04259354,"about_ca_system_score_codex":0.004350975,"about_ca_system_score_gemma":0.0030697247,"threshold_uncertainty_score":0.08568871},"labels":[],"label_agreement":null},{"id":"W2036293513","doi":"10.1029/2006gl026241","title":"Three‐dimensional investigation of volcanic textures by X‐ray microtomography and implications for conduit processes","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Strombolian eruption; Geology; Explosive eruption; Scoria; Pyroclastic rock; Pumice; Volcano; Petrology; Mineralogy; Geochemistry","score_opus":0.024577467864920995,"score_gpt":0.2579487136187192,"score_spread":0.2333712457537982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036293513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99583507,0.00021127754,0.003076249,0.000028918796,0.00000220325,0.0000069868584,0.000082859864,0.00003189753,0.00072449155],"genre_scores_gemma":[0.9966445,0.0001358204,0.0029449316,0.0000050533704,0.0000020588673,0.000003885236,0.000065781256,0.0000065744216,0.00019143464],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999703,0.000003975571,0.0000017593272,0.000008170485,0.000009151574,0.0000065155514],"domain_scores_gemma":[0.99990404,0.000027850368,0.000023195009,0.000014663718,0.000016157941,0.000014000079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009282451,0.00014563174,0.00008910913,0.00058478536,0.00022202778,0.00060266675,0.00016348326,0.00024482826,0.00048618822],"category_scores_gemma":[0.00020683897,0.00016466144,0.00009523293,0.00031724825,0.00039586527,0.0002723241,0.00012491597,0.00020596852,0.000073604395],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010765143,0.00001635821,0.029393144,0.00006306481,0.000013779645,0.0006573936,0.00031998617,0.0017916352,0.9586368,0.0012264646,0.00008239341,0.0076913335],"study_design_scores_gemma":[0.000020582545,0.000108759195,0.6704136,0.000024686615,0.000035742494,0.003846866,0.0008939844,0.044495102,0.2753057,0.0011208821,0.0037023223,0.000031742897],"about_ca_topic_score_codex":0.0020423674,"about_ca_topic_score_gemma":0.002871097,"teacher_disagreement_score":0.0020423674,"about_ca_system_score_codex":0.00022460302,"about_ca_system_score_gemma":0.00016020863,"threshold_uncertainty_score":0.004060924},"labels":[],"label_agreement":null},{"id":"W2036452987","doi":"10.1029/2006gl028866","title":"Emissions of gaseous mercury from biomass burning in South America in 2005 observed during CARIBIC flights","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Biomass burning; Environmental science; Southern Hemisphere; Mercury (programming language); Atmospheric sciences; Northern Hemisphere; Meteorology; Climatology; Geography; Aerosol; Geology","score_opus":0.05020229653388327,"score_gpt":0.3182273771534309,"score_spread":0.26802508061954766,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036452987","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99964094,0.000040527077,0.000028080156,0.000011872856,5.509637e-7,0.0000017663436,0.000052344396,0.0000021223893,0.0002217967],"genre_scores_gemma":[0.9990709,0.00015563182,0.00017025505,0.000028002947,0.0000016975374,0.0000073214364,0.0002742794,0.0000020904595,0.00028986644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999548,0.000007016647,0.0000022804365,0.000013665367,0.000010762342,0.000011457141],"domain_scores_gemma":[0.9998888,0.00001453769,0.000041074494,0.00000636157,0.000030104038,0.00001897523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012483548,0.00024896985,0.00016268303,0.00045959625,0.00048840616,0.00029373835,0.00013014309,0.00018278912,0.00036946934],"category_scores_gemma":[0.0001956758,0.0001704266,0.00014264633,0.0004470684,0.00030608778,0.00016768056,0.00037805812,0.00016042586,0.000053846004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002114229,0.000034522494,0.95574194,0.000051932853,0.00007309096,0.00053613,0.0031400912,0.00016205115,0.03535696,0.000038165137,0.00016584822,0.004487818],"study_design_scores_gemma":[0.0000031485097,0.00003147223,0.9973634,0.0000075821026,0.000016589747,0.00010046757,0.00094595196,0.00010441536,0.0009071842,0.000013810084,0.0005025765,0.0000034178638],"about_ca_topic_score_codex":0.11080005,"about_ca_topic_score_gemma":0.34237602,"teacher_disagreement_score":0.11080005,"about_ca_system_score_codex":0.0007931432,"about_ca_system_score_gemma":0.0005237455,"threshold_uncertainty_score":0.22031027},"labels":[],"label_agreement":null},{"id":"W2036477816","doi":"10.1029/2005gl024413","title":"A decrease in discharge‐normalized DOC export by the Yukon River during summer through autumn","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":423,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Dissolved organic carbon; Environmental science; Subarctic climate; Arctic; Ecosystem; Drainage basin; Oceanography; Terrestrial ecosystem; Hydrology (agriculture); Ecology; Geology; Geography","score_opus":0.06545903028359579,"score_gpt":0.3194453702743636,"score_spread":0.2539863399907678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036477816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994105,0.000040147515,0.000069657195,0.000024514387,0.0000012560315,6.04104e-7,0.00023186803,0.000010068055,0.0002114118],"genre_scores_gemma":[0.99914694,0.00003799356,0.00005537855,0.0000125982,0.0000010001772,0.0000015451963,0.0004006224,0.0000032824776,0.00034076767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999664,0.000002811123,0.0000028067136,0.000012244348,0.0000047887775,0.000010913128],"domain_scores_gemma":[0.99991035,0.000013557011,0.000026283005,0.000008791345,0.000026627411,0.000014461024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000059034217,0.000110651265,0.00014398528,0.00016751357,0.00025716797,0.00029739708,0.000103211605,0.00015014103,0.0008431178],"category_scores_gemma":[0.00017335312,0.000099876874,0.000115899,0.00028365853,0.00015207,0.000223397,0.00016377673,0.00012646541,0.00007765465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029002773,0.00002693629,0.9133835,0.000056994115,0.00008344955,0.00013706108,0.00039412332,0.00074660697,0.07033635,0.00014047393,0.0004347782,0.013969675],"study_design_scores_gemma":[0.0000022444003,0.000008808461,0.9986395,8.4371317e-7,0.000006200535,0.000018744757,0.000047789646,0.00024420384,0.0008144511,0.000012793449,0.00020287864,0.0000016199036],"about_ca_topic_score_codex":0.05474057,"about_ca_topic_score_gemma":0.10193373,"teacher_disagreement_score":0.05474057,"about_ca_system_score_codex":0.00065344677,"about_ca_system_score_gemma":0.00047654018,"threshold_uncertainty_score":0.10884392},"labels":[],"label_agreement":null},{"id":"W2036778254","doi":"10.1002/2014gl062748","title":"North‐south asymmetry of the high‐latitude thermospheric density: IMF <i>B</i><sub><i>Y</i></sub> effect","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; Universität Bremen; Sight Research UK; Florida Institute of Technology; Natural Environment Research Council; Alberta Agricultural Research Institute; National Aeronautics and Space Administration","keywords":"Northern Hemisphere; Southern Hemisphere; Earth's magnetic field; Atmospheric sciences; Latitude; Interplanetary magnetic field; Asymmetry; Thermosphere; Climatology; Geology; Solar wind; Physics; Ionosphere; Geophysics; Magnetic field; Geodesy","score_opus":0.00595682170786143,"score_gpt":0.22708607091105418,"score_spread":0.22112924920319274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2036778254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971763,0.000053472453,0.00037650228,0.00010546129,0.0000072028133,0.000003676715,0.000254006,0.000035479738,0.0019879537],"genre_scores_gemma":[0.99962246,0.000019122643,0.00005468855,0.00002753432,0.000007118818,0.0000018904499,0.00009661507,0.0000059055637,0.00016452011],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999889,0.000028475148,0.0000060454922,0.00003183444,0.000021041722,0.000023490757],"domain_scores_gemma":[0.9993488,0.00022667924,0.00018808075,0.000064602464,0.00009872501,0.00007299045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028638463,0.00014560313,0.0002433725,0.00030419885,0.00015947627,0.0002246043,0.00013821955,0.0002116122,0.0019931262],"category_scores_gemma":[0.00086554466,0.00010927566,0.00026746216,0.00022888827,0.00025963952,0.00020807883,0.00024442756,0.00023954934,0.0002161682],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006743635,0.00006874881,0.88496417,0.00007234751,0.00021945703,0.00029442925,0.00018096495,0.008661572,0.09428085,0.00032636535,0.001378382,0.008878347],"study_design_scores_gemma":[0.0000047316094,0.000017504142,0.99645543,0.0000019936963,0.000011616186,0.000033992004,0.00003448916,0.0020007107,0.0012420899,0.000028982382,0.00016614677,0.0000024013002],"about_ca_topic_score_codex":0.0072171944,"about_ca_topic_score_gemma":0.0059143873,"teacher_disagreement_score":0.0072171944,"about_ca_system_score_codex":0.00020123331,"about_ca_system_score_gemma":0.00012903924,"threshold_uncertainty_score":0.014350355},"labels":[],"label_agreement":null},{"id":"W2037542249","doi":"10.1029/2007gl029934","title":"Measuring heterogeneous remanence in paleomagnetism","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Paleomagnetism; Remanence; Geology; Geophysics; Rock magnetism; Seismology; Physics; Magnetization; Magnetic field","score_opus":0.037448176742235106,"score_gpt":0.2987290430374054,"score_spread":0.2612808662951703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2037542249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9670069,0.00049864926,0.029357515,0.000048190483,0.000024693582,0.00006209274,0.00017181641,0.00011444142,0.0027156298],"genre_scores_gemma":[0.98193306,0.00016715909,0.016446618,0.000028205111,0.000007516526,0.000060875478,0.00015841798,0.0000625568,0.0011357088],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99974424,0.000053606323,0.000025488866,0.000087683475,0.000051343875,0.000037573656],"domain_scores_gemma":[0.99943966,0.00015577227,0.000070622445,0.0001370481,0.00014130533,0.000055540568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008646762,0.00033840872,0.000283823,0.0009843826,0.0005616704,0.00045654675,0.0003085651,0.00034345535,0.0017647747],"category_scores_gemma":[0.001088806,0.00039876162,0.000121553705,0.0007078059,0.00073090446,0.00039010914,0.00056341646,0.00047312133,0.00025066143],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011732674,0.000015071193,0.0051040216,0.000046061323,0.00001767985,0.00006623797,0.000118963144,0.0002351112,0.9899663,0.00026742954,0.00003063302,0.0040152557],"study_design_scores_gemma":[0.000029322311,0.00024144811,0.101098835,0.00001757168,0.00009323047,0.00085741316,0.00025301642,0.002921261,0.89102864,0.0008614051,0.0025686128,0.000029234523],"about_ca_topic_score_codex":0.0010635027,"about_ca_topic_score_gemma":0.003823076,"teacher_disagreement_score":0.0017647747,"about_ca_system_score_codex":0.00029535222,"about_ca_system_score_gemma":0.0002778317,"threshold_uncertainty_score":0.0059037805},"labels":[],"label_agreement":null},{"id":"W2038550574","doi":"10.1029/2005gl022682","title":"Sea ice drift and its relationship to altimetry‐derived ocean currents in the Labrador Sea","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Geology; Empirical orthogonal functions; Altimeter; Sea ice; Climatology; Forcing (mathematics); Sea ice concentration; Ocean current; Sea ice thickness; Oceanography; Arctic ice pack; Geodesy","score_opus":0.03680861817623315,"score_gpt":0.29978949980656516,"score_spread":0.262980881630332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038550574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993512,0.000085699816,0.000030536554,0.000023982157,0.0000017206561,9.580804e-7,0.00030865867,0.0000052950736,0.00019203346],"genre_scores_gemma":[0.99855953,0.00010525687,0.00006321037,0.000011218685,0.0000058053984,0.0000029024156,0.0010400742,0.0000032675587,0.00020881784],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983263,0.000025691219,0.000022693815,0.000037577265,0.000029056879,0.000052378204],"domain_scores_gemma":[0.9993923,0.000120141565,0.0002997949,0.000042948977,0.000092644514,0.000052164603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004152932,0.00024412014,0.00019879758,0.0012434627,0.00020743838,0.00080876227,0.00022866468,0.00030085174,0.0005992259],"category_scores_gemma":[0.0013199848,0.00012916898,0.0002811272,0.001291714,0.00026394604,0.00036015338,0.00032567076,0.00024092777,0.0002495773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015706514,0.00004513608,0.9888657,0.000013252796,0.00007327281,0.00008508561,0.00011537152,0.0013765248,0.0009778744,0.00005340296,0.00026441563,0.0079728635],"study_design_scores_gemma":[0.0000035411597,0.00002208382,0.9985702,0.0000038266285,0.000011033968,0.000030770338,0.000060880608,0.0008315432,0.00022693678,0.000010844684,0.00022464828,0.0000036644763],"about_ca_topic_score_codex":0.071985066,"about_ca_topic_score_gemma":0.11088626,"teacher_disagreement_score":0.92801493,"about_ca_system_score_codex":0.0011071723,"about_ca_system_score_gemma":0.00037742918,"threshold_uncertainty_score":0.14313215},"labels":[],"label_agreement":null},{"id":"W2038660920","doi":"10.1029/2004gl022080","title":"Summertime total ozone variations over middle and polar latitudes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Middle latitudes; Ozone; Latitude; Atmospheric sciences; Polar; Environmental science; Northern Hemisphere; Climatology; Ozone depletion; Southern Hemisphere; Polar night; Stratosphere; Meteorology; Geology; Geography; Physics","score_opus":0.0335648414008604,"score_gpt":0.2791349148735394,"score_spread":0.245570073472679,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038660920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971288,0.00045162547,0.000089486,0.00002363345,0.0000051291004,0.0000017032028,0.0012121457,0.000014720514,0.0010728765],"genre_scores_gemma":[0.998642,0.0001900769,0.00005912318,0.000009126441,0.000008344868,0.0000022968072,0.00085931143,0.0000019944655,0.00022773234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.00000857418,0.0000038184808,0.000016891558,0.000010667474,0.000022504375],"domain_scores_gemma":[0.99987376,0.000026768377,0.00003412485,0.000007336669,0.000027044194,0.000030940184],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012396988,0.00014103134,0.00013295126,0.000504211,0.00019362333,0.00033684555,0.0000538034,0.00009427849,0.001085237],"category_scores_gemma":[0.00023158349,0.00006592943,0.0001471179,0.000493849,0.00007188336,0.00010891311,0.00014616986,0.00009265922,0.00019907813],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000837407,0.000030987416,0.9653764,0.000058751255,0.00015823587,0.00018238493,0.00043181085,0.00091502327,0.013371336,0.00025404867,0.0011733003,0.017210439],"study_design_scores_gemma":[0.000003236005,0.000021082697,0.9989349,0.0000024148471,0.000011867593,0.00003242002,0.00006132452,0.00011451751,0.00024573779,0.000022934692,0.00054790435,0.0000017335976],"about_ca_topic_score_codex":0.0139135085,"about_ca_topic_score_gemma":0.019073127,"teacher_disagreement_score":0.0139135085,"about_ca_system_score_codex":0.00022365592,"about_ca_system_score_gemma":0.000109483,"threshold_uncertainty_score":0.027665079},"labels":[],"label_agreement":null},{"id":"W2038690968","doi":"10.1029/2000gl000034","title":"Neutral winds in the lower thermosphere observed by WINDII during the April 4–5th, 1993 storm","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Thermosphere; Geomagnetic storm; Atmospheric sciences; Storm; Daytime; Earth's magnetic field; Latitude; Altitude (triangle); Geomagnetic latitude; Low latitude; Environmental science; Climatology; Geology; Ionosphere; Physics; Geophysics; Geodesy; Oceanography; Magnetic field","score_opus":0.017248578999603217,"score_gpt":0.26384929770987775,"score_spread":0.24660071871027453,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038690968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989826,0.00003145183,0.0000385902,0.000014498386,0.0000028703805,0.0000045312945,0.00054184545,0.000008227846,0.0003753234],"genre_scores_gemma":[0.99652714,0.000059966784,0.00014089972,0.000015313484,0.000012523582,0.000009826479,0.0029631846,0.000004052155,0.0002671085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998977,0.000008127726,0.0000075698567,0.000014220472,0.00002443969,0.000047864647],"domain_scores_gemma":[0.9997204,0.000016826541,0.00012499983,0.000013377434,0.000052537907,0.000071784314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015476381,0.00020889305,0.0002901199,0.00056925154,0.00047133112,0.00046463715,0.00013252143,0.00022706804,0.0006791468],"category_scores_gemma":[0.000344773,0.00012966136,0.00013662392,0.00057742326,0.00015134382,0.0001596858,0.00028459256,0.00029470414,0.00018732654],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005355018,0.000085775195,0.9750484,0.000018902856,0.00005132413,0.000471545,0.00045447578,0.00031512757,0.01767376,0.00006644218,0.0008067654,0.004471917],"study_design_scores_gemma":[0.000004095365,0.000030448782,0.9992061,0.0000016974628,0.0000051238853,0.00003490854,0.000053354903,0.00010017343,0.00025287372,0.000005138791,0.0003045815,0.0000015103336],"about_ca_topic_score_codex":0.037411105,"about_ca_topic_score_gemma":0.080468096,"teacher_disagreement_score":0.037411105,"about_ca_system_score_codex":0.000506862,"about_ca_system_score_gemma":0.00026365326,"threshold_uncertainty_score":0.07438666},"labels":[],"label_agreement":null},{"id":"W2038697544","doi":"10.1029/2004gl022284","title":"Magma plumbing processes for persistent activity at Poás volcano, Costa Rica","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Impact crater; Geology; Volcano; Magma; Crater lake; Mass wasting; Seismology; Geomorphology; Landslide; Astrobiology","score_opus":0.043584508071807845,"score_gpt":0.27689280896028795,"score_spread":0.2333083008884801,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038697544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987311,0.00009381349,0.000046920235,0.00006141096,0.0000010444224,0.0000046413925,0.0005032249,0.0000100854195,0.0005478273],"genre_scores_gemma":[0.9993505,0.000050865718,0.000048153364,0.0000057005673,0.0000018003544,0.0000033891931,0.0004033784,0.0000022719862,0.00013408005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.000009663884,0.0000038951744,0.000014056631,0.0000082058405,0.000015161217],"domain_scores_gemma":[0.9997775,0.000026740923,0.00008515983,0.000026447738,0.000053866497,0.000030281562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017323019,0.0001424601,0.00014047824,0.0006310275,0.00026537752,0.00045066167,0.00022364334,0.00019216776,0.0005834364],"category_scores_gemma":[0.0006575258,0.0000979011,0.00014022824,0.0007725879,0.00020479396,0.00020072148,0.00042977266,0.00013234199,0.000092304166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006343206,0.000022021106,0.98951226,0.000017932134,0.00004749551,0.00012399832,0.0005882233,0.0010652497,0.0025501763,0.00010105115,0.00053569477,0.0053724498],"study_design_scores_gemma":[9.418034e-7,0.0000023669731,0.99902105,0.0000017322037,0.0000037996579,0.000016015429,0.00010753764,0.0005707265,0.000047618523,0.0000083894,0.00021857444,0.000001200619],"about_ca_topic_score_codex":0.17071848,"about_ca_topic_score_gemma":0.26189923,"teacher_disagreement_score":0.17071848,"about_ca_system_score_codex":0.0008432676,"about_ca_system_score_gemma":0.0003719155,"threshold_uncertainty_score":0.33944958},"labels":[],"label_agreement":null},{"id":"W2038779670","doi":"10.1029/2006gl027895","title":"Descent of the ancient Farallon slab drives localized mantle flow below the New Madrid seismic zone","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Université du Québec à Montréal","funders":"","keywords":"Geology; Intraplate earthquake; Seismology; Induced seismicity; Mantle (geology); Slab; Slab window; Seismic zone; Lithosphere; Geophysics; Plate tectonics; Seismic tomography; Subduction; Tectonics; Oceanic crust","score_opus":0.02706150407703296,"score_gpt":0.27074786822548674,"score_spread":0.2436863641484538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2038779670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867815,0.00003064559,0.00019763266,0.000050762606,0.0000022963686,8.5132655e-7,0.000017094426,0.000012138861,0.0010104096],"genre_scores_gemma":[0.99963605,0.000023557177,0.000063057734,0.000005632593,0.000002762184,7.0253316e-7,0.000019858748,0.0000019617198,0.00024641945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994874,0.00000557594,0.0000017514079,0.000019864505,0.000008895554,0.000015069864],"domain_scores_gemma":[0.9998753,0.000018983805,0.0000523722,0.000010755073,0.000015482521,0.00002710088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009644641,0.00013409152,0.00012432004,0.00024283638,0.00020380109,0.00046271976,0.00019834204,0.00016615678,0.000914754],"category_scores_gemma":[0.0005460771,0.00012886658,0.00009426861,0.00010188095,0.00044068584,0.00021832094,0.00049167004,0.0001682772,0.00014934258],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086801586,0.00010187566,0.635704,0.000094729716,0.00006999114,0.00091863883,0.0018635793,0.017890614,0.3039341,0.006624629,0.00088124553,0.031048648],"study_design_scores_gemma":[0.00004597054,0.000091666996,0.9746074,0.000012991564,0.000024436502,0.000107001295,0.0007469737,0.012285437,0.009693723,0.000997324,0.001363884,0.000023292272],"about_ca_topic_score_codex":0.011946477,"about_ca_topic_score_gemma":0.0130742,"teacher_disagreement_score":0.011946477,"about_ca_system_score_codex":0.00055138126,"about_ca_system_score_gemma":0.00037164043,"threshold_uncertainty_score":0.023753881},"labels":[],"label_agreement":null},{"id":"W2039730779","doi":"10.1029/2006gl028721","title":"Imaging slow failure in triaxially deformed Etna basalt using 3D acoustic‐emission location and X‐ray computed tomography","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Acoustic emission; Basalt; Geology; Deformation (meteorology); Volcano; Shear (geology); Fault (geology); Volume (thermodynamics); Strain rate; Seismology; Compression (physics); Mineralogy; Materials science; Petrology; Composite material; Physics","score_opus":0.027716970181402355,"score_gpt":0.2878585940900741,"score_spread":0.26014162390867174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039730779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891174,0.000034982328,0.0006020414,0.000006584214,0.0000011827111,0.0000049764903,0.00005814992,0.000011993816,0.0003683585],"genre_scores_gemma":[0.99861693,0.0000278719,0.0010028327,0.000004824992,0.0000018271301,0.0000061467013,0.000078691504,0.0000045414786,0.0002563737],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998394,0.000016937322,0.000013970593,0.00003365088,0.00007137152,0.00002460763],"domain_scores_gemma":[0.9996892,0.00005334975,0.0000892684,0.000055326185,0.00007366915,0.000039252463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021243072,0.00019533896,0.00018771882,0.00069250277,0.00019555682,0.00038788616,0.00034405815,0.00042302796,0.00078195456],"category_scores_gemma":[0.0004709539,0.0002240134,0.00012798976,0.00041213873,0.00051149627,0.0002342881,0.0003083275,0.00022710938,0.00021043334],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003152464,0.00007579722,0.07850032,0.000045827917,0.000024221672,0.0005511778,0.00039684726,0.0035897873,0.90907335,0.000084074716,0.000050069906,0.007293298],"study_design_scores_gemma":[0.00003297348,0.00036695803,0.839,0.000014009653,0.00002676234,0.0014216397,0.000336418,0.021066979,0.13690501,0.00007978962,0.0007174026,0.00003199281],"about_ca_topic_score_codex":0.0027679985,"about_ca_topic_score_gemma":0.00453278,"teacher_disagreement_score":0.0027679985,"about_ca_system_score_codex":0.00019637017,"about_ca_system_score_gemma":0.000113441885,"threshold_uncertainty_score":0.005503714},"labels":[],"label_agreement":null},{"id":"W2039751512","doi":"10.1002/2014gl062509","title":"Decadal increase in Ningaloo<i>Niño</i>since the late 1990s","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Prairie Oat Growers Association","keywords":"Subtropics; Oceanography; Climatology; Environmental science; Pacific decadal oscillation; Geology; Current (fluid); Spring (device); Sea surface temperature; Fishery; Biology","score_opus":0.029031392314408367,"score_gpt":0.2970742136960774,"score_spread":0.268042821381669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039751512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.891,0.0193353,0.0022100713,0.004346571,0.0016874417,0.000037511007,0.032735705,0.00023359817,0.0484139],"genre_scores_gemma":[0.9715505,0.008305167,0.0007380146,0.0005903311,0.00035808707,0.000034112563,0.012664779,0.000030651587,0.0057283826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.0000097993825,0.000009473914,0.00003053356,0.000022114737,0.000024803921],"domain_scores_gemma":[0.99964416,0.000027551809,0.00016053235,0.000013085503,0.000103322986,0.000051404873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025337056,0.00026424063,0.00013097933,0.0005488464,0.00026413458,0.00062815956,0.00015810662,0.00016142293,0.0025941147],"category_scores_gemma":[0.0004815501,0.000094976545,0.00017479333,0.0011684308,0.00014516313,0.00029643293,0.00044425332,0.00045803664,0.0004346477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003467768,0.000045793422,0.8298052,0.00092927646,0.0003717999,0.00094490114,0.0011434781,0.0051486585,0.0072692316,0.0067043733,0.03813462,0.10915577],"study_design_scores_gemma":[0.000004650068,0.000013193155,0.9385523,0.000045324814,0.000023303619,0.00018428572,0.00023861583,0.00050045917,0.00031192866,0.00015962904,0.05995635,0.000009855523],"about_ca_topic_score_codex":0.025424697,"about_ca_topic_score_gemma":0.030936979,"teacher_disagreement_score":0.025424697,"about_ca_system_score_codex":0.00060098874,"about_ca_system_score_gemma":0.00035169348,"threshold_uncertainty_score":0.05055338},"labels":[],"label_agreement":null},{"id":"W2039801837","doi":"10.1029/2004gl020111","title":"Testing the linearity of the response to combined greenhouse gas and sulfate aerosol forcing","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Sulfate aerosol; Aerosol; Sulfate; Greenhouse gas; Atmospheric sciences; Forcing (mathematics); Environmental science; Radiative forcing; Climatology; Greenhouse effect; Troposphere; Meteorology; Global warming; Climate change; Chemistry; Geology; Physics","score_opus":0.059539132448832556,"score_gpt":0.3038554358301945,"score_spread":0.24431630338136193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039801837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973864,0.000024670515,0.001558816,0.00008265019,0.0000060133502,0.000009877796,0.00015224489,0.00004447966,0.0007347787],"genre_scores_gemma":[0.9993249,0.0000064580686,0.00027047464,0.000020320276,0.000006547818,0.000010264801,0.00023093744,0.000010092195,0.00011996197],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99827075,0.000593878,0.00010378501,0.0004913926,0.0002974524,0.00024265853],"domain_scores_gemma":[0.99011093,0.0069928076,0.0006086603,0.0013204297,0.00060248864,0.00036456942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026377072,0.00045464645,0.00040825986,0.0003016499,0.00028541888,0.00067220355,0.00064507604,0.0005709798,0.00160377],"category_scores_gemma":[0.011159684,0.00034830195,0.0010224511,0.00029707432,0.0007014033,0.0008237216,0.0014320184,0.0009010092,0.00031240607],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031502137,0.00038720644,0.78481513,0.00012268091,0.001176727,0.00030041998,0.0003815916,0.088741146,0.106619485,0.0010044368,0.00029944672,0.013001426],"study_design_scores_gemma":[0.00012143998,0.00096250756,0.8311151,0.000008256477,0.00020615934,0.0002280801,0.0002946831,0.14586833,0.01949574,0.0011347365,0.00051269645,0.000052244384],"about_ca_topic_score_codex":0.0064382427,"about_ca_topic_score_gemma":0.003628747,"teacher_disagreement_score":0.0064382427,"about_ca_system_score_codex":0.00060076365,"about_ca_system_score_gemma":0.0006145756,"threshold_uncertainty_score":0.013949752},"labels":[],"label_agreement":null},{"id":"W2039805183","doi":"10.1029/2007gl032507","title":"A changing Arctic seasonal ice zone: Observations from 1870–2003 and possible oceanographic consequences","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; Geological Survey of Canada","funders":"","keywords":"Oceanography; Geology; Thermohaline circulation; Arctic; Sea ice; Arctic ice pack; Climatology; Arctic dipole anomaly; Drift ice","score_opus":0.04622993316172107,"score_gpt":0.2612095113617616,"score_spread":0.21497957820004054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2039805183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99428385,0.00044632197,0.00015010228,0.00008819406,0.000019822657,0.000005463009,0.0038594115,0.000009900074,0.0011368695],"genre_scores_gemma":[0.9925648,0.0005500741,0.00047291344,0.00006282352,0.000029579156,0.000014548079,0.0059246165,0.000008599238,0.0003719882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998658,0.000022229226,0.000017791643,0.000035138033,0.000029313662,0.000029704604],"domain_scores_gemma":[0.9994336,0.000056254758,0.0002276956,0.000030285672,0.00018326082,0.00006892286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055749074,0.00019115058,0.00022439603,0.0008318816,0.00030217637,0.00064206286,0.00020435895,0.00025769987,0.0004817698],"category_scores_gemma":[0.00088236376,0.00012641358,0.00024929765,0.0017490092,0.0002291621,0.00033200264,0.00036247514,0.00026751036,0.0002066397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085873224,0.000021219043,0.9917715,0.000046001725,0.000046572175,0.00007142459,0.00046800537,0.00040649864,0.00086675887,0.000044580873,0.00096181023,0.005209878],"study_design_scores_gemma":[0.0000018734675,0.000008161794,0.9980829,0.000010853014,0.00001025523,0.000028593093,0.00019127518,0.00021602813,0.00010972567,0.000007058629,0.0013309495,0.000002341765],"about_ca_topic_score_codex":0.11245651,"about_ca_topic_score_gemma":0.18297073,"teacher_disagreement_score":0.11245651,"about_ca_system_score_codex":0.000885372,"about_ca_system_score_gemma":0.000704058,"threshold_uncertainty_score":0.22360384},"labels":[],"label_agreement":null},{"id":"W2040081989","doi":"10.1029/2009gl039985","title":"Modeling EMIC wave growth during the compression event of 29 June 2007","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Emic and etic; Event (particle physics); Compression (physics); Geology; Seismology; Geodesy; Physics; Astrophysics; Thermodynamics","score_opus":0.01639454376684116,"score_gpt":0.2820954643629387,"score_spread":0.2657009205960975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040081989","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902175,0.000061309736,0.003511586,0.0001739925,0.000022259277,0.000026292804,0.00058565265,0.00015504242,0.005246136],"genre_scores_gemma":[0.99772435,0.000039081577,0.0012989987,0.000021066448,0.00001018027,0.000014326338,0.00038437932,0.000023309403,0.00048430677],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993324,0.000008890937,0.000003013006,0.000012281305,0.000015989395,0.000026646005],"domain_scores_gemma":[0.99982566,0.000054481843,0.000028276023,0.0000135451355,0.000037280453,0.00004079552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018509563,0.00043446006,0.00027895923,0.00026603896,0.0004899057,0.00055131246,0.00070218946,0.000837206,0.0009881774],"category_scores_gemma":[0.00076173694,0.00026981853,0.00035443532,0.00029153485,0.00038945346,0.00038682212,0.00044400775,0.00064808474,0.00014670046],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016833039,0.000079110716,0.023342464,0.000021491227,0.00003265503,0.00030983175,0.0000943723,0.9677776,0.0030230936,0.0014404468,0.0009075051,0.0028030153],"study_design_scores_gemma":[0.000031277912,0.000017636363,0.0061287507,0.0000025666448,0.0000060612974,0.000018352124,0.000028540258,0.99272,0.0006319672,0.00011472781,0.00029303032,0.0000070277893],"about_ca_topic_score_codex":0.08106059,"about_ca_topic_score_gemma":0.045682397,"teacher_disagreement_score":0.08106059,"about_ca_system_score_codex":0.001166144,"about_ca_system_score_gemma":0.0006146649,"threshold_uncertainty_score":0.16117752},"labels":[],"label_agreement":null},{"id":"W2040131119","doi":"10.1029/2005gl023991","title":"The 1999 Chi‐Chi, Taiwan, earthquake as a typical example of seismic activation and quiescence","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Epicenter; Seismology; Geology; Foreshock; Aftershock; Seismic hazard; Shock (circulatory); Earthquake prediction; Seismic microzonation; Peak ground acceleration; Hazard; Ground motion; Medicine","score_opus":0.03426168776906671,"score_gpt":0.2810443119238127,"score_spread":0.24678262415474597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040131119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9905736,0.00011936387,0.0054890807,0.00012589675,0.000017564209,0.000034212346,0.0009450666,0.00011437531,0.0025808695],"genre_scores_gemma":[0.9949064,0.000073589894,0.0034584105,0.000013081768,0.0000079816455,0.000015158207,0.0011349283,0.000005553683,0.0003849449],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996567,0.0000053461363,0.0000041924345,0.000007839748,0.000009248728,0.000007669644],"domain_scores_gemma":[0.99979323,0.00005908536,0.000051637693,0.000025203191,0.000031487376,0.000039418912],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109049244,0.00018129722,0.00011714064,0.0007353096,0.00024800678,0.00020445036,0.0001497073,0.00021607321,0.0008266455],"category_scores_gemma":[0.000541148,0.000047377333,0.00009051572,0.0012505447,0.00017120548,0.00016359989,0.00028087696,0.00016837975,0.00009557983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012428926,0.00022634736,0.71128476,0.00036815912,0.00014127883,0.013156565,0.0014761138,0.023830533,0.08615689,0.006523008,0.010671295,0.14492211],"study_design_scores_gemma":[0.00006915983,0.000532856,0.9285162,0.000027318061,0.00008488206,0.005872545,0.0009472534,0.040546052,0.011164817,0.0020391685,0.010157342,0.00004241928],"about_ca_topic_score_codex":0.0037961612,"about_ca_topic_score_gemma":0.010417193,"teacher_disagreement_score":0.0037961612,"about_ca_system_score_codex":0.00013356844,"about_ca_system_score_gemma":0.00018838476,"threshold_uncertainty_score":0.0075481534},"labels":[],"label_agreement":null},{"id":"W2040245103","doi":"10.1029/2006gl027323","title":"Critical point theory of earthquakes: Observation of correlated and cooperative behavior on earthquake fault systems","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Seismology; Geology; Induced seismicity; Foreshock; Magnitude (astronomy); Remotely triggered earthquakes; Fault (geology); Scaling law; Earthquake swarm; Scaling; Geometry; Physics","score_opus":0.04360130499371933,"score_gpt":0.29147636342607736,"score_spread":0.24787505843235802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040245103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9428719,0.00036295364,0.050964616,0.00015751507,0.000011100853,0.000032918168,0.00011873114,0.00012553933,0.0053546415],"genre_scores_gemma":[0.99799997,0.00007981439,0.0016823573,0.000007260509,0.0000139755775,0.00000880313,0.000042868043,0.0000040864907,0.00016092061],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9999087,0.000011611941,0.000003134254,0.000021441854,0.000035124096,0.000020044148],"domain_scores_gemma":[0.99900407,0.00038432586,0.00021736695,0.00013570924,0.00013474912,0.00012394105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019788378,0.00013949382,0.00023887561,0.0011217587,0.00029400003,0.0003739979,0.00037127075,0.0002538147,0.0011068006],"category_scores_gemma":[0.0024860825,0.00014057686,0.00013773552,0.00068109744,0.0010373277,0.00071895204,0.00045607958,0.00031033996,0.000092495015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004389474,0.00016056656,0.19914289,0.00031905065,0.00016383702,0.0025734028,0.0039098193,0.12257578,0.105902515,0.4759757,0.0058092694,0.08302827],"study_design_scores_gemma":[0.00012694926,0.00019287557,0.22319317,0.0000471889,0.000053753134,0.0023427454,0.0007414216,0.42455503,0.015297161,0.32681465,0.0065450636,0.00008992578],"about_ca_topic_score_codex":0.0012160845,"about_ca_topic_score_gemma":0.0004293247,"teacher_disagreement_score":0.0012160845,"about_ca_system_score_codex":0.00035001108,"about_ca_system_score_gemma":0.00016350056,"threshold_uncertainty_score":0.003702581},"labels":[],"label_agreement":null},{"id":"W2040569206","doi":"10.1029/2000gl012044","title":"Parameterizing tidal dissipation over rough topography","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":479,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Office of Naval Research; National Aeronautics and Space Administration; National Science Foundation","keywords":"Barotropic fluid; Dissipation; Dissipative system; Geology; Geophysics; Internal tide; Boundary layer; Mechanics; Drag; Flow (mathematics); Energy flux; Internal wave; Drag coefficient; Work (physics); Tidal power; Physics; Climatology; Oceanography","score_opus":0.03376805408820652,"score_gpt":0.29350171245542095,"score_spread":0.2597336583672144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040569206","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9339422,0.00016902604,0.060584947,0.00018367317,0.00003860632,0.000046912224,0.0005238088,0.00031872548,0.0041920333],"genre_scores_gemma":[0.9948368,0.00006653093,0.0045236475,0.000009090182,0.000004554344,0.000016165179,0.00014909703,0.000021298982,0.0003728907],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998975,0.00002444108,0.000007720424,0.000021636877,0.000022861685,0.000025843256],"domain_scores_gemma":[0.9996043,0.00020097959,0.000048795202,0.000076465774,0.000038193615,0.000031275904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029259323,0.0005814404,0.00036152266,0.00039436977,0.00029039747,0.00088546355,0.00050222996,0.0005420266,0.0013062241],"category_scores_gemma":[0.0018221185,0.0003247407,0.00058069715,0.0003764889,0.0004476539,0.0010383896,0.0006442604,0.00048399554,0.00014925447],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012106467,0.000011739184,0.0034158449,0.00001022058,0.000014567398,0.000027030897,0.000016096139,0.99273187,0.0012475405,0.00075360015,0.00006292369,0.001696414],"study_design_scores_gemma":[0.00001050347,0.000020267022,0.002319989,0.000003764191,0.00001028973,0.000014641317,0.000012384588,0.9954436,0.0008505215,0.0010622671,0.00024091949,0.00001080778],"about_ca_topic_score_codex":0.011207184,"about_ca_topic_score_gemma":0.0064483928,"teacher_disagreement_score":0.011207184,"about_ca_system_score_codex":0.00052707584,"about_ca_system_score_gemma":0.00049722556,"threshold_uncertainty_score":0.022283912},"labels":[],"label_agreement":null},{"id":"W2040588772","doi":"10.1029/2003gl018080","title":"Causes and development of repeated Arctic Ocean warming events","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Halocline; Oceanography; Climatology; Arctic sea ice decline; Global warming; Arctic; Effects of global warming on oceans; Geology; Thermohaline circulation; Ridge; Sea ice; Environmental science; Arctic ice pack; Inflow; Climate change; Antarctic sea ice; Salinity","score_opus":0.03409518335703358,"score_gpt":0.2766865613214821,"score_spread":0.24259137796444855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040588772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984884,0.00018938149,0.000053473876,0.00012112847,0.000011804418,0.0000045320558,0.00036108037,0.000013870776,0.0007562624],"genre_scores_gemma":[0.99949634,0.000072178605,0.000029460585,0.000011678491,0.000016514752,0.0000027188169,0.00028181882,0.0000025398,0.00008666655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995701,0.00008262814,0.00005058154,0.000128141,0.00007084876,0.00009768665],"domain_scores_gemma":[0.99800986,0.0003392801,0.0009781946,0.00016074014,0.0002591772,0.00025281584],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005622033,0.00018632843,0.00024782217,0.0010028234,0.00041570098,0.0007005228,0.00029448312,0.0006388129,0.0018560366],"category_scores_gemma":[0.0026446406,0.00026274988,0.00049474236,0.0006858445,0.00027237655,0.00032077712,0.0007840871,0.0005491388,0.00019012958],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010762596,0.000025303489,0.9951593,0.000012652958,0.0000860068,0.00025609537,0.0001310348,0.0008978334,0.0004801026,0.00008246022,0.00029826956,0.0024633242],"study_design_scores_gemma":[0.0000046784858,0.000023426855,0.99770075,0.0000065088093,0.00002207819,0.00020000162,0.0001533805,0.0012740551,0.00013863039,0.00004961504,0.00042071208,0.0000061176743],"about_ca_topic_score_codex":0.015748762,"about_ca_topic_score_gemma":0.02052275,"teacher_disagreement_score":0.015748762,"about_ca_system_score_codex":0.0006038049,"about_ca_system_score_gemma":0.0004177377,"threshold_uncertainty_score":0.031314194},"labels":[],"label_agreement":null},{"id":"W2040626118","doi":"10.1029/2002gl015498","title":"Solar wind drivers of Traveling Convection Vortices","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Space and Astronautical Science; Natural Resources Canada; Canadian Space Agency; Augsburg University; National Science Foundation","keywords":"Foreshock; Physics; Solar wind; Magnetosphere; Convection; Geophysics; Vortex; Line (geometry); Interplanetary magnetic field; Mechanics; Geology; Magnetic field; Seismology; Geometry","score_opus":0.01709162584116131,"score_gpt":0.2814677524026792,"score_spread":0.2643761265615179,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2040626118","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909985,0.00012975643,0.00014388694,0.000017622295,0.000004828205,0.0000026480764,0.000079657904,0.0000068461627,0.0005148511],"genre_scores_gemma":[0.9996929,0.000041072755,0.00007868048,0.000004532791,0.000005129795,0.0000013592785,0.00010761797,0.0000011842684,0.00006761021],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999329,0.0000059316726,0.0000047768535,0.000011244319,0.000016457881,0.000028717208],"domain_scores_gemma":[0.99960476,0.00006951808,0.00018479128,0.000026714386,0.00005996212,0.0000543232],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010280436,0.00008614938,0.00012154258,0.00037610668,0.00016505837,0.00032841077,0.00010436201,0.00012905116,0.00066621415],"category_scores_gemma":[0.00059509726,0.0000863695,0.000088772686,0.0002201208,0.00010339237,0.00018031643,0.0003227456,0.00016281015,0.00006320237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055009767,0.000048433507,0.88016313,0.000103399434,0.00010515743,0.001412216,0.00059059093,0.0015793386,0.08249258,0.0011685647,0.00089666486,0.030889757],"study_design_scores_gemma":[0.000019748588,0.0001189088,0.98905164,0.000021428488,0.000029854224,0.0004534465,0.0003164204,0.0025261664,0.0055021765,0.00032740438,0.0016211481,0.000011563353],"about_ca_topic_score_codex":0.0016280658,"about_ca_topic_score_gemma":0.0032274183,"teacher_disagreement_score":0.0016280658,"about_ca_system_score_codex":0.00012819031,"about_ca_system_score_gemma":0.0001140607,"threshold_uncertainty_score":0.0032371283},"labels":[],"label_agreement":null},{"id":"W2041371274","doi":"10.1029/2001gl014052","title":"The changing relationship between the NAO and northern hemisphere climate variability","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Northern Hemisphere; Proxy (statistics); Climatology; Storm; Climate change; Geology; North Atlantic oscillation; Oceanography","score_opus":0.03998716178029668,"score_gpt":0.26913539094573047,"score_spread":0.2291482291654338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041371274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974546,0.000113772265,0.00009308529,0.000106444495,0.000007946467,0.0000013397481,0.00016734736,0.0000062544323,0.002049249],"genre_scores_gemma":[0.9994998,0.00006771362,0.000053391097,0.00001670252,0.000011349574,9.891626e-7,0.00016236048,0.0000025251804,0.00018515553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000023888491,0.00000986667,0.000036752943,0.000019018049,0.000021959895],"domain_scores_gemma":[0.9991485,0.00025811009,0.00027431428,0.000064721535,0.000140856,0.00011345548],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029615892,0.00007256887,0.00013729047,0.00051771884,0.00023720179,0.00070833764,0.00009614238,0.00019583559,0.0012549171],"category_scores_gemma":[0.0022964461,0.000091873175,0.0000988282,0.00072551786,0.0003271455,0.00032584317,0.00026775838,0.00023514345,0.00020225397],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005647057,0.000009282235,0.99418795,0.000005534441,0.000040866802,0.000037237478,0.00015330438,0.00029968578,0.0013731468,0.0002697117,0.00014915079,0.0034177457],"study_design_scores_gemma":[0.0000010459734,0.000006726518,0.9991817,0.0000012581485,0.000004408086,0.000023049148,0.00006153883,0.0003482743,0.00005705949,0.0000686601,0.00024453405,0.0000016742862],"about_ca_topic_score_codex":0.014027829,"about_ca_topic_score_gemma":0.02155229,"teacher_disagreement_score":0.014027829,"about_ca_system_score_codex":0.0004188428,"about_ca_system_score_gemma":0.0002798735,"threshold_uncertainty_score":0.027892351},"labels":[],"label_agreement":null},{"id":"W2041449060","doi":"10.1029/2009gl039588","title":"Smoothness of Titan's Ontario Lacus: Constraints from Cassini RADAR specular reflection data","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Titan (rocket family); Specular reflection; Geology; Radar; Remote sensing; Geodesy; Optics; Physics; Astrobiology; Computer science","score_opus":0.07445118864732758,"score_gpt":0.3394828341154601,"score_spread":0.2650316454681325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041449060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99565256,0.000047423986,0.0012685902,0.00008575246,0.000002356128,0.0000062368363,0.0007206095,0.000054065247,0.0021624418],"genre_scores_gemma":[0.9984742,0.000026502052,0.000624998,0.00000766905,0.0000022511408,0.0000022027505,0.00069422304,0.000018215515,0.00014974168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997757,0.000023679382,0.000010706602,0.000051151314,0.00007612938,0.00006257217],"domain_scores_gemma":[0.99908674,0.00031732317,0.00013621297,0.00014743254,0.00021566998,0.00009653843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030818378,0.00020405132,0.00024614084,0.0005637938,0.0007802385,0.0010639178,0.00037466557,0.00024295473,0.0008059688],"category_scores_gemma":[0.002724857,0.0002816305,0.00021463545,0.0006918224,0.0006101252,0.00034101275,0.0005193925,0.0003171766,0.00019490361],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007375168,0.000065370026,0.8002037,0.00013466815,0.00010913073,0.0006833305,0.0012531251,0.034817733,0.13030694,0.0024423236,0.0026739328,0.02657219],"study_design_scores_gemma":[0.000015538317,0.000016819635,0.9573334,0.000007484874,0.000019336163,0.00006338421,0.0002915262,0.037611153,0.0030127664,0.00027461624,0.0013229776,0.000030973035],"about_ca_topic_score_codex":0.32750037,"about_ca_topic_score_gemma":0.48441198,"teacher_disagreement_score":0.32750037,"about_ca_system_score_codex":0.0014002055,"about_ca_system_score_gemma":0.0014380758,"threshold_uncertainty_score":0.65118825},"labels":[],"label_agreement":null},{"id":"W2041476815","doi":"10.1002/2014gl061975","title":"Static stress triggering explains the empirical aftershock distance decay","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aftershock; Induced seismicity; Geology; Scaling; Coulomb; Stress (linguistics); Seismology; Fractal; Range (aeronautics); Exponent; Statistical physics; Fractal dimension; Physics; Magnitude (astronomy); Fault (geology); Geometry; Mathematics; Astrophysics; Mathematical analysis; Electron; Materials science","score_opus":0.08962667359589133,"score_gpt":0.3236759746102895,"score_spread":0.2340493010143982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041476815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99333936,0.00006768096,0.0048923786,0.000058680107,0.000004032411,0.000007914421,0.000063490756,0.00005130524,0.0015151447],"genre_scores_gemma":[0.9997099,0.000017169907,0.00016873537,0.0000038568255,0.000001103149,0.0000020926723,0.000020640624,0.0000046560767,0.00007183718],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999341,0.000010088067,0.0000034505138,0.000014692673,0.000013289912,0.000024410667],"domain_scores_gemma":[0.99939835,0.00025143276,0.00012310158,0.00010122323,0.000063677006,0.00006224928],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033072513,0.00021462297,0.00025377478,0.00038618155,0.00020314613,0.00039369584,0.00040715138,0.00030843125,0.0012842029],"category_scores_gemma":[0.0023399354,0.00013500603,0.00027494732,0.00026040606,0.0004687072,0.0004718528,0.00026963154,0.00030908003,0.000116933166],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021509256,0.00016046959,0.12545136,0.0001291839,0.00008819765,0.00051323336,0.000310533,0.8203509,0.019186143,0.015861787,0.0013485273,0.016384564],"study_design_scores_gemma":[0.000021640479,0.000056717712,0.033614494,0.000010638989,0.00001330447,0.00007510588,0.000055199693,0.96177584,0.0012608073,0.0028713197,0.00023436287,0.000010594086],"about_ca_topic_score_codex":0.0061305366,"about_ca_topic_score_gemma":0.004177548,"teacher_disagreement_score":0.0061305366,"about_ca_system_score_codex":0.00047722246,"about_ca_system_score_gemma":0.00025204348,"threshold_uncertainty_score":0.012189746},"labels":[],"label_agreement":null},{"id":"W2041616631","doi":"10.1002/2014gl060184","title":"Isolating the anthropogenic component of Arctic warming","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Los Alamos National Laboratory; Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Climatology; Arctic; Environmental science; Forcing (mathematics); Radiative forcing; Arctic oscillation; Atmospheric sciences; Climate model; Arctic geoengineering; The arctic; Global warming; Climate change; Arctic ice pack; Sea ice; Oceanography; Geology","score_opus":0.027567898074099744,"score_gpt":0.28131004868556536,"score_spread":0.2537421506114656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041616631","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909905,0.00013819423,0.006587722,0.00026076718,0.000017264914,0.0000064391525,0.00031660983,0.000024651943,0.0016579062],"genre_scores_gemma":[0.9990476,0.000057826215,0.00057916867,0.000008033105,0.000010093245,0.000002458466,0.0001944599,0.0000040060186,0.0000963973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994862,0.00025437697,0.00003045761,0.00008880877,0.00008477311,0.000055320543],"domain_scores_gemma":[0.99771535,0.001134064,0.0004318418,0.0002091212,0.00043076207,0.00007882752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012149591,0.00025668147,0.00020120379,0.00091234903,0.0003099733,0.00058842765,0.00020391245,0.0001512939,0.0012904543],"category_scores_gemma":[0.0045505567,0.00011554941,0.0006110939,0.0010294071,0.00037458184,0.00047563371,0.0008037094,0.00043467898,0.00009837763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000088728615,0.00005143349,0.952129,0.000062214414,0.00035160081,0.000051695893,0.00028959097,0.022645285,0.0018797531,0.0038609535,0.00032284233,0.018266954],"study_design_scores_gemma":[0.000010342668,0.00009903196,0.89569706,0.000057297704,0.0002205328,0.00006296248,0.0007492051,0.09446213,0.0024808655,0.0041501317,0.0019915265,0.000018747809],"about_ca_topic_score_codex":0.01783861,"about_ca_topic_score_gemma":0.031848174,"teacher_disagreement_score":0.01783861,"about_ca_system_score_codex":0.0004217819,"about_ca_system_score_gemma":0.0011019281,"threshold_uncertainty_score":0.035469532},"labels":[],"label_agreement":null},{"id":"W2041790123","doi":"10.1029/2006gl025785","title":"Role of plasma waves in Mars' atmospheric loss","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Mars Exploration Program; Ionosphere; Atmosphere of Mars; Solar wind; Polar wind; Physics; Atmospheric sciences; Plasma; Geophysics; Atmosphere (unit); Outflow; Population; Exosphere; Astrobiology; Ion; Environmental science; Magnetopause; Meteorology; Martian","score_opus":0.013545361788601707,"score_gpt":0.2587625197461066,"score_spread":0.24521715795750487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041790123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9884321,0.0029432469,0.0005132132,0.0007596926,0.000023180748,0.000005109764,0.000070327886,0.000033724766,0.007219388],"genre_scores_gemma":[0.99830854,0.00093560846,0.00012773696,0.00003236387,0.000043303848,0.0000029423704,0.00004885061,0.0000042205793,0.0004963606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993694,0.000011574268,0.0000031093193,0.000007180557,0.000017778628,0.000023450471],"domain_scores_gemma":[0.9998281,0.000048184742,0.000050348874,0.000015238715,0.000034847053,0.000023305196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002301773,0.0001577392,0.000108795095,0.00036737134,0.00054388295,0.00074087793,0.0002486714,0.00028524638,0.0010721112],"category_scores_gemma":[0.00052926457,0.00010717885,0.00010307558,0.00023079327,0.00030879228,0.0005300074,0.00044226483,0.00026597304,0.0001645624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014668272,0.00023579468,0.6743286,0.00032785372,0.0001683987,0.0040483195,0.0019780484,0.0059481,0.082684934,0.015022295,0.0052230335,0.20856778],"study_design_scores_gemma":[0.00007982588,0.00020819744,0.94253993,0.0000536897,0.00007872804,0.0015891258,0.0015043806,0.009968138,0.012225268,0.00970254,0.022025244,0.000024885943],"about_ca_topic_score_codex":0.0010435963,"about_ca_topic_score_gemma":0.0006024497,"teacher_disagreement_score":0.0010721112,"about_ca_system_score_codex":0.00028712332,"about_ca_system_score_gemma":0.000111908375,"threshold_uncertainty_score":0.0035865903},"labels":[],"label_agreement":null},{"id":"W2041798110","doi":"10.1029/2006gl027930","title":"Zooplankton anomalies in the California Current system before and during the warm ocean conditions of 2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Consejo Nacional de Ciencia y Tecnología","keywords":"Zooplankton; Upwelling; Oceanography; Dominance (genetics); Current (fluid); Spring (device); Productivity; Environmental science; Phytoplankton; Biomass (ecology); Geology; Ecology; Nutrient; Biology","score_opus":0.01208401406107181,"score_gpt":0.24410484526590354,"score_spread":0.23202083120483172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041798110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99758613,0.00019528822,0.00003429987,0.000058075682,0.000013574965,0.0000048822453,0.00071621017,0.000009588718,0.0013819947],"genre_scores_gemma":[0.99806565,0.00016259885,0.00007592925,0.00003544841,0.000009276923,0.000004094863,0.0011635543,0.0000025879183,0.00048083637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988925,0.000005500627,0.000011022526,0.0000329536,0.000032142496,0.000029179182],"domain_scores_gemma":[0.9995022,0.000026595837,0.00017318285,0.000019285417,0.00017377861,0.00010505103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020056519,0.00016571897,0.00020499242,0.0009372471,0.0006734671,0.00096356665,0.00020097273,0.00026346455,0.00076938386],"category_scores_gemma":[0.0006151241,0.00018214295,0.00015876075,0.0006799573,0.0001831562,0.00031525112,0.00037686556,0.00031257828,0.00008325728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016183933,0.00005992003,0.98878914,0.000027478922,0.00009771079,0.00009778406,0.0005085531,0.0004729027,0.0011232243,0.00012387367,0.0018398822,0.0066978163],"study_design_scores_gemma":[0.0000015756747,0.000008188096,0.99944085,0.0000037192024,0.0000062552667,0.0000073325905,0.00008596962,0.00006138683,0.000027573775,0.000005067182,0.00035026082,0.0000017317353],"about_ca_topic_score_codex":0.2956661,"about_ca_topic_score_gemma":0.5110145,"teacher_disagreement_score":0.2956661,"about_ca_system_score_codex":0.0018824851,"about_ca_system_score_gemma":0.00073527533,"threshold_uncertainty_score":0.58789027},"labels":[],"label_agreement":null},{"id":"W2041809164","doi":"10.1029/2008gl033263","title":"Megatides in the Arctic Ocean under glacial conditions","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Oceanography; Geology; Arctic; Archipelago; Ocean current; Glacial period; Climatology; Arctic dipole anomaly; Stratification (seeds); Arctic sea ice decline; The arctic; Last Glacial Maximum; Ocean surface topography; Thermohaline circulation; Ice sheet; Arctic ice pack; Drift ice; Holocene; Paleontology","score_opus":0.06008868364985213,"score_gpt":0.3156957482450388,"score_spread":0.2556070645951867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2041809164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944711,0.00013402631,0.0011455895,0.00015831002,0.000051617862,0.0000057818,0.00018872642,0.00004126048,0.0038037333],"genre_scores_gemma":[0.99870014,0.0001055571,0.0004615278,0.000034023702,0.000009653214,0.00001174195,0.00027987178,0.00001542588,0.00038203932],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989676,0.00002136917,0.0000063015036,0.000024790277,0.000020171216,0.00003054527],"domain_scores_gemma":[0.9996933,0.00008882106,0.00006902017,0.000032614076,0.00005041261,0.000065934175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037166046,0.00028158646,0.00040219008,0.0003131244,0.0007798159,0.0014047828,0.00045843108,0.00059327227,0.0027996434],"category_scores_gemma":[0.0014300238,0.00027731594,0.0005076588,0.00034351804,0.0005025539,0.000765657,0.00095350767,0.0005876902,0.00019546397],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030265606,0.000103862156,0.12037153,0.00008718356,0.00022316114,0.0006632427,0.0003566282,0.8517063,0.0032012598,0.0132878665,0.0021007452,0.0075955736],"study_design_scores_gemma":[0.0001575108,0.0001642557,0.06345924,0.00004862428,0.0001029434,0.00015436091,0.00079574366,0.9221982,0.0011893766,0.00814601,0.0035308674,0.00005285979],"about_ca_topic_score_codex":0.01992293,"about_ca_topic_score_gemma":0.025117183,"teacher_disagreement_score":0.01992293,"about_ca_system_score_codex":0.0006540346,"about_ca_system_score_gemma":0.0006967066,"threshold_uncertainty_score":0.039613962},"labels":[],"label_agreement":null},{"id":"W2042508250","doi":"10.1029/2005gl025020","title":"Neutral atom emission in the direction of the high‐latitude magnetopause for northward IMF: Simultaneous observations from IMAGE spacecraft and SuperDARN radar","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Magnetopause; Magnetosphere; Geophysics; Ionosphere; Physics; Energetic neutral atom; Interplanetary magnetic field; Magnetic reconnection; Solar wind; Field line; Geology; Magnetosheath; Magnetic field; Plasma","score_opus":0.01246064601563833,"score_gpt":0.259306625727117,"score_spread":0.24684597971147865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042508250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965481,0.00014009152,0.000361261,0.000056744128,0.000007521531,0.000008188226,0.00044275413,0.000037855687,0.0023976264],"genre_scores_gemma":[0.9959423,0.00011195906,0.001976666,0.00006510391,0.000019924579,0.000008259354,0.0011459207,0.00001391241,0.000715858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.0000043611117,0.0000013697011,0.000013368325,0.000014858361,0.000012289056],"domain_scores_gemma":[0.9998909,0.000011501117,0.0000310473,0.000009357657,0.000019350318,0.000037944115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001400867,0.00013376102,0.00018115985,0.0004335042,0.00022883502,0.0003022089,0.00016405761,0.00019814678,0.0005916508],"category_scores_gemma":[0.00019201738,0.00016796043,0.0001255077,0.00021047748,0.00012324264,0.00017884659,0.00026888706,0.0002617058,0.0001589004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078386633,0.00014495775,0.5158244,0.00007134577,0.00011400565,0.0008036917,0.00062054273,0.0005783465,0.45426473,0.00030386142,0.0019895164,0.024500718],"study_design_scores_gemma":[0.0000329959,0.000051415027,0.9917902,0.00000478702,0.000023872113,0.0002770044,0.000059154747,0.0008147706,0.005860592,0.00004336799,0.0010335969,0.0000083197],"about_ca_topic_score_codex":0.0037646,"about_ca_topic_score_gemma":0.0145494575,"teacher_disagreement_score":0.0037646,"about_ca_system_score_codex":0.00029859887,"about_ca_system_score_gemma":0.00014546326,"threshold_uncertainty_score":0.0074853897},"labels":[],"label_agreement":null},{"id":"W2042536594","doi":"10.1029/2002gl016275","title":"Orbital control of low‐latitude seasonality during the Eemian","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"","keywords":"Eemian; Climatology; Latitude; Low latitude; Milankovitch cycles; Seasonality; Environmental science; Forcing (mathematics); Climate oscillation; Insolation; Range (aeronautics); Atmospheric sciences; Paleoclimatology; Orbital forcing; Climate change; Geology; Glacial period; Global warming; Oceanography; Interglacial; Effects of global warming; Ecology","score_opus":0.02166337344506962,"score_gpt":0.2803391848781738,"score_spread":0.25867581143310414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042536594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998604,0.000087524015,0.00016699974,0.00001812636,0.0000026441282,0.0000017179289,0.000098888224,0.000009147546,0.0010108642],"genre_scores_gemma":[0.99955994,0.00002692586,0.0000966245,0.0000046823566,0.0000021854032,0.000001987765,0.00010822113,0.0000037847706,0.00019563263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.000008014968,0.0000041444446,0.000014527162,0.0000060035118,0.000015102935],"domain_scores_gemma":[0.99978155,0.000028446277,0.00010176624,0.000017431781,0.000042576983,0.000028215783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015473666,0.00012346814,0.0001912671,0.00038908553,0.00025038197,0.000374368,0.00011185823,0.0000894478,0.000725136],"category_scores_gemma":[0.0005281309,0.00010844697,0.00006367011,0.00024956805,0.00019522985,0.00011733896,0.00024496182,0.00012389105,0.00010836634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000745897,0.000058180747,0.79284376,0.000080224905,0.00007581429,0.0001841526,0.0011176948,0.0017356457,0.17088413,0.0007170602,0.0006195633,0.030937897],"study_design_scores_gemma":[0.000004512747,0.00001473678,0.9976909,0.000003607128,0.000008709189,0.000019826835,0.000060168873,0.00068740547,0.00092776475,0.000033995904,0.0005453246,0.000002980384],"about_ca_topic_score_codex":0.008002972,"about_ca_topic_score_gemma":0.027869422,"teacher_disagreement_score":0.008002972,"about_ca_system_score_codex":0.0003155533,"about_ca_system_score_gemma":0.00013178852,"threshold_uncertainty_score":0.015912771},"labels":[],"label_agreement":null},{"id":"W2042588300","doi":"10.1029/2000gl012778","title":"Imaging the Seattle Fault Zone with high‐resolution seismic tomography","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Seismology; Fault (geology); Thrust fault; Geophysical imaging; Quaternary; Slip (aerodynamics); Paleontology","score_opus":0.016817016607523855,"score_gpt":0.25069661388051073,"score_spread":0.23387959727298688,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042588300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98109686,0.00029089735,0.012830128,0.00015139225,0.000013800225,0.000017126358,0.0005478859,0.00017830441,0.004873581],"genre_scores_gemma":[0.9832481,0.00028748187,0.014875967,0.000026926838,0.000012208527,0.000013297109,0.00041016008,0.000016356784,0.0011095873],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999666,0.000006131165,0.0000018204965,0.000008392225,0.000009967611,0.0000070202636],"domain_scores_gemma":[0.9999305,0.000013397981,0.000015507727,0.000010877803,0.000017703664,0.0000119704],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000824212,0.00016160018,0.000059493057,0.0007795046,0.00014055434,0.00036959563,0.00014150118,0.00023209631,0.00092395593],"category_scores_gemma":[0.00028875837,0.00017751192,0.00007210016,0.00049149623,0.00012140799,0.00028119612,0.0002454537,0.00019713539,0.00012453028],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042400038,0.00021338875,0.18485571,0.00015967574,0.000114990704,0.0025174133,0.0010229461,0.017573934,0.6484454,0.0020949696,0.005009746,0.1375677],"study_design_scores_gemma":[0.00014644966,0.00029930228,0.8078239,0.00013827597,0.00012421366,0.0042039244,0.0018507182,0.105711944,0.0516648,0.0021256555,0.025809396,0.0001014582],"about_ca_topic_score_codex":0.0069215475,"about_ca_topic_score_gemma":0.018741347,"teacher_disagreement_score":0.0069215475,"about_ca_system_score_codex":0.00014108406,"about_ca_system_score_gemma":0.0001774048,"threshold_uncertainty_score":0.013762534},"labels":[],"label_agreement":null},{"id":"W2042620826","doi":"10.1029/2001gl013514","title":"Simulations of Heinrich Events in a coupled ocean‐atmosphere‐sea ice model","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Meltwater; Geology; Iceberg; Ice sheet; Climatology; Sea ice; Atmosphere (unit); Northern Hemisphere; Climate model; North Atlantic Deep Water; Oceanography; Cryosphere; Ice-sheet model; Antarctic sea ice; Glacial period; Thermohaline circulation; Climate change; Meteorology; Geomorphology; Geography","score_opus":0.05152854474769118,"score_gpt":0.3027551918251927,"score_spread":0.25122664707750153,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042620826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936056,0.000100600155,0.0011113529,0.0002844606,0.000026503307,0.000024308096,0.000893857,0.000120992656,0.003832276],"genre_scores_gemma":[0.99675155,0.00007645369,0.001107058,0.00006584268,0.000009324896,0.000034948644,0.0009641347,0.000039294562,0.0009515019],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998306,0.00004497092,0.000010766516,0.000032486994,0.0000207674,0.000060467795],"domain_scores_gemma":[0.9993513,0.0002674522,0.00007141638,0.000038289738,0.00008791766,0.00018368683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004231401,0.0005973875,0.0006876155,0.00043890288,0.0007370906,0.000979348,0.0012539498,0.0015013503,0.0022773272],"category_scores_gemma":[0.001786783,0.00054696423,0.000793292,0.00061193196,0.00076386024,0.0009005676,0.001066475,0.0011424207,0.00019033001],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019823929,0.00008979107,0.006359804,0.000017911383,0.000059689577,0.00008851726,0.000062345396,0.9901031,0.00060643954,0.001220396,0.0005338259,0.0006599528],"study_design_scores_gemma":[0.000108142,0.000051154235,0.0027246766,0.000004511188,0.000020564581,0.000007080714,0.00006655228,0.9960924,0.00017426813,0.0005145251,0.00022510739,0.00001098374],"about_ca_topic_score_codex":0.0949805,"about_ca_topic_score_gemma":0.061688054,"teacher_disagreement_score":0.0949805,"about_ca_system_score_codex":0.0018025091,"about_ca_system_score_gemma":0.0011920393,"threshold_uncertainty_score":0.18885529},"labels":[],"label_agreement":null},{"id":"W2042624076","doi":"10.1029/1999gl011333","title":"A model estimate of cooling in the mesosphere and lower thermosphere due to the CO<sub>2</sub> Increase over the last 3–4 decades","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Thermosphere; Mesosphere; Atmospheric sciences; Environmental science; Mixing ratio; Altitude (triangle); Forcing (mathematics); Radiative cooling; Ozone; Climatology; Physics; Ionosphere; Meteorology; Stratosphere; Geophysics; Geology","score_opus":0.012616611304539912,"score_gpt":0.2833517143833144,"score_spread":0.2707351030787745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042624076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9828263,0.00014436705,0.011771154,0.00023539073,0.000014399134,0.000018871933,0.0013387151,0.0002122716,0.0034385493],"genre_scores_gemma":[0.996906,0.000051489013,0.0021403006,0.000018661018,0.0000066282423,0.00002148339,0.0006603491,0.000016317243,0.00017880774],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999664,0.000007709867,0.0000015818133,0.000010240443,0.00000557564,0.0000085138845],"domain_scores_gemma":[0.9998247,0.000062904975,0.000030417988,0.000019493968,0.0000433577,0.000019108971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026292703,0.00046736724,0.00022758954,0.00023675441,0.0002451312,0.00036522147,0.00039797986,0.00039427725,0.0007797583],"category_scores_gemma":[0.0005688952,0.00019661953,0.00042904547,0.0001720148,0.00015389631,0.0004773915,0.00025519638,0.00029707517,0.0001660084],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002020714,0.00007675107,0.04510787,0.000066179775,0.00015183298,0.00007840208,0.00003870037,0.925409,0.01869209,0.0024765509,0.0011517114,0.006548828],"study_design_scores_gemma":[0.00007212004,0.000097072196,0.053461287,0.000010902609,0.000065085966,0.00003211507,0.00003068641,0.93700045,0.006124308,0.0021822602,0.0008983839,0.000025252979],"about_ca_topic_score_codex":0.014255181,"about_ca_topic_score_gemma":0.010892644,"teacher_disagreement_score":0.014255181,"about_ca_system_score_codex":0.00064140814,"about_ca_system_score_gemma":0.00059655076,"threshold_uncertainty_score":0.028344393},"labels":[],"label_agreement":null},{"id":"W2042704881","doi":"10.1029/2007gl031812","title":"Transformation of the Labrador Sea Water in the subpolar North Atlantic","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Thermohaline circulation; Isopycnal; Geology; Oceanography; North Atlantic Deep Water; Hydrography; Salinity; Temperature salinity diagrams; Water mass; Structural basin; Climatology; Convection; Geography; Geomorphology; Meteorology","score_opus":0.01747641290078835,"score_gpt":0.2465302299427043,"score_spread":0.22905381704191594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2042704881","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99849236,0.00015526173,0.000026314956,0.000019829711,0.0000014410051,0.0000025126444,0.00011592944,0.0000052222977,0.0011811053],"genre_scores_gemma":[0.9991253,0.0001493393,0.00005110132,0.000012803846,0.0000016553213,0.0000022040251,0.00015507374,0.0000028703553,0.0004996729],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999584,0.000004721979,0.0000027389071,0.000011617502,0.000008355453,0.000014130554],"domain_scores_gemma":[0.9999242,0.0000048813963,0.000026476277,0.0000058062737,0.000021508007,0.000017170329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000063868654,0.00011292275,0.00012229884,0.00049059076,0.0002419614,0.0004962795,0.0001221958,0.000098782315,0.00062726036],"category_scores_gemma":[0.00016974902,0.00006214115,0.00014490535,0.00043156897,0.0002781744,0.00018127199,0.00022828912,0.000115872484,0.0001887962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057949364,0.00004045639,0.7957898,0.00007217994,0.00003934848,0.00060966366,0.0017654835,0.0008424827,0.13862273,0.0005733662,0.0003780911,0.060686912],"study_design_scores_gemma":[0.0000016256143,0.0000297007,0.9968839,0.0000029155012,0.000004304626,0.0000521639,0.00033308964,0.00017154982,0.001518694,0.000024562518,0.0009746272,0.0000028763181],"about_ca_topic_score_codex":0.07010735,"about_ca_topic_score_gemma":0.0785803,"teacher_disagreement_score":0.07010735,"about_ca_system_score_codex":0.0009225001,"about_ca_system_score_gemma":0.000397404,"threshold_uncertainty_score":0.13939852},"labels":[],"label_agreement":null},{"id":"W2043120550","doi":"10.1029/2006gl028329","title":"Ground based identification of dispersionless electron injections","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Riometer; Physics; Electron; Substorm; Flux (metallurgy); Scattering; Ionosphere; Computational physics; Range (aeronautics); Energy (signal processing); Geophysics; Atomic physics; Astrophysics; Magnetosphere; Nuclear physics; Optics; Chemistry; Plasma; Materials science","score_opus":0.014304547217755823,"score_gpt":0.3068877082927324,"score_spread":0.29258316107497656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043120550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968791,0.0000565653,0.0016683454,0.000009182256,0.000002576985,0.000007810996,0.00019311607,0.00006821607,0.0011150193],"genre_scores_gemma":[0.997538,0.000019673915,0.0017121024,0.0000069100947,0.0000034620346,0.000003426864,0.00046524167,0.000011602355,0.00023959739],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980277,0.000029440684,0.000012638635,0.00006129988,0.00005131839,0.000042494485],"domain_scores_gemma":[0.99863786,0.00038620777,0.00039825265,0.00019932499,0.00027578953,0.000102522914],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027417796,0.00015560667,0.00025575224,0.000930543,0.00016908735,0.0005157249,0.00027107346,0.00029952152,0.0006920765],"category_scores_gemma":[0.001250793,0.000107676606,0.00015656604,0.0004759625,0.00016003137,0.00030390464,0.0004186979,0.00015785084,0.00017608021],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006016131,0.000057363908,0.8663503,0.000060155635,0.00008052846,0.0005371362,0.00044954548,0.003924988,0.07912878,0.00061020046,0.0004745385,0.04772483],"study_design_scores_gemma":[0.000024959772,0.00013313738,0.93397784,0.00001533186,0.000056830744,0.0006225678,0.00017172581,0.027023543,0.03583472,0.00040667603,0.0017160025,0.000016745264],"about_ca_topic_score_codex":0.0013451242,"about_ca_topic_score_gemma":0.0027452386,"teacher_disagreement_score":0.0013451242,"about_ca_system_score_codex":0.00020132046,"about_ca_system_score_gemma":0.0000981024,"threshold_uncertainty_score":0.00267452},"labels":[],"label_agreement":null},{"id":"W2043178035","doi":"10.1002/2014gl061272","title":"Bayesian confidence intervals for the magnitude of the largest aftershock","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Aftershock; Magnitude (astronomy); Confidence interval; Bayesian probability; Statistics; Sequence (biology); Geology; Seismology; Mathematics; Physics; Biology","score_opus":0.04009245604456699,"score_gpt":0.2969755475921919,"score_spread":0.2568830915476249,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043178035","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.18613766,0.0016147397,0.8058261,0.00037027398,0.00006596005,0.00009469612,0.0011193121,0.00048880384,0.0042824433],"genre_scores_gemma":[0.91939706,0.00096216664,0.07558243,0.00009725669,0.00013727273,0.00015391437,0.0027199283,0.00008624341,0.0008638265],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9958056,0.0017783627,0.0002746396,0.0009937396,0.00088979845,0.0002577229],"domain_scores_gemma":[0.89640546,0.0910859,0.0047794147,0.002712022,0.004296752,0.00072044437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.013989419,0.0008233854,0.0011825034,0.003033973,0.00059100863,0.0023042436,0.0020412537,0.0014482761,0.0034868377],"category_scores_gemma":[0.090074845,0.00040460526,0.0013437574,0.0019412237,0.0016740056,0.002445931,0.001436235,0.002011522,0.00058672344],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009414355,0.00019646938,0.04769694,0.00039112472,0.00063584,0.00050841423,0.0006510901,0.6393105,0.0030182502,0.14669052,0.0038259395,0.15613346],"study_design_scores_gemma":[0.00006777082,0.00014635288,0.019772852,0.0002227235,0.00013377762,0.00029180315,0.00017968404,0.89083004,0.0016912777,0.08494249,0.0016171887,0.00010407231],"about_ca_topic_score_codex":0.0030951868,"about_ca_topic_score_gemma":0.002055345,"teacher_disagreement_score":0.013989419,"about_ca_system_score_codex":0.000776489,"about_ca_system_score_gemma":0.0008168863,"threshold_uncertainty_score":0.07398403},"labels":[],"label_agreement":null},{"id":"W2043208768","doi":"10.1029/2000gl012404","title":"Observed changes in Arctic Ocean temperature structure over the past half decade","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research; U.S. Navy","keywords":"Geology; Oceanography; Arctic; Advection; Climatology; Arctic dipole anomaly; The arctic; Canada Basin; Boundary current; Thermohaline circulation; Structural basin; Oceanic basin; Ocean current; Arctic ice pack; Drift ice; Paleontology","score_opus":0.027740077924359688,"score_gpt":0.2637878413514499,"score_spread":0.23604776342709022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043208768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960743,0.00068757957,0.00019825836,0.00006332296,0.000014979654,0.0000030737501,0.0017390158,0.000012889105,0.0012066823],"genre_scores_gemma":[0.99645644,0.0005237837,0.00018928705,0.000043588112,0.000019116236,0.000007341723,0.0021483763,0.0000032343335,0.0006088491],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998692,0.000012889023,0.00001801379,0.00005047999,0.00002462771,0.000024707555],"domain_scores_gemma":[0.9991598,0.00009202074,0.00036837163,0.000046247507,0.00027821772,0.0000553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043805977,0.00013267594,0.00013783194,0.0006384362,0.00027300703,0.00046924836,0.00020796178,0.00025869807,0.0009701239],"category_scores_gemma":[0.0010853186,0.00011727956,0.000174758,0.00090764614,0.000104040366,0.00031389823,0.00020224857,0.00024509896,0.00026680506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016724443,0.000029508123,0.9795725,0.00005052558,0.0001485198,0.00007905946,0.00031017244,0.0007613149,0.002564412,0.000087723594,0.0005992844,0.015629712],"study_design_scores_gemma":[0.0000016482226,0.000020513722,0.99743986,0.0000082772585,0.000018443741,0.00008623168,0.00007496227,0.00024344101,0.00049403484,0.0000118914695,0.0015979001,0.0000027759816],"about_ca_topic_score_codex":0.014884855,"about_ca_topic_score_gemma":0.024694765,"teacher_disagreement_score":0.014884855,"about_ca_system_score_codex":0.0005372897,"about_ca_system_score_gemma":0.00021663801,"threshold_uncertainty_score":0.029596448},"labels":[],"label_agreement":null},{"id":"W2043284444","doi":"10.1029/2003gl018034","title":"The role of hydrologically‐driven ice fracture in drainage system evolution on an Arctic glacier","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Glacier; Drainage; Drainage system (geomorphology); Outflow; Geomorphology; Arctic; Ice stream; Hydrology (agriculture); Cryosphere; Oceanography; Geotechnical engineering; Sea ice","score_opus":0.019964972867205884,"score_gpt":0.25872678751341865,"score_spread":0.23876181464621277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043284444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998148,0.000013592635,0.000032780077,0.000010683846,3.3054096e-7,5.5478546e-7,0.000023294242,0.0000028817583,0.00010107206],"genre_scores_gemma":[0.9998454,0.000013369757,0.000049334096,0.0000033877689,9.746711e-7,7.902044e-7,0.000039604634,0.0000012829881,0.000045904075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.000020452853,0.000003374587,0.000011130304,0.0000061673063,0.000019960056],"domain_scores_gemma":[0.99972194,0.00008042403,0.00005485431,0.000013897185,0.000049541755,0.00007925997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029818123,0.000103246944,0.00014667612,0.00057139137,0.00047619938,0.0004971853,0.00017141145,0.00027281683,0.0005460599],"category_scores_gemma":[0.000628826,0.00015804618,0.00015882283,0.0002481111,0.00046477048,0.0002066377,0.0002764358,0.00016711075,0.00006915572],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025375522,0.0000841679,0.9468778,0.000017006882,0.00004359624,0.00025982715,0.00041388292,0.007119016,0.03306623,0.00042036438,0.00018466705,0.011259612],"study_design_scores_gemma":[0.0000044424205,0.000032114047,0.9935277,0.0000020474804,0.000008559969,0.00006108111,0.00011969849,0.0053942534,0.00063328893,0.00011187961,0.000099606616,0.000005180152],"about_ca_topic_score_codex":0.02716372,"about_ca_topic_score_gemma":0.04181506,"teacher_disagreement_score":0.02716372,"about_ca_system_score_codex":0.00076651445,"about_ca_system_score_gemma":0.00039048473,"threshold_uncertainty_score":0.054011226},"labels":[],"label_agreement":null},{"id":"W2043494594","doi":"10.1029/2003gl018521","title":"Responses of the mesospheric wind at high latitudes to the April 2002 space storm","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Thermosphere; Storm; Atmospheric sciences; Atmosphere (unit); Mesosphere; Environmental science; Convection; Incoherent scatter; Radar; Meteorology; Ionosphere; Climatology; Geology; Geophysics; Physics; Stratosphere","score_opus":0.01660862461644868,"score_gpt":0.2720618513271373,"score_spread":0.2554532267106886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043494594","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99935704,0.000024789942,0.000023914536,0.000017677705,0.0000039911492,0.000002710372,0.00006713602,0.0000036249974,0.000499099],"genre_scores_gemma":[0.9995092,0.000029992736,0.00002206516,0.000014000664,0.00000567565,0.0000023962823,0.00016580084,0.0000019632487,0.0002488225],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999312,0.000011105991,0.0000037955397,0.000011414621,0.0000165386,0.000025873967],"domain_scores_gemma":[0.9998259,0.000021720898,0.000033836037,0.000013366156,0.000037430655,0.000067767556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000086578955,0.00012880958,0.00019901285,0.00018631795,0.00020964009,0.00033280218,0.00006612064,0.00022064401,0.0009700828],"category_scores_gemma":[0.0003274107,0.00011730931,0.00010241717,0.00011532112,0.00011886219,0.00007714802,0.00020168281,0.00023788556,0.00023821737],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021343196,0.00016964917,0.6602918,0.000045223314,0.00014305345,0.0013637863,0.00072150957,0.0026327444,0.31582907,0.00014138522,0.0015831561,0.014944311],"study_design_scores_gemma":[0.000012636801,0.00011456901,0.99704903,0.000001984743,0.000006321652,0.00007216068,0.00014393326,0.0005346887,0.0016672492,0.000019246323,0.0003743759,0.000003722359],"about_ca_topic_score_codex":0.0041229054,"about_ca_topic_score_gemma":0.007464263,"teacher_disagreement_score":0.0041229054,"about_ca_system_score_codex":0.00018811249,"about_ca_system_score_gemma":0.000085973756,"threshold_uncertainty_score":0.008197844},"labels":[],"label_agreement":null},{"id":"W2043535092","doi":"10.1029/2009gl039737","title":"First Satellite Observations of Meteoric Smoke in the Middle Atmosphere","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Space Agency","funders":"","keywords":"Aeronomy; Atmosphere (unit); Atmospheric sciences; Altitude (triangle); Satellite; Mesosphere; Occultation; Geology; Meteor (satellite); Environmental science; Climatology; Meteorology; Stratosphere; Geography; Astronomy; Physics","score_opus":0.0867168186426846,"score_gpt":0.29787787222624407,"score_spread":0.21116105358355947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043535092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9909978,0.0007511737,0.0010456431,0.00011646188,0.000055586162,0.000020481386,0.0011750496,0.00009016787,0.0057475716],"genre_scores_gemma":[0.9954159,0.00017079919,0.001982895,0.00006333575,0.00004838461,0.000008993453,0.0012241581,0.000012046386,0.0010734524],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999294,0.000004619487,0.0000036155457,0.0000152233515,0.000030021345,0.000017163818],"domain_scores_gemma":[0.9998104,0.00001702392,0.000023362774,0.000030279063,0.00005953174,0.000059530037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017969015,0.0001300224,0.00013147986,0.00038392135,0.00034604437,0.00038159903,0.00012581902,0.00023834096,0.0008087184],"category_scores_gemma":[0.00029910033,0.00010581118,0.0001386155,0.00023857468,0.00012061375,0.00024524413,0.0004091197,0.00029640438,0.00021612224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005782927,0.00017122967,0.79099697,0.00013133467,0.00017066217,0.0007677846,0.0020849304,0.000948153,0.09384398,0.0011005992,0.00390857,0.10529753],"study_design_scores_gemma":[0.000035525976,0.0002225086,0.9561111,0.000031587337,0.0000652396,0.00025026908,0.00039853266,0.0012255453,0.010452291,0.00024771903,0.030946577,0.000013074188],"about_ca_topic_score_codex":0.005379677,"about_ca_topic_score_gemma":0.016026808,"teacher_disagreement_score":0.005379677,"about_ca_system_score_codex":0.0002623636,"about_ca_system_score_gemma":0.00021310587,"threshold_uncertainty_score":0.010696709},"labels":[],"label_agreement":null},{"id":"W2043825060","doi":"10.1029/2009gl039706","title":"NO<sub>x</sub> descent in the Arctic middle atmosphere in early 2009","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":181,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Waterloo","funders":"","keywords":"Stratosphere; Thermosphere; Atmosphere (unit); Descent (aeronautics); Mesosphere; Atmospheric sciences; Polar night; Precipitation; Arctic; Climatology; Environmental science; The arctic; Atmosphere of Earth; Stratopause; Meteorology; Physics; Ionosphere; Geology; Geophysics; Oceanography","score_opus":0.029535924001588984,"score_gpt":0.2578242940467165,"score_spread":0.22828837004512748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2043825060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990532,0.00007665587,0.000040690087,0.000038742866,0.000008742425,0.0000017026973,0.00022477342,0.0000030390531,0.0005525185],"genre_scores_gemma":[0.99920315,0.000061694045,0.00008360421,0.000023896217,0.00000650915,0.0000018684791,0.00031304272,0.000001595484,0.0003045283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999428,0.000008255114,0.0000036671834,0.000012738111,0.000012589851,0.000019927818],"domain_scores_gemma":[0.99985945,0.000012376409,0.000032129716,0.0000075609673,0.000045367146,0.000043054948],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022413432,0.00012445477,0.0001281143,0.00031110126,0.00049440784,0.00046717018,0.0000881229,0.00019092819,0.00026619196],"category_scores_gemma":[0.00026054488,0.000071676164,0.000111317255,0.00025418182,0.00012620652,0.00021049294,0.00038733968,0.00020166532,0.000077318735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055327546,0.00005423222,0.98009616,0.00001663885,0.00005317308,0.0005587876,0.00071790064,0.00028005432,0.009934888,0.00013972002,0.00049660343,0.0070986007],"study_design_scores_gemma":[0.0000016017468,0.000020900372,0.9982734,0.0000025626223,0.000005744002,0.000034155462,0.00022171813,0.00015807354,0.0006199746,0.000016940234,0.0006428559,0.0000021755457],"about_ca_topic_score_codex":0.07361144,"about_ca_topic_score_gemma":0.14160733,"teacher_disagreement_score":0.07361144,"about_ca_system_score_codex":0.00053838495,"about_ca_system_score_gemma":0.00034231774,"threshold_uncertainty_score":0.14636594},"labels":[],"label_agreement":null},{"id":"W2044079658","doi":"10.1029/2004gl020299","title":"Observation of coherent echoes with narrow spectra near 150 km altitude during daytime away from the dip equator","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Western University","funders":"","keywords":"Daytime; Equator; Geology; Earth's magnetic field; Magnetic dip; Altitude (triangle); Doppler effect; Latitude; Morning; Geophysics; Ionosphere; Geodesy; Atmospheric sciences; Physics; Astronomy; Magnetic field","score_opus":0.017867716865089395,"score_gpt":0.26171308979369606,"score_spread":0.24384537292860667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044079658","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99886286,0.000062288775,0.00027481,0.000012055773,0.000004935812,0.0000012745236,0.00007989438,0.000017924955,0.00068397046],"genre_scores_gemma":[0.99929035,0.0000333841,0.0002772877,0.000011953181,0.0000053222407,0.0000010489422,0.00014075405,0.000003609312,0.00023623902],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999801,0.0000012015619,0.0000011689488,0.0000046108826,0.0000055546307,0.000007354662],"domain_scores_gemma":[0.99989915,0.00001610448,0.000023577402,0.000010192279,0.000019561236,0.000031447376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000038705188,0.00008274202,0.00011453099,0.00022990751,0.00015897631,0.00013459996,0.00010151922,0.00015114466,0.0006828604],"category_scores_gemma":[0.00017880193,0.000055866385,0.00005483042,0.00017133154,0.0000918893,0.00009973592,0.00015094965,0.00013267847,0.0001888765],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028131105,0.000060823306,0.22618109,0.0001155456,0.00006120857,0.0023271118,0.0013843836,0.00028047818,0.74739224,0.00015327786,0.0007100566,0.021052524],"study_design_scores_gemma":[0.0000072229777,0.00012366669,0.98214483,0.000008894503,0.000028415543,0.0011555178,0.000447258,0.0004164548,0.014401115,0.000039661005,0.0012175271,0.000009490695],"about_ca_topic_score_codex":0.0014070328,"about_ca_topic_score_gemma":0.0040039388,"teacher_disagreement_score":0.0014070328,"about_ca_system_score_codex":0.000056409317,"about_ca_system_score_gemma":0.000059752667,"threshold_uncertainty_score":0.0027976632},"labels":[],"label_agreement":null},{"id":"W2044085330","doi":"10.1002/2015gl063186","title":"The tilt of mean sea level along the east coast of North America","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Bedford Institute of Oceanography","funders":"Natural Environment Research Council; Sight Research UK; Technische Universität München; European Space Agency","keywords":"Tide gauge; Geoid; Geodetic datum; Geology; Sea level; Geodesy; Oceanography; Climatology; Ocean current; Tilt (camera); Geophysics","score_opus":0.12575244014221018,"score_gpt":0.2964215894997075,"score_spread":0.1706691493574973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044085330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957082,0.00023044072,0.00012391739,0.00013598999,0.000016385597,0.000001164126,0.0004026513,0.000008296321,0.003372966],"genre_scores_gemma":[0.99946433,0.00009175273,0.00008746019,0.000016852675,0.0000045537886,6.328109e-7,0.00016573032,0.0000012775722,0.00016736118],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999212,0.000014007611,0.000005328781,0.000018871207,0.00002913004,0.000011476276],"domain_scores_gemma":[0.9995739,0.00005440852,0.000089663175,0.000021595992,0.00022503668,0.00003546391],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020526059,0.00007927438,0.00008631803,0.00039237566,0.00014278963,0.00045460725,0.0000705716,0.00009557528,0.0008826232],"category_scores_gemma":[0.00081678247,0.00006525298,0.00007445342,0.00055712153,0.00023532107,0.00025257486,0.00022760323,0.0001523841,0.0001280569],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066082415,0.0000046577443,0.9844648,0.000017312026,0.000039919993,0.000047613725,0.00022527314,0.00069879,0.002111097,0.00026825018,0.0008906697,0.011165499],"study_design_scores_gemma":[7.794145e-7,0.0000055951436,0.9987717,0.000004594046,0.0000041888948,0.000015269623,0.00019464608,0.0003064705,0.000113365764,0.00006941916,0.00051155704,0.0000023139166],"about_ca_topic_score_codex":0.051080346,"about_ca_topic_score_gemma":0.10361903,"teacher_disagreement_score":0.94891965,"about_ca_system_score_codex":0.0005102314,"about_ca_system_score_gemma":0.00026812754,"threshold_uncertainty_score":0.10156608},"labels":[],"label_agreement":null},{"id":"W2044123278","doi":"10.1029/2009gl040027","title":"Deep low‐frequency earthquakes in tremor localize to the plate interface in multiple subduction zones","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":195,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Subduction; Episodic tremor and slip; Seismology; Geology; Plate tectonics; Induced seismicity; Slip (aerodynamics); Low frequency; Shear (geology); Pacific Plate; Tectonics; Petrology","score_opus":0.037225261122115716,"score_gpt":0.2884871284448063,"score_spread":0.25126186732269057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044123278","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99962735,0.000017641001,0.00012361289,0.000004257559,2.1410301e-7,0.0000014539759,0.000022241164,0.0000033897961,0.0001998973],"genre_scores_gemma":[0.99972016,0.000017413315,0.00012582338,0.0000019189085,0.0000011444183,0.000001507456,0.000054491058,0.0000011236968,0.000076383665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998994,0.000011501302,0.000010995592,0.000035395573,0.0000177317,0.00002503811],"domain_scores_gemma":[0.99916375,0.00010579581,0.0004214038,0.000048376787,0.00013224855,0.00012842954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017782126,0.00013185904,0.00020193122,0.0013804514,0.00024481962,0.00039308795,0.00015546844,0.0001347997,0.00051949697],"category_scores_gemma":[0.000883603,0.00014257997,0.00009435657,0.0009285879,0.00030947957,0.00026778877,0.00050509826,0.00010996609,0.00012895079],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008412298,0.00002576409,0.9739769,0.000015820928,0.000025287873,0.0001389714,0.00058350584,0.00044303175,0.016663438,0.000077239034,0.000054017062,0.007911876],"study_design_scores_gemma":[0.0000023436933,0.000011532477,0.9989819,0.0000018172371,0.0000055107243,0.000057368004,0.00015829847,0.00045110608,0.00027440302,0.000021719768,0.00003235384,0.0000016938449],"about_ca_topic_score_codex":0.011988291,"about_ca_topic_score_gemma":0.026380014,"teacher_disagreement_score":0.011988291,"about_ca_system_score_codex":0.00028786776,"about_ca_system_score_gemma":0.0001940732,"threshold_uncertainty_score":0.02383703},"labels":[],"label_agreement":null},{"id":"W2044196627","doi":"10.1029/2005gl023289","title":"Estimating the energy flux from the wind to ocean inertial motions: The sensitivity to surface wind fields","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Energy flux; Flux (metallurgy); Geology; Sensitivity (control systems); Geophysics; Inertial frame of reference; Wind stress; Wind power; Solar wind; Atmospheric sciences; Meteorology; Environmental science; Climatology; Physics; Plasma; Astronomy; Classical mechanics","score_opus":0.02181854682131738,"score_gpt":0.2638241692600408,"score_spread":0.24200562243872345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044196627","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.966867,0.0004927441,0.028886316,0.000119670265,0.000031887837,0.000022810344,0.0013780289,0.00011447671,0.0020870348],"genre_scores_gemma":[0.9889921,0.00029173202,0.008901781,0.000037416095,0.000020326217,0.000013879053,0.0013833788,0.00004441322,0.00031513232],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994837,0.0001758181,0.000040316787,0.00011795002,0.00013927218,0.00004299266],"domain_scores_gemma":[0.996761,0.0022673518,0.00030398314,0.0003171998,0.0003150286,0.000035488847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014155303,0.00045174407,0.00037569227,0.00076372665,0.00020244672,0.0010519205,0.00025673336,0.0005212824,0.00047796662],"category_scores_gemma":[0.010730212,0.0002865922,0.00033632666,0.00079079496,0.00022922701,0.0014482898,0.00048957096,0.00031912143,0.00019025199],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000285381,0.000053001088,0.82365894,0.00010937314,0.0004415142,0.00014625852,0.00013978557,0.103336915,0.011046591,0.0008259454,0.0007840261,0.059172258],"study_design_scores_gemma":[0.000015753116,0.00004831006,0.8074536,0.00003742366,0.00010864561,0.0001518294,0.00010648327,0.17559801,0.013310359,0.0016781647,0.0014290959,0.00006237981],"about_ca_topic_score_codex":0.015677344,"about_ca_topic_score_gemma":0.010586035,"teacher_disagreement_score":0.015677344,"about_ca_system_score_codex":0.0002783848,"about_ca_system_score_gemma":0.00023957787,"threshold_uncertainty_score":0.031172156},"labels":[],"label_agreement":null},{"id":"W2044202010","doi":"10.1029/2004gl021532","title":"Can near‐inertial internal waves in the East Sea be observed by synthetic aperture radar?","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Synthetic aperture radar; Internal wave; Geology; Peninsula; Radar; Wavelength; Geodesy; Inertial frame of reference; Inertial wave; Remote sensing; Geophysics; Wave propagation; Physics; Optics; Mechanical wave; Oceanography; Longitudinal wave; Geography","score_opus":0.029454431220065774,"score_gpt":0.2521328369319346,"score_spread":0.22267840571186884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044202010","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949385,0.00066974614,0.0022913553,0.00028351968,0.000021707205,0.000004286747,0.00009741445,0.000025716949,0.0016677923],"genre_scores_gemma":[0.9977198,0.0006344393,0.0010494443,0.0000752732,0.00003203602,0.0000026640766,0.00019932947,0.00000430771,0.000282768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992764,0.000018923702,0.0000036242802,0.000017496424,0.000016009752,0.000016367076],"domain_scores_gemma":[0.999574,0.00011389621,0.00015931808,0.000053726057,0.000063040054,0.000036057758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041159004,0.00016871677,0.00016283497,0.00032606875,0.00008279768,0.00038006672,0.0001376637,0.0003468536,0.00033236845],"category_scores_gemma":[0.0014304646,0.00016509865,0.00015085755,0.0003684911,0.00031419643,0.0008100198,0.00017250393,0.00018828061,0.0001896646],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045546825,0.000119068274,0.76994616,0.00018215281,0.00011917517,0.00052403036,0.00055275497,0.0039630705,0.101494275,0.0016314149,0.0011921171,0.11982035],"study_design_scores_gemma":[0.000032936852,0.00013323546,0.97078806,0.00003024442,0.00005845994,0.0005321719,0.0005022917,0.015762515,0.008538869,0.0014536697,0.0021351979,0.000032448857],"about_ca_topic_score_codex":0.0010393012,"about_ca_topic_score_gemma":0.0017848451,"teacher_disagreement_score":0.0010393012,"about_ca_system_score_codex":0.000101690326,"about_ca_system_score_gemma":0.00006988443,"threshold_uncertainty_score":0.002176702},"labels":[],"label_agreement":null},{"id":"W2044374307","doi":"10.1029/1999gl007002","title":"Spatial and temporal dynamics of colored dissolved organic matter in the north water polynya","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Colored dissolved organic matter; Environmental science; Arctic; Oceanography; Sea ice; Dissolved organic carbon; Water column; Ecosystem; Arctic ice pack; Climatology; Surface water; Geology; Phytoplankton; Ecology; Nutrient","score_opus":0.011553293284080737,"score_gpt":0.22532334751391783,"score_spread":0.21377005422983708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044374307","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993918,0.00008239498,0.000023333047,0.000025393228,0.000001522561,0.000002414779,0.00016603516,0.0000016106957,0.00030534228],"genre_scores_gemma":[0.99898773,0.00014646165,0.00008407506,0.000016957305,0.000004472163,0.000009682847,0.00034140097,0.0000016371217,0.0004074837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999107,0.000010934396,0.000005654046,0.000027775171,0.00001922842,0.000025734276],"domain_scores_gemma":[0.9994635,0.00007528763,0.00017237979,0.00002196849,0.00013016353,0.000136776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019023819,0.00014720715,0.00016467588,0.0008734155,0.0005164987,0.0004759972,0.00016487307,0.00023148548,0.0006066759],"category_scores_gemma":[0.0006845213,0.00018459737,0.000098575765,0.0007412971,0.00039683425,0.0003094135,0.0005229017,0.00019977237,0.000113951886],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014097216,0.000021241822,0.9902291,0.0000191167,0.000035625537,0.00015903344,0.0011631413,0.00007813583,0.0037558319,0.00003269417,0.00012127344,0.0042439546],"study_design_scores_gemma":[9.0412897e-7,0.000009344073,0.9994931,0.0000018633937,0.0000033610634,0.000020920661,0.00020011995,0.00003586362,0.000067646615,0.0000045679,0.00016108454,0.0000011216903],"about_ca_topic_score_codex":0.119530655,"about_ca_topic_score_gemma":0.2474925,"teacher_disagreement_score":0.119530655,"about_ca_system_score_codex":0.00092922687,"about_ca_system_score_gemma":0.00046592514,"threshold_uncertainty_score":0.23766983},"labels":[],"label_agreement":null},{"id":"W2044382601","doi":"10.1029/2006gl028797","title":"Response of the global carbon cycle to human‐induced changes in Southern Hemisphere winds","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Extratropical cyclone; Southern Hemisphere; Climatology; Northern Hemisphere; Atmospheric sciences; Forcing (mathematics); Environmental science; Carbon cycle; Carbon sink; Greenhouse gas; Geology; Climate change; Oceanography; Ecosystem","score_opus":0.017124197881713824,"score_gpt":0.28810754419437834,"score_spread":0.2709833463126645,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044382601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99814916,0.000038588278,0.00039508703,0.00016368025,0.00001159331,0.0000040949203,0.00033182304,0.000031958512,0.00087404595],"genre_scores_gemma":[0.9995136,0.00004515156,0.00008487519,0.000017596403,0.000002813309,0.0000036654174,0.0001568467,0.000005037931,0.00017029331],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998958,0.000048442165,0.0000041045237,0.000017013848,0.000007912499,0.000026821892],"domain_scores_gemma":[0.999688,0.00013993979,0.00005251216,0.000028464567,0.000041294108,0.00004967387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035487604,0.0003721029,0.0003005814,0.00022138451,0.00027537966,0.000618086,0.00024771516,0.0009036431,0.0014899217],"category_scores_gemma":[0.0016648902,0.00019414595,0.00043173484,0.00040589346,0.0004246372,0.00036074754,0.00037217277,0.00037264993,0.000111867725],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035520177,0.000077951605,0.08877331,0.000033590517,0.0001808189,0.00020932496,0.00006622137,0.9002922,0.004240286,0.0015558025,0.001192306,0.003022959],"study_design_scores_gemma":[0.00013528041,0.00023794656,0.108106,0.000009911424,0.00008790826,0.00007129477,0.00018884274,0.88683134,0.001269015,0.002180101,0.0008426877,0.00003963757],"about_ca_topic_score_codex":0.033508584,"about_ca_topic_score_gemma":0.019133212,"teacher_disagreement_score":0.033508584,"about_ca_system_score_codex":0.0006482073,"about_ca_system_score_gemma":0.00043799548,"threshold_uncertainty_score":0.066627085},"labels":[],"label_agreement":null},{"id":"W2044481113","doi":"10.1029/2004gl019646","title":"On the advective‐diffusive transport in porous media in the presence of time‐dependent velocities","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Advanced Mathematical Modeling in Engineering","field":"Computer Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Advection; Porous medium; Mechanics; Discontinuity (linguistics); Diffusion; Front (military); Flow (mathematics); Boundary value problem; Darcy's law; Stability (learning theory); Physics; Mathematical analysis; Geology; Porosity; Mathematics; Meteorology; Computer science; Geotechnical engineering; Thermodynamics","score_opus":0.026166714730950957,"score_gpt":0.2851756562751048,"score_spread":0.2590089415441539,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044481113","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.05523081,0.0032037776,0.91666305,0.0013630852,0.00024847925,0.00008070549,0.0000719348,0.000113920716,0.023024239],"genre_scores_gemma":[0.7343053,0.01045361,0.22041486,0.0007424775,0.00085223065,0.00023160815,0.00023197422,0.00022016627,0.0325476],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99966514,0.000115004994,0.000019282455,0.000041904575,0.000121835634,0.00003691075],"domain_scores_gemma":[0.99825615,0.0012231075,0.00012228776,0.00008145989,0.00024665636,0.00007030738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014126457,0.0009796326,0.00060988683,0.0009761021,0.0007096636,0.0013426463,0.0007039879,0.0014612769,0.0009941364],"category_scores_gemma":[0.005186528,0.00037881103,0.0007304045,0.00053979515,0.003043286,0.002707049,0.0014193802,0.0013795306,0.00027512328],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037784255,0.00005108759,0.00034573677,0.00022447649,0.000018980192,0.00029434927,0.00025994272,0.26995325,0.006299365,0.70643365,0.0012493903,0.01483196],"study_design_scores_gemma":[0.00001535433,0.00002991768,0.00015087613,0.000032571148,0.000008999664,0.0001665377,0.000036995763,0.8381882,0.0014564065,0.15725885,0.002634949,0.000020434567],"about_ca_topic_score_codex":0.002688172,"about_ca_topic_score_gemma":0.0014447889,"teacher_disagreement_score":0.002688172,"about_ca_system_score_codex":0.00076729496,"about_ca_system_score_gemma":0.0010720515,"threshold_uncertainty_score":0.007470846},"labels":[],"label_agreement":null},{"id":"W2044944036","doi":"10.1029/2006gl028495","title":"Cooling of Northwest Atlantic slope waters during the Holocene","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Holocene; Geology; Oceanography; Insolation; Holocene climatic optimum; Climatology; Glacial period; Temperature record; Post-glacial rebound; Paleoclimatology; Climate change; Physical geography; Ice sheet; Geomorphology; Geography","score_opus":0.026148237876993285,"score_gpt":0.2828509920348061,"score_spread":0.25670275415781285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2044944036","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99692744,0.0002452491,0.000038817183,0.00010807104,0.000014104284,0.0000032099454,0.00041066637,0.000007365192,0.0022450918],"genre_scores_gemma":[0.99807006,0.0003410449,0.00008674135,0.000104828505,0.000015112984,0.000005233888,0.0006691586,0.000005911589,0.0007020347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.00001210237,0.0000075224634,0.000029624849,0.000025308394,0.000029265611],"domain_scores_gemma":[0.9997081,0.000018132427,0.00010034905,0.000020431367,0.000103276296,0.000049637452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015745818,0.00012696335,0.00016492621,0.00024775838,0.0006145709,0.00069727516,0.00016065608,0.00021472349,0.0015105689],"category_scores_gemma":[0.00060325646,0.00009759238,0.00011739973,0.0003172649,0.00034628413,0.00026521157,0.0002656109,0.000249559,0.00029577996],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015539528,0.000020841546,0.9678445,0.000025045203,0.000037829537,0.00015622412,0.0005054047,0.0002654453,0.020315483,0.00017030786,0.0008620118,0.009641723],"study_design_scores_gemma":[0.0000024748786,0.000011837663,0.99792767,0.0000041187186,0.0000043419604,0.00003853772,0.00015267263,0.000056985864,0.00040046318,0.00001635855,0.0013827573,0.0000018135752],"about_ca_topic_score_codex":0.13174887,"about_ca_topic_score_gemma":0.26534736,"teacher_disagreement_score":0.13174887,"about_ca_system_score_codex":0.0013464079,"about_ca_system_score_gemma":0.001287533,"threshold_uncertainty_score":0.26196396},"labels":[],"label_agreement":null},{"id":"W2045258053","doi":"10.1029/2007gl032583","title":"CO<sub>2</sub> sensitivity of Southern Ocean phytoplankton","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":297,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Office of Polar Programs; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Phytoplankton; Biogeochemical cycle; Oceanography; Environmental science; Carbon cycle; Water column; Productivity; Seawater; Diatom; Biological pump; Cycling; Environmental chemistry; Chemistry; Ecology; Nutrient; Ecosystem; Biology; Geology","score_opus":0.025977608687053445,"score_gpt":0.2448322507776421,"score_spread":0.21885464209058864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045258053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998139,0.0003423717,0.00018676253,0.000049982602,0.0000044622393,0.0000029903085,0.00017497544,0.000012805244,0.0010865608],"genre_scores_gemma":[0.9993851,0.00013588925,0.000095251446,0.000033142333,0.0000034977395,0.000003404673,0.000107692205,0.000004317781,0.00023176397],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999435,0.000011357698,0.000003529831,0.00001613385,0.000013566564,0.000011856441],"domain_scores_gemma":[0.99987435,0.000026683392,0.000038264097,0.000017925355,0.000024603985,0.00001818435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008179022,0.00020528739,0.00013183855,0.0001888142,0.00015249151,0.00034402785,0.000081568236,0.00016185202,0.0006465917],"category_scores_gemma":[0.00022645853,0.00015087322,0.00009460342,0.00019683168,0.00022590539,0.00012624047,0.00019067676,0.00014473978,0.00013978995],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026872475,0.000014621232,0.040088598,0.000048644062,0.000026796966,0.00011218022,0.000050559393,0.001173399,0.953899,0.00011659582,0.00012051099,0.004080364],"study_design_scores_gemma":[0.000010569397,0.00011198948,0.84034795,0.0000048327734,0.000026549296,0.00032411877,0.0001159305,0.0040761563,0.15322421,0.00035508748,0.0013903325,0.000012271443],"about_ca_topic_score_codex":0.004611859,"about_ca_topic_score_gemma":0.005413484,"teacher_disagreement_score":0.004611859,"about_ca_system_score_codex":0.00040668802,"about_ca_system_score_gemma":0.00013580616,"threshold_uncertainty_score":0.009169996},"labels":[],"label_agreement":null},{"id":"W2045343181","doi":"10.1029/2004gl019725","title":"Global glaciation in the Neoproterozoic: Reconciling previous modelling results","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Glacial period; Geology; Paleontology","score_opus":0.0435033298318747,"score_gpt":0.30151342710424456,"score_spread":0.25801009727236984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045343181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9731661,0.0032070298,0.008568002,0.0068463203,0.00013689407,0.000008637174,0.00061579933,0.00033592206,0.007115246],"genre_scores_gemma":[0.99724907,0.0008978973,0.0011628688,0.00021328618,0.000041403007,0.0000048761103,0.00021287244,0.000059655424,0.00015806669],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994485,0.00022705756,0.000059367,0.00011530489,0.00008988093,0.000059981623],"domain_scores_gemma":[0.99903274,0.00039634915,0.00012820994,0.00021386358,0.00016709918,0.00006173366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019934494,0.0007949986,0.00058113405,0.0011985827,0.00050853175,0.0015873006,0.0014349985,0.001062775,0.0012153722],"category_scores_gemma":[0.0051863464,0.00030216627,0.0005678567,0.001429616,0.00068861106,0.0016343902,0.0015206264,0.00078494794,0.00022055903],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010246856,0.00014007279,0.28356907,0.0006241517,0.0016535212,0.0009982215,0.002508588,0.59955186,0.009426289,0.04385413,0.004256737,0.05239261],"study_design_scores_gemma":[0.00029946282,0.00014657364,0.17892379,0.0003090684,0.0009175735,0.0003464638,0.0021409963,0.72084296,0.0063349563,0.075183176,0.014342564,0.00021233657],"about_ca_topic_score_codex":0.012332185,"about_ca_topic_score_gemma":0.009741792,"teacher_disagreement_score":0.012332185,"about_ca_system_score_codex":0.0017466182,"about_ca_system_score_gemma":0.00060827646,"threshold_uncertainty_score":0.024520755},"labels":[],"label_agreement":null},{"id":"W2045398695","doi":"10.1029/2006gl025677","title":"Recent changes in the fire regime across the North American boreal region—Spatial and temporal patterns of burning across Canada and Alaska","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":799,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Boreal; Fire regime; Environmental science; Climatology; Taiga; Climate change; Physical geography; Period (music); Ecosystem; Atmospheric sciences; Geography; Geology; Oceanography; Ecology; Forestry; Archaeology","score_opus":0.01363676577246977,"score_gpt":0.2676724779239913,"score_spread":0.25403571215152154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045398695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99868494,0.00023346994,0.000046033852,0.000029340425,0.0000035380285,0.0000024002663,0.00039210616,0.0000034517716,0.0006047266],"genre_scores_gemma":[0.998906,0.00022412198,0.000120581164,0.000012148395,0.0000040329523,0.0000030440203,0.0005154291,0.0000013164484,0.00021329163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998242,0.000020024341,0.000017921651,0.000055380013,0.00003853963,0.000043988668],"domain_scores_gemma":[0.9991726,0.00006788753,0.0002790623,0.000044212687,0.0003005568,0.0001356897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050595985,0.00011508734,0.00015256148,0.0013607091,0.0007389023,0.0006826925,0.00028297055,0.00017096518,0.00036681644],"category_scores_gemma":[0.00084991514,0.00015729282,0.00016882394,0.0013317626,0.0003833294,0.00039545906,0.00037741495,0.00020613238,0.00005772812],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000030536157,0.000011879474,0.99489933,0.00001036327,0.000039019895,0.000048850798,0.00042919576,0.00018128891,0.00047205025,0.00003531779,0.00011239256,0.0037296873],"study_design_scores_gemma":[3.2382022e-7,0.0000027357753,0.9994716,0.0000026964785,0.000004213268,0.000023446088,0.00018973472,0.000051717907,0.00002398267,0.000005063594,0.00022292045,0.000001717486],"about_ca_topic_score_codex":0.6819716,"about_ca_topic_score_gemma":0.8747742,"teacher_disagreement_score":0.3180284,"about_ca_system_score_codex":0.0020047256,"about_ca_system_score_gemma":0.00090674247,"threshold_uncertainty_score":0.63980263},"labels":[],"label_agreement":null},{"id":"W2045411558","doi":"10.1029/2009gl041252","title":"Azimuthal structures of ray auroras at the beginning of auroral substorms","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Ministry of Education, Culture, Sports, Science and Technology","keywords":"Substorm; Physics; Luminosity; Astrophysics; Electron precipitation; Electric field; Geophysics; Azimuth; Electron; Wavenumber; Magnetic field; Astronomy; Magnetosphere; Optics; Galaxy","score_opus":0.01758252736773471,"score_gpt":0.29635086571242314,"score_spread":0.27876833834468845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045411558","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971551,0.00014770537,0.00029464022,0.000022849352,0.000005618068,0.0000064668984,0.00020751834,0.000028506041,0.0021317082],"genre_scores_gemma":[0.9990771,0.0000610537,0.0002530893,0.000006448738,0.00000906728,0.000003567314,0.0002771418,0.000006322802,0.00030624217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994445,0.0000039136185,0.000003336582,0.000011803472,0.000016019581,0.00002050699],"domain_scores_gemma":[0.99958223,0.000054403892,0.00013328275,0.000019697452,0.000110007306,0.000100391444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001263815,0.00010648562,0.00017301741,0.0011647713,0.00031197333,0.00051275105,0.00009541163,0.0001850455,0.0010031655],"category_scores_gemma":[0.0005387728,0.00013477566,0.00014760887,0.00047348026,0.00021057425,0.00025891128,0.00034508127,0.00030687818,0.00014755623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073378306,0.000072940216,0.70652896,0.00010451024,0.00010308542,0.0012809987,0.001622158,0.0012856739,0.24957496,0.00090819685,0.0010655435,0.03671913],"study_design_scores_gemma":[0.0000023422228,0.000016101096,0.9981133,0.0000029536332,0.0000062076665,0.00006440376,0.000087810586,0.00024648375,0.001093511,0.000023828621,0.00033897787,0.0000041788217],"about_ca_topic_score_codex":0.0035625496,"about_ca_topic_score_gemma":0.006192679,"teacher_disagreement_score":0.0035625496,"about_ca_system_score_codex":0.00027833678,"about_ca_system_score_gemma":0.00010805348,"threshold_uncertainty_score":0.007083595},"labels":[],"label_agreement":null},{"id":"W2045506912","doi":"10.1029/2007gl030674","title":"Warming of the subpolar Atlantic triggered by freshwater discharge at the continental boundary","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Environment and Climate Change Canada","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"North Atlantic Deep Water; Shutdown of thermohaline circulation; Oceanography; Thermohaline circulation; Climatology; Gulf Stream; Geology; Atlantic multidecadal oscillation; Atlantic Equatorial mode; Ocean current; North Atlantic oscillation","score_opus":0.014063586962051419,"score_gpt":0.25050597698836313,"score_spread":0.2364423900263117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045506912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99945384,0.000030223297,0.0001327062,0.000016591526,0.000004908657,0.0000017191925,0.000055283574,0.000014618893,0.00029017177],"genre_scores_gemma":[0.99974066,0.000028727272,0.00008653469,0.000015401814,0.0000022684878,0.0000022939,0.000050274324,0.0000029200971,0.000070861395],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999967,0.000007045901,0.0000020273974,0.000011243223,0.0000053799818,0.000007337402],"domain_scores_gemma":[0.99992,0.000011995908,0.000028596918,0.000013757115,0.0000060784364,0.000019489802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005458511,0.00013757485,0.00018200441,0.000094180374,0.00016556846,0.0002579464,0.000096220974,0.0001448686,0.0007873241],"category_scores_gemma":[0.0001485957,0.00007778079,0.00016000436,0.00007167903,0.00019667315,0.00013543255,0.00030225702,0.00023888722,0.00007830426],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007304313,0.00009675249,0.06658593,0.000051002487,0.00008247843,0.00021544355,0.00014646437,0.005036553,0.9220434,0.00037371338,0.00023078785,0.004407107],"study_design_scores_gemma":[0.00007514548,0.000465864,0.8709934,0.000006605141,0.000092636044,0.00018625062,0.00017764413,0.018650897,0.10734333,0.00081533764,0.001165631,0.00002728762],"about_ca_topic_score_codex":0.0023954976,"about_ca_topic_score_gemma":0.0030714732,"teacher_disagreement_score":0.0023954976,"about_ca_system_score_codex":0.00028138465,"about_ca_system_score_gemma":0.00012470128,"threshold_uncertainty_score":0.0047631264},"labels":[],"label_agreement":null},{"id":"W2045507465","doi":"10.1029/2003gl018457","title":"IMF By effects in the magnetospheric convection on closed magnetic field lines","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Magnetosphere; Geophysics; Field line; Ionosphere; Physics; Convection; Dynamo; Polar; Interplanetary magnetic field; Solar wind; Magnetic field; Geology; Mechanics; Astronomy","score_opus":0.009127936615169271,"score_gpt":0.26893846967808854,"score_spread":0.2598105330629193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045507465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960705,0.00021104151,0.0013076433,0.00002995318,0.000006784772,0.000005145599,0.00006141095,0.00006539513,0.0022420466],"genre_scores_gemma":[0.99940467,0.000046283334,0.00020207248,0.0000072077924,0.0000052374985,0.0000018965163,0.000040293307,0.000015403144,0.00027703764],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999143,0.000021154365,0.000005444966,0.000014650266,0.000013830097,0.000030552827],"domain_scores_gemma":[0.9994405,0.00019924296,0.00013798603,0.00008170398,0.000055519853,0.00008510174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018608448,0.0002898169,0.00025842988,0.00023843777,0.00019349321,0.0003183174,0.00015411526,0.0001594559,0.0027619242],"category_scores_gemma":[0.0013402093,0.00013574077,0.00019591347,0.00011760051,0.0003438883,0.00048884866,0.00056939916,0.00024567498,0.00025562788],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0038778991,0.00033706875,0.07672487,0.00024879715,0.00010472648,0.0013267986,0.000741628,0.013728588,0.84196514,0.006834361,0.00086582726,0.053244364],"study_design_scores_gemma":[0.0003196359,0.00096093595,0.7341244,0.000065300155,0.0001848112,0.0021664724,0.00029381135,0.041946698,0.20590095,0.008780701,0.0052186544,0.000037666752],"about_ca_topic_score_codex":0.0005090512,"about_ca_topic_score_gemma":0.00025299037,"teacher_disagreement_score":0.0027619242,"about_ca_system_score_codex":0.0002691084,"about_ca_system_score_gemma":0.00007477674,"threshold_uncertainty_score":0.009239554},"labels":[],"label_agreement":null},{"id":"W2045515896","doi":"10.1029/2005gl024483","title":"Trends in the draft and extent of seasonal pack ice, Canadian Beaufort Sea","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Guelph; Fisheries and Oceans Canada","funders":"","keywords":"Arctic ice pack; Sea ice; Oceanography; Beaufort scale; Climatology; Beaufort sea; Cryosphere; Antarctic sea ice; Geology; Climate change; Environmental science; Physical geography; Geography","score_opus":0.02011922074593774,"score_gpt":0.2714652006661821,"score_spread":0.2513459799202444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045515896","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98554707,0.0010828725,0.00032357086,0.00041663458,0.000016085267,0.000010439826,0.008707949,0.000059375205,0.003836099],"genre_scores_gemma":[0.9879643,0.0006947908,0.0008731996,0.00007865822,0.000010678195,0.000010828432,0.006960237,0.000015432544,0.0033918754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997553,0.000008062803,0.00001381606,0.00005855505,0.00011692435,0.000047340433],"domain_scores_gemma":[0.9973763,0.00009143992,0.00031750763,0.00006122931,0.0019462503,0.00020736613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036229275,0.00018853859,0.00013584734,0.0016446038,0.00089510373,0.00079694105,0.0005020296,0.00023099955,0.0015015083],"category_scores_gemma":[0.0016271654,0.00012523333,0.00015563917,0.0022565683,0.00053878024,0.0005307551,0.0002910122,0.00028005714,0.00019251271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014705583,0.00001922347,0.95727134,0.00006227264,0.00008582183,0.00006418613,0.0011264319,0.0009580466,0.002597967,0.00038167636,0.004969821,0.032316078],"study_design_scores_gemma":[0.0000010853731,0.000005933409,0.9969496,0.000004147519,0.000004852813,0.000016703556,0.00012365903,0.00021274583,0.00010553872,0.000009515675,0.0025611985,0.0000049193723],"about_ca_topic_score_codex":0.9797564,"about_ca_topic_score_gemma":0.99145186,"teacher_disagreement_score":0.020243585,"about_ca_system_score_codex":0.009775905,"about_ca_system_score_gemma":0.0050984514,"threshold_uncertainty_score":0.07092953},"labels":[],"label_agreement":null},{"id":"W2045522461","doi":"10.1029/2000gl012455","title":"Near surface atmospheric characteristics over the North Bay of Bengal during the Indian Summer Monsoon","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Bay; Radiosonde; Potential temperature; Mixed layer; Convective available potential energy; Convection; Monsoon; Climatology; Atmospheric convection; Convective inhibition; Environmental science; BENGAL; Atmospheric sciences; Sensible heat; Wind speed; Geology; Oceanography; Meteorology; Troposphere; Geography","score_opus":0.017710350840345643,"score_gpt":0.2463237328738064,"score_spread":0.22861338203346077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045522461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969656,0.00010973535,0.000048553287,0.000050662897,0.0000063213038,0.0000054200473,0.0010226108,0.000024022742,0.0017671701],"genre_scores_gemma":[0.99880695,0.00006995026,0.000035561286,0.0000129046975,0.0000118746875,0.0000046573446,0.00060846226,0.0000040069563,0.00044550112],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998671,0.000011850064,0.000009216561,0.000027117567,0.000035412526,0.000049307364],"domain_scores_gemma":[0.9997008,0.000038576123,0.00008624609,0.000022238408,0.00007940325,0.0000728352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009777803,0.00024702246,0.00023058233,0.00056736515,0.00075037475,0.00061828806,0.000272607,0.0001648998,0.0015488969],"category_scores_gemma":[0.00040656087,0.000119306635,0.00012529174,0.0011291368,0.0002084118,0.00032147946,0.0003689961,0.0001823002,0.0005137055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004463218,0.00010391004,0.9502524,0.000100012054,0.00010574658,0.0018711486,0.0035162892,0.00080698787,0.02463096,0.00014582677,0.0017595871,0.01626084],"study_design_scores_gemma":[0.0000032550672,0.000020754032,0.9972289,0.000002709614,0.000011829307,0.00014469188,0.0008319997,0.00024617143,0.0003763331,0.000009218123,0.0011173151,0.0000067020496],"about_ca_topic_score_codex":0.089898065,"about_ca_topic_score_gemma":0.09073279,"teacher_disagreement_score":0.089898065,"about_ca_system_score_codex":0.00086688914,"about_ca_system_score_gemma":0.00030283016,"threshold_uncertainty_score":0.17874956},"labels":[],"label_agreement":null},{"id":"W2045544028","doi":"10.1029/2007gl031427","title":"The Generalized heat function","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Mixing (physics); Heat flux; Climatology; Function (biology); Geology; Ocean current; Work (physics); Geophysics; Oceanography; Meteorology; Mechanics; Heat transfer; Thermodynamics; Physics","score_opus":0.02545903543351062,"score_gpt":0.277545290942141,"score_spread":0.25208625550863034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045544028","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04267773,0.004921184,0.915779,0.0009849429,0.00093757367,0.00014484925,0.0017820237,0.0007159348,0.03205692],"genre_scores_gemma":[0.85364664,0.0046121865,0.10325829,0.0006628033,0.0014172379,0.00045122724,0.0015205838,0.0005512752,0.033879675],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991923,0.00021381513,0.000037945963,0.00020320786,0.00021218156,0.00014059174],"domain_scores_gemma":[0.99878186,0.0004608352,0.0001454436,0.00018602307,0.00034829666,0.00007754862],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010587228,0.0009263681,0.00086238794,0.0019091509,0.0006289015,0.0020885675,0.001064987,0.0011992526,0.0063343216],"category_scores_gemma":[0.004014825,0.0002543125,0.00095537317,0.001776389,0.0020530117,0.0025870465,0.0011829907,0.0009313462,0.0017334512],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007286806,0.000028183977,0.0036422866,0.00032040445,0.00010600653,0.00027502008,0.00032206994,0.14887363,0.008741129,0.73635185,0.012170766,0.08909581],"study_design_scores_gemma":[0.000020656655,0.00010153812,0.005357967,0.00008608918,0.00005582986,0.00051399117,0.00016638351,0.46365014,0.0037024978,0.47242007,0.053767584,0.00015733762],"about_ca_topic_score_codex":0.0031798873,"about_ca_topic_score_gemma":0.0008772747,"teacher_disagreement_score":0.0063343216,"about_ca_system_score_codex":0.0010407671,"about_ca_system_score_gemma":0.0009801269,"threshold_uncertainty_score":0.021190464},"labels":[],"label_agreement":null},{"id":"W2045590754","doi":"10.1029/2007gl030492","title":"Observations of Pi2 pulsations by the Wallops HF radar in association with substorm expansion","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Substorm; Electrojet; Geophysics; Ionosphere; Solar wind; Radar; Physics; Geomagnetic storm; Amplitude; Magnetic field; Geology; Magnetometer; Earth's magnetic field; Atmospheric sciences; Magnetosphere","score_opus":0.01859530750063934,"score_gpt":0.27532850621396454,"score_spread":0.25673319871332523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045590754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99813867,0.00007598493,0.00028276554,0.000022477667,0.0000051126935,0.0000049585124,0.000104730876,0.000014623694,0.0013505825],"genre_scores_gemma":[0.99908555,0.000044670953,0.00022341422,0.000016338996,0.000020780066,0.0000034895054,0.00027916313,0.0000026450448,0.00032396216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993503,0.000006468103,0.000003193523,0.000008729745,0.00001732989,0.000029216384],"domain_scores_gemma":[0.99974686,0.000038996666,0.0000773845,0.00002847197,0.000045087818,0.00006328976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016123633,0.00014441759,0.00010607952,0.00040345557,0.0001778862,0.00025956405,0.000106950065,0.00018556073,0.0007781846],"category_scores_gemma":[0.00037242533,0.00007246687,0.00005231709,0.00024803658,0.00017991252,0.00017711174,0.00024791693,0.00022542536,0.00014378977],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005223209,0.00008718908,0.808017,0.000047753216,0.000072953415,0.0028170773,0.00085107115,0.0003455206,0.15221314,0.0003831433,0.0014834729,0.033159263],"study_design_scores_gemma":[0.000013880405,0.00017242653,0.9901097,0.000004821284,0.000014242552,0.0010635563,0.00013341688,0.00038769454,0.006024474,0.00006872731,0.002001577,0.0000056087365],"about_ca_topic_score_codex":0.0017013865,"about_ca_topic_score_gemma":0.0029674356,"teacher_disagreement_score":0.0017013865,"about_ca_system_score_codex":0.000082196566,"about_ca_system_score_gemma":0.00005922486,"threshold_uncertainty_score":0.0033830404},"labels":[],"label_agreement":null},{"id":"W2045692948","doi":"10.1029/2003gl016995","title":"Signal‐to‐noise ratios of observed monthly tropical ocean color","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"SeaWiFS; Upwelling; Biogeochemical cycle; Environmental science; Climatology; Data assimilation; Oceanography; Noise (video); Tropics; Geology; Meteorology; Geography","score_opus":0.04245552074555529,"score_gpt":0.2587325975951015,"score_spread":0.2162770768495462,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045692948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9812526,0.000111845584,0.013603257,0.00005615064,0.000037419304,0.000029759472,0.0027596187,0.00045601133,0.0016933781],"genre_scores_gemma":[0.9851719,0.00006770915,0.0066771274,0.000033012337,0.00002534748,0.000038123937,0.0072729005,0.00007516394,0.0006385989],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994215,0.00007806099,0.000046607904,0.00013734352,0.00022821697,0.000088242705],"domain_scores_gemma":[0.9987816,0.00042092154,0.00019129286,0.00014220152,0.00039460062,0.000069294365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009830035,0.00044498232,0.00031196675,0.0012791259,0.0001963638,0.00051421596,0.000322312,0.00029709018,0.0009909568],"category_scores_gemma":[0.0035157138,0.00021621335,0.0005087706,0.000970171,0.00018664403,0.0003768873,0.0004067394,0.00028871378,0.00030597256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022479333,0.00048107663,0.6257223,0.00022218013,0.000842247,0.00039175726,0.00027623615,0.10191049,0.057848852,0.0018487389,0.004028207,0.20418006],"study_design_scores_gemma":[0.000054513275,0.00024577868,0.82342446,0.000020672938,0.00015122027,0.0003358922,0.00008883468,0.14615698,0.025464745,0.00074091373,0.0032443977,0.000071589275],"about_ca_topic_score_codex":0.006147501,"about_ca_topic_score_gemma":0.006115004,"teacher_disagreement_score":0.006147501,"about_ca_system_score_codex":0.0004993501,"about_ca_system_score_gemma":0.00029667298,"threshold_uncertainty_score":0.0122234225},"labels":[],"label_agreement":null},{"id":"W2045884461","doi":"10.1029/2000gl011944","title":"Cirrus horizontal inhomogeneity and OLR bias","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Cirrus; Outgoing longwave radiation; Troposphere; Radiative transfer; Longwave; Environmental science; Optical depth; Atmospheric sciences; Horizontal plane; Cloud cover; Meteorology; Physics; Cloud computing; Convection; Geology; Optics; Geodesy","score_opus":0.0342281182706324,"score_gpt":0.2881355950598995,"score_spread":0.2539074767892671,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2045884461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9632091,0.0008631634,0.026484648,0.00012044694,0.000057223777,0.000032188993,0.0007323651,0.00031387713,0.008187069],"genre_scores_gemma":[0.997021,0.00026476648,0.0016494768,0.000045771085,0.000034862675,0.0000071379786,0.00035336838,0.000055329594,0.0005683883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996536,0.00007488585,0.000023269216,0.00009038577,0.000079298625,0.000078699464],"domain_scores_gemma":[0.99803203,0.0008280969,0.0005259178,0.00034340358,0.00023822967,0.000032457883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00075595325,0.0003440772,0.00023302162,0.0005144822,0.0001959669,0.00047123837,0.00028180884,0.00023352607,0.0013156252],"category_scores_gemma":[0.0034074245,0.00016179924,0.0002989746,0.00076810695,0.00026244944,0.0007260138,0.00040818437,0.00021588025,0.0003161875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005017194,0.00009384833,0.63186175,0.00027433498,0.00034108016,0.00082353613,0.00028369648,0.14869273,0.11951831,0.010653702,0.0016717154,0.08528359],"study_design_scores_gemma":[0.000058055924,0.00011279728,0.76180166,0.00004480519,0.00027429915,0.00083999446,0.00015873068,0.1672267,0.05893081,0.005201951,0.0052605676,0.0000895396],"about_ca_topic_score_codex":0.004721882,"about_ca_topic_score_gemma":0.0032806294,"teacher_disagreement_score":0.004721882,"about_ca_system_score_codex":0.00039177056,"about_ca_system_score_gemma":0.00021877376,"threshold_uncertainty_score":0.009388804},"labels":[],"label_agreement":null},{"id":"W2046176281","doi":"10.1029/2006gl029085","title":"Retroflection of part of the east Greenland current at Cape Farewell","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Natural Environment Research Council; Sight Research UK","keywords":"Oceanography; Ocean gyre; Cape; Current (fluid); Boundary current; Geology; Structural basin; Arctic; The arctic; Water mass; Latitude; Ocean current; Climatology; Geography; Geomorphology; Archaeology; Subtropics","score_opus":0.03445547418211196,"score_gpt":0.2792539396545146,"score_spread":0.24479846547240267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046176281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95589614,0.0006954474,0.00039963116,0.001074106,0.00009027105,0.00003522979,0.0003270004,0.00004643787,0.04143572],"genre_scores_gemma":[0.9875636,0.00029980548,0.0005539134,0.00027509444,0.000017056364,0.000008094378,0.00028124425,0.000018439181,0.010982716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989426,0.0000069931484,0.000003498467,0.000025495072,0.000034696714,0.000035139343],"domain_scores_gemma":[0.9997795,0.000011539055,0.000051497515,0.0000150812,0.000092874536,0.000049580816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012440649,0.0001878825,0.00014593017,0.0007535147,0.00065075356,0.00060265616,0.00032274745,0.0001887881,0.0031209206],"category_scores_gemma":[0.00043438902,0.00007406847,0.000118414086,0.0004398683,0.00047418888,0.0004602668,0.000556412,0.00038006133,0.00026110516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005127325,0.00013837554,0.64089775,0.00018620626,0.00013407673,0.0066842134,0.004303302,0.0027424253,0.06592003,0.013690507,0.017996915,0.24679345],"study_design_scores_gemma":[0.00003222757,0.000058979193,0.94361466,0.00009434569,0.000030294985,0.00047593826,0.0012770861,0.001286225,0.0023491369,0.00068760605,0.050073404,0.000020100138],"about_ca_topic_score_codex":0.4798618,"about_ca_topic_score_gemma":0.693836,"teacher_disagreement_score":0.4798618,"about_ca_system_score_codex":0.0044095586,"about_ca_system_score_gemma":0.002143543,"threshold_uncertainty_score":0.9541374},"labels":[],"label_agreement":null},{"id":"W2046286396","doi":"10.1029/2008gl035819","title":"Spatial and temporal variability of biogenic gases during the Southern Ocean spring bloom","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Biogeochemical cycle; Oceanography; Environmental science; Spring bloom; Phytoplankton; Spring (device); Trace gas; Bloom; Water mass; Temporal scales; Atmospheric sciences; Spatial ecology; Pelagic zone; Geology; Chemistry; Environmental chemistry; Ecology; Nutrient; Biology","score_opus":0.015993645606099623,"score_gpt":0.23609203046289967,"score_spread":0.22009838485680006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046286396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994715,0.000047675443,0.00007154427,0.000021380745,0.0000014792231,0.0000011633975,0.00014395983,0.000010491169,0.00023093607],"genre_scores_gemma":[0.999406,0.000057607314,0.00011456134,0.0000102672,0.0000046115374,0.0000040217974,0.00023055126,0.0000032302619,0.00016908141],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999522,0.0000059272743,0.0000034318173,0.000015730231,0.000011678181,0.000011031255],"domain_scores_gemma":[0.9997707,0.00005750657,0.0000851872,0.000015370333,0.00003912343,0.000032103766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023734341,0.00011468924,0.00017756863,0.0005191158,0.0001889055,0.00030280332,0.00011080479,0.00015172022,0.00041473654],"category_scores_gemma":[0.00038241092,0.00014263096,0.000096606105,0.0004535148,0.00022968357,0.00021145186,0.00025836236,0.0001476694,0.000094372044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005683925,0.00005991253,0.8458197,0.00004681718,0.00010722028,0.00025634977,0.0007340493,0.0019659067,0.13520303,0.0001710223,0.0003581984,0.0147093935],"study_design_scores_gemma":[0.0000037560644,0.000015546037,0.9979965,0.0000015849063,0.0000072465173,0.000023718667,0.000067497545,0.00069453206,0.00097501714,0.000030787465,0.00018055394,0.00000321573],"about_ca_topic_score_codex":0.010618388,"about_ca_topic_score_gemma":0.01466068,"teacher_disagreement_score":0.010618388,"about_ca_system_score_codex":0.000286333,"about_ca_system_score_gemma":0.00013982074,"threshold_uncertainty_score":0.021113157},"labels":[],"label_agreement":null},{"id":"W2046389114","doi":"10.1029/1999gl002389","title":"Arctic oscillation and Arctic sea‐ice oscillation","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":155,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Center for Atmospheric Research","keywords":"Sea ice; Empirical orthogonal functions; Arctic oscillation; Climatology; Arctic ice pack; Arctic sea ice decline; North Atlantic oscillation; Arctic; Geology; Mode (computer interface); The arctic; Sea ice concentration; Oceanography; Oscillation (cell signaling); Drift ice; Sea ice thickness","score_opus":0.021440304595280492,"score_gpt":0.2636833516003319,"score_spread":0.24224304700505142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046389114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9384321,0.02348769,0.004254417,0.00075248623,0.00028821672,0.000043907938,0.008190193,0.000081102284,0.024469923],"genre_scores_gemma":[0.97925377,0.010334022,0.0028595421,0.000120500576,0.00037228919,0.000052717958,0.0039716945,0.000017963292,0.0030174772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996959,0.00008017757,0.000026772323,0.000074779055,0.00007943596,0.000042822292],"domain_scores_gemma":[0.99929535,0.0001510617,0.00034298806,0.000020883932,0.00012385086,0.000065808315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004951521,0.00027650435,0.000244271,0.0010627107,0.00027457034,0.00065906165,0.00010909845,0.00015045733,0.0015805968],"category_scores_gemma":[0.0022341858,0.00006502593,0.00017023885,0.002551552,0.00020938618,0.00049926346,0.00034287106,0.00021438574,0.00022811006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022179258,0.000039863786,0.88423395,0.0002441583,0.00014028721,0.00021998117,0.0006061043,0.002993706,0.00082790497,0.0051523093,0.004783591,0.10053645],"study_design_scores_gemma":[0.0000050758645,0.00002523331,0.9811593,0.000051523104,0.000023207076,0.00015980478,0.0002039598,0.0012101114,0.00008740594,0.0013545607,0.01571223,0.0000075424296],"about_ca_topic_score_codex":0.014469935,"about_ca_topic_score_gemma":0.017561682,"teacher_disagreement_score":0.014469935,"about_ca_system_score_codex":0.0003960661,"about_ca_system_score_gemma":0.000443954,"threshold_uncertainty_score":0.0287714},"labels":[],"label_agreement":null},{"id":"W2046504753","doi":"10.1029/2006gl026206","title":"Inter‐ and intra‐continental transport of radioactive cesium released by boreal forest fires","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Radioactive contamination and transfer","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Health Canada","funders":"","keywords":"Taiga; Environmental science; Atmosphere (unit); Radionuclide; Boreal; Caesium; Atmospheric sciences; Geology; Physical geography; Meteorology; Geography; Physics; Paleontology; Nuclear physics; Forestry","score_opus":0.008511784110770785,"score_gpt":0.2472602261916912,"score_spread":0.23874844208092041,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046504753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999548,0.00002222901,0.00008138241,0.0000044661697,0.0000010938203,0.0000013073176,0.00008164554,0.000005159459,0.00025475907],"genre_scores_gemma":[0.9993843,0.00003709508,0.00022749726,0.000002692571,8.045047e-7,0.0000016883362,0.00017705259,0.000003151984,0.00016556997],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999052,0.000009477891,0.0000032917173,0.000035115034,0.000021421545,0.000025365844],"domain_scores_gemma":[0.9998611,0.000023212713,0.000038126123,0.000013472286,0.000042231164,0.00002182272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021298684,0.00023080228,0.00015432689,0.00052072643,0.00056797575,0.0004976094,0.00030192005,0.00016790103,0.0003298746],"category_scores_gemma":[0.00022615732,0.00014790644,0.0001883176,0.00039946777,0.00029056476,0.00024320478,0.0002808585,0.00022105232,0.00007183019],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006492438,0.00009003325,0.8668536,0.000028134637,0.00013217634,0.0002885227,0.0005993854,0.0047475942,0.11001251,0.00026163354,0.00018952608,0.016147763],"study_design_scores_gemma":[0.0000153036,0.00010369901,0.9851238,0.000004545371,0.00003763434,0.00010741504,0.00032109584,0.0038529062,0.009814749,0.000046261903,0.0005588757,0.000013747461],"about_ca_topic_score_codex":0.24017777,"about_ca_topic_score_gemma":0.2544492,"teacher_disagreement_score":0.24017777,"about_ca_system_score_codex":0.0012652152,"about_ca_system_score_gemma":0.0005201428,"threshold_uncertainty_score":0.4775595},"labels":[],"label_agreement":null},{"id":"W2046557917","doi":"10.1029/2005gl023646","title":"Observed and predicted responses of plant growth to climate across Canada","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Climate change; Environmental science; Physical geography; Geology; Geography; Meteorology; Oceanography","score_opus":0.04693636064846808,"score_gpt":0.2941701971931653,"score_spread":0.24723383654469722,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046557917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946709,0.00012782316,0.00014901617,0.00007179186,0.0000028803634,0.000004424109,0.0042292736,0.000030997464,0.00071285805],"genre_scores_gemma":[0.99679583,0.00009969154,0.00014810881,0.000012448975,0.0000013327129,0.0000037203563,0.0025970996,0.0000040853884,0.00033774698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999838,0.0000135250875,0.000007934074,0.000052979583,0.000036295118,0.00005114099],"domain_scores_gemma":[0.99927205,0.00011247261,0.00008094334,0.00002702962,0.0003988611,0.00010869889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032476452,0.0002853941,0.00016076333,0.0005371197,0.00059363345,0.0005816303,0.00039574225,0.00024522917,0.00087577564],"category_scores_gemma":[0.0011968121,0.00016001916,0.000292189,0.0009789743,0.00023794429,0.00021445565,0.0002500518,0.00025271843,0.00013155887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013346724,0.000025954174,0.9597824,0.000036163936,0.000099179895,0.00006485546,0.00020124068,0.030720973,0.0011916432,0.00026575453,0.0013193502,0.0061589982],"study_design_scores_gemma":[0.00001100666,0.000009222687,0.9791047,0.000008727837,0.000019732135,0.000023059261,0.00016847468,0.019307308,0.00027010025,0.000058371235,0.0010071737,0.000012227519],"about_ca_topic_score_codex":0.9792875,"about_ca_topic_score_gemma":0.98447454,"teacher_disagreement_score":0.020712495,"about_ca_system_score_codex":0.012584385,"about_ca_system_score_gemma":0.004627754,"threshold_uncertainty_score":0.09130657},"labels":[],"label_agreement":null},{"id":"W2046619880","doi":"10.1029/2004gl021480","title":"Voyager 2 observations related to the October–November 2003 solar events","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Jet Propulsion Laboratory; Association of Canadian Universities for Northern Studies","keywords":"Ejecta; Cosmic ray; Forbush decrease; Physics; Shock (circulatory); Astrophysics; Heliosphere; Flux (metallurgy); Solar wind; Intensity (physics); Astronomy; Coronal mass ejection; Plasma; Supernova; Optics; Nuclear physics","score_opus":0.02876988211085792,"score_gpt":0.3119608668166731,"score_spread":0.2831909847058152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046619880","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98968166,0.00018086743,0.00050250656,0.00009079957,0.00004117666,0.00003548455,0.0017169826,0.00019176184,0.0075587486],"genre_scores_gemma":[0.99351805,0.00011800522,0.0008287488,0.00006254826,0.00003828081,0.000018713563,0.0034389754,0.000025766685,0.0019509317],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986076,0.0000065810427,0.000005334641,0.00003847053,0.000042808162,0.000046039728],"domain_scores_gemma":[0.99976104,0.000027930057,0.000059667826,0.000042526357,0.000046240177,0.00006250106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019983065,0.00024648747,0.00020051796,0.0008500479,0.0004998382,0.0005413853,0.00028315085,0.0007322601,0.00077533553],"category_scores_gemma":[0.00044584827,0.00016868315,0.00019455992,0.00073815417,0.00016433393,0.00024264937,0.0006412104,0.0005738255,0.00025867193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019529705,0.00029811653,0.80008674,0.00016311604,0.00023718333,0.0047443477,0.0034370793,0.0049110414,0.122539535,0.0014565325,0.013902326,0.046270963],"study_design_scores_gemma":[0.00004056995,0.00009386294,0.9800965,0.000011869049,0.00002188998,0.0005149967,0.00018922504,0.0019088037,0.004781307,0.00014351412,0.012179432,0.000017986193],"about_ca_topic_score_codex":0.009753018,"about_ca_topic_score_gemma":0.029407535,"teacher_disagreement_score":0.009753018,"about_ca_system_score_codex":0.00064134394,"about_ca_system_score_gemma":0.0002611918,"threshold_uncertainty_score":0.01939249},"labels":[],"label_agreement":null},{"id":"W2046925220","doi":"10.1029/2003gl017828","title":"Comparing continental and oceanic cloud susceptibilities to aerosols","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Effective radius; Liquid water path; Environmental science; Cloud computing; Atmospheric sciences; RADIUS; Liquid water content; Meteorology; Climatology; Geology; Geography; Physics","score_opus":0.031010293993201477,"score_gpt":0.28649216073461786,"score_spread":0.2554818667414164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2046925220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979346,0.00007810424,0.00025215268,0.000016436288,0.0000017348718,0.000005749549,0.000114619164,0.000009079846,0.0015875105],"genre_scores_gemma":[0.9994785,0.00006118516,0.0001323061,0.0000065432873,0.0000030034275,0.0000029219414,0.00019138561,0.000004001239,0.00012014769],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985266,0.000029316687,0.000012420548,0.000029213923,0.000031964395,0.00004450005],"domain_scores_gemma":[0.9994548,0.00022207729,0.000086241394,0.00005346227,0.00010187473,0.00008147654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027350124,0.00029331888,0.00016919218,0.00072829437,0.00025739783,0.00051435444,0.00018381348,0.00028440513,0.0015391118],"category_scores_gemma":[0.0013507941,0.00014010341,0.00042700127,0.0006525266,0.00021649245,0.00037873248,0.00096872,0.00019497462,0.00014501579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037865984,0.000052875886,0.90441066,0.00009614838,0.00042255854,0.00028483995,0.00024481668,0.038934268,0.040352598,0.0014913776,0.00022682385,0.013104256],"study_design_scores_gemma":[0.000024822955,0.00006831533,0.9590428,0.000009262241,0.00012962711,0.000092700146,0.00022078172,0.029366974,0.009955029,0.0004832841,0.00059095747,0.00001551542],"about_ca_topic_score_codex":0.013301909,"about_ca_topic_score_gemma":0.009642705,"teacher_disagreement_score":0.013301909,"about_ca_system_score_codex":0.00030542727,"about_ca_system_score_gemma":0.00018270027,"threshold_uncertainty_score":0.026448965},"labels":[],"label_agreement":null},{"id":"W2047027756","doi":"10.1029/2002gl015366","title":"How do high‐latitude North Atlantic climate signals the crossover between the Deep Western Boundary Current and the Gulf Stream?","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Boundary current; Geology; Ocean gyre; Bathymetry; Water mass; Jet stream; Gulf Stream; Inflow; Rossby wave; Climatology; Zonal and meridional; Forcing (mathematics); Oceanography; Current (fluid); Ocean current; Jet (fluid); Subtropics; Mechanics","score_opus":0.022288283461650377,"score_gpt":0.26762034465476153,"score_spread":0.24533206119311116,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047027756","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98985344,0.000092478534,0.0024084263,0.00080360036,0.00003738602,0.00001329798,0.0002024885,0.000040793657,0.0065481174],"genre_scores_gemma":[0.9988427,0.000051105922,0.00014938993,0.000046746012,0.000008026318,0.0000025770178,0.000035097295,0.000004216492,0.0008601602],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999342,0.000020752108,0.0000023292325,0.0000132966325,0.000007449827,0.00002198131],"domain_scores_gemma":[0.99977833,0.00007842246,0.000050180657,0.000012163412,0.000025758021,0.000055231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031094442,0.00020450613,0.0002752248,0.00014526947,0.00030357655,0.0011752952,0.0002259336,0.0007206313,0.002254937],"category_scores_gemma":[0.0013593937,0.00023063268,0.00033565285,0.00016024911,0.00041404055,0.00074384746,0.0003037679,0.00036071226,0.00027025567],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008762444,0.000262614,0.409035,0.00012408485,0.00027847957,0.0010984332,0.0004960701,0.4998863,0.027803477,0.03863361,0.0028065944,0.018699089],"study_design_scores_gemma":[0.00014393467,0.00014997927,0.14511183,0.0000174418,0.00008214731,0.00014419337,0.00038431492,0.8380677,0.001122196,0.013383599,0.0013534789,0.000039185335],"about_ca_topic_score_codex":0.026619833,"about_ca_topic_score_gemma":0.022898337,"teacher_disagreement_score":0.026619833,"about_ca_system_score_codex":0.00075307145,"about_ca_system_score_gemma":0.0005490638,"threshold_uncertainty_score":0.05292976},"labels":[],"label_agreement":null},{"id":"W2047255752","doi":"10.1029/2005gl025139","title":"Influence of assimilated eddies on the large‐scale circulation in a model of the northwest Atlantic Ocean","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Ocean gyre; Eddy; Circulation (fluid dynamics); Geology; Climatology; Ridge; Ocean current; Gulf Stream; Oceanography; General Circulation Model; Scale (ratio); Meteorology; Geography; Climate change; Turbulence; Subtropics; Mechanics; Physics; Paleontology","score_opus":0.016866239289197633,"score_gpt":0.23776324858820025,"score_spread":0.2208970092990026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047255752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894098,0.000062680294,0.009038268,0.00024473554,0.000041427247,0.000010996721,0.00006562671,0.000074339136,0.001052238],"genre_scores_gemma":[0.9974209,0.000024199444,0.0021951345,0.000036092777,0.0000066390885,0.0000075869307,0.000042787804,0.000012108351,0.0002544563],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989533,0.00004280556,0.0000064929377,0.000022245302,0.000015340996,0.000017749815],"domain_scores_gemma":[0.9994733,0.00026185057,0.000072477604,0.00005054448,0.0000621856,0.000079685844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045411524,0.00048801288,0.00032700173,0.00009199556,0.0005405168,0.00094402523,0.0004899486,0.0006584972,0.00044294033],"category_scores_gemma":[0.0021831985,0.00042058824,0.0003723183,0.000071826486,0.00075695745,0.00052200013,0.0007711992,0.0006584329,0.000058978734],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000240198,0.00007264258,0.019158138,0.000017939774,0.000075187476,0.0002142339,0.000057395453,0.96835226,0.0072395406,0.001055189,0.00020209077,0.0033151514],"study_design_scores_gemma":[0.00003299803,0.000025546145,0.0017838728,0.0000019923716,0.000011126946,0.000008675225,0.000010080304,0.9971161,0.000754288,0.00016309721,0.00008424911,0.000007952312],"about_ca_topic_score_codex":0.053757,"about_ca_topic_score_gemma":0.031460628,"teacher_disagreement_score":0.053757,"about_ca_system_score_codex":0.0006992859,"about_ca_system_score_gemma":0.0010537378,"threshold_uncertainty_score":0.106888235},"labels":[],"label_agreement":null},{"id":"W2047323617","doi":"10.1029/2008gl035640","title":"Improve the utility of a coastal circulation model by assimilating hydrographic observations into the model momentum equation","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Hydrography; Circulation (fluid dynamics); Bay; Momentum (technical analysis); Environmental science; Ocean current; Climatology; General Circulation Model; Oceanography; Salinity; Geology; Meteorology; Physics; Climate change; Mechanics","score_opus":0.08060867871478102,"score_gpt":0.27680377094993297,"score_spread":0.19619509223515197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047323617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.59024286,0.00031821823,0.3938968,0.0006497716,0.00020086317,0.00017229996,0.0009300662,0.0024165367,0.011172656],"genre_scores_gemma":[0.9111276,0.0001338599,0.08537649,0.000049197926,0.000024767283,0.000044848697,0.000438257,0.000115252675,0.0026896878],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999201,0.0000126860805,0.0000061327687,0.000016703836,0.000033684806,0.000010603803],"domain_scores_gemma":[0.9996866,0.0000785903,0.00003840573,0.000063014326,0.00010574896,0.000027754702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034855626,0.0005499835,0.000304377,0.00018955016,0.00033307137,0.0008433159,0.0008488562,0.0005041872,0.0012370133],"category_scores_gemma":[0.0017186498,0.0002537259,0.00038043014,0.00018979485,0.00024410617,0.0007142039,0.0006345813,0.0006039758,0.00045743928],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004917694,0.00007660615,0.018019486,0.000037284117,0.000054878004,0.00009780673,0.000087631925,0.9364007,0.010882427,0.0025903888,0.00093028956,0.030773304],"study_design_scores_gemma":[0.000014660263,0.00001358278,0.001100316,0.0000039828137,0.000007162976,0.000007883986,0.0000066593816,0.99726224,0.0007118249,0.00028819658,0.0005778049,0.000005660968],"about_ca_topic_score_codex":0.20315456,"about_ca_topic_score_gemma":0.1502041,"teacher_disagreement_score":0.20315456,"about_ca_system_score_codex":0.00131647,"about_ca_system_score_gemma":0.0022923488,"threshold_uncertainty_score":0.40394413},"labels":[],"label_agreement":null},{"id":"W2047409381","doi":"10.1029/2000gl012740","title":"The Laptev Sea as a source for recent Arctic Ocean salinity changes","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs; International Arctic Research Center, University of Alaska, Fairbanks; National Science Foundation","keywords":"Halocline; Geology; Arctic; Canada Basin; Oceanography; Salinity; Structural basin; Thermohaline circulation; Sea ice; Climatology; Stratification (seeds); Geomorphology","score_opus":0.041831530730548724,"score_gpt":0.29798088734184247,"score_spread":0.25614935661129373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047409381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952571,0.00078515016,0.00040506016,0.00035731366,0.000021650963,0.0000039122115,0.0001795355,0.000020511196,0.0029698422],"genre_scores_gemma":[0.9988771,0.00034970092,0.00010927559,0.00003128285,0.000020308515,0.0000019840293,0.0001948048,0.000004813145,0.00041059576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.000008919317,0.0000036367742,0.000010515359,0.000012263161,0.000020307194],"domain_scores_gemma":[0.9998344,0.000024090949,0.00006273657,0.000014909147,0.00003388205,0.000030023644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017462857,0.0001458317,0.0001833414,0.0007811558,0.0003860669,0.001089797,0.0002323206,0.00024382447,0.0013470972],"category_scores_gemma":[0.0005483187,0.00010565965,0.00018056144,0.0007834048,0.00021510194,0.0006015985,0.001078456,0.00024543828,0.00018393148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031100653,0.00003738738,0.93133336,0.000107466425,0.00015789161,0.0021753174,0.0006177307,0.003557096,0.011786293,0.004546212,0.0007253278,0.0446449],"study_design_scores_gemma":[0.000023464245,0.00008596159,0.97823673,0.00006617186,0.00006513751,0.001086859,0.0010982577,0.0063549797,0.002442177,0.0017781183,0.008744262,0.000017818647],"about_ca_topic_score_codex":0.006861077,"about_ca_topic_score_gemma":0.009351618,"teacher_disagreement_score":0.006861077,"about_ca_system_score_codex":0.00046560168,"about_ca_system_score_gemma":0.00044000227,"threshold_uncertainty_score":0.013642311},"labels":[],"label_agreement":null},{"id":"W2047535475","doi":"10.1029/2005gl022392","title":"Simulation of the October–November 2003 solar proton events in the CMAM GCM: Comparison with observations","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mesosphere; Atmospheric sciences; GCM transcription factors; Atmosphere (unit); Descent (aeronautics); Proton; Polar; Environmental science; Storm; Climatology; Thermosphere; Polar night; Physics; Meteorology; General Circulation Model; Geology; Stratosphere; Ionosphere; Climate change; Astronomy; Oceanography","score_opus":0.03538073877307437,"score_gpt":0.3190369025414412,"score_spread":0.28365616376836683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047535475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935788,0.00007994737,0.0006395869,0.00045795715,0.000049218645,0.000027163187,0.0013714359,0.0001286505,0.0036670845],"genre_scores_gemma":[0.9974663,0.000033276483,0.00097059313,0.000111293215,0.000011710803,0.000022167043,0.0009009968,0.00002397947,0.0004597139],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986815,0.000040742394,0.000006658394,0.000026628522,0.000018240076,0.00003950557],"domain_scores_gemma":[0.9989945,0.00045756073,0.00010710901,0.000054853037,0.0001470659,0.0002388755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005478384,0.0005008741,0.0004762182,0.000413258,0.00060503365,0.00076241844,0.0011326304,0.0019106189,0.003069294],"category_scores_gemma":[0.0019498438,0.00037968595,0.0006711883,0.0005948622,0.00070058426,0.00052563846,0.00048120503,0.0012779849,0.00023389753],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000666847,0.00031594242,0.025750676,0.000043145657,0.00014120147,0.00020748879,0.0000991745,0.966165,0.0011238474,0.001120907,0.002252073,0.0021136606],"study_design_scores_gemma":[0.00018546914,0.00009316418,0.010697984,0.0000072927296,0.000034980174,0.000018426472,0.00013732041,0.9878406,0.0003144123,0.00026263946,0.0003926799,0.000015070073],"about_ca_topic_score_codex":0.11517761,"about_ca_topic_score_gemma":0.08238283,"teacher_disagreement_score":0.11517761,"about_ca_system_score_codex":0.0017503584,"about_ca_system_score_gemma":0.0011694657,"threshold_uncertainty_score":0.2290144},"labels":[],"label_agreement":null},{"id":"W2047972613","doi":"10.1029/2003gl017433","title":"The impact of varying atmospheric forcing on the thickness of arctic multi‐year sea ice","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Sea ice; Arctic ice pack; Arctic sea ice decline; Climatology; Arctic oscillation; Arctic; Forcing (mathematics); Geology; Arctic geoengineering; Arctic dipole anomaly; Drift ice; Anomaly (physics); Sea ice thickness; Atmospheric sciences; Oceanography; Physics; Northern Hemisphere","score_opus":0.031916916027237466,"score_gpt":0.29328097777580825,"score_spread":0.2613640617485708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2047972613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987197,0.000050803996,0.0002968458,0.000054754022,0.000018408746,0.0000046515047,0.00035714326,0.00002242806,0.0004752761],"genre_scores_gemma":[0.9993067,0.000051653187,0.00016978297,0.00001522371,0.0000045568413,0.000005734527,0.00033435994,0.000009727001,0.00010232756],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982953,0.00006398041,0.000012412978,0.000031431246,0.000022674081,0.000040042498],"domain_scores_gemma":[0.99855524,0.0010350072,0.00013296424,0.00008332974,0.00008655284,0.00010686014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005431517,0.0005538746,0.00024118059,0.00024470364,0.00045176863,0.00061085017,0.00038525552,0.00064377364,0.000856786],"category_scores_gemma":[0.0032590386,0.00032722566,0.0006214935,0.00025707434,0.00039202961,0.00045147561,0.000489595,0.0005247654,0.00013451694],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011283035,0.00028199572,0.2221036,0.00008599592,0.0003425263,0.00036892729,0.000064133004,0.7509059,0.016049052,0.00048776026,0.0007641662,0.007417647],"study_design_scores_gemma":[0.0001471082,0.000621803,0.24669488,0.00001831094,0.00017107396,0.00011805133,0.00013458646,0.74265,0.008098849,0.00038106876,0.00090298156,0.00006136513],"about_ca_topic_score_codex":0.023508614,"about_ca_topic_score_gemma":0.017573021,"teacher_disagreement_score":0.023508614,"about_ca_system_score_codex":0.00076465623,"about_ca_system_score_gemma":0.0004744229,"threshold_uncertainty_score":0.04674357},"labels":[],"label_agreement":null},{"id":"W2048731507","doi":"10.1002/2014gl061178","title":"Periodic time‐dependent parameters improving forecasting abilities of biological ocean models","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Plankton; Biogeochemical cycle; Satellite; Estimation theory; Series (stratigraphy); Representation (politics); Computer science; Climatology; Environmental science; Geology; Oceanography; Algorithm; Ecology; Biology; Physics","score_opus":0.06068540133891102,"score_gpt":0.2489104755978454,"score_spread":0.1882250742589344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048731507","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89569,0.00006854144,0.102696374,0.000121269244,0.000017312928,0.000015631964,0.00007154436,0.0003513288,0.0009680413],"genre_scores_gemma":[0.97369725,0.000024998619,0.025999295,0.000010174148,0.000008206442,0.000014126497,0.00007927697,0.00002745302,0.0001392618],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997968,0.00010420379,0.000013763083,0.000038457838,0.000027896316,0.00001891926],"domain_scores_gemma":[0.99843353,0.0009902486,0.00015488465,0.00023938017,0.00014368008,0.000038315913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009892083,0.0004164286,0.0003655036,0.00034946942,0.00015998849,0.0004424645,0.00044244848,0.0004828495,0.00045696145],"category_scores_gemma":[0.005382252,0.00024821472,0.00027869578,0.00024416344,0.0002006591,0.0005843786,0.00048114263,0.00044474273,0.0000984039],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011454312,0.00006477757,0.011322988,0.000016271131,0.000058312467,0.00003399312,0.00003072994,0.95523477,0.004091276,0.00081596803,0.00015432495,0.028062094],"study_design_scores_gemma":[0.000008062753,0.00001626922,0.0010433665,0.0000014657678,0.0000057916704,0.000003886757,0.0000019050005,0.9975701,0.0011329927,0.00017273273,0.000039654107,0.0000037346258],"about_ca_topic_score_codex":0.0056730355,"about_ca_topic_score_gemma":0.0038530878,"teacher_disagreement_score":0.0056730355,"about_ca_system_score_codex":0.00022574433,"about_ca_system_score_gemma":0.0005604164,"threshold_uncertainty_score":0.01128},"labels":[],"label_agreement":null},{"id":"W2048880726","doi":"10.1029/2003gl018838","title":"A fully coupled constitutive model for thermo‐hydro‐mechanical analysis in elastic media with double porosity","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":137,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Mechanics; Heat flux; Constitutive equation; Conservation law; Darcy's law; Porous medium; Isothermal process; Partial differential equation; Porosity; Fluid dynamics; Materials science; Conservation of mass; Heat transfer; Thermodynamics; Physics; Finite element method; Composite material","score_opus":0.026443725451505872,"score_gpt":0.27820697899194935,"score_spread":0.2517632535404435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048880726","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.025405852,0.0007601982,0.96072656,0.0003215789,0.0001630704,0.00010495774,0.0004716019,0.00023493114,0.011811272],"genre_scores_gemma":[0.6591331,0.0023391815,0.28950545,0.00022967331,0.00019474745,0.0013329266,0.0008925488,0.00024895993,0.046123587],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997987,0.00003408979,0.00001348255,0.00003333356,0.000095178606,0.00002515276],"domain_scores_gemma":[0.9998221,0.000069759684,0.000028573946,0.000028911814,0.000032375527,0.000018245777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032114892,0.0005592534,0.00077422627,0.0005829403,0.0004886718,0.0011262193,0.0015435229,0.0015560566,0.0020809676],"category_scores_gemma":[0.0007044748,0.00055939466,0.00074226415,0.0007580207,0.00087404577,0.001351164,0.000996087,0.0011313678,0.00055042823],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001878192,0.00004948746,0.00037787296,0.00009055322,0.000021751992,0.00019560558,0.0000933381,0.86119556,0.012034608,0.11446332,0.00090246997,0.010556705],"study_design_scores_gemma":[0.000006192295,0.000012667763,0.0001493199,0.000008637757,0.0000068201507,0.00006761048,0.000012554434,0.98406374,0.0006228867,0.011222133,0.0038171937,0.000010198782],"about_ca_topic_score_codex":0.0018817936,"about_ca_topic_score_gemma":0.002134307,"teacher_disagreement_score":0.0020809676,"about_ca_system_score_codex":0.00060760754,"about_ca_system_score_gemma":0.001120697,"threshold_uncertainty_score":0.006961584},"labels":[],"label_agreement":null},{"id":"W2048927550","doi":"10.1029/2004gl021316","title":"Atlantic versus Indo‐Pacific influence on Atlantic‐European climate","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Bundesministerium für Bildung und Forschung","keywords":"Atlantic Equatorial mode; Tropical Atlantic; Atlantic multidecadal oscillation; North Atlantic oscillation; Oceanography; Climatology; North Atlantic Deep Water; Gulf Stream; Thermohaline circulation; Geology; Boreal; Forcing (mathematics); Sea surface temperature; Atlantic hurricane; Tropical cyclone","score_opus":0.0430969919678158,"score_gpt":0.31059750362008853,"score_spread":0.26750051165227273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048927550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885378,0.00020800931,0.00017948136,0.00014504684,0.000015246564,0.000002633203,0.00034252022,0.000009776102,0.010559551],"genre_scores_gemma":[0.9990102,0.0002531332,0.00009830998,0.000031467578,0.000009572371,0.0000026138803,0.00018598772,0.000006145311,0.00040269893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989784,0.000026985485,0.0000066470316,0.00002386103,0.000015586218,0.000028982111],"domain_scores_gemma":[0.9996933,0.00011981647,0.000058967664,0.00003461779,0.00005083786,0.00004239649],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031366816,0.0001740353,0.0001802214,0.0002463841,0.00034179242,0.00072672474,0.00018438857,0.00018308216,0.0028816592],"category_scores_gemma":[0.00085305877,0.00007912265,0.00030324186,0.00049241324,0.00025327515,0.00035336515,0.0006249981,0.00019111797,0.00017148272],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009671663,0.00012370045,0.8787217,0.00014226718,0.0005539692,0.0006440318,0.00031783254,0.044842053,0.019311137,0.009428462,0.00226229,0.04268537],"study_design_scores_gemma":[0.0000357529,0.00005141372,0.96764207,0.0000272447,0.00022895423,0.00007407502,0.00024294357,0.025775502,0.0015001881,0.0010382674,0.0033664864,0.00001718115],"about_ca_topic_score_codex":0.020060616,"about_ca_topic_score_gemma":0.034752928,"teacher_disagreement_score":0.020060616,"about_ca_system_score_codex":0.0003524593,"about_ca_system_score_gemma":0.00031752212,"threshold_uncertainty_score":0.039887726},"labels":[],"label_agreement":null},{"id":"W2048952305","doi":"10.1029/2006gl026611","title":"Importance of groundwater in the water balance of an alpine headwater lake","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Parks Canada; University of Calgary","keywords":"Groundwater; STREAMS; Hydrology (agriculture); Water balance; Glacier; Watershed; Outflow; Snowmelt; Groundwater flow; Snow; Inflow; Environmental science; Geology; Groundwater discharge; Streamflow; Aquifer; Drainage basin; Geomorphology; Oceanography; Geography","score_opus":0.030776687979528344,"score_gpt":0.27431673362924147,"score_spread":0.24354004564971313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048952305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991387,0.00012858406,0.00009669734,0.000044996665,7.459979e-7,0.0000011918808,0.00004670424,0.000005008023,0.0005374414],"genre_scores_gemma":[0.9996644,0.000095066316,0.00009963045,0.000008519411,0.0000014762867,6.379444e-7,0.000031497377,8.7507476e-7,0.00009800028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994683,0.000011243919,0.000004246137,0.000009635088,0.000015078088,0.000012973479],"domain_scores_gemma":[0.9999238,0.000018094392,0.000020832518,0.0000022541599,0.000022516451,0.000012436437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119442775,0.00009429792,0.00015449707,0.00033002306,0.0005571574,0.000861299,0.00010839332,0.00016350164,0.00041380612],"category_scores_gemma":[0.00026092774,0.00009495627,0.00006487023,0.00049249653,0.00032528787,0.00036657415,0.00029574754,0.00012620389,0.000039846207],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029318297,0.000060536582,0.8803295,0.00007917091,0.0000591298,0.0004813593,0.001407525,0.0046092276,0.06959241,0.0007406583,0.00018155252,0.042165745],"study_design_scores_gemma":[0.000019178895,0.00011161561,0.97928256,0.00001724864,0.000054733682,0.00013038862,0.0017696073,0.009091684,0.0072826087,0.00059387274,0.0016282243,0.00001822271],"about_ca_topic_score_codex":0.09947887,"about_ca_topic_score_gemma":0.16802761,"teacher_disagreement_score":0.09947887,"about_ca_system_score_codex":0.0007993882,"about_ca_system_score_gemma":0.00065720314,"threshold_uncertainty_score":0.19779968},"labels":[],"label_agreement":null},{"id":"W2048977640","doi":"10.1029/2007gl030469","title":"Absence of geomagnetic conjugacy in pulsating auroras","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Conjugacy class; Earth's magnetic field; Conjugate points; Physics; Flux (metallurgy); Northern Hemisphere; Astrophysics; Magnetic field; Southern Hemisphere; Geophysics; Geodesy; Geology; Astronomy; Geometry; Mathematics; Chemistry","score_opus":0.01757661044415648,"score_gpt":0.3088103748843886,"score_spread":0.29123376444023213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2048977640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967384,0.00010577206,0.0005924587,0.0000148180025,0.0000040483937,0.0000061506216,0.00009150449,0.000008268297,0.0024386982],"genre_scores_gemma":[0.9994773,0.000048795755,0.00017121466,0.0000046626224,0.000006926923,0.0000028040251,0.00011458133,0.0000045180304,0.00016921043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974006,0.00004198804,0.000032699136,0.00007068963,0.00006672977,0.000047913636],"domain_scores_gemma":[0.99799937,0.0004752303,0.0008141079,0.00026105758,0.00028599196,0.00016422651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040483775,0.00014700207,0.00032397718,0.0011560257,0.00057323487,0.00096063205,0.00018871106,0.00019489229,0.0013766729],"category_scores_gemma":[0.0038230487,0.00017828846,0.00015467455,0.0011315413,0.00071314396,0.0004610735,0.0008601754,0.00024958493,0.0003013225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037874526,0.000032024556,0.93964,0.000043664313,0.000048075843,0.00033343316,0.0010718908,0.0003704896,0.03660107,0.00048790706,0.00007489619,0.020917768],"study_design_scores_gemma":[0.000005773405,0.000060017457,0.99636143,0.000004658164,0.000016124819,0.00032106118,0.00021573267,0.0002864731,0.0020880625,0.0001753068,0.0004603324,0.000005065429],"about_ca_topic_score_codex":0.0015619849,"about_ca_topic_score_gemma":0.0020241558,"teacher_disagreement_score":0.0015619849,"about_ca_system_score_codex":0.00022017055,"about_ca_system_score_gemma":0.00020557064,"threshold_uncertainty_score":0.004605353},"labels":[],"label_agreement":null},{"id":"W2049013926","doi":"10.1029/2004gl022013","title":"Improvements in the estimates of ice thickness and production in the Chukchi Sea polynyas derived from AMSR‐E","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Sea ice; Climatology; Remote sensing; Radiometer; Arctic; Arctic ice pack; Environmental science; Synthetic aperture radar; Pixel; Advanced very-high-resolution radiometer; Geology; Meteorology; Oceanography; Geography; Computer science; Satellite","score_opus":0.02244940521240937,"score_gpt":0.2764400367049265,"score_spread":0.25399063149251716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049013926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99067664,0.00041800225,0.004543943,0.00007525278,0.000012897385,0.00003433034,0.0018460386,0.00011153175,0.0022812397],"genre_scores_gemma":[0.98008955,0.00029973604,0.015868647,0.00003134335,0.00001315121,0.000038322258,0.0027469543,0.00003062712,0.00088166544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997087,0.00006452498,0.00003590904,0.00008806106,0.000063844804,0.000038881106],"domain_scores_gemma":[0.99926156,0.00012257177,0.00017329807,0.000113827606,0.00028518587,0.000043537828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067313376,0.0007589741,0.00018765118,0.0012578263,0.000434459,0.00059292914,0.00032031018,0.00018268058,0.0011078095],"category_scores_gemma":[0.0018839254,0.00042158694,0.00025468133,0.0012308159,0.0002497368,0.0006381281,0.00057803997,0.0002743283,0.00030418814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027335022,0.000078260004,0.88335836,0.000118056436,0.00023370159,0.00023024237,0.00042639486,0.01247865,0.036544412,0.00025167078,0.0006428535,0.065363966],"study_design_scores_gemma":[0.000012508514,0.000025118907,0.9856263,0.000010983689,0.000046350873,0.00008255659,0.00013059864,0.008236573,0.0039275517,0.000046240322,0.0018343364,0.000020841055],"about_ca_topic_score_codex":0.09230902,"about_ca_topic_score_gemma":0.22593576,"teacher_disagreement_score":0.09230902,"about_ca_system_score_codex":0.0008255745,"about_ca_system_score_gemma":0.0006377845,"threshold_uncertainty_score":0.18354344},"labels":[],"label_agreement":null},{"id":"W2049136717","doi":"10.1029/2001gl013778","title":"Multi‐station infrasonic observations of two large bolides: signal interpretation and implications for monitoring of atmospheric explosions","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Infrasound; Satellite; Atmosphere (unit); Energy (signal processing); Environmental science; Event (particle physics); Geology; SIGNAL (programming language); Meteorology; Remote sensing; Physics; Acoustics; Astronomy; Astrophysics","score_opus":0.08029429081958324,"score_gpt":0.33119036435064664,"score_spread":0.2508960735310634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049136717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99791795,0.00008583904,0.00079151854,0.00003765037,0.0000031791612,0.0000068649388,0.00023005917,0.000043385226,0.0008836712],"genre_scores_gemma":[0.99818283,0.000063092106,0.0010667844,0.000011291421,0.000011006349,0.000006152719,0.00044341042,0.000006179858,0.00020926626],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992704,0.000009303546,0.000004526128,0.000016347845,0.000022118847,0.000020556325],"domain_scores_gemma":[0.9995901,0.00007996078,0.00017293847,0.000030122783,0.000058362024,0.00006853687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015949893,0.0002443276,0.00016080934,0.00082397595,0.00019453229,0.0005087626,0.00027989672,0.00024854863,0.0007061892],"category_scores_gemma":[0.0006995415,0.00014727624,0.00009174903,0.00066546537,0.00015227837,0.00031795105,0.00055718765,0.00037432145,0.00011287894],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011913046,0.00017942682,0.8066451,0.00009714548,0.0000969514,0.0012904226,0.00063796446,0.0038644273,0.10502602,0.00021666674,0.0010299681,0.07972462],"study_design_scores_gemma":[0.000016236017,0.000081506594,0.99264467,0.000008754816,0.000024431116,0.00020933695,0.00020175424,0.0033553806,0.0027957081,0.0000563742,0.00059516256,0.000010568646],"about_ca_topic_score_codex":0.0030400367,"about_ca_topic_score_gemma":0.010156064,"teacher_disagreement_score":0.0030400367,"about_ca_system_score_codex":0.0002917214,"about_ca_system_score_gemma":0.00010206735,"threshold_uncertainty_score":0.006044686},"labels":[],"label_agreement":null},{"id":"W2049536551","doi":"10.1002/2014gl062349","title":"Switching predominance of organic versus inorganic carbon exports from an intermediate‐size subarctic watershed","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey","keywords":"Permafrost; Subarctic climate; Dissolved organic carbon; Total organic carbon; Watershed; Hydrology (agriculture); Tributary; Environmental science; Arctic; Geology; Environmental chemistry; Oceanography; Chemistry","score_opus":0.06998976273443307,"score_gpt":0.3051280882670595,"score_spread":0.23513832553262642,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2049536551","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998122,0.0000055157416,0.000012409886,0.0000023185196,1.219302e-7,4.0057498e-7,0.0000325522,0.0000014335035,0.00013309669],"genre_scores_gemma":[0.9997795,0.000010780701,0.00004359007,0.0000043496448,3.554757e-7,8.634044e-7,0.000092544746,0.000001017079,0.00006694282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993336,0.000007226104,0.000004470261,0.000028410388,0.0000066951106,0.000019848841],"domain_scores_gemma":[0.9997962,0.00004198592,0.000051870415,0.000014459057,0.000037051806,0.000058392434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001620387,0.00010438818,0.00014967905,0.00037450183,0.0002828597,0.00060912466,0.00016552093,0.000102243386,0.0006666499],"category_scores_gemma":[0.00027992047,0.00008034073,0.00010647912,0.00041494836,0.0002838766,0.00022051047,0.0002823704,0.000106856896,0.00006634246],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022728152,0.000027820553,0.96931946,0.000013043883,0.000035924546,0.0001340323,0.00031016854,0.00044050996,0.02555569,0.0001018829,0.00005826605,0.0037759624],"study_design_scores_gemma":[0.0000020057075,0.000014474022,0.99841344,0.0000013396874,0.00000782631,0.000024345412,0.00026209131,0.00038187395,0.00079924264,0.00001504265,0.0000765618,0.000001809012],"about_ca_topic_score_codex":0.022040183,"about_ca_topic_score_gemma":0.048711117,"teacher_disagreement_score":0.022040183,"about_ca_system_score_codex":0.0006444118,"about_ca_system_score_gemma":0.00035643522,"threshold_uncertainty_score":0.04382378},"labels":[],"label_agreement":null},{"id":"W2050240875","doi":"10.1002/2014gl062590","title":"Observation of polar cap patches and calculation of gradient drift instability growth times: A Swarm case study","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Calgary","funders":"Norges Forskningsråd","keywords":"Polar; Polar cap; Noon; Instability; Physics; Magnetosphere; Geodesy; Geophysics; Electrojet; Scintillation; Swarm behaviour; Geology; F region; Ionosphere; Atmospheric sciences; Plasma; Astronomy; Mechanics; Optics; Magnetic field; Computer science","score_opus":0.022137403370648776,"score_gpt":0.28414333259583646,"score_spread":0.2620059292251877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050240875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99533725,0.0000561289,0.0034822274,0.000011747587,0.000003871469,0.000016881006,0.00012362174,0.000044882352,0.00092329876],"genre_scores_gemma":[0.9974826,0.00002550932,0.0022787212,8.001913e-7,0.000002510968,0.0000035850662,0.00008756333,0.0000067961982,0.00011191875],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.000010621771,0.000004312837,0.000018333236,0.000017880422,0.000011210003],"domain_scores_gemma":[0.9994566,0.00027287644,0.000083297804,0.00004888711,0.00008763575,0.00005071891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022369751,0.00026023953,0.00018317645,0.0010545332,0.0002733855,0.0005076937,0.00022902165,0.00023110442,0.0005263148],"category_scores_gemma":[0.0009478777,0.00012583988,0.00029379802,0.00065328676,0.0001973782,0.00024721897,0.00025390257,0.0001818072,0.000073396295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009275607,0.00018073099,0.6468003,0.00024269987,0.0001734769,0.005772888,0.00092873443,0.22575851,0.05337171,0.0018506815,0.0011237033,0.062868915],"study_design_scores_gemma":[0.000024461435,0.00021197014,0.31266776,0.000018731693,0.000054171873,0.0008619155,0.00072653795,0.6697314,0.01402323,0.00052468316,0.0011208119,0.00003438038],"about_ca_topic_score_codex":0.007429635,"about_ca_topic_score_gemma":0.005860864,"teacher_disagreement_score":0.007429635,"about_ca_system_score_codex":0.00029623066,"about_ca_system_score_gemma":0.000114730574,"threshold_uncertainty_score":0.014772773},"labels":[],"label_agreement":null},{"id":"W2050321199","doi":"10.1029/2005gl022471","title":"Mixing estimates from a large‐scale hydrographic survey in the North Atlantic","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Hydrography; Geology; Mid-Atlantic Ridge; Hydrographic survey; Oceanography; Bathymetry; Mixing (physics); Ridge; Scale (ratio); Boundary current; Climatology; Ocean current; Geography; Cartography","score_opus":0.029626673255954247,"score_gpt":0.26949253243341814,"score_spread":0.2398658591774639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050321199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99832565,0.000064733635,0.00043988824,0.000016009975,0.000001279646,0.0000053796557,0.00061483437,0.00001386444,0.0005184633],"genre_scores_gemma":[0.9968803,0.00006882865,0.0012953962,0.000004437159,0.000002407661,0.0000069306757,0.0015623883,0.0000026556936,0.0001767308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999224,0.000012132423,0.000009934372,0.000021292211,0.000021637996,0.000012595334],"domain_scores_gemma":[0.9997497,0.000045067787,0.00007528412,0.00002074652,0.00007818067,0.000030982315],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022645899,0.0001345058,0.00010007793,0.0010732522,0.00021928792,0.00025820624,0.00008081568,0.00011308471,0.0004973993],"category_scores_gemma":[0.0005417993,0.00011849496,0.00017601524,0.0006003438,0.00007827261,0.0002238569,0.00026826304,0.00011006595,0.00012770132],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000995796,0.000023640321,0.95958966,0.000020163216,0.000046097623,0.000052797583,0.00031983995,0.0013919382,0.015496614,0.00009321171,0.00032967824,0.02253677],"study_design_scores_gemma":[0.000003611404,0.000012599968,0.9978872,0.0000031697994,0.000008421146,0.000017772461,0.00008231379,0.0011311958,0.0005201037,0.000015542197,0.0003146806,0.0000035218768],"about_ca_topic_score_codex":0.044576593,"about_ca_topic_score_gemma":0.10277475,"teacher_disagreement_score":0.044576593,"about_ca_system_score_codex":0.0004746056,"about_ca_system_score_gemma":0.00027766803,"threshold_uncertainty_score":0.08863425},"labels":[],"label_agreement":null},{"id":"W2050355831","doi":"10.1029/2006gl026619","title":"Transient creep, aseismic damage and slow failure in Carrara marble deformed across the brittle‐ductile transition","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Brittleness; Creep; Differential stress; Materials science; Cataclastic rock; Coalescence (physics); Overburden pressure; Acoustic emission; Composite material; Dislocation creep; Stress (linguistics); Deformation (meteorology); Geology; Geotechnical engineering; Seismology; Fault (geology)","score_opus":0.013980587860768353,"score_gpt":0.2568126704906531,"score_spread":0.24283208262988473,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050355831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996499,0.000054824155,0.00016351508,0.0000054668544,0.00000114422,0.000002752569,0.00002412356,0.0000057494217,0.00009252384],"genre_scores_gemma":[0.9994217,0.000029244835,0.00019998678,0.000002355189,0.0000012743345,0.0000045536294,0.000049498263,0.0000029434163,0.00028842816],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99984205,0.000017774193,0.000008878334,0.00003496245,0.00005310236,0.000043194774],"domain_scores_gemma":[0.99963033,0.0000981858,0.000085083506,0.000045830082,0.00006569178,0.00007492884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020936342,0.00030470043,0.00025762885,0.00053415593,0.00035222145,0.00024814915,0.0003100939,0.00046579633,0.0012935201],"category_scores_gemma":[0.0004256658,0.00019357514,0.00019008789,0.0002791529,0.00042624385,0.00031377378,0.00019305536,0.00032761553,0.00016636842],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028612785,0.000031853622,0.0023447461,0.00002153645,0.000006982673,0.00044059372,0.00012898735,0.00048285988,0.994726,0.00003673206,0.00001745794,0.0014761651],"study_design_scores_gemma":[0.000020033905,0.0017132878,0.08372432,0.0000061827795,0.000020851227,0.00064243696,0.00021224524,0.004804079,0.9082844,0.00006136177,0.00048519543,0.0000255269],"about_ca_topic_score_codex":0.002024359,"about_ca_topic_score_gemma":0.0022357267,"teacher_disagreement_score":0.002024359,"about_ca_system_score_codex":0.00020908375,"about_ca_system_score_gemma":0.00007867896,"threshold_uncertainty_score":0.0043272376},"labels":[],"label_agreement":null},{"id":"W2050369487","doi":"10.1029/2004gl022281","title":"Thermohaline circulation at three key sections in the North Atlantic over 1985–2002","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council","keywords":"Thermohaline circulation; Subtropics; Climatology; Hydrography; Context (archaeology); Shutdown of thermohaline circulation; Oceanography; Latitude; Geology; Ocean current; North Atlantic Deep Water","score_opus":0.029898413819061234,"score_gpt":0.26420395658715856,"score_spread":0.23430554276809734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050369487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987256,0.00003515974,0.00007839414,0.000043782635,0.0000023601947,0.0000025327402,0.00064552797,0.000015407308,0.00045119986],"genre_scores_gemma":[0.99862635,0.000029112385,0.00010004907,0.000012211123,0.0000023006799,0.0000023310004,0.0009736713,0.0000017002486,0.00025234718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999397,0.000007450415,0.000004421194,0.000022313112,0.000012804535,0.000013407078],"domain_scores_gemma":[0.9999063,0.000009585197,0.00003259516,0.0000102019785,0.00002062032,0.000020738631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012856245,0.00016578045,0.00014050557,0.00027342694,0.00033326002,0.00043732795,0.00023803461,0.0002905642,0.0006471475],"category_scores_gemma":[0.00036593768,0.00014474611,0.00027859057,0.0003546192,0.00014408761,0.00022669727,0.0002948025,0.00019141231,0.00009849345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041419503,0.00010892419,0.9535431,0.000036546953,0.00018459898,0.00027997603,0.00036224056,0.028662873,0.005441976,0.00030100672,0.0012832154,0.009381332],"study_design_scores_gemma":[0.0000166762,0.000026678092,0.9822887,0.000005024621,0.000030479167,0.000040795396,0.00008737196,0.016211858,0.00048816335,0.000043342152,0.0007543936,0.000006501586],"about_ca_topic_score_codex":0.12058999,"about_ca_topic_score_gemma":0.2255482,"teacher_disagreement_score":0.12058999,"about_ca_system_score_codex":0.001418316,"about_ca_system_score_gemma":0.00042530277,"threshold_uncertainty_score":0.23977613},"labels":[],"label_agreement":null},{"id":"W2050597575","doi":"10.1029/2004gl020063","title":"Variability in Arctic sea ice drift","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research; National Oceanic and Atmospheric Administration","keywords":"Sea ice; Arctic ice pack; Drift ice; Geology; Antarctic sea ice; Fast ice; Arctic; Oceanography; Arctic sea ice decline; Ocean gyre; Climatology; Canada Basin; Subtropics","score_opus":0.020870305416890063,"score_gpt":0.2725060876778616,"score_spread":0.25163578226097155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050597575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99678,0.00029328043,0.0001521001,0.000036225265,0.00001055648,0.000002597825,0.0012282586,0.0000070291544,0.0014899153],"genre_scores_gemma":[0.9961216,0.00022862064,0.000132826,0.000014102321,0.00001778791,0.000005570397,0.003099506,0.0000043701034,0.0003756393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996879,0.000040312916,0.000035726778,0.00011026757,0.00007671489,0.00004904142],"domain_scores_gemma":[0.99919313,0.0001666641,0.00020081185,0.00005147178,0.00030816786,0.00007973542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007205396,0.0001383307,0.00018681888,0.0011354289,0.0002748658,0.000590483,0.00019248592,0.00021188273,0.0005146943],"category_scores_gemma":[0.0012171796,0.000080243495,0.00018155809,0.0011944876,0.00012898019,0.00028942537,0.00027107808,0.00020945969,0.00020552949],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013407171,0.000026341186,0.9828188,0.000022787137,0.000142939,0.000109686516,0.00047848144,0.00069609674,0.0014833432,0.00023104533,0.00067364244,0.013182696],"study_design_scores_gemma":[0.0000017047154,0.000012946282,0.9973236,0.0000073290203,0.000010574452,0.00008679964,0.00010978606,0.00041783342,0.00019870588,0.000023827326,0.0018035339,0.0000034000127],"about_ca_topic_score_codex":0.01732897,"about_ca_topic_score_gemma":0.021523902,"teacher_disagreement_score":0.01732897,"about_ca_system_score_codex":0.0005478598,"about_ca_system_score_gemma":0.0002682119,"threshold_uncertainty_score":0.034456253},"labels":[],"label_agreement":null},{"id":"W2050738249","doi":"10.1029/2004gl021494","title":"A nonlinear expression of the North Atlantic Oscillation in the North Pacific","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; University of East Anglia","keywords":"Nonlinear system; Climatology; North Atlantic oscillation; Geology; Amplitude; Oscillation (cell signaling); Expression (computer science); Pacific decadal oscillation; Forcing (mathematics); Sign (mathematics); Jet stream; Mode (computer interface); Jet (fluid); El Niño Southern Oscillation; Physics; Biology; Mathematics; Computer science; Mechanics; Mathematical analysis","score_opus":0.035090952716310964,"score_gpt":0.2866992742321301,"score_spread":0.25160832151581913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050738249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.62849015,0.001045602,0.32008097,0.0020549002,0.0001659952,0.000041313957,0.00032014574,0.00027144307,0.04752945],"genre_scores_gemma":[0.96419793,0.0008674611,0.022278797,0.000096746946,0.00011035232,0.00002094116,0.00011994715,0.00007605264,0.012231727],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999274,0.000016177222,0.0000029376208,0.000018737364,0.00002774765,0.0000069839957],"domain_scores_gemma":[0.9998431,0.000046877067,0.000045138924,0.000015731768,0.000042113326,0.000006956281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001762102,0.00022045853,0.00007512854,0.000108264285,0.00017382618,0.00030247844,0.00018271506,0.00017820655,0.0010729469],"category_scores_gemma":[0.0010253994,0.00010419445,0.00017912069,0.0001578707,0.0004448042,0.00034136404,0.000251302,0.00043097162,0.00016798846],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013166017,0.00005554279,0.024830101,0.00026524972,0.000090384536,0.0012830322,0.0010338665,0.3689941,0.207973,0.26993543,0.0038662944,0.12154132],"study_design_scores_gemma":[0.0000080396185,0.000030972515,0.020773133,0.000015919279,0.000021175714,0.00023852145,0.00007919034,0.9423003,0.0058596977,0.025555424,0.005088285,0.00002931541],"about_ca_topic_score_codex":0.005738256,"about_ca_topic_score_gemma":0.0058804913,"teacher_disagreement_score":0.005738256,"about_ca_system_score_codex":0.0002704887,"about_ca_system_score_gemma":0.00031010158,"threshold_uncertainty_score":0.0114097},"labels":[],"label_agreement":null},{"id":"W2050757789","doi":"10.1029/2005gl024254","title":"The third Arctic climate pattern: 1930s and early 2000s","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Joint Institute for the Study of the Atmosphere and Ocean","keywords":"Arctic; Climatology; Arctic oscillation; Arctic dipole anomaly; Oceanography; Bay; Geology; Period (music); Siberian High; Arctic ecology; Arctic ice pack; The arctic; Geography; East Asia; Drift ice","score_opus":0.01785789112140642,"score_gpt":0.2615693469993841,"score_spread":0.24371145587797768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2050757789","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9617945,0.0022110397,0.00068388454,0.0014761738,0.00018714613,0.000026416548,0.0065006125,0.0000780607,0.027042232],"genre_scores_gemma":[0.99323165,0.0009241387,0.00046195765,0.00022607707,0.00006966583,0.000018616049,0.0023908087,0.000016690597,0.0026604193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998431,0.00000809186,0.000012749139,0.000046775698,0.00004212803,0.000047111014],"domain_scores_gemma":[0.9995554,0.000015557094,0.0001312802,0.000026238544,0.0002003589,0.00007115432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000346298,0.00023979704,0.00018828707,0.0011199047,0.0006822499,0.00097314967,0.00023508785,0.00027387595,0.0017469525],"category_scores_gemma":[0.000714544,0.00010289449,0.00022995574,0.001361516,0.00035262614,0.00034260293,0.0005639868,0.00036962802,0.00035685714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041809664,0.0000733498,0.89298016,0.00025351273,0.00018526918,0.00037855946,0.002694336,0.0012602678,0.004711233,0.0055002025,0.010042554,0.08150261],"study_design_scores_gemma":[0.0000062255167,0.00002027391,0.9827765,0.00004462092,0.0000145778,0.000093440074,0.0003109179,0.00023646484,0.00042468045,0.00020812776,0.015857387,0.000006761693],"about_ca_topic_score_codex":0.15047824,"about_ca_topic_score_gemma":0.19960278,"teacher_disagreement_score":0.15047824,"about_ca_system_score_codex":0.0018811461,"about_ca_system_score_gemma":0.0012227998,"threshold_uncertainty_score":0.2992047},"labels":[],"label_agreement":null},{"id":"W2051114812","doi":"10.1029/2007gl032699","title":"Vertical propagation of information in a middle atmosphere data assimilation system by gravity‐wave drag feedbacks","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Canadian Space Agency; Scheme for Promotion of Academic and Research Collaboration; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Mesosphere; Gravity wave; Orographic lift; Atmosphere (unit); Atmospheric sciences; Geology; Drag; Thermosphere; Wave drag; Atmospheric model; Geophysics; Stratosphere; Gravitational wave; Meteorology; Physics; Drag coefficient; Ionosphere; Mechanics; Oceanography","score_opus":0.03353683199344517,"score_gpt":0.2701688544995051,"score_spread":0.23663202250605994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051114812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9740448,0.00016905362,0.023003008,0.00023271778,0.00005709563,0.00002697058,0.00065388554,0.0006828948,0.001129593],"genre_scores_gemma":[0.9895564,0.000033277043,0.009478093,0.000021276597,0.000010718694,0.000011087128,0.00058416254,0.0000263544,0.00027857878],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997546,0.00004171414,0.000021437403,0.00007002085,0.00006417898,0.000047929367],"domain_scores_gemma":[0.99963176,0.00008067648,0.000042877,0.000081680584,0.0001237191,0.000039257768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008475504,0.00036700026,0.00038373013,0.00035236924,0.0005945567,0.0010452663,0.00043813977,0.00035744824,0.0005177603],"category_scores_gemma":[0.0018820937,0.00037391233,0.00041275818,0.00058663485,0.0003326956,0.00080173864,0.00061250996,0.0005783759,0.00012046639],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00092073367,0.0002508843,0.10810641,0.000054284006,0.0004965991,0.00016760245,0.0004609593,0.7275125,0.04723042,0.004981944,0.0023787164,0.10743902],"study_design_scores_gemma":[0.000042139396,0.00004741548,0.028566515,0.0000040712953,0.000042694795,0.000009472285,0.000027590211,0.9647149,0.0049119364,0.00063405524,0.0009725583,0.000026658267],"about_ca_topic_score_codex":0.16997495,"about_ca_topic_score_gemma":0.12540846,"teacher_disagreement_score":0.16997495,"about_ca_system_score_codex":0.0011307131,"about_ca_system_score_gemma":0.0015945269,"threshold_uncertainty_score":0.33797115},"labels":[],"label_agreement":null},{"id":"W2051518395","doi":"10.1029/2003gl018471","title":"The role of the western Pacific in decadal variability","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Equator; Pacific decadal oscillation; Climatology; Forcing (mathematics); Western Hemisphere Warm Pool; Ocean heat content; Geology; Oceanography; Pacific ocean; Sea surface temperature; Environmental science; Latitude","score_opus":0.021946161881001736,"score_gpt":0.28768180013374134,"score_spread":0.2657356382527396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051518395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9751369,0.0030292335,0.0026774774,0.0009461847,0.000041191164,0.0000055146656,0.0005781879,0.00010133543,0.017483998],"genre_scores_gemma":[0.99895597,0.0003693142,0.00019299444,0.00003458415,0.0000116143265,0.0000023761459,0.000072545045,0.000011034694,0.0003495213],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992955,0.000019700126,0.000005830353,0.000020502383,0.000012416563,0.000011974202],"domain_scores_gemma":[0.9994987,0.00015828403,0.00013799038,0.000053918746,0.000092793394,0.000058293394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003684454,0.000097009615,0.00010945451,0.00042810966,0.00033351558,0.0011450922,0.00014325304,0.00012587517,0.0011810265],"category_scores_gemma":[0.0019267347,0.00010583944,0.000088648245,0.0007334072,0.00033324034,0.00054656656,0.0004806455,0.0002362171,0.00009153694],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034941992,0.000051246567,0.84795725,0.00013914236,0.0002398032,0.00036103328,0.0014979669,0.013673983,0.009851885,0.026140256,0.0025632498,0.09717469],"study_design_scores_gemma":[0.000013711944,0.000022954733,0.9596114,0.000062395826,0.00008970136,0.0001422901,0.00056446454,0.015297823,0.0006240002,0.013669316,0.009882152,0.000019799449],"about_ca_topic_score_codex":0.0110246865,"about_ca_topic_score_gemma":0.010744266,"teacher_disagreement_score":0.0110246865,"about_ca_system_score_codex":0.00028145866,"about_ca_system_score_gemma":0.00030998807,"threshold_uncertainty_score":0.021921039},"labels":[],"label_agreement":null},{"id":"W2051608494","doi":"10.1029/2006gl027070","title":"Land water storage within the Congo Basin inferred from GRACE satellite gravity data","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":183,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Water storage; Surface runoff; Evapotranspiration; Precipitation; Water balance; Structural basin; Hydrology (agriculture); Water year; Environmental science; Climatology; Drainage basin; Satellite; Surface water; Geology; Atmospheric sciences; Geography; Meteorology; Geomorphology","score_opus":0.06884183336887441,"score_gpt":0.2869510261145355,"score_spread":0.2181091927456611,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051608494","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99333256,0.000095665964,0.0004149756,0.000057815432,0.0000014218397,0.000003788529,0.0051514907,0.00004867415,0.0008936245],"genre_scores_gemma":[0.9972561,0.0000785328,0.00029172076,0.0000054413986,0.0000025272586,0.0000063765574,0.0022133223,0.000008408807,0.00013759178],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999019,0.000015407239,0.000011565521,0.000024476809,0.000019794097,0.00002687598],"domain_scores_gemma":[0.9996296,0.000056971945,0.00014866194,0.000060298677,0.00007329448,0.000031134918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019865738,0.00023867503,0.00019936459,0.001322909,0.0002941405,0.0005990055,0.00020277532,0.00012716981,0.0010175068],"category_scores_gemma":[0.0009789626,0.00014331508,0.000182098,0.0019230455,0.00023550357,0.00076779636,0.00040997294,0.00014231524,0.00018942406],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029170324,0.000044867404,0.9341376,0.00006834484,0.0001771706,0.00030581668,0.0005602967,0.026015447,0.012193789,0.0011323567,0.0015426937,0.023530085],"study_design_scores_gemma":[0.000015712802,0.000024348417,0.95677584,0.000021115533,0.000056634126,0.0000803732,0.00018782202,0.03594037,0.004628309,0.0002596558,0.0019822053,0.000027610851],"about_ca_topic_score_codex":0.08193788,"about_ca_topic_score_gemma":0.095792115,"teacher_disagreement_score":0.08193788,"about_ca_system_score_codex":0.0012673036,"about_ca_system_score_gemma":0.00042621882,"threshold_uncertainty_score":0.1629219},"labels":[],"label_agreement":null},{"id":"W2051989512","doi":"10.1029/2004gl020044","title":"Detection of volcanic influence on global precipitation","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Precipitation; Climatology; Shortwave; Volcano; Longwave; Environmental science; Atmospheric sciences; Climate model; Vulcanian eruption; Climate change; Geology; Meteorology; Radiative transfer; Geography","score_opus":0.027843014518589306,"score_gpt":0.31285741719099247,"score_spread":0.2850144026724032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2051989512","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984395,0.00009259697,0.00019371556,0.000046774938,0.0000030711153,0.000001065247,0.00012750665,0.000012314302,0.0010834205],"genre_scores_gemma":[0.9997106,0.00004188822,0.000050387724,0.00000682033,0.0000073111464,5.053069e-7,0.00013045286,0.0000016075597,0.00005048652],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981683,0.00004334533,0.000011962557,0.000055362016,0.000041882802,0.000030739757],"domain_scores_gemma":[0.99856573,0.0005266619,0.000445443,0.00014137714,0.0001964325,0.00012439622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004627575,0.000113698545,0.000173518,0.0005168937,0.00012631368,0.00042466895,0.0001237751,0.00020137383,0.0005060348],"category_scores_gemma":[0.002135958,0.00011031329,0.00020134906,0.00038763758,0.00027472118,0.00024668424,0.000492528,0.00027930783,0.000051992312],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021745413,0.000022268148,0.96969706,0.000031536856,0.0001183154,0.00011700815,0.0002031844,0.002361896,0.013729325,0.00037444895,0.00015771168,0.012969719],"study_design_scores_gemma":[0.0000051610778,0.000027814685,0.9969881,0.0000024528506,0.00001832127,0.000052693926,0.00003406104,0.0017729572,0.000801523,0.000070803566,0.00022301917,0.00000308222],"about_ca_topic_score_codex":0.0034194542,"about_ca_topic_score_gemma":0.0048821517,"teacher_disagreement_score":0.0034194542,"about_ca_system_score_codex":0.00024386003,"about_ca_system_score_gemma":0.00019913357,"threshold_uncertainty_score":0.006799102},"labels":[],"label_agreement":null},{"id":"W2052139900","doi":"10.1029/2007gl029859","title":"Anthropogenic speed‐up of oceanic planetary waves","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Environmental science; Climate change; Climatology; Latitude; Global warming; Atmospheric sciences; Climate model; Geology; Oceanography; Geodesy","score_opus":0.047539040096072835,"score_gpt":0.3248105719307131,"score_spread":0.27727153183464026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052139900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949538,0.00008791051,0.0012789202,0.00016191576,0.000022574766,0.000004674289,0.0008966405,0.00007434191,0.002519213],"genre_scores_gemma":[0.9985776,0.00009341985,0.00028848866,0.000011967048,0.0000074903164,0.000004098534,0.0008430002,0.000008748285,0.00016524049],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984217,0.00004137104,0.000012997506,0.00003839838,0.000036387388,0.000028752722],"domain_scores_gemma":[0.99940956,0.00020573579,0.0001312056,0.00010475038,0.000112495494,0.000036282574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039845952,0.00029279134,0.00015060531,0.00028787873,0.00022939798,0.0006587948,0.0002795623,0.00024564358,0.0015198144],"category_scores_gemma":[0.0018014739,0.00018471798,0.00044463208,0.0005382536,0.00023129376,0.0005162201,0.00047917478,0.00043529808,0.00014292721],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034336603,0.00013421987,0.32315537,0.00011690743,0.00034578427,0.00014742294,0.00010710252,0.6420832,0.0057518207,0.0065439185,0.0023086232,0.018962275],"study_design_scores_gemma":[0.00014508239,0.00030919374,0.35561904,0.00002480456,0.0001941445,0.00015634771,0.00015123145,0.6183935,0.012554418,0.0049856175,0.007384406,0.00008221864],"about_ca_topic_score_codex":0.005655635,"about_ca_topic_score_gemma":0.0063185995,"teacher_disagreement_score":0.005655635,"about_ca_system_score_codex":0.00036739986,"about_ca_system_score_gemma":0.00031370076,"threshold_uncertainty_score":0.0112454295},"labels":[],"label_agreement":null},{"id":"W2052497313","doi":"10.1029/1999gl010481","title":"Shear velocities in Cascadia from seafloor compliance measurements","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Seafloor spreading; Gravimeter; Shear (geology); Seismology; Sediment; Geodesy; Geophysics; Geomorphology; Petrology","score_opus":0.10564928177573887,"score_gpt":0.3121685758626159,"score_spread":0.20651929408687705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052497313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99419147,0.000051414718,0.00042925702,0.000024886538,0.0000070986653,0.0000066895354,0.0012191103,0.00013006256,0.003940023],"genre_scores_gemma":[0.9964941,0.00004386633,0.00059421454,0.00000837071,0.0000028346915,0.000011849394,0.001927274,0.000022884673,0.00089461973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974126,0.000018727678,0.000018102133,0.00011397058,0.000078818055,0.00002918739],"domain_scores_gemma":[0.999476,0.0000368572,0.00010284918,0.00005997504,0.00025174406,0.00007253866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021135792,0.0005651173,0.00024297278,0.0016258407,0.00045797924,0.00047642982,0.0003125741,0.00023601673,0.0017054252],"category_scores_gemma":[0.001169713,0.00030279957,0.00019216501,0.0017860001,0.00031232537,0.00020672403,0.0005434311,0.00025774038,0.00073194236],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034897964,0.000060001217,0.9278472,0.0000918952,0.000112177884,0.00039225817,0.0019980343,0.0044541736,0.04098246,0.00033599042,0.0016921394,0.021684654],"study_design_scores_gemma":[0.000007700247,0.000026603358,0.99630225,0.0000067407605,0.0000111723375,0.00004045552,0.00015986864,0.0008344855,0.0012766385,0.00004369298,0.0012807018,0.000009695981],"about_ca_topic_score_codex":0.076247275,"about_ca_topic_score_gemma":0.1329846,"teacher_disagreement_score":0.076247275,"about_ca_system_score_codex":0.0009490413,"about_ca_system_score_gemma":0.0004502879,"threshold_uncertainty_score":0.15160692},"labels":[],"label_agreement":null},{"id":"W2052666772","doi":"10.1029/2009gl041476","title":"Equatorward moving auroral signatures of a flow burst observed prior to auroral onset","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Canadian Space Agency; University of Alberta; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Substorm; Arc (geometry); Geophysics; Sky; Physics; Geology; Astrophysics; Wedge (geometry); Magnetosphere; Magnetic field; Optics; Geometry","score_opus":0.027816580883204843,"score_gpt":0.29871923162723685,"score_spread":0.270902650744032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052666772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99683553,0.0000957779,0.00040021935,0.000029752782,0.000008422803,0.0000070882816,0.00021339381,0.00005989668,0.002349909],"genre_scores_gemma":[0.99858,0.00006687405,0.0005215457,0.000020350355,0.000024034991,0.0000061576798,0.00036885755,0.000011516388,0.00040068236],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999962,0.0000019365732,0.0000013766925,0.000009143368,0.0000104338515,0.000015003054],"domain_scores_gemma":[0.99985206,0.000016073618,0.0000442166,0.000011382195,0.000033493016,0.000042757078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000066968685,0.00012020867,0.00015956177,0.0004789513,0.00029426417,0.00027592367,0.000134389,0.0002480368,0.0009418148],"category_scores_gemma":[0.00022641322,0.00011506815,0.00010008767,0.00022838383,0.00014928165,0.00018808396,0.00028383735,0.00037450826,0.00017706226],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010655606,0.00016762126,0.31201243,0.0001188929,0.00007340463,0.0020838047,0.0013738441,0.0006107881,0.65043837,0.00048843154,0.0021608965,0.029405994],"study_design_scores_gemma":[0.000012878239,0.00008101197,0.9898553,0.0000105618365,0.000015952355,0.0003140765,0.000109025794,0.0007390867,0.0075100316,0.00004016856,0.0013048275,0.0000070620313],"about_ca_topic_score_codex":0.0037788637,"about_ca_topic_score_gemma":0.008487671,"teacher_disagreement_score":0.0037788637,"about_ca_system_score_codex":0.00021528908,"about_ca_system_score_gemma":0.0000974332,"threshold_uncertainty_score":0.0075137615},"labels":[],"label_agreement":null},{"id":"W2052792497","doi":"10.1029/1999gl003731","title":"Quasi‐periodic ionospheric disturbances with a 40‐min period during prolonged northward interplanetary magnetic field","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Augsburg University; National Science Foundation","keywords":"Ionosphere; Geophysics; Electrojet; Interplanetary magnetic field; Magnetometer; Equatorial electrojet; Physics; Magnetosphere; Solar wind; Interplanetary spaceflight; Geology; Magnetic field; Atmospheric sciences; Earth's magnetic field","score_opus":0.006729828510643139,"score_gpt":0.2369150580808369,"score_spread":0.23018522957019377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2052792497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909437,0.000115359704,0.00021782634,0.0000138194155,0.0000035880796,0.0000036103977,0.00006458023,0.000016669046,0.00047015885],"genre_scores_gemma":[0.9994937,0.000065444074,0.00013114962,0.000010035638,0.0000069201105,0.0000035215974,0.00013426485,0.000002079925,0.00015270629],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999622,0.000003083597,0.000002556638,0.000008988824,0.000009801034,0.00001339087],"domain_scores_gemma":[0.99982184,0.000015876,0.00010215891,0.000012961334,0.00001664284,0.000030532785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000069911686,0.000113399474,0.00011721225,0.00031647703,0.00018195428,0.00016203964,0.00008295296,0.00015398879,0.0007185161],"category_scores_gemma":[0.0002252069,0.00008245178,0.000072506686,0.00023748128,0.00017973762,0.000116469346,0.00021805112,0.00011609235,0.000121047204],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012887582,0.00010973391,0.44925842,0.00015631146,0.00013397164,0.0016213129,0.0013974671,0.0012688978,0.5119573,0.0003860608,0.00085388473,0.031567838],"study_design_scores_gemma":[0.0000075056637,0.00008428626,0.9951982,0.0000047780795,0.000011668039,0.00027493367,0.00011454331,0.00026967254,0.0033309283,0.000059635593,0.0006393171,0.0000046781356],"about_ca_topic_score_codex":0.001360534,"about_ca_topic_score_gemma":0.0025202383,"teacher_disagreement_score":0.001360534,"about_ca_system_score_codex":0.00017166465,"about_ca_system_score_gemma":0.00007607411,"threshold_uncertainty_score":0.0027052164},"labels":[],"label_agreement":null},{"id":"W2053063646","doi":"10.1002/2014gl062634","title":"Anomalous winter winds decrease 2014 transition zone productivity in the NE Pacific","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and fisheries research","field":"Environmental Science","cited_by":153,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Subarctic climate; Oceanography; North Pacific High; Productivity; Environmental science; Subtropics; Biomass (ecology); Nutrient; Phytoplankton; Geography; Geology; Fishery; Pacific ocean; Pacific decadal oscillation; Ecology; Biology","score_opus":0.03296715709992283,"score_gpt":0.28715590495196996,"score_spread":0.25418874785204715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053063646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993666,0.000040164017,0.000017496064,0.00003357519,0.0000036362294,0.0000015314521,0.00019211647,0.0000031411166,0.0003418144],"genre_scores_gemma":[0.99951935,0.000048086324,0.000023975468,0.000014018469,0.0000033645,0.000002034949,0.00024052955,9.874175e-7,0.00014768273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999225,0.000008863405,0.000007968126,0.000019300318,0.000014988317,0.000026347547],"domain_scores_gemma":[0.9995466,0.000031680553,0.00018550656,0.00002500885,0.000086324035,0.00012487374],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016739462,0.00013149892,0.00009800422,0.00043450994,0.0003576158,0.00057291804,0.00016475709,0.00017916391,0.0011775773],"category_scores_gemma":[0.00054850744,0.00008988807,0.0001826184,0.00042122323,0.00019844116,0.00027099412,0.00039363618,0.0002618371,0.00009584323],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009821499,0.000024062605,0.99601775,0.000008595002,0.000044069093,0.00010076565,0.00014199936,0.0001180069,0.0011376196,0.000032729633,0.0002276233,0.0020485327],"study_design_scores_gemma":[0.0000010581102,0.000007890442,0.999582,0.0000019292668,0.0000028362715,0.00001610192,0.00015392154,0.00007618848,0.00004276265,0.0000056281815,0.000108970016,6.541578e-7],"about_ca_topic_score_codex":0.06472709,"about_ca_topic_score_gemma":0.10025149,"teacher_disagreement_score":0.06472709,"about_ca_system_score_codex":0.00055384764,"about_ca_system_score_gemma":0.00040928664,"threshold_uncertainty_score":0.12870067},"labels":[],"label_agreement":null},{"id":"W2053066861","doi":"10.1029/2003gl018853","title":"Trends in atmospheric haze induced by peat fires in Sumatra Island, Indonesia and El Niño phenomenon from 1973 to 2003","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Forest Service","funders":"","keywords":"Haze; Visibility; Peat; El Niño Southern Oscillation; Environmental science; Climatology; Air quality index; Southern oscillation; Atmospheric sciences; Biomass burning; Meteorology; Geology; Geography; Aerosol","score_opus":0.013343209736881287,"score_gpt":0.2712719045511975,"score_spread":0.2579286948143162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053066861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995437,0.00005565871,0.000022112708,0.000018568117,0.0000031656525,0.0000013632269,0.00021754805,0.0000024561803,0.00013532273],"genre_scores_gemma":[0.99930894,0.00006369742,0.000035812278,0.000009190453,0.0000058321216,0.0000028395611,0.00044412535,0.0000010656746,0.00012836936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999163,0.00000942629,0.000014213157,0.000018718476,0.000019155885,0.000022165781],"domain_scores_gemma":[0.99924684,0.00008583375,0.00043376783,0.000021803053,0.00010348907,0.0001083419],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022575662,0.00016953632,0.00015153846,0.00050628785,0.00016120651,0.00040962698,0.0001609583,0.00021879023,0.00042275203],"category_scores_gemma":[0.0005571664,0.00011420751,0.00019798552,0.00053940533,0.00019752806,0.00021477693,0.0002520579,0.00034778417,0.00010119283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014640726,0.000041374034,0.99498993,0.000016278305,0.00005888208,0.0001764754,0.00017823717,0.00023125071,0.0021289017,0.0000140363345,0.00011817846,0.0019000364],"study_design_scores_gemma":[8.547963e-7,0.000012643453,0.9995042,0.0000014471364,0.000007858702,0.000064224194,0.000077717355,0.00012219755,0.0001375939,0.0000036128295,0.000066266606,0.0000013887251],"about_ca_topic_score_codex":0.0147768445,"about_ca_topic_score_gemma":0.030095821,"teacher_disagreement_score":0.0147768445,"about_ca_system_score_codex":0.00044010297,"about_ca_system_score_gemma":0.00019703186,"threshold_uncertainty_score":0.029381692},"labels":[],"label_agreement":null},{"id":"W2053332298","doi":"10.1029/2009gl038068","title":"Does sedimentary <sup>231</sup>Pa/<sup>230</sup>Th from the Bermuda Rise monitor past Atlantic Meridional Overturning Circulation?","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institute of Particle Physics","funders":"Deutsche Forschungsgemeinschaft","keywords":"Oceanography; Geology; Thermohaline circulation; Ocean current; Shutdown of thermohaline circulation; North Atlantic Deep Water; Zonal and meridional; Climatology","score_opus":0.020069851629106072,"score_gpt":0.27306294055261204,"score_spread":0.25299308892350597,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053332298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99662304,0.00042283963,0.00021510758,0.00018160854,0.000013650692,0.0000036761194,0.00044757896,0.000018783741,0.0020735986],"genre_scores_gemma":[0.999057,0.00018389754,0.00013796597,0.00004347221,0.000015230912,0.0000018486676,0.000261053,0.0000058775863,0.00029363576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999931,0.000011192325,0.000006491857,0.00002052479,0.000011593819,0.000019266863],"domain_scores_gemma":[0.99958676,0.00004908699,0.0001746265,0.00003224962,0.00010543832,0.000051844516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022730826,0.00023966882,0.00022509697,0.0003358989,0.00024181863,0.0007617885,0.00023841074,0.00033922936,0.0012099596],"category_scores_gemma":[0.0007773219,0.00013222429,0.00010026898,0.00052310014,0.0004588471,0.00056036457,0.00023742896,0.00025187363,0.0005927418],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000069492184,0.0000069753355,0.98462766,0.000020452595,0.000032962213,0.000042012372,0.00009670843,0.00016358573,0.008661949,0.000049567203,0.00016517029,0.006063514],"study_design_scores_gemma":[6.52778e-7,0.000007759035,0.9992398,0.00000242794,0.0000038061119,0.000014612404,0.00005840097,0.00011958124,0.00034841182,0.00001823743,0.00018509572,0.0000012374065],"about_ca_topic_score_codex":0.02364399,"about_ca_topic_score_gemma":0.054076582,"teacher_disagreement_score":0.02364399,"about_ca_system_score_codex":0.0005618347,"about_ca_system_score_gemma":0.00021440291,"threshold_uncertainty_score":0.047012746},"labels":[],"label_agreement":null},{"id":"W2053358409","doi":"10.1029/2001gl013812","title":"methyl bromide loss rate constants in the north Pacific Ocean","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Seawater; Reaction rate constant; Bromide; Subtropics; Degradation (telecommunications); Environmental chemistry; Surface water; Chemistry; Oceanography; Environmental science; Geology; Kinetics; Ecology; Biology; Inorganic chemistry; Environmental engineering","score_opus":0.03437180418730689,"score_gpt":0.27162863652065056,"score_spread":0.23725683233334366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053358409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945081,0.001447879,0.0017485295,0.000055371493,0.000004054093,0.000016364598,0.0008473172,0.00003699959,0.0013354212],"genre_scores_gemma":[0.99214184,0.001665038,0.0015032097,0.000042101605,0.0000038475227,0.00004608878,0.0023150588,0.000027637197,0.0022551576],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998115,0.000013660998,0.000013379725,0.0000557672,0.00007925474,0.000026544787],"domain_scores_gemma":[0.99932003,0.000174793,0.00024330587,0.00003994385,0.00018862984,0.00003335868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005417593,0.00032024973,0.00020647266,0.00041926003,0.00017316909,0.00037244076,0.00026857757,0.00027393262,0.00067666394],"category_scores_gemma":[0.0013147577,0.0002492268,0.00030057938,0.00030357423,0.00013765122,0.00042902929,0.00024750174,0.0004122193,0.0002770197],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012866372,0.00007466349,0.27544403,0.00053375855,0.00015808582,0.00022187243,0.00037311035,0.015336824,0.66295475,0.00028614534,0.0004156311,0.042914502],"study_design_scores_gemma":[0.00005440335,0.00065239455,0.6369642,0.000039642175,0.00014058218,0.00045738634,0.00026181832,0.038367838,0.31789723,0.00047553444,0.004615649,0.00007328818],"about_ca_topic_score_codex":0.025935834,"about_ca_topic_score_gemma":0.01694122,"teacher_disagreement_score":0.025935834,"about_ca_system_score_codex":0.0012710486,"about_ca_system_score_gemma":0.00048353279,"threshold_uncertainty_score":0.05156976},"labels":[],"label_agreement":null},{"id":"W2053723288","doi":"10.1029/2005gl023435","title":"Decrease of emissions required to stabilize atmospheric CO<sub>2</sub> due to positive carbon cycle–climate feedbacks","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Environmental science; Carbon cycle; Greenhouse gas; Climate change; Climate model; Atmospheric sciences; Climatology; Carbon fibers; Atmospheric carbon cycle; Ecosystem; Geology; Oceanography; Ecology","score_opus":0.01040970667217208,"score_gpt":0.2675355635900776,"score_spread":0.2571258569179055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2053723288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99403447,0.00006357816,0.0024166026,0.00015273936,0.000022721262,0.0000061052756,0.00013322316,0.00006142246,0.0031091701],"genre_scores_gemma":[0.9994173,0.000021225009,0.0002758942,0.000023785235,0.0000014319143,0.0000044549342,0.000054399276,0.0000076985525,0.0001938731],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988806,0.000018416755,0.0000066288803,0.000024034618,0.000022978675,0.000039820574],"domain_scores_gemma":[0.99976414,0.000115434836,0.000039412993,0.000016652675,0.000034451943,0.000029926432],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025288932,0.00027636494,0.0002213153,0.00017073825,0.00029802238,0.0005428458,0.00032305345,0.00038384463,0.0015358126],"category_scores_gemma":[0.0015084263,0.00022419589,0.0005821796,0.00017446064,0.0004241008,0.0004614275,0.00042405128,0.00048324317,0.000085541236],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023968033,0.00006599298,0.020207005,0.000098485325,0.00010471677,0.0001992595,0.000045133707,0.9352039,0.036188867,0.0034451585,0.0004991519,0.003702644],"study_design_scores_gemma":[0.00025131274,0.00030994177,0.057805896,0.000015575244,0.00017643755,0.00012461877,0.0001410736,0.88432705,0.05101877,0.0035877787,0.0021866416,0.000054997254],"about_ca_topic_score_codex":0.0191201,"about_ca_topic_score_gemma":0.012211658,"teacher_disagreement_score":0.0191201,"about_ca_system_score_codex":0.0009961587,"about_ca_system_score_gemma":0.0009342694,"threshold_uncertainty_score":0.03801763},"labels":[],"label_agreement":null},{"id":"W2054267692","doi":"10.1029/1999gl002356","title":"Slow variations in mean path of the Gulf Stream east of Cape Hatteras","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Gulf Stream; Oceanography; Geology; Cape; Outflow; Thermohaline circulation; Current (fluid); Seamount; Geography","score_opus":0.018267606535112293,"score_gpt":0.24510561314975518,"score_spread":0.22683800661464287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054267692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891496,0.000047489986,0.000036529393,0.000040077623,0.000005397276,0.0000018184451,0.0002451021,0.0000025426161,0.00070619985],"genre_scores_gemma":[0.99917346,0.000055903387,0.00007597548,0.0000122035835,0.0000044721496,0.00000238862,0.000259722,0.0000021350545,0.00041369876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995124,0.0000060958437,0.000003974184,0.000017398199,0.000011743549,0.000009574409],"domain_scores_gemma":[0.99951255,0.00007773379,0.00014927813,0.000025651198,0.00016597797,0.00006876883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011789288,0.00007972089,0.000071946175,0.00044793283,0.00019889731,0.0003250563,0.00008292537,0.00009719906,0.0011565171],"category_scores_gemma":[0.0010805421,0.00007051529,0.000050146256,0.0003446396,0.00017692623,0.00019014753,0.00017148421,0.00014023212,0.00013874775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007585219,0.000008495387,0.98658687,0.000012863461,0.00002909003,0.00009587281,0.00043347702,0.00032971828,0.0035107085,0.00012002311,0.00064872555,0.008148214],"study_design_scores_gemma":[0.0000012966353,0.000006143062,0.99927336,0.0000024261192,0.0000026565046,0.000019041549,0.000097302625,0.00018020603,0.000063385145,0.000013531587,0.00033899923,0.0000015976823],"about_ca_topic_score_codex":0.049036343,"about_ca_topic_score_gemma":0.13074037,"teacher_disagreement_score":0.049036343,"about_ca_system_score_codex":0.00049792207,"about_ca_system_score_gemma":0.0003050184,"threshold_uncertainty_score":0.097501874},"labels":[],"label_agreement":null},{"id":"W2054372242","doi":"10.1029/2008gl035007","title":"Flow‐weighted values of runoff tracers (<i>δ</i><sup>18</sup>O, DOC, Ba, alkalinity) from the six largest Arctic rivers","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":267,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"","keywords":"Alkalinity; Arctic; Terrigenous sediment; Environmental science; Dissolved organic carbon; Thermohaline circulation; Oceanography; Surface runoff; Hydrology (agriculture); TRACER; Water mass; Geology; Structural basin; Ecology; Chemistry; Geomorphology","score_opus":0.033885850264818274,"score_gpt":0.2600355663069427,"score_spread":0.22614971604212442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054372242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975836,0.00004206483,0.0008018744,0.0000074013055,0.0000043211094,0.000004667638,0.0010594057,0.00003281453,0.00046394748],"genre_scores_gemma":[0.99119055,0.00013908983,0.00427054,0.000016669233,0.000010252883,0.000020452555,0.0037562584,0.000018188744,0.00057797896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999497,0.0000033233696,0.0000035789592,0.000020303933,0.0000138182195,0.000009277494],"domain_scores_gemma":[0.9997954,0.000029328932,0.00007415937,0.000014494055,0.000063177766,0.000023574463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001546921,0.00019763733,0.00016185663,0.0007332063,0.00021898682,0.0003575031,0.00012119169,0.00012870535,0.0004150346],"category_scores_gemma":[0.00038470974,0.0000869983,0.00014292872,0.0007368897,0.00012643225,0.00030170457,0.00019800062,0.00021888746,0.00010290529],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006038257,0.00013676421,0.8132005,0.00006567133,0.00015827992,0.00008617364,0.00046835397,0.0050576613,0.12461301,0.00022691954,0.0006127988,0.05477012],"study_design_scores_gemma":[0.00002499036,0.00018802514,0.9468007,0.0000083442055,0.000101631995,0.00013733025,0.00018257821,0.006755195,0.041175034,0.00020831509,0.0043815807,0.00003614892],"about_ca_topic_score_codex":0.012370483,"about_ca_topic_score_gemma":0.024329698,"teacher_disagreement_score":0.012370483,"about_ca_system_score_codex":0.00036044826,"about_ca_system_score_gemma":0.00024522777,"threshold_uncertainty_score":0.02459699},"labels":[],"label_agreement":null},{"id":"W2054624794","doi":"10.1029/1999gl010949","title":"The impact of rising atmospheric CO<sub>2</sub> on Simulated sea ice induced thermohaline circulation variability","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Thermohaline circulation; Climatology; Sea ice; Arctic ice pack; Shutdown of thermohaline circulation; Forcing (mathematics); Environmental science; Geology; Oceanography; Atmospheric circulation; Atmosphere (unit); Atmospheric sciences; North Atlantic Deep Water; Meteorology; Geography","score_opus":0.0227893942251509,"score_gpt":0.295599069804198,"score_spread":0.27280967557904706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054624794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985329,0.00002799593,0.0002183058,0.00006804643,0.000009960157,0.0000030619708,0.00034324775,0.000033408018,0.00076301285],"genre_scores_gemma":[0.9995473,0.000023017486,0.000108278706,0.000017672828,0.0000022537947,0.0000035552414,0.00021088352,0.000007487558,0.00007942097],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999218,0.000022711516,0.00000512193,0.000014438548,0.000008814776,0.000027105501],"domain_scores_gemma":[0.9997466,0.00013796249,0.00002710406,0.000016487567,0.000025707952,0.000046119458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021787283,0.00037616963,0.00023010685,0.00012496971,0.0002750771,0.00065366353,0.00031768897,0.00059495494,0.0015523502],"category_scores_gemma":[0.0008835302,0.00023941143,0.00042408018,0.00020009222,0.0003157826,0.00030034964,0.00031097585,0.0004945139,0.00011309657],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000791911,0.00017089974,0.07863016,0.00007924243,0.00015277424,0.00035306596,0.000071010785,0.8943588,0.01989957,0.00064136717,0.0009223984,0.0039287526],"study_design_scores_gemma":[0.00011800063,0.000263829,0.09933549,0.000009916338,0.00008809514,0.000058062367,0.000086215754,0.89466584,0.004735208,0.0002421488,0.0003695929,0.000027525743],"about_ca_topic_score_codex":0.034099396,"about_ca_topic_score_gemma":0.023342796,"teacher_disagreement_score":0.034099396,"about_ca_system_score_codex":0.0005888259,"about_ca_system_score_gemma":0.0004855076,"threshold_uncertainty_score":0.06780183},"labels":[],"label_agreement":null},{"id":"W2054705424","doi":"10.1029/2000gl011930","title":"Ørsted Initial Field Model","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":140,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Epoch (astronomy); Earth's magnetic field; Physics; Magnetic field; Geodesy; Geophysics; Scalar (mathematics); Degree (music); Spherical harmonics; Computational physics; Geology; Astrophysics; Mathematics; Geometry","score_opus":0.029727519268559814,"score_gpt":0.3234906264030028,"score_spread":0.293763107134443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054705424","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.099572025,0.0012411397,0.45572764,0.001963858,0.0007129362,0.0010110597,0.063599564,0.007490264,0.36868152],"genre_scores_gemma":[0.61086845,0.0014139508,0.09025101,0.00072002015,0.0003311475,0.0014858122,0.054899525,0.0013717529,0.23865834],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985635,0.000022004851,0.000009243864,0.000043280914,0.000039964445,0.00002907736],"domain_scores_gemma":[0.99943656,0.00006908318,0.000045458586,0.00008952748,0.00031509498,0.000044128057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029839226,0.0006280865,0.0008180236,0.00060730765,0.0006079661,0.0012051683,0.0025973641,0.001253202,0.036149047],"category_scores_gemma":[0.0012896359,0.00060078915,0.00067680614,0.0009685355,0.00046086128,0.0016757838,0.00096433115,0.0012079258,0.021634098],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003493135,0.00006471986,0.003457722,0.00022697684,0.00006883929,0.00021319612,0.00023999838,0.8186166,0.0026455761,0.0894861,0.049795225,0.034835707],"study_design_scores_gemma":[0.00013295544,0.000069721464,0.0018268948,0.000055550758,0.00005964593,0.000116439114,0.000078838275,0.8688819,0.0013881255,0.036958847,0.090372056,0.00005896307],"about_ca_topic_score_codex":0.03131496,"about_ca_topic_score_gemma":0.015952466,"teacher_disagreement_score":0.036149047,"about_ca_system_score_codex":0.0014169888,"about_ca_system_score_gemma":0.0013531136,"threshold_uncertainty_score":0.12093061},"labels":[],"label_agreement":null},{"id":"W2054749637","doi":"10.1029/2006gl027875","title":"Inferring the eddy‐induced diffusivity for heat in the surface mixed layer using satellite data","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Eddy diffusion; Thermal diffusivity; Sea-surface height; Geology; Mixed layer; Flux (metallurgy); Satellite; Gulf Stream; Altimeter; Surface layer; Sea surface temperature; Heat flux; Eddy covariance; Range (aeronautics); Climatology; Atmospheric sciences; Environmental science; Meteorology; Turbulence; Layer (electronics); Remote sensing; Heat transfer; Physics; Materials science; Mechanics; Thermodynamics","score_opus":0.12762875291449688,"score_gpt":0.3362385798300684,"score_spread":0.2086098269155715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054749637","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99527884,0.00010159643,0.0037991393,0.000025606641,0.000003990868,0.00000672582,0.00035258158,0.00003583287,0.00039562825],"genre_scores_gemma":[0.9936433,0.00007688558,0.005842023,0.0000031968214,0.000005200367,0.0000061446995,0.00033697547,0.0000057469792,0.000080599],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999899,0.00002899583,0.000009896903,0.000023901528,0.000020631343,0.000017533206],"domain_scores_gemma":[0.9995758,0.00021958296,0.00005925504,0.000038101036,0.000067756366,0.00003950136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041611827,0.0003338827,0.00025181478,0.00094954093,0.0001937332,0.000445837,0.00024455693,0.00029543726,0.00027360738],"category_scores_gemma":[0.0022255967,0.000377981,0.0003713743,0.0004847398,0.00012309372,0.0005601881,0.00021311601,0.00023730923,0.00012156356],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030088477,0.00016279543,0.75796723,0.0001460347,0.00023834496,0.00021959169,0.00024164372,0.0938234,0.09409304,0.0017794757,0.00048429813,0.050543312],"study_design_scores_gemma":[0.000061108454,0.00007995899,0.3979302,0.00003320306,0.00010165486,0.00009925222,0.00015030865,0.574119,0.025427528,0.0010718835,0.00088079926,0.00004505988],"about_ca_topic_score_codex":0.01683413,"about_ca_topic_score_gemma":0.023917632,"teacher_disagreement_score":0.01683413,"about_ca_system_score_codex":0.00057431194,"about_ca_system_score_gemma":0.00066568324,"threshold_uncertainty_score":0.0334723},"labels":[],"label_agreement":null},{"id":"W2054861871","doi":"10.1029/2000gl003790","title":"Ground magnetic signatures of ULF and substorm activity during an interval of abnormally weak solar wind on May 11, 1999","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institute of Space and Astronautical Science; Canadian Space Agency; University of Alberta","keywords":"Substorm; Solar wind; Interplanetary magnetic field; Magnetometer; Geophysics; Physics; Plasma sheet; Latitude; Geology; Magnetic field; Atmospheric sciences; Geodesy; Magnetosphere","score_opus":0.011032654142456091,"score_gpt":0.2635989242045324,"score_spread":0.2525662700620763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2054861871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990895,0.00003169283,0.000055274486,0.000022517088,0.0000041653298,0.0000034702048,0.00013800692,0.000010353865,0.0006450338],"genre_scores_gemma":[0.99934536,0.000020762329,0.000063470354,0.000014498561,0.000009742045,0.0000021439535,0.00034891538,0.0000018991077,0.00019316966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999269,0.000007521783,0.000005229951,0.000013076567,0.000020720001,0.00002643641],"domain_scores_gemma":[0.9995603,0.00005245185,0.00015239873,0.00003289749,0.00007854486,0.00012343226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011466047,0.00012141481,0.00021902942,0.0006710933,0.0003591188,0.00039446185,0.00013493035,0.00026480455,0.0006262216],"category_scores_gemma":[0.0005763049,0.000085618274,0.00006270416,0.00032805934,0.0002697668,0.00015658082,0.00029523706,0.00025364658,0.0001282172],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009900811,0.00015878776,0.92494416,0.00002989578,0.000066086126,0.001506676,0.0008635559,0.00031090828,0.052329708,0.00021142034,0.0009967517,0.01759202],"study_design_scores_gemma":[0.0000046475093,0.00006762264,0.9987054,0.0000028669635,0.000004478418,0.00013257534,0.000106431005,0.00015584497,0.00054287293,0.000019150248,0.000255962,0.0000021138414],"about_ca_topic_score_codex":0.004425547,"about_ca_topic_score_gemma":0.013078133,"teacher_disagreement_score":0.004425547,"about_ca_system_score_codex":0.00030569875,"about_ca_system_score_gemma":0.00006852297,"threshold_uncertainty_score":0.0087996125},"labels":[],"label_agreement":null},{"id":"W2055123544","doi":"10.1029/2003gl018644","title":"Effects of metamorphic crustal densification on earthquake size in warm slabs","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Crust; Geology; Slab; Seismology; Metamorphic rock; Mantle (geology); Deep-focus earthquake; Compression (physics); Petrology; Geophysics; Subduction; Tectonics; Materials science","score_opus":0.02895967934539929,"score_gpt":0.2760373169740348,"score_spread":0.2470776376286355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055123544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953043,0.00008697313,0.00003866379,0.000019418289,6.7127746e-7,8.969408e-7,0.000060905048,0.0000040078976,0.00025801302],"genre_scores_gemma":[0.9997135,0.000033038108,0.00001941314,0.0000052746514,0.0000016384394,7.971998e-7,0.000057208013,0.0000027173805,0.00016639696],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998523,0.00003461805,0.0000139285485,0.000027298485,0.000024671534,0.000047151585],"domain_scores_gemma":[0.9978161,0.00070244964,0.00057941844,0.00020437023,0.00011854782,0.0005790889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043826527,0.00019627508,0.00026302983,0.0004177094,0.00024426193,0.0005931038,0.00021252209,0.00024574666,0.003982652],"category_scores_gemma":[0.0029586875,0.00024484086,0.0002496816,0.00021407484,0.0007176566,0.000379909,0.00096676854,0.00036255445,0.00023046718],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022980592,0.00013036556,0.84605736,0.00008320003,0.00020498979,0.000685937,0.00065827905,0.0061870483,0.13101928,0.00048788392,0.00016441979,0.012023143],"study_design_scores_gemma":[0.000007943761,0.00009465563,0.99648464,0.0000026987673,0.000020885536,0.00013157321,0.00011931624,0.0003945339,0.002552447,0.000094498784,0.00009226667,0.0000045493493],"about_ca_topic_score_codex":0.0040527787,"about_ca_topic_score_gemma":0.005498787,"teacher_disagreement_score":0.0040527787,"about_ca_system_score_codex":0.0004490262,"about_ca_system_score_gemma":0.00016224742,"threshold_uncertainty_score":0.013323307},"labels":[],"label_agreement":null},{"id":"W2055238722","doi":"10.1029/2000gl012785","title":"OH production from the reaction of vibrationally excited H<sub>2</sub> in the mesosphere","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Excited state; Mesosphere; Altitude (triangle); Oxygen; Atomic physics; Reaction mechanism; Ground state; Chemical reaction; Physics; Chemistry; Atmospheric sciences; Stratosphere; Catalysis","score_opus":0.01725389425210684,"score_gpt":0.2672174454596705,"score_spread":0.2499635512075637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055238722","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9850382,0.0014322913,0.011331557,0.0001822065,0.000030426658,0.000017308435,0.00014655931,0.000109015265,0.0017124661],"genre_scores_gemma":[0.99689734,0.00040385732,0.0022027993,0.000023631663,0.0000091281845,0.0000073018728,0.00008075899,0.000007373473,0.0003677519],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994516,0.0000068636355,0.00000219024,0.000015538602,0.000014875532,0.000015343487],"domain_scores_gemma":[0.9999217,0.000021320177,0.000025172027,0.000011409114,0.000009646116,0.000010730656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019916642,0.00054600183,0.00016797725,0.00024839916,0.00026200517,0.00034366036,0.00032664312,0.0002979491,0.00080490886],"category_scores_gemma":[0.00018729921,0.00024637446,0.00032340628,0.00013648329,0.00031622793,0.0005581263,0.00036650116,0.00030897133,0.00022533168],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002649063,0.000058651778,0.042042434,0.0002584018,0.00010230037,0.0007422897,0.0002038615,0.01450517,0.9234811,0.004055307,0.0004698855,0.013815795],"study_design_scores_gemma":[0.00020284975,0.0007189173,0.16691144,0.000036270554,0.0002125383,0.0014970769,0.00035071932,0.14313218,0.6648478,0.014312016,0.0076763206,0.00010188095],"about_ca_topic_score_codex":0.0009104715,"about_ca_topic_score_gemma":0.00093318755,"teacher_disagreement_score":0.0009104715,"about_ca_system_score_codex":0.00036212357,"about_ca_system_score_gemma":0.00015117392,"threshold_uncertainty_score":0.0026926398},"labels":[],"label_agreement":null},{"id":"W2055466659","doi":"10.1029/2008gl036732","title":"Characterization of ULF pulsations by THEMIS","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Physics; Magnetosphere; Geophysics; Polarization (electrochemistry); Oscillation (cell signaling); Magnetic field; Substorm; Computational physics; Electric field; Line (geometry); Field (mathematics); Instrumentation (computer programming); Phase (matter)","score_opus":0.011932417433761618,"score_gpt":0.2775985983863142,"score_spread":0.26566618095255257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055466659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.986541,0.00021106361,0.0024397974,0.000083569794,0.000019394485,0.00001763885,0.0009899813,0.00013504336,0.009562488],"genre_scores_gemma":[0.996624,0.000057942707,0.0013824004,0.000014247734,0.000026376641,0.000011027459,0.0013804954,0.000015866552,0.00048769574],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998354,0.000021396017,0.000008097417,0.000038579074,0.000051105802,0.00004541557],"domain_scores_gemma":[0.9997136,0.000044238055,0.00009986233,0.00004311704,0.000057937603,0.000041222527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028809867,0.00017922011,0.00020457458,0.0010480848,0.00031813054,0.00035875302,0.00020405697,0.00016946552,0.0006112482],"category_scores_gemma":[0.0006368109,0.00007234755,0.00011040296,0.0011020829,0.00013170297,0.00022780187,0.00031130837,0.00023385626,0.00013098396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072145724,0.00008794154,0.7501551,0.00007877782,0.00007678213,0.0005345679,0.00089107454,0.0039870115,0.09492901,0.0038363342,0.0041531213,0.14054884],"study_design_scores_gemma":[0.000017676386,0.0001471595,0.96150476,0.000015370799,0.00002325479,0.00041790435,0.00022859668,0.009417624,0.014898787,0.00034779462,0.01296836,0.000012775647],"about_ca_topic_score_codex":0.0024186806,"about_ca_topic_score_gemma":0.003182505,"teacher_disagreement_score":0.0024186806,"about_ca_system_score_codex":0.00035168245,"about_ca_system_score_gemma":0.00013114205,"threshold_uncertainty_score":0.0048092604},"labels":[],"label_agreement":null},{"id":"W2055666743","doi":"10.1029/2008gl034832","title":"Differences in the non‐stationary influence of the North Atlantic Oscillation on European precipitation under different scenarios of greenhouse gas concentrations","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"North Atlantic oscillation; Precipitation; Climatology; Greenhouse gas; Environmental science; Atmospheric sciences; Oscillation (cell signaling); Common spatial pattern; Spatial variability; Meteorology; Geology; Chemistry; Geography; Oceanography; Ecology; Mathematics","score_opus":0.04946945043399957,"score_gpt":0.27775602457858894,"score_spread":0.22828657414458936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055666743","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99872017,0.000047209673,0.00021169736,0.000038678972,0.000003895266,0.000002561455,0.0002263194,0.000008496352,0.00074098905],"genre_scores_gemma":[0.9995009,0.000043798114,0.00008965022,0.0000071701465,0.0000022779582,0.0000029817813,0.00028117685,0.0000044203784,0.00006770187],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999706,0.00012544871,0.000021725109,0.000058604448,0.000028080241,0.000060094542],"domain_scores_gemma":[0.99880576,0.00080966816,0.00011756354,0.00008374992,0.00010065068,0.00008266849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001118165,0.00032949648,0.00022999631,0.00032825835,0.00022283281,0.0007319772,0.00031040743,0.0006008435,0.0008014896],"category_scores_gemma":[0.0029333294,0.00018850893,0.00086009834,0.00046700228,0.00033787632,0.0005010847,0.00036748164,0.00026314723,0.00008827017],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002152456,0.00017667189,0.47791508,0.00017976717,0.0013035226,0.00088951585,0.00025057676,0.46159825,0.037641678,0.0039811404,0.0010506242,0.012860801],"study_design_scores_gemma":[0.00015131086,0.00021018613,0.7849059,0.00001768378,0.00027401155,0.00011064397,0.00022795676,0.2073335,0.0047754454,0.0012539661,0.0006869732,0.0000524175],"about_ca_topic_score_codex":0.018599546,"about_ca_topic_score_gemma":0.0158728,"teacher_disagreement_score":0.018599546,"about_ca_system_score_codex":0.0006703888,"about_ca_system_score_gemma":0.0002856783,"threshold_uncertainty_score":0.036982536},"labels":[],"label_agreement":null},{"id":"W2055680888","doi":"10.1029/2008gl034005","title":"What drove the dramatic retreat of arctic sea ice during summer 2007?","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":212,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Arctic ice pack; Sea ice; Antarctic sea ice; Sea ice thickness; Cryosphere; Drift ice; Geology; Arctic sea ice decline; Climatology; Oceanography; Fast ice; Arctic; Ice-albedo feedback; Arctic geoengineering","score_opus":0.03130509893192266,"score_gpt":0.2684075967444587,"score_spread":0.23710249781253603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055680888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891235,0.00048180536,0.0006273801,0.002513331,0.00012404444,0.000013591596,0.0010304474,0.000060103484,0.0060258536],"genre_scores_gemma":[0.99846977,0.000214895,0.00020450664,0.00013789475,0.00003422081,0.000004721821,0.0003809499,0.000018030642,0.00053493504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999007,0.00001694088,0.000005662234,0.000028528131,0.000012002312,0.000036038975],"domain_scores_gemma":[0.99974424,0.00004228962,0.00007290648,0.0000104630435,0.000050285103,0.00007972449],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005214519,0.00037263022,0.0003444185,0.0003018999,0.00056173326,0.0013820416,0.0003513587,0.00094619585,0.002119729],"category_scores_gemma":[0.0011044261,0.00026639126,0.0004771684,0.00027428698,0.00031882463,0.00095049135,0.00039369042,0.00057320506,0.0002914634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012418116,0.00029778064,0.83712053,0.00044039186,0.00032973665,0.0022198972,0.0017241924,0.07674019,0.017071234,0.017175011,0.015901836,0.029737411],"study_design_scores_gemma":[0.0001721839,0.00026718818,0.7629519,0.00018990946,0.00017357076,0.0005606001,0.0058838786,0.18837275,0.005779852,0.013716515,0.021794781,0.00013690488],"about_ca_topic_score_codex":0.0378852,"about_ca_topic_score_gemma":0.043993264,"teacher_disagreement_score":0.0378852,"about_ca_system_score_codex":0.0014478093,"about_ca_system_score_gemma":0.00087525,"threshold_uncertainty_score":0.07532936},"labels":[],"label_agreement":null},{"id":"W2055734101","doi":"10.1029/2004gl020358","title":"Accelerated thawing of subarctic peatland permafrost over the last 50 years","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":410,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Natural Sciences and Engineering Research Council of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds Québécois de la Recherche sur la Nature et les Technologies","keywords":"Permafrost; Peat; Subarctic climate; Thermokarst; Bog; Environmental science; Plateau (mathematics); Snow; Physical geography; Geology; Sink (geography); Hydrology (agriculture); Ecology; Geomorphology; Oceanography; Geography","score_opus":0.07595326024290197,"score_gpt":0.311881205929928,"score_spread":0.23592794568702605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055734101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991283,0.00018462396,0.00007466628,0.000011934453,0.0000031979203,0.0000012391071,0.00028843616,0.0000065745594,0.00030098663],"genre_scores_gemma":[0.99905473,0.00014778014,0.00009937247,0.000009866051,0.000007270768,0.0000019454587,0.00045153304,0.0000015544639,0.0002259106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999292,0.000007235811,0.000007402347,0.000021756232,0.000016647104,0.000017744052],"domain_scores_gemma":[0.9995708,0.000040694358,0.00023573337,0.000030388608,0.00007937808,0.000043125598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026750934,0.00015109437,0.00015085755,0.0005890061,0.00023474047,0.0003411023,0.000085615335,0.00012302179,0.00093707256],"category_scores_gemma":[0.00054446544,0.000049787595,0.00014482136,0.00045485477,0.00015877104,0.00025853634,0.00026066267,0.00014721698,0.00012546523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001027075,0.000010217483,0.9851773,0.00003061702,0.000048420923,0.00012968744,0.00025747044,0.000395013,0.0030772872,0.000053230975,0.000112234906,0.010605919],"study_design_scores_gemma":[4.6472883e-7,0.000011053784,0.9990651,0.0000021452395,0.0000052125824,0.00006980027,0.000052561383,0.00008279238,0.00041790213,0.000010700114,0.0002813619,9.86297e-7],"about_ca_topic_score_codex":0.0055251657,"about_ca_topic_score_gemma":0.015796173,"teacher_disagreement_score":0.0055251657,"about_ca_system_score_codex":0.0003206102,"about_ca_system_score_gemma":0.00017637931,"threshold_uncertainty_score":0.01098603},"labels":[],"label_agreement":null},{"id":"W2055856266","doi":"10.1029/2001gl014551","title":"Interannual variations of the diurnal tide in the mesosphere induced by a zonal‐mean wind oscillation in the tropics","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Solstice; Mesosphere; Atmospheric tide; Thermosphere; Atmospheric sciences; Equinox; Climatology; Stratosphere; Atmosphere (unit); Geology; Subtropics; Oscillation (cell signaling); Amplitude; Environmental science; Latitude; Ionosphere; Meteorology; Physics; Geophysics","score_opus":0.03655010611397061,"score_gpt":0.27481873765712106,"score_spread":0.23826863154315045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055856266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984157,0.000015310176,0.00043710653,0.000044948494,0.000009802269,0.0000042905313,0.0003588133,0.00004975981,0.00066442974],"genre_scores_gemma":[0.9993093,0.000022319278,0.00022298227,0.000008744215,0.0000033730478,0.000006154882,0.00029170926,0.000008653327,0.00012669417],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.000026382027,0.0000042556676,0.000013627384,0.000011443562,0.000017563545],"domain_scores_gemma":[0.99978477,0.00006900174,0.000044068598,0.00002679897,0.000032565844,0.000042792544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024821117,0.00027303724,0.00016826691,0.00018379158,0.00025852278,0.00038923672,0.0002742376,0.00038787528,0.0011775689],"category_scores_gemma":[0.00063333154,0.00018315321,0.00044558654,0.00032167564,0.00024293781,0.0002454336,0.00022754137,0.00034852352,0.00011513641],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035121158,0.0002125052,0.14988247,0.00004745812,0.00030139074,0.00022824063,0.00011129757,0.82922757,0.011181207,0.0017904558,0.0016345611,0.0050316826],"study_design_scores_gemma":[0.0001151356,0.00018608748,0.11685667,0.0000071000964,0.00008129862,0.000050297913,0.0000793852,0.87982786,0.0015373388,0.000573793,0.0006656757,0.000019260144],"about_ca_topic_score_codex":0.018304588,"about_ca_topic_score_gemma":0.016457666,"teacher_disagreement_score":0.018304588,"about_ca_system_score_codex":0.00049296505,"about_ca_system_score_gemma":0.00041488127,"threshold_uncertainty_score":0.036396086},"labels":[],"label_agreement":null},{"id":"W2055896228","doi":"10.1029/2009gl038201","title":"Energy dissipation and the spectral distribution of whitecaps","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Core Research for Evolutional Science and Technology","keywords":"Dissipation; Breaking wave; Physics; Computational physics; Doppler effect; Energy (signal processing); Mechanics; Wave propagation; Optics","score_opus":0.014907476175190556,"score_gpt":0.2526010086956984,"score_spread":0.23769353252050784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055896228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9811204,0.00009238111,0.016312527,0.000026724414,0.000008897266,0.000005958418,0.00021567082,0.000087583954,0.0021298672],"genre_scores_gemma":[0.99878067,0.000031764233,0.0006353505,0.0000041196963,0.000004629157,0.000004680933,0.0001505455,0.000014875051,0.00037321576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987435,0.000012139304,0.0000074872364,0.00003893787,0.000042810338,0.00002423825],"domain_scores_gemma":[0.9989843,0.0003602353,0.0003017364,0.00010502794,0.00018961293,0.00005908532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030131475,0.00024942556,0.00017256795,0.0012592671,0.00022928952,0.0007138267,0.00025525404,0.0002087905,0.0021041147],"category_scores_gemma":[0.0025335178,0.00019213716,0.0001952492,0.00070712157,0.00042044133,0.0008556765,0.0004568212,0.00025670888,0.0003506055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013176029,0.00030933612,0.42517525,0.00026606338,0.0002960479,0.00068393676,0.0012981142,0.13470657,0.21454622,0.01118767,0.0016370561,0.20857622],"study_design_scores_gemma":[0.000021922999,0.00022474468,0.8014377,0.000043379772,0.00003718744,0.00042305008,0.0004391507,0.16644107,0.023481056,0.0060056597,0.0013606031,0.000084477055],"about_ca_topic_score_codex":0.0008561788,"about_ca_topic_score_gemma":0.0005856923,"teacher_disagreement_score":0.0021041147,"about_ca_system_score_codex":0.0002512486,"about_ca_system_score_gemma":0.000085486114,"threshold_uncertainty_score":0.007038951},"labels":[],"label_agreement":null},{"id":"W2055930308","doi":"10.1029/2008gl033671","title":"Steady magnetospheric convection selection criteria: Implications of global SuperDARN convection measurements","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Electrojet; Convection; Ionosphere; Geophysics; Atmospheric sciences; Geology; Physics; Meteorology; Earth's magnetic field; Magnetic field","score_opus":0.042357781046808346,"score_gpt":0.3183424979469228,"score_spread":0.2759847169001145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2055930308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9667849,0.00051291345,0.03110552,0.00014543028,0.000016161432,0.000024303166,0.00019140202,0.00012277355,0.0010967164],"genre_scores_gemma":[0.99275607,0.000042013246,0.0068928204,0.000030494648,0.000013392379,0.0000069638354,0.00016898978,0.000016024866,0.00007327023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99874,0.0006368409,0.00012325266,0.00021281795,0.00017476152,0.000112338894],"domain_scores_gemma":[0.98227304,0.0120476335,0.0021392219,0.0018065065,0.0011527698,0.0005807518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005781946,0.0002918104,0.00045586049,0.001041078,0.00028918264,0.0008244468,0.0005198278,0.00025807408,0.00045231564],"category_scores_gemma":[0.020339986,0.00010276124,0.0002139614,0.00092933176,0.00039561628,0.00064129505,0.00068114063,0.00030175172,0.00007626143],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006189145,0.00005827772,0.8657311,0.00009281066,0.00017936874,0.0002083295,0.0003388351,0.02446258,0.010434725,0.0017960538,0.00072903803,0.09534996],"study_design_scores_gemma":[0.00011756583,0.00026514038,0.65930986,0.00005037787,0.00012702555,0.00038212124,0.00038078197,0.32224107,0.011030888,0.004690603,0.0013597609,0.00004468641],"about_ca_topic_score_codex":0.0017023862,"about_ca_topic_score_gemma":0.0021429637,"teacher_disagreement_score":0.005781946,"about_ca_system_score_codex":0.00023095991,"about_ca_system_score_gemma":0.00025730138,"threshold_uncertainty_score":0.030578256},"labels":[],"label_agreement":null},{"id":"W2056262142","doi":"10.1029/2007gl029463","title":"On the relative importance of mineral phase transitions and viscosity stratification in controlling the sinking rates of detached slab remnants","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Toronto","funders":"","keywords":"Mantle (geology); Slab; Stratification (seeds); Geology; Viscosity; Transition zone; Phase boundary; Convection; Geophysics; Mantle convection; Mechanics; Mineralogy; Thermodynamics; Phase (matter); Physics; Subduction; Seismology; Tectonics","score_opus":0.04722508059434411,"score_gpt":0.3297997697540928,"score_spread":0.2825746891597487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056262142","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99357516,0.00009234282,0.005541027,0.000056345358,0.0000034301534,0.0000048463326,0.000021297425,0.000032637636,0.0006729],"genre_scores_gemma":[0.999228,0.00004610129,0.00058133504,0.0000033454508,0.0000020307116,0.000003066023,0.000013261947,0.00000975427,0.00011308478],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999293,0.000017162574,0.0000040201985,0.000014300303,0.000010777288,0.00002442646],"domain_scores_gemma":[0.9993279,0.00037532087,0.00011279051,0.000058780057,0.000043256387,0.000081916965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045196782,0.00049246347,0.00034082422,0.00038907476,0.0003791118,0.0008096629,0.00053000945,0.00039368667,0.0004912042],"category_scores_gemma":[0.002343186,0.00039157004,0.00037438975,0.00019596018,0.0007288206,0.00082554854,0.0006388327,0.00033898154,0.00009028229],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006304945,0.000090835674,0.043400668,0.00009513952,0.000056651443,0.00032594235,0.00024784153,0.741016,0.19264096,0.014169155,0.0001532274,0.0071731126],"study_design_scores_gemma":[0.000045961944,0.00007976815,0.0075397287,0.0000034273041,0.000021847052,0.000036813308,0.00004474152,0.97799265,0.012151144,0.0019374524,0.00012407679,0.000022357739],"about_ca_topic_score_codex":0.0063518225,"about_ca_topic_score_gemma":0.0024381494,"teacher_disagreement_score":0.0063518225,"about_ca_system_score_codex":0.0004751701,"about_ca_system_score_gemma":0.00031765108,"threshold_uncertainty_score":0.012629688},"labels":[],"label_agreement":null},{"id":"W2056275475","doi":"10.1029/2003gl017755","title":"Structure and mixing across an Arctic/Atlantic front in northern Baffin Bay","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; North Pacific Marine Science Organization; University of Victoria","funders":"","keywords":"Oceanography; Bay; Geology; Current (fluid); Front (military); Thermohaline circulation; Groenlandia; Arctic; Temperature salinity diagrams; Salinity; Water mass; Climatology; Ice sheet","score_opus":0.01703503221263037,"score_gpt":0.27183387712778617,"score_spread":0.2547988449151558,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056275475","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999121,0.000053484386,0.000020372356,0.000028556631,0.0000017681259,0.000002648289,0.000043222695,0.0000016189992,0.0007272115],"genre_scores_gemma":[0.9992964,0.00005852282,0.00007501361,0.000021935677,0.0000034010482,0.000004048068,0.00014774388,0.0000012645462,0.00039161823],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998658,0.000011959288,0.0000070609076,0.000028392435,0.000029839783,0.000057074925],"domain_scores_gemma":[0.99974984,0.00001599802,0.000057977173,0.0000092249065,0.000083310086,0.000083755884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018289512,0.00012701021,0.00023233434,0.0013253461,0.0015312647,0.0008462467,0.0002811468,0.00038572095,0.001747805],"category_scores_gemma":[0.00044170153,0.0002532761,0.00014185067,0.0008995304,0.00070316816,0.00030455174,0.0007739939,0.0002488481,0.0003338827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031657488,0.0000583636,0.9706405,0.000020482255,0.000034046694,0.00041132965,0.0033821326,0.00020009646,0.015169049,0.00019567422,0.00030688464,0.009264892],"study_design_scores_gemma":[0.0000032940318,0.000012629385,0.99859864,0.000005012797,0.000005572152,0.00004149005,0.0007708333,0.00016405564,0.000086787455,0.000015376138,0.0002932828,0.0000029456237],"about_ca_topic_score_codex":0.47383592,"about_ca_topic_score_gemma":0.64235497,"teacher_disagreement_score":0.47383592,"about_ca_system_score_codex":0.0023734504,"about_ca_system_score_gemma":0.0010812625,"threshold_uncertainty_score":0.9421558},"labels":[],"label_agreement":null},{"id":"W2056395871","doi":"10.1029/2008gl034921","title":"Thirty‐year gravity change at Mount Baker Volcano, Washington, USA: Extracting the signal from under the ice","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Impact crater; Geology; Volcano; Magma; Gravity anomaly; Geophysics; Earth science; Geochemistry; Paleontology; Astrobiology","score_opus":0.07966269247260362,"score_gpt":0.2746205955241547,"score_spread":0.19495790305155108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056395871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993863,0.00001956493,0.000027318727,0.000016033115,0.0000019109002,0.0000013952274,0.0002470079,0.0000063940547,0.00029406635],"genre_scores_gemma":[0.9988368,0.00003559132,0.00012340974,0.0000064122173,0.0000068894615,0.00000226435,0.00080706406,0.000001647433,0.00017995888],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999565,0.0000040033283,0.000003300814,0.00001176574,0.000011068405,0.00001329646],"domain_scores_gemma":[0.9998336,0.000021706113,0.000048101625,0.000013172519,0.000041202715,0.00004214137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009202758,0.00012437043,0.000092591996,0.0006703786,0.00025531367,0.00023587502,0.00013127142,0.0001723928,0.00044581067],"category_scores_gemma":[0.00031953547,0.00007860292,0.000076259756,0.0005411109,0.00014552457,0.00011450587,0.00017670318,0.00016247127,0.00013429088],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000051184496,0.000021548933,0.9851414,0.000010649106,0.000023830346,0.00015309588,0.0003017984,0.00014686934,0.006318613,0.000020177182,0.00062849966,0.007182296],"study_design_scores_gemma":[6.7964817e-7,0.0000042995825,0.99933475,8.0504043e-7,0.0000030437593,0.000019229044,0.00010372604,0.00015127266,0.0001877865,0.0000022521767,0.00019114104,9.592632e-7],"about_ca_topic_score_codex":0.06671902,"about_ca_topic_score_gemma":0.22678342,"teacher_disagreement_score":0.06671902,"about_ca_system_score_codex":0.00030587573,"about_ca_system_score_gemma":0.00021996428,"threshold_uncertainty_score":0.13266134},"labels":[],"label_agreement":null},{"id":"W2056681173","doi":"10.1029/2005gl022478","title":"Variations in the Pacific Decadal Oscillation over the past millennium","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":580,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Pacific decadal oscillation; Dendrochronology; Climatology; Proxy (statistics); Southern oscillation; Range (aeronautics); Geology; El Niño Southern Oscillation; Environmental science; Secular variation; Oceanography; Physical geography; Geography; Paleontology","score_opus":0.035275155934073106,"score_gpt":0.2981407412389245,"score_spread":0.2628655853048514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056681173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957431,0.00048573315,0.00013931381,0.00008542705,0.000012632604,0.0000024620372,0.0019817278,0.000019685282,0.0015299309],"genre_scores_gemma":[0.998044,0.00025341418,0.00015561737,0.000014602824,0.0000060939383,0.0000024524272,0.0012519283,0.000003834188,0.0002680685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996173,0.000003169055,0.0000031885293,0.0000131637835,0.000011477069,0.000007224945],"domain_scores_gemma":[0.99971,0.000033064505,0.00009152346,0.000017905955,0.00010822024,0.000039249615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021526341,0.00009143835,0.000062957544,0.0006526719,0.00021176983,0.000475027,0.00011500913,0.00010489117,0.0005610179],"category_scores_gemma":[0.0008052153,0.00007030125,0.00007505579,0.00097428006,0.00010677825,0.0001690988,0.0001971995,0.00017120304,0.00007925594],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041864405,0.000008780186,0.9858392,0.00002459636,0.000089476714,0.00006872008,0.0002766539,0.001010606,0.0012980559,0.00018748801,0.0008286821,0.010325949],"study_design_scores_gemma":[9.66932e-7,0.000002282212,0.99843603,0.0000039894717,0.000008362407,0.000022651786,0.000056533503,0.00041229476,0.00006302283,0.000021035085,0.00097138615,0.0000014620108],"about_ca_topic_score_codex":0.1121375,"about_ca_topic_score_gemma":0.22405677,"teacher_disagreement_score":0.1121375,"about_ca_system_score_codex":0.00075233774,"about_ca_system_score_gemma":0.00033182703,"threshold_uncertainty_score":0.22296959},"labels":[],"label_agreement":null},{"id":"W2056786549","doi":"10.1029/2000gl011705","title":"Gravitational braking of inner‐core rotation in geodynamo simulations","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Centre for Supercomputing Applications; National Science Foundation","keywords":"Inner core; Mantle (geology); Dynamo theory; Differential rotation; Physics; Outer core; Rotation (mathematics); Mechanics; Geophysics; Dynamo; Geology; Magnetic field; Geometry","score_opus":0.02622991357515964,"score_gpt":0.3221585408050877,"score_spread":0.2959286272299281,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2056786549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9479302,0.00022114986,0.023982855,0.00067827094,0.00014477246,0.0001299612,0.001159324,0.00072934653,0.025024047],"genre_scores_gemma":[0.9885315,0.00011248714,0.008472969,0.00014426676,0.000023380644,0.00014749174,0.00049834984,0.0001934212,0.0018761416],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997576,0.00008243347,0.0000102699105,0.000028525166,0.000043467902,0.00007770674],"domain_scores_gemma":[0.9989324,0.00047191686,0.00010426971,0.000118244825,0.000170952,0.00020209221],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060826837,0.000540851,0.0011616688,0.0005152183,0.0008651752,0.0010140766,0.0018530576,0.0015153916,0.003394142],"category_scores_gemma":[0.0033348366,0.0005581303,0.00055527425,0.00056778226,0.0010062854,0.0007764875,0.00096756883,0.0013041378,0.00037590845],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010867514,0.00008811027,0.0024968411,0.00003251386,0.000030448091,0.00006554253,0.000089458976,0.9898196,0.0016755933,0.0034893882,0.00057672476,0.0015271881],"study_design_scores_gemma":[0.000034076962,0.000012737018,0.00048002033,0.00000424529,0.000004884747,0.000004082698,0.000013223578,0.9983535,0.00024734472,0.00051692704,0.00032289105,0.0000061656783],"about_ca_topic_score_codex":0.02667224,"about_ca_topic_score_gemma":0.015268331,"teacher_disagreement_score":0.02667224,"about_ca_system_score_codex":0.0011278066,"about_ca_system_score_gemma":0.0016682055,"threshold_uncertainty_score":0.053034008},"labels":[],"label_agreement":null},{"id":"W2057169085","doi":"10.1029/2006gl026286","title":"Intra‐seasonal relationship between the Northern Hemisphere sea ice variability and the North Atlantic Oscillation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Northern Hemisphere; Climatology; Rossby wave; North Atlantic oscillation; Geology; Seesaw molecular geometry; Sea ice; Oceanography; Pacific decadal oscillation; Sea surface temperature","score_opus":0.03157588070776457,"score_gpt":0.27414136199688033,"score_spread":0.24256548128911576,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057169085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99591583,0.00025927278,0.00031100988,0.00008170784,0.000008823386,0.0000034318725,0.00013453075,0.000008209897,0.003277181],"genre_scores_gemma":[0.9991442,0.00012958955,0.00012980564,0.000017077207,0.000013132541,0.00000380212,0.00011387112,0.0000035237078,0.00044495313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995315,0.000013231561,0.000003585124,0.000010727964,0.000010152161,0.000009172317],"domain_scores_gemma":[0.9994997,0.0001896941,0.00015351614,0.000031110863,0.00006438954,0.00006164636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018568462,0.00009933916,0.000092868686,0.00023715045,0.00016378205,0.00036948567,0.00008697043,0.00013884397,0.0011534711],"category_scores_gemma":[0.0010227886,0.00008192503,0.00009388797,0.0002450618,0.00015673826,0.00019868066,0.00020443945,0.00018286565,0.00017981064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033600972,0.00006943455,0.9572261,0.000033878478,0.00011619009,0.00018448285,0.00021277346,0.0019569923,0.019759005,0.00079448405,0.00052992377,0.018780705],"study_design_scores_gemma":[0.0000032380876,0.000022835444,0.99818605,0.0000021694507,0.000013027584,0.000036846264,0.00003408434,0.0009800454,0.00020869616,0.00011576155,0.00039498278,0.0000023303862],"about_ca_topic_score_codex":0.0027217541,"about_ca_topic_score_gemma":0.006399035,"teacher_disagreement_score":0.0027217541,"about_ca_system_score_codex":0.00015769378,"about_ca_system_score_gemma":0.00015105779,"threshold_uncertainty_score":0.005411744},"labels":[],"label_agreement":null},{"id":"W2057318181","doi":"10.1029/2003gl017681","title":"Atlantic deep circulation controlled by freshening in the Southern Ocean","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Pycnocline; Thermohaline circulation; Geology; Oceanography; North Atlantic Deep Water; Southern Hemisphere; Climatology; Shutdown of thermohaline circulation; Ocean current; Zonal and meridional; Subtropics","score_opus":0.01712983203744639,"score_gpt":0.24657075374686377,"score_spread":0.22944092170941738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057318181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979956,0.000028369235,0.00045136243,0.00006549459,0.000005491556,0.0000028656966,0.00005777073,0.000028445742,0.001364746],"genre_scores_gemma":[0.99960166,0.000023342998,0.0000964194,0.000007381801,0.000002513738,0.0000012787035,0.00004179448,0.0000044615776,0.00022111955],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999966,0.000008482241,0.0000019491042,0.000007866697,0.000004661336,0.000011016016],"domain_scores_gemma":[0.9998567,0.000026958087,0.000033060056,0.000014462524,0.000017931809,0.000050917402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012240419,0.00024236707,0.0002585748,0.00014496036,0.00031620258,0.0006707857,0.00021843587,0.00030353747,0.0011810664],"category_scores_gemma":[0.00074951,0.00022053148,0.00039699598,0.00015313704,0.00045409013,0.00042725654,0.0005048499,0.0003685148,0.000080940925],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007410752,0.00008276781,0.09486315,0.000055995544,0.00013829811,0.0007174761,0.00027194378,0.8376839,0.046419427,0.01251855,0.0008389313,0.0056684413],"study_design_scores_gemma":[0.00025373916,0.00016321766,0.06971962,0.000008706041,0.00006105282,0.00005882204,0.00010390082,0.924286,0.0013790791,0.0031045603,0.00083356345,0.000027750346],"about_ca_topic_score_codex":0.037158113,"about_ca_topic_score_gemma":0.020414375,"teacher_disagreement_score":0.037158113,"about_ca_system_score_codex":0.0010117915,"about_ca_system_score_gemma":0.0007126487,"threshold_uncertainty_score":0.07388365},"labels":[],"label_agreement":null},{"id":"W2057431298","doi":"10.1029/2003gl018014","title":"Source model for the M<sub><i>w</i></sub> 6.7, 23 October 2002, Nenana Mountain Earthquake (Alaska) from InSAR","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":209,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hypocenter; Geology; Seismology; Interferometric synthetic aperture radar; Crust; Geodesy; Slip (aerodynamics); Source model; Synthetic aperture radar; Induced seismicity; Geophysics; Remote sensing","score_opus":0.041195945501439804,"score_gpt":0.2670367976828869,"score_spread":0.22584085218144712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2057431298","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.33300042,0.0013222405,0.41785705,0.0025506692,0.0010323253,0.0005195855,0.11197131,0.009684034,0.12206236],"genre_scores_gemma":[0.85666984,0.00070227444,0.031004205,0.00024549954,0.00018148484,0.0004459705,0.032988,0.00091013685,0.07685252],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999447,0.0000069287216,0.00000388506,0.000015658941,0.000018436283,0.000010362797],"domain_scores_gemma":[0.99987996,0.000020760799,0.000016018868,0.000011209324,0.00006316986,0.000008887362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011021941,0.00071842846,0.0005522146,0.0006480455,0.0005290227,0.00070487836,0.001803466,0.0015410071,0.014461377],"category_scores_gemma":[0.00039150193,0.00047392186,0.00046917994,0.00087097596,0.00020812228,0.00070484716,0.00034519084,0.0007813884,0.0049730754],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001347923,0.000084690364,0.005189681,0.000108598455,0.000051799816,0.00040726733,0.00014823688,0.944431,0.0050847647,0.013566972,0.018271422,0.012520742],"study_design_scores_gemma":[0.00006670357,0.000026919854,0.0021439388,0.000012320894,0.00003176887,0.000106337364,0.000047172023,0.9842604,0.0006796445,0.002458645,0.010141926,0.000024297458],"about_ca_topic_score_codex":0.0777477,"about_ca_topic_score_gemma":0.05237429,"teacher_disagreement_score":0.0777477,"about_ca_system_score_codex":0.0007961551,"about_ca_system_score_gemma":0.001035504,"threshold_uncertainty_score":0.15459031},"labels":[],"label_agreement":null},{"id":"W2058050440","doi":"10.1029/2003gl017534","title":"The importance of the third dimension in granular shear","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Shear (geology); Granular material; Amplitude; Mechanics; Fault gouge; Shear rate; Geotechnical engineering; Materials science; Physics; Statistical physics; Geology; Thermodynamics; Fault (geology); Rheology; Optics; Composite material","score_opus":0.02833553622571882,"score_gpt":0.2734755420952547,"score_spread":0.24514000586953588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058050440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9009037,0.00048201962,0.08764198,0.00058574206,0.000117819094,0.000022867453,0.00010131594,0.00036897892,0.009775659],"genre_scores_gemma":[0.99465334,0.00012595965,0.0048909076,0.000029133382,0.000011172776,0.000012625111,0.0000151694185,0.00002370977,0.00023806324],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998745,0.000024408795,0.00000761471,0.000017650478,0.000044526623,0.000031223048],"domain_scores_gemma":[0.9988254,0.0006098605,0.00016656621,0.00016746743,0.00008221332,0.0001485398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030981968,0.0003008288,0.00043387542,0.00030812822,0.0007753108,0.001807166,0.00031912874,0.0007979585,0.0006084757],"category_scores_gemma":[0.0022721717,0.00038975113,0.0005815989,0.00032031385,0.0013761648,0.0011726421,0.001110168,0.0009757715,0.00009367646],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023812316,0.00007486656,0.007371209,0.00006058867,0.000042743482,0.0002862917,0.00018287562,0.92562395,0.017524017,0.042362723,0.00048370415,0.0057488913],"study_design_scores_gemma":[0.000015238545,0.00003471346,0.001453844,0.0000076529195,0.000011253656,0.000045563578,0.000018373867,0.9873378,0.0017884095,0.008746038,0.0005193096,0.000021785823],"about_ca_topic_score_codex":0.0046176133,"about_ca_topic_score_gemma":0.003736093,"teacher_disagreement_score":0.0046176133,"about_ca_system_score_codex":0.000634367,"about_ca_system_score_gemma":0.0009428926,"threshold_uncertainty_score":0.00918144},"labels":[],"label_agreement":null},{"id":"W2058117322","doi":"10.1029/2003gl017360","title":"Solar wind electric field modulation of the NAO: A correlation analysis in the lower atmosphere","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Troposphere; Geopotential height; Stratosphere; North Atlantic oscillation; Geopotential; Environmental science; Atmospheric sciences; Climatology; Arctic oscillation; Atmosphere (unit); Geology; Meteorology; Northern Hemisphere; Physics; Precipitation","score_opus":0.016022985022809397,"score_gpt":0.2577752226007418,"score_spread":0.2417522375779324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058117322","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990546,0.00006618269,0.00024296352,0.000020680534,0.0000014128361,0.0000024275782,0.00014105717,0.000010117446,0.00046053683],"genre_scores_gemma":[0.99932194,0.000054741082,0.00013944578,0.0000033868123,0.0000037635966,0.0000021119818,0.000296259,0.0000033201304,0.00017504921],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999144,0.000019216724,0.000004506607,0.00002009387,0.000016451411,0.000025320469],"domain_scores_gemma":[0.99947304,0.0002494952,0.000084939595,0.00003378464,0.000086911175,0.000071951305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020900222,0.00011689459,0.00022067703,0.00053296844,0.00020756798,0.00047064605,0.00011440339,0.000110688416,0.0009607542],"category_scores_gemma":[0.0011033892,0.00013364818,0.00020218783,0.00082708476,0.0001423352,0.00015870687,0.00017830769,0.00020001289,0.00022877657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003364917,0.000063096624,0.96730316,0.000028276903,0.00011036921,0.00023419774,0.00016193547,0.004739279,0.012381626,0.00042218156,0.00036750745,0.013851853],"study_design_scores_gemma":[0.0000066922003,0.000022927774,0.99187005,0.000002417185,0.000015559448,0.000044345077,0.000022107179,0.007248458,0.00042366155,0.000080531085,0.00025788066,0.000005452606],"about_ca_topic_score_codex":0.01396949,"about_ca_topic_score_gemma":0.014743989,"teacher_disagreement_score":0.01396949,"about_ca_system_score_codex":0.00020451607,"about_ca_system_score_gemma":0.00022113514,"threshold_uncertainty_score":0.02777636},"labels":[],"label_agreement":null},{"id":"W2058604123","doi":"10.1029/2004gl022262","title":"The role of Fram Strait winter cyclones on sea ice flux and on Spitsbergen air temperatures","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic ice pack; Climatology; Geology; Sea ice; Oceanography; Cyclone (programming language); Cyclogenesis; Arctic; Arctic sea ice decline; Arctic dipole anomaly; Antarctic sea ice","score_opus":0.010053372567488944,"score_gpt":0.25368385326534176,"score_spread":0.2436304806978528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058604123","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997717,0.00035124374,0.000013782857,0.00006494472,0.000010498482,0.0000012172549,0.00013768833,0.0000012026283,0.0017024021],"genre_scores_gemma":[0.99868673,0.0003736201,0.000021355932,0.00001956858,0.000018457149,0.0000015246998,0.00018087671,0.0000019697145,0.00069586275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989176,0.000036158868,0.0000061071073,0.000016682921,0.0000087816625,0.00004050915],"domain_scores_gemma":[0.99892634,0.0005500125,0.0002098824,0.0000410111,0.00007991722,0.0001927292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002707519,0.00022955966,0.00020737747,0.00044775332,0.00028968847,0.0007945797,0.000110622364,0.00022831002,0.0023111633],"category_scores_gemma":[0.0013913455,0.000108888504,0.000257295,0.0002449971,0.0002789273,0.00031066054,0.0003253378,0.000193194,0.00024240912],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069945166,0.000045289555,0.9887029,0.000022665983,0.00010644046,0.00031553663,0.0001982442,0.00048685982,0.0012519328,0.0002814334,0.00041400985,0.0074752253],"study_design_scores_gemma":[0.0000056816425,0.000039284918,0.99907327,0.000011820775,0.000029743087,0.000041946878,0.00014952078,0.00025000074,0.00007351508,0.00004174132,0.0002815553,0.0000019563342],"about_ca_topic_score_codex":0.013076987,"about_ca_topic_score_gemma":0.030525858,"teacher_disagreement_score":0.013076987,"about_ca_system_score_codex":0.00031223992,"about_ca_system_score_gemma":0.00028284997,"threshold_uncertainty_score":0.026001751},"labels":[],"label_agreement":null},{"id":"W2058692935","doi":"10.1029/2003gl019019","title":"Trends in time‐varying percentiles of daily minimum and maximum temperature over North America","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Percentile; Climate change; Environmental science; Air temperature; Western europe; Climatology; Distribution (mathematics); Maximum temperature; Air quality index; Mean radiant temperature; Geography; Physical geography; Atmospheric sciences; Meteorology; Geology; Mathematics; Statistics; Oceanography","score_opus":0.0200449935518123,"score_gpt":0.2828024971139367,"score_spread":0.26275750356212435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058692935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99584925,0.00037737368,0.00036362905,0.0001711051,0.0000062724175,0.0000028298516,0.0014378434,0.000056754703,0.0017349416],"genre_scores_gemma":[0.9977175,0.00021544343,0.00031447652,0.000020088652,0.000009600679,0.000006922869,0.0013082119,0.000006443796,0.00040133172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990356,0.000013609083,0.000007143094,0.00003232883,0.000025121306,0.000018200513],"domain_scores_gemma":[0.99925727,0.00015020695,0.00020465876,0.000047905844,0.0002851732,0.000054789976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002574626,0.00010953856,0.00012880247,0.0007360956,0.00019142455,0.00037819147,0.0001765208,0.00020557731,0.0008419642],"category_scores_gemma":[0.001087634,0.00010114334,0.00010907733,0.0009285012,0.00015859643,0.00038383898,0.00019012921,0.0002445567,0.00014386533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015588713,0.000027505113,0.9567728,0.00006570041,0.00013700365,0.00007570181,0.0010770711,0.0044577243,0.0037606724,0.0006338006,0.0033552025,0.029480925],"study_design_scores_gemma":[0.000002014223,0.000011527577,0.9956714,0.00000582162,0.00001301611,0.000037653488,0.00017303119,0.0016645486,0.0002302602,0.00008153089,0.0021045227,0.000004578755],"about_ca_topic_score_codex":0.051040303,"about_ca_topic_score_gemma":0.08218772,"teacher_disagreement_score":0.9489597,"about_ca_system_score_codex":0.00049509737,"about_ca_system_score_gemma":0.00023883187,"threshold_uncertainty_score":0.101486385},"labels":[],"label_agreement":null},{"id":"W2058905852","doi":"10.1029/2002gl015571","title":"The likelihood of winter sprites over the Gulf Stream","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Lightning and Electromagnetic Phenomena","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Sprite (computer graphics); Upper-atmospheric lightning; Thunderstorm; Storm; Environmental science; Lightning detection; Meteorology; Lightning (connector); Atmospheric sciences; Geology; Climatology; Geography; Lightning strike; Physics","score_opus":0.017587424146169494,"score_gpt":0.272108073024397,"score_spread":0.2545206488782275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2058905852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993567,0.00003194668,0.000018579876,0.00005414196,0.0000019869744,0.0000019868494,0.00007340967,0.000002778567,0.00045847456],"genre_scores_gemma":[0.9996184,0.00004825211,0.000023074337,0.000012248951,0.000003326504,0.0000012685923,0.00011350418,6.3563294e-7,0.00017918962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980754,0.000033163516,0.000013205382,0.00003151132,0.0000588306,0.000055734232],"domain_scores_gemma":[0.998606,0.00025943472,0.00053842855,0.000050177347,0.00025290318,0.0002931267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029682717,0.00014713811,0.000094202915,0.0006253482,0.0005156152,0.000580602,0.00013857428,0.000324667,0.0013995903],"category_scores_gemma":[0.0020724337,0.00009310571,0.0000971229,0.0002791721,0.00032286468,0.00025671575,0.000409945,0.00031658448,0.000119610326],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013812278,0.00001617321,0.9949656,0.0000055133314,0.0000115057255,0.00019010928,0.00013998848,0.00020688267,0.0003153327,0.00003330124,0.00022018136,0.0037573245],"study_design_scores_gemma":[0.000007380272,0.000068914196,0.99686927,0.000011400589,0.0000061315914,0.000275331,0.0011483707,0.0009033703,0.00022849243,0.00009243372,0.0003854536,0.0000034698878],"about_ca_topic_score_codex":0.041767936,"about_ca_topic_score_gemma":0.07782653,"teacher_disagreement_score":0.041767936,"about_ca_system_score_codex":0.0007027994,"about_ca_system_score_gemma":0.00042367206,"threshold_uncertainty_score":0.083049595},"labels":[],"label_agreement":null},{"id":"W2059117250","doi":"10.1029/2005gl025243","title":"Ground surface paleotemperature reconstruction using information measures and empirical Bayes","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University; University of Manitoba","funders":"","keywords":"Akaike information criterion; Bayesian probability; Bayesian information criterion; Mean squared error; Singular value decomposition; Root mean square; Geology; Borehole; Statistics; Mathematics; Meteorology; Algorithm","score_opus":0.04644492144033593,"score_gpt":0.30000988011769447,"score_spread":0.25356495867735857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059117250","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.018792743,0.00019032179,0.97979194,0.00016531818,0.0000060052093,0.000016025531,0.00005751286,0.00012708403,0.00085315434],"genre_scores_gemma":[0.4986869,0.0004064846,0.49916646,0.00010405118,0.00006937327,0.00012530027,0.00037573936,0.00013342775,0.00093227567],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989611,0.00047249897,0.000064395004,0.00014455916,0.00029682752,0.000060567047],"domain_scores_gemma":[0.99570787,0.0029515706,0.00044555037,0.00036052428,0.00044846028,0.00008601384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004353651,0.0005329362,0.00078710925,0.0025062533,0.0004934822,0.0017771418,0.0013930809,0.0008353916,0.0009582868],"category_scores_gemma":[0.015583866,0.00073369936,0.00073048595,0.0012274091,0.0015400926,0.0022166818,0.0014340278,0.0011384337,0.00022275634],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052604657,0.00005278804,0.005261698,0.00008347587,0.00012994882,0.0000882236,0.00018250951,0.7233377,0.0018552812,0.15233031,0.0008030376,0.115822375],"study_design_scores_gemma":[0.000005046146,0.0000075196317,0.0007882269,0.00001687207,0.0000048795805,0.000015829815,0.000011277447,0.932117,0.00032072212,0.06639388,0.00030441978,0.000014474853],"about_ca_topic_score_codex":0.0061475737,"about_ca_topic_score_gemma":0.0050990754,"teacher_disagreement_score":0.0061475737,"about_ca_system_score_codex":0.0014904566,"about_ca_system_score_gemma":0.001100482,"threshold_uncertainty_score":0.023024619},"labels":[],"label_agreement":null},{"id":"W2059519417","doi":"10.1029/2004gl021611","title":"Average nighttime <i>F</i> region disturbance neutral winds measured by UARS WINDII: Initial results","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Atmospheric sciences; Local time; Latitude; Thermosphere; Earth's magnetic field; Zonal and meridional; Perturbation (astronomy); Daytime; Geomagnetic latitude; Geology; Ionosphere; Climatology; Environmental science; Physics; Geophysics; Geodesy; Astronomy; Magnetic field","score_opus":0.01830102711393996,"score_gpt":0.2745522962489268,"score_spread":0.25625126913498686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059519417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99410915,0.000050503964,0.0010624387,0.000012663495,0.000005562792,0.000019651125,0.003016181,0.00012472487,0.001599174],"genre_scores_gemma":[0.99309444,0.000038238588,0.0016707473,0.000006575427,0.000007519391,0.000011137066,0.004744934,0.000017614484,0.0004088106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980503,0.000035919835,0.000014594507,0.000048425016,0.00006171019,0.00003440079],"domain_scores_gemma":[0.9996598,0.000056658424,0.000042699958,0.000045341476,0.00012641304,0.00006913387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003855632,0.00034002113,0.00019907377,0.00044530776,0.00026986687,0.00045636378,0.00026500484,0.00021879627,0.0006704112],"category_scores_gemma":[0.0006595175,0.00013384114,0.00036260925,0.0005012051,0.00009338196,0.00030404635,0.00016364078,0.00018255363,0.00025306517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005700186,0.00023308871,0.94309837,0.000056609562,0.00020017341,0.00013920313,0.00017946184,0.020031111,0.011415918,0.00021001755,0.0014058462,0.022460233],"study_design_scores_gemma":[0.000020647904,0.00014351949,0.9779587,0.0000041324683,0.000037939044,0.000053261065,0.00007516066,0.016458374,0.004055635,0.000039569357,0.0011379885,0.000015078206],"about_ca_topic_score_codex":0.044327885,"about_ca_topic_score_gemma":0.04938683,"teacher_disagreement_score":0.044327885,"about_ca_system_score_codex":0.00036580025,"about_ca_system_score_gemma":0.00016692012,"threshold_uncertainty_score":0.08813971},"labels":[],"label_agreement":null},{"id":"W2059636550","doi":"10.1029/2005gl024897","title":"First detection of meso‐thermospheric Nitric Oxide (NO) by ground‐based FTIR solar absorption spectroscopy","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Stratosphere; Thermosphere; Fourier transform infrared spectroscopy; Absorption (acoustics); Environmental science; Atmospheric sciences; Absorption spectroscopy; Analytical Chemistry (journal); Spectroscopy; Materials science; Chemistry; Physics; Ionosphere; Optics; Environmental chemistry; Astronomy","score_opus":0.012535684697722113,"score_gpt":0.2413695372862373,"score_spread":0.22883385258851519,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059636550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964953,0.00026983305,0.0014316683,0.000061055616,0.000008045293,0.00001028115,0.00024633802,0.000032202475,0.001445163],"genre_scores_gemma":[0.9963257,0.00014659345,0.0027161862,0.00002522187,0.0000056396016,0.0000049708688,0.00029259824,0.000006165343,0.0004769552],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99992883,0.0000049491064,0.0000015930975,0.000023851917,0.000025907584,0.000014964703],"domain_scores_gemma":[0.99993515,0.000011927836,0.000011187238,0.000010590258,0.00001963974,0.000011409376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010325414,0.00016651333,0.000097591,0.00020067593,0.0002696511,0.00018778864,0.00024396725,0.0002751054,0.00046877138],"category_scores_gemma":[0.00017061505,0.00011959208,0.00011076296,0.00013549869,0.000245749,0.00019214174,0.00022936494,0.00021773553,0.00010718263],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022730345,0.000052134663,0.059554793,0.000079986756,0.00004149931,0.00023217335,0.00030642646,0.0007323143,0.9232983,0.00017208993,0.0005862382,0.014716833],"study_design_scores_gemma":[0.000032670978,0.00025138518,0.55628985,0.000022357743,0.00006489263,0.00040182713,0.00033187182,0.0113008795,0.42533845,0.00018882751,0.005746543,0.000030500656],"about_ca_topic_score_codex":0.013561072,"about_ca_topic_score_gemma":0.036380995,"teacher_disagreement_score":0.013561072,"about_ca_system_score_codex":0.000391863,"about_ca_system_score_gemma":0.0001906413,"threshold_uncertainty_score":0.026964247},"labels":[],"label_agreement":null},{"id":"W2059738590","doi":"10.1029/2004gl021750","title":"Hockey sticks, principal components, and spurious significance","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":178,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Principal component analysis; Spurious relationship; Statistics; Monte Carlo method; Statistic; Range (aeronautics); Mathematics; Engineering","score_opus":0.04602605845047049,"score_gpt":0.2993096214417604,"score_spread":0.2532835629912899,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2059738590","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":"methods","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":"methods","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22948396,0.001357921,0.7560417,0.0024877784,0.0004656933,0.00013610098,0.00024024611,0.0007203344,0.009066254],"genre_scores_gemma":[0.92681456,0.00016314523,0.070839375,0.00041926303,0.0001721347,0.00008129548,0.00019106014,0.00019964072,0.0011195086],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9721905,0.01767784,0.0011591166,0.00485941,0.0034640986,0.0006490497],"domain_scores_gemma":[0.6531064,0.28772926,0.011835603,0.040341664,0.0055382596,0.0014488697],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.045576524,0.00090131664,0.0010691156,0.0019502493,0.0021732904,0.0039437977,0.002413898,0.0019341828,0.00442498],"category_scores_gemma":[0.3039499,0.0007277303,0.0010088999,0.0019663724,0.010647437,0.0032274413,0.0029961916,0.0035819632,0.0004160203],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010386562,0.000101530466,0.1557109,0.00039351158,0.0010876638,0.0011837834,0.0027480498,0.089500435,0.002291574,0.56877995,0.009106875,0.16805716],"study_design_scores_gemma":[0.00014205143,0.00021352243,0.036166687,0.00018268332,0.0001562381,0.00079923635,0.0007782311,0.3268104,0.0040367106,0.6242892,0.0063064825,0.00011859088],"about_ca_topic_score_codex":0.0037880263,"about_ca_topic_score_gemma":0.0031159993,"teacher_disagreement_score":0.9544235,"about_ca_system_score_codex":0.0013636318,"about_ca_system_score_gemma":0.0014889636,"threshold_uncertainty_score":0.24103463},"labels":[],"label_agreement":null},{"id":"W2060161302","doi":"10.1029/2007gl030620","title":"Ozone depletion in the 2006/2007 Arctic winter","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"H2020 European Research Council; Canadian Space Agency; Tekes; Centre National d’Etudes Spatiales","keywords":"Ozone; Ozone depletion; Environmental science; Atmospheric sciences; Arctic; Climatology; Latitude; Polar vortex; Data assimilation; TRACER; Meteorology; Geology; Oceanography; Physics","score_opus":0.030412875038537353,"score_gpt":0.2965074422307591,"score_spread":0.26609456719222174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060161302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968606,0.00012328039,0.00011746301,0.00008589721,0.000015878177,0.000006081073,0.0018646829,0.000035102523,0.0008909565],"genre_scores_gemma":[0.99272233,0.00020673654,0.00036245422,0.000091107206,0.000017884657,0.000012735084,0.0061627356,0.000013883097,0.00041001904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998859,0.000009807889,0.0000082418865,0.00003201293,0.00003270593,0.000031412255],"domain_scores_gemma":[0.99981445,0.00001252367,0.000051680963,0.000010811048,0.00007821996,0.00003228916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002774333,0.00028743254,0.00040819254,0.00036767506,0.0005691596,0.00050901313,0.0002066649,0.0004920308,0.00033755729],"category_scores_gemma":[0.0002834382,0.00015194043,0.00038070406,0.0004808852,0.00013874775,0.00021401486,0.00025449926,0.0003835515,0.0001436767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019007826,0.0006056196,0.88448745,0.0002120854,0.0005151617,0.0007391024,0.000539057,0.03789047,0.04431241,0.0006738711,0.009729189,0.018394776],"study_design_scores_gemma":[0.000027565915,0.00013697783,0.97295296,0.000017031869,0.000072500916,0.00012727692,0.00022728134,0.014993998,0.007950861,0.00006814937,0.003403021,0.000022238646],"about_ca_topic_score_codex":0.0845443,"about_ca_topic_score_gemma":0.08602503,"teacher_disagreement_score":0.0845443,"about_ca_system_score_codex":0.001113208,"about_ca_system_score_gemma":0.00061471824,"threshold_uncertainty_score":0.16810441},"labels":[],"label_agreement":null},{"id":"W2060211264","doi":"10.1029/2005gl024234","title":"Observed twentieth century land surface air temperature and precipitation covariability","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"University of Northern British Columbia","keywords":"Precipitation; Climatology; Surface air temperature; Environmental science; Atmospheric sciences; Air temperature; Geography; Meteorology; Geology","score_opus":0.038909701184953946,"score_gpt":0.294984204334413,"score_spread":0.25607450314945907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060211264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99407095,0.000206769,0.0005512557,0.00012098976,0.00000970414,0.0000032643939,0.0028646758,0.00002057174,0.002151714],"genre_scores_gemma":[0.9971143,0.00017567,0.00013154879,0.000015938329,0.000006747316,0.000005133107,0.0021625815,0.0000042600227,0.00038382868],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.0000060993625,0.0000040046707,0.000028391316,0.00000995962,0.0000124341595],"domain_scores_gemma":[0.9997662,0.000045228997,0.000087520646,0.000031171734,0.00005124814,0.000018681427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001746532,0.00011665029,0.00009388366,0.00036398545,0.00019351867,0.00036221262,0.0001259967,0.00015886509,0.0014407398],"category_scores_gemma":[0.0010574028,0.00010540213,0.00014267802,0.0008279951,0.00013854522,0.00032070375,0.0003445745,0.0002352134,0.00016672541],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017333606,0.000030534244,0.9571725,0.000061131446,0.00015720478,0.00019853226,0.0005058036,0.009363916,0.009426388,0.0022925125,0.0019156851,0.018702464],"study_design_scores_gemma":[0.0000045432353,0.000009450051,0.9933808,0.0000041999265,0.000014277851,0.000070658076,0.000043751177,0.002558799,0.00075239385,0.00027374807,0.0028796373,0.000007754712],"about_ca_topic_score_codex":0.015483107,"about_ca_topic_score_gemma":0.019020373,"teacher_disagreement_score":0.015483107,"about_ca_system_score_codex":0.00043484147,"about_ca_system_score_gemma":0.0001342558,"threshold_uncertainty_score":0.030785978},"labels":[],"label_agreement":null},{"id":"W2060245706","doi":"10.1002/2014gl062543","title":"Small‐scale variability patterns of DMS and phytoplankton in surface waters of the tropical and subtropical Atlantic, Indian, and Pacific Oceans","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"Ministerio de Economía y Competitividad; Ministry of Earth Sciences; National Science Foundation","keywords":"Subtropics; Phytoplankton; Latitude; Oceanography; Environmental science; Salinity; Climatology; Tropical Atlantic; Sea surface temperature; Atmospheric sciences; Geology; Nutrient; Biology; Ecology","score_opus":0.02709691513457916,"score_gpt":0.23319256093944135,"score_spread":0.2060956458048622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060245706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997173,0.000018857574,0.000029171468,0.0000066923362,6.769638e-7,0.0000010792944,0.00005723945,0.0000019095796,0.00016711069],"genre_scores_gemma":[0.9997639,0.000016474225,0.000039226354,0.000004218473,0.0000017950357,0.0000014929615,0.0001287115,9.0744004e-7,0.00004329239],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999286,0.000011346173,0.0000062971867,0.000020424513,0.000016783597,0.000016552867],"domain_scores_gemma":[0.99966097,0.00009512122,0.00007229378,0.000025441668,0.00007600617,0.00007015244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002236813,0.00014472997,0.00018518126,0.0006835607,0.00028022382,0.000491071,0.00017405472,0.00014677251,0.00037423437],"category_scores_gemma":[0.00048566735,0.00014797851,0.00024598834,0.00063017977,0.00038044393,0.00022827389,0.00043603376,0.00014597153,0.00007389802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010391181,0.000020059624,0.9820711,0.00001421769,0.00007810168,0.000074009105,0.00042806455,0.000368134,0.013549406,0.00005390982,0.000049544462,0.0031896268],"study_design_scores_gemma":[0.000001259363,0.000007011861,0.9995597,7.0755107e-7,0.0000045995394,0.000010147392,0.00011571387,0.00015959212,0.00010653933,0.000007375271,0.000025973806,0.000001439216],"about_ca_topic_score_codex":0.02223432,"about_ca_topic_score_gemma":0.027172508,"teacher_disagreement_score":0.02223432,"about_ca_system_score_codex":0.00028823054,"about_ca_system_score_gemma":0.0002401606,"threshold_uncertainty_score":0.04420978},"labels":[],"label_agreement":null},{"id":"W2060398476","doi":"10.1029/2005gl024127","title":"Potential of MODIS EVI and surface temperature for directly estimating per‐pixel ecosystem C fluxes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":231,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Manitoba Medical Service Foundation; Texas Tech University; National Aeronautics and Space Administration","keywords":"Eddy covariance; Enhanced vegetation index; Primary production; Environmental science; Ecosystem respiration; Vegetation (pathology); Atmospheric sciences; Flux (metallurgy); Ecosystem; Remote sensing; Carbon flux; Range (aeronautics); Leaf area index; Vegetation Index; Normalized Difference Vegetation Index; Geology; Ecology","score_opus":0.013095540754217599,"score_gpt":0.2736018160358502,"score_spread":0.2605062752816326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060398476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81454223,0.0016252744,0.17507263,0.00036396505,0.00009083555,0.00012550209,0.0015273953,0.0010404128,0.005611795],"genre_scores_gemma":[0.8811411,0.0003250881,0.1171301,0.00007828909,0.00003905165,0.000102484904,0.0006368772,0.00010107458,0.00044593686],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99714583,0.0016823183,0.00010816876,0.0004920045,0.0004730018,0.00009863672],"domain_scores_gemma":[0.98860115,0.00801174,0.00060995365,0.001551345,0.0010559815,0.00016977747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007377776,0.0008559606,0.00065813895,0.0009182242,0.00032152818,0.0014992729,0.0009028191,0.0011263759,0.00079211936],"category_scores_gemma":[0.029351793,0.0007578286,0.0004945561,0.001775019,0.00034743344,0.0023813343,0.0008382757,0.00049277523,0.00041367186],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021820855,0.0005271419,0.40843588,0.0008308615,0.0013901067,0.0003373351,0.00064466905,0.22697605,0.05937125,0.0038855425,0.0015895128,0.29382965],"study_design_scores_gemma":[0.00014236382,0.0003954434,0.10333023,0.00008815964,0.0002771566,0.00042875385,0.00014885477,0.86361384,0.0242915,0.004388158,0.0027087808,0.00018674009],"about_ca_topic_score_codex":0.0056774323,"about_ca_topic_score_gemma":0.0069539137,"teacher_disagreement_score":0.007377776,"about_ca_system_score_codex":0.00047024176,"about_ca_system_score_gemma":0.00055038783,"threshold_uncertainty_score":0.039017856},"labels":[],"label_agreement":null},{"id":"W2060523373","doi":"10.1029/2002gl016250","title":"Differential mixing by breaking internal waves","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Eddy diffusion; Mixing (physics); Internal wave; Breaking wave; Thermal diffusivity; Geology; Temperature salinity diagrams; Mechanics; Atmospheric sciences; Salinity; Range (aeronautics); Turbulence; Geophysics; Environmental science; Oceanography; Physics; Thermodynamics; Wave propagation; Materials science","score_opus":0.018981432353179388,"score_gpt":0.2629172649873657,"score_spread":0.24393583263418628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060523373","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97349405,0.00056219636,0.020924507,0.00009282883,0.000029556597,0.000013400158,0.00013151777,0.00016795298,0.004583945],"genre_scores_gemma":[0.9976278,0.00018617955,0.0014654963,0.000015206992,0.0000052943974,0.0000063493767,0.00010359192,0.000013060044,0.0005769315],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998004,0.000031630443,0.000012741605,0.000044070464,0.000049437793,0.00006166173],"domain_scores_gemma":[0.99954885,0.0001346119,0.00011200992,0.000098522396,0.000039479848,0.00006648759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031861287,0.00046012472,0.00021347316,0.0005236651,0.00034174143,0.0012893878,0.0003772326,0.00034292677,0.001066766],"category_scores_gemma":[0.0013009036,0.00034383012,0.00043607267,0.00049634784,0.0007082938,0.0011001005,0.0014410713,0.0007722493,0.00015724932],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008109266,0.00010946804,0.03813513,0.00020032705,0.000094321374,0.00041703114,0.0004317892,0.04426043,0.82129204,0.048245326,0.00059978734,0.045403328],"study_design_scores_gemma":[0.00027765433,0.00037977673,0.049989335,0.000035990313,0.00017142236,0.00085832446,0.00020734513,0.41800994,0.4774609,0.04551874,0.006969174,0.00012141694],"about_ca_topic_score_codex":0.001310936,"about_ca_topic_score_gemma":0.00045917346,"teacher_disagreement_score":0.001310936,"about_ca_system_score_codex":0.00053898286,"about_ca_system_score_gemma":0.00021144257,"threshold_uncertainty_score":0.0039106607},"labels":[],"label_agreement":null},{"id":"W2060623760","doi":"10.1029/2007gl029895","title":"Spreading of near‐inertial energy in a 1/12° model of the North Atlantic Ocean","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Inertial wave; Mesoscale meteorology; Geology; Ocean gyre; Eddy; Forcing (mathematics); Anticyclone; Inertial frame of reference; Climatology; Dispersion (optics); Geophysics; Atmospheric sciences; Meteorology; Turbulence; Subtropics; Physics; Wave propagation","score_opus":0.02378841535987601,"score_gpt":0.2485273589402591,"score_spread":0.2247389435803831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060623760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940363,0.00007834474,0.0020084402,0.00026725215,0.000018042005,0.000008139323,0.00021151548,0.000047531543,0.0033245226],"genre_scores_gemma":[0.99807656,0.000097508135,0.00066592917,0.000035842622,0.000010186341,0.000011915685,0.00010548977,0.000018177067,0.000978211],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993205,0.00002274539,0.000003451889,0.000014599841,0.0000068096915,0.000020386618],"domain_scores_gemma":[0.9998461,0.00004480509,0.00003207078,0.000014233888,0.000018884626,0.000043964803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023680138,0.00036801942,0.00042560374,0.0002109271,0.0004605844,0.0009730045,0.0006969466,0.0012125925,0.0015346302],"category_scores_gemma":[0.00067304587,0.00043357653,0.0006342291,0.00024033857,0.00056028174,0.0004974223,0.0005434606,0.00067602715,0.00020009586],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011780943,0.00003870199,0.008097445,0.000011550153,0.00003725876,0.000100870246,0.000065061664,0.9865471,0.0019575094,0.0018042556,0.00023044155,0.0009920388],"study_design_scores_gemma":[0.0000534159,0.000034653996,0.002807654,0.000004069855,0.000021105021,0.000011914323,0.00004342839,0.9962024,0.0001234296,0.0004967915,0.00019109788,0.000010068378],"about_ca_topic_score_codex":0.11454266,"about_ca_topic_score_gemma":0.05167097,"teacher_disagreement_score":0.11454266,"about_ca_system_score_codex":0.0010806873,"about_ca_system_score_gemma":0.0008807271,"threshold_uncertainty_score":0.22775191},"labels":[],"label_agreement":null},{"id":"W2060756348","doi":"10.1029/2006gl027509","title":"Effect of temperature and atmospheric pressure on methane (CH<sub>4</sub>) ebullition from near‐surface peats","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Peat; Methane; Volume (thermodynamics); Environmental science; Atmospheric sciences; Flux (metallurgy); Atmosphere (unit); Atmospheric pressure; Greenhouse gas; Carbon dioxide; Bubble; Environmental chemistry; Chemistry; Geology; Meteorology; Thermodynamics; Mechanics; Physics; Oceanography; Ecology","score_opus":0.006569777558742922,"score_gpt":0.24995742086404082,"score_spread":0.2433876433052979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060756348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999498,0.00007770983,0.00017334554,0.000013858447,0.0000039372167,0.000001468913,0.000026124982,0.000006938915,0.000198656],"genre_scores_gemma":[0.99958616,0.000066009394,0.00016503995,0.0000066497773,0.0000016373574,0.000002139457,0.00003919788,0.000006905686,0.0001261796],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99988174,0.000026620859,0.000007411348,0.000026454029,0.000022248203,0.00003543304],"domain_scores_gemma":[0.9995547,0.00027660243,0.00004940901,0.000022542488,0.000040657396,0.00005605271],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022233577,0.00026257182,0.00031629906,0.000107693864,0.00022836664,0.0005282278,0.0001889163,0.00023304297,0.00063951744],"category_scores_gemma":[0.0008221153,0.00019450595,0.00022367128,0.00007491849,0.00035373456,0.00034518345,0.00029060492,0.0003490632,0.00012686037],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018680487,0.00022623307,0.015239592,0.00010739508,0.00005154966,0.00022586099,0.00010661086,0.015318219,0.960293,0.00016409547,0.000121158526,0.006278205],"study_design_scores_gemma":[0.00006278143,0.0012275267,0.07341354,0.000016031976,0.00006337492,0.00017485932,0.00020520165,0.0918978,0.8321458,0.00021895366,0.00052505994,0.000049042028],"about_ca_topic_score_codex":0.0051908256,"about_ca_topic_score_gemma":0.0035283004,"teacher_disagreement_score":0.0051908256,"about_ca_system_score_codex":0.00035197893,"about_ca_system_score_gemma":0.00024980635,"threshold_uncertainty_score":0.0103212},"labels":[],"label_agreement":null},{"id":"W2060897616","doi":"10.1002/grl.50438","title":"Stress tensor changes related to fluid injection at The Geysers geothermal field, California","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Helmholtz-Alberta Initiative","keywords":"Geothermal gradient; Geology; Cauchy stress tensor; Induced seismicity; Stress field; Principal stress; Seismology; Stress (linguistics); Focal mechanism; Orientation (vector space); Geophysics; Petrology; Viscous stress tensor; Geometry; Shear (geology); Mathematics; Physics; Finite element method","score_opus":0.0250694559058496,"score_gpt":0.2676124322029801,"score_spread":0.24254297629713048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060897616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926835,0.00001597835,0.00009606184,0.000010531506,0.0000012659441,0.000002478759,0.0002864168,0.000014879505,0.00030395135],"genre_scores_gemma":[0.9994286,0.000016126756,0.00013423587,0.0000024002195,0.0000017352055,0.0000025288684,0.00028192523,0.0000015910147,0.00013075965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.000004841866,0.000004362555,0.000026049469,0.00002360929,0.000016017177],"domain_scores_gemma":[0.99968445,0.00004343182,0.00010739898,0.000020977934,0.0001013378,0.000042489373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001696492,0.0002028962,0.00016147496,0.0006575803,0.0002935491,0.00031820455,0.00019512321,0.00016876246,0.00047726274],"category_scores_gemma":[0.0005035316,0.00013196269,0.000096596894,0.0005696396,0.00026856785,0.0001860976,0.0002449653,0.00019455882,0.00005188849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005057624,0.00012627551,0.9252852,0.000057787012,0.00011765962,0.00037294786,0.00066657446,0.018110339,0.037318606,0.00014905137,0.0010329637,0.016256807],"study_design_scores_gemma":[0.0000061973888,0.000024291125,0.9953381,0.0000033191282,0.000007494008,0.000017467732,0.00011212678,0.003048916,0.0012776249,0.000013813818,0.00014492084,0.000005723072],"about_ca_topic_score_codex":0.082410194,"about_ca_topic_score_gemma":0.13799083,"teacher_disagreement_score":0.082410194,"about_ca_system_score_codex":0.00056443905,"about_ca_system_score_gemma":0.00038295396,"threshold_uncertainty_score":0.16386104},"labels":[],"label_agreement":null},{"id":"W2060969197","doi":"10.1029/2008gl034456","title":"Annual period temperature and salinity signals of surface waters in Prince William Sound, Alaska","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"","keywords":"Salinity; Period (music); Oceanography; Climatology; Environmental science; Temperature salinity diagrams; Sound (geography); Geology","score_opus":0.020169573764263662,"score_gpt":0.2606775852549635,"score_spread":0.24050801149069984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2060969197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992217,0.000024906343,0.00008010767,0.000009484862,0.00000135052,0.0000015969538,0.0003011072,0.000005906282,0.00035391946],"genre_scores_gemma":[0.99883455,0.00006722287,0.0001855552,0.000004747948,0.0000018516574,0.0000037126454,0.00058281416,0.0000012662806,0.0003182561],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998852,0.000015342275,0.00001793348,0.000035159366,0.00003236297,0.000013993568],"domain_scores_gemma":[0.9994869,0.0000910194,0.00015411797,0.000033216143,0.0001778257,0.00005696897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031104643,0.000108255415,0.00009910811,0.0006773085,0.00031124635,0.0003330085,0.00016663164,0.00016966068,0.00033558073],"category_scores_gemma":[0.00088107167,0.00013670302,0.000097115124,0.00078016706,0.00022393909,0.00033734075,0.00034467326,0.00012216142,0.00010308443],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005965048,0.000013125609,0.98965746,0.000015252029,0.00003906475,0.00014333444,0.0006337008,0.0016769661,0.001583552,0.00003520829,0.00022898249,0.005913773],"study_design_scores_gemma":[0.0000016330847,0.000016406833,0.9981117,0.0000035831492,0.00000833805,0.000039372622,0.00046332623,0.00088765624,0.00017708077,0.00001556363,0.0002712349,0.000004001903],"about_ca_topic_score_codex":0.12631105,"about_ca_topic_score_gemma":0.226509,"teacher_disagreement_score":0.12631105,"about_ca_system_score_codex":0.000513955,"about_ca_system_score_gemma":0.0004037759,"threshold_uncertainty_score":0.25115168},"labels":[],"label_agreement":null},{"id":"W2061025621","doi":"10.1029/2007gl032165","title":"Wildfire smoke injection heights: Two perspectives from space","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":275,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Smoke; Environmental science; Aerosol; Lidar; Troposphere; Atmospheric sciences; Meteorology; Planetary boundary layer; Atmosphere (unit); Plume; Boundary layer; Remote sensing; Geology; Physics","score_opus":0.030585574955269774,"score_gpt":0.2955878523401755,"score_spread":0.2650022773849057,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061025621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85158974,0.021260194,0.029205438,0.009418456,0.00069313677,0.000035225086,0.003315649,0.0006956556,0.08378652],"genre_scores_gemma":[0.98672223,0.0034140716,0.0064456193,0.00035848955,0.00031685657,0.00001115216,0.001029754,0.00009141122,0.0016104577],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99952996,0.00008892461,0.000018821489,0.00008622321,0.000175557,0.000100582365],"domain_scores_gemma":[0.99866104,0.00049505424,0.00019400463,0.00014820775,0.0003454019,0.00015626384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094890466,0.000676233,0.00041766858,0.0021911405,0.00074746646,0.0035581277,0.00076979306,0.0011539387,0.0034847122],"category_scores_gemma":[0.0019743107,0.00031761717,0.0008013658,0.0018793851,0.0012738791,0.0040675793,0.0025425293,0.0017350817,0.00048401166],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013692827,0.00048279556,0.35473835,0.00070367364,0.00027355246,0.0017406874,0.010512336,0.0396111,0.022050766,0.16896768,0.010111841,0.3894379],"study_design_scores_gemma":[0.00016964182,0.001313997,0.5790425,0.0007771948,0.000481179,0.0017514445,0.021713916,0.14744757,0.023909433,0.13836451,0.084418945,0.0006097828],"about_ca_topic_score_codex":0.0141394,"about_ca_topic_score_gemma":0.021411413,"teacher_disagreement_score":0.0141394,"about_ca_system_score_codex":0.0013448431,"about_ca_system_score_gemma":0.00047464657,"threshold_uncertainty_score":0.0281142},"labels":[],"label_agreement":null},{"id":"W2061061173","doi":"10.1029/2008gl036412","title":"On the seasonal variability of eddy kinetic energy in the Gulf Stream region","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Baroclinity; Ekman transport; Kinetic energy; Dissipation; Environmental science; Climatology; Seasonality; Ekman layer; Atmospheric sciences; Oceanography; Geology; Physics; Mechanics","score_opus":0.030877879152209704,"score_gpt":0.2487110407583384,"score_spread":0.21783316160612867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061061173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99899656,0.00007437963,0.00007395433,0.00007426615,0.0000056222893,0.0000013731682,0.00019710643,0.000005150449,0.0005716478],"genre_scores_gemma":[0.99953413,0.0000535647,0.00004367307,0.00001734139,0.0000059466693,0.000001605606,0.00022947957,0.0000046668465,0.00010968064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998944,0.000022927816,0.000012341458,0.00002630232,0.000019696747,0.000024267556],"domain_scores_gemma":[0.99902725,0.00031245349,0.00021938546,0.00007539204,0.00024281231,0.00012271777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049212604,0.00012201183,0.00017264464,0.0006941903,0.00027478876,0.00052241056,0.00015569007,0.00029393556,0.0007182943],"category_scores_gemma":[0.0017367987,0.00015969084,0.0001858047,0.00068674615,0.00028595136,0.0002875315,0.0002872186,0.00022994544,0.000162322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003202975,0.00007034727,0.9748849,0.000028805449,0.00011613844,0.00022325912,0.00058418437,0.0027244817,0.011098736,0.00048364533,0.00089649804,0.008568593],"study_design_scores_gemma":[0.0000043194455,0.000012216442,0.9969103,0.0000071421973,0.0000101084,0.000030696785,0.00014159695,0.0023159839,0.00019453713,0.00007177448,0.0002969694,0.000004473396],"about_ca_topic_score_codex":0.01221515,"about_ca_topic_score_gemma":0.022606438,"teacher_disagreement_score":0.01221515,"about_ca_system_score_codex":0.00033736648,"about_ca_system_score_gemma":0.00023012793,"threshold_uncertainty_score":0.024288058},"labels":[],"label_agreement":null},{"id":"W2061072207","doi":"10.1029/2006gl027218","title":"Heat flux in magnetospheric convection: A calculation based on adiabatic drift theory","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Space Agency","funders":"","keywords":"Adiabatic process; Convection; Physics; Eulerian path; Heat flux; Flux (metallurgy); Mechanics; Classical mechanics; Thermodynamics; Heat transfer; Lagrangian; Materials science; Theoretical physics","score_opus":0.009176460318439897,"score_gpt":0.2599048857858421,"score_spread":0.2507284254674022,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061072207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.79685575,0.00080768246,0.18366458,0.0003259009,0.00008706634,0.000036736947,0.00010756796,0.0002323712,0.017882382],"genre_scores_gemma":[0.987914,0.00027455165,0.010652608,0.000017597491,0.000020877816,0.000019184961,0.000023654415,0.000036795227,0.0010407274],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9999658,0.000010245615,0.0000013423157,0.000004058916,0.000012140159,0.0000064924793],"domain_scores_gemma":[0.99990773,0.00004492646,0.000009378407,0.000011297382,0.00001655407,0.000010046154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002254129,0.00017911453,0.00024014368,0.00036941087,0.00039245648,0.00030916138,0.00046296112,0.00024191478,0.00083126995],"category_scores_gemma":[0.0007696108,0.00013584229,0.00028035181,0.00039966774,0.00045258284,0.0005985404,0.0004134895,0.00032775739,0.00011428966],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062048886,0.000030329515,0.003235134,0.00006907334,0.000036779787,0.00023698778,0.00016859767,0.8201366,0.009800474,0.14804739,0.0005689114,0.017607683],"study_design_scores_gemma":[0.000007089457,0.000015693648,0.0008438328,0.00000377154,0.0000065881036,0.000030823936,0.000011990571,0.9855274,0.0008914775,0.012181691,0.00047414404,0.0000055252885],"about_ca_topic_score_codex":0.002845478,"about_ca_topic_score_gemma":0.0012143239,"teacher_disagreement_score":0.002845478,"about_ca_system_score_codex":0.0005179523,"about_ca_system_score_gemma":0.00046757533,"threshold_uncertainty_score":0.005657792},"labels":[],"label_agreement":null},{"id":"W2061085839","doi":"10.1029/2007gl029957","title":"A twenty year reversal in water mass trends in the subtropical North Atlantic","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Thermocline; Water mass; Oceanography; Geology; Outflow; Salinity; North Atlantic Deep Water; Subtropics; Water column; Ekman transport; Temperature salinity diagrams; Climatology; Environmental science; Atmospheric sciences; Thermohaline circulation; Upwelling","score_opus":0.022997975690279213,"score_gpt":0.2687531644412066,"score_spread":0.2457551887509274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061085839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993655,0.00009993682,0.000026485923,0.00005325614,0.000008630704,0.0000012309084,0.00013175442,0.00000486616,0.00030839475],"genre_scores_gemma":[0.99926764,0.000086811575,0.000044616758,0.000046440877,0.0000064614933,0.0000021480885,0.000263553,9.2395703e-7,0.0002815094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993944,0.00000769064,0.0000070030346,0.000015485508,0.000015406567,0.000015018161],"domain_scores_gemma":[0.99969053,0.000023324179,0.00012700676,0.000024782352,0.00008082547,0.000053563585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023510534,0.00009828011,0.00009679809,0.00039340154,0.000253063,0.00033660556,0.00015045231,0.00023997658,0.00057714176],"category_scores_gemma":[0.00056335574,0.00006124353,0.00013548796,0.00040316547,0.00030244008,0.00017437481,0.0002725259,0.00015992002,0.00012571408],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034451068,0.0000467645,0.966437,0.0000477237,0.000088266796,0.00041249167,0.0008316453,0.0002064183,0.017143754,0.00012119774,0.00051618606,0.013804098],"study_design_scores_gemma":[0.0000015165034,0.000019810035,0.9993012,0.0000014354953,0.0000048231664,0.000030642084,0.00012340344,0.000035180477,0.00016140725,0.000006738913,0.00031195136,0.0000018021655],"about_ca_topic_score_codex":0.01791195,"about_ca_topic_score_gemma":0.040249307,"teacher_disagreement_score":0.01791195,"about_ca_system_score_codex":0.0004810427,"about_ca_system_score_gemma":0.0003282943,"threshold_uncertainty_score":0.035615385},"labels":[],"label_agreement":null},{"id":"W2061220904","doi":"10.1029/2004gl021894","title":"Auroral particles associated with a substorm brightening arc","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Air Force Research Laboratory; Japan Society for the Promotion of Science; Ministerio de Educación, Cultura y Deporte; Canadian Space Agency; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Substorm; Electron precipitation; Breakup; Geophysics; Plasma sheet; Latitude; Geology; Arc (geometry); Physics; Magnetosphere; Astrophysics; Plasma; Geodesy; Geometry","score_opus":0.019103431309144367,"score_gpt":0.27418212069406783,"score_spread":0.25507868938492345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061220904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995889,0.000042917218,0.000067341425,0.0000043169402,9.888225e-7,0.0000014484588,0.000037103593,0.0000054116726,0.00025157808],"genre_scores_gemma":[0.99938416,0.000036992693,0.00020089297,0.0000055773216,0.0000066889515,0.0000013787604,0.00019311509,0.0000028158033,0.00016831979],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995625,0.0000035369421,0.0000029674884,0.000010519717,0.000011839203,0.000014948054],"domain_scores_gemma":[0.99980205,0.000022049197,0.00008054192,0.00001604332,0.000036003406,0.00004329656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006783575,0.00010886224,0.00012473587,0.00049961003,0.00022420847,0.00033989735,0.00010483278,0.00013608564,0.00081639143],"category_scores_gemma":[0.00022294417,0.00009777515,0.000109060486,0.0003115061,0.00013250588,0.00013878533,0.00022579967,0.00014396869,0.0001114986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053998246,0.000048001006,0.559292,0.000043426295,0.00007576086,0.0015388393,0.00049844914,0.0003039879,0.4243571,0.0001391798,0.00023482516,0.012928408],"study_design_scores_gemma":[0.000005439977,0.0000628971,0.98752415,0.0000021375806,0.000015963733,0.0005592792,0.00009291627,0.00040188798,0.010796016,0.000023167762,0.00051270955,0.0000033709841],"about_ca_topic_score_codex":0.0024369145,"about_ca_topic_score_gemma":0.003454323,"teacher_disagreement_score":0.0024369145,"about_ca_system_score_codex":0.00015316012,"about_ca_system_score_gemma":0.000052972435,"threshold_uncertainty_score":0.0048455},"labels":[],"label_agreement":null},{"id":"W2061394982","doi":"10.1029/2006gl028430","title":"Migration characteristics of seismic tremors in the northern Cascadia margin","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Subduction; Seismology; Induced seismicity; Episodic tremor and slip; North American Plate; Plate tectonics; Slip (aerodynamics); Tectonics","score_opus":0.03176464825797792,"score_gpt":0.27900687758759707,"score_spread":0.24724222932961915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061394982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994259,0.000018411489,0.000028847873,0.0000075198072,5.785269e-7,0.0000017333153,0.00016592827,0.000008043268,0.00034298148],"genre_scores_gemma":[0.99936813,0.000019802183,0.000041103056,0.000002084008,0.0000015437809,0.0000028717977,0.00037396434,0.0000017436234,0.00018886194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998815,0.0000095954965,0.000012147463,0.00004080959,0.000029521898,0.00002636587],"domain_scores_gemma":[0.9995272,0.00005443027,0.00013959673,0.00003985965,0.000092284965,0.00014646979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013531018,0.00022203856,0.00019668048,0.001370764,0.0003607073,0.00033108634,0.00019439452,0.00018711161,0.00086297776],"category_scores_gemma":[0.0007781342,0.00016292877,0.00013861855,0.0011337899,0.00028871544,0.00013972877,0.00043749975,0.00011181195,0.00016267388],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016331673,0.0000252293,0.9809491,0.000021305623,0.000043711716,0.00043752862,0.0013638227,0.0009848507,0.008054389,0.000041146854,0.0002467618,0.007668731],"study_design_scores_gemma":[0.0000013024475,0.000010056201,0.99952745,0.0000012669923,0.000003426348,0.000042981792,0.00014641297,0.00011989158,0.000048565933,0.0000038199005,0.00009337058,0.0000014727646],"about_ca_topic_score_codex":0.058090813,"about_ca_topic_score_gemma":0.12245048,"teacher_disagreement_score":0.058090813,"about_ca_system_score_codex":0.0007148726,"about_ca_system_score_gemma":0.0002939283,"threshold_uncertainty_score":0.11550534},"labels":[],"label_agreement":null},{"id":"W2061414172","doi":"10.1029/2007gl032680","title":"Ice core record of rising lead pollution in the North Pacific atmosphere","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Heavy metals in environment","field":"Environmental Science","cited_by":114,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Ice core; Pollution; Lead (geology); Plateau (mathematics); Oceanography; Geology; Environmental science; Climatology; Physical geography; Geography; Paleontology","score_opus":0.061988534174727945,"score_gpt":0.30469388201418424,"score_spread":0.2427053478394563,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061414172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963683,0.00008853695,0.000042672433,0.00007839109,0.0000042018205,0.000003897964,0.0011542111,0.00001887318,0.0022410043],"genre_scores_gemma":[0.996788,0.00015292411,0.00024805774,0.000054617434,0.000014137835,0.000007561342,0.0021407923,0.000006610541,0.0005871832],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999653,0.000001995003,0.000002853641,0.000010281149,0.000011183319,0.000008398283],"domain_scores_gemma":[0.99986005,0.000009303152,0.000028879926,0.000011044564,0.00005634756,0.00003441571],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012599153,0.00012743444,0.0001482863,0.00054064736,0.00052866404,0.0004093836,0.00014475454,0.00016863908,0.00068648934],"category_scores_gemma":[0.00021459657,0.00011890685,0.00007064399,0.00067711005,0.00023516138,0.00023519051,0.000390835,0.00025661345,0.00015240909],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001777857,0.00006657567,0.94945824,0.00006294187,0.000068309724,0.0005274533,0.0006425651,0.00075831026,0.02929018,0.0001776896,0.0024434242,0.016326549],"study_design_scores_gemma":[0.0000036351048,0.000007475443,0.9981623,0.0000034990146,0.000008155113,0.000037456786,0.000056599885,0.00020881303,0.00037097523,0.000012480662,0.0011267074,0.0000017786748],"about_ca_topic_score_codex":0.0897907,"about_ca_topic_score_gemma":0.16049516,"teacher_disagreement_score":0.0897907,"about_ca_system_score_codex":0.00069705426,"about_ca_system_score_gemma":0.00047636306,"threshold_uncertainty_score":0.17853612},"labels":[],"label_agreement":null},{"id":"W2061749031","doi":"10.1029/1999gl008474","title":"Diffusion creep of fine‐grained garnetite: Implications for the flow strength of subducting slabs","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Polytechnique Montréal","funders":"","keywords":"Creep; Diffusion creep; Geology; Diffusion; Grain boundary diffusion coefficient; Grain boundary; Grain Boundary Sliding; Grain size; Lithosphere; Materials science; Mineralogy; Thermodynamics; Composite material; Microstructure; Seismology; Tectonics","score_opus":0.0337006040846132,"score_gpt":0.2932031854400066,"score_spread":0.2595025813553934,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061749031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994236,0.0001007236,0.00026291076,0.000022674149,0.0000011023326,0.0000028333864,0.000025000909,0.0000075400985,0.00015355031],"genre_scores_gemma":[0.9997396,0.000043214037,0.00012948326,0.0000032111418,5.385562e-7,0.0000016261251,0.000022267199,0.0000013848471,0.000058598147],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99995744,0.000004372239,0.0000039946553,0.000011658101,0.000010780995,0.000011729396],"domain_scores_gemma":[0.99985456,0.000032383898,0.000044454882,0.000013107246,0.000032352164,0.000023200964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017102536,0.00025171446,0.0002263765,0.00033498043,0.00023607277,0.0003368871,0.00017833455,0.00020746353,0.00042231035],"category_scores_gemma":[0.0004592523,0.00011453929,0.0001663716,0.00014356796,0.0005372546,0.00042113787,0.00021515139,0.00017086284,0.00003323086],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000115711024,0.000016286473,0.011743405,0.000036108348,0.0000061072756,0.00007132836,0.000050506405,0.001622447,0.98450154,0.0001688926,0.00000770577,0.001659928],"study_design_scores_gemma":[0.000054695993,0.00034105248,0.22427726,0.000025047571,0.000027554826,0.0004777571,0.00020702812,0.029293701,0.7436549,0.000957908,0.0006539074,0.000029163517],"about_ca_topic_score_codex":0.0053393873,"about_ca_topic_score_gemma":0.004003621,"teacher_disagreement_score":0.0053393873,"about_ca_system_score_codex":0.00048384123,"about_ca_system_score_gemma":0.00021148432,"threshold_uncertainty_score":0.0106166005},"labels":[],"label_agreement":null},{"id":"W2061842378","doi":"10.1029/2005gl023861","title":"Arctic Ocean change heralds North Atlantic freshening","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"","keywords":"Thermohaline circulation; Oceanography; Arctic dipole anomaly; North Atlantic Deep Water; Archipelago; Arctic; Geology; North Atlantic oscillation; Arctic ice pack; Climatology; Drift ice","score_opus":0.03980841355939079,"score_gpt":0.2724100164421643,"score_spread":0.23260160288277348,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061842378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9152653,0.004236844,0.00034941078,0.009332558,0.0005942267,0.000015171099,0.001892144,0.00007658727,0.0682377],"genre_scores_gemma":[0.9906093,0.0018980447,0.0000773401,0.0006666062,0.00021154186,0.000002421207,0.00037404898,0.000011156741,0.0061496296],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989855,0.000011719728,0.000005894072,0.000024378023,0.000029991601,0.000029493443],"domain_scores_gemma":[0.999603,0.00006603506,0.000113587645,0.000048817063,0.00007030334,0.00009838801],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003009068,0.00011230465,0.00013523654,0.00048839545,0.00048662495,0.0008614368,0.000102336155,0.0005225091,0.011411973],"category_scores_gemma":[0.0012006807,0.000079775265,0.00017433242,0.00050814176,0.0003607064,0.00056106894,0.00072673196,0.00044369278,0.00060219626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081446226,0.0001750879,0.72287583,0.0003173436,0.00020863647,0.0014945535,0.002997747,0.0013452925,0.008494358,0.020467756,0.027091766,0.21371728],"study_design_scores_gemma":[0.0000098764085,0.000067858826,0.915865,0.00006640488,0.00003263232,0.0002806181,0.0017117617,0.0003111531,0.0009212707,0.0023689563,0.07834982,0.000014733093],"about_ca_topic_score_codex":0.029708587,"about_ca_topic_score_gemma":0.04522861,"teacher_disagreement_score":0.029708587,"about_ca_system_score_codex":0.001234902,"about_ca_system_score_gemma":0.00048016175,"threshold_uncertainty_score":0.059071362},"labels":[],"label_agreement":null},{"id":"W2061943820","doi":"10.1029/2005gl022700","title":"Spreading of overflow water from the Greenland to the Labrador Sea","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Ocean gyre; Oceanography; Geology; Structural basin; Groenlandia; Climatology; Geomorphology; Fishery; Ice sheet","score_opus":0.02174280528435279,"score_gpt":0.2591239448514194,"score_spread":0.23738113956706658,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061943820","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980725,0.00010700882,0.00018599344,0.000029462612,0.0000025760623,0.0000040270943,0.0003621127,0.000021634494,0.0012145722],"genre_scores_gemma":[0.9977831,0.00013775483,0.0006311543,0.000027887645,0.0000016748438,0.0000048403494,0.0006362155,0.000008858057,0.0007684455],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998888,0.000008694621,0.000006203191,0.0000479023,0.000019531097,0.000028832157],"domain_scores_gemma":[0.9998759,0.000011950676,0.000054543067,0.000014242012,0.000020709422,0.00002254283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001623285,0.00027611418,0.00020112438,0.0008630834,0.00039684694,0.00073950173,0.00020929177,0.00014699744,0.00081022055],"category_scores_gemma":[0.00025062056,0.00009581673,0.0001833741,0.0007470865,0.00034625953,0.0003455087,0.0005676616,0.00020568632,0.00015972585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005006014,0.00003735159,0.8332096,0.00006464248,0.00007653182,0.0005844996,0.0016275904,0.0024687827,0.0999191,0.0005184077,0.0006463506,0.06034657],"study_design_scores_gemma":[0.0000074575346,0.000117794196,0.9838397,0.000016524322,0.00002501388,0.00012433006,0.0005715816,0.0011137496,0.010717656,0.0000748198,0.0033765507,0.00001465864],"about_ca_topic_score_codex":0.08670503,"about_ca_topic_score_gemma":0.14174017,"teacher_disagreement_score":0.08670503,"about_ca_system_score_codex":0.0019367049,"about_ca_system_score_gemma":0.00082594,"threshold_uncertainty_score":0.17240071},"labels":[],"label_agreement":null},{"id":"W2061987450","doi":"10.1029/2001gl013782","title":"Investigation of glacial isostatic adjustment in the northeast U.S. using GPS measurements","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Global Positioning System; Geology; Geodesy; Mantle (geology); Glacial period; Geophysics; Geomorphology","score_opus":0.1845133973571646,"score_gpt":0.3030379653866426,"score_spread":0.11852456802947803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2061987450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999005,0.000055119694,0.00014255545,0.000036781206,0.0000012723802,0.000001563345,0.00026170292,0.0000060273037,0.00048999727],"genre_scores_gemma":[0.9993125,0.000053467502,0.00019425398,0.000008752745,0.0000023003533,0.0000014435386,0.00035955847,0.0000015905266,0.00006617143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989307,0.00003328699,0.000010372357,0.000026302185,0.000024507961,0.000012384713],"domain_scores_gemma":[0.9993544,0.00013252404,0.0002630606,0.000054412038,0.0001445266,0.000051106115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028872892,0.00015698564,0.00014085797,0.000928442,0.0002964256,0.00042448542,0.00017372146,0.00014971515,0.0003481179],"category_scores_gemma":[0.0017104767,0.00014348408,0.00010720195,0.0015546646,0.000263282,0.00030771462,0.000327338,0.0001593837,0.000073024814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028944078,0.000008146942,0.9929496,0.0000056411764,0.00002415206,0.000035278044,0.00036852754,0.000647072,0.00072756,0.00008077766,0.00010946532,0.005014903],"study_design_scores_gemma":[0.0000015269803,0.000009478737,0.9981718,0.0000031428833,0.0000070541364,0.000017950279,0.00012719279,0.0012141152,0.00012214607,0.000023367811,0.0002999804,0.0000022324286],"about_ca_topic_score_codex":0.09384732,"about_ca_topic_score_gemma":0.25445774,"teacher_disagreement_score":0.09384732,"about_ca_system_score_codex":0.00047724272,"about_ca_system_score_gemma":0.00032525687,"threshold_uncertainty_score":0.18660218},"labels":[],"label_agreement":null},{"id":"W2062242883","doi":"10.1029/2009gl038837","title":"Contribution of under‐ice primary production to an ice‐edge upwelling phytoplankton bloom in the Canadian Beaufort Sea","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":254,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; University of Manitoba; Institut National de la Recherche Scientifique; Université du Québec à Rimouski","funders":"Bayer Canada","keywords":"Upwelling; Sea ice; Oceanography; Phytoplankton; Arctic sea ice decline; Environmental science; Arctic ice pack; Arctic; Antarctic sea ice; Hydrography; Cryosphere; Bloom; Geology; Climatology; Nutrient; Ecology; Biology","score_opus":0.024655260317499227,"score_gpt":0.275078469718741,"score_spread":0.2504232094012418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062242883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876,0.0001774019,0.00004486659,0.000049287213,0.0000031787533,0.0000035234816,0.00024999792,0.0000048137877,0.00070687215],"genre_scores_gemma":[0.9989691,0.00019894,0.000122042824,0.000023883968,0.0000028245452,0.0000022543843,0.00032143146,0.000004112681,0.0003553917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973243,0.000013889699,0.000007990161,0.000037330698,0.000095066716,0.00011325436],"domain_scores_gemma":[0.99941087,0.000056252946,0.000085677886,0.000027245556,0.00025134167,0.0001686582],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023687996,0.000344678,0.0002993274,0.00093856297,0.0015783859,0.0008379794,0.00030925157,0.00024851094,0.00053667935],"category_scores_gemma":[0.0007159755,0.00023713373,0.00025269552,0.0009189721,0.0006126664,0.00023150051,0.0005649743,0.00025708217,0.00005706725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039702872,0.00003069374,0.9510171,0.00005242296,0.00008502808,0.00041588017,0.00086065894,0.0015989625,0.029776858,0.0001557164,0.00058401865,0.015025605],"study_design_scores_gemma":[0.0000012511816,0.000007748323,0.99892384,0.0000016399298,0.000006947241,0.000029989722,0.00011300326,0.00026907842,0.00032774912,0.000008867786,0.0003062723,0.0000036280178],"about_ca_topic_score_codex":0.96853405,"about_ca_topic_score_gemma":0.9800417,"teacher_disagreement_score":0.031465948,"about_ca_system_score_codex":0.011091564,"about_ca_system_score_gemma":0.0076398375,"threshold_uncertainty_score":0.08047527},"labels":[],"label_agreement":null},{"id":"W2062283819","doi":"10.1029/2002gl015441","title":"Unbending combined with dehydration embrittlement as a cause for double and triple seismic zones","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Embrittlement; Slab; Induced seismicity; Geology; Fluid pressure; Mantle (geology); Seismology; Crust; Dehydration; Materials science; Geophysics; Composite material; Chemistry; Mechanics","score_opus":0.0643301016988033,"score_gpt":0.29469308589187004,"score_spread":0.23036298419306675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062283819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9824614,0.0003268222,0.012067648,0.00030794737,0.000070475704,0.000025558833,0.00006271055,0.00014494157,0.004532443],"genre_scores_gemma":[0.99863094,0.000072899704,0.0006249623,0.000011276308,0.0000072354223,0.0000043713217,0.000016775537,0.000013219876,0.0006182565],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99986076,0.000012213154,0.000009742721,0.000026628933,0.000035192257,0.00005541759],"domain_scores_gemma":[0.9996755,0.00005181254,0.00012083747,0.000037711503,0.000028987411,0.00008520273],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024363042,0.00094679964,0.0004947744,0.00070192886,0.0005557916,0.00080067274,0.00096778787,0.0008070298,0.0021567363],"category_scores_gemma":[0.00063403696,0.0005256798,0.0008976985,0.00031465958,0.00083382684,0.0005770948,0.0017416195,0.0007074249,0.00025435397],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010841021,0.00019820481,0.13431944,0.00035767627,0.00020788037,0.015640222,0.0007997144,0.4656802,0.28528884,0.05899317,0.0016606807,0.03576988],"study_design_scores_gemma":[0.00015063118,0.0003384775,0.07355681,0.000031335352,0.00020743713,0.0044674105,0.0006770053,0.8612701,0.039662458,0.015866332,0.0036661422,0.00010592851],"about_ca_topic_score_codex":0.0050409567,"about_ca_topic_score_gemma":0.0046669166,"teacher_disagreement_score":0.0050409567,"about_ca_system_score_codex":0.00058916473,"about_ca_system_score_gemma":0.00055169826,"threshold_uncertainty_score":0.010023177},"labels":[],"label_agreement":null},{"id":"W2062401828","doi":"10.1029/2008gl034250","title":"Relative importance of dynamical and chemical contributions to Arctic wintertime ozone","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Ozone; Diabatic; Polar vortex; Atmospheric sciences; Chemical transport model; Arctic; Environmental science; Climatology; Ozone depletion; Ozone layer; Stratosphere; Vortex; Flux (metallurgy); Meteorology; Oceanography; Geology; Chemistry; Physics","score_opus":0.02027158242686448,"score_gpt":0.287765495226324,"score_spread":0.2674939127994595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062401828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944734,0.001097623,0.0021398824,0.000095817035,0.000026702068,0.000006240629,0.0005156856,0.000030575062,0.0016142256],"genre_scores_gemma":[0.9977958,0.00058199104,0.00043616557,0.000020254403,0.0000451032,0.0000068366076,0.0007682076,0.00001890801,0.00032678043],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998832,0.000022033579,0.000010413307,0.000028453265,0.000029390028,0.000026518604],"domain_scores_gemma":[0.9995635,0.00015382258,0.00007229389,0.00003289289,0.00013290963,0.00004461218],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039725058,0.00050660886,0.00032775893,0.0009240523,0.00040380534,0.0006818982,0.0002490337,0.00022997569,0.00089980854],"category_scores_gemma":[0.0010671685,0.00033904068,0.00045754877,0.0005270947,0.00019040897,0.00052059937,0.00058551953,0.00017694716,0.00010206366],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050476415,0.00009953192,0.76249474,0.0003328601,0.0011649274,0.00029163386,0.00023730997,0.06004699,0.12137288,0.003025917,0.0004719166,0.049956556],"study_design_scores_gemma":[0.000017541235,0.00008427803,0.9342868,0.00002497696,0.00027163824,0.00013929527,0.00011714713,0.054790825,0.007507824,0.00093552057,0.0017957627,0.00002847957],"about_ca_topic_score_codex":0.0068855733,"about_ca_topic_score_gemma":0.008704868,"teacher_disagreement_score":0.0068855733,"about_ca_system_score_codex":0.00035349542,"about_ca_system_score_gemma":0.00033053884,"threshold_uncertainty_score":0.013691008},"labels":[],"label_agreement":null},{"id":"W2062829368","doi":"10.1029/1999gl011161","title":"An empirical model of the ionospheric electric potential","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; U.S. Geological Survey; University of Leicester; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; Southwest Research Institute; Air Force Research Laboratory; National Science Foundation","keywords":"Ionosphere; Empirical modelling; Electric field; Linear model; Interplanetary magnetic field; Geophysics; Linear regression; Electric potential; Interplanetary spaceflight; Physics; Computer science; Computational physics; Magnetic field; Solar wind; Voltage; Simulation","score_opus":0.01652944466460796,"score_gpt":0.29669587766193645,"score_spread":0.28016643299732846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062829368","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.52134234,0.0002503684,0.45746955,0.0014091438,0.0000516655,0.000042798438,0.000982034,0.00052267965,0.017929481],"genre_scores_gemma":[0.9879446,0.00014492607,0.00866414,0.00004845623,0.00002261094,0.00003672807,0.0002978845,0.000032750842,0.0028079401],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984384,0.000038614737,0.000006212413,0.000059301063,0.00002920102,0.000022775244],"domain_scores_gemma":[0.99937516,0.00028819614,0.00011908743,0.00006659787,0.0001243703,0.00002655591],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041805417,0.000259695,0.00022178802,0.00026186055,0.0001512799,0.0006821231,0.0008876832,0.00062968413,0.0020861032],"category_scores_gemma":[0.0029143973,0.0001972371,0.00022484409,0.00039062637,0.00046505613,0.0014805469,0.00034212592,0.0006845278,0.00036214115],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017860613,0.000022893666,0.005522086,0.000016261374,0.00002363107,0.0000684209,0.00008937881,0.96173304,0.0012213916,0.024829678,0.0006001262,0.005855142],"study_design_scores_gemma":[0.0000055583973,0.000008936468,0.0014773586,0.0000027175631,0.0000034273044,0.0000289048,0.000011769956,0.992695,0.000095356605,0.0050625647,0.00060367,0.0000047519106],"about_ca_topic_score_codex":0.007007239,"about_ca_topic_score_gemma":0.002677944,"teacher_disagreement_score":0.007007239,"about_ca_system_score_codex":0.0004690554,"about_ca_system_score_gemma":0.0005421565,"threshold_uncertainty_score":0.013932884},"labels":[],"label_agreement":null},{"id":"W2062950450","doi":"10.1029/2003gl018481","title":"High Arctic observations of mesospheric inversion layers","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Middle latitudes; Inversion (geology); Arctic; Atmospheric sciences; Geology; Lidar; The arctic; Rayleigh scattering; Climatology; Oceanography; Remote sensing; Physics; Geomorphology; Optics","score_opus":0.024872846311791423,"score_gpt":0.2735856957155448,"score_spread":0.24871284940375338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2062950450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972887,0.0001941283,0.0002499262,0.00002104396,0.000007017908,0.0000012150648,0.00053690176,0.000016999293,0.0016840829],"genre_scores_gemma":[0.99861693,0.00013441562,0.00032523755,0.000008469959,0.000009196262,0.0000015520144,0.00069321145,0.0000032790285,0.0002077647],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999871,0.000020210306,0.0000056672307,0.000028495608,0.000039483835,0.000035060697],"domain_scores_gemma":[0.99973613,0.000045505963,0.00006506585,0.000023530525,0.00009117678,0.00003856156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003004413,0.00013070884,0.00013434327,0.00039705355,0.00032187198,0.00035393238,0.00008366325,0.000119118165,0.00028068852],"category_scores_gemma":[0.00036336883,0.000107329404,0.00010500266,0.0003572544,0.000093617346,0.000119722026,0.00029315893,0.00017893923,0.00012069647],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081786455,0.000053041837,0.8592333,0.000058704343,0.00014454448,0.00027134054,0.0007490242,0.0016572652,0.10665684,0.00045525725,0.0010723455,0.02883047],"study_design_scores_gemma":[0.0000055572277,0.000024036493,0.99120164,0.000009658659,0.000023503211,0.000088934474,0.000134205,0.00094106945,0.0056605237,0.00004068476,0.0018637736,0.0000064184505],"about_ca_topic_score_codex":0.013270679,"about_ca_topic_score_gemma":0.029195877,"teacher_disagreement_score":0.013270679,"about_ca_system_score_codex":0.00024271948,"about_ca_system_score_gemma":0.00017220007,"threshold_uncertainty_score":0.026386857},"labels":[],"label_agreement":null},{"id":"W2063014502","doi":"10.1029/2004gl021722","title":"Density enhancement in plasmasphere‐ionosphere plasma during the 2003 Halloween Superstorm: Observations along the 330th magnetic meridian in North America","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Resources Canada","keywords":"Plasmasphere; Ionosphere; Magnetosphere; Geophysics; Geomagnetic storm; Solar wind; Total electron content; Atmospheric sciences; Geology; Field line; Physics; TEC; Plasma","score_opus":0.016132953502268926,"score_gpt":0.2473461890800158,"score_spread":0.23121323557774687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063014502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993445,0.000031922267,0.00003819141,0.000022703038,0.0000015863737,0.0000022935137,0.00010120822,0.000007901375,0.00044966786],"genre_scores_gemma":[0.99937326,0.000057764966,0.000114517505,0.000016165142,0.0000057225125,0.0000039872,0.00021544338,0.0000020268815,0.00021113735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999747,0.0000028253914,0.0000010074878,0.00000495692,0.00000751584,0.00000900621],"domain_scores_gemma":[0.99992347,0.000008234943,0.00002369108,0.0000034907705,0.000019825111,0.00002134872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000066548266,0.000093946175,0.00011085415,0.0003312518,0.00038887025,0.0002444264,0.00011672618,0.00014880755,0.0004545453],"category_scores_gemma":[0.00013492006,0.00010948102,0.000061897605,0.00025894263,0.00016832919,0.00015353838,0.0002402133,0.00015541626,0.00008213217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004995365,0.00005819139,0.8413521,0.000053758627,0.000067258035,0.0009655443,0.0030481587,0.00036245037,0.13742602,0.000120327,0.0014600483,0.014586682],"study_design_scores_gemma":[0.0000046731343,0.000021344067,0.9980081,0.000002560112,0.000005507884,0.00006805842,0.00027715063,0.00015616436,0.0010760748,0.000010584373,0.00036779404,0.000002095803],"about_ca_topic_score_codex":0.035167355,"about_ca_topic_score_gemma":0.097682886,"teacher_disagreement_score":0.96483266,"about_ca_system_score_codex":0.00033193777,"about_ca_system_score_gemma":0.00019119853,"threshold_uncertainty_score":0.06992537},"labels":[],"label_agreement":null},{"id":"W2063798466","doi":"10.1029/2001gl013037","title":"Anthropogenic signals recorded in an ice core from Eclipse Icefield, Yukon Territory, Canada","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ice core; Eclipse; Sulfate; Ice field; Arctic; Environmental science; Climatology; Nitrate; Physical geography; Oceanography; Precipitation; Atmospheric sciences; Geology; Geography; Meteorology; Chemistry","score_opus":0.07808680244205896,"score_gpt":0.3116128008650691,"score_spread":0.23352599842301014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2063798466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972952,0.000080789214,0.000036378176,0.000022848903,0.000003449553,0.000007682031,0.0017548366,0.0000034274055,0.0007953393],"genre_scores_gemma":[0.99477273,0.00021321153,0.0001276047,0.000033977834,0.0000043007153,0.000010887167,0.0037587266,0.000003207801,0.0010754672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998779,0.0000060354537,0.0000057515836,0.00001889755,0.000041090152,0.000050319362],"domain_scores_gemma":[0.9995931,0.000023760962,0.00004924419,0.000009967594,0.0002413679,0.000082515784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010313073,0.00022161049,0.00021184637,0.0008678822,0.001110852,0.0005652533,0.00029184046,0.00017343479,0.00054977596],"category_scores_gemma":[0.00033780225,0.0001088036,0.00010171544,0.0018179968,0.00032886257,0.00014573244,0.0003459456,0.00016971843,0.00008883679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001485783,0.00002758682,0.98817855,0.00003151707,0.00003573229,0.0002612574,0.001039063,0.00020360471,0.0048050596,0.000056232526,0.0007851488,0.004427549],"study_design_scores_gemma":[0.0000013413273,0.00000594877,0.99878174,0.0000032497464,0.0000032585385,0.00002618168,0.00046923218,0.000077314886,0.0001599785,0.0000026231928,0.00046735315,0.0000018619112],"about_ca_topic_score_codex":0.96246904,"about_ca_topic_score_gemma":0.9875687,"teacher_disagreement_score":0.03753096,"about_ca_system_score_codex":0.005849223,"about_ca_system_score_gemma":0.005361958,"threshold_uncertainty_score":0.075503945},"labels":[],"label_agreement":null},{"id":"W2064102246","doi":"10.1029/2005gl022737","title":"On sea ice concentration anomaly coherence in the southern Beaufort Sea","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Upwelling; Geology; Sea ice; Lead (geology); Coherence (philosophical gambling strategy); Oceanography; Climatology; Submarine pipeline; Circumpolar star; Anomaly (physics); Forcing (mathematics); Arctic ice pack; Geomorphology","score_opus":0.023975587029970987,"score_gpt":0.27173686778561196,"score_spread":0.24776128075564097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064102246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994456,0.000023596574,0.000024222982,0.000024690564,7.675901e-7,5.5135956e-7,0.00011385454,0.0000030549882,0.00036361566],"genre_scores_gemma":[0.9996761,0.000010918246,0.000023507759,0.000007541068,0.0000026163034,5.148555e-7,0.00021905739,0.0000013512166,0.000058448877],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984026,0.000025062143,0.000008949487,0.00003583713,0.00004292523,0.00004698574],"domain_scores_gemma":[0.99855834,0.0003655386,0.00055274775,0.000094211806,0.00031236935,0.000116881856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026558025,0.00007631432,0.000107595835,0.0007820652,0.00027017505,0.00056021847,0.00018795973,0.00018475567,0.000863598],"category_scores_gemma":[0.002163281,0.00009806339,0.00011295722,0.0010273752,0.000427943,0.00032266282,0.00035299544,0.00013427589,0.00010544224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052954983,0.0000089748855,0.99418914,0.0000031912832,0.000027582104,0.00007881666,0.00032615114,0.00051158067,0.00093493523,0.00007591023,0.00020761898,0.003583165],"study_design_scores_gemma":[8.4913034e-7,0.0000040680166,0.9993445,9.1886983e-7,0.0000017970398,0.000010283502,0.00007332797,0.0004259656,0.00003748685,0.000009781268,0.000089977155,0.0000010213312],"about_ca_topic_score_codex":0.16471373,"about_ca_topic_score_gemma":0.26289704,"teacher_disagreement_score":0.16471373,"about_ca_system_score_codex":0.00082109903,"about_ca_system_score_gemma":0.00045174704,"threshold_uncertainty_score":0.32751},"labels":[],"label_agreement":null},{"id":"W2064597380","doi":"10.1029/2008gl033666","title":"Intensification of preexisting auroral arc at substorm expansion phase onset: Wave‐like disruption during the first tens of seconds","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University; University of Calgary; Canadian Space Agency","funders":"","keywords":"Substorm; Gyroradius; Longitude; Arc (geometry); Geophysics; Geology; Plasma sheet; Phase (matter); Physics; Geodesy; Plasma; Magnetosphere; Instability; Latitude; Mechanics; Geometry","score_opus":0.03596437644456421,"score_gpt":0.29401689462310393,"score_spread":0.2580525181785397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064597380","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959793,0.0001522473,0.0011453133,0.000017762148,0.0000031430968,0.000014050963,0.0006778796,0.0000660343,0.001944286],"genre_scores_gemma":[0.9982083,0.0000752252,0.00041310093,0.0000051389497,0.000007863481,0.0000070635433,0.0010563621,0.0000064095943,0.00022050242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.0000057017132,0.000003737207,0.000015336627,0.000014913358,0.000014215153],"domain_scores_gemma":[0.9994454,0.00011762817,0.00021189312,0.00006556285,0.00008494615,0.0000746407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001634421,0.00008517211,0.00013494077,0.00075257034,0.00017560118,0.00033121198,0.000106348714,0.00008813652,0.0011441599],"category_scores_gemma":[0.00066240446,0.000060106886,0.00010286761,0.0005518692,0.00014471397,0.00025786893,0.0003003594,0.00016587421,0.0001573297],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005292584,0.00004614823,0.91070515,0.00009474106,0.00005602242,0.0007994986,0.0009202879,0.0008240872,0.05180883,0.00077734876,0.0009733572,0.032465238],"study_design_scores_gemma":[0.0000024208357,0.00002362047,0.9967512,0.0000031080501,0.000008088553,0.00021394221,0.000062852065,0.00043531205,0.0016947425,0.000064743086,0.00073768094,0.0000023582936],"about_ca_topic_score_codex":0.0019986227,"about_ca_topic_score_gemma":0.0037523946,"teacher_disagreement_score":0.0019986227,"about_ca_system_score_codex":0.00016628533,"about_ca_system_score_gemma":0.00007155992,"threshold_uncertainty_score":0.003973961},"labels":[],"label_agreement":null},{"id":"W2064605859","doi":"10.1029/2000gl011836","title":"CO<sub>2</sub> levels required for deglaciation of a “near‐snowball” Earth","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Snowball Earth; Deglaciation; Geology; Ice sheet; Glacial period; Climate model; Ice age; Ice-sheet model; Sea ice; Atmosphere (unit); Climatology; Equator; Sea ice growth processes; Atmospheric sciences; Environmental science; Cryosphere; Oceanography; Climate change; Antarctic sea ice; Geomorphology; Meteorology; Geodesy","score_opus":0.04553483647548488,"score_gpt":0.31071640095480707,"score_spread":0.2651815644793222,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064605859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99588335,0.00007160556,0.0016550365,0.000087213586,0.000015098464,0.000012815894,0.00023506967,0.000064955435,0.0019749398],"genre_scores_gemma":[0.99842936,0.000038927825,0.00060613983,0.00005542678,0.0000031206548,0.000014345228,0.00041607564,0.000016716705,0.00041991926],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998851,0.000013460331,0.000008135261,0.000023140396,0.000023230588,0.000046905912],"domain_scores_gemma":[0.9997323,0.00005687063,0.00006505213,0.000020707275,0.000028687748,0.00009624632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018327235,0.00022951393,0.0002976317,0.00012548246,0.00026147286,0.0005773908,0.0002011328,0.0003064937,0.0022723554],"category_scores_gemma":[0.0006803251,0.00019499878,0.00029444744,0.000113796705,0.00026911584,0.00038813715,0.00038442563,0.0005936997,0.0002520908],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011235263,0.00018216432,0.04583715,0.00019509078,0.000112321024,0.00095604797,0.00012261875,0.1240911,0.8153719,0.005026755,0.0009028321,0.006078419],"study_design_scores_gemma":[0.0002829627,0.0013280775,0.23358244,0.000032402517,0.00019101714,0.0008406606,0.0009257316,0.1967528,0.5494368,0.007886103,0.008657433,0.00008362399],"about_ca_topic_score_codex":0.0038269877,"about_ca_topic_score_gemma":0.0053296313,"teacher_disagreement_score":0.0038269877,"about_ca_system_score_codex":0.00052247575,"about_ca_system_score_gemma":0.00048939575,"threshold_uncertainty_score":0.007609427},"labels":[],"label_agreement":null},{"id":"W2064731502","doi":"10.1029/2007gl030642","title":"Amplification of Holocene multicentennial climate forcing by mode transitions in North Atlantic overturning circulation","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Forcing (mathematics); Thermohaline circulation; Climatology; Holocene; North Atlantic Deep Water; Geology; Oceanography; Shutdown of thermohaline circulation; Atlantic Equatorial mode; Climate model; Climate change; Climate state; Global warming; Effects of global warming","score_opus":0.031229956108011173,"score_gpt":0.30513423182518284,"score_spread":0.2739042757171717,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064731502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99577904,0.000022447019,0.0029542542,0.0000866963,0.000005273148,0.0000016802477,0.000031141426,0.00005132331,0.0010682271],"genre_scores_gemma":[0.99969304,0.000008382987,0.00017964037,0.0000049896767,0.0000018205246,0.0000012960584,0.000009798836,0.0000039342162,0.0000971303],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999956,0.000010555208,0.000002468072,0.000011903733,0.0000060590864,0.0000129057025],"domain_scores_gemma":[0.9998578,0.000049916627,0.000036958903,0.000017155995,0.000012381631,0.000025820995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015361643,0.00019508397,0.00014155921,0.00012223763,0.00026055757,0.00045222836,0.00021266175,0.0002946665,0.00087930873],"category_scores_gemma":[0.00075718435,0.0001665565,0.00036200587,0.00007917737,0.00035497046,0.00038461917,0.00047042107,0.0002828117,0.0000674614],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040879182,0.00011544564,0.13359775,0.000047360503,0.0001801727,0.0005356281,0.00044818115,0.7790963,0.05883726,0.010192767,0.000886798,0.01565354],"study_design_scores_gemma":[0.000036060977,0.000050182683,0.06544045,0.000003793629,0.00003951533,0.00007226066,0.00004285133,0.9299519,0.001512483,0.002560319,0.0002713911,0.000018681125],"about_ca_topic_score_codex":0.00631001,"about_ca_topic_score_gemma":0.006602986,"teacher_disagreement_score":0.00631001,"about_ca_system_score_codex":0.0005153752,"about_ca_system_score_gemma":0.00022255826,"threshold_uncertainty_score":0.012546599},"labels":[],"label_agreement":null},{"id":"W2064862074","doi":"10.1029/2001gl013125","title":"Multidomain hematite: A source of planetary magnetic anomalies?","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Hematite; Magnetite; Thermoremanent magnetization; Magnetization; Mars Exploration Program; Condensed matter physics; Demagnetizing field; Geology; Natural remanent magnetization; Magnetic field; Materials science; Mineralogy; Physics; Astrobiology; Remanence","score_opus":0.018766483475862367,"score_gpt":0.2771483497897367,"score_spread":0.25838186631387433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064862074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913434,0.0020415513,0.0033211745,0.0008219398,0.00003359982,0.00000420738,0.0001065683,0.000100142024,0.0022275695],"genre_scores_gemma":[0.9980616,0.00044757422,0.0007910747,0.00003611693,0.000017536388,0.0000010977261,0.000039188333,0.0000054474453,0.00060044264],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999788,0.0000013924472,5.63622e-7,0.000008720667,0.0000047271624,0.000005688072],"domain_scores_gemma":[0.9999316,0.000012151362,0.000025494759,0.000011406378,0.0000073648825,0.000011974684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055593642,0.000127889,0.00014075177,0.00029555953,0.0002601656,0.0003946593,0.00021119011,0.00035160483,0.0008820069],"category_scores_gemma":[0.0001693565,0.000111406356,0.00004856837,0.00023258968,0.00029068752,0.00036636597,0.00026439838,0.00022756393,0.00019146709],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021661384,0.000037588605,0.04067526,0.00015227176,0.000029558918,0.0012555128,0.00011754089,0.0006345159,0.9078562,0.008865973,0.0005449407,0.03961396],"study_design_scores_gemma":[0.00006692182,0.00020347782,0.276448,0.000066124,0.00010754007,0.0072832047,0.0007094207,0.015353206,0.63835645,0.03235028,0.029016018,0.00003939169],"about_ca_topic_score_codex":0.0004672256,"about_ca_topic_score_gemma":0.00073614967,"teacher_disagreement_score":0.0008820069,"about_ca_system_score_codex":0.00020757728,"about_ca_system_score_gemma":0.00015286801,"threshold_uncertainty_score":0.0029506087},"labels":[],"label_agreement":null},{"id":"W2064872575","doi":"10.1029/2005gl023213","title":"The relationship between the 0°C isotherm and atmospheric forcing in the Arctic Ocean","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Empirical orthogonal functions; Climatology; North Atlantic oscillation; Archipelago; Forcing (mathematics); Arctic; Environmental science; Mixed layer; Arctic oscillation; Mode (computer interface); Arctic dipole anomaly; The arctic; Atmospheric sciences; Geology; Oceanography; Northern Hemisphere; Sea ice; Arctic ice pack","score_opus":0.03655430306246089,"score_gpt":0.28371515973101913,"score_spread":0.24716085666855825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064872575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999342,0.000037474998,0.00013221867,0.000019966392,0.0000018946132,9.056404e-7,0.000090925525,0.000004242929,0.0003703999],"genre_scores_gemma":[0.9997789,0.000021467959,0.00006082661,0.000002934189,0.0000028380587,8.4512135e-7,0.00007311705,0.0000017151951,0.00005735106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999286,0.00002137254,0.000004817063,0.000012779177,0.000015816096,0.000016615135],"domain_scores_gemma":[0.99929464,0.00032146173,0.0001304727,0.000039051658,0.0001363869,0.00007802355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002921659,0.000102813385,0.00010757368,0.00048541394,0.00018028636,0.00036610654,0.000069692294,0.00013672936,0.00036685806],"category_scores_gemma":[0.0018060309,0.00007495593,0.00011732587,0.0004981373,0.00017843711,0.00014909984,0.00018178069,0.00014386946,0.000058328467],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043940447,0.0000149932175,0.9876425,0.000006000139,0.0000328223,0.00006618972,0.00008946343,0.0028251628,0.005240844,0.00022023718,0.00011962172,0.0036982165],"study_design_scores_gemma":[8.9711494e-7,0.0000059236695,0.99771,9.299961e-7,0.0000030214774,0.000021926873,0.000029545396,0.0019448713,0.000110296416,0.00007010927,0.00009999558,0.0000025633021],"about_ca_topic_score_codex":0.02238784,"about_ca_topic_score_gemma":0.02109079,"teacher_disagreement_score":0.02238784,"about_ca_system_score_codex":0.00030722067,"about_ca_system_score_gemma":0.00033240582,"threshold_uncertainty_score":0.044515014},"labels":[],"label_agreement":null},{"id":"W2064948279","doi":"10.1029/2003gl018885","title":"The nonlinear Northern Hemisphere winter atmospheric response to ENSO","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Northern Hemisphere; Teleconnection; Climatology; Geopotential height; North Atlantic oscillation; Sea surface temperature; El Niño Southern Oscillation; Geology; Oceanography; Southern Hemisphere; Pacific decadal oscillation; Geography; Precipitation; Meteorology","score_opus":0.021855129444493544,"score_gpt":0.29670396616386796,"score_spread":0.27484883671937443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2064948279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99244267,0.0000494252,0.0009787474,0.00025089824,0.00001763021,0.0000066701623,0.0004161519,0.00006250463,0.0057753753],"genre_scores_gemma":[0.99874157,0.000036596168,0.0001138527,0.000019467689,0.000005452175,0.0000022287513,0.00019290793,0.0000067035535,0.0008811017],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999521,0.000011196532,0.000002146397,0.000010833893,0.000010816259,0.000012921513],"domain_scores_gemma":[0.99984944,0.00004785859,0.000026825302,0.000012939696,0.000041924373,0.000020953981],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111597525,0.00014996131,0.00007110743,0.00008917901,0.00013987221,0.0002733503,0.00006087374,0.00012409643,0.001791953],"category_scores_gemma":[0.0011576274,0.00010776361,0.000110998524,0.00013241153,0.00011076085,0.00016624632,0.00021619625,0.00017337808,0.00019617852],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001051837,0.00014256516,0.4756247,0.00013435831,0.00025454455,0.0006878801,0.00068657985,0.25473022,0.16951732,0.005174796,0.0095851235,0.08241017],"study_design_scores_gemma":[0.000018969557,0.00006319297,0.80448246,0.000008892845,0.000023253782,0.00010891425,0.00022227662,0.18631698,0.004433379,0.0024476198,0.0018538613,0.000020146668],"about_ca_topic_score_codex":0.0144229,"about_ca_topic_score_gemma":0.015251207,"teacher_disagreement_score":0.0144229,"about_ca_system_score_codex":0.0002730919,"about_ca_system_score_gemma":0.00019996159,"threshold_uncertainty_score":0.02867788},"labels":[],"label_agreement":null},{"id":"W2065462315","doi":"10.1029/2001gl014070","title":"Vortex shedding and sediment resuspension associated with the interaction of an internal solitary wave and the bottom boundary layer","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Vortex shedding; Boundary layer; Vortex; Mechanics; Geology; Vorticity; Internal wave; Boundary (topology); Physics; Instability; Geophysics; Turbulence; Reynolds number","score_opus":0.028450696278250767,"score_gpt":0.26048798229086306,"score_spread":0.2320372860126123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065462315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935948,0.00005670106,0.0053527746,0.000026991898,0.00000684802,0.00000786752,0.000008107438,0.000016299502,0.0009295985],"genre_scores_gemma":[0.9984977,0.000024259369,0.0009843067,0.000008293278,0.000006982349,0.000005009323,0.000018615992,0.0000038124806,0.00045094592],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99980253,0.000027531589,0.000008205617,0.000013723462,0.00007702876,0.000071014],"domain_scores_gemma":[0.99930286,0.00024735904,0.00019056907,0.000052874984,0.00009053641,0.000115748255],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015230116,0.00026996725,0.00028472228,0.00029946584,0.00043956234,0.0005509899,0.00018259733,0.00029344248,0.00079144177],"category_scores_gemma":[0.0008202478,0.00017756439,0.00029750087,0.00011797026,0.0005944125,0.00023810564,0.00080396875,0.00034107256,0.00010759491],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007887544,0.00016982039,0.055032503,0.00012846214,0.000115373114,0.0056508393,0.00042870076,0.038910795,0.8738839,0.0048675104,0.00043886667,0.019584652],"study_design_scores_gemma":[0.00012910213,0.0009239921,0.10619218,0.000024720564,0.00010501957,0.0033608573,0.00050188357,0.52806515,0.35278818,0.0064926236,0.0013279233,0.00008839184],"about_ca_topic_score_codex":0.0012144512,"about_ca_topic_score_gemma":0.000726679,"teacher_disagreement_score":0.0012144512,"about_ca_system_score_codex":0.00023468427,"about_ca_system_score_gemma":0.00017922524,"threshold_uncertainty_score":0.0026475787},"labels":[],"label_agreement":null},{"id":"W2065763720","doi":"10.1029/2003gl017539","title":"Long distance transport of pollen to Greenland","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lamont-Doherty Earth Observatory, Columbia University; Institut Polaire Français Paul Emile Victor","keywords":"Pollen; Air mass (solar energy); Arctic; Groenlandia; Geology; Altitude (triangle); Greenland ice sheet; Physical geography; Vegetation (pathology); Climatology; Oceanography; Atmospheric sciences; Geography; Ice sheet; Boundary layer; Ecology","score_opus":0.04105392664994962,"score_gpt":0.28410980941910197,"score_spread":0.24305588276915235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065763720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895704,0.00007283698,0.00013011468,0.000017611359,0.0000020439911,0.0000014728762,0.00019779119,0.0000056847857,0.0006152802],"genre_scores_gemma":[0.9988587,0.00007247271,0.00021400726,0.000011685497,0.0000011760015,0.0000019005885,0.00033463901,0.0000026058408,0.0005027399],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999515,0.000004088625,0.0000018186956,0.00001533067,0.000008735361,0.000018554994],"domain_scores_gemma":[0.99987996,0.000021799478,0.000032313026,0.000014018045,0.000033826123,0.000018019655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087615466,0.00013306134,0.00012403846,0.0005061163,0.00048628045,0.00040775345,0.00012185103,0.00009506853,0.0006827107],"category_scores_gemma":[0.00018258549,0.00009512538,0.00010996535,0.00047126578,0.00019528905,0.0002035665,0.00029438006,0.0001639816,0.00009466804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015345657,0.00002564844,0.9201001,0.000028889946,0.000093612005,0.0005461733,0.0015531456,0.0022295595,0.04132927,0.00053603377,0.0005838388,0.032820303],"study_design_scores_gemma":[0.0000051567094,0.00004987391,0.99447364,0.000009114046,0.000015448566,0.000081172366,0.0003761917,0.0011474347,0.0021685003,0.00015206137,0.0015142298,0.0000070764986],"about_ca_topic_score_codex":0.14656357,"about_ca_topic_score_gemma":0.28675273,"teacher_disagreement_score":0.14656357,"about_ca_system_score_codex":0.0013711543,"about_ca_system_score_gemma":0.00060727727,"threshold_uncertainty_score":0.291421},"labels":[],"label_agreement":null},{"id":"W2065982200","doi":"10.1029/2003gl017386","title":"Heat flow in the western Superior Province of the Canadian shield","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National de la Recherche Scientifique","keywords":"Borehole; Archean; Geology; Heat flow; Shield; Flow (mathematics); High heat; Range (aeronautics); Geomorphology; Petrology; Thermal; Geotechnical engineering; Paleontology; Meteorology; Geography","score_opus":0.024553412321984592,"score_gpt":0.2651684339606039,"score_spread":0.2406150216386193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2065982200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939255,0.00019474332,0.00018657048,0.00013609987,0.000006026556,0.000012363886,0.0014377417,0.000031805048,0.004069115],"genre_scores_gemma":[0.9977851,0.00013850414,0.00041264214,0.000019953946,0.0000031111051,0.0000064505407,0.0005447391,0.000004826986,0.0010847081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997137,0.000008021252,0.0000064500664,0.0000421188,0.0001381299,0.000091552356],"domain_scores_gemma":[0.9995109,0.000023503606,0.000054541408,0.0000109974435,0.0003291047,0.000070960996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000153481,0.00023504056,0.00020641206,0.0011970936,0.002492577,0.00074335287,0.00032619157,0.000149912,0.0013126602],"category_scores_gemma":[0.00055053685,0.00018205613,0.00012961094,0.0021886306,0.00086610357,0.0002554437,0.00051040115,0.00021104336,0.00010228463],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036583567,0.000049466722,0.9131061,0.00014524693,0.00007276042,0.0004729762,0.007120281,0.004015737,0.017612483,0.001636397,0.0056231013,0.049779683],"study_design_scores_gemma":[0.000012447007,0.000013702722,0.99100083,0.000017304475,0.000014363615,0.000050101633,0.0011586734,0.0015577222,0.0009038295,0.000096001895,0.00515371,0.00002125661],"about_ca_topic_score_codex":0.99561137,"about_ca_topic_score_gemma":0.9986463,"teacher_disagreement_score":0.018311594,"about_ca_system_score_codex":0.018311594,"about_ca_system_score_gemma":0.025481554,"threshold_uncertainty_score":0.13286048},"labels":[],"label_agreement":null},{"id":"W2066070856","doi":"10.1029/2004gl019475","title":"A two‐directional freeze and thaw algorithm for hydrologic and land surface modelling","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Permafrost; Subarctic climate; Surface runoff; Frost (temperature); Environmental science; Temperate climate; Infiltration (HVAC); Arctic; Hydrology (agriculture); Greenhouse gas; Latitude; Soil science; Range (aeronautics); Water content; Atmospheric sciences; Geology; Meteorology; Geomorphology; Geotechnical engineering; Ecology","score_opus":0.08269205619137675,"score_gpt":0.3079564641282021,"score_spread":0.22526440793682534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066070856","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0066483472,0.000057257483,0.9917486,0.000042509226,0.000021890326,0.000023773602,0.000070830574,0.0006470207,0.0007397532],"genre_scores_gemma":[0.15998337,0.00019086644,0.8355485,0.000054569122,0.000033476495,0.00019601382,0.00044462414,0.00027474464,0.0032738913],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999045,0.000021284808,0.0000069322437,0.000016583375,0.000040283943,0.000010404735],"domain_scores_gemma":[0.999828,0.000064950545,0.000014615776,0.000024629842,0.000056884157,0.000010909203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038489813,0.00039782247,0.00040254756,0.0002900256,0.00039409407,0.00058791746,0.0007767421,0.000600028,0.0016040098],"category_scores_gemma":[0.00080432574,0.00037230516,0.0005746451,0.0004430493,0.00028134816,0.00078482484,0.00056887895,0.00075291825,0.00064983446],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000580587,0.000033280678,0.0011655753,0.000042403997,0.000036794114,0.000045663634,0.00006008459,0.8269682,0.0056034015,0.020360785,0.0025065565,0.14311922],"study_design_scores_gemma":[0.000007549895,0.00000521845,0.00006289699,0.000001436898,0.0000015603881,0.000006546314,0.0000032351209,0.99531037,0.0006432739,0.0025211624,0.0014334995,0.0000032531207],"about_ca_topic_score_codex":0.005787137,"about_ca_topic_score_gemma":0.0064708674,"teacher_disagreement_score":0.005787137,"about_ca_system_score_codex":0.00040487034,"about_ca_system_score_gemma":0.0007795046,"threshold_uncertainty_score":0.011506915},"labels":[],"label_agreement":null},{"id":"W2066090863","doi":"10.1029/2000gl011536","title":"Ocean loading corrections for continuous GPS: A case study at the Canadian coastal site Holberg","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"GNSS positioning and interference","field":"Engineering","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Zenith; Global Positioning System; Geodesy; Ocean tide; Geology; Environmental science; Troposphere; Climatology; Meteorology; Geography","score_opus":0.028745636843333523,"score_gpt":0.2952824791365723,"score_spread":0.26653684229323876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066090863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99446,0.00014070723,0.0025937916,0.00027281858,0.000019510717,0.000041300802,0.000312885,0.00012855354,0.0020303982],"genre_scores_gemma":[0.9935272,0.0001066573,0.0049640313,0.00005990577,0.000011273129,0.0000127737985,0.00039249286,0.000044813558,0.00088076276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99899703,0.0001603729,0.000035567406,0.00013720483,0.00048164092,0.00018815052],"domain_scores_gemma":[0.99545985,0.0022139095,0.00038127895,0.00036538637,0.0014348604,0.0001447554],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010632388,0.00052616856,0.00036639933,0.0005093245,0.0015556893,0.00091415714,0.0010105969,0.0007911948,0.0006967467],"category_scores_gemma":[0.008829393,0.00030135957,0.00030872517,0.0022201068,0.00062391313,0.0003979869,0.00040249922,0.0005634285,0.00015738283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014080993,0.0005112236,0.48555717,0.0003642286,0.00033097292,0.004377841,0.0026500355,0.25395527,0.026002984,0.0013809826,0.0069264504,0.21653469],"study_design_scores_gemma":[0.00019543292,0.0004391635,0.7886955,0.000049475606,0.00035302874,0.00050165266,0.0021961096,0.18574366,0.014575005,0.0004241544,0.006676663,0.00015021318],"about_ca_topic_score_codex":0.8888149,"about_ca_topic_score_gemma":0.91674936,"teacher_disagreement_score":0.111185074,"about_ca_system_score_codex":0.007236127,"about_ca_system_score_gemma":0.0051596407,"threshold_uncertainty_score":0.22367966},"labels":[],"label_agreement":null},{"id":"W2066143729","doi":"10.1029/2006gl028448","title":"Decontaminating tide gauge records for the influence of glacial isostatic adjustment: The potential impact of 3‐D Earth structure","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Lithosphere; Mantle (geology); Tide gauge; Geology; Sea level; Geodesy; Geophysics; Seismology; Oceanography; Tectonics","score_opus":0.01609485394625142,"score_gpt":0.2877439010671822,"score_spread":0.27164904712093074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066143729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98547125,0.00009963479,0.012373149,0.0004948551,0.000044420012,0.000016866914,0.0003612343,0.00019274357,0.00094576034],"genre_scores_gemma":[0.99666256,0.000038608672,0.002861071,0.00005193141,0.000009084078,0.000009904716,0.00021056447,0.000021716158,0.00013463214],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995622,0.00025576173,0.000023891585,0.00005659176,0.00005130947,0.000050157512],"domain_scores_gemma":[0.9971886,0.0016600451,0.00044357392,0.0003347411,0.00022117644,0.00015183572],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014739331,0.00078196794,0.0007271903,0.00040757642,0.0005167639,0.0011246545,0.0010536998,0.0009667538,0.00069382257],"category_scores_gemma":[0.008070407,0.00044542452,0.0010389056,0.00056642905,0.0004808348,0.0008514203,0.000580566,0.0007371651,0.00017719771],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003238634,0.000081968865,0.08915837,0.000032838627,0.00022178225,0.0001702227,0.00010646192,0.8959892,0.0035348672,0.0010157045,0.00029029985,0.0090744505],"study_design_scores_gemma":[0.000071504815,0.000076764256,0.03337736,0.000013786522,0.00006413484,0.00004388737,0.00004466556,0.9634367,0.0017455675,0.00061816466,0.00046584572,0.000041520747],"about_ca_topic_score_codex":0.049684867,"about_ca_topic_score_gemma":0.030576048,"teacher_disagreement_score":0.049684867,"about_ca_system_score_codex":0.0009570093,"about_ca_system_score_gemma":0.0012331101,"threshold_uncertainty_score":0.09879136},"labels":[],"label_agreement":null},{"id":"W2066277575","doi":"10.1029/2007gl030283","title":"Crustal uplift and sea level rise in northern Cascadia from GPS, absolute gravity, and tide gauge data","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geodesy; Tide gauge; Geology; Global Positioning System; Solid earth; Offset (computer science); Reference frame; Sea level; Seismology; Oceanography; Geophysics","score_opus":0.10678364567423944,"score_gpt":0.3173186617238018,"score_spread":0.21053501604956237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066277575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985795,0.00006686808,0.00011968755,0.0000384693,0.0000023125667,0.0000016601178,0.00045814793,0.00002247428,0.0007108597],"genre_scores_gemma":[0.99820375,0.000084253,0.0001810489,0.0000062945073,0.0000033615747,0.000003303533,0.001249733,0.0000069234957,0.00026130083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99958664,0.00007080589,0.000041996416,0.00011753142,0.00013320099,0.000049814178],"domain_scores_gemma":[0.99880767,0.00019947793,0.0002871455,0.0001854536,0.0002773415,0.0002429301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006060809,0.00035985722,0.0003192675,0.0015493562,0.00036761758,0.00064710184,0.0002645532,0.00018150047,0.0010702545],"category_scores_gemma":[0.00276456,0.00029701824,0.00048668133,0.0018050822,0.00037365025,0.00035491886,0.0010136869,0.0003729293,0.00026119704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000044470497,0.000007778611,0.9928585,0.000017559552,0.00011097439,0.00009721757,0.00028042498,0.0014023335,0.00083195686,0.00004880264,0.00019861058,0.004101294],"study_design_scores_gemma":[0.0000021534327,0.0000069500666,0.999191,0.000003925624,0.000015309706,0.000021888709,0.00008163911,0.00045931575,0.000045493514,0.000023982933,0.00014530016,0.0000029796547],"about_ca_topic_score_codex":0.13330527,"about_ca_topic_score_gemma":0.25477996,"teacher_disagreement_score":0.13330527,"about_ca_system_score_codex":0.00096638495,"about_ca_system_score_gemma":0.0006648543,"threshold_uncertainty_score":0.26505864},"labels":[],"label_agreement":null},{"id":"W2066477583","doi":"10.1029/2001gl013723","title":"Plasma density enhancements in the high‐altitude polar cap region observed on Akebono","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Ionosphere; Plasma; Polar; Electron temperature; Physics; Convection; Atmospheric sciences; Electron density; Geophysics; Ion; Altitude (triangle); F region; Drift velocity; Atomic physics; Meteorology; Astronomy; Nuclear physics","score_opus":0.048430697892433906,"score_gpt":0.27858547273783635,"score_spread":0.23015477484540245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066477583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970624,0.00010806774,0.000053276643,0.000022129707,0.000006988615,0.000002879784,0.00005420809,0.00000971917,0.0026803813],"genre_scores_gemma":[0.99943453,0.0000646844,0.000054522992,0.000012567058,0.000006635517,0.0000026773375,0.000089178866,0.0000017009756,0.00033344227],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997616,0.0000018087704,8.0387184e-7,0.0000048362936,0.0000054314346,0.000010898154],"domain_scores_gemma":[0.99993503,0.000008145923,0.0000146134535,0.0000052267524,0.000016568736,0.00002040329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000041611976,0.00013350706,0.00017285613,0.00025030487,0.00044241518,0.00031801834,0.00013412566,0.00014803652,0.0010909833],"category_scores_gemma":[0.00013972491,0.00013842939,0.00007384603,0.00023145878,0.0002161818,0.00016369772,0.00033919504,0.00025998484,0.0001902273],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019316084,0.0001937878,0.32820725,0.00023141531,0.00012485051,0.0077671483,0.0027633966,0.001299082,0.6369897,0.0006716966,0.0017249,0.01809511],"study_design_scores_gemma":[0.000021614873,0.000072995856,0.9919819,0.000010507609,0.000026573996,0.0003833053,0.00047159544,0.00055092544,0.005069022,0.00006132487,0.0013436388,0.000006643886],"about_ca_topic_score_codex":0.006733719,"about_ca_topic_score_gemma":0.00831524,"teacher_disagreement_score":0.006733719,"about_ca_system_score_codex":0.00019328928,"about_ca_system_score_gemma":0.00009872892,"threshold_uncertainty_score":0.013389051},"labels":[],"label_agreement":null},{"id":"W2066725172","doi":"10.1029/2007gl031517","title":"D″ beneath the Arctic from inversion of shear waveforms","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Inversion (geology); Seismometer; Arctic; The arctic; Geodesy; Seismology; Waveform; Physics; Oceanography","score_opus":0.028395404682785168,"score_gpt":0.27171156878979474,"score_spread":0.24331616410700957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066725172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98946464,0.000048043163,0.0056065316,0.00007024937,0.000020943118,0.000010934562,0.0010908098,0.00044520956,0.0032425707],"genre_scores_gemma":[0.99186456,0.000058781712,0.00628329,0.000009986598,0.0000076280694,0.000003661049,0.0013888024,0.000024079465,0.00035924252],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999474,0.00000397282,0.0000037427264,0.000011817012,0.000016789067,0.000016234562],"domain_scores_gemma":[0.999859,0.000023308405,0.000014527859,0.0000121787625,0.000070349924,0.00002060022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001307279,0.00036058165,0.00020576145,0.0005584616,0.0002885049,0.0006624786,0.00034136145,0.0002493844,0.0008568798],"category_scores_gemma":[0.0005830884,0.00022942029,0.00027688028,0.0008088089,0.00015365057,0.0001790674,0.00021711031,0.00028740487,0.00019450579],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016004331,0.0002643126,0.19919667,0.00023570623,0.00026016435,0.000968524,0.000578582,0.5164504,0.16054158,0.0026189608,0.0036843696,0.113600254],"study_design_scores_gemma":[0.00011221964,0.0000619981,0.09317117,0.000019507395,0.00008040009,0.00007607033,0.00025631583,0.88577366,0.017477365,0.00048421053,0.0024507644,0.000036402165],"about_ca_topic_score_codex":0.09965431,"about_ca_topic_score_gemma":0.11544118,"teacher_disagreement_score":0.09965431,"about_ca_system_score_codex":0.00046934548,"about_ca_system_score_gemma":0.001323659,"threshold_uncertainty_score":0.19814855},"labels":[],"label_agreement":null},{"id":"W2066820268","doi":"10.1029/2007gl029638","title":"An Antarctic ice‐related “superbloom” observed with the MERIS satellite imager","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Imaging spectrometer; Satellite; Remote sensing; Geology; Snow; Sea ice; Environmental science; Oceanography; Spectrometer; Geomorphology; Physics; Astronomy; Optics","score_opus":0.028651460303143046,"score_gpt":0.2634974156949565,"score_spread":0.23484595539181344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2066820268","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97601175,0.00023898299,0.0013049459,0.00019119987,0.00006298354,0.000057168167,0.007310435,0.00026940397,0.014553192],"genre_scores_gemma":[0.9845712,0.000271151,0.005058504,0.00014798949,0.000045600384,0.000024495992,0.0055354773,0.000039970328,0.004305658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996567,0.0000023465923,0.000001077413,0.000005621891,0.000014992967,0.000010284281],"domain_scores_gemma":[0.9999182,0.0000062964855,0.00001991424,0.000009719597,0.000016089652,0.000029809748],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000068655485,0.00020223585,0.00012473208,0.00095723424,0.0003075014,0.000247624,0.00010493159,0.00024850786,0.0024865414],"category_scores_gemma":[0.000086873035,0.000109859386,0.00010289547,0.0010758025,0.00013801422,0.00016996266,0.0002726652,0.00022670548,0.0004324643],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016172616,0.0002589092,0.43253392,0.0004605974,0.00022876599,0.004479956,0.0024062751,0.0029633797,0.36774084,0.0016598349,0.04782584,0.13782433],"study_design_scores_gemma":[0.000013629919,0.00007239544,0.98097163,0.000017648235,0.000014429931,0.00063005387,0.00037604602,0.0019631071,0.005747598,0.00011833846,0.01006563,0.000009432906],"about_ca_topic_score_codex":0.0071547185,"about_ca_topic_score_gemma":0.028939601,"teacher_disagreement_score":0.0071547185,"about_ca_system_score_codex":0.00019666791,"about_ca_system_score_gemma":0.00013895787,"threshold_uncertainty_score":0.014226198},"labels":[],"label_agreement":null},{"id":"W2067023630","doi":"10.1029/2005gl025257","title":"Impacts of winter storms on air‐sea gas exchange","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada; Bedford Institute of Oceanography; Dalhousie University","funders":"","keywords":"Storm; Environmental science; Winter storm; Atmospheric sciences; Sea state; Climatology; Geology; Oceanography","score_opus":0.02028217532910864,"score_gpt":0.26427666120191945,"score_spread":0.2439944858728108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067023630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947995,0.000030433117,0.000044389006,0.000017664963,0.000003125861,0.000001353399,0.000099752855,0.0000065085314,0.0003168356],"genre_scores_gemma":[0.999613,0.000046776306,0.00004169184,0.0000096245885,0.000006020984,0.0000020615619,0.00017664982,0.000002671635,0.00010148684],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989474,0.000021759404,0.0000060623624,0.000016880753,0.000021325683,0.00003918729],"domain_scores_gemma":[0.99955314,0.00017613711,0.000112192145,0.00002279552,0.000051080024,0.000084502644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020419224,0.00026503188,0.00026772596,0.00023865592,0.00030880905,0.00051165256,0.000112021335,0.0002701369,0.0010152222],"category_scores_gemma":[0.00062443694,0.00011505991,0.00020474593,0.00020079153,0.00021366231,0.0002614589,0.0003746679,0.00022333203,0.00011702888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008060733,0.000098656215,0.96175855,0.00003837812,0.0001133386,0.00072149455,0.00028500118,0.003733485,0.02168855,0.000103195096,0.0003503223,0.01030294],"study_design_scores_gemma":[0.000008346804,0.000121744306,0.9956801,0.0000042243787,0.000019616611,0.00008117401,0.00023373579,0.0021808129,0.0013653953,0.00005731417,0.00024383543,0.0000037225268],"about_ca_topic_score_codex":0.012459969,"about_ca_topic_score_gemma":0.011232093,"teacher_disagreement_score":0.012459969,"about_ca_system_score_codex":0.00033439844,"about_ca_system_score_gemma":0.0002490553,"threshold_uncertainty_score":0.02477485},"labels":[],"label_agreement":null},{"id":"W2067133458","doi":"10.1029/2008gl034795","title":"Natural abundance measurements of <sup>13</sup>C indicate increased deep soil carbon mineralization after forest disturbance","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Carbon and Nitrogen Dynamics","field":"Agricultural and Biological Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University; Dalhousie University","funders":"","keywords":"Chronosequence; Soil carbon; Environmental science; Ecosystem; Humus; Disturbance (geology); Mineralization (soil science); Soil water; Abundance (ecology); Soil science; Forest ecology; Soil horizon; Blue carbon; Ecology; Geology; Biology","score_opus":0.03132942936875977,"score_gpt":0.2522285368030712,"score_spread":0.22089910743431146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067133458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988606,0.0001456926,0.00029734615,0.0000081999815,0.0000016582635,0.000001907492,0.00015229713,0.000012172707,0.00052008947],"genre_scores_gemma":[0.9990588,0.000084623476,0.00031030652,0.000016511929,0.000002215745,0.0000026483867,0.00019147042,0.0000030538322,0.00033038226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995065,0.0000041857243,0.0000031278012,0.000015426558,0.0000133111125,0.00001328728],"domain_scores_gemma":[0.99960953,0.000056109693,0.00021237605,0.000028232029,0.000051421484,0.00004229497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013791255,0.000118201424,0.00011901745,0.0002202495,0.00021465388,0.00029730354,0.00013102194,0.00016922751,0.0009286033],"category_scores_gemma":[0.00028478497,0.000093553455,0.00007268079,0.00022890855,0.00037298334,0.00019758665,0.00014186988,0.00017968519,0.00020607794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034498074,0.000038541908,0.7826954,0.000060386785,0.000055930093,0.00017208503,0.00017285974,0.00028312963,0.19953033,0.00006573247,0.0001601534,0.016420405],"study_design_scores_gemma":[7.4854364e-7,0.00002231477,0.99572206,0.0000012038965,0.0000042567126,0.00009009875,0.00003971071,0.00006735604,0.0038761434,0.000024189258,0.00015059375,0.0000012465779],"about_ca_topic_score_codex":0.006428231,"about_ca_topic_score_gemma":0.0203966,"teacher_disagreement_score":0.006428231,"about_ca_system_score_codex":0.00025240926,"about_ca_system_score_gemma":0.00013695027,"threshold_uncertainty_score":0.01278168},"labels":[],"label_agreement":null},{"id":"W2067145150","doi":"10.1029/2006gl026124","title":"Sensitivity of the thermohaline circulation to Arctic Ocean runoff","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; University of Northern British Columbia","funders":"Canada Research Chairs; Government of Canada","keywords":"Thermohaline circulation; Surface runoff; Environmental science; Arctic; Oceanography; Arctic dipole anomaly; Ocean current; Arctic geoengineering; Climatology; Geology; Arctic ice pack; Ecology; Drift ice","score_opus":0.017779230626685228,"score_gpt":0.2531059894599497,"score_spread":0.23532675883326448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067145150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994266,0.000007775902,0.00020428177,0.000018297183,0.00000258571,0.0000025255806,0.0000513539,0.0000059597396,0.0002806087],"genre_scores_gemma":[0.9996952,0.000020730811,0.00012830537,0.000013666718,0.0000021569124,0.0000027891977,0.00006858574,0.0000025313382,0.00006611665],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998696,0.00005266309,0.000007977079,0.000028935172,0.000018399525,0.00002247749],"domain_scores_gemma":[0.9995485,0.00023703063,0.000057584984,0.000084167514,0.000029860912,0.000042871223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031363705,0.00017280455,0.00016673702,0.00011880066,0.00018257227,0.00043955812,0.00013758652,0.00018263633,0.0007321576],"category_scores_gemma":[0.0012807022,0.00012094821,0.00031681123,0.00010417488,0.00030394606,0.00027264157,0.00041491215,0.00036669982,0.000050639886],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00301131,0.00066720485,0.26241875,0.00011188682,0.00061607047,0.00029098333,0.00034973488,0.49094084,0.2235744,0.0036240893,0.0005570193,0.013837745],"study_design_scores_gemma":[0.00028640337,0.0023510945,0.40200746,0.000018258848,0.00030404874,0.000117697076,0.00028410263,0.52512956,0.06337844,0.004116711,0.0019153534,0.000090924455],"about_ca_topic_score_codex":0.007655884,"about_ca_topic_score_gemma":0.0046257973,"teacher_disagreement_score":0.007655884,"about_ca_system_score_codex":0.00042141898,"about_ca_system_score_gemma":0.00024533205,"threshold_uncertainty_score":0.015222669},"labels":[],"label_agreement":null},{"id":"W2067169353","doi":"10.1029/2005gl025251","title":"Atlantic meridional overturning and climate response to Arctic Ocean freshening","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Toronto","funders":"","keywords":"Younger Dryas; Deglaciation; Geology; Shutdown of thermohaline circulation; Oceanography; Thermohaline circulation; North Atlantic Deep Water; Meltwater; Climatology; Abrupt climate change; Ocean current; Arctic; Glacial period; Climate change; Holocene; Global warming; Effects of global warming; Paleontology","score_opus":0.0204768286498225,"score_gpt":0.27756563819289454,"score_spread":0.25708880954307206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067169353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99950004,0.000045428667,0.000017312212,0.00004788861,0.0000034250224,0.0000012085427,0.00003204553,0.0000017854529,0.00035095183],"genre_scores_gemma":[0.9995834,0.000056608944,0.000020132422,0.000030699095,0.0000060868297,0.000001090395,0.00004594284,0.0000014009925,0.00025454583],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999651,0.000007240026,0.0000019348051,0.000006885972,0.000004311487,0.000014573475],"domain_scores_gemma":[0.9997162,0.000053090618,0.00008546328,0.000018816292,0.000031850985,0.00009460997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013570944,0.000085563595,0.00013608279,0.00014745173,0.00016006174,0.00034825466,0.00008947032,0.00023676096,0.001183698],"category_scores_gemma":[0.000768717,0.00008756376,0.00010847313,0.00012588597,0.00015197518,0.00013140366,0.00018936428,0.00024112746,0.00014846017],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015802046,0.0002959688,0.8806613,0.000042663385,0.00012551718,0.0004151618,0.0005028731,0.0027004122,0.096571155,0.00038837438,0.0006285533,0.016087763],"study_design_scores_gemma":[0.000005818257,0.000051012456,0.9985813,0.0000013736332,0.000005508105,0.000029325545,0.00007556716,0.000657686,0.00038850072,0.000056988556,0.00014480548,0.0000021598908],"about_ca_topic_score_codex":0.0061232653,"about_ca_topic_score_gemma":0.011500606,"teacher_disagreement_score":0.0061232653,"about_ca_system_score_codex":0.0002461371,"about_ca_system_score_gemma":0.00013951177,"threshold_uncertainty_score":0.012175262},"labels":[],"label_agreement":null},{"id":"W2067255271","doi":"10.1029/2003gl018530","title":"A high‐resolution simulation of convective roll clouds during a cold‐air outbreak","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Convection; Meteorology; Momentum (technical analysis); Atmospheric sciences; Environmental science; Geology; Cloud computing; Mechanics; Physics; Computer science","score_opus":0.028721679548372715,"score_gpt":0.2998810766976527,"score_spread":0.27115939714927995,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067255271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955249,0.000038783535,0.0011116953,0.000181132,0.000023570808,0.000022089427,0.00028603338,0.00009287376,0.002718823],"genre_scores_gemma":[0.9976636,0.000021912161,0.0014954351,0.000034884677,0.000008100452,0.000019578798,0.00033182616,0.000020029413,0.00040461012],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998149,0.000041555362,0.000008911038,0.00002511163,0.000030343173,0.00007911772],"domain_scores_gemma":[0.99897826,0.00052829756,0.00007018253,0.000058648977,0.00012000879,0.00024466738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046283824,0.00047903688,0.0007590157,0.00039392393,0.0009217914,0.0010448721,0.0010943656,0.0016126281,0.0017314713],"category_scores_gemma":[0.0018388805,0.00044339613,0.0005933031,0.0005676521,0.0011328544,0.0005693389,0.0007339928,0.001305422,0.00012901684],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034273788,0.0002653011,0.007970768,0.000020389496,0.0000475149,0.00030787027,0.00008845068,0.9864096,0.0019363889,0.0009652972,0.0004921405,0.0011534807],"study_design_scores_gemma":[0.00013451587,0.000060811784,0.0027780344,0.00000355055,0.0000108703625,0.000011802739,0.000076954944,0.996102,0.00049450947,0.0001694675,0.00014903628,0.000008459625],"about_ca_topic_score_codex":0.058818314,"about_ca_topic_score_gemma":0.03345375,"teacher_disagreement_score":0.058818314,"about_ca_system_score_codex":0.0014967318,"about_ca_system_score_gemma":0.0013769357,"threshold_uncertainty_score":0.11695188},"labels":[],"label_agreement":null},{"id":"W2067301748","doi":"10.1029/2000gl012397","title":"Extra‐tropical response to ENSO as expressed in an ice core from the Saint Elias Mountain Range","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Toronto","funders":"","keywords":"Teleconnection; Climatology; Tropics; Multivariate ENSO index; Geology; El Niño Southern Oscillation; Atmosphere (unit); Snow; Ice core; La Niña; Geography; Meteorology; Geomorphology","score_opus":0.07660422457078148,"score_gpt":0.3475816895185245,"score_spread":0.270977464947743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067301748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998124,0.0000051220827,0.000013481808,0.0000041729977,2.7610025e-7,4.4685675e-7,0.0000652453,8.5298467e-7,0.00009795497],"genre_scores_gemma":[0.9995209,0.000015262272,0.00004512163,0.00000279109,0.000001162069,0.0000012375139,0.00030735624,5.03514e-7,0.000105662184],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99998164,0.0000026908988,0.0000012015315,0.0000036244965,0.0000042629613,0.000006567855],"domain_scores_gemma":[0.99991083,0.00002025978,0.000033512748,0.0000062414065,0.000016163292,0.000012939168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000062830695,0.000057390553,0.000052315736,0.00019147038,0.0001038554,0.00017630012,0.000050876242,0.00007092465,0.0002927037],"category_scores_gemma":[0.00023928565,0.000040461626,0.000049828544,0.00030495386,0.00008949789,0.00008264748,0.00011858934,0.000072560775,0.000033068496],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021064955,0.00005895832,0.960274,0.000021667207,0.000065144384,0.0003318741,0.0004165187,0.0037096674,0.027774185,0.0002291515,0.0003697448,0.006538358],"study_design_scores_gemma":[0.000001937695,0.000009247851,0.99810165,9.891381e-7,0.0000032932464,0.000025380094,0.000056270404,0.0013206041,0.00033925174,0.0000132382465,0.00012714165,9.352495e-7],"about_ca_topic_score_codex":0.013985296,"about_ca_topic_score_gemma":0.041982025,"teacher_disagreement_score":0.013985296,"about_ca_system_score_codex":0.00023637593,"about_ca_system_score_gemma":0.00015768685,"threshold_uncertainty_score":0.027807832},"labels":[],"label_agreement":null},{"id":"W2067365017","doi":"10.1029/2009gl038158","title":"High concentration of surface ozone observed along the Khumbu Valley Nepal April 2007","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Transect; Environmental science; Ozone; Atmospheric sciences; Troposphere; Range (aeronautics); Population; Tropospheric ozone; Descent (aeronautics); Pollutant; Ozone layer; Stratosphere; Climatology; Geology; Meteorology; Geography; Oceanography; Ecology","score_opus":0.042023276245459436,"score_gpt":0.2698885261709389,"score_spread":0.22786524992547946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067365017","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977852,0.00003137814,0.000040122304,0.00004434029,0.0000028058475,0.0000044036515,0.0001733501,0.000004643249,0.0019135369],"genre_scores_gemma":[0.99852043,0.000061117586,0.000085012216,0.000028182503,0.000004494993,0.0000090770445,0.0002935192,0.000001789916,0.0009962883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000007876316,0.0000029980945,0.000013557626,0.000016860336,0.000022088725],"domain_scores_gemma":[0.9998926,0.00001405836,0.000022927075,0.0000082018105,0.000037980673,0.000024173038],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000064063424,0.00010777626,0.00014778772,0.0006020396,0.0010576305,0.00061309396,0.00028432568,0.00026942443,0.0011058078],"category_scores_gemma":[0.0002474942,0.00015451123,0.00009471301,0.0005096413,0.00036222592,0.00017447976,0.0004142709,0.00030880788,0.00018900873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005984085,0.00006469734,0.9652223,0.00005577302,0.00006974414,0.0011525517,0.0062917583,0.00014728283,0.013925535,0.00013211631,0.0010176122,0.011860767],"study_design_scores_gemma":[9.718954e-7,0.00001550151,0.9968906,0.0000058741666,0.0000066675298,0.00023740527,0.0014748494,0.00004933135,0.00035336328,0.000014912704,0.00094685843,0.0000034897678],"about_ca_topic_score_codex":0.03800221,"about_ca_topic_score_gemma":0.12132227,"teacher_disagreement_score":0.03800221,"about_ca_system_score_codex":0.0003899184,"about_ca_system_score_gemma":0.00047058435,"threshold_uncertainty_score":0.07556206},"labels":[],"label_agreement":null},{"id":"W2067594137","doi":"10.1029/2000gl012627","title":"Light δ<sup>13</sup>C events during deglaciation of the East Greenland Continental Shelf attributed to methane release from gas hydrates","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Universitetet i Tromsø; National Science Foundation","keywords":"Deglaciation; Geology; Foraminifera; Oceanography; Meltwater; Continental shelf; Clathrate hydrate; Seafloor spreading; Benthic zone; Paleontology; Holocene; Glacial period; Hydrate; Chemistry","score_opus":0.017690051484481856,"score_gpt":0.2553240685438739,"score_spread":0.23763401705939205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067594137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996983,0.00003379544,0.000028531771,0.000010318446,0.0000010468166,8.8584216e-7,0.00010763527,0.0000044790577,0.00011503612],"genre_scores_gemma":[0.9994295,0.0000327646,0.0000807848,0.000017091797,0.0000029184923,0.0000018091476,0.0003032432,0.0000022364973,0.00012973156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.0000028902407,0.0000023145774,0.000008581003,0.0000080475875,0.000015595673],"domain_scores_gemma":[0.9997938,0.000018165189,0.00008875285,0.0000129481095,0.000049452043,0.00003679761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012518295,0.00014837596,0.00011371958,0.00049584615,0.00031963116,0.00026290174,0.00019785132,0.00017966618,0.0003725219],"category_scores_gemma":[0.00023889494,0.00011377338,0.00007439693,0.0004278098,0.0003296049,0.0001633047,0.00030344023,0.00017556302,0.00006118603],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021203503,0.000024642333,0.9433986,0.000024106688,0.000048467416,0.0004428872,0.00048549852,0.00019964411,0.047773648,0.000057257123,0.00020043258,0.007132822],"study_design_scores_gemma":[0.0000013062855,0.000008648933,0.9988865,0.0000012116634,0.000004778039,0.000039839157,0.00004690785,0.00007521876,0.00076521316,0.000012990508,0.00015587918,0.0000015636755],"about_ca_topic_score_codex":0.030369895,"about_ca_topic_score_gemma":0.113468915,"teacher_disagreement_score":0.030369895,"about_ca_system_score_codex":0.00050697575,"about_ca_system_score_gemma":0.0002597965,"threshold_uncertainty_score":0.06038624},"labels":[],"label_agreement":null},{"id":"W2067725954","doi":"10.1029/2005gl022394","title":"Carbon monoxide distribution from the ACE‐FTS solar occultation measurements","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; York University","funders":"Natural Sciences and Engineering Research Council of Canada; Fonds De La Recherche Scientifique - FNRS; Centre National d’Etudes Spatiales; Canadian Space Agency; Services Fédéraux des Affaires Scientifiques, Techniques et Culturelles; Canadian Foundation for Climate and Atmospheric Sciences; European Space Agency","keywords":"Occultation; Troposphere; Thermosphere; Atmospheric sciences; Environmental science; Carbon monoxide; Radio occultation; Spectral resolution; Atmospheric Infrared Sounder; Infrared; Remote sensing; Physics; Ionosphere; Geology; Astronomy; Spectral line; Chemistry","score_opus":0.05252271060894783,"score_gpt":0.2890072858150053,"score_spread":0.23648457520605745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067725954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97681946,0.00037591616,0.0020319945,0.000049761988,0.00001862121,0.000026200727,0.014510707,0.00015845924,0.006008948],"genre_scores_gemma":[0.97764343,0.0003507689,0.002646083,0.00001677093,0.000026476275,0.00001929757,0.018027019,0.000030684587,0.0012394988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998747,0.0000050153362,0.0000044272515,0.000022476579,0.00006604545,0.000027391518],"domain_scores_gemma":[0.99982494,0.000016759337,0.0000264129,0.00001437124,0.00009822814,0.000019314344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012639862,0.00035160163,0.0002729352,0.0012012505,0.00030695397,0.00044203154,0.00019393871,0.00019637709,0.000756004],"category_scores_gemma":[0.00026835385,0.00010676115,0.00023171116,0.0012427956,0.00009747567,0.00023767198,0.00021374607,0.00021466248,0.00027156936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010127891,0.00029697307,0.68200713,0.0002611828,0.00043668284,0.0008727833,0.00036382777,0.03189178,0.15910497,0.0012132926,0.009454324,0.11308426],"study_design_scores_gemma":[0.0000113601245,0.000039813433,0.9570954,0.000007730702,0.0000422734,0.00019307487,0.000053602533,0.0144018885,0.021171669,0.00010491504,0.006856771,0.000021512174],"about_ca_topic_score_codex":0.021307124,"about_ca_topic_score_gemma":0.025155239,"teacher_disagreement_score":0.021307124,"about_ca_system_score_codex":0.00040496414,"about_ca_system_score_gemma":0.00039930176,"threshold_uncertainty_score":0.042366207},"labels":[],"label_agreement":null},{"id":"W2067968537","doi":"10.1029/2008gl034590","title":"The World Avoided by the Montreal Protocol","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; European Commission; Sight Research UK","keywords":"Montreal Protocol; Ozone layer; Climatology; Environmental science; Atmospheric sciences; Ozone; Ozone depletion; Atmosphere (unit); Climate change; Latitude; Atmospheric temperature; Mode (computer interface); Polar; Stratosphere; Meteorology; Geography; Geology; Physics","score_opus":0.033920669582535666,"score_gpt":0.2998244988315394,"score_spread":0.26590382924900374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2067968537","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.030526282,0.004282788,0.0080575915,0.04240142,0.0025530637,0.0005450243,0.006906986,0.0006084321,0.90411836],"genre_scores_gemma":[0.36646143,0.0035657,0.010116531,0.026737198,0.00061796186,0.0009804025,0.004013236,0.0004251887,0.5870823],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99884135,0.00026400972,0.000037853566,0.00017131538,0.00029671047,0.0003887589],"domain_scores_gemma":[0.99890673,0.0001457776,0.00012850873,0.00023876068,0.00035130506,0.00022899044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015212036,0.00042406924,0.00026497932,0.00065987813,0.0026860442,0.0033132588,0.0009717909,0.0015422675,0.05302936],"category_scores_gemma":[0.0056708707,0.00020224761,0.0005437044,0.0009064548,0.001190986,0.0014400322,0.001923983,0.002062138,0.0034602734],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009907802,0.000031635333,0.00430605,0.00009158562,0.000044951383,0.0004316372,0.00036337235,0.0019469138,0.00055288064,0.6074341,0.32650086,0.05819694],"study_design_scores_gemma":[0.00002600846,0.000026679956,0.0036764764,0.00006496527,0.000012461335,0.000088903005,0.00009531535,0.0005473947,0.00023190396,0.010865613,0.9843352,0.000029159499],"about_ca_topic_score_codex":0.5974935,"about_ca_topic_score_gemma":0.6056124,"teacher_disagreement_score":0.5974935,"about_ca_system_score_codex":0.008690019,"about_ca_system_score_gemma":0.019431647,"threshold_uncertainty_score":0.80975384},"labels":[],"label_agreement":null},{"id":"W2068051936","doi":"10.1029/1999gl008461","title":"Effect of grain size and domain state on thermal demagnetization tails","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Aurora College; University of Toronto","funders":"","keywords":"Demagnetizing field; Magnetite; Geology; Remanence; Mineralogy; Grain size; Thermoremanent magnetization; Materials science; Condensed matter physics; Physics; Magnetic field; Geomorphology; Magnetization","score_opus":0.006894146210802871,"score_gpt":0.2734229599017193,"score_spread":0.2665288136909164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068051936","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99751955,0.00020209546,0.00067140674,0.000019278963,0.000008059171,0.000006489494,0.00016163166,0.00003252725,0.0013788899],"genre_scores_gemma":[0.9990145,0.000042143,0.00022186348,0.0000121688245,0.0000012133382,0.000004842165,0.0001043495,0.00002347312,0.00057539216],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999064,0.00001206961,0.0000095416035,0.00003138607,0.000019272033,0.000021257785],"domain_scores_gemma":[0.9993349,0.00037250997,0.00007117018,0.000059465357,0.000086770066,0.000075259275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024373173,0.00015626178,0.00012530119,0.00018260376,0.00017124222,0.0003915329,0.00017583105,0.00011926569,0.0023479995],"category_scores_gemma":[0.00093439705,0.00021773783,0.000094804716,0.00013090816,0.0003119513,0.00022314195,0.0001916194,0.00018896692,0.00016471201],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094224344,0.00003078076,0.009890918,0.00005569733,0.000023977658,0.00006740804,0.00011970242,0.00084233744,0.9813203,0.00013909911,0.00010340814,0.0064639836],"study_design_scores_gemma":[0.000021553687,0.0002353217,0.12113905,0.0000060250104,0.000042329615,0.00009849508,0.00009188573,0.003057873,0.87383664,0.00008279758,0.0013750885,0.000012914312],"about_ca_topic_score_codex":0.0035105224,"about_ca_topic_score_gemma":0.007205768,"teacher_disagreement_score":0.0035105224,"about_ca_system_score_codex":0.00025084455,"about_ca_system_score_gemma":0.00015428009,"threshold_uncertainty_score":0.007854879},"labels":[],"label_agreement":null},{"id":"W2068104727","doi":"10.1029/2001gl014047","title":"Partial recovery of the Arctic Ocean halocline","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Halocline; Oceanography; Geology; Salinity; Arctic; Ridge; Canada Basin; Fjord; Paleontology","score_opus":0.03220434724465853,"score_gpt":0.25647057724438743,"score_spread":0.2242662299997289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068104727","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979868,0.00044990287,0.00007288215,0.00005199029,0.0000035203745,0.0000043204823,0.00036628192,0.000010117396,0.001054175],"genre_scores_gemma":[0.998298,0.00022811048,0.000070074166,0.000038314804,0.000004536518,0.0000046942378,0.00088493974,0.000003385356,0.00046795345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986625,0.000012505366,0.0000113265905,0.000032175925,0.000034898603,0.000042794276],"domain_scores_gemma":[0.999321,0.00006437153,0.00025547843,0.00006498116,0.00018507529,0.000109035835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034462856,0.00017139119,0.00027907893,0.00060362136,0.00038846917,0.0006649665,0.0001976609,0.00035109688,0.0008846021],"category_scores_gemma":[0.0012117553,0.00014966505,0.0002595306,0.0006213564,0.0003829572,0.00030157802,0.0006135426,0.0003468577,0.00026459002],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000494447,0.000057270907,0.9228608,0.00012265074,0.00015847001,0.00035590155,0.0009935292,0.00060878485,0.036362525,0.0002591675,0.00072041544,0.03700614],"study_design_scores_gemma":[0.0000016090421,0.000035804143,0.99815446,0.00000607599,0.000006495209,0.00007327767,0.00009930916,0.00006972334,0.0006312338,0.000015123231,0.00090508803,0.0000018462226],"about_ca_topic_score_codex":0.017388549,"about_ca_topic_score_gemma":0.03011881,"teacher_disagreement_score":0.017388549,"about_ca_system_score_codex":0.0004983919,"about_ca_system_score_gemma":0.0005325437,"threshold_uncertainty_score":0.034574687},"labels":[],"label_agreement":null},{"id":"W2068352917","doi":"10.1029/2003gl017308","title":"The fate of mercury species in a sub‐arctic snowpack during snowmelt","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Centre National de la Recherche Scientifique","keywords":"Snowpack; Meltwater; Snowmelt; Snow; Mercury (programming language); Methylmercury; Arctic; Environmental science; Atmospheric sciences; Environmental chemistry; Oceanography; Geology; Chemistry; Bioaccumulation; Geomorphology","score_opus":0.03839352048183239,"score_gpt":0.30842089391005784,"score_spread":0.27002737342822547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068352917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995285,0.00008077724,0.00007822213,0.0000057040734,0.0000021164471,0.00000437188,0.00008726226,0.0000034593163,0.00020941834],"genre_scores_gemma":[0.9985514,0.00020047152,0.00028923148,0.000016186714,0.0000060968737,0.0000075034745,0.00034365244,0.000003945104,0.0005814763],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.000007476926,0.0000023898033,0.000016708553,0.000023182049,0.00002258633],"domain_scores_gemma":[0.9999118,0.000007987358,0.000016228796,0.0000032348569,0.000036831658,0.00002390516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015315483,0.00034800803,0.00031107786,0.0005557074,0.0011912776,0.0006192892,0.00018978707,0.0002618608,0.00032945408],"category_scores_gemma":[0.00012095571,0.00017044107,0.00018439577,0.00039177932,0.00024867474,0.00021916835,0.00031818877,0.00018297501,0.000097157266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016963693,0.0001896913,0.62078905,0.00009211839,0.0001691833,0.000908227,0.0018831783,0.00089729705,0.3575777,0.00009664628,0.00027759097,0.015422912],"study_design_scores_gemma":[0.00001854367,0.0006202165,0.9604898,0.000012121219,0.00005766943,0.00017757421,0.0010002748,0.0016042739,0.034175526,0.00008710955,0.0017458843,0.000010956887],"about_ca_topic_score_codex":0.11690863,"about_ca_topic_score_gemma":0.18079051,"teacher_disagreement_score":0.11690863,"about_ca_system_score_codex":0.00086167624,"about_ca_system_score_gemma":0.00066286983,"threshold_uncertainty_score":0.23245633},"labels":[],"label_agreement":null},{"id":"W2068465863","doi":"10.1029/2007gl031396","title":"Effect of lower mantle viscosity on the time‐dependence of plate velocities in three‐dimensional mantle convection models","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"","keywords":"Mantle convection; Mantle (geology); Geology; Geophysics; Convection; Viscosity; Earth's internal heat budget; Plate tectonics; Mechanics; Thermodynamics; Physics; Lithosphere; Seismology","score_opus":0.022327623940491547,"score_gpt":0.2707042091419947,"score_spread":0.24837658520150319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2068465863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98999584,0.00020929526,0.006766389,0.00025798,0.00001880952,0.000017760345,0.00009007172,0.00012122509,0.0025227258],"genre_scores_gemma":[0.9977093,0.000086460546,0.0018335914,0.000015665995,0.0000066632183,0.000011346867,0.00003675782,0.000035834248,0.00026436595],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998228,0.00006866537,0.00000982692,0.000018373643,0.00003689338,0.00004349379],"domain_scores_gemma":[0.9982546,0.0010684365,0.0003066146,0.00015555181,0.000073133866,0.00014153784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005760998,0.0006805219,0.0005638177,0.00052534166,0.00053333485,0.0010810955,0.00064174226,0.0006625866,0.0007208727],"category_scores_gemma":[0.004402568,0.0005019779,0.00075431366,0.00033640247,0.0010858565,0.0006999786,0.00086598436,0.0009345672,0.0000856044],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022924134,0.0000782975,0.006739851,0.000040318515,0.000038894155,0.00018171461,0.000082346305,0.9713415,0.016388517,0.002883085,0.00012262791,0.0018736785],"study_design_scores_gemma":[0.000022403048,0.000035894496,0.0011756396,0.0000048553184,0.000016832912,0.000015718082,0.000011295157,0.99582565,0.0023942336,0.00041030254,0.00007732912,0.000009816061],"about_ca_topic_score_codex":0.009826589,"about_ca_topic_score_gemma":0.0056695556,"teacher_disagreement_score":0.009826589,"about_ca_system_score_codex":0.00066929753,"about_ca_system_score_gemma":0.00053589774,"threshold_uncertainty_score":0.01953882},"labels":[],"label_agreement":null},{"id":"W2069344965","doi":"10.1029/2008gl035727","title":"Precipitation of radiation belt electrons by EMIC waves, observed from ground and space","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":309,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"","keywords":"Van Allen radiation belt; Physics; Electron precipitation; Electron; Plasmasphere; Van Allen Probes; Atomic physics; Ion; Relativistic particle; Proton; Pitch angle; Cyclotron; Computational physics; Geophysics; Magnetosphere; Astrophysics; Nuclear physics; Plasma","score_opus":0.019703683098352694,"score_gpt":0.26283078201482546,"score_spread":0.24312709891647277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069344965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983943,0.00020211843,0.00038905695,0.000014785867,0.000005133901,0.000002780016,0.000085382184,0.000017965995,0.0008884873],"genre_scores_gemma":[0.9992434,0.0000970172,0.00029902757,0.000011281922,0.000012139016,0.0000026098692,0.00017363556,0.0000054610678,0.00015541601],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.0000046937303,0.000002683308,0.0000151238155,0.000015882457,0.00001254703],"domain_scores_gemma":[0.99977726,0.000031157397,0.000121803285,0.000027791786,0.000024887438,0.000017144637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010371656,0.00017764754,0.00013782327,0.00046892196,0.0002424759,0.0003037398,0.00020284651,0.00022592608,0.0005165994],"category_scores_gemma":[0.00031703842,0.000092664246,0.000111741916,0.00051871984,0.00018902622,0.00025948757,0.00033723368,0.00023932103,0.00013717217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007409724,0.000118353586,0.72180784,0.00013024073,0.00016449299,0.0011026093,0.0007784131,0.0017581185,0.24406993,0.000565045,0.00084092666,0.027923113],"study_design_scores_gemma":[0.000046320347,0.00039068173,0.9606766,0.000014663387,0.00008208955,0.0009172033,0.0003583357,0.003668633,0.03059138,0.00033655815,0.0029048799,0.000012585791],"about_ca_topic_score_codex":0.0008965202,"about_ca_topic_score_gemma":0.0009817012,"teacher_disagreement_score":0.0008965202,"about_ca_system_score_codex":0.00011607609,"about_ca_system_score_gemma":0.00005436641,"threshold_uncertainty_score":0.0017825961},"labels":[],"label_agreement":null},{"id":"W2069435259","doi":"10.1029/2006gl027521","title":"Estimating canopy snow unloading timescales from daily observations of albedo and precipitation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Snow; Albedo (alchemy); Canopy; Environmental science; Precipitation; Atmospheric sciences; Taiga; Black spruce; Laplace transform; Climatology; Meteorology; Mathematics; Geology; Geography; Forestry","score_opus":0.04592554709538553,"score_gpt":0.2797579205520955,"score_spread":0.23383237345670993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069435259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5463256,0.000348195,0.4497919,0.000055156586,0.000026248355,0.00006228639,0.0007156046,0.0010038478,0.0016711352],"genre_scores_gemma":[0.85266346,0.00013556889,0.14603037,0.000009277086,0.00002068712,0.000045748195,0.00063137844,0.000061255574,0.0004022539],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995255,0.000005306168,0.0000029824462,0.000014250972,0.000016749636,0.00000815698],"domain_scores_gemma":[0.9997476,0.0000936505,0.00005794548,0.000025422092,0.00005292268,0.000022479895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025101105,0.0003903872,0.00022577061,0.00066968193,0.0002496247,0.0002878299,0.0003010885,0.0001993872,0.00044803685],"category_scores_gemma":[0.00095029944,0.00021519343,0.00023065775,0.00042980604,0.00010458377,0.0004530488,0.0002268045,0.00025389798,0.00009843243],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034544003,0.00024116936,0.22656032,0.00024974422,0.00023925572,0.00025129993,0.00029939154,0.33637097,0.09639434,0.0031255265,0.0013278851,0.33459464],"study_design_scores_gemma":[0.000034191842,0.00006522806,0.10532817,0.000012072676,0.000033959685,0.00015390519,0.00004511916,0.88287586,0.008794492,0.0015785388,0.0010381237,0.00004025316],"about_ca_topic_score_codex":0.019226681,"about_ca_topic_score_gemma":0.031167516,"teacher_disagreement_score":0.019226681,"about_ca_system_score_codex":0.0003194106,"about_ca_system_score_gemma":0.0005702885,"threshold_uncertainty_score":0.038229525},"labels":[],"label_agreement":null},{"id":"W2069468639","doi":"10.1029/2004gl020324","title":"Solar heating by the near‐IR CO<sub>2</sub> bands in the mesosphere","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Mesosphere; Atmospheric sciences; Atmosphere (unit); Thermal; Environmental science; Absorption (acoustics); Infrared; Near-infrared spectroscopy; Solar energy; Computational physics; Physics; Materials science; Meteorology; Optics; Stratosphere","score_opus":0.02078121894150912,"score_gpt":0.27084703763421264,"score_spread":0.2500658186927035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069468639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96931756,0.00035887805,0.018176023,0.00027381652,0.00004397556,0.00003822041,0.00065482827,0.00037314708,0.010763468],"genre_scores_gemma":[0.9978447,0.00014865145,0.0011587662,0.000017374152,0.000004373582,0.000008640052,0.00009934046,0.000024720626,0.0006933852],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000059970203,0.0000012528237,0.000010080167,0.000013334568,0.000016597827],"domain_scores_gemma":[0.9999567,0.000010704682,0.000005510676,0.000007905703,0.0000097289385,0.000009368095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000097558244,0.00040289116,0.0002026758,0.00012710436,0.00043812787,0.00052466133,0.00041782288,0.00035953574,0.0012691602],"category_scores_gemma":[0.00024549817,0.0002693759,0.00043402208,0.00024376335,0.0004580065,0.0005156745,0.00025708805,0.00038485025,0.00014658803],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019277714,0.00004687975,0.023484135,0.00008733451,0.00008491814,0.00015521517,0.00008278986,0.8689422,0.09336554,0.0053285174,0.000802802,0.0074269287],"study_design_scores_gemma":[0.000065799104,0.00005254549,0.058502696,0.0000106918405,0.00007137583,0.000068996196,0.00006378976,0.91797197,0.01813342,0.0027696884,0.002256031,0.000032943204],"about_ca_topic_score_codex":0.13245013,"about_ca_topic_score_gemma":0.12947021,"teacher_disagreement_score":0.13245013,"about_ca_system_score_codex":0.0018933555,"about_ca_system_score_gemma":0.0011059389,"threshold_uncertainty_score":0.26335835},"labels":[],"label_agreement":null},{"id":"W2069558280","doi":"10.1029/2003gl018294","title":"Transient and disruption cavity dimensions of complex terrestrial impact structures derived from magnetic data","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Geological Survey of Canada","funders":"","keywords":"Impact crater; Geology; Transient (computer programming); Magnetic anomaly; Anomaly (physics); Geophysics; Physics; Astrobiology","score_opus":0.09137808521510055,"score_gpt":0.3497060627850629,"score_spread":0.25832797756996234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069558280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99320036,0.00012296827,0.0042216703,0.000011964575,0.0000015087938,0.00001429332,0.000851559,0.000086927874,0.0014886237],"genre_scores_gemma":[0.99722856,0.000036718113,0.0019971004,0.000001716782,0.00000105372,0.0000070427473,0.0006529109,0.000008968509,0.000065810265],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976724,0.000021954134,0.000032430642,0.00005853727,0.000086683176,0.000033258715],"domain_scores_gemma":[0.9972989,0.0011332843,0.00084809284,0.00027513225,0.00029659912,0.00014793844],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040011207,0.00019391986,0.0001690335,0.0019636033,0.00026376892,0.0005395547,0.00023848712,0.00016688924,0.00076200225],"category_scores_gemma":[0.0045015346,0.00021519898,0.00016007821,0.00094876916,0.0004436173,0.0004736222,0.0007806404,0.00018744839,0.00015009595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029334318,0.000029515246,0.8921755,0.00012595447,0.000061053805,0.0003408957,0.00070778385,0.021878894,0.0281178,0.0014287763,0.00066180434,0.054178596],"study_design_scores_gemma":[0.000007103559,0.000054609696,0.96367645,0.000014037509,0.000016772457,0.0004517739,0.00017262949,0.022001665,0.011563046,0.00059301616,0.0014232198,0.000025620155],"about_ca_topic_score_codex":0.004418781,"about_ca_topic_score_gemma":0.0064840196,"teacher_disagreement_score":0.004418781,"about_ca_system_score_codex":0.0005052314,"about_ca_system_score_gemma":0.00025458253,"threshold_uncertainty_score":0.008786142},"labels":[],"label_agreement":null},{"id":"W2069582825","doi":"10.1029/2007gl032300","title":"Carbon monoxide pollution from cities and urban areas observed by the Terra/MOPITT mission","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Centro Internacional de Agricultura Tropical; University of Toronto; National Center for Atmospheric Research; National Science Foundation","keywords":"Environmental science; Troposphere; Pollution; Daytime; Atmospheric sciences; Carbon monoxide; Air pollution; Atmosphere (unit); Satellite; Planetary boundary layer; Remote sensing; Meteorology; Geography; Geology","score_opus":0.05055276520197368,"score_gpt":0.2485176756761248,"score_spread":0.1979649104741511,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069582825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99843305,0.000028642404,0.00011123313,0.000016238768,0.000002003751,0.000008879512,0.00080761116,0.000028920369,0.000563327],"genre_scores_gemma":[0.9954918,0.000052790154,0.0010163198,0.000021757713,0.000011038667,0.0000130306025,0.003143823,0.00001439351,0.00023511892],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998987,0.00000993211,0.000004544772,0.000026745034,0.000036580328,0.000023563118],"domain_scores_gemma":[0.9998758,0.000011433392,0.000037135946,0.000018388868,0.000026761107,0.000030338682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016166769,0.0003255246,0.00025280807,0.0007531285,0.000445246,0.00034336577,0.00023538704,0.0003233301,0.00040992117],"category_scores_gemma":[0.00017835239,0.00015719596,0.0002054515,0.0009916301,0.00018934622,0.00021879627,0.00040598636,0.00027248383,0.00016584623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008069362,0.00031738766,0.8240431,0.000080521655,0.00024428745,0.0012401049,0.0006893648,0.0039544804,0.14920765,0.00015727204,0.0022346545,0.017024215],"study_design_scores_gemma":[0.000015698792,0.00008310365,0.99217176,0.0000031453237,0.000023245473,0.00025897662,0.00009766459,0.0026087717,0.0041519688,0.000024089497,0.00055392453,0.000007726859],"about_ca_topic_score_codex":0.013247384,"about_ca_topic_score_gemma":0.022124732,"teacher_disagreement_score":0.013247384,"about_ca_system_score_codex":0.0002583752,"about_ca_system_score_gemma":0.00015046894,"threshold_uncertainty_score":0.026340544},"labels":[],"label_agreement":null},{"id":"W2069652628","doi":"10.1029/2004gl021002","title":"Signal propagation related to the North Atlantic overturning","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung; Deutsches Klimarechenzentrum","keywords":"Thermohaline circulation; Geology; Climatology; Forcing (mathematics); Flux (metallurgy); North Atlantic oscillation; Eddy; Subtropics; Zonal and meridional; Oscillation (cell signaling); Convection; Turbulence; Mechanics; Physics; Materials science","score_opus":0.029056336960950387,"score_gpt":0.2899531572499798,"score_spread":0.2608968202890294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069652628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920328,0.00009909877,0.0054173865,0.00006554259,0.000021732312,0.000008566462,0.0002302782,0.00022138523,0.0019030059],"genre_scores_gemma":[0.9986563,0.00004313729,0.0006727468,0.000006699556,0.000005535777,0.0000024888748,0.00025011363,0.000017378055,0.00034556896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.0000117526315,0.0000037271914,0.000014355229,0.000024314077,0.000016903628],"domain_scores_gemma":[0.9992699,0.00034921805,0.00012202348,0.000044430286,0.00015157287,0.00006292381],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022277971,0.00022519058,0.000113117385,0.00035197847,0.00016169636,0.00039472932,0.00012487703,0.00017260876,0.0015425641],"category_scores_gemma":[0.0016997124,0.00013965472,0.00014949263,0.00022704357,0.00011775066,0.00016696437,0.00026223357,0.00028918323,0.00010934038],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017785863,0.00019794494,0.35737514,0.0002166552,0.00016337281,0.0008156524,0.000561754,0.2921698,0.18416812,0.00698551,0.00254937,0.15301809],"study_design_scores_gemma":[0.00007127192,0.0003584282,0.3200775,0.0000180635,0.000090880065,0.00025490543,0.000059071284,0.64983636,0.02591445,0.0014916457,0.0017905845,0.000036773603],"about_ca_topic_score_codex":0.0076429076,"about_ca_topic_score_gemma":0.004053939,"teacher_disagreement_score":0.0076429076,"about_ca_system_score_codex":0.00041830871,"about_ca_system_score_gemma":0.0002906498,"threshold_uncertainty_score":0.0151968},"labels":[],"label_agreement":null},{"id":"W2069681072","doi":"10.1029/2008gl033244","title":"Ensemble 1‐Year predictions of Arctic sea ice for the spring and summer of 2008","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Arctic ice pack; Sea ice; Climatology; Spring (device); Cryosphere; Arctic sea ice decline; Forcing (mathematics); Drift ice; Antarctic sea ice; Arctic; Environmental science; Lead (geology); Sea ice thickness; Oceanography; Arctic geoengineering; Geology","score_opus":0.0430745930425501,"score_gpt":0.27465267979441704,"score_spread":0.23157808675186695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069681072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9764988,0.00016942393,0.010710247,0.00017457595,0.000084587125,0.000013288443,0.009121163,0.0002975355,0.0029302922],"genre_scores_gemma":[0.9776924,0.0001633608,0.0066139554,0.00004104609,0.0000367798,0.000050317394,0.014016874,0.0000557925,0.0013293171],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989104,0.000019439416,0.0000054835573,0.000035438206,0.000021868209,0.000026762076],"domain_scores_gemma":[0.999597,0.00011367009,0.000050619048,0.000060710307,0.00013752075,0.00004051281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054981,0.0005056365,0.0005287338,0.00038698112,0.00044812847,0.00041230908,0.0006809498,0.00066505204,0.0011896929],"category_scores_gemma":[0.0010726143,0.0003785363,0.000773564,0.000510086,0.00015278539,0.00087009545,0.0003035346,0.0007567786,0.0004781473],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001415963,0.000070655115,0.032315142,0.00001679857,0.0001479602,0.00004608718,0.000040861407,0.95414317,0.000875413,0.00042506322,0.0029183384,0.00885896],"study_design_scores_gemma":[0.0000369697,0.00003706212,0.020190742,0.0000055449395,0.00003639848,0.000017337019,0.000017922855,0.9774185,0.0007853496,0.00047610197,0.0009507716,0.000027261724],"about_ca_topic_score_codex":0.044163138,"about_ca_topic_score_gemma":0.047142662,"teacher_disagreement_score":0.044163138,"about_ca_system_score_codex":0.00060089823,"about_ca_system_score_gemma":0.000825672,"threshold_uncertainty_score":0.087812185},"labels":[],"label_agreement":null},{"id":"W2069743211","doi":"10.1029/2002gl015321","title":"Large‐amplitude internal wave generation in the lee of step‐shaped topography","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Internal wave; Buoyancy; Longitudinal wave; Stratified flows; Mechanics; Stratified flow; Amplitude; Mechanical wave; Geology; Wave propagation; Gravity wave; Physics; Surface wave; Geophysics; Optics; Turbulence","score_opus":0.055267252840775404,"score_gpt":0.27599495687595343,"score_spread":0.22072770403517802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069743211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984742,0.000009716646,0.00084026076,0.000008308013,0.0000017164693,0.0000026960493,0.000006475775,0.000014450378,0.0006422443],"genre_scores_gemma":[0.9993882,0.0000124568805,0.00035860797,0.000004916744,8.991065e-7,0.000002704786,0.000014270882,0.000002987958,0.0002148151],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996173,0.000006909269,0.0000011852898,0.000005168495,0.000010452731,0.000014506383],"domain_scores_gemma":[0.9998647,0.000044326804,0.000027635368,0.000016824668,0.000015980828,0.000030507146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000082307626,0.00008672248,0.000105920524,0.000113995244,0.00015482875,0.00025721604,0.000085864376,0.000113956004,0.00062954857],"category_scores_gemma":[0.00033437196,0.00010990455,0.0001122857,0.00007153482,0.00040303927,0.0002049127,0.00035124566,0.00019730594,0.000116541894],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036506046,0.0000785635,0.019093985,0.000043604494,0.000014805816,0.00043475133,0.00040351646,0.002638627,0.9643997,0.0012555879,0.00020138416,0.011070501],"study_design_scores_gemma":[0.00026103324,0.0018226351,0.23407525,0.000027272628,0.00008114986,0.00067483925,0.0011920087,0.070241205,0.68694025,0.0026047968,0.0020139457,0.00006564068],"about_ca_topic_score_codex":0.00070388895,"about_ca_topic_score_gemma":0.0008905156,"teacher_disagreement_score":0.00070388895,"about_ca_system_score_codex":0.00010916993,"about_ca_system_score_gemma":0.000109988316,"threshold_uncertainty_score":0.002106011},"labels":[],"label_agreement":null},{"id":"W2069794998","doi":"10.1029/2004gl020084","title":"Advective spreading of storm‐induced inertial oscillations in a model of the northwest Atlantic Ocean","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Advection; Storm; Geology; Geostrophic wind; Oceanography; Ocean current; Climatology; Inertial wave; Storm track; Environmental science","score_opus":0.042982642015648026,"score_gpt":0.28495385760529457,"score_spread":0.24197121558964654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069794998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951749,0.00007772782,0.0021457616,0.00017635712,0.000015518723,0.0000070651845,0.00015952866,0.00003489346,0.0022082075],"genre_scores_gemma":[0.99857616,0.000071141236,0.00040987768,0.0000117395075,0.0000074391555,0.000006452664,0.000071616305,0.000008110282,0.00083749834],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996686,0.000010580538,0.0000021204469,0.000006788997,0.0000043340115,0.000009362376],"domain_scores_gemma":[0.9998275,0.00006035319,0.00003777289,0.0000125247525,0.000024536732,0.000037308797],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015616912,0.00028471168,0.00024676754,0.00016990998,0.00040913236,0.0006739692,0.00060330326,0.0006416533,0.0011937233],"category_scores_gemma":[0.00063961156,0.00029492617,0.00045710648,0.00017204892,0.00045192623,0.00035173725,0.0003892176,0.00037927768,0.00011334252],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014251978,0.00003606824,0.009906983,0.000011999899,0.00003082133,0.00014998508,0.000049916634,0.98467386,0.002469559,0.0013309567,0.00020484818,0.000992467],"study_design_scores_gemma":[0.000024811889,0.000023482507,0.0023612871,0.000001581119,0.000008806462,0.000009967995,0.000016462507,0.99718434,0.00009243049,0.00019677928,0.00007595646,0.000004032999],"about_ca_topic_score_codex":0.13787211,"about_ca_topic_score_gemma":0.06744226,"teacher_disagreement_score":0.13787211,"about_ca_system_score_codex":0.0009922769,"about_ca_system_score_gemma":0.0007240067,"threshold_uncertainty_score":0.27413917},"labels":[],"label_agreement":null},{"id":"W2069813103","doi":"10.1029/2005gl024956","title":"The effects of geothermal heating on the ocean overturning circulation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"University of Canberra; Australian National University","keywords":"Thermocline; Heat flux; Buoyancy; Downwelling; Geothermal gradient; Geology; Geothermal heating; Plume; Flux (metallurgy); Forcing (mathematics); Thermohaline circulation; Geophysics; Circulation (fluid dynamics); Mechanics; Atmospheric sciences; Heat transfer; Climatology; Oceanography; Meteorology; Geothermal energy; Materials science; Upwelling; Physics","score_opus":0.01181732154663088,"score_gpt":0.23719067073813807,"score_spread":0.2253733491915072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2069813103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99928325,0.000027488173,0.00019860877,0.000022182572,0.0000053463154,0.0000025058132,0.00002101506,0.000013718073,0.00042590723],"genre_scores_gemma":[0.9997632,0.00001881389,0.00005864057,0.0000072377084,0.0000027506894,0.000001471705,0.0000139636795,0.0000037718823,0.00013009606],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999472,0.000011342814,0.000002398606,0.000008202164,0.0000073352,0.000023439576],"domain_scores_gemma":[0.9996791,0.00017394037,0.000037272428,0.000020408379,0.000025293346,0.00006398042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011873984,0.00023252117,0.00020450457,0.0001209842,0.0001927107,0.0003028218,0.00013489922,0.00023303363,0.0013394641],"category_scores_gemma":[0.0008374267,0.00012612833,0.00022918571,0.00007468524,0.0003960661,0.0001706406,0.0002686042,0.0003474808,0.0000961036],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014393626,0.00021604095,0.043655418,0.00013821716,0.00009069932,0.000768217,0.0002102477,0.09129131,0.84795034,0.0008516867,0.00028703024,0.013101554],"study_design_scores_gemma":[0.00024345373,0.00165362,0.5380916,0.00001934958,0.00016826951,0.00027608898,0.00030157916,0.31554675,0.14191703,0.0008339578,0.00088781415,0.000060492788],"about_ca_topic_score_codex":0.0028105115,"about_ca_topic_score_gemma":0.002022858,"teacher_disagreement_score":0.0028105115,"about_ca_system_score_codex":0.0003262591,"about_ca_system_score_gemma":0.00013849317,"threshold_uncertainty_score":0.0055883527},"labels":[],"label_agreement":null},{"id":"W2070219271","doi":"10.1029/2006gl027258","title":"Spatial variability and trends in observed snow depth over North America","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":206,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; University of Georgia; U.S. Department of Agriculture; National Aeronautics and Space Administration","keywords":"Snow; Snow line; Spring (device); Physical geography; Snow cover; Climatology; Geology; Spatial variability; Environmental science; Geography; Geomorphology","score_opus":0.04436347529009284,"score_gpt":0.2763822608982016,"score_spread":0.2320187856081088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070219271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99474347,0.000336126,0.0001285664,0.00006531111,0.0000038610274,0.0000032310463,0.003970391,0.00001688159,0.00073213305],"genre_scores_gemma":[0.99553853,0.00027450183,0.00020182822,0.000014403468,0.0000050826443,0.0000062705444,0.0036878139,0.0000040325913,0.000267508],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981517,0.000017897986,0.000014307756,0.000059843045,0.000049934595,0.00004288045],"domain_scores_gemma":[0.99929583,0.00013263714,0.0001533409,0.000043805296,0.00030520206,0.0000692481],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028638708,0.00012325839,0.0001615495,0.0011025707,0.00030634558,0.0004904718,0.0002719331,0.000123864,0.0005775069],"category_scores_gemma":[0.0010461021,0.00014610715,0.00018118888,0.0022873334,0.00021246515,0.00026121424,0.00026100213,0.00017385319,0.000081751234],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000025233529,0.000009749382,0.99115175,0.00002104722,0.00008086088,0.000034149496,0.0003999313,0.00073773216,0.0005725141,0.000061707855,0.0007605484,0.0061448226],"study_design_scores_gemma":[8.177596e-7,0.0000019126837,0.9988949,0.000003948185,0.000005238877,0.000012285694,0.000112795526,0.00036756287,0.000035670324,0.000008499961,0.0005547726,0.0000017644044],"about_ca_topic_score_codex":0.7706406,"about_ca_topic_score_gemma":0.8841959,"teacher_disagreement_score":0.22935939,"about_ca_system_score_codex":0.0020835954,"about_ca_system_score_gemma":0.001333408,"threshold_uncertainty_score":0.46142024},"labels":[],"label_agreement":null},{"id":"W2070387495","doi":"10.1029/2006gl027282","title":"Energy avalanches in the central plasma sheet","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Canadian Space Agency","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Plasma sheet; Instability; Physics; Plasma; Node (physics); Mechanics; Energy flux; Energy (signal processing); Energy distribution; Atomic physics; Magnetosphere; Quantum mechanics","score_opus":0.011601758432286231,"score_gpt":0.2533319614553916,"score_spread":0.24173020302310538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070387495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9899047,0.00006236828,0.0067773648,0.00007948358,0.00001384306,0.00000853397,0.000041121264,0.00010857302,0.0030040408],"genre_scores_gemma":[0.99894196,0.000017523105,0.0007118902,0.000007734982,0.000002059569,0.0000080652235,0.000020732206,0.000006364085,0.00028374034],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999372,0.000014504629,0.0000030739748,0.000013355093,0.000011036035,0.000020784315],"domain_scores_gemma":[0.99969995,0.00012335465,0.000051617026,0.000033391447,0.000036473128,0.000055231307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017304001,0.0002056267,0.00028864606,0.00029711623,0.00047272915,0.0007090752,0.0004083593,0.0003976306,0.0013609049],"category_scores_gemma":[0.000819616,0.00017511712,0.0003853554,0.000179057,0.0008613893,0.00037624367,0.0005312549,0.00033469408,0.000074302916],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013929296,0.00005157719,0.007745811,0.000028841603,0.000042168398,0.00032431984,0.00016640368,0.97119284,0.007054501,0.00986135,0.00038607122,0.0030068762],"study_design_scores_gemma":[0.000019627261,0.00003579768,0.0009396761,0.0000034106808,0.000008263334,0.000033358105,0.000031935517,0.99555403,0.0008866119,0.0022476718,0.00023340038,0.000006247863],"about_ca_topic_score_codex":0.006694202,"about_ca_topic_score_gemma":0.0025391828,"teacher_disagreement_score":0.006694202,"about_ca_system_score_codex":0.0006624549,"about_ca_system_score_gemma":0.00046775746,"threshold_uncertainty_score":0.013310492},"labels":[],"label_agreement":null},{"id":"W2070417935","doi":"10.1029/2002gl016807","title":"Evidence for recent changes in a surface‐air warming singularity in late winter over central North America","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Period (music); Global warming; Environmental science; Spring (device); Surface air temperature; Climate change; Geography; Geology; Oceanography","score_opus":0.09953326970802408,"score_gpt":0.34708326993600114,"score_spread":0.24755000022797707,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070417935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987149,0.0002553841,0.000060142123,0.00011396351,0.0000057897196,0.0000017274173,0.000078185294,0.0000069241482,0.0007628926],"genre_scores_gemma":[0.99956447,0.00009402214,0.000043770964,0.00003006837,0.000010778669,0.0000014233863,0.00014062159,0.0000016315282,0.000113270544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999372,0.0000053317326,0.0000047477074,0.000022931445,0.000012344046,0.000017342245],"domain_scores_gemma":[0.9994704,0.000058531667,0.00018095064,0.000032608987,0.000167978,0.00008946028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027994634,0.00011089316,0.00018952269,0.00067596557,0.00045612152,0.00067581394,0.0002565491,0.0002854069,0.0010633072],"category_scores_gemma":[0.0005997056,0.00014242071,0.00015408309,0.0006374898,0.00041875616,0.00028632017,0.00027918458,0.0002814831,0.000075639146],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017388955,0.000040302966,0.9768956,0.000058902053,0.00007671711,0.00022165471,0.00085511105,0.00039311725,0.013009581,0.0002526801,0.0003946348,0.0076278555],"study_design_scores_gemma":[0.0000015245533,0.0000072943544,0.99951506,0.0000026489345,0.0000042040274,0.00001887578,0.00007703481,0.00004657876,0.00007060218,0.000011593275,0.00024348476,0.0000010994946],"about_ca_topic_score_codex":0.05837885,"about_ca_topic_score_gemma":0.13287517,"teacher_disagreement_score":0.9416211,"about_ca_system_score_codex":0.00067632284,"about_ca_system_score_gemma":0.00045044435,"threshold_uncertainty_score":0.11607808},"labels":[],"label_agreement":null},{"id":"W2070758248","doi":"10.1029/2008gl033174","title":"COSMIC GPS Observations of Northern Hemisphere winter stratospheric gravity waves and comparisons with an atmospheric general circulation model","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Northern Hemisphere; Gravity wave; Atmospheric sciences; Climatology; Atmospheric wave; Stratosphere; Orographic lift; Atmospheric circulation; Jet stream; COSMIC cancer database; Environmental science; Geology; Gravitational wave; Jet (fluid); Meteorology; Physics; Precipitation; Astronomy","score_opus":0.03534645794689642,"score_gpt":0.2752312237892366,"score_spread":0.23988476584234017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2070758248","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.892095,0.00016045047,0.00542849,0.000130058,0.000066701105,0.00008954353,0.08547362,0.0017808595,0.014775147],"genre_scores_gemma":[0.90709215,0.00022393008,0.007235997,0.000059675265,0.000053273034,0.000078048106,0.083481774,0.0001601773,0.0016148456],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981016,0.00003815688,0.000013021929,0.000040593663,0.00006678901,0.00003133603],"domain_scores_gemma":[0.9994287,0.00006710402,0.00014794843,0.000117862124,0.00017075206,0.000067650384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002906243,0.00050511607,0.00028273783,0.0009750382,0.00020617542,0.00042337293,0.00031499303,0.00024988758,0.0024174787],"category_scores_gemma":[0.00092560315,0.00015903893,0.00047120513,0.0023954394,0.0001510248,0.00031511468,0.0002974053,0.00024167779,0.00063738594],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055204815,0.00018299918,0.75832444,0.00022188564,0.00046172773,0.0004177539,0.00041712294,0.1271482,0.011928136,0.0037423586,0.045912318,0.050691005],"study_design_scores_gemma":[0.00008083951,0.00011894532,0.88883895,0.000021804646,0.000116265444,0.00018785823,0.00009788216,0.08946236,0.0037189885,0.0006408415,0.016679399,0.000035842022],"about_ca_topic_score_codex":0.056646958,"about_ca_topic_score_gemma":0.06521784,"teacher_disagreement_score":0.056646958,"about_ca_system_score_codex":0.0005173585,"about_ca_system_score_gemma":0.00048534243,"threshold_uncertainty_score":0.11263442},"labels":[],"label_agreement":null},{"id":"W2071132211","doi":"10.1029/2007gl031713","title":"Analytical solution for flow of gelling solutions in porous media","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Grouting, Rheology, and Soil Mechanics","field":"Engineering","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Nutrasource; University of Windsor","funders":"","keywords":"Porous medium; Grout; Materials science; Polymer; Porosity; Viscosity; Dispersion (optics); Hydraulic conductivity; Chemical engineering; Flow (mathematics); Geotechnical engineering; Polymer solution; Petroleum engineering; Composite material; Mechanics; Environmental science; Geology; Soil science; Engineering; Soil water","score_opus":0.05891775052626754,"score_gpt":0.3172774968437085,"score_spread":0.25835974631744096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071132211","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009099381,0.004992584,0.9597257,0.0014991987,0.00040478577,0.00033463354,0.0004853382,0.0009633021,0.02249507],"genre_scores_gemma":[0.20711218,0.0129582,0.693064,0.0014703615,0.00091416534,0.0019462209,0.0009912379,0.0005840935,0.08095956],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994343,0.00006594274,0.00004346354,0.0001223736,0.0002761482,0.000057736495],"domain_scores_gemma":[0.99860185,0.0007848657,0.00011000427,0.00006133132,0.00040551083,0.000036481637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010548965,0.0010991797,0.0007098253,0.0018328391,0.00053824537,0.0008867097,0.0012053387,0.0016523516,0.005270223],"category_scores_gemma":[0.0043821367,0.0004505292,0.00069206435,0.0005527765,0.0008081352,0.0013263355,0.00087046943,0.001883168,0.0030517203],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014743091,0.000440312,0.0016049427,0.0026255136,0.00011905295,0.0016756573,0.0010797135,0.09712198,0.33608907,0.34024665,0.025973493,0.19287623],"study_design_scores_gemma":[0.00009276176,0.00021956468,0.0010079686,0.0003463582,0.000058970832,0.0010195916,0.00021127595,0.6385056,0.13960308,0.08004495,0.13878973,0.00010023302],"about_ca_topic_score_codex":0.0022361085,"about_ca_topic_score_gemma":0.0017337028,"teacher_disagreement_score":0.005270223,"about_ca_system_score_codex":0.0012382482,"about_ca_system_score_gemma":0.0011132743,"threshold_uncertainty_score":0.017630637},"labels":[],"label_agreement":null},{"id":"W2071343844","doi":"10.1029/1999gl011251","title":"On shifts in the long‐term Umkehr radiance records and their influence on retrieved ozone profiles","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Goddard Space Flight Center; National Oceanic and Atmospheric Administration; Centre National de la Recherche Scientifique","keywords":"Radiance; Zenith; Environmental science; Ozone; Solar zenith angle; Satellite; Remote sensing; Ozone Monitoring Instrument; Atmospheric sciences; Term (time); Standard deviation; Meteorology; Physics; Geology; Statistics; Mathematics","score_opus":0.031688116717597706,"score_gpt":0.2837386116655813,"score_spread":0.2520504949479836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071343844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99472094,0.000743818,0.0023569404,0.00006677207,0.00002092027,0.000012913322,0.00035191057,0.000045743953,0.0016802074],"genre_scores_gemma":[0.99780744,0.00036471375,0.0009995698,0.000022886858,0.000018790415,0.0000054479697,0.00043974002,0.000024518122,0.0003168815],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99951124,0.00011557889,0.000025260464,0.0000896149,0.00020221896,0.00005607984],"domain_scores_gemma":[0.99773276,0.0013714827,0.00024287957,0.00022503556,0.00035475474,0.000073008894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010523023,0.00023689147,0.0001648685,0.0003711651,0.0002545869,0.00031620258,0.00023466058,0.000304595,0.0009385022],"category_scores_gemma":[0.0054354435,0.00011620953,0.00021238536,0.00079112704,0.00024170268,0.0004588379,0.00034400585,0.00027527913,0.00040954773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0036176096,0.0001273951,0.5322489,0.00040164392,0.00027592818,0.0015455548,0.0011613931,0.03161213,0.22249326,0.0010237682,0.0015720782,0.20392036],"study_design_scores_gemma":[0.00001175104,0.00011768653,0.9580258,0.00002746769,0.00007233557,0.00034568494,0.00018783796,0.008978524,0.030483507,0.000115096795,0.0016147722,0.000019514247],"about_ca_topic_score_codex":0.008536195,"about_ca_topic_score_gemma":0.010277387,"teacher_disagreement_score":0.008536195,"about_ca_system_score_codex":0.00035738113,"about_ca_system_score_gemma":0.00023205297,"threshold_uncertainty_score":0.016973019},"labels":[],"label_agreement":null},{"id":"W2071630498","doi":"10.1029/2005gl022845","title":"Decreasing river discharge in northern Canada","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":278,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Army Research Office","keywords":"Discharge; Arctic; Archipelago; Environmental science; North Atlantic oscillation; Pacific decadal oscillation; Surface runoff; Precipitation; Latitude; Climatology; Northern Hemisphere; Arctic oscillation; Oceanography; Sink (geography); The arctic; Hydrology (agriculture); Drainage basin; Geology; El Niño Southern Oscillation; Geography; Meteorology; Ecology","score_opus":0.04627479408757152,"score_gpt":0.28483077352801667,"score_spread":0.23855597944044515,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071630498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953193,0.0005034159,0.000059427777,0.00018774446,0.000004266807,0.0000032462947,0.0014412677,0.000014463773,0.0024668945],"genre_scores_gemma":[0.99750996,0.00030703464,0.00006742373,0.000048923564,0.000002163673,0.0000025586708,0.000958004,0.000004107731,0.0010998129],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99966466,0.000012002214,0.0000145012855,0.00007277619,0.000099087716,0.00013698956],"domain_scores_gemma":[0.9990427,0.00005862978,0.0001576159,0.00002770254,0.0005253828,0.00018804932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020116771,0.00017821658,0.00024755413,0.0013286701,0.0019122498,0.0013072909,0.00051441917,0.00030044903,0.001580785],"category_scores_gemma":[0.0013846924,0.00015913694,0.00020021573,0.0037177023,0.0007546246,0.00027395666,0.0005514969,0.0003456583,0.00012606653],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008486473,0.000013908579,0.9806318,0.000038962477,0.000046685775,0.00019987873,0.001128924,0.00062672707,0.0010247179,0.00041753083,0.0014084761,0.014377435],"study_design_scores_gemma":[0.000001938551,0.000005315377,0.9978561,0.0000069673356,0.000009625574,0.000052518557,0.00041759308,0.00015726377,0.00009245554,0.000029950896,0.0013638292,0.0000064271494],"about_ca_topic_score_codex":0.9885393,"about_ca_topic_score_gemma":0.9951149,"teacher_disagreement_score":0.018284017,"about_ca_system_score_codex":0.018284017,"about_ca_system_score_gemma":0.015895922,"threshold_uncertainty_score":0.13266045},"labels":[],"label_agreement":null},{"id":"W2071694890","doi":"10.1002/2013gl058748","title":"Global imaging of polar cap patches with dual airglow imagers","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":165,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Airglow; Noon; Polar; Dusk; Latitude; Local time; Bay; Sky; Daytime; Midnight; Geology; Physics; Atmospheric sciences; Geodesy; Astrophysics; Astronomy; Oceanography","score_opus":0.008180591853048045,"score_gpt":0.2577895518846998,"score_spread":0.24960896003165178,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071694890","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831903,0.00026412468,0.006344817,0.0000673438,0.000043509546,0.00006401059,0.0029145258,0.00050406874,0.0066072852],"genre_scores_gemma":[0.97847307,0.00014342568,0.015007315,0.000070967144,0.00007580698,0.000037963415,0.004185314,0.00012512974,0.0018810326],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99988663,0.0000072174603,0.0000018949517,0.000037303103,0.000027793263,0.000039105846],"domain_scores_gemma":[0.9998746,0.0000087333565,0.000020860038,0.000021067803,0.000037107686,0.000037714162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012647397,0.0003342525,0.00030711613,0.001312734,0.0002453185,0.000432769,0.00029548514,0.00026473714,0.0020230918],"category_scores_gemma":[0.00011578821,0.00024699845,0.00024396212,0.0007041774,0.00014913539,0.00025802362,0.00050728105,0.0003556896,0.000323315],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010984878,0.0002224637,0.06310916,0.00016997193,0.00018942164,0.0007683321,0.00050258724,0.0037363386,0.8737741,0.00027112832,0.004989585,0.051168412],"study_design_scores_gemma":[0.00006811571,0.00024546398,0.9238796,0.00001992245,0.000106933905,0.0005844468,0.0003391374,0.018740257,0.050838117,0.00014424992,0.0049970252,0.000036754678],"about_ca_topic_score_codex":0.0041932664,"about_ca_topic_score_gemma":0.013035126,"teacher_disagreement_score":0.0041932664,"about_ca_system_score_codex":0.00020210457,"about_ca_system_score_gemma":0.0001543291,"threshold_uncertainty_score":0.008337736},"labels":[],"label_agreement":null},{"id":"W2071894701","doi":"10.1029/2004gl020235","title":"Vertical resolution and information content of CO profiles retrieved by MOPITT","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":159,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Troposphere; Environmental science; Middle latitudes; Remote sensing; Atmospheric sciences; Meteorology; Climatology; Geology; Geography","score_opus":0.01869788055340013,"score_gpt":0.2529139503187532,"score_spread":0.23421606976535306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071894701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99152374,0.00013476427,0.0040903487,0.000051652813,0.0000094315765,0.000011144199,0.0021658652,0.00031757692,0.0016953854],"genre_scores_gemma":[0.9931559,0.000064582564,0.0034177501,0.000014059156,0.0000075220014,0.0000069720363,0.0030416006,0.000045256093,0.00024635516],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998604,0.000010350181,0.000007448375,0.00003669738,0.000049954528,0.000035189023],"domain_scores_gemma":[0.9996594,0.00007253911,0.000046336696,0.000037529717,0.00015378425,0.000030422245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019465678,0.00019358935,0.000181741,0.00080960814,0.00019404525,0.00045385817,0.00021792413,0.00026439913,0.0008027771],"category_scores_gemma":[0.0013280052,0.0001281021,0.00016273749,0.0007256659,0.000110493114,0.00039432463,0.00023507417,0.00024058827,0.00022353826],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018043097,0.00020029824,0.23624064,0.00020014797,0.00027949546,0.0004987618,0.0004208174,0.057769552,0.56960094,0.0013212198,0.0043787747,0.12728506],"study_design_scores_gemma":[0.000052606974,0.00008398502,0.77609855,0.000027234446,0.00006577584,0.000311944,0.00013630748,0.12484726,0.095558904,0.00030218507,0.0024577465,0.00005756033],"about_ca_topic_score_codex":0.010030422,"about_ca_topic_score_gemma":0.007056271,"teacher_disagreement_score":0.010030422,"about_ca_system_score_codex":0.00031207802,"about_ca_system_score_gemma":0.00017271133,"threshold_uncertainty_score":0.019944072},"labels":[],"label_agreement":null},{"id":"W2071961096","doi":"10.1029/2007gl031626","title":"Stratospheric control of the extratropical circulation response to surface forcing","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Stratosphere; Forcing (mathematics); Extratropical cyclone; Climatology; Atmospheric sciences; Environmental science; Troposphere; Polar vortex; Atmospheric circulation; Sudden stratospheric warming; Snow; Circulation (fluid dynamics); Arctic oscillation; Northern Hemisphere; Meteorology; Geology; Physics","score_opus":0.0313314482838295,"score_gpt":0.30868002209545387,"score_spread":0.27734857381162437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2071961096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784505,0.000036790883,0.00053559267,0.00009701393,0.000010427293,0.0000028518573,0.000085480606,0.00003844845,0.001348376],"genre_scores_gemma":[0.99968946,0.000018194793,0.000043502176,0.000007820582,0.0000030408291,0.0000013890393,0.000035448975,0.0000044683356,0.00019669595],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994504,0.000020862843,0.0000022216989,0.000009185636,0.0000054277702,0.000017200136],"domain_scores_gemma":[0.9998442,0.00005202371,0.000023755898,0.000017182976,0.00001693388,0.00004595658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017308291,0.00032962312,0.000245217,0.00015426155,0.00026122943,0.00059201353,0.00019036322,0.00030010662,0.0016845273],"category_scores_gemma":[0.000640515,0.00015773046,0.00032550565,0.00011111533,0.0002950083,0.0002732604,0.00048333738,0.0003006106,0.00015012085],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009151075,0.00022007573,0.16745412,0.000092145696,0.0003894334,0.0010082963,0.00040557914,0.62331015,0.18494034,0.0053643878,0.0016150234,0.014285328],"study_design_scores_gemma":[0.00009345331,0.0001703284,0.21098694,0.000008082539,0.00006235243,0.000088046145,0.00012813584,0.7826016,0.0034778188,0.0019007706,0.0004573849,0.00002499997],"about_ca_topic_score_codex":0.011574357,"about_ca_topic_score_gemma":0.0077994033,"teacher_disagreement_score":0.011574357,"about_ca_system_score_codex":0.00040762225,"about_ca_system_score_gemma":0.00037721818,"threshold_uncertainty_score":0.02301395},"labels":[],"label_agreement":null},{"id":"W2072040027","doi":"10.1029/1999gl008472","title":"Crossover plots: A useful method for plotting SIRM data in paleomagnetism","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Windsor","funders":"","keywords":"Paleomagnetism; Hematite; Magnetite; Pyrrhotite; Remanence; Geology; Grain size; Demagnetizing field; Saturation (graph theory); Mineralogy; Goethite; Single domain; Geophysics; Magnetization; Magnetic field; Pyrite; Magnetic domain; Chemistry; Geomorphology; Physics; Paleontology","score_opus":0.05502391019383756,"score_gpt":0.369441172626827,"score_spread":0.31441726243298945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072040027","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.041962475,0.0011364882,0.8198924,0.00048755278,0.00045715092,0.0003492575,0.0102622,0.108842015,0.016610477],"genre_scores_gemma":[0.18458347,0.0010680784,0.77690554,0.00023999618,0.00022505429,0.0010892099,0.008579383,0.017538805,0.00977046],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99913293,0.0002542405,0.00013572688,0.00013154738,0.00029122585,0.00005428027],"domain_scores_gemma":[0.9942,0.0032106554,0.0006610793,0.0009283502,0.0008370717,0.00016283453],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019798356,0.001073199,0.0007792677,0.005372031,0.00054851425,0.0012280172,0.0010413919,0.0008189736,0.032328382],"category_scores_gemma":[0.008221279,0.0005852473,0.00050351,0.0049660774,0.00042049107,0.0018216713,0.0010480873,0.0023871048,0.005781296],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023213904,0.00059576397,0.011100004,0.0024856096,0.00040989806,0.0010814779,0.0037850488,0.0039511817,0.2506713,0.025581092,0.08997675,0.6080405],"study_design_scores_gemma":[0.00038974386,0.00079407834,0.051302373,0.0004615589,0.00029566482,0.0048035034,0.0013472418,0.08215215,0.4565605,0.033638746,0.3676736,0.00058086624],"about_ca_topic_score_codex":0.000795951,"about_ca_topic_score_gemma":0.00094860996,"teacher_disagreement_score":0.032328382,"about_ca_system_score_codex":0.00030207928,"about_ca_system_score_gemma":0.0003940163,"threshold_uncertainty_score":0.10814929},"labels":[],"label_agreement":null},{"id":"W2072114961","doi":"10.1029/2008gl035295","title":"First observations of surface ozone concentration from the summit region of Mount Everest","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Stratosphere; Troposphere; Ozone; Atmospheric sciences; Tropospheric ozone; Summit; Environmental science; Climatology; Mount; Meteorology; Geology; Physical geography; Geography","score_opus":0.08215037344786014,"score_gpt":0.27199816396659016,"score_spread":0.18984779051873002,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072114961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955728,0.00030733747,0.00040089944,0.00011168871,0.000037215388,0.000011652612,0.00047691012,0.000026778715,0.0030547304],"genre_scores_gemma":[0.99645174,0.0003080697,0.0010483139,0.000057195808,0.00006991003,0.000013616468,0.0009492202,0.000007343698,0.0010945695],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986684,0.000011627732,0.0000052183273,0.000020773914,0.000052011,0.000043548916],"domain_scores_gemma":[0.9997305,0.00002972711,0.0000724454,0.000021635287,0.00009844487,0.000047161717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107955326,0.00018850245,0.00018631405,0.00037952908,0.00075769896,0.0003321274,0.00016506246,0.0002766019,0.0006873246],"category_scores_gemma":[0.00033122653,0.00013941947,0.00015758406,0.0003526201,0.00015928752,0.00026095708,0.00052030716,0.00054674293,0.00012721929],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031081893,0.0001304269,0.80940676,0.00014011857,0.00022257291,0.0016532976,0.0024440028,0.0003201804,0.14389585,0.00016358572,0.002823811,0.038488626],"study_design_scores_gemma":[0.00000258177,0.00006466773,0.9933282,0.0000071979225,0.00001940032,0.00014007303,0.0002986529,0.00007060355,0.003061899,0.000017342138,0.0029837578,0.0000056293416],"about_ca_topic_score_codex":0.008931718,"about_ca_topic_score_gemma":0.04897865,"teacher_disagreement_score":0.008931718,"about_ca_system_score_codex":0.00013571049,"about_ca_system_score_gemma":0.00016078266,"threshold_uncertainty_score":0.017759502},"labels":[],"label_agreement":null},{"id":"W2072351876","doi":"10.1029/2000gl008522","title":"Thermal Enhancement of Magnetic Fabrics in High Grade Gneisses","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnetite; Silicate; Gneiss; Orientation (vector space); Materials science; Anisotropy; Geology; Mineralogy; Banded iron formation; Thermal; Geochemistry; Composite material; Metallurgy; Chemical engineering; Archean; Geometry; Thermodynamics; Optics; Metamorphic rock; Physics","score_opus":0.017822110443070138,"score_gpt":0.28249663227052996,"score_spread":0.2646745218274598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072351876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99869484,0.0000804871,0.00020418515,0.000007197606,0.000001797753,0.0000021585918,0.000036402835,0.000010415532,0.0009625626],"genre_scores_gemma":[0.9985057,0.00004330282,0.00020766727,0.000010456871,0.0000025162703,0.0000030243807,0.00009016488,0.000008439376,0.0011288015],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999449,0.000006938695,0.0000028039035,0.000015522217,0.000016336839,0.000013386948],"domain_scores_gemma":[0.9999012,0.000013174591,0.000030303856,0.000013914027,0.00002133304,0.000020127856],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007792623,0.00013890567,0.00010658579,0.00029675107,0.0001480313,0.0002128015,0.000071894676,0.00013507968,0.0010821425],"category_scores_gemma":[0.00017036292,0.00015404577,0.00012018919,0.00012481358,0.00036953186,0.00008908857,0.000181402,0.00018048089,0.00024011436],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057362966,0.000003566705,0.0033473454,0.000012663459,0.0000055804385,0.000044082153,0.000046482703,0.00007642332,0.99558926,0.00003610154,0.000008649898,0.00077246793],"study_design_scores_gemma":[0.0000076211827,0.00019722302,0.69222695,0.0000047440058,0.0000207909,0.0005736226,0.00013994426,0.00032713433,0.3051629,0.000087470464,0.0012426162,0.000008998825],"about_ca_topic_score_codex":0.001452398,"about_ca_topic_score_gemma":0.0029924177,"teacher_disagreement_score":0.001452398,"about_ca_system_score_codex":0.0002331712,"about_ca_system_score_gemma":0.00007621985,"threshold_uncertainty_score":0.0036201477},"labels":[],"label_agreement":null},{"id":"W2072455239","doi":"10.1029/2008gl033234","title":"Multi‐model decadal potential predictability of precipitation and temperature","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Predictability; Climatology; Northern Hemisphere; Precipitation; Environmental science; Climate model; Latitude; Sea surface temperature; Atmospheric sciences; Climate change; Meteorology; Geology; Oceanography; Geography; Mathematics; Statistics","score_opus":0.04017897891654407,"score_gpt":0.3041660117036199,"score_spread":0.2639870327870758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072455239","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9880101,0.00021256942,0.0075112167,0.00044285442,0.000040250605,0.000006805848,0.001385063,0.00016999587,0.0022211086],"genre_scores_gemma":[0.9984876,0.00003827789,0.00068224856,0.000014191198,0.000010592338,0.0000072408725,0.0005677061,0.000014059961,0.00017811934],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983895,0.000042192103,0.000013659314,0.000056812514,0.000017909339,0.000030394354],"domain_scores_gemma":[0.9993401,0.00030836958,0.000111611975,0.00009290369,0.000085777596,0.000061204344],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001021599,0.0003804943,0.0003707577,0.00052088307,0.00035812033,0.0009413442,0.00056616106,0.00037961718,0.0009768207],"category_scores_gemma":[0.0019951987,0.00030277617,0.00065140263,0.00051031384,0.00024651192,0.0007863629,0.00047628404,0.000627729,0.00011484332],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024480865,0.00004816841,0.04917208,0.00002393349,0.00029659076,0.00007492054,0.000047375703,0.93667233,0.0014096601,0.0031161231,0.0013571219,0.0075367405],"study_design_scores_gemma":[0.000022724469,0.000017329412,0.015346503,0.0000032065636,0.000043141277,0.000013832508,0.000012817488,0.982077,0.0004332054,0.0017064391,0.00031206082,0.000011799692],"about_ca_topic_score_codex":0.015149463,"about_ca_topic_score_gemma":0.0121025,"teacher_disagreement_score":0.015149463,"about_ca_system_score_codex":0.00079645513,"about_ca_system_score_gemma":0.0005536484,"threshold_uncertainty_score":0.030122578},"labels":[],"label_agreement":null},{"id":"W2072691575","doi":"10.1029/1999gl008395","title":"Kunhild and Ereshkigal, an extinct hot‐spot region on Venus","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University","keywords":"Venus; Geology; Volcano; Plume; Volcanism; Mantle plume; Shield volcano; Mantle (geology); Hotspot (geology); Upwelling; Tectonics; Paleontology; Seismology; Astrobiology; Lithosphere; Meteorology; Physics; Oceanography","score_opus":0.04946776220638379,"score_gpt":0.3057856615245813,"score_spread":0.25631789931819754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072691575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984267,0.00009802269,0.000042496216,0.000025158444,0.0000025518746,0.000004203135,0.00017555445,0.000008691102,0.0012167501],"genre_scores_gemma":[0.99876094,0.000048191367,0.00017608229,0.000010816355,0.000002589405,0.0000019319853,0.00060356176,0.0000021726432,0.00039369878],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.0000034245652,0.000002324596,0.000014741316,0.000011493595,0.000023695282],"domain_scores_gemma":[0.9999287,0.000007310399,0.000018549918,0.0000053054946,0.0000072090415,0.000032938504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056985733,0.00010284309,0.000117443735,0.0008616245,0.00039529626,0.00023867775,0.00019568177,0.00019658955,0.00062222074],"category_scores_gemma":[0.00012975177,0.00007783421,0.00008379484,0.00036216067,0.00038400732,0.00018840634,0.00054312375,0.00013767721,0.00009767637],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037065434,0.00007938422,0.88420606,0.00016895776,0.00007692098,0.0029699297,0.0054453933,0.0007664884,0.056282755,0.00085121405,0.0015725902,0.04720976],"study_design_scores_gemma":[0.0000070938427,0.000020617592,0.99462044,0.000011819199,0.0000067963083,0.0004931376,0.0013677595,0.00023594749,0.0009682163,0.00006620004,0.0021975439,0.0000043748596],"about_ca_topic_score_codex":0.010817444,"about_ca_topic_score_gemma":0.04773728,"teacher_disagreement_score":0.010817444,"about_ca_system_score_codex":0.00043240513,"about_ca_system_score_gemma":0.00030494688,"threshold_uncertainty_score":0.021508932},"labels":[],"label_agreement":null},{"id":"W2072729586","doi":"10.1029/2005gl023961","title":"Constraining hydrological and cryospheric mass flux in southeastern Alaska using space‐based gravity measurements","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Snow; Flux (metallurgy); Environmental science; Altimeter; Water mass; Scaling; Climatology; Amplitude; Water level; Geology; Oceanography; Geodesy; Geography; Geomorphology","score_opus":0.11801129414191426,"score_gpt":0.3095339319610999,"score_spread":0.19152263781918566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072729586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992505,0.00003611222,0.0002232975,0.000020077561,0.0000021257547,0.0000012467528,0.00016791477,0.000015470912,0.000283319],"genre_scores_gemma":[0.9992142,0.000041499632,0.00039914163,0.0000051281204,0.0000034662883,0.000002309909,0.00026518697,0.0000022601562,0.00006677754],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999279,0.000016754704,0.000008155005,0.000023184151,0.000013111956,0.000011017981],"domain_scores_gemma":[0.99977154,0.00005027991,0.000065067834,0.000028990917,0.00004801926,0.000036057903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034146494,0.00022861868,0.00016067446,0.0007782347,0.0004588569,0.00040422377,0.0002267472,0.00023596182,0.0003485996],"category_scores_gemma":[0.0008014003,0.0001917254,0.00018657323,0.0006308017,0.00031232266,0.00036845403,0.00037754036,0.00015311148,0.00008540903],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010866005,0.00006042959,0.9676518,0.00001563982,0.00006573811,0.00018556697,0.00034063967,0.01728918,0.006138073,0.00027518862,0.00026362264,0.007605564],"study_design_scores_gemma":[0.00002017131,0.000030248688,0.9554685,0.000018250012,0.0000473112,0.00005390314,0.00052960846,0.04097161,0.0015590341,0.00047207743,0.00081099634,0.000018386832],"about_ca_topic_score_codex":0.105163574,"about_ca_topic_score_gemma":0.19765684,"teacher_disagreement_score":0.105163574,"about_ca_system_score_codex":0.0005713925,"about_ca_system_score_gemma":0.00045271078,"threshold_uncertainty_score":0.20910293},"labels":[],"label_agreement":null},{"id":"W2072739993","doi":"10.1029/2005gl022428","title":"Properties of high‐altitude tropical cirrus clouds determined from ACE FTS observations","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"","keywords":"Cirrus; Atmospheric sciences; Altitude (triangle); Environmental science; Satellite; Effects of high altitude on humans; Extinction (optical mineralogy); Meteorology; Physics; Geology; Astronomy; Mineralogy","score_opus":0.06485800803347301,"score_gpt":0.2775578539644923,"score_spread":0.21269984593101926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072739993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982718,0.00004361941,0.00019749781,0.00000800908,0.0000017401068,0.000003372693,0.00075767696,0.0000081359185,0.0007080318],"genre_scores_gemma":[0.9981914,0.00006187687,0.00028318423,0.0000047401963,0.0000052219593,0.0000015888089,0.0013554578,0.0000035184648,0.00009291131],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998964,0.000007415833,0.0000061747714,0.000017852542,0.00004107101,0.00003097327],"domain_scores_gemma":[0.99966514,0.000081140446,0.00007761972,0.000028118433,0.00010619227,0.00004179143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001915847,0.00015226704,0.00013635764,0.00045556272,0.00028021578,0.0004476428,0.0001724421,0.00012607181,0.0004259451],"category_scores_gemma":[0.0005355135,0.00010333461,0.00014973628,0.00055382756,0.0001267079,0.0002785101,0.00013030252,0.00015435366,0.00009949369],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002895082,0.000079463956,0.8732189,0.00006815223,0.00011495453,0.00039836584,0.00028960846,0.009170496,0.10117956,0.00026861296,0.000831534,0.014090773],"study_design_scores_gemma":[0.000005444941,0.00002081854,0.98567295,0.0000020751847,0.00001665426,0.00008994454,0.000058936068,0.006932056,0.0068557295,0.000020870024,0.000318281,0.0000062109984],"about_ca_topic_score_codex":0.032212812,"about_ca_topic_score_gemma":0.032876875,"teacher_disagreement_score":0.032212812,"about_ca_system_score_codex":0.00039439194,"about_ca_system_score_gemma":0.00023245155,"threshold_uncertainty_score":0.064050674},"labels":[],"label_agreement":null},{"id":"W2072774152","doi":"10.1029/2009gl038777","title":"Arctic air temperature change amplification and the Atlantic Multidecadal Oscillation","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":312,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Climatology; Arctic geoengineering; Arctic dipole anomaly; Arctic; Atlantic multidecadal oscillation; Arctic sea ice decline; Thermohaline circulation; Environmental science; Global warming; Arctic ice pack; North Atlantic oscillation; The arctic; Climate change; Oceanography; Permafrost; Geology; Drift ice","score_opus":0.02897905628177375,"score_gpt":0.27356981907734906,"score_spread":0.24459076279557532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2072774152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950907,0.0010104149,0.0004599394,0.00025476184,0.000018532526,0.0000026625912,0.00020203239,0.000021061636,0.0029399972],"genre_scores_gemma":[0.9992588,0.0002792869,0.00014904964,0.000020885082,0.00002521279,0.00000216386,0.00007283362,0.0000037617765,0.00018786285],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987817,0.000029570263,0.000010893294,0.00003320137,0.000026050859,0.000022125698],"domain_scores_gemma":[0.99876785,0.00037423562,0.0005942626,0.00006722132,0.00012052391,0.00007602297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043366646,0.000109930115,0.00011263218,0.00055199437,0.00018014167,0.00055369304,0.000087401844,0.00014080318,0.001478873],"category_scores_gemma":[0.0020149997,0.00011632982,0.00016864824,0.00051352655,0.00025790263,0.0004789928,0.0005057799,0.00026555697,0.0001374238],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021410141,0.000032431035,0.96256757,0.00003373227,0.00012443094,0.00011307525,0.00033343112,0.0015674441,0.0050299685,0.0012429183,0.00049992325,0.028240873],"study_design_scores_gemma":[0.0000024150172,0.000013627649,0.9975382,0.0000056263607,0.000017656086,0.000044521705,0.000059224607,0.0011064783,0.00013465228,0.00044240835,0.00063217786,0.0000029881492],"about_ca_topic_score_codex":0.0049528787,"about_ca_topic_score_gemma":0.007970798,"teacher_disagreement_score":0.0049528787,"about_ca_system_score_codex":0.0002862173,"about_ca_system_score_gemma":0.00021905845,"threshold_uncertainty_score":0.009848118},"labels":[],"label_agreement":null},{"id":"W2073090076","doi":"10.1029/2002gl014828","title":"Analysis of lidar measurements of ice clouds at multiple incidence angles","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Lidar; Depolarization ratio; Ice crystals; Polarization (electrochemistry); Optics; Remote sensing; Oscillation (cell signaling); Materials science; Geology; Physics","score_opus":0.06088820667780453,"score_gpt":0.2981005228705559,"score_spread":0.23721231619275135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073090076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99820864,0.00006349321,0.0011459534,0.000008309344,0.0000024286126,0.0000043149157,0.00014482754,0.000019792471,0.00040236683],"genre_scores_gemma":[0.9986946,0.000036594967,0.0008770104,0.000004552291,0.000003684495,0.000003848869,0.00029007412,0.000003744745,0.000085921485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984026,0.00001220665,0.000005457965,0.00003134839,0.00007148145,0.000039121525],"domain_scores_gemma":[0.9997261,0.00007715152,0.00005157822,0.000018306595,0.000092548275,0.000034230292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023848123,0.00022292443,0.00025855185,0.00080860703,0.00021464814,0.0003256292,0.00027217277,0.00024131422,0.00033071786],"category_scores_gemma":[0.0006570757,0.00018919012,0.00015913449,0.0005296385,0.000113336144,0.00023839051,0.00026323055,0.00019829762,0.00011468934],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065750023,0.0001728871,0.5130967,0.00014641302,0.0001586742,0.0012101599,0.0006277954,0.01628449,0.42002168,0.00034911605,0.00033191394,0.046942733],"study_design_scores_gemma":[0.00004042159,0.00020671128,0.8598794,0.000030687726,0.000069228976,0.0009793264,0.00033128794,0.06446885,0.072335504,0.0001313288,0.0014881565,0.00003911046],"about_ca_topic_score_codex":0.0051743025,"about_ca_topic_score_gemma":0.010427368,"teacher_disagreement_score":0.0051743025,"about_ca_system_score_codex":0.00033509638,"about_ca_system_score_gemma":0.000223186,"threshold_uncertainty_score":0.010288358},"labels":[],"label_agreement":null},{"id":"W2073104006","doi":"10.1029/2005gl022391","title":"Approximate estimates of fracture speeds for dry slab avalanches","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Slab; Geophone; Snow; Geology; Fracture (geology); Shear (geology); Geotechnical engineering; Fracture mechanics; Seismology; Geophysics; Materials science; Geomorphology; Composite material; Petrology","score_opus":0.020676545527555493,"score_gpt":0.30169825132217254,"score_spread":0.28102170579461705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073104006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6727725,0.0010730913,0.3176629,0.00007988966,0.000027983795,0.000054594955,0.0008988354,0.00040653115,0.007023656],"genre_scores_gemma":[0.95030046,0.000348607,0.047901902,0.000008084741,0.000016336955,0.000030462303,0.00063735404,0.000038877177,0.00071788445],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981445,0.000026432326,0.000009137182,0.000055703367,0.00006885839,0.000025364361],"domain_scores_gemma":[0.99892336,0.0005136749,0.00017182883,0.0001305295,0.00020875174,0.00005182632],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066228706,0.000332945,0.00020833533,0.0020373557,0.0002134709,0.0006366585,0.00062091777,0.00032768675,0.0018815581],"category_scores_gemma":[0.005963183,0.00033114347,0.000217671,0.00057029777,0.0002840959,0.00085011194,0.00056650623,0.000413592,0.0004919228],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082202314,0.00010074092,0.18615869,0.00040209497,0.00020778066,0.00036236068,0.00090069213,0.4792431,0.054839905,0.055799443,0.0022522996,0.21891092],"study_design_scores_gemma":[0.000037830727,0.0001384247,0.093975805,0.00008792812,0.000039887575,0.0006799268,0.00025497572,0.86064297,0.015238791,0.023615438,0.0052045286,0.000083556806],"about_ca_topic_score_codex":0.0021171807,"about_ca_topic_score_gemma":0.0026207543,"teacher_disagreement_score":0.0021171807,"about_ca_system_score_codex":0.0005560229,"about_ca_system_score_gemma":0.00021610472,"threshold_uncertainty_score":0.006294489},"labels":[],"label_agreement":null},{"id":"W2073218181","doi":"10.1029/2008gl035464","title":"A mid‐Holocene transition in the nitrogen dynamics of the western equatorial Pacific: Evidence of a deepening thermocline?","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; Dalhousie University","funders":"Canadian Institute for Advanced Research","keywords":"Holocene; Thermocline; Geology; Oceanography; Nitrate; Sedimentary rock; Advection; Geochemistry; Ecology","score_opus":0.06236802858542637,"score_gpt":0.30620992888211435,"score_spread":0.24384190029668798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073218181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978015,0.0004924229,0.00006335791,0.00023928977,0.0000114448185,0.0000030210372,0.0001018485,0.0000068952954,0.0012801897],"genre_scores_gemma":[0.99915886,0.00028123296,0.00008029682,0.00011527697,0.000015677851,0.0000028540437,0.00010905049,0.0000018788027,0.00023479346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000039226334,0.0000041288554,0.000017979508,0.0000054515244,0.000015779173],"domain_scores_gemma":[0.9998159,0.000015989697,0.00006238633,0.000014394811,0.000035606445,0.000055743836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017617525,0.00010471419,0.00013268745,0.00038105642,0.000384082,0.00069705484,0.00019098226,0.00046086765,0.0014046932],"category_scores_gemma":[0.000465611,0.00021184214,0.00012448755,0.00035576455,0.0005926088,0.0005540462,0.00046199717,0.00034324566,0.00014237237],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045340386,0.00007553653,0.93519163,0.00010716002,0.00007639655,0.00065912865,0.00194597,0.00016047352,0.03709521,0.0007602313,0.0005837006,0.022891194],"study_design_scores_gemma":[0.0000039890206,0.000015815489,0.9988029,0.0000044813073,0.000005542528,0.000052306452,0.00024871968,0.00004451557,0.00016868408,0.00005100772,0.0005999069,0.0000021965957],"about_ca_topic_score_codex":0.012698605,"about_ca_topic_score_gemma":0.028598346,"teacher_disagreement_score":0.012698605,"about_ca_system_score_codex":0.0004892885,"about_ca_system_score_gemma":0.0004130449,"threshold_uncertainty_score":0.025249362},"labels":[],"label_agreement":null},{"id":"W2073563925","doi":"10.1029/2001gl014192","title":"Highly deformed basal ice in the Vostok core, Antarctica","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Belgian Federal Science Policy Office; Polar Knowledge Canada; Division of Polar Programs; National Science Foundation","keywords":"Geology; Ice core; Ice sheet; Ice stream; Basal (medicine); Ice divide; Pancake ice; Geomorphology; Cryosphere; Climatology; Sea ice","score_opus":0.08703283958889249,"score_gpt":0.293635182646559,"score_spread":0.20660234305766653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073563925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991322,0.00013957576,0.000015080767,0.000009682437,0.000003829469,0.000002705424,0.0002713649,0.0000033179144,0.00042223503],"genre_scores_gemma":[0.9991203,0.00014700729,0.00006254863,0.000011993072,0.000003230435,0.0000025652416,0.00046636714,0.000005071391,0.0001809625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999298,0.000005961211,0.0000056543586,0.000016034568,0.000017725764,0.00002489392],"domain_scores_gemma":[0.9999231,0.0000062815334,0.000021361562,0.000011909757,0.00001752958,0.00001977414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011956905,0.00018327167,0.00024482008,0.0009270819,0.00086238916,0.000727611,0.00017765432,0.0002683807,0.00036121588],"category_scores_gemma":[0.00019925645,0.00020145524,0.00018322676,0.0008527092,0.000653986,0.0002269715,0.00054737204,0.00015649394,0.00017399515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091223564,0.000052636453,0.85645187,0.00020828584,0.0002037887,0.0024352663,0.0030090415,0.0029114373,0.11724522,0.00033827254,0.00072096265,0.015510911],"study_design_scores_gemma":[0.000007729439,0.00001900634,0.9973763,0.000008756347,0.000012277433,0.00021817858,0.0004341164,0.00019431577,0.00097603013,0.000020601774,0.0007281905,0.0000044764947],"about_ca_topic_score_codex":0.04858159,"about_ca_topic_score_gemma":0.097822934,"teacher_disagreement_score":0.04858159,"about_ca_system_score_codex":0.00080832123,"about_ca_system_score_gemma":0.00058960007,"threshold_uncertainty_score":0.09659767},"labels":[],"label_agreement":null},{"id":"W2073700961","doi":"10.1029/2004gl021454","title":"Influence of lithospheric thickness variations on 3‐D crustal velocities due to glacial isostatic adjustment","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley; National Aeronautics and Space Administration","keywords":"Lithosphere; Geology; Post-glacial rebound; Geodetic datum; Discontinuity (linguistics); Ridge; Geodesy; Plate tectonics; Tectonics; Seismology; Glacial period; Geophysics; Geomorphology; Paleontology","score_opus":0.025752782456059716,"score_gpt":0.28633295965481625,"score_spread":0.26058017719875654,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073700961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980628,0.000053774726,0.0008011032,0.0000545376,0.000006734703,0.0000026554303,0.000120196135,0.000040443996,0.0008577301],"genre_scores_gemma":[0.9997552,0.000023062425,0.00009816296,0.000005867917,0.000001429778,0.0000011239754,0.000056825524,0.00000875163,0.000049610735],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998553,0.000053130778,0.000013478915,0.00002591749,0.000020653966,0.00003157642],"domain_scores_gemma":[0.99911517,0.00048783774,0.0001394748,0.00011673598,0.00006599648,0.000074853095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057064876,0.00037164876,0.00019213368,0.00041633056,0.00026275913,0.0009499766,0.00028950957,0.00032704975,0.00088718557],"category_scores_gemma":[0.0038172891,0.0003678742,0.0005623681,0.000357834,0.0006023691,0.00032680848,0.00061648985,0.00032054447,0.00013649501],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007482893,0.000054652395,0.25900865,0.00006605478,0.0002711538,0.000530113,0.00024396245,0.6805041,0.04128178,0.0017310174,0.00034464657,0.015215521],"study_design_scores_gemma":[0.00009233179,0.00016287346,0.48942164,0.000015338172,0.000111987305,0.0001637125,0.00013057055,0.49557963,0.012482491,0.0011613668,0.0006209609,0.000057169218],"about_ca_topic_score_codex":0.0121750785,"about_ca_topic_score_gemma":0.005528976,"teacher_disagreement_score":0.0121750785,"about_ca_system_score_codex":0.00070296886,"about_ca_system_score_gemma":0.00031225182,"threshold_uncertainty_score":0.024208426},"labels":[],"label_agreement":null},{"id":"W2073881801","doi":"10.1002/2014gl061273","title":"Neutral density variation from specular meteor echo observations spanning one solar cycle","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"National Aeronautics and Space Administration","keywords":"Meteor (satellite); Thermosphere; Atmospheric sciences; Solar cycle; Altitude (triangle); Physics; Environmental science; Meteorology; Ionosphere; Astronomy; Solar wind; Plasma","score_opus":0.02724084880775958,"score_gpt":0.26925322342486974,"score_spread":0.24201237461711017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2073881801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982703,0.000047911362,0.00034721429,0.0000060870016,0.0000023821858,0.00000260029,0.00081316405,0.000011845986,0.0004985125],"genre_scores_gemma":[0.99851865,0.000032794767,0.00019219176,0.0000028507468,0.0000024697756,0.0000020513469,0.0011494209,0.0000029814375,0.000096503965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999305,0.00001026871,0.000004536061,0.000021494612,0.000023522129,0.000009722535],"domain_scores_gemma":[0.9997577,0.00005691179,0.0000720347,0.000020067666,0.00007120524,0.000022183793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020409295,0.00014568467,0.00012917169,0.00052671874,0.00013569288,0.00028605305,0.00016324088,0.00013652405,0.0004433949],"category_scores_gemma":[0.00069012144,0.000080837715,0.00014754807,0.00042875088,0.000092327056,0.00016083142,0.00017954578,0.00010717242,0.00011991833],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014525112,0.000016947752,0.96795404,0.000027793185,0.00008512244,0.00007077327,0.00010139755,0.00448208,0.015030616,0.00007195898,0.00029753923,0.011716421],"study_design_scores_gemma":[0.00000194685,0.00002197106,0.9949582,0.0000023681177,0.00001253926,0.00004235901,0.000024326055,0.0037331213,0.00097298145,0.000015440537,0.00021131951,0.0000034729103],"about_ca_topic_score_codex":0.01792122,"about_ca_topic_score_gemma":0.02204064,"teacher_disagreement_score":0.01792122,"about_ca_system_score_codex":0.00026233785,"about_ca_system_score_gemma":0.00011006963,"threshold_uncertainty_score":0.035633802},"labels":[],"label_agreement":null},{"id":"W2074086068","doi":"10.1029/2003gl019190","title":"Numerical investigation of induced cracking and seismic velocity changes in brittle rock","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Brittleness; Geology; Hydrostatic equilibrium; Perpendicular; Cracking; Geotechnical engineering; Stress (linguistics); Seismic velocity; Mechanics; Materials science; Seismology; Composite material; Geometry; Physics","score_opus":0.04390629514457974,"score_gpt":0.28490490181192984,"score_spread":0.2409986066673501,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074086068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9488403,0.0001477011,0.04644768,0.00012895698,0.000025730322,0.000048631555,0.0001093511,0.00019084945,0.0040608956],"genre_scores_gemma":[0.9833635,0.000051327028,0.015813744,0.000007668816,0.0000039562137,0.000040216528,0.000047959405,0.000016115364,0.0006553996],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999088,0.000021175525,0.000005413549,0.000014948,0.00003455694,0.000015078577],"domain_scores_gemma":[0.999329,0.00037925865,0.000114206945,0.000066711305,0.00006746106,0.000043419604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002798332,0.00020875488,0.0002629852,0.00031526762,0.000257217,0.00030327713,0.0004858227,0.0005779287,0.0011600223],"category_scores_gemma":[0.0014382141,0.00020732648,0.00021538127,0.00023937262,0.0006904273,0.00030081588,0.00029536657,0.0003165205,0.000080314465],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009950162,0.00010069238,0.004757762,0.00007975905,0.000024826491,0.0001923762,0.000117362615,0.9409654,0.042610515,0.004538068,0.0001631082,0.006350595],"study_design_scores_gemma":[0.000007911406,0.000031881384,0.0005297753,0.0000019730023,0.0000018617284,0.00001475088,0.000009115295,0.99721897,0.0018495735,0.00022459688,0.000106161984,0.000003411205],"about_ca_topic_score_codex":0.0020099394,"about_ca_topic_score_gemma":0.0017318907,"teacher_disagreement_score":0.0020099394,"about_ca_system_score_codex":0.00040477273,"about_ca_system_score_gemma":0.00034901145,"threshold_uncertainty_score":0.003996432},"labels":[],"label_agreement":null},{"id":"W2074144717","doi":"10.1029/2000gl012491","title":"Recent change in organic carbon flux to Arctic Ocean deep basins: Evidence from acid volatile sulfide, manganese and rhenium discord in sediments","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Université du Québec à Rimouski; Institut du Savoir Montfort","funders":"Dartmouth College","keywords":"Anoxic waters; Diagenesis; Sediment; Sulfide; Total organic carbon; Geology; Arctic; Oceanography; Manganese; Geochemistry; Flux (metallurgy); Climate change; Earth science; Environmental science; Environmental chemistry; Geomorphology; Chemistry","score_opus":0.0395317080775955,"score_gpt":0.2969629417303927,"score_spread":0.25743123365279724,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074144717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992662,0.0002722399,0.00004121402,0.000042188607,0.0000037805346,8.1000155e-7,0.000118708784,0.0000031976172,0.00025159953],"genre_scores_gemma":[0.9990658,0.00036521777,0.000074565185,0.000027879907,0.000010349425,0.0000010420222,0.00027169724,0.0000014132078,0.00018210334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999492,0.000004497211,0.0000050271797,0.000014848776,0.000012011368,0.000014329175],"domain_scores_gemma":[0.99967754,0.000031080544,0.000100212375,0.000013638419,0.00010453634,0.00007305402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020008424,0.00015519044,0.00014335402,0.00068772066,0.00033276668,0.00046315845,0.0001486317,0.0003125389,0.0003939917],"category_scores_gemma":[0.0003802173,0.00018581339,0.00013770597,0.0005482239,0.0003727674,0.00024923086,0.0002444735,0.0001862389,0.00009762069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039909736,0.000041378647,0.8951157,0.00007608202,0.00012796979,0.00029496205,0.00046803558,0.00023665476,0.09537467,0.000116934716,0.00013851185,0.0076100742],"study_design_scores_gemma":[0.000003354932,0.000026969119,0.9974833,0.0000027997442,0.000018256345,0.00007790478,0.000091982234,0.00009532421,0.0018798846,0.000023986213,0.00029396694,0.0000022410156],"about_ca_topic_score_codex":0.016164403,"about_ca_topic_score_gemma":0.021263437,"teacher_disagreement_score":0.016164403,"about_ca_system_score_codex":0.00033151274,"about_ca_system_score_gemma":0.00023628895,"threshold_uncertainty_score":0.032140613},"labels":[],"label_agreement":null},{"id":"W2074255403","doi":"10.1029/2008gl034980","title":"Reply to comment by Igor Esau on “Do stable atmospheric layers exist?”","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Argument (complex analysis); Philosophy; Epistemology; Theoretical physics; Physics; Chemistry","score_opus":0.015385490318485445,"score_gpt":0.29336819227329275,"score_spread":0.2779827019548073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074255403","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00017208759,0.0014967571,0.00014253713,0.9802874,0.01715968,0.000003195371,0.000111870555,0.000029792642,0.0005967144],"genre_scores_gemma":[0.0031178512,0.0010596677,0.00016278191,0.9684383,0.024870157,0.000018096214,0.000058284968,0.00005359001,0.0022212453],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99741733,0.00073540374,0.0003004259,0.00058875006,0.0007187693,0.00023932224],"domain_scores_gemma":[0.98731846,0.0072566625,0.0010008718,0.00046394404,0.0032119034,0.0007481635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0053706323,0.0010517326,0.0014417912,0.0008644357,0.0029962955,0.0027192119,0.0036081239,0.02521246,0.008534303],"category_scores_gemma":[0.030528093,0.0008569375,0.0010820383,0.0011422259,0.0049638627,0.0069988994,0.002960824,0.036790412,0.008407331],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019261626,0.000003424996,0.00013391273,0.000034939752,0.000006993671,0.00009962688,0.00019047,0.000024784364,0.00005795295,0.0015807417,0.9966197,0.0012282109],"study_design_scores_gemma":[0.00004135386,0.00001994143,0.0017244364,0.00027491176,0.000024773975,0.00065525074,0.0010904943,0.00019811858,0.00044605555,0.008987694,0.98645407,0.00008288004],"about_ca_topic_score_codex":0.008603256,"about_ca_topic_score_gemma":0.007805512,"teacher_disagreement_score":0.02521246,"about_ca_system_score_codex":0.0028725034,"about_ca_system_score_gemma":0.0023850389,"threshold_uncertainty_score":0.028550148},"labels":[],"label_agreement":null},{"id":"W2074352581","doi":"10.1029/2002gl015080","title":"Photochemical production of nitrous acid on glass sample manifold surface","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Nitrous acid; Adsorption; Nitric acid; Photodissociation; Nitrate; Analytical Chemistry (journal); Materials science; Inlet; Fraction (chemistry); Photochemistry; Chemistry; Environmental chemistry; Inorganic chemistry; Geology; Chromatography; Organic chemistry","score_opus":0.0417786107383764,"score_gpt":0.2650957230731354,"score_spread":0.22331711233475898,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074352581","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986091,0.00007217997,0.00052983523,0.000007701253,0.000006294169,0.000009680653,0.0001310334,0.000020935173,0.0006132569],"genre_scores_gemma":[0.9976011,0.00006997571,0.00095895806,0.000011116901,0.0000037637037,0.000012939465,0.00029933776,0.000008518975,0.0010343195],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998666,0.000013290168,0.0000037578882,0.000041649757,0.00004850972,0.000026102234],"domain_scores_gemma":[0.9999145,0.000020680221,0.00001894693,0.000011420398,0.000020765081,0.00001367861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001090867,0.00028090805,0.00019730444,0.00021174682,0.00044675637,0.00021458961,0.0001795629,0.00025202593,0.0018042893],"category_scores_gemma":[0.00016950561,0.00016444633,0.00023133014,0.00016745432,0.00024715016,0.00013934425,0.0002390597,0.00024571433,0.00026417663],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013363229,0.000009037811,0.004141019,0.000018171315,0.000006814587,0.000048770984,0.000080506434,0.00005848378,0.9941789,0.00001633508,0.000038550974,0.0012698537],"study_design_scores_gemma":[0.0000052659516,0.0004075644,0.056303393,0.0000025858385,0.000012776138,0.00008381645,0.0001306111,0.0006768597,0.94176924,0.000026391956,0.00057558867,0.000005896001],"about_ca_topic_score_codex":0.0028569605,"about_ca_topic_score_gemma":0.005107334,"teacher_disagreement_score":0.0028569605,"about_ca_system_score_codex":0.00029506287,"about_ca_system_score_gemma":0.00015115978,"threshold_uncertainty_score":0.0060359836},"labels":[],"label_agreement":null},{"id":"W2074355503","doi":"10.1029/2003gl017124","title":"Vertical winds in the central polar cap","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Polar; Atmospheric sciences; Zonal flow (plasma); Polar cap; Flow (mathematics); Latitude; Divergence (linguistics); Geology; Prevailing winds; Horizontal and vertical; Climatology; Physics; Meteorology; Geodesy; Mechanics; Plasma","score_opus":0.015962660646965023,"score_gpt":0.2825934387698238,"score_spread":0.2666307781228588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074355503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844641,0.0011179586,0.000111967915,0.00011072036,0.000039706658,0.000006909214,0.0008464943,0.00002150438,0.013280577],"genre_scores_gemma":[0.99799794,0.0003333296,0.00006165831,0.000021037125,0.000020282014,0.0000027172173,0.00052635965,0.0000036060778,0.001033038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992704,0.000011282322,0.000003680334,0.000015158817,0.00001564174,0.000027176642],"domain_scores_gemma":[0.9997534,0.000017194201,0.00006315974,0.000011181611,0.000098181605,0.000056785553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001324762,0.00013849964,0.00014151415,0.00062817126,0.00040305004,0.0009147418,0.00008256855,0.0002096423,0.0018503483],"category_scores_gemma":[0.00041514065,0.000118446165,0.00009965939,0.000845975,0.0001696576,0.00022581236,0.00029098,0.0001591647,0.00042967394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061145925,0.000060620197,0.93392646,0.000112600275,0.000091384194,0.0009702327,0.001597362,0.0018428399,0.015890818,0.0009954477,0.006439757,0.037460916],"study_design_scores_gemma":[0.000006453952,0.000022065391,0.9957996,0.000019788988,0.00000836061,0.00008971426,0.00032183356,0.00030972605,0.00018022589,0.000059805112,0.0031781937,0.0000042567435],"about_ca_topic_score_codex":0.04208893,"about_ca_topic_score_gemma":0.03724747,"teacher_disagreement_score":0.04208893,"about_ca_system_score_codex":0.00043798983,"about_ca_system_score_gemma":0.000250461,"threshold_uncertainty_score":0.0836879},"labels":[],"label_agreement":null},{"id":"W2074376208","doi":"10.1002/2014gl061331","title":"Investigating high‐latitude ionospheric turbulence using global positioning system data","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"GNSS positioning and interference","field":"Engineering","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Kurtosis; Skewness; Amplitude; Ionosphere; Turbulence; Wavelet; Probability density function; Physics; Global Positioning System; Geodesy; Phase (matter); Geophysics; Computational physics; Geology; Statistical physics; Meteorology; Statistics; Mathematics; Optics; Computer science; Telecommunications","score_opus":0.0564223746257586,"score_gpt":0.3135717723800066,"score_spread":0.257149397754248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074376208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983714,0.000032568412,0.0010302216,0.000027291244,0.0000033518434,0.0000035875182,0.00021526619,0.000014385618,0.00030199133],"genre_scores_gemma":[0.99899405,0.000031343494,0.0005293492,0.000004592309,0.0000037969692,0.000001972671,0.00036875284,0.0000020804246,0.00006402707],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998423,0.00004055074,0.000009248928,0.000027448525,0.000048696544,0.000031652984],"domain_scores_gemma":[0.99961346,0.00016499958,0.00007715394,0.00003330419,0.0000806397,0.000030544277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000437535,0.00021693629,0.0001539559,0.00090920756,0.00019887494,0.0003934002,0.00013114042,0.00020767665,0.0003180541],"category_scores_gemma":[0.0009569101,0.00010999356,0.00014918446,0.0012916299,0.00014247696,0.0003037433,0.00016168851,0.00015270092,0.000096850075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003910594,0.000097179,0.88566166,0.000060078546,0.00015241075,0.00053897506,0.00036289598,0.033567924,0.045222096,0.0007417413,0.0005764786,0.032627515],"study_design_scores_gemma":[0.000012249933,0.000092498005,0.9632886,0.000006812083,0.000024836072,0.000061252125,0.00020101944,0.033213213,0.0025797281,0.00010282491,0.00040380086,0.000013126451],"about_ca_topic_score_codex":0.015161163,"about_ca_topic_score_gemma":0.021954883,"teacher_disagreement_score":0.015161163,"about_ca_system_score_codex":0.00028376133,"about_ca_system_score_gemma":0.00026840018,"threshold_uncertainty_score":0.030145824},"labels":[],"label_agreement":null},{"id":"W2074838276","doi":"10.1029/2005gl022995","title":"Quantifying CO emissions from the 2004 Alaskan wildfires using MOPITT CO data","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":188,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Troposphere; Atmospheric sciences; Ozone; Data assimilation; Pollution; Air pollution; Carbon monoxide; Meteorology; Climatology; Chemical transport model; Geography; Geology; Chemistry","score_opus":0.16454733987726458,"score_gpt":0.37476792504955575,"score_spread":0.21022058517229117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074838276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955249,0.000049905255,0.0031026788,0.000042599975,0.0000048246393,0.000008296936,0.0003542488,0.00009211911,0.00082044915],"genre_scores_gemma":[0.9925687,0.00004434107,0.006299839,0.000008284314,0.000004697703,0.000009730953,0.0008289227,0.00001631886,0.0002191937],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99986005,0.000025007583,0.0000062102217,0.00003618732,0.00005108265,0.000021358073],"domain_scores_gemma":[0.9998323,0.00003660742,0.000027718326,0.00002188885,0.000065388616,0.000016017448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033671275,0.00053610647,0.00022208811,0.0004474214,0.00047682438,0.00040640915,0.00027805535,0.00033380283,0.0002219979],"category_scores_gemma":[0.000664866,0.00022532717,0.00047506616,0.00037535717,0.00021413344,0.00040093373,0.0002949231,0.00036028388,0.000056261906],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032188394,0.00022855266,0.21080452,0.000051398878,0.0003117522,0.0002646685,0.00017477259,0.7348325,0.025577713,0.0009139919,0.0005774747,0.025940731],"study_design_scores_gemma":[0.000028472485,0.00008340387,0.11446285,0.000008945007,0.00009568468,0.00008472133,0.000088403016,0.8650924,0.018585358,0.0004501132,0.0009782015,0.000041452553],"about_ca_topic_score_codex":0.12255925,"about_ca_topic_score_gemma":0.14131814,"teacher_disagreement_score":0.12255925,"about_ca_system_score_codex":0.0009632789,"about_ca_system_score_gemma":0.00078794826,"threshold_uncertainty_score":0.24369174},"labels":[],"label_agreement":null},{"id":"W2074893592","doi":"10.1029/2009gl037946","title":"Can cosmic rays affect cloud condensation nuclei by altering new particle formation rates?","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":161,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Cosmic ray; Cloud condensation nuclei; Aerosol; Cloud cover; Atmospheric sciences; Physics; Flux (metallurgy); Particle (ecology); Astrophysics; Environmental science; Cloud computing; Meteorology; Geology; Chemistry","score_opus":0.025246074704050783,"score_gpt":0.2972073887875738,"score_spread":0.27196131408352303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2074893592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870907,0.0018569351,0.00353144,0.0016325787,0.00013249405,0.00003598755,0.00033404547,0.000111463974,0.0052742944],"genre_scores_gemma":[0.9986451,0.00054116745,0.0003212972,0.000111534035,0.000019618088,0.0000037353004,0.000036787318,0.000010088216,0.00031057466],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998394,0.000056647204,0.000007237287,0.000027453865,0.000019695137,0.00004946477],"domain_scores_gemma":[0.999495,0.0002873938,0.00008670852,0.000045333745,0.000037421192,0.000048073143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003781812,0.0004760639,0.0004145482,0.00027664463,0.00025665286,0.0007766226,0.0005101237,0.0009444337,0.002297268],"category_scores_gemma":[0.0028069254,0.00026594664,0.00072059664,0.00026295485,0.0004188516,0.0011528098,0.00026881683,0.0002961863,0.00021434546],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006804652,0.0005398742,0.69581664,0.00053119636,0.0011760081,0.0009491652,0.0003059281,0.17158775,0.071620785,0.02306328,0.0021193011,0.031609632],"study_design_scores_gemma":[0.00043996592,0.00083608256,0.6390701,0.000067062865,0.00071697636,0.00046549187,0.0005369904,0.29591295,0.029126529,0.0261326,0.006589313,0.00010595915],"about_ca_topic_score_codex":0.013831729,"about_ca_topic_score_gemma":0.011990907,"teacher_disagreement_score":0.013831729,"about_ca_system_score_codex":0.00072304235,"about_ca_system_score_gemma":0.00036904126,"threshold_uncertainty_score":0.027502477},"labels":[],"label_agreement":null},{"id":"W2075195458","doi":"10.1029/2006gl026702","title":"Deep Labrador Current and its variability in 1996–2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Current (fluid); Boundary current; Mooring; Deep water; Oceanography; Climatology; Geology; Period (music); Water mass; Term (time); Environmental science; Ocean current","score_opus":0.027927821531185743,"score_gpt":0.29878134217169194,"score_spread":0.2708535206405062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075195458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996497,0.00030403104,0.00008322263,0.00005382263,0.000007400848,0.000002639415,0.0018268828,0.000015746762,0.0012094367],"genre_scores_gemma":[0.995093,0.00012681112,0.00013773674,0.000022872426,0.000010558703,0.000004331246,0.003738651,0.000003659595,0.0008623924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998877,0.000007755392,0.000015857948,0.000036515656,0.000024990632,0.000027141463],"domain_scores_gemma":[0.9995154,0.000025958292,0.00025728234,0.000036303965,0.0001214462,0.000043645436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028556012,0.00015882889,0.00019172448,0.00083348085,0.00019422073,0.0006148925,0.00023147489,0.00023376553,0.0007428883],"category_scores_gemma":[0.00077404844,0.00008359459,0.00014661095,0.0010435157,0.00014893872,0.00044105024,0.00033004352,0.00018822389,0.00033262014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023416494,0.00004585179,0.9693709,0.000037158337,0.00010342207,0.000099704106,0.000375692,0.00081224815,0.0017758032,0.00017173307,0.0012506299,0.025722632],"study_design_scores_gemma":[0.0000024311475,0.000013005657,0.9976851,0.0000059726513,0.000009285766,0.00003716429,0.00006660048,0.00022649013,0.00022032086,0.000012083108,0.0017188782,0.00000268582],"about_ca_topic_score_codex":0.050770763,"about_ca_topic_score_gemma":0.07741744,"teacher_disagreement_score":0.050770763,"about_ca_system_score_codex":0.0012442481,"about_ca_system_score_gemma":0.00026285584,"threshold_uncertainty_score":0.10095048},"labels":[],"label_agreement":null},{"id":"W2075579764","doi":"10.1029/2004gl021831","title":"Theory of dispersive shear Alfvén wave focusing in Earth's magnetosphere","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Physics; Gyroradius; Alfvén wave; Magnetosphere; Amplitude; Field line; Earth's magnetic field; Computational physics; Geophysics; Shear (geology); Wavenumber; Ionosphere; Dispersion (optics); Earth radius; Magnetohydrodynamics; Magnetic field; Optics; Geology","score_opus":0.018038786215664144,"score_gpt":0.27319543396786894,"score_spread":0.2551566477522048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075579764","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0845237,0.01098262,0.68401295,0.004671806,0.00072820875,0.00009676089,0.0004223755,0.0005541315,0.21400756],"genre_scores_gemma":[0.9074578,0.0058084573,0.037083495,0.00089358643,0.00090699695,0.00024372876,0.00016728962,0.00011372369,0.04732492],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99993753,0.000011903921,0.000002083605,0.0000086893915,0.000025573932,0.000014218393],"domain_scores_gemma":[0.99989927,0.00003124318,0.000018999803,0.0000099035715,0.00002588701,0.000014698916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027627955,0.00046424023,0.00038953443,0.0005877166,0.00052706705,0.00070958247,0.0008934678,0.0008340799,0.0031965598],"category_scores_gemma":[0.0004748681,0.0001899578,0.0003204351,0.00043622876,0.001115085,0.0011541118,0.0005874397,0.00047923395,0.00074537523],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000011009216,0.000009215077,0.0002671609,0.000049925817,0.000011261535,0.0001279707,0.00014366813,0.052538667,0.0014119609,0.9358005,0.0032820997,0.006346578],"study_design_scores_gemma":[0.00001469241,0.000033240653,0.0008758133,0.000020576894,0.000006872771,0.00020631927,0.00005973881,0.25321496,0.00024661457,0.7373468,0.007955219,0.000019142351],"about_ca_topic_score_codex":0.0017312552,"about_ca_topic_score_gemma":0.00092197943,"teacher_disagreement_score":0.0031965598,"about_ca_system_score_codex":0.0008314077,"about_ca_system_score_gemma":0.0004302397,"threshold_uncertainty_score":0.01069361},"labels":[],"label_agreement":null},{"id":"W2075735424","doi":"10.1029/2000gl011403","title":"On the decrease of Arctic sea ice volume","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Hindcast; Arctic ice pack; Climatology; Arctic; Arctic sea ice decline; Archipelago; Bay; Geology; Oceanography; Environmental science; Antarctic sea ice","score_opus":0.020484381563501748,"score_gpt":0.2558885120567111,"score_spread":0.23540413049320935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075735424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967127,0.00006624231,0.0006876929,0.000094931354,0.000006834053,0.000002370525,0.00023287113,0.00002397518,0.0021723746],"genre_scores_gemma":[0.99926513,0.00006818848,0.0001806435,0.000015001351,0.000003144421,0.0000024696146,0.00017749367,0.000007892328,0.00028019655],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999311,0.000018633331,0.0000029822259,0.000017447563,0.0000111955715,0.000018675673],"domain_scores_gemma":[0.9997154,0.000143861,0.00005911875,0.000016889706,0.000042177835,0.000022518758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019164517,0.00023677429,0.00016194169,0.00017980704,0.00016728259,0.00048471737,0.000267299,0.00033598518,0.0015094401],"category_scores_gemma":[0.001360231,0.00015114654,0.00024020161,0.00022412108,0.00027177422,0.00031239475,0.00026688265,0.0002227366,0.00019567247],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035703593,0.000085004845,0.100038335,0.000052251682,0.000088157685,0.00025374832,0.00008076676,0.8790065,0.007110398,0.002330508,0.0009117111,0.009685442],"study_design_scores_gemma":[0.00006046554,0.00020184705,0.11853596,0.000021721826,0.00005713385,0.0000808065,0.00011610075,0.8744636,0.0033974247,0.0011408438,0.0019027687,0.000021308026],"about_ca_topic_score_codex":0.017279573,"about_ca_topic_score_gemma":0.012820319,"teacher_disagreement_score":0.017279573,"about_ca_system_score_codex":0.00051618397,"about_ca_system_score_gemma":0.00036637,"threshold_uncertainty_score":0.034357965},"labels":[],"label_agreement":null},{"id":"W2075810138","doi":"10.1029/2006gl026884","title":"Does atmospheric processing of saturated hydrocarbon surfaces by NO<sub>3</sub> lead to volatilization?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"X-ray photoelectron spectroscopy; Volatilisation; Monolayer; Hydrocarbon; Analytical Chemistry (journal); Substrate (aquarium); Chemistry; Mass spectrometry; Environmental chemistry; Organic chemistry; Chemical engineering; Chromatography; Geology","score_opus":0.010474050712997425,"score_gpt":0.24060357442080893,"score_spread":0.2301295237078115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2075810138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956772,0.0011388108,0.0013636977,0.00029443175,0.000031568085,0.000010507877,0.00007065634,0.000018827652,0.0013943709],"genre_scores_gemma":[0.9978859,0.0007807552,0.00039245546,0.00007060531,0.000013226766,0.000003035285,0.000057419726,0.0000052357223,0.0007914368],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99991405,0.000011788737,0.0000030187296,0.00001824375,0.00002336573,0.000029597986],"domain_scores_gemma":[0.99989355,0.000024679379,0.00003726322,0.00000882383,0.000026030448,0.000009689917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018898117,0.0001939439,0.00017743475,0.000079067664,0.00014917635,0.00025624354,0.00018730063,0.0005143829,0.00095529895],"category_scores_gemma":[0.00038625984,0.00014845663,0.00020539136,0.000079808895,0.00030624776,0.00042774927,0.000109757086,0.00014837427,0.0003072213],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029729982,0.00004265303,0.015134351,0.00014162937,0.000035893143,0.0003386977,0.000040562943,0.0003320423,0.9768594,0.00042284894,0.00013422199,0.006220411],"study_design_scores_gemma":[0.000018585019,0.00046332233,0.086656116,0.000014607595,0.00006384316,0.00080264546,0.0002805295,0.0039327866,0.9036931,0.0009431588,0.003118768,0.000012437284],"about_ca_topic_score_codex":0.0020489274,"about_ca_topic_score_gemma":0.0024302262,"teacher_disagreement_score":0.0020489274,"about_ca_system_score_codex":0.00025259846,"about_ca_system_score_gemma":0.00014272782,"threshold_uncertainty_score":0.0040739775},"labels":[],"label_agreement":null},{"id":"W2076084810","doi":"10.1029/2008gl034845","title":"Buoy observations from the windiest location in the world ocean, Cape Farewell, Greenland","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration; National Science Foundation","keywords":"Buoy; Wind speed; Climatology; Geology; Meteorology; Cape; Environmental science; Oceanography; Geography","score_opus":0.10224530836616785,"score_gpt":0.30649773974149735,"score_spread":0.2042524313753295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076084810","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99701846,0.0000706169,0.00009548181,0.000043715012,0.000009059416,0.000012183072,0.0012785515,0.000022025646,0.0014498633],"genre_scores_gemma":[0.9953147,0.00015323111,0.0009842011,0.00003674199,0.000009631727,0.00001513175,0.0021855934,0.0000069849266,0.0012938251],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999505,0.000002710063,0.0000028694733,0.000010835819,0.00001852741,0.000014591147],"domain_scores_gemma":[0.9998591,0.000010689315,0.00004673177,0.000008690781,0.000043210875,0.000031519976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010919088,0.00017074199,0.00015986359,0.0008069898,0.0004572087,0.00034054962,0.00018974004,0.0001393481,0.000780501],"category_scores_gemma":[0.0002721559,0.00008278148,0.00007114616,0.00067553605,0.00020795605,0.00019649003,0.00035200428,0.00012997157,0.00014224129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016892751,0.00010079429,0.89436024,0.0001315566,0.00008279702,0.0013256863,0.0019312708,0.0014765183,0.05676178,0.0002380125,0.0073897634,0.036032762],"study_design_scores_gemma":[0.000010195089,0.000017163924,0.99649316,0.000013095374,0.00000937383,0.00006600576,0.0002527814,0.00049188745,0.00078858784,0.000018041444,0.0018342457,0.0000054162233],"about_ca_topic_score_codex":0.35225773,"about_ca_topic_score_gemma":0.68562114,"teacher_disagreement_score":0.35225773,"about_ca_system_score_codex":0.00079914334,"about_ca_system_score_gemma":0.0007301769,"threshold_uncertainty_score":0.7004147},"labels":[],"label_agreement":null},{"id":"W2076091550","doi":"10.1029/2007gl030607","title":"Composition changes during disturbed conditions: Are mass spectrometers overestimating the concentrations of atomic oxygen?","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; University of Saskatchewan; Royal Military College of Canada","funders":"","keywords":"Oxygen; Mass spectrometry; Molecular oxygen; Chemistry; Atmosphere (unit); Spectrometer; Atomic oxygen; Aeronomy; Analytical Chemistry (journal); Atomic physics; Environmental chemistry; Chemical physics; Physics; Meteorology","score_opus":0.016174692584415746,"score_gpt":0.2949651592622116,"score_spread":0.2787904666777959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076091550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9871502,0.0011720031,0.008485401,0.00041781744,0.000054028354,0.000023808425,0.00045068868,0.00041534376,0.0018307423],"genre_scores_gemma":[0.9968053,0.0003181394,0.0022423954,0.0001401306,0.000023323564,0.000005795758,0.00022522446,0.000046055615,0.00019374536],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989079,0.00018127495,0.00009336737,0.0002645465,0.00039895935,0.0001540215],"domain_scores_gemma":[0.99645716,0.0008350077,0.0014318245,0.0003541014,0.0007929351,0.00012895602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014902622,0.0004898527,0.0006817673,0.0012488901,0.00047125277,0.0011372089,0.00070935366,0.0011191143,0.00062491803],"category_scores_gemma":[0.0068122786,0.0006153232,0.00030122083,0.0012339501,0.00055151427,0.0015719346,0.0005516996,0.00025515113,0.00069919886],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074834126,0.000045689438,0.9033148,0.0001501161,0.00018253113,0.0004170846,0.0003189941,0.003899631,0.061566573,0.00014520725,0.0005521434,0.028658886],"study_design_scores_gemma":[0.000049088485,0.00019718337,0.9017346,0.000042506126,0.00013962633,0.0011038429,0.0006909174,0.025499497,0.06609744,0.0007463705,0.0036505202,0.00004850178],"about_ca_topic_score_codex":0.011633619,"about_ca_topic_score_gemma":0.012465868,"teacher_disagreement_score":0.011633619,"about_ca_system_score_codex":0.00080227584,"about_ca_system_score_gemma":0.00021789152,"threshold_uncertainty_score":0.023131788},"labels":[],"label_agreement":null},{"id":"W2076225046","doi":"10.1029/2009gl040057","title":"Controls on Northern Hemisphere snow albedo feedback quantified using satellite Earth observations","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Snow; Albedo (alchemy); Northern Hemisphere; Environmental science; Climatology; Cloud cover; Satellite; Atmospheric sciences; Snow cover; Geology; Meteorology; Geography","score_opus":0.09866424089000546,"score_gpt":0.30684222012058615,"score_spread":0.20817797923058068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076225046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957202,0.00009117881,0.00090491434,0.000038400947,0.0000062083473,0.000009788978,0.0012064765,0.000082963605,0.001939848],"genre_scores_gemma":[0.9991804,0.000024312076,0.00015727992,0.0000068799063,0.0000036966478,0.0000040394652,0.00045168286,0.0000071111444,0.00016464114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997693,0.000054459808,0.000011130485,0.00008235461,0.000052906573,0.00002994811],"domain_scores_gemma":[0.99935514,0.00023872893,0.00019555748,0.00006581137,0.00009041318,0.000054340875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004715682,0.00031943436,0.00019558311,0.000364359,0.00016462816,0.00052947743,0.00013826833,0.0001389588,0.0012238602],"category_scores_gemma":[0.0017245715,0.00014821009,0.00024137867,0.0003321296,0.0001897784,0.00037584075,0.00024202067,0.0001412371,0.00012288579],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005911158,0.00006665475,0.8688033,0.00009104267,0.00040173778,0.0002304644,0.0004598643,0.038813528,0.06056353,0.0009575008,0.0014181186,0.027603175],"study_design_scores_gemma":[0.000011299925,0.000016238793,0.9784128,0.0000035234593,0.000024965335,0.000014215258,0.000034959947,0.019186415,0.0014249511,0.00026782605,0.0005935278,0.000009176862],"about_ca_topic_score_codex":0.0421121,"about_ca_topic_score_gemma":0.041127656,"teacher_disagreement_score":0.0421121,"about_ca_system_score_codex":0.0007355445,"about_ca_system_score_gemma":0.0002932987,"threshold_uncertainty_score":0.083733976},"labels":[],"label_agreement":null},{"id":"W2076348205","doi":"10.1029/2003gl017065","title":"Formation and propagation of great salinity anomalies","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; Universität Hamburg; Chinese Academy of Agricultural Sciences; Deutsche Forschungsgemeinschaft","keywords":"Thermohaline circulation; Oceanography; North Atlantic Deep Water; Geology; Archipelago; Sea ice; Climatology; Arctic ice pack; Arctic sea ice decline; Salinity; Arctic; Temperature salinity diagrams; Arctic dipole anomaly; Atlantic multidecadal oscillation; Drift ice","score_opus":0.030091371424630347,"score_gpt":0.2694853152405031,"score_spread":0.23939394381587278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076348205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985868,0.000036871952,0.00022810488,0.000026657319,0.0000026838031,0.0000023305636,0.00039693955,0.000021602953,0.0006979004],"genre_scores_gemma":[0.99905163,0.000044086497,0.00015702512,0.0000032949224,0.0000027818228,0.0000016074932,0.0005905024,0.0000030667975,0.000145986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999329,0.000010450706,0.000005430076,0.000026592126,0.000012105286,0.000012385738],"domain_scores_gemma":[0.9996723,0.00008843302,0.00013118879,0.00003322538,0.000042604213,0.000032133077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002407395,0.0001296118,0.00013136357,0.0004928678,0.00016075384,0.00039403563,0.0001413976,0.00017520948,0.0007415667],"category_scores_gemma":[0.00076466316,0.00013362474,0.000267752,0.0004942731,0.00018066632,0.00027304477,0.0002727289,0.00017245642,0.00011543489],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008781276,0.0000301268,0.9710325,0.00001764096,0.000081303886,0.00012409192,0.00016455521,0.0136706615,0.0027296732,0.00047288268,0.00050192943,0.011086778],"study_design_scores_gemma":[0.000010751645,0.000044807923,0.975021,0.0000050400117,0.000027919792,0.00007025893,0.00007582094,0.02296146,0.00069251214,0.00019004988,0.0008909276,0.000009458507],"about_ca_topic_score_codex":0.027184706,"about_ca_topic_score_gemma":0.030432507,"teacher_disagreement_score":0.027184706,"about_ca_system_score_codex":0.00047787774,"about_ca_system_score_gemma":0.00023391805,"threshold_uncertainty_score":0.05405295},"labels":[],"label_agreement":null},{"id":"W2076415385","doi":"10.1029/2006gl029059","title":"Solar wind–magnetosphere coupling efficiency for solar wind pressure impulses","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Science and Technology Facilities Council","keywords":"Magnetosphere; Solar wind; Physics; Polar wind; Magnetopause; Coupling (piping); Geophysics; Interplanetary magnetic field; Impulse (physics); Polar; Dynamic pressure; Interplanetary spaceflight; Environmental science; Computational physics; Atmospheric sciences; Mechanics; Magnetic field; Astronomy; Classical mechanics; Materials science","score_opus":0.01516564899882923,"score_gpt":0.2950806677933638,"score_spread":0.27991501879453456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076415385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986268,0.000034188713,0.00051901257,0.000010458278,0.0000013929684,0.000004422401,0.00015612919,0.000021174672,0.00062637834],"genre_scores_gemma":[0.99949527,0.000015582826,0.00010057849,0.0000030092406,0.000002260975,0.0000027141512,0.0002216297,0.000008082675,0.00015080546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998215,0.00002718707,0.000011910421,0.000049871847,0.000041192627,0.000048349215],"domain_scores_gemma":[0.99790156,0.0012197818,0.00039603384,0.000181073,0.00014739056,0.00015413185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004906494,0.00023951278,0.00032709874,0.0008601741,0.00013726417,0.00045540987,0.00018655881,0.00027782348,0.0015294622],"category_scores_gemma":[0.0033318838,0.00019653463,0.0003399129,0.00057273486,0.00019836436,0.00039027038,0.0003851694,0.00030376358,0.00024248194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011166316,0.00011523876,0.8192285,0.00011029357,0.0005556209,0.0005278675,0.0005043975,0.06518569,0.08441512,0.0005313632,0.0003836778,0.027325574],"study_design_scores_gemma":[0.000007798199,0.00006747978,0.9772385,0.0000026363648,0.00002751857,0.00013663879,0.00005060561,0.019713763,0.0025391353,0.00009265631,0.000111346104,0.000012023245],"about_ca_topic_score_codex":0.0014149649,"about_ca_topic_score_gemma":0.0011819466,"teacher_disagreement_score":0.0015294622,"about_ca_system_score_codex":0.00020094475,"about_ca_system_score_gemma":0.00009922556,"threshold_uncertainty_score":0.0051165223},"labels":[],"label_agreement":null},{"id":"W2076448919","doi":"10.1029/2007gl029748","title":"Cloud seeding as a technique for studying aerosol‐cloud interactions in marine stratocumulus","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Marine stratocumulus; Aerosol; Seeding; Atmospheric sciences; Transect; Environmental science; Cloud computing; Plume; Drizzle; Meteorology; Geology; Oceanography; Physics; Precipitation","score_opus":0.04318922658651603,"score_gpt":0.3538858883693647,"score_spread":0.31069666178284866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076448919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962017,0.00023399475,0.0032572362,0.000010392495,0.0000039642614,0.000023665967,0.000030090958,0.00001591055,0.00022311971],"genre_scores_gemma":[0.9952247,0.00015861822,0.0043783365,0.000014258006,0.000004090456,0.000014230252,0.000056419318,0.0000045321203,0.0001448387],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999343,0.000013475251,0.0000022241893,0.000013674564,0.000020351757,0.000015900061],"domain_scores_gemma":[0.9998853,0.00003918184,0.000027481452,0.000012018725,0.000012223603,0.000023710158],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015177549,0.0001696576,0.00011182921,0.00015773694,0.00022038499,0.00012276726,0.00016423306,0.00014299646,0.00018280376],"category_scores_gemma":[0.00014083488,0.000083030995,0.00012633247,0.00015486625,0.00018562691,0.000116076306,0.00018944933,0.00019321575,0.000036006695],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039088307,0.000011222874,0.0026477473,0.0000072401117,0.0000025067634,0.00004275475,0.000020581834,0.00017224578,0.995876,0.00003065678,0.000006669852,0.0011433447],"study_design_scores_gemma":[0.00002262358,0.00093951833,0.057404794,0.000003739078,0.000017114266,0.0002505307,0.00007549267,0.0072239353,0.9334753,0.00009058732,0.00048825593,0.000008106913],"about_ca_topic_score_codex":0.006240703,"about_ca_topic_score_gemma":0.0061351694,"teacher_disagreement_score":0.006240703,"about_ca_system_score_codex":0.00030541676,"about_ca_system_score_gemma":0.00017256234,"threshold_uncertainty_score":0.012408733},"labels":[],"label_agreement":null},{"id":"W2076489367","doi":"10.1029/2009gl040570","title":"Impact of a decreasing sea ice cover on the vertical export of particulate organic carbon in the northern Laptev Sea, Siberian Arctic Ocean","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski; Université Laval","funders":"Fonds Québécois de la Recherche sur la Nature et les Technologies; Networks of Centres of Excellence of Canada; University of Manitoba; Canada Research Chairs; ArcticNet; International Arctic Research Center, University of Alaska, Fairbanks","keywords":"Arctic; Oceanography; Sea ice; Environmental science; Arctic ice pack; Sediment; Geology; Total organic carbon; Particulates; Arctic geoengineering; Permafrost; Arctic sea ice decline; Climatology; Antarctic sea ice; Geomorphology; Ecology","score_opus":0.02116593198292863,"score_gpt":0.2706482390067976,"score_spread":0.24948230702386895,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076489367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996997,0.000034268654,0.000009448077,0.000021690732,0.0000032131793,6.636768e-7,0.000058461126,0.0000017072734,0.0001708896],"genre_scores_gemma":[0.9995654,0.000045406563,0.000024710744,0.00003053917,0.0000026287635,0.000002524932,0.0002142073,0.0000012388089,0.000113289454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989223,0.000023278837,0.000012258593,0.000023125272,0.000013818902,0.00003521196],"domain_scores_gemma":[0.9997199,0.000042184263,0.00008205319,0.0000212432,0.000043150223,0.00009141717],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041771278,0.00034398618,0.0002744654,0.00027575693,0.0006646627,0.0008870309,0.00021367618,0.00036291877,0.0008919278],"category_scores_gemma":[0.00058239413,0.0001404607,0.00029212105,0.00029900824,0.00041464588,0.00037539814,0.00069826795,0.00024136691,0.000113368784],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007741148,0.000098838995,0.9678551,0.0000433053,0.0001569492,0.0004984918,0.00022913003,0.0028376253,0.019421592,0.00006894068,0.0002228984,0.0077929473],"study_design_scores_gemma":[0.000009130158,0.00009437007,0.9981527,0.000004047841,0.000020700818,0.000027306896,0.00018724696,0.00076049584,0.00059380574,0.000015980935,0.00013195808,0.000002179995],"about_ca_topic_score_codex":0.05719384,"about_ca_topic_score_gemma":0.068210125,"teacher_disagreement_score":0.05719384,"about_ca_system_score_codex":0.001219025,"about_ca_system_score_gemma":0.0010439826,"threshold_uncertainty_score":0.11372191},"labels":[],"label_agreement":null},{"id":"W2076515674","doi":"10.1029/2002gl016039","title":"Model of the energization of outer‐zone electrons by whistler‐mode chorus during the October 9, 1990 geomagnetic storm","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":203,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Department of Science and Technology, Ministry of Science and Technology, India; National Aeronautics and Space Administration; National Science Foundation","keywords":"Van Allen radiation belt; Physics; Geomagnetic storm; Substorm; Electron; Whistler; Magnetosphere; Pitch angle; Geophysics; Chorus; Computational physics; Electron precipitation; Van Allen Probes; Hiss; Plasmasphere; Earth's magnetic field; Storm; Flux (metallurgy); Atmospheric sciences; Magnetic field; Meteorology; Nuclear physics; Quantum mechanics","score_opus":0.013764648497517063,"score_gpt":0.24573182912782568,"score_spread":0.2319671806303086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076515674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92911994,0.00023637505,0.044306383,0.0010851297,0.00005852155,0.00006669434,0.0006687449,0.00025399134,0.024204267],"genre_scores_gemma":[0.9932944,0.00010830884,0.0013175248,0.000039218296,0.000019347795,0.000043609,0.00013541253,0.000029091745,0.0050130626],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993193,0.000015991052,0.0000030784674,0.000013813916,0.00000986137,0.000025325211],"domain_scores_gemma":[0.9998197,0.000048183418,0.000044656776,0.000010031293,0.000031831623,0.000045651654],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020418153,0.00035151115,0.00037734877,0.00023988805,0.0005173856,0.0006243706,0.0009732062,0.0010877588,0.002386947],"category_scores_gemma":[0.00066638185,0.00035779565,0.00047735055,0.00022535467,0.0007257253,0.00076729676,0.0005091405,0.00044334502,0.00027411446],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001387381,0.000032046937,0.0040558656,0.000019608442,0.000027382508,0.00038451335,0.000105261,0.97042793,0.0037198223,0.01911818,0.0008571042,0.0011135446],"study_design_scores_gemma":[0.00005468481,0.000017329156,0.0012199236,0.0000021016215,0.0000072950634,0.000033347405,0.000026727046,0.9967193,0.00012030721,0.0015881022,0.0002023918,0.000008511518],"about_ca_topic_score_codex":0.036313727,"about_ca_topic_score_gemma":0.012787828,"teacher_disagreement_score":0.036313727,"about_ca_system_score_codex":0.0011221328,"about_ca_system_score_gemma":0.0008943834,"threshold_uncertainty_score":0.07220471},"labels":[],"label_agreement":null},{"id":"W2076560481","doi":"10.1029/2007gl031865","title":"Upscaling river networks for use in climate models","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Grid; Computer science; Resolution (logic); Measure (data warehouse); Flow (mathematics); Fraction (chemistry); Process (computing); Grid cell; Algorithm; Data mining; Hydrology (agriculture); Remote sensing; Geology; Artificial intelligence; Mathematics; Geodesy; Geometry","score_opus":0.08503181939375729,"score_gpt":0.33625313483160574,"score_spread":0.2512213154378484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076560481","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.11709728,0.00015944359,0.8671893,0.00023144967,0.00013980802,0.00024310045,0.0010912252,0.01095492,0.0028935291],"genre_scores_gemma":[0.3841499,0.00015309047,0.61251533,0.0000540977,0.000034339922,0.00021321606,0.0012429758,0.00070685777,0.00093022385],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997329,0.00007415225,0.000021873715,0.000066873785,0.00008592449,0.000018155924],"domain_scores_gemma":[0.99854314,0.00045168912,0.00017461479,0.0004329837,0.0003474498,0.000050065682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010420027,0.0007995516,0.00058557815,0.0011551644,0.00045225918,0.00089560024,0.0010037811,0.00055612624,0.002966471],"category_scores_gemma":[0.006731474,0.0005868733,0.00075023784,0.0011759811,0.00017466237,0.0013653731,0.0006721465,0.0009982974,0.0006181352],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041826494,0.00007117973,0.005763503,0.00004786759,0.00007628391,0.000079666366,0.00007845437,0.85055274,0.0049257437,0.002093343,0.0018903412,0.13437912],"study_design_scores_gemma":[0.00001642336,0.000011090116,0.0009925787,0.0000075435114,0.000008518678,0.00001574985,0.000018897676,0.99293923,0.0017401538,0.0026332282,0.0016015812,0.000014964997],"about_ca_topic_score_codex":0.016573628,"about_ca_topic_score_gemma":0.022921404,"teacher_disagreement_score":0.016573628,"about_ca_system_score_codex":0.00075858616,"about_ca_system_score_gemma":0.0008383436,"threshold_uncertainty_score":0.032954335},"labels":[],"label_agreement":null},{"id":"W2076599072","doi":"10.1029/2009gl040880","title":"Sensitivity of stable water isotopic values to convective parameterization schemes","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Energy Research Scientific Computing Center; Canadian Institute for Advanced Research; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Convective available potential energy; Convection; Environmental science; Water vapor; Atmospheric sciences; Troposphere; Precipitation; Free convective layer; Condensation; Climatology; Meteorology; Geology; Physics","score_opus":0.03658927890086663,"score_gpt":0.3130272121152459,"score_spread":0.2764379332143793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076599072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887621,0.00011184016,0.008442007,0.00011644252,0.000031444084,0.000029509223,0.0006084241,0.00016951484,0.0017288354],"genre_scores_gemma":[0.9981654,0.000034530654,0.0013191504,0.000031222873,0.0000027668646,0.0000152049315,0.0002986828,0.00003418918,0.0000988678],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999479,0.00016634127,0.0000600179,0.000145443,0.00006881205,0.00008032968],"domain_scores_gemma":[0.9980301,0.0010701392,0.00021544108,0.00046779643,0.00014155998,0.000074923766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001529669,0.00051527057,0.0003349766,0.00034507585,0.00032497264,0.0009026668,0.0006608026,0.0005166577,0.0009229256],"category_scores_gemma":[0.006180635,0.00039133176,0.0005292827,0.000364138,0.0004678917,0.0010817354,0.0008312985,0.0008041978,0.00012359642],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076616573,0.00013162091,0.11419869,0.00010369441,0.00037092084,0.00011588639,0.000192535,0.76538855,0.100305945,0.003852645,0.0006234726,0.013949816],"study_design_scores_gemma":[0.00010973849,0.00025575134,0.051868267,0.000024123938,0.000111053225,0.000051987186,0.00012892378,0.8659829,0.07536715,0.004196428,0.0018062086,0.000097527496],"about_ca_topic_score_codex":0.0066488143,"about_ca_topic_score_gemma":0.0037192535,"teacher_disagreement_score":0.0066488143,"about_ca_system_score_codex":0.00066597894,"about_ca_system_score_gemma":0.00030673193,"threshold_uncertainty_score":0.013220191},"labels":[],"label_agreement":null},{"id":"W2076606187","doi":"10.1029/2004gl020714","title":"The impact of Greenland's deglaciation on the Arctic circulation","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Arctic; Deglaciation; Climatology; Arctic dipole anomaly; Atmospheric circulation; Geology; Oceanography; Polar vortex; Arctic geoengineering; Arctic sea ice decline; Environmental science; Geopotential; Atmospheric sciences; Arctic ice pack; Stratosphere; Holocene; Antarctic sea ice","score_opus":0.04347258178340091,"score_gpt":0.3172173522936292,"score_spread":0.2737447705102283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076606187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968321,0.00025800135,0.0002096552,0.00017097661,0.000041101357,0.0000037452864,0.00043775295,0.000031590265,0.0020151148],"genre_scores_gemma":[0.998936,0.00018849786,0.0001455013,0.000047154535,0.0000063355733,0.0000021733617,0.00032370703,0.000015196628,0.00033541833],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987006,0.000030005622,0.0000057606785,0.00002101407,0.000011000891,0.000062271894],"domain_scores_gemma":[0.99975663,0.00006827089,0.00003383621,0.000023123901,0.000032681597,0.000085470165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035387216,0.00071819715,0.00039786077,0.00026872227,0.000600502,0.0010793925,0.0002825996,0.00042608235,0.0015680575],"category_scores_gemma":[0.0008789197,0.00018864434,0.00071627164,0.0003849662,0.00041068543,0.00051785854,0.00081040163,0.00032757557,0.00011396828],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016809636,0.00020202316,0.3056318,0.00021093086,0.0010410708,0.0018135121,0.00034468758,0.6422345,0.017870171,0.0028730677,0.0025188124,0.023578398],"study_design_scores_gemma":[0.00027819286,0.00043601327,0.76603514,0.000077546254,0.0005548361,0.00023512091,0.0007555059,0.2171076,0.005929571,0.0016758915,0.006840598,0.00007403602],"about_ca_topic_score_codex":0.11133451,"about_ca_topic_score_gemma":0.09734751,"teacher_disagreement_score":0.11133451,"about_ca_system_score_codex":0.0016779718,"about_ca_system_score_gemma":0.0013693906,"threshold_uncertainty_score":0.2213729},"labels":[],"label_agreement":null},{"id":"W2076616141","doi":"10.1029/1999gl011073","title":"An estimate of the eddy‐induced circulation in the Labrador Sea","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research; Lamont-Doherty Earth Observatory, Columbia University; National Oceanic and Atmospheric Administration","keywords":"Baroclinity; Eddy; Geology; Outflow; Geostrophic wind; Convection; Barotropic fluid; Inflow; Boundary current; Hydrography; Oceanography; Climatology; Geophysics; Ocean current; Mechanics; Turbulence; Physics","score_opus":0.027447340674073274,"score_gpt":0.2944783291708012,"score_spread":0.2670309884967279,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076616141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99617946,0.00014093681,0.0012203726,0.000025050955,0.0000040185746,0.0000064455676,0.000561993,0.000099017605,0.0017627187],"genre_scores_gemma":[0.99696964,0.00015634859,0.0011153284,0.000008167795,0.000008338333,0.000010609805,0.0013349032,0.000013357926,0.000383324],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991846,0.000017494829,0.000006923586,0.000015269625,0.000019064419,0.000022841201],"domain_scores_gemma":[0.9998311,0.00002471274,0.000044631146,0.000017913539,0.00006133969,0.00002036307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000118240205,0.00026274234,0.000120219665,0.000781117,0.00021117121,0.00043385767,0.00018235826,0.000111176494,0.00068998],"category_scores_gemma":[0.0006036786,0.00010169983,0.00022105337,0.00037392892,0.00011238435,0.0002887204,0.0001995321,0.00021146072,0.00036245305],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002617303,0.00010779071,0.8615589,0.00011421812,0.00015211948,0.00015087063,0.00030348913,0.016512446,0.049861472,0.0009873247,0.0008768397,0.06911285],"study_design_scores_gemma":[0.000016473285,0.00010238152,0.9595025,0.000016905498,0.000053553475,0.000094346164,0.000087420856,0.020060016,0.015369506,0.000108917644,0.0045707487,0.000017201335],"about_ca_topic_score_codex":0.017502183,"about_ca_topic_score_gemma":0.01853642,"teacher_disagreement_score":0.017502183,"about_ca_system_score_codex":0.0007395571,"about_ca_system_score_gemma":0.0003128645,"threshold_uncertainty_score":0.03480065},"labels":[],"label_agreement":null},{"id":"W2076820208","doi":"10.1029/2009gl038011","title":"Circulation responses to snow albedo feedback in climate change","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Climatology; Environmental science; Albedo (alchemy); Extratropical cyclone; Snow; Northern Hemisphere; Climate change; Atmospheric circulation; Climate model; General Circulation Model; Coupled model intercomparison project; Subtropics; Atmospheric sciences; Geology; Meteorology; Geography; Oceanography","score_opus":0.0815741864025115,"score_gpt":0.3476103317609938,"score_spread":0.2660361453584823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2076820208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99838793,0.000052695195,0.00046904988,0.00018637793,0.000012427263,0.0000025042607,0.00010192148,0.000052247236,0.00073495804],"genre_scores_gemma":[0.99969184,0.000031587857,0.00006958377,0.000012607595,0.000005194804,0.0000018384529,0.00005700636,0.0000055480214,0.00012475104],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999021,0.000041640913,0.0000048626566,0.000016704238,0.000013280821,0.000021416536],"domain_scores_gemma":[0.9997757,0.000083678206,0.00003853177,0.000022610067,0.000034977405,0.000044603865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024179628,0.00020141127,0.00020934746,0.00018737477,0.00018956317,0.0003656524,0.00014733002,0.00028318298,0.0011086109],"category_scores_gemma":[0.001054378,0.00016472646,0.00034282563,0.00018109007,0.00022017791,0.0003390575,0.00040777598,0.00025636205,0.00011271942],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041843278,0.00016842647,0.3155977,0.000061375235,0.00034744784,0.00033131044,0.00028722596,0.6157845,0.049498063,0.0020547654,0.0018237549,0.013626969],"study_design_scores_gemma":[0.00008378065,0.000111301575,0.36292273,0.000009586468,0.000087386536,0.000067182074,0.00012945796,0.6316273,0.0022831613,0.0018602571,0.0007878646,0.000030014551],"about_ca_topic_score_codex":0.010541264,"about_ca_topic_score_gemma":0.010644051,"teacher_disagreement_score":0.010541264,"about_ca_system_score_codex":0.00045350374,"about_ca_system_score_gemma":0.0002512982,"threshold_uncertainty_score":0.020959795},"labels":[],"label_agreement":null},{"id":"W2077137674","doi":"10.1029/2002gl014843","title":"Competitive adsorption of atmospheric trace gases onto ice at 228 K: HNO<sub>3</sub>/HCl, 1‐Butanol/Acetic acid and 1‐Butanol/HCl","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Carbon Dioxide Capture Technologies","field":"Engineering","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Adsorption; Butanol; Acetic acid; Chemistry; n-Butanol; Nitric acid; Trace gas; Inorganic chemistry; Hydrochloric acid; Analytical Chemistry (journal); Chromatography; Ethanol; Organic chemistry","score_opus":0.018694601358612218,"score_gpt":0.23674229343812006,"score_spread":0.21804769207950783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077137674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997329,0.00035562736,0.00063480315,0.00003467172,0.000014110799,0.00001795566,0.00027657356,0.000029115241,0.0013080668],"genre_scores_gemma":[0.9956755,0.00036109838,0.001269003,0.000026657077,0.000008991373,0.000024938192,0.0005337543,0.00002326713,0.0020768296],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997503,0.000018002753,0.000008586139,0.00005476444,0.000075317344,0.00009303422],"domain_scores_gemma":[0.99971753,0.00012790239,0.00002536181,0.00002129719,0.00006898651,0.00003884753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018352488,0.00041686092,0.00045724094,0.00015569483,0.00035347414,0.0003305111,0.00067380606,0.00034628116,0.0022334484],"category_scores_gemma":[0.00044902964,0.00028177552,0.0002842422,0.0001499812,0.0002836715,0.00024700174,0.00029020096,0.00036324433,0.0004960603],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003741703,0.000014874506,0.00082430756,0.00007429775,0.000015684964,0.00002766076,0.000031303152,0.00014503613,0.9973182,0.000053188465,0.0000769803,0.0010443473],"study_design_scores_gemma":[0.000013690372,0.00014442904,0.00414492,0.0000041823573,0.000014261227,0.000033763456,0.000037632428,0.0012409113,0.9939043,0.000016753955,0.00043885986,0.0000062943923],"about_ca_topic_score_codex":0.0088236695,"about_ca_topic_score_gemma":0.014899063,"teacher_disagreement_score":0.0088236695,"about_ca_system_score_codex":0.0006207432,"about_ca_system_score_gemma":0.00042143528,"threshold_uncertainty_score":0.017544627},"labels":[],"label_agreement":null},{"id":"W2077173640","doi":"10.1029/2003gl018203","title":"Partially soluble organics as cloud condensation nuclei: Role of trace soluble and surface active species","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":142,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Cloud condensation nuclei; Adipic acid; Surface tension; Solubility; Condensation; Succinic acid; Sulfate; Aerosol; Chemical engineering; Trace gas; Chemistry; Materials science; Environmental chemistry; Organic chemistry; Thermodynamics","score_opus":0.023503152860040767,"score_gpt":0.25707934229032803,"score_spread":0.23357618943028727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077173640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98879707,0.0030514,0.004519215,0.0000648908,0.000017147386,0.0000304086,0.000118335134,0.000030660547,0.0033709852],"genre_scores_gemma":[0.99759394,0.00055581937,0.0009772854,0.0000072216253,0.0000038459984,0.0000039033985,0.0000611613,0.0000054975294,0.0007913162],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989474,0.000019701733,0.0000031149991,0.000020532427,0.000029925031,0.000031994103],"domain_scores_gemma":[0.9997882,0.00009565881,0.000019323417,0.000019990668,0.000032684813,0.000044166827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028754602,0.00036572738,0.00018944682,0.00015187639,0.00025513239,0.0004386678,0.00032646596,0.00027213464,0.0010717165],"category_scores_gemma":[0.00029874296,0.00010886286,0.00016660368,0.00009452119,0.00035023203,0.00051435,0.00025104242,0.00017880432,0.00019097971],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027072773,0.000036093104,0.004352508,0.00012606445,0.000021496428,0.00010659324,0.0000562892,0.0045373575,0.9789629,0.0030490963,0.000060238566,0.008420551],"study_design_scores_gemma":[0.00003252823,0.00024859465,0.0060104458,0.000009669369,0.000023908242,0.00011790011,0.00005712243,0.03698576,0.9529568,0.0011285358,0.002412971,0.000015818592],"about_ca_topic_score_codex":0.004027953,"about_ca_topic_score_gemma":0.004031457,"teacher_disagreement_score":0.004027953,"about_ca_system_score_codex":0.00038547334,"about_ca_system_score_gemma":0.00029181765,"threshold_uncertainty_score":0.0080090165},"labels":[],"label_agreement":null},{"id":"W2077281041","doi":"10.1002/2013gl059070","title":"Breaking internal lee waves at Kaena Ridge, Hawaii","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Isopycnal; Internal tide; Internal wave; Geology; Ridge; Stratification (seeds); Seafloor spreading; Bathymetry; Turbulence; Dissipation; Pycnocline; Supercritical flow; Forcing (mathematics); Kelvin wave; Geophysics; Mechanics; Flow (mathematics); Atmospheric sciences; Oceanography; Physics","score_opus":0.020854929066066976,"score_gpt":0.26549437739693743,"score_spread":0.24463944833087045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077281041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995339,0.000008238536,0.000059114333,0.000005712237,6.437068e-7,0.0000015017789,0.000025126703,0.0000057204475,0.0003600257],"genre_scores_gemma":[0.9997229,0.000009305762,0.00007739483,0.0000018525355,4.2675822e-7,0.0000017294873,0.000039010203,8.521375e-7,0.00014650152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997294,0.0000018433559,0.0000013079257,0.0000071821373,0.000007860617,0.000008864206],"domain_scores_gemma":[0.99989736,0.000009710074,0.000025295878,0.000010117314,0.000027099515,0.000030477695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005677744,0.000098410186,0.00008426431,0.00022946755,0.00037273538,0.0004250053,0.00013881948,0.00012561881,0.00041919452],"category_scores_gemma":[0.00022057859,0.000098143566,0.000098800025,0.00015388442,0.00029997446,0.00013917455,0.0003964423,0.00017054805,0.00006421915],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011781676,0.00010278268,0.87920403,0.000049150116,0.0000753343,0.00079539814,0.002858731,0.0058767567,0.08714747,0.00028178585,0.00043097325,0.023059674],"study_design_scores_gemma":[0.000006257477,0.00007971635,0.989402,0.0000079769925,0.000015580052,0.00008955813,0.0013482608,0.0053957077,0.0031571216,0.00007811012,0.00040420156,0.000015513111],"about_ca_topic_score_codex":0.05868715,"about_ca_topic_score_gemma":0.06650159,"teacher_disagreement_score":0.05868715,"about_ca_system_score_codex":0.00032141295,"about_ca_system_score_gemma":0.00035126862,"threshold_uncertainty_score":0.11669111},"labels":[],"label_agreement":null},{"id":"W2077341065","doi":"10.1029/2003gl017303","title":"Large scale atmosphere‐ocean anomalies in the northeast Pacific during 2002","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Upwelling; Oceanography; Geology; Atmosphere (unit); Subarctic climate; Current (fluid); Wind stress; Climatology; Pacific ocean; Environmental science; Meteorology; Geography","score_opus":0.014975962591075153,"score_gpt":0.23895471863272497,"score_spread":0.22397875604164982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077341065","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99536777,0.00013234148,0.000094352006,0.0002540214,0.000028127677,0.000008989853,0.0018147755,0.00003143524,0.0022683062],"genre_scores_gemma":[0.9962806,0.00013369697,0.00015629284,0.000081352584,0.000019232444,0.00001155738,0.0025331313,0.000009116277,0.0007749519],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990034,0.000006763324,0.000008568482,0.000031821564,0.000031736254,0.000020828094],"domain_scores_gemma":[0.999691,0.000023462351,0.0000886014,0.000018444653,0.00011053828,0.00006795294],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015002368,0.00018499275,0.00016349759,0.00044735958,0.00061546953,0.0008850203,0.00019008643,0.00030328264,0.0005598622],"category_scores_gemma":[0.000691886,0.00016857237,0.000109307446,0.0007286935,0.00016746373,0.00034059378,0.00054620334,0.00032541755,0.00010302497],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022671811,0.00009924238,0.9675974,0.00005259872,0.00009933452,0.0007664426,0.0010906111,0.001096414,0.009062445,0.00020567344,0.0046727606,0.015030238],"study_design_scores_gemma":[0.0000066399994,0.000008465632,0.9962106,0.0000061429223,0.000011367432,0.0000656205,0.00024454604,0.00048600082,0.00035116,0.00003103112,0.0025737383,0.0000046888285],"about_ca_topic_score_codex":0.1325884,"about_ca_topic_score_gemma":0.2645938,"teacher_disagreement_score":0.1325884,"about_ca_system_score_codex":0.0010865497,"about_ca_system_score_gemma":0.0006966505,"threshold_uncertainty_score":0.26363325},"labels":[],"label_agreement":null},{"id":"W2077650774","doi":"10.1029/2003gl017861","title":"High aerosol optical depth biomass burning events: A comparison of optical properties for different source regions","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":241,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"","keywords":"AERONET; Aerosol; Single-scattering albedo; Smoke; Environmental science; Optical depth; Atmospheric sciences; Albedo (alchemy); Effective radius; Combustion; Boreal; Biomass (ecology); Peat; Taiga; Scattering; Meteorology; Geology; Optics; Chemistry; Physics; Geography","score_opus":0.052515707558356696,"score_gpt":0.309747326131131,"score_spread":0.25723161857277427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077650774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999716,0.000020356747,0.000063016,0.0000017905371,3.3133767e-7,0.000002087871,0.000067348694,0.000004539164,0.00012449508],"genre_scores_gemma":[0.99951863,0.000017639824,0.000108823326,0.0000019701035,0.0000011309447,0.0000018890515,0.00031305407,0.000002012621,0.000034887373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999231,0.00000653603,0.000006614632,0.000014849407,0.000017918503,0.000031060354],"domain_scores_gemma":[0.99971753,0.000079491256,0.00007138229,0.00002115428,0.00006298744,0.000047336296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001799597,0.0002626011,0.00016694813,0.00095297315,0.00024000448,0.0003087634,0.00013903859,0.00021746707,0.00032459243],"category_scores_gemma":[0.0004218105,0.00013219014,0.00023834914,0.00041831628,0.0001194035,0.00020305994,0.0002780487,0.00011709965,0.00008229947],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006123527,0.00008774363,0.91114444,0.000036933576,0.000113399896,0.00041567234,0.00038762297,0.0013529615,0.076474875,0.000077185025,0.00009155063,0.009205256],"study_design_scores_gemma":[0.0000060680572,0.00003815249,0.99545395,0.0000014484166,0.000018546134,0.00014097083,0.000073203504,0.0006877306,0.0035037901,0.000009913643,0.00006374648,0.0000023786527],"about_ca_topic_score_codex":0.006175611,"about_ca_topic_score_gemma":0.007730942,"teacher_disagreement_score":0.006175611,"about_ca_system_score_codex":0.00021179447,"about_ca_system_score_gemma":0.00006661894,"threshold_uncertainty_score":0.012279332},"labels":[],"label_agreement":null},{"id":"W2077805318","doi":"10.1029/2006gl025862","title":"Biases of SRTM in high‐mountain areas: Implications for the monitoring of glacier volume changes","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":222,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Shuttle Radar Topography Mission; Glacier; Geology; Physical geography; Altitude (triangle); Glacial period; Digital elevation model; Remote sensing; Geomorphology; Geography","score_opus":0.07743909695615597,"score_gpt":0.31799683588601874,"score_spread":0.24055773892986276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077805318","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9773446,0.0018897998,0.01627599,0.0009420858,0.00006123582,0.000022691378,0.00071122235,0.0002204354,0.0025320076],"genre_scores_gemma":[0.9929004,0.00023899645,0.0061631263,0.00011511825,0.000039623108,0.000010187047,0.0002925993,0.000034778965,0.0002051111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9987883,0.0005984716,0.000106766696,0.00015174739,0.0002749856,0.000079634585],"domain_scores_gemma":[0.9904765,0.0049177567,0.0022374126,0.0010269708,0.0012248895,0.00011643093],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0052702706,0.0004051914,0.00038312262,0.0006118495,0.00039012288,0.0011653285,0.00042610487,0.00052360597,0.0005068912],"category_scores_gemma":[0.014647073,0.00014721249,0.0003542492,0.0014000288,0.00044932036,0.0013451345,0.0004824005,0.00031222266,0.00017065136],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018697172,0.000032813856,0.937232,0.00011430268,0.00017595886,0.00010564225,0.00047782416,0.008079131,0.0076822923,0.0008060953,0.00041907025,0.04468783],"study_design_scores_gemma":[0.000022895114,0.00016972578,0.9477571,0.0001029066,0.00018239387,0.000597649,0.00047741644,0.030140111,0.015057443,0.003187878,0.002246597,0.000057675294],"about_ca_topic_score_codex":0.0068715117,"about_ca_topic_score_gemma":0.0081002675,"teacher_disagreement_score":0.0068715117,"about_ca_system_score_codex":0.00048641348,"about_ca_system_score_gemma":0.00043233935,"threshold_uncertainty_score":0.027872205},"labels":[],"label_agreement":null},{"id":"W2077883063","doi":"10.1029/2007gl030216","title":"Increased groundwater to stream discharge from permafrost thawing in the Yukon River basin: Potential impacts on lateral export of carbon and nitrogen","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":630,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Groundwater; Thermokarst; Streamflow; Dissolved organic carbon; Environmental science; Hydrology (agriculture); Arctic; Drainage basin; Subarctic climate; Groundwater discharge; Groundwater flow; Surface water; Climate change; Infiltration (HVAC); Oceanography; Geology; Aquifer; Geography; Environmental engineering","score_opus":0.03729623028381011,"score_gpt":0.2854219985349828,"score_spread":0.2481257682511727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2077883063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996972,0.000032672768,0.000036981488,0.000026873731,5.530742e-7,8.5192875e-7,0.000067225636,0.000002577629,0.00013517465],"genre_scores_gemma":[0.99974793,0.000031028125,0.000035823705,0.0000080166865,4.73815e-7,0.000001123829,0.000099449855,6.1263904e-7,0.00007553447],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995625,0.0000069674593,0.000004501886,0.000009734067,0.000006817732,0.000015763108],"domain_scores_gemma":[0.9999329,0.000011679671,0.000016447368,0.0000030647143,0.000023111794,0.000012817043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008067724,0.00008337868,0.00010960511,0.00023400171,0.00034496727,0.00033084117,0.000133369,0.00018184136,0.00074915757],"category_scores_gemma":[0.00023050915,0.00009666259,0.00011738899,0.0004956805,0.00022351822,0.0002575203,0.0002754209,0.000093003924,0.000042574487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010084574,0.000022929651,0.9776488,0.00003857406,0.000043305925,0.00025490613,0.00028732527,0.0012301172,0.009816605,0.00021535024,0.00017741769,0.010163863],"study_design_scores_gemma":[0.000004747612,0.000015808102,0.9970337,0.0000036879073,0.000013948392,0.000056893838,0.0003335199,0.0016103617,0.0006226057,0.00009009087,0.00021078294,0.0000037944071],"about_ca_topic_score_codex":0.09797108,"about_ca_topic_score_gemma":0.22235653,"teacher_disagreement_score":0.9020289,"about_ca_system_score_codex":0.0011104045,"about_ca_system_score_gemma":0.00086797395,"threshold_uncertainty_score":0.19480163},"labels":[],"label_agreement":null},{"id":"W2078010207","doi":"10.1029/2007gl031093","title":"Air‐sea interaction associated with a Greenland reverse tip jet","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Jet (fluid); Greenland ice sheet; Geology; Oceanography; Atmospheric sciences; Climatology; Geodesy; Mechanics; Ice sheet; Physics","score_opus":0.04513441730473084,"score_gpt":0.32118494532150327,"score_spread":0.27605052801677243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078010207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950913,0.000016879878,0.00030370033,0.00007864434,0.000010636374,0.000009869966,0.000083993335,0.000022443239,0.0043824203],"genre_scores_gemma":[0.9993135,0.000015950434,0.00015749916,0.000024813271,0.0000027630026,0.0000049561086,0.00006901731,0.000004803689,0.00040677816],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998946,0.000015639205,0.0000032116764,0.0000110447145,0.000013941032,0.00006156441],"domain_scores_gemma":[0.9998338,0.000046722565,0.000028863116,0.000011014003,0.00001577793,0.00006388124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013382813,0.00033154752,0.00034977554,0.0002613303,0.0006297076,0.0007784676,0.00034014645,0.000713421,0.0021020342],"category_scores_gemma":[0.00039371705,0.00018684864,0.00046948416,0.000244295,0.0005060968,0.00036999697,0.0009689337,0.00057470455,0.00011149775],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006291591,0.00038458224,0.12733269,0.000036981226,0.00017134112,0.0028786536,0.00034087957,0.8484567,0.0102714375,0.003330579,0.0017913303,0.0043757474],"study_design_scores_gemma":[0.00027616395,0.00038536772,0.10045303,0.000016377306,0.00010228021,0.00018716452,0.0009978558,0.8922257,0.0024665426,0.0012552942,0.0015889833,0.000045227778],"about_ca_topic_score_codex":0.06600322,"about_ca_topic_score_gemma":0.06452055,"teacher_disagreement_score":0.06600322,"about_ca_system_score_codex":0.0008804904,"about_ca_system_score_gemma":0.0008908177,"threshold_uncertainty_score":0.13123804},"labels":[],"label_agreement":null},{"id":"W2078170471","doi":"10.1029/2008gl036162","title":"Enhanced production of Labrador Sea Water in 2008","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":169,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Division of Ocean Sciences","keywords":"Argo; Oceanography; Convection; Atmosphere (unit); Climatology; Geology; Environmental science; Thermohaline circulation; Atmospheric sciences; Geography; Meteorology","score_opus":0.016968295686433123,"score_gpt":0.2603776270743673,"score_spread":0.24340933138793416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078170471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99711007,0.00012758948,0.00008040293,0.00010467276,0.000007166119,0.000004811068,0.0007032582,0.00003631129,0.0018257761],"genre_scores_gemma":[0.996342,0.00021931219,0.00026671524,0.0000622325,0.000012673928,0.000006735998,0.0014754503,0.000013238685,0.0016015809],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999162,0.000007451079,0.000005849601,0.000025240495,0.000018461691,0.000026774467],"domain_scores_gemma":[0.99984384,0.000006315597,0.00006810562,0.000010249271,0.000040541523,0.00003099516],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001502801,0.00025320513,0.00017234168,0.0007626314,0.00029240779,0.00068391126,0.000203064,0.00015673751,0.0014591848],"category_scores_gemma":[0.0002683257,0.00010178326,0.00017517807,0.0008652614,0.00017555564,0.00035305956,0.00043852502,0.00020234154,0.00038425103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009947297,0.00011438948,0.7215206,0.00025652675,0.00014433787,0.0011309526,0.0017671118,0.00079148775,0.16723412,0.0005488434,0.0037277949,0.10176918],"study_design_scores_gemma":[0.000008793061,0.00010596665,0.97796255,0.000010426366,0.000016944203,0.00013511605,0.00045495565,0.00032593118,0.012581241,0.000038889084,0.008350154,0.0000089801215],"about_ca_topic_score_codex":0.018930895,"about_ca_topic_score_gemma":0.040891547,"teacher_disagreement_score":0.018930895,"about_ca_system_score_codex":0.0013363404,"about_ca_system_score_gemma":0.00052814424,"threshold_uncertainty_score":0.037641406},"labels":[],"label_agreement":null},{"id":"W2078812110","doi":"10.1029/2007gl029344","title":"Changes in the Arctic Oscillation under increased atmospheric greenhouse gases","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; University of British Columbia","funders":"","keywords":"Greenhouse gas; Arctic oscillation; Climatology; North Atlantic oscillation; Environmental science; Atmospheric circulation; Atmospheric pressure; Atmospheric sciences; Oscillation (cell signaling); Climate change; General Circulation Model; The arctic; Arctic; Sea level; Geology; Oceanography; Chemistry","score_opus":0.0497319435768736,"score_gpt":0.31152535574100393,"score_spread":0.2617934121641303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078812110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989435,0.000047858935,0.00033816078,0.00005495721,0.00000918372,0.0000020794228,0.00010204017,0.000012377825,0.0004898021],"genre_scores_gemma":[0.9994874,0.00005015835,0.00023187435,0.000011686308,0.0000056629824,0.0000025693532,0.00013304241,0.0000043056148,0.00007310494],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99977547,0.00006610412,0.000016176895,0.000071203925,0.000032865744,0.000038083504],"domain_scores_gemma":[0.99971706,0.00009394508,0.000057525973,0.000038578557,0.00005751149,0.000035263387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063698203,0.00022068167,0.00031301845,0.00022659397,0.00036160558,0.00086599216,0.00022827998,0.00042672458,0.00046234083],"category_scores_gemma":[0.0018231685,0.00018331937,0.00057834166,0.0003823936,0.00036137347,0.00049469946,0.00050770334,0.00036652456,0.000068951194],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005195345,0.00013446936,0.4677766,0.00007184165,0.00073708716,0.00024557626,0.00030585466,0.5015031,0.016201224,0.0019142532,0.0008630758,0.009727424],"study_design_scores_gemma":[0.0001226922,0.00023159782,0.47466007,0.000018667466,0.00021150704,0.0001402475,0.00026076118,0.5185849,0.0025958535,0.0015184955,0.0016091474,0.000046073594],"about_ca_topic_score_codex":0.020433675,"about_ca_topic_score_gemma":0.01597526,"teacher_disagreement_score":0.020433675,"about_ca_system_score_codex":0.0007718399,"about_ca_system_score_gemma":0.00048062814,"threshold_uncertainty_score":0.040629447},"labels":[],"label_agreement":null},{"id":"W2078968904","doi":"10.1029/2007gl032006","title":"Photoenhanced uptake of NO<sub>2</sub> on mineral dust: Laboratory experiments and model simulations","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":293,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Université de Versailles Saint-Quentin-en-Yvelines; Université Cheikh Anta Diop de Dakar; Paul Scherrer Institut; Centre National de la Recherche Scientifique; Agence Universitaire de la Francophonie","keywords":"Mineral dust; Troposphere; Photocatalysis; Ozone; Environmental chemistry; Mass fraction; Fraction (chemistry); Mineral; Mineralogy; Atmospheric sciences; Chemistry; Analytical Chemistry (journal); Environmental science; Materials science; Geology; Metallurgy; Aerosol; Catalysis; Chromatography; Organic chemistry","score_opus":0.03790319421368463,"score_gpt":0.28289796665156985,"score_spread":0.24499477243788523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2078968904","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970715,0.00015186828,0.0009656917,0.00007507249,0.000012992775,0.000019308896,0.0002427253,0.000039315764,0.0014214054],"genre_scores_gemma":[0.99859315,0.00015637725,0.0005863124,0.000019888266,0.0000063942957,0.000030569256,0.00011929229,0.000009382035,0.00047872227],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989367,0.00001904434,0.0000040704613,0.00002847072,0.000017284874,0.00003749772],"domain_scores_gemma":[0.9994493,0.00037745354,0.000047480462,0.000023256254,0.00006636453,0.000036053225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028494795,0.0006308571,0.00080452237,0.00025807432,0.0003136652,0.00057547056,0.0007195378,0.0012939348,0.0012479911],"category_scores_gemma":[0.000728438,0.000354805,0.0007199226,0.00028768065,0.00049029366,0.0006177562,0.00031885534,0.00046479795,0.00017858349],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000656474,0.00038613833,0.0063751913,0.00022544953,0.000060389055,0.0003827501,0.000085955486,0.9496857,0.038542498,0.00084931677,0.0005193374,0.0022307716],"study_design_scores_gemma":[0.000119672615,0.00013491002,0.0018039325,0.000004013612,0.000019172085,0.000015429374,0.000041512412,0.9897301,0.007808709,0.00021043637,0.0000970959,0.000015012047],"about_ca_topic_score_codex":0.023390578,"about_ca_topic_score_gemma":0.00867805,"teacher_disagreement_score":0.023390578,"about_ca_system_score_codex":0.0015660237,"about_ca_system_score_gemma":0.0004716734,"threshold_uncertainty_score":0.04650891},"labels":[],"label_agreement":null},{"id":"W2079056560","doi":"10.1029/2006gl027388","title":"Does kinematic advection by superimposed waves provide an explanation for quasi‐universal gravity‐wave spectra?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Advection; Gravity wave; Superposition principle; Physics; Amplitude; Wavenumber; Eulerian path; Kinematics; Atmospheric wave; Gravitational wave; Classical mechanics; Spectral line; Standing wave; Mechanics; Wave propagation; Lagrangian; Optics; Astrophysics; Quantum mechanics","score_opus":0.012254879019023735,"score_gpt":0.26982834973338393,"score_spread":0.2575734707143602,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079056560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89686674,0.0009685079,0.08532769,0.0016087624,0.00014133852,0.00004983566,0.00034852585,0.0013880088,0.013300612],"genre_scores_gemma":[0.99738187,0.00016673397,0.0019200208,0.00006277876,0.00003018205,0.0000060676634,0.000059951402,0.000027559123,0.0003447651],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984837,0.000011282102,0.0000101057385,0.000041511674,0.000034172113,0.000054509794],"domain_scores_gemma":[0.999006,0.00023846942,0.0002446233,0.00033096017,0.00009054819,0.00008949062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004496171,0.00038961723,0.00034711143,0.00079328334,0.0004746694,0.00072862615,0.0014076246,0.0008247964,0.005252998],"category_scores_gemma":[0.0020548042,0.0003288494,0.00046555817,0.00046691482,0.0018135046,0.0022123682,0.00072563614,0.00054843037,0.0005502255],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008137175,0.00037637632,0.23987313,0.0011149568,0.00034411554,0.0070850863,0.0018275672,0.032116603,0.16142541,0.41132903,0.0039397287,0.13975425],"study_design_scores_gemma":[0.00018052434,0.0003627767,0.23536408,0.000097162934,0.00013887903,0.006102207,0.0011060081,0.3260121,0.02716161,0.394278,0.009037454,0.0001592004],"about_ca_topic_score_codex":0.0006159008,"about_ca_topic_score_gemma":0.0005339287,"teacher_disagreement_score":0.005252998,"about_ca_system_score_codex":0.00033383048,"about_ca_system_score_gemma":0.00022549352,"threshold_uncertainty_score":0.017572999},"labels":[],"label_agreement":null},{"id":"W2079138567","doi":"10.1029/2000gl011999","title":"Calibration changes in the isotopic thermometer for snow according to different climatic states","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Summit; Thermometer; Ice core; Snow; Calibration; Geology; Glacial period; Anomaly (physics); Climatology; Holocene; Mechanism (biology); Physical geography; Geomorphology; Paleontology; Physics; Thermodynamics; Geography","score_opus":0.08623389491408119,"score_gpt":0.32066043823040313,"score_spread":0.23442654331632196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079138567","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8830131,0.00053642475,0.1024271,0.0002286372,0.000328967,0.000077090066,0.001221522,0.0011833006,0.010983785],"genre_scores_gemma":[0.9692491,0.00023854498,0.027281547,0.00023226738,0.000029570178,0.000075381446,0.0007011644,0.0001436416,0.0020488633],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9993895,0.00013738735,0.000030034336,0.00020908011,0.00019218722,0.000041739488],"domain_scores_gemma":[0.99930537,0.00017779406,0.00014511212,0.00017637548,0.00017140884,0.000023941502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011955537,0.00041129783,0.0001805649,0.00076879055,0.00037798082,0.00032203007,0.00053696765,0.0004076485,0.001339986],"category_scores_gemma":[0.002549867,0.0003132301,0.00022008618,0.0007931133,0.0004137884,0.00037430786,0.0004701194,0.00033822475,0.00069045],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007273635,0.00012678435,0.33285794,0.00012926916,0.00021080699,0.00011736891,0.00060357194,0.0034481627,0.55590194,0.0026417237,0.001629746,0.101605296],"study_design_scores_gemma":[0.000051219253,0.00042958336,0.5109393,0.00003356047,0.00014155623,0.0009835447,0.00017570498,0.022660231,0.45082957,0.0015916195,0.012071594,0.000092381764],"about_ca_topic_score_codex":0.0015290093,"about_ca_topic_score_gemma":0.005223472,"teacher_disagreement_score":0.0015290093,"about_ca_system_score_codex":0.00039499486,"about_ca_system_score_gemma":0.00023091058,"threshold_uncertainty_score":0.0063227415},"labels":[],"label_agreement":null},{"id":"W2079261398","doi":"10.1029/2006gl026549","title":"The tropopause inversion layer in models and analyses","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; National Oceanic and Atmospheric Administration; Scheme for Promotion of Academic and Research Collaboration; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Tropopause; Radiosonde; Climatology; GCM transcription factors; General Circulation Model; Atmospheric sciences; Data assimilation; Inversion (geology); Atmospheric model; Environmental science; Stratification (seeds); Geology; Meteorology; Stratosphere; Climate change; Geography","score_opus":0.07423068502090195,"score_gpt":0.3285145948000542,"score_spread":0.2542839097791522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079261398","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.07437263,0.004280853,0.8210673,0.0030573346,0.00079796574,0.00026731053,0.018146649,0.005319457,0.07269052],"genre_scores_gemma":[0.7608608,0.002877714,0.19294195,0.0006183114,0.0005688253,0.00059379294,0.009102172,0.0017874088,0.030649055],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997278,0.00009723424,0.000016728105,0.00005891798,0.00006110862,0.000038265425],"domain_scores_gemma":[0.99962354,0.00014768912,0.000044316406,0.00008220489,0.00007665343,0.000025631814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009002957,0.0007631741,0.00045647143,0.00041118395,0.00046259852,0.0016086762,0.002009771,0.001125565,0.0067396755],"category_scores_gemma":[0.0025525826,0.0005968277,0.0007605039,0.00085313915,0.00036727413,0.0020406798,0.0011592308,0.0013167722,0.0020162554],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006496767,0.000030917396,0.0038697068,0.00008843308,0.00013268746,0.00008430034,0.000090704605,0.88736725,0.00072942965,0.0706122,0.0115874745,0.02534199],"study_design_scores_gemma":[0.000025042982,0.000010816288,0.000782002,0.00002833007,0.000032269152,0.000020651547,0.000031545664,0.9457058,0.0003915966,0.0354658,0.017488608,0.00001760207],"about_ca_topic_score_codex":0.02981443,"about_ca_topic_score_gemma":0.027069246,"teacher_disagreement_score":0.02981443,"about_ca_system_score_codex":0.0008053991,"about_ca_system_score_gemma":0.0014427169,"threshold_uncertainty_score":0.059281766},"labels":[],"label_agreement":null},{"id":"W2079799974","doi":"10.1029/2008gl036660","title":"Frictional behavior of materials in the 3D SAFOD volume","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Geology; Lithology; Siltstone; Outcrop; Borehole; Mineralogy; Talc; Fault gouge; Petrology; Mafic; Geochemistry; Quartz; Fault (geology); Geotechnical engineering; Seismology; Geomorphology; Facies","score_opus":0.04096782447316287,"score_gpt":0.29827752716952133,"score_spread":0.25730970269635844,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2079799974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963104,0.00008406993,0.0024766878,0.000010485821,0.0000022853317,0.0000033249823,0.00026953148,0.00008492588,0.0007583856],"genre_scores_gemma":[0.9986192,0.000032832428,0.00087939086,0.000002613191,0.0000011353247,0.000002603348,0.0003572691,0.000010887341,0.000094031646],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998957,0.000007412399,0.000007527806,0.00002750759,0.000043349784,0.000018503599],"domain_scores_gemma":[0.99978083,0.00007188476,0.000050618026,0.000035321074,0.000038592574,0.000022749324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011126738,0.00020593122,0.00024527826,0.0008553862,0.00027202076,0.00079839205,0.00029836752,0.00021521334,0.0010056865],"category_scores_gemma":[0.00073413405,0.00028190477,0.00030013896,0.00060453475,0.0003586453,0.00044569827,0.00031326473,0.00015448265,0.00013640407],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007194348,0.00012319394,0.30007634,0.00019586661,0.00026255858,0.0011431039,0.00090819714,0.4059299,0.23899116,0.001975254,0.00055718847,0.049117807],"study_design_scores_gemma":[0.000037215093,0.00017199734,0.4438368,0.000023348208,0.00006273214,0.0006821434,0.00032946494,0.4991066,0.05160133,0.0009234581,0.0031326867,0.00009226393],"about_ca_topic_score_codex":0.0039245845,"about_ca_topic_score_gemma":0.005018256,"teacher_disagreement_score":0.0039245845,"about_ca_system_score_codex":0.00039828368,"about_ca_system_score_gemma":0.00020636246,"threshold_uncertainty_score":0.00780344},"labels":[],"label_agreement":null},{"id":"W2080159644","doi":"10.1029/2007gl029533","title":"The possible role in the ocean heat budget of eddy‐induced mixing due to air‐sea interaction","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Mixing (physics); Eddy; Zonal and meridional; Environmental science; Ocean heat content; Ocean current; Climatology; Atmospheric sciences; Geology; Meteorology; Mechanics; Oceanography; Physics; Turbulence","score_opus":0.02073590650460502,"score_gpt":0.2919874747779829,"score_spread":0.27125156827337793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080159644","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792594,0.0009299941,0.014483766,0.00069325505,0.00010679761,0.000011731195,0.00016978644,0.00012247337,0.0042228396],"genre_scores_gemma":[0.9991411,0.00009034624,0.0004245055,0.000013895696,0.000016586317,0.0000028102552,0.000021274274,0.000009879673,0.00027956016],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992204,0.000019990637,0.0000057695493,0.000019438092,0.000009566956,0.000023292943],"domain_scores_gemma":[0.999788,0.00011448049,0.000030851235,0.000020086538,0.000019882365,0.000026662621],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000255048,0.0004158871,0.00025878838,0.00024766722,0.0003114013,0.000899974,0.0003920369,0.00033230634,0.0027595258],"category_scores_gemma":[0.0008986374,0.00020653685,0.00024394492,0.0002100701,0.00027862992,0.0010535356,0.0006956855,0.00022390128,0.00013657207],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017813642,0.00035415217,0.24943998,0.00065598194,0.00057674793,0.0015340847,0.0007375016,0.11043978,0.4650121,0.079375826,0.0015466852,0.08854582],"study_design_scores_gemma":[0.00022023209,0.00041286074,0.25858796,0.000048552865,0.00033794597,0.0005916417,0.00041162333,0.61858857,0.07499054,0.04173623,0.003984611,0.00008926739],"about_ca_topic_score_codex":0.0009800592,"about_ca_topic_score_gemma":0.0005821297,"teacher_disagreement_score":0.0027595258,"about_ca_system_score_codex":0.00021324227,"about_ca_system_score_gemma":0.00019101851,"threshold_uncertainty_score":0.009231508},"labels":[],"label_agreement":null},{"id":"W2080279668","doi":"10.1029/2000gl000029","title":"Shear AlfvéN waves on stretched magnetic field lines near midnight in Earth's magnetosphere","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Russian Foundation for Basic Research","keywords":"Magnetosphere; Physics; Field line; Magnetic field; Plasma sheet; L-shell; Geophysics; Mercury's magnetic field; Dipole; Computational physics; Earth's magnetic field","score_opus":0.011730265408838118,"score_gpt":0.27078742422576335,"score_spread":0.25905715881692526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080279668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955711,0.00014594362,0.003212887,0.000018963294,0.0000036486026,0.0000018264069,0.000017756627,0.00002218802,0.0010057288],"genre_scores_gemma":[0.9994449,0.00007235884,0.00031696743,0.0000018764392,0.000005153025,0.0000011276768,0.00001972815,0.0000029912724,0.00013482978],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999869,0.0000026271243,5.811876e-7,0.0000030114443,0.000003349764,0.00000358316],"domain_scores_gemma":[0.99991906,0.000019196721,0.00002668583,0.0000072381263,0.000011681626,0.00001612026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000063966305,0.00018927023,0.00009073099,0.0002876406,0.00012630681,0.0002269464,0.00013003392,0.00015013029,0.00035859455],"category_scores_gemma":[0.00024168631,0.00010767518,0.000109288056,0.00015197214,0.0002693348,0.00020311646,0.00016561613,0.00014178171,0.00008789924],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013382419,0.00010373247,0.1641508,0.00021355663,0.000104531304,0.006872307,0.0018589022,0.13579927,0.5625318,0.052404426,0.0021285305,0.07249389],"study_design_scores_gemma":[0.00012412356,0.00033034777,0.35659176,0.0000464754,0.000038275153,0.0018324452,0.0006947256,0.5953782,0.015978735,0.026774675,0.0021686244,0.000041562704],"about_ca_topic_score_codex":0.00046318446,"about_ca_topic_score_gemma":0.00030319966,"teacher_disagreement_score":0.00046318446,"about_ca_system_score_codex":0.00012928851,"about_ca_system_score_gemma":0.00003579385,"threshold_uncertainty_score":0.0011996031},"labels":[],"label_agreement":null},{"id":"W2080388873","doi":"10.1029/2003gl018099","title":"Nonlinearity and multifractality of climate change in the past 420,000 years","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":176,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Multifractal system; Climate change; Proxy (statistics); Series (stratigraphy); Scaling; Ice core; Nonlinear system; Climate model","score_opus":0.05980026816289886,"score_gpt":0.33299652489081977,"score_spread":0.2731962567279209,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080388873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998412,0.000056341232,0.0010217293,0.00008991574,0.0000015766501,0.0000011623416,0.00006136933,0.000012810274,0.00034309906],"genre_scores_gemma":[0.99967563,0.000019354104,0.00016562773,0.000004173461,0.0000035797668,0.0000013108481,0.00006586199,0.0000022449813,0.00006225338],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972326,0.00009168307,0.000017484992,0.00006858224,0.000060666403,0.00003822531],"domain_scores_gemma":[0.99534386,0.002534846,0.0011005085,0.00050101103,0.00038478285,0.00013494896],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006914947,0.000109762215,0.00014972243,0.000676319,0.0002802294,0.00041776197,0.00013875781,0.00023234433,0.0006964848],"category_scores_gemma":[0.0073026535,0.00014129448,0.00020144891,0.00055983954,0.0005745564,0.0007005886,0.00039457862,0.00035957617,0.00013892952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001111809,0.00002746459,0.9493724,0.000022661152,0.00009859038,0.00011941217,0.00041372448,0.024221335,0.00637434,0.0016936944,0.00028104836,0.017264137],"study_design_scores_gemma":[0.0000020474722,0.00002556946,0.93749523,0.0000039082156,0.000014144532,0.00011273278,0.0001018245,0.060002018,0.00041692404,0.0014966712,0.00031833196,0.000010674063],"about_ca_topic_score_codex":0.005474184,"about_ca_topic_score_gemma":0.0067814765,"teacher_disagreement_score":0.005474184,"about_ca_system_score_codex":0.0004674523,"about_ca_system_score_gemma":0.00021939373,"threshold_uncertainty_score":0.010884643},"labels":[],"label_agreement":null},{"id":"W2080830809","doi":"10.1029/2001gl014000","title":"Current disturbance and the diminishing peatland carbon sink","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":296,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Peat; Environmental science; Carbon sink; Boreal; Sink (geography); Carbon cycle; Carbon fibers; Carbon sequestration; Permafrost; Disturbance (geology); Hydrology (agriculture); Physical geography; Atmospheric sciences; Carbon dioxide; Climate change; Ecosystem; Geology; Ecology; Oceanography; Geography; Geomorphology","score_opus":0.02836007268137474,"score_gpt":0.2774943088095362,"score_spread":0.24913423612816143,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080830809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919491,0.00090113125,0.0012866193,0.00093590247,0.000013410953,0.0000015553023,0.00008634325,0.000032936383,0.0047929925],"genre_scores_gemma":[0.9994167,0.00024390769,0.000109622684,0.000024148982,0.0000067137685,3.821621e-7,0.000025339528,0.0000020723523,0.00017110765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993825,0.000008081709,0.000004134596,0.000013138554,0.000013763599,0.000022606802],"domain_scores_gemma":[0.9995977,0.00006186703,0.00017241183,0.000024788395,0.000059218204,0.00008397907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027283555,0.00011347348,0.00012982466,0.00031536384,0.00027377674,0.0008993813,0.00020556887,0.0003543068,0.0016237259],"category_scores_gemma":[0.0008097358,0.00008076552,0.00008400357,0.00020738874,0.0008030568,0.0012533983,0.00036702197,0.0002193682,0.000117830394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045521112,0.00011463027,0.8204893,0.00016567193,0.00011167605,0.001212439,0.0006948107,0.016539397,0.029350841,0.032254968,0.0017883955,0.09682262],"study_design_scores_gemma":[0.000009198732,0.00008862298,0.9549753,0.0000354829,0.000040274394,0.0007846909,0.0013388941,0.011736888,0.001675558,0.021903036,0.0073888,0.000023264925],"about_ca_topic_score_codex":0.007404952,"about_ca_topic_score_gemma":0.016332198,"teacher_disagreement_score":0.007404952,"about_ca_system_score_codex":0.0007646953,"about_ca_system_score_gemma":0.00038482895,"threshold_uncertainty_score":0.014723718},"labels":[],"label_agreement":null},{"id":"W2080851550","doi":"10.1029/2008gl036147","title":"Denitrification effects on air‐sea CO<sub>2</sub> flux in the coastal ocean: Simulations for the northwest North Atlantic","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":210,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Alkalinity; Denitrification; Biogeochemical cycle; Environmental science; Oceanography; Seawater; Flux (metallurgy); Sediment; Biogeochemistry; Particulates; Atmospheric sciences; Environmental chemistry; Nitrogen; Geology; Ecology; Chemistry; Geomorphology","score_opus":0.032234479358860986,"score_gpt":0.28006110021031144,"score_spread":0.24782662085145046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080851550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974016,0.00006454106,0.00045686253,0.00016970237,0.000015426142,0.0000109298235,0.00036072687,0.00004313,0.0014770434],"genre_scores_gemma":[0.99813855,0.00008742308,0.000795043,0.00005319593,0.0000067062374,0.00001907371,0.0003512807,0.000020236526,0.0005285164],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999038,0.000024346042,0.000007571614,0.000018341989,0.000013177591,0.00003259666],"domain_scores_gemma":[0.999514,0.00022637231,0.000056187113,0.000028622924,0.00007274246,0.00010195997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038757382,0.0006197666,0.0004896748,0.00028310358,0.0006687572,0.0007626514,0.00077309494,0.0014901693,0.00133396],"category_scores_gemma":[0.0011586447,0.00041632104,0.0008112052,0.000468362,0.00073006836,0.0004887159,0.00068053976,0.00078850886,0.00010736451],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035439103,0.00018692664,0.030277606,0.00004590263,0.00008564298,0.00021131807,0.000087410954,0.96343,0.0024401671,0.00061318366,0.00045801836,0.0018093309],"study_design_scores_gemma":[0.00018796822,0.000096581476,0.010682427,0.000008871842,0.000039126226,0.000016546102,0.00013976808,0.9874917,0.00076430733,0.00025678542,0.00029897256,0.000016929018],"about_ca_topic_score_codex":0.15864803,"about_ca_topic_score_gemma":0.10450755,"teacher_disagreement_score":0.15864803,"about_ca_system_score_codex":0.0015279622,"about_ca_system_score_gemma":0.0014311812,"threshold_uncertainty_score":0.31544918},"labels":[],"label_agreement":null},{"id":"W2080854033","doi":"10.1029/2000gl012543","title":"Sea surface temperatures in the subarctic northeast Pacific reflect millennial‐scale climate oscillations during the last 16 kyrs","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia","funders":"","keywords":"Younger Dryas; Subarctic climate; Alkenone; Geology; Climatology; Oceanography; Sea surface temperature; Pacific decadal oscillation; Climate change; Northern Hemisphere","score_opus":0.025086089519638994,"score_gpt":0.2878793924879816,"score_spread":0.26279330296834263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2080854033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987446,0.00015933809,0.00006259682,0.00003226362,0.0000036776546,9.82159e-7,0.00053584884,0.000009515405,0.00045117855],"genre_scores_gemma":[0.99844897,0.0003416724,0.00014022949,0.000014551991,0.0000063346474,0.0000028039196,0.00073326356,0.0000042523616,0.0003079283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996734,0.000003456728,0.0000027680553,0.000009756154,0.0000073791157,0.000009345065],"domain_scores_gemma":[0.99980754,0.000018821256,0.00009842373,0.00001329321,0.000035738343,0.000026116179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014119012,0.00014756384,0.000117097305,0.00034523688,0.0001752663,0.00034338495,0.00009751443,0.00009454552,0.0006942804],"category_scores_gemma":[0.0004687915,0.00012303411,0.00007897603,0.00052391476,0.00022645811,0.00026084142,0.000248068,0.00017069968,0.00014292434],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045479686,0.000008214502,0.98994154,0.00002069733,0.00004700461,0.00004655971,0.00024936156,0.0004156474,0.003235078,0.00003869094,0.00024722362,0.0057045887],"study_design_scores_gemma":[6.482807e-7,0.000002487001,0.9994789,0.0000013556969,0.000005290833,0.000016518967,0.000051370112,0.000059141865,0.00009423527,0.000009662639,0.00027967498,7.536521e-7],"about_ca_topic_score_codex":0.028582323,"about_ca_topic_score_gemma":0.071239896,"teacher_disagreement_score":0.028582323,"about_ca_system_score_codex":0.00044858942,"about_ca_system_score_gemma":0.0002830256,"threshold_uncertainty_score":0.056831956},"labels":[],"label_agreement":null},{"id":"W2081045078","doi":"10.1029/2005gl025471","title":"Nonlinear atmospheric teleconnections","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of British Columbia","funders":"","keywords":"Teleconnection; Arctic oscillation; Climatology; Geopotential height; Northern Hemisphere; Environmental science; Oscillation (cell signaling); Atmospheric sciences; Nonlinear system; Precipitation; El Niño Southern Oscillation; Geology; Meteorology; Physics","score_opus":0.02622342518675029,"score_gpt":0.29257701867549296,"score_spread":0.26635359348874266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081045078","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90267843,0.00087323814,0.07512992,0.0007825742,0.00007883699,0.000040656603,0.0011876503,0.00041965366,0.018808931],"genre_scores_gemma":[0.99574286,0.00028317765,0.0023619633,0.000027282438,0.000016624574,0.00001092558,0.00017285247,0.000015747846,0.0013685985],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999889,0.000028220269,0.0000047136923,0.000034292927,0.000025144383,0.000018596298],"domain_scores_gemma":[0.9996094,0.00017772321,0.00009756816,0.000031534986,0.000065355656,0.000018496521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019598728,0.00034200933,0.00011843962,0.00032723346,0.00026823697,0.00052274176,0.00023912509,0.00027755953,0.0020246943],"category_scores_gemma":[0.0019371841,0.00015674632,0.00022265996,0.0005539229,0.0003496242,0.00066045154,0.00047434462,0.00043070878,0.00014225635],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014947225,0.0000328461,0.03822784,0.00008966963,0.00011711062,0.00020082909,0.00016731257,0.8900578,0.007732616,0.020921493,0.0015344996,0.04076855],"study_design_scores_gemma":[0.000010348491,0.000016481516,0.0114969965,0.000006759138,0.000017398474,0.000041691852,0.00002342442,0.97665465,0.00087068183,0.009824843,0.0010251427,0.000011618921],"about_ca_topic_score_codex":0.012094926,"about_ca_topic_score_gemma":0.010153941,"teacher_disagreement_score":0.012094926,"about_ca_system_score_codex":0.00061967684,"about_ca_system_score_gemma":0.00026536384,"threshold_uncertainty_score":0.024049044},"labels":[],"label_agreement":null},{"id":"W2081287593","doi":"10.1029/2000gl012602","title":"The 8.2 kyr BP event simulated by a Global Atmosphere—Sea‐Ice—Ocean Model","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":207,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Thermohaline circulation; Meltwater; Geology; Climatology; Oceanography; Shutdown of thermohaline circulation; Atmosphere (unit); Sea ice; Ocean current; North Atlantic Deep Water; Environmental science; Glacial period; Meteorology; Geomorphology; Geography","score_opus":0.027609436046636904,"score_gpt":0.30892220744756577,"score_spread":0.28131277140092886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2081287593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979214,0.000019314006,0.00064847566,0.00008963241,0.000029813868,0.00002131272,0.00052462454,0.000057774087,0.000687579],"genre_scores_gemma":[0.9987643,0.000021934913,0.00043847662,0.000022163273,0.0000073417846,0.000027887712,0.0005591411,0.000009954924,0.00014883188],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999031,0.000027166689,0.0000051118545,0.0000197355,0.000009434493,0.00003546453],"domain_scores_gemma":[0.99971527,0.00009703109,0.00004216629,0.000029988334,0.000043945343,0.00007154964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003770715,0.00063742755,0.0004571775,0.00023722871,0.0003140141,0.0004302988,0.00063058955,0.00078115164,0.0013049316],"category_scores_gemma":[0.0008771678,0.00027368983,0.00063226494,0.00028869425,0.00047454092,0.00034808353,0.0004466916,0.0009481257,0.00010503431],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002384466,0.00067069987,0.05631329,0.000089177964,0.00031395312,0.00055744464,0.0000895188,0.91386676,0.018049445,0.0019514523,0.001988634,0.0037251902],"study_design_scores_gemma":[0.00054494647,0.00045565516,0.033710077,0.0000091266575,0.00013533779,0.00005049541,0.00007413969,0.9572766,0.006338281,0.00068286713,0.00068634766,0.000036168723],"about_ca_topic_score_codex":0.013662496,"about_ca_topic_score_gemma":0.009645338,"teacher_disagreement_score":0.013662496,"about_ca_system_score_codex":0.00072831206,"about_ca_system_score_gemma":0.00044157016,"threshold_uncertainty_score":0.02716595},"labels":[],"label_agreement":null},{"id":"W2082003487","doi":"10.1029/2004gl021830","title":"Nonlinear electron heating by resonant shear Alfvén waves in the ionosphere","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Ionosphere; Physics; Electron; Ionization; Atomic physics; Plasmasphere; Alfvén wave; Joule heating; Electron density; Magnetosphere; Magnetohydrodynamics; Electron temperature; Dissipation; Amplitude; Geophysics; Computational physics; Plasma; Ion; Optics","score_opus":0.011999863055168591,"score_gpt":0.28905774781639054,"score_spread":0.27705788476122195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082003487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99594915,0.00017470999,0.0017834087,0.000030337496,0.0000033263136,0.0000025411766,0.000010565469,0.000021504959,0.0020243735],"genre_scores_gemma":[0.9994753,0.00009362098,0.00017819066,0.0000028683967,0.0000023829766,0.0000014302368,0.0000065712316,0.0000028549805,0.00023678104],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999763,0.0000043190416,7.80283e-7,0.0000045841634,0.0000052642067,0.000008794836],"domain_scores_gemma":[0.9999448,0.000022525923,0.000014067032,0.0000056570975,0.000006945222,0.000006036738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007025092,0.00019028138,0.00011922419,0.00012889878,0.00019428243,0.00027044668,0.00014345192,0.0001467539,0.00040482133],"category_scores_gemma":[0.0002742653,0.00012074287,0.00015882328,0.00011128828,0.00036391622,0.0002450431,0.0002986356,0.0001062887,0.000095885924],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008777224,0.00009131858,0.07451986,0.00018437696,0.00014022127,0.0018811399,0.00089179154,0.40681553,0.4663119,0.016931618,0.00083138625,0.030523129],"study_design_scores_gemma":[0.00009418372,0.0002475256,0.092779614,0.000015460439,0.00006906102,0.0005467865,0.0004002226,0.857489,0.039355323,0.0075402483,0.0014218654,0.00004075859],"about_ca_topic_score_codex":0.0011457644,"about_ca_topic_score_gemma":0.0006688789,"teacher_disagreement_score":0.0011457644,"about_ca_system_score_codex":0.00023376933,"about_ca_system_score_gemma":0.0000862042,"threshold_uncertainty_score":0.0022782087},"labels":[],"label_agreement":null},{"id":"W2082074032","doi":"10.1029/2005gl023521","title":"The dual source region for the 2004 Sumatra tsunami","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Geology; Seismology; Dual (grammatical number); Oceanography; Climatology","score_opus":0.049511480265275444,"score_gpt":0.2951365846909577,"score_spread":0.24562510442568228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082074032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9603877,0.00033032394,0.0018569783,0.00033204255,0.000031215513,0.00004328913,0.01951758,0.000108478824,0.017392421],"genre_scores_gemma":[0.96391976,0.00031487833,0.0027003337,0.000057747347,0.000018621535,0.00009171315,0.026407223,0.000036550755,0.0064532505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998871,0.000012528415,0.000012203265,0.000031230913,0.000031419182,0.000025468667],"domain_scores_gemma":[0.99939513,0.000063969565,0.00025350545,0.000053920103,0.00016413874,0.00006929754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012745656,0.00021533917,0.00016702534,0.002145298,0.00049765204,0.0006545597,0.00020693583,0.0001828008,0.0060885297],"category_scores_gemma":[0.00081674976,0.0001269148,0.00015220897,0.002017773,0.0001875689,0.00030528253,0.0008558864,0.0003161966,0.0015412515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006370319,0.00016311897,0.76256025,0.00032053492,0.00016026538,0.0021786937,0.004147496,0.0044783005,0.038194247,0.004351447,0.028300444,0.15450822],"study_design_scores_gemma":[0.000014249319,0.000027741191,0.9759976,0.00002516024,0.000040454717,0.00075422437,0.001370575,0.0014933628,0.0015263609,0.0003204353,0.01841574,0.000014024953],"about_ca_topic_score_codex":0.029074006,"about_ca_topic_score_gemma":0.04429636,"teacher_disagreement_score":0.029074006,"about_ca_system_score_codex":0.0011325285,"about_ca_system_score_gemma":0.0008888058,"threshold_uncertainty_score":0.05780959},"labels":[],"label_agreement":null},{"id":"W2082116023","doi":"10.1029/2007gl030212","title":"Impact of the global warming on the fluvial thermal erosion over the Lena River in Central Siberia","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; Polar Knowledge Canada; National Science Foundation","keywords":"Fluvial; Tributary; Geology; Climate change; Global warming; Hydrology (agriculture); Erosion; Arctic; Physical geography; Spring (device); Climatology; Environmental science; Oceanography; Geomorphology; Geography; Structural basin","score_opus":0.05495314187210528,"score_gpt":0.327664672937438,"score_spread":0.27271153106533275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082116023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990796,0.0002343811,0.000022938404,0.00005409485,0.000004936968,0.0000010265917,0.00012054082,0.0000035687656,0.00047889014],"genre_scores_gemma":[0.9994671,0.00017468804,0.000034544075,0.000018826731,0.000006530501,0.000001340306,0.00016960241,0.0000013280303,0.00012608386],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999912,0.000021099937,0.000010150844,0.000019200119,0.000016730934,0.000020877578],"domain_scores_gemma":[0.9998572,0.000023025063,0.00004242075,0.000012803442,0.000028051378,0.000036486133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003011588,0.0002096283,0.00024039453,0.000687552,0.0005189046,0.00069191534,0.00010845286,0.00023487881,0.0010731207],"category_scores_gemma":[0.00034078833,0.000087849796,0.00024365043,0.0005979719,0.0004196285,0.0002808513,0.00062222127,0.00018088955,0.00010594657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002502673,0.00004840229,0.96931946,0.00006287913,0.0001583479,0.0009753406,0.0004846155,0.0046108793,0.0072280597,0.0001406558,0.00031192106,0.016409114],"study_design_scores_gemma":[0.0000021683861,0.000015619677,0.9988243,0.0000049605937,0.000015118637,0.000058151207,0.000160848,0.00047521802,0.00016606213,0.000024711575,0.0002501416,0.0000026058256],"about_ca_topic_score_codex":0.026300587,"about_ca_topic_score_gemma":0.03735295,"teacher_disagreement_score":0.026300587,"about_ca_system_score_codex":0.0008176017,"about_ca_system_score_gemma":0.00038754335,"threshold_uncertainty_score":0.05229497},"labels":[],"label_agreement":null},{"id":"W2082120379","doi":"10.1029/2006gl028462","title":"Evolution of a shoaling internal solitary wavetrain","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; Memorial University of Newfoundland","funders":"","keywords":"Shoaling and schooling; Context (archaeology); Internal wave; Geology; Mixing (physics); Kondratiev wave; Geophysics; Mechanics; Physics; Oceanography; Paleontology","score_opus":0.024065128903147767,"score_gpt":0.28526117750806146,"score_spread":0.2611960486049137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082120379","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981171,0.0000085328975,0.00072221,0.000009130215,0.0000016822072,0.0000031331856,0.000013395793,0.000012198671,0.0011127007],"genre_scores_gemma":[0.9993345,0.0000069694784,0.00030867854,0.0000041126746,0.000001126108,0.000002435822,0.00003734809,0.0000023033238,0.00030249],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999946,0.000003664839,0.0000019810445,0.000009983425,0.000021669566,0.000016624648],"domain_scores_gemma":[0.9996288,0.000065543114,0.000069316106,0.000042778604,0.000084378255,0.00010920732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007616825,0.00011468748,0.0001482634,0.0003512259,0.00028226138,0.00024075693,0.00019862196,0.00019491272,0.0008803278],"category_scores_gemma":[0.00064606784,0.00011068979,0.0000898119,0.00016451768,0.0003753436,0.00014675544,0.00041759375,0.0003598193,0.00011420512],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029098065,0.00016947163,0.09684571,0.00006188651,0.00005048641,0.0018063015,0.0008677241,0.006433979,0.8549181,0.0026597593,0.00054449664,0.035351142],"study_design_scores_gemma":[0.000032145683,0.00083410775,0.8448239,0.000029332406,0.000039815604,0.0018376806,0.00083472964,0.091232486,0.05760992,0.0011514431,0.0015156465,0.00005887744],"about_ca_topic_score_codex":0.0018485792,"about_ca_topic_score_gemma":0.0014491859,"teacher_disagreement_score":0.0018485792,"about_ca_system_score_codex":0.0002540864,"about_ca_system_score_gemma":0.00013562848,"threshold_uncertainty_score":0.0036756396},"labels":[],"label_agreement":null},{"id":"W2082192998","doi":"10.1029/2007gl031839","title":"Coherent whistler waves and oscilliton formation: Kinetic simulations","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Whistler; Physics; Instability; Computational physics; Wave packet; Electron; Phase velocity; Anisotropy; Dispersion relation; Wave propagation; Atomic physics; Optics; Mechanics; Quantum mechanics","score_opus":0.02205872620931369,"score_gpt":0.3047277019527521,"score_spread":0.2826689757434384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082192998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96024853,0.00017942418,0.02117776,0.0003615039,0.000046113655,0.00007757285,0.00078720954,0.000227108,0.016894788],"genre_scores_gemma":[0.9916161,0.000110453126,0.0059083146,0.000044227432,0.000012126606,0.00012572839,0.0003783718,0.00005999348,0.0017446157],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998696,0.000032515007,0.0000050753492,0.000013985985,0.00003448559,0.000044369735],"domain_scores_gemma":[0.9987348,0.0008048385,0.0000986444,0.00007525871,0.00016940237,0.000116981464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035515614,0.0004315126,0.00093952526,0.0004974408,0.00065538177,0.00074620143,0.0013221281,0.0013949669,0.0034141531],"category_scores_gemma":[0.0018663256,0.00036808927,0.0004959979,0.00070422306,0.00078124995,0.0005708696,0.0005764878,0.00088713696,0.0002442207],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007822201,0.000055254408,0.0013478653,0.000039111954,0.0000267304,0.00008848074,0.00006929663,0.9916351,0.00084813044,0.004662176,0.00027001637,0.00087966037],"study_design_scores_gemma":[0.000019444036,0.000010488269,0.00020958204,0.000002419188,0.000003372502,0.000004941082,0.00001681509,0.99890375,0.0001617939,0.0005415374,0.0001220431,0.000003884681],"about_ca_topic_score_codex":0.018550513,"about_ca_topic_score_gemma":0.007113311,"teacher_disagreement_score":0.018550513,"about_ca_system_score_codex":0.00094767904,"about_ca_system_score_gemma":0.0008649523,"threshold_uncertainty_score":0.036885083},"labels":[],"label_agreement":null},{"id":"W2082315312","doi":"10.1029/2003gl018645","title":"The Madden‐Julian Oscillation (MJO) and northern high latitude wintertime surface air temperatures","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Madden–Julian oscillation; Climatology; Geopotential height; Environmental science; Extratropical cyclone; Northern Hemisphere; Advection; Atmospheric sciences; Latitude; Middle latitudes; Geology; Meteorology; Convection; Precipitation; Geography","score_opus":0.018388543197059407,"score_gpt":0.27540078763204806,"score_spread":0.25701224443498866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082315312","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9058812,0.019878816,0.0052729207,0.0026113917,0.00048918417,0.00002390208,0.002968756,0.0001241732,0.06274967],"genre_scores_gemma":[0.9920061,0.0035771779,0.00079041993,0.00009029569,0.0003086206,0.000011591725,0.00069378346,0.000010657635,0.002511238],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990773,0.000019323774,0.0000048471643,0.0000237874,0.000023361663,0.00002087482],"domain_scores_gemma":[0.99974006,0.00004878452,0.00013946675,0.000011570809,0.000024576504,0.000035584224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019703466,0.00017678255,0.00014041636,0.000374534,0.00025840497,0.00092807447,0.0001586589,0.00023314118,0.0014138725],"category_scores_gemma":[0.0015378812,0.000082111954,0.00012787875,0.0009275294,0.00031545706,0.00043892066,0.0005178242,0.0002450688,0.00015107263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039398094,0.000056131274,0.74876237,0.0003612529,0.00026230203,0.0004792592,0.0010835325,0.019643674,0.003116848,0.076704316,0.020275079,0.12886125],"study_design_scores_gemma":[0.000016297436,0.00003652962,0.91608655,0.00008399797,0.000058141984,0.00015804794,0.0003578297,0.011619478,0.0003272841,0.019165153,0.05207303,0.000017639335],"about_ca_topic_score_codex":0.014654777,"about_ca_topic_score_gemma":0.019382777,"teacher_disagreement_score":0.014654777,"about_ca_system_score_codex":0.0005062406,"about_ca_system_score_gemma":0.0004901418,"threshold_uncertainty_score":0.029138982},"labels":[],"label_agreement":null},{"id":"W2082531481","doi":"10.1029/2005gl022468","title":"Initial intercomparison of ozone and nitrogen dioxide number density profiles retrieved by the ACE‐FTS and GOMOS occultation experiments","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Belgian Federal Science Policy Office","keywords":"Occultation; Nitrogen dioxide; Ozone; Atmospheric sciences; Environmental science; Nitrogen; Altitude (triangle); Atmospheric chemistry; Radio occultation; Meteorology; Physics; Ionosphere; Astrophysics; Astronomy","score_opus":0.03509356074080308,"score_gpt":0.32146027367966273,"score_spread":0.2863667129388596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082531481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937243,0.00024287813,0.0019138319,0.000030999996,0.000024358249,0.00003122696,0.0016442493,0.000097718395,0.0022904607],"genre_scores_gemma":[0.9901904,0.00015985455,0.003847226,0.000019887628,0.000009936462,0.000027149095,0.004747393,0.000017640847,0.000980609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996736,0.00004440646,0.000017326152,0.000098894314,0.00011374191,0.000052150284],"domain_scores_gemma":[0.9994216,0.00010960209,0.000045242312,0.00012399757,0.00026033365,0.000039236827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009303174,0.0004446609,0.00038878393,0.0005659938,0.00038314197,0.0005335214,0.00034033702,0.0003478848,0.0006184066],"category_scores_gemma":[0.001292708,0.00015211843,0.00026388362,0.0007945979,0.00015672031,0.0005085107,0.00052852294,0.00027256386,0.00020285054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0058463686,0.0007361503,0.47855353,0.000438292,0.0010163273,0.0007065055,0.0013466,0.07185422,0.2684424,0.0015606784,0.003186519,0.1663123],"study_design_scores_gemma":[0.00009688183,0.00022685944,0.92859715,0.000022006609,0.00017700954,0.000061053965,0.00015575206,0.021101851,0.044134486,0.00025178364,0.005145159,0.000030002773],"about_ca_topic_score_codex":0.027291842,"about_ca_topic_score_gemma":0.029096972,"teacher_disagreement_score":0.027291842,"about_ca_system_score_codex":0.00090245955,"about_ca_system_score_gemma":0.00045198787,"threshold_uncertainty_score":0.054265976},"labels":[],"label_agreement":null},{"id":"W2082597758","doi":"10.1029/2001gl013102","title":"The initiation of orogenic margin reverse faulting","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Lithosphere; Crust; Brittleness; Compression (physics); Petrology; Seismology; Tectonics; Geophysics","score_opus":0.06646318903321433,"score_gpt":0.28886097474338884,"score_spread":0.22239778571017452,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082597758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97901595,0.00045411944,0.0016094412,0.00009148609,0.000022160631,0.000026760257,0.00009721718,0.00010064123,0.018582186],"genre_scores_gemma":[0.9988954,0.000109174674,0.00021966653,0.000014735109,0.0000046495734,0.0000040066384,0.000059745245,0.000005715637,0.0006869622],"study_design_codex":"bench_or_experimental","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9997614,0.00002750883,0.000013658385,0.00004192052,0.000054053355,0.00010136086],"domain_scores_gemma":[0.9996506,0.000046249537,0.000102908845,0.000074471005,0.00007093722,0.000054782802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025052167,0.00022290742,0.00022124608,0.00024039131,0.00042990907,0.0005738657,0.00019462171,0.00032224873,0.0019645044],"category_scores_gemma":[0.0010106633,0.00018239218,0.00021018588,0.00012631307,0.0003867963,0.00038962037,0.00091920374,0.0003773779,0.00069842377],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010263049,0.00010752685,0.19852714,0.0004838524,0.00005505616,0.0042029046,0.0012877879,0.007428199,0.7140375,0.015220786,0.0013203295,0.056302663],"study_design_scores_gemma":[0.00011207871,0.00089878665,0.5501207,0.00014251228,0.00010872223,0.003647836,0.0015500144,0.008323889,0.38854858,0.004641194,0.041833982,0.00007167512],"about_ca_topic_score_codex":0.0016820279,"about_ca_topic_score_gemma":0.0019032619,"teacher_disagreement_score":0.0019645044,"about_ca_system_score_codex":0.0004719527,"about_ca_system_score_gemma":0.00038305362,"threshold_uncertainty_score":0.0065719485},"labels":[],"label_agreement":null},{"id":"W2082598850","doi":"10.1029/2008gl034639","title":"Quantification of subsurface heat storage in a GCM simulation","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"GCM transcription factors; Environmental science; Geology; Meteorology; Climatology; General Circulation Model; Climate change; Physics","score_opus":0.1472560790527569,"score_gpt":0.3452588304833658,"score_spread":0.19800275143060891,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082598850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9876182,0.000055736225,0.007494649,0.0001188757,0.000015632317,0.000017104549,0.0015352201,0.00036731886,0.0027771648],"genre_scores_gemma":[0.99602306,0.000023112452,0.0030959356,0.000016251797,0.0000036542194,0.00001622035,0.00064955413,0.000030989053,0.00014114658],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998567,0.00003452684,0.00000981095,0.000038142865,0.000029688616,0.00003120127],"domain_scores_gemma":[0.9995055,0.00018619889,0.000045929144,0.00010217764,0.00010052649,0.000059717633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033069486,0.00055375,0.00040033887,0.00043344678,0.00032769548,0.00066653016,0.00046445912,0.00076427637,0.0010497665],"category_scores_gemma":[0.0015966365,0.0003110402,0.00037362197,0.0008389513,0.00039719284,0.0007619612,0.0004563646,0.00055074674,0.00011416299],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001465607,0.00006173718,0.028829074,0.00003792669,0.000079019555,0.00006352543,0.000061530154,0.9553366,0.00821658,0.0015884524,0.00046906693,0.005109938],"study_design_scores_gemma":[0.000039798833,0.000029377321,0.009539964,0.000007374545,0.000020416956,0.000008103146,0.000029312843,0.986107,0.0030067635,0.0007318709,0.00046454553,0.000015440388],"about_ca_topic_score_codex":0.03666966,"about_ca_topic_score_gemma":0.017084349,"teacher_disagreement_score":0.03666966,"about_ca_system_score_codex":0.0010264878,"about_ca_system_score_gemma":0.0008292964,"threshold_uncertainty_score":0.072912455},"labels":[],"label_agreement":null},{"id":"W2082647032","doi":"10.1029/2009gl040230","title":"Laboratory simulation of fluid‐driven seismic sequences in shallow crustal conditions","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Induced seismicity; Geology; Seismology; Volcano; Aftershock; Slip (aerodynamics); Pore water pressure; Seismic hazard; Fluid pressure; Limiting; Geotechnical engineering; Mechanics","score_opus":0.03765208673907226,"score_gpt":0.3161034976753258,"score_spread":0.27845141093625353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082647032","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933395,0.000035699526,0.003951521,0.00007972044,0.000014034691,0.000021225993,0.00017533186,0.00009833613,0.0022846074],"genre_scores_gemma":[0.99819726,0.000023401593,0.0013257754,0.000010957191,0.0000027910141,0.00002688164,0.00010813772,0.0000063972366,0.0002986023],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999918,0.0000162769,0.0000054261895,0.000017021886,0.000016175496,0.000026966605],"domain_scores_gemma":[0.99918145,0.00046668868,0.00012529218,0.000053009564,0.00007937971,0.0000941863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025590564,0.0003031797,0.0003523056,0.00025637526,0.0002496623,0.00053661695,0.000739464,0.00073781237,0.0015797106],"category_scores_gemma":[0.0013651964,0.00024567498,0.00035034926,0.00023092159,0.0007003019,0.00043326893,0.0005027427,0.0006462889,0.000094412],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016250489,0.00020452117,0.005958085,0.000029147921,0.000030096786,0.00013762432,0.000055655328,0.9870674,0.0036464208,0.0009346675,0.00018962112,0.0015843287],"study_design_scores_gemma":[0.000037350474,0.000090218804,0.00056783145,0.0000020888185,0.0000065284453,0.0000060625252,0.000020180667,0.99782026,0.0011548216,0.00019426252,0.00009482599,0.0000055674686],"about_ca_topic_score_codex":0.009187146,"about_ca_topic_score_gemma":0.0057536876,"teacher_disagreement_score":0.009187146,"about_ca_system_score_codex":0.0006421179,"about_ca_system_score_gemma":0.0006171645,"threshold_uncertainty_score":0.018267334},"labels":[],"label_agreement":null},{"id":"W2082734245","doi":"10.1029/2009gl039883","title":"Are ocean deserts getting larger?","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":165,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University","funders":"","keywords":"Biome; Climatology; Environmental science; Climate change; Pacific decadal oscillation; Productivity; Spatial distribution; Geography; Oceanography; Physical geography; Sea surface temperature; Geology; Ecosystem; Ecology; Remote sensing","score_opus":0.03259274294089513,"score_gpt":0.275569882182564,"score_spread":0.2429771392416689,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082734245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8043805,0.02528088,0.00046064847,0.111575805,0.001661938,0.000017898274,0.002093177,0.00010486756,0.054424267],"genre_scores_gemma":[0.981093,0.007923703,0.00017368498,0.0064344555,0.00078690046,0.0000081681155,0.0003807278,0.000024286528,0.0031751383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995419,0.000083284336,0.000029504836,0.00011581294,0.00007125732,0.00015820378],"domain_scores_gemma":[0.99799675,0.000212031,0.0007338746,0.000136279,0.00023038474,0.0006906907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071040285,0.000162921,0.00033261825,0.00074737705,0.0010225908,0.002206194,0.0003543747,0.0010157716,0.012255652],"category_scores_gemma":[0.0034771417,0.00016523016,0.00025109103,0.0013448584,0.0024372821,0.002597442,0.0012399441,0.0009866726,0.0007773697],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054901285,0.000078465615,0.6794515,0.0006454554,0.00023260682,0.0027188724,0.013740324,0.0002295481,0.0025052084,0.025281213,0.06647516,0.20809254],"study_design_scores_gemma":[0.00005783818,0.00006885073,0.8058892,0.00029854602,0.00008936812,0.0021428254,0.032486174,0.00006996179,0.0004471309,0.014597373,0.14380676,0.000045902718],"about_ca_topic_score_codex":0.008922433,"about_ca_topic_score_gemma":0.01302873,"teacher_disagreement_score":0.012255652,"about_ca_system_score_codex":0.0009606192,"about_ca_system_score_gemma":0.0007810806,"threshold_uncertainty_score":0.040999174},"labels":[],"label_agreement":null},{"id":"W2082854283","doi":"10.1029/2009gl039778","title":"Deep mantle forces and the uplift of the Colorado Plateau","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":133,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Geology; Upwelling; Mantle (geology); Mantle plume; Magmatism; Canyon; Basin and Range Province; Hotspot (geology); Colorado plateau; Plateau (mathematics); Mantle convection; Transition zone; Structural basin; Geomorphology; Paleontology; Tectonics; Subduction; Geophysics; Oceanography; Lithosphere; Geochemistry","score_opus":0.017239512596728866,"score_gpt":0.2455190522221373,"score_spread":0.22827953962540842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2082854283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98802084,0.00035047153,0.0038542512,0.00056896824,0.0000052885257,0.000004261897,0.00012775358,0.000037389116,0.007030804],"genre_scores_gemma":[0.9989812,0.000079536934,0.00032272018,0.000008865429,0.0000041153203,0.0000026846326,0.000047020687,0.0000047204744,0.0005489617],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.000007067775,0.0000012400824,0.000010961546,0.0000082996,0.000012850972],"domain_scores_gemma":[0.9999068,0.00002202368,0.000023033384,0.000009326729,0.000019578743,0.000019356177],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013008999,0.00013869311,0.00012986144,0.0003320397,0.00062745024,0.0008101792,0.00038517837,0.00034032922,0.001780415],"category_scores_gemma":[0.00043323383,0.00016090044,0.00017907184,0.00025246074,0.0004921652,0.00045388195,0.00052198593,0.00026628713,0.000094703966],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014567378,0.000054521763,0.22351208,0.00005243791,0.000072549854,0.00044418676,0.001190317,0.62680066,0.016676698,0.105789855,0.0017346796,0.023526296],"study_design_scores_gemma":[0.000052370648,0.00006258545,0.17263839,0.00003718884,0.00003158594,0.0001670195,0.00069622335,0.77148116,0.001642302,0.043705083,0.009455616,0.000030386042],"about_ca_topic_score_codex":0.096264005,"about_ca_topic_score_gemma":0.075228356,"teacher_disagreement_score":0.096264005,"about_ca_system_score_codex":0.0015591839,"about_ca_system_score_gemma":0.0006431855,"threshold_uncertainty_score":0.19140738},"labels":[],"label_agreement":null},{"id":"W2083027891","doi":"10.1029/2006gl027910","title":"A climatology of sea ice embayments in the Cosmonaut Sea, Antarctica","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Amorfix (Canada); University of Toronto","funders":"","keywords":"Sea ice; Oceanography; Geology; Antarctic sea ice; Arctic ice pack; Climatology; Ice shelf; Cryosphere","score_opus":0.029722871220382144,"score_gpt":0.3071302462346716,"score_spread":0.27740737501428947,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083027891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963154,0.00030032478,0.000092232185,0.000042800257,0.0000043938653,0.000004396661,0.0020439776,0.00001403284,0.0011824503],"genre_scores_gemma":[0.996469,0.00027208772,0.00024432436,0.0000116321535,0.000010858855,0.000008846593,0.0025157896,0.0000044201865,0.00046297963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999318,0.000010309759,0.00000991877,0.000016646258,0.000016501632,0.000014927203],"domain_scores_gemma":[0.999556,0.000028506904,0.00020876544,0.000019799727,0.00009514335,0.0000917994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001592242,0.00019689213,0.00013104704,0.0016671917,0.00030140698,0.00046742673,0.00009376075,0.00015088519,0.00097398163],"category_scores_gemma":[0.00046314675,0.00007053957,0.00011727979,0.0017188984,0.00018271072,0.00025411957,0.0003020378,0.00012812432,0.0001960843],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009448325,0.000010192946,0.98610514,0.00004354882,0.00006174248,0.00023561968,0.00062484166,0.0006937728,0.003045903,0.00011956463,0.0013379888,0.007627281],"study_design_scores_gemma":[7.6958605e-7,0.000008293896,0.9988673,0.0000031665918,0.0000027406945,0.00006772312,0.00013819811,0.00009240099,0.000039214465,0.000008869559,0.00077021425,0.0000011366859],"about_ca_topic_score_codex":0.019893344,"about_ca_topic_score_gemma":0.056417998,"teacher_disagreement_score":0.019893344,"about_ca_system_score_codex":0.00030613886,"about_ca_system_score_gemma":0.00021476012,"threshold_uncertainty_score":0.039555132},"labels":[],"label_agreement":null},{"id":"W2083028953","doi":"10.1029/2006gl026385","title":"Vertical seismoelectric profiling in a borehole penetrating glaciofluvial sediments","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Geology; Borehole; Amplitude; Lithology; Vertical seismic profile; Permeability (electromagnetism); Porosity; Petrophysics; Seismology; Mineralogy; Petrology; Geotechnical engineering; Geophysics","score_opus":0.031078950541352044,"score_gpt":0.30410011140607246,"score_spread":0.2730211608647204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083028953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909663,0.000020104642,0.0006154808,0.000006379522,0.0000012592178,0.0000016785704,0.000029030725,0.000016827384,0.00021256263],"genre_scores_gemma":[0.99937004,0.000018454019,0.00045690298,0.0000047110484,0.0000015253095,0.0000012081182,0.000028816126,0.0000011615125,0.000117282034],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999542,0.000004388215,0.0000016470754,0.000011043024,0.000017998149,0.000010639151],"domain_scores_gemma":[0.9998672,0.000030542593,0.00003723606,0.000007653064,0.00003078117,0.000026628191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006375772,0.0001693565,0.00007947193,0.00037509104,0.00009416035,0.00016786213,0.00012558707,0.00015585881,0.00040953312],"category_scores_gemma":[0.00034663774,0.00010302585,0.000044806777,0.00021372407,0.00016864343,0.00020280665,0.00022488524,0.00009089197,0.000041663636],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025983888,0.000027765618,0.016768577,0.000023318422,0.0000059355375,0.00024683232,0.00016201219,0.00039490178,0.9719348,0.00006419918,0.000031742613,0.0100801075],"study_design_scores_gemma":[0.000046390967,0.0014177756,0.73607314,0.000016289172,0.000046928497,0.0013667383,0.00048292,0.006713779,0.2526718,0.00023441749,0.00089598785,0.00003382948],"about_ca_topic_score_codex":0.0010672351,"about_ca_topic_score_gemma":0.0018559166,"teacher_disagreement_score":0.0010672351,"about_ca_system_score_codex":0.00010426005,"about_ca_system_score_gemma":0.0000665343,"threshold_uncertainty_score":0.0021220446},"labels":[],"label_agreement":null},{"id":"W2083285955","doi":"10.1002/2014gl062051","title":"Seasonal variability of the warm Atlantic water layer in the vicinity of the Greenland shelf break","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Natural Environment Research Council; Sight Research UK; Pinngortitaleriffik; Society for Marine Mammalogy","keywords":"Argo; Oceanography; Advection; Geology; Climatology; Seasonality; Water mass; Groenlandia; Structural basin; Glacier; Ice sheet","score_opus":0.03394497127345603,"score_gpt":0.2642573228417327,"score_spread":0.23031235156827667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083285955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99869174,0.00006159846,0.000022789673,0.000040033185,0.0000060616603,0.0000023158593,0.0006006315,0.0000063971715,0.0005685239],"genre_scores_gemma":[0.9988399,0.000039063492,0.000043263473,0.000024313576,0.000005351017,0.0000025169613,0.0007437439,0.0000026656382,0.0002990671],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.0000042835113,0.0000030253514,0.000014240473,0.000009438175,0.000015363563],"domain_scores_gemma":[0.9997744,0.000022437618,0.000082368686,0.000012924467,0.00004429943,0.00006350408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014640937,0.00011204334,0.00013034415,0.00056028896,0.00024502046,0.0004762736,0.00017091515,0.00021233941,0.00096940185],"category_scores_gemma":[0.00029061546,0.00006451821,0.00012265482,0.0005701891,0.00022450367,0.00020981906,0.00029621765,0.00017309595,0.00019363698],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011160801,0.000021513979,0.9900152,0.000012459021,0.00005100551,0.00014228154,0.00025403016,0.00028464195,0.004598587,0.0000653682,0.0007890424,0.0036542073],"study_design_scores_gemma":[8.4020354e-7,0.000004367488,0.99962485,0.0000018298429,0.000002405609,0.000006962746,0.00006894494,0.00008043416,0.000041903724,0.000004458971,0.00016219275,7.536759e-7],"about_ca_topic_score_codex":0.078287005,"about_ca_topic_score_gemma":0.19782244,"teacher_disagreement_score":0.078287005,"about_ca_system_score_codex":0.00069492107,"about_ca_system_score_gemma":0.0003095805,"threshold_uncertainty_score":0.15566266},"labels":[],"label_agreement":null},{"id":"W2083421060","doi":"10.1029/2004gl020143","title":"How islands stir and fertilize the upper ocean","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Isopycnal; Geology; Upwelling; Shoal; Oceanography; Ridge; Wake; Crest; Internal wave; Atmospheric sciences; Physics; Mechanics; Paleontology","score_opus":0.021463980498885794,"score_gpt":0.25188709446938246,"score_spread":0.23042311397049667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083421060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8854799,0.0011009842,0.00086724944,0.0013006019,0.00008662405,0.000014149406,0.0001083961,0.0000664361,0.11097556],"genre_scores_gemma":[0.9930627,0.00048711465,0.0003830361,0.00016732147,0.000017783485,0.0000042085235,0.000037298207,0.000027597396,0.005812927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998746,0.000026336236,0.0000043174246,0.000020876538,0.000021368594,0.000052567615],"domain_scores_gemma":[0.99984086,0.000030372332,0.00003168592,0.000018986268,0.00002937203,0.00004870502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018684953,0.000130172,0.00015614337,0.00045814956,0.0008409026,0.0017887121,0.0002231043,0.00041514853,0.006901204],"category_scores_gemma":[0.0010923544,0.00019665236,0.00013104691,0.0003876511,0.0010514365,0.0008746318,0.0009091816,0.00026565522,0.001181691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006686441,0.000086250875,0.45241284,0.000764756,0.0004364107,0.0037596545,0.023099178,0.012127995,0.064899065,0.08973944,0.019711994,0.33229378],"study_design_scores_gemma":[0.000051216826,0.00012781385,0.7239468,0.00024272695,0.00018757682,0.0007873508,0.034041125,0.004330498,0.004992149,0.03758073,0.1936153,0.00009657148],"about_ca_topic_score_codex":0.024935916,"about_ca_topic_score_gemma":0.077323385,"teacher_disagreement_score":0.024935916,"about_ca_system_score_codex":0.0007133346,"about_ca_system_score_gemma":0.00069248595,"threshold_uncertainty_score":0.049581528},"labels":[],"label_agreement":null},{"id":"W2083488206","doi":"10.1029/1999gl010421","title":"A new fiber optic gradiometer for 4‐D absolute differential gravity","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Gravimetry; Interferometry; Gradiometer; Geodesy; Differential (mechanical device); Gravitational field; Optics; Geology; Physics; Remote sensing; Magnetic field; Classical mechanics","score_opus":0.05456684158720352,"score_gpt":0.29486119565186153,"score_spread":0.24029435406465802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083488206","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17545597,0.003226939,0.7887988,0.0013716341,0.0020124372,0.00039449416,0.0018316442,0.0053258818,0.0215821],"genre_scores_gemma":[0.40842482,0.0008842137,0.58023375,0.00047116572,0.00037852043,0.0002297538,0.0010857547,0.00016377444,0.008128244],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99962354,0.000044928554,0.000013258065,0.000063690255,0.00022046005,0.000034088273],"domain_scores_gemma":[0.9997559,0.000030518288,0.000031821946,0.000040276187,0.000109454784,0.000032016338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029545501,0.0005681436,0.00036744346,0.00084393204,0.00047471875,0.0005209064,0.0008827527,0.0005542699,0.0021550744],"category_scores_gemma":[0.0005097762,0.00026881223,0.00022230165,0.00079993263,0.00042491336,0.0012347815,0.00068108866,0.00048703866,0.0008486531],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051845785,0.00013599824,0.009230654,0.00040108163,0.000087653454,0.00033198172,0.00029813498,0.0048965137,0.4435591,0.01889346,0.012941187,0.5087058],"study_design_scores_gemma":[0.00028013095,0.0016011486,0.029194437,0.0001334897,0.0003078455,0.0039607533,0.00022812297,0.20014672,0.3158241,0.013128638,0.43470228,0.00049234496],"about_ca_topic_score_codex":0.0017421427,"about_ca_topic_score_gemma":0.0036860122,"teacher_disagreement_score":0.0021550744,"about_ca_system_score_codex":0.00047189827,"about_ca_system_score_gemma":0.00072615634,"threshold_uncertainty_score":0.00720942},"labels":[],"label_agreement":null},{"id":"W2083929945","doi":"10.1029/2006gl027275","title":"Trapping zones: The effect of fracture roughness on the directional anisotropy of fluid flow and colloid transport in a single fracture","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":167,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Fracture (geology); Surface finish; Materials science; Anisotropy; Surface roughness; Colloid; Flow (mathematics); Fluid dynamics; Phase (matter); Mechanics; Composite material; Geology; Optics; Chemistry","score_opus":0.011555915878185481,"score_gpt":0.24819462729731107,"score_spread":0.2366387114191256,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2083929945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99233043,0.000068699876,0.007273592,0.00001518598,0.0000022436823,0.000007679078,0.00002398306,0.000038542796,0.00023959161],"genre_scores_gemma":[0.9980762,0.00003383492,0.0017668364,0.000003097395,9.756615e-7,0.0000042281895,0.00001838345,0.000007706243,0.0000887504],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998374,0.000011135979,0.000008145912,0.00004421907,0.000047598023,0.000051503],"domain_scores_gemma":[0.99927217,0.0003428032,0.00017542118,0.000077931436,0.00007395329,0.000057649446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002881525,0.00027842302,0.00032462986,0.0003007927,0.00039055658,0.00069224444,0.00025094525,0.00030743488,0.00041192328],"category_scores_gemma":[0.0009813337,0.00026641513,0.00033147482,0.00012108172,0.00054465566,0.00036559682,0.00038020065,0.00034671972,0.00007218093],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024580455,0.00007065774,0.010976622,0.00006223357,0.000044525303,0.00025636033,0.00013791803,0.08232732,0.8976006,0.00095473154,0.000058698737,0.0072645335],"study_design_scores_gemma":[0.000059026155,0.0006197335,0.044646606,0.000016959923,0.00010460196,0.0004058478,0.00025819358,0.4581824,0.49405015,0.0009357205,0.00061053457,0.00011029021],"about_ca_topic_score_codex":0.0042942897,"about_ca_topic_score_gemma":0.0031380604,"teacher_disagreement_score":0.0042942897,"about_ca_system_score_codex":0.0005970289,"about_ca_system_score_gemma":0.0004648341,"threshold_uncertainty_score":0.008538544},"labels":[],"label_agreement":null},{"id":"W2084131940","doi":"10.1029/2005gl023047","title":"Simulation of the last glacial inception with the green McGill Paleoclimate Model","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Paleoclimatology; Geology; Ice sheet; Glacial period; Climatology; Milankovitch cycles; Ice age; Physical geography; Paleontology; Oceanography; Climate change; Geography","score_opus":0.038312103149873176,"score_gpt":0.2933567577185646,"score_spread":0.25504465456869146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084131940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93397534,0.0004598002,0.011344229,0.0016737509,0.00024331213,0.00012667161,0.012716527,0.0009774902,0.038482986],"genre_scores_gemma":[0.9876533,0.000104038176,0.005300975,0.00019049463,0.000026499301,0.000079122794,0.003511473,0.00011664097,0.0030175198],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998066,0.000046169356,0.000005475914,0.000035024448,0.00003111063,0.00007569806],"domain_scores_gemma":[0.99948287,0.0001187121,0.000042496406,0.00003713527,0.000110600464,0.00020815874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040577198,0.00056663423,0.0005789012,0.00040717833,0.000682865,0.0010021238,0.00228026,0.0011303175,0.005310215],"category_scores_gemma":[0.0014785813,0.000385718,0.0005103204,0.00083672313,0.00068652467,0.00048046024,0.0007927064,0.0010574753,0.00040733773],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027956706,0.000074904725,0.00858644,0.000034498604,0.000082865416,0.0001400677,0.00006413623,0.97614574,0.0018092291,0.0044017765,0.005246451,0.0031344146],"study_design_scores_gemma":[0.00015880085,0.000029054048,0.0041964604,0.0000072044168,0.000026555448,0.000008775081,0.000027572878,0.9923981,0.0003953365,0.00088675576,0.001839666,0.000025780064],"about_ca_topic_score_codex":0.38488618,"about_ca_topic_score_gemma":0.29378,"teacher_disagreement_score":0.38488618,"about_ca_system_score_codex":0.0032404605,"about_ca_system_score_gemma":0.0038149378,"threshold_uncertainty_score":0.7652918},"labels":[],"label_agreement":null},{"id":"W2084328953","doi":"10.1029/2006gl027977","title":"Origin of pingo‐like features on the Beaufort Sea shelf and their possible relationship to decomposing methane gas hydrates","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":140,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Natural Resources Canada","funders":"David and Lucile Packard Foundation; National Science Foundation","keywords":"Clathrate hydrate; Permafrost; Methane; Geology; Beaufort sea; Arctic; Oceanography; Submarine pipeline; Continental shelf; Seafloor spreading; Sediment; Hydrate; Environmental science; Geomorphology","score_opus":0.03686702365355038,"score_gpt":0.3139314032251678,"score_spread":0.27706437957161745,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084328953","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941325,0.00006143656,0.00006831328,0.000015759506,0.0000013756496,0.0000018727238,0.000028870627,0.0000031813117,0.00040594657],"genre_scores_gemma":[0.99957293,0.000040393395,0.00013921212,0.0000051034312,0.0000026241594,0.0000011776709,0.00005440868,7.690083e-7,0.00018334408],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999434,0.00000462283,0.0000018570165,0.0000134367965,0.000010342692,0.000026236665],"domain_scores_gemma":[0.99982005,0.000020263158,0.000079517835,0.000014269996,0.000028466126,0.000037468868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009256596,0.00015360779,0.00011986255,0.00054443843,0.00051339687,0.00039658503,0.00021645654,0.00026637322,0.0006197051],"category_scores_gemma":[0.00023460308,0.00016665533,0.00014319063,0.00038099452,0.00051112,0.00024484412,0.00025611752,0.00016456711,0.00009522984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018066194,0.000026663472,0.8967749,0.000027476459,0.000020275314,0.0028075078,0.0012700111,0.00029022543,0.08678711,0.00034917862,0.00012111406,0.011344877],"study_design_scores_gemma":[0.000001287716,0.000043090575,0.99600524,0.000002301771,0.000004072004,0.000648494,0.0005342082,0.00025939176,0.0020154445,0.000041798008,0.0004399944,0.000004660977],"about_ca_topic_score_codex":0.015622398,"about_ca_topic_score_gemma":0.021961397,"teacher_disagreement_score":0.015622398,"about_ca_system_score_codex":0.00024061832,"about_ca_system_score_gemma":0.00016641332,"threshold_uncertainty_score":0.03106296},"labels":[],"label_agreement":null},{"id":"W2084387349","doi":"10.1029/2004gl020025","title":"Deliquescence and crystallization of ammonium sulfate‐glutaric acid and sodium chloride‐glutaric acid particles","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Glutaric acid; Crystallization; Ammonium sulfate; Relative humidity; Mole fraction; Sodium; Chemistry; Inorganic chemistry; Sulfate; Ammonium chloride; Atmosphere (unit); Aerosol; Ammonium; Organic chemistry; Meteorology; Physical chemistry","score_opus":0.02365191439786409,"score_gpt":0.25765439783424493,"score_spread":0.23400248343638083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084387349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99204004,0.00092804397,0.004802652,0.000019447467,0.000014816202,0.00002490754,0.00028992025,0.00004732186,0.0018329091],"genre_scores_gemma":[0.9928429,0.00040179564,0.0042547206,0.000019361349,0.000008475319,0.000021633614,0.00046861998,0.000039285726,0.0019431604],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997948,0.00001696217,0.000012559448,0.0000413533,0.00009632892,0.00003810226],"domain_scores_gemma":[0.99973446,0.000088060304,0.00006619988,0.000023722523,0.000053524163,0.000034120618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027471018,0.00026766318,0.00016817662,0.00029658587,0.0001779924,0.00023888904,0.00017909387,0.00013782972,0.00070521166],"category_scores_gemma":[0.0003229463,0.00015184656,0.0002860637,0.00018323165,0.00021819753,0.00021560832,0.0002570231,0.00028501396,0.00011628546],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040090054,0.0000070674323,0.0016369725,0.00003182913,0.00001696631,0.00004442129,0.00004175044,0.00030231892,0.9965411,0.00007381055,0.000021458476,0.001242253],"study_design_scores_gemma":[0.000004218476,0.00006170782,0.013104336,0.0000019359584,0.000012044524,0.00009140669,0.0000375482,0.0014946301,0.98446184,0.000038366412,0.0006840612,0.0000078494595],"about_ca_topic_score_codex":0.003500435,"about_ca_topic_score_gemma":0.0041547124,"teacher_disagreement_score":0.003500435,"about_ca_system_score_codex":0.0003872042,"about_ca_system_score_gemma":0.00017756355,"threshold_uncertainty_score":0.006960094},"labels":[],"label_agreement":null},{"id":"W2084407436","doi":"10.1029/2008gl034187","title":"A late Quaternary climate reconstruction based on borehole heat flux data, borehole temperature data, and the instrumental record","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"I-Hub Foundation for Cobotics","keywords":"Borehole; Holocene; Geology; Quaternary; Heat flux; Flux (metallurgy); Glacial period; Climatology; Physical geography; Oceanography; Paleontology; Geography; Heat transfer","score_opus":0.04853258444230315,"score_gpt":0.2910967096791948,"score_spread":0.24256412523689166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084407436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93187237,0.0009223952,0.019206472,0.00042969754,0.00013819187,0.000039974424,0.03133973,0.0007233123,0.015327855],"genre_scores_gemma":[0.94146496,0.00050813745,0.02013658,0.000076282064,0.000053446347,0.000026243553,0.034312703,0.000101895675,0.0033198097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998946,0.00002020606,0.000010498223,0.000029194927,0.000029777051,0.000015628708],"domain_scores_gemma":[0.99950564,0.000033974302,0.00011942019,0.00009231035,0.00021495184,0.000033722583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035750447,0.00022394507,0.00015722023,0.0013433773,0.00028221027,0.00074974576,0.0001871664,0.00022005574,0.002309115],"category_scores_gemma":[0.0013352749,0.0002139628,0.00019298117,0.001345722,0.00019165101,0.00047408883,0.00026021124,0.00030556967,0.0006715968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006710019,0.00044483948,0.65963244,0.00023904942,0.00031711988,0.00039344237,0.0016361189,0.06655445,0.032945853,0.016980171,0.027333127,0.1928524],"study_design_scores_gemma":[0.00011185747,0.00012316732,0.8415399,0.00008779057,0.00015063742,0.0004522471,0.00036228413,0.06882933,0.006237862,0.0023138947,0.07972149,0.00006953759],"about_ca_topic_score_codex":0.019690394,"about_ca_topic_score_gemma":0.039291758,"teacher_disagreement_score":0.019690394,"about_ca_system_score_codex":0.0006066961,"about_ca_system_score_gemma":0.00079888257,"threshold_uncertainty_score":0.03915155},"labels":[],"label_agreement":null},{"id":"W2084414366","doi":"10.1029/2004gl020869","title":"Spatial relationship of equatorial plasma bubbles and field‐aligned irregularities observed with an all‐sky airglow imager and the Equatorial Atmosphere Radar","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Alberta Agricultural Research Institute; National Science Foundation","keywords":"Airglow; Atmosphere (unit); Backscatter (email); F region; Radar; Sky; Atmospheric sciences; Geology; Ionosphere; Remote sensing; Geophysics; Physics; Astronomy; Meteorology","score_opus":0.022163518070249497,"score_gpt":0.263943220804656,"score_spread":0.2417797027344065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084414366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923515,0.000064587846,0.00030839568,0.0000065348104,0.0000011662726,0.0000017070367,0.000056626526,0.000009648314,0.00031624097],"genre_scores_gemma":[0.99903107,0.00005030241,0.00058510684,0.000007028004,0.0000057179295,0.0000029434054,0.00019166096,0.0000050262,0.00012121567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992144,0.000007863301,0.0000037946847,0.000019325586,0.00002357413,0.000023937057],"domain_scores_gemma":[0.99966025,0.000050958985,0.0001381528,0.000016919274,0.000070931346,0.00006285541],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014317615,0.00014298105,0.00015253603,0.0006155587,0.00013690835,0.0002447356,0.000114464485,0.00017124598,0.00043991063],"category_scores_gemma":[0.0002966331,0.00016432405,0.00008006692,0.0002962202,0.00018196346,0.000257141,0.00035283866,0.00016332386,0.00009877468],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036919478,0.00003891192,0.72540534,0.000050608516,0.00008717648,0.0006130663,0.0007088432,0.00035027007,0.2590092,0.00008828125,0.00019505751,0.013084095],"study_design_scores_gemma":[0.0000055933815,0.000041717853,0.99337596,0.0000026993507,0.000018484892,0.000374118,0.00013513635,0.0006625699,0.0050965203,0.000018944791,0.00026320244,0.0000050143244],"about_ca_topic_score_codex":0.0017958422,"about_ca_topic_score_gemma":0.0033924377,"teacher_disagreement_score":0.0017958422,"about_ca_system_score_codex":0.000076590484,"about_ca_system_score_gemma":0.000074330695,"threshold_uncertainty_score":0.0035707355},"labels":[],"label_agreement":null},{"id":"W2084548800","doi":"10.1029/2005gl023974","title":"Array measurements of deep tremor signals in the Cascadia subduction zone","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Istituto Nazionale di Geofisica e Vulcanologia","keywords":"Slowness; Seismometer; Geology; Seismology; Azimuth; Subduction; Transverse plane; Seismic wave; Seismic array; Geodesy; Geophysics; Optics; Physics; Tectonics","score_opus":0.07824455294584534,"score_gpt":0.30410472088375584,"score_spread":0.2258601679379105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084548800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998475,0.000026454123,0.000529003,0.000020520094,0.0000018397524,0.0000044386197,0.00027007973,0.000020757308,0.0006519843],"genre_scores_gemma":[0.9983553,0.000031129766,0.00079096085,0.000006312543,0.0000035469302,0.000008114027,0.00047866188,0.0000041032686,0.00032184116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998349,0.000016925813,0.0000115865605,0.00006278192,0.000049245537,0.000024631423],"domain_scores_gemma":[0.99957234,0.00005628704,0.00008847193,0.00004498834,0.00013666258,0.0001012903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016045109,0.00024433158,0.00018810872,0.0007054503,0.00028490505,0.00022797327,0.00017339297,0.00018136915,0.0004894508],"category_scores_gemma":[0.0007995847,0.00018336938,0.00011021288,0.00081970356,0.00017721459,0.00014453345,0.00041120723,0.00021254113,0.00016030014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057557767,0.00007521283,0.66639405,0.00007775747,0.00011287759,0.00030191278,0.0021478927,0.004802642,0.29016423,0.00014841017,0.0006214606,0.03457791],"study_design_scores_gemma":[0.000014060874,0.000079511585,0.99477506,0.000003422545,0.000021488826,0.000062460924,0.00015727628,0.0016222683,0.0027590084,0.000039597646,0.00045733247,0.000008366525],"about_ca_topic_score_codex":0.019705582,"about_ca_topic_score_gemma":0.04498278,"teacher_disagreement_score":0.019705582,"about_ca_system_score_codex":0.00039368795,"about_ca_system_score_gemma":0.0002559249,"threshold_uncertainty_score":0.03918177},"labels":[],"label_agreement":null},{"id":"W2084657419","doi":"10.1029/2003gl019011","title":"Avoiding mineral alteration during microwave magnetization","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Mineral; Matrix (chemical analysis); Microwave; Magnetization; Materials science; Condensed matter physics; Absorption (acoustics); Nuclear magnetic resonance; Mineralogy; Magnetic field; Chemistry; Physics; Composite material; Metallurgy","score_opus":0.017377802138856455,"score_gpt":0.27870290464940095,"score_spread":0.26132510251054447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084657419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9623221,0.0014468106,0.029921582,0.00030876728,0.00011602085,0.000052555577,0.00006488139,0.00027110125,0.0054962835],"genre_scores_gemma":[0.9864073,0.00040799277,0.010617915,0.00007371808,0.000033939774,0.000028151822,0.000081190876,0.00006891776,0.0022808306],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99981457,0.000025242793,0.00001109739,0.00004239557,0.00006726816,0.000039480175],"domain_scores_gemma":[0.9997024,0.000083707346,0.0000617068,0.000063918,0.00006743918,0.000020742073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025395487,0.00019994882,0.0002539459,0.00014696144,0.00029456732,0.00028992747,0.0003022611,0.00031072513,0.0011006104],"category_scores_gemma":[0.00082839676,0.00016639095,0.00012180352,0.00010221853,0.0003984656,0.00042617152,0.00033862947,0.00045084214,0.0005117979],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008277273,0.000010092758,0.0005588942,0.000068627676,0.0000042376582,0.00004668687,0.000049293576,0.000082961524,0.9937808,0.00030974852,0.0000731786,0.0049327016],"study_design_scores_gemma":[0.000008239371,0.000119317614,0.0020281565,0.0000053474546,0.0000069770826,0.000173549,0.000030663174,0.00040410925,0.993274,0.00019273467,0.0037535254,0.000003261251],"about_ca_topic_score_codex":0.00025406916,"about_ca_topic_score_gemma":0.000794342,"teacher_disagreement_score":0.0011006104,"about_ca_system_score_codex":0.00014237143,"about_ca_system_score_gemma":0.0001669572,"threshold_uncertainty_score":0.0036818981},"labels":[],"label_agreement":null},{"id":"W2084661440","doi":"10.1029/1999gl008451","title":"Under the volcano: A new dimension in Ar‐Ar dating of volcanic ash","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Sanidine; Plagioclase; Geology; Volcano; Geochemistry; Radiometric dating; Quartz; Volcanic ash; Magma; Mineralogy; Paleontology","score_opus":0.03391126116742702,"score_gpt":0.27035111928245875,"score_spread":0.23643985811503174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084661440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.862924,0.03345549,0.06517382,0.0011841899,0.00022117453,0.000028973678,0.0009805751,0.0006118203,0.035419963],"genre_scores_gemma":[0.9468589,0.0056188055,0.042830426,0.00020932505,0.00020587939,0.000015385553,0.00048023261,0.00014138984,0.0036395853],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9992912,0.00016126761,0.000069652604,0.00024596072,0.00016652237,0.00006535728],"domain_scores_gemma":[0.99843484,0.0006632655,0.00010013182,0.0005545387,0.00019895974,0.000048267513],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020977606,0.0003916113,0.0006795083,0.0018000329,0.00041263326,0.0019637705,0.0007980023,0.0005020155,0.0017221884],"category_scores_gemma":[0.0018168681,0.00035453268,0.0003691308,0.0015799626,0.0012528336,0.0033031618,0.0009190294,0.00093808654,0.00041677468],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007010734,0.000107008585,0.19462037,0.0005921296,0.00043858582,0.0005820234,0.003024961,0.002092731,0.46609128,0.022048224,0.0012515791,0.30844995],"study_design_scores_gemma":[0.00010081759,0.0013406741,0.6743652,0.00033761613,0.0008065641,0.005749829,0.002758106,0.016319975,0.09334334,0.025926149,0.17865798,0.000293661],"about_ca_topic_score_codex":0.0015677589,"about_ca_topic_score_gemma":0.005955629,"teacher_disagreement_score":0.0020977606,"about_ca_system_score_codex":0.0002607862,"about_ca_system_score_gemma":0.0001948817,"threshold_uncertainty_score":0.011094153},"labels":[],"label_agreement":null},{"id":"W2084731508","doi":"10.1029/2005gl025164","title":"Isotopic constraints on non‐photochemical sulfate production in the Arctic winter","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Sulfate; Ozone; Arctic; Ozone depletion; Environmental chemistry; Sulfate aerosol; Aerosol; Atmospheric sciences; Oxygen; Environmental science; Photochemistry; Chemistry; Oceanography; Geology","score_opus":0.022172334598652196,"score_gpt":0.266382157689061,"score_spread":0.24420982309040878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084731508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988838,0.00014023678,0.00012877825,0.00001172683,0.0000024846436,0.0000016098586,0.00018364134,0.000005758542,0.0006419412],"genre_scores_gemma":[0.9985513,0.00021279986,0.00023637158,0.000011883691,0.0000030099156,0.0000031850707,0.0006633068,0.000007184194,0.00031089425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998702,0.000012419036,0.0000075020216,0.000025261055,0.000043595355,0.000040955136],"domain_scores_gemma":[0.9997478,0.000048835453,0.00003445598,0.000020029189,0.00010031552,0.0000484825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032451816,0.00040880602,0.00028913908,0.00061948964,0.00069501647,0.0006780635,0.00032077744,0.00019972723,0.0007797353],"category_scores_gemma":[0.00039712168,0.00024508237,0.00018866447,0.0003881991,0.00034370247,0.00023907518,0.00032812287,0.00011945065,0.00015935772],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015023352,0.00007995978,0.53054667,0.0000993116,0.0001040999,0.00031192583,0.0005711103,0.003732347,0.44960967,0.000935171,0.00024891994,0.012258512],"study_design_scores_gemma":[0.00002667845,0.00011478117,0.9466537,0.000016167924,0.000061924875,0.00012975822,0.0004778152,0.0062654563,0.043406967,0.0005654562,0.0022613741,0.000019922385],"about_ca_topic_score_codex":0.15843347,"about_ca_topic_score_gemma":0.28874463,"teacher_disagreement_score":0.15843347,"about_ca_system_score_codex":0.0017521289,"about_ca_system_score_gemma":0.00113574,"threshold_uncertainty_score":0.3150226},"labels":[],"label_agreement":null},{"id":"W2084929824","doi":"10.1029/2005gl025345","title":"Amplification of the mesospheric diurnal tide in a doubled CO<sub>2</sub> atmosphere","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University; University of Toronto","funders":"","keywords":"Thermosphere; Mesosphere; Atmospheric sciences; Atmosphere (unit); Troposphere; Atmospheric model; Environmental science; Atmospheric tide; Stratosphere; Tidal heating; Water vapor; Radiative transfer; Climatology; Ionosphere; Geology; Meteorology; Physics; Geophysics; Astronomy","score_opus":0.01190194991941641,"score_gpt":0.2649086439885493,"score_spread":0.2530066940691329,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2084929824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981047,0.000043232663,0.00032120667,0.00009036483,0.000010727124,0.0000034702707,0.0001083457,0.000051749877,0.0012662759],"genre_scores_gemma":[0.9996642,0.000025710124,0.000097834774,0.000008997817,0.000002260262,0.0000012709646,0.0000434961,0.000005790626,0.00015036101],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990475,0.000010200669,0.0000029657374,0.000019420466,0.000024206967,0.000038491344],"domain_scores_gemma":[0.9997167,0.00009657738,0.000034778303,0.000028165616,0.000053115815,0.00007057024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014589763,0.00045174302,0.00023518603,0.00013083615,0.00044103508,0.0005509048,0.000336521,0.00041467213,0.0014003502],"category_scores_gemma":[0.00080221164,0.00032522398,0.00040133507,0.00018786603,0.00046224165,0.00032548828,0.0004638479,0.00044601745,0.00012595742],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026602268,0.0002134625,0.17375337,0.00023205962,0.00039029482,0.0028139574,0.0005563573,0.35127625,0.44131133,0.0039703227,0.0024827512,0.020339672],"study_design_scores_gemma":[0.00029127637,0.00042475935,0.47185823,0.000013351027,0.0002452164,0.0002849867,0.00043608723,0.4885821,0.034783393,0.0012786281,0.0017118846,0.00009001855],"about_ca_topic_score_codex":0.07986504,"about_ca_topic_score_gemma":0.06420956,"teacher_disagreement_score":0.07986504,"about_ca_system_score_codex":0.0015866463,"about_ca_system_score_gemma":0.000615234,"threshold_uncertainty_score":0.15880036},"labels":[],"label_agreement":null},{"id":"W2085086480","doi":"10.1029/2007gl032164","title":"First radar measurements of ionospheric electric fields at sub‐second temporal resolution","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Substorm; Ionosphere; Radar; Doppler effect; Geophysics; Electric field; Remote sensing; Temporal resolution; Geology; Doppler radar; Magnetometer; Magnetosphere; Physics; Geodesy; Magnetic field; Optics","score_opus":0.031570823635491525,"score_gpt":0.2649062748391877,"score_spread":0.2333354512036962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085086480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.73105204,0.0059500397,0.23279239,0.000437393,0.0005987112,0.00025740216,0.0024148365,0.0010901709,0.025406975],"genre_scores_gemma":[0.8746364,0.0016058581,0.11464437,0.0002063372,0.0002661936,0.00013336953,0.0014537511,0.000060019327,0.006993778],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99981827,0.000020858348,0.000008690733,0.000037067075,0.00008484156,0.000030278637],"domain_scores_gemma":[0.99940693,0.00012463109,0.000069561356,0.00009985979,0.0002594089,0.000039599046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005522957,0.00026958348,0.00023519501,0.00058412354,0.00013601896,0.00038619115,0.00026369022,0.00037465218,0.0014351542],"category_scores_gemma":[0.0009905277,0.00017188904,0.00012389282,0.00040370776,0.0001554797,0.00047279877,0.00043989954,0.0005837863,0.0004109986],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039002916,0.00009041139,0.021634573,0.00029404802,0.00009767061,0.00026147213,0.00041072894,0.0015173692,0.76797205,0.003080492,0.0026077721,0.20164342],"study_design_scores_gemma":[0.00018363894,0.0011632679,0.28735247,0.00013445478,0.00032745005,0.0033645108,0.00035214153,0.029009761,0.57290834,0.0027593262,0.10227239,0.00017225767],"about_ca_topic_score_codex":0.00063694775,"about_ca_topic_score_gemma":0.0016204487,"teacher_disagreement_score":0.0014351542,"about_ca_system_score_codex":0.00015954,"about_ca_system_score_gemma":0.00019181646,"threshold_uncertainty_score":0.0048010945},"labels":[],"label_agreement":null},{"id":"W2085191604","doi":"10.1029/2006gl027001","title":"Influence of present day and glacial surface conditions on the Antarctic Oscillation/Southern Annular Mode","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Glacial period; Climatology; Baroclinity; Geology; Antarctic oscillation; Mode (computer interface); Atmospheric circulation; Atmospheric sciences; Oscillation (cell signaling); Environmental science; El Niño Southern Oscillation; Geomorphology","score_opus":0.02449264665825474,"score_gpt":0.2953908162418336,"score_spread":0.2708981695835789,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085191604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99751914,0.000053217245,0.000620008,0.000080000995,0.000015619797,0.0000032705636,0.00016214368,0.000027264929,0.0015194813],"genre_scores_gemma":[0.9996088,0.000029987257,0.0001342935,0.000012374936,0.0000039430493,0.0000020033845,0.000085554144,0.000011756256,0.00011135042],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999089,0.000034962224,0.0000054875113,0.000019673304,0.000008480754,0.000022487038],"domain_scores_gemma":[0.9996486,0.00015574081,0.000040772815,0.000032718723,0.000032614113,0.00008958355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063076173,0.0002798292,0.00034512236,0.00028609534,0.00049573765,0.0011340092,0.0003670134,0.00045076825,0.001413231],"category_scores_gemma":[0.001962927,0.0002798799,0.00053019007,0.00023489472,0.0005829417,0.00058656215,0.0005158964,0.0005807534,0.00012940864],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00069900247,0.00015525457,0.1620555,0.000064042455,0.0003400325,0.0003191519,0.00025429754,0.81381154,0.010447926,0.005135078,0.0011091011,0.00560916],"study_design_scores_gemma":[0.00012297959,0.00011814658,0.09158448,0.000015287224,0.00011290441,0.000062332896,0.0001308829,0.9045302,0.0011587621,0.0014973069,0.00061787217,0.000048794853],"about_ca_topic_score_codex":0.017437255,"about_ca_topic_score_gemma":0.019048858,"teacher_disagreement_score":0.017437255,"about_ca_system_score_codex":0.0005935175,"about_ca_system_score_gemma":0.000623105,"threshold_uncertainty_score":0.034671485},"labels":[],"label_agreement":null},{"id":"W2085271110","doi":"10.1029/2000gl011390","title":"The influence of a ductile crustal zone on glacial isostatic adjustment: Geodetic observables along the U.S. East Coast","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Post-glacial rebound; Geology; Lithosphere; Geodetic datum; Tide gauge; Glacial period; Sea level; Residual; East coast; Seismology; Geodesy; Oceanography; Geomorphology; Tectonics","score_opus":0.03786069061862198,"score_gpt":0.2667161495340047,"score_spread":0.2288554589153827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085271110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99922276,0.000035698373,0.000115212024,0.00007030663,0.0000034676139,0.00000128227,0.000090645335,0.00001060401,0.00045008177],"genre_scores_gemma":[0.99971074,0.000027979571,0.00006388909,0.000011486396,0.000002136559,7.399259e-7,0.00011423282,0.0000051804013,0.0000635545],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998228,0.000060928443,0.0000120664845,0.00005047187,0.000021249401,0.000032575652],"domain_scores_gemma":[0.999395,0.00021928607,0.00013880822,0.00006142676,0.000081862956,0.000103609294],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054332934,0.00043932104,0.00026676562,0.00029878283,0.0003315156,0.0010189824,0.0003369085,0.0005148297,0.0008166715],"category_scores_gemma":[0.001973453,0.00036963617,0.00038917697,0.0003236197,0.0006191688,0.00044894964,0.00064557017,0.00043888236,0.00010740834],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032257874,0.00006493183,0.6446963,0.000024059285,0.00018949722,0.0003357045,0.00014634694,0.3435407,0.0052572177,0.0008871178,0.00048222812,0.004053388],"study_design_scores_gemma":[0.000056759454,0.00013511317,0.62566906,0.000021644677,0.0000918805,0.000054410248,0.0002080549,0.37006542,0.0024749946,0.0005248213,0.0006578479,0.000039967574],"about_ca_topic_score_codex":0.09719617,"about_ca_topic_score_gemma":0.07411472,"teacher_disagreement_score":0.09719617,"about_ca_system_score_codex":0.0008270867,"about_ca_system_score_gemma":0.000642028,"threshold_uncertainty_score":0.19326085},"labels":[],"label_agreement":null},{"id":"W2085599725","doi":"10.1029/2004gl021495","title":"Tropical Pacific link to the two dominant patterns of atmospheric variability","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Extratropical cyclone; Climatology; Walker circulation; Atmospheric circulation; Environmental science; Tropical cyclone; Convection; Atmospheric sciences; Sea surface temperature; General Circulation Model; Boreal; Geology; Climate change; Oceanography; Meteorology; Geography","score_opus":0.027430127804671543,"score_gpt":0.3053134634824445,"score_spread":0.27788333567777296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2085599725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9795075,0.00059701287,0.002061644,0.00037767712,0.00003200214,0.0000106587,0.0018098392,0.00007414335,0.015529491],"genre_scores_gemma":[0.998304,0.00019809327,0.00040572885,0.000028532382,0.000013181161,0.00000600754,0.0003868248,0.000007685475,0.00064992876],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999441,0.0000069857842,0.0000029148728,0.000017947095,0.000012724309,0.000015320764],"domain_scores_gemma":[0.9997004,0.00004884488,0.00011030597,0.000023140161,0.00007762275,0.000039666545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011348418,0.00015200664,0.0000743156,0.00044097393,0.0001767716,0.0007601724,0.00010452694,0.000101333906,0.0019756162],"category_scores_gemma":[0.00079603476,0.0000993063,0.0001248125,0.00084079325,0.00014947365,0.00023493616,0.00046674596,0.0002425707,0.00013397995],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022442645,0.000052928965,0.89646584,0.00013137452,0.00016822234,0.0003669252,0.0006244362,0.008538886,0.011251558,0.0078212125,0.003809492,0.070544705],"study_design_scores_gemma":[0.000017320064,0.00002961522,0.97700197,0.000032103264,0.000093090144,0.00029669175,0.00023178587,0.010802075,0.0015786367,0.0031596469,0.006743052,0.0000141341225],"about_ca_topic_score_codex":0.012977354,"about_ca_topic_score_gemma":0.012707115,"teacher_disagreement_score":0.012977354,"about_ca_system_score_codex":0.000296574,"about_ca_system_score_gemma":0.0004892722,"threshold_uncertainty_score":0.025803626},"labels":[],"label_agreement":null},{"id":"W2086083843","doi":"10.1029/2006gl028468","title":"Direct polymerization of isoprene and <i>α</i>‐pinene on acidic aerosols","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Isoprene; Pinene; Aerosol; Polymerization; Polymer; Chemistry; Mass spectrometry; Relative humidity; Organic chemistry; Copolymer; Chromatography; Meteorology","score_opus":0.022541496949269633,"score_gpt":0.2750261475713598,"score_spread":0.25248465062209013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086083843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99522024,0.0006218708,0.0018895605,0.000011091745,0.000011208512,0.000021511773,0.00006451775,0.000014831443,0.0021451276],"genre_scores_gemma":[0.9958401,0.00063707615,0.0015472553,0.000014832601,0.000014397297,0.0000098706305,0.00009723436,0.0000074072705,0.0018318954],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99988127,0.000015832113,0.0000037696375,0.000033383654,0.00003366272,0.00003205959],"domain_scores_gemma":[0.9998653,0.000049213133,0.000028099506,0.000012071969,0.000017833388,0.0000273375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001348362,0.00036873936,0.0001575851,0.0001366393,0.00015198765,0.00016632702,0.00013788229,0.00015098363,0.00087580015],"category_scores_gemma":[0.00021557933,0.000109726214,0.00028625358,0.00006573075,0.00018911184,0.00022296245,0.00018598035,0.00031667502,0.00025121745],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053925847,0.000009144416,0.00028725463,0.00002783457,0.0000054783964,0.00003529882,0.00001831918,0.00009914831,0.99793494,0.00003210618,0.000009452695,0.001487207],"study_design_scores_gemma":[0.0000053850163,0.00022752979,0.0029420222,0.0000021575374,0.000007557972,0.00004982333,0.0000073920783,0.00045132716,0.99583554,0.000019031406,0.0004498024,0.0000024519059],"about_ca_topic_score_codex":0.00080640055,"about_ca_topic_score_gemma":0.00086679915,"teacher_disagreement_score":0.00087580015,"about_ca_system_score_codex":0.00016404915,"about_ca_system_score_gemma":0.000094262854,"threshold_uncertainty_score":0.0029298663},"labels":[],"label_agreement":null},{"id":"W2086155586","doi":"10.1002/2014gl062300","title":"Ten years of Martian nitric oxide nightglow observations","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Belgian Federal Science Policy Office; European Space Agency","keywords":"Airglow; Martian; Occultation; Atmospheric sciences; Brightness; Atmosphere (unit); Atmosphere of Mars; Mars Exploration Program; Radio occultation; Longitude; Latitude; Altitude (triangle); Environmental science; Scale height; Physics; Astrobiology; Astronomy; Ionosphere; Meteorology","score_opus":0.09173942854676433,"score_gpt":0.3089111175864062,"score_spread":0.2171716890396419,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086155586","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996488,0.00038326008,0.0005241348,0.000036593206,0.000016461434,0.00000952881,0.0012607416,0.000027097074,0.0012541886],"genre_scores_gemma":[0.9963779,0.00011285185,0.0002727367,0.000022685388,0.000019864976,0.000006749899,0.002695297,0.0000031774441,0.00048880395],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997886,0.00002989031,0.00001528285,0.00006557297,0.000045025674,0.000055617635],"domain_scores_gemma":[0.9993193,0.00011944428,0.00017942769,0.000076516546,0.00017155318,0.00013376425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006544829,0.00030147968,0.00026969428,0.0009870271,0.0003746988,0.00040372508,0.00029276288,0.00031647552,0.0005565847],"category_scores_gemma":[0.00057864824,0.00011189611,0.00023831439,0.00048273167,0.0001794958,0.00030840776,0.0005702627,0.00018559842,0.00017875044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031435175,0.0001498375,0.96374786,0.000053647695,0.00017789437,0.00042689295,0.00037874526,0.0012721682,0.006969594,0.0001232726,0.00068695314,0.025698725],"study_design_scores_gemma":[0.0000059632725,0.00013869964,0.9925728,0.000014389061,0.00004149869,0.0001478438,0.00012648864,0.0012115407,0.0017816037,0.000045143683,0.003905719,0.000008270188],"about_ca_topic_score_codex":0.0063928016,"about_ca_topic_score_gemma":0.0114830015,"teacher_disagreement_score":0.0063928016,"about_ca_system_score_codex":0.00032125856,"about_ca_system_score_gemma":0.0001703436,"threshold_uncertainty_score":0.012711167},"labels":[],"label_agreement":null},{"id":"W2086421485","doi":"10.1029/2003gl017221","title":"The carbon kinetic isotope effects of ozone‐alkene reactions in the gas‐phase and the impact of ozone reactions on the stable carbon isotope ratios of alkenes in the atmosphere","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Alkene; Isoprene; Chemistry; Cyclohexene; Propene; Ozone; Kinetic isotope effect; Isotope fractionation; Photochemistry; Isotopes of carbon; Carbon fibers; Organic chemistry; Fractionation; Catalysis; Total organic carbon; Materials science; Deuterium","score_opus":0.01892172823195887,"score_gpt":0.28231831310908934,"score_spread":0.26339658487713047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086421485","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99294865,0.0016686057,0.003365633,0.000027860293,0.000020649744,0.000015694523,0.0005550494,0.00004690799,0.0013509407],"genre_scores_gemma":[0.99541473,0.00091198797,0.0020800233,0.000018109944,0.00000645307,0.00001842036,0.000549412,0.000038142727,0.0009627287],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997054,0.000032689397,0.000012940755,0.00008156446,0.00010632118,0.00006103224],"domain_scores_gemma":[0.9997607,0.000107259555,0.0000375226,0.000017916069,0.0000546825,0.000021919639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033379995,0.00064179185,0.00032694064,0.00050320127,0.0002923771,0.00042425684,0.00033231522,0.00037828053,0.001131655],"category_scores_gemma":[0.00047729939,0.0003151775,0.0004993822,0.00034704062,0.00030856597,0.0004096963,0.00024838044,0.00062795694,0.00024700104],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021470201,0.000012688184,0.0025688687,0.000054771546,0.000023849909,0.00004992469,0.000031192387,0.00023253288,0.9948502,0.00006901252,0.000022913233,0.0018693133],"study_design_scores_gemma":[0.000005711819,0.000099145,0.012802291,0.0000039597912,0.000021569258,0.000060016457,0.000027303151,0.001105367,0.9853233,0.000040385014,0.0005014539,0.000009355112],"about_ca_topic_score_codex":0.0030253918,"about_ca_topic_score_gemma":0.0033513103,"teacher_disagreement_score":0.0030253918,"about_ca_system_score_codex":0.000488895,"about_ca_system_score_gemma":0.00027698427,"threshold_uncertainty_score":0.006015539},"labels":[],"label_agreement":null},{"id":"W2086768243","doi":"10.1029/2006gl027669","title":"Climate impacts of systematic errors in the simulation of the path of the North Atlantic Current","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Current (fluid); Climatology; Thermohaline circulation; Environmental science; Gulf Stream; North Atlantic Deep Water; Ocean current; Temperature salinity diagrams; Climate model; Sea surface temperature; Geology; Oceanography; Climate change; Salinity","score_opus":0.044375047418062,"score_gpt":0.32005543111206197,"score_spread":0.27568038369399994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086768243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968651,0.000033584518,0.0023865441,0.000058500143,0.000024251416,0.000009970079,0.00009283831,0.000048250306,0.00048087808],"genre_scores_gemma":[0.9983677,0.000025911826,0.0014037463,0.000017967215,0.000004022293,0.000011693953,0.00007078244,0.000011895326,0.00008624986],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994055,0.0002862876,0.0000577143,0.000083292434,0.00009511415,0.00007218506],"domain_scores_gemma":[0.99634933,0.002121007,0.00058605673,0.00049466395,0.00031627997,0.00013266808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012668311,0.0003790079,0.00020556437,0.0001758646,0.00033364914,0.0005214787,0.00030515887,0.00036609382,0.0003781913],"category_scores_gemma":[0.007871116,0.00028074955,0.0003323922,0.00036518264,0.00044223195,0.00040378261,0.00049367937,0.0005941225,0.000055812652],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012673078,0.00031867938,0.06704075,0.000080950704,0.0002322578,0.00009034873,0.00016815997,0.897412,0.021355404,0.0017448298,0.00030491885,0.009984456],"study_design_scores_gemma":[0.0005403157,0.0011519163,0.06029861,0.000026539707,0.00021919851,0.000044676188,0.00014530506,0.9012601,0.032957792,0.002162431,0.0011267269,0.00006636746],"about_ca_topic_score_codex":0.01509125,"about_ca_topic_score_gemma":0.016260374,"teacher_disagreement_score":0.01509125,"about_ca_system_score_codex":0.0006223183,"about_ca_system_score_gemma":0.0009892946,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W2086769994","doi":"10.1029/2006gl028337","title":"Anomalous uplift of the Apennines and subsidence of the Adriatic: The result of active mantle flow?","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Foundation","keywords":"Geology; Mantle (geology); Crust; Ocean surface topography; Residual; Transition zone; Geophysics; Seismic tomography; Seismology; Geodesy","score_opus":0.021821857532218082,"score_gpt":0.2712608261371332,"score_spread":0.24943896860491513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086769994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993131,0.000033215754,0.0001730976,0.00003834733,0.0000011507375,8.6305437e-7,0.000025154213,0.000005186075,0.0004098023],"genre_scores_gemma":[0.99978906,0.000021530344,0.00010232181,0.0000033966649,0.0000017218631,3.7502414e-7,0.000017966542,0.0000012547039,0.000062397274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999707,0.0000064431897,0.0000023623734,0.000009012926,0.0000036529223,0.000007800677],"domain_scores_gemma":[0.9999281,0.000018957271,0.00002563185,0.000010745513,0.000008180299,0.000008374393],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013223955,0.0001756094,0.00014080868,0.0002735075,0.00013203341,0.00057850295,0.00019202837,0.00020019452,0.0006398753],"category_scores_gemma":[0.0004147478,0.000107433436,0.00019012288,0.00026281903,0.00031885505,0.00030355976,0.00025087016,0.00011677216,0.000094349816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027107782,0.00004462016,0.8952219,0.0000717139,0.00020355001,0.0019678713,0.00056804396,0.032479495,0.04150892,0.002179276,0.00017583073,0.02530761],"study_design_scores_gemma":[0.000028994826,0.000064784894,0.9197805,0.0000087387,0.000053327665,0.00034607595,0.00035857054,0.075155295,0.0024397785,0.0010155072,0.0007352224,0.000013255482],"about_ca_topic_score_codex":0.008269529,"about_ca_topic_score_gemma":0.007730247,"teacher_disagreement_score":0.008269529,"about_ca_system_score_codex":0.00035245626,"about_ca_system_score_gemma":0.00015409043,"threshold_uncertainty_score":0.016442776},"labels":[],"label_agreement":null},{"id":"W2086788202","doi":"10.1029/2002gl016049","title":"Conditions for ferromagnetic resonance in nanoparticles and microwave magnetization","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Ferromagnetic resonance; Magnetization; Microwave; Condensed matter physics; Ferromagnetism; Materials science; Resonance (particle physics); Nanoparticle; Nuclear magnetic resonance; Physics; Nanotechnology; Atomic physics; Magnetic field; Quantum mechanics","score_opus":0.029646328584465424,"score_gpt":0.2918621272020474,"score_spread":0.262215798617582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086788202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7566933,0.0126340045,0.08031802,0.006940192,0.0018052385,0.00049889315,0.00097245676,0.0012910202,0.13884687],"genre_scores_gemma":[0.98022413,0.00080511963,0.008187903,0.00047147812,0.00019344533,0.00017872693,0.00042226448,0.00011219433,0.009404813],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99962986,0.00006232727,0.000018367871,0.000120021694,0.00011142341,0.000057977402],"domain_scores_gemma":[0.99966574,0.00014045852,0.00006984643,0.0000356984,0.00005353259,0.00003474106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003151048,0.00023294009,0.0002873624,0.00029265098,0.00069037796,0.00053088006,0.00045275906,0.00068856444,0.0051392554],"category_scores_gemma":[0.0010097562,0.00026451185,0.0001314914,0.00010728867,0.0010064265,0.0007513601,0.00066433556,0.0008858893,0.0016172734],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031862926,0.00006832478,0.0012071915,0.0005657917,0.000012315565,0.001496529,0.00064399693,0.00046291808,0.9419303,0.0409917,0.0047872486,0.0075150696],"study_design_scores_gemma":[0.0000797767,0.00038039702,0.0055358894,0.00011313345,0.000016459853,0.001910627,0.0006217052,0.0034934888,0.8975279,0.02899599,0.06126976,0.000054848755],"about_ca_topic_score_codex":0.0006847209,"about_ca_topic_score_gemma":0.0012860935,"teacher_disagreement_score":0.0051392554,"about_ca_system_score_codex":0.00048833544,"about_ca_system_score_gemma":0.00020110422,"threshold_uncertainty_score":0.017192543},"labels":[],"label_agreement":null},{"id":"W2086830267","doi":"10.1002/2014gl059826","title":"Numerical investigation of internal wave‐induced sediment motion: Resuspension versus entrainment","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Entrainment (biomusicology); Mechanics; Dimensionless quantity; Bubble; Boundary layer; Sediment transport; Geology; Bursting; Sediment; Instability; Internal wave; Physics; Geomorphology","score_opus":0.06852599477925084,"score_gpt":0.289366176541214,"score_spread":0.22084018176196316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2086830267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98888373,0.00006823209,0.0062897387,0.0002296197,0.000023200719,0.000027032456,0.00014299282,0.00010281429,0.0042326385],"genre_scores_gemma":[0.99739444,0.000034989866,0.0019962958,0.00002032104,0.0000050581043,0.000017393215,0.00007503832,0.000015002784,0.00044133878],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999012,0.000021647444,0.000007419568,0.000014983282,0.000023766677,0.00003101492],"domain_scores_gemma":[0.9989236,0.00053645467,0.0001877191,0.00007563315,0.00013359616,0.0001429645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002971562,0.00045627303,0.000523586,0.00046103573,0.00064429385,0.0007811718,0.00076147343,0.0010416658,0.0016059461],"category_scores_gemma":[0.0021453225,0.0003046464,0.0003918553,0.0005141407,0.0012242566,0.00054209994,0.000645985,0.0008801286,0.0001172098],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009145597,0.00013466305,0.0056746,0.000034574827,0.000029770825,0.00016977316,0.00007984321,0.9854585,0.0042001177,0.002432655,0.00017768607,0.0015162963],"study_design_scores_gemma":[0.000016355301,0.00003274411,0.00061483536,0.0000026143189,0.0000051033853,0.000007168499,0.000019027873,0.99865013,0.00041770586,0.00017806885,0.000051474726,0.000004746089],"about_ca_topic_score_codex":0.017692124,"about_ca_topic_score_gemma":0.008345291,"teacher_disagreement_score":0.017692124,"about_ca_system_score_codex":0.0008636692,"about_ca_system_score_gemma":0.000739054,"threshold_uncertainty_score":0.035178304},"labels":[],"label_agreement":null},{"id":"W2087047233","doi":"10.1029/2006gl026881","title":"Uptake and sequestration of atmospheric CO<sub>2</sub> in the Labrador Sea deep convection region","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Convection; Deep convection; Oceanography; Mixed layer; Atmospheric sciences; Sink (geography); Deep sea; Geology; Climatology; Meteorology; Geography","score_opus":0.021360805405741243,"score_gpt":0.26115279677292424,"score_spread":0.239791991367183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087047233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99976534,0.000019986988,0.000030589585,0.00000815466,3.027562e-7,3.8501207e-7,0.000049335744,0.000005486561,0.00012041553],"genre_scores_gemma":[0.9997454,0.000019337798,0.00004586142,0.000004431131,3.611722e-7,0.0000012570683,0.00007405827,0.0000024509168,0.00010681838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.000009190511,0.0000028278505,0.000014452569,0.000006290336,0.000020873276],"domain_scores_gemma":[0.99993694,0.000010722942,0.000022445845,0.0000065937884,0.00001139111,0.000011888225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000091337526,0.00020871249,0.00017974037,0.00020474124,0.00018838458,0.0003937007,0.0002063416,0.00019955114,0.00050510495],"category_scores_gemma":[0.00021595375,0.00017682908,0.0001908512,0.0002038977,0.00018751615,0.00026430562,0.00028182523,0.00015514695,0.00015308126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070661725,0.000082938386,0.6442467,0.00006387869,0.00014101031,0.00030871708,0.0003830615,0.01159848,0.32676697,0.00027169305,0.00039894422,0.015030881],"study_design_scores_gemma":[0.000014645723,0.000109477216,0.97064096,0.000004945457,0.00003236606,0.000058258134,0.00027463757,0.009361623,0.018897027,0.00005229028,0.0005408438,0.000012908927],"about_ca_topic_score_codex":0.052456934,"about_ca_topic_score_gemma":0.03688525,"teacher_disagreement_score":0.9475431,"about_ca_system_score_codex":0.0007300374,"about_ca_system_score_gemma":0.00025845107,"threshold_uncertainty_score":0.10430324},"labels":[],"label_agreement":null},{"id":"W2087296195","doi":"10.1029/2001gl014583","title":"Multiple auroral brightenings and associated Pi 2 pulsations","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency","keywords":"Substorm; Physics; Magnetic field; Astrophysics; Alfvén wave; Wave packet; Latitude; Magnetosphere; Luminosity; Magnetic reconnection; Geophysics; Magnetohydrodynamics; Astronomy; Atomic physics","score_opus":0.02324457011945075,"score_gpt":0.27093463899759235,"score_spread":0.2476900688781416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087296195","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907035,0.000045105247,0.00008328412,0.0000069442654,0.0000018382565,0.0000020970895,0.00011685817,0.000006938023,0.00066673436],"genre_scores_gemma":[0.9993167,0.000043327407,0.00008815069,0.0000040926047,0.000006865369,0.000002948158,0.00024653252,0.0000021153792,0.00028922912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992096,0.000007528757,0.0000073438973,0.000022359003,0.000015373567,0.000026433352],"domain_scores_gemma":[0.9993736,0.000100170546,0.00029618051,0.000053014905,0.000059577957,0.000117530355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012720656,0.00013648433,0.00016884712,0.001011076,0.00030723622,0.00035846687,0.00010310222,0.00013854812,0.0016788673],"category_scores_gemma":[0.000682207,0.00013247506,0.0000962945,0.00045988528,0.00028002297,0.00024761126,0.0005734264,0.00024063163,0.00013858604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039083837,0.000030839103,0.96254504,0.000029373938,0.000038538252,0.00048857176,0.00035522121,0.00030767024,0.024019213,0.000113763876,0.00014752765,0.011533312],"study_design_scores_gemma":[0.0000023897164,0.000021930096,0.9991222,0.0000012783585,0.0000050387534,0.00022184403,0.000039594786,0.00006397308,0.00036592,0.000023676746,0.00013053758,0.0000016157652],"about_ca_topic_score_codex":0.0021327164,"about_ca_topic_score_gemma":0.0050393376,"teacher_disagreement_score":0.0021327164,"about_ca_system_score_codex":0.0002029949,"about_ca_system_score_gemma":0.00009429575,"threshold_uncertainty_score":0.0056163073},"labels":[],"label_agreement":null},{"id":"W2087383254","doi":"10.1029/2002gl016663","title":"Cold halocline in the northern California Current: An invasion of subarctic water","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Office of Naval Research; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Halocline; Subarctic climate; Current (fluid); Oceanography; Geology; Downwelling; Spring (device); Submarine pipeline; Thermocline; Salinity; Upwelling","score_opus":0.03626028904872378,"score_gpt":0.2793574398666912,"score_spread":0.24309715081796743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087383254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99962056,0.000029456041,0.000006359984,0.000021133817,7.9355317e-7,0.000001252894,0.000021488811,0.0000012605319,0.0002975128],"genre_scores_gemma":[0.9994703,0.00008702814,0.00003295337,0.000018109935,0.000002325101,0.0000024575463,0.00007316549,8.6456095e-7,0.00031273457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.000004496254,0.0000023049904,0.000009622326,0.000011923009,0.000017900878],"domain_scores_gemma":[0.99978083,0.000014836736,0.000077140365,0.0000070592573,0.000032552547,0.000087592314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012117008,0.0001139873,0.00010086634,0.00034096072,0.00057891,0.00045089674,0.00015267309,0.0001745237,0.0009699839],"category_scores_gemma":[0.00028008624,0.00013411416,0.000080869715,0.00030247294,0.00038249278,0.00019403953,0.00037104165,0.00023961694,0.000059844704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021880613,0.00007752215,0.98704314,0.000019712714,0.000029679111,0.00029943354,0.0006466682,0.00026255834,0.00479929,0.00015259566,0.0004136232,0.006036977],"study_design_scores_gemma":[0.000005458733,0.000012453657,0.99926025,0.0000023281134,0.0000050282833,0.000037520742,0.00024595266,0.00008604932,0.0000884551,0.0000156727,0.00023916793,0.0000015669749],"about_ca_topic_score_codex":0.21308622,"about_ca_topic_score_gemma":0.47886387,"teacher_disagreement_score":0.21308622,"about_ca_system_score_codex":0.001387742,"about_ca_system_score_gemma":0.0006980664,"threshold_uncertainty_score":0.4236918},"labels":[],"label_agreement":null},{"id":"W2087401943","doi":"10.1029/2006gl028901","title":"Simulation of ozone loss in Arctic winter 2004/2005","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; European Centre for Medium-Range Weather Forecasts","keywords":"Stratosphere; Ozone; Polar vortex; Ozone depletion; Atmospheric sciences; Ozone layer; Environmental science; Vortex; Arctic; Total Ozone Mapping Spectrometer; Climatology; Mixing ratio; Polar; Meteorology; Geology; Physics; Oceanography","score_opus":0.029635375029236813,"score_gpt":0.3110993481935148,"score_spread":0.281463973164278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087401943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929744,0.00009175071,0.0013835836,0.0002755283,0.00004426804,0.00002836066,0.00103262,0.00012908617,0.004040402],"genre_scores_gemma":[0.99648786,0.00005420993,0.0015104498,0.000080743754,0.000009326201,0.000037856906,0.0010027705,0.000020617863,0.0007961151],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998266,0.00004286042,0.0000075277167,0.00002594207,0.000027368058,0.00006972455],"domain_scores_gemma":[0.9995766,0.0001379238,0.000051848194,0.000024578605,0.00010785315,0.000101160025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046130453,0.00077809306,0.0007744498,0.00043601447,0.0008175705,0.0008730348,0.00096628047,0.0013244491,0.0015577044],"category_scores_gemma":[0.0011706806,0.0003968961,0.0008932716,0.000526597,0.0006406698,0.0003998152,0.00057611516,0.00087680307,0.00015257487],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029613636,0.00016167726,0.010153079,0.000021402922,0.000082461374,0.00012690206,0.000047441274,0.9855322,0.0010945173,0.00064261234,0.000765732,0.001075735],"study_design_scores_gemma":[0.00013085821,0.000101299214,0.004087842,0.000006901918,0.000034938865,0.000013801948,0.00008237288,0.9941215,0.0007035453,0.0002234253,0.0004798341,0.000013633658],"about_ca_topic_score_codex":0.1240949,"about_ca_topic_score_gemma":0.053731102,"teacher_disagreement_score":0.1240949,"about_ca_system_score_codex":0.002005218,"about_ca_system_score_gemma":0.0014973155,"threshold_uncertainty_score":0.24674517},"labels":[],"label_agreement":null},{"id":"W2087533294","doi":"10.1029/2007gl032889","title":"Reply to comment by K. Gajewski on “Abrupt environmental change in Canada's northernmost lake”","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Canadian Obesity Network; University of Toronto; Université Laval","funders":"","keywords":"Interpretation (philosophy); Geology; History; Philosophy","score_opus":0.038560730791107445,"score_gpt":0.2639716605765136,"score_spread":0.22541092978540617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087533294","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00041408636,0.0008679883,0.000085016545,0.9812878,0.016277606,0.0000078671965,0.00019281989,0.000039932962,0.00082704844],"genre_scores_gemma":[0.004611848,0.0008404877,0.00018876298,0.977116,0.012584781,0.000024245724,0.000084092666,0.00005739119,0.0044924123],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9978829,0.0003073311,0.00024684533,0.00035065442,0.00086339336,0.0003489128],"domain_scores_gemma":[0.98677933,0.0036742836,0.0007361618,0.00039445877,0.0066507654,0.0017650467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003971217,0.00078229065,0.0009663215,0.0010601504,0.0049292604,0.0020403,0.004389656,0.017641174,0.006014846],"category_scores_gemma":[0.022449989,0.0006907656,0.000798168,0.0017825561,0.004413496,0.003381639,0.002072469,0.027833931,0.0045132963],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000014005262,0.0000029573755,0.00024493458,0.00002250901,0.0000049884466,0.00010124782,0.00018470567,0.000016432208,0.00005518877,0.00030812286,0.9977581,0.0012868042],"study_design_scores_gemma":[0.000044881694,0.000020321397,0.0067415154,0.00026404308,0.000038457176,0.0006431827,0.0027637654,0.0002089446,0.0005982086,0.0025259429,0.98600996,0.00014082243],"about_ca_topic_score_codex":0.3417544,"about_ca_topic_score_gemma":0.3913712,"teacher_disagreement_score":0.65824556,"about_ca_system_score_codex":0.008692209,"about_ca_system_score_gemma":0.0140665965,"threshold_uncertainty_score":0.6795304},"labels":[],"label_agreement":null},{"id":"W2087904261","doi":"10.1002/2014gl062558","title":"Intermediate‐scale plasma irregularities in the polar ionosphere inferred from GPS radio occultation","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"National Aeronautics and Space Administration","keywords":"Ionosphere; Interplanetary scintillation; Radio occultation; Scintillation; Polar; Occultation; Global Positioning System; Remote sensing; Physics; Geology; Astronomy; Solar wind; Plasma; Detector; Optics; Coronal mass ejection; Telecommunications","score_opus":0.024396854754468747,"score_gpt":0.2846628639182216,"score_spread":0.26026600916375286,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2087904261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99914753,0.000040133586,0.0004115444,0.000006489889,0.0000015941786,0.0000011533823,0.00006928499,0.000012384003,0.00030987718],"genre_scores_gemma":[0.99976975,0.000015472178,0.00013532532,0.0000011182171,0.000002674657,6.1799767e-7,0.00005849556,0.0000014304998,0.000015298005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999966,0.0000046099826,0.0000021819692,0.0000092242435,0.000009581475,0.000008427068],"domain_scores_gemma":[0.9997693,0.0000580819,0.000088303386,0.000027705084,0.00003282291,0.000023802917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093327035,0.000106757485,0.000091116395,0.00068012613,0.00012950382,0.0002941346,0.0000729797,0.00009400532,0.00030102363],"category_scores_gemma":[0.0005167294,0.000084502986,0.000091697424,0.0004891344,0.00019277631,0.00015220868,0.00025074818,0.000106568616,0.000053449825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005284999,0.000028366729,0.840776,0.000047827085,0.00008884717,0.0006016309,0.00044510778,0.0069858157,0.13362227,0.0005156067,0.00028851605,0.016071497],"study_design_scores_gemma":[0.0000045082857,0.000022352726,0.99247026,0.0000022402885,0.0000123352975,0.00008965561,0.000070659524,0.0042408756,0.0027615177,0.00008979697,0.00023103453,0.0000047758103],"about_ca_topic_score_codex":0.0018759881,"about_ca_topic_score_gemma":0.0020355172,"teacher_disagreement_score":0.0018759881,"about_ca_system_score_codex":0.00013570933,"about_ca_system_score_gemma":0.00005554849,"threshold_uncertainty_score":0.0037301779},"labels":[],"label_agreement":null},{"id":"W2088050192","doi":"10.1029/2002gl015637","title":"Microbiological degradation of atmospheric organic compounds","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; McGill University","funders":"","keywords":"Aerosol; Biodegradation; Environmental chemistry; Chemical transformation; Atmosphere (unit); Environmental science; Degradation (telecommunications); Organic compound; Nutrient; Chemistry; Organic chemistry; Meteorology","score_opus":0.03931123130652727,"score_gpt":0.2546132131520336,"score_spread":0.21530198184550634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088050192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93980247,0.028670069,0.014890849,0.00048825215,0.00017958136,0.00006592445,0.0006392131,0.00015042667,0.015113306],"genre_scores_gemma":[0.9882211,0.0063265227,0.0031791995,0.00008365123,0.000041210424,0.0000110327255,0.00023230736,0.0000075007683,0.0018973968],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9995715,0.000045081975,0.00001743876,0.00010236425,0.00019240873,0.00007124577],"domain_scores_gemma":[0.9997085,0.00005423462,0.0000865432,0.000038976246,0.00008373173,0.000027938899],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002335806,0.0003751645,0.0002129779,0.00029537783,0.00034532545,0.00058326265,0.00018329473,0.0004359974,0.000839988],"category_scores_gemma":[0.0005682148,0.00009094963,0.00023927451,0.00021674235,0.00032382525,0.0003311814,0.00043127412,0.0003111778,0.00039644967],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011043926,0.000022385544,0.004549876,0.00023578716,0.00001709945,0.00014323147,0.000036130623,0.00022078006,0.9758379,0.000831021,0.00015107758,0.017844344],"study_design_scores_gemma":[0.0000053263716,0.00021542213,0.009951959,0.000025453386,0.000018908278,0.00041393188,0.00005805295,0.00086346624,0.98037696,0.0006449989,0.0074167238,0.000008800549],"about_ca_topic_score_codex":0.0012369426,"about_ca_topic_score_gemma":0.00076421007,"teacher_disagreement_score":0.0012369426,"about_ca_system_score_codex":0.0004016719,"about_ca_system_score_gemma":0.00030943,"threshold_uncertainty_score":0.002914369},"labels":[],"label_agreement":null},{"id":"W2088122412","doi":"10.1029/2003gl018509","title":"Transition to Turbulence in Shear above the Tropopause","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Turbulence; Tropopause; Shear (geology); Wind shear; Geology; Mechanics; Vortex; Shear flow; Sawtooth wave; Physics; Meteorology; Wavelength; Geophysics; Atmospheric sciences; Optics; Wind speed; Troposphere","score_opus":0.023501048576255068,"score_gpt":0.2808605741112826,"score_spread":0.25735952553502756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088122412","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993906,0.000034475186,0.00008382005,0.000012058714,0.0000029911012,0.000002716166,0.000054629112,0.0000065032036,0.00041225625],"genre_scores_gemma":[0.9997677,0.000021329806,0.000047448597,0.000004039678,0.0000017721783,0.000001520121,0.000078263314,0.0000010910995,0.00007670047],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994135,0.000004690585,0.0000036333001,0.000012067915,0.0000119477645,0.000026425801],"domain_scores_gemma":[0.9998816,0.000012321298,0.00003416217,0.000007249564,0.000027620184,0.000036929167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010120875,0.00017000835,0.00016740212,0.00034373783,0.0003712863,0.0006763889,0.0000901651,0.00019350834,0.0006720265],"category_scores_gemma":[0.000304379,0.00018838799,0.00017729438,0.00021817692,0.00027301276,0.00020117979,0.00030222215,0.00028889359,0.00015259917],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014090501,0.00012343981,0.37503445,0.00007425572,0.000055458142,0.0013796082,0.0013243833,0.0035996407,0.6075426,0.0010047787,0.00043656453,0.008015845],"study_design_scores_gemma":[0.000028175917,0.00022201083,0.9834926,0.000012106252,0.000011865949,0.00013005744,0.00037600615,0.0034762947,0.011612114,0.0001265799,0.0004967505,0.000015425605],"about_ca_topic_score_codex":0.009520031,"about_ca_topic_score_gemma":0.009392613,"teacher_disagreement_score":0.009520031,"about_ca_system_score_codex":0.0005040219,"about_ca_system_score_gemma":0.00015237597,"threshold_uncertainty_score":0.018929243},"labels":[],"label_agreement":null},{"id":"W2088146835","doi":"10.1029/2007gl030825","title":"Tidally generated near‐resonant internal wave triads at a shelf break","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Internal wave; Amplitude; Stratification (seeds); Triad (sociology); Internal tide; Geology; Nonlinear system; Physics; Mode (computer interface); Mechanics; Geophysics; Optics","score_opus":0.030053268556814703,"score_gpt":0.27449768686298054,"score_spread":0.24444441830616584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088146835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957826,0.0000129784175,0.0025199135,0.000050065355,0.0000075784574,0.000005964561,0.000028473594,0.000053159878,0.0015392292],"genre_scores_gemma":[0.9993795,0.000009503691,0.00029844377,0.0000068747836,0.0000017429466,0.0000035223807,0.000023533259,0.000009037732,0.0002677494],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99994147,0.000010152073,0.0000030081214,0.0000086871305,0.000014016287,0.000022626999],"domain_scores_gemma":[0.9997682,0.000053398304,0.00004061546,0.000018816427,0.000030082329,0.0000888834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001621087,0.00021948999,0.0002523137,0.00019997379,0.0004747649,0.0005623767,0.00029906924,0.00039690858,0.001613221],"category_scores_gemma":[0.0005905252,0.00028221295,0.0003116457,0.00016593875,0.0006316945,0.0003247608,0.0005645934,0.00053909386,0.00012598325],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042709938,0.00016908087,0.020184793,0.000042050044,0.000066953915,0.0005029495,0.0004037786,0.92329484,0.04157157,0.007439297,0.00074736035,0.005150201],"study_design_scores_gemma":[0.0000897034,0.000117034346,0.010618372,0.00000435835,0.00001760596,0.00005623601,0.00012699573,0.98540604,0.0022739058,0.0011047553,0.00016497911,0.00001998494],"about_ca_topic_score_codex":0.0059761875,"about_ca_topic_score_gemma":0.0030898359,"teacher_disagreement_score":0.0059761875,"about_ca_system_score_codex":0.0005311964,"about_ca_system_score_gemma":0.00035608708,"threshold_uncertainty_score":0.011882842},"labels":[],"label_agreement":null},{"id":"W2088227404","doi":"10.1029/2004gl021435","title":"Climate‐driven deformation of the solid Earth from GRACE and GPS","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":217,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Global Positioning System; Geology; Earth's rotation; Structural basin; Geodesy; Climatology; Environmental science; Geomorphology","score_opus":0.03725295178439335,"score_gpt":0.2749428582711708,"score_spread":0.23768990648677746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088227404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878862,0.00005004157,0.0035221607,0.00008487544,0.000015980433,0.000014162228,0.0047268993,0.00024600123,0.0034536193],"genre_scores_gemma":[0.99250764,0.00005920177,0.0014046544,0.00001081119,0.000009137875,0.000009940281,0.005640132,0.000042300562,0.00031628873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997359,0.00004393741,0.000021944237,0.000039185994,0.000108184446,0.000050820494],"domain_scores_gemma":[0.9995415,0.00006621936,0.00015173775,0.000106674226,0.00010018775,0.000033719865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000390699,0.00036082888,0.00028685847,0.0009131116,0.00020144584,0.00054748607,0.00024777846,0.00016748242,0.0009705631],"category_scores_gemma":[0.0012012802,0.00015923315,0.00038866422,0.0023400343,0.0003693598,0.00044116544,0.00038885025,0.00032321762,0.00034126852],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008706442,0.00012828837,0.7135362,0.00015802312,0.00034060597,0.0006759997,0.0007465232,0.15769517,0.041959617,0.007137757,0.0071541057,0.069597125],"study_design_scores_gemma":[0.00002500186,0.000092123,0.86631244,0.000015847381,0.00006542124,0.00026300928,0.00014403008,0.11674777,0.009319803,0.0016159804,0.0053481166,0.000050524606],"about_ca_topic_score_codex":0.009401605,"about_ca_topic_score_gemma":0.011966311,"teacher_disagreement_score":0.009401605,"about_ca_system_score_codex":0.00043060776,"about_ca_system_score_gemma":0.0004240288,"threshold_uncertainty_score":0.018693805},"labels":[],"label_agreement":null},{"id":"W2088430767","doi":"10.1029/2008gl035721","title":"Response of the northern stratospheric polar vortex to the seasonal alignment of QBO phase transitions","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Stratosphere; Polar vortex; Quasi-biennial oscillation; Climatology; Northern Hemisphere; Atmospheric sciences; Polar; Environmental science; Radiosonde; Proxy (statistics); Physics; Geology; Mathematics","score_opus":0.028321526020472186,"score_gpt":0.28060462424485944,"score_spread":0.25228309822438727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088430767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989203,0.00009131113,0.00016362795,0.00003164063,0.000010954937,0.000007067537,0.000089657544,0.000006209316,0.00067920313],"genre_scores_gemma":[0.99954236,0.000046807494,0.00005316893,0.00002208075,0.000017496523,0.000005122492,0.00013962388,0.0000031467994,0.0001701156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986565,0.000036341564,0.000009101339,0.000028692886,0.000024767765,0.00003549433],"domain_scores_gemma":[0.9994286,0.0001816873,0.00018663643,0.000037303977,0.000069971116,0.00009575727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032787924,0.00011361228,0.0001684827,0.00027534604,0.00017230585,0.0003287046,0.00006966838,0.00013291361,0.0011141198],"category_scores_gemma":[0.0017633053,0.000096178504,0.000106208565,0.00017861568,0.00018076884,0.00019865851,0.000351671,0.00018050085,0.00012376283],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007457813,0.00009203722,0.9522997,0.00004296716,0.00010871838,0.00015015616,0.00020817696,0.0014795628,0.028004453,0.00022347379,0.00031071328,0.016334334],"study_design_scores_gemma":[0.0000052516784,0.00007134694,0.99876726,0.0000024077438,0.000004928501,0.00002136882,0.00006359881,0.00041080735,0.00035084205,0.000036676876,0.00026378027,0.000001806973],"about_ca_topic_score_codex":0.0024345822,"about_ca_topic_score_gemma":0.0038510642,"teacher_disagreement_score":0.0024345822,"about_ca_system_score_codex":0.0001676203,"about_ca_system_score_gemma":0.00019544031,"threshold_uncertainty_score":0.004840851},"labels":[],"label_agreement":null},{"id":"W2088669724","doi":"10.1029/2001gl013168","title":"Varieties of shallow temperature maximum waters in the Western Canadian Basin of the Arctic Ocean","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":189,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Canada Basin; Ridge; Geology; Arctic; Water mass; Plateau (mathematics); Temperature salinity diagrams; Arctic ice pack; Structural basin; Climatology; Environmental science; Salinity; Surface water","score_opus":0.01751261249643163,"score_gpt":0.23799519159985133,"score_spread":0.2204825791034197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088669724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979645,0.00021639263,0.00007558447,0.000031581156,0.0000017311227,0.000008359343,0.00082230597,0.000008642968,0.0008709477],"genre_scores_gemma":[0.9980311,0.0002149594,0.00031936745,0.000016738364,0.000001494148,0.000006529943,0.0010924117,0.0000033738258,0.00031402174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972385,0.0000100643465,0.000014094994,0.00005772189,0.00008843742,0.00010590025],"domain_scores_gemma":[0.9994542,0.00003406612,0.00010636495,0.000016305918,0.00027335083,0.00011576434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002304665,0.00029353343,0.00022692347,0.0020399517,0.0023293553,0.0010109156,0.0004425875,0.00017675576,0.00047614696],"category_scores_gemma":[0.0007758171,0.00025782493,0.00023424545,0.0038903465,0.0006776781,0.00028299753,0.0006457357,0.0001707044,0.000059484668],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016222787,0.00001622745,0.97685605,0.000053403637,0.000059056147,0.00015354386,0.0014673534,0.0008054321,0.0048881075,0.00023234879,0.00056023407,0.014745934],"study_design_scores_gemma":[0.0000025587199,0.000006524344,0.99787927,0.0000065945433,0.000011603346,0.00004056847,0.0005354195,0.00044136218,0.00024641774,0.000019424926,0.0008016257,0.000008614047],"about_ca_topic_score_codex":0.98570895,"about_ca_topic_score_gemma":0.99572456,"teacher_disagreement_score":0.014291048,"about_ca_system_score_codex":0.009883639,"about_ca_system_score_gemma":0.009829499,"threshold_uncertainty_score":0.07171118},"labels":[],"label_agreement":null},{"id":"W2088974269","doi":"10.1029/2008gl034238","title":"Objective global ocean biogeographic provinces","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":151,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University","funders":"","keywords":"Biogeochemical cycle; Transect; Geography; Climatology; Extrapolation; Forcing (mathematics); Biodiversity; Environmental science; Oceanography; Physical geography; Geology; Ecology","score_opus":0.023022986005487897,"score_gpt":0.25562044977692305,"score_spread":0.23259746377143514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2088974269","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5409299,0.00088720187,0.15335509,0.00038509574,0.00015497375,0.0012770017,0.18441848,0.0039941105,0.114598155],"genre_scores_gemma":[0.8436443,0.00042620665,0.087971635,0.00007847251,0.00004042903,0.0005033036,0.057024978,0.000290824,0.010019842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99952996,0.000058811685,0.0000464122,0.00013218577,0.0001647025,0.00006798017],"domain_scores_gemma":[0.9989254,0.00011511262,0.00029867768,0.00014843798,0.0004455669,0.000066818306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055440405,0.00042634705,0.00032225458,0.0028740116,0.00046015234,0.0014091912,0.00041525622,0.0002256632,0.005284388],"category_scores_gemma":[0.0021742212,0.00019131762,0.00041217133,0.0041701435,0.00042641268,0.0008135782,0.00083913724,0.00035247626,0.0011672992],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003496013,0.00006272401,0.54819274,0.00061629695,0.00016677359,0.000108935375,0.00079736346,0.031065375,0.0057573807,0.02125013,0.03274855,0.3588842],"study_design_scores_gemma":[0.00007905703,0.00007025138,0.79806536,0.00015131883,0.00010465088,0.00016479683,0.0011476208,0.08064045,0.004386428,0.013787258,0.101322435,0.000080289676],"about_ca_topic_score_codex":0.0857115,"about_ca_topic_score_gemma":0.10879257,"teacher_disagreement_score":0.0857115,"about_ca_system_score_codex":0.0015373542,"about_ca_system_score_gemma":0.00211335,"threshold_uncertainty_score":0.17042524},"labels":[],"label_agreement":null},{"id":"W2089086569","doi":"10.1029/2007gl032226","title":"Ultra‐relativistic acceleration of electrons in planetary magnetospheres","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Physics; Electron; Magnetosphere; Van Allen radiation belt; Whistler; Atomic physics; Pitch angle; Particle acceleration; Computational physics; Acceleration; Electromagnetic radiation; Plasma; Astrophysics; Nuclear physics; Geophysics; Quantum mechanics","score_opus":0.016909431290052,"score_gpt":0.29310422860766566,"score_spread":0.27619479731761365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089086569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9512577,0.006453372,0.019899843,0.0003438588,0.00017810549,0.000017811202,0.000045587283,0.0002119386,0.02159171],"genre_scores_gemma":[0.99612916,0.0005933193,0.0017486793,0.000028048113,0.00004875196,0.0000064065366,0.000025896787,0.000008185322,0.0014114559],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994516,0.000008370128,0.0000018211939,0.000010191688,0.000013022048,0.000021505406],"domain_scores_gemma":[0.9999223,0.000008634953,0.000029071929,0.000014268354,0.000011071311,0.000014633627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011541759,0.0001525641,0.00015223176,0.00036931297,0.0003996666,0.00041029882,0.00031420932,0.00025313054,0.0008179204],"category_scores_gemma":[0.00027123012,0.0001359614,0.00019785417,0.00020586074,0.00040811996,0.00043839627,0.00066199264,0.00020908196,0.00018071145],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052757765,0.00013634854,0.06840647,0.00037888213,0.00013548591,0.0038583041,0.001765624,0.050776042,0.14587998,0.5983843,0.009074338,0.120676644],"study_design_scores_gemma":[0.00027641686,0.00091277226,0.23734426,0.00014372192,0.00026343603,0.00921383,0.0014345933,0.20788006,0.048096243,0.34931278,0.14490865,0.00021319443],"about_ca_topic_score_codex":0.0006519327,"about_ca_topic_score_gemma":0.0005574466,"teacher_disagreement_score":0.0008179204,"about_ca_system_score_codex":0.00029183517,"about_ca_system_score_gemma":0.00012871456,"threshold_uncertainty_score":0.0027362108},"labels":[],"label_agreement":null},{"id":"W2089339079","doi":"10.1029/2006gl028543","title":"Uptake of natural and anthropogenic carbon by the Labrador Sea","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Advection; Environmental science; Disequilibrium; Carbon dioxide; Atmospheric sciences; Atmosphere (unit); Carbon fibers; Carbon dioxide in Earth's atmosphere; Greenhouse gas; Carbon cycle; Oceanography; Geology; Meteorology; Climate change; Ecosystem; Chemistry; Ecology; Geography; Materials science","score_opus":0.01034724807310866,"score_gpt":0.26532459543661063,"score_spread":0.25497734736350197,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089339079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968143,0.000052622872,0.00060628087,0.00003721328,0.0000014815463,0.0000026124535,0.00061684905,0.00004255897,0.0018261737],"genre_scores_gemma":[0.99875164,0.000048833386,0.0005491439,0.0000064840333,0.0000016977266,0.0000048015195,0.00039115438,0.0000137537045,0.00023248744],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998771,0.000022568089,0.000008521181,0.000043144657,0.00002019848,0.000028524002],"domain_scores_gemma":[0.99984694,0.000031423733,0.00005262294,0.000024499446,0.000024947869,0.000019531022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017473749,0.00034182597,0.00019229681,0.0006953033,0.00023453911,0.0009078758,0.00039883403,0.00022848097,0.0009905513],"category_scores_gemma":[0.0005664218,0.00016604163,0.0004310244,0.0011189565,0.0003017641,0.00055613654,0.0005000734,0.00014894184,0.00022972454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036048406,0.000052581687,0.8322828,0.00008093807,0.0002632409,0.00024999873,0.00023727621,0.102200516,0.015959084,0.0028157637,0.0005389505,0.044958312],"study_design_scores_gemma":[0.000059362763,0.00012238187,0.77818424,0.000018023633,0.00011120937,0.000116776835,0.00023302848,0.20378508,0.011432208,0.0011343625,0.0047287922,0.000074555566],"about_ca_topic_score_codex":0.097378604,"about_ca_topic_score_gemma":0.08134065,"teacher_disagreement_score":0.097378604,"about_ca_system_score_codex":0.001839946,"about_ca_system_score_gemma":0.0007358855,"threshold_uncertainty_score":0.1936236},"labels":[],"label_agreement":null},{"id":"W2089439943","doi":"10.1029/2002gl015702","title":"Climate from borehole data: Energy fluxes and temperatures since 1500","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Borehole; Heat flux; Flux (metallurgy); Inversion (geology); Geology; Energy balance; Geophysics; Energy flux; Environmental science; Climatology; Atmospheric sciences; Heat transfer; Materials science; Geomorphology; Physics; Thermodynamics; Structural basin","score_opus":0.05565562933819091,"score_gpt":0.29129979603656975,"score_spread":0.23564416669837884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089439943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9252408,0.00040035724,0.0018388869,0.00014444621,0.0000437227,0.000019755838,0.068014294,0.0003678851,0.0039298506],"genre_scores_gemma":[0.92176825,0.00034622222,0.0027905088,0.000042493444,0.00003629655,0.000024578874,0.074138835,0.000044831628,0.00080812606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998313,0.00002273681,0.000016699265,0.000049582537,0.00005056524,0.00002908537],"domain_scores_gemma":[0.999532,0.000053981716,0.00017826364,0.00006385179,0.00012610972,0.000045866498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003635762,0.00025986985,0.00015547822,0.00073255814,0.0001267015,0.00041043537,0.00020276605,0.00021902024,0.0014388841],"category_scores_gemma":[0.0013068309,0.00014875775,0.00026484014,0.0014091079,0.00013805622,0.00049344834,0.0002826578,0.00021589549,0.00047670893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004634166,0.00009035965,0.93027985,0.000197867,0.00022005432,0.0001783775,0.00043247957,0.007389714,0.010029999,0.0006382978,0.011652498,0.038426995],"study_design_scores_gemma":[0.000009517675,0.000024474444,0.99041873,0.000008646195,0.00002241143,0.00005738409,0.00006366722,0.0020462382,0.0011398278,0.00010713166,0.0060912073,0.000010829318],"about_ca_topic_score_codex":0.029879222,"about_ca_topic_score_gemma":0.048697587,"teacher_disagreement_score":0.029879222,"about_ca_system_score_codex":0.0003083322,"about_ca_system_score_gemma":0.00036199656,"threshold_uncertainty_score":0.059410572},"labels":[],"label_agreement":null},{"id":"W2089621327","doi":"10.1029/2006gl027893","title":"Thermal infrared reflectance and emission spectroscopy of quartzofeldspathic glasses","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Amorphous solid; Materials science; Mineralogy; Mars Exploration Program; Infrared; Mineral; Spectroscopy; Infrared spectroscopy; Spectral line; Astrobiology; Optics; Analytical Chemistry (journal); Geology; Chemistry; Crystallography; Physics; Environmental chemistry; Metallurgy","score_opus":0.030699215832850527,"score_gpt":0.33326698967565654,"score_spread":0.30256777384280603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089621327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907845,0.0003359047,0.0051343995,0.000028583885,0.000006351147,0.000017419272,0.00048494755,0.00007001954,0.0031378367],"genre_scores_gemma":[0.9938407,0.00021782189,0.0034935742,0.00001759576,0.000004317301,0.000011160859,0.0004335964,0.000017062155,0.0019641577],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99990094,0.0000064724486,0.0000033082727,0.000032299435,0.00004200946,0.000015034205],"domain_scores_gemma":[0.999938,0.000018224066,0.000014984977,0.0000049264677,0.000017666722,0.000006203277],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001414715,0.00015050195,0.00007577046,0.00036873706,0.0002536478,0.00019128242,0.00015128696,0.00019471212,0.0013327365],"category_scores_gemma":[0.00016487433,0.00012519203,0.00011852841,0.0002650359,0.0001646357,0.00020632231,0.000116485666,0.00017734003,0.00020560966],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000029429293,0.0000063939756,0.0009881165,0.000013182798,0.0000027063004,0.00001883841,0.00003599664,0.0002043203,0.99733835,0.000066362896,0.00004567083,0.0012505171],"study_design_scores_gemma":[0.0000172825,0.00018505141,0.05282422,0.00000982892,0.00002171121,0.00030135424,0.00023075752,0.0053947084,0.93689054,0.00015994276,0.0039417483,0.000022877719],"about_ca_topic_score_codex":0.0056303637,"about_ca_topic_score_gemma":0.0067707836,"teacher_disagreement_score":0.0056303637,"about_ca_system_score_codex":0.00030142278,"about_ca_system_score_gemma":0.00016587104,"threshold_uncertainty_score":0.011195183},"labels":[],"label_agreement":null},{"id":"W2089625625","doi":"10.1029/2004gl020133","title":"Heat flow and deep lithospheric thermal structure at Lac de Gras, Slave Province, Canada","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Centre National de la Recherche Scientifique","keywords":"Lithosphere; Geology; Archean; Heat generation; Heat flow; High heat; Geothermobarometry; Geothermal gradient; Shield; Outcrop; Craton; Petrology; Thermal; Geochemistry; Tectonics; Geophysics; Seismology; Meteorology; Materials science; Thermodynamics; Geography","score_opus":0.008345239763818638,"score_gpt":0.20809498689289282,"score_spread":0.19974974712907417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2089625625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99624324,0.00012530784,0.00009623503,0.00008406169,0.0000031170725,0.000010107457,0.00073536404,0.000012616045,0.0026901064],"genre_scores_gemma":[0.997869,0.00008830264,0.00021651413,0.000019467569,0.0000012530087,0.00000458169,0.00046723743,0.000005568155,0.0013279627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998388,0.0000048388406,0.0000030424612,0.000033678854,0.000054271914,0.00006527833],"domain_scores_gemma":[0.99972624,0.000014581504,0.000024933513,0.0000073488486,0.0001667632,0.000060201648],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012286106,0.00025432874,0.000202962,0.0010412207,0.0023655815,0.00072789466,0.00040581624,0.00020710933,0.0015597526],"category_scores_gemma":[0.00046535142,0.0002007722,0.00017743628,0.0012256491,0.00073874916,0.00020802645,0.00045059703,0.00028050927,0.00015253064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000517012,0.00007393833,0.91491514,0.00007989861,0.000085332984,0.0007349894,0.0061319135,0.0026693325,0.041591488,0.0016837085,0.0027363226,0.028780803],"study_design_scores_gemma":[0.000016926397,0.000015085608,0.9937588,0.000012809266,0.000007732903,0.00005875563,0.0012371573,0.0010520155,0.0009736281,0.0000677592,0.0027857164,0.000013634652],"about_ca_topic_score_codex":0.9947548,"about_ca_topic_score_gemma":0.9983463,"teacher_disagreement_score":0.01963591,"about_ca_system_score_codex":0.01963591,"about_ca_system_score_gemma":0.016601747,"threshold_uncertainty_score":0.14246917},"labels":[],"label_agreement":null},{"id":"W2090228849","doi":"10.1029/2006gl028687","title":"Retrieval of global mesospheric sodium densities from the Odin satellite","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Lidar; Satellite; Altitude (triangle); Environmental science; Latitude; Atmospheric sciences; Sodium; Remote sensing; Spectrograph; Meteorology; Geology; Materials science; Physics; Geodesy; Spectral line; Astronomy","score_opus":0.016782523548746698,"score_gpt":0.2892976276300761,"score_spread":0.2725151040813294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090228849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98037994,0.0002147291,0.00825774,0.00008874648,0.000016923354,0.000030687283,0.005473543,0.0004490293,0.005088603],"genre_scores_gemma":[0.9808343,0.00021012647,0.011006397,0.000031728134,0.000008843331,0.000015631758,0.0063431165,0.000051804363,0.001498038],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999676,0.000002511567,0.0000019785386,0.000009662064,0.000010453559,0.000007689462],"domain_scores_gemma":[0.9999522,0.0000036221022,0.000011753937,0.000007989449,0.000017862343,0.0000065317518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010165067,0.00036728673,0.00020129894,0.0004875152,0.0002808012,0.00042904707,0.00023222738,0.00016417309,0.00069234037],"category_scores_gemma":[0.00024348624,0.00015852235,0.00012689242,0.00057325506,0.00010344069,0.0004177333,0.00046957997,0.00014895276,0.00019481129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058605074,0.00016369302,0.56176144,0.00025628312,0.00023861985,0.00052499294,0.00060652575,0.07671936,0.14297777,0.0018348886,0.008193586,0.20613682],"study_design_scores_gemma":[0.00012873682,0.00009117253,0.7201057,0.000045529545,0.00008519856,0.00016224378,0.0005248979,0.21609186,0.04449168,0.0010252309,0.0171844,0.00006330188],"about_ca_topic_score_codex":0.02708564,"about_ca_topic_score_gemma":0.061425485,"teacher_disagreement_score":0.02708564,"about_ca_system_score_codex":0.0005400126,"about_ca_system_score_gemma":0.0004949442,"threshold_uncertainty_score":0.053855956},"labels":[],"label_agreement":null},{"id":"W2090266550","doi":"10.1029/2004gl021976","title":"Dielectric method of high‐resolution gas hydrate estimation","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lamont-Doherty Earth Observatory, Columbia University; U.S. Geological Survey; U.S. Department of Energy","keywords":"Hydrate; Clathrate hydrate; Dielectric; Saturation (graph theory); Ohm; Mineralogy; Electrical resistivity and conductivity; Geology; Materials science; Analytical Chemistry (journal); Chemistry; Physics","score_opus":0.021101021707547664,"score_gpt":0.30783274946582573,"score_spread":0.28673172775827804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090266550","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.050696522,0.0005939843,0.93443614,0.00008727711,0.00010367053,0.0001456742,0.0017062691,0.004282532,0.007947941],"genre_scores_gemma":[0.37276125,0.001116198,0.61101484,0.00009409208,0.000066017186,0.000311821,0.0021948933,0.00064878847,0.011792038],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99962366,0.0000401773,0.000015058759,0.000094402574,0.00018639679,0.000040315284],"domain_scores_gemma":[0.9992514,0.0001335819,0.00008438036,0.00014665912,0.0003522485,0.00003176109],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054703903,0.0005226142,0.00047100236,0.0016950801,0.00038416882,0.0008133514,0.0010688097,0.00038900672,0.005857289],"category_scores_gemma":[0.0017462906,0.0003540024,0.00030815235,0.001700151,0.00023794906,0.0008986613,0.0006521204,0.0009449237,0.0032853726],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000224041,0.00014052374,0.008018272,0.0004889188,0.00009296435,0.00021534083,0.00023728573,0.013688112,0.60792243,0.0059500197,0.007108749,0.3559134],"study_design_scores_gemma":[0.000060445986,0.00019769168,0.03186407,0.000055046883,0.0001278901,0.0010014392,0.00032251928,0.4095789,0.48514083,0.0042432086,0.067179374,0.00022864307],"about_ca_topic_score_codex":0.003783246,"about_ca_topic_score_gemma":0.0051117428,"teacher_disagreement_score":0.005857289,"about_ca_system_score_codex":0.00042026982,"about_ca_system_score_gemma":0.00069006486,"threshold_uncertainty_score":0.01959461},"labels":[],"label_agreement":null},{"id":"W2090620479","doi":"10.1029/2003gl017931","title":"Break‐up of the largest Arctic ice shelf and associated loss of an epishelf lake","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":137,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"","keywords":"Fjord; Ice shelf; Oceanography; Geology; Arctic ice pack; Arctic; Iceberg; Climate change; Cryosphere; Shelf ice; Sea ice; Physical geography; Climatology; Geography","score_opus":0.030791889266861966,"score_gpt":0.27029381057887897,"score_spread":0.239501921312017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2090620479","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995899,0.00009799961,0.00005170613,0.00013059395,0.000005292799,0.000003879339,0.00026563834,0.000005005705,0.003540879],"genre_scores_gemma":[0.9983543,0.00009331758,0.00008842229,0.000039025253,0.000005751479,0.0000021954709,0.00031965526,0.000001470015,0.0010959281],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.0000023475236,0.0000027214198,0.00001209471,0.000023518809,0.00002686268],"domain_scores_gemma":[0.9997584,0.000010019664,0.00009873552,0.0000141385635,0.00005737089,0.000061441955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010326939,0.000117105235,0.0000623303,0.00035754658,0.0006647551,0.00046790083,0.00015375257,0.00017565361,0.0015257363],"category_scores_gemma":[0.00041482973,0.00007362826,0.00006942425,0.000365994,0.00052821625,0.00020927242,0.0004830751,0.00024502582,0.00011900156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016215254,0.000031419146,0.9449981,0.000035604597,0.000026431573,0.0009465854,0.001024013,0.00024898184,0.010724137,0.00071492634,0.0022540146,0.03883361],"study_design_scores_gemma":[0.0000017121332,0.000009474131,0.9959443,0.0000043356213,0.0000020634236,0.00017064833,0.00027071094,0.000059087753,0.00061566016,0.000034910117,0.00288564,0.0000015160331],"about_ca_topic_score_codex":0.16097078,"about_ca_topic_score_gemma":0.42401424,"teacher_disagreement_score":0.16097078,"about_ca_system_score_codex":0.0013543442,"about_ca_system_score_gemma":0.0014562004,"threshold_uncertainty_score":0.32006764},"labels":[],"label_agreement":null},{"id":"W2091542222","doi":"10.1029/2000gl012597","title":"Sensitivity of ozone production rate to ozone precursors","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Ozone; Radical; Troposphere; Dilution; Atmospheric chemistry; Sink (geography); Chemistry; Environmental science; Atmospheric sciences; Photochemistry; Meteorology; Thermodynamics; Physics; Organic chemistry","score_opus":0.03350433317320653,"score_gpt":0.28412138196878367,"score_spread":0.2506170487955771,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091542222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955474,0.000116727744,0.0031813928,0.000030150451,0.000002285429,0.000012064119,0.00031605613,0.000074562966,0.000719254],"genre_scores_gemma":[0.9992719,0.00004176101,0.00033728944,0.000006772572,5.011087e-7,0.0000061685023,0.00021704404,0.000004106711,0.000114427516],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998129,0.000023991362,0.0000064971778,0.00009390464,0.00003179779,0.00003087219],"domain_scores_gemma":[0.9992493,0.00044032774,0.0000837955,0.00010004477,0.00010285665,0.000023824252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029266797,0.00025203192,0.00017901995,0.00018561576,0.00013839865,0.0004521141,0.0003868234,0.000334212,0.000851145],"category_scores_gemma":[0.0018758865,0.0002418101,0.00023158063,0.0001830708,0.00021804759,0.00035568693,0.0003093362,0.00037573793,0.00013306236],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00085304107,0.00014952112,0.18224135,0.00014899216,0.000255366,0.00025644762,0.00020757089,0.24819368,0.5489026,0.0010612694,0.0004482595,0.01728187],"study_design_scores_gemma":[0.000061358805,0.0004403283,0.3768449,0.000011528121,0.00009382317,0.00014999564,0.00011326951,0.22925478,0.39111584,0.00090865843,0.00094127166,0.00006424206],"about_ca_topic_score_codex":0.016862534,"about_ca_topic_score_gemma":0.00445094,"teacher_disagreement_score":0.016862534,"about_ca_system_score_codex":0.00056185,"about_ca_system_score_gemma":0.00020930915,"threshold_uncertainty_score":0.033528805},"labels":[],"label_agreement":null},{"id":"W2091679583","doi":"10.1029/2007gl032582","title":"Scaling laws and frequency distributions of avalanche areas in a self‐organized criticality model of solar flares","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Self-organized criticality; Physics; Power law; Anisotropy; Statistical physics; Criticality; Scaling; Critical exponent; Astrophysics; Geometry; Condensed matter physics; Quantum mechanics; Nuclear physics; Phase transition","score_opus":0.03083739388504353,"score_gpt":0.30017778746045737,"score_spread":0.26934039357541384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091679583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9731339,0.00012289474,0.025115311,0.00011673752,0.0000053699814,0.000012569667,0.00003114614,0.000050371244,0.0014117424],"genre_scores_gemma":[0.99850476,0.000040245777,0.0012622775,0.0000048647516,0.000003664502,0.000008797417,0.0000131932065,0.000004765266,0.00015744437],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999478,0.000014440356,0.0000029083972,0.000008101734,0.000012338399,0.000014391495],"domain_scores_gemma":[0.9994318,0.00027835663,0.00013755244,0.000037889888,0.000059467726,0.000054873595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027372272,0.00029764953,0.00024832904,0.0007157507,0.00033237512,0.0005721693,0.0005325607,0.0005664218,0.00058621564],"category_scores_gemma":[0.0014842326,0.00019456087,0.0003333916,0.0002789821,0.00070539245,0.0006877371,0.00026844573,0.00032228345,0.000053392054],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036846384,0.000036411067,0.007003888,0.0000255743,0.000027046799,0.00020407168,0.00013987505,0.9596353,0.004594677,0.026127327,0.00020042768,0.0019685347],"study_design_scores_gemma":[0.0000033543208,0.0000067927426,0.00044899603,0.0000012410798,0.0000018823303,0.000017279157,0.000009439176,0.9958968,0.00015500838,0.0034251928,0.000031357366,0.000002698364],"about_ca_topic_score_codex":0.0037473836,"about_ca_topic_score_gemma":0.0018220545,"teacher_disagreement_score":0.0037473836,"about_ca_system_score_codex":0.00067035534,"about_ca_system_score_gemma":0.00019825337,"threshold_uncertainty_score":0.007451117},"labels":[],"label_agreement":null},{"id":"W2091695577","doi":"10.1029/1999gl000014","title":"Auroral disturbances during the January 10, 1997 magnetic storm","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Substorm; Geophysics; Convection; Solar wind; Geomagnetic storm; Geology; Storm; Longitude; Dynamic pressure; Magnetosphere; Atmospheric sciences; Latitude; Physics; Magnetic field; Geodesy; Meteorology; Mechanics; Oceanography","score_opus":0.010077820736832041,"score_gpt":0.258983983712278,"score_spread":0.24890616297544593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091695577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972811,0.00023505009,0.00005775574,0.0000652797,0.000013625878,0.000014478384,0.00039650692,0.000022718992,0.0019134093],"genre_scores_gemma":[0.9970697,0.00049169024,0.000113492606,0.00006717971,0.00006476717,0.000020449144,0.0016352508,0.0000073941,0.00052998494],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998012,0.000016266791,0.000015525124,0.000030918145,0.00006777183,0.00006826951],"domain_scores_gemma":[0.999206,0.000080379534,0.0004266615,0.000029733312,0.00011006012,0.00014715035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025036716,0.00022121487,0.00031355544,0.0008422514,0.00071210257,0.0009116994,0.0002052594,0.00036118782,0.0008092788],"category_scores_gemma":[0.0009022051,0.00016242806,0.00013266518,0.0008196505,0.00039782474,0.0002936636,0.0006449476,0.00043292064,0.0002786955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016664664,0.00026809436,0.91701573,0.00015845544,0.00016152862,0.0027086178,0.0029898747,0.0006927415,0.033665985,0.00030714078,0.0058859843,0.034479376],"study_design_scores_gemma":[0.000014185181,0.00007615373,0.99699306,0.00001069224,0.000011953324,0.00021992355,0.00033015787,0.00011668472,0.00053904403,0.000024475972,0.0016589069,0.0000048248103],"about_ca_topic_score_codex":0.014284867,"about_ca_topic_score_gemma":0.032134704,"teacher_disagreement_score":0.014284867,"about_ca_system_score_codex":0.0007717101,"about_ca_system_score_gemma":0.00035091685,"threshold_uncertainty_score":0.028403461},"labels":[],"label_agreement":null},{"id":"W2091776742","doi":"10.1029/2005gl025298","title":"Correlation of airglow temperature and emission rate at Resolute Bay (74.68°N), over four winters (2001–2005)","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Airglow; Bay; Rotational temperature; Atmospheric sciences; Environmental science; Physics; Geodesy; Geology; Spectral line; Oceanography; Astronomy","score_opus":0.009331537686599027,"score_gpt":0.25662633737524493,"score_spread":0.2472947996886459,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2091776742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99919516,0.000027234377,0.000036385074,0.000011013972,0.0000018017543,0.0000013559081,0.0004943424,0.000008631809,0.00022402847],"genre_scores_gemma":[0.9971697,0.000037673126,0.00014865633,0.000008427056,0.0000034840598,0.0000034590573,0.0022396562,0.000003928959,0.00038508614],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992204,0.0000059514064,0.0000039612482,0.000029438468,0.000019648023,0.000019016585],"domain_scores_gemma":[0.9996234,0.000043196942,0.00012838328,0.000028598472,0.00010821127,0.00006823778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014401083,0.00017051813,0.00016359537,0.0005195182,0.00020129705,0.0003311498,0.00022957915,0.0002340856,0.0006423193],"category_scores_gemma":[0.0003940212,0.00013586224,0.00009013467,0.0004067536,0.0001386836,0.00019009387,0.0002123888,0.00022776105,0.00018712874],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001327233,0.000030907973,0.9897856,0.000008879951,0.00004775083,0.000055697576,0.00018542378,0.0005211773,0.0059192753,0.000022520344,0.0004148674,0.0028753227],"study_design_scores_gemma":[0.0000018140275,0.000008712756,0.99936527,6.491411e-7,0.0000039170254,0.000011521828,0.000031401167,0.00021058386,0.00021786879,0.0000014955376,0.0001454653,0.000001195724],"about_ca_topic_score_codex":0.07126262,"about_ca_topic_score_gemma":0.19420613,"teacher_disagreement_score":0.9287374,"about_ca_system_score_codex":0.0005868932,"about_ca_system_score_gemma":0.00021135087,"threshold_uncertainty_score":0.14169568},"labels":[],"label_agreement":null},{"id":"W2092188850","doi":"10.1029/2006gl026079","title":"Organosulfate formation during the uptake of pinonaldehyde on acidic sulfate aerosols","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":156,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Sulfate; Aerosol; Mass spectrometry; Mass fraction; Environmental chemistry; Chemistry; Mass spectrum; Sulfate aerosol; Mass concentration (chemistry); Inorganic chemistry; Chromatography; Organic chemistry; Physical chemistry","score_opus":0.020663897954076842,"score_gpt":0.24831154198522037,"score_spread":0.22764764403114354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092188850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973393,0.0003535736,0.0012301537,0.00001772544,0.000008268323,0.000022559896,0.00013173705,0.000023688248,0.0008729341],"genre_scores_gemma":[0.9977683,0.00017522166,0.0005709583,0.000014548894,0.000006121584,0.000011460799,0.00016841857,0.000008732313,0.0012763718],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99986255,0.000018061563,0.000005513742,0.000029392844,0.000051031704,0.000033505698],"domain_scores_gemma":[0.99988055,0.000030549556,0.000020208996,0.000008795076,0.00003426328,0.000025666759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019828836,0.00033984808,0.00024574922,0.00021350512,0.00021983849,0.00033532648,0.0002142809,0.0002356435,0.0010436599],"category_scores_gemma":[0.0003082831,0.00017015918,0.00018374216,0.00012887249,0.00022817314,0.00034662863,0.0002932604,0.00024965848,0.00028985366],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014019496,0.0000072080093,0.001517661,0.000030506211,0.0000065795743,0.000062190906,0.000055187647,0.000051003684,0.996855,0.00003324971,0.000012697528,0.0012285642],"study_design_scores_gemma":[0.000006532509,0.00017702831,0.013872894,0.0000017332387,0.000008427171,0.00006964243,0.000060122955,0.0007732489,0.98448086,0.000049559763,0.0004950289,0.0000048214897],"about_ca_topic_score_codex":0.002087866,"about_ca_topic_score_gemma":0.001228933,"teacher_disagreement_score":0.002087866,"about_ca_system_score_codex":0.00030251217,"about_ca_system_score_gemma":0.00018488061,"threshold_uncertainty_score":0.0041514635},"labels":[],"label_agreement":null},{"id":"W2092197041","doi":"10.1029/2006gl026612","title":"Some controls on flow and salinity in Bering Strait","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Salinity; Throughflow; Structural basin; Freshwater inflow; Geology; Inflow; Forcing (mathematics); Climatology","score_opus":0.020938424016865933,"score_gpt":0.26501152542126416,"score_spread":0.24407310140439822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092197041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944701,0.00020229457,0.000066650275,0.00032691704,0.00001088012,0.0000036026502,0.0002288292,0.000010760534,0.0046800417],"genre_scores_gemma":[0.9985642,0.00014495195,0.000048736718,0.000052115964,0.0000095154,0.0000016201292,0.00019480358,0.0000041061317,0.0009799064],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986506,0.00003221175,0.00001025291,0.00003350252,0.000012923112,0.0000461236],"domain_scores_gemma":[0.99960726,0.000055857945,0.00010560663,0.00002408017,0.000081490994,0.00012577906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024341496,0.00017261403,0.00013771502,0.00047007372,0.00044832565,0.00093849015,0.00020400892,0.00020510485,0.0030217608],"category_scores_gemma":[0.00078844134,0.00014029564,0.00019006379,0.00038470185,0.0006565036,0.00041614423,0.00037347112,0.00028304124,0.00035306666],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032686637,0.00006018507,0.96549326,0.00003660958,0.00005999092,0.0003741906,0.0015712855,0.0027335372,0.0106667355,0.0018695174,0.0015609636,0.015246882],"study_design_scores_gemma":[0.0000065124163,0.000026548432,0.9971138,0.000008767126,0.000009532549,0.000027131964,0.0003027891,0.0006707708,0.00023453467,0.00013529585,0.0014577269,0.000006581057],"about_ca_topic_score_codex":0.22602522,"about_ca_topic_score_gemma":0.27718392,"teacher_disagreement_score":0.22602522,"about_ca_system_score_codex":0.0021881568,"about_ca_system_score_gemma":0.0007840415,"threshold_uncertainty_score":0.4494192},"labels":[],"label_agreement":null},{"id":"W2092444956","doi":"10.1029/2006gl026144","title":"On the flux of oxygenated volatile organic compounds from organic aerosol oxidation","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; University of Hawai'i; U.S. Environmental Protection Agency; National Science Foundation","keywords":"Aerosol; Flux (metallurgy); Troposphere; Environmental chemistry; Environmental science; Atmospheric chemistry; Atmospheric sciences; Atmosphere (unit); Ozone; Chemistry; Meteorology; Organic chemistry; Geology; Physics","score_opus":0.019254976211762365,"score_gpt":0.23837116791855367,"score_spread":0.2191161917067913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092444956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99305177,0.000925621,0.001837087,0.00009730496,0.000022585222,0.00001295037,0.0004980011,0.000025854208,0.0035288637],"genre_scores_gemma":[0.99602294,0.0013238586,0.00092616817,0.000042486998,0.000038608778,0.000008038695,0.00055798516,0.000008530861,0.0010713289],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993825,0.000008344009,0.0000014835894,0.000019931966,0.000018458402,0.000013578454],"domain_scores_gemma":[0.9998054,0.000119435615,0.000021056783,0.0000073673955,0.00003774965,0.000008911829],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019669041,0.00037997018,0.00014227195,0.0004938728,0.00018997012,0.00029639617,0.00017263278,0.00028531306,0.0021402093],"category_scores_gemma":[0.00040570527,0.000080773534,0.0001624544,0.00025660906,0.00015144979,0.0005336033,0.00014953567,0.00016105224,0.00030545346],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017479701,0.00021857432,0.21605971,0.00044740207,0.00016719438,0.0010584418,0.0001390284,0.021088216,0.68332446,0.0023578086,0.0013825613,0.0720086],"study_design_scores_gemma":[0.00008802296,0.0005404258,0.52816385,0.000092052185,0.00018727066,0.00044631763,0.00029615252,0.08067736,0.37704664,0.003292935,0.009124154,0.000044802535],"about_ca_topic_score_codex":0.0044910167,"about_ca_topic_score_gemma":0.0024788538,"teacher_disagreement_score":0.0044910167,"about_ca_system_score_codex":0.00049848313,"about_ca_system_score_gemma":0.00009969893,"threshold_uncertainty_score":0.008929789},"labels":[],"label_agreement":null},{"id":"W2092530280","doi":"10.1029/2002gl016549","title":"Dynamical aspects of climate sensitivity","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Mixed layer; Radiative transfer; Climatology; Climate sensitivity; Positive feedback; Environmental science; Forcing (mathematics); Radiative forcing; Arctic; Climate model; Negative feedback; Atmospheric sciences; The arctic; Climate change; Oceanography; Geology; Physics","score_opus":0.030120192172892774,"score_gpt":0.3054583880993779,"score_spread":0.2753381959264851,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092530280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95823896,0.00043389414,0.01768157,0.0015547558,0.000083585765,0.000056689365,0.0006460304,0.0001380148,0.021166565],"genre_scores_gemma":[0.9992192,0.00007558234,0.0003276894,0.000037752176,0.0000113794495,0.000007501364,0.00004875204,0.000016745893,0.00025544167],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996195,0.00017836821,0.000020303036,0.000066225795,0.000051822488,0.00006376062],"domain_scores_gemma":[0.99883705,0.0007044561,0.00013147492,0.0001174677,0.0001179703,0.000091554364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008191312,0.00033703935,0.00032122392,0.00053312187,0.0004284763,0.0012051844,0.00041905305,0.0006433066,0.0022191026],"category_scores_gemma":[0.005818255,0.00041708455,0.0006626649,0.00038429207,0.00078888057,0.0017291288,0.0010290575,0.00058447936,0.000117426374],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013116248,0.0000646257,0.029505195,0.00009801737,0.00015436143,0.0002667699,0.0002510616,0.9180814,0.01174652,0.032608535,0.00078462635,0.006307774],"study_design_scores_gemma":[0.000037338305,0.00007106992,0.034472264,0.000018935094,0.00004776685,0.00011175995,0.0001660594,0.9386708,0.001244688,0.023915188,0.0011985109,0.00004561202],"about_ca_topic_score_codex":0.006606155,"about_ca_topic_score_gemma":0.002916331,"teacher_disagreement_score":0.006606155,"about_ca_system_score_codex":0.0010374943,"about_ca_system_score_gemma":0.00045616826,"threshold_uncertainty_score":0.013135433},"labels":[],"label_agreement":null},{"id":"W2092794500","doi":"10.1029/2005gl022972","title":"Salinity variability in the Arabian Sea","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Argo; Rossby wave; Oceanography; Climatology; Annual cycle; Geology; Salinity; Sea level; Forcing (mathematics); Sea-surface height; Water mass; Temperature salinity diagrams; Sea surface temperature","score_opus":0.03250282743056579,"score_gpt":0.28944861183190634,"score_spread":0.2569457844013405,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2092794500","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99931777,0.000041597967,0.00008050683,0.000018460218,0.0000027927701,7.402849e-7,0.00007830363,0.0000043930827,0.00045551886],"genre_scores_gemma":[0.9996172,0.00003677231,0.000062962674,0.00000676119,0.0000029128198,6.4253135e-7,0.00016300296,0.0000012428233,0.000108552216],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999083,0.0000151259255,0.0000082008755,0.00002726104,0.000025013322,0.000016050808],"domain_scores_gemma":[0.99971706,0.000030868116,0.00007079913,0.000025066609,0.00011626175,0.000039914245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017558695,0.000145647,0.00015183151,0.00040223938,0.000155468,0.0004482733,0.00010530066,0.00016203577,0.00035696587],"category_scores_gemma":[0.0005266008,0.000111129004,0.0001085732,0.0003993587,0.00015081972,0.00025971825,0.0003136269,0.00010639711,0.00018796133],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034516587,0.000037210815,0.92171746,0.000023936807,0.00011573777,0.00029461444,0.00064034987,0.0025949571,0.048577227,0.00034393382,0.000515928,0.024793454],"study_design_scores_gemma":[0.0000064964333,0.000041519896,0.9951923,0.0000045698444,0.000011146255,0.000104560444,0.00016099364,0.0023785254,0.0012950368,0.00005739491,0.0007387639,0.000008716598],"about_ca_topic_score_codex":0.005432869,"about_ca_topic_score_gemma":0.004968387,"teacher_disagreement_score":0.005432869,"about_ca_system_score_codex":0.0002778423,"about_ca_system_score_gemma":0.00013743101,"threshold_uncertainty_score":0.010802507},"labels":[],"label_agreement":null},{"id":"W2093306856","doi":"10.1029/2007gl029535","title":"New constraints on the upper mantle structure of the Slave craton from Rayleigh wave inversion","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Craton; Lithosphere; Geology; Mantle (geology); Geophysics; Anisotropy; Seismogram; Seismology; Amplitude; Tectonics; Physics","score_opus":0.026277385617072477,"score_gpt":0.2556632531616265,"score_spread":0.22938586754455403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093306856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99485236,0.00011549592,0.0015359643,0.00004268193,0.0000015290337,0.0000035444664,0.00024341556,0.000021297243,0.003183744],"genre_scores_gemma":[0.99801,0.00009521822,0.00094033545,0.000008366192,0.0000024865478,0.0000020464106,0.0005625167,0.000010464803,0.00036855348],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992347,0.000004524761,0.0000037269433,0.000015332844,0.000022727458,0.000030170155],"domain_scores_gemma":[0.99981385,0.000047680678,0.00003502524,0.000025575937,0.000051875733,0.000026081125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012844836,0.00031982837,0.0002784424,0.0009784236,0.00048203274,0.00093077484,0.0002249556,0.0001458178,0.0024821751],"category_scores_gemma":[0.001183503,0.0002685197,0.00026220083,0.0011979908,0.00047586838,0.00033738496,0.00069948414,0.00035006963,0.00022294588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007773191,0.000054433058,0.682154,0.00010386299,0.00009201049,0.00092135486,0.0020850997,0.013983189,0.22205347,0.007000481,0.0008079914,0.069966815],"study_design_scores_gemma":[0.000040456314,0.000032606265,0.9733006,0.000030162339,0.00003917434,0.00019102039,0.00075999077,0.016696183,0.0048972927,0.0010678085,0.002917488,0.00002725073],"about_ca_topic_score_codex":0.2255021,"about_ca_topic_score_gemma":0.4640408,"teacher_disagreement_score":0.77449787,"about_ca_system_score_codex":0.0009060511,"about_ca_system_score_gemma":0.0018009465,"threshold_uncertainty_score":0.4483791},"labels":[],"label_agreement":null},{"id":"W2093319542","doi":"10.1029/2001gl013079","title":"Electromagnetic heterogeneity of the seismogenic region of 1962 M6.5 Northern Miyagi Earthquake, northeastern Japan","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Earthquake Detection and Analysis","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of British Columbia Hospital","funders":"","keywords":"Magnetotellurics; Geology; Seismology; Crust; Pluton; Induced seismicity; Resistive touchscreen; Conductor; Geophysics; Far East; Tectonics; Electrical resistivity and conductivity","score_opus":0.028986043754716095,"score_gpt":0.2568703600451052,"score_spread":0.22788431629038913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093319542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967885,0.000037305705,0.000029847153,0.000008627762,6.6669514e-7,0.00000101661,0.00006488124,0.0000014270248,0.00017734022],"genre_scores_gemma":[0.99963665,0.000032299926,0.000032740187,0.0000037565007,0.0000036076958,0.0000015175291,0.00019335278,6.2434003e-7,0.000095511416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991024,0.000011440461,0.000007732068,0.000027540225,0.0000117992195,0.000031193802],"domain_scores_gemma":[0.9997596,0.00002546326,0.00008661526,0.000014336709,0.000060077477,0.000053859985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014069688,0.00015963298,0.00020229796,0.000948418,0.00036574708,0.00034631716,0.00013026514,0.00021244309,0.0005079013],"category_scores_gemma":[0.00044545063,0.00017845481,0.00011123524,0.00077148946,0.00028948442,0.0002296608,0.00036314182,0.00009417481,0.000115798146],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020091223,0.000021218708,0.9609448,0.000040580293,0.00005497403,0.00065972836,0.0011201593,0.00071168586,0.031266578,0.00006413492,0.00015229508,0.0047629904],"study_design_scores_gemma":[0.0000020817702,0.000008291847,0.9994943,0.000001018491,0.000006291799,0.0000691074,0.00013802874,0.00010527083,0.000107527136,0.0000053947338,0.000060758863,0.0000019055996],"about_ca_topic_score_codex":0.021590551,"about_ca_topic_score_gemma":0.033076864,"teacher_disagreement_score":0.021590551,"about_ca_system_score_codex":0.00035749306,"about_ca_system_score_gemma":0.00017326554,"threshold_uncertainty_score":0.04292977},"labels":[],"label_agreement":null},{"id":"W2093339808","doi":"10.1029/2005gl025480","title":"Carbon storage on exposed continental shelves during the glacial‐interglacial transition","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Continental shelf; Interglacial; Last Glacial Maximum; Environmental science; Carbon cycle; Climate change; Soil carbon; Carbon fibers; Vegetation (pathology); Geology; Physical geography; Carbon sequestration; Oceanography; Glacial period; Climatology; Atmospheric sciences; Soil science; Ecosystem; Carbon dioxide; Geomorphology; Ecology; Geography; Soil water","score_opus":0.01796092893934149,"score_gpt":0.2545279564342216,"score_spread":0.23656702749488012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093339808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99928373,0.000059783637,0.00008650611,0.0000030985673,4.6413817e-7,4.7008066e-7,0.00039067716,0.000004173413,0.00017102665],"genre_scores_gemma":[0.9986658,0.000086928325,0.00010144455,0.0000032212424,0.0000024708984,0.0000024196015,0.0010387148,0.0000036478664,0.00009539972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994636,0.000009540219,0.000006371347,0.00001582561,0.00000922547,0.000012800701],"domain_scores_gemma":[0.9995702,0.00012693625,0.00012866744,0.000059397396,0.00006552327,0.000049221322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022107527,0.00027352574,0.000230731,0.001402499,0.00027476152,0.00062679965,0.0002623771,0.00022325112,0.00095345086],"category_scores_gemma":[0.00066132133,0.00015895085,0.00033595125,0.0013171271,0.00037101455,0.00040237396,0.00055512745,0.00018023617,0.00015829307],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016862794,0.000015634452,0.98445976,0.00003186978,0.00018812201,0.00013799273,0.00048636962,0.0041437675,0.0025809868,0.00023148186,0.00012557827,0.0074297837],"study_design_scores_gemma":[0.0000023752666,0.00001532237,0.99678504,0.0000056507315,0.000031529697,0.0000615943,0.00012319608,0.0019918974,0.00058483984,0.00010079981,0.00029244903,0.000005303705],"about_ca_topic_score_codex":0.007485876,"about_ca_topic_score_gemma":0.013594921,"teacher_disagreement_score":0.007485876,"about_ca_system_score_codex":0.00031259793,"about_ca_system_score_gemma":0.00011803553,"threshold_uncertainty_score":0.014884591},"labels":[],"label_agreement":null},{"id":"W2093429038","doi":"10.1029/2007gl031474","title":"Recent Northern Hemisphere snow cover extent trends and implications for the snow‐albedo feedback","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":435,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos; University of Northern British Columbia","funders":"","keywords":"Northern Hemisphere; Albedo (alchemy); Climatology; Snow; Snow line; Latitude; Snow cover; Spring (device); Anomaly (physics); Environmental science; Physical geography; Geology; Geography","score_opus":0.05316503861263689,"score_gpt":0.31194167763542474,"score_spread":0.25877663902278786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093429038","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965528,0.00048798634,0.0001370988,0.0005599018,0.000010404152,0.000002092258,0.0003442324,0.000010455476,0.0018949655],"genre_scores_gemma":[0.99919945,0.00027330202,0.00006887853,0.000037029266,0.000022134816,0.0000011883019,0.0001582804,0.0000022874974,0.00023740159],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999559,0.000008927744,0.0000032909961,0.000011235703,0.000008714405,0.000011913896],"domain_scores_gemma":[0.9997075,0.00007525058,0.000089998844,0.000015164395,0.00007094769,0.000041171832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033686945,0.00010678955,0.00014068816,0.00034983875,0.00019976456,0.00038685126,0.00011617951,0.00016993008,0.0019955423],"category_scores_gemma":[0.0009736969,0.0001054171,0.00013783103,0.0004206993,0.00032443463,0.00034453627,0.00013791912,0.00015599276,0.00012694544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034185627,0.000041170646,0.95289814,0.00007194957,0.000085978034,0.00032532998,0.0006496926,0.002295617,0.009486329,0.0009367171,0.0009273641,0.031939887],"study_design_scores_gemma":[0.0000032206267,0.000013232441,0.9982797,0.0000042626834,0.000010020494,0.000029097311,0.000096209085,0.0005185809,0.00020423793,0.00019040138,0.0006491321,0.00000195675],"about_ca_topic_score_codex":0.013635643,"about_ca_topic_score_gemma":0.030280307,"teacher_disagreement_score":0.013635643,"about_ca_system_score_codex":0.0005629787,"about_ca_system_score_gemma":0.00030257623,"threshold_uncertainty_score":0.027112544},"labels":[],"label_agreement":null},{"id":"W2093461514","doi":"10.1029/2006gl028420","title":"Effect of flow depth and velocity on the scales of macroturbulent structures in gravel‐bed rivers","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"","keywords":"Geology; Flow (mathematics); Range (aeronautics); Scaling; Flow velocity; Sampling (signal processing); Geodesy; Hydrology (agriculture); Geotechnical engineering; Geometry; Mechanics; Physics; Mathematics; Optics; Materials science","score_opus":0.011013433946185926,"score_gpt":0.2670145170242006,"score_spread":0.25600108307801467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093461514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995333,0.000064086984,0.00023360742,0.000004774088,6.2343537e-7,0.000001816216,0.00002260937,0.0000066484877,0.00013267348],"genre_scores_gemma":[0.99970645,0.000032416916,0.00016543298,0.000005070419,0.0000014392159,0.0000023908012,0.000035873974,0.0000030181718,0.00004790453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998117,0.00004891894,0.0000192563,0.0000506025,0.00003198748,0.00003752205],"domain_scores_gemma":[0.99722147,0.0013701546,0.00079385703,0.00020178859,0.0001107928,0.0003019359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052485167,0.00017496891,0.00020255138,0.00045434968,0.00026285936,0.0007411611,0.0001408816,0.00021229424,0.0006166056],"category_scores_gemma":[0.003301418,0.00037716984,0.0001906635,0.0002446481,0.00069942744,0.00047449954,0.00068321684,0.0003809322,0.00005363527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001884264,0.00012359461,0.77743185,0.00008446155,0.00018689856,0.00029142998,0.00078914367,0.007899656,0.18507689,0.00052391936,0.00011648716,0.025591347],"study_design_scores_gemma":[0.00001280129,0.00014879022,0.9944554,0.000003826228,0.00001829909,0.000046240064,0.000101639176,0.0016880252,0.003355635,0.00008516067,0.00007510802,0.000009182391],"about_ca_topic_score_codex":0.0025977928,"about_ca_topic_score_gemma":0.00275901,"teacher_disagreement_score":0.0025977928,"about_ca_system_score_codex":0.00032858926,"about_ca_system_score_gemma":0.00017485033,"threshold_uncertainty_score":0.005165398},"labels":[],"label_agreement":null},{"id":"W2093509809","doi":"10.1029/2006gl027087","title":"A new hurricane wind retrieval algorithm for SAR images","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Wind speed; Eye; Scatterometer; Remote sensing; Meteorology; Synthetic aperture radar; Interpolation (computer graphics); Wind direction; Geology; Maximum sustained wind; Radar; Environmental science; Tropical cyclone; Geodesy; Computer science; Wind gradient; Image (mathematics); Geography; Artificial intelligence","score_opus":0.02083451311789785,"score_gpt":0.27745120879876195,"score_spread":0.2566166956808641,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093509809","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0033184472,0.00011443567,0.99542516,0.000031763095,0.000041507283,0.000029505914,0.000035858546,0.0005334489,0.00046986906],"genre_scores_gemma":[0.019571887,0.00017094043,0.9771145,0.000042491276,0.00005400076,0.00007592767,0.00027489752,0.00010682742,0.002588582],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997507,0.000022073498,0.000016065553,0.000064458865,0.00012612443,0.00002065208],"domain_scores_gemma":[0.99975914,0.000035035482,0.000022827024,0.000037126265,0.0001334236,0.00001238473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033671968,0.0005678415,0.0005773979,0.0007202468,0.000374769,0.0007509717,0.000746227,0.000547526,0.0024750165],"category_scores_gemma":[0.0008347307,0.00040344,0.0005065188,0.00068537804,0.00021846025,0.001107952,0.00061376573,0.00072998874,0.0017326873],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007658281,0.000033869077,0.00055806164,0.000097301876,0.000065951164,0.00006361156,0.00006299338,0.056044012,0.06755673,0.007336741,0.00516791,0.8629362],"study_design_scores_gemma":[0.000047821508,0.00005167706,0.00083519955,0.000012637659,0.000021314716,0.00017368457,0.000020506686,0.96523386,0.015099256,0.004017753,0.014460201,0.000025999383],"about_ca_topic_score_codex":0.0021642293,"about_ca_topic_score_gemma":0.003347137,"teacher_disagreement_score":0.0024750165,"about_ca_system_score_codex":0.00030596703,"about_ca_system_score_gemma":0.0004953525,"threshold_uncertainty_score":0.0082798},"labels":[],"label_agreement":null},{"id":"W2093835006","doi":"10.1029/2000gl012803","title":"Solar illumination as cause of the equinoctial preference for geomagnetic activity","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Earth's magnetic field; Magnetosphere; Ionosphere; Geomagnetic storm; Solar wind; Geomagnetic secular variation; Interplanetary magnetic field; Equinox; Geophysics; Southern Hemisphere; Substorm; Atmospheric sciences; Physics; Ring current; Solstice; Northern Hemisphere; Geology; Latitude; Geodesy; Magnetic field; Astronomy","score_opus":0.03847293953090996,"score_gpt":0.31270678173412864,"score_spread":0.27423384220321867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093835006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99506724,0.00057081133,0.0006998077,0.000059129427,0.000012995478,0.000009594792,0.00009924485,0.000021810141,0.0034593458],"genre_scores_gemma":[0.99953735,0.000072319446,0.000055601642,0.000013552948,0.0000049662185,0.0000017869268,0.00003385971,0.0000042524043,0.0002763606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999199,0.000015957297,0.000004433316,0.000022838249,0.000011853877,0.000025037192],"domain_scores_gemma":[0.99973816,0.0000725824,0.000079341575,0.000033181906,0.000036705875,0.000039984843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012539765,0.00010327274,0.00022020644,0.00020322631,0.00016543368,0.00032470847,0.00013027804,0.00017183644,0.0016379303],"category_scores_gemma":[0.00034933584,0.000080671765,0.00016535452,0.00023958269,0.00022399011,0.00011820042,0.00023027233,0.00020012067,0.00017573753],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011640599,0.00013922693,0.788171,0.000110301335,0.00008463003,0.0007689923,0.0004343425,0.001055538,0.17158774,0.0009538919,0.00048372408,0.03504654],"study_design_scores_gemma":[0.0000054308084,0.00008170382,0.9933609,0.000004220955,0.000014259929,0.0002555636,0.00012842347,0.00055160635,0.004757737,0.00020305665,0.00063207396,0.000005049505],"about_ca_topic_score_codex":0.0016545636,"about_ca_topic_score_gemma":0.0017670047,"teacher_disagreement_score":0.0016545636,"about_ca_system_score_codex":0.00024945362,"about_ca_system_score_gemma":0.000100694124,"threshold_uncertainty_score":0.005479455},"labels":[],"label_agreement":null},{"id":"W2093836617","doi":"10.1029/2000gl012121","title":"Warming asymmetry in climate change simulations","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":475,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Northern Hemisphere; Climatology; Southern Hemisphere; Global warming; Latitude; Climate change; Asymmetry; Environmental science; Climate model; Sea ice; Effects of global warming on oceans; Effects of global warming; Ocean heat content; Atmospheric sciences; Sea surface temperature; Oceanography; Geology; Physics","score_opus":0.08266891558762099,"score_gpt":0.34443970875881336,"score_spread":0.26177079317119234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093836617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9699135,0.00015278418,0.013209735,0.00033775193,0.000066483335,0.000086774475,0.0024132393,0.00040801358,0.013411764],"genre_scores_gemma":[0.9961356,0.00005078125,0.0026192737,0.000038031725,0.000010039917,0.000051306786,0.00063440524,0.000044429944,0.00041613664],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992587,0.00039866182,0.00004780542,0.00011284586,0.00009246452,0.0000895493],"domain_scores_gemma":[0.9980964,0.0011518883,0.00018005371,0.00022793135,0.00022960953,0.000114143455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016653206,0.000420396,0.00060439936,0.00064258964,0.0004037357,0.0009289241,0.0008768841,0.0008736087,0.0027345198],"category_scores_gemma":[0.008271696,0.00034962187,0.00060986506,0.0008863026,0.00032022072,0.0010904762,0.0008189057,0.00086638296,0.00020506125],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013356283,0.000028243756,0.010771449,0.000030519128,0.000052613475,0.000047465677,0.000052397212,0.97888285,0.0006007436,0.004335249,0.0005305003,0.0045344974],"study_design_scores_gemma":[0.00007788851,0.00004633187,0.0058063553,0.000010086689,0.00003787871,0.00001741433,0.000029338058,0.98773116,0.00077541015,0.004092441,0.0013568841,0.000018777466],"about_ca_topic_score_codex":0.016112767,"about_ca_topic_score_gemma":0.009401742,"teacher_disagreement_score":0.016112767,"about_ca_system_score_codex":0.0011962879,"about_ca_system_score_gemma":0.0007007128,"threshold_uncertainty_score":0.032037973},"labels":[],"label_agreement":null},{"id":"W2093901385","doi":"10.1029/2008gl033561","title":"A summer phytoplankton bloom triggered by high wind events in the Labrador Sea, July 2006","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Photic zone; Phytoplankton; Bloom; Mixed layer; Oceanography; Environmental science; Ekman transport; Nutrient; Algal bloom; New production; Spring bloom; Nitrate; Storm; Ekman layer; Chlorophyll a; Upwelling; Geology; Chemistry; Ecology; Biology","score_opus":0.029106033142099235,"score_gpt":0.2568652516003232,"score_spread":0.22775921845822397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2093901385","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999665,0.00002051045,0.000041313757,0.000019318788,0.0000017689537,0.0000027512353,0.00010210481,0.000019287749,0.00012794495],"genre_scores_gemma":[0.9995121,0.000029838076,0.00012932178,0.000011236791,0.0000025214213,0.000003462768,0.00021029127,0.0000025314203,0.00009882366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999254,0.000012046243,0.0000071031363,0.000014141627,0.000011048183,0.000030146655],"domain_scores_gemma":[0.9998357,0.00002307933,0.000060703038,0.000014561533,0.00002682432,0.00003911784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021559701,0.00033985847,0.00034861275,0.00026755244,0.0004887051,0.00049097737,0.00027171153,0.00038800933,0.00038137916],"category_scores_gemma":[0.0002707387,0.00023801214,0.00038758677,0.00029558348,0.00026897527,0.0002342372,0.00025258135,0.00020104172,0.00010392575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020012711,0.0002731284,0.8499881,0.00015621509,0.00022920976,0.0030410152,0.00044594108,0.022372182,0.110061266,0.00026669304,0.0013155853,0.009849384],"study_design_scores_gemma":[0.000084144696,0.0003743947,0.9622954,0.000009124684,0.000084547944,0.00024640886,0.000410509,0.023893157,0.012005855,0.0000859837,0.00048103195,0.000029393581],"about_ca_topic_score_codex":0.03424915,"about_ca_topic_score_gemma":0.048451357,"teacher_disagreement_score":0.03424915,"about_ca_system_score_codex":0.001271534,"about_ca_system_score_gemma":0.0006247914,"threshold_uncertainty_score":0.06809962},"labels":[],"label_agreement":null},{"id":"W2094345536","doi":"10.1029/2008gl034457","title":"Reduced ice thickness in Arctic Transpolar Drift favors rapid ice retreat","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":211,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Sea ice; Geology; Arctic ice pack; Drift ice; Antarctic sea ice; Sea ice thickness; Climatology","score_opus":0.030912785072392222,"score_gpt":0.2641635414793768,"score_spread":0.2332507564069846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094345536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994566,0.00008156921,0.000038572292,0.000011047365,0.0000030409383,8.6563074e-7,0.000053522,0.00000294142,0.00035179724],"genre_scores_gemma":[0.9996031,0.000048930702,0.000039151284,0.0000131084225,0.000003982265,0.0000015922245,0.00013481885,0.0000028950876,0.00015255518],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.000011122337,0.00000506403,0.000018430308,0.000011942055,0.000018265931],"domain_scores_gemma":[0.99977034,0.000029906132,0.00009386482,0.000011193322,0.000038642916,0.000056072124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028906108,0.0001749926,0.00022837034,0.0005128918,0.00024214071,0.0005570074,0.00011991317,0.00027620766,0.0009983529],"category_scores_gemma":[0.00058459135,0.00018077368,0.00013456275,0.00029885006,0.0002567182,0.0002140871,0.0002591422,0.00019180347,0.0002572945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082133466,0.00006801572,0.93689734,0.00003551593,0.000053788288,0.00043046128,0.00041338295,0.0005304331,0.05176086,0.00013985898,0.00029143027,0.0085575655],"study_design_scores_gemma":[0.00000329387,0.000043228803,0.998464,0.0000025371503,0.0000046875734,0.00014608003,0.000100756435,0.00016529199,0.00086302776,0.000029912435,0.00017486156,0.0000022867248],"about_ca_topic_score_codex":0.005517321,"about_ca_topic_score_gemma":0.008916982,"teacher_disagreement_score":0.005517321,"about_ca_system_score_codex":0.0002618713,"about_ca_system_score_gemma":0.00019908439,"threshold_uncertainty_score":0.010970414},"labels":[],"label_agreement":null},{"id":"W2094412572","doi":"10.1029/2007gl033005","title":"Interactions of wind‐transported snow with a rift in the Ross Ice Shelf, Antarctica","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Arctic Sciences","keywords":"Geology; Rift; Ice shelf; Snow; Firn; Oceanography; Antarctic sea ice; Sea ice; Cryosphere; Geomorphology","score_opus":0.05581940151120757,"score_gpt":0.2918659752764753,"score_spread":0.23604657376526772,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094412572","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967575,0.0000495074,0.000023587561,0.000017667042,0.0000014176203,0.0000018850021,0.00003874147,0.0000023031394,0.00018911748],"genre_scores_gemma":[0.99970585,0.00006074976,0.00005033993,0.0000092325445,0.0000030183112,0.00000253689,0.00007333916,0.0000018145489,0.00009306416],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999305,0.00002492306,0.000003745098,0.000010430319,0.000009549817,0.00002090131],"domain_scores_gemma":[0.9997969,0.000049886512,0.00005622071,0.000009417914,0.000028047572,0.00005957387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019468706,0.00025696403,0.0003067255,0.00040090352,0.00054565875,0.00051187986,0.0001635255,0.00037673194,0.00080317724],"category_scores_gemma":[0.00039703574,0.00017565678,0.0002823012,0.00029443848,0.00028205343,0.00023836052,0.00038314657,0.00015357704,0.00015527067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005399053,0.00009412474,0.9536415,0.00007434272,0.00025373432,0.00097154314,0.00060551555,0.010557121,0.025073687,0.00017361392,0.0005613925,0.0074536386],"study_design_scores_gemma":[0.000017816046,0.00013878864,0.9919214,0.0000074871323,0.00003441992,0.00008686281,0.0004990748,0.006467658,0.000463583,0.00007933023,0.00027547774,0.000008092377],"about_ca_topic_score_codex":0.01892785,"about_ca_topic_score_gemma":0.03745799,"teacher_disagreement_score":0.01892785,"about_ca_system_score_codex":0.00047006228,"about_ca_system_score_gemma":0.0002794136,"threshold_uncertainty_score":0.037635326},"labels":[],"label_agreement":null},{"id":"W2094448605","doi":"10.1029/2005gl023451","title":"Precipitation forecast skill of numerical weather prediction models and radar nowcasts","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":146,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Workforce Development for Teachers and Scientists","keywords":"Nowcasting; Quantitative precipitation forecast; Radar; Precipitation; Advection; Meteorology; Numerical weather prediction; Forecast skill; Climatology; Environmental science; Computer science; Geology; Geography","score_opus":0.051805432181205494,"score_gpt":0.2896427928643523,"score_spread":0.23783736068314681,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094448605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.978671,0.00024985324,0.012423131,0.0006341252,0.00008135867,0.000022924902,0.0011764346,0.00031261306,0.006428529],"genre_scores_gemma":[0.9969374,0.000061100705,0.0014129812,0.000038597118,0.0000230236,0.000006091397,0.0010080795,0.00003676373,0.0004759259],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990777,0.00022444605,0.00007015579,0.0002821993,0.00020921789,0.00013625252],"domain_scores_gemma":[0.9909315,0.0045642154,0.0012191739,0.0012004828,0.0015383416,0.00054619287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033276821,0.0003241749,0.0003992034,0.00076246646,0.00017563987,0.0014133918,0.0005742153,0.0008469175,0.0014798217],"category_scores_gemma":[0.024193352,0.0003248983,0.00044106852,0.00055287796,0.00048884447,0.0025807223,0.0009952427,0.000879564,0.00045800259],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010367914,0.00021474571,0.34907612,0.00012211292,0.00039491904,0.00017269758,0.000537114,0.5704682,0.0045877625,0.008980023,0.0046386337,0.05977085],"study_design_scores_gemma":[0.00008690119,0.00016382866,0.24198481,0.00004021849,0.00006342826,0.00007146688,0.00015985404,0.74714607,0.0032868825,0.0055395337,0.0013854501,0.000071538074],"about_ca_topic_score_codex":0.013868044,"about_ca_topic_score_gemma":0.008320321,"teacher_disagreement_score":0.013868044,"about_ca_system_score_codex":0.00073677883,"about_ca_system_score_gemma":0.000652452,"threshold_uncertainty_score":0.027574599},"labels":[],"label_agreement":null},{"id":"W2094479196","doi":"10.1029/2004gl019536","title":"Determination of apparent quantum yield spectra of DMS photo‐degradation in an in situ iron‐induced Northeast Pacific Ocean bloom","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Quantum yield; Bloom; Phytoplankton; Yield (engineering); Oceanography; Photodissociation; Degradation (telecommunications); Deep sea; Pacific ocean; In situ; Indian ocean; Environmental science; Chemistry; Photochemistry; Geology; Materials science; Fluorescence; Optics","score_opus":0.036032213575479526,"score_gpt":0.26965287646335984,"score_spread":0.2336206628878803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094479196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99935335,0.000022832908,0.00032250042,0.0000047929257,6.6368796e-7,0.0000022897311,0.00007353268,0.000004162399,0.00021584526],"genre_scores_gemma":[0.9986111,0.000051819505,0.00064079085,0.000008797306,0.000001080449,0.0000070648907,0.00019944267,0.0000041562344,0.000475799],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996924,0.000003533401,0.0000014391987,0.000010171368,0.000009585673,0.000006129976],"domain_scores_gemma":[0.99990094,0.000028098202,0.000024487712,0.0000068628287,0.000023443523,0.00001616387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009322271,0.00018155065,0.00012451105,0.00015380462,0.0002032736,0.00012730206,0.000108543085,0.00016209093,0.00045522497],"category_scores_gemma":[0.00020734387,0.00015884146,0.000117096075,0.00010246386,0.00022100277,0.00011701727,0.00009680262,0.00025512144,0.00006653564],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001263531,0.000010278014,0.018531803,0.000020191465,0.000008473562,0.000038350376,0.000073108524,0.00017956494,0.9800812,0.000022894596,0.000013845598,0.00089387124],"study_design_scores_gemma":[0.000008463881,0.00019273868,0.46892825,0.0000033037109,0.000021361415,0.00012619454,0.00010058285,0.0026739435,0.5275443,0.000043228843,0.00034979504,0.00000780483],"about_ca_topic_score_codex":0.006433361,"about_ca_topic_score_gemma":0.007931714,"teacher_disagreement_score":0.006433361,"about_ca_system_score_codex":0.00034710945,"about_ca_system_score_gemma":0.00012602698,"threshold_uncertainty_score":0.012791872},"labels":[],"label_agreement":null},{"id":"W2094552930","doi":"10.1029/2008gl034482","title":"Long‐term trends in sunshine duration over Yunnan‐Guizhou Plateau in Southwest China for 1961–2005","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Sunshine duration; Plateau (mathematics); Climatology; China; Environmental science; Latitude; Climate change; Duration (music); Geography; Precipitation; Meteorology; Geology; Oceanography","score_opus":0.03684028279607373,"score_gpt":0.29606547038070585,"score_spread":0.25922518758463214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094552930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983583,0.00022624755,0.000058960064,0.000029478048,0.0000028672578,0.0000034008117,0.0010305854,0.000008076284,0.0002820515],"genre_scores_gemma":[0.9970874,0.00013036592,0.00008881701,0.000011122903,0.0000056009803,0.000007801155,0.0023100288,0.0000023789187,0.00035643307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989355,0.000011375982,0.000014242821,0.000031381474,0.000022694874,0.000026877267],"domain_scores_gemma":[0.99958915,0.000040923172,0.000131393,0.000025672058,0.00013508633,0.00007776154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031245017,0.0002839957,0.00020763963,0.0009283469,0.00029350992,0.00035465945,0.00020422884,0.00020586661,0.00054668065],"category_scores_gemma":[0.00046462388,0.00009884762,0.0002887548,0.0016261587,0.00014092997,0.00021261715,0.00027186182,0.00014328596,0.000097949],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049701852,0.000007694093,0.99163556,0.00003741945,0.000090837,0.0001411351,0.00045575981,0.00047563284,0.002550437,0.000035885343,0.00024299366,0.0042770086],"study_design_scores_gemma":[8.5976507e-7,0.000005803838,0.99940467,0.0000017081064,0.000008636665,0.000013329802,0.00007048345,0.00011617566,0.000052588628,0.0000023486555,0.00032187905,0.0000014465272],"about_ca_topic_score_codex":0.11134149,"about_ca_topic_score_gemma":0.18730095,"teacher_disagreement_score":0.11134149,"about_ca_system_score_codex":0.0009552786,"about_ca_system_score_gemma":0.00054477167,"threshold_uncertainty_score":0.22138679},"labels":[],"label_agreement":null},{"id":"W2094986284","doi":"10.1029/2005gl024244","title":"The Brewer reference triad","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Triad (sociology); Environmental science; Calibration; Remote sensing; Statistics; Geology; Mathematics","score_opus":0.04958160829918827,"score_gpt":0.3095569691124595,"score_spread":0.2599753608132712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094986284","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.024011897,0.05742763,0.09069987,0.023768054,0.012170303,0.0021720286,0.115957856,0.008373638,0.66541874],"genre_scores_gemma":[0.082788765,0.026052438,0.11058333,0.0069821407,0.0019728274,0.0035556147,0.2573173,0.0029201787,0.50782746],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.98904055,0.0021272548,0.0009905946,0.0013265574,0.0056775287,0.00083747465],"domain_scores_gemma":[0.98400116,0.00049024896,0.0011047379,0.0021148585,0.011708772,0.00058021385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0077631692,0.0012350732,0.0017827478,0.0060745906,0.0029463742,0.0055820984,0.003087271,0.0023701559,0.044880074],"category_scores_gemma":[0.014071153,0.0005003018,0.00063227303,0.007232623,0.0012409325,0.0032484916,0.0042250846,0.002711378,0.06458341],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004445562,0.000121462836,0.008200533,0.0004078071,0.0000629467,0.00027376538,0.0003179909,0.00045065698,0.0030491394,0.0383623,0.75388384,0.19442505],"study_design_scores_gemma":[0.000021811526,0.000052867344,0.005037842,0.00015889294,0.000015945967,0.00019240612,0.000095309,0.00017720414,0.0007607027,0.0025245955,0.990936,0.00002639658],"about_ca_topic_score_codex":0.05035204,"about_ca_topic_score_gemma":0.049570214,"teacher_disagreement_score":0.05035204,"about_ca_system_score_codex":0.0038909563,"about_ca_system_score_gemma":0.008968803,"threshold_uncertainty_score":0.1501388},"labels":[],"label_agreement":null},{"id":"W2094999543","doi":"10.1002/2013gl058650","title":"Changes in global ocean wave heights as projected using multimodel CMIP5 simulations","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":217,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Coupled model intercomparison project; Climatology; Environmental science; Latitude; Northern Hemisphere; Climate change; Southern Hemisphere; Climate model; Significant wave height; Tropics; Submarine pipeline; Representative Concentration Pathways; Wind wave; Atmospheric sciences; Geology; Oceanography","score_opus":0.05991074702238255,"score_gpt":0.31667655674914486,"score_spread":0.25676580972676233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2094999543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98701525,0.00006226534,0.0034803418,0.00019328576,0.000028039398,0.000021433145,0.00615849,0.00018693245,0.0028539358],"genre_scores_gemma":[0.9909156,0.000085689535,0.0030850503,0.00004731477,0.000009248805,0.000045201916,0.0055033956,0.000026573192,0.00028183762],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985194,0.000034281944,0.000010444967,0.000050745843,0.000021766524,0.000030763826],"domain_scores_gemma":[0.9997017,0.00009619529,0.000051395185,0.00005176273,0.00006865686,0.000030330855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066834973,0.0005401629,0.00019063696,0.0005032938,0.00022670029,0.0005393701,0.00050952134,0.00050508714,0.0011955963],"category_scores_gemma":[0.0014832456,0.00022691807,0.00076799904,0.00090517476,0.00015364046,0.0006231065,0.0003089943,0.00045481423,0.00024274357],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017999351,0.00009207612,0.092777826,0.00006990593,0.00022758673,0.00009779314,0.00004820445,0.88870233,0.002091063,0.0015704413,0.0023876124,0.011755199],"study_design_scores_gemma":[0.00010828924,0.0000850062,0.0821195,0.000027868458,0.00008735133,0.0000352938,0.00011768303,0.911841,0.0024104104,0.0012216746,0.0018963903,0.00004947334],"about_ca_topic_score_codex":0.03248931,"about_ca_topic_score_gemma":0.017270505,"teacher_disagreement_score":0.03248931,"about_ca_system_score_codex":0.0007787751,"about_ca_system_score_gemma":0.00070749235,"threshold_uncertainty_score":0.06460041},"labels":[],"label_agreement":null},{"id":"W2095119391","doi":"10.1002/2014gl062969","title":"Enhanced sensitivity of oceanic CO<sub>2</sub> uptake to dust deposition by iron‐light colimitation","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; McGill University","keywords":"Phytoplankton; Biogeochemical cycle; Deposition (geology); Photosynthesis; Nutrient; Iron fertilization; Nitrate; Geotraces; Environmental chemistry; Environmental science; Oceanography; Chemistry; Seawater; Botany; Ecology; Geology; Biology","score_opus":0.025585790427298,"score_gpt":0.26046045238884025,"score_spread":0.23487466196154225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095119391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988073,0.0000910324,0.0005671989,0.000057353383,0.0000059415743,0.000003320453,0.000082171384,0.000017927634,0.0003677328],"genre_scores_gemma":[0.9997961,0.000020226202,0.00006212031,0.000016777036,0.0000014996408,0.0000013595044,0.000029756035,0.0000031657692,0.00006900958],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998518,0.00002723149,0.000010431628,0.000050117003,0.000025725472,0.00003454357],"domain_scores_gemma":[0.99956053,0.0001874848,0.00008801224,0.00007421686,0.0000451038,0.000044504624],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002058468,0.0002878115,0.0003291417,0.00017837418,0.00013949434,0.00048713846,0.00028041622,0.00039209874,0.001028399],"category_scores_gemma":[0.0005735696,0.00018347082,0.00023449752,0.00015385656,0.00031906605,0.0001792213,0.00040638904,0.00031564807,0.00010884854],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008424168,0.00005866467,0.08992222,0.00008123357,0.00011450615,0.00025477618,0.000065828244,0.0066753244,0.8986663,0.0002579941,0.0001244264,0.002936171],"study_design_scores_gemma":[0.000038186925,0.00017002579,0.6203851,0.000006240399,0.0000696769,0.00019039461,0.00014380075,0.033081308,0.34471875,0.00057960814,0.0005949046,0.00002202746],"about_ca_topic_score_codex":0.0069466205,"about_ca_topic_score_gemma":0.0029080773,"teacher_disagreement_score":0.0069466205,"about_ca_system_score_codex":0.00048471347,"about_ca_system_score_gemma":0.00014882712,"threshold_uncertainty_score":0.013812363},"labels":[],"label_agreement":null},{"id":"W2095535998","doi":"10.1029/2006gl029015","title":"Amplitude loss of sonic waveform due to source coupling to the medium","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Canadian Natural Resources Limited; Natural Resources Canada; U.S. Geological Survey; U.S. Department of Energy","keywords":"Attenuation; Amplitude; Waveform; Coupling (piping); Acoustics; Geology; Borehole; Optics; Physics; Materials science; Geotechnical engineering","score_opus":0.02372934883274949,"score_gpt":0.3021665680312994,"score_spread":0.2784372191985499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095535998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9560442,0.00021510478,0.038158175,0.00010918084,0.000033148885,0.000035622415,0.00026101383,0.00050866883,0.004634872],"genre_scores_gemma":[0.9941156,0.00009936661,0.0040732385,0.00003086135,0.000009820712,0.000012863011,0.0002506751,0.00008015826,0.0013273612],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99976724,0.00001617423,0.000009123611,0.000036153742,0.00013834653,0.00003287726],"domain_scores_gemma":[0.9993548,0.00024678325,0.00010028239,0.00008665023,0.00016531422,0.00004614933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022388954,0.00030035424,0.0002092056,0.0005782959,0.0001408115,0.00035493882,0.0003145672,0.00025255152,0.002432502],"category_scores_gemma":[0.0017306027,0.00019993797,0.00013604178,0.00052630797,0.0003800439,0.00040596604,0.00048334268,0.00048136926,0.00032157355],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006324492,0.000045170942,0.021446051,0.00015113477,0.000059173883,0.0007004384,0.0004008207,0.0032147118,0.8912065,0.00068553997,0.0005146784,0.08094337],"study_design_scores_gemma":[0.000056247518,0.0005077081,0.3449449,0.000033570148,0.0001422124,0.0022133205,0.00041590314,0.029988078,0.6149808,0.001127241,0.0055285697,0.00006145381],"about_ca_topic_score_codex":0.0008198672,"about_ca_topic_score_gemma":0.0006909671,"teacher_disagreement_score":0.002432502,"about_ca_system_score_codex":0.00022565697,"about_ca_system_score_gemma":0.00012363413,"threshold_uncertainty_score":0.008137524},"labels":[],"label_agreement":null},{"id":"W2095555068","doi":"10.1029/2007gl031018","title":"Long term climate implications of 2050 emission reduction targets","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Term (time); Environmental science; Reduction (mathematics); Climatology; Climate change; Atmospheric sciences; Geology; Oceanography; Physics","score_opus":0.017372558755392474,"score_gpt":0.30298316520161017,"score_spread":0.2856106064462177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095555068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9482938,0.0015699617,0.011992014,0.0026404017,0.0002336673,0.00003389303,0.0027099976,0.00029615432,0.03223013],"genre_scores_gemma":[0.9971814,0.00025498884,0.0009742112,0.00017269606,0.000009604345,0.000025062021,0.000626549,0.00002125974,0.0007343048],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997589,0.00008417961,0.000009472075,0.000024226692,0.000046704678,0.000076517135],"domain_scores_gemma":[0.9996493,0.0001459959,0.000052506468,0.000017053577,0.00008850607,0.000046595233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010507136,0.00048488143,0.0003157724,0.00030627375,0.0006498518,0.0012864113,0.0005843546,0.0010291552,0.0021889263],"category_scores_gemma":[0.001824712,0.00019524772,0.00063060364,0.00042452975,0.00031805443,0.00096422184,0.00084321026,0.00075876765,0.00021243357],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057242654,0.000119619624,0.02806968,0.00017557191,0.00021864513,0.00052614434,0.000119302895,0.9160437,0.0044770027,0.029582802,0.0070245345,0.013070593],"study_design_scores_gemma":[0.00017973455,0.0006043844,0.058306027,0.00010167668,0.00043745592,0.00019184056,0.00096121244,0.87348217,0.004962391,0.04874743,0.011855384,0.00017036329],"about_ca_topic_score_codex":0.01961672,"about_ca_topic_score_gemma":0.016009282,"teacher_disagreement_score":0.01961672,"about_ca_system_score_codex":0.0016730186,"about_ca_system_score_gemma":0.0010122928,"threshold_uncertainty_score":0.0390051},"labels":[],"label_agreement":null},{"id":"W2095557402","doi":"10.1029/2000gl011741","title":"Minimum relative entropy: Theory and application to surface temperature reconstruction from borehole temperature measurements","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"A priori and a posteriori; Borehole; Entropy (arrow of time); Kullback–Leibler divergence; Inverse problem; Inverse; Environmental science; Geology; Thermodynamics; Mathematics; Statistics; Physics; Geometry; Mathematical analysis; Geotechnical engineering","score_opus":0.03261086563632225,"score_gpt":0.280583792306994,"score_spread":0.24797292667067172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095557402","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.008393814,0.00053179904,0.98981726,0.00020995874,0.000026825091,0.000009892871,0.000043559117,0.000086161635,0.00088086457],"genre_scores_gemma":[0.61558056,0.0022726597,0.3776637,0.00022742304,0.0005252888,0.00015473063,0.00050460093,0.00021027817,0.0028608125],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989448,0.00043314364,0.00006656145,0.00019564244,0.00029126572,0.000068596964],"domain_scores_gemma":[0.9925011,0.0061194277,0.0004937054,0.00040984357,0.00038016596,0.000095815056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00316356,0.00065554766,0.0011198,0.0020292096,0.00048535515,0.0012407423,0.0012389477,0.0010171047,0.0009642885],"category_scores_gemma":[0.013241158,0.00058365555,0.0008750478,0.0014306764,0.0023112602,0.0025632225,0.0017775071,0.0014735745,0.00022573401],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008749834,0.00004388847,0.003221608,0.00025509758,0.0001353106,0.00019362582,0.00016651633,0.69752717,0.0047332267,0.19234939,0.0009491322,0.1003376],"study_design_scores_gemma":[0.000004872699,0.000023489254,0.0009374052,0.000022581555,0.00000845593,0.00007786332,0.00001021816,0.9087221,0.0012503152,0.08825292,0.0006645404,0.000025353167],"about_ca_topic_score_codex":0.0014032592,"about_ca_topic_score_gemma":0.0008453248,"teacher_disagreement_score":0.00316356,"about_ca_system_score_codex":0.000716428,"about_ca_system_score_gemma":0.00051929965,"threshold_uncertainty_score":0.016730726},"labels":[],"label_agreement":null},{"id":"W2095658930","doi":"10.1002/2013gl058761","title":"Local spring warming drives earlier river‐ice breakup in a large Arctic delta","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; Wilfrid Laurier University; University of Alberta; Simon Fraser University","funders":"Natural Resources Canada","keywords":"Arctic; Environmental science; Arctic ice pack; Sea ice; Snow; Breakup; Cryosphere; Spring (device); Climatology; Delta; River delta; Oceanography; Global warming; Arctic sea ice decline; Climate change; Antarctic sea ice; Geology","score_opus":0.014579756299274535,"score_gpt":0.2566112370488731,"score_spread":0.24203148074959857,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095658930","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99965715,0.0000151895965,0.000023396069,0.000010488436,0.0000010206292,8.002458e-7,0.000061463805,0.0000028181414,0.00022763405],"genre_scores_gemma":[0.9997886,0.000014668542,0.000020843749,0.000006392719,9.974826e-7,0.0000013600959,0.000067179164,0.0000011160946,0.000098893055],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999541,0.000007243255,0.0000032286016,0.000019512674,0.0000049606147,0.000010877167],"domain_scores_gemma":[0.9998191,0.000029232478,0.000059947073,0.000016131688,0.000032955566,0.000042540712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012516971,0.00009501424,0.00015086144,0.0003282164,0.0002735774,0.00042656512,0.000109031884,0.00013989836,0.0010596092],"category_scores_gemma":[0.00026892757,0.00009809117,0.00014025658,0.0002728665,0.00017806794,0.00012852985,0.00024363857,0.00012564805,0.0001118897],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010222046,0.000039450002,0.98541486,0.000013352223,0.000036022855,0.000110353416,0.0002170317,0.00048693086,0.010562856,0.00006112163,0.00017722229,0.002778455],"study_design_scores_gemma":[0.0000014365183,0.00001540108,0.99898297,0.0000018055907,0.0000055644277,0.000018897948,0.00017075552,0.00033958204,0.0003051612,0.000022474016,0.00013485385,0.0000011897326],"about_ca_topic_score_codex":0.013974339,"about_ca_topic_score_gemma":0.030476492,"teacher_disagreement_score":0.013974339,"about_ca_system_score_codex":0.00039577394,"about_ca_system_score_gemma":0.00023280733,"threshold_uncertainty_score":0.027786016},"labels":[],"label_agreement":null},{"id":"W2095982113","doi":"10.1029/2001gl013371","title":"Statistics of the mid‐altitude cusp observed by Polar","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Goddard Space Flight Center","keywords":"Interplanetary magnetic field; Polar; Cusp (singularity); Magnetic reconnection; Geophysics; Latitude; Field line; Ionosphere; Physics; Geology; Solar wind; Geodesy; Plasma; Astronomy; Geometry","score_opus":0.028752251758581766,"score_gpt":0.2724694008199461,"score_spread":0.24371714906136432,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2095982113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989104,0.000045238794,0.00017310772,0.000017278733,0.0000017010403,0.0000016453718,0.00047102207,0.000012471698,0.00036707296],"genre_scores_gemma":[0.9985266,0.000030797117,0.00006701558,0.000005015797,0.0000052443875,0.0000023305765,0.001270033,0.0000036595422,0.000089245485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976605,0.00003894048,0.000021246899,0.00007231302,0.000057165154,0.000044316555],"domain_scores_gemma":[0.9966377,0.0013125177,0.0009925944,0.00034487835,0.00035123836,0.00036108817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037507122,0.00009239734,0.00018984209,0.00083921355,0.00022836096,0.0004649369,0.00015572051,0.00021640123,0.00092922297],"category_scores_gemma":[0.0028628812,0.000117927404,0.0001292052,0.00054072624,0.00028701275,0.00026898785,0.00038563396,0.0002487677,0.0003072116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014146618,0.000008346501,0.9931318,0.000006091988,0.000019620295,0.00007278167,0.00008905176,0.0005525936,0.0021663513,0.000080545986,0.00021788565,0.003513526],"study_design_scores_gemma":[0.0000027085669,0.000041385465,0.99731714,0.0000015082505,0.0000059490726,0.00027225233,0.00012289245,0.0013911787,0.0004698648,0.00005292908,0.0003178114,0.0000044032604],"about_ca_topic_score_codex":0.001767655,"about_ca_topic_score_gemma":0.0020214221,"teacher_disagreement_score":0.001767655,"about_ca_system_score_codex":0.000121815014,"about_ca_system_score_gemma":0.00011149212,"threshold_uncertainty_score":0.003514707},"labels":[],"label_agreement":null},{"id":"W2096146674","doi":"10.1029/2006gl026614","title":"Anomalous pelagic nekton abundance, distribution, and apparent recruitment in the northern California Current in 2004 and 2005","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and fisheries research","field":"Environmental Science","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; National Marine Fisheries Service; Bonneville Power Administration","keywords":"Nekton; Pelagic zone; Upwelling; Productivity; Oceanography; Abundance (ecology); Range (aeronautics); Population; Environmental science; Juvenile; Ecology; Geology; Biology","score_opus":0.030759621144779762,"score_gpt":0.29801338306890707,"score_spread":0.2672537619241273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096146674","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994118,0.00008218396,0.000010345597,0.00002209042,0.0000028049326,0.0000011995363,0.00011184673,0.0000018471244,0.00035579852],"genre_scores_gemma":[0.99904174,0.000090576556,0.000053364798,0.00002058778,0.000003058694,0.000002580965,0.00034407733,0.0000012266769,0.00044276155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998845,0.000009567983,0.000012071165,0.00003647517,0.000026446458,0.00003092001],"domain_scores_gemma":[0.9993315,0.000045999208,0.00029191026,0.00002567959,0.00013808827,0.00016690606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029500015,0.00011528429,0.00016800064,0.00060230016,0.0006044852,0.00060265244,0.00021277391,0.00025271336,0.0006082997],"category_scores_gemma":[0.000826612,0.00018130691,0.000099879246,0.00039260744,0.00024170821,0.00030604753,0.000305988,0.00023699268,0.00007046092],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010982117,0.000029697292,0.99567884,0.000009829676,0.000024499135,0.000101440586,0.0003126289,0.000106673724,0.00050474034,0.00002526142,0.0003956476,0.0027009258],"study_design_scores_gemma":[8.8393864e-7,0.0000068382164,0.9996395,0.0000021731444,0.0000032475903,0.000027807337,0.0001189971,0.000041800045,0.000020055824,0.000004420726,0.00013308029,0.0000011019432],"about_ca_topic_score_codex":0.13431151,"about_ca_topic_score_gemma":0.4588356,"teacher_disagreement_score":0.13431151,"about_ca_system_score_codex":0.0011046323,"about_ca_system_score_gemma":0.00050564687,"threshold_uncertainty_score":0.26705945},"labels":[],"label_agreement":null},{"id":"W2096254420","doi":"10.1029/2001gl014184","title":"Coincidence of the ion precipitation boundary with the HF E region backscatter boundary in the dusk‐midnight sector of the auroral oval","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Communications Research Centre Canada; Western University","funders":"","keywords":"Dusk; Midnight; Ionosphere; Electron precipitation; Geophysics; Geology; Boundary (topology); Precipitation; Atmospheric sciences; Magnetosphere; Meteorology; Physics; Magnetic field; Astronomy","score_opus":0.021397848043782867,"score_gpt":0.2574412551728347,"score_spread":0.23604340712905186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096254420","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99915254,0.000045068366,0.00012267489,0.0000054580823,0.0000016771713,8.698768e-7,0.00003552904,0.000004306045,0.00063181465],"genre_scores_gemma":[0.99966574,0.000023594077,0.0001030143,0.000004429751,0.0000022107804,0.0000010462795,0.0000875855,0.0000014066856,0.00011097045],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.0000072865537,0.000002593877,0.000012043803,0.00000798065,0.00001734392],"domain_scores_gemma":[0.99970454,0.000053692194,0.00009631894,0.00001820149,0.00006501913,0.000062224186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000096717544,0.00006844003,0.00010921159,0.00042819744,0.00020302103,0.0003061917,0.00007093487,0.00012388467,0.0006560889],"category_scores_gemma":[0.00034896968,0.00007304216,0.00004323996,0.00016478018,0.00016102307,0.0001603243,0.00028377565,0.00012686267,0.00012724745],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008392637,0.000031305277,0.85152113,0.00003736674,0.000026753109,0.0006563977,0.0010930509,0.00045876243,0.13083407,0.00048528222,0.0002717642,0.013744866],"study_design_scores_gemma":[0.000006100323,0.00003524378,0.9945732,0.0000050852755,0.000004782179,0.00019349117,0.00027164805,0.00028619004,0.0040473277,0.000039515566,0.00053411734,0.0000033500573],"about_ca_topic_score_codex":0.0028796925,"about_ca_topic_score_gemma":0.0037050676,"teacher_disagreement_score":0.0028796925,"about_ca_system_score_codex":0.00010574593,"about_ca_system_score_gemma":0.00008061733,"threshold_uncertainty_score":0.0057258606},"labels":[],"label_agreement":null},{"id":"W2096325281","doi":"10.1029/2000gl011779","title":"Interdecadal climate variability and regime‐scale shifts in Pacific North America","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":280,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Climatology; Proxy (statistics); Transect; Climate change; Context (archaeology); Environmental science; Oceanography; Geography; Geology","score_opus":0.025289364736172625,"score_gpt":0.28551824627749983,"score_spread":0.26022888154132723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096325281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992136,0.00007982599,0.0000584298,0.000033860913,0.0000020263317,0.0000010636844,0.00007506564,0.0000034399377,0.0005327293],"genre_scores_gemma":[0.9996562,0.00009974771,0.000041366104,0.000012870004,0.0000036703932,0.0000025399763,0.00009067948,0.0000015060995,0.00009142023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994063,0.000009678459,0.00000373698,0.000019381734,0.000012069909,0.000014565491],"domain_scores_gemma":[0.99971277,0.00005896555,0.00011462658,0.000024704701,0.000045025266,0.0000438153],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020406884,0.000056356414,0.00007645956,0.0004203097,0.00022180814,0.00033841198,0.00009246124,0.0001093013,0.00057960895],"category_scores_gemma":[0.0008225255,0.00008526491,0.00006550904,0.0004934441,0.00020732076,0.00022081217,0.00026130938,0.00019726419,0.00005064674],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004726405,0.000033295226,0.98084176,0.000018087301,0.00007484171,0.00010031291,0.000837574,0.00078315526,0.005259563,0.00023597703,0.00029416702,0.011473939],"study_design_scores_gemma":[6.025095e-7,0.0000040030986,0.9994168,0.0000016360437,0.0000032973655,0.000017241638,0.000107204265,0.00019361507,0.000046356166,0.00004135092,0.00016679493,0.0000010112079],"about_ca_topic_score_codex":0.013794127,"about_ca_topic_score_gemma":0.037433326,"teacher_disagreement_score":0.013794127,"about_ca_system_score_codex":0.00029199908,"about_ca_system_score_gemma":0.000248953,"threshold_uncertainty_score":0.027427673},"labels":[],"label_agreement":null},{"id":"W2096566460","doi":"10.1029/2000gl003787","title":"Average daytime <i>F</i> region disturbance neutral winds measured by UARS: Initial results","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency; Utah State University; National Aeronautics and Space Administration","keywords":"Zonal and meridional; Daytime; Equator; Atmospheric sciences; Latitude; Morning; Perturbation (astronomy); Middle latitudes; Climatology; Global wind patterns; Geology; Meridional flow; Thermosphere; Environmental science; Ionosphere; Geodesy; Geophysics; Physics","score_opus":0.018120922398084473,"score_gpt":0.27538584823942147,"score_spread":0.257264925841337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096566460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99545175,0.000048982445,0.0009021735,0.0000075533585,0.0000033997635,0.000019176112,0.0019146794,0.00008250207,0.0015698969],"genre_scores_gemma":[0.9953505,0.000047139725,0.0014685605,0.000004895628,0.000007562176,0.000009593241,0.0027670448,0.00000976707,0.0003348538],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998566,0.000024458992,0.000010652936,0.000037745685,0.000045285145,0.000025252666],"domain_scores_gemma":[0.9997212,0.000039820803,0.000029802226,0.000031209776,0.0001210214,0.000057021138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028906908,0.00032709498,0.00017771989,0.00037183356,0.00028044483,0.0002790691,0.00020424384,0.00018354466,0.00062732585],"category_scores_gemma":[0.00049272756,0.00011327564,0.00018799343,0.00038466338,0.00009251248,0.00024205554,0.00013837437,0.00014017851,0.00022633551],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001270312,0.00044584365,0.8828561,0.00013465488,0.00017488666,0.00023864768,0.0004091079,0.011996252,0.051251575,0.00019170651,0.0014274291,0.049603604],"study_design_scores_gemma":[0.000021086204,0.0003270762,0.98276377,0.0000038087785,0.000037015172,0.000061592866,0.00009385092,0.006724337,0.008946701,0.000023801167,0.0009867606,0.000010164078],"about_ca_topic_score_codex":0.025738377,"about_ca_topic_score_gemma":0.03311944,"teacher_disagreement_score":0.025738377,"about_ca_system_score_codex":0.0002638796,"about_ca_system_score_gemma":0.00012240477,"threshold_uncertainty_score":0.051177144},"labels":[],"label_agreement":null},{"id":"W2096610963","doi":"10.1002/2014gl060754","title":"Constraining the carbon tetrachloride (CCl<sub>4</sub>) budget using its global trend and inter‐hemispheric gradient","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Greenhouse gas; Troposphere; Stratosphere; Environmental science; Montreal Protocol; Atmospheric sciences; Ozone; Atmosphere (unit); Carbon tetrachloride; Ozone depletion; Tropospheric ozone; Climatology; Ozone layer; Chemistry; Meteorology; Physics; Geology","score_opus":0.03034018054956622,"score_gpt":0.27419998485522595,"score_spread":0.24385980430565973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096610963","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98938483,0.00017027752,0.0037556388,0.00023591776,0.000014177896,0.0000117324535,0.0029942563,0.00013122386,0.0033019346],"genre_scores_gemma":[0.99682933,0.00009435971,0.0014284822,0.00003191592,0.000004205954,0.000008397277,0.0014274691,0.000025610603,0.00015020123],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999385,0.000012035514,0.0000030858362,0.00002006429,0.00000986278,0.000016460077],"domain_scores_gemma":[0.9998708,0.000036700592,0.000024858715,0.000015507601,0.00003696351,0.000015137768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025610116,0.0004064452,0.00017871977,0.00045420986,0.00025393162,0.0006334987,0.0003865243,0.00049109187,0.0010312785],"category_scores_gemma":[0.0006906007,0.00024028336,0.00055446115,0.0009081595,0.00020857403,0.0006389058,0.0002675866,0.00023791596,0.0001833124],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020910562,0.0000875878,0.38549915,0.000112526766,0.0003240233,0.00019800886,0.00005275965,0.56275386,0.032216918,0.002566289,0.0020023338,0.013977477],"study_design_scores_gemma":[0.00010680562,0.000054304215,0.243567,0.00002782511,0.00017035309,0.00003342556,0.00013171892,0.7404423,0.009106243,0.0017164492,0.0045865444,0.00005712637],"about_ca_topic_score_codex":0.23569258,"about_ca_topic_score_gemma":0.20739941,"teacher_disagreement_score":0.23569258,"about_ca_system_score_codex":0.0018781967,"about_ca_system_score_gemma":0.0015011487,"threshold_uncertainty_score":0.46864134},"labels":[],"label_agreement":null},{"id":"W2096635607","doi":"10.1029/2005gl025397","title":"Aerosol indirect effect over the Indian Ocean","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Effective radius; Moderate-resolution imaging spectroradiometer; Climatology; Ice nucleus; Nucleation; Ice crystals; Pollution; Satellite; Meteorology; Geology; Physics","score_opus":0.010128656848172391,"score_gpt":0.2637024311767829,"score_spread":0.2535737743286105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096635607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99745935,0.00018147098,0.00033334838,0.000030725,0.000004608533,0.0000071166482,0.00031120417,0.000029866897,0.001642262],"genre_scores_gemma":[0.9992945,0.00009399595,0.00015917607,0.000006456677,0.0000065038867,0.0000031330846,0.00030750033,0.0000055429823,0.00012299692],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997055,0.000046063407,0.000018912624,0.00006012799,0.0000896778,0.000079698664],"domain_scores_gemma":[0.9993303,0.00022937938,0.00014063544,0.00007686867,0.00016494782,0.000057844452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022379009,0.00036286842,0.00030050747,0.0006133529,0.00027679477,0.00068672426,0.0002944348,0.00018257888,0.0010390353],"category_scores_gemma":[0.0007426667,0.00014922231,0.0006258833,0.00083549187,0.00024342285,0.00028162886,0.00076885836,0.0002447475,0.000093638955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028153232,0.00008239657,0.9196098,0.00018064711,0.0006931394,0.00091194594,0.00015219326,0.03216407,0.02488031,0.0005881425,0.00042062163,0.0200352],"study_design_scores_gemma":[0.000015241252,0.000041466934,0.9761126,0.000007890544,0.00023137666,0.0001245318,0.00010934234,0.018356327,0.00420816,0.0001270936,0.00065125193,0.000014712406],"about_ca_topic_score_codex":0.022138664,"about_ca_topic_score_gemma":0.026162561,"teacher_disagreement_score":0.022138664,"about_ca_system_score_codex":0.00044409177,"about_ca_system_score_gemma":0.00045544136,"threshold_uncertainty_score":0.04401958},"labels":[],"label_agreement":null},{"id":"W2096729982","doi":"10.1029/2004gl021201","title":"Anatomy of cirrus clouds: Results from the Emerald airborne campaigns","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Cirrus; Ice crystals; Outflow; Thunderstorm; Geology; Cloud physics; Lidar; Middle latitudes; Atmospheric sciences; Latitude; Meteorology; Remote sensing; Physics; Oceanography; Cloud computing; Geodesy","score_opus":0.024286833250340596,"score_gpt":0.2992660055135651,"score_spread":0.2749791722632245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096729982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942151,0.00014142157,0.00021490017,0.000026367949,0.0000052991754,0.000011429181,0.0019665987,0.000046295423,0.0033725847],"genre_scores_gemma":[0.9962329,0.00007041902,0.00043944363,0.000015653828,0.000010314697,0.0000043123796,0.0027910424,0.0000097984275,0.00042593555],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976355,0.000030000938,0.0000100113675,0.00006152776,0.00006377492,0.00007119018],"domain_scores_gemma":[0.9994931,0.00008250517,0.00010917117,0.000068350084,0.0001764167,0.00007039236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028015167,0.00022311835,0.00012367989,0.0009029132,0.0003053201,0.00047528037,0.00014542497,0.000183071,0.0005046622],"category_scores_gemma":[0.0005142522,0.00008634957,0.00015726357,0.0006526933,0.00020926844,0.00033085095,0.0003353599,0.00016436372,0.00021384677],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047936518,0.00016724286,0.92233723,0.00007306815,0.00012627874,0.0003992514,0.0014036406,0.004364497,0.021262312,0.00050955336,0.0026905562,0.04618708],"study_design_scores_gemma":[0.00000554172,0.000036424983,0.99626404,0.0000030860413,0.000007570647,0.00007424625,0.00013582318,0.000921927,0.0012374341,0.000028158642,0.0012805042,0.0000051200113],"about_ca_topic_score_codex":0.014968241,"about_ca_topic_score_gemma":0.02683258,"teacher_disagreement_score":0.014968241,"about_ca_system_score_codex":0.000379836,"about_ca_system_score_gemma":0.000110802255,"threshold_uncertainty_score":0.029762268},"labels":[],"label_agreement":null},{"id":"W2096757157","doi":"10.1029/2001gl014273","title":"A “broad‐shelf effect” upon postglacial relative sea level history","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Sea level; Continental shelf; Geology; Holocene; Oceanography; Physical geography; Glacial period; Last Glacial Maximum; Paleontology; Geography","score_opus":0.06731416758228782,"score_gpt":0.28742883836611954,"score_spread":0.22011467078383173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2096757157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949951,0.0002328275,0.0013407967,0.00009076204,0.000008139128,0.0000054122966,0.00011663951,0.000027454762,0.0031828072],"genre_scores_gemma":[0.99947125,0.00007346236,0.00011224374,0.00003439275,0.0000049026326,0.0000015206765,0.000079499194,0.000003892271,0.00021890934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997693,0.000058719554,0.00001445136,0.00006220181,0.000049594735,0.000045780973],"domain_scores_gemma":[0.999124,0.00036117292,0.00016616615,0.00015752428,0.00013040069,0.000060768965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080514594,0.00022893302,0.00023643972,0.0005759954,0.00039216664,0.000690248,0.0002256731,0.00026419075,0.0019407397],"category_scores_gemma":[0.0021809598,0.0002171188,0.00026701804,0.0006052869,0.0010293154,0.0005305687,0.0006644498,0.000305445,0.00026706516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036152432,0.00003169129,0.8915022,0.000082803475,0.00024483466,0.0007901951,0.0008561628,0.017408174,0.03556992,0.0026882484,0.0004972677,0.04996707],"study_design_scores_gemma":[0.0000033094386,0.00006983085,0.9937791,0.000006905966,0.00003468985,0.00014242367,0.00013937251,0.0037261206,0.0009727042,0.00045266404,0.00066259416,0.000010345611],"about_ca_topic_score_codex":0.006208446,"about_ca_topic_score_gemma":0.015578337,"teacher_disagreement_score":0.006208446,"about_ca_system_score_codex":0.00041232165,"about_ca_system_score_gemma":0.00028584996,"threshold_uncertainty_score":0.012344599},"labels":[],"label_agreement":null},{"id":"W2097156483","doi":"10.1029/2011gl048491","title":"An increase in crevasse extent, West Greenland: Hydrologic implications","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Crevasse; Geology; Physical geography; Climatology; Earth science; Environmental science; Geomorphology; Geography","score_opus":0.09087661522484883,"score_gpt":0.3122488373516201,"score_spread":0.2213722221267713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097156483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984983,0.00008657977,0.00005882723,0.00007317628,0.0000016167842,0.0000022037514,0.00038274264,0.000009162529,0.00088725006],"genre_scores_gemma":[0.99957365,0.000036519123,0.00005906011,0.000014313661,0.0000019415434,9.92935e-7,0.00019061072,0.0000017827633,0.00012121062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.0000054125426,0.0000018280238,0.000010839006,0.0000068439354,0.00001572535],"domain_scores_gemma":[0.99987555,0.000016367907,0.000053100142,0.000009506957,0.00002120299,0.000024337904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010587416,0.00009077348,0.00007430135,0.00046577878,0.00012972308,0.00044971952,0.00018293105,0.00019949826,0.0012046753],"category_scores_gemma":[0.00022637329,0.00005397973,0.0001043631,0.0005622901,0.0002605747,0.0002648409,0.00022357277,0.00008415607,0.000058751615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020330228,0.000045677953,0.9498068,0.000056303485,0.0001224223,0.00049319415,0.00043202043,0.005392873,0.025357319,0.00042322322,0.000980809,0.016686136],"study_design_scores_gemma":[0.0000017409644,0.000005717338,0.9984781,0.0000035429034,0.000005197203,0.000028007853,0.00009625566,0.0006288382,0.00028599138,0.00002636057,0.00043879746,0.0000014055183],"about_ca_topic_score_codex":0.09192766,"about_ca_topic_score_gemma":0.19766523,"teacher_disagreement_score":0.09192766,"about_ca_system_score_codex":0.0007254159,"about_ca_system_score_gemma":0.00027800153,"threshold_uncertainty_score":0.18278515},"labels":[],"label_agreement":null},{"id":"W2097288863","doi":"10.1029/2001gl014263","title":"Potential predictability of seasonal precipitation over the United States from canonical ensemble correlation predictions","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Predictability; Climatology; Boreal; Precipitation; Environmental science; Sea surface temperature; Forecast skill; Canonical correlation; Atmospheric sciences; Meteorology; Geography; Geology; Mathematics; Statistics","score_opus":0.0316313482737598,"score_gpt":0.28323395155212244,"score_spread":0.25160260327836265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097288863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898023,0.00007987343,0.0076744966,0.00015491874,0.000012891141,0.0000046300815,0.0005111483,0.00012412474,0.0016355834],"genre_scores_gemma":[0.99858046,0.000045572506,0.0007575391,0.000008579823,0.0000045362526,0.0000033817087,0.00049437926,0.000006066612,0.000099527264],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999056,0.00003823542,0.000004016708,0.000018641726,0.000017841696,0.000015600004],"domain_scores_gemma":[0.9993722,0.00030564165,0.00005177341,0.00005920744,0.00017827153,0.000032922115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005488634,0.00024088666,0.00016374457,0.0002396567,0.00016638984,0.00037648264,0.00014253362,0.00012125538,0.00047331935],"category_scores_gemma":[0.0026204712,0.00011259138,0.00021496211,0.0004379101,0.0001404524,0.0003685034,0.00025895052,0.00024948764,0.000075075826],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020676389,0.00004104157,0.19793828,0.000021202099,0.00012387513,0.00010009821,0.000050055613,0.7640466,0.001124123,0.0020724202,0.0032593876,0.03101618],"study_design_scores_gemma":[0.000005222605,0.000008561115,0.018136833,0.0000025203524,0.000011692968,0.000008130136,0.000010266375,0.98065233,0.00028561405,0.00068222434,0.00019208991,0.0000045063557],"about_ca_topic_score_codex":0.04368683,"about_ca_topic_score_gemma":0.057937607,"teacher_disagreement_score":0.04368683,"about_ca_system_score_codex":0.0003105933,"about_ca_system_score_gemma":0.0007050182,"threshold_uncertainty_score":0.08686513},"labels":[],"label_agreement":null},{"id":"W2097674982","doi":"10.1029/2010gl044315","title":"Impact of the Madden‐Julian Oscillation on the intraseasonal forecast skill of the North Atlantic Oscillation","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Madden–Julian oscillation; Extratropical cyclone; Climatology; Forecast skill; Anomaly (physics); Hindcast; Initialization; Environmental science; Convection; Oscillation (cell signaling); Geology; Atmospheric sciences; Meteorology; Geography; Physics","score_opus":0.03082971476337877,"score_gpt":0.2964463872838529,"score_spread":0.26561667252047416,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2097674982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983949,0.00006988795,0.00046819553,0.000108612905,0.000020225862,0.0000020123514,0.00012798923,0.000028487371,0.0007797453],"genre_scores_gemma":[0.99955875,0.000021350477,0.00014222668,0.000011047789,0.000008144427,8.175534e-7,0.00014865877,0.0000067754854,0.00010224216],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969316,0.00010650935,0.000030168814,0.00007584577,0.00004907148,0.000045289664],"domain_scores_gemma":[0.99499583,0.0033379202,0.00050198805,0.00034218573,0.00042752174,0.00039455562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017038494,0.00027173874,0.00022280627,0.00017896942,0.0002624244,0.0008631286,0.00018062137,0.00032368544,0.0007782258],"category_scores_gemma":[0.011235954,0.00017943865,0.00026804546,0.00015117493,0.00024693698,0.0005217484,0.00055072684,0.00047079567,0.00013826476],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014731069,0.00015551588,0.8576307,0.00003676198,0.00027116088,0.00016622843,0.00012035158,0.099731244,0.008230443,0.0006052728,0.0007418331,0.030837366],"study_design_scores_gemma":[0.000098514545,0.0003866509,0.72780293,0.000015958274,0.00009040264,0.00006360547,0.00011499397,0.2659675,0.0043110056,0.00042371286,0.0006984851,0.00002621747],"about_ca_topic_score_codex":0.02155596,"about_ca_topic_score_gemma":0.022268292,"teacher_disagreement_score":0.02155596,"about_ca_system_score_codex":0.000363369,"about_ca_system_score_gemma":0.00072600134,"threshold_uncertainty_score":0.042860985},"labels":[],"label_agreement":null},{"id":"W2098049985","doi":"10.1002/2015gl063469","title":"Ebullition of methane from peatlands: Does peat act as a signal shredder?","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"","keywords":"Peat; Methane; Environmental science; Greenhouse gas; Decoupling (probability); Atmospheric methane; Atmospheric sciences; Soil science; Geology; Chemistry; Ecology; Oceanography","score_opus":0.03573807390113104,"score_gpt":0.30893682242751525,"score_spread":0.2731987485263842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098049985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981127,0.000025064262,0.0015576697,0.0000518138,0.0000030391325,0.000002484637,0.000011680601,0.000014733227,0.00022076955],"genre_scores_gemma":[0.99958354,0.000015019762,0.0003415347,0.0000054360426,7.381713e-7,0.0000011504683,0.0000058166524,0.0000023000994,0.000044401273],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99990344,0.00003369337,0.0000067130163,0.000019565685,0.000012031582,0.00002455756],"domain_scores_gemma":[0.9993055,0.0003986305,0.00010402454,0.00004056733,0.000059005644,0.000092323986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039610744,0.00018596706,0.0003481725,0.00020030202,0.00019338456,0.00068831607,0.00042434403,0.00047227016,0.00045512148],"category_scores_gemma":[0.001761453,0.0001966906,0.00020100667,0.00011536886,0.0005982749,0.0007660515,0.00030351637,0.00023394103,0.000043449283],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090156373,0.00022784105,0.23215055,0.00019489421,0.00017664788,0.0009663977,0.00033896032,0.5710201,0.17883925,0.0048939567,0.0002131718,0.010076623],"study_design_scores_gemma":[0.000030085048,0.00012140716,0.033914898,0.000012800798,0.00003364796,0.000058213525,0.00013980397,0.95263785,0.0116954,0.0011837465,0.00014545258,0.00002667493],"about_ca_topic_score_codex":0.011786615,"about_ca_topic_score_gemma":0.009256108,"teacher_disagreement_score":0.011786615,"about_ca_system_score_codex":0.000549956,"about_ca_system_score_gemma":0.00040423093,"threshold_uncertainty_score":0.02343601},"labels":[],"label_agreement":null},{"id":"W2098081069","doi":"10.1029/2001gl014569","title":"Ozone production rate and hydrocarbon reactivity in 5 urban areas: A cause of high ozone concentration in Houston","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":198,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Ozone; Metropolitan area; Environmental science; Atmosphere (unit); Phoenix; Environmental chemistry; Petrochemical; Hydrocarbon; Production rate; Atmospheric sciences; Environmental engineering; Meteorology; Chemistry; Geography; Geology; Archaeology","score_opus":0.028848586765438448,"score_gpt":0.24886778027261391,"score_spread":0.22001919350717547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098081069","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996898,0.00003755825,0.000023604953,0.0000226289,7.55367e-7,0.0000015491115,0.00007656908,0.0000032117414,0.00014434806],"genre_scores_gemma":[0.999793,0.000025592655,0.000023802053,0.0000043579666,0.0000023522314,0.0000011601682,0.00007582933,0.0000010148779,0.00007285157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999207,0.000015061798,0.000004187539,0.000014555537,0.000017318393,0.000028205022],"domain_scores_gemma":[0.99971217,0.000021581724,0.00014294493,0.000010909074,0.000039310227,0.000073053976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014952284,0.00016207655,0.00011031023,0.00060355116,0.00025302678,0.0003299441,0.00020152557,0.00018043528,0.0010713189],"category_scores_gemma":[0.0003209169,0.00014924009,0.00015038003,0.00053068425,0.0002239393,0.00015920431,0.00029057942,0.00017409207,0.00017868604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001177231,0.000030136463,0.9957568,0.00000535518,0.000021337635,0.0003507168,0.00014191549,0.00025392085,0.0017197602,0.000026814818,0.00015795771,0.0014175127],"study_design_scores_gemma":[0.000002654268,0.000028078312,0.9990521,9.2984766e-7,0.000006443855,0.00011574007,0.0001481903,0.00026156957,0.00027188065,0.0000112896,0.00009921142,0.0000019803726],"about_ca_topic_score_codex":0.019155445,"about_ca_topic_score_gemma":0.013872361,"teacher_disagreement_score":0.019155445,"about_ca_system_score_codex":0.0006361327,"about_ca_system_score_gemma":0.0002479389,"threshold_uncertainty_score":0.038087904},"labels":[],"label_agreement":null},{"id":"W2098381289","doi":"10.1029/2009gl038771","title":"On the origins of temporal power‐law behavior in the global atmospheric circulation","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Hurst exponent; Scaling; Power law; Statistical physics; Environmental science; Atmospheric circulation; Climate model; Climatology; Climate change; Temporal scales; Meteorology; Atmospheric sciences; Physics; Geology; Mathematics; Statistics","score_opus":0.03951021672682697,"score_gpt":0.326292972300753,"score_spread":0.286782755573926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098381289","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92824084,0.0005927754,0.06225832,0.0009321417,0.000035987694,0.000023688934,0.00032520376,0.00028954138,0.0073014577],"genre_scores_gemma":[0.9968568,0.00023771371,0.002433962,0.000029394387,0.000019910947,0.000008767675,0.00013953295,0.00004191525,0.00023192911],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998745,0.00004423041,0.0000071011154,0.0000339823,0.000026629374,0.000013530587],"domain_scores_gemma":[0.99730587,0.0017662145,0.000362741,0.00034204382,0.00016639914,0.0000566849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009448337,0.00023676052,0.00012454821,0.00045599366,0.00025459367,0.00058374985,0.00028237738,0.00027524657,0.0013373608],"category_scores_gemma":[0.009321463,0.00017518442,0.00032571302,0.00054554205,0.00068218913,0.001323797,0.00028726735,0.000532263,0.00017605754],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025061634,0.00010794023,0.26708913,0.00020847404,0.00018819483,0.00079043204,0.0012054201,0.5080331,0.021281904,0.11386493,0.0040276814,0.08295227],"study_design_scores_gemma":[0.000022112265,0.000036257454,0.078652896,0.000038103735,0.000025169325,0.00020379662,0.00013127229,0.8663076,0.003208823,0.049428534,0.0019120335,0.000033387918],"about_ca_topic_score_codex":0.0051918086,"about_ca_topic_score_gemma":0.003480117,"teacher_disagreement_score":0.0051918086,"about_ca_system_score_codex":0.00047840056,"about_ca_system_score_gemma":0.0002877292,"threshold_uncertainty_score":0.010323167},"labels":[],"label_agreement":null},{"id":"W2098781985","doi":"10.1029/2005gl022377","title":"Validation of ACE‐FTS stratospheric ozone profiles against Odin/OSIRIS measurements","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Waterloo; University of Saskatchewan","funders":"","keywords":"Osiris; Ozone; Stratosphere; Northern Hemisphere; Atmospheric sciences; Environmental science; Spectrograph; Altitude (triangle); Latitude; Ozone layer; Satellite; Meteorology; Physics; Astronomy","score_opus":0.06409006545589818,"score_gpt":0.3016991800023267,"score_spread":0.23760911454642852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098781985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98303694,0.00008046484,0.0057198657,0.000042023134,0.00005077187,0.000055852146,0.007573003,0.00048430852,0.0029568013],"genre_scores_gemma":[0.9803545,0.00006092042,0.008844318,0.000038683993,0.000012882121,0.00003113559,0.010058876,0.00006873842,0.00052999926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99904746,0.00015743682,0.0000814786,0.00024842142,0.00034910068,0.00011616549],"domain_scores_gemma":[0.9979188,0.00021722463,0.00024608106,0.00048606825,0.0010110475,0.00012069266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002407505,0.00045930545,0.00027854834,0.00068352587,0.00045073451,0.0008517547,0.0006622864,0.0003384731,0.00079279894],"category_scores_gemma":[0.0037924354,0.00019504807,0.000263398,0.00083195535,0.00016553167,0.0007608352,0.00051576394,0.0002895275,0.00053957733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004139799,0.0014558196,0.63167524,0.00032164672,0.0007850689,0.0003737146,0.00085209886,0.06781789,0.1513302,0.0014384361,0.0069008465,0.1329093],"study_design_scores_gemma":[0.00025211615,0.0002898614,0.7990843,0.000040253653,0.00010955557,0.0001372588,0.00033573052,0.11987175,0.07301874,0.0003393995,0.006478835,0.00004226117],"about_ca_topic_score_codex":0.020527208,"about_ca_topic_score_gemma":0.018343097,"teacher_disagreement_score":0.020527208,"about_ca_system_score_codex":0.00056079146,"about_ca_system_score_gemma":0.0005875477,"threshold_uncertainty_score":0.040815473},"labels":[],"label_agreement":null},{"id":"W2098844080","doi":"10.1029/2011gl047890","title":"Biomass burning emission estimates inferred from satellite column measurements of HCHO: Sensitivity to co-emitted aerosol and injection height","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"SCIAMACHY; Aerosol; Environmental science; Atmospheric sciences; Northern Hemisphere; Boreal; Sulfate aerosol; Albedo (alchemy); Single-scattering albedo; Mixing ratio; Climatology; Meteorology; Troposphere; Geology; Geography","score_opus":0.07700264736644061,"score_gpt":0.2977410654692277,"score_spread":0.22073841810278708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098844080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99043417,0.00022669465,0.006804262,0.000071794464,0.00001026225,0.000019298339,0.00096916256,0.00012801605,0.0013362464],"genre_scores_gemma":[0.99724615,0.00006059064,0.0019352676,0.000017299137,0.0000040538957,0.000005966227,0.0006462878,0.000011966443,0.00007249233],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999742,0.000045997396,0.00001800717,0.00008405962,0.000071491464,0.000038439226],"domain_scores_gemma":[0.9990607,0.0005358242,0.00014619995,0.00010473519,0.0001204063,0.000032044947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008989992,0.000583895,0.0002133173,0.00053337245,0.00019341796,0.00054516934,0.00045524252,0.00042515525,0.00045546546],"category_scores_gemma":[0.002929721,0.00039090618,0.00054341345,0.00042084875,0.00023279266,0.0004593624,0.00041862985,0.00029859974,0.00012972296],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019389551,0.000078978715,0.8417464,0.00009115736,0.00048554683,0.00014122513,0.000110453366,0.11857984,0.021150019,0.00038621822,0.00023658472,0.016799632],"study_design_scores_gemma":[0.00003586598,0.000045059616,0.6809636,0.00004078374,0.00016528477,0.0001100209,0.000074654236,0.29292333,0.024419013,0.000489229,0.0006869713,0.0000461625],"about_ca_topic_score_codex":0.028735006,"about_ca_topic_score_gemma":0.022076935,"teacher_disagreement_score":0.028735006,"about_ca_system_score_codex":0.0006689838,"about_ca_system_score_gemma":0.0002846536,"threshold_uncertainty_score":0.057135522},"labels":[],"label_agreement":null},{"id":"W2098932641","doi":"10.1002/grl.50684","title":"Turbulent mixing and hydraulic control of abyssal water in the Samoan Passage","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Sill; Geology; Turbulence; Hydraulic jump; Abyssal zone; Seafloor spreading; Mixing (physics); Bathymetry; Oceanography; Bedform; Turbidity current; Geophysics; Flow (mathematics); Geomorphology; Sediment; Sediment transport; Mechanics; Petrology; Physics","score_opus":0.015567565229736754,"score_gpt":0.23822950075003577,"score_spread":0.222661935520299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2098932641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999356,0.000032758224,0.00012859963,0.000012485926,0.0000034180944,0.000002020443,0.000037775204,0.000009376048,0.00041760004],"genre_scores_gemma":[0.9994821,0.000033997712,0.00024397112,0.000007304472,0.0000049016435,0.000002673342,0.00006354232,0.0000030585338,0.00015850375],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999485,0.000004827948,0.0000032708774,0.000015304053,0.00001567125,0.0000125016],"domain_scores_gemma":[0.9999052,0.000008988337,0.000029301624,0.0000048610214,0.000019761721,0.00003177029],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000076427415,0.00031399907,0.00019716377,0.0005207989,0.0004935636,0.00040189573,0.0001859809,0.00017179876,0.00063415116],"category_scores_gemma":[0.00021539607,0.00014477607,0.00015982367,0.0004098846,0.00039824063,0.00024600993,0.0004833708,0.00023345304,0.00010217955],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008891226,0.000100888225,0.47841182,0.000099243436,0.00011604426,0.0022735265,0.0028890688,0.0024283163,0.48836365,0.0004719105,0.0002408755,0.023715543],"study_design_scores_gemma":[0.000018933253,0.00019093954,0.987743,0.000008760347,0.000019493411,0.00015559098,0.0007527416,0.0028671855,0.007221042,0.00009346928,0.00091003685,0.000018634495],"about_ca_topic_score_codex":0.015002447,"about_ca_topic_score_gemma":0.021969121,"teacher_disagreement_score":0.015002447,"about_ca_system_score_codex":0.00034393222,"about_ca_system_score_gemma":0.00031615916,"threshold_uncertainty_score":0.029830277},"labels":[],"label_agreement":null},{"id":"W2099152712","doi":"10.1029/2011gl049351","title":"Oxidation of ambient biogenic secondary organic aerosol by hydroxyl radicals: Effects on cloud condensation nuclei activity","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"","keywords":"Aerosol; Cloud condensation nuclei; Scavenging; Chemistry; Condensation; Chemical composition; Ambient pressure; Fraction (chemistry); Environmental chemistry; Meteorology; Organic chemistry; Antioxidant","score_opus":0.025417122435007964,"score_gpt":0.25083280515855133,"score_spread":0.22541568272354337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099152712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99889106,0.00031753708,0.00011440103,0.000009343985,0.000003002856,0.000017116277,0.00017564768,0.0000045717356,0.00046737242],"genre_scores_gemma":[0.9991605,0.00016260686,0.00015182376,0.0000069235325,0.0000033075323,0.000005648452,0.00016586571,0.0000017481725,0.00034165676],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999155,0.000006529158,0.0000030212107,0.000023919683,0.000028427878,0.000022701583],"domain_scores_gemma":[0.9999118,0.000013440396,0.000016687267,0.0000057940433,0.000030887968,0.000021400734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011898852,0.0002813208,0.0001436904,0.00019055662,0.0003661575,0.00026446267,0.00017769667,0.00022203242,0.0005968934],"category_scores_gemma":[0.0001273618,0.00009101001,0.000092750095,0.00014693479,0.00025680487,0.000109733126,0.00010442273,0.000166672,0.00007874982],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036307596,0.000042029795,0.03500514,0.00006320585,0.000017428003,0.00006784102,0.00005171765,0.0002556892,0.9605664,0.000016400034,0.00007230702,0.0034787732],"study_design_scores_gemma":[0.000024046436,0.00046919612,0.620736,0.0000045396664,0.000027894514,0.000075554104,0.000076465054,0.0009695036,0.37681887,0.00003066811,0.00075646426,0.00001076402],"about_ca_topic_score_codex":0.095850095,"about_ca_topic_score_gemma":0.1727839,"teacher_disagreement_score":0.095850095,"about_ca_system_score_codex":0.0012700853,"about_ca_system_score_gemma":0.0004828732,"threshold_uncertainty_score":0.19058442},"labels":[],"label_agreement":null},{"id":"W2099190133","doi":"10.1029/2004gl019756","title":"Reconstructed warm season temperatures for Nome, Seward Peninsula, Alaska","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"U.S. Bureau of Land Management; Lamont-Doherty Earth Observatory, Columbia University; U.S. Department of Energy; Inter-American Institute for Global Change Research; National Science Foundation","keywords":"Peninsula; Nome; Geology; Climatology; Oceanography; Environmental science; Geography; Archaeology","score_opus":0.03193391523614996,"score_gpt":0.295996516860748,"score_spread":0.26406260162459805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099190133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99766064,0.00012646055,0.0003565931,0.000015501475,0.0000028106012,0.000002027762,0.0010809479,0.00002497226,0.00072996103],"genre_scores_gemma":[0.99641776,0.00011567413,0.0007807021,0.000003275841,0.00000202558,0.0000032208768,0.0023172528,0.0000072891503,0.00035279896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.0000058685628,0.0000038945473,0.000013087274,0.0000047009835,0.0000052538876],"domain_scores_gemma":[0.9998989,0.000014101511,0.000032905653,0.000014120876,0.000023785851,0.000016138732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014453937,0.00017774226,0.00009137603,0.00080092234,0.0002901166,0.00041240733,0.0001358476,0.00016971213,0.001052401],"category_scores_gemma":[0.00035654005,0.0001654474,0.00021782212,0.00042750512,0.00013771214,0.00022117775,0.00025220067,0.0001597021,0.00026747212],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018221403,0.000022996666,0.9560305,0.000024511455,0.00012142136,0.00016124098,0.00039349395,0.026110513,0.002574994,0.0003237855,0.00043415555,0.013620274],"study_design_scores_gemma":[0.000009852054,0.000032507298,0.9823418,0.000019460264,0.00003193792,0.00016699903,0.00054993073,0.013593774,0.0008731222,0.00022513575,0.0021380838,0.000017271217],"about_ca_topic_score_codex":0.025921619,"about_ca_topic_score_gemma":0.063231185,"teacher_disagreement_score":0.025921619,"about_ca_system_score_codex":0.0003582667,"about_ca_system_score_gemma":0.00036877644,"threshold_uncertainty_score":0.051541448},"labels":[],"label_agreement":null},{"id":"W2099239436","doi":"10.1029/2005gl022404","title":"Labrador Sea Water property variations in the northeastern Atlantic Ocean","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Hydrography; Equator; Geology; Plateau (mathematics); Oceanography; Climatology; Latitude; Geodesy","score_opus":0.02318096026902265,"score_gpt":0.25142552673145685,"score_spread":0.2282445664624342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099239436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987023,0.000034201406,0.000015110189,0.000011584832,7.7292293e-7,0.0000011249116,0.0008641274,0.0000045073775,0.00036633818],"genre_scores_gemma":[0.9971419,0.00007690448,0.000066882254,0.000011283369,0.000003553952,0.0000038254507,0.0023550875,0.000003171035,0.00033740685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998958,0.000011767821,0.0000118342205,0.000028356593,0.000019830388,0.000032414035],"domain_scores_gemma":[0.9995092,0.000045685854,0.00027712053,0.00003507884,0.00007971426,0.000053121097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017548067,0.00014309945,0.0001340951,0.0010098456,0.00019183547,0.0005054349,0.00014178292,0.00011359885,0.0007979133],"category_scores_gemma":[0.0005799046,0.00007816192,0.00020457576,0.0013180628,0.00020524923,0.0002854409,0.00027162995,0.00011476034,0.00020007165],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000045696605,0.0000105517865,0.9951196,0.0000054337293,0.000032782427,0.000027671334,0.00009184884,0.00020248306,0.0005228017,0.000026397827,0.00020769105,0.003707014],"study_design_scores_gemma":[7.28202e-7,0.0000040356153,0.99964464,0.0000011046614,0.0000031174113,0.000006576458,0.000048206457,0.000089627545,0.00005037527,0.0000018344659,0.00014888424,8.9332707e-7],"about_ca_topic_score_codex":0.16616662,"about_ca_topic_score_gemma":0.32731745,"teacher_disagreement_score":0.16616662,"about_ca_system_score_codex":0.00092214503,"about_ca_system_score_gemma":0.0003408897,"threshold_uncertainty_score":0.3303988},"labels":[],"label_agreement":null},{"id":"W2099553137","doi":"10.1029/2002gl016733","title":"Sound scattering from oceanic turbulence","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine animal studies overview","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Scattering; Backscatter (email); Turbulence; Zooplankton; Physics; Amplitude; Sound (geography); Acoustics; Geology; Computational physics; Optics; Oceanography; Meteorology; Telecommunications","score_opus":0.044844002758695815,"score_gpt":0.30262573029863504,"score_spread":0.2577817275399392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099553137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9690221,0.0009419392,0.015900614,0.00013576302,0.000052574185,0.000010496602,0.000102923674,0.00007745207,0.013756151],"genre_scores_gemma":[0.99707496,0.0002620636,0.0016661767,0.000021863132,0.000012410068,0.000003314852,0.000073701216,0.000008119,0.0008773936],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998715,0.00001290919,0.0000073482834,0.000025590125,0.000058245936,0.000024284896],"domain_scores_gemma":[0.9997576,0.00009518604,0.000033583783,0.000029644283,0.00006016772,0.000023780538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018174862,0.00016860709,0.00019387383,0.00032373142,0.0002391714,0.0004557773,0.000092942835,0.0001487047,0.0011741443],"category_scores_gemma":[0.00045525472,0.00013379674,0.000121384255,0.00036061098,0.00034504177,0.0002221038,0.00061222044,0.00028998524,0.0002592786],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003346676,0.00003083495,0.097314216,0.00020511093,0.000069252965,0.0005996372,0.0005722783,0.007010343,0.78819907,0.0066960976,0.00091790746,0.098050535],"study_design_scores_gemma":[0.00005667697,0.00055460463,0.5547198,0.00010249424,0.00017231637,0.0019476784,0.00096070766,0.030147769,0.38332486,0.015689494,0.012208838,0.000114713475],"about_ca_topic_score_codex":0.0015783753,"about_ca_topic_score_gemma":0.0015355451,"teacher_disagreement_score":0.0015783753,"about_ca_system_score_codex":0.00021821314,"about_ca_system_score_gemma":0.0001468904,"threshold_uncertainty_score":0.003927946},"labels":[],"label_agreement":null},{"id":"W2099767981","doi":"10.1002/grl.50912","title":"Large‐scale circulation associated with moisture intrusions into the Arctic during winter","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":319,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Middle latitudes; Moisture; Environmental science; Arctic; Geology; Outgoing longwave radiation; Siberian High; Atmospheric circulation; Atmospheric sciences; Oceanography; Geography; East Asia; Meteorology","score_opus":0.011217887388383103,"score_gpt":0.2372182078817147,"score_spread":0.22600032049333157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2099767981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995043,0.00002876404,0.00003971084,0.000011214617,0.0000030852555,0.0000010783979,0.00015663836,0.0000060298157,0.00024914637],"genre_scores_gemma":[0.99936956,0.00004539658,0.000064911175,0.000004503971,0.000009530044,0.0000018575887,0.000430229,0.000002524531,0.00007142347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994767,0.0000071483637,0.0000041557414,0.000014432753,0.000010387832,0.000016203583],"domain_scores_gemma":[0.9998142,0.000035655758,0.00007565426,0.000011579637,0.000023880066,0.000039061495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013727765,0.00017368783,0.0001495535,0.0004947841,0.00026150502,0.00046437234,0.000100608515,0.00014937264,0.0005479985],"category_scores_gemma":[0.00037006242,0.00011433566,0.00018472591,0.00052372477,0.00020357521,0.0002833142,0.00032872998,0.00016253124,0.00008718533],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027039638,0.00008866493,0.9778216,0.000020965663,0.00007530458,0.00024843347,0.0003753581,0.0019217955,0.011509054,0.00016651378,0.0005140976,0.006988008],"study_design_scores_gemma":[0.0000027094386,0.000019150884,0.99799216,0.0000023721536,0.000007688058,0.00003968651,0.00008879702,0.0014182256,0.0002150958,0.00002154192,0.00018998818,0.0000026434207],"about_ca_topic_score_codex":0.021465257,"about_ca_topic_score_gemma":0.034975033,"teacher_disagreement_score":0.021465257,"about_ca_system_score_codex":0.00035680138,"about_ca_system_score_gemma":0.0002011825,"threshold_uncertainty_score":0.04268062},"labels":[],"label_agreement":null},{"id":"W2100179781","doi":"10.1029/2005gl023483","title":"Ionospheric characteristics above Martian crustal magnetic anomalies","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Ionosphere; Martian; Geophysics; Mars Exploration Program; Geology; Dynamo; Magnetic anomaly; Magnetic field; Electron density; Planet; Physics; Electron; Astrobiology; Astronomy","score_opus":0.021845487552085072,"score_gpt":0.2745611229458761,"score_spread":0.252715635393791,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100179781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992756,0.000052869957,0.000031359625,0.0000060260277,6.5029485e-7,9.850504e-7,0.0002804794,0.000002943559,0.00034919177],"genre_scores_gemma":[0.9992625,0.00003906333,0.000041432275,0.0000025348556,0.0000019051976,7.71445e-7,0.0005343819,0.0000014328425,0.00011587755],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999683,0.000003616024,0.0000023640646,0.0000080489845,0.0000069243733,0.000010790019],"domain_scores_gemma":[0.9997583,0.000045265195,0.000101387726,0.000023046005,0.000037354203,0.000034673507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008855598,0.000107430365,0.00012403858,0.00045645208,0.00019624196,0.0003008767,0.00006888442,0.00010838525,0.00066468486],"category_scores_gemma":[0.00040493827,0.00006012477,0.00009380572,0.00041217133,0.000102466605,0.00016686824,0.00018584687,0.00009474616,0.00013206428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021031406,0.000020838512,0.96799904,0.000021555143,0.00005094267,0.00026125752,0.00036469515,0.0007050732,0.022829453,0.0001646838,0.00021831402,0.007153884],"study_design_scores_gemma":[0.0000018395065,0.000023641625,0.99835485,0.0000014087611,0.000007343045,0.00012174814,0.00006976581,0.0002017307,0.00072977546,0.000036673027,0.00044876608,0.0000024306855],"about_ca_topic_score_codex":0.00187006,"about_ca_topic_score_gemma":0.0023493515,"teacher_disagreement_score":0.00187006,"about_ca_system_score_codex":0.00009804432,"about_ca_system_score_gemma":0.000048768685,"threshold_uncertainty_score":0.0037183166},"labels":[],"label_agreement":null},{"id":"W2100183713","doi":"10.1002/2014gl061927","title":"Observational evidence of electron pitch angle scattering driven by ECH waves","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Aeronautics and Space Administration","keywords":"Physics; Scattering; Pitch angle; Whistler; Computational physics; Electron; Diffusion; Atomic physics; Optics; Geophysics; Nuclear physics","score_opus":0.031635804383171026,"score_gpt":0.31085702187220055,"score_spread":0.2792212174890295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100183713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998212,0.000054614356,0.0004103034,0.000018565992,0.0000023636178,0.0000027333385,0.0001328179,0.000013643669,0.0011530087],"genre_scores_gemma":[0.99973303,0.000018598257,0.000102790604,0.0000035076905,0.000003517687,9.4646475e-7,0.00009627851,0.000002130771,0.000039175084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999037,0.000013236383,0.000008140014,0.00002742224,0.000028614675,0.000018903444],"domain_scores_gemma":[0.99927515,0.00019400605,0.00023185232,0.00010726566,0.000098223674,0.00009349402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024311924,0.0001300983,0.00013935992,0.000532585,0.0002084132,0.0003820398,0.00013281757,0.00021115104,0.0005119431],"category_scores_gemma":[0.000955396,0.0001235646,0.000094956355,0.00044871983,0.00033451006,0.00028034564,0.00047069672,0.00023321924,0.00009125203],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027734318,0.00004319848,0.9035922,0.000037744452,0.00007045999,0.0005125265,0.00044706144,0.0010087366,0.08347076,0.0007153566,0.00029083755,0.009533691],"study_design_scores_gemma":[0.000009308438,0.000032007632,0.9945123,0.000004780154,0.000008349459,0.00019859886,0.00009974271,0.0015806134,0.002914616,0.00015269799,0.0004816079,0.000005452926],"about_ca_topic_score_codex":0.0018888678,"about_ca_topic_score_gemma":0.0022378082,"teacher_disagreement_score":0.0018888678,"about_ca_system_score_codex":0.0001615076,"about_ca_system_score_gemma":0.00008044837,"threshold_uncertainty_score":0.0037557483},"labels":[],"label_agreement":null},{"id":"W2100271147","doi":"10.1029/2008gl035342","title":"Plumes anchored by a high viscosity lower mantle in a 3D mantle convection model featuring dynamically evolving plates","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mantle (geology); Geology; Mantle convection; Plate tectonics; Lithosphere; Intraplate earthquake; Geophysics; Mantle plume; Convection; Hotspot (geology); Plume; Mechanics; Seismology; Physics; Tectonics; Meteorology","score_opus":0.01834063965403833,"score_gpt":0.24661709777241883,"score_spread":0.2282764581183805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100271147","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910199,0.0000749487,0.0046128803,0.00018103584,0.000015264888,0.000019531688,0.00026262825,0.0000966655,0.0037172243],"genre_scores_gemma":[0.995046,0.00007381947,0.003686763,0.000028770082,0.000007601751,0.000034705197,0.00016874015,0.000027203558,0.00092644687],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999292,0.000016167165,0.0000036698134,0.000009110846,0.000016577302,0.000025287229],"domain_scores_gemma":[0.9997451,0.00009676414,0.000048765927,0.00002285127,0.000030982468,0.00005554186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019679398,0.00048688223,0.0005373542,0.0005024986,0.0005358587,0.0010797657,0.0009327875,0.001196359,0.0017625534],"category_scores_gemma":[0.0007362008,0.00044291985,0.0007736827,0.0004381851,0.00091280893,0.00044410385,0.0007011684,0.00051529735,0.00014272878],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012031924,0.00003729944,0.0022522497,0.000023585946,0.0000207794,0.00017323311,0.00006304899,0.98999023,0.004600322,0.0019468729,0.00010067921,0.00067133806],"study_design_scores_gemma":[0.0000742807,0.000036082405,0.0007438867,0.0000033003648,0.000014668183,0.000018649418,0.00003041951,0.9977991,0.0007793661,0.00037767453,0.000111139605,0.00001142564],"about_ca_topic_score_codex":0.024223575,"about_ca_topic_score_gemma":0.009420084,"teacher_disagreement_score":0.024223575,"about_ca_system_score_codex":0.00095430476,"about_ca_system_score_gemma":0.00085642806,"threshold_uncertainty_score":0.048165143},"labels":[],"label_agreement":null},{"id":"W2100333913","doi":"10.1002/grl.50317","title":"Multi‐system seasonal predictions of Arctic sea ice","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Sea ice; Climate Forecast System; Anomaly (physics); Environmental science; Arctic; Precipitation; Arctic ice pack; Forecast skill; The arctic; Meteorology; Geology; Oceanography; Geography","score_opus":0.02416450850325247,"score_gpt":0.26048982898002504,"score_spread":0.23632532047677257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100333913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840223,0.00015065167,0.0124886185,0.00015480073,0.000050069008,0.00002686006,0.00036149626,0.00018809993,0.002557125],"genre_scores_gemma":[0.99733126,0.00003046908,0.0022249105,0.000009131828,0.000009331103,0.00000946614,0.00018909348,0.0000063943694,0.00019006344],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979204,0.000059279446,0.000017573779,0.000056770255,0.000046593803,0.00002781399],"domain_scores_gemma":[0.99907494,0.00043959,0.00012910763,0.00008278324,0.00020325725,0.00007027023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010063507,0.0005069485,0.0003819653,0.00033846858,0.0003202659,0.00060183194,0.00037026903,0.00042050108,0.00083893014],"category_scores_gemma":[0.002335858,0.0003226296,0.0004892614,0.00025929813,0.00017581278,0.000836649,0.0006738739,0.00048305345,0.0001050318],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014039774,0.00005729205,0.01764351,0.000023408818,0.00012102534,0.000030753414,0.000031398995,0.9689021,0.0020937463,0.00021696134,0.00025211438,0.01048731],"study_design_scores_gemma":[0.00001168003,0.000036735837,0.006803718,0.0000023334721,0.00001640592,0.0000040154778,0.0000120961595,0.99222916,0.0006373548,0.00015575216,0.000084098385,0.0000066273524],"about_ca_topic_score_codex":0.02736584,"about_ca_topic_score_gemma":0.026502086,"teacher_disagreement_score":0.02736584,"about_ca_system_score_codex":0.0006904576,"about_ca_system_score_gemma":0.00084348227,"threshold_uncertainty_score":0.05441308},"labels":[],"label_agreement":null},{"id":"W2100489636","doi":"10.1029/2004gl021216","title":"Effects of future climate change on regional air pollution episodes in the United States","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":276,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Environmental Protection Agency","keywords":"Environmental science; Climatology; Climate change; Pollution; Atmospheric sciences; Air pollution; Oceanography; Geology","score_opus":0.029011189983137474,"score_gpt":0.27626349966443936,"score_spread":0.24725230968130188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100489636","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99892944,0.000054214535,0.00012938908,0.00013389836,0.0000065427303,0.0000030052747,0.00031825752,0.0000142143845,0.00041111824],"genre_scores_gemma":[0.9993605,0.00005041328,0.00011466926,0.00002732469,0.0000030321962,0.000003499175,0.00038054597,0.000002659276,0.000057385696],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998221,0.00007247497,0.000011414834,0.000035764027,0.00002068549,0.00003749461],"domain_scores_gemma":[0.9995504,0.00016673832,0.00009866942,0.0000325322,0.000068033514,0.00008355123],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005089891,0.00025505968,0.0002449074,0.00028940054,0.00036237686,0.00068884593,0.0002819206,0.0006235657,0.00096884696],"category_scores_gemma":[0.0016527829,0.00019166416,0.0005736552,0.0004098422,0.0003115937,0.0005222288,0.0005245844,0.00044395082,0.0000747381],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046377056,0.00022816018,0.78110015,0.000039543094,0.00035158603,0.00037428635,0.00017310119,0.20722173,0.0022715433,0.0011118936,0.0013605352,0.005303675],"study_design_scores_gemma":[0.000088937646,0.00036845036,0.67964804,0.000020273661,0.00017901316,0.00014125257,0.00055642007,0.3158582,0.0011754876,0.00068617205,0.0012379634,0.000039781065],"about_ca_topic_score_codex":0.077845134,"about_ca_topic_score_gemma":0.0736942,"teacher_disagreement_score":0.077845134,"about_ca_system_score_codex":0.0011045334,"about_ca_system_score_gemma":0.0004912782,"threshold_uncertainty_score":0.15478402},"labels":[],"label_agreement":null},{"id":"W2100510566","doi":"10.1029/2007gl032268","title":"Probability distribution of sea surface wind stresses","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Canadian Institute for Advanced Research","funders":"","keywords":"Wind stress; Probability density function; Log wind profile; Geology; Surface (topology); Gaussian; Probability distribution; Wind speed; Surface stress; Surface layer; Planetary boundary layer; Boundary layer; Meteorology; Wind shear; Mechanics; Atmospheric sciences; Mathematics; Wind gradient; Physics; Geometry; Layer (electronics); Statistics; Materials science; Oceanography","score_opus":0.05613771647561327,"score_gpt":0.27365694026384746,"score_spread":0.21751922378823418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100510566","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36467862,0.001346756,0.6214431,0.0008164668,0.00014082527,0.0001135424,0.0020564229,0.00068636256,0.008717945],"genre_scores_gemma":[0.988453,0.0010064973,0.0064852363,0.00003618085,0.00010026159,0.00008332899,0.0010944785,0.000053418,0.002687698],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999337,0.00013654366,0.000036581336,0.00017509893,0.00019796666,0.00011679732],"domain_scores_gemma":[0.9940163,0.003857385,0.0005810907,0.0005043997,0.0009013044,0.00013955195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00166903,0.0005055055,0.0005686618,0.0011870492,0.0003512842,0.0015482339,0.00079444,0.0009056527,0.0029737204],"category_scores_gemma":[0.010473162,0.00037268404,0.00058582885,0.001036291,0.0011348228,0.0014687707,0.00050487655,0.00089708803,0.0006237315],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017413512,0.000045092347,0.023245772,0.00015870311,0.00007321731,0.0005683642,0.00015315607,0.82548904,0.0043611573,0.11459732,0.0028702733,0.028263748],"study_design_scores_gemma":[0.000012568209,0.000037945247,0.009659922,0.000033823344,0.000014958546,0.00018132523,0.0000510465,0.9540355,0.0008611621,0.03410526,0.00096237985,0.00004416927],"about_ca_topic_score_codex":0.004058707,"about_ca_topic_score_gemma":0.0013911686,"teacher_disagreement_score":0.004058707,"about_ca_system_score_codex":0.00066611735,"about_ca_system_score_gemma":0.0004989595,"threshold_uncertainty_score":0.009948015},"labels":[],"label_agreement":null},{"id":"W2100919693","doi":"10.1029/2004gl020621","title":"High Himalayan meteorology: Weather at the South Col of Mount Everest","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Climatology; Troposphere; Synoptic scale meteorology; Meteorology; Elevation (ballistics); Environmental science; Mountain range (options); Intrusion; Geology; Geography","score_opus":0.03846622358371912,"score_gpt":0.272536628814572,"score_spread":0.2340704052308529,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2100919693","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99314606,0.00018257274,0.000038747028,0.00016861531,0.0000106204625,0.0000038608464,0.002757864,0.000015353324,0.0036762366],"genre_scores_gemma":[0.99680316,0.00019423336,0.0001120022,0.000024795876,0.000046127738,0.0000030068018,0.002198266,0.000003131001,0.00061528024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999486,0.00000830754,0.000003159128,0.000008723248,0.000018103558,0.000012967169],"domain_scores_gemma":[0.9998516,0.000017528128,0.00005166642,0.000014627542,0.000031007614,0.00003362322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007432538,0.00010708722,0.00007964513,0.0005458562,0.000395473,0.00045104523,0.00010711837,0.00011344307,0.001355179],"category_scores_gemma":[0.00020775846,0.000049319726,0.000057357942,0.0009323277,0.0001366939,0.00022730936,0.00025073718,0.00015468901,0.0002387795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000097534336,0.000025724154,0.98242444,0.000054698605,0.000036348138,0.0005033253,0.0011671139,0.0005347291,0.0023355915,0.00022444442,0.00460536,0.0079905605],"study_design_scores_gemma":[0.0000013927372,0.000005451284,0.9982127,0.000001846547,0.0000029985597,0.00007234831,0.00018054534,0.000070839305,0.00012976678,0.000011261335,0.0013093854,0.0000014925923],"about_ca_topic_score_codex":0.04271314,"about_ca_topic_score_gemma":0.0839849,"teacher_disagreement_score":0.04271314,"about_ca_system_score_codex":0.00029120565,"about_ca_system_score_gemma":0.0002229193,"threshold_uncertainty_score":0.08492905},"labels":[],"label_agreement":null},{"id":"W2101006738","doi":"10.1029/2008gl037049","title":"Reconstructing annual inflows to the headwater catchments of the Murray River, Australia, using the Pacific Decadal Oscillation","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"","keywords":"Pacific decadal oscillation; El Niño Southern Oscillation; Oceanography; Climatology; Geology; Hydrology (agriculture); Southern oscillation; Environmental science","score_opus":0.044902889099003446,"score_gpt":0.32460495552025054,"score_spread":0.27970206642124706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101006738","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99908125,0.000023767285,0.00030876725,0.000028376002,0.0000013222601,0.0000032330702,0.00012040661,0.0000066511743,0.00042628575],"genre_scores_gemma":[0.998042,0.00003852622,0.0011610758,0.0000054552193,0.0000016533971,0.0000044801272,0.00036810042,0.0000031646543,0.00037550574],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999529,0.00000962866,0.0000037383948,0.0000150251535,0.000009956814,0.000008763409],"domain_scores_gemma":[0.99981576,0.000024802268,0.00004778237,0.000019195011,0.00004976054,0.000042807504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016201491,0.000109731445,0.00006956176,0.0007020332,0.0002551864,0.00035477913,0.00016197444,0.00016875281,0.00038599217],"category_scores_gemma":[0.0010234856,0.00016091947,0.00011342631,0.0005440906,0.00012624949,0.00026407794,0.00048568912,0.00015561275,0.00007665273],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000074637086,0.000083597944,0.9436616,0.00002411058,0.000079135956,0.00020526716,0.0011091391,0.011734921,0.0075014834,0.00056736084,0.0005349801,0.034423664],"study_design_scores_gemma":[0.0000065825707,0.000020765956,0.9602449,0.0000067797596,0.00001736749,0.00005423412,0.00036978142,0.037209623,0.0006196191,0.00022859409,0.0012133323,0.000008408517],"about_ca_topic_score_codex":0.072269484,"about_ca_topic_score_gemma":0.13897999,"teacher_disagreement_score":0.072269484,"about_ca_system_score_codex":0.0005574166,"about_ca_system_score_gemma":0.00065466826,"threshold_uncertainty_score":0.14369768},"labels":[],"label_agreement":null},{"id":"W2101284883","doi":"10.1029/2002gl016022","title":"Percolating magmas and explosive volcanism","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Theoretical and Computational Physics","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"","keywords":"Singularity; Bubble; Percolation theory; Explosive material; Volcanism; Percolation (cognitive psychology); Rheology; Void (composites); Physics; Brittleness; Percolation threshold; Geology; Statistical physics; Mechanics; Materials science; Thermodynamics; Geometry; Tectonics; Chemistry; Mathematics","score_opus":0.024580650624343923,"score_gpt":0.3007649173642323,"score_spread":0.27618426673988833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101284883","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9728804,0.0039552115,0.0083280355,0.0009821873,0.00003094758,0.000010474251,0.000036106212,0.00011018764,0.013666368],"genre_scores_gemma":[0.99810505,0.000920024,0.00042830038,0.000035612014,0.000033425276,0.0000031004279,0.000014398054,0.000004093806,0.00045595903],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999428,0.000014596601,0.0000022200377,0.000008453603,0.000019329076,0.00001261651],"domain_scores_gemma":[0.99969065,0.00015249914,0.00009554244,0.000014519653,0.000013449374,0.000033317436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010494151,0.00012291686,0.00011252655,0.00031328594,0.000278517,0.00043210722,0.0001775996,0.00030219136,0.0007073163],"category_scores_gemma":[0.00085981854,0.000101023914,0.00008620551,0.00024856426,0.00093113765,0.00056052237,0.0004322269,0.00028463866,0.000076273136],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002484278,0.0002479121,0.032297514,0.00037066854,0.00007860809,0.0029055804,0.001971506,0.106587924,0.06892435,0.7181862,0.0043954533,0.063785814],"study_design_scores_gemma":[0.00004772201,0.00008560342,0.028352825,0.00003414896,0.000034732806,0.0021160145,0.0003420726,0.123874925,0.008498335,0.8256524,0.01093395,0.00002713246],"about_ca_topic_score_codex":0.000914534,"about_ca_topic_score_gemma":0.0010994404,"teacher_disagreement_score":0.000914534,"about_ca_system_score_codex":0.0003595023,"about_ca_system_score_gemma":0.00011919349,"threshold_uncertainty_score":0.0026084185},"labels":[],"label_agreement":null},{"id":"W2101394879","doi":"10.1029/2008gl034235","title":"Highly periodic stormtime activations observed by THEMIS prior to substorm onset","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Alberta","funders":"","keywords":"Substorm; Magnetosphere; Oscillation (cell signaling); Geophysics; Physics; Surge; Dusk; Flow (mathematics); Magnetic field; Geology; Mechanics; Meteorology; Astronomy","score_opus":0.03217309851995205,"score_gpt":0.278976997514141,"score_spread":0.24680389899418897,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101394879","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99321765,0.00008148499,0.00027150015,0.000075597774,0.000021419692,0.000010546918,0.0004047528,0.00006195357,0.005855031],"genre_scores_gemma":[0.9984913,0.000047198857,0.00016821048,0.000027520453,0.000033363547,0.0000071346726,0.0006821705,0.000006917305,0.0005362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989665,0.000007963568,0.0000049238083,0.000018301005,0.000031329717,0.000040879542],"domain_scores_gemma":[0.9997316,0.000027088667,0.00008225394,0.000024590718,0.00006915809,0.00006538129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017059504,0.00013779699,0.00032547492,0.000576348,0.00048014987,0.00043069234,0.00016922574,0.00025856122,0.0009655645],"category_scores_gemma":[0.0004258868,0.00011427833,0.000121603676,0.00039051712,0.00019307579,0.0001612737,0.0004367016,0.0004232607,0.00022379031],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010425113,0.00013133793,0.76670873,0.0000771362,0.00009109537,0.0018184253,0.0023770197,0.0010293147,0.18204692,0.0013288553,0.0056417696,0.03770684],"study_design_scores_gemma":[0.0000085108195,0.000068948786,0.99232316,0.00001104842,0.000010603791,0.00019403298,0.00028532534,0.0005592119,0.003716918,0.00008055443,0.002736557,0.0000051689008],"about_ca_topic_score_codex":0.0055930857,"about_ca_topic_score_gemma":0.016368471,"teacher_disagreement_score":0.0055930857,"about_ca_system_score_codex":0.00050979684,"about_ca_system_score_gemma":0.00019017146,"threshold_uncertainty_score":0.011121094},"labels":[],"label_agreement":null},{"id":"W2101435360","doi":"10.1029/2001gl014007","title":"A polar low over The Labrador Sea: Interactions with topography and an upper‐level potential vorticity anomaly, and an observation by RADARSAT‐1 SAR","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Mesoscale meteorology; Anomaly (physics); Climatology; Potential vorticity; Polar; Cyclone (programming language); Troposphere; Vorticity; Synthetic aperture radar; Meteorology; Remote sensing; Vortex; Geography","score_opus":0.053022768323591166,"score_gpt":0.28588325476135096,"score_spread":0.2328604864377598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101435360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866796,0.000034610763,0.00022811908,0.00007286849,0.0000017565199,0.0000022572538,0.00015936095,0.000011147729,0.0008219362],"genre_scores_gemma":[0.99946827,0.000032742693,0.0001854862,0.0000069875027,0.0000037004186,0.0000022082513,0.00020749176,0.0000026177909,0.000090536014],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993396,0.000019794543,0.0000031513484,0.000010969787,0.000010454755,0.00002163422],"domain_scores_gemma":[0.9998161,0.00005171398,0.00007765017,0.00001030038,0.000017061546,0.00002725923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014442187,0.00016554495,0.00011988106,0.00039708495,0.00025438963,0.00072361145,0.00014022249,0.00020191948,0.0005344712],"category_scores_gemma":[0.00040934773,0.000091263006,0.00014442283,0.00056599703,0.00036511058,0.00025883896,0.00030753718,0.00023558148,0.00007454137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003082842,0.00013094007,0.942229,0.000055746415,0.00008806475,0.0006637274,0.0002019609,0.025244115,0.010855143,0.0017317773,0.0011466191,0.017344683],"study_design_scores_gemma":[0.000031128824,0.00009078928,0.93192506,0.000013345394,0.00006658808,0.00021436204,0.00046518608,0.06112085,0.0037919472,0.0005856641,0.0016783426,0.000016877611],"about_ca_topic_score_codex":0.021707958,"about_ca_topic_score_gemma":0.026889725,"teacher_disagreement_score":0.97829205,"about_ca_system_score_codex":0.0005464955,"about_ca_system_score_gemma":0.00021357251,"threshold_uncertainty_score":0.04316318},"labels":[],"label_agreement":null},{"id":"W2101607837","doi":"10.1002/2015gl065903","title":"Multisensor profiling of a concentric gravity wave event propagating from the troposphere to the ionosphere","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":158,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Office of Naval Research; National Oceanic and Atmospheric Administration; Natural Resources Canada; National Aeronautics and Space Administration","keywords":"Ionosphere; Airglow; Troposphere; Mesosphere; Gravity wave; Stratosphere; Geology; Atmospheric sciences; Remote sensing; Environmental science; Geophysics; Physics; Gravitational wave; Astronomy","score_opus":0.03450341707112612,"score_gpt":0.3042782144203374,"score_spread":0.2697747973492113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101607837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954333,0.00008484828,0.0017944456,0.000036353533,0.000019858864,0.00000878932,0.00070546765,0.00009043343,0.001826458],"genre_scores_gemma":[0.9967962,0.000042398344,0.0021410885,0.0000151098975,0.000008273534,0.0000049252903,0.00054387207,0.000006299181,0.00044186242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.000003860338,0.0000027791348,0.000016121263,0.000022497934,0.000011661748],"domain_scores_gemma":[0.9999056,0.000008767926,0.000023016757,0.000009973897,0.0000335346,0.000019146455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008773436,0.00015649156,0.000119594464,0.0006963919,0.00020041036,0.00028994266,0.00013025098,0.00016484682,0.00072104076],"category_scores_gemma":[0.00015783594,0.000084841784,0.00011444452,0.00048772994,0.00006992996,0.00022063937,0.00033661324,0.00014964664,0.00011649689],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061567343,0.00022347955,0.60163635,0.00007475198,0.00017468727,0.00039497737,0.0007752292,0.010933408,0.2897136,0.00038939636,0.0033899667,0.091678485],"study_design_scores_gemma":[0.00001775477,0.000112985676,0.9648671,0.000013528206,0.000042096955,0.00009309721,0.00034936352,0.020937642,0.011242409,0.00009744295,0.0022104525,0.0000162082],"about_ca_topic_score_codex":0.009771854,"about_ca_topic_score_gemma":0.031421974,"teacher_disagreement_score":0.009771854,"about_ca_system_score_codex":0.00018341905,"about_ca_system_score_gemma":0.00018558286,"threshold_uncertainty_score":0.019429922},"labels":[],"label_agreement":null},{"id":"W2101785952","doi":"10.1029/2004gl020410","title":"First near‐global retrievals of OH rotational temperatures from satellite‐based Meinel band emission measurements","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Bundesministerium für Bildung und Forschung","keywords":"SCIAMACHY; Mesopause; Satellite; Rotational temperature; Latitude; Airglow; Environmental science; Atmospheric sciences; Remote sensing; Atmosphere (unit); Mesosphere; Spectrometer; Atmospheric Infrared Sounder; Meteorology; Physics; Geodesy; Stratosphere; Spectral line; Geology; Astronomy; Optics","score_opus":0.05163414221073773,"score_gpt":0.3024831036621262,"score_spread":0.25084896145138846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2101785952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96821207,0.0016705024,0.017906832,0.0001191164,0.000059068432,0.000088108536,0.00457915,0.0007312142,0.006633817],"genre_scores_gemma":[0.93686473,0.0008262153,0.046581075,0.000069851645,0.000047112368,0.00006252623,0.013112368,0.00020108478,0.0022349893],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990785,0.0000105715235,0.000004161679,0.000027677153,0.000027703269,0.000022047869],"domain_scores_gemma":[0.999821,0.000024252542,0.000032326436,0.00004072711,0.000066020686,0.000015693988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032827148,0.0005230936,0.00034243477,0.00053333055,0.00023674585,0.00048757982,0.00026666952,0.00036366514,0.0009249317],"category_scores_gemma":[0.00042000329,0.00027579375,0.00033945288,0.0006306857,0.00021643072,0.0006872503,0.0007033692,0.0003706741,0.00034602772],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014807694,0.0003501064,0.15177853,0.0007559735,0.0008132322,0.00049615314,0.0008939066,0.03657594,0.4673037,0.0015276402,0.008027026,0.32999712],"study_design_scores_gemma":[0.0003195809,0.0009231673,0.7746445,0.00012506328,0.00059330015,0.0003981825,0.00044869483,0.049216177,0.1315117,0.0011753237,0.040461507,0.00018274477],"about_ca_topic_score_codex":0.004987953,"about_ca_topic_score_gemma":0.00934464,"teacher_disagreement_score":0.004987953,"about_ca_system_score_codex":0.00024647714,"about_ca_system_score_gemma":0.0002538525,"threshold_uncertainty_score":0.009917855},"labels":[],"label_agreement":null},{"id":"W2102133128","doi":"10.1029/2006gl026013","title":"Ice core evidence for a second volcanic eruption around 1809 in the Northern Hemisphere","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Tephra; Geology; Volcano; Dense-rock equivalent; Vulcanian eruption; Northern Hemisphere; Ice core; Phreatomagmatic eruption; Peléan eruption; Explosive eruption; Climatology; Paleontology; Magma","score_opus":0.09130495776659567,"score_gpt":0.3417765368478451,"score_spread":0.2504715790812494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102133128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955107,0.00024987015,0.000059618204,0.0000893684,0.0000125006,0.000004608759,0.0004260199,0.000008513279,0.003638859],"genre_scores_gemma":[0.9982368,0.00016160401,0.00009263002,0.000050630784,0.00002952037,0.0000037789928,0.0010349263,0.0000044638896,0.00038568428],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988234,0.000008864308,0.000007368644,0.000031467578,0.000030231065,0.000039605377],"domain_scores_gemma":[0.9993875,0.00004696325,0.00023605522,0.000038472754,0.00015128209,0.00013975156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029598616,0.00013710967,0.0001917969,0.0005040841,0.0005582631,0.0006244408,0.00014919626,0.00029264454,0.0018978104],"category_scores_gemma":[0.0005464819,0.000120797224,0.00013368286,0.0003940535,0.00029725395,0.00024128087,0.00025682102,0.00020434706,0.000258668],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051773456,0.00006129413,0.9356247,0.00006010034,0.00007199204,0.00064477214,0.00092077174,0.0002134407,0.04952543,0.0002699214,0.0013009728,0.010788884],"study_design_scores_gemma":[0.000008237034,0.00001504931,0.99790895,0.0000041046424,0.000007314024,0.00012268296,0.00011916507,0.00005130312,0.0005728065,0.00001693258,0.0011717363,0.0000016941505],"about_ca_topic_score_codex":0.025391825,"about_ca_topic_score_gemma":0.041765016,"teacher_disagreement_score":0.025391825,"about_ca_system_score_codex":0.00062556815,"about_ca_system_score_gemma":0.0004285584,"threshold_uncertainty_score":0.050488055},"labels":[],"label_agreement":null},{"id":"W2102331366","doi":"10.1029/2000gl011653","title":"Western Mediterranean sea‐level rise: Changing exchange flow through the Strait of Gibraltar","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Mediterranean climate; Oceanography; Mediterranean sea; Sea level; Tide gauge; Inflow; Climatology; Geology; Altimeter; Sea level rise; Climate change; Geography","score_opus":0.060817788571718844,"score_gpt":0.2928747720445423,"score_spread":0.23205698347282347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102331366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99901354,0.00011501929,0.00002190397,0.00008927998,0.0000026822654,0.0000018712359,0.00013088473,0.0000069700172,0.0006177594],"genre_scores_gemma":[0.999542,0.00007662824,0.000047170455,0.00003738778,0.0000034326351,0.0000020516054,0.00013054284,0.0000018270043,0.00015908298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994016,0.0000144672895,0.000005298982,0.00001401127,0.0000072483294,0.00001885302],"domain_scores_gemma":[0.9998635,0.000017220746,0.000056086817,0.000008883234,0.00002845192,0.000025755378],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000120732395,0.000120099816,0.0001416228,0.00045317534,0.00012983111,0.00052075024,0.00014732973,0.00028542022,0.00092056487],"category_scores_gemma":[0.00062358915,0.00006894686,0.00014088013,0.000528789,0.00017562413,0.00019469002,0.00022442298,0.000121223355,0.00015850995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055072736,0.00003931656,0.9546727,0.000047522437,0.000117843374,0.0012983781,0.0019459147,0.00067530543,0.009733922,0.00036688976,0.0010539774,0.029497452],"study_design_scores_gemma":[0.0000067329547,0.000028047933,0.99901676,0.0000033208357,0.000008607918,0.00007090799,0.00017457505,0.00020520297,0.00006839808,0.00001626811,0.0003992101,0.0000019097347],"about_ca_topic_score_codex":0.05327547,"about_ca_topic_score_gemma":0.04804189,"teacher_disagreement_score":0.05327547,"about_ca_system_score_codex":0.00063157536,"about_ca_system_score_gemma":0.0002180137,"threshold_uncertainty_score":0.105930746},"labels":[],"label_agreement":null},{"id":"W2102453364","doi":"10.1029/2009gl039818","title":"Quantifying biological carbon export for the northwest North Atlantic continental shelves","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Continental shelf; Biogeochemical cycle; Continental margin; Oceanography; Advection; Biological pump; Environmental science; Carbon cycle; Total organic carbon; Geology; Ecosystem; Ecology; Biology; Paleontology","score_opus":0.06970414091553673,"score_gpt":0.2925171361625888,"score_spread":0.22281299524705206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102453364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990736,0.00002721071,0.00021515418,0.000013848919,9.5292705e-7,0.0000012808466,0.00026043667,0.000009717186,0.00039782448],"genre_scores_gemma":[0.9986028,0.000052839147,0.00044697063,0.0000070478873,0.0000013985747,0.0000028841532,0.0005992598,0.00000564222,0.00028101506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999728,0.000003671349,0.0000024094318,0.000009863344,0.000006440058,0.000004875186],"domain_scores_gemma":[0.9999101,0.000026601463,0.000019160389,0.000010819954,0.000021825681,0.000011461852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013789597,0.00028020135,0.00014089841,0.0002611495,0.00024962515,0.0003702325,0.00014522113,0.00021763219,0.0006024302],"category_scores_gemma":[0.00032956435,0.00013969812,0.00021986406,0.00022013402,0.00012892632,0.00028613053,0.00026349016,0.00014785552,0.0000891093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021317537,0.000045938614,0.89742285,0.00003649015,0.00010295716,0.00015027655,0.00010362383,0.062237248,0.029265992,0.00035895332,0.00019753932,0.009865038],"study_design_scores_gemma":[0.000023091437,0.00004786825,0.8998285,0.000005993431,0.00003568411,0.00004110872,0.00013968056,0.09409627,0.0050888737,0.00023181691,0.0004514471,0.000009636487],"about_ca_topic_score_codex":0.058754373,"about_ca_topic_score_gemma":0.104073964,"teacher_disagreement_score":0.058754373,"about_ca_system_score_codex":0.0006282071,"about_ca_system_score_gemma":0.0002710143,"threshold_uncertainty_score":0.116824806},"labels":[],"label_agreement":null},{"id":"W2102499426","doi":"10.1029/2003gl017585","title":"Detection of a D″ discontinuity in the south Atlantic using PKKP","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Coda; Discontinuity (linguistics); Mantle (geology); Amplitude; Jump; Seismology; Core–mantle boundary; Geodesy; Classification of discontinuities; Reflection (computer programming); Geophysics; Physics; Optics","score_opus":0.05857724332399869,"score_gpt":0.29559151099123376,"score_spread":0.23701426766723507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2102499426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99573225,0.000044034576,0.0019041878,0.000042205676,0.000004898692,0.0000063439516,0.00031414814,0.00005497963,0.0018969484],"genre_scores_gemma":[0.99774337,0.000031534044,0.0017716119,0.000005893664,0.000002351893,0.000002273129,0.00031090147,0.000004205325,0.00012788852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999287,0.000007155806,0.000004821439,0.000026384772,0.000015978347,0.000017046179],"domain_scores_gemma":[0.9998035,0.00003667447,0.00005272041,0.000030778298,0.00004197297,0.00003447098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012588261,0.00012907381,0.00010419703,0.0004110397,0.00028346363,0.00037197382,0.00021950064,0.0002634505,0.0008133577],"category_scores_gemma":[0.0008020343,0.00019667222,0.00012902348,0.00042288547,0.0001611017,0.00031561105,0.00048717097,0.00028964953,0.00020336607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005531556,0.000036082452,0.70569605,0.00011606012,0.000051852163,0.00042412014,0.00047179905,0.0048907404,0.21824598,0.0009429095,0.00046671732,0.06810457],"study_design_scores_gemma":[0.000020047946,0.000061568084,0.97004426,0.000016836642,0.000025137078,0.00035013142,0.00017448424,0.019863889,0.008245611,0.00026228657,0.00091748656,0.00001823309],"about_ca_topic_score_codex":0.01289305,"about_ca_topic_score_gemma":0.023796782,"teacher_disagreement_score":0.01289305,"about_ca_system_score_codex":0.00030366625,"about_ca_system_score_gemma":0.0002411677,"threshold_uncertainty_score":0.025636017},"labels":[],"label_agreement":null},{"id":"W2103011744","doi":"10.1029/2012gl052740","title":"Maximum wind speeds and US hurricane losses","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":114,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Division of Ocean Sciences; Canadian Institute for Theoretical Astrophysics","keywords":"Quantile; Wind speed; Environmental science; Meteorology; Population; Roughness length; Climatology; Precipitation; Atmospheric sciences; Exponential function; Climate change; Statistics; Wind profile power law; Mathematics; Geography; Demography; Geology","score_opus":0.0405966149694859,"score_gpt":0.29868424591792725,"score_spread":0.25808763094844134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103011744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649364,0.00019710297,0.00033127016,0.00012157472,0.0000074402483,0.0000029472517,0.0009758458,0.000017393206,0.0018527335],"genre_scores_gemma":[0.9988638,0.00006091431,0.00006524814,0.0000096490885,0.000006002625,0.000002491128,0.00073994516,0.0000030576302,0.00024896342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998184,0.000050004997,0.000014468949,0.000025755813,0.00005088924,0.000040525876],"domain_scores_gemma":[0.99799687,0.0006308532,0.00081257854,0.00018603967,0.00022713876,0.00014649707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003928201,0.00015537048,0.000114909046,0.0005182645,0.00017581681,0.0004509543,0.000091990296,0.00015792355,0.0022098636],"category_scores_gemma":[0.0035710705,0.00011812042,0.00016193397,0.0005052682,0.00018914304,0.00030671584,0.00038597875,0.00038255457,0.00027683933],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019027173,0.0000343099,0.9815456,0.000012361508,0.00005974321,0.000052796608,0.00008241576,0.006188641,0.00028234656,0.00046552715,0.0013805234,0.009705488],"study_design_scores_gemma":[0.000003936272,0.000033359447,0.9947162,0.000007793551,0.0000065730005,0.00007120219,0.00009675023,0.0037468192,0.00015194449,0.00046567526,0.0006942837,0.000005463154],"about_ca_topic_score_codex":0.0054932353,"about_ca_topic_score_gemma":0.0063999845,"teacher_disagreement_score":0.0054932353,"about_ca_system_score_codex":0.00023359731,"about_ca_system_score_gemma":0.000083684405,"threshold_uncertainty_score":0.010922492},"labels":[],"label_agreement":null},{"id":"W2103165697","doi":"10.1029/2012gl051886","title":"Lake‐size dependency of wind shear and convection as controls on gas exchange","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":322,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of the Environment, Conservation and Parks","funders":"","keywords":"Wind shear; Convection; Turbulence; Atmospheric sciences; Environmental science; Geology; Mixed layer; Shear (geology); Wind speed; Hydrology (agriculture); Climatology; Meteorology; Oceanography; Geography","score_opus":0.023617408732189493,"score_gpt":0.27284139164328297,"score_spread":0.2492239829110935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103165697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960595,0.000047871905,0.00011670971,0.00000539405,7.1856834e-7,0.0000023097,0.000046407225,0.0000050073368,0.00016973099],"genre_scores_gemma":[0.99972504,0.000022160717,0.0001102764,0.0000026735531,0.0000011138567,0.0000034620593,0.000055404147,0.0000031440386,0.000076800396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.000028240169,0.000008996331,0.000023716013,0.000015879265,0.000021652613],"domain_scores_gemma":[0.99966824,0.00015294431,0.00007880898,0.00002192175,0.000035604207,0.000042489657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000301624,0.00017795322,0.00022949972,0.00030699142,0.00026596567,0.00045523778,0.00011349177,0.0001414893,0.00043768933],"category_scores_gemma":[0.00085020345,0.00026059334,0.00021924735,0.00027762118,0.00036743924,0.00043640783,0.000442361,0.0001086281,0.00006173367],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00109142,0.000037671707,0.7818986,0.00009888817,0.00015618258,0.00021051688,0.00089993427,0.0026741016,0.20217733,0.00020970596,0.00014908462,0.010396595],"study_design_scores_gemma":[0.0000067498454,0.000044717413,0.99507195,0.0000016594772,0.000023413375,0.000019116385,0.00007882641,0.0018804468,0.0027007111,0.000034123255,0.00013261293,0.0000054893917],"about_ca_topic_score_codex":0.008419559,"about_ca_topic_score_gemma":0.015503707,"teacher_disagreement_score":0.008419559,"about_ca_system_score_codex":0.00030618996,"about_ca_system_score_gemma":0.00024080445,"threshold_uncertainty_score":0.016741157},"labels":[],"label_agreement":null},{"id":"W2103498300","doi":"10.1029/2002gl016766","title":"Abrupt thermal transition reveals hydrothermal boundary and role of seamounts within the Cocos Plate","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Lithosphere; Geology; Seafloor spreading; Hydrothermal circulation; Crust; Seamount; Geophysics; Plate tectonics; Basement; Transition zone; Thermal; Tectonics; Oceanic crust; Petrology; Seismology; Geochemistry; Subduction","score_opus":0.015858580463106293,"score_gpt":0.24078098864901493,"score_spread":0.22492240818590864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103498300","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99937636,0.00003472779,0.000037523278,0.0000057813722,9.971608e-7,9.771068e-7,0.00007456668,0.000005279555,0.0004638301],"genre_scores_gemma":[0.99972576,0.000021323765,0.000041157,0.0000024916849,0.0000015821929,0.0000016762668,0.00013145682,0.0000024514388,0.000072244286],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999429,0.0000043289338,0.000003566247,0.000021772159,0.000007793323,0.000019627383],"domain_scores_gemma":[0.9998566,0.000022452798,0.0000418459,0.000012403113,0.000037245536,0.00002955181],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009085237,0.00011979581,0.00015283783,0.00076253363,0.0002983533,0.00047747046,0.0001467451,0.00015888948,0.0010045685],"category_scores_gemma":[0.00033521236,0.00011475772,0.00010006248,0.0005279183,0.0004409069,0.00019045272,0.00039350113,0.00013138312,0.00011735362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043360065,0.000024442452,0.91667044,0.00003300485,0.00003305216,0.0002876337,0.0010502316,0.00079417945,0.068155415,0.00027915102,0.0001712626,0.012067591],"study_design_scores_gemma":[0.000001755894,0.0000077393925,0.9987483,0.0000024569606,0.000004303925,0.000026016458,0.00013984197,0.00037130844,0.00055940205,0.000019523186,0.0001173341,0.0000019724414],"about_ca_topic_score_codex":0.032164,"about_ca_topic_score_gemma":0.050041523,"teacher_disagreement_score":0.032164,"about_ca_system_score_codex":0.00042994946,"about_ca_system_score_gemma":0.0002245996,"threshold_uncertainty_score":0.06395358},"labels":[],"label_agreement":null},{"id":"W2103573068","doi":"10.1029/2012gl051691","title":"Bubble‐induced turbulence suppression in Langmuir circulation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Dissipation; Turbulence; Turbulence kinetic energy; Physics; Buoyancy; Bubble; Stratification (seeds); Mechanics; Eddy; Atmospheric sciences; Meteorology; Thermodynamics","score_opus":0.04387468541631784,"score_gpt":0.29653676233212384,"score_spread":0.252662076915806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103573068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99945337,0.00004002568,0.00020427398,0.000007480523,0.0000012903786,0.0000018207288,0.000026179503,0.0000101326505,0.00025547936],"genre_scores_gemma":[0.9996939,0.0000135154805,0.00008748511,0.000002899595,0.0000012570205,0.0000027398462,0.000047743113,0.000002521322,0.00014793746],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999471,0.0000049870723,0.0000039268707,0.000011309286,0.0000136896,0.000018952931],"domain_scores_gemma":[0.99976903,0.00003111578,0.000085712265,0.0000170257,0.000043951608,0.000053128166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008139916,0.00010124322,0.00014237971,0.00021449165,0.00011056268,0.00023045157,0.00009753805,0.00009556106,0.00072268693],"category_scores_gemma":[0.00045809647,0.00014991987,0.0001381235,0.00010053132,0.00020109925,0.00018429803,0.00028868928,0.00015201548,0.00013051629],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090026023,0.000058616763,0.10969882,0.000054449414,0.00002821376,0.00025125273,0.00029974867,0.0009831376,0.8802542,0.00025916926,0.0001491394,0.0070629898],"study_design_scores_gemma":[0.000024703897,0.00028163556,0.9328011,0.0000058108885,0.000020903315,0.0001965786,0.000111133246,0.0059748646,0.060041253,0.00010785301,0.00041853785,0.000015629947],"about_ca_topic_score_codex":0.0021271969,"about_ca_topic_score_gemma":0.0016015681,"teacher_disagreement_score":0.0021271969,"about_ca_system_score_codex":0.00027386734,"about_ca_system_score_gemma":0.00015276295,"threshold_uncertainty_score":0.004229605},"labels":[],"label_agreement":null},{"id":"W2103576714","doi":"10.1029/2007gl030892","title":"Using reversed magnetic flux spots to determine a planet's inner core size","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Inner core; Planet; Dynamo; Physics; Dynamo theory; Magnetic flux; Flux (metallurgy); Core (optical fiber); Magnetic field; Astrobiology; Geophysics; Astrophysics; Materials science; Optics","score_opus":0.049371162500705716,"score_gpt":0.32659988366961573,"score_spread":0.27722872116891,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103576714","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9691478,0.00029914486,0.027398594,0.000038270133,0.0000096989415,0.0000072243915,0.00021463884,0.00015334265,0.0027312324],"genre_scores_gemma":[0.99165994,0.00009933086,0.0077840877,0.0000075335483,0.0000033218703,0.0000074581662,0.0001353178,0.000014412355,0.0002886119],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995244,0.0000078599915,0.0000023606951,0.00002145977,0.000011213292,0.0000046564287],"domain_scores_gemma":[0.9997136,0.00011678619,0.00007313773,0.000045402423,0.000035797133,0.000015212577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015576342,0.0001263344,0.00012325945,0.00048139473,0.000121891586,0.00030544936,0.00019618377,0.00019284213,0.000604423],"category_scores_gemma":[0.0008093486,0.00013383884,0.00010398749,0.0001830263,0.00021039361,0.0003414664,0.00018827792,0.00012482941,0.00024770832],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036299878,0.000031823223,0.1721972,0.00012314587,0.00005864445,0.00015880035,0.00023484796,0.026214695,0.74035835,0.004509277,0.0003872631,0.055362996],"study_design_scores_gemma":[0.000034937395,0.00015989397,0.35475284,0.000019935036,0.000052552587,0.0007125621,0.00014373375,0.20445457,0.4318462,0.0045732604,0.003185637,0.000063814805],"about_ca_topic_score_codex":0.0012461061,"about_ca_topic_score_gemma":0.0014341698,"teacher_disagreement_score":0.0012461061,"about_ca_system_score_codex":0.0002179711,"about_ca_system_score_gemma":0.000077419965,"threshold_uncertainty_score":0.0024777055},"labels":[],"label_agreement":null},{"id":"W2103979543","doi":"10.1002/grl.50188","title":"Pre‐modern Arctic Ocean circulation from surface sediment neodymium isotopes","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Oceanography; Arctic; Authigenic; North Atlantic Deep Water; Canada Basin; Sediment; Seafloor spreading; Arctic dipole anomaly; Surface water; Ocean current; Water column; Circumpolar deep water; Bottom water; Thermohaline circulation; Arctic ice pack; Environmental science; Paleontology; Drift ice","score_opus":0.028251893057907186,"score_gpt":0.2740878336195875,"score_spread":0.24583594056168032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2103979543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938817,0.0008983575,0.00035061216,0.00003597994,0.0000110364845,0.000001788705,0.0006704521,0.000008660661,0.004141475],"genre_scores_gemma":[0.9982761,0.0004565289,0.00031410845,0.000009645215,0.000009394838,0.0000018072079,0.0004876703,0.0000034195564,0.0004413257],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996006,0.000005254647,0.000003739755,0.000012886937,0.000008936409,0.000009138634],"domain_scores_gemma":[0.99982685,0.000022099151,0.000031658503,0.00001455971,0.00008262809,0.000022193073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019889636,0.00017043295,0.00008962249,0.0010476735,0.00042077774,0.00065001467,0.00008661835,0.00010318336,0.0010772902],"category_scores_gemma":[0.000324815,0.00010188688,0.000102197075,0.00064610044,0.00026374124,0.00028445583,0.0002655438,0.00018170894,0.00025472505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016002997,0.000013379799,0.9550999,0.000039215232,0.00006989418,0.00012285612,0.0007292482,0.0005135486,0.013447394,0.00054133334,0.00021388374,0.029049264],"study_design_scores_gemma":[8.2185903e-7,0.000011907208,0.9959883,0.000011199129,0.000010189302,0.0000813184,0.00018343989,0.00017243795,0.00092982943,0.0000888395,0.0025187891,0.0000029030534],"about_ca_topic_score_codex":0.020543182,"about_ca_topic_score_gemma":0.053433064,"teacher_disagreement_score":0.020543182,"about_ca_system_score_codex":0.00046040988,"about_ca_system_score_gemma":0.000259494,"threshold_uncertainty_score":0.040847242},"labels":[],"label_agreement":null},{"id":"W2104259026","doi":"10.1029/2006gl029209","title":"Impact of diapycnal mixing on the saturation state of argon in the subtropical North Pacific","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Joint Institute for the Study of the Atmosphere and Ocean; University of Washington; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Thermocline; Transect; Geology; TRACER; Mixing (physics); Ocean gyre; Oceanography; Atmospheric sciences; Environmental science; Subtropics; Physics","score_opus":0.027307293228132936,"score_gpt":0.2870731501900536,"score_spread":0.25976585696192067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104259026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991548,0.00005061533,0.00011291336,0.00004128433,0.000001192332,0.0000011012492,0.000048024616,0.0000080804,0.00058199355],"genre_scores_gemma":[0.99984944,0.000024910061,0.000036096564,0.0000061543933,8.437024e-7,9.086955e-7,0.000029609484,0.0000023743826,0.000049687762],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988043,0.000027613041,0.000007935177,0.000038542054,0.000021754902,0.000023651322],"domain_scores_gemma":[0.99942017,0.00028820417,0.00008576885,0.00005402656,0.00008980058,0.00006202085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039357765,0.00030828986,0.00019681254,0.00036445263,0.00040613752,0.0004014171,0.00021335616,0.00024813734,0.000744524],"category_scores_gemma":[0.0014097979,0.00031226344,0.00025263216,0.00023877926,0.00057271385,0.0005906232,0.0006805916,0.00020497406,0.00008840731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001057869,0.00004863497,0.773895,0.00006502842,0.00017559751,0.00049831404,0.0005242796,0.014973085,0.19608456,0.00062178867,0.00014955246,0.011906255],"study_design_scores_gemma":[0.000018213623,0.0000518992,0.97574097,0.000005849991,0.00004473107,0.000049153998,0.00016646956,0.014223955,0.009281014,0.00019108686,0.00021224312,0.000014309513],"about_ca_topic_score_codex":0.03914278,"about_ca_topic_score_gemma":0.03732191,"teacher_disagreement_score":0.03914278,"about_ca_system_score_codex":0.0007250517,"about_ca_system_score_gemma":0.00041109207,"threshold_uncertainty_score":0.0778299},"labels":[],"label_agreement":null},{"id":"W2104616124","doi":"10.1029/2005gl022396","title":"Comparisons between ACE‐FTS and ground‐based measurements of stratospheric HCl and ClONO<sub>2</sub> loadings at northern latitudes","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; University of Toronto","funders":"","keywords":"Stratosphere; Atmospheric sciences; Atmospheric chemistry; Environmental science; Latitude; Northern Hemisphere; Mixing ratio; Middle latitudes; Climatology; Atmosphere of Earth; Hydrogen chloride; Atmosphere (unit); Ozone; Meteorology; Chemistry; Geology; Physics; Geodesy","score_opus":0.058790210962507757,"score_gpt":0.28515589562933746,"score_spread":0.22636568466682971,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104616124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987105,0.000030862073,0.0001553241,0.0000050383446,0.0000015038138,0.0000015484769,0.00047002078,0.000007825533,0.00061735243],"genre_scores_gemma":[0.99739337,0.000044275137,0.0004832399,0.000008034754,0.000003510472,0.0000035202481,0.0018130305,0.0000038921544,0.00024712406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999044,0.000011251572,0.0000045695356,0.000023861323,0.000037363225,0.000018605382],"domain_scores_gemma":[0.99977475,0.000039102848,0.000048023994,0.00002187772,0.00009220954,0.000024050993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001730636,0.00018319653,0.00012826062,0.00036305859,0.00018740067,0.0002941133,0.00012332977,0.00014745131,0.00031395152],"category_scores_gemma":[0.00035294346,0.00011403818,0.00011046309,0.00038296983,0.00011022644,0.00015760328,0.00013422611,0.00009265083,0.00009773357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011607344,0.00008704196,0.8234339,0.000058658992,0.00015845905,0.00022645477,0.0007077028,0.004081758,0.14830525,0.00018345109,0.00046481652,0.021131814],"study_design_scores_gemma":[0.0000076461,0.00003460795,0.9887552,0.000001540369,0.000018882025,0.000038021655,0.0000834212,0.0013706763,0.009327615,0.000011811821,0.00034632665,0.0000042228035],"about_ca_topic_score_codex":0.04366277,"about_ca_topic_score_gemma":0.09417977,"teacher_disagreement_score":0.04366277,"about_ca_system_score_codex":0.0005057407,"about_ca_system_score_gemma":0.00022551179,"threshold_uncertainty_score":0.086817265},"labels":[],"label_agreement":null},{"id":"W2104706002","doi":"10.1029/2011gl048794","title":"Revisiting the Earth's sea-level and energy budgets from 1961 to 2008","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":661,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Glacier; Tide gauge; Sea level; Environmental science; Radiative forcing; Future sea level; Sea level rise; Climatology; Forcing (mathematics); Climate change; Atmospheric sciences; Geology; Oceanography; Cryosphere; Sea ice; Geomorphology; Ice shelf","score_opus":0.09978770720068345,"score_gpt":0.27432288423005124,"score_spread":0.1745351770293678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104706002","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.06620984,0.8711229,0.005241429,0.008971823,0.002183834,0.000043142292,0.018033935,0.00022245132,0.027970629],"genre_scores_gemma":[0.18157747,0.7835636,0.007873576,0.0025439553,0.002412021,0.000055015604,0.010311851,0.00013611364,0.011526395],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99987864,0.000013633633,0.00001782363,0.000035799767,0.000039643663,0.0000143015295],"domain_scores_gemma":[0.9998369,0.000023309936,0.00006024921,0.0000090932,0.000058907895,0.000011631233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024996357,0.00082819554,0.00023311719,0.0016178864,0.00022235657,0.0008486196,0.0003548869,0.0003328203,0.0016751998],"category_scores_gemma":[0.00090816343,0.0002074819,0.00028656353,0.0034039484,0.00031660832,0.0018162541,0.0004919021,0.0006183906,0.00059862685],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002457562,0.000037186775,0.03712147,0.0077758064,0.00036715495,0.00044442658,0.00068676536,0.018374853,0.0072359117,0.013191946,0.07503543,0.8394834],"study_design_scores_gemma":[0.000010978842,0.000049236518,0.08520326,0.0026174218,0.00020339558,0.00036190051,0.00016353537,0.0010899494,0.0013033533,0.0023557616,0.9066068,0.000034421704],"about_ca_topic_score_codex":0.039321523,"about_ca_topic_score_gemma":0.053406443,"teacher_disagreement_score":0.039321523,"about_ca_system_score_codex":0.0019448511,"about_ca_system_score_gemma":0.0017475663,"threshold_uncertainty_score":0.07818526},"labels":[],"label_agreement":null},{"id":"W2104913197","doi":"10.1029/2003gl018046","title":"Temperatures at the base of the Laurentide Ice Sheet inferred from borehole temperature data","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique","keywords":"Geology; Ice sheet; Ice stream; Glacier morphology; Glacier; Borehole; Ice tongue; Last Glacial Maximum; Ice-sheet model; Climatology; Glacial period; Cryosphere; Physical geography; Geomorphology; Paleontology; Sea ice; Geography","score_opus":0.05604307933754996,"score_gpt":0.28860016424720647,"score_spread":0.23255708490965651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2104913197","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947625,0.000045389435,0.00039981573,0.00001612122,0.0000018125324,0.0000073401757,0.0021501933,0.00004167636,0.0025752378],"genre_scores_gemma":[0.995542,0.00006114153,0.0012060108,0.000006903539,0.0000014947417,0.000009528829,0.0024165332,0.000006057782,0.0007503218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998728,0.000004361603,0.0000038476883,0.000030891475,0.000044659788,0.000043390693],"domain_scores_gemma":[0.99972636,0.00002310376,0.000057295456,0.000017865124,0.00013515966,0.000040190473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114632276,0.00019792831,0.00013249199,0.00083615567,0.00053770747,0.00045769315,0.00028870002,0.000105125895,0.0007108655],"category_scores_gemma":[0.0004760421,0.00013925924,0.000119279226,0.0007287279,0.00022694857,0.00022363843,0.00029438487,0.00015411805,0.00020857403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016514675,0.000031655993,0.9599673,0.000029678613,0.000025659629,0.000106868225,0.0012240158,0.0026952052,0.016734073,0.0002623805,0.0010962035,0.01766182],"study_design_scores_gemma":[0.000005950145,0.000013420527,0.9926439,0.000009037705,0.000008026015,0.00003931761,0.0002851118,0.0024966213,0.0026287744,0.000044652144,0.0018146078,0.000010638706],"about_ca_topic_score_codex":0.7786361,"about_ca_topic_score_gemma":0.9208497,"teacher_disagreement_score":0.7786361,"about_ca_system_score_codex":0.0023769476,"about_ca_system_score_gemma":0.0027327766,"threshold_uncertainty_score":0.4453351},"labels":[],"label_agreement":null},{"id":"W2105092996","doi":"10.1029/2007gl031059","title":"Asthenospheric upwelling, oceanic slab retreat, and exhumation of UHP mantle rocks: Insights from Greater Antilles","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Ottawa","funders":"Centre National de la Recherche Scientifique; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Geology; Subduction; Mantle (geology); Upwelling; Asthenosphere; Mantle wedge; Slab; Oceanic crust; Geochemistry; Peridotite; Petrology; Geophysics; Seismology; Oceanography; Tectonics","score_opus":0.023055182653510406,"score_gpt":0.24496291808321916,"score_spread":0.22190773542970876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105092996","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99920636,0.000047218877,0.00007587668,0.00005178872,6.1015385e-7,0.0000012883801,0.00004132699,0.000005243085,0.00057029346],"genre_scores_gemma":[0.9995789,0.000105382605,0.00011988711,0.0000078735275,0.000002153404,0.0000016577477,0.000050607996,0.0000034348247,0.00013012358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999727,0.0000050149097,0.0000019002691,0.000007360095,0.000004263199,0.000008748977],"domain_scores_gemma":[0.99990594,0.000028524419,0.000027098506,0.000011769713,0.000009677708,0.000016987224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107338616,0.00024256979,0.00022826192,0.0003764609,0.00031945235,0.0004951051,0.00028529836,0.00034282706,0.0011442935],"category_scores_gemma":[0.0003264971,0.00023852442,0.0003658175,0.00037516095,0.00045810084,0.00041540503,0.00057172996,0.00022783663,0.00014465189],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006619403,0.0001725859,0.7810376,0.00018520163,0.00014711953,0.0018577399,0.0016718198,0.06265756,0.13559903,0.0019649668,0.0003167931,0.013727651],"study_design_scores_gemma":[0.00007798532,0.00012255643,0.89587986,0.000018166495,0.000050717175,0.00030749923,0.0006393027,0.0959455,0.00514062,0.00086201733,0.0009315604,0.000024083502],"about_ca_topic_score_codex":0.031738758,"about_ca_topic_score_gemma":0.026599353,"teacher_disagreement_score":0.031738758,"about_ca_system_score_codex":0.0007478815,"about_ca_system_score_gemma":0.00028268498,"threshold_uncertainty_score":0.06310803},"labels":[],"label_agreement":null},{"id":"W2105361124","doi":"10.1002/2014gl061313","title":"Impact of Weddell Sea deep convection on natural and anthropogenic carbon in a climate model","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Oceanic and Atmospheric Administration; Sight Research UK; Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research; Natural Environment Research Council; Princeton University","keywords":"Environmental science; Climate change; Convection; Climatology; Deep sea; Climate model; Atmospheric sciences; Oceanography; Deep convection; Carbon fibers; Carbon cycle; Geology; Meteorology; Ecosystem; Ecology; Geography; Biology","score_opus":0.025777678060423723,"score_gpt":0.3256336788331523,"score_spread":0.29985600077272856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2105361124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981914,0.000033137138,0.00031075493,0.00007606566,0.000012159402,0.000007803145,0.0003704621,0.000027451462,0.000970799],"genre_scores_gemma":[0.9990958,0.00002920133,0.00025913925,0.000021090114,0.0000032305131,0.000010159828,0.00028688504,0.000009188711,0.00028526396],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998424,0.00006290681,0.000010250781,0.000034252273,0.000014224907,0.000035963367],"domain_scores_gemma":[0.9993943,0.00030713802,0.000055677996,0.000056957662,0.00008510284,0.00010086743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000573157,0.0006471854,0.00049760065,0.00030793648,0.0006163997,0.0013058753,0.00062732527,0.00081667234,0.0017944254],"category_scores_gemma":[0.0014277344,0.00044690567,0.00073375745,0.0002932629,0.0006398558,0.00067122636,0.0007414398,0.00064041244,0.00012724417],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003627793,0.00010997365,0.05253865,0.00003274693,0.00016605161,0.00017172571,0.000058978665,0.9418288,0.0020588103,0.00081457495,0.0004046386,0.0014523212],"study_design_scores_gemma":[0.00020456854,0.00017242669,0.014736185,0.000010913865,0.00006534906,0.000017019007,0.00006177355,0.98257875,0.0014875312,0.00027511327,0.0003691928,0.000021218606],"about_ca_topic_score_codex":0.10382057,"about_ca_topic_score_gemma":0.045634463,"teacher_disagreement_score":0.10382057,"about_ca_system_score_codex":0.001847621,"about_ca_system_score_gemma":0.001550596,"threshold_uncertainty_score":0.20643252},"labels":[],"label_agreement":null},{"id":"W2106112227","doi":"10.1029/2000gl012523","title":"Assessment of the effect of the Montreal Protocol on atmospheric ozone","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Montreal Protocol; Ozone; Environmental science; Southern Hemisphere; Northern Hemisphere; Stratosphere; Ozone layer; Atmospheric sciences; Atmosphere (unit); Ozone depletion; Atmospheric dynamics; Chlorine; Climatology; Meteorology; Chemistry; Geography; Geology","score_opus":0.01725387464590287,"score_gpt":0.3120101309530505,"score_spread":0.29475625630714763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106112227","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.52928793,0.005165058,0.058037244,0.015065281,0.00179928,0.011372065,0.055873662,0.0017919294,0.32160753],"genre_scores_gemma":[0.86342025,0.003135417,0.07458088,0.0022006044,0.00014566623,0.0058698906,0.02105442,0.00030035843,0.029292459],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9887656,0.0037099996,0.0002997359,0.00040072505,0.0061419695,0.0006819521],"domain_scores_gemma":[0.98431766,0.003959561,0.0010088661,0.001294486,0.008972927,0.0004463971],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.012687568,0.0009051778,0.0005032466,0.0019484811,0.0023213164,0.0021739781,0.0029717954,0.0015480923,0.004667118],"category_scores_gemma":[0.028509224,0.00046054838,0.0014140435,0.002488766,0.00079646497,0.0013712216,0.001312142,0.0012083,0.0006089987],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018487357,0.0007316213,0.09174347,0.0011390991,0.00100716,0.0007401515,0.00043976028,0.55750966,0.011522115,0.0832684,0.116136074,0.13391373],"study_design_scores_gemma":[0.0010464796,0.002653722,0.20813093,0.00065259804,0.0011715963,0.00021595233,0.00094201486,0.40184417,0.033507127,0.017971803,0.33111462,0.00074899616],"about_ca_topic_score_codex":0.61297715,"about_ca_topic_score_gemma":0.5099572,"teacher_disagreement_score":0.61297715,"about_ca_system_score_codex":0.011270466,"about_ca_system_score_gemma":0.018647892,"threshold_uncertainty_score":0.7786042},"labels":[],"label_agreement":null},{"id":"W2106524201","doi":"10.1002/2015gl063191","title":"Decadal changes in Gulf of Alaska upwelling source waters","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Fisheries and Oceans Canada; College of Computing; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Ocean gyre; Upwelling; Oceanography; Pacific decadal oscillation; Geology; Climatology; Sea surface temperature; Current (fluid); Ekman transport; Predictability; Marine ecosystem; Ecosystem; Environmental science; Subtropics","score_opus":0.04511316956757794,"score_gpt":0.27874718533148873,"score_spread":0.2336340157639108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2106524201","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967031,0.00017360458,0.00008427384,0.000049469563,0.000015907524,0.0000011611713,0.001640973,0.00001356044,0.0013179932],"genre_scores_gemma":[0.9983191,0.00010812782,0.00005776124,0.000009906419,0.0000049787436,0.0000020352131,0.0010142796,0.0000020949312,0.0004816075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999511,0.000005837679,0.00000593701,0.000020186113,0.000009688571,0.0000072661196],"domain_scores_gemma":[0.99970573,0.000038252467,0.000103195314,0.000023771823,0.000093788076,0.000035261102],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020136671,0.00012363201,0.000071892275,0.0007659007,0.00015971535,0.0004150957,0.000079718,0.00015039738,0.001158585],"category_scores_gemma":[0.00063670136,0.000060378734,0.00011392417,0.00059032516,0.00008232489,0.0002569229,0.0002842517,0.00018857131,0.000194414],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000068140864,0.000024512963,0.98524296,0.000018092574,0.00009931851,0.00008542258,0.00029965202,0.0014795318,0.0023545558,0.00017762688,0.00077180483,0.009378467],"study_design_scores_gemma":[9.353297e-7,0.000007577309,0.9980483,0.000006035894,0.00001012804,0.000025721522,0.00017343683,0.00059343566,0.00024696792,0.0000586936,0.00082562485,0.0000030914298],"about_ca_topic_score_codex":0.016222715,"about_ca_topic_score_gemma":0.02031869,"teacher_disagreement_score":0.016222715,"about_ca_system_score_codex":0.0002912623,"about_ca_system_score_gemma":0.00012383389,"threshold_uncertainty_score":0.032256603},"labels":[],"label_agreement":null},{"id":"W2107452779","doi":"10.1029/2008gl036945","title":"Keeling plots are non‐linear in non‐steady state diffusive environments","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Linearity; Mixing (physics); Statistical physics; Transfer function; Plot (graphics); Physics; Environmental science; Mathematics; Statistics","score_opus":0.014438550134692061,"score_gpt":0.26942563154196075,"score_spread":0.25498708140726867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107452779","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3939312,0.00041013653,0.58917964,0.00033189156,0.000037642025,0.00010907153,0.00063716766,0.002627421,0.012735797],"genre_scores_gemma":[0.96068496,0.00009813334,0.033465058,0.00007738822,0.000009045387,0.00006710972,0.00021711476,0.00024217623,0.005139094],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9991592,0.00017786828,0.000045601442,0.00028796768,0.00022125071,0.00010801507],"domain_scores_gemma":[0.99318683,0.0043701255,0.0009170836,0.0008184949,0.0005999037,0.000107558604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013222774,0.00049794244,0.00039674138,0.0007499769,0.00056037446,0.0015263065,0.0010501366,0.00085894193,0.0031973014],"category_scores_gemma":[0.011517167,0.00062063645,0.00050620246,0.0006606999,0.0012588792,0.002624587,0.0009238313,0.001380408,0.0009355708],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001446229,0.0003759407,0.10438415,0.0008288098,0.0002685673,0.0014295245,0.006901607,0.2984621,0.17482331,0.15641329,0.0075164884,0.24714999],"study_design_scores_gemma":[0.000059433747,0.00026184862,0.06347866,0.000084087784,0.00006289229,0.0009938534,0.0007889307,0.7297131,0.091333024,0.09565822,0.017279085,0.00028692643],"about_ca_topic_score_codex":0.0031179711,"about_ca_topic_score_gemma":0.0028673073,"teacher_disagreement_score":0.0031973014,"about_ca_system_score_codex":0.00069892773,"about_ca_system_score_gemma":0.00036321714,"threshold_uncertainty_score":0.0106960535},"labels":[],"label_agreement":null},{"id":"W2107939894","doi":"10.1029/2006gl028628","title":"Abrupt changes in rainfall during the twentieth century","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":139,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"James S. McDonnell Foundation","keywords":"Climatology; Climate change; Magnitude (astronomy); Environmental science; Precipitation; Geography; Geology; Meteorology; Oceanography","score_opus":0.033219468636162576,"score_gpt":0.3103222389908469,"score_spread":0.2771027703546843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2107939894","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99322927,0.0009934923,0.00041146416,0.0005066688,0.000026461605,0.000005518126,0.0014367442,0.000028392758,0.0033620652],"genre_scores_gemma":[0.99819034,0.00062589656,0.000109541535,0.000047213394,0.000029113942,0.0000027036162,0.00063344144,0.000004124858,0.00035759876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985766,0.000014096209,0.000012315562,0.000038341375,0.000036585767,0.000041047377],"domain_scores_gemma":[0.9996401,0.00006466735,0.00017361889,0.000024905416,0.00006131434,0.00003529728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026350172,0.00011813551,0.0001604188,0.00093306263,0.00032602617,0.00090187753,0.00015231685,0.00023809452,0.0013493192],"category_scores_gemma":[0.0014818445,0.000099509925,0.00012312284,0.0017149044,0.00043413712,0.000522022,0.0004913454,0.00030332486,0.0001371408],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014451073,0.000019671712,0.9404831,0.00009541652,0.00011501848,0.00051134557,0.00103425,0.009170607,0.0021096156,0.003927124,0.0021751376,0.040214147],"study_design_scores_gemma":[0.000005991589,0.000011016499,0.99165726,0.0000142671,0.000015732307,0.00010952216,0.00022749144,0.0013491662,0.00027222408,0.00049467187,0.0058332323,0.000009510248],"about_ca_topic_score_codex":0.015884694,"about_ca_topic_score_gemma":0.022667404,"teacher_disagreement_score":0.015884694,"about_ca_system_score_codex":0.00079661835,"about_ca_system_score_gemma":0.0002655205,"threshold_uncertainty_score":0.0315845},"labels":[],"label_agreement":null},{"id":"W2108119518","doi":"10.1002/2014gl060313","title":"Momentum balance of katabatic flow on steep slopes covered with short vegetation","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Katabatic wind; Atmospheric sciences; Wind speed; Terrain; Turbulence; Geology; Vegetation (pathology); Momentum (technical analysis); Environmental science; Jet (fluid); Flow (mathematics); Pressure gradient; Meteorology; Mechanics; Physics; Geography","score_opus":0.012637447719838647,"score_gpt":0.24603496615259993,"score_spread":0.23339751843276127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108119518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992993,0.000009660359,0.00033438875,0.000017972698,0.0000020438433,0.0000027198653,0.00004294404,0.000014184027,0.00027673357],"genre_scores_gemma":[0.9998184,0.000007861179,0.00005920214,0.0000015655164,0.0000010432287,0.0000017152496,0.000027969565,0.0000013050375,0.00008099817],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999691,0.000005641428,0.000002656788,0.000008661081,0.00000416272,0.000009761076],"domain_scores_gemma":[0.9998971,0.000033834254,0.000023422604,0.000006335468,0.00001562368,0.00002362692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009285673,0.0003040104,0.00026408295,0.00036343708,0.00043439274,0.0004948702,0.00030881347,0.00038561446,0.00099784],"category_scores_gemma":[0.00041233207,0.00018234749,0.00029736507,0.00025108215,0.0005889974,0.00033799617,0.00027592026,0.00025503585,0.00005882203],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053371856,0.00024741451,0.1275547,0.00006344968,0.00010511857,0.00072016875,0.00025468107,0.81815636,0.040950786,0.0036034337,0.00034447634,0.007465762],"study_design_scores_gemma":[0.00004288668,0.00007537039,0.0974251,0.000005592045,0.000018432705,0.000033269138,0.000061124,0.90084577,0.0009515234,0.00043224363,0.00008700847,0.000021632708],"about_ca_topic_score_codex":0.043695793,"about_ca_topic_score_gemma":0.016883027,"teacher_disagreement_score":0.043695793,"about_ca_system_score_codex":0.0007922559,"about_ca_system_score_gemma":0.0004097887,"threshold_uncertainty_score":0.08688295},"labels":[],"label_agreement":null},{"id":"W2108154709","doi":"10.1029/2008gl033884","title":"Chemical aging of ambient organic aerosol from heterogeneous reaction with hydroxyl radicals","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"","keywords":"Radical; Aerosol; Hydroxyl radical; Photochemistry; Environmental chemistry; Environmental science; Chemistry; Materials science; Organic chemistry","score_opus":0.023284819615013285,"score_gpt":0.24497189086923532,"score_spread":0.22168707125422205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108154709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982009,0.00042450178,0.00048532503,0.000007669058,0.000005386283,0.000010100282,0.00013546842,0.000007425681,0.0007232859],"genre_scores_gemma":[0.99876225,0.00025348557,0.00020253354,0.000010072095,0.000004607288,0.000005042441,0.00024197868,0.000002676491,0.0005174618],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989057,0.000006758454,0.0000033181568,0.000023803375,0.000045539437,0.00003001992],"domain_scores_gemma":[0.99993193,0.0000062071867,0.00001771311,0.0000059980052,0.000026818358,0.000011332283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000113903974,0.00027318147,0.00013108454,0.00028346333,0.00027769743,0.00030654922,0.00017466488,0.00016267947,0.0005070425],"category_scores_gemma":[0.00012770474,0.00009846153,0.00013739394,0.00017347696,0.00018550854,0.00015239559,0.0001744139,0.00012777685,0.00010135294],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010130824,0.000011624848,0.015702635,0.000039358325,0.00002445271,0.00013787438,0.00006430271,0.0001906315,0.9807052,0.000035359022,0.000053652886,0.0029335278],"study_design_scores_gemma":[0.000016843487,0.00030120075,0.4471216,0.000007016818,0.00007628873,0.0002144579,0.00018719985,0.0009275558,0.54837734,0.000077464676,0.0026818912,0.000011118775],"about_ca_topic_score_codex":0.019686254,"about_ca_topic_score_gemma":0.024708929,"teacher_disagreement_score":0.019686254,"about_ca_system_score_codex":0.0007076939,"about_ca_system_score_gemma":0.00021918547,"threshold_uncertainty_score":0.039143324},"labels":[],"label_agreement":null},{"id":"W2108631247","doi":"10.1029/2002gl015585","title":"Evidence of nonlinear dynamics in the eastward shift of the NAO","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"North Atlantic oscillation; Climatology; Geology; Forcing (mathematics); Diabatic; Index (typography); Nonlinear system; Oscillation (cell signaling); Atmospheric sciences; Physics","score_opus":0.06337923187543831,"score_gpt":0.32890794656986494,"score_spread":0.2655287146944266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2108631247","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99386215,0.00011629911,0.0018059553,0.0002889534,0.000007315985,0.000003848083,0.0001901072,0.000028837869,0.0036964768],"genre_scores_gemma":[0.99908614,0.00009228111,0.00038808509,0.000016564194,0.0000036214303,0.0000014869182,0.000094006464,0.0000054440534,0.0003124117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995327,0.0000088768065,0.000004327167,0.000015538846,0.000009919078,0.000008111651],"domain_scores_gemma":[0.99963343,0.00012052842,0.000086433116,0.00005821941,0.000068920475,0.000032528882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016798654,0.0001294711,0.00011998651,0.0001718289,0.00026398202,0.00041784224,0.00019797627,0.00023203946,0.0018845686],"category_scores_gemma":[0.0010692395,0.00019624157,0.00019634845,0.00029469433,0.000369093,0.0003850952,0.00046626793,0.00033369494,0.00025908634],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047730407,0.00009668718,0.8533136,0.00013666009,0.0001807202,0.0006053935,0.00085741456,0.05905357,0.05619097,0.009431107,0.0013284654,0.018328035],"study_design_scores_gemma":[0.000055250013,0.00006838576,0.81594306,0.000018508414,0.000052081585,0.000321141,0.00025597343,0.16965061,0.0058623445,0.0047749467,0.0029631103,0.00003459364],"about_ca_topic_score_codex":0.01005975,"about_ca_topic_score_gemma":0.009982642,"teacher_disagreement_score":0.01005975,"about_ca_system_score_codex":0.0002738864,"about_ca_system_score_gemma":0.00033252596,"threshold_uncertainty_score":0.020002365},"labels":[],"label_agreement":null},{"id":"W2109198545","doi":"10.1002/2014gl060814","title":"Explaining Jupiter's magnetic field and equatorial jet dynamics","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Dynamo; Jupiter (rocket family); Jovian; Physics; Dynamo theory; Jet (fluid); Magnetic field; Observable; Geophysics; Gas giant; Planet; Mercury's magnetic field; Astrophysics; Spacecraft; L-shell; Mechanics; Astronomy; Earth's magnetic field; Saturn","score_opus":0.014596526995801424,"score_gpt":0.2801924507354838,"score_spread":0.2655959237396824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109198545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885456,0.00010733097,0.0050291154,0.0004174493,0.000017206414,0.0000100908865,0.00012266375,0.00013292085,0.005617563],"genre_scores_gemma":[0.9992611,0.000039490205,0.00038786273,0.000013827997,0.000005639697,0.000002989345,0.000023687808,0.000011033265,0.00025448558],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997365,0.0000066508073,0.0000010063064,0.0000073002348,0.0000031922855,0.000008182115],"domain_scores_gemma":[0.999928,0.00001885378,0.000019405034,0.000008833438,0.0000074669583,0.000017352822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010474055,0.00026080065,0.00021447343,0.00018376179,0.0003033367,0.0007107984,0.00032159043,0.0004929587,0.0010572578],"category_scores_gemma":[0.0005550311,0.00016169653,0.00020591354,0.00013217313,0.0003834091,0.00048388203,0.00027052377,0.00024401772,0.00012494969],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008544645,0.000047390688,0.044735968,0.000027303007,0.000042012936,0.00036711863,0.00016767922,0.92951745,0.0088120075,0.011335206,0.0010627641,0.0037995803],"study_design_scores_gemma":[0.000033684257,0.00001655241,0.010822869,0.0000037667073,0.000007202327,0.00003760866,0.000035313762,0.9851916,0.00042536305,0.0029783375,0.00044166268,0.000005988389],"about_ca_topic_score_codex":0.0112850405,"about_ca_topic_score_gemma":0.0040474297,"teacher_disagreement_score":0.0112850405,"about_ca_system_score_codex":0.00071271625,"about_ca_system_score_gemma":0.00027555798,"threshold_uncertainty_score":0.022438705},"labels":[],"label_agreement":null},{"id":"W2109506574","doi":"10.1029/2001gl013298","title":"Impact of improved near infrared water vapor line data on absorption of solar radiation in GCMs","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"HITRAN; Water vapor; Absorption (acoustics); Environmental science; Infrared; Radiation; Materials science; Atmospheric sciences; Remote sensing; Absorption spectroscopy; Meteorology; Physics; Optics; Geology","score_opus":0.044699909905990175,"score_gpt":0.32204629729361894,"score_spread":0.2773463873876288,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109506574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9256817,0.0013085256,0.015934493,0.001859821,0.0002757935,0.000119774035,0.045915484,0.0051878067,0.003716538],"genre_scores_gemma":[0.9305768,0.00047779866,0.022065334,0.000503812,0.00011813023,0.000089113266,0.04476108,0.0005812472,0.0008267194],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9952839,0.001990859,0.0003052285,0.0009997053,0.0011730446,0.00024714877],"domain_scores_gemma":[0.98472506,0.0073667774,0.0012651891,0.003861037,0.002423805,0.00035810328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0071803317,0.0012193723,0.0012289837,0.0010749087,0.00051352725,0.0015356585,0.0020595717,0.0013272926,0.0019103469],"category_scores_gemma":[0.024579877,0.00070291664,0.0013808149,0.0024374234,0.00048641718,0.0034514663,0.0011077669,0.0013074358,0.00063353224],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021322374,0.00035735936,0.26500422,0.00062198786,0.0016945599,0.0002561975,0.00021218524,0.6221606,0.017887764,0.0023276282,0.014697128,0.07264816],"study_design_scores_gemma":[0.0008365943,0.00026017497,0.46283084,0.00017983901,0.0007319658,0.00015507512,0.00020475092,0.4676556,0.034494106,0.0018762429,0.030472543,0.00030216173],"about_ca_topic_score_codex":0.07396246,"about_ca_topic_score_gemma":0.05422373,"teacher_disagreement_score":0.07396246,"about_ca_system_score_codex":0.0019018123,"about_ca_system_score_gemma":0.001056479,"threshold_uncertainty_score":0.14706391},"labels":[],"label_agreement":null},{"id":"W2109758285","doi":"10.1029/2003gl018910","title":"Multiple equilibrium states and the abrupt transitions in a dynamical system of soil water interacting with vegetation","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Aeronautics and Space Administration","keywords":"Environmental science; Grassland; Biomass (ecology); Ecosystem; Vegetation (pathology); Water content; Arid; Precipitation; Atmospheric sciences; Temperate climate; Range (aeronautics); Hydrology (agriculture); Soil science; Ecology; Geology; Physics; Meteorology","score_opus":0.00863329768565744,"score_gpt":0.23651718260669752,"score_spread":0.2278838849210401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109758285","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89588946,0.00033313158,0.09779657,0.0008600418,0.000029045683,0.000024697109,0.00011001806,0.00021485139,0.004742184],"genre_scores_gemma":[0.99728453,0.00008113162,0.0020506745,0.000031119784,0.000014347114,0.000024004454,0.000031088726,0.000010282543,0.00047274178],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99967694,0.000109232686,0.000017490001,0.00006699444,0.00005227773,0.00007696804],"domain_scores_gemma":[0.99864346,0.0007322141,0.0003162174,0.000055738077,0.00005487823,0.0001974907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008163331,0.00033104658,0.0005328958,0.00070322544,0.0007116093,0.0010962788,0.0006615439,0.00083061866,0.0011541371],"category_scores_gemma":[0.0033071623,0.00040243057,0.00060826255,0.0003610718,0.0019819716,0.0020668919,0.0014796081,0.0009728456,0.00010685384],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022666185,0.00010209029,0.022508895,0.00010763363,0.0002375083,0.0015326495,0.0012433059,0.74267393,0.006164356,0.21192375,0.0013376175,0.0119416155],"study_design_scores_gemma":[0.000038096812,0.00004962037,0.003751396,0.000013296643,0.000025070638,0.00012747789,0.00017203795,0.8857776,0.00030856108,0.109041445,0.00065857754,0.000036749534],"about_ca_topic_score_codex":0.0024590855,"about_ca_topic_score_gemma":0.0017071645,"teacher_disagreement_score":0.0024590855,"about_ca_system_score_codex":0.00076115166,"about_ca_system_score_gemma":0.00039445018,"threshold_uncertainty_score":0.005522549},"labels":[],"label_agreement":null},{"id":"W2109772998","doi":"10.1002/2015gl066389","title":"Evaluation of Operation IceBridge quick‐look snow depth estimates on sea ice","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; York University; Environment and Climate Change Canada","funders":"Canadian Space Agency; Canada Research Chairs; Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Snow; Mean squared error; Environmental science; Remote sensing; Root mean square; Sea ice; Geology; Climatology; Geomorphology; Physics; Mathematics; Statistics","score_opus":0.09220862172972227,"score_gpt":0.34496916623640006,"score_spread":0.2527605445066778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109772998","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99762684,0.00003489238,0.0011896024,0.000030541014,0.000008536697,0.000010728125,0.00035991773,0.00006798222,0.0006710126],"genre_scores_gemma":[0.9964581,0.000022246113,0.002416181,0.000018697694,0.0000056543536,0.00000770046,0.0008151827,0.000011123094,0.00024507547],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995584,0.00010061026,0.00002307911,0.00006814432,0.00018479435,0.00006491632],"domain_scores_gemma":[0.9992142,0.00021710248,0.00015103171,0.00007990899,0.0002570545,0.00008066455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015685211,0.00037132544,0.00029087323,0.0007007175,0.0002618119,0.00065613986,0.0005034366,0.00030462173,0.00061193574],"category_scores_gemma":[0.002444826,0.00020019567,0.00022498026,0.00048377918,0.00023255796,0.0006606432,0.0006139694,0.00015950669,0.0001663946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020506817,0.00032824615,0.6542798,0.00014795015,0.00030909185,0.0003991075,0.0008299077,0.1584169,0.069424435,0.00033214266,0.0030455021,0.1104362],"study_design_scores_gemma":[0.00011603206,0.00052412867,0.7461519,0.000027894206,0.00005584572,0.00008878281,0.00045677376,0.234815,0.015904782,0.00012251303,0.0016866433,0.000049656282],"about_ca_topic_score_codex":0.030180212,"about_ca_topic_score_gemma":0.06278741,"teacher_disagreement_score":0.030180212,"about_ca_system_score_codex":0.00065247377,"about_ca_system_score_gemma":0.00050493213,"threshold_uncertainty_score":0.060009122},"labels":[],"label_agreement":null},{"id":"W2109960092","doi":"10.1002/2015gl064888","title":"Robust comparison of climate models with observations using blended land air and ocean sea surface temperatures","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":182,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Climate model; Environmental science; Climatology; Surface air temperature; Climate change; Temperature record; Atmospheric sciences; Sea surface temperature; Sea ice; Radiative forcing; Geology; Oceanography","score_opus":0.17386290493544315,"score_gpt":0.3376838915518274,"score_spread":0.16382098661638422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2109960092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9826785,0.00016262122,0.011484637,0.00026153921,0.000078395264,0.000042779757,0.0026000964,0.00078864885,0.0019028654],"genre_scores_gemma":[0.99499184,0.000026782645,0.002758431,0.000023971294,0.00001786874,0.000021593401,0.001983335,0.00007500277,0.000101230034],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99846673,0.0006994115,0.00011277137,0.00047593034,0.00013843655,0.00010683539],"domain_scores_gemma":[0.9958603,0.002050343,0.0005160754,0.0008816477,0.00052685116,0.00016482889],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.004504741,0.00075915636,0.0006997248,0.0006243144,0.00045439473,0.0017614648,0.001334061,0.00094746694,0.0011434006],"category_scores_gemma":[0.010884643,0.00060131476,0.001159608,0.0010184709,0.00043800886,0.0015107918,0.0010602676,0.00084802863,0.00043497907],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007195264,0.00022957553,0.09514355,0.0000669941,0.00089414493,0.00006233843,0.00008187976,0.8883178,0.0021867414,0.0009688802,0.0011830282,0.010145618],"study_design_scores_gemma":[0.00015739155,0.00008082143,0.040426593,0.000014986736,0.000090201356,0.000012638693,0.00005219105,0.9555636,0.0020808096,0.00076158845,0.00071880955,0.000040403414],"about_ca_topic_score_codex":0.03747333,"about_ca_topic_score_gemma":0.021601124,"teacher_disagreement_score":0.03747333,"about_ca_system_score_codex":0.0012637536,"about_ca_system_score_gemma":0.0010914053,"threshold_uncertainty_score":0.074510396},"labels":[],"label_agreement":null},{"id":"W2110010757","doi":"10.1029/2002gl015539","title":"Timing of magnetic reconnection initiation during a global magnetospheric substorm onset","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":117,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Substorm; Magnetic reconnection; Physics; Geophysics; Plasma sheet; Geostationary orbit; Field line; Magnetosphere; Astrophysics; Magnetic field; Satellite; Astronomy","score_opus":0.02782154960445778,"score_gpt":0.2767687116808803,"score_spread":0.2489471620764225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110010757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989592,0.000044950964,0.00014042135,0.000008011027,0.000001386974,0.0000038466883,0.00011271461,0.000013430001,0.000715998],"genre_scores_gemma":[0.99936765,0.000026392889,0.00012811125,0.000005504489,0.0000033409858,0.0000036984304,0.000319222,0.0000025848326,0.0001436036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.000005054389,0.0000020281332,0.000011762751,0.0000068292293,0.000016399039],"domain_scores_gemma":[0.99980694,0.000036277514,0.000071270166,0.000015888305,0.000030085388,0.000039600316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000086138214,0.00009071447,0.00016788582,0.00032907078,0.00017546612,0.00027581898,0.000083154926,0.00012979856,0.00083633413],"category_scores_gemma":[0.00033811334,0.000057510533,0.00006152539,0.00020129781,0.00014160984,0.00015181674,0.00025625576,0.00019068402,0.00011557994],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011500658,0.00008595226,0.7917691,0.000049313578,0.000068952446,0.00095302716,0.00081471493,0.0012541949,0.17491974,0.00044284028,0.0005496018,0.027942445],"study_design_scores_gemma":[0.000009944971,0.0001254621,0.99376774,0.0000045119623,0.000011111082,0.0002014506,0.000103274586,0.00044570482,0.00474706,0.000047466747,0.0005319607,0.0000043031114],"about_ca_topic_score_codex":0.0021642826,"about_ca_topic_score_gemma":0.0056646415,"teacher_disagreement_score":0.0021642826,"about_ca_system_score_codex":0.00017351023,"about_ca_system_score_gemma":0.000066111505,"threshold_uncertainty_score":0.0043033957},"labels":[],"label_agreement":null},{"id":"W2110082266","doi":"10.1029/2002gl015986","title":"Prolonged post‐seismic deformation of the 1960 great Chile earthquake and implications for mantle rheology","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Subduction; Mantle (geology); Deformation (meteorology); Slip (aerodynamics); Geophysics; Tectonics","score_opus":0.03909561833715969,"score_gpt":0.26922787059837233,"score_spread":0.23013225226121264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110082266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972964,0.0005580851,0.00006674676,0.00034293946,0.000005907091,0.0000020478083,0.00012400749,0.0000076141782,0.0015962188],"genre_scores_gemma":[0.9995478,0.0001605348,0.000016245212,0.000011936755,0.0000059675776,0.0000010677444,0.00003575084,0.0000016175946,0.00021917553],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.0000123816335,0.000006021404,0.000011970812,0.0000085425,0.000022861546],"domain_scores_gemma":[0.99974793,0.000055734414,0.000083888895,0.00003495996,0.00003329787,0.00004425063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021439372,0.00014211386,0.0001955227,0.0004225224,0.00026769456,0.0006117841,0.00023509031,0.00047829587,0.002278346],"category_scores_gemma":[0.0012333503,0.00015593358,0.0001864811,0.0005082301,0.0006508801,0.0007300242,0.00045888816,0.00021396914,0.00028057562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001005094,0.00010147285,0.8928744,0.000204963,0.000105122046,0.0043455022,0.001835654,0.016448973,0.047514774,0.0031382183,0.0012940799,0.031131713],"study_design_scores_gemma":[0.000011970447,0.000037399357,0.9953761,0.0000144374635,0.000007357385,0.00018152288,0.00055943243,0.0018744541,0.0005064007,0.0006862944,0.0007326406,0.00001196756],"about_ca_topic_score_codex":0.016288092,"about_ca_topic_score_gemma":0.013317527,"teacher_disagreement_score":0.016288092,"about_ca_system_score_codex":0.0010518167,"about_ca_system_score_gemma":0.00029078065,"threshold_uncertainty_score":0.0323866},"labels":[],"label_agreement":null},{"id":"W2110126423","doi":"10.1029/2008gl036338","title":"Distributions and seasonal variations of tropospheric ethene (C<sub>2</sub>H<sub>4</sub>) from Atmospheric Chemistry Experiment (ACE‐FTS) solar occultation spectra","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Occultation; Troposphere; Atmospheric sciences; Environmental science; Atmospheric chemistry; Latitude; Haze; Mixing ratio; Climatology; Geology; Meteorology; Ozone; Physics; Astrophysics; Geodesy","score_opus":0.012943440528909604,"score_gpt":0.25304551910916173,"score_spread":0.24010207858025212,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110126423","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99789375,0.00006070549,0.00017639378,0.000010333843,0.000002300628,0.0000017792513,0.0012298098,0.000025376938,0.00059967814],"genre_scores_gemma":[0.99671483,0.000080001395,0.00033483794,0.0000065791382,0.0000042053994,0.0000029165585,0.0024892988,0.000008937913,0.0003584137],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999709,0.0000020447042,0.000002071185,0.0000086641285,0.000008066373,0.000008201921],"domain_scores_gemma":[0.9998784,0.000022159025,0.00004083181,0.000008919443,0.00003034753,0.000019236972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006939758,0.00015699942,0.00008278354,0.00045483245,0.00011975344,0.00020805423,0.00010126745,0.00013508549,0.00092438556],"category_scores_gemma":[0.00015332815,0.000088988214,0.00009063112,0.00041728158,0.000089142704,0.00014993701,0.00011513751,0.00012396515,0.00013013427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059297995,0.00006603644,0.8152718,0.000071050556,0.00012498072,0.00033558786,0.00047378396,0.002067408,0.15241325,0.00010836292,0.0010721633,0.02740254],"study_design_scores_gemma":[0.0000012392736,0.0000104521705,0.99630237,0.0000010523439,0.0000068941545,0.000033196502,0.000020916394,0.00044094783,0.0028714032,0.0000060667576,0.00030304858,0.0000023893185],"about_ca_topic_score_codex":0.0077579594,"about_ca_topic_score_gemma":0.02492161,"teacher_disagreement_score":0.0077579594,"about_ca_system_score_codex":0.00016741647,"about_ca_system_score_gemma":0.00007136788,"threshold_uncertainty_score":0.015425622},"labels":[],"label_agreement":null},{"id":"W2110164758","doi":"10.1029/2006gl027081","title":"Observation of glacial isostatic adjustment in “stable” North America with GPS","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":362,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"U.S. Geological Survey","keywords":"Post-glacial rebound; Geology; Deglaciation; Glacial period; Geodesy; Subsidence; Shore; Tectonic uplift; Bay; Global Positioning System; Tide gauge; Geomorphology; Sea level; Oceanography; Seismology; Tectonics","score_opus":0.051542131517854646,"score_gpt":0.28163312479914465,"score_spread":0.23009099328129,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110164758","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977512,0.000047196405,0.00016103414,0.000026497439,0.0000028589052,0.000003639059,0.00069629966,0.000016321066,0.0012950159],"genre_scores_gemma":[0.99771297,0.000086517524,0.00045360593,0.000019107058,0.00000395056,0.000004868716,0.0013001984,0.000003003651,0.00041586137],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993455,0.000008017716,0.0000034040377,0.000015499394,0.000022467573,0.000016075435],"domain_scores_gemma":[0.9997553,0.000021877275,0.00006899201,0.000019033552,0.000083370316,0.000051306557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008227678,0.0000973654,0.00008209466,0.00064057455,0.00041696825,0.0002912648,0.00017033337,0.00011816964,0.00063552096],"category_scores_gemma":[0.00034044313,0.00012203858,0.000073280826,0.001122899,0.00029883668,0.00017310948,0.0002678498,0.00015918155,0.00012765483],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046694622,0.000022980972,0.9795202,0.000016357779,0.00003387527,0.00007700272,0.0010367488,0.00044183218,0.004918938,0.00019324763,0.0012726896,0.012419429],"study_design_scores_gemma":[0.0000015951779,0.0000075691432,0.9985447,0.0000016088425,0.00000323004,0.000017458866,0.00017735995,0.00018947473,0.000157085,0.000016933642,0.0008814087,0.0000015231924],"about_ca_topic_score_codex":0.22121696,"about_ca_topic_score_gemma":0.50065553,"teacher_disagreement_score":0.778783,"about_ca_system_score_codex":0.0006341221,"about_ca_system_score_gemma":0.00048786617,"threshold_uncertainty_score":0.43985868},"labels":[],"label_agreement":null},{"id":"W2110246618","doi":"10.1029/2012gl054328","title":"Seismic anisotropy of subducting oceanic uppermost mantle from fossil spreading","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Geology; Subduction; Mantle (geology); Seismic anisotropy; Anisotropy; Slab; Seismology; Geophysics; Receiver function; Shear wave splitting; Mantle wedge; Lithosphere; Tectonics","score_opus":0.037958787889965845,"score_gpt":0.285744309520322,"score_spread":0.24778552163035614,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110246618","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995414,0.000017242044,0.000092236034,0.0000049598398,1.7446666e-7,4.0927847e-7,0.00006156362,0.000010358124,0.00027166563],"genre_scores_gemma":[0.999676,0.000017502232,0.00009097413,8.9447786e-7,3.5703698e-7,3.7881367e-7,0.00014323929,0.000003550413,0.00006724114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999652,0.0000043869745,0.0000021294532,0.000008744732,0.000008862067,0.0000106698535],"domain_scores_gemma":[0.99989223,0.000021735497,0.000033468496,0.000014433165,0.000024744768,0.000013269878],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010666255,0.00022872553,0.0001008473,0.0006010311,0.00012463673,0.00030404577,0.00013686711,0.00009895937,0.00071437145],"category_scores_gemma":[0.00038835272,0.00014763954,0.00013078464,0.0004996191,0.0001936152,0.00011071945,0.00024324606,0.00011425086,0.00011382189],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032372007,0.000032324115,0.6218581,0.00006729328,0.000095697964,0.0003058767,0.00066772115,0.013576431,0.34266865,0.00037262496,0.00013441705,0.019897105],"study_design_scores_gemma":[0.0000048624242,0.000013078086,0.9828315,0.0000039790775,0.000018976998,0.00006644134,0.0000900239,0.008831566,0.007930449,0.00004258365,0.00016130386,0.000005252728],"about_ca_topic_score_codex":0.018473288,"about_ca_topic_score_gemma":0.018752057,"teacher_disagreement_score":0.018473288,"about_ca_system_score_codex":0.00033376302,"about_ca_system_score_gemma":0.00017246758,"threshold_uncertainty_score":0.03673154},"labels":[],"label_agreement":null},{"id":"W2110331018","doi":"10.1029/2006gl028170","title":"Hotspots of deep ocean mixing on the Oregon continental slope","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Geology; Turbulence; Barotropic fluid; Continental shelf; Turbulence kinetic energy; Bathymetry; Stratification (seeds); Oceanography; Ridge; Internal tide; Geophysics; Meteorology; Internal wave; Physics; Paleontology","score_opus":0.022943886489545963,"score_gpt":0.2664748147914893,"score_spread":0.24353092830194337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110331018","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994247,0.000014091745,0.00001929575,0.00000759271,5.242348e-7,0.0000012079896,0.0000638758,0.0000043692426,0.00046440828],"genre_scores_gemma":[0.9996464,0.000024148057,0.000039519415,0.000003625542,0.000001476325,0.0000016321756,0.000117016585,0.0000015115468,0.00016473758],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999409,0.0000035944568,0.0000043656246,0.000017832186,0.000015966263,0.000017355413],"domain_scores_gemma":[0.9998192,0.000015639278,0.00008370915,0.000012169328,0.000021808282,0.00004755496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000623057,0.0001160928,0.00014135864,0.0010567714,0.0005253607,0.00070832885,0.00013396755,0.00017794083,0.00090547674],"category_scores_gemma":[0.00018226473,0.00015031823,0.00012800783,0.0007486331,0.0003249776,0.00021892691,0.0006249127,0.00015476336,0.00008659093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001263274,0.00002639067,0.97369283,0.000013094265,0.000032492917,0.00031535368,0.00047102597,0.00018690326,0.019804338,0.00010461241,0.00011271037,0.0051138485],"study_design_scores_gemma":[0.0000025341762,0.000010855638,0.99851173,0.0000045113675,0.000006849452,0.000091810594,0.00034790376,0.00016571343,0.00062700454,0.000024971216,0.00020308785,0.0000030770664],"about_ca_topic_score_codex":0.014697334,"about_ca_topic_score_gemma":0.044121314,"teacher_disagreement_score":0.014697334,"about_ca_system_score_codex":0.00039791138,"about_ca_system_score_gemma":0.0001970217,"threshold_uncertainty_score":0.029223561},"labels":[],"label_agreement":null},{"id":"W2110413095","doi":"10.1002/2015gl063769","title":"GRACE gravity observations constrain Weichselian ice thickness in the Barents Sea","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Norges Forskningsråd","keywords":"Geology; Ice sheet; Cryosphere; Antarctic sea ice; Post-glacial rebound; Sea ice; Climatology; Arctic ice pack; Drift ice; Ice divide; Antarctic ice sheet; Ice stream; Ice-sheet model; Future sea level; Oceanography","score_opus":0.15236451751296706,"score_gpt":0.32557753321466576,"score_spread":0.1732130157016987,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2110413095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978764,0.000046857822,0.00017834932,0.000014590796,0.0000045906722,0.0000021064764,0.00094684254,0.00002940989,0.0009007296],"genre_scores_gemma":[0.99811554,0.00003380123,0.00021203316,0.000004317571,0.0000053134945,0.0000022997858,0.0014999384,0.000008762251,0.00011802605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999866,0.000018260766,0.000010332507,0.000042507952,0.00003372345,0.000029102916],"domain_scores_gemma":[0.99962866,0.000057644498,0.000085506006,0.000056402198,0.00009574375,0.00007606861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034110653,0.00042498426,0.00023416484,0.000981035,0.00026653227,0.0006600932,0.00021975611,0.00021669111,0.0006391677],"category_scores_gemma":[0.0008629893,0.00012972073,0.00029292426,0.0005892807,0.00028830528,0.00045233508,0.00043595023,0.00015881738,0.00037250362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020729385,0.000062541076,0.967649,0.000010490488,0.00010095076,0.00015354638,0.00017959643,0.011327708,0.0057773762,0.00014659394,0.0007537724,0.0136311045],"study_design_scores_gemma":[0.000014689458,0.000026120397,0.98917705,0.0000082227225,0.000017518918,0.00001808439,0.00013804967,0.008965496,0.00080172665,0.000103489016,0.00072037516,0.000009130639],"about_ca_topic_score_codex":0.044882815,"about_ca_topic_score_gemma":0.08685411,"teacher_disagreement_score":0.044882815,"about_ca_system_score_codex":0.0004146494,"about_ca_system_score_gemma":0.00041297762,"threshold_uncertainty_score":0.089243114},"labels":[],"label_agreement":null},{"id":"W2111002935","doi":"10.1002/grl.50374","title":"Thermal structure and megathrust seismogenic potential of the Makran subduction zone","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Subduction; Geology; Seismology; Induced seismicity; Episodic tremor and slip; Tsunami earthquake; Tectonics","score_opus":0.01643012888993572,"score_gpt":0.23551273789956395,"score_spread":0.21908260900962823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111002935","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991026,0.00002181898,0.00014463646,0.000018410485,8.1088444e-7,0.0000016701174,0.000029169662,0.000005905454,0.0006750353],"genre_scores_gemma":[0.99985504,0.000012536116,0.00004946847,0.0000018782963,7.7363285e-7,0.0000013268618,0.00002168467,9.875363e-7,0.000056367808],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995685,0.000008155771,0.0000033403485,0.000010537355,0.0000052012374,0.000015830728],"domain_scores_gemma":[0.9998529,0.000028712557,0.00005780961,0.000014772714,0.000022670458,0.00002313098],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007831569,0.000244058,0.00012795217,0.00039177836,0.00028455674,0.0006431598,0.00035425596,0.00031549466,0.00094078964],"category_scores_gemma":[0.00044627962,0.00023587231,0.00023897491,0.0002458458,0.00031536323,0.00032391355,0.00045225376,0.00021116978,0.00013656818],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043065092,0.00009105709,0.58744264,0.00007395741,0.00011338303,0.001124677,0.00069550175,0.37628204,0.022259424,0.0033348128,0.0003070488,0.007844712],"study_design_scores_gemma":[0.00006205685,0.00013808797,0.5603954,0.000028661034,0.00005017433,0.00028270195,0.00064713333,0.43439877,0.001925965,0.0013978466,0.0006221539,0.000051120714],"about_ca_topic_score_codex":0.012689162,"about_ca_topic_score_gemma":0.010799314,"teacher_disagreement_score":0.012689162,"about_ca_system_score_codex":0.0007697098,"about_ca_system_score_gemma":0.00025721308,"threshold_uncertainty_score":0.025230646},"labels":[],"label_agreement":null},{"id":"W2111009690","doi":"10.1029/2009gl041847","title":"Carbonate compensation dynamics","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; University of Hawai'i","keywords":"Carbonate; Dissolution; Ocean acidification; Seawater; Sediment–water interface; Saturation (graph theory); Aragonite; Sediment; Geology; Ion; Mineralogy; Oceanography; Environmental chemistry; Chemistry; Physical chemistry; Geomorphology; Organic chemistry","score_opus":0.02328055602567726,"score_gpt":0.2866244817144031,"score_spread":0.26334392568872583,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111009690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9488063,0.0011053557,0.025862155,0.0005475311,0.000061355066,0.000039618186,0.0011968164,0.00041449303,0.02196652],"genre_scores_gemma":[0.9978538,0.00012860315,0.00062735524,0.000022812414,0.0000027736983,0.0000060251314,0.00011947506,0.000012534348,0.0012266653],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999286,0.0000034590346,0.0000037059306,0.000024267089,0.000018152516,0.000021822381],"domain_scores_gemma":[0.9998355,0.000029307655,0.00003919386,0.000009749688,0.000053283216,0.00003293273],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001250287,0.00025992535,0.00016963268,0.00029262446,0.00025704125,0.00054927735,0.0003751751,0.0003750914,0.003373448],"category_scores_gemma":[0.0006682497,0.00023595935,0.00024998837,0.00025752865,0.00027651753,0.00073090306,0.00053986796,0.00028010868,0.00025072045],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006014668,0.00006574431,0.14340858,0.00050071545,0.00016225509,0.00051990553,0.0005517607,0.12309736,0.5318175,0.09451044,0.004353736,0.100410685],"study_design_scores_gemma":[0.00009957527,0.00034322572,0.2878612,0.000042633063,0.0001276995,0.00069423486,0.00065741496,0.49434152,0.14788452,0.031403124,0.036378358,0.00016641118],"about_ca_topic_score_codex":0.009954124,"about_ca_topic_score_gemma":0.007900056,"teacher_disagreement_score":0.009954124,"about_ca_system_score_codex":0.0012274332,"about_ca_system_score_gemma":0.0006019802,"threshold_uncertainty_score":0.019792378},"labels":[],"label_agreement":null},{"id":"W2111350510","doi":"10.1029/2009gl041677","title":"Contribution of land surface initialization to subseasonal forecast skill: First results from a multi‐model experiment","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":452,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Guelph","funders":"","keywords":"Initialization; Forecast skill; Climatology; Precipitation; Anomaly (physics); Environmental science; Meteorology; Atmosphere (unit); Quantitative precipitation forecast; Magnitude (astronomy); Atmospheric sciences; Geology; Computer science; Geography; Physics","score_opus":0.05056631768639262,"score_gpt":0.3288887279731577,"score_spread":0.2783224102867651,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111350510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981108,0.000034559962,0.0007606085,0.0000662385,0.000009094919,0.000016736349,0.0004860602,0.0000495203,0.00046643228],"genre_scores_gemma":[0.99815863,0.000015510188,0.00072858314,0.000021009433,0.000007047689,0.00001648433,0.0008598007,0.000020263198,0.00017267451],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99950063,0.00019625093,0.000044958306,0.00010223699,0.000089626,0.000066347246],"domain_scores_gemma":[0.9942333,0.0034967798,0.00035614212,0.0009652897,0.0004599438,0.00048848346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028975978,0.00048087168,0.0004262534,0.00022600556,0.00033631639,0.0007047921,0.0003630214,0.0005684182,0.00061881926],"category_scores_gemma":[0.007647314,0.0002241123,0.0004989274,0.00022880884,0.00042655866,0.00082038343,0.0007545089,0.0009199095,0.0001143422],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.013187811,0.0023294396,0.36205354,0.00016696552,0.0011755488,0.00023619612,0.0006997062,0.5098673,0.062095057,0.0021065166,0.0038964725,0.04218547],"study_design_scores_gemma":[0.0009512912,0.003561636,0.3378864,0.000018931154,0.00026744237,0.000070419985,0.00020014582,0.61914194,0.03394014,0.0018773596,0.0019698169,0.00011447605],"about_ca_topic_score_codex":0.011871458,"about_ca_topic_score_gemma":0.010911937,"teacher_disagreement_score":0.011871458,"about_ca_system_score_codex":0.00046320102,"about_ca_system_score_gemma":0.0004201845,"threshold_uncertainty_score":0.023604691},"labels":[],"label_agreement":null},{"id":"W2111721033","doi":"10.1029/2010gl043975","title":"Efficient formation of stratospheric aerosol for climate engineering by emission of condensible vapor from aircraft","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":163,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Dalhousie University","funders":"","keywords":"Atmospheric sciences; Aerosol; Environmental science; Astrobiology; Water vapor; Stratosphere; Meteorology; Climate change; Atmospheric chemistry; Climatology; Physics; Geology; Ozone","score_opus":0.02021106915666623,"score_gpt":0.27346543106992477,"score_spread":0.25325436191325856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111721033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95123976,0.0013672876,0.043408595,0.00014376623,0.000041915755,0.000056307024,0.00008298544,0.00024486732,0.0034144511],"genre_scores_gemma":[0.97621745,0.00047964338,0.02196964,0.000026660211,0.000015623125,0.000020968791,0.00005513676,0.000029608545,0.0011854141],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992454,0.00001809104,0.0000026941088,0.000011654005,0.000025880161,0.000017108792],"domain_scores_gemma":[0.9999399,0.000016090613,0.000014137692,0.0000118870585,0.0000069269513,0.000010983796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019766617,0.00025391564,0.0001956926,0.00018964597,0.00019768332,0.00029094284,0.00015121876,0.0001854302,0.00081875664],"category_scores_gemma":[0.00012035226,0.00012660332,0.00025202762,0.00008539275,0.00026110615,0.00021990515,0.00032481682,0.00023320144,0.0001309586],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054602137,0.000030059558,0.0011225225,0.000034781024,0.000009245694,0.000037311776,0.000016700393,0.0013597051,0.9904613,0.0006435616,0.000044699602,0.0061856047],"study_design_scores_gemma":[0.00002917262,0.00024310785,0.003989039,0.000002989305,0.000016912696,0.000058684385,0.000022131599,0.010358682,0.9825379,0.00033955713,0.0023930126,0.000008853101],"about_ca_topic_score_codex":0.0008909103,"about_ca_topic_score_gemma":0.0023283805,"teacher_disagreement_score":0.0008909103,"about_ca_system_score_codex":0.00022622655,"about_ca_system_score_gemma":0.00020716483,"threshold_uncertainty_score":0.0027390122},"labels":[],"label_agreement":null},{"id":"W2111880928","doi":"10.1029/2002gl015192","title":"Basal temperature evolution of North American ice sheets and implications for the 100‐kyr cycle","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Ice sheet; Deglaciation; Geology; Ice stream; Ice-sheet model; Glacial period; Last Glacial Maximum; Climatology; Antarctic ice sheet; Oceanography; Physical geography; Geomorphology; Sea ice; Cryosphere; Geography","score_opus":0.030458483047772312,"score_gpt":0.29323765138525926,"score_spread":0.26277916833748693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111880928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99687505,0.000058377893,0.00034559815,0.00014531096,0.0000059055415,0.000004215874,0.00035357673,0.00004118306,0.0021708356],"genre_scores_gemma":[0.99928856,0.00005309266,0.00018473777,0.00002379492,0.0000018822534,0.0000064093388,0.00021958708,0.000013602048,0.00020836573],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993026,0.000023319317,0.0000036957967,0.000017040938,0.000008871575,0.000016808854],"domain_scores_gemma":[0.9998379,0.000049962215,0.000026522817,0.000021674456,0.000032484564,0.000031317002],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028859655,0.00026147286,0.00025814568,0.00029941674,0.0005327714,0.0008739529,0.00041660946,0.00058990304,0.0016362531],"category_scores_gemma":[0.00093835517,0.0002973557,0.0005033034,0.00039768557,0.00050974044,0.00044411188,0.00033843453,0.00035703392,0.00016657446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000098405304,0.000068184425,0.12126128,0.000024114728,0.00009152111,0.00009542509,0.000118515876,0.87097603,0.0020182736,0.0014078598,0.00063568336,0.0032047066],"study_design_scores_gemma":[0.000100281664,0.000051939336,0.12672757,0.000017599872,0.000057895893,0.000045062847,0.00021063756,0.8690252,0.0008289258,0.001687961,0.0012167438,0.000030250703],"about_ca_topic_score_codex":0.088616505,"about_ca_topic_score_gemma":0.056139003,"teacher_disagreement_score":0.088616505,"about_ca_system_score_codex":0.0013669281,"about_ca_system_score_gemma":0.0007844701,"threshold_uncertainty_score":0.17620134},"labels":[],"label_agreement":null},{"id":"W2111951664","doi":"10.1029/1999gl011212","title":"Atmospheric vortex streets on a RADARSAT SAR image","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Vortex; Synthetic aperture radar; Radiosonde; Satellite; Geology; Meteorology; Atmosphere (unit); Remote sensing; Geodesy; Physics; Astronomy","score_opus":0.023126282038086084,"score_gpt":0.28081528219290147,"score_spread":0.2576890001548154,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2111951664","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980252,0.000027452284,0.00041645652,0.0000074877503,0.000004239974,0.0000036411104,0.00023888737,0.000022696384,0.0012540286],"genre_scores_gemma":[0.9974865,0.000040750798,0.0011736734,0.0000051631264,0.000009122924,0.0000023801656,0.0008670655,0.0000065144277,0.0004088235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.0000028168054,0.0000015020597,0.000007504929,0.000011115158,0.000016067952],"domain_scores_gemma":[0.9999223,0.000012813999,0.000021885706,0.000007349883,0.000020972622,0.000014614716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000062915235,0.00010583338,0.00007636768,0.00070120377,0.00011837108,0.00021940397,0.000046861536,0.000119533695,0.0006943118],"category_scores_gemma":[0.00016212632,0.000055270084,0.000106782536,0.00041985538,0.00011159072,0.000117134834,0.000113907554,0.00009459891,0.00012097808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010986672,0.00022559929,0.5666152,0.00012367741,0.00016046525,0.0023327535,0.00096569734,0.041636717,0.2494109,0.0018646908,0.0044291136,0.13113652],"study_design_scores_gemma":[0.00001019908,0.00008768982,0.9644089,0.000012270942,0.000024824769,0.00026680008,0.0002232385,0.025484648,0.007175193,0.00013092761,0.0021664377,0.00000879681],"about_ca_topic_score_codex":0.0035084297,"about_ca_topic_score_gemma":0.005664048,"teacher_disagreement_score":0.0035084297,"about_ca_system_score_codex":0.000119683675,"about_ca_system_score_gemma":0.00009030131,"threshold_uncertainty_score":0.0069760084},"labels":[],"label_agreement":null},{"id":"W2112431801","doi":"10.1029/2003gl018587","title":"Widespread persistent near‐surface ozone depletion at northern high latitudes in spring","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ozone depletion; Latitude; Atmospheric sciences; Ozone; Troposphere; Environmental science; Snow; Climatology; Aerosol; Middle latitudes; Stratosphere; Geology; Meteorology; Geography","score_opus":0.02840273817342021,"score_gpt":0.2543241416149281,"score_spread":0.2259214034415079,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112431801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99898344,0.000030482292,0.0002847402,0.000014829795,0.0000017110866,0.0000018700307,0.00016091965,0.00004147984,0.00048048905],"genre_scores_gemma":[0.99924695,0.000029185256,0.0001727339,0.000004844747,8.7047687e-7,0.0000019992092,0.00025945719,0.0000032057326,0.00028083508],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997044,0.0000038060844,0.0000012331967,0.000010157867,0.00000597582,0.00000841034],"domain_scores_gemma":[0.99994946,0.000008671018,0.000013613613,0.000007222121,0.000005683556,0.00001532048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009402495,0.000163171,0.00018724476,0.00007716553,0.00024405241,0.00030667023,0.00015633227,0.00017875129,0.00086830114],"category_scores_gemma":[0.00015513347,0.00015037443,0.00020046481,0.00011120363,0.0001486144,0.00014694153,0.00012793594,0.00012626189,0.00015646768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006518287,0.00021310667,0.75894934,0.00012508793,0.0001404632,0.0005860819,0.00062310824,0.07915957,0.14083983,0.0005436392,0.0014667329,0.016701147],"study_design_scores_gemma":[0.00004742192,0.00017061399,0.9306766,0.0000060573752,0.00003416233,0.000113424634,0.00019913269,0.061572313,0.005813814,0.00024611896,0.0011075316,0.000012708124],"about_ca_topic_score_codex":0.06487044,"about_ca_topic_score_gemma":0.094412655,"teacher_disagreement_score":0.06487044,"about_ca_system_score_codex":0.0005188999,"about_ca_system_score_gemma":0.0003139042,"threshold_uncertainty_score":0.1289857},"labels":[],"label_agreement":null},{"id":"W2112744568","doi":"10.1029/2002gl016401","title":"Stratospheric ozone profiles retrieved from limb scattered sunlight radiance spectra measured by the OSIRIS instrument on the Odin satellite","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; University of Saskatchewan; University of Toronto; York University","funders":"","keywords":"Radiance; Osiris; Satellite; Environmental science; Stratosphere; Remote sensing; Ozone layer; Ozone; Radiative transfer; Sunlight; Atmospheric sciences; Meteorology; Physics; Geology; Optics; Astronomy","score_opus":0.0430088028729706,"score_gpt":0.25423684341761293,"score_spread":0.21122804054464234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112744568","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946149,0.000043530177,0.0010442925,0.000011234033,0.0000032005516,0.00001592484,0.0026040496,0.000072784846,0.001590122],"genre_scores_gemma":[0.98973185,0.000088837674,0.0027899363,0.0000115081575,0.0000020281748,0.000013588171,0.0063766153,0.000017969634,0.0009676804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.0000039483007,0.0000023038667,0.000007993116,0.000014013379,0.0000106788475],"domain_scores_gemma":[0.99995625,0.000004286526,0.000011523717,0.000005589223,0.0000150146325,0.0000072377534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008015165,0.00017643801,0.00016639428,0.00033833436,0.000268216,0.00022297692,0.00012081645,0.00014020498,0.0011057409],"category_scores_gemma":[0.00017378078,0.0001043631,0.00009736568,0.0004042814,0.00007598464,0.00015036209,0.00018815984,0.00014354853,0.00021709832],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086052786,0.00025611697,0.6595928,0.00024074424,0.00021561494,0.00029204827,0.0007515502,0.024078032,0.22359204,0.0009322738,0.0036227487,0.08556555],"study_design_scores_gemma":[0.000037369187,0.00007974397,0.96629655,0.000011754209,0.000027438278,0.00007322508,0.00023486881,0.012769371,0.017041562,0.00016488406,0.003249715,0.00001355162],"about_ca_topic_score_codex":0.017137118,"about_ca_topic_score_gemma":0.040303852,"teacher_disagreement_score":0.017137118,"about_ca_system_score_codex":0.00024332007,"about_ca_system_score_gemma":0.0003089793,"threshold_uncertainty_score":0.034074724},"labels":[],"label_agreement":null},{"id":"W2112779016","doi":"10.1029/2002gl015847","title":"The role of the Beaufort Gyre in Arctic climate variability: Seasonal to decadal climate scales","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":335,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Ocean gyre; Anticyclone; Arctic; Climatology; Anomaly (physics); Oceanography; Environmental science; Beaufort sea; The arctic; Climate change; Beaufort scale; Geology; Subtropics; Fishery","score_opus":0.014948921934194167,"score_gpt":0.25148894935874416,"score_spread":0.23654002742455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112779016","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98895454,0.0022992892,0.001361024,0.000653505,0.000041511623,0.000002899497,0.00014880464,0.000025545536,0.006512901],"genre_scores_gemma":[0.99921834,0.00029971355,0.00020520034,0.000028478204,0.00003500027,8.380025e-7,0.000035628967,0.0000028378904,0.0001739335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994135,0.000015293526,0.000002746249,0.000017230414,0.00000885172,0.000014559904],"domain_scores_gemma":[0.99956685,0.00010532748,0.00017717869,0.00003270058,0.00005640581,0.000061562954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003385599,0.00012012685,0.000105750165,0.0003086663,0.00039217187,0.0009100305,0.00014899482,0.00016527523,0.0006611944],"category_scores_gemma":[0.00086187903,0.00006586119,0.0000854707,0.00030991124,0.000445309,0.00054300623,0.00026523485,0.00013835721,0.00007055034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003021967,0.00002712424,0.9283789,0.00005524908,0.000116924384,0.00020792743,0.0010936544,0.0042551137,0.010717482,0.007509594,0.0011507778,0.04618504],"study_design_scores_gemma":[0.000002010848,0.000018651255,0.99481875,0.000006226861,0.000014107131,0.000047287664,0.00015286978,0.0014949085,0.00023042464,0.0012252528,0.0019845034,0.0000050071467],"about_ca_topic_score_codex":0.014623804,"about_ca_topic_score_gemma":0.023670763,"teacher_disagreement_score":0.014623804,"about_ca_system_score_codex":0.00033766718,"about_ca_system_score_gemma":0.0001827208,"threshold_uncertainty_score":0.029077351},"labels":[],"label_agreement":null},{"id":"W2112825532","doi":"10.1002/2014gl060301","title":"Day‐night coupling by a localized flow channel visualized by polar cap patch propagation","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Calgary","funders":"Natural Environment Research Council; Applied Physics Laboratory, Johns Hopkins University; National Aeronautics and Space Administration; Norges Forskningsråd; Sight Research UK; Science and Technology Facilities Council; Johns Hopkins University; Air Force Research Laboratory; National Science Foundation","keywords":"Polar; Physics; Geophysics; Polar cap; Ionosphere; Plasma sheet; Substorm; Defense Meteorological Satellite Program; Atmospheric sciences; Plasma; Magnetosphere; Astronomy","score_opus":0.010440034765333037,"score_gpt":0.28290396049071626,"score_spread":0.2724639257253832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112825532","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99622416,0.000083821615,0.0011202049,0.000031082338,0.000014192285,0.000008603073,0.00028303723,0.000076701916,0.002158117],"genre_scores_gemma":[0.9989309,0.000035368266,0.00064372976,0.000010851519,0.000014134192,0.000004617167,0.00018313216,0.000008418159,0.00016871213],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997044,0.0000022698578,7.046782e-7,0.000009529146,0.000004790875,0.000012331232],"domain_scores_gemma":[0.99992085,0.000013042262,0.000021487169,0.00001012844,0.000010766719,0.000023815655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004176312,0.00009237056,0.00012129031,0.00036297878,0.0002013892,0.00029711513,0.00014112335,0.00015431245,0.000980329],"category_scores_gemma":[0.00011976268,0.000095659154,0.00008002365,0.00024214578,0.000162912,0.00016755382,0.00021152788,0.0002494831,0.000118735654],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011973376,0.00018437124,0.40931782,0.00009811849,0.000119887336,0.002184902,0.00097163673,0.004244172,0.5243258,0.0016082089,0.004394844,0.05135294],"study_design_scores_gemma":[0.000030253525,0.000087159286,0.9763204,0.000008264672,0.000023620461,0.00047228805,0.00020766657,0.009296938,0.01096144,0.00035091577,0.002223239,0.000017907143],"about_ca_topic_score_codex":0.0028212806,"about_ca_topic_score_gemma":0.0036830136,"teacher_disagreement_score":0.0028212806,"about_ca_system_score_codex":0.00010215051,"about_ca_system_score_gemma":0.00011137683,"threshold_uncertainty_score":0.005609691},"labels":[],"label_agreement":null},{"id":"W2112895954","doi":"10.1029/2005gl022386","title":"Atmospheric Chemistry Experiment (ACE): Mission overview","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":1186,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Research Manitoba; Canadian Space Agency; York University; Université Laval; University of Saskatchewan; ABB (Canada); Environment and Climate Change Canada; Emka Technologies (Canada); University of Toronto; Western University; Trent University; University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; National Aeronautics and Space Administration","keywords":"Occultation; Satellite; Remote sensing; Spectral resolution; Atmosphere (unit); Atmospheric chemistry; Altitude (triangle); Spectrometer; Environmental science; Mixing ratio; Physics; Atmospheric pressure; Meteorology; Geology; Atmospheric sciences; Optics; Spectral line; Ozone; Astronomy","score_opus":0.038673083792388555,"score_gpt":0.31485027078012223,"score_spread":0.2761771869877337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112895954","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.089121304,0.06119934,0.04064102,0.0055048508,0.0011141116,0.010419402,0.64443696,0.013194946,0.13436817],"genre_scores_gemma":[0.12384417,0.024151558,0.1302753,0.0015457582,0.0015213436,0.0037288442,0.69933444,0.0012215237,0.014377146],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99935704,0.00007242732,0.000041171177,0.000114019815,0.00031763886,0.00009762989],"domain_scores_gemma":[0.9987476,0.000047721856,0.000112377886,0.00013428519,0.0007352028,0.0002227951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023752046,0.0011816933,0.00058290083,0.00296021,0.0008471459,0.0013211985,0.0010441282,0.0008482282,0.0031402095],"category_scores_gemma":[0.00089307624,0.0003462442,0.0004457554,0.004310812,0.00015124487,0.0015795308,0.0010671599,0.00076331996,0.0026424006],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002304794,0.0010452968,0.06064384,0.0038362588,0.0006324689,0.00031615287,0.00022115084,0.015216427,0.032678187,0.004606945,0.4945591,0.3839394],"study_design_scores_gemma":[0.00047534314,0.0003239925,0.08040543,0.00019144676,0.00019902871,0.00020567584,0.00010489277,0.005621656,0.008593418,0.0012574468,0.9025188,0.0001029459],"about_ca_topic_score_codex":0.041220386,"about_ca_topic_score_gemma":0.03301114,"teacher_disagreement_score":0.041220386,"about_ca_system_score_codex":0.0010456353,"about_ca_system_score_gemma":0.0038062532,"threshold_uncertainty_score":0.08196092},"labels":[],"label_agreement":null},{"id":"W2112995327","doi":"10.1029/2006gl026232","title":"The diffusive ocean conveyor","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Langara College; University of British Columbia","funders":"National Science Foundation","keywords":"Advection; Oceanography; Geology; Deep sea; Flux (metallurgy); Deep water; Ocean current; Boundary current; Eddy diffusion; Thermohaline circulation; Environmental science; Climatology; Meteorology; Turbulence; Geography","score_opus":0.014717215855725182,"score_gpt":0.24957614572010692,"score_spread":0.23485892986438173,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2112995327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84451306,0.000472591,0.13656473,0.00067007815,0.00012055088,0.00007378149,0.0012718905,0.00075992465,0.015553529],"genre_scores_gemma":[0.98993826,0.00011633226,0.0083088875,0.000028631628,0.000017174987,0.000018247703,0.00014467418,0.000019170118,0.0014086909],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999511,0.0000062894,0.0000021553053,0.00001801348,0.000011296332,0.000011071651],"domain_scores_gemma":[0.9998652,0.000027208698,0.00004013461,0.000015510517,0.000030187275,0.000021790242],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014950716,0.00040065325,0.00016817935,0.0004790321,0.00035846911,0.0006021294,0.0005816297,0.00042184666,0.0014463884],"category_scores_gemma":[0.00082825165,0.00018467766,0.00035640463,0.00037671797,0.00040351212,0.0008042951,0.00064045185,0.0003026189,0.00013912466],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041778255,0.0000752986,0.12527213,0.00014535931,0.00016197874,0.00053720444,0.0005881298,0.59264886,0.041400425,0.17262667,0.0051159016,0.06101025],"study_design_scores_gemma":[0.00006102286,0.0000903427,0.011236144,0.000012334676,0.000046478588,0.00012421957,0.00006022134,0.9701764,0.0026316224,0.00922915,0.006290643,0.00004146281],"about_ca_topic_score_codex":0.025749594,"about_ca_topic_score_gemma":0.008718598,"teacher_disagreement_score":0.025749594,"about_ca_system_score_codex":0.0008286451,"about_ca_system_score_gemma":0.00079655077,"threshold_uncertainty_score":0.051199436},"labels":[],"label_agreement":null},{"id":"W2113103639","doi":"10.1002/grl.50998","title":"Critical role for mesoscale eddy diffusion in supplying oxygen to hypoxic ocean waters","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Institute for Advanced Research; U.S. Department of Energy; National Science Foundation","keywords":"Thermocline; Diffusion; Environmental science; Mesoscale meteorology; Oxygen; Eddy diffusion; Geology; Oceanography; Atmospheric sciences; Meteorology; Turbulence; Chemistry; Physics; Thermodynamics","score_opus":0.02107008271547659,"score_gpt":0.2732489238574932,"score_spread":0.2521788411420166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113103639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99405295,0.0003384138,0.002176078,0.0006365709,0.000015608717,0.000008446772,0.000090897054,0.000042088956,0.0026389135],"genre_scores_gemma":[0.9996425,0.000059648177,0.00016542585,0.000015413805,0.000003425452,0.0000019963989,0.000015321666,0.0000035776688,0.00009256613],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999496,0.000012718168,0.0000046425107,0.000016955511,0.0000052644323,0.0000108101385],"domain_scores_gemma":[0.9994611,0.00029965176,0.000086861335,0.00002854846,0.00004914354,0.00007473747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002931788,0.00027298153,0.00023366437,0.00023304074,0.00047191555,0.0008857909,0.00020607951,0.00038710912,0.0015822485],"category_scores_gemma":[0.0015307334,0.00028059835,0.0002445152,0.00008596851,0.00055309065,0.0009699127,0.000592414,0.00025443497,0.0000997635],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001532993,0.00022298843,0.36314598,0.0003885547,0.00032739973,0.0009843742,0.00039134684,0.15989932,0.42348218,0.027548237,0.0015756619,0.02050087],"study_design_scores_gemma":[0.00021845213,0.00019799978,0.3392482,0.00006254564,0.00015272001,0.00033584773,0.0004793005,0.62113804,0.024680478,0.011540599,0.0018630567,0.000082838014],"about_ca_topic_score_codex":0.006555244,"about_ca_topic_score_gemma":0.0045965575,"teacher_disagreement_score":0.006555244,"about_ca_system_score_codex":0.0007131321,"about_ca_system_score_gemma":0.0005003237,"threshold_uncertainty_score":0.013034165},"labels":[],"label_agreement":null},{"id":"W2113144554","doi":"10.1029/2002gl016500","title":"Current sheet flapping motion and structure observed by Cluster","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":256,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Russian Foundation for Basic Research; York University","keywords":"Flapping; Plasma sheet; Current sheet; Tilt (camera); Physics; Amplitude; Plasma; Current (fluid); Current density; Magnetosphere; Geometry; Optics","score_opus":0.021160211073289602,"score_gpt":0.2792136265836683,"score_spread":0.2580534155103787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113144554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99653864,0.000053818414,0.0003684874,0.000057506168,0.000007842494,0.0000063295015,0.00023513575,0.000060199254,0.002672144],"genre_scores_gemma":[0.9982988,0.000031055773,0.0006560196,0.000020012105,0.000006583476,0.000008095883,0.00046916323,0.000015732117,0.00049455365],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99988854,0.0000066710127,0.000002377022,0.000029678493,0.000027920754,0.00004479759],"domain_scores_gemma":[0.99969494,0.000037837315,0.00004693073,0.00005312631,0.000083783714,0.000083404084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016301022,0.0001693468,0.0002468859,0.0007130981,0.00090350874,0.00048071519,0.00029975633,0.00034096412,0.00079102407],"category_scores_gemma":[0.00048673255,0.00021656038,0.00014747957,0.00063326425,0.00030440892,0.00016871774,0.0006937469,0.0004923503,0.00022187838],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021877869,0.00017624215,0.39867592,0.00013437748,0.00014059411,0.0035953,0.0040165526,0.008231192,0.53601354,0.0019746458,0.010841757,0.03401214],"study_design_scores_gemma":[0.000081576734,0.00023350972,0.9462906,0.000019077737,0.00003744127,0.0011618959,0.0005357538,0.012091211,0.031227957,0.00046564083,0.00779428,0.000061080085],"about_ca_topic_score_codex":0.0049423054,"about_ca_topic_score_gemma":0.005566672,"teacher_disagreement_score":0.0049423054,"about_ca_system_score_codex":0.0005520994,"about_ca_system_score_gemma":0.00024986922,"threshold_uncertainty_score":0.009827077},"labels":[],"label_agreement":null},{"id":"W2113855495","doi":"10.1002/grl.50358","title":"Climate impact of stratospheric ozone recovery","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Scheme for Promotion of Academic and Research Collaboration; Natural Environment Research Council; European Commission; Sight Research UK; Royal Society","keywords":"Ozone layer; Stratosphere; Ozone; Atmospheric sciences; Ozone depletion; Environmental science; Radiative forcing; Greenhouse gas; Montreal Protocol; Climatology; Forcing (mathematics); Climate change; Meteorology; Physics; Geology","score_opus":0.02539603613179254,"score_gpt":0.29169838693297495,"score_spread":0.2663023508011824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2113855495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872701,0.0010655912,0.00060487527,0.0016009827,0.000058808266,0.0000051241186,0.0022677106,0.0001084612,0.0070182933],"genre_scores_gemma":[0.99922276,0.00014948183,0.00004387584,0.00006298521,0.000009557019,0.0000014396559,0.0003233889,0.0000068844247,0.00017962232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983966,0.000039209805,0.0000057759057,0.000028427781,0.00001722909,0.00006969428],"domain_scores_gemma":[0.99971825,0.000053708907,0.00008183681,0.000034891975,0.00005636187,0.00005484945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003778394,0.00027966785,0.00019586267,0.00028609645,0.00029341647,0.0005469832,0.0002690943,0.00054286397,0.002110963],"category_scores_gemma":[0.00071055966,0.00009081209,0.00064848136,0.0003271093,0.00026794404,0.00038456274,0.000639522,0.0003988932,0.00019197271],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020086772,0.0002075915,0.6944658,0.0003068469,0.0015189574,0.001044863,0.00022516122,0.2059248,0.047917742,0.008827857,0.006500222,0.031051468],"study_design_scores_gemma":[0.000069373986,0.0002673411,0.94022673,0.000029324301,0.00034931023,0.00017102342,0.0003039729,0.03938544,0.0071924445,0.003054076,0.008903779,0.000047066525],"about_ca_topic_score_codex":0.01708061,"about_ca_topic_score_gemma":0.009481834,"teacher_disagreement_score":0.01708061,"about_ca_system_score_codex":0.0007789815,"about_ca_system_score_gemma":0.0003927274,"threshold_uncertainty_score":0.03396237},"labels":[],"label_agreement":null},{"id":"W2114603113","doi":"10.1029/2011gl050273","title":"Air quality over the Canadian oil sands: A first assessment using satellite observations","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":171,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Earth Sciences Division","keywords":"Satellite; Oil sands; Environmental science; Geology; Quality (philosophy); Meteorology; Climatology; Remote sensing; Geography; Asphalt; Archaeology","score_opus":0.07346129336432966,"score_gpt":0.3402563756545224,"score_spread":0.2667950822901927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114603113","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991435,0.00038448407,0.0004867849,0.000111275316,0.0000068373383,0.00007638198,0.004038316,0.000039244496,0.0034216521],"genre_scores_gemma":[0.99509746,0.00040849263,0.0011489618,0.00003977985,0.0000046318196,0.000022192888,0.0023416711,0.000006111583,0.00093061826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994035,0.000036433878,0.000016554388,0.00005910876,0.00038065578,0.00010379719],"domain_scores_gemma":[0.99911994,0.000047939615,0.00008595931,0.000026836067,0.0006390144,0.00008024417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057173264,0.0006560839,0.00026452544,0.0010757692,0.001041015,0.00074692565,0.00040611852,0.00033661164,0.00046908113],"category_scores_gemma":[0.0008054061,0.00019456867,0.00039393033,0.0021107972,0.00046498427,0.00023793751,0.00040217245,0.00020234098,0.000090743706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037816106,0.00009766062,0.9243599,0.0002913117,0.00024392777,0.00026765864,0.0009971105,0.0063259494,0.0118403435,0.00015953023,0.0018790258,0.053159446],"study_design_scores_gemma":[0.0000075025705,0.000059419905,0.99456316,0.000010862133,0.000033573047,0.000024174473,0.0003389424,0.0016669764,0.0012762174,0.000010952275,0.001992021,0.000016153845],"about_ca_topic_score_codex":0.9879281,"about_ca_topic_score_gemma":0.99416625,"teacher_disagreement_score":0.0120719075,"about_ca_system_score_codex":0.00955985,"about_ca_system_score_gemma":0.008279484,"threshold_uncertainty_score":0.069361925},"labels":[],"label_agreement":null},{"id":"W2114702547","doi":"10.1029/2008gl034271","title":"Lateral organic carbon supply to the deep Canada Basin","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Total organic carbon; Sediment trap; Abyssal zone; Carbon cycle; Arctic; Structural basin; Oceanography; Environmental science; Radiocarbon dating; Deep sea; Productivity; Geology; Carbon fibers; Sediment; Water column; Geomorphology; Paleontology; Environmental chemistry; Ecosystem","score_opus":0.015285211833352366,"score_gpt":0.23872482552313273,"score_spread":0.22343961368978038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114702547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99616313,0.00016370906,0.00007158306,0.000088487584,0.0000032675227,0.000001902359,0.0004419365,0.000010356365,0.003055593],"genre_scores_gemma":[0.9977857,0.00020280785,0.00012650463,0.00003337735,0.0000023628338,0.0000022644017,0.00034790332,0.0000055742885,0.001493439],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999182,0.0000018931854,0.0000020320176,0.000017271554,0.000022978185,0.00003761239],"domain_scores_gemma":[0.9997631,0.00001479393,0.000027257394,0.000007752008,0.00012351593,0.000063669024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000048252834,0.00020547284,0.00015801378,0.0005791719,0.0011610665,0.0008472287,0.00018883921,0.00015038016,0.0017470156],"category_scores_gemma":[0.00035569267,0.00013290449,0.0000988659,0.0006828835,0.000396905,0.00020222487,0.0007043922,0.00019381654,0.00015572704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032295918,0.000030622843,0.8524433,0.000115105344,0.00008903503,0.0007349052,0.0016643557,0.0032495453,0.093511626,0.0037874293,0.0018974976,0.042153656],"study_design_scores_gemma":[0.000009030464,0.000020258274,0.98158044,0.000025134816,0.000029885958,0.00015804124,0.0014364782,0.001725797,0.0040228055,0.0006384996,0.010337491,0.000016159454],"about_ca_topic_score_codex":0.8883232,"about_ca_topic_score_gemma":0.9503967,"teacher_disagreement_score":0.11167681,"about_ca_system_score_codex":0.007693667,"about_ca_system_score_gemma":0.008608175,"threshold_uncertainty_score":0.22466898},"labels":[],"label_agreement":null},{"id":"W2114777234","doi":"10.1002/grl.50452","title":"Interpreting seasonal changes in the carbon balance of southern Amazonia using measurements of XCO<sub>2</sub> and chlorophyll fluorescence from GOSAT","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Oceanic and Atmospheric Administration; Instituto Nacional de Pesquisas da Amazônia; European Commission; National Aeronautics and Space Administration; California Institute of Technology; Universidade de São Paulo; Jet Propulsion Laboratory; Deutsche Forschungsgemeinschaft","keywords":"Environmental science; Carbon cycle; Dry season; Amazon rainforest; Atmospheric sciences; Biomass (ecology); Greenhouse gas; Primary production; Climatology; Ecosystem; Ecology; Geology; Biology","score_opus":0.02135270849501673,"score_gpt":0.24256273258491992,"score_spread":0.2212100240899032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114777234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99831885,0.00013266085,0.0005214138,0.000070586786,0.0000048023053,0.0000051013517,0.0003557241,0.00004262902,0.0005482504],"genre_scores_gemma":[0.9989573,0.00006386433,0.0006178442,0.00002130721,0.0000067455744,0.000004294943,0.00026156244,0.000007916412,0.000059047332],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999615,0.0000054714064,0.0000030629874,0.000012448903,0.000008933431,0.000008584514],"domain_scores_gemma":[0.99983037,0.00003267871,0.00006833091,0.000015801319,0.000029497536,0.00002343239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020518758,0.0002705052,0.00017385154,0.0003692651,0.00019158158,0.00032804185,0.00017962026,0.00022018775,0.0004164911],"category_scores_gemma":[0.0004562124,0.00017662418,0.00015177854,0.0003755082,0.00015998528,0.00034672298,0.00023616236,0.00014206726,0.00007224711],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012575532,0.00002993036,0.9036904,0.00007315117,0.00010184084,0.00014694998,0.00023788003,0.0019973405,0.08256846,0.00010233171,0.00029267505,0.010633247],"study_design_scores_gemma":[0.00000840579,0.0000143870375,0.9913378,0.000005559296,0.00002736475,0.000041170897,0.00010743026,0.005276601,0.0025945157,0.00008305796,0.00049829617,0.0000053816857],"about_ca_topic_score_codex":0.030797282,"about_ca_topic_score_gemma":0.06529832,"teacher_disagreement_score":0.030797282,"about_ca_system_score_codex":0.00028803083,"about_ca_system_score_gemma":0.00024150895,"threshold_uncertainty_score":0.061236024},"labels":[],"label_agreement":null},{"id":"W2114797592","doi":"10.1029/2011gl049714","title":"Western Arctic Ocean temperature variability during the last 8000 years","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Université du Québec à Montréal","funders":"","keywords":"Geology; Dinocyst; Oceanography; Arctic; Climatology; Thermohaline circulation","score_opus":0.02945163358167828,"score_gpt":0.2640547501806418,"score_spread":0.2346031165989635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114797592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966009,0.00019384074,0.00012295337,0.000024143605,0.000006254958,0.0000012812689,0.002246362,0.000009506216,0.00079464883],"genre_scores_gemma":[0.99458116,0.00020775395,0.0002331883,0.000011576064,0.0000087626395,0.0000039499023,0.004452324,0.000004976857,0.0004963164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993,0.0000074627596,0.0000073231495,0.000026324033,0.000015543732,0.000013376246],"domain_scores_gemma":[0.99980384,0.000010939402,0.00006350848,0.000012335658,0.00008986068,0.000019500107],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020129858,0.00016043289,0.0001143579,0.00045324405,0.00030500794,0.00039460216,0.000119918106,0.00012212928,0.00044223428],"category_scores_gemma":[0.0004325373,0.00009049277,0.00014830807,0.00080614164,0.00009650299,0.00020131911,0.00020028408,0.00012739131,0.00016039266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096730444,0.000008017763,0.9910391,0.000015800739,0.00008540381,0.00006225929,0.00020774106,0.0010516446,0.0010607877,0.00008346658,0.00048636057,0.0058026924],"study_design_scores_gemma":[0.0000013264713,0.000006095074,0.99734503,0.0000061203004,0.000015465668,0.000043351018,0.000056460525,0.0006036771,0.00020256542,0.000011951445,0.0017055302,0.0000024355766],"about_ca_topic_score_codex":0.15474452,"about_ca_topic_score_gemma":0.24302728,"teacher_disagreement_score":0.15474452,"about_ca_system_score_codex":0.00063572876,"about_ca_system_score_gemma":0.00036791788,"threshold_uncertainty_score":0.30768758},"labels":[],"label_agreement":null},{"id":"W2114871109","doi":"10.1029/2004gl020292","title":"The effect of hydrate content on seismic attenuation: A case study for Mallik 2L‐38 well data, Mackenzie delta, Canada","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Attenuation; Hydrate; Saturation (graph theory); Geology; Mineralogy; Lithology; Sediment; Delta; Clathrate hydrate; Petrology; Geomorphology; Optics; Chemistry; Physics","score_opus":0.05061978217756426,"score_gpt":0.3110940912610834,"score_spread":0.26047430908351915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2114871109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983005,0.00004192562,0.00035723398,0.000062285486,9.1721245e-7,0.000019230256,0.00041029986,0.00004443699,0.0007631231],"genre_scores_gemma":[0.99885476,0.00003607345,0.0005803215,0.0000088357965,6.841302e-7,0.000004178538,0.00027781018,0.000007678079,0.00022954174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996388,0.00004214409,0.000022102393,0.000057810408,0.00012533698,0.00011381597],"domain_scores_gemma":[0.9984906,0.0005709773,0.00014577176,0.000118727774,0.0005619807,0.000111980575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063664216,0.00053509464,0.00033631045,0.0009128777,0.0011520786,0.0007790999,0.0012345298,0.000743536,0.0006573554],"category_scores_gemma":[0.002560318,0.00036732506,0.0003648486,0.0017445666,0.0012276208,0.0004724181,0.00043613292,0.00036437425,0.0000799457],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000688759,0.00024016417,0.69530904,0.0001579391,0.00014502363,0.0040862225,0.0015699998,0.26315963,0.0143274395,0.0013906815,0.0017173329,0.01720776],"study_design_scores_gemma":[0.00014238023,0.00014311781,0.7111274,0.000037833728,0.0001374779,0.0005100656,0.0022642843,0.27469575,0.008681582,0.00041336028,0.0017216726,0.00012512969],"about_ca_topic_score_codex":0.95348287,"about_ca_topic_score_gemma":0.9720172,"teacher_disagreement_score":0.046517134,"about_ca_system_score_codex":0.010454415,"about_ca_system_score_gemma":0.0045026527,"threshold_uncertainty_score":0.09358209},"labels":[],"label_agreement":null},{"id":"W2115365017","doi":"10.1029/2012gl053978","title":"Reconciling tracer and float observations of the export pathways of Labrador Sea Water","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Boundary current; Oceanography; Geology; Water mass; TRACER; Ocean current; Potential vorticity; Equator; Latitude; Structural basin; Subtropics; Climatology; Vorticity; Geography; Geomorphology","score_opus":0.06541313463588147,"score_gpt":0.25714537878521887,"score_spread":0.1917322441493374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115365017","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969405,0.00013532421,0.0010911528,0.00016015727,0.000013059862,0.0000070027504,0.0006965509,0.000072028306,0.00088431814],"genre_scores_gemma":[0.9981408,0.000081273494,0.0006182171,0.000029425737,0.00000840507,0.000004731276,0.000920789,0.000033596785,0.00016276081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974924,0.00006315816,0.000027726363,0.00008563033,0.000037792848,0.00003642699],"domain_scores_gemma":[0.999156,0.00025238018,0.0002260667,0.00015845899,0.0001486906,0.00005841852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081070245,0.0004108979,0.00036143686,0.0007803317,0.00027795462,0.0012490733,0.0004928161,0.00046236374,0.0005636767],"category_scores_gemma":[0.0025435972,0.00030341742,0.00044543744,0.0006242016,0.0002966908,0.0009603021,0.0006226517,0.00036282765,0.00014716716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004341862,0.00011478279,0.93713295,0.00008482322,0.00042896127,0.00031488793,0.0004621135,0.02730549,0.013184428,0.0016397865,0.0008065495,0.018090963],"study_design_scores_gemma":[0.0001250501,0.00007738552,0.87580156,0.00003433536,0.00017745019,0.00011476938,0.00037281952,0.110345215,0.0078632245,0.0014689836,0.0035527037,0.00006639885],"about_ca_topic_score_codex":0.039168432,"about_ca_topic_score_gemma":0.036518376,"teacher_disagreement_score":0.039168432,"about_ca_system_score_codex":0.0012172839,"about_ca_system_score_gemma":0.00059265346,"threshold_uncertainty_score":0.07788086},"labels":[],"label_agreement":null},{"id":"W2115936040","doi":"10.1029/2011gl050168","title":"Abrupt onset of the Little Ice Age triggered by volcanism and sustained by sea‐ice/ocean feedbacks","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":887,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs; National Science Foundation","keywords":"Climatology; Sea ice; Geology; Volcanism; Arctic sea ice decline; Cryosphere; Northern Hemisphere; Arctic; Ice age; Volcano; Insolation; Oceanography; Arctic ice pack; Atmospheric sciences; Antarctic sea ice; Glacial period; Geomorphology","score_opus":0.020409130612705408,"score_gpt":0.2780169934553428,"score_spread":0.2576078628426374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115936040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984676,0.000107125845,0.00019938966,0.000045301487,0.0000057799725,0.0000020553189,0.00014360253,0.000032813674,0.000996112],"genre_scores_gemma":[0.9997385,0.000032905675,0.00004670479,0.000009330434,0.000003038459,8.9636904e-7,0.0000971982,0.000002451793,0.00006915429],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996996,0.0000029486393,0.0000016450401,0.000007449717,0.000006736526,0.000011237232],"domain_scores_gemma":[0.99989414,0.000018111066,0.000021735788,0.000008067631,0.000018087954,0.000039906394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011818148,0.00015223584,0.0002641973,0.00031578023,0.0003088114,0.0004992442,0.00020698139,0.00022773909,0.0007167865],"category_scores_gemma":[0.00033355498,0.00010958725,0.00018907669,0.00019898171,0.00034473205,0.00018802371,0.00031562222,0.0001887305,0.000075673415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006069158,0.000064271546,0.8682219,0.000112800924,0.00018774813,0.0013190873,0.00045014816,0.017651608,0.09775143,0.0014837284,0.0010429596,0.011107474],"study_design_scores_gemma":[0.000023126391,0.000054270917,0.97819114,0.000013039298,0.000055296205,0.00016112346,0.0002145028,0.014739546,0.004719359,0.00047135138,0.0013423946,0.00001496772],"about_ca_topic_score_codex":0.038915113,"about_ca_topic_score_gemma":0.046041597,"teacher_disagreement_score":0.038915113,"about_ca_system_score_codex":0.0009195077,"about_ca_system_score_gemma":0.00054057885,"threshold_uncertainty_score":0.0773772},"labels":[],"label_agreement":null},{"id":"W2115953659","doi":"10.1002/2015gl065665","title":"Using scaling for macroweather forecasting including the pause","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration","keywords":"Hindcast; Coupled model intercomparison project; Climatology; Scaling; Meteorology; Climate model; Environmental science; Scalar (mathematics); Climate change; Mathematics; Geology; Geography","score_opus":0.40279610353068607,"score_gpt":0.4117115776717455,"score_spread":0.00891547414105942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115953659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7968842,0.0004902828,0.18281087,0.0011109272,0.0006699224,0.00004891812,0.0011135025,0.0026510782,0.014220206],"genre_scores_gemma":[0.9871651,0.000050390125,0.012071456,0.000035241643,0.00004807489,0.000011179234,0.00020053262,0.000073177776,0.00034480193],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999908,0.00002299119,0.0000068761624,0.000024283929,0.000024532577,0.000013246442],"domain_scores_gemma":[0.9995677,0.00014393702,0.00005860193,0.00008861101,0.00009968373,0.000041359523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041747393,0.00031712733,0.00027990603,0.00025400694,0.00022742011,0.00055200444,0.0004255591,0.00030382903,0.0012712204],"category_scores_gemma":[0.0021465109,0.00015800865,0.00028703792,0.00027873536,0.00018315286,0.00077445613,0.00046726968,0.0006855687,0.00018807447],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014864234,0.00004722225,0.021259308,0.00004562051,0.000048006983,0.00012333441,0.000095310534,0.9075709,0.007777599,0.0076904185,0.0035302541,0.051663417],"study_design_scores_gemma":[0.000007801925,0.000006673111,0.0014620019,0.000003950009,0.0000028280533,0.0000059198464,0.0000066821417,0.99566346,0.00061708514,0.0014850111,0.0007321431,0.000006360135],"about_ca_topic_score_codex":0.009292314,"about_ca_topic_score_gemma":0.0076004723,"teacher_disagreement_score":0.009292314,"about_ca_system_score_codex":0.00032360735,"about_ca_system_score_gemma":0.00046508628,"threshold_uncertainty_score":0.018476427},"labels":[],"label_agreement":null},{"id":"W2115958816","doi":"10.1029/2006gl028024","title":"Future abrupt reductions in the summer Arctic sea ice","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":750,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Ice-albedo feedback; Climatology; Sea ice; Environmental science; Arctic sea ice decline; Arctic ice pack; Arctic geoengineering; Radiative forcing; Arctic; Climate model; Albedo (alchemy); Forcing (mathematics); Atmospheric sciences; Shortwave; Cryosphere; Climate change; Drift ice; Oceanography; Geology; Radiative transfer","score_opus":0.022959913910417334,"score_gpt":0.2767693721234971,"score_spread":0.25380945821307976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2115958816","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961081,0.00007281109,0.0009891803,0.00039073394,0.000019518651,0.00000428088,0.00043390403,0.0000473987,0.0019341046],"genre_scores_gemma":[0.9991222,0.00006714214,0.00026471962,0.000038990333,0.000005341418,0.000005692616,0.00032305985,0.0000058974315,0.00016697521],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99982834,0.00004951401,0.000008223668,0.000030977986,0.000031499352,0.000051414645],"domain_scores_gemma":[0.999655,0.00010528454,0.000080139354,0.00002593925,0.000060024522,0.0000735922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000749314,0.00033358872,0.00021015323,0.00025466553,0.0004355849,0.0007218482,0.00038061044,0.00068701484,0.001582473],"category_scores_gemma":[0.0023303973,0.00022464759,0.0005163914,0.00036740073,0.0003462295,0.00070358044,0.0004957346,0.0005476664,0.00017439444],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003678783,0.00010615436,0.19683771,0.00007543669,0.00019928672,0.00042260537,0.00031859125,0.78099895,0.0030456968,0.0058029494,0.0030423729,0.008782442],"study_design_scores_gemma":[0.00018959981,0.00034037136,0.19925828,0.000041522206,0.0001614964,0.00032032232,0.0010492388,0.779926,0.0028287508,0.00952643,0.0062906737,0.000067373156],"about_ca_topic_score_codex":0.011368631,"about_ca_topic_score_gemma":0.014845143,"teacher_disagreement_score":0.011368631,"about_ca_system_score_codex":0.00089429395,"about_ca_system_score_gemma":0.00060816255,"threshold_uncertainty_score":0.022604942},"labels":[],"label_agreement":null},{"id":"W2116061942","doi":"10.1029/2009gl042239","title":"Role of tropical Pacific SSTs in global medieval hydroclimate: A modeling study","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"PricewaterhouseCoopers (Canada)","funders":"","keywords":"Climatology; Tropics; Tropical Atlantic; Sea surface temperature; Climate model; Geology; Tropical climate; Southern Hemisphere; Oceanography; Northern Hemisphere; Environmental science; Climate change; Geography","score_opus":0.026730963759626473,"score_gpt":0.31022403194041276,"score_spread":0.2834930681807863,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116061942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992786,0.00036768915,0.0015710834,0.00039984685,0.00000930892,0.000009846104,0.000639421,0.000051223873,0.004165509],"genre_scores_gemma":[0.99778676,0.0004816037,0.0007603008,0.00002428185,0.000017678989,0.000013306066,0.00022303485,0.000017682765,0.00067522115],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994826,0.00001929592,0.0000027236024,0.000013217169,0.000005909224,0.000010578668],"domain_scores_gemma":[0.9998097,0.000098663215,0.000029017054,0.00001555141,0.00001615161,0.0000309485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002483333,0.000501352,0.00026018766,0.00033145648,0.00042672642,0.0008505227,0.0007063049,0.0006226728,0.0018668906],"category_scores_gemma":[0.0006122015,0.00031548532,0.00055715657,0.000771702,0.00027221793,0.0008701725,0.00042224032,0.00037763503,0.00019169085],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020881457,0.00014314611,0.09592374,0.00009342685,0.00021860238,0.00032808608,0.00022992813,0.8855387,0.0019618408,0.0058894474,0.0012524222,0.008211889],"study_design_scores_gemma":[0.00006638717,0.00005497888,0.02094798,0.000015917489,0.000077565484,0.00006106909,0.00011743881,0.9752172,0.00040593627,0.001377085,0.0016433154,0.000014994868],"about_ca_topic_score_codex":0.05206204,"about_ca_topic_score_gemma":0.032750104,"teacher_disagreement_score":0.05206204,"about_ca_system_score_codex":0.0009497834,"about_ca_system_score_gemma":0.0007079283,"threshold_uncertainty_score":0.10351801},"labels":[],"label_agreement":null},{"id":"W2116397004","doi":"10.1029/2009gl039663","title":"Sources and fate of freshwater exported in the East Greenland Current","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Oceanography; Meltwater; Hydrography; Water mass; Current (fluid); Geology; Arctic; Sea ice; Climatology; Glacier; Geomorphology","score_opus":0.03388485262669855,"score_gpt":0.27937027792710917,"score_spread":0.24548542530041062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116397004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99927956,0.00016549818,0.00004154238,0.00002012947,0.000001791586,9.472425e-7,0.00013953952,0.0000030657307,0.00034791004],"genre_scores_gemma":[0.9987043,0.00026577155,0.0001630922,0.00003136789,0.000002506342,0.0000018261139,0.00036417245,0.000006948676,0.00045985583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993634,0.000006195516,0.000004825027,0.00002091274,0.000013489551,0.000018338213],"domain_scores_gemma":[0.9998394,0.000014832398,0.00007034378,0.000009251547,0.00004327919,0.000022932067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013303293,0.00015218533,0.00022773324,0.0010842377,0.00036362474,0.0007922314,0.0001866033,0.00016753736,0.00042499095],"category_scores_gemma":[0.00023439113,0.00014046243,0.0001356387,0.000746768,0.00039863677,0.0006305093,0.0005254223,0.0001755046,0.00009006053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048402298,0.000036369092,0.85613453,0.000054951157,0.00010013445,0.00068425626,0.0008069994,0.0017990689,0.11979214,0.00060933986,0.00027748386,0.019220792],"study_design_scores_gemma":[0.0000053328035,0.000031119722,0.9934977,0.000017937587,0.000019656745,0.00007737234,0.00040365753,0.00072020566,0.004015709,0.00013670824,0.0010663746,0.0000081803],"about_ca_topic_score_codex":0.04483458,"about_ca_topic_score_gemma":0.09883634,"teacher_disagreement_score":0.04483458,"about_ca_system_score_codex":0.0022798586,"about_ca_system_score_gemma":0.0006665387,"threshold_uncertainty_score":0.08914721},"labels":[],"label_agreement":null},{"id":"W2116460859","doi":"10.1029/2000gl012051","title":"Can the direct and semi‐direct aerosol effect compete with the indirect effect on a global scale?","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":186,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Deutsches Klimarechenzentrum","keywords":"Aerosol; Environmental science; Atmospheric sciences; Cloud cover; Sea salt aerosol; Cloud albedo; Liquid water path; Liquid water content; Northern Hemisphere; Albedo (alchemy); Climatology; Cloud computing; Meteorology; Physics; Geology","score_opus":0.008549125456379461,"score_gpt":0.25677086725946824,"score_spread":0.24822174180308879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116460859","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91303074,0.011392657,0.014312129,0.0049949144,0.00036535243,0.00017312072,0.0008783092,0.00031158252,0.05454113],"genre_scores_gemma":[0.99223083,0.0023244643,0.001551839,0.0010213713,0.00011240648,0.00003919357,0.00019466454,0.00008552714,0.0024398805],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99927646,0.00013029278,0.000027427131,0.00020281259,0.00010666801,0.00025637864],"domain_scores_gemma":[0.9982134,0.00091528415,0.00027469287,0.00018513517,0.0001990416,0.00021250156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017266825,0.0014705068,0.0025325792,0.000711067,0.00087910646,0.001813797,0.0013350664,0.002435737,0.014874482],"category_scores_gemma":[0.0021496753,0.000821845,0.0017947502,0.0007823235,0.0013490301,0.0051369634,0.002697818,0.00091845513,0.0012026334],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002545018,0.0009884508,0.44124278,0.006147032,0.006997227,0.0029764236,0.00073410996,0.061855868,0.15324114,0.10604047,0.006272819,0.21095867],"study_design_scores_gemma":[0.0005947524,0.0017356582,0.80908936,0.00031079337,0.0023467443,0.0012834363,0.001735827,0.050067294,0.02353605,0.090717,0.018208884,0.00037416167],"about_ca_topic_score_codex":0.01050664,"about_ca_topic_score_gemma":0.01219677,"teacher_disagreement_score":0.014874482,"about_ca_system_score_codex":0.0009355885,"about_ca_system_score_gemma":0.00063497823,"threshold_uncertainty_score":0.049760103},"labels":[],"label_agreement":null},{"id":"W2116628938","doi":"10.1029/2003gl017902","title":"Deep dissolved iron profiles in the eastern North Atlantic in relation to water masses","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Water mass; Abyssal zone; Geology; Oceanography; Outflow; Plateau (mathematics); Mediterranean sea; Remineralisation; Surface water; Bottom water; Forcing (mathematics); Mediterranean climate; Environmental science; Atmospheric sciences; Chemistry","score_opus":0.024884874605639772,"score_gpt":0.2530491017420665,"score_spread":0.22816422713642676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116628938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99964845,0.000037062546,0.000013092913,0.000007866614,7.891429e-7,7.474299e-7,0.00006440269,0.0000014347663,0.00022616841],"genre_scores_gemma":[0.99931145,0.000049249753,0.000060005896,0.000014667961,0.0000014888217,0.0000018757592,0.00020899162,9.917661e-7,0.0003512929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999714,0.0000019306608,0.000002290732,0.00000850226,0.0000071719896,0.00000876934],"domain_scores_gemma":[0.9998913,0.000011878933,0.000031786367,0.0000036352737,0.000032586835,0.000028771057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060766088,0.0001267762,0.00013186809,0.00035729952,0.00024849412,0.0002946443,0.0001084328,0.00017541174,0.0003927967],"category_scores_gemma":[0.00018141413,0.00013700983,0.000065925284,0.0003072907,0.00015647677,0.000113205984,0.00020899187,0.00013524349,0.00008988353],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022374948,0.000028277154,0.9561726,0.000020866199,0.000035000874,0.000255008,0.0005956655,0.00017000939,0.036542695,0.000035955836,0.00009994183,0.0058202427],"study_design_scores_gemma":[0.0000025824436,0.000016145787,0.9992575,0.0000016179872,0.0000044687736,0.000027513746,0.00011840101,0.00010020601,0.00030785514,0.00000506418,0.00015738029,0.0000012339921],"about_ca_topic_score_codex":0.0700962,"about_ca_topic_score_gemma":0.14368416,"teacher_disagreement_score":0.0700962,"about_ca_system_score_codex":0.00056241016,"about_ca_system_score_gemma":0.00018507092,"threshold_uncertainty_score":0.1393764},"labels":[],"label_agreement":null},{"id":"W2116653258","doi":"10.1002/2015gl063643","title":"Nonlinear interactions of waves and tides in a subterranean estuary","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Estuary; Aquifer; Submarine groundwater discharge; Geology; Oceanography; Salinity; Groundwater; Submarine pipeline; Shore; Surf zone; Hydrology (agriculture); Geotechnical engineering","score_opus":0.057578157021036254,"score_gpt":0.3071183221027285,"score_spread":0.24954016508169224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116653258","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926883,0.0000059133126,0.0002293609,0.000022626877,0.0000017105459,0.0000017806634,0.00002638479,0.000006908393,0.0004365165],"genre_scores_gemma":[0.99961567,0.0000108866225,0.00012504181,0.0000052956057,8.837911e-7,0.0000021156188,0.000024873925,0.0000016136429,0.00021368878],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996376,0.0000074326963,0.0000028844615,0.0000070243686,0.000005746008,0.000013147901],"domain_scores_gemma":[0.9999052,0.00003375637,0.0000189016,0.000007109004,0.000015222227,0.000019654815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010803916,0.0002387194,0.00021108784,0.00025148178,0.0005437772,0.00050178065,0.00022166013,0.00045070017,0.00064164907],"category_scores_gemma":[0.0003216174,0.00017107249,0.00037641532,0.00024341242,0.00035674302,0.00024788786,0.00040692807,0.00021709003,0.000050726405],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021382124,0.00018304595,0.10079709,0.000034286746,0.00011750645,0.0009196377,0.00018514325,0.8738613,0.017817087,0.0013455695,0.0002764531,0.004249086],"study_design_scores_gemma":[0.00004567117,0.00012765847,0.064419664,0.00000473646,0.00004280654,0.000045574623,0.00027585356,0.93352336,0.00088508194,0.00037180027,0.00023564535,0.000022166141],"about_ca_topic_score_codex":0.04580547,"about_ca_topic_score_gemma":0.037048545,"teacher_disagreement_score":0.04580547,"about_ca_system_score_codex":0.0006056654,"about_ca_system_score_gemma":0.000595828,"threshold_uncertainty_score":0.091077685},"labels":[],"label_agreement":null},{"id":"W2116985822","doi":"10.1029/2000gl011385","title":"On the use of isotopic composition measurements of volatile organic compounds to determine the “photochemical age” of an air mass","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Hydrocarbon; Chemistry; Isotope; Radical; Environmental chemistry; Isotopes of carbon; Methane; Isotope analysis; Composition (language); Photochemistry; Kinetic isotope effect; Stable isotope ratio; Carbon fibers; Total organic carbon; Organic chemistry; Materials science; Deuterium; Geology","score_opus":0.049528670356673854,"score_gpt":0.27000449561272344,"score_spread":0.22047582525604958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2116985822","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14864567,0.0098904045,0.8251837,0.00032172757,0.00028301455,0.00016227496,0.0010800894,0.0006945585,0.013738593],"genre_scores_gemma":[0.79230887,0.008706536,0.19480921,0.00013979686,0.00017563508,0.0001349589,0.0006291246,0.00014547791,0.0029503792],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99947137,0.00008755093,0.000024550714,0.00013984343,0.00024959425,0.00002708066],"domain_scores_gemma":[0.9988644,0.00055060297,0.00023774084,0.00013555538,0.0001923181,0.000019330395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011343581,0.00070991897,0.0003074598,0.001857614,0.00032109473,0.0006197462,0.0007007449,0.0006558476,0.0007614626],"category_scores_gemma":[0.0023782437,0.00027969238,0.00038134478,0.0012432442,0.00090426195,0.0015695601,0.00072890153,0.00062231,0.00039436354],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047884355,0.000096888725,0.04397967,0.0008957047,0.00022103303,0.00048252367,0.0003245154,0.016834408,0.55655456,0.057068158,0.0010202117,0.32204363],"study_design_scores_gemma":[0.00003056446,0.0004957387,0.043668654,0.0001264549,0.0001569057,0.0016357546,0.000115004616,0.09325659,0.79600936,0.039575476,0.024742201,0.0001872413],"about_ca_topic_score_codex":0.0010277046,"about_ca_topic_score_gemma":0.0013741283,"teacher_disagreement_score":0.001857614,"about_ca_system_score_codex":0.0004831962,"about_ca_system_score_gemma":0.00027610472,"threshold_uncertainty_score":0.0059990883},"labels":[],"label_agreement":null},{"id":"W2117541961","doi":"10.1029/2006gl027261","title":"Abrupt climatic events during the last glacial‐interglacial transition in Alaska","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Stadial; Interglacial; Geology; Glacial period; Younger Dryas; Paleoclimatology; Ice core; Climatology; Oceanography; Holocene; Boreal; Physical geography; Abrupt climate change; Period (music); Climate change; Global warming; Paleontology; Geography; Effects of global warming","score_opus":0.017228444300728632,"score_gpt":0.27441325189482946,"score_spread":0.25718480759410084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117541961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993038,0.00014441747,0.000021172584,0.000041532774,0.0000057253737,8.3560417e-7,0.000070688984,0.00000388009,0.00040789804],"genre_scores_gemma":[0.99969554,0.00009911903,0.000024012419,0.000011380522,0.0000055462647,0.0000018125999,0.000100897065,9.369574e-7,0.000060786275],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998822,0.000023022169,0.000017423265,0.000028451967,0.000020208026,0.000028640487],"domain_scores_gemma":[0.9996557,0.000049815717,0.00015288524,0.000015576145,0.000047403795,0.00007862191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032430474,0.00007773748,0.00013858789,0.0008129427,0.0007380877,0.0006568218,0.00014008417,0.00030110253,0.0005378538],"category_scores_gemma":[0.0010252099,0.0001188776,0.00010963753,0.00067277974,0.00047011246,0.0004020084,0.00064865354,0.0002650531,0.00008058612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012017977,0.00001925774,0.9917468,0.000018679382,0.00003185741,0.00024647676,0.0012481754,0.00028495875,0.0019859916,0.00012891846,0.0001740103,0.003994702],"study_design_scores_gemma":[0.0000017567705,0.000009327492,0.99883527,0.0000053612644,0.000006258516,0.00005438958,0.0006059845,0.00008816672,0.000076174634,0.00004819785,0.00026648992,0.0000027308415],"about_ca_topic_score_codex":0.020989789,"about_ca_topic_score_gemma":0.051743142,"teacher_disagreement_score":0.020989789,"about_ca_system_score_codex":0.00071200344,"about_ca_system_score_gemma":0.00036672133,"threshold_uncertainty_score":0.041735232},"labels":[],"label_agreement":null},{"id":"W2117619048","doi":"10.1029/2008gl034897","title":"Dual‐probe heat pulse method for snow density and thermal properties measurement","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Snow; Thermal; Remote sensing; Pulse (music); Environmental science; Materials science; Atmospheric sciences; Dual (grammatical number); Meteorology; Optics; Geology; Physics","score_opus":0.14301596681034395,"score_gpt":0.3012156457684556,"score_spread":0.15819967895811166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117619048","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.14376341,0.002384845,0.8420105,0.00040502712,0.00057339045,0.0002764811,0.0010736695,0.0018284353,0.007684203],"genre_scores_gemma":[0.5597159,0.0012625101,0.4304602,0.00029160097,0.00013409596,0.00073373795,0.000544853,0.00010088798,0.00675607],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99931574,0.00013635232,0.000018975174,0.00017686476,0.0003109721,0.000041180272],"domain_scores_gemma":[0.99936503,0.00021026452,0.000066201676,0.00011060441,0.00020838386,0.000039564165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051902945,0.00045839875,0.0004342166,0.0007633672,0.0003390861,0.00033372868,0.0009046303,0.0005900844,0.0029791002],"category_scores_gemma":[0.001209327,0.0004162579,0.00020370122,0.00079379155,0.00031209557,0.00062903157,0.00056384725,0.00089863996,0.0010655193],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037760034,0.00011393161,0.0039246385,0.000311789,0.000028543243,0.00012626436,0.00014018828,0.0011533229,0.88088596,0.0018203773,0.0035092437,0.107608214],"study_design_scores_gemma":[0.00007396983,0.00048566406,0.011763556,0.000030503015,0.00006120822,0.0011531336,0.00012486118,0.07645612,0.8835336,0.0017736176,0.024422413,0.000121462326],"about_ca_topic_score_codex":0.0007754963,"about_ca_topic_score_gemma":0.0010773686,"teacher_disagreement_score":0.0029791002,"about_ca_system_score_codex":0.00037035393,"about_ca_system_score_gemma":0.00034894957,"threshold_uncertainty_score":0.009966075},"labels":[],"label_agreement":null},{"id":"W2117998036","doi":"10.1002/2015gl064360","title":"Exploring the impact of CMIP5 model biases on the simulation of North Atlantic decadal variability","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ocean gyre; Climatology; Anomaly (physics); Environmental science; Temperature salinity diagrams; Climate model; Ensemble average; Data assimilation; Coupled model intercomparison project; Climate change; Salinity; Geology; Oceanography; Subtropics; Meteorology; Geography; Ecology","score_opus":0.3068499878182161,"score_gpt":0.37891517116240464,"score_spread":0.07206518334418854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2117998036","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978684,0.000040260307,0.0010949436,0.000091569185,0.000011364923,0.0000034395193,0.00026960898,0.00004827723,0.0005720177],"genre_scores_gemma":[0.9992772,0.000017344571,0.00044630887,0.000014324407,0.0000035887292,0.0000050465765,0.00015788038,0.000009349059,0.00006897547],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998185,0.00008010645,0.000013924385,0.000037786096,0.000016752709,0.000032936947],"domain_scores_gemma":[0.99870265,0.00078092905,0.00011583991,0.00016838268,0.00015091927,0.00008121995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015038355,0.000377901,0.00026284758,0.00021864404,0.0002969319,0.0006989444,0.00059363066,0.0004743711,0.0008911059],"category_scores_gemma":[0.003737332,0.0002515194,0.00040836007,0.00033188492,0.00024990545,0.0005289435,0.00042376778,0.0005194702,0.0000909381],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002060749,0.000102158665,0.16605458,0.000029424695,0.00024070988,0.00004775225,0.00006301073,0.8241147,0.0016366622,0.0011011917,0.0007407474,0.0056630573],"study_design_scores_gemma":[0.000026856334,0.000048065347,0.02631243,0.00000821334,0.000044097065,0.000008215314,0.000036815887,0.9719883,0.0009691868,0.00031014372,0.00023859733,0.000009109234],"about_ca_topic_score_codex":0.032579247,"about_ca_topic_score_gemma":0.016155297,"teacher_disagreement_score":0.032579247,"about_ca_system_score_codex":0.0005784156,"about_ca_system_score_gemma":0.00073115836,"threshold_uncertainty_score":0.06477922},"labels":[],"label_agreement":null},{"id":"W2118210391","doi":"10.1029/2006gl026425","title":"Comparison of Odin‐OSIRIS OH A<sup>2</sup>Σ<sup>+</sup>‐X<sup>2</sup>Π 0‐0 mesospheric observations and ACE‐FTS water vapor observations","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Saskatchewan","funders":"Canadian Space Agency; Tekes; Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales","keywords":"Osiris; Mesosphere; Water vapor; Stratosphere; Altitude (triangle); Aeronomy; Atmospheric sciences; Spectrograph; Analytical Chemistry (journal); Chemistry; Atmosphere (unit); Physics; Spectral line; Meteorology; Environmental chemistry","score_opus":0.06844671859970594,"score_gpt":0.30210749263805514,"score_spread":0.2336607740383492,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118210391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97832644,0.00012197234,0.0052171554,0.00008859877,0.00003140504,0.000023387018,0.008943619,0.0006123456,0.0066350894],"genre_scores_gemma":[0.9842582,0.00006413343,0.006948625,0.000027192033,0.000009445186,0.000015610665,0.007829028,0.00005588944,0.0007919249],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985325,0.000022719554,0.000013556778,0.00004595612,0.00004517121,0.0000193004],"domain_scores_gemma":[0.9997186,0.000051226452,0.00004050785,0.000051783307,0.000119012075,0.000018765424],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00046142854,0.00023992098,0.00013926854,0.00043453483,0.00016170592,0.0004264897,0.00023020318,0.00019243857,0.001131676],"category_scores_gemma":[0.00073564996,0.00014658859,0.00018476501,0.0005396728,0.00007813308,0.0004067429,0.0002182306,0.00017116337,0.00032004676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017555285,0.00046242905,0.5588809,0.00030974273,0.00050961686,0.00018205745,0.0004793264,0.07529682,0.15262616,0.0030592266,0.009937351,0.19650078],"study_design_scores_gemma":[0.00013943981,0.000103065526,0.75553083,0.000024940813,0.00010564075,0.00012708083,0.0004088351,0.17299405,0.05622451,0.0006408337,0.013656386,0.00004448004],"about_ca_topic_score_codex":0.007727604,"about_ca_topic_score_gemma":0.013185656,"teacher_disagreement_score":0.007727604,"about_ca_system_score_codex":0.00038791742,"about_ca_system_score_gemma":0.00021773762,"threshold_uncertainty_score":0.015365243},"labels":[],"label_agreement":null},{"id":"W2118422517","doi":"10.1029/2010gl046085","title":"Local electrodynamics of a solar eclipse at the magnetic equator in the early afternoon hours","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Equator; Solar eclipse; Dynamo; Equatorial electrojet; Magnetometer; Local time; Geology; Physics; Geophysics; Oscillation (cell signaling); Amplitude; Electric field; Magnetic field; Geodesy; Astronomy; Earth's magnetic field; Optics; Latitude","score_opus":0.021933897430591768,"score_gpt":0.26823841346405974,"score_spread":0.24630451603346798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118422517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764687,0.00005404696,0.000068398425,0.00002755919,0.0000026891644,0.0000025931604,0.000081244354,0.000004011634,0.002112589],"genre_scores_gemma":[0.9997639,0.000019778969,0.000014426524,0.0000029915223,0.000003410833,9.302297e-7,0.000043899767,0.0000014608659,0.00014922413],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999727,0.0000047079902,0.0000012773593,0.0000067384203,0.0000054892585,0.000009027853],"domain_scores_gemma":[0.9998354,0.000033287608,0.00003913828,0.000007423893,0.000024430848,0.00006033197],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000788039,0.000074612486,0.00014259697,0.00027418556,0.00024298324,0.00048162675,0.00009828348,0.00018369891,0.0013298335],"category_scores_gemma":[0.00038495887,0.0000744202,0.0000728262,0.00021620055,0.00016596344,0.00017555263,0.0002607964,0.00013235309,0.00018540776],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020707652,0.00016530382,0.866843,0.00007696966,0.00010458254,0.002483916,0.0027192684,0.004886582,0.09370339,0.003460038,0.0022539764,0.021232193],"study_design_scores_gemma":[0.000009752616,0.000058567846,0.99663585,0.0000045788343,0.000007031463,0.0001280764,0.00044474006,0.0016646553,0.00042083277,0.00013745965,0.00048316404,0.000005318795],"about_ca_topic_score_codex":0.002814344,"about_ca_topic_score_gemma":0.005030991,"teacher_disagreement_score":0.002814344,"about_ca_system_score_codex":0.00021852546,"about_ca_system_score_gemma":0.00007256285,"threshold_uncertainty_score":0.0055959225},"labels":[],"label_agreement":null},{"id":"W2118750130","doi":"10.1002/2015gl063538","title":"Bubbles attenuate elastic waves at seismic frequencies: First experimental evidence","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Carbon Management Canada; Kommission für Technologie und Innovation; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Attenuation; Geology; Seismic wave; Bubble; Geophysics; Seismology; Dissolution; Biosphere; Mechanics; Petrology; Physics; Optics; Chemistry","score_opus":0.09724428884038662,"score_gpt":0.31812442294213344,"score_spread":0.22088013410174684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118750130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886891,0.00043254887,0.009363384,0.00013356144,0.00001659697,0.000016171532,0.000076811855,0.00006592516,0.0012058753],"genre_scores_gemma":[0.9978948,0.0001443703,0.0015576789,0.000015168082,0.000004811035,0.00000800011,0.00004247885,0.0000069871294,0.0003258074],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998692,0.00001893841,0.000006305496,0.000019350136,0.00005526827,0.0000308425],"domain_scores_gemma":[0.9994861,0.00027460203,0.00008417487,0.000039717088,0.000082652725,0.000032716216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018196554,0.00022128111,0.00016739573,0.00012464504,0.00015310141,0.00023904716,0.00038414594,0.0003737812,0.0018896844],"category_scores_gemma":[0.00085623184,0.00017420581,0.000072596005,0.00012214617,0.0005880704,0.0004453617,0.00040238377,0.00040962527,0.00017178369],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005607806,0.0001148397,0.0028033871,0.00013098819,0.000016884376,0.00023433017,0.00012535973,0.0024786778,0.9852202,0.0009568661,0.00022524827,0.0071323616],"study_design_scores_gemma":[0.000058159003,0.00077079993,0.0073409253,0.000013128959,0.000026990972,0.00020396299,0.0001237955,0.032425366,0.9567034,0.0007501022,0.0015692633,0.000014091026],"about_ca_topic_score_codex":0.0012169327,"about_ca_topic_score_gemma":0.00090445153,"teacher_disagreement_score":0.0018896844,"about_ca_system_score_codex":0.00019090144,"about_ca_system_score_gemma":0.000093599134,"threshold_uncertainty_score":0.006321609},"labels":[],"label_agreement":null},{"id":"W2118828749","doi":"10.1029/2001gl013228","title":"Recent changes in wind chill temperatures at high latitudes in North America","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Climatology; Latitude; Wind speed; Atmospheric sciences; Air temperature; Apparent temperature; Period (music); Meteorology; Geography; Geology; Humidity","score_opus":0.027590153466301327,"score_gpt":0.26180167434323187,"score_spread":0.23421152087693053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118828749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985857,0.00029899413,0.000046628473,0.00009559689,0.000009886883,0.0000017517181,0.00019867577,0.0000034790392,0.0007592843],"genre_scores_gemma":[0.9989949,0.00032588982,0.0000756563,0.000034680816,0.0000148135405,0.0000029085588,0.00033071227,0.0000010484162,0.00021944697],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000010017629,0.000006436658,0.000021092896,0.000022428681,0.00002614343],"domain_scores_gemma":[0.9996238,0.00003328466,0.00012544976,0.0000118664475,0.00012802842,0.000077530836],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020374473,0.00009605285,0.000115972194,0.00039099113,0.00046150247,0.00037594643,0.00011588784,0.00020954138,0.0006156285],"category_scores_gemma":[0.00053758477,0.000101771715,0.000086256325,0.00055248314,0.00031224973,0.0002528657,0.0002105393,0.00023571675,0.000073257215],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009703935,0.000019437988,0.9886445,0.000039454473,0.000057082732,0.00013141875,0.000939346,0.0002687365,0.0016537117,0.000041541887,0.0005958468,0.00751193],"study_design_scores_gemma":[5.8960137e-7,0.000005256664,0.9992847,0.0000022024665,0.0000044857015,0.000018095472,0.00020394211,0.000019296544,0.000037832866,0.0000048233082,0.00041773598,0.0000010204767],"about_ca_topic_score_codex":0.1652214,"about_ca_topic_score_gemma":0.46372578,"teacher_disagreement_score":0.8347786,"about_ca_system_score_codex":0.00083375606,"about_ca_system_score_gemma":0.00040828707,"threshold_uncertainty_score":0.3285194},"labels":[],"label_agreement":null},{"id":"W2118889573","doi":"10.1029/2005gl025161","title":"Violent pyro‐convective storm devastates Australia's capital and pollutes the stratosphere","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":221,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Tornado; Stratosphere; Storm; Climatology; Headline; Meteorology; Environmental science; Precipitation; Convective storm detection; Atmospheric sciences; Geology; Geography","score_opus":0.023988468294186938,"score_gpt":0.2739675217355893,"score_spread":0.24997905344140237,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118889573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993073,0.000013300328,0.000039187355,0.000018612083,8.7596175e-7,0.0000016260994,0.000030948173,0.0000038398907,0.00058433996],"genre_scores_gemma":[0.99961096,0.000035842102,0.000071368006,0.000014313991,0.0000020060156,0.0000010091999,0.000049335606,8.4906355e-7,0.00021443106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999435,0.0000066472335,0.0000014861008,0.0000113897295,0.000016891414,0.000020128116],"domain_scores_gemma":[0.99989414,0.000007261577,0.000037607544,0.000016654603,0.000017857374,0.000026342528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009209817,0.00014125044,0.00009224274,0.00024780232,0.0006866539,0.00039102003,0.0001474537,0.00015485696,0.0004901757],"category_scores_gemma":[0.00018632523,0.00009095986,0.00008403826,0.00023257127,0.00039062582,0.00019186841,0.00048810203,0.00023610453,0.00006561144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013979903,0.000102659294,0.9306126,0.000025155176,0.000101315534,0.0010434205,0.001604897,0.0019048683,0.039614003,0.00053922005,0.0012796111,0.023032324],"study_design_scores_gemma":[0.0000023901969,0.000034274657,0.9963492,0.0000033760966,0.000008193793,0.00010508309,0.00035431318,0.00094892754,0.0012912333,0.000076462915,0.00082382874,0.0000027983244],"about_ca_topic_score_codex":0.060680926,"about_ca_topic_score_gemma":0.106685385,"teacher_disagreement_score":0.060680926,"about_ca_system_score_codex":0.00052229554,"about_ca_system_score_gemma":0.00036624496,"threshold_uncertainty_score":0.12065542},"labels":[],"label_agreement":null},{"id":"W2118943646","doi":"10.1029/2012gl053329","title":"Two distinct modes in one‐day rainfall event during MC3E field campaign: Analyses of disdrometer observations and WRF‐SBM simulation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Weather Research and Forecasting Model; Disdrometer; Environmental science; Middle latitudes; Bin; Graupel; Meteorology; Atmospheric sciences; RADIUS; Cloud physics; Convection; Climatology; Precipitation; Physics; Geology; Cloud computing; Mathematics","score_opus":0.1022679966278329,"score_gpt":0.3739133143025829,"score_spread":0.27164531767475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2118943646","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989273,0.000017209115,0.00021845264,0.000027204986,0.000005043568,0.000007781621,0.0005169312,0.000046607784,0.0002334787],"genre_scores_gemma":[0.9987993,0.000010618283,0.00020849206,0.0000072663383,0.0000047193316,0.00000731766,0.00088666216,0.000007194488,0.00006833477],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986315,0.00001609627,0.00000925212,0.000051852618,0.00002252198,0.00003702094],"domain_scores_gemma":[0.9996055,0.00012319945,0.000067879446,0.000042784253,0.000057651134,0.000102976956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003949642,0.0004357097,0.00036761214,0.00064723444,0.00030761663,0.00042369892,0.00046478884,0.0008069616,0.0006685835],"category_scores_gemma":[0.0006856426,0.00024212709,0.00057381374,0.0005197547,0.0002711766,0.00039159862,0.00022264106,0.0004088491,0.00013215924],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011437796,0.0006990787,0.7511908,0.00008483934,0.0002960306,0.0011145261,0.00032776318,0.2097435,0.017900163,0.0010318293,0.0026203468,0.013847365],"study_design_scores_gemma":[0.00006570162,0.00005819536,0.6029897,0.0000059041804,0.000039198458,0.00007241286,0.000093320195,0.39450705,0.0017530627,0.00009245438,0.00029428632,0.000028786328],"about_ca_topic_score_codex":0.038454667,"about_ca_topic_score_gemma":0.02701693,"teacher_disagreement_score":0.038454667,"about_ca_system_score_codex":0.00064756273,"about_ca_system_score_gemma":0.00033788264,"threshold_uncertainty_score":0.07646161},"labels":[],"label_agreement":null},{"id":"W2119095982","doi":"10.1029/2004gl021911","title":"An examination of historical mixed layer depths along Line P in the Gulf of Alaska","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada; University of Alberta","funders":"","keywords":"Mixed layer; Submarine pipeline; Oceanography; Climatology; Geology; Shoaling and schooling; Period (music); Environmental science","score_opus":0.0346449703395121,"score_gpt":0.28330330475269444,"score_spread":0.24865833441318233,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119095982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977174,0.00015482566,0.00016577894,0.000012166349,0.0000036230208,0.0000024869641,0.0010806136,0.00000856515,0.0008546882],"genre_scores_gemma":[0.9983687,0.000144317,0.00023027683,0.0000037299953,0.0000026551984,0.000003218046,0.0009954622,0.0000018207397,0.00024988232],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998952,0.000011833187,0.0000149020925,0.000036417438,0.000028905464,0.000012654252],"domain_scores_gemma":[0.9994506,0.00008431882,0.00016786881,0.000037648835,0.00019510298,0.00006442521],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002481617,0.0001290562,0.000088184024,0.0013225727,0.0003124332,0.00030970952,0.0001361016,0.0001804198,0.00041805973],"category_scores_gemma":[0.00080036226,0.00012348098,0.00012620135,0.001210826,0.00014471976,0.00032185973,0.00020812961,0.00012987247,0.00012078191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003070344,0.000010749949,0.9910155,0.000018178753,0.000038288712,0.00010008436,0.00026522132,0.0004690254,0.0010645079,0.00005732396,0.00013388565,0.0067966203],"study_design_scores_gemma":[4.3630808e-7,0.000012387789,0.99893564,0.0000033628205,0.000006563651,0.000044907403,0.00017474074,0.0002592218,0.00015665272,0.000011104354,0.0003933349,0.0000017708587],"about_ca_topic_score_codex":0.041520655,"about_ca_topic_score_gemma":0.08959808,"teacher_disagreement_score":0.95847934,"about_ca_system_score_codex":0.0005011103,"about_ca_system_score_gemma":0.00019066785,"threshold_uncertainty_score":0.082557976},"labels":[],"label_agreement":null},{"id":"W2119096125","doi":"10.1029/2002gl015062","title":"The arrival of a « new » Labrador Sea Water signal in the tropical Atlantic in 1996","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Centre National de la Recherche Scientifique; Institut Français de Recherche pour l'Exploitation de la Mer","keywords":"Tropical Atlantic; Climatology; Series (stratigraphy); Oceanography; Atlantic hurricane; Geology; Structural basin; Tropics; Salinity; Water mass; Environmental science; Tropical cyclone; Sea surface temperature","score_opus":0.03067245902827495,"score_gpt":0.2517600372541829,"score_spread":0.22108757822590794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119096125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991922,0.00007098047,0.000026989595,0.000052875428,0.0000024394312,0.0000022086988,0.00015730713,0.000007212875,0.00048784626],"genre_scores_gemma":[0.99913603,0.00006663599,0.00007920174,0.00003472722,0.000009588507,0.00000387144,0.00035424536,0.000002555559,0.00031317485],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998832,0.0000112400085,0.000008881578,0.00002510525,0.000026242793,0.000045353037],"domain_scores_gemma":[0.99951756,0.00004252821,0.00020964044,0.00003341992,0.00013386633,0.00006305675],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021450003,0.0001269113,0.00015126215,0.0006251211,0.00038386093,0.00068204285,0.00025769442,0.00021542665,0.00079644914],"category_scores_gemma":[0.00057959766,0.00007739804,0.00013725174,0.0005765106,0.00028524667,0.0002032858,0.0003168529,0.00019041204,0.00014328856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003765332,0.00003389164,0.9547502,0.00003995529,0.00004783085,0.00037287723,0.0009720198,0.0002971034,0.018440478,0.00016872624,0.00046028956,0.024040177],"study_design_scores_gemma":[0.0000033062483,0.000033588763,0.9979796,0.000004238167,0.000010536576,0.00006548324,0.00022120605,0.000096264775,0.00077270414,0.0000068272,0.000802805,0.0000035517514],"about_ca_topic_score_codex":0.13440321,"about_ca_topic_score_gemma":0.22145376,"teacher_disagreement_score":0.13440321,"about_ca_system_score_codex":0.001836012,"about_ca_system_score_gemma":0.00050201983,"threshold_uncertainty_score":0.26724184},"labels":[],"label_agreement":null},{"id":"W2119423854","doi":"10.1002/grl.50298","title":"Numerical simulations on megathrust rupture stabilized under strong dilatancy strengthening in slow slip region","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Slip (aerodynamics); Geology; Dilatant; Episodic tremor and slip; Subduction; Seismology; Fault (geology); Geotechnical engineering; Tectonics","score_opus":0.05449481965468384,"score_gpt":0.2987603176669797,"score_spread":0.24426549801229586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119423854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9825967,0.00026688707,0.0060863486,0.00046715813,0.000059359027,0.00003308642,0.0006679439,0.0001552839,0.009667108],"genre_scores_gemma":[0.99608314,0.000104780076,0.002393648,0.000050801536,0.000009668753,0.000034600384,0.0003206533,0.000025872314,0.0009767951],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983525,0.00004128609,0.000011215827,0.00002702263,0.000022261578,0.00006290479],"domain_scores_gemma":[0.99867415,0.00074397656,0.00020064747,0.000056798195,0.00018781617,0.00013658327],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043554627,0.000616464,0.0007623753,0.0006955028,0.0006822577,0.00080329285,0.0009371074,0.0016888855,0.0032251028],"category_scores_gemma":[0.0021334023,0.0004306357,0.00079662056,0.0006755885,0.0008411418,0.00061086327,0.00068876427,0.0008931967,0.00018778292],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006823598,0.00006665288,0.0041463342,0.000031275318,0.000024705469,0.00011427561,0.000049045568,0.9923962,0.0005880629,0.0013135556,0.0002857178,0.00091587246],"study_design_scores_gemma":[0.000019918833,0.000018308921,0.0008270742,0.0000059447343,0.0000067553024,0.0000053931417,0.00003671969,0.9985354,0.00012714088,0.0003046855,0.000108069995,0.0000045735956],"about_ca_topic_score_codex":0.0329619,"about_ca_topic_score_gemma":0.022893995,"teacher_disagreement_score":0.0329619,"about_ca_system_score_codex":0.0009765732,"about_ca_system_score_gemma":0.0009940829,"threshold_uncertainty_score":0.065540075},"labels":[],"label_agreement":null},{"id":"W2119611203","doi":"10.1029/2006gl026752","title":"Severe Arctic ozone loss in the winter 2004/2005: observations from ACE‐FTS","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; York University","funders":"","keywords":"Ozone; Atmospheric sciences; Arctic; Environmental science; Climatology; The arctic; Ozone depletion; Meteorology; Oceanography; Geology; Geography","score_opus":0.038137625279311235,"score_gpt":0.273194857780605,"score_spread":0.23505723250129373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119611203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99663687,0.00010651396,0.00021080999,0.000045157056,0.000010700129,0.000004828379,0.0021140904,0.00006477104,0.000806397],"genre_scores_gemma":[0.99371076,0.000107402186,0.0004455804,0.00003481592,0.000023667204,0.0000073068945,0.005405852,0.0000113464675,0.00025324567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982435,0.000013989768,0.000013132736,0.000033882,0.0000706348,0.00004400756],"domain_scores_gemma":[0.99972636,0.000021260446,0.00008263365,0.000029690833,0.000077419674,0.00006265585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003572612,0.00053363154,0.0005331206,0.0006896707,0.000511704,0.00074203464,0.00028557074,0.00050557556,0.00028305256],"category_scores_gemma":[0.0004271114,0.00020910149,0.00047848924,0.0007239556,0.00020894186,0.00035669253,0.00040376416,0.0003686334,0.00013067768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0024158072,0.00052286795,0.878455,0.00018024447,0.00097481156,0.0009946416,0.00066653994,0.039701693,0.041774493,0.0005145663,0.0065165837,0.027282717],"study_design_scores_gemma":[0.000024214773,0.00007840823,0.9836294,0.000008175468,0.000066796485,0.00012261231,0.00007116534,0.01043541,0.004003503,0.000041562664,0.0015008871,0.000017872844],"about_ca_topic_score_codex":0.06683574,"about_ca_topic_score_gemma":0.059059773,"teacher_disagreement_score":0.06683574,"about_ca_system_score_codex":0.000906672,"about_ca_system_score_gemma":0.00047149244,"threshold_uncertainty_score":0.13289338},"labels":[],"label_agreement":null},{"id":"W2119789633","doi":"10.1029/2012gl052348","title":"Regional biases in absolute sea‐level estimates from tide gauge data due to residual unmodeled vertical land movement","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Environment Research Council; Research Councils UK; Sight Research UK","keywords":"Tide gauge; Post-glacial rebound; Geodesy; Residual; Sea level; Geology; Global Positioning System; Climatology; Reference frame; Data set; Oceanography; Frame (networking); Statistics; Mathematics","score_opus":0.2463110660505461,"score_gpt":0.34999808751320677,"score_spread":0.10368702146266068,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119789633","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9730733,0.0005943431,0.02011336,0.00040348782,0.00007137707,0.000016719361,0.0017398405,0.00048983743,0.003497672],"genre_scores_gemma":[0.99595547,0.000088550754,0.00263424,0.00007555109,0.000010305737,0.000006978194,0.000997732,0.00009898024,0.00013212244],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9982436,0.0006324907,0.00019628489,0.00053297763,0.00029178165,0.00010297061],"domain_scores_gemma":[0.99549615,0.0016558444,0.00081429706,0.0014539213,0.0005071234,0.0000726762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005071072,0.0005194247,0.0005420088,0.0007460254,0.00030737332,0.0013724426,0.0007736219,0.00035100398,0.0008698807],"category_scores_gemma":[0.012726171,0.0004797991,0.0010741686,0.001317614,0.0005744912,0.0009899026,0.0008539712,0.00046841044,0.0005690473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026633218,0.000045141755,0.9105504,0.000120764125,0.0011261335,0.00014802512,0.00060698256,0.040138274,0.012256668,0.0011587028,0.0015463249,0.03203615],"study_design_scores_gemma":[0.00004086639,0.00007759007,0.9421713,0.00005691268,0.0003965024,0.00029393315,0.00028266115,0.04222472,0.009767657,0.0023858354,0.002248935,0.000053101292],"about_ca_topic_score_codex":0.010263811,"about_ca_topic_score_gemma":0.014262306,"teacher_disagreement_score":0.010263811,"about_ca_system_score_codex":0.0006905013,"about_ca_system_score_gemma":0.00044126261,"threshold_uncertainty_score":0.026818693},"labels":[],"label_agreement":null},{"id":"W2119899902","doi":"10.1029/2006gl027300","title":"Relationships between albedo and microwave emissions over thin newly formed sea ice during fall freeze‐up","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Albedo (alchemy); Sea ice; Environmental science; Snow; Cryosphere; Climatology; Sea ice concentration; Arctic ice pack; Ice-albedo feedback; Microwave; Atmospheric sciences; Arctic; Sea ice thickness; Geology; Meteorology; Oceanography; Geography","score_opus":0.02986922299111877,"score_gpt":0.26510883760222276,"score_spread":0.235239614611104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2119899902","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996778,0.00002241342,0.00008941298,0.000005521215,9.131981e-7,6.898791e-7,0.00006358854,0.000003142694,0.0001364003],"genre_scores_gemma":[0.9994823,0.000032285545,0.000107374806,0.0000027068186,0.0000023915056,0.0000011587904,0.00025646298,0.0000021576645,0.00011303215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997103,0.00000440111,0.0000020655125,0.0000064678297,0.000008216828,0.0000078029425],"domain_scores_gemma":[0.9997676,0.00006777602,0.000077972974,0.000012737385,0.00004524986,0.000028637969],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111642126,0.00019649528,0.000110891255,0.0002509517,0.00017289899,0.00027774958,0.000082521154,0.00010029212,0.00045445064],"category_scores_gemma":[0.00062646763,0.000113944494,0.00009591107,0.00015459847,0.000112485344,0.00015020231,0.00013455634,0.00014549404,0.00009261267],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011613137,0.000016661334,0.98581994,0.000008429634,0.00003809917,0.00006579801,0.000107743224,0.0013162979,0.009050822,0.000013942564,0.00005339738,0.0033928126],"study_design_scores_gemma":[0.0000010687406,0.000011673758,0.9987645,8.304712e-7,0.000004914135,0.000027734868,0.00004005344,0.0006170794,0.00045013652,0.000008446758,0.00007233351,0.0000011614355],"about_ca_topic_score_codex":0.0110791065,"about_ca_topic_score_gemma":0.024275888,"teacher_disagreement_score":0.0110791065,"about_ca_system_score_codex":0.00023016939,"about_ca_system_score_gemma":0.00009777571,"threshold_uncertainty_score":0.022029221},"labels":[],"label_agreement":null},{"id":"W2120181597","doi":"10.1029/2012gl051958","title":"Field information links permafrost carbon to physical vulnerabilities of thawing","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":361,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada","funders":"Vetenskapsrådet; U.S. Geological Survey; U.S. Department of Energy","keywords":"Permafrost; Environmental science; Ecosystem; Soil carbon; Soil horizon; Climate change; Atmosphere (unit); Hydrology (agriculture); Total organic carbon; Carbon fibers; Atmospheric sciences; Soil science; Soil water; Geology; Environmental chemistry; Ecology; Oceanography; Meteorology; Geography; Chemistry","score_opus":0.056164993531377175,"score_gpt":0.31550420515737115,"score_spread":0.259339211625994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120181597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6408431,0.00012299696,0.008611626,0.00020576676,0.000021647815,0.0005550984,0.30968434,0.0011918752,0.03876362],"genre_scores_gemma":[0.82564026,0.00013753328,0.01933825,0.00013501984,0.000030659827,0.0008378199,0.14589228,0.00019174366,0.007796355],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997856,0.000041486754,0.000018687813,0.000055494445,0.00006351048,0.000035158144],"domain_scores_gemma":[0.9973322,0.00078806275,0.00041797015,0.00052222086,0.00074113836,0.00019835336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00084867614,0.00023728772,0.00021954397,0.0017969598,0.0005186808,0.00033630087,0.0005298854,0.0003214384,0.014850026],"category_scores_gemma":[0.0014140637,0.00018134997,0.00019264879,0.0024468014,0.0002087897,0.00051846675,0.00025432752,0.00024348949,0.001990416],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008447514,0.0008408709,0.7498591,0.00042359094,0.000108420914,0.00045527745,0.00068410055,0.025660599,0.01599857,0.0018483545,0.045867514,0.15740879],"study_design_scores_gemma":[0.00009436934,0.00024443882,0.9151347,0.00008268987,0.000052990097,0.00015067686,0.0005260295,0.01667103,0.007943184,0.0019945817,0.057050027,0.00005526101],"about_ca_topic_score_codex":0.01735982,"about_ca_topic_score_gemma":0.06129285,"teacher_disagreement_score":0.01735982,"about_ca_system_score_codex":0.0008025974,"about_ca_system_score_gemma":0.00058022136,"threshold_uncertainty_score":0.049678266},"labels":[],"label_agreement":null},{"id":"W2120233006","doi":"10.1002/2015gl065462","title":"Sea ice convergence along the Arctic coasts of Greenland and the Canadian Arctic Archipelago: Variability and extremes (1992–2014)","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Arctic; Archipelago; Arctic ice pack; Climatology; Sea ice; Oceanography; Arctic geoengineering; Convergence (economics); Arctic dipole anomaly; Geology; Antarctic sea ice","score_opus":0.0296714913090638,"score_gpt":0.2553251478519447,"score_spread":0.22565365654288091,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120233006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927946,0.00045248086,0.000050429964,0.00010791264,0.000010855833,0.000010694901,0.0049915365,0.0000140268985,0.0015674634],"genre_scores_gemma":[0.99338067,0.0002573126,0.00014502423,0.000027749216,0.0000085310285,0.000008963474,0.005461853,0.000005594492,0.0007043857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996332,0.000017214872,0.000021056489,0.00006951641,0.00013999899,0.00011893009],"domain_scores_gemma":[0.9985091,0.00005183576,0.0001844719,0.000040622,0.000936037,0.00027779985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006852866,0.00035689186,0.00030796672,0.0033997644,0.0013838368,0.0011241613,0.000534129,0.0002858039,0.00071401475],"category_scores_gemma":[0.0010180649,0.00015990644,0.00035474636,0.005057008,0.00060021394,0.00032818574,0.0008029439,0.0003277536,0.0001471033],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014478351,0.000029240618,0.9872486,0.000032919692,0.0001692126,0.00009001404,0.0005016478,0.0007573269,0.0007512381,0.00015485659,0.0020572473,0.008063007],"study_design_scores_gemma":[0.0000016290534,0.000004081944,0.9988709,0.000006495125,0.0000076280608,0.000011420866,0.0001685923,0.00019072901,0.000043298336,0.000007929085,0.00068366586,0.000003701813],"about_ca_topic_score_codex":0.96551526,"about_ca_topic_score_gemma":0.9853457,"teacher_disagreement_score":0.034484744,"about_ca_system_score_codex":0.009740615,"about_ca_system_score_gemma":0.010163977,"threshold_uncertainty_score":0.070673466},"labels":[],"label_agreement":null},{"id":"W2120254366","doi":"10.1002/2013gl059079","title":"The implication of radiative forcing and feedback for meridional energy transport","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Equator; Cloud forcing; Cloud feedback; Radiative forcing; Zonal and meridional; Atmospheric sciences; Environmental science; Forcing (mathematics); Shortwave; Longwave; Shortwave radiation; Climatology; Radiative equilibrium; Albedo (alchemy); Northern Hemisphere; Radiative transfer; Latitude; Coupled model intercomparison project; Climate model; Geology; Physics; Climate sensitivity; Aerosol; Radiation; Climate change; Meteorology","score_opus":0.019851000938870784,"score_gpt":0.26996060061222565,"score_spread":0.2501095996733549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120254366","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99337995,0.00028501183,0.0022641423,0.0004432495,0.0000400383,0.000011061736,0.00073954294,0.00011623803,0.002720742],"genre_scores_gemma":[0.99935585,0.000044512697,0.0002460461,0.000022378932,0.0000073932574,0.0000028854229,0.00010191041,0.000008749903,0.0002102275],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982494,0.000051994935,0.000012396512,0.000043332664,0.000034247885,0.00003312705],"domain_scores_gemma":[0.9992341,0.00036473013,0.00009583007,0.00007532951,0.0001656547,0.000064454995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000784918,0.00032144942,0.00021191628,0.0004773624,0.00028521483,0.0006480878,0.00037654885,0.0002930368,0.0022355278],"category_scores_gemma":[0.0020466344,0.00018555684,0.000333673,0.00025852892,0.00033059806,0.0006335564,0.00024713363,0.00022893169,0.00011935454],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00181873,0.00027235548,0.5876759,0.00030553841,0.0004742966,0.0004490991,0.00018980795,0.18349159,0.17527114,0.012230585,0.0017082194,0.036112733],"study_design_scores_gemma":[0.00012294242,0.00012916957,0.7695024,0.000031158408,0.00009583554,0.00008876805,0.000105507395,0.21284093,0.011028363,0.004336464,0.0016774599,0.000041008505],"about_ca_topic_score_codex":0.010467298,"about_ca_topic_score_gemma":0.0072324523,"teacher_disagreement_score":0.010467298,"about_ca_system_score_codex":0.0010798351,"about_ca_system_score_gemma":0.00035310467,"threshold_uncertainty_score":0.02081275},"labels":[],"label_agreement":null},{"id":"W2120514973","doi":"10.1029/2005gl023089","title":"Reply to comment by von Storch and Zorita on “Hockey sticks, principal components, and spurious significance”","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Spurious relationship; Principal component analysis; Geology; Mathematics; Statistics","score_opus":0.039132141997958454,"score_gpt":0.29968409170986376,"score_spread":0.2605519497119053,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120514973","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00019542284,0.0013971836,0.00025946315,0.9783839,0.019213213,0.000007659011,0.00012134022,0.00005375184,0.00036799195],"genre_scores_gemma":[0.0016640807,0.0006204658,0.0002980772,0.97444975,0.021881204,0.00003624739,0.000034766945,0.00006881768,0.00094675727],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99142915,0.0026424457,0.0011659089,0.0019240415,0.0022616058,0.0005767728],"domain_scores_gemma":[0.9487934,0.03275715,0.002768196,0.0020787644,0.010990712,0.0026116897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.01685813,0.0018252853,0.0026998278,0.0016346812,0.006018319,0.005265633,0.0075506247,0.047040906,0.0077278516],"category_scores_gemma":[0.0903889,0.0015852208,0.002185051,0.002013201,0.01309479,0.012860455,0.005121248,0.07102942,0.008508398],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027662983,0.000009749622,0.00021289029,0.00005215748,0.000015274487,0.000089262554,0.00029247277,0.00006404738,0.000055671022,0.0025486124,0.99446917,0.002162943],"study_design_scores_gemma":[0.00015047188,0.0000498796,0.0018192581,0.0006558414,0.00005319544,0.00051612343,0.0013956559,0.0006527482,0.0006698758,0.024119291,0.9696453,0.0002724],"about_ca_topic_score_codex":0.016483845,"about_ca_topic_score_gemma":0.015592472,"teacher_disagreement_score":0.047040906,"about_ca_system_score_codex":0.0045355414,"about_ca_system_score_gemma":0.007016794,"threshold_uncertainty_score":0.089155376},"labels":[],"label_agreement":null},{"id":"W2120547066","doi":"10.1002/2013gl057623","title":"Adjoint estimation of ozone climate penalties","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"","keywords":"Estimation; Environmental science; Ozone; Meteorology; Atmospheric sciences; Climatology; Geology; Geography; Economics","score_opus":0.028161845027426986,"score_gpt":0.27610353020291717,"score_spread":0.24794168517549017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2120547066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84760845,0.00004788699,0.1487332,0.00021050654,0.000049936116,0.000030883097,0.00031759843,0.00053380313,0.0024678186],"genre_scores_gemma":[0.9945831,0.0000049591276,0.0051180287,0.00001422721,0.0000044676203,0.00000803694,0.00008726925,0.000010662905,0.00016922232],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998136,0.000069478316,0.00000858074,0.000033306223,0.000038657345,0.000036463018],"domain_scores_gemma":[0.9990876,0.00048019827,0.00011213518,0.00006459236,0.00017810758,0.000077371835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007777706,0.00031488616,0.0004695439,0.00037181162,0.0002843387,0.00064568646,0.00042924285,0.0007157523,0.00078950514],"category_scores_gemma":[0.0028164939,0.00030878405,0.0004613406,0.00021125434,0.00039285942,0.00040688232,0.00059736724,0.0009349617,0.000070296155],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061771105,0.00003365134,0.0035801413,0.0000054159223,0.000019890811,0.000020322426,0.0000078361445,0.9912513,0.0013627766,0.001072927,0.00011451635,0.0024693308],"study_design_scores_gemma":[0.00000351861,0.0000061884944,0.0003096776,4.6223147e-7,0.0000013048616,0.0000011560885,0.0000018911335,0.9992632,0.00018964126,0.00020108734,0.00001970892,0.0000022040854],"about_ca_topic_score_codex":0.022670193,"about_ca_topic_score_gemma":0.008665448,"teacher_disagreement_score":0.022670193,"about_ca_system_score_codex":0.00071842264,"about_ca_system_score_gemma":0.0013376634,"threshold_uncertainty_score":0.04507643},"labels":[],"label_agreement":null},{"id":"W2121491416","doi":"10.1029/2000gl011969","title":"Width and structure of mesoscale optical auroral arcs","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"","keywords":"Zenith; Mesoscale meteorology; Arc (geometry); Amplitude; Physics; Standard deviation; Cutoff; Gaussian; Sky; Optics; Geology; Astrophysics; Geometry; Meteorology; Mathematics","score_opus":0.01274710819894813,"score_gpt":0.28198596306373547,"score_spread":0.2692388548647873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121491416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99765056,0.00008001833,0.00058310566,0.000009856048,8.6187976e-7,0.0000024352262,0.000575015,0.000027855287,0.0010703251],"genre_scores_gemma":[0.99855596,0.000032079686,0.0005000446,0.0000015930478,0.0000015306421,0.0000028804943,0.0006771303,0.000009673015,0.00021917805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.000004207978,0.000004059242,0.00002384928,0.000014221117,0.000016289903],"domain_scores_gemma":[0.9994174,0.000115840034,0.00018652261,0.000057561512,0.00015657202,0.000066067776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012340023,0.00011237224,0.00006464649,0.0012607708,0.00017379783,0.00036035033,0.00015236797,0.000090404275,0.0008686256],"category_scores_gemma":[0.0008157425,0.00012165819,0.00013461652,0.00097386335,0.00016099805,0.0002540527,0.00022424075,0.00013495133,0.0001409304],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012867576,0.000017692168,0.9540075,0.0000366179,0.00007032665,0.00007378376,0.0002971646,0.003551035,0.01576174,0.0006279951,0.000315196,0.025112228],"study_design_scores_gemma":[0.0000014276794,0.0000061418045,0.9965642,0.0000016690818,0.000007202059,0.000043835164,0.00005779938,0.0016406535,0.001186821,0.00008116245,0.000406177,0.0000028232382],"about_ca_topic_score_codex":0.009092054,"about_ca_topic_score_gemma":0.015204742,"teacher_disagreement_score":0.009092054,"about_ca_system_score_codex":0.0004248099,"about_ca_system_score_gemma":0.00016261711,"threshold_uncertainty_score":0.018078268},"labels":[],"label_agreement":null},{"id":"W2121744614","doi":"10.1002/2014gl060984","title":"Charcoal dispersion and deposition in boreal lakes from 3 years of monitoring: Differences between local and regional fires","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec en Abitibi-Témiscamingue; Université du Québec à Montréal; Natural Sciences and Engineering Research Council of Canada","funders":"Canadian Forest Service; Université du Québec à Montréal; U.S. Forest Service; Centre National de la Recherche Scientifique; Natural Resources Canada; Université du Québec à Chicoutimi","keywords":"Charcoal; Deposition (geology); Environmental science; Boreal; Taiga; Sediment; Watershed; Dispersion (optics); Physical geography; Atmospheric sciences; Hydrology (agriculture); Geology; Geography; Forestry; Geomorphology; Chemistry; Paleontology; Physics","score_opus":0.021267084059885245,"score_gpt":0.26687346329735073,"score_spread":0.24560637923746548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2121744614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999681,0.00004167115,0.00003321382,0.0000043207815,7.127117e-7,0.0000018249162,0.0001233188,0.0000016600623,0.000112220514],"genre_scores_gemma":[0.9995297,0.000024138792,0.000076557975,0.000005244312,0.0000016372042,0.000003139218,0.00026320058,0.0000010461561,0.00009527904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999793,0.000031794913,0.000013696488,0.000054844975,0.000055137712,0.000051458344],"domain_scores_gemma":[0.9991147,0.00010355948,0.00031443287,0.000042858912,0.00025989258,0.00016461933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053329265,0.00020540114,0.00020652424,0.00068078854,0.0005628451,0.00057504454,0.00028863671,0.0002555616,0.00033458692],"category_scores_gemma":[0.0010167888,0.0001668054,0.0001928938,0.0005993407,0.00034227435,0.00028844745,0.00034271434,0.00021704243,0.00006204588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011573308,0.000014599432,0.997054,0.000004427605,0.00003654788,0.000028822531,0.00024638328,0.00006804012,0.0011730151,0.0000045395714,0.0000339114,0.0012200098],"study_design_scores_gemma":[5.2586216e-7,0.000007967168,0.9997564,7.955843e-7,0.000004258929,0.000011492761,0.00008510145,0.000049955714,0.000057130976,9.68594e-7,0.000024426403,9.2268715e-7],"about_ca_topic_score_codex":0.24570654,"about_ca_topic_score_gemma":0.5179606,"teacher_disagreement_score":0.24570654,"about_ca_system_score_codex":0.0010877718,"about_ca_system_score_gemma":0.00051898765,"threshold_uncertainty_score":0.48855275},"labels":[],"label_agreement":null},{"id":"W2122119847","doi":"10.1029/2006gl026604","title":"Changes in the leading ENSO modes associated with the late 1970s climate shift: Role of surface zonal current","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Korea Science and Engineering Foundation","keywords":"Climatology; El Niño Southern Oscillation; Mode (computer interface); Oscillation (cell signaling); Geology; Sea surface temperature; Structural basin; Current (fluid); Oceanography","score_opus":0.03734991635977392,"score_gpt":0.2989910062958588,"score_spread":0.26164108993608487,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122119847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99622726,0.0001235276,0.0011544656,0.00010921044,0.000015872523,0.0000049146734,0.00010078299,0.000026622498,0.0022372792],"genre_scores_gemma":[0.998899,0.000099594705,0.00029906197,0.000013939653,0.0000111752615,0.0000020062275,0.000072300834,0.0000045627908,0.00059826765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999703,0.0000028883976,0.0000017827414,0.000008384224,0.0000068065046,0.000009831699],"domain_scores_gemma":[0.99987185,0.000021416989,0.000034957357,0.000008556397,0.000037438836,0.000025793104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011055012,0.00014556093,0.0000804595,0.00034521832,0.00018247376,0.0003364086,0.00006261979,0.00010928305,0.001103733],"category_scores_gemma":[0.00071743847,0.000071007686,0.00012775601,0.00028990617,0.00023092798,0.00029640328,0.00024584885,0.00025314477,0.00014245466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055613637,0.00016136067,0.7678984,0.00009993394,0.000087421424,0.0005908827,0.0014304941,0.016545743,0.10212694,0.009147726,0.0015857845,0.099769205],"study_design_scores_gemma":[0.0000050882604,0.000027478744,0.98568994,0.000006185811,0.0000114705645,0.00008652654,0.00021321804,0.00856791,0.0023063943,0.0012954547,0.0017774408,0.000012868348],"about_ca_topic_score_codex":0.0077639003,"about_ca_topic_score_gemma":0.011346887,"teacher_disagreement_score":0.0077639003,"about_ca_system_score_codex":0.00033043267,"about_ca_system_score_gemma":0.00025754387,"threshold_uncertainty_score":0.015437424},"labels":[],"label_agreement":null},{"id":"W2122123598","doi":"10.1029/2002gl016364","title":"Polar cap observations of mesospheric and lower thermospheric 4‐hour waves in temperature","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Airglow; Oscillation (cell signaling); Rotational temperature; Atmospheric sciences; Wavelength; Gravity wave; Latitude; Wavenumber; Physics; Thermosphere; Gravitational wave; Mesosphere; Geology; Geodesy; Geophysics; Astrophysics; Ionosphere; Stratosphere; Chemistry; Spectral line; Astronomy; Optics","score_opus":0.016252862012963054,"score_gpt":0.2642833848888256,"score_spread":0.24803052287586252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122123598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99034435,0.0001529773,0.00047654376,0.000039835213,0.000023193545,0.000014488785,0.002483641,0.00007135583,0.006393661],"genre_scores_gemma":[0.991784,0.00012707012,0.0011996311,0.000044353874,0.00002923429,0.000016961983,0.005668521,0.00001593513,0.0011143398],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986947,0.000011710046,0.0000039364495,0.000030014591,0.000040592815,0.000044226224],"domain_scores_gemma":[0.99971634,0.000027200966,0.00006083376,0.000027318472,0.00010709178,0.00006119447],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015325184,0.00028679447,0.00021138029,0.0007327222,0.00044264,0.0005721257,0.00017878368,0.00029686396,0.0012782856],"category_scores_gemma":[0.00028998937,0.00020779512,0.00015740925,0.0008793151,0.00022156737,0.00023737714,0.00035246214,0.00033202957,0.00049685244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002118115,0.00017046707,0.69986326,0.00012997388,0.00013470481,0.00027275266,0.0010132517,0.0017007162,0.2513682,0.00034235767,0.0027289044,0.040157273],"study_design_scores_gemma":[0.000018943998,0.000049053884,0.99232787,0.000004208174,0.000020848118,0.000053633037,0.00007071571,0.0010315913,0.004938295,0.000031178733,0.0014433828,0.00001018706],"about_ca_topic_score_codex":0.030629538,"about_ca_topic_score_gemma":0.064072564,"teacher_disagreement_score":0.030629538,"about_ca_system_score_codex":0.00041137842,"about_ca_system_score_gemma":0.00029876575,"threshold_uncertainty_score":0.060902536},"labels":[],"label_agreement":null},{"id":"W2122224298","doi":"10.1029/2003gl017892","title":"Limestones distinguished by magnetic hysteresis in three‐dimensional projections","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"Natural Sciences and Engineering Research Council of Canada; Lakehead University","keywords":"Hysteresis; Geology; Projection (relational algebra); Paleomagnetism; Magnetic hysteresis; Plane (geometry); Space (punctuation); Orientation (vector space); Rock magnetism; Magnetite; Geometry; Sedimentary depositional environment; Remanence; Mineralogy; Physics; Paleontology; Mathematics; Magnetization; Condensed matter physics; Magnetic field; Computer science","score_opus":0.02256494103233131,"score_gpt":0.2925646079872667,"score_spread":0.2699996669549354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122224298","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.992155,0.00024196348,0.004882128,0.00006243112,0.000012800551,0.000011734892,0.00018364724,0.00011770113,0.0023325658],"genre_scores_gemma":[0.9856289,0.00034963808,0.01202328,0.000036801568,0.00000810162,0.000020906544,0.00049431965,0.00002851395,0.0014094528],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999043,0.000012153151,0.000010445466,0.000021335121,0.000028975526,0.000022773796],"domain_scores_gemma":[0.9997731,0.000051658226,0.000064231725,0.000035794757,0.000033288805,0.000041958727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017698124,0.0003091593,0.00024566584,0.0009348718,0.00026242316,0.0010632216,0.00021362037,0.0003294588,0.0018739073],"category_scores_gemma":[0.00041786113,0.00029078755,0.00022687716,0.0004853302,0.00042613634,0.000306765,0.00058934273,0.0004555961,0.00041932537],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002939852,0.000035367375,0.009118414,0.00007473804,0.000024512286,0.0006059191,0.00023560031,0.00049973023,0.9782566,0.0009730403,0.00013903854,0.009743115],"study_design_scores_gemma":[0.000033394237,0.00019635813,0.21678518,0.000024659581,0.000053496682,0.0041917986,0.0005925251,0.0047877072,0.7655896,0.0012161492,0.0064788796,0.000050315713],"about_ca_topic_score_codex":0.0008694436,"about_ca_topic_score_gemma":0.0013720961,"teacher_disagreement_score":0.0018739073,"about_ca_system_score_codex":0.00017047033,"about_ca_system_score_gemma":0.00020637721,"threshold_uncertainty_score":0.006268859},"labels":[],"label_agreement":null},{"id":"W2122928827","doi":"10.1029/2001gl014140","title":"Localization of abrupt change in the North Atlantic thermohaline circulation","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Thermohaline circulation; Shutdown of thermohaline circulation; Atlantic Equatorial mode; North Atlantic Deep Water; Atlantic multidecadal oscillation; Climatology; Oceanography; Atlantic hurricane; Geology; Ocean current; Forcing (mathematics); Northern Hemisphere; Climate change; Abrupt climate change; North Atlantic oscillation; Environmental science; Global warming; Effects of global warming","score_opus":0.08384465761773327,"score_gpt":0.3041230816289049,"score_spread":0.22027842401117162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2122928827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983822,0.000059462294,0.00052961585,0.00006977531,0.000004497123,0.0000017731653,0.0000637722,0.000045141715,0.0008436559],"genre_scores_gemma":[0.99970764,0.000033860277,0.00009325917,0.000008838813,0.0000038753697,0.0000011709328,0.00005101971,0.0000028245506,0.000097405464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999578,0.000005267223,0.0000018789641,0.000014046571,0.0000062568615,0.000014735104],"domain_scores_gemma":[0.9998288,0.000038909,0.00005004421,0.00002466458,0.000020346271,0.00003714362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008242993,0.00007841246,0.00011615137,0.00025142496,0.00015264573,0.00026190726,0.00010875723,0.00018080091,0.0011497637],"category_scores_gemma":[0.00064311596,0.00012311204,0.00016254178,0.00013839878,0.00026755678,0.00019156624,0.00032440398,0.00024467494,0.00012412459],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006821511,0.00011119987,0.6444293,0.00012058045,0.000209023,0.00083559536,0.00069532247,0.036208574,0.27015626,0.0035387527,0.0011365856,0.04187666],"study_design_scores_gemma":[0.000019591353,0.00005726309,0.9750568,0.000008075516,0.000028248323,0.00012782602,0.000099759316,0.01981307,0.0033096971,0.00072370836,0.00074151845,0.000014486262],"about_ca_topic_score_codex":0.005440599,"about_ca_topic_score_gemma":0.0066344095,"teacher_disagreement_score":0.005440599,"about_ca_system_score_codex":0.00033804646,"about_ca_system_score_gemma":0.0001741804,"threshold_uncertainty_score":0.010817826},"labels":[],"label_agreement":null},{"id":"W2123125910","doi":"10.1002/2015gl063494","title":"Rapid injection of near‐inertial shear into the stratified upper ocean at an Antarctic Circumpolar Current front","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Geology; Storm; Circumpolar star; Stratification (seeds); Inertial wave; Mixed layer; Turbulence; Current (fluid); Oceanography; Front (military); Wind shear; Ocean current; Climatology; Meteorology; Wind speed; Physics","score_opus":0.04069981199135304,"score_gpt":0.2890802878155689,"score_spread":0.24838047582421585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123125910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987463,0.000062607556,0.00008765085,0.00001950104,0.0000048354436,0.0000066389966,0.000048435224,0.000013817736,0.0010102009],"genre_scores_gemma":[0.99946636,0.000062130515,0.000091894864,0.000016573722,0.0000064241817,0.0000036602523,0.00005347971,0.0000019336833,0.0002975472],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999542,0.0000050128465,0.000002235027,0.000006054587,0.000017382034,0.000015032984],"domain_scores_gemma":[0.9998859,0.000014708367,0.000032725093,0.0000083935965,0.000019204452,0.00003897094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010009808,0.00016483628,0.00016372366,0.00039637185,0.00031505703,0.0004417548,0.00009156557,0.00019314777,0.00081355416],"category_scores_gemma":[0.00018145322,0.00013258147,0.00013872882,0.0002077353,0.000232953,0.00017270523,0.00035675,0.00029341507,0.00021658081],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015048847,0.00018020277,0.26181856,0.00008227357,0.00008223732,0.0030278822,0.00094758725,0.0016105532,0.7122834,0.0007529304,0.00060393394,0.01710554],"study_design_scores_gemma":[0.000032932912,0.0004586469,0.9693638,0.000014934717,0.000024726045,0.00029157597,0.00041823706,0.0017028112,0.026417619,0.00011105015,0.0011502535,0.000013364956],"about_ca_topic_score_codex":0.0051300526,"about_ca_topic_score_gemma":0.0048629222,"teacher_disagreement_score":0.0051300526,"about_ca_system_score_codex":0.00038439705,"about_ca_system_score_gemma":0.00019305185,"threshold_uncertainty_score":0.010200381},"labels":[],"label_agreement":null},{"id":"W2123494392","doi":"10.1029/2004gl021315","title":"Heavy ion mass loading of the geomagnetic field near the plasmapause and ULF wave implications","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Plasmasphere; Ion; Physics; Earth's magnetic field; Magnetosphere; Atomic physics; Field line; Discontinuity (linguistics); Geophysics; Electron; Magnetic field; Plasma; Electron density; Computational physics; Ionosphere; Nuclear physics","score_opus":0.017004670587184557,"score_gpt":0.2710724709743376,"score_spread":0.25406780038715304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123494392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99595886,0.000048685553,0.00076380465,0.000040695762,0.0000031175916,0.0000046318914,0.00010050939,0.000031057527,0.003048655],"genre_scores_gemma":[0.99933857,0.000019430418,0.00022226674,0.000006881402,0.0000021477738,0.0000030363137,0.00006285346,0.00000788394,0.00033686234],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000008082831,0.0000024789488,0.000012191135,0.000018687664,0.000020554668],"domain_scores_gemma":[0.9998561,0.000038491376,0.000037848757,0.00001555489,0.00003320611,0.000018671994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010863337,0.000159281,0.00013685628,0.00035550605,0.00026619754,0.00033804518,0.00018512546,0.00020168627,0.0011310601],"category_scores_gemma":[0.0006916259,0.00013853477,0.00009879089,0.00021633727,0.00020873516,0.0003285332,0.00038805298,0.00015405694,0.00018203669],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012021635,0.00006179712,0.36810017,0.000078967016,0.00004898369,0.0012181301,0.0006603689,0.014892824,0.56811196,0.0026628189,0.0010326055,0.041929238],"study_design_scores_gemma":[0.000026435375,0.00017991781,0.91294,0.000015879683,0.000021255808,0.00051389245,0.0004118366,0.026947347,0.05581974,0.0011483753,0.0019550067,0.000020259507],"about_ca_topic_score_codex":0.003196168,"about_ca_topic_score_gemma":0.001821066,"teacher_disagreement_score":0.003196168,"about_ca_system_score_codex":0.0002267885,"about_ca_system_score_gemma":0.00009461966,"threshold_uncertainty_score":0.0063551664},"labels":[],"label_agreement":null},{"id":"W2123788505","doi":"10.1029/2008gl035389","title":"A multi‐model study of the hemispheric transport and deposition of oxidised nitrogen","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Environment Research Council; Sight Research UK; Department for Environment, Food and Rural Affairs, UK Government; Lawrence Livermore National Laboratory; U.S. Department of Energy","keywords":"East Asia; Far East; Geography; Nitrogen; Deposition (geology); Climatology; Geology; China; Chemistry; Archaeology; Geomorphology; Structural basin","score_opus":0.03778331100933705,"score_gpt":0.2641070355455095,"score_spread":0.22632372453617247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2123788505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99297696,0.00017181267,0.0024966826,0.0003107496,0.000031346968,0.000031540774,0.0012185435,0.000092262235,0.0026700082],"genre_scores_gemma":[0.99499184,0.00013004553,0.0024309857,0.00004622223,0.000024863904,0.000054717104,0.0008652064,0.000035504123,0.0014205172],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99973935,0.00010410871,0.0000130984,0.000051881318,0.000029627237,0.00006185685],"domain_scores_gemma":[0.99869066,0.000843855,0.000105771236,0.0000971847,0.00012577127,0.00013688624],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011499894,0.001124825,0.00082916644,0.0006853013,0.0011614292,0.0011125263,0.0014126357,0.0021181009,0.0015186425],"category_scores_gemma":[0.0015598951,0.00062726456,0.001828184,0.0008958149,0.0005679698,0.001045338,0.0006685191,0.00106613,0.0001969815],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029810442,0.00021039956,0.01360406,0.0000364597,0.0002442622,0.00018312146,0.00005481826,0.9796265,0.0017456193,0.0013532465,0.00061338855,0.0020299423],"study_design_scores_gemma":[0.000087053486,0.00008667864,0.006766111,0.0000037067252,0.0000474184,0.000021445834,0.00004946011,0.99169755,0.00049371895,0.00036650608,0.00036137842,0.000019002691],"about_ca_topic_score_codex":0.12164023,"about_ca_topic_score_gemma":0.056785583,"teacher_disagreement_score":0.12164023,"about_ca_system_score_codex":0.0031141068,"about_ca_system_score_gemma":0.0014232051,"threshold_uncertainty_score":0.24186444},"labels":[],"label_agreement":null},{"id":"W2124108257","doi":"10.1002/2015gl063750","title":"Joint analysis of the 2014 Kangding, southwest China, earthquake sequence with seismicity relocation and InSAR inversion","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Seismology; Aftershock; Geology; Interferometric synthetic aperture radar; Seismic moment; Seismic gap; Hypocenter; Slip (aerodynamics); Moment magnitude scale; Induced seismicity; Geodesy; Fault (geology); Synthetic aperture radar; Scaling; Remote sensing","score_opus":0.062441935785573444,"score_gpt":0.2755993013895912,"score_spread":0.21315736560401777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124108257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982126,0.000057219502,0.00030274945,0.00001935003,0.000006993281,0.000005973057,0.0011021269,0.000023174309,0.0002699284],"genre_scores_gemma":[0.9942386,0.000041865766,0.0004247164,0.000010822601,0.000010239239,0.00000720555,0.0046957918,0.0000060726716,0.00056464534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998266,0.00001709562,0.000017606746,0.00005370131,0.0000439158,0.0000411216],"domain_scores_gemma":[0.9995901,0.000032586217,0.0001196357,0.00006207909,0.00011132955,0.000084270774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041372763,0.0004055709,0.00033396643,0.0013261474,0.00027555824,0.00031139178,0.00021521829,0.00018384031,0.0008402157],"category_scores_gemma":[0.00052266655,0.00018841027,0.00033681662,0.0018926268,0.00020211826,0.00019403471,0.0003278902,0.00016669331,0.00025930506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025423983,0.0000926335,0.9578298,0.000055605626,0.00024382946,0.00063800946,0.00025998792,0.007341228,0.011307602,0.0001634429,0.0014739605,0.020339753],"study_design_scores_gemma":[0.000007924774,0.000027270848,0.992767,0.000003507246,0.000052954176,0.00004615949,0.00012331051,0.0056600417,0.00059142715,0.000022561137,0.00068823894,0.0000096231015],"about_ca_topic_score_codex":0.0351582,"about_ca_topic_score_gemma":0.0656142,"teacher_disagreement_score":0.0351582,"about_ca_system_score_codex":0.00044684537,"about_ca_system_score_gemma":0.0007856787,"threshold_uncertainty_score":0.06990707},"labels":[],"label_agreement":null},{"id":"W2124120791","doi":"10.1029/2007gl032137","title":"Tropical tape recorder observed in HCN","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Waterloo","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Mixing ratio; Stratosphere; Atmospheric sciences; Environmental science; Mixing (physics); Climatology; Microwave Limb Sounder; Annual cycle; Meteorology; Satellite; Geology; Physics; Astronomy","score_opus":0.0757119416958622,"score_gpt":0.28926188834593847,"score_spread":0.21354994665007626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124120791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9769026,0.0004037445,0.0007464304,0.000090407484,0.00004966362,0.00002034893,0.006711063,0.000120511875,0.014955284],"genre_scores_gemma":[0.99592376,0.00015583048,0.00047992344,0.00005772468,0.000038958544,0.0000115325665,0.0021039895,0.000011957437,0.0012163],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999811,0.000013222264,0.000010953668,0.000054341766,0.000080458885,0.000030079656],"domain_scores_gemma":[0.99923086,0.00007075868,0.00024639218,0.00009326457,0.00024409711,0.000114694194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001475603,0.00012477835,0.00013715177,0.0005208466,0.00035178286,0.00027677996,0.00017448426,0.00015041645,0.002021044],"category_scores_gemma":[0.0007857561,0.00006886386,0.000053595955,0.0007802485,0.00015361307,0.00019292875,0.00033070272,0.00018850047,0.00037579614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005036957,0.00005391961,0.844531,0.00013293812,0.00009305445,0.00075598067,0.0010562008,0.00040735063,0.10453285,0.0004043215,0.0059495075,0.041579127],"study_design_scores_gemma":[0.000003903386,0.000020832706,0.99042517,0.000008793759,0.000011763746,0.0003243721,0.00013634458,0.00022264595,0.004740872,0.000026768865,0.0040734718,0.0000051610514],"about_ca_topic_score_codex":0.0097867865,"about_ca_topic_score_gemma":0.013544975,"teacher_disagreement_score":0.0097867865,"about_ca_system_score_codex":0.00026826435,"about_ca_system_score_gemma":0.00017379718,"threshold_uncertainty_score":0.019459665},"labels":[],"label_agreement":null},{"id":"W2124268981","doi":"10.1029/2008gl036876","title":"A new framework for estimating englacial water content and pore geometry using combined radar and seismic wave velocities","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Glacier; Liquid water content; Radar; Water content; Mixing (physics); Liquid water; Inclusion (mineral); Geophysics; Mineralogy; Geomorphology; Geometry; Geotechnical engineering; Earth science; Law","score_opus":0.09376904094949277,"score_gpt":0.30247018192091907,"score_spread":0.20870114097142628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124268981","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0017982189,0.00004162,0.99783903,0.000019282912,0.000006228005,0.000007774931,0.000034754223,0.00008316148,0.00016999697],"genre_scores_gemma":[0.13767585,0.00031341187,0.8601142,0.000044064847,0.00007904685,0.00015875476,0.00029484186,0.000100440106,0.0012193103],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99950767,0.000110161396,0.000033799795,0.00014210229,0.00016065668,0.000045578992],"domain_scores_gemma":[0.9993175,0.0003128395,0.000081404774,0.000089086316,0.00016316619,0.00003594956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001165872,0.000764134,0.0008530233,0.0013857373,0.0005794736,0.0015027504,0.0018829519,0.0009056773,0.00096123305],"category_scores_gemma":[0.0034248126,0.00056128425,0.0009049045,0.00091582705,0.00089094165,0.0017424137,0.0012853465,0.000943204,0.00033706124],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003502853,0.000077825294,0.0023464968,0.000074669966,0.00009912789,0.00011975935,0.00008826485,0.8173503,0.013300411,0.07474279,0.0008219205,0.090943426],"study_design_scores_gemma":[0.000004254554,0.0000125143015,0.00031370367,0.0000055352743,0.000009653156,0.000030105455,0.000009787186,0.98507756,0.0007638427,0.012724504,0.0010362128,0.0000123562795],"about_ca_topic_score_codex":0.0119506875,"about_ca_topic_score_gemma":0.01024645,"teacher_disagreement_score":0.0119506875,"about_ca_system_score_codex":0.0006705604,"about_ca_system_score_gemma":0.0013590474,"threshold_uncertainty_score":0.023762286},"labels":[],"label_agreement":null},{"id":"W2124343231","doi":"10.1029/2003gl018541","title":"Possible emplacement of crustal rocks into the forearc mantle of the Cascadia Subduction Zone","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"","keywords":"Geology; Forearc; Subduction; Mantle (geology); Mantle wedge; Oceanic crust; Crust; Transition zone; Seismology; Crustal recycling; Continental crust; Geophysics; Geochemistry; Petrology; Tectonics","score_opus":0.030598301204228504,"score_gpt":0.2792226327507885,"score_spread":0.24862433154656,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124343231","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99680126,0.00044453613,0.00020417501,0.00016363,0.0000039014135,0.0000037771117,0.00009012022,0.000034459234,0.0022540966],"genre_scores_gemma":[0.99825794,0.0003513338,0.00027012196,0.000023033375,0.000004609272,0.0000034634268,0.00019884083,0.0000059104973,0.000884644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998398,0.000016822758,0.000010168431,0.000037877857,0.000040797222,0.000054604745],"domain_scores_gemma":[0.9995409,0.000056892615,0.00014292971,0.000080567435,0.000105747065,0.000072917086],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036236268,0.0004154215,0.00024320548,0.0012632302,0.000806648,0.0007224325,0.000493837,0.0006239741,0.0018130057],"category_scores_gemma":[0.0012096622,0.0005124296,0.00033380918,0.0011123752,0.0007126158,0.0006117092,0.0012637086,0.0004453432,0.00027152896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000587294,0.000036008903,0.8794576,0.00019975424,0.00014473373,0.0039561396,0.006222045,0.0023117303,0.07891093,0.0014480455,0.00035587503,0.02636984],"study_design_scores_gemma":[0.000010099212,0.000037349295,0.9948014,0.000019390294,0.00003331493,0.00033511844,0.00070536486,0.00033272276,0.0017026429,0.00019898349,0.0018150078,0.000008529926],"about_ca_topic_score_codex":0.032343954,"about_ca_topic_score_gemma":0.039575275,"teacher_disagreement_score":0.967656,"about_ca_system_score_codex":0.00097510184,"about_ca_system_score_gemma":0.0006348653,"threshold_uncertainty_score":0.064311385},"labels":[],"label_agreement":null},{"id":"W2124949732","doi":"10.1029/2003gl016954","title":"Worldwide trend of atmospheric mercury since 1977","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":217,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Deutsche Forschungsgemeinschaft","keywords":"Mercury (programming language); Environmental science; Atmospheric emissions; Atmospheric sciences; Climatology; Geology","score_opus":0.03306456836779414,"score_gpt":0.3161621270241689,"score_spread":0.28309755865637476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2124949732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86601955,0.043347042,0.001785345,0.0026597204,0.00040444822,0.000035165638,0.04232474,0.0004576753,0.042966284],"genre_scores_gemma":[0.93376815,0.018496769,0.0020399562,0.0005480151,0.00044970718,0.000042212752,0.037428044,0.000060129652,0.0071670716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997118,0.000026941074,0.00003624419,0.00010546569,0.000065537555,0.000054000957],"domain_scores_gemma":[0.9989236,0.00009812013,0.00035201394,0.000046943514,0.00050817884,0.00007105863],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032817165,0.0003365327,0.00027430477,0.0034305884,0.00026077576,0.0006568744,0.00028984758,0.00044223553,0.003858694],"category_scores_gemma":[0.0007946979,0.00009586846,0.00033398584,0.0049747224,0.00022700006,0.00070928637,0.00038064018,0.00046023066,0.0018101163],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001746709,0.000038207832,0.83838093,0.00060312834,0.00067362224,0.0004966091,0.00054136384,0.0011139843,0.0030764488,0.0021750974,0.015164071,0.13756183],"study_design_scores_gemma":[0.000007015159,0.00007764825,0.9162517,0.00011212999,0.0001578404,0.00059374084,0.00023038714,0.00031678416,0.0013782782,0.00019183262,0.08066008,0.000022552944],"about_ca_topic_score_codex":0.016668744,"about_ca_topic_score_gemma":0.019553123,"teacher_disagreement_score":0.016668744,"about_ca_system_score_codex":0.00076000293,"about_ca_system_score_gemma":0.0004828283,"threshold_uncertainty_score":0.0331434},"labels":[],"label_agreement":null},{"id":"W2125097581","doi":"10.1029/2006gl025944","title":"Gravity‐driven advective transport during deep geological disposal of contaminants","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Max-Planck-Gesellschaft; McGill University","keywords":"Advection; Geology; Contamination; Environmental science; Hydrology (agriculture); Geophysics; Earth science; Geotechnical engineering","score_opus":0.014115666319443042,"score_gpt":0.2647571362896115,"score_spread":0.25064146997016845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125097581","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4449409,0.0007288744,0.5426199,0.0014652992,0.000105880215,0.000086392196,0.00023441877,0.00026756836,0.009550769],"genre_scores_gemma":[0.9907369,0.00027935594,0.004908494,0.00005814623,0.00002248805,0.00004521239,0.000041247346,0.000022282638,0.0038859183],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998648,0.000029276194,0.0000051919283,0.000027614557,0.000033983626,0.00003909459],"domain_scores_gemma":[0.9997985,0.00007306063,0.000062370375,0.000013618103,0.000024030493,0.000028498134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023258035,0.0005013862,0.0005302717,0.0003585942,0.00051795976,0.00065791694,0.00070084305,0.0011344682,0.00066888524],"category_scores_gemma":[0.0006456059,0.00035784394,0.0006159733,0.00026220884,0.0016076227,0.0011730258,0.00092259765,0.0005648922,0.00010583591],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047367554,0.000027833552,0.0011151532,0.000042214717,0.000015814976,0.00041440656,0.00010805771,0.89657456,0.020902844,0.077443436,0.00043546408,0.0028727888],"study_design_scores_gemma":[0.00001501433,0.000027343765,0.00032293657,0.000002527695,0.000005510005,0.00006301539,0.000019935535,0.9895672,0.0010525787,0.008482033,0.00043075092,0.000011080462],"about_ca_topic_score_codex":0.00923848,"about_ca_topic_score_gemma":0.003679332,"teacher_disagreement_score":0.00923848,"about_ca_system_score_codex":0.0012977812,"about_ca_system_score_gemma":0.00091411226,"threshold_uncertainty_score":0.018369436},"labels":[],"label_agreement":null},{"id":"W2125158094","doi":"10.1002/2015gl065779","title":"Gas hydrate dissociation prolongs acidification of the Anthropocene oceans","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Clathrate hydrate; Carbonate; Anthropocene; Ocean acidification; Carbon cycle; Carbon dioxide; Biogeochemical cycle; Methane; Environmental science; Oceanography; Environmental chemistry; Geology; Earth science; Hydrate; Ecosystem; Climate change; Chemistry; Ecology; Paleontology","score_opus":0.039521144119997784,"score_gpt":0.3036216216445216,"score_spread":0.2641004775245238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125158094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99909484,0.000075232296,0.00025169557,0.00007375121,0.0000039782512,0.0000012898172,0.000042456337,0.000015853053,0.0004409545],"genre_scores_gemma":[0.99972695,0.000043520573,0.000079807236,0.0000111374675,0.0000018037829,0.00000117029,0.000030150362,0.0000019063449,0.00010357839],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999685,0.00000443744,0.000002027466,0.000009114228,0.000005039743,0.000010887007],"domain_scores_gemma":[0.99992466,0.000016013857,0.000021985166,0.000012064307,0.0000068619966,0.000018395309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012569754,0.00015152995,0.00017954662,0.00008856173,0.0001711105,0.00033282186,0.00018294832,0.00029430122,0.0013727112],"category_scores_gemma":[0.00031253626,0.00011045118,0.0002624194,0.000092642076,0.0003127434,0.00025038052,0.000510569,0.0002694229,0.00008782216],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018095109,0.0001672411,0.34441206,0.00024073326,0.00027811716,0.0010587679,0.00027606706,0.07842696,0.55313563,0.005457568,0.0005694628,0.014167989],"study_design_scores_gemma":[0.00017288918,0.0008182692,0.7820355,0.000018684159,0.00014958615,0.0004694347,0.00078507117,0.1156414,0.090731755,0.0045663337,0.004557917,0.00005321226],"about_ca_topic_score_codex":0.00600466,"about_ca_topic_score_gemma":0.0056786463,"teacher_disagreement_score":0.00600466,"about_ca_system_score_codex":0.00056795136,"about_ca_system_score_gemma":0.0003064227,"threshold_uncertainty_score":0.011939406},"labels":[],"label_agreement":null},{"id":"W2125356070","doi":"10.1029/2004gl019416","title":"Space‐based diagnosis of surface ozone sensitivity to anthropogenic emissions","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":365,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Division of Ocean Sciences; Dalhousie University","keywords":"Ozone; Environmental science; Nitrogen dioxide; Satellite; Northern Hemisphere; Tropospheric ozone; Atmospheric sciences; Pollution; Formaldehyde; Air pollution; Troposphere; Atmosphere (unit); Environmental chemistry; Meteorology; Chemistry; Geology; Geography","score_opus":0.03688315638822547,"score_gpt":0.3056440846486885,"score_spread":0.268760928260463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2125356070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97837716,0.0003337675,0.018207436,0.00006124722,0.000015385873,0.00001767259,0.0005676261,0.00031156515,0.002108117],"genre_scores_gemma":[0.9941543,0.00005429227,0.0054134745,0.0000118716425,0.000012570623,0.0000043302566,0.00021301274,0.0000044045255,0.00013184288],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998605,0.000036227186,0.000008815817,0.00003243453,0.00004160707,0.000020334523],"domain_scores_gemma":[0.99943465,0.00022161985,0.00014871517,0.00007017162,0.00008288812,0.00004190402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026337992,0.00031232447,0.00020574125,0.0012068644,0.00013991904,0.00044573416,0.00021790482,0.00030481926,0.00079778064],"category_scores_gemma":[0.0010920449,0.00008700626,0.00014089169,0.00053271576,0.00016607932,0.0003033526,0.00030650332,0.0001551641,0.00013786586],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006372322,0.00014808147,0.6579517,0.00011404512,0.00022826115,0.00027883225,0.00022142509,0.036040418,0.15107757,0.0010368167,0.00073771033,0.15152799],"study_design_scores_gemma":[0.000032856362,0.00058424816,0.66202396,0.000019947025,0.00015716266,0.0005791633,0.0003424962,0.26400405,0.06805131,0.0018971552,0.0022495075,0.00005815302],"about_ca_topic_score_codex":0.0027322632,"about_ca_topic_score_gemma":0.0032678624,"teacher_disagreement_score":0.0027322632,"about_ca_system_score_codex":0.00016481178,"about_ca_system_score_gemma":0.00013479842,"threshold_uncertainty_score":0.005432725},"labels":[],"label_agreement":null},{"id":"W2126084414","doi":"10.1002/2015gl063898","title":"Effects of temperature and precipitation on snowpack variability in the Central Rocky Mountains as a function of elevation","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Snowpack; Elevation (ballistics); Snow; Lapse rate; Precipitation; Environmental science; Atmospheric sciences; Climatology; Range (aeronautics); Geology; Meteorology; Geography; Geomorphology","score_opus":0.027200993968716395,"score_gpt":0.2765083743435319,"score_spread":0.24930738037481553,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126084414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993486,0.000047958954,0.00023971385,0.0000146351385,0.0000012988506,0.0000013983757,0.00012159419,0.000012739212,0.00021211157],"genre_scores_gemma":[0.99973506,0.000012871326,0.000078975034,0.0000029803703,0.0000023199573,0.000001225755,0.00012050126,0.0000028411569,0.00004329023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997718,0.000096919575,0.000011659584,0.000045446217,0.000034822104,0.000039348506],"domain_scores_gemma":[0.9989785,0.0004919141,0.00020659613,0.000095349176,0.00014737608,0.00008024322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071141875,0.00015756978,0.00021628922,0.00040027263,0.000218215,0.0005119953,0.00027439397,0.00015178636,0.00062329473],"category_scores_gemma":[0.0013191736,0.00011361314,0.00041194842,0.00052041357,0.00024162159,0.00017486067,0.0002489155,0.00018692242,0.0001415356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031261647,0.000039921368,0.9714546,0.00002855164,0.00027804554,0.000197964,0.00016676552,0.012798338,0.00754239,0.00016882354,0.0002220655,0.006789831],"study_design_scores_gemma":[0.0000046693485,0.000030734784,0.9900538,0.000003260878,0.000024871162,0.00003230046,0.00004873677,0.009312285,0.0003658979,0.000022808614,0.000096638694,0.0000039362817],"about_ca_topic_score_codex":0.021786954,"about_ca_topic_score_gemma":0.01586207,"teacher_disagreement_score":0.021786954,"about_ca_system_score_codex":0.00018586512,"about_ca_system_score_gemma":0.00020685888,"threshold_uncertainty_score":0.0433203},"labels":[],"label_agreement":null},{"id":"W2126113351","doi":"10.1029/2001gl013192","title":"On the mid‐depth circulation in the Labrador and Irminger Seas","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research; San Diego Supercomputer Center; National Aeronautics and Space Administration","keywords":"Barotropic fluid; Baroclinity; Geology; Circulation (fluid dynamics); Forcing (mathematics); Oceanography; Climatology; Plume; Ocean current; Meteorology; Geography; Mechanics","score_opus":0.03629089889504423,"score_gpt":0.2745432530970587,"score_spread":0.23825235420201446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126113351","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940626,0.00017527354,0.001623428,0.0001604053,0.000008279726,0.000008156353,0.00037671265,0.000096977354,0.0034881232],"genre_scores_gemma":[0.99773264,0.00019029267,0.00073017075,0.000026422584,0.0000111752615,0.0000068020718,0.0002238015,0.000017138644,0.0010615506],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993765,0.000016022344,0.000003254038,0.00001475828,0.000007415962,0.000020980346],"domain_scores_gemma":[0.9999181,0.000014804623,0.00002397968,0.000011080496,0.000010253513,0.000021827835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010435324,0.00045680968,0.000470082,0.00036092952,0.0005005801,0.00080175884,0.0006038233,0.00052677625,0.0010954291],"category_scores_gemma":[0.00043327865,0.00025646767,0.0005375202,0.0002834463,0.00052403886,0.0005761986,0.0005766593,0.00037698867,0.0003059918],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024163291,0.00004705575,0.018476294,0.000024863344,0.000043687785,0.00024192667,0.00012259088,0.96293575,0.005595112,0.0068785325,0.00063898397,0.0047535026],"study_design_scores_gemma":[0.00004969383,0.000059297898,0.017318556,0.000012493177,0.000028198065,0.00002636304,0.000064507985,0.97991896,0.00055338093,0.00097632885,0.00096441474,0.000027815566],"about_ca_topic_score_codex":0.1180874,"about_ca_topic_score_gemma":0.052177995,"teacher_disagreement_score":0.8819126,"about_ca_system_score_codex":0.0015926856,"about_ca_system_score_gemma":0.0005238049,"threshold_uncertainty_score":0.23480016},"labels":[],"label_agreement":null},{"id":"W2126354444","doi":"10.1002/2014gl060832","title":"The “footloose” mechanism: Iceberg decay from hydrostatic stresses","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Iceberg; Geology; Hydrostatic equilibrium; Buoyancy; Overburden; Ridge; Geodesy; Geophysics; Seismology; Mechanics; Oceanography; Geotechnical engineering; Sea ice; Physics; Paleontology","score_opus":0.01815341793201951,"score_gpt":0.2596487678314166,"score_spread":0.24149534989939708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126354444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9670113,0.00024643194,0.028533524,0.0002459321,0.000026542815,0.000024246021,0.00003968386,0.000077281315,0.0037951944],"genre_scores_gemma":[0.9989524,0.00005199932,0.00051945046,0.000010833749,0.0000053595004,0.0000046133364,0.0000063159027,0.0000041362314,0.00044492248],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993646,0.000007213169,0.000003124284,0.0000107323285,0.000016001375,0.000026568823],"domain_scores_gemma":[0.9997491,0.000053983764,0.00010436064,0.000025090852,0.000030173122,0.000037212245],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022014577,0.00029491467,0.0002620446,0.0003665651,0.00036018755,0.0005877942,0.0005273847,0.00032700424,0.0012988268],"category_scores_gemma":[0.0006983618,0.00014394904,0.00036221452,0.00010994784,0.000821452,0.0008556246,0.00052605773,0.00035506437,0.00012420559],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006840284,0.00038797018,0.11670855,0.00051651447,0.00026318556,0.0036991206,0.0012453799,0.3105999,0.3591423,0.13159436,0.0021826122,0.07297609],"study_design_scores_gemma":[0.000056827343,0.00043342912,0.053883158,0.000055741068,0.00006773955,0.00053360197,0.00056344504,0.8612936,0.058317047,0.02255416,0.0021807377,0.00006045964],"about_ca_topic_score_codex":0.004314045,"about_ca_topic_score_gemma":0.002873188,"teacher_disagreement_score":0.004314045,"about_ca_system_score_codex":0.00059158204,"about_ca_system_score_gemma":0.00029159235,"threshold_uncertainty_score":0.008577824},"labels":[],"label_agreement":null},{"id":"W2126518970","doi":"10.1002/grl.50769","title":"Modeling evidence that ozone depletion has impacted extreme precipitation in the austral summer","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Precipitation; Climatology; Ozone depletion; Atmospheric sciences; Environmental science; Middle latitudes; Subtropics; Ozone; Latitude; Ozone layer; Total Ozone Mapping Spectrometer; Climate model; Stratosphere; Climate change; Geology; Meteorology; Oceanography; Geography; Ecology","score_opus":0.2785132968416296,"score_gpt":0.3618275402334945,"score_spread":0.08331424339186488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126518970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99635375,0.00007607522,0.0006383986,0.00031604437,0.00001113046,0.000004867066,0.00031584522,0.00003261916,0.0022512737],"genre_scores_gemma":[0.9993437,0.000054691554,0.00020401778,0.000020886815,0.0000040259565,0.0000034997101,0.0001382854,0.000005008,0.00022589018],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999136,0.0000302462,0.000003593207,0.000017582286,0.000011484586,0.000023537372],"domain_scores_gemma":[0.99979013,0.00008533196,0.000036879897,0.000016741662,0.0000368959,0.00003405733],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003302884,0.00031480688,0.00021287537,0.00017900526,0.00023386431,0.00059961475,0.0005453897,0.0005471209,0.0017797321],"category_scores_gemma":[0.00069146807,0.0002371613,0.00038686802,0.00029781388,0.00018590057,0.0003491246,0.0003779644,0.00037200237,0.00011032781],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005188319,0.00030369518,0.18917516,0.00009858933,0.00038212055,0.00026782852,0.0001491828,0.7877984,0.009957963,0.0022230283,0.001546231,0.0075790007],"study_design_scores_gemma":[0.00029161957,0.00022075792,0.12068309,0.00001918224,0.00017051905,0.000038989547,0.00015803662,0.87335664,0.0018298903,0.0014688052,0.0017379132,0.000024568924],"about_ca_topic_score_codex":0.06893824,"about_ca_topic_score_gemma":0.056546517,"teacher_disagreement_score":0.06893824,"about_ca_system_score_codex":0.00076544285,"about_ca_system_score_gemma":0.00061240577,"threshold_uncertainty_score":0.137074},"labels":[],"label_agreement":null},{"id":"W2126623081","doi":"10.1029/2006gl028712","title":"Surface eddy diffusivity for heat in a model of the northwest Atlantic Ocean","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Eddy; Thermal diffusivity; Heat flux; Geology; Eddy diffusion; Mesoscale meteorology; Flux (metallurgy); Heat transfer; Thermal; Gulf Stream; Turbulence; Surface (topology); Surface layer; Geophysics; Climatology; Atmospheric sciences; Meteorology; Mechanics; Thermodynamics; Materials science; Layer (electronics); Physics; Geometry","score_opus":0.023303759933847274,"score_gpt":0.2540619133121483,"score_spread":0.230758153378301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126623081","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96115476,0.00056905294,0.025706792,0.0010788876,0.00009274061,0.000032076103,0.0008067551,0.0002554584,0.010303446],"genre_scores_gemma":[0.99325305,0.00017085182,0.0026797159,0.000032383523,0.000024649198,0.000036754882,0.0002476429,0.000061046056,0.0034939854],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993515,0.000022458931,0.0000034672612,0.000013723816,0.000009841061,0.000015358486],"domain_scores_gemma":[0.99981254,0.00008707014,0.000026740434,0.000013327817,0.000026597598,0.000033833712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002646695,0.00041898395,0.0004094242,0.000245468,0.000602651,0.00074290636,0.00065565447,0.0010621474,0.0016489296],"category_scores_gemma":[0.0008388274,0.0003910349,0.0006793656,0.00025421166,0.0005289201,0.00064966944,0.0005337073,0.00073873054,0.00017793149],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006642992,0.000026060148,0.003390103,0.000014778596,0.000021376045,0.00006251952,0.000026169555,0.9899732,0.0025002453,0.0027615384,0.00033937438,0.0008181177],"study_design_scores_gemma":[0.000019099109,0.000006530013,0.0008541702,0.000001738578,0.00000342227,0.0000050132903,0.000006031159,0.9982169,0.0001458287,0.00054302206,0.0001937725,0.000004433099],"about_ca_topic_score_codex":0.06253743,"about_ca_topic_score_gemma":0.037280586,"teacher_disagreement_score":0.06253743,"about_ca_system_score_codex":0.0015465948,"about_ca_system_score_gemma":0.0011803533,"threshold_uncertainty_score":0.12434685},"labels":[],"label_agreement":null},{"id":"W2126891415","doi":"10.1029/2001gl013578","title":"Satellite‐derived increases in net primary productivity across North America, 1982–1998","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Primary production; Environmental science; Sink (geography); Carbon cycle; Carbon sink; Primary productivity; Satellite; Climatology; Productivity; Atmospheric sciences; Ecosystem; Geography; Geology; Ecology; Biology","score_opus":0.02108876878496656,"score_gpt":0.2580229526011867,"score_spread":0.2369341838162201,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2126891415","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822074,0.00009673544,0.000106505446,0.000034139077,0.0000026630232,0.0000019335494,0.0012571412,0.000013378568,0.00026690695],"genre_scores_gemma":[0.9959408,0.00022304576,0.0005221646,0.000017093807,0.000009935211,0.000011491899,0.0029941928,0.000005274729,0.00027589002],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995255,0.0000052660403,0.000003242352,0.000018650017,0.0000118350845,0.000008450074],"domain_scores_gemma":[0.9997516,0.000038823935,0.00008299889,0.000024418041,0.00007760881,0.000024565472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002026872,0.0001831527,0.00015459434,0.00031487414,0.00020431766,0.0002630045,0.00014419784,0.00017142372,0.0005287512],"category_scores_gemma":[0.0006077013,0.0001648935,0.00012936867,0.0006561161,0.0001627378,0.00036496285,0.0002172619,0.00018524395,0.00009537825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002468456,0.000077643344,0.96309304,0.00008953568,0.00020598757,0.00019818378,0.00056008575,0.0058100275,0.007597647,0.00013710414,0.0014910842,0.020492963],"study_design_scores_gemma":[0.000009279138,0.000010840066,0.9965784,0.000003681417,0.000025866027,0.000036700472,0.000062973755,0.002053367,0.0003617907,0.000035137797,0.00081907987,0.0000028672764],"about_ca_topic_score_codex":0.09304298,"about_ca_topic_score_gemma":0.19306128,"teacher_disagreement_score":0.90695703,"about_ca_system_score_codex":0.0007741824,"about_ca_system_score_gemma":0.000352465,"threshold_uncertainty_score":0.1850028},"labels":[],"label_agreement":null},{"id":"W2127303034","doi":"10.1029/2008gl033950","title":"A 1,000‐year, annually‐resolved record of hurricane activity from Boston, Massachusetts","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Institut National de la Recherche Scientifique; Université du Québec à Montréal","funders":"National Oceanic and Atmospheric Administration","keywords":"Varve; Centennial; Geology; Flooding (psychology); Paleoclimatology; Precipitation; Storm; Period (music); Climatology; Sediment; Deposition (geology); Peat; Tropical cyclone; Holocene; Atlantic hurricane; Physical geography; Vegetation (pathology); Oceanography; Climate change; Archaeology; Geography; Geomorphology; Meteorology","score_opus":0.04642658055211109,"score_gpt":0.2849092246889354,"score_spread":0.23848264413682435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127303034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9728467,0.0016837959,0.00044143313,0.0008792578,0.000029173318,0.00002426572,0.019487215,0.00007946187,0.004528568],"genre_scores_gemma":[0.97875094,0.00075630593,0.00028781354,0.000101348975,0.00006255193,0.000020301055,0.014417713,0.000009811689,0.005593274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999397,0.00000615772,0.0000053826366,0.000023343122,0.000015042977,0.00001038551],"domain_scores_gemma":[0.99966466,0.000021030823,0.00012439008,0.000023180944,0.00010974999,0.00005692995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010311029,0.00016807226,0.000108472195,0.0010260401,0.00033210966,0.00039315244,0.00024610962,0.0001910637,0.0021089842],"category_scores_gemma":[0.00045339638,0.00009978395,0.000059147707,0.0011963419,0.00010795049,0.0002585117,0.00036373344,0.00020283043,0.00062366313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003364955,0.000030010384,0.9548922,0.00005966769,0.000121292636,0.000283069,0.0010265034,0.0003948033,0.0062030503,0.00021552505,0.014206712,0.022533478],"study_design_scores_gemma":[0.0000016885983,0.00000773378,0.99402976,0.0000050789213,0.00000865126,0.000030122952,0.000101780315,0.0001233045,0.00014590374,0.000010535709,0.0055333204,0.000001987872],"about_ca_topic_score_codex":0.25489742,"about_ca_topic_score_gemma":0.58742064,"teacher_disagreement_score":0.25489742,"about_ca_system_score_codex":0.0009726297,"about_ca_system_score_gemma":0.00029445082,"threshold_uncertainty_score":0.5068275},"labels":[],"label_agreement":null},{"id":"W2127369033","doi":"10.1029/2006gl027094","title":"Exchange of sea ice between the Arctic Ocean and the Canadian Arctic Archipelago","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Sea ice; Arctic ice pack; Oceanography; Archipelago; Arctic; Arctic geoengineering; Arctic sea ice decline; Antarctic sea ice; Sea ice thickness; Climatology; Geology; Drift ice; Flux (metallurgy); Environmental science","score_opus":0.020070344962367925,"score_gpt":0.24355477722787255,"score_spread":0.22348443226550463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127369033","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9767659,0.0032749611,0.00042314915,0.00042240202,0.000023626282,0.000012132482,0.0030013954,0.000024973586,0.016051529],"genre_scores_gemma":[0.9957789,0.0010898731,0.00040379376,0.000044584718,0.0000069344824,0.0000049094733,0.0011517444,0.000007185439,0.0015120456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971145,0.000020808913,0.000009203059,0.000045078483,0.00011304772,0.00010039513],"domain_scores_gemma":[0.99962306,0.000035104185,0.00004546187,0.000018539316,0.00020297272,0.00007477375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039423065,0.0002245981,0.00025909895,0.001819814,0.0021935857,0.0017282055,0.00038947334,0.00014839931,0.0013863768],"category_scores_gemma":[0.0011720251,0.00014589138,0.00025634398,0.0029875834,0.0003934775,0.00047682488,0.00062352413,0.00023601156,0.00009245639],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048350383,0.00003876563,0.90432096,0.00011656866,0.0003321907,0.00035588373,0.0014595249,0.006725272,0.00472451,0.0046997312,0.0053815315,0.071361475],"study_design_scores_gemma":[0.0000056536237,0.00000723758,0.9901743,0.00002523438,0.0000345283,0.000054810836,0.0006384786,0.001766916,0.00033384436,0.0002848854,0.00665732,0.000016811004],"about_ca_topic_score_codex":0.98182124,"about_ca_topic_score_gemma":0.99255085,"teacher_disagreement_score":0.018178761,"about_ca_system_score_codex":0.014721924,"about_ca_system_score_gemma":0.009468833,"threshold_uncertainty_score":0.10681552},"labels":[],"label_agreement":null},{"id":"W2127418807","doi":"10.1002/2013gl058479","title":"Gypsum crystals observed in experimental and natural sea ice","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Comisión de Investigaciones Científicas; Canada Excellence Research Chairs, Government of Canada; Kommissionen for Videnskabelige Undersøgelser i Grønland; University of Manitoba","keywords":"Gypsum; Natural (archaeology); Geology; Sea ice; Oceanography; Mineralogy; Astrobiology; Earth science; Atmospheric sciences; Paleontology; Physics","score_opus":0.030157261060365304,"score_gpt":0.27592486661974513,"score_spread":0.24576760555937982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127418807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987534,0.00011506196,0.00032167055,0.0000057453067,0.0000059003114,0.000009240406,0.00020724372,0.000008716203,0.0005730901],"genre_scores_gemma":[0.9987796,0.00010390487,0.0004029888,0.0000073279625,0.0000041259946,0.000018440109,0.00035548155,0.000006207275,0.00032189165],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998454,0.000020893476,0.000018299439,0.000041448417,0.00004389657,0.00002999178],"domain_scores_gemma":[0.9996859,0.000087326785,0.00007182689,0.000050484938,0.00007051102,0.000033935932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019621034,0.0002474779,0.00020813537,0.0003859111,0.00038328834,0.00032789705,0.00017366829,0.00020600368,0.00095160585],"category_scores_gemma":[0.00037165196,0.00012804603,0.00017558243,0.00024019153,0.00063901296,0.00016231055,0.0002756268,0.00021474762,0.00008166685],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042710578,0.00007210098,0.031846263,0.00011017325,0.00005512727,0.00028189426,0.00018144032,0.0005891747,0.9642072,0.00016220649,0.000078707235,0.0019885586],"study_design_scores_gemma":[0.000050065133,0.00046227034,0.16391486,0.0000120847435,0.00004808559,0.00046371197,0.00029977795,0.002377316,0.8304058,0.00009752039,0.0018538205,0.000014657082],"about_ca_topic_score_codex":0.0030383144,"about_ca_topic_score_gemma":0.0028149544,"teacher_disagreement_score":0.0030383144,"about_ca_system_score_codex":0.00031651655,"about_ca_system_score_gemma":0.00021112227,"threshold_uncertainty_score":0.0060412884},"labels":[],"label_agreement":null},{"id":"W2127685082","doi":"10.1002/grl.50879","title":"Lithospheric fabric variations in central North America: Influence of rifting and Archean tectonic styles","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Manitoba Hydro","keywords":"Geology; Lithosphere; Terrane; Archean; Tectonics; Rift; Mantle (geology); Seismology; Shear wave splitting; Shear zone; Paleontology; Geophysics","score_opus":0.015363985784493824,"score_gpt":0.2477553071575118,"score_spread":0.23239132137301796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127685082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996997,0.00005112563,0.000009170098,0.0000066847174,3.3925045e-7,6.921896e-7,0.0000720793,0.000002144967,0.00015803332],"genre_scores_gemma":[0.99969685,0.000061485705,0.000034981982,0.000005165446,0.0000011119531,0.0000016269677,0.00013062659,0.0000013202855,0.0000668096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.000011398839,0.0000037342554,0.000016321637,0.000011153118,0.00001938845],"domain_scores_gemma":[0.99974316,0.000047661397,0.00007994794,0.000019415644,0.000060072365,0.00004969101],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001499885,0.00019104946,0.00012480513,0.0009693095,0.0003199952,0.00044660264,0.00014979369,0.00012763766,0.0006252773],"category_scores_gemma":[0.00041276877,0.00014462994,0.00011505959,0.0011938217,0.00036777795,0.00017885392,0.00030641773,0.00008520801,0.00006903613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004916049,0.000010646465,0.9933849,0.000009567031,0.000039913797,0.00008020987,0.00048789973,0.00024203134,0.002126366,0.000023977014,0.000084179715,0.003461173],"study_design_scores_gemma":[7.085131e-7,0.0000021816497,0.99969375,0.0000011465597,0.0000030260853,0.0000115024795,0.00014864258,0.00006819516,0.000027512348,0.0000033858953,0.000039489525,5.4908446e-7],"about_ca_topic_score_codex":0.22165924,"about_ca_topic_score_gemma":0.4647964,"teacher_disagreement_score":0.77834076,"about_ca_system_score_codex":0.0007454395,"about_ca_system_score_gemma":0.00044273012,"threshold_uncertainty_score":0.44073808},"labels":[],"label_agreement":null},{"id":"W2127838438","doi":"10.1029/2004gl021982","title":"Vertical variation of NLC particle sizes retrieved from Odin/OSIRIS limb scattering observations","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Tekes; Centre National d’Etudes Spatiales","keywords":"Osiris; Spectrograph; Particle (ecology); Northern Hemisphere; Range (aeronautics); Particle-size distribution; Mie scattering; Physics; Particle size; Satellite; Atmospheric sciences; Astrophysics; Scattering; Computational physics; Optics; Light scattering; Materials science; Astronomy; Spectral line; Geology","score_opus":0.06096768025609447,"score_gpt":0.28722393349256453,"score_spread":0.22625625323647006,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2127838438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967244,0.00002927336,0.00054550543,0.000007269259,0.000002669609,0.000007561472,0.0017181512,0.00003167829,0.0009335205],"genre_scores_gemma":[0.9938735,0.000025520882,0.0009295804,0.0000071652157,0.0000025015725,0.000009270063,0.004953329,0.000010094047,0.00018908035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985313,0.0000128597785,0.000012352936,0.00003488889,0.0000641303,0.000022607355],"domain_scores_gemma":[0.9996563,0.00007033124,0.00007060354,0.00003199581,0.00013861377,0.000032270385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028111783,0.00016481696,0.00013442425,0.000729046,0.00022330882,0.0002571724,0.00018459508,0.00013754927,0.0003833968],"category_scores_gemma":[0.00065198925,0.00009951105,0.0001242397,0.00059692725,0.00012248837,0.00015191667,0.00018636485,0.000117094736,0.000108317676],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027596066,0.000087891225,0.8983431,0.0000602471,0.000085775595,0.0001821065,0.00025488035,0.014052462,0.06291407,0.000277143,0.0018538566,0.021612601],"study_design_scores_gemma":[0.0000071675254,0.000008602531,0.9848402,0.0000028580298,0.0000076200254,0.000034879984,0.000047281585,0.011120158,0.003244675,0.000026112888,0.00065418816,0.000006219544],"about_ca_topic_score_codex":0.040719718,"about_ca_topic_score_gemma":0.056006033,"teacher_disagreement_score":0.040719718,"about_ca_system_score_codex":0.000562711,"about_ca_system_score_gemma":0.00024674024,"threshold_uncertainty_score":0.0809654},"labels":[],"label_agreement":null},{"id":"W2128012785","doi":"10.1029/2003gl018878","title":"Convection dynamics and driving mechanism of a small substorm during dominantly IMF By+, Bz+ conditions","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Substorm; Geophysics; Magnetosphere; Solar wind; Physics; Interplanetary magnetic field; Convection; Excursion; Ionosphere; Geology; Magnetic field; Meteorology","score_opus":0.008276849252665433,"score_gpt":0.2512900680877321,"score_spread":0.24301321883506666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128012785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943537,0.000033096552,0.00012371947,0.00001259852,0.000001313353,0.0000035885137,0.00005747473,0.000012951419,0.00031987537],"genre_scores_gemma":[0.99980754,0.000009981585,0.000058568443,0.0000026801356,0.000002238265,0.0000017280146,0.000062194886,0.0000014555712,0.000053582935],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999751,0.0000020140012,0.0000015482375,0.0000065589365,0.0000030970023,0.000011719216],"domain_scores_gemma":[0.9999144,0.000010268799,0.000021374559,0.0000061795067,0.000013776784,0.00003398716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000068236965,0.00010914381,0.0001587317,0.00021946823,0.00023335691,0.00020103424,0.00011549356,0.00013783274,0.000516178],"category_scores_gemma":[0.00014958416,0.000081403814,0.00007953151,0.00010238769,0.00015305805,0.0001277453,0.00019226417,0.00012468832,0.0001047982],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008704112,0.0000775724,0.25243533,0.000038333943,0.00002812089,0.00086876797,0.00041388988,0.0019522029,0.7334665,0.00061126164,0.0005488892,0.008688678],"study_design_scores_gemma":[0.000033298536,0.00016396493,0.95897657,0.000005056485,0.000019247818,0.00028403616,0.00014846996,0.010812062,0.028820857,0.0001800957,0.0005475089,0.000008798161],"about_ca_topic_score_codex":0.0037597264,"about_ca_topic_score_gemma":0.0028888737,"teacher_disagreement_score":0.0037597264,"about_ca_system_score_codex":0.00025355784,"about_ca_system_score_gemma":0.00009053956,"threshold_uncertainty_score":0.007475674},"labels":[],"label_agreement":null},{"id":"W2128021995","doi":"10.1002/2013gl057188","title":"Unprecedented recent summer warmth in Arctic Canada","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Tundra; Climatology; Arctic; Glacier; Environmental science; Arctic ice pack; Sea ice; Climate change; Snow; Physical geography; Holocene; Latitude; Arctic geoengineering; Precipitation; Permafrost; Oceanography; Geology; Geography; Antarctic sea ice; Meteorology","score_opus":0.04010888544315926,"score_gpt":0.28730081486209136,"score_spread":0.2471919294189321,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128021995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99356824,0.00060079637,0.0001841526,0.00036862656,0.000017409373,0.0000020923578,0.0020492107,0.00002247005,0.0031870238],"genre_scores_gemma":[0.9983865,0.00030812703,0.000106406056,0.000054276246,0.000007870272,0.0000010234776,0.00068797165,0.0000035061782,0.00044440504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999063,0.0000032256928,0.000002548438,0.000027183389,0.000029392784,0.000031336534],"domain_scores_gemma":[0.9997423,0.000011183,0.000040977015,0.000011724658,0.0001494019,0.00004428399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019411003,0.00014180875,0.00011788209,0.00055074494,0.0012303054,0.00082003715,0.00022457798,0.00018763688,0.0014512927],"category_scores_gemma":[0.00033244895,0.00007914219,0.00016968121,0.0010620786,0.00030169418,0.0002296363,0.00031586783,0.00027722365,0.00009284575],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010348853,0.00001683779,0.9702417,0.000047762675,0.00010764255,0.00014566092,0.0006439788,0.0015752473,0.0059488257,0.00074420345,0.0024680712,0.017956562],"study_design_scores_gemma":[0.0000020340774,0.000005421409,0.99255365,0.000010026394,0.000017918286,0.00004685911,0.0004789008,0.0005606972,0.00046650617,0.00007371228,0.0057768724,0.0000075891203],"about_ca_topic_score_codex":0.94395745,"about_ca_topic_score_gemma":0.9773516,"teacher_disagreement_score":0.056042552,"about_ca_system_score_codex":0.005893415,"about_ca_system_score_gemma":0.005871083,"threshold_uncertainty_score":0.112745166},"labels":[],"label_agreement":null},{"id":"W2128056009","doi":"10.1029/2003gl017503","title":"Identification of CO plumes from MOPITT data: Application to the August 2000 Idaho‐Montana forest fires","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Plume; Environmental science; Troposphere; Period (music); Climatology; Atmospheric sciences; Physical geography; Meteorology; Geology; Geography","score_opus":0.020320165364271912,"score_gpt":0.2851658293150245,"score_spread":0.2648456639507526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128056009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957605,0.00008556741,0.0022028543,0.00012343957,0.00000995063,0.00003440107,0.0006114008,0.0003012277,0.0008706472],"genre_scores_gemma":[0.9877061,0.00008168021,0.010557778,0.000023031624,0.000012647048,0.000025699735,0.0012870418,0.00003338625,0.00027266153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993217,0.000013836741,0.00000439099,0.000017153803,0.000017019322,0.000015421052],"domain_scores_gemma":[0.9998355,0.00006484916,0.00002110736,0.000016381775,0.000038643004,0.000023565515],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002459569,0.00048295673,0.00025481443,0.0007468933,0.00053474895,0.00052493624,0.0003654642,0.0005509148,0.0002866075],"category_scores_gemma":[0.0006261831,0.00026363667,0.00036073412,0.00058369583,0.00017328685,0.00029301445,0.000374935,0.0003156297,0.00008113807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015386859,0.0005995513,0.47684664,0.00018454695,0.00028269083,0.0027523274,0.00081319,0.35050887,0.060805283,0.00097052864,0.002528004,0.102169596],"study_design_scores_gemma":[0.00010275753,0.0000651449,0.1706841,0.000014533034,0.000042488136,0.0002153115,0.0003762923,0.8147581,0.012233748,0.00030807583,0.0011654181,0.000033991255],"about_ca_topic_score_codex":0.05924843,"about_ca_topic_score_gemma":0.07302043,"teacher_disagreement_score":0.05924843,"about_ca_system_score_codex":0.0008037503,"about_ca_system_score_gemma":0.00060398586,"threshold_uncertainty_score":0.11780709},"labels":[],"label_agreement":null},{"id":"W2128257997","doi":"10.1029/2011gl050699","title":"On the dynamics of the secondary eyewall genesis in Hurricane Wilma (2005)","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Eye; Rossby wave; Geology; Climatology; Tropical cyclone; Troposphere; Wavenumber; Atmospheric sciences; Meteorology; Physics","score_opus":0.02704117750075456,"score_gpt":0.2717874224508603,"score_spread":0.24474624495010575,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128257997","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985233,0.000021506734,0.0003828486,0.000078143465,0.000005851355,0.000003533656,0.000055631164,0.000014107368,0.0009151134],"genre_scores_gemma":[0.9994041,0.00002449441,0.00019281088,0.0000072880935,0.0000028533561,0.0000021010976,0.00006743757,0.0000029123155,0.00029601422],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999974,0.0000073687715,9.417519e-7,0.0000037072268,0.000004112525,0.000009858569],"domain_scores_gemma":[0.9998528,0.00004122355,0.00003241449,0.0000061928126,0.000035540954,0.00003190285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015474256,0.00028070138,0.0001695672,0.0002153289,0.00034671012,0.00035726718,0.00020512441,0.00030755534,0.0009958227],"category_scores_gemma":[0.00076348905,0.0001446781,0.00020702505,0.00011308612,0.00023860653,0.00021927724,0.00030682175,0.00028454588,0.00006746358],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021290137,0.00010676541,0.09009346,0.000022917886,0.000057697547,0.0006891219,0.0002015829,0.8897323,0.007184278,0.004002913,0.0019180415,0.005778053],"study_design_scores_gemma":[0.000021350903,0.000042005013,0.02527058,0.0000042431775,0.000012792786,0.00002081528,0.000085196996,0.9729758,0.0008579841,0.00032502375,0.00037759097,0.0000066552407],"about_ca_topic_score_codex":0.05570354,"about_ca_topic_score_gemma":0.044301108,"teacher_disagreement_score":0.05570354,"about_ca_system_score_codex":0.0006409731,"about_ca_system_score_gemma":0.00035411786,"threshold_uncertainty_score":0.11075866},"labels":[],"label_agreement":null},{"id":"W2128264797","doi":"10.1029/2001gl012845","title":"Adrift in the Beaufort Gyre: A model intercomparison","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"","keywords":"Ocean gyre; Arctic; Oceanography; Beaufort scale; Climatology; Beaufort sea; Climate model; Sea ice; Geology; Forcing (mathematics); The arctic; Continental shelf; Environmental science; Climate change; Subtropics; Fishery","score_opus":0.049150560703269223,"score_gpt":0.30810893796591393,"score_spread":0.2589583772626447,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128264797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98872733,0.00052526605,0.0026104015,0.00051852653,0.00009579472,0.000012513966,0.0020112016,0.0005180202,0.004980903],"genre_scores_gemma":[0.9935202,0.00015210694,0.0029091283,0.00007740265,0.000023789558,0.000013696964,0.0022248041,0.00010753624,0.00097145804],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993918,0.00024373466,0.00003004853,0.00016264667,0.000091555354,0.000080329264],"domain_scores_gemma":[0.9990256,0.00035981258,0.00014287958,0.00014344783,0.0002526798,0.000075487886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021285505,0.0007658281,0.00070670457,0.00060545333,0.0008835984,0.0019230968,0.001077749,0.0008680873,0.0009298676],"category_scores_gemma":[0.0022339448,0.0004147069,0.00093408115,0.0008802409,0.0004919729,0.0011203187,0.0005893992,0.0004259418,0.00027098533],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007042107,0.000119304554,0.09505511,0.00007713363,0.0006758772,0.00031312407,0.00056596124,0.87029743,0.0013969367,0.0020253793,0.004717446,0.024052136],"study_design_scores_gemma":[0.00030068698,0.00018892463,0.10090114,0.000051072468,0.00027490236,0.00010031549,0.00039206244,0.8811154,0.003249362,0.0017383901,0.011565551,0.00012224652],"about_ca_topic_score_codex":0.27869263,"about_ca_topic_score_gemma":0.18616225,"teacher_disagreement_score":0.27869263,"about_ca_system_score_codex":0.002027498,"about_ca_system_score_gemma":0.0013200565,"threshold_uncertainty_score":0.5541409},"labels":[],"label_agreement":null},{"id":"W2128380931","doi":"10.1002/grl.50820","title":"The influence of recent Antarctic ice sheet retreat on simulated sea ice area trends","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":142,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Western Canada Research Grid; Compute Canada; University of Victoria","keywords":"Ice sheet; Forcing (mathematics); Coupled model intercomparison project; Climatology; Sea ice; Antarctic ice sheet; Ice-sheet model; Geology; Environmental science; Antarctic sea ice; Oceanography; Climate change; Arctic ice pack; Climate model; Cryosphere","score_opus":0.04768498667345262,"score_gpt":0.291893888097786,"score_spread":0.24420890142433338,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128380931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980876,0.00006672146,0.0003312392,0.00007310483,0.000012613511,0.000003473519,0.00054111227,0.00003581599,0.00084837666],"genre_scores_gemma":[0.9990244,0.000046598,0.00021223353,0.000019695604,0.0000040642703,0.0000055325017,0.0005284568,0.000012142328,0.00014692984],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997569,0.00010668816,0.000019451218,0.00004937383,0.00002970828,0.000037972623],"domain_scores_gemma":[0.9984621,0.00090307323,0.00019269217,0.00012631145,0.00018027674,0.0001355535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011738099,0.0004995579,0.0002675509,0.0003416893,0.00030940966,0.0007665089,0.0004251704,0.00060241297,0.0010726838],"category_scores_gemma":[0.00379606,0.00025701796,0.00071815914,0.00047831,0.00031253864,0.00047132533,0.0003522223,0.0004060734,0.00016148189],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035015482,0.00010028488,0.20365229,0.00004065035,0.00027298383,0.000109179986,0.000047332927,0.78678346,0.0024098195,0.00037819336,0.0006272152,0.0052283616],"study_design_scores_gemma":[0.00011579493,0.00034979414,0.16443679,0.000025375157,0.00017654074,0.000079925354,0.00009751394,0.83083725,0.0026442755,0.0003225803,0.00088173954,0.000032407967],"about_ca_topic_score_codex":0.025825806,"about_ca_topic_score_gemma":0.020052675,"teacher_disagreement_score":0.025825806,"about_ca_system_score_codex":0.0007290404,"about_ca_system_score_gemma":0.000581824,"threshold_uncertainty_score":0.05135095},"labels":[],"label_agreement":null},{"id":"W2128544697","doi":"10.1029/2006gl027160","title":"Enhanced NO<sub>x</sub> in 2006 linked to strong upper stratospheric Arctic vortex","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":196,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Stratosphere; Stratopause; Polar vortex; Atmospheric sciences; Arctic; Atmosphere (unit); Ozone; Environmental science; Sudden stratospheric warming; Mesosphere; Climatology; Vortex; Polar; Precipitation; The arctic; Geology; Meteorology; Physics; Oceanography","score_opus":0.015520693872563085,"score_gpt":0.25944507959684787,"score_spread":0.2439243857242848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128544697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981773,0.0001578515,0.00010909587,0.00020654286,0.000033868375,0.0000066015973,0.00061433925,0.000009737528,0.0006845617],"genre_scores_gemma":[0.9986325,0.00010871244,0.00008501948,0.00006455309,0.000029119561,0.000004304477,0.00062900205,0.0000022096224,0.00044455566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999417,0.00000865385,0.000005696525,0.000016434218,0.0000093534745,0.000018197476],"domain_scores_gemma":[0.99975425,0.00001608192,0.00011732242,0.000013277147,0.00003823357,0.00006091148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019017962,0.00020522457,0.0001941328,0.00027912416,0.0003731359,0.00046740667,0.000109385124,0.0004154227,0.00061855186],"category_scores_gemma":[0.00027120943,0.000098983626,0.000085970394,0.00028329017,0.00014487785,0.00018378755,0.00034817745,0.00035069993,0.00010260917],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001270112,0.000161341,0.9757648,0.0000615879,0.00007773289,0.0012356095,0.00036152377,0.0002959675,0.011688051,0.00020638348,0.0016949361,0.0071820524],"study_design_scores_gemma":[0.0000036073022,0.000051937997,0.99846065,0.0000033425406,0.000008146589,0.0001317763,0.00007708591,0.00012108201,0.0005752051,0.000028376717,0.0005370305,0.000001743383],"about_ca_topic_score_codex":0.0071080932,"about_ca_topic_score_gemma":0.0123499995,"teacher_disagreement_score":0.0071080932,"about_ca_system_score_codex":0.00029373865,"about_ca_system_score_gemma":0.00016423776,"threshold_uncertainty_score":0.014133453},"labels":[],"label_agreement":null},{"id":"W2128612888","doi":"10.1029/2008gl034031","title":"Emissions of CH<sub>4</sub> and N<sub>2</sub>O over the United States and Canada based on a receptor‐oriented modeling framework and COBRA‐NA atmospheric observations","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":175,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"NOAA Research; U.S. Department of Defense; National Defense Science and Engineering Graduate; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Greenhouse gas; Nitrous oxide; Environmental science; Methane; Atmospheric sciences; Lagrangian; Atmospheric dispersion modeling; Dispersion (optics); Scaling; Meteorology; Air pollution; Physics; Chemistry; Geology; Mathematics; Oceanography","score_opus":0.017839428412148983,"score_gpt":0.23256474167241975,"score_spread":0.21472531326027078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128612888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9941598,0.00016293234,0.0008453593,0.00009018425,0.0000046953314,0.000011489502,0.0024669585,0.00011415055,0.0021443283],"genre_scores_gemma":[0.99469155,0.00026902911,0.0015096442,0.000024824207,0.000002589822,0.00000848134,0.0027893896,0.000014176763,0.0006903272],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998841,0.000008031609,0.0000037800378,0.000024192115,0.000041876436,0.00003802725],"domain_scores_gemma":[0.99989116,0.000014371204,0.000019434987,0.000006358139,0.000051094958,0.00001750817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015142784,0.00054846145,0.00016042951,0.0004827676,0.00067684415,0.0005483337,0.00052713515,0.00021152383,0.0006124633],"category_scores_gemma":[0.0003344316,0.0002482043,0.0003683455,0.00081607216,0.00036383644,0.00023034237,0.00035388398,0.00022386287,0.00008762324],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000990579,0.00012570953,0.59488004,0.00014250612,0.00052730314,0.0006608876,0.0004110532,0.34139875,0.01881593,0.003170231,0.0050661354,0.03381099],"study_design_scores_gemma":[0.00009010699,0.000050130282,0.74934363,0.000035673722,0.00025743054,0.00010259889,0.00043738505,0.23681194,0.006022569,0.00067177217,0.00610176,0.00007497531],"about_ca_topic_score_codex":0.982394,"about_ca_topic_score_gemma":0.98603487,"teacher_disagreement_score":0.01760602,"about_ca_system_score_codex":0.010779207,"about_ca_system_score_gemma":0.0063424096,"threshold_uncertainty_score":0.07820892},"labels":[],"label_agreement":null},{"id":"W2128639106","doi":"10.1029/2012gl051871","title":"Stochastic and scaling climate sensitivities: Solar, volcanic and orbital forcings","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Climatology; Scaling; Volcano; Climate change; Environmental science; Sensitivity (control systems); Forcing (mathematics); Range (aeronautics); Climate model; GCM transcription factors; Climate sensitivity; Statistical physics; Meteorology; Atmospheric sciences; Geology; Mathematics; General Circulation Model; Physics","score_opus":0.032470877202438964,"score_gpt":0.2922157576714093,"score_spread":0.2597448804689703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128639106","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.84952074,0.0010102907,0.11732365,0.0018132208,0.00009832963,0.000034659774,0.0010204825,0.0005192396,0.028659401],"genre_scores_gemma":[0.99659014,0.00013046889,0.0025228735,0.000054901673,0.000051954485,0.000009184699,0.00010509567,0.00003348942,0.0005019625],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99957055,0.00016317965,0.000026475169,0.00008948392,0.00010215028,0.000048221646],"domain_scores_gemma":[0.9968605,0.001861102,0.0005702401,0.0003957286,0.00020369973,0.00010870609],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013104285,0.00032302385,0.00020508668,0.0006738658,0.00025086847,0.0009368789,0.00027235213,0.00044643812,0.0014846043],"category_scores_gemma":[0.007524816,0.00029101942,0.00043627326,0.0007334191,0.0007411022,0.0011315165,0.00077615055,0.000494948,0.00015098894],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006492353,0.00004403382,0.05351585,0.00006890725,0.00011071273,0.00016641915,0.00024043792,0.8386601,0.006675683,0.07902217,0.0012912226,0.020139523],"study_design_scores_gemma":[0.000013718802,0.000041019124,0.117727384,0.000033168344,0.000031982825,0.0001878828,0.00008708213,0.75042737,0.0015633951,0.12560777,0.004188939,0.00009028671],"about_ca_topic_score_codex":0.0043001184,"about_ca_topic_score_gemma":0.0027989578,"teacher_disagreement_score":0.0043001184,"about_ca_system_score_codex":0.0006258508,"about_ca_system_score_gemma":0.0003147412,"threshold_uncertainty_score":0.008550167},"labels":[],"label_agreement":null},{"id":"W2128782888","doi":"10.1002/2014gl062180","title":"Axisymmetric circulation driven by marginal heating in ice‐covered lakes","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Ocean gyre; Buoyancy; Upwelling; Katabatic wind; Anticyclone; Oceanography; Flux (metallurgy); Atmospheric sciences; Mechanics","score_opus":0.05680019003576866,"score_gpt":0.30916239899091086,"score_spread":0.2523622089551422,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128782888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985089,0.00001588742,0.00041629214,0.000027364433,0.0000024709907,0.0000018411628,0.000042286778,0.00001897709,0.00096590543],"genre_scores_gemma":[0.9997203,0.0000106344105,0.00009734485,0.000003855858,0.0000033637934,0.0000017648017,0.00002952105,0.0000036626104,0.00012955847],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99998486,0.0000029559362,9.039882e-7,0.0000032789108,0.0000023935847,0.000005599825],"domain_scores_gemma":[0.99995446,0.000007253461,0.000011922517,0.0000026831588,0.000007694872,0.000015970683],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000039929317,0.00011916485,0.00011242991,0.00018106002,0.00028443008,0.00032867197,0.000112427224,0.00013015997,0.00083663303],"category_scores_gemma":[0.00013533547,0.00011830687,0.00014715508,0.0001308736,0.00033910855,0.00018190726,0.00032198126,0.00012962848,0.0000563375],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094609783,0.00020842606,0.36366826,0.0001091254,0.00022102638,0.0035575281,0.0022936994,0.20269217,0.3752747,0.02549904,0.0035554895,0.02197451],"study_design_scores_gemma":[0.000080856786,0.00014251539,0.43977347,0.000009440507,0.0000363621,0.00022251665,0.0003764334,0.54956436,0.0052994546,0.0032449584,0.0012089267,0.00004065603],"about_ca_topic_score_codex":0.007916866,"about_ca_topic_score_gemma":0.005183835,"teacher_disagreement_score":0.007916866,"about_ca_system_score_codex":0.0005009631,"about_ca_system_score_gemma":0.00030108675,"threshold_uncertainty_score":0.015741587},"labels":[],"label_agreement":null},{"id":"W2128834511","doi":"10.1002/2014gl061895","title":"Has the number of Indian summer monsoon depressions decreased over the last 30 years?","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Center for Prototype Climate Modeling, New York University Abu Dhabi; York University; Office of Naval Research; New York University Abu Dhabi; National Science Foundation","keywords":"Monsoon; Climatology; BENGAL; Bay; Monsoon of South Asia; Storm; Geology; Satellite; Environmental science; Geography; Oceanography","score_opus":0.04110339058403073,"score_gpt":0.30541222031991394,"score_spread":0.2643088297358832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128834511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9857737,0.0055329218,0.00014387305,0.0018496029,0.00013327278,0.000008528811,0.0038005863,0.00002737911,0.002730231],"genre_scores_gemma":[0.997844,0.001029298,0.000040979317,0.00011184372,0.0000838155,0.0000029950772,0.00069401617,0.0000026495493,0.00019036475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99947995,0.00007458806,0.000084573694,0.00015052252,0.000077123106,0.00013322844],"domain_scores_gemma":[0.99739754,0.00020673906,0.0014193779,0.00014957065,0.0005604299,0.0002664123],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070825394,0.00015209711,0.0002603234,0.0010763182,0.00025634887,0.0009556494,0.0004230683,0.00039142487,0.001648275],"category_scores_gemma":[0.0023101554,0.00012549825,0.00045806108,0.0025729367,0.00045816545,0.0006880996,0.00033147735,0.0006541521,0.00036283248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000072415874,0.0000120170325,0.9918064,0.00004998118,0.000092659924,0.00006358477,0.00014892823,0.000076755015,0.00021308563,0.00006843309,0.0005277162,0.006868128],"study_design_scores_gemma":[6.7499474e-7,0.000012129684,0.9989706,0.000009515834,0.00001914578,0.000062172105,0.00014785455,0.000047163277,0.000030399193,0.000010215329,0.0006877177,0.0000022446993],"about_ca_topic_score_codex":0.03137009,"about_ca_topic_score_gemma":0.04514528,"teacher_disagreement_score":0.03137009,"about_ca_system_score_codex":0.00068320736,"about_ca_system_score_gemma":0.00059839926,"threshold_uncertainty_score":0.06237501},"labels":[],"label_agreement":null},{"id":"W2128876288","doi":"10.1029/2001gl013485","title":"Formation and maintenance of the extratropical tropopause by baroclinic eddies","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Extratropical cyclone; Baroclinity; Tropopause; Eddy; Atmospheric sciences; Climatology; Middle latitudes; Cyclogenesis; Geology; Environmental science; Stratosphere; Atmosphere (unit); Lapse rate; Cyclone (programming language); Meteorology; Physics; Turbulence","score_opus":0.025908656204775924,"score_gpt":0.2785636022547396,"score_spread":0.25265494604996364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128876288","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939598,0.000105269784,0.0039056335,0.00006838287,0.000012608633,0.000008538363,0.000112296926,0.000051928815,0.0017755692],"genre_scores_gemma":[0.9992211,0.00004090116,0.00047558095,0.0000060615484,0.000002674296,0.0000040436767,0.00003610227,0.0000054121065,0.00020804926],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999652,0.000006199158,0.0000022353072,0.0000075879966,0.0000042585025,0.000014467528],"domain_scores_gemma":[0.9998971,0.000012679862,0.000027202484,0.000013400652,0.000010216421,0.00003938716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014402936,0.0001766252,0.00021712543,0.0001705731,0.0003324521,0.00066310714,0.00025495634,0.00032356847,0.0007504942],"category_scores_gemma":[0.0004477365,0.00023508898,0.00033430694,0.00011116367,0.00039637863,0.0004145182,0.00047476555,0.0001997518,0.000074206466],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047707921,0.00017769675,0.10930796,0.00015998312,0.0002488727,0.0008187364,0.0005478803,0.73609835,0.102858946,0.03275578,0.0017256788,0.014822987],"study_design_scores_gemma":[0.000220288,0.00010533921,0.06153183,0.000018246701,0.000074341355,0.00011468777,0.00015641852,0.9274672,0.0032951299,0.0054719984,0.0015142153,0.000030269663],"about_ca_topic_score_codex":0.0073720235,"about_ca_topic_score_gemma":0.0044144746,"teacher_disagreement_score":0.0073720235,"about_ca_system_score_codex":0.0004236771,"about_ca_system_score_gemma":0.00042149934,"threshold_uncertainty_score":0.014658213},"labels":[],"label_agreement":null},{"id":"W2128994117","doi":"10.1029/2003gl018807","title":"Bed topography and surges in ice streams","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Drag; Ice stream; Surge; Pressure ridge; Ice sheet; Mechanics; Flow (mathematics); Pancake ice; STREAMS; Drumlin; Geomorphology; Sea ice; Climatology; Physics; Cryosphere","score_opus":0.0373898105618802,"score_gpt":0.28198541039598063,"score_spread":0.24459559983410042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2128994117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99639845,0.000098627665,0.00046806922,0.000050552822,0.000008283873,0.0000067519504,0.00012395563,0.00003108935,0.0028141902],"genre_scores_gemma":[0.99937844,0.000075054835,0.00011515153,0.000006082692,0.000011867814,0.000001965097,0.00012314551,0.0000037045631,0.00028446052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999665,0.00000749743,0.0000027666172,0.0000051558623,0.000009341957,0.000008755892],"domain_scores_gemma":[0.999741,0.00008183103,0.00009137299,0.000015886984,0.000029987275,0.000039865936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009896429,0.00006313641,0.000110106885,0.0004957679,0.00018226022,0.00045639963,0.00009787645,0.00011460778,0.0017044313],"category_scores_gemma":[0.0007917982,0.00012428069,0.000079923215,0.00049147796,0.0002969036,0.00025318004,0.00020742751,0.00014073995,0.00022306688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007220115,0.00022754377,0.83396983,0.0002206,0.000080161546,0.0030216884,0.0026611902,0.0151094515,0.050401405,0.008147418,0.0037437535,0.0816949],"study_design_scores_gemma":[0.00002994401,0.00008410084,0.9880937,0.000012496552,0.000015624519,0.00024921226,0.0006660205,0.007604793,0.0007007845,0.0017280546,0.0008053436,0.000010078274],"about_ca_topic_score_codex":0.0024772673,"about_ca_topic_score_gemma":0.0032838772,"teacher_disagreement_score":0.0024772673,"about_ca_system_score_codex":0.00017474384,"about_ca_system_score_gemma":0.00011933429,"threshold_uncertainty_score":0.00570184},"labels":[],"label_agreement":null},{"id":"W2129641766","doi":"10.1029/2007gl031536","title":"Considerations for spaceborne 94 GHz radar observations of precipitation","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Precipitation Measurement and Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"","keywords":"Radar; Snow; Precipitation; Remote sensing; Environmental science; Sampling (signal processing); Doppler radar; Global Precipitation Measurement; Rain and snow mixed; Attenuation; Meteorology; Geology; Computer science; Optics; Physics; Telecommunications","score_opus":0.13708950086114363,"score_gpt":0.33337337337039435,"score_spread":0.19628387250925072,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129641766","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.25022742,0.02905828,0.51331216,0.14539033,0.002543928,0.0005009716,0.0014259233,0.0014680937,0.056072894],"genre_scores_gemma":[0.6472503,0.0106946975,0.3206802,0.009001824,0.0030619015,0.00045401728,0.00067625736,0.0002102762,0.00797054],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9973947,0.0010415117,0.00015919359,0.00023084819,0.0010686882,0.000105091276],"domain_scores_gemma":[0.989233,0.0067846966,0.00080548215,0.00073118915,0.0020385005,0.00040719498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006199077,0.0004154896,0.00048418657,0.0007537144,0.000761439,0.0017674302,0.0008669256,0.0021495721,0.0025699914],"category_scores_gemma":[0.013067488,0.00044502853,0.00039351988,0.00073428033,0.0010096994,0.0023233704,0.0008984443,0.0015956166,0.0009957294],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017530165,0.00019614334,0.052186113,0.001294635,0.00016250514,0.0020403299,0.001973802,0.032650616,0.122061,0.11780321,0.04316297,0.6247156],"study_design_scores_gemma":[0.0004676569,0.0030988613,0.16742668,0.0015817551,0.0003950189,0.009370126,0.008455354,0.10414911,0.04576661,0.15804768,0.50058925,0.00065189373],"about_ca_topic_score_codex":0.0035000825,"about_ca_topic_score_gemma":0.0048772455,"teacher_disagreement_score":0.006199077,"about_ca_system_score_codex":0.0006305986,"about_ca_system_score_gemma":0.0009797683,"threshold_uncertainty_score":0.032784224},"labels":[],"label_agreement":null},{"id":"W2129670970","doi":"10.1002/2015gl065066","title":"A method for estimating the height of a mesospheric density level using meteor radar","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Australian Antarctic Division; University of Adelaide; Australian Research Council; Administrative Sciences Association of Canada","keywords":"Meteor (satellite); Thermosphere; Microwave Limb Sounder; Radar; Mesosphere; Incoherent scatter; Airglow; Altitude (triangle); Atmosphere (unit); Environmental science; Remote sensing; Atmospheric sciences; Geology; Atmospheric sounding; Meteorology; Ionosphere; Troposphere; Geophysics; Physics; Stratosphere","score_opus":0.09051818454234217,"score_gpt":0.36883233571476653,"score_spread":0.27831415117242436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129670970","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1540615,0.00073719677,0.84038156,0.000046043213,0.000077868215,0.00008163391,0.00058416394,0.0016740025,0.0023560652],"genre_scores_gemma":[0.47323802,0.00034350634,0.52444273,0.000023566317,0.000057845482,0.00007092995,0.00049344153,0.00007306311,0.0012568253],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99985135,0.000020513353,0.000006979523,0.00004867748,0.000057659814,0.000014703455],"domain_scores_gemma":[0.9996363,0.000096424024,0.000070134054,0.000045243745,0.000121704725,0.000030134635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027056842,0.00030088704,0.0002537731,0.0013773134,0.00017064842,0.00040638572,0.00034288067,0.00027092797,0.000928925],"category_scores_gemma":[0.0006190924,0.00025662128,0.00018618225,0.0006131846,0.00014908933,0.00043430127,0.00034555467,0.00037357918,0.0005386226],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030619866,0.00005693663,0.034253903,0.00015261493,0.000077005505,0.00016136254,0.00016249587,0.008775856,0.4358019,0.0018946958,0.0013364385,0.5170207],"study_design_scores_gemma":[0.00012664817,0.00043352254,0.17761756,0.0000679832,0.00015440882,0.0016175493,0.0002538649,0.5857916,0.2160863,0.0032386472,0.014424164,0.0001877327],"about_ca_topic_score_codex":0.00095972035,"about_ca_topic_score_gemma":0.001125639,"teacher_disagreement_score":0.0013773134,"about_ca_system_score_codex":0.00014214408,"about_ca_system_score_gemma":0.00021152465,"threshold_uncertainty_score":0.0031076074},"labels":[],"label_agreement":null},{"id":"W2129754946","doi":"10.1029/2004gl021359","title":"Evidence for microbial enhanced electrical conductivity in hydrocarbon‐contaminated sediments","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"","keywords":"Microbial population biology; Environmental chemistry; Water column; Contamination; Weathering; Conductivity; Population; Microorganism; Environmental science; Geology; Mineralogy; Soil science; Chemistry; Ecology; Biology; Geochemistry; Oceanography; Bacteria","score_opus":0.0819608490583891,"score_gpt":0.3528195348855901,"score_spread":0.27085868582720096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2129754946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992937,0.00009323549,0.0002700873,0.000012041124,0.00000186665,0.000003420014,0.00010689857,0.000006717399,0.0002119141],"genre_scores_gemma":[0.9991211,0.00009096917,0.00038824306,0.000011664492,0.0000023367772,0.000004919796,0.00015770344,0.00000256519,0.00022033328],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9997825,0.000020857502,0.000018765013,0.00006313966,0.0000804157,0.000034328437],"domain_scores_gemma":[0.9996636,0.00005639922,0.0000934996,0.0000231916,0.00009614439,0.000067108595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001109506,0.000248321,0.00022180518,0.00028269956,0.00018500705,0.0004436644,0.0001272056,0.0002754965,0.0004336104],"category_scores_gemma":[0.00036372407,0.00019774007,0.00013884794,0.000212622,0.0003258605,0.00020359871,0.00038816768,0.00021920011,0.00011527495],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001479437,0.000016450827,0.014767334,0.000031078453,0.000008484182,0.000056488898,0.000042534175,0.00005606411,0.98398596,0.000019593534,0.0000070081633,0.00086111267],"study_design_scores_gemma":[0.000030891268,0.000615287,0.2964646,0.000011025666,0.00004207965,0.00062382326,0.00029956485,0.0009715949,0.7001364,0.00014961846,0.0006371498,0.00001801078],"about_ca_topic_score_codex":0.001299089,"about_ca_topic_score_gemma":0.0016457151,"teacher_disagreement_score":0.001299089,"about_ca_system_score_codex":0.00020714567,"about_ca_system_score_gemma":0.00020455274,"threshold_uncertainty_score":0.002583027},"labels":[],"label_agreement":null},{"id":"W2130270839","doi":"10.1029/2008gl034564","title":"Towards a robust test on North America warming trend and precipitable water content increase","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"University of Colorado Boulder; National Aeronautics and Space Administration","keywords":"Precipitable water; Relative humidity; Climatology; Environmental science; Water content; Meteorology; Series (stratigraphy); Humidity; Atmospheric sciences; Linear regression; Mathematics; Water vapor; Statistics; Geography; Physics; Geology","score_opus":0.08216145105859574,"score_gpt":0.27950404514882293,"score_spread":0.1973425940902272,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130270839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7819466,0.00047340823,0.2055364,0.0011598901,0.00014596053,0.00018243602,0.0016367465,0.00093798904,0.007980529],"genre_scores_gemma":[0.9627774,0.000048517923,0.03477793,0.00023566265,0.000078963756,0.0001217098,0.0012858735,0.0001134273,0.0005605628],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9764558,0.0147565175,0.00081513013,0.0051535205,0.0022030596,0.00061598764],"domain_scores_gemma":[0.83641964,0.13636974,0.011126885,0.011125347,0.0037153338,0.0012430026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.030071966,0.000727715,0.0014630641,0.001888794,0.0007697025,0.0019189935,0.0020539048,0.0017400458,0.0040008766],"category_scores_gemma":[0.1293167,0.0006867635,0.0014935994,0.0027882261,0.0025927853,0.002317298,0.0021577617,0.0022335176,0.00067982316],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.004463876,0.0009166964,0.63029927,0.0005025233,0.01115018,0.0012705259,0.0011940347,0.09891863,0.02569054,0.039421633,0.006124195,0.18004799],"study_design_scores_gemma":[0.00085524895,0.0032046353,0.43373248,0.00018938596,0.0010657996,0.00072031544,0.0010738146,0.4968263,0.0112610385,0.041973628,0.008902046,0.00019540741],"about_ca_topic_score_codex":0.004639476,"about_ca_topic_score_gemma":0.0027665552,"teacher_disagreement_score":0.030071966,"about_ca_system_score_codex":0.00056644715,"about_ca_system_score_gemma":0.0014896642,"threshold_uncertainty_score":0.15903765},"labels":[],"label_agreement":null},{"id":"W2130656353","doi":"10.1029/2000gl008483","title":"Energy balance at the Earth's surface: Heat flux history in eastern Canada","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Heat flux; Flux (metallurgy); Geothermal gradient; Energy balance; Environmental science; Geothermal energy; Geology; Geothermal heating; Geophysics; Range (aeronautics); Atmospheric sciences; Climatology; Heat transfer; Physics; Materials science; Mechanics; Thermodynamics","score_opus":0.011597030495918089,"score_gpt":0.2151787803935106,"score_spread":0.2035817498975925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130656353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.990615,0.0011352691,0.00018495563,0.00034729159,0.000005347527,0.000008458213,0.003446606,0.000021585645,0.0042355466],"genre_scores_gemma":[0.9973189,0.0004469161,0.00014440207,0.000023117289,0.0000012751777,0.0000020480948,0.0010097751,0.000005907405,0.0010477003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985576,0.000006027273,0.000006886605,0.000028335022,0.000044981956,0.00005799034],"domain_scores_gemma":[0.99965084,0.000027334452,0.000025128877,0.000010675129,0.0002333461,0.000052632695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020074713,0.00017796933,0.00028221967,0.0015444902,0.0015498113,0.001132459,0.00058398274,0.00024330337,0.0015619016],"category_scores_gemma":[0.00057894253,0.00014757733,0.00027080093,0.0032068503,0.0005895762,0.00043171152,0.0004610909,0.00031560595,0.00009971158],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023438052,0.000052896376,0.9186304,0.00015998309,0.00026639766,0.0004204394,0.0024079985,0.015610781,0.0044797715,0.003922911,0.0038402954,0.049973663],"study_design_scores_gemma":[0.000007719209,0.000005141332,0.9891055,0.000028055667,0.000032627937,0.00003646149,0.000866875,0.004368256,0.00060075603,0.00025736308,0.004662488,0.000028743978],"about_ca_topic_score_codex":0.99779236,"about_ca_topic_score_gemma":0.99851733,"teacher_disagreement_score":0.029566359,"about_ca_system_score_codex":0.029566359,"about_ca_system_score_gemma":0.015324626,"threshold_uncertainty_score":0.21451998},"labels":[],"label_agreement":null},{"id":"W2130725980","doi":"10.1029/2003gl018012","title":"Gale force winds over the Irminger Sea to the east of Cape Farewell, Greenland","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Climatology; Geology; Oceanography; Cape; Deep convection; Forcing (mathematics); Tropical cyclone; Convection; Meteorology; Geography","score_opus":0.04019858722972577,"score_gpt":0.2976624985460752,"score_spread":0.25746391131634944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2130725980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998762,0.000051054543,0.000020800515,0.00006180499,0.0000025158843,0.0000033278218,0.00025287658,0.0000046238993,0.0008409644],"genre_scores_gemma":[0.99861825,0.0001224179,0.00011988057,0.0000334439,0.0000045475135,0.0000035255796,0.00036743656,0.000001911401,0.00072857813],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999633,0.000004259591,0.0000014192904,0.0000096790745,0.00000809071,0.0000131808765],"domain_scores_gemma":[0.9999206,0.000008345787,0.00003064968,0.000004078253,0.000015442994,0.000020852565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007828582,0.00013799555,0.00008890424,0.0004501793,0.000283803,0.00027010034,0.00012783986,0.0001012379,0.00096171116],"category_scores_gemma":[0.0002530198,0.00004957412,0.00008535407,0.00037369155,0.0001754544,0.00016039098,0.00025982375,0.0001274658,0.00006184244],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013548779,0.00006324969,0.95618856,0.000048534406,0.000103748534,0.0012190477,0.00096314255,0.0045265327,0.006490975,0.0003397601,0.0033461722,0.026574725],"study_design_scores_gemma":[0.0000075256694,0.000010825106,0.9978631,0.00000783028,0.000007909763,0.00003857527,0.0002255239,0.0007277793,0.00013277226,0.000029965478,0.00094518665,0.000002967485],"about_ca_topic_score_codex":0.40546763,"about_ca_topic_score_gemma":0.6939935,"teacher_disagreement_score":0.40546763,"about_ca_system_score_codex":0.0013288979,"about_ca_system_score_gemma":0.000686596,"threshold_uncertainty_score":0.8062151},"labels":[],"label_agreement":null},{"id":"W2131159450","doi":"10.1029/2006gl027600","title":"Temporal decrease in upper atmospheric chlorine","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Microwave Limb Sounder; Chlorine; Environmental science; Hydrogen chloride; Atmospheric sciences; Ozone; Context (archaeology); Stratosphere; Ozone layer; Satellite; Atmosphere (unit); Atmospheric chemistry; Climatology; Meteorology; Chemistry; Geology; Physics","score_opus":0.01996456178088597,"score_gpt":0.26773923136769057,"score_spread":0.2477746695868046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131159450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99237317,0.001010894,0.0002947185,0.00022039044,0.000024937157,0.000008103085,0.003199499,0.000074326716,0.002793867],"genre_scores_gemma":[0.99539703,0.00029711617,0.00028523643,0.0001452215,0.000026010097,0.000010954091,0.002811614,0.000006785657,0.0010201089],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998914,0.000008810903,0.0000083966215,0.000043482425,0.000027499447,0.000020404812],"domain_scores_gemma":[0.9994424,0.000053414307,0.00019225181,0.00004265543,0.00022075018,0.000048449067],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020467116,0.00011940304,0.00019194874,0.0005325475,0.0002840642,0.00043541988,0.00019779173,0.00028526163,0.0012944057],"category_scores_gemma":[0.00056950416,0.000095219766,0.00012988015,0.0005664819,0.00012702632,0.00028311278,0.00030882054,0.00028339605,0.00026402102],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006015211,0.00009565016,0.92210907,0.000121138655,0.00016201551,0.0002368803,0.00057177426,0.00039460754,0.034294177,0.00019722487,0.003276937,0.037938874],"study_design_scores_gemma":[0.0000028217269,0.00006521421,0.9932836,0.0000056956105,0.000017928145,0.00012328694,0.000062245526,0.00018106942,0.0025933066,0.00002395528,0.003636599,0.000004243576],"about_ca_topic_score_codex":0.011384871,"about_ca_topic_score_gemma":0.014540519,"teacher_disagreement_score":0.011384871,"about_ca_system_score_codex":0.0003274082,"about_ca_system_score_gemma":0.00020647798,"threshold_uncertainty_score":0.022637188},"labels":[],"label_agreement":null},{"id":"W2131539855","doi":"10.1029/2003gl019106","title":"Vertical crustal motion determined by satellite altimetry and tide gauge data in Fennoscandia","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":94,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Tide gauge; Post-glacial rebound; Geodesy; Geology; Altimeter; Sea level; Satellite altimetry; Satellite geodesy; Global Positioning System; Satellite; Geodetic datum; Ocean tide; Climatology; Oceanography","score_opus":0.05523044382918108,"score_gpt":0.3010945617664081,"score_spread":0.245864117937227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131539855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936575,0.0003390511,0.0035430097,0.000057668516,0.000016596752,0.000012562592,0.0006150862,0.000049213864,0.0017092272],"genre_scores_gemma":[0.9877857,0.00015195603,0.010396901,0.000020712576,0.000007878689,0.000015746553,0.0011531659,0.000013440769,0.00045450396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99953926,0.000078126934,0.000028309792,0.00014837898,0.00011873296,0.00008717528],"domain_scores_gemma":[0.99959713,0.000048495538,0.000078832396,0.000052627456,0.0001717972,0.000051094747],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001026681,0.00043414292,0.00034855687,0.0020497816,0.00054357306,0.0007923968,0.00049016165,0.00029581494,0.000501823],"category_scores_gemma":[0.0019415193,0.00031563634,0.0003729675,0.002836193,0.00029261972,0.00045372668,0.0006372678,0.0003133705,0.00010219377],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012592986,0.00003560806,0.8297414,0.00004545089,0.00035395625,0.00018662502,0.00039654394,0.032951128,0.0063437773,0.0004738301,0.0007270642,0.12861858],"study_design_scores_gemma":[0.000017378676,0.000031922787,0.9534549,0.00003265726,0.00006737269,0.00007248065,0.00025673353,0.04211473,0.0016337913,0.00023966742,0.0020511895,0.00002704494],"about_ca_topic_score_codex":0.41698444,"about_ca_topic_score_gemma":0.5438136,"teacher_disagreement_score":0.41698444,"about_ca_system_score_codex":0.0018012226,"about_ca_system_score_gemma":0.0019147405,"threshold_uncertainty_score":0.8291147},"labels":[],"label_agreement":null},{"id":"W2131825986","doi":"10.1002/grl.50641","title":"The Novaya Zemlya Bora and its impact on Barents Sea air‐sea interaction","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Archipelago; Geology; Arctic; The arctic; Prevailing winds; Oceanography; Climatology; Wind speed","score_opus":0.02325113532150634,"score_gpt":0.30817810355981495,"score_spread":0.2849269682383086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131825986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699867,0.00017472538,0.00003088734,0.00012040832,0.00001416936,0.0000029046023,0.00022312131,0.000005487907,0.0024296755],"genre_scores_gemma":[0.9991954,0.000090148285,0.00003734065,0.000011963654,0.0000046795685,0.0000021224816,0.00018698425,0.0000037359189,0.00046777772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998995,0.000013722764,0.000005481309,0.000017994695,0.000017965784,0.000045226105],"domain_scores_gemma":[0.9998115,0.000021114784,0.000057937694,0.000011067023,0.000023748347,0.000074732154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020728871,0.00015169677,0.00027292373,0.00041284456,0.0011082169,0.0015068916,0.00018732333,0.00023301585,0.0013379736],"category_scores_gemma":[0.0004311292,0.00010706976,0.0002237148,0.0003451385,0.0005608161,0.00027104863,0.0013162186,0.00037155545,0.00016543557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007361062,0.000095375704,0.9658948,0.00008697948,0.00014855401,0.0017912193,0.0015610156,0.0036080321,0.008992428,0.0013073895,0.0015453385,0.014232757],"study_design_scores_gemma":[0.000006725415,0.000021886835,0.9961618,0.000012540643,0.000007666336,0.0000468718,0.0006813794,0.0004168326,0.00013294847,0.0000644759,0.0024423613,0.0000043873138],"about_ca_topic_score_codex":0.07431138,"about_ca_topic_score_gemma":0.113731325,"teacher_disagreement_score":0.07431138,"about_ca_system_score_codex":0.0016161143,"about_ca_system_score_gemma":0.0009025902,"threshold_uncertainty_score":0.14775765},"labels":[],"label_agreement":null},{"id":"W2131976712","doi":"10.1002/2014gl062610","title":"Swarm in situ observations of <b><i>F</i></b> region polar cap patches created by cusp precipitation","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Alberta; University of Saskatchewan","funders":"Canadian Space Agency; Norges Forskningsråd; European Space Agency","keywords":"In situ; Polar; Polar cap; Cusp (singularity); Precipitation; Swarm behaviour; Geology; Physics; Atmospheric sciences; Meteorology; Geometry; Astronomy; Mathematics","score_opus":0.04596316658550865,"score_gpt":0.2959665913275916,"score_spread":0.250003424742083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131976712","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970983,0.000022576953,0.0005741823,0.00001706117,0.000006095769,0.000005473125,0.00023954523,0.000053593194,0.0019831925],"genre_scores_gemma":[0.9988558,0.000013782557,0.00069510035,0.0000099558165,0.0000055308356,0.000003598729,0.0002147746,0.000010175693,0.00019135066],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999629,0.000003090627,0.0000013338208,0.000012270221,0.0000092563805,0.000011145102],"domain_scores_gemma":[0.9998982,0.00001487262,0.000025228393,0.000013905893,0.000017902496,0.000029860708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009598289,0.00012915174,0.0001381725,0.00031776013,0.00030056218,0.00035234774,0.00015962157,0.00022884201,0.00083122164],"category_scores_gemma":[0.00014300847,0.00012176461,0.0001339733,0.00018524236,0.00019228543,0.00016793673,0.00023752904,0.00019843814,0.00015985065],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061415,0.000108600514,0.25896987,0.00007189757,0.00010095244,0.00056920736,0.0012424358,0.0013265507,0.71858656,0.00022856501,0.0015166128,0.016664617],"study_design_scores_gemma":[0.00003075155,0.0001238255,0.9703368,0.0000070759597,0.000036347596,0.0002617671,0.00047539134,0.004648213,0.022288581,0.00007561401,0.0017047024,0.000010897449],"about_ca_topic_score_codex":0.0033283418,"about_ca_topic_score_gemma":0.006088809,"teacher_disagreement_score":0.0033283418,"about_ca_system_score_codex":0.00014771784,"about_ca_system_score_gemma":0.00006726842,"threshold_uncertainty_score":0.0066179633},"labels":[],"label_agreement":null},{"id":"W2131992829","doi":"10.1029/2002gl015511","title":"Evidence for both crustal and mantle earthquakes in the subducting Juan de Fuca plate","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Geology; Seismology; Induced seismicity; Receiver function; Mantle (geology); Crust; Intraplate earthquake; Subduction; Oceanic crust; Geophysics; Tectonics; Lithosphere","score_opus":0.13049638660479815,"score_gpt":0.34409689491728235,"score_spread":0.2136005083124842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2131992829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994011,0.000051156097,0.000025782361,0.000013200252,5.5090453e-7,5.8802476e-7,0.000027476293,0.0000021286094,0.00047801767],"genre_scores_gemma":[0.99970275,0.000039359187,0.000039639257,0.0000034478865,0.0000013638639,8.834189e-7,0.00007065263,5.156162e-7,0.00014142314],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998709,0.000012672228,0.000007428591,0.000030139265,0.000033260865,0.00004557104],"domain_scores_gemma":[0.99915695,0.00014772412,0.00034508127,0.000066608605,0.0001572236,0.00012648388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018219453,0.00017478765,0.00011534092,0.000758913,0.00033997107,0.00044902557,0.0001790546,0.00027274012,0.0007337487],"category_scores_gemma":[0.0014577542,0.00017502115,0.00006526125,0.00071379024,0.0006809994,0.00018113428,0.0004391569,0.00013292705,0.00010086201],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008829999,0.000008782503,0.98035973,0.000020266956,0.000018777542,0.0001877893,0.00070840865,0.00025973612,0.012106286,0.000105506544,0.000045900528,0.0060903328],"study_design_scores_gemma":[0.0000018201739,0.000007874194,0.99931276,0.0000023388309,0.000003338633,0.00010012796,0.00021121801,0.00007473949,0.00014679,0.000018117753,0.000118901036,0.0000019942868],"about_ca_topic_score_codex":0.08522281,"about_ca_topic_score_gemma":0.1361606,"teacher_disagreement_score":0.08522281,"about_ca_system_score_codex":0.0005551266,"about_ca_system_score_gemma":0.00042763472,"threshold_uncertainty_score":0.1694535},"labels":[],"label_agreement":null},{"id":"W2132298983","doi":"10.1002/2014gl059251","title":"New permafrost is forming around shrinking Arctic lakes, but will it last?","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Permafrost; Aggradation; Geology; Ecological succession; Climate change; Environmental science; Hydrology (agriculture); Global warming; Physical geography; Geomorphology; Ecology; Oceanography; Structural basin; Geotechnical engineering; Geography","score_opus":0.05854334567834521,"score_gpt":0.29829003638479007,"score_spread":0.23974669070644486,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132298983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990421,0.000054788783,0.00011996268,0.00010920945,0.0000032941496,9.876691e-7,0.00002627579,0.000007570625,0.00063571497],"genre_scores_gemma":[0.99983156,0.000026714204,0.00006418834,0.000006047319,0.000001390297,3.507904e-7,0.000012388841,9.773886e-7,0.00005638858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999671,0.0000073437877,0.0000020219795,0.000007810371,0.0000046782548,0.000011090978],"domain_scores_gemma":[0.9998989,0.000015436328,0.000032748183,0.0000072969888,0.000015402917,0.000030162048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014991057,0.00008362034,0.00015571828,0.0001791733,0.0006163915,0.0006752303,0.00018510656,0.00024456394,0.0013753322],"category_scores_gemma":[0.00032089735,0.00008643418,0.00015860703,0.00019220862,0.00054248015,0.00046942444,0.00030151158,0.00015859658,0.00005061604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001919828,0.00006198087,0.93381065,0.00007577922,0.00010261968,0.0005438037,0.00089664146,0.042758487,0.008801277,0.0028289934,0.0005221805,0.009405525],"study_design_scores_gemma":[0.000027949336,0.00013789881,0.896596,0.00004619507,0.000060607606,0.00027859912,0.0044159675,0.09123272,0.0015849291,0.003363017,0.002227487,0.000028623546],"about_ca_topic_score_codex":0.027020168,"about_ca_topic_score_gemma":0.055668272,"teacher_disagreement_score":0.027020168,"about_ca_system_score_codex":0.00060067896,"about_ca_system_score_gemma":0.00037330578,"threshold_uncertainty_score":0.05372578},"labels":[],"label_agreement":null},{"id":"W2132413867","doi":"10.1029/2010gl044867","title":"Recent shoaling of the nutricline and thermocline in the western tropical Pacific","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Andrew W. Mellon Foundation; Geological Society of America; Woods Hole Oceanographic Institution; PADI Foundation; National Science Foundation","keywords":"Thermocline; Oceanography; Walker circulation; Geology; Shoaling and schooling; Photic zone; Climatology; Sea surface temperature; Phytoplankton","score_opus":0.030275566934081375,"score_gpt":0.2949988331373122,"score_spread":0.2647232662032308,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132413867","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991454,0.0001704484,0.00006298796,0.000029327759,0.0000021461487,0.0000013134153,0.00007149386,0.000004827518,0.00051203405],"genre_scores_gemma":[0.9994185,0.00018534683,0.00012630578,0.000018563844,0.0000045621123,0.0000020885875,0.00010026374,0.000002124805,0.00014220456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.0000035536038,0.0000048538855,0.000011223798,0.000008414384,0.000006142912],"domain_scores_gemma":[0.9997378,0.000025987109,0.00011735217,0.000019566362,0.00006267891,0.00003653512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013401086,0.00010469691,0.00010709273,0.00046343004,0.00033783767,0.00043974293,0.0001087731,0.0001425127,0.0004924733],"category_scores_gemma":[0.00053878356,0.00012733362,0.000075280725,0.0006102232,0.00047805544,0.0002866862,0.00038716246,0.00017701095,0.00006022186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000073891795,0.000009278919,0.9642945,0.00004465143,0.00004193118,0.00016617554,0.00083645503,0.00019363224,0.021885986,0.000075173404,0.00012729195,0.012250972],"study_design_scores_gemma":[9.2546776e-7,0.0000075998255,0.99924004,0.0000017590855,0.000005589467,0.00007390269,0.00015141463,0.000045786026,0.00022377225,0.000013614377,0.00023396133,0.0000017065519],"about_ca_topic_score_codex":0.013350406,"about_ca_topic_score_gemma":0.03482067,"teacher_disagreement_score":0.013350406,"about_ca_system_score_codex":0.0002712208,"about_ca_system_score_gemma":0.00024027054,"threshold_uncertainty_score":0.026545405},"labels":[],"label_agreement":null},{"id":"W2132534227","doi":"10.1029/2002gl015484","title":"Substorm onset location and the equatorward boundary of the proton auroral oval","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Substorm; Geophysics; Proton; Geology; Boundary (topology); Interplanetary magnetic field; Interplanetary spaceflight; Polar; Magnetosphere; Physics; Magnetic field; Solar wind; Astronomy","score_opus":0.01946966485978836,"score_gpt":0.26802019318203524,"score_spread":0.2485505283222469,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132534227","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99603707,0.00015522461,0.00104315,0.000016416556,0.0000049946484,0.000005590647,0.00017063592,0.00002393148,0.0025431444],"genre_scores_gemma":[0.99923337,0.00006347771,0.00028090278,0.0000046318996,0.0000049578757,0.0000025632037,0.00013382366,0.000004770217,0.00027141254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.000007999967,0.00000440533,0.000012978125,0.000010937038,0.00001930234],"domain_scores_gemma":[0.9995401,0.000086119806,0.00016205298,0.000026786407,0.00011521048,0.00006978945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000108595676,0.000059143702,0.00011706214,0.00034548022,0.00020768894,0.0002651403,0.000051869843,0.000081260565,0.0016619397],"category_scores_gemma":[0.000564854,0.000049630595,0.00005892606,0.0001705474,0.00018406358,0.00020808815,0.0002071591,0.00013020106,0.00028887705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011676381,0.00003328341,0.6275004,0.000085052576,0.000025797886,0.0015292712,0.0012315157,0.0007567218,0.31979826,0.0014592025,0.0007303611,0.04568253],"study_design_scores_gemma":[0.0000100534035,0.000058373473,0.98788005,0.000009481272,0.000008902874,0.00058156066,0.0002618706,0.00033092182,0.009096342,0.00016880715,0.0015893225,0.0000042766874],"about_ca_topic_score_codex":0.0018217275,"about_ca_topic_score_gemma":0.0024254299,"teacher_disagreement_score":0.0018217275,"about_ca_system_score_codex":0.00012561581,"about_ca_system_score_gemma":0.00008852314,"threshold_uncertainty_score":0.005559683},"labels":[],"label_agreement":null},{"id":"W2132846084","doi":"10.1029/2007gl031106","title":"Signal strength and climate calibration of a European tree‐ring isotope network","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":225,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Dendroclimatology; Precipitation; Temperate climate; Mediterranean climate; Environmental science; Dendrochronology; Climatology; Principal component analysis; Climate change; Physical geography; Geography; Atmospheric sciences; Geology; Ecology; Meteorology; Biology","score_opus":0.031969756068550154,"score_gpt":0.28317373884330893,"score_spread":0.25120398277475875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132846084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962339,0.000099656056,0.0026507,0.000023019711,0.000005305972,0.000004449562,0.00036536687,0.000027559474,0.0005901203],"genre_scores_gemma":[0.9975526,0.000024314611,0.0017871897,0.0000064600563,0.0000033722406,0.000004657319,0.00055608235,0.000008522625,0.000056886867],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99933773,0.00029125722,0.000031422765,0.00021461546,0.00005710253,0.0000678449],"domain_scores_gemma":[0.99784577,0.0007777453,0.0004002711,0.00033229784,0.00051060854,0.00013320598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023074632,0.00029851546,0.00023503003,0.00068939995,0.00022225143,0.0005754061,0.00043522214,0.00033989688,0.00045041196],"category_scores_gemma":[0.005301895,0.00017811041,0.00017600987,0.00074486004,0.00023249544,0.00042169527,0.00049830426,0.00015540425,0.000118811186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005775701,0.00004900507,0.89700234,0.00004429469,0.00024754176,0.00015481553,0.0002366407,0.043696254,0.021522695,0.0010065511,0.00059300975,0.03486921],"study_design_scores_gemma":[0.000039613966,0.000058160997,0.89471596,0.000016448786,0.00007727967,0.00017707907,0.000069550675,0.09784645,0.0050408132,0.0005073045,0.0014287023,0.0000226998],"about_ca_topic_score_codex":0.0069198795,"about_ca_topic_score_gemma":0.00750593,"teacher_disagreement_score":0.0069198795,"about_ca_system_score_codex":0.00039437838,"about_ca_system_score_gemma":0.00024796778,"threshold_uncertainty_score":0.013759196},"labels":[],"label_agreement":null},{"id":"W2132858992","doi":"10.1029/2004gl021947","title":"Recent ice loss from the Fleming and other glaciers, Wordie Bay, West Antarctic Peninsula","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":109,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Jet Propulsion Laboratory; European Space Agency; California Institute of Technology; Goddard Space Flight Center; Tinker Foundation","keywords":"Geology; Ice shelf; Glacier; Oceanography; Thinning; Antarctic sea ice; Ice stream; Peninsula; Cryosphere; Bay; Glacier ice accumulation; Front (military); Iceberg; Ice sheet; Glacier mass balance; Snow; Sea ice; Climatology; Geomorphology; Geography","score_opus":0.04625444829606914,"score_gpt":0.28983841699091145,"score_spread":0.2435839686948423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132858992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99818856,0.00014086568,0.000021556354,0.000031942312,0.0000031548489,0.000002346545,0.0008690049,0.0000038742146,0.0007386309],"genre_scores_gemma":[0.99435306,0.00048066958,0.0001447781,0.00003876331,0.0000052587116,0.000007752891,0.003196193,0.0000043699065,0.0017692217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991906,0.000004734076,0.00001070732,0.00002275184,0.000020789825,0.000021990767],"domain_scores_gemma":[0.9996853,0.00002311255,0.00015417355,0.000022706185,0.000073045805,0.000041671803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015593877,0.00024604207,0.00017712187,0.00090788613,0.000533583,0.0006188113,0.00016894183,0.00016457653,0.0011741649],"category_scores_gemma":[0.00052375696,0.00013685941,0.0001436493,0.0012847712,0.00040662754,0.0006738363,0.00042590103,0.00019049668,0.00025718095],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009507675,0.000012801841,0.9817139,0.00004344661,0.000050342078,0.0002711017,0.00092720444,0.00025311473,0.0026451207,0.00005022071,0.0006476716,0.013289985],"study_design_scores_gemma":[8.1974355e-7,0.000008298958,0.9985024,0.000004466926,0.00000601465,0.00005634026,0.00027998665,0.000034585988,0.0001733829,0.000007827738,0.0009239128,0.0000020427783],"about_ca_topic_score_codex":0.121985115,"about_ca_topic_score_gemma":0.3529486,"teacher_disagreement_score":0.121985115,"about_ca_system_score_codex":0.0009596902,"about_ca_system_score_gemma":0.0006077946,"threshold_uncertainty_score":0.24255013},"labels":[],"label_agreement":null},{"id":"W2132889817","doi":"10.1029/2000gl012603","title":"Magnification of atmospheric mercury deposition to polar regions in springtime: The link to tropospheric ozone depletion chemistry","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":269,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Research Manitoba; Environment and Climate Change Canada","funders":"","keywords":"Mercury (programming language); Biogeochemical cycle; Arctic; Snow; Environmental science; Environmental chemistry; Ozone depletion; Troposphere; Atmospheric sciences; Ozone; Meteorology; Chemistry; Oceanography; Geology; Geography","score_opus":0.024587562943959973,"score_gpt":0.30148295136992104,"score_spread":0.27689538842596106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132889817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942642,0.00076019025,0.0002135603,0.00042029485,0.000030671887,0.0000046437153,0.0005899598,0.00003047775,0.0036859938],"genre_scores_gemma":[0.9982021,0.00036524897,0.000088337416,0.000065260596,0.000046055673,0.0000028550821,0.00028870103,0.0000050749563,0.0009362312],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996614,0.000006103544,0.0000016123101,0.000009459793,0.000007330975,0.0000093384615],"domain_scores_gemma":[0.99985003,0.000030359291,0.000037929938,0.000013134101,0.000035134195,0.000033420485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012266664,0.00017302137,0.00015069984,0.000499189,0.00047652837,0.00044702942,0.00015171993,0.00024080146,0.0027998618],"category_scores_gemma":[0.0002612608,0.00009737765,0.00012900896,0.00047624134,0.00020405833,0.00016263356,0.00029099666,0.00021047707,0.0002784225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016425602,0.00008136281,0.87814766,0.00018600206,0.0001694308,0.0006556658,0.0012212859,0.00039094247,0.08524137,0.0006249251,0.0021739241,0.029464977],"study_design_scores_gemma":[0.000004651026,0.00003067383,0.9974975,0.0000036045824,0.000014258072,0.00006443515,0.0002390748,0.00006168119,0.0012806569,0.00007507142,0.0007263709,0.0000018221601],"about_ca_topic_score_codex":0.02273336,"about_ca_topic_score_gemma":0.026156124,"teacher_disagreement_score":0.02273336,"about_ca_system_score_codex":0.0003201209,"about_ca_system_score_gemma":0.0002573706,"threshold_uncertainty_score":0.045202076},"labels":[],"label_agreement":null},{"id":"W2132983905","doi":"10.1029/2012gl053381","title":"North Atlantic wave height trends as reconstructed from the 20th century reanalysis","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Significant wave height; Classification of discontinuities; Latitude; Geology; Homogeneous; North Atlantic oscillation; Geography; Geodesy; Oceanography; Wind wave; Mathematics","score_opus":0.04250563141105721,"score_gpt":0.2862113469419558,"score_spread":0.24370571553089862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2132983905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9798869,0.00054515124,0.0010769112,0.00013083353,0.00005299812,0.0000066489147,0.014205029,0.00008797211,0.004007475],"genre_scores_gemma":[0.9616122,0.0012183636,0.0015274577,0.000035724934,0.00005210986,0.000017583177,0.033948015,0.000032059008,0.0015564052],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984837,0.000018173752,0.000018153863,0.0000366707,0.000053525062,0.000025192132],"domain_scores_gemma":[0.9995437,0.00004620183,0.00019225334,0.00004845717,0.00014517069,0.000024311805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040618202,0.00024248679,0.00015570596,0.0012679049,0.00012765737,0.0005203814,0.00014968432,0.00013902917,0.00095300586],"category_scores_gemma":[0.001179298,0.00014069461,0.0003808692,0.0018571024,0.00011757774,0.0004227627,0.00033057696,0.0003000574,0.00040835285],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011732158,0.000045125416,0.92963684,0.00008677463,0.00039313268,0.000083999534,0.0002804605,0.016502934,0.0015169462,0.0011312447,0.00602508,0.044180024],"study_design_scores_gemma":[0.00000474542,0.000019223115,0.98817897,0.000016922926,0.000041613777,0.00003644255,0.00008014185,0.0056925905,0.0003926193,0.0001223608,0.0053994553,0.000014896534],"about_ca_topic_score_codex":0.029297542,"about_ca_topic_score_gemma":0.045058783,"teacher_disagreement_score":0.029297542,"about_ca_system_score_codex":0.0004501173,"about_ca_system_score_gemma":0.00043082377,"threshold_uncertainty_score":0.058254004},"labels":[],"label_agreement":null},{"id":"W2133057110","doi":"10.1029/2012gl053892","title":"Effects of subducted seamounts on megathrust earthquake nucleation and rupture propagation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Seamount; Geology; Subduction; Seismology; Trench; Episodic tremor and slip; Nucleation; Tectonics; Oceanography; Materials science","score_opus":0.022354555514667283,"score_gpt":0.2668477002257578,"score_spread":0.24449314471109054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133057110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995528,0.00003336985,0.00016746859,0.0000057755374,0.0000012935108,0.0000014519248,0.000016675898,0.000008146848,0.00021304254],"genre_scores_gemma":[0.9998048,0.000020583375,0.00011882476,0.0000016728237,3.1905913e-7,0.000001118008,0.000012967876,0.0000011797632,0.000038545313],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999069,0.000016419484,0.000010811554,0.00002127406,0.00001656557,0.00002792875],"domain_scores_gemma":[0.9994029,0.00025301543,0.00013865557,0.00007465582,0.000033250653,0.0000975922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022131107,0.00020816295,0.0003089207,0.00026045126,0.0002975823,0.00044397305,0.00031958026,0.00028694462,0.001253495],"category_scores_gemma":[0.0013385019,0.00019670842,0.00021263013,0.00016331031,0.0004697418,0.0002999902,0.00052935584,0.0002263327,0.00006567141],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022059751,0.0004432877,0.1760039,0.00043206938,0.00020443798,0.0012778325,0.00066676043,0.29467517,0.502268,0.0030606796,0.00021676101,0.018545102],"study_design_scores_gemma":[0.00014853568,0.0024813784,0.32687017,0.000062979256,0.00020576363,0.00034866278,0.0007695241,0.5149005,0.15195288,0.0012985329,0.00088571385,0.00007531293],"about_ca_topic_score_codex":0.0038674155,"about_ca_topic_score_gemma":0.003349674,"teacher_disagreement_score":0.0038674155,"about_ca_system_score_codex":0.00037281943,"about_ca_system_score_gemma":0.00021058106,"threshold_uncertainty_score":0.0076898336},"labels":[],"label_agreement":null},{"id":"W2133106709","doi":"10.1029/2009gl037341","title":"Tracer‐derived freshwater composition of the Siberian continental shelf and slope following the extreme Arctic summer of 2007","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Office of Polar Programs; Natural Environment Research Council; Sight Research UK; Alberta Agricultural Research Institute; National Science Foundation","keywords":"Oceanography; Arctic; TRACER; Geology; Ridge; Sea ice; Continental shelf; Water mass; The arctic; Barium; Climatology; Paleontology","score_opus":0.026344097501113987,"score_gpt":0.25637256658380353,"score_spread":0.23002846908268954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133106709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993368,0.000037993243,0.000026031192,0.000008310108,0.0000020163698,0.0000010164415,0.00037300427,0.0000030055312,0.00021178645],"genre_scores_gemma":[0.99817634,0.000056490775,0.00007957176,0.000009778932,0.0000029220444,0.00000470164,0.0015126434,0.0000029842179,0.00015443123],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.0000076025935,0.00000530488,0.0000133750345,0.000007613615,0.0000121759],"domain_scores_gemma":[0.99985874,0.000010780526,0.000041859363,0.000012269434,0.00004367946,0.00003276008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022976879,0.0002472239,0.00028582188,0.0007838868,0.0005306699,0.00047783766,0.00020751337,0.00021864382,0.00064881676],"category_scores_gemma":[0.00031370585,0.0001321571,0.0002591044,0.00068748347,0.0001839457,0.0002648828,0.000461152,0.0001519542,0.00018302108],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014358306,0.00002541687,0.98784816,0.000014655908,0.000082029524,0.00012292384,0.00024359865,0.0006958241,0.0066439393,0.000031573636,0.0001664689,0.0039817565],"study_design_scores_gemma":[0.0000024116655,0.000011227782,0.99903655,0.0000028280704,0.000008316886,0.000022485661,0.00006281033,0.00045423087,0.00023767729,0.0000070740575,0.00015227283,0.0000020657874],"about_ca_topic_score_codex":0.044556655,"about_ca_topic_score_gemma":0.072652236,"teacher_disagreement_score":0.044556655,"about_ca_system_score_codex":0.0006574541,"about_ca_system_score_gemma":0.00047806755,"threshold_uncertainty_score":0.088594615},"labels":[],"label_agreement":null},{"id":"W2133252855","doi":"10.1029/2006gl028546","title":"Effects of bottom boundary placement on subsurface heat storage: Implications for climate model simulations","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Boundary (topology); Environmental science; Boundary value problem; Climate model; Geology; Thermal energy storage; Climate change; Climatology; Atmospheric sciences; Meteorology; Mathematics; Thermodynamics; Physics","score_opus":0.06777984500004894,"score_gpt":0.35360577160427525,"score_spread":0.28582592660422634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133252855","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99115026,0.000114141396,0.0055261673,0.00025553798,0.00003698211,0.00001907949,0.0005057334,0.00012735774,0.0022647262],"genre_scores_gemma":[0.99798065,0.000044286677,0.0015163269,0.000033454373,0.0000038470857,0.00001690619,0.00019613477,0.00003866147,0.00016979295],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999645,0.00017721078,0.000019148589,0.00004367275,0.000042944765,0.00007197315],"domain_scores_gemma":[0.99792385,0.001317922,0.00018262348,0.00013467981,0.00020916469,0.00023177253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010512148,0.00071386475,0.00091143016,0.00044854663,0.0009610091,0.0013859173,0.0007136365,0.0011477416,0.0018627811],"category_scores_gemma":[0.0049740877,0.0005332194,0.00078315026,0.00051876483,0.00090783724,0.0012935706,0.0010658539,0.001002107,0.00016641444],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015549456,0.00004501125,0.010938386,0.000022210897,0.000019976935,0.00006540391,0.00002901232,0.984461,0.0021374929,0.000757102,0.00021742086,0.0011514552],"study_design_scores_gemma":[0.00006975233,0.00008746559,0.004096168,0.000018065542,0.000029110393,0.000013864573,0.00008313034,0.99244213,0.0018892575,0.0010204229,0.00022595165,0.000024654784],"about_ca_topic_score_codex":0.02600605,"about_ca_topic_score_gemma":0.014020195,"teacher_disagreement_score":0.02600605,"about_ca_system_score_codex":0.0010712643,"about_ca_system_score_gemma":0.0010103484,"threshold_uncertainty_score":0.051709354},"labels":[],"label_agreement":null},{"id":"W2133578844","doi":"10.1029/2004gl021481","title":"The reflectance spectra of opal‐A (0.5–25 μm) from the Taupo Volcanic Zone: Spectra that may identify hydrothermal systems on planetary surfaces","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geochemistry and Geologic Mapping","field":"Computer Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Hydrothermal circulation; Spectral line; Volcano; Silicate; Geology; Porosity; Mineralogy; Wavelength; Reflectivity; Silanol; Mars Exploration Program; Geochemistry; Materials science; Astrobiology; Chemistry; Optics; Optoelectronics; Paleontology","score_opus":0.04072797001330862,"score_gpt":0.29671688878681196,"score_spread":0.2559889187735033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133578844","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994645,0.00018677695,0.0016405162,0.00003681446,0.0000072977946,0.0000073338724,0.0005221177,0.00017803237,0.002776119],"genre_scores_gemma":[0.99491876,0.00017892793,0.0031722272,0.000030652853,0.0000053721474,0.000008238428,0.0006145879,0.000039284452,0.001031928],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.0000025078818,0.0000014884097,0.000012702548,0.000012382335,0.0000105603895],"domain_scores_gemma":[0.9998832,0.000020763124,0.000025672556,0.000008153414,0.00003359563,0.00002868291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008378732,0.00027164107,0.00014129274,0.0010480763,0.00022679908,0.00021732012,0.00013938053,0.00029092454,0.0015657285],"category_scores_gemma":[0.00014519373,0.00010251049,0.00013302443,0.0005970741,0.00015772386,0.00025614706,0.00015433865,0.0002815991,0.0004180755],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020301683,0.00004484274,0.014856839,0.000064737935,0.000024030991,0.00019930572,0.00021184969,0.00014258362,0.9673913,0.00006797832,0.0004251383,0.016368384],"study_design_scores_gemma":[0.000019264933,0.00016124919,0.6708598,0.000016286196,0.00008822843,0.00131607,0.0007893419,0.0023676895,0.319918,0.00015189998,0.00427966,0.00003256188],"about_ca_topic_score_codex":0.0020646488,"about_ca_topic_score_gemma":0.0037434888,"teacher_disagreement_score":0.0020646488,"about_ca_system_score_codex":0.00013384178,"about_ca_system_score_gemma":0.000068210094,"threshold_uncertainty_score":0.0052378774},"labels":[],"label_agreement":null},{"id":"W2133755418","doi":"10.1029/2001gl013484","title":"Satellite detection of a continental‐scale plume of nitrogen oxides from boreal forest fires","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Plume; Environmental science; Total Ozone Mapping Spectrometer; Taiga; Atmospheric sciences; Troposphere; Boreal; Satellite; Haze; Aerosol; Climatology; Ozone; Meteorology; Stratosphere; Ozone layer; Geology; Geography","score_opus":0.019208524321915183,"score_gpt":0.2508807801483829,"score_spread":0.2316722558264677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2133755418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895644,0.00007296132,0.00025949976,0.000017514138,0.0000059551016,0.000003661495,0.00010850519,0.00002233326,0.0005531976],"genre_scores_gemma":[0.9985796,0.000068552596,0.00087233476,0.000014822414,0.000005506205,0.0000029059331,0.0002836174,0.000002243564,0.00017036001],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999536,0.0000047602443,0.0000022860343,0.00000926191,0.000019611092,0.000010451072],"domain_scores_gemma":[0.9998808,0.000017540577,0.00004311405,0.000007898245,0.000025862793,0.0000247637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014911137,0.00019481702,0.00010013683,0.0002714464,0.00024661323,0.00022639507,0.00013813021,0.00019439694,0.00022537679],"category_scores_gemma":[0.00026964082,0.00011421591,0.00012188601,0.00019380248,0.00013887548,0.00013303774,0.00020201576,0.0001311862,0.000036287638],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048754783,0.00012098803,0.77272713,0.000077112505,0.000106529485,0.0006766646,0.00055679283,0.0023909449,0.1985078,0.00014843824,0.0005763418,0.023623707],"study_design_scores_gemma":[0.000014862614,0.0001107834,0.9842322,0.000006448232,0.000035155674,0.00038786404,0.00011699776,0.0039487276,0.010210484,0.00005860383,0.00086870056,0.000009276568],"about_ca_topic_score_codex":0.02248491,"about_ca_topic_score_gemma":0.055415723,"teacher_disagreement_score":0.02248491,"about_ca_system_score_codex":0.00022103838,"about_ca_system_score_gemma":0.00017754035,"threshold_uncertainty_score":0.044708073},"labels":[],"label_agreement":null},{"id":"W2134011247","doi":"10.1002/2015gl063345","title":"The impact of a catastrophic mine tailings impoundment spill into one of North America's largest fjord lakes: Quesnel Lake, British Columbia, Canada","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of British Columbia; University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of Northern British Columbia","keywords":"Hypolimnion; Fjord; Seiche; Thermocline; Geology; Tailings; Oceanography; Hydrology (agriculture); Turbidity current; Structural basin; Turbidity; Environmental science; Geomorphology; Eutrophication","score_opus":0.026313758794788606,"score_gpt":0.2902058882193149,"score_spread":0.26389212942452633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134011247","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939737,0.000094825264,0.00004228236,0.00045784083,0.000012415198,0.000016175694,0.00079226115,0.000014727828,0.0045958087],"genre_scores_gemma":[0.99651283,0.000115718816,0.00011602214,0.00013654243,0.0000035796345,0.0000071558866,0.00034660698,0.00000435559,0.002757366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998381,0.000009438326,0.000005508704,0.000022094278,0.000054584765,0.00007020637],"domain_scores_gemma":[0.9994579,0.000024023178,0.00006213229,0.000014805854,0.00028794582,0.00015317995],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013323376,0.000224575,0.00017482883,0.0004950025,0.003101069,0.0009454159,0.00041540904,0.00035872567,0.0025690566],"category_scores_gemma":[0.0005329349,0.00016060354,0.00013451862,0.0007297874,0.0007680005,0.00032290778,0.0008252678,0.00055907137,0.00019156004],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040697283,0.00010523389,0.9622957,0.00005232319,0.00009548943,0.00096182345,0.0019417745,0.0013342489,0.006285598,0.00022357276,0.00782509,0.018472208],"study_design_scores_gemma":[0.0000081578455,0.000030207777,0.9917066,0.000021550572,0.00001971936,0.00004454413,0.0035454764,0.00055929576,0.00051896326,0.000038997186,0.0034943875,0.00001213316],"about_ca_topic_score_codex":0.9885718,"about_ca_topic_score_gemma":0.99729127,"teacher_disagreement_score":0.016583774,"about_ca_system_score_codex":0.016583774,"about_ca_system_score_gemma":0.015439571,"threshold_uncertainty_score":0.120324254},"labels":[],"label_agreement":null},{"id":"W2134232075","doi":"10.1029/2007gl029749","title":"Diagnosing a partly standing internal wave in Mamala Bay, Oahu","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Baroclinity; Bay; Energy flux; Standing wave; Internal wave; Geology; Ridge; Flux (metallurgy); Kinetic energy; Oceanography; Work (physics); Geodesy; Meteorology; Physics","score_opus":0.042436155485460945,"score_gpt":0.2999165603112379,"score_spread":0.257480404825777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134232075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989422,0.000012909818,0.00064519705,0.000029079576,0.0000028696513,0.0000057765246,0.000049181534,0.000019454725,0.00029346987],"genre_scores_gemma":[0.99916637,0.000013823046,0.00059695187,0.0000037974826,0.0000013464381,0.0000021888136,0.00010230158,0.0000024190422,0.00011075456],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993885,0.000008143841,0.0000045028637,0.00001490182,0.000011605417,0.000021988792],"domain_scores_gemma":[0.9998909,0.000029132352,0.000019697372,0.000009687609,0.000019512892,0.000031071857],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001519539,0.00035561045,0.00016366605,0.00024897387,0.00033134528,0.00067682104,0.00034742363,0.00039870612,0.00038039262],"category_scores_gemma":[0.0005529733,0.00018777576,0.00023992786,0.00026950432,0.00028339418,0.00037436013,0.00048994937,0.00024171098,0.000056898094],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000400413,0.00010629395,0.8058427,0.00006738706,0.00011974588,0.002748168,0.0011467633,0.11074008,0.04141752,0.0006671606,0.00065708224,0.036086697],"study_design_scores_gemma":[0.00004827872,0.00011344403,0.44153947,0.000015114276,0.00006112089,0.00015452183,0.001725675,0.5521155,0.003588559,0.0002789029,0.00033181751,0.000027514738],"about_ca_topic_score_codex":0.0948797,"about_ca_topic_score_gemma":0.11159645,"teacher_disagreement_score":0.0948797,"about_ca_system_score_codex":0.0005739768,"about_ca_system_score_gemma":0.0005340643,"threshold_uncertainty_score":0.18865484},"labels":[],"label_agreement":null},{"id":"W2134298468","doi":"10.1002/2015gl063550","title":"The impact of resolution on the representation of southeast Greenland barrier winds and katabatic flows","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Katabatic wind; Mesoscale meteorology; Climatology; Orographic lift; Geology; Orography; Arctic; Meteorology; Environmental science; Geography; Oceanography; Precipitation","score_opus":0.07578069281507399,"score_gpt":0.3443001168113184,"score_spread":0.2685194239962444,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134298468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.989884,0.00049322133,0.0040437784,0.00041954394,0.000060087146,0.000016393451,0.0009106006,0.00015835566,0.0040139896],"genre_scores_gemma":[0.99611425,0.00014364603,0.0027621167,0.000047433765,0.000014464922,0.0000066818525,0.00058776257,0.000028120385,0.0002955323],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992337,0.00041171926,0.000059459282,0.000112460686,0.00009299431,0.000089578316],"domain_scores_gemma":[0.9949137,0.0035096803,0.00032560044,0.0005847358,0.00047626224,0.0001900457],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002321807,0.00032578537,0.0004322384,0.00033796878,0.00029002753,0.0018450675,0.0004760764,0.00036185334,0.001328364],"category_scores_gemma":[0.0113756005,0.0002384869,0.00040763954,0.00071253296,0.00034618116,0.0011818627,0.000731133,0.00066417793,0.00029730212],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002439637,0.00024466327,0.46015307,0.00021282981,0.0006078896,0.00037079543,0.0005811841,0.40193492,0.02100631,0.0035895498,0.0040371055,0.10482205],"study_design_scores_gemma":[0.00015271282,0.00020517406,0.32337826,0.00015030666,0.00021644509,0.00014350133,0.00061016186,0.66174847,0.007993559,0.0016033136,0.003712552,0.000085639294],"about_ca_topic_score_codex":0.03354393,"about_ca_topic_score_gemma":0.03726572,"teacher_disagreement_score":0.03354393,"about_ca_system_score_codex":0.00046729596,"about_ca_system_score_gemma":0.000675491,"threshold_uncertainty_score":0.06669742},"labels":[],"label_agreement":null},{"id":"W2134500700","doi":"10.1029/2007gl032785","title":"Intensified turbulent mixing in the boundary current system of southern Greenland","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Oceanography; Boundary current; Geology; Entrainment (biomusicology); Sill; Thermohaline circulation; Groenlandia; Current (fluid); North Atlantic Deep Water; Water mass; Mixing (physics); Water column; Bay; Ocean current; Gulf Stream; North Atlantic oscillation; Climatology","score_opus":0.04343616465097732,"score_gpt":0.2672851186707766,"score_spread":0.22384895401979926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134500700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99950695,0.000029124138,0.000024611276,0.00002192524,0.000001092237,0.0000011210535,0.000021790413,0.0000038447065,0.00038964138],"genre_scores_gemma":[0.99971503,0.000018523027,0.00004269955,0.000014159026,7.8867333e-7,6.444753e-7,0.000061751736,0.0000012488429,0.00014519155],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995935,0.0000037936925,0.0000019222396,0.000009705305,0.000006420299,0.000018780614],"domain_scores_gemma":[0.99993277,0.0000045540296,0.000021969878,0.0000036077663,0.00001527034,0.00002193571],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008367498,0.00009275646,0.00013578932,0.0004295036,0.00034523837,0.00052931544,0.00010703116,0.00014995632,0.00062057876],"category_scores_gemma":[0.0002394605,0.00011256841,0.00006709736,0.00031516486,0.0004584389,0.00029996448,0.0003477699,0.000111819616,0.00007427925],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019618832,0.000050611674,0.91437274,0.000040414383,0.00006421143,0.000675396,0.0022238789,0.002141405,0.060834244,0.0011183703,0.00055936544,0.017723247],"study_design_scores_gemma":[0.0000058209716,0.0000081658945,0.99815875,0.000005870768,0.0000060157467,0.000027229487,0.00027986683,0.000915557,0.00018913814,0.00008535097,0.0003150885,0.000003093984],"about_ca_topic_score_codex":0.18399179,"about_ca_topic_score_gemma":0.31920296,"teacher_disagreement_score":0.18399179,"about_ca_system_score_codex":0.0015516469,"about_ca_system_score_gemma":0.0007022771,"threshold_uncertainty_score":0.3658417},"labels":[],"label_agreement":null},{"id":"W2134732162","doi":"10.1029/2004gl021358","title":"Halocline structure in the Canada Basin of the Arctic Ocean","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":163,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"North Pacific Marine Science Organization; Fisheries and Oceans Canada","funders":"","keywords":"Halocline; Oceanography; Canada Basin; Geology; Arctic; Hydrography; Ocean gyre; Structural basin; Thermohaline circulation; Salinity; Paleontology; Fishery","score_opus":0.01335835269636997,"score_gpt":0.24135832227477547,"score_spread":0.2279999695784055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134732162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962304,0.00040080058,0.000119046694,0.00005122122,0.0000027774165,0.0000070852825,0.0014656852,0.000015135753,0.0017078595],"genre_scores_gemma":[0.9980573,0.00023338286,0.00017528496,0.000012767835,0.0000015810355,0.0000048534075,0.0011415527,0.0000049969476,0.00036827638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981445,0.000010374588,0.000007293353,0.000030446177,0.00006013179,0.00007730793],"domain_scores_gemma":[0.9993753,0.000031061758,0.00011486863,0.000018670135,0.0003361908,0.00012395043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018200182,0.00016890332,0.00017666207,0.0023926995,0.0012044727,0.0011122216,0.00031491945,0.00014246703,0.00061189],"category_scores_gemma":[0.00070672715,0.00016077208,0.00022550081,0.0039776014,0.0005119648,0.00024393795,0.0005710383,0.0001409929,0.000088564506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053654447,0.0000065881236,0.9893839,0.000017621605,0.000048916336,0.0000731655,0.0006229732,0.0007934682,0.000898348,0.00034888237,0.00077744276,0.006975066],"study_design_scores_gemma":[0.0000015911725,0.0000021920287,0.99773717,0.000006962945,0.000006274978,0.000023680595,0.00038129915,0.0006549131,0.000086454136,0.000034101195,0.0010614101,0.0000039320234],"about_ca_topic_score_codex":0.9697722,"about_ca_topic_score_gemma":0.9851291,"teacher_disagreement_score":0.03022778,"about_ca_system_score_codex":0.0066957492,"about_ca_system_score_gemma":0.008356075,"threshold_uncertainty_score":0.06081152},"labels":[],"label_agreement":null},{"id":"W2134754510","doi":"10.1029/2011gl050118","title":"Atmospheric forcing on the drift of Arctic sea ice in 1989–2009","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Circumpolar star; Arctic oscillation; Arctic; Sea ice; Arctic sea ice decline; Arctic dipole anomaly; Arctic ice pack; Atmospheric circulation; Environmental science; Geology; Forcing (mathematics); Atmospheric sciences; Oceanography; Northern Hemisphere; Sea ice thickness; Drift ice","score_opus":0.038128767823927344,"score_gpt":0.25604367862963,"score_spread":0.21791491080570266,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134754510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954922,0.00018993998,0.00010321659,0.00008297223,0.00003687682,0.0000052899104,0.003261076,0.000026370368,0.00080188276],"genre_scores_gemma":[0.9955907,0.00015506496,0.00015304166,0.000025645879,0.000025408033,0.000006068307,0.0038195471,0.000008469809,0.00021615704],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982685,0.000020421248,0.000023232824,0.000053220643,0.00003990279,0.000036385998],"domain_scores_gemma":[0.99955267,0.00007312603,0.00015552521,0.000029166635,0.00013180422,0.00005776244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004006103,0.0004211786,0.0003540841,0.0006017281,0.00033160535,0.000489961,0.00026577123,0.00035865064,0.0008072678],"category_scores_gemma":[0.0012634763,0.00021336693,0.0005446411,0.00068248535,0.00013595309,0.0002375544,0.00039818787,0.0003260806,0.00033353816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000423254,0.000063021165,0.9786879,0.00007176523,0.00027672038,0.00023517206,0.00012319638,0.0061923936,0.0041650813,0.00013922353,0.0019241038,0.0076981955],"study_design_scores_gemma":[0.000008199952,0.00002612576,0.99558073,0.000010008729,0.000019205503,0.000036812216,0.000030675325,0.0032005145,0.00021081083,0.000016757473,0.00085381244,0.000006471015],"about_ca_topic_score_codex":0.07942479,"about_ca_topic_score_gemma":0.11767608,"teacher_disagreement_score":0.07942479,"about_ca_system_score_codex":0.0010955693,"about_ca_system_score_gemma":0.00056640635,"threshold_uncertainty_score":0.15792501},"labels":[],"label_agreement":null},{"id":"W2134783943","doi":"10.1029/2007gl031566","title":"Internal waves across the Pacific","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":164,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Geology; Internal tide; Internal wave; Inertial wave; Ridge; Baroclinity; Energy flux; Latitude; Mooring; Geodesy; Geophysics; Instability; Seismology; Atmospheric sciences; Oceanography; Wave propagation; Physics; Mechanics; Longitudinal wave","score_opus":0.024985138853352563,"score_gpt":0.3018245489219432,"score_spread":0.27683941006859064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2134783943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9773581,0.0002947641,0.00092900504,0.00009613431,0.0000148092295,0.000013112119,0.00019688174,0.000053265376,0.021043995],"genre_scores_gemma":[0.9977004,0.0002601824,0.000363544,0.00002646619,0.000007981955,0.0000057877446,0.00018686266,0.000008757964,0.0014400772],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993,0.0000040452687,0.0000033109097,0.000015142852,0.000031970223,0.000015511301],"domain_scores_gemma":[0.9996706,0.000029051562,0.00007772473,0.000032060994,0.00013491916,0.00005564619],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008048712,0.00018470372,0.00009197977,0.00057411246,0.0004601355,0.0006345622,0.00015224119,0.000085420674,0.0017131803],"category_scores_gemma":[0.00048438,0.000119528115,0.0001063466,0.0006561205,0.00025759498,0.00023855695,0.00076567486,0.00033032274,0.0001359151],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013546798,0.000066408604,0.7374363,0.00015294421,0.00012310749,0.000961794,0.004870208,0.002229408,0.042909477,0.003508833,0.002749652,0.20485644],"study_design_scores_gemma":[0.0000063696148,0.000050183295,0.9854655,0.000040571587,0.0000648271,0.00030169965,0.0014576344,0.0010455273,0.0024181486,0.0005671832,0.008571945,0.000010403958],"about_ca_topic_score_codex":0.026249677,"about_ca_topic_score_gemma":0.033965237,"teacher_disagreement_score":0.026249677,"about_ca_system_score_codex":0.0004693996,"about_ca_system_score_gemma":0.0005114692,"threshold_uncertainty_score":0.05219376},"labels":[],"label_agreement":null},{"id":"W2135089526","doi":"10.1002/2014gl059475","title":"Laboratory measurements of cryogenic liquid alkane microwave absorptivity and implications for the composition of Ligeia Mare, Titan","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Methane; Titan (rocket family); Hydrocarbon; Alkane; Geology; Astrobiology; Materials science; Chemistry; Physics; Organic chemistry","score_opus":0.07812209199513202,"score_gpt":0.32775989133774763,"score_spread":0.2496377993426156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135089526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891365,0.000027700491,0.00029868327,0.000017096761,0.0000017458581,0.0000029880234,0.00010234156,0.000015108517,0.00062067265],"genre_scores_gemma":[0.99962544,0.000012364099,0.000117809795,0.000009810459,0.0000015585323,0.000003342166,0.00010435449,0.000004024738,0.00012127484],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993813,0.000006566035,0.0000022268637,0.000023677017,0.000014931369,0.000014472007],"domain_scores_gemma":[0.9999161,0.000015543708,0.000020844318,0.000010262981,0.000021514892,0.000015747897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017127488,0.00015000223,0.00011113696,0.00030751253,0.00036195669,0.00043477328,0.00020963971,0.00017582637,0.00042684335],"category_scores_gemma":[0.00029248698,0.00012176601,0.000100499965,0.00015422655,0.00047507315,0.0002192258,0.00018143072,0.00020757453,0.0002047994],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024262106,0.000074779346,0.11626197,0.00001913671,0.000030249683,0.00012670102,0.0002602688,0.00049126404,0.87876314,0.00015182939,0.00011267636,0.0034654026],"study_design_scores_gemma":[0.00003199794,0.00027144534,0.83668375,0.0000049932623,0.000031895877,0.0001489321,0.00032216508,0.0036739479,0.15774077,0.00012599195,0.000953085,0.000010996965],"about_ca_topic_score_codex":0.005910184,"about_ca_topic_score_gemma":0.006146831,"teacher_disagreement_score":0.005910184,"about_ca_system_score_codex":0.00036551335,"about_ca_system_score_gemma":0.00016699304,"threshold_uncertainty_score":0.011751592},"labels":[],"label_agreement":null},{"id":"W2135266095","doi":"10.1002/2013gl059113","title":"Observed linkages between the northern annular mode/North Atlantic Oscillation, cloud incidence, and cloud radiative forcing","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Jet Propulsion Laboratory; National Science Foundation","keywords":"Climatology; Northern Hemisphere; North Atlantic oscillation; Cloud forcing; Cloud cover; Forcing (mathematics); Troposphere; Radiative forcing; Extratropical cyclone; Atmospheric sciences; Environmental science; Geology; Southern Hemisphere; Cloud feedback; Climate model; Climate change; Cloud computing; Oceanography; Climate sensitivity","score_opus":0.04406908873252787,"score_gpt":0.2906969916130961,"score_spread":0.2466279028805682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135266095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987804,0.00004004495,0.00006177725,0.00003321439,0.0000036024474,0.000001872236,0.00047977813,0.000004421411,0.00059494044],"genre_scores_gemma":[0.99949574,0.000025121575,0.00004563325,0.000008485047,0.0000034940656,0.0000017666581,0.00033428194,9.644053e-7,0.00008448797],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994814,0.000009749139,0.0000052515284,0.000013616012,0.000010439121,0.000012736247],"domain_scores_gemma":[0.9994374,0.00015405258,0.00019992985,0.000042779102,0.00008615162,0.00007965078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023731489,0.000069245136,0.00010489159,0.00024965062,0.00017803807,0.00032866825,0.000089334426,0.00012230713,0.0010250821],"category_scores_gemma":[0.00091815856,0.00008418801,0.00009263369,0.0003208585,0.00011660003,0.00014142282,0.0002055426,0.00016166475,0.000084261585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041187915,0.000021170506,0.9938059,0.000007401861,0.00002434478,0.000023963832,0.000063924264,0.00036004573,0.003443748,0.00005915339,0.00017480116,0.001974411],"study_design_scores_gemma":[0.0000013604647,0.0000055213754,0.9994628,0.0000011608738,0.000002580999,0.000008394479,0.000023353983,0.0002779395,0.00008439909,0.000014490836,0.00011719956,8.8172646e-7],"about_ca_topic_score_codex":0.018462481,"about_ca_topic_score_gemma":0.043292824,"teacher_disagreement_score":0.018462481,"about_ca_system_score_codex":0.00024035556,"about_ca_system_score_gemma":0.00020320386,"threshold_uncertainty_score":0.036710024},"labels":[],"label_agreement":null},{"id":"W2135299131","doi":"10.1029/2005gl025238","title":"Were extreme waves in the Rockall Trough the largest ever recorded?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council","keywords":"Hindcast; Trough (economics); Crest; Geology; Seismology; Rogue wave; Significant wave height; Wind wave; Meteorology; Wave height; Wind speed; Climatology; Oceanography; Geodesy; Geography; Physics","score_opus":0.042762177513097646,"score_gpt":0.2664784168222673,"score_spread":0.22371623930916967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135299131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993087,0.0008451802,0.00024812104,0.0016649603,0.00012303058,0.000007668035,0.00039128636,0.000010959512,0.0036218008],"genre_scores_gemma":[0.998054,0.00040453285,0.0001029488,0.00020227877,0.00017915096,0.0000031168472,0.00016824027,0.0000040013974,0.0008817442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997131,0.000030318448,0.000014576766,0.00004103283,0.000055401375,0.00014553271],"domain_scores_gemma":[0.99865544,0.00017106376,0.0005406428,0.00006933525,0.0002934153,0.00027010535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042293323,0.00017857394,0.00025182634,0.00051969383,0.0006013743,0.001221396,0.00023653894,0.00065288186,0.0021607135],"category_scores_gemma":[0.0025554807,0.00016498835,0.00011259072,0.0007854043,0.0006499242,0.00079266826,0.00042389668,0.00048005418,0.00045774662],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003817894,0.00003663247,0.9571454,0.00006432069,0.000032420885,0.0015329301,0.0020645363,0.000033963574,0.0025296928,0.0002921438,0.0035379117,0.032348245],"study_design_scores_gemma":[0.0000058775345,0.00010044034,0.9884886,0.00002281625,0.000012557791,0.0008600722,0.004781331,0.00002610244,0.00034222112,0.00014947496,0.0052005644,0.000009751341],"about_ca_topic_score_codex":0.012243062,"about_ca_topic_score_gemma":0.03928083,"teacher_disagreement_score":0.012243062,"about_ca_system_score_codex":0.00040934613,"about_ca_system_score_gemma":0.0002771687,"threshold_uncertainty_score":0.02434361},"labels":[],"label_agreement":null},{"id":"W2135456474","doi":"10.1002/2013gl058877","title":"Surface of Ligeia Mare, Titan, from Cassini altimeter and radiometer analysis","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Titan (rocket family); Radiometer; Geology; Altimeter; Nadir; Radar; Radar altimeter; Specular reflection; Terrain; Astrobiology; Remote sensing; Atmospheric sciences; Satellite; Optics; Physics; Astronomy","score_opus":0.02492147039343082,"score_gpt":0.2930961222273613,"score_spread":0.26817465183393047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135456474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924745,0.00008071368,0.00022228282,0.000053931337,0.000006906457,0.00000865528,0.00350162,0.00006229615,0.0035891484],"genre_scores_gemma":[0.99165875,0.000048066013,0.0006247769,0.00002730202,0.0000103902075,0.00001153449,0.006580346,0.0000145346885,0.0010243572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999442,0.000004731992,0.0000025111058,0.000019029816,0.000018276794,0.000011294723],"domain_scores_gemma":[0.99989474,0.000013123745,0.000021176398,0.000016878854,0.000037506918,0.000016493768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012635211,0.00014066859,0.00011225958,0.0007227813,0.00029008533,0.00032027843,0.00016291557,0.00019639732,0.00083927275],"category_scores_gemma":[0.00029277097,0.00008518616,0.00020462589,0.00069201324,0.0001332175,0.00016672318,0.0002728894,0.00017455581,0.00048962975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045467578,0.00008645111,0.92678845,0.000067119836,0.00012242381,0.0005399025,0.0006769005,0.004527339,0.035145566,0.0003844113,0.0075138183,0.023692846],"study_design_scores_gemma":[0.0000034481618,0.000012520738,0.9969015,0.0000020657494,0.000007967733,0.000034217865,0.000049873666,0.0013498549,0.00040654762,0.000013683837,0.0012159304,0.0000022922661],"about_ca_topic_score_codex":0.045938835,"about_ca_topic_score_gemma":0.075616494,"teacher_disagreement_score":0.045938835,"about_ca_system_score_codex":0.0005721527,"about_ca_system_score_gemma":0.0002647119,"threshold_uncertainty_score":0.091342926},"labels":[],"label_agreement":null},{"id":"W2135474850","doi":"10.1029/2007gl032374","title":"Isotopic fractionation in non‐equilibrium diffusive environments","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; Atlantic Canada Opportunities Agency; Canadian Foundation for Climate and Atmospheric Sciences; Acadia University","keywords":"Fractionation; Diffusion; Equilibrium fractionation; Soil water; Steady state (chemistry); Mass-independent fractionation; TRACER; Isotope fractionation; Geology; Environmental chemistry; Environmental science; Chemistry; Chemical physics; Soil science; Thermodynamics; Physics; Chromatography; Nuclear physics","score_opus":0.025812486633179227,"score_gpt":0.27988541825591867,"score_spread":0.2540729316227395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2135474850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9805813,0.000102231475,0.018534243,0.00005098159,0.000008412471,0.000007448326,0.00002272932,0.00006491197,0.0006277527],"genre_scores_gemma":[0.9982798,0.000057538342,0.0015082726,0.000009528571,0.0000015564997,0.000003226068,0.000018838937,0.0000073338433,0.000113953516],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998592,0.000036816447,0.000009551896,0.000044450895,0.000029128985,0.000020821537],"domain_scores_gemma":[0.99966955,0.00017626787,0.000043045213,0.00004716172,0.000044291115,0.000019713343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036468412,0.00023747946,0.00022044338,0.00023663865,0.00029276876,0.0005372974,0.00041318787,0.0004141473,0.0003049015],"category_scores_gemma":[0.0012738802,0.00020274786,0.00020540919,0.00020249056,0.00051983877,0.00068152894,0.00044679423,0.00020812922,0.00006256171],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005120283,0.00009774282,0.036213208,0.00014491883,0.000046020752,0.0006846268,0.00059018744,0.11640351,0.8112708,0.022499429,0.00015697491,0.011380626],"study_design_scores_gemma":[0.00013610107,0.00038429638,0.033268612,0.000012597396,0.00005269404,0.00056932087,0.0003432398,0.45281616,0.47574878,0.033640977,0.0029383663,0.00008888765],"about_ca_topic_score_codex":0.0017681936,"about_ca_topic_score_gemma":0.001256488,"teacher_disagreement_score":0.0017681936,"about_ca_system_score_codex":0.00061415636,"about_ca_system_score_gemma":0.0002372269,"threshold_uncertainty_score":0.0044559836},"labels":[],"label_agreement":null},{"id":"W2136001518","doi":"10.1002/2013gl059024","title":"Effect of EMIC waves on relativistic and ultrarelativistic electron populations: Ground‐based and Van Allen Probes observations","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":365,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Physics; Pitch angle; Van Allen radiation belt; Van Allen Probes; Electron; Emic and etic; Scattering; Computational physics; Diffusion; Electron scattering; Geomagnetic storm; Electron precipitation; Astrophysics; Nuclear physics; Atomic physics; Geophysics; Magnetosphere; Solar wind; Plasma; Optics","score_opus":0.022161561713400186,"score_gpt":0.3003295195297312,"score_spread":0.278167957816331,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136001518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985261,0.000026307012,0.00025960748,0.000012785738,0.0000013025779,0.0000031883362,0.00011775759,0.000014666249,0.0010382759],"genre_scores_gemma":[0.99936754,0.00002193155,0.00020803609,0.0000054905845,0.0000012532781,0.0000020771256,0.00019165128,0.000005041269,0.00019691522],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999299,0.000005514923,0.0000014517955,0.000019332054,0.000021559472,0.000022259272],"domain_scores_gemma":[0.99990714,0.000020246724,0.000025022502,0.000010773546,0.000022205884,0.000014641922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001261892,0.00017635459,0.00018219645,0.00031345742,0.00030346398,0.0003851547,0.00037240863,0.0002086874,0.00066609296],"category_scores_gemma":[0.00024678258,0.00015731457,0.00013239487,0.00035207495,0.00025129603,0.00027081952,0.00026715812,0.0002911182,0.00009079521],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017140688,0.0001419347,0.47621238,0.000067031586,0.00016703681,0.0005411169,0.0013321959,0.01473274,0.48247176,0.00094623497,0.00072857336,0.020944957],"study_design_scores_gemma":[0.000043564265,0.00020553953,0.936004,0.000007618766,0.00004099257,0.00013143693,0.00045114759,0.017563317,0.04366778,0.00014589452,0.001711875,0.000026948992],"about_ca_topic_score_codex":0.058033686,"about_ca_topic_score_gemma":0.085323624,"teacher_disagreement_score":0.058033686,"about_ca_system_score_codex":0.0007421036,"about_ca_system_score_gemma":0.0002988794,"threshold_uncertainty_score":0.11539179},"labels":[],"label_agreement":null},{"id":"W2136089348","doi":"10.1002/2014gl061644","title":"A 3‐D spectral‐element and frequency‐wave number hybrid method for high‐resolution seismic array imaging","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Waveform; Geology; Seismology; Spectral element method; Subduction; Scattering; Reflection (computer programming); Seismic wave; Resolution (logic); Plane wave; Acoustics; Optics; Finite element method; Computer science; Physics; Telecommunications","score_opus":0.024613013329622544,"score_gpt":0.29499813561629545,"score_spread":0.2703851222866729,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136089348","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009902792,0.000022785445,0.9887454,0.00003543905,0.000012035805,0.000014909522,0.00002552102,0.00026106744,0.0009800423],"genre_scores_gemma":[0.1947836,0.000057675672,0.80247986,0.00006231744,0.000016955531,0.00009863319,0.00009476502,0.00012541043,0.0022807615],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998869,0.00003102838,0.000005223625,0.000013462588,0.000053276606,0.000010065268],"domain_scores_gemma":[0.9996834,0.0001365105,0.00002930932,0.000048457558,0.00008251505,0.00001983145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029493266,0.00039769465,0.0002733099,0.00039331793,0.00024775107,0.00047283617,0.0008605754,0.00076425634,0.0024276702],"category_scores_gemma":[0.0006253607,0.00032502037,0.0005553714,0.0003185102,0.00037018524,0.00056600996,0.000506431,0.0005658611,0.00061440165],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007146115,0.000067119254,0.0012724146,0.00006685247,0.000055668177,0.0001029826,0.00012852476,0.845293,0.036907293,0.013040209,0.0011926834,0.10180178],"study_design_scores_gemma":[0.0000034467741,0.0000066079965,0.000065308086,0.0000016230761,0.000001553448,0.000016383923,0.000005466891,0.9977337,0.0010004429,0.00065770734,0.000503144,0.0000045865677],"about_ca_topic_score_codex":0.0035615666,"about_ca_topic_score_gemma":0.0053010094,"teacher_disagreement_score":0.0035615666,"about_ca_system_score_codex":0.00035394725,"about_ca_system_score_gemma":0.0006290843,"threshold_uncertainty_score":0.008121371},"labels":[],"label_agreement":null},{"id":"W2136482752","doi":"10.1029/2005gl024942","title":"Multidecadal variations and decline in spring discharge in the Canadian middle Arctic since 1550 AD","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Queen's University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Varve; Spring (device); Arctic; Sediment; Snow; Atlantic multidecadal oscillation; Period (music); Environmental science; Geology; Arctic oscillation; Discharge; Climatology; Sediment transport; Flood myth; Oceanography; Hydrology (agriculture); Physical geography; North Atlantic oscillation; Drainage basin; The arctic; Geomorphology; Geography","score_opus":0.06745096014905716,"score_gpt":0.2939782173236321,"score_spread":0.22652725717457495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136482752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99746704,0.0002691951,0.00005400919,0.00006831231,0.0000044222634,0.0000029988641,0.0011668504,0.000007968612,0.0009592678],"genre_scores_gemma":[0.9986399,0.00013782292,0.000086795924,0.000013452083,0.0000022495549,0.0000023048285,0.00074046006,0.0000019539573,0.0003751063],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981755,0.000007205779,0.000011253599,0.000044936594,0.000057688558,0.00006143047],"domain_scores_gemma":[0.9994355,0.000030710424,0.00009012971,0.000013981486,0.00033764413,0.00009207167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032560434,0.00018562214,0.00016828426,0.002086814,0.0011131167,0.0008842545,0.00037122084,0.00022883613,0.0007394958],"category_scores_gemma":[0.0007412908,0.00013929988,0.00016908525,0.0022846763,0.0004559133,0.00022468656,0.0004295703,0.00022915927,0.00008336262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007301957,0.000010263764,0.98646355,0.000023600636,0.00007058829,0.00007514687,0.0011160768,0.0003202579,0.002030124,0.0001328332,0.0005375744,0.00914692],"study_design_scores_gemma":[5.3513526e-7,0.0000018151956,0.9991689,0.000002929422,0.000004571686,0.000010746009,0.00021471635,0.00010945281,0.00003823597,0.000005193354,0.00044076057,0.000002148745],"about_ca_topic_score_codex":0.96499854,"about_ca_topic_score_gemma":0.9873948,"teacher_disagreement_score":0.035001457,"about_ca_system_score_codex":0.007632449,"about_ca_system_score_gemma":0.004239618,"threshold_uncertainty_score":0.07041514},"labels":[],"label_agreement":null},{"id":"W2136499382","doi":"10.1029/2002gl015797","title":"Recent cooling in coastal southern Greenland and relation with the North Atlantic Oscillation","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"North Atlantic oscillation; Greenland ice sheet; Atlantic multidecadal oscillation; Climatology; Groenlandia; Geology; Oceanography; Period (music); Future sea level; Climate change; Sea surface temperature; Ice sheet; Sea ice; Arctic ice pack; Antarctic sea ice","score_opus":0.03204940027292169,"score_gpt":0.2656061297160449,"score_spread":0.23355672944312322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136499382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990226,0.00019034438,0.00003075505,0.00012586408,0.000004694635,8.33778e-7,0.00028749366,0.000003913353,0.00033362224],"genre_scores_gemma":[0.99928254,0.00010080807,0.000037596186,0.000032004416,0.00000562517,0.0000013183144,0.00042698177,0.0000015601759,0.00011158628],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990654,0.000014691427,0.000008899234,0.0000263744,0.0000143335255,0.000029150373],"domain_scores_gemma":[0.99934465,0.0000806774,0.0002826421,0.000060387592,0.00014985235,0.00008172015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000435805,0.00012735523,0.00016355015,0.0005925077,0.00024442337,0.00046848302,0.00022288425,0.00020540075,0.0005469444],"category_scores_gemma":[0.0011537947,0.000081439524,0.00015475333,0.0012662833,0.00045824234,0.00028915977,0.00037620656,0.00019246004,0.000070682465],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054677563,0.00000832441,0.9912015,0.000020979498,0.00007364332,0.00012412546,0.0004109969,0.0009128327,0.0010592706,0.00013253193,0.0003746024,0.0056265597],"study_design_scores_gemma":[9.2667256e-7,0.0000026299438,0.9994822,0.0000030036904,0.0000037553834,0.000014508957,0.000048790083,0.00009564988,0.000017906947,0.000014406031,0.00031540822,9.031815e-7],"about_ca_topic_score_codex":0.15602988,"about_ca_topic_score_gemma":0.29170406,"teacher_disagreement_score":0.15602988,"about_ca_system_score_codex":0.0015400243,"about_ca_system_score_gemma":0.00074358843,"threshold_uncertainty_score":0.31024337},"labels":[],"label_agreement":null},{"id":"W2136641669","doi":"10.1029/2002gl015082","title":"Paleoclimate studies of minerogenic sediments using annually resolved textural parameters","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Varve; Paleoclimatology; Snowmelt; Geology; Sediment; Meltwater; Precipitation; Arctic; Snow; Sedimentary rock; Environmental science; Physical geography; Climatology; Climate change; Oceanography; Geomorphology; Paleontology; Meteorology","score_opus":0.14719278457184123,"score_gpt":0.35304275901302956,"score_spread":0.20584997444118833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2136641669","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991742,0.00006688787,0.00030044894,0.000008146932,3.83379e-7,0.0000012546786,0.00020255467,0.00000880963,0.00023740873],"genre_scores_gemma":[0.999241,0.000035991507,0.000315954,0.0000015764838,9.846152e-7,0.0000013611956,0.0002931677,0.0000046259934,0.0001053054],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999887,0.000018942179,0.0000061140827,0.000037701648,0.000021537338,0.00002871392],"domain_scores_gemma":[0.9994752,0.00011599089,0.00012717719,0.00006772402,0.0001525134,0.00006146762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004793073,0.00022901445,0.00013140617,0.0014929945,0.0003423737,0.0005232492,0.0002608235,0.00017522469,0.00031375044],"category_scores_gemma":[0.0016594606,0.00017677412,0.00018825296,0.0014703913,0.00031746944,0.00024356911,0.00027355054,0.00015351671,0.00006411635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010279374,0.000018923756,0.9612001,0.000023281567,0.00009928483,0.00008028874,0.00044336464,0.008517684,0.018204398,0.0004235148,0.00008944207,0.010796946],"study_design_scores_gemma":[0.0000017742889,0.000008531194,0.992419,0.0000030561741,0.000009428459,0.000038209844,0.00008167448,0.006075842,0.0008129188,0.00009592397,0.00044866186,0.000005041499],"about_ca_topic_score_codex":0.12287412,"about_ca_topic_score_gemma":0.29404068,"teacher_disagreement_score":0.12287412,"about_ca_system_score_codex":0.0010120961,"about_ca_system_score_gemma":0.00047724432,"threshold_uncertainty_score":0.24431783},"labels":[],"label_agreement":null},{"id":"W2137078396","doi":"10.1029/1999gl011200","title":"Observations of boreal forest fire smoke in the stratosphere by POAM III, SAGE II, and lidar in 1998","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":251,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Forest Service","funders":"","keywords":"Aerosol; Environmental science; Atmospheric sciences; Tropopause; Stratosphere; Lidar; Taiga; Boreal; Smoke; Extinction (optical mineralogy); Climatology; Volcano; Meteorology; Remote sensing; Geology; Geography; Forestry","score_opus":0.030129583468298825,"score_gpt":0.26991101380208943,"score_spread":0.2397814303337906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137078396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999278,0.000030047457,0.000076137054,0.000012930597,0.000002467577,0.000002436488,0.00022156631,0.000010486588,0.00036596466],"genre_scores_gemma":[0.9984622,0.000048753263,0.00054705754,0.00002740217,0.000005943828,0.000004923144,0.0007229256,0.0000022958375,0.00017848413],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993086,0.000007141491,0.000003380635,0.000010675838,0.000026666532,0.000021288088],"domain_scores_gemma":[0.9998148,0.000021919153,0.000047042427,0.000011702854,0.000044358425,0.000060205894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016626375,0.00016084124,0.00012814827,0.0003811698,0.00031031898,0.00020191907,0.00015781636,0.00019892918,0.00018438944],"category_scores_gemma":[0.00027068763,0.000092323535,0.00007694787,0.00031497714,0.0001274037,0.00017120222,0.00022397388,0.00016885453,0.00005366525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003035696,0.00008696618,0.9525734,0.000021229702,0.000041238338,0.00035077432,0.0010082185,0.00038830438,0.031936023,0.000073064955,0.0005488947,0.012668345],"study_design_scores_gemma":[0.000006200237,0.000049217324,0.9972572,0.0000032130226,0.000012414064,0.00016095747,0.00019861101,0.0005478912,0.0012071225,0.000014868007,0.00053816504,0.0000040541104],"about_ca_topic_score_codex":0.028792886,"about_ca_topic_score_gemma":0.10654888,"teacher_disagreement_score":0.028792886,"about_ca_system_score_codex":0.00024821897,"about_ca_system_score_gemma":0.00021467496,"threshold_uncertainty_score":0.05725062},"labels":[],"label_agreement":null},{"id":"W2137083686","doi":"10.1029/2004gl019981","title":"Seesaw structure of subsurface temperature anomalies between the Barents Sea and the Labrador Sea","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography","funders":"Japan Agency for Marine-Earth Science and Technology","keywords":"Sea ice; Geology; Oceanography; Arctic; Climatology; Thermohaline circulation; Sea surface temperature; Arctic ice pack; Arctic sea ice decline; Hydrography; Advection; North Atlantic oscillation; Antarctic sea ice","score_opus":0.012871889944427952,"score_gpt":0.2487213320460742,"score_spread":0.23584944210164624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137083686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991984,0.000011523112,0.00032574768,0.000013594168,0.0000021892763,0.0000019551078,0.00008223641,0.000015203621,0.00034927632],"genre_scores_gemma":[0.99959725,0.000010466255,0.00015404461,0.0000023383502,0.0000012369063,0.00000203202,0.000105937244,0.0000035541716,0.00012321687],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995303,0.0000076124616,0.0000027001506,0.000016158116,0.000006024469,0.0000144210535],"domain_scores_gemma":[0.99990666,0.000019204923,0.00003163305,0.0000067539045,0.000014430331,0.000021379574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010560798,0.00032467474,0.00022350541,0.00025045263,0.0002484721,0.0007618106,0.000362025,0.0002614751,0.000510728],"category_scores_gemma":[0.00036743085,0.00022957695,0.00043070383,0.00020425514,0.00024506275,0.00030268528,0.0003307989,0.00020150539,0.00006270583],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005153813,0.00013022606,0.22578254,0.000021022212,0.00029503682,0.0004896881,0.0001609386,0.7503101,0.01441348,0.0013154487,0.00036866698,0.006197483],"study_design_scores_gemma":[0.00005275146,0.00009185587,0.09581967,0.0000046191053,0.000050231876,0.000030331323,0.00010189368,0.9018841,0.0012116758,0.000494951,0.0002385311,0.000019351271],"about_ca_topic_score_codex":0.061300904,"about_ca_topic_score_gemma":0.051107347,"teacher_disagreement_score":0.061300904,"about_ca_system_score_codex":0.0005750741,"about_ca_system_score_gemma":0.00046429556,"threshold_uncertainty_score":0.12188816},"labels":[],"label_agreement":null},{"id":"W2137179110","doi":"10.1002/2014gl060800","title":"Earliest Holocene south Greenland ice sheet retreat within its late Holocene extent","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria","funders":"National Geographic Society","keywords":"Holocene; Greenland ice sheet; Geology; Deglaciation; Ice sheet; Holocene climatic optimum; Surface exposure dating; Oceanography; Physical geography; Climatology; Glacial period; Paleontology; Moraine; Geography","score_opus":0.037582419230934534,"score_gpt":0.2794345700785231,"score_spread":0.2418521508475886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137179110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9881022,0.00020115206,0.0004077871,0.00011082556,0.000012475867,0.0000049036566,0.0013647327,0.000032290147,0.009763738],"genre_scores_gemma":[0.9969837,0.0001295971,0.00032463227,0.000060261587,0.0000040825516,0.000005215084,0.001228424,0.00001028401,0.001253889],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993944,0.000004222128,0.000002876129,0.000017380615,0.000012099282,0.000023984307],"domain_scores_gemma":[0.99982136,0.000015462016,0.000054641507,0.000016421085,0.000058150606,0.000034068173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018727957,0.0001936115,0.00012566661,0.0007979908,0.0004343642,0.0005556756,0.00014367985,0.0001571035,0.0017262619],"category_scores_gemma":[0.00028414113,0.00008923848,0.00011518803,0.00057941925,0.00027785104,0.0003261182,0.0004515548,0.00023527622,0.00023048936],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009179998,0.000017275488,0.9627578,0.000044146997,0.000062874205,0.00018507976,0.0008530711,0.0015588265,0.008719247,0.00087264046,0.0021080475,0.022729188],"study_design_scores_gemma":[0.00000117577,0.0000046013506,0.9961062,0.000012256187,0.0000039455367,0.000030002342,0.00016470946,0.00016208767,0.00033830368,0.00007728933,0.0030977875,0.0000016291057],"about_ca_topic_score_codex":0.08422155,"about_ca_topic_score_gemma":0.2685292,"teacher_disagreement_score":0.08422155,"about_ca_system_score_codex":0.0009649078,"about_ca_system_score_gemma":0.00046452534,"threshold_uncertainty_score":0.16746265},"labels":[],"label_agreement":null},{"id":"W2137479725","doi":"10.1029/2006gl026602","title":"Seasonal cycles of O<sub>3</sub>, CO, and convective outflow at the tropical tropopause","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Dalhousie University","funders":"Canadian Foundation for Climate and Atmospheric Sciences; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Tropopause; Atmospheric sciences; Environmental science; Annual cycle; Climatology; Outflow; Seasonality; Altitude (triangle); Troposphere; Upwelling; Diurnal cycle; Ozone; Meteorology; Geography; Geology; Oceanography","score_opus":0.016886580699830588,"score_gpt":0.26148110920897455,"score_spread":0.24459452850914395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137479725","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99783045,0.00010131128,0.00024644236,0.0000446282,0.0000041242206,0.0000055726787,0.00084499764,0.000048574137,0.00087377976],"genre_scores_gemma":[0.998852,0.00006548231,0.00016899107,0.000017455715,0.0000045993343,0.0000040909513,0.00067578966,0.0000063713032,0.00020514116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997175,0.0000030980286,0.000002432573,0.000006870898,0.0000070447722,0.0000088840425],"domain_scores_gemma":[0.99984,0.00003512078,0.00004792738,0.000010027594,0.00003187973,0.000035053254],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012726359,0.00010131082,0.00011506628,0.00023238685,0.00016585444,0.00022631176,0.000095057825,0.00015228374,0.0010826167],"category_scores_gemma":[0.00034442657,0.00007877535,0.00010758321,0.00026777346,0.000120189754,0.0001661205,0.00014486762,0.00013752382,0.00015473682],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000497845,0.000050114013,0.9169833,0.00009049146,0.00009458964,0.0002886435,0.00038155197,0.0058264066,0.05827909,0.00044269624,0.0021145968,0.014950799],"study_design_scores_gemma":[0.000011669179,0.000045219233,0.991907,0.0000040034693,0.000018265431,0.00009532862,0.000077409146,0.0046660905,0.002180687,0.00007588969,0.0009128828,0.0000056488875],"about_ca_topic_score_codex":0.009203306,"about_ca_topic_score_gemma":0.015355532,"teacher_disagreement_score":0.009203306,"about_ca_system_score_codex":0.00029514136,"about_ca_system_score_gemma":0.00011067384,"threshold_uncertainty_score":0.01829952},"labels":[],"label_agreement":null},{"id":"W2137880621","doi":"10.1029/2009gl037339","title":"Origins of the extremely warm European fall of 2006","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"Agence Nationale de la Recherche","keywords":"Anomaly (physics); Climatology; Sea surface temperature; Environmental science; Atmospheric circulation; Climate model; Climate change; Atmospheric sciences; Geology; Oceanography; Physics","score_opus":0.05059461387262744,"score_gpt":0.30340332829441025,"score_spread":0.2528087144217828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137880621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9790983,0.001198247,0.001760392,0.0013874631,0.00023264792,0.000021804295,0.0039980533,0.00012841582,0.012174614],"genre_scores_gemma":[0.99437124,0.00034134468,0.0007828867,0.00027702536,0.000118522235,0.000013919133,0.0030963665,0.00003862096,0.0009600915],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996309,0.000044384582,0.000036925543,0.00012465367,0.00007007223,0.000092953414],"domain_scores_gemma":[0.9991997,0.000049750462,0.00029217254,0.00006414165,0.00019692384,0.0001973602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00103685,0.00041717794,0.0005283079,0.00097042386,0.0012889403,0.002079845,0.00030772254,0.0006086279,0.0015181112],"category_scores_gemma":[0.0014915627,0.00017313375,0.00035389108,0.0012753225,0.0006500568,0.00044300492,0.001343744,0.00085688074,0.00040957195],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006792041,0.00014673865,0.91709715,0.00021041243,0.00024558193,0.0009149208,0.0015059786,0.001911655,0.010096662,0.0054230797,0.01425624,0.047512315],"study_design_scores_gemma":[0.00001314839,0.000045765995,0.9769934,0.00005701023,0.000021015818,0.0003039686,0.0002375236,0.0006399025,0.0005825206,0.00076147215,0.020330815,0.000013524649],"about_ca_topic_score_codex":0.014995023,"about_ca_topic_score_gemma":0.02065368,"teacher_disagreement_score":0.014995023,"about_ca_system_score_codex":0.001053394,"about_ca_system_score_gemma":0.0006972356,"threshold_uncertainty_score":0.029815435},"labels":[],"label_agreement":null},{"id":"W2137945591","doi":"10.1029/2008gl033906","title":"Light absorbing carbon emissions from commercial shipping","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lockheed Martin (Canada)","funders":"National Oceanic and Atmospheric Administration","keywords":"Environmental science; Aerosol; Arctic; Air quality index; Atmospheric sciences; The arctic; Climatology; Meteorology; Oceanography; Geography; Geology","score_opus":0.05294051348286676,"score_gpt":0.28193212140862617,"score_spread":0.2289916079257594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137945591","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987974,0.000070881746,0.00012495519,0.000004735571,6.9819833e-7,0.0000026187697,0.00018327661,0.000008153473,0.00080713653],"genre_scores_gemma":[0.9983699,0.0001523257,0.000297514,0.0000059675126,0.0000043769396,0.000005149545,0.00054821017,0.0000050841613,0.000611496],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000008409365,0.000003594849,0.000028734434,0.00003558439,0.000020571248],"domain_scores_gemma":[0.99986815,0.000021619455,0.00003257645,0.000009738594,0.000055740216,0.000012183894],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010702371,0.00022903584,0.00007697342,0.0006831149,0.00044215904,0.00026901017,0.0001679167,0.00017223966,0.0011419164],"category_scores_gemma":[0.00016919007,0.000087074906,0.00012314339,0.00092526537,0.00013280871,0.0001652519,0.00021773906,0.00013250197,0.00023769193],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005612433,0.00020348084,0.5823207,0.00025404207,0.00016709344,0.0009335914,0.0006856033,0.0024909878,0.35375583,0.00016124854,0.0011221494,0.057344075],"study_design_scores_gemma":[0.000008629981,0.00022059622,0.9211382,0.000010857276,0.000040092986,0.00044231262,0.0003026812,0.0018958194,0.072891444,0.000052411735,0.002982049,0.00001493619],"about_ca_topic_score_codex":0.015337771,"about_ca_topic_score_gemma":0.019867538,"teacher_disagreement_score":0.015337771,"about_ca_system_score_codex":0.0004568665,"about_ca_system_score_gemma":0.000102747224,"threshold_uncertainty_score":0.030496955},"labels":[],"label_agreement":null},{"id":"W2137966418","doi":"10.1002/2013gl058759","title":"Dynamics of sea level rise and coastal flooding on a changing landscape","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":208,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Center for Sponsored Coastal Ocean Research; National Oceanic and Atmospheric Administration; Canadian Centre for Applied Research in Cancer Control","keywords":"Storm surge; Flooding (psychology); Storm; Environmental science; Urbanization; Land cover; Sea level rise; Coastal flood; Sea level; Numerical modeling; Surge; Land use; Climatology; Climate change; Geology; Oceanography; Meteorology; Geography; Civil engineering; Ecology","score_opus":0.03662849073235787,"score_gpt":0.27762344345375595,"score_spread":0.2409949527213981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137966418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998035,0.000012440299,0.00064483064,0.00010358184,0.0000018958816,0.000002189054,0.00004997663,0.000010873067,0.0011392178],"genre_scores_gemma":[0.9997272,0.000011990243,0.00012663925,0.0000052680075,9.70749e-7,0.0000012375615,0.000017097327,0.0000013355694,0.00010831926],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993324,0.00003060937,0.0000028741563,0.000012962222,0.000007939743,0.000012371575],"domain_scores_gemma":[0.9998419,0.00004944876,0.00004096711,0.000012956663,0.000027163005,0.000027424809],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017014408,0.00010482409,0.00013084739,0.00023234433,0.00023243715,0.00074311806,0.00021656841,0.0002733443,0.0012426452],"category_scores_gemma":[0.0007943708,0.00013153015,0.00023367551,0.00025664843,0.0004883696,0.00046886926,0.0003315883,0.00025222232,0.00007489685],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000121047255,0.00013099618,0.21745163,0.000023979554,0.00011306585,0.00069316075,0.00028947313,0.75346273,0.0117043145,0.008682285,0.0008252384,0.006502155],"study_design_scores_gemma":[0.00002542702,0.00010637366,0.119249284,0.0000066331104,0.000024518917,0.00011610133,0.00049733935,0.87633306,0.0005669643,0.0023966362,0.00066271704,0.000015015267],"about_ca_topic_score_codex":0.017606022,"about_ca_topic_score_gemma":0.013379551,"teacher_disagreement_score":0.017606022,"about_ca_system_score_codex":0.00082002976,"about_ca_system_score_gemma":0.00023860154,"threshold_uncertainty_score":0.03500706},"labels":[],"label_agreement":null},{"id":"W2137980068","doi":"10.1029/2007gl030638","title":"Connecting surface emissions, convective uplifting, and long‐range transport of carbon monoxide in the upper troposphere: New observations from the Aura Microwave Limb Sounder","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Microwave Limb Sounder; Troposphere; Environmental science; Atmospheric sciences; Boreal; Convection; Climatology; Range (aeronautics); Geology; Meteorology; Geography; Materials science","score_opus":0.04146750853937198,"score_gpt":0.27711926978624724,"score_spread":0.23565176124687526,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2137980068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989262,0.00021066367,0.000090503745,0.000037878162,0.000004989688,0.0000018433029,0.00045572204,0.000004459528,0.00026765655],"genre_scores_gemma":[0.9983883,0.00012654638,0.00015707657,0.000013235421,0.000012862939,0.000003994093,0.0011728376,0.000001958744,0.00012325236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.000013604934,0.00001064241,0.000024611938,0.000025883819,0.000029083207],"domain_scores_gemma":[0.99955934,0.00009264551,0.00016149115,0.00003746095,0.00008373322,0.00006526388],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024189058,0.00020268101,0.00016441294,0.0004720121,0.00025436294,0.0005566178,0.00014872372,0.00035183772,0.00030278802],"category_scores_gemma":[0.0005680516,0.00017118247,0.00025383505,0.00061238854,0.0001798386,0.00039753944,0.00036571568,0.00021544515,0.00010291157],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011249973,0.000042843785,0.990864,0.00001785002,0.00008879547,0.00012875961,0.00014161329,0.00045199136,0.0038222831,0.000033741584,0.00020023635,0.004095453],"study_design_scores_gemma":[0.0000021412218,0.000009327265,0.999012,0.0000014696374,0.0000136762,0.000049465518,0.000035763962,0.00038386535,0.00022243557,0.00001113513,0.00025627363,0.0000024528822],"about_ca_topic_score_codex":0.02061336,"about_ca_topic_score_gemma":0.036986988,"teacher_disagreement_score":0.02061336,"about_ca_system_score_codex":0.00032796772,"about_ca_system_score_gemma":0.00022451975,"threshold_uncertainty_score":0.040986776},"labels":[],"label_agreement":null},{"id":"W2138019458","doi":"10.1002/2015gl065434","title":"Laboratory investigation of perchlorate deliquescence at the surface of Mars with a Raman scattering lidar","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency","keywords":"Mars Exploration Program; Perchlorate; Relative humidity; Eutectic system; Analytical Chemistry (journal); Frost (temperature); Water vapor; Materials science; Mineralogy; Brine; Chemistry; Environmental chemistry; Astrobiology; Meteorology; Composite material","score_opus":0.04916964203074902,"score_gpt":0.2888891430257381,"score_spread":0.23971950099498907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138019458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988986,0.00002026805,0.00060410745,0.000028611332,0.0000027630042,0.000011125841,0.00005298961,0.00002223977,0.0003592687],"genre_scores_gemma":[0.9986136,0.000021900441,0.0010181868,0.00001545041,0.000006146886,0.000010111689,0.00006804032,0.0000045917204,0.0002418887],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99979657,0.000037254205,0.0000065767613,0.000047820202,0.00007279912,0.000038952625],"domain_scores_gemma":[0.9998281,0.00003663703,0.00002718834,0.000017631088,0.00006309301,0.000027430708],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033801084,0.00030066966,0.0002367271,0.00025555625,0.0007488335,0.00029596727,0.00043261045,0.00053999975,0.0006840742],"category_scores_gemma":[0.0002855996,0.00016233609,0.00021899163,0.0001592242,0.0003849508,0.00023880706,0.00027528516,0.00042821944,0.0002167901],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010830377,0.0001110048,0.0053315144,0.00001599731,0.000011991239,0.00015446657,0.00019339485,0.00037909602,0.99224347,0.000056108333,0.000058828453,0.0013357812],"study_design_scores_gemma":[0.00006483695,0.0029496609,0.048442375,0.0000072222456,0.000024604873,0.00042519148,0.00075059955,0.0074764183,0.9380738,0.000115796865,0.0016462017,0.000023242988],"about_ca_topic_score_codex":0.0013204745,"about_ca_topic_score_gemma":0.0013578862,"teacher_disagreement_score":0.0013204745,"about_ca_system_score_codex":0.00019860339,"about_ca_system_score_gemma":0.0001884879,"threshold_uncertainty_score":0.0026255846},"labels":[],"label_agreement":null},{"id":"W2138289208","doi":"10.1029/2005gl023032","title":"Measurements of O<sub>3</sub>, NO<sub>2</sub> and Temperature during the 2004 Canadian Arctic ACE Validation Campaign","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Radiosonde; Arctic; Environmental science; Occultation; Atmospheric sciences; Meteorology; Lidar; Climatology; Satellite; Geology; Remote sensing; Geography; Oceanography; Physics","score_opus":0.021176032078921703,"score_gpt":0.2416536881689326,"score_spread":0.22047765609001088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138289208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9837493,0.00022961714,0.0019847022,0.00012005983,0.00002059517,0.00003893533,0.0057590315,0.00014384252,0.007953961],"genre_scores_gemma":[0.98594856,0.00021798792,0.0033439975,0.00009683567,0.00001068527,0.000045490397,0.0077586905,0.000055618973,0.0025222183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99937636,0.000036861715,0.000011677001,0.000090340196,0.0003553156,0.000129537],"domain_scores_gemma":[0.99869674,0.00005574541,0.00008449017,0.00006719975,0.0009925927,0.000103248196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070594053,0.00046239438,0.0003196939,0.00041925025,0.0017153209,0.0005525764,0.0005691916,0.00025636426,0.0005549653],"category_scores_gemma":[0.0009790554,0.00024566817,0.00018496119,0.0006772042,0.00032614492,0.00028368286,0.0003613483,0.00043880474,0.0001957805],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002624353,0.00042380672,0.69318753,0.00020420576,0.0005570457,0.00035393392,0.0017364593,0.042171333,0.16689312,0.0013460678,0.019835314,0.07066679],"study_design_scores_gemma":[0.00006037272,0.00007699861,0.95149904,0.00001825521,0.000071518196,0.00004898018,0.00023173509,0.011899375,0.026768794,0.00008323391,0.009189251,0.000052488962],"about_ca_topic_score_codex":0.88092226,"about_ca_topic_score_gemma":0.9514751,"teacher_disagreement_score":0.11907774,"about_ca_system_score_codex":0.005882658,"about_ca_system_score_gemma":0.005315542,"threshold_uncertainty_score":0.23955798},"labels":[],"label_agreement":null},{"id":"W2138401170","doi":"10.1002/2013gl058909","title":"The timing of alluvial activity in Gale crater, Mars","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Impact crater; Geology; Noachian; Hesperian; Mars Exploration Program; Fluvial; Alluvial fan; Alluvium; Astrobiology; Sedimentary depositional environment; Earth science; Diagenesis; Geomorphology; Paleontology; Geochemistry; Sedimentary rock; Martian","score_opus":0.04592257461157909,"score_gpt":0.31292655220534815,"score_spread":0.26700397759376904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138401170","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979552,0.00019688914,0.00008288255,0.00004893313,0.0000037253583,0.000004535748,0.00037955015,0.000018587432,0.001309664],"genre_scores_gemma":[0.99926907,0.000081236656,0.00009971573,0.000010333716,0.000005037102,0.0000031424788,0.00024602804,0.000004735522,0.00028077542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983513,0.000026684482,0.000009666083,0.000046583813,0.000033540266,0.00004846482],"domain_scores_gemma":[0.99944633,0.00009461104,0.00015636078,0.000042739888,0.00015552883,0.000104473496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031937618,0.00023869642,0.00019784775,0.0026191878,0.00051969953,0.0011086499,0.00027266445,0.0003911365,0.0013762048],"category_scores_gemma":[0.0009433491,0.00018509086,0.00016239275,0.0009397993,0.00071128085,0.00044565214,0.0012828441,0.00024215477,0.00026165042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002535024,0.000017602897,0.9748369,0.000050530616,0.000087549204,0.00037662167,0.0022201054,0.00080792414,0.0064256815,0.00027006664,0.00057653594,0.014077024],"study_design_scores_gemma":[0.0000018189768,0.000015895303,0.99863356,0.0000054374523,0.0000033058445,0.00004142409,0.00024316378,0.00008555656,0.00018269043,0.000015889798,0.00076816225,0.0000029049459],"about_ca_topic_score_codex":0.023902375,"about_ca_topic_score_gemma":0.0412114,"teacher_disagreement_score":0.023902375,"about_ca_system_score_codex":0.0006016536,"about_ca_system_score_gemma":0.00025207832,"threshold_uncertainty_score":0.04752654},"labels":[],"label_agreement":null},{"id":"W2138488625","doi":"10.1029/2000gl012238","title":"Surface heat flux histories from geothermal data: Inferences from inversion","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geothermal gradient; Inversion (geology); Geology; Heat flux; Geophysics; Geothermal heating; Geothermal energy; Singular value decomposition; Energy balance; Seismology; Heat transfer; Mechanics; Thermodynamics; Physics; Tectonics; Mathematics; Algorithm","score_opus":0.14596433449985702,"score_gpt":0.3216769731764779,"score_spread":0.1757126386766209,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138488625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92316556,0.00026620209,0.070971124,0.00023842684,0.000013304836,0.000033516208,0.0008851352,0.00037333043,0.0040534646],"genre_scores_gemma":[0.9886148,0.00013977778,0.0103709325,0.000011535319,0.000013140998,0.000008789713,0.00069222186,0.000017549517,0.0001312715],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99983704,0.00005181345,0.000010479534,0.000021895028,0.000052233725,0.00002650163],"domain_scores_gemma":[0.99923646,0.00044908462,0.00006296997,0.00008594032,0.0001378132,0.000027655165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00066479226,0.00029861595,0.00022948263,0.00084799185,0.00017201973,0.00072602485,0.00023045024,0.0002897053,0.0006253708],"category_scores_gemma":[0.0076252753,0.0002583141,0.00034188756,0.00070352346,0.0004934549,0.0008671114,0.00029254414,0.000384853,0.00020126805],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000530186,0.00018768871,0.15462567,0.0002220908,0.00022379351,0.00030435508,0.00037104744,0.5530058,0.029782334,0.010994706,0.0013525765,0.24839978],"study_design_scores_gemma":[0.00005224361,0.000052018993,0.047762763,0.00004615128,0.000057675617,0.00008948092,0.00016009047,0.9295845,0.010758796,0.009989814,0.0014092303,0.000037306712],"about_ca_topic_score_codex":0.014698137,"about_ca_topic_score_gemma":0.014550648,"teacher_disagreement_score":0.014698137,"about_ca_system_score_codex":0.00045141194,"about_ca_system_score_gemma":0.00071139744,"threshold_uncertainty_score":0.02922517},"labels":[],"label_agreement":null},{"id":"W2138520970","doi":"10.1002/2013gl057814","title":"Tide‐induced microseismicity in the Mertz glacier grounding area, East Antarctica","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Institut Polaire Français Paul Emile Victor; Centre National de la Recherche Scientifique; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Polar Knowledge Canada","keywords":"Geology; Glacier; Oceanography; Outflow; Seismometer; Tidewater glacier cycle; Iceberg; Seismology; Geomorphology; Ice sheet; Ice calving","score_opus":0.08294011936000019,"score_gpt":0.29380985166986356,"score_spread":0.2108697323098634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2138520970","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992673,0.00003951475,0.000020128127,0.00002139653,0.0000014604522,0.0000019780696,0.000351231,0.0000030653773,0.00029398422],"genre_scores_gemma":[0.99950993,0.00004446826,0.000039241902,0.000007644539,0.0000038159665,0.0000028286063,0.00027504598,0.0000013380594,0.000115733375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999424,0.000011923237,0.0000043755263,0.000011104082,0.000013213587,0.000016928261],"domain_scores_gemma":[0.9997032,0.000039931776,0.00012696393,0.000028060464,0.000060204053,0.000041598934],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016988213,0.00020782443,0.00015280549,0.0011917952,0.00034858746,0.00045603173,0.00015460188,0.00019765674,0.00086890365],"category_scores_gemma":[0.00048362106,0.00010038321,0.00013457995,0.0011853876,0.00029769525,0.0001963153,0.00037681242,0.00012168476,0.00016355701],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007005713,0.000011829721,0.9928625,0.0000130469525,0.000029696355,0.00011413975,0.0002814069,0.0004476434,0.0028368188,0.000023628516,0.00021309436,0.0030961272],"study_design_scores_gemma":[0.0000011628865,0.000008055397,0.9995394,0.0000014503858,0.0000033014705,0.000015904167,0.00014755447,0.0001135971,0.00007281309,0.0000060269977,0.00008983074,9.0997355e-7],"about_ca_topic_score_codex":0.03409825,"about_ca_topic_score_gemma":0.07072647,"teacher_disagreement_score":0.03409825,"about_ca_system_score_codex":0.00043018418,"about_ca_system_score_gemma":0.00029637557,"threshold_uncertainty_score":0.06779951},"labels":[],"label_agreement":null},{"id":"W2139128218","doi":"10.1029/2011gl048054","title":"Nighttime nitric oxide densities in the Southern Hemisphere mesosphere–lower thermosphere","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Waterloo; University of Toronto","funders":"","keywords":"Mesosphere; Thermosphere; Atmospheric sciences; Stratosphere; Mesopause; Environmental science; Airglow; Ozone layer; Solstice; Southern Hemisphere; Northern Hemisphere; Climatology; Latitude; Ionosphere; Geology; Physics; Astronomy","score_opus":0.0227308856000558,"score_gpt":0.25632006167543514,"score_spread":0.23358917607537935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139128218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980894,0.00016810364,0.000084743326,0.000057306203,0.000006412725,0.0000016749776,0.0006666663,0.000007696613,0.0009181155],"genre_scores_gemma":[0.99869627,0.00008188143,0.00011039556,0.000018658338,0.0000073985734,0.0000026340906,0.00079230056,0.0000015080519,0.000289076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997413,0.0000030534484,0.0000014302111,0.000009581305,0.000005941128,0.000005816767],"domain_scores_gemma":[0.999918,0.000008201017,0.000021353284,0.000006394962,0.000022153288,0.000023879244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011786714,0.00007944798,0.00006530159,0.00027026367,0.00013761906,0.00018006818,0.00007202574,0.000112840185,0.0005427493],"category_scores_gemma":[0.00016273704,0.000066099026,0.000077078745,0.00018985785,0.0000842223,0.00016820885,0.00010981696,0.00012075,0.00010294945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002062934,0.00003060219,0.9511257,0.000024981591,0.00005949863,0.000118492135,0.00020244693,0.0007465067,0.036742747,0.00016630517,0.00080963713,0.009766722],"study_design_scores_gemma":[0.0000018544685,0.000006073318,0.99887806,0.0000011844774,0.0000028182367,0.000010495704,0.000017080769,0.00026643017,0.00041024355,0.000021916501,0.00038287672,0.0000010708231],"about_ca_topic_score_codex":0.018570192,"about_ca_topic_score_gemma":0.03201791,"teacher_disagreement_score":0.018570192,"about_ca_system_score_codex":0.00023773251,"about_ca_system_score_gemma":0.00012043688,"threshold_uncertainty_score":0.036924183},"labels":[],"label_agreement":null},{"id":"W2139394660","doi":"10.1029/2000gl011676","title":"Realistic semiannual oscillation simulated in a middle atmosphere general circulation model","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University","funders":"","keywords":"Atmosphere (unit); Oscillation (cell signaling); General Circulation Model; Mesosphere; Climatology; Atmospheric sciences; Geology; Gravity wave; Atmospheric model; Circulation (fluid dynamics); Amplitude; Quasi-biennial oscillation; Environmental science; Meteorology; Troposphere; Stratosphere; Gravitational wave; Physics; Mechanics; Climate change","score_opus":0.03171736259286063,"score_gpt":0.3008432901791647,"score_spread":0.2691259275863041,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139394660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9833572,0.00014689163,0.0031035293,0.00039662787,0.00004336617,0.000040827545,0.0038875036,0.00027329515,0.00875079],"genre_scores_gemma":[0.99501026,0.00008058975,0.0017127051,0.000046735222,0.000007402411,0.000029634759,0.0020151203,0.000028781948,0.0010688],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985933,0.000026827434,0.000005462938,0.000029836574,0.000020693324,0.000057803867],"domain_scores_gemma":[0.999655,0.00007297085,0.000031164644,0.00003182195,0.00009917657,0.0001098415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028965145,0.0005045843,0.0004947744,0.00036908084,0.0009017221,0.001008139,0.0017410201,0.0012286666,0.0025929199],"category_scores_gemma":[0.0011312789,0.0002824334,0.00047244175,0.0008609712,0.0005809784,0.000692247,0.0005582553,0.0010045561,0.00026425952],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032353876,0.00011163641,0.012027368,0.0000375234,0.000097284676,0.00016616716,0.00012705859,0.975599,0.0031197702,0.0039291424,0.002077786,0.0023837772],"study_design_scores_gemma":[0.00014222121,0.00003872953,0.008144424,0.000005349614,0.0000394236,0.000012482025,0.000067078945,0.9892944,0.00045786705,0.00061528897,0.0011595283,0.000023155524],"about_ca_topic_score_codex":0.51483244,"about_ca_topic_score_gemma":0.35359576,"teacher_disagreement_score":0.51483244,"about_ca_system_score_codex":0.003740328,"about_ca_system_score_gemma":0.002969132,"threshold_uncertainty_score":0.9760496},"labels":[],"label_agreement":null},{"id":"W2139808719","doi":"10.1029/2008gl033172","title":"Western Canadian glaciers advance in concert with climate change circa 4.2 ka","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":65,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Calgary; Simon Fraser University; University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; China Scholarship Council","keywords":"Glacier; Radiocarbon dating; Climate change; Geology; Physical geography; Period (music); Northern Hemisphere; Clastic rock; Southern Hemisphere; Climatology; Oceanography; Structural basin; Geography; Geomorphology; Paleontology","score_opus":0.058494857610223085,"score_gpt":0.295769516989674,"score_spread":0.23727465937945094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2139808719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97425205,0.0019249659,0.0005947755,0.0011108546,0.000045796758,0.000018091676,0.002054669,0.000108477405,0.019890353],"genre_scores_gemma":[0.99239254,0.0010046023,0.00045955373,0.000117661286,0.0000106922935,0.000003175216,0.0008197413,0.00000937224,0.005182672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998715,0.000004324598,0.0000030509811,0.000026371641,0.000041914624,0.000052769927],"domain_scores_gemma":[0.99952626,0.000018167655,0.00008142768,0.000015210596,0.0002960998,0.00006288824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001696555,0.00026676996,0.00013790689,0.0005892793,0.0020523954,0.0010206783,0.00022421083,0.00019557416,0.0025204842],"category_scores_gemma":[0.00044143025,0.00013467096,0.000169315,0.00082260545,0.00042843854,0.00035710508,0.00041943893,0.00040358023,0.00021252918],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024104468,0.000027893104,0.9133125,0.000111956004,0.00017605882,0.00030212302,0.0020986672,0.0017328573,0.017802292,0.0021649522,0.0064879577,0.05554165],"study_design_scores_gemma":[0.000005434951,0.000009318349,0.9778862,0.00001682545,0.000032268268,0.00009740773,0.00078265805,0.00026595642,0.0009462873,0.00016062347,0.019786548,0.000010512874],"about_ca_topic_score_codex":0.9616182,"about_ca_topic_score_gemma":0.9911015,"teacher_disagreement_score":0.038381815,"about_ca_system_score_codex":0.011278334,"about_ca_system_score_gemma":0.010149389,"threshold_uncertainty_score":0.08183038},"labels":[],"label_agreement":null},{"id":"W2140051688","doi":"10.1002/grl.50249","title":"Annular mode changes in the CMIP5 simulations","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":218,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Coupled model intercomparison project; Mode (computer interface); Volcano; Climatology; Environmental science; Atmospheric sciences; Arctic oscillation; Irradiance; Oscillation (cell signaling); Aerosol; Climate model; Meteorology; Geology; Climate change; Physics; Optics","score_opus":0.05749989835012122,"score_gpt":0.33721286300214176,"score_spread":0.27971296465202056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140051688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98694044,0.00021653454,0.002499452,0.00037810905,0.000073345196,0.000035279954,0.004176655,0.0002906281,0.005389629],"genre_scores_gemma":[0.99565977,0.0000686382,0.0012831695,0.00007807304,0.0000131792995,0.00003072941,0.0025118222,0.00006014783,0.000294435],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99946684,0.0001470395,0.000040348958,0.00017350553,0.000062577834,0.00010972293],"domain_scores_gemma":[0.99852484,0.00055466156,0.00017967,0.0001995002,0.00033605116,0.00020531309],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016162028,0.0009562871,0.0006191936,0.0006629924,0.00056994945,0.0014445392,0.0013779176,0.0012793788,0.002365722],"category_scores_gemma":[0.005235657,0.00056438334,0.001023002,0.0011751256,0.0004895073,0.0012900628,0.0007349597,0.0011991583,0.00036801572],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002736003,0.00011102047,0.048107743,0.00005411624,0.00019499626,0.00015111444,0.00013722095,0.9410961,0.002212162,0.0024171395,0.0024876525,0.0027572252],"study_design_scores_gemma":[0.00014193862,0.00011187972,0.023367964,0.000036489717,0.00008534802,0.000061775536,0.00017389256,0.9701342,0.0023782116,0.001322065,0.0021234879,0.00006275506],"about_ca_topic_score_codex":0.035945937,"about_ca_topic_score_gemma":0.01632607,"teacher_disagreement_score":0.035945937,"about_ca_system_score_codex":0.0015381236,"about_ca_system_score_gemma":0.0008544701,"threshold_uncertainty_score":0.07147342},"labels":[],"label_agreement":null},{"id":"W2140466297","doi":"10.1029/1999gl010884","title":"Latitudinal distribution of atmospheric methyl bromide: Measurements and modeling","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Northern Hemisphere; Latitude; Southern Hemisphere; Environmental science; Atmospheric sciences; Tropics; Bromide; Troposphere; Climatology; Middle latitudes; Geology; Chemistry; Ecology","score_opus":0.0438474410574739,"score_gpt":0.29011320194716833,"score_spread":0.24626576088969443,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140466297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9881011,0.00019512394,0.0070746457,0.00006833783,0.0000074738105,0.0000148296085,0.0017320199,0.00023876439,0.002567761],"genre_scores_gemma":[0.9955011,0.00012009086,0.0027545863,0.000014099546,0.000005959577,0.000020524874,0.0010550616,0.000035821802,0.00049270206],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989545,0.000028985498,0.0000059743575,0.000043507822,0.0000131094685,0.000012982825],"domain_scores_gemma":[0.9998714,0.000029830331,0.000027789127,0.000026423093,0.000033084005,0.000011488702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037823583,0.00038329908,0.00019255107,0.00029951497,0.00019294219,0.00032067162,0.00041859772,0.00038389023,0.0006005106],"category_scores_gemma":[0.00036870124,0.00031570377,0.0005154359,0.00052796304,0.000117882446,0.00024874302,0.0001954815,0.00017505135,0.00032602556],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014915776,0.00006352222,0.5019548,0.000060903334,0.00021207175,0.0001956139,0.00016681157,0.46878442,0.01703767,0.000923056,0.00067543774,0.009776497],"study_design_scores_gemma":[0.00004975037,0.000048118192,0.25701562,0.000012441447,0.00006806466,0.00009541422,0.000071567534,0.7367777,0.0037516935,0.0002796723,0.00179329,0.00003668957],"about_ca_topic_score_codex":0.034989513,"about_ca_topic_score_gemma":0.024808904,"teacher_disagreement_score":0.034989513,"about_ca_system_score_codex":0.0004191156,"about_ca_system_score_gemma":0.0002625588,"threshold_uncertainty_score":0.069571674},"labels":[],"label_agreement":null},{"id":"W2140783961","doi":"10.1029/2011gl046863","title":"The 1992-2009 transport variability of the East Greenland-Irminger Current at 60°N","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Current (fluid); Oceanography; Climatology; Geography; Environmental science; Geology","score_opus":0.04219499129368376,"score_gpt":0.257912632269211,"score_spread":0.21571764097552726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140783961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99759775,0.00007830741,0.0000864362,0.000046368972,0.000008427861,0.0000039589513,0.0010570537,0.000013172552,0.0011086235],"genre_scores_gemma":[0.9973022,0.00006504873,0.00015832843,0.000023356984,0.000010062609,0.0000035010044,0.0019814596,0.0000058854316,0.00045006763],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999547,0.0000033948731,0.0000034684535,0.000017144555,0.00001011828,0.000011198633],"domain_scores_gemma":[0.9998615,0.000007786775,0.000048020465,0.000011110174,0.00005584535,0.000015716252],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001746632,0.00013742014,0.00009380805,0.00062834844,0.00021149601,0.00030042639,0.00013597525,0.0001899962,0.00075365225],"category_scores_gemma":[0.00029979236,0.000058281203,0.00010005904,0.0005830548,0.00015561956,0.00025218216,0.00021896845,0.00015135406,0.00020442347],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015919418,0.00008032606,0.95306927,0.000050998693,0.00010526941,0.00024445335,0.00046503285,0.0045607947,0.0109628355,0.0003476333,0.0034612715,0.026492914],"study_design_scores_gemma":[0.0000020010484,0.000008628308,0.9981072,0.000004927579,0.00000804496,0.000016144419,0.000036722577,0.00086471107,0.00019910205,0.000011876116,0.0007375983,0.0000030056658],"about_ca_topic_score_codex":0.08611331,"about_ca_topic_score_gemma":0.16430475,"teacher_disagreement_score":0.08611331,"about_ca_system_score_codex":0.00096595095,"about_ca_system_score_gemma":0.00039774965,"threshold_uncertainty_score":0.17122412},"labels":[],"label_agreement":null},{"id":"W2140785031","doi":"10.1002/2014gl059649","title":"Shifts in biological productivity inferred from nutrient drawdown in the southern Beaufort Sea (2003-2011) and northern Baffin Bay (1997-2011), Canadian Arctic","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval","funders":"","keywords":"Bay; Oceanography; Beaufort sea; Arctic; Productivity; Drawdown (hydrology); Environmental science; The arctic; Fishery; Beaufort scale; Geology","score_opus":0.021283834810143478,"score_gpt":0.23644806996442408,"score_spread":0.2151642351542806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2140785031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966234,0.00039492824,0.00007172509,0.00010266583,0.0000072329804,0.0000041916287,0.0013706301,0.000008560992,0.001416702],"genre_scores_gemma":[0.99781895,0.00019395756,0.0001454079,0.000033538712,0.0000039872757,0.000004196725,0.0014196519,0.0000035294768,0.00037675712],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996978,0.00001729725,0.000017374492,0.00006663939,0.000108861306,0.000092047376],"domain_scores_gemma":[0.9990677,0.000053974756,0.00015708772,0.000032401647,0.00052347546,0.00016534099],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005085798,0.00031256277,0.00026923005,0.0015597214,0.0016586737,0.001122221,0.0005811919,0.00031633195,0.0007242713],"category_scores_gemma":[0.0011489136,0.0002886901,0.0003347292,0.0025740722,0.00075781636,0.0003937651,0.0006279447,0.00031139475,0.0001406274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011826419,0.000011414489,0.98937166,0.000029956902,0.00008384652,0.00009844894,0.0010731771,0.00038764763,0.002517918,0.00012171217,0.0006273861,0.005558669],"study_design_scores_gemma":[8.0673146e-7,0.000002361412,0.9992912,0.0000031184911,0.0000052424202,0.0000101048745,0.00018743695,0.00009143995,0.00005834986,0.0000040071945,0.0003433961,0.000002485273],"about_ca_topic_score_codex":0.9851349,"about_ca_topic_score_gemma":0.9927891,"teacher_disagreement_score":0.0148651,"about_ca_system_score_codex":0.013134313,"about_ca_system_score_gemma":0.008420606,"threshold_uncertainty_score":0.09529656},"labels":[],"label_agreement":null},{"id":"W2141146292","doi":"10.1029/2003gl018207","title":"Airborne measurements of gravity wave breaking at the tropopause","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Environment Research Council; Eli Lilly and Company","keywords":"Tropopause; Breaking wave; Gravity wave; Turbulence; Wavelength; Atmospheric sciences; Geology; Gravitational wave; Zonal flow (plasma); Geophysics; Atmospheric wave; Meteorology; Stratosphere; Physics; Wave propagation; Optics; Astrophysics","score_opus":0.04190988580571262,"score_gpt":0.2981817388422731,"score_spread":0.25627185303656047,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141146292","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996727,0.000040066458,0.0006151443,0.00002625135,0.000010605645,0.000009184794,0.0005565444,0.000023911496,0.0019912398],"genre_scores_gemma":[0.9974734,0.00006336867,0.0012327827,0.000016897839,0.000015800255,0.0000073654596,0.00082463125,0.0000040472087,0.00036155677],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000008030024,0.0000026628584,0.000021546444,0.000031253447,0.000022598126],"domain_scores_gemma":[0.99980205,0.000032211192,0.000037712718,0.000020698099,0.00007344742,0.00003394583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001090531,0.00018487021,0.00008848794,0.00031865385,0.0002215786,0.00028026119,0.00016861207,0.0001849499,0.00071357127],"category_scores_gemma":[0.00026345928,0.000119809745,0.00008010473,0.00025276278,0.00008482407,0.00016285485,0.00018850173,0.00021642103,0.000118339805],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005000155,0.00025360743,0.36674175,0.0001022366,0.00013956186,0.00030941117,0.0013839783,0.0020720807,0.58210796,0.00049399387,0.0013866702,0.04450869],"study_design_scores_gemma":[0.00006745829,0.0003210117,0.9739803,0.000011533976,0.00006216345,0.00020832686,0.00040374743,0.004544984,0.017728483,0.00011436968,0.0025420429,0.00001550152],"about_ca_topic_score_codex":0.007828372,"about_ca_topic_score_gemma":0.013325731,"teacher_disagreement_score":0.007828372,"about_ca_system_score_codex":0.00012872608,"about_ca_system_score_gemma":0.00012378182,"threshold_uncertainty_score":0.015565634},"labels":[],"label_agreement":null},{"id":"W2141422941","doi":"10.1029/2012gl053545","title":"Recent changes in the dynamic properties of declining Arctic sea ice: A model study","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs; Office of Naval Research; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Arctic ice pack; Sea ice; Antarctic sea ice; Sea ice thickness; Fast ice; Geology; Drift ice; Ice-albedo feedback; Sea ice growth processes; Cryosphere; Arctic; Climatology; Atmospheric sciences; Oceanography","score_opus":0.08095345238424943,"score_gpt":0.3173544779028284,"score_spread":0.23640102551857894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141422941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962986,0.00006234563,0.0007011724,0.00010294832,0.000008559825,0.000011767,0.0007329665,0.00004269273,0.0020390349],"genre_scores_gemma":[0.99793774,0.000079607824,0.0006761769,0.00002692447,0.0000053359154,0.000023021046,0.0007670159,0.000020679963,0.00046346552],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999866,0.000036420715,0.000010505674,0.000036888217,0.000017549755,0.00003262799],"domain_scores_gemma":[0.9993986,0.00028041867,0.00009210192,0.00006181684,0.000101573896,0.00006543385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00063640985,0.0005677449,0.00058930035,0.0004937932,0.000639193,0.0009856331,0.0009960547,0.0015507732,0.0014966491],"category_scores_gemma":[0.0015217258,0.00034358288,0.0013356521,0.0008258369,0.0005334782,0.0008128858,0.00037411327,0.0006732123,0.00023625989],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015998975,0.00013235451,0.028179694,0.000038124894,0.00007539816,0.00015534565,0.000080604405,0.96762764,0.0011701981,0.00051752926,0.0004959558,0.001367114],"study_design_scores_gemma":[0.00006578434,0.00009988616,0.014514819,0.000011549338,0.000036283822,0.0000442414,0.000111047986,0.9838815,0.00049059786,0.00025296697,0.00046770027,0.000023599958],"about_ca_topic_score_codex":0.073087916,"about_ca_topic_score_gemma":0.03613199,"teacher_disagreement_score":0.073087916,"about_ca_system_score_codex":0.001762029,"about_ca_system_score_gemma":0.0008907014,"threshold_uncertainty_score":0.145325},"labels":[],"label_agreement":null},{"id":"W2141710657","doi":"10.1029/2011gl047013","title":"Mapping sea surface oil slicks using RADARSAT-2 quad-polarization SAR image","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oil Spill Detection and Mitigation","field":"Environmental Science","cited_by":191,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Racing slick; Remote sensing; Synthetic aperture radar; Geology; Scattering; Polarimetry; Environmental science; Polarization (electrochemistry); Optics; Physics","score_opus":0.051907261253306636,"score_gpt":0.29252962562569285,"score_spread":0.2406223643723862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141710657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.885771,0.0001273638,0.11163811,0.00006094302,0.0000104151095,0.00003879571,0.00079171255,0.00033903422,0.0012225484],"genre_scores_gemma":[0.90201706,0.00015172295,0.09664698,0.000017289529,0.000007351435,0.000012793734,0.00078042323,0.00001594236,0.00035047613],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.0000080554955,0.000002791897,0.000012430491,0.000022676035,0.000008825236],"domain_scores_gemma":[0.999892,0.000012524045,0.000030008741,0.0000118459975,0.00004397961,0.000009545015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013497578,0.000388707,0.0001788807,0.00083487545,0.000112065136,0.0002562516,0.0001534715,0.00016215185,0.00038321211],"category_scores_gemma":[0.00032519177,0.00011168205,0.000109932,0.00040662015,0.00013338058,0.0002574781,0.00018777236,0.00010717016,0.00012861211],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000546471,0.00012927914,0.1090742,0.00020805452,0.00013127667,0.00029143674,0.00022768397,0.072887406,0.46035236,0.0006103247,0.001517009,0.35402444],"study_design_scores_gemma":[0.00004597658,0.00016248942,0.31068727,0.000024947998,0.00010409949,0.00045629474,0.00022425145,0.55272603,0.13349529,0.0006501883,0.0013661748,0.00005704182],"about_ca_topic_score_codex":0.0054136096,"about_ca_topic_score_gemma":0.007887084,"teacher_disagreement_score":0.0054136096,"about_ca_system_score_codex":0.00016260907,"about_ca_system_score_gemma":0.0002939151,"threshold_uncertainty_score":0.010764241},"labels":[],"label_agreement":null},{"id":"W2141921649","doi":"10.1029/2004gl021436","title":"Evidence of lightning NO<sub>x</sub> and convective transport of pollutants in satellite observations over North America","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Lightning (connector); Convection; Troposphere; Satellite; Environmental science; Altitude (triangle); Meteorology; Atmospheric sciences; Chemical transport model; Geology; Climatology; Geography; Physics","score_opus":0.04398219951975068,"score_gpt":0.2741628293561447,"score_spread":0.23018062983639404,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2141921649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996006,0.00002890155,0.00004108647,0.000027033067,7.617006e-7,0.000001012075,0.00009719646,0.0000067009046,0.00019688865],"genre_scores_gemma":[0.9995409,0.00005181935,0.00008867507,0.000012960213,0.0000021420306,0.0000019950216,0.00021849555,0.0000015450524,0.0000814953],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995124,0.000009730416,0.000003819771,0.000011277711,0.0000114310815,0.000012519938],"domain_scores_gemma":[0.9995346,0.0001321007,0.0001543648,0.000023880175,0.00008410536,0.00007091465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014073768,0.000113239774,0.00012702147,0.00026648905,0.00020965686,0.00024322612,0.00013037064,0.00023736806,0.0003829094],"category_scores_gemma":[0.00048792872,0.00018238416,0.00013320746,0.00030164619,0.00019637634,0.00021283906,0.00017600702,0.00013948968,0.00004435558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001500815,0.00004575494,0.9800961,0.00003067822,0.00007417509,0.00020198445,0.00024943607,0.0022088415,0.013132179,0.000076848686,0.00037582222,0.0033581622],"study_design_scores_gemma":[0.000007505291,0.000024002344,0.9963253,0.0000038232292,0.000019878764,0.000067348155,0.00010681661,0.002535396,0.000737319,0.000019437375,0.00015050719,0.000002709274],"about_ca_topic_score_codex":0.05619145,"about_ca_topic_score_gemma":0.10446162,"teacher_disagreement_score":0.05619145,"about_ca_system_score_codex":0.0004591656,"about_ca_system_score_gemma":0.0002907468,"threshold_uncertainty_score":0.11172873},"labels":[],"label_agreement":null},{"id":"W2142041006","doi":"10.1029/2007gl029942","title":"Global phosgene observations from the Atmospheric Chemistry Experiment (ACE) mission","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; University of Waterloo","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Stratosphere; Phosgene; Occultation; Atmospheric sciences; Equator; Atmospheric chemistry; Altitude (triangle); Environmental science; Latitude; Mixing ratio; Ozone; Ozone layer; Longitude; Meteorology; Chemistry; Physics; Astrophysics; Astronomy; Organic chemistry","score_opus":0.04485102625483447,"score_gpt":0.3078813227370183,"score_spread":0.26303029648218385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142041006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93715423,0.00020470419,0.0009180795,0.00014909216,0.000031274965,0.00012364206,0.04790907,0.0001904546,0.013319505],"genre_scores_gemma":[0.9355173,0.00035062913,0.0038053244,0.00015014644,0.00006792784,0.00011990828,0.057989836,0.00004059907,0.0019582743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984336,0.000012774043,0.0000067867927,0.000039501574,0.00006834482,0.0000292151],"domain_scores_gemma":[0.9997558,0.000013999191,0.00008493332,0.000031421525,0.0000787307,0.00003501963],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026970456,0.00037092157,0.00021552364,0.0006672114,0.00023883117,0.00037447613,0.00021636554,0.00027759816,0.0010697835],"category_scores_gemma":[0.00027936403,0.0001375119,0.00013841357,0.0012369491,0.0001601709,0.00033754198,0.0005412326,0.0002459602,0.00022329051],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007493141,0.00024340776,0.8629338,0.00036985188,0.00031508677,0.00051818,0.0006674479,0.008788142,0.06378307,0.0009941029,0.018615235,0.042022314],"study_design_scores_gemma":[0.00005175786,0.000050593953,0.98248315,0.000009840794,0.000032873042,0.000046545636,0.00007801934,0.001458163,0.0037773605,0.00010865267,0.011890811,0.000012320516],"about_ca_topic_score_codex":0.020290494,"about_ca_topic_score_gemma":0.029029587,"teacher_disagreement_score":0.020290494,"about_ca_system_score_codex":0.00040339306,"about_ca_system_score_gemma":0.0005874005,"threshold_uncertainty_score":0.040344775},"labels":[],"label_agreement":null},{"id":"W2142163627","doi":"10.1029/2011gl048540","title":"In-situ degassing study on crystal-bearing Stromboli basaltic magmas: Implications for Stromboli explosions","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Geology; Volcano; Basalt; Seismology; Petrology","score_opus":0.13077145597004364,"score_gpt":0.327131406946434,"score_spread":0.19635995097639036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2142163627","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959265,0.00042388085,0.00039681362,0.000033529865,0.000011185114,0.00002112231,0.00074066984,0.000017150762,0.002429222],"genre_scores_gemma":[0.99689686,0.00045507457,0.000885262,0.00001743867,0.000017284057,0.000009973231,0.0005168446,0.0000072548355,0.0011941348],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999167,0.0000065605864,0.000007425672,0.000032153068,0.000019584948,0.00001771176],"domain_scores_gemma":[0.99977165,0.000044378387,0.000057168912,0.000012722018,0.00007833329,0.00003577778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002099025,0.00017879989,0.0003258708,0.0012093154,0.00060317735,0.000525246,0.0002682454,0.00033061227,0.0015548925],"category_scores_gemma":[0.00039835318,0.00010385283,0.00015649783,0.0011065049,0.00024123557,0.00045452645,0.00029398268,0.00021923521,0.00033325242],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010274517,0.00015391089,0.61315256,0.00036773767,0.000088940295,0.0011128256,0.0015296459,0.00047478135,0.35675335,0.0005173644,0.0007630438,0.02405839],"study_design_scores_gemma":[0.000019691703,0.00019053638,0.9669849,0.0000213081,0.000081614315,0.00034923342,0.0013323757,0.001182557,0.025632653,0.000201624,0.0039936504,0.000009876618],"about_ca_topic_score_codex":0.009096472,"about_ca_topic_score_gemma":0.014870381,"teacher_disagreement_score":0.009096472,"about_ca_system_score_codex":0.00038864717,"about_ca_system_score_gemma":0.00039262633,"threshold_uncertainty_score":0.01808703},"labels":[],"label_agreement":null},{"id":"W2143108104","doi":"10.1029/2005gl024214","title":"Atmospheric Chemistry Experiment (ACE) measurements of elevated Southern Hemisphere upper tropospheric CO, C<sub>2</sub>H<sub>6</sub>, HCN, and C<sub>2</sub>H<sub>2</sub> mixing ratios from biomass burning emissions and long‐range transport","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"North Dakota Soybean Council","keywords":"Stratosphere; Troposphere; Atmospheric sciences; Mixing ratio; Southern Hemisphere; Atmospheric chemistry; Northern Hemisphere; Latitude; Atmosphere (unit); Environmental science; Climatology; Ozone; Analytical Chemistry (journal); Chemistry; Meteorology; Geology; Physics; Environmental chemistry; Geodesy","score_opus":0.021011787016616254,"score_gpt":0.2498282506659631,"score_spread":0.22881646364934682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143108104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9753517,0.00018938091,0.0013956059,0.00015940021,0.000052804266,0.00012910394,0.014945281,0.00016390879,0.007612809],"genre_scores_gemma":[0.9752793,0.00021897412,0.0040039117,0.00018217448,0.00005326321,0.000072183975,0.018332407,0.00001829237,0.0018394911],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997942,0.000020744354,0.0000070266005,0.00004997218,0.000096687065,0.00003137868],"domain_scores_gemma":[0.9994848,0.000041380474,0.00012420009,0.000054319167,0.00017710467,0.00011823058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047172332,0.00034987828,0.0002663133,0.00033000956,0.0006145287,0.00036140223,0.00019093293,0.0002921865,0.0008996676],"category_scores_gemma":[0.0003775305,0.00015725772,0.00012614661,0.0005059796,0.00015162188,0.00027780043,0.00023604489,0.00037783454,0.00017983293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.003736924,0.0011418847,0.6637674,0.00020244734,0.00052791374,0.00050071464,0.0004324894,0.002135304,0.2703648,0.001067849,0.013151834,0.042970415],"study_design_scores_gemma":[0.000091859045,0.00019273654,0.9737021,0.0000034284242,0.000062869796,0.00010387386,0.000029141078,0.0010500137,0.019359421,0.00010544395,0.0052860808,0.000013118538],"about_ca_topic_score_codex":0.037436668,"about_ca_topic_score_gemma":0.06721269,"teacher_disagreement_score":0.037436668,"about_ca_system_score_codex":0.0007591354,"about_ca_system_score_gemma":0.00050968333,"threshold_uncertainty_score":0.0744375},"labels":[],"label_agreement":null},{"id":"W2143386652","doi":"10.1029/2007gl031738","title":"Neglecting ice‐atmosphere interactions underestimates ice sheet melt in millennial‐scale deglaciation simulations","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Alberta","funders":"","keywords":"Deglaciation; Ice sheet; Geology; Ice-sheet model; Atmospheric model; Climatology; Atmosphere (unit); Ice age; Sea ice growth processes; Atmospheric sciences; Sea ice; Cryosphere; Sea ice thickness; Ice stream; Holocene; Meteorology; Geomorphology; Glacial period; Oceanography; Physics","score_opus":0.053939136255036664,"score_gpt":0.32510223697424223,"score_spread":0.2711631007192056,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143386652","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9915069,0.00010948321,0.006304567,0.00016095923,0.000021176089,0.000019330262,0.00035200975,0.00020396926,0.0013216478],"genre_scores_gemma":[0.9973912,0.000090436486,0.0020204,0.0000480629,0.000006853572,0.00001633875,0.00023373967,0.000030699473,0.00016218105],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996805,0.00013576864,0.000028859076,0.00005996775,0.00003634336,0.000058555528],"domain_scores_gemma":[0.99839634,0.0010363066,0.00013505478,0.00021576053,0.00009553784,0.00012093274],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013512836,0.00057574763,0.0005910559,0.00029686026,0.00041614665,0.0009561227,0.0006195676,0.00065640506,0.00051498995],"category_scores_gemma":[0.005393414,0.00053188746,0.0005312787,0.00040180917,0.0004303464,0.0010024604,0.0005732529,0.0006357197,0.000115076815],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007662798,0.00003828092,0.026264159,0.000023975701,0.000076617674,0.00003355997,0.000055181117,0.96873426,0.0019105308,0.0006166202,0.00018024303,0.0019899],"study_design_scores_gemma":[0.000048288766,0.000055093253,0.010870337,0.00001019638,0.0000300131,0.000013616056,0.000033576875,0.9863638,0.0017354158,0.00052212283,0.00030483428,0.000012591809],"about_ca_topic_score_codex":0.02565242,"about_ca_topic_score_gemma":0.023869058,"teacher_disagreement_score":0.02565242,"about_ca_system_score_codex":0.0008629013,"about_ca_system_score_gemma":0.0014272628,"threshold_uncertainty_score":0.051006198},"labels":[],"label_agreement":null},{"id":"W2143622440","doi":"10.1029/2005gl023962","title":"Melt season duration on Canadian Arctic ice caps, 2000–2004","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Alberta","funders":"","keywords":"Bay; Elevation (ballistics); Scatterometer; Arctic; Climatology; Duration (music); Arctic ice pack; Environmental science; Geology; Atmospheric sciences; Sea ice; Oceanography; Wind speed","score_opus":0.01948482799457496,"score_gpt":0.25819956327426496,"score_spread":0.23871473527969,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143622440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9751242,0.001340322,0.00014397757,0.00019830665,0.000024294755,0.000014961771,0.019140705,0.00004828268,0.0039649913],"genre_scores_gemma":[0.9794723,0.00075848005,0.00028571713,0.00006489703,0.000012038747,0.000019541114,0.01686332,0.00001579766,0.0025080498],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99971956,0.000010575633,0.000015735797,0.000061724575,0.00011286152,0.00007951287],"domain_scores_gemma":[0.998114,0.000082133614,0.0002647879,0.00003430519,0.0012494194,0.00025534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039530755,0.00040624922,0.0003211734,0.0028183428,0.001924472,0.00092935446,0.0006716762,0.0002724968,0.0015992472],"category_scores_gemma":[0.0015215825,0.00028072813,0.00032906767,0.0028994307,0.00046691616,0.00037626267,0.00059824355,0.00033508043,0.00021388345],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062284607,0.000034266825,0.9606834,0.00017123073,0.0001909778,0.00014770418,0.0018393456,0.0017895481,0.0040930365,0.00019945193,0.0085743,0.02165394],"study_design_scores_gemma":[0.0000026299629,0.0000062749546,0.99650097,0.0000141382125,0.000013745344,0.000020535754,0.00025180102,0.00025879452,0.00020830431,0.000007666839,0.0027072423,0.000007917941],"about_ca_topic_score_codex":0.98955286,"about_ca_topic_score_gemma":0.9970208,"teacher_disagreement_score":0.017236242,"about_ca_system_score_codex":0.017236242,"about_ca_system_score_gemma":0.010259775,"threshold_uncertainty_score":0.12505823},"labels":[],"label_agreement":null},{"id":"W2143719229","doi":"10.1029/2000gl011874","title":"Monthly fractional green vegetation cover associated with land cover classes of the conterminous USA","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"NOAA Research; National Aeronautics and Space Administration","keywords":"Land cover; Grid cell; Vegetation (pathology); Biosphere; Environmental science; Cover (algebra); Grid; Land use; Climatology; Physical geography; Geography; Geology; Ecology","score_opus":0.016414197010711222,"score_gpt":0.25392272561402446,"score_spread":0.23750852860331323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143719229","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952147,0.000029638417,0.00011412715,0.000013545925,0.0000016382998,0.0000024803091,0.0034750912,0.000014190754,0.0011345546],"genre_scores_gemma":[0.9942676,0.00003163853,0.00017951908,0.000005800818,0.000003737458,0.000004647661,0.004814063,0.0000034334475,0.0006894252],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997115,0.0000048522866,0.0000017645914,0.00000809549,0.000006456282,0.00000770334],"domain_scores_gemma":[0.99984825,0.0000347598,0.00006003309,0.000009411366,0.000028133027,0.00001938464],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000735083,0.00009369701,0.000066675624,0.0005035647,0.00009347382,0.00017115456,0.00006438877,0.00007165443,0.0013856852],"category_scores_gemma":[0.00032297615,0.00003393059,0.00006323963,0.0005157386,0.00006282632,0.00010836035,0.000111326495,0.00008472447,0.0001281242],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076264536,0.000016641898,0.98616505,0.000012311816,0.000039864426,0.000052397852,0.00014626508,0.00117702,0.0018975273,0.0002073338,0.0016305204,0.008578765],"study_design_scores_gemma":[0.0000013533388,0.0000061384894,0.9980506,0.0000012986031,0.000005739621,0.000024198931,0.00005233818,0.0007827866,0.00018596133,0.000036385805,0.00085217046,0.0000010943588],"about_ca_topic_score_codex":0.021027219,"about_ca_topic_score_gemma":0.04783167,"teacher_disagreement_score":0.021027219,"about_ca_system_score_codex":0.0002035659,"about_ca_system_score_gemma":0.00006561545,"threshold_uncertainty_score":0.04180962},"labels":[],"label_agreement":null},{"id":"W2143902752","doi":"10.1002/grl.50919","title":"Statistics of vertical vorticity, divergence, and strain in a developed submesoscale turbulence field","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":242,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Vorticity; Acoustic Doppler current profiler; Pycnocline; Skewness; Geology; Potential vorticity; Turbulence; Divergence (linguistics); Geodesy; Physics; Meteorology; Statistics; Mathematics; Current (fluid); Oceanography; Vortex","score_opus":0.02531929550370401,"score_gpt":0.2711332071451468,"score_spread":0.2458139116414428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143902752","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992077,0.0000056381214,0.00046959598,0.0000069230205,7.788636e-7,0.0000016947464,0.00012851607,0.000018557485,0.00016073533],"genre_scores_gemma":[0.999521,0.000005016485,0.00016517342,0.000001150923,0.0000013774929,0.0000015759513,0.00024546048,0.0000022977324,0.00005698276],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999354,0.000008691288,0.0000057509487,0.000014887137,0.000015985419,0.00001933474],"domain_scores_gemma":[0.999511,0.00014761392,0.0001033178,0.00002734497,0.00010608439,0.00010471567],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002366867,0.00017627238,0.00020539822,0.0011736115,0.00017057115,0.00037067113,0.00011508812,0.0001068081,0.00035982463],"category_scores_gemma":[0.0007762094,0.00012755797,0.00016781251,0.00045102293,0.00026581332,0.00034471942,0.00020055982,0.00013708301,0.00007202855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052984833,0.00015623649,0.77758104,0.000038529586,0.00010135775,0.0007092257,0.0003480103,0.044033512,0.15223259,0.0018510163,0.0005403899,0.021878237],"study_design_scores_gemma":[0.000008198651,0.000082612954,0.93122137,0.0000031767024,0.000009498591,0.00006632626,0.00007472767,0.06425508,0.0038646038,0.00024228326,0.00015295894,0.000019180363],"about_ca_topic_score_codex":0.006266074,"about_ca_topic_score_gemma":0.0047723884,"teacher_disagreement_score":0.006266074,"about_ca_system_score_codex":0.00032190362,"about_ca_system_score_gemma":0.00018866267,"threshold_uncertainty_score":0.0124592185},"labels":[],"label_agreement":null},{"id":"W2143962435","doi":"10.1029/2012gl051445","title":"Transient nature of Arctic spring systems driven by subglacial meltwater","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Permafrost; Meltwater; Geology; Spring (device); Groundwater flow; Geomorphology; Arctic; Groundwater; Glacial period; Groundwater discharge; Fjord; Hydrology (agriculture); Aquifer; Oceanography; Geotechnical engineering","score_opus":0.04161667746095996,"score_gpt":0.29114454073239365,"score_spread":0.2495278632714337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143962435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955422,0.000058648875,0.0017218929,0.00010829637,0.000013807759,0.000007234152,0.00015448032,0.00012523662,0.002268164],"genre_scores_gemma":[0.9995933,0.000024361634,0.00012254281,0.000009217095,0.0000026598502,0.0000043029513,0.00006320862,0.0000074131262,0.00017299147],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999497,0.0000069244693,0.0000029869007,0.000011922324,0.0000061159008,0.000022400753],"domain_scores_gemma":[0.99984205,0.000034372842,0.000038199203,0.00001249188,0.000020796911,0.00005219873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013101942,0.00018368034,0.00034343798,0.00029109436,0.0005788397,0.00069439417,0.00044388103,0.00049339636,0.002184733],"category_scores_gemma":[0.00047914832,0.0002456424,0.0004073793,0.00018902081,0.0005077067,0.00045966616,0.0004236678,0.0003109311,0.00017801193],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006399025,0.00033403336,0.117885806,0.00014539271,0.00026245497,0.0014796251,0.0006000754,0.79486364,0.060632415,0.008993032,0.0025735116,0.011590038],"study_design_scores_gemma":[0.000061937215,0.00012964207,0.050486997,0.000014773209,0.00004622287,0.000096526746,0.00028147022,0.94217193,0.00316539,0.0026085894,0.0009112655,0.000025345296],"about_ca_topic_score_codex":0.013431724,"about_ca_topic_score_gemma":0.013957739,"teacher_disagreement_score":0.013431724,"about_ca_system_score_codex":0.0008932039,"about_ca_system_score_gemma":0.0005193338,"threshold_uncertainty_score":0.026707113},"labels":[],"label_agreement":null},{"id":"W2143992733","doi":"10.1029/2005gl023655","title":"Thermohaline circulation hysteresis: A model intercomparison","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":588,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; McGill University","funders":"","keywords":"Thermohaline circulation; Climate model; Climatology; Ocean current; Hysteresis; Forcing (mathematics); Advection; Environmental science; Coupled model intercomparison project; General Circulation Model; Circulation (fluid dynamics); Climate system; Climate change; Atmospheric sciences; Geology; Oceanography; Physics; Mechanics","score_opus":0.05150966677057363,"score_gpt":0.2999080331407785,"score_spread":0.2483983663702049,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2143992733","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962968,0.0001200463,0.0015702005,0.00016639526,0.000023714409,0.000018400237,0.00056237134,0.0002107055,0.0010312427],"genre_scores_gemma":[0.99733824,0.000051925894,0.001521776,0.000045345456,0.000012852585,0.000032958356,0.0008261173,0.000042177304,0.00012865676],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99890876,0.0005294986,0.00006701649,0.00028515587,0.00009856848,0.00011090683],"domain_scores_gemma":[0.99744594,0.0014819304,0.0001963352,0.0005365415,0.00024511444,0.00009421983],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031001184,0.00084454863,0.001015749,0.0006172733,0.00065240444,0.0014458329,0.001593985,0.0015685107,0.0010947135],"category_scores_gemma":[0.0045269895,0.00047978817,0.0014732989,0.00090941164,0.0004631158,0.0018153759,0.0010625487,0.00096165075,0.00014332395],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021188739,0.00056308706,0.096043244,0.00023937941,0.0018678758,0.00045326224,0.00092074665,0.8512983,0.018611092,0.002141089,0.0028810184,0.022862079],"study_design_scores_gemma":[0.0008593551,0.0010143147,0.08622581,0.00004610767,0.00076920615,0.00014413986,0.00043726366,0.8878508,0.016039746,0.0034996176,0.002939479,0.00017412474],"about_ca_topic_score_codex":0.010274462,"about_ca_topic_score_gemma":0.004675079,"teacher_disagreement_score":0.010274462,"about_ca_system_score_codex":0.0011330647,"about_ca_system_score_gemma":0.00060008495,"threshold_uncertainty_score":0.020429313},"labels":[],"label_agreement":null},{"id":"W2144015283","doi":"10.1029/2005gl022383","title":"Stratospheric abundances of water and methane based on ACE‐FTS measurements","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Stratosphere; Occultation; Water vapor; Trace gas; Atmospheric sciences; Mixing ratio; Methane; Environmental science; Atmospheric chemistry; Middle latitudes; Ozone; Chemistry; Meteorology; Physics","score_opus":0.05190234065994101,"score_gpt":0.29598302795757914,"score_spread":0.24408068729763813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2144015283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878755,0.00014216616,0.0006231768,0.00002916213,0.000010499819,0.000008097229,0.006739848,0.000092270944,0.0044792416],"genre_scores_gemma":[0.9939188,0.0001154255,0.0010124844,0.000014530752,0.000009205486,0.0000072007597,0.0044566696,0.000012890364,0.00045282135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.000003816937,0.0000028447257,0.0000114268705,0.000023662355,0.000014863181],"domain_scores_gemma":[0.99990606,0.000013629417,0.000024152258,0.000009512725,0.000030890442,0.00001569724],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008012314,0.00025095412,0.00013652274,0.0006000778,0.00019585557,0.0002776376,0.00017380728,0.00011742761,0.0014697984],"category_scores_gemma":[0.00029049552,0.00008605504,0.00012984386,0.00043373465,0.00008817847,0.00031567065,0.00017820587,0.00011042822,0.00022669144],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010497295,0.00013819063,0.75512314,0.00013110682,0.00021753338,0.00024501336,0.00025251767,0.007575014,0.20097102,0.000767523,0.0025378272,0.030991407],"study_design_scores_gemma":[0.000021007238,0.00007831561,0.93521696,0.000008641784,0.000049214454,0.00009854542,0.00011653476,0.012169849,0.04754341,0.00021233683,0.00447041,0.000014743046],"about_ca_topic_score_codex":0.012373716,"about_ca_topic_score_gemma":0.018562438,"teacher_disagreement_score":0.012373716,"about_ca_system_score_codex":0.0003340626,"about_ca_system_score_gemma":0.00013065674,"threshold_uncertainty_score":0.024603367},"labels":[],"label_agreement":null},{"id":"W2145440754","doi":"10.1029/2002gl015359","title":"Magnetotelluric and teleseismic study across the Snowbird Tectonic Zone, Canadian Shield: A Neoarchean mantle suture?","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; Geological Survey of Canada","funders":"","keywords":"Geology; Archean; Lithosphere; Crust; Magnetotellurics; Mantle (geology); Fibrous joint; Tectonics; Plate tectonics; Shield; Shear zone; Seismology; Indian Shield; Geophysics; Craton; Geochemistry; Paleontology","score_opus":0.040137429442154204,"score_gpt":0.29789576842977017,"score_spread":0.25775833898761596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145440754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99787843,0.00015600148,0.000060486465,0.00004640795,0.000002048148,0.0000053354356,0.0002665387,0.0000025100007,0.0015823819],"genre_scores_gemma":[0.9985563,0.00019904146,0.00013896116,0.000019400512,0.000003887539,0.0000032567311,0.0003325392,0.0000024761162,0.0007440775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998468,0.000008125086,0.000004344714,0.000023966952,0.0000441652,0.000072544535],"domain_scores_gemma":[0.9996419,0.00001700181,0.00006360292,0.000015269945,0.0001909598,0.00007127362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021372896,0.00017676233,0.00013021496,0.001453734,0.0012636851,0.0005425872,0.0003699818,0.00019173563,0.00084518094],"category_scores_gemma":[0.0005904757,0.00014811446,0.00012860316,0.0023737869,0.0005939224,0.00017383165,0.00045185428,0.00021865946,0.00013426156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096690484,0.000023930681,0.9678987,0.000032863325,0.00005334437,0.00034480428,0.002944236,0.0002156614,0.01134306,0.0005791932,0.00036855965,0.016098976],"study_design_scores_gemma":[0.0000012375742,0.000006509209,0.9983321,0.0000041750486,0.000007134936,0.000049773866,0.0006095145,0.00006533697,0.00017054469,0.00001326652,0.00073857896,0.0000019060557],"about_ca_topic_score_codex":0.9501764,"about_ca_topic_score_gemma":0.9807966,"teacher_disagreement_score":0.049823582,"about_ca_system_score_codex":0.004430134,"about_ca_system_score_gemma":0.004809892,"threshold_uncertainty_score":0.10023397},"labels":[],"label_agreement":null},{"id":"W2145568254","doi":"10.1029/2009gl039387","title":"Detection of a ULVZ at the base of the mantle beneath the northwest Pacific","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Subduction; Mantle (geology); Seismology; Slab; Slowness; Pacific Plate; Seismic tomography; Pacific ocean; Geophysics; Tectonics; Oceanography","score_opus":0.019877142993391966,"score_gpt":0.24824349785047187,"score_spread":0.2283663548570799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145568254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850684,0.0001076573,0.0007919713,0.000017231756,0.0000015875083,0.0000032282605,0.00011186669,0.000023540353,0.00043615993],"genre_scores_gemma":[0.9993048,0.00002944758,0.00045919593,0.000006066093,0.0000010540966,0.0000033414221,0.00008427678,0.0000027933197,0.00010903854],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.0000046580913,0.0000027619185,0.000020794727,0.000016063803,0.0000182796],"domain_scores_gemma":[0.9998273,0.000026126461,0.000065237684,0.000018189668,0.00003223936,0.000031028547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001236201,0.00010838059,0.00012634427,0.00052080536,0.00022162782,0.0004871387,0.00023253889,0.0002333985,0.00046342605],"category_scores_gemma":[0.000564417,0.00018247115,0.00006863028,0.00034722465,0.00038160302,0.00025083832,0.00075512595,0.00020063423,0.00008271205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020421697,0.000015582993,0.6710327,0.000059789232,0.000029341982,0.0003263916,0.0007071721,0.0010551062,0.30112547,0.00046797356,0.00015678402,0.02481948],"study_design_scores_gemma":[0.000006887825,0.000024687522,0.9858855,0.000009910611,0.000009873959,0.00017843276,0.00022333553,0.0019548195,0.011201544,0.000121411416,0.00037751746,0.000006136824],"about_ca_topic_score_codex":0.009886417,"about_ca_topic_score_gemma":0.011443169,"teacher_disagreement_score":0.009886417,"about_ca_system_score_codex":0.0002026692,"about_ca_system_score_gemma":0.00018733958,"threshold_uncertainty_score":0.019657731},"labels":[],"label_agreement":null},{"id":"W2145652841","doi":"10.1029/2011gl048598","title":"Spaced transmitter measurements of medium scale traveling ionospheric disturbances near the equator","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; Western University","funders":"","keywords":"Ionosphere; Equator; Transmitter; Scale (ratio); Geophysics; Geology; Remote sensing; Atmospheric sciences; Meteorology; Environmental science; Geodesy; Physics; Latitude; Telecommunications; Computer science","score_opus":0.04790128357287237,"score_gpt":0.28003664134772727,"score_spread":0.2321353577748549,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145652841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968051,0.00011628085,0.0011378941,0.00001828117,0.000010341014,0.0000067818155,0.00040706442,0.000017990746,0.0014802815],"genre_scores_gemma":[0.99843234,0.000065080094,0.0010181308,0.0000056811173,0.000006968893,0.0000030278202,0.00023710103,0.000002802841,0.00022881033],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.0000065063336,0.0000043137693,0.000017329634,0.000021958665,0.000008763407],"domain_scores_gemma":[0.9998406,0.00002126695,0.00005250395,0.000016590382,0.000038703096,0.000030251203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001358638,0.00009787478,0.00010130212,0.00037219393,0.00015972053,0.00019437341,0.00017703102,0.00016869408,0.00050601165],"category_scores_gemma":[0.0005434199,0.00009380822,0.000082667655,0.00037234667,0.00009572906,0.00014585312,0.00024135565,0.00020049195,0.00010860178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006202326,0.000081878075,0.7804983,0.00010467134,0.00011833497,0.00067256496,0.0013365528,0.0030813196,0.17333764,0.00053229154,0.00068496267,0.038931224],"study_design_scores_gemma":[0.000027860557,0.00018890748,0.9899032,0.000012458812,0.0000435271,0.00028502234,0.00024346098,0.0020272157,0.0060247835,0.00006802439,0.0011676167,0.000007867991],"about_ca_topic_score_codex":0.0030599849,"about_ca_topic_score_gemma":0.010049878,"teacher_disagreement_score":0.0030599849,"about_ca_system_score_codex":0.00016608788,"about_ca_system_score_gemma":0.000110730856,"threshold_uncertainty_score":0.006084323},"labels":[],"label_agreement":null},{"id":"W2145798994","doi":"10.1029/2005gl024709","title":"Long‐term stratospheric carbon tetrafluoride (CF<sub>4</sub>) increase inferred from 1985–2004 infrared space‐based solar occultation measurements","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Belgian Federal Science Policy Office","keywords":"Stratosphere; Occultation; Mixing ratio; Atmospheric sciences; Atmospheric chemistry; Environmental science; Trace gas; Analytical Chemistry (journal); Ozone; Physics; Meteorology; Chemistry; Astrophysics; Environmental chemistry","score_opus":0.03082381254381368,"score_gpt":0.2628035776975502,"score_spread":0.23197976515373653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145798994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99721056,0.00027503862,0.00027957506,0.000028122755,0.00000425191,0.000003591705,0.00083383836,0.000020375699,0.0013446519],"genre_scores_gemma":[0.99805605,0.00013339093,0.00032444444,0.000023870196,0.0000061214814,0.000004503782,0.0011311918,0.000002782331,0.00031769645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998983,0.0000069928965,0.000007452494,0.000035665016,0.000027032944,0.000024497316],"domain_scores_gemma":[0.9998178,0.000025071859,0.00007387282,0.000013036069,0.000053167,0.000017076583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002034392,0.0003224949,0.00016974207,0.0007804995,0.00032091906,0.0002789071,0.00017896412,0.00035001975,0.00045495754],"category_scores_gemma":[0.0002496668,0.00018173095,0.00024099278,0.0005886066,0.00015364792,0.00025237628,0.00018446225,0.00020000774,0.000118385185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002615768,0.00003665404,0.93044394,0.000063784195,0.00013119983,0.0001631062,0.00014175712,0.0023816123,0.057229716,0.000081557424,0.0006073638,0.00845776],"study_design_scores_gemma":[0.0000011817197,0.0000106212465,0.9974101,0.0000018957592,0.00001312466,0.000013582825,0.000012687697,0.00029599442,0.0019257527,0.0000043293744,0.00030879217,0.0000018721082],"about_ca_topic_score_codex":0.046871547,"about_ca_topic_score_gemma":0.08190964,"teacher_disagreement_score":0.046871547,"about_ca_system_score_codex":0.0010558873,"about_ca_system_score_gemma":0.00020646362,"threshold_uncertainty_score":0.093197465},"labels":[],"label_agreement":null},{"id":"W2145804569","doi":"10.1002/2014gl060450","title":"Kelvin-Helmholtz unstable magnetotail flow channels: Deceleration and radiation of MHD waves","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnetohydrodynamics; Physics; Mechanics; Kelvin wave; Flow (mathematics); Instability; Geophysics; Magnetic field; Meteorology","score_opus":0.012599345499868287,"score_gpt":0.25952775256715477,"score_spread":0.24692840706728647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2145804569","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9836901,0.0005232408,0.011854674,0.00008871444,0.000013004206,0.000017082639,0.00004552943,0.00010075592,0.003667038],"genre_scores_gemma":[0.99912375,0.000051775056,0.000573648,0.0000045314896,0.0000055082073,0.0000037796206,0.000011577934,0.000004226202,0.00022114751],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995756,0.00000604163,0.0000015028397,0.000008283721,0.00000965192,0.000016917738],"domain_scores_gemma":[0.9998822,0.00003429096,0.000039147504,0.000011085891,0.000011880705,0.000021384414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009380921,0.00022509482,0.00019836152,0.00031527726,0.00026018097,0.000422017,0.00018510656,0.00021646787,0.00050192745],"category_scores_gemma":[0.00031705174,0.00010473815,0.00011387757,0.00017500111,0.0005495433,0.00039731857,0.00038005968,0.00020011229,0.00007490235],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012150839,0.00013119163,0.07649357,0.00033225687,0.000054587355,0.002098508,0.0013080137,0.037327215,0.78051317,0.036317363,0.0013639912,0.06284513],"study_design_scores_gemma":[0.00027710418,0.0004054959,0.21416776,0.000063688014,0.000041841256,0.0026634503,0.0011806332,0.5491121,0.18641527,0.039633002,0.0059183724,0.00012124062],"about_ca_topic_score_codex":0.00047169995,"about_ca_topic_score_gemma":0.00023625605,"teacher_disagreement_score":0.00050192745,"about_ca_system_score_codex":0.00029265293,"about_ca_system_score_gemma":0.000107287146,"threshold_uncertainty_score":0.0021234155},"labels":[],"label_agreement":null},{"id":"W2146310519","doi":"10.1029/2003gl018025","title":"A CHAMP‐only gravity field model from kinematic orbits using the energy integral","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Gravitational field; Geodesy; Satellite; Orbit (dynamics); Physics; Kinematics; A priori and a posteriori; Field (mathematics); Gravitation; Gravitational potential; Potential energy; Classical mechanics; Geophysics; Geology; Mathematics; Astronomy; Aerospace engineering","score_opus":0.07736494257911786,"score_gpt":0.29991700756404405,"score_spread":0.2225520649849262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146310519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.67477345,0.00038493358,0.30856895,0.00041574516,0.000082813756,0.00010351246,0.0019112871,0.0032412002,0.010518141],"genre_scores_gemma":[0.9474435,0.00015225791,0.047170386,0.000026479256,0.000018440038,0.00006185425,0.0024069666,0.00028655885,0.0024335512],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998996,0.000016993192,0.000006593976,0.000022396684,0.000042071948,0.000012342842],"domain_scores_gemma":[0.99981886,0.00004769097,0.000025552736,0.000059835278,0.000038332502,0.000009726772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003917145,0.0004412321,0.00046820487,0.00050252303,0.00028223958,0.00047595342,0.0006038,0.00038424664,0.0013222717],"category_scores_gemma":[0.00096595,0.00024583456,0.0004974899,0.00078486075,0.0003090049,0.0007982357,0.00035485625,0.00052015495,0.0004255997],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110264526,0.000034341563,0.0055315676,0.000047591908,0.00008382477,0.00007704535,0.00007062733,0.9540254,0.0051377877,0.0051736212,0.0009956651,0.02871239],"study_design_scores_gemma":[0.000015427235,0.00002043905,0.002234304,0.0000050469826,0.000010855658,0.000031280593,0.000010653266,0.9942338,0.0012839899,0.0012791542,0.00086077565,0.000014275427],"about_ca_topic_score_codex":0.017864259,"about_ca_topic_score_gemma":0.010348428,"teacher_disagreement_score":0.017864259,"about_ca_system_score_codex":0.0004805001,"about_ca_system_score_gemma":0.00075105863,"threshold_uncertainty_score":0.035520554},"labels":[],"label_agreement":null},{"id":"W2146588345","doi":"10.1002/2015gl063093","title":"Hydraulic fracture energy budget: Insights from the laboratory","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":159,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Induced seismicity; Hydraulic fracturing; Fracture (geology); Geology; Deformation (meteorology); Range (aeronautics); Displacement (psychology); Acoustic emission; Energy budget; Energy (signal processing); Geotechnical engineering; Seismology; Materials science; Composite material; Physics","score_opus":0.027504609083892587,"score_gpt":0.26444310293093004,"score_spread":0.23693849384703747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146588345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947483,0.000090231784,0.0034493913,0.00006042066,0.0000035964001,0.000009266974,0.00021722198,0.000057473513,0.0013641976],"genre_scores_gemma":[0.99895525,0.00004111661,0.0006771182,0.000011078634,0.0000020489506,0.000009089324,0.000093310366,0.000006665123,0.00020428884],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998436,0.000024928047,0.000008299785,0.000039987422,0.000049997245,0.00003318243],"domain_scores_gemma":[0.9997919,0.000090704845,0.000035381003,0.000027794844,0.000038722996,0.000015470456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031820062,0.00018500775,0.00030224465,0.00033984793,0.0002714495,0.0004128428,0.00044727218,0.00043932936,0.002022803],"category_scores_gemma":[0.0004639348,0.00011054643,0.00017757998,0.00034447532,0.00064756244,0.0005518989,0.00034772616,0.00040797878,0.0001872826],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005235696,0.000421952,0.03024257,0.000106365755,0.00005195404,0.0002575801,0.000101450976,0.01709759,0.93386734,0.0013464486,0.00042821313,0.015554971],"study_design_scores_gemma":[0.00014863988,0.0018152186,0.11616348,0.00002917404,0.00007086342,0.0005290891,0.0006535093,0.09605165,0.7782714,0.0024086393,0.0037598524,0.000098542514],"about_ca_topic_score_codex":0.0020153315,"about_ca_topic_score_gemma":0.0025918137,"teacher_disagreement_score":0.002022803,"about_ca_system_score_codex":0.00047490295,"about_ca_system_score_gemma":0.00025476437,"threshold_uncertainty_score":0.006766975},"labels":[],"label_agreement":null},{"id":"W2146639246","doi":"10.1029/2001gl013408","title":"Electromagnetic images of a strike‐slip fault: The Tintina fault—Northern Canadian","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; Geological Survey of Canada","funders":"","keywords":"Geology; Magnetotellurics; Seismology; Strike-slip tectonics; Fault (geology); Slip (aerodynamics); Crust; Transform fault; Geophysics; Electrical resistivity and conductivity","score_opus":0.030966767050141793,"score_gpt":0.273129184710274,"score_spread":0.2421624176601322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2146639246","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99494743,0.00004468978,0.00030282585,0.00003932052,0.0000037743682,0.000009146598,0.0012435293,0.000027982744,0.003381219],"genre_scores_gemma":[0.9966253,0.000066787325,0.0006566347,0.0000141107985,0.000002572106,0.0000030333708,0.0011265829,0.0000065622557,0.0014984425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992824,0.0000015956555,0.0000016776092,0.000011385994,0.00002727953,0.000029808398],"domain_scores_gemma":[0.99984324,0.000007220122,0.000013007515,0.000005276342,0.00009150311,0.000039668732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005404813,0.00017786432,0.00012262264,0.0009092154,0.00059869303,0.00036033144,0.00027189968,0.00018459788,0.0012029113],"category_scores_gemma":[0.00024784156,0.00010863047,0.0000671731,0.0013769475,0.0002144125,0.00008279049,0.00020078656,0.00015977598,0.00015421186],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00096787396,0.00020758116,0.4917033,0.00022088706,0.00012756608,0.0024380477,0.0028883864,0.010659606,0.35949767,0.00085035176,0.0068581863,0.1235805],"study_design_scores_gemma":[0.000008497497,0.000013057614,0.99229217,0.00000590391,0.000015222836,0.00017137159,0.00039882382,0.0023357936,0.0031253765,0.000024607676,0.0015985294,0.000010498734],"about_ca_topic_score_codex":0.8742672,"about_ca_topic_score_gemma":0.9584595,"teacher_disagreement_score":0.12573278,"about_ca_system_score_codex":0.0022070883,"about_ca_system_score_gemma":0.0018889839,"threshold_uncertainty_score":0.25294644},"labels":[],"label_agreement":null},{"id":"W2147084362","doi":"10.1029/2006gl027764","title":"Reduction in seasonal sea ice concentration surrounding southern Baffin Island 1979–2004","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Sea ice; Arctic ice pack; Arctic; Oceanography; Climatology; Environmental science; Climate change; Arctic sea ice decline; Range (aeronautics); Geology; Physical geography; Antarctic sea ice; Geography","score_opus":0.017975865648715648,"score_gpt":0.25706254620633945,"score_spread":0.2390866805576238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147084362","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953003,0.00034242103,0.0000811056,0.0003334984,0.00001875307,0.0000073912483,0.0007389769,0.0000071181335,0.0031703836],"genre_scores_gemma":[0.99638724,0.00019601705,0.00016311856,0.00009146152,0.000022728564,0.000012184721,0.0014275076,0.0000027197277,0.0016970247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998043,0.000019490857,0.000010354082,0.00004706069,0.00006933027,0.000049474304],"domain_scores_gemma":[0.99934906,0.000052191106,0.00016887438,0.000023914026,0.00029002264,0.000115994175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026321673,0.00013233782,0.00021698717,0.0010225134,0.00097479677,0.0006044976,0.00045571037,0.00044275983,0.0015495162],"category_scores_gemma":[0.0009919528,0.00012628394,0.0001082168,0.0011637976,0.0006171139,0.00021805405,0.00040056964,0.00034568383,0.0002456602],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033859193,0.00007147004,0.9618944,0.00009983277,0.00012362008,0.0007126984,0.0017126439,0.00075735286,0.01051334,0.00014296825,0.0035441683,0.020088898],"study_design_scores_gemma":[0.0000020921862,0.000009773022,0.99783945,0.000005471336,0.000005280472,0.000039358314,0.00024826615,0.000095616226,0.00016424233,0.0000066606694,0.0015815923,0.0000021837275],"about_ca_topic_score_codex":0.59199554,"about_ca_topic_score_gemma":0.8046931,"teacher_disagreement_score":0.40800446,"about_ca_system_score_codex":0.002813426,"about_ca_system_score_gemma":0.0014270792,"threshold_uncertainty_score":0.82081455},"labels":[],"label_agreement":null},{"id":"W2147347127","doi":"10.1029/2009gl038261","title":"Nutrient and salinity decadal variations in the central and eastern North Pacific","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Ocean gyre; Pacific decadal oscillation; Oceanography; Salinity; Hindcast; Environmental science; Climatology; Climate change; Geology; Current (fluid); Sea surface temperature; Ecology","score_opus":0.023137783337258983,"score_gpt":0.2603337828524998,"score_spread":0.2371959995152408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147347127","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99961025,0.000025177318,0.000047230034,0.000015321813,0.0000017504611,5.196993e-7,0.00010321814,0.0000048565203,0.00019157429],"genre_scores_gemma":[0.9995704,0.0000323809,0.000063409316,0.000003920827,0.000002384829,0.0000012493197,0.00022962822,0.0000013827826,0.00009522541],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999646,0.0000052424075,0.0000028932193,0.000014027096,0.0000070403903,0.000006205957],"domain_scores_gemma":[0.99975675,0.0000378183,0.00009344938,0.0000224579,0.000046294605,0.000043268345],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017449592,0.0000943715,0.00008703772,0.00042955313,0.00017994425,0.00028819786,0.00008464291,0.00012530584,0.00039132597],"category_scores_gemma":[0.0006580872,0.00009693711,0.000117180076,0.00044685023,0.00018709627,0.00024373127,0.00028091742,0.00018686948,0.000062580926],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000088469176,0.00002696133,0.9832259,0.000010612247,0.00007596207,0.000087718945,0.00039613474,0.003002269,0.004951146,0.0001647036,0.00035212142,0.007617968],"study_design_scores_gemma":[0.0000023734358,0.0000070495144,0.9980849,0.0000016496598,0.0000066913944,0.000021676255,0.00006472364,0.0014592969,0.00016402488,0.000040150167,0.00014467112,0.000002829151],"about_ca_topic_score_codex":0.023041306,"about_ca_topic_score_gemma":0.038763236,"teacher_disagreement_score":0.023041306,"about_ca_system_score_codex":0.00032767674,"about_ca_system_score_gemma":0.00020681905,"threshold_uncertainty_score":0.045814395},"labels":[],"label_agreement":null},{"id":"W2147575495","doi":"10.1029/2007gl032057","title":"A millennial perspective on Arctic warming from <sup>14</sup>C in quartz and plants emerging from beneath ice caps","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs; University of Arizona; Geological Society of America","keywords":"Geology; Holocene; Physical geography; Arctic; Macrofossil; Arctic ice pack; Oceanography; Paleoclimatology; Plateau (mathematics); Antarctic sea ice; Cryosphere; Ice core; Volcano; Sea ice; Climatology; Climate change; Paleontology; Geography","score_opus":0.03662284079077501,"score_gpt":0.29164120743294525,"score_spread":0.25501836664217026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147575495","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.32401854,0.4815442,0.0032632009,0.071118735,0.0046180203,0.0000131924835,0.0036137032,0.00017871332,0.11163162],"genre_scores_gemma":[0.83694696,0.1461146,0.0016197097,0.0050926097,0.002633859,0.000011547789,0.0007855852,0.000043468,0.0067517064],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998841,0.00002939973,0.000008052314,0.000027972845,0.00001682877,0.00003358265],"domain_scores_gemma":[0.999564,0.00009648604,0.0000894683,0.000025196643,0.00013688266,0.000087884386],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067663135,0.00040153175,0.00018736834,0.0013300083,0.00084692397,0.0015616792,0.0002907884,0.00092799845,0.0042090276],"category_scores_gemma":[0.0006815939,0.00014249407,0.00019371048,0.0013727301,0.0010902487,0.0019233723,0.00084870646,0.0010876236,0.00036575002],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012581619,0.0001337654,0.23177819,0.0022841673,0.0005405175,0.0031096388,0.009739573,0.0050989734,0.021550858,0.12659007,0.07544871,0.5224674],"study_design_scores_gemma":[0.000012255873,0.00013242985,0.3634142,0.000660522,0.00013308288,0.0010627271,0.0050473856,0.0003597102,0.0021261333,0.017417919,0.6095828,0.00005083529],"about_ca_topic_score_codex":0.01450966,"about_ca_topic_score_gemma":0.045573734,"teacher_disagreement_score":0.01450966,"about_ca_system_score_codex":0.0014427691,"about_ca_system_score_gemma":0.00071427645,"threshold_uncertainty_score":0.028850377},"labels":[],"label_agreement":null},{"id":"W2147825978","doi":"10.1029/2005gl022403","title":"Comparison of atmospheric retrievals from ACE and HALOE","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Environmental science; Traceability; Atmospheric sciences; Remote sensing; Meteorology; Geology; Physics; Statistics; Mathematics","score_opus":0.04514603686299225,"score_gpt":0.33192495218216195,"score_spread":0.2867789153191697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2147825978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96621245,0.00067991996,0.010127591,0.00020982222,0.00010395088,0.00003850268,0.010147821,0.00139316,0.011086874],"genre_scores_gemma":[0.9747113,0.00029127515,0.00886221,0.00011279706,0.00010301758,0.000020063033,0.014348658,0.00022578772,0.0013248246],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99922943,0.00007184923,0.00003992225,0.00018769385,0.00033081014,0.00014033885],"domain_scores_gemma":[0.99893695,0.00022357515,0.00009951742,0.00022372977,0.00045595493,0.000060249942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00080988125,0.00036691368,0.0004898746,0.00080820103,0.00032685028,0.0009329524,0.0003483581,0.00035621444,0.0015421808],"category_scores_gemma":[0.0029200562,0.00025953088,0.0003926196,0.0011038639,0.00018348692,0.00094266987,0.00059387146,0.00031074646,0.0004970981],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0040508946,0.00044874885,0.3223069,0.0007110568,0.0017408255,0.00065051543,0.00078579097,0.08220924,0.24407408,0.0032180748,0.020057421,0.31974652],"study_design_scores_gemma":[0.0004434413,0.0003607262,0.80483156,0.000053373147,0.00035024705,0.00049878395,0.00037613578,0.10044437,0.06787535,0.0011645862,0.023431398,0.00017007842],"about_ca_topic_score_codex":0.014250578,"about_ca_topic_score_gemma":0.014478514,"teacher_disagreement_score":0.014250578,"about_ca_system_score_codex":0.0003135103,"about_ca_system_score_gemma":0.0003717246,"threshold_uncertainty_score":0.028335273},"labels":[],"label_agreement":null},{"id":"W2148039128","doi":"10.1029/2006gl026782","title":"Evolution of chemical, biological, and physical water properties in the northern California Current in 2005: Remote or local wind forcing?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Upwelling; Oceanography; Forcing (mathematics); Advection; Current (fluid); Environmental science; Wind stress; Salinity; Geology; Water column; Atmospheric sciences; Climatology","score_opus":0.02841014877678332,"score_gpt":0.2520396047035682,"score_spread":0.22362945592678485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148039128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994511,0.00005457686,0.00003222096,0.00003412028,0.0000025275365,0.0000017898526,0.00007417294,0.0000043783093,0.0003451774],"genre_scores_gemma":[0.9994404,0.000054981767,0.00007397195,0.000015646983,0.000001927688,0.000002123073,0.00020375244,0.0000013630574,0.00020589621],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993885,0.000006328624,0.000003968613,0.000025327005,0.000010561109,0.000014955579],"domain_scores_gemma":[0.99970895,0.000036010355,0.000091631235,0.000021345055,0.00007255294,0.000069502195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020550146,0.00014534596,0.00017359942,0.00032620152,0.00039717808,0.0005486659,0.00021282746,0.00036449605,0.0005314886],"category_scores_gemma":[0.00066197466,0.00021491438,0.00015872714,0.00027807124,0.00024818964,0.00024789022,0.00019158651,0.0002760084,0.00007412888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001869525,0.00011150717,0.9858445,0.00001286553,0.000059425816,0.00014567944,0.0003184196,0.0017161568,0.004353221,0.00011280308,0.00043475738,0.0067038434],"study_design_scores_gemma":[0.0000024939884,0.000015465579,0.99893934,0.0000023612606,0.000008248702,0.00001359828,0.000098998535,0.000631237,0.0001246801,0.000010340528,0.00015022847,0.0000030277808],"about_ca_topic_score_codex":0.15880279,"about_ca_topic_score_gemma":0.27116752,"teacher_disagreement_score":0.15880279,"about_ca_system_score_codex":0.0014059981,"about_ca_system_score_gemma":0.00043547194,"threshold_uncertainty_score":0.31575692},"labels":[],"label_agreement":null},{"id":"W2148104872","doi":"10.1029/2002gl016606","title":"Optical and meteorological properties of smoke‐dominated haze at the ARM Southern Great Plains Central Facility","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Oceanic and Atmospheric Administration; Killam Trusts; Dalhousie University; U.S. Department of Energy","keywords":"Haze; Environmental science; Single-scattering albedo; Atmospheric sciences; Smoke; Angstrom exponent; Radiative forcing; Aerosol; Cloud cover; Albedo (alchemy); Precipitation; Climatology; Shortwave; Forcing (mathematics); Liquid water path; Optical depth; Shortwave radiation; Radiative transfer; Meteorology; Geology; Radiation; Physics; Cloud computing","score_opus":0.037318030740446075,"score_gpt":0.2583645664209935,"score_spread":0.2210465356805474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148104872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99932873,0.000013932344,0.000032236378,0.000008353259,4.2969148e-7,0.0000018781294,0.00038885346,0.0000072616526,0.00021824594],"genre_scores_gemma":[0.9991623,0.000012848148,0.00008320572,0.0000048466795,0.0000017109867,0.0000025370634,0.00051999587,0.0000018702995,0.000210746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.000005523626,0.0000035829844,0.000017485076,0.000027284346,0.0000168169],"domain_scores_gemma":[0.99956995,0.000064852095,0.00019492226,0.00002076131,0.000090463756,0.000059046033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019915671,0.00012979645,0.00008997511,0.00044940028,0.00025747193,0.00022820251,0.0001850928,0.00011889053,0.0006913975],"category_scores_gemma":[0.0005239739,0.00014034516,0.00007092993,0.00043714728,0.00014729027,0.00017936165,0.00017319154,0.00015143953,0.00008973032],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000119199016,0.000042223364,0.98679346,0.000014645037,0.000035022695,0.00014210568,0.00021606767,0.0012072774,0.0072108605,0.000022892518,0.000500526,0.0036956714],"study_design_scores_gemma":[0.000001575343,0.000012938445,0.9991905,6.6031356e-7,0.0000033590175,0.0000227311,0.000028109613,0.00037546383,0.00026892906,0.0000029516311,0.00009147381,0.0000013591681],"about_ca_topic_score_codex":0.06502759,"about_ca_topic_score_gemma":0.1149198,"teacher_disagreement_score":0.06502759,"about_ca_system_score_codex":0.00050453935,"about_ca_system_score_gemma":0.00020938378,"threshold_uncertainty_score":0.12929821},"labels":[],"label_agreement":null},{"id":"W2148141140","doi":"10.1029/2003gl017436","title":"Enhanced southward flow over the Oregon shelf in 2002: A conduit for subarctic water","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Anomaly (physics); Oceanography; Latitude; Current (fluid); Sea level; Subarctic climate; Climatology; Geodesy","score_opus":0.025148565860183318,"score_gpt":0.2666933282602634,"score_spread":0.24154476240008005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148141140","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989599,0.000027338858,0.00002153819,0.000056431534,0.0000038183216,0.0000031703878,0.00023856307,0.0000034048767,0.00068582856],"genre_scores_gemma":[0.998514,0.00010597766,0.000114161165,0.000031243515,0.0000058308897,0.000004741579,0.0005778602,0.0000028043696,0.0006433719],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.0000039982688,0.000005753654,0.000015957592,0.000018980641,0.000012204601],"domain_scores_gemma":[0.99970216,0.0000284543,0.00012253955,0.000019946312,0.000059857743,0.00006709314],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014056038,0.00014252587,0.00012078744,0.00037279454,0.0005106515,0.00075394387,0.00019078678,0.00013749262,0.0010274501],"category_scores_gemma":[0.0004229286,0.00010688685,0.00009536544,0.0006013586,0.00026197894,0.0004138675,0.00045277638,0.0002659715,0.0001060873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007735688,0.00003594161,0.9933041,0.000008745146,0.000016667984,0.00032801967,0.00046538812,0.00003519518,0.0014227587,0.000047658694,0.00022436383,0.004033859],"study_design_scores_gemma":[0.0000028110378,0.000011698503,0.99812204,0.0000053874296,0.000009570174,0.00008653756,0.00070305215,0.00013409798,0.00023571383,0.000011234793,0.0006759652,0.0000018144891],"about_ca_topic_score_codex":0.12356281,"about_ca_topic_score_gemma":0.37946385,"teacher_disagreement_score":0.12356281,"about_ca_system_score_codex":0.0008865573,"about_ca_system_score_gemma":0.00065160444,"threshold_uncertainty_score":0.24568719},"labels":[],"label_agreement":null},{"id":"W2148702592","doi":"10.1002/2014gl062401","title":"Crustal thickness variations and isostatic disequilibrium across the North Anatolian Fault, western Turkey","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Environment Research Council; Sight Research UK","keywords":"North Anatolian Fault; Geology; Lithosphere; Seismology; Crust; Mantle (geology); Fault (geology); Sedimentary rock; Subduction; Tectonics; Petrology; Geophysics; Paleontology","score_opus":0.054521033228973795,"score_gpt":0.3189080846461486,"score_spread":0.26438705141717483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2148702592","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995914,0.00003898302,0.000045863057,0.000005314439,8.0893403e-7,8.716544e-7,0.0001004941,0.000003386033,0.00021291875],"genre_scores_gemma":[0.99970007,0.000021326205,0.000059274786,0.0000014914203,6.6134623e-7,0.0000011017063,0.0001494205,0.0000010858398,0.000065521344],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999144,0.0000120783425,0.0000121723315,0.000032884796,0.000013454052,0.000014967527],"domain_scores_gemma":[0.99975353,0.00003234538,0.000099355144,0.000022707605,0.00007188479,0.000020179736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016176993,0.00028135887,0.00019476206,0.0010665319,0.00020236163,0.0004225665,0.00021385062,0.00018757355,0.00056164304],"category_scores_gemma":[0.00039075006,0.00013356819,0.00010062175,0.0008706229,0.00024534584,0.00024244172,0.00028290367,0.00009814572,0.000121531346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017246595,0.000036417132,0.9737055,0.000024170038,0.00009427706,0.0004166311,0.0004980626,0.0026126234,0.008769793,0.00008603152,0.00013449402,0.013449518],"study_design_scores_gemma":[0.0000028014106,0.000008950282,0.99853396,0.0000030720887,0.000008349616,0.00006115492,0.00017585821,0.0008866862,0.00020806248,0.000015453761,0.000093611256,0.0000020539896],"about_ca_topic_score_codex":0.021563264,"about_ca_topic_score_gemma":0.027542438,"teacher_disagreement_score":0.021563264,"about_ca_system_score_codex":0.00048305202,"about_ca_system_score_gemma":0.00020153038,"threshold_uncertainty_score":0.04287553},"labels":[],"label_agreement":null},{"id":"W2149352528","doi":"10.1029/2005gl023209","title":"A model intercomparison of changes in the Atlantic thermohaline circulation in response to increasing atmospheric CO<sub>2</sub> concentration","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":635,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Thermohaline circulation; Coupled model intercomparison project; Environmental science; Climatology; Climate model; Atmospheric sciences; Flux (metallurgy); Climate change; General Circulation Model; Atmospheric circulation; Representative Concentration Pathways; Circulation (fluid dynamics); Greenhouse gas; Atmospheric model; Oceanography; Geology; Chemistry; Thermodynamics","score_opus":0.049610349405216636,"score_gpt":0.32158854015134763,"score_spread":0.271978190746131,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149352528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962692,0.000028525188,0.0014033517,0.000085267435,0.00002499157,0.000023180113,0.0006288986,0.00014963487,0.0013869087],"genre_scores_gemma":[0.99580115,0.000021496553,0.0026485885,0.00002986685,0.000008332834,0.00004990754,0.0010956319,0.000023248993,0.00032177544],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997688,0.00008752296,0.00001288,0.0000670449,0.000024302231,0.000039466246],"domain_scores_gemma":[0.99947804,0.0002320631,0.00004863333,0.00009172406,0.000082153194,0.00006742031],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010200338,0.0007869243,0.00052791624,0.00023606422,0.000561744,0.00069427537,0.0010049777,0.001031709,0.0010470967],"category_scores_gemma":[0.0012485773,0.00041556885,0.0010824611,0.00041928043,0.00040287545,0.0006629984,0.0005154278,0.0006706301,0.00013836382],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015553231,0.00047867838,0.03877484,0.00009365063,0.00084042974,0.00018126087,0.00032347871,0.9302001,0.01289651,0.001398986,0.001864526,0.011392228],"study_design_scores_gemma":[0.00077577017,0.0007566757,0.039919604,0.000008231932,0.0003604399,0.00004108276,0.00015363802,0.9477939,0.0077945585,0.0007841553,0.0015343617,0.00007764462],"about_ca_topic_score_codex":0.028605811,"about_ca_topic_score_gemma":0.0195108,"teacher_disagreement_score":0.028605811,"about_ca_system_score_codex":0.0009473405,"about_ca_system_score_gemma":0.0009547239,"threshold_uncertainty_score":0.056878626},"labels":[],"label_agreement":null},{"id":"W2149532796","doi":"10.1029/2006gl027233","title":"A note on pore fluid pressure ratios in the Coulomb wedge theory","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Wedge (geometry); Coulomb; Geology; Pore water pressure; Fluid pressure; Geophysics; Mechanics; Physics; Geotechnical engineering; Nuclear physics; Optics","score_opus":0.026215877926289027,"score_gpt":0.28512644870175685,"score_spread":0.2589105707754678,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2149532796","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04561082,0.03985664,0.75974506,0.0153572,0.009735657,0.000075071745,0.00027437301,0.00077154394,0.12857372],"genre_scores_gemma":[0.78569144,0.027187183,0.14361185,0.0030210812,0.006411455,0.00012376666,0.00011605719,0.0006414916,0.03319568],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99868304,0.00034046912,0.00007366579,0.00018651714,0.000641153,0.00007521233],"domain_scores_gemma":[0.9978816,0.0015395734,0.000108845044,0.00023757487,0.00017949483,0.00005292738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022393782,0.000720287,0.0007865004,0.00065597665,0.00068839354,0.001534918,0.0021528783,0.0013078587,0.0035140305],"category_scores_gemma":[0.007451253,0.0003839089,0.0006380876,0.00058635,0.0041612047,0.0048073544,0.0020985233,0.0042442605,0.0011599173],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":"theoretical_or_conceptual","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042522126,0.000028067589,0.00020148815,0.00017059487,0.000011156958,0.0005236313,0.00019011387,0.011609493,0.0044593355,0.9404036,0.0071669994,0.035193097],"study_design_scores_gemma":[0.000019395635,0.00013659286,0.00046316336,0.00009931895,0.000013899969,0.00044023016,0.000092271526,0.06348212,0.0056039323,0.87811583,0.05146914,0.000064093285],"about_ca_topic_score_codex":0.0011472119,"about_ca_topic_score_gemma":0.0004125908,"teacher_disagreement_score":0.0035140305,"about_ca_system_score_codex":0.0005105593,"about_ca_system_score_gemma":0.00040156563,"threshold_uncertainty_score":0.011843085},"labels":[],"label_agreement":null},{"id":"W2150043131","doi":"10.1029/2007gl032117","title":"Disequilibrium response of permafrost thaw to climate warming in Canada over 1850–2100","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Permafrost; Climate change; Environmental science; Global warming; Disequilibrium; Biogeochemistry; Latitude; Atmospheric sciences; Climatology; Physical geography; Geology; Hydrology (agriculture); Geography; Oceanography","score_opus":0.05680431093761289,"score_gpt":0.29409533885318867,"score_spread":0.23729102791557577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150043131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975956,0.00007346357,0.00017904324,0.00015562268,0.0000056766808,0.0000060868215,0.00059522555,0.000029568388,0.0013596173],"genre_scores_gemma":[0.9991467,0.000040625146,0.00012379346,0.000024116498,8.9215774e-7,0.000002265921,0.00035958434,0.000004326853,0.00029782415],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999871,0.000015742055,0.000005328117,0.000026353426,0.000021458043,0.00006005679],"domain_scores_gemma":[0.9997396,0.000041029376,0.000021526155,0.000015861408,0.00010531424,0.00007663907],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032407106,0.00028727774,0.00023399165,0.00042464002,0.001215551,0.0009392067,0.0006717335,0.000518447,0.001635659],"category_scores_gemma":[0.0010526036,0.00025129507,0.00056410587,0.0005678172,0.00074338436,0.00033591135,0.0004954181,0.00039737558,0.000080722944],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003625397,0.00009976519,0.40757415,0.00003970346,0.00023590864,0.00022297094,0.0002536369,0.57870436,0.0021469414,0.001753421,0.0017402122,0.0068664234],"study_design_scores_gemma":[0.00018011274,0.00008024432,0.38129196,0.000020820193,0.000116426345,0.00007290118,0.00072172174,0.6121282,0.0013668835,0.0008299935,0.0031259719,0.00006474468],"about_ca_topic_score_codex":0.97930634,"about_ca_topic_score_gemma":0.97409195,"teacher_disagreement_score":0.02069366,"about_ca_system_score_codex":0.016452659,"about_ca_system_score_gemma":0.012078534,"threshold_uncertainty_score":0.119372904},"labels":[],"label_agreement":null},{"id":"W2150065186","doi":"10.1029/2004gl021089","title":"Relationship between atmospheric circulation and winter precipitation δ<sup>18</sup>O in central New York State","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"International Atomic Energy Agency","keywords":"Precipitation; Atmospheric circulation; Climatology; Low-pressure area; Environmental science; Circulation (fluid dynamics); Atmospheric pressure; Atmospheric sciences; Geology; Meteorology; Oceanography; Geography","score_opus":0.051577712264508906,"score_gpt":0.27722927422597965,"score_spread":0.22565156196147074,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150065186","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946564,0.000037241698,0.000023952696,0.000027566626,0.0000019340914,0.000001526886,0.00023610475,0.000002661002,0.00020341529],"genre_scores_gemma":[0.99929583,0.0000692814,0.000039004583,0.0000066186267,0.0000034763443,0.000003949197,0.00039709563,0.0000014030306,0.00018334623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999608,0.000005663212,0.000004123305,0.000009965062,0.000008332398,0.000011067684],"domain_scores_gemma":[0.99957854,0.00010615491,0.00013370147,0.00001553689,0.00009711149,0.000068965935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008656302,0.00007066959,0.00009414033,0.0004172983,0.00023509502,0.00034451,0.00013460805,0.00009604937,0.0011209111],"category_scores_gemma":[0.00056247454,0.000103123464,0.00006771276,0.0005259905,0.00017563568,0.00016838618,0.00022135455,0.00018255485,0.000068215435],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004660376,0.0000149376765,0.9963826,0.0000059067575,0.000028317954,0.00005279936,0.00019017133,0.00021750273,0.0007814071,0.00003387286,0.00028291324,0.0019630182],"study_design_scores_gemma":[0.0000024766885,0.0000065659992,0.99917954,0.000002511491,0.0000061778164,0.000014265331,0.0001338144,0.0003752766,0.000072833056,0.0000080793525,0.00019730486,0.0000012678322],"about_ca_topic_score_codex":0.375067,"about_ca_topic_score_gemma":0.57116,"teacher_disagreement_score":0.624933,"about_ca_system_score_codex":0.0007873545,"about_ca_system_score_gemma":0.0005624833,"threshold_uncertainty_score":0.7457677},"labels":[],"label_agreement":null},{"id":"W2150313828","doi":"10.1029/2001gl014153","title":"Time‐series of zenith radiance and surface flux under cloudy skies: Radiative smoothing, optical thickness retrievals and large‐scale stationarity","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Radiance; Radiative transfer; Zenith; Radiative flux; Smoothing; Environmental science; Atmospheric radiative transfer codes; Scale (ratio); Flux (metallurgy); Solar zenith angle; Remote sensing; Physics; Atmospheric sciences; Optics; Geology; Materials science; Mathematics","score_opus":0.020086143471273712,"score_gpt":0.2716430817623174,"score_spread":0.2515569382910437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150313828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990368,0.000029327424,0.0005157061,0.000023658044,0.0000015340275,0.000002025712,0.00024120597,0.000022673741,0.0001270905],"genre_scores_gemma":[0.99912447,0.00002472763,0.0002533194,0.0000022719855,0.0000028586035,0.0000015252544,0.0005356122,0.00000440014,0.000050886814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999323,0.000011325384,0.0000051736047,0.00002198326,0.000011876145,0.000017400193],"domain_scores_gemma":[0.99926215,0.00033155782,0.00018373142,0.000087261134,0.00008627659,0.000049058137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038610646,0.00022534264,0.00022020435,0.0005016252,0.00020634297,0.0003443005,0.00022758238,0.00037657397,0.00047107847],"category_scores_gemma":[0.0018166432,0.00013549623,0.0002598733,0.0006865103,0.00031665812,0.0005103644,0.00023406706,0.00020243766,0.00009342365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010980319,0.00017115525,0.74269396,0.000099983656,0.00025697734,0.00048538652,0.00028320827,0.1923923,0.032487217,0.0015606715,0.0007594001,0.027711753],"study_design_scores_gemma":[0.00001946053,0.000041143096,0.83186525,0.0000065334166,0.00003461868,0.00008584833,0.00007313323,0.16364743,0.0035838499,0.00035949322,0.00026259694,0.00002072531],"about_ca_topic_score_codex":0.021369506,"about_ca_topic_score_gemma":0.022389734,"teacher_disagreement_score":0.021369506,"about_ca_system_score_codex":0.00044836706,"about_ca_system_score_gemma":0.00026796805,"threshold_uncertainty_score":0.042490244},"labels":[],"label_agreement":null},{"id":"W2150531251","doi":"10.1029/1999gl011227","title":"Modeling recent climate variability in the Arctic Ocean","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":121,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Thermohaline circulation; Arctic sea ice decline; Sea ice; Northern Hemisphere; Arctic dipole anomaly; Arctic ice pack; Forcing (mathematics); Arctic geoengineering; Arctic; Geology; Atmospheric circulation; Canada Basin; Arctic oscillation; Ocean current; Climate model; Environmental science; North Atlantic oscillation; Oceanography; Climate change; Drift ice","score_opus":0.03172389223104119,"score_gpt":0.2804853280505516,"score_spread":0.2487614358195104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150531251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9778676,0.00060449925,0.013755976,0.0005915328,0.000083423474,0.000011267314,0.0011218541,0.00017215448,0.005791607],"genre_scores_gemma":[0.9954743,0.00047027512,0.0024005608,0.000036841604,0.000038528568,0.000019574958,0.0005223447,0.000024742612,0.0010126835],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989355,0.000036429086,0.0000071420964,0.000029860224,0.000014008519,0.000018948012],"domain_scores_gemma":[0.9997106,0.00010610326,0.00007396499,0.000026756074,0.000054279393,0.000028247625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006143405,0.00027637705,0.00024867614,0.00046249846,0.00038972442,0.0010075796,0.0006745109,0.000596888,0.0008361421],"category_scores_gemma":[0.0017554775,0.00029553447,0.0005310883,0.00071472314,0.00024455227,0.00075942196,0.0004172261,0.00039305724,0.00016139123],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027639866,0.000033925455,0.022610096,0.00002096511,0.00009837668,0.00007395909,0.000064366,0.9698812,0.00061690697,0.002234136,0.00045031685,0.0038882003],"study_design_scores_gemma":[0.00001350278,0.000019369898,0.008340378,0.000009242901,0.000039598715,0.0000244968,0.00003995697,0.9880454,0.0001878619,0.0013422301,0.0019266288,0.000011426419],"about_ca_topic_score_codex":0.060833827,"about_ca_topic_score_gemma":0.054643415,"teacher_disagreement_score":0.060833827,"about_ca_system_score_codex":0.0011182731,"about_ca_system_score_gemma":0.0007978354,"threshold_uncertainty_score":0.12095946},"labels":[],"label_agreement":null},{"id":"W2150866077","doi":"10.1029/2005gl025624","title":"Pacific Ocean inflow: Influence on catastrophic reduction of sea ice cover in the Arctic Ocean","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":531,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"JST-Mirai Program; Fisheries and Oceans Canada; Japan Agency for Marine-Earth Science and Technology; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Arctic sea ice decline; Halocline; Arctic ice pack; Sea ice; Oceanography; Geology; Climatology; Canada Basin; Antarctic sea ice; Drift ice; Anticyclone; Fast ice; Structural basin; Arctic; Environmental science; Salinity","score_opus":0.013212088464764942,"score_gpt":0.245582210313922,"score_spread":0.23237012184915706,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150866077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99918324,0.000055876062,0.000021811959,0.00007619979,0.0000055352552,0.0000014848492,0.00014755508,0.0000036738454,0.0005046384],"genre_scores_gemma":[0.9996253,0.00007568614,0.000012836204,0.000012269472,0.000007118315,0.000001099748,0.0001281439,0.000002327219,0.00013509122],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999018,0.00002388022,0.000007952558,0.000013765,0.000015185549,0.000037429214],"domain_scores_gemma":[0.9990465,0.00021152392,0.00030492462,0.000036076144,0.00007936089,0.00032170818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003302204,0.00019434503,0.00015236638,0.0003339384,0.00025138757,0.00058026944,0.00012586701,0.00026987947,0.0015683688],"category_scores_gemma":[0.0016282683,0.0001337614,0.00022452531,0.0003236885,0.00029552626,0.00023485151,0.0004520361,0.0002810819,0.00015223771],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003972568,0.00005375099,0.99212885,0.000013725633,0.000063402564,0.00031442312,0.000069908296,0.0014539228,0.002120147,0.0000983582,0.00025938515,0.0030269313],"study_design_scores_gemma":[0.0000069407533,0.000032204,0.9986117,0.0000030561064,0.000015087724,0.00008392816,0.00007750745,0.00083872996,0.00018254068,0.00003892617,0.000107401545,0.00000203045],"about_ca_topic_score_codex":0.024726197,"about_ca_topic_score_gemma":0.023920938,"teacher_disagreement_score":0.024726197,"about_ca_system_score_codex":0.0004680663,"about_ca_system_score_gemma":0.0007544211,"threshold_uncertainty_score":0.049164593},"labels":[],"label_agreement":null},{"id":"W2150966988","doi":"10.1029/1999gl011098","title":"Why is the cloud albedo — Particle size relationship different in optically thick and optically thin clouds?","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Liquid water content; Albedo (alchemy); Cloud albedo; Effective radius; Adiabatic process; Sign (mathematics); RADIUS; Atmospheric sciences; Environmental science; Cloud computing; Cloud fraction; Materials science; Physics; Cloud cover; Astrophysics; Thermodynamics; Mathematics","score_opus":0.022883426043441568,"score_gpt":0.2792280906991944,"score_spread":0.25634466465575284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2150966988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98814,0.004405141,0.0026486914,0.0016760331,0.000074301526,0.000014656323,0.00026643972,0.000059300175,0.002715452],"genre_scores_gemma":[0.9982681,0.00071209186,0.0003707148,0.00032528493,0.0000669172,0.0000031933332,0.000095813244,0.000013261596,0.00014454528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997838,0.000036573823,0.000012748152,0.00007390653,0.00003812052,0.000054881093],"domain_scores_gemma":[0.997335,0.0013478718,0.0006762682,0.00015353528,0.00020817628,0.00027910937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00062569755,0.00016640205,0.0003552853,0.00064634,0.00023771549,0.0007112927,0.00036127583,0.0007761706,0.0008047627],"category_scores_gemma":[0.004836749,0.00020672992,0.00030114417,0.00060314895,0.0010353812,0.001070231,0.00032110483,0.00060433283,0.00024399423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027612504,0.00008182285,0.94042647,0.00016567319,0.00035005412,0.00030320385,0.0004568833,0.0011940972,0.019001659,0.0019531676,0.001053205,0.03473764],"study_design_scores_gemma":[0.000009891561,0.000056496912,0.99487853,0.00001814073,0.00002990872,0.00023791398,0.0002715519,0.00088619196,0.0011571782,0.001958632,0.00048177122,0.000013714631],"about_ca_topic_score_codex":0.0038542522,"about_ca_topic_score_gemma":0.0038069077,"teacher_disagreement_score":0.0038542522,"about_ca_system_score_codex":0.0003242837,"about_ca_system_score_gemma":0.00015575407,"threshold_uncertainty_score":0.0076636076},"labels":[],"label_agreement":null},{"id":"W2151214053","doi":"10.1002/grl.50826","title":"Scattered waves from low‐frequency earthquakes and plate boundary structure in northern Cascadia","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Geology; Subduction; Seismology; Plate tectonics; Waveform; Boundary (topology); Transect; Scattering; Geophysics; Tectonics; Physics; Optics; Oceanography","score_opus":0.01926826764238308,"score_gpt":0.2478294325732843,"score_spread":0.22856116493090123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2151214053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988242,0.000011153834,0.0005977427,0.000031034568,0.0000012920898,0.000001519876,0.00010254058,0.000042319214,0.00038811783],"genre_scores_gemma":[0.99954623,0.000010219266,0.00017728862,0.0000016677483,8.465378e-7,0.0000016695449,0.0001209963,0.0000054479624,0.00013568957],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999405,0.000011273289,0.0000037195148,0.000018470331,0.000017064369,0.000008995584],"domain_scores_gemma":[0.99978846,0.000045940524,0.00003909242,0.000031325042,0.000046754234,0.0000485243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015862216,0.00029613182,0.00021141759,0.0005294813,0.0003388945,0.00050098135,0.0003934287,0.00036553878,0.0009293947],"category_scores_gemma":[0.0008011952,0.00035442115,0.0003734526,0.0004532347,0.0002828624,0.0002671334,0.0003429567,0.00029490708,0.00017922063],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019994196,0.00011062122,0.41228864,0.000051593892,0.0001615305,0.0006287932,0.000807393,0.5559755,0.018352024,0.00062597025,0.00046094725,0.010337034],"study_design_scores_gemma":[0.000032924036,0.00004673834,0.4589375,0.000009289459,0.00003081501,0.00006855967,0.0002991709,0.5383339,0.0014379417,0.0004500249,0.0003283015,0.000024924833],"about_ca_topic_score_codex":0.103647195,"about_ca_topic_score_gemma":0.08434357,"teacher_disagreement_score":0.103647195,"about_ca_system_score_codex":0.0011037877,"about_ca_system_score_gemma":0.0005413515,"threshold_uncertainty_score":0.20608783},"labels":[],"label_agreement":null},{"id":"W2152258617","doi":"10.1029/2006gl028469","title":"Caribbean and Pacific moisture sources on the Isthmus of Panama revealed from stalagmite and surface water <i>δ</i><sup>18</sup>O gradients","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Stalagmite; Intertropical Convergence Zone; Panama; Moisture; Geology; Oceanography; Sea surface temperature; Pacific ocean; Climatology; δ18O; Cave; Tropical Eastern Pacific; Geography; Holocene; Precipitation; Stable isotope ratio; Meteorology","score_opus":0.02518392802891144,"score_gpt":0.2572895589166334,"score_spread":0.23210563088772196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152258617","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99966896,0.000030348408,0.000020702113,0.000005260441,2.6224112e-7,8.191382e-7,0.000047641952,0.0000013689923,0.00022462601],"genre_scores_gemma":[0.99980444,0.0000332337,0.00005357127,0.0000017910319,0.0000011837218,0.000001378496,0.00008097233,0.0000011180565,0.000022273656],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.000012368864,0.0000053517074,0.00002132209,0.000009765298,0.000014988066],"domain_scores_gemma":[0.9997086,0.000057924324,0.00012124572,0.000025564736,0.000052563195,0.00003414877],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012885295,0.00018589596,0.00017309464,0.0010258406,0.00034668067,0.00063340965,0.00014558037,0.00010988254,0.00064678834],"category_scores_gemma":[0.0006983335,0.00013074411,0.000112375565,0.0013225707,0.0003210528,0.000361898,0.00060174847,0.00013794213,0.000056837842],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008688751,0.0000071221284,0.9859346,0.000011824078,0.000042610405,0.00011425004,0.0007380414,0.00023259134,0.004910519,0.000130377,0.000043303306,0.007747978],"study_design_scores_gemma":[0.0000017291508,0.0000051093643,0.9991301,0.0000026927771,0.000011076305,0.000030890766,0.00019299476,0.0003563921,0.00013815172,0.000022887492,0.00010660877,0.000001471873],"about_ca_topic_score_codex":0.040156867,"about_ca_topic_score_gemma":0.07584737,"teacher_disagreement_score":0.040156867,"about_ca_system_score_codex":0.00025363814,"about_ca_system_score_gemma":0.0002012176,"threshold_uncertainty_score":0.07984626},"labels":[],"label_agreement":null},{"id":"W2152290863","doi":"10.1029/2005gl023822","title":"The glacial North Atlantic Oscillation","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Atlantic multidecadal oscillation; Glacial period; Last Glacial Maximum; Climatology; North Atlantic oscillation; Geology; Oscillation (cell signaling); General Circulation Model; Mode (computer interface); Atmosphere (unit); Oceanography; Climate change; Geography; Meteorology; Geomorphology","score_opus":0.036201385113693536,"score_gpt":0.3024491849982548,"score_spread":0.26624779988456126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152290863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91138774,0.0023289605,0.01779088,0.0014970613,0.0005316768,0.00003222565,0.0042545735,0.0005249042,0.06165199],"genre_scores_gemma":[0.996897,0.00036925165,0.001241196,0.0000842998,0.000033858625,0.00000915012,0.00046061957,0.00002566714,0.0008790149],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999397,0.00001727733,0.0000029874434,0.000023669963,0.000009852234,0.0000065041645],"domain_scores_gemma":[0.99992514,0.000015747832,0.000020688369,0.000010663688,0.00001248239,0.000015132802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019704782,0.000119551376,0.00012305618,0.00021816861,0.0002523041,0.0007899247,0.00014840752,0.00022539055,0.001674138],"category_scores_gemma":[0.0010403448,0.00010146705,0.00020519424,0.00027298986,0.00027086472,0.00046227008,0.00038303845,0.00025372277,0.00016271546],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030605355,0.000051014522,0.30594,0.00022480729,0.0007315156,0.0003683666,0.00065599807,0.42174238,0.012877318,0.12765475,0.02423827,0.105209425],"study_design_scores_gemma":[0.00015457624,0.00008988124,0.37776378,0.00012913912,0.00024584273,0.00034095088,0.0002370333,0.47627854,0.0011650998,0.06631064,0.07720363,0.00008089879],"about_ca_topic_score_codex":0.015905123,"about_ca_topic_score_gemma":0.019546082,"teacher_disagreement_score":0.015905123,"about_ca_system_score_codex":0.00059698167,"about_ca_system_score_gemma":0.00051925017,"threshold_uncertainty_score":0.031625092},"labels":[],"label_agreement":null},{"id":"W2152531357","doi":"10.1029/2012gl053763","title":"Stability of the Atlantic meridional overturning circulation: A model intercomparison","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":245,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Belgian Federal Science Policy Office; University of Victoria","keywords":"Coupled model intercomparison project; Climatology; Environmental science; Thermohaline circulation; General Circulation Model; Climate model; Ocean current; Flux (metallurgy); Climate change; Zonal and meridional; Atmospheric sciences; Geology; Oceanography; Chemistry","score_opus":0.08455978273954286,"score_gpt":0.31703642283220956,"score_spread":0.23247664009266672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152531357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978479,0.00008360253,0.0007510928,0.00010306211,0.000011676679,0.0000126113,0.00027059205,0.000048202353,0.00087133027],"genre_scores_gemma":[0.9975726,0.000049173297,0.0013911537,0.00003257371,0.000007719247,0.000023422035,0.000748205,0.00002091484,0.00015426234],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993285,0.00030525596,0.000040183022,0.00018944107,0.00006341839,0.00007326367],"domain_scores_gemma":[0.9980167,0.0011557884,0.00019838239,0.00031741167,0.00020428502,0.000107442334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0034164933,0.0008391164,0.0006413904,0.0005815324,0.00048268013,0.0013478037,0.0012011119,0.0013926798,0.00058947224],"category_scores_gemma":[0.0041212337,0.0004220456,0.0013550757,0.0006604959,0.00033410365,0.0011916743,0.00090891175,0.00073482597,0.00011477173],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023306604,0.0005288273,0.2849479,0.000119606826,0.00239749,0.00054400135,0.0011584596,0.6586051,0.015120575,0.002567492,0.0024954856,0.029184408],"study_design_scores_gemma":[0.000572511,0.0006914477,0.123412125,0.000029548099,0.0005080724,0.00010355344,0.00034843953,0.8656119,0.005598919,0.0015460165,0.0014771211,0.00010031279],"about_ca_topic_score_codex":0.021875955,"about_ca_topic_score_gemma":0.012412025,"teacher_disagreement_score":0.021875955,"about_ca_system_score_codex":0.0012293895,"about_ca_system_score_gemma":0.0008989667,"threshold_uncertainty_score":0.043497205},"labels":[],"label_agreement":null},{"id":"W2152824096","doi":"10.1029/2004gl021146","title":"Diagnosing the role of eddies in driving the circulation of the northwest Atlantic Ocean","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Eddy; Gulf Stream; Oceanography; Ocean current; Geology; Circulation (fluid dynamics); Climatology; Temperature salinity diagrams; Thermohaline circulation; Scale (ratio); Salinity; Meteorology; Geography; Turbulence; Mechanics","score_opus":0.012377394365543458,"score_gpt":0.23790571917242284,"score_spread":0.22552832480687937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152824096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98359954,0.00009540383,0.015060836,0.00020850777,0.00003186316,0.000010510924,0.00019052139,0.00010098694,0.0007017682],"genre_scores_gemma":[0.9940268,0.000044652646,0.0055620377,0.000019439492,0.000008950028,0.0000029420926,0.00012855197,0.000007841556,0.00019868789],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998987,0.00003788934,0.000008932223,0.000016012875,0.00001783611,0.000020618983],"domain_scores_gemma":[0.9991768,0.00033889263,0.00015039566,0.000089697074,0.0001493876,0.00009477984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006244598,0.00033760926,0.00018282991,0.00026837815,0.00026798004,0.00055626617,0.00034031592,0.0004815857,0.00059372146],"category_scores_gemma":[0.003185527,0.00027537468,0.0001540725,0.00017288284,0.00020084881,0.00071752735,0.0005489047,0.00035311142,0.000091542264],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037862558,0.00010938757,0.770841,0.00007571363,0.00006593534,0.00033117458,0.00015380081,0.16328825,0.024091369,0.0014193552,0.00061673,0.03862852],"study_design_scores_gemma":[0.00003977728,0.000060619106,0.10895274,0.00001464169,0.00002142713,0.00007635407,0.00012990258,0.88265765,0.00669257,0.0007236828,0.0006117533,0.000018864312],"about_ca_topic_score_codex":0.01944893,"about_ca_topic_score_gemma":0.027382711,"teacher_disagreement_score":0.01944893,"about_ca_system_score_codex":0.0005242459,"about_ca_system_score_gemma":0.00076974946,"threshold_uncertainty_score":0.038671434},"labels":[],"label_agreement":null},{"id":"W2152906989","doi":"10.1029/2005gl022422","title":"First measurements of CFC‐113 and HCFC‐142b from space using ACE‐FTS infrared spectra","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Atmosphere (unit); Satellite; Atmospheric sciences; Mixing ratio; Environmental science; Infrared; Atmospheric composition; Mixing (physics); Remote sensing; Meteorology; Materials science; Physics; Geology; Astronomy","score_opus":0.0671691958326488,"score_gpt":0.2947004497463271,"score_spread":0.2275312539136783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2152906989","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96461827,0.001180187,0.012008731,0.00019040986,0.00005311325,0.00017149697,0.0066179424,0.00044643704,0.014713349],"genre_scores_gemma":[0.9689534,0.00046766966,0.022138426,0.00013521113,0.00003203763,0.00007469509,0.004922459,0.00006461308,0.0032116144],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99926764,0.000025453206,0.000010674497,0.000102349324,0.0004837677,0.00011009662],"domain_scores_gemma":[0.9996068,0.000047635356,0.000032779262,0.000042344494,0.0002238025,0.00004672617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006224586,0.0005960183,0.0005097715,0.0012681826,0.0014599097,0.00089175993,0.00044755044,0.0009211062,0.0010170174],"category_scores_gemma":[0.0009543065,0.00030079295,0.0003485084,0.0010953179,0.0004810888,0.0007563831,0.00071802293,0.001036893,0.00028803165],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013258082,0.00039418682,0.08156474,0.00027034068,0.00015481147,0.00032033212,0.00083469885,0.0050336933,0.81310165,0.002106722,0.0046227,0.09027031],"study_design_scores_gemma":[0.00014663547,0.0006325051,0.25751176,0.000052783987,0.00011843134,0.00026144861,0.00022681586,0.017866012,0.6926716,0.0005907449,0.029781088,0.00014013167],"about_ca_topic_score_codex":0.04595348,"about_ca_topic_score_gemma":0.04689853,"teacher_disagreement_score":0.04595348,"about_ca_system_score_codex":0.0015451625,"about_ca_system_score_gemma":0.00086094625,"threshold_uncertainty_score":0.09137201},"labels":[],"label_agreement":null},{"id":"W2153361527","doi":"10.1002/2015gl066104","title":"Increasing atmospheric water vapor and higher daily precipitation intensity over northern Eurasia","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration; National Science Foundation","keywords":"Precipitation; Environmental science; Water vapor; Humidity; Atmospheric sciences; Climatology; Atmosphere (unit); Intensity (physics); Relative humidity; Percentile; Meteorology; Geology; Geography","score_opus":0.04680589148919691,"score_gpt":0.2962094391133382,"score_spread":0.2494035476241413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153361527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997038,0.00002687773,0.00005163337,0.000011017192,5.8007635e-7,4.573586e-7,0.000046834884,0.0000020138466,0.00015665527],"genre_scores_gemma":[0.9998419,0.000016013875,0.000035107718,0.0000027251263,0.0000017737217,5.178386e-7,0.000055750923,5.0560175e-7,0.00004567418],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999095,0.000024619005,0.000007239479,0.000028078379,0.0000124933895,0.000017955532],"domain_scores_gemma":[0.99975175,0.000059072263,0.00010091785,0.000017880151,0.000028583818,0.000041727268],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025508666,0.00012021577,0.00016204627,0.00023572483,0.00010403669,0.0002692103,0.00011416734,0.000121611214,0.0005676805],"category_scores_gemma":[0.0004072733,0.000093643415,0.00016974175,0.0003296762,0.00019268315,0.0002205647,0.00023654594,0.00012824728,0.000044226927],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009697213,0.000020589987,0.98482335,0.000015827787,0.00013971579,0.00014715752,0.00017636281,0.0019204402,0.009140923,0.0000789334,0.000068744856,0.0033709598],"study_design_scores_gemma":[0.0000023794107,0.000010875005,0.99900705,9.641949e-7,0.000008664218,0.00003211429,0.000044098575,0.0006685083,0.00013376925,0.000021286072,0.00006913823,0.000001178352],"about_ca_topic_score_codex":0.019469492,"about_ca_topic_score_gemma":0.019942265,"teacher_disagreement_score":0.019469492,"about_ca_system_score_codex":0.0001956579,"about_ca_system_score_gemma":0.00017880193,"threshold_uncertainty_score":0.038712323},"labels":[],"label_agreement":null},{"id":"W2153374388","doi":"10.1029/2011gl050064","title":"Shear wave reflectivity imaging of the Nazca‐South America subduction zone: Stagnant slab in the mantle transition zone?","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Transition zone; Subduction; Slab; Seismology; Mantle (geology); Discontinuity (linguistics); Classification of discontinuities; Slab window; Mantle wedge; Shear zone; Convergent boundary; Oceanic crust; Geophysics; Petrology; Tectonics","score_opus":0.043922225755914084,"score_gpt":0.28618831028623637,"score_spread":0.24226608453032228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153374388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984818,0.000100706544,0.0006330568,0.000021281254,0.0000010136667,0.000002992428,0.00007381253,0.000014877396,0.00067035685],"genre_scores_gemma":[0.9981541,0.00009880428,0.0013598851,0.00000947695,0.00000252359,0.0000026695986,0.00011087822,0.000005011545,0.00025662512],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997175,0.0000027422286,0.000001607811,0.0000071852323,0.000007829104,0.000008907091],"domain_scores_gemma":[0.999956,0.0000057377115,0.000010739931,0.0000047238955,0.000014072114,0.000008757387],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011182473,0.0001496976,0.00010045771,0.0004740671,0.0001352996,0.00029727435,0.000175667,0.00017442972,0.00059362105],"category_scores_gemma":[0.00022183478,0.00013390381,0.00008628059,0.00039986786,0.000099187426,0.00024019749,0.00023626238,0.00011745998,0.00015615171],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025077313,0.00006355988,0.3777185,0.00006814026,0.00008497274,0.00036107213,0.0007292296,0.0015696881,0.56550264,0.00021635163,0.00026457434,0.05317049],"study_design_scores_gemma":[0.000008778522,0.00004198584,0.98015094,0.00000803625,0.000042891385,0.00026117568,0.00033649558,0.004772725,0.013448559,0.000079723926,0.0008418112,0.0000067840338],"about_ca_topic_score_codex":0.0060163005,"about_ca_topic_score_gemma":0.013828562,"teacher_disagreement_score":0.0060163005,"about_ca_system_score_codex":0.000107701875,"about_ca_system_score_gemma":0.00015563144,"threshold_uncertainty_score":0.011962593},"labels":[],"label_agreement":null},{"id":"W2153442034","doi":"10.1029/2004gl019599","title":"Low‐frequency variability of the statistical moments of sea surface winds","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Canadian Institute for Advanced Research","funders":"","keywords":"Skewness; Standard deviation; Climatology; Atmospheric sciences; Drag; Environmental science; Meteorology; Geology; Physics; Statistics; Mathematics; Mechanics","score_opus":0.03063894328888188,"score_gpt":0.30862094748918556,"score_spread":0.27798200420030367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153442034","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96982354,0.00022933759,0.02463825,0.00014485039,0.000036343656,0.000011273533,0.0007244323,0.00012736836,0.004264554],"genre_scores_gemma":[0.9981572,0.00007958715,0.0006593128,0.000009789586,0.00003474088,0.000005283922,0.0005798908,0.0000150199285,0.00045912768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983454,0.000038926144,0.000011616385,0.000034506324,0.00005021388,0.000030228843],"domain_scores_gemma":[0.9975044,0.0014511221,0.00037298418,0.00019994969,0.00039226768,0.00007922585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000538368,0.00018878539,0.00015281525,0.0007001771,0.00020339729,0.0005866236,0.00015446584,0.00018792263,0.0008530286],"category_scores_gemma":[0.004273444,0.00009665125,0.00026135848,0.0005330749,0.00025407452,0.0003940227,0.00025004844,0.00034861141,0.00023339494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040023396,0.0001553037,0.53528,0.000201932,0.00033772446,0.0009453182,0.00043934095,0.29716575,0.03735511,0.014888898,0.0042906483,0.10853978],"study_design_scores_gemma":[0.000013647523,0.00012539979,0.6453884,0.000024517678,0.00006625426,0.0005466701,0.00014700131,0.33732623,0.0036269804,0.009352138,0.0033303062,0.000052409483],"about_ca_topic_score_codex":0.0017411156,"about_ca_topic_score_gemma":0.0015359113,"teacher_disagreement_score":0.0017411156,"about_ca_system_score_codex":0.00024189749,"about_ca_system_score_gemma":0.00013662419,"threshold_uncertainty_score":0.003461957},"labels":[],"label_agreement":null},{"id":"W2153443072","doi":"10.1002/2015gl064156","title":"Changes in ocean vertical heat transport with global warming","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Australian Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Downwelling; Effects of global warming on oceans; Climatology; Upwelling; Global warming; Environmental science; Ocean heat content; Deep ocean water; Ocean current; Oceanography; Deep sea; Thermohaline circulation; Ocean general circulation model; Forcing (mathematics); Southern Hemisphere; Climate change; Sea surface temperature; Lead (geology); Geology; General Circulation Model","score_opus":0.035775016556771386,"score_gpt":0.2756236932385972,"score_spread":0.2398486766818258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153443072","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99666697,0.00018349277,0.00041649307,0.00024392281,0.000018547515,0.0000035527978,0.000603732,0.00004174703,0.0018215601],"genre_scores_gemma":[0.99955577,0.00004227725,0.00005868585,0.000011856727,0.000004654484,0.0000018886209,0.00014559197,0.000004146525,0.00017518621],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999254,0.000017266872,0.0000040512496,0.000023868513,0.0000073843676,0.000022021903],"domain_scores_gemma":[0.9998005,0.00007353934,0.000046701323,0.000029481356,0.00003349873,0.000016234946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022417941,0.00023894417,0.00014285349,0.00037467454,0.00018569296,0.0006438988,0.000143528,0.00033188178,0.002488128],"category_scores_gemma":[0.0008431331,0.00015597223,0.0003784149,0.0005277316,0.00035247958,0.0006547225,0.00040996392,0.000316794,0.00016540986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065040315,0.00011135302,0.6986541,0.0001986656,0.00066948374,0.00028755606,0.00038299314,0.23326093,0.032253686,0.0077335825,0.002186462,0.023610733],"study_design_scores_gemma":[0.00006372845,0.00015124532,0.90553343,0.000027544686,0.00014061146,0.000107442684,0.0003876376,0.07866065,0.0069595375,0.0048658503,0.0030633095,0.000039033806],"about_ca_topic_score_codex":0.0074225212,"about_ca_topic_score_gemma":0.0041776868,"teacher_disagreement_score":0.0074225212,"about_ca_system_score_codex":0.00070134416,"about_ca_system_score_gemma":0.0002142194,"threshold_uncertainty_score":0.014758587},"labels":[],"label_agreement":null},{"id":"W2153639575","doi":"10.1029/2010gl045310","title":"Discovery of the FeO orange bands in the terrestrial night airglow spectrum obtained with OSIRIS on the Odin spacecraft","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; York University","funders":"Tekes; Centre National d’Etudes Spatiales","keywords":"Airglow; Radiance; Afterglow; Physics; Spectrograph; Spectral line; Osiris; Atmospheric sciences; Emission spectrum; Mesosphere; Astrophysics; Astronomy; Optics; Stratosphere","score_opus":0.012898882725218282,"score_gpt":0.25773514278754706,"score_spread":0.24483626006232878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153639575","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99673957,0.00002254134,0.00065440184,0.000019243598,0.0000034409993,0.000005117036,0.00028210165,0.000034636658,0.0022389838],"genre_scores_gemma":[0.99738103,0.000018219413,0.00150149,0.000019656212,0.000003860949,0.0000040067653,0.0006368364,0.000010666493,0.0004242741],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996483,0.0000022072047,8.792625e-7,0.000012043571,0.000010797434,0.000009215827],"domain_scores_gemma":[0.9999262,0.000007927159,0.00001730982,0.00000993752,0.000014241044,0.000024479436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010503772,0.00015802312,0.000079322315,0.0003800796,0.00031401828,0.00024199531,0.00012576887,0.00015019673,0.0006943227],"category_scores_gemma":[0.00014607496,0.00012959795,0.00009209298,0.0002892287,0.00015989774,0.00014519539,0.00023712876,0.00018329159,0.00014006895],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059952657,0.00014799261,0.5780479,0.00005201336,0.000054900236,0.0008013751,0.0006843639,0.00084318634,0.3818171,0.0004626109,0.0011708081,0.035318222],"study_design_scores_gemma":[0.000008820976,0.00003664152,0.99138206,0.0000034910256,0.0000064347832,0.00014177237,0.000072211624,0.00077696925,0.0064903134,0.000045533878,0.0010328771,0.0000028745326],"about_ca_topic_score_codex":0.002736851,"about_ca_topic_score_gemma":0.008730355,"teacher_disagreement_score":0.002736851,"about_ca_system_score_codex":0.00016659162,"about_ca_system_score_gemma":0.00009252907,"threshold_uncertainty_score":0.0054418445},"labels":[],"label_agreement":null},{"id":"W2153742375","doi":"10.1029/2005gl022433","title":"Co‐located ACE‐FTS and Odin/SMR stratospheric‐mesospheric CO 2004 measurements and comparison with a GCM","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; York University","funders":"Canadian Foundation for Climate and Atmospheric Sciences","keywords":"Stratosphere; Thermosphere; Atmospheric sciences; Troposphere; Occultation; Environmental science; Climatology; Mesosphere; Latitude; Polar night; Polar; Arctic; Middle latitudes; Ionosphere; Geology; Physics; Geophysics; Geodesy; Astronomy","score_opus":0.053583648104156265,"score_gpt":0.30848276070657293,"score_spread":0.25489911260241666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2153742375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920034,0.0003012016,0.00089659647,0.00004831784,0.000031901043,0.0000118415755,0.0026035996,0.00007080041,0.004032391],"genre_scores_gemma":[0.9952421,0.00011603045,0.0016582431,0.00001592431,0.000019554276,0.000007864513,0.002514696,0.00001256827,0.0004130588],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996859,0.000048178717,0.000015070846,0.00008777331,0.000108650296,0.000054432316],"domain_scores_gemma":[0.99929,0.00009650633,0.00012007819,0.00007959506,0.00035926964,0.000054567543],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034668087,0.00029391903,0.00024668025,0.0010565419,0.00036348906,0.0005649097,0.00022702366,0.00030753747,0.00063017587],"category_scores_gemma":[0.0009044916,0.00015751479,0.00019105511,0.0014252857,0.00013038095,0.0004037072,0.00031969117,0.00019019286,0.0002564261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016919466,0.00017633481,0.8739937,0.0001700229,0.00044330652,0.00036102673,0.0004486807,0.010334045,0.052986838,0.0005322672,0.0027835637,0.056078278],"study_design_scores_gemma":[0.000026252188,0.00008502968,0.9798962,0.000011117402,0.00009074283,0.00018087047,0.00018531745,0.0069405492,0.009667584,0.000055500775,0.0028470757,0.000013869254],"about_ca_topic_score_codex":0.031775467,"about_ca_topic_score_gemma":0.06688465,"teacher_disagreement_score":0.031775467,"about_ca_system_score_codex":0.00067838986,"about_ca_system_score_gemma":0.0004407064,"threshold_uncertainty_score":0.06318104},"labels":[],"label_agreement":null},{"id":"W2154201151","doi":"10.1029/2001gl014162","title":"High‐resolution measurements and simulation of stratospheric and tropospheric intrusions in the vicinity of the polar jet stream","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Troposphere; Stratosphere; Tropopause; Potential vorticity; Atmospheric sciences; Jet stream; Polar; Environmental science; Polar vortex; TRACER; Geology; Jet (fluid); Climatology; Physics; Meteorology; Vorticity; Vortex","score_opus":0.04909768623395231,"score_gpt":0.27624121996649603,"score_spread":0.22714353373254373,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154201151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993455,0.000010948182,0.0002676188,0.000009480547,0.0000019024743,0.0000033953133,0.000102534235,0.000030001323,0.00022855985],"genre_scores_gemma":[0.999074,0.000015632464,0.00058081653,0.0000027639662,0.0000014864762,0.0000028386228,0.00023257911,0.00000381863,0.00008610116],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996114,0.000005184917,0.0000015582679,0.000007960984,0.000007690271,0.000016409165],"domain_scores_gemma":[0.99990106,0.000038226786,0.000014195708,0.000009972263,0.000014639193,0.000021832542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010411311,0.00021759754,0.00016160404,0.00015568563,0.00029697322,0.00030900518,0.000311797,0.0003003402,0.000425639],"category_scores_gemma":[0.00033608178,0.00021316989,0.00020048965,0.00025040488,0.0002627689,0.00015241376,0.0001457401,0.00021015464,0.000050701543],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012828954,0.0005996432,0.18438506,0.00009809981,0.00017733671,0.0011523536,0.0005079433,0.7049543,0.09051181,0.00065401895,0.00090830773,0.0147682475],"study_design_scores_gemma":[0.00015382143,0.0001955058,0.17582467,0.000006025276,0.00003901719,0.00007248161,0.00016849747,0.81214285,0.010707921,0.00014972233,0.0005211188,0.000018240748],"about_ca_topic_score_codex":0.062279068,"about_ca_topic_score_gemma":0.046810552,"teacher_disagreement_score":0.062279068,"about_ca_system_score_codex":0.00058814697,"about_ca_system_score_gemma":0.00040467025,"threshold_uncertainty_score":0.12383312},"labels":[],"label_agreement":null},{"id":"W2154309921","doi":"10.1029/2000gl000016","title":"Influence of ionospheric electron density fluctuations on satellite radar interferometry","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":241,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Ionosphere; Azimuth; Geology; Remote sensing; Radar; Satellite; Interferometry; Synthetic aperture radar; Geodesy; Geophysics; Physics; Optics; Computer science; Telecommunications; Astronomy","score_opus":0.010984280661453986,"score_gpt":0.272737623586153,"score_spread":0.26175334292469904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154309921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99537766,0.00023179332,0.0028066128,0.0000360275,0.000012123877,0.0000055803007,0.00011893515,0.000055773347,0.0013554927],"genre_scores_gemma":[0.9993647,0.00009352843,0.0003487027,0.000009352563,0.0000053416647,0.000001655473,0.00008768956,0.000010777522,0.00007822467],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998362,0.00004947277,0.000008756973,0.00002726703,0.00004738731,0.00003087627],"domain_scores_gemma":[0.99942905,0.00031986114,0.00009234923,0.000054338056,0.00007685809,0.000027499895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026979716,0.0002324642,0.00020228619,0.0002758821,0.00016755781,0.00035561417,0.00010368906,0.00016531117,0.00039573357],"category_scores_gemma":[0.0022914622,0.000114913106,0.000111125824,0.000347059,0.00022608337,0.00024303001,0.0002734577,0.0001602815,0.000095477626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002258673,0.00012038,0.47611287,0.00015484629,0.00031798126,0.0023554843,0.00056099717,0.114711076,0.28512743,0.0011718641,0.0012208351,0.11588751],"study_design_scores_gemma":[0.000035638826,0.00032364824,0.8832161,0.00001820267,0.00010618501,0.0008521386,0.00021848298,0.064446665,0.04910238,0.00042410012,0.0012213233,0.000035103232],"about_ca_topic_score_codex":0.0017381526,"about_ca_topic_score_gemma":0.0013911512,"teacher_disagreement_score":0.0017381526,"about_ca_system_score_codex":0.00013510829,"about_ca_system_score_gemma":0.00008646847,"threshold_uncertainty_score":0.0034560561},"labels":[],"label_agreement":null},{"id":"W2154746660","doi":"10.1029/2004gl020939","title":"Lithospheric anisotropy structure inferred from collocated teleseismic and magnetotelluric observations: Great Slave Lake shear zone, northern Canada","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Manitoba; Western University","funders":"","keywords":"Geology; Lithosphere; Shear wave splitting; Anisotropy; Seismology; Magnetotellurics; Geophysics; Shear (geology); Seismic anisotropy; Mantle (geology); Shear zone; Tectonics; Petrology; Electrical resistivity and conductivity","score_opus":0.018176033042577228,"score_gpt":0.22455137456006172,"score_spread":0.2063753415174845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154746660","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956911,0.00015838865,0.00010840143,0.00008151703,0.0000022226668,0.000010857913,0.0016850403,0.000019608187,0.0022427887],"genre_scores_gemma":[0.99678963,0.00018402888,0.0003269553,0.000018180135,0.0000017933279,0.000005187157,0.0015445912,0.000009672622,0.0011199465],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997948,0.0000090002795,0.000009154219,0.000034154775,0.000069097725,0.000083778985],"domain_scores_gemma":[0.99933213,0.000035664503,0.000058401463,0.00002696137,0.00041742323,0.00012943285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024640452,0.00026991396,0.00023762733,0.0013569586,0.0017391498,0.0010383975,0.0005541061,0.00020770934,0.0013425983],"category_scores_gemma":[0.0010279254,0.00029680028,0.00018047744,0.0030596808,0.0006504249,0.00022507765,0.000618129,0.00027171284,0.00018030286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002477278,0.000028730607,0.96284205,0.000052449897,0.00011163474,0.0002644705,0.0018617905,0.0031537432,0.009935976,0.0007342368,0.0021524935,0.01861471],"study_design_scores_gemma":[0.000014119718,0.0000047546664,0.9959266,0.00001538225,0.00002292812,0.000026095262,0.00066242606,0.0014685679,0.000629788,0.000048103484,0.0011692655,0.00001186865],"about_ca_topic_score_codex":0.9962443,"about_ca_topic_score_gemma":0.9985947,"teacher_disagreement_score":0.0140602365,"about_ca_system_score_codex":0.0140602365,"about_ca_system_score_gemma":0.015729845,"threshold_uncertainty_score":0.10201466},"labels":[],"label_agreement":null},{"id":"W2154775863","doi":"10.1002/2015gl063737","title":"Revealing important nocturnal and day‐to‐day variations in fire smoke emissions through a multiplatform inversion","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Center for Research Resources; National Aeronautics and Space Administration; University of Nevada, Reno; University of Lethbridge; National Science Foundation","keywords":"Environmental science; Inversion (geology); Meteorology; Smoke; Nocturnal; Satellite; Air quality index; Atmospheric sciences; Climatology; Aerosol; Present day; Diurnal cycle; Geology; Geography","score_opus":0.07034019979807318,"score_gpt":0.3154563582598923,"score_spread":0.24511615846181914,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2154775863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9720044,0.000016862235,0.025926003,0.00005452106,0.0000085891825,0.000017949738,0.00026488217,0.00034589347,0.001360912],"genre_scores_gemma":[0.9819131,0.000012060325,0.017408816,0.000022296119,0.0000052702535,0.000011560855,0.00037996526,0.000039554132,0.00020740976],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.0000142589715,0.00000525681,0.000028512244,0.000023385524,0.000027125949],"domain_scores_gemma":[0.9996859,0.00013553016,0.00004222457,0.000054332686,0.000052805684,0.000029348494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039840332,0.000494868,0.00024358096,0.00036655497,0.0003361614,0.00042663995,0.00071648293,0.00040205437,0.0009817348],"category_scores_gemma":[0.0011580322,0.0003567036,0.0006513946,0.00039060685,0.00033058296,0.0005205453,0.0005294007,0.0004976065,0.0001201083],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015871959,0.0002665595,0.046705082,0.000021547823,0.00010680509,0.00011907324,0.00006872083,0.90393984,0.023718268,0.0005834606,0.00034967667,0.023962282],"study_design_scores_gemma":[0.000017618466,0.000019809519,0.0065237307,0.000001483228,0.000008606221,0.000013300244,0.000013840423,0.9907691,0.0023762528,0.00013804798,0.00011028745,0.0000079222855],"about_ca_topic_score_codex":0.04097394,"about_ca_topic_score_gemma":0.0481552,"teacher_disagreement_score":0.04097394,"about_ca_system_score_codex":0.00050299504,"about_ca_system_score_gemma":0.0011194198,"threshold_uncertainty_score":0.08147085},"labels":[],"label_agreement":null},{"id":"W2155104583","doi":"10.1029/2008gl033969","title":"Correlation of substorm injections, auroral modulations, and ground Pi2","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"","keywords":"Substorm; Magnetometer; Physics; Geophysics; Latitude; Spacecraft; Longitude; Phase (matter); Ion; Magnetosphere; Astrophysics; Geology; Geodesy; Astronomy; Magnetic field","score_opus":0.02239655418214759,"score_gpt":0.27896232815465194,"score_spread":0.25656577397250435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155104583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966918,0.00010996363,0.0011744994,0.00005665054,0.000008486344,0.000022139062,0.00009594125,0.000038636328,0.0018017933],"genre_scores_gemma":[0.9992939,0.000042679654,0.0003136542,0.000015127218,0.00001484567,0.00000383348,0.000071174654,0.000005991132,0.00023877807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998528,0.000013321034,0.0000124569315,0.000038228587,0.000041126637,0.000042016007],"domain_scores_gemma":[0.99954706,0.00007687875,0.00020735836,0.000050703962,0.00005818574,0.000059875],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016886064,0.00026886014,0.00022608553,0.00077819236,0.00041478776,0.0004807374,0.0002394934,0.00043409536,0.0009707891],"category_scores_gemma":[0.0008831464,0.00010814584,0.00015289322,0.00059581833,0.00032239684,0.00023187579,0.00034724252,0.0003587821,0.00012409277],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004802285,0.00010352029,0.8715256,0.00006227573,0.000081864346,0.06705949,0.001478865,0.0012611154,0.025636654,0.0006390906,0.00081448973,0.030856889],"study_design_scores_gemma":[0.000021179745,0.0004695082,0.8927278,0.000021498367,0.00010133754,0.07958394,0.0011201409,0.0043318616,0.01606723,0.00040920626,0.0051098056,0.000036317942],"about_ca_topic_score_codex":0.0040459516,"about_ca_topic_score_gemma":0.005120682,"teacher_disagreement_score":0.0040459516,"about_ca_system_score_codex":0.00036392178,"about_ca_system_score_gemma":0.00016142077,"threshold_uncertainty_score":0.008044839},"labels":[],"label_agreement":null},{"id":"W2155364327","doi":"10.1029/2006gl027687","title":"Denitrification in the Arctic winter 2004/2005: Observations from ACE‐FTS","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; York University","funders":"","keywords":"Denitrification; TRACER; Arctic; Atmospheric sciences; Environmental science; Polar vortex; Methane; Vortex; Stratosphere; The arctic; Polar; Breakup; Climatology; Nitrogen; Oceanography; Meteorology; Geology; Chemistry; Physics","score_opus":0.049849165352471726,"score_gpt":0.2821880424550288,"score_spread":0.2323388771025571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155364327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976695,0.00014556815,0.00028879588,0.00003458734,0.0000102537415,0.0000031607956,0.0010998367,0.00004634048,0.00070196646],"genre_scores_gemma":[0.99450606,0.00020499893,0.0012079894,0.00002972243,0.000020053114,0.0000064343844,0.003574984,0.000011278888,0.0004385746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998574,0.000015652291,0.000010830801,0.000027826,0.00005524496,0.000033097116],"domain_scores_gemma":[0.9997923,0.000019528203,0.000049979903,0.000012504369,0.00008214134,0.0000435937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040850745,0.00048593868,0.00038234657,0.0005548053,0.0005007171,0.0005786694,0.00021212915,0.0003742711,0.0001635726],"category_scores_gemma":[0.00032025127,0.00020013766,0.0002930212,0.0005446998,0.00015330783,0.00023979934,0.00025405127,0.00025567322,0.00008082716],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018789978,0.00036828022,0.87622523,0.00017340109,0.00059336744,0.00070940936,0.0010463774,0.02628478,0.062130023,0.0004981819,0.0041219853,0.025969958],"study_design_scores_gemma":[0.000028485,0.00010004082,0.9658563,0.000016632845,0.00008210258,0.0001425488,0.00017396439,0.016819725,0.013338765,0.00006369603,0.0033535266,0.000024124603],"about_ca_topic_score_codex":0.11027864,"about_ca_topic_score_gemma":0.11676119,"teacher_disagreement_score":0.11027864,"about_ca_system_score_codex":0.00090365857,"about_ca_system_score_gemma":0.00058715197,"threshold_uncertainty_score":0.21927351},"labels":[],"label_agreement":null},{"id":"W2155523560","doi":"10.1002/grl.50129","title":"Seasonal forecast skill of Arctic sea ice area in a dynamical forecast system","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":140,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"University of Toronto","keywords":"Forecast skill; Climatology; Lead (geology); Environmental science; Anomaly (physics); Sea ice; Lead time; Arctic; Arctic ice pack; Forecast period; Lag; Meteorology; Geology; Geography; Oceanography; Computer science","score_opus":0.021127958720921332,"score_gpt":0.24643608479314896,"score_spread":0.22530812607222764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155523560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9921416,0.00006455507,0.0059138136,0.00015909219,0.00002127347,0.000009125623,0.00063619216,0.00009526655,0.00095899537],"genre_scores_gemma":[0.9981743,0.000022397391,0.00094982475,0.0000101441865,0.000010437123,0.0000027129897,0.0007365063,0.000007045636,0.0000865818],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99953365,0.00013771858,0.0000539571,0.00013169643,0.00009238215,0.000050646595],"domain_scores_gemma":[0.99363434,0.00375046,0.0008043422,0.00045675927,0.001048004,0.00030599986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030518218,0.0003355566,0.00031865353,0.0006592809,0.00019610728,0.0008111699,0.00026597732,0.0003467078,0.0006955025],"category_scores_gemma":[0.013263038,0.00017760706,0.00036079224,0.00042969463,0.00023462233,0.00082654785,0.00045534456,0.00049679115,0.00013922379],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002821856,0.000066125234,0.42528474,0.00004065377,0.00033665306,0.00007892236,0.00011255245,0.55173784,0.00238491,0.0007392508,0.0009802101,0.017955959],"study_design_scores_gemma":[0.000020815727,0.00011897711,0.14265984,0.000014013977,0.000039583894,0.000026376283,0.00006417189,0.85438395,0.0014880659,0.00079989206,0.00035782,0.000026512847],"about_ca_topic_score_codex":0.024889577,"about_ca_topic_score_gemma":0.017813247,"teacher_disagreement_score":0.024889577,"about_ca_system_score_codex":0.0004381903,"about_ca_system_score_gemma":0.0007704855,"threshold_uncertainty_score":0.04948944},"labels":[],"label_agreement":null},{"id":"W2155612666","doi":"10.1002/2014gl061241","title":"Continental microseismic intensity delineates oceanic upwelling timing along the west coast of North America","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada; Fisheries and Oceans Canada","funders":"U.S. Navy; National Oceanic and Atmospheric Administration","keywords":"Upwelling; Downwelling; Oceanography; Microseism; Geology; Submarine pipeline; Continental shelf; Climatology; Wind stress; Climate change; Productivity; Seismology","score_opus":0.020936702881309527,"score_gpt":0.24708434491687778,"score_spread":0.22614764203556825,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155612666","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989963,0.000057645186,0.000040379302,0.000012496333,6.295225e-7,0.0000021815981,0.00018268953,0.0000037065383,0.0007040089],"genre_scores_gemma":[0.9994832,0.000055570377,0.00005425297,0.0000041469043,0.0000010859316,0.000002309337,0.00019358861,0.0000010733803,0.00020473609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993575,0.000006835854,0.0000057070943,0.00001805355,0.000014043998,0.000019602663],"domain_scores_gemma":[0.9995177,0.00005276398,0.00014630936,0.000017343915,0.00016849727,0.000097373864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011076158,0.00009976922,0.000084562154,0.0013434452,0.0003404391,0.00056061486,0.00014799854,0.00010398997,0.0010746139],"category_scores_gemma":[0.0005105016,0.00010355951,0.00006555916,0.0009387231,0.00023504751,0.00018011265,0.00032673497,0.0001135278,0.00010679149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003188029,0.000007203664,0.99248934,0.000008681732,0.000015285947,0.000030630043,0.00042435524,0.0000917625,0.002250865,0.00003457017,0.00012125467,0.0044942084],"study_design_scores_gemma":[1.9953119e-7,0.0000012901052,0.99979264,0.0000014918572,0.0000010159648,0.0000035178898,0.00010084029,0.000032373184,0.000019698029,0.000002132644,0.000044630622,3.085152e-7],"about_ca_topic_score_codex":0.37189242,"about_ca_topic_score_gemma":0.6884949,"teacher_disagreement_score":0.62810755,"about_ca_system_score_codex":0.0008411975,"about_ca_system_score_gemma":0.00060959853,"threshold_uncertainty_score":0.7394555},"labels":[],"label_agreement":null},{"id":"W2155930555","doi":"10.1002/2014gl061266","title":"Metabolic balance of coastal Antarctic waters revealed by autonomous <i>p</i>CO<sub>2</sub> and ΔO<sub>2</sub>/Ar measurements","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Phytoplankton; Environmental science; Primary production; Diel vertical migration; Autotroph; Oceanography; Biomass (ecology); Primary producers; Productivity; Bloom; Plankton; Polar night; Ecosystem; Spring bloom; Atmospheric sciences; Photosynthesis; Ecology; Nutrient; Arctic; Biology; Geology","score_opus":0.019607779110344625,"score_gpt":0.23893785796781492,"score_spread":0.2193300788574703,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155930555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990262,0.000024935784,0.00023515351,0.000011643036,0.0000017226936,0.0000021931407,0.00024580737,0.000014018248,0.00043841678],"genre_scores_gemma":[0.9989937,0.00003777675,0.0006116613,0.000014538921,0.0000032144765,0.000006264525,0.00023932838,0.000005512714,0.00008803811],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999503,0.000008856174,0.0000031619425,0.000016929896,0.000012969441,0.000007665402],"domain_scores_gemma":[0.99986124,0.00002820996,0.000050305953,0.000017358336,0.000023484099,0.000019347399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011825645,0.00022677185,0.00013592871,0.00034961305,0.00019302368,0.00035542843,0.0001645028,0.00020692636,0.00037924445],"category_scores_gemma":[0.00023987866,0.00019144337,0.00013277048,0.0004596287,0.000231,0.00021229626,0.00028346307,0.0002054899,0.00010684262],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005859378,0.000040293253,0.5186394,0.000055862845,0.000097120675,0.00020126156,0.00029509777,0.0016671849,0.4654521,0.00013528565,0.00019638769,0.01263405],"study_design_scores_gemma":[0.000009840501,0.000068829875,0.97401196,0.0000035190499,0.000024238641,0.00007940575,0.00014080072,0.004147611,0.021073077,0.000080148755,0.00034644114,0.00001402044],"about_ca_topic_score_codex":0.0036633275,"about_ca_topic_score_gemma":0.005112041,"teacher_disagreement_score":0.0036633275,"about_ca_system_score_codex":0.00017977928,"about_ca_system_score_gemma":0.00016235173,"threshold_uncertainty_score":0.007284045},"labels":[],"label_agreement":null},{"id":"W2155962616","doi":"10.1029/2005gl024370","title":"Precipitation controls Sahel greening trend","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":261,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Goddard Space Flight Center","keywords":"Greening; Environmental science; Vegetation (pathology); Precipitation; Carbon sink; Climatology; Ecosystem; Sink (geography); Forcing (mathematics); Global change; Climate change; Atmospheric sciences; Carbon cycle; Meteorology; Geography; Ecology; Geology","score_opus":0.04838908870483329,"score_gpt":0.3274768871281446,"score_spread":0.27908779842331133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2155962616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974821,0.00022740601,0.00037162204,0.00011545485,0.000009999254,0.000001611065,0.0002867007,0.000032833133,0.0014723863],"genre_scores_gemma":[0.9995933,0.000101610836,0.00006094944,0.000010799436,0.000008125793,8.587432e-7,0.00010984268,0.0000052119717,0.00010942665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.000019280878,0.0000045175793,0.000015728223,0.0000057900143,0.000016451015],"domain_scores_gemma":[0.99967825,0.00012600722,0.00009050695,0.000018446108,0.00004014977,0.00004670803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017436234,0.00014090794,0.00015717198,0.0003724118,0.00013655658,0.0005275672,0.00009590513,0.0001355138,0.0017830906],"category_scores_gemma":[0.00092447276,0.00008926111,0.00012311885,0.00034475475,0.00014724575,0.00025625137,0.00021494756,0.00012429751,0.00019925968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047218136,0.000048438917,0.9277255,0.000085033134,0.00027289733,0.00042930982,0.00040104362,0.014240195,0.023416284,0.0023291348,0.0014354023,0.029144648],"study_design_scores_gemma":[0.000024306872,0.00005205587,0.97344875,0.00001062617,0.00007026387,0.0001258851,0.00024583229,0.020306073,0.0017777439,0.0020274308,0.0019003142,0.000010659735],"about_ca_topic_score_codex":0.004749676,"about_ca_topic_score_gemma":0.0030303448,"teacher_disagreement_score":0.004749676,"about_ca_system_score_codex":0.0002079751,"about_ca_system_score_gemma":0.00015181385,"threshold_uncertainty_score":0.009444058},"labels":[],"label_agreement":null},{"id":"W2156019889","doi":"10.1002/2014gl059255","title":"Variability and trends in anticyclonic circulation over the Greenland ice sheet, 1948–2013","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Greenland ice sheet; Anticyclone; Climatology; Atmospheric circulation; Geology; Geopotential; Geopotential height; Ice sheet; Groenlandia; Atmospheric sciences; Environmental science; Precipitation; Oceanography; Meteorology; Geography","score_opus":0.032986373759677196,"score_gpt":0.28272675979061607,"score_spread":0.24974038603093887,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156019889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975127,0.00010498841,0.00004286575,0.00005611848,0.000006733996,0.0000022823447,0.0018362494,0.000009433065,0.00042868452],"genre_scores_gemma":[0.9969061,0.00009537577,0.00008282693,0.000027227963,0.00001520888,0.000005134302,0.0025400927,0.0000042490556,0.000323779],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999299,0.000006670862,0.0000067632723,0.000019266457,0.000015040248,0.000022323069],"domain_scores_gemma":[0.9996081,0.000034368863,0.00014708664,0.000026921329,0.000119050455,0.00006460025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024405334,0.00016400959,0.00012639584,0.0010865052,0.0002276577,0.00041103992,0.00017451854,0.00014049352,0.0008192866],"category_scores_gemma":[0.00047715814,0.00006807066,0.00020562357,0.0012740575,0.00026203363,0.0002604165,0.0003769473,0.00017092966,0.0001672161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007287595,0.000022051598,0.9886557,0.000018592591,0.000095784846,0.000057399182,0.00029753198,0.0006700346,0.0017973487,0.0000943191,0.0012767965,0.0069416002],"study_design_scores_gemma":[9.374773e-7,0.0000033954166,0.9993187,0.0000031840611,0.000003503466,0.000007745474,0.000052753378,0.00021807397,0.000045728186,0.000010217906,0.00033462874,0.0000011420403],"about_ca_topic_score_codex":0.109613314,"about_ca_topic_score_gemma":0.20866835,"teacher_disagreement_score":0.109613314,"about_ca_system_score_codex":0.0010674003,"about_ca_system_score_gemma":0.00050924555,"threshold_uncertainty_score":0.21795058},"labels":[],"label_agreement":null},{"id":"W2156087273","doi":"10.1029/2011gl047381","title":"Extreme melt on Canada's Arctic ice caps in the 21st century","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":105,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Campbell Scientific (Canada); Trent University; University of Alberta","funders":"","keywords":"Glacier; Snow; Glacier mass balance; Glacier ice accumulation; Climatology; Atmospheric sciences; Warm front; Environmental science; Precipitation; Cryosphere; Geology; Ice stream; Sea ice; Physical geography; Oceanography; Geography; Meteorology; Geomorphology","score_opus":0.08917003295926793,"score_gpt":0.26132276413123423,"score_spread":0.1721527311719663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156087273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.860217,0.0151049085,0.0003509927,0.0158911,0.0004723902,0.00002346048,0.013176325,0.0000593345,0.09470452],"genre_scores_gemma":[0.9844093,0.005325506,0.00014661164,0.0006563268,0.0001749428,0.0000044277435,0.0017541635,0.000018864008,0.0075100167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997396,0.000012612887,0.0000066360803,0.000021368254,0.00010320836,0.00011655878],"domain_scores_gemma":[0.9993868,0.000017443055,0.00012060653,0.000010895761,0.0003113316,0.00015300613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003191695,0.00017211883,0.00011833337,0.0010402412,0.0030849134,0.0016170555,0.00039292197,0.00046694177,0.0046140025],"category_scores_gemma":[0.00093828765,0.00011618371,0.00014782084,0.0015516209,0.00077491713,0.0005760989,0.0011438717,0.00059280737,0.00023111454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033018444,0.000048039332,0.7990397,0.00030449772,0.00010639833,0.0012099227,0.0072377888,0.0028550173,0.002116689,0.011026567,0.06774164,0.107983574],"study_design_scores_gemma":[0.000004611642,0.000010050069,0.91554475,0.00012951574,0.000014969491,0.00013235454,0.0022849794,0.00031596815,0.00027424708,0.0004048892,0.08086693,0.000016832624],"about_ca_topic_score_codex":0.9767641,"about_ca_topic_score_gemma":0.9925161,"teacher_disagreement_score":0.023235917,"about_ca_system_score_codex":0.01839298,"about_ca_system_score_gemma":0.015698558,"threshold_uncertainty_score":0.13345104},"labels":[],"label_agreement":null},{"id":"W2156214799","doi":"10.1029/2001gl014310","title":"Continental heat gain in the global climate system","year":2002,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":122,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"St. Francis Xavier University","funders":"","keywords":"Cryosphere; Lithosphere; Atmosphere (unit); Heat flux; Geology; Climatology; Climate model; Atmospheric sciences; Environmental science; Global warming; Flux (metallurgy); Climate change; Earth science; Geophysics; Heat transfer; Meteorology; Sea ice; Oceanography; Tectonics; Geography; Seismology; Materials science","score_opus":0.04058961897692358,"score_gpt":0.2923049767949353,"score_spread":0.2517153578180117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156214799","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9226402,0.0066804825,0.0021122894,0.0015145342,0.0001277114,0.0000172249,0.006493695,0.00017797721,0.060235854],"genre_scores_gemma":[0.9957337,0.0012994499,0.00035523903,0.000059910122,0.00003710451,0.000007778878,0.0009265859,0.000018990118,0.0015611814],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998754,0.000028578143,0.000008509912,0.000024895082,0.000037211477,0.00002539544],"domain_scores_gemma":[0.99987316,0.000024721887,0.000020070673,0.000019051087,0.000050384097,0.000012605553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002104199,0.0002558388,0.0001498887,0.0007995687,0.00025159112,0.0010190202,0.00015528237,0.00024503635,0.0034346944],"category_scores_gemma":[0.0010870808,0.00011834951,0.00025170317,0.0017582473,0.00027430686,0.00090187846,0.00074647955,0.00033939397,0.0004794494],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035026914,0.00006184994,0.5490875,0.00047784063,0.001040097,0.00041971207,0.0010782692,0.22098206,0.0068623694,0.055829212,0.010727357,0.1530834],"study_design_scores_gemma":[0.00003256731,0.000058833433,0.8766918,0.000117857046,0.00017933115,0.00033645701,0.0007090774,0.029604163,0.0023634643,0.021309827,0.06854166,0.000054933793],"about_ca_topic_score_codex":0.013783226,"about_ca_topic_score_gemma":0.01206775,"teacher_disagreement_score":0.013783226,"about_ca_system_score_codex":0.0010767207,"about_ca_system_score_gemma":0.0003715609,"threshold_uncertainty_score":0.027405977},"labels":[],"label_agreement":null},{"id":"W2156312801","doi":"10.1002/grl.50575","title":"Diurnal variations of land surface wind speed probability distributions under clear‐sky and low‐cloud conditions","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Environmental science; Wind speed; Ceilometer; Atmospheric sciences; Thermal wind; Geostrophic wind; Atmosphere (unit); Wind shear; Skewness; Probability density function; Meteorology; Lidar; Maximum sustained wind; Daytime; Planetary boundary layer; Wind gradient; Climatology; Geology; Physics; Remote sensing; Mathematics; Turbulence","score_opus":0.03870718838678544,"score_gpt":0.3015597428694135,"score_spread":0.26285255448262806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156312801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99847645,0.00004663676,0.00021857073,0.000009316816,0.0000017842029,0.0000031085078,0.00074378814,0.00001786983,0.0004824822],"genre_scores_gemma":[0.99859375,0.00002167058,0.00008952001,0.0000018791156,0.0000019617216,0.0000034297645,0.0011725746,0.000004112822,0.000111187925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999162,0.000011910196,0.000006680416,0.0000245314,0.000016738617,0.000023977072],"domain_scores_gemma":[0.99947935,0.00019176488,0.000116843374,0.000042028205,0.00009006183,0.00007997],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018223052,0.0000949655,0.00015228693,0.0003738628,0.00012755468,0.00029531843,0.00013633892,0.000115853145,0.00068311003],"category_scores_gemma":[0.00066629454,0.0000918596,0.00012425083,0.00033932703,0.00015370596,0.00021365643,0.0001431475,0.000111097004,0.0001771026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044035027,0.0000629185,0.9261521,0.00009261678,0.00012164196,0.00028970596,0.0006840527,0.009247223,0.04356164,0.00021984037,0.0009847457,0.01814319],"study_design_scores_gemma":[0.000004328273,0.000016491931,0.9958448,0.0000021074347,0.0000059951076,0.00003563586,0.00006055329,0.0032451556,0.00060167693,0.00002799292,0.00014979581,0.000005543648],"about_ca_topic_score_codex":0.008366762,"about_ca_topic_score_gemma":0.015421736,"teacher_disagreement_score":0.008366762,"about_ca_system_score_codex":0.00016473667,"about_ca_system_score_gemma":0.00011767265,"threshold_uncertainty_score":0.016636133},"labels":[],"label_agreement":null},{"id":"W2156401148","doi":"10.1029/2009gl038706","title":"Links between fluid circulation, temperature, and metamorphism in subducting slabs","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Eclogite; Subduction; Crust; Eclogitization; Slab; Oceanic crust; Lithosphere; Petrology; Metamorphism; Underplating; Fluid dynamics; Geophysics; Metamorphic rock; Seismology; Tectonics; Mechanics","score_opus":0.03688265034562253,"score_gpt":0.27442685014087076,"score_spread":0.23754419979524824,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156401148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99973243,0.000062320054,0.00006158502,0.0000132640125,4.3680188e-7,8.955945e-7,0.00004108641,0.0000032411501,0.00008467512],"genre_scores_gemma":[0.99978155,0.000031737447,0.00006689197,0.000003233714,0.000001029841,0.0000010971468,0.00005586459,0.0000014326123,0.000057035566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.000017886436,0.0000056819963,0.000014501268,0.00000775137,0.000016031583],"domain_scores_gemma":[0.9996062,0.00010045141,0.00016242873,0.000019097764,0.000049763967,0.00006210353],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017742833,0.00013825764,0.00016356044,0.00057387585,0.00019063568,0.0004816908,0.00014962268,0.00018988481,0.00077027996],"category_scores_gemma":[0.00095195597,0.000222968,0.0001418358,0.00041460138,0.00037486298,0.00032436597,0.00035142837,0.0002342095,0.0000887093],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004746806,0.00005828482,0.97397083,0.000015060592,0.00008727869,0.000110105764,0.0002789548,0.0015473837,0.019210583,0.00018266548,0.000044083085,0.004020036],"study_design_scores_gemma":[0.0000060795855,0.0000329051,0.9978236,0.000001878881,0.000011714852,0.000038714967,0.000083468156,0.0012356689,0.0005496732,0.00016422609,0.000048366626,0.000003608289],"about_ca_topic_score_codex":0.010935899,"about_ca_topic_score_gemma":0.010913151,"teacher_disagreement_score":0.010935899,"about_ca_system_score_codex":0.00041885814,"about_ca_system_score_gemma":0.00027401332,"threshold_uncertainty_score":0.02174449},"labels":[],"label_agreement":null},{"id":"W2156572528","doi":"10.1029/2007gl033054","title":"How does the northern‐winter wave driving of the Brewer‐Dobson circulation increase in an enhanced‐CO<sub>2</sub> climate simulation?","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Troposphere; Stratosphere; Extratropical cyclone; Atmospheric sciences; Environmental science; Climatology; Flux (metallurgy); Heat flux; Climate model; Middle latitudes; Greenhouse gas; Atmospheric circulation; Climate change; Geology; Heat transfer; Materials science; Physics; Mechanics; Oceanography","score_opus":0.01575193165952638,"score_gpt":0.25633809986794914,"score_spread":0.24058616820842277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156572528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99347526,0.000087105145,0.00079221884,0.0009429272,0.000040513838,0.000017499473,0.00033922013,0.00005234786,0.004252845],"genre_scores_gemma":[0.9988813,0.00006177707,0.00038436547,0.00008239131,0.0000117426025,0.000005566505,0.000114561386,0.000019278583,0.0004390814],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984515,0.00006552436,0.0000075477756,0.00002728283,0.000013303489,0.000041210384],"domain_scores_gemma":[0.9995524,0.00021688269,0.00007113884,0.000034158806,0.00005061177,0.000074784795],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005923386,0.0003523889,0.00035068358,0.00019996389,0.0003862296,0.0011724031,0.00038152953,0.0011445666,0.0020320176],"category_scores_gemma":[0.0023002864,0.00031449043,0.0005033056,0.00023997066,0.00043180783,0.0008434537,0.0003531153,0.0004913363,0.00017457046],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004738766,0.00017852757,0.10957925,0.00009210676,0.00018335252,0.00039308102,0.00018337595,0.8681395,0.009082024,0.0047500166,0.0017394392,0.005205598],"study_design_scores_gemma":[0.00019253574,0.000071792376,0.036950827,0.000013778681,0.000054534314,0.000036650195,0.00017250926,0.95904607,0.001265969,0.0012396309,0.00093009823,0.00002572037],"about_ca_topic_score_codex":0.069870375,"about_ca_topic_score_gemma":0.057363205,"teacher_disagreement_score":0.069870375,"about_ca_system_score_codex":0.0009106337,"about_ca_system_score_gemma":0.00075406465,"threshold_uncertainty_score":0.1389274},"labels":[],"label_agreement":null},{"id":"W2156844335","doi":"10.1029/2004gl022305","title":"A simple method to improve ensemble‐based ozone forecasts","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Science; National Oceanic and Atmospheric Administration","keywords":"Ozone; Ensemble forecasting; Ensemble average; Mean squared error; Environmental science; Statistics; Meteorology; Ensemble learning; Mean square; Simple (philosophy); Mathematics; Computer science; Climatology; Geography; Machine learning; Geology","score_opus":0.02271086886443073,"score_gpt":0.31552554973911284,"score_spread":0.2928146808746821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2156844335","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.040583346,0.00021936961,0.9536752,0.00011831924,0.00026129137,0.00012743923,0.00032536275,0.0031495537,0.0015401365],"genre_scores_gemma":[0.20594361,0.00016118448,0.7895756,0.00008550872,0.00022875245,0.00028121128,0.0008526073,0.0003506715,0.002520877],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99894494,0.00023953979,0.00006172083,0.00017741225,0.00051515317,0.00006131782],"domain_scores_gemma":[0.99768543,0.0007690102,0.00017831093,0.00041587072,0.000879797,0.00007160786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014093388,0.0010265914,0.0008626148,0.0016002404,0.0004382467,0.0005248977,0.000857011,0.00057456765,0.002794099],"category_scores_gemma":[0.0073379516,0.0005068117,0.0008979748,0.0010849735,0.00017739077,0.00084130286,0.0011797004,0.0009873873,0.0010182676],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017291463,0.00014019047,0.0036218483,0.000117677795,0.00034041298,0.00010025691,0.00010950435,0.17944708,0.026159765,0.0025772094,0.009004404,0.7782088],"study_design_scores_gemma":[0.000073717616,0.00011157246,0.0033886777,0.000012639795,0.00009195932,0.000067870606,0.000011579829,0.9773303,0.0092974305,0.0026109142,0.0069601675,0.00004317728],"about_ca_topic_score_codex":0.003727928,"about_ca_topic_score_gemma":0.0063875006,"teacher_disagreement_score":0.003727928,"about_ca_system_score_codex":0.0002983069,"about_ca_system_score_gemma":0.0006436577,"threshold_uncertainty_score":0.009347141},"labels":[],"label_agreement":null},{"id":"W2157398194","doi":"10.1029/2009gl040948","title":"Surface‐melt driven Laurentide Ice Sheet retreat during the early Holocene","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"University of Wisconsin-Madison; Goddard Institute for Space Studies; National Science Foundation","keywords":"Ice sheet; Greenland ice sheet; Geology; Holocene; Ice-sheet model; Ice stream; Climatology; Glacier mass balance; Insolation; Cryosphere; Oceanography; Glacier; Sea ice; Geomorphology","score_opus":0.03298157140233405,"score_gpt":0.27441312147008695,"score_spread":0.2414315500677529,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157398194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993048,0.000021780521,0.00008840507,0.000039768624,0.0000012853712,0.0000010454769,0.000072404466,0.000009390871,0.0004611383],"genre_scores_gemma":[0.9996482,0.000020985337,0.00008891257,0.000007650849,0.0000014599894,0.0000016340723,0.00009344779,0.0000032031012,0.00013453583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995077,0.000008675314,0.0000034249465,0.000012751898,0.000009448216,0.00001490936],"domain_scores_gemma":[0.99988484,0.000019873316,0.000032049,0.000009213472,0.00002157261,0.000032394575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023948286,0.00021000279,0.00021497175,0.00024952117,0.00038286284,0.00050806836,0.0002929617,0.00024348346,0.0007798453],"category_scores_gemma":[0.00060079404,0.0001543444,0.0002426723,0.00016075246,0.00027693834,0.00033240518,0.00037276864,0.00023451228,0.000106042906],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044327622,0.000090939226,0.85959667,0.00006452636,0.00010029211,0.0008081105,0.00078664464,0.089427665,0.035273224,0.0013704217,0.00061027956,0.011427905],"study_design_scores_gemma":[0.000057661473,0.00011854836,0.8332223,0.000020914815,0.000040728315,0.00017509806,0.00039739624,0.1587924,0.0053645526,0.00045436216,0.0013289847,0.000027063408],"about_ca_topic_score_codex":0.039788164,"about_ca_topic_score_gemma":0.07522966,"teacher_disagreement_score":0.039788164,"about_ca_system_score_codex":0.0010956968,"about_ca_system_score_gemma":0.00059145206,"threshold_uncertainty_score":0.079113126},"labels":[],"label_agreement":null},{"id":"W2157609843","doi":"10.1029/2003gl017139","title":"Properties of high heliolatitude solar energetic particle events and constraints on models of acceleration and propagation","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Ecliptic; Physics; Coronal mass ejection; Solar wind; Heliosphere; Interplanetary spaceflight; Solar energetic particles; Particle acceleration; Astrophysics; Flare; Solar flare; Acceleration; Solar maximum; Astronomy; Computational physics; Plasma; Nuclear physics; Classical mechanics","score_opus":0.036597793702039756,"score_gpt":0.27372349449004746,"score_spread":0.2371257007880077,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157609843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985783,0.00005927799,0.00057752023,0.000011956175,8.0627285e-7,0.0000022872352,0.00011180814,0.000022923683,0.00063508213],"genre_scores_gemma":[0.9995425,0.00003573255,0.00013038752,0.0000011334433,0.000002559902,0.0000012307014,0.00022233625,0.000004827111,0.000059503185],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994993,0.00001157283,0.0000047922294,0.0000099518475,0.000011320151,0.000012406614],"domain_scores_gemma":[0.99890065,0.00055581704,0.0003436523,0.00006388074,0.00005976066,0.000076171265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028828936,0.000246868,0.00016240329,0.00067164033,0.00016544788,0.0005746432,0.00014309958,0.00019781908,0.0010054316],"category_scores_gemma":[0.0016036921,0.00019494227,0.00018260795,0.00055937335,0.00020548284,0.0002996552,0.00020028732,0.00016501335,0.00016272416],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041945445,0.000035192188,0.92765963,0.000053584565,0.00007953556,0.0006552279,0.00042810454,0.036428176,0.02179821,0.0022417537,0.00027485535,0.009926447],"study_design_scores_gemma":[0.000030408895,0.00010833897,0.9144085,0.0000109736475,0.000037178073,0.0006538713,0.00014320848,0.07904726,0.0037149424,0.001148907,0.0006829925,0.000013404148],"about_ca_topic_score_codex":0.0024324583,"about_ca_topic_score_gemma":0.0020515928,"teacher_disagreement_score":0.0024324583,"about_ca_system_score_codex":0.00025808858,"about_ca_system_score_gemma":0.00007606548,"threshold_uncertainty_score":0.004836619},"labels":[],"label_agreement":null},{"id":"W2157688053","doi":"10.1029/2005gl023596","title":"Mid‐Holocene NAO: A PMIP2 model intercomparison","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Met Office","keywords":"Holocene; North Atlantic oscillation; Climatology; Paleoclimatology; Geology; Proxy (statistics); Environmental science; Oceanography; Climate change","score_opus":0.06143796603787125,"score_gpt":0.32895546458715397,"score_spread":0.2675174985492827,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2157688053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98253655,0.00017608138,0.0034706327,0.0005295069,0.00007947191,0.000030644176,0.007498858,0.0005635743,0.0051146983],"genre_scores_gemma":[0.98782545,0.00009199898,0.003820891,0.00008857696,0.000029937195,0.00006670523,0.0074114357,0.00012486447,0.0005401679],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978775,0.0000713304,0.000010930697,0.000081324564,0.000022973982,0.000025679728],"domain_scores_gemma":[0.9997013,0.00008704311,0.00002929375,0.000069794914,0.0000707055,0.000041850417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011620478,0.0006933424,0.0004881139,0.00038935267,0.0006279474,0.0008078957,0.0011897751,0.00079833955,0.0014564561],"category_scores_gemma":[0.0014898451,0.00038898966,0.0007604416,0.00084076676,0.00018361694,0.000778066,0.00057836616,0.0006175961,0.00036148445],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014993204,0.00029265703,0.22638169,0.00013603672,0.0015723308,0.00041392643,0.00058121124,0.70742995,0.0066655106,0.002516262,0.01658266,0.03592847],"study_design_scores_gemma":[0.00082225667,0.00016920126,0.16234311,0.000029187257,0.00037868196,0.000149716,0.0002529265,0.8193034,0.004220981,0.0023620923,0.009872185,0.000096310556],"about_ca_topic_score_codex":0.032948073,"about_ca_topic_score_gemma":0.025462337,"teacher_disagreement_score":0.032948073,"about_ca_system_score_codex":0.0007648249,"about_ca_system_score_gemma":0.00078186556,"threshold_uncertainty_score":0.0655126},"labels":[],"label_agreement":null},{"id":"W2158162619","doi":"10.1029/2010gl044056","title":"What causes the irregular cycle of the atmospheric tape recorder signal in HCN?","year":2010,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Stratosphere; Microwave Limb Sounder; Environmental science; Atmospheric sciences; SIGNAL (programming language); Annual cycle; Water vapor; Mixing ratio; Meteorology; Climatology; Geology; Physics","score_opus":0.01778980567020363,"score_gpt":0.2679212516105871,"score_spread":0.2501314459403835,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158162619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956163,0.00013624132,0.002483221,0.00028769954,0.000025736408,0.000017862163,0.00024984166,0.00008958627,0.001093499],"genre_scores_gemma":[0.9992366,0.00005373656,0.00043178312,0.000022895869,0.000010041556,0.0000035653663,0.00010663131,0.0000168974,0.00011794403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990046,0.000017674065,0.000005850162,0.000035679444,0.000015453554,0.000024885356],"domain_scores_gemma":[0.9996227,0.00011333431,0.000118672,0.000035735826,0.0000539333,0.000055577657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004312001,0.00026305465,0.00031352497,0.00028966664,0.00032516386,0.00058887474,0.0004413785,0.00068535516,0.0011331652],"category_scores_gemma":[0.0018244132,0.0002500277,0.0004984368,0.00033771017,0.0003671602,0.0005259652,0.00024160015,0.0003303341,0.00012986937],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005557789,0.00020817216,0.7466221,0.0002169842,0.0002883398,0.0015812968,0.0004236821,0.1727121,0.05075199,0.0038201422,0.0022817529,0.020537712],"study_design_scores_gemma":[0.00008749925,0.00010739153,0.3828373,0.000024203859,0.000095225776,0.00030650763,0.00029773026,0.60579437,0.007319773,0.0018610167,0.0012282588,0.00004074043],"about_ca_topic_score_codex":0.0125648,"about_ca_topic_score_gemma":0.008251068,"teacher_disagreement_score":0.0125648,"about_ca_system_score_codex":0.0005422064,"about_ca_system_score_gemma":0.000358914,"threshold_uncertainty_score":0.024983346},"labels":[],"label_agreement":null},{"id":"W2158261139","doi":"10.1029/2008gl036935","title":"Impact of the assimilation of ozone from the Tropospheric Emission Spectrometer on surface ozone across North America","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":108,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Canadian Foundation for Climate and Atmospheric Sciences; National Oceanic and Atmospheric Administration; Harvard University; National Aeronautics and Space Administration","keywords":"Ozone; Troposphere; Tropospheric ozone; Atmospheric sciences; Environmental science; Total Ozone Mapping Spectrometer; Climatology; Planetary boundary layer; Boundary layer; Ozone layer; Flux (metallurgy); Meteorology; Geology; Chemistry; Geography; Physics","score_opus":0.024873957122856543,"score_gpt":0.30312125397976003,"score_spread":0.27824729685690347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158261139","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99868697,0.00007404303,0.00022699579,0.0002059874,0.00002245733,0.0000051897305,0.00023173838,0.000039128532,0.0005075103],"genre_scores_gemma":[0.9984068,0.00006865699,0.000510871,0.000092276336,0.0000065566114,0.0000060074026,0.0006665452,0.000014754416,0.00022740093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995546,0.00014217918,0.000036139503,0.00013407084,0.000058779435,0.00007432749],"domain_scores_gemma":[0.99895644,0.0003599423,0.0001639042,0.00013520208,0.0002611562,0.00012338994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012347779,0.0007876171,0.00052415853,0.00019317117,0.0006173027,0.0010326265,0.0005680957,0.0006888338,0.00065737515],"category_scores_gemma":[0.0030710835,0.00047095347,0.00078454893,0.0002707679,0.00040948723,0.0007515014,0.0008616844,0.00062639866,0.00011314037],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018854314,0.0006164218,0.5305071,0.00009436354,0.0015356658,0.00047689702,0.0003217542,0.4036597,0.041684367,0.0006964075,0.0018823942,0.016639503],"study_design_scores_gemma":[0.0003922832,0.000502632,0.59306234,0.000035779925,0.0005945139,0.000068318615,0.0003922475,0.38684735,0.01573684,0.00044860604,0.0018289349,0.000090189176],"about_ca_topic_score_codex":0.22100824,"about_ca_topic_score_gemma":0.17083775,"teacher_disagreement_score":0.77899176,"about_ca_system_score_codex":0.0013950133,"about_ca_system_score_gemma":0.0018192347,"threshold_uncertainty_score":0.43944365},"labels":[],"label_agreement":null},{"id":"W2158581587","doi":"10.1002/2015gl066592","title":"On the dependence of storm time ULF wave power on magnetopause location: Impacts for ULF wave radial diffusion","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; University of Alberta; National Aeronautics and Space Administration","keywords":"Magnetopause; Magnetosphere; Physics; Van Allen radiation belt; Geophysics; Van Allen Probes; Wave power; Geomagnetic storm; Solar wind; Ring current; Plasmasphere; Amplitude; Computational physics; Ultra low frequency; Alfvén wave; Magnetohydrodynamics; Plasma; Power (physics); Astronomy","score_opus":0.03080865151538404,"score_gpt":0.2836769156025575,"score_spread":0.25286826408717344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2158581587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99804795,0.00008975772,0.00038712096,0.0000729492,0.0000026814828,0.0000028763338,0.00017530555,0.000010131795,0.0012111505],"genre_scores_gemma":[0.99975616,0.000023112028,0.000038330283,0.0000050320937,0.0000022896188,8.425351e-7,0.000059777114,0.0000039644915,0.000110616886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999049,0.000021144446,0.0000053914555,0.000022620647,0.000016159618,0.000029821973],"domain_scores_gemma":[0.9971623,0.0020921547,0.000342926,0.00011842338,0.00015588921,0.00012836311],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035947384,0.00014353948,0.0001601874,0.00026095883,0.00015870536,0.00051024434,0.00024861522,0.00026429983,0.0027146705],"category_scores_gemma":[0.0032799277,0.00010658131,0.00019602259,0.00023643523,0.00022741276,0.00048478896,0.0002534184,0.00028986332,0.00023793342],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016493323,0.00017375381,0.86794406,0.000099355304,0.00015080784,0.0008122538,0.00028778764,0.01616328,0.09169579,0.0013138322,0.00078937743,0.018920485],"study_design_scores_gemma":[0.000021881107,0.000096383716,0.9698556,0.000009717352,0.00003734977,0.0001582131,0.00017918403,0.024285862,0.004796218,0.00025459903,0.00029411344,0.000010861663],"about_ca_topic_score_codex":0.0034066378,"about_ca_topic_score_gemma":0.0019140972,"teacher_disagreement_score":0.0034066378,"about_ca_system_score_codex":0.00020517662,"about_ca_system_score_gemma":0.000108379354,"threshold_uncertainty_score":0.009081483},"labels":[],"label_agreement":null},{"id":"W2159225273","doi":"10.1029/2006gl027511","title":"Mass balance of glaciers and ice caps: Consensus estimates for 1961–2004","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":492,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University","funders":"","keywords":"Glacier; Balance (ability); Ice caps; Ice sheet; Physical geography; Geology; Climatology; Glacier mass balance; Sea level rise; Environmental science; Geography; Oceanography; Climate change; Medicine","score_opus":0.03377188071368704,"score_gpt":0.2857052510563226,"score_spread":0.2519333703426356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159225273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6457015,0.042744365,0.019655382,0.0021947222,0.00089278916,0.00022514154,0.21896024,0.0011446455,0.06848123],"genre_scores_gemma":[0.7697914,0.012912644,0.02187908,0.0005847694,0.00027203042,0.00015872662,0.18848634,0.0003430997,0.005571967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889416,0.00011701531,0.00022962852,0.00032167538,0.00035128658,0.000086351814],"domain_scores_gemma":[0.99475753,0.00033493398,0.001178637,0.0005240271,0.0030063447,0.00019856222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025713756,0.0009345877,0.0006897808,0.0072931536,0.0004445755,0.00081677665,0.0012161382,0.00042274155,0.0017970187],"category_scores_gemma":[0.0036033206,0.00037107946,0.0009971661,0.0056919674,0.00026195197,0.00094300124,0.0014326813,0.00043242183,0.0011336948],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043836364,0.000080034115,0.7418597,0.0023604594,0.0022691896,0.00020038211,0.0011559504,0.012603778,0.003336433,0.0014458691,0.04743728,0.18681252],"study_design_scores_gemma":[0.000026038088,0.000027036622,0.9320163,0.00040817112,0.0003247904,0.00010716529,0.00041485857,0.001690994,0.0018892344,0.00034966227,0.0626969,0.000048845446],"about_ca_topic_score_codex":0.059228424,"about_ca_topic_score_gemma":0.077728644,"teacher_disagreement_score":0.059228424,"about_ca_system_score_codex":0.0020350078,"about_ca_system_score_gemma":0.0012498433,"threshold_uncertainty_score":0.117767334},"labels":[],"label_agreement":null},{"id":"W2159474914","doi":"10.1029/2004gl020547","title":"Verification of mesoscale modeling for the severe rainfall event over southern Ontario in May 2000","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"MEG-3 (Canada)","funders":"","keywords":"Mesoscale meteorology; Precipitation; Environmental science; Climatology; Rain gauge; Streamflow; Flood myth; Atmospheric model; Meteorology; Atmospheric sciences; Geology; Drainage basin; Geography","score_opus":0.06565145077412748,"score_gpt":0.3022867112368617,"score_spread":0.2366352604627342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159474914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974624,0.000022877266,0.00052014366,0.00006202806,0.0000049275664,0.000015049405,0.00042351751,0.00009180083,0.0013972694],"genre_scores_gemma":[0.9992219,0.000010805043,0.00029159556,0.0000047624712,0.0000013213621,0.0000045689076,0.00027321695,0.000004173533,0.00018763283],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998518,0.000021329079,0.000008785567,0.00003394726,0.000037872927,0.00004619135],"domain_scores_gemma":[0.9996325,0.00007971816,0.00006507343,0.00004101254,0.00012221078,0.000059472688],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027771754,0.0004403785,0.0002625025,0.00018442425,0.00073589187,0.00053853175,0.0009219096,0.00043746346,0.0007974154],"category_scores_gemma":[0.0010493351,0.0002878115,0.00031657482,0.00029098557,0.0004471528,0.00028060342,0.00037051886,0.0002979968,0.00009756373],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023290381,0.000084337444,0.11918601,0.00003763407,0.000071793314,0.00039061485,0.00021932913,0.86921483,0.0042433827,0.0005862199,0.000809582,0.0049233614],"study_design_scores_gemma":[0.00008743452,0.00005813962,0.062391993,0.000004991473,0.000023229102,0.000021316895,0.0001320144,0.9349019,0.00147271,0.0001376143,0.0007544969,0.000014164149],"about_ca_topic_score_codex":0.82785064,"about_ca_topic_score_gemma":0.83022857,"teacher_disagreement_score":0.17214936,"about_ca_system_score_codex":0.0057141506,"about_ca_system_score_gemma":0.00451807,"threshold_uncertainty_score":0.34632635},"labels":[],"label_agreement":null},{"id":"W2159804391","doi":"10.1002/2013gl058121","title":"Arctic Ocean basin liquid freshwater storage trend 1992–2012","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":219,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Sixth Framework Programme","keywords":"Arctic; Oceanography; Arctic dipole anomaly; Arctic sea ice decline; Sea ice; Climatology; Canada Basin; Arctic ice pack; Salinity; Environmental science; Geology; Ocean current; Arctic geoengineering; Drift ice","score_opus":0.019211629963145894,"score_gpt":0.25334041325334583,"score_spread":0.23412878329019993,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159804391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92986387,0.0006593862,0.00034618677,0.00028596047,0.000051826373,0.000008154261,0.06345909,0.00021538216,0.005110109],"genre_scores_gemma":[0.948286,0.0005146218,0.0005220568,0.000076284006,0.000043039716,0.000020086498,0.04824694,0.00002994381,0.0022609653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999002,0.000008371206,0.000015549971,0.000029114794,0.000026378286,0.000020426056],"domain_scores_gemma":[0.9995301,0.000023416353,0.00012706331,0.00002357587,0.00026301577,0.000032946762],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022119316,0.0002916819,0.00022820839,0.0012000679,0.00029094506,0.0005478525,0.0001645351,0.00016613539,0.0011593578],"category_scores_gemma":[0.0005593144,0.00014193551,0.00024240844,0.0018480881,0.000118600095,0.00032584034,0.00029241532,0.00018896637,0.00058941945],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012049415,0.00006795397,0.8831812,0.00050049764,0.00057361,0.0002987045,0.0004670401,0.012589987,0.011178966,0.00097075506,0.025318956,0.0636473],"study_design_scores_gemma":[0.000017983988,0.000038266266,0.97692686,0.000037896345,0.000064022366,0.000094472845,0.00008563642,0.00313199,0.0013503804,0.000092716466,0.018144082,0.000015773083],"about_ca_topic_score_codex":0.12114829,"about_ca_topic_score_gemma":0.13190806,"teacher_disagreement_score":0.12114829,"about_ca_system_score_codex":0.0012422174,"about_ca_system_score_gemma":0.0008333117,"threshold_uncertainty_score":0.24088627},"labels":[],"label_agreement":null},{"id":"W2159841501","doi":"10.1002/2013gl058951","title":"Changes in Arctic melt season and implications for sea ice loss","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":777,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration; National Science Foundation","keywords":"Beaufort sea; Arctic; Sea ice; Arctic ice pack; Beaufort scale; Arctic sea ice decline; Environmental science; Climatology; Canada Basin; Oceanography; Geology; Atmospheric sciences; The arctic; Antarctic sea ice","score_opus":0.028686678752968656,"score_gpt":0.29291101418100274,"score_spread":0.2642243354280341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159841501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897621,0.0025164122,0.00014533318,0.0014409455,0.00014280653,0.0000054781717,0.0019946187,0.000025195217,0.003967104],"genre_scores_gemma":[0.99801767,0.00080726633,0.00005785962,0.000116405085,0.00011094229,0.0000023315936,0.0005355962,0.0000058082833,0.00034625156],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998222,0.00004126851,0.000022807508,0.000030889616,0.000031303967,0.00005152074],"domain_scores_gemma":[0.99916375,0.00010305914,0.00033187727,0.000030838553,0.00020572993,0.00016485789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007641857,0.00019931897,0.00021119455,0.0009548672,0.0005969213,0.0017619402,0.00025377286,0.0003865053,0.002678139],"category_scores_gemma":[0.0017556254,0.00009336959,0.00037057116,0.0009866905,0.0002944539,0.0006525767,0.00046634834,0.00036575837,0.00028170377],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004379562,0.000055583478,0.9745694,0.00007039865,0.00010695172,0.00024352649,0.00024349887,0.0014523005,0.0014595087,0.0003403888,0.0014585361,0.019561933],"study_design_scores_gemma":[0.0000036838358,0.000029560015,0.99666554,0.000027447297,0.000017302376,0.000060472026,0.00040629733,0.0007529473,0.00020961578,0.00016528847,0.0016574354,0.0000044009043],"about_ca_topic_score_codex":0.03493067,"about_ca_topic_score_gemma":0.028087262,"teacher_disagreement_score":0.03493067,"about_ca_system_score_codex":0.001012861,"about_ca_system_score_gemma":0.0008109033,"threshold_uncertainty_score":0.06945473},"labels":[],"label_agreement":null},{"id":"W2159918304","doi":"10.1029/2004gl019561","title":"The dominant influence of the Icelandic Low on the position of the Gulf Stream northwall","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Icelandic; North Atlantic oscillation; Oceanography; Lag; Gulf Stream; Rossby wave; Climatology","score_opus":0.010372873104767099,"score_gpt":0.23297169883570043,"score_spread":0.22259882573093334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2159918304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882196,0.00028124487,0.00017350705,0.00013715724,0.00003144611,0.0000042634215,0.00042115944,0.000011026892,0.010720609],"genre_scores_gemma":[0.9976235,0.00016805001,0.00007190567,0.000030126663,0.000021009186,0.000001512787,0.00030306724,0.0000053875897,0.001775431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.000018802944,0.000008000806,0.00003074244,0.000025125202,0.000032196178],"domain_scores_gemma":[0.999292,0.0001386829,0.0002207978,0.000037063684,0.00013932504,0.00017206528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015887887,0.00021736819,0.00024104425,0.00044860414,0.00036992997,0.0007101708,0.00009747437,0.00009983526,0.0028056032],"category_scores_gemma":[0.0007508422,0.000074926065,0.00015954548,0.00033156172,0.00031867938,0.00017338866,0.0004076697,0.00020370142,0.00033929385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026014782,0.000029194964,0.94912124,0.000042431693,0.00008346102,0.0003206606,0.00018519463,0.0012032099,0.017118495,0.0007512395,0.0016749932,0.029209761],"study_design_scores_gemma":[0.0000016382028,0.000016360227,0.99812704,0.000007639446,0.000016521673,0.000038992788,0.00010176384,0.00022267856,0.0005114042,0.000040538584,0.00091298367,0.0000024190851],"about_ca_topic_score_codex":0.020654373,"about_ca_topic_score_gemma":0.038985707,"teacher_disagreement_score":0.020654373,"about_ca_system_score_codex":0.0004013982,"about_ca_system_score_gemma":0.00065282895,"threshold_uncertainty_score":0.041068316},"labels":[],"label_agreement":null},{"id":"W2160037192","doi":"10.1002/2015gl063858","title":"Deep source model for Nevado del Ruiz Volcano, Colombia, constrained by interferometric synthetic aperture radar observations","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Tectonic Studies in Latin America","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Canadian Space Agency; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Geology; Volcano; Sill; Seismology; Interferometric synthetic aperture radar; Context (archaeology); Dike; Synthetic aperture radar; Petrology; Paleontology; Remote sensing","score_opus":0.08270342546863639,"score_gpt":0.289831403133416,"score_spread":0.20712797766477958,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160037192","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9713577,0.00069721445,0.01096398,0.00047503106,0.000034797315,0.000053460317,0.0035064714,0.00047053178,0.012440735],"genre_scores_gemma":[0.9978538,0.000072136114,0.00086797815,0.000011637593,0.000006336972,0.000012552484,0.0005198007,0.00001878362,0.0006368777],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99994934,0.0000069498515,0.0000023737864,0.000018565559,0.000006602497,0.000016228136],"domain_scores_gemma":[0.99986243,0.000039885876,0.000028454197,0.000010581533,0.000029167079,0.000029420773],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012131379,0.00063896,0.0003223065,0.0006828952,0.00040796204,0.0009650205,0.00077369856,0.0007466649,0.0020455567],"category_scores_gemma":[0.0005878298,0.0003054485,0.0002977299,0.00029601215,0.00029395436,0.00045008812,0.00035576135,0.00028369424,0.00021490412],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018263409,0.000050938677,0.051861543,0.000060449478,0.000056867026,0.00046888078,0.00008973047,0.93279856,0.0045079575,0.0023443305,0.0013333792,0.006244743],"study_design_scores_gemma":[0.00007200108,0.000015339876,0.020100227,0.000013907383,0.000024945468,0.000049780985,0.00008565676,0.97789717,0.0002623943,0.0006846126,0.00076992635,0.000024153964],"about_ca_topic_score_codex":0.25721648,"about_ca_topic_score_gemma":0.18750264,"teacher_disagreement_score":0.25721648,"about_ca_system_score_codex":0.0014997507,"about_ca_system_score_gemma":0.0010801922,"threshold_uncertainty_score":0.5114386},"labels":[],"label_agreement":null},{"id":"W2160349706","doi":"10.1029/2008gl035585","title":"Paleointensity of the ancient Martian magnetic field","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Martian; Meteorite; Mars Exploration Program; Natural remanent magnetization; Geology; Geophysics; Astrobiology; Remanence; Paleomagnetism; Magnetization; Earth's magnetic field; Earth science; Magnetic field; Physics","score_opus":0.037861640600920524,"score_gpt":0.27002841064392674,"score_spread":0.23216677004300623,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160349706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99541485,0.0003872716,0.00032464298,0.00005332315,0.0000019705994,8.967788e-7,0.00016484113,0.000011228968,0.003640881],"genre_scores_gemma":[0.999358,0.00013989385,0.00015786575,0.0000064363076,0.0000061737187,7.668679e-7,0.00007953795,0.0000022991244,0.00024900635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999707,0.0000053304016,0.0000015537789,0.000010263405,0.0000071759596,0.0000049857344],"domain_scores_gemma":[0.9998857,0.000031672687,0.000028411689,0.00001550356,0.000024586909,0.000014199322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017120973,0.00007245878,0.000066724344,0.00073129847,0.00013838861,0.00037897503,0.00008646122,0.000111928326,0.0022086021],"category_scores_gemma":[0.00039068743,0.00009691927,0.00005709594,0.0003674133,0.0003013142,0.00029181293,0.00024941223,0.00018788823,0.00017866115],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032215824,0.000018938932,0.8055878,0.00010442154,0.000095924355,0.00023152174,0.0008475788,0.0012658098,0.106783696,0.0032535791,0.0004175989,0.08107097],"study_design_scores_gemma":[0.0000033282734,0.00001777338,0.9929765,0.000007048011,0.000011614777,0.0004376068,0.00013413205,0.00049953465,0.0031884855,0.000881241,0.0018369573,0.000005780416],"about_ca_topic_score_codex":0.00095701125,"about_ca_topic_score_gemma":0.0015406866,"teacher_disagreement_score":0.0022086021,"about_ca_system_score_codex":0.00013708496,"about_ca_system_score_gemma":0.00006911459,"threshold_uncertainty_score":0.0073884726},"labels":[],"label_agreement":null},{"id":"W2160893194","doi":"10.1029/2005gl023992","title":"Can synthetic aperture radars be used to estimate hurricane force winds?","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":88,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Space Agency","funders":"","keywords":"Synthetic aperture radar; Geology; Meteorology; Remote sensing; Environmental science; Physics","score_opus":0.03065377299199722,"score_gpt":0.30312916886316577,"score_spread":0.27247539587116854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160893194","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9781083,0.0017957825,0.01420837,0.00079383317,0.00017976818,0.000024966277,0.0005453521,0.00029696902,0.004046557],"genre_scores_gemma":[0.9819903,0.00078772526,0.015715776,0.0001262332,0.000091373855,0.000010549567,0.00083101564,0.00002335115,0.00042366804],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99963105,0.00014676101,0.000028464328,0.000063066975,0.00009354275,0.000037075126],"domain_scores_gemma":[0.9989398,0.00040260414,0.0002066086,0.00014935089,0.00026079544,0.000040840932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017389306,0.0005313699,0.00031691845,0.0010558114,0.00014242329,0.0008372495,0.00027579162,0.0006559129,0.0005965454],"category_scores_gemma":[0.006297882,0.0002193084,0.00031243704,0.0007954718,0.00032977838,0.0015129987,0.00031725614,0.00021852984,0.00044097772],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001349309,0.00019398423,0.47243762,0.00026917766,0.00071011117,0.00022876055,0.00018643864,0.08923725,0.02323332,0.0024840026,0.0028199707,0.40685016],"study_design_scores_gemma":[0.00025247046,0.00058469246,0.42926234,0.00011783997,0.00023815956,0.00041455743,0.00041911344,0.5385054,0.01658132,0.0049631107,0.0085424315,0.00011862181],"about_ca_topic_score_codex":0.0029533582,"about_ca_topic_score_gemma":0.0037114506,"teacher_disagreement_score":0.0029533582,"about_ca_system_score_codex":0.00020354474,"about_ca_system_score_gemma":0.00013418605,"threshold_uncertainty_score":0.00919646},"labels":[],"label_agreement":null},{"id":"W2160912900","doi":"10.1029/2002gl016419","title":"Advective‐diffusive mass flux and implications for stratosphere‐troposphere exchange","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Langara College; University of British Columbia","funders":"","keywords":"Tropopause; Stratosphere; Troposphere; Mass flux; Advection; Flux (metallurgy); Atmospheric sciences; Context (archaeology); Physics; Environmental science; Mechanics; Geology; Chemistry","score_opus":0.030692846775383583,"score_gpt":0.2973085727989975,"score_spread":0.2666157260236139,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160912900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91301495,0.006884631,0.050020177,0.0035370328,0.00011917989,0.000010977329,0.00018985484,0.00010787427,0.026115403],"genre_scores_gemma":[0.9974235,0.00064337015,0.0010584584,0.000048282036,0.000038629532,0.0000042747556,0.000019469531,0.000008617631,0.0007553935],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"observational","domain_scores_codex":[0.9999224,0.00001579806,0.0000033060353,0.000016804135,0.000016820826,0.000024815701],"domain_scores_gemma":[0.99933654,0.00045241762,0.00008107596,0.00003752797,0.000040669773,0.000051698593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000451216,0.00029003416,0.00020971647,0.0006293746,0.00054663274,0.0013958113,0.0003564347,0.00044546614,0.0019447256],"category_scores_gemma":[0.002079829,0.00010719562,0.00025702507,0.00036788968,0.0014878312,0.002373691,0.00085637544,0.00046750493,0.00011967843],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028298766,0.00003142478,0.034471173,0.00016084373,0.000029180514,0.0007465479,0.00067547365,0.05367231,0.020518359,0.8634803,0.0011308673,0.024800416],"study_design_scores_gemma":[0.000036970607,0.00008795609,0.03984185,0.00008732681,0.000034257144,0.0009744783,0.00045906633,0.13331172,0.0073145945,0.81004703,0.0077692447,0.000035538353],"about_ca_topic_score_codex":0.0017967178,"about_ca_topic_score_gemma":0.0006865891,"teacher_disagreement_score":0.0019447256,"about_ca_system_score_codex":0.00085649494,"about_ca_system_score_gemma":0.00022220587,"threshold_uncertainty_score":0.006505728},"labels":[],"label_agreement":null},{"id":"W2160945476","doi":"10.1002/2013gl058247","title":"Wind‐driven Arctic freshwater anomalies","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Johns Hopkins University; National Science Foundation","keywords":"Anticyclone; Arctic; Climatology; Arctic dipole anomaly; Environmental science; Archipelago; The arctic; Oceanography; Atmospheric sciences; Geology; Arctic ice pack","score_opus":0.021740412353987933,"score_gpt":0.25253983334163127,"score_spread":0.23079942098764333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2160945476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99338865,0.000075384276,0.0018426995,0.00014616981,0.000034754616,0.0000052847163,0.00063748163,0.00006727066,0.0038022227],"genre_scores_gemma":[0.99904114,0.0000679538,0.00025230736,0.0000143770885,0.000006323805,0.0000029144053,0.00021388088,0.000009792099,0.00039133994],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996054,0.000006788896,0.000002633276,0.000010694681,0.0000061413507,0.000013123195],"domain_scores_gemma":[0.99992645,0.000012289365,0.000020882857,0.000007708684,0.000018073883,0.000014530392],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000115531235,0.00024941415,0.0001717809,0.0001482945,0.00022868169,0.00055186107,0.0002029703,0.00025239118,0.0007761181],"category_scores_gemma":[0.00030853716,0.00015801634,0.00032389685,0.00020082179,0.000234428,0.0003125121,0.00025456917,0.00022145863,0.0001153165],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028698603,0.00007660946,0.14178927,0.00006424076,0.00013650811,0.0004518103,0.0001115014,0.8029324,0.03746881,0.0064634094,0.0017735539,0.008444894],"study_design_scores_gemma":[0.000055684202,0.00007029402,0.1270045,0.000017764165,0.000047650396,0.000097073666,0.00012750155,0.86332625,0.004127146,0.0024486848,0.0026238554,0.000053695596],"about_ca_topic_score_codex":0.04931782,"about_ca_topic_score_gemma":0.040219102,"teacher_disagreement_score":0.04931782,"about_ca_system_score_codex":0.00076599047,"about_ca_system_score_gemma":0.0006694219,"threshold_uncertainty_score":0.09806156},"labels":[],"label_agreement":null},{"id":"W2161082169","doi":"10.1002/2014gl062325","title":"Small lakes show muted climate change signal in deepwater temperatures","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":129,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Geological Survey; Global Lake Ecological Observatory Network; Wisconsin Department of Natural Resources; National Science Foundation","keywords":"Climate change; Environmental science; Global warming; Oceanography; Hydrology (agriculture); Atmospheric sciences; Climatology; Physical geography; Geology; Geography","score_opus":0.043915414978745224,"score_gpt":0.25433487737570926,"score_spread":0.21041946239696402,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161082169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991935,0.000042682324,0.00006525921,0.000023940831,0.000002104577,0.0000017140794,0.00021233688,0.000006074917,0.00045223706],"genre_scores_gemma":[0.999663,0.000016491691,0.00004583534,0.000014169204,0.0000021488338,0.0000029183975,0.0001353358,0.0000017678353,0.00011832623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998202,0.000031236155,0.000013776602,0.00007107211,0.0000273322,0.000036448128],"domain_scores_gemma":[0.9994241,0.00009199857,0.00023431283,0.000047110854,0.00013296549,0.00006949504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024225708,0.00016569906,0.00021696214,0.00044899047,0.00037915984,0.00068478845,0.0001427466,0.00018799899,0.0010162769],"category_scores_gemma":[0.00077008107,0.00018929008,0.00016938895,0.00065986987,0.0003503596,0.00037661506,0.0005617788,0.00015222479,0.00012044504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002797828,0.000020067338,0.9737403,0.000022590668,0.0000853247,0.00007518226,0.0005394495,0.0001801397,0.020969272,0.0000555763,0.00025814204,0.0037742467],"study_design_scores_gemma":[0.0000014741255,0.000014892244,0.9990238,0.0000017421452,0.000011621608,0.00001351936,0.00018981891,0.00010515618,0.0004272286,0.000011887862,0.0001967758,0.0000020861012],"about_ca_topic_score_codex":0.028519534,"about_ca_topic_score_gemma":0.0697766,"teacher_disagreement_score":0.028519534,"about_ca_system_score_codex":0.00043609197,"about_ca_system_score_gemma":0.00022059226,"threshold_uncertainty_score":0.056707084},"labels":[],"label_agreement":null},{"id":"W2161107826","doi":"10.1029/2009gl038727","title":"Ice particle growth in the polar summer mesosphere: Formation time and equilibrium size","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; Regional Municipality of Waterloo; University of Waterloo","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Mesosphere; Polar; Atmospheric sciences; Water vapor; Particle (ecology); Range (aeronautics); Particle size; Polar night; Volume (thermodynamics); Environmental science; Materials science; Physics; Meteorology; Chemistry; Stratosphere; Geology; Thermodynamics; Astronomy","score_opus":0.023812431318465336,"score_gpt":0.27018075948103176,"score_spread":0.24636832816256643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161107826","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99773407,0.00030084478,0.0008575511,0.000026376872,0.0000058538435,0.000004869915,0.00033055645,0.000029570238,0.00071030424],"genre_scores_gemma":[0.99888617,0.00012277336,0.00041461666,0.0000037438208,0.0000027647038,0.000005389416,0.0003965785,0.000008218175,0.00015985368],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999627,0.0000025740485,0.0000012451629,0.0000141753435,0.000008540657,0.0000107754795],"domain_scores_gemma":[0.9998004,0.00007752694,0.00003142086,0.000013546575,0.00004675666,0.000030373014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018578593,0.00024235898,0.00015251318,0.00032351667,0.00022788551,0.0002814525,0.00014957873,0.00019620136,0.00065460365],"category_scores_gemma":[0.0003535621,0.00015549868,0.00026308678,0.00015793485,0.0001746224,0.00035554828,0.00013191222,0.00022098339,0.00016733637],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011830742,0.00011855156,0.26232335,0.00016923332,0.00009427322,0.00043579686,0.00032298572,0.029158577,0.6892029,0.0009887218,0.0007597708,0.01524279],"study_design_scores_gemma":[0.000045188353,0.0002926825,0.5914676,0.000012061938,0.000037342295,0.00022835561,0.00017552802,0.13550547,0.2703305,0.00038481486,0.001488705,0.00003173981],"about_ca_topic_score_codex":0.0071796277,"about_ca_topic_score_gemma":0.0048046745,"teacher_disagreement_score":0.0071796277,"about_ca_system_score_codex":0.00040790852,"about_ca_system_score_gemma":0.00019060679,"threshold_uncertainty_score":0.01427567},"labels":[],"label_agreement":null},{"id":"W2161153103","doi":"10.1029/2006gl026613","title":"Subsurface temperature maxima in the Labrador Sea and the subpolar North Atlantic","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ocean gyre; Geology; Oceanography; Buoyancy; Deep convection; Convection; Water mass; North Atlantic Deep Water; Forcing (mathematics); Mixed layer; Maxima; Deep sea; Subsurface flow; Deep water; Climatology; Subtropics; Groundwater; Meteorology; Geography","score_opus":0.010399380853989849,"score_gpt":0.22421255741007304,"score_spread":0.2138131765560832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161153103","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866736,0.00015504641,0.000017735068,0.000038006554,0.000001985956,0.0000010474848,0.00030216528,0.000007931197,0.00080872147],"genre_scores_gemma":[0.9993899,0.000082967286,0.000035377027,0.000013090113,0.0000040261425,0.0000017993698,0.00031893785,0.0000019946197,0.00015189916],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999936,0.0000073627452,0.000005511602,0.000014813021,0.0000094120305,0.00002697015],"domain_scores_gemma":[0.99980813,0.000015078425,0.00009287029,0.000010038383,0.000040750943,0.000033205342],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009201968,0.00011946056,0.00017009008,0.0006979433,0.00020057398,0.0004851223,0.00013946748,0.00013966417,0.0010582343],"category_scores_gemma":[0.00035886336,0.00010205977,0.00011917542,0.0008470502,0.0002278049,0.00026916256,0.00042229146,0.00012457209,0.0001898106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047164122,0.000026362313,0.96451527,0.00005702292,0.00007353237,0.00019818914,0.0005563265,0.0007137916,0.012943741,0.00017836742,0.0006287923,0.019637069],"study_design_scores_gemma":[0.000003963993,0.000012322245,0.99905115,0.000003793165,0.0000073263072,0.000018075876,0.00023566138,0.0001269253,0.00021415611,0.000024129098,0.0003000526,0.0000023949763],"about_ca_topic_score_codex":0.07601271,"about_ca_topic_score_gemma":0.12736551,"teacher_disagreement_score":0.07601271,"about_ca_system_score_codex":0.00083236775,"about_ca_system_score_gemma":0.00037142987,"threshold_uncertainty_score":0.15114051},"labels":[],"label_agreement":null},{"id":"W2161514023","doi":"10.1029/2005gl025403","title":"Sensitivity of inverse estimation of annual mean CO<sub>2</sub> sources and sinks to ocean‐only sites versus all‐sites observational networks","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Environmental science; Sensitivity (control systems); Flux (metallurgy); Range (aeronautics); Atmospheric sciences; Atmospheric models; Inverse; Climatology; Meteorology; Atmosphere (unit); Geology; Mathematics; Geography; Chemistry","score_opus":0.023295285973791484,"score_gpt":0.26612333065993093,"score_spread":0.24282804468613944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161514023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9745866,0.00022820967,0.021775605,0.00025952462,0.00003264972,0.000027955246,0.0007459722,0.00022529748,0.0021181814],"genre_scores_gemma":[0.99633324,0.000054487293,0.0024850399,0.000064467626,0.000009562129,0.000009900149,0.00080985506,0.000035163604,0.00019823559],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9961957,0.0021919617,0.00018001613,0.0008378421,0.00042790239,0.00016662687],"domain_scores_gemma":[0.95259136,0.038256705,0.0025634416,0.0037367994,0.0024848168,0.00036677517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010100065,0.00042399325,0.00042275386,0.0007977772,0.00022937347,0.0010810241,0.0005452803,0.00075077923,0.0007051052],"category_scores_gemma":[0.05806276,0.000423407,0.00058821565,0.0006042416,0.00071902847,0.0011596865,0.0013749904,0.00072406913,0.0002139008],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019613404,0.0000866248,0.41411754,0.00014739971,0.0009767994,0.00022810325,0.0003803666,0.52851284,0.010595077,0.0018671253,0.0010517789,0.04007498],"study_design_scores_gemma":[0.00007102393,0.00018645868,0.33292183,0.000056371813,0.00029831537,0.0004548192,0.00027954282,0.64009976,0.020311197,0.0037916368,0.0014256032,0.00010339037],"about_ca_topic_score_codex":0.0134154875,"about_ca_topic_score_gemma":0.00482035,"teacher_disagreement_score":0.0134154875,"about_ca_system_score_codex":0.000782643,"about_ca_system_score_gemma":0.0004286673,"threshold_uncertainty_score":0.05341488},"labels":[],"label_agreement":null},{"id":"W2161566772","doi":"10.1029/2005gl022425","title":"Atmospheric Chemistry Experiment (ACE) Arctic stratospheric measurements of NO<sub>x</sub> during February and March 2004: Impact of intense solar flares","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Waterloo","funders":"","keywords":"Stratosphere; Atmospheric sciences; Polar vortex; Mixing ratio; Environmental science; Occultation; Polar night; Arctic; Solar flare; Atmospheric chemistry; Climatology; Ozone; Physics; Meteorology; Geology; Astrophysics; Oceanography","score_opus":0.023219108538492943,"score_gpt":0.27466413560394226,"score_spread":0.2514450270654493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161566772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98682135,0.00018283006,0.0006751308,0.00014177224,0.00007236716,0.00003853932,0.009012765,0.00008920894,0.0029660773],"genre_scores_gemma":[0.9838666,0.00020802507,0.0016346062,0.00007723044,0.000037124868,0.000033247336,0.013106789,0.00001030593,0.0010259752],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998499,0.000019601672,0.0000059792837,0.000030388079,0.00006675162,0.000027423981],"domain_scores_gemma":[0.999668,0.000029424169,0.00006725997,0.000034775876,0.00011796514,0.0000825636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045313447,0.0004726627,0.00026768717,0.0002089546,0.0007195378,0.0003737707,0.00019491087,0.00023459322,0.0003310166],"category_scores_gemma":[0.0003267646,0.00015160901,0.00014258799,0.00025508058,0.00016051398,0.00017587248,0.00025404833,0.0002966857,0.00009771223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.008664435,0.0014240603,0.83183587,0.0001657654,0.00080059515,0.00048168006,0.000336013,0.01238197,0.099651724,0.00088131253,0.014609075,0.02876746],"study_design_scores_gemma":[0.00013954307,0.00043416145,0.96300584,0.0000064344626,0.00012277905,0.00006309681,0.00004542977,0.005679239,0.024231177,0.00012526396,0.00612928,0.00001787027],"about_ca_topic_score_codex":0.108775236,"about_ca_topic_score_gemma":0.17879356,"teacher_disagreement_score":0.108775236,"about_ca_system_score_codex":0.00097031664,"about_ca_system_score_gemma":0.0007847882,"threshold_uncertainty_score":0.21628416},"labels":[],"label_agreement":null},{"id":"W2161792782","doi":"10.1002/2014gl061205","title":"Sulfur budget and global climate impact of the A.D. 1835 eruption of Cosigüina volcano, Nicaragua","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Volcano; Explosive eruption; Impact crater; Geology; Vulcanian eruption; Atmosphere (unit); Earth science; Ice core; Climatology; Physical geography; Magma; Geochemistry; Astrobiology; Geography; Meteorology","score_opus":0.018134755763055354,"score_gpt":0.2828117036364632,"score_spread":0.26467694787340784,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161792782","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964001,0.00054916996,0.000027887048,0.00010238121,0.000004731879,0.0000027806857,0.0010435606,0.000007916453,0.0018615797],"genre_scores_gemma":[0.9984995,0.00032395837,0.000052198484,0.000018095003,0.000005288916,0.0000035463365,0.0008052143,0.0000043352775,0.00028788898],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.000011870703,0.000005173651,0.000021989012,0.000014200165,0.000021836357],"domain_scores_gemma":[0.9998708,0.000013136101,0.000046804656,0.000010766518,0.00004141699,0.000017059892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001764836,0.0002521259,0.00016430386,0.0009197675,0.00037907256,0.0006297421,0.00026138936,0.00032811097,0.0011828493],"category_scores_gemma":[0.00044756345,0.000114782015,0.00018203045,0.0010556912,0.0003473322,0.00027465753,0.00039541587,0.00018168973,0.00013891124],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035525227,0.000043251082,0.9677004,0.000107497995,0.00030326107,0.0005108819,0.0004535794,0.0061649783,0.0108666085,0.0005936037,0.0007822194,0.012118342],"study_design_scores_gemma":[0.000004102396,0.000013864165,0.99649954,0.000010242381,0.00002405038,0.000051543862,0.00018742937,0.0008632051,0.00062454026,0.000050743878,0.0016656693,0.0000049926657],"about_ca_topic_score_codex":0.22700985,"about_ca_topic_score_gemma":0.2436951,"teacher_disagreement_score":0.22700985,"about_ca_system_score_codex":0.003694587,"about_ca_system_score_gemma":0.00054552796,"threshold_uncertainty_score":0.45137697},"labels":[],"label_agreement":null},{"id":"W2161950628","doi":"10.1029/2007gl032162","title":"Circulation in Lake Vostok: A laboratory analogue study","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Convection; Clockwise; Water mass; Boundary current; Oceanography; Hydrology (agriculture); Earth science; Geophysics; Ocean current; Meteorology; Rotation (mathematics)","score_opus":0.05452572582517627,"score_gpt":0.3080320173161639,"score_spread":0.25350629149098763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161950628","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999419,0.000021398022,0.00010693105,0.000014782775,0.0000032391326,0.000010184858,0.00010608788,0.0000072504336,0.00031114128],"genre_scores_gemma":[0.99910873,0.00003519927,0.00032753136,0.000011673162,0.0000031300774,0.000022464608,0.0002013558,0.000003383646,0.0002865016],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987555,0.000020301266,0.0000077994455,0.000036538342,0.000017962202,0.000041822794],"domain_scores_gemma":[0.99988234,0.000028611008,0.000022939897,0.000019906347,0.000020455773,0.000025724295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012505756,0.00020400502,0.00032495375,0.00017612,0.00054645096,0.000564037,0.00031316676,0.00038236592,0.0011777955],"category_scores_gemma":[0.0002904534,0.00013775562,0.00036870386,0.00023121152,0.00084066385,0.00034906485,0.00046928035,0.00040255583,0.00010927492],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028181835,0.0024815714,0.11723746,0.0002478213,0.00016473889,0.0007329099,0.0022559878,0.021748604,0.84044653,0.0022305236,0.0011299432,0.008505739],"study_design_scores_gemma":[0.0023779087,0.01389503,0.6513281,0.000051471878,0.0005809903,0.0007164933,0.0037127852,0.14794646,0.16743512,0.0029804017,0.008768598,0.0002066541],"about_ca_topic_score_codex":0.059836246,"about_ca_topic_score_gemma":0.039285924,"teacher_disagreement_score":0.059836246,"about_ca_system_score_codex":0.0016221512,"about_ca_system_score_gemma":0.00088975905,"threshold_uncertainty_score":0.11897588},"labels":[],"label_agreement":null},{"id":"W2161964316","doi":"10.1029/2007gl028987","title":"Seismic interferometry using non‐volcanic tremor in Cascadia","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Geology; Seismology; Subduction; Seismic interferometry; Interferometry; Episodic tremor and slip; Volcano; Transect; Noise (video); Reflection (computer programming); Arrival time; Seismic array; Geodesy; Optics; Tectonics; Physics","score_opus":0.044880083304495964,"score_gpt":0.31661981904492037,"score_spread":0.2717397357404244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161964316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880874,0.000020844003,0.00035707344,0.00001459606,0.0000013239018,0.0000029945297,0.00010232028,0.000023691857,0.0006684285],"genre_scores_gemma":[0.9989089,0.000025848598,0.0005275986,0.0000034086797,0.000001735996,0.0000034336815,0.00029465446,0.0000055017313,0.00022888306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998221,0.000019280922,0.000009626556,0.0000634755,0.00005656816,0.000028863298],"domain_scores_gemma":[0.999726,0.000042318625,0.00006654829,0.000038928378,0.000074417265,0.00005183755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002436604,0.00042510987,0.0002260338,0.001014136,0.0004166885,0.00042054354,0.0003180414,0.00025217782,0.0005492687],"category_scores_gemma":[0.0011543944,0.00021886555,0.00025970562,0.001142972,0.00027778614,0.00016848961,0.00051343034,0.00020473088,0.00013539536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064863404,0.000097512246,0.7790862,0.0001099312,0.00024018374,0.0010505001,0.0019110031,0.017898194,0.1553352,0.00028200794,0.00043351256,0.042907126],"study_design_scores_gemma":[0.000014996227,0.000054023214,0.987739,0.0000051132765,0.000035938996,0.00010096187,0.00019089381,0.00805356,0.003375685,0.000063423366,0.0003557286,0.000010757707],"about_ca_topic_score_codex":0.075356565,"about_ca_topic_score_gemma":0.13186526,"teacher_disagreement_score":0.075356565,"about_ca_system_score_codex":0.0008722831,"about_ca_system_score_gemma":0.00054429553,"threshold_uncertainty_score":0.14983588},"labels":[],"label_agreement":null},{"id":"W2161998600","doi":"10.1002/2014gl061413","title":"Dansgaard‐Oeschger oscillations predicted in a comprehensive model of glacial climate: A “kicked” salt oscillator in the Atlantic","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":274,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Compute Canada","keywords":"Glacial period; Geology; Ice core; Climatology; North Atlantic Deep Water; North Atlantic oscillation; Oscillation (cell signaling); Milankovitch cycles; Oceanography; Thermohaline circulation; Paleontology; Chemistry","score_opus":0.045245593295534944,"score_gpt":0.2986453990685493,"score_spread":0.25339980577301435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2161998600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97642046,0.000060624414,0.019340463,0.0003619827,0.000017387949,0.000014902899,0.00020237184,0.00006121025,0.003520605],"genre_scores_gemma":[0.99837804,0.00003776384,0.0007170861,0.00001715346,0.000008273634,0.0000123992495,0.00004218296,0.000007712478,0.00077936077],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999424,0.000016332997,0.0000032871783,0.000015438205,0.000008828933,0.00001366379],"domain_scores_gemma":[0.99977547,0.000074394695,0.000052004856,0.000020828511,0.000027020293,0.000050277657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034776528,0.0003074337,0.00031141998,0.00018144387,0.00037738995,0.00060589204,0.0005290529,0.00044999117,0.00080313254],"category_scores_gemma":[0.00088372093,0.00022317344,0.00040134575,0.00015150452,0.00065004133,0.00078521646,0.0004264257,0.00034563837,0.000118163116],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006690696,0.000026821948,0.011175116,0.00001210469,0.000042552754,0.000058879028,0.00006296967,0.97578853,0.0016507286,0.009405201,0.00027897692,0.0014312696],"study_design_scores_gemma":[0.000017764212,0.000014334076,0.0023852736,0.0000013997267,0.000010131766,0.0000061791475,0.000011976066,0.99446434,0.00006488688,0.0028850462,0.00013346139,0.000005180489],"about_ca_topic_score_codex":0.019247157,"about_ca_topic_score_gemma":0.01160848,"teacher_disagreement_score":0.019247157,"about_ca_system_score_codex":0.00069275295,"about_ca_system_score_gemma":0.0007510512,"threshold_uncertainty_score":0.038270235},"labels":[],"label_agreement":null},{"id":"W2162264552","doi":"10.1029/2004gl021046","title":"Mount Everest snow plume: A case study","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Plume; Snow; Summit; Mount; Geology; Jet stream; Meteorology; Physical geography; Climatology; Environmental science; Jet (fluid); Atmospheric sciences; Geography; Geomorphology; Aerospace engineering","score_opus":0.06679315497196611,"score_gpt":0.3193737222904504,"score_spread":0.25258056731848433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162264552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940183,0.0002860189,0.0008068207,0.00058033067,0.000016199378,0.000058536487,0.00025690996,0.000050749433,0.003926116],"genre_scores_gemma":[0.99605405,0.000477145,0.0017705793,0.000067765926,0.000036671543,0.000021744812,0.00024851089,0.000010377782,0.0013131496],"study_design_codex":"observational","study_design_gemma":"case_report","domain_scores_codex":[0.9998196,0.00003844221,0.000009373065,0.000018895942,0.00006462525,0.000049079837],"domain_scores_gemma":[0.9996538,0.00013358473,0.000059981245,0.00003064688,0.000047580026,0.00007446513],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002464078,0.0004749643,0.00021302339,0.0006144034,0.0016653714,0.00071703386,0.00087105396,0.0017651074,0.0009915574],"category_scores_gemma":[0.00077161635,0.00019214522,0.00044272398,0.00081786694,0.00040840346,0.0004758058,0.0007567548,0.00061190105,0.00015046608],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010254834,0.0016782476,0.43616414,0.00065513427,0.00039026546,0.35373116,0.01047338,0.09090813,0.02801282,0.0066830353,0.01250844,0.057769857],"study_design_scores_gemma":[0.0005117987,0.0022308524,0.43548077,0.00028234397,0.00046829504,0.09858701,0.04238544,0.3273429,0.028028814,0.0065417923,0.05788884,0.00025111221],"about_ca_topic_score_codex":0.037863035,"about_ca_topic_score_gemma":0.08348311,"teacher_disagreement_score":0.037863035,"about_ca_system_score_codex":0.0008537576,"about_ca_system_score_gemma":0.0006007365,"threshold_uncertainty_score":0.075285316},"labels":[],"label_agreement":null},{"id":"W2162428985","doi":"10.1029/2005gl023740","title":"One more step toward a warmer Arctic","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":402,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Office of Naval Research; National Science Foundation","keywords":"Arctic; Arctic dipole anomaly; Oceanography; Geology; Climatology; The arctic; Structural basin; Canada Basin; Latitude; Arctic sea ice decline; Norwegian; Anomaly (physics); Polar; Arctic ice pack; Paleontology; Drift ice","score_opus":0.03902616060488812,"score_gpt":0.28904536579038276,"score_spread":0.25001920518549464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162428985","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.51160663,0.009086449,0.028536707,0.2439935,0.00726445,0.00017289625,0.0012070569,0.0005859959,0.19754623],"genre_scores_gemma":[0.84308696,0.0057251086,0.04912793,0.036293514,0.0028071487,0.00013646478,0.0006569383,0.00023274419,0.061933167],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9997038,0.00008720335,0.000014372212,0.000079457655,0.000064886335,0.00005026787],"domain_scores_gemma":[0.9992526,0.000112593094,0.00009296353,0.00009391119,0.00020257133,0.0002453087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010337747,0.00024634838,0.0002993471,0.0003435765,0.0016496149,0.0017861945,0.00049425755,0.0012801698,0.012028422],"category_scores_gemma":[0.0014780978,0.0000972203,0.00028162645,0.00031576937,0.0006907623,0.0021712696,0.0021113036,0.001592572,0.0016851816],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006754377,0.0010745726,0.14054184,0.0026031095,0.00050985534,0.0022521925,0.019303791,0.0040861,0.0928647,0.20289066,0.09428371,0.43891406],"study_design_scores_gemma":[0.000099107005,0.0012272683,0.15856528,0.00067134114,0.00012755736,0.0016569775,0.019920088,0.0011884456,0.013936589,0.060762644,0.74170554,0.00013913213],"about_ca_topic_score_codex":0.0025755726,"about_ca_topic_score_gemma":0.010610646,"teacher_disagreement_score":0.012028422,"about_ca_system_score_codex":0.0003428385,"about_ca_system_score_gemma":0.0014354131,"threshold_uncertainty_score":0.040239096},"labels":[],"label_agreement":null},{"id":"W2162796817","doi":"10.1002/2015gl063846","title":"Heat sources for glacial ice melt in a west Greenland tidewater outlet glacier fjord: The role of subglacial freshwater discharge","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Division of Arctic Sciences; Comisión de Investigaciones Científicas; Nationale Geologiske Undersøgelser for Danmark og Grønland; Danish Agency for Science and Higher Education; Energistyrelsen; Aage V. Jensens Fonde; ArcticNet","keywords":"Fjord; Tidewater; Geology; Tidewater glacier cycle; Glacier; Glacial period; Rock glacier; Iceberg; Oceanography; Glacier morphology; Geomorphology; Ice stream; Cryosphere; Ice sheet; Sea ice; Ice calving","score_opus":0.04364245105035337,"score_gpt":0.2820711115990105,"score_spread":0.23842866054865713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162796817","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996331,0.000026641132,0.000034487133,0.00001691265,0.0000010796966,0.0000019455251,0.00009830825,0.00000828206,0.0001793227],"genre_scores_gemma":[0.9996387,0.000017070985,0.00006985047,0.000007668943,0.0000015346825,0.0000017840462,0.0001566881,0.0000038735798,0.00010278306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999629,0.0000027972658,0.0000019881113,0.000007885933,0.00000927001,0.0000150289725],"domain_scores_gemma":[0.999931,0.000013474742,0.000012347844,0.0000025704444,0.000018527067,0.000022147853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000082800674,0.00025304948,0.00025533437,0.0006951112,0.00042027986,0.0005451137,0.00022385283,0.0002811532,0.00061830104],"category_scores_gemma":[0.00017164845,0.00017547968,0.0002197312,0.0004107495,0.0003018484,0.00029664583,0.00032148525,0.00024865338,0.00010136241],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007262888,0.00014825315,0.75214934,0.000072622264,0.00011753464,0.00097242504,0.0013350064,0.004459953,0.2270463,0.00022296392,0.00040580766,0.012343547],"study_design_scores_gemma":[0.000015092915,0.00003303252,0.9928247,0.000003934786,0.0000129105165,0.00004243762,0.0002557225,0.00412203,0.0024667087,0.000042750435,0.00017338069,0.0000072788694],"about_ca_topic_score_codex":0.07205803,"about_ca_topic_score_gemma":0.08817799,"teacher_disagreement_score":0.07205803,"about_ca_system_score_codex":0.0012736905,"about_ca_system_score_gemma":0.0004974709,"threshold_uncertainty_score":0.14327717},"labels":[],"label_agreement":null},{"id":"W2162940647","doi":"10.1002/grl.50844","title":"Direct temperature and salinity acoustic full waveform inversion","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"FP7 People: Marie-Curie Actions; Ministerio de Economía y Competitividad","keywords":"Inversion (geology); Waveform; Geology; Temperature salinity diagrams; Salinity; Speed of sound; Electrical impedance; Geophysics; Seismology; Acoustics; Physics; Voltage; Oceanography","score_opus":0.021578830735783212,"score_gpt":0.2606107589372408,"score_spread":0.23903192820145758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2162940647","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13724688,0.00018722033,0.85038143,0.00025222098,0.0001084552,0.0000670347,0.0009972916,0.0017015494,0.009057932],"genre_scores_gemma":[0.7841914,0.00031435088,0.20763342,0.00011079497,0.00005404775,0.000112872505,0.0012971021,0.00021667458,0.00606933],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998485,0.000015847741,0.000010088051,0.000038737926,0.00006696595,0.000019813739],"domain_scores_gemma":[0.9997539,0.000059708156,0.000027090638,0.000047602673,0.00009164838,0.000020080588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002674999,0.0006180539,0.00043771625,0.0004805793,0.00018686593,0.00073439965,0.00073202286,0.0007611539,0.0021444988],"category_scores_gemma":[0.0017069547,0.0004970903,0.0004970751,0.00044191256,0.00036562418,0.001294963,0.0010436027,0.00072069274,0.0007223003],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017804663,0.00015329957,0.005697644,0.00021710925,0.00008388658,0.0002682779,0.00017335963,0.5905448,0.18920206,0.01759128,0.0019166577,0.19397351],"study_design_scores_gemma":[0.000016577203,0.000020104802,0.0013412185,0.0000065124123,0.0000084063195,0.000067004315,0.000016821949,0.98236614,0.011420331,0.0032164955,0.0015014283,0.000019060386],"about_ca_topic_score_codex":0.004513168,"about_ca_topic_score_gemma":0.0047484664,"teacher_disagreement_score":0.004513168,"about_ca_system_score_codex":0.00025711453,"about_ca_system_score_gemma":0.0011690385,"threshold_uncertainty_score":0.008973837},"labels":[],"label_agreement":null},{"id":"W2163117943","doi":"10.1002/2015gl063613","title":"Ambient noise tomography across the southern Alaskan Cordillera","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Seismology; Volcano; Subduction; Lithosphere; Crust; Anomaly (physics); Gravity anomaly; Fault (geology); Seismic tomography; Neogene; Tectonics; Geophysics; Paleontology; Mantle (geology)","score_opus":0.04264789394817565,"score_gpt":0.29659639902956,"score_spread":0.25394850508138433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163117943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998494,0.000043445183,0.00042040643,0.000011686201,0.000001129946,0.000003804744,0.00039054512,0.000019245635,0.00061574817],"genre_scores_gemma":[0.99828666,0.000053088817,0.0006951904,0.0000039260485,0.0000020202704,0.0000035838523,0.00051476236,0.0000042540883,0.00043656703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989057,0.0000102966105,0.000007635294,0.000039146413,0.00003719299,0.000015161112],"domain_scores_gemma":[0.9998419,0.000013407147,0.000029183566,0.000009964296,0.00008703991,0.000018438644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013299932,0.00019271125,0.00012634379,0.0011507126,0.0004521152,0.00044531302,0.00019882753,0.00012061318,0.00058168237],"category_scores_gemma":[0.0003261356,0.00009784528,0.00010318544,0.0013742278,0.00013689738,0.00014678748,0.00042233412,0.00009596862,0.000115130046],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017549667,0.000050881335,0.9162486,0.000038682756,0.00007979734,0.0006828349,0.0008540476,0.0077801426,0.022973757,0.00022267544,0.00029182088,0.05060117],"study_design_scores_gemma":[0.000006587104,0.000026085541,0.9897469,0.000008113055,0.000028692019,0.00011952375,0.0005058852,0.006797449,0.0018076916,0.000058254056,0.00088546495,0.000009220198],"about_ca_topic_score_codex":0.21160983,"about_ca_topic_score_gemma":0.37567592,"teacher_disagreement_score":0.21160983,"about_ca_system_score_codex":0.00061404693,"about_ca_system_score_gemma":0.00070596946,"threshold_uncertainty_score":0.42075628},"labels":[],"label_agreement":null},{"id":"W2163407781","doi":"10.1029/2009gl041434","title":"Perennial pack ice in the southern Beaufort Sea was not as it appeared in the summer of 2009","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; Environment and Climate Change Canada; Bedford Institute of Oceanography; University of Manitoba","funders":"","keywords":"Sea ice; Beaufort sea; Arctic ice pack; Geology; Freeboard; Oceanography; Antarctic sea ice; Drift ice; Fast ice; Sea ice thickness; Canada Basin; Beaufort scale; Climatology","score_opus":0.03804322059713662,"score_gpt":0.29781638750504863,"score_spread":0.259773166907912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163407781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99463403,0.00015832057,0.00015111694,0.00016885278,0.000019078638,0.0000033545946,0.000684729,0.000038047372,0.004142421],"genre_scores_gemma":[0.9974406,0.000046094592,0.00015990772,0.000051069524,0.000011630966,0.0000021183926,0.00080062135,0.000005438301,0.001482533],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988437,0.000010853314,0.00000395675,0.00002726837,0.00003453089,0.000038955866],"domain_scores_gemma":[0.99969554,0.000027483757,0.000086239634,0.00003133767,0.00009551148,0.000063878375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020162147,0.00014355798,0.00013202209,0.00038386698,0.0012846293,0.0007949766,0.00020593965,0.00024710892,0.0017541319],"category_scores_gemma":[0.00036047972,0.000085267755,0.00014663809,0.00043596272,0.00031401016,0.00026803245,0.00021015444,0.00021747805,0.0001945961],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002121167,0.000023175746,0.9605578,0.0000318593,0.00005515934,0.0007346896,0.0018053809,0.0010069058,0.008166682,0.00034149885,0.0045564934,0.022508381],"study_design_scores_gemma":[0.0000026083694,0.000022177504,0.99270976,0.0000053062554,0.0000044487397,0.00012674253,0.00040679998,0.0002477136,0.00035733572,0.00001877095,0.0060941484,0.000004122392],"about_ca_topic_score_codex":0.31632614,"about_ca_topic_score_gemma":0.63992774,"teacher_disagreement_score":0.31632614,"about_ca_system_score_codex":0.0010719886,"about_ca_system_score_gemma":0.0008943468,"threshold_uncertainty_score":0.62896985},"labels":[],"label_agreement":null},{"id":"W2163450348","doi":"10.1002/2014gl061307","title":"Removal of systematic seasonal atmospheric signal from interferometric synthetic aperture radar ground deformation time series","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Synthetic Aperture Radar (SAR) Applications and Techniques","field":"Engineering","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Natural Resources Canada","funders":"","keywords":"Radiosonde; Interferometric synthetic aperture radar; Subsidence; Geology; Geodesy; Troposphere; Synthetic aperture radar; Interferometry; Deformation (meteorology); Levelling; Geodetic datum; Amplitude; Series (stratigraphy); Remote sensing; Atmospheric sciences; Geomorphology; Optics; Physics","score_opus":0.01191853809209984,"score_gpt":0.23697029372603887,"score_spread":0.22505175563393903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163450348","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96576715,0.00014256037,0.03115308,0.000097688826,0.000066186374,0.000026805237,0.001192807,0.0006596635,0.0008941025],"genre_scores_gemma":[0.98092574,0.00008637604,0.015571164,0.000021001713,0.000024072015,0.000021472215,0.002547939,0.000074719304,0.00072745985],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999037,0.000011276185,0.000006425044,0.000029359508,0.000027578575,0.000021689571],"domain_scores_gemma":[0.9998565,0.00002936347,0.000024789588,0.000033330878,0.000046510097,0.000009533577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021974501,0.00048670635,0.00027214087,0.0006763632,0.00017253208,0.0004050599,0.0002448509,0.00017808985,0.00095097686],"category_scores_gemma":[0.0007897768,0.00014761448,0.00038070115,0.00073256897,0.00012847004,0.00018380105,0.00020331005,0.00022618515,0.00035786864],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046759183,0.00024091154,0.17530617,0.000262061,0.00034586378,0.0005710024,0.00033823517,0.18807893,0.19728872,0.0013634076,0.0044966782,0.43124044],"study_design_scores_gemma":[0.000027018823,0.00008887454,0.49060088,0.0000161471,0.00007351303,0.00012809693,0.000094535295,0.4821533,0.022423834,0.00026327232,0.004102602,0.000027913791],"about_ca_topic_score_codex":0.009374909,"about_ca_topic_score_gemma":0.01115559,"teacher_disagreement_score":0.009374909,"about_ca_system_score_codex":0.0001973752,"about_ca_system_score_gemma":0.000523913,"threshold_uncertainty_score":0.018640697},"labels":[],"label_agreement":null},{"id":"W2163757177","doi":"10.1002/2014gl060258","title":"Mercury's surface magnetic field determined from proton‐reflection magnetometry","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Carnegie Institution of Washington; Johns Hopkins University; National Aeronautics and Space Administration","keywords":"Magnetometer; Solar wind; Mercury's magnetic field; Geophysics; Mercury (programming language); Magnetic field; Northern Hemisphere; Latitude; Atmospheric sciences; Magnetosphere; Earth's magnetic field; Physics; Geology; Interplanetary magnetic field; Astronomy","score_opus":0.029552396408636026,"score_gpt":0.30820652963406575,"score_spread":0.2786541332254297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163757177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982445,0.000017353073,0.00027645752,0.000015531285,0.0000015293592,0.0000016487297,0.00010387783,0.000031839965,0.0013072288],"genre_scores_gemma":[0.9993512,0.000016668497,0.0003031856,0.00000588358,0.0000033323709,0.0000015695765,0.00012681457,0.0000058268142,0.00018555348],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999654,0.0000030210795,5.7309643e-7,0.000007702592,0.000016204644,0.000007014299],"domain_scores_gemma":[0.9999621,0.0000069256316,0.000010857791,0.0000040000305,0.000008681578,0.0000074240834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004948905,0.00013739681,0.00013282568,0.00023658336,0.00014528082,0.00019989755,0.00009952994,0.00013683709,0.0008686557],"category_scores_gemma":[0.00018710377,0.00005879449,0.000067799214,0.00022505727,0.00015770762,0.00009220819,0.00015557729,0.0001401113,0.00021246476],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002899288,0.000020980333,0.14615048,0.000041665004,0.00004174694,0.00019754219,0.00035893818,0.0004859716,0.832612,0.00016856121,0.0005430197,0.01908913],"study_design_scores_gemma":[0.00002121072,0.00017998174,0.9452993,0.0000039504193,0.000028747245,0.00019066088,0.00017946394,0.0018218139,0.05116076,0.00010853413,0.0009980717,0.0000073760484],"about_ca_topic_score_codex":0.0020855356,"about_ca_topic_score_gemma":0.0028120552,"teacher_disagreement_score":0.0020855356,"about_ca_system_score_codex":0.00011949313,"about_ca_system_score_gemma":0.00010677581,"threshold_uncertainty_score":0.0041467547},"labels":[],"label_agreement":null},{"id":"W2163998383","doi":"10.1029/2004gl022339","title":"Reply to comment by Dekker and Rietkerk on “Multiple equilibrium states and the abrupt transitions in a dynamical system of soil water interacting with vegetation”","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ecosystem dynamics and resilience","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Vegetation (pathology); Transpiration; Surface runoff; Spatial ecology; Arid; Hydrology (agriculture); Environmental science; Common spatial pattern; Geology; Soil science; Mathematics; Ecology; Statistics","score_opus":0.006810708818027065,"score_gpt":0.248727700191953,"score_spread":0.24191699137392594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2163998383","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00012184441,0.0020453993,0.00021653852,0.97955555,0.017634537,0.0000045707366,0.00010608643,0.000039818664,0.00027572046],"genre_scores_gemma":[0.0023997694,0.0016697048,0.00027286613,0.959302,0.034679003,0.000034962115,0.000050333252,0.0000720517,0.0015192935],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9950264,0.0014070718,0.000698756,0.0012483371,0.001256666,0.0003627488],"domain_scores_gemma":[0.9737264,0.017431082,0.0018133151,0.0009330586,0.0047769044,0.0013192034],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010177153,0.0019277793,0.0029044223,0.0012386988,0.003826888,0.0041373754,0.008567119,0.042315055,0.00716422],"category_scores_gemma":[0.0432799,0.001345246,0.002454119,0.0015803837,0.008221329,0.014763267,0.0045134183,0.06284506,0.00789712],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000039715476,0.000012048642,0.00013749413,0.000091631904,0.000014919276,0.00012990065,0.00024057238,0.00009134485,0.00006399055,0.0036289766,0.9932636,0.0022857045],"study_design_scores_gemma":[0.00013564197,0.000054733326,0.0014911762,0.0004947725,0.000051908268,0.0006908764,0.000792589,0.0010180903,0.0005909159,0.028708726,0.96573466,0.00023586523],"about_ca_topic_score_codex":0.01545179,"about_ca_topic_score_gemma":0.010826044,"teacher_disagreement_score":0.042315055,"about_ca_system_score_codex":0.0056557558,"about_ca_system_score_gemma":0.005181072,"threshold_uncertainty_score":0.053822577},"labels":[],"label_agreement":null},{"id":"W2164037590","doi":"10.1029/2006gl026736","title":"Planktivorous auklet <i>Ptychoramphus aleuticus</i> responses to ocean climate, 2005: Unusual atmospheric blocking?","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and fisheries research","field":"Environmental Science","cited_by":189,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Upwelling; Oceanography; Predation; Regime shift; Environmental science; Jet stream; Ecology; Geography; Climatology; Ecosystem; Geology; Biology; Jet (fluid); Physics","score_opus":0.01744756737123115,"score_gpt":0.28879045878814086,"score_spread":0.2713428914169097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164037590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996075,0.000021604379,0.000011259424,0.00001835958,0.0000014512665,0.0000012587855,0.000029358203,0.000002879521,0.00030637058],"genre_scores_gemma":[0.999332,0.00003198827,0.000049764454,0.00004848679,0.0000018724485,0.000002899574,0.00009040764,0.0000018129691,0.0004406457],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996185,0.0000036418737,0.000002833169,0.000013231071,0.0000044543954,0.000013962459],"domain_scores_gemma":[0.99984884,0.000008539766,0.00007156343,0.0000102857275,0.000016202783,0.000044532233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000091615526,0.00014590083,0.00017412893,0.00015331236,0.00044514652,0.00036747483,0.00012852077,0.0002432004,0.0010970305],"category_scores_gemma":[0.00023799331,0.00013641095,0.000096951066,0.0000982997,0.00031313006,0.0001795266,0.0003198119,0.00024154464,0.00015647901],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00092099915,0.0001693762,0.82250106,0.000087128785,0.00010571822,0.00093065354,0.0010675747,0.00028140636,0.15975927,0.00008236988,0.0009110048,0.013183404],"study_design_scores_gemma":[0.000003651006,0.00008144375,0.9983535,0.0000022289225,0.0000075056514,0.000102826496,0.0003318581,0.00009293419,0.00074020674,0.00001631462,0.00026514003,0.0000025020759],"about_ca_topic_score_codex":0.018388199,"about_ca_topic_score_gemma":0.08606997,"teacher_disagreement_score":0.018388199,"about_ca_system_score_codex":0.00038917715,"about_ca_system_score_gemma":0.00021767389,"threshold_uncertainty_score":0.036562383},"labels":[],"label_agreement":null},{"id":"W2164522518","doi":"10.1002/2014gl062734","title":"Seasonal changes of CO<sub>2</sub>, CH<sub>4</sub>, N<sub>2</sub>O, and SF<sub>6</sub> in the upper troposphere/lower stratosphere over the Eurasian continent observed by commercial airliner","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Institute for Environmental Studies; York University","keywords":"Stratosphere; Troposphere; Tropopause; Atmospheric sciences; Altitude (triangle); Subsidence; Latitude; Environmental science; Seasonality; Climatology; Subtropics; Geology","score_opus":0.025314088160087872,"score_gpt":0.25520085529012343,"score_spread":0.22988676713003556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164522518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996697,0.000014765079,0.000023198798,0.000005095643,9.419701e-7,0.0000012640199,0.0001524772,0.0000041005987,0.00012850353],"genre_scores_gemma":[0.9993407,0.000018748493,0.000078310564,0.000005774191,0.0000028835882,0.0000029889275,0.00042210252,0.0000016657382,0.00012677358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.000007656022,0.0000050372196,0.000021784012,0.000016324391,0.000019936273],"domain_scores_gemma":[0.99979573,0.000021149921,0.00006769027,0.0000109446455,0.000058862228,0.000045596647],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012404734,0.00023957173,0.00017823052,0.00039551448,0.00026620895,0.00026266897,0.00017070863,0.00029175784,0.00067793747],"category_scores_gemma":[0.00017397442,0.00012235857,0.00015125006,0.0004219957,0.00016129031,0.0001954612,0.00018788698,0.00016487275,0.00014704553],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024423026,0.000038792306,0.9546263,0.000020349833,0.00006111052,0.00020933557,0.00037810748,0.00031487446,0.040402602,0.000012427176,0.00020224706,0.0034895753],"study_design_scores_gemma":[0.0000010078909,0.000019338331,0.9990858,6.9707716e-7,0.0000053176864,0.000020379857,0.00009419175,0.00013415286,0.0005711289,0.0000014746149,0.00006536865,0.0000011585495],"about_ca_topic_score_codex":0.016732736,"about_ca_topic_score_gemma":0.035428073,"teacher_disagreement_score":0.016732736,"about_ca_system_score_codex":0.0002678434,"about_ca_system_score_gemma":0.00010890418,"threshold_uncertainty_score":0.033270657},"labels":[],"label_agreement":null},{"id":"W2164695358","doi":"10.1002/2014gl062279","title":"Vertical velocities and turbulence in midlatitude anvil cirrus: A comparison between in situ aircraft measurements and ground‐based Doppler cloud radar retrievals","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy; National Science Foundation","keywords":"Cirrus; Middle latitudes; Radar; Turbulence; Doppler effect; Turbulence kinetic energy; Geology; Lidar; Doppler radar; Atmospheric sciences; Remote sensing; Meteorology; Environmental science; Physics; Astronomy; Aerospace engineering","score_opus":0.050508543848171834,"score_gpt":0.30870986405723233,"score_spread":0.2582013202090605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2164695358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988642,0.000031646272,0.0006956957,0.000006999595,0.0000055968144,0.000003052087,0.00014538903,0.000017714761,0.00022963894],"genre_scores_gemma":[0.9989524,0.000018912766,0.0005831039,0.0000045564852,0.0000048646957,0.0000021662188,0.00039750623,0.0000037546133,0.00003266658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997353,0.000055549575,0.000025004843,0.000074554766,0.00006977313,0.000039901195],"domain_scores_gemma":[0.9988311,0.00039795347,0.0002859992,0.00013137601,0.0002724478,0.000081129445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005552031,0.00020914157,0.00018341189,0.000847355,0.0001791885,0.0005659612,0.00020908297,0.00018892405,0.0002124287],"category_scores_gemma":[0.0017549585,0.00013645961,0.00016696469,0.0005440989,0.00013891455,0.00034450422,0.00021185081,0.00013954238,0.00007557642],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030823593,0.00016347245,0.9227241,0.000039318413,0.00012890252,0.00018557627,0.0002543178,0.0048175836,0.054604508,0.00013839683,0.00035042912,0.016285036],"study_design_scores_gemma":[0.00000843958,0.00008275535,0.9812825,0.0000054989614,0.000017485549,0.00005920014,0.00008918229,0.014004305,0.004190953,0.00003436104,0.00021813344,0.000007250148],"about_ca_topic_score_codex":0.006463438,"about_ca_topic_score_gemma":0.00926694,"teacher_disagreement_score":0.006463438,"about_ca_system_score_codex":0.0003008635,"about_ca_system_score_gemma":0.00014819075,"threshold_uncertainty_score":0.0128516555},"labels":[],"label_agreement":null},{"id":"W2165163954","doi":"10.1002/2014gl059651","title":"Coupling dry deposition to vegetation phenology in the Community Earth System Model: Implications for the simulation of surface O<sub>3</sub>","year":2014,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":157,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lockheed Martin (Canada)","funders":"","keywords":"Deposition (geology); Environmental science; Vegetation (pathology); Atmospheric sciences; Ozone; Phenology; Atmospheric model; Seasonality; Climatology; Leaf area index; Meteorology; Ecology; Geology; Geography","score_opus":0.04820932849886689,"score_gpt":0.30285313790212975,"score_spread":0.25464380940326287,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165163954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9740305,0.00019728055,0.019013407,0.00082329253,0.00008012377,0.00006623395,0.0008019895,0.0004293416,0.004557932],"genre_scores_gemma":[0.986463,0.00011921582,0.01158385,0.00015598205,0.000022257147,0.00007360541,0.00048248944,0.00009960504,0.0010000265],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998388,0.000056030636,0.000007750148,0.000028985072,0.000030422132,0.000038001454],"domain_scores_gemma":[0.999127,0.0003402197,0.0001075635,0.000059485767,0.00018018273,0.00018559978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074314704,0.00064018456,0.00056963717,0.00024432782,0.0006656535,0.0007501549,0.001719527,0.0015946697,0.00183736],"category_scores_gemma":[0.0032297368,0.00037402127,0.00067499606,0.00059895957,0.00049478665,0.0011014191,0.0009675439,0.0010291296,0.00019308315],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009878077,0.0001079712,0.010644523,0.00002695604,0.000051656014,0.00005496772,0.00004012303,0.98231137,0.0020782324,0.0010669616,0.00052377937,0.002994673],"study_design_scores_gemma":[0.000053780313,0.00001958295,0.0013300383,0.0000023058021,0.000008804205,0.00000577254,0.000017539836,0.99774677,0.0002392397,0.00032734667,0.00024044717,0.000008358914],"about_ca_topic_score_codex":0.105298266,"about_ca_topic_score_gemma":0.06453029,"teacher_disagreement_score":0.105298266,"about_ca_system_score_codex":0.0015040117,"about_ca_system_score_gemma":0.0020227463,"threshold_uncertainty_score":0.20937073},"labels":[],"label_agreement":null},{"id":"W2165664796","doi":"10.1029/2009gl038986","title":"Evidence for complete and partial surface renewal at an air‐water interface","year":2009,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Interface (matter); Surface (topology); Environmental science; Surface water; Geology; Meteorology; Geometry; Physics; Mathematics","score_opus":0.12089754971117177,"score_gpt":0.3459867403689226,"score_spread":0.2250891906577508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165664796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988703,0.0000787581,0.00061930204,0.000008303552,0.000001866192,0.0000026822336,0.000055446286,0.000012188925,0.0003510622],"genre_scores_gemma":[0.9996112,0.00001737877,0.00018388325,0.000005930771,0.0000018423167,0.0000032534101,0.00009457107,0.0000026202686,0.0000793321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970573,0.00002420776,0.000025402804,0.00007454567,0.00008341341,0.000086689586],"domain_scores_gemma":[0.9981382,0.00041876835,0.0006081833,0.0002547972,0.0002904466,0.0002896754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044428743,0.00015792807,0.00033728755,0.00042134468,0.00032955428,0.00065205817,0.00030535652,0.00032653354,0.00084959687],"category_scores_gemma":[0.0019627307,0.00026081555,0.0003360313,0.00029570947,0.0006309292,0.0005493608,0.0006948632,0.0003230257,0.00020572025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010494178,0.0000707454,0.71166724,0.00010633014,0.000115877316,0.00023430017,0.00043606412,0.0015974295,0.26849857,0.00047757316,0.0001639835,0.015582489],"study_design_scores_gemma":[0.000015418824,0.00024477317,0.97690624,0.000009178806,0.00004073003,0.00034050707,0.00031424555,0.0040625716,0.01729593,0.00030227096,0.00045361643,0.000014516618],"about_ca_topic_score_codex":0.0016870005,"about_ca_topic_score_gemma":0.0018811891,"teacher_disagreement_score":0.0016870005,"about_ca_system_score_codex":0.00018514064,"about_ca_system_score_gemma":0.00016762812,"threshold_uncertainty_score":0.0033543706},"labels":[],"label_agreement":null},{"id":"W2165786812","doi":"10.1002/grl.50680","title":"The sensitivity of hurricane frequency to ITCZ changes and radiatively forced warming in aquaplanet simulations","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Intertropical Convergence Zone; Equator; Climatology; Forcing (mathematics); Atmospheric sciences; Heat flux; Sea surface temperature; Environmental science; Walker circulation; Tropical cyclone; Amplitude; Convection; Radiative forcing; Geology; Physics; Meteorology; Heat transfer; Climate change; Precipitation; Oceanography; Latitude; Geodesy; Mechanics","score_opus":0.03382046938192221,"score_gpt":0.2925228328988032,"score_spread":0.25870236351688103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165786812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99711716,0.00002766571,0.00030983254,0.00014221849,0.000011085915,0.000011271366,0.00047487882,0.000055626413,0.0018502102],"genre_scores_gemma":[0.99894935,0.000020171525,0.0004082631,0.00004117248,0.0000028986792,0.000014313236,0.00029248148,0.00001711049,0.00025430482],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99971074,0.0001193841,0.000016404572,0.00005675319,0.000028044888,0.000068658075],"domain_scores_gemma":[0.99881136,0.0007374601,0.00012549268,0.00008407769,0.0000975018,0.00014409186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006092858,0.000539798,0.0006016025,0.00038396817,0.00064274156,0.00081379997,0.001426218,0.0011041343,0.0024224448],"category_scores_gemma":[0.0030641146,0.0005029931,0.00053623266,0.00056790974,0.00081209996,0.00062665535,0.0006278819,0.0010593105,0.00014419289],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000358866,0.00010032069,0.012416973,0.000022494094,0.00005718887,0.00012663982,0.000051678406,0.98401165,0.0011487578,0.0005541268,0.00047547917,0.0006757625],"study_design_scores_gemma":[0.00016005035,0.00013627243,0.009736829,0.000009614237,0.000025826037,0.000022470384,0.00010925753,0.9879629,0.0010888276,0.00041199732,0.0003054805,0.000030527885],"about_ca_topic_score_codex":0.091829985,"about_ca_topic_score_gemma":0.034319747,"teacher_disagreement_score":0.091829985,"about_ca_system_score_codex":0.0015258756,"about_ca_system_score_gemma":0.00081767444,"threshold_uncertainty_score":0.18259096},"labels":[],"label_agreement":null},{"id":"W2165900605","doi":"10.1029/2006gl027128","title":"First space‐based observations of formic acid (HCOOH): Atmospheric Chemistry Experiment austral spring 2004 and 2005 Southern Hemisphere tropical‐mid‐latitude upper tropospheric measurements","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Waterloo","funders":"","keywords":"Mixing ratio; Troposphere; Atmospheric sciences; Altitude (triangle); Formic acid; Latitude; Atmospheric chemistry; SCIAMACHY; Microwave Limb Sounder; Environmental science; Climatology; Ozone; Chemistry; Geology; Meteorology; Physics; Astronomy","score_opus":0.03657805186176277,"score_gpt":0.25950357463628587,"score_spread":0.2229255227745231,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165900605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856871,0.0004247705,0.0013949688,0.00024763297,0.000045124463,0.00012450533,0.0058847056,0.00013232483,0.0060589164],"genre_scores_gemma":[0.97640127,0.00036222802,0.008386968,0.00024390934,0.000041020903,0.00008685359,0.010597733,0.000018933039,0.003861187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977165,0.000017501088,0.00000912265,0.000051670468,0.00010061273,0.00004944623],"domain_scores_gemma":[0.99943346,0.000034803285,0.00009246879,0.000042943135,0.00023917723,0.00015706118],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044566402,0.00039067128,0.000281191,0.00051059,0.0009771767,0.00047458138,0.0002757083,0.00034724764,0.00076070393],"category_scores_gemma":[0.00045430442,0.000247748,0.00014932749,0.00039211634,0.00018304515,0.00032337577,0.00039779156,0.0005174352,0.00017038827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0030372622,0.00080352166,0.73305124,0.00019758943,0.00032818594,0.00056005217,0.001283931,0.0015609062,0.17989977,0.00061416725,0.009697537,0.068965785],"study_design_scores_gemma":[0.00009353578,0.0004225687,0.9613888,0.000015050084,0.00005221713,0.00013969725,0.00015767952,0.0011993133,0.022727061,0.00010205304,0.013682044,0.000019838884],"about_ca_topic_score_codex":0.079794325,"about_ca_topic_score_gemma":0.16797227,"teacher_disagreement_score":0.079794325,"about_ca_system_score_codex":0.0011160526,"about_ca_system_score_gemma":0.0009576656,"threshold_uncertainty_score":0.1586597},"labels":[],"label_agreement":null},{"id":"W2165984004","doi":"10.1029/2006gl027493","title":"Sensitivity of global river discharges under Holocene and future climate conditions","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":131,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Center for Atmospheric Research","keywords":"Holocene; Climate change; Discharge; Environmental science; Proxy (statistics); Drainage basin; Global warming; Amazon rainforest; Climatology; Hydrology (agriculture); Physical geography; Geography; Geology; Oceanography; Ecology","score_opus":0.01318001552318238,"score_gpt":0.2823521278345786,"score_spread":0.2691721123113962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2165984004","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99770075,0.000059656155,0.00050506287,0.00011955885,0.000005964998,0.0000040036334,0.000492107,0.00003239529,0.0010805806],"genre_scores_gemma":[0.99928457,0.00006586982,0.00008466068,0.000018007002,0.0000026520236,0.0000030111178,0.00041710195,0.0000054467496,0.000118736556],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985564,0.00003828638,0.000010449529,0.00003618882,0.000017626395,0.000041680254],"domain_scores_gemma":[0.99962795,0.00018709518,0.00007258941,0.000040976156,0.00003713648,0.00003416849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034522061,0.00017467237,0.00015065903,0.00029156846,0.00013349547,0.0005767926,0.00016442563,0.00038198952,0.0010695155],"category_scores_gemma":[0.001741539,0.00016345474,0.0004003923,0.0004998844,0.00034141022,0.00051984616,0.00042373347,0.00024356192,0.00009202188],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002745008,0.00009612402,0.5221874,0.00006891354,0.000326209,0.00025698022,0.0002829683,0.45614848,0.005413868,0.0015436645,0.0012992731,0.012101609],"study_design_scores_gemma":[0.00004171333,0.00017684675,0.8226547,0.000015901793,0.00009821184,0.00018933356,0.00039795737,0.16832528,0.0028227316,0.002749901,0.0024774247,0.000049992446],"about_ca_topic_score_codex":0.015923822,"about_ca_topic_score_gemma":0.012339929,"teacher_disagreement_score":0.015923822,"about_ca_system_score_codex":0.00081139687,"about_ca_system_score_gemma":0.00022445124,"threshold_uncertainty_score":0.031662285},"labels":[],"label_agreement":null},{"id":"W2166020037","doi":"10.1002/2014gl062661","title":"Ice motion of the Patagonian Icefields of South America: 1984–2014","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":96,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; European Space Agency; Japan Aerospace Exploration Agency; National Aeronautics and Space Administration","keywords":"Geology; Glacier; Ice stream; Ice sheet; Climatology; Geomorphology; Geodesy; Physical geography; Cryosphere; Sea ice; Geography","score_opus":0.06425236208458049,"score_gpt":0.28365608067016046,"score_spread":0.21940371858557997,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166020037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9894196,0.00031451602,0.00017060405,0.00010171458,0.000011421903,0.000015914737,0.007302569,0.000029914787,0.002633791],"genre_scores_gemma":[0.99162626,0.0001789278,0.00042443813,0.00003195358,0.00001554247,0.000017606015,0.0068298304,0.000008768876,0.0008667728],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.000012358083,0.000006239676,0.000027250873,0.000027538883,0.000025089028],"domain_scores_gemma":[0.9995933,0.000026736789,0.00014602282,0.000033781133,0.00015601046,0.00004417738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020233363,0.00019453082,0.00015099556,0.0014522155,0.00036129268,0.00047525048,0.0002144358,0.00015376475,0.00090629363],"category_scores_gemma":[0.00043203845,0.00011318385,0.00016207207,0.001827315,0.00025582075,0.00025138134,0.00034975953,0.00019419278,0.00016414569],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002281054,0.000037844547,0.95981365,0.000097812816,0.00018692283,0.00025629415,0.0009211604,0.0027724605,0.0051335837,0.000095997275,0.0054232646,0.025032884],"study_design_scores_gemma":[0.0000019190925,0.000005020847,0.99762064,0.0000044928447,0.0000044837016,0.000024567804,0.00012316747,0.00021698065,0.00013847591,0.0000066308435,0.0018516071,0.0000020076657],"about_ca_topic_score_codex":0.27138445,"about_ca_topic_score_gemma":0.42185327,"teacher_disagreement_score":0.27138445,"about_ca_system_score_codex":0.0012441789,"about_ca_system_score_gemma":0.00085789216,"threshold_uncertainty_score":0.5396097},"labels":[],"label_agreement":null},{"id":"W2166211519","doi":"10.1029/2005gl024239","title":"Multidecadal North Atlantic climate variability and its effect on North American salmon abundance","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Atlantic multidecadal oscillation; Fishing; Abundance (ecology); Climate change; Environmental science; Stock (firearms); Oceanography; Pacific decadal oscillation; Sea surface temperature; Overwintering; Fish stock; Fishery; Climatology; Geography; Ecology; Biology; Geology","score_opus":0.021059148523861888,"score_gpt":0.2988473039816631,"score_spread":0.2777881554578012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166211519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880433,0.00015971778,0.00013108838,0.00022981096,0.000008572487,8.6879777e-7,0.00019370837,0.000008511529,0.00046345763],"genre_scores_gemma":[0.9996383,0.00007264336,0.00003559954,0.00002362968,0.0000051083084,0.0000014987824,0.000088644825,0.0000018372643,0.00013264907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998776,0.000037883914,0.0000053732556,0.000031569718,0.000015223374,0.000032348158],"domain_scores_gemma":[0.9994349,0.00018651538,0.0001626861,0.000053856664,0.00006764151,0.00009445849],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032631008,0.00013559873,0.00014063666,0.00021338524,0.00021588539,0.00039815292,0.00011926182,0.00023346284,0.0010702723],"category_scores_gemma":[0.0011513365,0.00010287458,0.0002441681,0.0002410121,0.00017092869,0.00022272216,0.00047679324,0.00033032527,0.000106847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014618623,0.000035759414,0.98587114,0.000012868958,0.00015501217,0.0000837326,0.000102259604,0.004313557,0.002045553,0.00019521381,0.00068986934,0.0063489107],"study_design_scores_gemma":[0.0000021993596,0.000012718016,0.9971103,0.0000028110044,0.00001486993,0.000017550628,0.000060268205,0.0024032234,0.000061647486,0.000061881816,0.00024966188,0.0000030257497],"about_ca_topic_score_codex":0.0613191,"about_ca_topic_score_gemma":0.13302872,"teacher_disagreement_score":0.0613191,"about_ca_system_score_codex":0.0007039282,"about_ca_system_score_gemma":0.00040031123,"threshold_uncertainty_score":0.1219244},"labels":[],"label_agreement":null},{"id":"W2166574479","doi":"10.1029/2005gl025595","title":"Wildfires threaten mercury stocks in northern soils","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":148,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Forest Service","funders":"","keywords":"Mercury (programming language); Environmental science; Boreal; Peat; Wetland; Methylmercury; Climate change; Soil water; Taiga; Environmental chemistry; Ecology; Geology; Soil science; Geography; Oceanography; Bioaccumulation; Forestry; Chemistry","score_opus":0.030905945789428575,"score_gpt":0.31171795951852965,"score_spread":0.2808120137291011,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166574479","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989888,0.000030941646,0.000051944415,0.000011024768,3.4477432e-7,9.543394e-7,0.000049664224,0.00000718236,0.0008591025],"genre_scores_gemma":[0.999619,0.00004108296,0.00009779874,0.000006308652,9.032603e-7,0.0000010748661,0.00006664704,0.0000016359113,0.00016547278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.0000089423975,0.0000040041264,0.000022151482,0.00003847994,0.00004120731],"domain_scores_gemma":[0.99980086,0.000020244572,0.00007491389,0.000013611358,0.000054563166,0.000035722976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015779547,0.00020452778,0.00015177969,0.0004681908,0.00082936947,0.0006567655,0.00016587104,0.00012490418,0.00068855035],"category_scores_gemma":[0.00038349262,0.00011341397,0.00013872962,0.0005671324,0.00032558944,0.0002765365,0.00034306035,0.00010993829,0.00009669145],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018728952,0.000042971176,0.9552614,0.00002282317,0.000067532266,0.00015283356,0.00073234487,0.0019343552,0.019974012,0.00028958297,0.00024684946,0.021087972],"study_design_scores_gemma":[0.0000030956226,0.000019663912,0.9963928,0.0000041024146,0.000014434235,0.00006323668,0.0004408125,0.0008420182,0.001427939,0.00017777446,0.0006104509,0.0000038157655],"about_ca_topic_score_codex":0.3157095,"about_ca_topic_score_gemma":0.54831064,"teacher_disagreement_score":0.3157095,"about_ca_system_score_codex":0.0011786608,"about_ca_system_score_gemma":0.0009157407,"threshold_uncertainty_score":0.6277437},"labels":[],"label_agreement":null},{"id":"W2166585109","doi":"10.1002/2013gl058628","title":"Modulation of the seasonal footprinting mechanism by the boreal spring Arctic Oscillation","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Natural Science Foundation of China","keywords":"Footprinting; Climatology; Spring (device); Arctic oscillation; Boreal; Oscillation (cell signaling); Arctic; Environmental science; The arctic; Subtropics; Modulation (music); Atmospheric sciences; Oceanography; Chemistry; Geology; Physics; Biology; Ecology","score_opus":0.029076960066522998,"score_gpt":0.2716503891410956,"score_spread":0.24257342907457263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166585109","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99660337,0.000107118525,0.0012720901,0.00008743009,0.000016001999,0.0000049045025,0.00009014531,0.000035180186,0.0017836776],"genre_scores_gemma":[0.99972767,0.000022588358,0.00014772112,0.0000071700433,0.0000047309222,0.0000013969624,0.000023126297,0.0000024121077,0.00006305605],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999355,0.000023740127,0.0000054167253,0.000015494947,0.000009245574,0.000010638161],"domain_scores_gemma":[0.99971205,0.000071104005,0.000103604805,0.0000367528,0.00004182034,0.00003473472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034714089,0.00015422786,0.00014641201,0.00015800082,0.0001364639,0.00033087714,0.00018709467,0.000119386306,0.0009649598],"category_scores_gemma":[0.0007355073,0.00010165184,0.00017915826,0.00014798882,0.00020226343,0.00024823457,0.00022124883,0.000123946,0.00006703053],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005399119,0.00012583971,0.853926,0.000059254446,0.00021907352,0.0002085337,0.0002938405,0.008240592,0.09939258,0.0027960874,0.0007693322,0.03342882],"study_design_scores_gemma":[0.000018617022,0.0000817613,0.97909343,0.0000071692507,0.000027526981,0.00009626819,0.00011424337,0.017012052,0.0018339722,0.0009465817,0.0007569527,0.000011521688],"about_ca_topic_score_codex":0.0038365289,"about_ca_topic_score_gemma":0.0035331673,"teacher_disagreement_score":0.0038365289,"about_ca_system_score_codex":0.00015563352,"about_ca_system_score_gemma":0.0001401662,"threshold_uncertainty_score":0.007628441},"labels":[],"label_agreement":null},{"id":"W2166974154","doi":"10.1029/2007gl031267","title":"Stability of hydrated minerals on Mars","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; COM DEV International; MPB Technologies & Communications (Canada); University of Winnipeg","funders":"","keywords":"Mars Exploration Program; Astrobiology; Geology; Mineralogy; Stability (learning theory); Geochemistry; Earth science; Geophysics; Physics","score_opus":0.05703711643067451,"score_gpt":0.32590225855429056,"score_spread":0.26886514212361606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2166974154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905604,0.00023100503,0.00017105455,0.000015256251,0.000002510711,0.0000027319998,0.00011366026,0.000015428463,0.00039231344],"genre_scores_gemma":[0.9992581,0.00011393331,0.00020017632,0.0000097147185,0.0000034108696,0.0000032090595,0.000217517,0.0000048412353,0.00018899249],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998617,0.000022076476,0.0000070976125,0.000045569315,0.00004065724,0.00002285165],"domain_scores_gemma":[0.9998349,0.000024646602,0.00004028786,0.00002423119,0.000050279064,0.000025665637],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017638537,0.00019481183,0.00018337603,0.0005330619,0.0005899725,0.0005082275,0.00040004187,0.00041248737,0.0011163115],"category_scores_gemma":[0.00036579222,0.00020451374,0.00019393096,0.00019234998,0.0003899537,0.00033853488,0.00054531044,0.00025297902,0.00017529572],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005597904,0.000029458159,0.024272276,0.000105995736,0.000085050975,0.0001532862,0.00023704281,0.0012812924,0.96695596,0.00020276045,0.00009233957,0.006024826],"study_design_scores_gemma":[0.00006631928,0.0012229553,0.3123506,0.00003530019,0.000104752806,0.0009343802,0.0009554503,0.0048710075,0.67043215,0.00077187974,0.008202476,0.00005266599],"about_ca_topic_score_codex":0.0010109508,"about_ca_topic_score_gemma":0.0005631799,"teacher_disagreement_score":0.0011163115,"about_ca_system_score_codex":0.00022829697,"about_ca_system_score_gemma":0.00009442425,"threshold_uncertainty_score":0.0037344098},"labels":[],"label_agreement":null},{"id":"W2167030887","doi":"10.1029/2004gl020860","title":"Penetration of the 1990s warm temperature anomaly of Atlantic Water in the Canada Basin","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"North Pacific Marine Science Organization","funders":"JST-Mirai Program; Fisheries and Oceans Canada; National Science Foundation","keywords":"Geology; Structural basin; Oceanography; Advection; Ocean gyre; Seafloor spreading; Temperature salinity diagrams; Ridge; Salinity; Climatology; Geomorphology; Paleontology","score_opus":0.016846934168071828,"score_gpt":0.24554768236736718,"score_spread":0.22870074819929537,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2167030887","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944898,0.00044874262,0.00005135746,0.00012078233,0.0000041544376,0.0000036854467,0.0006032261,0.000008758125,0.0042694933],"genre_scores_gemma":[0.99868137,0.00030385974,0.00006076354,0.000030649317,0.0000019659376,0.0000014732029,0.000428618,0.0000015765868,0.00048960705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982315,0.0000075530606,0.0000061037654,0.00002377339,0.0000632023,0.00007624139],"domain_scores_gemma":[0.99940014,0.000032609863,0.000100291356,0.000013206624,0.00030361596,0.00015021955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019734679,0.0001668757,0.00013664059,0.001005299,0.0009225176,0.0009604691,0.0002117979,0.00026138738,0.0005881234],"category_scores_gemma":[0.00088228565,0.00012751977,0.00015212715,0.0011242175,0.0004364829,0.00029651492,0.0006318992,0.00031674508,0.00007509473],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022098771,0.000026337824,0.96775895,0.00005604955,0.000081885475,0.000286059,0.0017079221,0.0017076022,0.008110301,0.00085904496,0.0012869064,0.017898073],"study_design_scores_gemma":[0.0000020559992,0.000006433518,0.99770147,0.0000096788035,0.000006470689,0.000029352399,0.0003509257,0.0003221473,0.00028791578,0.000019647645,0.0012599749,0.000003962332],"about_ca_topic_score_codex":0.94856983,"about_ca_topic_score_gemma":0.9817727,"teacher_disagreement_score":0.051430166,"about_ca_system_score_codex":0.0108119035,"about_ca_system_score_gemma":0.006267639,"threshold_uncertainty_score":0.103466034},"labels":[],"label_agreement":null},{"id":"W2168212007","doi":"10.1002/2014gl062773","title":"China experiencing the recent warming hiatus","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Hiatus; Climatology; Mean radiant temperature; Environmental science; Context (archaeology); Dryness; Global warming; Climate change; Atmospheric sciences; Geography; Geology; Oceanography; Biology","score_opus":0.08752064380217166,"score_gpt":0.3398770999990178,"score_spread":0.2523564561968461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168212007","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982728,0.00009373467,0.00006285443,0.0000797821,0.0000067774954,0.0000045648903,0.0010112124,0.000011446884,0.00045668587],"genre_scores_gemma":[0.9977684,0.0000797532,0.000047378096,0.000028068454,0.000015725169,0.0000056995164,0.0018786473,0.000001974982,0.00017432247],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998486,0.000013661218,0.000018099761,0.00003664106,0.000022963177,0.000059976974],"domain_scores_gemma":[0.99964225,0.00001936869,0.00014542999,0.000042356176,0.0000737848,0.000076807504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041263248,0.00031747276,0.00036080962,0.0010665414,0.00047244757,0.00064896734,0.0002426413,0.0003018009,0.0011641374],"category_scores_gemma":[0.00043183647,0.00016730446,0.00037661384,0.0014532517,0.00032745316,0.00045005104,0.0006754987,0.00022055798,0.00012218229],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000115071736,0.000022342676,0.9855759,0.000052160747,0.00015406526,0.00040018043,0.00032745954,0.002551176,0.002555949,0.0003334115,0.0013131902,0.006599188],"study_design_scores_gemma":[0.000003150454,0.000014050849,0.99820685,0.0000026481935,0.000017968996,0.000036193116,0.000106386906,0.00073755125,0.00011285907,0.000030651936,0.0007273995,0.0000042815454],"about_ca_topic_score_codex":0.038753048,"about_ca_topic_score_gemma":0.051587276,"teacher_disagreement_score":0.038753048,"about_ca_system_score_codex":0.00089871784,"about_ca_system_score_gemma":0.0007045144,"threshold_uncertainty_score":0.07705492},"labels":[],"label_agreement":null},{"id":"W2168214100","doi":"10.1029/1999gl011173","title":"Interannual changes of total ozone and northern hemisphere circulation patterns","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Northern Hemisphere; Geopotential height; Arctic oscillation; Environmental science; Atmospheric sciences; Stratosphere; Polar vortex; Atmospheric circulation; Ozone layer; Ozone; Ozone depletion; Tropospheric ozone; Troposphere; Arctic; Precipitation; Geology; Geography; Oceanography; Meteorology","score_opus":0.025623997599127705,"score_gpt":0.27180247272247643,"score_spread":0.24617847512334873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168214100","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99855655,0.00009952374,0.00010934121,0.000037931513,0.000005360607,0.0000013833693,0.00053585117,0.00001214103,0.00064202474],"genre_scores_gemma":[0.9987717,0.00006979381,0.00007034591,0.000011103483,0.0000071926293,0.0000032269193,0.0006477189,0.0000058658748,0.00041302023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989855,0.00002124406,0.000004846228,0.000028156934,0.0000144882815,0.000032601685],"domain_scores_gemma":[0.99973255,0.000049288934,0.00010258471,0.00003262513,0.000035822166,0.00004705462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020648213,0.00011389962,0.00011382341,0.00032441484,0.00012327285,0.00032300508,0.00009819946,0.00013614235,0.0012388062],"category_scores_gemma":[0.0006900599,0.00008386254,0.0001365135,0.00041156964,0.00008920155,0.00016583974,0.00018232696,0.000115287585,0.00017698393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012829415,0.000024244644,0.98273736,0.000013268571,0.00016241118,0.0000672256,0.00016683301,0.0010630023,0.0039730757,0.00020024965,0.0006673983,0.010796711],"study_design_scores_gemma":[0.0000010232652,0.000004180402,0.9993443,7.599716e-7,0.00000705265,0.0000094634,0.000015387226,0.00033933867,0.00007294712,0.000019898367,0.00018494463,7.5624604e-7],"about_ca_topic_score_codex":0.018000504,"about_ca_topic_score_gemma":0.02925937,"teacher_disagreement_score":0.018000504,"about_ca_system_score_codex":0.00027090707,"about_ca_system_score_gemma":0.00016423431,"threshold_uncertainty_score":0.035791457},"labels":[],"label_agreement":null},{"id":"W2168331175","doi":"10.1029/2001gl012928","title":"Paleomagnetic pole positions and pole reversals of Mars","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Paleomagnetism; Mars Exploration Program; Geology; RADIUS; North pole; Geophysics; Magnetic anomaly; Geodesy; Geomagnetic pole; Physics; Earth's magnetic field; Geometry; Magnetic field; Astrobiology; Geography; Mathematics","score_opus":0.028697328428677657,"score_gpt":0.29555903924110455,"score_spread":0.2668617108124269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168331175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99868435,0.000034953187,0.00036381808,0.000017262042,0.0000019015911,0.0000015547339,0.00006967691,0.000021283722,0.0008052396],"genre_scores_gemma":[0.9995683,0.000020213898,0.00017843545,0.0000014912607,0.0000028050024,0.0000015240473,0.00012007086,0.0000055403625,0.0001016396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999447,0.000009287371,0.0000023293192,0.000024027384,0.000008546109,0.000011056154],"domain_scores_gemma":[0.9998704,0.000022258222,0.000033710767,0.000018718367,0.00003094132,0.000023922852],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012824814,0.00018422425,0.00019793719,0.000875801,0.00040249963,0.0006114688,0.00019484527,0.00022913916,0.0010274955],"category_scores_gemma":[0.00054067624,0.0002249202,0.0003415966,0.00046890613,0.00028147854,0.00018787445,0.00023242341,0.0002404995,0.0002841219],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078644365,0.00007298617,0.78315145,0.000050851784,0.00028299418,0.00038758136,0.00083432073,0.13326062,0.054098237,0.002383666,0.0009611998,0.023729606],"study_design_scores_gemma":[0.000057784913,0.00007981843,0.89964575,0.000011277515,0.00005546759,0.00017203581,0.0001504845,0.093018115,0.003145759,0.0010951171,0.0025415872,0.000026777316],"about_ca_topic_score_codex":0.005975967,"about_ca_topic_score_gemma":0.004258597,"teacher_disagreement_score":0.005975967,"about_ca_system_score_codex":0.00029289717,"about_ca_system_score_gemma":0.0001802525,"threshold_uncertainty_score":0.011882365},"labels":[],"label_agreement":null},{"id":"W2168371433","doi":"10.1029/2005gl023400","title":"Disappearance of Pacific Water in the northwestern Fram Strait","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Oceanography; Hydrography; Halocline; Archipelago; Arctic; Pacific ocean; Geology; Thermohaline circulation; The arctic; Water mass; Climatology; Salinity","score_opus":0.02146447394824547,"score_gpt":0.2676917566463671,"score_spread":0.2462272826981216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168371433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972657,0.00032828873,0.00003287303,0.00012991806,0.000014994153,0.0000018188999,0.00023584042,0.0000041567114,0.0019864568],"genre_scores_gemma":[0.99736255,0.00048276992,0.00011665942,0.000086585846,0.000020127753,0.0000029097137,0.00068808947,0.0000045624683,0.0012356493],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998926,0.000009965095,0.000008849777,0.000034680383,0.000023512222,0.000030396535],"domain_scores_gemma":[0.9996032,0.00003772777,0.00012040461,0.00002708834,0.00013829177,0.000073347364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002293258,0.00014075285,0.00020070828,0.00071589666,0.00091881846,0.0008508295,0.00020649964,0.00031675113,0.0008618802],"category_scores_gemma":[0.000712393,0.00014449624,0.0001710653,0.00089898973,0.0007061027,0.00044957228,0.0004919084,0.00043333933,0.00019838424],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053573016,0.000032443004,0.9588987,0.00007706443,0.00006021414,0.0008573517,0.0022927746,0.00012213236,0.010598832,0.00021262735,0.0010880111,0.02522402],"study_design_scores_gemma":[0.0000037183313,0.000036279154,0.99460053,0.000014451207,0.000014063274,0.00012424953,0.0009116666,0.000036453883,0.0006294808,0.0000147552155,0.0036114156,0.0000029763817],"about_ca_topic_score_codex":0.091985,"about_ca_topic_score_gemma":0.16595028,"teacher_disagreement_score":0.091985,"about_ca_system_score_codex":0.0011583648,"about_ca_system_score_gemma":0.0012576837,"threshold_uncertainty_score":0.18289918},"labels":[],"label_agreement":null},{"id":"W2168445329","doi":"10.1029/2004gl022003","title":"Stratospheric effects of energetic particle precipitation in 2003–2004","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":310,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Northern Hemisphere; Stratosphere; Atmospheric sciences; Precipitation; Polar vortex; Environmental science; Context (archaeology); Atmosphere (unit); Latitude; Climatology; Storm; High latitude; Meteorology; Geology; Physics","score_opus":0.015519626279541846,"score_gpt":0.26967131665661553,"score_spread":0.2541516903770737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2168445329","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976561,0.00021983299,0.00005101314,0.00022137297,0.000022683102,0.000004013906,0.0008711171,0.00002391526,0.0009298448],"genre_scores_gemma":[0.99802953,0.000098949226,0.00007492123,0.00011299366,0.000017023474,0.0000052635673,0.0012454303,0.000005432029,0.0004104773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990463,0.00001814824,0.00000654795,0.000021437922,0.00001508139,0.00003409259],"domain_scores_gemma":[0.9997602,0.00003721273,0.00007335119,0.000020033316,0.00005884633,0.000050360915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023177126,0.0002896575,0.00035245123,0.0002818846,0.0004535057,0.0006492271,0.00021530324,0.0005852074,0.0005753499],"category_scores_gemma":[0.00039493275,0.00014071648,0.00027759315,0.00041101305,0.00017966788,0.00019328007,0.00029350823,0.00038551854,0.00016828201],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0083418675,0.0006474671,0.8634543,0.0002007633,0.00090274843,0.0018944197,0.0010284302,0.005563195,0.08415664,0.0003359044,0.007478679,0.025995573],"study_design_scores_gemma":[0.000021386708,0.000114579816,0.99539477,0.000005735605,0.0000495218,0.00011922678,0.00015765817,0.0005486195,0.0021776007,0.00003209848,0.0013714775,0.0000072263924],"about_ca_topic_score_codex":0.05223704,"about_ca_topic_score_gemma":0.07593947,"teacher_disagreement_score":0.05223704,"about_ca_system_score_codex":0.0010519215,"about_ca_system_score_gemma":0.00037667147,"threshold_uncertainty_score":0.10386598},"labels":[],"label_agreement":null},{"id":"W2169174396","doi":"10.1029/2005gl022913","title":"Abrupt climate change and variability in the past four millennia of the southern Vancouver Island, Canada","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Royal British Columbia Museum; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; University of Victoria","keywords":"Climate change; Climatology; Geology; Oceanography; Geography; Physical geography","score_opus":0.03464179563462081,"score_gpt":0.25713550833529825,"score_spread":0.22249371270067744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169174396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9842866,0.001906502,0.00010153325,0.00068380835,0.00002634583,0.000017643142,0.007998561,0.000018913677,0.0049600597],"genre_scores_gemma":[0.9933159,0.0012015498,0.0001566704,0.00009126093,0.000007633572,0.000009362691,0.0029855664,0.000008394472,0.0022237655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997876,0.000010982711,0.000012762907,0.000041722196,0.000065018394,0.00008186224],"domain_scores_gemma":[0.99915624,0.00003811291,0.00009375163,0.000023261611,0.0005216982,0.00016693091],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022606138,0.00019650484,0.00024370827,0.0013983466,0.0021835382,0.0015173337,0.0005331488,0.00031034558,0.0019519839],"category_scores_gemma":[0.00088193134,0.00020635576,0.00018766352,0.0034045277,0.0004382427,0.00028562767,0.0007135757,0.00049443,0.00023391313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000656084,0.00002344948,0.9718587,0.00006470128,0.00013458836,0.00019729078,0.0016725379,0.0006703953,0.0010760853,0.00033301426,0.004767742,0.01913589],"study_design_scores_gemma":[0.0000021863214,0.0000021430078,0.9958305,0.000022098695,0.000010633835,0.00002662159,0.0008566716,0.00020673912,0.000043816763,0.000023464945,0.002967945,0.000007331173],"about_ca_topic_score_codex":0.99616516,"about_ca_topic_score_gemma":0.99862206,"teacher_disagreement_score":0.0135695515,"about_ca_system_score_codex":0.0135695515,"about_ca_system_score_gemma":0.01296427,"threshold_uncertainty_score":0.098454416},"labels":[],"label_agreement":null},{"id":"W2169265549","doi":"10.1029/2007gl030519","title":"Joint inversion of teleseismic receiver functions and magnetotelluric data using a genetic algorithm: Are seismic velocities and electrical conductivities compatible?","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Magnetotellurics; Lithosphere; Geology; Inversion (geology); Seismology; Geophysics; Mantle (geology); Joint (building); Tectonics; Geodesy; Electrical resistivity and conductivity","score_opus":0.09730205146205656,"score_gpt":0.30813858453539184,"score_spread":0.21083653307333527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169265549","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48980597,0.00011583299,0.50846446,0.0002357049,0.000015471567,0.000038318725,0.000033993674,0.00026633346,0.0010238916],"genre_scores_gemma":[0.82803035,0.000044083765,0.17124663,0.00004821656,0.000013275914,0.000046958616,0.00008315691,0.000032059233,0.00045535885],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993562,0.00031591541,0.000029351299,0.00013311887,0.00009832265,0.0000671243],"domain_scores_gemma":[0.99792635,0.0013791332,0.00027850753,0.0001429504,0.00022275907,0.00005027602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00273868,0.0006687416,0.00061969546,0.0006833405,0.00039102638,0.00083983,0.0007037578,0.00091801595,0.0003036489],"category_scores_gemma":[0.009737631,0.000383493,0.00044893226,0.0007746469,0.00077625754,0.00087598927,0.00061487884,0.000499661,0.00012306814],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043185655,0.00021062953,0.032858625,0.00003840735,0.0002902341,0.00010844036,0.00029790387,0.7488843,0.01165677,0.008583671,0.00028265463,0.19635645],"study_design_scores_gemma":[0.000029639925,0.00003783095,0.0016373851,0.000004483682,0.00002262827,0.000020549722,0.000026759366,0.9947017,0.0014817334,0.0019202807,0.00010810942,0.00000882703],"about_ca_topic_score_codex":0.0068766586,"about_ca_topic_score_gemma":0.0066243294,"teacher_disagreement_score":0.0068766586,"about_ca_system_score_codex":0.00057492865,"about_ca_system_score_gemma":0.0012600932,"threshold_uncertainty_score":0.01448375},"labels":[],"label_agreement":null},{"id":"W2169367869","doi":"10.1029/2012gl051241","title":"Greenland ice core evidence for spatial and temporal variability of the Atlantic Multidecadal Oscillation","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Atlantic multidecadal oscillation; Climatology; North Atlantic oscillation; Ice core; Groenlandia; Geology; Arctic oscillation; Pacific decadal oscillation; Sea ice; Arctic ice pack; Arctic; Proxy (statistics); Oceanography; Sea surface temperature; Ice sheet; Northern Hemisphere","score_opus":0.10197937507906073,"score_gpt":0.3473870968069177,"score_spread":0.24540772172785696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169367869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947909,0.0004059191,0.000072840856,0.00015767271,0.000014034385,0.0000048907864,0.002283062,0.000013354818,0.0022574698],"genre_scores_gemma":[0.99698406,0.00015051868,0.00014684694,0.00010043129,0.000015365955,0.000008903545,0.0022316487,0.000006423756,0.000355858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990845,0.000011808316,0.0000101936275,0.000025375119,0.000020367113,0.000023674147],"domain_scores_gemma":[0.99932253,0.000081663486,0.00029254166,0.000052825417,0.0001556808,0.0000947492],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029426898,0.00010035316,0.00010210357,0.00080908684,0.00018545991,0.00032219713,0.00013368884,0.0001153109,0.00082071696],"category_scores_gemma":[0.00065297895,0.000067788475,0.00009897834,0.00075695093,0.00016874347,0.00016409093,0.00027688054,0.00010749707,0.00011953301],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009175852,0.000019205001,0.9863209,0.000024418947,0.00007880699,0.000093432944,0.00018271628,0.0001695944,0.005162136,0.00015353756,0.0012656212,0.0064379093],"study_design_scores_gemma":[0.0000010997223,0.0000030348992,0.99956673,0.0000028103266,0.0000029363823,0.000009928491,0.000025771096,0.00005241589,0.000034532535,0.000009493514,0.0002906826,6.236453e-7],"about_ca_topic_score_codex":0.044694338,"about_ca_topic_score_gemma":0.11690611,"teacher_disagreement_score":0.044694338,"about_ca_system_score_codex":0.000497928,"about_ca_system_score_gemma":0.00031647523,"threshold_uncertainty_score":0.08886838},"labels":[],"label_agreement":null},{"id":"W2169420869","doi":"10.1029/2006gl029165","title":"Deep resistivity structure of the northwest Indian Himalaya and its tectonic implications","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Geology; Magnetotellurics; Fibrous joint; Crust; Electrical resistivity and conductivity; Indus; Tectonics; Seismology; Sedimentary rock; Petrology; Geophysics; Geomorphology; Geochemistry","score_opus":0.024339747920178727,"score_gpt":0.29952713285688165,"score_spread":0.2751873849367029,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169420869","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975879,0.00013440612,0.00029057148,0.00005297229,0.0000017434063,0.0000027719332,0.00021648908,0.00002111457,0.0016919009],"genre_scores_gemma":[0.99952936,0.000048169928,0.00013162529,0.000004000569,0.000002354881,0.0000010221526,0.00009959059,0.000001428967,0.00018258857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994063,0.000008421157,0.0000038272747,0.000012543575,0.000012612344,0.000021973738],"domain_scores_gemma":[0.9998017,0.000036496152,0.000049464976,0.000018007695,0.000058315403,0.000036080728],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007708919,0.00016599399,0.00012231925,0.0011909464,0.00033372644,0.0007363036,0.00022805156,0.00013599703,0.00070631533],"category_scores_gemma":[0.00029240944,0.00013820808,0.0000777194,0.0015338128,0.00034055856,0.00023342167,0.0003722897,0.0001882842,0.00010827998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015444092,0.00005732851,0.9046022,0.00007701398,0.000059816317,0.0012482466,0.0026057782,0.005350803,0.043789323,0.0012554958,0.00033684744,0.040462725],"study_design_scores_gemma":[0.0000018489346,0.000011771574,0.9976949,0.000003995988,0.000006552905,0.00012071427,0.00032529535,0.0009565249,0.00042335477,0.000106498585,0.00034319723,0.000005306947],"about_ca_topic_score_codex":0.031134853,"about_ca_topic_score_gemma":0.03592312,"teacher_disagreement_score":0.031134853,"about_ca_system_score_codex":0.0005526722,"about_ca_system_score_gemma":0.0003136652,"threshold_uncertainty_score":0.06190723},"labels":[],"label_agreement":null},{"id":"W2169447972","doi":"10.1029/1999gl011111","title":"A regime view of northern hemisphere atmospheric variability and change under global warming","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Arctic oscillation; Climatology; Northern Hemisphere; Troposphere; North Atlantic oscillation; Forcing (mathematics); Environmental science; Atmospheric circulation; Arctic; Ridge; Atmospheric sciences; Oscillation (cell signaling); Geology; Oceanography","score_opus":0.04201989452454604,"score_gpt":0.3014534396768557,"score_spread":0.25943354515230965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169447972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.68997,0.004895784,0.13636188,0.0031082777,0.00018934051,0.00009654175,0.004359864,0.00061500596,0.16040328],"genre_scores_gemma":[0.9894433,0.0012742208,0.0055795894,0.00017910708,0.00011031342,0.000051899875,0.00029112207,0.000040648272,0.0030298491],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999136,0.000021845895,0.0000041532385,0.00002720415,0.000017081282,0.000016166296],"domain_scores_gemma":[0.99990785,0.00002016292,0.000024048002,0.000018068824,0.000014888204,0.000014891243],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020495882,0.00013441707,0.00011900145,0.0007850444,0.00027875212,0.0010658705,0.00026516255,0.00024423443,0.0035096717],"category_scores_gemma":[0.0004254559,0.000102998936,0.0003003674,0.00055242964,0.0006231997,0.00072033465,0.00027826778,0.0002579796,0.00024837142],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032274582,0.00011162949,0.16664262,0.0002736603,0.00044173526,0.00058225065,0.0021277734,0.11685279,0.042999566,0.5626923,0.009740927,0.09721197],"study_design_scores_gemma":[0.00003218733,0.00008830888,0.33999178,0.00006828194,0.000097730655,0.0004907994,0.00065066596,0.14165755,0.0013271667,0.48685998,0.028679488,0.00005614036],"about_ca_topic_score_codex":0.007211229,"about_ca_topic_score_gemma":0.005006076,"teacher_disagreement_score":0.007211229,"about_ca_system_score_codex":0.0007079115,"about_ca_system_score_gemma":0.00028176207,"threshold_uncertainty_score":0.014338553},"labels":[],"label_agreement":null},{"id":"W2169504254","doi":"10.1029/2003gl017268","title":"Stepwise and continuous low‐temperature demagnetization","year":2003,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Minnesota; W. M. Keck Foundation; National Science Foundation","keywords":"Remanence; Demagnetizing field; Magnetocrystalline anisotropy; Materials science; Saturation (graph theory); Magnetite; Geology; Mineralogy; Analytical Chemistry (journal); Condensed matter physics; Magnetization; Magnetic anisotropy; Magnetic field; Chemistry; Physics; Metallurgy","score_opus":0.010648130006563498,"score_gpt":0.26609837777492706,"score_spread":0.25545024776836356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169504254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98157287,0.00042073487,0.014025654,0.000052920266,0.00003852294,0.000079293626,0.0007235382,0.00039931556,0.0026871942],"genre_scores_gemma":[0.9755225,0.00031001828,0.01964752,0.000041797583,0.000014276516,0.00019111132,0.0009772851,0.00012643714,0.0031689683],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99975103,0.000015561445,0.000019429874,0.0000914576,0.00006539104,0.00005714287],"domain_scores_gemma":[0.9996259,0.00007543052,0.00005635484,0.00010591886,0.00009724028,0.0000391499],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003000783,0.00026420032,0.00032003273,0.00026253902,0.00015090301,0.00024185459,0.00054482435,0.00018859468,0.002454048],"category_scores_gemma":[0.00042380777,0.00025886734,0.00018204104,0.00029392072,0.00032906642,0.00024238115,0.00042416446,0.0006933807,0.00040998796],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019078088,0.000018700082,0.0003983048,0.000045156194,0.0000071895993,0.00002561567,0.000041976957,0.00019132986,0.9956469,0.00013676872,0.000082307604,0.003214908],"study_design_scores_gemma":[0.000042488977,0.00027926156,0.006098746,0.000005622343,0.00001662498,0.00008519546,0.000021219836,0.002691994,0.9885083,0.00007169718,0.0021626672,0.000016151993],"about_ca_topic_score_codex":0.0012436557,"about_ca_topic_score_gemma":0.0020089764,"teacher_disagreement_score":0.002454048,"about_ca_system_score_codex":0.00023564257,"about_ca_system_score_gemma":0.0003125163,"threshold_uncertainty_score":0.008209586},"labels":[],"label_agreement":null},{"id":"W2169736640","doi":"10.1002/2015gl065704","title":"Ice thickness in the Northwest Passage","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; York University; University of Alberta","funders":"Alberta Ingenuity; ArcticNet","keywords":"Sea ice; Arctic ice pack; Geology; Sea ice thickness; Drift ice; Breakup; Climatology; Cryosphere; Antarctic sea ice; Pancake ice; Atmospheric sciences; Meteorology; Geography","score_opus":0.04523998354013403,"score_gpt":0.29084359883616717,"score_spread":0.24560361529603314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169736640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983718,0.00006793334,0.00007499304,0.00000911058,0.0000040139057,0.0000011488172,0.00058427395,0.000003978274,0.00088280335],"genre_scores_gemma":[0.99843746,0.00006691636,0.00014757577,0.00000672975,0.0000040834852,0.000002531261,0.0008493408,0.0000023310754,0.00048301675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000006641432,0.0000050319104,0.000029827146,0.000015582045,0.000011439449],"domain_scores_gemma":[0.9997731,0.000027520697,0.000096085525,0.000013239022,0.00005651093,0.000033599074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014758437,0.0001647607,0.00011304945,0.0005109695,0.00022962686,0.00041900473,0.00012199496,0.00015370919,0.0007536835],"category_scores_gemma":[0.00039697858,0.00007048464,0.00009900496,0.00041930104,0.00013472581,0.00023839595,0.0002352964,0.00015657007,0.00018902747],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000097636366,0.000015300258,0.9877505,0.000014821377,0.000028144008,0.00024410478,0.00024724402,0.0006575078,0.003941068,0.000047188743,0.00036410132,0.0065924795],"study_design_scores_gemma":[9.872269e-7,0.000018725446,0.99837494,0.0000035597382,0.000003855244,0.000112146285,0.00013579163,0.00020598159,0.00057042384,0.0000113468395,0.0005602696,0.0000018801073],"about_ca_topic_score_codex":0.01687052,"about_ca_topic_score_gemma":0.026737021,"teacher_disagreement_score":0.01687052,"about_ca_system_score_codex":0.00027384018,"about_ca_system_score_gemma":0.00018911815,"threshold_uncertainty_score":0.03354466},"labels":[],"label_agreement":null},{"id":"W2169916919","doi":"10.1029/2004gl020265","title":"Cluster observations of velocity space‐restricted ion distributions near the plasma sheet","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Physics; Plasma sheet; Current sheet; Ion; Cluster (spacecraft); Plasma; Perpendicular; Transverse plane; Computational physics; Atomic physics; Range (aeronautics); Space physics; Astrophysics; Geophysics; Magnetosphere; Geometry; Nuclear physics; Magnetohydrodynamics; Materials science","score_opus":0.023905415248912362,"score_gpt":0.2768532271236697,"score_spread":0.25294781187475734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2169916919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982135,0.000022839167,0.00022020894,0.000013444506,0.0000024860801,0.000004870578,0.0003055672,0.000042606964,0.0011744907],"genre_scores_gemma":[0.9982967,0.000022827175,0.00061504345,0.000007055335,0.000009001229,0.0000059772133,0.000672349,0.00001376817,0.0003572883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995565,0.000002116195,0.000001005874,0.000012928586,0.000009120118,0.000019171826],"domain_scores_gemma":[0.9998578,0.000015774427,0.000033701275,0.000016706907,0.000021785383,0.000054229586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056808796,0.00012815022,0.00015808431,0.0006564729,0.00049825775,0.00029252042,0.00018427818,0.00019750641,0.0009400961],"category_scores_gemma":[0.00017479382,0.00011852479,0.00010453481,0.00051846827,0.00015518274,0.00012017658,0.00037264868,0.00022002344,0.00021565313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002087942,0.000259986,0.612958,0.000073333686,0.00014540051,0.0010720312,0.002380912,0.007232028,0.34078455,0.0008740316,0.0044698208,0.027661858],"study_design_scores_gemma":[0.000029201194,0.000105305364,0.9883133,0.000004454232,0.000017299435,0.00022058292,0.00017740605,0.0036015906,0.005853669,0.00008508083,0.0015758242,0.000016334008],"about_ca_topic_score_codex":0.007329621,"about_ca_topic_score_gemma":0.014356773,"teacher_disagreement_score":0.007329621,"about_ca_system_score_codex":0.00021737898,"about_ca_system_score_gemma":0.00012696238,"threshold_uncertainty_score":0.014573872},"labels":[],"label_agreement":null},{"id":"W216997101","doi":"10.1029/2008gl034762","title":"Ground surface temperature reconstructions: Using in situ estimates for thermal conductivity acquired with a fiber‐optic distributed thermal perturbation sensor","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Thermal conductivity; Borehole; Permafrost; Geothermal gradient; Thermal; Temperature measurement; Arctic; Environmental science; Atmospheric sciences; Geology; Materials science; Meteorology; Geophysics; Physics; Thermodynamics; Geotechnical engineering; Composite material","score_opus":0.08861363041930803,"score_gpt":0.3019261260628222,"score_spread":0.21331249564351418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W216997101","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9548179,0.00008003725,0.041556735,0.00008628222,0.00001751608,0.000024180052,0.00080368336,0.0005977739,0.0020158992],"genre_scores_gemma":[0.9730285,0.00003875433,0.026145356,0.000010333191,0.0000076079773,0.000013299306,0.00047379188,0.000030149564,0.00025215722],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998821,0.000014524842,0.000005671706,0.000041106476,0.000037287,0.000019196505],"domain_scores_gemma":[0.9998441,0.000019256135,0.000033998644,0.000027271823,0.000061304745,0.000014172203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020723537,0.00039012864,0.00023845052,0.00064524694,0.00024565787,0.00046498296,0.0005078081,0.00037648316,0.00058494863],"category_scores_gemma":[0.00057460595,0.00025036285,0.00026674985,0.000718638,0.00019637561,0.0007188986,0.00032555344,0.00033652474,0.00020269415],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004114076,0.000461982,0.28519654,0.0001419436,0.00018244839,0.00033519638,0.00045912797,0.17729877,0.40103474,0.0011796415,0.0012780781,0.13202007],"study_design_scores_gemma":[0.00011351469,0.00016616359,0.2573098,0.000024231793,0.000085408254,0.0001612566,0.0002714909,0.64731866,0.09095027,0.0012996031,0.0022382287,0.00006125714],"about_ca_topic_score_codex":0.008874035,"about_ca_topic_score_gemma":0.020679839,"teacher_disagreement_score":0.008874035,"about_ca_system_score_codex":0.00047364953,"about_ca_system_score_gemma":0.0005140322,"threshold_uncertainty_score":0.017644763},"labels":[],"label_agreement":null},{"id":"W2170150538","doi":"10.1029/2008gl034081","title":"A coastal ocean extreme bloom incubator","year":2008,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North Pacific Marine Science Organization","funders":"Office of Naval Research","keywords":"Bloom; Thermocline; Bay; Oceanography; Dinoflagellate; Upwelling; Algal bloom; Red tide; Environmental science; Wind stress; Phytoplankton; Nutrient; Geology; Ecology; Biology","score_opus":0.05407228535849768,"score_gpt":0.2569369905408572,"score_spread":0.20286470518235955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170150538","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.25359666,0.0035210052,0.021372603,0.029168403,0.010863776,0.0011257977,0.011099401,0.008168866,0.6610835],"genre_scores_gemma":[0.264407,0.003522113,0.03693981,0.004788402,0.0019025052,0.00055461924,0.011723303,0.0006077841,0.67555445],"study_design_codex":"design_other","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999775,0.000024744037,0.000015818267,0.00004914824,0.00008033952,0.000054943346],"domain_scores_gemma":[0.9991302,0.000032130843,0.000050274346,0.00011248336,0.00019558563,0.00047935147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056156516,0.0002492394,0.00011718867,0.00052623625,0.001291425,0.00082112645,0.00046231286,0.00032063006,0.017508695],"category_scores_gemma":[0.00070033025,0.00013783589,0.00017744185,0.00038570864,0.00018406937,0.00061047915,0.0026034368,0.00060360815,0.00674246],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021774687,0.00029092713,0.04908964,0.000078042125,0.000013037236,0.001661705,0.0010277951,0.00016267573,0.011090363,0.0047507207,0.4579147,0.4737027],"study_design_scores_gemma":[0.000015206576,0.00007588466,0.02743429,0.000027086038,0.000008013232,0.00046511553,0.00038591842,0.00023429179,0.0010668916,0.0003197561,0.9699552,0.000012253051],"about_ca_topic_score_codex":0.006862722,"about_ca_topic_score_gemma":0.02312184,"teacher_disagreement_score":0.017508695,"about_ca_system_score_codex":0.00061702356,"about_ca_system_score_gemma":0.0010604408,"threshold_uncertainty_score":0.05857241},"labels":[],"label_agreement":null},{"id":"W2170247593","doi":"10.1029/2006gl027339","title":"Reduction in Himalayan snow accumulation and weakening of the trade winds over the Pacific since the 1840s","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Snow; Monsoon; Climatology; Snow line; Indian ocean; Monsoon of South Asia; Geology; Snow cover; Trade wind; Oceanography; Physical geography; Geography","score_opus":0.04112538685432937,"score_gpt":0.30564021531260027,"score_spread":0.2645148284582709,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170247593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978607,0.00034267767,0.000058739006,0.00011385366,0.0000066026137,0.0000015398479,0.00031096916,0.000007333436,0.0012975023],"genre_scores_gemma":[0.99918646,0.00023757834,0.000069555026,0.000023332836,0.00001751595,9.92204e-7,0.00021726238,0.0000010924961,0.0002462013],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999275,0.0000074807685,0.000006994141,0.00001779807,0.000017924734,0.000022290935],"domain_scores_gemma":[0.9997173,0.000026262422,0.00012965189,0.000024700337,0.00006049203,0.00004148455],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015548326,0.0001422881,0.00017982026,0.00061015546,0.00047224335,0.0005711531,0.0001741022,0.00020807606,0.00090023986],"category_scores_gemma":[0.00052074256,0.000104823186,0.000136243,0.0013224903,0.00047773818,0.00028603207,0.0003178989,0.0002555353,0.00011356982],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014578731,0.000018233539,0.9793282,0.000076894954,0.00011288498,0.00044927516,0.0014337448,0.0010124268,0.005271488,0.0005266576,0.00043381416,0.011190547],"study_design_scores_gemma":[0.000001161118,0.0000074827663,0.9987086,0.0000033702743,0.000007569216,0.000056251007,0.00013073464,0.00008977877,0.0001612002,0.00003224505,0.0008001055,0.0000016428601],"about_ca_topic_score_codex":0.030037818,"about_ca_topic_score_gemma":0.046125002,"teacher_disagreement_score":0.030037818,"about_ca_system_score_codex":0.000698693,"about_ca_system_score_gemma":0.00037113222,"threshold_uncertainty_score":0.05972594},"labels":[],"label_agreement":null},{"id":"W2170656341","doi":"10.1002/2015gl063693","title":"Elemental composition of organic aerosol: The gap between ambient and laboratory measurements","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Biological and Environmental Research; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Aerosol; Carbon fibers; Environmental science; Total organic carbon; Environmental chemistry; Atmospheric sciences; Chemistry; Meteorology; Materials science; Geology; Physics","score_opus":0.08285905939361238,"score_gpt":0.2979436025361871,"score_spread":0.21508454314257475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170656341","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98481894,0.001959722,0.009616275,0.00006385228,0.000028463415,0.0000180221,0.0010989817,0.00016029182,0.0022353905],"genre_scores_gemma":[0.99615544,0.0002353183,0.002778947,0.000041450043,0.000013594244,0.000009230206,0.0006747382,0.00002453343,0.000066822526],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99889153,0.00022919998,0.00008215841,0.00040730071,0.00033455045,0.000055224762],"domain_scores_gemma":[0.9987643,0.00047647776,0.00015461448,0.0003114503,0.00024547518,0.000047676705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013905201,0.00021599473,0.000373594,0.00072778127,0.00023900294,0.0007405674,0.00041027338,0.0004370706,0.00032232003],"category_scores_gemma":[0.001963097,0.00016592737,0.0002272138,0.00068879745,0.0003427189,0.00056615786,0.00043994837,0.00021707201,0.00016581033],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008198599,0.00041496128,0.54754764,0.0004036519,0.0005607982,0.00019535617,0.0004833964,0.004195711,0.33921087,0.000838619,0.0007228827,0.10460631],"study_design_scores_gemma":[0.000031208947,0.0002742209,0.9121658,0.000054067328,0.00015855847,0.00037676046,0.0003218073,0.008976317,0.07121629,0.0007801284,0.0056014173,0.00004343856],"about_ca_topic_score_codex":0.0024186578,"about_ca_topic_score_gemma":0.0028320733,"teacher_disagreement_score":0.0024186578,"about_ca_system_score_codex":0.0002907518,"about_ca_system_score_gemma":0.00022565869,"threshold_uncertainty_score":0.0073538423},"labels":[],"label_agreement":null},{"id":"W2170731713","doi":"10.1029/2004gl021954","title":"First observations of SBAS/WAAS scintillations: Using collocated scintillation measurements and all‐sky images to study equatorial plasma bubbles","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministère de la Santé et des Services sociaux","keywords":"Scintillation; Satellite; Ionosphere; Earth's magnetic field; Amplitude; Geology; Sky; Physics; Remote sensing; Geodesy; Meteorology; Geophysics; Optics; Magnetic field; Astronomy; Detector","score_opus":0.09353483975928552,"score_gpt":0.3428848790994554,"score_spread":0.24935003934016992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2170731713","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99334586,0.00016937486,0.0039025568,0.000032320826,0.00001161317,0.000036447327,0.0002646735,0.000109560504,0.002127689],"genre_scores_gemma":[0.99420375,0.00005561478,0.0049945186,0.000013948066,0.000011417263,0.000012469101,0.00033731686,0.000017315098,0.0003538101],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99990857,0.000010240007,0.0000041971716,0.000017735616,0.000035788238,0.000023507015],"domain_scores_gemma":[0.99965537,0.00004991209,0.00005388766,0.000039304097,0.00012039757,0.00008123404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029433772,0.00019224914,0.00016731178,0.00058473577,0.00041017056,0.0003760463,0.00020278229,0.00029544713,0.00047211492],"category_scores_gemma":[0.00048573606,0.00018417822,0.0001322731,0.00044372768,0.00017877773,0.0003022314,0.0004615042,0.00039898368,0.00009702951],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000996792,0.00020023105,0.46171048,0.00013566528,0.00012388256,0.0019574622,0.0028296073,0.0017707637,0.46709242,0.00084308145,0.0015277681,0.06081184],"study_design_scores_gemma":[0.000052482483,0.00063344405,0.9199772,0.000022331127,0.00006081337,0.0011462213,0.0005774781,0.008879106,0.06173764,0.0002572866,0.006612572,0.00004337929],"about_ca_topic_score_codex":0.0045446316,"about_ca_topic_score_gemma":0.011986636,"teacher_disagreement_score":0.0045446316,"about_ca_system_score_codex":0.0002325278,"about_ca_system_score_gemma":0.00016629958,"threshold_uncertainty_score":0.009036362},"labels":[],"label_agreement":null},{"id":"W2171008592","doi":"10.1029/1999gl011239","title":"Application of ionospheric tomography to real‐time GPS carrier‐phase ambiguities Resolution, at scales of 400–1000 km and with high geomagnetic activity","year":2000,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Global Positioning System; Ionosphere; Earth's magnetic field; Remote sensing; Geodesy; Ambiguity resolution; Geology; GPS signals; Satellite; Meteorology; Computer science; Geophysics; Physics; Assisted GPS; GNSS applications; Telecommunications; Magnetic field","score_opus":0.006113882915612118,"score_gpt":0.2526213965984202,"score_spread":0.24650751368280807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171008592","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36603776,0.00041948844,0.6261544,0.0004998912,0.0000587751,0.000052950156,0.0005637162,0.00074655283,0.0054664593],"genre_scores_gemma":[0.85878485,0.0003484519,0.13927048,0.00003733834,0.000017906113,0.000035804456,0.00037541022,0.00005389807,0.0010757842],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992776,0.000022311144,0.0000030075066,0.000017160992,0.000020483092,0.000009325929],"domain_scores_gemma":[0.9997621,0.00007859474,0.000045630655,0.0000629245,0.000038489303,0.000012176259],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017783904,0.00028303397,0.00015201056,0.00029914995,0.00015150858,0.00058381405,0.00028712823,0.00023235207,0.0010490108],"category_scores_gemma":[0.0012904119,0.0002406674,0.00017430335,0.0005082653,0.00037492445,0.0006049564,0.00045816484,0.00028067167,0.00019303363],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028189484,0.00008060356,0.056051087,0.00018156793,0.00013361055,0.00036089335,0.00047758696,0.58573896,0.14351478,0.010072045,0.0016381786,0.20146886],"study_design_scores_gemma":[0.000030067902,0.00010999714,0.02922792,0.000015299805,0.000031395375,0.00044064995,0.00021522946,0.932966,0.02623605,0.005012226,0.005687493,0.000027665134],"about_ca_topic_score_codex":0.0070495186,"about_ca_topic_score_gemma":0.007858071,"teacher_disagreement_score":0.0070495186,"about_ca_system_score_codex":0.0003738813,"about_ca_system_score_gemma":0.0004867982,"threshold_uncertainty_score":0.014016986},"labels":[],"label_agreement":null},{"id":"W2171023808","doi":"10.1029/2001gl012863","title":"Sea surface height changes in the North Atlantic Ocean related to the North Atlantic Oscillation","year":2001,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Oceanic and Atmospheric Administration; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft","keywords":"Sea-surface height; Atlantic Equatorial mode; North Atlantic oscillation; Gulf Stream; Altimeter; Ocean gyre; Climatology; Ocean surface topography; Atlantic multidecadal oscillation; Geology; Thermohaline circulation; Oceanography; North Atlantic Deep Water; Sea surface temperature; Ocean current; Ocean dynamics; Ocean heat content; Forcing (mathematics); Ocean general circulation model; Wind stress; Subtropics; General Circulation Model; Climate change","score_opus":0.03697103465374925,"score_gpt":0.28540757402404915,"score_spread":0.2484365393702999,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171023808","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991702,0.00008681577,0.0000584631,0.000040486015,0.0000061655746,0.0000015179728,0.00021384018,0.000006203499,0.00041629345],"genre_scores_gemma":[0.99924505,0.00008308161,0.000048010817,0.000010917702,0.000008508888,0.0000021555095,0.00044307215,0.0000014634256,0.00015784746],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994254,0.000010122403,0.000005065545,0.00001324781,0.000015292231,0.000013762017],"domain_scores_gemma":[0.99967706,0.000064956046,0.00015399535,0.000017669307,0.00004953264,0.000036746223],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016064396,0.00012954223,0.000107269545,0.0003401844,0.00016116379,0.00035955047,0.000088257635,0.0002450854,0.00072821556],"category_scores_gemma":[0.00085737236,0.00008958771,0.00016712253,0.00045200269,0.00017499043,0.0002321623,0.00019123865,0.0001763756,0.00014660663],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014357435,0.00005058188,0.98145455,0.00001633743,0.00008695021,0.00015227759,0.0001386178,0.003364708,0.0043054605,0.0001312402,0.00051037624,0.009645255],"study_design_scores_gemma":[0.000003471223,0.000022195529,0.99821764,0.0000013052937,0.0000073245938,0.000033177665,0.000031016458,0.0013289071,0.000108375316,0.000041391995,0.00020283896,0.0000022504983],"about_ca_topic_score_codex":0.008916101,"about_ca_topic_score_gemma":0.013610249,"teacher_disagreement_score":0.008916101,"about_ca_system_score_codex":0.0003481008,"about_ca_system_score_gemma":0.00014222231,"threshold_uncertainty_score":0.017728448},"labels":[],"label_agreement":null},{"id":"W2171047464","doi":"10.1029/2007gl031809","title":"Rapid loss of the Ayles Ice Shelf, Ellesmere Island, Canada","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Armed Forces; University of Ottawa","funders":"","keywords":"Ice shelf; Iceberg; Sea ice; Oceanography; Geology; Antarctic sea ice; Arctic ice pack; Ice calving; Cryosphere; Arctic; Climatology; Physical geography; Geography","score_opus":0.029163882991699114,"score_gpt":0.25997668116202854,"score_spread":0.23081279817032943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171047464","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9353592,0.0042913794,0.0003046585,0.0045392755,0.00013317962,0.000077150966,0.00889386,0.0000881686,0.04631315],"genre_scores_gemma":[0.93974507,0.0029045204,0.00093799987,0.0010313203,0.00002321752,0.000024911305,0.0045974883,0.000031529427,0.05070402],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977213,0.000008378399,0.0000055119654,0.00004521047,0.000087418484,0.00008143832],"domain_scores_gemma":[0.99942255,0.000015220249,0.000049377795,0.0000124768785,0.00033268836,0.0001678172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021011235,0.00020255601,0.00019647916,0.0006857645,0.0036330356,0.0016549085,0.0004722594,0.00034292124,0.004616364],"category_scores_gemma":[0.00056967896,0.00020247008,0.00012550256,0.0007807297,0.0006153525,0.0005229785,0.00077915814,0.0005721587,0.0005016828],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047935796,0.00013392132,0.78478605,0.0003290889,0.00017009495,0.0020495339,0.004900662,0.0016905783,0.0073117344,0.002762374,0.08668572,0.10870094],"study_design_scores_gemma":[0.000016302327,0.000019256395,0.95370966,0.00009856984,0.000015313186,0.00011901036,0.0034493634,0.00055018463,0.0006754965,0.000076976234,0.041252393,0.000017403789],"about_ca_topic_score_codex":0.99303377,"about_ca_topic_score_gemma":0.99887675,"teacher_disagreement_score":0.019325268,"about_ca_system_score_codex":0.019325268,"about_ca_system_score_gemma":0.018553378,"threshold_uncertainty_score":0.14021534},"labels":[],"label_agreement":null},{"id":"W2171664796","doi":"10.1029/2010gl046131","title":"Impact of the North Atlantic Oscillation on the forecast skill of the Madden-Julian Oscillation","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Madden–Julian oscillation; Hindcast; Climatology; Extratropical cyclone; Forecast skill; North Atlantic oscillation; Environmental science; Oscillation (cell signaling); Amplitude; Forcing (mathematics); Meteorology; Atmospheric sciences; Geology; Geography; Convection; Physics","score_opus":0.06824602601395681,"score_gpt":0.2987817904456401,"score_spread":0.23053576443168333,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171664796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99813783,0.000116233394,0.0006046086,0.00012573162,0.00001994743,0.0000029803289,0.00017295982,0.000030088086,0.0007895617],"genre_scores_gemma":[0.9994691,0.00002795166,0.00021520387,0.000014348982,0.000009602128,0.0000010379647,0.00017327971,0.000006795325,0.0000825682],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973136,0.00009739663,0.00002133082,0.000062763684,0.000051385687,0.00003581976],"domain_scores_gemma":[0.99574274,0.002996695,0.00046047368,0.00025349506,0.0003019005,0.000244737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013825335,0.0002904437,0.00024101876,0.00017882681,0.00023427294,0.00071168225,0.00018942983,0.00033068855,0.0007248596],"category_scores_gemma":[0.0087832175,0.0001652393,0.00029970205,0.00017182957,0.00024285908,0.00046045685,0.0004106784,0.0004420063,0.00009485454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012434562,0.00013681833,0.80844253,0.000058850164,0.00035394216,0.0002678796,0.00011929467,0.14989878,0.0151124885,0.00071192515,0.0009007785,0.022753246],"study_design_scores_gemma":[0.00006855905,0.0002693907,0.7434341,0.000013939645,0.00009122504,0.00006538052,0.000073100746,0.25069326,0.004292135,0.0004446104,0.0005251852,0.000029149463],"about_ca_topic_score_codex":0.018367635,"about_ca_topic_score_gemma":0.016999718,"teacher_disagreement_score":0.018367635,"about_ca_system_score_codex":0.00038629092,"about_ca_system_score_gemma":0.0005765507,"threshold_uncertainty_score":0.036521494},"labels":[],"label_agreement":null},{"id":"W2171837839","doi":"10.1029/2005gl022671","title":"ACE‐FTS measurements across the edge of the winter 2004 Arctic vortex","year":2005,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Occultation; Middle latitudes; Atmospheric sciences; Arctic; Vortex; Polar vortex; Stratosphere; Latitude; Descent (aeronautics); Environmental science; Geology; Physics; Climatology; Meteorology; Oceanography; Geodesy; Astrophysics","score_opus":0.053411576782750145,"score_gpt":0.3129188387464425,"score_spread":0.25950726196369234,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2171837839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997142,0.000036073845,0.00024694658,0.0000146764,0.0000072289768,0.0000028550928,0.001393574,0.000020059839,0.001136469],"genre_scores_gemma":[0.99527407,0.000045695288,0.0007572695,0.000012319157,0.000011554978,0.0000045406086,0.0034051433,0.0000060465713,0.0004834096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999051,0.000010584588,0.000005358609,0.000021380438,0.00003495962,0.000022597407],"domain_scores_gemma":[0.9997576,0.000024180128,0.00004982488,0.000016997907,0.00010919859,0.000042268694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016968446,0.00015608204,0.00018316685,0.00048934796,0.00030534546,0.000326902,0.000118221935,0.00012676774,0.0003320169],"category_scores_gemma":[0.00035915393,0.000099930985,0.00011971895,0.0004408327,0.000080581274,0.00013523034,0.00017388801,0.00012051603,0.00009557965],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015081306,0.0001626292,0.9082481,0.000053886062,0.00015435371,0.00020862973,0.00047733396,0.005850778,0.054526124,0.00032794874,0.0021439241,0.02633814],"study_design_scores_gemma":[0.000014406705,0.00005431649,0.9857459,0.0000045265706,0.000024770905,0.00005120887,0.00008353398,0.005275227,0.0069228075,0.00003535568,0.001779863,0.000008075382],"about_ca_topic_score_codex":0.03379104,"about_ca_topic_score_gemma":0.055656333,"teacher_disagreement_score":0.03379104,"about_ca_system_score_codex":0.0003849675,"about_ca_system_score_gemma":0.00022610709,"threshold_uncertainty_score":0.06718868},"labels":[],"label_agreement":null},{"id":"W2172097513","doi":"10.1002/grl.50937","title":"El Niño, the 2006 Indonesian peat fires, and the distribution of atmospheric methane","year":2013,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Jet Propulsion Laboratory; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration; California Institute of Technology; University of Toronto; National Center for Atmospheric Research; National Science Foundation","keywords":"Troposphere; Environmental science; Methane; Atmospheric sciences; Climatology; Biomass burning; Atmospheric methane; Peat; Meteorology; Geology; Chemistry; Aerosol; Geography","score_opus":0.008661377625694763,"score_gpt":0.24051261329025356,"score_spread":0.23185123566455879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2172097513","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949133,0.000048520473,0.000029061533,0.000030638683,0.000002827049,5.668448e-7,0.0000678495,0.0000016530796,0.0003275574],"genre_scores_gemma":[0.9996842,0.000058478006,0.000033971817,0.00001363388,0.0000041570834,0.000001044602,0.0000995892,0.0000012943967,0.00010356488],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.000009179682,0.0000030545366,0.0000110728315,0.000009077245,0.00001665852],"domain_scores_gemma":[0.9998264,0.00003083459,0.00006865154,0.000008127184,0.000015565527,0.000050375682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001752561,0.0001106538,0.000106178486,0.00016843404,0.00017590082,0.00031133508,0.00009125073,0.000116168434,0.00037263468],"category_scores_gemma":[0.00033681392,0.000100947254,0.000090371344,0.0001547864,0.00018763955,0.00016758672,0.00021745215,0.00023701528,0.000073114774],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007006172,0.00014017931,0.97960395,0.000016114618,0.00006037167,0.0002075501,0.00013096,0.0022238956,0.01056942,0.0001445385,0.00025771538,0.0059447344],"study_design_scores_gemma":[0.0000032159005,0.00000899985,0.9983388,0.000002150304,0.0000056931453,0.00003749111,0.00009345773,0.00090087415,0.00043496778,0.000028505228,0.00014411136,0.000001708804],"about_ca_topic_score_codex":0.013942475,"about_ca_topic_score_gemma":0.02056614,"teacher_disagreement_score":0.013942475,"about_ca_system_score_codex":0.0004083667,"about_ca_system_score_gemma":0.0001874938,"threshold_uncertainty_score":0.027722657},"labels":[],"label_agreement":null},{"id":"W2181141303","doi":"10.1002/2015gl066111","title":"Strong eddy compensation for the Gulf Stream heat transport","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Gulf Stream; Eddy; Atmosphere (unit); Heat flux; Geology; Climatology; Ocean heat content; Environmental science; Atmospheric sciences; Heat transfer; Ocean current; Meteorology; Turbulence; Mechanics; Geography; Physics","score_opus":0.06258973179809248,"score_gpt":0.29920727745755504,"score_spread":0.23661754565946258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2181141303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99508107,0.00013734656,0.002566231,0.00020789169,0.00007377513,0.000010347356,0.00028207846,0.0002057583,0.0014355488],"genre_scores_gemma":[0.9990103,0.00003951657,0.00045409118,0.000019702617,0.00001603797,0.0000034958812,0.00015056937,0.000012463932,0.00029374668],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999882,0.000021604295,0.0000086913615,0.000034720222,0.000024270008,0.000028624834],"domain_scores_gemma":[0.9998042,0.00004014365,0.000033470336,0.00004575516,0.000053571053,0.000022873946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003613833,0.00065640314,0.0003377134,0.00025604645,0.00035608013,0.0006129514,0.00034767596,0.00040420413,0.0012521448],"category_scores_gemma":[0.00084186223,0.00030315833,0.0005269214,0.00033172805,0.00031748277,0.00053358654,0.0004637051,0.0004028664,0.00012895238],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008670287,0.00031420166,0.1121533,0.00014741125,0.0004652569,0.00053751515,0.00009610105,0.7197542,0.11515769,0.005211749,0.002785978,0.04250956],"study_design_scores_gemma":[0.00016962075,0.00011702396,0.121563666,0.000011838348,0.00010409142,0.00004358989,0.000033898694,0.86124974,0.01447445,0.0006090513,0.0015943401,0.000028600116],"about_ca_topic_score_codex":0.015810495,"about_ca_topic_score_gemma":0.01424595,"teacher_disagreement_score":0.015810495,"about_ca_system_score_codex":0.00068365806,"about_ca_system_score_gemma":0.0010370901,"threshold_uncertainty_score":0.03143692},"labels":[],"label_agreement":null},{"id":"W2184994971","doi":"10.1002/2015gl066361","title":"Static stress drop in the <i>M<sub>w</sub></i> 9 Tohoku‐oki earthquake: Heterogeneous distribution and low average value","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Victoria","funders":"","keywords":"Drop (telecommunication); Geology; Slip (aerodynamics); Seismology; Fault plane; Mechanics; Fault (geology); Physics; Thermodynamics; Engineering","score_opus":0.030609092748966612,"score_gpt":0.2666330343537852,"score_spread":0.2360239416048186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2184994971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984913,0.000044256547,0.0006584055,0.000012988217,0.0000015876593,0.0000024023402,0.0002656269,0.000025020501,0.0004984378],"genre_scores_gemma":[0.9995976,0.00002257844,0.00010366786,0.0000023138298,0.0000012017794,0.000002080189,0.00021054626,0.000003833468,0.000056130113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999261,0.0000058781907,0.000009122747,0.00002797327,0.000012408234,0.000018492026],"domain_scores_gemma":[0.99978966,0.0000386217,0.000056796223,0.0000348926,0.000046237266,0.000033798882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022200787,0.0003751713,0.000451262,0.00089677604,0.00031361796,0.00063040777,0.0006414497,0.0005468589,0.0005293097],"category_scores_gemma":[0.00039321146,0.00038176548,0.0007033015,0.0010157059,0.00031525863,0.0006816634,0.00033781308,0.00017888243,0.00017962763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032920146,0.00016658388,0.61823374,0.00022917104,0.0003641105,0.0011738598,0.00032390375,0.32861155,0.03360432,0.00054103555,0.0007265871,0.015695943],"study_design_scores_gemma":[0.000020859396,0.0001378762,0.5274472,0.000013449574,0.00013642632,0.00033117077,0.00025216557,0.46374956,0.0069876662,0.00053982105,0.00032244917,0.00006138658],"about_ca_topic_score_codex":0.010325857,"about_ca_topic_score_gemma":0.009268443,"teacher_disagreement_score":0.010325857,"about_ca_system_score_codex":0.0008435566,"about_ca_system_score_gemma":0.0002566685,"threshold_uncertainty_score":0.020531476},"labels":[],"label_agreement":null},{"id":"W2185848116","doi":"10.1002/2015gl065539","title":"The response of SST to insolation and ice sheet variability from MIS 3 to MIS 11 in the northwestern Mediterranean Sea (Gulf of Lions)","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"FPInnovations","keywords":"Geology; Climatology; Middle latitudes; Marine isotope stage; Sea surface temperature; Ice sheet; Latitude; Mediterranean climate; Mediterranean sea; Oceanography; Sea level; Proxy (statistics); Glacial period; Insolation; Greenland ice sheet; Interglacial; Geomorphology; Geography","score_opus":0.05790750889461901,"score_gpt":0.31519811771400263,"score_spread":0.25729060881938365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2185848116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996921,0.000016527281,0.000013369186,0.000017395316,0.0000017795822,5.868366e-7,0.000121977726,0.0000022699487,0.0001338925],"genre_scores_gemma":[0.9995615,0.0000141655755,0.00002326186,0.000012219984,0.0000029602804,0.0000018273415,0.0002810277,0.0000014154064,0.00010154793],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989676,0.000020964088,0.000008559744,0.00003430533,0.000012473432,0.000026903177],"domain_scores_gemma":[0.9995529,0.000076767545,0.0001579747,0.00003737065,0.00009058497,0.00008435013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033431174,0.0001801585,0.00018645443,0.0004188781,0.00018857437,0.000479152,0.00018580134,0.0002618743,0.0006986258],"category_scores_gemma":[0.00074445026,0.00010815614,0.00024379147,0.00036285445,0.0002692511,0.00023833824,0.00033512642,0.00019470692,0.00013593935],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010336017,0.000013310197,0.9953998,0.000004424468,0.000047148395,0.0000637585,0.0001681605,0.00034985508,0.0019753077,0.000015990663,0.00014504929,0.0017139721],"study_design_scores_gemma":[0.0000013622819,0.000009044976,0.99957126,0.0000012908754,0.000003657311,0.000009033693,0.000058250662,0.00024014003,0.000049336188,0.0000042570846,0.000051317667,9.90758e-7],"about_ca_topic_score_codex":0.025274592,"about_ca_topic_score_gemma":0.035819102,"teacher_disagreement_score":0.025274592,"about_ca_system_score_codex":0.00046126303,"about_ca_system_score_gemma":0.00022800546,"threshold_uncertainty_score":0.050255},"labels":[],"label_agreement":null},{"id":"W2187637860","doi":"10.1002/2015gl066858","title":"Revisiting trends in wetness and dryness in the presence of internal climate variability and water limitations over land","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Dryness; Environmental science; Precipitation; Potential evaporation; Water cycle; Evaporation; Climate change; Climatology; Dry season; Atmospheric sciences; Moisture; Water content; Meteorology; Ecology; Geography; Geology","score_opus":0.07447378411359015,"score_gpt":0.33634329330271695,"score_spread":0.26186950918912677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2187637860","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923825,0.000015525766,0.00021773868,0.000032682787,0.0000014404666,0.0000015530037,0.00016153722,0.00001220178,0.00031907897],"genre_scores_gemma":[0.99974865,0.0000097459315,0.00006975456,0.000003403645,0.0000016120455,0.0000011986012,0.00012642972,0.000003433954,0.000035751647],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998983,0.000029352437,0.0000063509615,0.000029357923,0.000012615466,0.000024047382],"domain_scores_gemma":[0.9993382,0.00025809903,0.00014748286,0.0000922493,0.000084768246,0.000079113415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005951157,0.00019058606,0.00032421108,0.00051358994,0.00021507325,0.00088833587,0.00037708192,0.00027942265,0.0011243798],"category_scores_gemma":[0.0011241812,0.0001485236,0.00040741617,0.00072653353,0.00045454723,0.0006442429,0.0004780543,0.00026160452,0.00011834038],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029574224,0.00009814796,0.8877271,0.000049293474,0.0002341107,0.00015980394,0.00022364025,0.09131787,0.012183945,0.0012876686,0.0005760784,0.0058466573],"study_design_scores_gemma":[0.00003124754,0.00010804738,0.74795157,0.000007225206,0.00007771636,0.000053022675,0.00030797304,0.24706833,0.0027049328,0.0010596367,0.0006086201,0.000021732028],"about_ca_topic_score_codex":0.01111894,"about_ca_topic_score_gemma":0.010722783,"teacher_disagreement_score":0.01111894,"about_ca_system_score_codex":0.0005885664,"about_ca_system_score_gemma":0.00026213133,"threshold_uncertainty_score":0.022108436},"labels":[],"label_agreement":null},{"id":"W2189536228","doi":"10.1002/2015gl066344","title":"Obliquity‐driven expansion of North Atlantic sea ice during the last glacial","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Australian Research Council; National Oceanic and Atmospheric Administration; Australian National University; National Computational Infrastructure","keywords":"Geology; Glacial period; Last Glacial Maximum; Climatology; Oceanography; Ice sheet; Northern Hemisphere; Climate change; Pleistocene; Paleontology","score_opus":0.04136976263997539,"score_gpt":0.29000706199792,"score_spread":0.2486372993579446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2189536228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991146,0.000028019906,0.000045450226,0.00003241534,0.0000025153952,8.8507755e-7,0.00014589973,0.000004844927,0.00062524324],"genre_scores_gemma":[0.9997181,0.000023929519,0.00001883444,0.000008948744,0.0000017426927,7.514861e-7,0.000087921326,0.0000017504631,0.00013788807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997854,0.0000024458534,0.0000016592932,0.0000063676766,0.0000036555612,0.000007323952],"domain_scores_gemma":[0.99993193,0.000008401575,0.00002335011,0.0000047197022,0.00001561944,0.000016014064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007623656,0.00008659786,0.00007740461,0.00021806026,0.00014296852,0.00027689215,0.00006741059,0.00006985891,0.0007535083],"category_scores_gemma":[0.00023192645,0.00006600278,0.00009998512,0.00014006547,0.0001692769,0.00010665604,0.00020161972,0.00009869108,0.00010979393],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024593968,0.000035281028,0.8873103,0.00004324569,0.00006012762,0.00019409582,0.00033045368,0.005317701,0.09196953,0.0006109334,0.0010518911,0.012830377],"study_design_scores_gemma":[0.0000040585182,0.000013393321,0.9959402,0.0000023633202,0.000005867022,0.000020971498,0.0000634387,0.0021149511,0.0012716196,0.00011305881,0.00044636297,0.0000036875076],"about_ca_topic_score_codex":0.01875476,"about_ca_topic_score_gemma":0.03593678,"teacher_disagreement_score":0.01875476,"about_ca_system_score_codex":0.00056150014,"about_ca_system_score_gemma":0.00029196875,"threshold_uncertainty_score":0.03729117},"labels":[],"label_agreement":null},{"id":"W2202665948","doi":"10.1002/2015gl066235","title":"Rapid and highly variable warming of lake surface waters around the globe","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":1300,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of the Environment, Conservation and Parks; International Institute for Sustainable Development; Ministry of Environment; Laurentian University; University of Sudbury; York University","funders":"Natural Environment Research Council; Earth Sciences Division; National Aeronautics and Space Administration; Institute of Agriculture and Natural Resources; Inter-American Institute for Global Change Research; Russian Science Foundation; National Science Foundation; Haridus- ja Teadusministeerium; Deutsche Forschungsgemeinschaft; Sight Research UK; National Institute of Food and Agriculture; U.S. Department of Agriculture; Institut National Du Cancer","keywords":"Environmental science; Global warming; Climate change; Climatology; Cloud cover; Oceanography; Geology; Cloud computing","score_opus":0.03353558089674506,"score_gpt":0.27234722818455154,"score_spread":0.23881164728780646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2202665948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930647,0.0013901123,0.00036593142,0.0002746063,0.0000137176585,0.0000045747097,0.0030843476,0.000036042158,0.0017660466],"genre_scores_gemma":[0.99742573,0.0005213696,0.00024712217,0.00008610802,0.000017169325,0.0000043031514,0.0015250405,0.0000075457074,0.0001656041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989426,0.000022143957,0.000010945651,0.00003494174,0.000020618007,0.000017036036],"domain_scores_gemma":[0.9996363,0.000051299474,0.00016918813,0.00004283706,0.000076305914,0.000024052935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038130916,0.00014771686,0.00015917639,0.0010819688,0.00014768263,0.00052492094,0.000108899505,0.00015054645,0.00062525313],"category_scores_gemma":[0.0005494483,0.00007477097,0.00022052666,0.002004697,0.00023477066,0.00044795763,0.00057656446,0.00020072474,0.000077716504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009154128,0.00000841216,0.9566321,0.00020897691,0.00054131,0.00019390493,0.0008470138,0.0012311373,0.007831652,0.00037519683,0.0023305556,0.029708335],"study_design_scores_gemma":[0.0000010372645,0.0000059415456,0.9980788,0.000009172201,0.000024847886,0.00002044284,0.00008862021,0.00007809557,0.00024006497,0.00004388123,0.0014060587,0.0000029487126],"about_ca_topic_score_codex":0.012979327,"about_ca_topic_score_gemma":0.026213564,"teacher_disagreement_score":0.012979327,"about_ca_system_score_codex":0.0003170744,"about_ca_system_score_gemma":0.00027834898,"threshold_uncertainty_score":0.02580756},"labels":[],"label_agreement":null},{"id":"W2220004450","doi":"10.1002/2015gl066954","title":"Size separation method for absorption characterization in brown carbon: Application to an aged biomass burning sample","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"Absorbance; Size-exclusion chromatography; Absorption (acoustics); Mass spectrometry; Aerosol; Analytical Chemistry (journal); Electrospray ionization; Electrospray; Chromatography; Carbon fibers; Chemistry; Materials science; Organic chemistry","score_opus":0.052249013639787525,"score_gpt":0.34959996675290295,"score_spread":0.29735095311311543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2220004450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81522274,0.0030028787,0.17567797,0.0003414315,0.00022959142,0.00047444,0.00074841676,0.0010408595,0.0032617548],"genre_scores_gemma":[0.7849088,0.0019446323,0.20803352,0.00039060396,0.00007580769,0.0004048554,0.00071575976,0.00017403997,0.0033521324],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9996786,0.00005965892,0.000023189097,0.000094633026,0.0001125583,0.00003130228],"domain_scores_gemma":[0.99921,0.00028746095,0.000075698794,0.00006283298,0.0002968055,0.0000670775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074562564,0.0005121263,0.00021920011,0.0011253168,0.00048095972,0.00030455086,0.0003359139,0.0005123197,0.0016759736],"category_scores_gemma":[0.0010756473,0.00016620923,0.00019496235,0.00048322754,0.00031775224,0.00023780481,0.00022749387,0.00047920516,0.0006192485],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043918968,0.000032312895,0.0008340396,0.000020671438,0.000007053139,0.000040431165,0.000039664963,0.000078229845,0.9949032,0.000046654986,0.000051562343,0.003902351],"study_design_scores_gemma":[0.000012819925,0.00033618588,0.015186251,0.000013119637,0.000039162773,0.00043665047,0.00009016999,0.004286997,0.97680646,0.00010565774,0.0026647348,0.000021805057],"about_ca_topic_score_codex":0.0020041952,"about_ca_topic_score_gemma":0.0025190664,"teacher_disagreement_score":0.0020041952,"about_ca_system_score_codex":0.00019854015,"about_ca_system_score_gemma":0.00037717342,"threshold_uncertainty_score":0.0056066513},"labels":[],"label_agreement":null},{"id":"W2222082876","doi":"10.1002/2015gl066675","title":"A global Mars dust composition refined by the Alpha‐Particle X‐ray Spectrometer in Gale Crater","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":134,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; University of Guelph; Brock University; Western University","funders":"Australian Research Council; Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; California Institute of Technology; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Impact crater; Martian soil; Volatiles; Martian; Atmosphere of Mars; Astrobiology; Regolith; Martian surface; Basalt; Geology; Soil water; Mars landing; Crust; Mineralogy; Exploration of Mars; Geochemistry; Physics; Soil science","score_opus":0.04603225109663016,"score_gpt":0.30979903867613906,"score_spread":0.2637667875795089,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2222082876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987464,0.00005883214,0.00009332948,0.000010203398,0.0000011416128,0.0000036205236,0.00064558355,0.000019524377,0.00042138022],"genre_scores_gemma":[0.99850047,0.000038721137,0.0002674027,0.00001532227,0.0000022268134,0.0000042297283,0.0010225769,0.000007821992,0.0001413447],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998659,0.000016084681,0.000008673313,0.000060345952,0.000024802803,0.000024220853],"domain_scores_gemma":[0.999846,0.000016367581,0.00004061657,0.000020691745,0.000045245553,0.00003100552],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023883437,0.00048628062,0.00025031655,0.0018948285,0.00040775305,0.000722056,0.000265044,0.00037374895,0.0009194783],"category_scores_gemma":[0.0001831595,0.00025290716,0.0003640165,0.00088531466,0.00022499484,0.00024644117,0.00045774595,0.00016551842,0.0002890848],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015304903,0.000020084168,0.9728641,0.00001621078,0.00015191345,0.00015931575,0.00014541765,0.0006996248,0.021748614,0.000028065198,0.00026248468,0.0037512039],"study_design_scores_gemma":[0.0000027913077,0.000009975441,0.99882704,0.0000012616687,0.000010754254,0.00005186018,0.00005356634,0.0003175582,0.0005538628,0.000004893416,0.0001652419,0.0000012304598],"about_ca_topic_score_codex":0.0210146,"about_ca_topic_score_gemma":0.018655337,"teacher_disagreement_score":0.0210146,"about_ca_system_score_codex":0.00033316948,"about_ca_system_score_gemma":0.00010300238,"threshold_uncertainty_score":0.041784585},"labels":[],"label_agreement":null},{"id":"W2252465257","doi":"10.1002/2015gl067618","title":"First observations of triple‐frequency radar Doppler spectra in snowfall: Interpretation and applications","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Precipitation Measurement and Analysis","field":"Earth and Planetary Sciences","cited_by":101,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Deutscher Akademischer Austauschdienst; Natural Environment Research Council; Sight Research UK","keywords":"Snow; Spectral line; Radar; Doppler effect; Doppler radar; Environmental science; Meteorology; Physics; Remote sensing; Precipitation; Computational physics; Geology; Computer science; Telecommunications","score_opus":0.053719885810689774,"score_gpt":0.2853494138241053,"score_spread":0.23162952801341552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2252465257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9846176,0.00039665552,0.013643828,0.000042260115,0.00001977289,0.000011058189,0.00022795309,0.00011596241,0.0009249673],"genre_scores_gemma":[0.99418914,0.000064699285,0.0055710156,0.0000068749996,0.000008969931,0.0000028283882,0.00008549578,0.0000055343467,0.00006539405],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999928,0.000011920041,0.000004029536,0.000019521003,0.000020948135,0.000015467014],"domain_scores_gemma":[0.9997507,0.000069421556,0.00004189553,0.000032036878,0.00006333437,0.000042673066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024672094,0.00022159718,0.00024790133,0.00078767457,0.00023510645,0.00033576423,0.0001942189,0.00030483815,0.0006082475],"category_scores_gemma":[0.00043495733,0.00012826857,0.00016944064,0.0005810742,0.00021906389,0.00031323577,0.0003252175,0.00026856887,0.00012883096],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008143511,0.00017510408,0.20114802,0.00023390769,0.000083440296,0.00071249186,0.0004371905,0.0056062867,0.6704593,0.0011771644,0.0008226299,0.11833013],"study_design_scores_gemma":[0.00006938873,0.000516806,0.7095773,0.0000772282,0.00010845462,0.0017274739,0.00054734905,0.11532796,0.1639251,0.004104079,0.0039554397,0.00006337684],"about_ca_topic_score_codex":0.00052245264,"about_ca_topic_score_gemma":0.0009135455,"teacher_disagreement_score":0.00078767457,"about_ca_system_score_codex":0.00011396959,"about_ca_system_score_gemma":0.00009888438,"threshold_uncertainty_score":0.0020347238},"labels":[],"label_agreement":null},{"id":"W2253677266","doi":"10.1002/2015gl065702","title":"The changing ozone depletion potential of N<sub>2</sub>O in a future climate","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Eidgenössische Technische Hochschule Zürich; National Aeronautics and Space Administration","keywords":"Ozone depletion; Ozone; Ozone layer; Stratosphere; Nitrous oxide; Greenhouse gas; Atmospheric sciences; Environmental science; NOx; Nitrogen; Atmospheric chemistry; Environmental chemistry; Montreal Protocol; Chemistry; Geology; Oceanography","score_opus":0.021374521181893157,"score_gpt":0.2631871575495385,"score_spread":0.24181263636764533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2253677266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996414,0.00016137278,0.00031894364,0.00026436316,0.000020851558,0.0000036037072,0.00063873094,0.000016304026,0.0021618607],"genre_scores_gemma":[0.99960285,0.000043969114,0.00008111543,0.000023627266,0.000004019215,0.000002500982,0.00016070264,0.0000020199402,0.00007928583],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990964,0.00001607396,0.000004064064,0.00002310416,0.000011838527,0.00003529013],"domain_scores_gemma":[0.999813,0.000053409763,0.000042465344,0.000009795602,0.000042228367,0.00003914808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039650753,0.00028106128,0.0001655885,0.0003063228,0.00032393145,0.00065604417,0.00023109537,0.00096567115,0.001008454],"category_scores_gemma":[0.000567973,0.00011577638,0.00035513463,0.0002898357,0.0003087078,0.00071076077,0.00031745888,0.00027273645,0.000112326175],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002952437,0.0003200622,0.6916055,0.00033981187,0.00057389465,0.0027417287,0.0002204311,0.14374563,0.124755174,0.008275965,0.0055167894,0.018952599],"study_design_scores_gemma":[0.00007708877,0.00036625966,0.86870366,0.000041969954,0.00019372482,0.0003789298,0.0006873616,0.105974,0.014385312,0.0045341626,0.0045880647,0.00006960532],"about_ca_topic_score_codex":0.009617343,"about_ca_topic_score_gemma":0.0085449405,"teacher_disagreement_score":0.009617343,"about_ca_system_score_codex":0.0009477133,"about_ca_system_score_gemma":0.00027163874,"threshold_uncertainty_score":0.01912272},"labels":[],"label_agreement":null},{"id":"W2259483905","doi":"10.1002/2016gl067717","title":"Wave equation‐based reflection tomography of the 1992 Landers earthquake area","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canada Foundation for Innovation; National Natural Science Foundation of China; Southern California Earthquake Center","keywords":"Geology; Seismology; Crust; Seismic tomography; Tomography; High resolution; Tectonics; Mantle (geology); Upwelling; Geophysics; Remote sensing","score_opus":0.07395879891498357,"score_gpt":0.2831078538515182,"score_spread":0.20914905493653463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2259483905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98705506,0.000037010323,0.010487643,0.00005936395,0.0000026924004,0.000012029388,0.0005049635,0.00035096402,0.0014902372],"genre_scores_gemma":[0.99234664,0.000028257662,0.006808022,0.000005277748,0.000003626181,0.000004308678,0.0004267001,0.000023416798,0.00035369102],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999504,0.000006885681,0.0000032974274,0.000015562218,0.000015760428,0.000008078094],"domain_scores_gemma":[0.9998909,0.000020369687,0.000030865885,0.000018200368,0.000032419593,0.00000718009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013345106,0.00018584794,0.000109235756,0.00046914845,0.00007174715,0.0003631735,0.00027864715,0.00018391885,0.001125125],"category_scores_gemma":[0.0005893442,0.0001756541,0.00015337714,0.0004538508,0.00010841966,0.00030007286,0.00017043506,0.00021658989,0.00017553306],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005592294,0.00021679822,0.36307448,0.00012584036,0.00022415079,0.00073556585,0.00063354074,0.3024476,0.15050496,0.0026078173,0.002396401,0.17647368],"study_design_scores_gemma":[0.0000877643,0.00008576705,0.3863068,0.000008665967,0.00006701245,0.00013659358,0.00011687324,0.603376,0.00857124,0.00041609432,0.00079545495,0.00003179252],"about_ca_topic_score_codex":0.027021145,"about_ca_topic_score_gemma":0.037069295,"teacher_disagreement_score":0.027021145,"about_ca_system_score_codex":0.00027681162,"about_ca_system_score_gemma":0.00033798587,"threshold_uncertainty_score":0.053727746},"labels":[],"label_agreement":null},{"id":"W2260594164","doi":"10.1002/2015gl066855","title":"Regional variability of a projected sea ice‐free Arctic during the summer months","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Environment and Climate Change Canada","funders":"U.S. Department of Energy","keywords":"Sea ice; Arctic ice pack; Arctic; Climatology; Arctic sea ice decline; Arctic geoengineering; Climate change; Cryosphere; Oceanography; The arctic; Physical geography; Environmental science; Geology; Drift ice; Geography","score_opus":0.050001972226491005,"score_gpt":0.2843235320008067,"score_spread":0.23432155977431568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2260594164","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99698657,0.000053483294,0.00073470303,0.000040952233,0.000008519268,0.0000025163315,0.0011805586,0.000030121933,0.0009625767],"genre_scores_gemma":[0.99819785,0.000035125817,0.00026089814,0.0000058234095,0.000005428941,0.0000040262366,0.0012889138,0.0000052581627,0.00019671665],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988675,0.000028451523,0.000006774322,0.000035441702,0.000020480027,0.00002206099],"domain_scores_gemma":[0.99955374,0.00007989956,0.00010227558,0.000029091663,0.0001598934,0.00007505032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006140867,0.00029648974,0.00016577018,0.00034979574,0.00024965394,0.00062884006,0.0001905332,0.0003027473,0.00068478874],"category_scores_gemma":[0.0006220574,0.00013587896,0.00039179687,0.00032754338,0.000120205004,0.00023839984,0.000250477,0.00021745503,0.00033806806],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000983922,0.00009205902,0.9253964,0.00003614336,0.00023209212,0.00017092245,0.00031754785,0.055600647,0.0068104155,0.0007725035,0.001873847,0.0077135116],"study_design_scores_gemma":[0.000017233313,0.00020145088,0.95784813,0.000011822345,0.000046236364,0.00012088534,0.0002406115,0.037623115,0.0015761136,0.00018436769,0.0021156915,0.0000143823945],"about_ca_topic_score_codex":0.014798813,"about_ca_topic_score_gemma":0.00936139,"teacher_disagreement_score":0.014798813,"about_ca_system_score_codex":0.0003682874,"about_ca_system_score_gemma":0.00023799422,"threshold_uncertainty_score":0.029425383},"labels":[],"label_agreement":null},{"id":"W2260766045","doi":"10.1002/2015gl066970","title":"Is the subarctic landscape still a carbon sink? Evidence from a detailed catchment balance","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Vetenskapsrådet","keywords":"Subarctic climate; Sink (geography); Environmental science; Drainage basin; Peat; Carbon sink; Watershed; Water balance; Soil water; Catchment hydrology; Hydrology (agriculture); Climate change; Ecology; Geography; Geology; Soil science; Biology","score_opus":0.0760555123091823,"score_gpt":0.3081105046601811,"score_spread":0.2320549923509988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2260766045","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99235356,0.00055961695,0.0014352954,0.00022435402,0.000005792253,0.0000071010136,0.0011624253,0.000059713017,0.0041921283],"genre_scores_gemma":[0.99885225,0.00019217844,0.00025954744,0.00003992321,0.000009050261,0.0000027308747,0.00039274135,0.0000097500815,0.0002418766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988854,0.000021959771,0.000008909995,0.000041777297,0.000022864317,0.000015883845],"domain_scores_gemma":[0.99902487,0.00020018381,0.00026035815,0.00017270408,0.00023082715,0.00011115523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005437593,0.00019619182,0.0003720827,0.00094394386,0.00020300921,0.0009727117,0.00032617166,0.0002021092,0.0034999894],"category_scores_gemma":[0.0012694594,0.000138539,0.00020654731,0.001183976,0.00055302866,0.0010426685,0.0005582205,0.00015994349,0.00022044173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019790743,0.00003351209,0.9548993,0.00013341654,0.00048364274,0.00019073636,0.00035785246,0.0061494554,0.009130392,0.0028694493,0.0004951285,0.02505916],"study_design_scores_gemma":[0.0000046356527,0.000008809316,0.99460644,0.0000075541598,0.000066040004,0.00003528612,0.00008980027,0.0030104795,0.00021409537,0.0010742885,0.0008777269,0.0000048434854],"about_ca_topic_score_codex":0.014813927,"about_ca_topic_score_gemma":0.02457215,"teacher_disagreement_score":0.014813927,"about_ca_system_score_codex":0.0007442999,"about_ca_system_score_gemma":0.00033722195,"threshold_uncertainty_score":0.029455423},"labels":[],"label_agreement":null},{"id":"W2262372491","doi":"10.1002/2015gl067580","title":"High‐resolution auroral acceleration signatures within a highly dynamic onset arc","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; National Aeronautics and Space Administration","keywords":"Physics; Acceleration; Electron; Astrophysics; Particle acceleration; Flux (metallurgy); Spacecraft; Electron precipitation; Arc (geometry); Pitch angle; Magnetic field; Geophysics; Astronomy; Magnetosphere; Materials science; Geometry","score_opus":0.014318451219645848,"score_gpt":0.27878417550440043,"score_spread":0.26446572428475457,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2262372491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959253,0.0001209155,0.0003590538,0.000021693122,0.0000041672442,0.000005199432,0.00018505057,0.0000396084,0.0033389712],"genre_scores_gemma":[0.99878293,0.000045616453,0.00053042045,0.0000071593954,0.000006719994,0.0000026856285,0.00023575297,0.0000091756865,0.0003796344],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999516,0.0000031318993,0.0000013720122,0.000016124906,0.0000123210775,0.000015448053],"domain_scores_gemma":[0.9998994,0.000015218553,0.000027286782,0.000013842689,0.000020411631,0.000023888892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009143574,0.00013187413,0.00018135687,0.00047543788,0.0002791239,0.0004298544,0.00015918959,0.00015709033,0.00086392596],"category_scores_gemma":[0.00015079642,0.0001456566,0.00012634294,0.0003076753,0.00015319136,0.00016275053,0.0003959668,0.00035300842,0.00015744093],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009930006,0.0000993736,0.37174082,0.000097728145,0.000115961004,0.0030738788,0.0011492376,0.0018234166,0.5743598,0.0006272554,0.0012928387,0.044626772],"study_design_scores_gemma":[0.000012961341,0.00007462515,0.9873395,0.00000784689,0.000016751783,0.0005536024,0.0001692164,0.0011772676,0.008375373,0.000068694295,0.0021948419,0.000009331244],"about_ca_topic_score_codex":0.0021965976,"about_ca_topic_score_gemma":0.0045016883,"teacher_disagreement_score":0.0021965976,"about_ca_system_score_codex":0.00019512359,"about_ca_system_score_gemma":0.000093161834,"threshold_uncertainty_score":0.0043676496},"labels":[],"label_agreement":null},{"id":"W2262592349","doi":"10.1002/2015gl067370","title":"MESSENGER observations of induced magnetic fields in Mercury's core","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Carnegie Institution of Washington; Johns Hopkins University; National Aeronautics and Space Administration","keywords":"Magnetopause; Magnetosphere; Mercury (programming language); Geophysics; Magnetometer; Physics; Spacecraft; Dipole; Mercury's magnetic field; Magnetosheath; Geodesy; Electrojet; Magnetic field; Geology; Earth's magnetic field; Astronomy; L-shell","score_opus":0.10302242378408176,"score_gpt":0.32367282348702237,"score_spread":0.2206503997029406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2262592349","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99892455,0.000023447896,0.000071359274,0.0000125195165,0.0000014381999,0.0000013209299,0.00021480372,0.00001862347,0.00073188916],"genre_scores_gemma":[0.9994646,0.000013193804,0.0000962144,0.0000064569817,0.0000031826341,0.0000014147213,0.00025829297,0.0000025787353,0.0001541929],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999684,0.0000026505174,9.696388e-7,0.000007126003,0.0000135368155,0.000007215009],"domain_scores_gemma":[0.99990225,0.000014211533,0.00003231165,0.000009241266,0.000020733287,0.00002119359],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001088805,0.00009009325,0.00010996346,0.0004949949,0.000113653994,0.00016534347,0.00009652774,0.00011713907,0.0003855406],"category_scores_gemma":[0.00023504975,0.00006360214,0.00008466664,0.0002447489,0.00012359265,0.00008769973,0.00025918765,0.00013360335,0.00008972775],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044739913,0.00007286135,0.6789121,0.00004736465,0.000094567506,0.0003428075,0.0006089092,0.0016268556,0.29750526,0.00042378335,0.0009931106,0.018925006],"study_design_scores_gemma":[0.000009157197,0.000073188414,0.9910122,0.0000031423401,0.000012497668,0.00005441402,0.000026744452,0.00067692256,0.0072433325,0.000051022464,0.00083320204,0.000004207852],"about_ca_topic_score_codex":0.002894476,"about_ca_topic_score_gemma":0.0052027297,"teacher_disagreement_score":0.002894476,"about_ca_system_score_codex":0.00031988812,"about_ca_system_score_gemma":0.000100084326,"threshold_uncertainty_score":0.0057552457},"labels":[],"label_agreement":null},{"id":"W2264582771","doi":"10.1002/2015gl067193","title":"Permafrost thaw and wildfire: Equally important drivers of boreal tree cover changes in the Taiga Plains, Canada","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal","funders":"","keywords":"Permafrost; Taiga; Boreal; Physical geography; Thermokarst; Environmental science; Disturbance (geology); Land cover; Climate change; Geology; Climatology; Ecology; Land use; Geography; Forestry; Geomorphology; Oceanography; Paleontology","score_opus":0.036594040422700216,"score_gpt":0.2664611962029873,"score_spread":0.2298671557802871,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2264582771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983669,0.00019511479,0.00006425477,0.00009328316,0.0000034862974,0.0000045831976,0.000609055,0.0000063347184,0.0006571338],"genre_scores_gemma":[0.99935526,0.00007837492,0.000046026107,0.000014839799,0.0000018642759,0.0000017068724,0.00030029798,0.0000019307859,0.00019967505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980253,0.000017568904,0.000009625569,0.000041347073,0.00004470796,0.00008419083],"domain_scores_gemma":[0.99913424,0.00007900228,0.0001907571,0.00002963702,0.00026381077,0.00030245996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028738214,0.00021676013,0.00021600212,0.0009202474,0.0012924476,0.0009053119,0.00043283406,0.00019112199,0.0012829719],"category_scores_gemma":[0.0008860708,0.00011262724,0.00040089645,0.0013225129,0.000521874,0.0003335238,0.00057926105,0.00031787346,0.00007162055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026137956,0.000010124473,0.99724495,0.0000054081243,0.000033432738,0.00003332476,0.0001734912,0.00022063314,0.00033786002,0.000056967354,0.00017555097,0.0016821446],"study_design_scores_gemma":[0.00000106014,0.0000023280138,0.99898976,0.000003911258,0.000008352807,0.000012044915,0.0004170501,0.00036452696,0.000028911394,0.000016460292,0.0001531272,0.0000024299268],"about_ca_topic_score_codex":0.96959025,"about_ca_topic_score_gemma":0.9894225,"teacher_disagreement_score":0.030409753,"about_ca_system_score_codex":0.0058078878,"about_ca_system_score_gemma":0.0075733555,"threshold_uncertainty_score":0.06117761},"labels":[],"label_agreement":null},{"id":"W2273604364","doi":"10.1002/2015gl067388","title":"Enhanced terrestrial carbon preservation promoted by reactive iron in deltaic sediments","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"University of Florida","keywords":"Subaerial; Coprecipitation; Chronosequence; Authigenic; Adsorption; Geology; Environmental chemistry; Total organic carbon; Mineralogy; Carbon fibers; Chemistry; Diagenesis; Geochemistry; Inorganic chemistry; Soil science; Soil water; Organic chemistry","score_opus":0.030331848769450925,"score_gpt":0.2936296081680333,"score_spread":0.26329775939858235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2273604364","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995086,0.00008413398,0.00008293615,0.000008134859,5.898933e-7,0.0000013644875,0.00003644254,0.000005505003,0.0002722696],"genre_scores_gemma":[0.9996264,0.000044976357,0.00010803775,0.000006724085,8.5779425e-7,0.0000010495532,0.000025729927,0.0000019201802,0.00018423291],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999455,0.000005502128,0.000003106533,0.000018039236,0.000010583643,0.000017261109],"domain_scores_gemma":[0.99986756,0.000012721273,0.00003521932,0.000007490199,0.00005387839,0.000023196399],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013239992,0.00023844461,0.0001546865,0.0006201737,0.0005070828,0.0004739953,0.00021558425,0.00026436636,0.00053905946],"category_scores_gemma":[0.00015629426,0.0001711167,0.00008531689,0.00026899707,0.0003663352,0.00020764518,0.00023454806,0.00016635796,0.00008643781],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022215885,0.00002740794,0.18074703,0.000105143365,0.000062046594,0.00042391085,0.00039254728,0.0009277945,0.8108395,0.0001662169,0.00005996816,0.0060263015],"study_design_scores_gemma":[0.000008215577,0.00012268222,0.933191,0.000011079088,0.000029962275,0.00016528454,0.0004386654,0.0013922463,0.063256904,0.00008272644,0.0012923586,0.0000088618],"about_ca_topic_score_codex":0.018068202,"about_ca_topic_score_gemma":0.025008615,"teacher_disagreement_score":0.018068202,"about_ca_system_score_codex":0.0006039646,"about_ca_system_score_gemma":0.000266714,"threshold_uncertainty_score":0.035926044},"labels":[],"label_agreement":null},{"id":"W2274376048","doi":"10.1002/2015gl067532","title":"Potential near‐future carbon uptake overcomes losses from a large insect outbreak in British Columbia, Canada","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria; Canadian Forest Service; Natural Resources Canada; Environment and Climate Change Canada","funders":"Natural Resources Canada; University of East Anglia; Pacific Institute for Climate Solutions; University of Victoria","keywords":"Climate change; Environmental science; Carbon sink; Outbreak; Ecosystem; Atmospheric sciences; Carbon fibers; Mountain pine beetle; Sink (geography); Climatology; Ecology; Geography; Forestry; Biology; Geology","score_opus":0.0072733176388864226,"score_gpt":0.21963776325453963,"score_spread":0.2123644456156532,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2274376048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9930506,0.00020108839,0.00022816112,0.00048374914,0.000009746825,0.000014445607,0.0009451056,0.000030257946,0.0050368537],"genre_scores_gemma":[0.99825734,0.00010601572,0.00016755362,0.00005151777,0.0000014483709,0.0000041309304,0.0002922117,0.0000041362837,0.0011156406],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998381,0.000016074773,0.0000041974286,0.00002447966,0.0000203222,0.00009679899],"domain_scores_gemma":[0.9997267,0.000031903422,0.000026549955,0.000010801021,0.00010651374,0.00009744905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025420656,0.00033293103,0.00033034038,0.00042436123,0.0016667728,0.0017577785,0.0009899103,0.0006664053,0.0033155663],"category_scores_gemma":[0.000706207,0.00022443819,0.0003641543,0.00071458524,0.00056624063,0.00049130135,0.0004925921,0.00056280673,0.00020476857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012424935,0.0004057146,0.6416618,0.000244977,0.0004490451,0.0012364774,0.00080834754,0.2928834,0.012343846,0.0038905225,0.012137269,0.03269608],"study_design_scores_gemma":[0.00019436936,0.00017662208,0.73623264,0.00006645023,0.00023366201,0.00015174213,0.004562171,0.24679989,0.001948208,0.0014442466,0.008089473,0.000100581354],"about_ca_topic_score_codex":0.9939208,"about_ca_topic_score_gemma":0.9961463,"teacher_disagreement_score":0.030769635,"about_ca_system_score_codex":0.030769635,"about_ca_system_score_gemma":0.016122045,"threshold_uncertainty_score":0.22325033},"labels":[],"label_agreement":null},{"id":"W2275686692","doi":"10.1002/2015gl067623","title":"Emissions of coalbed and natural gas methane from abandoned oil and gas wells in the United States","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Regional Municipality of Niagara","funders":"Robertson Foundation; Walton Family Foundation; U.S. Forest Service; Environmental Defense Fund; National Science Foundation","keywords":"Coalbed methane; Natural gas; Methane; Fossil fuel; Environmental science; Methane emissions; Geology; Isotopes of carbon; Water well; Hydrology (agriculture); Petroleum engineering; Isotope; Greenhouse gas; Coal; Groundwater; Coal mining; Geography; Waste management; Chemistry; Oceanography","score_opus":0.013100296790053341,"score_gpt":0.2625073795958336,"score_spread":0.24940708280578025,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2275686692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995535,0.000036527723,0.0000683127,0.000010731964,6.686822e-7,9.877366e-7,0.00016330765,0.0000031272507,0.00016272698],"genre_scores_gemma":[0.9995938,0.00004045797,0.000115395356,0.0000058790397,4.2269102e-7,0.0000020784776,0.00014517173,7.167699e-7,0.000096096424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991417,0.000021871841,0.0000056913727,0.000018850425,0.00002572855,0.000013594076],"domain_scores_gemma":[0.99974793,0.00005119318,0.00010110868,0.00001130783,0.00006104602,0.000027470496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014950332,0.00013988795,0.00011857939,0.00030872045,0.00019745952,0.00026256556,0.00015080822,0.0001453012,0.00030933265],"category_scores_gemma":[0.00023427718,0.000101153564,0.0001186356,0.000509215,0.0001829661,0.00020129033,0.00022950431,0.000121934376,0.000048467187],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013556232,0.000041433614,0.98697567,0.000018558096,0.000049777645,0.0001302415,0.0002094151,0.0014897102,0.004421015,0.000057339636,0.00020968649,0.006261569],"study_design_scores_gemma":[0.000006413753,0.000068310095,0.99336326,0.000015033539,0.000023318356,0.00008032823,0.0006117837,0.003321182,0.0018750877,0.00007462344,0.00055318966,0.000007509916],"about_ca_topic_score_codex":0.06448223,"about_ca_topic_score_gemma":0.15321419,"teacher_disagreement_score":0.06448223,"about_ca_system_score_codex":0.0006704566,"about_ca_system_score_gemma":0.0003084939,"threshold_uncertainty_score":0.12821376},"labels":[],"label_agreement":null},{"id":"W2275741740","doi":"10.1002/2015gl067418","title":"Rapid automated W‐phase slip inversion for the Illapel great earthquake (2015, <i>M</i><i><sub>w</sub></i> = 8.3)","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Comisión Nacional de Investigación Científica y Tecnológica; Australian Research Council","keywords":"Seismology; Geology; Trench; Inversion (geology); Slip (aerodynamics); Rake; Geodesy; Tectonics; Physics; Geomorphology","score_opus":0.04202746635573346,"score_gpt":0.2932098401865539,"score_spread":0.2511823738308204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2275741740","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9338728,0.00006184359,0.053131055,0.00016272294,0.000037439517,0.00008341121,0.0018227347,0.0052412795,0.0055866763],"genre_scores_gemma":[0.9444123,0.000016086598,0.052676864,0.000032487394,0.000013132255,0.000027503098,0.0017373065,0.00014726607,0.0009369777],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9998989,0.000018050923,0.000004415392,0.000022987078,0.0000313262,0.000024294017],"domain_scores_gemma":[0.99974257,0.00007871367,0.00003759309,0.00003403782,0.00008165139,0.000025516694],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000290408,0.00036408,0.00027867878,0.000630741,0.00019090761,0.00034899582,0.00041992564,0.00021502998,0.0029142143],"category_scores_gemma":[0.0011188756,0.00017645468,0.00016972102,0.00035059097,0.00013557197,0.00032535888,0.00039899015,0.00022657885,0.00060978107],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018813042,0.00055882335,0.083300605,0.00018599938,0.00024130695,0.0010326339,0.0007429496,0.25849447,0.12959403,0.001993716,0.015889678,0.5060844],"study_design_scores_gemma":[0.00022174031,0.00012945599,0.034953948,0.00001196824,0.000022545431,0.000098620825,0.00017425523,0.94316703,0.017999643,0.0006277865,0.0025550271,0.0000380004],"about_ca_topic_score_codex":0.012104228,"about_ca_topic_score_gemma":0.022585448,"teacher_disagreement_score":0.012104228,"about_ca_system_score_codex":0.00020328503,"about_ca_system_score_gemma":0.0007043855,"threshold_uncertainty_score":0.024067521},"labels":[],"label_agreement":null},{"id":"W2276738526","doi":"10.1002/2015gl066151","title":"Effects of lateral variations in megaregolith thickness on predicted lunar seismic signals","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Seismogram; Geology; Seismology; Scattering; Crust; Seismic energy; Seismic wave; Geophysics; Synthetic seismogram; Optics; Physics","score_opus":0.03223193662184847,"score_gpt":0.29609810050627583,"score_spread":0.26386616388442735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2276738526","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931676,0.00003087909,0.006278176,0.000015796997,0.0000028365027,0.000003152534,0.000087204484,0.00007590068,0.00033854652],"genre_scores_gemma":[0.99919015,0.000018822071,0.00064302114,0.0000030154224,8.8744184e-7,0.0000020489808,0.00007244202,0.000015529518,0.00005409898],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981743,0.00006310358,0.000009747494,0.000029221672,0.000040165127,0.00004031933],"domain_scores_gemma":[0.99829274,0.0011987613,0.00015517607,0.00014145282,0.0001343289,0.00007748891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061439374,0.00035915547,0.00020473088,0.00025300484,0.00018012003,0.00041227762,0.0003203392,0.00037001199,0.001095463],"category_scores_gemma":[0.0036050244,0.00032508202,0.00038284517,0.00024678657,0.00034919995,0.00036771153,0.00042572527,0.00024867756,0.00015030519],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009253106,0.00008476204,0.11823918,0.00007921152,0.00015410993,0.0005703762,0.00013622703,0.74503523,0.119653314,0.00070333993,0.00011906308,0.014299863],"study_design_scores_gemma":[0.000029248191,0.0001321749,0.09379228,0.000012530124,0.0000628194,0.00009652193,0.00007974745,0.8744165,0.03097945,0.00024055477,0.00012380855,0.000034391014],"about_ca_topic_score_codex":0.0034308594,"about_ca_topic_score_gemma":0.0029658717,"teacher_disagreement_score":0.0034308594,"about_ca_system_score_codex":0.00024435905,"about_ca_system_score_gemma":0.00026004433,"threshold_uncertainty_score":0.006821811},"labels":[],"label_agreement":null},{"id":"W2277027043","doi":"10.1002/2016gl067730","title":"Surface temperature dependence of tropical cyclone‐permitting simulations in a spherical model with uniform thermal forcing","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Compute Canada; U.S. Department of Energy","keywords":"Convection; Spherical geometry; Forcing (mathematics); Tropical cyclone; Radiative transfer; Atmospheric sciences; Radiative cooling; Sea surface temperature; Thermal; Radiative equilibrium; Physics; Geology; Climatology; Environmental science; Geometry; Mechanics; Meteorology; Mathematics","score_opus":0.03004716786195146,"score_gpt":0.2824195274450032,"score_spread":0.25237235958305176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2277027043","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99457055,0.00004896957,0.00085002556,0.00009486194,0.000014613918,0.00001595047,0.00037466528,0.0001181086,0.0039122193],"genre_scores_gemma":[0.99863666,0.000037837945,0.00057144946,0.000024090194,0.000004388874,0.00001611473,0.00041146288,0.000035801124,0.0002621274],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982303,0.000053176358,0.0000117168975,0.000025759935,0.000028799126,0.000057562145],"domain_scores_gemma":[0.99902534,0.00044350183,0.00010786822,0.00010012284,0.00019362231,0.0001294962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041806613,0.00056419725,0.0005857892,0.00035171764,0.0005564709,0.00073755434,0.00070815167,0.0006501216,0.0018733249],"category_scores_gemma":[0.0024171234,0.00037112122,0.0008089893,0.00044521948,0.00058892474,0.00047382383,0.00045035873,0.0006316942,0.00019163749],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013843292,0.00007775506,0.007149019,0.000030234554,0.000051717554,0.000086691914,0.00004636798,0.9870569,0.0033589578,0.00066915486,0.00033399215,0.0010007784],"study_design_scores_gemma":[0.000062473555,0.00010489326,0.0041792197,0.000006682071,0.000027087463,0.000013884978,0.00004991144,0.994152,0.0010721282,0.0001430506,0.00017543731,0.000013236231],"about_ca_topic_score_codex":0.051089916,"about_ca_topic_score_gemma":0.024001569,"teacher_disagreement_score":0.051089916,"about_ca_system_score_codex":0.00073261047,"about_ca_system_score_gemma":0.0009484103,"threshold_uncertainty_score":0.10158509},"labels":[],"label_agreement":null},{"id":"W2279844682","doi":"10.1002/2015gl067235","title":"Variability of the directly observed, middepth subpolar North Atlantic circulation","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Oceanography; Bathymetry; Ocean current; North Atlantic Deep Water; Climatology; Geology; Ridge; Thermohaline circulation; Gulf Stream; Boundary current; Structural basin; Geomorphology","score_opus":0.036607339162984594,"score_gpt":0.24556979447755015,"score_spread":0.20896245531456556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2279844682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887973,0.000030906478,0.00006869973,0.000014539177,0.0000024802773,0.000001038471,0.0005779376,0.0000046415967,0.00042015553],"genre_scores_gemma":[0.9991365,0.000020942376,0.000046346966,0.0000054634943,0.0000033184826,0.0000010513413,0.0006827115,0.000001108028,0.00010249383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989676,0.000016271557,0.000007256405,0.00003845046,0.000022023123,0.000019176457],"domain_scores_gemma":[0.9996393,0.00007498584,0.00010841339,0.00004102346,0.00008290555,0.000053296895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020395328,0.000081984654,0.00011118115,0.00040751018,0.00012433558,0.0004414814,0.00012904772,0.00014734716,0.0006410781],"category_scores_gemma":[0.0008390209,0.000071935894,0.00012297476,0.00037626075,0.0001672365,0.00024910708,0.00022575489,0.00016658875,0.00016817069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047577534,0.000020171414,0.99227,0.000005825378,0.000042345688,0.00002271511,0.000075800126,0.00042570874,0.0029295003,0.00006472685,0.00022232838,0.003873231],"study_design_scores_gemma":[8.768366e-7,0.0000059364966,0.99929464,0.0000013325913,0.000002973684,0.000012112186,0.000024113308,0.00041098095,0.00011510862,0.000007824303,0.00012293548,0.0000011771522],"about_ca_topic_score_codex":0.014041911,"about_ca_topic_score_gemma":0.022215657,"teacher_disagreement_score":0.014041911,"about_ca_system_score_codex":0.00025374358,"about_ca_system_score_gemma":0.00012610416,"threshold_uncertainty_score":0.027920306},"labels":[],"label_agreement":null},{"id":"W2281567183","doi":"10.1002/2015gl067050","title":"What would happen to Superstorm Sandy under the influence of a substantially warmer Atlantic Ocean?","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Pacific Northwest National Laboratory; NASA Headquarters; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Extratropical cyclone; Storm; Climatology; Landfall; Middle latitudes; Oceanography; Clockwise; Nova scotia; Environmental science; Latitude; Geology; Rotation (mathematics)","score_opus":0.03569803730450973,"score_gpt":0.292608502139277,"score_spread":0.2569104648347673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2281567183","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99475265,0.000042154425,0.0005671868,0.0013275445,0.00006730318,0.00000851147,0.000117520976,0.000024656554,0.0030923893],"genre_scores_gemma":[0.99969375,0.00001626999,0.00004777399,0.00008965982,0.00000813621,0.0000014008639,0.000016502692,0.0000027738245,0.00012384554],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983835,0.00004379306,0.0000065303666,0.000031849653,0.000016369484,0.00006305269],"domain_scores_gemma":[0.999548,0.0001245636,0.00008788416,0.000029690236,0.00006795385,0.00014188458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005565863,0.00017857566,0.00028096457,0.00011668456,0.00052700704,0.0007373017,0.0003355254,0.00078016333,0.002124389],"category_scores_gemma":[0.0019324549,0.00013691383,0.00039437666,0.000098792676,0.0004972298,0.0005059142,0.00041953032,0.0005446624,0.000116644616],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010008122,0.00020469468,0.566822,0.00015482405,0.0006278195,0.0024641622,0.00052581704,0.37821686,0.023440452,0.011039176,0.0069342456,0.008569185],"study_design_scores_gemma":[0.00030467974,0.00044363586,0.38934955,0.000038744365,0.0002853766,0.00022227546,0.0030135652,0.5884549,0.004747539,0.00976512,0.003257383,0.0001172049],"about_ca_topic_score_codex":0.036850754,"about_ca_topic_score_gemma":0.033795554,"teacher_disagreement_score":0.036850754,"about_ca_system_score_codex":0.0009142295,"about_ca_system_score_gemma":0.00050395844,"threshold_uncertainty_score":0.073272526},"labels":[],"label_agreement":null},{"id":"W2283604196","doi":"10.1002/2016gl067897","title":"Earth's ion upflow associated with polar cap patches: Global and in situ observations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Key Research and Development Program of China; Science and Technology Facilities Council; Natural Environment Research Council; Natural Science Foundation of Shandong Province; Chinese Arctic and Antarctic Administration; National Natural Science Foundation of China; University of Leicester; National Oceanic and Atmospheric Administration; Sight Research UK; Norges Forskningsråd; National Aeronautics and Space Administration; National Science Foundation","keywords":"Ionosphere; Magnetosphere; Geophysics; Polar; Geomagnetic storm; Earth's magnetic field; Ion; Satellite; Upwelling; In situ; Physics; Atmospheric sciences; Geology; Plasma; Environmental science; Meteorology; Magnetic field; Astronomy; Oceanography","score_opus":0.01968906095537475,"score_gpt":0.2645938292552782,"score_spread":0.24490476829990343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2283604196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985605,0.000044968092,0.00016856934,0.00001403378,0.000004964157,0.0000039939896,0.00047791703,0.000020060195,0.0007049582],"genre_scores_gemma":[0.9989035,0.000046199457,0.00029899087,0.00001032255,0.00001432547,0.0000039113716,0.00060239393,0.000005240881,0.00011505116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999949,0.000004499428,0.000002127235,0.000019701634,0.000010535011,0.00001420797],"domain_scores_gemma":[0.9998511,0.000016550937,0.000056289853,0.00001392549,0.000025985764,0.000036146434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011930652,0.00021504004,0.00024732153,0.0007960474,0.00028870083,0.00038586545,0.00017196282,0.0002777313,0.0005763244],"category_scores_gemma":[0.00016723028,0.00013087857,0.00017353454,0.0006606203,0.0002069388,0.00028382626,0.0004044084,0.00016456631,0.00012036076],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003850807,0.00009455961,0.85683215,0.000061586295,0.00011070784,0.0003790473,0.0005958141,0.0011417521,0.12988473,0.00006905157,0.0005950594,0.009850392],"study_design_scores_gemma":[0.0000055592377,0.00003839531,0.9967006,0.0000036184313,0.000016508026,0.00008192333,0.00014558068,0.0008264166,0.0018291025,0.000015448943,0.00033352425,0.0000034295263],"about_ca_topic_score_codex":0.0043501775,"about_ca_topic_score_gemma":0.0064141545,"teacher_disagreement_score":0.0043501775,"about_ca_system_score_codex":0.00016024667,"about_ca_system_score_gemma":0.00009249977,"threshold_uncertainty_score":0.008649707},"labels":[],"label_agreement":null},{"id":"W2284585119","doi":"10.1002/2016gl067720","title":"The implication of nonradiative energy fluxes dominating Greenland ice sheet exceptional ablation area surface melt in 2012","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":108,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Nationale Geologiske Undersøgelser for Danmark og Grønland; Danmarks Frie Forskningsfond; NordForsk","keywords":"Greenland ice sheet; Climatology; Environmental science; Ice sheet; Ablation; Ablation zone; Atmospheric sciences; Climate model; Dominance (genetics); Geology; Climate change; Oceanography; Glacier; Geomorphology","score_opus":0.03655846987866508,"score_gpt":0.2823046120047866,"score_spread":0.24574614212612156,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2284585119","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891305,0.000059848495,0.00013108953,0.00007834936,0.0000036884405,0.0000014132207,0.00026863423,0.000017705377,0.00052622496],"genre_scores_gemma":[0.9995536,0.0000310769,0.000095773634,0.000018338153,0.0000034382906,0.0000011728579,0.00022007851,0.000005808928,0.000070691414],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998658,0.000025111734,0.000011361918,0.000040271665,0.000022784283,0.000034776724],"domain_scores_gemma":[0.99974734,0.0000545566,0.00008460632,0.000021836682,0.00005659199,0.000035008816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004640018,0.00019410059,0.00020712927,0.00047893118,0.0004405689,0.0008924319,0.00019989623,0.00026448056,0.0005213415],"category_scores_gemma":[0.00059312984,0.00013583673,0.00023322279,0.00046851562,0.00037595237,0.0005675912,0.00038576618,0.00023464579,0.00005413422],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021518147,0.000029145818,0.965451,0.000046250487,0.00012392674,0.0002833502,0.00043638877,0.009023531,0.013529921,0.00037408556,0.00062622095,0.009860953],"study_design_scores_gemma":[0.0000037856937,0.00000879987,0.99186337,0.0000069588737,0.0000151223685,0.000031905365,0.00018071622,0.005857038,0.0014522494,0.000090810216,0.00048408404,0.0000052914224],"about_ca_topic_score_codex":0.061262462,"about_ca_topic_score_gemma":0.14349538,"teacher_disagreement_score":0.061262462,"about_ca_system_score_codex":0.0011210019,"about_ca_system_score_gemma":0.00046909542,"threshold_uncertainty_score":0.12181175},"labels":[],"label_agreement":null},{"id":"W2285322365","doi":"10.1002/2015gl067514","title":"Linking fossil reefs with earthquakes: Geologic insight to where induced seismicity occurs in Alberta","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Induced seismicity; Reef; Tectonics; Precambrian; Basement; Sedimentary basin; Sedimentary rock; Seismology; Devonian; Structural basin; Paleontology; Earth science; Oceanography","score_opus":0.04390893715569616,"score_gpt":0.27873332066356615,"score_spread":0.23482438350787,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2285322365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980926,0.00006588205,0.00007113643,0.00004541006,8.835603e-7,0.0000032621147,0.00036072163,0.000004690551,0.0013554194],"genre_scores_gemma":[0.9990251,0.00009577148,0.00009633447,0.0000061681435,8.1981926e-7,0.000001280909,0.00025398453,0.0000012160085,0.00051924976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998728,0.000014478931,0.000007584829,0.000020992395,0.000039168903,0.00004482441],"domain_scores_gemma":[0.9994648,0.00006676512,0.0001136298,0.000029323095,0.00021937065,0.00010607211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019555048,0.000108356006,0.00008535188,0.0013112556,0.00057279,0.00063957414,0.0004074261,0.00015835754,0.0015560508],"category_scores_gemma":[0.0009076046,0.000100858924,0.00007547753,0.0022122955,0.0004333697,0.00013073377,0.0004955565,0.00016127339,0.00010661669],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050387578,0.000019413143,0.99008876,0.000013411076,0.000015896338,0.00017935678,0.00065063155,0.0006879977,0.0014397636,0.00019067373,0.00021155574,0.0064521506],"study_design_scores_gemma":[8.911567e-7,0.000003422531,0.99860543,0.000003285044,0.0000031738905,0.000021242844,0.00074598566,0.00027862162,0.00007349138,0.000028881976,0.00023384843,0.0000017371361],"about_ca_topic_score_codex":0.92153484,"about_ca_topic_score_gemma":0.9786357,"teacher_disagreement_score":0.07846516,"about_ca_system_score_codex":0.0047546923,"about_ca_system_score_gemma":0.0039865393,"threshold_uncertainty_score":0.1578545},"labels":[],"label_agreement":null},{"id":"W2293879242","doi":"10.1002/2016gl067759","title":"Ice mass loss in Greenland, the Gulf of Alaska, and the Canadian Archipelago: Seasonal cycles and decadal trends","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Groenlandia; Archipelago; Glacier; Greenland ice sheet; Iceberg; Geology; Oceanography; Climatology; Arctic ice pack; Sea ice; Future sea level; Ice core; Cryosphere; Ice sheet; Physical geography; Antarctic sea ice; Geography; Geomorphology","score_opus":0.029579075732313012,"score_gpt":0.26286780278670524,"score_spread":0.23328872705439224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2293879242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897026,0.001406581,0.00012266205,0.00020841871,0.000017345095,0.000006539777,0.006486128,0.00002285423,0.0020269004],"genre_scores_gemma":[0.99471974,0.00058373914,0.00013444955,0.000049806393,0.000009502816,0.0000046059977,0.0036240623,0.0000055912565,0.0008684293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986506,0.0000060142715,0.000010171957,0.000030968935,0.00005108734,0.000036714002],"domain_scores_gemma":[0.9990978,0.00004549283,0.00020750269,0.000029606308,0.00050464214,0.00011499784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034170854,0.00024281554,0.00017788434,0.0022903983,0.00044923255,0.00067549606,0.00028499495,0.00019006451,0.00077172363],"category_scores_gemma":[0.0007019152,0.000073780146,0.00021468436,0.0029041434,0.00033939982,0.00041057877,0.00038147715,0.00024610164,0.00012619064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042044212,0.000011814277,0.99144626,0.00001832496,0.000088125045,0.0000247953,0.00015143894,0.0005193553,0.00037080594,0.000057438203,0.0009568753,0.0063127372],"study_design_scores_gemma":[5.191315e-7,0.0000025827635,0.9986172,0.0000065267154,0.000008788411,0.000010462556,0.0001585567,0.00033042431,0.000065905544,0.000011330806,0.0007849612,0.0000027275646],"about_ca_topic_score_codex":0.8477951,"about_ca_topic_score_gemma":0.92304295,"teacher_disagreement_score":0.15220487,"about_ca_system_score_codex":0.0037507603,"about_ca_system_score_gemma":0.0026082105,"threshold_uncertainty_score":0.3062024},"labels":[],"label_agreement":null},{"id":"W2295085913","doi":"10.1002/2015gl066712","title":"Albedo feedback enhanced by smoother Arctic sea ice","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; ArcticNet","keywords":"Sea ice; Melt pond; Arctic ice pack; Sea ice thickness; Ice-albedo feedback; Albedo (alchemy); Climatology; Environmental science; Arctic; Advanced very-high-resolution radiometer; Sea ice concentration; Antarctic sea ice; Geology; Arctic sea ice decline; Cryosphere; Drift ice; Atmospheric sciences; Oceanography; Satellite","score_opus":0.02964064845356034,"score_gpt":0.27671846419718965,"score_spread":0.2470778157436293,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2295085913","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99503726,0.00008915007,0.002303141,0.0001595944,0.00003842251,0.00000564431,0.00044613928,0.0002701847,0.0016504204],"genre_scores_gemma":[0.9995171,0.000017863103,0.00023196905,0.000014461555,0.000010658198,0.0000011674897,0.00009364053,0.000016690674,0.00009651354],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989045,0.000020605761,0.0000051204456,0.00004028257,0.000020012018,0.00002355005],"domain_scores_gemma":[0.9997813,0.00006759795,0.00004187213,0.000027768956,0.000051729643,0.000029819712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021044878,0.00039520845,0.00029840847,0.0004392283,0.00023054605,0.0005060196,0.00016672176,0.0003254467,0.0011797121],"category_scores_gemma":[0.0007769183,0.00027059653,0.0003873631,0.00026591014,0.00023103038,0.00038305746,0.00034070777,0.00032446865,0.00018395463],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006891959,0.00021810926,0.5287576,0.00012954565,0.0003307187,0.0008102393,0.00033779585,0.1243659,0.30233732,0.0010731671,0.0029366312,0.038013853],"study_design_scores_gemma":[0.000033214863,0.000039265426,0.81272936,0.000009875832,0.000056048717,0.00007446054,0.000100193785,0.17844199,0.0070191654,0.00047252406,0.000987557,0.00003638842],"about_ca_topic_score_codex":0.012012867,"about_ca_topic_score_gemma":0.0112006795,"teacher_disagreement_score":0.012012867,"about_ca_system_score_codex":0.00046581856,"about_ca_system_score_gemma":0.00021055316,"threshold_uncertainty_score":0.023885906},"labels":[],"label_agreement":null},{"id":"W2296285750","doi":"10.1002/2016gl067853","title":"Formation of energetic electron butterfly distributions by magnetosonic waves via Landau resonance","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":99,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National Natural Science Foundation of China; National Aeronautics and Space Administration; National Science Foundation","keywords":"Van Allen radiation belt; Physics; Pitch angle; Magnetosphere; Magnetopause; Electron; Van Allen Probes; Geophysics; Geomagnetic storm; Computational physics; Plasmasphere; Test particle; Earth's magnetic field; Classical mechanics; Plasma; Magnetic field; Nuclear physics","score_opus":0.0076921322585812016,"score_gpt":0.2561628419078764,"score_spread":0.2484707096492952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2296285750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98964244,0.000036580117,0.0067799482,0.000081818565,0.0000089910645,0.000010391365,0.000017385788,0.000097614815,0.0033248658],"genre_scores_gemma":[0.9993272,0.000011021132,0.00039617266,0.000006636108,0.000001981141,0.0000032687517,0.000006541317,0.000007302943,0.00023992597],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999966,0.000006615314,9.1626816e-7,0.000004785493,0.0000067406763,0.00001476754],"domain_scores_gemma":[0.99989593,0.000031913936,0.00002315283,0.000015308473,0.000009986173,0.00002371674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101606194,0.00021553782,0.0001867085,0.00022314578,0.00036594062,0.00044243544,0.0002789515,0.0002600984,0.0012991899],"category_scores_gemma":[0.00028032082,0.00019376204,0.00022281264,0.000104926985,0.0006021791,0.0003564211,0.00029619224,0.00017209207,0.00010092637],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00089809473,0.00028111067,0.043687176,0.00012061168,0.00019650775,0.0023921311,0.0013019305,0.5239221,0.33395398,0.07726197,0.0023852966,0.013599107],"study_design_scores_gemma":[0.00008423637,0.0000654445,0.0081474865,0.000003988354,0.000013824173,0.0000754173,0.00010422587,0.97549903,0.009246836,0.006301631,0.00043825732,0.000019621933],"about_ca_topic_score_codex":0.0020059824,"about_ca_topic_score_gemma":0.0011407948,"teacher_disagreement_score":0.0020059824,"about_ca_system_score_codex":0.00043143547,"about_ca_system_score_gemma":0.0001522804,"threshold_uncertainty_score":0.0043462515},"labels":[],"label_agreement":null},{"id":"W2297136396","doi":"10.1002/2015gl066917","title":"Source analysis of a potential hydraulic‐fracturing‐induced earthquake near Fox Creek, Alberta","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Hypocenter; Geology; Seismology; Hydraulic fracturing; Seismic moment; Focal mechanism; Fault plane; Aftershock; Moment magnitude scale; Magnitude (astronomy); Fault (geology); Oil shale; Induced seismicity; Geotechnical engineering; Paleontology","score_opus":0.04808137418258863,"score_gpt":0.2906286624480128,"score_spread":0.24254728826542415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2297136396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913557,0.000051833136,0.0015092305,0.000084071165,0.000011820647,0.000020827656,0.0028867195,0.00013462557,0.0039453055],"genre_scores_gemma":[0.99427044,0.00004374966,0.001151373,0.0000099519175,0.0000045587713,0.000004847116,0.0024065874,0.000013498965,0.002095011],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.0000013807205,0.000001415144,0.0000068190357,0.000022928349,0.000013565761],"domain_scores_gemma":[0.99988747,0.000009587532,0.000008685742,0.0000041499147,0.00007497313,0.000015048534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006295028,0.0002178857,0.00013295798,0.0007360487,0.00052543706,0.00041994522,0.00047396836,0.00017959303,0.0021189253],"category_scores_gemma":[0.00024223838,0.00009903971,0.000111221234,0.0010861601,0.00012832179,0.00009461317,0.00023518717,0.00014479527,0.00022641169],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063557224,0.00026574038,0.67184424,0.00017223551,0.00016200905,0.0044030286,0.0012456921,0.08044868,0.07520967,0.0030079698,0.013437831,0.14916734],"study_design_scores_gemma":[0.000064491614,0.000039785442,0.8699643,0.000021139544,0.00006409418,0.00021955428,0.0014333472,0.11638175,0.0055560186,0.0004595334,0.0057557467,0.000040206192],"about_ca_topic_score_codex":0.8240661,"about_ca_topic_score_gemma":0.86126655,"teacher_disagreement_score":0.1759339,"about_ca_system_score_codex":0.0019320438,"about_ca_system_score_gemma":0.0027906122,"threshold_uncertainty_score":0.35393995},"labels":[],"label_agreement":null},{"id":"W2298700813","doi":"10.1002/2016gl068015","title":"Subsidence along the Atlantic Coast of North America: Insights from GPS and late Holocene relative sea level data","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Institute of Food and Agriculture; University of Toronto; Rhode Island Agricultural Experiment Station; U.S. Geological Survey; South Carolina Department of Natural Resources; U.S. Department of Agriculture; National Aeronautics and Space Administration; National Science Foundation","keywords":"Holocene; Geology; Tide gauge; Sea level; Subsidence; Post-glacial rebound; Oceanography; Climatology; Physical geography; Geomorphology; Geography","score_opus":0.11132848056697962,"score_gpt":0.28837603241738846,"score_spread":0.17704755185040882,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2298700813","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997142,0.00018678802,0.00006535182,0.00010852969,0.0000045462853,0.0000031205927,0.000922183,0.0000050855024,0.0015624176],"genre_scores_gemma":[0.9971629,0.0003062422,0.00023812575,0.00003360589,0.0000068546765,0.0000052259593,0.0017949502,0.000003779383,0.00044822003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991894,0.000018831974,0.000008197257,0.000016756581,0.000021110269,0.000016175496],"domain_scores_gemma":[0.9994754,0.000102370796,0.00013879343,0.000034791203,0.00017948345,0.000069251175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020285463,0.0000934723,0.00010938043,0.0009658654,0.00027266235,0.00047275642,0.00015461042,0.00014611216,0.0007617525],"category_scores_gemma":[0.0007977282,0.00008678486,0.000100249956,0.0020529649,0.00017604344,0.00029670776,0.00026163497,0.00013303026,0.00014276554],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00001085419,0.000010445733,0.99142295,0.000010082784,0.0000142511235,0.000063279185,0.00052232476,0.00011220821,0.0004925757,0.000032877124,0.0003173966,0.0069908146],"study_design_scores_gemma":[5.341173e-7,0.00000451949,0.998911,0.0000049296477,0.0000032415273,0.000016047437,0.00036534457,0.00011088826,0.00001696291,0.00001016545,0.0005553592,9.573195e-7],"about_ca_topic_score_codex":0.15598947,"about_ca_topic_score_gemma":0.4591089,"teacher_disagreement_score":0.84401053,"about_ca_system_score_codex":0.0004622525,"about_ca_system_score_gemma":0.00046899996,"threshold_uncertainty_score":0.31016302},"labels":[],"label_agreement":null},{"id":"W2300624505","doi":"10.1002/2015gl066664","title":"On determining the zenith angle dependence of the Martian radiation environment at Gale Crater altitudes","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lockheed Martin (Canada)","funders":"Human Exploration and Operations Mission Directorate; Southwest Research Institute; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Martian; Impact crater; Zenith; Astrobiology; Martian surface; Regolith; Geology; Tilt (camera); Exploration of Mars; Radiation; Atmosphere of Mars; Environmental science; Remote sensing; Physics; Optics; Geometry","score_opus":0.04651534061745898,"score_gpt":0.2805856585566615,"score_spread":0.23407031793920252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2300624505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949297,0.00016469481,0.0005846435,0.000017623239,0.000002568744,0.000004396483,0.000496919,0.000023943523,0.003775565],"genre_scores_gemma":[0.99926764,0.00005073661,0.00027027298,0.000010578275,0.0000020257032,0.0000017677413,0.00025452682,0.000010941003,0.00013146125],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990606,0.00001744305,0.0000029866678,0.000026173308,0.000024151037,0.000023095003],"domain_scores_gemma":[0.99961793,0.00015445203,0.000050226463,0.000042101998,0.00008935666,0.000045889956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013943823,0.00020238882,0.00013088644,0.0007015988,0.00022013235,0.00034498126,0.0001577055,0.00011927605,0.0017282566],"category_scores_gemma":[0.00055713084,0.000116358664,0.00013592678,0.0005102973,0.00025435252,0.00021119071,0.00032955522,0.0002336724,0.00035206048],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052942353,0.00003314078,0.86476207,0.00007591377,0.000105475774,0.00019488993,0.00043853157,0.0046675215,0.111288376,0.00041692494,0.0004082161,0.017079452],"study_design_scores_gemma":[0.0000050631365,0.000038884053,0.99066544,0.000004576645,0.000009204531,0.000056868506,0.000079978396,0.00093005254,0.007416528,0.000040989806,0.0007436454,0.000008846661],"about_ca_topic_score_codex":0.008139998,"about_ca_topic_score_gemma":0.0127610145,"teacher_disagreement_score":0.008139998,"about_ca_system_score_codex":0.0001928651,"about_ca_system_score_gemma":0.00012886782,"threshold_uncertainty_score":0.016185224},"labels":[],"label_agreement":null},{"id":"W2301748736","doi":"10.1002/2015gl066446","title":"Terrane‐controlled crustal shear wave splitting in Taiwan","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Terrane; Geology; Shear wave splitting; Lithosphere; Metamorphic rock; Seismology; Shear (geology); Tectonics; Shear zone; Plate tectonics; Crust; Continental collision; Petrology; Geophysics","score_opus":0.08361527928235694,"score_gpt":0.305338154665588,"score_spread":0.22172287538323104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301748736","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997689,0.000012517727,0.000025414321,0.0000031030888,1.5421931e-7,6.187697e-7,0.00004052515,0.0000018583596,0.00014700709],"genre_scores_gemma":[0.99978083,0.000012538462,0.000023205515,0.0000013591751,3.002126e-7,9.931939e-7,0.00011677834,9.391379e-7,0.0000629126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.0000040986506,0.0000030310277,0.000013409256,0.0000067666247,0.000011715866],"domain_scores_gemma":[0.9998996,0.00001126899,0.000031530904,0.000009194613,0.000023629324,0.000024673078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000080836566,0.000113729344,0.0001211017,0.0005524539,0.00017492472,0.00031399252,0.00011654789,0.00010485517,0.00067602517],"category_scores_gemma":[0.00019891477,0.00011184127,0.00009274426,0.0005287991,0.0001475506,0.00013744754,0.0002675282,0.00010141222,0.000091151844],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033464067,0.00006372475,0.6817098,0.000038341015,0.00007749272,0.00067409757,0.00075228815,0.0028779646,0.30159926,0.00020834508,0.00021367756,0.01145033],"study_design_scores_gemma":[0.000008677298,0.00003663844,0.9941902,0.0000022604095,0.000012908377,0.00011253601,0.00023199155,0.0019285094,0.003235185,0.000053655243,0.00018147008,0.000006079173],"about_ca_topic_score_codex":0.012433436,"about_ca_topic_score_gemma":0.012321851,"teacher_disagreement_score":0.012433436,"about_ca_system_score_codex":0.0002516703,"about_ca_system_score_gemma":0.0001610753,"threshold_uncertainty_score":0.024722159},"labels":[],"label_agreement":null},{"id":"W2301858794","doi":"10.1002/2015gl066903","title":"The impact of equilibrating hemispheric albedos on tropical performance in the HadGEM2‐ES coupled climate model","year":2015,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Pacific Northwest National Laboratory; Sight Research UK; Department for International Development, UK Government; Department for Environment, Food and Rural Affairs, UK Government; Battelle; Fund for Innovative Climate and Energy Research; Natural Environment Research Council; Met Office; U.S. Department of Energy","keywords":"Hadley cell; Climatology; Northern Hemisphere; Climate model; Environmental science; Precipitation; Monsoon; Atmospheric sciences; Southern Hemisphere; Climate change; General Circulation Model; Geology; Geography; Meteorology","score_opus":0.07104244303191593,"score_gpt":0.3454224755184933,"score_spread":0.2743800324865774,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2301858794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98654985,0.00027065654,0.006432943,0.0006940969,0.00007996884,0.000026281245,0.00080653024,0.00028115147,0.004858515],"genre_scores_gemma":[0.9987406,0.000037670055,0.0008334187,0.00006528522,0.0000061224096,0.000006361868,0.0001499822,0.000027483416,0.00013311149],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99935585,0.00034814407,0.000033027805,0.00010682125,0.000053766245,0.000102434045],"domain_scores_gemma":[0.99869907,0.00060228334,0.00015587299,0.0002620288,0.00014063834,0.00014018384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002095837,0.0006881235,0.00040881365,0.00024066053,0.00056862383,0.0015275555,0.00081539474,0.0009006864,0.0013232556],"category_scores_gemma":[0.0053089783,0.00029065952,0.00057894556,0.00045215766,0.0007508261,0.0009218441,0.0009254867,0.0008555048,0.00020281806],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044421307,0.00005991043,0.040541712,0.00004424783,0.00026677884,0.0001023896,0.000057745772,0.9453268,0.005613064,0.0015279871,0.00073784305,0.0052772895],"study_design_scores_gemma":[0.00041212438,0.00030506193,0.038818534,0.000033188157,0.00024888248,0.000050336253,0.00014024455,0.9458378,0.010334714,0.001667567,0.0020561276,0.0000953817],"about_ca_topic_score_codex":0.034818195,"about_ca_topic_score_gemma":0.016408673,"teacher_disagreement_score":0.034818195,"about_ca_system_score_codex":0.0009166001,"about_ca_system_score_gemma":0.00070571795,"threshold_uncertainty_score":0.06923109},"labels":[],"label_agreement":null},{"id":"W2302777734","doi":"10.1002/2015gl067536","title":"Longitudinal frequency variation of long‐lasting EMIC Pc1‐Pc2 waves localized in the inner magnetosphere","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Athabasca University; University of Alberta","funders":"Canadian Space Agency; National Oceanic and Atmospheric Administration; Korea Polar Research Institute","keywords":"Plasmasphere; Physics; Magnetosphere; Geophysics; Magnetometer; Local time; Cyclotron; Ionosphere; Van Allen radiation belt; Computational physics; Geodesy; Atmospheric sciences; Magnetic field; Geology","score_opus":0.020154807718370717,"score_gpt":0.28313086674146587,"score_spread":0.2629760590230952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2302777734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988464,0.00001570154,0.000177296,0.000010728157,0.0000013124427,0.0000019887248,0.00013341714,0.000011365272,0.0008018668],"genre_scores_gemma":[0.99950457,0.000009114362,0.00008379524,0.0000031336745,0.0000024047188,0.0000020724476,0.00017471676,0.0000017428406,0.00021845532],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997175,0.0000028055995,9.90982e-7,0.0000075713056,0.000007775455,0.000009196855],"domain_scores_gemma":[0.99980766,0.000030583502,0.000056454493,0.000012315792,0.000057534475,0.000035352787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000808991,0.00011309626,0.000059129776,0.00047351702,0.00014474225,0.00015641653,0.00010674903,0.00011964774,0.0007985146],"category_scores_gemma":[0.00027298465,0.000064786276,0.00005029539,0.0002541811,0.00011356744,0.00010560908,0.00015756827,0.00013029682,0.00012298778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035234322,0.0000560686,0.8097538,0.000027874492,0.000049570106,0.00035478003,0.00043295725,0.0016710417,0.16779378,0.00020446783,0.0008575416,0.018445767],"study_design_scores_gemma":[0.0000028274524,0.000024740264,0.99543387,0.0000015593826,0.0000053169315,0.000039847644,0.000050102837,0.0010444728,0.0030922664,0.000010688395,0.0002915709,0.0000028483812],"about_ca_topic_score_codex":0.0063751256,"about_ca_topic_score_gemma":0.0072317743,"teacher_disagreement_score":0.0063751256,"about_ca_system_score_codex":0.00023058672,"about_ca_system_score_gemma":0.00006922593,"threshold_uncertainty_score":0.01267606},"labels":[],"label_agreement":null},{"id":"W2313428280","doi":"10.1002/2015gl067038","title":"On the influence of cold‐water coral mound size on flow hydrodynamics, and vice versa","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Isopycnal; Geology; Mixing (physics); Oceanography; Turbulence; Flow (mathematics); Environmental science; Hydrology (agriculture); Mechanics; Physics; Geotechnical engineering","score_opus":0.013319280463842786,"score_gpt":0.24663779753999912,"score_spread":0.23331851707615633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2313428280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985481,0.000038280938,0.0007222187,0.00004213506,0.0000048084953,0.0000024461729,0.000049082024,0.000021008475,0.0005718374],"genre_scores_gemma":[0.99980265,0.000020020814,0.00010808803,0.000004507535,0.0000016855688,0.0000011723873,0.000015730742,0.0000043398422,0.0000418745],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.00001819537,0.0000029256985,0.000012482271,0.00000863063,0.0000116938245],"domain_scores_gemma":[0.9989819,0.0007058091,0.00011734633,0.000059893162,0.000054880446,0.0000801352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030366657,0.00018363673,0.0001690082,0.00016581113,0.00012844444,0.0003583234,0.00018379334,0.00018913149,0.000948874],"category_scores_gemma":[0.0014245211,0.00016624345,0.00023873034,0.00009183429,0.0003257646,0.00019140996,0.00020596597,0.00016308468,0.0000636386],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009326378,0.00022879333,0.278668,0.00019522013,0.00019831293,0.00064168026,0.00017448585,0.46116844,0.23990612,0.0016362129,0.0006985774,0.01555155],"study_design_scores_gemma":[0.000067612214,0.00017967682,0.3988163,0.000010931087,0.00008170209,0.000093265524,0.00009942836,0.58331704,0.016640926,0.00031362235,0.00033782257,0.000041628027],"about_ca_topic_score_codex":0.007579953,"about_ca_topic_score_gemma":0.004311092,"teacher_disagreement_score":0.007579953,"about_ca_system_score_codex":0.0002521045,"about_ca_system_score_gemma":0.0002732445,"threshold_uncertainty_score":0.01507169},"labels":[],"label_agreement":null},{"id":"W2317515852","doi":"10.1002/2016gl068240","title":"The dry season intensity as a key driver of NPP trends","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Consejo Nacional de Ciencia y Tecnología; University of Exeter; Consejo Estatal de Ciencia, Tecnología e Innovación; European Commission; Australian Research Council; Sight Research UK","keywords":"Environmental science; Dry season; Primary production; Biomass (ecology); Growing season; Vegetation (pathology); Precipitation; Ecosystem; Productivity; Wet season; Carbon cycle; Climate change; Atmospheric sciences; Hydrology (agriculture); Agronomy; Ecology; Geography; Meteorology; Biology","score_opus":0.015081432186648272,"score_gpt":0.2639212231433867,"score_spread":0.24883979095673842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2317515852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99820995,0.00010961715,0.0004005581,0.000038921018,0.00000324683,0.000002749621,0.00036642744,0.0000099616655,0.0008586568],"genre_scores_gemma":[0.9994254,0.00003669712,0.000081122154,0.0000108536815,0.000007842951,0.0000021997412,0.0002673198,0.000005762775,0.0001627235],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993813,0.000009751991,0.000004930125,0.000020111218,0.0000113611795,0.000015769527],"domain_scores_gemma":[0.99957865,0.00012955333,0.00013920813,0.000027962564,0.000056367062,0.00006831045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024243962,0.00011954659,0.00018905361,0.00040906217,0.0001491331,0.0005304167,0.00014122459,0.0001262336,0.0019455964],"category_scores_gemma":[0.00060653425,0.00006823026,0.00021756745,0.00046547767,0.00021329045,0.0003835109,0.00025404544,0.00020646637,0.00023004564],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001346569,0.000032714666,0.96774006,0.000037604397,0.00010983386,0.00010463623,0.0000919929,0.001756752,0.02188782,0.00021059072,0.00026721327,0.0076262434],"study_design_scores_gemma":[0.0000018201375,0.00001421626,0.9969121,0.0000017920044,0.000016084294,0.00002559039,0.00005329687,0.0018737245,0.00058091024,0.000096758464,0.00042091773,0.0000027780927],"about_ca_topic_score_codex":0.0034191422,"about_ca_topic_score_gemma":0.003258921,"teacher_disagreement_score":0.0034191422,"about_ca_system_score_codex":0.00013747584,"about_ca_system_score_gemma":0.00013840274,"threshold_uncertainty_score":0.006798446},"labels":[],"label_agreement":null},{"id":"W2323524345","doi":"10.1002/2016gl068339","title":"Near‐surface salinity and stratification in the north Bay of Bengal from moored observations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bangladesh University of Engineering and Technology; National Oceanic and Atmospheric Administration; Agence Nationale de la Recherche; Indian National Centre for Ocean Information Services; University of Engineering and Technology, Lahore","keywords":"Salinity; Bay; Oceanography; Mooring; Stratification (seeds); Geology; Eddy; Monsoon; Temperature salinity diagrams; BENGAL; Mixed layer; Environmental science; Surface runoff; Climatology; Turbulence; Meteorology; Geography","score_opus":0.054133302387801986,"score_gpt":0.27236512991897793,"score_spread":0.21823182753117595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2323524345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99861836,0.000038127902,0.00008899937,0.000034967048,0.000004097041,0.0000031736229,0.00065053033,0.00001439472,0.00054741866],"genre_scores_gemma":[0.999161,0.00003158677,0.000096884105,0.0000069937537,0.000004453367,0.0000027980257,0.0005483681,0.0000020014102,0.00014603026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999013,0.000012110561,0.000008461173,0.000025938267,0.000026394671,0.00002578228],"domain_scores_gemma":[0.99976605,0.000021027841,0.0000811385,0.000030041094,0.0000512239,0.000050501796],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010942267,0.00021965454,0.00016184892,0.0006353114,0.00027190693,0.0005501277,0.00028735775,0.00016499888,0.0008017523],"category_scores_gemma":[0.0004860471,0.0001320022,0.0002067187,0.0009529109,0.00019641998,0.00032323613,0.0005066577,0.00014811488,0.00025821806],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012252905,0.000038529524,0.96957505,0.000039540995,0.00008880966,0.00034877093,0.00066700304,0.0013789844,0.0144832,0.00006752927,0.00047087442,0.01271919],"study_design_scores_gemma":[0.0000041110115,0.00001048267,0.9966248,0.0000049840305,0.00001417456,0.000036052897,0.00033553262,0.0016649989,0.0007638541,0.000014373877,0.0005192986,0.000007343055],"about_ca_topic_score_codex":0.13655321,"about_ca_topic_score_gemma":0.1559634,"teacher_disagreement_score":0.13655321,"about_ca_system_score_codex":0.00084556034,"about_ca_system_score_gemma":0.00040294457,"threshold_uncertainty_score":0.2715168},"labels":[],"label_agreement":null},{"id":"W2336422795","doi":"10.1002/2015gl067353","title":"Nitrous oxide in the atmosphere: First measurements of a lower thermospheric source","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Toronto","funders":"Canadian Space Agency","keywords":"Thermosphere; Stratosphere; Atmosphere (unit); Atmospheric sciences; Troposphere; Nitrous oxide; Atmospheric chemistry; Environmental science; Mixing ratio; Ozone; Middle latitudes; Atmosphere of Earth; Ozone layer; Mesosphere; Precipitation; Ionosphere; Meteorology; Geology; Physics; Chemistry; Geophysics","score_opus":0.0412881143515145,"score_gpt":0.2666493257337664,"score_spread":0.22536121138225187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2336422795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99305445,0.00082670746,0.0010020706,0.00008607718,0.000021098791,0.000024130206,0.0013523432,0.00009180677,0.0035413879],"genre_scores_gemma":[0.99620616,0.00027197108,0.0015085639,0.00005512054,0.000031255782,0.000017797838,0.0013917251,0.000016749333,0.0005007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999897,0.000006109807,0.0000035368712,0.000034676465,0.000039550512,0.000019055702],"domain_scores_gemma":[0.9998542,0.000017552962,0.000017640883,0.000012738804,0.0000677479,0.000030161966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017172293,0.00049681315,0.00024478298,0.00055322587,0.000598648,0.0005061354,0.00025634715,0.0005746402,0.0006781937],"category_scores_gemma":[0.00017605133,0.00026879145,0.00016525063,0.00052175863,0.00026393496,0.0003695523,0.00046810802,0.0005003354,0.00033228385],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081540865,0.00034157795,0.5127535,0.00013314455,0.00011840214,0.00039454206,0.0007047674,0.0008991721,0.44907206,0.0003595853,0.0010904528,0.03331739],"study_design_scores_gemma":[0.00003148853,0.00019748541,0.95397234,0.000022312764,0.00005722957,0.00011769361,0.00010115487,0.0021157875,0.037521236,0.00013722442,0.0057109925,0.000015133208],"about_ca_topic_score_codex":0.023265965,"about_ca_topic_score_gemma":0.02496094,"teacher_disagreement_score":0.023265965,"about_ca_system_score_codex":0.0005047096,"about_ca_system_score_gemma":0.00037874386,"threshold_uncertainty_score":0.046261072},"labels":[],"label_agreement":null},{"id":"W2339250340","doi":"10.1002/2016gl068368","title":"Tsunami data assimilation of Cascadia seafloor pressure gauge records from the 2012 Haida Gwaii earthquake","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Seafloor spreading; Geology; Tsunami earthquake; Seismology; Submarine pipeline; Tide gauge; Data assimilation; Tsunami wave; Oceanography; Meteorology; Sea level; Geography","score_opus":0.06899769150526015,"score_gpt":0.29984606076648074,"score_spread":0.2308483692612206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339250340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974132,0.0000130103,0.00074617023,0.00005779855,0.000019797362,0.0000132011755,0.00063792284,0.00013667934,0.0009621757],"genre_scores_gemma":[0.9980611,0.000013051033,0.00074088183,0.000008054745,0.0000043181594,0.000008441977,0.000893995,0.000008396668,0.00026170418],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998814,0.00001485733,0.000008177647,0.000033707987,0.000035015946,0.00002675827],"domain_scores_gemma":[0.9995115,0.000081123726,0.000049680537,0.00009034759,0.00019881655,0.00006844893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030202427,0.0006187659,0.0003291342,0.0003248125,0.000498968,0.0006247072,0.0006747391,0.00050739397,0.0010832383],"category_scores_gemma":[0.0013520187,0.00039159524,0.00048365537,0.00050779746,0.00043211482,0.0003611245,0.00033820004,0.00060986995,0.00018800651],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039553773,0.0002231682,0.08904458,0.000033148157,0.00016271917,0.00018591656,0.00015404707,0.88860226,0.005877078,0.00030033698,0.0013792022,0.013642057],"study_design_scores_gemma":[0.00014254717,0.000107518295,0.104493946,0.000008711429,0.000051296825,0.000024863642,0.00011947177,0.8910913,0.0031577933,0.00014101212,0.00061971956,0.000041711537],"about_ca_topic_score_codex":0.4283666,"about_ca_topic_score_gemma":0.40886125,"teacher_disagreement_score":0.5716334,"about_ca_system_score_codex":0.0015989192,"about_ca_system_score_gemma":0.0019295748,"threshold_uncertainty_score":0.85174644},"labels":[],"label_agreement":null},{"id":"W2339668439","doi":"10.1002/2016gl068688","title":"Linear analysis of melt band formation in a mid‐ocean ridge corner flow","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Asthenosphere; Streamlines, streaklines, and pathlines; Anisotropy; Porosity; Isotropy; Mineralogy; Lithosphere; Geophysics; Mechanics; Geotechnical engineering; Optics; Seismology","score_opus":0.03125748140665406,"score_gpt":0.2821310240945426,"score_spread":0.25087354268788853,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2339668439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927562,0.000019125044,0.006105414,0.000028446082,0.0000022573427,0.000008523918,0.000057387526,0.00007144384,0.00095111586],"genre_scores_gemma":[0.9988945,0.0000072039484,0.000826855,0.0000036922504,0.0000017618783,0.000004670501,0.000034808905,0.000007808209,0.00021879346],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999261,0.000014781575,0.0000047481885,0.000012985563,0.000016941083,0.000024423514],"domain_scores_gemma":[0.9996581,0.00012619661,0.00009718816,0.000021132939,0.00006586699,0.00003141444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016678916,0.00021638122,0.00017482867,0.0004626102,0.00023504616,0.00052069617,0.00022037384,0.0002741555,0.0013035075],"category_scores_gemma":[0.000772536,0.00015275348,0.00039821005,0.0001541601,0.0003612367,0.00018001598,0.0003167581,0.0002907396,0.00010627584],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010598939,0.00030576397,0.112771876,0.00015438648,0.00018406342,0.00062209624,0.0004396722,0.53588873,0.3133548,0.008779321,0.0006279835,0.02581137],"study_design_scores_gemma":[0.000014159965,0.0000618171,0.013416229,0.0000038931516,0.000010936349,0.000017318454,0.000041016847,0.9769931,0.009058857,0.00028895462,0.00008393731,0.000009902818],"about_ca_topic_score_codex":0.0049356055,"about_ca_topic_score_gemma":0.002492122,"teacher_disagreement_score":0.0049356055,"about_ca_system_score_codex":0.00042204192,"about_ca_system_score_gemma":0.0003563542,"threshold_uncertainty_score":0.009813726},"labels":[],"label_agreement":null},{"id":"W2341356865","doi":"10.1002/2016gl068648","title":"Separating climate‐induced mass transfers and instrumental effects from tectonic signal in repeated absolute gravity measurements","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Institut Universitaire de France; Centre National d’Etudes Spatiales","keywords":"Tectonics; Geology; Geodesy; Satellite; Seismology; Climatology; Physics","score_opus":0.057235602278118886,"score_gpt":0.287369363960157,"score_spread":0.2301337616820381,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341356865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778783,0.000052447947,0.0012459,0.000020472697,0.000005500921,0.0000048194925,0.00026058214,0.000037911752,0.00058467215],"genre_scores_gemma":[0.99928975,0.000010929878,0.00032731058,0.0000056348267,0.000006480811,0.0000030891795,0.0002631477,0.000006743265,0.00008684512],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999509,0.0001153607,0.000031009615,0.00010112019,0.00014439464,0.000099152625],"domain_scores_gemma":[0.99835855,0.0004610783,0.0006148341,0.00025160052,0.00024384355,0.00007004033],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00091133505,0.00034076168,0.00021011697,0.0010804443,0.0002517248,0.0004838945,0.0005239659,0.00035664884,0.000804471],"category_scores_gemma":[0.0039188103,0.00015755762,0.00023654096,0.0016563975,0.00040703305,0.0004478255,0.0004450718,0.00024559698,0.00015670613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018567691,0.000046533183,0.9632261,0.000033165154,0.00016252801,0.00017059858,0.00021662416,0.0050860317,0.017740846,0.00014666641,0.0002197394,0.01276543],"study_design_scores_gemma":[0.000004429527,0.00002549678,0.99253535,0.000003332625,0.000019187664,0.000058950627,0.00004789148,0.0044119027,0.0026709673,0.000048824597,0.0001660349,0.000007611493],"about_ca_topic_score_codex":0.014147046,"about_ca_topic_score_gemma":0.021581441,"teacher_disagreement_score":0.014147046,"about_ca_system_score_codex":0.0004526611,"about_ca_system_score_gemma":0.000253473,"threshold_uncertainty_score":0.028129399},"labels":[],"label_agreement":null},{"id":"W2341511228","doi":"10.1002/2016gl067931","title":"Large‐scale ocean circulation‐cloud interactions reduce the pace of transient climate change","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"McGill University","keywords":"Cloud feedback; Environmental science; Climatology; Radiative transfer; Radiative forcing; Radiative flux; Climate change; Atmospheric sciences; Global warming; Cloud forcing; Climate model; Radiative cooling; Ocean current; Climate sensitivity; Meteorology; Geology; Oceanography; Geography; Physics","score_opus":0.06436881644374322,"score_gpt":0.33243846462047866,"score_spread":0.26806964817673545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2341511228","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953141,0.00006986652,0.0017938484,0.00039039477,0.000035307123,0.00001139136,0.0001502733,0.000083357234,0.0021513426],"genre_scores_gemma":[0.9994172,0.000027873493,0.00017407232,0.000029260884,0.0000058670184,0.0000048260085,0.000041010982,0.000015216757,0.00028469978],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997631,0.00007197232,0.000011240533,0.000043869513,0.000031483243,0.00007845986],"domain_scores_gemma":[0.9991116,0.00041941667,0.00015789412,0.00008213169,0.00006308387,0.0001658114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005685534,0.0006357303,0.00053483836,0.00023185967,0.00063001073,0.0014710326,0.0006199249,0.0009439083,0.0027801753],"category_scores_gemma":[0.002314307,0.0004246631,0.00073680864,0.00026449646,0.0005926094,0.0012352101,0.0010978538,0.0007334761,0.00017921158],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040608295,0.00023380599,0.026420776,0.000052376345,0.00022249769,0.00016285824,0.000060934606,0.9505811,0.01580736,0.00268105,0.00074693677,0.002624156],"study_design_scores_gemma":[0.0001735987,0.00021022618,0.017425623,0.000006516557,0.00009424124,0.000032369764,0.00009577535,0.9764063,0.0030001316,0.0020185995,0.00051153783,0.000025084792],"about_ca_topic_score_codex":0.012259611,"about_ca_topic_score_gemma":0.008761189,"teacher_disagreement_score":0.012259611,"about_ca_system_score_codex":0.00086612714,"about_ca_system_score_gemma":0.0009641952,"threshold_uncertainty_score":0.024376512},"labels":[],"label_agreement":null},{"id":"W2342453700","doi":"10.1002/2016gl068184","title":"A new characterization of the turbulent diapycnal diffusivities of mass and momentum in the ocean","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Turbulence; Momentum (technical analysis); Mixing (physics); Turbulent Prandtl number; Thermal diffusivity; Prandtl number; Mechanics; Mass flux; Environmental science; Meteorology; Atmospheric sciences; Geology; Climatology; Physics; Thermodynamics; Reynolds number; Convection","score_opus":0.01475362583539128,"score_gpt":0.22913182840950982,"score_spread":0.21437820257411855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2342453700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93583137,0.00037070527,0.059688162,0.00015183377,0.000016945703,0.000016414819,0.00025449423,0.000057118606,0.0036129623],"genre_scores_gemma":[0.9936466,0.00010816719,0.0057887817,0.000006138898,0.000010596084,0.000008796576,0.0000868249,0.000008152815,0.00033608198],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.000007926702,0.0000049658515,0.000022048624,0.000020582604,0.0000081521885],"domain_scores_gemma":[0.9998385,0.000056611938,0.000040129864,0.000028047882,0.00002553667,0.00001120092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023470576,0.00030280853,0.00021531741,0.0007010795,0.00015286058,0.0007758582,0.00021020153,0.0001851057,0.0003102926],"category_scores_gemma":[0.0006007708,0.00014488572,0.00019037284,0.00040562925,0.0005012846,0.00084218517,0.00032555158,0.00031332535,0.000050000424],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020288632,0.0001596955,0.13428451,0.00017563389,0.000086895016,0.00022283128,0.0002818141,0.21013923,0.5370957,0.049540833,0.00042398673,0.06738598],"study_design_scores_gemma":[0.000027311582,0.00013835815,0.11669846,0.00002013505,0.00004665312,0.00021996838,0.00010989754,0.8345319,0.033974715,0.010979039,0.0031913228,0.00006219564],"about_ca_topic_score_codex":0.0019122635,"about_ca_topic_score_gemma":0.0014442819,"teacher_disagreement_score":0.0019122635,"about_ca_system_score_codex":0.00038358732,"about_ca_system_score_gemma":0.00028012658,"threshold_uncertainty_score":0.00380224},"labels":[],"label_agreement":null},{"id":"W2344204093","doi":"10.1002/2016gl068374","title":"The contribution of the GRAV‐D airborne gravity to geoid determination in the Great Lakes region","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Geoid; Geodetic datum; Geodesy; Geology; Altimeter; Satellite; Gravitational field; Remote sensing; Geophysics","score_opus":0.0402665738177702,"score_gpt":0.28445466608974074,"score_spread":0.24418809227197052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2344204093","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99149853,0.00024798088,0.0033706024,0.00042897867,0.000023534432,0.000010165624,0.0010197294,0.00028270143,0.0031177953],"genre_scores_gemma":[0.9965335,0.00008840878,0.0023635817,0.000023302464,0.000007973456,0.000003838193,0.0006518258,0.000019874367,0.0003077127],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976224,0.000078441466,0.000011555947,0.000059420254,0.000067397435,0.000020941407],"domain_scores_gemma":[0.99971086,0.00007650573,0.00003329108,0.000058853075,0.00009634445,0.000024215113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005328986,0.00030801783,0.00017925687,0.0005232221,0.00023994068,0.0008231547,0.00036730283,0.00023336048,0.00061130885],"category_scores_gemma":[0.0016466798,0.00018360416,0.00029467267,0.000858586,0.00028526515,0.00048710618,0.0007379811,0.0002138062,0.0002123969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014601514,0.000053144766,0.6752674,0.000084978885,0.0002610325,0.00017080898,0.0002944817,0.22979367,0.0049657105,0.0014912523,0.0037626424,0.083708785],"study_design_scores_gemma":[0.000049863727,0.00007041113,0.5178624,0.00004248228,0.00008872351,0.000055240194,0.00041930945,0.4730761,0.002709798,0.0010081952,0.004569489,0.000047960246],"about_ca_topic_score_codex":0.21569256,"about_ca_topic_score_gemma":0.22328271,"teacher_disagreement_score":0.21569256,"about_ca_system_score_codex":0.00087276957,"about_ca_system_score_gemma":0.00091281196,"threshold_uncertainty_score":0.4288742},"labels":[],"label_agreement":null},{"id":"W2345234563","doi":"10.1002/2016gl068513","title":"A major increase in winter snowfall during the middle Holocene on western Greenland caused by reduced sea ice in Baffin Bay and the Labrador Sea","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Holocene; Bay; Oceanography; Snow; Sea ice; Arctic; Geology; Arctic ice pack; Climatology; Cryosphere; Precipitation; Geography; Geomorphology","score_opus":0.024639869350537982,"score_gpt":0.26045347602796426,"score_spread":0.2358136066774263,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345234563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993563,0.00005478491,0.000028265551,0.000055759625,0.0000022022211,0.0000014389752,0.00015297186,0.0000073943966,0.0003409311],"genre_scores_gemma":[0.9994842,0.000029102985,0.000050729985,0.000028137161,0.0000017927478,0.0000018655427,0.00022500101,0.000002145274,0.00017706135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998878,0.000017683366,0.000005429044,0.000027729835,0.000017884035,0.00004344285],"domain_scores_gemma":[0.9998252,0.000014790814,0.000049627222,0.000010109697,0.000035375462,0.00006500192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022551737,0.00023779484,0.00021390265,0.0008952394,0.00069272384,0.00074016664,0.00035883652,0.0002922651,0.001026722],"category_scores_gemma":[0.0002973849,0.00016446545,0.0002044186,0.0007388343,0.0004837006,0.00032788864,0.0004497069,0.0001897952,0.00011880292],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016253177,0.000028507902,0.9832476,0.00002073037,0.00008611802,0.00018475878,0.00037891098,0.00035185678,0.009387448,0.00005289764,0.00035095582,0.005747639],"study_design_scores_gemma":[0.0000016616495,0.000004937731,0.999498,0.0000017645775,0.0000048657193,0.000008773978,0.00012921369,0.00012746837,0.00010200377,0.0000047504673,0.000115443734,0.0000010780929],"about_ca_topic_score_codex":0.35322738,"about_ca_topic_score_gemma":0.5983869,"teacher_disagreement_score":0.6467726,"about_ca_system_score_codex":0.0019517295,"about_ca_system_score_gemma":0.001050629,"threshold_uncertainty_score":0.70234275},"labels":[],"label_agreement":null},{"id":"W2345267547","doi":"10.1002/2016gl068064","title":"Fast and slow precipitation responses to individual climate forcers: A PDRMIP multimodel study","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":290,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Goddard Space Flight Center; National Institute for Environmental Studies; Natural Environment Research Council; Met Office; Deutsches Klimarechenzentrum; Japan Society for the Promotion of Science; Norges Forskningsråd; National Aeronautics and Space Administration; Department for Environment, Food and Rural Affairs, UK Government; National Science Foundation","keywords":"Precipitation; Environmental science; Climatology; Radiative forcing; Atmospheric sciences; Climate model; Climate change; Climate sensitivity; Forcing (mathematics); Atmosphere (unit); Meteorology; Geology; Geography","score_opus":0.06929062028111369,"score_gpt":0.3503491433377809,"score_spread":0.28105852305666723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2345267547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968394,0.000059350423,0.0012616764,0.00014418116,0.0000109050325,0.000013944277,0.0008630772,0.00010003619,0.0007074168],"genre_scores_gemma":[0.99742633,0.000041587155,0.0010087673,0.0000536652,0.000017181717,0.000029071356,0.0011312924,0.000045617355,0.00024642688],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99961936,0.00014692903,0.000018165674,0.00012391253,0.00002747126,0.000064183645],"domain_scores_gemma":[0.99845564,0.00080830173,0.00016186791,0.0002785665,0.00015006756,0.00014551429],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021225358,0.00077515864,0.0006606275,0.00054872106,0.0005309504,0.0008839273,0.0014805095,0.0010773239,0.0011651524],"category_scores_gemma":[0.00233071,0.00040388177,0.001513014,0.00068224897,0.00044834166,0.0010957333,0.00088413653,0.001022508,0.00024380822],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065765285,0.0006735395,0.30948702,0.00013782944,0.0018902803,0.00024701853,0.0002656866,0.656365,0.0068968465,0.0021014505,0.0055968524,0.015680954],"study_design_scores_gemma":[0.00014411275,0.00015943068,0.08719765,0.000011289861,0.00021705824,0.000044365024,0.00015653975,0.90851706,0.0017431135,0.0008218998,0.00092766783,0.00005971664],"about_ca_topic_score_codex":0.02428826,"about_ca_topic_score_gemma":0.011861457,"teacher_disagreement_score":0.02428826,"about_ca_system_score_codex":0.0006489971,"about_ca_system_score_gemma":0.0005490439,"threshold_uncertainty_score":0.04829377},"labels":[],"label_agreement":null},{"id":"W2346900238","doi":"10.1002/2016gl068562","title":"Inherited structure and coupled crust‐mantle lithosphere evolution: Numerical models of Central Australia","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Geology; Intraplate earthquake; Lithosphere; Crust; Tectonics; Mantle (geology); Plate tectonics; Glacial period; Context (archaeology); Geophysics; Earth science; Paleontology","score_opus":0.03677834702067186,"score_gpt":0.26620635893816963,"score_spread":0.22942801191749776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2346900238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959288,0.00007661142,0.00080093724,0.00024524538,0.000008339436,0.000011420365,0.00016765579,0.000029421855,0.002731586],"genre_scores_gemma":[0.9982481,0.00005376051,0.0005030782,0.000037159418,0.0000038519865,0.000015176868,0.00010559034,0.000013170032,0.0010201577],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988425,0.000037760983,0.000006411875,0.00002802211,0.000013958873,0.000029583249],"domain_scores_gemma":[0.9994061,0.00026600546,0.00007354301,0.00004532258,0.00009707363,0.00011199477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041050735,0.00048857357,0.0005774546,0.0006042317,0.00064486364,0.0011595207,0.0017261656,0.0017465673,0.0026244386],"category_scores_gemma":[0.0020712654,0.0006493364,0.0007837595,0.0006382862,0.0011088289,0.0007329897,0.0011379437,0.00089070015,0.00019350337],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007487757,0.000088061824,0.008953997,0.000022459866,0.00006012808,0.0001527214,0.0001101173,0.9878,0.0004666245,0.0011231599,0.00025117747,0.0008966301],"study_design_scores_gemma":[0.0000463707,0.00002272094,0.0034390835,0.000005811068,0.000016978893,0.000010001462,0.000058460006,0.9956892,0.00007609106,0.0004872295,0.00013881888,0.000009151724],"about_ca_topic_score_codex":0.20545316,"about_ca_topic_score_gemma":0.086888835,"teacher_disagreement_score":0.20545316,"about_ca_system_score_codex":0.002355371,"about_ca_system_score_gemma":0.0014554102,"threshold_uncertainty_score":0.40851456},"labels":[],"label_agreement":null},{"id":"W2363088680","doi":"10.1002/2016gl069230","title":"A comparison between large‐scale irregularities and scintillations in the polar ionosphere","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"National Key Research and Development Program of China; Natural Environment Research Council; Natural Science Foundation of Shandong Province; National Natural Science Foundation of China; National Aeronautics and Space Administration; Norges Forskningsråd; Sight Research UK; Science and Technology Facilities Council; Johns Hopkins University","keywords":"TEC; Ionosphere; Scintillation; Geomagnetic storm; Earth's magnetic field; Polar; Geology; Total electron content; Geophysics; Storm; Polar cap; Latitude; Trough (economics); Amplitude; Atmospheric sciences; Geodesy; Physics; Magnetic field; Astronomy; Optics","score_opus":0.024367358832702794,"score_gpt":0.3192748515578011,"score_spread":0.2949074927250983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2363088680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954726,0.000033102337,0.0031552827,0.0000056198965,0.0000056230756,0.000011308438,0.00023903337,0.000083252286,0.0009942196],"genre_scores_gemma":[0.99907243,0.000013831743,0.00065539597,9.977191e-7,0.0000034376087,0.000002851452,0.0001898964,0.0000071769764,0.000053926804],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990714,0.000017549439,0.000008595451,0.000023773302,0.000027103863,0.000015895626],"domain_scores_gemma":[0.99950397,0.00021878938,0.00010425219,0.000041743864,0.00008531324,0.00004590065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029419013,0.00015709871,0.00011840212,0.0016537397,0.00017236911,0.0004390334,0.00010135488,0.00011938778,0.0007635956],"category_scores_gemma":[0.0007975237,0.00008256752,0.00015184656,0.0009123451,0.00017696217,0.00026855606,0.0002730406,0.00008908798,0.000073866315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001770468,0.00015766658,0.7327118,0.00013210147,0.00025593326,0.0008618157,0.00059925864,0.07207038,0.11492067,0.0012451016,0.00081802,0.07445672],"study_design_scores_gemma":[0.000038588467,0.00020612344,0.91285837,0.0000103473485,0.00004788217,0.0003586515,0.00031276798,0.0704052,0.0141954515,0.0003683818,0.0011723646,0.000025933323],"about_ca_topic_score_codex":0.0025056575,"about_ca_topic_score_gemma":0.0020656472,"teacher_disagreement_score":0.0025056575,"about_ca_system_score_codex":0.000177326,"about_ca_system_score_gemma":0.00012855559,"threshold_uncertainty_score":0.0049821734},"labels":[],"label_agreement":null},{"id":"W2366255264","doi":"10.1002/2015gl066479","title":"Poroelastic response of mid‐ocean ridge hydrothermal systems to ocean tidal loading: Implications for shallow permeability structure","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Victoria; Woods Hole Oceanographic Institution","keywords":"Hydrothermal vent; Hydrothermal circulation; Geology; Poromechanics; Permeability (electromagnetism); Ridge; Oceanography; Mid-ocean ridge; Amplitude; Seabed; Petrology; Geophysics; Seismology; Paleontology; Geotechnical engineering; Porous medium; Porosity","score_opus":0.026693354657617737,"score_gpt":0.28226178438369454,"score_spread":0.2555684297260768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2366255264","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993839,0.000004848887,0.00042922844,0.000009611223,6.833069e-7,0.0000018774238,0.0000365654,0.000010944176,0.00012226583],"genre_scores_gemma":[0.9998591,0.00000340295,0.00009265412,0.0000013067147,4.0133062e-7,9.965119e-7,0.000015705291,0.0000015887914,0.000024883351],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995685,0.000010626586,0.0000038997923,0.000010638226,0.0000046306673,0.000013247797],"domain_scores_gemma":[0.9997774,0.00006739408,0.000055605455,0.000028986802,0.00001804434,0.000052568616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018378266,0.00019523097,0.00019452896,0.00021406423,0.00016823484,0.0005535661,0.00028943364,0.00033974266,0.000636691],"category_scores_gemma":[0.0007101548,0.00020229872,0.00034614716,0.00015847218,0.00038738066,0.0003256267,0.0003201859,0.0001933584,0.00007064439],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003246646,0.00015563724,0.5017743,0.00003324042,0.00012215607,0.00021234617,0.00013189187,0.42393973,0.06766713,0.00070533407,0.00010160642,0.0048319004],"study_design_scores_gemma":[0.000025574083,0.00008651163,0.30064347,0.00000269508,0.000015288368,0.000038420476,0.00007831791,0.695207,0.0035309708,0.0002756872,0.00008119626,0.000014877891],"about_ca_topic_score_codex":0.009003987,"about_ca_topic_score_gemma":0.004700638,"teacher_disagreement_score":0.009003987,"about_ca_system_score_codex":0.00045280097,"about_ca_system_score_gemma":0.0002503495,"threshold_uncertainty_score":0.01790315},"labels":[],"label_agreement":null},{"id":"W2382749861","doi":"10.1002/2016gl068891","title":"Thermohaline instability and the formation of glacial North Atlantic super polynyas at the onset of Dansgaard‐Oeschger warming events","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Stadial; Thermohaline circulation; Geology; Glacial period; Climatology; North Atlantic Deep Water; Oceanography; Instability; Shutdown of thermohaline circulation; Geomorphology","score_opus":0.02895912027373255,"score_gpt":0.2771012871749049,"score_spread":0.24814216690117236,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2382749861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995559,0.00001111552,0.00007038711,0.000014541445,0.0000010223513,8.248926e-7,0.00003064858,0.00000330281,0.00031214335],"genre_scores_gemma":[0.99986887,0.000007633171,0.00002949361,0.0000018552303,3.0950775e-7,6.9892997e-7,0.000025756253,9.111038e-7,0.000064318614],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999778,0.0000037523969,0.0000015866663,0.000006893189,0.000003072933,0.0000068608756],"domain_scores_gemma":[0.9999025,0.000023484623,0.000022794226,0.0000073721803,0.000009768546,0.00003409642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011025451,0.00015256657,0.000091071044,0.000099938414,0.0002437336,0.00046405662,0.00012719612,0.00017272515,0.0011024153],"category_scores_gemma":[0.00048691098,0.00015233326,0.00016277567,0.0000766811,0.0002424126,0.00023671944,0.0002950505,0.00018131139,0.0000651666],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059680827,0.00011180113,0.8418832,0.000039465715,0.00017285689,0.00032748774,0.00043934994,0.118426025,0.029424017,0.0025530225,0.00047979548,0.005546144],"study_design_scores_gemma":[0.00005456853,0.000081555845,0.81540924,0.0000073579386,0.000044697947,0.00006521177,0.00024504124,0.17995374,0.0027383608,0.0008397651,0.00054634374,0.000014122979],"about_ca_topic_score_codex":0.036753003,"about_ca_topic_score_gemma":0.049997274,"teacher_disagreement_score":0.036753003,"about_ca_system_score_codex":0.0007380631,"about_ca_system_score_gemma":0.00046593446,"threshold_uncertainty_score":0.073078156},"labels":[],"label_agreement":null},{"id":"W2396292382","doi":"10.1002/2016gl068996","title":"Vulnerability of a semienclosed estuarine sea to ocean acidification in contrast with hypoxia","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Fisheries and Oceans Canada","funders":"","keywords":"Ocean acidification; Oceanography; Aragonite; Hypoxia (environmental); Shoal; Geology; Estuary; Environmental science; Ocean current; Climate change; Oxygen; Geochemistry; Calcite; Chemistry","score_opus":0.027357677482972218,"score_gpt":0.28648500786697084,"score_spread":0.2591273303839986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2396292382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996743,0.000014350778,0.000013256249,0.000010289661,9.808576e-7,0.0000012877573,0.00005492435,0.000001465387,0.00022916007],"genre_scores_gemma":[0.9998642,0.000009017659,0.000013717125,0.000009258423,6.831491e-7,8.219591e-7,0.00006421247,4.4144537e-7,0.000037558497],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998901,0.000017488794,0.0000139087915,0.000025949334,0.000013979444,0.000038608312],"domain_scores_gemma":[0.99950635,0.000042391595,0.00023077549,0.00004064055,0.00006200863,0.00011790681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015437073,0.00013716369,0.00021671859,0.00040523795,0.00036742087,0.00060358824,0.00019855058,0.00029465018,0.0006636818],"category_scores_gemma":[0.00043375714,0.00011184298,0.00018030888,0.000499621,0.00055760605,0.00025785837,0.0010266961,0.00015862336,0.00007442517],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037649766,0.000034408175,0.9759873,0.000024040577,0.00006952313,0.0005019337,0.00045161476,0.0005524752,0.019848466,0.00008614715,0.00011173219,0.0019558072],"study_design_scores_gemma":[0.0000018178863,0.0000460045,0.998708,0.000002877462,0.0000062144345,0.00006896577,0.00060997374,0.00015803744,0.00023314713,0.00004294893,0.0001195795,0.0000024438548],"about_ca_topic_score_codex":0.017697744,"about_ca_topic_score_gemma":0.03361607,"teacher_disagreement_score":0.017697744,"about_ca_system_score_codex":0.00047824415,"about_ca_system_score_gemma":0.00031319275,"threshold_uncertainty_score":0.03518945},"labels":[],"label_agreement":null},{"id":"W2398047876","doi":"10.1002/2016gl069049","title":"A scalable model for methane consumption in arctic mineral soils","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Danmarks Grundforskningsfond; National Research Foundation","keywords":"Methane; Soil water; Sink (geography); Environmental science; Arctic; Microcosm; Methanotroph; Flux (metallurgy); Environmental chemistry; Atmospheric sciences; Greenhouse gas; Soil science; Chemistry; Ecology; Anaerobic oxidation of methane; Geology; Biology","score_opus":0.03698599648168018,"score_gpt":0.29742941520258653,"score_spread":0.26044341872090637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2398047876","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.71293575,0.00046663717,0.25573662,0.0011766496,0.00018533933,0.00023583588,0.003382195,0.0013600738,0.024520863],"genre_scores_gemma":[0.97638273,0.00013269331,0.019319935,0.00008888622,0.000028799179,0.00025319905,0.00055673067,0.00008301772,0.0031540596],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998229,0.000047223326,0.000007365171,0.00004181162,0.000032080134,0.000048623766],"domain_scores_gemma":[0.9993087,0.00038918658,0.00007030209,0.000042558346,0.00010798035,0.000081381935],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050674385,0.00075582654,0.0008318393,0.0004045717,0.0007271137,0.0010601524,0.001547716,0.001553815,0.003113503],"category_scores_gemma":[0.0019101442,0.0004894072,0.00077393086,0.0004570209,0.0008154033,0.0008917685,0.001069188,0.00093498576,0.00028974618],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019865187,0.000010093094,0.00032686646,0.000007146674,0.0000055384767,0.00001765519,0.000004902548,0.99777967,0.0002502093,0.0011367236,0.000094606345,0.00034671382],"study_design_scores_gemma":[0.000008777313,0.0000030081742,0.000033119646,6.715717e-7,0.00000120121,0.0000012287497,0.000002282189,0.9994766,0.000047214173,0.00036179827,0.00006282853,0.0000013131818],"about_ca_topic_score_codex":0.05533591,"about_ca_topic_score_gemma":0.021538015,"teacher_disagreement_score":0.05533591,"about_ca_system_score_codex":0.0017912111,"about_ca_system_score_gemma":0.0025327022,"threshold_uncertainty_score":0.11002761},"labels":[],"label_agreement":null},{"id":"W2398233130","doi":"10.1002/2016gl068782","title":"The contribution of an overlooked transport process to a wetland's methane emissions","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Philomathia Foundation; Department of Water Resources; U.S. Department of Energy","keywords":"Methane; Wetland; Environmental science; Greenhouse gas; Temperate climate; Atmosphere (unit); Atmospheric sciences; Atmospheric methane; Marsh; Convection; Methanogenesis; Hydrology (agriculture); Ecology; Geology; Meteorology; Physics; Oceanography","score_opus":0.01749225917949278,"score_gpt":0.3139254944682451,"score_spread":0.2964332352887523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2398233130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99609274,0.0000509096,0.0028517866,0.000091766095,0.000011026049,0.0000069992852,0.00006784422,0.000025745212,0.00080112397],"genre_scores_gemma":[0.999526,0.000023499726,0.00026479407,0.000005202062,0.0000023921943,0.0000029981325,0.000022429433,0.0000052789205,0.00014743618],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999063,0.000021859867,0.000005471897,0.000024941002,0.000011724144,0.000029729244],"domain_scores_gemma":[0.9997278,0.00012272457,0.00004275209,0.000025216901,0.00004092994,0.000040552284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031738018,0.00038883675,0.00032406088,0.0002803347,0.00052729796,0.00068115036,0.00037812712,0.00054782565,0.0007179525],"category_scores_gemma":[0.0008490887,0.0001892594,0.0005717076,0.00017446397,0.00034984542,0.0008099882,0.00053766574,0.00035088923,0.00006681183],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038827042,0.0002662552,0.28525373,0.00017547664,0.00019183861,0.00064077973,0.00019453767,0.59342533,0.09963296,0.004700639,0.00047877012,0.0146514345],"study_design_scores_gemma":[0.000020832606,0.0001257284,0.06594863,0.000011077892,0.000068885056,0.000089924324,0.00018239231,0.924226,0.007310049,0.0013190926,0.0006629538,0.000034441335],"about_ca_topic_score_codex":0.032386117,"about_ca_topic_score_gemma":0.01654004,"teacher_disagreement_score":0.032386117,"about_ca_system_score_codex":0.0012382919,"about_ca_system_score_gemma":0.0008652861,"threshold_uncertainty_score":0.06439525},"labels":[],"label_agreement":null},{"id":"W2403113376","doi":"10.1002/2016gl069140","title":"Electron dropout echoes induced by interplanetary shock: Van Allen Probes observations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Physics; Interplanetary spaceflight; Dropout (neural networks); Electron; Substorm; Magnetosphere; Astrophysics; Magnetopause; Computational physics; Solar wind; Atomic physics; Plasma; Nuclear physics","score_opus":0.021475161003744508,"score_gpt":0.28617849491107766,"score_spread":0.26470333390733314,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2403113376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957681,0.0001397539,0.001303202,0.000056475266,0.000009359678,0.000011044732,0.00033371308,0.00009301807,0.0022853394],"genre_scores_gemma":[0.99801826,0.000053233667,0.0008829972,0.00002411857,0.0000061916394,0.000006842411,0.00043344384,0.000011175625,0.00056364987],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993753,0.0000051213215,0.0000016792414,0.000015623835,0.000021660828,0.000018386181],"domain_scores_gemma":[0.99988616,0.000021579017,0.000024396139,0.000015163909,0.000023102848,0.00002948551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013535316,0.00016006036,0.0001811906,0.0005106564,0.0002034968,0.00027761483,0.0003072948,0.00033022984,0.00062961155],"category_scores_gemma":[0.000258994,0.00017148453,0.00009986849,0.00034695794,0.00014254382,0.0002413927,0.0004085799,0.00048557593,0.00014717599],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064415776,0.0000793081,0.1195275,0.00008677441,0.00009643721,0.0022627285,0.0018827502,0.001250606,0.8417656,0.00068949757,0.0013983848,0.030316347],"study_design_scores_gemma":[0.000052811112,0.0004347831,0.9162318,0.00003770743,0.00007069955,0.0011516602,0.0006329569,0.007862856,0.06344038,0.00039586812,0.009642922,0.00004553358],"about_ca_topic_score_codex":0.003238708,"about_ca_topic_score_gemma":0.0061303475,"teacher_disagreement_score":0.003238708,"about_ca_system_score_codex":0.00020929557,"about_ca_system_score_gemma":0.00010532808,"threshold_uncertainty_score":0.006439686},"labels":[],"label_agreement":null},{"id":"W2405500967","doi":"10.1002/2016gl068964","title":"Enhancement of non‐CO<sub>2</sub> radiative forcing via intensified carbon cycle feedbacks","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Victoria","keywords":"Radiative forcing; Environmental science; Greenhouse gas; Carbon cycle; Atmospheric sciences; Forcing (mathematics); Carbon fibers; Carbon sink; Global warming; Atmosphere (unit); Carbon dioxide; Greenhouse effect; Climatology; Climate change; Climate model; Chemistry; Meteorology; Materials science; Physics; Geology; Ecosystem; Ecology","score_opus":0.011465692804885812,"score_gpt":0.2560101487839973,"score_spread":0.24454445597911148,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2405500967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932017,0.00005771907,0.003209924,0.00011337331,0.000018015891,0.000011902714,0.00006864697,0.00009796785,0.0032207791],"genre_scores_gemma":[0.99902904,0.000028774964,0.0006063714,0.000025264078,0.000005787427,0.000004886794,0.000014531645,0.000007125109,0.00027804045],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999081,0.000023094915,0.0000040213517,0.000020714748,0.000018197417,0.00002578152],"domain_scores_gemma":[0.99966323,0.0001553556,0.00006484752,0.00004791434,0.000027322334,0.00004138782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002148306,0.00031447512,0.00027190018,0.00012827101,0.00016820774,0.00060281676,0.0002462972,0.00031370108,0.0040448164],"category_scores_gemma":[0.00055115455,0.00018155809,0.0003222939,0.00010929139,0.0006273414,0.0005407548,0.0005795363,0.00045072078,0.0001734151],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014844807,0.00036333967,0.020270271,0.0001989891,0.00013825054,0.00070605375,0.000107176864,0.28986266,0.66420835,0.01136683,0.0006649742,0.010628593],"study_design_scores_gemma":[0.0007246845,0.0011563132,0.11536226,0.00002520352,0.00016967278,0.00056834536,0.00019140932,0.6486733,0.2113194,0.016548613,0.0051330207,0.0001278001],"about_ca_topic_score_codex":0.0017739123,"about_ca_topic_score_gemma":0.0018239574,"teacher_disagreement_score":0.0040448164,"about_ca_system_score_codex":0.00046837068,"about_ca_system_score_gemma":0.00022981215,"threshold_uncertainty_score":0.013531327},"labels":[],"label_agreement":null},{"id":"W2406028171","doi":"10.1002/2016gl068760","title":"Future acidification of marginal seas: A comparative study of the Japan/East Sea and the South China Sea","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ocean acidification; Sink (geography); Biogeochemical cycle; Environmental science; Oceanography; China sea; Structural basin; China; Seawater; Geology; Climatology; Geography; Environmental chemistry; Chemistry","score_opus":0.03175961564457665,"score_gpt":0.2823538602686199,"score_spread":0.2505942446240433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2406028171","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99982053,0.000016831822,0.0000130224,0.000009571432,3.7265505e-7,8.658898e-7,0.00002166354,3.431472e-7,0.000116835894],"genre_scores_gemma":[0.99983287,0.000031866308,0.000023969109,0.0000038494836,0.0000010421481,0.0000010760624,0.000048257538,3.48426e-7,0.000056593377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994993,0.000009936258,0.000004536889,0.000010036714,0.000007775782,0.000017820648],"domain_scores_gemma":[0.9997886,0.00003784165,0.000054370565,0.000011757931,0.000037624017,0.000069775706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023721467,0.00017122524,0.0001953129,0.0004492705,0.0003087761,0.00046564674,0.00015372809,0.00020092043,0.00089505943],"category_scores_gemma":[0.00043739824,0.00010848462,0.00051855575,0.0007221104,0.00039034666,0.0004918925,0.0005573892,0.00013930892,0.000042239557],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021478996,0.000027479013,0.99145424,0.000028982684,0.00009852934,0.00040996572,0.000597878,0.002731914,0.002208286,0.00024364205,0.00005444753,0.0019298109],"study_design_scores_gemma":[0.0000061333585,0.000044556047,0.99602354,0.0000036031747,0.000027663316,0.00003571214,0.0011959714,0.0022844025,0.00015545939,0.00006620964,0.00015204005,0.000004683158],"about_ca_topic_score_codex":0.06395915,"about_ca_topic_score_gemma":0.08331539,"teacher_disagreement_score":0.06395915,"about_ca_system_score_codex":0.00064402557,"about_ca_system_score_gemma":0.00065227423,"threshold_uncertainty_score":0.12717372},"labels":[],"label_agreement":null},{"id":"W2409045691","doi":"10.1002/2016gl070233","title":"Van Allen Probes observations of oxygen cyclotron harmonic waves in the inner magnetosphere","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Aeronautics and Space Administration","keywords":"Magnetosphere; Physics; Poynting vector; Ring current; Van Allen Probes; Van Allen radiation belt; Cyclotron; Electromagnetic radiation; Geomagnetic storm; Plasmasphere; Atomic physics; Amplitude; Geophysics; Computational physics; Earth's magnetic field; Electron; Magnetic field; Nuclear physics; Optics","score_opus":0.02982211597443287,"score_gpt":0.28212744124661077,"score_spread":0.2523053252721779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2409045691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99325895,0.00010024285,0.0002702005,0.00005415045,0.0000069591283,0.000007788809,0.00028405132,0.000024621762,0.005993031],"genre_scores_gemma":[0.9981046,0.00007732254,0.0005506445,0.00002300003,0.000009464053,0.00000613163,0.00034431662,0.0000069629327,0.00087745447],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.0000050386043,0.0000018329755,0.000014068374,0.000023732831,0.000020168012],"domain_scores_gemma":[0.99988747,0.000022562168,0.000038421324,0.00000899207,0.000021143796,0.00002147336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010190893,0.00010961075,0.0000939615,0.000567034,0.0002503094,0.0002806184,0.00021402586,0.00015660396,0.0005966344],"category_scores_gemma":[0.00024352243,0.000097589036,0.000053293774,0.000365085,0.00013704249,0.00019294953,0.00033319712,0.0001902422,0.00009040332],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000493505,0.00009218638,0.28788358,0.000106771055,0.00012662579,0.0010115124,0.0025585725,0.0022667858,0.6549806,0.0023074152,0.0027523122,0.045420118],"study_design_scores_gemma":[0.000042010673,0.00019747975,0.95605063,0.000030204057,0.000043932603,0.00032737377,0.00063016464,0.0032261428,0.02732828,0.00034339965,0.011758434,0.000021994842],"about_ca_topic_score_codex":0.011687169,"about_ca_topic_score_gemma":0.027388407,"teacher_disagreement_score":0.011687169,"about_ca_system_score_codex":0.00022706587,"about_ca_system_score_gemma":0.000108223,"threshold_uncertainty_score":0.023238242},"labels":[],"label_agreement":null},{"id":"W2410304542","doi":"10.1002/2016gl069084","title":"First‐principles prediction of fast migration channels of potassium ions in KAlSi<sub>3</sub>O<sub>8</sub> hollandite: Implications for high conductivity anomalies in subduction zones","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Nuclear materials and radiation effects","field":"Materials Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Hollandite; Ringwoodite; Ionic conductivity; Conductivity; Alkali metal; Biogeosciences; Geology; Ionic bonding; Mineralogy; Materials science; Ion; Mantle (geology); Geochemistry; Chemistry; Physical chemistry; Electrolyte","score_opus":0.038126513530782044,"score_gpt":0.2844305075254258,"score_spread":0.24630399399464376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2410304542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.92918235,0.00061325205,0.043074265,0.0006002035,0.000056004556,0.000120569144,0.0004592185,0.00038423282,0.025509873],"genre_scores_gemma":[0.9901147,0.0002739138,0.006782524,0.00006386773,0.000011702553,0.0001195644,0.00018602822,0.00009528469,0.002352492],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998952,0.000024328494,0.000003177723,0.0000091982565,0.000035251414,0.000032688462],"domain_scores_gemma":[0.99968517,0.00015945484,0.00003151371,0.000023369206,0.00006886399,0.00003172059],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003980364,0.000648123,0.0007888419,0.0006185793,0.00077199284,0.00093238236,0.0010619846,0.0016308539,0.002108327],"category_scores_gemma":[0.00061879185,0.00057154964,0.0008809722,0.00046697113,0.0006619384,0.00053505634,0.0004107957,0.0005129488,0.00035890559],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008325382,0.000088465415,0.0017153042,0.00015318871,0.00003901068,0.0002905301,0.00010028068,0.97723037,0.007821287,0.008787749,0.0006446706,0.0030459159],"study_design_scores_gemma":[0.000028203664,0.00001796888,0.00054099545,0.000006824564,0.0000056208955,0.000012284321,0.000027120015,0.9968135,0.0007290491,0.0016611004,0.00015142221,0.0000060382185],"about_ca_topic_score_codex":0.009489795,"about_ca_topic_score_gemma":0.00921108,"teacher_disagreement_score":0.009489795,"about_ca_system_score_codex":0.0009782154,"about_ca_system_score_gemma":0.001223872,"threshold_uncertainty_score":0.018869162},"labels":[],"label_agreement":null},{"id":"W2412363337","doi":"10.1002/2016gl069296","title":"Anthropogenic influence on the frequency of extreme temperatures in China","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China; Bijzonder Onderzoeksfonds UGent","keywords":"Coupled model intercomparison project; Environmental science; Climatology; Daytime; Atmospheric sciences; Climate model; China; Climate change; Geology; Geography; Oceanography","score_opus":0.042522257735647835,"score_gpt":0.3072911892175147,"score_spread":0.26476893148186686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2412363337","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995845,0.000023081366,0.00011222241,0.000013712045,0.0000015021043,6.436075e-7,0.00006591072,0.000004467155,0.00019389039],"genre_scores_gemma":[0.9998779,0.000011510393,0.000021097025,0.0000015660665,0.0000021905878,5.859055e-7,0.00006112357,6.017949e-7,0.000023376922],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998387,0.00003854379,0.000013266358,0.00004471162,0.000033687877,0.000030995358],"domain_scores_gemma":[0.9994512,0.000114777045,0.00018960371,0.000070877366,0.0001129279,0.000060598497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039018592,0.00018633304,0.0001564365,0.00057160435,0.00018953173,0.0003777852,0.00016087267,0.00009328656,0.00038331095],"category_scores_gemma":[0.0007599258,0.000112294576,0.00023513492,0.0007058339,0.0003464798,0.00020607263,0.0003359807,0.000106799234,0.000032941807],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006193234,0.000012654268,0.9832696,0.000014549702,0.000079655605,0.00009864929,0.0002270818,0.008134276,0.0034959256,0.00026157452,0.000095117684,0.004249041],"study_design_scores_gemma":[0.0000023387481,0.00001147613,0.99484825,0.0000016396436,0.000012036301,0.000018267168,0.00005156038,0.0045698746,0.00025564936,0.000053143332,0.00017163846,0.000004160539],"about_ca_topic_score_codex":0.018182712,"about_ca_topic_score_gemma":0.020462459,"teacher_disagreement_score":0.018182712,"about_ca_system_score_codex":0.00062460214,"about_ca_system_score_gemma":0.00034394534,"threshold_uncertainty_score":0.036153793},"labels":[],"label_agreement":null},{"id":"W2416278938","doi":"10.1002/2016gl067862","title":"Austral winter external and internal atmospheric variability between 1980 and 2014","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Bundesministerium für Bildung und Forschung","keywords":"Empirical orthogonal functions; Predictability; Climatology; Southern Hemisphere; Atmospheric circulation; Monsoon; Northern Hemisphere; Mode (computer interface); Environmental science; Sea surface temperature; Atmospheric dynamics; Atmospheric research; Atmospheric sciences; Geology; Geography; Atmosphere (unit); Meteorology","score_opus":0.031194275684870636,"score_gpt":0.3036387696341715,"score_spread":0.27244449394930087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2416278938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965407,0.00007010309,0.000103734856,0.000053027925,0.000013377595,0.0000024287897,0.001986631,0.000017779737,0.001212078],"genre_scores_gemma":[0.9967744,0.00006351612,0.000088650704,0.000011067318,0.000016416427,0.0000043080704,0.0023627642,0.0000069559674,0.0006719572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993,0.000007362224,0.000006066752,0.000022665527,0.000016373842,0.000017592956],"domain_scores_gemma":[0.9996432,0.000026380056,0.00015012975,0.000023851222,0.000097455675,0.000058936377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021828513,0.00021395547,0.00014820261,0.00063590566,0.00019427037,0.0005097448,0.00012283002,0.00016289631,0.001002213],"category_scores_gemma":[0.0005988942,0.00008886957,0.00023101806,0.0007166584,0.00019490994,0.00031927816,0.00044994915,0.00023622747,0.00019957875],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001311777,0.00003248536,0.98016053,0.000046303954,0.00015394666,0.00012746996,0.00036351223,0.0028063285,0.002511111,0.00030128306,0.0021821333,0.0111837415],"study_design_scores_gemma":[0.0000021921262,0.000009165072,0.9979785,0.0000050622243,0.0000100026655,0.000020317395,0.000063080515,0.00086938275,0.00010097421,0.000036631067,0.00090220594,0.0000025504057],"about_ca_topic_score_codex":0.044520587,"about_ca_topic_score_gemma":0.073643506,"teacher_disagreement_score":0.044520587,"about_ca_system_score_codex":0.0005590165,"about_ca_system_score_gemma":0.0003051048,"threshold_uncertainty_score":0.08852291},"labels":[],"label_agreement":null},{"id":"W2416838478","doi":"10.1002/2016gl069245","title":"Relevance of dissolved organic nutrients for the Arctic Ocean nutrient budget","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Biogeochemical cycle; Nutrient; Oceanography; Environmental science; Arctic; Lead (geology); Geology; Ecology; Chemistry; Environmental chemistry; Biology","score_opus":0.019477574851639368,"score_gpt":0.264601571598278,"score_spread":0.24512399674663865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2416838478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98482776,0.004701061,0.0019738746,0.0010387077,0.00007930098,0.000011638722,0.0011955367,0.00002275715,0.006149446],"genre_scores_gemma":[0.99696016,0.001351279,0.00088517176,0.000055922996,0.000030567764,0.0000030774638,0.0003229987,0.000008469094,0.00038230504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987173,0.000030177169,0.000015380112,0.000034391505,0.000031019063,0.000017281165],"domain_scores_gemma":[0.99944335,0.00019380568,0.00012592656,0.000027734377,0.00015370072,0.00005545027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000725789,0.00032369007,0.00023342343,0.000544185,0.00043425197,0.0016658328,0.00023041882,0.00026526494,0.00068240176],"category_scores_gemma":[0.0016707886,0.00013455263,0.00022819969,0.00047303046,0.00027267457,0.0007881927,0.00041334328,0.00020467701,0.00011299342],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006883087,0.000050865186,0.88639355,0.000572728,0.00041231242,0.00033088584,0.00021949245,0.024912676,0.033109296,0.0054399744,0.00073769357,0.047132265],"study_design_scores_gemma":[0.000048375463,0.0001901922,0.8425905,0.00036238824,0.00044958555,0.00024123736,0.001273409,0.11376674,0.013527055,0.017281076,0.01021664,0.00005280691],"about_ca_topic_score_codex":0.0347761,"about_ca_topic_score_gemma":0.028091006,"teacher_disagreement_score":0.0347761,"about_ca_system_score_codex":0.0010816746,"about_ca_system_score_gemma":0.0007997436,"threshold_uncertainty_score":0.06914735},"labels":[],"label_agreement":null},{"id":"W2418881573","doi":"10.1002/2016gl069219","title":"The effect of crack orientation on the nonlinear interaction of a <i>P</i> wave with an <i>S</i> wave","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Research and Development Corporation of Newfoundland and Labrador; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Chevron","keywords":"Nonlinear system; Amplitude; Orientation (vector space); Anisotropy; SIGNAL (programming language); Scale (ratio); Work (physics); Mechanics; Acoustics; Materials science; Geology; Physics; Optics; Geometry; Mathematics; Computer science; Thermodynamics","score_opus":0.026852632488733076,"score_gpt":0.28583965491388086,"score_spread":0.25898702242514776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2418881573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865025,0.000027673177,0.0006695204,0.00002139368,0.0000036713743,0.00000452568,0.000021480279,0.000012290455,0.00058930553],"genre_scores_gemma":[0.9994289,0.000027166108,0.00036209772,0.0000094648785,0.0000030487813,0.000003272937,0.000015663125,0.000006337074,0.00014387355],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998405,0.000029023513,0.0000075018133,0.000032011838,0.00005104766,0.00003994187],"domain_scores_gemma":[0.99885,0.00060907344,0.00027197658,0.00006376698,0.00010355585,0.00010160211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031615706,0.00022424696,0.00013230147,0.00021366864,0.00017868621,0.0003848706,0.00018589312,0.00020681886,0.001346763],"category_scores_gemma":[0.0011530746,0.00019208588,0.00011012201,0.00016802562,0.0006283703,0.0002754306,0.00030087554,0.00039451523,0.00014900562],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036976795,0.000052062584,0.004810426,0.000035046687,0.000011932089,0.000085686035,0.00009814054,0.0012302998,0.989938,0.00013977558,0.000051748746,0.0031771662],"study_design_scores_gemma":[0.000042082276,0.0006447092,0.09529501,0.00001407793,0.000047365935,0.0001684078,0.0001934633,0.024997223,0.87799746,0.00009063639,0.00047590994,0.00003359382],"about_ca_topic_score_codex":0.0011521433,"about_ca_topic_score_gemma":0.0010805051,"teacher_disagreement_score":0.001346763,"about_ca_system_score_codex":0.00019996199,"about_ca_system_score_gemma":0.00017608743,"threshold_uncertainty_score":0.004505396},"labels":[],"label_agreement":null},{"id":"W2419125919","doi":"10.1002/2016gl068496","title":"First assessment of continental energy storage in CMIP5 simulations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal; St. Francis Xavier University","funders":"","keywords":"Coupled model intercomparison project; Permafrost; Continental shelf; Environmental science; Climate change; Climatology; Range (aeronautics); Earth science; Climate model; Geothermal gradient; Earth system science; Energy storage; Geology; Atmospheric sciences; Geophysics; Oceanography; Physics","score_opus":0.060442609354195445,"score_gpt":0.3309883719116322,"score_spread":0.2705457625574368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2419125919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9913345,0.00024272513,0.0014844447,0.00018420035,0.000018573386,0.000022636004,0.0025650223,0.00017169132,0.0039763097],"genre_scores_gemma":[0.997558,0.000039201255,0.0009066554,0.000040569023,0.000004300854,0.000015918678,0.0012771286,0.000020281695,0.00013799775],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99962616,0.00015267191,0.000030320436,0.00006680367,0.000056380115,0.000067699766],"domain_scores_gemma":[0.9984485,0.00071675103,0.00014838154,0.0002955434,0.00028126093,0.000109556066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0022114643,0.0010056003,0.0006789148,0.0006512235,0.0005612845,0.0009571566,0.0008720227,0.0010379243,0.0016443995],"category_scores_gemma":[0.0049487017,0.00031111817,0.0007460386,0.0010413934,0.00048174246,0.000925567,0.0009100548,0.00060898793,0.00015346329],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062343024,0.00014143353,0.078955434,0.00021057561,0.0004605671,0.00020808859,0.00021214038,0.9001448,0.004495936,0.0027775103,0.0020784484,0.009691717],"study_design_scores_gemma":[0.000110074594,0.00024840492,0.04833761,0.00006474606,0.00010119352,0.000055009197,0.0002310558,0.94370437,0.0046851826,0.0010679123,0.0013481479,0.00004626641],"about_ca_topic_score_codex":0.023515956,"about_ca_topic_score_gemma":0.017873557,"teacher_disagreement_score":0.023515956,"about_ca_system_score_codex":0.001011899,"about_ca_system_score_gemma":0.0006058291,"threshold_uncertainty_score":0.046758175},"labels":[],"label_agreement":null},{"id":"W2428299833","doi":"10.1002/2016gl069824","title":"On how spatial variations of channel width influence river profile curvature","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Curvature; Geology; Channel (broadcasting); Flow (mathematics); Surface finish; Hydrology (agriculture); Geomorphology; Alluvium; Geometry; Mechanics; Geotechnical engineering; Physics; Materials science; Mathematics","score_opus":0.015524699307300714,"score_gpt":0.2650205666254386,"score_spread":0.2494958673181379,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2428299833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99496776,0.000050196188,0.0037363488,0.000048584625,0.0000027050792,0.00000303979,0.000037417863,0.000025625457,0.0011281585],"genre_scores_gemma":[0.99979204,0.000009537865,0.00013439538,0.0000026672913,6.7379443e-7,5.800091e-7,0.000008099608,0.0000034052669,0.00004854322],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999828,0.000069959235,0.000007280873,0.00004549266,0.000021454849,0.000027864906],"domain_scores_gemma":[0.9981882,0.0011539118,0.0002583607,0.00015649445,0.00017167225,0.00007130055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003972025,0.00013536903,0.00014251718,0.00032833937,0.00015055692,0.00052423344,0.00016622682,0.00019091416,0.00070283626],"category_scores_gemma":[0.0032979115,0.00013929112,0.00012595525,0.00024113964,0.00042250202,0.00039561535,0.00035485305,0.00018787711,0.00006991016],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006797073,0.00017117678,0.5345553,0.00009975745,0.0001625801,0.00045122395,0.00085912156,0.2298597,0.1537652,0.00788112,0.0010393448,0.07047573],"study_design_scores_gemma":[0.000015852514,0.00013620658,0.66422963,0.000016954085,0.00006547009,0.00010780829,0.00049007067,0.31911424,0.012083386,0.002975451,0.0007165125,0.00004841649],"about_ca_topic_score_codex":0.003989746,"about_ca_topic_score_gemma":0.0031372237,"teacher_disagreement_score":0.003989746,"about_ca_system_score_codex":0.00025631173,"about_ca_system_score_gemma":0.00015170446,"threshold_uncertainty_score":0.00793308},"labels":[],"label_agreement":null},{"id":"W2444550892","doi":"10.1002/2016gl069579","title":"Acoustic observations of near‐bed sediment concentration and flux statistics above migrating sand dunes","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sediment; Geology; Mass flux; Flux (metallurgy); Sediment transport; Acoustic Doppler current profiler; Bed load; Flow (mathematics); Geomorphology; Mechanics; Current (fluid); Physics; Oceanography","score_opus":0.029125310182644828,"score_gpt":0.28689033694819704,"score_spread":0.25776502676555224,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2444550892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999383,0.000007782974,0.0004085691,0.0000035461142,9.1808704e-7,0.0000012322982,0.000035423673,0.000010587014,0.00014891967],"genre_scores_gemma":[0.9995028,0.000009860447,0.0003169057,0.0000027385336,0.0000020669447,0.000001731856,0.00005206078,0.000001680161,0.00011021277],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999466,0.000006143461,0.0000021439894,0.000013854199,0.000020474477,0.000010713417],"domain_scores_gemma":[0.99977607,0.00007276015,0.00003848397,0.000010812623,0.000060396495,0.000041508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011196302,0.000118994416,0.00015037615,0.00056964613,0.00016460854,0.00022253132,0.000110718815,0.00012321386,0.00045368538],"category_scores_gemma":[0.0004939516,0.00014147205,0.00006078116,0.0002113841,0.00015196287,0.00015441225,0.00014738004,0.00015579358,0.00008985919],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048623295,0.00009879218,0.34177756,0.000050633866,0.00004677252,0.00026687857,0.00086249923,0.002504993,0.630608,0.0002695603,0.0002320171,0.022796063],"study_design_scores_gemma":[0.000013104521,0.00017470328,0.97813874,0.000004403897,0.000020024376,0.0001286341,0.000205275,0.0086532,0.012345948,0.00005003524,0.0002517095,0.000014249385],"about_ca_topic_score_codex":0.003951166,"about_ca_topic_score_gemma":0.004124358,"teacher_disagreement_score":0.003951166,"about_ca_system_score_codex":0.00015579238,"about_ca_system_score_gemma":0.00009621052,"threshold_uncertainty_score":0.007856309},"labels":[],"label_agreement":null},{"id":"W2460375565","doi":"10.1002/2015gl067152","title":"Submesoscale streamers exchange water on the north wall of the Gulf Stream","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Water mass; Gulf Stream; Mode water; Geology; Oceanography; Front (military); North Atlantic Deep Water; Salinity; Mesoscale meteorology; Circumpolar deep water; Flux (metallurgy); Mixing (physics); Subtropics; Thermohaline circulation; Ocean gyre","score_opus":0.025395321748736002,"score_gpt":0.2371825133473822,"score_spread":0.21178719159864617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2460375565","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907553,0.000004765172,0.00012574668,0.00002650967,0.000004308621,0.0000050058015,0.00005699219,0.000012496001,0.0006886201],"genre_scores_gemma":[0.9993236,0.000008647413,0.00017289071,0.000012339426,0.0000019558918,0.000005273741,0.000081027756,0.0000036824651,0.00039077213],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.000009860245,0.0000022938516,0.000010798391,0.0000062855042,0.000020361576],"domain_scores_gemma":[0.99985886,0.00003292866,0.000024252557,0.000011509635,0.000016078848,0.000056374847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012495623,0.00032159776,0.00028372806,0.00021762284,0.00044321487,0.0006208245,0.0004040614,0.00062632107,0.0021012432],"category_scores_gemma":[0.00031087417,0.00017094042,0.0003821385,0.00017154946,0.00040910955,0.00036497417,0.00038846675,0.00038303627,0.00011513839],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062789413,0.00048492788,0.1016266,0.000023897823,0.000094981275,0.00048084228,0.00015004554,0.8805142,0.0077353823,0.0028155604,0.0009622006,0.004483471],"study_design_scores_gemma":[0.00020738016,0.0002616256,0.031016158,0.000008577661,0.000032694854,0.00002776995,0.00022514617,0.9653737,0.001760978,0.0005758388,0.00049361435,0.000016649492],"about_ca_topic_score_codex":0.030712623,"about_ca_topic_score_gemma":0.021868033,"teacher_disagreement_score":0.030712623,"about_ca_system_score_codex":0.00086395757,"about_ca_system_score_gemma":0.0006037612,"threshold_uncertainty_score":0.06106776},"labels":[],"label_agreement":null},{"id":"W2460507574","doi":"10.1002/2016gl069179","title":"Chemical stability of levoglucosan: An isotopic perspective","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Levoglucosan; Chemistry; Aerosol; Mass spectrometry; Particulates; Stable isotope ratio; Chemical stability; Analytical Chemistry (journal); Fractionation; Environmental chemistry; Chromatography; Organic chemistry; Biomass burning","score_opus":0.04111792019693436,"score_gpt":0.29755320979708383,"score_spread":0.2564352896001495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2460507574","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934909,0.0014100843,0.003190108,0.00005542448,0.000014509946,0.000008212933,0.00035441166,0.000021002601,0.0014553664],"genre_scores_gemma":[0.9979189,0.00037160562,0.0008622527,0.000016989381,0.000005210466,0.0000045846637,0.00017598049,0.0000075485164,0.0006368685],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993336,0.000010095586,0.000003709357,0.000017870867,0.00002280804,0.0000122630145],"domain_scores_gemma":[0.99988437,0.000022011009,0.000019933155,0.000009420857,0.000053499272,0.00001078936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016763709,0.00018880554,0.00013408717,0.00039378426,0.00016821398,0.00035164622,0.00020039505,0.00024083705,0.0013044272],"category_scores_gemma":[0.00024828405,0.00007775135,0.00015795261,0.00025654203,0.00024832596,0.00030104283,0.00014316374,0.00026530516,0.00017825617],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000091274545,0.000005047213,0.0018711736,0.000020934967,0.000010122484,0.000026352129,0.00001380843,0.00013710666,0.9960977,0.000086945816,0.000013842288,0.0016256489],"study_design_scores_gemma":[0.0000032064172,0.0000867553,0.016837502,0.000004798795,0.000013910148,0.00008474473,0.00006706067,0.0013439571,0.9803478,0.00016869695,0.0010323992,0.000009256131],"about_ca_topic_score_codex":0.0020073242,"about_ca_topic_score_gemma":0.0012172683,"teacher_disagreement_score":0.0020073242,"about_ca_system_score_codex":0.00030630382,"about_ca_system_score_gemma":0.00012465348,"threshold_uncertainty_score":0.0043637156},"labels":[],"label_agreement":null},{"id":"W2461234094","doi":"10.1002/2016gl070111","title":"Impacts of sea spray geoengineering on ocean biogeochemistry","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"European Research Council","keywords":"Biogeochemistry; Environmental science; Upwelling; Oceanography; Phytoplankton; Seawater; Context (archaeology); Nutrient; Primary production; Ocean current; Atmospheric sciences; Ecosystem; Geology; Chemistry; Ecology","score_opus":0.026944915434538894,"score_gpt":0.2815311867464356,"score_spread":0.2545862713118967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2461234094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982401,0.000029439612,0.00050585734,0.000094021416,0.00000945444,0.0000056873787,0.00008288439,0.000035736637,0.0009968578],"genre_scores_gemma":[0.999708,0.000014691859,0.00014346547,0.00001994384,0.0000020223945,0.0000028333195,0.000029517843,0.000003899989,0.000075594435],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983954,0.00006099795,0.0000085874135,0.000022636346,0.0000227038,0.000045554007],"domain_scores_gemma":[0.9996344,0.00014726822,0.00007516776,0.000040282317,0.000038973023,0.000063833606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002985926,0.00043026888,0.00041806532,0.00023720201,0.0003252432,0.0007080805,0.00043308127,0.0005900917,0.0015127892],"category_scores_gemma":[0.00095695286,0.0002037834,0.0007807115,0.00031645352,0.0006566378,0.00042429345,0.0006505207,0.0005360178,0.00005439353],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002595439,0.0001566892,0.03678965,0.000041680167,0.00015844038,0.0003334097,0.000043312913,0.94226134,0.014638124,0.0018798724,0.00035521196,0.003082683],"study_design_scores_gemma":[0.0002372272,0.000536999,0.04212337,0.0000071696827,0.00010946498,0.000040873227,0.0001269897,0.94847876,0.006600289,0.0010501696,0.00064989127,0.00003879203],"about_ca_topic_score_codex":0.025118057,"about_ca_topic_score_gemma":0.009792976,"teacher_disagreement_score":0.025118057,"about_ca_system_score_codex":0.0009513031,"about_ca_system_score_gemma":0.0006231317,"threshold_uncertainty_score":0.049943686},"labels":[],"label_agreement":null},{"id":"W2463053877","doi":"10.1002/2016gl069671","title":"Evolution of the eddy field in the Arctic Ocean's Canada Basin, 2005–2015","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Halocline; Ocean gyre; Eddy; Baroclinity; Geology; Canada Basin; Oceanography; Arctic; Climatology; Boundary current; Anticyclone; Ocean current; Salinity; Meteorology; Geography; Subtropics; Turbulence","score_opus":0.013128590229316273,"score_gpt":0.24100259440773625,"score_spread":0.22787400417841996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463053877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9937662,0.00032932695,0.00009036743,0.00011796335,0.00001011427,0.000005713712,0.004077229,0.000016090306,0.0015869669],"genre_scores_gemma":[0.9956974,0.00016124026,0.00016200046,0.00003142751,0.0000033706845,0.0000035773944,0.0031545057,0.000003718199,0.0007827904],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980944,0.0000084107105,0.000010873043,0.000040703926,0.000073964264,0.000056600416],"domain_scores_gemma":[0.9991806,0.00003177532,0.00010233612,0.000019475467,0.00051325426,0.0001525333],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033740315,0.00025138157,0.00020397353,0.001625165,0.0010720115,0.001277977,0.0003885551,0.00030499892,0.000684733],"category_scores_gemma":[0.00086699246,0.00016333882,0.0002896854,0.002104407,0.0003723073,0.0002489886,0.00046189746,0.0002196805,0.00013180725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012723097,0.00002687072,0.98574686,0.000031191517,0.00012324854,0.000101987665,0.0004078933,0.0015485183,0.0015564527,0.00025852944,0.0020999261,0.007971363],"study_design_scores_gemma":[0.0000014642013,0.0000042290476,0.99774015,0.000009700387,0.000006895917,0.000013846297,0.00019385626,0.0007755559,0.00014740917,0.000009400287,0.0010928855,0.0000045181937],"about_ca_topic_score_codex":0.9736763,"about_ca_topic_score_gemma":0.9847611,"teacher_disagreement_score":0.026323676,"about_ca_system_score_codex":0.011343139,"about_ca_system_score_gemma":0.00810062,"threshold_uncertainty_score":0.0823006},"labels":[],"label_agreement":null},{"id":"W2463113218","doi":"10.1002/2016gl069750","title":"Very low frequency earthquakes spatiotemporally asynchronous with strong tremor during the 2014 episodic tremor and slip event in Cascadia","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Episodic tremor and slip; Slip (aerodynamics); Moment tensor; Slow earthquake; Asynchronous communication; Inversion (geology); Foreshock; Aftershock; Subduction; Interplate earthquake; Computer science; Deformation (meteorology); Physics; Tectonics","score_opus":0.015822641693187405,"score_gpt":0.2450076607388373,"score_spread":0.22918501904564992,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2463113218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989172,0.000022483962,0.00012825809,0.00004478849,0.0000028501527,0.000002607838,0.0001876871,0.000014400621,0.0006797285],"genre_scores_gemma":[0.9996456,0.000012322066,0.00004848443,0.000003811196,0.0000024793399,0.000002041442,0.00016019872,0.0000020546963,0.00012301924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998443,0.000020056508,0.00001770943,0.00004393329,0.000036832967,0.000037118312],"domain_scores_gemma":[0.9992842,0.00008599329,0.00019353474,0.000059809212,0.0002003567,0.00017612817],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002785186,0.00018922584,0.0002510338,0.0012187957,0.0005636651,0.00047976803,0.00028671874,0.00028078302,0.0014188307],"category_scores_gemma":[0.0017583735,0.00018040415,0.00016516022,0.0010868288,0.0005228235,0.00024839866,0.0006304531,0.00021253424,0.00022953779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011755315,0.000028495408,0.9845353,0.00003506366,0.00007055896,0.00035963068,0.0008723866,0.0012934651,0.0062235454,0.00010170691,0.00046948492,0.0058927867],"study_design_scores_gemma":[0.0000025326779,0.000007916071,0.9989963,0.0000032500259,0.000008080119,0.000025780791,0.00027930248,0.00045099753,0.00008620825,0.000022819702,0.00011358867,0.0000032172452],"about_ca_topic_score_codex":0.06400572,"about_ca_topic_score_gemma":0.1144733,"teacher_disagreement_score":0.06400572,"about_ca_system_score_codex":0.00061074074,"about_ca_system_score_gemma":0.0005166149,"threshold_uncertainty_score":0.12726635},"labels":[],"label_agreement":null},{"id":"W2467285336","doi":"10.1002/2016gl069292","title":"No significant increase in long‐term CH<sub>4</sub> emissions on North Slope of Alaska despite significant increase in air temperature","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Tundra; Environmental science; Atmospheric sciences; Climatology; Methane; Arctic; Greenhouse gas; Biogeochemical cycle; Term (time); Atmospheric methane; Climate change; Methane emissions; Oceanography; Chemistry; Geology; Physics; Environmental chemistry","score_opus":0.009686407921178494,"score_gpt":0.23967494197740105,"score_spread":0.22998853405622255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2467285336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806255,0.000060738977,0.00005650077,0.000019390658,0.000006250871,9.5095726e-7,0.00022647557,0.000007989132,0.0015590836],"genre_scores_gemma":[0.9990251,0.000039639595,0.000037685637,0.000008797856,0.0000025227973,0.0000013407792,0.00029288695,0.0000013276532,0.00059065706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.00000313636,0.0000034635718,0.000019054061,0.000010187287,0.000010322894],"domain_scores_gemma":[0.99988127,0.000012834093,0.00002894241,0.00001224661,0.000036761863,0.000027941382],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008162581,0.00011608771,0.0001189479,0.00025036643,0.00040420628,0.00037938182,0.00015505865,0.0002644077,0.0016743483],"category_scores_gemma":[0.00011808043,0.00010646561,0.00019332448,0.0002047055,0.00023184573,0.0002887339,0.00025536455,0.00017793455,0.00020034578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039770285,0.0000481786,0.92212224,0.000046524186,0.00011879483,0.0004448856,0.00029442296,0.0005565724,0.069028355,0.00009081272,0.00037081723,0.006480772],"study_design_scores_gemma":[8.4144216e-7,0.000022136608,0.9980385,0.0000040250984,0.000014145275,0.000043984706,0.00019612556,0.00015259699,0.0011388916,0.000013954421,0.00037266145,0.0000023145517],"about_ca_topic_score_codex":0.031967968,"about_ca_topic_score_gemma":0.06557992,"teacher_disagreement_score":0.031967968,"about_ca_system_score_codex":0.00035370607,"about_ca_system_score_gemma":0.00027309553,"threshold_uncertainty_score":0.063563764},"labels":[],"label_agreement":null},{"id":"W2468955254","doi":"10.1002/2016gl069800","title":"Stress drop estimates and hypocenter relocations of induced seismicity near Crooked Lake, Alberta","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; McGill University","funders":"","keywords":"Hypocenter; Geology; Seismology; Lineation; Induced seismicity; Fault plane; Tectonics; Fault (geology); Focal mechanism; Magnitude (astronomy); Drop (telecommunication)","score_opus":0.039138615529297455,"score_gpt":0.2834721154750596,"score_spread":0.24433349994576217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2468955254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972536,0.000032444383,0.0003628628,0.000011514799,0.0000014667007,0.000010539038,0.0010093128,0.00003564814,0.001282684],"genre_scores_gemma":[0.9975199,0.000037881044,0.00047225284,0.0000033564281,0.0000010984306,0.000005324132,0.0013967936,0.000005546109,0.0005578036],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986994,0.000006169934,0.000007035938,0.000024885923,0.000058664,0.000033274348],"domain_scores_gemma":[0.9996861,0.000024479019,0.000076313794,0.000012383189,0.00015699845,0.000043778964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012778428,0.00021256323,0.0001290599,0.0018808981,0.00037724175,0.0005345805,0.0004434834,0.00012954434,0.0013137759],"category_scores_gemma":[0.0008224541,0.000112289556,0.00010126368,0.0017038494,0.00020595321,0.00015206392,0.00030010293,0.00015138625,0.00017863374],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013944179,0.000037050508,0.9594697,0.000033205906,0.000043404554,0.00017760482,0.0004397451,0.0069929557,0.010716965,0.00013429706,0.00060114573,0.021214351],"study_design_scores_gemma":[0.0000027451515,0.000006991523,0.99654925,0.0000026976275,0.000004245089,0.000014272626,0.00021087851,0.0024263093,0.00053568895,0.000011222162,0.00023262743,0.0000030979636],"about_ca_topic_score_codex":0.7420767,"about_ca_topic_score_gemma":0.8877424,"teacher_disagreement_score":0.2579233,"about_ca_system_score_codex":0.0022996243,"about_ca_system_score_gemma":0.001403864,"threshold_uncertainty_score":0.51888454},"labels":[],"label_agreement":null},{"id":"W2469158815","doi":"10.1002/2016gl069507","title":"Pattern of dynamic displacements in a strike‐slip earthquake","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; Strong","keywords":"Geology; Seismology; Slip (aerodynamics); Attenuation; Strike-slip tectonics; Geodesy; Directivity; Fault (geology); Trough (economics); Seismic gap","score_opus":0.03077124801852221,"score_gpt":0.29631266527972133,"score_spread":0.2655414172611991,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2469158815","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99902177,0.000022695596,0.00014196523,0.000009380684,0.0000012724502,0.000002065958,0.00025237154,0.00000737417,0.00054100517],"genre_scores_gemma":[0.9994542,0.00001192003,0.00006477282,0.0000020528655,0.0000014280885,0.0000014880079,0.00025742687,8.705354e-7,0.00020593934],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993074,0.0000060229268,0.00000670785,0.00002449608,0.000018696675,0.0000134045795],"domain_scores_gemma":[0.9997708,0.000032648197,0.00009331835,0.000018723284,0.00005244499,0.000032093365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000057659458,0.0001422626,0.00012367695,0.0009773578,0.0001255235,0.00021294157,0.00012920484,0.00020541897,0.0010644717],"category_scores_gemma":[0.00042324193,0.000108096145,0.00005885906,0.0007766152,0.00016831988,0.0001293535,0.00019777702,0.00008307384,0.00025376608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036018732,0.000065357795,0.90343565,0.000054154123,0.00006464066,0.0007067628,0.00061324035,0.00231851,0.06527767,0.00023915825,0.00047015038,0.026394526],"study_design_scores_gemma":[0.0000024559647,0.000039736347,0.9977951,0.0000027793867,0.000004843136,0.00023284851,0.00012416692,0.00090858754,0.00063843007,0.000018345667,0.0002295192,0.0000030562003],"about_ca_topic_score_codex":0.0025004619,"about_ca_topic_score_gemma":0.0037825722,"teacher_disagreement_score":0.0025004619,"about_ca_system_score_codex":0.00017236944,"about_ca_system_score_gemma":0.000073593095,"threshold_uncertainty_score":0.004971862},"labels":[],"label_agreement":null},{"id":"W2470608361","doi":"10.1002/2016gl068097","title":"Long‐term variability of surface nutrient concentrations in the North Pacific","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"Division of Ocean Sciences; Japan Agency for Marine-Earth Science and Technology; Japan Society for the Promotion of Science; Fisheries and Oceans Canada","keywords":"Subarctic climate; Pacific decadal oscillation; Nutrient; Ocean gyre; Oceanography; Environmental science; Pacific ocean; North Pacific High; Geology; Nitrate; Climatology; Biology; Ecology","score_opus":0.02641457141480499,"score_gpt":0.2611895620488298,"score_spread":0.23477499063402482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2470608361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993352,0.00008318664,0.00006829974,0.000030946678,0.0000029035955,6.620557e-7,0.00019723023,0.0000036209137,0.00027796792],"genre_scores_gemma":[0.9993229,0.00006953494,0.000059605514,0.000007761855,0.0000049114133,0.000002219309,0.0003960019,0.0000014197875,0.00013569975],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992263,0.000012134809,0.0000059822055,0.00002889956,0.000017074579,0.000013303911],"domain_scores_gemma":[0.9995654,0.00008041082,0.0001244672,0.00003336658,0.00014390198,0.000052344385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028447292,0.00010749687,0.00015717107,0.0003926153,0.00022894656,0.00037720127,0.00013759203,0.00020074636,0.00036467696],"category_scores_gemma":[0.0007524926,0.00011828295,0.00014464595,0.0005786063,0.00024909474,0.00031495342,0.00030387106,0.00019736917,0.00009810558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007802912,0.000017282939,0.98822254,0.00001692188,0.00010125019,0.00012095789,0.0002095611,0.0011590188,0.004707413,0.0000370192,0.00028290658,0.0050471774],"study_design_scores_gemma":[5.9087307e-7,0.0000047199915,0.9993506,0.0000018885197,0.0000054866496,0.000018201155,0.000051276988,0.00035186697,0.000080581056,0.0000076766755,0.00012573393,0.0000014773934],"about_ca_topic_score_codex":0.027984222,"about_ca_topic_score_gemma":0.043989204,"teacher_disagreement_score":0.027984222,"about_ca_system_score_codex":0.00035779344,"about_ca_system_score_gemma":0.00022719582,"threshold_uncertainty_score":0.055642664},"labels":[],"label_agreement":null},{"id":"W2472931104","doi":"10.1002/2016gl069109","title":"Oxidation of manganese in an ancient aquifer, Kimberley formation, Gale crater, Mars","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geochemistry and Elemental Analysis","field":"Earth and Planetary Sciences","cited_by":147,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; University of New Brunswick; University of Guelph","funders":"Canadian Space Agency; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Geology; Evaporite; Impact crater; Geochemistry; Astrobiology; Manganese; Atmosphere (unit); Meteorite; Earth (classical element); Deposition (geology); Mineralogy; Paleontology; Sedimentary rock; Chemistry","score_opus":0.03196338841466855,"score_gpt":0.28457839500068766,"score_spread":0.2526150065860191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2472931104","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997093,0.000033607055,0.000021692138,0.000008654249,5.1887423e-7,0.0000014351656,0.000051939365,0.0000037845816,0.00016905484],"genre_scores_gemma":[0.9996105,0.00004074697,0.00011461965,0.000007252335,0.0000012480075,0.0000011745499,0.0000650483,0.000001811789,0.00015764097],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999248,0.000008499642,0.0000035997093,0.000029832181,0.000017059008,0.000016304059],"domain_scores_gemma":[0.9999378,0.000007857088,0.000015899206,0.0000056620447,0.000018546441,0.000014259636],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012025544,0.0002943234,0.00022340594,0.0013684272,0.0012017459,0.0005456299,0.00040197853,0.00036730425,0.00046763197],"category_scores_gemma":[0.00017110887,0.00023061904,0.00013711909,0.00066681736,0.0006308937,0.00024446205,0.00049173285,0.00014590875,0.00010155514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004396404,0.00006986141,0.8681387,0.00008120737,0.00013384658,0.0015861037,0.0029738068,0.0008932381,0.11478792,0.00015458997,0.00023651714,0.010504617],"study_design_scores_gemma":[0.00000980708,0.000064169515,0.99298275,0.0000058963674,0.000019282108,0.00034843705,0.00089162245,0.0006079502,0.004102813,0.00003057824,0.00093160593,0.0000050758367],"about_ca_topic_score_codex":0.040779065,"about_ca_topic_score_gemma":0.06786538,"teacher_disagreement_score":0.040779065,"about_ca_system_score_codex":0.0008764618,"about_ca_system_score_gemma":0.00031968905,"threshold_uncertainty_score":0.08108342},"labels":[],"label_agreement":null},{"id":"W2473004929","doi":"10.1002/2016gl069918","title":"Direct injection of water vapor into the stratosphere by volcanic eruptions","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Stratosphere; Volcano; Microwave Limb Sounder; Atmospheric sciences; Plume; Water vapor; Environmental science; Geology; Vulcanian eruption; Troposphere; Mixing ratio; Climatology; Meteorology; Seismology; Physics","score_opus":0.018914895665442265,"score_gpt":0.26739067858380505,"score_spread":0.24847578291836278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2473004929","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988545,0.000078049525,0.00034210028,0.000010803503,0.0000030859355,0.0000029486582,0.00006113495,0.000018349774,0.0006290822],"genre_scores_gemma":[0.9996928,0.000028622122,0.00010461583,0.0000032104463,0.0000029334747,0.0000010608607,0.000051654766,0.0000016745772,0.00011340172],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.0000038066307,0.0000014975948,0.000011450816,0.000009816714,0.000013888998],"domain_scores_gemma":[0.99992526,0.000021275791,0.000025005183,0.0000062590684,0.000009637591,0.0000125541055],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006497195,0.00012970985,0.00013008689,0.0002783373,0.0001361382,0.0002463167,0.00013073863,0.0001419148,0.0006837757],"category_scores_gemma":[0.00015737067,0.00008895199,0.00011424815,0.00016920976,0.00016214798,0.00022436309,0.00021752159,0.0002042191,0.000068892434],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052816654,0.000109939254,0.2698556,0.00007736461,0.00012822225,0.00082376006,0.00030345996,0.002029005,0.7030908,0.00030061294,0.00026155516,0.022491507],"study_design_scores_gemma":[0.000021935479,0.0003455386,0.81463295,0.000013745093,0.00006549005,0.00022418829,0.0002274008,0.018547533,0.16414082,0.00020640335,0.0015628409,0.000011147528],"about_ca_topic_score_codex":0.002113004,"about_ca_topic_score_gemma":0.0025289345,"teacher_disagreement_score":0.002113004,"about_ca_system_score_codex":0.00017106302,"about_ca_system_score_gemma":0.00006405799,"threshold_uncertainty_score":0.0042013526},"labels":[],"label_agreement":null},{"id":"W2476854040","doi":"10.1002/2016gl069333","title":"Contributions of growth and deformation to monthly variability in sea ice thickness north of the coasts of Greenland and the Canadian Arctic Archipelago","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Archipelago; Geology; Sea ice; Arctic ice pack; Arctic; Climatology; Groenlandia; Greenland ice sheet; Oceanography; Ice sheet","score_opus":0.009987923937812657,"score_gpt":0.2292750219612278,"score_spread":0.21928709802341512,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2476854040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980546,0.00010194499,0.00008370377,0.000053292908,0.0000046846594,0.000002961913,0.0011269146,0.000014364522,0.00055770326],"genre_scores_gemma":[0.9988501,0.000049401027,0.00007788307,0.000010235863,0.0000026914245,0.0000019276245,0.0008327501,0.0000059311287,0.0001689782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980694,0.000018946155,0.000011043356,0.000054683416,0.000043468805,0.00006482802],"domain_scores_gemma":[0.9994205,0.000085823944,0.0000889768,0.00003564892,0.0002428683,0.00012613078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005108334,0.0003596149,0.00020698318,0.0014725751,0.0006063863,0.00082874857,0.00030400837,0.00018713676,0.0006953392],"category_scores_gemma":[0.0012477101,0.00020195259,0.0004066006,0.0014879813,0.0004245858,0.00028743173,0.00043831376,0.00022437592,0.0000974161],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078148056,0.000010239635,0.9895928,0.0000095795895,0.000095673604,0.000040198334,0.00021472064,0.0016198269,0.0022226756,0.00009014451,0.00042062558,0.005605264],"study_design_scores_gemma":[6.259495e-7,0.0000012956413,0.9989196,0.0000017973828,0.0000048154157,0.0000055615337,0.000069886475,0.0008214454,0.000048376456,0.000009686009,0.0001144473,0.000002518502],"about_ca_topic_score_codex":0.8975131,"about_ca_topic_score_gemma":0.9335024,"teacher_disagreement_score":0.10248691,"about_ca_system_score_codex":0.0043008253,"about_ca_system_score_gemma":0.0030887537,"threshold_uncertainty_score":0.20618093},"labels":[],"label_agreement":null},{"id":"W2479659107","doi":"10.1002/2016gl069846","title":"Destabilization of glacial climate by the radiative impact of Atlantic Meridional Overturning Circulation disruptions","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"University of Toronto; Compute Canada","keywords":"Deglaciation; Climatology; Geology; Shutdown of thermohaline circulation; Oceanography; Climate model; Stadial; Climate change; Glacial period; Thermohaline circulation; North Atlantic Deep Water; Holocene; Geomorphology","score_opus":0.031462720292197155,"score_gpt":0.32240815162578496,"score_spread":0.2909454313335878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2479659107","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981346,0.00004872932,0.0005407968,0.00014143878,0.00003125611,0.000004277065,0.000110184155,0.000037672522,0.0009509494],"genre_scores_gemma":[0.99969697,0.000023466584,0.00010396788,0.000019979334,0.000005401043,0.0000021575622,0.00004932376,0.0000068595446,0.000091992624],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999187,0.000022146967,0.0000058556548,0.000018831035,0.000008389038,0.000026115322],"domain_scores_gemma":[0.9998598,0.00003072613,0.000031698488,0.000023077464,0.000014482152,0.000040143892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029935536,0.00036784966,0.00034264082,0.00016053357,0.00048882415,0.00092119625,0.0002923512,0.00047358903,0.0011409161],"category_scores_gemma":[0.00091409485,0.00020884587,0.0005429384,0.00016445888,0.00062685815,0.0004929108,0.0005713214,0.0005971256,0.000075520584],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037038393,0.00014320553,0.18604319,0.00006858775,0.00061177614,0.00045896054,0.0001936045,0.7866154,0.01645264,0.0027568664,0.0016397447,0.0046456885],"study_design_scores_gemma":[0.00020136857,0.0003188115,0.15370399,0.00001587481,0.0002258904,0.000119309894,0.0003255579,0.83761084,0.0031166691,0.0023825539,0.0019337165,0.000045408524],"about_ca_topic_score_codex":0.016042639,"about_ca_topic_score_gemma":0.013224415,"teacher_disagreement_score":0.016042639,"about_ca_system_score_codex":0.00064210384,"about_ca_system_score_gemma":0.00059890305,"threshold_uncertainty_score":0.03189856},"labels":[],"label_agreement":null},{"id":"W2483564506","doi":"10.1002/2016gl069688","title":"The abandoned ice sheet base at Camp Century, Greenland, in a warming climate","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"U.S. Army Corps of Engineers; University of Colorado Boulder","keywords":"Greenland ice sheet; Ice sheet; Nuclear decommissioning; Snow; Ice-sheet model; Climate change; Ice caps; Geology; Global warming; Earth science; Physical geography; Climatology; Oceanography; Cryosphere; Glacier; Ice shelf; Geography; Paleontology; Geomorphology; Sea ice; Engineering","score_opus":0.036269523376272914,"score_gpt":0.27586990443482323,"score_spread":0.2396003810585503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2483564506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964734,0.000054091244,0.000029665602,0.0002628895,0.0000065300683,0.000003258152,0.00018313322,0.0000032396547,0.00298382],"genre_scores_gemma":[0.9979691,0.00007158759,0.0001223816,0.00009764597,0.0000030803078,0.0000022961087,0.00018540396,0.0000029586947,0.0015455547],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999113,0.000011499312,0.0000014651613,0.0000144379,0.000018379038,0.00004297116],"domain_scores_gemma":[0.99989104,0.000011366215,0.00002644252,0.000008633234,0.000017718385,0.000044780278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023064896,0.00013545618,0.00013128869,0.0003262995,0.0023416972,0.0009679856,0.00033551626,0.0004280852,0.0009792579],"category_scores_gemma":[0.00016874219,0.00010307961,0.00009745169,0.00047179303,0.0013146744,0.0004183869,0.0010913064,0.00047289726,0.000093382056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017170144,0.00045766163,0.8467925,0.000117600575,0.00010777575,0.026623776,0.020896444,0.006947843,0.027248364,0.009757923,0.013935932,0.045397125],"study_design_scores_gemma":[0.000035300203,0.00017459768,0.9315964,0.0000611685,0.000027813901,0.0009141392,0.0360116,0.0021512124,0.0025375786,0.0013205468,0.02514485,0.000024883762],"about_ca_topic_score_codex":0.300934,"about_ca_topic_score_gemma":0.6913978,"teacher_disagreement_score":0.300934,"about_ca_system_score_codex":0.0041423216,"about_ca_system_score_gemma":0.0026343411,"threshold_uncertainty_score":0.5983647},"labels":[],"label_agreement":null},{"id":"W2485158535","doi":"10.1002/2016gl069946","title":"SMAP soil moisture drying more rapid than observed in situ following rainfall events","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Moisture and Remote Sensing","field":"Environmental Science","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Agriculture and Agri-Food Canada; University of Guelph","funders":"Canadian Space Agency; Agricultural Research Service; Goddard Space Flight Center; Environment Canada; U.S. Department of Agriculture; National Aeronautics and Space Administration","keywords":"In situ; Environmental science; Water content; Moisture; Soil science; Atmospheric sciences; Meteorology; Geology; Geotechnical engineering","score_opus":0.03578605675179609,"score_gpt":0.2915422725231582,"score_spread":0.2557562157713621,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2485158535","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99839276,0.000024853662,0.0006986221,0.0000067294804,0.0000021992523,0.000003295715,0.00034652956,0.00003526359,0.00048982934],"genre_scores_gemma":[0.99923646,0.000019263658,0.0003253931,0.000007253563,0.0000023593582,0.000004347573,0.00030175873,0.000005833657,0.000097358534],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991226,0.000009761284,0.0000051946317,0.000040049403,0.0000187259,0.000014009182],"domain_scores_gemma":[0.9996124,0.00009757254,0.00015189778,0.000046469882,0.000056040284,0.000035617806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023588334,0.0001545902,0.00018045558,0.0003520816,0.00014599838,0.00026138985,0.00016523694,0.00018490653,0.0008836333],"category_scores_gemma":[0.0007590305,0.00012427311,0.00014175223,0.0003225564,0.0001029261,0.0003879973,0.00016063172,0.00023397738,0.00014518583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038648347,0.000120824814,0.74909747,0.00008946081,0.00015165251,0.00020075313,0.0002695199,0.0029686245,0.22983019,0.0001332581,0.00050198124,0.01624986],"study_design_scores_gemma":[0.0000046251366,0.000052503587,0.97754943,0.000002947681,0.000014647284,0.000102263344,0.00006971681,0.004802715,0.016875813,0.000054290373,0.0004654753,0.00000563382],"about_ca_topic_score_codex":0.0018403821,"about_ca_topic_score_gemma":0.0020918755,"teacher_disagreement_score":0.0018403821,"about_ca_system_score_codex":0.00013437799,"about_ca_system_score_gemma":0.00006832911,"threshold_uncertainty_score":0.003659308},"labels":[],"label_agreement":null},{"id":"W2488428319","doi":"10.1002/2016gl070428","title":"Giant natural fluctuation models and anthropogenic warming","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Complex Systems and Time Series Analysis","field":"Economics, Econometrics and Finance","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Climate change; Global warming; Series (stratigraphy); Natural (archaeology); Climatology; Environmental science; Econometrics; Climate system; Atmospheric sciences; Mathematics; Geography; Geology; Oceanography","score_opus":0.06444614220587418,"score_gpt":0.2886197707362916,"score_spread":0.2241736285304174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2488428319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.66978717,0.0031259912,0.26175505,0.015034748,0.00053145527,0.000024738554,0.00065499346,0.0008068767,0.048279002],"genre_scores_gemma":[0.9964005,0.00033754722,0.0014185635,0.000105842744,0.000084179104,0.000010674854,0.000089988425,0.000026174988,0.0015266064],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"not_applicable","domain_scores_codex":[0.99977165,0.000121344754,0.000007571025,0.000038602855,0.000031724783,0.000029122823],"domain_scores_gemma":[0.9984908,0.0009664164,0.00024383143,0.00008449031,0.00012714768,0.00008735017],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010249316,0.00031691603,0.00029661556,0.0006313457,0.0003153028,0.00079309667,0.0004550274,0.000557597,0.0015115041],"category_scores_gemma":[0.0053505823,0.00011222854,0.00042188625,0.00053186493,0.0009899952,0.00086301274,0.00067108654,0.0005726775,0.000111123496],"study_design_candidate":"not_applicable","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003411687,0.000021391366,0.009834212,0.00003865601,0.00006322218,0.00020553338,0.00015981878,0.38876915,0.00033199377,0.58533794,0.0056746714,0.009529206],"study_design_scores_gemma":[0.0000060867774,0.000009850085,0.0022629835,0.0000116668725,0.000008831875,0.000043818734,0.00003390098,0.72652817,0.000059379938,0.26908526,0.00194188,0.000008247403],"about_ca_topic_score_codex":0.005599672,"about_ca_topic_score_gemma":0.0027874266,"teacher_disagreement_score":0.005599672,"about_ca_system_score_codex":0.0007500341,"about_ca_system_score_gemma":0.00034578107,"threshold_uncertainty_score":0.011134148},"labels":[],"label_agreement":null},{"id":"W2497279828","doi":"10.1002/2016gl068965","title":"Small global effect on terrestrial net primary production due to increased fossil fuel aerosol emissions from East Asia since the turn of the century","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Biological and Environmental Research; Oak Ridge National Laboratory; Sight Research UK; Université Laval; Microsoft Research; Natural Environment Research Council; U.S. Department of Energy; National Science Foundation","keywords":"Fossil fuel; Aerosol; Environmental science; Sink (geography); Primary production; Atmospheric sciences; Atmospheric carbon cycle; Carbon sink; Carbon fibers; Earth science; Carbon sequestration; Carbon dioxide; Climate change; Ecology; Meteorology; Geology; Oceanography; Ecosystem; Geography; Biology","score_opus":0.014136490431068634,"score_gpt":0.23979945138890793,"score_spread":0.2256629609578393,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2497279828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924776,0.0008552341,0.00073164754,0.00045808303,0.00003350335,0.0000061562437,0.0006073522,0.000042983636,0.0047875247],"genre_scores_gemma":[0.9989336,0.00027519878,0.00014361474,0.00009565455,0.000015437492,0.0000025390336,0.00022507491,0.000009725966,0.00029908633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998431,0.000026731357,0.000012795402,0.000055829576,0.000023463728,0.000038110058],"domain_scores_gemma":[0.99933916,0.00021924853,0.00018276759,0.000080704805,0.00010114391,0.00007701736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005816921,0.00044831942,0.00033172645,0.00030158376,0.00020807644,0.00077432476,0.00024482896,0.00033541233,0.0033979234],"category_scores_gemma":[0.00094451505,0.00018984209,0.00084853225,0.00040652562,0.00048122177,0.00061159587,0.0007239487,0.00042109133,0.0002572619],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006480101,0.000083380466,0.90365833,0.00047510955,0.0011079229,0.00084861246,0.00019746764,0.036159504,0.032582723,0.0023597197,0.0008399737,0.02103922],"study_design_scores_gemma":[0.00003591653,0.0001429023,0.98297036,0.000028979497,0.00051986525,0.00018036173,0.00021694429,0.008374113,0.0049334564,0.0008646727,0.0017140385,0.000018436729],"about_ca_topic_score_codex":0.009474877,"about_ca_topic_score_gemma":0.007710467,"teacher_disagreement_score":0.009474877,"about_ca_system_score_codex":0.00063899194,"about_ca_system_score_gemma":0.00036861704,"threshold_uncertainty_score":0.018839419},"labels":[],"label_agreement":null},{"id":"W2500520687","doi":"10.1002/2016gl070114","title":"Long‐range transport of NH<sub>3</sub>, CO, HCN, and C<sub>2</sub>H<sub>6</sub> from the 2014 Canadian Wildfires","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Eurostars; Canadian Space Agency; National Oceanic and Atmospheric Administration; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Vrije Universiteit Amsterdam; Government of Canada; National Aeronautics and Space Administration","keywords":"Moderate-resolution imaging spectroradiometer; Atmospheric sciences; Arctic; Environmental science; Atmosphere (unit); Carbon monoxide; Boreal; Ammonia; The arctic; Meteorology; Climatology; Chemistry; Geology; Physics; Oceanography; Catalysis","score_opus":0.010160289753775023,"score_gpt":0.22220622904724968,"score_spread":0.21204593929347465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2500520687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960078,0.00019641651,0.00026222467,0.000096161195,0.000012148757,0.000008150551,0.0011781057,0.000024953104,0.0022140725],"genre_scores_gemma":[0.996968,0.00024090627,0.00047037788,0.000045759225,0.000007600427,0.0000055948854,0.0011205818,0.00000809834,0.0011331028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986875,0.0000029834991,0.000002641704,0.000021713378,0.00005646166,0.000047392426],"domain_scores_gemma":[0.9998299,0.0000078831845,0.000021538903,0.000005413741,0.00010763671,0.000027602746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016572925,0.00032601436,0.00017349269,0.00041108183,0.0016235798,0.00068569387,0.00032060806,0.00021980518,0.0006308874],"category_scores_gemma":[0.00017627071,0.00020558594,0.00022809244,0.0005006305,0.0003448241,0.0002572587,0.00035368514,0.00036872775,0.000092297916],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040248712,0.00009026863,0.83842784,0.00010526463,0.00024343145,0.00066025666,0.0008926229,0.0054450533,0.12338431,0.0003266426,0.0035070363,0.026514793],"study_design_scores_gemma":[0.000008444966,0.000025783547,0.983832,0.000015839325,0.000045034336,0.00005334889,0.0005028754,0.0025726787,0.009864305,0.00005308468,0.0030035768,0.000023014367],"about_ca_topic_score_codex":0.9450451,"about_ca_topic_score_gemma":0.97813785,"teacher_disagreement_score":0.054954886,"about_ca_system_score_codex":0.006606828,"about_ca_system_score_gemma":0.005007751,"threshold_uncertainty_score":0.11055702},"labels":[],"label_agreement":null},{"id":"W2500703720","doi":"10.1002/2016gl069558","title":"Subglacial bed form morphology controlled by ice speed and sediment thickness","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Western Canada Research Grid; Durham University; Compute Canada; Lunds Universitet; University of Calgary","keywords":"Geology; Geomorphology; Moraine; Lineation; Bedform; Ice stream; Drumlin; Glacier; Sediment; Ice sheet; Sediment transport; Geophysics; Sea ice; Paleontology; Cryosphere; Oceanography","score_opus":0.024095892649553755,"score_gpt":0.28604459609609034,"score_spread":0.2619487034465366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2500703720","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986524,0.00001106456,0.000559043,0.00001838705,0.0000022023453,0.000001732144,0.000042685417,0.000018360119,0.00069427845],"genre_scores_gemma":[0.9997019,0.000010625862,0.00009685432,0.0000036019972,4.893255e-7,0.0000019121492,0.00002431716,0.0000035298767,0.00015674837],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99997103,0.0000050028016,0.0000010557234,0.00000770254,0.0000021290352,0.000013031901],"domain_scores_gemma":[0.99992144,0.00002225524,0.000014232505,0.000008193705,0.000006150711,0.000027735978],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010965582,0.00021201915,0.00020484999,0.00014607985,0.00021582963,0.0005168139,0.00024491278,0.00024111137,0.001564724],"category_scores_gemma":[0.00027264937,0.00018408395,0.00033464338,0.000096667936,0.00040362813,0.00026390274,0.00024999338,0.00018776323,0.000111294015],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040032555,0.00016766344,0.07018088,0.000043885866,0.00010621317,0.00022883614,0.00014987175,0.8801085,0.039315563,0.0043027434,0.0005715816,0.004424049],"study_design_scores_gemma":[0.00005146998,0.00009804383,0.030879818,0.0000050701424,0.00003438388,0.000031052346,0.00008906294,0.96572065,0.0018214755,0.0010317855,0.00022216114,0.000014982461],"about_ca_topic_score_codex":0.012455382,"about_ca_topic_score_gemma":0.00847155,"teacher_disagreement_score":0.012455382,"about_ca_system_score_codex":0.00055382913,"about_ca_system_score_gemma":0.000365723,"threshold_uncertainty_score":0.02476573},"labels":[],"label_agreement":null},{"id":"W2509336587","doi":"10.1002/2016gl070066","title":"Rapid reinflation following the 2011–2012 rhyodacite eruption at Cordón Caulle volcano (Southern Andes) imaged by InSAR: Evidence for magma reservoir refill","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; Science Mission Directorate; Comisión Nacional de Investigación Científica y Tecnológica; U.S. Geological Survey; National Aeronautics and Space Administration","keywords":"Geology; Volcano; Effusive eruption; Lateral eruption; Magma; Interferometric synthetic aperture radar; Lava; Seismology; Silicic; Phreatic eruption; Subsidence; Explosive eruption; Geomorphology; Synthetic aperture radar; Remote sensing","score_opus":0.06710667966637987,"score_gpt":0.29876295742793973,"score_spread":0.23165627776155986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2509336587","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977028,0.000096492,0.00006400959,0.000082955754,0.000009972987,0.0000057934353,0.0003745035,0.000037727248,0.0016257261],"genre_scores_gemma":[0.99910563,0.00004577611,0.00012969051,0.000021437017,0.000009235506,0.000003098163,0.00036491654,0.000007115625,0.00031304857],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998932,0.0000042686856,0.0000045014044,0.00002722441,0.00003107788,0.00003962579],"domain_scores_gemma":[0.99963987,0.000029221776,0.0001064391,0.000030327446,0.00012668472,0.00006750162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022751774,0.00021805175,0.00019531997,0.00095481717,0.0006029219,0.000627889,0.00039601512,0.00044266786,0.0014497312],"category_scores_gemma":[0.00051823753,0.00016301378,0.00013092838,0.00065538177,0.0003721859,0.00030019076,0.00041855863,0.0003715076,0.00022532846],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026515184,0.00007639942,0.95110196,0.00004743494,0.000061537656,0.0011361188,0.0007020208,0.0006249005,0.029934913,0.00016908717,0.001989335,0.013891022],"study_design_scores_gemma":[0.0000035862904,0.0000067662945,0.9980363,0.0000046835553,0.0000065748814,0.000048542246,0.00010560843,0.00066650566,0.00055040966,0.000007228722,0.00056073803,0.0000029621692],"about_ca_topic_score_codex":0.14340347,"about_ca_topic_score_gemma":0.25780776,"teacher_disagreement_score":0.14340347,"about_ca_system_score_codex":0.0010136102,"about_ca_system_score_gemma":0.00053255126,"threshold_uncertainty_score":0.28513753},"labels":[],"label_agreement":null},{"id":"W2513355907","doi":"10.1002/2016gl069755","title":"Tectonic tremor on Vancouver Island, Cascadia, modulated by the body and surface waves of the <i>M<sub>w</sub></i> 8.6 and 8.2, 2012 East Indian Ocean earthquakes","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Seismology; Geology; Subduction; Tectonics; Episodic tremor and slip; Tsunami wave; Slip (aerodynamics); Plate tectonics; Seismic wave; Indian ocean; Surface wave; Modulation (music); Oceanography; Physics","score_opus":0.01349101572858114,"score_gpt":0.22360118370808893,"score_spread":0.2101101679795078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2513355907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835074,0.000031463274,0.000012627104,0.00003083663,0.000002649247,0.0000035519136,0.00023326941,0.0000069727844,0.0013279034],"genre_scores_gemma":[0.9991239,0.000055754044,0.00002520549,0.0000068938216,0.0000023270986,0.000003161246,0.00021403938,0.0000017990606,0.0005668713],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.0000039114175,0.0000034363113,0.000015106179,0.000021603611,0.000016941205],"domain_scores_gemma":[0.9997855,0.000011515455,0.00003667836,0.000008244123,0.000073181014,0.0000849224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006274089,0.00028466093,0.00018373008,0.000604833,0.00074671605,0.00045956933,0.0002649803,0.00028130418,0.0014314892],"category_scores_gemma":[0.00040405255,0.00018538247,0.00011286366,0.00066297915,0.00031608864,0.00010919024,0.0005449605,0.0002503619,0.00026891605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000559094,0.00012938559,0.91181165,0.00012497441,0.00013025856,0.0018717169,0.0019894135,0.002721001,0.05788164,0.000108267894,0.0026496057,0.020023042],"study_design_scores_gemma":[0.0000054394063,0.000017939989,0.99891055,0.00000379902,0.0000082372235,0.000036510908,0.00023846985,0.0003079617,0.00018359917,0.000008570602,0.0002750481,0.0000038225626],"about_ca_topic_score_codex":0.486215,"about_ca_topic_score_gemma":0.7363471,"teacher_disagreement_score":0.513785,"about_ca_system_score_codex":0.0013741172,"about_ca_system_score_gemma":0.0009877689,"threshold_uncertainty_score":0.9667698},"labels":[],"label_agreement":null},{"id":"W2514477882","doi":"10.1002/2016gl068713","title":"The grain size gap and abrupt gravel‐sand transitions in rivers due to suspension fallout","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Bed load; Grain size; Geology; Silt; Sediment transport; Fluvial; Sediment; Suspension (topology); Geotechnical engineering; Hydrology (agriculture); Geomorphology","score_opus":0.02070579577006133,"score_gpt":0.2812805481438736,"score_spread":0.2605747523738123,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2514477882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99971753,0.000012573962,0.000112425245,0.000007385889,5.848815e-7,9.216038e-7,0.000015472522,0.000009756768,0.00012331177],"genre_scores_gemma":[0.9999144,0.0000027950985,0.00003314499,0.0000030258152,4.890647e-7,9.765528e-7,0.000015900472,0.0000011975146,0.00002809483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000006022339,0.000004608021,0.000017884406,0.000011949493,0.000028114231],"domain_scores_gemma":[0.9996537,0.00007385872,0.00014641401,0.000029384124,0.000019913794,0.000076704884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010327836,0.00008850693,0.00020255697,0.0003211027,0.00025762565,0.00043792682,0.00016506277,0.00026796677,0.0008120888],"category_scores_gemma":[0.0004407823,0.00013723015,0.00011331398,0.00016989751,0.00051785633,0.00021051742,0.0005815787,0.0003151087,0.00009334351],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012772006,0.00028841567,0.6143004,0.000058673926,0.00008531659,0.0024548694,0.00072465173,0.0038297647,0.36179537,0.001714962,0.0004679257,0.013002409],"study_design_scores_gemma":[0.000013004326,0.00013759751,0.98355097,0.0000040343425,0.0000086628315,0.00048253872,0.0002911284,0.004678106,0.009835254,0.0008167125,0.00017187162,0.000010111624],"about_ca_topic_score_codex":0.0013119802,"about_ca_topic_score_gemma":0.0013716017,"teacher_disagreement_score":0.0013119802,"about_ca_system_score_codex":0.00029798146,"about_ca_system_score_gemma":0.00011019072,"threshold_uncertainty_score":0.0027166605},"labels":[],"label_agreement":null},{"id":"W2515581021","doi":"10.1002/2016gl070612","title":"On the origin of the ionosphere at the Moon using results from Chandrayaan‐1 S band radio occultation experiment and a photochemical model","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Ionosphere; Radio occultation; Ionization; Physics; Ion; Occultation; Electron density; Exosphere; Solar wind; Proton; Atmosphere (unit); Atomic physics; Electron; Plasma; Geophysics; Astronomy; Meteorology","score_opus":0.06261354480638642,"score_gpt":0.30613413087678276,"score_spread":0.24352058607039634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2515581021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961637,0.00036981393,0.0007304632,0.00004521968,0.0000049536784,0.000008994169,0.0004916819,0.000065656845,0.0021193533],"genre_scores_gemma":[0.9990501,0.00010287401,0.0003674796,0.0000066061725,0.0000019416536,0.0000054162965,0.00031922647,0.000009065288,0.00013735678],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991953,0.00001548412,0.0000030075364,0.000024694335,0.000020580457,0.000016722874],"domain_scores_gemma":[0.9997019,0.00015900983,0.000032544147,0.000034997312,0.000044173295,0.0000272616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029915993,0.00038141425,0.00030156536,0.00051017257,0.0003225693,0.0004736653,0.00028825557,0.00025955413,0.00082590105],"category_scores_gemma":[0.00045748663,0.0001548159,0.0004712685,0.00032819918,0.00020203715,0.00038008305,0.00028889798,0.00019720627,0.0001422162],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0033926629,0.0002115042,0.65655816,0.00041956425,0.0005131303,0.00074102415,0.00037947725,0.077532984,0.22922923,0.0032919303,0.0012822318,0.026448037],"study_design_scores_gemma":[0.00016113587,0.00024421734,0.8436861,0.00003290027,0.00024660007,0.0002138371,0.00017956062,0.10358138,0.04857793,0.0008087232,0.0022073037,0.000060323924],"about_ca_topic_score_codex":0.024426037,"about_ca_topic_score_gemma":0.017677993,"teacher_disagreement_score":0.024426037,"about_ca_system_score_codex":0.0008230492,"about_ca_system_score_gemma":0.00028223204,"threshold_uncertainty_score":0.048567712},"labels":[],"label_agreement":null},{"id":"W2516965707","doi":"10.1002/2016gl069922","title":"Phytoplankton blooms weakly influence the cloud forming ability of sea spray aerosol","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Aerosol; Cloud condensation nuclei; Sea spray; Phytoplankton; Environmental science; Algal bloom; Algae; Oceanography; Biogeochemistry; Seawater; Dimethyl sulfide; Bloom; Sea salt aerosol; Atmospheric sciences; Cloud physics; Environmental chemistry; Chemistry; Nutrient; Meteorology; Sea salt; Ecology; Biology; Cloud computing; Geology; Physics","score_opus":0.021240533543139657,"score_gpt":0.2680881832497809,"score_spread":0.24684764970664125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2516965707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99854904,0.000101725636,0.00033835604,0.000014273266,0.000004675177,0.000009464043,0.00009848751,0.00001024851,0.000873743],"genre_scores_gemma":[0.9993826,0.000044724948,0.00017540394,0.000017035829,0.0000011639178,0.000005262933,0.000058854406,0.0000040606865,0.0003108488],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999163,0.000014869402,0.0000063114844,0.000022638731,0.00001964926,0.000020171861],"domain_scores_gemma":[0.9997075,0.00010294603,0.000055932793,0.00003502258,0.000037686284,0.000060889004],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014409173,0.00019096788,0.00013366615,0.000074317795,0.00016585556,0.0003378132,0.00009953459,0.00011312958,0.00069161237],"category_scores_gemma":[0.00033119653,0.000120124445,0.00015373263,0.000047426332,0.00028049218,0.00015835451,0.00026969996,0.00027947352,0.000108649634],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012617289,0.000024717154,0.012955521,0.000017528659,0.000008391498,0.00002026474,0.000024024594,0.00026060065,0.9852969,0.000044929635,0.000017501065,0.0012035794],"study_design_scores_gemma":[0.000017505026,0.0006167752,0.20781918,0.00000718583,0.000028126338,0.00005344205,0.0001387062,0.0034744707,0.7865497,0.00014906883,0.001136449,0.000009412774],"about_ca_topic_score_codex":0.002132628,"about_ca_topic_score_gemma":0.0030290054,"teacher_disagreement_score":0.002132628,"about_ca_system_score_codex":0.00039890042,"about_ca_system_score_gemma":0.00021052845,"threshold_uncertainty_score":0.0042404532},"labels":[],"label_agreement":null},{"id":"W2517355480","doi":"10.1002/2016gl070008","title":"Fast modulations of pulsating proton aurora related to subpacket structures of Pc1 geomagnetic pulsations at subauroral latitudes","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"Athabasca University","keywords":"Physics; Proton; Amplitude; Cyclotron; Earth's magnetic field; Geomagnetic latitude; Geophysics; Computational physics; Electron; Astrophysics; Optics; Magnetic field; Nuclear physics","score_opus":0.01795769040604537,"score_gpt":0.30250643501290103,"score_spread":0.28454874460685564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2517355480","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977647,0.00012268453,0.00058350834,0.000010958117,0.0000039864435,0.0000045336146,0.000090956026,0.000024970244,0.0013936792],"genre_scores_gemma":[0.99922395,0.000056369416,0.00030102924,0.000005856589,0.0000059600716,0.0000050383537,0.00009204596,0.0000062104864,0.0003034513],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999747,0.0000024693047,0.0000011127344,0.0000072594203,0.0000075293206,0.0000070168935],"domain_scores_gemma":[0.9998622,0.00003401904,0.000042366224,0.000012609791,0.000022916805,0.000025951975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000614804,0.00011835865,0.00011730529,0.0004272753,0.00012819984,0.00022752467,0.00008120781,0.0001561392,0.0011750102],"category_scores_gemma":[0.00023113945,0.00010650106,0.0000832395,0.00023220568,0.00014444624,0.00015924196,0.00019951841,0.00023204763,0.0001571089],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045953906,0.000026972191,0.060584974,0.00010782838,0.000040613533,0.0005522469,0.00047483618,0.00052820746,0.91765344,0.0003148355,0.00026191742,0.018994607],"study_design_scores_gemma":[0.000006040665,0.00006052403,0.9687186,0.0000040747905,0.000013245362,0.00022131298,0.00010986757,0.0012400594,0.028885294,0.00007000444,0.00066360435,0.0000074453883],"about_ca_topic_score_codex":0.0005193274,"about_ca_topic_score_gemma":0.0008609557,"teacher_disagreement_score":0.0011750102,"about_ca_system_score_codex":0.000106513035,"about_ca_system_score_gemma":0.000042090658,"threshold_uncertainty_score":0.003930807},"labels":[],"label_agreement":null},{"id":"W2518151687","doi":"10.1002/2016gl070191","title":"High export of dissolved silica from the Greenland Ice Sheet","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":139,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Vlaamse regering; Fonds Wetenschappelijk Onderzoek","keywords":"Greenland ice sheet; Ice sheet; Geology; Ice core; Climatology; Oceanography; Earth science","score_opus":0.03470194281902746,"score_gpt":0.2806382662809321,"score_spread":0.2459363234619046,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2518151687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993093,0.000039818595,0.00001767799,0.000012237084,0.0000011298596,6.7632817e-7,0.0002589599,0.0000057715483,0.0003544864],"genre_scores_gemma":[0.99877065,0.000045627552,0.000074857824,0.000022598306,0.0000030858675,0.0000018006041,0.0006569468,0.000004813164,0.0004195361],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.00000196235,0.0000025248594,0.000014539141,0.000008260809,0.000011738458],"domain_scores_gemma":[0.99986994,0.000014761475,0.000048420912,0.000009548136,0.000025776382,0.00003159167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008603174,0.00029712755,0.00030171833,0.00044642366,0.00035680085,0.0008445869,0.00012372046,0.00016001351,0.00058153464],"category_scores_gemma":[0.000124232,0.00010385897,0.00012791874,0.00040446976,0.00029921584,0.0002554062,0.0003468802,0.0001651777,0.00010409216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043226295,0.000035952944,0.746404,0.00007841814,0.00013364664,0.00066721597,0.0007116797,0.0010094419,0.23967132,0.00017710235,0.0005410493,0.010138012],"study_design_scores_gemma":[0.0000023120708,0.000011908362,0.9972996,0.000002799378,0.00000712717,0.00003103454,0.00009396213,0.00023207418,0.0019519975,0.00001985847,0.000345075,0.000002280576],"about_ca_topic_score_codex":0.032777764,"about_ca_topic_score_gemma":0.051037747,"teacher_disagreement_score":0.032777764,"about_ca_system_score_codex":0.0009937836,"about_ca_system_score_gemma":0.0004170523,"threshold_uncertainty_score":0.065173924},"labels":[],"label_agreement":null},{"id":"W2518496520","doi":"10.1002/2016gl070421","title":"Poroelastic stress triggering of the December 2013 Crooked Lake, Alberta, induced seismicity sequence","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":177,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Induced seismicity; Poromechanics; Geology; Pore water pressure; Hydraulic fracturing; Coulomb; Seismology; Stress (linguistics); Sequence (biology); Geotechnical engineering; Physics; Porous medium","score_opus":0.053895171252366376,"score_gpt":0.2861689851266961,"score_spread":0.23227381387432972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2518496520","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976433,0.000029549166,0.00019526608,0.000044466513,0.000003557204,0.000015823409,0.00043868093,0.000038555263,0.0015907474],"genre_scores_gemma":[0.9990331,0.000024965771,0.0001043417,0.000006272747,0.0000010064796,0.0000037298444,0.00024612853,0.0000031305954,0.00057740015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.0000028561694,0.0000032133698,0.000010815027,0.000033497687,0.000023794366],"domain_scores_gemma":[0.9998679,0.000007657918,0.0000214996,0.000004397191,0.000057367655,0.000041246272],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009716645,0.0002233301,0.00013998456,0.000618482,0.0006273955,0.0005301117,0.00050454825,0.000321649,0.0013277782],"category_scores_gemma":[0.0004331919,0.00012887875,0.00011290929,0.0007434162,0.00048105046,0.000108396205,0.00032047083,0.000201673,0.00011619679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011107555,0.00026047774,0.81673956,0.00020353345,0.00013925093,0.003942966,0.001212088,0.079055406,0.059634585,0.0013129002,0.004377469,0.032011114],"study_design_scores_gemma":[0.000020549982,0.000032581298,0.9802822,0.000008561738,0.000015178379,0.000054217584,0.00047695008,0.01633611,0.0018606725,0.00006169132,0.0008384457,0.000012900705],"about_ca_topic_score_codex":0.86609805,"about_ca_topic_score_gemma":0.9402418,"teacher_disagreement_score":0.13390195,"about_ca_system_score_codex":0.005438863,"about_ca_system_score_gemma":0.0042928015,"threshold_uncertainty_score":0.269381},"labels":[],"label_agreement":null},{"id":"W2518704075","doi":"10.1002/2016gl069964","title":"An initial assessment of SMAP soil moisture retrievals using high‐resolution model simulations and in situ observations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Moisture and Remote Sensing","field":"Environmental Science","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Environmental science; Data assimilation; Forcing (mathematics); Water content; Boreal; Taiga; Radar; In situ; Climate model; Climatology; Remote sensing; Atmospheric sciences; Meteorology; Climate change; Geology","score_opus":0.07875328962845725,"score_gpt":0.36874138096792136,"score_spread":0.2899880913394641,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2518704075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928866,0.00006404067,0.0029853538,0.00015836529,0.00002411973,0.00007130504,0.0017488297,0.00041316368,0.0016482288],"genre_scores_gemma":[0.9946036,0.000030464844,0.003786024,0.000021815411,0.000008438259,0.000036457262,0.0012997633,0.000032825512,0.00018067072],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99956423,0.0001575982,0.000027533584,0.000088515844,0.00010107941,0.00006107008],"domain_scores_gemma":[0.99861085,0.00050294865,0.0001128111,0.0002281463,0.0004349071,0.00011032317],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030357318,0.0009791361,0.0005345846,0.0003547012,0.0006780706,0.00094701885,0.0009814734,0.00074881606,0.00087677164],"category_scores_gemma":[0.0027154258,0.00043671433,0.000558947,0.0005630782,0.00035461667,0.0011898703,0.00041255596,0.0006452051,0.00019595156],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021210737,0.0016453696,0.14120412,0.00018098712,0.0004385287,0.00027413023,0.00019917302,0.786259,0.028712723,0.0008838549,0.003640754,0.034440335],"study_design_scores_gemma":[0.0003130434,0.0006929236,0.058399796,0.00001726259,0.00006930039,0.000030744737,0.000090037094,0.9260525,0.012880042,0.00020214096,0.0012128105,0.00003934521],"about_ca_topic_score_codex":0.05714274,"about_ca_topic_score_gemma":0.03490172,"teacher_disagreement_score":0.05714274,"about_ca_system_score_codex":0.0014878474,"about_ca_system_score_gemma":0.000953068,"threshold_uncertainty_score":0.11362028},"labels":[],"label_agreement":null},{"id":"W2519167552","doi":"10.1002/2016gl070427","title":"Relocation of long‐period (LP) seismic events reveals en echelon fractures in the upper edifice of Turrialba volcano, Costa Rica","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"Consejo Nacional de Rectores; Science Foundation Ireland","keywords":"Geology; Volcano; Echelon formation; Seismology; Relocation; Joint (building); Shearing (physics); Fault (geology); Geotechnical engineering; Computer science","score_opus":0.024604067946953963,"score_gpt":0.30011295111814185,"score_spread":0.2755088831711879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2519167552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992855,0.000030196257,0.00019038883,0.0000118201315,0.0000010531962,0.00000442742,0.00013579837,0.0000143385905,0.00032655933],"genre_scores_gemma":[0.9995403,0.000011426428,0.00020868455,0.0000023695952,0.0000012831729,0.0000025107618,0.00016086768,0.0000019729423,0.000070704096],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999094,0.000015229871,0.000007292418,0.000029459245,0.000017172073,0.000021414606],"domain_scores_gemma":[0.99973065,0.000032774537,0.000087620836,0.000053389984,0.0000624721,0.00003314952],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020675537,0.00015461321,0.0001577968,0.0006030279,0.00021294905,0.00027532846,0.00027304215,0.00024039976,0.00033923678],"category_scores_gemma":[0.0005620844,0.00010010208,0.00014389648,0.0005509605,0.00024218112,0.00012813251,0.00035331145,0.00012193368,0.00008502645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030925052,0.000113810966,0.90121156,0.00008278321,0.00012683848,0.00091968983,0.0016943899,0.008816048,0.05033785,0.0002218233,0.00056987704,0.03559605],"study_design_scores_gemma":[0.0000046260075,0.000016773163,0.9946577,0.0000054536195,0.00001150426,0.00007867578,0.00027415593,0.0040177144,0.0006271704,0.000011903134,0.00029075428,0.000003683356],"about_ca_topic_score_codex":0.029500853,"about_ca_topic_score_gemma":0.06389388,"teacher_disagreement_score":0.029500853,"about_ca_system_score_codex":0.00033251423,"about_ca_system_score_gemma":0.00022886819,"threshold_uncertainty_score":0.058658242},"labels":[],"label_agreement":null},{"id":"W2520299185","doi":"10.1002/2016gl070333","title":"Observational evidence of the nonlinear wave growth theory of plasmaspheric hiss","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada","keywords":"Hiss; Amplitude; Physics; Nonlinear system; Equator; Computational physics; Waveform; Dispersion (optics); Dispersion relation; Geophysics; Quantum electrodynamics; Optics; Quantum mechanics","score_opus":0.057508467442787224,"score_gpt":0.2980882304053094,"score_spread":0.24057976296252218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2520299185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926018,0.000047197453,0.0035682493,0.00010131911,0.0000041936405,0.000009234571,0.00009156893,0.00004212458,0.0035343126],"genre_scores_gemma":[0.9995235,0.000014029067,0.0003259435,0.0000031512568,0.0000040291275,0.0000016857846,0.000044810073,0.0000025844836,0.00008019876],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983823,0.00003055744,0.000008066041,0.000035266246,0.00007011317,0.000017679587],"domain_scores_gemma":[0.9983706,0.00074764184,0.0002818431,0.0002467411,0.00024256943,0.000110707944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006245206,0.00019301708,0.0001110306,0.00043969892,0.00029466988,0.00038518407,0.0002722343,0.00026661207,0.00068773935],"category_scores_gemma":[0.002209341,0.00016119007,0.0001451039,0.0002477631,0.00068766833,0.00047977833,0.0004344116,0.00031109477,0.00013529754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060190394,0.00011360787,0.74142474,0.00013730046,0.000102384816,0.00056639337,0.0011323573,0.024168788,0.16356815,0.028830681,0.00087999593,0.038473647],"study_design_scores_gemma":[0.000051279876,0.00022993553,0.8685192,0.000019026502,0.00003153885,0.00044164824,0.00033849868,0.10443518,0.0158855,0.00799724,0.0020165795,0.000034533266],"about_ca_topic_score_codex":0.0025535296,"about_ca_topic_score_gemma":0.0018844806,"teacher_disagreement_score":0.0025535296,"about_ca_system_score_codex":0.00040859138,"about_ca_system_score_gemma":0.00012216806,"threshold_uncertainty_score":0.0050773025},"labels":[],"label_agreement":null},{"id":"W2521012645","doi":"10.1002/2016gl070799","title":"Radar imaging of intense nonlinear Ekman divergence","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"Canadian Space Agency; National Oceanic and Atmospheric Administration; National Natural Science Foundation of China; Nanjing University of Information Science and Technology; Government of Jiangsu Province; Natural Science Foundation of Jiangsu Province; Startup Foundation for Introducing Talent of Nanjing University of Information Science and Technology; Marine Environmental Observation Prediction and Response Network","keywords":"Geology; Front (military); Sea surface temperature; Synthetic aperture radar; Ekman transport; Ocean dynamics; Backscatter (email); Radar; Gulf Stream; Divergence (linguistics); Geophysics; Ocean current; Climatology; Oceanography; Remote sensing","score_opus":0.025780321108624077,"score_gpt":0.27469114435531156,"score_spread":0.24891082324668748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521012645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98204273,0.0002764788,0.0135140885,0.00007925188,0.000014779726,0.000010709743,0.0001402434,0.000103969775,0.0038178025],"genre_scores_gemma":[0.99341714,0.00009509184,0.00603315,0.000029241548,0.000016286986,0.0000030982983,0.000078272205,0.000007279935,0.00032036894],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999485,0.000010574575,0.0000030166407,0.0000120697505,0.000013435495,0.000012408654],"domain_scores_gemma":[0.99981016,0.000051601746,0.000039109418,0.000023632232,0.000047853515,0.000027633358],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018416646,0.00017990924,0.0001241027,0.00045289766,0.00006740667,0.00024982874,0.000104744046,0.0002195806,0.0007505006],"category_scores_gemma":[0.000362911,0.00010769026,0.00007391917,0.00024629367,0.00011915179,0.00023039972,0.00025010353,0.00021708959,0.00014752753],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046321846,0.00009633203,0.0444731,0.00015033089,0.000078587254,0.00151842,0.00029461863,0.0046582264,0.88326454,0.0020034362,0.0011514497,0.061847854],"study_design_scores_gemma":[0.00016189886,0.000804722,0.45189732,0.00008725745,0.0002459833,0.008889241,0.00057105476,0.2251138,0.30044183,0.0042404155,0.007455266,0.00009117334],"about_ca_topic_score_codex":0.00019980609,"about_ca_topic_score_gemma":0.0002582636,"teacher_disagreement_score":0.0007505006,"about_ca_system_score_codex":0.0000717878,"about_ca_system_score_gemma":0.00006543493,"threshold_uncertainty_score":0.0025107265},"labels":[],"label_agreement":null},{"id":"W2521079701","doi":"10.1002/2016gl070138","title":"SHARAD detection and characterization of subsurface water ice deposits in Utopia Planitia, Mars","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":161,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Mars Exploration Program; Ground-penetrating radar; Radar; Terrain; Expansive; Water ice; Geomorphology; Astrobiology; Materials science","score_opus":0.021872864686750166,"score_gpt":0.25521760917803876,"score_spread":0.23334474449128859,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521079701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99921036,0.0000310694,0.00029875946,0.00000945708,7.320863e-7,0.000003627252,0.00008906861,0.00001830607,0.00033865037],"genre_scores_gemma":[0.9991591,0.000021117818,0.00062508625,0.0000041572307,0.000001037813,0.0000026852874,0.00012191456,0.0000017689185,0.000063036605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999733,0.000003350984,0.0000011264452,0.000006894144,0.00000653864,0.000008804653],"domain_scores_gemma":[0.99991715,0.000012268044,0.000027454847,0.0000087154895,0.00001685631,0.000017583154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010355389,0.00016064045,0.000114125214,0.00090093794,0.00017496508,0.0002696313,0.000109908324,0.00011610487,0.0003329774],"category_scores_gemma":[0.00017721478,0.00009453993,0.000074405376,0.00035178437,0.00019432281,0.0001525526,0.0002081975,0.00011606678,0.00005982548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022307427,0.000045138302,0.82427377,0.00007002862,0.000055233762,0.0006002442,0.0007444238,0.0023907134,0.13147035,0.00012682383,0.0003076831,0.039692476],"study_design_scores_gemma":[0.0000043487807,0.00003075434,0.9930987,0.0000057894304,0.000014812464,0.00021267195,0.00024413138,0.0027121739,0.0033397505,0.000028055849,0.00030509787,0.0000038459043],"about_ca_topic_score_codex":0.004663697,"about_ca_topic_score_gemma":0.009511684,"teacher_disagreement_score":0.004663697,"about_ca_system_score_codex":0.000097437565,"about_ca_system_score_gemma":0.00009538735,"threshold_uncertainty_score":0.009273112},"labels":[],"label_agreement":null},{"id":"W2521501615","doi":"10.1002/2016gl070248","title":"Ionospheric conductances and currents of a morning sector auroral arc from Swarm‐A electric and magnetic field measurements","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Academy of Finland","keywords":"Electrojet; Electric field; Ionosphere; Geophysics; Arc (geometry); Swarm behaviour; Magnetic field; Electric current; Equatorial electrojet; Physics; Electric potential; Field (mathematics); Magnetometer; Geodesy; Geology; Earth's magnetic field; Voltage; Geometry; Mathematics","score_opus":0.03507547868346093,"score_gpt":0.2882624965107886,"score_spread":0.25318701782732767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521501615","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986858,0.00003084077,0.00048476516,0.000008243432,0.0000028324234,0.0000038425487,0.00013828494,0.00003629193,0.000609185],"genre_scores_gemma":[0.99956495,0.00001076729,0.00022890871,0.0000021104654,0.0000018369157,0.0000018577749,0.00012098345,0.000004193825,0.00006450893],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.000008313257,0.0000033688752,0.000014641879,0.000012457763,0.000007293396],"domain_scores_gemma":[0.9997441,0.00007515952,0.0000579879,0.000032355812,0.000044929864,0.000045369874],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014814228,0.00018324528,0.00023065138,0.0006828321,0.00021347213,0.00037104377,0.00014088053,0.00020199957,0.0006124203],"category_scores_gemma":[0.0005221534,0.00012217459,0.00020526412,0.00036582758,0.00024755814,0.00022421895,0.00029831205,0.00021811122,0.0000963103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001151224,0.00009398817,0.4824197,0.0001893263,0.00017659357,0.00086601527,0.0017874978,0.0050496934,0.4818316,0.0003369629,0.0005556008,0.025541777],"study_design_scores_gemma":[0.000014611371,0.00018109288,0.97819465,0.000009859863,0.000042097545,0.00029097157,0.00034304534,0.0063142953,0.013941877,0.00011268112,0.00053889997,0.000016016993],"about_ca_topic_score_codex":0.0018902179,"about_ca_topic_score_gemma":0.0026679428,"teacher_disagreement_score":0.0018902179,"about_ca_system_score_codex":0.0001564274,"about_ca_system_score_gemma":0.00007829568,"threshold_uncertainty_score":0.00375849},"labels":[],"label_agreement":null},{"id":"W2521927654","doi":"10.1002/2016gl070454","title":"Wind‐driven mixing at intermediate depths in an ice‐free Arctic Ocean","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Drift ice; Sea ice; Arctic ice pack; Geology; Arctic sea ice decline; Arctic; Antarctic sea ice; Oceanography; Stratification (seeds); Climatology; Cryosphere; Canada Basin; Atmospheric sciences","score_opus":0.024815976246563787,"score_gpt":0.27262856937867297,"score_spread":0.24781259313210918,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521927654","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957126,0.000020239539,0.00006664271,0.000004456029,0.0000010899535,9.652916e-7,0.00004887351,0.0000029907205,0.0002835473],"genre_scores_gemma":[0.99980074,0.000012144282,0.0000673302,0.0000019156676,8.7020965e-7,8.2250517e-7,0.00006812685,0.0000010367833,0.000046975685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996626,0.000003220209,0.0000018165523,0.0000068740587,0.000006982003,0.000014803373],"domain_scores_gemma":[0.9998883,0.000016672875,0.000024236693,0.0000043804166,0.000021579392,0.000044845285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009734776,0.00018361992,0.00015335753,0.00040737208,0.0003871106,0.00051124644,0.000150861,0.00014230574,0.0005710715],"category_scores_gemma":[0.00020887733,0.00014517641,0.00015461881,0.00029308684,0.00019033872,0.00025359893,0.00036045138,0.00021488467,0.00006169954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020078516,0.00023606469,0.6652993,0.000060798422,0.0001049159,0.00046713385,0.0006562599,0.009351515,0.31191772,0.0010794032,0.00022453356,0.008594513],"study_design_scores_gemma":[0.000028887589,0.00013541852,0.9794128,0.000007563461,0.000026492087,0.00005113496,0.00030858922,0.011964007,0.007499723,0.00024997775,0.00029959137,0.000015841159],"about_ca_topic_score_codex":0.027682353,"about_ca_topic_score_gemma":0.033771493,"teacher_disagreement_score":0.027682353,"about_ca_system_score_codex":0.00054710085,"about_ca_system_score_gemma":0.00035529057,"threshold_uncertainty_score":0.055042446},"labels":[],"label_agreement":null},{"id":"W2521961519","doi":"10.1002/2016gl070042","title":"A preliminary statistical model for hydraulic fracture‐induced seismicity in the Western Canada Sedimentary Basin","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Seismology; Structural basin; Sedimentary rock; Geotechnical engineering; Geomorphology; Geochemistry","score_opus":0.04681803951420596,"score_gpt":0.2925469930871686,"score_spread":0.24572895357296262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2521961519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8630463,0.0004066783,0.12333814,0.001593657,0.00003974901,0.00021986864,0.0038638564,0.000559721,0.006932063],"genre_scores_gemma":[0.9897983,0.00019004893,0.0032363562,0.00007136404,0.000024605666,0.00010048302,0.00076956756,0.000039322516,0.005769985],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99933654,0.00013031156,0.00002307115,0.00017126076,0.0001243292,0.00021436422],"domain_scores_gemma":[0.99698347,0.0015327017,0.0005390864,0.00018116953,0.0005490923,0.00021441841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024298204,0.00065721065,0.00090988696,0.0015711751,0.001236273,0.0017059905,0.0028773767,0.0008486879,0.0037413],"category_scores_gemma":[0.007550574,0.0008073363,0.00085353194,0.0014844404,0.002547616,0.000867611,0.000837969,0.00094517,0.00037613342],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007964375,0.000022856082,0.0131988395,0.000015404834,0.00005790908,0.00013143689,0.000119057324,0.964267,0.0006373126,0.017489182,0.00091075373,0.0030705873],"study_design_scores_gemma":[0.0000130539165,0.00001868698,0.004975972,0.0000057500506,0.000020445646,0.000021632339,0.000043662785,0.9917303,0.00008695978,0.002745232,0.00032378017,0.000014596385],"about_ca_topic_score_codex":0.81004524,"about_ca_topic_score_gemma":0.6206012,"teacher_disagreement_score":0.18995476,"about_ca_system_score_codex":0.008012005,"about_ca_system_score_gemma":0.006855391,"threshold_uncertainty_score":0.38214684},"labels":[],"label_agreement":null},{"id":"W2522493641","doi":"10.1002/2016gl070023","title":"An unprecedented coastwide toxic algal bloom linked to anomalous ocean conditions","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine Toxins and Detection Methods","field":"Environmental Science","cited_by":572,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Institute of Environmental Health Sciences; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; Joint Institute for the Study of the Atmosphere and Ocean; National Oceanic and Atmospheric Administration; Center for Sponsored Coastal Ocean Research; National Institutes of Health; National Science Foundation","keywords":"Domoic acid; Upwelling; Bloom; Algal bloom; Oceanography; Spring bloom; Diatom; Nutrient; Environmental science; Range (aeronautics); Fishery; Phytoplankton; Ecology; Biology; Geology; Toxin","score_opus":0.029971683963992177,"score_gpt":0.3517541906534865,"score_spread":0.3217825066894943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2522493641","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998722,0.00004973901,0.00030921394,0.000060707163,0.000008465147,0.0000072390644,0.00021744135,0.000022132404,0.0006030739],"genre_scores_gemma":[0.9990609,0.00007445817,0.00040586985,0.000045692326,0.000007476452,0.0000046374557,0.00019138504,0.0000019741224,0.000207614],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998932,0.00001049939,0.000006393077,0.000037510366,0.00003556704,0.000016776792],"domain_scores_gemma":[0.99983335,0.000013569728,0.00006581405,0.000018457558,0.00003135499,0.000037488593],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016004709,0.00019865339,0.00013683591,0.00030034248,0.00041974592,0.0004303751,0.00011457435,0.00024967824,0.00043077715],"category_scores_gemma":[0.00021054193,0.0001112083,0.000094726194,0.00031334057,0.0002974779,0.00017411547,0.0004653971,0.00036660442,0.00011395536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002848157,0.0000631273,0.74331445,0.00003236485,0.000037317244,0.0014255929,0.00029478536,0.0003849516,0.24565604,0.00014428885,0.00036358408,0.007998713],"study_design_scores_gemma":[0.0000065451554,0.00020114264,0.9684095,0.000007024734,0.000018739305,0.0010985598,0.00045010526,0.0013187018,0.026918506,0.00019116752,0.0013684666,0.0000115255125],"about_ca_topic_score_codex":0.004687532,"about_ca_topic_score_gemma":0.010226946,"teacher_disagreement_score":0.004687532,"about_ca_system_score_codex":0.00054959964,"about_ca_system_score_gemma":0.00020613906,"threshold_uncertainty_score":0.009320438},"labels":[],"label_agreement":null},{"id":"W2524755861","doi":"10.1002/2016gl070969","title":"Meltwater pathways from marine terminating glaciers of the Greenland ice sheet","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Meltwater; Oceanography; Greenland ice sheet; Geology; Glacier; Ice sheet; Water mass; Hydrography; Climatology; Flux (metallurgy); Ice-sheet model; Cryosphere; Ocean current; Iceberg; Sea ice; Ice shelf; Geomorphology","score_opus":0.041026934508698557,"score_gpt":0.2575446794923004,"score_spread":0.21651774498360188,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2524755861","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99931085,0.000029165449,0.000032283177,0.000016683569,0.0000015366655,0.0000022566142,0.00022007292,0.000009337773,0.000377917],"genre_scores_gemma":[0.99916446,0.000025418341,0.00006978452,0.00000923827,9.0909975e-7,0.0000016846519,0.00047557804,0.000004051179,0.00024881947],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999746,0.000003339497,0.0000017775423,0.0000064480096,0.000003137215,0.000010734243],"domain_scores_gemma":[0.9998983,0.000021137734,0.000024776844,0.000006876345,0.000019450721,0.000029406287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001216604,0.00025391468,0.00017092738,0.0006030512,0.000387876,0.0005804194,0.0001766294,0.00022736962,0.000951227],"category_scores_gemma":[0.00025366351,0.00014194039,0.00023952514,0.00035903495,0.00029724828,0.00024208438,0.00037680418,0.00014596344,0.0000778896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013007136,0.00013673345,0.8274739,0.00008445251,0.0002524951,0.00074524997,0.0009509625,0.07718719,0.067021474,0.0015278767,0.0014772438,0.021841837],"study_design_scores_gemma":[0.00004583966,0.0001004254,0.9615892,0.00002462453,0.000042759384,0.000046716537,0.00038217392,0.032908134,0.0031322814,0.0005341168,0.0011729292,0.00002078894],"about_ca_topic_score_codex":0.073814794,"about_ca_topic_score_gemma":0.10639063,"teacher_disagreement_score":0.073814794,"about_ca_system_score_codex":0.0013981595,"about_ca_system_score_gemma":0.00053402333,"threshold_uncertainty_score":0.1467703},"labels":[],"label_agreement":null},{"id":"W2525694283","doi":"10.1002/2016gl070952","title":"Peat bogs in northern Alberta, Canada reveal decades of declining atmospheric Pb contamination","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Alberta Innovates; University of Alberta; Alberta Environment and Parks","keywords":"Bog; Peat; Ombrotrophic; Environmental science; Macrofossil; Deposition (geology); Atmosphere (unit); Contamination; Physical geography; Environmental chemistry; Hydrology (agriculture); Geology; Oceanography; Sediment; Ecology; Archaeology; Geography; Geomorphology; Chemistry; Holocene; Meteorology","score_opus":0.021140543571405514,"score_gpt":0.2734799615140922,"score_spread":0.2523394179426867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2525694283","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99853015,0.00024565062,0.000057398414,0.000029409826,0.0000020542484,0.0000036024517,0.00033160354,0.000009515032,0.0007906318],"genre_scores_gemma":[0.9987281,0.00015663094,0.00015700317,0.000013264657,0.0000012014682,0.0000017081584,0.0002786569,0.0000021300425,0.00066134945],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990475,0.000005146844,0.0000038695002,0.000016100086,0.000031170945,0.000038982933],"domain_scores_gemma":[0.9997284,0.000017197459,0.000041322404,0.000010284843,0.00013650896,0.00006629772],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016642317,0.00013869893,0.00012865418,0.0010583814,0.0010762397,0.0006772775,0.00026602755,0.0001610461,0.00048629014],"category_scores_gemma":[0.0002590587,0.000113432805,0.00007413178,0.0010991106,0.0004187322,0.0001278212,0.00029352616,0.00013185752,0.0000945173],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020579972,0.000027501212,0.9636686,0.000058747526,0.000031628446,0.0007787134,0.003288001,0.00033885884,0.012015086,0.000102248516,0.00053396524,0.018950762],"study_design_scores_gemma":[7.387198e-7,0.000004903842,0.997869,0.0000055135806,0.0000036959848,0.000053253734,0.0012355107,0.00008016839,0.00019638383,0.0000094692305,0.00053952174,0.0000018253785],"about_ca_topic_score_codex":0.93283933,"about_ca_topic_score_gemma":0.98514104,"teacher_disagreement_score":0.067160666,"about_ca_system_score_codex":0.0030047584,"about_ca_system_score_gemma":0.003189568,"threshold_uncertainty_score":0.13511235},"labels":[],"label_agreement":null},{"id":"W2527760657","doi":"10.1002/2016gl069799","title":"Persistent artifacts in the NSIDC ice motion data set and their implications for analysis","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Buoy; Sea ice; Geology; Climatology; Data set; Geodesy; Arctic ice pack; Meteorology; Oceanography; Geography; Computer science; Artificial intelligence","score_opus":0.11110872654943939,"score_gpt":0.3303669303899105,"score_spread":0.21925820384047112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527760657","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95587,0.0005859881,0.03377858,0.0010521875,0.00026838138,0.00013619271,0.0055941143,0.001189707,0.0015249838],"genre_scores_gemma":[0.97720385,0.00008802036,0.015756462,0.00018516605,0.000069444686,0.000057471494,0.006067743,0.00025067088,0.00032128603],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9891165,0.005147454,0.0017002393,0.0015018131,0.0022200912,0.00031389834],"domain_scores_gemma":[0.91691715,0.05676871,0.007112028,0.014280538,0.004379173,0.00054240297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.017858002,0.00041761802,0.00035418538,0.0014062611,0.0006988708,0.002340669,0.0008098138,0.0006214165,0.0005229431],"category_scores_gemma":[0.07638739,0.00025581612,0.0005017369,0.0029663057,0.0010708638,0.0013222169,0.0011393141,0.00068595505,0.0001789766],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091186614,0.00040536097,0.7909485,0.00024476432,0.00057082996,0.0005054999,0.00072607846,0.109112896,0.0064709797,0.00475003,0.012526096,0.072827],"study_design_scores_gemma":[0.00016862352,0.00028702567,0.618243,0.00015914743,0.0001288439,0.00063428323,0.0011218151,0.3459219,0.014973634,0.005979443,0.0122751985,0.000107063475],"about_ca_topic_score_codex":0.010767087,"about_ca_topic_score_gemma":0.010405157,"teacher_disagreement_score":0.017858002,"about_ca_system_score_codex":0.0010737885,"about_ca_system_score_gemma":0.0010823095,"threshold_uncertainty_score":0.09444326},"labels":[],"label_agreement":null},{"id":"W2527887797","doi":"10.1002/2016gl070760","title":"The Circumglobal North American wave pattern and its relation to cold events in eastern North America","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Teleconnection; Climatology; Geology; Jet stream; Rossby wave; Sea surface temperature; Zonal and meridional; Jet (fluid); El Niño Southern Oscillation; Physics","score_opus":0.03633273433429864,"score_gpt":0.28982446886117413,"score_spread":0.2534917345268755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2527887797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999156,0.000042021984,0.000036724967,0.000042409283,0.0000017998736,0.0000013888596,0.00010732552,0.0000015823382,0.00061083084],"genre_scores_gemma":[0.99973756,0.000038124756,0.00002222701,0.000007521205,0.000004275705,0.000001417581,0.000118221345,8.135585e-7,0.000069851114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.0000079458005,0.0000036601837,0.000013417679,0.000008426837,0.00001257577],"domain_scores_gemma":[0.99955064,0.00006932854,0.00019476,0.000030037543,0.00007103126,0.00008421587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011211943,0.000064542575,0.00008278615,0.0006091772,0.00019512972,0.00034590586,0.00008927763,0.00013412823,0.0014158727],"category_scores_gemma":[0.00050385663,0.000056245917,0.00008956251,0.0007711944,0.0002249987,0.00018837993,0.00024205852,0.00015020547,0.000077259036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040303315,0.00001024447,0.9954945,0.0000044234966,0.000022143084,0.000046244568,0.00010725894,0.00023893287,0.0010863884,0.00009491041,0.00015106257,0.0027035554],"study_design_scores_gemma":[7.8804584e-7,0.0000025066076,0.9997478,7.9574136e-7,0.0000019940746,0.000011189314,0.00004658832,0.000094053205,0.000013805973,0.000019535979,0.000060441977,5.290013e-7],"about_ca_topic_score_codex":0.023355924,"about_ca_topic_score_gemma":0.04255288,"teacher_disagreement_score":0.9766441,"about_ca_system_score_codex":0.0001954185,"about_ca_system_score_gemma":0.0001418669,"threshold_uncertainty_score":0.046439946},"labels":[],"label_agreement":null},{"id":"W2528625256","doi":"10.1002/2016gl070918","title":"The Northern Appalachian Anomaly: A modern asthenospheric upwelling","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"U.S. Geological Survey; U.S. Forest Service; National Science Foundation","keywords":"Geology; Upwelling; Asthenosphere; Anomaly (physics); Geophysics; Seismology; Continental margin; Shear (geology); Mantle (geology); Paleontology; Subduction; Oceanography; Tectonics","score_opus":0.023001524204591214,"score_gpt":0.2380872310049729,"score_spread":0.2150857068003817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528625256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952284,0.0002779536,0.00009595445,0.00011975517,0.000007484869,0.0000020494056,0.000073074574,0.0000073080246,0.004188038],"genre_scores_gemma":[0.99959785,0.000086435066,0.000045134788,0.000008371052,0.000012210281,5.559546e-7,0.000030015597,5.48169e-7,0.00021886421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999552,0.000004231022,0.0000028967702,0.000012920593,0.000012246091,0.000012572537],"domain_scores_gemma":[0.9998646,0.000015070277,0.000041458938,0.000011099067,0.000046300745,0.000021449538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007862931,0.0001042344,0.00009882113,0.00046262675,0.00053775136,0.0006267136,0.00011305646,0.00015984317,0.0013669488],"category_scores_gemma":[0.00020138151,0.00005374018,0.000050294333,0.0006506587,0.00062968896,0.00032385055,0.0002748957,0.00013803529,0.00008721826],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013035497,0.000022440505,0.9461476,0.00006206986,0.000028487553,0.0017559187,0.0012639221,0.00018981373,0.026289998,0.0012800776,0.00044667764,0.022382678],"study_design_scores_gemma":[0.0000011811384,0.000006480717,0.9984913,0.00000425649,0.0000032956443,0.00014963691,0.00025547453,0.00007613206,0.00017809197,0.00007020473,0.00076213095,0.0000017707531],"about_ca_topic_score_codex":0.029925428,"about_ca_topic_score_gemma":0.06280446,"teacher_disagreement_score":0.029925428,"about_ca_system_score_codex":0.00052198075,"about_ca_system_score_gemma":0.00030752076,"threshold_uncertainty_score":0.059502482},"labels":[],"label_agreement":null},{"id":"W2528743917","doi":"10.1002/2016gl070763","title":"A new model for the electron pressure nongyrotropy in the outer electron diffusion region","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Russian Science Foundation; Registered Nurses’ Foundation of Ontario","keywords":"Electron; Physics; Anisotropy; Population; Outflow; Superposition principle; Computational physics; Optics; Meteorology; Quantum mechanics","score_opus":0.019347729674883477,"score_gpt":0.29074896359108,"score_spread":0.2714012339161965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528743917","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42156082,0.00088849844,0.5179723,0.0018004753,0.00026387564,0.0001298988,0.0003721232,0.0004794722,0.056532577],"genre_scores_gemma":[0.9713747,0.00041113506,0.014104708,0.00019724086,0.00011410365,0.00011817405,0.000097693555,0.000089003945,0.013493359],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991107,0.000021293677,0.0000031474979,0.000019329256,0.000019529723,0.00002569659],"domain_scores_gemma":[0.9998135,0.000038162758,0.000036126883,0.000033400116,0.0000366937,0.000042095216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002598592,0.0004774457,0.00048818046,0.00033352574,0.00052374497,0.00094946,0.0014561698,0.0010403071,0.00246741],"category_scores_gemma":[0.0005498852,0.00032526956,0.0006027142,0.00022575511,0.0008184981,0.0015743604,0.00083187333,0.00070682104,0.00040439703],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000596089,0.00004758854,0.00093969965,0.000027548727,0.000022574339,0.0004713553,0.00010800111,0.8526182,0.012613015,0.13007855,0.00076972955,0.0022440273],"study_design_scores_gemma":[0.0000190849,0.000016327871,0.00017642292,0.00000220036,0.0000036288013,0.000049401442,0.00001215302,0.99071395,0.00028585896,0.007824839,0.0008892604,0.000006878943],"about_ca_topic_score_codex":0.003911352,"about_ca_topic_score_gemma":0.0014092355,"teacher_disagreement_score":0.003911352,"about_ca_system_score_codex":0.00056247076,"about_ca_system_score_gemma":0.00058385666,"threshold_uncertainty_score":0.008254349},"labels":[],"label_agreement":null},{"id":"W2528827837","doi":"10.1002/2016gl070983","title":"Nontrivial clustering of microseismicity induced by hydraulic fracturing","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium; University of Calgary; ConocoPhillips","keywords":"Microseism; Induced seismicity; Geology; Hydraulic fracturing; Magnitude (astronomy); Seismology; Layering; Aftershock; Fault (geology); Geophysics; Geotechnical engineering; Physics","score_opus":0.03513628772004963,"score_gpt":0.2813511092821919,"score_spread":0.2462148215621423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2528827837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99024045,0.000025196481,0.008916307,0.00002054748,0.0000028526465,0.000016700411,0.00015878383,0.000056515997,0.0005626244],"genre_scores_gemma":[0.99937004,0.0000072273665,0.0003817402,0.0000021691012,0.0000027978879,0.000005068529,0.0001320262,0.000004767649,0.00009424578],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998048,0.000024898782,0.000017176826,0.00005474325,0.0000497311,0.00004866505],"domain_scores_gemma":[0.9973122,0.00066198705,0.0009238762,0.00042720864,0.0004188254,0.0002559684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027695735,0.00012351088,0.00023047991,0.0012175784,0.00021241189,0.00043503192,0.00029409226,0.00019138787,0.0012152363],"category_scores_gemma":[0.0027775974,0.000119825745,0.0001881315,0.0007083795,0.0004571917,0.0003937362,0.00049438974,0.00017392731,0.00013949847],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073551777,0.00018607642,0.69370747,0.00023579446,0.00030736506,0.0017940257,0.0014658436,0.109625995,0.122477055,0.022480095,0.0024218955,0.04456288],"study_design_scores_gemma":[0.000020543745,0.00010759945,0.8210896,0.000011321749,0.00003921854,0.00046884918,0.00038222843,0.15937439,0.007687173,0.009907073,0.0008607849,0.00005120123],"about_ca_topic_score_codex":0.00132489,"about_ca_topic_score_gemma":0.0012819201,"teacher_disagreement_score":0.00132489,"about_ca_system_score_codex":0.0003577283,"about_ca_system_score_gemma":0.00018470705,"threshold_uncertainty_score":0.0040653944},"labels":[],"label_agreement":null},{"id":"W2530214392","doi":"10.1002/2016gl070500","title":"Sensitivity of Pine Island Glacier to observed ocean forcing","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Science and Technology Facilities Council; Natural Environment Research Council; U.S. Air Force; Korea Polar Research Institute; National Oceanic and Atmospheric Administration; York University; Sight Research UK; New York University Abu Dhabi; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Glacier; Ice stream; Oceanography; Antarctic ice sheet; Ice sheet; Thinning; Climatology; Ice shelf; Ocean heat content; Antarctic sea ice; Glacier ice accumulation; Sea ice; Cryosphere; Ocean current; Geomorphology; Geography","score_opus":0.06362833726003281,"score_gpt":0.28455030882069837,"score_spread":0.22092197156066556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2530214392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699664,0.0000903185,0.00019814825,0.00010013759,0.00002176593,0.000007737352,0.0011736549,0.000063235304,0.0013483772],"genre_scores_gemma":[0.999035,0.000028468905,0.000060588398,0.000020934556,0.0000075788926,0.0000028348113,0.00071504025,0.000007336774,0.00012217922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997969,0.0000455578,0.000010961602,0.0000735611,0.000026408203,0.0000465799],"domain_scores_gemma":[0.99898773,0.00045251384,0.00018004203,0.0001445393,0.00011374552,0.00012139737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007145978,0.00026863953,0.00029875865,0.00040066036,0.0003132092,0.0008313733,0.00032997338,0.00050204684,0.0014024483],"category_scores_gemma":[0.002378712,0.00023830823,0.00041699805,0.00031710402,0.00024344282,0.00032512136,0.00037811737,0.0005075429,0.00020475761],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036438392,0.000096521326,0.93705726,0.000049410526,0.00045757295,0.00023995113,0.00009470383,0.045423407,0.008507869,0.00016523211,0.0017071646,0.0058364817],"study_design_scores_gemma":[0.0000114663035,0.00002769578,0.96199954,0.000011542731,0.00002503702,0.000043030497,0.000050855822,0.03640257,0.0009817873,0.000062440304,0.0003700906,0.000014070154],"about_ca_topic_score_codex":0.04465206,"about_ca_topic_score_gemma":0.03537377,"teacher_disagreement_score":0.04465206,"about_ca_system_score_codex":0.0005544498,"about_ca_system_score_gemma":0.00033901032,"threshold_uncertainty_score":0.08878428},"labels":[],"label_agreement":null},{"id":"W2531332762","doi":"10.1002/2016gl069547","title":"Enhanced sedimentation beneath particle‐laden flows in lakes and the ocean due to double‐diffusive convection","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"University of Toronto Scarborough; Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Settling; Geology; Sedimentation; Sediment; Turbulence; Convection; Particle (ecology); Sediment transport; Geomorphology; Mechanics; Oceanography; Environmental science; Physics","score_opus":0.025875807092168898,"score_gpt":0.27954194327715953,"score_spread":0.2536661361849906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2531332762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997428,0.00003399841,0.000108228225,0.0000046752075,6.10666e-7,8.0254614e-7,0.000009033554,0.0000076074934,0.00009223614],"genre_scores_gemma":[0.9997712,0.000014803238,0.00013996824,0.0000021780372,0.0000011113891,0.0000012031028,0.0000111736645,0.0000015068703,0.000056953173],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999386,0.0000065670274,0.000006136094,0.000011803989,0.00001589464,0.000021139553],"domain_scores_gemma":[0.99976903,0.000052490635,0.00008320529,0.000010694611,0.000027759559,0.000056868925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014680736,0.00021890375,0.0002461291,0.00055428414,0.00032782144,0.0005225891,0.00010653243,0.00015149586,0.00044087495],"category_scores_gemma":[0.0003577189,0.0002384371,0.00013013974,0.00024154993,0.00049713644,0.0002989444,0.0007941505,0.00015490997,0.000061021598],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050901214,0.000023722507,0.14140643,0.00008627764,0.000026469896,0.00031614915,0.00046143896,0.0012818904,0.85065377,0.000385705,0.000057348465,0.004791735],"study_design_scores_gemma":[0.000063937776,0.0002195271,0.8665001,0.000015399719,0.000051649764,0.00021053287,0.0004470546,0.011924106,0.11970327,0.0003017525,0.0005302658,0.00003238964],"about_ca_topic_score_codex":0.004467192,"about_ca_topic_score_gemma":0.0035748,"teacher_disagreement_score":0.004467192,"about_ca_system_score_codex":0.0005602337,"about_ca_system_score_gemma":0.0002472296,"threshold_uncertainty_score":0.008882403},"labels":[],"label_agreement":null},{"id":"W2531909705","doi":"10.1002/2016gl071144","title":"An assessment of the radiative effects of ice supersaturation based on in situ observations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; China Scholarship Council; National Natural Science Foundation of China; Natural Sciences and Engineering Research Council of Canada; European Commission; Institut National Du Cancer; National Science Foundation","keywords":"Radiative transfer; Supersaturation; Environmental science; Atmospheric sciences; Water vapor; Ice cloud; Atmosphere (unit); Ice crystals; Climate change; Climatology; Meteorology; Physics; Geology; Thermodynamics","score_opus":0.02815582023473493,"score_gpt":0.3107046640242598,"score_spread":0.28254884378952483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2531909705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977865,0.000047660476,0.0014579085,0.000021447215,0.000005933006,0.0000063565667,0.00019873065,0.00003467106,0.00044065982],"genre_scores_gemma":[0.99912995,0.000028781576,0.00060859375,0.0000074056984,0.000006241429,0.000003855022,0.00017065446,0.000006079846,0.000038473627],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99974316,0.000117595235,0.0000146409575,0.000049506867,0.000047441186,0.00002764909],"domain_scores_gemma":[0.99837995,0.0009125464,0.00022425658,0.00016983302,0.0002562896,0.000057174057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009450917,0.0005730486,0.0002955553,0.00036615122,0.00020476153,0.00039420417,0.00029174227,0.00030762955,0.00044266175],"category_scores_gemma":[0.0015612176,0.0002327381,0.0004887699,0.0004081264,0.00016152239,0.00068587495,0.0002445518,0.00022892276,0.00007783369],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005302133,0.00027289576,0.70563096,0.00012469714,0.0004870009,0.00019581593,0.00018882434,0.16404799,0.10864082,0.00031704837,0.00033249872,0.019231204],"study_design_scores_gemma":[0.000031462623,0.00027687466,0.61312366,0.000015143227,0.0002220798,0.00005877095,0.00012634005,0.34549204,0.03986874,0.00021742113,0.0005319972,0.00003547323],"about_ca_topic_score_codex":0.012930237,"about_ca_topic_score_gemma":0.009246099,"teacher_disagreement_score":0.012930237,"about_ca_system_score_codex":0.00039706906,"about_ca_system_score_gemma":0.00018997246,"threshold_uncertainty_score":0.025709987},"labels":[],"label_agreement":null},{"id":"W2532891280","doi":"10.1002/2016gl070776","title":"Estimation of cloud fraction profile in shallow convection using a scanning cloud radar","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Biological and Environmental Research; Office of Science; Battelle; U.S. Department of Energy","keywords":"Radar; Meteorology; Zenith; Cloud computing; Wind profiler; Convection; Environmental science; Geology; Remote sensing; Computer science; Physics","score_opus":0.029160779675995483,"score_gpt":0.3103857933585106,"score_spread":0.28122501368251507,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2532891280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9868685,0.000028627734,0.012620331,0.00001114182,0.0000017275454,0.000008412534,0.00007394933,0.00010893435,0.00027838966],"genre_scores_gemma":[0.9958834,0.000010562344,0.004039097,0.0000014159132,8.3178764e-7,0.0000021570977,0.0000327167,0.0000034135471,0.000026365135],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999536,0.000011452496,0.0000031062057,0.000010096176,0.000012821613,0.000008904943],"domain_scores_gemma":[0.99976057,0.00009833748,0.000046829322,0.000029239382,0.00003771248,0.000027355343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023228471,0.00023560575,0.00020190273,0.00030732146,0.0001103012,0.00021220135,0.00020532832,0.00016904657,0.00020688749],"category_scores_gemma":[0.00051078567,0.00013813746,0.00018482843,0.00022791135,0.0001274212,0.0002232456,0.00017385668,0.0001417744,0.000047723497],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003488504,0.00010975735,0.13794634,0.00007574329,0.000099077064,0.00022064251,0.00013337172,0.5978091,0.22259812,0.0005538196,0.000188038,0.039917093],"study_design_scores_gemma":[0.000013826563,0.00004088549,0.022886034,0.0000027876044,0.000010042035,0.000021178854,0.000013313536,0.96403694,0.012827146,0.000094433446,0.000045467485,0.00000792553],"about_ca_topic_score_codex":0.009432128,"about_ca_topic_score_gemma":0.0065098493,"teacher_disagreement_score":0.009432128,"about_ca_system_score_codex":0.00022184939,"about_ca_system_score_gemma":0.00031591905,"threshold_uncertainty_score":0.018754482},"labels":[],"label_agreement":null},{"id":"W2547522661","doi":"10.1002/2016gl071153","title":"Preexplosive conduit conditions during the 2010 eruption of Merapi volcano (Java, Indonesia)","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Encana (Canada)","funders":"Agence Nationale de la Recherche; California Institute of Technology","keywords":"Geology; Volcano; Explosive eruption; Lava dome; Pumice; Magma; Lava; Dome (geology); Seismology; Electrical conduit; Strombolian eruption; Effusive eruption; Explosive material; Geochemistry; Magma chamber; Petrology; Geomorphology","score_opus":0.035675762359453765,"score_gpt":0.2693030266649342,"score_spread":0.23362726430548045,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2547522661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949884,0.00001910965,0.000019721598,0.000006508512,0.0000011055836,0.0000028544596,0.000101531004,0.0000023166083,0.00034800434],"genre_scores_gemma":[0.9996226,0.000019589012,0.000037746246,0.000006617325,0.0000024082985,0.000004190229,0.00016875363,0.0000021646254,0.00013600907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992883,0.0000051732213,0.0000055157802,0.000022067203,0.000014109694,0.000024385457],"domain_scores_gemma":[0.9998554,0.00002297131,0.000039794824,0.00000663859,0.00003411794,0.000041110117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015397264,0.0002616861,0.0002944435,0.00051415374,0.00062451436,0.000755154,0.00032920385,0.00044389666,0.00085281045],"category_scores_gemma":[0.00028750135,0.00027084973,0.0001454272,0.0003113511,0.0004130506,0.00051009504,0.00047830754,0.0004346247,0.0001717742],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010378213,0.00028261464,0.86289334,0.00007925999,0.00006125076,0.001289948,0.0017024529,0.0005130547,0.12533706,0.00010971423,0.00021332751,0.006480117],"study_design_scores_gemma":[0.0000046572613,0.00006201308,0.996253,0.0000032132484,0.000008969107,0.00009997925,0.000538936,0.0002540876,0.0026118995,0.000013624636,0.00014575153,0.0000038895887],"about_ca_topic_score_codex":0.017208243,"about_ca_topic_score_gemma":0.035130303,"teacher_disagreement_score":0.017208243,"about_ca_system_score_codex":0.00060660945,"about_ca_system_score_gemma":0.00023459077,"threshold_uncertainty_score":0.034216166},"labels":[],"label_agreement":null},{"id":"W2551251376","doi":"10.1002/2016gl070906","title":"The impact of Labrador Sea temperature and salinity variability on density and the subpolar AMOC in a decadal prediction system","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University of Reading; Natural Environment Research Council; Sight Research UK; Met Office; Department for Environment, Food and Rural Affairs, UK Government","keywords":"Salinity; Climatology; Temperature salinity diagrams; Oceanography; Environmental science; Sea surface temperature; Geology","score_opus":0.009930241145216132,"score_gpt":0.2492681606424574,"score_spread":0.23933791949724129,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2551251376","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966648,0.00003354986,0.0021027245,0.00015443563,0.000015473424,0.0000056219496,0.00027447948,0.00011383504,0.0006350795],"genre_scores_gemma":[0.99900144,0.000012015707,0.0006741314,0.000014211479,0.00000373389,0.000002876288,0.0001864978,0.0000056848753,0.00009948029],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982256,0.00006116398,0.000016807668,0.000050475806,0.00001984369,0.00002923364],"domain_scores_gemma":[0.99914384,0.00032566593,0.00012832598,0.000094578165,0.00017543545,0.00013221716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00087644137,0.00039224423,0.00030875226,0.00018728367,0.00032363512,0.000970822,0.0004123415,0.00039975822,0.0007636448],"category_scores_gemma":[0.001956004,0.0002539241,0.00027686203,0.00018269573,0.0002551426,0.0005201961,0.00047807096,0.0005288324,0.00012100542],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037069307,0.00015271766,0.20709619,0.000020268253,0.00013246619,0.00008717446,0.00007188448,0.7766269,0.0027010695,0.0005542808,0.0006939071,0.011492515],"study_design_scores_gemma":[0.0000286633,0.000059988302,0.039687693,0.0000048920774,0.000026882264,0.000008300589,0.000031281794,0.95869106,0.0011086059,0.00018324991,0.00015739369,0.000012060101],"about_ca_topic_score_codex":0.06515047,"about_ca_topic_score_gemma":0.03226632,"teacher_disagreement_score":0.06515047,"about_ca_system_score_codex":0.0006199013,"about_ca_system_score_gemma":0.0008709258,"threshold_uncertainty_score":0.12954253},"labels":[],"label_agreement":null},{"id":"W2551373400","doi":"10.1002/2016gl071489","title":"The influence of declining sea ice on shipping activity in the Canadian Arctic","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":181,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration","keywords":"Bay; Sea ice; Beaufort sea; Arctic; Oceanography; Arctic ice pack; Arctic sea ice decline; Canada Basin; Beaufort scale; Climatology; Geology; Environmental science; Physical geography; Antarctic sea ice; Geography","score_opus":0.03611522947917065,"score_gpt":0.29150079214203695,"score_spread":0.2553855626628663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2551373400","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939727,0.00055133447,0.00017271673,0.00022960706,0.000013003635,0.000008052088,0.0027202414,0.000016063243,0.002316234],"genre_scores_gemma":[0.99853134,0.00019032371,0.00012124727,0.000020706162,0.000003685987,0.0000021828193,0.00087482436,0.0000038064431,0.00025193294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99942905,0.000050077706,0.000027068641,0.000116106836,0.00018477342,0.00019285102],"domain_scores_gemma":[0.9982508,0.00014841797,0.0003034372,0.00005788958,0.0009774747,0.00026197062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00077562494,0.00040674172,0.00036500566,0.0015491445,0.0013878326,0.001605618,0.0008510359,0.0002788446,0.00096275995],"category_scores_gemma":[0.0032512688,0.0002146324,0.00046052775,0.0032011352,0.0008168069,0.00036281257,0.0007817958,0.00039439302,0.00011866152],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008270774,0.000008989574,0.99188656,0.000029655848,0.000111629524,0.00007124884,0.0002511995,0.0017166731,0.00068558234,0.00010126396,0.0004973871,0.004557096],"study_design_scores_gemma":[9.849996e-7,0.000003825842,0.998563,0.0000054179063,0.000014184259,0.00000956264,0.00023348106,0.00070146204,0.00005914895,0.000014275983,0.0003912739,0.0000034535497],"about_ca_topic_score_codex":0.9922438,"about_ca_topic_score_gemma":0.99487597,"teacher_disagreement_score":0.0134254955,"about_ca_system_score_codex":0.0134254955,"about_ca_system_score_gemma":0.01777328,"threshold_uncertainty_score":0.09740925},"labels":[],"label_agreement":null},{"id":"W2551871807","doi":"10.1002/2016gl071396","title":"Skillful seasonal forecasts of Arctic sea ice retreat and advance dates in a dynamical forecast system","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Sea ice; Arctic; Arctic ice pack; Forecast skill; Environmental science; The arctic; Meteorology; Oceanography; Geology; Geography","score_opus":0.014559323618205038,"score_gpt":0.2531530823741726,"score_spread":0.23859375875596758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2551871807","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9335864,0.00008025422,0.0638526,0.000225442,0.000033941935,0.000022012106,0.0005198555,0.00019094588,0.0014885112],"genre_scores_gemma":[0.9934902,0.000023394088,0.0060453457,0.0000139289405,0.000011340402,0.000005951323,0.000277565,0.000006067718,0.0001261081],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99977964,0.000081307386,0.000018556408,0.000059949507,0.000038112692,0.000022431916],"domain_scores_gemma":[0.99796814,0.0011408554,0.00027919177,0.00022570042,0.00026340337,0.00012270368],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014324078,0.00037283826,0.00032179346,0.00031960677,0.00018261786,0.0006202509,0.00025282832,0.00031631597,0.00042832276],"category_scores_gemma":[0.0073227054,0.00023492987,0.00023033314,0.00022346132,0.00021371753,0.00069226226,0.00048576805,0.0005238508,0.000083675775],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076271805,0.000030350317,0.016312718,0.000011715114,0.000046895148,0.000028332428,0.000020551923,0.97240776,0.0023766155,0.0009780875,0.00029822346,0.0074123614],"study_design_scores_gemma":[0.0000075807834,0.000017191658,0.004283468,0.0000021701192,0.0000063126645,0.0000042145916,0.000004269961,0.9943997,0.00055332156,0.0006167405,0.00010001354,0.0000050849803],"about_ca_topic_score_codex":0.018944751,"about_ca_topic_score_gemma":0.011710849,"teacher_disagreement_score":0.018944751,"about_ca_system_score_codex":0.00040871953,"about_ca_system_score_gemma":0.0006931542,"threshold_uncertainty_score":0.037668943},"labels":[],"label_agreement":null},{"id":"W2554317204","doi":"10.1002/2016gl070817","title":"Multidecadal increases in the Yukon River Basin of chemical fluxes as indicators of changing flowpaths, groundwater, and permafrost","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":162,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Tributary; Drainage basin; Hydrology (agriculture); Climate change; Groundwater; Precipitation; Flux (metallurgy); Environmental science; Structural basin; Geology; Weathering; Physical geography; Oceanography; Geochemistry; Geomorphology; Geography","score_opus":0.03182270407699821,"score_gpt":0.28354494030217814,"score_spread":0.2517222362251799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2554317204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99905425,0.00005091537,0.00005601284,0.000023377454,0.0000018884963,0.0000022107413,0.000618089,0.000007080818,0.00018609031],"genre_scores_gemma":[0.9990996,0.000033314318,0.000079585676,0.000010161146,7.8797734e-7,0.000004546734,0.00065685704,0.0000017575405,0.00011341833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990165,0.00001415203,0.000012651558,0.0000348453,0.000015544743,0.000021228127],"domain_scores_gemma":[0.9997124,0.00003999434,0.00008249596,0.00002580397,0.00009833443,0.000040933723],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018012176,0.00014166873,0.0001931196,0.00068503973,0.00032176432,0.0004957287,0.0001726466,0.0002501331,0.00055316364],"category_scores_gemma":[0.0003611837,0.00013576745,0.00019838424,0.0011408221,0.00019862669,0.00033570168,0.0004170237,0.00016152994,0.000053479293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005927546,0.000012760865,0.9929548,0.000019438427,0.0001020708,0.000063382104,0.00022985214,0.00040705042,0.002714992,0.00005630696,0.00021745886,0.0031626394],"study_design_scores_gemma":[0.0000015355171,0.0000041994654,0.9991584,0.0000017366995,0.000010257082,0.000013344119,0.00016921597,0.0003372085,0.00011512091,0.000008111482,0.00017880525,0.0000020715165],"about_ca_topic_score_codex":0.110112995,"about_ca_topic_score_gemma":0.20892222,"teacher_disagreement_score":0.889887,"about_ca_system_score_codex":0.00079058995,"about_ca_system_score_gemma":0.0005796026,"threshold_uncertainty_score":0.21894413},"labels":[],"label_agreement":null},{"id":"W2554428333","doi":"10.1002/2016gl071334","title":"Semiautomatic mapping of permafrost in the Yukon Flats, Alaska","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Arctic; Workflow; Cluster analysis; Geology; Hydrogeology; Physical geography; Thermokarst; Climate change; Remote sensing; Earth science; Computer science; Oceanography; Machine learning; Geography; Geotechnical engineering; Database","score_opus":0.07560515780359289,"score_gpt":0.3048910561513871,"score_spread":0.22928589834779423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2554428333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9323915,0.0001083197,0.061666183,0.000064058055,0.000013905228,0.00004827836,0.0011473641,0.0013633858,0.0031971596],"genre_scores_gemma":[0.9502125,0.00003000596,0.048500035,0.0000104734245,0.0000038963863,0.000016968655,0.00063794694,0.000036168807,0.00055207807],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983096,0.000028898397,0.00001506273,0.000060480965,0.000046002104,0.000018631217],"domain_scores_gemma":[0.999663,0.00006778909,0.00004926863,0.000060480954,0.00014071299,0.000018798592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031398053,0.00020375192,0.00016024699,0.0013305474,0.00032215845,0.00057572266,0.00024102312,0.00021779494,0.0005833135],"category_scores_gemma":[0.0005191475,0.00014890832,0.0001932795,0.0007353584,0.00024976133,0.00021487463,0.00032875597,0.00012107895,0.000227062],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002979332,0.00010705225,0.33609873,0.00022944924,0.00014019532,0.0003370067,0.0016949808,0.09853603,0.15440397,0.0011781667,0.0021310041,0.40484548],"study_design_scores_gemma":[0.000022580529,0.000038316015,0.5730268,0.000032926997,0.00003946197,0.0001489444,0.0010196364,0.3943974,0.025733292,0.0016521796,0.0038362416,0.000052254443],"about_ca_topic_score_codex":0.025087649,"about_ca_topic_score_gemma":0.06529697,"teacher_disagreement_score":0.025087649,"about_ca_system_score_codex":0.00032129715,"about_ca_system_score_gemma":0.0007112768,"threshold_uncertainty_score":0.049883246},"labels":[],"label_agreement":null},{"id":"W2556251739","doi":"10.1002/2016gl070457","title":"Fate of the Atlantic Meridional Overturning Circulation: Strong decline under continued warming and Greenland melting","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":264,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions","funders":"Japan Agency for Marine-Earth Science and Technology; Office of Science; National Oceanic and Atmospheric Administration; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Netherlands Earth System Science Centre; Natural Environment Research Council; U.S. Department of Energy","keywords":"Climatology; Greenland ice sheet; Climate change; Greenhouse gas; Environmental science; Climate model; Ocean current; Ice sheet; Geology; Oceanography","score_opus":0.05218092735764648,"score_gpt":0.2856871612543602,"score_spread":0.23350623389671374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2556251739","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981511,0.00005432165,0.00027146505,0.0003781239,0.000007606864,0.0000025508689,0.00033778913,0.000011807646,0.00078523904],"genre_scores_gemma":[0.9996642,0.000025261197,0.00004990953,0.000017049797,0.0000031062189,9.560015e-7,0.00015479082,0.0000018671266,0.000082878694],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998989,0.000026082473,0.0000055693918,0.000020752286,0.000017937165,0.000030748084],"domain_scores_gemma":[0.99937457,0.00009791983,0.00020344816,0.000059015125,0.00016784595,0.000097126125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008980078,0.00026784698,0.00021569859,0.00035863693,0.00034636667,0.0008048874,0.00031860554,0.00043306453,0.0008251003],"category_scores_gemma":[0.001343923,0.00012668181,0.00044811566,0.00033818168,0.0005014132,0.0006494769,0.00062007474,0.00038716654,0.000100120604],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046038436,0.00008615532,0.87549484,0.000030504872,0.0002874137,0.0005153548,0.00016581774,0.09746129,0.009249188,0.0033341325,0.0015735086,0.011341294],"study_design_scores_gemma":[0.000030726867,0.00012986184,0.809255,0.00002201534,0.000094717645,0.00007540552,0.00030995693,0.18232802,0.002982105,0.003287456,0.0014508946,0.000033800294],"about_ca_topic_score_codex":0.035620756,"about_ca_topic_score_gemma":0.024025528,"teacher_disagreement_score":0.035620756,"about_ca_system_score_codex":0.0014184715,"about_ca_system_score_gemma":0.0006416068,"threshold_uncertainty_score":0.07082683},"labels":[],"label_agreement":null},{"id":"W2559166964","doi":"10.1002/2016gl071317","title":"Impacts of the Last Glacial Cycle on ground surface temperature reconstructions over the last millennium","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland; St. Francis Xavier University; Université du Québec à Montréal","funders":"","keywords":"Borehole; Geology; Geothermal gradient; Glacial period; Climate change; Climatology; Ice sheet; Last Glacial Maximum; Thermal; Environmental science; Geomorphology; Geophysics; Meteorology; Oceanography; Paleontology; Geography","score_opus":0.03469457027385688,"score_gpt":0.28430203508579244,"score_spread":0.24960746481193555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2559166964","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784696,0.00013782227,0.00054934697,0.00012273104,0.000017788872,0.0000029993912,0.0006974416,0.000044363464,0.000580544],"genre_scores_gemma":[0.99902177,0.000058487152,0.00021578578,0.0000238035,0.000005575002,0.0000031121283,0.00057052285,0.000016763772,0.00008416032],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99972373,0.00009774324,0.000020361758,0.00007564972,0.00003650953,0.00004601924],"domain_scores_gemma":[0.99956614,0.00012638951,0.00009158617,0.00008597244,0.00007627423,0.000053542517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010535251,0.00037255656,0.0004249466,0.00043296564,0.00030312192,0.0007451689,0.00040531947,0.00041134175,0.0012498213],"category_scores_gemma":[0.001986107,0.00031181303,0.00088354456,0.0006096047,0.0004155455,0.0006131501,0.0005618315,0.0003806391,0.00014954251],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003445014,0.00007916613,0.7497466,0.000051202434,0.0008089497,0.00015487446,0.0000852117,0.23353855,0.00552283,0.0005959022,0.00073996716,0.008332335],"study_design_scores_gemma":[0.000074754236,0.00012611959,0.8224654,0.000037265163,0.00022036607,0.00009907096,0.0001509926,0.17262435,0.0021692936,0.00052688125,0.0014580548,0.0000474166],"about_ca_topic_score_codex":0.030288419,"about_ca_topic_score_gemma":0.0307061,"teacher_disagreement_score":0.030288419,"about_ca_system_score_codex":0.00068420917,"about_ca_system_score_gemma":0.0005377231,"threshold_uncertainty_score":0.060224235},"labels":[],"label_agreement":null},{"id":"W2561023687","doi":"10.1002/2016gl072347","title":"A model intercomparison of the tropical precipitation response to a CO<sub>2</sub> doubling in aquaplanet simulations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Science ICT and Future Planning; National Research Foundation of Korea","keywords":"Intertropical Convergence Zone; Equator; Hadley cell; Climatology; Atmospheric sciences; Environmental science; Precipitation; Walker circulation; Convergence zone; Energetics; Latitude; Climate model; Tropical wave; Convection; Sea surface temperature; Climate change; Geology; Physics; General Circulation Model; Meteorology; Tropical cyclone; Oceanography; Thermodynamics","score_opus":0.06615599416671658,"score_gpt":0.3416341421019818,"score_spread":0.2754781479352652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2561023687","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975325,0.000020827854,0.0003571483,0.00012795297,0.000012891795,0.0000072359057,0.00043350935,0.00006102935,0.0014469405],"genre_scores_gemma":[0.99877864,0.00001555374,0.0004931402,0.000024598385,0.0000028151949,0.000012643762,0.0003649965,0.000014470039,0.00029308454],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998553,0.000056494882,0.000007824109,0.000035662015,0.0000143158095,0.000030344976],"domain_scores_gemma":[0.99949205,0.00025186146,0.00005020319,0.000049134887,0.00007269412,0.00008413162],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00052933337,0.00058384164,0.0005827625,0.00023678217,0.00047457303,0.0006078925,0.0013917304,0.00093389204,0.0020375224],"category_scores_gemma":[0.0008617665,0.00037922274,0.0006888913,0.00048203257,0.00059151865,0.00058309257,0.00046032894,0.0008597059,0.000152395],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054599304,0.00019281705,0.012115275,0.000024174771,0.00013597148,0.000113460854,0.000055350854,0.9820663,0.0019329363,0.000697397,0.0007983436,0.0013220217],"study_design_scores_gemma":[0.00029800952,0.00019157083,0.008306999,0.0000048098523,0.000057927806,0.000015270061,0.000081241225,0.9884565,0.0016876098,0.00042369028,0.00045002968,0.0000264032],"about_ca_topic_score_codex":0.072437264,"about_ca_topic_score_gemma":0.03069534,"teacher_disagreement_score":0.072437264,"about_ca_system_score_codex":0.0015433921,"about_ca_system_score_gemma":0.0008936691,"threshold_uncertainty_score":0.14403123},"labels":[],"label_agreement":null},{"id":"W2561850601","doi":"10.1002/2016gl071230","title":"Characterizing near‐surface firn using the scattered signal component of the glacier surface return from airborne radio‐echo sounding","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta; Natural Environment Research Council; Alberta Innovates; Sight Research UK; Alberta Innovates - Technology Futures; National Aeronautics and Space Administration","keywords":"Firn; Geology; Glacier; Scattering; Surface roughness; Echo sounding; Stratigraphy; Geomorphology; Remote sensing; Optics; Seismology; Physics; Tectonics","score_opus":0.06566523652233135,"score_gpt":0.28133190560827637,"score_spread":0.215666669085945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2561850601","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982291,0.000028621836,0.0012838861,0.0000028382055,6.990786e-7,0.0000021238554,0.000083601204,0.000010416246,0.000358654],"genre_scores_gemma":[0.9984864,0.000033573597,0.0011340139,0.0000030664482,0.0000016236145,0.0000012614213,0.00022538431,0.000003217339,0.00011136411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999639,0.0000031230973,9.76711e-7,0.000009148741,0.000014557289,0.0000083692],"domain_scores_gemma":[0.9998963,0.000028172075,0.000017313725,0.0000074911713,0.00003556457,0.000015211599],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012442072,0.00021820399,0.00010231868,0.00053075457,0.0001246668,0.00027213152,0.00009933301,0.00009353516,0.000365041],"category_scores_gemma":[0.00024694475,0.000073833566,0.00010905341,0.00031762265,0.00013492482,0.00014920594,0.00011399296,0.00007363212,0.00008818142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018165189,0.0000711294,0.683054,0.00006595234,0.00008487433,0.00018877175,0.00043818163,0.017022902,0.23332316,0.00014323917,0.00014891746,0.06527729],"study_design_scores_gemma":[0.000005831632,0.000042046093,0.9623531,0.0000060918996,0.000023139704,0.00008291278,0.00023506825,0.024537057,0.01236854,0.00006644552,0.00026943564,0.000010250003],"about_ca_topic_score_codex":0.025719887,"about_ca_topic_score_gemma":0.07937199,"teacher_disagreement_score":0.025719887,"about_ca_system_score_codex":0.0002232456,"about_ca_system_score_gemma":0.0002167056,"threshold_uncertainty_score":0.051140368},"labels":[],"label_agreement":null},{"id":"W2563795912","doi":"10.1002/2016gl070764","title":"Satellite‐based observations of tsunami‐induced mesosphere airglow perturbations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"","keywords":"Airglow; Thermosphere; Mesosphere; Depth sounding; Atmosphere (unit); Atmospheric sciences; Satellite; Spacecraft; Gravity wave; Ionosphere; Geophysics; Geology; Physics; Environmental science; Remote sensing; Astronomy; Meteorology; Gravitational wave; Stratosphere; Oceanography","score_opus":0.04303536240312389,"score_gpt":0.30080452526314516,"score_spread":0.2577691628600213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2563795912","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99912554,0.000030429406,0.00014800487,0.000008103221,0.0000027405276,0.0000034658979,0.00031262342,0.000021892974,0.00034736216],"genre_scores_gemma":[0.9991048,0.00002603791,0.00022131884,0.000004058315,0.0000035926982,0.0000029486462,0.0005563528,0.0000030318772,0.000077885925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.0000056491313,0.0000029107841,0.000011560365,0.000013037531,0.000009414137],"domain_scores_gemma":[0.9998733,0.000015695348,0.00003860571,0.000014766212,0.000028175778,0.000029471528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014218503,0.00020340504,0.00012814191,0.0005180261,0.00014229542,0.00019678063,0.000110868525,0.00016593718,0.00047951905],"category_scores_gemma":[0.00026365227,0.00009975227,0.00018896261,0.0004018708,0.000111956615,0.00016942999,0.0002176492,0.00013496909,0.00009399054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005500079,0.000117944815,0.8259437,0.00005943615,0.00030172398,0.00028132432,0.00034912967,0.011823065,0.14463918,0.00017620818,0.00054447376,0.015213804],"study_design_scores_gemma":[0.000018563533,0.00006227183,0.98942626,0.000003213178,0.000029802111,0.00003042166,0.000053220807,0.006882971,0.0031512054,0.000030095405,0.00030594293,0.0000060603275],"about_ca_topic_score_codex":0.009254836,"about_ca_topic_score_gemma":0.014332974,"teacher_disagreement_score":0.009254836,"about_ca_system_score_codex":0.0002205603,"about_ca_system_score_gemma":0.0001581027,"threshold_uncertainty_score":0.01840192},"labels":[],"label_agreement":null},{"id":"W2566479556","doi":"10.1002/2016gl071668","title":"Further intensification of deep convection in the Labrador Sea in 2016","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":190,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Argo; Climatology; North Atlantic oscillation; Geology; Oceanography; Forcing (mathematics); Shutdown of thermohaline circulation; North Atlantic Deep Water; Thermohaline circulation; General Circulation Model; Convection; Climate change; Geography; Meteorology","score_opus":0.023148283593229815,"score_gpt":0.26383935342929044,"score_spread":0.24069106983606062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2566479556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974717,0.00026518543,0.0000742171,0.00025808517,0.00002713953,0.00000410117,0.0005254574,0.00002648931,0.0013476599],"genre_scores_gemma":[0.9987035,0.000090800815,0.00006606781,0.00005776502,0.000019960582,0.000002285228,0.00047098735,0.0000042225192,0.0005842688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985516,0.00001735606,0.000014128529,0.000032156244,0.000020912657,0.00006023698],"domain_scores_gemma":[0.99975497,0.000009781982,0.0001065515,0.00001822471,0.000054147116,0.000056362653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002787205,0.00019837401,0.00019423019,0.0006597102,0.00027255813,0.0009553932,0.00019097606,0.00023355568,0.0013942112],"category_scores_gemma":[0.0003374564,0.000066991364,0.0002556045,0.0006038953,0.00029881243,0.00041146312,0.0007014989,0.00029684612,0.0002778725],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062587776,0.00008554044,0.9345259,0.00015524126,0.00010339592,0.0004489984,0.0012307004,0.00065032777,0.018201478,0.000523703,0.002567708,0.040881064],"study_design_scores_gemma":[0.0000056825966,0.000025668822,0.99531794,0.000013102651,0.000010336858,0.00004814814,0.00032406423,0.00022323855,0.00086425524,0.000025443283,0.0031371827,0.0000050623444],"about_ca_topic_score_codex":0.028206145,"about_ca_topic_score_gemma":0.038641106,"teacher_disagreement_score":0.028206145,"about_ca_system_score_codex":0.0008843965,"about_ca_system_score_gemma":0.00062142836,"threshold_uncertainty_score":0.056083918},"labels":[],"label_agreement":null},{"id":"W2568979982","doi":"10.1002/2016gl071789","title":"Snow cover response to temperature in observational and climate model ensembles","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Toronto; Environment and Climate Change Canada","funders":"","keywords":"Climatology; Snow; Snow cover; Environmental science; Climate model; Climate change; Arctic; Climate sensitivity; Land cover; Forcing (mathematics); Atmospheric sciences; Meteorology; Geology; Geography; Land use; Ecology","score_opus":0.08617378584775487,"score_gpt":0.3531179490172101,"score_spread":0.26694416316945524,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2568979982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99786407,0.00007000871,0.0008030861,0.00006135642,0.000013609511,0.0000046150567,0.00086144306,0.000046751324,0.0002751677],"genre_scores_gemma":[0.997652,0.00003946619,0.0003462236,0.000017778984,0.000012175638,0.000008731113,0.0018481862,0.000010604296,0.000064896274],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99951637,0.00022587193,0.0000358478,0.00011685884,0.00005199728,0.000053148236],"domain_scores_gemma":[0.9973972,0.0015016883,0.00025742236,0.000414106,0.00028082868,0.00014880545],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002507347,0.0004157349,0.00046638993,0.00036385778,0.0003149309,0.0006274816,0.00039787043,0.0005020153,0.00041228725],"category_scores_gemma":[0.004763471,0.00029846653,0.0008398468,0.00048514307,0.00025651438,0.0007844469,0.0005601822,0.00045591703,0.00011019828],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00084855716,0.00020592565,0.38022733,0.000066065,0.0014504744,0.00009629752,0.00015153049,0.59909165,0.0045643076,0.00051045645,0.0014330749,0.011354279],"study_design_scores_gemma":[0.00006968427,0.00014045619,0.2925641,0.00001412434,0.00020078382,0.00004850339,0.00005964096,0.7033539,0.0023151205,0.00050485163,0.00068656116,0.000042203777],"about_ca_topic_score_codex":0.014200187,"about_ca_topic_score_gemma":0.013070834,"teacher_disagreement_score":0.014200187,"about_ca_system_score_codex":0.0006580721,"about_ca_system_score_gemma":0.00037965193,"threshold_uncertainty_score":0.028235078},"labels":[],"label_agreement":null},{"id":"W2569537545","doi":"10.1002/2016gl072251","title":"Generation of Multiband Chorus in the Earth's Magnetosphere: 1‐D PIC Simulation","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Youth Innovation Promotion Association of the Chinese Academy of Sciences; Youth Innovation Promotion Association; Chinese Academy of Sciences; National Natural Science Foundation of China; Canadian Anesthesiologists' Society","keywords":"Chorus; Physics; Magnetosphere; Computational physics; Harmonic; Cascade; Amplitude; Optics; Acoustics; Plasma; Quantum mechanics","score_opus":0.05592729961851574,"score_gpt":0.34219805673092474,"score_spread":0.286270757112409,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2569537545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9648479,0.00028314078,0.015298003,0.00063875195,0.00010101127,0.00006084644,0.00075699197,0.00037680613,0.017636549],"genre_scores_gemma":[0.99486095,0.000113696115,0.0035138882,0.00007677577,0.000016035963,0.00006595531,0.00033555506,0.000047978425,0.00096920616],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998754,0.000029234097,0.000004503549,0.000015113836,0.000027115413,0.00004865921],"domain_scores_gemma":[0.9994849,0.0002825109,0.00004081103,0.00003873725,0.00008734312,0.00006558883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025036285,0.0005711597,0.0008403907,0.0004526223,0.0008565134,0.0007535359,0.0010809818,0.0016851536,0.0024679266],"category_scores_gemma":[0.0011521818,0.00036946035,0.00069812423,0.0005863665,0.00071609626,0.0005617346,0.0005869284,0.00088056014,0.0001728535],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007602548,0.00006392323,0.0036914854,0.000052600375,0.00004001122,0.00021365595,0.0000891854,0.9901136,0.0010087688,0.0029010414,0.0006417,0.0011079663],"study_design_scores_gemma":[0.000019278592,0.000009988239,0.00035406413,0.0000030810788,0.000004717889,0.000007288362,0.000020795687,0.9990465,0.00015859476,0.00022010198,0.00015032916,0.0000052214205],"about_ca_topic_score_codex":0.027604802,"about_ca_topic_score_gemma":0.008285691,"teacher_disagreement_score":0.027604802,"about_ca_system_score_codex":0.0007498568,"about_ca_system_score_gemma":0.0009826242,"threshold_uncertainty_score":0.05488825},"labels":[],"label_agreement":null},{"id":"W2573802682","doi":"10.1002/2016gl071881","title":"Eutrophication‐induced acidification of coastal waters in the northern Gulf of Mexico: Insights into origin and processes from a coupled physical‐biogeochemical model","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":149,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Oceanography; Biogeochemical cycle; Eutrophication; Benthic zone; Environmental science; Ocean acidification; Hypoxia (environmental); Biogeochemistry; Bottom water; Water column; Stratification (seeds); Phytoplankton; Nutrient; Geology; Environmental chemistry; Seawater; Ecology; Oxygen; Chemistry","score_opus":0.044400709114593165,"score_gpt":0.3064939468614351,"score_spread":0.26209323774684196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2573802682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961876,0.00006423477,0.0011457303,0.00024282094,0.000008610967,0.000013517335,0.00037056895,0.000050569608,0.0019163389],"genre_scores_gemma":[0.9985985,0.00006232897,0.00059516623,0.00002050741,0.000005776399,0.000019990563,0.00019351595,0.000007631292,0.00049655477],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994504,0.0000148131285,0.0000031559548,0.000014896569,0.0000050867416,0.000017043301],"domain_scores_gemma":[0.9998258,0.000063744286,0.000038495862,0.00001088044,0.000024898382,0.00003627903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017851964,0.0005110759,0.00044988783,0.00030560113,0.00058789115,0.000985618,0.00068307226,0.0013211872,0.0011467614],"category_scores_gemma":[0.0005287731,0.00039301132,0.00054989284,0.00030251563,0.00057051063,0.00042926782,0.00072461757,0.00047368248,0.00006444879],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012836055,0.00007849546,0.015797406,0.000017939803,0.000070010065,0.00012680146,0.000039391256,0.98054713,0.0014840459,0.00065419375,0.0002162731,0.00083992333],"study_design_scores_gemma":[0.000081280705,0.000034780784,0.007158667,0.000003536948,0.000028655852,0.0000066257276,0.000051916362,0.9921051,0.00016703186,0.0002067535,0.00014678898,0.000008883851],"about_ca_topic_score_codex":0.16363207,"about_ca_topic_score_gemma":0.086441115,"teacher_disagreement_score":0.16363207,"about_ca_system_score_codex":0.0018499248,"about_ca_system_score_gemma":0.0012249529,"threshold_uncertainty_score":0.32535923},"labels":[],"label_agreement":null},{"id":"W2575349173","doi":"10.1002/2016gl071045","title":"Observed warming trend in sea surface temperature at tropical cyclone genesis","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Tropical cyclone; Climatology; Sea surface temperature; Environmental science; Forcing (mathematics); Global warming; Climate change; Atmospheric sciences; Oceanography; Geology","score_opus":0.06805007655397553,"score_gpt":0.3068277136108274,"score_spread":0.23877763705685184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2575349173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99737096,0.00009080237,0.00012450204,0.00004576131,0.000010348543,0.000001545287,0.0013737646,0.000020518293,0.00096171716],"genre_scores_gemma":[0.9989241,0.000045796172,0.000058977275,0.000010398141,0.00000604353,0.0000021702556,0.0008197149,0.0000023612472,0.0001304313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.000004397365,0.0000027409733,0.00001323357,0.000005330345,0.000008500307],"domain_scores_gemma":[0.9998229,0.00003825093,0.000048445603,0.000019189274,0.000044453263,0.00002677077],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011247527,0.00013384165,0.00009497791,0.00018880412,0.00012582357,0.00023961077,0.000092520866,0.00017183578,0.0015461235],"category_scores_gemma":[0.0002834263,0.00006935054,0.00015378659,0.00024982827,0.000091765745,0.00017267953,0.00017816987,0.00026253928,0.00014344373],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015807888,0.000039712933,0.97807044,0.000054426855,0.00010889155,0.00007290491,0.0000961631,0.0056356755,0.009507777,0.00022729821,0.0011609396,0.0048676147],"study_design_scores_gemma":[0.00000945757,0.000038720344,0.9927858,0.0000072549183,0.000027788967,0.000033234748,0.000053648168,0.003956136,0.001957869,0.000044169316,0.0010815926,0.00000437514],"about_ca_topic_score_codex":0.0069975834,"about_ca_topic_score_gemma":0.010799553,"teacher_disagreement_score":0.0069975834,"about_ca_system_score_codex":0.0002061709,"about_ca_system_score_gemma":0.00015726147,"threshold_uncertainty_score":0.013913691},"labels":[],"label_agreement":null},{"id":"W2577369584","doi":"10.1002/2016gl072455","title":"On the role of ice‐nucleating aerosol in the formation of ice particles in tropical mesoscale convective systems","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Transport Canada; Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Ice nucleus; Mesoscale meteorology; Aerosol; Ice crystals; Atmospheric sciences; Convection; Particle (ecology); Nucleation; Climatology; Environmental science; Meteorology; Geology; Physics; Thermodynamics; Oceanography","score_opus":0.026229199742974323,"score_gpt":0.28690030944706674,"score_spread":0.2606711097040924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2577369584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979552,0.0009859222,0.00022503745,0.000039167116,0.000004394194,0.0000059551276,0.000057699013,0.0000031550862,0.00072341174],"genre_scores_gemma":[0.99957436,0.00023071637,0.00012330117,0.000005779458,0.0000061716228,0.0000012614862,0.000022733955,0.000001171657,0.000034464396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.000016955051,0.000007707675,0.000027389062,0.000021209484,0.00002333455],"domain_scores_gemma":[0.99970895,0.00013670772,0.00006545167,0.00001353156,0.000035525034,0.000039802202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004154496,0.0002473345,0.00018279992,0.00041291284,0.00046033904,0.00070792256,0.00030090395,0.0002721821,0.00036654028],"category_scores_gemma":[0.00038441978,0.00012234597,0.00020069508,0.00018950661,0.0004934114,0.00046405688,0.00032163854,0.00015439121,0.00007352421],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060486473,0.00017138748,0.76571435,0.00029270723,0.00017537137,0.0007239439,0.0005653951,0.0068802675,0.20521967,0.0015836896,0.00020714189,0.017861262],"study_design_scores_gemma":[0.000015562158,0.0001720383,0.94564575,0.000033666493,0.000068816145,0.0001811854,0.00041916192,0.014288337,0.03776392,0.00057436957,0.0008244257,0.000012747443],"about_ca_topic_score_codex":0.0081184395,"about_ca_topic_score_gemma":0.00574966,"teacher_disagreement_score":0.0081184395,"about_ca_system_score_codex":0.0005241555,"about_ca_system_score_gemma":0.00027828236,"threshold_uncertainty_score":0.016142368},"labels":[],"label_agreement":null},{"id":"W2579759697","doi":"10.1002/2016gl072190","title":"Urban heat island‐induced increases in evapotranspirative demand","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":126,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Impervious surface; Environmental science; Urban heat island; Evapotranspiration; Urbanization; Vegetation (pathology); Land cover; Growing season; Atmospheric sciences; Hydrology (agriculture); Land use; Ecology; Geography; Meteorology; Geology","score_opus":0.04722618182617807,"score_gpt":0.3248605719980135,"score_spread":0.27763439017183544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2579759697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987999,0.0000350806,0.0001789608,0.000018371815,0.00000199429,0.0000020065302,0.00029204172,0.000008395618,0.00066321075],"genre_scores_gemma":[0.9996112,0.000017628541,0.000050239636,0.000005886963,8.210861e-7,0.0000029815674,0.00012511582,0.0000019095012,0.0001842324],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997246,0.0000044593226,0.0000014228445,0.000008002414,0.0000038553967,0.000009856091],"domain_scores_gemma":[0.9999273,0.00001510135,0.00002010214,0.000008374737,0.000014079294,0.000014972502],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000043955766,0.000102699625,0.00010248536,0.00009781357,0.00010604958,0.0002555509,0.00008287714,0.0000989943,0.001957818],"category_scores_gemma":[0.00009749816,0.000050509614,0.0000897364,0.00019177457,0.000105874475,0.0001289771,0.00016711536,0.00015125755,0.0001481201],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013521506,0.00029393221,0.34337434,0.00015327726,0.00016111831,0.00031329735,0.00023239126,0.009135033,0.62216854,0.0004990282,0.0014902622,0.020826647],"study_design_scores_gemma":[0.0000044183494,0.00009244228,0.9626753,0.0000033266065,0.000016635842,0.000055602828,0.00027035375,0.004267327,0.031292345,0.00017383235,0.0011413378,0.0000072046146],"about_ca_topic_score_codex":0.0045378306,"about_ca_topic_score_gemma":0.00808459,"teacher_disagreement_score":0.0045378306,"about_ca_system_score_codex":0.00023845324,"about_ca_system_score_gemma":0.00010947727,"threshold_uncertainty_score":0.009022832},"labels":[],"label_agreement":null},{"id":"W2580027604","doi":"10.1002/2016gl071895","title":"Gyre‐scale deep convection in the subpolar North Atlantic Ocean during winter 2014–2015","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Institut national des sciences de l'Univers; European Regional Development Fund; Horizon 2020 Framework Programme; Ministerio de Economía y Competitividad; Centre National de la Recherche Scientifique; Equipex; Agence Nationale de la Recherche; Institut Français de Recherche pour l'Exploitation de la Mer","keywords":"Ocean gyre; Thermocline; Argo; Geology; Mixed layer; Oceanography; Deep sea; Convection; Thermohaline circulation; Climatology; Convective mixing; Structural basin; Deep convection; Oceanic basin; Deep water; North Atlantic Deep Water; Subtropics; Meteorology; Geography; Geomorphology","score_opus":0.018446276853089142,"score_gpt":0.2667042848444793,"score_spread":0.24825800799139014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2580027604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99939847,0.00003308123,0.000035100587,0.00001991642,0.0000072149005,0.0000015939617,0.00028959807,0.00000567672,0.00020930285],"genre_scores_gemma":[0.9991893,0.000022179345,0.000050498133,0.000011005172,0.000007194079,0.0000025030245,0.0005610443,0.0000022105721,0.00015412013],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990153,0.0000129929485,0.000008683644,0.0000318335,0.00001588175,0.000029096956],"domain_scores_gemma":[0.9997738,0.000022403563,0.000076514196,0.00002057683,0.000043190095,0.000063562926],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030903082,0.00018309736,0.00021715503,0.0004743175,0.00028641656,0.00051053596,0.00018914304,0.00024324814,0.00057403115],"category_scores_gemma":[0.000431967,0.00011214766,0.00023930414,0.00026005748,0.00025083497,0.00031367686,0.0005072941,0.00016707617,0.00016915491],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026257217,0.00005034054,0.98574233,0.00001967476,0.0001224074,0.000083663,0.00030438317,0.00074026297,0.0070957025,0.00006307143,0.00057721406,0.00493845],"study_design_scores_gemma":[0.0000032190624,0.0000157775,0.9986211,0.0000039151314,0.000011004159,0.000011061629,0.00011873651,0.0006413193,0.00023523936,0.00001129431,0.0003242003,0.0000031966993],"about_ca_topic_score_codex":0.032057274,"about_ca_topic_score_gemma":0.061017346,"teacher_disagreement_score":0.032057274,"about_ca_system_score_codex":0.00052260474,"about_ca_system_score_gemma":0.00029284833,"threshold_uncertainty_score":0.063741386},"labels":[],"label_agreement":null},{"id":"W2580994841","doi":"10.1002/2016gl071542","title":"Improving synoptic and intraseasonal variability in CFSv2 via stochastic representation of organized convection","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Madden–Julian oscillation; Climatology; Precipitation; Climate Forecast System; Convection; Environmental science; Forcing (mathematics); Climate model; Oscillation (cell signaling); Meteorology; Atmospheric sciences; Geology; Climate change; Physics","score_opus":0.03218320700637482,"score_gpt":0.3161282530940645,"score_spread":0.28394504608768967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2580994841","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9810363,0.00008081982,0.014462565,0.00025073337,0.000045186116,0.000028109676,0.0009933489,0.0005426998,0.0025602537],"genre_scores_gemma":[0.9960033,0.000016427854,0.003229727,0.000018961722,0.000013317493,0.000016269185,0.00050763035,0.000032217347,0.00016218086],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998129,0.00007759758,0.000010296743,0.000033667642,0.00002644333,0.000039134113],"domain_scores_gemma":[0.9995134,0.00021983514,0.000054549815,0.000058790352,0.00010040388,0.00005295026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008560251,0.00064803933,0.00044457233,0.00034944626,0.00036275497,0.0006248349,0.0006628534,0.00056385424,0.0011357496],"category_scores_gemma":[0.0015628568,0.00023058322,0.00058410683,0.0004137308,0.00027218886,0.00061118795,0.00047704307,0.00057485246,0.000101826554],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006160898,0.000047854905,0.0052790167,0.000010191735,0.000027893482,0.000019295967,0.000013929733,0.9902624,0.0011766392,0.00047309743,0.00035573347,0.002272386],"study_design_scores_gemma":[0.000030252244,0.00001643621,0.0012414177,0.0000013299846,0.0000032298367,0.0000017071412,0.000003644785,0.9982058,0.0002756,0.00010349686,0.00011298106,0.0000041252524],"about_ca_topic_score_codex":0.053641587,"about_ca_topic_score_gemma":0.036220763,"teacher_disagreement_score":0.053641587,"about_ca_system_score_codex":0.0007629443,"about_ca_system_score_gemma":0.0011582302,"threshold_uncertainty_score":0.1066587},"labels":[],"label_agreement":null},{"id":"W2583912670","doi":"10.1002/2016gl072398","title":"Observations of the shape and group dynamics of rogue waves","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Waves and Remote Sensing","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Core Research for Evolutional Science and Technology","keywords":"Rogue wave; Crest; Geology; Superposition principle; Love wave; Rayleigh wave; Wind wave; Front (military); Longitudinal wave; Significant wave height; Mechanical wave; Surface wave; Physics; Wave propagation; Seismology; Meteorology; Nonlinear system; Optics; Oceanography","score_opus":0.05466847401724544,"score_gpt":0.2842454882856818,"score_spread":0.22957701426843635,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2583912670","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989839,0.000011661934,0.00038659116,0.0000065078643,8.002592e-7,0.0000039034503,0.00010077766,0.000006904764,0.0004989046],"genre_scores_gemma":[0.99950194,0.0000092535865,0.00021342172,0.0000015829949,0.0000012723215,0.0000022876618,0.00018557826,0.0000018599728,0.00008272138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998336,0.000029625453,0.0000081621565,0.000043214557,0.000056098834,0.000029299748],"domain_scores_gemma":[0.999132,0.00020634626,0.00024371778,0.00011639932,0.00021651275,0.000085026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002425543,0.00010158168,0.00015991819,0.0008298264,0.00022409797,0.00026628232,0.00016871934,0.00018881889,0.0003982818],"category_scores_gemma":[0.0013195832,0.00011818553,0.00010202319,0.0004906392,0.0002266698,0.0002861057,0.00030228673,0.00022724045,0.00016447032],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011996577,0.000055043096,0.9624724,0.00001547508,0.000048818525,0.0001427271,0.0007345974,0.0012424398,0.022231791,0.00013260891,0.00022307236,0.0125810485],"study_design_scores_gemma":[0.0000030286717,0.000047943176,0.994902,0.000002531378,0.000007772352,0.000094504576,0.00024365672,0.003630397,0.0008082796,0.000044213975,0.00021080277,0.0000050023727],"about_ca_topic_score_codex":0.0038331153,"about_ca_topic_score_gemma":0.0052373037,"teacher_disagreement_score":0.0038331153,"about_ca_system_score_codex":0.00015670627,"about_ca_system_score_gemma":0.00007733503,"threshold_uncertainty_score":0.0076215863},"labels":[],"label_agreement":null},{"id":"W2586709157","doi":"10.1002/2016gl071567","title":"The United States “warming hole”: Quantifying the forced aerosol response given large internal variability","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Science Foundation","keywords":"Aerosol; Environmental science; Forcing (mathematics); Climatology; Atmospheric sciences; Climate model; Radiative forcing; Climate change; Meteorology; Oceanography; Geology; Geography","score_opus":0.0829527760994677,"score_gpt":0.36704799141483957,"score_spread":0.28409521531537185,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2586709157","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999366,0.000016980137,0.00021399287,0.000033962395,0.000005075367,0.0000030146446,0.00013285357,0.00001726997,0.00021081248],"genre_scores_gemma":[0.9996501,0.000007797239,0.00014388301,0.000010376841,0.0000029090625,0.0000043792224,0.00015104674,0.0000040560326,0.000025516865],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998901,0.00004249564,0.0000053779368,0.000029466119,0.000008689767,0.000023913399],"domain_scores_gemma":[0.9995834,0.00015485038,0.000071064496,0.0000758156,0.000049828937,0.00006509035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00076633913,0.00038029673,0.00035593097,0.0003494241,0.00040677082,0.00059011055,0.00042757706,0.00065984816,0.0007294881],"category_scores_gemma":[0.0014993252,0.00028697963,0.0005748643,0.0003422871,0.00043758107,0.00048852863,0.0005581468,0.000477952,0.000057226],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006252613,0.0002807381,0.50752616,0.000053930995,0.0004907872,0.00032967277,0.00015580587,0.46874025,0.01295797,0.001651596,0.0015575573,0.0056302045],"study_design_scores_gemma":[0.00011631635,0.00021487701,0.22567858,0.000012769508,0.000112048554,0.000043640594,0.00011882989,0.76858866,0.003991896,0.0006116795,0.00047974268,0.000030946172],"about_ca_topic_score_codex":0.029683163,"about_ca_topic_score_gemma":0.023103014,"teacher_disagreement_score":0.029683163,"about_ca_system_score_codex":0.00066607044,"about_ca_system_score_gemma":0.00038568507,"threshold_uncertainty_score":0.059020817},"labels":[],"label_agreement":null},{"id":"W2587866114","doi":"10.1002/2017gl072538","title":"On factors controlling precursor slip fronts in the laboratory and their relation to slow slip events in nature","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Slip (aerodynamics); Nucleation; Asperity (geotechnical engineering); Materials science; Drop (telecommunication); Stress field; Standard deviation; Mechanics; Stress (linguistics); Geology; Slip line field; Composite material; Thermodynamics; Physics; Shear (geology)","score_opus":0.029732347309283445,"score_gpt":0.29365780601295693,"score_spread":0.2639254587036735,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2587866114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991059,0.00015236402,0.00041741133,0.0000104367755,0.000002199581,0.000010416303,0.000046330384,0.0000075446915,0.0002473275],"genre_scores_gemma":[0.9993948,0.00006299719,0.00030707137,0.000008386002,0.0000025487477,0.000011587284,0.00006466991,0.0000035929597,0.00014440004],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99979,0.00003939436,0.000017521548,0.000048036363,0.000057930258,0.000047129364],"domain_scores_gemma":[0.9991715,0.00021836002,0.00032857782,0.000050287264,0.00013098471,0.000100189834],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027611025,0.0001725222,0.0002428748,0.00040704833,0.00015052735,0.00047830044,0.00014521809,0.00020884405,0.00093500357],"category_scores_gemma":[0.0009820168,0.00014967575,0.00016063095,0.00018235078,0.00029863275,0.00030858538,0.00025660245,0.00035924948,0.0001304302],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021880321,0.00006767783,0.024825187,0.000038875227,0.000007985161,0.000104148756,0.000074615695,0.00023022937,0.97120494,0.00008550833,0.00003695605,0.0031050628],"study_design_scores_gemma":[0.000014572296,0.000834176,0.4522779,0.000013644245,0.000023530687,0.00025285644,0.00033292457,0.004795803,0.54034543,0.00014199715,0.00094321737,0.000023920442],"about_ca_topic_score_codex":0.0011031748,"about_ca_topic_score_gemma":0.0008825887,"teacher_disagreement_score":0.0011031748,"about_ca_system_score_codex":0.0003033101,"about_ca_system_score_gemma":0.00014693227,"threshold_uncertainty_score":0.0031279325},"labels":[],"label_agreement":null},{"id":"W2588503365","doi":"10.1002/2016gl072201","title":"Time‐varying extreme rainfall intensity‐duration‐frequency curves in a changing climate","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Drought Analysis","field":"Environmental Science","cited_by":177,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Precipitation; Environmental science; Climate change; Duration (music); Probabilistic logic; Markov chain; Climatology; Intensity (physics); Reliability (semiconductor); Markov chain Monte Carlo; Bayesian probability; Computer science; Meteorology; Econometrics; Statistics; Mathematics; Geology; Geography; Physics","score_opus":0.04736813058221395,"score_gpt":0.31427587152622394,"score_spread":0.26690774094401,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588503365","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9895663,0.000020587726,0.009011855,0.000075808006,0.0000046001082,0.000008041376,0.00023946371,0.00005865463,0.0010146777],"genre_scores_gemma":[0.9992029,0.000009156576,0.00062276446,0.00000426375,0.0000019076347,0.0000028871032,0.000079109355,0.0000055539244,0.000071523886],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998424,0.00005694327,0.000009450452,0.000033694138,0.000029936939,0.000027631933],"domain_scores_gemma":[0.9980215,0.0012042454,0.0003498855,0.00014154242,0.00019492938,0.000087981294],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008160547,0.00014890406,0.00013638988,0.00052335503,0.00015571175,0.0003880243,0.00030037572,0.0003650773,0.0007380898],"category_scores_gemma":[0.0035126985,0.00013291437,0.00021276926,0.0005079231,0.0003275665,0.0005178299,0.0002522442,0.0003740455,0.000081792874],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019039222,0.00006387261,0.16365677,0.000044722554,0.00008806624,0.00031263847,0.00021727929,0.812465,0.0064400877,0.004329992,0.0005944825,0.011596647],"study_design_scores_gemma":[0.000010980078,0.000057398982,0.16604525,0.000006989693,0.000020091144,0.00010852731,0.00014735016,0.82861173,0.0014300954,0.0030511855,0.00047858566,0.000031867254],"about_ca_topic_score_codex":0.0063647674,"about_ca_topic_score_gemma":0.004104156,"teacher_disagreement_score":0.0063647674,"about_ca_system_score_codex":0.00037575245,"about_ca_system_score_gemma":0.00016297291,"threshold_uncertainty_score":0.012655437},"labels":[],"label_agreement":null},{"id":"W2588534335","doi":"10.1002/2016gl071826","title":"Statistical azimuthal structuring of the substorm onset arc: Implications for the onset mechanism","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration; National Science Foundation","keywords":"Substorm; Arc (geometry); Geophysics; Instability; Homogeneous; Physics; Amplitude; Plasma; Astrophysics; Geology; Magnetosphere; Statistical physics; Mechanics; Optics; Geometry; Mathematics","score_opus":0.03185943617578382,"score_gpt":0.33017771484890335,"score_spread":0.29831827867311955,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2588534335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9847935,0.00019563446,0.012607175,0.0000870659,0.000007887551,0.000014122752,0.0003004895,0.00011510908,0.0018790065],"genre_scores_gemma":[0.9994634,0.000021290212,0.00037156505,0.0000044687567,0.000006966144,0.0000030748954,0.00006903063,0.000007510185,0.000052816187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997999,0.00004014183,0.000016784732,0.00006885672,0.000039469807,0.00003487792],"domain_scores_gemma":[0.99497885,0.0026829129,0.0009991564,0.00052329263,0.00045586776,0.00035999998],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00070258573,0.00007992016,0.0002532633,0.00097560417,0.00029779432,0.0008297817,0.00021769092,0.00016260022,0.0021360393],"category_scores_gemma":[0.0046538333,0.00010101852,0.00016819779,0.00057656283,0.0006726508,0.0005506053,0.00035989028,0.00021514748,0.00016246864],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003921476,0.00006693833,0.8371595,0.00014296568,0.00012254268,0.00040056658,0.00078987685,0.013565883,0.10564487,0.013225174,0.000847028,0.027642542],"study_design_scores_gemma":[0.000009616573,0.00008053785,0.96103454,0.000007850314,0.000032974684,0.00030347108,0.00035133152,0.026140695,0.0044731186,0.006831588,0.0007108454,0.000023381237],"about_ca_topic_score_codex":0.0010956258,"about_ca_topic_score_gemma":0.0007696537,"teacher_disagreement_score":0.0021360393,"about_ca_system_score_codex":0.00021057425,"about_ca_system_score_gemma":0.00018936952,"threshold_uncertainty_score":0.007145822},"labels":[],"label_agreement":null},{"id":"W2590257084","doi":"10.1002/2016gl071941","title":"Aerosol‐driven increase in Arctic sea ice over the middle of the twentieth century","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Alaska Sea Grant, University of Alaska Fairbanks","keywords":"Climatology; Arctic sea ice decline; Sea ice; Arctic geoengineering; Arctic; Arctic ice pack; Environmental science; Climate change; Cryosphere; Aerosol; Global warming; Forcing (mathematics); Atmospheric sciences; Ice-albedo feedback; Oceanography; Geology; Antarctic sea ice; Meteorology; Geography","score_opus":0.03217838964081755,"score_gpt":0.271072236667725,"score_spread":0.23889384702690747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2590257084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99715316,0.00016498135,0.00033365499,0.00029940717,0.000032514894,0.0000036138345,0.0005505085,0.000020286385,0.0014418062],"genre_scores_gemma":[0.99912244,0.00016331555,0.00011382207,0.000021625057,0.000008179985,0.000003664049,0.000232976,0.000004330781,0.00032956715],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999428,0.000011246629,0.0000036846168,0.000015886977,0.000007938729,0.000018460158],"domain_scores_gemma":[0.99992144,0.000014166974,0.000020709436,0.0000061758797,0.000018500104,0.000018937702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002515662,0.00029596416,0.00018454564,0.00028436907,0.00032683933,0.00094762543,0.00025636086,0.0005946372,0.0016837785],"category_scores_gemma":[0.00055131427,0.00017852442,0.0004993608,0.0004099438,0.0002826284,0.0005112206,0.00042044473,0.0003774655,0.00013204198],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003561491,0.0001624014,0.32371983,0.00015845992,0.0004111964,0.00072505936,0.00034866252,0.6467601,0.007856594,0.0057748533,0.002235713,0.011490967],"study_design_scores_gemma":[0.00022977829,0.00018688435,0.46866328,0.00007347014,0.00018322353,0.00019090337,0.0005410139,0.517952,0.0031310539,0.0022507403,0.0065334323,0.00006415957],"about_ca_topic_score_codex":0.0946309,"about_ca_topic_score_gemma":0.07709742,"teacher_disagreement_score":0.0946309,"about_ca_system_score_codex":0.0013396619,"about_ca_system_score_gemma":0.0007859321,"threshold_uncertainty_score":0.18816018},"labels":[],"label_agreement":null},{"id":"W2591598241","doi":"10.1002/2017gl072811","title":"Ultra‐relativistic radiation belt extinction and ULF wave radial diffusion: Modeling the September 2014 extended dropout event","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency","keywords":"Van Allen radiation belt; Physics; Flux (metallurgy); Van Allen Probes; Hiss; Geophysics; Diffusion; Scattering; Solar wind; Ultra low frequency; Extinction (optical mineralogy); Computational physics; Atmospheric sciences; Electron; Astrophysics; Astronomy; Magnetosphere; Plasma; Optics","score_opus":0.019855062196912816,"score_gpt":0.2954733701810425,"score_spread":0.27561830798412973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2591598241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968741,0.0000593148,0.0010782302,0.00023318622,0.000014715253,0.0000101235655,0.00020101141,0.000052826665,0.0014763707],"genre_scores_gemma":[0.9990902,0.000029761099,0.00037461318,0.000029408564,0.000006998456,0.000006277558,0.00013828288,0.000014518433,0.00031004235],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999107,0.000021378966,0.000004859287,0.00001620008,0.000008372586,0.00003851008],"domain_scores_gemma":[0.9996517,0.00013844072,0.00006322955,0.000028774535,0.000039388156,0.00007833837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038840622,0.0004366947,0.00050171034,0.00031054596,0.0004210042,0.0006645904,0.0012428198,0.0011839985,0.0015733982],"category_scores_gemma":[0.0012180586,0.00029347886,0.0007478698,0.00026220607,0.0005624833,0.00059672253,0.00066658383,0.0009268677,0.00015003227],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023617368,0.00017911117,0.029180208,0.000024469444,0.00006590803,0.00025527357,0.000067015564,0.9653796,0.0014010874,0.0012463272,0.00048700097,0.0014779175],"study_design_scores_gemma":[0.00007099847,0.000042507792,0.0051644584,0.000003992272,0.000015616595,0.000015156432,0.000050526454,0.9939374,0.00023637307,0.00024978144,0.00020344227,0.0000097439615],"about_ca_topic_score_codex":0.049729273,"about_ca_topic_score_gemma":0.018987125,"teacher_disagreement_score":0.049729273,"about_ca_system_score_codex":0.0011089256,"about_ca_system_score_gemma":0.0005496418,"threshold_uncertainty_score":0.098879635},"labels":[],"label_agreement":null},{"id":"W2592800041","doi":"10.1002/2016gl072387","title":"Arctic sea ice decline and continental cold anomalies: Upstream and downstream effects of Greenland blocking","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"North Atlantic oscillation; Oceanography; Climatology; Geology; Arctic oscillation; Bay; Arctic; Greenland ice sheet; Northern Hemisphere; Sea ice; Arctic dipole anomaly; Arctic ice pack; Ice sheet; Antarctic sea ice","score_opus":0.021652768183402563,"score_gpt":0.29419359850446375,"score_spread":0.2725408303210612,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2592800041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991073,0.000059117792,0.00003590976,0.00004674132,0.0000038260337,0.000001396716,0.0001423684,0.0000045483603,0.00059867784],"genre_scores_gemma":[0.9996618,0.000023818728,0.000014512975,0.000012191234,0.0000047231274,6.1731134e-7,0.00015398918,0.0000024657743,0.00012585972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998192,0.000057639765,0.000007452978,0.000035380923,0.000020909849,0.00005939911],"domain_scores_gemma":[0.99905497,0.00027076853,0.00019686564,0.00005934589,0.000112830276,0.00030525832],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049321394,0.00023937854,0.00027153955,0.00044718033,0.00023420168,0.0005591841,0.000219151,0.00024168403,0.0013912314],"category_scores_gemma":[0.0010141463,0.00009533016,0.00040456362,0.00035359449,0.0003457265,0.00026435804,0.0003671028,0.0002725054,0.00011926239],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005160042,0.00007807967,0.9870733,0.0000101705655,0.0001377043,0.00024736146,0.000089265486,0.0028659862,0.004844093,0.00014349808,0.00026815056,0.003726344],"study_design_scores_gemma":[0.000002726807,0.000024145951,0.99860257,0.0000017087452,0.000020809792,0.000011270945,0.000045179117,0.0010065541,0.00016448255,0.000023739974,0.000095096024,0.000001678936],"about_ca_topic_score_codex":0.058657527,"about_ca_topic_score_gemma":0.061396502,"teacher_disagreement_score":0.058657527,"about_ca_system_score_codex":0.0008022429,"about_ca_system_score_gemma":0.00061686605,"threshold_uncertainty_score":0.11663222},"labels":[],"label_agreement":null},{"id":"W2593086661","doi":"10.1002/2017gl072590","title":"Erosion of Northern Hemisphere blanket peatlands under 21st‐century climate change","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; University of Leeds; University of East Anglia","keywords":"Peat; Climate change; Erosion; Fluvial; Environmental science; Physical geography; Hydrology (agriculture); Precipitation; Geology; Geography; Structural basin; Geomorphology; Oceanography","score_opus":0.03988362601440883,"score_gpt":0.3089308349189882,"score_spread":0.2690472089045794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2593086661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990669,0.000030338171,0.00012303329,0.000036930127,0.0000029458472,0.00000185446,0.00037486284,0.000016071597,0.0003470171],"genre_scores_gemma":[0.9993988,0.00003148453,0.00008266711,0.0000068059503,0.000001983372,0.000002534278,0.00039081532,0.0000028457048,0.00008197139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988616,0.00002647676,0.0000073150322,0.000031195224,0.000018772722,0.000030117773],"domain_scores_gemma":[0.9997929,0.000040691604,0.00005847656,0.000022641312,0.000043351196,0.000041866584],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043083812,0.00024552652,0.00028607817,0.0003287312,0.0002555789,0.00070231827,0.00024684754,0.00042087602,0.0008143725],"category_scores_gemma":[0.0006510498,0.00013180145,0.0004469774,0.000409248,0.00023607188,0.00038758028,0.00031305666,0.00019494414,0.00010977854],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000365963,0.00008506594,0.7568283,0.00003476872,0.00018532417,0.00027200356,0.00010045734,0.23171362,0.0028806378,0.00028827018,0.0007583675,0.006487186],"study_design_scores_gemma":[0.000041732,0.00006518176,0.8792137,0.000011028075,0.000038552604,0.00007382821,0.00013075853,0.118591584,0.0009706716,0.00031509908,0.0005288161,0.000019015668],"about_ca_topic_score_codex":0.06963225,"about_ca_topic_score_gemma":0.07561583,"teacher_disagreement_score":0.06963225,"about_ca_system_score_codex":0.00116046,"about_ca_system_score_gemma":0.00055489835,"threshold_uncertainty_score":0.13845384},"labels":[],"label_agreement":null},{"id":"W2594943952","doi":"10.1002/2017gl072690","title":"Subsidence at Cerro Prieto Geothermal Field and postseismic slip along the Indiviso fault from 2011 to 2016 RADARSAT‐2 DInSAR time series analysis","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Geology; Interferometric synthetic aperture radar; Seismology; Geothermal gradient; Slip (aerodynamics); Geodesy; Fault (geology); Subsidence; Synthetic aperture radar; Geomorphology; Geophysics; Remote sensing; Structural basin","score_opus":0.02597927326330838,"score_gpt":0.27471805245615205,"score_spread":0.24873877919284368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2594943952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978364,0.00006431434,0.00008467363,0.000019308587,0.0000043647333,0.00000404153,0.001072749,0.000016414324,0.0008976934],"genre_scores_gemma":[0.99703395,0.00005950234,0.00019149976,0.0000074976115,0.000011335208,0.000005056999,0.0023818319,0.000003852655,0.0003054134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998802,0.000010568661,0.0000084311905,0.00004014199,0.00003247036,0.000028255676],"domain_scores_gemma":[0.9996754,0.000034102137,0.0001289542,0.00004318016,0.00008345441,0.000034963487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024374078,0.0001889399,0.00015515418,0.0008440406,0.00009584725,0.0003563564,0.00019114003,0.00017324457,0.00042697787],"category_scores_gemma":[0.0006988855,0.00006622048,0.0001355456,0.00068949885,0.0001378698,0.00013331167,0.0002489333,0.00013224309,0.00013150381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032744705,0.00008980628,0.9614964,0.000059305246,0.00011336046,0.00035066664,0.00028715268,0.00557001,0.007103896,0.00018068709,0.0017634594,0.022657843],"study_design_scores_gemma":[0.000003006687,0.000010584871,0.99772376,0.0000047088574,0.0000059062645,0.000035041867,0.00004168462,0.0010712906,0.00029622164,0.0000067563033,0.00079848187,0.0000026643056],"about_ca_topic_score_codex":0.023605892,"about_ca_topic_score_gemma":0.032586075,"teacher_disagreement_score":0.023605892,"about_ca_system_score_codex":0.0004525162,"about_ca_system_score_gemma":0.00023095417,"threshold_uncertainty_score":0.04693699},"labels":[],"label_agreement":null},{"id":"W2595216645","doi":"10.1002/2016gl071791","title":"Understanding ozone‐meteorology correlations: A role for dry deposition","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":219,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Ozone; Environmental science; Atmospheric sciences; Humidity; Relative humidity; Water vapor; Deposition (geology); Meteorology; Climatology; Air quality index; Vapour Pressure Deficit; Geography; Chemistry; Geology","score_opus":0.10069556460982715,"score_gpt":0.31636945212590467,"score_spread":0.21567388751607752,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2595216645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891747,0.00097325345,0.007173598,0.0006598243,0.000016696109,0.000017307448,0.00070201466,0.000070891874,0.0012117793],"genre_scores_gemma":[0.99876344,0.0001427898,0.0007281554,0.000048767415,0.000017335555,0.0000045225,0.00018011255,0.000008600542,0.000106237516],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996263,0.0001763137,0.000023962488,0.00009506696,0.000032567885,0.00004588264],"domain_scores_gemma":[0.9959686,0.0026020517,0.00059604255,0.0005119268,0.00014044494,0.00018098578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019608028,0.00042842343,0.00057597156,0.00064851966,0.0003039707,0.0014703646,0.0003966894,0.00032031842,0.001198875],"category_scores_gemma":[0.0064484505,0.00026492425,0.0005563176,0.00073621207,0.0004973476,0.0018447881,0.0007833111,0.00061065896,0.00016511802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013370725,0.00010732967,0.956803,0.000085661966,0.00043879444,0.00012546244,0.00020712303,0.021941256,0.0034530978,0.00426985,0.00074969005,0.011684944],"study_design_scores_gemma":[0.000018437966,0.00009542854,0.8285752,0.00003048628,0.00011575653,0.000087575994,0.00026935845,0.15931365,0.0012002507,0.009079619,0.0011903448,0.000023986488],"about_ca_topic_score_codex":0.0075114127,"about_ca_topic_score_gemma":0.005939304,"teacher_disagreement_score":0.0075114127,"about_ca_system_score_codex":0.00026002873,"about_ca_system_score_gemma":0.0006454619,"threshold_uncertainty_score":0.014935374},"labels":[],"label_agreement":null},{"id":"W2595296361","doi":"10.1002/2017gl072920","title":"The complex behavior of El Niño winter 2015–2016","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Ministerio de Economía y Competitividad; FPInnovations; Met Office","keywords":"Teleconnection; Stratosphere; Polar vortex; Climatology; Precipitation; Polar; Environmental science; Oceanography; Atmospheric sciences; Geology; El Niño Southern Oscillation; Geography; Meteorology; Physics","score_opus":0.09245152752830209,"score_gpt":0.3861369545402735,"score_spread":0.2936854270119714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2595296361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9897995,0.0005305578,0.00043016823,0.00066629314,0.00022292967,0.000010780066,0.0035797986,0.00006371158,0.0046962113],"genre_scores_gemma":[0.9963569,0.00014412183,0.00007995436,0.000053326043,0.00006532211,0.00000778149,0.0025792597,0.000012878642,0.0007004528],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99964166,0.000045167206,0.000049503305,0.000086029875,0.00011041873,0.00006722286],"domain_scores_gemma":[0.99864167,0.00017071134,0.00058626675,0.00007689751,0.00033033505,0.00019406009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011761328,0.00024082373,0.0002578665,0.0009293539,0.00033906865,0.0012395941,0.0002207246,0.00034635214,0.001726274],"category_scores_gemma":[0.002554871,0.000092176626,0.00024321451,0.00072201504,0.00026842143,0.00058094406,0.00079947384,0.00029187134,0.00039058246],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004651837,0.000064877306,0.95889235,0.00012623117,0.00026878386,0.00016252672,0.00068369234,0.006558713,0.006171767,0.0024468089,0.006735441,0.01742359],"study_design_scores_gemma":[0.0000065151403,0.000028921831,0.9872519,0.00004804914,0.000016869215,0.00006586738,0.00042858926,0.0034873453,0.0007557497,0.000631088,0.007260991,0.000018153169],"about_ca_topic_score_codex":0.011659169,"about_ca_topic_score_gemma":0.014162144,"teacher_disagreement_score":0.011659169,"about_ca_system_score_codex":0.00058443705,"about_ca_system_score_gemma":0.00046361383,"threshold_uncertainty_score":0.02318263},"labels":[],"label_agreement":null},{"id":"W2598114332","doi":"10.1029/2004gl019990","title":"SO<sub>2</sub> depletion in tropospheric volcanic plumes","year":2004,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":86,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Plume; Volcano; Troposphere; Atmospheric sciences; Environmental science; Panache; Flux (metallurgy); Relative humidity; Aerosol; Geology; Climatology; Meteorology","score_opus":0.01747720181834025,"score_gpt":0.25133665734481114,"score_spread":0.2338594555264709,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2598114332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996848,0.00007814331,0.00005029343,0.0000061521714,4.4749822e-7,0.000001825574,0.000024708675,0.000004471819,0.00014920848],"genre_scores_gemma":[0.99965,0.00004927584,0.00012567927,0.0000044452927,6.719419e-7,0.000003779942,0.000071808216,0.0000023563898,0.00009199892],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999962,0.0000061294695,0.0000021923997,0.000009352237,0.000009076713,0.000011313509],"domain_scores_gemma":[0.99993,0.000012418072,0.00002126936,0.0000064057876,0.000020387472,0.000009542384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009882697,0.00015464771,0.0001988791,0.00028600317,0.00020550263,0.00028234994,0.00013722882,0.00016192008,0.0002867633],"category_scores_gemma":[0.00023048079,0.00012981477,0.00010405643,0.00015995874,0.00018765028,0.00021121529,0.0001818327,0.00015951887,0.000054892727],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003361119,0.000047029345,0.098390825,0.00004955758,0.000035061945,0.0001536317,0.00039059317,0.0011344238,0.8940176,0.0000600034,0.00006291938,0.0053222543],"study_design_scores_gemma":[0.000019920122,0.00024195161,0.84375244,0.0000106620155,0.00003202718,0.0003202631,0.0006054643,0.009706844,0.14447774,0.000122017984,0.0006943817,0.000016208342],"about_ca_topic_score_codex":0.013748152,"about_ca_topic_score_gemma":0.01502514,"teacher_disagreement_score":0.013748152,"about_ca_system_score_codex":0.0004329898,"about_ca_system_score_gemma":0.000093232484,"threshold_uncertainty_score":0.02733624},"labels":[],"label_agreement":null},{"id":"W2598342431","doi":"10.1002/2017gl073138","title":"North Pacific twentieth century decadal‐scale variability is unique for the past 342 years","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Archipelago; Pacific decadal oscillation; Climatology; Storm; Oceanography; Pacific ocean; Geology; Sea surface temperature","score_opus":0.041027629601569436,"score_gpt":0.3148606665617767,"score_spread":0.2738330369602073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2598342431","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99539644,0.0005336474,0.00023381165,0.00017848215,0.000019454605,0.000002114896,0.0017455709,0.000030504922,0.0018599492],"genre_scores_gemma":[0.99809605,0.00030229005,0.00007376495,0.000015562924,0.000011189966,0.0000022011222,0.0010042198,0.000004831512,0.0004898138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.0000041982034,0.0000031897948,0.000023782814,0.000007535933,0.000010867474],"domain_scores_gemma":[0.99983835,0.000013458008,0.000070315546,0.000024826257,0.00003254976,0.000020495976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013978514,0.000103379156,0.00008682824,0.00046303304,0.00021773866,0.00056530425,0.000100440375,0.0001051273,0.0012234203],"category_scores_gemma":[0.00045003902,0.0000899952,0.00017376104,0.0006706233,0.00012480524,0.000287441,0.00033682192,0.00021323514,0.00017031046],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058494217,0.000013879199,0.9708803,0.000032726966,0.00020854159,0.00014801133,0.00028582843,0.000988316,0.0023338965,0.00025589459,0.0013030272,0.023491018],"study_design_scores_gemma":[8.207168e-7,0.000004560227,0.9973405,0.0000047167728,0.000019942565,0.000042603984,0.00006870988,0.00039020446,0.00013648937,0.000050768056,0.0019379535,0.0000026990742],"about_ca_topic_score_codex":0.011029595,"about_ca_topic_score_gemma":0.025861109,"teacher_disagreement_score":0.011029595,"about_ca_system_score_codex":0.00017173865,"about_ca_system_score_gemma":0.00016950398,"threshold_uncertainty_score":0.021930814},"labels":[],"label_agreement":null},{"id":"W2598558071","doi":"10.1002/2016gl072345","title":"Change in dust seasonality as the primary driver for orbital‐scale dust storm variability in East Asia","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Leibniz-Gemeinschaft; Lamont-Doherty Earth Observatory, Columbia University; Dalhousie University; Universität Potsdam; Deutsche Forschungsgemeinschaft; National Science Foundation","keywords":"Subarctic climate; Climatology; Northern Hemisphere; Dust storm; Glacial period; Storm; Environmental science; Geology; Latitude; Mineral dust; Interglacial; Atmospheric sciences; Seasonality; Oceanography; Geography; Meteorology; Aerosol; Geomorphology","score_opus":0.06671436766976996,"score_gpt":0.32867953265579414,"score_spread":0.2619651649860242,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2598558071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995987,0.0000515102,0.000051068906,0.00001597798,0.0000013254328,6.878833e-7,0.000104623134,0.0000019032702,0.00017422503],"genre_scores_gemma":[0.99975663,0.000033137614,0.000030311123,0.000004457246,0.0000019408267,6.791367e-7,0.000112857626,0.0000010228375,0.00005898287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999378,0.000010278249,0.000008097799,0.000019691928,0.000009449227,0.000014743651],"domain_scores_gemma":[0.9995927,0.000088259425,0.00014762556,0.00004362892,0.000070885035,0.000056835044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038580108,0.00012410518,0.00018577298,0.00039412692,0.00021313004,0.00056573574,0.00016754137,0.00012314151,0.0007235283],"category_scores_gemma":[0.00040174407,0.00012724052,0.00016168511,0.00045310106,0.00025500447,0.00026124436,0.0002574064,0.00017711696,0.00008388734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004415573,0.000009946061,0.9934237,0.000009370193,0.000040780596,0.00006258576,0.00014837667,0.00018285276,0.0035686232,0.000042761625,0.000057569505,0.0024092526],"study_design_scores_gemma":[9.978925e-7,0.000005322619,0.99926895,0.0000020464433,0.000009909852,0.000021521584,0.0000998319,0.00031038155,0.00020142306,0.000013867328,0.00006479189,9.548256e-7],"about_ca_topic_score_codex":0.014075361,"about_ca_topic_score_gemma":0.015410141,"teacher_disagreement_score":0.014075361,"about_ca_system_score_codex":0.00029597883,"about_ca_system_score_gemma":0.0002303975,"threshold_uncertainty_score":0.027986884},"labels":[],"label_agreement":null},{"id":"W2600777534","doi":"10.1002/2016gl072235","title":"Revisiting the contribution of transpiration to global terrestrial evapotranspiration","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":539,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Core Research for Evolutional Science and Technology; Raymond and Beverly Sackler Institute for Biological, Physical and Engineering Sciences, Yale University; National Science Foundation; Yale University; Ministry of Environment; Ministry of Education, Culture, Sports, Science and Technology","keywords":"Evapotranspiration; Transpiration; Environmental science; Water cycle; Vegetation (pathology); Leaf area index; Interception; Scale (ratio); Atmospheric sciences; Flux (metallurgy); Climatology; Geology; Ecology; Geography","score_opus":0.03180343089965986,"score_gpt":0.3170317513800366,"score_spread":0.2852283204803767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2600777534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95391387,0.00039053545,0.044127002,0.00014106363,0.000022540968,0.000009756661,0.00015033697,0.000115907475,0.0011290031],"genre_scores_gemma":[0.993473,0.000114277806,0.0061224564,0.000013226485,0.0000063950133,0.0000045645256,0.000102675534,0.000036424924,0.00012698388],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993134,0.000017998838,0.0000046137193,0.000026928672,0.000012229541,0.000006817393],"domain_scores_gemma":[0.9998142,0.000116040195,0.000017701737,0.000018105215,0.000025617861,0.00000831606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004659358,0.0003674855,0.00020757313,0.00034076362,0.0001475385,0.00044121547,0.0002973991,0.00023480244,0.00035817875],"category_scores_gemma":[0.001150814,0.00018226403,0.00020787159,0.0004507985,0.00019141214,0.0009442546,0.0002961674,0.00031152155,0.0000793575],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018684193,0.000095963085,0.15656662,0.00017737146,0.00020326821,0.00023985178,0.00018989832,0.5468376,0.15025128,0.005907493,0.0007048759,0.1386389],"study_design_scores_gemma":[0.000010410336,0.000022739587,0.05641003,0.000009193566,0.000027880129,0.000030082596,0.000039045073,0.9286964,0.011945975,0.002032296,0.0007620383,0.000013961783],"about_ca_topic_score_codex":0.0056936033,"about_ca_topic_score_gemma":0.006736485,"teacher_disagreement_score":0.0056936033,"about_ca_system_score_codex":0.0003069203,"about_ca_system_score_gemma":0.00033195678,"threshold_uncertainty_score":0.011320949},"labels":[],"label_agreement":null},{"id":"W2602279165","doi":"10.1002/2016gl072394","title":"The projected demise of Barnes Ice Cap: Evidence of an unusually warm 21st century Arctic","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Simon Fraser University","funders":"Lawrence Livermore National Laboratory; Natural Sciences and Engineering Research Council of Canada; Compute Canada; Western Canada Research Grid; Baylor University; Simon Fraser University; National Aeronautics and Space Administration; U.S. Department of Energy; National Science Foundation","keywords":"Ice sheet; Ice caps; Ice-sheet model; Arctic ice pack; Ice stream; Geology; Climatology; Cryosphere; Glacial period; Sea ice; Ice core; Greenland ice sheet; Demise; Antarctic sea ice; Oceanography; Glacier; Geomorphology","score_opus":0.0681180209582804,"score_gpt":0.351437736076345,"score_spread":0.2833197151180646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2602279165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9903441,0.0004102971,0.0004903346,0.0022641497,0.0000814223,0.0000036772021,0.0009404028,0.000030338108,0.0054351334],"genre_scores_gemma":[0.99874556,0.00016412296,0.00022223231,0.00011841215,0.000038787857,0.0000019990828,0.00031471532,0.000002778868,0.0003913882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999206,0.00001185565,0.00000374739,0.000013915956,0.000022890621,0.000027067163],"domain_scores_gemma":[0.9993844,0.000035717258,0.00025555823,0.00003012802,0.00019414388,0.00009999542],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035312187,0.00013598186,0.00007547443,0.00031021662,0.00041366077,0.00060550583,0.00019359436,0.00035953813,0.0022492474],"category_scores_gemma":[0.0008103062,0.00006584687,0.000118329874,0.00037405227,0.00032551217,0.00052593363,0.0004553285,0.00033747987,0.0002716263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005539766,0.00004865259,0.9345732,0.000092531416,0.000060210594,0.0010166747,0.0008006453,0.0049607065,0.012031359,0.0047054566,0.0066676238,0.03448901],"study_design_scores_gemma":[0.000011378025,0.00007725363,0.9744621,0.000024495666,0.000020196258,0.00042500402,0.00098598,0.0042673885,0.0021241957,0.0015797465,0.016005402,0.00001680997],"about_ca_topic_score_codex":0.01780946,"about_ca_topic_score_gemma":0.038093407,"teacher_disagreement_score":0.01780946,"about_ca_system_score_codex":0.0006851557,"about_ca_system_score_gemma":0.00044621245,"threshold_uncertainty_score":0.035411596},"labels":[],"label_agreement":null},{"id":"W2603493125","doi":"10.1002/2017gl072754","title":"The role of sulfur dioxide in stratospheric aerosol formation evaluated by using in situ measurements in the tropical lower stratosphere","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Waterloo","funders":"Canadian Space Agency; National Oceanic and Atmospheric Administration; Langley Research Center; University of Waterloo; National Aeronautics and Space Administration","keywords":"Stratosphere; Tropopause; Environmental science; Atmospheric sciences; Troposphere; Climatology; Aerosol; Meteorology; Geology; Geography","score_opus":0.055942154542703404,"score_gpt":0.31152790581628464,"score_spread":0.25558575127358124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2603493125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993223,0.000032865606,0.00031793697,0.000008941047,0.0000026588145,0.000002416894,0.000093218325,0.000006409665,0.00021334755],"genre_scores_gemma":[0.99943215,0.000032139298,0.00041976833,0.0000043501163,0.0000026156526,0.000001918127,0.000079132784,0.0000017190241,0.000026247446],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999244,0.000019882254,0.000005760541,0.00002252267,0.000015984924,0.00001141439],"domain_scores_gemma":[0.99987996,0.00004162061,0.000030190282,0.000011388855,0.000025453457,0.0000113427],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023261829,0.00035050692,0.00014037084,0.0002970327,0.00023853034,0.0003688649,0.00019067021,0.00026250473,0.00030440572],"category_scores_gemma":[0.00024119139,0.00013919552,0.00024516604,0.00027012688,0.0001560252,0.0003416087,0.00016676406,0.000121436584,0.000041302734],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047710305,0.00012327082,0.42249587,0.000087844324,0.0001786112,0.00009837862,0.0002328895,0.005281369,0.5649017,0.00012476505,0.000086996784,0.0059112497],"study_design_scores_gemma":[0.000040228202,0.00042294565,0.7182138,0.000015539037,0.0002813111,0.00009687368,0.0005372999,0.048176367,0.23135647,0.0001707796,0.00066332653,0.000024933397],"about_ca_topic_score_codex":0.009918833,"about_ca_topic_score_gemma":0.012601124,"teacher_disagreement_score":0.009918833,"about_ca_system_score_codex":0.0002678881,"about_ca_system_score_gemma":0.00015544916,"threshold_uncertainty_score":0.019722223},"labels":[],"label_agreement":null},{"id":"W2604090828","doi":"10.1002/2016gl072397","title":"Rapid decline in river icings detected in Arctic Alaska: Implications for a changing hydrologic cycle and river ecosystems","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Gillings School of Public Health; National Aeronautics and Space Administration; National Science Foundation","keywords":"Ephemeral key; Arctic; Arctic ecology; Ecosystem; Environmental science; Climate change; Physical geography; Oceanography; Climatology; Hydrology (agriculture); Geology; Ecology; Geography","score_opus":0.07455953590527029,"score_gpt":0.32254290682148296,"score_spread":0.24798337091621267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604090828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985274,0.000074776886,0.00008932321,0.00002984694,0.00000337136,0.0000017151241,0.00045398463,0.0000067342276,0.0008128288],"genre_scores_gemma":[0.99933213,0.000045875524,0.00010205173,0.000009137348,0.0000036844003,0.0000020655655,0.00034958252,0.0000015550912,0.00015392153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999033,0.000015164299,0.000013051589,0.000030455272,0.000021057842,0.000017015895],"domain_scores_gemma":[0.9993598,0.00006629034,0.00022067258,0.000051775634,0.00021252032,0.000088985296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036179263,0.00009207534,0.00014207701,0.0007479353,0.00040501027,0.000608891,0.00014313697,0.0001887528,0.0009083712],"category_scores_gemma":[0.0007469406,0.00009171036,0.00012329331,0.0007224057,0.00022596444,0.0003297108,0.00025719494,0.00018387694,0.00012614048],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027928027,0.000009770925,0.9950789,0.000008401644,0.00001388003,0.000026016394,0.00013214383,0.00014059247,0.0019152157,0.000019438514,0.00012634904,0.0025013175],"study_design_scores_gemma":[2.8708763e-7,0.00000562334,0.9993481,0.0000023338823,0.000002725776,0.000015351388,0.0001973835,0.00017286511,0.00007747827,0.000008711892,0.0001681108,0.0000010181527],"about_ca_topic_score_codex":0.056333367,"about_ca_topic_score_gemma":0.09125975,"teacher_disagreement_score":0.056333367,"about_ca_system_score_codex":0.0004350019,"about_ca_system_score_gemma":0.00032330392,"threshold_uncertainty_score":0.112010956},"labels":[],"label_agreement":null},{"id":"W2604783552","doi":"10.1002/2017gl072785","title":"Time‐evolving seismic tomography: The method and its application to the 1989 Loma Prieta and 2014 South Napa earthquake area, California","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"NAPA; Seismology; Geology; Window (computing); Tomography; Seismic tomography; Geophysical imaging; Geophysics; Physics","score_opus":0.023483791424980863,"score_gpt":0.2867231938723975,"score_spread":0.2632394024474166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2604783552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.71210843,0.00020968785,0.2845145,0.00024113458,0.000018445326,0.00008159668,0.000223929,0.00038411532,0.0022181517],"genre_scores_gemma":[0.84204835,0.00018154898,0.15688679,0.000013939989,0.000011788784,0.00003425819,0.00015513327,0.00003095755,0.0006373406],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999404,0.000012834068,0.0000034914556,0.000020344176,0.000015950687,0.000007031141],"domain_scores_gemma":[0.9998565,0.00004595224,0.000028701106,0.000013647808,0.000042067928,0.000013116861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023221388,0.00022679455,0.00012015595,0.00055911293,0.00024568106,0.000353509,0.00056867726,0.00029042875,0.00041207],"category_scores_gemma":[0.0010609516,0.0001735506,0.00016529886,0.00070639147,0.00018764724,0.0003545139,0.0002566093,0.0002350919,0.000047733964],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001727975,0.00012772031,0.056672134,0.00006887478,0.00007067041,0.00073096383,0.00038534668,0.603961,0.030815674,0.004028313,0.0009672179,0.30199933],"study_design_scores_gemma":[0.000008530992,0.000013079851,0.009956013,0.0000034074326,0.000009377221,0.00006492052,0.000060031187,0.98726594,0.0018124073,0.0003436507,0.0004524817,0.000010069313],"about_ca_topic_score_codex":0.05618076,"about_ca_topic_score_gemma":0.056263193,"teacher_disagreement_score":0.05618076,"about_ca_system_score_codex":0.00044153922,"about_ca_system_score_gemma":0.000568677,"threshold_uncertainty_score":0.11170751},"labels":[],"label_agreement":null},{"id":"W2608253988","doi":"10.1002/2017gl073056","title":"Microphysical explanation of the RH‐dependent water affinity of biogenic organic aerosol and its importance for climate","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":145,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; McGill University","funders":"H2020 European Research Council; Natural Environment Research Council; Horizon 2020 Framework Programme; Norges Forskningsråd; NordForsk; Natural Sciences and Engineering Research Council of Canada; Knut och Alice Wallenbergs Stiftelse; Svenska Forskningsrådet Formas; National Oceanic and Atmospheric Administration; Sight Research UK; U.S. Environmental Protection Agency; National Supercomputing Centre Singapore; Georgia Institute of Technology; U.S. Department of Energy; Electric Power Research Institute; Vetenskapsrådet; National Science Foundation","keywords":"Isoprene; Aerosol; Environmental science; Atmospheric sciences; Atmosphere (unit); Climate model; Environmental chemistry; Climate change; Meteorology; Chemistry; Geology; Oceanography; Polymer","score_opus":0.03628900993836692,"score_gpt":0.2825884886879513,"score_spread":0.24629947874958436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608253988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9615623,0.0015376185,0.030655764,0.00034093732,0.000050557184,0.000037313494,0.00038395287,0.00012881818,0.0053027733],"genre_scores_gemma":[0.9989973,0.00019181629,0.00052923936,0.000012348355,0.000017047752,0.000007222053,0.00004220856,0.0000094301,0.0001935519],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995244,0.000005868521,0.000002315137,0.000017669303,0.000008952796,0.000012877232],"domain_scores_gemma":[0.9999094,0.000033476666,0.000016815477,0.000020271946,0.000011128925,0.0000089186815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017860683,0.0004285484,0.00018636433,0.0002654704,0.00020174013,0.00022347752,0.00045446103,0.0003950668,0.0008547458],"category_scores_gemma":[0.00024439517,0.0001567015,0.00035453876,0.00012985723,0.00037128438,0.0006635136,0.00027856798,0.00028361284,0.00014306234],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017574226,0.0001440277,0.042494193,0.000287183,0.0001836032,0.000781197,0.00014361377,0.26084676,0.6519317,0.027641283,0.0006725514,0.014698187],"study_design_scores_gemma":[0.000027804052,0.00008155202,0.05803832,0.0000084601115,0.000058326248,0.00014377548,0.00006259235,0.87717307,0.048481967,0.014696111,0.0011949299,0.00003305985],"about_ca_topic_score_codex":0.0036703355,"about_ca_topic_score_gemma":0.001958118,"teacher_disagreement_score":0.0036703355,"about_ca_system_score_codex":0.00042342657,"about_ca_system_score_gemma":0.00017457729,"threshold_uncertainty_score":0.007297933},"labels":[],"label_agreement":null},{"id":"W2608846545","doi":"10.1002/2017gl073323","title":"Diagenetic silica enrichment and late‐stage groundwater activity in Gale crater, Mars","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":128,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; University of Guelph","funders":"Science and Technology Facilities Council; Jet Propulsion Laboratory; UK Space Agency; Danmarks Frie Forskningsfond; Villum Fonden; Natur og Univers, Det Frie Forskningsråd; California Institute of Technology; National Aeronautics and Space Administration","keywords":"Diagenesis; Geology; Impact crater; Bedrock; Geochemistry; Sedimentary rock; Aeolian processes; Mars Exploration Program; Deposition (geology); Sedimentary depositional environment; Geomorphology; Astrobiology; Structural basin","score_opus":0.04436853330567238,"score_gpt":0.31813015402597905,"score_spread":0.2737616207203067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2608846545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999681,0.000058420293,0.000015329155,0.000012369457,4.824602e-7,0.0000013593867,0.00008936596,0.0000040287173,0.00013767653],"genre_scores_gemma":[0.99975795,0.000035374094,0.000044442066,0.000005184556,0.0000011283689,0.0000013323474,0.000076711265,0.0000010211604,0.000076862125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993575,0.000011812625,0.000004589839,0.000017819786,0.000009268362,0.000020691452],"domain_scores_gemma":[0.9998573,0.000022406288,0.00005364425,0.000009902343,0.000025882468,0.000030841955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012366468,0.00024990164,0.00015212075,0.001698382,0.00040545705,0.0005234917,0.00019566053,0.00028167988,0.0007378022],"category_scores_gemma":[0.00024363672,0.00019083628,0.00015230336,0.0006589944,0.0004988553,0.00024429988,0.00044189193,0.00012074978,0.000099546545],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023818447,0.000025245075,0.9727227,0.000023714196,0.0000724099,0.00039078417,0.0007302439,0.00038569234,0.018519264,0.000058672827,0.00010125581,0.0067317025],"study_design_scores_gemma":[0.0000023000146,0.000015507943,0.9994122,0.0000016524538,0.0000032865787,0.00003675169,0.000127729,0.00006768083,0.00021268515,0.0000069983944,0.00011203423,0.0000013207432],"about_ca_topic_score_codex":0.04641462,"about_ca_topic_score_gemma":0.074148245,"teacher_disagreement_score":0.04641462,"about_ca_system_score_codex":0.0006930022,"about_ca_system_score_gemma":0.00020113146,"threshold_uncertainty_score":0.09228891},"labels":[],"label_agreement":null},{"id":"W2610129872","doi":"10.1002/2017gl073042","title":"Seasonally derived components of the Canada Basin halocline","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Polar Programs; Woods Hole Oceanographic Institution; Division of Polar Programs; National Science Foundation","keywords":"Halocline; Stratification (seeds); Oceanography; Canada Basin; Geology; Arctic; Climatology; Sea ice; Hydrography; Mixed layer; Environmental science; Salinity","score_opus":0.03280882531232745,"score_gpt":0.2670832254504653,"score_spread":0.23427440013813786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2610129872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99350244,0.00010197479,0.00038317995,0.00007348788,0.000008584202,0.000008749313,0.003166349,0.000082113256,0.0026732346],"genre_scores_gemma":[0.99786574,0.00004951721,0.00019217329,0.000011282302,0.0000015603415,0.000003503437,0.0014444259,0.000014067054,0.0004177774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994576,0.0000030094084,0.0000014521135,0.000013364686,0.000015546391,0.00002098952],"domain_scores_gemma":[0.99983764,0.000012794599,0.000012549689,0.0000066065654,0.0000857767,0.00004464263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000102969774,0.00028225087,0.00013075296,0.0005243454,0.00076110166,0.00072891574,0.00035261267,0.0002845996,0.0016951818],"category_scores_gemma":[0.000434312,0.00019548691,0.00029724883,0.0006763174,0.0002526553,0.00015150264,0.0002771087,0.00024368482,0.00015721154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046621732,0.000077223216,0.84695125,0.00010203677,0.0002468618,0.00020745661,0.0004091046,0.09448515,0.031619154,0.0019364064,0.0054917904,0.018007342],"study_design_scores_gemma":[0.000023550234,0.000008942873,0.9390989,0.000011973417,0.000021302441,0.000019192054,0.00017206148,0.056863006,0.0016097726,0.00012393478,0.0020206277,0.000026821239],"about_ca_topic_score_codex":0.9049655,"about_ca_topic_score_gemma":0.92469037,"teacher_disagreement_score":0.09503448,"about_ca_system_score_codex":0.0050959196,"about_ca_system_score_gemma":0.0044695577,"threshold_uncertainty_score":0.19118828},"labels":[],"label_agreement":null},{"id":"W2611534766","doi":"10.1002/2016gl072452","title":"Efficiency of turbulent mixing in the abyssal ocean circulation","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":113,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Australian Research Council; Engineering and Physical Sciences Research Council","keywords":"Downwelling; Abyssal zone; Mixing (physics); Upwelling; Turbulence; Circulation (fluid dynamics); Geology; Thermohaline circulation; Deep sea; Oceanography; Climatology; Meteorology; Atmospheric sciences; Environmental science; Mechanics; Physics","score_opus":0.036858226418807594,"score_gpt":0.296023031921197,"score_spread":0.2591648055023894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2611534766","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925953,0.00004025723,0.00014247486,0.000009521927,7.9566377e-7,7.188511e-7,0.0000504481,0.0000065580507,0.00048963993],"genre_scores_gemma":[0.99976,0.00002272684,0.00007104458,0.0000011956351,0.000001354212,5.7409727e-7,0.000061484716,0.0000021826536,0.00007947205],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993145,0.000012314005,0.0000060376938,0.000019690264,0.0000162168,0.000014274214],"domain_scores_gemma":[0.9997328,0.00008554584,0.00007275297,0.000024808489,0.000052348907,0.000031768148],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020301579,0.00018068131,0.00011069159,0.0005557651,0.00015179878,0.00060659467,0.000100105804,0.00009418442,0.00056309055],"category_scores_gemma":[0.00080761634,0.000111837006,0.00013062138,0.00028175188,0.00028775854,0.0002636598,0.00038562165,0.0001428505,0.00012144561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044940473,0.00006103653,0.80270743,0.00006913344,0.0002235536,0.00033652183,0.0004759851,0.037589133,0.1328421,0.00337477,0.00031908762,0.021551792],"study_design_scores_gemma":[0.000013087309,0.000033314034,0.9665494,0.0000049566734,0.000014544387,0.00005541307,0.00008366844,0.027877657,0.0047822087,0.0003017531,0.0002725912,0.000011403464],"about_ca_topic_score_codex":0.010445964,"about_ca_topic_score_gemma":0.003819725,"teacher_disagreement_score":0.010445964,"about_ca_system_score_codex":0.00037460632,"about_ca_system_score_gemma":0.00017396595,"threshold_uncertainty_score":0.020770311},"labels":[],"label_agreement":null},{"id":"W2614371085","doi":"10.1002/2017gl072946","title":"Validation of the Soil Moisture Active Passive (SMAP) satellite soil moisture retrieval in an Arctic tundra environment","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Moisture and Remote Sensing","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wilfrid Laurier University; University of Guelph","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; Canadian Space Agency; Jet Propulsion Laboratory; European Centre for Medium-Range Weather Forecasts; W. Garfield Weston Foundation; National Aeronautics and Space Administration; California Institute of Technology; ArcticNet; Polar Knowledge Canada","keywords":"Environmental science; Brightness temperature; Water content; Moisture; Satellite; Tundra; Remote sensing; Atmospheric sciences; Soil science; Brightness; Meteorology; Arctic; Geology; Geography","score_opus":0.024517943583534596,"score_gpt":0.28818364722796175,"score_spread":0.26366570364442715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2614371085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964031,0.000027742828,0.0017717495,0.000018661249,0.000012554691,0.000011084644,0.000846389,0.00016633113,0.0007423545],"genre_scores_gemma":[0.99547416,0.000021387352,0.0027651226,0.000016763,0.0000051488983,0.000007210728,0.0015408611,0.00002043822,0.00014905377],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995608,0.00011583389,0.000027304739,0.00013606902,0.000115314215,0.000044694374],"domain_scores_gemma":[0.9994672,0.00009381882,0.000060683727,0.00012196402,0.00019770677,0.00005874297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010855425,0.00054473715,0.00032840826,0.00044418284,0.0003852081,0.00070721086,0.0005804664,0.00033733336,0.00033599656],"category_scores_gemma":[0.0016940959,0.00016551114,0.00040187617,0.000675736,0.00023308185,0.00055586157,0.0004425312,0.00027576167,0.0002453358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016955364,0.0006251098,0.6315928,0.00013562686,0.0005863667,0.00064864784,0.00035170748,0.17914273,0.118473046,0.00047758556,0.0014309165,0.06483998],"study_design_scores_gemma":[0.00025490602,0.00040012915,0.5909921,0.000028742883,0.00012865609,0.00017586545,0.0003208094,0.36166203,0.04374626,0.00015812508,0.0020810657,0.0000512718],"about_ca_topic_score_codex":0.057650324,"about_ca_topic_score_gemma":0.059298832,"teacher_disagreement_score":0.057650324,"about_ca_system_score_codex":0.0004212698,"about_ca_system_score_gemma":0.0006113963,"threshold_uncertainty_score":0.11462951},"labels":[],"label_agreement":null},{"id":"W2615101319","doi":"10.1002/2017gl073322","title":"The rapid yet uneven turnover of Earth's groundwater","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; University of Calgary","funders":"National Science Foundation","keywords":"Groundwater; Aquifer; Groundwater recharge; Geology; Hydrology (agriculture); Weathering; Environmental science; Last Glacial Maximum; Glacial period; Geomorphology","score_opus":0.03465870830326272,"score_gpt":0.28227485646975553,"score_spread":0.2476161481664928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2615101319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99227726,0.0006400769,0.003406171,0.00018309797,0.000009688154,0.0000040199025,0.00096206396,0.00009794297,0.0024196447],"genre_scores_gemma":[0.99946636,0.000083178355,0.00019144683,0.00001477454,0.0000029034004,0.0000010329209,0.00015391667,0.000003914546,0.00008246968],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985766,0.00001601309,0.000008666238,0.00004944383,0.00003960236,0.000028573191],"domain_scores_gemma":[0.9997639,0.000050601626,0.00007629456,0.000026821372,0.000054878852,0.000027608165],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002473187,0.00008095112,0.00018089643,0.0006948807,0.00021046022,0.0005829875,0.00017458794,0.00021510625,0.0010689308],"category_scores_gemma":[0.0007175496,0.00010067789,0.00009503109,0.000792643,0.000322482,0.00063530385,0.00035044362,0.00014304597,0.00019998943],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014287395,0.000020536203,0.86439055,0.00015646237,0.00016226374,0.0002894651,0.0002148727,0.0108794775,0.057745762,0.0030618103,0.0019114055,0.061024487],"study_design_scores_gemma":[0.000006816178,0.0000665072,0.9596842,0.000023238708,0.000034801364,0.00037588773,0.00040231142,0.019376254,0.010037084,0.0048128315,0.0051557976,0.000024288689],"about_ca_topic_score_codex":0.0047868798,"about_ca_topic_score_gemma":0.005119297,"teacher_disagreement_score":0.0047868798,"about_ca_system_score_codex":0.00046843925,"about_ca_system_score_gemma":0.00014899766,"threshold_uncertainty_score":0.009518027},"labels":[],"label_agreement":null},{"id":"W2617856857","doi":"10.1002/2017gl073583","title":"Melting glaciers stimulate large summer phytoplankton blooms in southwest Greenland waters","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":137,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Meltwater; Oceanography; Fjord; Glacier; Glacial period; Phytoplankton; Geology; Greenland ice sheet; Algal bloom; Ice sheet; Sea ice; Environmental science; Physical geography; Nutrient; Geography; Ecology; Geomorphology","score_opus":0.06723449615044398,"score_gpt":0.3209037521424009,"score_spread":0.25366925599195694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2617856857","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992361,0.000036177677,0.00001366581,0.000043358057,0.0000022298593,0.0000024590192,0.00015706792,0.000012806268,0.00049618183],"genre_scores_gemma":[0.9993777,0.000042746127,0.0000612101,0.000042317923,0.0000037217667,0.0000029215685,0.00019515984,0.0000038761973,0.00027029245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.0000075907774,0.0000031782247,0.000009688302,0.000007820941,0.00001780005],"domain_scores_gemma":[0.9998005,0.00002762063,0.00006969614,0.00001326198,0.000028186654,0.00006074398],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011815838,0.00019356095,0.00019708821,0.0003813075,0.00037463917,0.00033648268,0.00012477359,0.00017983826,0.0015150396],"category_scores_gemma":[0.00023005113,0.000119028926,0.00016162777,0.00026670436,0.00022623347,0.00017226709,0.00036263518,0.0001702387,0.00025107714],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005728624,0.00011761084,0.84711605,0.000064253836,0.0000558231,0.00032311463,0.0006385259,0.0006599258,0.14035082,0.0000697514,0.0011956318,0.008835712],"study_design_scores_gemma":[0.000005289762,0.000037250065,0.99818027,0.0000030626795,0.0000037820487,0.000013595829,0.00022693603,0.0001430277,0.001119659,0.000018654442,0.0002468336,0.0000017175554],"about_ca_topic_score_codex":0.031946756,"about_ca_topic_score_gemma":0.091420844,"teacher_disagreement_score":0.031946756,"about_ca_system_score_codex":0.001003907,"about_ca_system_score_gemma":0.00053307664,"threshold_uncertainty_score":0.06352162},"labels":[],"label_agreement":null},{"id":"W2618216561","doi":"10.1002/2017gl073519","title":"A global enhancement of hydrogen cyanide in the lower stratosphere throughout 2016","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Toronto","funders":"Canadian Space Agency","keywords":"Stratosphere; Troposphere; Atmospheric sciences; Climatology; Environmental science; Latitude; Hydrogen cyanide; Polar vortex; Polar; Geology; Chemistry; Physics","score_opus":0.03318334632365209,"score_gpt":0.32321365641956273,"score_spread":0.2900303100959106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618216561","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945452,0.0005174851,0.0001679474,0.00041168724,0.000051572304,0.0000071508216,0.0018479035,0.000027213913,0.002423833],"genre_scores_gemma":[0.9978522,0.00020052058,0.0000890319,0.000059592705,0.00002068186,0.0000031177149,0.0011655213,0.00000419492,0.0006051635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993837,0.0000041731173,0.0000047054227,0.000020046884,0.000013342162,0.000019367686],"domain_scores_gemma":[0.99984777,0.0000049106247,0.00005202464,0.000010506976,0.000052333908,0.00003255181],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017841517,0.00017829018,0.00017521015,0.00039037457,0.0002822646,0.00050102355,0.00010317835,0.00020661663,0.0007244487],"category_scores_gemma":[0.00016235792,0.0000849156,0.0002117234,0.0004493418,0.00019206591,0.0003131426,0.0004293218,0.00018712338,0.00016177147],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004717669,0.00006036307,0.9005385,0.00011545444,0.00021128218,0.00032218805,0.00054726127,0.0010687591,0.074497,0.00046610125,0.0019615344,0.019739721],"study_design_scores_gemma":[0.0000030373708,0.000022229988,0.9947582,0.0000075063317,0.000017060798,0.00002983224,0.0001485903,0.000312912,0.0021944332,0.00004155953,0.0024613983,0.0000031067323],"about_ca_topic_score_codex":0.027149092,"about_ca_topic_score_gemma":0.02905114,"teacher_disagreement_score":0.027149092,"about_ca_system_score_codex":0.00057082745,"about_ca_system_score_gemma":0.0004872773,"threshold_uncertainty_score":0.05398214},"labels":[],"label_agreement":null},{"id":"W2618514174","doi":"10.1002/2017gl073708","title":"Angular normalization of GOME‐2 Sun‐induced chlorophyll fluorescence observation as a better proxy of vegetation productivity","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Space Agency","keywords":"Primary production; Boreal ecosystem; Atmospheric sciences; Chlorophyll fluorescence; Environmental science; Deciduous; Canopy; Remote sensing; Fluorescence; Geology; Taiga; Physics; Ecosystem; Geography; Optics; Botany; Forestry; Ecology","score_opus":0.03295627871591546,"score_gpt":0.2983463189059218,"score_spread":0.26539004019000634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618514174","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9790956,0.00013892705,0.017909797,0.00004600623,0.000038275575,0.000017103213,0.0008590126,0.00051315123,0.0013820224],"genre_scores_gemma":[0.99027914,0.000054586064,0.007963613,0.000019838773,0.0000073858846,0.000014263654,0.0013849473,0.000058047517,0.00021819957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998,0.000047535912,0.000008028956,0.00007606968,0.000043757904,0.000024624549],"domain_scores_gemma":[0.99975353,0.00006228969,0.000042796593,0.00006124123,0.00006331729,0.000016920256],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054716604,0.00046712026,0.00026705113,0.0005118469,0.00014285935,0.0003345684,0.00019710457,0.0001599827,0.00066010514],"category_scores_gemma":[0.0010431719,0.0001045698,0.00034759042,0.000821903,0.0001408111,0.0003380205,0.00019600784,0.00027470285,0.00019543454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035867264,0.00014659236,0.67851055,0.00009732922,0.00047764127,0.000089317204,0.00010471728,0.08817441,0.15594672,0.000767073,0.0021866572,0.0731403],"study_design_scores_gemma":[0.000014357165,0.000029471748,0.88380325,0.0000049542186,0.00003180153,0.000035118428,0.000040622363,0.10241373,0.012248936,0.00018407394,0.0011706601,0.000023030636],"about_ca_topic_score_codex":0.013288755,"about_ca_topic_score_gemma":0.01989488,"teacher_disagreement_score":0.013288755,"about_ca_system_score_codex":0.000373979,"about_ca_system_score_gemma":0.0003277783,"threshold_uncertainty_score":0.026422858},"labels":[],"label_agreement":null},{"id":"W2618616759","doi":"10.1002/2017gl072803","title":"Strain release at the trench during shallow slow slip: The example of Nicoya Peninsula, Costa Rica","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration; National Science Foundation","keywords":"Subduction; Trench; Geology; Seismology; Slip (aerodynamics); Episodic tremor and slip; Seafloor spreading; Geophysics; Tectonics","score_opus":0.05895102504109099,"score_gpt":0.2932685783590058,"score_spread":0.23431755331791485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2618616759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983102,0.000050921863,0.00007462486,0.00002897677,0.0000010162297,0.000004906778,0.0002565473,0.0000130109765,0.0012597167],"genre_scores_gemma":[0.99945325,0.000034283214,0.000104849314,0.000004219773,0.0000013988516,0.000002744851,0.00018497308,0.0000018349491,0.00021228778],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000010687832,0.000003583432,0.000017787428,0.000011951861,0.000018159872],"domain_scores_gemma":[0.999845,0.000017802917,0.00004415426,0.000018860595,0.00005648595,0.000017655986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011243087,0.00015278217,0.00012387983,0.00068161264,0.00028822065,0.0004533043,0.00020327477,0.00018104054,0.0006412339],"category_scores_gemma":[0.00041646493,0.0000628985,0.00008972715,0.000802558,0.00022690443,0.00017846058,0.00038230632,0.00010503541,0.0000903225],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009833212,0.000034636763,0.9683266,0.00004295771,0.000059054353,0.0007566292,0.0012030824,0.0035886283,0.008156736,0.00018906621,0.0004945525,0.017049795],"study_design_scores_gemma":[0.0000015696528,0.000006451332,0.99558324,0.0000059065965,0.000007667527,0.000052281783,0.0005954802,0.0028767148,0.00033704174,0.000015877655,0.00051383907,0.000003936526],"about_ca_topic_score_codex":0.20716245,"about_ca_topic_score_gemma":0.31279865,"teacher_disagreement_score":0.20716245,"about_ca_system_score_codex":0.00092922425,"about_ca_system_score_gemma":0.00040399306,"threshold_uncertainty_score":0.41191322},"labels":[],"label_agreement":null},{"id":"W2619506828","doi":"10.1002/2017gl072686","title":"Evaluating the size and extent of paleolakes in central Tibet during the late Pleistocene","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Nanyang Technological University; National Research Foundation Singapore; National Research Foundation; Chinese Academy of Sciences; Earth Observatory of Singapore; National Science Foundation","keywords":"Shore; Geology; Pleistocene; Interglacial; Chronology; Period (music); Marine isotope stage; Elevation (ballistics); Quaternary; Oceanography; Physical geography; Paleontology; Climatology; Geography","score_opus":0.0658048701446705,"score_gpt":0.35200709268243313,"score_spread":0.2862022225377626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619506828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995832,0.00004037202,0.00003170108,0.0000099650615,0.0000010178921,0.0000011357781,0.00011257869,0.0000014981451,0.00021837522],"genre_scores_gemma":[0.9996923,0.000019329065,0.00002940208,0.000003040261,0.0000014183809,0.0000015152939,0.00016099545,7.5316416e-7,0.00009118965],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992454,0.000014295463,0.0000067444607,0.0000208823,0.000009656665,0.000023853701],"domain_scores_gemma":[0.9997092,0.00004515092,0.000076897675,0.000010865506,0.00007561039,0.00008234297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043763843,0.0002080929,0.00011512972,0.0017002594,0.0006799132,0.0006509387,0.0002629115,0.0002656276,0.001332513],"category_scores_gemma":[0.0005770942,0.00015266509,0.00016806136,0.0013622774,0.00048780412,0.0004051651,0.00037781618,0.00019361632,0.000112791466],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113739596,0.000014822921,0.9904428,0.00001524701,0.000031488107,0.00012440373,0.00082761684,0.0004786292,0.002686188,0.000083719046,0.00008552305,0.0050957156],"study_design_scores_gemma":[0.0000019583883,0.000010877398,0.9990202,0.000004048231,0.000005277266,0.000015599695,0.00034755896,0.00040489127,0.00007764358,0.000014538268,0.000095785166,0.000001655927],"about_ca_topic_score_codex":0.069201834,"about_ca_topic_score_gemma":0.16701351,"teacher_disagreement_score":0.069201834,"about_ca_system_score_codex":0.00083957956,"about_ca_system_score_gemma":0.00043102563,"threshold_uncertainty_score":0.13759804},"labels":[],"label_agreement":null},{"id":"W2619624483","doi":"10.1002/2017gl073426","title":"An Argo mixed layer climatology and database","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":381,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Natural Science Foundation of China","keywords":"Argo; Mixed layer; Climatology; Layer (electronics); Database; Geology; Meteorology; Environmental science; Computer science; Geography; Materials science","score_opus":0.05219957411106854,"score_gpt":0.3287462891151968,"score_spread":0.2765467150041283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2619624483","genre_codex":"dataset","genre_gemma":"dataset","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"dataset","genre_consensus":"dataset","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04701161,0.00022459531,0.006253222,0.00015863543,0.000078051264,0.00024412187,0.92966074,0.0053259903,0.011042989],"genre_scores_gemma":[0.060244802,0.00012487388,0.015137773,0.00007240439,0.000036122787,0.0002773914,0.92199,0.00036868552,0.0017479506],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99943465,0.000054449163,0.00011215029,0.00014387436,0.00020024567,0.00005466149],"domain_scores_gemma":[0.99851567,0.00011869691,0.00024925597,0.00036481392,0.000566923,0.0001845639],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00090592593,0.00073500635,0.0006968254,0.0038656215,0.0003626326,0.0013683497,0.0010839083,0.00056595117,0.008636507],"category_scores_gemma":[0.0016690705,0.000356639,0.00041127036,0.004664525,0.0001677287,0.00093281816,0.0005907124,0.0005207721,0.0076109064],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000999248,0.0005176027,0.15839571,0.0011680287,0.00051424466,0.0007953006,0.00028392952,0.043415684,0.011723565,0.0052617285,0.62625736,0.15066764],"study_design_scores_gemma":[0.00067409006,0.00013694186,0.27037978,0.00027037077,0.00017202734,0.00037064916,0.00039778216,0.08387395,0.010766408,0.0034000776,0.6293265,0.00023145563],"about_ca_topic_score_codex":0.017404264,"about_ca_topic_score_gemma":0.012446558,"teacher_disagreement_score":0.017404264,"about_ca_system_score_codex":0.00065241684,"about_ca_system_score_gemma":0.0010042456,"threshold_uncertainty_score":0.03460592},"labels":[],"label_agreement":null},{"id":"W2620116606","doi":"10.1002/2017gl073270","title":"Depletion of ozone and reservoir species of chlorine and nitrogen oxide in the lower Antarctic polar vortex measured from aircraft","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Toronto","funders":"Deutsche Forschungsgemeinschaft; Helmholtz-Gemeinschaft","keywords":"Polar vortex; Ozone depletion; Stratosphere; Ozone; Atmospheric sciences; Reactive nitrogen; Environmental science; Trace gas; Altitude (triangle); Nitrogen oxide; Atmospheric chemistry; Nitrogen; NOx; Geology; Chemistry; Meteorology; Physics","score_opus":0.039504485119688106,"score_gpt":0.2728795548128048,"score_spread":0.2333750696931167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2620116606","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995154,0.000023404711,0.000046626064,0.000005816667,0.0000013279172,0.0000017536718,0.0001518952,0.0000038647418,0.0002499707],"genre_scores_gemma":[0.9993604,0.000027475226,0.000110761495,0.000009036595,0.000002424094,0.0000032592386,0.0003834355,0.0000021688609,0.00010112378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995565,0.0000048800975,0.0000020782113,0.000011248619,0.000009870392,0.000016247503],"domain_scores_gemma":[0.9999285,0.000011179048,0.000018228464,0.0000064442083,0.000016198157,0.000019461402],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109589964,0.00030832045,0.00020249015,0.0005594624,0.00031646495,0.00043694064,0.00015856695,0.00026893013,0.00037927626],"category_scores_gemma":[0.00011702262,0.00015891311,0.00013887203,0.00030712932,0.00020336492,0.00016779588,0.0002539936,0.00019515595,0.00010740363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006590717,0.00008852736,0.77225995,0.000040752013,0.00008922594,0.00029017535,0.00045334626,0.0010306056,0.21981314,0.000081508566,0.00022834586,0.0049653784],"study_design_scores_gemma":[0.000009616586,0.000082128776,0.98910004,0.0000050626963,0.000019974526,0.000047802154,0.0001693265,0.0009720478,0.009248908,0.000013637717,0.00032651986,0.0000050024396],"about_ca_topic_score_codex":0.014564198,"about_ca_topic_score_gemma":0.014064347,"teacher_disagreement_score":0.014564198,"about_ca_system_score_codex":0.00029319918,"about_ca_system_score_gemma":0.00016571976,"threshold_uncertainty_score":0.028958797},"labels":[],"label_agreement":null},{"id":"W2620874994","doi":"10.1002/2017gl073485","title":"Dissolved black carbon in the global cryosphere: Concentrations and chemical signatures","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Consortium of Universities for the Advancement of Hydrologic Science; United States Agency for International Development; National Science Foundation","keywords":"dBc; Snow; Cryosphere; Carbon black; Environmental science; Glacier; Arctic; Physical geography; Atmospheric sciences; Earth science; Geology; Environmental chemistry; Sea ice; Oceanography; Chemistry; Geomorphology; Materials science; Geography","score_opus":0.02642489258796225,"score_gpt":0.29482947152383987,"score_spread":0.2684045789358776,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2620874994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975231,0.00027682268,0.000117251664,0.000024722232,0.0000040985974,0.000002412835,0.0015440024,0.000006459114,0.00050127803],"genre_scores_gemma":[0.9981292,0.00014568788,0.000198656,0.000025507703,0.000008382998,0.0000043766195,0.001341434,0.0000036239496,0.00014330477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.00000943555,0.0000043413856,0.000024281622,0.000021841115,0.000014729752],"domain_scores_gemma":[0.99981135,0.000017140988,0.000057595684,0.000012560518,0.00007840755,0.000023017923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020293587,0.00027200364,0.000173714,0.00089837326,0.00031379922,0.0005016123,0.00012414188,0.00019920839,0.00042921666],"category_scores_gemma":[0.00017200496,0.000089737085,0.00019312587,0.001021655,0.00021037033,0.0002551942,0.00024323797,0.00013964034,0.00009504623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078819285,0.000019188079,0.9655853,0.000035543642,0.00019500204,0.000040438183,0.00011775137,0.0006356146,0.028169852,0.000073461204,0.000207576,0.0048415484],"study_design_scores_gemma":[0.0000012543155,0.000017301296,0.9972498,0.0000033412134,0.000016485035,0.000019942347,0.00010078546,0.0003055113,0.0018048233,0.000021753214,0.0004565158,0.000002450576],"about_ca_topic_score_codex":0.02366722,"about_ca_topic_score_gemma":0.027227601,"teacher_disagreement_score":0.02366722,"about_ca_system_score_codex":0.00037559253,"about_ca_system_score_gemma":0.0001603847,"threshold_uncertainty_score":0.04705894},"labels":[],"label_agreement":null},{"id":"W2622983352","doi":"10.1002/2017gl073285","title":"Higher temperature variability reduces temperature sensitivity of vegetation growth in Northern Hemisphere","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"State Key Laboratory of Earth Surface Processes and Resource Ecology; National Natural Science Foundation of China","keywords":"Environmental science; Vegetation (pathology); Northern Hemisphere; Growing season; Normalized Difference Vegetation Index; Climatology; Atmospheric sciences; Shrub; Ecosystem; Climate change; Ecology; Geology","score_opus":0.011726717304729916,"score_gpt":0.25987294939524563,"score_spread":0.24814623209051573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2622983352","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988355,0.000037651334,0.000521249,0.000026275065,0.0000029639139,0.000001009822,0.00009155108,0.00002781631,0.00045591735],"genre_scores_gemma":[0.9997975,0.000013318342,0.00005718419,0.000005861186,0.0000010693748,8.038409e-7,0.00005579733,0.0000038965945,0.000064555024],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.000013921591,0.00000270873,0.000029336285,0.000007462059,0.000018707873],"domain_scores_gemma":[0.99988425,0.00003656212,0.00003316657,0.00001580924,0.000012147334,0.000018078186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014770897,0.00015228301,0.0001630926,0.00009807275,0.00017275677,0.0004066126,0.00015859236,0.00015033572,0.001109622],"category_scores_gemma":[0.00043514188,0.000103534825,0.00024710444,0.0001557952,0.00017756304,0.0002905556,0.00020657665,0.00016370196,0.00007658712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031169647,0.00015660921,0.57077646,0.0001123555,0.00035971403,0.00026377232,0.00035506277,0.19669147,0.21440163,0.0011523113,0.0012361569,0.014182768],"study_design_scores_gemma":[0.00001015557,0.00004240084,0.88782847,0.0000043976574,0.000034706536,0.00004012138,0.00012878636,0.10764427,0.003439237,0.0003443719,0.0004704304,0.000012654635],"about_ca_topic_score_codex":0.028427847,"about_ca_topic_score_gemma":0.024542937,"teacher_disagreement_score":0.028427847,"about_ca_system_score_codex":0.0004755226,"about_ca_system_score_gemma":0.00028064463,"threshold_uncertainty_score":0.056524754},"labels":[],"label_agreement":null},{"id":"W2624109847","doi":"10.1002/2017gl074014","title":"WINDII airglow observations of wave superposition and the possible association with historical “bright nights”","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency","keywords":"Airglow; Longitude; Middle latitudes; Atmospheric sciences; Thermosphere; Atmosphere (unit); Maxima; Latitude; Physics; Satellite; Geology; Environmental science; Ionosphere; Geodesy; Astronomy; Meteorology","score_opus":0.023275285982119618,"score_gpt":0.26040269728398097,"score_spread":0.23712741130186135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2624109847","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990644,0.00005143036,0.00015409822,0.000022351762,0.0000047956955,0.0000022142958,0.00010597685,0.000005703345,0.00058906747],"genre_scores_gemma":[0.99961275,0.000026855269,0.00007472272,0.000005321095,0.000011296386,0.0000011014704,0.00017965729,0.0000014953247,0.0000867003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998528,0.000030622796,0.000012935297,0.000028404576,0.00003712946,0.000037950773],"domain_scores_gemma":[0.9989611,0.00016944154,0.00045639055,0.00011544093,0.00012160211,0.00017607913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036835324,0.00009320884,0.000101230275,0.00092151394,0.0003027606,0.0003164695,0.00011982939,0.00016231209,0.0008409751],"category_scores_gemma":[0.0011572967,0.00012449692,0.00009839677,0.0005151063,0.00030881612,0.00019967141,0.0003177986,0.00019571296,0.000101804326],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015536833,0.000023499228,0.98557925,0.00001293251,0.00002555409,0.00014371498,0.00022143999,0.0000740096,0.008443892,0.000101008554,0.00018327494,0.0050360155],"study_design_scores_gemma":[0.0000011280058,0.000018625762,0.9993857,0.0000012139811,0.0000036029053,0.00007669844,0.000043944307,0.00009166312,0.00024185627,0.000013956652,0.00012040654,0.000001135962],"about_ca_topic_score_codex":0.0029683246,"about_ca_topic_score_gemma":0.007818925,"teacher_disagreement_score":0.0029683246,"about_ca_system_score_codex":0.0001338474,"about_ca_system_score_gemma":0.0000963035,"threshold_uncertainty_score":0.005902052},"labels":[],"label_agreement":null},{"id":"W2626612493","doi":"10.1002/2017gl073359","title":"Evidence for marine biogenic influence on summertime Arctic aerosol","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph; Environment and Climate Change Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Sulfate; Sea salt aerosol; Sea salt; Sulfate aerosol; Arctic; Environmental science; Atmospheric sciences; Cloud condensation nuclei; Environmental chemistry; Climatology; Oceanography; Chemistry; Meteorology; Geology; Geography","score_opus":0.1025545580621368,"score_gpt":0.3471751122429792,"score_spread":0.2446205541808424,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2626612493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819416,0.000281829,0.0000844218,0.00003638542,0.000014097729,0.0000015123132,0.00027385712,0.000009100026,0.0011046908],"genre_scores_gemma":[0.9992256,0.00017158472,0.00010394364,0.000019964009,0.00002106481,0.0000016579648,0.0003156645,0.0000035491757,0.00013681622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989235,0.000018615878,0.000008551809,0.000023914297,0.000031101194,0.000025449597],"domain_scores_gemma":[0.9995363,0.000077148055,0.00009239896,0.000025535526,0.00016169746,0.00010697533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029973604,0.00032362554,0.00026226134,0.00055191916,0.0005186116,0.00053640065,0.00014972857,0.00024993095,0.00097052514],"category_scores_gemma":[0.00048481693,0.0001733604,0.00025929566,0.00039362267,0.0001984459,0.000157968,0.00029274027,0.00015283872,0.00017908857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005487733,0.0000640545,0.89099485,0.00008360578,0.00016337185,0.00025272006,0.00017315973,0.0005391349,0.099751875,0.00013209415,0.0002647587,0.007031496],"study_design_scores_gemma":[0.0000031789098,0.00003756111,0.99752694,0.0000062328536,0.000019743205,0.000026385385,0.000060688097,0.00036511265,0.001639794,0.0000145549775,0.0002978445,0.000002067909],"about_ca_topic_score_codex":0.03771697,"about_ca_topic_score_gemma":0.05130517,"teacher_disagreement_score":0.03771697,"about_ca_system_score_codex":0.00045746984,"about_ca_system_score_gemma":0.00036535467,"threshold_uncertainty_score":0.07499492},"labels":[],"label_agreement":null},{"id":"W2647927681","doi":"10.1002/2017gl074041","title":"Constrained variability of modeled <i>T</i>:<i>ET</i> ratio across biomes","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":151,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Center for Northern Studies","funders":"Stavros Niarchos Foundation; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Biome; Evapotranspiration; Precipitation; Atmospheric sciences; Standard deviation; Range (aeronautics); Environmental science; Potential evaporation; Transpiration; Evaporation; Interception; Leaf area index; Climatology; Mathematics; Statistics; Geology; Ecosystem; Ecology; Geography; Meteorology; Biology","score_opus":0.02889626529804623,"score_gpt":0.32594579362412307,"score_spread":0.29704952832607684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2647927681","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99402654,0.000040562307,0.004776544,0.00004867045,0.0000032314224,0.000005740441,0.00049283035,0.00007430883,0.00053157023],"genre_scores_gemma":[0.9991949,0.000012660944,0.0004780011,0.0000078900575,0.000001153141,0.000006161307,0.00024886715,0.00000980832,0.00004043924],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999811,0.000044367564,0.000014068101,0.00009772502,0.000011035589,0.000021833534],"domain_scores_gemma":[0.99940515,0.0002978856,0.00007624012,0.00012889672,0.0000644632,0.000027388265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007874543,0.00028470057,0.00029656524,0.0002690281,0.0002187802,0.00077597273,0.00057675136,0.0005637409,0.0005866429],"category_scores_gemma":[0.0013967275,0.00021795864,0.00064098,0.00046134766,0.00052261224,0.0007978354,0.00031124635,0.0003153542,0.000113013244],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019545716,0.0001449824,0.19193952,0.00010571974,0.00045507384,0.00018284928,0.00012205505,0.7689831,0.029496493,0.0016310331,0.00043941807,0.006304217],"study_design_scores_gemma":[0.00005211417,0.00005053545,0.14112699,0.000012129619,0.000069975365,0.0000732937,0.000103351806,0.8512117,0.005402455,0.0012918145,0.0005609837,0.00004462776],"about_ca_topic_score_codex":0.0074130907,"about_ca_topic_score_gemma":0.0034460975,"teacher_disagreement_score":0.0074130907,"about_ca_system_score_codex":0.00044332157,"about_ca_system_score_gemma":0.00028261117,"threshold_uncertainty_score":0.014739871},"labels":[],"label_agreement":null},{"id":"W2655300270","doi":"10.1002/2017gl074369","title":"Multistage 8.2 kyr event revealed through high‐resolution XRF core scanning of Cuban sinkhole sediments","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; McGill University; Bishop's University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Association for Applied Sport Psychology","keywords":"Sinkhole; Geology; Upwelling; Oceanography; Salinity; Paleontology","score_opus":0.07450552382742191,"score_gpt":0.35605429400609906,"score_spread":0.28154877017867713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2655300270","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982887,0.000050523733,0.00010434452,0.000026822998,0.000002663964,0.0000059933304,0.0004136031,0.000013248205,0.0010941931],"genre_scores_gemma":[0.99896324,0.00003709862,0.00017120659,0.000011137114,0.0000028022514,0.000006928909,0.00042483993,0.000005975155,0.0003767788],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993575,0.00000478376,0.0000031733093,0.000016540995,0.000012309103,0.00002737089],"domain_scores_gemma":[0.9998234,0.000011086296,0.00006193324,0.00001654423,0.00006202167,0.000025011532],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019196686,0.00017844886,0.00018580417,0.00093292975,0.0005238798,0.0005574931,0.00025498794,0.00023202,0.00082490727],"category_scores_gemma":[0.00032376352,0.00014425353,0.00014261206,0.00066217815,0.00021795716,0.00025302486,0.0005709343,0.0001939132,0.0001467623],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002730745,0.00005030098,0.9435269,0.000057817942,0.00008168238,0.0018461671,0.0016367089,0.00069158355,0.040833045,0.00027212378,0.00087322894,0.009857381],"study_design_scores_gemma":[0.0000014658744,0.000006550125,0.99821943,0.0000041486414,0.0000063143325,0.00008569489,0.00028880217,0.0002229414,0.0004605476,0.0000130455255,0.00068811275,0.0000028873578],"about_ca_topic_score_codex":0.089077316,"about_ca_topic_score_gemma":0.17603631,"teacher_disagreement_score":0.089077316,"about_ca_system_score_codex":0.0010151844,"about_ca_system_score_gemma":0.00046918532,"threshold_uncertainty_score":0.17711765},"labels":[],"label_agreement":null},{"id":"W2655620776","doi":"10.1002/2017gl073859","title":"Long‐term (2005–2014) trends in formaldehyde (HCHO) columns across North America as seen by the OMI satellite instrument: Evidence of changing emissions of volatile organic compounds","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Earth Sciences Division; Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Isoprene; Environmental science; Volatile organic compound; Formaldehyde; Ozone Monitoring Instrument; Atmospheric sciences; Ozone; Satellite; Atmosphere (unit); Environmental chemistry; Latitude; Troposphere; Meteorology; Chemistry; Geography; Geology","score_opus":0.02402323459168597,"score_gpt":0.31091327439984556,"score_spread":0.2868900398081596,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2655620776","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974892,0.00015512497,0.00007933215,0.000071081624,0.0000055705227,0.0000026928478,0.0015624006,0.000010606855,0.0006238892],"genre_scores_gemma":[0.99742293,0.0001698958,0.00019840982,0.000040477007,0.000009057906,0.000006078553,0.0017746332,0.0000028560441,0.0003757253],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.0000052134205,0.0000053116246,0.000023093493,0.000015626347,0.000015551019],"domain_scores_gemma":[0.99968326,0.000022268514,0.000118739976,0.00001614969,0.00011878167,0.000040863142],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001406407,0.00012901486,0.00009644476,0.00049027684,0.00022024992,0.00032414927,0.00018867507,0.00021429561,0.00075197604],"category_scores_gemma":[0.0002245373,0.00010433832,0.00017402369,0.0007103152,0.00014588538,0.0002664047,0.00024303533,0.00016766872,0.00011278071],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000046324218,0.000025709256,0.9888497,0.000021345699,0.00009821802,0.000043898723,0.00012580921,0.00027431108,0.0054419544,0.000039209935,0.0006034685,0.0044301],"study_design_scores_gemma":[5.850599e-7,0.000005311552,0.9991769,0.0000023905013,0.000009343548,0.0000066650446,0.000062518295,0.00013524664,0.00028773092,0.000003681679,0.00030855337,0.0000010641363],"about_ca_topic_score_codex":0.10287994,"about_ca_topic_score_gemma":0.17539601,"teacher_disagreement_score":0.89712006,"about_ca_system_score_codex":0.0005695226,"about_ca_system_score_gemma":0.0003891818,"threshold_uncertainty_score":0.20456225},"labels":[],"label_agreement":null},{"id":"W2680663249","doi":"10.1002/2017gl073701","title":"Quantifying black carbon deposition over the Greenland ice sheet from forest fires in Canada","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agence Nationale Des Parcs Nationaux; National Science Foundation","keywords":"Deposition (geology); Aerosol; Environmental science; Snow; Weather Research and Forecasting Model; Atmospheric sciences; Greenland ice sheet; Precipitation; Storm; Climatology; Moderate-resolution imaging spectroradiometer; Meteorology; Physical geography; Glacier; Geology; Geography; Satellite; Geomorphology","score_opus":0.04136923759267876,"score_gpt":0.2776449759508119,"score_spread":0.23627573835813312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2680663249","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953773,0.00022961751,0.00039250834,0.000059243535,0.0000067824494,0.000023418595,0.0019478755,0.00007358429,0.0018896074],"genre_scores_gemma":[0.99676764,0.00017900471,0.0008560279,0.000031522803,0.0000029774296,0.0000081424,0.0016717918,0.000014583663,0.00046833913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998117,0.0000075049466,0.000006200796,0.00004260556,0.000079150755,0.00005286978],"domain_scores_gemma":[0.9997764,0.000024379044,0.000026315549,0.000011800971,0.000115706185,0.00004537099],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022943341,0.00075424067,0.00028601842,0.0009904692,0.0016264514,0.0010436951,0.00069953944,0.0004449562,0.0006741635],"category_scores_gemma":[0.00041390696,0.00027471778,0.0005446336,0.0011917561,0.0003661727,0.0003462546,0.0003931003,0.00028584286,0.000089858164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017702865,0.00015431232,0.8417772,0.00012730944,0.00038158265,0.00038221525,0.0003645875,0.1203029,0.010739926,0.00046810886,0.00235453,0.02277027],"study_design_scores_gemma":[0.000030430334,0.000028821853,0.8417501,0.000043128304,0.00011106988,0.000055721335,0.0005266456,0.15021615,0.004414673,0.0001873946,0.0025954812,0.000040387604],"about_ca_topic_score_codex":0.98685837,"about_ca_topic_score_gemma":0.99103326,"teacher_disagreement_score":0.021188917,"about_ca_system_score_codex":0.021188917,"about_ca_system_score_gemma":0.011225561,"threshold_uncertainty_score":0.15373707},"labels":[],"label_agreement":null},{"id":"W2726858476","doi":"10.1002/2017gl074312","title":"Mantle flow through a tear in the Nazca slab inferred from shear wave splitting","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Division of Earth Sciences; National Science Foundation of Sri Lanka; Colorado College; National Science Foundation","keywords":"Geology; Slab; Shear wave splitting; Mantle wedge; Lithosphere; Mantle (geology); Seismology; Geophysics; Seismic anisotropy; Slab window; Shear (geology); Subduction; Petrology; Tectonics; Oceanic crust","score_opus":0.07471687260724563,"score_gpt":0.3188396457844851,"score_spread":0.24412277317723946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2726858476","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99884856,0.000022487564,0.00009236322,0.00001643138,0.000001559653,0.0000050705726,0.00020553502,0.000011027826,0.0007969276],"genre_scores_gemma":[0.9993838,0.000020031772,0.00019211188,0.000003004151,0.0000018264626,0.0000038062576,0.00022167938,0.0000024806725,0.00017127342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999169,0.0000056522476,0.000004730744,0.000020317446,0.000024468563,0.00002786029],"domain_scores_gemma":[0.9998056,0.000018285942,0.00005790371,0.000014900431,0.000065010325,0.00003830868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012776673,0.0002689258,0.00031415868,0.0014117245,0.0005238681,0.00069736585,0.00031416738,0.0002782808,0.0012236492],"category_scores_gemma":[0.00063830963,0.00025470948,0.00011280792,0.0010444829,0.0004030095,0.00021884282,0.0005308585,0.00027540355,0.00018833231],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004323459,0.000047430978,0.9312451,0.000026587699,0.000030772728,0.00033239395,0.001051388,0.0006841055,0.057406124,0.00018973676,0.00018949588,0.008364559],"study_design_scores_gemma":[0.00001241426,0.000025338011,0.9965551,0.00000773683,0.000008329654,0.000051004146,0.0005260342,0.0013662754,0.0010908111,0.000048224218,0.00030492106,0.000003743207],"about_ca_topic_score_codex":0.08508801,"about_ca_topic_score_gemma":0.105390094,"teacher_disagreement_score":0.08508801,"about_ca_system_score_codex":0.0006146002,"about_ca_system_score_gemma":0.0003589525,"threshold_uncertainty_score":0.16918552},"labels":[],"label_agreement":null},{"id":"W2727303116","doi":"10.1002/2017gl073834","title":"Glacierized headwater streams as aquifer recharge corridors, subarctic Alaska","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Engineer Research and Development Center; Strategic Environmental Research and Development Program; U.S. Geological Survey; National Institutes for Water Resources; Alaska Department of Transportation and Public Facilities; National Science Foundation; U.S. Department of Transportation; U.S. Department of Defense","keywords":"Groundwater recharge; Aquifer; Hydrology (agriculture); Permafrost; Streamflow; Glacier; Meltwater; Geology; Surface runoff; STREAMS; Baseflow; Perennial stream; Subarctic climate; Snowmelt; Drainage basin; Environmental science; Groundwater; Snow; Geomorphology; Oceanography; Geography; Ecology","score_opus":0.06425318514452241,"score_gpt":0.3207677321779384,"score_spread":0.25651454703341603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2727303116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989249,0.0001224513,0.000055377706,0.000027094986,0.0000018240298,0.0000012523396,0.00012325395,0.0000045965476,0.00073930196],"genre_scores_gemma":[0.9994867,0.0000982603,0.000062373045,0.000005694845,0.0000011635096,0.000001119819,0.00007637275,6.6857626e-7,0.00026773114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993885,0.000016371663,0.0000054165416,0.000017281567,0.000009859134,0.0000122499205],"domain_scores_gemma":[0.99968433,0.000054648768,0.000116479896,0.000016250315,0.00006766214,0.000060649523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027157064,0.00010352614,0.000084432024,0.0006441554,0.00036202156,0.0007311838,0.00013537574,0.00010766326,0.0015202392],"category_scores_gemma":[0.0004940253,0.00008566254,0.00009572322,0.0007813932,0.0002890856,0.00043889158,0.0004265131,0.00013849382,0.00010024317],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033910437,0.000009234235,0.99375916,0.0000136408735,0.000018440072,0.000072117014,0.00041103206,0.0006729829,0.00073691213,0.00014289917,0.00007958499,0.0040500727],"study_design_scores_gemma":[0.0000011506191,0.000009439824,0.99802846,0.000010277042,0.000012795159,0.000030656633,0.0008473032,0.00048738503,0.00015090228,0.00012610413,0.00029341909,0.0000020301375],"about_ca_topic_score_codex":0.07101543,"about_ca_topic_score_gemma":0.17018573,"teacher_disagreement_score":0.07101543,"about_ca_system_score_codex":0.00075084687,"about_ca_system_score_gemma":0.0005331567,"threshold_uncertainty_score":0.14120412},"labels":[],"label_agreement":null},{"id":"W2728119899","doi":"10.1002/2017gl073388","title":"Large‐scale fluid‐deposited mineralization in Margaritifer Terra, Mars","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Jet Propulsion Laboratory; Ministère de la Santé et des Services sociaux; University of Arizona; California Institute of Technology","keywords":"Geology; Mars Exploration Program; Impact crater; Geochemistry; Ridge; Context (archaeology); Mineralization (soil science); Earth science; Astrobiology; Hydrothermal circulation; Geomorphology; Paleontology","score_opus":0.03313671164174451,"score_gpt":0.30998664327115216,"score_spread":0.27684993162940763,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2728119899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993938,0.000041029896,0.00003561837,0.000008694968,8.03793e-7,0.0000027561555,0.00015361325,0.000005343339,0.0003583329],"genre_scores_gemma":[0.99941206,0.00002054233,0.00014589974,0.0000038343646,0.0000019763795,0.0000028363086,0.00020778146,0.0000019205027,0.00020295581],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999281,0.000005349623,0.000003105004,0.000027462716,0.000016461287,0.000019573072],"domain_scores_gemma":[0.9998534,0.000014659605,0.00005290663,0.000014534929,0.000034156612,0.000030248415],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014076493,0.00016961539,0.00013478877,0.0014259627,0.00082233653,0.00046866926,0.00029823216,0.00027977556,0.0012718108],"category_scores_gemma":[0.00019917666,0.00015208218,0.00016381391,0.00057738664,0.00045919212,0.00017806167,0.00044941631,0.00013604906,0.0002454268],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022786333,0.000042113552,0.9103125,0.00004312454,0.00006754803,0.00074746576,0.0019029,0.0003491446,0.07441544,0.000113741415,0.0002442892,0.011533937],"study_design_scores_gemma":[0.0000010033007,0.00001319567,0.9991904,0.0000014276666,0.0000025568386,0.00006218211,0.00018820989,0.00007676122,0.00023870142,0.0000072834014,0.00021709877,0.0000011813962],"about_ca_topic_score_codex":0.019184014,"about_ca_topic_score_gemma":0.038353153,"teacher_disagreement_score":0.019184014,"about_ca_system_score_codex":0.00039646783,"about_ca_system_score_gemma":0.00021381414,"threshold_uncertainty_score":0.038144708},"labels":[],"label_agreement":null},{"id":"W2730317824","doi":"10.1002/2017gl074081","title":"Ice‐dammed lake drainage in west Greenland: Drainage pattern and implications on ice flow and bedrock motion","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Danmarks Frie Forskningsfond","keywords":"Geology; Bedrock; Drainage; Ice stream; Ice sheet; Geomorphology; Groenlandia; Oceanography; Hydrology (agriculture); Cryosphere; Sea ice; Geotechnical engineering","score_opus":0.04658232738942708,"score_gpt":0.2993080592860491,"score_spread":0.252725731896622,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2730317824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957734,0.000027862066,0.000024696008,0.00002005865,6.080883e-7,0.0000010081386,0.00015334065,0.000003824469,0.00019129012],"genre_scores_gemma":[0.9997358,0.000016178348,0.000033380198,0.0000067298506,5.8247025e-7,8.255825e-7,0.00010947033,0.0000012771443,0.00009567076],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999529,0.0000074662476,0.000002846973,0.000009588004,0.000005849972,0.000021282467],"domain_scores_gemma":[0.99988484,0.0000141031005,0.00004170931,0.000007358971,0.00001731564,0.000034642264],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016020863,0.00011748518,0.00012855142,0.00063170295,0.00024804912,0.0005054761,0.00016883668,0.00014241053,0.00087634823],"category_scores_gemma":[0.00025209296,0.000089666,0.00011027017,0.00078729715,0.00038525183,0.00031517117,0.0003147628,0.00009025552,0.0000709469],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070084214,0.000030030658,0.98743606,0.000017862487,0.000038524697,0.00016216193,0.00047111345,0.0013336826,0.0033351667,0.00009836585,0.00027859013,0.006728393],"study_design_scores_gemma":[0.0000012351536,0.000004727248,0.9986998,0.0000026432474,0.0000036703314,0.000014651169,0.00020387035,0.0008078558,0.0000955185,0.000019677904,0.00014499764,0.0000013465744],"about_ca_topic_score_codex":0.16996376,"about_ca_topic_score_gemma":0.34213683,"teacher_disagreement_score":0.16996376,"about_ca_system_score_codex":0.0015552257,"about_ca_system_score_gemma":0.00065402064,"threshold_uncertainty_score":0.33794898},"labels":[],"label_agreement":null},{"id":"W2730360842","doi":"10.1002/2017gl074376","title":"River networks dampen long‐term hydrological signals of climate change","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"Simon Fraser University","keywords":"Climate change; Environmental science; Biota; Drainage basin; Null (SQL); Streamflow; Discharge; Hydrology (agriculture); Term (time); Ecology; Geography; Geology; Biology","score_opus":0.0652551175117651,"score_gpt":0.3322082187553327,"score_spread":0.2669531012435676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2730360842","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986779,0.000017790548,0.00051175326,0.00006399161,0.0000010197384,0.0000012694031,0.000040723437,0.000012707567,0.0006727296],"genre_scores_gemma":[0.9998727,0.0000049166797,0.000046951296,0.000004369326,7.5822715e-7,3.134573e-7,0.000014868439,8.093215e-7,0.000054364093],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997905,0.00006380638,0.000011235494,0.000045268764,0.000042932053,0.00004634308],"domain_scores_gemma":[0.9988217,0.00036292837,0.00036963745,0.00013454795,0.00019280128,0.00011849303],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00058197486,0.00011309808,0.0001321774,0.00035112715,0.00030675268,0.0007442974,0.00019670768,0.00017986826,0.0012288333],"category_scores_gemma":[0.002434646,0.00009930005,0.00007677608,0.0003420108,0.0006246557,0.00039871508,0.0004612474,0.0002206939,0.000073281044],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016058818,0.00006761154,0.9502186,0.000020798892,0.00011697164,0.00010180006,0.0006362811,0.017318262,0.010401407,0.0016249757,0.000507543,0.018825125],"study_design_scores_gemma":[0.0000025617248,0.000032786545,0.9883201,0.000003770422,0.000020881816,0.00002031806,0.0003225259,0.009689666,0.0005316813,0.00063520623,0.0004159661,0.0000043819114],"about_ca_topic_score_codex":0.07849069,"about_ca_topic_score_gemma":0.127545,"teacher_disagreement_score":0.07849069,"about_ca_system_score_codex":0.0009813075,"about_ca_system_score_gemma":0.0004947317,"threshold_uncertainty_score":0.15606761},"labels":[],"label_agreement":null},{"id":"W2734613673","doi":"10.1002/2017gl073597","title":"Thermal structure of the Kanto region, Japan","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"","keywords":"Geology; Slab; Mantle wedge; Subduction; Forearc; Seismology; Mantle (geology); Pacific Plate; Volcanic arc; Thermal; Geophysics; Tectonics","score_opus":0.04249591997501954,"score_gpt":0.2877568427443841,"score_spread":0.2452609227693646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2734613673","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99674475,0.00010969023,0.0010053519,0.000095948904,0.000005400924,0.000006893546,0.00028063403,0.000036704918,0.001714558],"genre_scores_gemma":[0.99911577,0.000057814777,0.0003396965,0.000011935215,0.000002876875,0.0000103264465,0.00020745437,0.0000057009947,0.00024841187],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993527,0.000010663827,0.0000038868166,0.000023163526,0.000007379274,0.000019572317],"domain_scores_gemma":[0.9999131,0.000011398892,0.00001761828,0.000009005328,0.00002109845,0.000027774151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008225828,0.0004252242,0.00032098487,0.00044445304,0.00086402183,0.0008966355,0.0004389215,0.00053637044,0.0009862492],"category_scores_gemma":[0.00022870219,0.00041927022,0.00060463045,0.0006752274,0.0005881495,0.0005179205,0.00060693384,0.00024874776,0.00013150118],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028564525,0.000093899915,0.16867298,0.00010173269,0.00020247458,0.00051007775,0.00074968603,0.8145931,0.0073219314,0.0022309185,0.00066941435,0.004568097],"study_design_scores_gemma":[0.00010588935,0.00006627498,0.16212256,0.000021178232,0.00013294285,0.00011551212,0.0006914447,0.833592,0.0007585179,0.0012616166,0.0010385572,0.000093525035],"about_ca_topic_score_codex":0.10836501,"about_ca_topic_score_gemma":0.07081199,"teacher_disagreement_score":0.10836501,"about_ca_system_score_codex":0.0013473096,"about_ca_system_score_gemma":0.0012131019,"threshold_uncertainty_score":0.21546847},"labels":[],"label_agreement":null},{"id":"W2735049131","doi":"10.1002/2017gl074006","title":"Relativistic electron dynamics produced by azimuthally localized poloidal mode ULF waves: Boomerang‐shaped pitch angle evolutions","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Physics; Pitch angle; Electron; Van Allen radiation belt; Energy flux; Spacecraft; Radiation; Van Allen Probes; Computational physics; Resonance (particle physics); Geophysics; Plasma; Magnetosphere; Atomic physics; Optics; Astronomy","score_opus":0.014309536362313439,"score_gpt":0.307560883223468,"score_spread":0.29325134686115456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2735049131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99708945,0.000042350108,0.0018378489,0.000019313167,0.000002893917,0.0000047735425,0.00004385438,0.00002734634,0.00093225617],"genre_scores_gemma":[0.99956447,0.0000139148215,0.0002714999,0.0000020483553,0.0000013506406,0.0000015761581,0.000033539854,0.000005001631,0.00010663162],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999647,0.000005483266,0.0000013641134,0.000007729245,0.000006941956,0.00001385638],"domain_scores_gemma":[0.9998276,0.00004374359,0.00005816611,0.0000216544,0.000025278005,0.00002352792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000102341706,0.00018272674,0.00013765109,0.00053040514,0.00017767024,0.0002976317,0.00019346295,0.00016231225,0.0007273028],"category_scores_gemma":[0.000551117,0.00012895226,0.0001830572,0.00031097763,0.0002844412,0.00018674372,0.0002063973,0.00018140564,0.000058936006],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014875203,0.0002191648,0.326157,0.00012118236,0.0002883475,0.004807433,0.0012221116,0.25904825,0.3508788,0.013220876,0.0011607602,0.041388527],"study_design_scores_gemma":[0.000048100468,0.00016535522,0.50955814,0.00001251408,0.000036747268,0.000566353,0.00026019005,0.46465525,0.021220362,0.002189468,0.001229692,0.000057866837],"about_ca_topic_score_codex":0.0016823073,"about_ca_topic_score_gemma":0.0009665212,"teacher_disagreement_score":0.0016823073,"about_ca_system_score_codex":0.00031203785,"about_ca_system_score_gemma":0.000086414235,"threshold_uncertainty_score":0.003344953},"labels":[],"label_agreement":null},{"id":"W2736252047","doi":"10.1002/2017gl073697","title":"The 1200 year composite ice core record of Aleutian Low intensification","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Ice core; Forcing (mathematics); Climatology; Geology; Oceanography; Environmental science","score_opus":0.07148311498081508,"score_gpt":0.33236934483954245,"score_spread":0.26088622985872734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2736252047","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952238,0.000084269624,0.00012491713,0.000031413016,0.0000042778306,0.0000032793132,0.0031528762,0.00001445031,0.0013607111],"genre_scores_gemma":[0.99529475,0.00010098157,0.00031042105,0.000015708054,0.000007946278,0.0000069480598,0.0038124442,0.0000050226595,0.0004457577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.0000056459326,0.000006161079,0.000014543018,0.000010915906,0.000008821055],"domain_scores_gemma":[0.9996408,0.000021234837,0.0001299766,0.000041877185,0.0001189462,0.000047132846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022977404,0.00011195821,0.00010675718,0.00087888906,0.00023953653,0.0004988299,0.00013354844,0.00010029719,0.00061971997],"category_scores_gemma":[0.00034896153,0.00008873146,0.000100606485,0.0010428483,0.00014609168,0.00027913987,0.00033880738,0.00020968648,0.000112136855],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000799439,0.000018809244,0.9877424,0.000018723105,0.000060326805,0.00003980318,0.00018099863,0.00032818815,0.0040503354,0.000109633795,0.00067266333,0.0066980748],"study_design_scores_gemma":[0.0000015676914,0.000004213596,0.9985642,0.0000022532383,0.0000051177517,0.000016055028,0.00003738941,0.0002276985,0.00032300138,0.000010484195,0.0008063514,0.0000016811401],"about_ca_topic_score_codex":0.030619852,"about_ca_topic_score_gemma":0.0665702,"teacher_disagreement_score":0.030619852,"about_ca_system_score_codex":0.00041578859,"about_ca_system_score_gemma":0.0002947401,"threshold_uncertainty_score":0.060883284},"labels":[],"label_agreement":null},{"id":"W2736524504","doi":"10.1002/2017gl074264","title":"Comparison of observed and modeled seasonal crustal vertical displacements derived from multi‐institution GPS and GRACE solutions","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Natural Science Foundation of China","keywords":"Global Positioning System; Geodesy; Internal consistency; Vertical displacement; Displacement (psychology); Geology; Satellite; Consistency (knowledge bases); Series (stratigraphy); Institution; Computer science; Mathematics; Statistics; Telecommunications; Engineering; Political science; Aerospace engineering","score_opus":0.19832577660353085,"score_gpt":0.35763121837040723,"score_spread":0.1593054417668764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2736524504","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99428517,0.00004238218,0.0024578967,0.00004056419,0.00001526575,0.0000098424825,0.0019037774,0.00028874326,0.00095629576],"genre_scores_gemma":[0.99641377,0.000017826911,0.0014414497,0.0000056599506,0.000004093067,0.0000055134524,0.0019619237,0.000021309645,0.00012856767],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997334,0.00005266777,0.000026697473,0.000084677304,0.000061485254,0.00004106862],"domain_scores_gemma":[0.99950624,0.00009322215,0.00009545916,0.00011942778,0.00014889812,0.000036750283],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006053668,0.00041785813,0.00021549693,0.00070714456,0.0001899835,0.000504335,0.00047529014,0.00034214876,0.000627624],"category_scores_gemma":[0.0016215151,0.00019510592,0.00055655575,0.0010690943,0.00019233182,0.00052242,0.0003497712,0.00025428462,0.00016763501],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007076988,0.00018583664,0.59322816,0.000103947394,0.00037784418,0.00024132931,0.00028151576,0.32639396,0.018109748,0.00080349407,0.0025246935,0.057041783],"study_design_scores_gemma":[0.00010329285,0.00016750087,0.69105524,0.000020714893,0.00010579421,0.000110978755,0.00018617357,0.29574412,0.010031839,0.00022716726,0.002178441,0.000068738154],"about_ca_topic_score_codex":0.021109948,"about_ca_topic_score_gemma":0.029879263,"teacher_disagreement_score":0.021109948,"about_ca_system_score_codex":0.0008239131,"about_ca_system_score_gemma":0.0005318953,"threshold_uncertainty_score":0.041974127},"labels":[],"label_agreement":null},{"id":"W2736540001","doi":"10.1002/2017gl074327","title":"Remarkable separability of circulation response to Arctic sea ice loss and greenhouse gas forcing","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Climatology; Arctic ice pack; Sea ice; Environmental science; Arctic sea ice decline; Arctic; Forcing (mathematics); Climate change; Greenhouse gas; Arctic geoengineering; Climate model; Ice-albedo feedback; Atmospheric sciences; Arctic oscillation; Atmospheric circulation; Drift ice; Geology; Oceanography","score_opus":0.030818996763405465,"score_gpt":0.3013463219779248,"score_spread":0.2705273252145194,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2736540001","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99421906,0.00011025032,0.0028683355,0.00017396812,0.00002405239,0.000007766038,0.00036371802,0.00010960329,0.0021232679],"genre_scores_gemma":[0.9993894,0.000022169743,0.00021229954,0.000019612442,0.000009342211,0.000004031039,0.00018270584,0.000011389196,0.0001490849],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980456,0.000042823765,0.000013931642,0.000068122565,0.000026915526,0.00004367772],"domain_scores_gemma":[0.99940205,0.00018962944,0.00013762746,0.00012786714,0.00005855055,0.00008431746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036632316,0.00018595801,0.00038600012,0.0002962137,0.00028948745,0.00058348174,0.00017710024,0.00028111675,0.00090303365],"category_scores_gemma":[0.0016040372,0.00024867756,0.00049709476,0.00022544707,0.00035479892,0.00047099972,0.00079895527,0.00043642073,0.00011924874],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0028537659,0.00043661322,0.38965705,0.00022542047,0.0013273339,0.0006251808,0.00083902804,0.17409836,0.37794462,0.0064095664,0.00269265,0.042890385],"study_design_scores_gemma":[0.00009690287,0.00012485521,0.79445815,0.00001788505,0.00013613608,0.00012948118,0.00020486166,0.19196536,0.00724432,0.0043177293,0.001241861,0.00006239996],"about_ca_topic_score_codex":0.004316065,"about_ca_topic_score_gemma":0.0028508205,"teacher_disagreement_score":0.004316065,"about_ca_system_score_codex":0.00027842436,"about_ca_system_score_gemma":0.00029057832,"threshold_uncertainty_score":0.008581877},"labels":[],"label_agreement":null},{"id":"W2736681395","doi":"10.1002/2017gl073744","title":"Links between clay transformation and earthquakes along the Costa Rican subduction margin","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada); University of Calgary","funders":"United States Science Support Program; National Science Foundation","keywords":"Geology; Subduction; Slip (aerodynamics); Lithification; Trench; Clay minerals; Seismology; Tectonics; Sediment; Geochemistry; Geomorphology","score_opus":0.054938431841057705,"score_gpt":0.30549704570654757,"score_spread":0.25055861386548983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2736681395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99950254,0.000020740497,0.000044326855,0.000016281452,1.8999164e-7,9.821641e-7,0.00006585524,0.000005708317,0.0003433017],"genre_scores_gemma":[0.9999025,0.00000774813,0.000015992258,0.0000012496752,2.9661106e-7,3.903124e-7,0.000034352208,7.302107e-7,0.000036835885],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994004,0.00001325656,0.000004264113,0.000015702788,0.000012090685,0.000014634362],"domain_scores_gemma":[0.99975246,0.00004759675,0.00010234216,0.00002703622,0.000045365927,0.000025160329],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014448026,0.00012215595,0.000096279626,0.0005172508,0.00015115042,0.00035017694,0.00014134408,0.00015488487,0.0006382074],"category_scores_gemma":[0.0006576615,0.00009341706,0.00011891286,0.000526301,0.00025286278,0.00013369381,0.00037435425,0.00009203504,0.00007996224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005916996,0.000010476999,0.9879006,0.000009633877,0.000037464444,0.0000843566,0.00034668564,0.0044618472,0.003157482,0.00014266075,0.00007671817,0.0037128853],"study_design_scores_gemma":[0.0000013039063,0.0000036457286,0.9968629,0.0000018043845,0.000002680545,0.000014342828,0.00010184172,0.0027284098,0.00014353891,0.000020567128,0.000117518735,0.0000015016503],"about_ca_topic_score_codex":0.043818567,"about_ca_topic_score_gemma":0.061658,"teacher_disagreement_score":0.043818567,"about_ca_system_score_codex":0.00059301674,"about_ca_system_score_gemma":0.00018360854,"threshold_uncertainty_score":0.08712703},"labels":[],"label_agreement":null},{"id":"W2737373063","doi":"10.1002/2017gl073392","title":"Charged particle behavior in localized ultralow frequency waves: Theory and observations","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency; National Natural Science Foundation of China","keywords":"Magnetosphere; Physics; Van Allen radiation belt; Amplitude; Resonance (particle physics); Charged particle; Wave–particle duality; Computational physics; Geophysics; Van Allen Probes; Longitude; Quantum electrodynamics; Plasmasphere; Classical mechanics; Latitude; Ion; Atomic physics; Magnetic field; Quantum mechanics; Astronomy","score_opus":0.038027793549784264,"score_gpt":0.32156776422481176,"score_spread":0.2835399706750275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2737373063","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93442553,0.00038594357,0.061196037,0.000092608614,0.000008866788,0.000020322488,0.00007816162,0.00017630159,0.003616227],"genre_scores_gemma":[0.9980034,0.000073806295,0.0017597158,0.0000051769675,0.000004590806,0.000004971178,0.000033464614,0.0000050242106,0.00010977041],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999448,0.0000138027945,0.0000025521842,0.00001613347,0.000016231374,0.000006544162],"domain_scores_gemma":[0.99983823,0.000062592015,0.000038758186,0.00003379292,0.000016376353,0.000010330751],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003202766,0.00024794033,0.00021776876,0.00042310663,0.00017833948,0.0004190293,0.0007638235,0.00044744636,0.0004032583],"category_scores_gemma":[0.0005954471,0.0001475098,0.00023387032,0.00025285195,0.00060956716,0.0005346098,0.0004523937,0.00029416857,0.000073425275],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028328094,0.00031174187,0.16041754,0.00028856442,0.00013821805,0.0011707157,0.0009465413,0.5124375,0.13847734,0.1370746,0.0011011199,0.047352802],"study_design_scores_gemma":[0.00003600862,0.00008963465,0.0500142,0.000017548111,0.000015217375,0.00011328212,0.00012031788,0.92605823,0.0050508543,0.017731052,0.0007254662,0.000028206028],"about_ca_topic_score_codex":0.0013284695,"about_ca_topic_score_gemma":0.00060790643,"teacher_disagreement_score":0.0013284695,"about_ca_system_score_codex":0.00039687226,"about_ca_system_score_gemma":0.00011775941,"threshold_uncertainty_score":0.00287956},"labels":[],"label_agreement":null},{"id":"W2739329179","doi":"10.1002/2017gl073439","title":"Polar cap hot patches: Enhanced density structures different from the classical patches in the ionosphere","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Office of Naval Research; Science and Technology Facilities Council; Multidisciplinary University Research Initiative; Natural Science Foundation of Shandong Province; National Natural Science Foundation of China; National Oceanic and Atmospheric Administration; New Brunswick Innovation Foundation; Canadian Space Agency; Massachusetts Institute of Technology; Norges Forskningsråd; National Aeronautics and Space Administration; National Science Foundation","keywords":"Polar; Ionosphere; Physics; Geophysics; Geology; Atmospheric sciences; Astronomy","score_opus":0.02332885660361489,"score_gpt":0.2913760855506595,"score_spread":0.26804722894704464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2739329179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99497294,0.00026708716,0.0015846259,0.000029132072,0.000020382802,0.000020147774,0.00022305756,0.000053815398,0.0028287552],"genre_scores_gemma":[0.99922013,0.000047645684,0.0003447759,0.0000134586035,0.000021045058,0.0000044780345,0.00013326306,0.000005888983,0.00020924273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999541,0.0000029845621,0.00000172359,0.00001526723,0.000010314453,0.000015583886],"domain_scores_gemma":[0.99987864,0.000017310249,0.00003270529,0.000017804057,0.000029316274,0.00002420786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007285232,0.00016769639,0.00017656322,0.00066010613,0.0002550186,0.0004825907,0.00020084152,0.00013747715,0.0014220489],"category_scores_gemma":[0.00017032555,0.00016127339,0.000112268885,0.00047421668,0.00044583506,0.00029277152,0.000355026,0.00014234251,0.00014415014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001924416,0.000106894506,0.47470635,0.00029904832,0.00022600453,0.002831445,0.0010237831,0.00269085,0.46821794,0.0015820864,0.0028434407,0.043547705],"study_design_scores_gemma":[0.000027865393,0.000048187274,0.9860044,0.000007207389,0.000034465887,0.0005541257,0.0002344201,0.002822881,0.008766095,0.00026060504,0.001229813,0.000010030144],"about_ca_topic_score_codex":0.0026073335,"about_ca_topic_score_gemma":0.002483941,"teacher_disagreement_score":0.0026073335,"about_ca_system_score_codex":0.00019162652,"about_ca_system_score_gemma":0.000087093424,"threshold_uncertainty_score":0.0051843524},"labels":[],"label_agreement":null},{"id":"W2741410973","doi":"10.1002/2017gl074027","title":"The postearthquake stress state on the Tohoku megathrust as constrained by reanalysis of the JFAST breakout data","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Gordon and Betty Moore Foundation","keywords":"Geology; Breakout; Seismology; Borehole; Fault (geology); Stress (linguistics); Stress field; Subduction; Geotechnical engineering; Tectonics; Structural engineering","score_opus":0.059175216550201554,"score_gpt":0.3132076940645925,"score_spread":0.25403247751439095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2741410973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991892,0.00002484563,0.00019919456,0.000016410984,0.0000023811338,0.0000018558902,0.00037838376,0.000015839936,0.00017185324],"genre_scores_gemma":[0.99855274,0.00003668239,0.00031368888,0.00000643991,0.000003196779,0.0000036390143,0.0010086759,0.000006531026,0.00006829203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998642,0.000019936575,0.000014729623,0.000045783137,0.000025261337,0.000030008996],"domain_scores_gemma":[0.99953413,0.000048478887,0.00012207133,0.000090553294,0.00012593332,0.00007887473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039313405,0.00034615936,0.00032944654,0.000924641,0.0003035441,0.00053799816,0.00033266292,0.00026031793,0.00044129562],"category_scores_gemma":[0.00078712014,0.00022829324,0.0004906539,0.0010189615,0.00029277347,0.00048792156,0.00044569888,0.00028322724,0.00008375129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026487524,0.00009214884,0.9384758,0.000053057258,0.0002978453,0.00027470032,0.0003797801,0.024419576,0.022781558,0.0002201506,0.0005604704,0.012180039],"study_design_scores_gemma":[0.000011631216,0.00002812931,0.9818733,0.0000059297763,0.000062709485,0.00002602521,0.00013270459,0.016476385,0.0010460331,0.00005814632,0.00026042378,0.00001847702],"about_ca_topic_score_codex":0.06779732,"about_ca_topic_score_gemma":0.113337524,"teacher_disagreement_score":0.06779732,"about_ca_system_score_codex":0.00060587557,"about_ca_system_score_gemma":0.0005684897,"threshold_uncertainty_score":0.13480538},"labels":[],"label_agreement":null},{"id":"W2741473875","doi":"10.1002/2017gl073415","title":"The stabilizing effect of collision‐induced velocity shear on the ionospheric feedback instability in Earth's magnetosphere","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency","keywords":"Ionosphere; Physics; Magnetosphere; Plasma sheet; Instability; Geophysics; Collision frequency; Mechanics; Plasma; Convection; Computational physics; Atomic physics","score_opus":0.023970317723109903,"score_gpt":0.30188890101946386,"score_spread":0.27791858329635394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2741473875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953334,0.00005197638,0.0029720955,0.000056104225,0.000009597285,0.000005147591,0.000014576475,0.000036504967,0.0015206931],"genre_scores_gemma":[0.9997868,0.000009752336,0.00013082325,0.000002946823,0.0000011364201,0.0000011011894,0.0000024927951,0.0000021027304,0.00006284341],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999936,0.000019461102,0.000002875864,0.000008917542,0.000012724158,0.000019981118],"domain_scores_gemma":[0.9997563,0.00009368285,0.000054690237,0.000019572995,0.000032166863,0.000043638804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022310112,0.00028064518,0.00026977787,0.00022713082,0.0005375799,0.00065032573,0.00028687404,0.00033283487,0.0007931964],"category_scores_gemma":[0.0012480709,0.00016523332,0.00027979558,0.00010092117,0.0005694974,0.00041044457,0.00064894883,0.00022410268,0.00006747915],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039594003,0.00006309843,0.012445698,0.00003558923,0.00004713809,0.00039695067,0.00014536444,0.9272182,0.048975784,0.006656764,0.00018800201,0.003431525],"study_design_scores_gemma":[0.00005170699,0.00011960037,0.0028879144,0.000004148361,0.000013604729,0.000023058687,0.000035881065,0.9934909,0.0027245863,0.0005613378,0.000077227094,0.000010015849],"about_ca_topic_score_codex":0.005637649,"about_ca_topic_score_gemma":0.0015868616,"teacher_disagreement_score":0.005637649,"about_ca_system_score_codex":0.0005376104,"about_ca_system_score_gemma":0.00035873457,"threshold_uncertainty_score":0.011209667},"labels":[],"label_agreement":null},{"id":"W2742791359","doi":"10.1002/2017gl074651","title":"Effect of deformation on the thermal conductivity of granular porous media with rough grain surface","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Granular flow and fluidized beds","field":"Engineering","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Materials science; Thermal conductivity; Thermal conduction; Thermal contact conductance; Heat transfer; Porous medium; Fractal dimension; Surface finish; Surface roughness; Porosity; Composite material; Mechanics; Deformation (meteorology); Fractal; Thermal resistance; Physics; Mathematics","score_opus":0.02245929073224693,"score_gpt":0.27650809758493483,"score_spread":0.2540488068526879,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2742791359","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987924,0.00003375709,0.0008324178,0.000012479563,0.0000043040577,0.0000025227027,0.000012416005,0.00001252087,0.00029705465],"genre_scores_gemma":[0.9998715,0.000009930145,0.00008595911,0.0000015283322,6.480247e-7,5.9157526e-7,0.000005597166,0.000001252948,0.000023029235],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998857,0.00001754401,0.000007709215,0.000019489209,0.000032314932,0.000037201],"domain_scores_gemma":[0.9996013,0.0002253418,0.00007119818,0.00004644221,0.000024540705,0.000031269814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016437545,0.00018803717,0.00031004747,0.00028623093,0.00033057193,0.0005904141,0.00016138892,0.00028793886,0.0004454744],"category_scores_gemma":[0.0007654994,0.00013891945,0.00027530143,0.00021248219,0.00095076166,0.000294911,0.00031093313,0.00023819647,0.00003877745],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009989518,0.00017582744,0.009995051,0.00012022037,0.00007688405,0.0010512295,0.00022991214,0.43556494,0.5433998,0.0021803826,0.00013268013,0.006074148],"study_design_scores_gemma":[0.00005214488,0.00048410636,0.0206384,0.000010216568,0.00003045636,0.00018484762,0.00015686317,0.7683436,0.20903498,0.0007540197,0.00026976384,0.000040635463],"about_ca_topic_score_codex":0.0012728925,"about_ca_topic_score_gemma":0.00050693785,"teacher_disagreement_score":0.0012728925,"about_ca_system_score_codex":0.0003224949,"about_ca_system_score_gemma":0.00012155312,"threshold_uncertainty_score":0.002530992},"labels":[],"label_agreement":null},{"id":"W2743047548","doi":"10.1002/2017gl073941","title":"Latitude and lake size are important predictors of over‐lake atmospheric stability","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of the Environment, Conservation and Parks","funders":"Horizon 2020; Natural Environment Research Council; Sight Research UK; Global Lake Ecological Observatory Network; Inter-American Institute for Global Change Research; National Science Foundation","keywords":"Environmental science; Atmosphere (unit); Atmospheric sciences; Latitude; Atmospheric instability; Planetary boundary layer; Evaporation; Water cycle; Climatology; Turbulence; Meteorology; Geology; Wind speed; Geography; Ecology","score_opus":0.023446497606117774,"score_gpt":0.26203136859934406,"score_spread":0.23858487099322628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2743047548","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993149,0.000080392965,0.00011733306,0.000018966744,0.0000013478049,7.5849465e-7,0.00016812669,0.000004151591,0.00029416455],"genre_scores_gemma":[0.9997925,0.000015499321,0.000026233633,0.000002096285,0.0000015864115,8.604892e-7,0.00010095816,0.0000018715971,0.00005842514],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998872,0.000040136263,0.000009931674,0.000024453793,0.000013239247,0.000025064277],"domain_scores_gemma":[0.9986212,0.00075477595,0.0003194682,0.00007631644,0.000085814536,0.00014237734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028294628,0.00013653484,0.00018315585,0.00031273894,0.00023367419,0.00044917324,0.0000892115,0.00014777067,0.0017526787],"category_scores_gemma":[0.001771926,0.00011329789,0.00023468965,0.00045248878,0.00022715899,0.00024379333,0.00030170396,0.00012528876,0.00020334164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007029696,0.000003294449,0.9975581,0.000003954779,0.000038614373,0.000026308919,0.00005502296,0.00037241247,0.0007098777,0.000027237042,0.00005173742,0.0010830893],"study_design_scores_gemma":[0.0000014909423,0.000009316914,0.99902225,0.0000011329323,0.000010019612,0.00002119694,0.000052301224,0.0006719047,0.00008793062,0.000031027164,0.000089793175,0.0000016429123],"about_ca_topic_score_codex":0.005763623,"about_ca_topic_score_gemma":0.01058265,"teacher_disagreement_score":0.005763623,"about_ca_system_score_codex":0.00010586226,"about_ca_system_score_gemma":0.00013130659,"threshold_uncertainty_score":0.011460125},"labels":[],"label_agreement":null},{"id":"W2746591632","doi":"10.1002/2017gl073933","title":"Intense oceanic uptake of oxygen during 2014–2015 winter convection in the Labrador Sea","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"","keywords":"Mixed layer; Oxygen; Convection; Forcing (mathematics); Atmospheric sciences; Mooring; Environmental science; Geology; Deep convection; Climatology; Oceanography; Chemistry; Meteorology; Physics","score_opus":0.02945947231710832,"score_gpt":0.2802237697949837,"score_spread":0.2507642974778754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2746591632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99934083,0.000027316753,0.000045593337,0.000014095401,0.0000020440218,0.0000021861208,0.0003580239,0.000014744577,0.00019517423],"genre_scores_gemma":[0.999212,0.000017386183,0.000053417483,0.00000896658,0.0000024093604,0.000003330147,0.0005823154,0.0000034828354,0.000116777366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998424,0.000020302316,0.000014524127,0.00005500892,0.000019979763,0.000047696867],"domain_scores_gemma":[0.9998386,0.0000181432,0.00006194004,0.000017896682,0.000032493448,0.000030842522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030580544,0.0004200051,0.00037115024,0.00061537983,0.00036376482,0.00072394905,0.00036574565,0.00036768595,0.00050433114],"category_scores_gemma":[0.0003676493,0.00019948265,0.000447169,0.00048244555,0.00031397722,0.00045233508,0.00050752284,0.00020342483,0.00019881787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009419223,0.00012272206,0.9594437,0.00006319028,0.00030996243,0.0001989908,0.00034002092,0.0045439876,0.02373141,0.00007670316,0.0005732545,0.009654191],"study_design_scores_gemma":[0.000008163248,0.0000591068,0.9948602,0.0000047973745,0.000029980018,0.000014606956,0.00014814749,0.0024784992,0.0021184853,0.000010395675,0.00025856064,0.000009103053],"about_ca_topic_score_codex":0.09407223,"about_ca_topic_score_gemma":0.08243814,"teacher_disagreement_score":0.09407223,"about_ca_system_score_codex":0.0012264503,"about_ca_system_score_gemma":0.0005623209,"threshold_uncertainty_score":0.18704933},"labels":[],"label_agreement":null},{"id":"W2747033520","doi":"10.1002/2017gl074388","title":"Considerable contribution of the Montreal Protocol to declining greenhouse gas emissions from the United States","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Climate Program Office; Biological and Environmental Research; National Oceanic and Atmospheric Administration; California Air Resources Board; U.S. Department of Energy","keywords":"Montreal Protocol; Greenhouse gas; Environmental science; Kyoto Protocol; Atmospheric sciences; Atmosphere (unit); Climatology; Ozone; Ozone layer; Environmental protection; Meteorology; Geography","score_opus":0.03012061154421803,"score_gpt":0.31935638706043634,"score_spread":0.2892357755162183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2747033520","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3383337,0.030421471,0.025221327,0.10890107,0.0034515096,0.0018827257,0.07190012,0.0015414428,0.41834667],"genre_scores_gemma":[0.8956211,0.009761721,0.010951924,0.012827649,0.00046516836,0.00065493287,0.017069206,0.00020519589,0.052443024],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99744177,0.00041861227,0.00010254045,0.00034024208,0.0013445225,0.000352254],"domain_scores_gemma":[0.99258375,0.00079101144,0.001045247,0.00043988266,0.0046140696,0.000526036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003398248,0.0005337981,0.00017980755,0.0020603165,0.0014812512,0.002352023,0.0015242907,0.0006991866,0.0051861713],"category_scores_gemma":[0.009076597,0.00024373196,0.00043238286,0.0024760587,0.00085866736,0.0011034964,0.0012841779,0.0014435737,0.00037966025],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025776547,0.00015178758,0.20775172,0.000887833,0.0003502738,0.0005867037,0.0009915229,0.010921272,0.006303718,0.07060119,0.34528318,0.35591307],"study_design_scores_gemma":[0.00002770703,0.00011893591,0.46108663,0.0004650046,0.0000889361,0.00010471473,0.0005115007,0.004182823,0.0032722573,0.003424172,0.526581,0.00013640843],"about_ca_topic_score_codex":0.8790784,"about_ca_topic_score_gemma":0.8861297,"teacher_disagreement_score":0.8790784,"about_ca_system_score_codex":0.014615815,"about_ca_system_score_gemma":0.0273401,"threshold_uncertainty_score":0.24326742},"labels":[],"label_agreement":null},{"id":"W2749120426","doi":"10.1002/2017gl075381","title":"Mapping fluids to subduction megathrust locking and slip behavior","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Subduction; Geology; Magnetotellurics; Seismology; Episodic tremor and slip; Slip (aerodynamics); Electrical resistivity and conductivity; Thrust; Pore water pressure; Electrical conductor; Creep; Geophysics; Petrology; Geotechnical engineering; Tectonics; Materials science","score_opus":0.0751477371591958,"score_gpt":0.32332269394164453,"score_spread":0.24817495678244872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2749120426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988763,0.00013466932,0.00052296004,0.000020561885,0.0000021054786,0.0000037090877,0.00012663903,0.000021811686,0.00029124352],"genre_scores_gemma":[0.9993544,0.0000513501,0.00039431066,0.0000041334315,0.0000020376851,0.0000021503577,0.00009146205,0.0000037100317,0.00009637551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993134,0.000012156366,0.0000051424227,0.000022502216,0.000011153968,0.000017701059],"domain_scores_gemma":[0.99966574,0.00006888124,0.00013645187,0.00002028675,0.00005457452,0.000054093096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019746498,0.0002646912,0.00019273697,0.0020696388,0.00021342676,0.0008443716,0.00018229862,0.00031319755,0.0008026697],"category_scores_gemma":[0.0009739844,0.00016325162,0.00014381131,0.0011916828,0.0003645395,0.00059802434,0.0007661953,0.00021486172,0.00022790549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004282657,0.000110032,0.8976904,0.00008151658,0.00007803345,0.00020167927,0.00090644567,0.0022143165,0.061479386,0.0003641659,0.00019539466,0.03625036],"study_design_scores_gemma":[0.000011638134,0.00008309626,0.9825173,0.000022408118,0.000034529152,0.000112024776,0.0009182151,0.00830534,0.006912331,0.00042888767,0.00064060773,0.000013560216],"about_ca_topic_score_codex":0.0026895646,"about_ca_topic_score_gemma":0.0039988784,"teacher_disagreement_score":0.0026895646,"about_ca_system_score_codex":0.00023180619,"about_ca_system_score_gemma":0.00016005212,"threshold_uncertainty_score":0.0053477883},"labels":[],"label_agreement":null},{"id":"W2749130577","doi":"10.1002/2017gl074602","title":"Net community production in the bottom of first‐year sea ice over the Arctic spring bloom","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Canada Excellence Research Chairs, Government of Canada; Canada Foundation for Innovation; University of Manitoba; ArcticNet; Marine Environmental Observation Prediction and Response Network","keywords":"Autotroph; Productivity; Environmental science; Photosynthesis; Algae; Spring bloom; Sea ice; Oceanography; Dominance (genetics); Bloom; Trophic level; Heterotroph; Arctic; Phytoplankton; Ecology; Biology; Nutrient; Botany; Geology","score_opus":0.039175577352801735,"score_gpt":0.2878210653647861,"score_spread":0.24864548801198433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2749130577","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990771,0.0000797937,0.00006676417,0.00000949051,0.0000026831908,0.000001415549,0.00050965726,0.0000037475868,0.00024930245],"genre_scores_gemma":[0.99886936,0.00005563697,0.00009691219,0.0000064062465,0.000003256755,0.0000035676403,0.0007344424,0.0000023342864,0.0002280785],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992883,0.000011283762,0.0000032075163,0.00001575498,0.000018362647,0.000022502354],"domain_scores_gemma":[0.99968374,0.000039442573,0.00008160868,0.000011596548,0.00009672904,0.00008683612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028483194,0.00026119032,0.00023703155,0.00081758684,0.00045747223,0.0006225891,0.00014474406,0.00017315455,0.00065920013],"category_scores_gemma":[0.00044452804,0.00014693874,0.0002235749,0.0004022039,0.00018934911,0.00023749008,0.00032513286,0.00014042895,0.00022452061],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038391846,0.00002273478,0.96749663,0.00003602257,0.00007749166,0.00009531383,0.0003021125,0.00073742087,0.025977336,0.00007135525,0.0002101029,0.0045895376],"study_design_scores_gemma":[0.0000012707246,0.000022137761,0.9989151,0.0000024785254,0.0000063247317,0.00002769208,0.00012710072,0.00039759354,0.00035336608,0.00002077535,0.0001243949,0.0000018480841],"about_ca_topic_score_codex":0.026631363,"about_ca_topic_score_gemma":0.051271204,"teacher_disagreement_score":0.026631363,"about_ca_system_score_codex":0.0007789477,"about_ca_system_score_gemma":0.00036414145,"threshold_uncertainty_score":0.052952707},"labels":[],"label_agreement":null},{"id":"W2750687209","doi":"10.1002/2017gl074095","title":"Significant lateral dip changes may have limited the scale of the 2015 <i>M</i><sub><i>w</i></sub> 7.8 Gorkha earthquake","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Japan Aerospace Exploration Agency; National Natural Science Foundation of China","keywords":"Geology; Seismology; Aftershock; Geodetic datum; Anomaly (physics); Earthquake rupture; Slip (aerodynamics); Fault (geology); Magnetic dip; Slab; Geodesy; Geophysics; Physics","score_opus":0.046186534312128075,"score_gpt":0.2847731819454449,"score_spread":0.2385866476333168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2750687209","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99546874,0.0000600973,0.0007369658,0.00009158109,0.000014282694,0.000007664379,0.0002610209,0.000054504224,0.003305144],"genre_scores_gemma":[0.9995049,0.000019491004,0.00011899129,0.000012175705,0.0000035897663,0.000002575261,0.00012037429,0.000005603049,0.00021230138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998851,0.000018709716,0.000011999367,0.000029617573,0.000014018745,0.00004048331],"domain_scores_gemma":[0.9996835,0.000050507882,0.0000980014,0.000049127524,0.00006754642,0.00005130121],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022793375,0.00019470356,0.00031352197,0.00033981522,0.00024355286,0.00065903494,0.00027838824,0.00019114897,0.0046388814],"category_scores_gemma":[0.0008585251,0.00013914362,0.0002349028,0.00038393945,0.00034153217,0.00045170292,0.00057883386,0.00029847052,0.0005811612],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027653252,0.0001097554,0.8911971,0.00018199948,0.00013900062,0.0005449027,0.0004946497,0.0049802437,0.0673805,0.002029237,0.0010278716,0.031638235],"study_design_scores_gemma":[0.000011093268,0.00009585616,0.9894587,0.000016554855,0.000039556355,0.0001537152,0.00051192957,0.0047929087,0.0026922717,0.0005239005,0.0016887136,0.000014816314],"about_ca_topic_score_codex":0.0057274248,"about_ca_topic_score_gemma":0.009509079,"teacher_disagreement_score":0.0057274248,"about_ca_system_score_codex":0.00032276096,"about_ca_system_score_gemma":0.00030876254,"threshold_uncertainty_score":0.015518606},"labels":[],"label_agreement":null},{"id":"W2751094819","doi":"10.1002/2017gl074186","title":"Low Evapotranspiration Enhances the Resilience of Peatland Carbon Stocks to Fire","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; McMaster University; University of Lethbridge; University of Alberta","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Peat; Evapotranspiration; Environmental science; Boreal; Ecohydrology; Hydrology (agriculture); Disturbance (geology); Ecosystem; Ecology; Geology; Geomorphology","score_opus":0.0233291798313626,"score_gpt":0.3119148137775006,"score_spread":0.28858563394613795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2751094819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938035,0.000018756999,0.00009697721,0.0000067359706,6.5467043e-7,9.0267264e-7,0.000035831097,0.000007540685,0.00045221485],"genre_scores_gemma":[0.9998274,0.000006491172,0.00003951613,0.0000027483961,2.8986838e-7,3.7690518e-7,0.000019175803,0.0000011701019,0.00010299716],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999627,0.0000029762768,0.0000016453043,0.000008575049,0.000004838323,0.00001915701],"domain_scores_gemma":[0.9998233,0.000021862243,0.000041176205,0.000017253848,0.000027953276,0.00006853881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010499546,0.00009071161,0.0001351842,0.00018787336,0.0002237406,0.0004008661,0.00014217675,0.00011584696,0.0014737872],"category_scores_gemma":[0.00023896557,0.00006778486,0.00007761756,0.0001155871,0.000259908,0.00021280049,0.00020308373,0.00014928877,0.000097079756],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005386386,0.00013206764,0.42328754,0.000054302163,0.000079460304,0.000311835,0.00025839862,0.0033078745,0.55724204,0.00059998117,0.00027714128,0.013910664],"study_design_scores_gemma":[0.0000018952893,0.000043867778,0.989301,0.0000036653298,0.000008278236,0.00009465675,0.00017851232,0.001053395,0.008820532,0.00021053439,0.00027979937,0.0000037723253],"about_ca_topic_score_codex":0.020636365,"about_ca_topic_score_gemma":0.05642865,"teacher_disagreement_score":0.020636365,"about_ca_system_score_codex":0.0004831234,"about_ca_system_score_gemma":0.00032087317,"threshold_uncertainty_score":0.041032553},"labels":[],"label_agreement":null},{"id":"W2751299226","doi":"10.1002/2017gl074759","title":"Experimental Evidence of Arctic Summer Mesospheric Upwelling and Its Connection to Cold Summer Mesopause","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Jet Propulsion Laboratory; Canada Excellence Research Chairs, Government of Canada; Canada Research Chairs","keywords":"Mesopause; Mesosphere; Atmospheric sciences; Global wind patterns; Wind speed; Geology; Thermosphere; Geostrophic wind; Divergence (linguistics); Environmental science; Climatology; Stratosphere; Geophysics; Ionosphere; Oceanography","score_opus":0.06122173321687211,"score_gpt":0.35711839908011883,"score_spread":0.2958966658632467,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2751299226","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987349,0.0000899564,0.00013553766,0.000010984275,0.0000074098825,0.0000066499465,0.00032952227,0.000005742264,0.0006793935],"genre_scores_gemma":[0.99894446,0.000055065917,0.00014546492,0.000017933908,0.000008121378,0.0000129145765,0.0005240179,0.0000039300107,0.0002882228],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998733,0.000024876848,0.000009537776,0.00003503023,0.000027933113,0.00002937259],"domain_scores_gemma":[0.9992859,0.00011944358,0.00019240586,0.000088801884,0.00015114054,0.00016237635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029267944,0.00018067494,0.00019148168,0.00032971174,0.00045423929,0.0002922581,0.00013905556,0.00019637092,0.0012722173],"category_scores_gemma":[0.00044037073,0.00013772526,0.00012431697,0.00021407606,0.00027590184,0.00017395699,0.00021174965,0.0003037937,0.00017438015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002402805,0.00038233475,0.5659762,0.00006896535,0.00012389624,0.00022386175,0.000275231,0.00024185175,0.42293957,0.00007988243,0.00027269902,0.0070128003],"study_design_scores_gemma":[0.0000060710704,0.0003116815,0.98914146,0.0000028967918,0.000011695879,0.000044811673,0.0000761444,0.00016304746,0.009889018,0.000018360235,0.00033122557,0.0000035763474],"about_ca_topic_score_codex":0.005797621,"about_ca_topic_score_gemma":0.010931243,"teacher_disagreement_score":0.005797621,"about_ca_system_score_codex":0.0003158588,"about_ca_system_score_gemma":0.00016769751,"threshold_uncertainty_score":0.011527777},"labels":[],"label_agreement":null},{"id":"W2752523941","doi":"10.1002/2017gl074046","title":"What are the contemporary sources of sediment in the Mississippi River?","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia; Simon Fraser University; University of British Columbia","funders":"U.S. Geological Survey","keywords":"Sediment; Erosion; Hydrology (agriculture); Drainage basin; Arable land; Sedimentary budget; Floodplain; Environmental science; Structural basin; Land use; Geology; Sediment transport; Agriculture; Geography; Ecology; Geomorphology; Archaeology","score_opus":0.10803952108899478,"score_gpt":0.3203086432743244,"score_spread":0.21226912218532962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2752523941","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981744,0.0004120441,0.00016513646,0.0002837834,0.000002361582,8.689184e-7,0.0002173097,0.0000052972423,0.00073870714],"genre_scores_gemma":[0.99942577,0.00022552063,0.00008211836,0.000017055196,0.0000074173,0.0000010739719,0.000111267516,0.0000022855882,0.00012756858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984443,0.000024032079,0.000014527426,0.000058408783,0.00003045342,0.000027996712],"domain_scores_gemma":[0.9992605,0.0000924781,0.00028367335,0.000043615746,0.00023330103,0.000086476706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041286915,0.00012115471,0.00013226377,0.001325557,0.00069245853,0.0012931142,0.000295767,0.00032383853,0.00092534826],"category_scores_gemma":[0.0014671317,0.00015800355,0.0001158621,0.0021336593,0.00054736395,0.0009236552,0.00049726653,0.00022516651,0.00015058149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022077924,0.000011456814,0.9798306,0.000034015062,0.00007387851,0.00016045473,0.0016290166,0.00044371386,0.0013292768,0.00045331448,0.00028403915,0.015728135],"study_design_scores_gemma":[5.3597523e-7,0.0000070711394,0.99717593,0.000013062697,0.0000075716675,0.00007954069,0.0010257127,0.00034038696,0.00009850123,0.00018537714,0.0010619229,0.0000043234077],"about_ca_topic_score_codex":0.04350374,"about_ca_topic_score_gemma":0.1275667,"teacher_disagreement_score":0.04350374,"about_ca_system_score_codex":0.0011138321,"about_ca_system_score_gemma":0.0005013372,"threshold_uncertainty_score":0.086501},"labels":[],"label_agreement":null},{"id":"W2753057425","doi":"10.1002/2017gl074826","title":"Thermal State, Slab Metamorphism, and Interface Seismicity in the Cascadia Subduction Zone Based On 3‐D Modeling","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Subduction; Geology; Slab; Seismology; Eclogitization; Episodic tremor and slip; Metamorphism; Induced seismicity; Slab window; Geophysics; Petrology; Oceanic crust; Tectonics","score_opus":0.0629607306426964,"score_gpt":0.3067962757409377,"score_spread":0.2438355450982413,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2753057425","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920568,0.00004819981,0.005433083,0.000107779604,0.000007631964,0.000012779744,0.00034442337,0.0002028984,0.0017864003],"genre_scores_gemma":[0.9983991,0.00003418802,0.0011092279,0.0000091078755,0.0000030542901,0.000012591964,0.00014749554,0.000018130715,0.0002670626],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993944,0.000015443551,0.0000050793988,0.00001772066,0.000010009224,0.000012239991],"domain_scores_gemma":[0.99977165,0.00008156971,0.000043953314,0.000025735433,0.000032162854,0.00004486469],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018426975,0.0006732556,0.00035584276,0.00072041433,0.0005012739,0.00067715964,0.00081107527,0.00087904785,0.0013519729],"category_scores_gemma":[0.0006509235,0.0006222142,0.0012479792,0.00045678354,0.00046436815,0.00030046562,0.0004792294,0.0004665876,0.00015838153],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002863813,0.00002599948,0.012532551,0.000007148487,0.000033344757,0.000052975844,0.000037795664,0.9853419,0.0010514864,0.00019792956,0.00006123204,0.00062905485],"study_design_scores_gemma":[0.0000073461024,0.0000073357833,0.004669167,0.0000016965239,0.000008270054,0.0000060701163,0.000013345276,0.9950342,0.000083349696,0.00010633487,0.00005616867,0.0000067039527],"about_ca_topic_score_codex":0.126739,"about_ca_topic_score_gemma":0.058995575,"teacher_disagreement_score":0.126739,"about_ca_system_score_codex":0.0014973312,"about_ca_system_score_gemma":0.00097418355,"threshold_uncertainty_score":0.2520026},"labels":[],"label_agreement":null},{"id":"W2754463559","doi":"10.1002/2017gl074394","title":"Local‐Scale Advection of Sensible and Latent Heat During Snowmelt","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Snowmelt; Sensible heat; Latent heat; Advection; Environmental science; Snow; Humidity; Atmospheric sciences; Climatology; Meteorology; Geology; Geography; Thermodynamics; Physics","score_opus":0.040353711071505004,"score_gpt":0.28445354175215726,"score_spread":0.24409983068065225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2754463559","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999421,0.000013836226,0.0001864863,0.00000585728,0.000002040069,0.000003609412,0.00007354439,0.00001942974,0.000274114],"genre_scores_gemma":[0.9997745,0.000006496687,0.0000588116,0.0000027769597,0.0000013506179,0.0000023139833,0.000069796624,0.0000035757805,0.000080474376],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.0000037238806,0.0000012211199,0.000009915132,0.000008079877,0.000009867353],"domain_scores_gemma":[0.9998975,0.000030440053,0.00001561338,0.000009017287,0.000019737723,0.000027670769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009444748,0.000114862705,0.00019476096,0.00019684556,0.00022953648,0.0002961996,0.00012799451,0.00013771778,0.0008221301],"category_scores_gemma":[0.00015879997,0.000116874086,0.00012616068,0.00015163055,0.00025561254,0.00032912666,0.00018830036,0.00025334134,0.00015646023],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001203369,0.00020960285,0.091227055,0.00006552663,0.00004413218,0.00018535493,0.000470926,0.0027637067,0.8958942,0.00016861282,0.00024534424,0.0075221285],"study_design_scores_gemma":[0.000048467497,0.00037873068,0.9149051,0.0000059811678,0.000017629072,0.00006816226,0.00030795712,0.014584198,0.06904275,0.00014035587,0.00048526813,0.000015506055],"about_ca_topic_score_codex":0.0027563286,"about_ca_topic_score_gemma":0.0030802346,"teacher_disagreement_score":0.0027563286,"about_ca_system_score_codex":0.00019127986,"about_ca_system_score_gemma":0.00011186847,"threshold_uncertainty_score":0.005480647},"labels":[],"label_agreement":null},{"id":"W2755213029","doi":"10.1002/2017gl073570","title":"GPS Signal Corruption by the Discrete Aurora: Precise Measurements From the Mahali Experiment","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Sleep Foundation; National Science Foundation","keywords":"Global Positioning System; Substorm; GPS signals; Geodesy; SIGNAL (programming language); Context (archaeology); Scintillation; Ionosphere; Lock (firearm); Geology; Phase (matter); Remote sensing; Interplanetary scintillation; Amplitude; Physics; Geophysics; Meteorology; Assisted GPS; Computer science; Geography; Telecommunications; Optics; Magnetic field; Magnetosphere; Detector","score_opus":0.05057544048858411,"score_gpt":0.3302412302366582,"score_spread":0.2796657897480741,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2755213029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936813,0.0000062855415,0.0003119877,0.000006123318,5.8413315e-7,0.0000026875045,0.00008389047,0.000009205393,0.00021107768],"genre_scores_gemma":[0.99951947,0.0000074180093,0.00023296858,0.0000042214497,0.0000020816099,0.0000035559833,0.00014889172,0.0000032400578,0.000078155805],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99967515,0.000070082686,0.000014972239,0.00007206887,0.000116626434,0.00005101401],"domain_scores_gemma":[0.99910116,0.000246481,0.00018737718,0.00019605165,0.000166994,0.000102041085],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034063242,0.00014605228,0.00017665046,0.0004170519,0.00040083303,0.00040669172,0.00035037697,0.00024144955,0.00036607042],"category_scores_gemma":[0.0011718454,0.0001153142,0.00007760209,0.00047340302,0.00045566825,0.00028535575,0.00045531438,0.00033039672,0.0001356973],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021635839,0.00034684504,0.7515677,0.000049397328,0.00015093629,0.0002989683,0.0029381467,0.0034440102,0.21439895,0.00067223946,0.00043465776,0.023534648],"study_design_scores_gemma":[0.000028659979,0.00027591424,0.97740513,0.000003365703,0.000045034285,0.00009173266,0.00027912162,0.003447075,0.017744929,0.00006462303,0.0005966697,0.0000176664],"about_ca_topic_score_codex":0.02216151,"about_ca_topic_score_gemma":0.038747124,"teacher_disagreement_score":0.02216151,"about_ca_system_score_codex":0.0004531991,"about_ca_system_score_gemma":0.0002536807,"threshold_uncertainty_score":0.04406506},"labels":[],"label_agreement":null},{"id":"W2755256037","doi":"10.1002/2017gl075127","title":"In Situ Stress and Pore Pressure in the Deep Interior of the Nankai Accretionary Prism, Integrated Ocean Drilling Program Site C0002","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"Japan Agency for Marine-Earth Science and Technology; Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology; National Science Foundation","keywords":"Accretionary wedge; Geology; Pore water pressure; Drilling; Seismology; Borehole; Slip (aerodynamics); Subduction; Petrology; Décollement; Differential stress; Fault (geology); Geotechnical engineering; Tectonics; Deformation (meteorology)","score_opus":0.027340922005032187,"score_gpt":0.29618032709234343,"score_spread":0.26883940508731125,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2755256037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993886,0.000006031217,0.00007347814,0.0000044182807,6.367389e-7,0.0000032340895,0.00019634199,0.0000064576916,0.0003208368],"genre_scores_gemma":[0.99890435,0.000012825638,0.00042055774,0.000006446228,0.0000012108926,0.0000103913535,0.0004210319,0.000003008012,0.00022023254],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989045,0.000007014482,0.000007129471,0.00004312446,0.00003131297,0.000020842554],"domain_scores_gemma":[0.99980575,0.00002099327,0.000048228667,0.000014118348,0.000056194083,0.000054741893],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015932444,0.00028418476,0.00018440386,0.00066875585,0.00041204525,0.00041617578,0.00043309218,0.00031538188,0.00045308637],"category_scores_gemma":[0.00036510782,0.0002738856,0.00014699591,0.0005351872,0.00035347484,0.00029810308,0.0005710892,0.00025075322,0.00012844506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026414567,0.00015740986,0.83068085,0.000037890506,0.000038958773,0.00030882857,0.0013383876,0.0008507959,0.15812801,0.0000739577,0.00016726622,0.007953542],"study_design_scores_gemma":[0.000008052464,0.000043361586,0.996071,0.0000027381825,0.000008237294,0.000045883993,0.00022381285,0.001232023,0.0022128783,0.000011579547,0.00013551328,0.00000494194],"about_ca_topic_score_codex":0.04340556,"about_ca_topic_score_gemma":0.095994644,"teacher_disagreement_score":0.04340556,"about_ca_system_score_codex":0.00046375062,"about_ca_system_score_gemma":0.00049993757,"threshold_uncertainty_score":0.08630586},"labels":[],"label_agreement":null},{"id":"W2756223094","doi":"10.1002/2017gl074702","title":"Quantifying CO<sub>2</sub> Emissions From Individual Power Plants From Space","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":351,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Waterloo; Environment and Climate Change Canada","funders":"California Institute of Technology; U.S. Environmental Protection Agency; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Environmental science; Observatory; Greenhouse gas; Satellite; Emission inventory; Plume; Meteorology; Atmospheric sciences; Remote sensing; Aerospace engineering; Geography; Geology; Engineering; Physics","score_opus":0.04709844231046258,"score_gpt":0.31180132387826404,"score_spread":0.2647028815678015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2756223094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99093443,0.000096414566,0.006139481,0.000040741073,0.000007618983,0.000011315026,0.0005594735,0.000114549526,0.002095908],"genre_scores_gemma":[0.9973246,0.00003261385,0.0020740828,0.000009842863,0.000003351287,0.000005270012,0.0002967567,0.000011786927,0.00024171287],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999013,0.000010136911,0.0000024580434,0.0000381041,0.00003367781,0.000014250864],"domain_scores_gemma":[0.9998939,0.000023876322,0.00002351786,0.000017116477,0.00002766249,0.000013983951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013487453,0.00033658792,0.0001989104,0.00045845774,0.0002747919,0.00038423348,0.00024521022,0.0004088491,0.0007723137],"category_scores_gemma":[0.0002567444,0.00011668145,0.0001709903,0.00066147203,0.00019132528,0.0005840824,0.00024678517,0.00027076117,0.00015130342],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052874355,0.00020302444,0.513353,0.0001314997,0.00034426828,0.0003814842,0.00023863839,0.12556349,0.29823267,0.0011258932,0.001643186,0.05825414],"study_design_scores_gemma":[0.000026434645,0.00024224863,0.5320021,0.00001742978,0.00014568967,0.00021937351,0.0004933356,0.27789485,0.18209541,0.0016050398,0.0051945597,0.00006353618],"about_ca_topic_score_codex":0.007458998,"about_ca_topic_score_gemma":0.018516812,"teacher_disagreement_score":0.007458998,"about_ca_system_score_codex":0.00037462343,"about_ca_system_score_gemma":0.0001974678,"threshold_uncertainty_score":0.014831126},"labels":[],"label_agreement":null},{"id":"W2756297478","doi":"10.1002/2017gl074954","title":"BedMachine v3: Complete Bed Topography and Ocean Bathymetry Mapping of Greenland From Multibeam Echo Sounding Combined With Mass Conservation","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":1070,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; University of Ottawa","funders":"Natural Environment Research Council; University of California, Irvine; University of Bristol; York University; Sight Research UK; Pinngortitaleriffik; National Aeronautics and Space Administration; National Science Foundation","keywords":"Bathymetry; Echo sounding; Geology; Depth sounding; Echo (communications protocol); Remote sensing; Oceanography; Water mass; Geomorphology","score_opus":0.034616332352679004,"score_gpt":0.27759755790897583,"score_spread":0.24298122555629684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2756297478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49855894,0.00042432113,0.11934698,0.00025724564,0.00013615712,0.00039126343,0.2873181,0.06813592,0.025431164],"genre_scores_gemma":[0.65219855,0.0003978083,0.13928376,0.00022258436,0.000057682584,0.00043827825,0.18972747,0.004864808,0.012808965],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998764,0.000008417155,0.0000056869526,0.000038364844,0.000041360698,0.000029729008],"domain_scores_gemma":[0.9998306,0.000019812895,0.000024046716,0.00003842431,0.00005119009,0.00003586947],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023913104,0.00059943105,0.00028104198,0.0013411555,0.00021598504,0.00062382815,0.0006290382,0.000308376,0.014329895],"category_scores_gemma":[0.00037338355,0.0003791096,0.00038043867,0.0011155088,0.0001861995,0.00047602467,0.0010037511,0.00032012883,0.0034330853],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050212507,0.00027156013,0.16782808,0.0005225615,0.0004210824,0.0009347178,0.0018552679,0.023360299,0.10813017,0.001733512,0.19508971,0.49935085],"study_design_scores_gemma":[0.00018309422,0.00012284465,0.74132705,0.00013501963,0.00009897031,0.00051022886,0.00074585655,0.09312841,0.024531782,0.0019832063,0.13705613,0.0001774395],"about_ca_topic_score_codex":0.04235132,"about_ca_topic_score_gemma":0.09368061,"teacher_disagreement_score":0.04235132,"about_ca_system_score_codex":0.00030950023,"about_ca_system_score_gemma":0.0008207385,"threshold_uncertainty_score":0.08420956},"labels":[],"label_agreement":null},{"id":"W2756374360","doi":"10.1002/2017gl075123","title":"Using Noble Gas Measurements to Derive Air‐Sea Process Information and Predict Physical Gas Saturations","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Noble gas; Supersaturation; Environmental science; Bubble; Thermodynamics; Saturation (graph theory); Atmospheric sciences; Mechanics; Physics; Atomic physics","score_opus":0.06901564791017623,"score_gpt":0.3294261007380271,"score_spread":0.26041045282785086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2756374360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9562628,0.000102103586,0.039501365,0.000042770138,0.000008023443,0.00001972855,0.0006234724,0.00043160052,0.0030082336],"genre_scores_gemma":[0.9962423,0.000033742457,0.0034533828,0.000004534535,0.0000014180035,0.0000059821396,0.00011256092,0.000016435886,0.00012965706],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999474,0.000008095506,0.0000033746096,0.00001637986,0.000016855452,0.000007948645],"domain_scores_gemma":[0.99982184,0.00009167594,0.00003206826,0.000020828486,0.000024366484,0.000009325741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029641768,0.00036347882,0.00012650412,0.0006185592,0.00021235824,0.00031501078,0.0002473555,0.00025638504,0.0005982327],"category_scores_gemma":[0.0006724967,0.00017601709,0.00026928063,0.00031973782,0.00028828552,0.0005836016,0.00026587694,0.0002617537,0.00013280314],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047211978,0.00010047735,0.30401078,0.00014670331,0.0001660975,0.00015764956,0.00034709557,0.28133425,0.35596934,0.005614049,0.00048290245,0.05119852],"study_design_scores_gemma":[0.000021692018,0.000070145274,0.07038004,0.000007732035,0.00003480582,0.0000345182,0.000057764566,0.8047414,0.12240819,0.0013268567,0.00089516246,0.000021715718],"about_ca_topic_score_codex":0.014231186,"about_ca_topic_score_gemma":0.015515115,"teacher_disagreement_score":0.014231186,"about_ca_system_score_codex":0.00048523952,"about_ca_system_score_gemma":0.00027531586,"threshold_uncertainty_score":0.028296709},"labels":[],"label_agreement":null},{"id":"W2756451716","doi":"10.1002/2017gl074699","title":"A Dynamic Model of Mercury's Magnetospheric Magnetic Field","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Science Mission Directorate; National Aeronautics and Space Administration","keywords":"Magnetosphere; Magnetopause; Mercury's magnetic field; Physics; Dipole model of the Earth's magnetic field; Solar wind; Magnetic field; Interplanetary magnetic field; Geophysics; Computational physics; L-shell; Earth's magnetic field","score_opus":0.02470586056458812,"score_gpt":0.3021505949961351,"score_spread":0.277444734431547,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2756451716","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.5120346,0.0008371769,0.40099767,0.002195646,0.00029522943,0.00010274562,0.004656362,0.0019091555,0.076971434],"genre_scores_gemma":[0.97385967,0.0004735535,0.010896775,0.00012911757,0.000113430106,0.00009030035,0.0011868863,0.00016577698,0.013084456],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991524,0.000013358481,0.0000032415203,0.000032428572,0.000021582999,0.000014157986],"domain_scores_gemma":[0.9998623,0.000030430738,0.000027716173,0.0000161632,0.00004201024,0.000021329097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001447562,0.00045329306,0.00052167085,0.0003899011,0.00046576635,0.00080032076,0.0013141818,0.0008457888,0.0022429875],"category_scores_gemma":[0.0005541991,0.00033092822,0.00051537104,0.0006369062,0.00048739763,0.000973803,0.0006251581,0.000489403,0.00040265964],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027674261,0.000012293104,0.0013629786,0.000021639402,0.000026482396,0.000054307267,0.000035971843,0.9871503,0.0016025412,0.005694116,0.0007084705,0.003303212],"study_design_scores_gemma":[0.000021753829,0.000012916256,0.0010930015,0.0000036359395,0.000016414922,0.00002243611,0.00001206227,0.995261,0.00014456206,0.0018379117,0.0015642628,0.000009957368],"about_ca_topic_score_codex":0.044848222,"about_ca_topic_score_gemma":0.023194315,"teacher_disagreement_score":0.044848222,"about_ca_system_score_codex":0.0010414132,"about_ca_system_score_gemma":0.0011534052,"threshold_uncertainty_score":0.08917439},"labels":[],"label_agreement":null},{"id":"W2757846965","doi":"10.1002/2017gl075104","title":"Bounce Resonance Scattering of Radiation Belt Electrons by Low‐Frequency Hiss: Comparison With Cyclotron and Landau Resonances","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Hiss; Physics; Scattering; Electron; Pitch angle; Van Allen radiation belt; Cyclotron resonance; Resonance (particle physics); Atomic physics; Plasmasphere; Adiabatic invariant; Computational physics; Magnetosphere; Cyclotron; Magnetic field; Optics; Geophysics; Nuclear physics","score_opus":0.011349070985891972,"score_gpt":0.28858528428210267,"score_spread":0.2772362132962107,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2757846965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99712545,0.00012376271,0.0016051295,0.000010677772,0.0000035049468,0.0000040615037,0.000010747857,0.000019679945,0.0010970633],"genre_scores_gemma":[0.999673,0.000024326939,0.00013487895,0.0000015639607,0.0000010089315,0.0000014255256,0.00001056372,0.000002757028,0.00015061823],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992454,0.000012862402,0.0000036071071,0.000015095807,0.000016176713,0.000027762791],"domain_scores_gemma":[0.9997428,0.000109422246,0.000053127027,0.000028410881,0.00003786288,0.000028310671],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028442926,0.00021827161,0.00017595198,0.0003040597,0.0002446008,0.0003485717,0.00023141222,0.00011897445,0.0012007807],"category_scores_gemma":[0.00042318873,0.00012018633,0.00018207003,0.00014132657,0.00032738232,0.0002880693,0.00023424189,0.00019959948,0.00010203622],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011896022,0.00013135254,0.08186803,0.00029352252,0.00012996445,0.0006940168,0.000886469,0.031662554,0.8530646,0.009798927,0.00022383103,0.020057172],"study_design_scores_gemma":[0.000099780984,0.00084851217,0.18215415,0.000024988176,0.0001191143,0.00052875536,0.00087977806,0.32544035,0.48475468,0.0029201466,0.0021640514,0.00006569026],"about_ca_topic_score_codex":0.0012271595,"about_ca_topic_score_gemma":0.00075831544,"teacher_disagreement_score":0.0012271595,"about_ca_system_score_codex":0.00036260133,"about_ca_system_score_gemma":0.000102822014,"threshold_uncertainty_score":0.004017055},"labels":[],"label_agreement":null},{"id":"W2761240152","doi":"10.1002/2017gl075434","title":"Ice and Snow Thickness Variability and Change in the High Arctic Ocean Observed by In Situ Measurements","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Precision Nanosystems (Canada); University of Alberta; Environment and Climate Change Canada; York University","funders":"British Antarctic Survey; Office of Naval Research; Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Sight Research UK; National Aeronautics and Space Administration; European Space Agency; Environment and Climate Change Canada","keywords":"Snow; Sea ice; Geology; Arctic; Arctic ice pack; Climatology; Cryosphere; Glacier; Oceanography; Geomorphology","score_opus":0.09149556377561827,"score_gpt":0.2986880464324421,"score_spread":0.20719248265682386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2761240152","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991117,0.0000290633,0.00019052935,0.0000048200404,0.0000042367037,0.000001676396,0.00034050486,0.0000069274806,0.00031040877],"genre_scores_gemma":[0.9987704,0.00004160862,0.0003301395,0.000006468257,0.000008984476,0.0000051023258,0.00071038253,0.0000036975703,0.00012324183],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998598,0.00002872856,0.000012211047,0.00004220409,0.000032058466,0.00002502664],"domain_scores_gemma":[0.99949276,0.00009189256,0.00016909222,0.000042996864,0.0001515178,0.000051646057],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000445068,0.00026829296,0.00021438963,0.0010588821,0.00030540684,0.0005753093,0.0002047547,0.00020814966,0.00034971774],"category_scores_gemma":[0.0006009401,0.00017583274,0.00018718388,0.001089687,0.00017525494,0.00036801436,0.00029712505,0.0001702301,0.00013284266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000147165,0.000053111584,0.979353,0.000016741493,0.00007847333,0.000058147212,0.00022630005,0.00069627224,0.015410764,0.000029224482,0.00013244427,0.0037984643],"study_design_scores_gemma":[0.000002648666,0.00002744796,0.9961176,0.000004279741,0.000020512922,0.000038190923,0.00017061293,0.0011466789,0.0021358116,0.000014483369,0.00031816834,0.0000036520923],"about_ca_topic_score_codex":0.00871978,"about_ca_topic_score_gemma":0.019669995,"teacher_disagreement_score":0.00871978,"about_ca_system_score_codex":0.00036240363,"about_ca_system_score_gemma":0.00019717017,"threshold_uncertainty_score":0.017338037},"labels":[],"label_agreement":null},{"id":"W2761305915","doi":"10.1002/2017gl074506","title":"Effect of Snow Salinity on CryoSat‐2 Arctic First‐Year Sea Ice Freeboard Measurements","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Victoria; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Polar Knowledge Canada; University of Calgary","keywords":"Freeboard; Snow; Sea ice; Sea ice thickness; Environmental science; Arctic; Radar altimeter; Geology; Arctic ice pack; Radar; Atmospheric sciences; Remote sensing; Climatology; Altimeter; Oceanography; Geomorphology","score_opus":0.04819525929819964,"score_gpt":0.3110400817572009,"score_spread":0.26284482245900126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2761305915","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99260664,0.00017141004,0.0045851064,0.000054000902,0.000059488015,0.000016961423,0.0011029876,0.00016569502,0.0012375491],"genre_scores_gemma":[0.996317,0.00010316822,0.0019102411,0.000036499874,0.000008689494,0.000009322502,0.001356358,0.000027127146,0.00023150264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995328,0.00009778834,0.000030276113,0.00012366309,0.0001658209,0.00004967004],"domain_scores_gemma":[0.99877733,0.00041029957,0.0001381949,0.00015225032,0.00046383662,0.000057982565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009343397,0.0004497234,0.00028231333,0.0005366969,0.00033362018,0.0005809745,0.00034237275,0.00029040023,0.00039573395],"category_scores_gemma":[0.0030283832,0.0001502877,0.0004530499,0.00052694645,0.00021383187,0.00046169342,0.00041084623,0.00023720157,0.0002048205],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007827055,0.00015178647,0.66157186,0.00023267833,0.00046366625,0.00041279092,0.00038293254,0.12842149,0.10818462,0.0003788802,0.0020973468,0.09691922],"study_design_scores_gemma":[0.000043032465,0.0001890154,0.78536487,0.00006740034,0.00013921884,0.00015132065,0.00020412776,0.14672858,0.06452252,0.0001230761,0.0024147902,0.00005201072],"about_ca_topic_score_codex":0.044673443,"about_ca_topic_score_gemma":0.048101336,"teacher_disagreement_score":0.044673443,"about_ca_system_score_codex":0.0006234581,"about_ca_system_score_gemma":0.00046225026,"threshold_uncertainty_score":0.088826835},"labels":[],"label_agreement":null},{"id":"W2761889840","doi":"10.1002/2017gl074042","title":"Permeability Evolution in Variably Glassy Basaltic Andesites Measured Under Magmatic Conditions","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Andesites; Outgassing; Geology; Volcano; Overpressure; Permeability (electromagnetism); Basalt; Volcanic glass; Petrology; Electrical conduit; Geochemistry; Mineralogy; Volcanic rock; Andesite","score_opus":0.04815682655144893,"score_gpt":0.29902550266081585,"score_spread":0.2508686761093669,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2761889840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99940896,0.00004759755,0.00008521535,0.0000048491843,8.004928e-7,0.0000023971734,0.00013803379,0.0000062767826,0.00030588586],"genre_scores_gemma":[0.9995407,0.000025825535,0.00013125349,0.0000041595363,0.0000011178873,0.000003976805,0.00013633282,0.0000035557807,0.00015308647],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.0000075704434,0.000008398406,0.000025983836,0.000018224222,0.000018080109],"domain_scores_gemma":[0.9998012,0.000025394718,0.000076672906,0.000013326574,0.0000420565,0.000041407435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010879115,0.00015233588,0.00018339543,0.00048351733,0.00026723428,0.00048824603,0.00018067166,0.00029322968,0.00076667697],"category_scores_gemma":[0.00027133798,0.00019660828,0.00013563935,0.00027317784,0.00038199316,0.00033145113,0.00027598155,0.00034122166,0.00016308468],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022886856,0.000026151061,0.049935304,0.00002444293,0.000023794992,0.000108354376,0.0002853541,0.0001840544,0.94806015,0.000049991086,0.000018461635,0.0010549868],"study_design_scores_gemma":[0.000009799423,0.00017148744,0.8205835,0.0000059895533,0.000032177253,0.00031314362,0.00052165246,0.0013558518,0.17644697,0.00006407743,0.00048217046,0.00001313884],"about_ca_topic_score_codex":0.0032729357,"about_ca_topic_score_gemma":0.0032567699,"teacher_disagreement_score":0.0032729357,"about_ca_system_score_codex":0.0002490197,"about_ca_system_score_gemma":0.00011057701,"threshold_uncertainty_score":0.006507814},"labels":[],"label_agreement":null},{"id":"W2762334003","doi":"10.1002/2017gl075207","title":"Depth of Origin of the Peak (Inner) Ring in Lunar Impact Basins","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Curtin University of Technology","keywords":"Geology; Impact crater; Crust; Mantle (geology); Structural basin; Geophysics; Impact structure; Geomorphology; Astrobiology; Physics","score_opus":0.06203088366244907,"score_gpt":0.3573157789615898,"score_spread":0.2952848952991407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762334003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989975,0.000025983074,0.00022217604,0.000013863666,4.5861512e-7,0.000001399931,0.000075996664,0.000014340953,0.00064824044],"genre_scores_gemma":[0.9998123,0.000011571688,0.00008279941,0.0000010692223,2.6187854e-7,9.739466e-7,0.000034335128,0.0000029109942,0.000053799577],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995804,0.000005105047,0.0000020663329,0.000012954189,0.0000071370414,0.000014717005],"domain_scores_gemma":[0.99977845,0.000090630994,0.000044894783,0.000020863365,0.000022365584,0.00004273803],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015153573,0.00012934377,0.00020617955,0.0004920888,0.00029659012,0.00054822443,0.00028965063,0.0003024277,0.0018106616],"category_scores_gemma":[0.00090927124,0.00025042397,0.00022015668,0.00030747004,0.00033817894,0.0003617683,0.000576509,0.00021622446,0.00009697678],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045625115,0.00011770851,0.44307312,0.00010314955,0.00011960263,0.0005298123,0.00061291666,0.50378543,0.03409969,0.0040656384,0.0003861516,0.012650475],"study_design_scores_gemma":[0.00006630212,0.00013907075,0.5286622,0.000031112126,0.00006136993,0.00020465639,0.0004887864,0.4583775,0.009158712,0.0017873326,0.0009684765,0.000054526],"about_ca_topic_score_codex":0.007922876,"about_ca_topic_score_gemma":0.0050909324,"teacher_disagreement_score":0.007922876,"about_ca_system_score_codex":0.0005743026,"about_ca_system_score_gemma":0.00024780302,"threshold_uncertainty_score":0.015753567},"labels":[],"label_agreement":null},{"id":"W2762881444","doi":"10.1002/2017gl075678","title":"Differential Radiative Heating Drives Tropical Atmospheric Circulation Weakening","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Forcing (mathematics); Climatology; Radiative forcing; Radiative transfer; Atmospheric sciences; Walker circulation; Environmental science; Atmospheric circulation; Circulation (fluid dynamics); General Circulation Model; GCM transcription factors; Atmosphere (unit); Climate change; Physics; Meteorology; Geology; Mechanics; Sea surface temperature; Aerosol","score_opus":0.04326013256784874,"score_gpt":0.3219912363793997,"score_spread":0.278731103811551,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2762881444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99882716,0.000027457501,0.00058187405,0.00004275771,0.000007081598,0.000002915026,0.000047332673,0.000040537085,0.00042288358],"genre_scores_gemma":[0.999846,0.00001019899,0.000086390755,0.0000072717608,0.0000017110165,0.0000010693522,0.000016286163,0.0000024706212,0.00002868975],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991846,0.000016272794,0.000005378577,0.000023136998,0.000011494064,0.000025351426],"domain_scores_gemma":[0.99973506,0.000074036674,0.000063378764,0.000052534167,0.000024405996,0.000050488285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017935241,0.00021935692,0.00029019406,0.0001341272,0.00022237904,0.00042429368,0.00023604263,0.00022086587,0.00122079],"category_scores_gemma":[0.0007870166,0.00022631868,0.00024831697,0.0001208562,0.0004212541,0.00029551162,0.00050587807,0.0003262093,0.00009252625],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006081085,0.00021857547,0.07556713,0.00013572436,0.00017632512,0.00036037774,0.00013924461,0.12801528,0.7852803,0.0017461623,0.0005625436,0.007190292],"study_design_scores_gemma":[0.0003092983,0.00036217587,0.32595822,0.000011036478,0.00012810032,0.00015296112,0.00015544356,0.5889062,0.08050746,0.0026272913,0.0008366612,0.000045141674],"about_ca_topic_score_codex":0.0032736498,"about_ca_topic_score_gemma":0.0019247989,"teacher_disagreement_score":0.0032736498,"about_ca_system_score_codex":0.0003485348,"about_ca_system_score_gemma":0.00020409141,"threshold_uncertainty_score":0.006509185},"labels":[],"label_agreement":null},{"id":"W2763270683","doi":"10.1002/2017gl075069","title":"Turbulent Entrainment Into Volcanic Plumes: New Constraints From Laboratory Experiments on Buoyant Jets Rising in a Stratified Crossflow","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Plume; Turbulence; Buoyancy; Entrainment (biomusicology); Mechanics; Volcano; Atmospheric sciences; Stratification (seeds); Geology; Neutral buoyancy; Meteorology; Environmental science; Physics; Seismology","score_opus":0.07174433765655935,"score_gpt":0.33913032744455573,"score_spread":0.2673859897879964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763270683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99854976,0.00002997795,0.0011501322,0.00001691833,0.0000030967667,0.0000052133323,0.000046517802,0.000014181392,0.0001841816],"genre_scores_gemma":[0.9995028,0.000025815198,0.00036102603,0.0000048851916,0.00000228145,0.0000057173024,0.000053638425,0.0000029442278,0.000041005227],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99987805,0.00003306546,0.000012424358,0.000024606423,0.000027980492,0.000023891433],"domain_scores_gemma":[0.99913484,0.0004961905,0.0001308346,0.00010261914,0.00006820111,0.000067376146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044885118,0.00031973416,0.00025865147,0.00016442421,0.0003225641,0.00055719906,0.00034038682,0.0002512498,0.00046734404],"category_scores_gemma":[0.0013064475,0.00015697847,0.00026883784,0.00012478002,0.0006705093,0.000382166,0.0004804385,0.0005380233,0.000047351634],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00093130494,0.000986604,0.037752222,0.00012192006,0.00008233639,0.00025088477,0.0003361385,0.1553372,0.79539835,0.0021447528,0.00028886975,0.006369403],"study_design_scores_gemma":[0.00017756179,0.0021082344,0.03309068,0.000019623161,0.00007089867,0.000063181564,0.00016485236,0.7392848,0.22358178,0.0010519259,0.00032715814,0.000059250768],"about_ca_topic_score_codex":0.003588204,"about_ca_topic_score_gemma":0.0020189716,"teacher_disagreement_score":0.003588204,"about_ca_system_score_codex":0.00034550903,"about_ca_system_score_gemma":0.00023886352,"threshold_uncertainty_score":0.0071346164},"labels":[],"label_agreement":null},{"id":"W2763330049","doi":"10.1002/2017gl075122","title":"A Near‐Global Atmospheric Distribution of N<sub>2</sub>O Isotopologues","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Canadian Space Agency; University of Pittsburgh","keywords":"Isotopologue; Stratosphere; Atmospheric sciences; Isotopomers; Atmosphere (unit); Environmental science; Atmospheric chemistry; Northern Hemisphere; Atmosphere of Earth; Latitude; Isotope; Physics; Ozone; Meteorology; Spectral line; Nuclear physics; Astronomy","score_opus":0.02625446809549148,"score_gpt":0.29255840442346115,"score_spread":0.26630393632796967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763330049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99748033,0.00015786092,0.00016574177,0.000056222616,0.0000034782188,0.0000014603578,0.00058565254,0.000018231238,0.0015310865],"genre_scores_gemma":[0.9988049,0.00011297655,0.00014725102,0.000014934759,0.0000058971896,0.000001603046,0.00068108767,0.000004388065,0.0002267835],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997675,0.0000022579604,7.5147693e-7,0.00001160694,0.0000037296595,0.000005020701],"domain_scores_gemma":[0.9999478,0.000006488351,0.000015014391,0.000005120573,0.0000143102,0.000011226732],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007150992,0.00013030886,0.00009147943,0.0003133896,0.00013433698,0.00018069286,0.00006731681,0.00017528402,0.0009282716],"category_scores_gemma":[0.00007683459,0.000079877645,0.0001426772,0.0003431467,0.000093541945,0.00024750244,0.00016334676,0.00010801659,0.00015234126],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037213674,0.00004752673,0.7695284,0.000067432025,0.00020496892,0.00018845775,0.00024557783,0.0043250336,0.1943763,0.00074554264,0.0009917393,0.02890687],"study_design_scores_gemma":[0.0000032833389,0.00002073077,0.9964988,0.0000025175987,0.000018160883,0.000021331898,0.0000392454,0.000973056,0.0012624608,0.000089373956,0.0010677302,0.0000033656406],"about_ca_topic_score_codex":0.00900299,"about_ca_topic_score_gemma":0.010403011,"teacher_disagreement_score":0.00900299,"about_ca_system_score_codex":0.00018413241,"about_ca_system_score_gemma":0.00008847799,"threshold_uncertainty_score":0.017901182},"labels":[],"label_agreement":null},{"id":"W2763596080","doi":"10.1002/2017gl074956","title":"The Magnetospheric Source Region of the Bright Proton Aurora","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Space Agency; University of Calgary","keywords":"Physics; Substorm; Plasma sheet; Proton; Magnetosphere; Field line; Pitch angle; Luminosity; Dipole; Curvature; Astrophysics; Plasma; Geophysics; Magnetosheath; Computational physics; Magnetopause; Nuclear physics; Geometry","score_opus":0.01875904757624638,"score_gpt":0.28457919786348385,"score_spread":0.2658201502872375,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763596080","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99747354,0.000100476274,0.00097125105,0.000020683123,0.0000013234136,0.00000367698,0.00025019146,0.00003865185,0.0011402438],"genre_scores_gemma":[0.9994754,0.00002856115,0.00020065473,0.0000025845961,0.000005073813,0.0000016540373,0.00019336901,0.0000031730408,0.00008946226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999541,0.0000059616004,0.0000025380477,0.000012123368,0.000012165156,0.000013161048],"domain_scores_gemma":[0.9995222,0.0001352601,0.00016944265,0.00003293899,0.00007783706,0.00006237104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015125611,0.00008489325,0.00013505688,0.0007053774,0.00029902562,0.00044521416,0.00012280894,0.00009009524,0.0010737993],"category_scores_gemma":[0.00043985178,0.00008604019,0.00010943343,0.00044595875,0.00019011453,0.00017430002,0.00035609084,0.000077713325,0.000187178],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018113482,0.000020974798,0.8935216,0.00005386833,0.000065000415,0.00044945773,0.00039662802,0.0013096473,0.0864071,0.001176657,0.00042652388,0.015991384],"study_design_scores_gemma":[0.000005406414,0.000034325447,0.9924314,0.0000037358889,0.000013256338,0.0002750813,0.00011971177,0.0016822873,0.004562155,0.00025707556,0.00061088207,0.000004535315],"about_ca_topic_score_codex":0.0019325543,"about_ca_topic_score_gemma":0.001988233,"teacher_disagreement_score":0.0019325543,"about_ca_system_score_codex":0.00022691893,"about_ca_system_score_gemma":0.00013849713,"threshold_uncertainty_score":0.0038426518},"labels":[],"label_agreement":null},{"id":"W2763841608","doi":"10.1002/2017gl075671","title":"Organic Condensation and Particle Growth to CCN Sizes in the Summertime Marine Arctic Is Driven by Materials More Semivolatile Than at Continental Sites","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; University of British Columbia; Environment and Climate Change Canada; University of Toronto","funders":"Environment and Climate Change Canada; Natural Sciences and Engineering Research Council of Canada; Government of Canada; ArcticNet","keywords":"Aerosol; Cloud condensation nuclei; Nucleation; Arctic; Atmospheric sciences; Isoprene; Condensation; Particle (ecology); Environmental science; Middle latitudes; Particle number; Sea spray; Sulfate; Oceanography; Chemistry; Meteorology; Geology; Physics; Thermodynamics","score_opus":0.022823350665293837,"score_gpt":0.27221324296436655,"score_spread":0.2493898922990727,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2763841608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999549,0.000027555649,0.000052330444,0.000005956503,0.0000011501564,0.0000010547908,0.00007512127,0.0000040323093,0.00028367486],"genre_scores_gemma":[0.99971384,0.000028041497,0.000057752808,0.0000024188237,0.0000015389164,0.0000010854696,0.00010483245,0.00000179979,0.00008867004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.0000034921604,0.0000016114379,0.000012111446,0.000008183932,0.000013504042],"domain_scores_gemma":[0.999918,0.000016779528,0.000019343923,0.000004127244,0.00001930117,0.000022446062],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012807753,0.00019258966,0.00009647473,0.00031839544,0.0003524561,0.0003752475,0.00009389021,0.00012474076,0.00048346294],"category_scores_gemma":[0.00016400614,0.00013357608,0.00019585183,0.00015931245,0.00016062528,0.00014718385,0.00016212401,0.00010921117,0.00007158613],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030719078,0.00006397086,0.855129,0.00003449633,0.000088179244,0.0001862849,0.00025061544,0.0038162991,0.13362513,0.00028330387,0.00022405476,0.005991415],"study_design_scores_gemma":[0.000004249998,0.000027980093,0.987678,0.0000020580671,0.000012816207,0.000028761435,0.00013804343,0.005406792,0.006397711,0.00003689306,0.00026361996,0.0000031551447],"about_ca_topic_score_codex":0.07680812,"about_ca_topic_score_gemma":0.0843186,"teacher_disagreement_score":0.07680812,"about_ca_system_score_codex":0.00074646634,"about_ca_system_score_gemma":0.00029746827,"threshold_uncertainty_score":0.15272212},"labels":[],"label_agreement":null},{"id":"W2765581898","doi":"10.1002/2017gl075016","title":"Attribution of Observed Streamflow Changes in Key British Columbia Drainage Basins","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Pacific Institute for Climate Solutions; University of Victoria; Western University","funders":"","keywords":"Streamflow; Forcing (mathematics); Environmental science; Coupled model intercomparison project; Climatology; Drainage basin; Climate change; Structural basin; Hydrology (agriculture); Climate model; Geology; Geography; Oceanography","score_opus":0.05335731443799018,"score_gpt":0.2936384000386297,"score_spread":0.2402810856006395,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765581898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982132,0.000023574108,0.00013544889,0.00003428224,0.0000020016582,0.0000057946963,0.0007879424,0.000025615042,0.0007721814],"genre_scores_gemma":[0.99887735,0.0000203903,0.00013211308,0.000008854757,8.545437e-7,0.0000046862506,0.000710669,0.0000038885332,0.00024108008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997377,0.000034909892,0.000016279088,0.00007843467,0.00007572439,0.000057010875],"domain_scores_gemma":[0.99886286,0.00019965986,0.00020185106,0.000104948995,0.00045211392,0.00017857569],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040458812,0.00013893719,0.00014088363,0.0009503791,0.00071405695,0.000985372,0.00041707276,0.00021923793,0.0006972496],"category_scores_gemma":[0.001860049,0.00013624846,0.000098959754,0.0013563405,0.00047156462,0.0001643634,0.0004539341,0.00024876127,0.00007212423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008701269,0.000031425312,0.97504085,0.000019377954,0.000044415337,0.0000761501,0.00032356588,0.0061091715,0.0028922968,0.0002362779,0.00082673127,0.014312638],"study_design_scores_gemma":[0.000005478727,0.000004933816,0.9901882,0.0000045388074,0.0000057927796,0.000011628159,0.0001716867,0.00851752,0.0004137527,0.00005621415,0.0006133631,0.000006935834],"about_ca_topic_score_codex":0.8466387,"about_ca_topic_score_gemma":0.8974653,"teacher_disagreement_score":0.15336132,"about_ca_system_score_codex":0.0062684673,"about_ca_system_score_gemma":0.003469167,"threshold_uncertainty_score":0.30852896},"labels":[],"label_agreement":null},{"id":"W2765713703","doi":"10.1002/2017gl074375","title":"Revising Estimates of Aquatic Gross Oxygen Production by the Triple Oxygen Isotope Method to Incorporate the Local Isotopic Composition of Water","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; National Defense Science and Engineering Graduate; National Science Foundation","keywords":"Seawater; Composition (language); Oxygen; Isotopes of oxygen; Salinity; Oxygen-18; Stable isotope ratio; Isotope; Chemistry; Environmental science; Analytical Chemistry (journal); Environmental chemistry; Geology; Oceanography; Physics; Nuclear chemistry","score_opus":0.03725298045160309,"score_gpt":0.30653260348790656,"score_spread":0.2692796230363035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2765713703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6910865,0.0010723694,0.30400974,0.00025677093,0.00011517122,0.000048455408,0.0006956061,0.00046068223,0.002254653],"genre_scores_gemma":[0.8760093,0.0004170033,0.12252961,0.00005630118,0.000025045429,0.000046219306,0.00036884035,0.000102396894,0.0004452963],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99961567,0.00007474888,0.000027298634,0.00009290874,0.00017198367,0.000017421313],"domain_scores_gemma":[0.99922514,0.00024028066,0.00013163706,0.00013637819,0.00022873293,0.000037841182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012022824,0.0004337731,0.0003866927,0.0008055684,0.0003538963,0.0005754642,0.00074960425,0.0004237856,0.00021534514],"category_scores_gemma":[0.0031184456,0.000392313,0.00035426844,0.0005209998,0.00031457678,0.0010076794,0.00067713455,0.0006099613,0.00016274555],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017932804,0.00012184506,0.316081,0.00029197353,0.00048413308,0.00020112749,0.0003375661,0.14873211,0.26320258,0.004260142,0.0013515003,0.26475668],"study_design_scores_gemma":[0.000027839715,0.00015128464,0.15002619,0.00006103481,0.00011025196,0.000115981005,0.00014903267,0.73464805,0.10461213,0.0043398454,0.005665567,0.000092820206],"about_ca_topic_score_codex":0.011531307,"about_ca_topic_score_gemma":0.020495767,"teacher_disagreement_score":0.011531307,"about_ca_system_score_codex":0.00065821235,"about_ca_system_score_gemma":0.0006966727,"threshold_uncertainty_score":0.022928357},"labels":[],"label_agreement":null},{"id":"W2766056458","doi":"10.1002/2017gl075452","title":"Joint Modulation of Intraseasonal Rainfall in Tropical Australia by the Madden‐Julian Oscillation and El Niño‐Southern Oscillation","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Monash University","keywords":"Madden–Julian oscillation; Climatology; El Niño Southern Oscillation; Precipitation; Wet season; Environmental science; Dry season; Southern oscillation; Oscillation (cell signaling); Atmospheric sciences; Geography; Geology; Convection; Meteorology","score_opus":0.06898112626664303,"score_gpt":0.33262943395902284,"score_spread":0.2636483076923798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766056458","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994437,0.000030986124,0.000064394226,0.000030718027,0.0000017932581,0.0000016367151,0.000044181557,0.000003634381,0.00037900463],"genre_scores_gemma":[0.9998018,0.000020274754,0.00003061773,0.000005124398,0.0000019776578,0.0000013807462,0.00003595824,9.68687e-7,0.00010173618],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999149,0.000024870387,0.0000059514937,0.000015637104,0.000017076352,0.000021607026],"domain_scores_gemma":[0.99972624,0.00006277324,0.000092778224,0.000015464808,0.000057864723,0.00004490674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020796855,0.00011618615,0.00014571175,0.00022488995,0.00016756804,0.00034963453,0.00010974023,0.000111823894,0.0007160382],"category_scores_gemma":[0.00075718074,0.00012901782,0.0001263238,0.0002964259,0.00016471687,0.00020687665,0.0004662519,0.00015025775,0.000077170684],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019395535,0.0000858536,0.9679405,0.000029469316,0.00015706249,0.00019008096,0.00050373044,0.0040702075,0.015096545,0.00032225283,0.0003701039,0.011040224],"study_design_scores_gemma":[0.0000029463642,0.000011855463,0.9971794,0.0000017383335,0.000008170667,0.000011673575,0.000071819464,0.002444574,0.000117985874,0.000034185254,0.00011424715,0.0000014771783],"about_ca_topic_score_codex":0.012619363,"about_ca_topic_score_gemma":0.019345207,"teacher_disagreement_score":0.012619363,"about_ca_system_score_codex":0.00026887452,"about_ca_system_score_gemma":0.0002188451,"threshold_uncertainty_score":0.025091827},"labels":[],"label_agreement":null},{"id":"W2766099597","doi":"10.1002/2017gl075157","title":"Oxygen Minimum Zone Contrasts Between the Arabian Sea and the Bay of Bengal Implied by Differences in Remineralization Depth","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"York University; New York University Abu Dhabi","keywords":"Oxygen minimum zone; Bay; Denitrification; Oceanography; Oxygen; Environmental science; Water column; BENGAL; Geology; Atmospheric sciences; Nitrogen; Chemistry","score_opus":0.03165013955325713,"score_gpt":0.26854546005847746,"score_spread":0.23689532050522033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766099597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984445,0.00003444567,0.00016313905,0.00009350864,0.0000049427354,0.0000029724436,0.00012885623,0.000013836859,0.0011137989],"genre_scores_gemma":[0.9997639,0.0000152351495,0.000047451675,0.0000071247014,0.0000012659488,0.0000018763079,0.000047505597,0.0000025974937,0.000112999856],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998977,0.000023422352,0.00000712747,0.000022109172,0.000008669941,0.000040901505],"domain_scores_gemma":[0.9997149,0.00011182411,0.00004731514,0.000025599737,0.00003565327,0.00006469002],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021938347,0.00044886593,0.00036692695,0.0003618121,0.0004201741,0.001159164,0.000795758,0.00090009364,0.001477051],"category_scores_gemma":[0.0011166453,0.000294361,0.0006255371,0.00037948115,0.0006005922,0.0005723578,0.00071406853,0.00036626993,0.00011159242],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006104431,0.00013780505,0.110728025,0.00009347986,0.00016682142,0.0005447185,0.0001890219,0.8670064,0.015020165,0.0027727152,0.00047089765,0.0022593678],"study_design_scores_gemma":[0.00026891162,0.00014917966,0.07148368,0.000015854208,0.00007679126,0.00006539047,0.00040239806,0.9233619,0.002756561,0.000884693,0.00048799135,0.000046670422],"about_ca_topic_score_codex":0.09733871,"about_ca_topic_score_gemma":0.032699663,"teacher_disagreement_score":0.09733871,"about_ca_system_score_codex":0.0016885551,"about_ca_system_score_gemma":0.0007338235,"threshold_uncertainty_score":0.19354427},"labels":[],"label_agreement":null},{"id":"W2766628814","doi":"10.1002/2017gl076020","title":"Determining Coastal Mean Dynamic Topography by Geodetic Methods","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada","keywords":"Geoid; Geodetic datum; Geodesy; Remote sensing; Geology; Global Positioning System; Tide gauge; Altimeter; Satellite; Interferometric synthetic aperture radar; Synthetic aperture radar; Ocean surface topography; Sea level; Computer science; Geophysics; Oceanography; Aerospace engineering","score_opus":0.06550396360906702,"score_gpt":0.3709828818693205,"score_spread":0.3054789182602535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766628814","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15937375,0.0004818628,0.8283378,0.00022814017,0.00007205409,0.000059229,0.0014611689,0.0016349067,0.008351163],"genre_scores_gemma":[0.62319624,0.00020221886,0.37357357,0.000055983575,0.000033777313,0.000047501588,0.0012829961,0.000077249155,0.0015304161],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99979514,0.000049497496,0.0000125620645,0.000066896835,0.000062007915,0.000013980356],"domain_scores_gemma":[0.99967587,0.000060196548,0.000057335852,0.000057705252,0.0001309439,0.000018002924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031657994,0.0003103157,0.0001722477,0.0016663412,0.00025243353,0.0007215023,0.00039096692,0.0002442726,0.0014422595],"category_scores_gemma":[0.001113775,0.00018628384,0.00021931696,0.0015219351,0.00022939754,0.00040971977,0.00038803948,0.00025578833,0.00075287954],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010018211,0.00007732862,0.089150034,0.00012578504,0.00012066305,0.00010250183,0.0001256492,0.18401033,0.028988069,0.012352349,0.0050517516,0.6797954],"study_design_scores_gemma":[0.000027060523,0.00003976994,0.03694815,0.000030970677,0.000017261138,0.00009623946,0.000110808236,0.9453352,0.006026151,0.004162504,0.0071730097,0.000032807657],"about_ca_topic_score_codex":0.007015047,"about_ca_topic_score_gemma":0.014526039,"teacher_disagreement_score":0.007015047,"about_ca_system_score_codex":0.00034128237,"about_ca_system_score_gemma":0.0007188143,"threshold_uncertainty_score":0.013948441},"labels":[],"label_agreement":null},{"id":"W2766816162","doi":"10.1002/2017gl075342","title":"Seismic Interferometry Using Persistent Noise Sources for Temporal Subsurface Monitoring","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Seismic interferometry; Microseism; Ambient noise level; Geology; Noise (video); Seismology; Seismic noise; Interferometry; Block (permutation group theory); Acoustics; Remote sensing; Computer science; Optics; Geomorphology; Sound (geography)","score_opus":0.10103895802608022,"score_gpt":0.3398445795556639,"score_spread":0.23880562152958368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766816162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6821882,0.00034209157,0.31251702,0.00017995009,0.00003369175,0.000042536743,0.0004986739,0.0009264786,0.0032713846],"genre_scores_gemma":[0.896157,0.000112307454,0.10312706,0.000018280281,0.000023272542,0.000022180973,0.00018197478,0.000034044493,0.00032380765],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999187,0.00002006814,0.0000033772812,0.000017940583,0.000032239044,0.000007753858],"domain_scores_gemma":[0.99971324,0.000100569916,0.00006552922,0.000043480562,0.00006092171,0.000016239599],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022809266,0.00028145735,0.00017274113,0.0009914794,0.00013256718,0.0003191546,0.00024411664,0.00024023435,0.00053981115],"category_scores_gemma":[0.0007090836,0.00013603763,0.0001253337,0.0009111202,0.00020909312,0.00041996106,0.0003834917,0.00027942559,0.000107699605],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061351317,0.00019861558,0.059417423,0.00012749445,0.00012929192,0.00035560623,0.00021193088,0.081250936,0.4452722,0.005260867,0.0015299736,0.40563214],"study_design_scores_gemma":[0.00004926989,0.00018554158,0.065683305,0.000016880444,0.00006748424,0.00025960695,0.00007760717,0.8851573,0.04310562,0.003405343,0.0019525853,0.000039434748],"about_ca_topic_score_codex":0.0016553018,"about_ca_topic_score_gemma":0.0043572057,"teacher_disagreement_score":0.0016553018,"about_ca_system_score_codex":0.00019192642,"about_ca_system_score_gemma":0.00022596013,"threshold_uncertainty_score":0.0032913089},"labels":[],"label_agreement":null},{"id":"W2766985662","doi":"10.1002/2017gl075049","title":"Constraints on Inner Core Anisotropy Using Array Observations of P′P′","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Sleep Foundation; National Science Foundation","keywords":"Anisotropy; Inner core; Core (optical fiber); Geology; Polar; Rotation (mathematics); Geodesy; Sampling (signal processing); Geophysics; Phase (matter); Latitude; Physics; Computational physics; Geometry; Optics; Mathematics; Astronomy","score_opus":0.1509275144354192,"score_gpt":0.3458538752737842,"score_spread":0.19492636083836498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2766985662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947685,0.000030415054,0.0023281856,0.000018638062,0.0000024596693,0.0000027646738,0.0006006233,0.00004745817,0.002200943],"genre_scores_gemma":[0.99867475,0.000015162128,0.0007921585,0.0000056695,0.0000025851546,0.0000026790094,0.00040799362,0.000009618701,0.00008944551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.000014259485,0.0000057636557,0.00003193177,0.000017943114,0.000027757807],"domain_scores_gemma":[0.99930096,0.00021487052,0.00013436934,0.000110880246,0.0001597111,0.00007913129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024201607,0.00020490373,0.00016449322,0.0005832023,0.00022055778,0.00050759205,0.000214314,0.00015689092,0.0010682752],"category_scores_gemma":[0.0015308748,0.00021685171,0.000137756,0.00047213788,0.00020661761,0.00045115643,0.00036591623,0.00022871987,0.0002944536],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024220906,0.00002999276,0.9013267,0.000033408705,0.000046480724,0.00013922087,0.00031408397,0.0031294124,0.07564567,0.00071396976,0.00050286244,0.017876],"study_design_scores_gemma":[0.000007808,0.000020182788,0.98311263,0.000007726047,0.000016213213,0.00013244827,0.0001157654,0.009863406,0.005444577,0.0003264751,0.0009435481,0.000009244259],"about_ca_topic_score_codex":0.009196657,"about_ca_topic_score_gemma":0.017567284,"teacher_disagreement_score":0.009196657,"about_ca_system_score_codex":0.00020040097,"about_ca_system_score_gemma":0.0002068297,"threshold_uncertainty_score":0.018286288},"labels":[],"label_agreement":null},{"id":"W2767293332","doi":"10.1002/2017gl075981","title":"Nitrogen Availability Dampens the Positive Impacts of CO<sub>2</sub> Fertilization on Terrestrial Ecosystem Carbon and Water Cycles","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Space Agency","keywords":"Environmental science; Evapotranspiration; Water-use efficiency; Primary production; Ecosystem; Photosynthesis; Terrestrial ecosystem; Carbon cycle; Carbon sink; Atmospheric sciences; Water cycle; Stomatal conductance; Agronomy; FluxNet; Ecology; Eddy covariance; Botany; Biology","score_opus":0.01995987752241036,"score_gpt":0.2726683282918206,"score_spread":0.25270845076941023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767293332","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972248,0.00020700981,0.00064091693,0.00012276089,0.000027082297,0.0000040350865,0.00015066937,0.000052418505,0.0015702458],"genre_scores_gemma":[0.99965477,0.00003418851,0.000083744555,0.000041131196,0.0000030951894,0.0000013079936,0.000042114512,0.000005820508,0.00013387334],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999194,0.000013005728,0.000007997343,0.000029298853,0.000009424683,0.00002092609],"domain_scores_gemma":[0.9997305,0.00009589269,0.00006441234,0.000020837688,0.000028250153,0.00006016437],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002700164,0.0003675118,0.0002935872,0.00014184364,0.00020569672,0.0004988451,0.00025534607,0.000350529,0.0019594417],"category_scores_gemma":[0.0005826192,0.00023755281,0.00029016056,0.000096038646,0.0003138414,0.00044537336,0.00038836274,0.00021128538,0.00016272182],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0026812572,0.00037353364,0.24694854,0.0005741907,0.0007207799,0.00076252973,0.000099823934,0.17732334,0.5457682,0.001999943,0.002194437,0.02055337],"study_design_scores_gemma":[0.0001409845,0.0005122098,0.7014592,0.00003850422,0.00030705662,0.00013314832,0.00018188289,0.25835067,0.034214176,0.0018791909,0.0027357352,0.000047206013],"about_ca_topic_score_codex":0.012378093,"about_ca_topic_score_gemma":0.017027518,"teacher_disagreement_score":0.012378093,"about_ca_system_score_codex":0.00055137236,"about_ca_system_score_gemma":0.0004021462,"threshold_uncertainty_score":0.02461207},"labels":[],"label_agreement":null},{"id":"W2767348160","doi":"10.1002/2017gl074825","title":"Decomposition of the Mean Barotropic Transport in a High‐Resolution Model of the North Atlantic Ocean","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Natural Sciences and Engineering Research Council of Canada; Leibniz-Institut für Meereswissenschaften; Marine Environmental Observation Prediction and Response Network","keywords":"Barotropic fluid; Baroclinity; Advection; Eddy; Geology; Mean flow; Gulf Stream; Vorticity; Flux (metallurgy); Current meter; Climatology; Ocean current; Potential vorticity; Continental shelf; Momentum (technical analysis); Oceanography; Turbulence; Mechanics; Physics; Vortex","score_opus":0.023783893585393845,"score_gpt":0.2579573533287709,"score_spread":0.23417345974337705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767348160","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9459948,0.00013905473,0.0483879,0.00072849594,0.000051442792,0.00002568716,0.00054760644,0.00045053856,0.0036744666],"genre_scores_gemma":[0.98980206,0.0000775813,0.008406551,0.000058212423,0.000026688624,0.000033079454,0.00028181777,0.00007210025,0.0012419568],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990857,0.000029081819,0.0000067277083,0.000019130379,0.000021221047,0.000015325642],"domain_scores_gemma":[0.9997757,0.00007359856,0.000036265315,0.00003368598,0.000045202996,0.000035622295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004233475,0.00043994965,0.0004776933,0.00028620093,0.00059265294,0.0011270323,0.00068042043,0.000976716,0.0009850379],"category_scores_gemma":[0.0011466853,0.0006512043,0.00083119195,0.00026623992,0.00052234106,0.00074754836,0.00055201567,0.0008999406,0.00014964736],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033006538,0.000029081426,0.002827716,0.0000080990285,0.0000356398,0.00003444075,0.000019422278,0.9917108,0.0027673037,0.0011592734,0.0001691464,0.0012061759],"study_design_scores_gemma":[0.000007317462,0.000005243692,0.00046566213,7.343233e-7,0.000003485824,0.0000018432843,0.0000027633528,0.99919814,0.000085725515,0.00018896187,0.00003732918,0.0000028424],"about_ca_topic_score_codex":0.06990306,"about_ca_topic_score_gemma":0.032000884,"teacher_disagreement_score":0.06990306,"about_ca_system_score_codex":0.0014599875,"about_ca_system_score_gemma":0.0016288412,"threshold_uncertainty_score":0.13899237},"labels":[],"label_agreement":null},{"id":"W2767447169","doi":"10.1002/2017gl075135","title":"Snow Accumulation Variability Over the West Antarctic Ice Sheet Since 1900: A Comparison of Ice Core Records With ERA‐20C Reanalysis","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Natural Environment Research Council; Sight Research UK; Multiple Sclerosis Scientific Research Foundation","keywords":"Firn; Snow; Ice core; Antarctic ice sheet; Climatology; Ice sheet; Precipitation; Geology; Peninsula; Physical geography; Sea ice; Snow field; Cryosphere; Oceanography; Geography; Snow cover; Meteorology; Geomorphology","score_opus":0.1032255059084522,"score_gpt":0.36061914261917094,"score_spread":0.25739363671071874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2767447169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99672,0.00013686912,0.00009052477,0.000014322675,0.000006942235,0.0000030379354,0.0025413495,0.000012508696,0.00047458717],"genre_scores_gemma":[0.9925626,0.00018462248,0.00020915859,0.000013730481,0.000013026752,0.0000072361595,0.0068388125,0.0000061215896,0.00016471182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998815,0.000018698413,0.00001735086,0.00003224295,0.000029991834,0.00002014096],"domain_scores_gemma":[0.99951375,0.00006066462,0.00014394807,0.000053953914,0.00018453074,0.000043109445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005172631,0.00023567202,0.00015996226,0.0013822155,0.0001382036,0.00044274912,0.00015102956,0.00013914204,0.00039158293],"category_scores_gemma":[0.000744529,0.00009655665,0.0002667898,0.0015742021,0.000108982305,0.00035209523,0.0002525101,0.000112951726,0.00020818102],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089415415,0.000025222194,0.98981607,0.000024812272,0.00014326816,0.00004657513,0.00014488884,0.0008308273,0.0012257824,0.000035271405,0.0004887038,0.007129118],"study_design_scores_gemma":[0.0000015838069,0.000011671406,0.9988576,0.000004141685,0.000014624349,0.000020230045,0.00003644674,0.00044039474,0.00017355545,0.000004477691,0.00043364186,0.000001614515],"about_ca_topic_score_codex":0.023709996,"about_ca_topic_score_gemma":0.031226596,"teacher_disagreement_score":0.023709996,"about_ca_system_score_codex":0.00035254617,"about_ca_system_score_gemma":0.00023753653,"threshold_uncertainty_score":0.047143936},"labels":[],"label_agreement":null},{"id":"W2768532429","doi":"10.1002/2017gl075483","title":"A Census of Atmospheric Variability From Seconds to Decades","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Core Research for Evolutional Science and Technology; NOAA Pacific Marine Environmental Laboratory; Australian Research Council; Japan Society for the Promotion of Science; Horizon 2020 Framework Programme; Israel Science Foundation; European Commission; National Science Foundation; Royal Society; Japan Science and Technology Agency; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Met Office; Department for Environment, Food and Rural Affairs, UK Government; Climate Extremes","keywords":"Stratosphere; Climatology; Environmental science; Troposphere; Atmosphere (unit); Hydrosphere; North Atlantic oscillation; Teleconnection; Atmospheric sciences; Meteorology; Geology; Geography; El Niño Southern Oscillation; Biosphere; Physics","score_opus":0.05343296874701619,"score_gpt":0.34139125572646223,"score_spread":0.28795828697944603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768532429","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.53104764,0.13803554,0.05552168,0.01669023,0.0054096123,0.00018443153,0.08908573,0.0016681493,0.16235705],"genre_scores_gemma":[0.9158328,0.043252975,0.0072905496,0.0011118058,0.0026258673,0.00011650398,0.022137783,0.00032982914,0.0073018842],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99952066,0.00007789494,0.0000586316,0.00009637684,0.00020811145,0.000038353024],"domain_scores_gemma":[0.99745804,0.00094229955,0.0003434592,0.0003536607,0.0007687221,0.00013393108],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006749536,0.00018812038,0.00022285682,0.0031175013,0.00036268582,0.0014681177,0.00020208569,0.00020663436,0.0038405438],"category_scores_gemma":[0.0039423048,0.00014024161,0.00032267976,0.006049328,0.0004168174,0.0021155744,0.00073280145,0.0009094831,0.0005627764],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005150112,0.00006221704,0.15868366,0.001630054,0.000319657,0.0003680361,0.0026258696,0.008310409,0.006919818,0.124377966,0.11422286,0.58196443],"study_design_scores_gemma":[0.000016891567,0.0001258645,0.3778337,0.0005191208,0.000061711056,0.0005580744,0.0012499719,0.0044448343,0.0011056198,0.032021917,0.5819808,0.00008150102],"about_ca_topic_score_codex":0.0070739933,"about_ca_topic_score_gemma":0.0051023373,"teacher_disagreement_score":0.0070739933,"about_ca_system_score_codex":0.00044682427,"about_ca_system_score_gemma":0.000549574,"threshold_uncertainty_score":0.014065623},"labels":[],"label_agreement":null},{"id":"W2768885536","doi":"10.1002/2017gl075488","title":"Using Multitemporal and Multispectral Airborne Lidar to Assess Depth of Peat Loss and Correspondence With a New Active Normalized Burn Ratio for Wildfires","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; Optech (Canada); University of Lethbridge","funders":"","keywords":"Lidar; Peat; Multispectral image; Environmental science; Remote sensing; Wetland; Geology; Hydrology (agriculture); Geography","score_opus":0.0651339966233212,"score_gpt":0.359090212450458,"score_spread":0.2939562158271368,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2768885536","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903464,0.000032899166,0.0005020444,0.000006650166,9.790417e-7,0.0000033974213,0.000078252255,0.000013160688,0.0003280003],"genre_scores_gemma":[0.99841464,0.000015687405,0.001338783,0.0000047857984,7.384889e-7,0.0000020627933,0.00011103586,0.0000016747281,0.000110649176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987197,0.000020546002,0.0000072252546,0.00002111266,0.00005502167,0.000024040673],"domain_scores_gemma":[0.99961495,0.00006630747,0.00007985006,0.000028136496,0.00015679783,0.000053925476],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045093952,0.000153747,0.00011802089,0.0010880423,0.00020933768,0.0004642677,0.0002641517,0.00019186072,0.0003972417],"category_scores_gemma":[0.0006545806,0.000115353236,0.00009318333,0.00064435805,0.00017070261,0.00033964906,0.00019418889,0.00012512185,0.000081100625],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017717577,0.00005533824,0.96204144,0.000016147944,0.000031697233,0.000036579237,0.00020864327,0.002001775,0.016562484,0.00006666637,0.00010122029,0.01870087],"study_design_scores_gemma":[0.0000040350446,0.000029708366,0.98931724,0.000005040142,0.000008236603,0.000054633292,0.00042343588,0.008438312,0.0015432553,0.00003978787,0.0001300749,0.0000062496297],"about_ca_topic_score_codex":0.102273166,"about_ca_topic_score_gemma":0.3307502,"teacher_disagreement_score":0.102273166,"about_ca_system_score_codex":0.00054506277,"about_ca_system_score_gemma":0.00044867772,"threshold_uncertainty_score":0.20335573},"labels":[],"label_agreement":null},{"id":"W2769340760","doi":"10.1002/2017gl075661","title":"Predicting the Geothermal Heat Flux in Greenland: A Machine Learning Approach","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":104,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation of Sri Lanka","keywords":"Greenland ice sheet; Geology; Glacier; Geothermal gradient; Ice core; Groenlandia; Volcano; Plume; Glaciology; Climatology; Ice stream; Flux (metallurgy); Ice sheet; Geophysics; Geomorphology; Oceanography; Paleontology; Tectonics; Volcanism; Cryosphere; Meteorology; Sea ice","score_opus":0.054817158947392086,"score_gpt":0.28888285737820113,"score_spread":0.23406569843080904,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2769340760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95993805,0.0001909128,0.03683136,0.00059594493,0.000015633834,0.000027288,0.0005809347,0.00044102006,0.001378734],"genre_scores_gemma":[0.9931705,0.000034463166,0.006080646,0.0000511446,0.000009404398,0.000014300364,0.0002989705,0.000010730188,0.00033000426],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988854,0.000037618556,0.0000052536543,0.000037876813,0.0000096561325,0.00002101516],"domain_scores_gemma":[0.99952555,0.0003089387,0.000044483208,0.00003248216,0.000057174246,0.000031450018],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00059624866,0.00065079203,0.0004725676,0.0007748861,0.000359844,0.0006454561,0.0006276302,0.0007488414,0.0007057956],"category_scores_gemma":[0.0010557763,0.00029816988,0.00048361756,0.0006098839,0.0006227363,0.00046485045,0.00042746597,0.00053041877,0.00014234796],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000019233412,0.000024871351,0.00585167,0.00000333829,0.000022815182,0.000019602996,0.000006082282,0.9893534,0.00023267181,0.00011243026,0.00013593401,0.004217987],"study_design_scores_gemma":[0.0000022165998,0.000002529279,0.0008356774,8.1505283e-7,0.0000016140077,9.432209e-7,0.0000027629053,0.99887437,0.000069166825,0.0001906122,0.000018232551,0.0000010445065],"about_ca_topic_score_codex":0.087118216,"about_ca_topic_score_gemma":0.057289686,"teacher_disagreement_score":0.087118216,"about_ca_system_score_codex":0.0018749402,"about_ca_system_score_gemma":0.0010280233,"threshold_uncertainty_score":0.17322224},"labels":[],"label_agreement":null},{"id":"W2769821060","doi":"10.1002/2017gl074678","title":"The Solar Flux Dependence of Ionospheric 150 km Radar Echoes and Implications","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Ionosphere; Flux (metallurgy); Radar; Physics; Extreme ultraviolet lithography; Amplitude; Geophysics; Plasma; Atmospheric sciences; Computational physics; Daytime; Astrophysics; Optics; Materials science","score_opus":0.01923563422917307,"score_gpt":0.3037353844420915,"score_spread":0.28449975021291846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2769821060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980422,0.00015109012,0.0005160328,0.000033000277,0.000004070145,0.0000019261151,0.000077116085,0.000010407545,0.0011641646],"genre_scores_gemma":[0.9998061,0.000032426426,0.000056566503,0.000005626046,0.0000026842758,6.420799e-7,0.000041463234,0.000002215923,0.000052299198],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999356,0.000012589041,0.000004086237,0.000022257,0.000012728839,0.00001268722],"domain_scores_gemma":[0.99932957,0.00037183557,0.00014370293,0.000052263906,0.00006809896,0.00003453066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022137396,0.000114646915,0.00012607867,0.00037136435,0.00010820639,0.00031570948,0.00013078576,0.00027938857,0.0008697494],"category_scores_gemma":[0.0012590591,0.000078394514,0.000115291325,0.00025146955,0.0002034613,0.00029081528,0.00017178436,0.0001462616,0.00009953478],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006363721,0.000110815396,0.64223796,0.00011114297,0.00013572312,0.0006888048,0.00031922277,0.008828439,0.31851882,0.000993134,0.0003423095,0.027077142],"study_design_scores_gemma":[0.000004518878,0.000047326484,0.98512137,0.000004811082,0.000016637337,0.0001941224,0.000098409764,0.0046431343,0.009302085,0.00026854323,0.0002880551,0.000011004089],"about_ca_topic_score_codex":0.0007229917,"about_ca_topic_score_gemma":0.00044545764,"teacher_disagreement_score":0.0008697494,"about_ca_system_score_codex":0.00011197829,"about_ca_system_score_gemma":0.000037767066,"threshold_uncertainty_score":0.0029096007},"labels":[],"label_agreement":null},{"id":"W2772047527","doi":"10.1002/2017gl076028","title":"Hot Plasma Effects on the Cyclotron‐Resonant Pitch‐Angle Scattering Rates of Radiation Belt Electrons Due to EMIC Waves","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Seventh Framework Programme; National Natural Science Foundation of China; Deutsche Forschungsgemeinschaft","keywords":"Pitch angle; Physics; Dispersion relation; Electron; Scattering; Atomic physics; Emic and etic; Cyclotron; Van Allen radiation belt; Plasma; Computational physics; Optics; Nuclear physics; Geophysics; Magnetosphere","score_opus":0.015196937480174954,"score_gpt":0.29313729242937137,"score_spread":0.2779403549491964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2772047527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9880882,0.00020011445,0.008054168,0.000026276077,0.0000089298355,0.0000074843547,0.000051887546,0.00006643927,0.0034964192],"genre_scores_gemma":[0.9993789,0.00006148216,0.0002895317,0.000003556626,0.000001895202,0.000002526313,0.000027112626,0.000011038586,0.00022385972],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998996,0.000027500302,0.0000041649564,0.000012876257,0.000028653556,0.000027209817],"domain_scores_gemma":[0.99971193,0.00016412408,0.000040669613,0.000026777041,0.00003957979,0.000016924152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002764002,0.00048281497,0.00022341871,0.00026364674,0.00018191767,0.0003186238,0.000305021,0.00023704398,0.0008094527],"category_scores_gemma":[0.000787571,0.00017859644,0.0003533941,0.0002450228,0.0002667735,0.00033760266,0.00037035462,0.00023889472,0.0000945466],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005716125,0.000055678833,0.029800814,0.00018067317,0.00014547391,0.00073122093,0.00029222923,0.84076715,0.111041985,0.0049188533,0.000265621,0.011228743],"study_design_scores_gemma":[0.00006513593,0.00014530722,0.023817714,0.000013299068,0.0000549727,0.00011833903,0.00014322984,0.92725724,0.047061414,0.0007558523,0.00054145756,0.000026009497],"about_ca_topic_score_codex":0.002792172,"about_ca_topic_score_gemma":0.0010701077,"teacher_disagreement_score":0.002792172,"about_ca_system_score_codex":0.00024943365,"about_ca_system_score_gemma":0.00012704037,"threshold_uncertainty_score":0.0055518746},"labels":[],"label_agreement":null},{"id":"W2775080550","doi":"10.1002/2017gl075373","title":"High‐Frequency Observations of Temperature and Dissolved Oxygen Reveal Under‐Ice Convection in a Large Lake","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of the Environment, Conservation and Parks; The Scarborough Hospital; General Electric (Canada); University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Convection; Atmospheric sciences; Oxygen; Supersaturation; Geology; Climatology; Convective mixing; Environmental science; Meteorology; Chemistry; Geography","score_opus":0.03407416414501567,"score_gpt":0.2833973746476922,"score_spread":0.24932321050267653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2775080550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997234,0.000010882604,0.00006303816,0.000007738722,6.001237e-7,0.0000014118848,0.00005870112,0.000005981367,0.00012823523],"genre_scores_gemma":[0.9996848,0.0000073002216,0.00013848585,0.000003954496,0.0000018380823,0.0000027296032,0.00007007621,0.0000017169548,0.00008915264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996185,0.0000022687257,0.000002446818,0.000010820338,0.0000080969585,0.000014483204],"domain_scores_gemma":[0.99991786,0.000009021824,0.000021022912,0.000004279871,0.000011898205,0.000035884234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000089427245,0.00014076465,0.00017447861,0.00037003652,0.00060213346,0.00038084836,0.00014297261,0.00022261898,0.00054936553],"category_scores_gemma":[0.00012219987,0.00017921191,0.00011495409,0.0003048934,0.00026764147,0.00036001852,0.00041249185,0.00015482491,0.00011369898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044607458,0.0001263979,0.62942225,0.00004795045,0.00006772856,0.00045016504,0.0013844152,0.0011666692,0.36043552,0.00010941248,0.00028335737,0.0060600797],"study_design_scores_gemma":[0.000009300608,0.00006399886,0.9920264,0.0000022950608,0.000015020983,0.00007558202,0.00026621498,0.0026658068,0.0045902114,0.00003071753,0.00024675208,0.000007621263],"about_ca_topic_score_codex":0.008259703,"about_ca_topic_score_gemma":0.01522173,"teacher_disagreement_score":0.008259703,"about_ca_system_score_codex":0.00034552222,"about_ca_system_score_gemma":0.00028770426,"threshold_uncertainty_score":0.016423285},"labels":[],"label_agreement":null},{"id":"W2776406487","doi":"10.1002/2017gl075974","title":"Disturbance Impacts on Thermal Hot Spots and Hot Moments at the Peatland‐Atmosphere Interface","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Waterloo; University of Alberta","funders":"Natural Environment Research Council; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Sight Research UK","keywords":"Environmental science; Biogeochemical cycle; Ecosystem; Atmospheric sciences; Peat; Vegetation (pathology); Atmosphere (unit); Soil science; Ecology; Geology; Meteorology; Geography","score_opus":0.024585492198232934,"score_gpt":0.30777488225665334,"score_spread":0.2831893900584204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2776406487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996544,0.000018435678,0.00009350489,0.0000034524678,7.3029696e-7,5.901645e-7,0.00003154823,0.0000042522206,0.00019318685],"genre_scores_gemma":[0.9999176,0.0000052881705,0.000023315219,0.0000016970102,4.649165e-7,7.197198e-7,0.000019492545,9.856071e-7,0.000030391644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999356,0.00000881373,0.0000042581614,0.000017176846,0.0000094471525,0.000024669851],"domain_scores_gemma":[0.99973804,0.000058269718,0.00009230495,0.000022292961,0.000025875532,0.00006312861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013038407,0.000104067454,0.00021871598,0.0003074718,0.00025969572,0.00044086002,0.00009345724,0.00014537659,0.00084437354],"category_scores_gemma":[0.00032356603,0.00008446254,0.00013520739,0.00015217996,0.0003891436,0.00023592451,0.00045455352,0.00017179894,0.000065067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009839406,0.000113365895,0.69385296,0.000066363405,0.00013211893,0.0003507094,0.0004517547,0.0055819945,0.28547835,0.00041187493,0.00022899186,0.012347613],"study_design_scores_gemma":[0.0000018440084,0.000029293886,0.99644214,0.0000020321618,0.000007345673,0.00004178266,0.00015967042,0.0011454964,0.001983185,0.00008199666,0.00010187399,0.0000032838318],"about_ca_topic_score_codex":0.0032730398,"about_ca_topic_score_gemma":0.007906955,"teacher_disagreement_score":0.0032730398,"about_ca_system_score_codex":0.00028054084,"about_ca_system_score_gemma":0.00011245897,"threshold_uncertainty_score":0.0065079927},"labels":[],"label_agreement":null},{"id":"W2777722773","doi":"10.1002/2017gl075751","title":"Which Triggers Produce the Most Erosive, Frequent, and Longest Runout Turbidity Currents on Deltas?","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; University of Southampton; Sight Research UK; University of New Brunswick","keywords":"Turbidity current; Subaerial; Geology; Settling; Submarine landslide; Submarine pipeline; Sediment; River delta; Delta; Geomorphology; Turbidity; Landslide; Sediment transport; Oceanography; Sedimentation; Hydrology (agriculture); Geochemistry; Environmental science; Geotechnical engineering; Structural basin; Sedimentary depositional environment","score_opus":0.07308159894556876,"score_gpt":0.3261306636198278,"score_spread":0.253049064674259,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2777722773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990089,0.00012888259,0.000097217424,0.000025029607,0.0000024780798,0.0000044970634,0.00014636939,0.000007465276,0.00057918625],"genre_scores_gemma":[0.99944836,0.000088632536,0.00008648208,0.000010929455,0.0000026915832,0.0000019212337,0.00009217925,0.0000022811168,0.00026635284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987566,0.000012000856,0.000007817855,0.000031738407,0.000021329566,0.000051422176],"domain_scores_gemma":[0.9995722,0.00003274451,0.00016940977,0.00002273122,0.00011957299,0.00008336363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020883829,0.00011911941,0.00021916542,0.00053904834,0.00042049965,0.0007600467,0.0001594071,0.00019908971,0.0010013689],"category_scores_gemma":[0.000547865,0.00014027959,0.00013361199,0.00039496645,0.00034375835,0.00022704141,0.00028001895,0.00012685928,0.00018790185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054224005,0.000010421011,0.98331696,0.000023782835,0.000030370184,0.0001426989,0.00034896733,0.00020026897,0.008593196,0.00006725863,0.00024139501,0.006970493],"study_design_scores_gemma":[7.709903e-7,0.00000655423,0.99899167,0.0000035797543,0.0000071925597,0.00003400269,0.00033405892,0.000092434086,0.00031191923,0.000019797366,0.00019642113,0.0000016653041],"about_ca_topic_score_codex":0.057722095,"about_ca_topic_score_gemma":0.13655199,"teacher_disagreement_score":0.057722095,"about_ca_system_score_codex":0.0006402303,"about_ca_system_score_gemma":0.0004947605,"threshold_uncertainty_score":0.1147722},"labels":[],"label_agreement":null},{"id":"W2780917047","doi":"10.1002/2017gl075765","title":"Spreading Speed of Magnetopause Reconnection X‐Lines Using Ground‐Satellite Coordination","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Air Force Office of Scientific Research; National Aeronautics and Space Administration; National Science Foundation","keywords":"Magnetopause; Geophysics; Physics; Magnetic reconnection; Spacecraft; Field line; Field (mathematics); Current (fluid); Computational physics; Magnetic field; Magnetosphere; Geology; Astronomy","score_opus":0.04787790662841466,"score_gpt":0.3359875786765856,"score_spread":0.2881096720481709,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2780917047","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99838734,0.000025884056,0.0006560549,0.000015766045,0.0000015000821,0.0000021330309,0.00010207988,0.000025843381,0.0007834155],"genre_scores_gemma":[0.9996792,0.0000073996075,0.00018516123,5.7724486e-7,5.5717186e-7,8.0472523e-7,0.00007608813,0.0000024029973,0.000047783316],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999143,0.000021854246,0.0000047775843,0.000025161951,0.00001978217,0.000014190591],"domain_scores_gemma":[0.99881196,0.000567194,0.00030448605,0.00011067168,0.00014357126,0.00006209173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035259858,0.00015804362,0.00009921979,0.0006327233,0.00013751622,0.0004369717,0.00019631138,0.00014254244,0.00090301863],"category_scores_gemma":[0.002220786,0.00010365486,0.00013798146,0.00047898485,0.00017035074,0.00038247893,0.0001983515,0.00016615598,0.00007306487],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003419256,0.000042074556,0.46583688,0.00003666733,0.000106640415,0.00017634139,0.0001843263,0.50379527,0.0067853723,0.0034411754,0.0006668565,0.018586496],"study_design_scores_gemma":[0.000030571788,0.00008070987,0.19383833,0.000009859038,0.000028848857,0.00009122734,0.00012208849,0.79987764,0.0046161655,0.00087968697,0.00040365136,0.000021220045],"about_ca_topic_score_codex":0.0066758688,"about_ca_topic_score_gemma":0.003696841,"teacher_disagreement_score":0.0066758688,"about_ca_system_score_codex":0.00038325615,"about_ca_system_score_gemma":0.00012308716,"threshold_uncertainty_score":0.013274014},"labels":[],"label_agreement":null},{"id":"W2782554811","doi":"10.1002/2017gl075910","title":"Simulated Impact of Glacial Runoff on CO<sub>2</sub> Uptake in the Gulf of Alaska","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Tula Foundation","funders":"Integrated Ocean Observing System; NOAA Pacific Marine Environmental Laboratory; Hakai Institute; University of Washington; Joint Institute for the Study of the Atmosphere and Ocean; National Oceanic and Atmospheric Administration; National Research Council Sri Lanka","keywords":"Alkalinity; Glacial period; Tidewater; Surface runoff; Meltwater; Environmental science; Biogeochemical cycle; Sink (geography); Climate change; Hydrology (agriculture); Oceanography; Carbon cycle; Ecosystem; Geology; Glacier; Ecology; Geography; Geomorphology","score_opus":0.027326080354492188,"score_gpt":0.32195607276910604,"score_spread":0.29462999241461385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782554811","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983181,0.0000224041,0.00024031587,0.000055986406,0.000007570717,0.0000042468764,0.00026892396,0.0000510876,0.001031386],"genre_scores_gemma":[0.9995192,0.000013750526,0.00012987554,0.000010155046,0.0000012018604,0.000004500867,0.00014440865,0.000004355103,0.00017253347],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999312,0.000019101826,0.000004879429,0.000016640583,0.000009968683,0.000018091576],"domain_scores_gemma":[0.99981576,0.0000782785,0.000021645285,0.000012601224,0.00003193555,0.000039770446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021661118,0.0004714747,0.00032319853,0.0002672246,0.0004687242,0.0006039031,0.00044466575,0.0010175267,0.0019232844],"category_scores_gemma":[0.00055580726,0.00026988436,0.00055895816,0.0003499927,0.00046328138,0.0003765957,0.00042881136,0.00043792868,0.00012381712],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018202867,0.000084351326,0.026436968,0.000019292373,0.000052458712,0.00013856505,0.000031587042,0.9691796,0.0023768959,0.0002944434,0.00023098328,0.00097280287],"study_design_scores_gemma":[0.0001237868,0.00017736324,0.02159624,0.000009090507,0.00005014639,0.000023048331,0.00010855416,0.97514504,0.0020756647,0.00029765844,0.00036661024,0.000026772967],"about_ca_topic_score_codex":0.07580149,"about_ca_topic_score_gemma":0.033782274,"teacher_disagreement_score":0.07580149,"about_ca_system_score_codex":0.0014716492,"about_ca_system_score_gemma":0.00088210154,"threshold_uncertainty_score":0.15072054},"labels":[],"label_agreement":null},{"id":"W2782821898","doi":"10.1002/2017gl076015","title":"Tracking the Subsurface Signal of Decadal Climate Warming to Quantify Vertical Groundwater Flow Rates","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Groundwater; Hydrogeology; Groundwater flow; Inflection point; Borehole; Environmental science; Geology; Global warming; Hydrology (agriculture); Inversion (geology); Climate change; Soil science; Aquifer; Geomorphology; Geotechnical engineering; Oceanography","score_opus":0.062374218985762474,"score_gpt":0.32998422577327585,"score_spread":0.2676100067875134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2782821898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99515426,0.00006189143,0.0031814952,0.000022030365,0.000006523078,0.0000059480144,0.0007737373,0.00006415774,0.00073004904],"genre_scores_gemma":[0.9979849,0.000023226341,0.0015356807,0.0000059557133,0.000002300621,0.000004809717,0.00036009584,0.0000057907423,0.00007729513],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999392,0.000011308506,0.000004275364,0.000020803971,0.000011396004,0.000012901499],"domain_scores_gemma":[0.9997911,0.00004141021,0.00006227291,0.000024544333,0.00005690246,0.00002387553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003017077,0.00012411182,0.00013132312,0.00070059794,0.00011258385,0.00030636223,0.0001284382,0.0001988958,0.00054402446],"category_scores_gemma":[0.00050003646,0.000101573154,0.00010424414,0.0008183479,0.00009783558,0.0002971406,0.00029238325,0.00023946165,0.00010809738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024914579,0.00009482335,0.8327063,0.000058289024,0.00008886371,0.00007164409,0.0003189808,0.013650709,0.11629064,0.00056853495,0.0004417501,0.035460476],"study_design_scores_gemma":[0.000008841504,0.00007266475,0.9624801,0.000007564299,0.00002107954,0.00003833321,0.00016360565,0.02608354,0.009776219,0.0003101337,0.0010252745,0.000012593026],"about_ca_topic_score_codex":0.005697241,"about_ca_topic_score_gemma":0.010633882,"teacher_disagreement_score":0.005697241,"about_ca_system_score_codex":0.00018812451,"about_ca_system_score_gemma":0.00013917839,"threshold_uncertainty_score":0.011328161},"labels":[],"label_agreement":null},{"id":"W2783981603","doi":"10.1002/2017gl076883","title":"What Has Controlled the Poleward Migration of Annual Averaged Location of Tropical Cyclone Lifetime Maximum Intensity Over the Western North Pacific Since 1961?","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"National Key Research and Development Program of China; China Meteorological Administration; National Natural Science Foundation of China; G. Unger Vetlesen Foundation; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Latitude; Tropical cyclone; Climatology; Environmental science; Atmospheric sciences; Geology; Geodesy","score_opus":0.02508205002936188,"score_gpt":0.26771357475843344,"score_spread":0.24263152472907157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2783981603","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938623,0.0022468858,0.0001789153,0.0004799467,0.000059969654,0.0000051248967,0.00035914994,0.000007958076,0.0027998327],"genre_scores_gemma":[0.9988249,0.00055087556,0.000034363035,0.000040971318,0.000044544835,0.0000014045778,0.000110108835,0.0000024768437,0.00039043187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984694,0.000022527585,0.000012983359,0.00006794332,0.000012401893,0.00003721514],"domain_scores_gemma":[0.999044,0.00015332125,0.00042749767,0.00005466681,0.00016388371,0.00015655113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049941556,0.00013840366,0.00019024184,0.00045397654,0.0004185259,0.0008004939,0.00016645362,0.00025945986,0.0020773613],"category_scores_gemma":[0.0011310201,0.000112858594,0.00017734747,0.0006452657,0.0005094424,0.0005090813,0.00023809136,0.00028779916,0.0001981789],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014081565,0.000027928114,0.9823172,0.000085178166,0.00011224929,0.00013531848,0.00045058687,0.0003314454,0.0024075413,0.00050863833,0.00056650705,0.012916409],"study_design_scores_gemma":[0.0000013051744,0.000010680655,0.99882144,0.000008777109,0.000014068714,0.000022526767,0.00018155908,0.000077690485,0.000068731504,0.000030969462,0.0007597758,0.0000024554588],"about_ca_topic_score_codex":0.028627379,"about_ca_topic_score_gemma":0.055519827,"teacher_disagreement_score":0.028627379,"about_ca_system_score_codex":0.0005561599,"about_ca_system_score_gemma":0.00045446536,"threshold_uncertainty_score":0.056921482},"labels":[],"label_agreement":null},{"id":"W2784252378","doi":"10.1002/2017gl076333","title":"Causes of Glacier Melt Extremes in the Alps Since 1949","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Institut national des sciences de l'Univers; Center for Neuroscience and Regenerative Medicine; Agence Nationale de la Recherche","keywords":"Glacier; Latent heat; Climatology; Snow; Energy balance; Environmental science; Sensible heat; Heat wave; Glacier mass balance; Term (time); Atmospheric sciences; Geology; Climate change; Meteorology; Geography","score_opus":0.07918354527363504,"score_gpt":0.31835465822238473,"score_spread":0.2391711129487497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2784252378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99856514,0.00023034564,0.000099481986,0.00011728653,0.0000047082285,0.0000014251074,0.00036450147,0.000019016443,0.0005980666],"genre_scores_gemma":[0.99968266,0.000046307552,0.000020418576,0.000006816465,0.000007853241,7.766661e-7,0.00019860422,0.0000020923878,0.000034488356],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986625,0.00002057571,0.00001167397,0.000043842007,0.000022783792,0.000034825658],"domain_scores_gemma":[0.99961925,0.000067498804,0.00017707936,0.000025454052,0.000049075577,0.00006162022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037373952,0.00015117507,0.00022497168,0.0011445105,0.0005183287,0.0008172086,0.00019821878,0.0003086619,0.0011682977],"category_scores_gemma":[0.00074307696,0.00009456969,0.00033042702,0.0009119865,0.000467897,0.00024019586,0.0005165445,0.00031633102,0.000107804415],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000143832,0.000022034497,0.984937,0.000027752978,0.00009747765,0.0002728866,0.00021060776,0.004595041,0.0025394224,0.0005233782,0.0004600039,0.0061705788],"study_design_scores_gemma":[0.000009162316,0.000021324873,0.9913051,0.000009534627,0.000021798809,0.00015691611,0.00018928706,0.006199158,0.00039595758,0.00046405598,0.0012191823,0.0000085066295],"about_ca_topic_score_codex":0.008235104,"about_ca_topic_score_gemma":0.009254918,"teacher_disagreement_score":0.008235104,"about_ca_system_score_codex":0.00059223955,"about_ca_system_score_gemma":0.00017111377,"threshold_uncertainty_score":0.01637435},"labels":[],"label_agreement":null},{"id":"W2784456439","doi":"10.1002/2016gl071805","title":"Amplified North Atlantic warming in the late Pliocene by changes in Arctic gateways","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Department of Energy; Office of Science; National Science Foundation","keywords":"Arctic dipole anomaly; Arctic; Oceanography; Archipelago; Geology; Climatology; Arctic sea ice decline; Arctic geoengineering; Arctic ecology; Thermohaline circulation; Arctic ice pack; Drift ice","score_opus":0.042326289025826455,"score_gpt":0.2829232117867136,"score_spread":0.24059692276088712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2784456439","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981579,0.000044799363,0.00015645182,0.00011687265,0.0000057066045,0.000002439492,0.0001622316,0.000022665357,0.0013309093],"genre_scores_gemma":[0.99965477,0.000033223307,0.00006002262,0.000013044663,0.0000024493559,0.0000023379764,0.00011173574,0.0000063424304,0.00011611489],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999237,0.000012721866,0.000004979679,0.000031176438,0.000008985847,0.000018399924],"domain_scores_gemma":[0.9997596,0.00003651787,0.00007803678,0.000030080695,0.00003925672,0.000056550278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037235784,0.00026740503,0.00028223096,0.0005047291,0.00053801795,0.0010299918,0.00030387047,0.0005301683,0.0028511987],"category_scores_gemma":[0.0012670567,0.0003074387,0.00037171572,0.0006387195,0.0008154103,0.00061055884,0.001175008,0.0004703859,0.00023507733],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064585067,0.000050425966,0.94669247,0.000060680246,0.00016011513,0.0005698449,0.0011143108,0.011544633,0.02524091,0.0021072514,0.0006205701,0.011192933],"study_design_scores_gemma":[0.000038091133,0.0000415357,0.99282336,0.000017548988,0.00003455787,0.0000684599,0.00044729072,0.00407171,0.0006312044,0.0005852207,0.0012317506,0.000009288059],"about_ca_topic_score_codex":0.024924586,"about_ca_topic_score_gemma":0.033263803,"teacher_disagreement_score":0.024924586,"about_ca_system_score_codex":0.0008631706,"about_ca_system_score_gemma":0.0005215801,"threshold_uncertainty_score":0.049558997},"labels":[],"label_agreement":null},{"id":"W2786092450","doi":"10.1002/2017gl076763","title":"Stratospheric Smoke With Unprecedentedly High Backscatter Observed by Lidars Above Southern France","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":180,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Institut national des sciences de l'Univers; Langley Research Center; Centre National d’Etudes Spatiales","keywords":"Lidar; Aerosol; Environmental science; Volcano; Plume; Smoke; Stratosphere; Backscatter (email); Atmospheric sciences; Climatology; Southern Hemisphere; Geology; Remote sensing; Meteorology; Geography; Seismology","score_opus":0.019659329184655502,"score_gpt":0.2610072908726081,"score_spread":0.24134796168795258,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786092450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99849343,0.000054303757,0.00023786887,0.00004237635,0.000003471884,0.0000032837768,0.00017281546,0.00005401575,0.0009383913],"genre_scores_gemma":[0.99946815,0.000020500329,0.00016743908,0.000011186322,0.0000044420176,0.0000023887435,0.00015203774,0.0000026609835,0.00017129949],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990046,0.000009420928,0.0000025029053,0.000022860184,0.00003305356,0.000031770505],"domain_scores_gemma":[0.999897,0.000017330885,0.000019508208,0.000008099152,0.00003573759,0.00002230212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001536683,0.00027020517,0.00018349392,0.0008672655,0.00044804558,0.00062825356,0.00022779948,0.0004007102,0.0006512291],"category_scores_gemma":[0.00015640845,0.00011318774,0.00016996734,0.00042266137,0.00021450841,0.00027342094,0.00029823612,0.00022756653,0.00014320017],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013756048,0.0001197848,0.85222125,0.00003222652,0.000107863656,0.001399369,0.0015810864,0.004003595,0.114054225,0.00035161097,0.00077886647,0.025212616],"study_design_scores_gemma":[0.000008996418,0.0000390983,0.98971516,0.0000075297166,0.000015218252,0.00020239847,0.0005803034,0.004777934,0.0030175378,0.000051604784,0.0015712656,0.000012834389],"about_ca_topic_score_codex":0.05664148,"about_ca_topic_score_gemma":0.06271569,"teacher_disagreement_score":0.05664148,"about_ca_system_score_codex":0.0005003876,"about_ca_system_score_gemma":0.00034833598,"threshold_uncertainty_score":0.11262357},"labels":[],"label_agreement":null},{"id":"W2786707315","doi":"10.1002/2017gl074830","title":"Decline in Antarctic Ozone Depletion and Lower Stratospheric Chlorine Determined From Aura Microwave Limb Sounder Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Microwave Limb Sounder; Ozone depletion; Ozone layer; Aura; Environmental science; Stratosphere; Atmospheric sciences; Chlorine; Microwave; Meteorology; Geology; Geography; Chemistry; Physics","score_opus":0.047625243557829294,"score_gpt":0.28499673225352523,"score_spread":0.23737148869569594,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2786707315","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998317,0.000027886765,0.000079813944,0.000028053424,0.0000019075562,0.0000040928953,0.0008202565,0.000010060559,0.00071098364],"genre_scores_gemma":[0.99880636,0.000022074575,0.000076214725,0.00001750324,0.0000019080583,0.000003090599,0.000876328,0.0000017519047,0.00019478041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.0000075385956,0.000003692572,0.000012814341,0.000015383544,0.000017269747],"domain_scores_gemma":[0.9997683,0.000024153398,0.00009513388,0.00001502761,0.000062873536,0.00003441649],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002483011,0.00010605918,0.00008724388,0.00045196543,0.00019202965,0.00036128252,0.0001297269,0.00017826722,0.000621344],"category_scores_gemma":[0.00058855186,0.000065965905,0.00014119456,0.0005048066,0.00016781251,0.00018635757,0.00020395953,0.00019309309,0.00009217962],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011777751,0.000016008968,0.98877084,0.0000086326,0.000032135726,0.000034250606,0.00008211217,0.0008138697,0.0076368325,0.00004102757,0.0002966576,0.0021498306],"study_design_scores_gemma":[0.0000017426653,0.000012324388,0.9982248,0.0000014386296,0.000004673106,0.0000070650344,0.000039529954,0.0005598129,0.00092535716,0.0000058551923,0.00021597913,0.0000014162649],"about_ca_topic_score_codex":0.14806306,"about_ca_topic_score_gemma":0.13587229,"teacher_disagreement_score":0.14806306,"about_ca_system_score_codex":0.0006368142,"about_ca_system_score_gemma":0.0004468654,"threshold_uncertainty_score":0.29440248},"labels":[],"label_agreement":null},{"id":"W2789283244","doi":"10.1002/2017gl075860","title":"Compiling and Mapping Global Permeability of the Unconsolidated and Consolidated Earth: GLobal HYdrogeology MaPS 2.0 (GLHYMPS 2.0)","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":194,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; Ocean Networks Canada Society; University of Victoria","funders":"","keywords":"Geology; Hydrogeology; Permeability (electromagnetism); Groundwater; Soil science; Hydrology (agriculture); Geotechnical engineering","score_opus":0.027305588909790447,"score_gpt":0.28819167724182787,"score_spread":0.2608860883320374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789283244","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.75046355,0.00023748427,0.05378066,0.00031608558,0.00006983716,0.00020987034,0.16953266,0.015789233,0.00960056],"genre_scores_gemma":[0.7238973,0.00027427357,0.098562844,0.000061497136,0.000047369092,0.00027963138,0.17243679,0.0021633776,0.002276901],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998324,0.000020486688,0.0000139507765,0.00004972299,0.000057911777,0.000025442878],"domain_scores_gemma":[0.99942005,0.0000783023,0.00012591318,0.00012336059,0.00017803237,0.00007432925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048614948,0.0006149568,0.00023091676,0.0032072954,0.00017716747,0.0006482855,0.00031925197,0.0002625678,0.001572341],"category_scores_gemma":[0.0011015644,0.0003419474,0.00036019544,0.0029309094,0.00019113273,0.00081445393,0.00086063944,0.00035971846,0.0007326004],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006261511,0.00031426115,0.34307164,0.0006888842,0.00056207314,0.000948323,0.0014852966,0.17739424,0.0712253,0.004793074,0.08507247,0.31381825],"study_design_scores_gemma":[0.00014478527,0.00008134484,0.70457417,0.000073208794,0.00011939336,0.00018200955,0.000515752,0.18527383,0.03380236,0.0030416155,0.0720184,0.0001731077],"about_ca_topic_score_codex":0.014079743,"about_ca_topic_score_gemma":0.016975893,"teacher_disagreement_score":0.014079743,"about_ca_system_score_codex":0.00035049775,"about_ca_system_score_gemma":0.0005916551,"threshold_uncertainty_score":0.027995586},"labels":[],"label_agreement":null},{"id":"W2789713209","doi":"10.1002/2018gl076995","title":"Numerical Solutions of the Mean‐Value Theorem: New Methods for Downward Continuation of Potential Fields","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Imaging and Inversion Techniques","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Chinese Academy of Geological Sciences; China Geological Survey; Natural Resources Canada; National Natural Science Foundation of China","keywords":"Continuation; Analytic continuation; Divergence (linguistics); Taylor series; Mathematics; Applied mathematics; Series (stratigraphy); Fourier transform; Stability (learning theory); Interpretation (philosophy); Mathematical analysis; Computer science; Geology","score_opus":0.05241514884754016,"score_gpt":0.35705895222286754,"score_spread":0.30464380337532737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789713209","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0073785726,0.00009813948,0.9908614,0.00010265477,0.00004552624,0.00002294149,0.0000126278655,0.00009311475,0.0013850302],"genre_scores_gemma":[0.19481441,0.0004274922,0.79831535,0.000090622605,0.00012148139,0.00021193338,0.00008099949,0.00024139123,0.005696344],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9997693,0.0000930619,0.000016032332,0.00002644288,0.000078943856,0.000016267404],"domain_scores_gemma":[0.9991972,0.00040376405,0.000079407764,0.000077338715,0.00020868992,0.000033577475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012200826,0.0007151581,0.00042284897,0.0007443449,0.0004408762,0.0006480894,0.000884132,0.00090903643,0.0019841073],"category_scores_gemma":[0.0043653883,0.00030383424,0.00071976206,0.00043373878,0.0008462798,0.0011712316,0.001173237,0.0013844616,0.00046873896],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014873313,0.0001143749,0.0017226891,0.00028303984,0.00005554092,0.00030224794,0.0004925364,0.4090316,0.06150921,0.3336122,0.003223635,0.18950422],"study_design_scores_gemma":[0.0000096540525,0.000017767275,0.000064813954,0.00001077609,0.0000034503664,0.00003225588,0.00001086959,0.98192364,0.0023569479,0.013873645,0.0016861954,0.000010026618],"about_ca_topic_score_codex":0.0010929998,"about_ca_topic_score_gemma":0.0007331689,"teacher_disagreement_score":0.0019841073,"about_ca_system_score_codex":0.00039391205,"about_ca_system_score_gemma":0.0005688426,"threshold_uncertainty_score":0.0066375136},"labels":[],"label_agreement":null},{"id":"W2789820279","doi":"10.1002/2017gl076446","title":"Collapse of the 2017 Winter Beaufort High: A Response to Thinning Sea Ice?","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Office of Naval Research; National Science Foundation of Sri Lanka; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Arctic sea ice decline; Sea ice; Arctic ice pack; Geology; Arctic dipole anomaly; Arctic geoengineering; Arctic; Oceanography; Climatology; Extratropical cyclone; Beaufort scale; Drift ice; Siberian High; Canada Basin; Geography; East Asia","score_opus":0.026539927944542366,"score_gpt":0.2914897992071857,"score_spread":0.26494987126264335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2789820279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98736703,0.00035811384,0.00018448482,0.0049144113,0.00038252797,0.000027027521,0.00026922883,0.000044407025,0.00645272],"genre_scores_gemma":[0.9972071,0.00013150998,0.00007107888,0.0005765485,0.00016696379,0.000008289016,0.00029420972,0.000008205597,0.0015360573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998159,0.000029990608,0.00001095624,0.00003020577,0.000041468542,0.00007152874],"domain_scores_gemma":[0.9990741,0.000069118476,0.0002903687,0.00003750896,0.00015541694,0.00037344932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004517841,0.00019907358,0.00023562035,0.00032607093,0.0012571537,0.0013797922,0.00036429823,0.00076831784,0.0037440346],"category_scores_gemma":[0.0017147404,0.000078111705,0.00024555437,0.0002886334,0.00060534425,0.0002971021,0.0006352905,0.0008362816,0.0004331913],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017815813,0.0006300249,0.8799545,0.00014922007,0.00020097724,0.0112870075,0.0056656566,0.0012030544,0.01447531,0.0018473126,0.0338892,0.048916053],"study_design_scores_gemma":[0.000023016813,0.00026559472,0.96920973,0.000056646175,0.000023921173,0.00077882595,0.01034324,0.0007878359,0.0011610561,0.0008044249,0.016520698,0.000025032],"about_ca_topic_score_codex":0.025093708,"about_ca_topic_score_gemma":0.05016164,"teacher_disagreement_score":0.025093708,"about_ca_system_score_codex":0.0010889184,"about_ca_system_score_gemma":0.00086566625,"threshold_uncertainty_score":0.049895287},"labels":[],"label_agreement":null},{"id":"W2790045453","doi":"10.1002/2017gl076311","title":"Low‐Fe(III) Greenalite Was a Primary Mineral From Neoarchean Oceans","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Research Council Canada; Canadian Institutes of Health Research; Agouron Institute; University of Saskatchewan","keywords":"Banded iron formation; Mineral; Geology; Biogeochemistry; Primary (astronomy); Geochemistry; Earth science; Mineralogy; Oceanography; Archean; Materials science; Metallurgy","score_opus":0.03477211188957483,"score_gpt":0.2853260062109049,"score_spread":0.2505538943213301,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790045453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975044,0.00017642468,0.00045901848,0.000048113576,0.0000049433443,0.0000026371645,0.00013870942,0.000019171395,0.001646455],"genre_scores_gemma":[0.99840325,0.00010380818,0.0005464121,0.000018548382,0.0000018192078,0.0000012119276,0.000077997975,0.000007404936,0.00083970395],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993694,0.0000025083898,0.0000033979873,0.000025783025,0.000019447078,0.000011883339],"domain_scores_gemma":[0.99990547,0.0000092931205,0.000019644325,0.000011007085,0.000041407762,0.000013212546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013632969,0.00016498094,0.00014281945,0.000619572,0.0005049615,0.000588452,0.00014564603,0.00023820033,0.00095322885],"category_scores_gemma":[0.00020417392,0.00014929617,0.00011944038,0.0004397698,0.0005499945,0.00030799463,0.00042672135,0.00021605796,0.00013068167],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028610355,0.000017951525,0.36308584,0.0001363718,0.00006611228,0.00037622164,0.0010238464,0.00038958312,0.6089592,0.0012092933,0.00019602755,0.024253383],"study_design_scores_gemma":[0.0000060132857,0.000036872218,0.9303171,0.000017879382,0.00003916771,0.00023568857,0.000860375,0.00090054213,0.06402903,0.0003539863,0.0031952804,0.000008031517],"about_ca_topic_score_codex":0.029475186,"about_ca_topic_score_gemma":0.061954614,"teacher_disagreement_score":0.029475186,"about_ca_system_score_codex":0.0008661064,"about_ca_system_score_gemma":0.00034403455,"threshold_uncertainty_score":0.05860722},"labels":[],"label_agreement":null},{"id":"W2790124446","doi":"10.1002/2017gl076907","title":"Multi‐Instrument Observations of Prolonged Stratified Wind Layers at Iqaluit, Nunavut","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Radiosonde; Lidar; Stratification (seeds); Radar; Wind profiler; Environmental science; Doppler radar; Geology; Wind speed; Meteorology; Wind shear; Prevailing winds; Wind direction; Atmospheric sciences; Remote sensing; Oceanography; Geography","score_opus":0.050121937707422785,"score_gpt":0.2903355886004192,"score_spread":0.2402136508929964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790124446","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99175936,0.00019290879,0.00027153906,0.000059414622,0.00001147355,0.000030416424,0.0020936278,0.0000671691,0.005514089],"genre_scores_gemma":[0.9956736,0.00008516689,0.0006100266,0.000027874848,0.000006980145,0.000025406829,0.0021531172,0.000011619987,0.001406209],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983203,0.000013117591,0.0000061728847,0.000047299025,0.000050062845,0.000051267798],"domain_scores_gemma":[0.9996706,0.00002301363,0.000043556734,0.000017397497,0.00018917386,0.000056185418],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030047397,0.00026029933,0.00020240252,0.00071451097,0.0009973552,0.00082613324,0.00089773315,0.00017011132,0.0009427584],"category_scores_gemma":[0.00049081387,0.00015682794,0.00009509536,0.00083009724,0.0003565411,0.00022422131,0.0006424987,0.000379123,0.00018227185],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005064267,0.00018261498,0.9353741,0.00006473803,0.00011813413,0.0005191224,0.003230778,0.0034081119,0.017335564,0.00038021756,0.0036687732,0.035211463],"study_design_scores_gemma":[0.000018920226,0.00003096648,0.99158174,0.000028307219,0.000022352488,0.000036634152,0.0013060695,0.0031215872,0.0009645718,0.00004121509,0.0028303538,0.000017351349],"about_ca_topic_score_codex":0.86738026,"about_ca_topic_score_gemma":0.93577135,"teacher_disagreement_score":0.13261974,"about_ca_system_score_codex":0.0038580217,"about_ca_system_score_gemma":0.0020399136,"threshold_uncertainty_score":0.26680148},"labels":[],"label_agreement":null},{"id":"W2790305234","doi":"10.1002/2018gl077298","title":"Evidence for Neutrals‐Foreshock Electrons Impact at Mars","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Centre National d’Etudes Spatiales","keywords":"Physics; Exosphere; Solar wind; Foreshock; Mars Exploration Program; Bow shock (aerodynamics); Electron; Flux (metallurgy); Interplanetary spaceflight; Geophysics; Computational physics; Atomic physics; Plasma; Astrobiology; Shock wave; Ion; Geology; Mechanics; Nuclear physics; Materials science","score_opus":0.11355119866970659,"score_gpt":0.3960044977014186,"score_spread":0.282453299031712,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790305234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99852693,0.00014706157,0.0000606149,0.00003014161,0.000004750543,0.0000017145983,0.00007915896,0.0000080078125,0.001141615],"genre_scores_gemma":[0.9994981,0.00007312629,0.00004627327,0.000010085458,0.000008657389,0.0000012194138,0.000092420116,0.0000017324326,0.00026831625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990654,0.000008557886,0.0000039500133,0.000017035725,0.000028890165,0.000035064313],"domain_scores_gemma":[0.9997075,0.000058758444,0.000108201086,0.00002726196,0.000048532354,0.000049741586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014969717,0.00026490656,0.00015664562,0.00075097533,0.0005946417,0.0004547169,0.00023532353,0.00047323768,0.0032804438],"category_scores_gemma":[0.00034085865,0.00013113579,0.00017927361,0.00036930045,0.0002995735,0.00029256477,0.00061055884,0.00020839354,0.0002524942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019716192,0.00008668599,0.80412966,0.00018372544,0.00016396858,0.005866707,0.0013338608,0.00041209493,0.16559874,0.0010828952,0.0006771388,0.018492898],"study_design_scores_gemma":[0.000013959266,0.00021340227,0.9829148,0.000016379223,0.000028221573,0.0014534532,0.0005394587,0.00023710854,0.012394671,0.00018596013,0.00199571,0.000006877183],"about_ca_topic_score_codex":0.0014729854,"about_ca_topic_score_gemma":0.0018194944,"teacher_disagreement_score":0.0032804438,"about_ca_system_score_codex":0.00017075014,"about_ca_system_score_gemma":0.00006136121,"threshold_uncertainty_score":0.010974109},"labels":[],"label_agreement":null},{"id":"W2790334991","doi":"10.1002/2017gl076770","title":"Historical Tropospheric and Stratospheric Ozone Radiative Forcing Using the CMIP6 Database","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Stratosphere; Ozone layer; Environmental science; Atmospheric sciences; Shortwave; Coupled model intercomparison project; Ozone; Longwave; Climatology; Forcing (mathematics); Radiative forcing; Tropospheric ozone; Quasi-biennial oscillation; Northern Hemisphere; Ozone depletion; Troposphere; Radiative transfer; Climate model; Meteorology; Aerosol; Climate change; Physics; Geology","score_opus":0.050821020089817585,"score_gpt":0.3013919853366438,"score_spread":0.2505709652468262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790334991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8734068,0.0004031255,0.002500619,0.00017056691,0.000058324313,0.000023072564,0.120458364,0.0001790445,0.0028000355],"genre_scores_gemma":[0.8888251,0.0004290267,0.0033182916,0.000059782647,0.000037012145,0.000051311887,0.10643505,0.000039765306,0.00080459967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998958,0.000014432858,0.000010783559,0.000037112648,0.000023719429,0.000018176434],"domain_scores_gemma":[0.99978536,0.00002775292,0.000050620427,0.000029503637,0.0000865147,0.000020154528],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032026134,0.00030779766,0.00013576422,0.0011348601,0.00017763975,0.0003079268,0.0002876447,0.00024013953,0.0015390554],"category_scores_gemma":[0.0007860887,0.00012619726,0.00031493508,0.001630011,0.00009138753,0.00032800337,0.0002054752,0.0002398382,0.00047434986],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018272422,0.00014187703,0.82923084,0.0003560392,0.0006024132,0.00029774883,0.00017096735,0.099274375,0.004483172,0.0018216773,0.030402936,0.033035155],"study_design_scores_gemma":[0.000025000776,0.000030769934,0.94211787,0.000041900774,0.00009060637,0.00015955995,0.000079372105,0.025179919,0.0031067966,0.0003175726,0.02882066,0.000029930628],"about_ca_topic_score_codex":0.022376368,"about_ca_topic_score_gemma":0.016772203,"teacher_disagreement_score":0.022376368,"about_ca_system_score_codex":0.0004287897,"about_ca_system_score_gemma":0.00021649945,"threshold_uncertainty_score":0.044492245},"labels":[],"label_agreement":null},{"id":"W2790590221","doi":"10.1002/2017gl076485","title":"Flow Shears at the Poleward Boundary of Omega Bands Observed During Conjunctions of Swarm and THEMIS ASI","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Saskatchewan","funders":"UC Berkeley College of Chemistry; National Sleep Foundation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Omega; Plasma sheet; Ionosphere; Geophysics; Physics; Substorm; Convection; Shear (geology); Geology; Plasma; Instability; Shear flow; Astrophysics; Magnetosphere; Mechanics","score_opus":0.021983887313923214,"score_gpt":0.27422370220787784,"score_spread":0.25223981489395464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790590221","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986696,0.0000393208,0.00014560198,0.000018530307,0.000007236683,0.000006121659,0.00026273399,0.000022404745,0.0008283766],"genre_scores_gemma":[0.9993437,0.00002746028,0.00019110375,0.000008054827,0.000015023376,0.000006139325,0.0002652469,0.0000039653805,0.00013929504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994516,0.000005231109,0.000003976131,0.000012944587,0.00001542112,0.000017395489],"domain_scores_gemma":[0.9997209,0.000034317974,0.00010416429,0.000016081443,0.000040990086,0.000083588915],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015420787,0.00020111592,0.00025111638,0.0013193124,0.0004385919,0.0004141929,0.0001130776,0.00022716916,0.0011614857],"category_scores_gemma":[0.00033030164,0.0001291308,0.00012331917,0.0006257139,0.00020968169,0.00024037341,0.00039180208,0.00027737697,0.00016073177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005575716,0.00009106991,0.90717995,0.00004050965,0.00006977081,0.0007402085,0.0015423379,0.0006910367,0.07074865,0.00029202463,0.0012110499,0.016835785],"study_design_scores_gemma":[0.000003111105,0.000024151806,0.9987437,0.0000031667103,0.000004845605,0.00004789744,0.00017219012,0.00035576522,0.0003846515,0.000023268643,0.00023434655,0.000002973601],"about_ca_topic_score_codex":0.0032623857,"about_ca_topic_score_gemma":0.008009039,"teacher_disagreement_score":0.0032623857,"about_ca_system_score_codex":0.00018065306,"about_ca_system_score_gemma":0.00009053842,"threshold_uncertainty_score":0.006486833},"labels":[],"label_agreement":null},{"id":"W2790645477","doi":"10.1002/2017gl076486","title":"Discovery of 1 Hz Range Modulation of Isolated Proton Aurora at Subauroral Latitudes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada; Athabasca University","funders":"Canada Foundation for Innovation","keywords":"Physics; Magnetosphere; Proton; Modulation (music); Luminosity; Cyclotron; Computational physics; Range (aeronautics); Electron; Astrophysics; Geophysics; Plasma; Nuclear physics; Acoustics","score_opus":0.020380468472753537,"score_gpt":0.2981298612933567,"score_spread":0.2777493928206032,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790645477","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951976,0.00051426864,0.000785034,0.000055598113,0.00001665116,0.000008176482,0.0002501141,0.000048500748,0.003124124],"genre_scores_gemma":[0.9992774,0.00008366809,0.0002670361,0.000016979038,0.000024079824,0.0000042003267,0.00009821574,0.000006300773,0.0002221135],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994135,0.0000052963815,0.0000017775814,0.000020878648,0.000012483533,0.000018129047],"domain_scores_gemma":[0.99974316,0.000058679445,0.000094610885,0.000028547967,0.000034462195,0.000040553216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009360672,0.00015811325,0.00018576147,0.0006916164,0.00021894673,0.00040470308,0.00019533618,0.00028802233,0.0016168716],"category_scores_gemma":[0.00033482365,0.00014599004,0.000117576965,0.000331606,0.00020492423,0.00026009738,0.00037049467,0.0003476627,0.00036806116],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045498658,0.00005907343,0.2554855,0.00019162968,0.0000947773,0.0012734666,0.0007664007,0.00036084355,0.7090375,0.0010222121,0.0007217291,0.030531956],"study_design_scores_gemma":[0.000009707556,0.00008807458,0.9846631,0.00001160633,0.000028869386,0.0004654939,0.000114454946,0.00037487052,0.012414445,0.00022392655,0.0015970888,0.000008272764],"about_ca_topic_score_codex":0.00040601246,"about_ca_topic_score_gemma":0.0007558643,"teacher_disagreement_score":0.0016168716,"about_ca_system_score_codex":0.00011652989,"about_ca_system_score_gemma":0.00004812733,"threshold_uncertainty_score":0.0054089427},"labels":[],"label_agreement":null},{"id":"W2790779039","doi":"10.1002/2017gl072652","title":"Submicroscopic metallic iron in lunar soils estimated from the in situ spectra of the Chang'E‐3 mission","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg","funders":"National Natural Science Foundation of China","keywords":"Regolith; Space weathering; Lunar soil; Rocket (weapon); Maturity (psychological); Weathering; Spectral line; Metal; Geology; Soil water; Atmospheric radiative transfer codes; Radiative transfer; Environmental science; Materials science; Mineralogy; Astrobiology; Optics; Physics; Geochemistry; Astronomy; Metallurgy; Soil science","score_opus":0.06414916918364517,"score_gpt":0.33596781555330796,"score_spread":0.2718186463696628,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790779039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995956,0.0000135334585,0.00015287401,0.0000025180752,4.926587e-7,0.0000011399233,0.00006995952,0.000010109853,0.00015386243],"genre_scores_gemma":[0.9995915,0.000010170125,0.00021126162,0.0000028376269,6.255175e-7,0.0000013943845,0.000114241426,0.00000464269,0.00006327099],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999653,0.0000026653909,0.0000015812988,0.000011656237,0.000008819988,0.000009986551],"domain_scores_gemma":[0.9999161,0.000019772946,0.000018231316,0.0000052955506,0.000021144138,0.000019530213],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008408155,0.00024614506,0.00011305248,0.00080524647,0.0001977991,0.00021537901,0.00013321065,0.00027085564,0.0005053149],"category_scores_gemma":[0.0001371935,0.00013681257,0.000138436,0.00028382734,0.00011294407,0.00017640201,0.00013832688,0.00013152162,0.000109459936],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030147072,0.00006125228,0.4824236,0.000039635946,0.000043873035,0.00017437739,0.00022809186,0.0013322986,0.50464976,0.000055825487,0.00013679679,0.010553058],"study_design_scores_gemma":[0.0000069631187,0.000053055912,0.97025394,0.00000295082,0.000014611973,0.00008549143,0.00015886892,0.002394963,0.026797576,0.000023501108,0.00020278117,0.000005175671],"about_ca_topic_score_codex":0.0062328447,"about_ca_topic_score_gemma":0.011040945,"teacher_disagreement_score":0.0062328447,"about_ca_system_score_codex":0.0001494718,"about_ca_system_score_gemma":0.000089588815,"threshold_uncertainty_score":0.012393177},"labels":[],"label_agreement":null},{"id":"W2790864481","doi":"10.1002/2017gl076621","title":"Monitoring and Modeling the Rapid Evolution of Earth's Newest Volcanic Island: <i>Hunga Tonga Hunga Ha'apai</i> (Tonga) Using High Spatial Resolution Satellite Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canadian Space Agency","funders":"NASA Headquarters; National Aeronautics and Space Administration; Earth Sciences Division; National Science Foundation","keywords":"Volcano; Geology; Subaerial; Satellite; Physical geography; Digital elevation model; High resolution; Remote sensing; Oceanography; Seismology; Geography","score_opus":0.07724679731044752,"score_gpt":0.29887419416343214,"score_spread":0.2216273968529846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2790864481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979278,0.00006588367,0.0009839279,0.00007508746,0.000006425061,0.000011769101,0.00051702186,0.00004651282,0.00036552802],"genre_scores_gemma":[0.9983637,0.000045641937,0.0010851336,0.0000060653124,0.000003219347,0.000008599978,0.00034665415,0.000005270223,0.00013578557],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999368,0.000012111685,0.0000042055885,0.000021948563,0.0000073060323,0.000017698067],"domain_scores_gemma":[0.99983454,0.000039399005,0.00003658437,0.000017350438,0.00003387356,0.000038218775],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028777146,0.0003408829,0.00024786446,0.0004542133,0.00023973006,0.00076656695,0.0004925606,0.0004591444,0.00060705387],"category_scores_gemma":[0.00061281654,0.0002606137,0.00036470342,0.00062176486,0.00027108664,0.0004291279,0.00043759463,0.00028113578,0.00008099135],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000104143495,0.00010300816,0.43212375,0.000083095,0.00030983586,0.00038988635,0.00016397845,0.5488245,0.0068360493,0.0004722207,0.0006679791,0.009921586],"study_design_scores_gemma":[0.000025403166,0.000032027157,0.19198357,0.000007918294,0.00006380396,0.000028754748,0.00013690768,0.80648005,0.0004794803,0.00010934339,0.0006370573,0.00001558868],"about_ca_topic_score_codex":0.16803496,"about_ca_topic_score_gemma":0.15154864,"teacher_disagreement_score":0.16803496,"about_ca_system_score_codex":0.001258441,"about_ca_system_score_gemma":0.0008245705,"threshold_uncertainty_score":0.33411378},"labels":[],"label_agreement":null},{"id":"W2791470514","doi":"10.1002/2017gl076164","title":"Massive Mortality of a Planktivorous Seabird in Response to a Marine Heatwave","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":284,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Ministry of Agriculture; Abbotsford Veterinary Clinic","funders":"Division of Research on Learning in Formal and Informal Settings; California Department of Fish and Wildlife; Washington Department of Fish and Wildlife; National Science Foundation","keywords":"Oceanography; Seabird; Zooplankton; Energetics; Abundance (ecology); Foraging; Population; Biomass (ecology); Environmental science; Climate change; Global warming; Ecology; Geography; Biology; Geology","score_opus":0.05281924499872885,"score_gpt":0.3459150408028506,"score_spread":0.29309579580412176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791470514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993667,0.0000118443595,0.0001035005,0.00005098456,0.000004156691,0.000001775073,0.00017802759,0.0000061429446,0.0002769159],"genre_scores_gemma":[0.9995783,0.000014235669,0.000062656,0.000017220085,0.000002697242,0.0000021905225,0.00018297473,7.4760555e-7,0.00013889419],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993014,0.00001362751,0.000003064031,0.000021354786,0.000010550165,0.000021209202],"domain_scores_gemma":[0.9997341,0.000041201918,0.00010647309,0.00002066813,0.000031294167,0.00006625898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023708805,0.00013434327,0.000105083294,0.00020287358,0.00025265073,0.00044744895,0.00015530695,0.00019039698,0.0011604334],"category_scores_gemma":[0.00054313306,0.00008764831,0.00022938727,0.00017356647,0.00017969993,0.00015525614,0.0003589357,0.00025874347,0.00013675191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000093100294,0.000041219108,0.99152887,0.000009727899,0.00007637318,0.00009556422,0.00009458057,0.0019992865,0.0025220595,0.00008250943,0.00061336276,0.002843374],"study_design_scores_gemma":[0.0000031631052,0.00004523101,0.99471575,0.0000033248568,0.00001742147,0.00004044394,0.00024095234,0.004387135,0.0002787592,0.000085250496,0.00017907015,0.00000355764],"about_ca_topic_score_codex":0.0434889,"about_ca_topic_score_gemma":0.07841667,"teacher_disagreement_score":0.0434889,"about_ca_system_score_codex":0.00054642203,"about_ca_system_score_gemma":0.00026476668,"threshold_uncertainty_score":0.0864715},"labels":[],"label_agreement":null},{"id":"W2791584082","doi":"10.1002/2017gl076587","title":"Increasing Mobility of High Arctic Sea Ice Increases Marine Hazards Off the East Coast of Newfoundland","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Canadian Armed Forces; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; ArcticNet; Manitoba Hydro","keywords":"Sea ice; Oceanography; Arctic ice pack; Coast guard; Archipelago; Arctic; Drift ice; Geology; Cryosphere; Antarctic sea ice; Arctic sea ice decline; Iceberg; Environmental science; Environmental protection","score_opus":0.019531245439599578,"score_gpt":0.2650685442082003,"score_spread":0.24553729876860073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791584082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99856,0.000057244008,0.000022837858,0.00016087583,0.000002560153,0.0000016456795,0.00018963907,0.000002637806,0.0010025407],"genre_scores_gemma":[0.9991117,0.000100285935,0.00005201585,0.000044853292,0.0000025132347,0.0000017802766,0.00012366158,0.0000013199834,0.00056179607],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998565,0.000013182976,0.000006532547,0.000029629693,0.000021191589,0.000072871895],"domain_scores_gemma":[0.99943346,0.0000621024,0.00025583903,0.000025098912,0.00009701252,0.00012648705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015431421,0.000118655415,0.00012233523,0.00057025783,0.0009381111,0.0009827773,0.00030580195,0.00020428143,0.0017097375],"category_scores_gemma":[0.00053072424,0.00012159822,0.0001622652,0.00062690896,0.0006007181,0.00044313207,0.00071104674,0.00026976294,0.00012171829],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026408616,0.000012315923,0.9937126,0.000011687925,0.000026828993,0.0002603478,0.00086535903,0.00019802648,0.000938631,0.00006823442,0.00061494374,0.0032646605],"study_design_scores_gemma":[5.667637e-7,0.000004747129,0.9975924,0.0000073880633,0.000004963864,0.00003138494,0.001840375,0.00007549254,0.00005810076,0.000007783417,0.00037507122,0.0000017396358],"about_ca_topic_score_codex":0.8812361,"about_ca_topic_score_gemma":0.9684003,"teacher_disagreement_score":0.11876392,"about_ca_system_score_codex":0.0046580117,"about_ca_system_score_gemma":0.0023878736,"threshold_uncertainty_score":0.23892665},"labels":[],"label_agreement":null},{"id":"W2791589553","doi":"10.1002/2017gl076100","title":"The Geological Susceptibility of Induced Earthquakes in the Duvernay Play","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":102,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismology; Tectonics; Seismic hazard; Basement; Sedimentary rock; Paleontology","score_opus":0.0656186787181504,"score_gpt":0.316037116866944,"score_spread":0.2504184381487936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791589553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993081,0.000011304894,0.00010520155,0.000028224486,3.8454215e-7,0.0000014540177,0.00006627509,0.000004934651,0.00047427282],"genre_scores_gemma":[0.99979776,0.00000437029,0.000026769943,0.0000014992157,2.0056318e-7,4.085979e-7,0.0000701777,8.999984e-7,0.00009792029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997731,0.00007610413,0.000016285425,0.000047529466,0.00003322911,0.000053699412],"domain_scores_gemma":[0.9991289,0.0002879762,0.00018934111,0.000082071565,0.00017054625,0.00014114019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003126167,0.00011788569,0.00018012863,0.0009098758,0.00046306153,0.0007598914,0.00040708308,0.00027822718,0.002079],"category_scores_gemma":[0.0028174652,0.0001256121,0.00013582585,0.00051746506,0.00069718016,0.00029627274,0.00067223137,0.0002070207,0.0002597606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012118826,0.000019385461,0.98680633,0.00001095382,0.000051343173,0.00015070003,0.0011777185,0.0045189383,0.002174095,0.0008170989,0.00018569505,0.0039664507],"study_design_scores_gemma":[0.0000033824451,0.000026040292,0.98550236,0.000004088873,0.0000066443313,0.00005643294,0.0008766785,0.012775611,0.00019347064,0.00016175765,0.00038781334,0.0000057705597],"about_ca_topic_score_codex":0.24035707,"about_ca_topic_score_gemma":0.351331,"teacher_disagreement_score":0.24035707,"about_ca_system_score_codex":0.0015755824,"about_ca_system_score_gemma":0.0005073768,"threshold_uncertainty_score":0.47791606},"labels":[],"label_agreement":null},{"id":"W2791608688","doi":"10.1002/2017gl076251","title":"Limited Impact of Subglacial Supercooling Freeze‐on for Greenland Ice Sheet Stratigraphy","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Excellence Research Chairs, Government of Canada","keywords":"Geology; Supercooling; Ice sheet; Greenland ice sheet; Ice stream; Cryosphere; Freezing point; Depth sounding; Ice formation; Geomorphology; Climatology; Geophysics; Atmospheric sciences; Oceanography; Sea ice; Meteorology; Geography","score_opus":0.06784395507980612,"score_gpt":0.33093332980662216,"score_spread":0.26308937472681604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791608688","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990552,0.000022132801,0.0002051459,0.000016914388,0.0000014331779,0.0000012998198,0.00014915805,0.000025773461,0.0005230108],"genre_scores_gemma":[0.99975115,0.000008252273,0.000058521535,0.000004244148,4.769374e-7,6.262848e-7,0.00010137105,0.0000055616692,0.000069702335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990106,0.00002035137,0.0000048783654,0.000024858284,0.000017652126,0.000031226824],"domain_scores_gemma":[0.99975723,0.00008921149,0.00003905271,0.000042314216,0.000028053842,0.000044126642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027689742,0.00023865317,0.00017171573,0.00024922303,0.00020684468,0.0006543513,0.00024060249,0.00020068894,0.001090218],"category_scores_gemma":[0.0006057318,0.00015656112,0.0002932238,0.00018005323,0.0002770453,0.00038600454,0.00029570694,0.00015632153,0.00012844984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017848582,0.000049873437,0.8199891,0.000021346243,0.00012557326,0.0001983432,0.00009799505,0.15626544,0.012643602,0.00042267918,0.00032065462,0.009686936],"study_design_scores_gemma":[0.00002080071,0.00008152518,0.7948219,0.000011414622,0.00005256929,0.000059130158,0.00021559431,0.19794235,0.0057634767,0.00027481734,0.00074083486,0.000015543217],"about_ca_topic_score_codex":0.052457184,"about_ca_topic_score_gemma":0.064730994,"teacher_disagreement_score":0.052457184,"about_ca_system_score_codex":0.0010117249,"about_ca_system_score_gemma":0.00066483434,"threshold_uncertainty_score":0.10430372},"labels":[],"label_agreement":null},{"id":"W2791728858","doi":"10.1002/2017gl076647","title":"Pan‐Arctic Distribution of Bioavailable Dissolved Organic Matter and Linkages With Productivity in Ocean Margins","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Prince Albert II of Monaco Foundation; Institut national des sciences de l'Univers; Government of Canada; National Oceanic and Atmospheric Administration; Centre National d’Etudes Spatiales; Agence Nationale de la Recherche; European Space Agency; National Science Foundation; Japan Agency for Marine-Earth Science and Technology; Office of Naval Research; Centre National de la Recherche Scientifique; Canadian Institute for Advanced Research","keywords":"Dissolved organic carbon; Oceanography; Arctic; Environmental science; Productivity; Colored dissolved organic matter; Bay; Plankton; Total organic carbon; Ecosystem; Organic matter; Environmental chemistry; Phytoplankton; Geology; Ecology; Chemistry; Nutrient; Biology","score_opus":0.013744605588075725,"score_gpt":0.24131605358071365,"score_spread":0.22757144799263793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791728858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947745,0.00011348796,0.00002457204,0.0000068702984,0.0000012623096,2.8851093e-7,0.0001604566,0.0000015597274,0.00021396714],"genre_scores_gemma":[0.99967206,0.000066728346,0.000028261273,0.0000026347366,0.0000018749425,5.019298e-7,0.00016748122,8.6656655e-7,0.000059448957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999928,0.000009879056,0.0000061963865,0.000025148527,0.000010177517,0.000020606003],"domain_scores_gemma":[0.999556,0.00006806596,0.00013924601,0.000019106423,0.00011934651,0.000098164266],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002370946,0.0001395799,0.00013193286,0.00089044386,0.00031556442,0.00061428663,0.000090572794,0.00014527584,0.0005728534],"category_scores_gemma":[0.0004077369,0.00010664851,0.00013923667,0.00079217134,0.00019065422,0.0002053293,0.0003451504,0.000121022036,0.00008537751],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008737089,0.000008114909,0.9925909,0.000010010843,0.000051022125,0.00003456952,0.00022622812,0.00012764992,0.004261814,0.000038061193,0.000040495146,0.0025238523],"study_design_scores_gemma":[3.8343182e-7,0.0000057736934,0.99955875,0.0000020912469,0.0000057610487,0.000014322938,0.0001599,0.000063704356,0.00010890006,0.000009741227,0.00006997029,7.903954e-7],"about_ca_topic_score_codex":0.032807037,"about_ca_topic_score_gemma":0.042189438,"teacher_disagreement_score":0.032807037,"about_ca_system_score_codex":0.00030856332,"about_ca_system_score_gemma":0.00021464875,"threshold_uncertainty_score":0.06523222},"labels":[],"label_agreement":null},{"id":"W2791748154","doi":"10.1002/2017gl076789","title":"Determining Near‐Bottom Fluxes of Passive Tracers in Aquatic Environments","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada","keywords":"Dissipation; Turbulence; TRACER; Flux (metallurgy); Eddy covariance; Scalar (mathematics); Turbulence kinetic energy; Environmental science; Kinetic energy; Mechanics; Energy flux; Atmospheric sciences; Geology; Physics; Materials science; Ecosystem; Classical mechanics; Geometry; Thermodynamics; Mathematics","score_opus":0.024715809595693434,"score_gpt":0.29542018685795557,"score_spread":0.27070437726226215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2791748154","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993548,0.00007298041,0.0059048664,0.000008559866,0.000003951621,0.000008831198,0.000056693254,0.000017865834,0.00037831438],"genre_scores_gemma":[0.9944563,0.00007621961,0.005049109,0.000010276329,0.000002992231,0.000010567203,0.00006438148,0.000007673295,0.00032252196],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999193,0.0000113555725,0.0000034033171,0.000026714994,0.000027498903,0.000011596018],"domain_scores_gemma":[0.9998073,0.00007240027,0.000041284544,0.000009335447,0.000049559218,0.000020142925],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026095932,0.00019169213,0.00020171108,0.00040476536,0.00023615653,0.00040338116,0.00018113048,0.00022773932,0.00023818696],"category_scores_gemma":[0.00050247106,0.00013186068,0.00009155945,0.00020801673,0.00023470445,0.00041656021,0.00025836064,0.00028929792,0.0000948929],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019204088,0.00010044844,0.09559715,0.00006203694,0.000026253769,0.00006433238,0.00017264181,0.005169551,0.878076,0.0006838765,0.0000949795,0.0197606],"study_design_scores_gemma":[0.000057737936,0.00083184184,0.37680364,0.00004965317,0.000063191525,0.0001869985,0.0004835689,0.1672471,0.45084873,0.0013247521,0.002034822,0.00006803906],"about_ca_topic_score_codex":0.0042842296,"about_ca_topic_score_gemma":0.0042567244,"teacher_disagreement_score":0.0042842296,"about_ca_system_score_codex":0.00034461293,"about_ca_system_score_gemma":0.0002695691,"threshold_uncertainty_score":0.008518577},"labels":[],"label_agreement":null},{"id":"W2792141141","doi":"10.1002/2017gl076606","title":"Was the Deepwater Horizon Well Discharge Churn Flow? Implications on the Estimation of the Oil Discharge and Droplet Size Distribution","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oil Spill Detection and Mitigation","field":"Environmental Science","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Gulf of Mexico Research Initiative","keywords":"Wellhead; Flow (mathematics); Plume; Petroleum engineering; Mechanics; Environmental science; Fluid dynamics; Geology; Meteorology; Physics","score_opus":0.015418664326742298,"score_gpt":0.27121780007044416,"score_spread":0.25579913574370183,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792141141","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97212744,0.0002047428,0.025818013,0.00033265603,0.000017028098,0.000025145217,0.00035201284,0.0001656144,0.00095747894],"genre_scores_gemma":[0.9966252,0.00008862602,0.0030458139,0.00003445308,0.0000047948347,0.0000044380845,0.000059834663,0.000010226024,0.00012681274],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969375,0.000055772547,0.000024802932,0.00007880988,0.000103893806,0.00004295845],"domain_scores_gemma":[0.9990883,0.0004563908,0.00023438896,0.00005550219,0.00013043285,0.000035075172],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009555166,0.00029566773,0.00025307818,0.00063563365,0.00021352341,0.0007481039,0.0003258043,0.00037525216,0.00038806663],"category_scores_gemma":[0.0037111857,0.00020376552,0.00018162926,0.00045966683,0.00040988717,0.001066067,0.0002814885,0.00036870054,0.00008686177],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064950116,0.0001048534,0.6275294,0.00020793096,0.000091007045,0.0009856978,0.0006107632,0.0696343,0.22244409,0.0036610267,0.0006488316,0.07343271],"study_design_scores_gemma":[0.00003191919,0.0002511199,0.47664398,0.00006465754,0.0000521542,0.00028212543,0.0007589481,0.39261934,0.124288395,0.00283288,0.0020726603,0.00010179774],"about_ca_topic_score_codex":0.024130164,"about_ca_topic_score_gemma":0.01906298,"teacher_disagreement_score":0.024130164,"about_ca_system_score_codex":0.00097534107,"about_ca_system_score_gemma":0.00041377617,"threshold_uncertainty_score":0.047979414},"labels":[],"label_agreement":null},{"id":"W2792489731","doi":"10.1002/2017gl076591","title":"Coastal Freshening Prevents Fjord Bottom Water Renewal in Northeast Greenland: A Mooring Study From 2003 to 2015","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Horizon 2020 Framework Programme; Canada Excellence Research Chairs, Government of Canada; Canada Foundation for Innovation; Research Manitoba; Pinngortitaleriffik; Aarhus Universitet","keywords":"Fjord; Oceanography; Mooring; Geology; Bottom water; Water mass; Environmental science; Climatology","score_opus":0.026322456837857715,"score_gpt":0.29209083894920385,"score_spread":0.2657683821113461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792489731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994727,0.000032399075,0.000018397976,0.000017014761,0.000002339685,0.0000015669733,0.00030031666,0.0000018392246,0.00015345625],"genre_scores_gemma":[0.9991497,0.000029069724,0.000037691345,0.000016186546,0.0000025677427,0.000002177493,0.0004769581,0.0000014986298,0.00028409803],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985933,0.000014522684,0.000015845344,0.000034599976,0.000024703044,0.00005098323],"domain_scores_gemma":[0.9994398,0.000048685342,0.0002121649,0.000051203962,0.00010517558,0.00014288566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040066015,0.00017001355,0.00022623368,0.0006900974,0.00049299817,0.0006572426,0.00038552113,0.0002947314,0.0005803981],"category_scores_gemma":[0.00059967046,0.0001233247,0.00031892952,0.00082359486,0.00035577017,0.00031935336,0.0005415954,0.00021430032,0.00010368521],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059726957,0.000019849616,0.99728394,0.0000056666117,0.000035817706,0.00007511012,0.00023164334,0.00009711965,0.00050754915,0.000015389996,0.00012754358,0.0015406064],"study_design_scores_gemma":[5.0295836e-7,0.0000074950844,0.9995783,0.0000024966312,0.0000047708763,0.000008132005,0.00016392898,0.000064844535,0.00004253396,0.0000029713133,0.00012321572,7.5000213e-7],"about_ca_topic_score_codex":0.25097564,"about_ca_topic_score_gemma":0.4885149,"teacher_disagreement_score":0.25097564,"about_ca_system_score_codex":0.001425085,"about_ca_system_score_gemma":0.0012873564,"threshold_uncertainty_score":0.49902958},"labels":[],"label_agreement":null},{"id":"W2792673356","doi":"10.1002/2017gl076649","title":"Regional Climate Sensitivity‐ and Historical‐Based Projections to 2100","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"GCM transcription factors; Climatology; Forcing (mathematics); Climate change; Environmental science; Climate model; Scale (ratio); General Circulation Model; Representative Concentration Pathways; Projection (relational algebra); Climate sensitivity; Sensitivity (control systems); Transient climate simulation; Computer science; Geography; Geology; Cartography","score_opus":0.08467677143256351,"score_gpt":0.3304492788645488,"score_spread":0.24577250743198525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2792673356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95887583,0.00048217986,0.019039473,0.0003904305,0.000059075064,0.000020142512,0.011202682,0.00028836844,0.009641745],"genre_scores_gemma":[0.98862654,0.00025729416,0.0051516746,0.000030599294,0.000014082463,0.000046268156,0.005486704,0.00003907955,0.0003477974],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997665,0.000088679444,0.000013824241,0.000046579193,0.00004877437,0.000035665857],"domain_scores_gemma":[0.9994548,0.000118842996,0.000093670766,0.00006780665,0.00022527997,0.00003965313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001221353,0.0004139833,0.00017542396,0.00077107165,0.00013299589,0.0004443308,0.000391196,0.000287415,0.0013437349],"category_scores_gemma":[0.0016953804,0.00019232447,0.00064525893,0.00096002716,0.00020908754,0.00060679327,0.00036489137,0.000333954,0.0003561156],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037427223,0.000067957466,0.13114525,0.00021510547,0.00042482413,0.00024048387,0.00017126821,0.81714016,0.0053436914,0.011102363,0.0051448154,0.02862986],"study_design_scores_gemma":[0.000076011595,0.00032202082,0.38484958,0.0001586484,0.00035131018,0.00038328767,0.000360388,0.5607947,0.012961695,0.0120287,0.02757063,0.00014308131],"about_ca_topic_score_codex":0.011022077,"about_ca_topic_score_gemma":0.00735379,"teacher_disagreement_score":0.011022077,"about_ca_system_score_codex":0.00074100617,"about_ca_system_score_gemma":0.00043502325,"threshold_uncertainty_score":0.021915853},"labels":[],"label_agreement":null},{"id":"W2793021219","doi":"10.1002/2017gl075774","title":"GNSS Observations of Ionospheric Variations During the 21 August 2017 Solar Eclipse","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":169,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Office of Naval Research; Fondation Muriel McQueen Fergusson; National Aeronautics and Space Administration","keywords":"TEC; Total electron content; Ionosphere; Solar eclipse; GNSS applications; Eclipse; Satellite; Geology; Daytime; Environmental science; Geodesy; Atmospheric sciences; Astronomy; Physics; Geophysics","score_opus":0.037878233937089306,"score_gpt":0.3044515004227868,"score_spread":0.26657326648569746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793021219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953277,0.000042078515,0.00012554179,0.00003678798,0.000014418118,0.000006123307,0.0015317893,0.000030665717,0.0028847475],"genre_scores_gemma":[0.9954798,0.00007033345,0.00018195501,0.000018070756,0.000013657678,0.000006187192,0.0032415355,0.000007758723,0.0009806913],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999527,0.000004015135,0.000002748321,0.000009132285,0.000019149295,0.000012242557],"domain_scores_gemma":[0.99988353,0.000009900893,0.000023527395,0.000009910501,0.00005064109,0.000022443555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009330586,0.00018784471,0.000109083674,0.00046839617,0.00030647617,0.00031544323,0.000108444285,0.00018521814,0.00074627076],"category_scores_gemma":[0.00025849984,0.000060279894,0.00009117219,0.00038601574,0.00012563905,0.00013856331,0.00032269297,0.00018894927,0.00023381592],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000424086,0.000085973785,0.93497837,0.000039823255,0.00010431788,0.0008034291,0.00076689664,0.0035312958,0.028377542,0.0003056404,0.004820168,0.025762457],"study_design_scores_gemma":[0.000009211987,0.000040277464,0.9923913,0.0000095780015,0.000012083654,0.00007434126,0.00018529754,0.0014920944,0.0013985318,0.000044335346,0.0043377397,0.0000051861925],"about_ca_topic_score_codex":0.021599371,"about_ca_topic_score_gemma":0.07591676,"teacher_disagreement_score":0.021599371,"about_ca_system_score_codex":0.0004217972,"about_ca_system_score_gemma":0.00022734859,"threshold_uncertainty_score":0.042947292},"labels":[],"label_agreement":null},{"id":"W2793484645","doi":"10.1002/2017gl076361","title":"Understanding the Dynamics of Future Changes in Extreme Precipitation Intensity","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Precipitation; Climatology; Environmental science; Equator; Subtropics; Intensity (physics); Atmospheric sciences; Climate change; Geology; Meteorology; Latitude; Geography; Geodesy; Physics; Ecology","score_opus":0.17944621828782725,"score_gpt":0.3236447538290642,"score_spread":0.14419853554123696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793484645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9792363,0.00034920918,0.006645214,0.0025217275,0.00002473291,0.000011258835,0.0017298149,0.000079697624,0.0094019715],"genre_scores_gemma":[0.9987085,0.00013604248,0.00040433608,0.00003564412,0.0000070587707,0.0000022808981,0.00033515092,0.0000067439464,0.00036434125],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999194,0.0000110477795,0.0000045297124,0.000025002439,0.00001699518,0.000022987857],"domain_scores_gemma":[0.9996172,0.00008109548,0.00010976949,0.000022158898,0.00011060405,0.00005912901],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00050199084,0.0001762082,0.00016055332,0.00043473992,0.000334111,0.001308632,0.0004521695,0.00048880134,0.0020910813],"category_scores_gemma":[0.0021566902,0.00022480122,0.00020876066,0.00048534613,0.00038769006,0.0012291009,0.00047371906,0.0006707365,0.00018160329],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011266798,0.00007290915,0.52405083,0.00006192093,0.00017934015,0.00016783191,0.00040615108,0.4121401,0.0064677205,0.029610105,0.005676635,0.021053828],"study_design_scores_gemma":[0.0000121288085,0.000016722915,0.46465713,0.000020594014,0.00003698141,0.000040478513,0.00035731515,0.51286554,0.0007023138,0.016230851,0.00502945,0.000030515965],"about_ca_topic_score_codex":0.27041155,"about_ca_topic_score_gemma":0.22067958,"teacher_disagreement_score":0.27041155,"about_ca_system_score_codex":0.0019413806,"about_ca_system_score_gemma":0.001137702,"threshold_uncertainty_score":0.53767514},"labels":[],"label_agreement":null},{"id":"W2793564039","doi":"10.1002/2017gl076051","title":"Alfvénic Dynamics and Fine Structuring of Discrete Auroral Arcs: Swarm and e‐POP Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Magna International (Canada); University of Calgary; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; European Space Agency; University of Iowa","keywords":"Physics; Ionosphere; Swarm behaviour; Geophysics; Spacecraft; Outflow; Magnetic field; Magnetosphere; Computational physics; Electric field; Meteorology; Astronomy","score_opus":0.022350287219654003,"score_gpt":0.2930802367916123,"score_spread":0.27072994957195834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2793564039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739,0.00003058695,0.00073926576,0.000018416315,0.0000030333078,0.000005033876,0.00021040627,0.000040173898,0.0015631871],"genre_scores_gemma":[0.99860954,0.00001976874,0.0008923966,0.000008172402,0.00000700221,0.000003827086,0.00027922523,0.000008850315,0.00017113928],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999966,0.0000036850222,0.0000014927992,0.000012709053,0.000008444824,0.000007565661],"domain_scores_gemma":[0.9998386,0.00002777934,0.0000384597,0.000022703563,0.00002059045,0.000051742576],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011980369,0.000107098866,0.00011090658,0.00052608753,0.00020515804,0.0002863098,0.00015223234,0.0001930721,0.00067900826],"category_scores_gemma":[0.00028341552,0.00011467217,0.000119055134,0.00031128194,0.0001843316,0.00024865742,0.00042728102,0.00020438859,0.00010879374],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008514113,0.00013298806,0.4724016,0.00008947438,0.000120731274,0.00089854427,0.00095747295,0.0024504666,0.48540956,0.0007160514,0.0011766638,0.03479508],"study_design_scores_gemma":[0.000031802454,0.00010239715,0.98801756,0.000006846737,0.00001556184,0.00029753736,0.0002149939,0.0049006077,0.0049198116,0.00022933172,0.0012547572,0.000008884306],"about_ca_topic_score_codex":0.0007537941,"about_ca_topic_score_gemma":0.0014056615,"teacher_disagreement_score":0.0007537941,"about_ca_system_score_codex":0.000087819564,"about_ca_system_score_gemma":0.000051407398,"threshold_uncertainty_score":0.002271533},"labels":[],"label_agreement":null},{"id":"W2794301846","doi":"10.1002/2017gl076357","title":"Oxidative Processing Lowers the Ice Nucleation Activity of Birch and Alder Pollen","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Ice nucleus; Supersaturation; Nucleation; Alder; Cloud chamber; Pollen; Chemistry; Environmental chemistry; Chemical engineering; Organic chemistry; Botany; Biology","score_opus":0.03253595908060531,"score_gpt":0.29812404165084244,"score_spread":0.26558808257023714,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794301846","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996118,0.00006695093,0.00005783769,0.0000042821202,0.000002911407,0.0000017132572,0.000031557713,0.0000021142107,0.00022092935],"genre_scores_gemma":[0.9994733,0.000042768323,0.000069648144,0.0000060223933,0.0000025396546,0.0000012351935,0.000086081774,0.0000031095494,0.0003154216],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999224,0.000011999884,0.000003171101,0.000015454912,0.000018735218,0.000028248947],"domain_scores_gemma":[0.9999138,0.000017077034,0.000024699328,0.000007451331,0.000016849937,0.000020187668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000094322655,0.00022632362,0.00014955178,0.00015159918,0.0001839699,0.00033574825,0.000109885266,0.00013446719,0.0012966581],"category_scores_gemma":[0.00013283303,0.00009238007,0.0001189993,0.000065882865,0.00016091057,0.0001481971,0.00010802669,0.00016678122,0.00009388618],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018689083,0.00002514662,0.0037564386,0.000016744265,0.000011967043,0.000020966272,0.00002471392,0.00004852707,0.9951566,0.000028201957,0.000017099284,0.0007067512],"study_design_scores_gemma":[0.000010601727,0.0003849569,0.12758914,0.0000027327796,0.000024746512,0.00007652114,0.00009070053,0.0004947981,0.8705484,0.00005792883,0.00071578386,0.000003743483],"about_ca_topic_score_codex":0.002295673,"about_ca_topic_score_gemma":0.0022711947,"teacher_disagreement_score":0.002295673,"about_ca_system_score_codex":0.0002603815,"about_ca_system_score_gemma":0.000101726895,"threshold_uncertainty_score":0.004564643},"labels":[],"label_agreement":null},{"id":"W2794353718","doi":"10.1002/2017gl076988","title":"Effects of Asymmetric Secondary Eyewall on Tropical Cyclone Evolution in Hurricane <i>Ike</i> (2008)","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Environment and Climate Change Canada; East China Normal University; National Natural Science Foundation of China; Dental Foundation of Oregon","keywords":"Eye; Tropical cyclone; Rainband; Geology; Climatology; Maximum sustained wind; Synthetic aperture radar; Meteorology; Oceanography; Wind shear; Remote sensing; Geography; Wind speed","score_opus":0.01401587206864983,"score_gpt":0.27062890151817826,"score_spread":0.2566130294495284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794353718","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997062,0.000007817618,0.000034265606,0.0000070296755,0.0000011125044,8.5830874e-7,0.000027732915,0.0000023170799,0.00021269964],"genre_scores_gemma":[0.9998832,0.0000056778977,0.000023233777,0.0000025405361,8.733793e-7,5.712896e-7,0.00004295819,7.9263526e-7,0.00004023371],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999633,0.000006963921,0.0000028385712,0.000007908167,0.000006363451,0.000012640447],"domain_scores_gemma":[0.9997938,0.00004062278,0.000067124056,0.000013694226,0.000033467884,0.00005125298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000088724526,0.0001090217,0.00012646324,0.00018976354,0.00021156073,0.00025277675,0.000066359986,0.00010498503,0.0007989062],"category_scores_gemma":[0.00043094967,0.000050744544,0.00011371481,0.0001102051,0.00012315054,0.00009913532,0.00019343085,0.00016663641,0.000067158944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008465651,0.00012339666,0.8827337,0.000041678693,0.00008636248,0.00085599296,0.00023162592,0.009779812,0.08739086,0.000288838,0.00062126335,0.016999893],"study_design_scores_gemma":[0.000005613629,0.00006266241,0.99119735,0.0000029583382,0.000010823866,0.0000706501,0.0001137389,0.0064907847,0.0018396406,0.000027285856,0.00017496129,0.0000034735458],"about_ca_topic_score_codex":0.0056858044,"about_ca_topic_score_gemma":0.0074777002,"teacher_disagreement_score":0.0056858044,"about_ca_system_score_codex":0.00019235768,"about_ca_system_score_gemma":0.00011324842,"threshold_uncertainty_score":0.011305451},"labels":[],"label_agreement":null},{"id":"W2794680378","doi":"10.1002/2017gl075345","title":"Significant Weakening of Brewer‐Dobson Circulation Trends Over the 21st Century as a Consequence of the Montreal Protocol","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":116,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; Oficina Regional de Coordinación de Salud Mental, Comunidad de Madrid; National Aeronautics and Space Administration","keywords":"Montreal Protocol; Stratosphere; Ozone depletion; Ozone; Ozone layer; Environmental science; Forcing (mathematics); Climatology; Atmospheric sciences; Greenhouse gas; Meteorology; Oceanography; Geology; Geography","score_opus":0.03632808495363027,"score_gpt":0.31653364134827583,"score_spread":0.28020555639464556,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794680378","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95350665,0.0020285863,0.0019362757,0.006817933,0.00028839268,0.000070841765,0.01212662,0.00021209268,0.023012621],"genre_scores_gemma":[0.9941704,0.0005072098,0.00049851456,0.00028311447,0.000059373393,0.00002529431,0.001929124,0.000020037363,0.0025069362],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996014,0.000050838426,0.000014551318,0.0000855678,0.0001240077,0.00012360272],"domain_scores_gemma":[0.99913627,0.0000785385,0.00021662853,0.00008733639,0.0003409566,0.00014019679],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007197161,0.00027280356,0.00030759673,0.0005509605,0.0006963438,0.0014009887,0.00059698336,0.00048840314,0.0031171814],"category_scores_gemma":[0.0026467547,0.00013035012,0.00049010164,0.00082104193,0.00045287586,0.00056268845,0.0010424902,0.0006713031,0.00017541744],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00057599327,0.00012997496,0.7895314,0.00034897847,0.0012142116,0.0007086667,0.0008279288,0.060052622,0.01509746,0.03785395,0.037028063,0.05663065],"study_design_scores_gemma":[0.0000365791,0.000056690646,0.94481415,0.000047429276,0.000106512736,0.000033660537,0.00014626114,0.013571589,0.0025583897,0.0013404262,0.03722488,0.00006346902],"about_ca_topic_score_codex":0.69864,"about_ca_topic_score_gemma":0.68504965,"teacher_disagreement_score":0.69864,"about_ca_system_score_codex":0.0054459446,"about_ca_system_score_gemma":0.005688242,"threshold_uncertainty_score":0.60626954},"labels":[],"label_agreement":null},{"id":"W2794895367","doi":"10.1002/2017gl075547","title":"Winter Sentinel‐1 Backscatter as a Predictor of Spring Arctic Sea Ice Melt Pond Fraction","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Calgary; University of Victoria","funders":"European Space Agency; Natural Sciences and Engineering Research Council of Canada; Marine Environmental Observation Prediction and Response Network","keywords":"Melt pond; Arctic; Sea ice; Environmental science; Archipelago; Arctic ice pack; Backscatter (email); Oceanography; Satellite; Climatology; The arctic; Geology; Remote sensing; Sea ice thickness","score_opus":0.024710257486929114,"score_gpt":0.2921014696050356,"score_spread":0.26739121211810646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794895367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978276,0.000064659514,0.0008785798,0.000021209808,0.0000085497095,0.000002684772,0.00069262716,0.00006604362,0.0004379618],"genre_scores_gemma":[0.99781823,0.0000400526,0.0009781326,0.000009204256,0.000005032619,0.0000022942381,0.0009832752,0.000005655218,0.00015819688],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994075,0.000010268697,0.0000044197814,0.000014806934,0.000015901938,0.000013953979],"domain_scores_gemma":[0.9997172,0.00008060424,0.000056314744,0.000016416807,0.000099128454,0.00003031117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037968272,0.00026217758,0.00015699373,0.0004309864,0.00015118084,0.00030850066,0.000113652044,0.00013421816,0.0006615319],"category_scores_gemma":[0.0006669098,0.00010027252,0.00018788716,0.00030663575,0.00009085852,0.00021226794,0.00012745376,0.00014214477,0.00015127716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031427573,0.000053904347,0.94628376,0.000025262556,0.00008290718,0.000035395897,0.00004629148,0.016130773,0.01458555,0.000073743315,0.0009420039,0.021426063],"study_design_scores_gemma":[0.000018469058,0.0000906263,0.89673144,0.000012320963,0.00004765011,0.000048661528,0.000119880606,0.09679048,0.0054551237,0.000081295955,0.000590712,0.00001344841],"about_ca_topic_score_codex":0.04752976,"about_ca_topic_score_gemma":0.08755441,"teacher_disagreement_score":0.04752976,"about_ca_system_score_codex":0.00027860387,"about_ca_system_score_gemma":0.0003901885,"threshold_uncertainty_score":0.094506204},"labels":[],"label_agreement":null},{"id":"W2794985864","doi":"10.1002/2018gl077536","title":"Spatially Resolved Isotopic Source Signatures of Wetland Methane Emissions","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Natural Environment Research Council; Sight Research UK; Met Office; Department for Environment, Food and Rural Affairs, UK Government; Gordon and Betty Moore Foundation","keywords":"Wetland; Environmental science; Latitude; Atmospheric sciences; Ecosystem; Methane; Isotopic signature; Geology; Stable isotope ratio; Physics; Ecology; Geodesy","score_opus":0.01645671463367328,"score_gpt":0.27741381367673423,"score_spread":0.26095709904306097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2794985864","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99818784,0.000035150497,0.00075600087,0.000011903894,0.000002035621,0.000001653544,0.0005032926,0.00004233709,0.00045976267],"genre_scores_gemma":[0.99852633,0.000019334213,0.00092946604,0.0000034841182,0.0000022936954,0.0000023406571,0.00042736906,0.000007311336,0.00008196562],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997234,0.0000032531516,0.000001065707,0.000010380314,0.0000055940004,0.0000073499077],"domain_scores_gemma":[0.9999269,0.000012776072,0.00001966634,0.000011061979,0.000022684617,0.0000068736044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093431576,0.00012789825,0.00011834522,0.00069045136,0.000115930954,0.00020774617,0.00013529883,0.00013702067,0.00043950303],"category_scores_gemma":[0.00018094234,0.00013474315,0.00015267717,0.0005115209,0.000096519274,0.00016865855,0.00017943572,0.00009004018,0.00007805809],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007543283,0.00012828705,0.47193098,0.00010266645,0.00027372706,0.00037245697,0.00035067665,0.03362017,0.44068068,0.00046388,0.0011090991,0.050213136],"study_design_scores_gemma":[0.000015032506,0.00002212366,0.95666564,0.000006440999,0.000047320405,0.0000692865,0.000086961285,0.024421612,0.01764735,0.00015987142,0.00083520066,0.000023085999],"about_ca_topic_score_codex":0.011532068,"about_ca_topic_score_gemma":0.017597307,"teacher_disagreement_score":0.011532068,"about_ca_system_score_codex":0.00021941715,"about_ca_system_score_gemma":0.00015999094,"threshold_uncertainty_score":0.022929907},"labels":[],"label_agreement":null},{"id":"W2795017649","doi":"10.1002/2017gl075714","title":"Impact of Resolution on the Representation of Precipitation Variability Associated With the ITCZ","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Oceanic and Atmospheric Administration; George Mason University","keywords":"Intertropical Convergence Zone; Climatology; Precipitation; Decorrelation; Upwelling; Sea surface temperature; Convergence zone; Geology; Convection; Environmental science; Atmospheric sciences; Meteorology; Oceanography; Geography","score_opus":0.07572680178827022,"score_gpt":0.3658541444201482,"score_spread":0.29012734263187795,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795017649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9887727,0.00011965791,0.00779024,0.00013183274,0.000024976469,0.000016105501,0.0008377474,0.00022515874,0.0020815788],"genre_scores_gemma":[0.99626714,0.000030696767,0.003203766,0.000017124556,0.0000047859953,0.000007777659,0.00037453993,0.000025051844,0.00006920473],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995384,0.00019378457,0.000049426966,0.000082483806,0.00008356705,0.00005232979],"domain_scores_gemma":[0.9978016,0.0011912534,0.00020877877,0.00046561682,0.00024601465,0.00008681417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001158547,0.00030869574,0.0003184528,0.00033317425,0.00016374067,0.0011664656,0.0004151553,0.00028088957,0.00080499746],"category_scores_gemma":[0.005984507,0.0001834047,0.00035511365,0.0005609922,0.00027306168,0.00073307776,0.0006434559,0.00047813932,0.00014354497],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017038822,0.00026532458,0.28056386,0.00016042303,0.0005652021,0.00025823043,0.00027401722,0.5976603,0.048615135,0.004487497,0.0016422229,0.06380387],"study_design_scores_gemma":[0.0001370016,0.00016541472,0.10876685,0.00004234344,0.00012264944,0.00010339323,0.00022754048,0.87097985,0.016286263,0.0014712551,0.0016411345,0.000056324094],"about_ca_topic_score_codex":0.0093186945,"about_ca_topic_score_gemma":0.0057556685,"teacher_disagreement_score":0.0093186945,"about_ca_system_score_codex":0.0003571071,"about_ca_system_score_gemma":0.0003469503,"threshold_uncertainty_score":0.018528938},"labels":[],"label_agreement":null},{"id":"W2795265422","doi":"10.1002/2018gl077548","title":"Correlation Between Fracture Network Properties and Stress Variability in Geological Media","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Rock Mechanics and Modeling","field":"Engineering","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Geology; Stress (linguistics); Stress field; Fracture (geology); Finite element method; Geotechnical engineering; Physics","score_opus":0.04691182691652661,"score_gpt":0.27346504710675007,"score_spread":0.22655322019022345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795265422","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99653375,0.00002255049,0.0031944274,0.000017026663,9.985932e-7,0.0000025118134,0.000054202912,0.000016061225,0.0001585573],"genre_scores_gemma":[0.99979216,0.000006216905,0.00015389241,0.0000010462592,0.0000013527738,0.0000012461563,0.000025106294,0.0000015588932,0.000017496306],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99978036,0.000050920946,0.000017101418,0.000062959436,0.000054701886,0.000034000434],"domain_scores_gemma":[0.99581593,0.0023551476,0.001102349,0.00028881902,0.00031659033,0.00012110047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006336944,0.00022114613,0.00024719918,0.0012198369,0.00021751705,0.00068224734,0.00024493216,0.0003584529,0.00041295477],"category_scores_gemma":[0.00443646,0.00017823833,0.0001556724,0.00059515657,0.00087864336,0.00076670875,0.0003818508,0.00021029153,0.00004134691],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002928085,0.00013898681,0.37978882,0.000055353772,0.00018357049,0.00045646704,0.00018884602,0.5454427,0.058729775,0.0048594465,0.00016939513,0.0096939085],"study_design_scores_gemma":[0.0000076415445,0.000084448264,0.17492266,0.0000078470575,0.000021200476,0.00017723066,0.00011649326,0.8116983,0.009159336,0.003668232,0.000102712336,0.000033957902],"about_ca_topic_score_codex":0.0011482965,"about_ca_topic_score_gemma":0.0010413537,"teacher_disagreement_score":0.0012198369,"about_ca_system_score_codex":0.00034619455,"about_ca_system_score_gemma":0.0001256151,"threshold_uncertainty_score":0.0033513904},"labels":[],"label_agreement":null},{"id":"W2795673623","doi":"10.1002/2016gl069649","title":"Saturation of superstorms and finite compressibility of the magnetosphere: Results of the magnetogram inversion technique and global PPMLR‐MHD model","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cascades (Canada)","funders":"Siberian Branch, Russian Academy of Sciences; Russian Foundation for Basic Research; National Natural Science Foundation of China","keywords":"Magnetosphere; Magnetogram; Physics; Magnetohydrodynamics; Solar wind; Interplanetary spaceflight; Poynting vector; Geophysics; Saturation (graph theory); Interplanetary magnetic field; Magnetopause; Computational physics; Magnetic field; Magnetic flux; Mathematics","score_opus":0.014654294809934004,"score_gpt":0.2636019725532754,"score_spread":0.2489476777433414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795673623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98218256,0.00016919509,0.014370523,0.000057846668,0.0000058961127,0.000007806626,0.00010845878,0.00010805799,0.002989662],"genre_scores_gemma":[0.99918514,0.000030544557,0.00057345437,0.000002430998,0.0000020757109,0.0000029671746,0.000041546777,0.000009983023,0.00015192702],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997246,0.0000064448423,0.000001303057,0.000004631853,0.000005812338,0.000009324318],"domain_scores_gemma":[0.99980825,0.00009951354,0.000033522094,0.000018040802,0.000020034242,0.000020724377],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011116026,0.00026885813,0.0002764403,0.00024352103,0.00017142012,0.00025111903,0.0002684209,0.00015760855,0.00072451367],"category_scores_gemma":[0.0007639301,0.000121623736,0.0003136816,0.00014024483,0.00040428757,0.0003085342,0.00041613393,0.00025667073,0.00008260801],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056003087,0.000057334517,0.032150023,0.00023560635,0.00016357434,0.0013142909,0.00036720996,0.81397307,0.12481772,0.011584196,0.00046631158,0.014310508],"study_design_scores_gemma":[0.000014406642,0.00002774814,0.006442014,0.000004979434,0.000012396263,0.000052978838,0.000042322765,0.98567295,0.006710931,0.00085539196,0.0001556097,0.000008340946],"about_ca_topic_score_codex":0.004827341,"about_ca_topic_score_gemma":0.0016352088,"teacher_disagreement_score":0.004827341,"about_ca_system_score_codex":0.00018296383,"about_ca_system_score_gemma":0.00022419522,"threshold_uncertainty_score":0.009598494},"labels":[],"label_agreement":null},{"id":"W2795764127","doi":"10.1002/2017gl076674","title":"The Global Statistical Response of the Outer Radiation Belt During Geomagnetic Storms","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science and Technology Facilities Council; Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Van Allen radiation belt; Geomagnetic storm; Adiabatic process; Physics; Storm; Radiation; Adiabatic invariant; Population; Earth's magnetic field; Van Allen Probes; Acceleration; Atmospheric sciences; Phase space; Electron; Computational physics; Meteorology; Nuclear physics; Magnetosphere; Magnetic field; Classical mechanics; Quantum mechanics","score_opus":0.009011281834482077,"score_gpt":0.28570028608506126,"score_spread":0.2766890042505792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2795764127","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989266,0.000020031068,0.00038883675,0.0000069726157,9.770592e-7,0.0000017147104,0.000117018666,0.000014465339,0.0005234062],"genre_scores_gemma":[0.99966407,0.000011538592,0.00004967476,0.0000015971428,0.000001798832,0.0000015324487,0.0001609496,0.0000034038344,0.00010545453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999678,0.0000047717294,0.0000014700379,0.000010527998,0.000006455836,0.000009064024],"domain_scores_gemma":[0.9997739,0.00004936911,0.00008396807,0.00002333035,0.000042774125,0.00002652322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000103449864,0.00007770791,0.00010999565,0.0004131867,0.00009694044,0.00020083998,0.00011410857,0.00008802246,0.00079263054],"category_scores_gemma":[0.00041922508,0.00005953035,0.00009174256,0.00023177103,0.00012986975,0.00015923225,0.00019306382,0.00008103585,0.0001289942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064954575,0.000040194303,0.77992535,0.00004680803,0.00012165569,0.00019805266,0.00043345045,0.011692314,0.1818273,0.00086994126,0.0003705593,0.023824766],"study_design_scores_gemma":[0.000003269344,0.00006990558,0.9906798,0.0000014638712,0.000010758889,0.00006446192,0.00006850898,0.0053186696,0.0033894347,0.00011393446,0.00027583173,0.000003954473],"about_ca_topic_score_codex":0.0012788799,"about_ca_topic_score_gemma":0.001000441,"teacher_disagreement_score":0.0012788799,"about_ca_system_score_codex":0.00010489268,"about_ca_system_score_gemma":0.00004977179,"threshold_uncertainty_score":0.0026515722},"labels":[],"label_agreement":null},{"id":"W2799368995","doi":"10.1029/2018gl077722","title":"High‐Latitude Observations of a Localized Wind Wall and Its Coupling to the Lower Thermosphere","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Thermosphere; Geology; Latitude; Longitude; Atmospheric sciences; Atmosphere (unit); Global wind patterns; Divergence (linguistics); Ionosphere; Geophysics; Geodesy; Climatology; Meteorology; Physics","score_opus":0.027270031882827728,"score_gpt":0.29173990437825903,"score_spread":0.2644698724954313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799368995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817586,0.000042782634,0.00019464985,0.000024053625,0.000004156928,0.0000016246892,0.00014741307,0.000021969625,0.0013874635],"genre_scores_gemma":[0.9993395,0.000023859853,0.00014683174,0.000009655213,0.000006983366,0.0000017455166,0.00020764772,0.0000030533154,0.0002605671],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996936,0.0000027327508,0.0000011615685,0.000007858168,0.0000059070385,0.000012933153],"domain_scores_gemma":[0.99988806,0.000011758945,0.00004300661,0.000009308871,0.000014627797,0.00003321855],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007356973,0.00009227653,0.00011513311,0.00027964305,0.00026924827,0.0003656524,0.00007970143,0.00015160712,0.0009078585],"category_scores_gemma":[0.00013973398,0.000103073224,0.000061364895,0.00021934228,0.0001821652,0.000107997854,0.00020880662,0.000240829,0.00022558599],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004670243,0.00007783203,0.60083926,0.000048159767,0.00004632602,0.0006933847,0.0007089101,0.00062251557,0.37484196,0.00071079715,0.0010849654,0.019858837],"study_design_scores_gemma":[0.000009619991,0.00005309673,0.99273103,0.0000049741784,0.0000068982877,0.000114762785,0.00009808321,0.00039590272,0.005278308,0.0000623119,0.0012407616,0.000004355611],"about_ca_topic_score_codex":0.0031087585,"about_ca_topic_score_gemma":0.005993318,"teacher_disagreement_score":0.0031087585,"about_ca_system_score_codex":0.00008926401,"about_ca_system_score_gemma":0.00008205732,"threshold_uncertainty_score":0.0061813593},"labels":[],"label_agreement":null},{"id":"W2799536474","doi":"10.1002/2017gl075839","title":"Seafloor Displacement After the 2011 Tohoku‐oki Earthquake in the Northern Japan Trench Examined by Repeated Bathymetric Surveys","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Japan Agency for Marine-Earth Science and Technology; Bundesministerium für Bildung und Forschung; Ministry of Education, Culture, Sports, Science and Technology; Ministry of Education","keywords":"Trench; Geology; Bathymetry; Seafloor spreading; Seismology; Submarine pipeline; Slip (aerodynamics); Displacement (psychology); Submarine landslide; Vertical displacement; Landslide; Geomorphology; Oceanography","score_opus":0.03984361399257743,"score_gpt":0.2843468162861515,"score_spread":0.24450320229357406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799536474","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978656,0.000013168031,0.000010970785,0.000004785428,9.011864e-7,0.0000014465667,0.00003413385,7.894628e-7,0.00014728164],"genre_scores_gemma":[0.99954283,0.000035205027,0.000037113598,0.000008147389,0.0000020155242,0.000003762311,0.00010076868,0.0000010221498,0.00026916736],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999051,0.000010421156,0.0000056935355,0.00001924699,0.000019750923,0.00003975883],"domain_scores_gemma":[0.9996675,0.00001813418,0.00012785879,0.000017759825,0.000082635015,0.000086129716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015277984,0.00023109428,0.00025624136,0.00057328155,0.0006237449,0.00040669812,0.0002045038,0.00031167277,0.0006095875],"category_scores_gemma":[0.0003584643,0.0001826461,0.00015877528,0.0006910402,0.00036201102,0.00025264325,0.0005302706,0.00021254335,0.00015782224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006990902,0.000026734146,0.98956513,0.000016871936,0.000027872245,0.0005508026,0.001614738,0.0002607925,0.004859894,0.000011469322,0.000107506545,0.0028882502],"study_design_scores_gemma":[7.738217e-7,0.000012247258,0.99924684,0.0000014027771,0.0000046364835,0.000021713164,0.00053598185,0.000054917833,0.000058720274,0.0000012895435,0.000059896876,0.000001611822],"about_ca_topic_score_codex":0.096893586,"about_ca_topic_score_gemma":0.23355068,"teacher_disagreement_score":0.096893586,"about_ca_system_score_codex":0.000739697,"about_ca_system_score_gemma":0.0005555257,"threshold_uncertainty_score":0.1926592},"labels":[],"label_agreement":null},{"id":"W2799895525","doi":"10.1029/2018gl077096","title":"Mechanisms and Early Detections of Multidecadal Oxygen Changes in the Interior Subpolar North Atlantic","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Norges Forskningsråd","keywords":"Ocean gyre; Oxygen; Isotopes of oxygen; Oceanography; Oxygen minimum zone; Water mass; Geology; Climate change; Salinity; Climatology; Environmental science; Atmospheric sciences; Chemistry; Ecology","score_opus":0.0257631263076519,"score_gpt":0.256529784336206,"score_spread":0.2307666580285541,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2799895525","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895096,0.00008749224,0.00027368002,0.000052072144,0.00000421229,0.0000014385068,0.00018493603,0.000019230221,0.0004259666],"genre_scores_gemma":[0.9997271,0.000030314244,0.00006376116,0.000005464081,0.0000018962544,0.0000010241464,0.00011661603,0.0000025769734,0.00005118821],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.000009506621,0.0000045286706,0.000022452836,0.000007822304,0.0000105475065],"domain_scores_gemma":[0.9995932,0.00007773695,0.00015815685,0.00004803341,0.000057510126,0.00006537635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036720218,0.00015265927,0.0001801154,0.00035126763,0.0001761803,0.00063778,0.0001914899,0.00034403196,0.0006727505],"category_scores_gemma":[0.0008000729,0.00017304662,0.00020954116,0.00025231348,0.000223515,0.00036387544,0.0005801423,0.00024252033,0.00009822559],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002071934,0.00003187666,0.9737168,0.000021781323,0.000082867904,0.000066736386,0.00015602236,0.0064717904,0.0139579335,0.0005163034,0.00020469283,0.0045660622],"study_design_scores_gemma":[0.000008966712,0.000030865358,0.98479015,0.000008982785,0.000021074178,0.000021360958,0.00011355582,0.013332992,0.0009052415,0.0003127117,0.00044587385,0.000008249557],"about_ca_topic_score_codex":0.00916633,"about_ca_topic_score_gemma":0.0102586625,"teacher_disagreement_score":0.00916633,"about_ca_system_score_codex":0.00029266102,"about_ca_system_score_gemma":0.00013136883,"threshold_uncertainty_score":0.018225968},"labels":[],"label_agreement":null},{"id":"W2800495075","doi":"10.1029/2018gl077676","title":"Using Vertically Integrated Ocean Fields to Characterize Greenland Icebergs' Distribution and Lifetime","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; University of Alberta","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Polar Knowledge Canada","keywords":"Iceberg; Oceanography; Geology; Buoyancy; Keel; Water mass; Climatology; Ocean current; Sea ice","score_opus":0.033409596847639195,"score_gpt":0.28452770317356607,"score_spread":0.2511181063259269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800495075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99764377,0.00002426587,0.0013888204,0.000032018153,0.000004537806,0.000004152094,0.00042938674,0.00005039954,0.00042269062],"genre_scores_gemma":[0.99878305,0.000016024584,0.0006402072,0.000009680604,0.0000014354449,0.000002524024,0.0004410269,0.0000072147286,0.00009883863],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.000013088891,0.000005111459,0.00002306972,0.0000062697954,0.000016194468],"domain_scores_gemma":[0.99977463,0.000063302374,0.000050254843,0.000031919684,0.00005031268,0.000029557898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029813833,0.000398885,0.0001899953,0.00044641836,0.00018039814,0.00074066967,0.00038318767,0.00033719142,0.00037737624],"category_scores_gemma":[0.00088033656,0.00018096046,0.00032868484,0.00047876895,0.0002666713,0.00067687355,0.00031026185,0.0002270687,0.000050744788],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099151686,0.00006918603,0.1955729,0.000011726183,0.00010160518,0.00006228772,0.00005439737,0.7931887,0.0037439072,0.000557275,0.0002650599,0.006273887],"study_design_scores_gemma":[0.000020590725,0.00002555426,0.07984466,0.0000068609925,0.000021098045,0.000009384056,0.00005432471,0.9185119,0.0009051973,0.00037735607,0.00020801507,0.000015015985],"about_ca_topic_score_codex":0.13516937,"about_ca_topic_score_gemma":0.07195198,"teacher_disagreement_score":0.13516937,"about_ca_system_score_codex":0.001483839,"about_ca_system_score_gemma":0.00073292933,"threshold_uncertainty_score":0.2687652},"labels":[],"label_agreement":null},{"id":"W2800579668","doi":"10.1029/2018gl077560","title":"Changes in the Shadow: The Shifting Role of Shaded Leaves in Global Carbon and Water Cycles Under Climate Change","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":75,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Space Agency","keywords":"Environmental science; Deciduous; Evergreen; Climate change; Transpiration; Primary production; Atmospheric sciences; Boreal; Canopy; Global warming; Global change; Leaf area index; Ecosystem; Taiga; Climatology; Agronomy; Ecology; Forestry; Geography; Botany; Biology; Photosynthesis; Geology","score_opus":0.028419359312178982,"score_gpt":0.2829012196813239,"score_spread":0.25448186036914494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800579668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9965287,0.00043209209,0.0006373018,0.00041187363,0.000013434635,0.0000019517313,0.0002724722,0.000020057427,0.0016821288],"genre_scores_gemma":[0.99973637,0.00005260859,0.00006109651,0.000025273119,0.000004985327,3.7453512e-7,0.000033559474,0.0000030508365,0.00008273967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995005,0.00000956903,0.000002298491,0.000017813347,0.000007584424,0.000012696107],"domain_scores_gemma":[0.9998442,0.000018251802,0.000045283803,0.000014933783,0.000035959798,0.000041330743],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018271123,0.00009225524,0.00012453148,0.00029122233,0.00018636681,0.00046528847,0.00012405112,0.00022476263,0.0017269966],"category_scores_gemma":[0.00030410464,0.00008817796,0.0001299484,0.00034853866,0.00045052596,0.0006003881,0.0003929111,0.00017671903,0.00014655896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004925117,0.00005979334,0.7685721,0.00013687745,0.00014761894,0.0004221647,0.001534815,0.005344253,0.13797005,0.00463143,0.0030921474,0.07759619],"study_design_scores_gemma":[0.0000030692015,0.000017094602,0.9929182,0.0000067745323,0.000012934904,0.000041682288,0.00049907033,0.0023572033,0.0012024167,0.0012292084,0.001704253,0.000008143624],"about_ca_topic_score_codex":0.0050410284,"about_ca_topic_score_gemma":0.006813883,"teacher_disagreement_score":0.0050410284,"about_ca_system_score_codex":0.00031956777,"about_ca_system_score_gemma":0.00015767798,"threshold_uncertainty_score":0.0100233555},"labels":[],"label_agreement":null},{"id":"W2800844271","doi":"10.1029/2018gl077212","title":"Electron Scattering by Plasmaspheric Hiss in a Nightside Plume","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Hiss; Electron; Plume; Physics; Van Allen radiation belt; Plasmasphere; Scattering; Van Allen Probes; Atomic physics; Pitch angle; Geophysics; Magnetosphere; Plasma; Nuclear physics; Meteorology; Optics","score_opus":0.0112765664067634,"score_gpt":0.2810304921961578,"score_spread":0.2697539257893944,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2800844271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865925,0.000065176384,0.00031263102,0.000022685434,0.0000032854593,0.0000025792046,0.00008385639,0.00002483494,0.00082568795],"genre_scores_gemma":[0.9992975,0.00003233081,0.00020538576,0.000008438051,0.0000038595535,0.0000014035294,0.0001595895,0.0000051336474,0.00028637625],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999589,0.0000032366233,0.0000013126331,0.00000899074,0.000014865412,0.000012653826],"domain_scores_gemma":[0.9999157,0.000010837281,0.0000160603,0.0000075267367,0.000023891535,0.000026035346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008798973,0.00016817742,0.00014002889,0.00043615786,0.00021461747,0.00024420998,0.00018040261,0.00019594505,0.0012424126],"category_scores_gemma":[0.00014551458,0.000103957755,0.00016464591,0.00022132773,0.00013755032,0.00023990979,0.00036356843,0.00019209467,0.00014250196],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004754272,0.00007469771,0.18825595,0.000042621185,0.00006765388,0.00085012935,0.00049626495,0.0019078269,0.79000276,0.0004708936,0.0006236346,0.016732134],"study_design_scores_gemma":[0.000023573939,0.00023507989,0.92079,0.000011769799,0.000023354685,0.00065078033,0.0005979657,0.013628934,0.060656104,0.00038106542,0.0029706259,0.000030620064],"about_ca_topic_score_codex":0.0026650678,"about_ca_topic_score_gemma":0.0031611295,"teacher_disagreement_score":0.0026650678,"about_ca_system_score_codex":0.00021620777,"about_ca_system_score_gemma":0.000077861085,"threshold_uncertainty_score":0.0052990317},"labels":[],"label_agreement":null},{"id":"W2801266318","doi":"10.1029/2018gl078303","title":"Appreciation of 2017 <i>GRL</i> Peer Reviewers","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Environmental Monitoring and Data Management","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Computer science; Information retrieval","score_opus":0.05820436561593725,"score_gpt":0.3173230790808565,"score_spread":0.25911871346491927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801266318","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006350379,0.0027968409,0.0021764417,0.25657272,0.6951781,0.0002524246,0.0030616694,0.0016060476,0.03772075],"genre_scores_gemma":[0.012242685,0.0040990384,0.0038883935,0.10579471,0.29438612,0.00056423276,0.0037392478,0.005123383,0.5701621],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9841287,0.0024662532,0.0012963152,0.0019793017,0.009217143,0.0009122588],"domain_scores_gemma":[0.6020826,0.009630074,0.0076508983,0.007166267,0.35654473,0.016925426],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.011722643,0.0013496547,0.0021617983,0.0040785237,0.0037331406,0.00994043,0.0021972354,0.003251666,0.14070366],"category_scores_gemma":[0.12666823,0.0005474104,0.00095740426,0.0029251736,0.0016391245,0.004669329,0.0038960106,0.00803833,0.2153947],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000007627743,0.0000015255501,0.000039970215,0.000023682967,0.0000014848739,0.000028358752,0.000030001527,0.000007007559,0.00006903824,0.00013729015,0.9966227,0.003031349],"study_design_scores_gemma":[0.000005619764,0.000005139806,0.0002488975,0.00006235411,0.0000034416119,0.00008733842,0.00022919347,0.00005996045,0.00014342669,0.00036758435,0.9987727,0.000014338848],"about_ca_topic_score_codex":0.00609281,"about_ca_topic_score_gemma":0.014275377,"teacher_disagreement_score":0.9882774,"about_ca_system_score_codex":0.0031289253,"about_ca_system_score_gemma":0.007913687,"threshold_uncertainty_score":0.47070062},"labels":[{"model":"gemma","categories":[],"domain":null,"study_design":"not_applicable","genre":"other","about_ca_system":false,"about_ca_topic":false,"confidence":"low"},{"model":"gpt","categories":[],"domain":null,"study_design":"not_applicable","genre":"editorial","about_ca_system":false,"about_ca_topic":false,"confidence":"high"}],"label_agreement":"agree"},{"id":"W2801962875","doi":"10.1029/2017gl076752","title":"Assessment of the Barren Ground Caribou Die‐off During Winter 2015–2016 Using Passive Microwave Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Center for Northern Studies; Université de Sherbrooke","funders":"Natural Sciences and Engineering Research Council of Canada; Ministry of Education and Science of the Russian Federation; Polar Knowledge Canada; Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Snow; Winter storm; Environmental science; Arctic; Storm; Climatology; Spring (device); Atmospheric sciences; Physical geography; Oceanography; Geology; Geography; Meteorology","score_opus":0.10325057728210416,"score_gpt":0.3472499472840318,"score_spread":0.24399937000192765,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2801962875","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99892396,0.000121326884,0.00022746187,0.000016135855,0.000004007051,0.000003318593,0.0002834791,0.0000068025147,0.0004134941],"genre_scores_gemma":[0.9988336,0.00009596092,0.00021151031,0.000008187781,0.000003799898,0.000004749021,0.0005375735,0.0000017578502,0.00030285984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998872,0.000018541898,0.000006856624,0.000025984547,0.00003640701,0.000024905468],"domain_scores_gemma":[0.9997831,0.000032316955,0.000060048587,0.0000115756675,0.00007985649,0.000033067143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034309877,0.00020426039,0.00013458278,0.00063318096,0.00027409877,0.00042368134,0.00016635652,0.00019005238,0.00046709063],"category_scores_gemma":[0.0004682841,0.00009480336,0.00015677174,0.00047838755,0.00015826017,0.00016627026,0.00032332243,0.00013310005,0.00010870974],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062462874,0.000017585127,0.9890132,0.000028232385,0.000072311515,0.00014023154,0.00069343497,0.00053996965,0.0032264886,0.000047501173,0.00019613202,0.0059623593],"study_design_scores_gemma":[9.1977125e-7,0.00001595011,0.9967823,0.00001412091,0.000019720133,0.000039016424,0.00071649044,0.0014962165,0.0002886084,0.000013529507,0.0006101368,0.0000028111708],"about_ca_topic_score_codex":0.1164332,"about_ca_topic_score_gemma":0.27089736,"teacher_disagreement_score":0.1164332,"about_ca_system_score_codex":0.00035795156,"about_ca_system_score_gemma":0.0003339782,"threshold_uncertainty_score":0.231511},"labels":[],"label_agreement":null},{"id":"W2802226397","doi":"10.1029/2018gl078409","title":"The Persistence of Brines in Sedimentary Basins","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; W. M. Keck Foundation; National Science Foundation","keywords":"Geology; Evaporite; Sedimentary basin; Sedimentary rock; Paleozoic; Geochemistry; Diagenesis; Crust; Geomorphology","score_opus":0.05529572189503713,"score_gpt":0.29479313721071054,"score_spread":0.23949741531567342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802226397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936026,0.00006449524,0.00003239318,0.000011636115,6.201636e-7,9.224015e-7,0.00010141011,0.0000033389033,0.0004250011],"genre_scores_gemma":[0.99982786,0.000022164964,0.00002071844,0.0000025848467,7.986425e-7,6.7586006e-7,0.00006046584,7.0708444e-7,0.00006403329],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982846,0.000018387438,0.000017912738,0.000054627046,0.000031142,0.00004949896],"domain_scores_gemma":[0.9989349,0.00013416163,0.00053023704,0.00007326352,0.00019793287,0.00012942261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023781843,0.00010452095,0.00021272746,0.0015067662,0.00066981727,0.000895082,0.0002973455,0.00024131467,0.0015869378],"category_scores_gemma":[0.0011482527,0.00015185091,0.00010786385,0.0012074456,0.00078001583,0.0005203305,0.0009380106,0.00020917607,0.00019803157],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008270813,0.000010514377,0.98663074,0.00002654761,0.000035190333,0.0001726986,0.0006386593,0.00017376815,0.008300276,0.00024881694,0.00008884566,0.00359121],"study_design_scores_gemma":[0.0000014960441,0.000017598606,0.9984584,0.000005842299,0.0000064532073,0.00007692762,0.0005038927,0.00014792566,0.00039813857,0.00006864056,0.00031188267,0.000002861355],"about_ca_topic_score_codex":0.010888499,"about_ca_topic_score_gemma":0.019232046,"teacher_disagreement_score":0.010888499,"about_ca_system_score_codex":0.0005089527,"about_ca_system_score_gemma":0.000249693,"threshold_uncertainty_score":0.021650195},"labels":[],"label_agreement":null},{"id":"W2802307607","doi":"10.1002/2017gl074609","title":"Changes in Fe Oxidation Rate in Hydrothermal Plumes as a Potential Driver of Enhanced Hydrothermal Input to Near‐Ridge Sediments During Glacial Terminations","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Interglacial; Hydrothermal circulation; Glacial period; Geology; Oceanography; Ridge; Hydrothermal vent; Mid-ocean ridge; Deep sea; Seawater; Geochemistry; Earth science; Paleontology","score_opus":0.020995688750476367,"score_gpt":0.30397388535999254,"score_spread":0.2829781966095162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802307607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99942756,0.000038595605,0.00023605344,0.000032652242,0.0000018028024,0.0000014707043,0.00005077067,0.000015396845,0.00019570338],"genre_scores_gemma":[0.9998317,0.000012330803,0.00006989687,0.0000036488907,0.0000010754721,4.5738264e-7,0.000030406687,0.0000021226324,0.000048215894],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994826,0.00001046971,0.0000034669692,0.000017583601,0.0000070571273,0.000013185544],"domain_scores_gemma":[0.9998592,0.000035426703,0.00003625707,0.0000123602695,0.000025544412,0.000031257932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003086666,0.00019689475,0.0002960669,0.00040779446,0.00019850532,0.000558522,0.00020955096,0.00031664997,0.0008252127],"category_scores_gemma":[0.00049814995,0.0002154361,0.00029698765,0.00023137892,0.00033480834,0.00033898733,0.0003239679,0.00019968723,0.00008995281],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004734323,0.000090367044,0.8304743,0.00006658248,0.00015721757,0.0003289015,0.00024318745,0.013863403,0.14621602,0.0008828228,0.00015368756,0.007050116],"study_design_scores_gemma":[0.000018149034,0.00012307646,0.96914256,0.0000057695584,0.00003430203,0.00007192843,0.00018628316,0.024442242,0.005164096,0.0006065805,0.0001909089,0.000014224652],"about_ca_topic_score_codex":0.00822051,"about_ca_topic_score_gemma":0.0067561576,"teacher_disagreement_score":0.00822051,"about_ca_system_score_codex":0.0004646608,"about_ca_system_score_gemma":0.00020409978,"threshold_uncertainty_score":0.016345322},"labels":[],"label_agreement":null},{"id":"W2802464737","doi":"10.1029/2018gl077509","title":"Predicting the Dominant Patterns of Subseasonal Variability of Wintertime Surface Air Temperature in Extratropical Northern Hemisphere","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Oceanic and Atmospheric Administration","keywords":"Extratropical cyclone; Climatology; Northern Hemisphere; Madden–Julian oscillation; Environmental science; Mode (computer interface); Surface air temperature; Boreal; Atmospheric sciences; Meteorology; Geology; Geography; Convection; Precipitation","score_opus":0.01923039332332936,"score_gpt":0.281289731969585,"score_spread":0.26205933864625564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802464737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998953,0.00003875842,0.00045366125,0.00003126599,0.0000057025186,0.000001780437,0.00012070189,0.000031658656,0.00036348737],"genre_scores_gemma":[0.99952054,0.00001921729,0.00022700227,0.000002556869,0.0000022420486,9.2003665e-7,0.00015033281,0.0000019715264,0.000075230986],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999629,0.000006607267,0.000002085447,0.000012205307,0.000006441604,0.000009782794],"domain_scores_gemma":[0.9998894,0.000023866789,0.000023781904,0.000013508819,0.000022741338,0.00002662812],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022765051,0.00029482247,0.00014106267,0.00016582741,0.00013118194,0.0004010396,0.00015188451,0.00017750564,0.00046872176],"category_scores_gemma":[0.00040751934,0.00007345805,0.00022917347,0.00018375355,0.0001267275,0.00024361323,0.00019120637,0.00015980446,0.0000706058],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040602154,0.00014233116,0.6973567,0.0000324589,0.00013768226,0.00018218256,0.0001482738,0.2505355,0.016795283,0.00044486485,0.0015110952,0.032307588],"study_design_scores_gemma":[0.000028262852,0.00006855804,0.6113074,0.0000063319135,0.000026069984,0.000030892566,0.00017122901,0.38594735,0.0015536826,0.0003001445,0.00054795167,0.000012120129],"about_ca_topic_score_codex":0.043790996,"about_ca_topic_score_gemma":0.053387307,"teacher_disagreement_score":0.043790996,"about_ca_system_score_codex":0.00025520806,"about_ca_system_score_gemma":0.00032594876,"threshold_uncertainty_score":0.08707219},"labels":[],"label_agreement":null},{"id":"W2802853037","doi":"10.1002/2016gl071565","title":"The role of natural variability in projections of climate change impacts on U.S. ozone pollution","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Pacific Northwest National Laboratory; University of Waterloo; U.S. Environmental Protection Agency; U.S. Department of Energy; Office of Science; National Science Foundation","keywords":"Environmental science; Climate change; Air quality index; Climatology; Ozone; Pollutant; Air pollution; Atmospheric sciences; Pollution; Natural (archaeology); Ground Level Ozone; Climate model; Meteorology; Geography; Ecology; Oceanography; Geology","score_opus":0.0324117232827227,"score_gpt":0.3069991119501443,"score_spread":0.2745873886674216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2802853037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9888421,0.00016244892,0.0069485498,0.0005923068,0.000045933433,0.000016023088,0.0012046273,0.00008139532,0.0021064617],"genre_scores_gemma":[0.9982597,0.00005251395,0.0010485697,0.000038053848,0.000006560267,0.000011337038,0.00048058922,0.000009804515,0.0000927974],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994425,0.00032112104,0.000029832927,0.00008960951,0.000056833982,0.000060177448],"domain_scores_gemma":[0.99777764,0.0013394047,0.00019871086,0.0002518852,0.00029928942,0.00013300864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0025811545,0.00034836656,0.00036962715,0.00038663796,0.0005657463,0.0010170625,0.0005858098,0.00070118404,0.0006468694],"category_scores_gemma":[0.00627939,0.0002957106,0.0008691052,0.0003925199,0.00039742974,0.0009975401,0.00059967156,0.0008771678,0.000077567245],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000097025055,0.000066061184,0.057321344,0.00001544275,0.00015610107,0.000048475835,0.000022171387,0.9375866,0.0006851977,0.0011007616,0.00056653674,0.0023342457],"study_design_scores_gemma":[0.000032195967,0.00005692801,0.030136183,0.00001463716,0.00004359443,0.000015542042,0.000047644626,0.9671369,0.0006819375,0.0012863964,0.0005215956,0.000026562977],"about_ca_topic_score_codex":0.04070148,"about_ca_topic_score_gemma":0.027030027,"teacher_disagreement_score":0.04070148,"about_ca_system_score_codex":0.0009004939,"about_ca_system_score_gemma":0.0010242283,"threshold_uncertainty_score":0.08092916},"labels":[],"label_agreement":null},{"id":"W2803841719","doi":"10.1029/2018gl077406","title":"Recent Decline in Extratropical Lower Stratospheric Ozone Attributed to Circulation Changes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":175,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; Goddard Space Flight Center; National Oceanic and Atmospheric Administration","keywords":"Tropopause; Extratropical cyclone; Stratosphere; Climatology; Ozone layer; Environmental science; Ozone; Atmospheric sciences; Ozone depletion; Radiosonde; Meteorology; Geology; Geography","score_opus":0.05249210377738314,"score_gpt":0.3137934402466601,"score_spread":0.261301336469277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2803841719","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997528,0.00018557829,0.00009047555,0.000106312946,0.00001218121,0.0000026802468,0.0016502835,0.000018449859,0.00040611275],"genre_scores_gemma":[0.9970548,0.0002452863,0.000110008914,0.000020622727,0.000011804524,0.000003038072,0.0023149075,0.000005450447,0.0002339951],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.000009135643,0.000006664042,0.000022114677,0.00001736079,0.000015314212],"domain_scores_gemma":[0.99953246,0.000046351535,0.00020080632,0.000041790547,0.00012558159,0.000053074633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033349812,0.00018465793,0.00014996919,0.000440147,0.00015727272,0.00046195887,0.00023365123,0.00023520464,0.00072904467],"category_scores_gemma":[0.001096401,0.00010743087,0.0002645078,0.0008615387,0.00016549726,0.00040785235,0.00030931647,0.0002638489,0.00015035449],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014332685,0.000032096894,0.98576003,0.000050191684,0.0001034789,0.00010781603,0.00012451621,0.0023586876,0.002776567,0.00014235992,0.0007358977,0.0076650055],"study_design_scores_gemma":[0.0000025722986,0.000012040524,0.997687,0.0000026937953,0.000014752977,0.000016254515,0.000042646752,0.0013561923,0.00020224719,0.00001623617,0.0006457003,0.0000016589044],"about_ca_topic_score_codex":0.058540486,"about_ca_topic_score_gemma":0.075070664,"teacher_disagreement_score":0.058540486,"about_ca_system_score_codex":0.0006644593,"about_ca_system_score_gemma":0.00035206566,"threshold_uncertainty_score":0.11639953},"labels":[],"label_agreement":null},{"id":"W2804276086","doi":"10.1029/2018gl077879","title":"Numerical Modeling of Dynamically Triggered Shallow Slow Slip Events in New Zealand by the 2016 <i>M</i><sub><i>w</i></sub> 7.8 Kaikoura Earthquake","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Royal Society Te Apārangi; National Science Foundation","keywords":"Subduction; Perturbation (astronomy); Slip (aerodynamics); Amplitude; Geology; Dynamic stress; Seismology; Geotechnical engineering; Physics; Dynamic loading; Tectonics; Structural engineering; Engineering","score_opus":0.025754102777399132,"score_gpt":0.2636020691499413,"score_spread":0.23784796637254213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804276086","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99496955,0.000054703356,0.0010695464,0.00016713432,0.000017360064,0.000026825654,0.0002489202,0.00002810211,0.0034179755],"genre_scores_gemma":[0.998659,0.000043916916,0.00060691324,0.000016306047,0.0000035367289,0.000015853453,0.00013409184,0.00000859642,0.0005117789],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999107,0.000016231967,0.000006976577,0.000019967127,0.000014242222,0.000031861735],"domain_scores_gemma":[0.99958915,0.00014163907,0.00008983942,0.000021598791,0.00008340838,0.00007433161],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002699783,0.0006100746,0.0004718202,0.00036319724,0.0005185419,0.0009912552,0.001241665,0.0012943797,0.0023398064],"category_scores_gemma":[0.0014282056,0.0004931072,0.00059928105,0.00033443444,0.0010914251,0.00062548765,0.00068796624,0.0006874828,0.0001567278],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015563439,0.00013001633,0.021046983,0.00002529381,0.000048195863,0.00027459432,0.00007128364,0.9743367,0.0017720953,0.000540255,0.00025661266,0.0013424191],"study_design_scores_gemma":[0.000074143034,0.00005465479,0.007362136,0.0000058796486,0.00002123401,0.000015103981,0.00009397296,0.9918731,0.00018073402,0.00014253876,0.0001644408,0.000012080938],"about_ca_topic_score_codex":0.25651395,"about_ca_topic_score_gemma":0.13072814,"teacher_disagreement_score":0.25651395,"about_ca_system_score_codex":0.001789699,"about_ca_system_score_gemma":0.0012455472,"threshold_uncertainty_score":0.5100417},"labels":[],"label_agreement":null},{"id":"W2804375516","doi":"10.1029/2018gl077823","title":"Reevaluating the Use of O<sub>2</sub> <i>a</i><sup>1</sup>Δ<sub><i>g</i></sub> Band in Spaceborne Remote Sensing of Greenhouse Gases","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"School of Engineering and Applied Science, University of Pennsylvania; Australian Renewable Energy Agency; Smithsonian Institution","keywords":"Airglow; Remote sensing; Nadir; SCIAMACHY; Spectrometer; Stratosphere; Spectral resolution; Mesosphere; Environmental science; Absorption (acoustics); Atmosphere (unit); Spectroscopy; Spectral bands; Imaging spectrometer; Atmospheric sciences; Physics; Satellite; Spectral line; Optics; Geology; Meteorology; Astronomy","score_opus":0.06143028961921862,"score_gpt":0.28618766674008156,"score_spread":0.22475737712086294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804375516","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9799136,0.0014449892,0.014337641,0.0009783031,0.00006519704,0.000023780236,0.00016894448,0.000116449744,0.0029511955],"genre_scores_gemma":[0.9824576,0.0005119089,0.016266888,0.00022162877,0.000014116947,0.000011112688,0.00009278463,0.00003904868,0.0003847916],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998418,0.000049489234,0.000008629129,0.00003990012,0.00003962463,0.000020618714],"domain_scores_gemma":[0.9995116,0.00017712124,0.000039072358,0.000068394715,0.00017980227,0.00002398235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010279758,0.0003392486,0.00022067051,0.00021046706,0.00031966987,0.0010824966,0.0008496884,0.0006401107,0.00062423345],"category_scores_gemma":[0.0012535302,0.00020217359,0.00029864698,0.00024666096,0.00031274938,0.0011101945,0.0003203337,0.00034279047,0.00018172835],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066505047,0.00039918005,0.17703786,0.00046317402,0.0003234142,0.0003238497,0.00043281025,0.022383839,0.5885151,0.0027484517,0.0018612586,0.20484602],"study_design_scores_gemma":[0.00014297137,0.0009696973,0.27770606,0.00022806338,0.0007515028,0.00039176832,0.002261853,0.3046222,0.37405568,0.0042244373,0.034500528,0.00014525969],"about_ca_topic_score_codex":0.014956911,"about_ca_topic_score_gemma":0.03208676,"teacher_disagreement_score":0.014956911,"about_ca_system_score_codex":0.0004811083,"about_ca_system_score_gemma":0.0006605633,"threshold_uncertainty_score":0.029739738},"labels":[],"label_agreement":null},{"id":"W2804791937","doi":"10.1029/2017gl076885","title":"Weakened Lithosphere Beneath Greenland Inferred From Effective Elastic Thickness: A Hot Spot Effect?","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Crust; Mantle (geology); Gravity anomaly; Isostasy; Geophysics; Tectonics; Seismology; Paleontology","score_opus":0.016112745065475206,"score_gpt":0.2598638949343245,"score_spread":0.24375114986884927,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804791937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983677,0.000111625406,0.00041474326,0.000032459175,0.0000024598173,0.0000016694287,0.00042267598,0.000048861144,0.0005978141],"genre_scores_gemma":[0.999483,0.000041453117,0.00017687025,0.000007584526,0.0000013209175,7.3629025e-7,0.00022999407,0.000007100718,0.000051897703],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992776,0.000008941722,0.0000049518626,0.000024000436,0.0000075566895,0.000026831727],"domain_scores_gemma":[0.99985707,0.000029150988,0.00003764562,0.000024732644,0.000024789437,0.000026564408],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024059012,0.00038770743,0.00033037155,0.0014317333,0.00021549629,0.0006957955,0.00031533136,0.00027828023,0.0012678371],"category_scores_gemma":[0.00042227775,0.00024963063,0.00025338627,0.0013703189,0.00046621144,0.00050579995,0.0006925512,0.00014526906,0.000194014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034438103,0.00003263416,0.91626966,0.00007803632,0.00028179222,0.00064876303,0.000278377,0.023979342,0.042235713,0.00046624662,0.00035275982,0.015032237],"study_design_scores_gemma":[0.000011372332,0.000012310573,0.9820002,0.000014173275,0.000048946116,0.000046490113,0.00017734997,0.015326042,0.0018271374,0.00024037364,0.00028447568,0.000011229341],"about_ca_topic_score_codex":0.03560546,"about_ca_topic_score_gemma":0.04211641,"teacher_disagreement_score":0.03560546,"about_ca_system_score_codex":0.0004578712,"about_ca_system_score_gemma":0.0003120819,"threshold_uncertainty_score":0.07079643},"labels":[],"label_agreement":null},{"id":"W2804937978","doi":"10.1029/2018gl077491","title":"A Statistical Survey of the 630.0‐nm Optical Signature of Periodic Auroral Arcs Resulting From Magnetospheric Field Line Resonances","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Calgary","funders":"Science and Technology Facilities Council; European Space Agency; Canadian Space Agency; University of Alberta; University of Calgary; National Science Foundation","keywords":"Physics; Sky; Line (geometry); Geophysics; Magnetic field; Satellite; Observatory; Field (mathematics); Airglow; Magnetosphere; Computational physics; Astrophysics; Optics; Geometry; Astronomy; Mathematics","score_opus":0.022499215206728287,"score_gpt":0.30301373189946273,"score_spread":0.2805145166927345,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2804937978","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925715,0.00003201505,0.00018070734,0.000007028696,9.4530986e-7,0.0000015411238,0.00017360548,0.000008764455,0.00033833244],"genre_scores_gemma":[0.9994716,0.000018392588,0.0000893296,0.0000033035678,0.0000041946173,0.0000020258635,0.00033252072,0.000002244459,0.00007642369],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998313,0.000027156191,0.00001181883,0.000058670295,0.000037414444,0.000033646822],"domain_scores_gemma":[0.99839646,0.00044344674,0.00068624853,0.00014586188,0.00018238458,0.0001455906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003366654,0.00009495736,0.00011838676,0.0011190546,0.000247607,0.00029679688,0.00012362884,0.00014357932,0.0007173232],"category_scores_gemma":[0.00088377314,0.000093903094,0.00012630453,0.00075810164,0.00025718243,0.00020122259,0.00023236049,0.00011622526,0.00014676034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008441101,0.00001897652,0.9859045,0.000007593942,0.000034059856,0.00008813316,0.0000740211,0.00018867318,0.007553462,0.00004769045,0.00019568586,0.0058027403],"study_design_scores_gemma":[9.869291e-7,0.000018136996,0.9987583,8.8126217e-7,0.000006953758,0.00009478587,0.00006700148,0.00047196285,0.00037733236,0.0000123956,0.00018972557,0.0000013826212],"about_ca_topic_score_codex":0.0018416782,"about_ca_topic_score_gemma":0.0025684054,"teacher_disagreement_score":0.0018416782,"about_ca_system_score_codex":0.00011367123,"about_ca_system_score_gemma":0.00008358893,"threshold_uncertainty_score":0.003661871},"labels":[],"label_agreement":null},{"id":"W2805020085","doi":"10.1029/2018gl077219","title":"Nitrogen and Phosphorus Loads to Temperate Seepage Lakes Associated With Allochthonous Dissolved Organic Carbon Loads","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg","funders":"Northern Research Station; U.S. Department of Agriculture; U.S. Forest Service; National Science Foundation","keywords":"Dissolved organic carbon; Nutrient; Environmental science; Phosphorus; Watershed; Organic matter; Leaching (pedology); Temperate climate; Nitrogen; Nutrient cycle; Environmental chemistry; Hydrology (agriculture); Total organic carbon; Water quality; Ecology; Soil water; Soil science; Geology; Chemistry; Biology","score_opus":0.012505139843568836,"score_gpt":0.24809434699155805,"score_spread":0.23558920714798923,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805020085","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998054,0.000011718064,0.000023975514,0.0000043716195,3.1160857e-7,0.0000012028606,0.00006488457,0.000001746532,0.000086316424],"genre_scores_gemma":[0.9996313,0.000021959273,0.0000600967,0.000008004949,0.000001250304,0.000004471204,0.00014283485,0.0000011274591,0.00012902994],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999254,0.000011215598,0.000005572801,0.00002692461,0.000014205399,0.000016633472],"domain_scores_gemma":[0.99969745,0.00004820823,0.00013863323,0.000010268333,0.000052555897,0.000052960517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019289012,0.00018746126,0.00016638445,0.00039247386,0.00035419737,0.00051964086,0.0001166037,0.0002223888,0.0005897069],"category_scores_gemma":[0.00038203853,0.00016693825,0.0001486582,0.0004372771,0.00026074197,0.00033505837,0.00042663267,0.00012507044,0.0000625808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003186029,0.000039183316,0.97418106,0.0000146546145,0.00005636374,0.0001163101,0.0002298372,0.0005971811,0.022638416,0.00003987688,0.000076896074,0.0016915784],"study_design_scores_gemma":[0.0000026411378,0.0000332602,0.9979752,0.0000014876861,0.000010493531,0.000016902066,0.00012615345,0.0008696237,0.0008603623,0.000020565094,0.000081220256,0.0000021579992],"about_ca_topic_score_codex":0.025830906,"about_ca_topic_score_gemma":0.049851183,"teacher_disagreement_score":0.025830906,"about_ca_system_score_codex":0.00062917365,"about_ca_system_score_gemma":0.0002964355,"threshold_uncertainty_score":0.051361084},"labels":[],"label_agreement":null},{"id":"W2805277319","doi":"10.1029/2018gl077898","title":"Generation of Electron Acoustic Waves in the Topside Ionosphere From Coupling With Kinetic Alfven Waves: A New Electron Energization Mechanism","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Fundamental Research Funds for the Central Universities; Japan Society for the Promotion of Science; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Physics; Ionosphere; Electron; Kinetic energy; Computational physics; Electron density; Acoustic wave; Ion acoustic wave; Electron temperature; Atomic physics; Geophysics; Optics; Classical mechanics","score_opus":0.019782881690185997,"score_gpt":0.2772584255089854,"score_spread":0.2574755438187994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805277319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9224153,0.0011066844,0.058214616,0.00028886495,0.00011236882,0.00004367302,0.00013174307,0.00031114652,0.017375678],"genre_scores_gemma":[0.9955362,0.00030517398,0.0024093124,0.00002484185,0.000027105187,0.000008437115,0.000039903494,0.000016246038,0.0016328004],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999521,0.0000039836436,0.000001831633,0.000010334253,0.00001468113,0.000017164914],"domain_scores_gemma":[0.9999064,0.000013322943,0.000019018156,0.00001784011,0.000018327139,0.000025005927],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011096879,0.00042276812,0.00030796378,0.0003315456,0.0002781532,0.0006935076,0.00038165555,0.0003178774,0.0020018104],"category_scores_gemma":[0.00017184152,0.0002968648,0.00039961655,0.00018257729,0.0004633527,0.00060381356,0.00082737365,0.0003865243,0.00029502716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065017794,0.00017727373,0.029618008,0.00038471268,0.00024716245,0.0033296272,0.0007014469,0.04417398,0.77603096,0.10998188,0.001677794,0.033027075],"study_design_scores_gemma":[0.0004542454,0.00074887834,0.09204235,0.00010410377,0.00030956764,0.0030517704,0.0009085008,0.67283213,0.13574034,0.08548966,0.008133,0.00018546171],"about_ca_topic_score_codex":0.0005732351,"about_ca_topic_score_gemma":0.00048859126,"teacher_disagreement_score":0.0020018104,"about_ca_system_score_codex":0.00017260348,"about_ca_system_score_gemma":0.0001894349,"threshold_uncertainty_score":0.0066967607},"labels":[],"label_agreement":null},{"id":"W2805351355","doi":"10.1002/2017gl075832","title":"Dry Deposition of Reactive Nitrogen From Satellite Observations of Ammonia and Nitrogen Dioxide Over North America","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Environment and Climate Change Canada; University of Wisconsin-Madison; National Aeronautics and Space Administration","keywords":"Nitrogen; Reactive nitrogen; Deposition (geology); Flux (metallurgy); Ecosystem; Environmental science; Ammonia; Nitrogen dioxide; Atmospheric sciences; Nutrient; Latitude; Dry season; Environmental chemistry; Chemistry; Ecology; Geography; Geology; Meteorology; Biology","score_opus":0.03373916561533704,"score_gpt":0.27133355947510535,"score_spread":0.2375943938597683,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805351355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9953425,0.0003161641,0.0002721165,0.000053441094,0.000007892349,0.0000058547394,0.0030684355,0.000036742946,0.0008967736],"genre_scores_gemma":[0.99466586,0.00035813972,0.0007267849,0.00003412352,0.000008096045,0.000010897996,0.0038419836,0.0000067061123,0.00034740393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991953,0.000009745738,0.0000060432903,0.000029053475,0.0000249961,0.000010517865],"domain_scores_gemma":[0.9998228,0.000023636094,0.00005715003,0.0000102190725,0.00006782742,0.000018409404],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019812978,0.00027159214,0.0001396611,0.0006294411,0.00021441968,0.00033459262,0.00016579263,0.00020872203,0.00041444984],"category_scores_gemma":[0.000295588,0.00017686383,0.00023531547,0.0009158428,0.00012421659,0.00020875408,0.00021461418,0.00013126653,0.00009668574],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013742247,0.000036969297,0.96339315,0.00011517808,0.00027555422,0.00022404855,0.00021890628,0.008157066,0.012493643,0.00008757816,0.0017588414,0.013101626],"study_design_scores_gemma":[0.0000075866733,0.000007501304,0.9931415,0.000011110637,0.000031423013,0.00002908,0.000099726414,0.0048140595,0.0007850833,0.000033269334,0.0010332527,0.0000065318995],"about_ca_topic_score_codex":0.38321763,"about_ca_topic_score_gemma":0.5169721,"teacher_disagreement_score":0.61678237,"about_ca_system_score_codex":0.0009181656,"about_ca_system_score_gemma":0.00073567586,"threshold_uncertainty_score":0.7619741},"labels":[],"label_agreement":null},{"id":"W2805640597","doi":"10.1029/2018gl078014","title":"The 1 May 2017 British Columbia‐Alaska Earthquake Doublet and Implication for Complexity Near Southern End of Denali Fault System","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China; Northwestern University","keywords":"Seismology; Geology; Aftershock; Focal mechanism; Fault (geology); Transpression; Geodesy; Collision; Induced seismicity; Sinistral and dextral","score_opus":0.05564822715405307,"score_gpt":0.29790047834493527,"score_spread":0.2422522511908822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805640597","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99581784,0.0000591668,0.000053698255,0.00026511762,0.000003664507,0.0000048886686,0.00013037065,0.000007413833,0.003657788],"genre_scores_gemma":[0.99947613,0.000032092656,0.000034761048,0.000011945351,0.0000013754726,7.72601e-7,0.0000702013,0.0000010404725,0.00037156255],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998826,0.000013446352,0.000006602793,0.0000320353,0.000023933137,0.000041448064],"domain_scores_gemma":[0.9995732,0.000041835872,0.00011194643,0.000020990805,0.000113736445,0.00013841242],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001035221,0.00014550709,0.00019623688,0.0010490393,0.0016633581,0.0018065837,0.00030496257,0.0003937527,0.003680178],"category_scores_gemma":[0.0009673536,0.00013451939,0.00009561849,0.0010006211,0.0008947853,0.00050225103,0.00081959035,0.00034197542,0.00016622334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012528274,0.00004653121,0.9739889,0.00003743947,0.000046201298,0.0012957247,0.0016143896,0.0031598913,0.0049443278,0.0015692412,0.0012739609,0.01189815],"study_design_scores_gemma":[0.0000031806487,0.000007371465,0.9953009,0.000012380003,0.000008820755,0.00007155979,0.0019918813,0.0013993641,0.0001239772,0.00030103556,0.0007714507,0.000008124224],"about_ca_topic_score_codex":0.48231712,"about_ca_topic_score_gemma":0.67544407,"teacher_disagreement_score":0.5176829,"about_ca_system_score_codex":0.003147611,"about_ca_system_score_gemma":0.0016801873,"threshold_uncertainty_score":0.9590194},"labels":[],"label_agreement":null},{"id":"W2805802214","doi":"","title":"NEPTUNE‐Canada(カナダ北東太平洋時系列水中ネットワーク実験)ケーブル観測所による2009年サモア津波の観測:業務地域津波予報モデルのためのテストデータ","year":2011,"lang":"ja","type":"article","venue":"Geophysical Research Letters","topic":"Military Technology and Strategies","field":"Engineering","cited_by":18,"is_retracted":false,"has_abstract":false,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Neptune; Geology; Astrobiology; Meteorology; Astronomy; Physics; Planet","score_opus":0.04238975284078418,"score_gpt":0.2657789807980888,"score_spread":0.22338922795730465,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805802214","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.17555483,0.004064675,0.0020392695,0.008545566,0.0004860295,0.00007442299,0.0010772988,0.00007044258,0.8080875],"genre_scores_gemma":[0.6689523,0.0025964982,0.002789746,0.0014184776,0.000058630347,0.000022865337,0.0005412199,0.000042692413,0.32357758],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99948895,0.000020905813,0.0000132721925,0.00007126701,0.00023624225,0.00016933653],"domain_scores_gemma":[0.99943167,0.000041176332,0.000039142553,0.000030573578,0.00035383823,0.00010356192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003776919,0.00032271573,0.00015401022,0.0006402783,0.004421498,0.002409016,0.00053627306,0.00070501416,0.011819351],"category_scores_gemma":[0.00082501024,0.00016463539,0.00022465228,0.0009720891,0.0018376539,0.00070851453,0.0006783637,0.0009662354,0.0011318679],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006209105,0.00012266268,0.058679618,0.00032502896,0.00015562295,0.0015460587,0.005124466,0.0020893072,0.019803286,0.6093487,0.072655275,0.22952902],"study_design_scores_gemma":[0.000033315726,0.0000428251,0.093821116,0.00013900085,0.00006187426,0.0006535204,0.0042406116,0.0011330405,0.0136080505,0.02115043,0.86504066,0.00007557879],"about_ca_topic_score_codex":0.93757904,"about_ca_topic_score_gemma":0.96197593,"teacher_disagreement_score":0.062420964,"about_ca_system_score_codex":0.022183266,"about_ca_system_score_gemma":0.021650888,"threshold_uncertainty_score":0.16095161},"labels":[],"label_agreement":null},{"id":"W2805916984","doi":"10.1029/2018gl078172","title":"Changes to the Air‐Sea Flux and Distribution of Radiocarbon in the Ocean Over the 21st Century","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; European Commission; Sight Research UK; University of Victoria","keywords":"Ocean gyre; Radiocarbon dating; Ocean current; Hydrography; Oceanography; Climatology; Environmental science; Flux (metallurgy); Carbon cycle; Carbon flux; Sea surface temperature; Thermohaline circulation; Subtropics; Ocean general circulation model; Geology; General Circulation Model; Climate change; Ecosystem","score_opus":0.011981383563882234,"score_gpt":0.25411168899361813,"score_spread":0.2421303054297359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2805916984","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99792296,0.00012610006,0.00053212116,0.00021779763,0.000011211651,0.0000022943655,0.00050874427,0.000016277594,0.0006624632],"genre_scores_gemma":[0.9991856,0.00011577762,0.00024939113,0.000023730063,0.0000054405673,0.0000026044422,0.000295873,0.000004626152,0.00011685049],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998518,0.000042694686,0.000009930547,0.00004357614,0.000020177948,0.000031867214],"domain_scores_gemma":[0.99956626,0.00012764044,0.00012806951,0.000047021043,0.000084602856,0.00004636376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006417521,0.0002091643,0.00021649493,0.0005311947,0.00023679416,0.0009772009,0.00029736705,0.0006791988,0.00080677174],"category_scores_gemma":[0.0016198601,0.0002196939,0.0007168268,0.0008537934,0.0004201729,0.0005659827,0.00044550223,0.0003411314,0.00010765167],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027937972,0.00008258019,0.69603467,0.000049033555,0.00038717038,0.00025220303,0.000114447284,0.28652963,0.005233524,0.0027201301,0.0009092116,0.0074080024],"study_design_scores_gemma":[0.00006610409,0.00014206131,0.6186274,0.000024307346,0.00015069339,0.00014415925,0.00020997501,0.3722602,0.0027330958,0.0028129255,0.0027664325,0.000062516185],"about_ca_topic_score_codex":0.023929521,"about_ca_topic_score_gemma":0.01844622,"teacher_disagreement_score":0.023929521,"about_ca_system_score_codex":0.0010006718,"about_ca_system_score_gemma":0.0004987429,"threshold_uncertainty_score":0.04758048},"labels":[],"label_agreement":null},{"id":"W2806445358","doi":"10.1002/2017gl074912","title":"Accelerating Thermokarst Transforms Ice‐Cored Terrain Triggering a Downstream Cascade to the Ocean","year":2017,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":92,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Geological Survey of Canada; Natural Resources Canada; Government of Northwest Territories; Queen's University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; W. Garfield Weston Foundation","keywords":"Thermokarst; Permafrost; Geology; Deglaciation; Physical geography; Arctic; Fluvial; Earth science; Geomorphology; Oceanography; Glacial period","score_opus":0.10746299830758575,"score_gpt":0.3351663553337603,"score_spread":0.22770335702617456,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806445358","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994269,0.000071334485,0.00036656146,0.00010635681,0.000011259328,0.000007846115,0.00015832919,0.00007348722,0.004935909],"genre_scores_gemma":[0.99876714,0.000054951386,0.00012720907,0.000034798726,0.0000037036918,0.0000016071765,0.000067094974,0.0000058569717,0.0009377225],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999639,0.0000010219203,0.000001010531,0.0000072472153,0.0000062301942,0.000020694893],"domain_scores_gemma":[0.99994004,0.0000035956884,0.000011267747,0.0000067255396,0.000014980907,0.000023346292],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000033613585,0.000112782436,0.000104261846,0.00025628775,0.00049626484,0.0006965986,0.00017387657,0.00020096355,0.0058345343],"category_scores_gemma":[0.00011839997,0.000104124236,0.00014192265,0.0001863684,0.0003577302,0.00020062448,0.00058899604,0.0003366603,0.00038862493],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005886805,0.00017453932,0.26996237,0.00011938449,0.00005567982,0.0043294686,0.0011407516,0.0056943614,0.6760404,0.0039016514,0.0029364743,0.035056274],"study_design_scores_gemma":[0.000020217629,0.00009039758,0.96468204,0.000021778982,0.000020875963,0.0005870377,0.0011493519,0.0040747267,0.02290708,0.0010969321,0.0053327302,0.000016885728],"about_ca_topic_score_codex":0.047376115,"about_ca_topic_score_gemma":0.085727274,"teacher_disagreement_score":0.047376115,"about_ca_system_score_codex":0.0010034475,"about_ca_system_score_gemma":0.00055179687,"threshold_uncertainty_score":0.09420073},"labels":[],"label_agreement":null},{"id":"W2806463632","doi":"10.1029/2018gl078577","title":"Geodetic Constraints of the 2017 M<sub>w</sub>7.3 Sarpol Zahab, Iran Earthquake, and Its Implications on the Structure and Mechanics of the Northwest Zagros Thrust‐Fold Belt","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Japan Aerospace Exploration Agency; Canadian Space Agency","keywords":"Geology; Seismology; Interferometric synthetic aperture radar; Slip (aerodynamics); Seismic gap; Geodetic datum; Synthetic aperture radar; Thrust fault; Interplate earthquake; Aftershock; Geodesy; Fold (higher-order function); Fault (geology); Foreshock; Remote sensing","score_opus":0.041707396895432895,"score_gpt":0.26761583204774286,"score_spread":0.22590843515230996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806463632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930525,0.0000210491,0.00004628491,0.000028317367,0.000002209648,0.0000013107448,0.000104381266,0.000004055136,0.0004871641],"genre_scores_gemma":[0.9996817,0.000022989208,0.000047437814,0.0000049675423,0.0000041965554,0.0000010839658,0.00018779778,0.0000010255025,0.00004886833],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.0000075616726,0.000004306063,0.000012382724,0.000016907721,0.000029857896],"domain_scores_gemma":[0.99977416,0.000019995057,0.00011485466,0.000016092028,0.00005085225,0.000023964158],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015620964,0.00014845295,0.00015429583,0.0006477152,0.00027503123,0.00031949038,0.00016937926,0.00019515837,0.00059599045],"category_scores_gemma":[0.00039265628,0.000100305326,0.00012768914,0.00048882933,0.00025349355,0.00020699305,0.0002447846,0.00015201607,0.00019547348],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001277998,0.000060922703,0.97362024,0.000020963462,0.000022862403,0.0003043005,0.0003749175,0.0014127132,0.008590086,0.0002856377,0.0006651034,0.014514591],"study_design_scores_gemma":[0.000003648186,0.000016091455,0.99861896,0.0000032375958,0.0000054770303,0.000031914853,0.00024263625,0.00062101224,0.00017369495,0.00003229755,0.0002492825,0.0000016871559],"about_ca_topic_score_codex":0.01791726,"about_ca_topic_score_gemma":0.034236394,"teacher_disagreement_score":0.01791726,"about_ca_system_score_codex":0.00034984478,"about_ca_system_score_gemma":0.0004999204,"threshold_uncertainty_score":0.035625994},"labels":[],"label_agreement":null},{"id":"W2806641233","doi":"10.1029/2018gl077294","title":"On the Relative Robustness of the Climate Response to High‐Latitude and Low‐Latitude Warming","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Latitude; Climatology; Environmental science; Sea ice; Global warming; Arctic ice pack; Climate change; Arctic; Climate model; Atmospheric sciences; Middle latitudes; Ice-albedo feedback; Geology; Antarctic sea ice; Oceanography","score_opus":0.021412296147673003,"score_gpt":0.27572291369098884,"score_spread":0.25431061754331585,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2806641233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949929,0.00014628304,0.0015020798,0.00022252851,0.000032412507,0.000017746519,0.00065732026,0.00011410422,0.0023146246],"genre_scores_gemma":[0.9992017,0.000029384035,0.00016250441,0.0000391487,0.000009166299,0.000008425856,0.00042585927,0.000023852834,0.00010003714],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99890566,0.0004618632,0.00008793563,0.00028411642,0.00011906816,0.00014136996],"domain_scores_gemma":[0.994672,0.0033893136,0.00043050462,0.0009924417,0.00027974215,0.00023604975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0028935282,0.0005752542,0.00052959,0.0005247899,0.0004023567,0.0014296392,0.0006754366,0.00073952187,0.001819834],"category_scores_gemma":[0.008554714,0.0003453225,0.001331864,0.0004431836,0.00078813965,0.00077332376,0.0012334102,0.00070504134,0.00027081073],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0052674096,0.00051849324,0.39682755,0.00045229605,0.0037944322,0.00045280228,0.00039906002,0.46854812,0.097446226,0.0032003268,0.0018881657,0.021205101],"study_design_scores_gemma":[0.00037605694,0.0007811512,0.61903834,0.000052176092,0.0009316802,0.00012627993,0.00039748763,0.35046366,0.02313531,0.0031398854,0.0014245017,0.00013343443],"about_ca_topic_score_codex":0.0072068227,"about_ca_topic_score_gemma":0.002560799,"teacher_disagreement_score":0.0072068227,"about_ca_system_score_codex":0.0004910965,"about_ca_system_score_gemma":0.0002932439,"threshold_uncertainty_score":0.0153025985},"labels":[],"label_agreement":null},{"id":"W2807613185","doi":"10.1029/2018gl078035","title":"Revisiting the Mystery of Recent Stratospheric Temperature Trends","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Marsden Fund; Scheme for Promotion of Academic and Research Collaboration; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Met Office; National Oceanic and Atmospheric Administration; Sight Research UK; Natural Environment Research Council; New Zealand Government; Austrian Science Fund; National Aeronautics and Space Administration; Department for Environment, Food and Rural Affairs, UK Government; Serono Symposia International Foundation; National Science Foundation","keywords":"Stratosphere; Ozone depletion; Environmental science; Satellite; Ozone layer; Depth sounding; Climatology; Atmospheric sciences; Ozone; Advanced Microwave Sounding Unit; Microwave Limb Sounder; Meteorology; Geography; Geology; Physics","score_opus":0.03726987086415398,"score_gpt":0.3006680778810733,"score_spread":0.2633982070169193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807613185","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9879523,0.0018870023,0.0036821717,0.002563522,0.00014387592,0.000007903364,0.0015840115,0.0002169561,0.0019622187],"genre_scores_gemma":[0.99838066,0.0003376305,0.00039451558,0.00010399559,0.000050127375,0.0000024178266,0.0006080089,0.000036997513,0.0000856838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99972624,0.000058922218,0.00003241725,0.00011879788,0.00003882887,0.000024792811],"domain_scores_gemma":[0.99918526,0.00021763434,0.00023232102,0.00018827319,0.00013871954,0.000037766917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013467965,0.00024681858,0.00030048657,0.00049959077,0.00026563875,0.0014409175,0.00078969175,0.0005816264,0.0008469735],"category_scores_gemma":[0.0035820892,0.00031156014,0.000689788,0.0006683319,0.0006240832,0.0019953097,0.00069741934,0.00065775996,0.00014128641],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002404016,0.00009370836,0.86888206,0.00029927236,0.0011651628,0.00024561182,0.0008451361,0.07411653,0.011228014,0.006209803,0.0038431769,0.032831136],"study_design_scores_gemma":[0.000072702045,0.000082696286,0.7147288,0.00019426004,0.00030531184,0.0001206807,0.00058465725,0.26149368,0.0043560015,0.006100134,0.011881437,0.00007966556],"about_ca_topic_score_codex":0.0185094,"about_ca_topic_score_gemma":0.01863493,"teacher_disagreement_score":0.0185094,"about_ca_system_score_codex":0.0007233891,"about_ca_system_score_gemma":0.0005879965,"threshold_uncertainty_score":0.036803305},"labels":[],"label_agreement":null},{"id":"W2807951116","doi":"10.1029/2018gl078425","title":"A New Magnetic Field Activity Proxy for Mars From MAVEN Data","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; University of British Columbia","keywords":"Mars Exploration Program; Geophysics; Interplanetary magnetic field; Dipole model of the Earth's magnetic field; Geology; Martian; Interplanetary spaceflight; Exploration of Mars; Magnetometer; Ionosphere; Solar wind; Astrobiology; Magnetic field; Physics; Remote sensing","score_opus":0.08049000280881766,"score_gpt":0.3489041104849658,"score_spread":0.26841410767614815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2807951116","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9205198,0.0007304132,0.03064622,0.00033267745,0.00006523018,0.00012693251,0.039706472,0.0027507953,0.0051215584],"genre_scores_gemma":[0.92336696,0.00028557537,0.027096821,0.000045288296,0.000044137127,0.00008464454,0.048359785,0.00016140181,0.0005554413],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996283,0.00009736737,0.00003990735,0.00011650781,0.00007740507,0.00004037769],"domain_scores_gemma":[0.99886656,0.00015844619,0.00035116062,0.0002551663,0.00025572418,0.00011297049],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00055682374,0.00040124496,0.00035824926,0.0023639142,0.00020373658,0.0019923039,0.0005208694,0.0004304061,0.0009888606],"category_scores_gemma":[0.0031637945,0.0001674995,0.00042398518,0.0024905528,0.00014460762,0.0009472738,0.00074577413,0.0004543787,0.00048780272],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005524862,0.00013988062,0.80132663,0.00036476366,0.00057808304,0.00032596127,0.0003874934,0.08807534,0.014446123,0.002434271,0.011226735,0.08014226],"study_design_scores_gemma":[0.00007200363,0.00012545579,0.61365896,0.00011637916,0.000104928644,0.0003039111,0.0004569583,0.34365565,0.0082520265,0.0015261192,0.031649955,0.00007766094],"about_ca_topic_score_codex":0.009392497,"about_ca_topic_score_gemma":0.010420648,"teacher_disagreement_score":0.009392497,"about_ca_system_score_codex":0.0003888321,"about_ca_system_score_gemma":0.00033253993,"threshold_uncertainty_score":0.018675685},"labels":[],"label_agreement":null},{"id":"W2808030200","doi":"10.1029/2018gl077837","title":"Dependence of Present and Future European Temperature Extremes on the Location of Atmospheric Blocking","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":157,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Environment and Climate Change Canada","funders":"Joint Research Centre; Norges Forskningsråd; Austrian Science Fund","keywords":"Blocking (statistics); Environmental science; Atmospheric sciences; Climatology; Meteorology; Climate extremes; Geology; Geography; Precipitation; Computer science","score_opus":0.0322466977279803,"score_gpt":0.28351379964698376,"score_spread":0.2512671019190035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2808030200","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996238,0.00015590878,0.00070278184,0.00007574238,0.0000077373725,0.0000020921339,0.00056579,0.000025617072,0.0022263369],"genre_scores_gemma":[0.9991365,0.00004122424,0.000103568374,0.0000070831097,0.0000036429858,0.0000010659165,0.00060753943,0.000006481245,0.0000929334],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997863,0.000034493016,0.000013745493,0.000065198874,0.000035538524,0.0000647917],"domain_scores_gemma":[0.99881196,0.0003836774,0.00024643244,0.00014038915,0.0002907924,0.0001267546],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009115561,0.00015110704,0.00017196774,0.0003413479,0.00026033903,0.0007251322,0.000241036,0.00036914242,0.0009622441],"category_scores_gemma":[0.0023165243,0.00012338822,0.00032276928,0.00038777656,0.00023177457,0.00044322183,0.00037090233,0.00031684898,0.00014447985],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003847449,0.000041708994,0.9070898,0.00003440728,0.00020419096,0.00017214194,0.00014859105,0.07376443,0.007410899,0.0019298949,0.0008906065,0.007928655],"study_design_scores_gemma":[0.000013202371,0.00004027304,0.9542003,0.000014046079,0.000044993296,0.000101411955,0.00010232193,0.042071704,0.0015909813,0.00040132986,0.0013955479,0.000023783585],"about_ca_topic_score_codex":0.026144164,"about_ca_topic_score_gemma":0.02876034,"teacher_disagreement_score":0.026144164,"about_ca_system_score_codex":0.00050091854,"about_ca_system_score_gemma":0.00034972222,"threshold_uncertainty_score":0.051984012},"labels":[],"label_agreement":null},{"id":"W2809629409","doi":"10.1029/2018gl078589","title":"A Case Study of Near‐Earth Magnetotail Conditions at Substorm and Pseudosubstorm Onsets","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Japan Society for the Promotion of Science; Canadian Space Agency; Center for Hierarchical Manufacturing, National Science Foundation; National Aeronautics and Space Administration","keywords":"Substorm; Geophysics; Physics; Magnetosphere; Geology; Astrophysics; Magnetic field","score_opus":0.024418630853298803,"score_gpt":0.3059202752269701,"score_spread":0.28150164437367126,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2809629409","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867517,0.000026336447,0.00034093336,0.000017687997,0.0000018583386,0.000008433922,0.000033694818,0.000008720152,0.0008869964],"genre_scores_gemma":[0.99964976,0.000013546795,0.00015424543,0.0000027007786,0.0000031349755,0.0000018776508,0.000026636722,0.000001545937,0.00014660737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998592,0.000028423403,0.000008957871,0.000023885628,0.000029245111,0.00005033229],"domain_scores_gemma":[0.99953604,0.00012574538,0.00010140144,0.000049186277,0.000052658474,0.00013497125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023706906,0.00013941017,0.00016640109,0.00051293854,0.00072691997,0.00042833766,0.00021558446,0.0003662378,0.0011260632],"category_scores_gemma":[0.0006881354,0.000082936036,0.00016702073,0.00047721976,0.00037022686,0.00026993713,0.0005258023,0.0002783694,0.00008484598],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006576621,0.00018435244,0.82797056,0.000087357075,0.000073488336,0.09328825,0.005426854,0.005263477,0.03198192,0.0016813886,0.00072479394,0.03265995],"study_design_scores_gemma":[0.000029812958,0.00044620078,0.96011466,0.000016192864,0.0000398862,0.01455748,0.006052748,0.007232097,0.0067184484,0.0009194023,0.0038453066,0.000027718963],"about_ca_topic_score_codex":0.005685368,"about_ca_topic_score_gemma":0.012162725,"teacher_disagreement_score":0.005685368,"about_ca_system_score_codex":0.00037544468,"about_ca_system_score_gemma":0.00019570735,"threshold_uncertainty_score":0.011304557},"labels":[],"label_agreement":null},{"id":"W2810091991","doi":"10.1029/2018gl077799","title":"Shear Rate‐Dependent Disequilibrium Rheology and Dynamics of Basalt Solidification","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Horizon 2020 Framework Programme; H2020 Marie Skłodowska-Curie Actions; Compagnia di San Paolo; H2020 European Research Council; Fondazione CRT","keywords":"Rheology; Lava; Basalt; Geology; Olivine; Shear (geology); Shear rate; Petrology; Shear zone; Magma; Peridotite; Crystallization; Mineralogy; Geochemistry; Geophysics; Thermodynamics; Volcano; Materials science; Composite material","score_opus":0.02722022259970406,"score_gpt":0.2745779374600338,"score_spread":0.24735771486032973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2810091991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994941,0.0000430627,0.00015044802,0.0000044002813,7.426297e-7,0.0000024581625,0.00007955705,0.0000058155942,0.00021946263],"genre_scores_gemma":[0.99980694,0.000019057712,0.000044522516,0.0000012201768,6.802086e-7,0.0000015937649,0.00006932384,0.0000022457775,0.00005448794],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999454,0.0000066194366,0.000004179591,0.0000181201,0.000010670618,0.000014956133],"domain_scores_gemma":[0.9997596,0.00004782984,0.00007479394,0.00002538313,0.000046794812,0.00004545295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017134806,0.00013156213,0.00018137971,0.00053838186,0.00014551249,0.0005734119,0.000117663214,0.00012616045,0.00081295206],"category_scores_gemma":[0.0005224342,0.00013037784,0.000117214266,0.00024985566,0.00022780622,0.00035110238,0.00019469317,0.00026058836,0.00016170624],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000799876,0.00014237963,0.24478361,0.000055921108,0.00008014745,0.00021340066,0.00038890826,0.006269579,0.73519546,0.0010035373,0.00035188487,0.010715341],"study_design_scores_gemma":[0.000024251909,0.00026085772,0.8062491,0.000014326596,0.00003535925,0.00012046458,0.00020726562,0.06625136,0.12570997,0.00036461535,0.0007240266,0.000038534607],"about_ca_topic_score_codex":0.0018248708,"about_ca_topic_score_gemma":0.001125535,"teacher_disagreement_score":0.0018248708,"about_ca_system_score_codex":0.00020905027,"about_ca_system_score_gemma":0.00011462954,"threshold_uncertainty_score":0.0036284924},"labels":[],"label_agreement":null},{"id":"W2844611649","doi":"10.1029/2018gl079147","title":"Impacts of 1.5 and 2.0 °C Warming on Pan‐Arctic River Discharge Into the Hudson Bay Complex Through 2070","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos; University of Manitoba; University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bay; Environmental science; Discharge; Global warming; Arctic; Precipitation; Climatology; Oceanography; Spring (device); Climate change; Drainage basin; Geology; Geography; Meteorology","score_opus":0.041093593535649085,"score_gpt":0.3117977714118061,"score_spread":0.270704177876157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2844611649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935946,0.0001147144,0.0001541503,0.00037022965,0.00003858579,0.000014719095,0.0024352854,0.0000225306,0.0032551826],"genre_scores_gemma":[0.99694663,0.00017224162,0.00017560192,0.00011985397,0.000007742897,0.000014498935,0.001478888,0.000003977326,0.0010806874],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981636,0.00003520308,0.000011154196,0.000022865283,0.0000531829,0.00006128697],"domain_scores_gemma":[0.99966955,0.000029199939,0.00007754548,0.000013462744,0.00012364001,0.00008653827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037578933,0.0004023431,0.00015496937,0.0003103595,0.00030504717,0.00089931366,0.00024827695,0.00023247482,0.002166196],"category_scores_gemma":[0.0005699782,0.00012930158,0.00061127247,0.00033354675,0.00024652647,0.00027608074,0.0006954803,0.00027290033,0.00013382839],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006765956,0.00010745833,0.95385945,0.000084803374,0.00018386504,0.0005956727,0.0002427,0.024654668,0.004116571,0.0010909887,0.0035804282,0.010806848],"study_design_scores_gemma":[0.00003471142,0.00022677254,0.986446,0.00002648514,0.00005956571,0.00006526647,0.000728207,0.006306712,0.001631223,0.00021176708,0.0042462833,0.00001696443],"about_ca_topic_score_codex":0.23157848,"about_ca_topic_score_gemma":0.2485879,"teacher_disagreement_score":0.76842153,"about_ca_system_score_codex":0.0024331894,"about_ca_system_score_gemma":0.0024401823,"threshold_uncertainty_score":0.46046108},"labels":[],"label_agreement":null},{"id":"W2854262204","doi":"10.1029/2018gl078304","title":"In Situ Permeability and Scale Dependence of an Active Accretionary Prism Determined From Cross‐Borehole Experiments","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"National Science Foundation","keywords":"Borehole; Geology; Accretionary wedge; Permeability (electromagnetism); Advection; Tectonics; Fluid dynamics; Petrology; Submarine pipeline; Drilling fluid; Drilling; Subduction; Seismology; Geotechnical engineering; Mechanics; Materials science","score_opus":0.039331178857534455,"score_gpt":0.3334711768420309,"score_spread":0.29413999798449647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2854262204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990613,0.000010576604,0.0007034044,0.0000035579753,6.0767815e-7,0.000003067611,0.000047412763,0.0000113612905,0.00015875796],"genre_scores_gemma":[0.9995827,0.000008940614,0.00034862265,0.0000017348046,4.1554782e-7,0.0000027142696,0.000027338014,0.0000010346236,0.00002657693],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99989176,0.000011655424,0.000010475231,0.00003851677,0.000025095436,0.00002247362],"domain_scores_gemma":[0.999678,0.00008544038,0.00011456772,0.000029783832,0.000055201184,0.000037133523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018926914,0.00020614061,0.00013780067,0.00022638042,0.00018567985,0.0002091689,0.00022708645,0.0001951273,0.00027581293],"category_scores_gemma":[0.0006248239,0.00016637001,0.00011821969,0.00017181956,0.00033690094,0.00030065535,0.00028100636,0.00019189822,0.000043789958],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016680369,0.0000547277,0.04287434,0.00003307676,0.000012357265,0.00012436116,0.0002132819,0.0014960245,0.95280397,0.000078592704,0.000028096658,0.002114296],"study_design_scores_gemma":[0.00003483035,0.0005534178,0.5984208,0.000008569002,0.000040796833,0.00024883074,0.0003484607,0.021367634,0.378436,0.000105537656,0.0004049341,0.000030202375],"about_ca_topic_score_codex":0.0025997185,"about_ca_topic_score_gemma":0.0030725247,"teacher_disagreement_score":0.0025997185,"about_ca_system_score_codex":0.00017588641,"about_ca_system_score_gemma":0.00009305165,"threshold_uncertainty_score":0.005169153},"labels":[],"label_agreement":null},{"id":"W2866581105","doi":"10.1029/2018gl077551","title":"Geomechanical Sensitivities of Injection‐Induced Earthquakes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geomechanica (Canada)","funders":"","keywords":"Induced seismicity; Geology; Pore water pressure; Seismology; Hydrostatic equilibrium; Slip (aerodynamics); Overburden; Fluid pressure; Hydrostatic pressure; Geotechnical engineering; Mechanics","score_opus":0.056116360086624115,"score_gpt":0.30083686376065805,"score_spread":0.24472050367403392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2866581105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991793,0.000023831675,0.00027686238,0.00001008251,0.0000010576717,0.0000033318038,0.0001247818,0.000014209184,0.00036649656],"genre_scores_gemma":[0.99986446,0.000008114327,0.000027473307,0.0000025301017,4.986096e-7,0.0000011190058,0.000059393467,0.0000015472338,0.00003483091],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985206,0.000024415558,0.000016487638,0.00003471256,0.000032892687,0.000039438077],"domain_scores_gemma":[0.99942964,0.00017279267,0.00016683046,0.00005553556,0.00010452626,0.00007076278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019764091,0.00016466662,0.00022101754,0.00048732822,0.00012338128,0.00027710976,0.0001704349,0.00026244667,0.0014024036],"category_scores_gemma":[0.0010106902,0.00014354443,0.00018432616,0.00033319203,0.00019285867,0.00022105883,0.0003430208,0.00020313333,0.00016100633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097432005,0.00017270679,0.5436898,0.00011495123,0.0002264337,0.00058451813,0.00025913803,0.06805724,0.37064806,0.0004577883,0.00030331084,0.014511751],"study_design_scores_gemma":[0.0000096429985,0.00047064965,0.91592216,0.000005614224,0.00004308302,0.0002724427,0.00029144384,0.037002504,0.04537743,0.0002679402,0.000310041,0.000026994034],"about_ca_topic_score_codex":0.0012727809,"about_ca_topic_score_gemma":0.0013437477,"teacher_disagreement_score":0.0014024036,"about_ca_system_score_codex":0.0002718455,"about_ca_system_score_gemma":0.00008593425,"threshold_uncertainty_score":0.004691541},"labels":[],"label_agreement":null},{"id":"W2869678948","doi":"10.1029/2018gl078074","title":"Diverse Continental Subduction Scenarios Along the Arabia‐Eurasia Collision Zone","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"King Saud University; Institute of Population and Public Health; Deutsche Forschungsgemeinschaft","keywords":"Subduction; Geology; Collision zone; Continental collision; Lithosphere; Seismology; Mantle (geology); Convergent boundary; Slab; Eclogitization; Eurasian Plate; Slab window; Collision; Plate tectonics; Oceanic crust; Paleontology; Tectonics","score_opus":0.031529447381176044,"score_gpt":0.28286718660001586,"score_spread":0.25133773921883984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2869678948","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980039,0.000106273015,0.00038665984,0.000056688128,0.0000027485294,0.0000053158096,0.00013411893,0.000020864583,0.001283487],"genre_scores_gemma":[0.9994985,0.00005235226,0.00018011518,0.0000056542544,9.844173e-7,0.000002161446,0.000079907564,0.0000035815908,0.00017680453],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.000019102721,0.0000051120146,0.000014265451,0.000010614353,0.00001662528],"domain_scores_gemma":[0.9999175,0.000017534263,0.000016602136,0.000009901824,0.000014576841,0.000023966451],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017249571,0.00044051072,0.00027529564,0.0005195331,0.0005008631,0.0011660975,0.0005580867,0.00068531954,0.0016092806],"category_scores_gemma":[0.0003787899,0.00026430536,0.00045418774,0.00043256386,0.0004472937,0.00041098037,0.00073595886,0.00029216954,0.00015431408],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055517105,0.000078127916,0.39561644,0.000077469806,0.00031283902,0.0020448773,0.0010220974,0.56885314,0.018767156,0.0048091616,0.00054887164,0.007314653],"study_design_scores_gemma":[0.00029497853,0.00022178314,0.23017026,0.000054269083,0.00016863074,0.0007892382,0.00182618,0.75543755,0.0034578051,0.004873358,0.0026306384,0.00007532705],"about_ca_topic_score_codex":0.035610437,"about_ca_topic_score_gemma":0.022297239,"teacher_disagreement_score":0.035610437,"about_ca_system_score_codex":0.0008401505,"about_ca_system_score_gemma":0.00038232762,"threshold_uncertainty_score":0.070806324},"labels":[],"label_agreement":null},{"id":"W2883045199","doi":"10.1029/2018gl077736","title":"Low Phosphorus Availability Decreases Susceptibility of Tropical Primary Productivity to Droughts","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Canadian Foundation for Climate and Atmospheric Sciences; U.S. Department of Energy; H2020 European Research Council; Environment Canada; BIOCAP Canada; National Science Foundation","keywords":"Environmental science; Phosphorus; Primary production; Precipitation; Ecosystem; Soil water; Tropics; Productivity; Eddy covariance; Mineralization (soil science); Atmospheric sciences; Hydrology (agriculture); Ecology; Soil science; Chemistry; Biology; Geography; Geology","score_opus":0.016501623496531715,"score_gpt":0.2701122346179895,"score_spread":0.2536106111214578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883045199","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994311,0.00007608462,0.00014965623,0.000020718495,0.0000015477494,0.0000012003547,0.000058053505,0.000008738778,0.0002529478],"genre_scores_gemma":[0.99983096,0.000022427183,0.000044631695,0.000005255637,0.0000010657443,7.974759e-7,0.000032641412,0.000002005688,0.000060142647],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998989,0.00001978498,0.000006110611,0.000026892307,0.000011359066,0.00003701623],"domain_scores_gemma":[0.9992175,0.00023998247,0.00023853676,0.00006264085,0.000046134013,0.00019517695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000159305,0.00012172247,0.0002351811,0.00021914368,0.00015521575,0.00038856958,0.00014708872,0.00013877594,0.0014639873],"category_scores_gemma":[0.0008772259,0.00013014533,0.00011117712,0.00014886545,0.00026150426,0.00023020273,0.0004564366,0.00021197063,0.00010058194],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012422304,0.00014667289,0.33692804,0.00016798243,0.00021048468,0.00038266162,0.0003431768,0.0022628177,0.6482109,0.0003472239,0.00022581428,0.009532053],"study_design_scores_gemma":[0.000020526835,0.00036147784,0.9757178,0.0000075451444,0.000051687744,0.00023026497,0.00021530173,0.0036694296,0.018565103,0.00045598942,0.0006964915,0.000008404584],"about_ca_topic_score_codex":0.003241377,"about_ca_topic_score_gemma":0.0029052787,"teacher_disagreement_score":0.003241377,"about_ca_system_score_codex":0.00021832448,"about_ca_system_score_gemma":0.00019523842,"threshold_uncertainty_score":0.0064450502},"labels":[],"label_agreement":null},{"id":"W2883464991","doi":"10.1029/2018gl079026","title":"Chemical Diversity of Sands Within the Linear and Barchan Dunes of the Bagnold Dunes, Gale Crater, as Revealed by APXS Onboard Curiosity","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph; University of New Brunswick","funders":"Core Research for Evolutional Science and Technology; Canadian Space Agency; National Aeronautics and Space Administration","keywords":"Geology; Weathering; Impact crater; Mafic; Geomorphology; Bedform; Geochemistry; Earth science; Astrobiology; Sediment transport; Sediment","score_opus":0.02503634807852873,"score_gpt":0.2752587284387506,"score_spread":0.2502223803602219,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883464991","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99888057,0.00005509822,0.000060141258,0.000010055379,0.0000012838873,0.0000037543257,0.00024772182,0.000008656588,0.0007327614],"genre_scores_gemma":[0.9986675,0.00008600073,0.00023925137,0.0000147696455,0.000003125033,0.000004832056,0.00026556157,0.0000067377932,0.0007122908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992156,0.000004575405,0.000004431151,0.000027097947,0.000021362017,0.000020987653],"domain_scores_gemma":[0.999908,0.000012605511,0.000023301835,0.000006007175,0.000024348768,0.000025850133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008526873,0.00024143643,0.00019476187,0.0018901952,0.00051582395,0.00089624606,0.00017812179,0.0002334065,0.0011128596],"category_scores_gemma":[0.00014968746,0.00022183711,0.00013772014,0.00080561795,0.00040845294,0.00024136095,0.00044625052,0.00013499419,0.00015268344],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003074303,0.00003561249,0.8624462,0.00009449136,0.000115796756,0.0006188665,0.0017730916,0.00054381654,0.11545418,0.00018216205,0.00029085786,0.01813745],"study_design_scores_gemma":[0.0000021082292,0.000013809271,0.9979917,0.0000032039657,0.0000066269868,0.000080213664,0.00032783102,0.00011150443,0.0010500242,0.000010323007,0.00040035578,0.000002347727],"about_ca_topic_score_codex":0.02277613,"about_ca_topic_score_gemma":0.054057173,"teacher_disagreement_score":0.02277613,"about_ca_system_score_codex":0.0004170831,"about_ca_system_score_gemma":0.00019926728,"threshold_uncertainty_score":0.045287132},"labels":[],"label_agreement":null},{"id":"W2883715313","doi":"10.1029/2018gl078550","title":"High‐Latitude Westward Jets in the Earth's Outer Core Due to Small‐Scale Convection","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Buoyancy; Equator; Convection; Geostrophic wind; Geophysics; Latitude; Hydrostatic equilibrium; Atmospheric sciences; Climatology; Mechanics; Physics; Geodesy","score_opus":0.0321230761509627,"score_gpt":0.30128615418771254,"score_spread":0.2691630780367498,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883715313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99776876,0.000077646444,0.001205561,0.000041350853,0.000009557467,0.000003095608,0.000014897527,0.00005262285,0.00082653144],"genre_scores_gemma":[0.9996722,0.000027187963,0.00012838516,0.000006299722,0.000007198894,0.0000013019082,0.0000180501,0.000004404828,0.00013503147],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99997234,0.0000046470723,0.0000011142214,0.0000032553241,0.000005750459,0.000013014307],"domain_scores_gemma":[0.9999043,0.000026092166,0.000027280488,0.0000106160405,0.0000072493344,0.00002439628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007800429,0.00017593219,0.00019404766,0.00013114467,0.00013023632,0.00035395517,0.00011004843,0.00013298892,0.000826842],"category_scores_gemma":[0.00020949842,0.00012136446,0.00019810713,0.000078181,0.0002285119,0.00013617247,0.00023618308,0.000188701,0.00011708881],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095106603,0.00012463737,0.05688197,0.00008316998,0.00009730132,0.0045491713,0.00022403638,0.05121695,0.86553496,0.008574816,0.0011651099,0.010596788],"study_design_scores_gemma":[0.00060996925,0.00060713704,0.4888579,0.000016138878,0.00012623395,0.0020348614,0.00013209927,0.4266348,0.07059477,0.007636259,0.0027125583,0.000037345228],"about_ca_topic_score_codex":0.0012979686,"about_ca_topic_score_gemma":0.00055961864,"teacher_disagreement_score":0.0012979686,"about_ca_system_score_codex":0.00025021206,"about_ca_system_score_gemma":0.00007954676,"threshold_uncertainty_score":0.0027660131},"labels":[],"label_agreement":null},{"id":"W2883736166","doi":"10.1029/2018gl078895","title":"An Explanation for the Nitrous Oxide Layer Observed in the Mesopause Region","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Toronto","funders":"University of Leeds; University of Waterloo; Sight Research UK; National Oceanic and Atmospheric Administration; Natural Environment Research Council; Met Office","keywords":"Mesopause; Thermosphere; Atmospheric sciences; Airglow; Mesosphere; Atmosphere (unit); Environmental science; Aeronomy; Ionosphere; Nitrous oxide; Atmospheric chemistry; Physics; Ozone; Stratosphere; Meteorology; Chemistry; Geophysics","score_opus":0.10970738000302462,"score_gpt":0.32999706108197924,"score_spread":0.22028968107895464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883736166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99533266,0.00013081101,0.0015191358,0.00021053271,0.000012630215,0.0000059198833,0.0001616558,0.00012696475,0.0024996158],"genre_scores_gemma":[0.99963236,0.000015342082,0.00017621291,0.000011689308,0.0000020534899,0.0000013983553,0.000035281253,0.000003369646,0.00012225576],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999977,0.0000013440202,8.132894e-7,0.000009636857,0.0000030226702,0.000008184569],"domain_scores_gemma":[0.99997437,0.0000047255594,0.000007554347,0.0000037479851,0.0000033760973,0.000006315759],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000051456147,0.00014920154,0.00007862241,0.00014288402,0.00027876406,0.00019159657,0.00027301977,0.0002521355,0.0013597712],"category_scores_gemma":[0.00006878045,0.00013436658,0.00019438248,0.000113920585,0.00023640275,0.00017582151,0.00018236018,0.00016447471,0.00009271136],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002652674,0.0000612323,0.41488057,0.000106399646,0.00009970854,0.0010962591,0.00022212906,0.018083448,0.55213267,0.0034769587,0.0011976114,0.008377744],"study_design_scores_gemma":[0.00005122079,0.00007618415,0.923866,0.000010446048,0.000046464727,0.00035010872,0.00019817548,0.03702302,0.033432875,0.0023587456,0.0025663734,0.000020499956],"about_ca_topic_score_codex":0.012249949,"about_ca_topic_score_gemma":0.017271059,"teacher_disagreement_score":0.012249949,"about_ca_system_score_codex":0.00043320426,"about_ca_system_score_gemma":0.00022065705,"threshold_uncertainty_score":0.02435726},"labels":[],"label_agreement":null},{"id":"W2883999508","doi":"10.1029/2018gl078767","title":"Spatial Variation in the Slip Zone Thickness of a Seismogenic Fault","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"University of California, Riverside; U.S. Geological Survey; Southern California Earthquake Center; National Science Foundation","keywords":"Slip (aerodynamics); Geology; Seismology; Crust; Geophysics","score_opus":0.03753241815705789,"score_gpt":0.2914589624862413,"score_spread":0.25392654432918343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2883999508","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99973625,0.000008758268,0.00008957175,0.0000023782243,2.4768363e-7,3.9128872e-7,0.000048857248,0.0000040891878,0.00010941402],"genre_scores_gemma":[0.9998536,0.000004672922,0.000049559625,0.0000011654283,5.554359e-7,6.002396e-7,0.000047322337,0.000001040154,0.00004137187],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995244,0.000007778962,0.0000029890405,0.000018795894,0.0000073178544,0.000010706094],"domain_scores_gemma":[0.99966526,0.000100854,0.00011174022,0.000033876124,0.00005210615,0.000036194284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011649378,0.00008606817,0.00009328834,0.00058539625,0.00013571179,0.00023293498,0.000103111066,0.00014425477,0.0007168333],"category_scores_gemma":[0.00035088105,0.00010624686,0.00009725812,0.00034987144,0.00023323124,0.0001236201,0.0002023701,0.00010811842,0.000072276394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038250966,0.0000636065,0.685173,0.000035713543,0.00011840825,0.0004663387,0.001023565,0.0034428712,0.2989921,0.00023040987,0.00015729433,0.0099141495],"study_design_scores_gemma":[0.0000014400888,0.000017749422,0.99591994,0.000001201415,0.0000075852586,0.000084724365,0.00010031432,0.00077277975,0.00299443,0.00002063449,0.00007660365,0.0000026038642],"about_ca_topic_score_codex":0.002017844,"about_ca_topic_score_gemma":0.0019520266,"teacher_disagreement_score":0.002017844,"about_ca_system_score_codex":0.00014450864,"about_ca_system_score_gemma":0.00004892021,"threshold_uncertainty_score":0.004012227},"labels":[],"label_agreement":null},{"id":"W2884168214","doi":"10.1029/2018gl077869","title":"Vertical Structure of Diurnal Englacial Hydrology Cycle at Helheim Glacier, East Greenland","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Jet Propulsion Laboratory; York University; Sight Research UK; New York University Abu Dhabi; National Aeronautics and Space Administration; Norsk Sykepleierforbund; National Science Foundation","keywords":"Meltwater; Glacier; Geology; Diurnal cycle; Glacier mass balance; Ice stream; Climatology; Glacier ice accumulation; Tidewater glacier cycle; Geomorphology; Cryosphere; Sea ice; Ice calving","score_opus":0.03004533331328146,"score_gpt":0.27727253768041965,"score_spread":0.2472272043671382,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884168214","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994049,0.000024067787,0.000034778997,0.000010653079,0.0000010316554,8.16418e-7,0.00026982333,0.000012914196,0.00024094763],"genre_scores_gemma":[0.9994318,0.00002160835,0.000045026434,0.000005492027,0.0000015066692,0.0000010682204,0.00035817586,0.0000032041123,0.0001321069],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996746,0.0000036026515,0.0000014982667,0.000010946306,0.0000052981463,0.000011172832],"domain_scores_gemma":[0.9998553,0.000028921544,0.000038673188,0.000011294452,0.000029665876,0.000036231693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000113425325,0.00011565843,0.000092631475,0.0005316913,0.00014378648,0.00033643024,0.00009017732,0.00012224288,0.00058489514],"category_scores_gemma":[0.00020521674,0.00006455846,0.00006737608,0.00028877982,0.00019187153,0.00015916515,0.00015216965,0.00009733291,0.00011408103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013909623,0.00004379997,0.97162735,0.0000134131415,0.000047391004,0.00016168454,0.00061904057,0.0015791528,0.016205018,0.00009333698,0.0006279141,0.008842805],"study_design_scores_gemma":[0.0000017345883,0.0000070117835,0.99915314,0.0000018972654,0.0000032434853,0.0000101712885,0.000075896234,0.00041284593,0.0001754754,0.000009649767,0.00014718677,0.0000017388317],"about_ca_topic_score_codex":0.04786845,"about_ca_topic_score_gemma":0.10569811,"teacher_disagreement_score":0.04786845,"about_ca_system_score_codex":0.0003308784,"about_ca_system_score_gemma":0.00024909544,"threshold_uncertainty_score":0.09517968},"labels":[],"label_agreement":null},{"id":"W2884775273","doi":"10.1029/2018gl078596","title":"On the Role of Heterogeneous Chemistry in Ozone Depletion and Recovery","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Goddard Space Flight Center; Sight Research UK; Office of Science; National Aeronautics and Space Administration; Natural Environment Research Council; U.S. Department of Energy; National Center for Atmospheric Research; National Science Foundation","keywords":"Ozone; Ozone depletion; Volcano; Aerosol; Stratosphere; Ozone layer; Atmospheric sciences; Atmospheric chemistry; Environmental science; Trace gas; Climatology; Meteorology; Geology; Geography","score_opus":0.01690073656702232,"score_gpt":0.25140986589708086,"score_spread":0.23450912933005855,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884775273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940645,0.00025769978,0.0027666262,0.0002391854,0.000008070421,0.00003280747,0.0002640705,0.000037770962,0.002329284],"genre_scores_gemma":[0.9993604,0.00008359791,0.00023859521,0.000013908199,0.000002756355,0.0000054048237,0.00004476953,0.00000386777,0.000246695],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9998148,0.000046962192,0.0000076230754,0.000037870446,0.00003245845,0.000060328428],"domain_scores_gemma":[0.99953735,0.00020732392,0.00009381073,0.00004572916,0.000056928613,0.000058876765],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006334055,0.0004306441,0.00025072525,0.0004425067,0.00047109625,0.0007403973,0.0006509024,0.0003381707,0.0012171065],"category_scores_gemma":[0.0016133514,0.00018848071,0.00041253673,0.00029622953,0.000432154,0.0008491154,0.0006987509,0.00023258214,0.00010477042],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056349207,0.00039486986,0.45393285,0.00011372658,0.00043502534,0.0007734311,0.00015568192,0.46075466,0.054570477,0.0075806263,0.0008316452,0.019893602],"study_design_scores_gemma":[0.000093281655,0.00028117385,0.34351245,0.000011959424,0.00020211961,0.00007819511,0.00016370254,0.6312115,0.020090671,0.0028336116,0.0014795245,0.000041801733],"about_ca_topic_score_codex":0.10599034,"about_ca_topic_score_gemma":0.06227148,"teacher_disagreement_score":0.10599034,"about_ca_system_score_codex":0.0011641175,"about_ca_system_score_gemma":0.0011118149,"threshold_uncertainty_score":0.21074682},"labels":[],"label_agreement":null},{"id":"W2884844075","doi":"10.1029/2018gl079025","title":"Bagnold Dunes Campaign Phase 2: Visible/Near‐Infrared Reflectance Spectroscopy of Longitudinal Ripple Sands","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; University of Winnipeg","funders":"Jet Propulsion Laboratory; Centre National d’Etudes Spatiales","keywords":"Hematite; Geology; Impact crater; Mineralogy; Phase (matter); Infrared spectroscopy; Infrared; Geochemistry; Chemistry; Optics; Astrobiology","score_opus":0.044768136028153216,"score_gpt":0.3629562951299407,"score_spread":0.3181881591017875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2884844075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99470735,0.00007922242,0.00034758908,0.000018017943,0.000009215892,0.000040194554,0.0023417983,0.00006618056,0.0023904627],"genre_scores_gemma":[0.99079365,0.00007544275,0.0017539127,0.000050470022,0.000012399176,0.000058190108,0.0051149023,0.000030517318,0.0021105655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998369,0.000016091411,0.00000553876,0.000045003464,0.000060781833,0.000035743076],"domain_scores_gemma":[0.99988484,0.000010328346,0.000024267418,0.000017957916,0.000039780705,0.000022781524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022938398,0.00031546847,0.00019589497,0.000864483,0.0005511882,0.0005724184,0.00028734814,0.00026739,0.0010580034],"category_scores_gemma":[0.00019505084,0.00018993045,0.00018717852,0.00052623474,0.0001451789,0.00021730147,0.00032947387,0.00020017583,0.00028686968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018665168,0.0005243147,0.718063,0.00016569138,0.00020876055,0.00054765807,0.0012467297,0.0015764333,0.22785215,0.00013316839,0.0051616062,0.042653985],"study_design_scores_gemma":[0.000016380016,0.00006675266,0.992728,0.0000037788282,0.000013488323,0.00003921975,0.000114219554,0.00030850017,0.0049860897,0.000005831364,0.0017118031,0.000005965718],"about_ca_topic_score_codex":0.048539136,"about_ca_topic_score_gemma":0.16201618,"teacher_disagreement_score":0.048539136,"about_ca_system_score_codex":0.00063127535,"about_ca_system_score_gemma":0.0003655799,"threshold_uncertainty_score":0.09651321},"labels":[],"label_agreement":null},{"id":"W2885434630","doi":"10.1029/2018gl078789","title":"Global Freshwater Availability Below Normal Conditions and Population Impact Under 1.5 and 2 °C Stabilization Scenarios","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Key Research and Development Program of China; Swedish Foundation for International Cooperation in Research and Higher Education; Chinese Academy of Sciences; Office of Science; Norges Forskningsråd; Sight Research UK; Natural Environment Research Council; U.S. Department of Energy","keywords":"Precipitation; Environmental science; Evapotranspiration; Population; Middle latitudes; Tropics; Climatology; Global warming; Amazon rainforest; Climate change; Geography; Physical geography; Oceanography; Ecology; Geology; Meteorology; Demography","score_opus":0.033465124546297444,"score_gpt":0.33506282267566223,"score_spread":0.30159769812936477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885434630","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961474,0.000033378274,0.00062182924,0.00016628417,0.000024092466,0.000010711827,0.0018735678,0.000051872106,0.0010709137],"genre_scores_gemma":[0.9987973,0.000013105815,0.00017379837,0.000025293966,0.0000036962313,0.000013691123,0.0008739548,0.0000044619132,0.00009466599],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998122,0.00007687722,0.0000091672555,0.000046043726,0.000014072546,0.000041694027],"domain_scores_gemma":[0.9995734,0.00013471615,0.00006373817,0.00007411865,0.00008478132,0.00006913786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00085660187,0.00040807817,0.0003023778,0.00023041926,0.00029042957,0.0005644038,0.00034296748,0.00045594154,0.0012623317],"category_scores_gemma":[0.0011758684,0.00010781562,0.00058692764,0.00030231726,0.00036903864,0.00049906556,0.00036595704,0.0004216842,0.00011158592],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016706501,0.00036909166,0.19275512,0.00010812754,0.0005054396,0.00026210863,0.00009988258,0.7727794,0.012160001,0.00409282,0.0065784096,0.008618908],"study_design_scores_gemma":[0.0004428474,0.0013406258,0.29823965,0.000032852447,0.00037906555,0.00008402128,0.00040575306,0.6813876,0.008148191,0.0055225687,0.0038916632,0.00012507154],"about_ca_topic_score_codex":0.017219448,"about_ca_topic_score_gemma":0.011272482,"teacher_disagreement_score":0.017219448,"about_ca_system_score_codex":0.0008735482,"about_ca_system_score_gemma":0.00036265163,"threshold_uncertainty_score":0.034238458},"labels":[],"label_agreement":null},{"id":"W2885496707","doi":"10.1029/2018gl078428","title":"The Early Collapse of the 2017 Lincoln Sea Ice Arch in Response to Anomalous Sea Ice and Wind Forcing","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dairy Farmers of Ontario; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Universität Bremen; University of Washington; National Center for Atmospheric Research","keywords":"Sea ice; Arctic ice pack; Geology; Climatology; Drift ice; Oceanography; Antarctic sea ice; Arctic; Fast ice; Climate change; Arctic sea ice decline; Forcing (mathematics)","score_opus":0.021264154450855673,"score_gpt":0.28090316664697385,"score_spread":0.2596390121961182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885496707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990909,0.000029855953,0.000045524284,0.000050981034,0.000012155837,0.0000028713682,0.000090505724,0.0000058556634,0.000671424],"genre_scores_gemma":[0.99962556,0.000017097676,0.000023999246,0.0000146698,0.0000061468395,0.0000025127295,0.0001829635,0.0000014345774,0.00012547261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999899,0.000013038297,0.000009404192,0.000013824769,0.000028968909,0.000035695764],"domain_scores_gemma":[0.99933904,0.00009579984,0.00019307931,0.000040455376,0.00012850942,0.0002030244],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035541286,0.00015028068,0.00023702094,0.0007140604,0.0006467464,0.000850084,0.00018614215,0.00037351833,0.0011239804],"category_scores_gemma":[0.0012974291,0.000108340915,0.00020579812,0.00031488464,0.0005140665,0.00025803052,0.00090435066,0.00055400975,0.00017406417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060628215,0.0001064037,0.9698504,0.00003446206,0.00014536991,0.0016468384,0.0006445982,0.002012553,0.017485272,0.0004542446,0.0015028878,0.0055106548],"study_design_scores_gemma":[0.000005928559,0.000065029795,0.99511874,0.000011790325,0.000011461736,0.00020715341,0.00061155093,0.0023438951,0.00087610824,0.00012154924,0.00061568647,0.000011129402],"about_ca_topic_score_codex":0.016432777,"about_ca_topic_score_gemma":0.03133103,"teacher_disagreement_score":0.016432777,"about_ca_system_score_codex":0.0009157752,"about_ca_system_score_gemma":0.00047121884,"threshold_uncertainty_score":0.032674253},"labels":[],"label_agreement":null},{"id":"W2885974297","doi":"10.1029/2018gl078107","title":"Investigation of Acoustic Waves in the Ionosphere Generated by a Deep Convection System Using Distributed Networks of GPS Receivers and Numerical Modeling","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Resources Canada; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Ionosphere; Geology; Amplitude; Convection; Thunderstorm; Gravity wave; Wavelength; Total electron content; Geophysics; Atmosphere (unit); Acoustic wave; Storm; Gravitational wave; Meteorology; Physics; Acoustics; TEC; Optics","score_opus":0.022022455415330155,"score_gpt":0.2634858365510107,"score_spread":0.24146338113568055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2885974297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99401903,0.000039597977,0.0051986813,0.000043906814,0.000005129114,0.000010957574,0.000041388525,0.000029872226,0.00061153347],"genre_scores_gemma":[0.998703,0.000018245544,0.0010968959,0.0000028269535,0.000002971589,0.0000047950716,0.000019995286,0.0000021008896,0.00014922339],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991095,0.000030207231,0.0000043293576,0.000023048908,0.000013353316,0.000018191224],"domain_scores_gemma":[0.9994869,0.00026402142,0.00010762442,0.000037172766,0.00005917117,0.000045006505],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002736285,0.00044254653,0.00028802123,0.00037621212,0.00041102566,0.0005175911,0.00058296975,0.0005106593,0.00045428865],"category_scores_gemma":[0.0009423448,0.00036023153,0.00037118915,0.00031600037,0.00052709767,0.00048749798,0.00046198067,0.00039306586,0.00005152499],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054968397,0.000081413615,0.022034938,0.000010527444,0.000032348355,0.000104507046,0.000064988555,0.97245526,0.002499952,0.00052016607,0.000062242936,0.0020786345],"study_design_scores_gemma":[0.000010157608,0.000017981942,0.0020739501,0.0000010713219,0.00000434654,0.0000048905367,0.000019161293,0.9976255,0.0001426871,0.000074475385,0.000023364913,0.0000023954049],"about_ca_topic_score_codex":0.033217732,"about_ca_topic_score_gemma":0.017084725,"teacher_disagreement_score":0.033217732,"about_ca_system_score_codex":0.0009747443,"about_ca_system_score_gemma":0.00044818036,"threshold_uncertainty_score":0.06604874},"labels":[],"label_agreement":null},{"id":"W2886115924","doi":"10.1029/2018gl079564","title":"Spatiotemporal Changes of China's Carbon Emissions","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Environmental Impact and Sustainability","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University; McMaster University; University of Regina; University of Prince Edward Island","funders":"Foundation for Innovative Research Team of Jimei University; University of Prince Edward Island; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"China; Greenhouse gas; Urbanization; Carbon fibers; Environmental science; Climate change; Relaxation (psychology); Horizontal resolution; Climatology; Geography; Meteorology; Geology; Materials science; Economic growth","score_opus":0.025755824217217883,"score_gpt":0.32461968278893527,"score_spread":0.2988638585717174,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886115924","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994949,0.00009528417,0.00017189041,0.00008056319,0.0000059866534,0.0000046113887,0.003808048,0.000027512042,0.0008572232],"genre_scores_gemma":[0.9958476,0.00008425757,0.00015752575,0.000012402074,0.000005151365,0.000005640713,0.0035796629,0.0000029277146,0.00030487665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998752,0.000011871833,0.000013203643,0.000041465384,0.000029453095,0.000028827282],"domain_scores_gemma":[0.99965024,0.000036840782,0.00010453987,0.000050524897,0.00011536942,0.00004253592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030297745,0.00023714911,0.00018675959,0.0011161525,0.00022493005,0.0005365364,0.00024487986,0.00024405101,0.00085701665],"category_scores_gemma":[0.0005553108,0.00014880484,0.0003293938,0.0020108635,0.0002121441,0.0003104456,0.0003947103,0.00015828462,0.00010985142],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010095227,0.000037896545,0.95731866,0.000089497276,0.00028876608,0.00039924958,0.00032365785,0.01920675,0.0045155883,0.0010301014,0.0024949722,0.014193997],"study_design_scores_gemma":[0.0000030597062,0.000011320941,0.99149114,0.000005561736,0.000021547618,0.000038148355,0.00010896067,0.006128392,0.00047161663,0.00006328246,0.001646158,0.0000109306775],"about_ca_topic_score_codex":0.075062126,"about_ca_topic_score_gemma":0.069173984,"teacher_disagreement_score":0.075062126,"about_ca_system_score_codex":0.0008989362,"about_ca_system_score_gemma":0.00063155004,"threshold_uncertainty_score":0.14925045},"labels":[],"label_agreement":null},{"id":"W2886545044","doi":"10.1029/2018gl079133","title":"On the Emergence of Anthropogenic Signal in Extreme Precipitation Change Over China","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China; China Scholarship Council; National Natural Science Foundation of China; Agence Nationale de la Recherche","keywords":"Coupled model intercomparison project; Precipitation; Climate change; Environmental science; Climatology; China; Climate model; Climate system; Meteorology; Geology; Geography; Oceanography","score_opus":0.13600548959751402,"score_gpt":0.34601910446360307,"score_spread":0.21001361486608905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2886545044","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999106,0.00003247218,0.00025812347,0.00007983308,0.0000027718604,0.000001988572,0.00007996452,0.0000067804035,0.00043194045],"genre_scores_gemma":[0.9998554,0.000013310326,0.000028988703,0.000004802757,0.000002233647,7.027879e-7,0.000062979845,7.4974724e-7,0.000030770334],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985385,0.000033986526,0.00000960065,0.000042729393,0.000028075023,0.000031679137],"domain_scores_gemma":[0.99865806,0.00049862347,0.00035624157,0.000080125734,0.00026012634,0.0001469023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082297745,0.00015585047,0.00016680684,0.0005001194,0.0002604088,0.00046247177,0.00022965316,0.00025925983,0.0010671187],"category_scores_gemma":[0.002430796,0.00014789937,0.00022871113,0.0005018316,0.0004526812,0.00039685203,0.00041784343,0.000261925,0.000069303336],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031373036,0.00006541936,0.9429162,0.000037448455,0.00012101578,0.0004896293,0.00016517266,0.03987309,0.006161728,0.0017386259,0.0004628267,0.0076551135],"study_design_scores_gemma":[0.00001651856,0.000076004864,0.934925,0.000007516183,0.000028601127,0.000057194426,0.00012765436,0.06271211,0.001077951,0.0005888281,0.00036789058,0.0000147740775],"about_ca_topic_score_codex":0.012524646,"about_ca_topic_score_gemma":0.010446618,"teacher_disagreement_score":0.012524646,"about_ca_system_score_codex":0.0005865196,"about_ca_system_score_gemma":0.0003773896,"threshold_uncertainty_score":0.024903476},"labels":[],"label_agreement":null},{"id":"W2887305584","doi":"10.1029/2018gl078780","title":"Distribution of Vapor and Condensate in a Hydrothermal System: Insights From Self‐Potential Inversion at Mount Tongariro, New Zealand","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Volcano; Hydrothermal circulation; Geology; Groundwater; Inversion (geology); Mount; Permeability (electromagnetism); Petrology; Characterisation of pore space in soil; Geomorphology; Geophysics; Hydraulic conductivity; Groundwater flow; Magnetotellurics; Mineralogy; Geochemistry; Soil science; Seismology; Electrical resistivity and conductivity; Geotechnical engineering; Aquifer; Porosity; Chemistry","score_opus":0.018769937070969748,"score_gpt":0.2606748564996574,"score_spread":0.24190491942868764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887305584","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99885845,0.000017018549,0.00024465742,0.000017944272,8.249949e-7,0.0000040120535,0.00021045198,0.000014628518,0.0006320138],"genre_scores_gemma":[0.99954706,0.00001216134,0.0001919149,0.000002099317,6.8099297e-7,0.000001978148,0.0001142783,0.0000035708645,0.00012612678],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993944,0.0000040556247,0.0000036685947,0.000019001414,0.000018008734,0.00001585638],"domain_scores_gemma":[0.999853,0.000023134467,0.00003648456,0.000010583653,0.000050378225,0.000026388185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011095694,0.00015546562,0.0002193565,0.00069126283,0.00037163138,0.00052570255,0.00040873434,0.00020953458,0.00084590854],"category_scores_gemma":[0.0006074373,0.00019473865,0.0001989821,0.00072943134,0.00045349903,0.0003971957,0.00041537874,0.00018632862,0.00009888824],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029545915,0.0000751202,0.8050665,0.000092620336,0.00010466423,0.00086857827,0.0026616848,0.008627359,0.16109703,0.00043556254,0.00051383855,0.020161571],"study_design_scores_gemma":[0.00001928468,0.000023331284,0.97787786,0.000006343864,0.00001778853,0.00007136881,0.00041972028,0.018821044,0.0022879199,0.00006869601,0.0003679809,0.000018531806],"about_ca_topic_score_codex":0.32587498,"about_ca_topic_score_gemma":0.35643002,"teacher_disagreement_score":0.32587498,"about_ca_system_score_codex":0.0010602766,"about_ca_system_score_gemma":0.0005298905,"threshold_uncertainty_score":0.6479564},"labels":[],"label_agreement":null},{"id":"W2887424155","doi":"10.1029/2018gl079027","title":"Faults and Non‐Double‐Couple Components for Induced Earthquakes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; Geological Survey of Canada; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey","keywords":"Induced seismicity; Geology; Seismology; Tectonics; Hydraulic fracturing; Thrust fault; Fault (geology); Focal mechanism; Slip (aerodynamics); Structural basin; Geomorphology; Geotechnical engineering","score_opus":0.08624623253716447,"score_gpt":0.3245176244466853,"score_spread":0.23827139190952085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2887424155","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981207,0.00006211488,0.0010043165,0.000014047131,0.0000018566693,0.0000072754033,0.000070742186,0.000013659816,0.00070525386],"genre_scores_gemma":[0.9996112,0.000021624393,0.00018399535,0.0000017744187,0.0000027926044,0.000001924437,0.00007269718,0.0000020627417,0.00010200598],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999044,0.000010646315,0.000008184725,0.000017063167,0.000033656113,0.000026046971],"domain_scores_gemma":[0.9995136,0.00009183095,0.00019149604,0.00004365181,0.00008032863,0.000079112746],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015542975,0.0002647707,0.00015408985,0.0013253391,0.00018274783,0.0003880495,0.00016115532,0.00014621642,0.0014974452],"category_scores_gemma":[0.000903668,0.00012373249,0.00021071383,0.0006988608,0.00026046715,0.00027446437,0.00038498806,0.00013973305,0.00010325531],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030072598,0.000090383655,0.90191406,0.00008596918,0.00011831184,0.00044929312,0.00039554312,0.005334976,0.05852473,0.0011277526,0.00023624634,0.031421993],"study_design_scores_gemma":[0.000004517062,0.000025581287,0.9905095,0.0000029703788,0.00001635111,0.00012076745,0.00010181819,0.00746404,0.0014277678,0.00015521378,0.0001664364,0.000005088618],"about_ca_topic_score_codex":0.004974064,"about_ca_topic_score_gemma":0.010958559,"teacher_disagreement_score":0.004974064,"about_ca_system_score_codex":0.000330421,"about_ca_system_score_gemma":0.00021593747,"threshold_uncertainty_score":0.009890258},"labels":[],"label_agreement":null},{"id":"W2888102960","doi":"10.1002/2016gl069872","title":"Current‐driven Langmuir oscillations and formation of wave packets via modulational instability: Relevance to STEREO observations","year":2016,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Modulational instability; Physics; Langmuir Turbulence; Plasma oscillation; Instability; Solar wind; Plasma; Electron; Electric field; Population; Atomic physics; Computational physics; Waves in plasmas; Two-stream instability; Mechanics","score_opus":0.04714352415975041,"score_gpt":0.30392243981526973,"score_spread":0.2567789156555193,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888102960","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97845775,0.0001800493,0.015732799,0.00025747082,0.000022004497,0.000015513873,0.00006424308,0.00014600708,0.005124004],"genre_scores_gemma":[0.9989806,0.000035071054,0.0007731085,0.000013579273,0.0000064434557,0.000002932123,0.000013909809,0.0000042996985,0.00017007413],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997437,0.000004442734,9.565645e-7,0.0000038378103,0.000009567273,0.000006847922],"domain_scores_gemma":[0.9998702,0.00003452869,0.0000420742,0.0000150336855,0.000023526969,0.000014629544],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010075847,0.00009716079,0.00008860683,0.00018728404,0.00015163097,0.00020715831,0.000214472,0.0002021674,0.0011286363],"category_scores_gemma":[0.00041022236,0.00007269389,0.0001012803,0.00011894893,0.00024505384,0.0003474359,0.00020314903,0.0002140328,0.00008722167],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081562257,0.00037628537,0.05666813,0.00026853362,0.00007056276,0.00161777,0.000539205,0.09740678,0.7013053,0.0841967,0.003093274,0.053641856],"study_design_scores_gemma":[0.00011048721,0.0001920988,0.037258036,0.000014004309,0.000015688764,0.00041321878,0.00019673776,0.9002624,0.035162617,0.024405733,0.0019294455,0.000039597882],"about_ca_topic_score_codex":0.00046757446,"about_ca_topic_score_gemma":0.00023246398,"teacher_disagreement_score":0.0011286363,"about_ca_system_score_codex":0.00018998478,"about_ca_system_score_gemma":0.00009334493,"threshold_uncertainty_score":0.0037757158},"labels":[],"label_agreement":null},{"id":"W2888348179","doi":"10.1029/2018gl078509","title":"On the Origin of STEVE: Particle Precipitation or Ionospheric Skyglow?","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; Canadian Space Agency; University of Calgary; National Science Foundation","keywords":"Ionosphere; Sky; Satellite; Precipitation; Night sky; Electron precipitation; Airglow; Geology; Physics; Astronomy; Geophysics; Meteorology; Magnetosphere; Plasma","score_opus":0.032197488506551394,"score_gpt":0.3218697040835833,"score_spread":0.2896722155770319,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888348179","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970079,0.00036143317,0.0012176328,0.000093042894,0.000011152371,0.0000062420636,0.000119897915,0.000017027942,0.0011655901],"genre_scores_gemma":[0.9995303,0.00008813658,0.0001721045,0.00001558046,0.000016422538,0.0000014518658,0.000087007465,0.000002494462,0.000086413565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999548,0.0000047184644,0.000004066105,0.000011351796,0.000008002066,0.000017121145],"domain_scores_gemma":[0.99975294,0.000055313412,0.00011159165,0.000022163556,0.00003057168,0.00002738698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013687102,0.0001049352,0.00024150134,0.00046694643,0.00028108593,0.00039943424,0.00015020533,0.00028632922,0.00055786833],"category_scores_gemma":[0.0003937927,0.000053734388,0.00018257035,0.00049855345,0.00040917078,0.000364875,0.00038436282,0.00020931593,0.00009058316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000378122,0.000055123906,0.94492036,0.000074585274,0.000084762934,0.0022380396,0.00057831424,0.0022142364,0.030300513,0.002052228,0.0007537898,0.016349817],"study_design_scores_gemma":[0.0000047824624,0.0000434544,0.9905861,0.000011998424,0.00001601656,0.00044861314,0.00035680484,0.0043935836,0.0024267482,0.00052274216,0.0011808126,0.000008247624],"about_ca_topic_score_codex":0.0020701697,"about_ca_topic_score_gemma":0.0031059934,"teacher_disagreement_score":0.0020701697,"about_ca_system_score_codex":0.00017605905,"about_ca_system_score_gemma":0.00005960129,"threshold_uncertainty_score":0.004116297},"labels":[],"label_agreement":null},{"id":"W2888352368","doi":"10.1029/2018gl079038","title":"Nonlinear Drift Resonance Between Charged Particles and Ultralow Frequency Waves: Theory and Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Japan Society for the Promotion of Science London","keywords":"Physics; Resonance (particle physics); Nonlinear system; Magnetosphere; Computational physics; Nonlinear resonance; Amplitude; Classical mechanics; Quantum electrodynamics; Particle (ecology); Observable; Charged particle; Geophysics; Statistical physics; Atomic physics; Quantum mechanics; Ion; Plasma; Geology","score_opus":0.029156896470832486,"score_gpt":0.2966700609079687,"score_spread":0.26751316443713624,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888352368","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9424441,0.0013805028,0.045984585,0.00032488402,0.000022571483,0.000026930593,0.00014265548,0.00027978816,0.009394002],"genre_scores_gemma":[0.9966434,0.000148951,0.0029566507,0.000014492908,0.000008848596,0.0000049813393,0.000038360602,0.0000052988976,0.00017902884],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999959,0.000007597769,0.0000015215956,0.000011214626,0.000014146283,0.000006457774],"domain_scores_gemma":[0.9998981,0.000051252508,0.000018809915,0.000014875342,0.000008030633,0.000008986816],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018838783,0.00017776717,0.00017494004,0.00030420697,0.00018310155,0.00029376103,0.00053637277,0.0004644755,0.00038211464],"category_scores_gemma":[0.00035005595,0.00014668885,0.000121489975,0.00023859381,0.00058333745,0.0005333394,0.00051722216,0.00044434352,0.00007829179],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000647186,0.0002687152,0.108314864,0.00059838255,0.00013112306,0.0015508581,0.00136646,0.14244981,0.5224702,0.15411413,0.0025396587,0.06554863],"study_design_scores_gemma":[0.00011176204,0.00016014763,0.058975283,0.000050965547,0.000029914821,0.0003535063,0.00019984404,0.84486747,0.042388972,0.048266564,0.0045354264,0.000060110142],"about_ca_topic_score_codex":0.0007647007,"about_ca_topic_score_gemma":0.00040016128,"teacher_disagreement_score":0.0007647007,"about_ca_system_score_codex":0.00025935698,"about_ca_system_score_gemma":0.000083313025,"threshold_uncertainty_score":0.0018817782},"labels":[],"label_agreement":null},{"id":"W2888575256","doi":"10.1029/2018gl079306","title":"Temporal Dynamics of Aerodynamic Canopy Height Derived From Eddy Covariance Momentum Flux Data Across North American Flux Networks","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Guelph; McMaster University","funders":"Office of Science; U.S. Department of Energy","keywords":"Eddy covariance; Environmental science; Canopy; Atmospheric sciences; Flux (metallurgy); Vegetation (pathology); Grassland; Climatology; Ecosystem; Geology; Geography; Ecology","score_opus":0.02574920876353207,"score_gpt":0.2970075352166841,"score_spread":0.271258326453152,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888575256","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984914,0.000041801522,0.0004678957,0.000022140657,0.0000023757386,0.0000030933627,0.0006021488,0.000015614189,0.0003534679],"genre_scores_gemma":[0.9983652,0.000028261471,0.0004057267,0.000005828092,0.0000026580876,0.000006020882,0.0010891524,0.0000033398728,0.00009387988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997677,0.00007508334,0.000018080029,0.00006886711,0.00003950808,0.000030729334],"domain_scores_gemma":[0.9984469,0.000601411,0.00033770074,0.00012768952,0.0004345426,0.000051832827],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010744863,0.00016867992,0.00018150374,0.0009447168,0.00027017813,0.00059133035,0.00020852688,0.00024556209,0.00045037142],"category_scores_gemma":[0.002379141,0.0001447079,0.0001653531,0.0011710586,0.00016055393,0.0004991462,0.00029523397,0.00018749022,0.00008140715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000076132324,0.000044576256,0.9778281,0.000019326615,0.00009500689,0.000040544546,0.00019849843,0.007260442,0.0015409169,0.0001658197,0.0005416754,0.012189069],"study_design_scores_gemma":[0.000001943068,0.000008238352,0.98627895,0.000005949224,0.000018109735,0.000012378559,0.00010612312,0.012908625,0.00023346675,0.000077551864,0.00034306917,0.000005570384],"about_ca_topic_score_codex":0.04981364,"about_ca_topic_score_gemma":0.082712375,"teacher_disagreement_score":0.04981364,"about_ca_system_score_codex":0.00040221596,"about_ca_system_score_gemma":0.00027656657,"threshold_uncertainty_score":0.09904736},"labels":[],"label_agreement":null},{"id":"W2888771143","doi":"10.1029/2018gl078568","title":"Changes in Deep Water Oxygenation of the South China Sea Since the Last Glacial Period","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Youth Innovation Promotion Association of the Chinese Academy of Sciences; Chinese Academy of Sciences; Natural Science Foundation of Guangdong Province; National Natural Science Foundation of China","keywords":"Oceanography; Geology; Last Glacial Maximum; North Atlantic Deep Water; Deep sea; Glacial period; Period (music); Benthic zone; Circumpolar deep water; Deep water; Stadial; Climatology; Holocene; Paleontology","score_opus":0.023488472112564798,"score_gpt":0.2698002257965081,"score_spread":0.24631175368394329,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888771143","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930465,0.00012573799,0.000013964066,0.000041855998,0.0000054396123,0.0000012681894,0.00020622414,0.000001334734,0.00029953173],"genre_scores_gemma":[0.9993418,0.00011125021,0.000018107725,0.000015950978,0.0000069929383,0.000001894387,0.00030958737,9.414564e-7,0.00019339957],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992955,0.0000075951107,0.000009391133,0.000020696789,0.000014103731,0.000018636769],"domain_scores_gemma":[0.99962986,0.000029176012,0.00014403427,0.00002223191,0.00009406157,0.00008063533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029025742,0.00023745817,0.00016653062,0.00079280837,0.0003746497,0.00046343464,0.00015578243,0.00024143205,0.00092650176],"category_scores_gemma":[0.000533817,0.00012082486,0.00021644375,0.0013383809,0.00032378634,0.0003235537,0.00039200086,0.00022823451,0.00011865732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038594542,0.0000057708835,0.9946392,0.000015971666,0.000052773066,0.0000835303,0.0003187921,0.000095842515,0.001571055,0.000037124573,0.000108346205,0.0030329095],"study_design_scores_gemma":[0.0000010040939,0.000006002661,0.9995988,0.0000017582779,0.000005763434,0.000012857488,0.000097807206,0.00004128605,0.000054525455,0.0000064886917,0.00017274036,9.5365885e-7],"about_ca_topic_score_codex":0.03300415,"about_ca_topic_score_gemma":0.061274137,"teacher_disagreement_score":0.03300415,"about_ca_system_score_codex":0.000687667,"about_ca_system_score_gemma":0.00052388303,"threshold_uncertainty_score":0.06562412},"labels":[],"label_agreement":null},{"id":"W2888894196","doi":"10.1029/2018gl080083","title":"Last Century Warming Over the Canadian Atlantic Shelves Linked to Weak Atlantic Meridional Overturning Circulation","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University of Victoria","keywords":"Shutdown of thermohaline circulation; Oceanography; Climatology; Foraminifera; Geology; North Atlantic Deep Water; Latitude; Thermohaline circulation; Global warming; Climate change; Benthic zone; Environmental science","score_opus":0.03160385915841005,"score_gpt":0.2882602502246509,"score_spread":0.25665639106624083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888894196","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99376243,0.00064401835,0.00006144062,0.00029978156,0.000017260765,0.000003791694,0.002797842,0.000011014257,0.0024023822],"genre_scores_gemma":[0.99857724,0.00026333221,0.000052317777,0.000042268784,0.000009094415,0.0000016048477,0.0007202437,0.0000024132987,0.00033148637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998449,0.0000055986293,0.000008307914,0.00003618429,0.0000469628,0.000058027275],"domain_scores_gemma":[0.9988212,0.00004727221,0.00026203835,0.000047528065,0.0006750049,0.00014685626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028559525,0.00018006576,0.00017663091,0.0013452626,0.001390799,0.0007663158,0.0003579922,0.0002228566,0.001744652],"category_scores_gemma":[0.00080039544,0.00009249034,0.00021178437,0.002050326,0.00048178175,0.0002365588,0.00046430464,0.00030039804,0.00009453281],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003732731,0.0000056782433,0.991557,0.00002072822,0.000060943676,0.00006529528,0.00025549487,0.0001634464,0.0013279812,0.00013411157,0.0008201861,0.005551801],"study_design_scores_gemma":[5.707377e-7,0.0000013662384,0.9991165,0.0000051470747,0.000007741765,0.000010847068,0.000096030206,0.00005856185,0.000062764455,0.0000075851294,0.0006309493,0.0000020614577],"about_ca_topic_score_codex":0.957639,"about_ca_topic_score_gemma":0.9821206,"teacher_disagreement_score":0.04236102,"about_ca_system_score_codex":0.004916495,"about_ca_system_score_gemma":0.0060835625,"threshold_uncertainty_score":0.08522093},"labels":[],"label_agreement":null},{"id":"W2888958070","doi":"10.1029/2018gl079419","title":"Retreat of the Western Cordilleran Ice Sheet Margin During the Last Deglaciation","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":107,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of the Fraser Valley; University of Northern British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Hakai Institute; Canada Foundation for Innovation; Tula Foundation","keywords":"Deglaciation; Geology; Ice sheet; Diachronous; Physical geography; Last Glacial Maximum; Oceanography; Glacial period; Geomorphology; Geography","score_opus":0.0261126350245721,"score_gpt":0.2793115010208905,"score_spread":0.25319886599631836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2888958070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99756974,0.00028135206,0.000028592623,0.00007675565,0.000006461443,0.0000028524164,0.00019115295,0.0000074020572,0.0018356075],"genre_scores_gemma":[0.9991584,0.000106652056,0.000047661648,0.000019183453,0.0000062054437,0.0000020265945,0.00018967743,0.0000026498835,0.00046750042],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990666,0.000007806883,0.0000052881223,0.00003112104,0.00001966343,0.000029514644],"domain_scores_gemma":[0.9996495,0.000024688607,0.00013485533,0.00001560888,0.00011493128,0.000060400598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002804507,0.00024932998,0.00014653381,0.00093070616,0.0007824536,0.00076151884,0.00020866115,0.0002591575,0.0016170724],"category_scores_gemma":[0.00072826864,0.00008481323,0.00010539037,0.00072636496,0.00032527052,0.00023310095,0.00045439322,0.00020638056,0.00017941503],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029769845,0.00001884971,0.9720029,0.000045316618,0.000046658108,0.0004615626,0.001143754,0.0004513631,0.0067993347,0.00015963076,0.0006512876,0.017921546],"study_design_scores_gemma":[0.0000015289955,0.000008310599,0.9986355,0.000007360339,0.0000046329355,0.00005103391,0.00013478265,0.00014540121,0.00023445683,0.000012389844,0.00076302903,0.000001682845],"about_ca_topic_score_codex":0.24562576,"about_ca_topic_score_gemma":0.39797434,"teacher_disagreement_score":0.24562576,"about_ca_system_score_codex":0.0016423496,"about_ca_system_score_gemma":0.0006928335,"threshold_uncertainty_score":0.4883921},"labels":[],"label_agreement":null},{"id":"W2889260993","doi":"10.1029/2018gl079073","title":"Sand Mineralogy Within the Bagnold Dunes, Gale Crater, as Observed In Situ and From Orbit","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"National Aeronautics and Space Administration","keywords":"Geology; Plagioclase; Impact crater; Mars Exploration Program; Aeolian processes; Igneous rock; Lava; Ilmenite; Basalt; Geomorphology; Olivine; Sand dune stabilization; Martian surface; Volcano; Bedform; Mineralogy; Martian; Geochemistry; Paleontology; Astrobiology; Quartz","score_opus":0.05244182688753209,"score_gpt":0.2954526506635905,"score_spread":0.2430108237760584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889260993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99870324,0.00004839348,0.000030590472,0.000008672219,0.0000013838761,0.0000036679824,0.00048224328,0.0000072155012,0.0007144236],"genre_scores_gemma":[0.998453,0.000058197926,0.00014235119,0.000014233753,0.000002342419,0.0000067249657,0.0006098003,0.000004492564,0.00070875825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995255,0.0000030012147,0.0000023480366,0.000016656593,0.000011757192,0.000013650605],"domain_scores_gemma":[0.9999256,0.0000063735724,0.000017723338,0.0000047456156,0.000017877104,0.000027609838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000532215,0.00022496074,0.00013337421,0.0013324382,0.00049917685,0.0005705982,0.00020887335,0.00022284704,0.0010328911],"category_scores_gemma":[0.00013729087,0.00017598302,0.000115560215,0.00063633826,0.00025266086,0.00017535756,0.000377578,0.00013512773,0.00015557164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023610923,0.000035611858,0.906163,0.000049688297,0.000088479515,0.0003448328,0.0014520232,0.00039516087,0.08133522,0.00007605591,0.0004655165,0.009358347],"study_design_scores_gemma":[0.0000015994278,0.000006565363,0.99900657,0.0000019220518,0.0000028146023,0.000023740702,0.00015683845,0.00006186017,0.00046148806,0.000002771394,0.00027279335,0.0000010398201],"about_ca_topic_score_codex":0.053208157,"about_ca_topic_score_gemma":0.17716482,"teacher_disagreement_score":0.053208157,"about_ca_system_score_codex":0.00065629906,"about_ca_system_score_gemma":0.00021560625,"threshold_uncertainty_score":0.10579693},"labels":[],"label_agreement":null},{"id":"W2889652082","doi":"10.1029/2018gl078748","title":"Mineral Weathering and the Permafrost Carbon‐Climate Feedback","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; University of Alberta","funders":"Environment Canada; Alberta Innovates; Natural Resources Canada; University of Alberta; Natural Sciences and Engineering Research Council of Canada; Arctic Institute of North America","keywords":"Thermokarst; Permafrost; Weathering; Carbonate; Arctic; Earth science; Geology; Carbon cycle; Carbon dioxide; Environmental chemistry; Sulfuric acid; Ocean acidification; Environmental science; Geochemistry; Climate change; Oceanography; Ecosystem; Chemistry; Ecology; Inorganic chemistry","score_opus":0.04692128193484107,"score_gpt":0.2908194674886854,"score_spread":0.24389818555384435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2889652082","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940148,0.00066533574,0.0005886062,0.0004349035,0.000016234133,0.0000041204885,0.00026999664,0.00005319917,0.0039527914],"genre_scores_gemma":[0.9993648,0.00015844313,0.00013053589,0.000028897211,0.0000032079486,6.2189457e-7,0.00003777972,0.0000033779768,0.0002723631],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.0000043666196,0.0000020312905,0.000009682616,0.000018673345,0.000027196125],"domain_scores_gemma":[0.9999013,0.000012236372,0.000017697474,0.0000041084313,0.00004025098,0.000024461324],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010549212,0.00020218204,0.00016560509,0.00027120195,0.0007684939,0.00047446112,0.00020971765,0.0002718893,0.0015172275],"category_scores_gemma":[0.00020878413,0.000105964566,0.00011118858,0.00029401435,0.0004052884,0.00027427025,0.0003050562,0.00017160966,0.00009824301],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006848667,0.00008359273,0.35669446,0.00027311855,0.0001585056,0.0010021484,0.00075331534,0.02759459,0.55757576,0.007254052,0.002354746,0.045570787],"study_design_scores_gemma":[0.000025619112,0.000081157676,0.93639106,0.000020903011,0.00006488083,0.00026708256,0.0012459275,0.020911178,0.02604191,0.0041668047,0.010740419,0.000043005162],"about_ca_topic_score_codex":0.42852512,"about_ca_topic_score_gemma":0.58802193,"teacher_disagreement_score":0.42852512,"about_ca_system_score_codex":0.003066564,"about_ca_system_score_gemma":0.0020508568,"threshold_uncertainty_score":0.8520616},"labels":[],"label_agreement":null},{"id":"W2890007213","doi":"10.1029/2018gl078971","title":"Warming From Recent Marine Heatwave Lingers in Deep British Columbia Fjord","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":91,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; University of British Columbia","funders":"NOAA Research; Center for Sponsored Coastal Ocean Research; NOAA Pacific Marine Environmental Laboratory; Climate Program Office; Hakai Institute; National Oceanic and Atmospheric Administration; University of British Columbia; Fisheries and Oceans Canada; Mitacs; Tula Foundation; U.S. Department of Commerce","keywords":"Argo; Oceanography; Fjord; Sill; Geology; Inlet; Marine ecosystem; Shoaling and schooling; Environmental science; Ecosystem; Climatology","score_opus":0.022564987311724745,"score_gpt":0.2629069537321783,"score_spread":0.24034196642045358,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890007213","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972433,0.00012810717,0.000017130695,0.00013267536,0.000006775861,0.000002587066,0.0009359329,0.0000054888133,0.0015279821],"genre_scores_gemma":[0.9981762,0.00010871511,0.000025644229,0.00006686479,0.0000035714468,0.000004094551,0.00067804503,0.000003046674,0.0009337085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998648,0.000007936203,0.000008148366,0.00003529407,0.000030836833,0.000052942316],"domain_scores_gemma":[0.99953556,0.000030636882,0.0000914699,0.000024919013,0.00020051052,0.00011688761],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014946995,0.00015231351,0.00020335134,0.0007241909,0.0013638189,0.0012213745,0.00033850374,0.00041272552,0.0025983762],"category_scores_gemma":[0.00067753834,0.0001452908,0.00013604101,0.0013809438,0.00047115667,0.00026400844,0.0006596797,0.00046744494,0.0002608444],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059034235,0.000021185608,0.9906262,0.00001661281,0.000035194756,0.00012464922,0.0006260731,0.00015130675,0.0013794148,0.0000424712,0.0010977592,0.005819987],"study_design_scores_gemma":[7.1003143e-7,0.0000014263178,0.99924743,0.000004269836,0.000002821719,0.000007967244,0.0003135191,0.00002487579,0.000023354585,0.0000034394407,0.00036863395,0.0000015075424],"about_ca_topic_score_codex":0.93911815,"about_ca_topic_score_gemma":0.97982657,"teacher_disagreement_score":0.060881853,"about_ca_system_score_codex":0.0055185826,"about_ca_system_score_gemma":0.0034958338,"threshold_uncertainty_score":0.12248075},"labels":[],"label_agreement":null},{"id":"W2890325955","doi":"10.1029/2018gl078857","title":"Global Distribution of ULF Waves During Magnetic Storms: Comparison of Arase, Ground Observations, and BATSRUS + CRCM Simulation","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Russian Academy of Sciences; Goddard Space Flight Center; Sveriges Geologiska Undersökning; Ministry of Science and Higher Education of the Russian Federation; Siberian Branch, Russian Academy of Sciences; Danmarks Tekniske Universitet; Japan Society for the Promotion of Science; Russian Foundation for Basic Research; Japan Aerospace Exploration Agency; National Institute of Polar Research; Alberta Agricultural Research Institute","keywords":"Physics; Ultra low frequency; Solar wind; Geophysics; Electron; Magnetosphere; Computational physics; Magnetic field; Astronomy","score_opus":0.03047977512613762,"score_gpt":0.3278964125063921,"score_spread":0.2974166373802545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890325955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99445975,0.000046539422,0.0012665883,0.00011937179,0.000016989881,0.000015833048,0.0006853674,0.00021072837,0.0031789173],"genre_scores_gemma":[0.9978999,0.000028712553,0.00093531824,0.000022044047,0.000008477739,0.000013550839,0.0008317199,0.000034173503,0.00022613678],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998903,0.000029754441,0.0000061837677,0.000022587552,0.000016978129,0.000034174984],"domain_scores_gemma":[0.99963677,0.00014697897,0.000052292635,0.000043416374,0.00006555889,0.000054967666],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033184918,0.0004546575,0.00046158186,0.00048419024,0.00029677624,0.00045628438,0.0007028419,0.00089547486,0.0013587906],"category_scores_gemma":[0.0010877657,0.00024171144,0.00061472936,0.0004955348,0.00038087106,0.000418046,0.00038217692,0.00050213805,0.00016756692],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013645194,0.000085761996,0.026343567,0.000023251323,0.0000633634,0.0001540103,0.00005884153,0.9677213,0.001556705,0.00061832136,0.0008329113,0.0024055117],"study_design_scores_gemma":[0.000073420924,0.000038785198,0.007553716,0.000004280251,0.000015372496,0.000016524948,0.000043009986,0.99141484,0.0004137303,0.00013465439,0.00028204528,0.0000096204485],"about_ca_topic_score_codex":0.027567005,"about_ca_topic_score_gemma":0.012082114,"teacher_disagreement_score":0.027567005,"about_ca_system_score_codex":0.00059726444,"about_ca_system_score_gemma":0.0005138725,"threshold_uncertainty_score":0.054813087},"labels":[],"label_agreement":null},{"id":"W2890765287","doi":"10.1029/2018gl079045","title":"Water Abundance of Dunes in Gale Crater, Mars From Active Neutron Experiments and Implications for Amorphous Phases","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Connecticut Space Grant College Consortium; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Impact crater; Geology; Basalt; Amorphous solid; Volcano; Abundance (ecology); Albedo (alchemy); Crater lake; Neutron; Mineralogy; Astrobiology; Geochemistry; Chemistry; Physics","score_opus":0.0550222385648539,"score_gpt":0.3507869367665612,"score_spread":0.2957646982017073,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890765287","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99952877,0.000058741047,0.000047919457,0.000007107263,8.73557e-7,9.556369e-7,0.00013588907,0.000005315059,0.00021443573],"genre_scores_gemma":[0.9996362,0.000048016096,0.00010403654,0.0000050460735,0.000002008616,0.0000013176784,0.00012633113,0.0000023466446,0.00007474293],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999156,0.000010311008,0.0000058016185,0.000032238026,0.000019253857,0.000016725426],"domain_scores_gemma":[0.999869,0.000025520943,0.000035242858,0.000011500294,0.000033111577,0.00002560776],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011810285,0.0004149412,0.00025816562,0.002238131,0.00053892174,0.0006411114,0.00033484728,0.0003397742,0.0008838418],"category_scores_gemma":[0.0002342575,0.00024535684,0.00015450503,0.00055245915,0.00047256178,0.00036467696,0.00040099217,0.00015104252,0.00012268944],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049300725,0.00004543448,0.67205805,0.00009632332,0.00017766551,0.00048659762,0.00064309465,0.0014288173,0.31524652,0.000107850254,0.00016528941,0.009051419],"study_design_scores_gemma":[0.0000071621425,0.000034514058,0.98930055,0.0000055328123,0.000018398105,0.00015101755,0.00022943142,0.001086864,0.008730487,0.000029203278,0.00040018512,0.0000067307456],"about_ca_topic_score_codex":0.013165735,"about_ca_topic_score_gemma":0.018794127,"teacher_disagreement_score":0.013165735,"about_ca_system_score_codex":0.0004760217,"about_ca_system_score_gemma":0.00008010435,"threshold_uncertainty_score":0.02617824},"labels":[],"label_agreement":null},{"id":"W2890953917","doi":"10.1029/2018gl079081","title":"A Numerical Model for Twin Nucleation in Shocked Zircon and Comparison With Natural Samples","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Zircon; Nucleation; Geology; Shock metamorphism; Metamorphism; Shock (circulatory); Impact structure; Crust; Metamictization; Stress (linguistics); Geophysics; Petrology; Meteorite; Geochemistry; Impact crater; Astrobiology; Physics; Thermodynamics","score_opus":0.052040792729096674,"score_gpt":0.3137940702999393,"score_spread":0.2617532775708426,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2890953917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94133943,0.0001358308,0.051058464,0.00018510058,0.00004508702,0.000073919124,0.00048768483,0.00020288823,0.0064715045],"genre_scores_gemma":[0.99093866,0.00006291614,0.0075097554,0.000024525973,0.000007693638,0.000051352563,0.00015995398,0.000030551633,0.0012145233],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989116,0.000020480997,0.000008326771,0.000024557841,0.000030260406,0.000025124351],"domain_scores_gemma":[0.9995142,0.00022534387,0.00007760237,0.000048178204,0.000094522315,0.000040152063],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036711554,0.0002864302,0.0003937548,0.00051220955,0.00048678386,0.00080057245,0.0011693661,0.001045097,0.0018432015],"category_scores_gemma":[0.0015826585,0.00032078693,0.00054393633,0.00039016808,0.00071680837,0.0004856567,0.0004455209,0.0004078938,0.00015509842],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023433811,0.000027309148,0.0024070288,0.000011155975,0.000010240481,0.000055857912,0.000021177993,0.993008,0.0017964988,0.0019579013,0.000059078287,0.0006224336],"study_design_scores_gemma":[0.0000040330933,0.000005951023,0.0002557595,0.0000012289476,0.0000014587671,0.000004463146,0.0000052887767,0.99927145,0.00020337674,0.00019149219,0.000053122498,0.0000022920951],"about_ca_topic_score_codex":0.019147903,"about_ca_topic_score_gemma":0.007846106,"teacher_disagreement_score":0.019147903,"about_ca_system_score_codex":0.001168615,"about_ca_system_score_gemma":0.000687121,"threshold_uncertainty_score":0.038072884},"labels":[],"label_agreement":null},{"id":"W2891947925","doi":"10.1029/2018gl079598","title":"Seasonal Variations in Airflow Over the Namib Dune, Gale Crater, Mars: Implications for Dune Dynamics","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Natural Environment Research Council; Sight Research UK; Ulster University; National Aeronautics and Space Administration","keywords":"Aeolian processes; Geology; Mars Exploration Program; Bedform; Mesoscale meteorology; Airflow; Sand dune stabilization; Geomorphology; Sediment; Oceanography; Sediment transport; Astrobiology","score_opus":0.02576761117320589,"score_gpt":0.3095555349793522,"score_spread":0.28378792380614626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2891947925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999302,0.00004320946,0.000055146174,0.000027158023,0.000002797388,0.000002237232,0.00020986424,0.000011769022,0.00034584105],"genre_scores_gemma":[0.99970406,0.00002856232,0.00007241682,0.0000037336881,0.0000028704353,0.0000029309183,0.00011268329,0.0000017639082,0.000071071845],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.0000069577814,0.0000025978186,0.000011502236,0.0000059781155,0.000013325939],"domain_scores_gemma":[0.9999131,0.000020765528,0.000017920851,0.000007155257,0.000017036877,0.000024108589],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012400995,0.00019007754,0.00015755325,0.000630254,0.00029690214,0.0005459035,0.00015728576,0.0002630765,0.0012186993],"category_scores_gemma":[0.000346215,0.00009350984,0.00015945468,0.00043502531,0.0001994627,0.00024762045,0.00029675246,0.00014014375,0.000095256],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003122566,0.000068433335,0.95401984,0.000053332842,0.00007892547,0.00034098662,0.0006951657,0.003866976,0.017556924,0.00012206717,0.00043230742,0.022452725],"study_design_scores_gemma":[0.0000032147893,0.000009519112,0.99749714,0.0000035718024,0.000004024535,0.000018641571,0.00013301156,0.0019016586,0.00016421307,0.0000106335765,0.00025202893,0.0000023229572],"about_ca_topic_score_codex":0.026268892,"about_ca_topic_score_gemma":0.030661423,"teacher_disagreement_score":0.026268892,"about_ca_system_score_codex":0.0004400761,"about_ca_system_score_gemma":0.00013958603,"threshold_uncertainty_score":0.052231967},"labels":[],"label_agreement":null},{"id":"W2892099838","doi":"10.1029/2018gl078841","title":"No Impact of Anthropogenic Aerosols on Early 21st Century Global Temperature Trends in a Large Initial‐Condition Ensemble","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Radiative forcing; Climatology; Forcing (mathematics); Pacific decadal oscillation; Spurious relationship; Environmental science; Climate model; Climate system; Atlantic multidecadal oscillation; Aerosol; Atmospheric sciences; Climate change; El Niño Southern Oscillation; Meteorology; North Atlantic oscillation; Geography; Geology; Oceanography; Mathematics","score_opus":0.021452091318471065,"score_gpt":0.331030117513105,"score_spread":0.3095780261946339,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892099838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99668014,0.000052986907,0.00083165214,0.00017192138,0.000044772347,0.000005927507,0.000859668,0.000038715807,0.0013141779],"genre_scores_gemma":[0.9985934,0.000015848482,0.00018347034,0.000022074351,0.000009642319,0.0000034937289,0.00091872545,0.0000069465464,0.00024643846],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99968946,0.00009740388,0.000020771955,0.00009032155,0.00004425868,0.000057857906],"domain_scores_gemma":[0.9985682,0.00048036216,0.00012522555,0.00029658715,0.0003697238,0.00015984577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018256258,0.00027633543,0.00021346766,0.00016632654,0.0004470684,0.00064599083,0.00032790581,0.00033313455,0.0012188641],"category_scores_gemma":[0.004098403,0.00017567018,0.00048018713,0.00016965793,0.0002521062,0.0006130957,0.00051314954,0.00045765715,0.00019087394],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009473141,0.0002500655,0.7576064,0.00006323864,0.0010112071,0.00023913062,0.0001490435,0.20232344,0.008695476,0.0023137373,0.004908846,0.02149212],"study_design_scores_gemma":[0.000060872768,0.00021416938,0.5498333,0.00002136937,0.00025615052,0.000043314943,0.00014464694,0.43927658,0.0064779297,0.0009209242,0.002703638,0.000047156194],"about_ca_topic_score_codex":0.042335805,"about_ca_topic_score_gemma":0.05386696,"teacher_disagreement_score":0.042335805,"about_ca_system_score_codex":0.0005171672,"about_ca_system_score_gemma":0.0009012634,"threshold_uncertainty_score":0.084178746},"labels":[],"label_agreement":null},{"id":"W2892198682","doi":"10.1029/2018gl079777","title":"Substorm‐Associated Ionospheric Flow Fluctuations During the 27 March 2017 Magnetic Storm: SuperDARN‐Arase Conjunction","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"Japan Society for the Promotion of Science; Canada Foundation for Innovation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Substorm; Ionosphere; Geophysics; Magnetosphere; Geology; Mesoscale meteorology; Electric field; Ring current; Storm; Geomagnetic storm; Physics; Magnetic field; Earth's magnetic field; Climatology","score_opus":0.01589312548907616,"score_gpt":0.27314709308011714,"score_spread":0.25725396759104097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892198682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975285,0.000048448008,0.0001290073,0.00010125183,0.000022372762,0.000008183886,0.00040079077,0.000025996384,0.0017355129],"genre_scores_gemma":[0.99864966,0.000044501397,0.00016153077,0.000022744052,0.000032533306,0.0000049035802,0.00081243616,0.0000058979263,0.00026581273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998696,0.000013037116,0.000007094684,0.00002693664,0.000044684526,0.00003859504],"domain_scores_gemma":[0.9996288,0.00003484835,0.000097033524,0.00003689343,0.00010552746,0.000096932614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032740665,0.0001804826,0.00022183459,0.0005489411,0.00042624158,0.00036582167,0.00019818175,0.00023038346,0.00077171746],"category_scores_gemma":[0.0005647931,0.00007784148,0.00013317369,0.00046128652,0.00025557843,0.00022345898,0.00049999525,0.000374398,0.00018933522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013294296,0.00022281501,0.9070848,0.0000434277,0.0001677766,0.0022247282,0.0011321988,0.0032594875,0.046608254,0.00070289604,0.006670806,0.030553408],"study_design_scores_gemma":[0.000027465217,0.00009851904,0.9926023,0.0000058142227,0.00001789036,0.00015665284,0.00023979554,0.0026796767,0.001500281,0.00008676475,0.0025762042,0.000008578217],"about_ca_topic_score_codex":0.013048187,"about_ca_topic_score_gemma":0.027940048,"teacher_disagreement_score":0.013048187,"about_ca_system_score_codex":0.0005961248,"about_ca_system_score_gemma":0.00042255805,"threshold_uncertainty_score":0.025944471},"labels":[],"label_agreement":null},{"id":"W2892938895","doi":"10.1029/2018gl079110","title":"Greenland Submarine Melt Water Observed in the Labrador and Irminger Sea","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft","keywords":"Oceanography; Geology; Salinity; Submarine; Greenland ice sheet; Groenlandia; Water mass; Flux (metallurgy); Seawater; Climatology; Ice sheet","score_opus":0.03892745496818219,"score_gpt":0.2696449450584499,"score_spread":0.2307174900902677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892938895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99840957,0.00004214135,0.000019813908,0.000008594675,0.0000010238203,0.0000012280632,0.0011209169,0.000015224396,0.00038139932],"genre_scores_gemma":[0.99722147,0.000051163497,0.00007990943,0.000010045984,0.0000022784013,0.000003760657,0.0022951912,0.000004674709,0.00033154342],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999472,0.0000031417396,0.0000037324883,0.000016703014,0.000011032178,0.000018166122],"domain_scores_gemma":[0.99988925,0.0000059529248,0.00005817824,0.000007492862,0.000019626143,0.000019416668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011892533,0.00024159947,0.00013491284,0.0012951277,0.00019617984,0.00029522384,0.0001703142,0.00013791885,0.0004946098],"category_scores_gemma":[0.00015215688,0.000065878965,0.00016153348,0.0009765681,0.00017085177,0.00023659329,0.00028282384,0.000107075684,0.00017997222],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027809787,0.000026578315,0.97465646,0.00002977144,0.00009250567,0.00015025723,0.00036309182,0.00071291433,0.0089043025,0.00007446669,0.00083206524,0.013879477],"study_design_scores_gemma":[0.0000014763567,0.00001316052,0.99885416,0.000003098423,0.000006758432,0.000016129758,0.00006268051,0.00016939804,0.00049914606,0.0000056283598,0.00036660553,0.0000017835642],"about_ca_topic_score_codex":0.06202886,"about_ca_topic_score_gemma":0.120980754,"teacher_disagreement_score":0.06202886,"about_ca_system_score_codex":0.0008097343,"about_ca_system_score_gemma":0.00028721476,"threshold_uncertainty_score":0.1233356},"labels":[],"label_agreement":null},{"id":"W2892948131","doi":"10.1029/2018gl079327","title":"Strong Influence of Eddy Length on Boreal Summertime Extreme Precipitation Projections","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"York University; Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Climatology; Precipitation; Environmental science; Northern Hemisphere; Atmospheric sciences; Eddy covariance; Southern Hemisphere; Boreal; Subtropics; Geology; Meteorology; Geography; Ecosystem","score_opus":0.07833878880589244,"score_gpt":0.34446631480400075,"score_spread":0.2661275259981083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2892948131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974891,0.000064915024,0.00058473804,0.00010551529,0.000009235893,0.000002635608,0.00040808425,0.000038898284,0.0012968594],"genre_scores_gemma":[0.99939597,0.000027520366,0.00012917524,0.000009018543,0.0000047805393,0.0000010303975,0.00035264218,0.000006773361,0.00007311345],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99965036,0.0000960741,0.000023550327,0.00008330799,0.00009280844,0.000053840955],"domain_scores_gemma":[0.998723,0.0005121146,0.00023593246,0.000100350604,0.0003004476,0.00012811471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010214755,0.00022883131,0.00020931233,0.00031076543,0.00034381027,0.00086625747,0.0001992515,0.00019785039,0.0006864909],"category_scores_gemma":[0.0029575569,0.00018049206,0.00026375006,0.0002822404,0.00028954708,0.00042125993,0.000548104,0.00031198253,0.00009830439],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002465804,0.000040960607,0.9421045,0.000029061408,0.00022094663,0.000130013,0.00010882393,0.03750069,0.007761343,0.0006276106,0.00061481656,0.010614621],"study_design_scores_gemma":[0.000009151643,0.000033314493,0.9729393,0.000006861465,0.000018947858,0.000032950586,0.000048985105,0.025249885,0.0010023518,0.00019994356,0.00044577566,0.000012609855],"about_ca_topic_score_codex":0.032194152,"about_ca_topic_score_gemma":0.058678158,"teacher_disagreement_score":0.032194152,"about_ca_system_score_codex":0.00052620115,"about_ca_system_score_gemma":0.00051005394,"threshold_uncertainty_score":0.06401348},"labels":[],"label_agreement":null},{"id":"W2893438849","doi":"10.1029/2018gl079406","title":"Upper Mantle Seismic Structure of Alaska From Rayleigh and <i>S</i> Wave Tomography","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Geology; Seismology; Subduction; Lithosphere; Terrane; Intraplate earthquake; Mantle (geology); Seismic tomography; Crust; Volcano; Rayleigh wave; Slab; Geophysics; Tectonics; Surface wave","score_opus":0.01651020926988033,"score_gpt":0.24663366682446122,"score_spread":0.23012345755458088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893438849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99673766,0.00006704478,0.0005611666,0.000022049473,0.000003935783,0.0000021107835,0.00044285186,0.00004787911,0.002115235],"genre_scores_gemma":[0.9981236,0.00006726919,0.00075351476,0.0000042977067,0.0000018560197,0.0000017688827,0.0006521042,0.0000053761255,0.0003901899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999964,0.0000027812846,0.0000030117487,0.000012916271,0.000010488294,0.000006859479],"domain_scores_gemma":[0.9999094,0.000007768678,0.000018316467,0.000005867093,0.00004425609,0.000014402035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000106939966,0.00014082964,0.00008584842,0.00085696846,0.00026190776,0.00051187497,0.00012348038,0.00016702407,0.00093984447],"category_scores_gemma":[0.00028484798,0.00013304067,0.00009936948,0.0007645925,0.00017139594,0.00020705583,0.00040211,0.00011799073,0.0002358622],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029515548,0.00006432254,0.7779409,0.00008265633,0.000066598695,0.00065742346,0.0018125386,0.0076187393,0.15097064,0.00060352794,0.0009143019,0.05897317],"study_design_scores_gemma":[0.000006385234,0.000025801099,0.9859685,0.000027605143,0.000029341025,0.0002157483,0.00085841835,0.006139414,0.004969497,0.00014658611,0.00159963,0.000013143724],"about_ca_topic_score_codex":0.052805856,"about_ca_topic_score_gemma":0.09832773,"teacher_disagreement_score":0.052805856,"about_ca_system_score_codex":0.00024123599,"about_ca_system_score_gemma":0.00039382683,"threshold_uncertainty_score":0.10499698},"labels":[],"label_agreement":null},{"id":"W2893596885","doi":"10.1029/2018gl079500","title":"Continued Emissions of the Ozone‐Depleting Substance Carbon Tetrachloride From Eastern Asia","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Sight Research UK; Scheme for Promotion of Academic and Research Collaboration; Natural Environment Research Council; National Research Foundation of Korea; Department of Energy and Climate Change; National Aeronautics and Space Administration","keywords":"Ozone; Montreal Protocol; Environmental science; China; Troposphere; Carbon tetrachloride; Greenhouse gas; Atmospheric sciences; Chlorine; Geography; Ozone layer; Meteorology; Chemistry; Geology","score_opus":0.030447056500837986,"score_gpt":0.27005684276945463,"score_spread":0.23960978626861665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2893596885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99824274,0.0001040454,0.00012713004,0.00008795465,0.000003906995,0.0000027470196,0.00030712658,0.000006141762,0.0011182175],"genre_scores_gemma":[0.9986273,0.00013261352,0.000117665564,0.000048139907,0.000005513373,0.00000339004,0.00040888178,0.0000024884107,0.000654068],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986863,0.000010213617,0.000012822333,0.000037469545,0.000033164815,0.000037614616],"domain_scores_gemma":[0.99946195,0.00004856636,0.00018345627,0.00004447096,0.00021724871,0.000044380547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033959353,0.00024094501,0.00016727063,0.00047571983,0.0003670646,0.0007006377,0.00020956415,0.00018612316,0.00076027453],"category_scores_gemma":[0.00035116263,0.000136592,0.00029102358,0.0009883865,0.0002760068,0.0005574931,0.00044989918,0.00024319366,0.00013899524],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009091161,0.000029004053,0.96002233,0.00009380927,0.000091722395,0.00058877567,0.00092694437,0.0008747234,0.023519833,0.00044287418,0.0005580312,0.01276089],"study_design_scores_gemma":[0.0000021081876,0.000025141471,0.99521095,0.000013339361,0.000030842366,0.000076544515,0.0003825843,0.00047756862,0.0025005569,0.000056767298,0.0012172177,0.0000063106004],"about_ca_topic_score_codex":0.05587661,"about_ca_topic_score_gemma":0.055015363,"teacher_disagreement_score":0.05587661,"about_ca_system_score_codex":0.0008783826,"about_ca_system_score_gemma":0.001062564,"threshold_uncertainty_score":0.11110276},"labels":[],"label_agreement":null},{"id":"W2894152094","doi":"10.1029/2018gl078903","title":"Evidence for Radiative‐Convective Bistability in Tropical Atmospheres","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canadian Space Agency","keywords":"Convection; Atmospheric sciences; Outgoing longwave radiation; Longwave; Environmental science; Atmosphere (unit); Radiative transfer; Radiant energy; Greenhouse effect; Radiative cooling; Troposphere; Climate model; Climatology; Physics; Climate change; Meteorology; Global warming; Radiation; Geology","score_opus":0.1264230599465907,"score_gpt":0.3851859874987849,"score_spread":0.2587629275521942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894152094","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99676174,0.00007930379,0.0011343099,0.00011738025,0.0000069372236,0.000002233005,0.00012003877,0.00006641548,0.0017117689],"genre_scores_gemma":[0.99987245,0.000009169661,0.00006214081,0.000008513792,0.0000020389612,6.9365143e-7,0.000027867582,0.0000020332232,0.0000151805725],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998956,0.000017876688,0.000007339635,0.000019395284,0.000030243982,0.000029469935],"domain_scores_gemma":[0.9989692,0.00040374915,0.00025501152,0.00019368345,0.00007714305,0.00010125226],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021285872,0.00012591119,0.00016847,0.00028187654,0.00017318394,0.00042972428,0.00025375106,0.0002624557,0.0020414956],"category_scores_gemma":[0.0015823946,0.00018556268,0.00025733327,0.0002547544,0.00040450596,0.0003398706,0.00041438604,0.00025733255,0.00013145217],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011289851,0.00023503628,0.66503054,0.00018855369,0.00033177115,0.000917158,0.00055988226,0.033207837,0.2603105,0.011285094,0.0010872331,0.025717469],"study_design_scores_gemma":[0.00013638532,0.00015659546,0.8787981,0.000017457185,0.000087273525,0.00042903,0.00018154204,0.09692355,0.011760608,0.010707917,0.00075369526,0.00004792216],"about_ca_topic_score_codex":0.0020760067,"about_ca_topic_score_gemma":0.0015805629,"teacher_disagreement_score":0.0020760067,"about_ca_system_score_codex":0.000246335,"about_ca_system_score_gemma":0.0001283738,"threshold_uncertainty_score":0.0068294406},"labels":[],"label_agreement":null},{"id":"W2894677206","doi":"10.1029/2018gl079103","title":"Purple Auroral Rays and Global Pc1 Pulsations Observed at the CIR‐Associated Solar Wind Density Enhancement on 21 March 2017","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"Centre for Water Technology, Aarhus University; Japan Society for the Promotion of Science; Siberian Branch, Russian Academy of Sciences","keywords":"Magnetosphere; Local time; Physics; Geomagnetic storm; Solar wind; Ionosphere; Substorm; Geomagnetic latitude; Earth's magnetic field; Latitude; Geophysics; Night sky; Plasmasphere; Sky; Astrophysics; Atmospheric sciences; Astronomy; Plasma; Magnetic field","score_opus":0.0383285761711116,"score_gpt":0.3071420410723735,"score_spread":0.2688134649012619,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2894677206","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964169,0.00006446019,0.00012220339,0.000022915856,0.000015697431,0.0000089809555,0.0006524691,0.000026870237,0.002669543],"genre_scores_gemma":[0.9976077,0.00006464386,0.00015262382,0.000016067987,0.00002558503,0.000007650026,0.001307728,0.00000835751,0.00080957706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999472,0.000003758399,0.0000020278444,0.000011437994,0.000015098799,0.00002047369],"domain_scores_gemma":[0.9998522,0.000012042076,0.000041514963,0.000013805729,0.00003645194,0.000044040687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000104991654,0.00021553432,0.00018649586,0.00053919456,0.00036607828,0.00036491398,0.00011564719,0.00016741217,0.0014340914],"category_scores_gemma":[0.00016242728,0.000078865254,0.00011534664,0.00039835984,0.00016609326,0.00012450143,0.0004384784,0.00029544346,0.00022741732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062193687,0.00009463649,0.8872677,0.000080727164,0.00008529449,0.0015837805,0.0007868649,0.0008554984,0.0835178,0.00026172798,0.0026243692,0.022219695],"study_design_scores_gemma":[0.0000025123088,0.000026360995,0.9980743,0.0000023311368,0.000004578543,0.00007061514,0.000055038836,0.000111888854,0.0008942187,0.000007476695,0.00074895547,0.0000017035597],"about_ca_topic_score_codex":0.0046302546,"about_ca_topic_score_gemma":0.010118975,"teacher_disagreement_score":0.0046302546,"about_ca_system_score_codex":0.00023733707,"about_ca_system_score_gemma":0.00015801242,"threshold_uncertainty_score":0.009206653},"labels":[],"label_agreement":null},{"id":"W2895322433","doi":"10.1029/2018gl079660","title":"Fluvial Response to a Period of Hydrometeorological Change and Landscape Disturbance in the Canadian High Arctic","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Environment and Protected Areas; Queen's University","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; Coordenação de Aperfeiçoamento de Pessoal de Nível Superior; ArcticNet","keywords":"Hydrometeorology; Fluvial; Permafrost; Arctic; Sediment; Hydrology (agriculture); Pluvial; Disturbance (geology); Environmental science; Climate change; Geology; Channel (broadcasting); Sediment transport; Precipitation; Geomorphology; Oceanography; Geography; Meteorology","score_opus":0.07933724467315373,"score_gpt":0.2985178222205696,"score_spread":0.21918057754741588,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895322433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994393,0.00003942029,0.000018322438,0.00006274445,0.0000024252936,0.0000026562413,0.00013830695,0.000002437058,0.0002943595],"genre_scores_gemma":[0.9995987,0.00003135577,0.000023232882,0.000024177922,0.0000020349476,0.0000027520764,0.00014227389,9.810145e-7,0.00017461294],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99965906,0.000030098674,0.000013149312,0.00005793665,0.00007875589,0.00016102157],"domain_scores_gemma":[0.9991221,0.0000691987,0.00014442798,0.000030274932,0.00038007094,0.00025391064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004635694,0.00017903496,0.00030565183,0.0008683499,0.0020052523,0.0011030639,0.0004983506,0.0004889094,0.0008350322],"category_scores_gemma":[0.0012553583,0.00016579642,0.00023277404,0.0010022736,0.0010497221,0.00020503934,0.00058631925,0.00033712215,0.00008019821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023651568,0.00007800925,0.9886324,0.000019546533,0.00009572899,0.00017450901,0.0012991738,0.000683379,0.003553529,0.00009263898,0.00045458844,0.004679975],"study_design_scores_gemma":[0.0000014442478,0.000009011575,0.99917346,0.0000017495745,0.000004548245,0.000012384655,0.00043741427,0.00015007408,0.000056272307,0.0000060050643,0.00014447825,0.000003077362],"about_ca_topic_score_codex":0.9467562,"about_ca_topic_score_gemma":0.9747798,"teacher_disagreement_score":0.053243816,"about_ca_system_score_codex":0.0104221,"about_ca_system_score_gemma":0.0066660224,"threshold_uncertainty_score":0.10711473},"labels":[],"label_agreement":null},{"id":"W2895831433","doi":"10.1029/2018gl079288","title":"Induced Seismicity in Western Canada Linked to Tectonic Strain Rate: Implications for Regional Seismic Hazard","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; Geoscience BC; University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Seismology; Seismic hazard; Tectonics; Strain rate; Foothills; Seismic moment; Fault (geology); Geography; Cartography","score_opus":0.077273001913778,"score_gpt":0.32394754289259886,"score_spread":0.24667454097882086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895831433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99769694,0.00014180061,0.00006144744,0.00009680139,0.0000016287626,0.000006505744,0.0006994044,0.000006544899,0.0012888937],"genre_scores_gemma":[0.99931526,0.0000880107,0.000045429886,0.000016391312,0.0000010784253,0.0000017705082,0.0002259874,0.0000015231922,0.00030463425],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981683,0.000012528872,0.000009488384,0.0000316072,0.000043061904,0.00008652212],"domain_scores_gemma":[0.9991123,0.00007076709,0.00018727082,0.000021211752,0.0003757031,0.0002327953],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018529358,0.00020190427,0.00020530737,0.001155631,0.00071553275,0.0007417183,0.00035001923,0.00017908806,0.0016641881],"category_scores_gemma":[0.0009642315,0.00010103798,0.00015966251,0.0019744958,0.0005463072,0.00014984155,0.0004713264,0.0002327008,0.00009001373],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006124146,0.00001602601,0.9934569,0.000014962094,0.000034126046,0.00009854699,0.0002892521,0.00047679417,0.0010376761,0.00008767542,0.0002493794,0.00417752],"study_design_scores_gemma":[0.000001543745,0.0000049031632,0.9990095,0.0000050326817,0.0000068747418,0.000016334916,0.0004675161,0.00023412697,0.00006691187,0.0000129954415,0.00017127788,0.0000029089397],"about_ca_topic_score_codex":0.9859139,"about_ca_topic_score_gemma":0.99104816,"teacher_disagreement_score":0.014086127,"about_ca_system_score_codex":0.008366338,"about_ca_system_score_gemma":0.007055676,"threshold_uncertainty_score":0.060702264},"labels":[],"label_agreement":null},{"id":"W2895974873","doi":"10.1029/2018gl079826","title":"Understanding Rapid Adjustments to Diverse Forcing Agents","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":262,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions","funders":"H2020 European Research Council; Natural Environment Research Council; U.S. Department of Energy; European Commission; Japan Society for the Promotion of Science; Norges Forskningsråd; Environmental Restoration and Conservation Agency; National Aeronautics and Space Administration; Department for Environment, Food and Rural Affairs, UK Government; Goddard Space Flight Center; Grand Équipement National De Calcul Intensif; Sight Research UK; Alexander von Humboldt-Stiftung; Met Office","keywords":"Radiative forcing; Forcing (mathematics); Stratosphere; Environmental science; Cloud forcing; Atmospheric sciences; Troposphere; Tropospheric ozone; Climatology; Global warming; Perturbation (astronomy); Climate change; Meteorology; Physics; Geology; Aerosol","score_opus":0.10963293219771492,"score_gpt":0.31942281328123967,"score_spread":0.20978988108352475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2895974873","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8858382,0.0029837335,0.07990097,0.0023919966,0.00017452361,0.00014755446,0.00079221715,0.0005254722,0.027245292],"genre_scores_gemma":[0.9910234,0.0006933917,0.006904043,0.00017801097,0.000063030224,0.00005233618,0.0001436073,0.00006315809,0.00087896513],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99954224,0.00008897956,0.00002806563,0.00015394963,0.00008319974,0.00010361942],"domain_scores_gemma":[0.99870086,0.00058182905,0.00023993527,0.0002097426,0.00012968,0.00013797838],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015540333,0.00051404146,0.00055843947,0.0005587312,0.00035419382,0.0020957952,0.00078965595,0.0008432893,0.0032734664],"category_scores_gemma":[0.004169785,0.0005020339,0.00043335688,0.0003463132,0.0008920808,0.0033977216,0.0021304435,0.0014275454,0.00040016373],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007130951,0.00028184569,0.15466644,0.0011916725,0.0008830997,0.0011976443,0.0027464658,0.31034848,0.19901103,0.15301064,0.004639015,0.17131059],"study_design_scores_gemma":[0.00010473557,0.00036187313,0.28350446,0.00020495182,0.00024225833,0.0005473019,0.0023559676,0.38341373,0.015330954,0.28726387,0.026340978,0.0003289009],"about_ca_topic_score_codex":0.0026578002,"about_ca_topic_score_gemma":0.0014600508,"teacher_disagreement_score":0.0032734664,"about_ca_system_score_codex":0.00077818276,"about_ca_system_score_gemma":0.000420653,"threshold_uncertainty_score":0.010950804},"labels":[],"label_agreement":null},{"id":"W2896088697","doi":"10.1029/2018gl079404","title":"Physical Properties of Aerosol Internally Mixed With Soot Particles in a Biogenically Dominated Environment in California","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Department of Energy","keywords":"Soot; Aerosol; Radiative forcing; Viscosity; Mixing (physics); Radiative transfer; Particle (ecology); Materials science; Atmospheric sciences; Chemical physics; Mineralogy; Environmental science; Chemistry; Meteorology; Geology; Physics; Combustion; Optics; Composite material","score_opus":0.02539944506924385,"score_gpt":0.24511726952574678,"score_spread":0.21971782445650292,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896088697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938357,0.000025285653,0.000022253984,0.0000045986494,0.0000012334806,0.0000030636647,0.00013287948,0.0000041658172,0.00042296524],"genre_scores_gemma":[0.9993647,0.000037174173,0.000094082905,0.0000055745177,0.0000026985695,0.0000028231507,0.00029879817,0.0000024421197,0.00019165622],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998171,0.0000062173744,0.000009651824,0.00007682621,0.000056986213,0.00003327567],"domain_scores_gemma":[0.999813,0.000021831327,0.000029807123,0.000009059899,0.00008109799,0.00004525882],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014015779,0.00031800137,0.00035200614,0.0009120448,0.0013872505,0.0009496292,0.0004563655,0.0003377686,0.0006977348],"category_scores_gemma":[0.00019154669,0.0002699199,0.00023780028,0.00061878236,0.00039855583,0.0002932221,0.0004012184,0.00024548252,0.00011771159],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033992736,0.00017071572,0.93695587,0.000058264297,0.00013956074,0.000418785,0.0006733952,0.0015799266,0.05384411,0.00009790897,0.00031115345,0.0054102764],"study_design_scores_gemma":[0.000008214649,0.000025716441,0.99756384,0.0000036657511,0.000016990041,0.000023539256,0.00027001783,0.00085886766,0.0010063825,0.000009128331,0.00020864484,0.0000049226187],"about_ca_topic_score_codex":0.23182043,"about_ca_topic_score_gemma":0.2463681,"teacher_disagreement_score":0.23182043,"about_ca_system_score_codex":0.0015319729,"about_ca_system_score_gemma":0.00049414,"threshold_uncertainty_score":0.46094215},"labels":[],"label_agreement":null},{"id":"W2896317821","doi":"10.1029/2018gl079615","title":"Statistical Analysis of SAR Arc Detachment From the Main Oval Based on 11‐Year, All‐Sky Imaging Observation at Athabasca, Canada","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Athabasca University","funders":"Japan Society for the Promotion of Science; Natural Resources Canada; Athabasca University","keywords":"Substorm; Geology; Sky; Arc (geometry); Latitude; Geophysics; Magnetosphere; Geodesy; Meteorology; Magnetic field; Physics; Geometry","score_opus":0.01747423106448901,"score_gpt":0.28229333266649814,"score_spread":0.2648191016020091,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896317821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929611,0.00012918469,0.0003855597,0.000038151207,0.0000074914064,0.000015481117,0.0052642897,0.000044813612,0.0011540457],"genre_scores_gemma":[0.9924541,0.00004983409,0.00024938205,0.000014523307,0.0000044664753,0.000008778775,0.0067453757,0.000011472962,0.00046208623],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995091,0.000022831282,0.000026112442,0.000101037884,0.0001907115,0.00015017032],"domain_scores_gemma":[0.99831283,0.00017602798,0.00037305694,0.00011455408,0.0007768556,0.00024656922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047375314,0.00036573867,0.000278483,0.0015568525,0.0009810821,0.000770621,0.0005086966,0.0001722229,0.00065312925],"category_scores_gemma":[0.0011665773,0.00013413512,0.00041877234,0.0019355108,0.00047923328,0.0002362092,0.000493001,0.00032361198,0.00014376441],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010122436,0.000017260463,0.9911026,0.000017661969,0.00012133805,0.00014837443,0.00012621855,0.0013605291,0.0023664334,0.00004952807,0.0012198531,0.003369065],"study_design_scores_gemma":[0.0000011681213,0.0000036947354,0.998175,0.0000016993537,0.00001164637,0.000018071067,0.00012300813,0.0010688513,0.000182515,0.00000365019,0.00040681043,0.0000037419939],"about_ca_topic_score_codex":0.8265315,"about_ca_topic_score_gemma":0.88602036,"teacher_disagreement_score":0.17346847,"about_ca_system_score_codex":0.0031941691,"about_ca_system_score_gemma":0.002802234,"threshold_uncertainty_score":0.34898007},"labels":[],"label_agreement":null},{"id":"W2896480963","doi":"10.1029/2018gl079589","title":"Coral Reef Island Initiation and Development Under Higher Than Present Sea Levels","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Atoll; Reef; Oceanography; Geology; Coral reef; Sea level; Fringing reef; Coral; Sea level rise; Climate change","score_opus":0.10015135966857343,"score_gpt":0.32832182279332783,"score_spread":0.22817046312475442,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896480963","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841154,0.000030520325,0.000056766854,0.000012521683,8.4468616e-7,0.0000031210159,0.00016927085,0.0000032609794,0.0013121567],"genre_scores_gemma":[0.9994622,0.000033058484,0.00004906379,0.0000023209902,0.0000014462464,0.0000021847104,0.0001533863,6.3068404e-7,0.00029566686],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998969,0.000015916608,0.000008715213,0.000023017961,0.000018745479,0.000036757912],"domain_scores_gemma":[0.99914074,0.00009459637,0.0003464147,0.00005060834,0.00017430523,0.00019346434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003534339,0.00010402965,0.0000829593,0.00073016546,0.00023257636,0.00066970114,0.00015326017,0.00014487702,0.0023932674],"category_scores_gemma":[0.00095319934,0.00006918191,0.00015843472,0.00045063614,0.00022412556,0.0002818803,0.00049641624,0.00019478842,0.0002903266],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007100414,0.000019849827,0.9939703,0.000008822491,0.000012803893,0.000071358765,0.00015265348,0.00025580134,0.0025653646,0.00013685622,0.00007660016,0.002658692],"study_design_scores_gemma":[2.9750592e-7,0.0000131387815,0.99947697,0.0000010836426,0.0000017209958,0.000018735856,0.00012533522,0.00009100253,0.00016466803,0.000013901307,0.00009234318,7.907544e-7],"about_ca_topic_score_codex":0.0134863695,"about_ca_topic_score_gemma":0.02203697,"teacher_disagreement_score":0.0134863695,"about_ca_system_score_codex":0.0004038658,"about_ca_system_score_gemma":0.0003163476,"threshold_uncertainty_score":0.026815712},"labels":[],"label_agreement":null},{"id":"W2896497619","doi":"10.1029/2018gl079269","title":"Eclipse‐Induced Changes to Topside Ion Composition and Field‐Aligned Ion Flows in the August 2017 Solar Eclipse: e‐POP Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; European Space Agency","keywords":"Ion; Eclipse; Solar eclipse; Physics; Plasma; Polar; Outflow; Photoionization; Electron density; Astrophysics; Ionization; Atmospheric sciences; Astronomy; Meteorology","score_opus":0.04770992416143729,"score_gpt":0.3203040849573927,"score_spread":0.27259416079595544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896497619","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986267,0.000031033873,0.00012408862,0.0000144823325,0.0000053978183,0.0000027897208,0.00040780343,0.000015521842,0.0007722545],"genre_scores_gemma":[0.9987104,0.00004560009,0.00019509056,0.000018959228,0.000010805919,0.0000053835925,0.00074379006,0.000010517147,0.0002593688],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999589,0.000002701645,0.0000013821344,0.000011025607,0.000010670904,0.000015272863],"domain_scores_gemma":[0.99992085,0.000011686427,0.000018755745,0.000006409542,0.000020869064,0.000021505188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000085114625,0.00017066323,0.00018885093,0.00035921473,0.0002299189,0.00027557663,0.0001229519,0.00025378447,0.000591334],"category_scores_gemma":[0.00019866986,0.000091821144,0.00011471942,0.00024373383,0.00014319882,0.00018176579,0.00032397316,0.0002443453,0.00017196512],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016745229,0.00012726693,0.5699949,0.000099567966,0.00008873918,0.0011698741,0.0007869916,0.00095270545,0.40080595,0.00014969146,0.0013466241,0.022803131],"study_design_scores_gemma":[0.000011783589,0.00007035044,0.9899588,0.0000075453377,0.000011903494,0.00015138199,0.00021810153,0.00074123975,0.0078463815,0.00002937051,0.00094795885,0.0000051580805],"about_ca_topic_score_codex":0.003666263,"about_ca_topic_score_gemma":0.007539955,"teacher_disagreement_score":0.003666263,"about_ca_system_score_codex":0.00017572816,"about_ca_system_score_gemma":0.00010301407,"threshold_uncertainty_score":0.007289827},"labels":[],"label_agreement":null},{"id":"W2896697168","doi":"10.1029/2018gl080291","title":"Diagnosis of ULF Wave‐Particle Interactions With Megaelectron Volt Electrons: The Importance of Ultrahigh‐Resolution Energy Channels","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Physics; Electron; Amplitude; Computational physics; Flux (metallurgy); Resolution (logic); Range (aeronautics); Spectrometer; Van Allen Probes; Atomic physics; Particle (ecology); Phase (matter); Plasma; Magnetosphere; Optics; Van Allen radiation belt; Nuclear physics; Materials science; Quantum mechanics","score_opus":0.015701972818808904,"score_gpt":0.2770766770457015,"score_spread":0.2613747042268926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2896697168","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98699176,0.000406396,0.010885201,0.000063439606,0.000010030178,0.000009245821,0.00010897737,0.00007083952,0.0014541947],"genre_scores_gemma":[0.99529415,0.00007903778,0.004438793,0.000014461037,0.0000072030743,0.000004116948,0.00003662851,0.0000068605236,0.00011869652],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99986327,0.0000419965,0.0000074945115,0.0000247265,0.000030333935,0.00003225814],"domain_scores_gemma":[0.99942786,0.0002725448,0.0001159133,0.000069461115,0.00007872049,0.000035447774],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039598963,0.00012803871,0.00012933314,0.0007264017,0.00015169765,0.00047627042,0.00025373607,0.00038412304,0.0006347664],"category_scores_gemma":[0.0010595669,0.00011787513,0.00004805624,0.00038968632,0.0002163616,0.0005686594,0.0002965084,0.00018872456,0.00011005336],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011217839,0.00013006294,0.42688078,0.00014270404,0.00009016331,0.0007871315,0.0003308732,0.003808006,0.49215347,0.0022663658,0.00080826605,0.07148043],"study_design_scores_gemma":[0.000039682505,0.00021635488,0.632809,0.000046560024,0.000075066324,0.00229551,0.00072338514,0.08226565,0.2740264,0.0027093631,0.0047422256,0.000050833125],"about_ca_topic_score_codex":0.00023756552,"about_ca_topic_score_gemma":0.00060473126,"teacher_disagreement_score":0.0007264017,"about_ca_system_score_codex":0.00009545595,"about_ca_system_score_gemma":0.000050643168,"threshold_uncertainty_score":0.002123475},"labels":[],"label_agreement":null},{"id":"W2897031124","doi":"10.1029/2018gl079362","title":"Predicted Chance That Global Warming Will Temporarily Exceed 1.5 °C","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Office of Science; Bundesministerium für Bildung und Forschung; U.S. Department of Energy; Barcelona Supercomputing Center; European Commission; Sight Research UK; National Oceanic and Atmospheric Administration; National Science Council; National Science Foundation; Climate Program Office; Division of Grants and Agreements; Horizon 2020 Framework Programme; Department for Business, Energy and Industrial Strategy, UK Government; Met Office; Department for Environment, Food and Rural Affairs, UK Government","keywords":"Global warming; Environmental science; Climatology; Warning system; Climate change; Meteorology; Geography; Geology; Computer science; Oceanography","score_opus":0.05780176343076542,"score_gpt":0.3256195146995203,"score_spread":0.26781775126875484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897031124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9576613,0.0003265319,0.019486994,0.002323923,0.00034302488,0.000035333916,0.0048863143,0.00055717316,0.0143794315],"genre_scores_gemma":[0.99751735,0.000052244555,0.000722578,0.00005960379,0.000020637885,0.000010500125,0.00081595697,0.000011738675,0.00078930083],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998172,0.000031778163,0.0000085497795,0.000048642036,0.000043627893,0.000050157963],"domain_scores_gemma":[0.9990017,0.00034598613,0.00025414335,0.00005588765,0.0002232781,0.00011904145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006591637,0.00040545067,0.0002028461,0.0004390801,0.00027523475,0.0007201655,0.00042815437,0.00066966633,0.0044166357],"category_scores_gemma":[0.002160148,0.00017497041,0.00049439585,0.0002395635,0.00029314918,0.0007058938,0.00039602062,0.00065496966,0.000824697],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014004033,0.000042695792,0.2078461,0.00003364091,0.00007038782,0.00017425042,0.00004566136,0.77203214,0.0014292451,0.0036206143,0.0064338143,0.008131344],"study_design_scores_gemma":[0.000028743823,0.00011972552,0.12293164,0.000059921505,0.00005723036,0.00013377036,0.0001618376,0.8609669,0.0025756464,0.0068956674,0.0059960634,0.00007287542],"about_ca_topic_score_codex":0.023919305,"about_ca_topic_score_gemma":0.01791789,"teacher_disagreement_score":0.023919305,"about_ca_system_score_codex":0.0009437244,"about_ca_system_score_gemma":0.0006227642,"threshold_uncertainty_score":0.047560155},"labels":[],"label_agreement":null},{"id":"W2897215218","doi":"10.1029/2018gl079519","title":"A Lack of Dynamic Triggering of Slow Slip and Tremor Indicates That the Shallow Cascadia Megathrust Offshore Vancouver Island Is Likely Locked","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ocean Networks Canada Society; University of Victoria; Geological Survey of Canada","funders":"W. M. Keck Foundation; National Science Foundation","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Trench; Submarine pipeline; Seafloor spreading; Slip (aerodynamics); Borehole; Tectonics; Geotechnical engineering; Geophysics","score_opus":0.05126037502936796,"score_gpt":0.2986008548861235,"score_spread":0.2473404798567555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897215218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99686474,0.000019698831,0.000126103,0.000025024689,0.0000021581427,0.0000059024737,0.00019017648,0.000013027648,0.002753173],"genre_scores_gemma":[0.9990833,0.000020407617,0.000069593494,0.000008238436,7.5171107e-7,0.0000027271335,0.00018124231,0.0000017772861,0.00063211686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990237,0.000005306793,0.000006086856,0.00002099636,0.000032394342,0.000032812444],"domain_scores_gemma":[0.99943155,0.000044442557,0.00016130072,0.00006212497,0.00012244553,0.00017800689],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007618191,0.00017097383,0.00014947666,0.00039073385,0.0005364944,0.0005139092,0.0002644309,0.00021030997,0.0026237036],"category_scores_gemma":[0.0004889493,0.00019241252,0.00008741526,0.0004724595,0.00037626878,0.00019930149,0.00042197376,0.00021300714,0.00025189188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001906842,0.000046553472,0.88333976,0.000056717825,0.00003853876,0.0008404039,0.0005121842,0.0005822354,0.105891205,0.00015733301,0.0003037637,0.008040632],"study_design_scores_gemma":[0.0000027971064,0.000035752528,0.9975809,0.0000031185323,0.0000037982788,0.00009682245,0.00020741261,0.00020949081,0.0015047584,0.000023282062,0.0003302215,0.0000016155914],"about_ca_topic_score_codex":0.11007683,"about_ca_topic_score_gemma":0.33032924,"teacher_disagreement_score":0.88992316,"about_ca_system_score_codex":0.0009763365,"about_ca_system_score_gemma":0.00065279286,"threshold_uncertainty_score":0.21887225},"labels":[],"label_agreement":null},{"id":"W2897342583","doi":"10.1029/2018gl079698","title":"On the Connection Between Global Hydrologic Sensitivity and Regional Wet Extremes","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Climate Program Office; Nature Conservancy of Canada; Nature Conservancy; U.S. Department of Energy; Office of Science; University of California, Los Angeles; National Science Foundation","keywords":"Precipitation; Environmental science; Climatology; Water cycle; Subtropics; Climate change; Tropics; Climate model; Atmospheric sciences; General Circulation Model; Climate sensitivity; Global change; Global warming; Hydrological modelling; Meteorology; Geology; Geography; Ecology","score_opus":0.08594642143506147,"score_gpt":0.32564161836859556,"score_spread":0.23969519693353408,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897342583","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99653995,0.00012495022,0.00097337784,0.00024214796,0.000005800579,0.0000018504154,0.00018359296,0.000018342102,0.0019100627],"genre_scores_gemma":[0.99978346,0.000030165727,0.0000537531,0.000011102846,0.000004468594,5.1179813e-7,0.00004884749,0.0000032687444,0.00006449511],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985564,0.00006835096,0.000007849628,0.000029937162,0.00001762073,0.000020515397],"domain_scores_gemma":[0.9980281,0.0014570133,0.00022099224,0.00013078444,0.00008309177,0.00008010612],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074693776,0.00014172832,0.00012018666,0.00033817443,0.00011150253,0.0006335564,0.00017337296,0.00021685832,0.002094211],"category_scores_gemma":[0.0034309928,0.00013521177,0.00021855628,0.0003601436,0.00035911662,0.0005253682,0.00054751686,0.000351412,0.00012946173],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025070968,0.00006009428,0.75846857,0.000041209612,0.00051793765,0.00017920043,0.00015980547,0.22105682,0.0039645773,0.0042444463,0.0007929968,0.010263751],"study_design_scores_gemma":[0.000018111998,0.00006200878,0.7239503,0.000021672386,0.00012293147,0.00008702062,0.0002549825,0.26366788,0.0015956986,0.009477406,0.0007143456,0.00002761576],"about_ca_topic_score_codex":0.004257319,"about_ca_topic_score_gemma":0.0035418589,"teacher_disagreement_score":0.004257319,"about_ca_system_score_codex":0.00017858249,"about_ca_system_score_gemma":0.000141386,"threshold_uncertainty_score":0.008465111},"labels":[],"label_agreement":null},{"id":"W2897412148","doi":"10.1029/2018gl079745","title":"Linkage Between Westerly Wind Bursts and Tropical Cyclones","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"National Natural Science Foundation of China","keywords":"Tropical cyclone; Climatology; Westerlies; Seasonality; Environmental science; Atmospheric sciences; Geology; Biology; Ecology","score_opus":0.04417710027312145,"score_gpt":0.3103819763110811,"score_spread":0.26620487603795967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897412148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99772936,0.00014936438,0.0004990085,0.00008711882,0.000018603228,0.000004723529,0.000670377,0.00002128039,0.0008201439],"genre_scores_gemma":[0.99905056,0.000060359573,0.00014163474,0.000013292181,0.000017460383,0.000002674806,0.000602314,0.000004133594,0.00010736855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997898,0.000036151185,0.000025049001,0.00007717159,0.000035809288,0.000036180016],"domain_scores_gemma":[0.9977342,0.00042725186,0.00114891,0.00018758625,0.00026648442,0.00023551306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037595327,0.0001352938,0.0001835408,0.0007975309,0.00025633737,0.000742843,0.00011251292,0.00017752206,0.0019752712],"category_scores_gemma":[0.0021024805,0.00013583827,0.00015722579,0.0008108844,0.00019152733,0.00033994645,0.00062472984,0.0003962753,0.00018382909],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004934443,0.0000181791,0.9928328,0.000013424026,0.00007776129,0.000051792133,0.00011143879,0.00069048896,0.001192189,0.00021177417,0.00035298578,0.0043978347],"study_design_scores_gemma":[0.0000027282663,0.0000085220645,0.9983493,0.0000056677604,0.000011296342,0.000022101432,0.00008124079,0.0009599652,0.00009010898,0.00013178521,0.00033382533,0.0000034401662],"about_ca_topic_score_codex":0.0076888846,"about_ca_topic_score_gemma":0.008395735,"teacher_disagreement_score":0.0076888846,"about_ca_system_score_codex":0.00013320721,"about_ca_system_score_gemma":0.00019084773,"threshold_uncertainty_score":0.015288234},"labels":[],"label_agreement":null},{"id":"W2897529245","doi":"10.1029/2018gl078711","title":"Holocene Surface Rupture History of an Active Forearc Fault Redefines Seismic Hazard in Southwestern British Columbia, Canada","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Shared Services Canada; University of Victoria","funders":"Washington State University; Northwestern University; National Science Foundation","keywords":"Forearc; Geology; Seismology; Quaternary; Seismic hazard; Holocene; Induced seismicity; Active fault; Subduction; Fault scarp; Fault (geology); Tectonics; Paleontology","score_opus":0.02517472811469667,"score_gpt":0.24661081151124342,"score_spread":0.22143608339654675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897529245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99120164,0.00041226298,0.00011656774,0.00022145429,0.0000068363943,0.00001277477,0.0031290567,0.000019438983,0.004879958],"genre_scores_gemma":[0.996033,0.00029233017,0.00015665253,0.0000411498,0.0000019806,0.0000058686323,0.0013220275,0.0000060143266,0.002140985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998318,0.000008781304,0.0000089395835,0.00003637702,0.00004540727,0.00006867542],"domain_scores_gemma":[0.99885535,0.00006367046,0.00012007783,0.000032344007,0.0007228079,0.00020581987],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017731839,0.0002213039,0.00019052974,0.001853819,0.0021306968,0.001162741,0.00065974635,0.00032355243,0.0033264],"category_scores_gemma":[0.00083634217,0.0002013959,0.00011704093,0.0029805126,0.00051586324,0.000278306,0.00049787696,0.0004076421,0.00033693627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005807015,0.000027117132,0.96791774,0.000040740142,0.000040964358,0.00029798696,0.0020063668,0.00084550254,0.0014495285,0.00013166164,0.0033313842,0.023852982],"study_design_scores_gemma":[0.000001923328,0.0000038645135,0.9962437,0.000020997824,0.000008147438,0.000032679105,0.0015989995,0.0003070707,0.00011082909,0.000015508316,0.0016503135,0.0000059729364],"about_ca_topic_score_codex":0.9952571,"about_ca_topic_score_gemma":0.9990833,"teacher_disagreement_score":0.016380368,"about_ca_system_score_codex":0.016380368,"about_ca_system_score_gemma":0.010508753,"threshold_uncertainty_score":0.11884844},"labels":[],"label_agreement":null},{"id":"W2897977828","doi":"10.1029/2018gl078995","title":"Northward Expansion and Intensification of Phytoplankton Growth During the Early Ice‐Free Season in Arctic","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Université Laval","funders":"Agence Nationale de la Recherche; ArcticNet; Canada Excellence Research Chairs, Government of Canada; National Aeronautics and Space Administration","keywords":"Phytoplankton; Oceanography; Sea ice; Environmental science; Arctic; Arctic ice pack; Marine ecosystem; Arctic sea ice decline; Spring (device); Primary productivity; Spring bloom; Climatology; Ecosystem; Geology; Drift ice; Ecology; Nutrient","score_opus":0.01864635811516031,"score_gpt":0.24804974249584108,"score_spread":0.22940338438068078,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2897977828","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99882895,0.00019209004,0.000077492165,0.000028106517,0.000006228205,0.0000012174696,0.0002171405,0.000003686319,0.00064523716],"genre_scores_gemma":[0.999481,0.00011997465,0.000059886406,0.000009532334,0.000006203565,0.0000012929618,0.00016043714,0.0000013583866,0.0001603755],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992466,0.000010604456,0.0000067250903,0.00002107396,0.000017291477,0.000019671792],"domain_scores_gemma":[0.9996449,0.000043455373,0.000106454754,0.000018381974,0.00012638659,0.00006045841],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031459896,0.00012954323,0.00014076171,0.00081996724,0.0003179265,0.00046220465,0.00009644623,0.00013408909,0.0004734721],"category_scores_gemma":[0.00033141856,0.00008739392,0.00017642119,0.0006001367,0.00021644951,0.00017751733,0.00028859242,0.00015730901,0.00011747767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022324131,0.000026041287,0.97284013,0.000044239125,0.000051985782,0.00014711301,0.0007912686,0.00038339774,0.016007725,0.000115163486,0.0003511017,0.009018574],"study_design_scores_gemma":[4.9069274e-7,0.0000053045833,0.9993851,0.0000027405677,0.0000030359458,0.000019855446,0.000107434214,0.00008118064,0.00015102557,0.000008765803,0.00023420539,8.2771123e-7],"about_ca_topic_score_codex":0.03241626,"about_ca_topic_score_gemma":0.059449643,"teacher_disagreement_score":0.03241626,"about_ca_system_score_codex":0.00038220588,"about_ca_system_score_gemma":0.00034086176,"threshold_uncertainty_score":0.06445515},"labels":[],"label_agreement":null},{"id":"W2898595988","doi":"10.1029/2018gl080222","title":"Energetic Electron Precipitation Associated With Pulsating Aurora Observed by VLF Radio Propagation During the Recovery Phase of a Substorm on 27 March 2017","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"Institute of Space and Astronautical Science; National Aeronautics and Space Administration; Japan Society for the Promotion of Science; Ministry of Education, Culture, Sports, Science and Technology; Athabasca University; Japan Aerospace Exploration Agency","keywords":"Substorm; Electron precipitation; Electron; Physics; Ionosphere; Microburst; Van Allen radiation belt; Atmospheric sciences; Astrophysics; Precipitation; Geophysics; Magnetosphere; Computational physics; Meteorology; Plasma; Nuclear physics","score_opus":0.022451273970347147,"score_gpt":0.2876081307840333,"score_spread":0.26515685681368617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2898595988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998808,0.000091252725,0.00020551297,0.00003574691,0.0000086504715,0.000006820934,0.0001541301,0.000036887508,0.0006528178],"genre_scores_gemma":[0.99936444,0.000040526953,0.00011402131,0.000010231761,0.00001845499,0.000004449986,0.0002806148,0.000006285788,0.00016098347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999187,0.0000063096522,0.000004407343,0.000014025461,0.000024511839,0.000032051033],"domain_scores_gemma":[0.99970144,0.00003297555,0.0001197657,0.00002757794,0.00005622885,0.00006191583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018503492,0.00021589342,0.00031688614,0.00063139264,0.0004306515,0.00040525416,0.00025678772,0.00026994923,0.00062341476],"category_scores_gemma":[0.00035868754,0.0000954413,0.000197318,0.00039412375,0.00027437642,0.00013542028,0.000435195,0.0004368798,0.00018519431],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00089590444,0.0001395668,0.76694244,0.00007018394,0.00018882664,0.0047624097,0.0011565649,0.000927779,0.20266926,0.00022350105,0.001298909,0.020724656],"study_design_scores_gemma":[0.000009716946,0.0000889371,0.9942263,0.0000050565027,0.000025939524,0.0003469313,0.00017304425,0.0005305253,0.0038290038,0.000029325543,0.0007297489,0.000005578265],"about_ca_topic_score_codex":0.0046742116,"about_ca_topic_score_gemma":0.0057791644,"teacher_disagreement_score":0.0046742116,"about_ca_system_score_codex":0.00029035815,"about_ca_system_score_gemma":0.0001930607,"threshold_uncertainty_score":0.009294033},"labels":[],"label_agreement":null},{"id":"W2899619037","doi":"10.1029/2018gl079382","title":"Earthquake Stress Drop in the Charlevoix Seismic Zone, Eastern Canada","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Intraplate earthquake; Geology; Seismology; Induced seismicity; Crust; Scaling; Drop (telecommunication); Geophysics; Tectonics; Geometry","score_opus":0.031706644885183675,"score_gpt":0.2686663522198223,"score_spread":0.23695970733463864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2899619037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970282,0.000103878374,0.000071913906,0.000028127775,0.0000016010675,0.000008199854,0.0014301435,0.000013838157,0.0013142144],"genre_scores_gemma":[0.99765885,0.00007998841,0.00012319004,0.000011380397,0.000001331169,0.0000055626515,0.0012712325,0.0000031479647,0.0008453461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997701,0.0000074772797,0.00001138732,0.000042707037,0.000088083514,0.00008025329],"domain_scores_gemma":[0.9992957,0.000036373538,0.00010816023,0.000024781473,0.0003849008,0.00015007755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019725045,0.0003036304,0.00021925948,0.0022648845,0.0010216249,0.00084747165,0.00052842195,0.00021295677,0.0010444028],"category_scores_gemma":[0.000657586,0.00014918005,0.00015413643,0.0027608566,0.0005166592,0.00018770595,0.0006952977,0.00022355316,0.0001371034],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000120888915,0.000021106747,0.9823647,0.000038463342,0.000049567218,0.00020312578,0.00076670636,0.0014756556,0.0026367814,0.00013845452,0.00076159864,0.011422912],"study_design_scores_gemma":[0.0000018720742,0.000004377071,0.99863213,0.000004631427,0.0000031314528,0.000015262012,0.00033724855,0.00043669538,0.00016664887,0.000006549878,0.00038823977,0.0000032010907],"about_ca_topic_score_codex":0.9821618,"about_ca_topic_score_gemma":0.99207664,"teacher_disagreement_score":0.01783818,"about_ca_system_score_codex":0.0109593235,"about_ca_system_score_gemma":0.007005779,"threshold_uncertainty_score":0.079515874},"labels":[],"label_agreement":null},{"id":"W2900084613","doi":"10.1029/2018gl080077","title":"Challenges in the Search for Perchlorate and Other Hydrated Minerals With 2.1‐μm Absorptions on Mars","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Nuclear Safety and Security Commission; Natural Sciences and Engineering Research Council of Canada; Rose Hills Foundation; National Aeronautics and Space Administration; National Science Foundation","keywords":"Mars Exploration Program; Astrobiology; Perchlorate; Geology; Mineralogy; Geochemistry; Chemistry; Physics; Ion; Organic chemistry","score_opus":0.14044196861332484,"score_gpt":0.34754150325064964,"score_spread":0.2070995346373248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900084613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.63782024,0.014392212,0.24359527,0.0594997,0.0009571719,0.00036622686,0.008095275,0.009334979,0.025938917],"genre_scores_gemma":[0.48490146,0.0037673241,0.4934513,0.006615502,0.00049121364,0.00026038548,0.0052044727,0.0010078829,0.0043003703],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.99704665,0.0005595727,0.00024110917,0.0009329686,0.0009636331,0.00025611458],"domain_scores_gemma":[0.99082446,0.002675894,0.00092269894,0.0008496994,0.004112237,0.0006150364],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.006909781,0.000576301,0.0005825334,0.0021220492,0.0019013507,0.003877105,0.002277,0.0022083216,0.0034852657],"category_scores_gemma":[0.010404872,0.00065017457,0.00080788956,0.0016237237,0.001110075,0.0031841374,0.002105012,0.0019961977,0.0036658677],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047561192,0.0002198661,0.22850469,0.0021007988,0.00025528274,0.0017889653,0.004635126,0.004850492,0.21760316,0.0036143106,0.03475259,0.5011991],"study_design_scores_gemma":[0.0001003418,0.00081536593,0.39085686,0.0010943637,0.00038706968,0.01159632,0.03165655,0.055290442,0.14439648,0.02814228,0.33520216,0.0004617625],"about_ca_topic_score_codex":0.006360312,"about_ca_topic_score_gemma":0.014033181,"teacher_disagreement_score":0.006909781,"about_ca_system_score_codex":0.0006373665,"about_ca_system_score_gemma":0.0014603545,"threshold_uncertainty_score":0.036542892},"labels":[],"label_agreement":null},{"id":"W2900258110","doi":"10.1029/2018gl079784","title":"Phosgene in the Upper Troposphere and Lower Stratosphere: A Marker for Product Gas Injection Due to Chlorine‐Containing Very Short Lived Substances","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Waterloo","funders":"Natural Environment Research Council; Sight Research UK; UK Research and Innovation; National Aeronautics and Space Administration","keywords":"Phosgene; Stratosphere; Troposphere; Ozone; Chlorine; Atmospheric sciences; Atmospheric chemistry; Ozone depletion; Ozone layer; Chemistry; Carbon tetrachloride; Environmental science; Meteorology; Physics; Organic chemistry","score_opus":0.03192955210480465,"score_gpt":0.29019673814170693,"score_spread":0.2582671860369023,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900258110","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99609816,0.00009565604,0.0005140685,0.000041484356,0.0000045490597,0.000008425245,0.0017401839,0.00005956158,0.0014380051],"genre_scores_gemma":[0.9987531,0.000039615352,0.00027017397,0.0000128466345,0.0000024126696,0.000003638172,0.00076979946,0.000006014204,0.00014239573],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991417,0.000006146251,0.000003999751,0.000025798377,0.00003227452,0.000017578706],"domain_scores_gemma":[0.99988186,0.000016496248,0.000037495272,0.000011011822,0.00003625333,0.000016791551],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014412883,0.0002949332,0.00010277388,0.00053530606,0.00025480907,0.00045286832,0.00016351756,0.00024343704,0.00073289894],"category_scores_gemma":[0.00017144937,0.000105513456,0.00019137071,0.00049165485,0.00020449344,0.00042143287,0.0002723955,0.00020966148,0.0000882042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003388274,0.00008471691,0.81497115,0.00007910655,0.00008085324,0.00020771634,0.00018443233,0.00465526,0.17023179,0.00035564337,0.0009171009,0.007893416],"study_design_scores_gemma":[0.000012940749,0.0000753094,0.93850917,0.00001077784,0.0000318492,0.00006220202,0.00014154369,0.00939228,0.049935963,0.00011430529,0.0017013792,0.00001233478],"about_ca_topic_score_codex":0.0424167,"about_ca_topic_score_gemma":0.040996,"teacher_disagreement_score":0.0424167,"about_ca_system_score_codex":0.0006893392,"about_ca_system_score_gemma":0.00038035,"threshold_uncertainty_score":0.08433962},"labels":[],"label_agreement":null},{"id":"W2900281336","doi":"10.1029/2018gl079023","title":"How Asymmetries Between Arctic and Antarctic Climate Sensitivity Are Modified by the Ocean","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"U.S. Department of Energy","keywords":"Climatology; Environmental science; Northern Hemisphere; Forcing (mathematics); Climate model; Arctic sea ice decline; Arctic; Climate sensitivity; Southern Hemisphere; Arctic dipole anomaly; Sea ice; Arctic geoengineering; Albedo (alchemy); Coupled model intercomparison project; Climate change; Atmospheric sciences; Geology; Oceanography; Arctic ice pack; Antarctic sea ice","score_opus":0.04692999764711616,"score_gpt":0.29558932813498884,"score_spread":0.24865933048787267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900281336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970974,0.000046318055,0.00056418276,0.000078894634,0.0000066995804,0.0000018996268,0.00011221275,0.000018744337,0.0020736845],"genre_scores_gemma":[0.9998056,0.000015634501,0.0000609775,0.000013852947,0.0000013840763,8.822654e-7,0.000022931838,0.0000040169803,0.00007458149],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998784,0.000044288918,0.0000068708728,0.000023942737,0.000016010856,0.000030458928],"domain_scores_gemma":[0.9996195,0.00014953919,0.0000739871,0.00007085739,0.000047040052,0.000039033297],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040101208,0.00022557177,0.0002026758,0.0002601299,0.00018070973,0.0008052288,0.00015293945,0.00026605165,0.001764008],"category_scores_gemma":[0.0016010687,0.00016929432,0.00026966215,0.00018577265,0.0003632947,0.00048350095,0.0005314615,0.0002598322,0.00012942494],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019300214,0.00011337325,0.38856944,0.00014296139,0.0005914111,0.00052595575,0.00054539955,0.23421367,0.3249944,0.015190106,0.0014535862,0.031729743],"study_design_scores_gemma":[0.00008121801,0.00017492504,0.74754864,0.000025352445,0.00017675557,0.00014701634,0.00056791794,0.20768435,0.030536417,0.011210529,0.0017713229,0.00007559688],"about_ca_topic_score_codex":0.005088629,"about_ca_topic_score_gemma":0.003303394,"teacher_disagreement_score":0.005088629,"about_ca_system_score_codex":0.00038263886,"about_ca_system_score_gemma":0.00028917877,"threshold_uncertainty_score":0.010118008},"labels":[],"label_agreement":null},{"id":"W2900373457","doi":"10.1029/2018gl080963","title":"Late‐July Barrier for Subseasonal Forecast of Summer Daily Maximum Temperature Over Yangtze River Basin","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Natural Science Foundation of China","keywords":"Geopotential height; Climatology; Subtropical ridge; Predictability; Environmental science; Subtropics; Forecast skill; Geopotential; Yangtze river; Madden–Julian oscillation; Structural basin; Precipitation; China; Geology; Meteorology; Geography; Convection","score_opus":0.04078560932810267,"score_gpt":0.30974291378912816,"score_spread":0.2689573044610255,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900373457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998664,0.00005622329,0.00038573644,0.00006331327,0.000008322527,0.0000028350994,0.0005034873,0.000036019163,0.0002801116],"genre_scores_gemma":[0.9989784,0.000018347624,0.00012609205,0.00000476359,0.0000042924416,0.0000017633507,0.0008088653,0.000002574361,0.000055007004],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998561,0.000027042892,0.000012983243,0.00004559466,0.000031341922,0.000026918457],"domain_scores_gemma":[0.99941814,0.00013086108,0.000114125025,0.000058277077,0.00016814341,0.00011051961],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081136473,0.00031251332,0.00025561132,0.0005786593,0.00021550924,0.00053104426,0.00024679504,0.00019352882,0.0005820678],"category_scores_gemma":[0.0012731713,0.00015966769,0.00032175693,0.00040404854,0.0001334396,0.00045125405,0.00034373195,0.00030564074,0.00009663633],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038334963,0.00008442229,0.86066544,0.00003268605,0.00019320752,0.0001478545,0.00010670125,0.12167464,0.0037092094,0.000309871,0.0016145534,0.011078191],"study_design_scores_gemma":[0.00004012044,0.000068674424,0.6315675,0.000010889939,0.000044075834,0.000025201174,0.00010439253,0.36595377,0.0012530809,0.00019815551,0.0007122471,0.000021861651],"about_ca_topic_score_codex":0.060800873,"about_ca_topic_score_gemma":0.061817013,"teacher_disagreement_score":0.060800873,"about_ca_system_score_codex":0.00043532523,"about_ca_system_score_gemma":0.0007767366,"threshold_uncertainty_score":0.120893955},"labels":[],"label_agreement":null},{"id":"W2900802495","doi":"10.1029/2018gl078759","title":"Concentrations and Water Mass Transport of Legacy POPs in the Arctic Ocean","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Toxic Organic Pollutants Impact","field":"Environmental Science","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"FP7 People: Marie-Curie Actions; Research Executive Agency; National Natural Science Foundation of China; National Science Foundation","keywords":"Hexachlorobenzene; Arctic; Environmental science; Oceanography; Pollutant; Archipelago; The arctic; Environmental chemistry; Geology; Chemistry","score_opus":0.022708803768105468,"score_gpt":0.29124984376022267,"score_spread":0.2685410399921172,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2900802495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981457,0.00015301227,0.00010641103,0.0000150412,0.0000045831703,0.0000027009594,0.000637071,0.0000055183496,0.0009299663],"genre_scores_gemma":[0.99711275,0.0004096769,0.0003458563,0.000019870415,0.0000054175603,0.0000055222786,0.0010474909,0.0000050256276,0.0010483852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999188,0.0000051216557,0.0000032833534,0.000030746236,0.000021051139,0.000020866175],"domain_scores_gemma":[0.9998952,0.000008423362,0.000020610792,0.0000033038807,0.00005910773,0.000013266602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013999564,0.00034576096,0.00017205466,0.00058877683,0.0006379748,0.00071762374,0.00018693437,0.00023345706,0.0005317952],"category_scores_gemma":[0.00015834605,0.0001881019,0.000244435,0.0006878128,0.00019238591,0.0002939297,0.00039432556,0.0001836215,0.00019431779],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006186019,0.000055374152,0.83343166,0.00007231,0.00012350065,0.00022018176,0.0005745195,0.002047164,0.14993727,0.00018244678,0.0004033951,0.012333577],"study_design_scores_gemma":[0.000010605009,0.00012760179,0.981265,0.00001397559,0.00005867855,0.000045766672,0.0007971614,0.0020027328,0.013429541,0.0000631096,0.0021735884,0.000012222681],"about_ca_topic_score_codex":0.27460504,"about_ca_topic_score_gemma":0.23908816,"teacher_disagreement_score":0.27460504,"about_ca_system_score_codex":0.0016534517,"about_ca_system_score_gemma":0.00092443,"threshold_uncertainty_score":0.54601336},"labels":[],"label_agreement":null},{"id":"W2901164369","doi":"10.1029/2018gl079798","title":"The 16‐Day Planetary Wave Triggers the SW1‐Tidal‐Like Signatures During 2009 Sudden Stratospheric Warming","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Sudden stratospheric warming; Atmospheric sciences; Oscillation (cell signaling); Atmospheric tide; Thermosphere; Climatology; Physics; Stratosphere; Geology; Ionosphere; Geophysics; Polar vortex; Chemistry","score_opus":0.012986204633385047,"score_gpt":0.25843764174957606,"score_spread":0.24545143711619102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901164369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99870396,0.00005033804,0.000103881044,0.00002417255,0.000007833232,0.000002281819,0.0002741044,0.000011928793,0.00082150626],"genre_scores_gemma":[0.99944085,0.000025688892,0.00007413922,0.000006260805,0.000007436493,0.0000015237802,0.00025778997,0.0000025757395,0.00018366423],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999652,0.00000312901,0.0000029403639,0.0000106136085,0.0000069867115,0.000011095612],"domain_scores_gemma":[0.99990964,0.000008383396,0.000031756983,0.000008687707,0.000016885962,0.000024653615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009007221,0.00011351081,0.00011289046,0.0004549933,0.00020636973,0.0002792253,0.000096805205,0.0001278835,0.001325261],"category_scores_gemma":[0.00020683897,0.00007232838,0.000096513024,0.00032914925,0.00020079385,0.00015224556,0.00042970057,0.00012865172,0.00019062223],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030784975,0.00004198926,0.88402474,0.000064528875,0.00007067901,0.0003714489,0.00049897446,0.0007610059,0.08800607,0.00041148873,0.0011401414,0.024301123],"study_design_scores_gemma":[0.0000025605236,0.000019462846,0.9978849,0.0000029172213,0.0000073087367,0.000042778895,0.000077867866,0.0004324879,0.0010132453,0.000044672237,0.0004691262,0.0000025173504],"about_ca_topic_score_codex":0.0025202085,"about_ca_topic_score_gemma":0.0047664894,"teacher_disagreement_score":0.0025202085,"about_ca_system_score_codex":0.00012668762,"about_ca_system_score_gemma":0.000093316274,"threshold_uncertainty_score":0.0050110817},"labels":[],"label_agreement":null},{"id":"W2901433068","doi":"10.1029/2018gl079812","title":"Microscopic Observations of Pulsating Aurora Associated With Chorus Element Structures: Coordinated Arase Satellite‐PWING Observations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"Japan Society for the Promotion of Science","keywords":"Chorus; Magnetosphere; Equator; Physics; Ionosphere; Geophysics; Latitude; Satellite; Substorm; Astrophysics; Astronomy; Magnetic field","score_opus":0.04062763361264258,"score_gpt":0.3052163423921929,"score_spread":0.2645887087795503,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901433068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969506,0.0000794441,0.0009768625,0.000014480892,0.00000559347,0.000008907459,0.00018936051,0.000036829344,0.0017378943],"genre_scores_gemma":[0.997981,0.000050171675,0.0012562162,0.000009096997,0.0000072377647,0.000008323159,0.00016139231,0.0000062647546,0.00052027067],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996996,0.0000024780923,0.0000011292898,0.000010306113,0.000008204824,0.000007936507],"domain_scores_gemma":[0.99991727,0.000009430615,0.000018250943,0.000012070685,0.000018096966,0.00002484418],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005736817,0.0000877413,0.00008526109,0.00039387977,0.00018487162,0.00017729489,0.00011093917,0.000110307934,0.0008081695],"category_scores_gemma":[0.000113169066,0.00012034263,0.000101527265,0.00020239076,0.00014231524,0.00011860529,0.00024969038,0.00017893034,0.00012493003],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012284749,0.000019354557,0.08403323,0.00003749257,0.000052219388,0.00026864672,0.00027648621,0.0005337415,0.90818304,0.0001456955,0.00025394655,0.006073289],"study_design_scores_gemma":[0.000012035147,0.0000802417,0.9725911,0.0000045059505,0.000029968322,0.00025920424,0.00025370158,0.0031530405,0.022222834,0.000055390774,0.0013289603,0.000009117414],"about_ca_topic_score_codex":0.0032291627,"about_ca_topic_score_gemma":0.0050349883,"teacher_disagreement_score":0.0032291627,"about_ca_system_score_codex":0.0001223364,"about_ca_system_score_gemma":0.00006449514,"threshold_uncertainty_score":0.0064207315},"labels":[],"label_agreement":null},{"id":"W2901490327","doi":"10.1029/2018gl080763","title":"Localized Plumes Drive Front‐Wide Ocean Melting of A Greenlandic Tidewater Glacier","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":125,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography","funders":"Ocean Life Institute, Woods Hole Oceanographic Institution; Natural Environment Research Council; Sight Research UK; Woods Hole Oceanographic Institution; National Science Foundation","keywords":"Tidewater; Fjord; Glacier; Geology; Tidewater glacier cycle; Greenland ice sheet; Ice calving; Front (military); Oceanography; Future sea level; Ocean current; Climatology; Geomorphology; Ice stream; Cryosphere; Sea ice","score_opus":0.03597348228525012,"score_gpt":0.2843289217526825,"score_spread":0.24835543946743235,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901490327","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996717,0.000011641706,0.00012753089,0.000013994717,9.904164e-7,0.0000013858655,0.00003221824,0.000008324778,0.00013220578],"genre_scores_gemma":[0.9996797,0.000013450431,0.0001839348,0.0000046844807,7.0030814e-7,9.988742e-7,0.000053367818,0.0000015208659,0.00006177117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999833,0.0000018904218,8.7741745e-7,0.000004819739,0.0000034499662,0.0000056547096],"domain_scores_gemma":[0.99995184,0.000010005807,0.000011461698,0.000004515294,0.000008053675,0.000014087968],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007165409,0.00015266553,0.00014946226,0.00019624851,0.00023610497,0.00042153592,0.00015978786,0.00017678137,0.00044413304],"category_scores_gemma":[0.00015762087,0.00010981445,0.00025729058,0.00013993305,0.0001740904,0.00018977694,0.00031245762,0.00022806134,0.00004797163],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043101778,0.00031439902,0.5815735,0.00006632914,0.00020381501,0.000536248,0.0006260758,0.1238321,0.27611652,0.00089992816,0.0006033051,0.014796803],"study_design_scores_gemma":[0.0000640154,0.00016746072,0.6408456,0.000009347462,0.00007827758,0.00007560379,0.00042098554,0.3478201,0.009652878,0.00043359358,0.00040721236,0.000024950801],"about_ca_topic_score_codex":0.028547835,"about_ca_topic_score_gemma":0.027272284,"teacher_disagreement_score":0.028547835,"about_ca_system_score_codex":0.00062272826,"about_ca_system_score_gemma":0.0003390743,"threshold_uncertainty_score":0.05676329},"labels":[],"label_agreement":null},{"id":"W2901562893","doi":"10.1029/2018gl080221","title":"Decadal Variation in IOD Predictability During 1881–2016","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"National Key Research and Development Program of China; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Ministry of Science and Technology of the People's Republic of China; Met Office","keywords":"Predictability; Climatology; Indian Ocean Dipole; El Niño Southern Oscillation; Hindcast; Boreal; Variation (astronomy); Environmental science; Geology; Mathematics; Statistics; Physics","score_opus":0.031152826445706307,"score_gpt":0.3084864709065253,"score_spread":0.277333644460819,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2901562893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99901533,0.000022680259,0.00015068158,0.000018378756,0.000007440831,0.0000014030112,0.00049653795,0.000009796508,0.0002776927],"genre_scores_gemma":[0.99883336,0.00001980537,0.00006241216,0.0000030098875,0.0000061073483,0.0000018490013,0.0009821195,0.000003326657,0.000088100154],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999236,0.000010514479,0.000006190511,0.000026726982,0.000014918967,0.000018012193],"domain_scores_gemma":[0.99968946,0.00007477266,0.00009436513,0.000040961288,0.00006529877,0.000035177498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033395656,0.00015767873,0.00017968279,0.0002322927,0.00015011957,0.0003558263,0.0001000702,0.00012644492,0.00056806643],"category_scores_gemma":[0.0008175961,0.000074561416,0.00020350302,0.0002579828,0.00018125902,0.00020260584,0.00028252145,0.00029865323,0.00013202737],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004882998,0.00009258087,0.9480061,0.000036770325,0.00013106057,0.00018516643,0.00020271144,0.029651716,0.008632088,0.00043206665,0.00091394,0.011227523],"study_design_scores_gemma":[0.000012307056,0.00006228588,0.9784388,0.000006216834,0.000026697848,0.000046755973,0.00008987482,0.018275522,0.0019399837,0.00007676975,0.001014228,0.000010486542],"about_ca_topic_score_codex":0.006351645,"about_ca_topic_score_gemma":0.006891335,"teacher_disagreement_score":0.006351645,"about_ca_system_score_codex":0.00020567651,"about_ca_system_score_gemma":0.00016592958,"threshold_uncertainty_score":0.01262933},"labels":[],"label_agreement":null},{"id":"W2902018380","doi":"10.1029/2018gl080125","title":"Statistical Distributions of Dayside ECH Waves Observed by MMS","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; University of Science and Technology of China; National Natural Science Foundation of China","keywords":"Magnetosphere; Physics; Ionosphere; Daytime; Amplitude; Geophysics; Local time; Earth's magnetic field; Plasmasphere; Atmospheric sciences; Magnetic field; Optics","score_opus":0.027022796893542585,"score_gpt":0.3085207837022602,"score_spread":0.2814979868087176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902018380","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998706,0.000027801114,0.00029772343,0.000012700922,0.00000239676,0.0000036130405,0.00042863897,0.00000974805,0.0005114327],"genre_scores_gemma":[0.99871016,0.000017295824,0.0001164291,0.0000038115827,0.000006368011,0.0000039747215,0.0010220393,0.0000035074318,0.000116568095],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997638,0.000029616493,0.000025881429,0.000060027673,0.00007643612,0.000044366654],"domain_scores_gemma":[0.99865854,0.0003654334,0.0005143087,0.00011797184,0.00021167056,0.00013212975],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003739906,0.0001469987,0.0001861134,0.0012751701,0.00016794715,0.00036877836,0.00016242852,0.00017893717,0.0006611777],"category_scores_gemma":[0.0013204241,0.000102248356,0.00021099266,0.00084423163,0.00029989297,0.00028598326,0.00049054186,0.0001900964,0.00012218274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010761216,0.000013794181,0.98725826,0.000012797622,0.00006261943,0.000093551265,0.00012342079,0.0010635545,0.005727079,0.00015109521,0.0002064756,0.0051796944],"study_design_scores_gemma":[0.0000019229012,0.000019222109,0.99774903,0.0000015989829,0.0000070860206,0.000054510627,0.00009242349,0.0012604899,0.00047901945,0.000039321887,0.00029157032,0.000003863405],"about_ca_topic_score_codex":0.001699269,"about_ca_topic_score_gemma":0.0022199082,"teacher_disagreement_score":0.001699269,"about_ca_system_score_codex":0.00015419493,"about_ca_system_score_gemma":0.00009125142,"threshold_uncertainty_score":0.003378749},"labels":[],"label_agreement":null},{"id":"W2902108975","doi":"10.1029/2018gl079746","title":"Bilinear Magnitude‐Frequency Distributions and Characteristic Earthquakes During Hydraulic Fracturing","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Magnitude (astronomy); Geology; Hydraulic fracturing; Seismology; Bilinear interpolation; Superposition principle; Fault (geology); Range (aeronautics); Earthquake magnitude; Geotechnical engineering; Statistics; Mathematics; Geometry; Physics","score_opus":0.029525458107763178,"score_gpt":0.2822454876317737,"score_spread":0.2527200295240105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902108975","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99843067,0.000016203381,0.0004409355,0.000008519516,5.7884165e-7,0.0000037227,0.00034806115,0.000014015773,0.00073718146],"genre_scores_gemma":[0.9995005,0.000005065527,0.00009567543,0.0000010260042,5.5245937e-7,0.0000011080226,0.00031199807,0.0000015772406,0.00008237903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997805,0.000035756606,0.000018226949,0.000037782138,0.00006829812,0.000059520764],"domain_scores_gemma":[0.99757487,0.000589607,0.00079886796,0.00027400453,0.00047674755,0.00028587985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004372948,0.00012366244,0.00015036209,0.0017271906,0.00025705007,0.0005029332,0.00019971713,0.00014708059,0.0013437144],"category_scores_gemma":[0.0026438762,0.00012112376,0.000091695154,0.0015282902,0.00043716916,0.00025646228,0.00047999996,0.0001914554,0.00020698358],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013592871,0.000022725872,0.9856252,0.000013243714,0.000022782464,0.00008490997,0.0006607894,0.0012612343,0.005619378,0.0002246675,0.00018530573,0.0061438144],"study_design_scores_gemma":[0.0000012617866,0.000010679948,0.9982926,0.0000014399188,0.0000023040227,0.000048723232,0.0002016939,0.0009804057,0.00025992104,0.000070544964,0.0001271432,0.0000033423157],"about_ca_topic_score_codex":0.0677102,"about_ca_topic_score_gemma":0.07628631,"teacher_disagreement_score":0.0677102,"about_ca_system_score_codex":0.0005279326,"about_ca_system_score_gemma":0.00031856424,"threshold_uncertainty_score":0.13463217},"labels":[],"label_agreement":null},{"id":"W2902139091","doi":"10.1029/2018gl080839","title":"Mars Science Laboratory Observations of the 2018/Mars Year 34 Global Dust Storm","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":185,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Canadian Space Agency; Jet Propulsion Laboratory","keywords":"Mars Exploration Program; Dust storm; Martian; Storm; Environmental science; Atmosphere of Mars; Exploration of Mars; Impact crater; Atmospheric sciences; Astrobiology; Meteorology; Geology; Physics","score_opus":0.05195803188292957,"score_gpt":0.3117419190559398,"score_spread":0.2597838871730102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902139091","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9900393,0.00028634074,0.00034095082,0.00016412145,0.00002353263,0.000038643615,0.003438836,0.00021345093,0.0054548434],"genre_scores_gemma":[0.9904827,0.00020752724,0.0016803368,0.000064555024,0.00005399147,0.000029482924,0.0061316714,0.000023206963,0.0013264382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978846,0.00001996642,0.000009619543,0.000042472806,0.00009998807,0.000039519527],"domain_scores_gemma":[0.9997464,0.00001860074,0.000066812725,0.000029450115,0.000086137414,0.000052594616],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040693252,0.00030046853,0.00021685522,0.0008619661,0.0004369652,0.00042373565,0.00025894807,0.00032010474,0.0010735517],"category_scores_gemma":[0.00023742442,0.00010506907,0.00019337518,0.00049932103,0.0001139609,0.00024278267,0.0004936127,0.00033925747,0.0003682177],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021025783,0.00047772404,0.708338,0.00021336655,0.0002572028,0.0015017702,0.0012216213,0.0054914667,0.15915391,0.00036605043,0.02168798,0.09918836],"study_design_scores_gemma":[0.00009808033,0.00044366336,0.9710978,0.00001877841,0.00004274356,0.0001791195,0.00020242501,0.0030209224,0.00860811,0.000066017536,0.01620256,0.000019702835],"about_ca_topic_score_codex":0.005684594,"about_ca_topic_score_gemma":0.011694046,"teacher_disagreement_score":0.005684594,"about_ca_system_score_codex":0.00039682686,"about_ca_system_score_gemma":0.00019653799,"threshold_uncertainty_score":0.011303008},"labels":[],"label_agreement":null},{"id":"W2902276125","doi":"10.1029/2018gl080635","title":"Nonlinear Coupling Between Whistler‐Mode Chorus and Electron Cyclotron Harmonic Waves in the Magnetosphere","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Physics; Magnetosphere; Chorus; Electron; Whistler; Computational physics; Dispersion relation; Harmonic; Van Allen radiation belt; Electron precipitation; Particle acceleration; Electromagnetic radiation; Cyclotron; Quantum electrodynamics; Atomic physics; Plasma; Optics; Acoustics; Quantum mechanics","score_opus":0.01910700377326147,"score_gpt":0.3126805789777138,"score_spread":0.2935735752044523,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2902276125","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966731,0.00008190241,0.00075004116,0.00002955525,0.0000030275107,0.000005109122,0.000014780943,0.000016706537,0.0024258278],"genre_scores_gemma":[0.999587,0.000014073269,0.00014846108,0.0000036042222,0.0000021228782,0.0000020574778,0.000007932363,0.0000016293538,0.00023322442],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.000007267698,0.0000011425416,0.000007375955,0.000011437162,0.000012344075],"domain_scores_gemma":[0.99983144,0.000054435102,0.000044524964,0.00001585388,0.000026060052,0.000027619693],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008499855,0.00012651402,0.000094280105,0.00044069742,0.00021402669,0.00026009418,0.00014555635,0.0001334144,0.0009705385],"category_scores_gemma":[0.000398215,0.00013631876,0.00006995124,0.00023842847,0.00041853107,0.00020190851,0.00041405493,0.00015847973,0.00007104406],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00063731725,0.0000744621,0.15298243,0.00012151275,0.00012020949,0.0023434116,0.0013603378,0.008182088,0.80296046,0.006560275,0.0007329135,0.0239246],"study_design_scores_gemma":[0.00009539264,0.0002541374,0.8356709,0.00002953478,0.00006713292,0.0012018095,0.0010421581,0.07576805,0.07705906,0.0056867,0.0030661141,0.00005916176],"about_ca_topic_score_codex":0.0023408106,"about_ca_topic_score_gemma":0.0019850582,"teacher_disagreement_score":0.0023408106,"about_ca_system_score_codex":0.00017771852,"about_ca_system_score_gemma":0.000101475765,"threshold_uncertainty_score":0.004654348},"labels":[],"label_agreement":null},{"id":"W2903131436","doi":"10.1029/2018gl080126","title":"Temporal and Spatial Correspondence of Pc1/EMIC Waves and Relativistic Electron Precipitations Observed With Ground‐Based Multi‐Instruments on 27 March 2017","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Athabasca University","funders":"Japan Society for the Promotion of Science; Canadian Space Agency; Canada Foundation for Innovation; National Aeronautics and Space Administration","keywords":"Emic and etic; Electron precipitation; Physics; Van Allen radiation belt; Geophysics; Van Allen Probes; Ionosphere; Astrophysics; Computational physics; Electron; Radio wave; Atmospheric sciences; Geology; Magnetosphere; Magnetic field; Nuclear physics","score_opus":0.03496168716817637,"score_gpt":0.30573120587373565,"score_spread":0.27076951870555926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903131436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972193,0.00006596222,0.00014823308,0.00003786024,0.000013938328,0.000009768178,0.0008635609,0.00002489121,0.0016164859],"genre_scores_gemma":[0.9976532,0.00007087046,0.00019546626,0.000011983469,0.000025800304,0.000012078125,0.0015143579,0.000006917368,0.00050937256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998455,0.000011001293,0.0000078493085,0.000031661024,0.000057681315,0.000046268346],"domain_scores_gemma":[0.9995091,0.000041190204,0.00018340423,0.00003679492,0.00013781572,0.00009163406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020017335,0.00019740513,0.00022770242,0.0010854251,0.0003745349,0.0004203067,0.0002979011,0.00024984326,0.0009593437],"category_scores_gemma":[0.0004676578,0.00009180469,0.00014662913,0.0008558656,0.00025951825,0.00016088081,0.00059370446,0.000330199,0.00027481627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003915464,0.00008611117,0.9562989,0.000044679982,0.000109933666,0.0008436302,0.00079368986,0.00089351746,0.023112535,0.00018485705,0.0020504622,0.0151901655],"study_design_scores_gemma":[0.0000037361945,0.000016447459,0.997835,0.0000046471355,0.000009425446,0.000053603744,0.00015941614,0.0002636972,0.00072434865,0.00000945796,0.0009169724,0.00000328071],"about_ca_topic_score_codex":0.025929254,"about_ca_topic_score_gemma":0.052367155,"teacher_disagreement_score":0.025929254,"about_ca_system_score_codex":0.0005001389,"about_ca_system_score_gemma":0.00037969011,"threshold_uncertainty_score":0.051556647},"labels":[],"label_agreement":null},{"id":"W2903160602","doi":"10.1029/2018gl080693","title":"Large‐Scale Ducting of Pc1 Pulsations Observed by Swarm Satellites and Multiple Ground Networks","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Japan Society for the Promotion of Science; Japan Society for the Promotion of Science London; Canadian Space Agency; Korea Astronomy and Space Science Institute; University of Alberta","keywords":"Substorm; Atmospheric duct; Ionosphere; Geophysics; Earth's magnetic field; Local time; Storm; Magnetometer; Geomagnetic storm; Physics; Magnetosphere; Swarm behaviour; Geomagnetic latitude; Middle latitudes; Atmospheric sciences; Geology; Meteorology; Magnetic field; Atmosphere (unit)","score_opus":0.02523699920074005,"score_gpt":0.2829866173250352,"score_spread":0.25774961812429514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903160602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995159,0.000015800104,0.00011281604,0.0000069710027,0.0000014900652,0.0000016018572,0.00006126768,0.00000827288,0.00027586118],"genre_scores_gemma":[0.99969125,0.000011040542,0.000081010425,0.0000022242216,0.0000038818534,0.0000014842885,0.00014655558,0.0000017428271,0.000060798655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999285,0.000008793265,0.0000040449463,0.000020496222,0.000017271781,0.000020876607],"domain_scores_gemma":[0.9996463,0.00006949962,0.00013236492,0.000038568178,0.000043464097,0.000069747286],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012620665,0.00014286659,0.00013618871,0.0007708527,0.00022501094,0.00026998398,0.00012448172,0.00014862078,0.0005452455],"category_scores_gemma":[0.00039094157,0.0000913215,0.0001334788,0.00054921216,0.00016195868,0.00022597908,0.00037991622,0.0001749514,0.000068175505],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001901871,0.000047529324,0.95429945,0.00002416524,0.000075907694,0.0005003653,0.00046279398,0.0030934885,0.028876787,0.0001686876,0.00037550146,0.011885052],"study_design_scores_gemma":[0.0000050430594,0.000041476727,0.9949297,0.000002482689,0.000014294454,0.00010713114,0.00015587994,0.0034516116,0.0009801362,0.00004279477,0.00026636894,0.0000030897831],"about_ca_topic_score_codex":0.0027703743,"about_ca_topic_score_gemma":0.003834377,"teacher_disagreement_score":0.0027703743,"about_ca_system_score_codex":0.00015802945,"about_ca_system_score_gemma":0.00007895668,"threshold_uncertainty_score":0.0055084825},"labels":[],"label_agreement":null},{"id":"W2903451779","doi":"10.1029/2018gl080262","title":"Rapid Loss of Relativistic Electrons by EMIC Waves in the Outer Radiation Belt Observed by Arase, Van Allen Probes, and the PWING Ground Stations","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"Ministry of Science and Higher Education of the Russian Federation; Siberian Branch, Russian Academy of Sciences; Japan Society for the Promotion of Science; National Aeronautics and Space Administration; Russian Foundation for Basic Research; Russian Academy of Sciences; Canada Foundation for Innovation","keywords":"Emic and etic; Physics; Van Allen radiation belt; Electron; Van Allen Probes; Cyclotron; Computational physics; Atomic physics; Nuclear physics; Astrophysics; Geophysics; Magnetosphere; Plasma","score_opus":0.018176381568261527,"score_gpt":0.27516637557128515,"score_spread":0.25698999400302364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903451779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991437,0.000026589541,0.00014883306,0.000010001211,0.0000013797492,0.0000029621942,0.00008236307,0.000012096228,0.0005719055],"genre_scores_gemma":[0.9994087,0.00002369743,0.00015713833,0.0000059820513,0.0000032744695,0.000003911029,0.00022666171,0.0000030780925,0.00016764243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991727,0.000009580148,0.000004586578,0.00002190506,0.000025072346,0.000021649505],"domain_scores_gemma":[0.9997242,0.000039598395,0.00011867895,0.000033235123,0.000048356083,0.000035824698],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023814857,0.00016837205,0.0001702637,0.0008642083,0.00020123026,0.00035630848,0.00026131686,0.00021026187,0.0004704617],"category_scores_gemma":[0.0005662663,0.00013754822,0.00010419485,0.00050100114,0.00017973043,0.00034242534,0.00048242693,0.00024945528,0.0001194191],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032885038,0.000052688367,0.93542176,0.000019559298,0.00005399069,0.00025882828,0.0006256537,0.00040105506,0.05110003,0.0001850507,0.0002036278,0.01134892],"study_design_scores_gemma":[0.000005709827,0.000043267097,0.99695444,0.0000026539922,0.000009725785,0.000067778885,0.00013714255,0.000564435,0.0017255617,0.000023358685,0.00046326546,0.0000026315158],"about_ca_topic_score_codex":0.00426604,"about_ca_topic_score_gemma":0.005579912,"teacher_disagreement_score":0.00426604,"about_ca_system_score_codex":0.00018831741,"about_ca_system_score_gemma":0.0000804509,"threshold_uncertainty_score":0.008482456},"labels":[],"label_agreement":null},{"id":"W2903701390","doi":"10.1029/2018gl079992","title":"Observations of Zooplankton Diel Vertical Migration From High‐Resolution Surface Ocean Optical Measurements","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Diel vertical migration; Zooplankton; Hydrography; Oceanography; Environmental science; Backscatter (email); Geology; Plankton; Polar front; Submarine pipeline","score_opus":0.07766796754690196,"score_gpt":0.27636001351497325,"score_spread":0.19869204596807127,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2903701390","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99851984,0.00003023828,0.0006090797,0.0000072051207,0.0000025568488,0.0000036112583,0.00019502951,0.000021866268,0.00061060727],"genre_scores_gemma":[0.9984711,0.00003588583,0.0009553944,0.000010800889,0.0000049124524,0.000004847887,0.0003109938,0.0000046700084,0.00020134919],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994445,0.000006646086,0.0000026195578,0.000010615252,0.000026538572,0.000009122609],"domain_scores_gemma":[0.9997009,0.00007357424,0.00007780407,0.000020661691,0.00008340529,0.00004369802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018374444,0.00013480728,0.000103995626,0.00058671227,0.00012201777,0.00026197918,0.00009270066,0.00011625131,0.0003724505],"category_scores_gemma":[0.00045431248,0.00010362471,0.00006404449,0.00038968262,0.000087657834,0.00015344603,0.00023086855,0.00012975957,0.000109038956],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024774935,0.00006652737,0.81021714,0.00006230495,0.00007266888,0.00017303793,0.00038674418,0.0017043218,0.14308149,0.000119976175,0.0005203234,0.043347772],"study_design_scores_gemma":[0.0000033906858,0.000030347092,0.994729,0.000004129804,0.000005854988,0.000043745054,0.000058047695,0.0022661125,0.0026098634,0.000021476872,0.0002240164,0.0000039872716],"about_ca_topic_score_codex":0.0020678292,"about_ca_topic_score_gemma":0.006119976,"teacher_disagreement_score":0.0020678292,"about_ca_system_score_codex":0.0001229369,"about_ca_system_score_gemma":0.00009810745,"threshold_uncertainty_score":0.0041115284},"labels":[],"label_agreement":null},{"id":"W2904032259","doi":"10.1029/2018gl080187","title":"Evidence for Stable Holocene Basin‐Scale Overturning Circulation Despite Variable Currents Along the Deep Western Boundary of the North Atlantic Ocean","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"University of North Carolina Wilmington; National Science Foundation","keywords":"Holocene; Thermohaline circulation; Geology; Oceanography; Climatology; Ocean current; Holocene climatic optimum; Younger Dryas; Boundary current; Current (fluid); Climate change","score_opus":0.06252844061836979,"score_gpt":0.31431536280315076,"score_spread":0.25178692218478094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904032259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999241,0.00003544963,0.000048757705,0.000014447898,0.0000013448728,4.5767513e-7,0.000074605094,0.000004385353,0.00057949714],"genre_scores_gemma":[0.99974304,0.000018792603,0.000038308182,0.0000045864745,0.0000010816583,4.966338e-7,0.00010897011,0.0000012838261,0.000083416206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999633,0.000004433813,0.000003013706,0.00001205095,0.0000070784185,0.000010168261],"domain_scores_gemma":[0.99960333,0.000081595885,0.00011168439,0.000047320507,0.00008436178,0.00007180685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012999265,0.00006610495,0.000083882136,0.0003086004,0.00029313407,0.0005412726,0.00015318245,0.00011720611,0.001115639],"category_scores_gemma":[0.00049963576,0.000094935895,0.000078523655,0.00029072852,0.00030726375,0.00018386502,0.00020171396,0.0001634513,0.00015278552],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006607803,0.000013011758,0.9740727,0.000012543503,0.000034400924,0.00006105597,0.00029698116,0.00015044604,0.018742986,0.00012514008,0.00011241998,0.0063121705],"study_design_scores_gemma":[0.0000011026814,0.0000045511147,0.99926037,0.0000020415935,0.0000043586533,0.000018376708,0.000089335255,0.00015072817,0.0003243475,0.000013990012,0.00012966729,0.0000010002107],"about_ca_topic_score_codex":0.020688226,"about_ca_topic_score_gemma":0.052221876,"teacher_disagreement_score":0.020688226,"about_ca_system_score_codex":0.00029971718,"about_ca_system_score_gemma":0.00028305716,"threshold_uncertainty_score":0.04113561},"labels":[],"label_agreement":null},{"id":"W2904427177","doi":"10.1029/2018gl080634","title":"Deglacial to Holocene Ocean Temperatures in the Humboldt Current System as Indicated by Alkenone Paleothermometry","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Partenariat Canadien Contre Le Cancer; Deutsche Forschungsgemeinschaft","keywords":"Alkenone; Holocene; Oceanography; Upwelling; Geology; Sea surface temperature; Climatology; Anticyclone; Subtropics; Walker circulation; Ecology","score_opus":0.02686547631343219,"score_gpt":0.3161072315901135,"score_spread":0.28924175527668133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904427177","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988832,0.00011418878,0.00008107891,0.000032099688,0.000002221097,0.0000010924019,0.00011029266,0.0000051356214,0.00077070115],"genre_scores_gemma":[0.99948895,0.000082739796,0.000084577754,0.000007861116,0.000004320009,0.000001589955,0.00012502918,0.0000019242495,0.00020297743],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997425,0.0000048931815,0.0000015883576,0.00000864806,0.0000039703054,0.0000067651526],"domain_scores_gemma":[0.9998776,0.000013041325,0.000056121156,0.000009691249,0.000025883932,0.00001770649],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011494181,0.00010055489,0.00007717112,0.0005966665,0.00018408622,0.00038104356,0.00008426319,0.00014412719,0.0014300015],"category_scores_gemma":[0.0004229963,0.00007241306,0.00008237469,0.00036363065,0.00022698406,0.0002759,0.00031979725,0.00012228229,0.0001874995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007488629,0.000009838093,0.97503656,0.000022172515,0.00006538036,0.00011902408,0.00054481893,0.00048144572,0.012378105,0.00021063958,0.00013037602,0.010926739],"study_design_scores_gemma":[0.0000013166527,0.000006257471,0.9989066,0.00000379309,0.0000054137577,0.000027525286,0.000095782045,0.00023458514,0.00030895713,0.000040084742,0.0003684202,0.000001298187],"about_ca_topic_score_codex":0.0034995503,"about_ca_topic_score_gemma":0.008593205,"teacher_disagreement_score":0.0034995503,"about_ca_system_score_codex":0.00019608953,"about_ca_system_score_gemma":0.00012314304,"threshold_uncertainty_score":0.0069583654},"labels":[],"label_agreement":null},{"id":"W2904441986","doi":"10.1029/2018gl078608","title":"The Signature of Ozone Depletion in Recent Antarctic Precipitation Change: A Study With the Community Earth System Model","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"North American Construction Group (Canada)","funders":"","keywords":"Precipitation; Environmental science; Ozone depletion; Climatology; Climate change; Atmospheric sciences; Ice core; Climate model; Ozone; Geology; Oceanography; Meteorology; Geography","score_opus":0.08244181128645658,"score_gpt":0.30572084297644847,"score_spread":0.22327903168999189,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904441986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99918956,0.000021574928,0.000150732,0.00006778736,0.000003925902,0.00000414684,0.00030005182,0.000019035177,0.0002430932],"genre_scores_gemma":[0.99905974,0.000019353804,0.0002385075,0.0000151467375,0.0000050234116,0.0000069195007,0.0005860048,0.000008156772,0.00006118875],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998068,0.00009213865,0.000009172899,0.00003619209,0.000022302915,0.000033397184],"domain_scores_gemma":[0.9988281,0.00054180867,0.00013832931,0.00016858075,0.0001682844,0.00015494571],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0014278209,0.00040659073,0.00031426776,0.000437259,0.00047448935,0.0005073393,0.00069345144,0.0006673686,0.0007453528],"category_scores_gemma":[0.0028348756,0.00019420963,0.0006634959,0.00066687807,0.00028118564,0.00060141104,0.0005391748,0.0005251787,0.000103199796],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078200485,0.0007199502,0.63380986,0.00006450967,0.00080628373,0.0002632562,0.00014308577,0.34889343,0.0030445491,0.00088774314,0.0027451776,0.007840087],"study_design_scores_gemma":[0.00021196497,0.0001713437,0.15842967,0.000008223658,0.000113749404,0.000040994288,0.00016425387,0.8388901,0.0010315388,0.00029913938,0.0006131,0.00002583289],"about_ca_topic_score_codex":0.057968616,"about_ca_topic_score_gemma":0.043898184,"teacher_disagreement_score":0.057968616,"about_ca_system_score_codex":0.0006245985,"about_ca_system_score_gemma":0.00066075224,"threshold_uncertainty_score":0.11526239},"labels":[],"label_agreement":null},{"id":"W2904569343","doi":"10.1029/2018gl080099","title":"Air‐Sea CO<sub>2</sub> Flux Estimates in Stratified Arctic Coastal Waters: How Wrong Can We Be?","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of British Columbia; University of Manitoba; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Natural Sciences and Engineering Research Council of Canada; Norsk Polarinstitutt; ArcticNet","keywords":"Seawater; Sink (geography); Environmental science; Arctic; Salinity; Oceanography; Flux (metallurgy); Atmospheric sciences; Sampling (signal processing); Surface water; Surface runoff; Hydrology (agriculture); Geology","score_opus":0.028769485594293532,"score_gpt":0.27204399058172923,"score_spread":0.2432745049874357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904569343","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42392486,0.29512975,0.027423456,0.21770991,0.008385107,0.00013869768,0.0039063767,0.0011065849,0.022275303],"genre_scores_gemma":[0.9203027,0.042583548,0.015761888,0.015467967,0.0021392237,0.00004790046,0.00061727647,0.00012730806,0.0029521906],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9970362,0.0011231257,0.00040531103,0.00038677795,0.00078669103,0.00026183637],"domain_scores_gemma":[0.9807653,0.004455182,0.0014634499,0.0008370009,0.011377936,0.0011011097],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.016791306,0.0010954932,0.0015787513,0.0018300271,0.0020941135,0.007563402,0.0017372303,0.002728646,0.000960686],"category_scores_gemma":[0.03529993,0.00053926423,0.0005737438,0.0014878396,0.0044038934,0.004585829,0.0013319599,0.0022506048,0.00077647093],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005075138,0.000102162274,0.5468583,0.0014497834,0.0015735629,0.00047328777,0.0038080406,0.0058788955,0.002952184,0.0041920836,0.04376533,0.38843888],"study_design_scores_gemma":[0.00007193122,0.00029143956,0.7333449,0.009517332,0.0015673501,0.0007132664,0.030597346,0.018267576,0.0054882523,0.048193805,0.15138747,0.00055924273],"about_ca_topic_score_codex":0.40138185,"about_ca_topic_score_gemma":0.4788121,"teacher_disagreement_score":0.40138185,"about_ca_system_score_codex":0.0056040254,"about_ca_system_score_gemma":0.0064064553,"threshold_uncertainty_score":0.7980911},"labels":[],"label_agreement":null},{"id":"W2904916449","doi":"10.1029/2018gl080902","title":"What Caused the Remarkable February 2018 North Greenland Polynya?","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Office of Naval Research; National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Climatology; Geology; Sea ice; Forcing (mathematics); Oceanography; Environmental science","score_opus":0.029721394289010817,"score_gpt":0.2724227182447689,"score_spread":0.24270132395575805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2904916449","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98266464,0.0005199043,0.00019690237,0.005543129,0.0001071603,0.000009967793,0.00057498564,0.0000287224,0.010354646],"genre_scores_gemma":[0.9968731,0.00038078858,0.0001229337,0.0004362541,0.00004394382,0.0000037054747,0.00013493504,0.000013323721,0.001991037],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.000007727089,0.0000031956176,0.00002868206,0.0000116050005,0.000028502121],"domain_scores_gemma":[0.9997626,0.000016083894,0.00006554139,0.000018248293,0.000061297644,0.0000763189],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022550017,0.00013724701,0.00008805428,0.00030274846,0.0009128246,0.00095451524,0.00016350913,0.00030976973,0.0028324893],"category_scores_gemma":[0.0007494479,0.00007836447,0.000108409746,0.00053088233,0.000654274,0.0004284387,0.00053411245,0.000492066,0.00018825188],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018375067,0.000035883175,0.92312604,0.00013301648,0.000113073766,0.0026656159,0.0034546726,0.002049582,0.008057228,0.0044629704,0.011169957,0.044548284],"study_design_scores_gemma":[0.000006087431,0.000016172313,0.9580186,0.000052770447,0.000022873772,0.00016823322,0.0043359087,0.000919133,0.0011010338,0.0011057943,0.034239866,0.000013601541],"about_ca_topic_score_codex":0.26415953,"about_ca_topic_score_gemma":0.39369753,"teacher_disagreement_score":0.26415953,"about_ca_system_score_codex":0.0038124092,"about_ca_system_score_gemma":0.0013927573,"threshold_uncertainty_score":0.5252439},"labels":[],"label_agreement":null},{"id":"W2905213451","doi":"10.1029/2018gl080942","title":"Heterogeneous Changes in Western North American Glaciers Linked to Decadal Variability in Zonal Wind Strength","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":120,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Global Water Futures; Jet Propulsion Laboratory; Centre National d’Etudes Spatiales; BC Hydro; Ames Research Center; Tula Foundation; Hakai Institute; Ohio State University; National Aeronautics and Space Administration; National Park Service; U.S. Geological Survey; University of Northern British Columbia; National Science Foundation","keywords":"Glacier; Climatology; Glacier mass balance; Climate change; Geology; Terrain; Elevation (ballistics); Physical geography; Digital elevation model; Sea level rise; Sea level; Environmental science; Oceanography; Geography; Geomorphology; Remote sensing; Cartography","score_opus":0.0405472274358932,"score_gpt":0.3021799853572252,"score_spread":0.261632757921332,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905213451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99931026,0.000019936362,0.000040000603,0.000021630152,0.0000020979492,0.0000014346941,0.00034567376,0.000006901133,0.0002519819],"genre_scores_gemma":[0.9992937,0.000017954453,0.000045494588,0.000006915599,0.0000021646415,0.0000022133934,0.000536977,0.000001826986,0.00009268486],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993396,0.0000106913385,0.000005075647,0.000026076921,0.000011658417,0.000012515423],"domain_scores_gemma":[0.9996276,0.0000530893,0.00012959725,0.000049237675,0.00008837781,0.00005204638],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031910196,0.0001451969,0.00009954607,0.00061848137,0.00021498938,0.00051054254,0.00012615538,0.00016065499,0.000767789],"category_scores_gemma":[0.00066151936,0.00010322027,0.00013410328,0.00065023307,0.00021371385,0.00028671653,0.00030314707,0.00018210823,0.00010551758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043726708,0.000026706186,0.9937459,0.0000053002877,0.000042407213,0.00003477421,0.00014773733,0.001155696,0.0013451126,0.000039731996,0.0003117076,0.0031011642],"study_design_scores_gemma":[9.168055e-7,0.0000032455566,0.9987839,0.0000014310954,0.0000048653505,0.000008548196,0.00007103751,0.0009213972,0.000056073834,0.000015903743,0.00013104195,0.0000015074553],"about_ca_topic_score_codex":0.028501969,"about_ca_topic_score_gemma":0.049174722,"teacher_disagreement_score":0.971498,"about_ca_system_score_codex":0.00031505252,"about_ca_system_score_gemma":0.00017405722,"threshold_uncertainty_score":0.056672096},"labels":[],"label_agreement":null},{"id":"W2905349995","doi":"10.1029/2018gl080956","title":"Extreme Variability in Irminger Sea Winter Heat Loss Revealed by Ocean Observatories Initiative Mooring and the ERA5 Reanalysis","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":60,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dairy Farmers of Ontario; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Mooring; Climatology; Environmental science; Forcing (mathematics); Oceanography; Latitude; North Atlantic oscillation; Middle latitudes; Sea surface temperature; Atmospheric sciences; Geology","score_opus":0.06366129747426981,"score_gpt":0.30632065645419976,"score_spread":0.24265935897992996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905349995","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99941194,0.000010339147,0.00003838354,0.000009594668,0.0000014404916,0.0000012162171,0.00022017893,0.0000062608274,0.0003006486],"genre_scores_gemma":[0.99937564,0.000012020323,0.000051695537,0.0000052836563,0.000003564224,0.0000023127072,0.0004447482,0.0000024639592,0.00010234399],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999219,0.000010054338,0.000005765682,0.000022515656,0.000013678177,0.000026065243],"domain_scores_gemma":[0.9997923,0.000025944222,0.00008941478,0.000028116727,0.000026211394,0.000038049042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027599497,0.00020217145,0.00018924027,0.00048754236,0.00019761284,0.00035377097,0.00014535926,0.00023506318,0.00063616666],"category_scores_gemma":[0.000487076,0.00010574543,0.00025746238,0.00042887614,0.00021045862,0.00029775884,0.00040742318,0.00021364907,0.00012221583],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028855162,0.000050248258,0.9800096,0.000012219529,0.00014677545,0.0001570283,0.0002545653,0.0027084062,0.009199329,0.000104662664,0.00049425144,0.0065742824],"study_design_scores_gemma":[0.0000017853876,0.00001588309,0.9987355,0.0000013345921,0.000006876895,0.000012307678,0.000028563969,0.0007867706,0.00029309146,0.000010622882,0.00010504245,0.0000023323626],"about_ca_topic_score_codex":0.008610865,"about_ca_topic_score_gemma":0.013911952,"teacher_disagreement_score":0.008610865,"about_ca_system_score_codex":0.00029441516,"about_ca_system_score_gemma":0.00015442698,"threshold_uncertainty_score":0.017121494},"labels":[],"label_agreement":null},{"id":"W2905540889","doi":"10.1029/2018gl080473","title":"Limited Retention of Wildfire‐Derived PAHs and Trace Elements in Indoor Environments","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta; Alberta Environment and Protected Areas; Public Health Ontario; University of Toronto","funders":"Canadian HIV Trials Network, Canadian Institutes of Health Research","keywords":"Environmental science; Pollutant; Pollution; Air pollution; Environmental chemistry; Environmental protection; Chemistry","score_opus":0.02219226018479494,"score_gpt":0.2779439148495501,"score_spread":0.2557516546647552,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2905540889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984754,0.00023330389,0.0002517185,0.000013654169,0.0000024376466,0.0000036403287,0.00015960001,0.0000068002446,0.00085339666],"genre_scores_gemma":[0.9985966,0.00013568858,0.00029128973,0.000014081948,0.0000016168261,0.0000026278965,0.0001605715,0.0000020736318,0.00079530134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997886,0.000015731812,0.000008176264,0.00005225222,0.00007880157,0.000056500277],"domain_scores_gemma":[0.9997154,0.000027270862,0.00009075908,0.000028502724,0.00010258549,0.000035343994],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019727321,0.00017237947,0.00017912511,0.00027918137,0.0005413481,0.00089965895,0.0003571725,0.00020955017,0.000894533],"category_scores_gemma":[0.0002559137,0.00010858688,0.000110214045,0.0003544485,0.00042588153,0.00026329604,0.00030064702,0.00018158181,0.00012530896],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048655577,0.00013035182,0.78470474,0.00014228257,0.000091070906,0.00031043097,0.00085970823,0.00065624894,0.18505971,0.0002305658,0.00036320655,0.026965203],"study_design_scores_gemma":[0.0000026814175,0.0001407911,0.9696581,0.00001797886,0.000019582088,0.00019639813,0.0013065563,0.00029318238,0.026947122,0.00013163107,0.0012794255,0.000006597422],"about_ca_topic_score_codex":0.11459692,"about_ca_topic_score_gemma":0.29124376,"teacher_disagreement_score":0.11459692,"about_ca_system_score_codex":0.0010072481,"about_ca_system_score_gemma":0.0010158389,"threshold_uncertainty_score":0.22785974},"labels":[],"label_agreement":null},{"id":"W2906710521","doi":"10.1029/2018gl080260","title":"Observed Spatiotemporal Changes in the Mechanisms of Extreme Water Available for Runoff in the Western United States","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Pacific Northwest National Laboratory; Strategic Environmental Research and Development Program; Natural Resources Conservation Service; Battelle; Commission for Environmental Cooperation; U.S. Department of Energy","keywords":"Snowmelt; Snowpack; Environmental science; Hydrometeorology; Snow; Surface runoff; Climatology; Climate change; Water year; Hydrology (agriculture); Water resources; Atmospheric sciences; Precipitation; Meteorology; Geography; Geology; Oceanography; Ecology","score_opus":0.13321464974117217,"score_gpt":0.2853608050322389,"score_spread":0.1521461552910667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2906710521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988697,0.00008411557,0.000116587384,0.000037106045,0.0000024842554,0.0000022904615,0.0005743144,0.000007787647,0.00030555727],"genre_scores_gemma":[0.999236,0.000056972433,0.00010093468,0.0000121584835,0.000003236894,0.0000041503245,0.0005269139,0.000001398749,0.00005826084],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989736,0.000023176879,0.00001052307,0.000031634234,0.000020694899,0.00001661349],"domain_scores_gemma":[0.9994848,0.00008143843,0.00023897222,0.000045728153,0.00010405729,0.000045007357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030692705,0.00010702229,0.00015284921,0.0006255392,0.00020718045,0.00039951593,0.00019743072,0.0001461601,0.00044447382],"category_scores_gemma":[0.00069431344,0.00009848547,0.0001227386,0.00093388575,0.00020520303,0.00027391015,0.00034322296,0.00016274044,0.00005976544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003334017,0.000021493539,0.9944003,0.0000086060745,0.000056877714,0.000033479824,0.0001577159,0.0003709673,0.0011164615,0.00006236973,0.0003376306,0.003400874],"study_design_scores_gemma":[8.484081e-7,0.0000065134473,0.99922514,0.0000021085955,0.000005532975,0.000012612049,0.00008909253,0.00028013266,0.00011225485,0.000012210956,0.00025218996,0.000001342701],"about_ca_topic_score_codex":0.040746875,"about_ca_topic_score_gemma":0.07466154,"teacher_disagreement_score":0.040746875,"about_ca_system_score_codex":0.0003639223,"about_ca_system_score_gemma":0.00021689408,"threshold_uncertainty_score":0.0810194},"labels":[],"label_agreement":null},{"id":"W2907878779","doi":"10.1029/2018gl080749","title":"Distribution of Areal Strain on Mercury: Insights Into the Interaction of Volcanism and Global Contraction","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Lithosphere; Geology; Volcano; Volcanism; Tectonics; Spatial distribution; Contraction (grammar); Seismology; Remote sensing","score_opus":0.028428659093035623,"score_gpt":0.31672843939973444,"score_spread":0.28829978030669884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2907878779","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990879,0.00002510723,0.00010706632,0.000019394058,3.4787698e-7,8.37965e-7,0.00011236902,0.000007850411,0.00063912984],"genre_scores_gemma":[0.99980384,0.00001511359,0.00006358745,0.0000025801446,0.0000015537361,6.423082e-7,0.00006486394,0.0000031068544,0.00004473727],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989176,0.000025241226,0.0000054685415,0.000028045177,0.00002783991,0.000021614316],"domain_scores_gemma":[0.9994867,0.00018313917,0.00014303744,0.000039637456,0.00009050005,0.00005681644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024261631,0.00011668278,0.0002228411,0.0018251608,0.00019779059,0.0004736035,0.00024303189,0.00020980046,0.0012603686],"category_scores_gemma":[0.00094124116,0.00014701384,0.00013982221,0.0018799397,0.00043999244,0.00029836607,0.00036859175,0.00014072063,0.00014945869],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007490616,0.00001802429,0.9745617,0.000015827829,0.00006214157,0.000116543444,0.00039289964,0.0020338113,0.013862559,0.00023660093,0.00010737499,0.008517537],"study_design_scores_gemma":[5.964951e-7,0.0000045839856,0.99823487,9.2805794e-7,0.000002987474,0.00002043666,0.00007333168,0.0014313377,0.00013440121,0.00004331288,0.000051402607,0.0000017867201],"about_ca_topic_score_codex":0.008679903,"about_ca_topic_score_gemma":0.010822495,"teacher_disagreement_score":0.008679903,"about_ca_system_score_codex":0.00031326205,"about_ca_system_score_gemma":0.000096171905,"threshold_uncertainty_score":0.017258763},"labels":[],"label_agreement":null},{"id":"W2908078625","doi":"10.1029/2018gl081274","title":"Warming Effects of Spring Rainfall Increase Methane Emissions From Thawing Permafrost","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":130,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Pacific Northwest Research Station; National Science Foundation of Sri Lanka; Biological and Environmental Research; U.S. Forest Service; U.S. Geological Survey; Office of Science; U.S. Department of Agriculture; U.S. Department of Energy; National Science Foundation","keywords":"Permafrost; Environmental science; Tundra; Wetland; Methane; Soil water; Global warming; Atmospheric methane; Greenhouse gas; Radiative forcing; Thermokarst; Snowmelt; Hydrology (agriculture); Spring (device); Climate change; Atmospheric sciences; Snow; Arctic; Geology; Soil science; Ecology; Oceanography","score_opus":0.03782632328377082,"score_gpt":0.2959893349199445,"score_spread":0.25816301163617367,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908078625","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984011,0.000107869935,0.00016713022,0.000046604473,0.0000053748163,0.0000024366864,0.00023200901,0.000020528989,0.0010168792],"genre_scores_gemma":[0.99967194,0.000029153818,0.000069680325,0.000018147046,0.000003825072,0.0000018117552,0.00007315345,0.00000269741,0.00012949872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993575,0.000013236884,0.0000037717778,0.000019438134,0.000008175222,0.000019524003],"domain_scores_gemma":[0.9998209,0.00007475781,0.000037460108,0.000012838141,0.000021241844,0.000032953234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001740154,0.00012645082,0.00014936778,0.00017142094,0.00021743432,0.00032082514,0.00012492311,0.00016588482,0.00259146],"category_scores_gemma":[0.00022443649,0.000086459404,0.00018719262,0.00013747676,0.00014566298,0.00021385166,0.00027488728,0.00028955837,0.00012213814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082929555,0.00013790243,0.7088889,0.00013418314,0.00015713021,0.00035656674,0.00028552473,0.003212734,0.27175203,0.0003532897,0.0005675663,0.013324936],"study_design_scores_gemma":[0.000005187558,0.0000566501,0.991608,0.0000042311763,0.000017896502,0.000048735645,0.00012858622,0.0011766384,0.0063486267,0.00013206157,0.00046992855,0.0000034798666],"about_ca_topic_score_codex":0.003889007,"about_ca_topic_score_gemma":0.0053540124,"teacher_disagreement_score":0.003889007,"about_ca_system_score_codex":0.0003200495,"about_ca_system_score_gemma":0.00016638428,"threshold_uncertainty_score":0.008669317},"labels":[],"label_agreement":null},{"id":"W2908418060","doi":"10.1029/2018gl081095","title":"High‐Resolution Mapping of Nitrogen Dioxide With TROPOMI: First Results and Validation Over the Canadian Oil Sands","year":2018,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":449,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Dalhousie University; University of Saskatchewan; Environment and Climate Change Canada","funders":"","keywords":"Environmental science; Nitrogen dioxide; Remote sensing; Oil sands; Troposphere; Satellite; Nadir; Atmospheric sciences; Meteorology; Geology; Materials science","score_opus":0.013991115522306998,"score_gpt":0.23164747106821995,"score_spread":0.21765635554591295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908418060","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99272186,0.00016508691,0.001577919,0.000069092035,0.000014336291,0.000076287055,0.002603085,0.00025697306,0.0025153456],"genre_scores_gemma":[0.9890939,0.00016868509,0.0064166663,0.000049179333,0.0000078805815,0.000035795998,0.0034135142,0.000050647825,0.0007636403],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99961084,0.00001672559,0.000010340101,0.000082888335,0.00017676607,0.00010251208],"domain_scores_gemma":[0.99962735,0.000033641176,0.000038358547,0.000038057675,0.000197116,0.00006544633],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005374293,0.0010373747,0.0005077481,0.0009441481,0.0015268145,0.0007615863,0.0011451221,0.0005216885,0.00059212523],"category_scores_gemma":[0.0005827378,0.00036464966,0.00047386088,0.0014449299,0.0005579072,0.00048138353,0.00058484025,0.0005247209,0.0001892659],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022461521,0.0019205386,0.5048123,0.0003863705,0.000725129,0.0016012825,0.0019057756,0.08609623,0.3093595,0.000628557,0.005797738,0.08452038],"study_design_scores_gemma":[0.00027619535,0.00027076853,0.8572911,0.000040806783,0.00017195,0.00016781758,0.00068794173,0.09874598,0.03710812,0.00012954994,0.00497988,0.00012983738],"about_ca_topic_score_codex":0.8604528,"about_ca_topic_score_gemma":0.92534643,"teacher_disagreement_score":0.13954723,"about_ca_system_score_codex":0.003796922,"about_ca_system_score_gemma":0.0044774,"threshold_uncertainty_score":0.28073806},"labels":[],"label_agreement":null},{"id":"W2908794046","doi":"10.1029/2018gl081603","title":"Forage Species Swarm in Response to Coastal Upwelling","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and fisheries research","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"McGill University; W. M. Keck Foundation; David and Lucile Packard Foundation","keywords":"Upwelling; Bay; Forage; Biomass (ecology); Ecosystem; Oceanography; Environmental science; Ecology; Krill; Biology; Geology","score_opus":0.02895230902115571,"score_gpt":0.29888152884531516,"score_spread":0.26992921982415946,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2908794046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99955446,0.00003529459,0.00003503679,0.0000071325358,0.0000012900562,0.0000023493321,0.00006613849,0.0000037705804,0.0002945664],"genre_scores_gemma":[0.99945253,0.000029524292,0.00010129893,0.000015222448,0.0000026041344,0.0000049387027,0.00013040315,0.000001725613,0.00026159952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999316,0.000008963767,0.000004708192,0.000023959385,0.000015506135,0.000015366108],"domain_scores_gemma":[0.99939466,0.00010264916,0.00022081292,0.000034497592,0.00011046601,0.00013703198],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014577054,0.000111203204,0.00017588203,0.0005515692,0.00035030916,0.000344162,0.00017018986,0.00015040253,0.0012836539],"category_scores_gemma":[0.0005430774,0.00014997162,0.00012183894,0.00024571925,0.00023624187,0.00017603471,0.00040500137,0.00023979934,0.00014735419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024355415,0.00007596079,0.9152526,0.00006087762,0.00008520293,0.0001940537,0.0013682191,0.0002965644,0.07241423,0.000050296247,0.00039072652,0.009567727],"study_design_scores_gemma":[0.0000015199323,0.000032400723,0.9992471,0.0000022214613,0.0000048418,0.000023071374,0.00020110348,0.00013430252,0.0002335029,0.000006956518,0.00011129272,0.0000017270953],"about_ca_topic_score_codex":0.009743495,"about_ca_topic_score_gemma":0.030873327,"teacher_disagreement_score":0.009743495,"about_ca_system_score_codex":0.00029934253,"about_ca_system_score_gemma":0.0001015379,"threshold_uncertainty_score":0.019373536},"labels":[],"label_agreement":null},{"id":"W2909658472","doi":"10.1029/2018gl080301","title":"Insights on Hydrothermal‐Magmatic Interactions and Eruptive Processes at Poás Volcano (Costa Rica) From High‐Frequency Gas Monitoring and Drone Measurements","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Phreatomagmatic eruption; Phreatic eruption; Geology; Volcano; Phreatic; Explosive eruption; Maar; Magma; Hydrothermal circulation; Geochemistry; Earth science; Seismology; Geophysics; Petrology; Aquifer; Groundwater","score_opus":0.04392882884632292,"score_gpt":0.270861168632074,"score_spread":0.22693233978575106,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909658472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976234,0.00020147795,0.00013578625,0.00005083537,0.000001279889,0.0000057402403,0.0003495027,0.00001107572,0.0016208094],"genre_scores_gemma":[0.9994288,0.000104050676,0.00011890634,0.00000697112,0.0000023764094,0.0000023323155,0.0001695327,0.0000018536851,0.00016509503],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996483,0.000009227629,0.0000025378329,0.000008195546,0.0000068047148,0.000008493678],"domain_scores_gemma":[0.99986947,0.000019955243,0.000049603867,0.000013669557,0.000032218893,0.00001512981],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016747379,0.00012378844,0.00009005821,0.0005349975,0.00016248801,0.00030587282,0.00014255618,0.00018409011,0.00039930712],"category_scores_gemma":[0.00030048197,0.000073486706,0.000076161064,0.0005076927,0.00018690317,0.00017960418,0.00025267675,0.00010393328,0.00006600952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006798515,0.000025182353,0.96206385,0.00005264409,0.00004884837,0.0002859139,0.000688272,0.0014123798,0.020575995,0.00020202764,0.00033944292,0.014237416],"study_design_scores_gemma":[0.0000010237138,0.00000501816,0.9978963,0.000004487165,0.0000061642245,0.000027877937,0.00017395818,0.0010024789,0.00030599372,0.000016385935,0.0005587239,0.0000015340925],"about_ca_topic_score_codex":0.041707948,"about_ca_topic_score_gemma":0.07897545,"teacher_disagreement_score":0.041707948,"about_ca_system_score_codex":0.00033929953,"about_ca_system_score_gemma":0.0002087051,"threshold_uncertainty_score":0.08293033},"labels":[],"label_agreement":null},{"id":"W2909737041","doi":"10.1029/2018gl081550","title":"Sensitivity of EMIC Wave‐Driven Scattering Loss of Ring Current Protons to Wave Normal Angle Distribution","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Scattering; Cyclotron; Ring current; Physics; Pitch angle; Atomic physics; Computational physics; Ion; Magnetic field; Optics; Magnetosphere","score_opus":0.01852862647672558,"score_gpt":0.28591423358813883,"score_spread":0.26738560711141324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909737041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99045676,0.00019159364,0.0062433667,0.000041624226,0.00001883,0.00001652763,0.0002576923,0.00014635765,0.00262732],"genre_scores_gemma":[0.999278,0.000053921493,0.00028466422,0.0000119525885,0.0000026407376,0.0000035042556,0.00011068278,0.000013730881,0.00024085064],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998411,0.000023485463,0.0000055991795,0.000058173002,0.00003655294,0.000035009663],"domain_scores_gemma":[0.9993654,0.00026584603,0.00011033443,0.000071180286,0.00014126679,0.000045975903],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045693657,0.0002555168,0.00024344074,0.00037418102,0.00014502823,0.00043974462,0.00034726667,0.00023439804,0.0017818232],"category_scores_gemma":[0.0016261117,0.00015528282,0.00015477902,0.0002765684,0.0002897329,0.00053087703,0.00040032418,0.00035756806,0.00026765195],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020430938,0.00018914053,0.15603954,0.00020734683,0.00025539583,0.00046555573,0.00028229412,0.19125809,0.6149866,0.00198805,0.001131013,0.03115381],"study_design_scores_gemma":[0.00005728504,0.00034296178,0.15481645,0.000017215958,0.000054128188,0.00026128703,0.00020966413,0.547734,0.2946205,0.00080622925,0.0010225696,0.00005765736],"about_ca_topic_score_codex":0.0020071894,"about_ca_topic_score_gemma":0.00057836564,"teacher_disagreement_score":0.0020071894,"about_ca_system_score_codex":0.00033424576,"about_ca_system_score_gemma":0.000118264456,"threshold_uncertainty_score":0.0059607625},"labels":[],"label_agreement":null},{"id":"W2909981771","doi":"10.1029/2018gl081011","title":"Crustal Structure in Alaska From Receiver Function Analysis","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Crust; Receiver function; Underplating; Seismology; Isostasy; Mantle (geology); Upper crust; Oceanic crust; Tectonics; Lithosphere; Subduction; Geophysics","score_opus":0.015178299849226057,"score_gpt":0.2532966569183458,"score_spread":0.23811835706911974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2909981771","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994464,0.00038831925,0.0020460277,0.000011540839,0.0000032491023,0.0000023350149,0.0011840239,0.00007495576,0.001825677],"genre_scores_gemma":[0.9977314,0.00009975722,0.0010138979,0.0000018007353,0.0000017564364,0.000001991805,0.00084510684,0.000004474221,0.0002998781],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999461,0.0000077596105,0.0000050400627,0.00001593565,0.000016410313,0.000008700196],"domain_scores_gemma":[0.99979824,0.0000337057,0.00004745095,0.00001636087,0.00008543451,0.000018828334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001817871,0.000181141,0.00009714773,0.0015594288,0.0001961834,0.00038208207,0.00013942346,0.00009472104,0.0010421169],"category_scores_gemma":[0.0005873196,0.00010452923,0.00016128707,0.0010210561,0.000089389905,0.00020071918,0.00024112286,0.00011880565,0.00024278082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012272375,0.00001392408,0.92236376,0.000052044605,0.0001354613,0.00024620368,0.00032871988,0.011288277,0.013837388,0.0003279283,0.00037590016,0.05090759],"study_design_scores_gemma":[0.0000023023838,0.000016135376,0.98808575,0.000016765325,0.000029727098,0.0001257987,0.00015671617,0.009182538,0.0011130788,0.00025753258,0.001003816,0.000009874548],"about_ca_topic_score_codex":0.07221354,"about_ca_topic_score_gemma":0.06374639,"teacher_disagreement_score":0.07221354,"about_ca_system_score_codex":0.00036061995,"about_ca_system_score_gemma":0.000278431,"threshold_uncertainty_score":0.1435864},"labels":[],"label_agreement":null},{"id":"W2912473035","doi":"10.1029/2018gl081087","title":"Meridional Gulf Stream Shifts Can Influence Wintertime Variability in the North Atlantic Storm Track and Greenland Blocking","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Climate Program Office; Division of Atmospheric and Geospace Sciences; Division of Ocean Sciences; National Science Foundation of Sri Lanka; Woods Hole Oceanographic Institution; National Aeronautics and Space Administration; National Science Foundation","keywords":"Storm track; Climatology; Storm; Gulf Stream; Jet stream; Zonal and meridional; Geology; Winter storm; Middle latitudes; Oceanography; Jet (fluid)","score_opus":0.02252356784161254,"score_gpt":0.2733726726179,"score_spread":0.25084910477628747,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912473035","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99935025,0.0000138860305,0.000014172811,0.000035129702,0.0000018486883,6.7096e-7,0.00013561056,0.000002189488,0.0004462549],"genre_scores_gemma":[0.99967706,0.000014581148,0.00001422212,0.000010038589,0.0000016025555,7.4965146e-7,0.00014424756,0.000001804887,0.000135781],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994206,0.000013145511,0.000003562994,0.00001277115,0.000009093723,0.000019363766],"domain_scores_gemma":[0.99955255,0.0000945437,0.00017362801,0.00003237066,0.00004564537,0.000101324236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001980903,0.00008910973,0.000094591516,0.00027601814,0.00017421278,0.00051312556,0.000112126174,0.00015175581,0.001302625],"category_scores_gemma":[0.0008401865,0.00006070944,0.00015475511,0.00034951937,0.0001836756,0.00018993825,0.00022315473,0.00017106434,0.00017186611],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006345084,0.000028914254,0.99577075,0.0000023700381,0.00002981312,0.000034726167,0.00012683395,0.0004033375,0.0013057408,0.000081054764,0.00027822814,0.0018747805],"study_design_scores_gemma":[0.0000010272885,0.0000036704296,0.99951744,9.672724e-7,0.0000028194893,0.0000034156747,0.00006666099,0.00025274322,0.00003680909,0.000013948896,0.00009986568,7.309179e-7],"about_ca_topic_score_codex":0.051811665,"about_ca_topic_score_gemma":0.121163785,"teacher_disagreement_score":0.051811665,"about_ca_system_score_codex":0.0004370835,"about_ca_system_score_gemma":0.00031896937,"threshold_uncertainty_score":0.10302019},"labels":[],"label_agreement":null},{"id":"W2912939321","doi":"10.1029/2018gl081584","title":"Arctic‐Boreal Lake Dynamics Revealed Using CubeSat Imagery","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Fish and Wildlife Service; University of Washington; National Aeronautics and Space Administration; University of North Carolina at Chapel Hill; National Science Foundation","keywords":"Environmental science; Boreal; Arctic; Satellite imagery; Surface water; Shore; Trace gas; Terrain; Vegetation (pathology); Physical geography; CubeSat; Landform; Climatology; Geology; Hydrology (agriculture); Satellite; Remote sensing; Oceanography; Atmospheric sciences; Ecology; Geography; Geomorphology","score_opus":0.06100942073590812,"score_gpt":0.3116006935421331,"score_spread":0.25059127280622495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2912939321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944939,0.000078419616,0.00058876554,0.00005983793,0.000008978261,0.000008742622,0.0027471741,0.00011717161,0.0018969903],"genre_scores_gemma":[0.9944944,0.00006130221,0.0018629783,0.000020413703,0.000007302356,0.0000059699755,0.0032559843,0.00001460511,0.00027691544],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999018,0.00000881439,0.000004839122,0.000029904415,0.000035567653,0.00001911183],"domain_scores_gemma":[0.9998311,0.000016613356,0.00003860014,0.000024347475,0.00006625012,0.000023083581],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016389781,0.00020685454,0.0001150427,0.00094952824,0.0003445686,0.00056727725,0.00013926177,0.00013984075,0.00071894936],"category_scores_gemma":[0.00037509872,0.00011908795,0.0002255333,0.0010890331,0.00019489117,0.00030336968,0.0003131226,0.0001496913,0.00015860036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023273987,0.00011743412,0.8969954,0.000042548007,0.00024858007,0.00019827358,0.00042316623,0.021122582,0.027893217,0.00034284408,0.0043393485,0.048043866],"study_design_scores_gemma":[0.0000070505785,0.000015082529,0.9638227,0.0000072123626,0.000027801934,0.00005993826,0.00023046097,0.031845946,0.0018509028,0.00011185923,0.0020051668,0.00001573301],"about_ca_topic_score_codex":0.13366945,"about_ca_topic_score_gemma":0.25258052,"teacher_disagreement_score":0.13366945,"about_ca_system_score_codex":0.00050659804,"about_ca_system_score_gemma":0.00042313666,"threshold_uncertainty_score":0.26578277},"labels":[],"label_agreement":null},{"id":"W2913179981","doi":"10.1029/2018gl080996","title":"Significant Floodplain Soil Organic Carbon Storage Along a Large High‐Latitude River and its Tributaries","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Fish and Wildlife Service; National Geographic Society; National Science Foundation","keywords":"Permafrost; Floodplain; Tributary; Environmental science; Soil carbon; Climate change; Hydrology (agriculture); Total organic carbon; Sediment; Physical geography; Geology; Soil water; Soil science; Oceanography; Geomorphology; Geography; Ecology","score_opus":0.03047761870707569,"score_gpt":0.2622680066935439,"score_spread":0.2317903879864682,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913179981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997507,0.00000614609,0.000029482444,0.0000048626202,2.0388849e-7,4.5207943e-7,0.00007421123,0.0000020459759,0.00013194793],"genre_scores_gemma":[0.99982446,0.0000051265574,0.000040021492,0.0000012502416,4.190689e-7,6.929736e-7,0.00006956851,3.333038e-7,0.000058165708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999466,0.000010771103,0.000004855607,0.000017918752,0.000008249896,0.000011615826],"domain_scores_gemma":[0.99973494,0.00006676699,0.00007646249,0.000031731666,0.00004644102,0.00004353719],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001302742,0.00008701539,0.000098270175,0.00044544722,0.00043264905,0.0004018804,0.00013503603,0.00014450755,0.0006979529],"category_scores_gemma":[0.00027944447,0.00008278235,0.00009793331,0.0005471441,0.00026921002,0.00026660113,0.00021861796,0.00008429477,0.000063645275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000026326856,0.000016892096,0.9944811,0.000005256811,0.000021470925,0.00007769579,0.00024109523,0.00033769567,0.002009055,0.000054493787,0.000060295133,0.002668565],"study_design_scores_gemma":[0.0000010570963,0.00000701661,0.9989146,0.0000012939912,0.000005263776,0.000028976569,0.00023240854,0.0005280831,0.00017285356,0.00002170195,0.00008527253,0.0000014641951],"about_ca_topic_score_codex":0.028028239,"about_ca_topic_score_gemma":0.067594685,"teacher_disagreement_score":0.028028239,"about_ca_system_score_codex":0.0003297683,"about_ca_system_score_gemma":0.00030778945,"threshold_uncertainty_score":0.055730224},"labels":[],"label_agreement":null},{"id":"W2913214501","doi":"10.1029/2018gl080720","title":"Atmospheric Rivers Increase Future Flood Risk in Western Canada's Largest Pacific River","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Northern British Columbia; Pacific Institute for Climate Solutions; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Streamflow; Coupled model intercomparison project; Pluvial; Snowpack; Environmental science; Drainage basin; Climatology; Flood myth; Snow; Climate change; Hydrometeorology; Surface runoff; Climate model; Hydrology (agriculture); Precipitation; Geology; Oceanography; Meteorology; Geography","score_opus":0.009978958072685342,"score_gpt":0.2392427406453013,"score_spread":0.22926378257261595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2913214501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958022,0.000045310997,0.000072729265,0.00039861948,0.0000037060013,0.00000377545,0.00089319574,0.00001543347,0.0027651147],"genre_scores_gemma":[0.9990264,0.000036739646,0.000056279372,0.00002609284,0.0000016797029,0.0000016013415,0.00021822902,0.0000026423093,0.00063032616],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999075,0.000009992357,0.0000034794145,0.000020302708,0.000021974622,0.00003679776],"domain_scores_gemma":[0.99964666,0.000051861567,0.00005750344,0.000016051232,0.000110720975,0.00011716043],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001763245,0.00013534077,0.00009889664,0.00031938046,0.0010085241,0.0011393153,0.00035665327,0.00033420214,0.0030604824],"category_scores_gemma":[0.00094536314,0.00011951284,0.0002466297,0.00053654634,0.0003091216,0.00027159628,0.00058346026,0.00043135573,0.00010448219],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005810042,0.000035640875,0.98428833,0.000007952478,0.00004535338,0.00014693597,0.00018731809,0.0075811576,0.00038001194,0.00087220105,0.002271287,0.0041258503],"study_design_scores_gemma":[0.000013043648,0.000013952775,0.97106737,0.000013559472,0.00004561964,0.00005423375,0.00111661,0.024647158,0.00021006439,0.00072763424,0.0020771998,0.000013606715],"about_ca_topic_score_codex":0.9491596,"about_ca_topic_score_gemma":0.9654319,"teacher_disagreement_score":0.050840378,"about_ca_system_score_codex":0.0060649193,"about_ca_system_score_gemma":0.0067665074,"threshold_uncertainty_score":0.102279544},"labels":[],"label_agreement":null},{"id":"W2914599041","doi":"10.1029/2018gl081317","title":"On the Close Correspondence Between Storm Time ULF Wave Power and the POES VLF Chorus Wave Amplitude Proxy","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Chorus; Amplitude; Storm; Geology; Proxy (statistics); Geophysics; Meteorology; Physics; Mathematics; Statistics; Oceanography; Art; Optics","score_opus":0.014342329363857261,"score_gpt":0.2648736364580173,"score_spread":0.25053130709416005,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2914599041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926085,0.00012356156,0.0014899018,0.00013156759,0.000009188188,0.000007632706,0.0006772403,0.000045805107,0.0049064793],"genre_scores_gemma":[0.9993086,0.000019055808,0.00016185916,0.000015064497,0.0000046739656,0.0000018252003,0.0003059158,0.000007380263,0.00017560636],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999742,0.000053205877,0.000015967196,0.00010862904,0.000039518178,0.000040632527],"domain_scores_gemma":[0.99831605,0.00079134287,0.0003268214,0.00023150833,0.00023128102,0.00010313072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005394742,0.00013196722,0.00015048732,0.00085345097,0.00020911625,0.0008356686,0.00018532484,0.00023613492,0.002016569],"category_scores_gemma":[0.0037106024,0.000117170566,0.00011569076,0.0007099119,0.00038529042,0.00050776795,0.0005175763,0.00025980742,0.00033264773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011844233,0.000012909716,0.9780105,0.000015743499,0.00008543188,0.0000887087,0.00024006942,0.0013980875,0.0047382335,0.0008683465,0.0008494253,0.01357405],"study_design_scores_gemma":[0.0000040866657,0.000010242396,0.99570113,0.000004735243,0.000011370561,0.000032723845,0.00014678502,0.0029744883,0.00037581875,0.00017551305,0.00055919343,0.00000393813],"about_ca_topic_score_codex":0.008411951,"about_ca_topic_score_gemma":0.008536102,"teacher_disagreement_score":0.008411951,"about_ca_system_score_codex":0.00021247184,"about_ca_system_score_gemma":0.00015568027,"threshold_uncertainty_score":0.016725957},"labels":[],"label_agreement":null},{"id":"W2921654445","doi":"10.1029/2018gl080773","title":"Time of Detection as a Metric for Prioritizing Between Climate Observation Quality, Frequency, and Duration","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Tula Foundation","funders":"National Science Foundation of Sri Lanka; Hakai Institute; National Oceanic and Atmospheric Administration; National Academies of Sciences, Engineering, and Medicine","keywords":"Metric (unit); Computer science; Duration (music); Environmental science; Range (aeronautics); Quality (philosophy); Variable (mathematics); Performance metric; Key (lock); Climate change; Mathematics; Geology; Engineering","score_opus":0.053068425068968014,"score_gpt":0.3138366995022375,"score_spread":0.2607682744332695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921654445","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.48550877,0.0016513215,0.49794224,0.00469221,0.0003137964,0.0002888514,0.0012074785,0.00049947813,0.007895837],"genre_scores_gemma":[0.9481571,0.00014067224,0.050649527,0.00017359824,0.000101835365,0.000109260065,0.00028254252,0.00004308462,0.0003424351],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9854842,0.008644413,0.0012016878,0.0017731389,0.0022498923,0.0006466917],"domain_scores_gemma":[0.7347987,0.22763228,0.0171488,0.0070043798,0.0100107305,0.0034050962],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.028038932,0.00063135446,0.0011036242,0.0034242528,0.0007184795,0.0031470545,0.0015279846,0.0020961103,0.002405203],"category_scores_gemma":[0.15934409,0.000418553,0.00061004964,0.0025489598,0.001503943,0.0046078702,0.0024127075,0.0015116236,0.00026584702],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0044618705,0.00056940655,0.46047908,0.00093035237,0.0008098995,0.00044195508,0.0016249047,0.15791602,0.017718138,0.054001838,0.0057156025,0.29533103],"study_design_scores_gemma":[0.00031890607,0.0027962045,0.23384368,0.00029338952,0.0005600409,0.001012161,0.0024423457,0.65249807,0.020070082,0.07639609,0.009430802,0.00033816072],"about_ca_topic_score_codex":0.0038361682,"about_ca_topic_score_gemma":0.0022380287,"teacher_disagreement_score":0.028038932,"about_ca_system_score_codex":0.0014528906,"about_ca_system_score_gemma":0.0018065358,"threshold_uncertainty_score":0.1482858},"labels":[],"label_agreement":null},{"id":"W2921871218","doi":"10.1029/2018gl080961","title":"Deciphering Patterns and Drivers of Heat and Carbon Storage in the Southern Ocean","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Australian Research Council; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Thermocline; Environmental science; Hydrography; Climatology; Greenhouse gas; Ocean heat content; Climate change; Carbon cycle; Atmospheric sciences; Ocean current; Oceanography; Geology; Ecosystem; Ecology","score_opus":0.014003528900885836,"score_gpt":0.23510420673147073,"score_spread":0.2211006778305849,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2921871218","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989981,0.000113045615,0.00023636798,0.00006553001,0.0000019151632,0.0000014172837,0.00015460023,0.000017778646,0.0004112014],"genre_scores_gemma":[0.9996965,0.00004080519,0.000095955,0.0000044549465,0.0000027402295,0.00000119144,0.00009708859,0.0000036737526,0.00005754103],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999558,0.0000081346325,0.000003921965,0.000016218852,0.0000059152226,0.000009962941],"domain_scores_gemma":[0.99980444,0.00005704454,0.00005867319,0.000021109963,0.00002857682,0.000030137577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002461359,0.00021707409,0.00022878246,0.00069321523,0.0001926084,0.00066501653,0.00020142393,0.00030709154,0.0010335969],"category_scores_gemma":[0.00055780297,0.00018295548,0.00027953376,0.000838189,0.0003406876,0.0006606795,0.00059811416,0.0001785903,0.00012510562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002665531,0.000049658986,0.9159123,0.00007795397,0.000162477,0.00019203276,0.00046855022,0.016843824,0.052283034,0.0012831955,0.0003080142,0.012152481],"study_design_scores_gemma":[0.000011510764,0.000021286367,0.97105473,0.000010722389,0.000024435798,0.000029849987,0.00035414693,0.026243022,0.0009792275,0.00078015967,0.00047905653,0.000011883269],"about_ca_topic_score_codex":0.016272567,"about_ca_topic_score_gemma":0.013107683,"teacher_disagreement_score":0.016272567,"about_ca_system_score_codex":0.0003376184,"about_ca_system_score_gemma":0.000322261,"threshold_uncertainty_score":0.032355726},"labels":[],"label_agreement":null},{"id":"W2922866193","doi":"10.1029/2018gl081166","title":"Detecting Signals of Large‐Scale Climate Phenomena in Discharge and Nutrient Loads in the Mississippi‐Atchafalaya River Basin","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Biological and Environmental Research; U.S. Geological Survey; Office of Science; U.S. Department of Agriculture; National Aeronautics and Space Administration; U.S. Department of Energy; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Biogeochemical cycle; Environmental science; Discharge; Drainage basin; Hydrology (agriculture); Structural basin; Nutrient; Surface runoff; Spatial ecology; Geology; Ecology; Geography; Geomorphology","score_opus":0.013935366569332778,"score_gpt":0.27199007938406383,"score_spread":0.2580547128147311,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2922866193","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995516,0.000012103625,0.00010274128,0.00002527064,7.8947664e-7,0.0000013463857,0.00013440035,0.0000058113324,0.00016588776],"genre_scores_gemma":[0.99973255,0.0000081928365,0.000092773684,0.000004121511,9.816858e-7,0.000003122893,0.00010689985,8.140014e-7,0.000050593862],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988806,0.000026718595,0.000007966431,0.00004451632,0.0000129109185,0.000019884263],"domain_scores_gemma":[0.9994634,0.00013952925,0.00017800169,0.00004353587,0.000106339045,0.00006914527],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021871264,0.00013012336,0.0001489481,0.0005905784,0.00042050844,0.0004884171,0.0002382535,0.000263822,0.000533746],"category_scores_gemma":[0.000926847,0.00013413053,0.0001505407,0.00075082574,0.00023276692,0.00027755369,0.0004883322,0.00018721404,0.000051627445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056688168,0.000034967292,0.98523337,0.000010750576,0.000077715915,0.00008271751,0.00050006533,0.001919402,0.005328053,0.0000855517,0.00015386079,0.0065168245],"study_design_scores_gemma":[0.0000026579794,0.000010351465,0.9951934,0.0000026016373,0.000008164947,0.000022313177,0.0002328628,0.0040915315,0.00020616497,0.00002844934,0.00019612475,0.000005270158],"about_ca_topic_score_codex":0.16621248,"about_ca_topic_score_gemma":0.2446642,"teacher_disagreement_score":0.16621248,"about_ca_system_score_codex":0.0008478909,"about_ca_system_score_gemma":0.0006687632,"threshold_uncertainty_score":0.33049005},"labels":[],"label_agreement":null},{"id":"W2923292181","doi":"10.1029/2018gl081439","title":"Interior Pathways of Labrador Sea Water in the North Atlantic From the Argo Perspective","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Argo; Ocean gyre; Geology; Boundary current; Oceanography; North Atlantic Deep Water; Ridge; Anticyclone; Thermohaline circulation; Atlantic hurricane; Shutdown of thermohaline circulation; Structural basin; Climatology; Mid-Atlantic Ridge; Ocean current; Subtropics; Geomorphology; Paleontology; Tropical cyclone","score_opus":0.019754581318417824,"score_gpt":0.24153565777050617,"score_spread":0.22178107645208836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923292181","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960871,0.00009262159,0.000155531,0.00007068239,0.0000036342997,0.0000030036676,0.00057212624,0.000015534577,0.0029998347],"genre_scores_gemma":[0.99852043,0.0000882694,0.00029140423,0.000019136385,0.0000035256985,0.000002010312,0.0005439259,0.0000074484446,0.0005237872],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.000007329905,0.0000038009791,0.00001619004,0.000010042966,0.00002223377],"domain_scores_gemma":[0.999775,0.00001591306,0.00008473641,0.000012802829,0.00005730256,0.00005418467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010375404,0.0001427458,0.000205107,0.0006133813,0.00035564147,0.0010589386,0.00015181559,0.00013630836,0.0012508478],"category_scores_gemma":[0.00033046197,0.0001076412,0.0001772866,0.0004793082,0.0002753967,0.0004801766,0.0005626817,0.00029280057,0.00016113628],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011068192,0.000029950952,0.9777535,0.000021264286,0.000042457632,0.00014780667,0.00043963623,0.0015233118,0.005679282,0.00050985685,0.00048806937,0.013254202],"study_design_scores_gemma":[0.000007430535,0.000030402587,0.99313724,0.000020029182,0.00002549726,0.000043459993,0.000443874,0.0027826042,0.00079984317,0.00018644652,0.0025117074,0.000011518168],"about_ca_topic_score_codex":0.067018636,"about_ca_topic_score_gemma":0.14367819,"teacher_disagreement_score":0.9329814,"about_ca_system_score_codex":0.00089577347,"about_ca_system_score_gemma":0.0005577905,"threshold_uncertainty_score":0.13325709},"labels":[],"label_agreement":null},{"id":"W2923509888","doi":"10.1029/2018gl081837","title":"Discrepancy in the Identification of the Atlantic/Pacific Front in the Central Arctic Ocean: NO Versus Nutrient Relationships","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Oceanography; Halocline; Geology; Ridge; Arctic; Front (military); Structural basin; Thermohaline circulation; Circumpolar deep water; Water mass; The arctic; Climatology; North Atlantic Deep Water; Salinity; Paleontology","score_opus":0.027691580221729874,"score_gpt":0.25899890396564385,"score_spread":0.23130732374391397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2923509888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99784195,0.00022660504,0.00022489093,0.000030572137,0.0000125794895,0.000002338754,0.0002170644,0.0000058624937,0.0014381355],"genre_scores_gemma":[0.99936503,0.00007004624,0.00016894168,0.000012594943,0.000005406633,0.0000013611387,0.00019423474,0.0000022907059,0.0001801925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999294,0.0000093815715,0.000009486964,0.000022257647,0.000015085246,0.000014272266],"domain_scores_gemma":[0.9996151,0.00009702848,0.00006744872,0.000028982731,0.00015151624,0.000039948707],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000441993,0.00013634321,0.00018492239,0.0008196102,0.00035091216,0.00069239386,0.00013839798,0.00021445585,0.00074398395],"category_scores_gemma":[0.00070939923,0.000096418175,0.00020127303,0.0005394848,0.0002129647,0.0003430023,0.0003734587,0.00018429346,0.00013214047],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041691953,0.000023507131,0.9437775,0.000062455765,0.00008894864,0.0001060565,0.0004991825,0.0006010346,0.038294926,0.00022674266,0.0001969377,0.01570585],"study_design_scores_gemma":[0.0000011921799,0.0000063547495,0.99811506,0.0000075726866,0.00000900695,0.000025585008,0.00020295045,0.00053633575,0.00079823454,0.000051800434,0.00024356911,0.0000023805098],"about_ca_topic_score_codex":0.028688822,"about_ca_topic_score_gemma":0.052369673,"teacher_disagreement_score":0.028688822,"about_ca_system_score_codex":0.00042415722,"about_ca_system_score_gemma":0.00033428048,"threshold_uncertainty_score":0.05704367},"labels":[],"label_agreement":null},{"id":"W2924568070","doi":"10.1029/2019gl082344","title":"Revisiting the Circulation of Hudson Bay: Evidence for a Seasonal Pattern","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; Manitoba Hydro; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Environment and Climate Change Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Western Canada Research Grid; Manitoba Hydro; Compute Canada","keywords":"Bay; Geostrophic wind; Anticyclone; Climatology; Oceanography; Circulation (fluid dynamics); Forcing (mathematics); Geology; Current (fluid); Ocean current; Boundary current; Surface runoff; Environmental science","score_opus":0.05916189297497962,"score_gpt":0.32034300610197636,"score_spread":0.26118111312699677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2924568070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99835265,0.00013703216,0.00008454383,0.0001375139,0.00001513775,0.000002858739,0.00044013976,0.00001679788,0.00081328076],"genre_scores_gemma":[0.99937916,0.00006222191,0.00009290855,0.000023647404,0.000006215231,0.0000014359114,0.00025148067,0.000002593727,0.00018021274],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.00000872765,0.0000042193456,0.00001949179,0.000013114705,0.000020169206],"domain_scores_gemma":[0.99965453,0.000044013763,0.00007272002,0.00003040475,0.000117122036,0.00008124861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021984626,0.00012551092,0.00016686649,0.00070814224,0.00038435272,0.00077606254,0.0003102459,0.0001639153,0.00157188],"category_scores_gemma":[0.0005749626,0.00013442386,0.00016857317,0.0010012973,0.00041260239,0.0002256146,0.00042427727,0.00020872522,0.000102307655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007116839,0.00002608805,0.9853851,0.000032184467,0.000041908777,0.00016975777,0.00060795,0.000706356,0.0039544785,0.00026637994,0.00124743,0.007491275],"study_design_scores_gemma":[0.000004143082,0.0000080716945,0.99726486,0.000008235763,0.000009422891,0.000015051678,0.00036012786,0.0013190176,0.00013487946,0.000030547522,0.0008426957,0.0000029918808],"about_ca_topic_score_codex":0.4295671,"about_ca_topic_score_gemma":0.50746566,"teacher_disagreement_score":0.4295671,"about_ca_system_score_codex":0.0014697647,"about_ca_system_score_gemma":0.0015280865,"threshold_uncertainty_score":0.8541335},"labels":[],"label_agreement":null},{"id":"W2925748543","doi":"10.1029/2019gl081991","title":"Induced Seismicity Reduces Seismic Hazard?","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Induced seismicity; Geology; Seismic hazard; Seismology; Crust; Hazard; Earthquake prediction; Geophysics","score_opus":0.04515377888619912,"score_gpt":0.29191313938782837,"score_spread":0.24675936050162925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2925748543","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9534287,0.0007917248,0.0047700396,0.008515688,0.00013306353,0.000021920385,0.0004817679,0.00011375765,0.03174327],"genre_scores_gemma":[0.9988127,0.00013591844,0.0001509084,0.00024206477,0.000041220035,0.0000027788428,0.000054316562,0.0000067807728,0.0005532928],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99974495,0.000065295986,0.000016056852,0.00007435128,0.000040236857,0.000059018646],"domain_scores_gemma":[0.9954869,0.0015737314,0.001854575,0.00031160522,0.000259895,0.0005132443],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007942284,0.00018151413,0.00024609882,0.00028680213,0.00019279083,0.0007514324,0.00049106963,0.00073218305,0.013949996],"category_scores_gemma":[0.009340836,0.00015344031,0.00016859456,0.00031256964,0.0009881053,0.0010163921,0.00071290886,0.0007672098,0.0007204936],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027244862,0.0019327255,0.5321278,0.0018944489,0.0006613477,0.0021770024,0.0018187298,0.04836102,0.056290068,0.15440096,0.024860535,0.17275093],"study_design_scores_gemma":[0.0001619743,0.0012730605,0.75194365,0.00014437128,0.00023794833,0.0011426009,0.0026185291,0.019458594,0.007079799,0.19461296,0.021253677,0.00007287996],"about_ca_topic_score_codex":0.001462644,"about_ca_topic_score_gemma":0.0016206778,"teacher_disagreement_score":0.013949996,"about_ca_system_score_codex":0.0006729821,"about_ca_system_score_gemma":0.00034744415,"threshold_uncertainty_score":0.046667337},"labels":[],"label_agreement":null},{"id":"W2925895976","doi":"10.1029/2018gl081539","title":"Storm Time Mesoscale Plasma Flows in the Nightside High‐Latitude Ionosphere: A Statistical Survey of Characteristics","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Air Force Office of Scientific Research; National Science Foundation of Sri Lanka; Department of Science and Technology, Ministry of Science and Technology, India; National Aeronautics and Space Administration; Canadian Space Agency; Academia Româna; National Science Foundation","keywords":"Mesoscale meteorology; Storm; Ionosphere; Geomagnetic storm; Geology; Atmospheric sciences; Polar; Coronal mass ejection; Climatology; Geophysics; Physics; Solar wind; Plasma","score_opus":0.013882910833922714,"score_gpt":0.2717563166121319,"score_spread":0.25787340577820916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2925895976","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987451,0.000073949464,0.000253532,0.000015266782,0.0000018903314,0.000002863061,0.0006113779,0.000010304087,0.00028567962],"genre_scores_gemma":[0.99915123,0.000035769455,0.0000706974,0.0000034985221,0.00000497896,0.000003326256,0.00065015163,0.0000024722337,0.0000779154],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998197,0.000031374337,0.000020752483,0.000055719865,0.000041149284,0.000031321062],"domain_scores_gemma":[0.99825186,0.00054801104,0.0006500535,0.00015974166,0.0001945958,0.00019568617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040072625,0.00007513033,0.0001579966,0.0009515179,0.0001541144,0.00038681566,0.00012004955,0.00012662372,0.0010907638],"category_scores_gemma":[0.0012897741,0.00006152239,0.0002181892,0.0010200042,0.00018559345,0.0002690843,0.00028194723,0.00012792191,0.00021771084],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049883285,0.00000648686,0.99674964,0.000004961151,0.000030915806,0.000021275499,0.000047969545,0.00015412582,0.00071056397,0.000027419814,0.000103302234,0.0020934718],"study_design_scores_gemma":[7.7436545e-7,0.000013011087,0.99934644,9.084454e-7,0.0000036778565,0.000035200832,0.00006735437,0.00034865993,0.000063418745,0.000016729731,0.00010252622,0.0000012421216],"about_ca_topic_score_codex":0.0016879532,"about_ca_topic_score_gemma":0.0012879162,"teacher_disagreement_score":0.0016879532,"about_ca_system_score_codex":0.00009952558,"about_ca_system_score_gemma":0.00012554361,"threshold_uncertainty_score":0.0036489964},"labels":[],"label_agreement":null},{"id":"W2933645048","doi":"10.1029/2018gl081426","title":"Decadal Variations in the Winter Beaufort High and the Stratospheric Polar Vortex","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Office of Energy Research and Development","keywords":"Polar vortex; Climatology; Anticyclone; Polar; Arctic; Northern Hemisphere; Atmospheric sciences; Baroclinity; Ozone depletion; Geology; Vortex; Arctic oscillation; Polar night; Environmental science; Oceanography; Stratosphere; Geography; Meteorology; Physics","score_opus":0.018777660105964804,"score_gpt":0.27976662215194964,"score_spread":0.2609889620459848,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2933645048","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998539,0.00013600761,0.000094274874,0.00005516243,0.000011546872,8.367645e-7,0.0003254821,0.000007631048,0.0008301864],"genre_scores_gemma":[0.99948347,0.000025089017,0.000027803022,0.000007695524,0.000007839234,8.5685326e-7,0.00028736965,0.0000013081747,0.00015853783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994123,0.000011583218,0.0000031511909,0.000016737613,0.000010817153,0.000016517834],"domain_scores_gemma":[0.9996251,0.000068687485,0.0001466664,0.00002967639,0.00006150211,0.0000683032],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022348134,0.000086066124,0.00010356821,0.0003851042,0.00018414961,0.00049444276,0.000094981355,0.000209525,0.0008501954],"category_scores_gemma":[0.0005159518,0.00004459173,0.000116268944,0.0003445346,0.00014104063,0.00016035564,0.00021808835,0.0002166186,0.00012102597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021561244,0.000036097084,0.9830058,0.000013488095,0.00013831106,0.00015791689,0.00032376553,0.0020219258,0.003367652,0.00047513857,0.0013418301,0.0089023225],"study_design_scores_gemma":[0.0000012794496,0.000010306009,0.99872667,0.000002239845,0.0000048586453,0.000017503131,0.00005190395,0.00044799232,0.000071089766,0.000041368337,0.0006226081,0.0000022144216],"about_ca_topic_score_codex":0.008064978,"about_ca_topic_score_gemma":0.011356504,"teacher_disagreement_score":0.008064978,"about_ca_system_score_codex":0.00017126017,"about_ca_system_score_gemma":0.00007541479,"threshold_uncertainty_score":0.016036093},"labels":[],"label_agreement":null},{"id":"W2937153686","doi":"10.1029/2019gl082110","title":"Volume, Heat, and Freshwater Divergences in the Subpolar North Atlantic Suggest the Nordic Seas as Key to the State of the Meridional Overturning Circulation","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":136,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Swedish National Space Agency; Havforskningsinstituttet","keywords":"Ocean gyre; Oceanography; Geology; Climatology; Buoyancy; Shutdown of thermohaline circulation; North Atlantic Deep Water; Thermohaline circulation; Subtropics","score_opus":0.012045810468703828,"score_gpt":0.23113647123837097,"score_spread":0.21909066076966716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937153686","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979595,0.00007671742,0.00007033289,0.000047295252,0.00000461803,9.84702e-7,0.00011494408,0.0000034386753,0.0017221587],"genre_scores_gemma":[0.99958056,0.00003135998,0.000058759608,0.000011809951,0.0000036259983,7.511964e-7,0.00010705671,0.0000012358116,0.00020480678],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999763,0.0000033687807,0.0000018871842,0.0000066001253,0.00000563364,0.0000062351514],"domain_scores_gemma":[0.99983895,0.000021493606,0.000054497636,0.00000706546,0.000042372958,0.00003550591],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008848432,0.0000779451,0.000090189176,0.00035931627,0.00025751,0.0004734536,0.00007721639,0.0001259017,0.0012611672],"category_scores_gemma":[0.0002614342,0.00006167018,0.00007264143,0.00029785876,0.00031942036,0.00025704934,0.00020180091,0.00015231685,0.000114503026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021000754,0.000013973897,0.96986437,0.000014341217,0.000029347348,0.00008213534,0.0002858762,0.0005695361,0.018484445,0.0004971343,0.00022600223,0.009722799],"study_design_scores_gemma":[0.0000016717248,0.0000047422736,0.9992729,0.0000018939728,0.0000024013382,0.00000772269,0.000099935554,0.00018733469,0.00015171983,0.000050239683,0.00021822563,0.0000011508745],"about_ca_topic_score_codex":0.026161019,"about_ca_topic_score_gemma":0.06244086,"teacher_disagreement_score":0.026161019,"about_ca_system_score_codex":0.00036321869,"about_ca_system_score_gemma":0.0002182845,"threshold_uncertainty_score":0.05201751},"labels":[],"label_agreement":null},{"id":"W2937340070","doi":"10.1029/2019gl082406","title":"Seismic Evidence for Lithospheric Thinning and Heat in the northern Canadian Cordillera","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Alberta; University of Ottawa","funders":"National Science Foundation of Sri Lanka; Natural Sciences and Engineering Research Council of Canada; Northwestern University","keywords":"Lithosphere; Geology; Mantle (geology); Asthenosphere; Lithospheric flexure; Crust; Geophysics; Tectonics; Seismology","score_opus":0.04576985167864338,"score_gpt":0.2956939261187276,"score_spread":0.2499240744400842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937340070","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99423766,0.00032514654,0.0000682443,0.00017422157,0.0000058473265,0.0000056334957,0.00051240955,0.000028583452,0.004642279],"genre_scores_gemma":[0.9991781,0.00009759463,0.00009626225,0.000014321089,0.0000020451962,0.0000017125695,0.0001990023,0.0000023839973,0.00040860902],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999912,0.000003569005,0.000002235295,0.000020291864,0.00003001378,0.000031749852],"domain_scores_gemma":[0.9997327,0.000015138217,0.000055817873,0.0000133822305,0.00013250469,0.000050516825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012350253,0.0002521586,0.00016176407,0.0013228233,0.0013131903,0.0006903974,0.0003983813,0.0002789712,0.003168311],"category_scores_gemma":[0.0005193452,0.00015169925,0.00013855762,0.0014693191,0.0005885033,0.0001331771,0.00039577982,0.00019194433,0.00015462057],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020290735,0.000026374877,0.95484287,0.000060838716,0.00006882368,0.00039735288,0.0012575767,0.0015350293,0.017381733,0.00067621726,0.0018342265,0.021716157],"study_design_scores_gemma":[0.000003280551,0.0000032783869,0.99825114,0.0000061653227,0.000005920194,0.000024437586,0.00024374152,0.00049408,0.00016915715,0.00003296695,0.0007623769,0.0000034849688],"about_ca_topic_score_codex":0.96827,"about_ca_topic_score_gemma":0.98394656,"teacher_disagreement_score":0.031729996,"about_ca_system_score_codex":0.007276628,"about_ca_system_score_gemma":0.0035543141,"threshold_uncertainty_score":0.063833654},"labels":[],"label_agreement":null},{"id":"W2937388604","doi":"10.1029/2019gl082611","title":"Pathways for Ecological Change in Canadian High Arctic Wetlands Under Rapid Twentieth Century Warming","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; Carleton University","funders":"Natural Resources Canada; Polar Knowledge Canada; Natural Environment Research Council; University of Ottawa","keywords":"Arctic; Wetland; Climate change; Environmental science; Global warming; Environmental change; Ecology; Arctic ecology; The arctic; Permafrost; Oceanography; Physical geography; Climatology; Geography; Earth science; Geology; Biology","score_opus":0.09063413548376056,"score_gpt":0.29827704642251357,"score_spread":0.207642910938753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2937388604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947194,0.0007397806,0.00022211351,0.0009450422,0.000011968084,0.0000068193,0.0007922656,0.000011736309,0.0025509375],"genre_scores_gemma":[0.9987772,0.00035702402,0.00022407896,0.000056965775,0.0000033485785,0.0000030112801,0.00012870276,0.0000022530915,0.0004474375],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989796,0.000009788085,0.0000027954575,0.000017014307,0.000018202476,0.000054284646],"domain_scores_gemma":[0.99968493,0.000021962527,0.00006297697,0.000008775561,0.0001474391,0.00007401891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002943686,0.00012657701,0.00013065027,0.0009484487,0.0009945296,0.00095189514,0.00020682636,0.0003010704,0.0014337213],"category_scores_gemma":[0.0004785287,0.00010453292,0.00022301475,0.00077765493,0.000652651,0.00029185603,0.00047477486,0.00025928378,0.000049947335],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024037072,0.000041925017,0.9437324,0.00010842678,0.00015447942,0.000386605,0.00196399,0.0033836921,0.01645348,0.004754391,0.0018715762,0.02690863],"study_design_scores_gemma":[0.0000017854559,0.0000062810177,0.99660814,0.000008281067,0.000009308309,0.0000241845,0.0006407356,0.0004820235,0.00020715661,0.00023529818,0.0017695548,0.0000072322628],"about_ca_topic_score_codex":0.8490611,"about_ca_topic_score_gemma":0.93002254,"teacher_disagreement_score":0.15093893,"about_ca_system_score_codex":0.005813143,"about_ca_system_score_gemma":0.004611688,"threshold_uncertainty_score":0.30365562},"labels":[],"label_agreement":null},{"id":"W2939006645","doi":"10.1029/2019gl082028","title":"An Odd Oxygen Framework for Wintertime Ammonium Nitrate Aerosol Pollution in Urban Areas: NO<sub>x</sub> and VOC Control as Mitigation Strategies","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":142,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Toronto; Dalhousie University","funders":"Utah Department of Environmental Quality; Utah State University; National Oceanic and Atmospheric Administration; U.S. Environmental Protection Agency","keywords":"Nitrate; Environmental science; Aerosol; Pollution; Ozone; Ammonium; Environmental chemistry; Pollutant; NOx; Air pollution; Ammonium nitrate; Air quality index; Nitrogen oxide; Atmospheric sciences; Environmental engineering; Chemistry; Meteorology; Geography; Ecology; Combustion; Geology","score_opus":0.01166949946656677,"score_gpt":0.2609939025752733,"score_spread":0.24932440310870652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939006645","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.58858925,0.001561549,0.3665913,0.0040679537,0.00017379434,0.00016550346,0.0006591361,0.00018197604,0.03800952],"genre_scores_gemma":[0.9876022,0.00020278583,0.009989596,0.00009355022,0.000035370336,0.00003707349,0.000065383356,0.000014804347,0.0019592806],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99964774,0.00019723717,0.00000816025,0.00004573203,0.000036588728,0.00006461305],"domain_scores_gemma":[0.99969125,0.000115911345,0.000056251876,0.000017542703,0.000067333545,0.000051727155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009426034,0.00061693776,0.00045735147,0.00046895348,0.0003805045,0.0010980504,0.00079661416,0.00057973736,0.0013248553],"category_scores_gemma":[0.00071568554,0.00016058593,0.0005524023,0.00022834986,0.0007816777,0.0007333091,0.0009935356,0.00051441917,0.00007321364],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000079435486,0.00014391702,0.005507475,0.000060157854,0.00007536596,0.00014934818,0.00009245257,0.87471265,0.004260937,0.10753517,0.0008881241,0.0064949454],"study_design_scores_gemma":[0.000011979071,0.00007231894,0.0015063974,0.0000065332315,0.000019402532,0.000006746754,0.00014432985,0.9776219,0.00029474078,0.019485394,0.00082235225,0.000007903891],"about_ca_topic_score_codex":0.03404068,"about_ca_topic_score_gemma":0.032518394,"teacher_disagreement_score":0.03404068,"about_ca_system_score_codex":0.0015390071,"about_ca_system_score_gemma":0.0014249111,"threshold_uncertainty_score":0.06768513},"labels":[],"label_agreement":null},{"id":"W2939712114","doi":"10.1029/2019gl082202","title":"The 2016 M7 Kumamoto, Japan, Earthquake Slip Field Derived From a Joint Inversion of Differential Lidar Topography, Optical Correlation, and InSAR Surface Displacements","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Centre National d’Etudes Spatiales; Canada Excellence Research Chairs, Government of Canada; European Space Agency; Institut de Radioprotection et de SÛreté Nucléaire; Arizona State University; National Science Foundation","keywords":"Geology; Interferometric synthetic aperture radar; Seismology; Slip (aerodynamics); Geodesy; Lidar; Synthetic aperture radar; Crust; Remote sensing; Geophysics","score_opus":0.01997087330812671,"score_gpt":0.247361497002225,"score_spread":0.2273906236940983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939712114","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987141,0.000024014138,0.0006387439,0.000034917615,0.0000045914335,0.000004049932,0.00019355828,0.000023180997,0.0003627405],"genre_scores_gemma":[0.9981078,0.000023351098,0.001190637,0.000008411223,0.0000042427237,0.0000039054316,0.0005017125,0.0000067505875,0.00015310572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999279,0.000010924506,0.000005072978,0.000021723861,0.000017282893,0.000017103059],"domain_scores_gemma":[0.9998461,0.000019068257,0.00004203112,0.000020244466,0.0000424444,0.00003002471],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022338802,0.00035173693,0.00034742447,0.0005284167,0.000244853,0.00035910463,0.00033714288,0.00039989644,0.0005181182],"category_scores_gemma":[0.00058981136,0.000321291,0.00030158923,0.0007027665,0.0002533056,0.00028683356,0.00045242193,0.00026125458,0.00020366376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004497074,0.0003465049,0.7070282,0.00016368186,0.00037231357,0.0014928433,0.00057950953,0.12445875,0.09455584,0.0011037485,0.00283967,0.066609204],"study_design_scores_gemma":[0.000067490815,0.000108501496,0.64134324,0.000033738892,0.000099314406,0.00017672605,0.00042427034,0.3509576,0.005525524,0.0002757346,0.0009404496,0.000047487712],"about_ca_topic_score_codex":0.019048912,"about_ca_topic_score_gemma":0.039543316,"teacher_disagreement_score":0.019048912,"about_ca_system_score_codex":0.00039552257,"about_ca_system_score_gemma":0.0008549323,"threshold_uncertainty_score":0.03787607},"labels":[],"label_agreement":null},{"id":"W2939919549","doi":"10.1029/2019gl082313","title":"Evidence for Whole Mantle Convection Driving Cordilleran Tectonics","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; St. Francis Xavier University","funders":"Australian Research Council","keywords":"Geology; Subduction; Mantle convection; Mantle (geology); Plate tectonics; Geophysics; Earth science; Mantle wedge; Tectonics; Paleontology","score_opus":0.065121385230466,"score_gpt":0.30527306447461816,"score_spread":0.24015167924415215,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2939919549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944148,0.00040015564,0.00015012707,0.00018588673,0.000009903124,0.0000037041073,0.00023053502,0.000026080957,0.0045787613],"genre_scores_gemma":[0.9989882,0.00012641972,0.0001304112,0.000032370775,0.000011956611,0.000002273401,0.00017149356,0.0000026986543,0.00053422205],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990463,0.0000095042415,0.00000482405,0.000034339344,0.000018417024,0.000028232611],"domain_scores_gemma":[0.9993327,0.0001371167,0.00019665166,0.00007474013,0.00016420083,0.000094517585],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020114507,0.00023316119,0.00015319764,0.0009210119,0.00039111415,0.000526469,0.00032697336,0.00026115097,0.0065955683],"category_scores_gemma":[0.00087154174,0.00011386596,0.00010420558,0.00065035303,0.00037762045,0.00025806547,0.00044753554,0.00015156825,0.00040247024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075080025,0.000044833505,0.8500526,0.00017871514,0.00007518775,0.0006125288,0.00087396294,0.00045342423,0.10647897,0.0025739605,0.0006420413,0.037262924],"study_design_scores_gemma":[0.000019355859,0.000042478834,0.9920466,0.00002218339,0.000023999466,0.00015439557,0.00022093674,0.00078148564,0.004305447,0.00054805574,0.0018285294,0.000006476838],"about_ca_topic_score_codex":0.037696987,"about_ca_topic_score_gemma":0.046686605,"teacher_disagreement_score":0.037696987,"about_ca_system_score_codex":0.0008782759,"about_ca_system_score_gemma":0.00036483014,"threshold_uncertainty_score":0.074955106},"labels":[],"label_agreement":null},{"id":"W2940206173","doi":"10.1029/2019gl082460","title":"Magnetospheric Signatures of STEVE: Implications for the Magnetospheric Energy Source and Interhemispheric Conjugacy","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Air Force Research Laboratory; Air Force Office of Scientific Research; National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Electron precipitation; Magnetosphere; Plasmasphere; Geophysics; Physics; Ionosphere; Field line; Electron; Plasma sheet; Plasma; Atmospheric sciences; Van Allen Probes; Van Allen radiation belt","score_opus":0.01117015016413256,"score_gpt":0.27147436180312945,"score_spread":0.26030421163899686,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2940206173","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99811697,0.00003181759,0.00017382202,0.000021600286,0.0000018021408,0.0000023817588,0.00007234158,0.000013059733,0.0015662044],"genre_scores_gemma":[0.9997857,0.0000068096756,0.00005568769,0.000004173475,0.0000017736592,8.7599926e-7,0.000057930785,0.000002162863,0.0000848418],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995244,0.0000051275265,0.0000025602728,0.000012238048,0.000009431936,0.00001825578],"domain_scores_gemma":[0.99978715,0.000034298133,0.00007498491,0.000030158733,0.00003453527,0.00003883931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000118497905,0.000117940894,0.00018744644,0.00062943756,0.0003605304,0.0003992879,0.00017627642,0.00022091136,0.0011929834],"category_scores_gemma":[0.00040229651,0.0000867957,0.00013556551,0.00031261283,0.0002967417,0.00028066765,0.00048567916,0.00019353585,0.00011342912],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042583625,0.000061327635,0.8933994,0.000020772817,0.000058745365,0.00076136034,0.0005284276,0.0010805158,0.08893987,0.0007224057,0.00024560528,0.013755689],"study_design_scores_gemma":[0.0000032698695,0.000022507125,0.99687374,0.0000026266398,0.0000035504152,0.00016864543,0.00011583173,0.00059655297,0.0017811345,0.00010348036,0.00032584576,0.0000028058466],"about_ca_topic_score_codex":0.0024388395,"about_ca_topic_score_gemma":0.00429484,"teacher_disagreement_score":0.0024388395,"about_ca_system_score_codex":0.00023348621,"about_ca_system_score_gemma":0.000076940836,"threshold_uncertainty_score":0.0048493147},"labels":[],"label_agreement":null},{"id":"W2940503454","doi":"10.1029/2019gl082749","title":"Fresh Submarine Groundwater Discharge to the Near‐Global Coast","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":139,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; University of Saskatchewan","funders":"","keywords":"Submarine groundwater discharge; Groundwater; Geology; Biogeochemical cycle; Aquifer; Oceanography; Submarine pipeline; Estuary; Hydrology (agriculture); Discharge; Groundwater discharge; Groundwater flow; Ecology; Geography","score_opus":0.01953599744954478,"score_gpt":0.2623149042464573,"score_spread":0.24277890679691252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2940503454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957468,0.00010601801,0.00045739432,0.000031203796,0.0000030839362,0.0000036992978,0.0020601193,0.000045307956,0.0015462866],"genre_scores_gemma":[0.9979096,0.00009819034,0.00032696826,0.000013301411,0.0000036402616,0.0000036927738,0.0012655625,0.0000063057846,0.00037268674],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996483,0.0000038055696,0.0000029502867,0.000016174848,0.0000075165904,0.0000047420917],"domain_scores_gemma":[0.99989104,0.000012560394,0.000036974587,0.0000117792515,0.000029481693,0.000018212178],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007936416,0.00019439954,0.00013936445,0.000678143,0.00011210147,0.0003029087,0.00013936285,0.00018704418,0.0009842231],"category_scores_gemma":[0.00024510667,0.00009490249,0.00019223026,0.00066417194,0.000117721014,0.00030847156,0.0002694373,0.00011755981,0.00021392998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058208527,0.000015257252,0.9623939,0.00005439687,0.00013016566,0.00012679656,0.0001488272,0.007714713,0.012471707,0.0002349704,0.0005943178,0.016056862],"study_design_scores_gemma":[0.0000066298994,0.000029180934,0.9924297,0.000009444101,0.000019548394,0.000047674494,0.00009601506,0.004378677,0.0013636762,0.00016436467,0.0014469918,0.000008103801],"about_ca_topic_score_codex":0.02903045,"about_ca_topic_score_gemma":0.03300362,"teacher_disagreement_score":0.02903045,"about_ca_system_score_codex":0.00026465108,"about_ca_system_score_gemma":0.00014693411,"threshold_uncertainty_score":0.057722926},"labels":[],"label_agreement":null},{"id":"W2941503471","doi":"10.1029/2019gl082391","title":"How Strong Is Influence of the Tropics and Midlatitudes on the Arctic Atmospheric Circulation and Climate Change?","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"European Commission","keywords":"Middle latitudes; Tropics; Climatology; Arctic; Environmental science; Arctic dipole anomaly; Global warming; Arctic geoengineering; Climate change; Arctic sea ice decline; Latitude; Sea surface temperature; Sea ice; Atmospheric circulation; Troposphere; Atmospheric sciences; Arctic ice pack; Oceanography; Geography; Geology; Antarctic sea ice; Ecology","score_opus":0.025889088112822985,"score_gpt":0.2492458290998097,"score_spread":0.2233567409869867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2941503471","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948435,0.00059884915,0.00030317536,0.00040156682,0.000024609495,0.000003097357,0.00024429525,0.000008743669,0.0035721848],"genre_scores_gemma":[0.9993517,0.00023641804,0.000088460154,0.00004210435,0.000018153796,0.0000013176942,0.000070112284,0.000004001403,0.00018773937],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980134,0.00009828374,0.00000835575,0.000034487577,0.000018309369,0.000039183553],"domain_scores_gemma":[0.9991748,0.0004496545,0.0001283012,0.0000487654,0.000071157,0.00012739142],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009058633,0.00021450494,0.00024523336,0.00021702194,0.00026003466,0.00075312704,0.00018306034,0.00023484006,0.0013956984],"category_scores_gemma":[0.0014927058,0.00014748337,0.00040978284,0.00016812836,0.00030595477,0.00047647548,0.00037490894,0.0003097919,0.00015378835],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001066322,0.00014105826,0.9046916,0.00014948165,0.00060747983,0.00029174346,0.00040936942,0.020671902,0.03699299,0.0030277758,0.0011470559,0.030803125],"study_design_scores_gemma":[0.000028884117,0.000121132456,0.9805305,0.000025292284,0.00020119175,0.000035367393,0.0003197139,0.014944323,0.0016116668,0.0007545519,0.0014126942,0.000014698819],"about_ca_topic_score_codex":0.012958109,"about_ca_topic_score_gemma":0.01597167,"teacher_disagreement_score":0.012958109,"about_ca_system_score_codex":0.0002478992,"about_ca_system_score_gemma":0.0003126379,"threshold_uncertainty_score":0.02576536},"labels":[],"label_agreement":null},{"id":"W2942616305","doi":"10.1029/2019gl082526","title":"Regularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":271,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Glacier; Geology; Antarctic ice sheet; Law; Ice sheet; Power law; Mechanics; Physics; Oceanography; Geomorphology; Sea ice; Mathematics","score_opus":0.030785334877627905,"score_gpt":0.2933676808969179,"score_spread":0.26258234601929,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942616305","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99369,0.00015779033,0.004127758,0.00017187736,0.000017195662,0.000028276545,0.0001895493,0.00014897404,0.0014685839],"genre_scores_gemma":[0.9984863,0.000038949394,0.0012675275,0.000012003602,0.0000031806017,0.000007084308,0.00004356604,0.000011847837,0.00012952856],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998938,0.000033664746,0.000008040345,0.000016232096,0.000021142114,0.000027164364],"domain_scores_gemma":[0.99937975,0.00032542576,0.000085445114,0.00007107211,0.000083704675,0.000054509295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005246123,0.00037152797,0.00055719796,0.0005670494,0.00055213406,0.00061745336,0.0007117263,0.00062532106,0.0007271549],"category_scores_gemma":[0.002612122,0.00018887108,0.00038919123,0.0005281297,0.0005407229,0.00032020576,0.0003432887,0.00042308704,0.000059594928],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047676214,0.00006310076,0.009306906,0.000029817917,0.000025616331,0.00010241658,0.000046834535,0.9859138,0.0010311702,0.00062453817,0.0002571783,0.002551004],"study_design_scores_gemma":[0.00001562492,0.000029753233,0.0023428893,0.0000034090183,0.0000039982883,0.000011490546,0.000027051694,0.99705315,0.00024616774,0.00017498508,0.0000852175,0.0000062891168],"about_ca_topic_score_codex":0.08496577,"about_ca_topic_score_gemma":0.050084535,"teacher_disagreement_score":0.08496577,"about_ca_system_score_codex":0.0010564323,"about_ca_system_score_gemma":0.000911842,"threshold_uncertainty_score":0.16894239},"labels":[],"label_agreement":null},{"id":"W2942652025","doi":"10.1029/2019gl082536","title":"Modeling Wind‐Driven Ionospheric Dynamo Currents at Mars: Expectations for InSight Magnetic Field Measurements","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Consejo Superior de Investigaciones Científicas; Instituto de Astrofísica de Andalucía; Centre National de la Recherche Scientifique; Ministerio de Ciencia, Innovación y Universidades; National Aeronautics and Space Administration","keywords":"Dynamo; Mars Exploration Program; Ionosphere; Martian; Physics; Solar wind; Thermosphere; Geophysics; Solstice; Atmospheric sciences; Magnetic field; Plasma; Interplanetary magnetic field; Computational physics; Magnetosphere; Astrobiology; Astronomy; Latitude","score_opus":0.06539761223602483,"score_gpt":0.31476970575679214,"score_spread":0.2493720935207673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942652025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9919046,0.000035414523,0.0051532523,0.00015546128,0.000010944479,0.00002019137,0.00058763544,0.00020922019,0.0019232201],"genre_scores_gemma":[0.9986259,0.000015701951,0.00094098796,0.00001374248,0.0000023530665,0.000009425983,0.00021138003,0.000010022182,0.00017046428],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999206,0.000024789357,0.0000037312998,0.000018511297,0.00001420563,0.000018246967],"domain_scores_gemma":[0.999749,0.00009759928,0.00004405463,0.000027870252,0.000041252857,0.000040153533],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000298386,0.0004092408,0.00026872125,0.00016836611,0.00023146761,0.00053079554,0.0004205638,0.0005008223,0.0008235121],"category_scores_gemma":[0.0009920596,0.00020684864,0.0003313952,0.00016314548,0.0002026609,0.0005158844,0.0002484825,0.00032286992,0.00011236464],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016956948,0.000066193694,0.040721983,0.000015564272,0.00003887632,0.00005673175,0.000039390812,0.9527549,0.002578753,0.00061506574,0.00033516312,0.0026077686],"study_design_scores_gemma":[0.00004854827,0.00007172815,0.00978482,0.000005036664,0.00001226946,0.0000119921215,0.000030044288,0.9888777,0.00067605166,0.00026262624,0.00021147236,0.000007675909],"about_ca_topic_score_codex":0.020961534,"about_ca_topic_score_gemma":0.010048996,"teacher_disagreement_score":0.020961534,"about_ca_system_score_codex":0.000580304,"about_ca_system_score_gemma":0.0005007696,"threshold_uncertainty_score":0.041679025},"labels":[],"label_agreement":null},{"id":"W2942670800","doi":"10.1029/2019gl083149","title":"Dissolved Organic Radiocarbon in the Central Pacific Ocean","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":40,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canada Research Chairs; American Chemical Society Petroleum Research Fund; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Downwelling; Dissolved organic carbon; Upwelling; Oceanography; Seawater; Geology; Subtropics; Radiocarbon dating; Total organic carbon; Surface water; Environmental science; Environmental chemistry; Chemistry","score_opus":0.015625792914249433,"score_gpt":0.23376933572851272,"score_spread":0.2181435428142633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942670800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957231,0.0011141937,0.000110965295,0.000039516493,0.00001773086,0.000006207187,0.0009428359,0.000010965939,0.0020344958],"genre_scores_gemma":[0.99710935,0.0006188429,0.0003307416,0.000055321514,0.000014622942,0.000012527458,0.001060504,0.0000044143167,0.00079380826],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999149,0.000006803285,0.0000056709723,0.000029160265,0.000028937477,0.000014511917],"domain_scores_gemma":[0.99949694,0.000050345257,0.00014008435,0.000018686942,0.00022733139,0.00006651559],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030030642,0.00026758562,0.00011509042,0.0014798032,0.00048323628,0.0006294642,0.00022430021,0.00013435351,0.00073054095],"category_scores_gemma":[0.00044683664,0.00013258918,0.000099165016,0.0014743761,0.00023824461,0.00020061358,0.0002826982,0.00020450476,0.00013600379],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019644422,0.000032092288,0.9608467,0.00006159078,0.000067489076,0.00023112838,0.00020540426,0.00022569249,0.021772305,0.000075215656,0.0002644225,0.01602148],"study_design_scores_gemma":[0.0000035502883,0.00002281605,0.99736303,0.000008496677,0.00001135425,0.000055431825,0.00010684906,0.000074119824,0.0011844609,0.00001616742,0.0011512296,0.000002427092],"about_ca_topic_score_codex":0.08003379,"about_ca_topic_score_gemma":0.10798895,"teacher_disagreement_score":0.08003379,"about_ca_system_score_codex":0.00067356275,"about_ca_system_score_gemma":0.00054613873,"threshold_uncertainty_score":0.15913588},"labels":[],"label_agreement":null},{"id":"W2942849662","doi":"10.1029/2018gl081339","title":"Natural Analogue Constraints on Europa's Non‐ice Surface Material","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation; Leverhulme Trust; University of Winnipeg","keywords":"Sulfate; Icy moon; Astrobiology; Geology; Chloride; Jupiter (rocket family); Mineralogy; Reflectivity; Geochemistry; Natural (archaeology); Chemistry; Planet; Paleontology; Physics; Saturn; Optics","score_opus":0.01586515845998168,"score_gpt":0.2768777122676638,"score_spread":0.2610125538076821,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942849662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979455,0.00007662012,0.00013405124,0.00001512165,0.000002235546,0.0000017173513,0.0001664506,0.0000050213753,0.0016532539],"genre_scores_gemma":[0.99938905,0.00004784422,0.00017814452,0.000010469845,0.0000015193149,0.000002041393,0.00022226418,0.0000072771904,0.00014133374],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998086,0.000019117779,0.000017764078,0.00007672979,0.000044441225,0.00003338769],"domain_scores_gemma":[0.99956197,0.00011713732,0.00009499848,0.00008636835,0.000098379096,0.000041159517],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020406669,0.00016704368,0.00028401034,0.00055534946,0.00038709177,0.00078372995,0.00027190743,0.00026776246,0.0016476405],"category_scores_gemma":[0.0006931683,0.00015366096,0.00013578324,0.00047528313,0.0005589251,0.0003121536,0.0006051882,0.00014423468,0.0002564002],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054712675,0.00004213323,0.24186125,0.00011857693,0.00007558327,0.0004644215,0.00031276842,0.0007412444,0.7448646,0.0009248566,0.00014507913,0.009902463],"study_design_scores_gemma":[0.000019210458,0.000102021266,0.928871,0.000018975245,0.00004082725,0.00042676824,0.00077148405,0.0018151882,0.06369794,0.00044069297,0.0037846458,0.000011234123],"about_ca_topic_score_codex":0.0038903113,"about_ca_topic_score_gemma":0.0056569977,"teacher_disagreement_score":0.0038903113,"about_ca_system_score_codex":0.00042655313,"about_ca_system_score_gemma":0.00018411748,"threshold_uncertainty_score":0.007735312},"labels":[],"label_agreement":null},{"id":"W2942891570","doi":"10.1029/2019gl082786","title":"Long‐Term Support of an Active Subglacial Hydrologic System in Southeast Greenland by Firn Aquifers","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center","keywords":"Meltwater; Firn; Geology; Aquifer; Geomorphology; Hydrology (agriculture); Glacier; Groundwater","score_opus":0.0281704581307122,"score_gpt":0.27204646653840797,"score_spread":0.24387600840769577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2942891570","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997408,0.0000057258017,0.000016485614,0.000040849165,5.9851885e-7,4.569587e-7,0.000065836015,0.0000030051724,0.0001262398],"genre_scores_gemma":[0.9998833,0.000004182386,0.000012026808,0.0000061677338,5.3596847e-7,4.261808e-7,0.00006201622,6.3954013e-7,0.00003069955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999167,0.000014916474,0.000004423647,0.000023005008,0.000009361683,0.000031582247],"domain_scores_gemma":[0.99965477,0.00005580091,0.000094659015,0.000032011205,0.00005288074,0.000109912515],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002919309,0.00010957565,0.00021160877,0.00023716401,0.00030936365,0.00063623884,0.00029408862,0.0002492665,0.0009234226],"category_scores_gemma":[0.00053136935,0.00010545612,0.00015418332,0.00023127744,0.00045904066,0.00032218362,0.00038756902,0.00019174276,0.000059309412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017860564,0.00009005513,0.9780001,0.00001402854,0.0000688906,0.0002043553,0.00030951452,0.008045737,0.00744602,0.000632448,0.00040464703,0.0046055145],"study_design_scores_gemma":[0.000009966672,0.00002241665,0.98961836,0.000004287982,0.000014811939,0.000015931146,0.00031235054,0.009230618,0.00036859952,0.00014118312,0.00025673833,0.000004640922],"about_ca_topic_score_codex":0.109099396,"about_ca_topic_score_gemma":0.16646884,"teacher_disagreement_score":0.109099396,"about_ca_system_score_codex":0.0022357139,"about_ca_system_score_gemma":0.0008727559,"threshold_uncertainty_score":0.21692872},"labels":[],"label_agreement":null},{"id":"W2943587111","doi":"10.1029/2018gl081766","title":"Spatiotemporal Variations in Crustal Seismic Anisotropy Surrounding Induced Earthquakes Near Fox Creek, Alberta","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University; University of Alberta","funders":"National Natural Science Foundation of China; Natural Environment Research Council; Sight Research UK; University of Alberta","keywords":"Geology; Seismology; Induced seismicity; Anisotropy; Shear wave splitting; Focal mechanism; Shear (geology); Seismic anisotropy; Hydraulic fracturing; Sedimentary rock; Fault (geology); Slip (aerodynamics); Geophysics; Petrology; Geotechnical engineering; Geochemistry","score_opus":0.04029212198769172,"score_gpt":0.2879887591184396,"score_spread":0.24769663713074785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2943587111","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982273,0.00004234978,0.00010981524,0.000015658456,0.0000013445391,0.0000047492535,0.00054278254,0.0000068930894,0.001049234],"genre_scores_gemma":[0.9983663,0.000046581652,0.000109113935,0.000005671204,0.000001621751,0.0000027043818,0.0006452739,0.0000017728969,0.00082081585],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998714,0.000007478629,0.000004096415,0.000028219232,0.00004867688,0.000040280574],"domain_scores_gemma":[0.9995628,0.0000434528,0.00008499738,0.000016664748,0.00022090354,0.00007121805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012179852,0.00012789277,0.00015649693,0.00106278,0.00051016675,0.0005588937,0.0003122176,0.00015064653,0.0010116956],"category_scores_gemma":[0.00057691766,0.00010510454,0.00006821615,0.0015129087,0.00033262296,0.00012785108,0.00031534367,0.00011551152,0.00012892485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019380564,0.000035276924,0.959339,0.000026057633,0.00005497735,0.00038614855,0.0017930886,0.0012922317,0.018977763,0.00013918009,0.00078283314,0.016979594],"study_design_scores_gemma":[0.0000011948367,0.000004393013,0.9988943,0.000002089191,0.0000033394158,0.000020714715,0.00039986084,0.00022663969,0.00017942648,0.000006737569,0.00025890645,0.0000025115953],"about_ca_topic_score_codex":0.8185466,"about_ca_topic_score_gemma":0.93211704,"teacher_disagreement_score":0.1814534,"about_ca_system_score_codex":0.002431211,"about_ca_system_score_gemma":0.0015743056,"threshold_uncertainty_score":0.365044},"labels":[],"label_agreement":null},{"id":"W2944659599","doi":"10.1029/2019gl082457","title":"Effects of an Explosive Polar Cyclone Crossing the Antarctic Marginal Ice Zone","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":132,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Swedish Foundation for International Cooperation in Research and Higher Education; Department of Science and Technology, Republic of South Africa; National Science Foundation, United Arab Emirates; National Research Foundation; York University; European Organization for the Exploitation of Meteorological Satellites; Vetenskapsrådet; ACE Foundation; Svenska Forskningsrådet Formas; New York University Abu Dhabi","keywords":"Extratropical cyclone; Sea ice; Geology; Cyclone (programming language); Climatology; Drift ice; Antarctic sea ice; Arctic ice pack; Middle latitudes","score_opus":0.013413940902057657,"score_gpt":0.2629990431094594,"score_spread":0.2495851022074017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2944659599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992704,0.000016489712,0.000025643369,0.000012907435,0.0000046436685,0.0000021048395,0.000039432503,0.0000023970101,0.0006259511],"genre_scores_gemma":[0.99983907,0.000016476924,0.000016216045,0.0000096284,0.0000027195886,0.0000011396293,0.000040338084,5.9032357e-7,0.000073749376],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996567,0.0000063932603,0.0000023034227,0.0000061494175,0.0000063399634,0.000013155251],"domain_scores_gemma":[0.9998553,0.000034683915,0.000028506087,0.000011064405,0.000020856414,0.00004956302],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000785152,0.0001611074,0.00009208596,0.00017573452,0.00027891347,0.0003329745,0.00007615039,0.00014879576,0.0010544308],"category_scores_gemma":[0.00021108102,0.00004145552,0.00008056783,0.00011670058,0.00017040176,0.00008963086,0.00032751873,0.00021426537,0.00008134802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025743083,0.0003067377,0.88623154,0.00006764525,0.0001482523,0.0027736283,0.00053533283,0.0067748837,0.07740911,0.00037569174,0.0012628621,0.021539984],"study_design_scores_gemma":[0.000019762772,0.00030570338,0.99368227,0.0000073964666,0.000021380272,0.00016989824,0.0005686413,0.0019613877,0.002437994,0.000039785904,0.0007811839,0.000004625625],"about_ca_topic_score_codex":0.008786158,"about_ca_topic_score_gemma":0.010877555,"teacher_disagreement_score":0.008786158,"about_ca_system_score_codex":0.00026068205,"about_ca_system_score_gemma":0.000117614196,"threshold_uncertainty_score":0.017470062},"labels":[],"label_agreement":null},{"id":"W2944715505","doi":"10.1029/2018gl081631","title":"Strong Intensification of the Arabian Sea Oxygen Minimum Zone in Response to Arabian Gulf Warming","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":100,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"York University; New York University Abu Dhabi","keywords":"Oxygen minimum zone; Oceanography; Sink (geography); Salinity; Biogeochemistry; Climate change; Hypoxia (environmental); Global warming; Environmental science; Geology; Climatology; Upwelling; Oxygen; Geography","score_opus":0.024638762566635,"score_gpt":0.2687096893647169,"score_spread":0.2440709267980819,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2944715505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99801695,0.000045324417,0.00024004643,0.00022859214,0.000011255809,0.0000037953323,0.00014556594,0.000015649543,0.0012927465],"genre_scores_gemma":[0.9995585,0.00004299973,0.00011901208,0.000041155254,0.0000028532854,0.0000028212971,0.00007897601,0.0000040153745,0.00014958641],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999143,0.000026973887,0.0000056536187,0.000016488444,0.000009990433,0.000026627971],"domain_scores_gemma":[0.9998253,0.000051248484,0.00003797384,0.000017437498,0.000025022984,0.000043022777],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002577635,0.0003576241,0.00028608635,0.00016161421,0.0003808164,0.00091187324,0.00037440102,0.0008256961,0.0024186107],"category_scores_gemma":[0.00065511605,0.00021411199,0.00073976326,0.00022020246,0.00036923747,0.00051788276,0.00077583856,0.00059285766,0.00012070143],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006722446,0.00037802634,0.26130804,0.00019434029,0.00054984813,0.0009482777,0.0003736598,0.67369294,0.046366367,0.006795837,0.0020560878,0.0066644317],"study_design_scores_gemma":[0.00038282858,0.00040564808,0.2720264,0.00004459625,0.0002228112,0.00016437547,0.0010205065,0.7127638,0.007109643,0.0027814826,0.0030120837,0.000065862674],"about_ca_topic_score_codex":0.026230535,"about_ca_topic_score_gemma":0.016610982,"teacher_disagreement_score":0.026230535,"about_ca_system_score_codex":0.00075350254,"about_ca_system_score_gemma":0.0006942443,"threshold_uncertainty_score":0.052155733},"labels":[],"label_agreement":null},{"id":"W2945551893","doi":"10.1029/2019gl082925","title":"Relationship Between the Pacific‐North American Pattern and the Frequency of Tropical Cyclones Over the Western North Pacific","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"National Key Research and Development Program of China; National Oceanic and Atmospheric Administration; Centers for Disease Control and Prevention","keywords":"Tropical cyclone; Wind shear; Climatology; Oceanography; Subtropics; Geology; Geography; Wind speed; Biology; Ecology","score_opus":0.03244253398608012,"score_gpt":0.2757630582098637,"score_spread":0.24332052422378356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2945551893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99871933,0.00007972726,0.000029071674,0.000039390543,0.0000037910481,0.0000015580747,0.00025047862,0.0000032345508,0.00087339],"genre_scores_gemma":[0.99965274,0.000046086414,0.000019601714,0.000004921682,0.000006317552,0.0000011788551,0.00013095124,8.4611787e-7,0.00013737282],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999199,0.000016256841,0.000009095255,0.000024723846,0.000015766773,0.00001438651],"domain_scores_gemma":[0.9988324,0.00018907276,0.000489447,0.000045655095,0.00020335022,0.00023996824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001575064,0.00008743994,0.00006503747,0.0005547122,0.00016562403,0.0003852599,0.00010272793,0.00013553293,0.0028146387],"category_scores_gemma":[0.0008233543,0.00008933494,0.00010857869,0.00063934067,0.00015003899,0.0001826461,0.0001689204,0.00024211415,0.00019354765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013121394,0.000005611166,0.9990752,0.000002155044,0.000017378929,0.000021853408,0.000015158431,0.00003176472,0.00013848074,0.000007916704,0.000065972694,0.0006053868],"study_design_scores_gemma":[3.838967e-7,0.0000038104995,0.99978894,9.776584e-7,0.0000028241013,0.00003123693,0.00003978812,0.00006308915,0.000012479023,0.0000033220242,0.000052593245,5.2039934e-7],"about_ca_topic_score_codex":0.014313263,"about_ca_topic_score_gemma":0.028204938,"teacher_disagreement_score":0.014313263,"about_ca_system_score_codex":0.00014273015,"about_ca_system_score_gemma":0.00017787484,"threshold_uncertainty_score":0.028459907},"labels":[],"label_agreement":null},{"id":"W2946391649","doi":"10.1029/2019gl083167","title":"Algal Export in the Arctic Ocean in Times of Global Warming","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"ArcticNet","keywords":"Arctic; Environmental science; Sea ice; Snowmelt; Oceanography; Carbon cycle; Arctic ice pack; Climatology; Global warming; Arctic sea ice decline; Productivity; Algae; Antarctic sea ice; Climate change; Snow; Geology; Ecology; Ecosystem; Biology","score_opus":0.017961493742299234,"score_gpt":0.27238649701392725,"score_spread":0.25442500327162804,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946391649","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984598,0.00014470919,0.000033138404,0.00004071229,0.000006169894,6.4575966e-7,0.00045402622,0.0000038528774,0.0008569036],"genre_scores_gemma":[0.9984806,0.00019702099,0.00006453932,0.000016825848,0.00001711042,0.0000020209002,0.00072571135,0.0000049432724,0.00049121527],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995065,0.000006707081,0.000004428141,0.0000129013015,0.000011491366,0.000013898376],"domain_scores_gemma":[0.9997658,0.000036503407,0.000082733895,0.0000126818,0.000069030655,0.000033270215],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024295194,0.00024019818,0.00017884727,0.0006220499,0.0003737263,0.0010485771,0.000080141406,0.00016846198,0.001015052],"category_scores_gemma":[0.00039455848,0.000092755225,0.00017194805,0.00084924686,0.00013810494,0.00038249002,0.0003793918,0.0001840443,0.00020017296],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000523401,0.000034858065,0.9746798,0.000046472032,0.000079484606,0.0002891383,0.0005126064,0.0012959893,0.012194283,0.00028394794,0.0004010922,0.009658922],"study_design_scores_gemma":[0.0000019819415,0.000017136521,0.9981857,0.000004939663,0.000008433695,0.00004571465,0.00017864176,0.00039851526,0.00035220588,0.000062994586,0.00074166013,0.0000021036176],"about_ca_topic_score_codex":0.019282736,"about_ca_topic_score_gemma":0.024348335,"teacher_disagreement_score":0.019282736,"about_ca_system_score_codex":0.0006344951,"about_ca_system_score_gemma":0.00025716133,"threshold_uncertainty_score":0.038340986},"labels":[],"label_agreement":null},{"id":"W2946448534","doi":"10.1029/2018gl081863","title":"Statistical Properties of Hiss in Plasmaspheric Plumes and Associated Scattering Losses of Radiation Belt Electrons","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Science Foundation of Hubei Province; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Hiss; Plasmasphere; Van Allen radiation belt; Van Allen Probes; Electron; Physics; Plume; Scattering; Radiation; Electron precipitation; Atomic physics; Geophysics; Computational physics; Magnetosphere; Meteorology; Nuclear physics; Plasma; Optics","score_opus":0.012004175237542642,"score_gpt":0.25763712860149096,"score_spread":0.24563295336394833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946448534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968087,0.000054330656,0.00243532,0.000026963682,0.0000017397751,0.000004901384,0.00019256893,0.000046082005,0.0004292868],"genre_scores_gemma":[0.99949515,0.000015805788,0.00023947547,0.0000025048082,0.0000018319906,0.0000018106196,0.0001776595,0.000004588084,0.000061254024],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993837,0.000008285703,0.0000034526843,0.00001677672,0.000018462453,0.0000146552175],"domain_scores_gemma":[0.99955624,0.00013627879,0.00012845843,0.00004121942,0.00009838754,0.000039404982],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003222389,0.00014317574,0.0001141374,0.0006627391,0.00017914135,0.0003231748,0.00022104177,0.00013125702,0.00063463027],"category_scores_gemma":[0.0011283428,0.000116482675,0.00025498917,0.00034794587,0.00020482167,0.000439586,0.0002779594,0.00016701946,0.000066283275],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034385483,0.00006342463,0.8164112,0.00005212056,0.00016728247,0.0004435282,0.00034038431,0.06531441,0.09960005,0.002244559,0.0005334949,0.014485723],"study_design_scores_gemma":[0.00001526737,0.000106382184,0.7608771,0.0000084611,0.00003491827,0.00029427177,0.00030761812,0.22166866,0.014568136,0.0013346466,0.00074735587,0.000037196758],"about_ca_topic_score_codex":0.003296617,"about_ca_topic_score_gemma":0.0020890427,"teacher_disagreement_score":0.003296617,"about_ca_system_score_codex":0.00029149093,"about_ca_system_score_gemma":0.00010478721,"threshold_uncertainty_score":0.006554842},"labels":[],"label_agreement":null},{"id":"W2946958783","doi":"10.1029/2019gl083289","title":"Responses of Different Types of Pulsating Aurora in Cosmic Noise Absorption","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of California Berkeley; Canadian Space Agency; University of Calgary; National Science Foundation","keywords":"Physics; Observatory; Cosmic ray; Satellite; Absorption (acoustics); Ionosphere; Intensity (physics); Noise (video); Astrophysics; Sky; COSMIC cancer database; Flux (metallurgy); Astronomy; Electron; Atmospheric sciences; Optics; Chemistry; Nuclear physics","score_opus":0.016235829893456784,"score_gpt":0.2905810904068335,"score_spread":0.2743452605133767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2946958783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99895215,0.000034730765,0.00011253026,0.0000071259606,0.000002602997,0.0000030657848,0.00008543429,0.0000057362768,0.00079669716],"genre_scores_gemma":[0.9995402,0.000019525218,0.000057203448,0.000009324679,0.00000434731,0.0000031938307,0.00014892647,0.0000035323972,0.00021375173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998259,0.000029239034,0.000009368424,0.00004993161,0.000039389688,0.00004619196],"domain_scores_gemma":[0.99942183,0.00015733384,0.00016381819,0.000043981283,0.000095294476,0.00011777323],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018284925,0.00018840202,0.0002223767,0.00060404086,0.00018924207,0.0005009393,0.00012047904,0.0002300474,0.0012548263],"category_scores_gemma":[0.0010724539,0.00010794164,0.0001234546,0.00040162055,0.00018115845,0.00017048854,0.0004528411,0.000200147,0.00017557306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007787698,0.00006962235,0.9063113,0.0000278447,0.00010490717,0.00015518682,0.00041201498,0.0003975809,0.07974811,0.00007372671,0.00017657013,0.011744335],"study_design_scores_gemma":[0.0000018353321,0.00004196678,0.998131,0.0000013335807,0.000007920885,0.00007959667,0.00012786817,0.00024859884,0.0012172856,0.000021050266,0.000119532066,0.0000020056414],"about_ca_topic_score_codex":0.0012754392,"about_ca_topic_score_gemma":0.0013097416,"teacher_disagreement_score":0.0012754392,"about_ca_system_score_codex":0.000162455,"about_ca_system_score_gemma":0.000060461298,"threshold_uncertainty_score":0.004197836},"labels":[],"label_agreement":null},{"id":"W2947218305","doi":"10.1029/2019gl083342","title":"Analytical Propagation of Runoff Uncertainty Into Discharge Uncertainty Through a Large River Network","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; University of Saskatchewan","funders":"Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Surface runoff; Discharge; Environmental science; Hydrology (agriculture); Propagation of uncertainty; Covariance; Routing (electronic design automation); Meteorology; Statistics; Geology; Drainage basin; Mathematics; Computer science; Geography; Geotechnical engineering; Ecology","score_opus":0.01939444046104345,"score_gpt":0.2973451681917762,"score_spread":0.27795072773073276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947218305","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2495732,0.00018740575,0.7447751,0.00065288355,0.000025381582,0.000030416475,0.00010986568,0.00028120945,0.004364572],"genre_scores_gemma":[0.96262985,0.00018818816,0.03594742,0.00004473938,0.000020726093,0.000023971574,0.000051800926,0.000045236884,0.0010478885],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995765,0.000164444,0.000021066804,0.00007771898,0.00012597325,0.000034325392],"domain_scores_gemma":[0.9919739,0.006119602,0.0008858549,0.00033995986,0.00057845726,0.000102275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019822395,0.0003357804,0.0002764171,0.0008518582,0.0003689083,0.0008180618,0.0005318431,0.000492279,0.0008172566],"category_scores_gemma":[0.013212548,0.00037286637,0.00034901113,0.00075411453,0.0013123844,0.0018341106,0.0010142685,0.00096756185,0.00007555429],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000010881669,0.000014548388,0.004243429,0.000009886258,0.00001617022,0.000101368125,0.00008018274,0.96212983,0.0010048761,0.024517208,0.00020025767,0.007671322],"study_design_scores_gemma":[0.0000014806196,0.000003919667,0.00064163434,0.0000029646994,0.0000029665546,0.000013351337,0.000011206086,0.9921783,0.00015078223,0.00688367,0.00010480729,0.000004799816],"about_ca_topic_score_codex":0.011882411,"about_ca_topic_score_gemma":0.00601478,"teacher_disagreement_score":0.011882411,"about_ca_system_score_codex":0.0014801641,"about_ca_system_score_gemma":0.0010616487,"threshold_uncertainty_score":0.023626506},"labels":[],"label_agreement":null},{"id":"W2947262781","doi":"10.1029/2019gl083195","title":"Topside Ionospheric Disturbances Detected Using Radio Occultation Measurements During the August 2017 Solar Eclipse","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; European Space Agency","keywords":"Ionosphere; Solar eclipse; Thermosphere; Total electron content; Eclipse; Radio occultation; Occultation; TEC; Atmospheric sciences; Environmental science; Altitude (triangle); Remote sensing; Geology; Physics; Astronomy; Geophysics","score_opus":0.03149505146867467,"score_gpt":0.29107993695272966,"score_spread":0.259584885484055,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2947262781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850744,0.000027955757,0.00016242481,0.000011955428,0.0000062308336,0.0000031536156,0.00055438303,0.000029670191,0.00069683307],"genre_scores_gemma":[0.9990325,0.00002504684,0.00013057815,0.000003453444,0.0000039470424,0.0000022974027,0.0006871414,0.0000037805842,0.00011131669],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995446,0.0000048029397,0.0000025891884,0.00001209169,0.000013407889,0.0000126359355],"domain_scores_gemma":[0.99988174,0.00002105799,0.000034801098,0.000011688411,0.000027386146,0.00002321886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009837097,0.00020164953,0.00012229185,0.00035707018,0.00014844956,0.00026844727,0.00009757861,0.00017424968,0.0005366898],"category_scores_gemma":[0.0003034851,0.000081671365,0.00011977079,0.00032573598,0.00008458957,0.000121830926,0.00018264122,0.00013419948,0.00015947933],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005693558,0.000052033578,0.9400472,0.000045713154,0.000097353106,0.0005582857,0.00032456452,0.0058825742,0.036116894,0.00010986783,0.0012874849,0.014908791],"study_design_scores_gemma":[0.000007220191,0.00004651529,0.9922517,0.000006987226,0.000016974936,0.00008894443,0.00007901893,0.0047810627,0.0020788382,0.000016176262,0.00062207103,0.0000045897914],"about_ca_topic_score_codex":0.008837116,"about_ca_topic_score_gemma":0.01688568,"teacher_disagreement_score":0.008837116,"about_ca_system_score_codex":0.00021935944,"about_ca_system_score_gemma":0.00012205093,"threshold_uncertainty_score":0.01757133},"labels":[],"label_agreement":null},{"id":"W2948398899","doi":"10.1029/2019gl082687","title":"Steve: The Optical Signature of Intense Subauroral Ion Drifts","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; University of Calgary; University of Saskatchewan","funders":"European Space Agency; Canadian Space Agency; University of Calgary; National Science Foundation","keywords":"Ion; Satellite; Physics; Astrophysics; Geophysics; Meteorology; Astronomy; Quantum mechanics","score_opus":0.011812798957336043,"score_gpt":0.27581667371678087,"score_spread":0.2640038747594448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2948398899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963726,0.0002759636,0.0005927377,0.000042946805,0.000009985274,0.0000055709024,0.00011145653,0.000021281916,0.0025675113],"genre_scores_gemma":[0.9993418,0.000071595256,0.00025101172,0.000016905014,0.000011679782,0.0000013077985,0.00004976143,0.000003367979,0.00025261616],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999126,0.000008699373,0.0000058865376,0.000016175316,0.000023840388,0.000032842367],"domain_scores_gemma":[0.9994462,0.000111796406,0.00026940712,0.000053375,0.000061030965,0.0000581943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018159792,0.0001603399,0.0001332015,0.0011490565,0.00031011368,0.0004950287,0.00015403608,0.0003081362,0.0011713164],"category_scores_gemma":[0.0007239249,0.00010365396,0.00009818025,0.00055264507,0.0003944611,0.00035354204,0.0006139817,0.00024408662,0.00015080995],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007993939,0.00006838149,0.8324358,0.00010941857,0.00009306367,0.008174053,0.0009632719,0.00033781037,0.115309365,0.00085808185,0.0008078552,0.040043507],"study_design_scores_gemma":[0.000007768624,0.00017802387,0.967506,0.00003076708,0.000024338347,0.016141536,0.0008661739,0.00056546036,0.011356995,0.00040377807,0.002904227,0.000014956605],"about_ca_topic_score_codex":0.0006651249,"about_ca_topic_score_gemma":0.0014893096,"teacher_disagreement_score":0.0011713164,"about_ca_system_score_codex":0.000096607764,"about_ca_system_score_gemma":0.00006696741,"threshold_uncertainty_score":0.003918469},"labels":[],"label_agreement":null},{"id":"W2949642527","doi":"10.1029/2019gl082908","title":"Larger Increases in More Extreme Local Precipitation Events as Climate Warms","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":143,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Pacific Institute for Climate Solutions; University of Victoria","funders":"","keywords":"Climatology; Precipitation; Environmental science; Climate change; General Circulation Model; Atmospheric circulation; Climate model; Extreme weather; Extreme value theory; Spatial ecology; Atmospheric sciences; Geology; Geography; Meteorology; Oceanography; Ecology","score_opus":0.038687017926349446,"score_gpt":0.32063928688365184,"score_spread":0.2819522689573024,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2949642527","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9925161,0.00012972234,0.0011230806,0.0002038681,0.000021334763,0.00000845566,0.00052902615,0.00011557136,0.0053529353],"genre_scores_gemma":[0.9985474,0.000077550605,0.0002582492,0.00006111796,0.000030999287,0.0000042974407,0.00033688018,0.000014871478,0.0006686016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987173,0.000020182044,0.000008726904,0.000048633647,0.00002846757,0.000022233811],"domain_scores_gemma":[0.9991703,0.0002080617,0.00030677178,0.00011061261,0.00009199275,0.000112326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002978187,0.00014155517,0.0002359785,0.00043739047,0.00029687953,0.00084197737,0.00017424834,0.0002565068,0.005275961],"category_scores_gemma":[0.0010761336,0.00012363531,0.0002459147,0.00053526676,0.00028411648,0.0004954037,0.0006269684,0.00054468133,0.00037534768],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033221047,0.0002882958,0.8928629,0.00019269196,0.0004906749,0.0005003873,0.0009352513,0.02625562,0.03243375,0.0023414523,0.004429828,0.038936954],"study_design_scores_gemma":[0.000010788998,0.000020648084,0.9939213,0.000004182629,0.000025890917,0.00006594827,0.000100731966,0.0024901663,0.000946473,0.0006159763,0.0017904175,0.0000074997447],"about_ca_topic_score_codex":0.002167498,"about_ca_topic_score_gemma":0.0038789546,"teacher_disagreement_score":0.005275961,"about_ca_system_score_codex":0.00020056346,"about_ca_system_score_gemma":0.00011890119,"threshold_uncertainty_score":0.017649889},"labels":[],"label_agreement":null},{"id":"W2950089093","doi":"10.1029/2019gl082767","title":"Computation of Magnetic Anomalies Caused by Two‐Dimensional Structures of Arbitrary Shape: Derivation and Matlab Implementation","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Computation; Magnetic anomaly; MATLAB; Software; Computer science; Anomaly (physics); Polar; Geophysics; Algorithm; Computational science; Geology; Physics; Programming language","score_opus":0.023128547911488398,"score_gpt":0.31651172941925587,"score_spread":0.2933831815077675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2950089093","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.009311733,0.00009027826,0.98045886,0.00020383325,0.000051574138,0.000027834447,0.0001356295,0.0016550331,0.008065276],"genre_scores_gemma":[0.25903267,0.00031338158,0.72380036,0.00015183844,0.000058838817,0.00017495223,0.00028045304,0.0011609592,0.015026607],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987483,0.000023142606,0.000010249432,0.000016230331,0.000062565545,0.000012942245],"domain_scores_gemma":[0.99940133,0.00030433614,0.00003883506,0.000063505206,0.00017028344,0.000021763937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002834485,0.00042219445,0.00032173426,0.00042028684,0.00026359974,0.0008137593,0.00092541834,0.00061105046,0.007301212],"category_scores_gemma":[0.0022079959,0.0002503137,0.00036596085,0.00045729327,0.00036557222,0.00057061046,0.00083986437,0.00060570985,0.0027121],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000103058715,0.0000764166,0.002230768,0.00045832602,0.00004732012,0.0008645978,0.00028941457,0.5741829,0.022527998,0.19378899,0.009884098,0.19554615],"study_design_scores_gemma":[0.000018237823,0.000014340912,0.0002989132,0.000026018755,0.000004368133,0.00016095798,0.000024288716,0.9694137,0.005608339,0.016892802,0.007528439,0.000009548752],"about_ca_topic_score_codex":0.002153701,"about_ca_topic_score_gemma":0.002134759,"teacher_disagreement_score":0.007301212,"about_ca_system_score_codex":0.0003957021,"about_ca_system_score_gemma":0.0006020078,"threshold_uncertainty_score":0.02442497},"labels":[],"label_agreement":null},{"id":"W2950567084","doi":"10.1029/2019gl082965","title":"Evaluating a Moist Isentropic Framework for Poleward Moisture Transport: Implications for Water Isotopes Over Antarctica","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Center for Atmospheric Research","keywords":"Moisture; Environmental science; Isentropic process; Atmospheric sciences; Polar; Sink (geography); TRACER; Climatology; Water content; Geology; Meteorology; Physics; Thermodynamics","score_opus":0.07243467113626388,"score_gpt":0.3633126049115245,"score_spread":0.2908779337752606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2950567084","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.89391905,0.0003814594,0.096324645,0.0011630675,0.000056366716,0.000090827234,0.0005778663,0.00013516567,0.0073514483],"genre_scores_gemma":[0.9920168,0.0001239211,0.0072418465,0.000045637786,0.00003226281,0.000020519385,0.00010109275,0.00003270556,0.00038510704],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997123,0.000171417,0.000012880771,0.00003919834,0.000032374846,0.000031797263],"domain_scores_gemma":[0.99870455,0.0007810068,0.00017065894,0.000067737405,0.00015616712,0.00011989185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002048817,0.00051666313,0.00041751075,0.0008635832,0.0005245709,0.0017914209,0.0011196246,0.00083083875,0.0020567677],"category_scores_gemma":[0.0046778712,0.00037914232,0.00078618637,0.00051036204,0.0009645435,0.0014851558,0.00095725886,0.0007459266,0.00011167289],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009160814,0.00008182971,0.015898164,0.000030329911,0.0000645184,0.00012388601,0.00006434794,0.94982827,0.003186352,0.026761027,0.00022587788,0.0036438406],"study_design_scores_gemma":[0.000012632348,0.0000359754,0.004001961,0.000006733501,0.000007839042,0.0000079102865,0.00006960472,0.9905441,0.0001624801,0.0050045173,0.00013665008,0.000009658605],"about_ca_topic_score_codex":0.052331638,"about_ca_topic_score_gemma":0.032696493,"teacher_disagreement_score":0.052331638,"about_ca_system_score_codex":0.0018620241,"about_ca_system_score_gemma":0.0012360769,"threshold_uncertainty_score":0.104054034},"labels":[],"label_agreement":null},{"id":"W2951253163","doi":"10.1029/2019gl082187","title":"Climate Change Drives Widespread and Rapid Thermokarst Development in Very Cold Permafrost in the Canadian High Arctic","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":321,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories","funders":"National Science Foundation of Sri Lanka","keywords":"Thermokarst; Permafrost; Arctic; Environmental science; Climate change; Physical geography; Vegetation (pathology); Climatology; Global warming; Geology; Atmospheric sciences; Oceanography; Geography","score_opus":0.05964038370090108,"score_gpt":0.2747940155079751,"score_spread":0.21515363180707403,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2951253163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973574,0.00009032922,0.000088707464,0.00010443745,0.00000413967,0.000006819164,0.0007407744,0.000011187306,0.0015959846],"genre_scores_gemma":[0.999446,0.000046140554,0.00007357752,0.000017983342,0.0000013728703,0.000001999064,0.00025373654,0.0000024061812,0.00015680677],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997608,0.000012535747,0.000007795583,0.00004787471,0.00006530518,0.00010576004],"domain_scores_gemma":[0.9994246,0.000035038756,0.00010031294,0.00002091863,0.0003048225,0.00011427835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025049085,0.000204767,0.00024463225,0.001062574,0.0023022757,0.0010251792,0.00046265495,0.0003367659,0.0012609762],"category_scores_gemma":[0.000604669,0.00019063405,0.00024289147,0.0013984784,0.0007286217,0.00027158175,0.0005971034,0.0003016358,0.000082048246],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000096294956,0.000035124795,0.98234034,0.000033779215,0.000052838248,0.00013136792,0.00080276607,0.0010631186,0.007951077,0.00023527569,0.00094019854,0.006317792],"study_design_scores_gemma":[0.0000013512936,0.000003238609,0.99862194,0.0000041936823,0.0000048276443,0.000011423684,0.00041517123,0.00036038464,0.00016674367,0.000018335533,0.00038770356,0.000004545007],"about_ca_topic_score_codex":0.98047,"about_ca_topic_score_gemma":0.9932294,"teacher_disagreement_score":0.019529998,"about_ca_system_score_codex":0.010860034,"about_ca_system_score_gemma":0.010932506,"threshold_uncertainty_score":0.07879549},"labels":[],"label_agreement":null},{"id":"W2953973323","doi":"10.1029/2019gl083673","title":"An Observation‐Based Correction for Aerosol Effects on Nitrogen Dioxide Column Retrievals Using the Absorbing Aerosol Index","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Dalhousie University","funders":"Goddard Space Flight Center","keywords":"Aerosol; Environmental science; Atmospheric sciences; Radiative transfer; Absorption (acoustics); Satellite; Trace gas; Nitrogen dioxide; Remote sensing; Chemical transport model; Meteorology; Physics; Optics; Geology","score_opus":0.041486641292084354,"score_gpt":0.2993429687608051,"score_spread":0.2578563274687207,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2953973323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85079324,0.00045426632,0.14156264,0.00030894275,0.00020508522,0.00010506333,0.0009523729,0.0024136258,0.0032047199],"genre_scores_gemma":[0.952377,0.00010255918,0.045874238,0.00008644918,0.000026049001,0.00003271511,0.00071200496,0.00015305045,0.0006359857],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9996493,0.00007877646,0.000021524786,0.00008927726,0.00012785218,0.00003322924],"domain_scores_gemma":[0.9994837,0.00015942208,0.00007464634,0.0001250687,0.00014023311,0.000016853357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00092752016,0.0004927339,0.0002668305,0.00036803732,0.00031235398,0.0005195403,0.00062040135,0.00036094032,0.0004413356],"category_scores_gemma":[0.002271642,0.00026401095,0.00044297095,0.00035924895,0.00021751993,0.00072407426,0.00047744586,0.00040373605,0.00017491855],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00048279876,0.0003714144,0.21303554,0.00028633018,0.0008286645,0.00022466063,0.00017476425,0.2570913,0.39095947,0.003377673,0.0034670779,0.12970035],"study_design_scores_gemma":[0.00008310891,0.000091002104,0.07401561,0.000025654837,0.00014230353,0.0000712332,0.000027487897,0.8331137,0.088944614,0.0005117131,0.0029140327,0.000059585782],"about_ca_topic_score_codex":0.017288458,"about_ca_topic_score_gemma":0.024666391,"teacher_disagreement_score":0.017288458,"about_ca_system_score_codex":0.0004741654,"about_ca_system_score_gemma":0.00089763606,"threshold_uncertainty_score":0.034375608},"labels":[],"label_agreement":null},{"id":"W2954927549","doi":"10.1029/2019gl082770","title":"Major Impact of Dust Deposition on the Productivity of the Arabian Sea","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK; York University; New York University Abu Dhabi","keywords":"Biogeochemical cycle; Biogeochemistry; Deposition (geology); Environmental science; Reactive nitrogen; Atmospheric sciences; Primary productivity; Nutrient; New production; Iron fertilization; Productivity; Primary production; Mineral dust; Nitrogen fixation; Nitrogen; Aerosol; Atmosphere (unit); Monsoon; Oceanography; Ecosystem; Environmental chemistry; Geology; Meteorology; Chemistry; Ecology; Geography; Phytoplankton; Biology","score_opus":0.02237138449950668,"score_gpt":0.2628994879121512,"score_spread":0.2405281034126445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2954927549","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99865985,0.00020812862,0.000099910736,0.00006986917,0.000010559215,0.0000011274295,0.0002359882,0.000008376639,0.0007061256],"genre_scores_gemma":[0.9995894,0.00009699638,0.000042593165,0.0000085928505,0.000004101122,5.969599e-7,0.00012407672,0.0000020631967,0.00013163521],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998815,0.000032388536,0.00000945432,0.000029764338,0.000017524137,0.000029377567],"domain_scores_gemma":[0.99971205,0.000097968594,0.000040635812,0.0000279055,0.000058405676,0.00006304586],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022640802,0.0004885626,0.00024681955,0.0003664124,0.00028829486,0.0007035637,0.0002083973,0.00032210743,0.00107127],"category_scores_gemma":[0.0003594348,0.00015799374,0.0005149451,0.0002723958,0.00025704713,0.00020692755,0.0003672652,0.00016997756,0.00019405544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009420851,0.000096479205,0.8841248,0.0001906432,0.00049247587,0.0010274444,0.00011338946,0.015088909,0.08059753,0.0008995253,0.0004410338,0.015985692],"study_design_scores_gemma":[0.000051479383,0.00012890477,0.9688853,0.000020109997,0.00014874293,0.00017700689,0.0002939139,0.014710041,0.01398599,0.00034241372,0.0012402007,0.000015828928],"about_ca_topic_score_codex":0.012853844,"about_ca_topic_score_gemma":0.006002631,"teacher_disagreement_score":0.012853844,"about_ca_system_score_codex":0.0005786014,"about_ca_system_score_gemma":0.0004612588,"threshold_uncertainty_score":0.025558054},"labels":[],"label_agreement":null},{"id":"W2955246071","doi":"10.1029/2019gl083272","title":"First Observations From the TREx Spectrograph: The Optical Spectrum of STEVE and the Picket Fence Phenomena","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Athabasca University; University of Calgary","funders":"Ministry of Economic Development and Trade, Government of Alberta; National Institute of Standards and Technology; Canada Foundation for Innovation; University of Calgary","keywords":"Picketing; Spectrograph; Emission spectrum; Physics; Spectral line; Line (geometry); Geology; Astrophysics; Astronomy; Law; Political science; Geometry","score_opus":0.017818550603256357,"score_gpt":0.25140204953745093,"score_spread":0.23358349893419458,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2955246071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966677,0.0000522854,0.0003340241,0.00003214529,0.00000434499,0.000005975324,0.00017949256,0.00003312495,0.0026908766],"genre_scores_gemma":[0.99848324,0.00003149955,0.0004979223,0.000025946874,0.0000043101672,0.00000292146,0.00023071916,0.000008534529,0.0007148441],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999422,0.000003686748,0.0000016338361,0.000012128197,0.000018389494,0.000021993228],"domain_scores_gemma":[0.9998313,0.00002887345,0.000021917383,0.000022851107,0.000049798153,0.00004522263],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012496399,0.0001215653,0.00015871806,0.0004415106,0.00052857585,0.00031371485,0.00018762202,0.00025420633,0.0009976755],"category_scores_gemma":[0.00023361514,0.00015918625,0.00012235099,0.00030634238,0.00026673792,0.0002780458,0.00041312014,0.00046936984,0.00010959487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010439631,0.00024356613,0.5948661,0.0000661018,0.00015742047,0.0030567364,0.0023115831,0.00086067145,0.35942015,0.00055472547,0.0029787554,0.034440216],"study_design_scores_gemma":[0.00001219788,0.00010888391,0.9879979,0.000009160357,0.000009447714,0.00036612875,0.00041565148,0.00056422304,0.007735877,0.000043177693,0.002728126,0.000009354232],"about_ca_topic_score_codex":0.013948102,"about_ca_topic_score_gemma":0.06696837,"teacher_disagreement_score":0.013948102,"about_ca_system_score_codex":0.00033545756,"about_ca_system_score_gemma":0.00020972147,"threshold_uncertainty_score":0.027733862},"labels":[],"label_agreement":null},{"id":"W2956053481","doi":"10.1029/2019gl083015","title":"Using Satellite‐Based Vegetation Cover as Indicator of Groundwater Storage in Natural Vegetation Areas","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Flood Risk Assessment and Management","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"","keywords":"Normalized Difference Vegetation Index; Groundwater; Environmental science; Vegetation (pathology); Water table; Hydrology (agriculture); Enhanced vegetation index; Remote sensing; Table (database); Soil science; Geology; Vegetation Index; Climate change; Computer science; Data mining","score_opus":0.02453639489216212,"score_gpt":0.3159649573391139,"score_spread":0.29142856244695176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2956053481","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99891365,0.000020658004,0.0004756675,0.000013173936,0.000001294006,0.0000028124866,0.00020472363,0.000012968011,0.00035497872],"genre_scores_gemma":[0.9992791,0.000012033291,0.000505032,0.0000027469202,8.884067e-7,0.000002078158,0.00014417294,8.6968424e-7,0.000053173684],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999863,0.000053526557,0.00001173537,0.000026553424,0.00002364,0.000021537482],"domain_scores_gemma":[0.99957234,0.00016128915,0.00011560172,0.00003828882,0.00007161218,0.000040861643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036118474,0.00016854118,0.00011657579,0.00096456916,0.00012959029,0.00039615805,0.00017286454,0.00015620844,0.00045360063],"category_scores_gemma":[0.0010572446,0.00008889373,0.00026136992,0.0010020923,0.000200813,0.00032823643,0.00022046674,0.00008789991,0.00007168786],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014019849,0.000054408913,0.95924914,0.00002390571,0.000093115385,0.00007886895,0.00008330237,0.02582291,0.003913056,0.00010226101,0.00011920798,0.010319755],"study_design_scores_gemma":[0.000007340343,0.00007191558,0.9197452,0.000007871345,0.000029650271,0.000058173617,0.0001449213,0.07751762,0.0020520252,0.00016072243,0.00019237956,0.000012117725],"about_ca_topic_score_codex":0.025407705,"about_ca_topic_score_gemma":0.04053229,"teacher_disagreement_score":0.025407705,"about_ca_system_score_codex":0.0005627662,"about_ca_system_score_gemma":0.00028361255,"threshold_uncertainty_score":0.050519645},"labels":[],"label_agreement":null},{"id":"W2956453037","doi":"10.1029/2019gl082320","title":"Is Arctic Amplification Dominated by Regional Radiative Forcing and Feedbacks: Perspectives From the World‐Avoided Scenario","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"The Scarborough Hospital; University of Toronto; University of Waterloo","funders":"","keywords":"Radiative forcing; Forcing (mathematics); Atmospheric sciences; Climatology; Environmental science; Albedo (alchemy); Radiative transfer; Cloud forcing; Arctic; Physics; Meteorology; Geology; Aerosol","score_opus":0.024707165424516,"score_gpt":0.273665309847842,"score_spread":0.24895814442332598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2956453037","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99364895,0.00014190072,0.0012121061,0.00049836945,0.00001792383,0.000005750921,0.00053042965,0.000045479974,0.0038990946],"genre_scores_gemma":[0.99923587,0.00005526809,0.00031523546,0.000030193689,0.000008629486,0.000003459494,0.00018172919,0.000012181625,0.00015742701],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997402,0.00009998954,0.000008983392,0.000048617654,0.00003324142,0.00006897013],"domain_scores_gemma":[0.9995142,0.00013967429,0.000093711,0.000056817247,0.000120773504,0.00007476625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007982574,0.0004656594,0.00043966123,0.00054968346,0.0005427925,0.0014435524,0.0005072334,0.00045351675,0.0012754216],"category_scores_gemma":[0.0013052549,0.00019227974,0.00068053004,0.0005457207,0.00051017426,0.00088067335,0.0007263636,0.00046654933,0.000084579086],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006681351,0.00015314731,0.21227083,0.00010532971,0.0008968099,0.0010761622,0.00037165234,0.73773843,0.012510432,0.023133969,0.0026330294,0.008442029],"study_design_scores_gemma":[0.000102067825,0.00009592189,0.1297926,0.00003100443,0.00033553917,0.000075463635,0.00052814634,0.8532106,0.003166789,0.009196544,0.0033530504,0.00011219145],"about_ca_topic_score_codex":0.1149275,"about_ca_topic_score_gemma":0.087597236,"teacher_disagreement_score":0.1149275,"about_ca_system_score_codex":0.0017570241,"about_ca_system_score_gemma":0.0010142544,"threshold_uncertainty_score":0.22851712},"labels":[],"label_agreement":null},{"id":"W2957623361","doi":"10.1029/2019gl083027","title":"Glacially Induced Hydromechanical Coupling in Shale May Have Caused Underpressured Water in the Eastern Michigan Basin Despite the Possible Presence of Gas Phase Methane","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"U.S. Geological Survey; Nuclear Waste Management Organization","keywords":"Methane; Geology; Hydraulic fracturing; Oil shale; Natural gas; Pore water pressure; Glacial period; Permeability (electromagnetism); Phase (matter); Hydrostatic pressure; Petrology; Petroleum engineering; Environmental science; Geotechnical engineering; Geomorphology; Paleontology; Mechanics; Chemistry","score_opus":0.03918186040543313,"score_gpt":0.31612308093231006,"score_spread":0.2769412205268769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2957623361","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99977344,0.0000026407017,0.00003727374,0.000012971897,4.3440778e-7,8.815659e-7,0.000014723428,0.000004567891,0.00015307817],"genre_scores_gemma":[0.9999095,0.0000035737914,0.000029107736,0.0000019895795,2.9427906e-7,8.1020147e-7,0.00001068438,0.0000010101668,0.000042986907],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999664,0.0000060975294,0.0000023350638,0.000007357746,0.0000056347767,0.000012136126],"domain_scores_gemma":[0.999943,0.000014385443,0.000011634276,0.000005236323,0.000007855601,0.000017795326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087413515,0.00012619834,0.00013386438,0.00025340487,0.00041319142,0.00043542424,0.00022557889,0.00039415344,0.0010602818],"category_scores_gemma":[0.0002512996,0.00018078952,0.00016558771,0.00016324851,0.00041766622,0.00023182009,0.00029436548,0.00016293935,0.000049702972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003876557,0.0002667344,0.6505142,0.0000791005,0.00020094404,0.001680053,0.0005779351,0.12782535,0.20712207,0.0015416857,0.00039477652,0.009409488],"study_design_scores_gemma":[0.000048052683,0.00017481437,0.8088599,0.000007222198,0.000042413867,0.00014802977,0.00077291136,0.17402183,0.014958778,0.00035090224,0.0005889439,0.00002628694],"about_ca_topic_score_codex":0.029824795,"about_ca_topic_score_gemma":0.05550924,"teacher_disagreement_score":0.029824795,"about_ca_system_score_codex":0.0009914445,"about_ca_system_score_gemma":0.00044748047,"threshold_uncertainty_score":0.05930239},"labels":[],"label_agreement":null},{"id":"W2962760885","doi":"10.1029/2019gl082116","title":"Northern Hemisphere Land Monsoon Precipitation Increased by the Green Sahara During Middle Holocene","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":61,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Priority Academic Program Development of Jiangsu Higher Education Institutions; National Key Research and Development Program of China; China Scholarship Council; Vetenskapsrådet; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Holocene; Monsoon; Northern Hemisphere; Precipitation; Climatology; Vegetation (pathology); Environmental science; Land cover; Physical geography; Geology; Land use; Oceanography; Geography; Ecology; Meteorology","score_opus":0.022886195725876347,"score_gpt":0.25410996204738856,"score_spread":0.2312237663215122,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2962760885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989513,0.00007596264,0.000055591623,0.00007054931,0.000008840477,0.0000013177895,0.00023185456,0.000018074088,0.0005865336],"genre_scores_gemma":[0.9997675,0.00003095047,0.000023330778,0.000009565431,0.000004593402,0.0000013680649,0.0001212731,0.000002287689,0.000039143164],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999187,0.000021801343,0.000005382006,0.000016062153,0.0000095470195,0.000028542905],"domain_scores_gemma":[0.99988306,0.000023290235,0.00002710388,0.000009525253,0.000016533704,0.000040440238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002072405,0.00027544555,0.0002590041,0.00034408458,0.00035578426,0.0006435405,0.00020908554,0.00030394405,0.0016461227],"category_scores_gemma":[0.00033879076,0.0001280354,0.00040501647,0.00038903934,0.0002893964,0.00027701995,0.00032069182,0.00022219995,0.00014022182],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00097127404,0.00013213904,0.93835664,0.00012299482,0.00051742693,0.0011857577,0.0006999551,0.022616575,0.018168632,0.0006618622,0.0016131225,0.014953693],"study_design_scores_gemma":[0.000043336608,0.000051127612,0.9886945,0.000008264707,0.00005312614,0.00008019804,0.00027712467,0.008530693,0.0011340902,0.00014972381,0.0009682484,0.000009550625],"about_ca_topic_score_codex":0.024704328,"about_ca_topic_score_gemma":0.01942362,"teacher_disagreement_score":0.024704328,"about_ca_system_score_codex":0.00072545395,"about_ca_system_score_gemma":0.00030326154,"threshold_uncertainty_score":0.04912108},"labels":[],"label_agreement":null},{"id":"W2963111335","doi":"10.1029/2019gl083566","title":"Frictional Stabilities on Induced Earthquake Fault Planes at Fox Creek, Alberta: A Pore Fluid Pressure Dilemma","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Alberta Energy; University of Alberta; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Helmholtz-Alberta Initiative","keywords":"Pore water pressure; Hydraulic fracturing; Slip (aerodynamics); Fluid pressure; Hydrostatic equilibrium; Fault (geology); Induced seismicity; Hydrostatic pressure","score_opus":0.03748806663023269,"score_gpt":0.2691873581612527,"score_spread":0.23169929153102004,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2963111335","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977736,0.000011355826,0.0011990324,0.00007651668,4.7216187e-7,0.0000017880553,0.000033760756,0.000009138483,0.0008943309],"genre_scores_gemma":[0.99987173,0.00000496753,0.00005863955,0.000001285393,2.6310323e-7,4.3102597e-7,0.0000065830413,7.691281e-7,0.000055348686],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999404,0.000009476669,0.000002799383,0.0000086654345,0.000019247265,0.000019509282],"domain_scores_gemma":[0.99945456,0.00028950965,0.00008616837,0.00003218765,0.0000914453,0.000046059966],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002466198,0.00012943518,0.00015465067,0.0004204277,0.00042868752,0.0007975572,0.00050600513,0.0004530792,0.0010868479],"category_scores_gemma":[0.002206559,0.00013812588,0.00012608191,0.00026801508,0.0012955762,0.00059598277,0.00040686427,0.00027195437,0.00004266142],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011064013,0.000052253978,0.08712937,0.000031202097,0.00003499822,0.00063496066,0.00029530015,0.8816848,0.0046468717,0.019041792,0.0003395693,0.005998289],"study_design_scores_gemma":[0.000023787594,0.000051490835,0.08177351,0.000007989981,0.000017271861,0.000101409314,0.00053102284,0.9051812,0.0015544306,0.0104555385,0.0002829742,0.00001928834],"about_ca_topic_score_codex":0.07889742,"about_ca_topic_score_gemma":0.05086358,"teacher_disagreement_score":0.9211026,"about_ca_system_score_codex":0.0019328541,"about_ca_system_score_gemma":0.0009267062,"threshold_uncertainty_score":0.15687639},"labels":[],"label_agreement":null},{"id":"W2964983675","doi":"10.1029/2019gl083169","title":"Changes in HCFC Emissions in China During 2011–2017","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China; University of Bristol; National Aeronautics and Space Administration","keywords":"Environmental science; Atmospheric sciences; China; Climatology; Emission inventory; Ozone; Meteorology; Geography; Geology; Air quality index","score_opus":0.02562704298942771,"score_gpt":0.28608671906346367,"score_spread":0.260459676074036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2964983675","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9946392,0.00015592216,0.00026647508,0.000052070023,0.000009704179,0.000007905387,0.0037090054,0.000028166389,0.0011316916],"genre_scores_gemma":[0.99224246,0.00023203352,0.00022291327,0.000028890852,0.000012678021,0.000015922104,0.0061500682,0.000006434327,0.0010887106],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998017,0.00001066286,0.000015699463,0.000053888147,0.00007029949,0.000047745623],"domain_scores_gemma":[0.99974424,0.00002005083,0.000055927645,0.00001614002,0.00013720902,0.000026490477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032701733,0.00047196733,0.00024730666,0.0014686036,0.00042594975,0.0004848202,0.00022212157,0.0002443339,0.00076459284],"category_scores_gemma":[0.0002961033,0.0001578939,0.00053910026,0.002137067,0.00020828188,0.00037726315,0.00043300015,0.0001550236,0.00016683387],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014834313,0.00005601538,0.95152086,0.00018733954,0.0003343911,0.00042319862,0.0005531679,0.01167006,0.008354533,0.0004549018,0.002696132,0.02360103],"study_design_scores_gemma":[0.000004456316,0.000017596269,0.9905284,0.000009867921,0.000054873122,0.000046744903,0.00017268317,0.0049292836,0.0017196662,0.000046646444,0.0024521141,0.000017586572],"about_ca_topic_score_codex":0.15557824,"about_ca_topic_score_gemma":0.1367762,"teacher_disagreement_score":0.15557824,"about_ca_system_score_codex":0.0018842188,"about_ca_system_score_gemma":0.0018195619,"threshold_uncertainty_score":0.30934536},"labels":[],"label_agreement":null},{"id":"W2965378851","doi":"10.1029/2019gl083525","title":"The Groundwater Recovery Paradox in South India","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Water resources management and optimization","field":"Engineering","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"University of Waterloo","keywords":"Groundwater; Environmental science; Water resource management; Odds; Groundwater resources; Resource (disambiguation); Hydrology (agriculture); Aquifer; Geology; Statistics; Mathematics; Computer science","score_opus":0.014800981311180052,"score_gpt":0.2347188529048653,"score_spread":0.21991787159368525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965378851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9788987,0.0004212903,0.0010736558,0.011894548,0.000016761009,0.0000062774584,0.00036848363,0.00006967747,0.007250557],"genre_scores_gemma":[0.9996369,0.00006413576,0.00004887723,0.00013003088,0.000004201894,0.0000015180418,0.000030547642,0.0000024032897,0.00008143685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994542,0.00017510762,0.00002958398,0.00007520347,0.00011908004,0.0001469587],"domain_scores_gemma":[0.99536645,0.0022123605,0.0013592147,0.00032621616,0.00046605922,0.00026964792],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008439541,0.00009717154,0.00036452213,0.0015390986,0.0009976955,0.0018019181,0.0006632724,0.00038979985,0.0018450526],"category_scores_gemma":[0.005037466,0.00013018132,0.00019251437,0.0038751792,0.0022560735,0.0009817624,0.001995836,0.0009231024,0.00010240975],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082475814,0.00023219154,0.6564103,0.00067043153,0.0003539813,0.008724693,0.013495013,0.048140038,0.0051255478,0.15231358,0.02644044,0.08726903],"study_design_scores_gemma":[0.000067962654,0.00010508368,0.72017866,0.0001702889,0.00011372227,0.0025962775,0.04821311,0.035411634,0.0018098718,0.17700416,0.014154817,0.0001743069],"about_ca_topic_score_codex":0.043764886,"about_ca_topic_score_gemma":0.047349587,"teacher_disagreement_score":0.043764886,"about_ca_system_score_codex":0.00233923,"about_ca_system_score_gemma":0.0014690295,"threshold_uncertainty_score":0.08702028},"labels":[],"label_agreement":null},{"id":"W2965411683","doi":"10.1029/2019gl083788","title":"Visibility and Line‐of‐Sight Extinction Estimates in Gale Crater During the 2018/MY34 Global Dust Storm","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"","keywords":"Impact crater; Environmental science; Extinction (optical mineralogy); Dust storm; Atmospheric sciences; Storm; Visibility; Geology; Climatology; Meteorology; Physics; Oceanography; Astronomy; Mineralogy","score_opus":0.02402115992711142,"score_gpt":0.2964071307909277,"score_spread":0.2723859708638163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965411683","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991289,0.000017147984,0.00003903982,0.000009003227,0.0000013714011,0.0000023989003,0.00034440693,0.000008709898,0.00044896908],"genre_scores_gemma":[0.9990631,0.000018305831,0.000103772625,0.000006175948,0.0000031543382,0.0000032086966,0.00065254903,0.0000034813531,0.00014633391],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999188,0.000008655368,0.0000043170553,0.00002160575,0.000022511422,0.000024099278],"domain_scores_gemma":[0.999728,0.000035707773,0.000074904005,0.00001975057,0.000082185186,0.000059294194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014964551,0.00021713701,0.00015031752,0.00083465147,0.00022617543,0.00040680685,0.00019005146,0.00021714841,0.0008068979],"category_scores_gemma":[0.0005042739,0.000112135356,0.00012561031,0.0003649987,0.00017120532,0.0001949538,0.0003562662,0.00019714386,0.00020216394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002346302,0.000043923006,0.9857406,0.000016116126,0.00004214269,0.00020290492,0.00060520845,0.00051119353,0.006015823,0.000034162254,0.00065508287,0.0058982205],"study_design_scores_gemma":[0.0000019942665,0.000012844193,0.9993331,0.0000022159563,0.0000028268385,0.000024286544,0.00009519492,0.00022751404,0.00014711224,0.000003131422,0.00014849502,0.0000013976154],"about_ca_topic_score_codex":0.0309167,"about_ca_topic_score_gemma":0.05153697,"teacher_disagreement_score":0.0309167,"about_ca_system_score_codex":0.00029696614,"about_ca_system_score_gemma":0.0000995719,"threshold_uncertainty_score":0.06147349},"labels":[],"label_agreement":null},{"id":"W2965752768","doi":"10.1029/2019gl083646","title":"Single‐Column Emulation of Reanalysis of the Northeast Pacific Marine Boundary Layer","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Department of Energy","keywords":"Emulation; Boundary layer; Realization (probability); Climatology; Environmental science; Meteorology; Radiative transfer; Boundary (topology); Geology; Physics; Optics; Mechanics; Mathematics","score_opus":0.03352831923155234,"score_gpt":0.28109296975197456,"score_spread":0.24756465052042223,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2965752768","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97625524,0.00007573187,0.018897062,0.0000963061,0.0000800075,0.00002642081,0.000991933,0.00069414434,0.0028831677],"genre_scores_gemma":[0.9965473,0.000015853171,0.0025385984,0.000010187031,0.000004901468,0.000012356604,0.0004043245,0.000016311466,0.0004501187],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999933,0.00001618151,0.0000036023832,0.000022770977,0.00001546771,0.000008957815],"domain_scores_gemma":[0.9997738,0.00007961469,0.000025205993,0.000032355412,0.00007355415,0.000015540354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002778897,0.00042377063,0.0002165742,0.00020023118,0.00016466017,0.0002851001,0.00042718143,0.00038372978,0.0014209476],"category_scores_gemma":[0.00072776224,0.00021610144,0.0003170738,0.0002024116,0.00019338679,0.00039437163,0.00013597927,0.00038997282,0.00021039601],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032871736,0.00002437298,0.0033661271,0.00000926019,0.000030114817,0.000017705614,0.000009577713,0.9877529,0.0014456174,0.00009859608,0.0003124571,0.0069003953],"study_design_scores_gemma":[0.0000048531424,0.000009469985,0.0020157353,0.0000012599785,0.0000031551644,0.0000016831298,0.000002639519,0.997177,0.00067580066,0.000039265404,0.000066403365,0.0000027654878],"about_ca_topic_score_codex":0.031148255,"about_ca_topic_score_gemma":0.022557456,"teacher_disagreement_score":0.031148255,"about_ca_system_score_codex":0.00047675482,"about_ca_system_score_gemma":0.00044289642,"threshold_uncertainty_score":0.061933875},"labels":[],"label_agreement":null},{"id":"W2966526791","doi":"10.1029/2019gl083849","title":"ULF Waves Modulating and Acting as Mass Spectrometer for Dayside Ionospheric Outflow Ions","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Goddard Space Flight Center; National Natural Science Foundation of China","keywords":"Magnetosphere; Outflow; Ionosphere; Physics; Geophysics; Polarization (electrochemistry); Ion; Computational physics; Atmospheric sciences; Plasma; Meteorology; Chemistry; Nuclear physics","score_opus":0.01696823466840396,"score_gpt":0.2933196764168515,"score_spread":0.27635144174844756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2966526791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936912,0.00044940092,0.0020347899,0.00011890191,0.00003579659,0.000010104137,0.00043711983,0.00006964843,0.003152918],"genre_scores_gemma":[0.99783725,0.00011133758,0.0012263871,0.000059143065,0.000023541736,0.0000062511413,0.00020698884,0.000014851763,0.00051423314],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993646,0.0000055720975,0.0000020688378,0.000017735789,0.000018469145,0.000019695208],"domain_scores_gemma":[0.99989426,0.000019104726,0.000041802403,0.000009720439,0.000019912888,0.000015191664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010148012,0.00020798857,0.00012843404,0.00047855996,0.00021105404,0.00031220986,0.00016460476,0.00029531223,0.0009743148],"category_scores_gemma":[0.00021491089,0.00007835162,0.00011131248,0.0002927523,0.00018864649,0.0002927506,0.00032820512,0.00028530162,0.00015777454],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005253403,0.00004663283,0.1455603,0.00009684753,0.00004067803,0.00035423564,0.00039108004,0.00023489253,0.8198193,0.00062188436,0.0011245321,0.031184372],"study_design_scores_gemma":[0.000033750188,0.00024691093,0.86312455,0.000053964082,0.00006286931,0.0007049324,0.00057719427,0.0038932161,0.12306618,0.00088553806,0.007319823,0.000031031464],"about_ca_topic_score_codex":0.00058596255,"about_ca_topic_score_gemma":0.000898066,"teacher_disagreement_score":0.0009743148,"about_ca_system_score_codex":0.00013327124,"about_ca_system_score_gemma":0.000060997503,"threshold_uncertainty_score":0.0032594204},"labels":[],"label_agreement":null},{"id":"W2967318772","doi":"10.1029/2019gl083547","title":"The Ocean CO<sub>2</sub> Sink in the Canadian Arctic Archipelago: A Present‐Day Budget and Past Trends Due to Climate Change","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Faculty of Arts, University of Calgary; Social Sciences and Humanities Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; Chinese Academy of Agricultural Sciences; Canadian HIV Trials Network, Canadian Institutes of Health Research; Networks of Centres of Excellence of Canada; ArcticNet","keywords":"Arctic; Sink (geography); Environmental science; Arctic sea ice decline; Sea ice; Archipelago; Climatology; Arctic dipole anomaly; Arctic geoengineering; Arctic ice pack; Oceanography; Open water; Atmospheric sciences; Antarctic sea ice; Geology; Geography","score_opus":0.019783936247242045,"score_gpt":0.2566834222273424,"score_spread":0.23689948598010038,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967318772","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886869,0.0009373414,0.00055855,0.00033667978,0.000019924222,0.000011494573,0.0067206654,0.000059241684,0.0026691933],"genre_scores_gemma":[0.99579865,0.0005508977,0.00050691457,0.00005369963,0.000007657069,0.00000471894,0.0023555525,0.000014312929,0.0007075954],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999083,0.0000031399793,0.000004852968,0.000021017038,0.000036861293,0.000025801548],"domain_scores_gemma":[0.9996014,0.000016403905,0.000050804887,0.000013666127,0.00027297766,0.000044737986],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026407666,0.00044521372,0.00021497648,0.0017219383,0.0009949598,0.0010562405,0.00039301507,0.00026158706,0.0009410841],"category_scores_gemma":[0.00041927464,0.00015334379,0.00034444823,0.0020045035,0.0004018722,0.00058144593,0.00035346622,0.00030019018,0.00012014884],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001330829,0.000032979307,0.9600361,0.00011230777,0.00028565218,0.00007907116,0.00020106345,0.010140668,0.0068307836,0.00063059514,0.0029498306,0.018567914],"study_design_scores_gemma":[0.0000037751745,0.0000039137476,0.9905421,0.000015377473,0.000048997746,0.000018927516,0.00014197006,0.00605253,0.0007402636,0.000092608025,0.0023247753,0.000014713153],"about_ca_topic_score_codex":0.9731425,"about_ca_topic_score_gemma":0.98053414,"teacher_disagreement_score":0.026857495,"about_ca_system_score_codex":0.009208526,"about_ca_system_score_gemma":0.0070295865,"threshold_uncertainty_score":0.06681287},"labels":[],"label_agreement":null},{"id":"W2967376008","doi":"10.1029/2019gl082873","title":"Contrasting Ice Algae and Snow‐Dependent Irradiance Relationships Between First‐Year and Multiyear Sea Ice","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba; Bedford Institute of Oceanography; York University; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research; Bundesministerium für Bildung und Forschung","keywords":"Snow; Sea ice; Arctic ice pack; Melt pond; Environmental science; Cryosphere; Arctic; Ice core; Algae; Oceanography; Antarctic sea ice; Geology; Atmospheric sciences; Geomorphology; Ecology; Biology","score_opus":0.03636160054011698,"score_gpt":0.2633451991150196,"score_spread":0.2269835985749026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2967376008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99977523,0.00001543053,0.000027081427,0.0000028137772,5.5104925e-7,6.2426466e-7,0.000073634474,9.652373e-7,0.00010368657],"genre_scores_gemma":[0.9996183,0.000009233514,0.00005172836,0.0000038088865,0.000001079591,0.0000021578082,0.00023706368,0.0000013412837,0.00007529117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.000009868959,0.0000039938586,0.000021400689,0.000012039162,0.000020161686],"domain_scores_gemma":[0.9995493,0.00010910351,0.00014953254,0.000017866083,0.00008860093,0.000085497275],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024895585,0.00012549633,0.00022174067,0.0005098687,0.00029970147,0.00046722937,0.00013720882,0.0001547579,0.000536566],"category_scores_gemma":[0.00057646557,0.00013014421,0.00014777729,0.00032164654,0.0001720135,0.00027782482,0.00033547403,0.00020866672,0.00009544021],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099011704,0.000021658083,0.9920094,0.0000052158657,0.00002115002,0.000021254617,0.00016037868,0.00012286978,0.0059915828,0.000016556934,0.000040838004,0.0014901517],"study_design_scores_gemma":[4.7398314e-7,0.000011620587,0.9995592,5.9575666e-7,0.0000016461657,0.000008393535,0.00007074678,0.00010858267,0.00020511869,0.0000036032354,0.000029335262,6.738721e-7],"about_ca_topic_score_codex":0.011171635,"about_ca_topic_score_gemma":0.036008563,"teacher_disagreement_score":0.011171635,"about_ca_system_score_codex":0.00039336647,"about_ca_system_score_gemma":0.0001795326,"threshold_uncertainty_score":0.02221322},"labels":[],"label_agreement":null},{"id":"W2968399039","doi":"10.1029/2019gl084204","title":"Radiative Control of the Interannual Variability of Arctic Sea Ice","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Mitacs","keywords":"Albedo (alchemy); Climatology; Environmental science; Sea ice; Shortwave radiation; Shortwave; Arctic; Arctic ice pack; Longwave; Outgoing longwave radiation; Atmospheric sciences; Arctic sea ice decline; Ice-albedo feedback; Radiative transfer; Radiation; Sea ice thickness; Geology; Oceanography; Meteorology; Geography","score_opus":0.011156111130766783,"score_gpt":0.2508478121156221,"score_spread":0.23969170098485534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2968399039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99701357,0.00013013888,0.0009251647,0.000053185813,0.000013004541,0.000002058198,0.00015541237,0.000032179152,0.0016752401],"genre_scores_gemma":[0.99961996,0.000032216598,0.0000942608,0.000005514991,0.000009049532,0.000001349746,0.000092248556,0.0000066707985,0.00013876201],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999323,0.000017925127,0.000004103038,0.000020429967,0.000012442071,0.000012905692],"domain_scores_gemma":[0.99966633,0.00010178538,0.0000893332,0.000037003138,0.000074303185,0.000031145682],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031985887,0.00019163456,0.00014915019,0.00034484843,0.00015982869,0.00050176267,0.00015041775,0.00012241365,0.00060018105],"category_scores_gemma":[0.000726669,0.000107195825,0.00015486198,0.00024690284,0.00014504428,0.0002038868,0.00024203036,0.0001543157,0.00012770608],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004639137,0.00024069705,0.7144938,0.000056336732,0.00029663515,0.00026303699,0.00027129948,0.062531605,0.1749891,0.0027030609,0.0016054306,0.042085066],"study_design_scores_gemma":[0.000010356281,0.00004008052,0.9467163,0.0000061871856,0.000019471414,0.00006746642,0.00006500972,0.046786282,0.004342776,0.00082853803,0.0011050929,0.000012349337],"about_ca_topic_score_codex":0.0031998144,"about_ca_topic_score_gemma":0.0031435292,"teacher_disagreement_score":0.0031998144,"about_ca_system_score_codex":0.00022658835,"about_ca_system_score_gemma":0.00015215413,"threshold_uncertainty_score":0.0063623786},"labels":[],"label_agreement":null},{"id":"W2969388886","doi":"10.1029/2019gl082764","title":"Mars Science Laboratory Observations of Chloride Salts in Gale Crater, Mars","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"California Institute of Technology; National Aeronautics and Space Administration; National Science Foundation","keywords":"Halite; Geology; Mars Exploration Program; Geochemistry; Sedimentary rock; Impact crater; Evaporite; Diagenesis; Aeolian processes; Mineralogy; Astrobiology; Geomorphology","score_opus":0.04128858248796609,"score_gpt":0.30320421402784703,"score_spread":0.26191563153988096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969388886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99692553,0.000112161535,0.000111506786,0.00007138824,0.0000048379693,0.00000996574,0.0007366734,0.00009411383,0.0019338374],"genre_scores_gemma":[0.99760336,0.00006152969,0.0006447583,0.000035776666,0.000011609557,0.000009509355,0.0006905896,0.00001440231,0.00092846126],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998789,0.000015155543,0.0000049892624,0.000034807705,0.000046317924,0.000019798967],"domain_scores_gemma":[0.9998055,0.000016641108,0.00004762184,0.00001592935,0.000067794615,0.00004644049],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014937094,0.00031925229,0.0001974486,0.0017350453,0.00073058583,0.0006134038,0.00036239292,0.00046658624,0.0013208966],"category_scores_gemma":[0.00027108585,0.00017688372,0.00018345,0.0005313661,0.00027246046,0.00027821073,0.0005739948,0.00026433813,0.00038257026],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075845805,0.00009330027,0.73713744,0.00008697661,0.00017874187,0.0014565625,0.0015555175,0.0015696976,0.22528824,0.00016704373,0.0033818407,0.02832626],"study_design_scores_gemma":[0.00003651084,0.0002023082,0.9860487,0.000009892853,0.000020325297,0.0002507412,0.00033482144,0.00096164685,0.0068361866,0.000030646384,0.005252998,0.000015208462],"about_ca_topic_score_codex":0.015242543,"about_ca_topic_score_gemma":0.024085913,"teacher_disagreement_score":0.015242543,"about_ca_system_score_codex":0.0004878576,"about_ca_system_score_gemma":0.00022066043,"threshold_uncertainty_score":0.03030765},"labels":[],"label_agreement":null},{"id":"W2969916003","doi":"10.1029/2019gl083800","title":"The Methane Diurnal Variation and Microseepage Flux at Gale Crater, Mars as Constrained by the ExoMars Trace Gas Orbiter and Curiosity Observations","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Science Mission Directorate; Canadian Space Agency; Universities Space Research Association; National Aeronautics and Space Administration","keywords":"Orbiter; Mars Exploration Program; Methane; Impact crater; Flux (metallurgy); Atmosphere of Mars; Environmental science; Astrobiology; Mixing ratio; Daytime; Trace gas; Atmospheric sciences; Volume (thermodynamics); Geology; Martian; Physics; Chemistry; Astronomy","score_opus":0.026397236564715827,"score_gpt":0.2741418733369906,"score_spread":0.24774463677227476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2969916003","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998585,0.00003838138,0.00033959895,0.00003926246,0.0000023416608,0.00000188006,0.00036532877,0.00003727153,0.00059088913],"genre_scores_gemma":[0.9995653,0.000018221792,0.00014478792,0.0000050208178,0.0000026902453,0.000002762355,0.00018883779,0.000004451398,0.000067850706],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.000013693238,0.0000022042427,0.000020138912,0.000011559103,0.000014388938],"domain_scores_gemma":[0.99982244,0.000053699037,0.000040400748,0.000027103946,0.000021551401,0.00003482473],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017657787,0.00026627647,0.00012784204,0.00045079942,0.00024499008,0.00036205744,0.00020896716,0.00038044248,0.00072541175],"category_scores_gemma":[0.00042635397,0.00017314713,0.00022959754,0.0002575272,0.00022018419,0.0003382481,0.00033257002,0.00019327877,0.00012292704],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007823478,0.00006679501,0.89812696,0.000053063974,0.0001999949,0.0003744787,0.0005745296,0.017904986,0.067022935,0.0006416493,0.0009582906,0.013293919],"study_design_scores_gemma":[0.000016076523,0.00003980473,0.9809373,0.000005658609,0.000014509724,0.00006214011,0.00010064179,0.014048409,0.0038758153,0.000112836926,0.0007743573,0.000012460635],"about_ca_topic_score_codex":0.009801645,"about_ca_topic_score_gemma":0.0106241945,"teacher_disagreement_score":0.009801645,"about_ca_system_score_codex":0.00021617438,"about_ca_system_score_gemma":0.000107637396,"threshold_uncertainty_score":0.019489229},"labels":[],"label_agreement":null},{"id":"W2970692350","doi":"10.1029/2019gl083975","title":"Impacts of Climate Change on Volcanic Stratospheric Injections: Comparison of 1‐D and 3‐D Plume Model Projections","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Horizon 2020 Framework Programme; Istituto Nazionale di Geofisica e Vulcanologia; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Royal Society; National Science Foundation","keywords":"Stratosphere; Volcano; Troposphere; Plume; Atmospheric sciences; Environmental science; Climatology; Climate change; Climate model; Explosive eruption; Geology; Meteorology; Geography; Magma; Seismology","score_opus":0.07980952104197851,"score_gpt":0.3581218396077967,"score_spread":0.2783123185658182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970692350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912027,0.00011556216,0.0030785806,0.00029826153,0.000026815953,0.000018038541,0.0028392565,0.0002844468,0.0021363993],"genre_scores_gemma":[0.99688256,0.0000686107,0.0015003431,0.000042025484,0.000008245861,0.000023113607,0.0012886801,0.000030259142,0.00015628277],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998166,0.0000685132,0.000013986591,0.00003921084,0.000022029108,0.000039682807],"domain_scores_gemma":[0.99910396,0.00042227725,0.00010411679,0.00010662031,0.00015860706,0.00010434512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00095138606,0.0006552331,0.0005648903,0.00056432985,0.0004430457,0.00095442485,0.00079268636,0.0012855264,0.0014795201],"category_scores_gemma":[0.0016320632,0.00042674536,0.0016045406,0.00067567837,0.00035977433,0.00074650155,0.00045033725,0.00088355213,0.00021409281],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010295526,0.00006298038,0.015172492,0.000014758894,0.000112226924,0.00003708737,0.00002537595,0.9815531,0.0008363286,0.00044586518,0.00030331395,0.0013334136],"study_design_scores_gemma":[0.00005919485,0.000044295757,0.010758708,0.000005914674,0.000037517464,0.0000163864,0.000036545447,0.9875266,0.00063590496,0.0005597167,0.0002907031,0.000028511202],"about_ca_topic_score_codex":0.061139118,"about_ca_topic_score_gemma":0.026606586,"teacher_disagreement_score":0.061139118,"about_ca_system_score_codex":0.0011344072,"about_ca_system_score_gemma":0.0009643992,"threshold_uncertainty_score":0.121566474},"labels":[],"label_agreement":null},{"id":"W2970762295","doi":"10.1029/2019gl083406","title":"Quantifying Fracture Networks Inferred From Microseismic Point Clouds by a Gaussian Mixture Model With Physical Constraints","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Canada First Research Excellence Fund","keywords":"Microseism; Hydraulic fracturing; Geology; Induced seismicity; Cluster analysis; Point process; Fracture (geology); Seismology; Slip (aerodynamics); Computer science; Geotechnical engineering; Artificial intelligence; Statistics","score_opus":0.014853387849000702,"score_gpt":0.26898691560459287,"score_spread":0.25413352775559217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970762295","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.40044868,0.000115955125,0.5975193,0.0001579723,0.000009035724,0.000049570528,0.0006201844,0.0004167825,0.0006625591],"genre_scores_gemma":[0.91087633,0.000049201102,0.0882259,0.000016465116,0.000010191143,0.00003632217,0.0004704387,0.00003161611,0.0002836544],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997099,0.00005679424,0.000014742385,0.00007939382,0.000099261975,0.00003978702],"domain_scores_gemma":[0.99893874,0.0004957095,0.0001932436,0.0001139232,0.00020475904,0.000053684435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00094926497,0.00043250408,0.00036434495,0.0020486582,0.00039429156,0.0007639003,0.0009255048,0.00074641156,0.00042772805],"category_scores_gemma":[0.0026953288,0.0003612522,0.00064155855,0.0013380712,0.0006249999,0.0007818398,0.0008013784,0.000536054,0.00014184309],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000066351604,0.00004984323,0.03762714,0.000034486762,0.000071943934,0.000054857053,0.00010155633,0.91727173,0.006278192,0.0034081796,0.0004056967,0.03463],"study_design_scores_gemma":[0.0000015461252,0.0000025248332,0.00433439,0.0000023084128,0.0000029101893,0.000006901329,0.000012712421,0.9944178,0.00038004908,0.00076742674,0.00006552709,0.000006045127],"about_ca_topic_score_codex":0.061482467,"about_ca_topic_score_gemma":0.079229854,"teacher_disagreement_score":0.061482467,"about_ca_system_score_codex":0.0011236384,"about_ca_system_score_gemma":0.0011488682,"threshold_uncertainty_score":0.122249186},"labels":[],"label_agreement":null},{"id":"W2970775993","doi":"10.1029/2019gl084611","title":"Constraining the Source Regions of Pulsating Auroras","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Magnetosphere; Physics; Geophysics; Proton; Magnetosheath; Astrophysics; Geology; Plasma; Magnetopause; Nuclear physics","score_opus":0.021681842092279024,"score_gpt":0.291498943438552,"score_spread":0.26981710134627296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2970775993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95170015,0.0011555989,0.03466529,0.00018074186,0.000049939634,0.000032638338,0.0017648798,0.00042567102,0.010025021],"genre_scores_gemma":[0.9874373,0.00026093077,0.0098719755,0.000051898583,0.0000338174,0.000024623596,0.0019087108,0.00010324634,0.00030741285],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99982244,0.000023025998,0.000010814362,0.00007741338,0.000022828097,0.000043430155],"domain_scores_gemma":[0.99919385,0.0003102023,0.0001793631,0.00014491408,0.00009893192,0.000072659204],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003981886,0.00032819825,0.00047097923,0.0011096991,0.00058185926,0.0014141378,0.00030458803,0.00032427817,0.0018552126],"category_scores_gemma":[0.0018976299,0.00026032265,0.00030225416,0.0012897354,0.00030227174,0.0005728277,0.0011748262,0.0006402624,0.0006899412],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004832878,0.0000740943,0.74471194,0.0003303109,0.00023317065,0.00044670052,0.00093498646,0.010926534,0.14995167,0.0041969535,0.0030249506,0.08468534],"study_design_scores_gemma":[0.000054917986,0.00005222625,0.93260217,0.00008014079,0.00020110093,0.0003885471,0.00047530892,0.020020181,0.018652162,0.0038138626,0.023604503,0.000054893168],"about_ca_topic_score_codex":0.0051973993,"about_ca_topic_score_gemma":0.0049603735,"teacher_disagreement_score":0.0051973993,"about_ca_system_score_codex":0.00021296003,"about_ca_system_score_gemma":0.00041228198,"threshold_uncertainty_score":0.010334313},"labels":[],"label_agreement":null},{"id":"W2971385441","doi":"10.1029/2019gl083321","title":"Preservation of Cyanobacterial UVR‐Shielding Pigment Scytonemin in Carbonate Ooids Formed in Pleistocene Salt Lakes in the Qaidam Basin, Tibetan Plateau","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Biocrusts and Microbial Ecology","field":"Agricultural and Biological Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Research Grants Council, University Grants Committee; National Natural Science Foundation of China","keywords":"Geology; Aragonite; Ooid; Halite; Gypsum; Evaporite; Geochemistry; Carbonate; Sedimentary depositional environment; Paleontology; Structural basin; Sedimentary rock; Calcite","score_opus":0.029727563478897257,"score_gpt":0.2697213774694965,"score_spread":0.23999381399059921,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971385441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99969983,0.000057909623,0.00004290672,0.00000411843,7.742419e-7,9.790042e-7,0.000037159305,0.000002449027,0.0001539601],"genre_scores_gemma":[0.9996043,0.000032538635,0.00010871077,0.0000064593814,0.0000014192789,0.0000015010113,0.00007269189,0.000001928425,0.00017046655],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994886,0.000004474528,0.0000037086152,0.000017837701,0.000012949908,0.000012194199],"domain_scores_gemma":[0.99991596,0.00000812795,0.000025932934,0.0000037175228,0.000024748351,0.000021413563],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015142711,0.00021675786,0.00015787191,0.00087906665,0.00057201204,0.00047417352,0.00016712587,0.0002580667,0.000682471],"category_scores_gemma":[0.00012914103,0.00020389048,0.00011757406,0.00048489228,0.0004838841,0.00025505188,0.0002872832,0.00018638813,0.00009345528],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018893769,0.00002201684,0.6373496,0.00007004749,0.00005311281,0.00029445512,0.0013546601,0.0002897615,0.35572127,0.000080382335,0.000053260264,0.0045224084],"study_design_scores_gemma":[0.000002707208,0.000019753135,0.99652976,0.0000029066714,0.000005231495,0.000058036545,0.0003795652,0.00022736596,0.0026139806,0.000009462602,0.00014852127,0.000002726646],"about_ca_topic_score_codex":0.016963486,"about_ca_topic_score_gemma":0.032172594,"teacher_disagreement_score":0.016963486,"about_ca_system_score_codex":0.00047011473,"about_ca_system_score_gemma":0.0002454523,"threshold_uncertainty_score":0.033729494},"labels":[],"label_agreement":null},{"id":"W2971425974","doi":"10.1029/2019gl084568","title":"The Wavelength‐Dependent Complex Refractive Index of Hygroscopic Aerosol Particles and Other Aqueous Media: An Effective Oscillator Model","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Spectroscopy and Quantum Chemical Studies","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Refractive index; Aqueous solution; Wavelength; Aerosol; Raman spectroscopy; Materials science; Optics; Physics; Chemistry; Optoelectronics; Meteorology; Physical chemistry","score_opus":0.03043556161720838,"score_gpt":0.32862091944043087,"score_spread":0.2981853578232225,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971425974","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.13687661,0.0006917331,0.8450741,0.0005279325,0.00011766238,0.00009059613,0.00017075849,0.00017195208,0.016278658],"genre_scores_gemma":[0.91705567,0.0013326426,0.05987325,0.00032397517,0.00015809342,0.00027435695,0.0001638832,0.00017081168,0.020647395],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997812,0.00004862127,0.0000059698937,0.00004690229,0.00009041688,0.000026857593],"domain_scores_gemma":[0.99953854,0.00022575482,0.00007315988,0.000053020925,0.00007701304,0.000032621287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005272942,0.0008737127,0.00046224915,0.0007176286,0.00035992204,0.0007113035,0.0017070196,0.0009321678,0.0016652311],"category_scores_gemma":[0.0012103878,0.0003636797,0.000634842,0.00033245084,0.0012184265,0.0020979652,0.00070523185,0.0007824104,0.00044025047],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052257205,0.00015626829,0.0013537713,0.00014425952,0.000064413136,0.0005099755,0.0002695988,0.44192544,0.10055509,0.44212243,0.0012991718,0.011547327],"study_design_scores_gemma":[0.000009471779,0.000022215621,0.00018121568,0.0000062183112,0.000008943726,0.000048550504,0.000014506886,0.9733546,0.0026989242,0.022789039,0.0008459408,0.000020424965],"about_ca_topic_score_codex":0.0016110583,"about_ca_topic_score_gemma":0.0010965122,"teacher_disagreement_score":0.0017070196,"about_ca_system_score_codex":0.0006066993,"about_ca_system_score_gemma":0.00073809293,"threshold_uncertainty_score":0.0055707693},"labels":[],"label_agreement":null},{"id":"W2971551468","doi":"10.1029/2019gl083831","title":"A Multimodel Approach for Improving Seasonal Probabilistic Forecasts of Regional Arctic Sea Ice","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Université du Québec à Montréal","funders":"","keywords":"Forecast skill; Climatology; Predictability; Probabilistic logic; Environmental science; Arctic; Calibration; Sea ice; Quantile; Ensemble average; The arctic; Benchmark (surveying); Arctic ice pack; Climate model; Meteorology; Climate change; Statistics; Mathematics; Geography; Geology; Oceanography; Geodesy","score_opus":0.03851375957625526,"score_gpt":0.2689104374822022,"score_spread":0.23039667790594698,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971551468","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1606719,0.00028162863,0.8344251,0.0004369481,0.000091380956,0.00004348461,0.0006850847,0.00086422387,0.0025003557],"genre_scores_gemma":[0.88073426,0.00014671155,0.11715476,0.0001329084,0.00009543452,0.000080396516,0.000701379,0.00010186767,0.00085236],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99973613,0.00011632596,0.00001833377,0.00005560496,0.000044808407,0.00002880011],"domain_scores_gemma":[0.99921143,0.00042303032,0.00009908927,0.000078533245,0.00014999823,0.00003792477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013699157,0.0004975036,0.00042605962,0.00056290085,0.00026389293,0.0006121137,0.0007001915,0.00052425766,0.0011649339],"category_scores_gemma":[0.0029907282,0.00040796594,0.0007092306,0.0004435276,0.00020020694,0.0006672744,0.00066195324,0.0006475276,0.00017866184],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000016486238,0.000015858623,0.0012947054,0.000009558698,0.00004311018,0.000014255654,0.0000092383425,0.983223,0.0007223454,0.001080509,0.00026220753,0.013308677],"study_design_scores_gemma":[0.0000022240063,0.0000054656803,0.00023430675,0.0000013175469,0.0000026588946,0.0000015354213,0.0000015351256,0.99877125,0.00015115246,0.0007177182,0.00010822601,0.00000262308],"about_ca_topic_score_codex":0.015545632,"about_ca_topic_score_gemma":0.01544395,"teacher_disagreement_score":0.015545632,"about_ca_system_score_codex":0.00055894296,"about_ca_system_score_gemma":0.00094857113,"threshold_uncertainty_score":0.030910313},"labels":[],"label_agreement":null},{"id":"W2971636029","doi":"10.1029/2019gl084536","title":"A Model of Shallow Viscoelastic Relaxation for Seismically Induced Tension Cracks in the Chile‐Peru Forearc","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Forearc; Geology; Tension (geology); Seismology; Crust; Submarine pipeline; Deformation (meteorology); Relaxation (psychology); Viscoelasticity; Subduction; Geotechnical engineering; Geophysics; Tectonics; Materials science; Compression (physics); Composite material","score_opus":0.06215352900652295,"score_gpt":0.2953673109117366,"score_spread":0.2332137819052137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971636029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93483573,0.00045255604,0.03382152,0.0018594094,0.000047006393,0.000079941965,0.0005335686,0.00026192618,0.02810838],"genre_scores_gemma":[0.9944305,0.0001267979,0.0007878153,0.0000408398,0.000009782566,0.000048951937,0.000050005383,0.000019489198,0.004485738],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999372,0.00001835921,0.000002740968,0.000014434433,0.0000072836406,0.000020054506],"domain_scores_gemma":[0.9997594,0.00008024677,0.000056113935,0.0000149763855,0.000038331465,0.000050895702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002385517,0.00040699285,0.00040776623,0.00046864757,0.00072372175,0.00089386763,0.0014632208,0.002387583,0.005310691],"category_scores_gemma":[0.0007568629,0.00045229128,0.00058375316,0.00032838574,0.000982995,0.0008678094,0.0006986434,0.00064712064,0.00034378355],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010004123,0.000096205775,0.0033294917,0.000049981772,0.000027403901,0.00068315456,0.00016203396,0.9715973,0.005382587,0.016350584,0.0008593311,0.0013618765],"study_design_scores_gemma":[0.000038605045,0.000028757948,0.0007779526,0.0000055942196,0.0000066580214,0.00003303737,0.000044802542,0.99729246,0.000085428546,0.0014188765,0.00025813282,0.000009778643],"about_ca_topic_score_codex":0.031098662,"about_ca_topic_score_gemma":0.011167585,"teacher_disagreement_score":0.031098662,"about_ca_system_score_codex":0.0013405528,"about_ca_system_score_gemma":0.00082681054,"threshold_uncertainty_score":0.06183529},"labels":[],"label_agreement":null},{"id":"W2971791208","doi":"10.1029/2019gl084473","title":"The Vertical Distribution of the Optical Emissions of a Steve and Picket Fence Event","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Government of Alberta; University of Calgary; University of Saskatchewan","funders":"","keywords":"Picketing; Fence (mathematics); Altitude (triangle); Geology; Event (particle physics); Physics; Law; Political science; Astrophysics; Engineering; Geometry","score_opus":0.010023939409258543,"score_gpt":0.27837272195693347,"score_spread":0.2683487825476749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2971791208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985864,0.000022591403,0.00006736222,0.000008704894,0.000001835191,0.0000018853738,0.00022318891,0.0000053253584,0.001082751],"genre_scores_gemma":[0.999331,0.00001865279,0.000095840376,0.0000035428575,0.0000035788262,0.0000017430682,0.00035193237,0.0000024266642,0.00019126396],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.0000051436937,0.0000028524341,0.000024016,0.000016234038,0.000028906346],"domain_scores_gemma":[0.9997719,0.000036596837,0.0000703493,0.00001385939,0.000045172015,0.00006213433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000090884954,0.0001197306,0.0001186949,0.0010369379,0.0003156869,0.00036299977,0.00018275113,0.0002631357,0.0014471366],"category_scores_gemma":[0.00027389842,0.00009450388,0.0001035452,0.000532226,0.00023478366,0.0002137367,0.00043849347,0.0001988376,0.00019237363],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045136752,0.00005918299,0.94459605,0.000024610725,0.000055956483,0.0006009315,0.0010039427,0.0005405007,0.039502144,0.00031686635,0.0005080766,0.012340349],"study_design_scores_gemma":[0.0000021533808,0.0000188418,0.9983935,0.000003738678,0.000003960802,0.000060160397,0.00030799815,0.00028220727,0.00054333906,0.000022342185,0.00035861184,0.0000030634328],"about_ca_topic_score_codex":0.008816775,"about_ca_topic_score_gemma":0.015703414,"teacher_disagreement_score":0.008816775,"about_ca_system_score_codex":0.0002588064,"about_ca_system_score_gemma":0.00011367405,"threshold_uncertainty_score":0.017530918},"labels":[],"label_agreement":null},{"id":"W2972211172","doi":"10.1029/2019gl084354","title":"Explanation for the Increase in High‐Altitude Water on Mars Observed by NOMAD During the 2018 Global Dust Storm","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"United Kingdom Space Agency; Agenzia Spaziale Italiana; Belgian Federal Science Policy Office","keywords":"Water vapor; Mars Exploration Program; Atmospheric sciences; Dust storm; Altitude (triangle); Atmosphere (unit); Environmental science; Atmosphere of Mars; Storm; Occultation; Trace gas; Orbiter; Nadir; Effects of high altitude on humans; Astrobiology; Geology; Martian; Meteorology; Physics; Satellite","score_opus":0.033134609895966914,"score_gpt":0.27718662836006214,"score_spread":0.24405201846409522,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972211172","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923018,0.00027503146,0.0022136196,0.0016908306,0.0000931003,0.000026762049,0.00081470754,0.00026422317,0.0023198435],"genre_scores_gemma":[0.999471,0.000033955956,0.00019797131,0.000032253854,0.000015448022,0.0000042138163,0.0001005235,0.00000834315,0.00013627678],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992526,0.00000990432,0.0000039085603,0.0000238773,0.000008866869,0.00002819727],"domain_scores_gemma":[0.99988556,0.000020008236,0.000029278088,0.000012532256,0.00001655386,0.000035967594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014225446,0.00042599704,0.0003275109,0.0003344807,0.0007327334,0.00053385284,0.00062352465,0.0014392924,0.0024400025],"category_scores_gemma":[0.00024240126,0.00031175537,0.00078050507,0.00021942073,0.00041110537,0.00046577147,0.00049565715,0.0005923302,0.00025587808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009574835,0.0005471539,0.7142041,0.0003161474,0.0005071814,0.0046389787,0.0006757415,0.1184737,0.12911136,0.008874809,0.009724556,0.011968762],"study_design_scores_gemma":[0.0005806909,0.00027435663,0.59657466,0.000039405302,0.00014711921,0.0005024241,0.00092152733,0.38166943,0.009219718,0.006023061,0.0039509167,0.000096742864],"about_ca_topic_score_codex":0.015090704,"about_ca_topic_score_gemma":0.009412736,"teacher_disagreement_score":0.015090704,"about_ca_system_score_codex":0.001018547,"about_ca_system_score_gemma":0.0003940522,"threshold_uncertainty_score":0.030005753},"labels":[],"label_agreement":null},{"id":"W2972251634","doi":"10.1029/2019gl084647","title":"Freezing Rain Events Related to Atmospheric Rivers and Associated Mechanisms for Western North America","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"","keywords":"Hydrometeorology; Climatology; Environmental science; Advection; Atmospheric sciences; Climate model; Western europe; Climate change; Precipitation; Oceanography; Geology; Meteorology; Geography","score_opus":0.021508963411556736,"score_gpt":0.28323066831861005,"score_spread":0.2617217049070533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972251634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947379,0.00037265563,0.0002631248,0.00028154106,0.00000980923,0.000016700676,0.0010798327,0.000055618028,0.0031827309],"genre_scores_gemma":[0.9985447,0.00025135532,0.00024045754,0.000039315993,0.000005900744,0.000008712911,0.0005298453,0.0000041630033,0.00037558938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995315,0.0000075051275,0.000003444083,0.000014601124,0.000009579652,0.000011705086],"domain_scores_gemma":[0.99981457,0.000017254226,0.000069900205,0.000011311626,0.000048198428,0.000038918202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001545827,0.00018872114,0.0001219517,0.00038029073,0.00032288532,0.00049557467,0.00025232093,0.00018916812,0.0019665651],"category_scores_gemma":[0.00029031164,0.0001031871,0.00029035786,0.00063532294,0.00015638804,0.00031451232,0.00031114725,0.00019102397,0.00007814851],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012131796,0.00006607528,0.9469624,0.000103898965,0.00021100455,0.000528286,0.00029148246,0.02316465,0.0045085973,0.0007653146,0.0035326725,0.01974422],"study_design_scores_gemma":[0.000024093164,0.000019676927,0.9753538,0.000024651536,0.000077931385,0.00005144612,0.00028529586,0.02109492,0.00043621947,0.00046551044,0.0021521086,0.000014476033],"about_ca_topic_score_codex":0.33935297,"about_ca_topic_score_gemma":0.37979043,"teacher_disagreement_score":0.33935297,"about_ca_system_score_codex":0.0009855072,"about_ca_system_score_gemma":0.0010586104,"threshold_uncertainty_score":0.67475545},"labels":[],"label_agreement":null},{"id":"W2972436466","doi":"10.1029/2019gl084485","title":"The Iron Invariance: Implications for Thermal Convection in Earth's Core","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; National Stroke Foundation; Canada Foundation for Innovation","keywords":"Dynamo theory; Inner core; Geophysics; Outer core; Convection; Thermal conductivity; Earth's magnetic field; Thermal; Core–mantle boundary; Natural convection; Heat flux; Electrical resistivity and conductivity; Geology; Thermodynamics; Mechanics; Heat transfer; Mantle (geology); Dynamo; Physics; Magnetic field","score_opus":0.02987074756421856,"score_gpt":0.3158077782369822,"score_spread":0.28593703067276366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972436466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943297,0.00018250257,0.0035696642,0.00012025135,0.0000065067056,0.0000034677055,0.00004440335,0.00004641088,0.0016970828],"genre_scores_gemma":[0.9997198,0.000021669746,0.00017635054,0.0000049589653,0.0000015864429,9.3020464e-7,0.000010848288,0.0000020230377,0.000061826635],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999666,0.0000031913833,0.0000012957285,0.000008578666,0.000011394676,0.000008826073],"domain_scores_gemma":[0.99991906,0.000029888852,0.000022372142,0.000008192287,0.000010543993,0.000009943013],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101691294,0.00012594204,0.00013470628,0.00022720773,0.00016113427,0.00028888806,0.00017636654,0.00016529368,0.00074240204],"category_scores_gemma":[0.0003447572,0.00008699133,0.00007800228,0.00010707302,0.0006147575,0.00027736166,0.00022863461,0.00021012378,0.00010113784],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025575413,0.000037147063,0.017195052,0.00006824258,0.000008552883,0.0003895046,0.00018436341,0.0047580907,0.9541773,0.0123572,0.0001529011,0.010415924],"study_design_scores_gemma":[0.0000615408,0.00034267624,0.1917048,0.000039075803,0.000021164418,0.0009316409,0.00035155314,0.08811459,0.67373127,0.04177039,0.0028905936,0.000040764993],"about_ca_topic_score_codex":0.00044445304,"about_ca_topic_score_gemma":0.00020324899,"teacher_disagreement_score":0.00074240204,"about_ca_system_score_codex":0.00015013831,"about_ca_system_score_gemma":0.00008027151,"threshold_uncertainty_score":0.0024836063},"labels":[],"label_agreement":null},{"id":"W2972748540","doi":"10.1029/2019gl084526","title":"Direct Monitoring Reveals Initiation of Turbidity Currents From Extremely Dilute River Plumes","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"European Research Council; Natural Environment Research Council; Sight Research UK; National Oceanic and Atmospheric Administration; ExxonMobil Research and Engineering Company; European Commission; Leverhulme Trust","keywords":"Turbidity; Turbidity current; Plume; Current (fluid); Sediment; Hydrology (agriculture); Oceanography; Environmental science; Turbidite; Geology; Geomorphology; Meteorology; Geography","score_opus":0.0716361922797628,"score_gpt":0.30825666434442067,"score_spread":0.23662047206465786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2972748540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960675,0.00011029509,0.0019901807,0.000034025237,0.0000072999705,0.000013036809,0.0002835081,0.00009288602,0.0014013846],"genre_scores_gemma":[0.99722147,0.000056107823,0.0020795853,0.00003486496,0.000006297591,0.000012664807,0.00022939622,0.000006776468,0.00035288438],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.0000046919336,0.0000022669503,0.000018401064,0.000023252964,0.0000133978265],"domain_scores_gemma":[0.99983835,0.000028032207,0.000040008956,0.000010055003,0.000036173216,0.00004737454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000088117355,0.00012624467,0.00018166096,0.00033693833,0.00020037328,0.00031750544,0.00016929934,0.00029191727,0.0006685593],"category_scores_gemma":[0.00023162612,0.00011100635,0.00008410937,0.00016114258,0.00017268086,0.00017063718,0.0003070816,0.00043167555,0.00020893548],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001538399,0.000053815176,0.0526512,0.00003173449,0.000014306147,0.00017754192,0.00017770047,0.00021706325,0.9389206,0.00011571474,0.0002367229,0.007249702],"study_design_scores_gemma":[0.00003799494,0.00067910634,0.7062226,0.00002069778,0.000050932635,0.0006940449,0.00035031856,0.01068453,0.27757505,0.0002556733,0.0033842651,0.000044837347],"about_ca_topic_score_codex":0.0010654574,"about_ca_topic_score_gemma":0.0016375195,"teacher_disagreement_score":0.0010654574,"about_ca_system_score_codex":0.00014829224,"about_ca_system_score_gemma":0.00008819689,"threshold_uncertainty_score":0.002236545},"labels":[],"label_agreement":null},{"id":"W2980384556","doi":"10.1029/2019gl084656","title":"Compliant Volcanic Arc and Backarc Crust in Southern Kurile Suggested by Interseismic Geodetic Deformation","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada","funders":"Japan Society for the Promotion of Science London","keywords":"Geology; Lithosphere; Volcano; Volcanic arc; Seismology; Geodetic datum; Crust; Forearc; Rigidity (electromagnetism); Back-arc basin; Subduction; Geodesy; Geophysics; Tectonics","score_opus":0.02326455681671819,"score_gpt":0.25588014383542246,"score_spread":0.23261558701870427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980384556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992199,0.000019637728,0.00042532396,0.0000120168,6.9702713e-7,0.0000014910993,0.000017737233,0.000008339089,0.00029481426],"genre_scores_gemma":[0.99981743,0.000010022406,0.00011874017,0.0000018792487,4.4883646e-7,7.053099e-7,0.000015813494,0.0000012962715,0.00003357718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998913,0.000030178247,0.000011853211,0.000025811001,0.000015232646,0.000025644746],"domain_scores_gemma":[0.99967897,0.000087492226,0.000112795824,0.000036624086,0.000029758592,0.00005430196],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033103616,0.00041094277,0.00023772978,0.0011115591,0.0002511978,0.0010806158,0.0003471543,0.0005012937,0.001515028],"category_scores_gemma":[0.001178315,0.0004094431,0.0003246286,0.0004793557,0.0006162881,0.0006177073,0.00086195994,0.00023299565,0.00017787043],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036581443,0.00007215331,0.8753347,0.00006708357,0.0001554034,0.00081893464,0.00044879827,0.08654424,0.024538264,0.0025235373,0.00012390738,0.009007243],"study_design_scores_gemma":[0.000028923136,0.000087310495,0.8154799,0.000023996126,0.000058242087,0.00029298366,0.00049811136,0.1810666,0.0012550555,0.00091602944,0.00025768564,0.000035203837],"about_ca_topic_score_codex":0.0042656856,"about_ca_topic_score_gemma":0.0046774116,"teacher_disagreement_score":0.0042656856,"about_ca_system_score_codex":0.00022404757,"about_ca_system_score_gemma":0.00019517886,"threshold_uncertainty_score":0.008481741},"labels":[],"label_agreement":null},{"id":"W2980519689","doi":"10.1029/2019gl084988","title":"Constraining the Variability of the Atlantic Meridional Overturning Circulation During the Holocene","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":115,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Holocene; Geology; Meltwater; Shutdown of thermohaline circulation; Oceanography; Context (archaeology); Climatology; North Atlantic Deep Water; Thermohaline circulation; Northern Hemisphere; Ocean current; Glacial period; Paleontology","score_opus":0.024086362093730263,"score_gpt":0.26690069265025124,"score_spread":0.24281433055652096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980519689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99866986,0.000038128743,0.0003726871,0.000012895103,0.000002292092,0.0000015387893,0.0002796429,0.000009585999,0.0006134168],"genre_scores_gemma":[0.9994418,0.00001608358,0.00016862852,0.0000058658093,0.0000024833632,0.00000140118,0.0003089529,0.0000027697317,0.000052118405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999479,0.000010457184,0.000003477505,0.000015913354,0.000007899913,0.000014426647],"domain_scores_gemma":[0.9997383,0.000095911535,0.00006172626,0.000027689433,0.000037270016,0.000039117687],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022942663,0.0001290961,0.00011317781,0.00047005242,0.00024089424,0.0004460689,0.00014306874,0.00014589498,0.00073172856],"category_scores_gemma":[0.0006380347,0.00008019423,0.00011741295,0.0004201817,0.00012856405,0.00018047314,0.00023441928,0.00018359208,0.00012609633],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010871065,0.00003292542,0.968529,0.000012976233,0.000059230726,0.00006534571,0.00013629014,0.001961327,0.01943106,0.00014070202,0.00019849394,0.009323894],"study_design_scores_gemma":[0.0000023492496,0.000012859704,0.99659914,0.000002789202,0.00000776082,0.0000135805585,0.000044198132,0.0022775738,0.00069157995,0.000026497177,0.00031939926,0.0000023845253],"about_ca_topic_score_codex":0.019597134,"about_ca_topic_score_gemma":0.048673116,"teacher_disagreement_score":0.019597134,"about_ca_system_score_codex":0.00021041206,"about_ca_system_score_gemma":0.0001630528,"threshold_uncertainty_score":0.03896618},"labels":[],"label_agreement":null},{"id":"W2980737410","doi":"10.1029/2019gl083722","title":"Spatiotemporal Variability of Sea Ice in the Arctic's Last Ice Area","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto","funders":"Office of Naval Research; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Sea ice; Arctic ice pack; Drift ice; Antarctic sea ice; Geology; Oceanography; Cryosphere; Archipelago; Arctic sea ice decline; Arctic; Climatology; Arctic geoengineering; Physical geography; Geography","score_opus":0.024009438886363803,"score_gpt":0.2659934664710004,"score_spread":0.2419840275846366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2980737410","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99873585,0.00009644996,0.00009810309,0.00003025884,0.000004566881,0.0000010603407,0.0005738783,0.000004645099,0.00045529203],"genre_scores_gemma":[0.9994087,0.000046080968,0.00005136729,0.0000036039403,0.0000031599677,0.000001219328,0.00040685493,0.0000012602455,0.00007765829],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000009286104,0.0000062608256,0.00002069791,0.000013228029,0.000012628547],"domain_scores_gemma":[0.99960953,0.000089045236,0.00012811,0.00002160904,0.00009857443,0.00005322938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025337876,0.00009451343,0.00012900602,0.0006030285,0.00016869279,0.0005264515,0.00011857826,0.00018642617,0.00041096134],"category_scores_gemma":[0.00062026,0.000072317205,0.0001562676,0.0008454456,0.0001263768,0.00022058238,0.00021876226,0.00016834139,0.00011365735],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009764948,0.000021995735,0.99008256,0.000013305079,0.00007554242,0.00010491437,0.00017178843,0.0029519044,0.0019368223,0.00017830645,0.00046499493,0.0039002376],"study_design_scores_gemma":[0.0000018446221,0.000011001729,0.9939355,0.0000073353326,0.000013049909,0.00003759329,0.00015986529,0.0050387126,0.00019278286,0.00003560555,0.0005631535,0.0000034894188],"about_ca_topic_score_codex":0.03324247,"about_ca_topic_score_gemma":0.03317622,"teacher_disagreement_score":0.03324247,"about_ca_system_score_codex":0.00028447754,"about_ca_system_score_gemma":0.0001733837,"threshold_uncertainty_score":0.066097915},"labels":[],"label_agreement":null},{"id":"W2981272490","doi":"10.1029/2019gl084375","title":"Remarkable Capacity for Anaerobic Oxidation of Methane at High Methane Concentration","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Science Foundation","keywords":"Methane; Anaerobic oxidation of methane; Anoxic waters; Sulfate; Environmental chemistry; Carbon cycle; Carbon fibers; Environmental science; Cold seep; Chemistry; Ecosystem; Materials science; Ecology","score_opus":0.02978542750925759,"score_gpt":0.28342972400191635,"score_spread":0.25364429649265874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981272490","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817,0.00016285454,0.0009051419,0.00001334215,0.0000040238865,0.000002917053,0.0001838198,0.000027484823,0.00053033436],"genre_scores_gemma":[0.9991559,0.000056406338,0.00038372696,0.0000065078298,0.0000016221408,0.0000029036337,0.00018796268,0.000004165853,0.00020071304],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99987054,0.000016418855,0.000006651504,0.000041675394,0.000034177956,0.000030451514],"domain_scores_gemma":[0.99988794,0.000021089512,0.000031471027,0.000016869888,0.000023648794,0.000019051151],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013407362,0.00028051785,0.00016932467,0.00024814656,0.00015879255,0.00034502533,0.0001203004,0.00012798989,0.00036407984],"category_scores_gemma":[0.0001669588,0.00015101544,0.000103527425,0.00019218626,0.00022013046,0.00015347061,0.0003655592,0.0002108877,0.00009240871],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000034154025,0.0000056007307,0.004372016,0.00001765296,0.000010358586,0.000020971007,0.0000256638,0.000052915944,0.99439275,0.00003170925,0.000013978019,0.0010223436],"study_design_scores_gemma":[0.000006533503,0.00018616347,0.12867217,0.000005471476,0.000024821464,0.00024755142,0.00015049847,0.0019171872,0.86713797,0.00017470669,0.0014639666,0.000012990833],"about_ca_topic_score_codex":0.0010311106,"about_ca_topic_score_gemma":0.0009844684,"teacher_disagreement_score":0.0010311106,"about_ca_system_score_codex":0.00011084897,"about_ca_system_score_gemma":0.0001061794,"threshold_uncertainty_score":0.002050221},"labels":[],"label_agreement":null},{"id":"W2981543050","doi":"10.1029/2019gl084652","title":"Episodic Extrema of Surface Stress Energy Input to the Western Arctic Ocean Contributed to Step Changes of Freshwater Content in the Beaufort Gyre","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Climate Program Office; Office of Naval Research; National Key Research and Development Program of China; China Scholarship Council; National Natural Science Foundation of China","keywords":"Ocean gyre; Arctic; Oceanography; Geology; Geostrophic current; Climatology; Sea ice; Beaufort sea; Canada Basin; Arctic ice pack; Ocean current; Wind stress; Environmental science; Atmospheric sciences; Ecology","score_opus":0.03176336702125005,"score_gpt":0.25827072537698187,"score_spread":0.22650735835573182,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981543050","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99897385,0.00003703111,0.00007572017,0.00006632804,0.0000070210967,0.000001467934,0.00019117081,0.000013680934,0.0006338344],"genre_scores_gemma":[0.9996339,0.000020848573,0.000045325778,0.000009743428,0.000003998008,9.685225e-7,0.00015914631,0.0000030800193,0.00012285811],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992466,0.000009624488,0.0000049355767,0.000020120004,0.00001496501,0.00002566755],"domain_scores_gemma":[0.9998449,0.000019734542,0.000042898006,0.000013547102,0.00004030917,0.000038635222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001588654,0.00021484328,0.00020048296,0.0005299281,0.0004567853,0.0008001419,0.00020672048,0.00032661663,0.00096128887],"category_scores_gemma":[0.00039378426,0.00016696437,0.00037972684,0.0005030967,0.0003633205,0.0003146263,0.00035513702,0.0002019162,0.00011123036],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022825053,0.00003841669,0.9688233,0.0000292659,0.000119954944,0.00048140011,0.0004076553,0.007922008,0.014114952,0.0002540432,0.00084114436,0.0067395167],"study_design_scores_gemma":[0.0000029165983,0.000013484234,0.99427336,0.00000501529,0.000010908719,0.000031312164,0.00019719003,0.0045153075,0.0004894994,0.000046354555,0.00040742924,0.0000071674217],"about_ca_topic_score_codex":0.093756914,"about_ca_topic_score_gemma":0.102866665,"teacher_disagreement_score":0.093756914,"about_ca_system_score_codex":0.001139172,"about_ca_system_score_gemma":0.00060533214,"threshold_uncertainty_score":0.18642235},"labels":[],"label_agreement":null},{"id":"W2981667604","doi":"10.1029/2019gl084281","title":"Contribution of Global warming and Urbanization to Changes in Temperature Extremes in Eastern China","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Urbanization; Global warming; Environmental science; China; Climatology; Climate change; Daytime; Atmospheric sciences; Geography; Geology; Ecology","score_opus":0.01914477786486422,"score_gpt":0.291032513308833,"score_spread":0.27188773544396877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2981667604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995382,0.000023298482,0.00024907116,0.000014566809,0.000001290013,8.4815684e-7,0.000054470434,0.0000055362925,0.00011280424],"genre_scores_gemma":[0.9998467,0.00000983309,0.00005748051,0.0000020434716,0.0000017586887,8.1622443e-7,0.000052005882,0.000001094355,0.000028153621],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985254,0.00004579378,0.000008690874,0.00004656388,0.000021056932,0.000025310283],"domain_scores_gemma":[0.9996685,0.00010202564,0.0000901007,0.0000477726,0.000054669115,0.000036958954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054268236,0.00027787223,0.00019679451,0.00042411557,0.00022871353,0.00037632816,0.00014255292,0.00016323496,0.0004048547],"category_scores_gemma":[0.0006106357,0.00014585798,0.00033944382,0.0005776712,0.00024027193,0.0002445047,0.00039858755,0.000156152,0.00003069798],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012583513,0.00002475455,0.9585458,0.000014862244,0.000166164,0.00010581606,0.00015176833,0.023003517,0.009763538,0.00025359538,0.000098549994,0.007745912],"study_design_scores_gemma":[0.0000049638106,0.000011745614,0.9778437,0.0000020742661,0.000028931088,0.000016250644,0.000054511936,0.021183401,0.0005993063,0.00012022737,0.0001266044,0.000008317608],"about_ca_topic_score_codex":0.015059183,"about_ca_topic_score_gemma":0.015030122,"teacher_disagreement_score":0.015059183,"about_ca_system_score_codex":0.00037138507,"about_ca_system_score_gemma":0.00031715634,"threshold_uncertainty_score":0.029943049},"labels":[],"label_agreement":null},{"id":"W2982239427","doi":"10.1029/2019gl083798","title":"Satellite Discovery of Anomalously Large Methane Point Sources From Oil/Gas Production","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":358,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"GHGSat (Canada)","funders":"Earth Sciences Division; Stichting voor de Technische Wetenschappen; Ministry of Economic Affairs","keywords":"Methane; Tonne; Environmental science; Satellite; Compressor station; Atmospheric methane; Natural gas; Atmosphere (unit); Atmospheric sciences; Methane gas; Meteorology; Remote sensing; Geology; Physics; Geography; Chemistry","score_opus":0.010744811020645341,"score_gpt":0.24447856881225052,"score_spread":0.23373375779160518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982239427","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962058,0.00016409701,0.0006864506,0.00009899974,0.000015068408,0.0000070529904,0.0011487845,0.000093521514,0.0015801801],"genre_scores_gemma":[0.9974119,0.00009173098,0.00093526527,0.000028617122,0.000021154056,0.0000047702574,0.0011966139,0.000009001223,0.00030095654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.0000031789812,0.00000253946,0.00001671013,0.000027170956,0.000014199051],"domain_scores_gemma":[0.9998448,0.000016688504,0.00006113688,0.000018061206,0.000034146484,0.000025146626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114161245,0.00020540252,0.00009708966,0.00068737374,0.00026351528,0.00026999635,0.00016890139,0.00025531344,0.0006521875],"category_scores_gemma":[0.00018091645,0.00010921888,0.00013046054,0.0006455554,0.00023572752,0.00020413655,0.00042615624,0.00029762258,0.00017779293],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034711038,0.000078526966,0.6926262,0.00010829302,0.00015239103,0.0021418987,0.00052099465,0.002144515,0.2760344,0.0005374549,0.0024423944,0.02286584],"study_design_scores_gemma":[0.000018021947,0.00008583674,0.95583653,0.000020312924,0.000058275844,0.0005768385,0.00024150612,0.0049136756,0.031077,0.00032853524,0.006821257,0.000022191933],"about_ca_topic_score_codex":0.008101402,"about_ca_topic_score_gemma":0.014405856,"teacher_disagreement_score":0.008101402,"about_ca_system_score_codex":0.00026205936,"about_ca_system_score_gemma":0.00017756372,"threshold_uncertainty_score":0.016108513},"labels":[],"label_agreement":null},{"id":"W2982554803","doi":"10.1029/2019gl085037","title":"Collisionless Electron Dynamics in the Magnetosheath of Mars","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Centre National d’Etudes Spatiales; National Aeronautics and Space Administration","keywords":"Magnetosheath; Bow shock (aerodynamics); Physics; Electron; Mars Exploration Program; Solar wind; Population; Computational physics; Ionization; Exosphere; Kinetic energy; Shock (circulatory); Shock wave; Atomic physics; Magnetopause; Plasma; Mechanics; Astronomy; Classical mechanics; Quantum mechanics","score_opus":0.018270142260618415,"score_gpt":0.2902525456826824,"score_spread":0.271982403422064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982554803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995195,0.000050800933,0.0030648236,0.00008700565,0.0000051279726,0.0000026473183,0.00002110615,0.00002287538,0.0015505464],"genre_scores_gemma":[0.99957794,0.000011246687,0.000094937604,0.0000050223375,0.000001442371,0.0000012239269,0.0000102755785,0.000002177367,0.00029572935],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999509,0.000008739355,0.0000011578752,0.000009060423,0.000010959056,0.000019132574],"domain_scores_gemma":[0.99991107,0.000022499959,0.000018795188,0.000010994148,0.000010519693,0.000026154328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011888451,0.00019794756,0.00028446966,0.00022273509,0.0006324244,0.0004903801,0.00047737287,0.0003819502,0.0015670588],"category_scores_gemma":[0.00038128864,0.00013009508,0.00023481343,0.00017117153,0.00053787924,0.00057776895,0.0007000386,0.00023900498,0.00011820245],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006571715,0.00014018128,0.055766936,0.00007896236,0.00014059577,0.0029416117,0.0010083806,0.77741146,0.06546014,0.08316501,0.0015524979,0.011677034],"study_design_scores_gemma":[0.00008458014,0.00031608954,0.04035908,0.000013223079,0.00002084107,0.00067547837,0.0005395271,0.9248581,0.0050021573,0.025867298,0.0022142339,0.00004940687],"about_ca_topic_score_codex":0.0015674521,"about_ca_topic_score_gemma":0.00063641404,"teacher_disagreement_score":0.0015674521,"about_ca_system_score_codex":0.00048106126,"about_ca_system_score_gemma":0.00011971381,"threshold_uncertainty_score":0.0052423477},"labels":[],"label_agreement":null},{"id":"W2982869726","doi":"10.1029/2019gl084832","title":"From Canopy‐Leaving to Total Canopy Far‐Red Fluorescence Emission for Remote Sensing of Photosynthesis: First Results From TROPOMI","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Science Foundation of Jiangsu Province; National Natural Science Foundation of China","keywords":"Canopy; Atmospheric sciences; Environmental science; Primary production; Remote sensing; Chlorophyll fluorescence; Satellite; Atmosphere (unit); Meteorology; Physics; Fluorescence; Geology; Botany; Optics; Ecosystem","score_opus":0.017629450149384353,"score_gpt":0.2654001752814915,"score_spread":0.24777072513210716,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2982869726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97873884,0.0009591489,0.016328234,0.00009004188,0.000014180127,0.000055890632,0.0016543077,0.00016967807,0.0019897097],"genre_scores_gemma":[0.949955,0.00040762805,0.047547486,0.000045115685,0.000006995565,0.000044779918,0.0015780687,0.00005691041,0.0003579194],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998634,0.00003205296,0.00000579331,0.000045648427,0.00003977526,0.00001319255],"domain_scores_gemma":[0.99979955,0.00008050164,0.0000144737005,0.0000279887,0.0000531494,0.000024379422],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000886208,0.0006102261,0.0003036958,0.00029885146,0.00032204142,0.0003680598,0.00033460252,0.00030904703,0.00049096334],"category_scores_gemma":[0.0006367008,0.00020528446,0.00053352065,0.00060811534,0.00022852758,0.00051490555,0.0002247442,0.00042636576,0.000108611304],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014840459,0.00033577633,0.23588695,0.00046589348,0.00071614416,0.00044955715,0.0004921769,0.08343256,0.5066319,0.00096300716,0.0022847448,0.16685715],"study_design_scores_gemma":[0.00019891665,0.0004984243,0.63698006,0.00004778368,0.00044517778,0.00032121607,0.0002427829,0.22481818,0.13080047,0.0006375603,0.00485168,0.00015790638],"about_ca_topic_score_codex":0.043505196,"about_ca_topic_score_gemma":0.0967764,"teacher_disagreement_score":0.043505196,"about_ca_system_score_codex":0.00064361165,"about_ca_system_score_gemma":0.00048280024,"threshold_uncertainty_score":0.08650392},"labels":[],"label_agreement":null},{"id":"W2983394461","doi":"10.1029/2019gl084848","title":"Lateral Variations in Lithospheric Mantle Structure Control the Location of Intracontinental Seismicity in Australia","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"University of Minnesota","keywords":"Intraplate earthquake; Induced seismicity; Geology; Lithosphere; Seismology; Mantle (geology); Attenuation; Geophysics; Tectonics; Physics","score_opus":0.01886868416152347,"score_gpt":0.27301027453107274,"score_spread":0.25414159036954925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983394461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999337,0.000045728368,0.00008884099,0.000015592503,3.3772793e-7,8.528897e-7,0.000018964503,0.0000021958579,0.0004904937],"genre_scores_gemma":[0.9998461,0.000019354136,0.00003316211,0.0000024700892,4.318856e-7,5.5174985e-7,0.000013685086,7.490678e-7,0.00008343523],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.000013860849,0.000004268015,0.000017241355,0.000012765766,0.000017548644],"domain_scores_gemma":[0.99954766,0.000075042706,0.00017573968,0.000027222999,0.00012454692,0.000049740225],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018193241,0.00009649084,0.000131592,0.00054672785,0.00019105784,0.00036666123,0.00020414143,0.00013979142,0.000909575],"category_scores_gemma":[0.0007711429,0.00013825712,0.00008228502,0.00044851055,0.00038866882,0.00026844573,0.00051716523,0.00013317382,0.000139561],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000113593436,0.000024317545,0.9261419,0.000034556433,0.000053817326,0.00014868798,0.0016514191,0.00086491206,0.057976086,0.00036064684,0.00009878284,0.012531182],"study_design_scores_gemma":[6.42719e-7,0.000008419012,0.99897504,0.0000023280993,0.0000038534026,0.000015403954,0.00018567865,0.00036428074,0.0003231888,0.00003942668,0.00008056215,0.0000012742754],"about_ca_topic_score_codex":0.017990785,"about_ca_topic_score_gemma":0.020280411,"teacher_disagreement_score":0.017990785,"about_ca_system_score_codex":0.0002879987,"about_ca_system_score_gemma":0.00023506208,"threshold_uncertainty_score":0.035772145},"labels":[],"label_agreement":null},{"id":"W2983684877","doi":"10.1029/2019gl084031","title":"Thank You to Our 2018 Peer Reviewers","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Reading (process); Library science; Peer review; Field (mathematics); Rigour; History; Engineering ethics; Political science; Public relations; Computer science; Law; Engineering; Epistemology; Philosophy","score_opus":0.056250858048869166,"score_gpt":0.3497348492281025,"score_spread":0.29348399117923335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983684877","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005461618,0.011594145,0.007528821,0.26560766,0.68483174,0.001025708,0.002619767,0.004210467,0.022035444],"genre_scores_gemma":[0.01052525,0.017395062,0.020627346,0.18266933,0.4151251,0.003330976,0.0051812152,0.007277817,0.33786795],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9610552,0.008864933,0.005570547,0.004922775,0.018164223,0.0014223141],"domain_scores_gemma":[0.4585966,0.016906545,0.013450667,0.014756756,0.47748515,0.018804308],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.03239166,0.002413479,0.0033776122,0.006517718,0.005328254,0.021757241,0.0035348062,0.0073275496,0.1472713],"category_scores_gemma":[0.24297267,0.0013518075,0.0021575647,0.0035310695,0.002707886,0.009153681,0.0054237815,0.010726983,0.24967551],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012961991,0.000005254397,0.000086447195,0.00009215103,0.0000055802657,0.00004759679,0.000059865375,0.000012397173,0.00006654344,0.00017664414,0.9859277,0.013506808],"study_design_scores_gemma":[0.0000120989525,0.000010570006,0.00018830421,0.00023365724,0.000008557869,0.00015192697,0.00024219886,0.00005532064,0.00008158219,0.00058204087,0.9984048,0.000028984769],"about_ca_topic_score_codex":0.002580973,"about_ca_topic_score_gemma":0.0043730363,"teacher_disagreement_score":0.96760833,"about_ca_system_score_codex":0.0035304923,"about_ca_system_score_gemma":0.014279597,"threshold_uncertainty_score":0.4926716},"labels":[],"label_agreement":null},{"id":"W2983893943","doi":"10.1029/2019gl084730","title":"Groundwater Buffers Decreasing Glacier Melt in an Andean Watershed—But Not Forever","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":123,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"École de Technologie Supérieure; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; United States Agency for International Development; National Science Foundation","keywords":"Groundwater recharge; Glacier; Groundwater; Meltwater; Evapotranspiration; Hydrology (agriculture); Climate change; Geology; Streamflow; Environmental science; Watershed; Surface water; Depression-focused recharge; Aquifer; Geomorphology; Oceanography; Geography; Drainage basin; Ecology","score_opus":0.05314008729968373,"score_gpt":0.29268288645530305,"score_spread":0.23954279915561932,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983893943","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940638,0.00008286953,0.00067164085,0.0006175204,0.000008134768,0.000012481538,0.00049269776,0.00010621789,0.0039445413],"genre_scores_gemma":[0.9988715,0.00005361472,0.00028805883,0.000042499138,0.0000027622493,0.000007788129,0.0002024404,0.000007933288,0.00052342756],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991786,0.000023200131,0.0000031747297,0.000025059211,0.000007754487,0.000022892697],"domain_scores_gemma":[0.9998745,0.00003498003,0.00002350581,0.000010158733,0.000022089604,0.0000348203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012965481,0.0002453875,0.00029825064,0.00041422315,0.00048432042,0.0014465468,0.0006341844,0.00065868866,0.0034826929],"category_scores_gemma":[0.0008541478,0.00018221974,0.00042591788,0.00054250134,0.00064539147,0.0007557217,0.0009622057,0.0003394076,0.00010498484],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052784826,0.0005021727,0.2549659,0.00015104203,0.00047277202,0.0005778165,0.001168913,0.70169044,0.009829032,0.010174029,0.0040079947,0.01593204],"study_design_scores_gemma":[0.00039449596,0.0002947078,0.12226309,0.0000624837,0.00021306348,0.00009713131,0.0015144,0.8594124,0.0015545591,0.0070167035,0.0070841997,0.00009285552],"about_ca_topic_score_codex":0.15181199,"about_ca_topic_score_gemma":0.16096991,"teacher_disagreement_score":0.15181199,"about_ca_system_score_codex":0.0028598744,"about_ca_system_score_gemma":0.0017195385,"threshold_uncertainty_score":0.3018567},"labels":[],"label_agreement":null},{"id":"W2983917889","doi":"10.1029/2019gl085202","title":"Hydroclimate in the Pamirs Was Driven by Changes in Precipitation‐Evaporation Seasonality Since the Last Glacial Period","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"German Academic Exchange Service London; Vetenskapsrådet; Svenska Forskningsrådet Formas; Deutsche Forschungsgemeinschaft","keywords":"Interglacial; Glacial period; Precipitation; Climatology; Seasonality; Climate change; Environmental science; Water cycle; Period (music); Paleoclimatology; Altitude (triangle); Physical geography; Geology; Atmospheric sciences; Oceanography; Ecology; Geography; Geomorphology","score_opus":0.027513464782094335,"score_gpt":0.2931548572850766,"score_spread":0.2656413925029823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2983917889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99940646,0.000018363837,0.000048447186,0.000022002983,0.0000013695717,0.0000019218185,0.00012699053,0.000007611341,0.00036677378],"genre_scores_gemma":[0.9998167,0.000009985562,0.000041223873,0.000005334417,0.0000014260121,0.0000019238344,0.000076797696,0.000001210788,0.000045468292],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995387,0.000010934034,0.0000023551577,0.000013252218,0.0000048434695,0.000014651504],"domain_scores_gemma":[0.9999106,0.000017299548,0.000025408326,0.000009373435,0.0000148108375,0.000022598631],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017047959,0.00013436633,0.00014577455,0.00033041218,0.00026601792,0.0002784732,0.00013885654,0.0000989139,0.0010989953],"category_scores_gemma":[0.00021991081,0.00010337867,0.0001726746,0.00035215565,0.00020375777,0.00014677405,0.00028507403,0.00014840497,0.00011040053],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042755873,0.000038955866,0.9373171,0.000057028003,0.00011415552,0.00047036534,0.00046861017,0.0014460905,0.04830041,0.00027563045,0.0003661906,0.010718009],"study_design_scores_gemma":[0.0000020506493,0.000012531275,0.9986524,0.0000012025234,0.0000070816354,0.000027441443,0.00007526571,0.0006789034,0.00042034083,0.000019526338,0.00010142181,0.0000017887327],"about_ca_topic_score_codex":0.008808527,"about_ca_topic_score_gemma":0.014563543,"teacher_disagreement_score":0.008808527,"about_ca_system_score_codex":0.00025881603,"about_ca_system_score_gemma":0.00027534133,"threshold_uncertainty_score":0.017514527},"labels":[],"label_agreement":null},{"id":"W2987052509","doi":"10.1029/2019gl084202","title":"Direct Observation of Subrelativistic Electron Precipitation Potentially Driven by EMIC Waves","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Air Force Office of Scientific Research; National Stroke Foundation; Canada Foundation for Innovation; Athabasca University; National Aeronautics and Space Administration; Canadian Space Agency; Nuclear Safety and Security Commission; University of Alberta; District of Columbia Space Grant Consortium; National Science Foundation","keywords":"Electron precipitation; Physics; Emic and etic; Van Allen Probes; Cyclotron; Van Allen radiation belt; Electron; Precipitation; Hiss; Atomic physics; Astrophysics; Nuclear physics; Magnetosphere; Meteorology; Plasma","score_opus":0.010958984359338094,"score_gpt":0.26584704562911576,"score_spread":0.25488806126977764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2987052509","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99411374,0.0001305396,0.0019195437,0.000071351504,0.00001697241,0.000005521702,0.00016622472,0.00006902276,0.003507069],"genre_scores_gemma":[0.999121,0.00003339831,0.00043921568,0.00002132709,0.00000761382,0.0000029592497,0.00007021344,0.000005864346,0.00029840445],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996984,0.0000021785424,7.8084975e-7,0.000009222361,0.000008957667,0.000008963666],"domain_scores_gemma":[0.99992883,0.000015968188,0.000019623363,0.000009961987,0.000013106231,0.000012402909],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000055604247,0.00010679373,0.00009188115,0.0001502738,0.00013794292,0.00014960469,0.00015809291,0.0001435903,0.0011404662],"category_scores_gemma":[0.00014647025,0.000064999214,0.000060005917,0.00012593591,0.00015887736,0.00014974485,0.00022888019,0.0002187314,0.00014160835],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081270136,0.00006574998,0.07802497,0.00008355971,0.00007517941,0.0010475884,0.00029026356,0.0017825131,0.899821,0.0011487955,0.0011461544,0.01570156],"study_design_scores_gemma":[0.00011675289,0.00044235293,0.54347366,0.000016247257,0.000056022385,0.0014658994,0.00032512276,0.01274616,0.43122315,0.0011826323,0.008927313,0.00002474195],"about_ca_topic_score_codex":0.0003680519,"about_ca_topic_score_gemma":0.0005145783,"teacher_disagreement_score":0.0011404662,"about_ca_system_score_codex":0.00012482036,"about_ca_system_score_gemma":0.00004232246,"threshold_uncertainty_score":0.0038152933},"labels":[],"label_agreement":null},{"id":"W2987662829","doi":"10.1029/2019gl085116","title":"The Dynamic Response of Sea Ice to Warming in the Canadian Arctic Archipelago","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Arctic ice pack; Sea ice; Arctic; Archipelago; Arctic sea ice decline; Arctic dipole anomaly; Arctic geoengineering; Antarctic sea ice; Oceanography; Drift ice; Geology; Climatology; Environmental science; Sea ice thickness; Ice-albedo feedback; Flux (metallurgy); Global warming; Climate change; Chemistry","score_opus":0.016743924962238654,"score_gpt":0.2708220981960338,"score_spread":0.25407817323379517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2987662829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99500054,0.0004142918,0.00003312247,0.00026709586,0.000010381468,0.0000065646477,0.002295384,0.000009008323,0.0019635535],"genre_scores_gemma":[0.99853754,0.00022398504,0.000051820138,0.00004043712,0.000005617257,0.0000039654783,0.000816376,0.0000030114304,0.00031725795],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977285,0.0000145352,0.000010146188,0.000047268495,0.00006358961,0.00009160196],"domain_scores_gemma":[0.998809,0.000089749694,0.0001273805,0.000039255618,0.0007521217,0.00018247179],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039233585,0.0002237997,0.00025153885,0.0019698536,0.0014165194,0.0013389087,0.00046591426,0.0003949096,0.0012328805],"category_scores_gemma":[0.0017933538,0.00018624513,0.00034814829,0.0025276453,0.00056578533,0.00034449587,0.0005736076,0.0003879165,0.000111839356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015798693,0.00002228639,0.9856389,0.00003886367,0.00012276933,0.00010184675,0.00056997436,0.0019103333,0.0020744028,0.00023746067,0.001614948,0.007510206],"study_design_scores_gemma":[0.0000011342444,0.0000024069773,0.99886465,0.0000053396543,0.0000078838175,0.000007282312,0.00024935996,0.0003202545,0.00005276809,0.000016318536,0.00046903559,0.0000035787427],"about_ca_topic_score_codex":0.97659975,"about_ca_topic_score_gemma":0.98402804,"teacher_disagreement_score":0.023400247,"about_ca_system_score_codex":0.010576884,"about_ca_system_score_gemma":0.007494465,"threshold_uncertainty_score":0.07674104},"labels":[],"label_agreement":null},{"id":"W2987783205","doi":"10.1029/2019gl082789","title":"Identifying STEVE's Magnetospheric Driver Using Conjugate Observations in the Magnetosphere and on the Ground","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University; University of Saskatchewan; University of Calgary","funders":"National Aeronautics and Space Administration","keywords":"Plasmasphere; Physics; Electron precipitation; Magnetosphere; Geophysics; Electron; Substorm; Van Allen radiation belt; Electric field; Field line; Ionosphere; Ion; Computational physics; Plasma; Atmospheric sciences; Atomic physics","score_opus":0.05139372664817662,"score_gpt":0.30029496874266004,"score_spread":0.24890124209448342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2987783205","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9972819,0.000033745375,0.0006965745,0.000015901924,0.0000035542137,0.0000063201205,0.00015274038,0.00002850249,0.0017807077],"genre_scores_gemma":[0.9992286,0.000014164964,0.0004289093,0.0000075417047,0.0000030706158,0.000002947853,0.00012858975,0.000005507304,0.00018068083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999192,0.000009696044,0.0000019605393,0.000025810736,0.000016655624,0.000026667087],"domain_scores_gemma":[0.9998765,0.000022905595,0.000031372376,0.000018406568,0.000024950441,0.000025925605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017085372,0.00015798546,0.00017050121,0.00041858235,0.00022145692,0.00037680706,0.00015726898,0.00024792308,0.0006388991],"category_scores_gemma":[0.00028265023,0.00015175321,0.00016233423,0.00031420094,0.00017421463,0.00028548663,0.00040632684,0.00023665781,0.00011535543],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054726354,0.00009791087,0.6218315,0.000045666988,0.00013034622,0.00044020455,0.0006831361,0.002278992,0.34576076,0.00082492596,0.0005136657,0.026845738],"study_design_scores_gemma":[0.000011186483,0.000073734256,0.98779964,0.000006100348,0.000018411252,0.0001082079,0.00012752075,0.0030559117,0.0078092506,0.00009146897,0.0008914987,0.000007024103],"about_ca_topic_score_codex":0.002948908,"about_ca_topic_score_gemma":0.0076516285,"teacher_disagreement_score":0.002948908,"about_ca_system_score_codex":0.00016278499,"about_ca_system_score_gemma":0.00010948081,"threshold_uncertainty_score":0.0058634877},"labels":[],"label_agreement":null},{"id":"W2987838825","doi":"10.1029/2019gl085142","title":"Areal Models for Spatially Coherent Trend Detection: The Case of British Peak River Flows","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Drought Analysis","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Statistic; Trend analysis; Focus (optics); Climate change; Series (stratigraphy); Change detection; Variable (mathematics); Environmental science; sort; Econometrics; Geography; Statistics; Climatology; Physical geography; Computer science; Remote sensing; Geology; Mathematics; Database; Oceanography","score_opus":0.022604278060589483,"score_gpt":0.27884127718860163,"score_spread":0.2562369991280121,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2987838825","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.649,0.0006687219,0.3410509,0.0027871227,0.00006045341,0.00007451763,0.00089716155,0.0005757258,0.0048853806],"genre_scores_gemma":[0.9787948,0.00016369353,0.017261576,0.00010899018,0.000039415394,0.00006562236,0.0003022872,0.000080663776,0.0031829886],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9985973,0.0008851418,0.00005058801,0.0002466903,0.00009115321,0.0001290645],"domain_scores_gemma":[0.9834119,0.01360153,0.0014316234,0.00059772696,0.00067482627,0.0002823419],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0068762777,0.0005097696,0.0010267929,0.0011844514,0.0005642145,0.0016179279,0.0016527796,0.0015122737,0.0023184107],"category_scores_gemma":[0.023055796,0.00064322166,0.0011318529,0.001141159,0.0018111789,0.0015859916,0.0014902019,0.0014657199,0.00031967656],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006522124,0.000020158639,0.0073034167,0.000021531698,0.00006221064,0.00008904228,0.00013287115,0.96958333,0.00021969159,0.016544601,0.00050637,0.005451529],"study_design_scores_gemma":[0.000006235565,0.000008456526,0.000898031,0.0000040662985,0.000006032591,0.000009132443,0.0000138377945,0.9943963,0.00001982838,0.004490703,0.00014180849,0.0000056405993],"about_ca_topic_score_codex":0.08732161,"about_ca_topic_score_gemma":0.041147094,"teacher_disagreement_score":0.08732161,"about_ca_system_score_codex":0.0019515193,"about_ca_system_score_gemma":0.000780221,"threshold_uncertainty_score":0.17362666},"labels":[],"label_agreement":null},{"id":"W2988566721","doi":"10.1029/2007gl029485","title":"Correction to “Critical point theory of earthquakes: Observation of correlated and cooperative behavior on earthquake fault systems”","year":2007,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Complex Systems and Time Series Analysis","field":"Economics, Econometrics and Finance","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Seismology; Earthquake prediction; Geology; Seismic gap; Foreshock; Fault (geology); Types of earthquake; Earthquake simulation; Intraplate earthquake; Urban seismic risk; Seismic hazard; Aftershock","score_opus":0.06208259569694611,"score_gpt":0.3016460223792983,"score_spread":0.23956342668235217,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2988566721","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00021196505,0.001955273,0.0028340248,0.061984118,0.92972606,0.00005135188,0.001136129,0.0006791387,0.00142194],"genre_scores_gemma":[0.018481681,0.007190075,0.0070064343,0.11550016,0.8025995,0.00032772028,0.0026407165,0.0012035678,0.045050208],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9915439,0.001514353,0.001151948,0.0016656755,0.0034392455,0.00068484276],"domain_scores_gemma":[0.9469449,0.012006174,0.0029630514,0.0038945603,0.032207962,0.001983341],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005954512,0.004825369,0.004046115,0.0066756504,0.003945673,0.0035540878,0.008636744,0.009622708,0.027914817],"category_scores_gemma":[0.07703924,0.0017452169,0.0032945198,0.005270191,0.004556308,0.0047593494,0.0044808467,0.016485624,0.020176422],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047264853,0.000010971349,0.00013802273,0.00021641605,0.0000332377,0.00014251709,0.00004948918,0.00011956395,0.00007642684,0.0017246107,0.99192274,0.00551878],"study_design_scores_gemma":[0.00011517659,0.000058001424,0.002382412,0.0002599446,0.00008041787,0.0004674162,0.00007882004,0.0014093063,0.00054791244,0.006082345,0.9884035,0.00011470338],"about_ca_topic_score_codex":0.019511616,"about_ca_topic_score_gemma":0.015331221,"teacher_disagreement_score":0.027914817,"about_ca_system_score_codex":0.005483517,"about_ca_system_score_gemma":0.005734864,"threshold_uncertainty_score":0.093384385},"labels":[],"label_agreement":null},{"id":"W2989743519","doi":"10.1029/2019gl085736","title":"Age of the Canada Basin, Arctic Ocean: Indications From High‐Resolution Magnetic Data","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Second Institute of Oceanography, State Oceanic Administration; Chinese Arctic and Antarctic Administration; National Natural Science Foundation of China","keywords":"Geology; Structural basin; Lineation; Arctic; Tectonics; Earth's magnetic field; Magnetic anomaly; Canada Basin; Oceanic basin; Paleomagnetism; Paleontology; Geophysics; Oceanography; Magnetic field","score_opus":0.0424055467985791,"score_gpt":0.24483307605102508,"score_spread":0.20242752925244598,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2989743519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9831117,0.002095686,0.0005817071,0.00030542965,0.000014631849,0.000010155088,0.0030867169,0.000039952698,0.01075396],"genre_scores_gemma":[0.9978758,0.0004853458,0.00032819208,0.000026881185,0.000004479121,0.0000017475189,0.00075771706,0.00000650418,0.0005132716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998547,0.000009604907,0.000006984394,0.00002881512,0.000059949205,0.000039945255],"domain_scores_gemma":[0.9990441,0.000066313725,0.00015602262,0.000044020126,0.00058326405,0.00010627285],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034602277,0.000145921,0.000098472425,0.0012665663,0.00060045195,0.00071806915,0.00022432994,0.00013973557,0.001044596],"category_scores_gemma":[0.0010872673,0.000071001865,0.000097440636,0.001849976,0.00042361816,0.00022589247,0.00040236706,0.00016307006,0.00014361645],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005614511,0.000005262715,0.9768779,0.00005087461,0.00007412314,0.0001617603,0.00061693805,0.00059923856,0.006301155,0.00053952174,0.00088669424,0.013830367],"study_design_scores_gemma":[0.0000014780476,0.0000022359927,0.99653745,0.000012400124,0.000009551464,0.00004342465,0.00027891333,0.0002493341,0.0003174073,0.00006314743,0.0024808175,0.0000038398007],"about_ca_topic_score_codex":0.859696,"about_ca_topic_score_gemma":0.9355076,"teacher_disagreement_score":0.14030403,"about_ca_system_score_codex":0.0025314991,"about_ca_system_score_gemma":0.0038229215,"threshold_uncertainty_score":0.2822606},"labels":[],"label_agreement":null},{"id":"W2989963127","doi":"10.1029/2019gl085301","title":"Sound Velocities in Shock‐Synthesized Stishovite to 72 GPa","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"National Nuclear Security Administration; Princeton University; Washington State University; Carnegie Institution of Washington; U.S. Department of Energy","keywords":"Stishovite; Speed of sound; Geology; Rutile; Shear (geology); Mineralogy; Bulk modulus; Materials science; Thermodynamics; Composite material; Quartz; Petrology; Physics","score_opus":0.02937837099783221,"score_gpt":0.28317988689154583,"score_spread":0.25380151589371364,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2989963127","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993981,0.000025669475,0.0001433659,0.0000046350588,0.000002364915,0.0000019966913,0.000082194274,0.000015714393,0.00032598496],"genre_scores_gemma":[0.9994092,0.000015695336,0.00008552622,0.0000030097276,0.0000018655807,0.0000031471545,0.00015241609,0.0000059317895,0.0003231807],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998877,0.0000061414717,0.0000037911852,0.000027984657,0.00004460206,0.000029712],"domain_scores_gemma":[0.9998474,0.000029300712,0.000029990812,0.000010858741,0.000049819424,0.00003252279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001337419,0.0003745454,0.00026723123,0.0006348611,0.00025786378,0.00032867672,0.00030532887,0.00027143318,0.0028691376],"category_scores_gemma":[0.00033810866,0.00019652862,0.00012830258,0.00039237287,0.00051240565,0.0002655162,0.00038565803,0.00039370617,0.00025890413],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003573489,0.000037392794,0.010336423,0.00002319762,0.00001232155,0.00014297738,0.00023976198,0.00074536743,0.98507524,0.00013955096,0.000051450657,0.002838932],"study_design_scores_gemma":[0.000055633314,0.0007924266,0.22747211,0.000014112877,0.000020609981,0.00015413885,0.0004939485,0.008741555,0.7607917,0.00021365962,0.0012141698,0.000036012316],"about_ca_topic_score_codex":0.0030903793,"about_ca_topic_score_gemma":0.0017103944,"teacher_disagreement_score":0.0030903793,"about_ca_system_score_codex":0.00041805755,"about_ca_system_score_gemma":0.00015363416,"threshold_uncertainty_score":0.009598196},"labels":[],"label_agreement":null},{"id":"W2991377956","doi":"10.1029/2019gl084969","title":"Detecting Climate Change Effects on Vb Cyclones in a 50‐Member Single‐Model Ensemble Using Machine Learning","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos","funders":"","keywords":"Climatology; Environmental science; Precipitation; Climate change; Cyclone (programming language); Meteorology; Geology; Computer science; Geography; Oceanography","score_opus":0.08175944423683938,"score_gpt":0.3254549564967628,"score_spread":0.24369551225992342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2991377956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9878429,0.000091096554,0.010934918,0.00009394131,0.000043075222,0.000010934739,0.0002898197,0.00017724621,0.00051601435],"genre_scores_gemma":[0.99773264,0.000016490563,0.0017170275,0.000009619667,0.000010101891,0.000006219768,0.000420459,0.0000078944695,0.00007961865],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998179,0.0000632677,0.000011542117,0.0000515802,0.000022105425,0.000033686567],"domain_scores_gemma":[0.99930584,0.0003280402,0.00006308676,0.00012309312,0.00011313567,0.00006669125],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011309696,0.00053006853,0.0006349131,0.00055283314,0.0003625652,0.00061395357,0.00044564385,0.00049533404,0.0005858185],"category_scores_gemma":[0.0015645616,0.00023552666,0.00089409115,0.00034022948,0.00025641805,0.0006059888,0.00049075607,0.00068559195,0.00008327332],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021895308,0.00014601705,0.06623564,0.000021051543,0.00038574814,0.00007027105,0.000029583232,0.91072917,0.004259859,0.00025872205,0.0008847665,0.016760223],"study_design_scores_gemma":[0.000005985866,0.000028042285,0.015031263,0.0000025046477,0.00002909858,0.0000053671292,0.000009291095,0.9840349,0.0006280159,0.00013525406,0.000082404986,0.000007906394],"about_ca_topic_score_codex":0.014262225,"about_ca_topic_score_gemma":0.01117712,"teacher_disagreement_score":0.014262225,"about_ca_system_score_codex":0.00043084574,"about_ca_system_score_gemma":0.00045191203,"threshold_uncertainty_score":0.0283584},"labels":[],"label_agreement":null},{"id":"W2992141643","doi":"10.1029/2019gl085725","title":"Mean European Carbon Sink Over 2010–2015 Estimated by Simultaneous Assimilation of Atmospheric CO<sub>2</sub>, Soil Moisture, and Vegetation Optical Depth","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Inversa Systems (Canada)","funders":"Swedish National Space Agency; European Commission; European Space Agency","keywords":"SCIAMACHY; Environmental science; Biosphere; Sink (geography); Carbon sink; Atmospheric sciences; Data assimilation; Atmospheric chemistry; Carbon dioxide; Climatology; Meteorology; Climate change; Geology; Troposphere; Ozone; Chemistry; Geography","score_opus":0.010807229898296897,"score_gpt":0.2529734926522128,"score_spread":0.2421662627539159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2992141643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9916313,0.00025085767,0.0026258451,0.000059407743,0.000019613344,0.000006533166,0.0045378236,0.0001726102,0.0006960691],"genre_scores_gemma":[0.98858976,0.00015383029,0.0018704387,0.000036727244,0.000009500071,0.0000140118245,0.008983918,0.00003729345,0.00030448902],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982435,0.000023781991,0.000017302542,0.00008814216,0.000022772718,0.000023741157],"domain_scores_gemma":[0.9997197,0.000062675026,0.000058575526,0.00004237279,0.0000937174,0.000022955423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000824164,0.0008645337,0.00039276804,0.0006755637,0.0001714551,0.0005838444,0.00022736202,0.0005513542,0.0005485597],"category_scores_gemma":[0.0006278038,0.00025792845,0.001065499,0.0008043315,0.0001928914,0.0009289556,0.0004199831,0.0002242149,0.00025535896],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001353332,0.0001463877,0.65110373,0.00031367573,0.0024063007,0.00048509162,0.00017974888,0.25995758,0.043861505,0.001699766,0.00469491,0.033798028],"study_design_scores_gemma":[0.000044103643,0.00008274885,0.8811865,0.00003683466,0.00032183618,0.000118868345,0.00007620086,0.102230884,0.010794287,0.00041197284,0.004611656,0.00008422544],"about_ca_topic_score_codex":0.02514543,"about_ca_topic_score_gemma":0.013914125,"teacher_disagreement_score":0.02514543,"about_ca_system_score_codex":0.0006259862,"about_ca_system_score_gemma":0.00041079882,"threshold_uncertainty_score":0.049998164},"labels":[],"label_agreement":null},{"id":"W2992220781","doi":"10.1029/2019gl085639","title":"Optical Spectra and Emission Altitudes of Double‐Layer STEVE: A Case Study","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University; University of Saskatchewan; University of Calgary","funders":"","keywords":"Elevation (ballistics); Altitude (triangle); Airglow; Zenith; Atmospheric sciences; Spectral line; Emission spectrum; Spectrograph; Geology; Meteorology; Physics; Geodesy; Astronomy; Geometry; Mathematics","score_opus":0.024811126227148803,"score_gpt":0.3262574187455237,"score_spread":0.3014462925183749,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2992220781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99849033,0.000018919058,0.00030255833,0.000027897193,0.000003870629,0.0000072564876,0.00010299754,0.000010530252,0.0010355599],"genre_scores_gemma":[0.99899644,0.00002512069,0.00041250573,0.000012487852,0.000007484016,0.000002326744,0.00017533565,0.000006496536,0.00036174382],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985373,0.000013168539,0.000008400574,0.000030815798,0.000042491298,0.000051475457],"domain_scores_gemma":[0.99969304,0.0000641467,0.00005672632,0.000050190396,0.00007028152,0.00006558685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018872852,0.00025182273,0.0002092389,0.0011294278,0.00096791144,0.00068835967,0.00041538608,0.0006596549,0.00087583356],"category_scores_gemma":[0.00055596244,0.00017541274,0.00025844836,0.00064034935,0.0004491005,0.0005059465,0.0009706842,0.00055054814,0.00014184134],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007559225,0.0006328121,0.84924555,0.00009664607,0.00015186143,0.07409146,0.0065339683,0.0030493368,0.037061106,0.0012462751,0.0020063447,0.02512872],"study_design_scores_gemma":[0.000028858996,0.00037205915,0.93778574,0.00004961441,0.000061592225,0.024421407,0.009252422,0.007823474,0.0128165,0.0006279777,0.0066989553,0.00006145399],"about_ca_topic_score_codex":0.0056756237,"about_ca_topic_score_gemma":0.012729243,"teacher_disagreement_score":0.0056756237,"about_ca_system_score_codex":0.0003280525,"about_ca_system_score_gemma":0.00014635785,"threshold_uncertainty_score":0.011285186},"labels":[],"label_agreement":null},{"id":"W2993203696","doi":"10.1029/2019gl084879","title":"How Far North Did the African Monsoon Fringe Expand During the African Humid Period? Insights From Southwest Moroccan Speleothems","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bishop's University","funders":"Postdoctoral Science Foundation of Jiangsu Province; National Natural Science Foundation of China; National Science Foundation","keywords":"Speleothem; Period (music); Monsoon; Climatology; Holocene; Geology; Stalagmite; Arid; Physical geography; Geography; Oceanography; Cave; Paleontology; Archaeology","score_opus":0.022864090636848643,"score_gpt":0.23761006319891334,"score_spread":0.2147459725620647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993203696","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99766266,0.0005355921,0.000037090304,0.0002593746,0.000004595681,0.0000010446232,0.0001232374,0.000002212942,0.0013741755],"genre_scores_gemma":[0.99968827,0.00012716718,0.000021796235,0.000027319242,0.0000063726675,6.977097e-7,0.000028513505,0.0000013396606,0.0000987203],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.0000103141465,0.000002573022,0.000015383326,0.000006234108,0.000031633943],"domain_scores_gemma":[0.9997644,0.00005366735,0.00008123639,0.000015863647,0.000038916212,0.000045795547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027939014,0.00009613129,0.00014269259,0.0005289385,0.00060522166,0.00058984593,0.00013306185,0.00019495547,0.0016173965],"category_scores_gemma":[0.0006352318,0.00008117382,0.00008951513,0.0004344712,0.00034214696,0.0004318523,0.00028774154,0.00016536965,0.00015517135],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021268465,0.000021816324,0.9094672,0.00008796247,0.000045918092,0.00095705764,0.0075353407,0.00020911967,0.03740901,0.0008788836,0.00077269395,0.04240235],"study_design_scores_gemma":[8.2990744e-7,0.000004273336,0.9975688,0.000008903789,0.000002758689,0.00003958997,0.0007849149,0.000050964423,0.00016227353,0.00005490964,0.0013198211,0.0000020647835],"about_ca_topic_score_codex":0.034587163,"about_ca_topic_score_gemma":0.10834862,"teacher_disagreement_score":0.034587163,"about_ca_system_score_codex":0.00064959883,"about_ca_system_score_gemma":0.0003703836,"threshold_uncertainty_score":0.06877172},"labels":[],"label_agreement":null},{"id":"W2993447891","doi":"10.1029/2019gl085651","title":"The August 2018 Kaktovik Earthquakes: Active Tectonics in Northeastern Alaska Revealed With InSAR and Seismology","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canada Foundation for Innovation","keywords":"Seismology; Geology; Interferometric synthetic aperture radar; Tectonics; Seismic hazard; Fault (geology); Sinistral and dextral; Active fault; Synthetic aperture radar; Remote sensing","score_opus":0.020494431141001378,"score_gpt":0.2563172188177325,"score_spread":0.23582278767673112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993447891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990128,0.00006284221,0.00009315481,0.000024285802,0.0000033694303,0.0000012287431,0.00014759297,0.000006819457,0.00064782245],"genre_scores_gemma":[0.9994844,0.00005437362,0.00011732679,0.0000027983815,0.0000023870377,6.4070656e-7,0.00014147251,8.813118e-7,0.0001956339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995375,0.000008414011,0.0000061245523,0.000014415647,0.000010041137,0.000007321927],"domain_scores_gemma":[0.9998779,0.00001267106,0.00004728884,0.000014236907,0.000026099791,0.000021675487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018636361,0.00013210798,0.000112336784,0.00046605486,0.00036837888,0.00038273406,0.0001114631,0.00018289947,0.0005430748],"category_scores_gemma":[0.00040283377,0.00008356319,0.000096526725,0.00037121575,0.0002274841,0.00038491812,0.0003728102,0.00013359378,0.00013522904],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011250374,0.000046210513,0.9767526,0.00002085097,0.00003611438,0.000544756,0.0009858925,0.0033101789,0.0049341726,0.00014305228,0.00029306443,0.012820631],"study_design_scores_gemma":[0.0000022325685,0.000023677827,0.99558663,0.00001249321,0.0000154929,0.000099502264,0.000910551,0.0023316261,0.00035796803,0.00008053053,0.0005736985,0.000005508293],"about_ca_topic_score_codex":0.041369822,"about_ca_topic_score_gemma":0.08006749,"teacher_disagreement_score":0.041369822,"about_ca_system_score_codex":0.00031484442,"about_ca_system_score_gemma":0.00028064463,"threshold_uncertainty_score":0.082258046},"labels":[],"label_agreement":null},{"id":"W2993824162","doi":"10.1029/2019gl084792","title":"Nitrogen Exsolution and Bubble Formation in Titan's Lakes","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration","keywords":"Titan (rocket family); Methane; Nitrogen; Bubble; Supersaturation; Metastability; Chemical physics; Atmosphere of Titan; Astrobiology; Materials science; Chemistry; Physics; Mechanics; Organic chemistry","score_opus":0.019091801942884776,"score_gpt":0.2729167788749561,"score_spread":0.2538249769320713,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2993824162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993825,0.00004622765,0.00009192212,0.00001867187,9.788354e-7,0.0000027479616,0.000024481995,0.000005309094,0.0004272353],"genre_scores_gemma":[0.99959296,0.00001644187,0.00007989881,0.000007207556,0.0000010350328,0.0000035735018,0.000039528004,0.0000018483034,0.00025744716],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999448,0.0000071327695,0.0000020887373,0.000012266466,0.000017132963,0.0000164895],"domain_scores_gemma":[0.9999006,0.00002703878,0.000028253127,0.0000046125433,0.000021282043,0.000018151577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010235596,0.000075409975,0.00010804214,0.00018761898,0.0003937114,0.00021020653,0.00019232008,0.00019706247,0.000747868],"category_scores_gemma":[0.00019614448,0.00010084777,0.00007003354,0.0001155439,0.00038338001,0.00022027953,0.00030441963,0.00017777989,0.00005845916],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034796857,0.00004838749,0.03541735,0.000053973043,0.000016961747,0.00041183375,0.00050280226,0.0006100039,0.9595237,0.00043425034,0.00013562237,0.002497131],"study_design_scores_gemma":[0.0000404182,0.00045833446,0.5009943,0.000008063283,0.000022572793,0.00027325953,0.0010374186,0.015024904,0.4784117,0.00049681345,0.0032112484,0.000020944222],"about_ca_topic_score_codex":0.016156139,"about_ca_topic_score_gemma":0.013274394,"teacher_disagreement_score":0.016156139,"about_ca_system_score_codex":0.0007325658,"about_ca_system_score_gemma":0.00023138752,"threshold_uncertainty_score":0.03212422},"labels":[],"label_agreement":null},{"id":"W2994291709","doi":"10.1029/2019gl083758","title":"Antarctic Sea Ice Expansion, Driven by Internal Variability, in the Presence of Increasing Atmospheric CO<sub>2</sub>","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Science Foundation","keywords":"Climatology; Satellite; Environmental science; Geology; Antarctic ice sheet; Sea ice; Oceanography; Cryosphere","score_opus":0.011537756713939262,"score_gpt":0.2527420502194609,"score_spread":0.24120429350552164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994291709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979551,0.000021844004,0.0007589402,0.000051615163,0.0000084583335,0.0000026721102,0.00014955924,0.000026092686,0.0010257567],"genre_scores_gemma":[0.9996985,0.0000121089715,0.000117839314,0.000008984449,0.0000024538842,0.0000022486329,0.000078482415,0.0000045252496,0.00007479479],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996114,0.000008276825,0.0000027014062,0.000013118622,0.000004670323,0.000010072287],"domain_scores_gemma":[0.9998518,0.000041983767,0.00003645895,0.000024615963,0.000018299732,0.00002675072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020475041,0.00029143115,0.00023403695,0.00014758663,0.0002588355,0.00054075685,0.0002261819,0.00026555444,0.00086356833],"category_scores_gemma":[0.00054844655,0.00020184768,0.0005903775,0.00017326504,0.00037493804,0.00034420975,0.00040420954,0.0003262298,0.00009318511],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003432751,0.00013550205,0.33931503,0.00006449597,0.0004579715,0.00032343034,0.0001298419,0.61267155,0.037080936,0.0023236475,0.0014023847,0.0057519763],"study_design_scores_gemma":[0.000043795328,0.0000714587,0.17884558,0.0000065990785,0.00009984016,0.00006572653,0.0000710253,0.81654894,0.0028149905,0.0010692267,0.00034083368,0.000021887548],"about_ca_topic_score_codex":0.010362659,"about_ca_topic_score_gemma":0.0076120123,"teacher_disagreement_score":0.010362659,"about_ca_system_score_codex":0.00038021567,"about_ca_system_score_gemma":0.00034872442,"threshold_uncertainty_score":0.02060467},"labels":[],"label_agreement":null},{"id":"W2994437692","doi":"10.1029/2019gl084965","title":"Foraminifera Trace Anthropogenic CO<sub>2</sub> in the NW Atlantic by 1950","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Environment and Climate Change Canada; Canadian Meteorological and Oceanographic Society; Natural Sciences and Engineering Research Council of Canada; Marine Environmental Observation Prediction and Response Network","keywords":"Foraminifera; Oceanography; Climate change; Environmental science; Geology; Isotopes of carbon; Ocean current; δ13C; Total organic carbon; Stable isotope ratio; Environmental chemistry; Chemistry","score_opus":0.025635707380731457,"score_gpt":0.2955165521585836,"score_spread":0.2698808447778521,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994437692","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99823135,0.00008267178,0.000055510463,0.000037141293,0.0000035898454,9.042431e-7,0.00030554202,0.0000036098738,0.0012797406],"genre_scores_gemma":[0.99948776,0.00003214758,0.00003220549,0.000007621323,0.000002153341,6.240435e-7,0.00018777084,6.808208e-7,0.00024906194],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999604,0.0000032296261,0.000003216231,0.000012541682,0.000010222507,0.000010360727],"domain_scores_gemma":[0.99978226,0.0000183328,0.00007050357,0.000017444167,0.000082379076,0.000029022127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014752401,0.00007528467,0.00005954153,0.00034702607,0.00023784584,0.00028182307,0.000101744066,0.00013098633,0.00094209745],"category_scores_gemma":[0.00057610276,0.0000547213,0.000060314393,0.0002677548,0.00017799089,0.000223979,0.00023517842,0.00012728677,0.00014267558],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032987464,0.0000054026013,0.9909827,0.00000403479,0.000013055115,0.000021284235,0.000115414055,0.000106682135,0.0038640215,0.00009248237,0.00019677372,0.0045651956],"study_design_scores_gemma":[4.128921e-7,0.0000045815696,0.9990711,0.0000013678085,0.0000031809416,0.000008852944,0.000050686394,0.000121120116,0.0002951563,0.000014079924,0.00042880938,6.456549e-7],"about_ca_topic_score_codex":0.06288742,"about_ca_topic_score_gemma":0.111183494,"teacher_disagreement_score":0.06288742,"about_ca_system_score_codex":0.00062717433,"about_ca_system_score_gemma":0.00018960131,"threshold_uncertainty_score":0.1250428},"labels":[],"label_agreement":null},{"id":"W2994798802","doi":"10.1029/2019gl086145","title":"Subauroral Green STEVE Arcs: Evidence for Low‐Energy Excitation","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Excitation; Astrophysics; Physics; Energy spectrum; Fence (mathematics); Emission spectrum; Arc (geometry); Precipitation; Electron precipitation; Ion; Geology; Atomic physics; Geophysics; Spectral line; Atmospheric sciences; Plasma; Magnetosphere; Astronomy; Meteorology; Geometry; Nuclear physics","score_opus":0.0378305631192451,"score_gpt":0.32761773534417876,"score_spread":0.28978717222493366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2994798802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9762224,0.0006605151,0.0016145516,0.00025540715,0.000030508574,0.000012268175,0.00034209507,0.00018822038,0.020674098],"genre_scores_gemma":[0.99834967,0.00010485867,0.0004245545,0.00006278774,0.000012819322,0.0000041877515,0.00016986318,0.000028317174,0.00084288215],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999213,0.0000037144348,0.0000023596133,0.00002548322,0.000022705484,0.000024422327],"domain_scores_gemma":[0.9998447,0.000029613804,0.000048807266,0.000018111552,0.000025850912,0.000032967564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009650307,0.00019730067,0.00015891115,0.0006989774,0.0004085637,0.00075013563,0.0003455634,0.00051586895,0.004041203],"category_scores_gemma":[0.00030222908,0.00019524251,0.00010951423,0.0004201937,0.0005582902,0.00025596493,0.0005505342,0.00043353435,0.0006437549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010967621,0.00014645427,0.4795075,0.00039357215,0.00019092459,0.0031217174,0.0009902889,0.0008957229,0.43170142,0.0036397078,0.004037807,0.074278094],"study_design_scores_gemma":[0.000016300248,0.000041534007,0.97090214,0.000030900446,0.000031237894,0.0013527229,0.00034272508,0.00090998283,0.017547682,0.00088256324,0.007928417,0.000013829369],"about_ca_topic_score_codex":0.0018343114,"about_ca_topic_score_gemma":0.0035479954,"teacher_disagreement_score":0.004041203,"about_ca_system_score_codex":0.00025248746,"about_ca_system_score_gemma":0.00012504695,"threshold_uncertainty_score":0.013519168},"labels":[],"label_agreement":null},{"id":"W2995048049","doi":"10.1029/2019gl085818","title":"Magnetized Dust Clouds Penetrating the Terrestrial Bow Shock Detected by Multiple Spacecraft","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University","funders":"","keywords":"Physics; Solar wind; Magnetosheath; Interplanetary magnetic field; Interplanetary dust cloud; Bow shock (aerodynamics); Interplanetary spaceflight; Spacecraft; Interplanetary medium; Astrobiology; Coronal mass ejection; Astronomy; Magnetic cloud; Magnetopause; Solar System; Shock wave; Magnetic field; Mechanics","score_opus":0.013529563746380435,"score_gpt":0.2660584260293863,"score_spread":0.25252886228300586,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995048049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887437,0.000039366463,0.00031135065,0.00001608888,0.0000056966724,0.0000028851166,0.00008638495,0.000016580942,0.0006473208],"genre_scores_gemma":[0.9992773,0.000015609186,0.000319668,0.000009273245,0.000005957196,0.0000017412981,0.00013157868,0.0000025041093,0.00023630331],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993384,0.000005093121,0.000002350641,0.000019929901,0.000016076081,0.000022707196],"domain_scores_gemma":[0.9998062,0.000019044035,0.00006265899,0.000024035147,0.000030783816,0.0000573208],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011215237,0.00015560904,0.00019245123,0.00050142297,0.0002964007,0.00041054218,0.00020652407,0.00029698623,0.0011230262],"category_scores_gemma":[0.00019262033,0.0001523013,0.0001549843,0.0003471505,0.0001621489,0.00019398774,0.0005641766,0.00031440976,0.00015959097],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008855303,0.0000871024,0.6406343,0.000044377713,0.00017437658,0.0036722226,0.0007135775,0.0014123553,0.33364913,0.00042935944,0.00064456364,0.01765315],"study_design_scores_gemma":[0.000027199627,0.00017720865,0.9798421,0.00000809984,0.000034907698,0.0011908942,0.0005061951,0.0025809256,0.014173704,0.00015370098,0.0012945668,0.000010408219],"about_ca_topic_score_codex":0.0016009712,"about_ca_topic_score_gemma":0.0023958874,"teacher_disagreement_score":0.0016009712,"about_ca_system_score_codex":0.00019923801,"about_ca_system_score_gemma":0.00006353934,"threshold_uncertainty_score":0.0037569404},"labels":[],"label_agreement":null},{"id":"W2995237608","doi":"10.1029/2019gl085990","title":"Biophysical Consequences of a Relaxing Beaufort Gyre","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Climate Program Office; Office of Polar Programs; Office of Naval Research; National Aeronautics and Space Administration; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Downwelling; Upwelling; Oceanography; Biomass (ecology); Ocean gyre; Environmental science; Productivity; Arctic; Nutrient; Geology; Fishery; Ecology; Subtropics; Biology","score_opus":0.02500964666128758,"score_gpt":0.27631412203346845,"score_spread":0.25130447537218087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995237608","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99551034,0.000089492794,0.00043123515,0.00095893664,0.000040201805,0.0000049161977,0.0005413622,0.000051757917,0.0023716998],"genre_scores_gemma":[0.9987373,0.00003229346,0.0001654415,0.00013849465,0.000015402815,0.000003874253,0.00045985784,0.000010078665,0.0004372442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996865,0.00004403541,0.000018772052,0.00008697054,0.00003494841,0.00012883688],"domain_scores_gemma":[0.99928087,0.00008367876,0.00013193398,0.00008151537,0.00011134065,0.00031054276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00071234856,0.00043660734,0.00047046863,0.00033819766,0.00094230345,0.0020930744,0.0006775848,0.0011748569,0.0019578089],"category_scores_gemma":[0.0015763553,0.00028695175,0.00081503275,0.0003604414,0.00088042795,0.0006163113,0.0007638901,0.0007569906,0.00023276782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011466504,0.00021615195,0.6803607,0.00008446649,0.0006503702,0.0018383816,0.00075408834,0.26849183,0.017285,0.009445908,0.009675865,0.01005062],"study_design_scores_gemma":[0.00017930393,0.000202838,0.7820528,0.000036990907,0.00016066493,0.00030141315,0.00096954964,0.19837737,0.0023678155,0.0028485304,0.012374609,0.00012804476],"about_ca_topic_score_codex":0.21780095,"about_ca_topic_score_gemma":0.1391291,"teacher_disagreement_score":0.21780095,"about_ca_system_score_codex":0.0023519648,"about_ca_system_score_gemma":0.0016890173,"threshold_uncertainty_score":0.43306643},"labels":[],"label_agreement":null},{"id":"W2995719732","doi":"10.1029/2019gl085318","title":"Sources and Radiative Absorption of Water‐Soluble Brown Carbon in the High Arctic Atmosphere","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Arctic; Environmental science; Atmospheric sciences; Atmosphere (unit); Radiative transfer; Latitude; Sunrise; The arctic; Carbon fibers; Biomass burning; Absorption (acoustics); Climatology; Environmental chemistry; Aerosol; Meteorology; Chemistry; Oceanography; Geography; Geology; Materials science; Physics","score_opus":0.015093479323534331,"score_gpt":0.23614681072523028,"score_spread":0.22105333140169595,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2995719732","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989526,0.00012009949,0.00025044635,0.00000731835,0.0000033008355,0.0000013785778,0.00013963375,0.000008132707,0.0005169313],"genre_scores_gemma":[0.9994271,0.0000672664,0.00017346207,0.000005176028,0.000003898306,0.0000017975825,0.00018258678,0.0000031128059,0.00013564687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992454,0.000013056983,0.0000025020372,0.000019452325,0.00002127042,0.000019241548],"domain_scores_gemma":[0.9999021,0.000021633308,0.000017258797,0.000004845862,0.000035738623,0.000018313678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021807877,0.00033390464,0.00016874477,0.00058946945,0.0004995967,0.0004007056,0.00013252218,0.00017568642,0.0003659666],"category_scores_gemma":[0.0001355889,0.00012734321,0.00017605552,0.0005066731,0.00016251048,0.00018456005,0.00018164016,0.00019632973,0.00011203265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00066848984,0.000150069,0.5763165,0.00009738969,0.00019569235,0.00026762698,0.0004210562,0.004316925,0.4047331,0.00028156734,0.00043450625,0.012117078],"study_design_scores_gemma":[0.000005975209,0.00005433006,0.9698322,0.000005090961,0.000030681706,0.00006622313,0.0001712359,0.0038894468,0.025298296,0.000048953854,0.00058784534,0.000009727715],"about_ca_topic_score_codex":0.035301577,"about_ca_topic_score_gemma":0.033634935,"teacher_disagreement_score":0.035301577,"about_ca_system_score_codex":0.0005127327,"about_ca_system_score_gemma":0.0002511451,"threshold_uncertainty_score":0.07019216},"labels":[],"label_agreement":null},{"id":"W2996582524","doi":"10.1029/2019gl085498","title":"Anthropogenic Control Over Wintertime Oxidation of Atmospheric Pollutants","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation of Sri Lanka; Goddard Space Flight Center; National Aeronautics and Space Administration; National Science Foundation","keywords":"Particulates; Oxidizing agent; Environmental science; Ozone; Environmental chemistry; Aerosol; Pollutant; Pollution; Atmosphere (unit); Middle latitudes; Atmospheric sciences; Air pollution; Nitrogen oxide; NOx; Chemistry; Meteorology; Combustion; Geology","score_opus":0.014414514322211818,"score_gpt":0.2676707036511786,"score_spread":0.2532561893289668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996582524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985002,0.00015323136,0.00029891232,0.000035807738,0.000007920709,0.0000025754318,0.00021285312,0.000017481649,0.0007709392],"genre_scores_gemma":[0.99947745,0.000056535126,0.00006879934,0.000011070734,0.0000060516945,0.000001806934,0.00018549622,0.0000043642085,0.00018852016],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999144,0.00001304596,0.0000059760896,0.00003066171,0.00001534685,0.00002051725],"domain_scores_gemma":[0.9998173,0.000025680463,0.000065158194,0.000016328137,0.000044570854,0.000030885523],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015552597,0.0002280296,0.00013678451,0.0002012456,0.00016016219,0.0004147854,0.000126691,0.00012804897,0.00064081117],"category_scores_gemma":[0.00015530782,0.00007505443,0.00015906047,0.0001834729,0.00018121168,0.00015137615,0.00018986725,0.00010788288,0.00010433484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007585493,0.00007031489,0.51245177,0.00009191928,0.00019483991,0.00016903254,0.0001829814,0.0026410671,0.4691748,0.00036015426,0.00032839924,0.013576165],"study_design_scores_gemma":[0.000005195205,0.00007097582,0.98630434,0.00000399861,0.000017647642,0.000029523168,0.000107049644,0.001470963,0.010920776,0.00009055471,0.0009749896,0.0000041688313],"about_ca_topic_score_codex":0.014041759,"about_ca_topic_score_gemma":0.016587056,"teacher_disagreement_score":0.014041759,"about_ca_system_score_codex":0.00040046635,"about_ca_system_score_gemma":0.0001974437,"threshold_uncertainty_score":0.027920067},"labels":[],"label_agreement":null},{"id":"W2996978505","doi":"10.1029/2019gl084414","title":"Contribution of Snow Cover Decline to Projected Warming Over North America","year":2019,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Snow; Snow cover; Environmental science; Climatology; Global warming; Climate change; Current (fluid); Physical geography; Snow line; Geography; Geology; Meteorology; Oceanography","score_opus":0.024895480012481055,"score_gpt":0.31127522331785495,"score_spread":0.2863797433053739,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2996978505","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736136,0.00013458656,0.00027397432,0.00032517145,0.0000069310117,0.000003843001,0.0005658921,0.000018722641,0.001309534],"genre_scores_gemma":[0.9993088,0.00008935083,0.00009094054,0.000026239077,0.000004669596,0.0000051485317,0.00028804978,0.000002241997,0.00018460325],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999169,0.0000211268,0.0000045038387,0.000020570276,0.000017544877,0.000019305144],"domain_scores_gemma":[0.9997539,0.000042293977,0.000054620683,0.000012613693,0.00010359669,0.00003299936],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034360174,0.00018913709,0.0001488284,0.00021571915,0.0002811398,0.0004928276,0.00019798758,0.00033681808,0.0012744525],"category_scores_gemma":[0.0006540973,0.00011075588,0.00024789022,0.00024038258,0.00019261094,0.00033862446,0.00028566498,0.00028361363,0.00010677621],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042436706,0.00007012578,0.91551954,0.000119247925,0.00020627474,0.00030865087,0.00038235,0.050956078,0.013660928,0.0013063592,0.0013913782,0.015654722],"study_design_scores_gemma":[0.000015304573,0.000091450944,0.9622187,0.000014885838,0.00004473998,0.00010222016,0.00038842845,0.033346068,0.0011015642,0.00072981976,0.0019374619,0.000009376147],"about_ca_topic_score_codex":0.03899239,"about_ca_topic_score_gemma":0.049491074,"teacher_disagreement_score":0.9610076,"about_ca_system_score_codex":0.0010379466,"about_ca_system_score_gemma":0.0005535616,"threshold_uncertainty_score":0.07753086},"labels":[],"label_agreement":null},{"id":"W2997062356","doi":"10.1029/2019gl085271","title":"A New Substorm Onset Mechanism: Increasingly Parallel Pressure Anisotropic Ballooning","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Substorm; Ballooning; Physics; Instability; Anisotropy; Geophysics; Gyroradius; Magnetosphere; Isotropy; Dipole; Plasma; Mechanics; Tokamak; Nuclear physics; Optics","score_opus":0.02112429992387169,"score_gpt":0.26857944189341737,"score_spread":0.24745514196954568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997062356","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99300414,0.00008675403,0.0034568794,0.00008548082,0.000011382408,0.000017027238,0.00006518032,0.00021468407,0.0030586268],"genre_scores_gemma":[0.9994215,0.000016263666,0.0003047384,0.000011411305,0.000006977228,0.0000029766693,0.000022192455,0.0000074159525,0.0002064405],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992955,0.00000503724,0.0000039525535,0.000017673077,0.000012440423,0.000031424588],"domain_scores_gemma":[0.99977726,0.000031336313,0.00006862121,0.000042228225,0.000030781335,0.00004984335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010424345,0.00015684904,0.00019102744,0.00029040605,0.00029166968,0.0005547257,0.00024180501,0.00023013822,0.0023768095],"category_scores_gemma":[0.00035354967,0.00012780317,0.00019943113,0.00012116419,0.00029181986,0.00046288234,0.00051446917,0.0003524388,0.00021156922],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000352714,0.00007921989,0.10247396,0.000088443296,0.000047325655,0.0012842811,0.0004996081,0.003162753,0.8720459,0.006212099,0.00065470545,0.013098981],"study_design_scores_gemma":[0.00012191789,0.00060045184,0.64782053,0.00003407665,0.00007351254,0.0028928781,0.0007063695,0.09407073,0.23866914,0.0075967233,0.0073490613,0.000064561485],"about_ca_topic_score_codex":0.001054358,"about_ca_topic_score_gemma":0.00078466366,"teacher_disagreement_score":0.0023768095,"about_ca_system_score_codex":0.00026460542,"about_ca_system_score_gemma":0.00009798543,"threshold_uncertainty_score":0.0079512},"labels":[],"label_agreement":null},{"id":"W2997107098","doi":"10.1029/2019gl086577","title":"September 2019 Antarctic Sudden Stratospheric Warming: Quasi‐6‐Day Wave Burst and Ionospheric Effects","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":179,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Goddard Space Flight Center; European Space Agency; Deutsche Forschungsgemeinschaft; National Aeronautics and Space Administration","keywords":"Sudden stratospheric warming; Stratosphere; Ionosphere; Thermosphere; Atmospheric sciences; Atmosphere (unit); Polar vortex; Mesosphere; Middle latitudes; Rossby wave; Geology; Environmental science; Climatology; Geophysics; Physics; Meteorology","score_opus":0.02747168848171822,"score_gpt":0.2646145808660676,"score_spread":0.23714289238434938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997107098","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99157095,0.0003977472,0.00013533948,0.00082294113,0.00016544826,0.0000147708315,0.0028959934,0.000034299024,0.003962453],"genre_scores_gemma":[0.9976553,0.00018277467,0.000046296704,0.00009028117,0.000086909626,0.000004567042,0.0011499054,0.000004832474,0.0007791193],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999951,0.0000065389486,0.0000041244416,0.00000769472,0.000013816116,0.000016730866],"domain_scores_gemma":[0.9997737,0.000032228654,0.000075738826,0.000020217149,0.000040717376,0.000057459267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016789557,0.00014508191,0.00013030563,0.00032340502,0.00026186206,0.00038278202,0.000086214306,0.00022493971,0.0032217063],"category_scores_gemma":[0.0003509585,0.000047788075,0.00015161162,0.0003089899,0.00016678424,0.00015151636,0.00038612157,0.00025089143,0.00030844627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014481264,0.00008464108,0.9407144,0.00012121441,0.00015915064,0.0016843687,0.00027530544,0.00095342426,0.021748176,0.0006066954,0.0075997636,0.024604788],"study_design_scores_gemma":[0.000011551452,0.0000930726,0.9943585,0.000009238923,0.000018749928,0.0001655985,0.00012365387,0.00032674908,0.0011446237,0.00012916936,0.0036143018,0.000004858014],"about_ca_topic_score_codex":0.0059261457,"about_ca_topic_score_gemma":0.009414542,"teacher_disagreement_score":0.0059261457,"about_ca_system_score_codex":0.00029422462,"about_ca_system_score_gemma":0.0001482822,"threshold_uncertainty_score":0.011783302},"labels":[],"label_agreement":null},{"id":"W2997516851","doi":"10.1029/2019gl084787","title":"Assessing Energy Budget of Laboratory Fault Slip Using Rotary Shear Experiments and Micro‐Computed Tomography","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Science Foundation","keywords":"Energy budget; Shear (geology); Energy (signal processing); Tomography; Slip (aerodynamics); Seismology; Computed tomography; Geology; Fault (geology); Physics; Engineering; Aerospace engineering; Statistics; Optics; Petrology; Mathematics; Radiology; Medicine","score_opus":0.056453853587233344,"score_gpt":0.31053803959683957,"score_spread":0.25408418600960625,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997516851","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99801505,0.00006514385,0.0015399804,0.0000080948785,0.0000021244455,0.000008959103,0.00011714704,0.0000104767105,0.0002329136],"genre_scores_gemma":[0.99875486,0.000046832567,0.0009850273,0.0000055253313,0.0000015812384,0.000013873311,0.000084556435,0.0000034291927,0.0001043201],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99982435,0.000023708892,0.000017201328,0.00003600565,0.00006653681,0.00003229656],"domain_scores_gemma":[0.9997032,0.000085244996,0.00009847768,0.00003924186,0.000048150425,0.000025664753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030981522,0.0002901379,0.00021209274,0.0003401588,0.00020021877,0.00024362787,0.00023078028,0.0002250577,0.0011055871],"category_scores_gemma":[0.00043721,0.00014622422,0.00015112665,0.0002773458,0.0004335879,0.00025799658,0.00023160405,0.00023011542,0.000083744024],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023104897,0.000067334884,0.012561735,0.000037836773,0.000019626352,0.00005901209,0.00003707601,0.0021859072,0.98247623,0.00010897714,0.000028935941,0.0021861189],"study_design_scores_gemma":[0.000030573443,0.0013703466,0.12219449,0.000009652636,0.000041781135,0.0001855807,0.00021514602,0.02534305,0.8499569,0.00013661123,0.0004927852,0.00002299737],"about_ca_topic_score_codex":0.0012485529,"about_ca_topic_score_gemma":0.0016727161,"teacher_disagreement_score":0.0012485529,"about_ca_system_score_codex":0.00020806295,"about_ca_system_score_gemma":0.00013811151,"threshold_uncertainty_score":0.0036985278},"labels":[],"label_agreement":null},{"id":"W2997662506","doi":"10.1029/2019gl085897","title":"Burial and Origin of Permafrost‐Derived Carbon in the Nearshore Zone of the Southern Canadian Beaufort Sea","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Daimler und Benz Stiftung","keywords":"Permafrost; Geology; Arctic; Oceanography; Total organic carbon; Sedimentary rock; Earth science; Organic matter; Erosion; Coastal erosion; Carbon fibers; Environmental science; Geomorphology; Paleontology; Ecology","score_opus":0.06688804068865296,"score_gpt":0.27869709508195445,"score_spread":0.2118090543933015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2997662506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978149,0.00023403575,0.00008626304,0.000045109136,0.0000015147432,0.0000027943574,0.0003821445,0.000009072387,0.0014240972],"genre_scores_gemma":[0.9988404,0.00010605519,0.00016014207,0.0000118146845,7.30535e-7,0.0000018026783,0.00029084753,0.0000033702436,0.00058486883],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986887,0.0000060816387,0.0000028343836,0.00004019436,0.00003672864,0.00004530108],"domain_scores_gemma":[0.99982005,0.000014430925,0.00002846759,0.000007694504,0.000089139445,0.00004020766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018244034,0.00028666708,0.00022486209,0.0011335507,0.002151243,0.00081409863,0.0006379058,0.00030539988,0.001332489],"category_scores_gemma":[0.0002964024,0.00019518983,0.000263741,0.001282645,0.0007683182,0.00031663396,0.0004914032,0.00019812562,0.00015652394],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013886146,0.00002215159,0.9670862,0.000041874286,0.00009070275,0.00033633204,0.0009999999,0.0056323404,0.0092105735,0.0006668297,0.0006494284,0.015124696],"study_design_scores_gemma":[0.0000026648029,0.0000057044576,0.9969901,0.00000889775,0.0000076272745,0.000030750467,0.00036671016,0.001425661,0.0002758598,0.000044216526,0.00083160657,0.000010205233],"about_ca_topic_score_codex":0.984027,"about_ca_topic_score_gemma":0.9918305,"teacher_disagreement_score":0.015972972,"about_ca_system_score_codex":0.010324654,"about_ca_system_score_gemma":0.0074235997,"threshold_uncertainty_score":0.074911},"labels":[],"label_agreement":null},{"id":"W2998858885","doi":"10.1029/2019gl085455","title":"Long‐Term SST Variability on the Northwest Atlantic Continental Shelf and Slope","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":87,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration","keywords":"Continental shelf; Climatology; Geology; Cape; Sea surface temperature; Oceanography; Structural basin; Zonal and meridional; Geography; Geomorphology","score_opus":0.04217350362933211,"score_gpt":0.2853713872917566,"score_spread":0.24319788366242448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2998858885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984591,0.000041590098,0.000032459448,0.000026190202,0.0000020668117,8.279038e-7,0.0009177731,0.0000040980476,0.00051596214],"genre_scores_gemma":[0.9986034,0.000044696983,0.000029332543,0.0000050396397,0.0000023625068,0.0000012722218,0.0011370305,0.0000013336484,0.00017550217],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992514,0.00000921236,0.0000076152837,0.000021964304,0.000020117632,0.00001589905],"domain_scores_gemma":[0.99951947,0.00005971579,0.00015406068,0.000039371982,0.00015859073,0.00006883892],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018831957,0.00011365194,0.00011681994,0.0004613263,0.0002370146,0.00055144064,0.00012950851,0.00012771289,0.0007799032],"category_scores_gemma":[0.0005728954,0.00007895149,0.00020921577,0.0007678655,0.00016506309,0.0002703371,0.00024348484,0.00015400966,0.00016928738],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018679872,0.00000768937,0.99636215,0.0000033071353,0.000032530024,0.00003794328,0.00006371659,0.0004696695,0.0008274488,0.000028690734,0.00018995538,0.00195829],"study_design_scores_gemma":[3.8258028e-7,0.0000021035698,0.999527,0.0000018202795,0.000002724642,0.000005669513,0.00003723056,0.0002702266,0.00003159394,0.0000051745515,0.00011531735,8.8025644e-7],"about_ca_topic_score_codex":0.15140305,"about_ca_topic_score_gemma":0.32800034,"teacher_disagreement_score":0.15140305,"about_ca_system_score_codex":0.0006897338,"about_ca_system_score_gemma":0.00041866535,"threshold_uncertainty_score":0.30104363},"labels":[],"label_agreement":null},{"id":"W2999290257","doi":"10.1029/2019gl086239","title":"Spaceborne Measurements of Formic and Acetic Acids: A Global View of the Regional Sources","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Isoprene; Seasonality; Environmental science; Northern Hemisphere; Formic acid; Atmosphere (unit); Atmospheric sciences; Nadir; Abundance (ecology); Tropics; Climatology; Chemistry; Environmental chemistry; Satellite; Meteorology; Geology; Geography; Organic chemistry; Physics; Ecology; Biology","score_opus":0.07706800912911663,"score_gpt":0.28528175261790206,"score_spread":0.20821374348878544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W2999290257","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99386436,0.0005674342,0.00089070335,0.00008855912,0.000012705843,0.000007820113,0.0017175667,0.00004725248,0.0028035084],"genre_scores_gemma":[0.99672407,0.0002303632,0.001435437,0.000021739132,0.000022093207,0.0000038507665,0.0012676406,0.000008926565,0.00028588675],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999435,0.000005073266,0.0000025288302,0.000024830195,0.000011165534,0.000012885593],"domain_scores_gemma":[0.9998864,0.000012438273,0.000025600026,0.000018255429,0.000042118205,0.000015237539],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020230818,0.00027340295,0.00014623496,0.00082657736,0.00016771605,0.00036799433,0.0001494718,0.00021858796,0.00068775355],"category_scores_gemma":[0.00019019775,0.000092361224,0.00021296978,0.000958563,0.0001660429,0.000419334,0.00033477577,0.00014322504,0.00016872867],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003098994,0.000077070865,0.8243594,0.000112525784,0.00030505323,0.0001857159,0.0002692332,0.009755966,0.10563941,0.00054027676,0.0013547252,0.057090644],"study_design_scores_gemma":[0.000012780473,0.000055110508,0.9844358,0.000016373435,0.00008879456,0.000057068944,0.00025058782,0.0065456056,0.0054775816,0.0002108202,0.0028354477,0.000014025363],"about_ca_topic_score_codex":0.009738881,"about_ca_topic_score_gemma":0.011987268,"teacher_disagreement_score":0.009738881,"about_ca_system_score_codex":0.00021157709,"about_ca_system_score_gemma":0.00016973495,"threshold_uncertainty_score":0.019364417},"labels":[],"label_agreement":null},{"id":"W3000104457","doi":"10.1029/2019gl085721","title":"Episodic Lithospheric Deformation in Eastern Tibet Inferred From Seismic Anisotropy","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Geology; Crust; Lithosphere; Seismology; Anisotropy; Plateau (mathematics); Upwelling; Geophysics; Seismic anisotropy; Mantle (geology); Tectonics","score_opus":0.03866680216127294,"score_gpt":0.27245319373371835,"score_spread":0.2337863915724454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000104457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99938846,0.000025853684,0.0001817365,0.000012617383,0.0000012306913,9.875124e-7,0.00014806839,0.0000079433385,0.00023318143],"genre_scores_gemma":[0.9997224,0.000015070678,0.00005471421,0.0000016520858,0.0000021058038,7.2491525e-7,0.00016782977,8.522777e-7,0.00003454124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999515,0.000011825921,0.0000048312518,0.000011435554,0.0000070414394,0.00001337388],"domain_scores_gemma":[0.9998652,0.000026625165,0.000035696194,0.000014634913,0.000025538107,0.000032375905],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027034793,0.00021286198,0.00016405963,0.0008148902,0.0002566749,0.00043209796,0.00016237526,0.00022384537,0.0006328971],"category_scores_gemma":[0.00039717258,0.00012885971,0.00017677143,0.0010450731,0.0002088349,0.00020900341,0.000247641,0.00013674356,0.00009606384],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023297995,0.000028198252,0.9685801,0.000022031723,0.000061027305,0.00028409512,0.00025748622,0.009578313,0.011267691,0.00020464223,0.00014237664,0.009341016],"study_design_scores_gemma":[0.000009530983,0.000021714015,0.98337054,0.0000055409537,0.000018017885,0.000042852284,0.000087296525,0.01589966,0.00030074807,0.00012040728,0.000117690535,0.000005882608],"about_ca_topic_score_codex":0.016780265,"about_ca_topic_score_gemma":0.015925279,"teacher_disagreement_score":0.016780265,"about_ca_system_score_codex":0.00043929112,"about_ca_system_score_gemma":0.00026041525,"threshold_uncertainty_score":0.03336519},"labels":[],"label_agreement":null},{"id":"W3000718560","doi":"10.1029/2019gl086421","title":"Two Decades of Ocean Acidification in the Surface Waters of the Beaufort Gyre, Arctic Ocean: Effects of Sea Ice Melt and Retreat From 1997–2016","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":66,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Aragonite; Oceanography; Canada Basin; Sea ice; Geology; Ocean acidification; Arctic sea ice decline; Arctic ice pack; Antarctic sea ice; Arctic; Ocean gyre; Seawater; Environmental science; Calcite; Mineralogy","score_opus":0.022813654956977878,"score_gpt":0.26849421148039804,"score_spread":0.24568055652342016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000718560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985598,0.00023759718,0.000016491176,0.00013066879,0.00001311255,0.0000021740086,0.00069976394,0.0000045744578,0.0003359775],"genre_scores_gemma":[0.9985851,0.000094814815,0.000022986625,0.000044485496,0.000013983398,0.0000028768393,0.00094563735,0.0000016541926,0.0002886086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980134,0.000021964266,0.000016086127,0.00004686188,0.000034612982,0.000079156875],"domain_scores_gemma":[0.9994154,0.000050674564,0.00020799368,0.000028857256,0.00015833696,0.00013874234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005133002,0.00027190772,0.0002975982,0.00066155335,0.00048461644,0.00088335515,0.0002711722,0.00057621585,0.0009655719],"category_scores_gemma":[0.00065214897,0.00018951944,0.00058815174,0.00082720886,0.00041998006,0.00041594656,0.0005597595,0.00034899462,0.00017901893],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003578187,0.000047753198,0.9937344,0.000023702145,0.00014765885,0.00021633235,0.00048354152,0.00033769532,0.0012500742,0.000030159385,0.00062627223,0.0027445469],"study_design_scores_gemma":[0.0000013154698,0.000013918381,0.9994722,0.0000030840883,0.000008447457,0.000013045092,0.0001622218,0.0000783983,0.00004128649,0.000003205975,0.00020078348,0.0000021793758],"about_ca_topic_score_codex":0.31481084,"about_ca_topic_score_gemma":0.3547666,"teacher_disagreement_score":0.31481084,"about_ca_system_score_codex":0.0015982441,"about_ca_system_score_gemma":0.0014819871,"threshold_uncertainty_score":0.6259569},"labels":[],"label_agreement":null},{"id":"W3000941914","doi":"10.1029/2019gl085576","title":"Oxygen Isotopes in Authigenic Clay Minerals: Toward Building a Reliable Salinity Proxy","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Division of Earth Sciences; American Chemical Society Petroleum Research Fund; National Geographic Society; National Science Foundation","keywords":"Authigenic; Geology; Clay minerals; Geochemistry; Isotopes of oxygen; Sedimentary rock; Carbonate; Pleistocene; Carbonate minerals; Earth science; Mineralogy; Paleontology; Calcite; Chemistry","score_opus":0.07233924902883995,"score_gpt":0.3243132374704305,"score_spread":0.2519739884415906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3000941914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.95725924,0.0008514944,0.039141633,0.00016740379,0.000018632858,0.000023904353,0.0009960547,0.00021259686,0.0013290796],"genre_scores_gemma":[0.9748243,0.00020288829,0.02441488,0.00002167058,0.000013867252,0.000011615287,0.0002843372,0.00002306735,0.00020330666],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9997899,0.000072113864,0.000017549557,0.000063608226,0.000039875682,0.000016958204],"domain_scores_gemma":[0.99945325,0.00012815912,0.00014984448,0.00006863077,0.00015318583,0.00004687604],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078332867,0.00057460484,0.0003382157,0.0013113905,0.00022848009,0.0008776017,0.0004255463,0.000513231,0.0004392383],"category_scores_gemma":[0.0017251397,0.00032433597,0.00012802955,0.0009707508,0.0004041683,0.00076308724,0.0007371728,0.00043613292,0.00021491745],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002460868,0.00007738187,0.6819666,0.00016791027,0.00015850979,0.00012650875,0.0002711081,0.018154435,0.2501033,0.0030227297,0.00037338596,0.04533204],"study_design_scores_gemma":[0.000100105484,0.00020917704,0.52065516,0.00012056741,0.00014708548,0.00019656794,0.00044852443,0.3118503,0.15109634,0.0064268964,0.008625099,0.00012429147],"about_ca_topic_score_codex":0.0035983797,"about_ca_topic_score_gemma":0.0070251385,"teacher_disagreement_score":0.0035983797,"about_ca_system_score_codex":0.00044442955,"about_ca_system_score_gemma":0.00031700215,"threshold_uncertainty_score":0.007154882},"labels":[],"label_agreement":null},{"id":"W3001443281","doi":"10.1029/2019gl086879","title":"Characterization of Pore Water Flow in 3‐D Heterogeneous Permeability Fields","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University; Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Aquifer; Multifractal system; Vortex; Advection; Groundwater flow; Groundwater; Geology; Porous medium; Permeability (electromagnetism); Soil science; Geophysics; Mechanics; Hydrology (agriculture); Porosity; Fractal; Geotechnical engineering; Physics; Thermodynamics; Mathematics","score_opus":0.030443768491379437,"score_gpt":0.26977908151787205,"score_spread":0.2393353130264926,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3001443281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99407876,0.000012074985,0.00568712,0.000009643171,8.8701387e-7,0.0000036395916,0.000034710036,0.000033878634,0.00013936561],"genre_scores_gemma":[0.99921036,0.0000046396444,0.00075446174,9.72643e-7,3.4188662e-7,0.0000015959339,0.000015589918,0.000001343979,0.0000105941845],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996865,0.000007683459,0.0000017677586,0.0000062745266,0.0000060482403,0.000009544527],"domain_scores_gemma":[0.99969506,0.00016622958,0.000059146983,0.000027602287,0.000025062183,0.000027042326],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018731582,0.00011137427,0.00011630132,0.00038780094,0.00015625687,0.00027820413,0.00012827432,0.0001902362,0.00023448546],"category_scores_gemma":[0.00049091375,0.0000982136,0.00016783028,0.00019452968,0.00032428556,0.00019889903,0.00013675583,0.00013707635,0.000017216988],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018191844,0.00010997447,0.049155187,0.00003623247,0.000043715878,0.00021527313,0.00018312279,0.7940861,0.14464957,0.0031265118,0.00010869468,0.00810369],"study_design_scores_gemma":[0.000008217937,0.00003234984,0.02842609,0.0000022041822,0.000005385622,0.000034994533,0.000025247766,0.96080977,0.009926504,0.0006282455,0.00009221071,0.000008832954],"about_ca_topic_score_codex":0.002061455,"about_ca_topic_score_gemma":0.001374739,"teacher_disagreement_score":0.002061455,"about_ca_system_score_codex":0.00026900528,"about_ca_system_score_gemma":0.00020967187,"threshold_uncertainty_score":0.0040988326},"labels":[],"label_agreement":null},{"id":"W3003486441","doi":"10.1029/2019gl085497","title":"Stripe Mystery in GRACE Geopotential Models Revealed","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geodesy; Geopotential; Geoid; Geology; Parallels; Sampling (signal processing); Gravitation; Nyquist frequency; Latitude; Physics; Geophysics; Computer science; Classical mechanics; Optics; Bandwidth (computing)","score_opus":0.10142320396770678,"score_gpt":0.28933343710582315,"score_spread":0.1879102331381164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003486441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9337884,0.00011574682,0.058788452,0.0009532754,0.00008331137,0.000017119795,0.00058730994,0.00091101695,0.004755433],"genre_scores_gemma":[0.99693954,0.000020792184,0.0024289188,0.000038662154,0.000013699519,0.0000052099713,0.00021058481,0.00006130273,0.000281291],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998456,0.000051913907,0.000011618265,0.000031977037,0.00003641907,0.000022371692],"domain_scores_gemma":[0.99930537,0.00017984834,0.0001209375,0.00023146783,0.00011473863,0.000047666428],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008398148,0.00016292195,0.00025421943,0.00029197236,0.0002735831,0.0006840719,0.0003678863,0.0004169561,0.0009754072],"category_scores_gemma":[0.004274006,0.00017735896,0.00022114527,0.00038543457,0.0004557853,0.00087292923,0.0004694083,0.0006060093,0.00013861075],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006736126,0.00011499215,0.10011364,0.0000656166,0.00014944434,0.00046640335,0.00046421148,0.7768,0.022934726,0.053676084,0.008622199,0.035919033],"study_design_scores_gemma":[0.000013131137,0.000023961005,0.007857621,0.000005995607,0.0000069028165,0.00003922971,0.00003052208,0.9846506,0.0012780349,0.005321168,0.00076210947,0.000010834166],"about_ca_topic_score_codex":0.0044592894,"about_ca_topic_score_gemma":0.0031534636,"teacher_disagreement_score":0.0044592894,"about_ca_system_score_codex":0.00029034624,"about_ca_system_score_gemma":0.00036327186,"threshold_uncertainty_score":0.008866668},"labels":[],"label_agreement":null},{"id":"W3003704886","doi":"10.1029/2019gl086426","title":"Constraining Reanalysis Snowfall Over the Arctic Ocean Using CloudSat Observations","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Waterloo; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Snow; Environmental science; Arctic; Climatology; Sea ice; Arctic ice pack; Range (aeronautics); Meteorology; Geology; Oceanography; Geography","score_opus":0.09855120243962948,"score_gpt":0.2994285829362016,"score_spread":0.20087738049657214,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003704886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9826094,0.00021303039,0.010442916,0.00007527965,0.00004392007,0.000033448814,0.0038924504,0.0004492785,0.002240352],"genre_scores_gemma":[0.9847718,0.00016418926,0.0105590895,0.000019761017,0.00001590129,0.000021563765,0.004080584,0.00006013671,0.00030701899],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998325,0.00003347633,0.000013497723,0.00004431363,0.000050413335,0.000025788473],"domain_scores_gemma":[0.9997054,0.000045593657,0.000059129998,0.00004347948,0.00012628072,0.000020035332],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056629296,0.00041014122,0.00020368083,0.00065784703,0.0003379198,0.00084958435,0.0002766127,0.00022740648,0.0004161415],"category_scores_gemma":[0.0011997614,0.00017774192,0.00044912295,0.0010037425,0.00015690304,0.00050688686,0.00030181443,0.00021687115,0.00024157295],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022957622,0.00012376986,0.58144313,0.00008430002,0.00042832602,0.0001876665,0.00025596158,0.33260018,0.017680714,0.00091103604,0.0030367086,0.063018635],"study_design_scores_gemma":[0.000077677316,0.000060154573,0.42194188,0.00008323051,0.00010723917,0.000041465923,0.00029385395,0.5560409,0.014058518,0.0007860101,0.0064661372,0.000042962583],"about_ca_topic_score_codex":0.1618397,"about_ca_topic_score_gemma":0.18915147,"teacher_disagreement_score":0.1618397,"about_ca_system_score_codex":0.0006465846,"about_ca_system_score_gemma":0.0014446382,"threshold_uncertainty_score":0.32179534},"labels":[],"label_agreement":null},{"id":"W3003969367","doi":"10.1029/2019gl085590","title":"Multi‐Instrument Observations of Ion‐Neutral Coupling in the Dayside Cusp","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Science and Technology Facilities Council; Japan Society for the Promotion of Science; Natural Environment Research Council; Sight Research UK; Lancaster University","keywords":"Ionosphere; Physics; Interplanetary magnetic field; Solar wind; Geophysics; Substorm; Cusp (singularity); Daytime; Plasma; Interplanetary spaceflight; Doppler effect; Joule heating; Convection; Magnetic reconnection; Astrophysics; Atmospheric sciences; Magnetosphere; Astronomy; Meteorology","score_opus":0.06656844741343433,"score_gpt":0.307901107355886,"score_spread":0.24133265994245168,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3003969367","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985879,0.000053115225,0.00016797667,0.000011966967,0.0000036412598,0.000002356161,0.000094475974,0.000010964615,0.0010674701],"genre_scores_gemma":[0.99915445,0.00002747268,0.00029512544,0.000010443088,0.00000670006,0.0000027191368,0.00020517744,0.000004634309,0.00029334362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.0000059268496,0.000002188013,0.000018497654,0.000021304746,0.000017162718],"domain_scores_gemma":[0.99984264,0.000023579623,0.000037333102,0.000016847162,0.000032116917,0.000047519356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016236195,0.00013965645,0.00020673664,0.00043106818,0.00034574926,0.0003241749,0.00018300554,0.00020707933,0.0005244099],"category_scores_gemma":[0.00032926758,0.00013040856,0.000130527,0.00022319365,0.00012558013,0.00017989383,0.00056859216,0.0002860247,0.000101871534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010718772,0.00012360283,0.60603625,0.000058863865,0.00015266608,0.0006021603,0.00093462167,0.0013517563,0.36598903,0.0003903538,0.0008157328,0.022473056],"study_design_scores_gemma":[0.000010714198,0.000059728973,0.9945167,0.000004958295,0.00001485764,0.00013534584,0.00011471294,0.0010209063,0.0032875105,0.000052497177,0.0007762936,0.0000057986485],"about_ca_topic_score_codex":0.0023551434,"about_ca_topic_score_gemma":0.0064357477,"teacher_disagreement_score":0.0023551434,"about_ca_system_score_codex":0.00015470479,"about_ca_system_score_gemma":0.000086522,"threshold_uncertainty_score":0.0046828985},"labels":[],"label_agreement":null},{"id":"W3004007419","doi":"10.1029/2019gl086361","title":"Assessing the Impact of Initialization on Decadal Prediction Skill","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Initialization; Climatology; Forcing (mathematics); Component (thermodynamics); Forecast skill; Variance (accounting); Environmental science; Variance components; Econometrics; Climate model; Computer science; Meteorology; Statistics; Climate change; Mathematics; Geology; Economics; Geography; Oceanography","score_opus":0.09465040196608768,"score_gpt":0.39713392548025855,"score_spread":0.30248352351417085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004007419","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98560345,0.00015694389,0.011482983,0.00013056723,0.000027311175,0.000022016586,0.00040491877,0.00013668525,0.0020351026],"genre_scores_gemma":[0.998168,0.00002170195,0.001286902,0.000019916193,0.000007394596,0.00000782767,0.00033895942,0.000020621825,0.0001286591],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99891067,0.00044531564,0.000109988774,0.00020657657,0.00020869236,0.000118672426],"domain_scores_gemma":[0.9804458,0.013347559,0.0017615618,0.0015585683,0.002308946,0.00057758234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0062528187,0.00033409477,0.00030955512,0.00052669365,0.00028685544,0.0014392677,0.00035353616,0.0004678112,0.0008185351],"category_scores_gemma":[0.02567617,0.00024321963,0.0003573874,0.00046262387,0.0004251449,0.0011420143,0.0009935659,0.00068835745,0.00015005888],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010502097,0.00011569611,0.6191162,0.00005494074,0.00042555993,0.00019267107,0.00018446376,0.3265316,0.0061234105,0.0022865662,0.00076034106,0.043158375],"study_design_scores_gemma":[0.000049055656,0.00034115507,0.38758954,0.00004263102,0.000104257284,0.000067682406,0.000108089356,0.6003517,0.009303652,0.001181049,0.0008090213,0.00005217945],"about_ca_topic_score_codex":0.011476741,"about_ca_topic_score_gemma":0.009457435,"teacher_disagreement_score":0.011476741,"about_ca_system_score_codex":0.0008991949,"about_ca_system_score_gemma":0.0008082172,"threshold_uncertainty_score":0.033068478},"labels":[],"label_agreement":null},{"id":"W3004592083","doi":"10.1029/2019gl086465","title":"An Experimental Assessment of the Importance of S(IV) Oxidation by Hypohalous Acids in the Marine Atmosphere","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Atmosphere (unit); Sulfate; Aerosol; Chemistry; Kinetics; Environmental chemistry; Atmospheric chemistry; Sulfate aerosol; Scavenging; Salt (chemistry); Ozone; Meteorology; Organic chemistry","score_opus":0.02686547122720386,"score_gpt":0.30354817975100123,"score_spread":0.2766827085237974,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3004592083","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99825996,0.00007329716,0.00095980056,0.000022339773,0.00000935707,0.000016020469,0.00012782545,0.0000115717185,0.000519662],"genre_scores_gemma":[0.9983419,0.000099706675,0.0010579638,0.000018448241,0.0000064665246,0.000014680041,0.000109344815,0.0000044556405,0.00034698113],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998447,0.000035583464,0.000010297355,0.00003626118,0.000043689175,0.000029446805],"domain_scores_gemma":[0.99972576,0.000117400006,0.000041079235,0.000028559587,0.000062785184,0.000024387946],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028849364,0.0002519601,0.00009458899,0.00009133717,0.00022609739,0.00025282663,0.00024544928,0.00033462868,0.001027523],"category_scores_gemma":[0.00041014867,0.00010544526,0.00017223736,0.00007161474,0.00030295493,0.00021140507,0.00021751187,0.00033851634,0.00012734796],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018173608,0.000035902278,0.001808605,0.000022748865,0.0000068955646,0.000015819836,0.000027873344,0.0003182172,0.99694437,0.00006855636,0.000022865055,0.0005464833],"study_design_scores_gemma":[0.000014149827,0.00048468105,0.005040133,0.0000020566317,0.000009068844,0.0000141197925,0.000045448687,0.0032214366,0.9908313,0.00004283396,0.00029061554,0.000004027135],"about_ca_topic_score_codex":0.0032595433,"about_ca_topic_score_gemma":0.0017931858,"teacher_disagreement_score":0.0032595433,"about_ca_system_score_codex":0.00036164955,"about_ca_system_score_gemma":0.0001852178,"threshold_uncertainty_score":0.006481111},"labels":[],"label_agreement":null},{"id":"W3005406355","doi":"10.1029/2019gl085707","title":"Airborne Mapping Reveals Emergent Power Law of Arctic Methane Emissions","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":76,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Permafrost; Environmental science; Arctic; Hotspot (geology); Greenhouse gas; Ecotone; Physical geography; Atmospheric sciences; Methane; Wetland; Power law; Climatology; Geology; Geography; Oceanography; Ecology","score_opus":0.033898192318632295,"score_gpt":0.28444065005704106,"score_spread":0.2505424577384088,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005406355","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99753535,0.000032127347,0.0013068223,0.000017302915,0.0000019041585,0.0000016041674,0.00021469328,0.000041570525,0.0008486087],"genre_scores_gemma":[0.99901557,0.000017035842,0.0007137534,0.000005385371,0.0000014787445,0.0000010633346,0.000121823134,0.0000030367803,0.000120896315],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999536,0.0000042248057,0.0000010115967,0.000019575551,0.000010874186,0.000010792969],"domain_scores_gemma":[0.99990547,0.000023747023,0.00001725051,0.000011351192,0.000030915002,0.000011299026],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008717611,0.00012459549,0.000066999986,0.00033700807,0.00014664352,0.00024364553,0.00011745494,0.00010625516,0.0006221537],"category_scores_gemma":[0.00020041245,0.00011372109,0.00009928614,0.00027015674,0.00016115964,0.000110006986,0.00011588166,0.00012817833,0.00009279459],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015092392,0.00008098964,0.75022006,0.00004064395,0.00008554554,0.00019979668,0.00058669935,0.013625982,0.18953265,0.000687242,0.0011751653,0.04361434],"study_design_scores_gemma":[0.000003509134,0.000025359503,0.9618075,0.000004091653,0.000013803905,0.00008153844,0.0002755883,0.029764198,0.0071750614,0.00021102678,0.0006288964,0.000009373589],"about_ca_topic_score_codex":0.037319873,"about_ca_topic_score_gemma":0.05772954,"teacher_disagreement_score":0.037319873,"about_ca_system_score_codex":0.00025427903,"about_ca_system_score_gemma":0.00016272167,"threshold_uncertainty_score":0.07420528},"labels":[],"label_agreement":null},{"id":"W3005579381","doi":"10.1029/2019gl086189","title":"Rapid Characterization of the July 2019 Ridgecrest, California, Earthquake Sequence From Raw Seismic Data Using Machine‐Learning Phase Picker","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":144,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; China Earthquake Administration; National Natural Science Foundation of China","keywords":"Aftershock; Seismology; Sequence (biology); Foreshock; Geology; Workflow; Earthquake simulation; Earthquake location; Remotely triggered earthquakes; Earthquake prediction; Artificial neural network; Seismic gap; Computer science; Fault (geology); Artificial intelligence; Induced seismicity; Database","score_opus":0.1272702395987289,"score_gpt":0.33665730553691753,"score_spread":0.20938706593818862,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3005579381","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9035536,0.00026260235,0.07335883,0.0002066537,0.000053002048,0.0001621612,0.01099083,0.0075230584,0.0038892196],"genre_scores_gemma":[0.88555187,0.00010819194,0.09852779,0.00003368845,0.000037551585,0.000057666275,0.014097278,0.00017705941,0.0014089199],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998616,0.000012788098,0.000010220463,0.000047620426,0.000052281008,0.000015361562],"domain_scores_gemma":[0.999238,0.0001245506,0.00016121076,0.00013432321,0.00025535296,0.0000866216],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004201981,0.0003105726,0.000242885,0.0021636044,0.00021784831,0.00040912905,0.000371969,0.00020814787,0.001122059],"category_scores_gemma":[0.001275435,0.00018349284,0.00014461686,0.00096868863,0.00012740066,0.00036748688,0.00037538758,0.00024052795,0.00074489345],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003893179,0.00028401648,0.44408262,0.00019612235,0.0001173196,0.0006207314,0.0005058431,0.054561578,0.062852174,0.00095740374,0.021811921,0.41362092],"study_design_scores_gemma":[0.000051257684,0.00011763924,0.44219774,0.000033322565,0.000037380236,0.00021119119,0.00025722134,0.52476287,0.021729443,0.0008933213,0.009665221,0.000043319422],"about_ca_topic_score_codex":0.013319244,"about_ca_topic_score_gemma":0.04515113,"teacher_disagreement_score":0.013319244,"about_ca_system_score_codex":0.00035522672,"about_ca_system_score_gemma":0.0006608738,"threshold_uncertainty_score":0.026483476},"labels":[],"label_agreement":null},{"id":"W3006253835","doi":"10.1029/2020gl087100","title":"Experimental Estimates of Optical Backscattering Associated With Submicron Particles in Clear Oceanic Waters","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Scattering; Backscatter (email); Coherent backscattering; Range (aeronautics); Materials science; Particle (ecology); Trophic level; Mineralogy; Analytical Chemistry (journal); Optics; Oceanography; Physics; Chemistry; Geology; Environmental chemistry; Composite material","score_opus":0.03482780184431293,"score_gpt":0.26155673636647647,"score_spread":0.22672893452216353,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006253835","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990435,0.00005133897,0.0005674442,0.0000032525238,0.000001191974,0.000004443431,0.00005084524,0.0000041685676,0.00027362996],"genre_scores_gemma":[0.99747795,0.00011117199,0.0018893083,0.000015108715,0.0000019556746,0.00002026008,0.00021068286,0.0000046129935,0.0002689904],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998399,0.000026181415,0.000010218487,0.000033765726,0.000064646105,0.000025289215],"domain_scores_gemma":[0.99955565,0.00019459796,0.00006901746,0.000026671683,0.00011943118,0.0000347073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035464557,0.00029390195,0.0001399013,0.00024987993,0.00027890364,0.00019341242,0.00010004254,0.00014954737,0.00061758485],"category_scores_gemma":[0.0005980138,0.00015502612,0.0001172098,0.00015345702,0.00032980542,0.00021751746,0.0002213613,0.00022973373,0.00010453959],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028142423,0.000035951634,0.038019884,0.000055312074,0.000021289814,0.000023113027,0.00018245284,0.00042037913,0.9564949,0.00006865642,0.00003567138,0.004360952],"study_design_scores_gemma":[0.000020186008,0.0008202655,0.3755018,0.000013539275,0.000037821777,0.00008879853,0.00038783718,0.002877366,0.61941147,0.000100029,0.00072418555,0.000016818945],"about_ca_topic_score_codex":0.0063011423,"about_ca_topic_score_gemma":0.007694395,"teacher_disagreement_score":0.0063011423,"about_ca_system_score_codex":0.00028706476,"about_ca_system_score_gemma":0.00022391237,"threshold_uncertainty_score":0.012528896},"labels":[],"label_agreement":null},{"id":"W3006555416","doi":"10.1029/2020gl087440","title":"Back to Einstein: Burial‐Induced Three‐Range Diffusion in Fluvial Sediment Transport","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bed load; TRACER; Diffusion; Fluvial; Geology; Range (aeronautics); Sediment transport; Random walk; Sediment; Rest (music); Anomalous diffusion; Geomorphology; Physics; Innovation diffusion; Materials science; Computer science","score_opus":0.0404327145818198,"score_gpt":0.28531323096182354,"score_spread":0.24488051638000374,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3006555416","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.15905382,0.046687383,0.5616444,0.12991832,0.0074306782,0.000119172095,0.0010995009,0.00104623,0.09300048],"genre_scores_gemma":[0.90019333,0.014283933,0.029489363,0.005704013,0.0029879282,0.00011356167,0.00015918649,0.00044185633,0.046626803],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99979585,0.00008021159,0.000008654734,0.000056996036,0.00003516618,0.00002306677],"domain_scores_gemma":[0.99940264,0.00033048526,0.00005225307,0.0000569337,0.00009326087,0.00006435456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006645566,0.00060287735,0.00062053057,0.00049118453,0.0008382945,0.0015463193,0.0007874036,0.0023158113,0.006094092],"category_scores_gemma":[0.002699747,0.00047790445,0.0008839609,0.0006540237,0.002287383,0.004537426,0.0009968199,0.0027957244,0.001453815],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005453589,0.00002831001,0.0009852753,0.00015436111,0.000034251134,0.00015975637,0.0002547374,0.051131155,0.001620412,0.912937,0.021103645,0.011536614],"study_design_scores_gemma":[0.000043591914,0.000037125264,0.0007162627,0.00009050692,0.000017884217,0.00013445027,0.0000612189,0.19129878,0.00053923344,0.7793083,0.027692692,0.000059934257],"about_ca_topic_score_codex":0.005099949,"about_ca_topic_score_gemma":0.001818928,"teacher_disagreement_score":0.006094092,"about_ca_system_score_codex":0.0014179015,"about_ca_system_score_gemma":0.00049373816,"threshold_uncertainty_score":0.020386815},"labels":[],"label_agreement":null},{"id":"W3007523049","doi":"10.1029/2019gl086888","title":"Orthogonal Fault Rupture and Rapid Postseismic Deformation Following 2019 Ridgecrest, California, Earthquake Sequence Revealed From Geodetic Observations","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"Fundamental Research Funds for the Central Universities","keywords":"Geology; Seismology; Sinistral and dextral; Aftershock; Geodetic datum; Geodesy; Interferometric synthetic aperture radar; Fault (geology); Slip (aerodynamics); Seismic moment; Synthetic aperture radar; Remote sensing","score_opus":0.06422997871925579,"score_gpt":0.2773728286163893,"score_spread":0.2131428498971335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3007523049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943024,0.000016546132,0.000033961536,0.0000090441235,0.0000013350085,0.0000017769676,0.00020779335,0.0000041666312,0.00029511712],"genre_scores_gemma":[0.9993518,0.000021019949,0.000056358193,0.0000036835947,0.0000028997392,0.000001974128,0.00042184902,9.645985e-7,0.0001394638],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000004147021,0.0000042796737,0.00001678703,0.000019518122,0.000018484268],"domain_scores_gemma":[0.99967456,0.00002155454,0.00016943875,0.00002199225,0.00007294026,0.000039541188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011717069,0.00012161318,0.00009953906,0.00047930292,0.00021004546,0.00027308328,0.00014399627,0.00016148019,0.0005276431],"category_scores_gemma":[0.00038844845,0.00009561866,0.0000701481,0.0005059738,0.00016701802,0.00013890276,0.00022268436,0.00013790451,0.00011399665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015896746,0.00005351561,0.9848363,0.000015202734,0.0000228418,0.00033400385,0.00018057472,0.0011355778,0.0070507852,0.00006173953,0.000600262,0.005550134],"study_design_scores_gemma":[0.0000022102101,0.000009264628,0.99930024,0.0000010571664,0.0000027189913,0.000018914356,0.00004069569,0.00036024326,0.00015289048,0.000004271801,0.0001063444,0.0000010765266],"about_ca_topic_score_codex":0.04175561,"about_ca_topic_score_gemma":0.09465837,"teacher_disagreement_score":0.04175561,"about_ca_system_score_codex":0.00038769818,"about_ca_system_score_gemma":0.00028520072,"threshold_uncertainty_score":0.08302516},"labels":[],"label_agreement":null},{"id":"W3008734677","doi":"10.1029/2019gl086705","title":"New Generation of Climate Models Track Recent Unprecedented Changes in Earth's Radiation Budget Observed by CERES","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":98,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Met Office; European Commission; Sight Research UK; European Research Council; National Science Foundation; Department for Business, Energy and Industrial Strategy, UK Government; Langley Research Center; National Aeronautics and Space Administration; Department for Environment, Food and Rural Affairs, UK Government; Horizon 2020; National Center for Atmospheric Research","keywords":"Shortwave; Longwave; Shortwave radiation; Equator; Climatology; Environmental science; Outgoing longwave radiation; Flux (metallurgy); Atmospheric sciences; Climate model; Sea surface temperature; Radiative flux; Atmosphere (unit); Radiative transfer; Sea ice; Cloud cover; Climate change; Geology; Meteorology; Radiation; Cloud computing; Physics; Oceanography; Latitude; Convection","score_opus":0.12699901552423667,"score_gpt":0.3124952275496927,"score_spread":0.18549621202545605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008734677","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96521455,0.0004243518,0.020671885,0.0013318033,0.00022653214,0.000025961774,0.004657138,0.0014590274,0.0059886873],"genre_scores_gemma":[0.9848091,0.00021145339,0.01051032,0.00014399335,0.00006734386,0.000032549622,0.003475866,0.00016043903,0.00058890064],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998287,0.000057015688,0.000007217607,0.000059043912,0.000028168424,0.000019803128],"domain_scores_gemma":[0.9995844,0.00011922907,0.00006639389,0.00012391432,0.000065000895,0.00004116786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009801624,0.00039604685,0.00044988716,0.00027157506,0.00023776197,0.0008400549,0.0008948846,0.00049809867,0.0015174759],"category_scores_gemma":[0.0015256505,0.00026779438,0.0006550521,0.00045841644,0.0002854812,0.0010803692,0.0004929521,0.00081208796,0.00018385643],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028928753,0.00013870417,0.05469782,0.000040056206,0.00046184225,0.00003129748,0.000062682266,0.9181612,0.004850524,0.0034301009,0.0047262004,0.013110174],"study_design_scores_gemma":[0.00019003713,0.000052925374,0.017480073,0.00000765248,0.000091669164,0.000014755972,0.00002428009,0.9740338,0.0011742759,0.0019059387,0.005002967,0.00002157017],"about_ca_topic_score_codex":0.016248822,"about_ca_topic_score_gemma":0.02189058,"teacher_disagreement_score":0.016248822,"about_ca_system_score_codex":0.00069975987,"about_ca_system_score_gemma":0.0005099076,"threshold_uncertainty_score":0.03230846},"labels":[],"label_agreement":null},{"id":"W3008831910","doi":"10.1029/2019gl086903","title":"QBO Changes in CMIP6 Climate Projections","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Stratosphere; Coupled model intercomparison project; Quasi-biennial oscillation; Climatology; Atmospheric sciences; Climate model; Environmental science; Climate system; Climate change; Geology; Oceanography","score_opus":0.06060600335107016,"score_gpt":0.3050946739485081,"score_spread":0.24448867059743792,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3008831910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9720542,0.00035417077,0.002737424,0.0016635404,0.00011087683,0.00002750688,0.015510626,0.00035796614,0.0071836165],"genre_scores_gemma":[0.9932708,0.00012850629,0.0007779849,0.00009740534,0.000021631753,0.000028030649,0.0052286037,0.00003773152,0.0004093373],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995994,0.00015742617,0.00002667272,0.000088246794,0.0000671817,0.000061102226],"domain_scores_gemma":[0.9989304,0.00028196725,0.00025165462,0.00010431983,0.00033202165,0.00009972701],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001723823,0.0006803715,0.00023628355,0.0006521577,0.00033346948,0.0009961041,0.00055983255,0.0008872675,0.0029060193],"category_scores_gemma":[0.0042455103,0.000330324,0.0007371212,0.0010629542,0.00026879788,0.0009917656,0.00067324477,0.00058018626,0.00043334428],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00091885123,0.00015173666,0.33352634,0.0003448102,0.0006739046,0.00030132456,0.00028416136,0.6153215,0.0053569567,0.008479791,0.017736059,0.016904533],"study_design_scores_gemma":[0.00032747738,0.00030205995,0.3439111,0.00013360387,0.00017577078,0.00022547321,0.0005624724,0.624132,0.004616262,0.0062512523,0.019212194,0.0001502878],"about_ca_topic_score_codex":0.023057561,"about_ca_topic_score_gemma":0.013395218,"teacher_disagreement_score":0.023057561,"about_ca_system_score_codex":0.0012463927,"about_ca_system_score_gemma":0.00053985824,"threshold_uncertainty_score":0.0458467},"labels":[],"label_agreement":null},{"id":"W3009016445","doi":"10.1029/2019gl086344","title":"High‐Accuracy Near‐Infrared Carbon Dioxide Intensity Measurements to Support Remote Sensing","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Environment and Climate Change Canada","funders":"National Institute of Standards and Technology; National Aeronautics and Space Administration","keywords":"HITRAN; Remote sensing; Near-infrared spectroscopy; Spectrometer; Carbon dioxide; Satellite; Infrared; Environmental science; Spectral bands; Line (geometry); Isotopologue; Intensity (physics); Carbon fibers; Spectral line; Materials science; Physics; Optics; Geology; Chemistry; Astronomy; Mathematics","score_opus":0.04430638870042114,"score_gpt":0.2793309955415709,"score_spread":0.23502460684114979,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009016445","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.917897,0.0001614766,0.0732027,0.00014013804,0.000052171355,0.00009966488,0.00116083,0.00168384,0.0056021423],"genre_scores_gemma":[0.9380441,0.000040644674,0.0605113,0.000057797817,0.000009814882,0.000049421917,0.00054261606,0.000050250204,0.00069407374],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.999474,0.000056465586,0.000021159858,0.00012812525,0.000273585,0.000046669556],"domain_scores_gemma":[0.9991285,0.00017243199,0.00009096681,0.00021801147,0.0003648273,0.000025261656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096027926,0.00028053575,0.00027772287,0.00050507823,0.0002973914,0.00045798317,0.0008194763,0.00031720957,0.0011960816],"category_scores_gemma":[0.0014544777,0.00024095649,0.0001581962,0.00045903324,0.00018042754,0.00056905975,0.0004484487,0.00037528187,0.00048669294],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022671066,0.00016089324,0.035430863,0.00005152009,0.000036140595,0.00004155649,0.000079467434,0.008818241,0.9018136,0.00071915844,0.0010299692,0.05159195],"study_design_scores_gemma":[0.00008718071,0.00020466855,0.10040159,0.000022900935,0.000046837325,0.00013825342,0.000087573106,0.15679787,0.73411995,0.00063757383,0.007394678,0.00006093106],"about_ca_topic_score_codex":0.0062103085,"about_ca_topic_score_gemma":0.01163952,"teacher_disagreement_score":0.0062103085,"about_ca_system_score_codex":0.000499601,"about_ca_system_score_gemma":0.000629803,"threshold_uncertainty_score":0.012348294},"labels":[],"label_agreement":null},{"id":"W3009900701","doi":"10.1029/2019gl086756","title":"Clumped Isotopes Link Older Carbon Substrates With Slower Rates of Methanogenesis in Northern Lakes","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Heising-Simons Foundation; Agouron Institute; Vetenskapsrådet; Shell","keywords":"Methanogenesis; Permafrost; Thermokarst; Isotopes of carbon; Methane; Carbon fibers; Environmental chemistry; Carbon cycle; Environmental science; Stable isotope ratio; Peat; Total organic carbon; Carbon dioxide; Substrate (aquarium); Carbon flux; δ13C; Ecology; Chemistry; Ecosystem; Biology; Materials science","score_opus":0.028071912879272184,"score_gpt":0.27817010993176605,"score_spread":0.25009819705249386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3009900701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997147,0.000045668672,0.000082209015,0.000008973163,6.370475e-7,6.1280156e-7,0.000044759487,0.0000049115397,0.00009763745],"genre_scores_gemma":[0.99962485,0.000026041576,0.00015821829,0.000009310967,0.0000016259386,0.0000018347463,0.000061326915,0.0000027739109,0.00011406789],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999343,0.000011068277,0.000005822918,0.00002047659,0.000014388543,0.00001388445],"domain_scores_gemma":[0.99954885,0.00009051725,0.0002149105,0.000023124563,0.00006613976,0.0000563621],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019145594,0.00014678735,0.0002031401,0.00046816672,0.00031855758,0.0004389625,0.00011779547,0.00020181437,0.0007200849],"category_scores_gemma":[0.0007459089,0.00026837355,0.0000829532,0.00038820432,0.00034140228,0.00029249728,0.00031820123,0.00015779125,0.00009822127],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050240953,0.000031171214,0.8539428,0.00003833613,0.00006253026,0.00020341855,0.0004470004,0.0006006129,0.1395878,0.00007947454,0.00008270967,0.0044218386],"study_design_scores_gemma":[0.0000029312662,0.000025575871,0.9942204,0.000002247066,0.000008057919,0.00006701693,0.00013824775,0.00066969055,0.004670071,0.00007127856,0.00012040119,0.0000041993735],"about_ca_topic_score_codex":0.009106255,"about_ca_topic_score_gemma":0.013404543,"teacher_disagreement_score":0.009106255,"about_ca_system_score_codex":0.00030363328,"about_ca_system_score_gemma":0.00019950604,"threshold_uncertainty_score":0.01810646},"labels":[],"label_agreement":null},{"id":"W3010870511","doi":"10.1029/2019gl086631","title":"El Niño‐Driven Oxygenation Impacts Peruvian Shelf Iron Supply to the South Pacific Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft","keywords":"Upwelling; Seawater; Oceanography; Redox; Environmental science; Water column; Oxygen minimum zone; Iodate; Environmental chemistry; Trace metal; Productivity; Chemistry; Geology; Iodide; Metal; Inorganic chemistry","score_opus":0.026173927783630493,"score_gpt":0.2544854833691792,"score_spread":0.22831155558554872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3010870511","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981931,0.0001695543,0.000041962914,0.00023526617,0.000004215856,0.0000020212951,0.00020736936,0.000008012429,0.0011386569],"genre_scores_gemma":[0.99907243,0.000266721,0.000049575152,0.00005589262,0.000006095345,0.000003793564,0.0002369166,0.000003512792,0.0003051487],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.000008170114,0.0000034644825,0.000013798967,0.000007372219,0.000013677866],"domain_scores_gemma":[0.99984586,0.000016286052,0.000059567643,0.000009060888,0.00004303097,0.000026197156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013864353,0.00022421681,0.00012754068,0.00033396704,0.00042583505,0.00053812255,0.0001667351,0.00026002995,0.0016918515],"category_scores_gemma":[0.00042737124,0.00013267227,0.00013968881,0.00036810787,0.0003167013,0.0003592325,0.0011245405,0.00022873818,0.00014397732],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002133141,0.000032370197,0.94143164,0.00013430988,0.00013786195,0.0006099202,0.00104104,0.0006729991,0.046110697,0.00024288463,0.00056800875,0.008804878],"study_design_scores_gemma":[0.000005402327,0.000024578336,0.99684685,0.000013888216,0.00001542946,0.00004214776,0.0007198793,0.00032497983,0.00083153974,0.00006905146,0.0011026998,0.0000035094254],"about_ca_topic_score_codex":0.03414255,"about_ca_topic_score_gemma":0.04402486,"teacher_disagreement_score":0.03414255,"about_ca_system_score_codex":0.00058682606,"about_ca_system_score_gemma":0.0005212896,"threshold_uncertainty_score":0.067887664},"labels":[],"label_agreement":null},{"id":"W3012183095","doi":"10.1029/2020gl087051","title":"Is the River a Chemostat?: Scale Versus Land Use Controls on Nitrate Concentration‐Discharge Dynamics in the Upper Mississippi River Basin","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil and Water Nutrient Dynamics","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Drainage basin; Environmental science; Structural basin; Hydrology (agriculture); Discharge; Nitrate; Land use; Tile drainage; Spatial ecology; Geology; Soil science; Ecology; Soil water; Geomorphology; Geography","score_opus":0.03882748626711975,"score_gpt":0.28395259930115707,"score_spread":0.24512511303403733,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3012183095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989017,0.000061101586,0.00016462962,0.00014494854,0.0000013165709,0.0000020338312,0.00014060718,0.000009686317,0.00057390105],"genre_scores_gemma":[0.99970967,0.000024728148,0.00005740312,0.000016001895,0.0000012758255,0.0000013469801,0.000048601567,0.000002502177,0.00013842908],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998493,0.00005870219,0.000007079043,0.000051400817,0.000016251433,0.000017333181],"domain_scores_gemma":[0.9990381,0.00047336507,0.00018764091,0.000061881714,0.00010798467,0.00013101808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004137724,0.000103892155,0.00019755066,0.00045958775,0.00035079388,0.00088696403,0.00021842547,0.00023441571,0.0012321995],"category_scores_gemma":[0.0015443299,0.00011339007,0.00020614022,0.0005870843,0.00064269896,0.00041536902,0.00049365225,0.00015886888,0.00008238773],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001124082,0.00005699157,0.9709991,0.000027956874,0.00016795512,0.00014269329,0.00044243777,0.01129184,0.007224941,0.0011504212,0.0006269919,0.0077563366],"study_design_scores_gemma":[0.000008133376,0.00002136187,0.9684918,0.000007635851,0.00002679563,0.000028086559,0.0004824821,0.029501913,0.0003593739,0.0004469513,0.0006146765,0.000010830998],"about_ca_topic_score_codex":0.07098906,"about_ca_topic_score_gemma":0.069886945,"teacher_disagreement_score":0.07098906,"about_ca_system_score_codex":0.00079462625,"about_ca_system_score_gemma":0.0004804687,"threshold_uncertainty_score":0.14115173},"labels":[],"label_agreement":null},{"id":"W3013876398","doi":"10.1029/2020gl088051","title":"Changes in the Arctic Ocean Carbon Cycle With Diminishing Ice Cover","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"North Pacific Marine Science Organization; Tula Foundation","funders":"National Oceanic and Atmospheric Administration; Hakai Institute; University of Montana; National Stroke Foundation; National Aeronautics and Space Administration; Office of Naval Research; Institut Français de Recherche pour l'Exploitation de la Mer; National Science Foundation","keywords":"Sea ice; Arctic ice pack; Environmental science; Sink (geography); Arctic sea ice decline; Climatology; Arctic; Oceanography; Cryosphere; Antarctic sea ice; Drift ice; Structural basin; Atmospheric sciences; Geology; Geography","score_opus":0.028323597471780846,"score_gpt":0.25402088834519115,"score_spread":0.2256972908734103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013876398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986546,0.00007572182,0.000036574453,0.00004083546,0.000003142467,0.0000016325447,0.00047987417,0.000003702233,0.0007039393],"genre_scores_gemma":[0.99926,0.000056088367,0.0000692274,0.00001532562,0.0000030229755,0.0000012471726,0.0003520789,0.0000014136523,0.00024151817],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993217,0.000008115411,0.000003269636,0.000013712745,0.000020877978,0.000021899617],"domain_scores_gemma":[0.9996401,0.00003348917,0.000077576326,0.00001659891,0.00017323202,0.000058986407],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017160673,0.000116292445,0.00012793778,0.0004169728,0.00040599174,0.0006269123,0.00013198344,0.00022472297,0.0006373555],"category_scores_gemma":[0.0006592592,0.00006864776,0.00010798241,0.00078017893,0.00034739778,0.00017230849,0.00017113955,0.00016536698,0.00010546838],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019732951,0.000027232834,0.984371,0.000014075624,0.00005252787,0.00007428543,0.00017925863,0.001397844,0.0075863223,0.00016759665,0.0004261716,0.0055062785],"study_design_scores_gemma":[0.0000011193355,0.000007851546,0.99898463,0.0000014200367,0.000002869171,0.000018116676,0.000063248495,0.00039565898,0.0002027317,0.000012883516,0.0003083207,0.0000011675],"about_ca_topic_score_codex":0.31705424,"about_ca_topic_score_gemma":0.4148918,"teacher_disagreement_score":0.31705424,"about_ca_system_score_codex":0.0015673431,"about_ca_system_score_gemma":0.0010074951,"threshold_uncertainty_score":0.6304176},"labels":[],"label_agreement":null},{"id":"W3013981126","doi":"10.1029/2020gl088136","title":"The 2020 <i>M</i><sub><i>w</i></sub> 6.8 Elazığ (Turkey) Earthquake Reveals Rupture Behavior of the East Anatolian Fault","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":97,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canada Foundation for Innovation","keywords":"Aftershock; Seismology; Geology; Slip (aerodynamics); North Anatolian Fault; Earthquake rupture; Fault (geology); Subduction; Plate tectonics; Geodesy; Tectonics","score_opus":0.029512691795815067,"score_gpt":0.26140195716969244,"score_spread":0.23188926537387738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3013981126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982969,0.00004167088,0.000055290457,0.00001810557,0.000003038476,0.0000014151049,0.0004835488,0.0000148628715,0.0010850684],"genre_scores_gemma":[0.99842876,0.000040428935,0.00008677708,0.0000075785206,0.0000041115227,0.0000018572141,0.0011128597,0.0000035528178,0.00031401418],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999778,0.0000014149078,0.0000014573307,0.0000065079685,0.0000041075,0.0000087513345],"domain_scores_gemma":[0.99994755,0.0000025129923,0.000021184627,0.0000034554996,0.000011490366,0.000013816661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000034039553,0.0001435518,0.00010435116,0.00056082464,0.00013572848,0.00022283962,0.00009197969,0.00020807942,0.0011379409],"category_scores_gemma":[0.00010591193,0.00007712625,0.00007072191,0.00043715123,0.000099697216,0.00016192425,0.00018275688,0.00011609014,0.00046088523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031220634,0.00012548118,0.8770767,0.000049207883,0.0000343609,0.0007032324,0.00030905966,0.0015944558,0.09188377,0.00019497001,0.0026621316,0.025054425],"study_design_scores_gemma":[0.0000016003659,0.000016537995,0.9979504,0.000002314661,0.0000026476139,0.00010608616,0.00008060249,0.0007058157,0.0007742257,0.000016067175,0.0003418439,0.0000018786932],"about_ca_topic_score_codex":0.00489701,"about_ca_topic_score_gemma":0.007320658,"teacher_disagreement_score":0.00489701,"about_ca_system_score_codex":0.00017749635,"about_ca_system_score_gemma":0.00008188816,"threshold_uncertainty_score":0.009737015},"labels":[],"label_agreement":null},{"id":"W3014166839","doi":"10.1029/2020gl088057","title":"Non‐Additivity of the Midlatitude Circulation Response to Regional Arctic Temperature Anomalies: The Role of the Stratosphere","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Graduate School, Purdue University; National Science Foundation","keywords":"Arctic geoengineering; Climatology; Stratosphere; Middle latitudes; Arctic sea ice decline; Arctic; Arctic ice pack; Sea ice; Arctic dipole anomaly; Arctic oscillation; Geology; Troposphere; Bay; Atmospheric sciences; Oceanography; Environmental science; Drift ice; Northern Hemisphere","score_opus":0.026761214709342476,"score_gpt":0.2714320409653359,"score_spread":0.24467082625599343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014166839","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9955487,0.00007687971,0.0014601866,0.00012442208,0.000023857165,0.000012497715,0.00024040921,0.000044672375,0.0024683422],"genre_scores_gemma":[0.9994497,0.00002718899,0.000080298596,0.00002573652,0.0000060123125,0.0000035203877,0.000085070715,0.000004508987,0.0003180269],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976903,0.00006758584,0.000013449735,0.00005237772,0.000039444734,0.000058089143],"domain_scores_gemma":[0.99953496,0.00019360047,0.000061094855,0.000074214826,0.00006923165,0.000066942084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038423383,0.0004724976,0.00038155247,0.00026753204,0.00023992738,0.0005059868,0.000292886,0.00025544566,0.0019068415],"category_scores_gemma":[0.0010027641,0.00023884917,0.00063868816,0.00014152021,0.00035211453,0.0002711983,0.00068797404,0.00045364472,0.00017370605],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016721368,0.0004967623,0.28880793,0.00026749648,0.0011710639,0.001062507,0.00041371165,0.22631879,0.45381024,0.0026390082,0.0011267491,0.022213614],"study_design_scores_gemma":[0.000053168253,0.00035324576,0.781233,0.000014484303,0.00015004742,0.00017201644,0.0001822925,0.203006,0.013156968,0.0009069761,0.00073818676,0.00003368829],"about_ca_topic_score_codex":0.008375937,"about_ca_topic_score_gemma":0.0059995875,"teacher_disagreement_score":0.008375937,"about_ca_system_score_codex":0.0003419536,"about_ca_system_score_gemma":0.00033832,"threshold_uncertainty_score":0.016654372},"labels":[],"label_agreement":null},{"id":"W3014403980","doi":"10.1029/2020gl087929","title":"Forcing Dependence of Atmospheric Lapse Rate Changes Dominates Residual Polar Warming in Solar Radiation Management Climate Scenarios","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Compute Canada","keywords":"Environmental science; Lapse rate; Atmospheric sciences; Latitude; Global warming; Forcing (mathematics); Climatology; Climate change; Residual; Greenhouse gas; Geology","score_opus":0.027732800105479183,"score_gpt":0.27511442578376655,"score_spread":0.24738162567828736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014403980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99572635,0.000058117814,0.00028367437,0.00020443955,0.000012019338,0.000008911033,0.00070906687,0.000055621604,0.0029418329],"genre_scores_gemma":[0.9994531,0.00002176241,0.00006117428,0.00002516981,0.00000377318,0.00000528263,0.00027526522,0.000009377988,0.00014498459],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999866,0.000046546702,0.0000060193383,0.000021898068,0.000010593283,0.000048801092],"domain_scores_gemma":[0.9994361,0.00029393547,0.00005882927,0.000052129886,0.000055024808,0.00010399092],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005766802,0.0005286106,0.00038708013,0.00034466473,0.0003021055,0.00081649644,0.00043011407,0.0008716821,0.0031677717],"category_scores_gemma":[0.0012587635,0.0002412206,0.0006613368,0.00027389682,0.00035790226,0.00050171703,0.00037945944,0.00049207354,0.0002479375],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0025522194,0.00028579374,0.117126495,0.00017553472,0.0004716397,0.0008794305,0.00012052628,0.8402065,0.023922341,0.004271975,0.0036014381,0.006386192],"study_design_scores_gemma":[0.00036678312,0.0005264383,0.18684015,0.000030621348,0.0001846061,0.000118461554,0.00028484588,0.80154884,0.0066072866,0.0025238765,0.00090858334,0.00005953151],"about_ca_topic_score_codex":0.015506422,"about_ca_topic_score_gemma":0.010363877,"teacher_disagreement_score":0.015506422,"about_ca_system_score_codex":0.00046045776,"about_ca_system_score_gemma":0.00031854573,"threshold_uncertainty_score":0.03083229},"labels":[],"label_agreement":null},{"id":"W3014920837","doi":"10.1029/2020gl087944","title":"Uncertainties of Glacial Isostatic Adjustment Model Predictions in North America Associated With 3D Structure","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Calgary","funders":"Earth Observatory of Singapore; Natural Sciences and Engineering Research Council of Canada; Ministry of Education, India; National Research Foundation Singapore; National Natural Science Foundation of China; University of Hong Kong; Ministry of Education - Singapore; National Research Foundation","keywords":"Post-glacial rebound; Geology; Bay; Last Glacial Maximum; Lithosphere; Mantle (geology); Glacial period; Sea level; Deglaciation; Ice sheet; Geodesy; Oceanography; Climatology; Physical geography; Geomorphology; Tectonics; Paleontology; Geography","score_opus":0.03123998254031833,"score_gpt":0.26796450717211734,"score_spread":0.236724524631799,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3014920837","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99125284,0.00018170566,0.005249796,0.00025436346,0.000016886452,0.0000058461683,0.00070808537,0.00021937102,0.002111187],"genre_scores_gemma":[0.9989052,0.000031693027,0.0006007324,0.000015342652,0.000003605228,0.0000036127549,0.0002978331,0.000017516011,0.00012454548],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99950695,0.00019272925,0.000032253905,0.00015791594,0.00006792371,0.00004223396],"domain_scores_gemma":[0.9977847,0.0011303102,0.00034164326,0.00027649416,0.0003825526,0.00008445343],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020070146,0.0005132689,0.00034125912,0.0007199267,0.00041593486,0.0014083284,0.00054044026,0.00042334263,0.0007121812],"category_scores_gemma":[0.0046893544,0.00044202167,0.0006962439,0.00063176616,0.0006823104,0.0005928984,0.0006985625,0.00040922716,0.00014493575],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007608304,0.00001145823,0.0753384,0.000010036454,0.0001430827,0.00004421164,0.000064312284,0.9184083,0.00062901207,0.00064745493,0.00033344878,0.0042942786],"study_design_scores_gemma":[0.00002844993,0.000025447373,0.072290115,0.000020744123,0.000047165362,0.000027702294,0.00006877458,0.9241016,0.00077559904,0.0016398682,0.0009298822,0.000044559634],"about_ca_topic_score_codex":0.092746764,"about_ca_topic_score_gemma":0.058810815,"teacher_disagreement_score":0.90725327,"about_ca_system_score_codex":0.0015212782,"about_ca_system_score_gemma":0.0010110876,"threshold_uncertainty_score":0.18441385},"labels":[],"label_agreement":null},{"id":"W3015322942","doi":"10.1029/2020gl087350","title":"Upstream Ultra‐Low Frequency Waves Observed by MESSENGER's Magnetometer: Implications for Particle Acceleration at Mercury's Bow Shock","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Foreshock; Physics; Amplitude; Solar wind; Polarization (electrochemistry); Population; Geophysics; Ultra low frequency; Magnetometer; Computational physics; Astrophysics; Magnetic field; Seismology; Geology; Astronomy; Optics; Aftershock","score_opus":0.06902907226388938,"score_gpt":0.3088155218701959,"score_spread":0.23978644960630652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015322942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925035,0.000018621642,0.00018397786,0.000027412607,0.000002065942,0.0000011603936,0.000111117886,0.000008762415,0.00039658102],"genre_scores_gemma":[0.9997682,0.000007242171,0.000051937666,0.0000048046286,0.0000045625816,8.2846765e-7,0.00009041622,0.0000015811243,0.0000706037],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989593,0.000016004236,0.0000051952993,0.0000219114,0.000032558873,0.00002833181],"domain_scores_gemma":[0.9991283,0.0003302446,0.0002791564,0.000061394036,0.00008751754,0.00011336871],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029514026,0.00010459443,0.00013384421,0.0006786408,0.00021100715,0.0003241363,0.00014562701,0.00015601568,0.0010315906],"category_scores_gemma":[0.0011531964,0.00007884495,0.0001462694,0.0005131471,0.00023936783,0.00014629897,0.00029878796,0.00017616469,0.0001447181],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020351265,0.000016418104,0.98002464,0.000008710979,0.00002506453,0.000121398094,0.00012036403,0.0004172355,0.013452508,0.0002048967,0.00021200691,0.005193355],"study_design_scores_gemma":[0.0000022046288,0.000022581922,0.99864644,9.725604e-7,0.0000052430064,0.000027919466,0.000053476015,0.0004467824,0.00063828874,0.000052633386,0.00010100499,0.0000026183839],"about_ca_topic_score_codex":0.0020393343,"about_ca_topic_score_gemma":0.0014743733,"teacher_disagreement_score":0.0020393343,"about_ca_system_score_codex":0.00015117493,"about_ca_system_score_gemma":0.00008954526,"threshold_uncertainty_score":0.004054904},"labels":[],"label_agreement":null},{"id":"W3015491438","doi":"10.1029/2019gl086236","title":"Insight Into Major Active Faults in Central Myanmar and the Related Geodynamic Sources","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China-Yunnan Joint Fund; CAS-SAFEA International Partnership Program for Creative Research Teams","keywords":"Seismology; Geology; Sinistral and dextral; Tectonics; Crust; Fault (geology); Seismotectonics; Focal mechanism; Active fault; Geophysics","score_opus":0.018692131466698438,"score_gpt":0.2510964730029014,"score_spread":0.23240434153620296,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3015491438","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978884,0.00025859836,0.0001510393,0.00012363779,0.0000015942071,0.0000037485938,0.00032295368,0.0000057918837,0.0012442843],"genre_scores_gemma":[0.999268,0.00010214527,0.00011197695,0.000010003581,0.0000031286393,0.000002518554,0.00021160148,9.753538e-7,0.00028974007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999658,0.0000050724884,0.0000030360065,0.0000097467555,0.000004320422,0.00001214471],"domain_scores_gemma":[0.99984384,0.000017351842,0.00007950236,0.00000937755,0.00003139739,0.000018597904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087857756,0.00012571899,0.00008597261,0.0011577411,0.00021483898,0.00026503616,0.00016656698,0.000146596,0.0018180341],"category_scores_gemma":[0.00027136668,0.00007433736,0.00007708309,0.0010367897,0.00014000524,0.00028282977,0.00041558588,0.00009265091,0.00016576322],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036875677,0.000016719005,0.9628615,0.00005712408,0.000025176134,0.0004933949,0.0017037682,0.00054518785,0.007885401,0.0007255527,0.0005380937,0.02511113],"study_design_scores_gemma":[0.0000010222038,0.000006738719,0.9978212,0.000009374478,0.000005262549,0.00009099389,0.0007148134,0.0003752444,0.00008651841,0.00006194052,0.00082539604,0.0000015733372],"about_ca_topic_score_codex":0.015723746,"about_ca_topic_score_gemma":0.03197212,"teacher_disagreement_score":0.015723746,"about_ca_system_score_codex":0.00027942104,"about_ca_system_score_gemma":0.00026993995,"threshold_uncertainty_score":0.031264424},"labels":[],"label_agreement":null},{"id":"W3016675885","doi":"10.1029/2020gl087372","title":"Toward a Universal Frequency of Occurrence Distribution for Tsunamis: Statistical Analysis of a 32‐Year Bottom Pressure Record at Axial Seamount","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"","keywords":"Amplitude; Geology; Seamount; Seismology; Geodesy; Power law; Series (stratigraphy); Standard deviation; Noise (video); Oceanography; Statistics; Physics; Mathematics; Paleontology","score_opus":0.050880409151253435,"score_gpt":0.2947564267229534,"score_spread":0.24387601757169994,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3016675885","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987948,0.000029929395,0.0006859033,0.000023638988,0.0000018158576,0.000004556175,0.00019051341,0.000018941748,0.00024992655],"genre_scores_gemma":[0.9992661,0.000016799242,0.00029883653,0.000004799615,0.0000045478996,0.0000038213207,0.00033313723,0.000005253229,0.00006680629],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99935454,0.00014311036,0.00007822821,0.00020805046,0.00014279583,0.00007321424],"domain_scores_gemma":[0.99403906,0.0022921304,0.0016960489,0.0009771109,0.0006301394,0.00036547918],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019263129,0.0001667674,0.00027037683,0.0023060443,0.0003164565,0.0007707091,0.00035895026,0.0004247939,0.0008983826],"category_scores_gemma":[0.0074808253,0.0002007123,0.0003997693,0.0013699249,0.0006159146,0.0005390196,0.0007690441,0.00036511407,0.00023769283],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000053960157,0.000015214357,0.99047863,0.000012005237,0.00007143339,0.000098595374,0.00026670663,0.0007575191,0.002821055,0.000091154,0.000110310546,0.005223511],"study_design_scores_gemma":[0.0000010204047,0.000022077804,0.99737227,0.0000026335329,0.00000770573,0.00006699776,0.00011479945,0.0021572916,0.00014544417,0.000025478152,0.000079559606,0.00000462438],"about_ca_topic_score_codex":0.008806358,"about_ca_topic_score_gemma":0.0056155478,"teacher_disagreement_score":0.008806358,"about_ca_system_score_codex":0.000263152,"about_ca_system_score_gemma":0.00030372824,"threshold_uncertainty_score":0.017510176},"labels":[],"label_agreement":null},{"id":"W3017049878","doi":"10.1029/2019gl086749","title":"Arctic Sea Ice in CMIP6","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":725,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Universität Hamburg; Max-Planck-Gesellschaft; Natural Sciences and Engineering Research Council of Canada; Knut och Alice Wallenbergs Stiftelse; Canadian Meteorological and Oceanographic Society; Bundesministerium für Bildung und Forschung; National Oceanic and Atmospheric Administration; Deutsche Forschungsgemeinschaft; National Science Foundation; Horizon 2020 Framework Programme; Norges Forskningsråd; Commonwealth Scientific and Industrial Research Organisation; Department for Business, Energy and Industrial Strategy, UK Government; Fonds De La Recherche Scientifique - FNRS; Seventh Framework Programme; Met Office; U.S. Department of Energy; Biological and Environmental Research; Department for Environment, Food and Rural Affairs, UK Government; National Center for Atmospheric Research","keywords":"Sea ice; Arctic; Climatology; Arctic ice pack; The arctic; Environmental science; Geology; Oceanography","score_opus":0.03765017705035711,"score_gpt":0.27669241587399596,"score_spread":0.23904223882363884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3017049878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.918039,0.0010276298,0.0069270814,0.0014253042,0.00037130187,0.000037302692,0.031690978,0.00064571435,0.03983562],"genre_scores_gemma":[0.9781446,0.000483008,0.0040544695,0.0001981123,0.000052331434,0.000056457317,0.015169482,0.00016155014,0.001679975],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998292,0.000053677333,0.000008258555,0.000041519943,0.00003323129,0.000034092165],"domain_scores_gemma":[0.9997111,0.00007566145,0.00004189619,0.000037757327,0.000093708375,0.000039851435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006751209,0.00056139287,0.0002324396,0.0004166146,0.00039664912,0.0008970303,0.0005203349,0.0005554294,0.004284205],"category_scores_gemma":[0.001687606,0.00019415317,0.00043451597,0.001329679,0.00021326238,0.0006364705,0.00044382768,0.00054244575,0.0007047185],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018997893,0.000038844046,0.037009884,0.000079752295,0.00012459348,0.00013629437,0.00006203952,0.938255,0.00079475594,0.0040452923,0.010756037,0.008507574],"study_design_scores_gemma":[0.00020886885,0.00010407049,0.06487766,0.00013653937,0.00009321846,0.00019455096,0.00019047421,0.8731148,0.003649083,0.0058038863,0.05154624,0.00008062447],"about_ca_topic_score_codex":0.025329243,"about_ca_topic_score_gemma":0.010849774,"teacher_disagreement_score":0.025329243,"about_ca_system_score_codex":0.00076370226,"about_ca_system_score_gemma":0.0005526825,"threshold_uncertainty_score":0.0503636},"labels":[],"label_agreement":null},{"id":"W3018421187","doi":"10.1029/2020gl087669","title":"River Inflow Dominates Methane Emissions in an Arctic Coastal System","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; University of Calgary; University of British Columbia","funders":"Marine Environmental Observation Prediction and Response Network; Nunavut Arctic College; Arctic Institute of North America; Polar Knowledge Canada; Natural Sciences and Engineering Research Council of Canada; Woods Hole Oceanographic Institution; National Aeronautics and Space Administration; National Defense Science and Engineering Graduate; Killam Trusts; U.S. Department of Defense","keywords":"Estuary; Bay; Environmental science; Greenhouse gas; Methane; Hydrology (agriculture); Carbon dioxide; Arctic ice pack; Inflow; Oceanography; Arctic; Discharge; Sea ice; Melt pond; Cryosphere; Atmospheric sciences; Geology; Drift ice; Drainage basin","score_opus":0.03345392115278885,"score_gpt":0.28276425949492184,"score_spread":0.249310338342133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3018421187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991725,0.00002492341,0.00002071203,0.000021925554,0.0000022089414,0.000001142882,0.00025068072,0.0000051633374,0.00050072686],"genre_scores_gemma":[0.9994042,0.000037545837,0.00004803807,0.000009571398,0.0000025712811,0.000001302852,0.00027513073,0.0000021306794,0.00021941277],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999323,0.0000082361075,0.0000042726124,0.000015885586,0.000015833117,0.00002345253],"domain_scores_gemma":[0.9998061,0.00002188617,0.000036535035,0.000008528853,0.00007971254,0.000047119964],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013557443,0.00019769651,0.00018225831,0.0004674334,0.00073675456,0.0009059065,0.00016479981,0.00018506669,0.00072447635],"category_scores_gemma":[0.00035078335,0.00017110023,0.00011050891,0.0006343485,0.00023436318,0.00020762558,0.0003697526,0.00014253375,0.000115779265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013879321,0.000038334154,0.9871977,0.000013867803,0.000039733306,0.00029280927,0.00037891231,0.0012523816,0.006689125,0.00008993749,0.00038695967,0.0034814102],"study_design_scores_gemma":[0.0000051551306,0.000017021044,0.99571,0.000006028084,0.000019226469,0.000041323347,0.00062966126,0.002280818,0.0006164472,0.00002426026,0.00064433384,0.000005655203],"about_ca_topic_score_codex":0.46253017,"about_ca_topic_score_gemma":0.62581164,"teacher_disagreement_score":0.46253017,"about_ca_system_score_codex":0.0019269445,"about_ca_system_score_gemma":0.0012386475,"threshold_uncertainty_score":0.9196759},"labels":[],"label_agreement":null},{"id":"W3018690166","doi":"10.1029/2020gl087535","title":"Ice Core Record of Persistent Short‐Chain Fluorinated Alkyl Acids: Evidence of the Impact From Global Environmental Regulations","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Per- and polyfluoroalkyl substances research","field":"Environmental Science","cited_by":114,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"General Electric (Canada); University of Toronto; Environment and Climate Change Canada; York University; University of Alberta; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Trifluoroacetic acid; Ice core; Chlorofluorocarbon; Acid deposition; Deposition (geology); Alkyl; Chlorinated paraffins; Environmental chemistry; Environmental science; Chemistry; Arctic; Degradation (telecommunications); Organic chemistry; Climatology; Geology; Oceanography; Soil water; Computer science; Soil science","score_opus":0.08439560701740233,"score_gpt":0.34679872220747815,"score_spread":0.2624031151900758,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3018690166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968041,0.00020489616,0.00016516945,0.000035572048,0.000006887077,0.0000037441744,0.0011652907,0.000011896113,0.0016025116],"genre_scores_gemma":[0.99808216,0.0001918313,0.0003173232,0.000025592219,0.00000837506,0.000004282448,0.0010418465,0.000004571123,0.00032406268],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999521,0.0000038266066,0.0000034282384,0.000014598408,0.000015470794,0.000010600137],"domain_scores_gemma":[0.9997656,0.000020245576,0.000053587788,0.000013444457,0.0001237562,0.000023430606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020471294,0.00020149884,0.00017315273,0.0006495453,0.0003825491,0.0003867069,0.00013753957,0.00024406126,0.00045242862],"category_scores_gemma":[0.00018368488,0.00008396889,0.00013848314,0.00052606245,0.00025333164,0.00021706663,0.0002257508,0.00016256132,0.00010066849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037919494,0.000060213966,0.88356847,0.00007162686,0.00011655352,0.00025000755,0.00035175326,0.0018576743,0.10046646,0.00036860086,0.00072512456,0.011784327],"study_design_scores_gemma":[0.0000074321238,0.000046540747,0.991975,0.000010186739,0.00002290098,0.000054435986,0.00013130857,0.0012342889,0.0044391854,0.000046741712,0.002026798,0.000005193528],"about_ca_topic_score_codex":0.09437456,"about_ca_topic_score_gemma":0.09679478,"teacher_disagreement_score":0.09437456,"about_ca_system_score_codex":0.0007161839,"about_ca_system_score_gemma":0.00050963013,"threshold_uncertainty_score":0.1876505},"labels":[],"label_agreement":null},{"id":"W3018707302","doi":"10.1029/2020gl086950","title":"Efficient Carbon Recycling at the Central‐Northern Lesser Antilles Arc: Implications to Deep Carbon Recycling in Global Subduction Zones","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Forearc; Subduction; Geology; Carbon fibers; Slab; Mantle (geology); Carbon cycle; Crust; Oceanic crust; Arc (geometry); Geochemistry; Earth science; Seismology; Paleontology; Tectonics; Materials science; Geometry","score_opus":0.03402926610644195,"score_gpt":0.2753565616834748,"score_spread":0.24132729557703284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3018707302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99805045,0.00013857374,0.00022452405,0.00008058189,0.0000011318657,0.000003277931,0.00024535522,0.000028212417,0.0012278699],"genre_scores_gemma":[0.9996331,0.00005129872,0.0001346755,0.000005081277,0.0000011216229,0.0000016476616,0.00006756659,0.000004259728,0.0001012838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999176,0.000014731604,0.000006366718,0.000027364913,0.000012376917,0.000021520404],"domain_scores_gemma":[0.9998275,0.000036708,0.00005934626,0.000021091737,0.000039320916,0.000015989288],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002560345,0.0003765707,0.00026745707,0.0010789654,0.00036697663,0.00075318373,0.00023959228,0.00029070635,0.0011104774],"category_scores_gemma":[0.0004266158,0.00019994272,0.00027819216,0.00086626003,0.000556923,0.00039957973,0.0004396962,0.00016319963,0.00012534588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024725328,0.000029020292,0.90172416,0.00012355292,0.00015377933,0.00039465094,0.00029983,0.026941894,0.056171134,0.0009666916,0.00017423271,0.012773771],"study_design_scores_gemma":[0.000010595656,0.00002096666,0.9810121,0.000014794068,0.000029684981,0.00010721889,0.00025995306,0.013998216,0.0033804716,0.00048810698,0.00066577946,0.000012075372],"about_ca_topic_score_codex":0.04215286,"about_ca_topic_score_gemma":0.03407164,"teacher_disagreement_score":0.04215286,"about_ca_system_score_codex":0.001048699,"about_ca_system_score_gemma":0.00039129728,"threshold_uncertainty_score":0.08381498},"labels":[],"label_agreement":null},{"id":"W3021140988","doi":"10.1029/2019gl086722","title":"Dayside Field‐Aligned Current Impacts on Ionospheric Irregularities","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan; University of Calgary","funders":"Direktoratet for internasjonalisering og kvalitetsutvikling i høgare utdanning; Norges Forskningsråd","keywords":"Ionosphere; GNSS applications; Context (archaeology); Earth's magnetic field; Physics; Satellite; Geophysics; Phase (matter); Spacecraft; Electron precipitation; Geodesy; Magnetosphere; Atmospheric sciences; Plasma; Geology; Magnetic field; Astronomy","score_opus":0.028659358169416723,"score_gpt":0.3072627776694539,"score_spread":0.2786034195000372,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021140988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993375,0.00002171176,0.000050015085,0.0000069362986,0.0000013952005,0.0000014995063,0.000078323996,0.0000044132157,0.000498206],"genre_scores_gemma":[0.9997814,0.000016427432,0.000021887383,0.0000026709336,0.0000024443711,8.2740956e-7,0.00008755045,0.0000016713079,0.000085127765],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999478,0.000008362715,0.0000033863616,0.000010389844,0.000015661215,0.00001446169],"domain_scores_gemma":[0.999607,0.00006905472,0.00016954805,0.000026751437,0.00007842084,0.000049216003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010154411,0.00016184399,0.00017738297,0.00036538672,0.0002140775,0.00039411022,0.0000707696,0.00013260738,0.00076868874],"category_scores_gemma":[0.0005456458,0.00005660892,0.00011263293,0.00030264142,0.00019190811,0.00018944284,0.00037781688,0.00012397532,0.00008818688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038478483,0.000050676128,0.9475083,0.0000282177,0.0000871483,0.0003473562,0.0003419132,0.002019733,0.041082125,0.000102674036,0.00023183234,0.007815328],"study_design_scores_gemma":[0.0000021503229,0.000050274895,0.99786216,0.0000017395205,0.000010650084,0.000051904488,0.00011686923,0.0006173438,0.0010712824,0.000022914584,0.00019114446,0.0000016430951],"about_ca_topic_score_codex":0.0031061352,"about_ca_topic_score_gemma":0.0030315623,"teacher_disagreement_score":0.0031061352,"about_ca_system_score_codex":0.00018172471,"about_ca_system_score_gemma":0.00010649699,"threshold_uncertainty_score":0.006176114},"labels":[],"label_agreement":null},{"id":"W3021315524","doi":"10.1029/2020gl089211","title":"Meltwater Penetration Through Temperate Ice Layers in the Percolation Zone at DYE‐2, Greenland Ice Sheet","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; National Science Foundation","keywords":"Meltwater; Firn; Greenland ice sheet; Ice sheet; Geology; Melt pond; Sea ice; Snow; Ice stream; Geomorphology; Cryosphere; Climatology","score_opus":0.07487412765109504,"score_gpt":0.29377419577993297,"score_spread":0.21890006812883794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021315524","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99959165,0.000016423453,0.000035652207,0.000004820751,3.3687454e-7,0.0000012932652,0.00008405099,0.0000056265767,0.00026007587],"genre_scores_gemma":[0.9996848,0.000012819144,0.00006297679,0.000005241925,3.8259031e-7,0.0000017738472,0.00009619092,0.0000017974049,0.00013394824],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996614,0.000002464686,0.0000011376825,0.0000134650045,0.0000048600564,0.0000118656235],"domain_scores_gemma":[0.9999496,0.000012223736,0.0000098081755,0.0000025000986,0.00000732242,0.00001859886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000075616575,0.00018571207,0.0001670787,0.00036164437,0.00034691146,0.00041738816,0.00019424631,0.00018690994,0.00071869075],"category_scores_gemma":[0.00011655867,0.00012582945,0.00011442902,0.00019927051,0.00032064872,0.00033304247,0.00024408872,0.00017492421,0.00007601566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00081932923,0.0001486329,0.60847247,0.000081475264,0.00008925916,0.00051382446,0.0017937598,0.004645795,0.36901274,0.0003776345,0.0003445784,0.013700628],"study_design_scores_gemma":[0.000009210577,0.000040410334,0.9923596,0.000007135032,0.000008589953,0.000035318393,0.00027887864,0.002121755,0.0048086685,0.000040641993,0.00028473508,0.0000050759513],"about_ca_topic_score_codex":0.072201304,"about_ca_topic_score_gemma":0.14321841,"teacher_disagreement_score":0.072201304,"about_ca_system_score_codex":0.0012447152,"about_ca_system_score_gemma":0.00040490952,"threshold_uncertainty_score":0.14356208},"labels":[],"label_agreement":null},{"id":"W3021450946","doi":"10.1029/2019gl086240","title":"Real‐Time Earthquake Location Based on the Kalman Filter Formulation","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Earthquake prediction; Geology; Seismology; Earthquake simulation; Kalman filter; Earthquake location; Geodesy; Computer science; Induced seismicity","score_opus":0.05336887173929608,"score_gpt":0.2975340587950763,"score_spread":0.2441651870557802,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021450946","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0068060244,0.00007020487,0.9920597,0.000055334032,0.0000178438,0.000008927301,0.0000347998,0.00019627048,0.0007508048],"genre_scores_gemma":[0.7421259,0.00032548278,0.25204265,0.00008075899,0.00007440463,0.00010493135,0.00022252895,0.00007172927,0.0049515553],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997843,0.000056888395,0.000013865273,0.00005911865,0.00006684082,0.000019008308],"domain_scores_gemma":[0.99959475,0.00020351511,0.000061095656,0.000026700414,0.00010340127,0.000010464782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004347832,0.00039680282,0.00036902615,0.0002278753,0.00016710213,0.00050317345,0.0005260998,0.00048399714,0.0017036785],"category_scores_gemma":[0.0013259851,0.00025965116,0.00025640338,0.0003133397,0.00035863352,0.00069353834,0.00032311716,0.00056406175,0.00044933215],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058815473,0.000020376972,0.0006499864,0.000052559044,0.000025993886,0.000038073045,0.000052395393,0.93855745,0.005913203,0.0076908646,0.0007276666,0.046212558],"study_design_scores_gemma":[0.0000058428136,0.000011384027,0.00011962208,0.0000019945637,0.0000030299082,0.000005757794,0.0000021939488,0.9985102,0.00057792524,0.00047783824,0.00027975903,0.000004580036],"about_ca_topic_score_codex":0.013516811,"about_ca_topic_score_gemma":0.009489639,"teacher_disagreement_score":0.013516811,"about_ca_system_score_codex":0.00055908685,"about_ca_system_score_gemma":0.000814315,"threshold_uncertainty_score":0.02687627},"labels":[],"label_agreement":null},{"id":"W3021451744","doi":"10.1029/2019gl086926","title":"Continuity of the Mass Loss of the World's Glaciers and Ice Caps From the GRACE and GRACE Follow‐On Missions","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":171,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Glacier; Arctic; Climatology; Glacier mass balance; Ice caps; Archipelago; Geology; Physical geography; Oceanography; Geography","score_opus":0.042641130032788285,"score_gpt":0.2731729582859108,"score_spread":0.23053182825312252,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021451744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9856279,0.0001631689,0.0008214054,0.00008492008,0.000015688647,0.00001118064,0.010314711,0.00011542083,0.0028455707],"genre_scores_gemma":[0.9859692,0.00008629465,0.0006523558,0.000027533386,0.000017733002,0.000014714471,0.012758068,0.00003839651,0.0004357366],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996973,0.00003702561,0.00003291675,0.00006848836,0.00011314028,0.000051195424],"domain_scores_gemma":[0.9990637,0.00009683042,0.00039117527,0.00014777906,0.00024117313,0.000059494312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007565586,0.00036583058,0.0002685315,0.0019875292,0.00023370472,0.000787756,0.00031292206,0.00024992545,0.0007150958],"category_scores_gemma":[0.0016837895,0.00013625651,0.00042635744,0.0021240716,0.00026842143,0.0005386817,0.00059726904,0.00032187047,0.00029051074],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042346673,0.0000509029,0.96525294,0.00004286368,0.00029089983,0.00015812617,0.00023649247,0.008239361,0.004674774,0.00035519028,0.0020678616,0.018207122],"study_design_scores_gemma":[0.0000066357975,0.00003635103,0.992063,0.000009871914,0.00003314556,0.000076282675,0.00008363428,0.003911514,0.0015413016,0.000082320934,0.0021441332,0.00001191631],"about_ca_topic_score_codex":0.01535676,"about_ca_topic_score_gemma":0.0127715375,"teacher_disagreement_score":0.01535676,"about_ca_system_score_codex":0.00039215037,"about_ca_system_score_gemma":0.00032720258,"threshold_uncertainty_score":0.030534744},"labels":[],"label_agreement":null},{"id":"W3021912068","doi":"10.1029/2020gl088100","title":"Sea Ice Retreat Contributes to Projected Increases in Extreme Arctic Ocean Surface Waves","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":56,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Coupled model intercomparison project; Arctic; Climatology; Sea ice; The arctic; Fetch; Environmental science; Wind wave; Arctic sea ice decline; Climate model; Arctic ice pack; Climate change; Geology; Atmospheric sciences; Oceanography; Drift ice","score_opus":0.055935337730734086,"score_gpt":0.27033267747746437,"score_spread":0.21439733974673028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021912068","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99424666,0.0002895955,0.0007620997,0.00079162366,0.000041993426,0.0000069068565,0.001077082,0.000050949802,0.0027331482],"genre_scores_gemma":[0.9987839,0.0001765895,0.00013954719,0.000035818935,0.000018061048,0.0000043172167,0.00054003927,0.000005919824,0.000295705],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99977773,0.00006415073,0.000018416127,0.000040577754,0.000041887077,0.000057248097],"domain_scores_gemma":[0.9992268,0.000110915695,0.0002711782,0.000037885227,0.00022101386,0.00013219209],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009078005,0.0004356158,0.00018602169,0.00049926585,0.0002597274,0.0008822465,0.00031214528,0.00046635568,0.0023977356],"category_scores_gemma":[0.0021996757,0.00021784664,0.00072648027,0.0005013334,0.00016101709,0.00040937174,0.00065192184,0.00050871796,0.000434441],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030169453,0.000049679842,0.9446641,0.000055315573,0.00020057058,0.00053681555,0.000102004975,0.034343727,0.0020418016,0.00050619314,0.0011596279,0.016038517],"study_design_scores_gemma":[0.000023408009,0.000161488,0.95150185,0.000032272907,0.00011763594,0.00023786465,0.00032467998,0.043169618,0.001111722,0.00078369153,0.0025179933,0.000017721033],"about_ca_topic_score_codex":0.013498594,"about_ca_topic_score_gemma":0.012536618,"teacher_disagreement_score":0.013498594,"about_ca_system_score_codex":0.0005758703,"about_ca_system_score_gemma":0.00064931315,"threshold_uncertainty_score":0.02684009},"labels":[],"label_agreement":null},{"id":"W3021980337","doi":"10.1029/2019gl086764","title":"Black Carbon Particles Do Not Matter for Immersion Mode Ice Nucleation","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":127,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Métis National Council","funders":"Eidgenössische Technische Hochschule Zürich; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Soot; Ice nucleus; Immersion (mathematics); Nucleation; Carbon black; Ice crystals; Materials science; Ice cloud; Particle size; Mineralogy; Clear ice; Chemical engineering; Geology; Chemistry; Thermodynamics; Sea ice; Composite material; Meteorology; Physics; Arctic ice pack; Combustion; Optics; Oceanography; Physical chemistry","score_opus":0.04047953394027738,"score_gpt":0.2855104277712915,"score_spread":0.24503089383101412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3021980337","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995099,0.00028003895,0.0015788091,0.00006232338,0.000040811985,0.000018912844,0.00027468224,0.00004737222,0.0025980598],"genre_scores_gemma":[0.9995122,0.00004076329,0.00016536993,0.00000690912,0.0000031773848,0.0000018966662,0.00011398946,0.000009263332,0.00014628192],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998253,0.000016841888,0.000006686845,0.000050480565,0.00005381788,0.00004682199],"domain_scores_gemma":[0.99945253,0.0002791895,0.00006793414,0.000034381148,0.00008478133,0.000081155384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017800022,0.00045298334,0.00023566416,0.00020955096,0.00030604287,0.0005860246,0.0003014932,0.0004285333,0.0022917413],"category_scores_gemma":[0.0009816384,0.00013843442,0.00026849232,0.0001173751,0.00029048303,0.00044439416,0.00016702042,0.00025450753,0.00020059502],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013115746,0.0003379503,0.12740663,0.0005007822,0.0003159478,0.00061344594,0.00010186074,0.07789994,0.77108985,0.0030159154,0.0009673841,0.016438724],"study_design_scores_gemma":[0.00012706859,0.0005689974,0.16557175,0.000049153237,0.00023200405,0.00025970786,0.00019272995,0.40702632,0.421438,0.0021730228,0.0022983106,0.00006295032],"about_ca_topic_score_codex":0.008379007,"about_ca_topic_score_gemma":0.0034685244,"teacher_disagreement_score":0.008379007,"about_ca_system_score_codex":0.00039244845,"about_ca_system_score_gemma":0.00024510457,"threshold_uncertainty_score":0.016660511},"labels":[],"label_agreement":null},{"id":"W3022185668","doi":"10.1029/2020gl088120","title":"A Comparison Between Station Observations and Reanalysis Data in the Identification of Extreme Temperature Events","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":119,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Environmental science; Extreme Cold; Heat wave; Extreme heat; Cold wave; Middle latitudes; Arctic; The arctic; Meteorology; Climate change; Geography; Geology; Oceanography","score_opus":0.29303628889138983,"score_gpt":0.39822236454252263,"score_spread":0.1051860756511328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022185668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.993483,0.00023230213,0.0018365382,0.000041966214,0.000021390502,0.000015973057,0.0027064215,0.000034911827,0.0016274877],"genre_scores_gemma":[0.99559695,0.00007534606,0.0012996272,0.000016195947,0.000011439544,0.000008292111,0.0028308774,0.000008436793,0.00015294633],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9989034,0.00035153146,0.00016710225,0.0003027092,0.00020792102,0.00006739415],"domain_scores_gemma":[0.9937231,0.0023977265,0.0014724068,0.00057869364,0.0016169196,0.00021125132],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002755524,0.00017254605,0.00022662639,0.001410916,0.00019709893,0.0010786,0.00022772825,0.0002331552,0.0009570121],"category_scores_gemma":[0.009996204,0.00013383426,0.00032451755,0.0021793302,0.00015608354,0.0008803743,0.00074183,0.00022399717,0.0002924482],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017503812,0.00001831097,0.9846799,0.000028994207,0.00018771723,0.000023784953,0.00018966482,0.0015677611,0.0009417068,0.00010692063,0.00040498716,0.011675209],"study_design_scores_gemma":[0.000007096181,0.000031426036,0.99343795,0.00001722813,0.000039517236,0.0000203767,0.00030839947,0.004919677,0.00051701325,0.00007197637,0.000620473,0.000008966351],"about_ca_topic_score_codex":0.014875208,"about_ca_topic_score_gemma":0.021236537,"teacher_disagreement_score":0.014875208,"about_ca_system_score_codex":0.00028765213,"about_ca_system_score_gemma":0.00036963617,"threshold_uncertainty_score":0.029577255},"labels":[],"label_agreement":null},{"id":"W3022916852","doi":"10.1029/2020gl087505","title":"Decreasing Landslide Erosion on Steeper Slopes in Soil‐Mantled Landscapes","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"ETH Zürich Foundation; Uniscientia Stiftung; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Landslide; Geology; Cohesion (chemistry); Erosion; Soil water; Geomorphology; Landslide mitigation; Creep; Geotechnical engineering; Landslide classification; Soil science","score_opus":0.026951668153520222,"score_gpt":0.281439914382408,"score_spread":0.25448824622888777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022916852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99958736,0.000015828184,0.00007140812,0.000004307689,2.8026693e-7,7.216935e-7,0.000051821266,0.00000663438,0.00026161812],"genre_scores_gemma":[0.9998054,0.0000108110335,0.00006427149,0.0000026743494,5.557281e-7,6.2571036e-7,0.00006751106,0.0000011306026,0.000046927453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994385,0.000005938235,0.0000033597616,0.00001847582,0.00000969509,0.000018758987],"domain_scores_gemma":[0.99971825,0.00003508842,0.00011923004,0.000029313556,0.000043687694,0.00005442479],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101360005,0.00014985798,0.00020673053,0.000883918,0.00024709385,0.00057302945,0.00015062297,0.00018890982,0.0011047291],"category_scores_gemma":[0.00042986483,0.00014086979,0.00014800673,0.00055728276,0.00031890368,0.00020480098,0.00026874227,0.00015206246,0.00016075998],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010424611,0.000045728633,0.9625573,0.000034608496,0.00006448684,0.00014420453,0.00023578592,0.004990665,0.02344633,0.00016504539,0.00014518746,0.00806647],"study_design_scores_gemma":[0.0000020812622,0.000012189496,0.9988304,0.0000014263398,0.000004137798,0.000021322452,0.00003920528,0.0006415813,0.00034230738,0.000034833734,0.000068658024,0.00000190857],"about_ca_topic_score_codex":0.00995411,"about_ca_topic_score_gemma":0.025323926,"teacher_disagreement_score":0.00995411,"about_ca_system_score_codex":0.00039073292,"about_ca_system_score_gemma":0.00012063779,"threshold_uncertainty_score":0.019792318},"labels":[],"label_agreement":null},{"id":"W3022998026","doi":"10.1029/2019gl086757","title":"Climate Model Projections of 21st Century Global Warming Constrained Using the Observed Warming Trend","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":167,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Coupled model intercomparison project; Climatology; Global warming; Environmental science; Climate model; Weighting; Cru; Climate sensitivity; Climate change; Geology","score_opus":0.1432999914926909,"score_gpt":0.3433602643250127,"score_spread":0.2000602728323218,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3022998026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9374088,0.00016807715,0.045086514,0.0005954507,0.0000920625,0.000048214974,0.006097822,0.00045176482,0.010051261],"genre_scores_gemma":[0.98182505,0.0001091986,0.013000804,0.000072492774,0.0000337053,0.00008545077,0.0040409574,0.00006652508,0.00076582277],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99969196,0.0001305048,0.000020200809,0.0000744236,0.00004729312,0.00003561188],"domain_scores_gemma":[0.9992083,0.00029901505,0.00010658519,0.0001332198,0.00020634626,0.000046578985],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0016876897,0.0004527123,0.00031663096,0.0005946125,0.0002514391,0.0005496143,0.0006048215,0.00047616445,0.0021395087],"category_scores_gemma":[0.0032300272,0.00026597327,0.00087555445,0.0010079003,0.00019921028,0.00071458117,0.00048046617,0.0006286115,0.00030669567],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000058835853,0.000025664878,0.009385799,0.000019339159,0.00010112722,0.000011655372,0.000011140349,0.9839969,0.00038490107,0.0018136958,0.00061370083,0.0035772333],"study_design_scores_gemma":[0.00006135457,0.00003556278,0.015770156,0.0000208795,0.000050634546,0.000011806506,0.000025153466,0.9774811,0.0008474266,0.004237864,0.0014325591,0.00002544555],"about_ca_topic_score_codex":0.02421264,"about_ca_topic_score_gemma":0.018782364,"teacher_disagreement_score":0.02421264,"about_ca_system_score_codex":0.0007024187,"about_ca_system_score_gemma":0.0010210843,"threshold_uncertainty_score":0.048143387},"labels":[],"label_agreement":null},{"id":"W3023579671","doi":"10.1029/2020gl087977","title":"Molecular Absorption and Evolution Mechanisms of PM<sub>2.5</sub>Brown Carbon Revealed by Electrospray Ionization Fourier Transform–Ion Cyclotron Resonance Mass Spectrometry During a Severe Winter Pollution Episode in Xi'an, China","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"China Scholarship Council; National Natural Science Foundation of China","keywords":"Fourier transform ion cyclotron resonance; Chemistry; Absorption (acoustics); Molecule; Analytical Chemistry (journal); Mass spectrometry; Electrospray ionization; Carbon fibers; Ion; Ionization; Materials science; Environmental chemistry; Organic chemistry; Chromatography","score_opus":0.0064861520445529805,"score_gpt":0.21104343796186747,"score_spread":0.2045572859173145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3023579671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949753,0.000045359593,0.000090322465,0.000012910357,0.0000023033697,0.0000034931393,0.00014473725,0.0000053671783,0.00019806511],"genre_scores_gemma":[0.9994574,0.000035341716,0.00012367876,0.000013720334,0.0000037265352,0.0000037721204,0.00016192665,0.0000015718075,0.00019887787],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999242,0.0000049199066,0.0000030559381,0.000028101294,0.000024989875,0.000014612876],"domain_scores_gemma":[0.99991965,0.0000070280657,0.00002769855,0.0000029818134,0.00002903406,0.00001357512],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013809097,0.00027459417,0.0001392234,0.00064890087,0.00036617863,0.00022011198,0.00020428824,0.00025054865,0.00040761373],"category_scores_gemma":[0.00009567075,0.00013961384,0.00014978326,0.00034759028,0.00019872538,0.00017178747,0.00016720606,0.00015625985,0.00005883397],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003014944,0.00007551361,0.6394997,0.00008454414,0.00013382778,0.00060243096,0.0005275902,0.0010189017,0.34802628,0.00018219004,0.0005300192,0.009017444],"study_design_scores_gemma":[0.000002098434,0.000019685205,0.99429685,0.0000015542598,0.000009986818,0.000040737224,0.00009444043,0.0010809696,0.0042731715,0.000014708681,0.00016176564,0.000003962746],"about_ca_topic_score_codex":0.03594632,"about_ca_topic_score_gemma":0.057460714,"teacher_disagreement_score":0.03594632,"about_ca_system_score_codex":0.00049015327,"about_ca_system_score_gemma":0.0002784562,"threshold_uncertainty_score":0.071474135},"labels":[],"label_agreement":null},{"id":"W3024164655","doi":"10.1029/2020gl086983","title":"Where Do Cold Air Outbreaks Occur, and How Have They Changed Over Time?","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Outbreak; Environmental science; Atmospheric sciences; Meteorology; Climatology; Geology; Geography; Medicine; Virology","score_opus":0.041502289125687396,"score_gpt":0.2874797653370401,"score_spread":0.2459774762113527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024164655","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9733542,0.01043791,0.0010065724,0.0044770357,0.00041660812,0.00004249423,0.006350538,0.000053464704,0.0038612292],"genre_scores_gemma":[0.99444467,0.0024846783,0.00022782649,0.0003375513,0.00019293277,0.000023110471,0.0019257138,0.0000126679615,0.00035093256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99852705,0.00030931135,0.00018592809,0.00047993872,0.0002058472,0.00029197527],"domain_scores_gemma":[0.99494725,0.0008895403,0.0023010448,0.00023996581,0.0012485093,0.0003737346],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0024421504,0.00027612105,0.00051521976,0.001942976,0.00047861494,0.0024251346,0.00047825073,0.0008001842,0.0020723036],"category_scores_gemma":[0.008211138,0.00022992899,0.000721494,0.0023850538,0.000740131,0.0024566688,0.0006725451,0.0011199013,0.00041861166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007325652,0.000019346528,0.9854896,0.00013054654,0.00021250993,0.000058029374,0.00058773236,0.00026178185,0.00017696753,0.00018799707,0.0018028838,0.0109992875],"study_design_scores_gemma":[0.0000033753765,0.000022172102,0.99490154,0.00014854783,0.00005530235,0.00006520374,0.001501245,0.0006107662,0.00010704641,0.00018748283,0.0023823432,0.000014986923],"about_ca_topic_score_codex":0.03969016,"about_ca_topic_score_gemma":0.040900588,"teacher_disagreement_score":0.03969016,"about_ca_system_score_codex":0.0012564253,"about_ca_system_score_gemma":0.0008580515,"threshold_uncertainty_score":0.07891828},"labels":[],"label_agreement":null},{"id":"W3024695573","doi":"10.1029/2020gl087695","title":"A Conceptual Model for Anticipating the Impact of Landscape Evolution on Groundwater Recharge in Degrading Permafrost Environments","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Center for Northern Studies","funders":"Natural Sciences and Engineering Research Council of Canada; Canada First Research Excellence Fund; Université Laval","keywords":"Permafrost; Groundwater recharge; Thermokarst; Groundwater; Water table; Vegetation (pathology); Hydrology (agriculture); Tundra; Environmental science; Geology; Arctic; Subarctic climate; Physical geography; Aquifer; Geography; Geotechnical engineering; Oceanography","score_opus":0.16344399411997257,"score_gpt":0.34546463045369014,"score_spread":0.18202063633371757,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3024695573","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4379867,0.00046012242,0.51522505,0.0041905195,0.00010972289,0.00019691556,0.0029699337,0.00057951396,0.038281605],"genre_scores_gemma":[0.9601569,0.0002729546,0.035101045,0.00012221356,0.000025882693,0.000195086,0.0004608983,0.00005712182,0.0036078766],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99985516,0.000043219734,0.000009108798,0.000044048003,0.000021386302,0.000027139442],"domain_scores_gemma":[0.99949443,0.00022505784,0.00008235474,0.000026754471,0.00010493556,0.000066467735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00060831243,0.00041276446,0.00037189774,0.000878771,0.0006247983,0.0018498403,0.002431454,0.0013832795,0.0045079817],"category_scores_gemma":[0.0015866939,0.00035128466,0.0007956003,0.0010776499,0.0010126497,0.0023335037,0.0008067249,0.0007469068,0.00025543224],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000018471177,0.000039275103,0.004581966,0.000035710287,0.00003251552,0.000130139,0.00018330745,0.9420405,0.0008949938,0.048838694,0.00043851245,0.0027658455],"study_design_scores_gemma":[0.000011713455,0.000015603939,0.0009664732,0.000008874617,0.000015321815,0.000024859895,0.00011559123,0.9830688,0.000096466596,0.0144636575,0.0012011257,0.000011410426],"about_ca_topic_score_codex":0.051982135,"about_ca_topic_score_gemma":0.04935506,"teacher_disagreement_score":0.051982135,"about_ca_system_score_codex":0.0028418056,"about_ca_system_score_gemma":0.0018613401,"threshold_uncertainty_score":0.1033591},"labels":[],"label_agreement":null},{"id":"W3026084050","doi":"10.1029/2020gl088507","title":"Irreversibility of Marine Climate Change Impacts Under Carbon Dioxide Removal","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"","keywords":"Overshoot (microwave communication); Environmental science; Representative Concentration Pathways; Carbon dioxide; Climate change; Cumulative effects; Carbon cycle; Cycling; Greenhouse gas; Climatology; Atmospheric sciences; Climate model; Oceanography; Ecosystem; Computer science; Ecology; Geology; Geography","score_opus":0.07186744363150202,"score_gpt":0.30580095049961903,"score_spread":0.233933506868117,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3026084050","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99827325,0.00003174958,0.0004375056,0.00007025871,0.0000065602935,0.0000045260736,0.00010964094,0.00002302793,0.0010434735],"genre_scores_gemma":[0.9998165,0.000009387474,0.000059423477,0.000007968322,7.2637584e-7,0.0000018656469,0.000040799267,0.0000014683416,0.00006187378],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999757,0.00007164625,0.000011719923,0.000051531777,0.000039114577,0.00006904452],"domain_scores_gemma":[0.9993728,0.00030361983,0.000100992125,0.00007535757,0.00008097373,0.00006617984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056986744,0.00033446413,0.0002837332,0.00023550064,0.00022279669,0.0005150464,0.00049899844,0.00051030825,0.00087558327],"category_scores_gemma":[0.0018191698,0.00012530907,0.00066055893,0.00024958327,0.0005384948,0.00042133944,0.00049404794,0.00037196884,0.00005244341],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015162731,0.0002579945,0.15861258,0.00012375135,0.0004884592,0.0007006597,0.00009138377,0.7762042,0.049455035,0.0033014985,0.0005527907,0.008695355],"study_design_scores_gemma":[0.00014239724,0.00110466,0.3394211,0.000014239743,0.0002327616,0.00018375118,0.00057168957,0.63022065,0.02296065,0.0036362652,0.0014343692,0.00007748563],"about_ca_topic_score_codex":0.015029119,"about_ca_topic_score_gemma":0.00849891,"teacher_disagreement_score":0.015029119,"about_ca_system_score_codex":0.0010506901,"about_ca_system_score_gemma":0.00047463522,"threshold_uncertainty_score":0.029883325},"labels":[],"label_agreement":null},{"id":"W3026339562","doi":"10.1029/2020gl087953","title":"Geography and Morphology Affect the Ice Duration Dynamics of Northern Hemisphere Lakes Worldwide","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"","keywords":"Northern Hemisphere; Physical geography; Climate change; Climatology; Latitude; Southern Hemisphere; Cryosphere; Duration (music); Environmental science; Geography; Sea ice; Geology; Oceanography","score_opus":0.015707678451252767,"score_gpt":0.24719377790244412,"score_spread":0.23148609945119136,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3026339562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993286,0.000066431305,0.000041870535,0.000014415952,6.2488493e-7,8.4602584e-7,0.00015763589,0.0000018318844,0.00038771477],"genre_scores_gemma":[0.9996043,0.000048836686,0.000043037766,0.0000042337947,0.0000016320788,0.0000014042455,0.0001848291,0.0000013718274,0.0001103906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999373,0.00001532731,0.000005025801,0.00001730496,0.000009982006,0.000015093884],"domain_scores_gemma":[0.9995666,0.00007987392,0.0002282044,0.000019832576,0.000058345126,0.000047127996],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021093735,0.00008983931,0.00012736484,0.0005582415,0.00018983829,0.00050221727,0.0000946842,0.00009444361,0.0011196203],"category_scores_gemma":[0.0008230856,0.00007780927,0.00014162766,0.0007369221,0.00020397974,0.0004005964,0.00031918258,0.00008350058,0.00010184811],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037225007,0.0000046080313,0.9951998,0.0000066125517,0.000024896652,0.000028086692,0.00018909934,0.0003525366,0.0015250692,0.00003099996,0.000071113405,0.0025298982],"study_design_scores_gemma":[3.6229093e-7,0.0000043884575,0.999632,9.992076e-7,0.0000028057539,0.000008721442,0.00009869535,0.00012405575,0.000038515358,0.000010826202,0.00007788987,6.663741e-7],"about_ca_topic_score_codex":0.020985661,"about_ca_topic_score_gemma":0.046602167,"teacher_disagreement_score":0.020985661,"about_ca_system_score_codex":0.0003200196,"about_ca_system_score_gemma":0.00019117903,"threshold_uncertainty_score":0.041727006},"labels":[],"label_agreement":null},{"id":"W3027188166","doi":"10.1029/2019gl086875","title":"Determining the Anthropogenic Greenhouse Gas Contribution to the Observed Intensification of Extreme Precipitation","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":141,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria; Environment and Climate Change Canada","funders":"National Research Foundation of Korea; Horizon 2020 Framework Programme; Korea Meteorological Administration; Australian Research Council; National Research Foundation","keywords":"Precipitation; Environmental science; Greenhouse gas; Climatology; Tropics; Northern Hemisphere; Atmospheric sciences; Southern Hemisphere; Global warming; Climate change; Meteorology; Ecology; Geology; Geography; Oceanography","score_opus":0.1537071073904688,"score_gpt":0.32815318842691577,"score_spread":0.17444608103644696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3027188166","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989876,0.000045677953,0.0003728969,0.000007719374,0.000003032074,0.0000022660163,0.00029553295,0.0000103960465,0.00027484304],"genre_scores_gemma":[0.99939466,0.000026225569,0.00022116168,0.000001970361,0.0000036767435,0.0000018784683,0.00031558066,0.0000012744606,0.000033540393],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993813,0.000012448481,0.0000053270824,0.000020708085,0.000011798817,0.000011509647],"domain_scores_gemma":[0.9998248,0.000050340645,0.000061519735,0.000019802203,0.000028580456,0.000014935175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028387876,0.00017055585,0.00011730775,0.00045930987,0.0001060162,0.00024330568,0.00011380083,0.00008928138,0.00048197762],"category_scores_gemma":[0.00046596487,0.000080624624,0.00022069324,0.0004572752,0.00011062868,0.00014915843,0.00018819788,0.000110677756,0.00006630268],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012027607,0.000022265309,0.9760936,0.000028882943,0.00008884787,0.0000578432,0.000037435595,0.005569508,0.009275541,0.00011018201,0.00011235912,0.008483205],"study_design_scores_gemma":[0.000002183411,0.000015651774,0.9942602,0.00000228309,0.000011827342,0.000031696432,0.000027535687,0.0039629405,0.0014617777,0.000026399795,0.00019508276,0.000002489822],"about_ca_topic_score_codex":0.005208323,"about_ca_topic_score_gemma":0.008138181,"teacher_disagreement_score":0.005208323,"about_ca_system_score_codex":0.0002576544,"about_ca_system_score_gemma":0.00019347754,"threshold_uncertainty_score":0.010356009},"labels":[],"label_agreement":null},{"id":"W3028059762","doi":"10.1029/2020gl087987","title":"Stratospheric Water Vapor Feedback Disclosed by a Locking Experiment","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Global warming; Water vapor; Troposphere; Atmospheric sciences; Climatology; Climate change; Humidity; Cloud feedback; Climate model; Meteorology; Climate sensitivity; Geology; Geography","score_opus":0.03621085255340194,"score_gpt":0.27675862376389293,"score_spread":0.24054777121049098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3028059762","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970594,0.000029012092,0.0023507911,0.000035214143,0.000025495727,0.000015380841,0.00011481609,0.000064101565,0.00030574235],"genre_scores_gemma":[0.99905163,0.000013008836,0.00065733376,0.000030871965,0.0000045526335,0.000023000961,0.0000501035,0.000011673707,0.00015775581],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997787,0.00006710972,0.000017538603,0.00006581704,0.000032040465,0.000038864695],"domain_scores_gemma":[0.99878997,0.0005994462,0.00019896276,0.00022792057,0.000062010295,0.000121700185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068034034,0.00035931813,0.00031546486,0.00017606326,0.00021811538,0.0004311779,0.00042588724,0.00037026533,0.0022392375],"category_scores_gemma":[0.0010169831,0.00017798443,0.00028340498,0.00014067099,0.0004263438,0.0004826413,0.00052082795,0.00065901235,0.00012910126],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0031411739,0.000604861,0.016871234,0.0000866832,0.00012687162,0.00011908919,0.000078576944,0.011249855,0.9601393,0.0018874797,0.00017502024,0.0055200206],"study_design_scores_gemma":[0.0011499452,0.006279479,0.027252292,0.000012149142,0.00022122277,0.00014152439,0.0001368957,0.0733864,0.88572335,0.0039982744,0.0016018213,0.000096703436],"about_ca_topic_score_codex":0.0006826183,"about_ca_topic_score_gemma":0.00046330833,"teacher_disagreement_score":0.0022392375,"about_ca_system_score_codex":0.00026317008,"about_ca_system_score_gemma":0.00025584735,"threshold_uncertainty_score":0.007490933},"labels":[],"label_agreement":null},{"id":"W3030130144","doi":"10.1029/2020gl088019","title":"Simultaneous Observations of Localized and Global Drift Resonance","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Resonance (particle physics); Physics; Electron; Atomic physics; Van Allen Probes; Electron spectrometer; Pitch angle; Van Allen radiation belt; Computational physics; Plasma; Magnetosphere; Geophysics; Cathode ray; Nuclear physics","score_opus":0.025862571426277455,"score_gpt":0.29002293070561214,"score_spread":0.2641603592793347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3030130144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969739,0.00013519898,0.0017695333,0.000018285138,0.0000049267173,0.000002616615,0.000028970786,0.000029128032,0.0010373745],"genre_scores_gemma":[0.9992205,0.000017015967,0.0004548885,0.0000075258367,0.0000022509744,0.0000016654822,0.000024511477,0.0000032699584,0.00026837553],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999629,0.0000033381843,8.046328e-7,0.000014194177,0.0000077112745,0.000010937638],"domain_scores_gemma":[0.99994564,0.000014057871,0.00001195347,0.000007272042,0.000009653341,0.000011410835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006554553,0.00014499907,0.00012203871,0.00026830652,0.00011164735,0.000135107,0.00016162053,0.00018483461,0.0007067422],"category_scores_gemma":[0.0001038657,0.00009200836,0.00007394504,0.00011244588,0.00014243892,0.00018193328,0.00028806957,0.00019187591,0.00008132831],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018003184,0.0000105882855,0.012368641,0.000025507366,0.000018523991,0.00022946192,0.00012902825,0.00029919567,0.9802194,0.00036392617,0.00011046144,0.0060451673],"study_design_scores_gemma":[0.000081226084,0.00059370225,0.3086442,0.000024556182,0.00010294806,0.0016458562,0.0006214489,0.01696916,0.66326815,0.0015589908,0.006440117,0.00004967875],"about_ca_topic_score_codex":0.00025779667,"about_ca_topic_score_gemma":0.00050811487,"teacher_disagreement_score":0.0007067422,"about_ca_system_score_codex":0.00007959874,"about_ca_system_score_gemma":0.000034399756,"threshold_uncertainty_score":0.0023642778},"labels":[],"label_agreement":null},{"id":"W3030442117","doi":"10.1029/2020gl087237","title":"Lipid Biomarker Record Documents Hydroclimatic Variability of the Mississippi River Basin During the Common Era","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Environmental science; Flood myth; Precipitation; Proxy (statistics); Structural basin; Climatology; Arid; Climate change; Flooding (psychology); Growing season; Drainage basin; Paleoclimatology; Hydrology (agriculture); Physical geography; Geology; Geography; Oceanography; Meteorology; Archaeology; Ecology","score_opus":0.0368137622560133,"score_gpt":0.2886043995263072,"score_spread":0.2517906372702939,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3030442117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993025,0.000031677133,0.00005051493,0.000027483042,5.39845e-7,9.4891885e-7,0.00031764273,0.000005709107,0.00026294886],"genre_scores_gemma":[0.99951136,0.000022873615,0.00007002778,0.000008344123,0.0000014047873,0.0000018946471,0.00029706326,0.0000012647046,0.00008563683],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999621,0.000005746447,0.0000025113277,0.000014168199,0.000007437661,0.00000805093],"domain_scores_gemma":[0.9998411,0.000012312622,0.00006195189,0.000014262965,0.00004180417,0.000028545128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014402084,0.0001292672,0.00010269933,0.0006453515,0.0004144848,0.0004050709,0.00016084246,0.00017596775,0.0006343923],"category_scores_gemma":[0.0002349122,0.00008267475,0.00008617839,0.00071056065,0.00019482891,0.00028144583,0.0003783754,0.00015076883,0.00008245816],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048172795,0.000019588557,0.9810079,0.000011887236,0.0000575474,0.00007782718,0.00035514566,0.0008388599,0.012818489,0.00009104457,0.00022255277,0.0044510467],"study_design_scores_gemma":[0.0000012736577,0.000009341996,0.9976941,0.0000025218735,0.00000670909,0.00002610545,0.00019832847,0.0009921826,0.0005697087,0.000023464574,0.00047301754,0.0000032935375],"about_ca_topic_score_codex":0.050546695,"about_ca_topic_score_gemma":0.13466084,"teacher_disagreement_score":0.050546695,"about_ca_system_score_codex":0.00060887885,"about_ca_system_score_gemma":0.000305213,"threshold_uncertainty_score":0.100504994},"labels":[],"label_agreement":null},{"id":"W3030491266","doi":"10.1029/2020gl087221","title":"A Long‐Lived Sharp Disruption on the Lower Clouds of Venus","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration; Japan Society for the Promotion of Science; Japan Aerospace Exploration Agency; Seventh Framework Programme; Fundação para a Ciência e a Tecnologia; Ministerio de Economía y Competitividad","keywords":"Venus; Rossby wave; Kelvin wave; Physics; Orbiter; Atmospheric wave; Geophysics; Geology; Atmospheric sciences; Astrophysics; Astrobiology; Astronomy; Meteorology; Gravity wave; Gravitational wave","score_opus":0.07242112389709386,"score_gpt":0.31495641404870656,"score_spread":0.24253529015161268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3030491266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991216,0.000036853125,0.0001074065,0.000023378585,0.00000178228,0.0000010760293,0.000054644366,0.00000571461,0.0006474551],"genre_scores_gemma":[0.9998068,0.0000062767253,0.000026823827,0.0000031490792,0.0000012127891,4.1402055e-7,0.000060332553,8.0896405e-7,0.00009432906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999573,0.000003837101,0.0000016730246,0.0000072688126,0.000009209212,0.000020758724],"domain_scores_gemma":[0.99983513,0.000019199906,0.000043989065,0.000015126406,0.00002090219,0.00006566157],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056577348,0.000058279424,0.00012938742,0.00029451537,0.00042818213,0.00029770262,0.00014874924,0.00013335234,0.0005928088],"category_scores_gemma":[0.00024565577,0.00005593382,0.00007105801,0.00027444446,0.0002524511,0.00013105804,0.0003308049,0.00030083512,0.0001019518],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006333074,0.000104877356,0.7786121,0.00006358519,0.00005576564,0.00095807813,0.0012017696,0.0044425996,0.1879284,0.0016162035,0.0007550165,0.02362829],"study_design_scores_gemma":[0.0000038208796,0.000045093388,0.9934082,0.0000050495387,0.0000051244124,0.00011712018,0.0001828541,0.0019307828,0.0032019212,0.00017314573,0.00092204113,0.0000049633272],"about_ca_topic_score_codex":0.015430955,"about_ca_topic_score_gemma":0.01858939,"teacher_disagreement_score":0.015430955,"about_ca_system_score_codex":0.0004688359,"about_ca_system_score_gemma":0.0001997219,"threshold_uncertainty_score":0.030682266},"labels":[],"label_agreement":null},{"id":"W3032602544","doi":"10.1029/2020gl087942","title":"Ice‐Wedge Evidence of Holocene Winter Warming in the Canadian Arctic","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; University of Alberta; General Electric (Canada); University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Resources Canada; Geological Society of America","keywords":"Arctic; Holocene; Climatology; Paleoclimatology; Arctic dipole anomaly; Arctic sea ice decline; Arctic ice pack; Insolation; Climate change; Precipitation; Environmental science; Arctic ecology; Arctic geoengineering; Oceanography; Sea ice; Physical geography; Geology; Geography; Drift ice; Meteorology","score_opus":0.09421409225709562,"score_gpt":0.32529571186745254,"score_spread":0.23108161961035692,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3032602544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9882996,0.00073305314,0.00026788574,0.00022821451,0.000018223753,0.0000055765713,0.0042204433,0.00004307139,0.0061838944],"genre_scores_gemma":[0.9980209,0.00019776136,0.00016693216,0.000043580923,0.000004787649,0.000002451713,0.001163051,0.000007636835,0.0003929631],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997986,0.000007725235,0.000009064539,0.00004971031,0.00007454037,0.000060480335],"domain_scores_gemma":[0.9990239,0.00003504743,0.00011271342,0.000034466382,0.0006752404,0.00011861867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027567675,0.00020873756,0.00021380762,0.0011283621,0.0015431291,0.0008430427,0.00043411582,0.00020836352,0.0017822098],"category_scores_gemma":[0.00069801684,0.00014053973,0.00014290556,0.0019550463,0.0005563871,0.00024830963,0.00054730556,0.00022575339,0.0001459665],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026465498,0.000024273822,0.95661026,0.00010916331,0.00013184825,0.00018517031,0.0013417653,0.00074215693,0.016151028,0.00048506618,0.0029261955,0.021028446],"study_design_scores_gemma":[0.0000021756157,0.0000036538365,0.99672157,0.000014008697,0.000013443309,0.000022071334,0.0003713012,0.00022301421,0.00039458423,0.00003007541,0.0021985455,0.0000056667764],"about_ca_topic_score_codex":0.9647595,"about_ca_topic_score_gemma":0.9872103,"teacher_disagreement_score":0.03524047,"about_ca_system_score_codex":0.005129274,"about_ca_system_score_gemma":0.007051735,"threshold_uncertainty_score":0.07089597},"labels":[],"label_agreement":null},{"id":"W3033015451","doi":"10.1029/2020gl088898","title":"Platelet Ice Under Arctic Pack Ice in Winter","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Natural Environment Research Council; Norges Forskningsråd; Sight Research UK","keywords":"Arctic ice pack; Sea ice; Antarctic sea ice; Ice formation; Drift ice; Geology; Arctic; Oceanography; Cryosphere; Fast ice; Sea ice thickness; Ice shelf; Climatology; Atmospheric sciences","score_opus":0.040331744387522066,"score_gpt":0.28011898768207877,"score_spread":0.2397872432945567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033015451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989748,0.000073212956,0.00007964596,0.0000055891664,0.000004224069,0.0000025142904,0.0002283189,0.000003421382,0.0006282504],"genre_scores_gemma":[0.9990602,0.00007681983,0.00014654802,0.000009956649,0.0000066019634,0.0000038560543,0.00044355437,0.0000027951778,0.00024970583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999485,0.0000049376063,0.0000023873833,0.0000152855,0.00001361342,0.000015305688],"domain_scores_gemma":[0.9998834,0.000011165716,0.000039097555,0.000005527546,0.00003626867,0.000024501835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011843588,0.0002152037,0.00022649569,0.00048998644,0.0005318439,0.00049874786,0.00012045663,0.0001624372,0.0004205245],"category_scores_gemma":[0.00015073347,0.000098004966,0.00010956102,0.00042282417,0.00024781248,0.0002126516,0.000325659,0.00019243326,0.00011900531],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042872576,0.000041776773,0.93887925,0.00005716528,0.00007399558,0.00044683428,0.001789947,0.00059443765,0.046619065,0.000088119144,0.00034087375,0.010639807],"study_design_scores_gemma":[9.806313e-7,0.000028815446,0.99787223,0.0000046335595,0.000008514906,0.000052455187,0.00046931018,0.00023397688,0.0008343944,0.000012791436,0.0004802112,0.0000017528052],"about_ca_topic_score_codex":0.024406208,"about_ca_topic_score_gemma":0.043012556,"teacher_disagreement_score":0.024406208,"about_ca_system_score_codex":0.00026487422,"about_ca_system_score_gemma":0.0002236135,"threshold_uncertainty_score":0.048528254},"labels":[],"label_agreement":null},{"id":"W3033352911","doi":"10.1029/2020gl088833","title":"Robust Longitudinally Variable Responses of the ITCZ to a Myriad of Climate Forcings","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Climatology; Hadley cell; Forcing (mathematics); Intertropical Convergence Zone; Orbital forcing; Climate model; Climate change; Atmospheric sciences; Environmental science; Geology; Extratropical cyclone; Zonal and meridional; Physics; Precipitation; Meteorology; General Circulation Model; Oceanography","score_opus":0.07204797382177475,"score_gpt":0.29508245808819966,"score_spread":0.22303448426642491,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033352911","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806565,0.000030370958,0.0005582834,0.00010369572,0.000010848274,0.000004838576,0.00056522014,0.000053982672,0.0006071864],"genre_scores_gemma":[0.9994011,0.00001326613,0.0001400578,0.000016512848,0.0000023371153,0.00000361256,0.00032464846,0.000009302457,0.000089146124],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998416,0.000049822986,0.000010419152,0.000042140622,0.00001565437,0.000040505107],"domain_scores_gemma":[0.99935323,0.00019603457,0.00011654852,0.00009905572,0.000117337564,0.00011783299],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008171121,0.0003300747,0.00031804197,0.00025443305,0.0003466037,0.00074349984,0.00039196573,0.00051122863,0.0015684755],"category_scores_gemma":[0.0024822708,0.00033351048,0.00061172,0.00025989462,0.00030328063,0.00046659357,0.00050274434,0.0005030643,0.00017177188],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060943904,0.00022233342,0.32927442,0.000071566115,0.00061853416,0.00026425545,0.0001052574,0.61599386,0.04488118,0.0014416119,0.001315165,0.005202409],"study_design_scores_gemma":[0.00012484645,0.0002822784,0.26872802,0.000019947105,0.00016143333,0.00006742043,0.00015366939,0.72156096,0.006987727,0.0009858228,0.0008537306,0.00007418334],"about_ca_topic_score_codex":0.02042812,"about_ca_topic_score_gemma":0.0138043845,"teacher_disagreement_score":0.02042812,"about_ca_system_score_codex":0.00051776157,"about_ca_system_score_gemma":0.00049293425,"threshold_uncertainty_score":0.04061842},"labels":[],"label_agreement":null},{"id":"W3033495728","doi":"10.1029/2020gl089394","title":"Real‐Time Earthquake Early Warning With Deep Learning: Application to the 2016 M 6.0 Central Apennines, Italy Earthquake","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Earthquake location; Warning system; Earthquake warning system; Earthquake simulation; Waveform; Seismic microzonation; Magnitude (astronomy); Earthquake prediction; Foreshock","score_opus":0.014931668050064567,"score_gpt":0.2654579676931105,"score_spread":0.2505262996430459,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033495728","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97937953,0.00032211037,0.014973883,0.0005560793,0.000101964506,0.00003225553,0.0004930094,0.0023413536,0.0017999737],"genre_scores_gemma":[0.9911917,0.00004717024,0.007393675,0.00004771853,0.000014498472,0.000009330969,0.0003496362,0.000021324611,0.000924864],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998908,0.000026542513,0.000008136897,0.000026100426,0.000024342244,0.000024073337],"domain_scores_gemma":[0.99964774,0.0001465443,0.00004157291,0.000035126486,0.00008586467,0.00004308202],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004382661,0.0006699031,0.0003072851,0.0005035455,0.00018511168,0.00029543866,0.00042808845,0.00057218655,0.0008443728],"category_scores_gemma":[0.0013049995,0.00018359751,0.00021461806,0.0004118212,0.00021060034,0.00022242928,0.0004916424,0.0004839757,0.00022294525],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010571219,0.000788772,0.041915163,0.00018571106,0.00016188834,0.0014392846,0.00022862825,0.67660654,0.023994673,0.00043037612,0.008422872,0.244769],"study_design_scores_gemma":[0.000033343527,0.000094859766,0.011079601,0.0000058239084,0.000013680971,0.00003686124,0.00003376441,0.9839824,0.0040417747,0.00021703368,0.00044855595,0.000012335741],"about_ca_topic_score_codex":0.017164849,"about_ca_topic_score_gemma":0.019484008,"teacher_disagreement_score":0.017164849,"about_ca_system_score_codex":0.00052234705,"about_ca_system_score_gemma":0.00045211366,"threshold_uncertainty_score":0.034129918},"labels":[],"label_agreement":null},{"id":"W3033705472","doi":"10.1029/2020gl087888","title":"Remote Sensing Retrieval of Isoprene Concentrations in the Southern Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Australian Research Council; National Oceanic and Atmospheric Administration; Universidade de Santiago de Compostela; Fundación Bancaria Caixa d'Estalvis i Pensions de Barcelona; Swiss Polar Institute; Centre National de la Recherche Scientifique; Université Laval; Centre of Excellence in Plant Energy Biology, Australian Research Council; Ministerio de Economía y Competitividad; Ferring; Australian Government; National Aeronautics and Space Administration","keywords":"Isoprene; Phytoplankton; Environmental science; Aerosol; Satellite; Chlorophyll a; Atmospheric sciences; Sea surface temperature; Ocean color; Oceanography; Seasonality; Climatology; Meteorology; Geology; Nutrient; Geography; Chemistry; Ecology; Biology","score_opus":0.043940124404008365,"score_gpt":0.27663575600098766,"score_spread":0.2326956315969793,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033705472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9934503,0.00010642735,0.0024469772,0.000025950985,0.000008606647,0.000009878114,0.0012827872,0.00035318287,0.002315861],"genre_scores_gemma":[0.9918698,0.000047670048,0.0054247337,0.000013639905,0.0000064354567,0.0000064338305,0.0020405387,0.000022676217,0.00056803843],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.000009527821,0.0000046820464,0.000022621356,0.000018039256,0.000009029349],"domain_scores_gemma":[0.9999074,0.000012831822,0.000019929468,0.000014341399,0.00003660553,0.000008958901],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002954305,0.00026952437,0.00020506632,0.00057040865,0.0000953657,0.00033175366,0.0001858894,0.00013715374,0.0005683697],"category_scores_gemma":[0.00029169137,0.000116954696,0.00020969566,0.00041440103,0.00009217417,0.00023700601,0.00023620336,0.00012645118,0.00021150426],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010146115,0.00032290185,0.37296283,0.0002889994,0.00025746532,0.00033305655,0.00022871832,0.1164867,0.30314636,0.0016184025,0.0036114336,0.19972849],"study_design_scores_gemma":[0.00014321457,0.0001649075,0.53504664,0.000030320876,0.00006704142,0.00009434433,0.00009921621,0.39844772,0.0585635,0.00056605245,0.0067349407,0.000042087617],"about_ca_topic_score_codex":0.008290798,"about_ca_topic_score_gemma":0.0074910955,"teacher_disagreement_score":0.008290798,"about_ca_system_score_codex":0.00028063366,"about_ca_system_score_gemma":0.0002463829,"threshold_uncertainty_score":0.016485095},"labels":[],"label_agreement":null},{"id":"W3033909961","doi":"10.1029/2020gl088599","title":"Role of Atmospheric Variability in Driving the “Warm‐Arctic, Cold‐Continent” Pattern Over the North America Sector and Sea Ice Variability Over the Chukchi‐Bering Sea","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation of Sri Lanka; National Key Research and Development Program of China; Climate Program Office; Directorate for Geosciences; National Natural Science Foundation of China; National Stroke Foundation","keywords":"Arctic ice pack; Climatology; Arctic; Geology; Oceanography; Sea ice","score_opus":0.010682668159635662,"score_gpt":0.22681034262816224,"score_spread":0.21612767446852657,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033909961","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990101,0.000065558044,0.000057409085,0.000053706914,0.0000068456197,0.0000018639112,0.00016449131,0.0000072000494,0.0006328426],"genre_scores_gemma":[0.9997031,0.00003558155,0.000035754078,0.000008526901,0.0000035948087,0.0000010142351,0.00010273569,0.0000017954676,0.000107824424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999454,0.000009849848,0.0000046415703,0.000014496811,0.000007045534,0.00001857891],"domain_scores_gemma":[0.9995384,0.00010057765,0.000120945166,0.000026533515,0.00011219798,0.00010135644],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017899094,0.0001706987,0.00011357719,0.00039454515,0.0004996139,0.0006779998,0.00013907612,0.00016417763,0.001083164],"category_scores_gemma":[0.0004674831,0.00012000308,0.0002166878,0.00048276735,0.00033166385,0.00020969327,0.00023408962,0.00025318822,0.00011801628],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008934165,0.000025360101,0.9907733,0.000018208364,0.00007084708,0.0001409125,0.00016071838,0.0009255922,0.004571092,0.00014521093,0.00023605359,0.002843346],"study_design_scores_gemma":[0.0000018577662,0.0000079900265,0.9985018,0.0000035817748,0.000015686754,0.000014777916,0.00014165876,0.0009642833,0.00017046879,0.00001688132,0.00015849559,0.00000249761],"about_ca_topic_score_codex":0.15425737,"about_ca_topic_score_gemma":0.21812297,"teacher_disagreement_score":0.15425737,"about_ca_system_score_codex":0.0006746134,"about_ca_system_score_gemma":0.00082287984,"threshold_uncertainty_score":0.30671895},"labels":[],"label_agreement":null},{"id":"W3033920046","doi":"10.1029/2020gl088580","title":"Crustal Deformation in Southern California Constrained by Radial Anisotropy From Ambient Noise Adjoint Tomography","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Toronto; Centre of Excellence for Core to Crust Fluid Systems, Australian Research Council; Natural Sciences and Engineering Research Council of Canada; National Stroke Foundation; Southern California Earthquake Center; National Science Foundation","keywords":"Geology; Subduction; Seismology; Anisotropy; Shear zone; Lithosphere; Crust; Amphibole; Shear (geology); Seismic anisotropy; Seismic tomography; Slab; Geophysics; Petrology; Tectonics; Paleontology; Mantle (geology); Quartz; Physics","score_opus":0.01957468448231128,"score_gpt":0.23575155684438046,"score_spread":0.21617687236206917,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3033920046","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9885262,0.00006286265,0.008635051,0.00006300988,0.000004601299,0.0000070644437,0.00028019655,0.00016965147,0.0022512851],"genre_scores_gemma":[0.9985967,0.000029298853,0.0009672114,0.000003987033,0.0000019580455,0.0000028098011,0.00014932979,0.000008723327,0.00024008969],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987984,0.000012603906,0.0000053929043,0.0000579374,0.000026395965,0.00001790027],"domain_scores_gemma":[0.99986947,0.00001637243,0.00003253495,0.000022460154,0.000042050986,0.00001702944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023592515,0.00048722787,0.00030199235,0.00045911962,0.00033733176,0.0010290042,0.000549821,0.00035015892,0.0005822387],"category_scores_gemma":[0.0006386522,0.00042141275,0.00030717236,0.00048372918,0.0005956276,0.000497631,0.0004918857,0.00029078173,0.00009016219],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001444792,0.000057032303,0.10638368,0.000023144377,0.00006718484,0.00015695264,0.00010850194,0.8696439,0.011592204,0.0017579873,0.00046098398,0.009603843],"study_design_scores_gemma":[0.00002693876,0.000016975195,0.055658586,0.0000051478924,0.00002335018,0.00002323436,0.000030616928,0.942613,0.00064446003,0.00062689115,0.00030965914,0.000021097743],"about_ca_topic_score_codex":0.19415252,"about_ca_topic_score_gemma":0.14560543,"teacher_disagreement_score":0.19415252,"about_ca_system_score_codex":0.0009782368,"about_ca_system_score_gemma":0.0011264451,"threshold_uncertainty_score":0.38604486},"labels":[],"label_agreement":null},{"id":"W3035115926","doi":"10.1029/2020gl088437","title":"Spatial Variability and Linkage Between Extreme Convections and Extreme Precipitation Revealed by 22‐Year Space‐Borne Precipitation Radar Data","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Precipitation Measurement and Analysis","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canmore Museum and Geoscience Centre; University of Saskatchewan","funders":"Global Water Futures","keywords":"Precipitation; Climatology; Environmental science; Radar; Spatial distribution; Extreme value theory; Latitude; Atmospheric sciences; Meteorology; Geology; Geography; Remote sensing","score_opus":0.11565606933282821,"score_gpt":0.29979291582732315,"score_spread":0.18413684649449494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035115926","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99943036,0.000034558958,0.00012722753,0.00001007617,0.0000013990077,9.695394e-7,0.00021698778,0.0000052262617,0.00017306294],"genre_scores_gemma":[0.99940515,0.00001861783,0.00011782585,0.000003398837,0.0000045728066,0.0000012957865,0.00040760616,0.0000010535051,0.000040451727],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990225,0.000017863973,0.000009861819,0.000032943,0.000016480824,0.000020621319],"domain_scores_gemma":[0.9995919,0.00007852638,0.00017204652,0.000044401728,0.00005406584,0.000059066082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028071395,0.00008480328,0.00013488391,0.00063997624,0.00011274963,0.00031633073,0.00009722771,0.00009220783,0.0003978414],"category_scores_gemma":[0.00052244414,0.00007170139,0.000105278275,0.00062117254,0.00011929219,0.00023332152,0.0003399928,0.00012002839,0.00008590058],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006430965,0.000023575045,0.98635095,0.000010293656,0.00006233004,0.00006670699,0.00011492524,0.00086329627,0.0054534357,0.00009375488,0.00018401624,0.0067124446],"study_design_scores_gemma":[0.0000022127508,0.000012528748,0.9984377,0.0000015369095,0.0000074721875,0.000034125333,0.00006061567,0.0010586143,0.00019762803,0.000023431418,0.00016195409,0.000002142719],"about_ca_topic_score_codex":0.002270596,"about_ca_topic_score_gemma":0.0033505461,"teacher_disagreement_score":0.002270596,"about_ca_system_score_codex":0.00008992117,"about_ca_system_score_gemma":0.00010929671,"threshold_uncertainty_score":0.004514754},"labels":[],"label_agreement":null},{"id":"W3035464903","doi":"10.1029/2020gl087439","title":"The Influence of Magma Mixing on the Composition of Andesite Magmas and Silicic Eruption Style","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Silicic; Geology; Volcanism; Andesite; Mafic; Volcano; Magma; Petrology; Geochemistry; Explosive eruption; Caldera; Fractional crystallization (geology); Basaltic andesite; Magma chamber; Igneous differentiation; Volcanic rock; Seismology; Tectonics","score_opus":0.030097676560691997,"score_gpt":0.2580010818365615,"score_spread":0.2279034052758695,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035464903","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929655,0.00006020683,0.000097509255,0.000008266657,0.000001450927,0.0000020333819,0.000050660423,0.000007082704,0.00047628567],"genre_scores_gemma":[0.99986076,0.0000089319265,0.00003898036,0.0000023482912,7.3603485e-7,6.387126e-7,0.000021461201,0.0000022443824,0.000063927575],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998981,0.000030061916,0.000008385826,0.000029664401,0.000017888755,0.000015964908],"domain_scores_gemma":[0.9994485,0.0002976111,0.00008230117,0.000031141568,0.000043876546,0.000096597425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022516845,0.00017074493,0.00014994688,0.00028784032,0.00018214625,0.0005694328,0.00012317792,0.00014626286,0.001525132],"category_scores_gemma":[0.0011668747,0.00014215765,0.00012903997,0.00012339433,0.000259692,0.0002217872,0.0002000127,0.00016023505,0.00016138799],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010433475,0.00010255944,0.108075924,0.00003813848,0.00008078076,0.0001472565,0.00009869189,0.0031326346,0.87977195,0.00025688554,0.000088431916,0.0071634096],"study_design_scores_gemma":[0.000038523078,0.00040641148,0.7508343,0.00000520967,0.000063509644,0.00020966989,0.00012426806,0.022977157,0.22445819,0.00022479304,0.0006403752,0.000017566363],"about_ca_topic_score_codex":0.0016343816,"about_ca_topic_score_gemma":0.0013527889,"teacher_disagreement_score":0.0016343816,"about_ca_system_score_codex":0.00022492083,"about_ca_system_score_gemma":0.00010499495,"threshold_uncertainty_score":0.005102098},"labels":[],"label_agreement":null},{"id":"W3035645161","doi":"10.1029/2020gl088000","title":"Spatial Dependence of Floods Shaped by Spatiotemporal Variations in Meteorological and Land‐Surface Processes","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Flood Risk Assessment and Management","field":"Environmental Science","cited_by":106,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"U.S. Army Corps of Engineers; Bureau of Reclamation; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung","keywords":"Flood myth; Environmental science; Spatial dependence; Spatial variability; Spatial ecology; Climatology; Physical geography; Geography; Geology; Statistics","score_opus":0.032627630757094905,"score_gpt":0.3025476464923304,"score_spread":0.2699200157352355,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035645161","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923587,0.000016406024,0.0002964969,0.000028815582,8.135597e-7,0.0000017246235,0.000118439784,0.0000065066874,0.00029490527],"genre_scores_gemma":[0.9998387,0.000006523877,0.000034616558,0.0000023957011,8.508832e-7,0.00000108071,0.000070585316,0.0000015876623,0.000043667842],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983823,0.000065368804,0.000010948107,0.000035888697,0.000019215408,0.00003033462],"domain_scores_gemma":[0.9967631,0.0017294189,0.00078348257,0.00021154908,0.00029808885,0.00021423756],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005962111,0.000083177605,0.00013417965,0.00080274994,0.00015848095,0.0004112304,0.0001685105,0.00019342257,0.0013970761],"category_scores_gemma":[0.0032947657,0.000118172684,0.00022855744,0.0005710704,0.0003764173,0.00034671705,0.00042185932,0.000244442,0.00018651845],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025409507,0.000041922707,0.9787648,0.00001489035,0.000100659076,0.00016689487,0.00036338752,0.011423564,0.0036742985,0.00056765764,0.0003517945,0.0042761527],"study_design_scores_gemma":[0.0000025064567,0.000020218646,0.985595,0.0000029681119,0.000010437048,0.000054463773,0.0002075553,0.013442589,0.00016701476,0.0004018131,0.00008893711,0.0000063671055],"about_ca_topic_score_codex":0.005680755,"about_ca_topic_score_gemma":0.00523372,"teacher_disagreement_score":0.005680755,"about_ca_system_score_codex":0.0002070965,"about_ca_system_score_gemma":0.000122061756,"threshold_uncertainty_score":0.011295378},"labels":[],"label_agreement":null},{"id":"W3035824700","doi":"10.1029/2020gl088796","title":"Elevation Changes of the Fennoscandian Ice Sheet Interior During the Last Deglaciation","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Environment Research Council; Norges Forskningsråd; Sight Research UK","keywords":"Deglaciation; Geology; Ice sheet; Younger Dryas; Antarctic ice sheet; Moraine; Ice-sheet model; Physical geography; Cryosphere; Thinning; Glaciology; Oceanography; Ice stream; Geomorphology; Glacier; Sea ice; Holocene; Paleontology; Geography; Volcanism","score_opus":0.03433611170368666,"score_gpt":0.2714492387065191,"score_spread":0.23711312700283244,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035824700","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99783486,0.00011658539,0.00007692952,0.0000208585,0.0000072981597,0.0000016470506,0.0006447185,0.000007698607,0.0012894586],"genre_scores_gemma":[0.9991856,0.00005005491,0.00009647565,0.0000069995112,0.0000030738033,0.0000017761431,0.0005227218,0.0000023102086,0.00013101968],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992514,0.0000075314456,0.000005083246,0.00002542382,0.000014093464,0.0000227002],"domain_scores_gemma":[0.99978095,0.000025258802,0.00004804234,0.000015929416,0.00009543004,0.000034355406],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000351838,0.00020866393,0.00019359268,0.00073158916,0.00044100758,0.0007898426,0.00021408097,0.00021879647,0.0010222528],"category_scores_gemma":[0.00053034496,0.000105067666,0.00013647015,0.0007251695,0.00039432725,0.00024016404,0.00035577323,0.0002152901,0.00014996275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017567803,0.00001869547,0.9783199,0.00003947487,0.00005494029,0.0001631915,0.0007426484,0.0033835,0.0043639923,0.0001744293,0.0004829158,0.012080498],"study_design_scores_gemma":[0.000001679374,0.000007629676,0.9984212,0.00000781997,0.0000058292694,0.000023499866,0.00015660655,0.00051068986,0.00015366467,0.000016077134,0.00069277495,0.0000024480744],"about_ca_topic_score_codex":0.10523235,"about_ca_topic_score_gemma":0.15932159,"teacher_disagreement_score":0.10523235,"about_ca_system_score_codex":0.0011391302,"about_ca_system_score_gemma":0.00055214093,"threshold_uncertainty_score":0.20923966},"labels":[],"label_agreement":null},{"id":"W3035898414","doi":"10.1029/2020gl087207","title":"Rapid Cooling and Increased Storminess Triggered by Freshwater in the North Atlantic","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Seventh Framework Programme; National Centre for Earth Observation; Natural Environment Research Council; Sight Research UK","keywords":"Anomaly (physics); North Atlantic oscillation; Climatology; Storm; Winter storm; Environmental science; Oceanography; Geology","score_opus":0.044756564116427845,"score_gpt":0.27584797797981897,"score_spread":0.23109141386339113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3035898414","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948704,0.000040312658,0.000055503166,0.000036521324,0.000002866642,9.991875e-7,0.000067095076,0.000006170607,0.0003034232],"genre_scores_gemma":[0.99982065,0.000030278248,0.00003017813,0.000010324355,0.000005564114,9.55339e-7,0.000052699597,0.0000011780033,0.000048208145],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999646,0.000005526688,0.000002362972,0.000010535045,0.000006527997,0.0000103759485],"domain_scores_gemma":[0.999884,0.00001429941,0.0000536487,0.000010664857,0.000016049147,0.000021268665],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013714172,0.00009276213,0.00014029753,0.00021894237,0.0001824153,0.00023916,0.00011597574,0.00016906156,0.00070334243],"category_scores_gemma":[0.0002373545,0.00007962561,0.00013941708,0.00019888423,0.00025530515,0.00018518265,0.0002284862,0.00013009942,0.000059480582],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034218177,0.00005207257,0.864302,0.00006413911,0.000116512565,0.0004802139,0.00040782557,0.0022600836,0.12158732,0.00026346912,0.0005423735,0.009581919],"study_design_scores_gemma":[0.000002516774,0.000012268813,0.99893516,0.0000013998263,0.000004701644,0.00002375171,0.000035102254,0.00037367363,0.00040853577,0.000042881296,0.00015837712,0.0000016870914],"about_ca_topic_score_codex":0.007962929,"about_ca_topic_score_gemma":0.01313323,"teacher_disagreement_score":0.007962929,"about_ca_system_score_codex":0.000367833,"about_ca_system_score_gemma":0.00015188435,"threshold_uncertainty_score":0.015833199},"labels":[],"label_agreement":null},{"id":"W3036008126","doi":"10.1029/2020gl088362","title":"The Contribution of Methane Photoproduction to the Oceanic Methane Paradox","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":70,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Université du Québec à Rimouski","funders":"Natural Sciences and Engineering Research Council of Canada; ArcticNet","keywords":"Methane; Colored dissolved organic matter; Methanogenesis; Environmental science; Environmental chemistry; Anaerobic oxidation of methane; Sink (geography); Greenhouse gas; Dissolved organic carbon; Atmosphere (unit); Oceanography; Seawater; Carbon cycle; Atmospheric sciences; Chemistry; Geology; Meteorology; Physics; Ecology; Ecosystem; Phytoplankton","score_opus":0.028978776942727852,"score_gpt":0.2931919427009038,"score_spread":0.264213165758176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036008126","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998061,0.00023673501,0.0010244171,0.00012471621,0.000007129741,0.000001966304,0.000048045662,0.000022477227,0.0004735784],"genre_scores_gemma":[0.99979657,0.000041130683,0.00009340971,0.0000070092833,0.0000016246366,0.0000011120917,0.00002429811,0.000002191908,0.00003249072],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993455,0.00001887571,0.0000034380203,0.000016142078,0.000014651891,0.000012245979],"domain_scores_gemma":[0.99978954,0.000095280906,0.000038246515,0.000024288069,0.000025562003,0.000027094731],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026610415,0.00021895049,0.00019551524,0.00020059329,0.00020676483,0.00035306124,0.00022190143,0.00028497292,0.0004316465],"category_scores_gemma":[0.0004707829,0.00012024295,0.00024370012,0.00019282557,0.00031224467,0.00028654054,0.00044555296,0.000253139,0.00005514399],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011692813,0.000099654,0.33561942,0.00024632877,0.00022733213,0.00093323446,0.00014904128,0.05864627,0.5805432,0.0036663385,0.00067148835,0.018028392],"study_design_scores_gemma":[0.00007781325,0.00037960825,0.56783926,0.000015941405,0.00013709422,0.0005494246,0.000689151,0.2593201,0.1577689,0.009960994,0.0031782887,0.000083387866],"about_ca_topic_score_codex":0.0016291885,"about_ca_topic_score_gemma":0.0012262348,"teacher_disagreement_score":0.0016291885,"about_ca_system_score_codex":0.0004464511,"about_ca_system_score_gemma":0.00025281048,"threshold_uncertainty_score":0.0032393932},"labels":[],"label_agreement":null},{"id":"W3036414272","doi":"10.1029/2020gl088647","title":"Temperature Proxies as a Solution to Biased Sampling of Lake Methane Emissions","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Vetenskapsrådet; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; McGill University; National Science Foundation","keywords":"Environmental science; Subarctic climate; Methane; Flux (metallurgy); Atmospheric sciences; Sampling (signal processing); Forcing (mathematics); Trace gas; Climatology; Geology; Oceanography; Chemistry; Physics","score_opus":0.04260920104330879,"score_gpt":0.31124400205309416,"score_spread":0.2686348010097854,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036414272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.93479383,0.0009141408,0.060747884,0.0002924147,0.00005130533,0.000038325314,0.0015777473,0.0004510899,0.0011332766],"genre_scores_gemma":[0.9856942,0.00011877149,0.012770826,0.00007121714,0.000017847855,0.000035309007,0.0009862183,0.00006378106,0.00024181484],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99772435,0.0012565779,0.00016867816,0.0004501575,0.0002751428,0.00012519158],"domain_scores_gemma":[0.9944523,0.002645513,0.0011265572,0.0009409973,0.00075464445,0.00007995229],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0042055775,0.00067726657,0.0006745915,0.0008690676,0.00047639417,0.0011179306,0.0006817108,0.0006212584,0.0005512554],"category_scores_gemma":[0.011294697,0.00046530153,0.0004651541,0.0013409704,0.0003971156,0.0007987474,0.00070778566,0.0005125832,0.00019387474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019116125,0.00004992783,0.9096598,0.00011608102,0.0006757351,0.000109949324,0.00022880315,0.042430144,0.017077962,0.0009914748,0.00096842507,0.027500432],"study_design_scores_gemma":[0.00003404473,0.000078269324,0.7034999,0.00007091526,0.00024102625,0.00019735313,0.00018317364,0.2609378,0.027575472,0.002268225,0.004830942,0.00008283121],"about_ca_topic_score_codex":0.011147488,"about_ca_topic_score_gemma":0.018027358,"teacher_disagreement_score":0.011147488,"about_ca_system_score_codex":0.00088915817,"about_ca_system_score_gemma":0.0006670328,"threshold_uncertainty_score":0.022241533},"labels":[],"label_agreement":null},{"id":"W3036735605","doi":"10.1029/2020gl088168","title":"Injection‐Induced Earthquakes on Complex Fault Zones of the Raton Basin Illuminated by Machine‐Learning Phase Picker and Dense Nodal Array","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Seismology; Induced seismicity; Geology; Hypocenter; Tectonics; Structural basin; Daytime; Basement; Focal mechanism; Fault (geology); Magnitude (astronomy); Geomorphology","score_opus":0.05314672318528116,"score_gpt":0.29197023750309015,"score_spread":0.238823514317809,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3036735605","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995505,0.000011711046,0.00011608474,0.000006691622,0.0000012677419,0.0000017591086,0.000103809296,0.000010589789,0.0001975148],"genre_scores_gemma":[0.99962986,0.000007273677,0.00012712313,0.000001346775,0.0000013545757,9.932247e-7,0.00014905863,0.0000013531129,0.00008157028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993753,0.000010227071,0.000004245474,0.000018316088,0.00001150805,0.000018026261],"domain_scores_gemma":[0.999811,0.000027262755,0.000049997238,0.00001890344,0.0000549261,0.000038008806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011943287,0.00020692243,0.00013552647,0.0011095433,0.00017172981,0.00024542774,0.00017760132,0.00013666757,0.00074679573],"category_scores_gemma":[0.00030854245,0.0001063322,0.000106799846,0.0007795403,0.00021255593,0.00015059885,0.00024529183,0.000084557796,0.000086198605],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003573312,0.00009201949,0.9352406,0.000038004113,0.00006549986,0.00080746,0.0005272792,0.009839935,0.02320883,0.00027258962,0.00064792164,0.02890258],"study_design_scores_gemma":[0.0000035214168,0.000024453037,0.9834222,0.000004378572,0.000013786944,0.000061169885,0.00016039684,0.015398625,0.0006623498,0.000039099254,0.00020484472,0.000005329837],"about_ca_topic_score_codex":0.021169467,"about_ca_topic_score_gemma":0.044702053,"teacher_disagreement_score":0.021169467,"about_ca_system_score_codex":0.0002586236,"about_ca_system_score_gemma":0.0002141706,"threshold_uncertainty_score":0.042092443},"labels":[],"label_agreement":null},{"id":"W3037392099","doi":"10.1029/2019gl086828","title":"Effects of Semistochastic Westerly Wind Bursts on ENSO Predictability","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Climatology; El Niño Southern Oscillation; Thermocline; Predictability; Wind stress; Environmental science; Multivariate ENSO index; Amplitude; Meteorology; Lead time; Wind speed; Climate model; Geology; La Niña; Climate change; Geography; Physics; Oceanography","score_opus":0.03064365610515864,"score_gpt":0.28981435994960025,"score_spread":0.25917070384444163,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037392099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998283,0.000046346784,0.00092333107,0.00009361182,0.000015882162,0.0000047851586,0.00013892457,0.000040461564,0.00045379045],"genre_scores_gemma":[0.99968266,0.000018705503,0.00013956877,0.000012782591,0.000003562413,0.0000025015202,0.000089485504,0.000005784424,0.000044876313],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996674,0.0001361422,0.000037860606,0.000062599116,0.000031932883,0.000064052256],"domain_scores_gemma":[0.9982967,0.0008382934,0.00026035972,0.00026570715,0.00015025401,0.00018864706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012374222,0.00044512062,0.00028472662,0.00019892084,0.00037631992,0.00073533104,0.00037617108,0.000496718,0.00093868823],"category_scores_gemma":[0.0039581847,0.00022318492,0.000430251,0.00020376514,0.0004887953,0.00077749864,0.0007459334,0.000586679,0.00009456175],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010749494,0.00022646156,0.34655344,0.00007117778,0.0002984231,0.00035478387,0.00015924977,0.61852616,0.016028058,0.002140437,0.0010059475,0.013560849],"study_design_scores_gemma":[0.00012363456,0.00015944558,0.14312768,0.000022351795,0.00006421972,0.0000352344,0.00013886018,0.85119116,0.0037338908,0.00071608427,0.00065362337,0.000033770648],"about_ca_topic_score_codex":0.01453743,"about_ca_topic_score_gemma":0.015142556,"teacher_disagreement_score":0.01453743,"about_ca_system_score_codex":0.00043947497,"about_ca_system_score_gemma":0.00065485545,"threshold_uncertainty_score":0.02890563},"labels":[],"label_agreement":null},{"id":"W3037544338","doi":"10.1029/2019gl086791","title":"A Post‐2013 Dropoff in Total Ozone at a Third of Global Ozonesonde Stations: Electrochemical Concentration Cell Instrument Artifacts?","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Goddard Space Flight Center; National Oceanic and Atmospheric Administration; National Aeronautics and Space Administration","keywords":"Satellite; Environmental science; Meteorology; Ozone; Ozone depletion; Climatology; Atmospheric sciences; Remote sensing; Geography; Geology; Physics","score_opus":0.01941961409826528,"score_gpt":0.2607158269238828,"score_spread":0.2412962128256175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3037544338","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97,0.00085348554,0.0056711994,0.005023509,0.0006837678,0.000070449496,0.006962947,0.000359053,0.010375567],"genre_scores_gemma":[0.9906781,0.0002486769,0.0018323314,0.0015184948,0.00011348725,0.00003193764,0.0032451048,0.00007060319,0.0022612878],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9985777,0.00014809749,0.00015675125,0.00027210813,0.00067062007,0.00017468647],"domain_scores_gemma":[0.99492717,0.0006281586,0.0012050713,0.00066987646,0.0024559866,0.00011387025],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001982549,0.00020256758,0.0002504765,0.00060644123,0.00051693653,0.00086045783,0.0006639694,0.00064984686,0.0019666483],"category_scores_gemma":[0.005349882,0.00013833585,0.00029907838,0.001391521,0.00044050027,0.0004430664,0.0006370428,0.00074607483,0.00067696103],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052078103,0.00010352588,0.90345484,0.0002020901,0.00018446018,0.0010218283,0.00080365996,0.00057086535,0.01842798,0.00094852457,0.016525272,0.057236105],"study_design_scores_gemma":[0.000010043266,0.00012650946,0.9521557,0.000055088618,0.000082592116,0.00044922225,0.00076282246,0.00090593373,0.02470435,0.000325861,0.020397434,0.0000244099],"about_ca_topic_score_codex":0.029690498,"about_ca_topic_score_gemma":0.03937913,"teacher_disagreement_score":0.029690498,"about_ca_system_score_codex":0.0011112796,"about_ca_system_score_gemma":0.00070192147,"threshold_uncertainty_score":0.05903536},"labels":[],"label_agreement":null},{"id":"W3038712726","doi":"10.1029/2020gl089436","title":"Application of Deep Learning to Estimate Atmospheric Gravity Wave Parameters in Reanalysis Data Sets","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Core Research for Evolutional Science and Technology; Precursory Research for Embryonic Science and Technology; Japan Science and Technology Agency","keywords":"Momentum (technical analysis); Gravity wave; Wavenumber; Gravitational wave; Atmosphere (unit); Flux (metallurgy); Geology; Zonal and meridional; Atmospheric sciences; Climatology; Meteorology; Geophysics; Physics; Optics; Astrophysics","score_opus":0.031162915325204234,"score_gpt":0.3274400727648475,"score_spread":0.2962771574396433,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3038712726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9627484,0.00034171014,0.033860166,0.0002347816,0.000071202725,0.000039925566,0.0008963781,0.001075391,0.00073206413],"genre_scores_gemma":[0.9836045,0.00005801124,0.014862843,0.00003058144,0.000012893839,0.00002067153,0.0011496868,0.000013785187,0.00024702],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99959594,0.00012054621,0.00004475451,0.00010694255,0.00006720914,0.00006457495],"domain_scores_gemma":[0.99856734,0.0006609804,0.00015097727,0.0001938997,0.00036180092,0.00006502536],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019075404,0.0009748678,0.00045160067,0.0012885886,0.00036593454,0.0006350257,0.00062323955,0.00073719845,0.0004169953],"category_scores_gemma":[0.004452514,0.00040140413,0.0005839727,0.00093478046,0.00032322563,0.00067271787,0.0006712305,0.0008006178,0.00014260852],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022140841,0.0002897387,0.049207084,0.000053286654,0.00026004997,0.000105914674,0.0001083598,0.81591254,0.0053249956,0.0004394622,0.0014253356,0.12665184],"study_design_scores_gemma":[0.0000059608565,0.000010079145,0.0047831493,0.0000027056005,0.0000068214454,0.0000027782808,0.000012479563,0.9941578,0.0007844255,0.0001379847,0.00008986152,0.0000059379004],"about_ca_topic_score_codex":0.046080966,"about_ca_topic_score_gemma":0.030727837,"teacher_disagreement_score":0.046080966,"about_ca_system_score_codex":0.00083594053,"about_ca_system_score_gemma":0.0011010189,"threshold_uncertainty_score":0.09162551},"labels":[],"label_agreement":null},{"id":"W3040748029","doi":"10.1029/2020gl087254","title":"Stress Chatter via Fluid Flow and Fault Slip in a Hydraulic Fracturing‐Induced Earthquake Sequence in the Montney Formation, British Columbia","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":62,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McGill University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Deutsche Forschungsgemeinschaft","keywords":"Geology; Aftershock; Seismology; Hydraulic fracturing; Seismometer; Slip (aerodynamics); Fluid pressure; Differential stress; Shear stress; Fluid dynamics; Geotechnical engineering; Deformation (meteorology)","score_opus":0.044634847299519886,"score_gpt":0.26609342637842703,"score_spread":0.22145857907890715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040748029","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99955684,0.00000915465,0.000034829096,0.000021042675,2.9921992e-7,0.0000017192484,0.00009217942,0.0000045895003,0.0002792586],"genre_scores_gemma":[0.99970204,0.000009778302,0.000033758784,0.0000034494528,3.3416046e-7,0.0000012385175,0.00006972404,8.7294796e-7,0.00017872383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999031,0.000010461552,0.0000062376625,0.000022217595,0.00002375641,0.00003430486],"domain_scores_gemma":[0.9996934,0.000045246932,0.00008633853,0.000015609448,0.00009103326,0.00006844937],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010414191,0.00016527476,0.00014964507,0.000942884,0.0005600311,0.00071859243,0.00039346263,0.00027767225,0.0012301848],"category_scores_gemma":[0.0006555626,0.0001819017,0.00011288088,0.0009923478,0.0005153239,0.00019579826,0.0004657966,0.00024289267,0.00011900474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007912083,0.0000487308,0.98465794,0.000010513297,0.000036961377,0.00027834496,0.00065838953,0.0018618399,0.005825854,0.000083859006,0.00024065831,0.0062179016],"study_design_scores_gemma":[0.000001439053,0.000005233574,0.9979151,0.0000021038138,0.0000037134253,0.000012951034,0.0003459602,0.0015066233,0.00012103201,0.000013199531,0.000069591246,0.000003037598],"about_ca_topic_score_codex":0.8658914,"about_ca_topic_score_gemma":0.9428075,"teacher_disagreement_score":0.1341086,"about_ca_system_score_codex":0.004253775,"about_ca_system_score_gemma":0.0021583603,"threshold_uncertainty_score":0.26979673},"labels":[],"label_agreement":null},{"id":"W3040857342","doi":"10.1029/2020gl087999","title":"Nanoconfined Water Effect on CO<sub>2</sub> Utilization and Geological Storage","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"","keywords":"Caprock; Oil shale; Petroleum engineering; Materials science; Intermolecular force; Permeability (electromagnetism); Environmental science; Chemical engineering; Soil science; Chemical physics; Geology; Chemistry; Molecule; Organic chemistry","score_opus":0.04949772829883774,"score_gpt":0.31865293967825814,"score_spread":0.2691552113794204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3040857342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99037445,0.00030785275,0.0072789704,0.00010292863,0.000023807388,0.0000095210435,0.00007870579,0.0000600674,0.0017636095],"genre_scores_gemma":[0.99846303,0.00012255821,0.0010048262,0.000014456503,0.0000013691417,0.000005942552,0.000021122736,0.000004962149,0.00036155892],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999342,0.000007745191,0.0000031052566,0.000016753178,0.000021439762,0.000016746037],"domain_scores_gemma":[0.99989593,0.000047167498,0.000021225153,0.000008545073,0.000020989437,0.000006179758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013372964,0.00021323473,0.000155864,0.00009908581,0.000115639246,0.00016152655,0.00019922681,0.00017139986,0.0012003902],"category_scores_gemma":[0.00027946846,0.00008007174,0.00010641131,0.0000941933,0.00031358833,0.00040212032,0.00033362687,0.00022986191,0.00008512055],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013997134,0.00003343743,0.0015378123,0.00014155591,0.000012290776,0.00012281233,0.00005670913,0.0076986915,0.9810766,0.0032949452,0.0002321093,0.005653084],"study_design_scores_gemma":[0.0000092640885,0.00008238672,0.0023875989,0.000004457783,0.000011631035,0.00003756987,0.000080050806,0.13863248,0.857078,0.0006530258,0.0010096342,0.000013786952],"about_ca_topic_score_codex":0.00189008,"about_ca_topic_score_gemma":0.0028310136,"teacher_disagreement_score":0.00189008,"about_ca_system_score_codex":0.0002447774,"about_ca_system_score_gemma":0.00027665755,"threshold_uncertainty_score":0.004015684},"labels":[],"label_agreement":null},{"id":"W3041827850","doi":"10.1029/2020gl088011","title":"Black Carbon Aerosols in the Lower Free Troposphere are Heavily Coated in Summer but Largely Uncoated in Winter at Jungfraujoch in the Swiss Alps","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Métis National Council","funders":"H2020 European Research Council; European Research Council; FP7 Ideas: European Research Council; Ferring","keywords":"Troposphere; Atmospheric sciences; Environmental science; Aerosol; Carbon black; Soot; Atmosphere (unit); Seasonality; Climatology; Radiative forcing; Meteorology; Geology; Combustion; Geography; Chemistry","score_opus":0.04099249484207111,"score_gpt":0.2711536243692505,"score_spread":0.23016112952717938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3041827850","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994148,0.000025060799,0.00003887049,0.000010749321,0.0000018643337,0.0000022060958,0.00018423713,0.000012340987,0.00030977803],"genre_scores_gemma":[0.99956447,0.000013013888,0.00006955401,0.00000539837,0.0000038305852,0.0000035236003,0.00020109619,0.0000029410896,0.0001362421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999049,0.000008784325,0.0000025966438,0.000028485216,0.000023024448,0.00003221549],"domain_scores_gemma":[0.9998919,0.000017357079,0.000025999318,0.0000064864666,0.00002295386,0.0000352192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016148128,0.00037590542,0.00022521483,0.00089720427,0.0007858715,0.0005823636,0.00022654061,0.0003939316,0.0012975192],"category_scores_gemma":[0.00012305289,0.00016152562,0.00019784097,0.0003640318,0.00033566487,0.00031003417,0.00022605126,0.00021900666,0.00021486932],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006923706,0.00021275497,0.8147317,0.00008367324,0.0001885336,0.0005842863,0.0016909731,0.0022309227,0.16701865,0.00016533416,0.0008312694,0.011569477],"study_design_scores_gemma":[0.000006516873,0.000027991551,0.9975526,0.0000023510106,0.0000075609237,0.00002268659,0.000122030964,0.0006820711,0.0013550879,0.00001077223,0.00020572518,0.0000046283617],"about_ca_topic_score_codex":0.087487735,"about_ca_topic_score_gemma":0.11478956,"teacher_disagreement_score":0.087487735,"about_ca_system_score_codex":0.0005481813,"about_ca_system_score_gemma":0.0003447664,"threshold_uncertainty_score":0.17395699},"labels":[],"label_agreement":null},{"id":"W3042171967","doi":"10.1029/2020gl088550","title":"Eddy Kinetic Energy in the Arctic Ocean From a Global Simulation With a 1‐km Arctic","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft; European Commission","keywords":"Halocline; Arctic; Eddy; Geology; Climatology; Mesoscale meteorology; Oceanography; Ocean current; Kinetic energy; Boundary current; Thermohaline circulation; Oceanic basin; Range (aeronautics); Canada Basin; Environmental science; Structural basin; Meteorology; Geomorphology; Geography; Physics; Turbulence; Salinity","score_opus":0.02535921892333559,"score_gpt":0.25946073071814835,"score_spread":0.23410151179481276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042171967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976084,0.00003697503,0.0006173641,0.00007351553,0.000015537324,0.0000066867074,0.00039523316,0.00004817626,0.0011980567],"genre_scores_gemma":[0.997757,0.00004703501,0.001251847,0.000024498044,0.000006654526,0.000012779351,0.0006326331,0.000017658915,0.00024993345],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992776,0.000023417762,0.000004394121,0.000015492165,0.000010301354,0.00001866516],"domain_scores_gemma":[0.9997681,0.0000961207,0.00002763507,0.000022618759,0.000040580228,0.000045018736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037676483,0.0005121898,0.00043086114,0.00037229914,0.00052460586,0.0007514986,0.00045314897,0.00084557536,0.0007778239],"category_scores_gemma":[0.000721864,0.00033560838,0.0007628483,0.00052069937,0.00042934556,0.00038487097,0.0004395135,0.00060747843,0.000112159956],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014056715,0.00012366219,0.018112665,0.000022256147,0.0000740799,0.00015794506,0.00004002929,0.97720796,0.0016147349,0.00043451856,0.00041480147,0.0016568269],"study_design_scores_gemma":[0.000073535666,0.00007796718,0.013834975,0.000007887024,0.00003563217,0.000019257472,0.00007449109,0.9846132,0.0006782103,0.00019872891,0.00037080707,0.000015329268],"about_ca_topic_score_codex":0.066849135,"about_ca_topic_score_gemma":0.04261786,"teacher_disagreement_score":0.066849135,"about_ca_system_score_codex":0.00091764174,"about_ca_system_score_gemma":0.0008856429,"threshold_uncertainty_score":0.13292009},"labels":[],"label_agreement":null},{"id":"W3042455009","doi":"10.1029/2020gl089077","title":"Observation of High‐Energy Electrons Precipitated by NWC Transmitter From PROBA‐V Low‐Earth Orbit Satellite","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Electron; Physics; Atomic physics; Population; Satellite; Pitch angle; Flux (metallurgy); Magnetosphere; Magnetic field; Geophysics; Materials science; Astronomy","score_opus":0.015228067527906826,"score_gpt":0.2409775914271485,"score_spread":0.2257495238992417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042455009","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99876106,0.000011572405,0.00007585415,0.000010130982,0.0000014098733,0.0000029758996,0.00007074943,0.000006361222,0.0010599096],"genre_scores_gemma":[0.9990062,0.000008254574,0.00025604374,0.000013527814,0.0000022926583,0.0000042130177,0.0002024229,0.0000040697,0.00050304993],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999286,0.000006690866,0.0000018392741,0.000015172117,0.000029038501,0.000018664745],"domain_scores_gemma":[0.99977237,0.00003704682,0.000042000534,0.000019730436,0.00006867383,0.000060214075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012538473,0.00012653139,0.00012729113,0.00051299966,0.0005575319,0.00024356796,0.0002292541,0.00021513968,0.00092829374],"category_scores_gemma":[0.00025517205,0.00013647744,0.00011942273,0.00025589296,0.0002189077,0.00013639379,0.0004465537,0.0002728873,0.0001614671],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039667098,0.00009263465,0.6768732,0.000044195815,0.000072198854,0.0012051277,0.001495617,0.00055041123,0.3106355,0.00026507338,0.00060430873,0.0077650854],"study_design_scores_gemma":[0.0000120806935,0.00008815708,0.9899743,0.0000056233725,0.000013365887,0.00017647052,0.00028444701,0.0010409264,0.0075924043,0.000027035288,0.000779254,0.0000059136464],"about_ca_topic_score_codex":0.011485692,"about_ca_topic_score_gemma":0.029312303,"teacher_disagreement_score":0.011485692,"about_ca_system_score_codex":0.00041660015,"about_ca_system_score_gemma":0.0001907928,"threshold_uncertainty_score":0.022837698},"labels":[],"label_agreement":null},{"id":"W3042654695","doi":"10.1029/2020gl088890","title":"Contrasting Recent Trends in Southern Hemisphere Westerlies Across Different Ocean Basins","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Science Foundation","keywords":"Westerlies; Southern Hemisphere; Climatology; Global wind patterns; Northern Hemisphere; Climate model; Geology; Middle latitudes; Antarctic oscillation; Oceanic basin; Climate change; Oceanography; Structural basin","score_opus":0.06883995998191274,"score_gpt":0.32728624925420774,"score_spread":0.258446289272295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042654695","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982109,0.00021385706,0.000088963316,0.00008036943,0.0000064328324,0.000001114073,0.00048191776,0.00000776594,0.0009087447],"genre_scores_gemma":[0.9988079,0.00019386246,0.00008419174,0.000014918533,0.000012455762,0.0000017416091,0.00068176555,0.0000025489715,0.0002004903],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999378,0.0000086805885,0.0000060963202,0.000019765304,0.0000132804325,0.0000145006825],"domain_scores_gemma":[0.99965525,0.00004999274,0.00012843931,0.000020200278,0.000106429165,0.00003969972],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00041229255,0.00011495299,0.00014815768,0.0006176661,0.00015904545,0.00051308447,0.000105553394,0.00014593826,0.001201073],"category_scores_gemma":[0.00060281355,0.000064943764,0.0001654067,0.00082711986,0.00016336684,0.00033919813,0.00020688039,0.00016364951,0.00014569522],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000090259644,0.000014996021,0.9850595,0.000045239125,0.00012150189,0.000052995674,0.0003621224,0.0009995126,0.0032212366,0.0003510333,0.0003924406,0.0092890905],"study_design_scores_gemma":[0.0000016607386,0.000008803431,0.9986929,0.000004319476,0.000010748535,0.000009831115,0.00009169948,0.0002857647,0.00012987564,0.000050182953,0.0007125335,0.0000017535945],"about_ca_topic_score_codex":0.014010093,"about_ca_topic_score_gemma":0.026220635,"teacher_disagreement_score":0.014010093,"about_ca_system_score_codex":0.00030533262,"about_ca_system_score_gemma":0.00021284026,"threshold_uncertainty_score":0.027857125},"labels":[],"label_agreement":null},{"id":"W3042697424","doi":"10.1029/2020gl088288","title":"Global Dam‐Driven Changes to Riverine N:P:Si Ratios Delivered to the Coastal Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":93,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Excellence Research Chairs, Government of Canada","keywords":"Biogeochemical cycle; Environmental science; Nutrient; Ecosystem; Nutrient cycle; Hydrology (agriculture); Discharge; Biogeochemistry; Oceanography; Hydroelectricity; Aquatic ecosystem; Phosphorus; Cycling; Ecology; Geology; Drainage basin; Chemistry; Geography; Biology","score_opus":0.030578726057880427,"score_gpt":0.2878988695153937,"score_spread":0.25732014345751325,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042697424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979279,0.000024177274,0.00077030854,0.00004628551,0.000003853778,0.00000261264,0.00047824485,0.000036419176,0.00071035046],"genre_scores_gemma":[0.9994537,0.000021647891,0.00018840175,0.000011562025,0.0000010054725,0.0000040079913,0.0001699314,0.000005014769,0.00014472345],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993265,0.000017330378,0.000004790977,0.000024582085,0.000010641439,0.000010093567],"domain_scores_gemma":[0.9998305,0.000035901565,0.00005312763,0.000029134788,0.00003104948,0.000020181444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029444267,0.00020808676,0.00014315978,0.00023265288,0.00010104568,0.00031866663,0.00021524167,0.00024591704,0.0009877608],"category_scores_gemma":[0.0004420855,0.00018173475,0.0003039849,0.000352135,0.00028987162,0.00038811826,0.000415767,0.00019286953,0.000120439516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067100476,0.00015048138,0.6572943,0.00010935503,0.0004537354,0.00021239396,0.0001944475,0.13466042,0.1850164,0.0022081384,0.0013610238,0.01766827],"study_design_scores_gemma":[0.000030380004,0.00017745911,0.8934105,0.000007842515,0.00007536029,0.0000784382,0.00017631217,0.09139478,0.011839738,0.0010786651,0.0016960247,0.00003460514],"about_ca_topic_score_codex":0.0053363447,"about_ca_topic_score_gemma":0.0052051884,"teacher_disagreement_score":0.0053363447,"about_ca_system_score_codex":0.0005243641,"about_ca_system_score_gemma":0.00021266539,"threshold_uncertainty_score":0.01061058},"labels":[],"label_agreement":null},{"id":"W3042816621","doi":"10.1029/2020gl088561","title":"Nearshore Zone Dynamics Determine Pathway of Organic Carbon From Eroding Permafrost Coasts","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"European Research Council; Horizon 2020 Framework Programme","keywords":"Permafrost; Total organic carbon; Arctic; Oceanography; Environmental science; Submarine pipeline; Sediment; Thermokarst; Geology; Radiocarbon dating; Settling; Hydrology (agriculture); Environmental chemistry; Geomorphology; Environmental engineering; Paleontology; Geotechnical engineering","score_opus":0.06565499353220627,"score_gpt":0.2754805222027674,"score_spread":0.20982552867056115,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042816621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990509,0.0000533519,0.000026058739,0.000011792566,6.5268824e-7,0.0000013371655,0.00021109238,0.0000030014526,0.000641909],"genre_scores_gemma":[0.99899787,0.000069442816,0.000056958856,0.0000095269625,7.7019405e-7,0.0000023279704,0.0003547731,0.0000032025137,0.0005052162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999505,0.0000016274566,0.0000032162882,0.00001829686,0.00000871347,0.000017624368],"domain_scores_gemma":[0.9998312,0.000014139323,0.00004719945,0.0000075219955,0.0000625309,0.00003737713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000061461586,0.00018740568,0.00016356012,0.000777456,0.000572671,0.00056066614,0.0002196608,0.00024390398,0.0020751453],"category_scores_gemma":[0.00020905124,0.00019586903,0.00012483714,0.0006545266,0.00031097763,0.000328698,0.00040963327,0.00016229555,0.0002538493],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011371093,0.000015928912,0.95698446,0.000035203135,0.000035877743,0.00025296243,0.00060486066,0.0004908023,0.034691412,0.00012398548,0.00015673398,0.0064940616],"study_design_scores_gemma":[9.104308e-7,0.0000068559175,0.9992028,0.0000020661748,0.0000029688401,0.000016333857,0.0002196916,0.00010564114,0.00026171506,0.000009551307,0.00016998046,0.0000015372938],"about_ca_topic_score_codex":0.18279159,"about_ca_topic_score_gemma":0.3537901,"teacher_disagreement_score":0.18279159,"about_ca_system_score_codex":0.001110652,"about_ca_system_score_gemma":0.00078823697,"threshold_uncertainty_score":0.36345524},"labels":[],"label_agreement":null},{"id":"W3042860767","doi":"10.1029/2020gl088322","title":"Subsurface Weathering Revealed in Hillslope‐Integrated Porosity Distributions","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Concordia University","funders":"University of Wyoming; National Aeronautics and Space Administration; Wyoming Space Grant Consortium; National Science Foundation","keywords":"Weathering; Geology; Porosity; Borehole; Seismic refraction; Mineralogy; Soil science; Geomorphology; Geophysics; Geotechnical engineering","score_opus":0.04453547153173556,"score_gpt":0.27786346471558143,"score_spread":0.23332799318384587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042860767","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99850583,0.000018436354,0.0009642863,0.0000026707764,3.6874556e-7,0.0000014748824,0.0001627497,0.000026431435,0.0003177599],"genre_scores_gemma":[0.99968004,0.000008904086,0.00018767483,0.0000010809497,4.013793e-7,8.677892e-7,0.00007900866,0.000003238941,0.000038888742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999429,0.000004973913,0.0000034558723,0.000023741572,0.000010679815,0.000014218876],"domain_scores_gemma":[0.99961495,0.00009045143,0.0001210052,0.000041607123,0.00010056425,0.000031442938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000157718,0.00015993434,0.00014841558,0.0011225898,0.00010121648,0.00042937134,0.00015774912,0.00012644021,0.0008660569],"category_scores_gemma":[0.00047754357,0.0001316083,0.000102370796,0.0007190031,0.0002875707,0.00044718033,0.00032356847,0.00012555103,0.00013164057],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019557455,0.000050377177,0.83971554,0.00004625926,0.000082428305,0.00020008572,0.00038713258,0.015585494,0.116046585,0.00042186247,0.00017286376,0.027095761],"study_design_scores_gemma":[0.0000031870322,0.000022987524,0.9790355,0.0000036009258,0.000011683144,0.00008747664,0.0001767874,0.016657114,0.0036739272,0.0001933859,0.00012364534,0.000010803679],"about_ca_topic_score_codex":0.0051872074,"about_ca_topic_score_gemma":0.0056104804,"teacher_disagreement_score":0.0051872074,"about_ca_system_score_codex":0.00019860452,"about_ca_system_score_gemma":0.000098612814,"threshold_uncertainty_score":0.010314047},"labels":[],"label_agreement":null},{"id":"W3042962682","doi":"10.1029/2020gl088808","title":"Temperature Control on Silicate Weathering Intensity and Evolution of the Neogene East Asian Summer Monsoon","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Weathering; Geology; Monsoon; East Asian Monsoon; Precipitation; Silicate; Cenozoic; Paleoclimatology; Climatology; Global cooling; Plateau (mathematics); Neogene; Monsoon of South Asia; Earth science; Oceanography; Paleontology; Climate change; Structural basin","score_opus":0.033235707802458755,"score_gpt":0.2568052575295933,"score_spread":0.22356954972713455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3042962682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995153,0.00004950644,0.000050444512,0.000009931144,9.1395225e-7,4.0146554e-7,0.00005071599,0.0000032169125,0.00031961367],"genre_scores_gemma":[0.9998048,0.000025955162,0.000021884574,0.000004812867,0.0000014317537,5.2916266e-7,0.00004474282,0.000001739589,0.000094156116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996305,0.000007816599,0.000003011206,0.000011772192,0.000005156484,0.000009250557],"domain_scores_gemma":[0.999764,0.000048960475,0.00007894661,0.000019433906,0.000044854296,0.000043823482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018560037,0.00010241337,0.00010579151,0.00036803642,0.00011206118,0.00033623082,0.000106355525,0.00011202325,0.00093978766],"category_scores_gemma":[0.00034772465,0.00009887702,0.00009742019,0.00024515085,0.0002530608,0.00020867029,0.00017840206,0.00011399567,0.00012677535],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004269183,0.000028897799,0.7965118,0.000034909663,0.00009282443,0.00014437949,0.0005896638,0.0014857308,0.19082244,0.0003570909,0.0001730805,0.009332128],"study_design_scores_gemma":[0.0000015213814,0.000012117826,0.9986137,0.0000011721216,0.0000046221103,0.000013813517,0.00006798298,0.00040467785,0.00075722265,0.000027336606,0.00009408073,0.0000017764406],"about_ca_topic_score_codex":0.0069184243,"about_ca_topic_score_gemma":0.009550622,"teacher_disagreement_score":0.0069184243,"about_ca_system_score_codex":0.00023477158,"about_ca_system_score_gemma":0.00013218333,"threshold_uncertainty_score":0.013756335},"labels":[],"label_agreement":null},{"id":"W3043046141","doi":"10.1029/2020gl088060","title":"Comparing Methods of Uncertainty Estimation in Optimal Fingerprinting","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Drought Analysis","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Smoothing; Sensitivity (control systems); Context (archaeology); Statistics; Noise (video); Measure (data warehouse); Scaling; Computer science; Mathematics; Algorithm; Data mining; Artificial intelligence","score_opus":0.06607578083358513,"score_gpt":0.3797550499287248,"score_spread":0.31367926909513966,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043046141","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.08265192,0.0017108455,0.91355646,0.00016566015,0.00006976173,0.00007308666,0.0001401923,0.0006371441,0.0009949416],"genre_scores_gemma":[0.5064623,0.00050151756,0.49198022,0.000050180246,0.000060226466,0.00009312618,0.0002659243,0.00021692923,0.00036961818],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9901509,0.0056793974,0.00062562263,0.0010772207,0.00203229,0.00043457455],"domain_scores_gemma":[0.9219891,0.06431919,0.0027415552,0.0060644536,0.0044435523,0.000442129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.021370055,0.0009854509,0.0017567639,0.004282946,0.0006267916,0.0023962327,0.001600728,0.0015453302,0.0011813022],"category_scores_gemma":[0.08147451,0.0007958315,0.0012167153,0.0024122095,0.0011817714,0.0030953474,0.0028196804,0.001291318,0.00026523965],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017772402,0.00017918731,0.010905145,0.0005555386,0.0006843369,0.00009329895,0.00032932847,0.46250272,0.005370559,0.014461939,0.0007704486,0.5023703],"study_design_scores_gemma":[0.000047790094,0.00014882418,0.004654696,0.00007475489,0.00008043245,0.00011215523,0.000095425035,0.97325706,0.007828081,0.01300995,0.0006007924,0.00008996005],"about_ca_topic_score_codex":0.0038551365,"about_ca_topic_score_gemma":0.0023046064,"teacher_disagreement_score":0.021370055,"about_ca_system_score_codex":0.00085689465,"about_ca_system_score_gemma":0.00093713065,"threshold_uncertainty_score":0.11301702},"labels":[],"label_agreement":null},{"id":"W3043557959","doi":"10.1029/2020gl088508","title":"Subseasonal Forecast Skill for Weekly Mean Atmospheric Variability Over the Northern Hemisphere in Winter and Its Relationship to Midlatitude Teleconnections","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Teleconnection; Middle latitudes; Climatology; Predictability; Geopotential height; Northern Hemisphere; Anomaly (physics); Forcing (mathematics); North Atlantic oscillation; Environmental science; Forecast skill; Southern Hemisphere; Atmospheric sciences; Arctic oscillation; Geology; El Niño Southern Oscillation; Meteorology; Geography; Precipitation; Mathematics; Physics","score_opus":0.048876733995867234,"score_gpt":0.29942444544118907,"score_spread":0.25054771144532184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043557959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983109,0.000030273468,0.00031975782,0.000069461814,0.0000060724756,0.0000015406807,0.00051259116,0.000029652048,0.00071972486],"genre_scores_gemma":[0.9992285,0.000013691979,0.000061350205,0.0000056376853,0.000004223684,9.872441e-7,0.000558339,0.000003549176,0.00012382626],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998721,0.000020607564,0.00001158697,0.00003734168,0.00003296127,0.000025408388],"domain_scores_gemma":[0.9987626,0.00056620775,0.00021293075,0.000095360396,0.00023222828,0.00013084662],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056152826,0.00017354893,0.00014969817,0.00035066967,0.00013124851,0.0005164391,0.0001551564,0.00018371151,0.0015925992],"category_scores_gemma":[0.0025895208,0.000094155585,0.0002294426,0.000260693,0.00012369569,0.0004462756,0.00025884833,0.00021632758,0.00023780619],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013357885,0.000032210315,0.9705761,0.00000811743,0.00008182458,0.000060164737,0.00009071852,0.01910952,0.0018518785,0.00016779888,0.00060375396,0.007284334],"study_design_scores_gemma":[0.0000071002573,0.000029856417,0.9621719,0.0000040564455,0.000009591607,0.000024997007,0.00008714417,0.03671738,0.00044897656,0.00016230247,0.00032944404,0.000007223269],"about_ca_topic_score_codex":0.045830384,"about_ca_topic_score_gemma":0.04991903,"teacher_disagreement_score":0.045830384,"about_ca_system_score_codex":0.00038769486,"about_ca_system_score_gemma":0.00033019678,"threshold_uncertainty_score":0.09112722},"labels":[],"label_agreement":null},{"id":"W3043719222","doi":"10.1029/2020gl088442","title":"Pyrocumulonimbus Stratospheric Plume Injections Measured by the ACE‐FTS","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Canadian Space Agency","keywords":"Stratosphere; Atmospheric sciences; Occultation; Environmental science; Plume; Troposphere; Aerosol; Atmospheric chemistry; Atmosphere (unit); Mixing ratio; Altitude (triangle); Meteorology; Geology; Ozone; Physics; Astronomy","score_opus":0.04774752131622143,"score_gpt":0.2816289563533644,"score_spread":0.23388143503714295,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043719222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99204904,0.00007132252,0.0007955832,0.000034323937,0.00001138065,0.000009606399,0.0022763754,0.00019435213,0.004557996],"genre_scores_gemma":[0.99687994,0.000034406326,0.0010576777,0.0000170877,0.000007482233,0.00000650364,0.0015537109,0.000011519093,0.00043168783],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998919,0.000005610058,0.0000023345067,0.000018190496,0.0000610947,0.000020724136],"domain_scores_gemma":[0.9998621,0.000017751696,0.000023661223,0.00001165421,0.000054269705,0.00003053929],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001496916,0.00022863265,0.00012970885,0.0006243019,0.0002335185,0.00040935574,0.00020376047,0.00021475992,0.00089091115],"category_scores_gemma":[0.00025172933,0.000084012536,0.0001166593,0.0004329514,0.000086401626,0.00024070231,0.00020192063,0.0002468666,0.00018370504],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021973054,0.00049379695,0.4551027,0.0000864318,0.00022073618,0.00040165268,0.00047983127,0.012122893,0.46124452,0.0012207731,0.0050855526,0.061343707],"study_design_scores_gemma":[0.00004498922,0.000132761,0.85608715,0.000011402471,0.000039484257,0.0001224696,0.00014493587,0.04718977,0.092155546,0.00018737555,0.0038529465,0.000031251217],"about_ca_topic_score_codex":0.013428172,"about_ca_topic_score_gemma":0.012709041,"teacher_disagreement_score":0.013428172,"about_ca_system_score_codex":0.0004375488,"about_ca_system_score_gemma":0.00019219817,"threshold_uncertainty_score":0.02670002},"labels":[],"label_agreement":null},{"id":"W3043940899","doi":"10.1029/2020gl088947","title":"Coseismic Uplift of the 1999 <i>M</i><sub>w</sub>7.6 Chi‐Chi Earthquake and Implication to Topographic Change in Frontal Mountain Belts","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Future Earth","funders":"Ministry of Science and Technology, Taiwan","keywords":"Geology; Landslide; Seismology; Interferometric synthetic aperture radar; Slip (aerodynamics); Earthquake rupture; Geomorphology; Synthetic aperture radar; Remote sensing; Fault (geology)","score_opus":0.035003523956662036,"score_gpt":0.26815399482679003,"score_spread":0.233150470870128,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3043940899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993235,0.000025224355,0.000083239145,0.000023177585,0.0000018051298,0.0000015475711,0.000081753955,0.0000055750747,0.0004542764],"genre_scores_gemma":[0.99976295,0.000020143336,0.00004272816,0.0000045306583,0.0000034728787,8.9545955e-7,0.00010844531,9.966031e-7,0.000055913384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994993,0.0000069844996,0.0000043128607,0.00001257559,0.000008576134,0.000017687704],"domain_scores_gemma":[0.99972826,0.0000329011,0.00011880128,0.000016059768,0.000056670084,0.000047273104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013922724,0.0001354673,0.00013218282,0.0009102195,0.00017107592,0.00035048605,0.000121941,0.00018186061,0.0008575741],"category_scores_gemma":[0.00042290764,0.000082616905,0.00013053982,0.0006252216,0.00022191223,0.00021745545,0.00025650117,0.00012929935,0.00011813754],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049621776,0.000018609393,0.98115563,0.000018576375,0.000033354034,0.0002776328,0.00015714567,0.0012603292,0.009615976,0.00010183544,0.0002141592,0.007097103],"study_design_scores_gemma":[0.0000010813504,0.000008851607,0.9986935,0.0000013307093,0.000006247937,0.000032470787,0.00007655605,0.00087425706,0.0001750416,0.000017382381,0.00011187256,0.0000013445181],"about_ca_topic_score_codex":0.016196337,"about_ca_topic_score_gemma":0.020466456,"teacher_disagreement_score":0.016196337,"about_ca_system_score_codex":0.0002637571,"about_ca_system_score_gemma":0.00016507316,"threshold_uncertainty_score":0.03220415},"labels":[],"label_agreement":null},{"id":"W3045541137","doi":"10.1029/2020gl089429","title":"Summer PM<sub>2.5</sub> Pollution Extremes Caused by Wildfires Over the Western United States During 2017–2018","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Oceanic and Atmospheric Administration","keywords":"Environmental science; Smoke; Aerosol; Atmospheric sciences; Air quality index; Pollution; Satellite; Air pollution; Climatology; Meteorology; Radiative transfer; Geography; Geology","score_opus":0.028057561534150254,"score_gpt":0.27073805848523014,"score_spread":0.24268049695107988,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3045541137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969229,0.000045650326,0.00014657434,0.00008928486,0.000012884471,0.000004705284,0.0021869028,0.000054935354,0.00053620397],"genre_scores_gemma":[0.99683493,0.00004830069,0.00018460977,0.000024562718,0.000012067781,0.000008420789,0.0027174195,0.0000074901764,0.00016224988],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999143,0.000011243166,0.00000609348,0.000030058649,0.000018721472,0.000019594094],"domain_scores_gemma":[0.9998653,0.000017837829,0.000042018502,0.000012534367,0.00003729893,0.000024933224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022030767,0.00040941796,0.0002499419,0.000328845,0.00033129854,0.00047677007,0.00026349898,0.00037912116,0.0008802376],"category_scores_gemma":[0.00030297457,0.0001798204,0.00037491514,0.00038052408,0.00017135851,0.00044296525,0.0003549067,0.00028871957,0.00016354577],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037033306,0.00021404964,0.94739527,0.000047314195,0.00021574613,0.00033014966,0.00017001196,0.031460073,0.0026967202,0.00016306556,0.0063047465,0.010632607],"study_design_scores_gemma":[0.000044688128,0.000056021654,0.9171842,0.00002374503,0.00009069507,0.000066056615,0.00030010418,0.07796274,0.0016680072,0.00019791855,0.0023856387,0.00002013664],"about_ca_topic_score_codex":0.12110969,"about_ca_topic_score_gemma":0.14933859,"teacher_disagreement_score":0.12110969,"about_ca_system_score_codex":0.0008828768,"about_ca_system_score_gemma":0.00050520804,"threshold_uncertainty_score":0.2408095},"labels":[],"label_agreement":null},{"id":"W3046189623","doi":"10.1029/2020gl088745","title":"Surface Wetness as an Unexpected Control on Forest Exchange of Volatile Organic Acids","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Toronto; Academy of Finland; U.S. Forest Service; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Dew; Dew point; Canopy; Environmental science; Volatility (finance); Sink (geography); Tree canopy; Partition coefficient; Atmospheric sciences; Chemistry; Environmental chemistry; Botany; Geology; Condensation; Meteorology; Physics; Biology; Chromatography","score_opus":0.02187127532230867,"score_gpt":0.2675830760469698,"score_spread":0.24571180072466112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046189623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99874145,0.00016969745,0.00050260493,0.000010560561,0.0000034273157,0.000003114669,0.00012190393,0.000016574484,0.00043075954],"genre_scores_gemma":[0.99971646,0.000021889675,0.00011171844,0.000006374835,0.0000019122847,0.0000015803474,0.000064896616,0.000003692446,0.00007149339],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999331,0.000008106075,0.0000031559866,0.000022871181,0.000015550866,0.000017332883],"domain_scores_gemma":[0.9998381,0.00006239034,0.00003662335,0.000015559237,0.000025782938,0.000021612372],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014198695,0.00013990597,0.0002220085,0.00024695863,0.00025268178,0.00053693616,0.0001265945,0.00015452066,0.00063519675],"category_scores_gemma":[0.00023805982,0.0001074938,0.000113352566,0.00020150309,0.00020448447,0.00040093088,0.00023714414,0.00023967591,0.00005795449],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004084649,0.000053661213,0.14599617,0.00006190125,0.000077807825,0.00018498585,0.00016581234,0.00089185254,0.84147507,0.00018637236,0.00014589413,0.010351942],"study_design_scores_gemma":[0.0000060451307,0.00007652187,0.9694819,0.000003629122,0.00001909139,0.00009315175,0.00016821291,0.0025389777,0.026939623,0.00015460128,0.00050843396,0.000009938868],"about_ca_topic_score_codex":0.003349575,"about_ca_topic_score_gemma":0.0041562063,"teacher_disagreement_score":0.003349575,"about_ca_system_score_codex":0.0001513571,"about_ca_system_score_gemma":0.0000839143,"threshold_uncertainty_score":0.0066601634},"labels":[],"label_agreement":null},{"id":"W3046235897","doi":"10.1029/2020gl090192","title":"Electrical Conductivity of Aqueous Magnesium Sulfate at High Pressure and Low Temperature With Application to Ganymede's Subsurface Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Electrical resistivity and conductivity; Aqueous solution; Magnesium; Conductivity; Conductance; Limiting; Analytical Chemistry (journal); Sulfate; Materials science; Mineralogy; Geology; Chemistry; Condensed matter physics; Physics; Environmental chemistry; Metallurgy; Physical chemistry","score_opus":0.0116349499030121,"score_gpt":0.2334152658545616,"score_spread":0.2217803159515495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3046235897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992735,0.000022472512,0.0002773658,0.000027890357,0.0000021811754,0.0000033427677,0.000052247913,0.0000103228385,0.00033070485],"genre_scores_gemma":[0.99947125,0.00001973776,0.00040889397,0.0000030645065,6.0605663e-7,0.0000022391605,0.000026669126,0.0000013353178,0.00006621881],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99994755,0.0000093192675,0.0000037663872,0.0000130149765,0.000015560527,0.000010705186],"domain_scores_gemma":[0.99991536,0.000033847937,0.000012319139,0.000009422003,0.000020108324,0.0000089261375],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010559015,0.00015915514,0.00016113796,0.00011062162,0.00015927583,0.0002472897,0.00028421864,0.00020639531,0.00042977656],"category_scores_gemma":[0.0002846018,0.00009400381,0.00015051688,0.00018336029,0.0002825368,0.0001458865,0.00019886621,0.00021190253,0.000064319975],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025481483,0.000034389475,0.007927991,0.000082691564,0.0000093979925,0.0001905916,0.00011204975,0.0083237905,0.98003525,0.00024541182,0.00008399585,0.0026996178],"study_design_scores_gemma":[0.00005973911,0.0006654247,0.01589711,0.000009114631,0.000013883423,0.00009302565,0.00020019367,0.041384973,0.9407287,0.0001493248,0.00078030466,0.000018119852],"about_ca_topic_score_codex":0.0031845642,"about_ca_topic_score_gemma":0.0018224205,"teacher_disagreement_score":0.0031845642,"about_ca_system_score_codex":0.00034851787,"about_ca_system_score_gemma":0.00015638713,"threshold_uncertainty_score":0.00633204},"labels":[],"label_agreement":null},{"id":"W3047070162","doi":"10.1029/2020gl087911","title":"Large Wildfires in the Western United States Exacerbated by Tropospheric Drying Linked to a Multi‐Decadal Trend in the Expansion of the Hadley Circulation","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Troposphere; Environmental science; Subsidence; Climate change; Relative humidity; Global warming; Hadley cell; Cloud cover; Greenhouse gas; Atmospheric circulation; Atmospheric sciences; Geography; General Circulation Model; Geology; Meteorology; Oceanography; Structural basin; Cloud computing","score_opus":0.028030649221268782,"score_gpt":0.2902096514274482,"score_spread":0.2621790022061794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047070162","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993864,0.00004423176,0.000042302432,0.000019798917,0.000005357832,0.0000016808403,0.00030793686,0.000004868917,0.00018741691],"genre_scores_gemma":[0.99932384,0.000039636518,0.0000725113,0.000016374783,0.0000038739336,0.000002927251,0.0004590683,8.5244585e-7,0.00008085572],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999131,0.000015049163,0.000010252591,0.000025289764,0.000019103538,0.000017260238],"domain_scores_gemma":[0.99958223,0.00005771184,0.00015266711,0.00004131487,0.000105223786,0.000060867384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035096135,0.00015069006,0.00013411952,0.00044522053,0.00036365475,0.00045602,0.00012376861,0.00013396908,0.0005426159],"category_scores_gemma":[0.00056609034,0.00009074241,0.000158171,0.0006014268,0.00019058025,0.00026316254,0.00031714243,0.00026009046,0.00004707316],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009074961,0.000060727318,0.9916306,0.000014673856,0.00012666309,0.00009739058,0.00012258181,0.00090677675,0.0016033496,0.000047463473,0.0005710587,0.0047279242],"study_design_scores_gemma":[0.0000022752597,0.000012178582,0.9984463,0.000003856806,0.000015402984,0.000018685147,0.00019105563,0.00084194774,0.00022099398,0.000020004716,0.00022478367,0.0000025120064],"about_ca_topic_score_codex":0.071820065,"about_ca_topic_score_gemma":0.18424235,"teacher_disagreement_score":0.071820065,"about_ca_system_score_codex":0.0005103406,"about_ca_system_score_gemma":0.0004184852,"threshold_uncertainty_score":0.14280409},"labels":[],"label_agreement":null},{"id":"W3047498112","doi":"10.1029/2020gl089469","title":"Intensification of Near‐Surface Currents and Shear in the Eastern Arctic Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":63,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Division of Ocean Sciences; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Geology; Oceanography; Stratification (seeds); Mooring; Current (fluid); Ocean current; Canada Basin; Sea ice; Inertial wave; Climatology","score_opus":0.050076757833100664,"score_gpt":0.28589786329088906,"score_spread":0.2358211054577884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047498112","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99906844,0.000089668625,0.000032137745,0.000021407803,0.0000049761743,0.00000126292,0.00034047535,0.0000054550005,0.000436177],"genre_scores_gemma":[0.9989937,0.00009098403,0.000067958536,0.000012100919,0.0000098413175,0.0000019957308,0.00056776183,0.0000014775392,0.00025417938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999074,0.000009587877,0.000011891184,0.000028847902,0.00002130928,0.000020953617],"domain_scores_gemma":[0.9996338,0.000019846813,0.00015780363,0.000027290125,0.0001047591,0.000056549416],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026252226,0.00016535341,0.00020646637,0.0009753058,0.00030973816,0.0006789636,0.000121825935,0.00025058282,0.0007208308],"category_scores_gemma":[0.00042902317,0.00013072503,0.00019829233,0.00078829366,0.00021480846,0.00035443399,0.00038753558,0.00016905897,0.0001626069],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008856934,0.000027541026,0.9847259,0.000030893356,0.000058866357,0.000110557936,0.00037612076,0.00031594242,0.0069316295,0.00008617466,0.00028535235,0.006962437],"study_design_scores_gemma":[6.5329925e-7,0.0000071154477,0.9993742,0.0000033345905,0.0000041510966,0.000017426957,0.00006562886,0.00008741027,0.00012918709,0.0000071637023,0.0003023529,0.0000013319909],"about_ca_topic_score_codex":0.029944468,"about_ca_topic_score_gemma":0.04401044,"teacher_disagreement_score":0.029944468,"about_ca_system_score_codex":0.00037912407,"about_ca_system_score_gemma":0.00038502805,"threshold_uncertainty_score":0.05954039},"labels":[],"label_agreement":null},{"id":"W3047594138","doi":"10.1029/2020gl089099","title":"Geophysical Observations of Phobos Transits by InSight","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Institut de Physique du Globe de Paris; Centre National de la Recherche Scientifique; Centre National d’Etudes Spatiales; Branco Weiss Fellowship – Society in Science; National Aeronautics and Space Administration; Agence Nationale de la Recherche; Max-Planck-Gesellschaft; UK Space Agency","keywords":"Seismometer; Geology; Geophysics; Regolith; Magnetometer; Transit (satellite); Mars Exploration Program; Planet; Astrobiology; Solar System; Seismology; Astronomy; Physics; Magnetic field","score_opus":0.0800429003643425,"score_gpt":0.29397393285843604,"score_spread":0.21393103249409354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3047594138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9962824,0.00004430185,0.00026391915,0.000033893044,0.00000610231,0.0000064056285,0.0009421094,0.000055204884,0.0023656907],"genre_scores_gemma":[0.9985354,0.000037868977,0.00036324514,0.000009735005,0.0000057912075,0.000003485825,0.0006663631,0.000005838427,0.00037221142],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995315,0.0000036513395,0.000002030016,0.000010934445,0.000015139535,0.000015113453],"domain_scores_gemma":[0.9998914,0.000008924008,0.000030664367,0.000009389978,0.000022745635,0.000036816335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008869246,0.00017624011,0.000098549455,0.0006793399,0.00021480743,0.00022622118,0.00012512317,0.00017327578,0.001068027],"category_scores_gemma":[0.00021787011,0.00007985724,0.00008291722,0.00049377297,0.00016445902,0.00019157902,0.00044286856,0.00025418645,0.00019540622],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016530432,0.00013060188,0.83749676,0.00009837386,0.00007524746,0.0009832204,0.0027394763,0.0022404762,0.096800335,0.00073359464,0.0039935433,0.053055402],"study_design_scores_gemma":[0.000022918059,0.0001696713,0.9882355,0.00001885028,0.00001898923,0.00023281018,0.00077065453,0.002271185,0.002836068,0.00010822261,0.0053043426,0.000010723648],"about_ca_topic_score_codex":0.0068474673,"about_ca_topic_score_gemma":0.012460339,"teacher_disagreement_score":0.0068474673,"about_ca_system_score_codex":0.00020917229,"about_ca_system_score_gemma":0.00011698749,"threshold_uncertainty_score":0.013615251},"labels":[],"label_agreement":null},{"id":"W3048339781","doi":"10.1029/2020gl088950","title":"Machine Learning for Source Identification of Dust on the Chinese Loess Plateau","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University","funders":"China Scholarship Council; Ministry of Science and Technology of the People's Republic of China; National Natural Science Foundation of China","keywords":"Aeolian processes; Interglacial; Loess; Geology; Loess plateau; Provenance; Glacial period; Earth science; Physical geography; Identification (biology); Geomorphology; Geochemistry; Soil science; Geography","score_opus":0.04468574851408419,"score_gpt":0.3041663892849183,"score_spread":0.2594806407708341,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048339781","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.981267,0.00019867043,0.017352024,0.00007002639,0.000007580686,0.000010466895,0.00025304852,0.00021725679,0.00062400836],"genre_scores_gemma":[0.99696106,0.000033807017,0.0025077437,0.000005337947,0.000005133131,0.0000048601123,0.00029245188,0.0000050533176,0.00018452978],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999243,0.000013640849,0.000004929112,0.000030396195,0.0000139265485,0.000012845054],"domain_scores_gemma":[0.9998122,0.00007473948,0.0000252085,0.000016283964,0.000057850608,0.000013797385],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030711057,0.000436788,0.00022181215,0.0011372062,0.00026190875,0.00041763415,0.00036480476,0.00026804343,0.00043722687],"category_scores_gemma":[0.00057998777,0.0001392805,0.00033710914,0.0006077526,0.00014590166,0.00037503903,0.00031901285,0.00017623826,0.00012275088],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002776384,0.00015593512,0.44196543,0.00010027577,0.0001894339,0.00070350716,0.00019044249,0.36100772,0.027863903,0.000997382,0.0010537216,0.16549467],"study_design_scores_gemma":[0.0000075643175,0.000012228201,0.040613838,0.0000036999168,0.000011157565,0.000017227809,0.000037235182,0.95649356,0.002144358,0.0004823137,0.00017240425,0.0000045278575],"about_ca_topic_score_codex":0.014789963,"about_ca_topic_score_gemma":0.013144248,"teacher_disagreement_score":0.014789963,"about_ca_system_score_codex":0.00041209985,"about_ca_system_score_gemma":0.000377046,"threshold_uncertainty_score":0.02940774},"labels":[],"label_agreement":null},{"id":"W3048496510","doi":"10.1029/2020gl089627","title":"Isostatic Control of Axial Rivers and Large Drainage Basins on Passive Margins","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Passive margin; Geology; Lithosphere; Margin (machine learning); Drainage system (geomorphology); Continental margin; Drainage basin; Flow (mathematics); Routing (electronic design automation); Geomorphology; Drainage; Structural basin; Paleontology; Tectonics; Geometry; Rift","score_opus":0.028325968176656446,"score_gpt":0.26591428491520985,"score_spread":0.2375883167385534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3048496510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99684286,0.000021741867,0.0020853044,0.000013751475,0.0000010167847,8.56435e-7,0.000022801041,0.00001453956,0.0009970808],"genre_scores_gemma":[0.99981517,0.0000058263067,0.00010051602,0.0000010318977,5.7295136e-7,4.811459e-7,0.00000620896,0.0000013183719,0.00006892295],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999621,0.000009219907,0.0000028666318,0.000015164714,0.000005126403,0.0000054799475],"domain_scores_gemma":[0.9998541,0.00003327652,0.000059773847,0.000020282214,0.000016015414,0.000016595115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000629525,0.00007846437,0.00011345833,0.00025035307,0.00013321242,0.00037226576,0.00016362002,0.00007895653,0.0011129482],"category_scores_gemma":[0.0004299837,0.00009014499,0.00009245842,0.00015949422,0.00046076003,0.00027298543,0.000338182,0.00007358004,0.00004893593],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003442534,0.00010573181,0.52363765,0.00010040144,0.000088715824,0.00089523656,0.00088100974,0.15304495,0.23341697,0.046185642,0.0005510548,0.0407483],"study_design_scores_gemma":[0.000037675334,0.00011675644,0.7180717,0.000013919575,0.000053744057,0.00041782073,0.00053580425,0.24584861,0.0135509195,0.01889957,0.0024184457,0.00003495345],"about_ca_topic_score_codex":0.0016247071,"about_ca_topic_score_gemma":0.001834521,"teacher_disagreement_score":0.0016247071,"about_ca_system_score_codex":0.00020203639,"about_ca_system_score_gemma":0.00013783116,"threshold_uncertainty_score":0.0037231445},"labels":[],"label_agreement":null},{"id":"W3065208261","doi":"10.1029/2020gl089138","title":"Potential Evidence of Low‐Energy Electron Scattering and Ionospheric Precipitation by Time Domain Structures","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Electron precipitation; Electron; Physics; Plasma sheet; Ionosphere; Scattering; Whistler; Atomic physics; Magnetosphere; Plasma; Computational physics; Geophysics; Nuclear physics; Optics","score_opus":0.008655364551731135,"score_gpt":0.2592971924480465,"score_spread":0.25064182789631534,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3065208261","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99798286,0.0000771535,0.00082050374,0.00002479522,0.0000039400907,0.0000022850083,0.00005602496,0.000012356327,0.0010200958],"genre_scores_gemma":[0.9996933,0.00001599663,0.00014700493,0.0000046663704,0.0000037998477,9.152368e-7,0.0000442808,0.000001462388,0.00008864606],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.0000071086965,0.0000027305819,0.000010936137,0.000014091539,0.00001169458],"domain_scores_gemma":[0.99966156,0.000081513914,0.00012252675,0.000042184132,0.000056959583,0.00003525763],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001219217,0.00010968667,0.000077238125,0.00039665197,0.0001771065,0.00030651092,0.00014458914,0.00014916399,0.0007939451],"category_scores_gemma":[0.00044857015,0.0000667351,0.00008000015,0.00034039773,0.00021428602,0.00023576236,0.00023910664,0.00014345752,0.000061210485],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000532138,0.00006990711,0.7023617,0.000051491636,0.00010344674,0.0006344966,0.00035497255,0.0030325789,0.27259257,0.0014676066,0.00047163523,0.018327387],"study_design_scores_gemma":[0.000016076849,0.000069968504,0.96746707,0.000006334473,0.00001872139,0.0003353537,0.0002435944,0.010196428,0.020089451,0.00063210883,0.0009174493,0.000007519948],"about_ca_topic_score_codex":0.0010022927,"about_ca_topic_score_gemma":0.0011460634,"teacher_disagreement_score":0.0010022927,"about_ca_system_score_codex":0.00014714777,"about_ca_system_score_gemma":0.00006040822,"threshold_uncertainty_score":0.002655983},"labels":[],"label_agreement":null},{"id":"W3075013849","doi":"10.1029/2020gl089269","title":"Disentangling the Impact of the COVID‐19 Lockdowns on Urban NO <sub>2</sub> From Natural Variability","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Air Quality and Health Impacts","field":"Environmental Science","cited_by":294,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Office of Fossil Energy; National Aeronautics and Space Administration","keywords":"Environmental science; Coronavirus disease 2019 (COVID-19); Air quality index; Atmospheric sciences; Satellite; Meteorology; Nitrogen dioxide; Climatology; Miami; 2019-20 coronavirus outbreak; Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2); Geography; Physics; Geology","score_opus":0.06377794707840577,"score_gpt":0.35720874180611406,"score_spread":0.2934307947277083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3075013849","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99556077,0.00007997975,0.00079585053,0.00012599355,0.000013995558,0.000008992378,0.0009698768,0.000025566842,0.0024189933],"genre_scores_gemma":[0.9987947,0.00002209599,0.00015015576,0.000024872157,0.000005785446,0.0000050114577,0.0007474674,0.000009101861,0.00024076378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996055,0.00008450465,0.000025243773,0.00009735967,0.00008214597,0.00010530273],"domain_scores_gemma":[0.9985765,0.00042259524,0.00033769867,0.00018020012,0.0002820717,0.0002008865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005725692,0.00029413291,0.0001999841,0.0006794216,0.00045241177,0.0009798276,0.00030344343,0.00021880984,0.0018803343],"category_scores_gemma":[0.0023658427,0.0001989453,0.0004686724,0.0007066894,0.00036276193,0.0005846769,0.00079417997,0.00037765483,0.00029159128],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000090548405,0.000026752736,0.9918676,0.000009980954,0.000102167636,0.00007942116,0.000079665195,0.0011514832,0.0017211186,0.00017359373,0.00045827235,0.0042393217],"study_design_scores_gemma":[0.0000011935095,0.000012964329,0.9971872,0.0000026551006,0.000012627275,0.000010743963,0.00012733179,0.0018447196,0.00032007572,0.00003576024,0.00044206926,0.0000025803959],"about_ca_topic_score_codex":0.09345977,"about_ca_topic_score_gemma":0.13535392,"teacher_disagreement_score":0.09345977,"about_ca_system_score_codex":0.00053304085,"about_ca_system_score_gemma":0.0007903178,"threshold_uncertainty_score":0.1858316},"labels":[],"label_agreement":null},{"id":"W3080490320","doi":"10.1029/2020gl089573","title":"A 4‐Month Lead Predictor of Open‐Water Onset in Bering Strait","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Lead (geology); Open water; Open sea; Cape; Oceanography; Climatology; Geology; Sea ice; Current (fluid); Environmental science; Atmospheric sciences; Geomorphology; Geography","score_opus":0.04740808562861737,"score_gpt":0.29118889848738366,"score_spread":0.2437808128587663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080490320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987237,0.000031078387,0.00016386353,0.000037359343,0.00001353573,0.0000022605143,0.00047732005,0.000013932622,0.0005368122],"genre_scores_gemma":[0.9989446,0.00002397727,0.00006829694,0.0000035695766,0.0000042168176,0.0000017838754,0.0005902232,0.000003391696,0.00035995417],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993575,0.000008010328,0.0000044301573,0.000018103203,0.000010109707,0.0000236467],"domain_scores_gemma":[0.99944276,0.0001198613,0.00013708786,0.000025089048,0.000106917796,0.00016822295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020645869,0.00019507318,0.00014128453,0.00037947754,0.00027061303,0.00059754576,0.00016311329,0.00020130414,0.0017361705],"category_scores_gemma":[0.0008087939,0.00010711039,0.00021207008,0.00022389104,0.00016085473,0.0002783633,0.00042580624,0.00033709162,0.0003708963],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008384157,0.000015809172,0.99353975,0.0000061303285,0.000018148135,0.00008170093,0.00009148543,0.0028900888,0.0006332957,0.00006369389,0.00029519552,0.0022809703],"study_design_scores_gemma":[0.0000040533346,0.00003843647,0.98921555,0.000007645926,0.000009916934,0.000028049371,0.00023662836,0.00933838,0.00034845227,0.00005411775,0.00071300915,0.0000057771863],"about_ca_topic_score_codex":0.09679981,"about_ca_topic_score_gemma":0.13217342,"teacher_disagreement_score":0.09679981,"about_ca_system_score_codex":0.00077518565,"about_ca_system_score_gemma":0.00075606606,"threshold_uncertainty_score":0.19247276},"labels":[],"label_agreement":null},{"id":"W3080947165","doi":"10.1029/2020gl089933","title":"Arctic Amplification: A Rapid Response to Radiative Forcing","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":80,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"National Science Foundation","keywords":"Radiative forcing; Arctic; Climatology; Forcing (mathematics); Ice-albedo feedback; Environmental science; Arctic geoengineering; Sea ice; Atmospheric sciences; Polar; Climate change; Arctic ice pack; The arctic; Global warming; Cryosphere; Radiative transfer; Geology; Oceanography; Drift ice; Physics","score_opus":0.08025377156893485,"score_gpt":0.3310737444325786,"score_spread":0.25081997286364377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3080947165","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99166286,0.0001918434,0.003077828,0.00032512235,0.000041172618,0.000012431849,0.00019280266,0.00023506985,0.0042608334],"genre_scores_gemma":[0.9996594,0.000026729533,0.00012875724,0.000023751461,0.0000053283716,0.0000024716635,0.000026994698,0.0000108443655,0.000115739975],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99989414,0.000024214887,0.0000060262623,0.00002673813,0.00001724974,0.000031544118],"domain_scores_gemma":[0.9995871,0.00014847513,0.00008267511,0.00004627201,0.000052702013,0.00008280444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028777748,0.00029390503,0.0002806457,0.00022547373,0.0002499314,0.00060096435,0.0002452205,0.00030714425,0.002145641],"category_scores_gemma":[0.0013563546,0.00022925434,0.00034760486,0.00013959294,0.00029459738,0.00031246326,0.00082603283,0.0005132332,0.00018576732],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015585427,0.00039825434,0.15005465,0.000346706,0.0004789327,0.0019691503,0.00048163696,0.50193185,0.30289838,0.007664933,0.00578547,0.026431607],"study_design_scores_gemma":[0.00012289142,0.00035096894,0.19598094,0.000038819297,0.00013673323,0.00048369274,0.0003489443,0.7694943,0.021917196,0.006695697,0.004319677,0.000110151486],"about_ca_topic_score_codex":0.0037780718,"about_ca_topic_score_gemma":0.0022731037,"teacher_disagreement_score":0.0037780718,"about_ca_system_score_codex":0.00027284882,"about_ca_system_score_gemma":0.0002966266,"threshold_uncertainty_score":0.007512152},"labels":[],"label_agreement":null},{"id":"W3081075437","doi":"10.1029/2020gl089612","title":"Heterogeneity Affects Intertidal Flow Topology in Coastal Beach Aquifers","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Science Foundation","keywords":"Intertidal zone; Aquifer; Biogeochemical cycle; Geology; Saltwater intrusion; Groundwater; Mixing (physics); Groundwater flow; Environmental science; Hydrology (agriculture); Oceanography; Ecology; Geotechnical engineering; Physics","score_opus":0.03779304801141051,"score_gpt":0.2839650350440581,"score_spread":0.24617198703264762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081075437","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956304,0.0000055144983,0.00024124236,0.000008584785,4.7279218e-7,0.0000010875885,0.000024461164,0.000008506239,0.00014707047],"genre_scores_gemma":[0.9999013,0.0000039905062,0.00004568948,0.0000010515844,1.6905256e-7,4.5302028e-7,0.000013971924,0.0000010114048,0.000032288513],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999386,0.0000141385235,0.0000041555886,0.000016332546,0.000005562802,0.000021144393],"domain_scores_gemma":[0.9996964,0.00014219935,0.00006018963,0.000021370166,0.000029466368,0.00005048133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015154816,0.0001624953,0.00017191298,0.00043174162,0.00030821905,0.00076103024,0.00021649078,0.00024454785,0.0007818185],"category_scores_gemma":[0.0007047081,0.00018267342,0.00018849417,0.00029637216,0.0003760796,0.00038283423,0.0003331431,0.00014417461,0.000051712148],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027939482,0.00012498838,0.26133445,0.000029409664,0.000072205534,0.00027857377,0.00021680415,0.7099979,0.020768072,0.0015708033,0.0002231689,0.0051042554],"study_design_scores_gemma":[0.000026037744,0.00007803382,0.078857854,0.0000050670355,0.000021756265,0.00003564175,0.0002661976,0.91802293,0.0020542399,0.0004913257,0.00012291252,0.000018014778],"about_ca_topic_score_codex":0.014632656,"about_ca_topic_score_gemma":0.010969014,"teacher_disagreement_score":0.014632656,"about_ca_system_score_codex":0.00061171764,"about_ca_system_score_gemma":0.00033718883,"threshold_uncertainty_score":0.029094934},"labels":[],"label_agreement":null},{"id":"W3081282254","doi":"10.1029/2020gl087917","title":"Massive Ice Control on Permafrost Coast Erosion and Sensitivity","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; Dalhousie University; Geological Survey of Canada; Natural Resources Canada","funders":"Sight Research UK","keywords":"Permafrost; Geology; Shore; Cliff; Spatial variability; Subsidence; Erosion; Physical geography; Oceanography; Geomorphology; Geography","score_opus":0.06421241189505068,"score_gpt":0.29083987222565544,"score_spread":0.22662746033060477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081282254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984707,0.00003790703,0.000120506666,0.000014457138,7.8299354e-7,9.256235e-7,0.00013007763,0.000007450589,0.0012172031],"genre_scores_gemma":[0.9998549,0.00001051474,0.000035143385,0.0000025140491,7.621175e-7,3.2496303e-7,0.000049894024,0.0000013190381,0.000044680546],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999299,0.000011387425,0.000004892918,0.000021585087,0.000014678746,0.00001755573],"domain_scores_gemma":[0.99965453,0.000087896035,0.00013708186,0.000038612987,0.000038529008,0.000043463046],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017981134,0.0001437599,0.000121143734,0.0004904397,0.00015506071,0.0004933468,0.00015541745,0.00013548344,0.0016202249],"category_scores_gemma":[0.00076887815,0.0000736025,0.00010908731,0.00042273168,0.00034463842,0.00027586136,0.00035463,0.00010429078,0.000107836706],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011922844,0.000021901718,0.9688418,0.000021178455,0.000060636714,0.00015654237,0.00014550597,0.0074190637,0.008901632,0.0002705403,0.00015872334,0.013883278],"study_design_scores_gemma":[0.0000013006155,0.000012132871,0.9966235,0.0000032893918,0.0000045585743,0.000055307533,0.000081258135,0.0022889776,0.0005859894,0.00015021248,0.00019065464,0.0000026838884],"about_ca_topic_score_codex":0.0055264886,"about_ca_topic_score_gemma":0.009555635,"teacher_disagreement_score":0.0055264886,"about_ca_system_score_codex":0.0003160052,"about_ca_system_score_gemma":0.00009983487,"threshold_uncertainty_score":0.010988653},"labels":[],"label_agreement":null},{"id":"W3081840895","doi":"10.1029/2020gl088048","title":"Thank You to Our 2019 Peer Reviewers","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Data Quality and Management","field":"Decision Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Presentation (obstetrics); Reading (process); Library science; Rigour; Quality (philosophy); Peer review; Computer science; Political science; History; Engineering ethics; Data science; Public relations; Law; Medicine; Epistemology; Engineering","score_opus":0.39791782158928635,"score_gpt":0.5136762855153798,"score_spread":0.11575846392609346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3081840895","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0006543297,0.007421312,0.0061164196,0.2711468,0.67837816,0.0012066594,0.0028328903,0.003785288,0.028458172],"genre_scores_gemma":[0.010319917,0.011151839,0.021614607,0.18078613,0.333838,0.0034467075,0.0055155684,0.006543771,0.42678344],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9488194,0.01222737,0.006914561,0.0058488795,0.023773136,0.0024166673],"domain_scores_gemma":[0.48655567,0.018070403,0.013873537,0.016041357,0.43382224,0.031636734],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.038799215,0.0023944483,0.0031228869,0.008602289,0.0074390997,0.029812742,0.004277573,0.009754386,0.18956932],"category_scores_gemma":[0.260407,0.0013962268,0.002252144,0.0047456454,0.003038475,0.0084298,0.007118435,0.010420501,0.2973887],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012908096,0.0000062095173,0.00010271822,0.00007207541,0.000004367533,0.00004720838,0.00004915575,0.000010404065,0.000045901208,0.00016945162,0.98644596,0.013033596],"study_design_scores_gemma":[0.0000126876785,0.000009986358,0.00018951998,0.00016348055,0.000006944826,0.00012952088,0.00024819828,0.000056695077,0.0000698335,0.0005214054,0.9985642,0.000027563125],"about_ca_topic_score_codex":0.0034432067,"about_ca_topic_score_gemma":0.006510022,"teacher_disagreement_score":0.9612008,"about_ca_system_score_codex":0.0041997265,"about_ca_system_score_gemma":0.019051112,"threshold_uncertainty_score":0.63417256},"labels":[],"label_agreement":null},{"id":"W3082247220","doi":"10.1029/2020gl089608","title":"Climate Change Drives Increases in Extreme Events for Lake Ice in the Northern Hemisphere","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Ontario Ministry of Research, Innovation and Science; York University","keywords":"Environmental science; Northern Hemisphere; Climatology; Cryosphere; Arctic ice pack; Climate change; Sea ice; Physical geography; Oceanography; Geology; Geography","score_opus":0.08926941854701312,"score_gpt":0.2886011858300088,"score_spread":0.1993317672829957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082247220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99848664,0.000041998755,0.000059029757,0.00005744443,0.0000025396944,0.0000024032042,0.0006641399,0.0000070568462,0.0006787597],"genre_scores_gemma":[0.99946195,0.000024590812,0.00002682749,0.000009583278,0.000004314968,0.0000028163824,0.00036909553,0.0000023076122,0.0000985298],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998933,0.000022161446,0.0000066235757,0.000026911912,0.000019687974,0.00003132256],"domain_scores_gemma":[0.9993957,0.00009990505,0.0003235868,0.000026635338,0.000063588726,0.0000905557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029187024,0.00012164752,0.00018005788,0.0004450139,0.00042738713,0.0008624106,0.00013753012,0.00021392385,0.0025504006],"category_scores_gemma":[0.0010776042,0.000107973756,0.00020139072,0.0006583981,0.00022536992,0.0003980637,0.00042771336,0.00021980747,0.0001962444],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000078485304,0.000022409433,0.9953507,0.000008778916,0.000029242523,0.00004488014,0.00016175807,0.00040458882,0.0017391209,0.000057140187,0.00033687387,0.0017659877],"study_design_scores_gemma":[0.0000011440017,0.0000036141205,0.99948007,0.0000012893576,0.0000025778263,0.000009061738,0.00008358664,0.00023369193,0.000048431863,0.000026970249,0.000108237866,0.0000013536354],"about_ca_topic_score_codex":0.022875622,"about_ca_topic_score_gemma":0.036467496,"teacher_disagreement_score":0.022875622,"about_ca_system_score_codex":0.0004785091,"about_ca_system_score_gemma":0.00028168526,"threshold_uncertainty_score":0.0454849},"labels":[],"label_agreement":null},{"id":"W3082441020","doi":"10.1029/2020gl089718","title":"Effects of Polarization Reversal on the Pitch Angle Scattering of Radiation Belt Electrons and Ring Current Protons by EMIC Waves","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National Postdoctoral Program for Innovative Talents; China Postdoctoral Science Foundation; Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; China National Space Administration","keywords":"Physics; Electron; Van Allen radiation belt; Scattering; Polarization (electrochemistry); Pitch angle; Atomic physics; Ring current; Diffusion; Emic and etic; Radiation; Ion; Computational physics; Nuclear physics; Optics; Plasma; Magnetosphere; Geophysics; Chemistry","score_opus":0.010169249552007622,"score_gpt":0.26286861681266094,"score_spread":0.25269936726065334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3082441020","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99414873,0.00007764323,0.0046773585,0.000028273927,0.000008080224,0.0000041279386,0.000015538986,0.000030972064,0.0010092073],"genre_scores_gemma":[0.99867177,0.00005149204,0.001136094,0.000005720983,0.0000023843897,0.0000021899136,0.00001152815,0.000009039483,0.00010978779],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992573,0.000025937416,0.0000040221244,0.000010456522,0.000015871685,0.00001790748],"domain_scores_gemma":[0.99935967,0.0003835921,0.00008537408,0.000058769543,0.000068474175,0.000044035623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004088027,0.00026845137,0.00017783006,0.00018789504,0.00017650583,0.00033126128,0.00028091314,0.0002343804,0.00058394764],"category_scores_gemma":[0.0016249275,0.00014881365,0.00021003284,0.00017997976,0.00039413743,0.0003810897,0.0002905697,0.0002833912,0.00005011222],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011599185,0.00011302122,0.0436703,0.00017827324,0.00011465356,0.0009868549,0.00029453123,0.72955024,0.19737537,0.00463755,0.00024911176,0.02167014],"study_design_scores_gemma":[0.00004670546,0.00017742284,0.011184441,0.000010852889,0.000027818684,0.00011416815,0.00010917859,0.9252447,0.062438417,0.0003211803,0.00030575597,0.000019358404],"about_ca_topic_score_codex":0.0020761448,"about_ca_topic_score_gemma":0.0011331324,"teacher_disagreement_score":0.0020761448,"about_ca_system_score_codex":0.00020993972,"about_ca_system_score_gemma":0.00019498,"threshold_uncertainty_score":0.004128158},"labels":[],"label_agreement":null},{"id":"W3084009690","doi":"10.1029/2020gl092171","title":"The Importance of Scale‐Dependent Groundwater Processes in Land‐Atmosphere Interactions Over the Central United States","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Global Water Futures; National Oceanic and Atmospheric Administration; University of Saskatchewan; National Science Foundation","keywords":"Atmosphere (unit); Scale (ratio); Environmental science; Groundwater; Land use; Atmospheric sciences; Hydrology (agriculture); Meteorology; Geography; Geology; Cartography; Engineering; Civil engineering","score_opus":0.012042551180918763,"score_gpt":0.26753619747616375,"score_spread":0.255493646295245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3084009690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987643,0.000049503644,0.00021631668,0.00016049923,0.000005980886,0.0000028238235,0.0001465689,0.000029186018,0.0006248136],"genre_scores_gemma":[0.99981457,0.000017186121,0.000052274012,0.000012863846,0.0000016016024,0.0000013233152,0.000046376827,0.0000029052874,0.000050931285],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987876,0.00004181204,0.0000068918616,0.0000320581,0.000012800763,0.00002762806],"domain_scores_gemma":[0.99978787,0.00009087314,0.000029399394,0.000015739739,0.000032653614,0.000043451066],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030248705,0.00026883915,0.0003094247,0.00036524027,0.00051360973,0.0009419027,0.0003976945,0.0005942072,0.00114893],"category_scores_gemma":[0.0009211874,0.00028140555,0.00037741568,0.0005248049,0.00041658306,0.00067273935,0.00051946007,0.00030508763,0.000057759506],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031708894,0.0002249458,0.39470726,0.000050589813,0.00028682957,0.00032456577,0.00024871205,0.5817086,0.0090982625,0.0022217578,0.0015233739,0.009288045],"study_design_scores_gemma":[0.00010214527,0.000077284094,0.25073686,0.000014332842,0.000069748225,0.000040053303,0.0004248336,0.7454986,0.0010945657,0.0010686811,0.0008297919,0.000043225547],"about_ca_topic_score_codex":0.18532829,"about_ca_topic_score_gemma":0.1553739,"teacher_disagreement_score":0.18532829,"about_ca_system_score_codex":0.0013862598,"about_ca_system_score_gemma":0.0009546457,"threshold_uncertainty_score":0.36849916},"labels":[],"label_agreement":null},{"id":"W3086498647","doi":"10.1029/2020gl090695","title":"Predictable Variations of the Carbon Sinks and Atmospheric CO <sub>2</sub> Growth in a Multi‐Model Framework","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Bundesministerium für Bildung und Forschung","keywords":"Predictability; Environmental science; Carbon sink; Sink (geography); Initialization; Climatology; Carbon cycle; Carbon dioxide in Earth's atmosphere; Carbon dioxide; Carbon sequestration; Tropics; Climate model; Atmospheric sciences; Climate change; Oceanography; Geography; Geology; Ecology; Computer science; Mathematics; Ecosystem","score_opus":0.018355546430439174,"score_gpt":0.24956469358054484,"score_spread":0.23120914715010565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3086498647","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9523121,0.00026122117,0.04213115,0.0010878431,0.000055342225,0.000024498806,0.00060779805,0.0004424818,0.0030775664],"genre_scores_gemma":[0.99651647,0.000051399096,0.0029815808,0.000026186028,0.000015202906,0.00001330645,0.00012795291,0.000026533338,0.00024138762],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980277,0.000072391515,0.000012100605,0.00005616338,0.000024758603,0.000031745658],"domain_scores_gemma":[0.99919206,0.00037086738,0.00015614116,0.000093058385,0.00009492014,0.00009292501],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009908406,0.00068500417,0.0006619491,0.00046265475,0.0005573592,0.0013877851,0.000978728,0.0010158854,0.00074469927],"category_scores_gemma":[0.0018162946,0.00043303004,0.00095377344,0.0003411765,0.0009234089,0.0013964602,0.00090576493,0.001146954,0.0000843884],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023847771,0.0000137843,0.0023684846,0.0000053370795,0.000038939164,0.000021952674,0.000008368569,0.99532664,0.00059292605,0.0010820009,0.00006485224,0.00045288345],"study_design_scores_gemma":[0.000004716025,0.0000057561892,0.0007942151,9.507268e-7,0.0000066362854,0.0000018250396,0.000003708187,0.99850035,0.00008828228,0.0005522789,0.000036706155,0.00000454405],"about_ca_topic_score_codex":0.04157432,"about_ca_topic_score_gemma":0.022887915,"teacher_disagreement_score":0.04157432,"about_ca_system_score_codex":0.0014778164,"about_ca_system_score_gemma":0.0014325174,"threshold_uncertainty_score":0.08266467},"labels":[],"label_agreement":null},{"id":"W3086613144","doi":"10.1029/2020gl089793","title":"Reconciling the Relationship Between the AMOC and Labrador Sea in OSNAP Observations and Climate Models","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":85,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Seventh Framework Programme; Met Office Academic Partnership","keywords":"Ocean gyre; Climatology; Oceanography; Forcing (mathematics); Climate model; Geology; Thermohaline circulation; General Circulation Model; Shutdown of thermohaline circulation; Ocean current; Climate change; North Atlantic Deep Water","score_opus":0.15563275481524189,"score_gpt":0.2954744598712347,"score_spread":0.13984170505599283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3086613144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9961635,0.000087981556,0.0010368091,0.00019337446,0.000016001788,0.000006038427,0.0008164181,0.00009887128,0.0015809337],"genre_scores_gemma":[0.9986131,0.000030623152,0.0005580279,0.000029154813,0.00001033511,0.000005736463,0.0006474216,0.000018957819,0.000086567175],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99963903,0.00012751602,0.000028393955,0.0001175526,0.000035286535,0.000052248884],"domain_scores_gemma":[0.9990646,0.0003258445,0.00016666618,0.00019305832,0.00015965018,0.000090339236],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010856331,0.00042269015,0.00036548878,0.0004076182,0.00035809987,0.0011806412,0.0009405979,0.0005491671,0.0010321612],"category_scores_gemma":[0.0024919286,0.00027151316,0.000593692,0.00060361216,0.0003628188,0.0011282379,0.00088335725,0.00045983618,0.0001704224],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040323244,0.00018792179,0.69156975,0.00010229591,0.00082244,0.00026793746,0.00034098505,0.28176647,0.0052799983,0.0037110886,0.0024758433,0.0130720325],"study_design_scores_gemma":[0.00010089179,0.00006759396,0.41437238,0.000037764417,0.0001439556,0.000051776144,0.0002901057,0.5793011,0.0015005061,0.0016351144,0.002440129,0.000058708625],"about_ca_topic_score_codex":0.09647823,"about_ca_topic_score_gemma":0.09457522,"teacher_disagreement_score":0.09647823,"about_ca_system_score_codex":0.0012419937,"about_ca_system_score_gemma":0.00060759916,"threshold_uncertainty_score":0.19183332},"labels":[],"label_agreement":null},{"id":"W3087909386","doi":"10.1029/2020gl089697","title":"SMAP Detects Soil Moisture Under Temperate Forest Canopies","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Moisture and Remote Sensing","field":"Environmental Science","cited_by":77,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Trois-Rivières","funders":"Goddard Space Flight Center; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Environmental science; Temperate forest; Temperate rainforest; Radiometry; Water content; Temperate climate; Remote sensing; Atmospheric sciences; Biogeochemical cycle; Vegetation (pathology); Brightness temperature; Brightness; Ecosystem; Geology; Ecology","score_opus":0.032712198772819806,"score_gpt":0.2757603888741011,"score_spread":0.2430481901012813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3087909386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980416,0.000013625155,0.0011784119,0.0000049928058,0.0000016452393,0.000004659207,0.00020107975,0.00006311272,0.0004907814],"genre_scores_gemma":[0.9986411,0.0000101963105,0.0010846519,0.000006009866,0.0000020990012,0.0000047296758,0.00019074259,0.000004007605,0.000056404595],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988747,0.000026079662,0.0000033082817,0.00003786634,0.000029034512,0.000016165843],"domain_scores_gemma":[0.99982446,0.000063909705,0.000033599295,0.000023644181,0.00003144308,0.000022986615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026623943,0.00021847629,0.0001878628,0.00042574742,0.00011604299,0.00022420315,0.00014749673,0.00015204723,0.0006275385],"category_scores_gemma":[0.00046381785,0.000099827645,0.00011130972,0.00035460282,0.00014223017,0.00025190148,0.00019761905,0.00013615846,0.0001526999],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00075293845,0.00020915126,0.6676047,0.00008394129,0.00015047398,0.00014228342,0.0001596687,0.012313141,0.26875943,0.00015253693,0.0006657627,0.049005933],"study_design_scores_gemma":[0.000018365734,0.0001278036,0.9484942,0.000004581613,0.00002588329,0.000051300656,0.0000734025,0.03827232,0.0125671225,0.00008579257,0.00026905088,0.000010106275],"about_ca_topic_score_codex":0.0043845675,"about_ca_topic_score_gemma":0.0101877935,"teacher_disagreement_score":0.0043845675,"about_ca_system_score_codex":0.00014750939,"about_ca_system_score_gemma":0.0001042866,"threshold_uncertainty_score":0.008718133},"labels":[],"label_agreement":null},{"id":"W3088256131","doi":"10.1029/2020gl089689","title":"The Synchronization between the Zonal Jet Stream and Temperature Anomalies Leads to an Extremely Freezing North America in January 2019","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China-Guangdong Joint Fund","keywords":"Baroclinity; Climatology; Perturbation (astronomy); Jet stream; Arctic; Explosive material; Instability; Environmental science; Surge; Geology; Meteorology; Atmospheric sciences; Jet (fluid); Physics; Mechanics; Geography; Oceanography","score_opus":0.03434260708510224,"score_gpt":0.2864940383833145,"score_spread":0.25215143129821227,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088256131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987148,0.000025232754,0.00009702083,0.0002560826,0.000015609865,0.0000029355645,0.00011838332,0.000020476322,0.00074940646],"genre_scores_gemma":[0.99964356,0.000013870515,0.000039349015,0.000020574776,0.000005502355,0.0000018393567,0.00013088698,0.0000023199818,0.00014207554],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993396,0.00001055242,0.000002466742,0.000017648903,0.000012006387,0.000023278031],"domain_scores_gemma":[0.9997491,0.000042115793,0.00007005393,0.000019651652,0.000040326573,0.00007874338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018656132,0.00010903823,0.00011370375,0.00017284972,0.00063055044,0.00044801162,0.00019698094,0.0002455635,0.0010824751],"category_scores_gemma":[0.00067771494,0.00008883035,0.00012503169,0.0002404853,0.00034274455,0.00016450357,0.00040969867,0.00042636695,0.00008724871],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00059533474,0.00015418051,0.9375758,0.000036418107,0.00015335945,0.0048917993,0.0022158439,0.0087817535,0.015397119,0.0015941028,0.010280167,0.018324105],"study_design_scores_gemma":[0.000015560096,0.000055626428,0.98590577,0.000008738867,0.00002257504,0.00012864679,0.0012979987,0.009436736,0.0010378544,0.00035038992,0.00172863,0.0000114957365],"about_ca_topic_score_codex":0.07230803,"about_ca_topic_score_gemma":0.10591724,"teacher_disagreement_score":0.92769194,"about_ca_system_score_codex":0.00060207944,"about_ca_system_score_gemma":0.0004905732,"threshold_uncertainty_score":0.14377433},"labels":[],"label_agreement":null},{"id":"W3088958634","doi":"10.1029/2020gl089859","title":"Latitudinal Response of Storm Activity to Abrupt Climate Change During the Last 6,500 Years","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Bedford Institute of Oceanography; Geological Survey of Canada; Natural Resources Canada","funders":"Canada First Research Excellence Fund; Ocean Frontier Institute; National Natural Science Foundation of China","keywords":"Storm; Climatology; Latitude; Storm track; Climate change; Middle latitudes; Geology; Oceanography; Environmental science","score_opus":0.07370078867795028,"score_gpt":0.31845815744694056,"score_spread":0.2447573687689903,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3088958634","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925715,0.00008536621,0.000033759785,0.000025489448,0.0000036651932,9.213938e-7,0.00033600666,0.0000033257395,0.00025430773],"genre_scores_gemma":[0.99946696,0.00004220175,0.000019119849,0.000006534282,0.0000046629116,9.542537e-7,0.00035067392,9.975897e-7,0.000107959444],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998869,0.000017716942,0.000010213666,0.000036314,0.000019441411,0.00002940755],"domain_scores_gemma":[0.9993864,0.0000811357,0.00023745917,0.000034591296,0.00014307248,0.000117291565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002480432,0.0000983236,0.00012713356,0.00048148353,0.00019956219,0.00037717182,0.00010395647,0.00018032538,0.00083177147],"category_scores_gemma":[0.0007470706,0.00006745599,0.00015819726,0.00038674672,0.00016345955,0.00015608473,0.0002355552,0.00016993914,0.00016758849],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060520848,0.0000051108195,0.9970669,0.000005766989,0.000041502055,0.00003567486,0.000088836015,0.00020398048,0.0011588513,0.000020415164,0.0000834499,0.0012290768],"study_design_scores_gemma":[5.661234e-7,0.000006431249,0.99972075,8.267488e-7,0.0000027230867,0.000012487934,0.00003407378,0.000080798396,0.000038439804,0.0000025219022,0.00009978212,6.5222326e-7],"about_ca_topic_score_codex":0.028146023,"about_ca_topic_score_gemma":0.051978096,"teacher_disagreement_score":0.028146023,"about_ca_system_score_codex":0.00028015595,"about_ca_system_score_gemma":0.0001735127,"threshold_uncertainty_score":0.05596441},"labels":[],"label_agreement":null},{"id":"W3089764019","doi":"10.1029/2020gl089547","title":"Near‐Complete Local Reduction of Arctic Stratospheric Ozone by Severe Chemical Loss in Spring 2020","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":187,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Ozone; Ozone depletion; Ozone layer; Polar vortex; Atmospheric sciences; Arctic; Environmental science; Mixing ratio; Spring (device); Stratosphere; Polar night; Climatology; Polar; The arctic; Mixing (physics); Oceanography; Meteorology; Geology; Physics","score_opus":0.024933280937324154,"score_gpt":0.25445937570079796,"score_spread":0.2295260947634738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3089764019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964055,0.0002569041,0.00014308975,0.00015131825,0.000034978915,0.0000046351884,0.000790392,0.000016423206,0.0021968728],"genre_scores_gemma":[0.9975063,0.00011691482,0.00007565481,0.00007049323,0.000020683585,0.0000045944084,0.00115991,0.000003910015,0.0010414895],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991524,0.000010064142,0.0000038658227,0.000015866797,0.000022946539,0.000032049455],"domain_scores_gemma":[0.999869,0.000006137492,0.00003604522,0.000008181633,0.000039320374,0.000041288786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002517464,0.00020952898,0.00019098335,0.0003618406,0.00046915872,0.00050552713,0.00011873067,0.0002873794,0.0007695074],"category_scores_gemma":[0.00017245133,0.000078318975,0.0001921148,0.0003028573,0.00013445091,0.0001382355,0.00033547243,0.0001947381,0.000243183],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013941776,0.00012866125,0.9042883,0.00010516599,0.00025115162,0.00064188335,0.0006759648,0.0009947672,0.06333041,0.00024527824,0.0033448553,0.024599357],"study_design_scores_gemma":[0.0000016156961,0.00005335831,0.9967326,0.0000033743177,0.0000109522425,0.00005435205,0.00018885132,0.0001309388,0.001272602,0.000017767685,0.0015310759,0.000002534638],"about_ca_topic_score_codex":0.03141833,"about_ca_topic_score_gemma":0.05095242,"teacher_disagreement_score":0.03141833,"about_ca_system_score_codex":0.0004991807,"about_ca_system_score_gemma":0.00043045531,"threshold_uncertainty_score":0.062470913},"labels":[],"label_agreement":null},{"id":"W3090785602","doi":"10.1029/2020gl089829","title":"A Fresh Look at Variography: Measuring Dependence and Possible Sensitivities Across Geophysical Systems From Any Given Data","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Probabilistic and Robust Engineering Design","field":"Decision Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; University of Saskatchewan","funders":"","keywords":"Robustness (evolution); Computer science; Sensitivity (control systems); Sampling (signal processing); Variogram; Data mining; Sample (material); Econometrics; Machine learning; Mathematics; Kriging","score_opus":0.24244019834115385,"score_gpt":0.37340346494878923,"score_spread":0.13096326660763538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3090785602","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2702274,0.00038470875,0.7254251,0.0010523698,0.00003466522,0.000050473205,0.00033082688,0.00019065508,0.0023037826],"genre_scores_gemma":[0.95068127,0.00016223671,0.04852926,0.00012608779,0.000030923933,0.000040803752,0.00016522258,0.000041379335,0.00022277105],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9958973,0.0025384128,0.00020506166,0.0005009237,0.00073723594,0.000121144214],"domain_scores_gemma":[0.9504891,0.04176033,0.002413234,0.003790564,0.001259702,0.00028709645],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010169192,0.00044691612,0.0007307638,0.002531941,0.00039102897,0.0019517611,0.00070762954,0.00081220287,0.0011706939],"category_scores_gemma":[0.047863703,0.00042256727,0.0008543684,0.0018609609,0.0021736843,0.00269761,0.0017416312,0.0020621477,0.00012482845],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041410438,0.00017884524,0.08908285,0.00023673383,0.0006944298,0.0003723002,0.0006162607,0.7118018,0.0178982,0.06904729,0.0009847245,0.108672395],"study_design_scores_gemma":[0.00001648583,0.0002118437,0.044136066,0.00007092127,0.00007909471,0.00019621433,0.0002991184,0.8029264,0.010735118,0.13993849,0.0012721391,0.000118128024],"about_ca_topic_score_codex":0.0014392355,"about_ca_topic_score_gemma":0.0009583164,"teacher_disagreement_score":0.010169192,"about_ca_system_score_codex":0.0006127213,"about_ca_system_score_gemma":0.0004813135,"threshold_uncertainty_score":0.053780496},"labels":[],"label_agreement":null},{"id":"W3091777064","doi":"10.1029/2020gl090420","title":"Identification of Geochemical Processes During Hydraulic Fracturing of a Shale Gas Reservoir: A Controlled Field and Laboratory Water‐Rock Interaction Experiment","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Youth Innovation Promotion Association of the Chinese Academy of Sciences; International Atomic Energy Agency; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Hydraulic fracturing; Oil shale; Geology; Produced water; Petroleum engineering; Mixing (physics)","score_opus":0.012418546492478777,"score_gpt":0.26415494922327154,"score_spread":0.2517364027307928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3091777064","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993901,0.000013446459,0.0003897166,0.0000067013784,0.0000021870733,0.00001752657,0.00006235572,0.000015864485,0.000102107006],"genre_scores_gemma":[0.99854124,0.00002237142,0.0009692892,0.000010772915,0.0000036334689,0.000041065094,0.00010509705,0.0000065426393,0.0002999318],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9998487,0.000022393579,0.000009559049,0.00004217023,0.000037210695,0.000039962695],"domain_scores_gemma":[0.9997446,0.000073273135,0.000045953057,0.000025719379,0.000057401732,0.00005300192],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024553586,0.00029733076,0.00029979664,0.00026186055,0.00054209016,0.00024328551,0.0003758669,0.00035533597,0.00061895314],"category_scores_gemma":[0.00024936112,0.00015316579,0.00025482487,0.00014499768,0.0004194529,0.0003015501,0.00027085026,0.00044886876,0.00009327463],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004749704,0.0003620699,0.0056651174,0.00002210106,0.000010405141,0.000057062938,0.00009615482,0.00030460587,0.99154913,0.000023885528,0.000031502237,0.001403069],"study_design_scores_gemma":[0.00009676665,0.005971442,0.072256364,0.000005677012,0.00004978589,0.000081710736,0.00031409855,0.008558216,0.9120963,0.00006908343,0.0004676566,0.000032904707],"about_ca_topic_score_codex":0.0032562285,"about_ca_topic_score_gemma":0.0055484436,"teacher_disagreement_score":0.0032562285,"about_ca_system_score_codex":0.00033924423,"about_ca_system_score_gemma":0.0003319327,"threshold_uncertainty_score":0.0064745545},"labels":[],"label_agreement":null},{"id":"W3091835895","doi":"10.1029/2020gl091188","title":"Constraining Fault Friction and Stability With Fluid‐Injection Field Experiments","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche; National Science Foundation","keywords":"Cabin pressurization; Slip (aerodynamics); Geology; Residual; Observable; Fault (geology); Mechanics; Geotechnical engineering; Seismology; Materials science; Computer science; Physics; Thermodynamics","score_opus":0.055627735141188746,"score_gpt":0.3023509885213441,"score_spread":0.24672325338015538,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3091835895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99563414,0.000059870214,0.0037702008,0.000027802062,0.000004881599,0.000009258313,0.00005899105,0.000041370942,0.00039360626],"genre_scores_gemma":[0.9994299,0.000020081872,0.00048931723,0.000002503842,0.0000011545777,0.0000043025843,0.000012934192,0.0000023417342,0.000037457317],"study_design_codex":"simulation_or_modeling","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99993503,0.000014837326,0.0000064302412,0.0000170859,0.000010823164,0.000015767853],"domain_scores_gemma":[0.9994766,0.0002622263,0.00013731312,0.000058853595,0.00003293579,0.000032146494],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021796506,0.00029916334,0.00031447544,0.0003179495,0.0001473119,0.00035799594,0.0004598051,0.0003553683,0.00087933143],"category_scores_gemma":[0.0009417457,0.00014775193,0.00022707843,0.00016080534,0.0005289183,0.0004273305,0.00028209348,0.000319647,0.000039567134],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005181653,0.0005992564,0.02666768,0.00019116321,0.0000971578,0.0002719279,0.00015837004,0.71468675,0.24292724,0.004825759,0.0002653254,0.008791211],"study_design_scores_gemma":[0.00006222687,0.0004751917,0.0051944307,0.000007733937,0.000028130597,0.000029056628,0.00003478638,0.94567496,0.047293473,0.000898385,0.00027779717,0.000023778512],"about_ca_topic_score_codex":0.0016901111,"about_ca_topic_score_gemma":0.0012190099,"teacher_disagreement_score":0.0016901111,"about_ca_system_score_codex":0.00043185975,"about_ca_system_score_gemma":0.00017259114,"threshold_uncertainty_score":0.0033605099},"labels":[],"label_agreement":null},{"id":"W3092249262","doi":"10.1029/2020gl088901","title":"Moulin Volumes Regulate Subglacial Water Pressure on the Greenland Ice Sheet","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canmore Museum and Geoscience Centre","funders":"National Science Foundation","keywords":"Meltwater; Geology; Water pressure; Greenland ice sheet; Hydrology (agriculture); Geomorphology; Ice sheet; Environmental science; Oceanography; Glacier; Geotechnical engineering","score_opus":0.053169435604597894,"score_gpt":0.26406615518105847,"score_spread":0.21089671957646058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092249262","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99951136,0.000031978547,0.00007091138,0.000008156602,3.930162e-7,6.4364076e-7,0.00004604462,0.0000072173943,0.00032321588],"genre_scores_gemma":[0.99979883,0.000019095762,0.00003416837,0.000004582729,5.0095423e-7,0.0000012530492,0.000041825533,0.00000351764,0.000096226926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999585,0.00000436112,0.0000021890978,0.000012567641,0.000007277089,0.000015109658],"domain_scores_gemma":[0.99987173,0.000029755533,0.000041932944,0.000009929721,0.000020194175,0.000026419979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008963727,0.00017254525,0.00017096713,0.00041862603,0.00023688808,0.0006453087,0.00017889556,0.00016021839,0.00076177943],"category_scores_gemma":[0.00021460968,0.00013837212,0.00013748699,0.00022036524,0.00049012684,0.00048551802,0.00058441056,0.00015427348,0.0001102275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00058604765,0.000046491255,0.4870589,0.00006181929,0.00010463596,0.00023209344,0.00065732317,0.01315789,0.48231974,0.0008483082,0.00038850328,0.014538139],"study_design_scores_gemma":[0.000005687882,0.000036103163,0.98044765,0.0000055815194,0.000012757389,0.000017834853,0.00027348835,0.0054957457,0.01299872,0.00019948646,0.0004997254,0.0000071548334],"about_ca_topic_score_codex":0.009733907,"about_ca_topic_score_gemma":0.012160044,"teacher_disagreement_score":0.009733907,"about_ca_system_score_codex":0.000727298,"about_ca_system_score_gemma":0.0002106658,"threshold_uncertainty_score":0.019354522},"labels":[],"label_agreement":null},{"id":"W3092327759","doi":"10.1029/2020gl090844","title":"Record‐Breaking Increases in Arctic Solar Ultraviolet Radiation Caused by Exceptionally Large Ozone Depletion in 2020","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"Miljødirektoratet; Environment and Climate Change Canada; European Space Agency; Norges Forskningsråd; European Commission; Academy of Finland","keywords":"Ozone depletion; Arctic; Environmental science; Ozone; Atmospheric sciences; Ultraviolet radiation; Ozone layer; Subarctic climate; The arctic; Climatology; Meteorology; Oceanography; Geography; Geology; Chemistry","score_opus":0.02150746696422707,"score_gpt":0.2679844001011197,"score_spread":0.24647693313689262,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3092327759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99425596,0.00066859927,0.00020363716,0.000084874024,0.00004594821,0.000003462977,0.0030953304,0.000030426794,0.0016116755],"genre_scores_gemma":[0.995256,0.00027199427,0.00015853382,0.000039329338,0.000030512692,0.0000045775823,0.003942087,0.0000034500754,0.00029350922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998634,0.000015286894,0.00001560719,0.00003234301,0.00003551023,0.000037799433],"domain_scores_gemma":[0.99930596,0.000069512214,0.00024668156,0.000048635808,0.000245721,0.00008346128],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048315726,0.00023240922,0.0002091675,0.0007942001,0.00034241925,0.0007078217,0.00017989485,0.00029976235,0.00045236674],"category_scores_gemma":[0.0007347577,0.00012239159,0.00020897234,0.0008708764,0.00014564118,0.00028237846,0.0003911557,0.00024661416,0.00022117565],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034903182,0.00003175927,0.9788519,0.000074418764,0.0001230815,0.00022935866,0.0002608022,0.0006706186,0.0057557393,0.00013865426,0.0014275163,0.012087045],"study_design_scores_gemma":[0.0000013717519,0.000024478215,0.99721944,0.000008018044,0.000014975509,0.0000762717,0.00010607854,0.00032138024,0.0006175932,0.0000156126,0.0015914491,0.0000033550396],"about_ca_topic_score_codex":0.03558459,"about_ca_topic_score_gemma":0.0510604,"teacher_disagreement_score":0.03558459,"about_ca_system_score_codex":0.0005696649,"about_ca_system_score_gemma":0.00042818332,"threshold_uncertainty_score":0.070754945},"labels":[],"label_agreement":null},{"id":"W3093010404","doi":"10.1029/2020gl089366","title":"Correlation Between Poroelastic Stress Perturbation and Multidisposal Wells Induced Earthquake Sequence in Cushing, Oklahoma","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Poromechanics; Geology; Seismology; Pore water pressure; Seismic hazard; Shear (geology); Perturbation (astronomy); Fault (geology); Induced seismicity; Shear stress; Geotechnical engineering; Petrology; Mechanics","score_opus":0.07250017230694451,"score_gpt":0.29727713367385067,"score_spread":0.22477696136690617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093010404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994135,0.00001332185,0.000026253716,0.000025961292,0.000001464369,0.0000037785828,0.0002587151,0.0000036624156,0.00025341994],"genre_scores_gemma":[0.999526,0.0000146090215,0.000048079815,0.000010473586,0.0000016062331,0.00000636661,0.00023178957,7.0452427e-7,0.00016038989],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983907,0.000018705574,0.000016984806,0.000040780662,0.000030731702,0.00005368017],"domain_scores_gemma":[0.99914014,0.00013946216,0.00033220823,0.00004971212,0.0001538296,0.00018463284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001324152,0.00016109264,0.00013782774,0.0007800251,0.0007692611,0.0004196933,0.0002721471,0.00037125463,0.0016182769],"category_scores_gemma":[0.00068757136,0.00013359111,0.00008926111,0.000881588,0.000341898,0.00022512038,0.0004642909,0.0002773585,0.00014031678],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000061963874,0.00003731869,0.99368393,0.000013736924,0.000032282034,0.0002147063,0.00033060054,0.00057423854,0.0016492023,0.000031461623,0.0002874834,0.003083044],"study_design_scores_gemma":[0.0000019047206,0.00001538053,0.9984285,0.0000044147096,0.0000051146903,0.000021595903,0.0008149086,0.00036354022,0.000119856195,0.0000058246333,0.00021541795,0.0000034242753],"about_ca_topic_score_codex":0.34015056,"about_ca_topic_score_gemma":0.6155665,"teacher_disagreement_score":0.34015056,"about_ca_system_score_codex":0.002095119,"about_ca_system_score_gemma":0.0013159404,"threshold_uncertainty_score":0.6763413},"labels":[],"label_agreement":null},{"id":"W3093298598","doi":"10.1029/2020gl088980","title":"The Apparent Motion of STEVE and the Picket Fence Phenomena","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Picketing; Convection; Geology; Fence (mathematics); Physics; Meteorology; Law; Political science; Mathematics","score_opus":0.02669266092010653,"score_gpt":0.28501058096270465,"score_spread":0.2583179200425981,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093298598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99587554,0.000076358156,0.0007071248,0.00002466469,0.0000064890814,0.000005467889,0.00021747976,0.00004545149,0.0030414339],"genre_scores_gemma":[0.9990213,0.000020850744,0.00044425757,0.0000058182673,0.0000035920075,0.0000018629439,0.00019311678,0.000013630454,0.00029563764],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999236,0.000003838545,0.0000026897803,0.000021760863,0.000023205332,0.000024775722],"domain_scores_gemma":[0.99987483,0.00001657806,0.000038537575,0.000016055998,0.00002815777,0.000025946783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000091033886,0.00015060474,0.00021956199,0.0009918148,0.00033494085,0.00054874015,0.00027717897,0.00024519596,0.001412536],"category_scores_gemma":[0.0003470365,0.000120388315,0.00013573961,0.00043398363,0.0002961321,0.00050566235,0.0005148825,0.00034099567,0.00021462707],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009733204,0.00013323622,0.60337526,0.00014928523,0.00016406912,0.0026767028,0.0018486131,0.004421455,0.31832808,0.0014975314,0.002159858,0.06427255],"study_design_scores_gemma":[0.000008421946,0.000042322834,0.98652655,0.0000107509995,0.000013291232,0.00054002076,0.00036241347,0.004034797,0.0063091004,0.00013078228,0.002004162,0.000017350036],"about_ca_topic_score_codex":0.0043641697,"about_ca_topic_score_gemma":0.008518924,"teacher_disagreement_score":0.0043641697,"about_ca_system_score_codex":0.00022670656,"about_ca_system_score_gemma":0.00012260009,"threshold_uncertainty_score":0.008677542},"labels":[],"label_agreement":null},{"id":"W3093763280","doi":"10.1029/2020gl088728","title":"African Humid Period Precipitation Sustained by Robust Vegetation, Soil, and Lake Feedbacks","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":112,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Precipitation; Climatology; Northern Hemisphere; Monsoon; Vegetation (pathology); Environmental science; Insolation; Period (music); Anomaly (physics); Steppe; Climate change; Atmospheric sciences; Physical geography; Geology; Geography; Meteorology; Oceanography","score_opus":0.02891590013542818,"score_gpt":0.26747917407902005,"score_spread":0.23856327394359186,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3093763280","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987821,0.00006336129,0.00029293832,0.00008625111,0.0000045462903,0.0000025456673,0.00012196542,0.000032800417,0.00061355095],"genre_scores_gemma":[0.9998568,0.000019914422,0.000051537267,0.0000050414537,0.0000028257318,8.5323e-7,0.000022086477,0.0000021567016,0.000038571518],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993443,0.000015339752,0.0000042699166,0.00001512873,0.000008231194,0.000022615557],"domain_scores_gemma":[0.9998578,0.00003370134,0.000037322312,0.000018104243,0.000022160237,0.000030943793],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016766458,0.00025331933,0.00027755133,0.00020562965,0.0003361978,0.00050378457,0.0002118171,0.00023759542,0.001377808],"category_scores_gemma":[0.00057330675,0.00016471845,0.00015620203,0.00022988033,0.000313786,0.00037306672,0.00041690204,0.00025463736,0.00009659432],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018738338,0.00030882587,0.4639195,0.00040523647,0.00062463415,0.0028149502,0.0008608968,0.17060192,0.30164528,0.007802988,0.0025623045,0.04657967],"study_design_scores_gemma":[0.00018162509,0.00020281269,0.80783117,0.000023419982,0.0001253766,0.00032953327,0.0005298754,0.17396557,0.0109654255,0.002980072,0.0028181125,0.00004691813],"about_ca_topic_score_codex":0.0073587163,"about_ca_topic_score_gemma":0.005774259,"teacher_disagreement_score":0.0073587163,"about_ca_system_score_codex":0.00055197836,"about_ca_system_score_gemma":0.00027520067,"threshold_uncertainty_score":0.014631808},"labels":[],"label_agreement":null},{"id":"W3094110234","doi":"10.1029/2020gl089342","title":"Using a Large‐<i>n</i> Seismic Array to Explore the Robustness of Spectral Estimations","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Deutsche Forschungsgemeinschaft","keywords":"Seismic moment; Geology; Seismology; Scaling; Spectral line; Physics; Mathematics; Geometry","score_opus":0.15385392303192055,"score_gpt":0.3362844622801319,"score_spread":0.18243053924821137,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094110234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.88950276,0.000113870265,0.10764664,0.00015607862,0.00003315534,0.000025199399,0.0004055025,0.00023546006,0.0018812998],"genre_scores_gemma":[0.9798543,0.000026602156,0.01966622,0.000029324614,0.000010031284,0.000011748356,0.00021560748,0.000018740584,0.0001674156],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99914277,0.00036056695,0.000052252937,0.0002695818,0.00012239556,0.000052323398],"domain_scores_gemma":[0.9928155,0.004661549,0.00062391325,0.0012809256,0.0005467452,0.00007125561],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017573576,0.00023185082,0.00020210304,0.0003748971,0.00024141156,0.0005025999,0.00030708627,0.00034012768,0.00062657415],"category_scores_gemma":[0.01049628,0.00016049041,0.00019791491,0.0004277799,0.00024894637,0.00049429195,0.0003962315,0.0002445469,0.00015029516],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001249666,0.00019440847,0.40965286,0.0001813758,0.0007700893,0.00029257877,0.000507996,0.26089978,0.14578235,0.0028185626,0.001138383,0.17651203],"study_design_scores_gemma":[0.00006976249,0.0005064376,0.335708,0.000046390895,0.0002177513,0.000421422,0.00034673628,0.6052483,0.052680697,0.0018378174,0.0028206927,0.00009599198],"about_ca_topic_score_codex":0.0051661674,"about_ca_topic_score_gemma":0.00574587,"teacher_disagreement_score":0.0051661674,"about_ca_system_score_codex":0.0002269715,"about_ca_system_score_gemma":0.00021535272,"threshold_uncertainty_score":0.010272205},"labels":[],"label_agreement":null},{"id":"W3094492627","doi":"10.1029/2020gl090134","title":"Using Thermal Springs to Quantify Deep Groundwater Flow and Its Thermal Footprint in the Alps and a Comparison With North American Orogens","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Karst Systems and Hydrogeology","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Deutsche Forschungsgemeinschaft","keywords":"Groundwater; Geology; Groundwater flow; Hydrology (agriculture); Spring (device); Thermal; Flow (mathematics); Environmental science; Aquifer; Geotechnical engineering; Meteorology; Mechanics; Geography","score_opus":0.07931984547795891,"score_gpt":0.30343368365678824,"score_spread":0.22411383817882935,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094492627","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99843377,0.00008255617,0.00024639504,0.000008223325,9.0933196e-7,0.000003417123,0.00063379685,0.000009298239,0.0005815986],"genre_scores_gemma":[0.998156,0.00009476531,0.00055040035,0.000006430326,0.0000035286762,0.000007391857,0.0010696237,0.0000051587044,0.00010662364],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997441,0.00006591281,0.0000217487,0.00005835961,0.00006664394,0.000043258315],"domain_scores_gemma":[0.9995615,0.00009359067,0.00016100386,0.0000445918,0.00009148658,0.0000477807],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004924921,0.00024834587,0.00030909388,0.0022421447,0.00026956422,0.0006130382,0.00015767709,0.00016428412,0.00060408405],"category_scores_gemma":[0.00057672005,0.00010065659,0.00028165357,0.002362835,0.00022387055,0.0003192611,0.00043985885,0.00011732185,0.00013639274],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019695445,0.000049657512,0.97957724,0.00004433612,0.00013726736,0.00004533163,0.00028317253,0.0021136638,0.005664612,0.000065126704,0.00009966718,0.011722997],"study_design_scores_gemma":[0.00000797558,0.000020367252,0.99488443,0.000009260645,0.0000352416,0.00003718288,0.00032039543,0.0033953662,0.0006798955,0.000040626168,0.0005646819,0.0000046235427],"about_ca_topic_score_codex":0.02209327,"about_ca_topic_score_gemma":0.037593752,"teacher_disagreement_score":0.02209327,"about_ca_system_score_codex":0.00026382023,"about_ca_system_score_gemma":0.00023697143,"threshold_uncertainty_score":0.04392934},"labels":[],"label_agreement":null},{"id":"W3094841974","doi":"10.1029/2020gl090482","title":"Role of Serpentinized Mantle Wedge in Affecting Megathrust Seismogenic Behavior in the Area of the 2010 <i>M</i> = 8.8 Maule Earthquake","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Aftershock; Seismology; Subduction; Intraplate earthquake; Mantle wedge; Wedge (geometry); Mantle (geology); Crust; Slip (aerodynamics); Seismic velocity; Geophysics; Tectonics","score_opus":0.04453511853104641,"score_gpt":0.27152782332204345,"score_spread":0.22699270479099704,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3094841974","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953675,0.000042131072,0.00003284358,0.000018939716,5.2494e-7,0.0000013358055,0.00003288153,0.0000033813496,0.00033124464],"genre_scores_gemma":[0.99989235,0.000015800642,0.000012903749,0.0000029172695,5.507292e-7,4.4184696e-7,0.000013124326,7.9851884e-7,0.000061137565],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999603,0.0000068650556,0.0000032697278,0.000010916528,0.0000042531487,0.000014352215],"domain_scores_gemma":[0.99978334,0.00002864301,0.00009762712,0.000012794952,0.000024436102,0.000053201788],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011005587,0.00015912433,0.00017497758,0.00038296837,0.00017742712,0.0004377901,0.00019511709,0.00021160573,0.0013697552],"category_scores_gemma":[0.0004455254,0.00012986355,0.00010840127,0.00019822577,0.00030314387,0.00022796917,0.00028515395,0.00013001545,0.00015886677],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038364355,0.00007661215,0.8920947,0.00006672176,0.00006231875,0.00086451776,0.000407974,0.0023711713,0.09585463,0.00029509235,0.000096172196,0.007426504],"study_design_scores_gemma":[0.0000029470204,0.000027403457,0.9977762,0.0000028816148,0.000007563491,0.00006298142,0.00020256914,0.0008523739,0.00091051246,0.00004588349,0.000105711784,0.000002998066],"about_ca_topic_score_codex":0.0066734464,"about_ca_topic_score_gemma":0.008053877,"teacher_disagreement_score":0.0066734464,"about_ca_system_score_codex":0.00032366722,"about_ca_system_score_gemma":0.00018225274,"threshold_uncertainty_score":0.013269246},"labels":[],"label_agreement":null},{"id":"W3095159451","doi":"10.1029/2020gl090219","title":"Sequential Fault Reactivation and Secondary Triggering in the March 2019 Red Deer Induced Earthquake Swarm","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University; Alberta Energy; Geological Survey of Canada; University of Alberta","funders":"","keywords":"Seismology; Seismometer; Geology; Induced seismicity; Fault (geology); Slip (aerodynamics); Stress field; Hypocenter; Geophone; Microseism; Earthquake swarm; Swarm behaviour; Strike-slip tectonics","score_opus":0.06894953226310341,"score_gpt":0.2966689986295678,"score_spread":0.2277194663664644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095159451","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99956316,0.000018414317,0.00004682606,0.000005944415,8.574333e-7,0.0000025594277,0.00006588424,0.0000032774747,0.00029313244],"genre_scores_gemma":[0.99965465,0.000010228956,0.000038052654,0.0000029573932,0.0000012540999,0.0000017646136,0.00011040722,4.2741866e-7,0.00018024041],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999155,0.00000962954,0.0000045710503,0.00002321805,0.000020650461,0.000026540689],"domain_scores_gemma":[0.9997093,0.000030849216,0.0001030696,0.00001777224,0.00006673186,0.00007226211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011620432,0.0000921124,0.0001298633,0.0006065276,0.00020054205,0.00036071797,0.00015362639,0.00015266349,0.00085248216],"category_scores_gemma":[0.00038619188,0.00006892306,0.00007511142,0.0003496202,0.00022265739,0.00007911533,0.0002899952,0.00010371991,0.00013068404],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028468636,0.000050184226,0.97571325,0.0000138651585,0.000029520135,0.0006719341,0.0005995667,0.00037433326,0.01460764,0.00007257096,0.00023914127,0.0073432713],"study_design_scores_gemma":[0.0000013933724,0.0000294918,0.99907374,0.0000016681003,0.0000038358166,0.00007435226,0.00021094829,0.00019913528,0.00027392674,0.000009854776,0.000120112214,0.0000014162748],"about_ca_topic_score_codex":0.041295268,"about_ca_topic_score_gemma":0.10507919,"teacher_disagreement_score":0.9587047,"about_ca_system_score_codex":0.0006242579,"about_ca_system_score_gemma":0.00035434242,"threshold_uncertainty_score":0.08210981},"labels":[],"label_agreement":null},{"id":"W3095859552","doi":"10.1029/2020gl090431","title":"The Rheological Behavior of CO<sub>2</sub> Ice: Application to Glacial Flow on Mars","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Woods Hole Oceanographic Institution; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Geology; Martian; Glacial period; Creep; Polar; Rheology; Flow (mathematics); Geophysics; Geomorphology; Astrobiology; Mechanics; Thermodynamics; Physics","score_opus":0.0366048618217952,"score_gpt":0.30729526355363807,"score_spread":0.2706904017318429,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3095859552","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993249,0.000058442107,0.00016163767,0.000018081622,0.0000031194888,0.000004233455,0.000058018948,0.000014373028,0.00035713534],"genre_scores_gemma":[0.9996456,0.00003090025,0.00023394359,0.0000046008863,0.0000029242865,0.0000019619292,0.000033717464,0.00000207157,0.00004420359],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999647,0.0000066489342,0.0000023501486,0.000009146663,0.000007721642,0.000009309886],"domain_scores_gemma":[0.9999088,0.000023247183,0.000022598893,0.000011109131,0.000017414626,0.00001672504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012337422,0.00025292282,0.00015962141,0.0005303429,0.0002595294,0.00034072774,0.00014273437,0.00022207815,0.00096625334],"category_scores_gemma":[0.00026305692,0.00009220159,0.00013630031,0.00030360668,0.0003247156,0.0002093239,0.00021176276,0.00018305109,0.00007844342],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004441568,0.00011643601,0.068453126,0.0000911277,0.00003509937,0.00029993936,0.00033868515,0.006700539,0.91029227,0.00018052633,0.00025117077,0.012797042],"study_design_scores_gemma":[0.00004167239,0.0009505318,0.60563624,0.000019708701,0.00004981855,0.0003717111,0.00066225085,0.09743666,0.29248288,0.00030845037,0.001997698,0.00004228199],"about_ca_topic_score_codex":0.002013426,"about_ca_topic_score_gemma":0.0015248467,"teacher_disagreement_score":0.002013426,"about_ca_system_score_codex":0.00020075345,"about_ca_system_score_gemma":0.00007670772,"threshold_uncertainty_score":0.004003465},"labels":[],"label_agreement":null},{"id":"W3096939545","doi":"10.1029/2020gl088823","title":"An Abrupt Aging of Dissolved Organic Carbon in Large Arctic Rivers","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":82,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Aurora College","funders":"Natural Environment Research Council; Sight Research UK; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Permafrost; Dissolved organic carbon; Total organic carbon; Arctic; Environmental science; Radiocarbon dating; Carbon fibers; Organic matter; Carbon cycle; Soil carbon; Nitrate; Drainage basin; Hydrology (agriculture); Physical geography; Oceanography; Geology; Environmental chemistry; Soil water; Ecosystem; Soil science; Geography; Ecology; Chemistry","score_opus":0.057846978995373804,"score_gpt":0.3067742344840926,"score_spread":0.24892725548871877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3096939545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967444,0.000032285254,0.00002672899,0.000013458984,0.0000010640136,7.458301e-7,0.000059931368,0.000002664138,0.00018871114],"genre_scores_gemma":[0.9997693,0.000029783057,0.00004837791,0.000009310446,0.0000025814877,0.0000012359365,0.00007178576,7.028024e-7,0.00006694335],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999362,0.000006591809,0.000005007224,0.000022064314,0.0000140799175,0.000016068028],"domain_scores_gemma":[0.9997986,0.00002441155,0.00007790322,0.000011627894,0.000051416642,0.000036024678],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021036614,0.0001102542,0.00014882117,0.00046087182,0.0005331211,0.0005320637,0.0001448367,0.00022103607,0.0002978082],"category_scores_gemma":[0.00033235355,0.00010956499,0.0000984375,0.0003949126,0.00031706868,0.00023472545,0.00029282205,0.00014846088,0.000054366254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011053389,0.00002263618,0.9818627,0.000012879688,0.000026958533,0.00016738575,0.0002869224,0.00024023549,0.012660897,0.00007065686,0.00009014813,0.004448093],"study_design_scores_gemma":[0.0000010233936,0.000011943359,0.9987226,0.0000020454984,0.0000045670436,0.000032111246,0.00015048867,0.0002049298,0.0006563228,0.000019832958,0.00019254991,0.0000014991153],"about_ca_topic_score_codex":0.02126827,"about_ca_topic_score_gemma":0.03670709,"teacher_disagreement_score":0.02126827,"about_ca_system_score_codex":0.00067157665,"about_ca_system_score_gemma":0.00032930053,"threshold_uncertainty_score":0.04228896},"labels":[],"label_agreement":null},{"id":"W3097887418","doi":"10.1029/2020gl089800","title":"Detection and Assessment of a Large and Potentially Tsunamigenic Periglacial Landslide in Barry Arm, Alaska","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Forests; Selkirk College","funders":"Office of Polar Programs; Nuclear Safety and Security Commission; University of Minnesota; National Aeronautics and Space Administration; National Science Foundation","keywords":"Landslide; Geology; Glacier; Fjord; Debris; Physical geography; Submarine landslide; Geomorphology; Oceanography; Geography","score_opus":0.03258448456319972,"score_gpt":0.29930809797966057,"score_spread":0.26672361341646084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3097887418","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99880147,0.000105935826,0.00019870319,0.00002016471,0.0000044693847,0.00000557999,0.00012811233,0.00000782362,0.0007275996],"genre_scores_gemma":[0.9992638,0.00005195406,0.00030570207,0.000009742663,0.0000022858737,0.000003426735,0.0001545022,8.6518565e-7,0.00020772686],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999863,0.000020842019,0.00001691809,0.000037827296,0.000035507743,0.000025860656],"domain_scores_gemma":[0.99953294,0.000045414658,0.000095641684,0.000028159204,0.00017289327,0.000124895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005502688,0.0001851484,0.00013212435,0.0010413239,0.00094375055,0.00080352335,0.00021716807,0.0003801666,0.0006482679],"category_scores_gemma":[0.00062689226,0.00012453289,0.0001301683,0.00053153775,0.00030895718,0.00031107193,0.0006099275,0.0002348018,0.00018901918],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057428184,0.000023147453,0.9907733,0.000012720474,0.000015355137,0.0001803201,0.0004849187,0.0006523864,0.0035389757,0.000032770902,0.00008111387,0.0041474826],"study_design_scores_gemma":[0.0000021449373,0.000042057378,0.99505264,0.000021184818,0.000015789183,0.00006765565,0.002259395,0.0017657628,0.00034511116,0.00003569673,0.00038818916,0.0000043878695],"about_ca_topic_score_codex":0.085367434,"about_ca_topic_score_gemma":0.20503014,"teacher_disagreement_score":0.085367434,"about_ca_system_score_codex":0.00051048753,"about_ca_system_score_gemma":0.00060346373,"threshold_uncertainty_score":0.1697411},"labels":[],"label_agreement":null},{"id":"W3098143493","doi":"10.1029/2020gl089651","title":"Machine Learning‐Based Analysis of Geological Susceptibility to Induced Seismicity in the Montney Formation, Canada","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Hydraulic fracturing; Tectonics; Seismology; Thrust; Geotechnical engineering","score_opus":0.06437693706879997,"score_gpt":0.28536853564272036,"score_spread":0.22099159857392037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3098143493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99827516,0.000055179687,0.00037296728,0.00004525014,0.0000010775865,0.0000051791676,0.00077282346,0.00002179411,0.00045053594],"genre_scores_gemma":[0.9981281,0.000028685397,0.00029238488,0.0000054881907,0.0000010915,0.0000021843198,0.0012512723,0.000002982546,0.00028785822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99975044,0.00003223359,0.000014016122,0.000057559282,0.00007232825,0.000073354946],"domain_scores_gemma":[0.9987914,0.00027353247,0.0001932645,0.000055206485,0.0005386422,0.00014794296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004238407,0.00028969647,0.00019355834,0.0012786497,0.00063975825,0.00061393075,0.0005747062,0.00018815177,0.00082792214],"category_scores_gemma":[0.0021654333,0.00010120248,0.00026767238,0.0017011265,0.0004969692,0.00019395999,0.00035332388,0.00023915681,0.00014290758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016146468,0.000038969098,0.95334345,0.000020336814,0.00010244289,0.00011584115,0.00018636134,0.026823934,0.002306586,0.00024021188,0.0007175958,0.015942907],"study_design_scores_gemma":[0.0000079575775,0.000014549191,0.9388208,0.0000080892305,0.00001647602,0.000023914014,0.00037530393,0.059494246,0.00058110163,0.00008832525,0.00055562815,0.000013545543],"about_ca_topic_score_codex":0.97549075,"about_ca_topic_score_gemma":0.98131573,"teacher_disagreement_score":0.024509251,"about_ca_system_score_codex":0.0068760985,"about_ca_system_score_gemma":0.005459199,"threshold_uncertainty_score":0.049889803},"labels":[],"label_agreement":null},{"id":"W3098171041","doi":"10.1029/2020gl091028","title":"Atlantic Deep Water Formation Occurs Primarily in the Iceland Basin and Irminger Sea by Local Buoyancy Forcing","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":165,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Ocean gyre; Oceanography; Buoyancy; Geology; Shutdown of thermohaline circulation; Forcing (mathematics); Structural basin; Subtropics; North Atlantic Deep Water; Thermohaline circulation; Climatology; Paleontology; Fishery","score_opus":0.01846007409675277,"score_gpt":0.23622809110463328,"score_spread":0.2177680170078805,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3098171041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988977,0.000020929085,0.00004486071,0.0000095317955,0.0000012065249,0.0000019248762,0.00007822414,0.000009382068,0.0009362486],"genre_scores_gemma":[0.9995814,0.00001697277,0.00007058863,0.0000062368454,0.0000021593587,0.0000024065785,0.00012697703,0.0000021221051,0.00019110362],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995005,0.000007745247,0.000003563138,0.000017043649,0.0000061281344,0.00001553041],"domain_scores_gemma":[0.9998722,0.000011954485,0.000056063134,0.00001262585,0.000013636783,0.000033621185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010651984,0.00021010854,0.00020011475,0.00038515523,0.00025370825,0.00029518275,0.00014109617,0.0000934765,0.0013018642],"category_scores_gemma":[0.00021890958,0.000101572965,0.00018840453,0.00024216932,0.0002494384,0.00019343935,0.0003422812,0.00009725219,0.00018304515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017541394,0.000044490156,0.9528374,0.000027040676,0.00006433412,0.00023913947,0.00019163587,0.0017714533,0.03294507,0.00042104223,0.00058811536,0.010694811],"study_design_scores_gemma":[0.0000059390923,0.000018461451,0.9979122,0.0000030117496,0.000009945236,0.000021040916,0.000056789348,0.001199756,0.0005213327,0.000038162616,0.00021120439,0.0000022535912],"about_ca_topic_score_codex":0.013104783,"about_ca_topic_score_gemma":0.028199373,"teacher_disagreement_score":0.013104783,"about_ca_system_score_codex":0.00044189126,"about_ca_system_score_gemma":0.00030338007,"threshold_uncertainty_score":0.026057065},"labels":[],"label_agreement":null},{"id":"W3099147803","doi":"10.1029/2020gl089237","title":"Necessary Conditions for Warm Inflow Toward the Filchner Ice Shelf, Weddell Sea","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; Norges Forskningsråd; Sight Research UK","keywords":"Ice shelf; Geology; Weddell Sea Bottom Water; Oceanography; Sea ice; Continental shelf; Circumpolar deep water; Front (military); Antarctic Bottom Water; Shelf ice; Iceberg; Antarctic ice sheet; Cryosphere; Climatology; Water mass; North Atlantic Deep Water; Thermohaline circulation","score_opus":0.08840251636867608,"score_gpt":0.3108190384864906,"score_spread":0.22241652211781454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3099147803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991911,0.000022430942,0.00010191353,0.000023486227,0.0000027841354,0.00000409932,0.00015715146,0.0000071656004,0.00048994925],"genre_scores_gemma":[0.9995516,0.00001949301,0.00014560025,0.000008158696,0.000002794537,0.0000031940679,0.00018925943,0.0000011966749,0.000078723475],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991834,0.000009906216,0.00001253459,0.000016610558,0.000007618109,0.000034947185],"domain_scores_gemma":[0.99948835,0.00014458472,0.00016582126,0.000037126403,0.000056014254,0.00010803653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018272203,0.00020198418,0.00023490457,0.00046160893,0.0004278241,0.0008080189,0.00017165794,0.00025904857,0.002745877],"category_scores_gemma":[0.0010538237,0.00021173875,0.0001692209,0.00019475036,0.000298571,0.0004575634,0.0006011434,0.00021334007,0.00012510741],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054854335,0.000096908094,0.95232606,0.000099785575,0.0000560892,0.0007755291,0.0002005328,0.010273606,0.029769044,0.0011008612,0.00037571404,0.0043774643],"study_design_scores_gemma":[0.00005416686,0.00016149461,0.9853919,0.000024729841,0.000028971843,0.00012410322,0.00060246757,0.008687585,0.0040310672,0.0005729668,0.00030848794,0.000012016177],"about_ca_topic_score_codex":0.015231775,"about_ca_topic_score_gemma":0.025184236,"teacher_disagreement_score":0.015231775,"about_ca_system_score_codex":0.0006621134,"about_ca_system_score_gemma":0.0007141111,"threshold_uncertainty_score":0.030286252},"labels":[],"label_agreement":null},{"id":"W3099951005","doi":"10.1029/2020gl091453","title":"Quasi‐10‐Day Wave and Semidiurnal Tide Nonlinear Interactions During the Southern Hemispheric SSW 2019 Observed in the Northern Hemispheric Mesosphere","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Natural Science Foundation of China; National Science Foundation","keywords":"Mesosphere; Northern Hemisphere; Atmospheric sciences; Geology; Stratopause; Southern Hemisphere; Gravity wave; Sudden stratospheric warming; Physics; Climatology; Stratosphere; Geophysics; Astrophysics; Polar vortex; Gravitational wave","score_opus":0.03858571215963947,"score_gpt":0.2611251420807687,"score_spread":0.22253942992112924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3099951005","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993248,0.000021732012,0.0000536761,0.000012776383,0.0000037408665,0.0000015641408,0.0002823792,0.0000050622034,0.00029434427],"genre_scores_gemma":[0.9992079,0.0000138628975,0.000027960938,0.0000042224524,0.0000044429707,0.0000033983151,0.0006157743,0.0000013695126,0.000121144556],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993706,0.000009658168,0.0000046837567,0.000011058306,0.000017632909,0.000019943578],"domain_scores_gemma":[0.9997056,0.000059235783,0.00008304226,0.000019965317,0.000043237258,0.000088820205],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020009892,0.00017948552,0.0001669376,0.00056353776,0.0003119302,0.00028776814,0.00010450621,0.00021804801,0.0010680717],"category_scores_gemma":[0.00030312105,0.00011849552,0.0002358424,0.00044443124,0.00020685852,0.00018030133,0.00030346715,0.00022069199,0.00018573101],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042868042,0.00008634015,0.96467054,0.000025350475,0.00012664484,0.00021678832,0.00021575479,0.0012039053,0.026427701,0.00015829338,0.0006454733,0.0057944926],"study_design_scores_gemma":[0.0000020196555,0.000016777061,0.9989712,0.0000010136434,0.000006074893,0.000018324148,0.000038606653,0.0005870092,0.00023717631,0.00000956239,0.00011033816,0.0000017624791],"about_ca_topic_score_codex":0.007933407,"about_ca_topic_score_gemma":0.020839889,"teacher_disagreement_score":0.007933407,"about_ca_system_score_codex":0.000257347,"about_ca_system_score_gemma":0.00016627104,"threshold_uncertainty_score":0.015774488},"labels":[],"label_agreement":null},{"id":"W3100067678","doi":"10.1029/2020gl090930","title":"Aseismic Deformation During the 2014 <i>M</i><sub><i>w</i></sub> 5.2 Karonga Earthquake, Malawi, From Satellite Interferometry and Earthquake Source Mechanisms","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Tulane University; National Science Foundation","keywords":"Geology; Seismology; Aftershock; Rift; Slip (aerodynamics); Deformation (meteorology); Paleoseismology; Tectonics; Crust; Interferometric synthetic aperture radar; Geophysics; Synthetic aperture radar","score_opus":0.02273814373486951,"score_gpt":0.23004378349462629,"score_spread":0.20730563975975677,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3100067678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991849,0.00006190792,0.00009985579,0.00002954838,0.0000016929729,0.0000030717088,0.00026802145,0.0000036941412,0.00034738047],"genre_scores_gemma":[0.99928814,0.00007835449,0.00010800532,0.000007574822,0.0000040047407,0.0000020336363,0.0003768478,0.0000012083833,0.00013378609],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999349,0.000009669398,0.0000064704345,0.000014614524,0.000010916032,0.000023370765],"domain_scores_gemma":[0.99981385,0.000023233806,0.00008340024,0.000011198743,0.000036395482,0.000031963278],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019046488,0.0002690089,0.0001342375,0.00072877685,0.00020698023,0.00051589526,0.00018615297,0.00020740872,0.00058548356],"category_scores_gemma":[0.00044061278,0.0001635751,0.00019060187,0.000829215,0.00031644627,0.00033077778,0.00044165188,0.00017441224,0.00010822971],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001307068,0.000036449983,0.9698108,0.00007731672,0.00008892805,0.00045348395,0.0010965117,0.0022009036,0.012476556,0.00022637585,0.0004615309,0.012940455],"study_design_scores_gemma":[0.0000028059196,0.000010042417,0.99699664,0.000011473689,0.000017865703,0.000045745484,0.00027515093,0.0019723913,0.0003687044,0.000022258519,0.00027340362,0.000003574422],"about_ca_topic_score_codex":0.04664582,"about_ca_topic_score_gemma":0.10808136,"teacher_disagreement_score":0.04664582,"about_ca_system_score_codex":0.00054765254,"about_ca_system_score_gemma":0.00047052067,"threshold_uncertainty_score":0.09274864},"labels":[],"label_agreement":null},{"id":"W3100459182","doi":"10.1029/2020gl089533","title":"Zonal Asymmetry of the QBO Temperature Signal in the Tropical Tropopause Region","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Saskatchewan","funders":"","keywords":"Tropopause; Quasi-biennial oscillation; Climatology; Stratosphere; Atmospheric sciences; Boreal; Convection; Environmental science; Magnitude (astronomy); Geology; Physics; Meteorology; Astrophysics","score_opus":0.03518373838900197,"score_gpt":0.26707500104500537,"score_spread":0.2318912626560034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3100459182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981711,0.00008292033,0.00030917337,0.00003832433,0.000009465136,0.0000034106151,0.0003515584,0.000026528367,0.0010074056],"genre_scores_gemma":[0.9995436,0.000026789208,0.00009657779,0.000010378468,0.000008273843,0.000002453806,0.00017971048,0.0000047873964,0.00012739797],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999639,0.0000046385944,0.0000021080725,0.000009428339,0.000007944758,0.000011900137],"domain_scores_gemma":[0.99978155,0.000037895632,0.000080972706,0.00001115134,0.00004869451,0.000039705417],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011802708,0.000106954554,0.00010832139,0.00040024004,0.0001302762,0.00027066746,0.00009140427,0.000116828734,0.0016754869],"category_scores_gemma":[0.00037165039,0.00009625493,0.00010204235,0.00023288993,0.00013970253,0.00017636182,0.00017307664,0.00013805319,0.00016900369],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007345318,0.00006380277,0.46486077,0.000096674325,0.00012366296,0.00033058217,0.00025114566,0.0016269396,0.51880103,0.00036631184,0.0010032259,0.011741168],"study_design_scores_gemma":[0.000011812174,0.00003574746,0.9949844,0.0000033731894,0.000009170381,0.000063018306,0.000044769848,0.0016541758,0.0028490766,0.000050014347,0.00028979353,0.0000047244985],"about_ca_topic_score_codex":0.0029005406,"about_ca_topic_score_gemma":0.0035192606,"teacher_disagreement_score":0.0029005406,"about_ca_system_score_codex":0.00012371008,"about_ca_system_score_gemma":0.000103026454,"threshold_uncertainty_score":0.005767286},"labels":[],"label_agreement":null},{"id":"W3102097954","doi":"10.1029/2020gl089870","title":"Out of the Ice Age: Megatides of the Arctic Ocean and the Bølling‐Ållerød, Younger Dryas Transition","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Younger Dryas; Deglaciation; Geology; Ice sheet; Oceanography; Arctic ice pack; Abrupt climate change; Sea ice; Climatology; Northern Hemisphere; Cryosphere; Last Glacial Maximum; Arctic; Glacial period; Climate change; Global warming; Holocene; Effects of global warming; Geomorphology","score_opus":0.03970286005816025,"score_gpt":0.2708079332016212,"score_spread":0.23110507314346096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3102097954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959765,0.0006167942,0.00004419104,0.0007504246,0.00003517442,0.0000012210093,0.00017643323,0.000002268645,0.0023970022],"genre_scores_gemma":[0.9993824,0.00020132646,0.000023369348,0.000055006374,0.000029487019,0.0000010424735,0.00008395489,0.0000015924592,0.00022170677],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999088,0.0000126978475,0.000005935864,0.00002395372,0.000014649907,0.00003394706],"domain_scores_gemma":[0.99958867,0.000051268078,0.00018006873,0.000011861596,0.000036708683,0.00013143565],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036525613,0.00008054932,0.00012199694,0.0003942748,0.00065140636,0.0009515483,0.00014649874,0.0003262146,0.002113836],"category_scores_gemma":[0.0006050325,0.00005478589,0.00009284664,0.0003714766,0.0005069371,0.00042754077,0.0007902175,0.00036716665,0.00011716175],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005381461,0.000086151675,0.96281075,0.00004842285,0.000054234846,0.000830225,0.0030285448,0.00034180953,0.0034713978,0.0050763777,0.0025479628,0.02116602],"study_design_scores_gemma":[0.000005877239,0.000020707956,0.9933936,0.000015841179,0.0000067738342,0.00010495698,0.0016899303,0.00016234568,0.00017928432,0.00052841305,0.0038888415,0.000003486126],"about_ca_topic_score_codex":0.012938206,"about_ca_topic_score_gemma":0.044777945,"teacher_disagreement_score":0.012938206,"about_ca_system_score_codex":0.0006470445,"about_ca_system_score_gemma":0.00040615065,"threshold_uncertainty_score":0.025725782},"labels":[],"label_agreement":null},{"id":"W3102800745","doi":"10.1029/2020gl088752","title":"Active Sediment Generation on Coral Reef Flats Contributes to Recent Reef Island Expansion","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"University of Auckland; Australian Institute of Nuclear Science and Engineering; Asia-Pacific Network for Global Change Research","keywords":"Atoll; Oceanography; Radiometric dating; Reef; Coral reef; Geology; Sediment; Aerial imagery; Remote sensing; Geomorphology","score_opus":0.07842754200928219,"score_gpt":0.31775746863735005,"score_spread":0.23932992662806785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3102800745","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994628,0.000066601555,0.00001840892,0.000027289749,8.0649e-7,0.0000014186787,0.000051187464,0.0000022611046,0.00036922432],"genre_scores_gemma":[0.9997954,0.00003675418,0.000018670164,0.0000030826739,0.0000020113323,6.073011e-7,0.000046196896,9.0349715e-7,0.00009642015],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998554,0.000031259304,0.000012698767,0.000037752692,0.000025339144,0.00003741042],"domain_scores_gemma":[0.9979538,0.00029718646,0.0010098419,0.00012223067,0.00029101342,0.00032585114],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003923209,0.00015346623,0.0001444406,0.0009618056,0.00031299307,0.0008971525,0.00034717846,0.00021437286,0.0024441378],"category_scores_gemma":[0.0023135033,0.00014632619,0.00017156843,0.00074098184,0.0004861678,0.0003199595,0.0007737292,0.0002861982,0.00020608323],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000028756624,0.000010515079,0.9963995,0.000009626615,0.000029438568,0.000099844256,0.0001717039,0.0001137353,0.0008026886,0.00003092983,0.00004034896,0.0022627823],"study_design_scores_gemma":[1.8653391e-7,0.0000035967887,0.9997092,0.000001299815,0.0000024995954,0.000014066871,0.00010553837,0.000098925,0.00001889928,0.0000052785285,0.000039888208,5.5465125e-7],"about_ca_topic_score_codex":0.03917897,"about_ca_topic_score_gemma":0.07071401,"teacher_disagreement_score":0.03917897,"about_ca_system_score_codex":0.0005039645,"about_ca_system_score_gemma":0.00032989535,"threshold_uncertainty_score":0.07790184},"labels":[],"label_agreement":null},{"id":"W3103972563","doi":"10.1029/2020gl089672","title":"The Morphometry of Impact Craters on Bennu","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; York University","funders":"Canadian Space Agency; Centre National d’Etudes Spatiales; European Commission; National Aeronautics and Space Administration","keywords":"Impact crater; Geology; Asteroid; Ejecta; Regolith; Impact structure; Astrobiology; Geomorphology; Physics; Astronomy","score_opus":0.0392373076078299,"score_gpt":0.3239255203437609,"score_spread":0.284688212735931,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3103972563","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99847823,0.00007469987,0.00009489014,0.0000062544054,0.0000013934479,0.0000032613964,0.00018143181,0.000012394368,0.0011474304],"genre_scores_gemma":[0.9990502,0.000028031624,0.00024836668,0.0000025797126,6.258952e-7,0.000002079359,0.00029254926,0.0000040599125,0.0003714492],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991274,0.000007731969,0.0000033523024,0.000028307439,0.000026312486,0.00002154143],"domain_scores_gemma":[0.99985564,0.000027386399,0.000034374163,0.000014508178,0.00003995771,0.000028248409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000089986956,0.0001468897,0.00016876328,0.0013283354,0.00036603503,0.0004759491,0.00015360325,0.00014123549,0.0015548815],"category_scores_gemma":[0.00029843493,0.0001350386,0.0000874271,0.0007353069,0.00026533424,0.00016609389,0.00047161587,0.00012922542,0.00018730116],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036381092,0.00003202832,0.91466033,0.000056923545,0.000051730418,0.00026383655,0.0008504615,0.0030676662,0.04069362,0.0001805149,0.00044091267,0.03933807],"study_design_scores_gemma":[0.0000014091155,0.000008941381,0.9968913,0.0000051353127,0.0000029958242,0.00009751531,0.00021534163,0.0011113179,0.0009560627,0.000008900502,0.00069781166,0.0000033315441],"about_ca_topic_score_codex":0.049379643,"about_ca_topic_score_gemma":0.08699947,"teacher_disagreement_score":0.049379643,"about_ca_system_score_codex":0.0005600773,"about_ca_system_score_gemma":0.00013594763,"threshold_uncertainty_score":0.09818447},"labels":[],"label_agreement":null},{"id":"W3105203633","doi":"10.1029/2020gl089764","title":"A New Mass Flux Correction Procedure for Vertically Integrated Energy Transport by Constraining Mass, Energy, and Water Budgets","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"York University; New York University Abu Dhabi","keywords":"Spurious relationship; Barotropic fluid; Mass flux; Energy transport; Flux (metallurgy); Environmental science; Energy (signal processing); Water mass; Energy flux; Mass transport; Energy budget; Energy transformation; Zonal and meridional; Circulation (fluid dynamics); Mechanics; Physics; Meteorology; Climatology; Atmospheric sciences; Geology; Materials science; Mathematics; Thermodynamics; Statistics","score_opus":0.01603251983879672,"score_gpt":0.22926429232841367,"score_spread":0.21323177248961694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3105203633","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.021693619,0.00010984332,0.97613996,0.00006983898,0.00012364311,0.000044691064,0.00008759963,0.0010611197,0.0006696838],"genre_scores_gemma":[0.12874264,0.00011051446,0.8680821,0.000042670075,0.00007962261,0.00007439713,0.00019588646,0.00028584167,0.0023863774],"study_design_codex":"design_other","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997962,0.000038465736,0.000011643756,0.0000537048,0.00008494185,0.000015025894],"domain_scores_gemma":[0.9997019,0.00007560969,0.000050284412,0.00003998458,0.00012291125,0.00000929433],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005176387,0.0006039686,0.00034637726,0.00075455377,0.00041036378,0.0004120517,0.00076273753,0.00043590268,0.0013902142],"category_scores_gemma":[0.0012603591,0.0002720161,0.0004937337,0.0005048999,0.0002555051,0.0005774791,0.00041704177,0.0006882197,0.00033875927],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001523778,0.00012558809,0.00831363,0.00019197293,0.00024337578,0.00022556262,0.00018880209,0.17958848,0.12893425,0.015298552,0.0041690487,0.6625683],"study_design_scores_gemma":[0.000041472365,0.00004600543,0.004120203,0.000013029862,0.000034537836,0.00010039764,0.000014539965,0.9650362,0.020249965,0.0019285439,0.008376889,0.00003820446],"about_ca_topic_score_codex":0.008955268,"about_ca_topic_score_gemma":0.010505663,"teacher_disagreement_score":0.008955268,"about_ca_system_score_codex":0.00032909494,"about_ca_system_score_gemma":0.00091103255,"threshold_uncertainty_score":0.017806292},"labels":[],"label_agreement":null},{"id":"W3110725524","doi":"10.1029/2020gl091236","title":"Observational Constraints on Warm Cloud Microphysical Processes Using Machine Learning and Optimization Techniques","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal","funders":"U.S. Department of Energy","keywords":"Drizzle; Accretion (finance); Environmental science; Cloud computing; Liquid water content; Meteorology; Cloud physics; Representation (politics); Atmospheric sciences; Computer science; Astrophysics; Physics","score_opus":0.05776324653679146,"score_gpt":0.31339839167107086,"score_spread":0.25563514513427943,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3110725524","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.21677007,0.0010114366,0.7749742,0.0009892399,0.000053526146,0.000048530874,0.0015613092,0.0007278469,0.00386385],"genre_scores_gemma":[0.930463,0.0005566063,0.06662323,0.0001504329,0.00014278713,0.000080679805,0.0013370333,0.00018915356,0.00045714245],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99947006,0.0002258089,0.000042600754,0.000140927,0.00007078798,0.000049839535],"domain_scores_gemma":[0.99588627,0.0025846537,0.00070841936,0.000529863,0.00018828869,0.0001025535],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002013975,0.0009344549,0.0007898314,0.0007910746,0.00045796638,0.0013726824,0.0012943484,0.000670027,0.0011293547],"category_scores_gemma":[0.008981115,0.00051389035,0.00082612224,0.0007511564,0.00076862396,0.0024002518,0.0010698936,0.0017811727,0.00018665276],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021294989,0.000024218729,0.0085244,0.000042053925,0.000074075106,0.000031498585,0.00002167653,0.967657,0.0011756438,0.010882798,0.00034416254,0.011201127],"study_design_scores_gemma":[0.000004335995,0.000003273287,0.0018990177,0.000007839598,0.0000046652917,0.0000051113025,0.000003678834,0.9906522,0.0002991262,0.006791344,0.000321053,0.000008492357],"about_ca_topic_score_codex":0.011575557,"about_ca_topic_score_gemma":0.009458266,"teacher_disagreement_score":0.011575557,"about_ca_system_score_codex":0.00088344776,"about_ca_system_score_gemma":0.0009913836,"threshold_uncertainty_score":0.023016334},"labels":[],"label_agreement":null},{"id":"W3111895545","doi":"10.1029/2020gl090864","title":"Multisatellite Imaging of a Gas Well Blowout Enables Quantification of Total Methane Emissions","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oil, Gas, and Environmental Issues","field":"Energy","cited_by":110,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"GHGSat (Canada)","funders":"","keywords":"Methane; Environmental science; Satellite; Methane emissions; Atmospheric methane; Greenhouse gas; Atmospheric sciences; Natural gas; Meteorology; Remote sensing; Geology; Physics","score_opus":0.04960589840903299,"score_gpt":0.3167241375293945,"score_spread":0.2671182391203615,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111895545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936767,0.00011494466,0.0030536966,0.000058383484,0.000011257698,0.0000062323124,0.00082218373,0.00013580354,0.0021208108],"genre_scores_gemma":[0.9931195,0.000055336488,0.0054710163,0.00003124768,0.000009568334,0.0000052539863,0.0008249411,0.000026884416,0.00045632478],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.0000036413123,0.0000013990327,0.000021886142,0.0000134668135,0.000012581189],"domain_scores_gemma":[0.99991274,0.000012886966,0.00002409849,0.000010604412,0.000024070443,0.000015603016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014008832,0.00020936264,0.00009910235,0.000558386,0.00021717616,0.00028718408,0.00017366813,0.00024851403,0.0010089778],"category_scores_gemma":[0.00012152844,0.0001260979,0.00017695711,0.00035399466,0.00013965604,0.00026562178,0.00027419627,0.0002470305,0.0001417744],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003678228,0.00016984734,0.19173208,0.00007121131,0.00013673112,0.00030450718,0.00025540913,0.011030056,0.76526064,0.00036016383,0.0012436688,0.029067786],"study_design_scores_gemma":[0.000021260765,0.00019405347,0.86007065,0.000023769115,0.00009547015,0.00026516197,0.00048890995,0.051960766,0.08311307,0.000335839,0.0033899602,0.000041037907],"about_ca_topic_score_codex":0.007540009,"about_ca_topic_score_gemma":0.021649823,"teacher_disagreement_score":0.007540009,"about_ca_system_score_codex":0.00023054893,"about_ca_system_score_gemma":0.00014226598,"threshold_uncertainty_score":0.014992237},"labels":[],"label_agreement":null},{"id":"W3111929460","doi":"10.1029/2020gl090632","title":"Detection of Hertz Frequency Multiharmonic Field Line Resonances at Low‐L (<i>L</i> = 1.1–1.5) During Van Allen Probe Perigee Passes","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Physics; Field line; Electric field; Harmonics; Ionosphere; Field (mathematics); Computational physics; Line (geometry); Van Allen Probes; Plasma; Atomic physics; Geophysics; Magnetosphere; Van Allen radiation belt; Quantum mechanics; Geometry","score_opus":0.018142843703308306,"score_gpt":0.2707878621288005,"score_spread":0.2526450184254922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3111929460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988172,0.000019745263,0.00035739993,0.000013385821,0.0000015041811,0.000002131049,0.000052428757,0.000019935327,0.0007161676],"genre_scores_gemma":[0.9996087,0.0000070305655,0.00015121429,0.0000051370926,0.0000013873225,0.0000023117866,0.000054271426,0.0000037149982,0.00016622647],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.000004807611,0.0000010631028,0.000011761783,0.000009855512,0.00001285297],"domain_scores_gemma":[0.9998665,0.000033611825,0.000039056195,0.00001177403,0.000021532234,0.000027432074],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010998013,0.0001150371,0.0001007432,0.00034051214,0.00020958853,0.00021460436,0.00020545756,0.00024997478,0.00073640153],"category_scores_gemma":[0.00027121976,0.00010820185,0.00007318313,0.0001359899,0.00015550417,0.00017928387,0.00022205296,0.00020172492,0.0001451418],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008137698,0.00009427224,0.28378648,0.000052419036,0.000054666365,0.0005359612,0.0014722068,0.00096002285,0.6905774,0.00029126092,0.0005578592,0.02080375],"study_design_scores_gemma":[0.000013757342,0.00015535319,0.97587174,0.000008021649,0.000013765478,0.00015239765,0.0002924672,0.0019341541,0.020533198,0.000072891366,0.0009403948,0.000011904193],"about_ca_topic_score_codex":0.0019659353,"about_ca_topic_score_gemma":0.003759164,"teacher_disagreement_score":0.0019659353,"about_ca_system_score_codex":0.00017386812,"about_ca_system_score_gemma":0.00004355598,"threshold_uncertainty_score":0.003908992},"labels":[],"label_agreement":null},{"id":"W3112202407","doi":"10.1029/2020gl091613","title":"On the Origin of Donut‐Shaped Electron Distributions Within Magnetic Cavities","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Electron; Physics; Pitch angle; Magnetic field; Plasma; Betatron; Atomic physics; Computational physics; Anisotropy; Optics; Geophysics; Nuclear physics","score_opus":0.022078762122918854,"score_gpt":0.2814707674056299,"score_spread":0.259392005282711,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112202407","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9202827,0.00044220474,0.071335316,0.00021319908,0.00004507774,0.000023356002,0.00004812653,0.00011961427,0.007490419],"genre_scores_gemma":[0.99771464,0.000062744446,0.0016965942,0.000015919446,0.0000047969916,0.000007322579,0.0000077508275,0.0000098981845,0.00048043195],"study_design_codex":"theoretical_or_conceptual","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994695,0.000012093606,0.0000010042806,0.00001477085,0.000005963377,0.000019234714],"domain_scores_gemma":[0.99971336,0.00011127215,0.000044079618,0.00004028642,0.000039959534,0.00005100122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022139253,0.00018211447,0.00023431315,0.0002823884,0.00040907017,0.00057747384,0.00052487344,0.00037884316,0.0008994648],"category_scores_gemma":[0.0010363755,0.00016366309,0.00014865368,0.00011733192,0.0010104905,0.0008074636,0.000550662,0.0002939011,0.00012849872],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005101721,0.00008434928,0.018477801,0.00012772353,0.000033063643,0.002228103,0.0011860771,0.20890531,0.11894681,0.6303196,0.0015080867,0.017672902],"study_design_scores_gemma":[0.000059734317,0.00010128303,0.008611046,0.000025635509,0.000009661615,0.0008193039,0.0002468746,0.8754433,0.015006812,0.09732888,0.0023009751,0.000046467172],"about_ca_topic_score_codex":0.00059655623,"about_ca_topic_score_gemma":0.00032040058,"teacher_disagreement_score":0.0008994648,"about_ca_system_score_codex":0.00044649513,"about_ca_system_score_gemma":0.00014738567,"threshold_uncertainty_score":0.003239572},"labels":[],"label_agreement":null},{"id":"W3112714077","doi":"10.1029/2020gl091430","title":"Three Western Pacific Typhoons Strengthened Fire Weather in the Recent Northwest U.S. Conflagration","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Biological and Environmental Research; Strategic Environmental Research and Development Program; Office of Science; U.S. Department of Energy","keywords":"Typhoon; Extratropical cyclone; Climatology; Trough (economics); Ridge; Atmospheric circulation; Pacific ocean; Tropical cyclone; Environmental science; Geology; Oceanography; Geography; Meteorology","score_opus":0.06080045708587332,"score_gpt":0.28536747303473675,"score_spread":0.22456701594886344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3112714077","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987087,0.000053219566,0.000027189075,0.00015569471,0.000010193133,0.0000044063027,0.00021834175,0.000002515227,0.00081971096],"genre_scores_gemma":[0.9994061,0.00007676505,0.000043311993,0.000041190993,0.000008449364,0.000002349015,0.0002591367,0.0000010749939,0.00016154879],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999443,0.000006315485,0.0000060048046,0.000012572076,0.000013253444,0.00001756982],"domain_scores_gemma":[0.99960726,0.000029647856,0.00012767599,0.000018414252,0.00010295662,0.00011406087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022635104,0.00012808962,0.00008507689,0.000453089,0.00059998716,0.0005770791,0.00011429162,0.00017487351,0.0007051297],"category_scores_gemma":[0.0005201939,0.00007303227,0.00008392078,0.000590624,0.000285959,0.00030743045,0.00046834012,0.00040845835,0.00005131673],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006247801,0.000032657103,0.99044496,0.0000107751075,0.000019936117,0.00019327292,0.00067592505,0.00011140373,0.00076492043,0.000059157897,0.0006885771,0.0069358633],"study_design_scores_gemma":[0.0000015354141,0.000012297067,0.9978326,0.000005480604,0.0000051692937,0.00003523557,0.001260411,0.00014607776,0.00012342037,0.000014213056,0.0005616944,0.0000018714514],"about_ca_topic_score_codex":0.14420839,"about_ca_topic_score_gemma":0.37413496,"teacher_disagreement_score":0.14420839,"about_ca_system_score_codex":0.0008847193,"about_ca_system_score_gemma":0.0007583336,"threshold_uncertainty_score":0.28673798},"labels":[],"label_agreement":null},{"id":"W3113225952","doi":"10.1029/2020gl091108","title":"Forecasting the Permanent Loss of Lake Ice in the Northern Hemisphere Within the 21st Century","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"York University","keywords":"Northern Hemisphere; Southern Hemisphere; Physical geography; Cryosphere; Oceanography; Greenhouse gas; Environmental science; Climatology; Sea ice; Geology; Geography","score_opus":0.03448728812303051,"score_gpt":0.2532792445665372,"score_spread":0.2187919564435067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113225952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99537104,0.00017892565,0.00047125955,0.00033755158,0.000013097005,0.000005009291,0.0024262865,0.000019928995,0.0011770006],"genre_scores_gemma":[0.9981694,0.00008295768,0.00023049932,0.000017811039,0.000013277648,0.000003319149,0.0012880268,0.0000028500485,0.00019173266],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998965,0.000016613525,0.0000073411265,0.00002580102,0.000022631397,0.000031051473],"domain_scores_gemma":[0.9995338,0.000052614483,0.00016167408,0.00001746408,0.00013962467,0.000094771036],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036859594,0.00019784739,0.0001660331,0.00070976105,0.00032396356,0.00071844214,0.0002205885,0.00033545293,0.0009716321],"category_scores_gemma":[0.0010968497,0.000101056095,0.00030325633,0.00074497575,0.00018298268,0.00048428256,0.0005008872,0.00027517258,0.0001930721],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055568406,0.0000127014,0.98329794,0.000014233457,0.000057682617,0.00008095663,0.00010992979,0.008579249,0.00042218753,0.00017235192,0.0017574322,0.0054396754],"study_design_scores_gemma":[0.0000055178843,0.000018768314,0.962157,0.000014312386,0.000023667995,0.000031830183,0.0006707057,0.03486233,0.00019941562,0.00031943538,0.0016895616,0.0000073677284],"about_ca_topic_score_codex":0.095500015,"about_ca_topic_score_gemma":0.12180852,"teacher_disagreement_score":0.095500015,"about_ca_system_score_codex":0.00087667187,"about_ca_system_score_gemma":0.000529668,"threshold_uncertainty_score":0.1898883},"labels":[],"label_agreement":null},{"id":"W3113341124","doi":"10.1029/2020gl089455","title":"Roles of Shear and Convection in Driving Mixing in the Ocean","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Rimouski","funders":"","keywords":"Convection; Mixing (physics); Convective mixing; Richardson number; Shear (geology); Thermal diffusivity; Mechanics; Geology; Shear flow; Meteorology; Physics; Thermodynamics; Turbulence; Petrology","score_opus":0.025298609723597553,"score_gpt":0.25934074973616134,"score_spread":0.2340421400125638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3113341124","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9881136,0.0003045305,0.0069709616,0.00022858537,0.000025257046,0.000018882174,0.000072628594,0.00006355775,0.0042020236],"genre_scores_gemma":[0.9992285,0.000076271,0.000546504,0.00001139965,0.0000074217364,0.000006844857,0.000015343403,0.0000048913325,0.00010275392],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999068,0.000027808008,0.000009195881,0.000022168108,0.000016401624,0.000017584784],"domain_scores_gemma":[0.9997379,0.0000986423,0.00006859273,0.000021074507,0.00003626744,0.000037504073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00040616054,0.00043646918,0.0002867666,0.00038300888,0.00042042648,0.0010926885,0.00023356658,0.00032168304,0.0005682443],"category_scores_gemma":[0.001120594,0.0002922322,0.00037587748,0.0001750405,0.00077201164,0.0007364984,0.00064940756,0.00046525564,0.00010412433],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006178952,0.0002249224,0.078437544,0.00023900115,0.00012571244,0.00046883937,0.00024040081,0.40169758,0.4735088,0.025100019,0.0004976117,0.018841647],"study_design_scores_gemma":[0.00012239101,0.00018197672,0.01882576,0.000025650901,0.000053343323,0.00006084108,0.00010376585,0.9380708,0.036919914,0.0050124777,0.0005836081,0.00003944386],"about_ca_topic_score_codex":0.00507165,"about_ca_topic_score_gemma":0.0019809222,"teacher_disagreement_score":0.00507165,"about_ca_system_score_codex":0.00084945036,"about_ca_system_score_gemma":0.00067559077,"threshold_uncertainty_score":0.010084212},"labels":[],"label_agreement":null},{"id":"W3115801026","doi":"10.1029/2020gl090461","title":"Deep Meteoric Water Circulation in Earth's Crust","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":52,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Geology; Meteoric water; Crust; Sedimentary rock; Groundwater; Subsurface flow; Geochemistry; Earth science","score_opus":0.02919573883142609,"score_gpt":0.2657357230311436,"score_spread":0.23653998419971753,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3115801026","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99675566,0.0008262783,0.00006677632,0.00006320736,0.0000035828432,0.0000010258324,0.00034000672,0.0000095472715,0.0019339118],"genre_scores_gemma":[0.99960107,0.0001513941,0.000030200088,0.000006838586,0.0000018828437,2.8194174e-7,0.000087476656,0.0000011057493,0.00011964466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999808,0.0000017764111,0.0000012927105,0.0000062998342,0.000003865988,0.000005992329],"domain_scores_gemma":[0.9999161,0.000007720957,0.00003045787,0.0000041411263,0.00001633115,0.000025237558],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000060124254,0.00008924247,0.00009048647,0.00042175376,0.00013514655,0.00043084184,0.00008788357,0.00012450428,0.0008918008],"category_scores_gemma":[0.00020574279,0.00006062174,0.00005660676,0.00047490202,0.00020048545,0.00027248956,0.00028504088,0.00012224184,0.000116317955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016623709,0.000021855589,0.9055912,0.00011507815,0.000082531,0.00033407976,0.00052386225,0.0030486833,0.05098582,0.0015042437,0.0008496529,0.036776766],"study_design_scores_gemma":[0.0000051017046,0.000026909653,0.9962478,0.000009515454,0.0000102960985,0.00005887325,0.00014195283,0.0006216586,0.00068353955,0.00038225017,0.0018077854,0.0000043249606],"about_ca_topic_score_codex":0.018151619,"about_ca_topic_score_gemma":0.0138286725,"teacher_disagreement_score":0.018151619,"about_ca_system_score_codex":0.00044643471,"about_ca_system_score_gemma":0.00020002834,"threshold_uncertainty_score":0.036091924},"labels":[],"label_agreement":null},{"id":"W3116674105","doi":"10.1029/2020gl091374","title":"A New Thermal Categorization of Ice‐Covered Lakes","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":68,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; Ministry of Natural Resources and Forestry; Queen's University; Ministry of the Environment, Conservation and Parks; University of Guelph; The Scarborough Hospital; Ministry of Environment; Environment and Climate Change Canada; Fisheries and Oceans Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Stratification (seeds); Thermal stratification; Geology; Water column; Trophic level; Climatology; Environmental science; Physical geography; Atmospheric sciences; Oceanography; Geography; Paleontology","score_opus":0.04661622446000701,"score_gpt":0.2873679633696221,"score_spread":0.2407517389096151,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3116674105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9751346,0.00023187298,0.009188241,0.00012703506,0.0000216167,0.000043275497,0.00058677484,0.00013220523,0.014534402],"genre_scores_gemma":[0.9952101,0.00004793914,0.0036452964,0.00002417025,0.00001152926,0.000019123067,0.000327101,0.000013070134,0.0007017696],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998945,0.000019916919,0.000012378992,0.000019527146,0.000024947012,0.00002876739],"domain_scores_gemma":[0.9997222,0.000045279186,0.000057934507,0.000021103639,0.00011667364,0.000036772173],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016687221,0.00019893695,0.00010959529,0.0012840708,0.00037861225,0.00083656417,0.00025638577,0.00016051091,0.0018738911],"category_scores_gemma":[0.000596272,0.00010563174,0.00020681412,0.0006193742,0.00052825554,0.00057203765,0.00055825827,0.00016286633,0.0002491869],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00054821384,0.00007452302,0.8397129,0.00016041008,0.00012574675,0.0004313547,0.0035288772,0.01830438,0.035791896,0.021331845,0.0043885224,0.07560126],"study_design_scores_gemma":[0.00004198902,0.00016100335,0.87424064,0.000074445736,0.00009464737,0.0005982902,0.003027946,0.091733895,0.004882916,0.012493691,0.012589819,0.000060763738],"about_ca_topic_score_codex":0.00867624,"about_ca_topic_score_gemma":0.0105981985,"teacher_disagreement_score":0.00867624,"about_ca_system_score_codex":0.0004787103,"about_ca_system_score_gemma":0.0003121411,"threshold_uncertainty_score":0.017251432},"labels":[],"label_agreement":null},{"id":"W3117896600","doi":"10.1029/2020gl089895","title":"Challenges on Mercury's Interior Structure Posed by the New Measurements of its Obliquity and Tides","year":2020,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Mantle (geology); Mercury (programming language); Geology; Geophysics; Moment of inertia; Inner core; Amplitude; Geodesy; Physics; Classical mechanics","score_opus":0.11872738018662046,"score_gpt":0.3235319778211653,"score_spread":0.2048045976345448,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3117896600","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9707544,0.00013017112,0.019619156,0.0006866676,0.000016328197,0.000008991714,0.00029708474,0.00023839148,0.008248904],"genre_scores_gemma":[0.9974396,0.000033766843,0.0023012124,0.00001873656,0.000008253254,0.0000068809923,0.00005224203,0.000037019185,0.00010221637],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980205,0.000069311995,0.0000059355925,0.00003113827,0.000060887447,0.000030628747],"domain_scores_gemma":[0.99937445,0.00025629328,0.00009176635,0.00016416197,0.00005406243,0.000059309183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056067493,0.0004017073,0.0005964342,0.00021417325,0.0005883581,0.00075811427,0.0009633757,0.0004907486,0.0009949522],"category_scores_gemma":[0.003035361,0.0003402749,0.0003878721,0.00029558095,0.000881641,0.0006714996,0.0009697474,0.00074412394,0.00015853596],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017255938,0.00004064104,0.0531555,0.00006993458,0.00009663303,0.00024742563,0.00031049846,0.90282613,0.012265248,0.021818012,0.00063956634,0.008357783],"study_design_scores_gemma":[0.00007579824,0.00009798494,0.01866618,0.000019218369,0.00003840532,0.000107068554,0.0002441541,0.9634458,0.0034259828,0.012442155,0.0013924324,0.000044802757],"about_ca_topic_score_codex":0.014397098,"about_ca_topic_score_gemma":0.009467447,"teacher_disagreement_score":0.014397098,"about_ca_system_score_codex":0.0006806941,"about_ca_system_score_gemma":0.0007239735,"threshold_uncertainty_score":0.028626561},"labels":[],"label_agreement":null},{"id":"W3118985795","doi":"10.1029/2020gl089673","title":"Periodicity Analysis of Earthquake Occurrence and Hypocenter Depth Near Parkfield, California, 1994–2002 Versus 2006–2014","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"U.S. Geological Survey; Southern California Earthquake Center","keywords":"Hypocenter; Seismology; Geology; Trough (economics); Foreshock; Induced seismicity; Aftershock","score_opus":0.04489871911694645,"score_gpt":0.2925265264584575,"score_spread":0.24762780734151105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3118985795","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99661106,0.00004903991,0.00010144991,0.000024909214,0.0000056371778,0.000005195892,0.0023476945,0.00001658998,0.0008384082],"genre_scores_gemma":[0.99633396,0.000034013443,0.00011318627,0.00000729337,0.000009555007,0.000007545791,0.0031483974,0.0000054007214,0.00034062963],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997868,0.000019376314,0.00002519505,0.00007517055,0.000054105065,0.000039409715],"domain_scores_gemma":[0.9983083,0.00020568144,0.00077796116,0.00010377277,0.00039650564,0.00020780391],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004429209,0.00015281174,0.00018386486,0.0014897855,0.0003084595,0.00059395324,0.00029776478,0.0001889644,0.0014323919],"category_scores_gemma":[0.0015852336,0.00015217415,0.0002450964,0.0013732754,0.0001664995,0.000313915,0.00031821092,0.00024997647,0.00020882675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010581192,0.00002372612,0.9953127,0.000013096562,0.000051980605,0.00002857204,0.00009954624,0.000619153,0.0005015668,0.00004026791,0.0006828771,0.002520755],"study_design_scores_gemma":[0.0000015450206,0.000008948168,0.99940026,0.0000017073497,0.0000057075476,0.0000089816485,0.00006297603,0.0003190361,0.00005051833,0.0000037306672,0.00013546109,0.0000010993452],"about_ca_topic_score_codex":0.057957698,"about_ca_topic_score_gemma":0.098030426,"teacher_disagreement_score":0.057957698,"about_ca_system_score_codex":0.0005513962,"about_ca_system_score_gemma":0.0004869184,"threshold_uncertainty_score":0.11524069},"labels":[],"label_agreement":null},{"id":"W3119843760","doi":"10.1029/2020gl090853","title":"Crustal Rotation and Fluids: Factors for the 2019 Ridgecrest Earthquake Sequence?","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Sinistral and dextral; Geology; Seismology; Clockwise; Shear (geology); Rotation (mathematics); Anisotropy; Fault (geology); Shear zone; Foreshock; Geodesy; Tectonics; Geometry; Petrology; Aftershock; Physics","score_opus":0.06959101381479219,"score_gpt":0.31140106436842596,"score_spread":0.24181005055363378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3119843760","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99644876,0.0011251705,0.00008669506,0.0007751799,0.000017448176,0.0000082615215,0.00026897877,0.000010822016,0.0012586006],"genre_scores_gemma":[0.9994879,0.00016976468,0.000029492945,0.000030147032,0.000021953632,0.0000012026356,0.000085530344,0.0000014735493,0.00017259028],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99976844,0.000037653484,0.000028668599,0.000043274136,0.000033567147,0.00008830584],"domain_scores_gemma":[0.9978951,0.00024937466,0.0012336096,0.00008523084,0.0001355586,0.00040108917],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003980394,0.0003064116,0.00026014404,0.0008840999,0.0002870891,0.0009183742,0.00022575833,0.0005042023,0.0038374327],"category_scores_gemma":[0.0026978422,0.00015482845,0.00032570434,0.0008265049,0.00061053183,0.00053814973,0.00043644838,0.00034119925,0.00030852156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018550476,0.000023758696,0.991764,0.000017636678,0.000024097193,0.0005087653,0.00008814488,0.000088097484,0.0014144087,0.000086140135,0.00012926813,0.005670167],"study_design_scores_gemma":[0.0000018065664,0.000031313404,0.999113,0.0000060660573,0.000009821668,0.00015906247,0.00018754619,0.0001176999,0.00012141004,0.00003764251,0.00021177458,0.0000027389517],"about_ca_topic_score_codex":0.009868452,"about_ca_topic_score_gemma":0.013399953,"teacher_disagreement_score":0.009868452,"about_ca_system_score_codex":0.00048234325,"about_ca_system_score_gemma":0.0006618453,"threshold_uncertainty_score":0.019622028},"labels":[],"label_agreement":null},{"id":"W3120013398","doi":"10.1029/2020gl092351","title":"On the Formation of Phantom Electron Phase Space Density Peaks in Single Spacecraft Radiation Belt Data","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; National Aeronautics and Space Administration; U.S. Department of Energy","keywords":"Physics; Acceleration; Van Allen radiation belt; Van Allen Probes; Computational physics; Electron; Diffusion; Phase (matter); Spacecraft; Electron density; Radiation; Plasmasphere; Magnetosphere; Astrophysics; Geophysics; Magnetic field; Optics; Classical mechanics; Astronomy","score_opus":0.033311130021400535,"score_gpt":0.32293527768200453,"score_spread":0.289624147660604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3120013398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949856,0.00008102825,0.0035008893,0.0000419204,0.000007701255,0.000009054293,0.00026034814,0.00007491529,0.0010383937],"genre_scores_gemma":[0.9981743,0.000017750368,0.0012589371,0.0000060711004,0.000007064758,0.0000030318338,0.00042778044,0.000013254332,0.00009190841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997198,0.0000570961,0.000016198068,0.00006987679,0.000092006565,0.00004498575],"domain_scores_gemma":[0.9982089,0.00087903294,0.0003935429,0.0002364968,0.00021621803,0.00006590103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000878383,0.00012437932,0.00015024701,0.0014716288,0.00026745885,0.00065782666,0.0002631919,0.00022881235,0.0006880239],"category_scores_gemma":[0.0034113019,0.00013140053,0.00013183264,0.0009668464,0.00026296615,0.0005651278,0.0004997798,0.000212152,0.00015163112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065504503,0.00010022766,0.8581566,0.00006557388,0.000114673036,0.00092123396,0.0013442119,0.009834122,0.041158773,0.0029979423,0.0012079449,0.08344359],"study_design_scores_gemma":[0.000018404062,0.00009698412,0.95102036,0.000020942607,0.000027800144,0.00053773675,0.00053506653,0.03285353,0.010855368,0.0010712781,0.0029407071,0.000021734228],"about_ca_topic_score_codex":0.0017988973,"about_ca_topic_score_gemma":0.003235863,"teacher_disagreement_score":0.0017988973,"about_ca_system_score_codex":0.00027676122,"about_ca_system_score_gemma":0.00013913713,"threshold_uncertainty_score":0.0046453476},"labels":[],"label_agreement":null},{"id":"W3120242590","doi":"10.1029/2020gl092128","title":"Seeing Through the Atmosphere of Venus: What Is on the Surface?","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Winnipeg","funders":"","keywords":"Venus; Igneous rock; Geology; Atmosphere (unit); Emissivity; Atmosphere of Venus; Opacity; Astrobiology; Geochemistry; Earth science; Meteorology; Physics; Optics","score_opus":0.05030478518040679,"score_gpt":0.3073875737304625,"score_spread":0.25708278855005573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3120242590","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86021125,0.045312677,0.0026037549,0.023280814,0.0010092286,0.00003433968,0.0020340264,0.00015335505,0.06536053],"genre_scores_gemma":[0.9909446,0.0048603746,0.0004164372,0.00090332155,0.00043033191,0.00000597482,0.0004742089,0.00003790422,0.0019266716],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99962664,0.00006920922,0.000010169803,0.00008403749,0.00009084055,0.00011917228],"domain_scores_gemma":[0.9991672,0.00019442088,0.000095702286,0.000042034757,0.0002644202,0.00023628357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003726132,0.00018029529,0.00034626204,0.00052979426,0.00082887296,0.00317064,0.000482178,0.00084238825,0.005388806],"category_scores_gemma":[0.002166271,0.00013789162,0.00021875331,0.0006221484,0.0011960765,0.002683612,0.0009521559,0.0006821605,0.0007064214],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003923127,0.00013555108,0.6761393,0.0011987037,0.00021969233,0.0006410064,0.010653193,0.0011246408,0.013750343,0.010109877,0.036660552,0.24897489],"study_design_scores_gemma":[0.000007655263,0.00009923077,0.9184711,0.00065074366,0.00009310007,0.00046942433,0.020543125,0.0014761058,0.0012841508,0.00903401,0.047819003,0.00005233943],"about_ca_topic_score_codex":0.03273569,"about_ca_topic_score_gemma":0.03288548,"teacher_disagreement_score":0.03273569,"about_ca_system_score_codex":0.0011556487,"about_ca_system_score_gemma":0.0005599425,"threshold_uncertainty_score":0.0650903},"labels":[],"label_agreement":null},{"id":"W3121962757","doi":"10.1029/2020gl091494","title":"Effects of Ion Slippage in Earth's Ionosphere and the Plasma Sheet","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Air Force Office of Scientific Research; National Natural Science Foundation of China; National Aeronautics and Space Administration; Chinese Academy of Sciences; National Science Foundation","keywords":"Substorm; Plasma sheet; Ionosphere; Electrojet; Geophysics; Plasma; Geology; Physics; Instability; Flux (metallurgy); Magnetic field; Magnetosphere; Earth's magnetic field; Mechanics; Materials science","score_opus":0.00718906930836164,"score_gpt":0.24980215835347672,"score_spread":0.24261308904511508,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3121962757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99945456,0.000009839099,0.00021720982,0.000009185965,0.0000017056815,0.0000012684085,0.00001643508,0.000012844555,0.00027700208],"genre_scores_gemma":[0.999882,0.0000053029507,0.000067643836,0.0000019681845,4.320766e-7,8.20186e-7,0.000009311292,0.000001653021,0.000030770887],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.000013804848,0.0000034652946,0.000007589695,0.0000077705245,0.000013000638],"domain_scores_gemma":[0.9996126,0.00019036763,0.00008001575,0.000043910462,0.000023561117,0.000049621685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001752658,0.00020833849,0.000215743,0.00012952223,0.00021848857,0.00037026056,0.00020269665,0.00016881445,0.0008795349],"category_scores_gemma":[0.0008621501,0.000104384104,0.00018591847,0.00008741377,0.00044046497,0.00021372142,0.00030018506,0.00022478256,0.000051358056],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014495032,0.00020432276,0.13476828,0.00012420311,0.00015350545,0.0010134601,0.00022652389,0.7117648,0.14078395,0.0036689749,0.0002672718,0.0055751954],"study_design_scores_gemma":[0.00017377395,0.0006957842,0.08511124,0.000014568102,0.000068416826,0.00016114175,0.0002438627,0.877962,0.033768903,0.0013576642,0.00041811183,0.00002458024],"about_ca_topic_score_codex":0.0029150764,"about_ca_topic_score_gemma":0.0011516031,"teacher_disagreement_score":0.0029150764,"about_ca_system_score_codex":0.00029751987,"about_ca_system_score_gemma":0.00019700988,"threshold_uncertainty_score":0.0057962537},"labels":[],"label_agreement":null},{"id":"W3122183651","doi":"10.1029/2020gl091384","title":"Magnetic Conjugacy of Pc1 Waves and Isolated Proton Precipitation at Subauroral Latitudes: Importance of Ionosphere as Intensity Modulation Region","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Research Institute for Sustainable Humanosphere, Kyoto University; Augsburg University; Japan Society for the Promotion of Science; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Physics; Ionosphere; Earth's magnetic field; Magnetosphere; Amplitude; Geophysics; Northern Hemisphere; Riometer; Computational physics; Electron precipitation; Middle latitudes; Atmospheric sciences; Magnetic field; Optics; Plasma; Nuclear physics","score_opus":0.017830141483972817,"score_gpt":0.28206541813928704,"score_spread":0.2642352766553142,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122183651","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975534,0.00012530462,0.00032233857,0.000016977716,0.0000045450042,0.0000036784495,0.00007486606,0.0000073104698,0.0018916373],"genre_scores_gemma":[0.99973696,0.000031888907,0.000072428804,0.0000037686623,0.000008150518,0.0000013227445,0.00004431417,0.0000021679987,0.00009901855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.000009767928,0.000002989979,0.000014106182,0.0000109739485,0.000015215953],"domain_scores_gemma":[0.99951637,0.00012188513,0.00017933494,0.00004746463,0.000070251415,0.00006465152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011539218,0.00013542545,0.00015740699,0.0006335621,0.000159126,0.00047583887,0.00012310746,0.00014651885,0.0013967727],"category_scores_gemma":[0.00074292545,0.00008271947,0.00008416747,0.0005318756,0.00025746433,0.000307812,0.0003417921,0.00018540333,0.00020621101],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00049442303,0.000037412254,0.84846467,0.000055651304,0.00007544211,0.00024001903,0.00048402935,0.00049144734,0.12638395,0.0004663432,0.00019224553,0.022614352],"study_design_scores_gemma":[0.0000018215147,0.000017007935,0.9984402,0.0000016788598,0.0000064040073,0.000047763024,0.00006442873,0.00019692603,0.0010821909,0.00004891701,0.00009130223,0.0000014073629],"about_ca_topic_score_codex":0.0015971534,"about_ca_topic_score_gemma":0.0013036806,"teacher_disagreement_score":0.0015971534,"about_ca_system_score_codex":0.00010340192,"about_ca_system_score_gemma":0.000075827564,"threshold_uncertainty_score":0.004672706},"labels":[],"label_agreement":null},{"id":"W3122649433","doi":"10.1029/2011gl049427","title":"Shrinking lakes of the Arctic: Spatial relationships and trajectory of change","year":2011,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":138,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Heliosphere; Physics; Interplanetary scintillation; Interplanetary spaceflight; Turbulence; Solar wind; Scintillation; Atmospheric sciences; Polar; Environmental science; Astrophysics; Astronomy; Meteorology; Coronal mass ejection; Plasma; Nuclear physics","score_opus":0.12921965279708145,"score_gpt":0.2855572273488604,"score_spread":0.15633757455177896,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3122649433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968317,0.00049577287,0.00025687384,0.00026184582,0.0000051084926,0.0000040277305,0.0011798182,0.000010456208,0.00095445686],"genre_scores_gemma":[0.9984629,0.0003259313,0.00031950072,0.000010887174,0.000005850777,0.00000282971,0.0006427238,0.0000027357107,0.00022659841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999256,0.000015201647,0.000003841409,0.000016897477,0.000015488971,0.000022975593],"domain_scores_gemma":[0.9995122,0.000059327598,0.00014880802,0.000020132311,0.00019463069,0.00006490886],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025252526,0.00009888014,0.00012294063,0.00087662594,0.0005670395,0.000521872,0.00023615474,0.00016139538,0.0010926219],"category_scores_gemma":[0.0009628673,0.00009546342,0.00013001422,0.0020575342,0.00029211715,0.00033770726,0.0004734132,0.00020378108,0.00009937413],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007114209,0.00001047701,0.9883435,0.000017049628,0.000037999078,0.000044566223,0.000657698,0.00045459674,0.00053294684,0.00024005395,0.0006596151,0.008930249],"study_design_scores_gemma":[8.5420527e-7,0.000005855867,0.997804,0.000005055213,0.000006337943,0.00003404895,0.00065996294,0.0007089558,0.000055747496,0.00008270522,0.0006346653,0.0000018130462],"about_ca_topic_score_codex":0.4879759,"about_ca_topic_score_gemma":0.6506042,"teacher_disagreement_score":0.4879759,"about_ca_system_score_codex":0.0011244554,"about_ca_system_score_gemma":0.0010388888,"threshold_uncertainty_score":0.9702711},"labels":[],"label_agreement":null},{"id":"W3123240499","doi":"10.1029/2020gl091094","title":"Deep Waters in British Columbia Mainland Fjords Show Rapid Warming and Deoxygenation From 1951 to 2020","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":53,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Hakai Institute; Tula Foundation","keywords":"Fjord; Inlet; Sill; Oceanography; Salinity; Temperature salinity diagrams; Inflow; Geology; Environmental science; Estuary; Hydrology (agriculture); Geochemistry","score_opus":0.01455817364851823,"score_gpt":0.23254617263262262,"score_spread":0.2179879989841044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3123240499","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9928282,0.00083395507,0.000046854242,0.00021887496,0.000015726899,0.0000033152705,0.003508374,0.000011375726,0.0025332414],"genre_scores_gemma":[0.9962536,0.00034406243,0.00005821717,0.00007212608,0.0000051750612,0.0000031031618,0.002156064,0.000002682739,0.0011048906],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988914,0.0000062596723,0.000007536204,0.000026527412,0.000029114026,0.000041504423],"domain_scores_gemma":[0.99957925,0.000025279727,0.00008599973,0.000021234948,0.00021206099,0.00007609751],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016037644,0.00016878193,0.00014811954,0.0010207172,0.0006935582,0.00089592376,0.00025145302,0.00031393263,0.0014650319],"category_scores_gemma":[0.0005013049,0.00012342376,0.00015223945,0.0019920461,0.00035934625,0.00021835278,0.0004076761,0.00025902363,0.00022483122],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008136621,0.0000111975305,0.9854012,0.00004413526,0.000060876988,0.00011664389,0.00050095934,0.0002530677,0.0013835257,0.000055400218,0.0017574648,0.010334145],"study_design_scores_gemma":[4.0119082e-7,0.0000012202214,0.99923146,0.000004333869,0.0000024476437,0.0000056878225,0.000107931955,0.000020850499,0.00002917462,0.0000022200436,0.0005930605,0.0000011292329],"about_ca_topic_score_codex":0.9059927,"about_ca_topic_score_gemma":0.9579923,"teacher_disagreement_score":0.09400731,"about_ca_system_score_codex":0.0040867906,"about_ca_system_score_gemma":0.00207864,"threshold_uncertainty_score":0.18912184},"labels":[],"label_agreement":null},{"id":"W3126091753","doi":"10.1029/2020gl091702","title":"Mode Coupling From Kinetic Alfvén Waves to Electron Acoustic Waves in the Topside Ionosphere","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Natural Science Foundation of China","keywords":"Physics; Ionosphere; Electron; Acoustic wave; Electron density; Wavelength; Ion acoustic wave; Kinetic energy; Landau damping; Dissipation; Mode coupling; Electron temperature; Coupling (piping); Computational physics; Amplitude; Geophysics; Optics; Materials science; Classical mechanics","score_opus":0.015507251908771237,"score_gpt":0.2971931615517376,"score_spread":0.28168590964296636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3126091753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9923822,0.00012012909,0.005550273,0.000022213806,0.0000058477576,0.000005800236,0.00002620738,0.000045187775,0.0018422024],"genre_scores_gemma":[0.9992017,0.000059283782,0.00036144155,0.0000033730769,0.000002524396,0.0000024633869,0.000015841448,0.0000054549837,0.00034793586],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999647,0.0000052192963,0.0000010475251,0.000007565911,0.00000984123,0.000011493259],"domain_scores_gemma":[0.99986637,0.00003363311,0.00003429552,0.000011637379,0.000027743788,0.000026192047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010079009,0.0003962874,0.0002363,0.00025468908,0.00015347851,0.00033952945,0.00021855754,0.00019787886,0.0008993886],"category_scores_gemma":[0.00028535575,0.00021958626,0.00024204399,0.00015258491,0.00028142112,0.00030343098,0.0005315879,0.0001993393,0.00015195114],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060706725,0.00007588734,0.062876046,0.00017142545,0.00013120037,0.0012726125,0.00048748433,0.108424865,0.8032206,0.006774605,0.00044009433,0.01551815],"study_design_scores_gemma":[0.000103473845,0.0005073658,0.16613834,0.00003060624,0.000114568196,0.0006975368,0.0005250396,0.745317,0.0803777,0.0049977233,0.0011175158,0.00007317171],"about_ca_topic_score_codex":0.0015479618,"about_ca_topic_score_gemma":0.0007223485,"teacher_disagreement_score":0.0015479618,"about_ca_system_score_codex":0.00016171594,"about_ca_system_score_gemma":0.00015147131,"threshold_uncertainty_score":0.0030778646},"labels":[],"label_agreement":null},{"id":"W3126563039","doi":"10.1029/2020gl092032","title":"PrecipGAN: Merging Microwave and Infrared Data for Satellite Precipitation Estimation Using Generative Adversarial Network","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Precipitation Measurement and Analysis","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Canmore Museum and Geoscience Centre; University of Saskatchewan","funders":"National Natural Science Foundation of China","keywords":"Satellite; Quantitative precipitation estimation; Computer science; Microwave; Precipitation; Environmental science; Remote sensing; Meteorology; Geology; Geography; Telecommunications","score_opus":0.1106043115874618,"score_gpt":0.3369423244989205,"score_spread":0.22633801291145866,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3126563039","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04030529,0.00019335341,0.95502627,0.00041041741,0.00006671303,0.00006432542,0.00022098022,0.0019893807,0.0017232925],"genre_scores_gemma":[0.8028826,0.00011527685,0.19112946,0.0004607162,0.00009213568,0.0001370429,0.0010669228,0.0002640347,0.0038516552],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996563,0.00013210003,0.00001002885,0.00010130422,0.000063073865,0.000037256723],"domain_scores_gemma":[0.999226,0.0004726851,0.00008142511,0.00008957395,0.00009133671,0.00003891147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012477314,0.00085451244,0.0005415425,0.00039251032,0.0002431517,0.000498852,0.0013713209,0.00075902545,0.002088501],"category_scores_gemma":[0.0024947324,0.00048630245,0.0005632661,0.00040371547,0.00060283486,0.0008456789,0.0015804215,0.0014553511,0.00049018994],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006496406,0.000027982904,0.0010477471,0.000016766646,0.000057016514,0.000045958994,0.00001739227,0.96036494,0.0010212808,0.0020874182,0.0016407232,0.033607896],"study_design_scores_gemma":[0.000002905774,0.000005630739,0.00006741147,0.000001390652,0.0000021803687,0.000004484809,0.0000013085563,0.99859625,0.0003016831,0.00090705266,0.00010788576,0.0000017169574],"about_ca_topic_score_codex":0.0053825863,"about_ca_topic_score_gemma":0.0057568615,"teacher_disagreement_score":0.0053825863,"about_ca_system_score_codex":0.0006359884,"about_ca_system_score_gemma":0.00058047444,"threshold_uncertainty_score":0.01070255},"labels":[],"label_agreement":null},{"id":"W3126639553","doi":"10.1029/2020gl089990","title":"Opposite Responses of the Dry and Moist Eddy Heat Transport Into the Arctic in the PAMIP Experiments","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Stevens Institute of Technology; National Science Foundation; Department for Business, Energy and Industrial Strategy, UK Government; Met Office; U.S. Department of Energy; Department for Environment, Food and Rural Affairs, UK Government","keywords":"Climatology; Sea ice; Environmental science; Atmospheric sciences; Isentropic process; Arctic; Arctic ice pack; Moisture; Latitude; Arctic sea ice decline; Atmospheric circulation; Sea ice thickness; Geology; Meteorology; Oceanography; Geography; Thermodynamics","score_opus":0.04456172401681261,"score_gpt":0.3249724097835778,"score_spread":0.28041068576676514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3126639553","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982324,0.000012770829,0.00036446186,0.00004427593,0.000008231207,0.000005699791,0.0002882652,0.000021803635,0.0010220226],"genre_scores_gemma":[0.99897325,0.000023878056,0.000344475,0.000055032746,0.000003833291,0.000033376054,0.0002517547,0.0000175686,0.00029688296],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982697,0.000054551114,0.000012481522,0.00004152053,0.00002528551,0.000039221723],"domain_scores_gemma":[0.99967325,0.000090756555,0.000041070853,0.00008203379,0.000041990803,0.00007091664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000430506,0.00029980062,0.00024119852,0.0001610068,0.00038767824,0.00039592112,0.0002843471,0.00023709779,0.0008177462],"category_scores_gemma":[0.00091413717,0.00016478742,0.00019705063,0.00013623702,0.00035458,0.00029004054,0.0005683326,0.000778862,0.00011227264],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.011587933,0.00095702976,0.06834485,0.00013205456,0.00032251724,0.00023146719,0.0006278615,0.03103016,0.8671781,0.0021144722,0.0015722831,0.015901307],"study_design_scores_gemma":[0.0004238603,0.002681346,0.4532743,0.000027953845,0.0002550425,0.00019433741,0.0008876451,0.101522036,0.4345537,0.002575229,0.0034883793,0.000116213494],"about_ca_topic_score_codex":0.006526304,"about_ca_topic_score_gemma":0.0056603784,"teacher_disagreement_score":0.006526304,"about_ca_system_score_codex":0.0004209011,"about_ca_system_score_gemma":0.00023797447,"threshold_uncertainty_score":0.012976587},"labels":[],"label_agreement":null},{"id":"W3127432954","doi":"10.1029/2020gl091873","title":"Observationally Constrained Cloud Phase Unmasks Orbitally Driven Climate Feedbacks","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Board; Yale University; National Science Foundation","keywords":"Cloud feedback; Climate model; Environmental science; Cloud computing; Ice cloud; Atmospheric sciences; Climate state; Climate change; Climatology; Geology; Global warming; Climate sensitivity; Effects of global warming; Computer science; Oceanography","score_opus":0.054779421382447346,"score_gpt":0.3293350708488708,"score_spread":0.27455564946642347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127432954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554586,0.00006460851,0.001316488,0.000109294786,0.000009171899,0.0000044448993,0.0013103797,0.00004831696,0.0015914517],"genre_scores_gemma":[0.9991616,0.000020010879,0.00017068413,0.00001785658,0.0000035868086,0.0000018878997,0.00057299034,0.000007759627,0.0000436401],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998241,0.00005229296,0.000011389249,0.00006457035,0.00002025329,0.000027312191],"domain_scores_gemma":[0.9990268,0.0003247027,0.00021666965,0.00023007597,0.00010273582,0.00009908873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005275742,0.00021167696,0.0002483487,0.00025004678,0.0003008922,0.0006574725,0.00028132857,0.00024859057,0.0020525623],"category_scores_gemma":[0.0022368066,0.00018972231,0.0002525527,0.00032483324,0.00040685612,0.0005943632,0.00056879676,0.00034307325,0.00016353783],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006897233,0.00015720516,0.8962682,0.00013305005,0.00026316516,0.00008469549,0.00021188286,0.042751543,0.04218975,0.0028534494,0.0012799246,0.0131174065],"study_design_scores_gemma":[0.000095768846,0.000086877364,0.9263718,0.000021390162,0.00008188372,0.00005030806,0.00016884138,0.062337603,0.0051192287,0.0030084064,0.0026250149,0.000032965218],"about_ca_topic_score_codex":0.014564692,"about_ca_topic_score_gemma":0.022845935,"teacher_disagreement_score":0.014564692,"about_ca_system_score_codex":0.0003906176,"about_ca_system_score_gemma":0.0003593161,"threshold_uncertainty_score":0.02895981},"labels":[],"label_agreement":null},{"id":"W3127656662","doi":"10.1029/2020gl091911","title":"Arctic Ozone Depletion in 2019/20: Roles of Chemistry, Dynamics and the Montreal Protocol","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":103,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ozone depletion; Ozone; Ozone layer; Montreal Protocol; Polar vortex; Atmospheric sciences; Chemical transport model; Arctic; Polar; Stratosphere; Bromine; Climatology; Environmental science; Chlorine; Meteorology; Chemistry; Oceanography; Geology; Physics","score_opus":0.012625437081587613,"score_gpt":0.26770346489933006,"score_spread":0.25507802781774247,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127656662","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8866787,0.0005513196,0.002548401,0.0054482617,0.0001621605,0.00022915124,0.04646282,0.00037618968,0.057543],"genre_scores_gemma":[0.98245347,0.00018674186,0.0008362464,0.0002541562,0.00001552828,0.0000981659,0.007093261,0.000030445432,0.009031836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998192,0.000037911155,0.0000059562562,0.000024132893,0.00004532804,0.00006752821],"domain_scores_gemma":[0.99964035,0.00004251263,0.000060568764,0.000018410226,0.00015197159,0.0000861913],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007148048,0.00022553372,0.00019665401,0.0004193268,0.0007157861,0.0014942603,0.00069673546,0.00045001673,0.0049378285],"category_scores_gemma":[0.0013323659,0.00014345055,0.00043598743,0.00051857997,0.00020896377,0.00040578147,0.0004790177,0.00042295497,0.0003610405],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008442475,0.00034085548,0.5558957,0.00019478898,0.0004674044,0.00040219087,0.00029628584,0.32394066,0.0030731137,0.031359926,0.051982187,0.0312027],"study_design_scores_gemma":[0.00026295843,0.0002761877,0.54155415,0.00011526784,0.00018689665,0.000043406373,0.00080899626,0.36220708,0.003546085,0.004174358,0.08665423,0.00017026468],"about_ca_topic_score_codex":0.8724883,"about_ca_topic_score_gemma":0.8674041,"teacher_disagreement_score":0.8724883,"about_ca_system_score_codex":0.0121153975,"about_ca_system_score_gemma":0.007822577,"threshold_uncertainty_score":0.25652522},"labels":[],"label_agreement":null},{"id":"W3127909190","doi":"10.1029/2020gl091987","title":"COVID‐19 Crisis Reduces Free Tropospheric Ozone Across the Northern Hemisphere","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":163,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Earth Sciences Division; Bundesministerium für Wirtschaft und Energie; Fonds De La Recherche Scientifique - FNRS; Deutsche Forschungsgemeinschaft","keywords":"Ozone; Atmospheric sciences; Stratosphere; Tropospheric ozone; Northern Hemisphere; Troposphere; Environmental science; Climatology; Anomaly (physics); Atmosphere (unit); Ozone layer; Altitude (triangle); Ozone depletion; Meteorology; Geology; Geography; Physics","score_opus":0.031943438486340583,"score_gpt":0.30985778447407414,"score_spread":0.27791434598773357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3127909190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9733128,0.0011364531,0.000092390736,0.0025516823,0.000091700334,0.000030871674,0.0029231142,0.00011454095,0.019746564],"genre_scores_gemma":[0.99535143,0.00048787406,0.000064659806,0.0006913619,0.000026758107,0.000015696114,0.0016113515,0.000014260134,0.0017365318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997683,0.000028972774,0.000009319135,0.000033834636,0.00004600133,0.00011356018],"domain_scores_gemma":[0.9994972,0.00002855845,0.0001354892,0.00002291696,0.00008679127,0.00022915595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024191478,0.00018644625,0.00019773291,0.00027176904,0.0005247514,0.00068194314,0.0002973988,0.00024872666,0.003979763],"category_scores_gemma":[0.0010969318,0.00007679468,0.00016320865,0.000375505,0.0002965135,0.0002665696,0.0007167093,0.00039228404,0.0004078248],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018311243,0.0007774265,0.77016866,0.00029264658,0.0001964501,0.0015364073,0.0012295885,0.003933831,0.021786507,0.002480944,0.09683081,0.09893556],"study_design_scores_gemma":[0.000031578867,0.000168863,0.98055124,0.000030731215,0.000024025907,0.00022934964,0.001329933,0.00064694835,0.0010863657,0.0003162174,0.01557389,0.000010828293],"about_ca_topic_score_codex":0.14303392,"about_ca_topic_score_gemma":0.12546583,"teacher_disagreement_score":0.14303392,"about_ca_system_score_codex":0.001369255,"about_ca_system_score_gemma":0.0014008451,"threshold_uncertainty_score":0.28440273},"labels":[],"label_agreement":null},{"id":"W3128632267","doi":"10.1029/2020gl091403","title":"Iron Regulation of North Atlantic Eddy Phytoplankton Productivity","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"H2020 Marie Skłodowska-Curie Actions; Bundesministerium für Bildung und Forschung; Natural Environment Research Council; Sight Research UK","keywords":"Oceanography; Upwelling; Eddy; Productivity; Phytoplankton; Environmental science; Continental shelf; Latitude; Biomass (ecology); Plankton; Geology; Nutrient; Ecology; Geography; Biology; Meteorology","score_opus":0.023420334169256887,"score_gpt":0.2507047905743236,"score_spread":0.22728445640506673,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3128632267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992048,0.000036637208,0.000043851123,0.000019440662,0.0000018452507,0.0000015771725,0.000075748234,0.0000042124,0.00061198167],"genre_scores_gemma":[0.99926513,0.000027419394,0.00005556477,0.000019064322,0.0000015564187,0.0000020542514,0.00009555316,0.000001699011,0.00053183676],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.000003375903,0.0000021491642,0.000010571174,0.0000060356133,0.000015207806],"domain_scores_gemma":[0.9998235,0.000027949576,0.00003998864,0.0000109528755,0.00005170287,0.00004586137],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006119198,0.00011098001,0.00013126315,0.00020250927,0.0002239092,0.00033117633,0.00010299924,0.00013037263,0.0005127127],"category_scores_gemma":[0.00019847468,0.00012670188,0.00008030672,0.00008675771,0.00017394108,0.000096861535,0.0002516871,0.00013752698,0.00008985867],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055656285,0.000085701184,0.38497388,0.000044547767,0.00005557081,0.00018695684,0.00031419963,0.0011338549,0.6035171,0.00019185017,0.0005656332,0.008374107],"study_design_scores_gemma":[0.0000030597355,0.000016472704,0.9967625,0.0000017737259,0.0000028402371,0.000011075675,0.000055301745,0.00048586147,0.0024733273,0.000016684631,0.00016946897,0.0000016600976],"about_ca_topic_score_codex":0.037081536,"about_ca_topic_score_gemma":0.07271108,"teacher_disagreement_score":0.037081536,"about_ca_system_score_codex":0.000829758,"about_ca_system_score_gemma":0.00021903151,"threshold_uncertainty_score":0.07373142},"labels":[],"label_agreement":null},{"id":"W3129716233","doi":"10.1029/2020gl089471","title":"Antarctic Circumpolar Current Impacts on Internal Wave Life Cycles","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Internal wave; Mesoscale meteorology; Circumpolar star; Advection; Geology; Mixing (physics); Breaking wave; Internal tide; Current (fluid); Circumpolar deep water; Flow (mathematics); Climatology; Oceanography; Mechanics; Thermohaline circulation; Wave propagation; Physics","score_opus":0.04579779866487342,"score_gpt":0.3019091893246719,"score_spread":0.2561113906597985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3129716233","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9942075,0.00012655626,0.00031185837,0.00009768334,0.000008849373,0.0000064855376,0.00045732138,0.000021110398,0.0047625955],"genre_scores_gemma":[0.999052,0.00013281843,0.00007401933,0.00001710611,0.0000052378427,0.0000034462603,0.0002500417,0.0000075074295,0.00045778393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999393,0.00001372797,0.0000052642035,0.000011474677,0.000014118161,0.000016115759],"domain_scores_gemma":[0.99947375,0.00015308878,0.00012910488,0.000058201447,0.0001160456,0.000069811234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000302462,0.00029860143,0.00018885489,0.0008149368,0.0002973197,0.00095619087,0.00014852715,0.00021031118,0.002581621],"category_scores_gemma":[0.0011223663,0.00011920157,0.00028560698,0.0006294196,0.00033210524,0.0004839122,0.0006384526,0.00031339438,0.00030000106],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032222536,0.00007505196,0.8683719,0.00014074848,0.00022531969,0.00036248245,0.00047006764,0.06797964,0.018473104,0.0038138316,0.0015515221,0.038214114],"study_design_scores_gemma":[0.000018165407,0.00009048355,0.95485336,0.000024590947,0.00006874664,0.00007046779,0.000397221,0.03916938,0.0021523396,0.0012872625,0.0018459251,0.000022106593],"about_ca_topic_score_codex":0.010711155,"about_ca_topic_score_gemma":0.0071259956,"teacher_disagreement_score":0.010711155,"about_ca_system_score_codex":0.00062225485,"about_ca_system_score_gemma":0.00026248672,"threshold_uncertainty_score":0.021297634},"labels":[],"label_agreement":null},{"id":"W3130404751","doi":"10.1029/2020gl091633","title":"Quasi‐Periodic Intensification of Convective Asymmetries in the Outer Eyewall of Typhoon Lekima (2019)","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"","keywords":"Eye; Typhoon; Wavenumber; Convection; Tropical cyclone; Geology; Rainband; Geophysics; Rossby wave; Vortex; Atmospheric sciences; Climatology; Meteorology; Physics; Optics","score_opus":0.04432300474335322,"score_gpt":0.30397846594835826,"score_spread":0.25965546120500504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3130404751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99966073,0.000014574321,0.00003647413,0.000006849196,0.0000015697213,0.0000012646815,0.000043321088,0.0000029734945,0.00023223572],"genre_scores_gemma":[0.99977106,0.000008582839,0.000036212237,0.000004865786,0.0000021315022,0.0000015931485,0.000070907416,8.9738694e-7,0.00010373926],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997866,0.0000019136598,0.0000013322959,0.0000051530296,0.0000031813722,0.000009708122],"domain_scores_gemma":[0.9998944,0.0000103040065,0.000038470833,0.00000695289,0.000020940779,0.000028888766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006129465,0.00011215098,0.00010950326,0.00038934598,0.00022716785,0.0002290422,0.00006830891,0.00012129446,0.0007558708],"category_scores_gemma":[0.00013149416,0.000063842046,0.00009924959,0.00021078394,0.00016351568,0.00010687574,0.00024447043,0.00013261054,0.00007907822],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045174782,0.000056377783,0.73309946,0.000059304188,0.00007249386,0.0010719473,0.0007042876,0.0010625692,0.25272623,0.0002633454,0.00036148497,0.010070805],"study_design_scores_gemma":[0.00000378745,0.000014138374,0.99789137,0.0000021089743,0.000004715131,0.00003913534,0.000095313466,0.00044326362,0.0013384904,0.000013519266,0.00015192185,0.0000023790142],"about_ca_topic_score_codex":0.006036431,"about_ca_topic_score_gemma":0.010431211,"teacher_disagreement_score":0.006036431,"about_ca_system_score_codex":0.00024947073,"about_ca_system_score_gemma":0.00012336634,"threshold_uncertainty_score":0.012002587},"labels":[],"label_agreement":null},{"id":"W3130928344","doi":"10.1029/2020gl092066","title":"Ocean Eddy Signature on SAR‐Derived Sea Ice Drift and Vorticity","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agence Nationale de la Recherche; European Space Agency","keywords":"Geology; Sea ice; Eddy; Climatology; Mesoscale meteorology; Geophysics; Potential vorticity; Mooring; Vorticity; Altimeter; Synthetic aperture radar; Remote sensing; Geodesy; Meteorology; Oceanography; Vortex; Turbulence; Geography","score_opus":0.02024008439525067,"score_gpt":0.26642262658113375,"score_spread":0.2461825421858831,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3130928344","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99366164,0.000083252664,0.0049333973,0.000022968114,0.0000088393035,0.0000066221387,0.00026327913,0.00007183072,0.00094815023],"genre_scores_gemma":[0.9963052,0.000040347102,0.00303875,0.000006798724,0.000005337235,0.0000023490634,0.0003874807,0.000008298611,0.00020533025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999341,0.000007780503,0.000004034902,0.000014605232,0.000024958565,0.000014520639],"domain_scores_gemma":[0.9997694,0.0000604649,0.000043942317,0.000017698076,0.000083588035,0.00002493659],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025382196,0.00024510737,0.00015606105,0.0005975042,0.00012419882,0.00040829097,0.0001241536,0.00012132651,0.00043066978],"category_scores_gemma":[0.0005187745,0.00009761287,0.00012238634,0.00037082576,0.00015473858,0.00016184768,0.00013104567,0.00011552539,0.00014623202],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005906397,0.00014451434,0.6195684,0.000103185135,0.00016445907,0.00038504353,0.00016202539,0.027100937,0.24675217,0.0004083621,0.00089772,0.10372253],"study_design_scores_gemma":[0.000015053384,0.000043718428,0.770786,0.0000125019815,0.00003572062,0.00014329595,0.00008385286,0.19374429,0.034317095,0.00006773781,0.000730229,0.000020469772],"about_ca_topic_score_codex":0.016283479,"about_ca_topic_score_gemma":0.029977432,"teacher_disagreement_score":0.016283479,"about_ca_system_score_codex":0.00025625943,"about_ca_system_score_gemma":0.0003793764,"threshold_uncertainty_score":0.03237742},"labels":[],"label_agreement":null},{"id":"W3132851765","doi":"10.1029/2020gl091508","title":"Mercury Evidence of Intense Volcanism Preceded Oceanic Anoxic Event 1d","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Volcanism; Geology; Anoxic waters; Volcano; Mercury (programming language); Large igneous province; Igneous rock; Geochemistry; Earth science; Paleontology; Oceanography; Tectonics","score_opus":0.06450321247434995,"score_gpt":0.3591346412461008,"score_spread":0.29463142877175086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3132851765","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99842787,0.00010812227,0.000046350324,0.000028589397,0.000004349236,0.0000027006822,0.00024729167,0.000005324701,0.0011294254],"genre_scores_gemma":[0.9993716,0.000042373875,0.000042019907,0.000012774544,0.000006526976,0.0000011281858,0.00027812042,6.880983e-7,0.00024483],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999459,0.0000037889554,0.0000040806863,0.000014507592,0.000014463993,0.000017311364],"domain_scores_gemma":[0.99975866,0.000022943885,0.00009642305,0.000010932932,0.00005147739,0.000059538706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013533587,0.000108940745,0.00015412366,0.0008907604,0.00029079587,0.00036057422,0.00014697152,0.00020450809,0.0014497843],"category_scores_gemma":[0.00026494014,0.00006383803,0.00008954244,0.0005526788,0.00024847232,0.00011446853,0.0003857886,0.0001944075,0.00008111857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023935591,0.000030425408,0.9621621,0.000037210222,0.000041334577,0.0004822509,0.00023624065,0.00012376066,0.031842794,0.00010930331,0.00013286408,0.0045623756],"study_design_scores_gemma":[0.0000014850141,0.000019835928,0.998755,0.0000023089974,0.000003348836,0.000037862137,0.00008511022,0.00003247703,0.00078646373,0.000017529352,0.00025755266,0.0000010426501],"about_ca_topic_score_codex":0.011907468,"about_ca_topic_score_gemma":0.02274063,"teacher_disagreement_score":0.011907468,"about_ca_system_score_codex":0.00038978385,"about_ca_system_score_gemma":0.00024757395,"threshold_uncertainty_score":0.023676276},"labels":[],"label_agreement":null},{"id":"W3135177098","doi":"10.1029/2020gl091883","title":"The Climate Response to Emissions Reductions Due to COVID‐19: Initial Results From CovidMIP","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"COVID-19 impact on air quality","field":"Environmental Science","cited_by":95,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China; Japan Agency for Marine-Earth Science and Technology; European Commission; Goddard Space Flight Center; Sight Research UK; Natural Environment Research Council; Center for Neuroscience and Regenerative Medicine; Met Office; Ministry of Education, Culture, Sports, Science and Technology; Department for Environment, Food and Rural Affairs, UK Government; National Aeronautics and Space Administration","keywords":"Environmental science; Atmospheric sciences; Shortwave radiation; Greenhouse gas; Climate model; Aerosol; Shortwave; Coronavirus disease 2019 (COVID-19); Climatology; Climate change; Air quality index; Ozone; Meteorology; Radiative transfer; Radiation; Geography; Geology","score_opus":0.100012535523313,"score_gpt":0.43736552351447644,"score_spread":0.3373529879911634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3135177098","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886938,0.00015299363,0.0012999218,0.0005103067,0.000042244927,0.00005872269,0.0043382603,0.00030708718,0.004596734],"genre_scores_gemma":[0.9932961,0.000067462126,0.0021073555,0.00010828919,0.000017861967,0.000062971034,0.0039634123,0.00004991591,0.00032653543],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993524,0.00023926572,0.00002491559,0.00012583865,0.00010494677,0.00015269272],"domain_scores_gemma":[0.99877435,0.0005299115,0.00007438096,0.00019672628,0.00025209042,0.00017250623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020274355,0.00090858364,0.00077969773,0.00036941457,0.0008665506,0.0009897127,0.0009929418,0.0011911455,0.0012691203],"category_scores_gemma":[0.0025203128,0.0003760212,0.0012709245,0.00061929453,0.00058823416,0.00082584633,0.0010523896,0.0017219457,0.00021998653],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010427686,0.0006070266,0.051562816,0.00010327584,0.00043613647,0.00025553996,0.00011406807,0.92636997,0.0047233324,0.0012156821,0.0053176885,0.008251725],"study_design_scores_gemma":[0.0008860261,0.0013194687,0.103343986,0.000037882106,0.00023973803,0.00006657913,0.0004901093,0.8724073,0.01329768,0.0024559489,0.0053061424,0.00014913453],"about_ca_topic_score_codex":0.06211233,"about_ca_topic_score_gemma":0.04029443,"teacher_disagreement_score":0.06211233,"about_ca_system_score_codex":0.0015451552,"about_ca_system_score_gemma":0.0010562434,"threshold_uncertainty_score":0.1235016},"labels":[],"label_agreement":null},{"id":"W3136046920","doi":"10.1029/2021gl092556","title":"Effects of Using High Resolution Satellite‐Based Inundation Time Series to Estimate Methane Fluxes From Forested Wetlands","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"National Science Foundation","keywords":"Wetland; Environmental science; Methane; Hydrology (agriculture); Surface water; Atmospheric methane; Satellite; Watershed; Atmospheric sciences; Geology; Ecology; Environmental engineering","score_opus":0.013928672096798256,"score_gpt":0.2822389191903638,"score_spread":0.26831024709356555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3136046920","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99817944,0.000025826643,0.0015012752,0.000023623701,0.000005028069,0.000003728545,0.00010711975,0.000028180833,0.00012579336],"genre_scores_gemma":[0.9980392,0.000015303116,0.0017029518,0.00000867311,0.000002799558,0.0000040516907,0.00018492958,0.0000053398994,0.000036709047],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996182,0.00019996811,0.000029376692,0.00008097886,0.000041329713,0.000030012085],"domain_scores_gemma":[0.9980344,0.0013405763,0.00020586616,0.00017580157,0.00018061107,0.00006274685],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001560838,0.00047026892,0.0002468506,0.0004500071,0.00023832687,0.00055713404,0.00032937241,0.00041007594,0.00023361939],"category_scores_gemma":[0.0034279518,0.00027466856,0.0005166304,0.0005120768,0.00023920699,0.0006320236,0.0002741301,0.00027538097,0.00006934803],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010481301,0.00037088007,0.6216671,0.00007210954,0.00057120126,0.00018557228,0.00011487894,0.3295612,0.023716211,0.00017721891,0.00025501422,0.022260442],"study_design_scores_gemma":[0.000042823696,0.0001271414,0.37757078,0.000010189859,0.00008650756,0.000046285044,0.000073786876,0.6120031,0.009651794,0.00012814003,0.00022935617,0.000030039768],"about_ca_topic_score_codex":0.017679831,"about_ca_topic_score_gemma":0.017292662,"teacher_disagreement_score":0.017679831,"about_ca_system_score_codex":0.00037810768,"about_ca_system_score_gemma":0.0002415769,"threshold_uncertainty_score":0.035153866},"labels":[],"label_agreement":null},{"id":"W3137621314","doi":"10.1029/2020gl092126","title":"Satellite Remote Sensing of Herring (<i>Clupea pallasii</i>) Spawning Events: A Case Study in the Strait of Georgia","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and fisheries research","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada","funders":"Nuclear Safety and Security Commission; National Natural Science Foundation of China; National Oceanic and Atmospheric Administration; U.S. Department of Commerce; National Aeronautics and Space Administration","keywords":"Clupea; Milt; Pacific herring; Herring; Oceanography; Satellite; Remote sensing; Environmental science; High resolution; Geology; Fishery; Fish <Actinopterygii>; Biology","score_opus":0.046174553195188164,"score_gpt":0.3281210850784654,"score_spread":0.28194653188327723,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3137621314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699676,0.000057718356,0.0009268009,0.00006952058,0.000005872429,0.000030585245,0.00014380073,0.00005473708,0.0017143154],"genre_scores_gemma":[0.99611306,0.00005607791,0.0030559248,0.000028489456,0.0000019300023,0.0000070454776,0.00012689403,0.0000066768,0.0006037859],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988234,0.000020404646,0.0000043750383,0.000023823506,0.000041780782,0.000027185199],"domain_scores_gemma":[0.9998442,0.000027818814,0.000015883836,0.000014439217,0.000067981055,0.000029781826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026620767,0.00024380191,0.00015178707,0.0003527571,0.0003641647,0.00040206758,0.00029480728,0.0002750126,0.00030980224],"category_scores_gemma":[0.00020392005,0.00008883866,0.00017050415,0.00052161637,0.0002584476,0.00014876867,0.00027632882,0.00017499745,0.00008404972],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00070754427,0.0005437395,0.599318,0.00030099467,0.00019086359,0.010174198,0.0019771487,0.045764983,0.21383438,0.0010337874,0.0050010243,0.12115327],"study_design_scores_gemma":[0.00008916623,0.00067611557,0.869563,0.000050257513,0.000118584554,0.0012960681,0.003997863,0.09578921,0.020909073,0.0002777002,0.007169332,0.00006366895],"about_ca_topic_score_codex":0.2183729,"about_ca_topic_score_gemma":0.48894134,"teacher_disagreement_score":0.7816271,"about_ca_system_score_codex":0.00069582474,"about_ca_system_score_gemma":0.00071864214,"threshold_uncertainty_score":0.43420362},"labels":[],"label_agreement":null},{"id":"W3138130580","doi":"10.1029/2020gl092263","title":"The Ocean Carbon Response to COVID‐Related Emissions Reductions","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"COVID-19 impact on air quality","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Science Foundation","keywords":"Environmental science; Carbon dioxide; Greenhouse gas; Coronavirus disease 2019 (COVID-19); Carbon dioxide in Earth's atmosphere; Atmospheric sciences; Carbon cycle; Atmosphere (unit); Carbon fibers; Climate change; Earth system science; Climatology; Meteorology; Oceanography; Chemistry; Geology; Geography; Ecology; Ecosystem; Computer science","score_opus":0.05065404539425998,"score_gpt":0.3878760330022869,"score_spread":0.3372219876080269,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138130580","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968911,0.00005212489,0.00091382675,0.00027626552,0.000025800222,0.0000075529774,0.00045777697,0.000050724084,0.0013248381],"genre_scores_gemma":[0.9993061,0.000020917863,0.0002553901,0.000038898113,0.000004776974,0.000005835922,0.0002599701,0.00000996325,0.00009818831],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9997781,0.000059752776,0.000011390223,0.00006516011,0.0000283379,0.00005716034],"domain_scores_gemma":[0.99938726,0.00024329858,0.00008801352,0.00010450359,0.00008968697,0.000087172906],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067948626,0.0004240909,0.0006163797,0.00030493728,0.0004888645,0.00083233917,0.0005546924,0.0009688142,0.0014262057],"category_scores_gemma":[0.0029598218,0.00030267774,0.00087237917,0.00038249203,0.00075283536,0.000829881,0.00087163056,0.0010130887,0.00010504262],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002465988,0.00013935608,0.06264759,0.0000409298,0.0002477347,0.00015247143,0.000041767253,0.9247756,0.0070866765,0.0015014288,0.00087317906,0.0022465861],"study_design_scores_gemma":[0.00011042961,0.0001988626,0.041927427,0.000011303688,0.000060884777,0.000042466138,0.00012879467,0.95249325,0.0029636698,0.0014551416,0.00055847707,0.000049286675],"about_ca_topic_score_codex":0.028980944,"about_ca_topic_score_gemma":0.012464165,"teacher_disagreement_score":0.028980944,"about_ca_system_score_codex":0.0008855939,"about_ca_system_score_gemma":0.0006972715,"threshold_uncertainty_score":0.05762452},"labels":[],"label_agreement":null},{"id":"W3138834838","doi":"10.1029/2020gl091540","title":"Limited Influence of Localized Tropical Sea‐Surface Temperatures on Moisture Transport into the Arctic","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Moisture; Climatology; Arctic; Environmental science; Sea surface temperature; Atmospheric sciences; Eddy; The arctic; Geology; Oceanography; Meteorology; Physics; Turbulence","score_opus":0.021664842130387756,"score_gpt":0.2903244390203762,"score_spread":0.2686595968899884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3138834838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971867,0.000024190187,0.0004341055,0.00005382127,0.000005665951,0.0000032936684,0.00012846092,0.000026833588,0.0021368298],"genre_scores_gemma":[0.99962723,0.000022461458,0.00008675531,0.000009155644,0.0000018706737,0.0000027575668,0.000044017976,0.000006834501,0.00019891412],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991834,0.00002560553,0.0000035224552,0.000019155064,0.0000063148514,0.000027011658],"domain_scores_gemma":[0.99970704,0.00017678205,0.000031193682,0.000024692901,0.000021723681,0.00003859116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019156898,0.00040180454,0.00038286013,0.00019329683,0.0003401518,0.0005895099,0.0003207331,0.00033662355,0.0021489912],"category_scores_gemma":[0.0007556623,0.00024439237,0.0004751212,0.00019787719,0.000477592,0.00042751996,0.0005752463,0.00040309943,0.000115104915],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026828548,0.00007588131,0.01454315,0.000036235953,0.0000649928,0.00019709501,0.000036824567,0.9710202,0.010647517,0.0009742364,0.00029968907,0.0018357307],"study_design_scores_gemma":[0.00014516801,0.000222676,0.022495056,0.000013609619,0.00007521893,0.00002982365,0.00011539616,0.97119033,0.0048027793,0.0006023627,0.00028542744,0.000022190972],"about_ca_topic_score_codex":0.03906985,"about_ca_topic_score_gemma":0.017178215,"teacher_disagreement_score":0.03906985,"about_ca_system_score_codex":0.00062345096,"about_ca_system_score_gemma":0.0008044162,"threshold_uncertainty_score":0.07768488},"labels":[],"label_agreement":null},{"id":"W3140593640","doi":"10.1029/2020gl091747","title":"Changes in Internal Wave‐Driven Mixing Across the Arctic Ocean: Finescale Estimates From an 18‐Year Pan‐Arctic Record","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Killam Trusts; National Science Foundation","keywords":"Sea ice; Arctic; Arctic ice pack; Drift ice; Arctic geoengineering; Arctic sea ice decline; Climatology; Internal wave; Hydrography; Geology; Proxy (statistics); Ice-albedo feedback; Oceanography; Environmental science; Atmospheric sciences","score_opus":0.036655567826528956,"score_gpt":0.3006252571027503,"score_spread":0.26396968927622133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3140593640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99778867,0.00008853955,0.00041761567,0.000020779313,0.0000046300133,0.000002134777,0.0013235775,0.000012146477,0.00034190866],"genre_scores_gemma":[0.99764305,0.00008933846,0.00045914465,0.000010028295,0.000008886103,0.0000048506254,0.0016661875,0.000005464205,0.00011295528],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999331,0.000010520014,0.00000793011,0.000025039957,0.000012396351,0.000010958747],"domain_scores_gemma":[0.9995172,0.000083903215,0.0001768935,0.000058998226,0.00011165869,0.00005127463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005031643,0.00019801383,0.00015176115,0.00068754045,0.00029456904,0.00058112596,0.00014639653,0.00019886091,0.00055182213],"category_scores_gemma":[0.0007105224,0.00014363356,0.0003504782,0.0006559773,0.00015533403,0.00033498392,0.00041241696,0.00023173942,0.00015751555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043136606,0.000023279821,0.9895705,0.000020076674,0.00012789466,0.000024874531,0.0001725494,0.0011944695,0.003249191,0.00004901256,0.0002929314,0.0052320543],"study_design_scores_gemma":[0.0000012204991,0.0000068104564,0.9984529,0.000004002641,0.000012252931,0.000011565636,0.000058203583,0.00090296764,0.00016778633,0.0000143651705,0.00036524006,0.0000025788977],"about_ca_topic_score_codex":0.02903062,"about_ca_topic_score_gemma":0.048429143,"teacher_disagreement_score":0.02903062,"about_ca_system_score_codex":0.00019542559,"about_ca_system_score_gemma":0.00015478212,"threshold_uncertainty_score":0.057723284},"labels":[],"label_agreement":null},{"id":"W3146278388","doi":"10.1029/2020gl091248","title":"The Seasonality of Global Land and Ocean Mass and the Changing Water Cycle","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; University of Saskatchewan","funders":"","keywords":"Water cycle; Environmental science; Climatology; Seasonality; Annual cycle; Cycling; Atmosphere (unit); Water mass; Global change; Atmospheric sciences; Oceanography; Climate change; Geology; Meteorology; Geography; Ecology","score_opus":0.02568013714741995,"score_gpt":0.26893954596332137,"score_spread":0.2432594088159014,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3146278388","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99818003,0.00006379334,0.00017100971,0.00008397408,0.000003664166,0.0000023022758,0.00031695567,0.00001209443,0.0011660922],"genre_scores_gemma":[0.99965584,0.000021203385,0.00005544339,0.0000100526695,0.0000030394888,0.000001026845,0.00013965332,0.0000024988065,0.00011118958],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999591,0.0000067266437,0.000002912749,0.0000120296345,0.0000084198355,0.000010834527],"domain_scores_gemma":[0.99982613,0.00004085612,0.00005235514,0.000014145564,0.000037916267,0.000028692957],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014047435,0.00007930099,0.000084687876,0.00045212812,0.0001214799,0.00032619995,0.000106898166,0.00013374546,0.0011255671],"category_scores_gemma":[0.00058815425,0.00005378504,0.00008827354,0.0005659857,0.0002321446,0.00020739272,0.0001607324,0.000112835674,0.0001335147],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016393863,0.00002828884,0.9642936,0.000022557766,0.000040278697,0.00015649849,0.00020312738,0.002482995,0.01979008,0.0006462705,0.00076324824,0.011409017],"study_design_scores_gemma":[0.000003034728,0.000017683347,0.9958643,0.0000018182227,0.000006436429,0.00004053445,0.000076135366,0.0024508294,0.0008443148,0.00014381309,0.000547571,0.0000035686637],"about_ca_topic_score_codex":0.005244965,"about_ca_topic_score_gemma":0.0074867015,"teacher_disagreement_score":0.005244965,"about_ca_system_score_codex":0.00021857608,"about_ca_system_score_gemma":0.00008998644,"threshold_uncertainty_score":0.0104289055},"labels":[],"label_agreement":null},{"id":"W3147189274","doi":"10.1029/2020gl091249","title":"Marine Electromagnetic Imaging and Volumetric Estimation of Freshwater Plumes Offshore Hawai'i","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Frontier Geosciences (Canada)","funders":"","keywords":"Submarine groundwater discharge; Electrical resistivity tomography; Biogeochemical cycle; Geology; Seafloor spreading; Oceanography; Water column; Plume; Submarine pipeline; Hydrogeology; Salinity; Seawater; Environmental science; Groundwater; Geophysics; Electrical resistivity and conductivity; Aquifer; Ecology","score_opus":0.01802683051650931,"score_gpt":0.27896776060344397,"score_spread":0.26094093008693464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3147189274","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911152,0.000058671576,0.0068264925,0.00004934191,0.000006321308,0.000011954621,0.00024572335,0.000076163225,0.00161004],"genre_scores_gemma":[0.99254155,0.00004322657,0.006829784,0.000015095059,0.000004010362,0.0000069867274,0.0001870299,0.0000066923008,0.00036554024],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999863,0.0000016739444,3.7979123e-7,0.000004749435,0.000003850643,0.000003059397],"domain_scores_gemma":[0.9999523,0.000011008073,0.000009184686,0.0000033464044,0.000015438314,0.000008642379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058957423,0.00018909814,0.00006881929,0.00039839192,0.00006634651,0.00017645989,0.00012298778,0.0001221506,0.00034977606],"category_scores_gemma":[0.00016696278,0.00009960058,0.00009899137,0.00021173853,0.000076406795,0.00012665839,0.00014973099,0.000117812866,0.00006304971],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026925575,0.0001030968,0.12531134,0.0000905479,0.00006793816,0.0006907609,0.00033671322,0.04510117,0.7483998,0.0005308368,0.001008687,0.07808979],"study_design_scores_gemma":[0.000058664053,0.00016752508,0.49070105,0.000030179786,0.0000706825,0.00035743354,0.0004937944,0.45442766,0.05164959,0.00041029582,0.0015811059,0.000052023457],"about_ca_topic_score_codex":0.0059521357,"about_ca_topic_score_gemma":0.009475678,"teacher_disagreement_score":0.0059521357,"about_ca_system_score_codex":0.00015687462,"about_ca_system_score_gemma":0.00012954223,"threshold_uncertainty_score":0.011834979},"labels":[],"label_agreement":null},{"id":"W3150637450","doi":"10.1029/2020gl092169","title":"First Simultaneous Observation of STEVE and SAR Arc Combining Data From Citizen Scientists, 630.0 nm All‐Sky Images, and Satellites","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Air Force Research Laboratory; Ames Laboratory; Air Force Office of Scientific Research; National Aeronautics and Space Administration; National Science Foundation","keywords":"Sky; Southern Hemisphere; Northern Hemisphere; Geology; Latitude; Satellite; Ionosphere; Arc (geometry); Remote sensing; Meteorology; Atmospheric sciences; Geodesy; Physics; Astronomy; Climatology; Geophysics","score_opus":0.04337712424743456,"score_gpt":0.3013273973762109,"score_spread":0.25795027312877633,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3150637450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98904186,0.000096113676,0.0014467089,0.00009414489,0.00001947854,0.000030892967,0.0022505946,0.00013025441,0.0068900078],"genre_scores_gemma":[0.98875976,0.00005983459,0.004510137,0.000056292545,0.000013008922,0.000016235537,0.0037622575,0.000026307682,0.0027961924],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983144,0.000009716455,0.000002470086,0.00003199266,0.00007490382,0.000049453338],"domain_scores_gemma":[0.9996872,0.000014687645,0.000027417533,0.000030276864,0.00017171704,0.00006867113],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027558688,0.00018344562,0.00018683955,0.00057164143,0.0006410992,0.0005365658,0.00019847241,0.00025664576,0.0010098736],"category_scores_gemma":[0.00023375308,0.00021266803,0.00014014723,0.00071074284,0.00021042852,0.00020983108,0.0004805003,0.0003833581,0.0002750134],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007413103,0.00022776407,0.62438977,0.00009046877,0.00022989241,0.0007253232,0.0015721807,0.0010202295,0.2715002,0.00038624555,0.0100466,0.089070015],"study_design_scores_gemma":[0.000012708121,0.000044969336,0.981584,0.000011549433,0.000028821078,0.000113668684,0.000525807,0.0013129426,0.009631393,0.000059137747,0.0066639604,0.00001101276],"about_ca_topic_score_codex":0.11310477,"about_ca_topic_score_gemma":0.48898238,"teacher_disagreement_score":0.11310477,"about_ca_system_score_codex":0.000725015,"about_ca_system_score_gemma":0.001299529,"threshold_uncertainty_score":0.22489285},"labels":[],"label_agreement":null},{"id":"W3150833021","doi":"10.1029/2021gl093207","title":"The Three‐Dimensional Light Field Within Sea Ice Ridges","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National d'Optique; Université Laval; Makivik Corporation","funders":"Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research; Norges Forskningsråd; Polarforskningssekretariatet","keywords":"Ridge; Light field; Geology; Distributed ray tracing; Ray tracing (physics); Field (mathematics); Light scattering; Transmittance; Monte Carlo method; Isotropy; Optics; Scattering; Physics; Paleontology","score_opus":0.021710854014313764,"score_gpt":0.2669173597280395,"score_spread":0.2452065057137257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3150833021","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97229385,0.000040187788,0.024415556,0.000063485524,0.000008819343,0.000015644073,0.00016619117,0.00020016376,0.0027960856],"genre_scores_gemma":[0.99774027,0.000023185952,0.0017664531,0.000008475219,0.0000028349684,0.0000062087506,0.00007427384,0.00002056751,0.00035776442],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992335,0.000016626269,0.0000028739112,0.000017282815,0.000017921684,0.000022002714],"domain_scores_gemma":[0.99976224,0.00008729973,0.0000308512,0.000021170725,0.00005999536,0.000038455477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022306238,0.00021028613,0.00024683648,0.0003861037,0.0003905134,0.00096648256,0.0002830256,0.00032393084,0.00070490764],"category_scores_gemma":[0.00047861948,0.0002545444,0.00036938462,0.0003314192,0.00058918295,0.00037642373,0.0003614765,0.0003219447,0.00009424183],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009606786,0.00010347073,0.015704276,0.000019567651,0.000027313383,0.00018759196,0.00012989144,0.9515497,0.024034135,0.0029979453,0.00021624775,0.004933816],"study_design_scores_gemma":[0.000022842165,0.000023553683,0.009941763,0.0000048652055,0.000005969565,0.000037093156,0.00004178362,0.9856602,0.0033243953,0.0007356993,0.00018284602,0.000018960221],"about_ca_topic_score_codex":0.012634624,"about_ca_topic_score_gemma":0.0043279435,"teacher_disagreement_score":0.012634624,"about_ca_system_score_codex":0.00077265233,"about_ca_system_score_gemma":0.0007935904,"threshold_uncertainty_score":0.025122166},"labels":[],"label_agreement":null},{"id":"W3153545921","doi":"10.1029/2021gl092889","title":"The Crustal Stress Field Inferred From Focal Mechanisms in Northern Chile","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Calgary; University of Victoria","funders":"Natural Resources Canada; Natural Sciences and Engineering Research Council of Canada; University of Victoria","keywords":"Geology; Crust; Seismology; Stress field; Focal mechanism; Compression (physics); Margin (machine learning); Slip (aerodynamics); Stress (linguistics); Continental margin; Geophysics; Tectonics","score_opus":0.0280776844329247,"score_gpt":0.27390957960832957,"score_spread":0.24583189517540488,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3153545921","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983139,0.00016647553,0.000102602906,0.000019603634,8.732186e-7,0.0000049730897,0.0004081583,0.000012887594,0.00097052014],"genre_scores_gemma":[0.9994647,0.0000764583,0.00006986282,0.0000021642977,0.0000012120596,0.0000052688392,0.00023058701,0.0000018476151,0.00014783234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999151,0.000010913265,0.000008445754,0.000023968749,0.00001681862,0.000024754445],"domain_scores_gemma":[0.9994823,0.000090856025,0.00019731004,0.000049190152,0.00011080258,0.000069560825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026525432,0.00020367597,0.00023735654,0.0022303136,0.0003141584,0.0007000573,0.00032351358,0.00020418853,0.0016661533],"category_scores_gemma":[0.0011253522,0.00019337848,0.0002362554,0.0015845206,0.00029765067,0.00033661808,0.0006902622,0.000121991114,0.00019321428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000099060606,0.000020998177,0.97988737,0.000065571985,0.000076590884,0.00033712146,0.00086280995,0.0019785028,0.0056620566,0.00020988777,0.00025678833,0.010543313],"study_design_scores_gemma":[0.0000073702095,0.000011091738,0.9971615,0.000017317196,0.000015282385,0.000068246,0.0005355268,0.0014649063,0.00023426041,0.000085418054,0.00039264586,0.0000065318363],"about_ca_topic_score_codex":0.036164932,"about_ca_topic_score_gemma":0.02903532,"teacher_disagreement_score":0.036164932,"about_ca_system_score_codex":0.0009280501,"about_ca_system_score_gemma":0.00049674045,"threshold_uncertainty_score":0.07190889},"labels":[],"label_agreement":null},{"id":"W3155202518","doi":"10.1029/2021gl095413","title":"Structure and Stress Field of the Lithosphere Between Pamir and Tarim","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Natural Environment Research Council; Sight Research UK","keywords":"Lithosphere; Geology; Slab; Induced seismicity; Seismology; Mantle (geology); Collision zone; Tarim basin; Stress field; Crust; Plateau (mathematics); Focal mechanism; Clockwise; Slab window; Geophysics; Subduction; Tectonics; Paleontology; Geometry","score_opus":0.01805791766745323,"score_gpt":0.2729232751220363,"score_spread":0.25486535745458305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155202518","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983078,0.000035624584,0.0000653015,0.000016483524,8.861222e-7,0.0000016870421,0.0000511627,0.000006481455,0.0015146133],"genre_scores_gemma":[0.9997271,0.000013679685,0.000053883097,0.0000032216594,0.0000011981458,0.0000011284061,0.000085730324,8.7466645e-7,0.00011325505],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999653,0.000003746557,0.0000017246584,0.000008630499,0.0000073977735,0.000013263787],"domain_scores_gemma":[0.99991155,0.000010661977,0.000024752302,0.000005450718,0.00002797956,0.000019507524],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008551645,0.00011601798,0.00012562923,0.0008338784,0.00035878195,0.00036691368,0.00020006248,0.00011623768,0.0014259341],"category_scores_gemma":[0.000242325,0.00009980157,0.000086205924,0.0007953524,0.00028405205,0.0001326247,0.00049819454,0.00012892067,0.00023327948],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006001094,0.00004859554,0.87987787,0.00008101902,0.00006127441,0.0008241333,0.002664645,0.001576448,0.06681931,0.001711139,0.00038924938,0.045346208],"study_design_scores_gemma":[0.0000056060458,0.000062685096,0.9970874,0.0000073617875,0.0000065608797,0.00012845143,0.0005974962,0.0009275135,0.0006895775,0.00014274009,0.00034112806,0.000003466962],"about_ca_topic_score_codex":0.0068385587,"about_ca_topic_score_gemma":0.008476891,"teacher_disagreement_score":0.0068385587,"about_ca_system_score_codex":0.00023947374,"about_ca_system_score_gemma":0.0002591281,"threshold_uncertainty_score":0.013597488},"labels":[],"label_agreement":null},{"id":"W3155442134","doi":"10.1029/2020gl092147","title":"Long‐Range Forecasting as a Past Value Problem: Untangling Correlations and Causality With Scaling","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Teleconnection; Causality (physics); Granger causality; Econometrics; Range (aeronautics); Statistical physics; Multivariate statistics; Scaling; Climatology; Mathematics; Statistics; Physics; Geology; El Niño Southern Oscillation","score_opus":0.06079440869520228,"score_gpt":0.30771614585119683,"score_spread":0.24692173715599455,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155442134","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.1991383,0.001607679,0.7793908,0.008546164,0.00027626188,0.000046969373,0.0003431563,0.00018751984,0.010463222],"genre_scores_gemma":[0.96340495,0.000623723,0.033803906,0.00021954725,0.0002607034,0.00006455631,0.000121749996,0.000042945907,0.001457849],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9987753,0.00069481035,0.00007147624,0.0002358454,0.00014394464,0.000078615165],"domain_scores_gemma":[0.9747995,0.021267558,0.0018268261,0.00088403927,0.0007367026,0.00048528652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0051274714,0.00056916854,0.0010012019,0.001019364,0.0008778872,0.002427557,0.0010591197,0.0015383088,0.0023388525],"category_scores_gemma":[0.026518704,0.000583234,0.0007990089,0.0014270099,0.0030899416,0.0047597536,0.001538407,0.0025827019,0.00009636156],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000032105872,0.000033993158,0.0039448626,0.000043036132,0.000050855215,0.00013011476,0.000094486866,0.6404251,0.00013534092,0.34395307,0.0013209553,0.009836125],"study_design_scores_gemma":[0.000005485406,0.000004291238,0.00029334816,0.000007535294,0.000003152489,0.000008376779,0.0000135802,0.78149945,0.000028853468,0.2179147,0.00021462445,0.000006664604],"about_ca_topic_score_codex":0.008588238,"about_ca_topic_score_gemma":0.0037145442,"teacher_disagreement_score":0.008588238,"about_ca_system_score_codex":0.0014079717,"about_ca_system_score_gemma":0.0012574531,"threshold_uncertainty_score":0.027117014},"labels":[],"label_agreement":null},{"id":"W3155815203","doi":"10.1029/2020gl091814","title":"Multidecadal Variability in Mediterranean Sea Surface Temperature and Its Sources","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Hohai University","keywords":"Atlantic multidecadal oscillation; North Atlantic oscillation; Climatology; Mediterranean climate; Mediterranean sea; Forcing (mathematics); Sea surface temperature; Environmental science; Lag; Oceanography; Climate change; Atlantic Equatorial mode; Geography; Geology","score_opus":0.040389267372456496,"score_gpt":0.3103774993165525,"score_spread":0.269988231944096,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3155815203","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954686,0.00062305725,0.0011611526,0.00018076405,0.00003881424,0.0000035961154,0.0013647812,0.000048319984,0.0011108351],"genre_scores_gemma":[0.99916315,0.00006863323,0.000111147296,0.000010405531,0.000017133812,0.000002422608,0.0004882701,0.0000050552385,0.0001339113],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999057,0.000015571366,0.00000925419,0.000040050476,0.00001717751,0.000012228937],"domain_scores_gemma":[0.99950814,0.000092502865,0.00016431737,0.00006856781,0.000117341995,0.000049107475],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043895913,0.00017213901,0.00016212044,0.0005430696,0.00012391456,0.0004733038,0.00013344736,0.0001775219,0.00073779834],"category_scores_gemma":[0.0010384303,0.00009204242,0.00031067064,0.0005573932,0.00007580429,0.00023373435,0.00047703783,0.00023784654,0.00015690514],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001349594,0.000024579711,0.9686402,0.00003491893,0.00035952995,0.00009276791,0.00016773205,0.0048567755,0.0037685048,0.0005829253,0.001022016,0.02031509],"study_design_scores_gemma":[0.0000031167021,0.0000110550445,0.99331504,0.0000075253665,0.000020031277,0.000027907701,0.00005014498,0.005118587,0.00021084503,0.00023385158,0.000996185,0.000005825155],"about_ca_topic_score_codex":0.0036677732,"about_ca_topic_score_gemma":0.0032692542,"teacher_disagreement_score":0.0036677732,"about_ca_system_score_codex":0.00025820476,"about_ca_system_score_gemma":0.000097280754,"threshold_uncertainty_score":0.0072928667},"labels":[],"label_agreement":null},{"id":"W3156740465","doi":"10.1029/2021gl093549","title":"Crustal Groundwater Volumes Greater Than Previously Thought","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":81,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Global Institute for Water Security; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; Jet Propulsion Laboratory","keywords":"Groundwater; Geology; Crust; Sedimentary rock; Continental crust; Earth science; Hydrology (agriculture); Geochemistry; Geotechnical engineering","score_opus":0.031067802071417582,"score_gpt":0.26874333634913916,"score_spread":0.2376755342777216,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156740465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9674004,0.005610979,0.0077082347,0.00038967346,0.00004748942,0.00001109582,0.0030348103,0.00033585337,0.015461519],"genre_scores_gemma":[0.9976205,0.0006118513,0.0008329537,0.000053150576,0.000008586702,0.0000027378326,0.00039743743,0.000009218928,0.00046360548],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99978346,0.000020850499,0.000011602019,0.00007986155,0.000057724064,0.00004656457],"domain_scores_gemma":[0.9996884,0.000055284312,0.00012791989,0.000040592087,0.000054081476,0.000033828866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021910794,0.0003645661,0.00029757776,0.0007554114,0.00022076395,0.0014409065,0.00040602544,0.00044738434,0.0029994836],"category_scores_gemma":[0.00073915545,0.00018206342,0.00026156413,0.0011571,0.0004118944,0.0013692818,0.0010384143,0.00036845403,0.00030769614],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004586839,0.000045356257,0.41411287,0.0011174767,0.00061260205,0.0010379205,0.001092298,0.025155753,0.39877263,0.02002938,0.0025939737,0.13497114],"study_design_scores_gemma":[0.00003630906,0.00029016085,0.7534442,0.0003940227,0.0003649536,0.002764332,0.0022172001,0.017509555,0.119514495,0.03120316,0.07209373,0.00016777823],"about_ca_topic_score_codex":0.005605556,"about_ca_topic_score_gemma":0.006484008,"teacher_disagreement_score":0.005605556,"about_ca_system_score_codex":0.0006125062,"about_ca_system_score_gemma":0.00039103677,"threshold_uncertainty_score":0.01114583},"labels":[],"label_agreement":null},{"id":"W3156749661","doi":"10.1029/2021gl092658","title":"Soil Moisture Active Passive Improves Global Soil Moisture Simulation in a Land Surface Scheme and Reveals Strong Irrigation Signals Over Farmlands","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil Moisture and Remote Sensing","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Toronto; Natural Resources Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency","keywords":"Environmental science; Water content; Irrigation; Evapotranspiration; Arid; Moisture; Infiltration (HVAC); Soil science; Agronomy; Meteorology; Geology","score_opus":0.017697141745267132,"score_gpt":0.3049312709495578,"score_spread":0.28723412920429064,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156749661","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699485,0.0000119235165,0.0021389842,0.000035144465,0.0000067878113,0.000005541038,0.00020106068,0.000187483,0.0004182121],"genre_scores_gemma":[0.99828315,0.0000061931646,0.0014523193,0.0000087073895,0.0000018670614,0.0000025698155,0.00014334219,0.000016816106,0.000085126994],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993646,0.000016742772,0.0000041294743,0.000021082533,0.000009492624,0.000012003417],"domain_scores_gemma":[0.9998398,0.000047178837,0.000020364607,0.00004267931,0.00002464724,0.000025330486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002605342,0.00030478527,0.0002527924,0.00015328618,0.00012087429,0.00033257256,0.0003433519,0.00031122292,0.00074862345],"category_scores_gemma":[0.00047619303,0.00012671686,0.00031863898,0.0002058005,0.0002406339,0.00044630875,0.00024325048,0.00028103206,0.00008008709],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005568387,0.00032359778,0.09573971,0.00007517494,0.00020804566,0.00022187714,0.00011361486,0.78086734,0.09218125,0.0007392873,0.0007740404,0.028199103],"study_design_scores_gemma":[0.00005607706,0.000117330615,0.040056307,0.0000025021914,0.00001700155,0.000010484166,0.00002097358,0.9537613,0.0055856523,0.00013257266,0.0002296786,0.000010129565],"about_ca_topic_score_codex":0.009771263,"about_ca_topic_score_gemma":0.007765491,"teacher_disagreement_score":0.009771263,"about_ca_system_score_codex":0.00022309048,"about_ca_system_score_gemma":0.0002467687,"threshold_uncertainty_score":0.01942879},"labels":[],"label_agreement":null},{"id":"W3156804144","doi":"10.1029/2020gl092113","title":"Fossil Reefs Reveal Temporally Distinct Late Holocene Lagoonal Reef Shutdown Episodes at Kiritimati Island, Central Pacific","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Marsden Fund; University of Auckland; Royal Society Te Apārangi; Royal Society","keywords":"Reef; Atoll; Holocene; Acropora; Geology; Coral reef; Oceanography; Environmental issues with coral reefs; Fringing reef; Porites; Coral; Resilience of coral reefs; Paleontology","score_opus":0.026310765751523246,"score_gpt":0.2729402453283583,"score_spread":0.24662947957683506,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3156804144","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877864,0.0000407582,0.00002728189,0.000010793773,0.0000010630653,0.0000023897449,0.0002837126,0.0000032307012,0.0008521283],"genre_scores_gemma":[0.99934953,0.00004179513,0.000056142733,0.000003724662,9.868421e-7,0.000003854112,0.00029194253,0.0000012075751,0.00025076172],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999956,0.000001969921,0.0000031068944,0.000010283692,0.000007958984,0.000020619162],"domain_scores_gemma":[0.99976784,0.000019383819,0.00008129294,0.000014669901,0.000040956726,0.00007582655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013459958,0.0001468278,0.00010439743,0.0010691651,0.0006841156,0.00047194574,0.0002839976,0.0001684835,0.00213872],"category_scores_gemma":[0.00037962242,0.00013358805,0.00008443918,0.00097286835,0.00037720273,0.00024807724,0.0007000267,0.00019107005,0.00013856014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000057454818,0.000012577497,0.9895536,0.000017798775,0.000012320729,0.00023639831,0.0010426103,0.00010664192,0.002802112,0.000052907908,0.00019020628,0.0059154932],"study_design_scores_gemma":[3.8174335e-7,0.0000034257607,0.99944276,0.0000018362848,0.0000015178382,0.000024893781,0.00033368295,0.000028750994,0.000039297724,0.000003980377,0.000118663316,6.881591e-7],"about_ca_topic_score_codex":0.11975108,"about_ca_topic_score_gemma":0.33257535,"teacher_disagreement_score":0.11975108,"about_ca_system_score_codex":0.000577481,"about_ca_system_score_gemma":0.0004916122,"threshold_uncertainty_score":0.23810816},"labels":[],"label_agreement":null},{"id":"W3157370717","doi":"10.1029/2021gl093231","title":"On the Relevance of Geodetic Deformation Rates to Earthquake Potential","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Seismology; Geodetic datum; Geology; Viscoelasticity; Slip (aerodynamics); Strain rate; Geodesy; Deformation (meteorology); Fault (geology); Engineering","score_opus":0.03083872391617542,"score_gpt":0.28070972160211727,"score_spread":0.24987099768594184,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3157370717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.956867,0.0024724186,0.0035595305,0.0045197397,0.0001086966,0.000013771544,0.00042335238,0.000037783524,0.0319977],"genre_scores_gemma":[0.99931157,0.00016045767,0.000072260234,0.000053787302,0.000059005382,0.0000011714941,0.000033877768,0.000007859376,0.00030010822],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9992755,0.00042543808,0.00003131509,0.00013638195,0.000077415105,0.000053898122],"domain_scores_gemma":[0.95342016,0.038631976,0.0034247558,0.0014674952,0.0018737679,0.0011819362],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027730009,0.00022032362,0.00022497853,0.0013530253,0.00031867056,0.0019865949,0.0006178578,0.00077477464,0.004160007],"category_scores_gemma":[0.04435317,0.0001599949,0.00023477874,0.0012882622,0.0019738579,0.0017124385,0.0010072485,0.0011542992,0.00052756065],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074223493,0.000059217084,0.90039986,0.00016264143,0.00013224533,0.00061608804,0.00090787024,0.011701475,0.002768626,0.041541617,0.0017173681,0.03925075],"study_design_scores_gemma":[0.000016489726,0.0001564348,0.9400409,0.00009022523,0.00008813079,0.0005394013,0.0013770418,0.014826056,0.0009976,0.039957397,0.0018753164,0.000034978595],"about_ca_topic_score_codex":0.0022800812,"about_ca_topic_score_gemma":0.0014504375,"teacher_disagreement_score":0.004160007,"about_ca_system_score_codex":0.0003364729,"about_ca_system_score_gemma":0.00022295566,"threshold_uncertainty_score":0.014665186},"labels":[],"label_agreement":null},{"id":"W3158311660","doi":"10.1029/2021gl093126","title":"Thank You to Our 2020 Peer Reviewers","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Scientific Research and Technology","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Peer review; Data science; Computer science; Political science","score_opus":0.062162915382245686,"score_gpt":0.3761836360795861,"score_spread":0.31402072069734044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158311660","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0024954004,0.011469902,0.00717754,0.20089947,0.70103747,0.0015157454,0.004161002,0.0039632986,0.0672802],"genre_scores_gemma":[0.011099599,0.009275269,0.013970465,0.045079272,0.1509819,0.001452009,0.0044727162,0.0046451264,0.75902367],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9697869,0.0058046784,0.002450303,0.0025994352,0.017995369,0.0013633322],"domain_scores_gemma":[0.5045705,0.011996394,0.0076846066,0.01151445,0.4463368,0.017897291],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.018474076,0.0018007992,0.0026819508,0.008293618,0.005279125,0.017337026,0.0029177496,0.005428712,0.25574446],"category_scores_gemma":[0.1805969,0.0011077657,0.0014831538,0.003631006,0.0021811312,0.006103379,0.00512282,0.0057203392,0.3417616],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002448053,0.00001114737,0.00021627091,0.00012743482,0.000007886335,0.00008567882,0.0000661079,0.000018289,0.00019277568,0.00025929575,0.97913647,0.019854186],"study_design_scores_gemma":[0.000018046549,0.000013216567,0.0005620152,0.00015927553,0.000018143412,0.00018648704,0.00035706602,0.00011175407,0.00021091785,0.0007589915,0.99757105,0.000032968383],"about_ca_topic_score_codex":0.0046704197,"about_ca_topic_score_gemma":0.011460702,"teacher_disagreement_score":0.9815259,"about_ca_system_score_codex":0.0024226406,"about_ca_system_score_gemma":0.011561217,"threshold_uncertainty_score":0.8555504},"labels":[{"model":"gemma","categories":[],"domain":null,"study_design":"not_applicable","genre":"editorial","about_ca_system":false,"about_ca_topic":false,"confidence":"low"},{"model":"gpt","categories":[],"domain":null,"study_design":"not_applicable","genre":"editorial","about_ca_system":false,"about_ca_topic":false,"confidence":"high"}],"label_agreement":"agree"},{"id":"W3158402404","doi":"10.1029/2020gl092091","title":"Inland Tidal Oscillations Within the Yucatan Peninsula","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; University of Waterloo","funders":"","keywords":"Geology; Aquifer; Peninsula; Cave; Flood myth; Hydrology (agriculture); Sediment; Water level; Oceanography; Groundwater; Geomorphology; Geotechnical engineering; Geography; Archaeology","score_opus":0.03114213605513714,"score_gpt":0.300814038805443,"score_spread":0.26967190275030584,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158402404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946016,0.000016190741,0.00003262626,0.000014285882,7.601351e-7,0.0000014173403,0.00016022983,0.0000038989556,0.00031053185],"genre_scores_gemma":[0.99948883,0.000014125912,0.000039605573,0.00000645781,8.943215e-7,0.0000022436373,0.00030746954,0.0000012801844,0.00013902807],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000082248525,0.000003474733,0.000012090546,0.0000065655718,0.000012416516],"domain_scores_gemma":[0.99967957,0.000055653374,0.000061682746,0.000030201192,0.00011709927,0.000055747507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012679941,0.00010412712,0.00015166699,0.00059851474,0.00041311228,0.0005169205,0.00018885867,0.00014869521,0.0008384571],"category_scores_gemma":[0.00033800877,0.00008358956,0.00008043932,0.0009085715,0.0002335018,0.00014522321,0.0003361723,0.000099402845,0.000091542606],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005400777,0.000025465159,0.9892117,0.000011051065,0.000042771244,0.00013028088,0.00048393328,0.00047761181,0.0038138302,0.00009634917,0.00029210755,0.005360985],"study_design_scores_gemma":[0.0000013866471,0.0000032565658,0.9991848,0.0000014932724,0.0000032550658,0.000011270732,0.000164412,0.00041664188,0.000056586796,0.000016334247,0.0001393566,0.0000012735198],"about_ca_topic_score_codex":0.10980578,"about_ca_topic_score_gemma":0.19546229,"teacher_disagreement_score":0.10980578,"about_ca_system_score_codex":0.0006253911,"about_ca_system_score_gemma":0.00048690313,"threshold_uncertainty_score":0.21833324},"labels":[],"label_agreement":null},{"id":"W3158601690","doi":"10.1029/2021gl095108","title":"Surface Deformation and Seismicity Induced by Poroelastic Stress at the Raft River Geothermal Field, Idaho, USA","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Science Foundation","keywords":"Induced seismicity; Geology; Poromechanics; Geothermal gradient; Pore water pressure; Basement; Seismology; Stress field; Geotechnical engineering; Geomorphology; Geophysics; Porosity; Porous medium","score_opus":0.028176851456275333,"score_gpt":0.2677490307637777,"score_spread":0.23957217930750238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158601690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99652725,0.000015613747,0.00023096241,0.00008014577,0.0000039125225,0.0000069389994,0.0013203985,0.000056603603,0.0017582101],"genre_scores_gemma":[0.9985672,0.000018824909,0.0002602471,0.000016677675,0.0000031726008,0.0000084269805,0.00080145686,0.000005659928,0.00031816424],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.000010009497,0.0000040249793,0.000021457725,0.000012733387,0.000012666108],"domain_scores_gemma":[0.99982184,0.000038665068,0.0000341401,0.000024141702,0.00005427394,0.000027026752],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018325071,0.00016072579,0.00012483512,0.0006384231,0.00025006823,0.00032750782,0.00033855927,0.00022753314,0.001177662],"category_scores_gemma":[0.00046030985,0.000122070254,0.00016516856,0.0005185953,0.00020765627,0.00016959937,0.0002480931,0.00018417121,0.00020181804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002633747,0.0001413905,0.94762933,0.00004491763,0.000096518204,0.00027621762,0.00025779824,0.023693,0.009614568,0.00021616607,0.0018903114,0.015876463],"study_design_scores_gemma":[0.000017523036,0.000026089707,0.96842366,0.0000088680135,0.000017370263,0.00004263329,0.00023666523,0.029506652,0.0012000002,0.00006254848,0.000448462,0.000009390556],"about_ca_topic_score_codex":0.08944924,"about_ca_topic_score_gemma":0.15679495,"teacher_disagreement_score":0.08944924,"about_ca_system_score_codex":0.0008302444,"about_ca_system_score_gemma":0.0005182795,"threshold_uncertainty_score":0.17785716},"labels":[],"label_agreement":null},{"id":"W3158820340","doi":"10.1029/2021gl093058","title":"Prospect of Increased Disruption to the QBO in a Changing Climate","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":89,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Engineering and Physical Sciences Research Council; Natural Environment Research Council; Sight Research UK","keywords":"Predictability; Quasi-biennial oscillation; Northern Hemisphere; Climatology; Stratosphere; Momentum (technical analysis); Environmental science; Oscillation (cell signaling); Atmospheric sciences; Flux (metallurgy); High latitude; Latitude; Geology; Physics; Geodesy; Biology","score_opus":0.026530016366566368,"score_gpt":0.29534946608627116,"score_spread":0.2688194497197048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3158820340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98627496,0.000285768,0.0014365516,0.0058278185,0.00015173014,0.0000073661495,0.00039864553,0.000075837546,0.0055412734],"genre_scores_gemma":[0.9994229,0.000045670455,0.0001140306,0.00017216004,0.000035053166,0.0000013728438,0.000060473467,0.0000048710826,0.00014342525],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998325,0.000035434947,0.000007580539,0.000034714463,0.00002915914,0.000060511524],"domain_scores_gemma":[0.9992015,0.000106192114,0.00024797517,0.00007242501,0.00014531113,0.00022659697],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006119854,0.00011192129,0.00015933736,0.00023504886,0.00066520885,0.0014305089,0.00025011352,0.0009939986,0.0025080054],"category_scores_gemma":[0.0018187749,0.00012232123,0.00017825312,0.0002472423,0.00067852344,0.0008710183,0.00084554707,0.0009796671,0.00025565957],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001485957,0.00026895083,0.8886364,0.00013584257,0.00020579722,0.0024081217,0.0017252319,0.014168626,0.025546575,0.020082908,0.0096146,0.035720944],"study_design_scores_gemma":[0.00006373394,0.00033298854,0.93321437,0.00006725806,0.000054592776,0.00046417362,0.0042243456,0.020492818,0.0025257326,0.014246036,0.024238653,0.00007529471],"about_ca_topic_score_codex":0.008016881,"about_ca_topic_score_gemma":0.008181709,"teacher_disagreement_score":0.008016881,"about_ca_system_score_codex":0.0008182235,"about_ca_system_score_gemma":0.00039711728,"threshold_uncertainty_score":0.015940428},"labels":[],"label_agreement":null},{"id":"W3159146448","doi":"10.1029/2020gl091957","title":"Hygrometric Control on the Lithosphere‐Asthenosphere Boundary: A 28 Million Year Record From the Canadian Cordillera","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Lithosphere; Geology; Mantle (geology); Asthenosphere; Peridotite; Intraplate earthquake; Geothermal gradient; Plate tectonics; Convergent boundary; Geophysics; Seismology; Tectonics; Petrology; Subduction; Oceanic crust","score_opus":0.02769437541974641,"score_gpt":0.23610815418323006,"score_spread":0.20841377876348366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159146448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9929369,0.00097477913,0.00009460501,0.00018599852,0.000004955421,0.000008943201,0.0021773179,0.00001597675,0.0036005145],"genre_scores_gemma":[0.99814165,0.00029158773,0.00011842647,0.000027088641,0.000003934661,0.00000385837,0.0007887004,0.000004381163,0.0006203653],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985373,0.0000070961955,0.0000063991806,0.000045497556,0.000042693868,0.000044496795],"domain_scores_gemma":[0.9993038,0.000036163743,0.00013343472,0.000034340846,0.000382226,0.00010992351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021024421,0.000252757,0.00022642163,0.0023258496,0.0014170139,0.00083600514,0.00053018826,0.00034231253,0.0020695934],"category_scores_gemma":[0.0006955555,0.00015888811,0.00013700173,0.0025830236,0.0006985369,0.00028506014,0.0007360609,0.0002703268,0.0002029856],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000087578555,0.000011882981,0.97370934,0.000060090282,0.00008594518,0.0002260828,0.0019469855,0.00032122157,0.006340335,0.00045222839,0.0010678855,0.015690424],"study_design_scores_gemma":[8.853397e-7,0.0000020857026,0.99816173,0.0000075595904,0.0000051430534,0.000024910405,0.0001696902,0.00006882846,0.00012005201,0.000010702405,0.0014252282,0.0000031447971],"about_ca_topic_score_codex":0.95763123,"about_ca_topic_score_gemma":0.98248994,"teacher_disagreement_score":0.04236877,"about_ca_system_score_codex":0.006556847,"about_ca_system_score_gemma":0.0034324392,"threshold_uncertainty_score":0.08523655},"labels":[],"label_agreement":null},{"id":"W3159342690","doi":"10.1029/2020gl091741","title":"Future Sea Level Change Under Coupled Model Intercomparison Project Phase 5 and Phase 6 Scenarios From the Greenland and Antarctic Ice Sheets","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":151,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"University at Buffalo; Los Alamos National Laboratory; National Nuclear Security Administration; European Commission; Sight Research UK; Natural Environment Research Council; U.S. Department of Energy","keywords":"Coupled model intercomparison project; Climatology; Future sea level; Ice sheet; Climate model; Environmental science; Sea ice; Cryosphere; Greenland ice sheet; Forcing (mathematics); Antarctic ice sheet; Snow; Climate change; Ice-sheet model; Atmospheric sciences; Geology; Oceanography; Antarctic sea ice","score_opus":0.17090176936223486,"score_gpt":0.3565371790614722,"score_spread":0.18563540969923734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159342690","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9873717,0.000087164895,0.0011259635,0.0003317871,0.000052306495,0.000027680626,0.008887111,0.0000818904,0.002034569],"genre_scores_gemma":[0.98525316,0.0000687049,0.001337952,0.000119072334,0.000014176518,0.00006258506,0.0128185,0.000016339774,0.00030951004],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996394,0.0001703175,0.000020143247,0.00005854413,0.000051516727,0.000060088303],"domain_scores_gemma":[0.99934703,0.00022445261,0.00010731144,0.0000671434,0.00017759102,0.0000764119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018372813,0.00065013615,0.00036000664,0.00049797073,0.0003396175,0.000867425,0.00060594315,0.00068330206,0.0013298874],"category_scores_gemma":[0.0017492389,0.00021834945,0.0012990519,0.0009257019,0.00024339758,0.00073330203,0.00052117184,0.00051460526,0.00021798004],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.002166787,0.00030280108,0.26761532,0.00024043207,0.0015261353,0.00056201057,0.0002094067,0.6953161,0.004837735,0.0030791261,0.010034651,0.014109607],"study_design_scores_gemma":[0.0011099421,0.0007030128,0.42701274,0.00010326954,0.0007491716,0.00018507078,0.0005363634,0.5492818,0.009366502,0.0036401474,0.0071238424,0.00018811811],"about_ca_topic_score_codex":0.032190386,"about_ca_topic_score_gemma":0.02439409,"teacher_disagreement_score":0.032190386,"about_ca_system_score_codex":0.0010795791,"about_ca_system_score_gemma":0.00093542103,"threshold_uncertainty_score":0.06400603},"labels":[],"label_agreement":null},{"id":"W3159569931","doi":"10.1029/2021gl092831","title":"On the Optimal Design of Field Significance Tests for Changes in Climate Extremes","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Pacific Institute for Climate Solutions; University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Precipitation; Climate change; Climatology; Environmental science; Extreme value theory; Field (mathematics); Statistics; Econometrics; Meteorology; Mathematics; Geography; Geology","score_opus":0.11599582094614311,"score_gpt":0.34568093454867005,"score_spread":0.22968511360252694,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159569931","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.04687449,0.00022804725,0.94981164,0.00027551648,0.000054173874,0.0009003846,0.00014867239,0.00055831985,0.0011488287],"genre_scores_gemma":[0.4148775,0.00016271116,0.58191013,0.00015142112,0.00011485538,0.0017260624,0.00041133352,0.00013635395,0.0005096575],"study_design_codex":"design_other","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9559996,0.03775249,0.0012800161,0.0028988486,0.001384224,0.0006847905],"domain_scores_gemma":[0.52671105,0.44541198,0.008628365,0.0076297624,0.008854225,0.0027645426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.080500335,0.0014537256,0.0034344592,0.0039692125,0.0009845532,0.0020314956,0.0023785478,0.0021115267,0.004154754],"category_scores_gemma":[0.2573158,0.0013693243,0.0010213674,0.001754019,0.0032782073,0.0041353386,0.0030479885,0.0028245207,0.0006423089],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.007853839,0.0010623,0.032676302,0.0012738317,0.0007466356,0.0008526233,0.0009413674,0.3245033,0.010650126,0.13702738,0.004597133,0.4778152],"study_design_scores_gemma":[0.0011755266,0.0033021027,0.010086958,0.00025084463,0.00015966521,0.00026629466,0.00038432286,0.8087029,0.008312101,0.16403167,0.0031688786,0.00015876195],"about_ca_topic_score_codex":0.0013114149,"about_ca_topic_score_gemma":0.001006018,"teacher_disagreement_score":0.080500335,"about_ca_system_score_codex":0.0010721157,"about_ca_system_score_gemma":0.0036947886,"threshold_uncertainty_score":0.42573154},"labels":[],"label_agreement":null},{"id":"W3159693898","doi":"10.1029/2021gl092509","title":"Significant Contribution of Severe Ozone Loss to the Siberian‐Arctic Surface Warming in Spring 2020","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Environmental science; Albedo (alchemy); Climatology; Ozone; Atmospheric sciences; Ozone depletion; Arctic; Stratosphere; Ice-albedo feedback; Arctic oscillation; Global warming; Ozone layer; Arctic geoengineering; Arctic ice pack; Climate change; Sea ice; Northern Hemisphere; Geology; Meteorology; Oceanography; Geography","score_opus":0.02070764902751311,"score_gpt":0.27212631672698234,"score_spread":0.25141866769946924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3159693898","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980508,0.0003414098,0.00010574531,0.00015497774,0.000024808025,0.000002314987,0.0006166402,0.000014061293,0.0006890826],"genre_scores_gemma":[0.99892515,0.00011014288,0.000037438258,0.0000316489,0.000012749806,0.0000025493969,0.000621659,0.0000021055114,0.0002564577],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990916,0.0000127029625,0.000007214912,0.000018793253,0.000022871855,0.000029224213],"domain_scores_gemma":[0.99983025,0.000017587998,0.000059077065,0.000012534574,0.000037319252,0.000043166423],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038434519,0.00037541834,0.0002730203,0.00042969768,0.00048392612,0.0006634807,0.00013369879,0.00026662071,0.0010292797],"category_scores_gemma":[0.00035226412,0.000098697856,0.00036078933,0.00037918027,0.00014470403,0.00022738762,0.00051587063,0.00033787408,0.00016386216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029196925,0.00004272161,0.97203773,0.000050691768,0.0002680127,0.00028201455,0.0001503574,0.0019613102,0.013404724,0.00011007351,0.0006717961,0.010728568],"study_design_scores_gemma":[0.0000012404062,0.0000114844315,0.9986022,0.000002446413,0.00001634044,0.000021401567,0.000050385937,0.0005530124,0.0003622669,0.000028084249,0.0003492897,0.0000019380423],"about_ca_topic_score_codex":0.027863732,"about_ca_topic_score_gemma":0.024235288,"teacher_disagreement_score":0.027863732,"about_ca_system_score_codex":0.00071155274,"about_ca_system_score_gemma":0.00056129065,"threshold_uncertainty_score":0.055403113},"labels":[],"label_agreement":null},{"id":"W3164167078","doi":"10.1029/2021gl092904","title":"Dissolved Organic Radiocarbon in the Eastern Pacific and Southern Oceans","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"American Chemical Society Petroleum Research Fund; Canada Research Chairs; National Science Foundation; American Chemical Society; Kavli Foundation; National Oceanic and Atmospheric Administration","keywords":"Dissolved organic carbon; Oceanography; Radiocarbon dating; Seawater; Geology; Circumpolar deep water; Ridge; Total organic carbon; Deep sea; Pacific ocean; Environmental science; Deep water; Environmental chemistry; North Atlantic Deep Water; Chemistry","score_opus":0.02226081341269788,"score_gpt":0.2405582450012179,"score_spread":0.21829743158852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3164167078","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958925,0.00047121762,0.000044322118,0.00004523781,0.000010965503,0.0000036484653,0.0013123652,0.000003896712,0.002215735],"genre_scores_gemma":[0.9961915,0.0006141982,0.00016999913,0.000055592955,0.000015720843,0.000009443526,0.0018685884,0.000003663509,0.0010713615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990094,0.000010903529,0.000007497067,0.000030777926,0.000029272562,0.000020580877],"domain_scores_gemma":[0.99949133,0.00005445729,0.0001775154,0.000021348123,0.00017722546,0.000078117984],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030648377,0.00020534771,0.000108920285,0.001100232,0.00031259764,0.00053987466,0.00013207056,0.00010455454,0.0009576223],"category_scores_gemma":[0.00064635667,0.00009532834,0.000091390146,0.0015051479,0.00022702734,0.00021213785,0.0003966372,0.00016007302,0.00014864275],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005619913,0.000008136649,0.9914664,0.000016551721,0.000030164709,0.00007257368,0.00020374397,0.000070780705,0.001417939,0.00004781148,0.00014816597,0.0064614583],"study_design_scores_gemma":[0.0000011712833,0.0000060229945,0.9989717,0.000003845482,0.0000044560834,0.000018367002,0.0001439864,0.000020458067,0.00008070491,0.0000066166695,0.00074171653,0.0000010422907],"about_ca_topic_score_codex":0.11010071,"about_ca_topic_score_gemma":0.16111046,"teacher_disagreement_score":0.11010071,"about_ca_system_score_codex":0.0004342226,"about_ca_system_score_gemma":0.00047616762,"threshold_uncertainty_score":0.2189197},"labels":[],"label_agreement":null},{"id":"W3167530115","doi":"10.1029/2021gl093526","title":"On Rates of Isopycnal Dispersion at the Submesoscale","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography","funders":"National Science Foundation","keywords":"Isopycnal; Dispersion (optics); Geology; Power law; Thermal diffusivity; Meteorology; Mineralogy; Mechanics; Atmospheric sciences; Physics; Thermodynamics; Mathematics; Climatology; Optics; Statistics","score_opus":0.02897016927899237,"score_gpt":0.27717054186713985,"score_spread":0.24820037258814748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3167530115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995453,0.000012318114,0.00014792028,0.000003769539,4.8911636e-7,0.0000011243676,0.00005548756,0.000003560507,0.00023011987],"genre_scores_gemma":[0.99954337,0.0000058549863,0.00013200249,0.0000010088122,6.846997e-7,0.0000024041196,0.00016068801,0.0000028934517,0.00015108912],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99979466,0.000046331163,0.0000115354005,0.00006362187,0.00004814445,0.00003564768],"domain_scores_gemma":[0.9986517,0.00047187376,0.00031922976,0.0001888713,0.00023607271,0.00013219942],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004671755,0.00015275946,0.00020495999,0.00079612696,0.0002617537,0.00032760022,0.00022636833,0.00017518442,0.00082110957],"category_scores_gemma":[0.0021424824,0.0001108902,0.00013170649,0.00031044293,0.0002717162,0.00037613968,0.00047335183,0.0002600917,0.0002102386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000512561,0.00013395779,0.8707579,0.000044764154,0.00013149742,0.00017841655,0.0006681774,0.008419676,0.097988024,0.0010677597,0.00031545854,0.019781778],"study_design_scores_gemma":[0.000006751859,0.00017169959,0.97141945,0.000004135169,0.000017632616,0.00017853967,0.00017665242,0.015521149,0.011767982,0.00026179964,0.00045667248,0.00001755292],"about_ca_topic_score_codex":0.0024344458,"about_ca_topic_score_gemma":0.0030881236,"teacher_disagreement_score":0.0024344458,"about_ca_system_score_codex":0.0003519902,"about_ca_system_score_gemma":0.00007910635,"threshold_uncertainty_score":0.004840553},"labels":[],"label_agreement":null},{"id":"W3167764780","doi":"10.1029/2021gl094739","title":"Surface Salinity Under Transitioning Ice Cover in the Canada Basin: Climate Model Biases Linked to Vertical Distribution of Fresh Water","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Fisheries and Oceans Canada; McGill University; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK; U.S. Department of Energy; National Science Foundation","keywords":"Climate model; Climatology; Sea ice; Arctic; Arctic ice pack; Environmental science; Geology; Climate change; Oceanography; Atmospheric sciences","score_opus":0.042754397999017944,"score_gpt":0.2802765896928383,"score_spread":0.23752219169382036,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3167764780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984358,0.00004796343,0.00014309133,0.00011826056,0.0000053901867,0.0000052149253,0.00062842254,0.000028426715,0.000587528],"genre_scores_gemma":[0.999164,0.00003940643,0.00012310053,0.000021083288,0.000001532154,0.0000026454118,0.00048496327,0.000008950618,0.00015435924],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998241,0.00003467969,0.000007942422,0.000047231173,0.000028731012,0.000057345995],"domain_scores_gemma":[0.9992853,0.00021298106,0.0000826891,0.000051107356,0.0002389956,0.00012897754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006564554,0.0005100206,0.00029632216,0.00034461165,0.00077155675,0.0012735649,0.00096290355,0.00057497603,0.0009531034],"category_scores_gemma":[0.0022407158,0.00026387506,0.0005617496,0.0005503577,0.000683689,0.00048989494,0.00047935895,0.00050364586,0.00009591693],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004901143,0.00015982003,0.574297,0.000045148583,0.00035998732,0.000120906865,0.0002535205,0.41398072,0.0034175792,0.0009511214,0.0018008432,0.0041233115],"study_design_scores_gemma":[0.00014170831,0.00006511434,0.38142246,0.000027906366,0.00014499083,0.000028200306,0.0004227076,0.6141068,0.0020892892,0.0004220838,0.0010658667,0.00006280058],"about_ca_topic_score_codex":0.9544505,"about_ca_topic_score_gemma":0.92548835,"teacher_disagreement_score":0.045549512,"about_ca_system_score_codex":0.010159659,"about_ca_system_score_gemma":0.00837005,"threshold_uncertainty_score":0.091635466},"labels":[],"label_agreement":null},{"id":"W3169630250","doi":"10.1029/2021gl094442","title":"Nutrient Supply to Planetary Biospheres From Anoxic Weathering of Mafic Oceanic Crust","year":2021,"lang":"en","type":"preprint","venue":"Geophysical Research Letters","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Department of Geology and Geophysics, Yale University; National Aeronautics and Space Administration","keywords":"Weathering; Anoxic waters; Biosphere; Phosphorus; Sink (geography); Earth science; Mafic; Nutrient; Environmental science; Geochemistry; Geology; Environmental chemistry; Oceanography; Chemistry; Ecology","score_opus":0.03638831547600695,"score_gpt":0.27927621178972495,"score_spread":0.242887896313718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3169630250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985997,0.0003063067,0.00023979408,0.00002852089,0.000004038223,0.0000023519053,0.00008252101,0.000010722112,0.000725883],"genre_scores_gemma":[0.9989825,0.00012864759,0.0002913884,0.000014047559,0.0000025085087,0.0000024742903,0.00013695106,0.000004674352,0.00043684614],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994504,0.0000050850244,0.0000033727868,0.0000206379,0.000015321377,0.000010486904],"domain_scores_gemma":[0.99989796,0.000032498287,0.000022966546,0.000010045002,0.00001541698,0.000021131276],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012284689,0.00022364953,0.00020267772,0.00034935717,0.00019180731,0.00039533203,0.00018670529,0.00031591032,0.0013131365],"category_scores_gemma":[0.0002468381,0.00011734567,0.00011423594,0.00024222843,0.00028486943,0.00027166543,0.00028973154,0.00029635636,0.00014531783],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020923812,0.000015490123,0.025764696,0.000076608456,0.000025553338,0.00017894951,0.00008258739,0.00025186373,0.9676519,0.00015765471,0.000039269675,0.005546237],"study_design_scores_gemma":[0.00002945067,0.0004097391,0.49818575,0.00002061517,0.00006206001,0.0004820026,0.00046401678,0.00406763,0.4891994,0.0007258482,0.006333874,0.00001970726],"about_ca_topic_score_codex":0.003516471,"about_ca_topic_score_gemma":0.0027734623,"teacher_disagreement_score":0.003516471,"about_ca_system_score_codex":0.00034799063,"about_ca_system_score_gemma":0.00023275938,"threshold_uncertainty_score":0.0069919825},"labels":[],"label_agreement":null},{"id":"W3170080236","doi":"10.1029/2021gl093548","title":"Circulation and Upwelling Induced by Coastal Trapped Waves Over a Submarine Canyon in an Idealized Eastern Boundary Margin","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Fondo Nacional de Desarrollo Científico y Tecnológico; Natural Sciences and Engineering Research Council of Canada","keywords":"Upwelling; Canyon; Geology; Submarine canyon; Oceanography; Continental shelf; Continental margin; Forcing (mathematics); Submarine; Boundary current; Climatology; Ocean current; Geomorphology; Tectonics; Seismology","score_opus":0.029603800006985453,"score_gpt":0.2821665915310164,"score_spread":0.25256279152403094,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170080236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99929726,0.0000102530885,0.00025768927,0.000019388059,0.000003925401,0.000003215729,0.000044479024,0.000008548267,0.00035515908],"genre_scores_gemma":[0.9996094,0.000009711926,0.0002017982,0.000004736755,0.0000014387275,0.000005071155,0.00004980139,0.0000016452077,0.00011644751],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999329,0.00001606301,0.0000043727155,0.00001682901,0.000006611922,0.000023258832],"domain_scores_gemma":[0.9997409,0.000076803,0.00006236309,0.000031825355,0.000028563125,0.00005951267],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019515559,0.0003301433,0.00039869602,0.00018221086,0.00042460565,0.0006352797,0.00039182152,0.0005056522,0.0011393217],"category_scores_gemma":[0.00047796892,0.00022590668,0.0002779072,0.00011443404,0.00090269954,0.0002997372,0.0005145925,0.00037632298,0.000060886334],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001056472,0.0004051965,0.027697891,0.000057582125,0.00009531373,0.00054259284,0.000107862135,0.9308361,0.035728734,0.0019028398,0.00029149314,0.0012778346],"study_design_scores_gemma":[0.0002461627,0.0004611701,0.019751342,0.000010482742,0.00004834199,0.000026984513,0.00018658047,0.9754136,0.003117521,0.0005637343,0.00014648067,0.000027518729],"about_ca_topic_score_codex":0.01834692,"about_ca_topic_score_gemma":0.0076707085,"teacher_disagreement_score":0.01834692,"about_ca_system_score_codex":0.0005295577,"about_ca_system_score_gemma":0.00062883616,"threshold_uncertainty_score":0.036480248},"labels":[],"label_agreement":null},{"id":"W3170617207","doi":"10.1029/2020gl091390","title":"Zircon U‐Pb Geochronology Constrains Continental Expression of Great Meteor Hotspot Magmatism","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lamont-Doherty Earth Observatory, Columbia University; National Science Foundation","keywords":"Magmatism; Geology; Zircon; Hotspot (geology); Geochronology; Igneous rock; Large igneous province; Lithosphere; Earth science; Geochemistry; Paleontology; Geophysics","score_opus":0.028268600983422758,"score_gpt":0.26871901433950607,"score_spread":0.2404504133560833,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3170617207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957249,0.00021587817,0.00055743905,0.000024600711,0.000002886172,0.000004125712,0.00073089974,0.000028427286,0.0027108362],"genre_scores_gemma":[0.9993249,0.000035691126,0.000118346456,0.0000023784296,6.3065755e-7,7.149463e-7,0.00022036835,0.0000027603899,0.0002942051],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994147,0.0000063392536,0.0000024915764,0.000017984332,0.000011101222,0.000020616268],"domain_scores_gemma":[0.99967,0.00003964106,0.0000614364,0.00002884441,0.00015733269,0.000042655058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002592608,0.00013966844,0.00013974716,0.0007722272,0.00044746386,0.00071488257,0.00024350364,0.0001400787,0.0021608379],"category_scores_gemma":[0.00074100896,0.000099270896,0.000082850114,0.00061360345,0.00035066684,0.00018955885,0.00025339253,0.00013522904,0.00020420684],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024024125,0.000009489372,0.96495396,0.00002683298,0.000048921254,0.00008445035,0.00045379545,0.0017578829,0.017160887,0.00044346554,0.00055706967,0.01426297],"study_design_scores_gemma":[0.0000016760957,0.000006817694,0.99786633,0.0000028106822,0.0000057571992,0.000020325555,0.000085449254,0.0007876314,0.0006230933,0.000020298106,0.0005777732,0.0000020375053],"about_ca_topic_score_codex":0.69655997,"about_ca_topic_score_gemma":0.8038705,"teacher_disagreement_score":0.69655997,"about_ca_system_score_codex":0.0021607885,"about_ca_system_score_gemma":0.0008242253,"threshold_uncertainty_score":0.6104541},"labels":[],"label_agreement":null},{"id":"W3172521784","doi":"10.1029/2021gl092506","title":"Annual Appearance of Hydrogen Chloride on Mars and a Striking Similarity With the Water Vapor Vertical Distribution Observed by TGO/NOMAD","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":33,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Ministerio de Ciencia e Innovación; European Space Agency; Agenzia Spaziale Italiana; Belgian Federal Science Policy Office; Waterbird Society; UK Space Agency; Centre National d’Etudes Spatiales; Ministerio de Ciencia, Innovación y Universidades; Fonds De La Recherche Scientifique - FNRS; Hill, Holliday, Connors, Cosmopulos; Agence Nationale de la Recherche; National Aeronautics and Space Administration","keywords":"Atmosphere of Mars; Water vapor; Mars Exploration Program; Dust storm; Martian; Orbiter; Atmospheric sciences; Hydrogen chloride; Trace gas; Environmental science; Storm; Atmosphere (unit); Sink (geography); Astrobiology; Meteorology; Geology; Chemistry; Physics; Geography","score_opus":0.02957432690637491,"score_gpt":0.2611515919453497,"score_spread":0.2315772650389748,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3172521784","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841535,0.00009872463,0.00012836015,0.000017726537,0.000005859746,0.000002184642,0.0006158306,0.000025123227,0.0006908282],"genre_scores_gemma":[0.9990908,0.000029085675,0.00012688035,0.000008857578,0.0000061450864,0.000002261207,0.00053232716,0.0000028049783,0.00020081313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.000003338332,0.0000015503172,0.0000131480465,0.000009954506,0.000012512042],"domain_scores_gemma":[0.9999007,0.000009552547,0.000034676228,0.000008866314,0.000020014972,0.000026104868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006235212,0.00014789021,0.00012608383,0.0005956639,0.00020945707,0.00022854938,0.00011530616,0.00016685679,0.000746514],"category_scores_gemma":[0.00010839662,0.00006644991,0.00010662838,0.0003123733,0.00010919263,0.000121325575,0.00016840656,0.0001470587,0.00010996985],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035188237,0.000059241283,0.80943686,0.000048075224,0.00010523491,0.00045762205,0.0002875731,0.00034902614,0.17365935,0.00009509031,0.0008456052,0.014304483],"study_design_scores_gemma":[0.0000017785007,0.00003881176,0.99648017,0.0000014477847,0.0000066620205,0.00007918308,0.00004822147,0.00018316382,0.0024860748,0.000008085807,0.00066416385,0.0000023778098],"about_ca_topic_score_codex":0.0027109655,"about_ca_topic_score_gemma":0.0040966948,"teacher_disagreement_score":0.0027109655,"about_ca_system_score_codex":0.00009519054,"about_ca_system_score_gemma":0.00004872847,"threshold_uncertainty_score":0.005390346},"labels":[],"label_agreement":null},{"id":"W3173426302","doi":"10.1029/2021gl094090","title":"Lithosphere Weakening During Arctic Ocean Opening: Evidence From Effective Elastic Thickness","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Lithosphere; Geology; Bathymetry; Lithospheric flexure; Breakup; Arctic; Tectonics; Ridge; Geophysics; Seafloor spreading; Ridge push; Seismology; Oceanography; Paleontology","score_opus":0.04592674574776014,"score_gpt":0.28436887932592614,"score_spread":0.238442133578166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3173426302","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999438,0.000038920687,0.00011966279,0.000003948268,0.0000011213546,6.079061e-7,0.000073468036,0.0000019765707,0.00032229713],"genre_scores_gemma":[0.99975747,0.000033988374,0.000067583445,0.0000019343277,0.0000017028545,7.0079693e-7,0.00009361009,0.0000015449716,0.000041525404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991465,0.000014948073,0.000007816795,0.000014455487,0.00002178571,0.000026295076],"domain_scores_gemma":[0.9992113,0.00020544424,0.00024335923,0.000052905794,0.00016701162,0.00011996413],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003220838,0.00015111973,0.00016418952,0.0010641954,0.00027127925,0.0005738061,0.00012508368,0.00017630264,0.0006375278],"category_scores_gemma":[0.0011406889,0.00014207701,0.00012305078,0.0006823279,0.0003379406,0.00024806117,0.00040325755,0.00021626055,0.00012745862],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002916716,0.00002449799,0.9573432,0.000030955365,0.000065235705,0.00021333373,0.0006525285,0.00077273895,0.03139403,0.0001157325,0.000065014974,0.009030896],"study_design_scores_gemma":[7.7338063e-7,0.000016327682,0.9984345,0.0000033810272,0.000006380756,0.000051629864,0.00019740626,0.00044806098,0.0007488529,0.000028916882,0.000061021077,0.0000026630091],"about_ca_topic_score_codex":0.0059295124,"about_ca_topic_score_gemma":0.006158821,"teacher_disagreement_score":0.0059295124,"about_ca_system_score_codex":0.000114296854,"about_ca_system_score_gemma":0.00012259366,"threshold_uncertainty_score":0.011789978},"labels":[],"label_agreement":null},{"id":"W3175559056","doi":"10.1029/2021gl094287","title":"Impacts of Sea Ice Mushy Thermodynamics in the Antarctic on the Coupled Earth System","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Earth Sciences Division; National Science Foundation","keywords":"Sea ice growth processes; Sea ice; Sea ice thickness; Cryosphere; Geology; Antarctic sea ice; Atmosphere (unit); Atmospheric sciences; Oceanography; Environmental science; Climatology; Meteorology; Geography","score_opus":0.024053527883080007,"score_gpt":0.2626860630461841,"score_spread":0.23863253516310406,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3175559056","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981103,0.000040183368,0.0003058916,0.0001222108,0.000008465233,0.0000078970215,0.00023912906,0.000023633242,0.0011422579],"genre_scores_gemma":[0.99956375,0.00002951986,0.00011382663,0.000038532562,0.0000030731549,0.000007631795,0.00010295273,0.0000072386943,0.00013340313],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998134,0.00006730055,0.000009667643,0.000023417762,0.00002403493,0.000062252926],"domain_scores_gemma":[0.9993554,0.00035199014,0.000066674715,0.000073472045,0.00005456757,0.00009788284],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00067655335,0.00059216,0.00054953183,0.00036445455,0.00062033214,0.00092257344,0.0004687048,0.0006886626,0.0022007874],"category_scores_gemma":[0.0017845512,0.00029205313,0.00082579406,0.00033605212,0.001204302,0.00083097257,0.000943138,0.000705569,0.00010841099],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003556669,0.00014591585,0.022343434,0.00004760881,0.00014709689,0.00021835945,0.000044365755,0.9675368,0.005954173,0.0016747741,0.00027347147,0.0012582944],"study_design_scores_gemma":[0.00025963946,0.0003955048,0.05575841,0.000010445664,0.00009649929,0.000032512664,0.00025785714,0.93708,0.003958178,0.0016177497,0.0004753151,0.000057914338],"about_ca_topic_score_codex":0.042880263,"about_ca_topic_score_gemma":0.017793968,"teacher_disagreement_score":0.042880263,"about_ca_system_score_codex":0.0012910339,"about_ca_system_score_gemma":0.00079747435,"threshold_uncertainty_score":0.085261345},"labels":[],"label_agreement":null},{"id":"W3176638204","doi":"10.1029/2021gl092815","title":"Misconception of Waveform Similarity in the Identification of Repeating Earthquakes","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"","keywords":"Waveform; Repeater (horology); Similarity (geometry); Robustness (evolution); Identification (biology); Azimuth; Computer science; Geology; Statistics; Geodesy; Mathematics; Artificial intelligence; Telecommunications","score_opus":0.05646824068064328,"score_gpt":0.31278783573998026,"score_spread":0.256319595059337,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3176638204","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9429952,0.0013607941,0.04759148,0.0024029282,0.00018909092,0.00004712761,0.00012800831,0.00020074163,0.0050846054],"genre_scores_gemma":[0.9951984,0.00012283269,0.0042555374,0.00019056386,0.000044115513,0.0000058069963,0.00003819515,0.000020418769,0.00012403633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.98639894,0.007321375,0.0010420568,0.0025058545,0.0024703126,0.00026145778],"domain_scores_gemma":[0.8286171,0.12615392,0.015816182,0.018534798,0.009410244,0.0014677078],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.028177429,0.00032723034,0.00047789735,0.0015438845,0.0006477751,0.002519935,0.0016424106,0.0014096032,0.0010380123],"category_scores_gemma":[0.16242789,0.0003342515,0.0002691225,0.0007037427,0.003619408,0.0031403138,0.0014812055,0.0012071932,0.00041340516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0020921943,0.00027364457,0.5771085,0.00097180204,0.0008160835,0.0017066615,0.017731372,0.014304213,0.051172875,0.03875245,0.0054310933,0.28963912],"study_design_scores_gemma":[0.00015607926,0.0016612499,0.5957875,0.0010971368,0.0004883437,0.0070714573,0.016680008,0.16004026,0.10191124,0.10161906,0.012961413,0.00052622426],"about_ca_topic_score_codex":0.0013422878,"about_ca_topic_score_gemma":0.0012602288,"teacher_disagreement_score":0.028177429,"about_ca_system_score_codex":0.00065119716,"about_ca_system_score_gemma":0.00041823197,"threshold_uncertainty_score":0.14901823},"labels":[],"label_agreement":null},{"id":"W3177527454","doi":"10.1029/2021gl094263","title":"Laurentide Ice Saddle Mergers Drive Rapid Sea Level Drops During Glaciations","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Chinese Government Scholarship; National Natural Science Foundation of China","keywords":"Ice sheet; Geology; Glacial period; Sea ice; Sea level; Oceanography; Antarctic sea ice; Arctic ice pack; Climatology; Geomorphology","score_opus":0.05125646780647642,"score_gpt":0.29676585891567214,"score_spread":0.24550939110919573,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3177527454","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988477,0.000011531577,0.00021214358,0.00004182581,0.0000051350275,0.000005673722,0.000059679867,0.000022476994,0.0007936856],"genre_scores_gemma":[0.99967766,0.000009741327,0.0001347965,0.000009265723,0.0000012892127,0.000004436116,0.000054904478,0.000004735678,0.000103161816],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992406,0.000016169255,0.0000044218496,0.000015909756,0.000012655607,0.000026814694],"domain_scores_gemma":[0.99983585,0.000035076988,0.00003749541,0.000012759592,0.0000149517855,0.00006386194],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019554971,0.00035577663,0.00028579327,0.00022952684,0.00049227267,0.00069097825,0.00041212045,0.00054155383,0.0020052295],"category_scores_gemma":[0.0007158656,0.0002666929,0.00046369652,0.00015465243,0.0004407409,0.00036732733,0.00066599133,0.00040568245,0.00013298054],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065025035,0.00027061702,0.1681855,0.000046601795,0.00020716005,0.00086922373,0.00025360222,0.80797154,0.014782426,0.0018492101,0.0010974539,0.0038164028],"study_design_scores_gemma":[0.00026554684,0.00048679014,0.1239178,0.000016741928,0.000071367096,0.00014989011,0.00039764697,0.8700378,0.0028478126,0.00082740834,0.0009502047,0.000030974577],"about_ca_topic_score_codex":0.019246023,"about_ca_topic_score_gemma":0.017224856,"teacher_disagreement_score":0.019246023,"about_ca_system_score_codex":0.000987378,"about_ca_system_score_gemma":0.000629911,"threshold_uncertainty_score":0.03826797},"labels":[],"label_agreement":null},{"id":"W3178099273","doi":"10.1029/2020gl090995","title":"New Radiocarbon Constraints on the Global Cycling of Solid‐Phase Extractable Dissolved Organic Carbon","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canada Research Chairs; American Chemical Society Petroleum Research Fund; National Science Foundation","keywords":"Dissolved organic carbon; Transect; Radiocarbon dating; Environmental science; Carbon cycle; Remineralisation; Deep sea; Oceanography; Biogeochemical cycle; Environmental chemistry; Geology; Chemistry; Ecology; Biology; Ecosystem","score_opus":0.03072642231542642,"score_gpt":0.30413128214525825,"score_spread":0.2734048598298318,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3178099273","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9886847,0.0018076547,0.0015132551,0.00014322961,0.00001510911,0.0000041616795,0.0014386385,0.000035962672,0.0063572917],"genre_scores_gemma":[0.99718153,0.0006480719,0.00094823557,0.0000794116,0.000020503287,0.0000076455335,0.00081764965,0.000013159072,0.00028391858],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998815,0.000015142552,0.000007131039,0.00005076952,0.000022563432,0.000022891953],"domain_scores_gemma":[0.9992693,0.00026685806,0.00019488891,0.00008598496,0.00013537501,0.000047613597],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042667982,0.00042226206,0.00022219573,0.0012754556,0.00026339572,0.0010617246,0.0002606614,0.00024119369,0.0016095879],"category_scores_gemma":[0.0007385408,0.00023647356,0.00019459221,0.0013375806,0.00070472393,0.0007952019,0.00060739013,0.0004062529,0.00026043688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00077457976,0.0000667401,0.6561179,0.00034918022,0.00025850788,0.00032696288,0.0007337761,0.005904052,0.26537582,0.0061476007,0.0007473842,0.063197516],"study_design_scores_gemma":[0.0000151518925,0.00006809063,0.9835284,0.000035242312,0.0000724794,0.00011524034,0.00040548606,0.0020268757,0.006821094,0.0015259347,0.005363182,0.000022974946],"about_ca_topic_score_codex":0.008640468,"about_ca_topic_score_gemma":0.011706832,"teacher_disagreement_score":0.008640468,"about_ca_system_score_codex":0.00044586524,"about_ca_system_score_gemma":0.00023374325,"threshold_uncertainty_score":0.017180324},"labels":[],"label_agreement":null},{"id":"W3180320542","doi":"10.1029/2021gl093618","title":"A Solid Interpretation of Bright Radar Reflectors Under the Mars South Polar Ice","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Mars Exploration Program; Polar; Liquid water; Geology; Depth sounding; Radar; Geophysics; Dielectric permittivity; Astrobiology; Ground-penetrating radar; Reflection (computer programming); Permittivity; Mineralogy; Dielectric; Physics; Astronomy; Earth science","score_opus":0.03200334801498888,"score_gpt":0.32902918842038553,"score_spread":0.29702584040539665,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3180320542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9867951,0.00016685731,0.005001733,0.00022982365,0.00003162365,0.0000054619895,0.00016491557,0.00012432737,0.0074801515],"genre_scores_gemma":[0.9981592,0.00004801613,0.001174935,0.000039704668,0.00001127839,0.0000016901193,0.000059139245,0.00001124382,0.0004947111],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.0000069229027,0.0000018154411,0.0000121334215,0.000015974809,0.000013687296],"domain_scores_gemma":[0.99986196,0.00004106869,0.00003930892,0.00001473143,0.000025034213,0.000017886096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012773884,0.00026927702,0.00015684366,0.00054874277,0.00025341404,0.00046692215,0.00020762184,0.00031618238,0.0032171768],"category_scores_gemma":[0.00022138389,0.0001476708,0.0001280088,0.00018140876,0.0004283099,0.00034047055,0.00031431118,0.0002798751,0.00043999328],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004590147,0.0000351864,0.040361725,0.00011969189,0.000031168158,0.0010251884,0.0005223252,0.0013792141,0.93872565,0.0014516466,0.00083097455,0.015058253],"study_design_scores_gemma":[0.00010584039,0.00044337288,0.5945659,0.000076434604,0.0001252111,0.0026176982,0.0031207302,0.020819886,0.36664084,0.0024406496,0.00896333,0.00008002573],"about_ca_topic_score_codex":0.00074980466,"about_ca_topic_score_gemma":0.0013500861,"teacher_disagreement_score":0.0032171768,"about_ca_system_score_codex":0.000103084036,"about_ca_system_score_gemma":0.00008614863,"threshold_uncertainty_score":0.010762572},"labels":[],"label_agreement":null},{"id":"W3181700346","doi":"10.1029/2021gl092816","title":"Chinese Regulations Are Working—Why Is Surface Ozone Over Industrialized Areas Still High? Applying Lessons From Northeast US Air Quality Evolution","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":124,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China; U.S. Environmental Protection Agency","keywords":"China; Delta; Yangtze river; Environmental science; Ozone; Air quality index; Climatology; Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.06108466555739631,"score_gpt":0.32489982489632907,"score_spread":0.26381515933893274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3181700346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.984139,0.00074559776,0.00055967394,0.0056393906,0.00005312394,0.000012398616,0.0008307382,0.00003240187,0.007987677],"genre_scores_gemma":[0.99847966,0.00038918966,0.00014215229,0.00036227927,0.000019702502,0.0000032088114,0.00022901765,0.000005405167,0.00036939568],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99973196,0.000044190125,0.000016248827,0.00007384957,0.000052670857,0.00008105739],"domain_scores_gemma":[0.99929297,0.000081062215,0.00021273301,0.00010968272,0.00021826186,0.00008528514],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009254546,0.00018832747,0.0002385374,0.00057438965,0.0007565925,0.00102001,0.00044797576,0.00033185678,0.0013806879],"category_scores_gemma":[0.0011844446,0.00011815522,0.00040219183,0.0016325752,0.0009119371,0.0009457934,0.0006325545,0.00043367845,0.000096269796],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060850325,0.00002515295,0.96405864,0.00009910061,0.00014338875,0.0004422096,0.0019144106,0.001856453,0.0013591152,0.0033445503,0.0038229947,0.022873105],"study_design_scores_gemma":[0.0000028465333,0.000018103205,0.9911026,0.00002860026,0.00004705566,0.000029910794,0.0019986385,0.0013388268,0.00039072483,0.0009813954,0.004050162,0.000011261995],"about_ca_topic_score_codex":0.26486152,"about_ca_topic_score_gemma":0.26506454,"teacher_disagreement_score":0.26486152,"about_ca_system_score_codex":0.0028092193,"about_ca_system_score_gemma":0.0026056503,"threshold_uncertainty_score":0.5266397},"labels":[],"label_agreement":null},{"id":"W3183427853","doi":"10.1029/2021gl094696","title":"A Strong Correlation Between Relativistic Electron Microbursts and Patchy Aurora","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":43,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"Goddard Space Flight Center","keywords":"Physics; Microburst; Electron precipitation; Electron; Satellite; Astrophysics; Van Allen radiation belt; Cosmic ray; Relativistic particle; Radiation; Magnetosphere; Geophysics; Computational physics; Astronomy; Nuclear physics; Plasma; Meteorology","score_opus":0.01735407572646065,"score_gpt":0.29064685588326433,"score_spread":0.2732927801568037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3183427853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99917185,0.000044697485,0.00010985104,0.00001950922,0.0000027560218,0.0000015881127,0.00009689311,0.0000057205953,0.0005472519],"genre_scores_gemma":[0.9996648,0.000014021658,0.00006712685,0.000006261552,0.000007793459,8.707869e-7,0.00008979782,0.0000016705586,0.00014762522],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998741,0.000015215426,0.000008272783,0.000038097365,0.000034018703,0.00003035148],"domain_scores_gemma":[0.99880135,0.00020760299,0.00052963075,0.000103259015,0.00018033852,0.00017772864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016230917,0.000093260765,0.00015581526,0.00054935296,0.00030653604,0.0004343909,0.00016883442,0.0001771923,0.0014455251],"category_scores_gemma":[0.0010520658,0.00009269271,0.00008857946,0.00042092355,0.00026664638,0.00018538407,0.0004381909,0.00019680955,0.00018032728],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000049468395,0.0000059244126,0.9942673,0.000004923075,0.000030036335,0.00016332927,0.000104454586,0.000084849096,0.003457336,0.000024430014,0.00010601485,0.0017021353],"study_design_scores_gemma":[6.155672e-7,0.000009388567,0.99946755,7.5305803e-7,0.0000032606201,0.00009383049,0.00007154379,0.0000633392,0.00016233201,0.0000062193453,0.00012030059,9.105314e-7],"about_ca_topic_score_codex":0.011411425,"about_ca_topic_score_gemma":0.023894167,"teacher_disagreement_score":0.011411425,"about_ca_system_score_codex":0.00016098854,"about_ca_system_score_gemma":0.0001454197,"threshold_uncertainty_score":0.022689998},"labels":[],"label_agreement":null},{"id":"W3184102313","doi":"10.1029/2020gl092267","title":"Aftershock Triggering and Spatial Aftershock Zones in Fluid‐Driven Settings: Discriminating Induced Seismicity From Natural Swarms","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Microseismic Industry Consortium","keywords":"Aftershock; Induced seismicity; Geology; Seismology; Magnitude (astronomy); Tectonics; Natural (archaeology); Spatial variability; Paleontology; Physics","score_opus":0.032852331797719014,"score_gpt":0.27755878431937026,"score_spread":0.24470645252165124,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184102313","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993455,0.000023260427,0.00014979333,0.000005460688,6.3426666e-7,0.000003708665,0.00015303132,0.0000061444603,0.0003124898],"genre_scores_gemma":[0.9997117,0.000011462201,0.000097125536,0.0000010380662,8.3587344e-7,0.0000014189792,0.00013284756,7.510442e-7,0.00004275185],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998634,0.000019921961,0.000018006644,0.000038496943,0.00002243619,0.00003779911],"domain_scores_gemma":[0.9988004,0.00019562274,0.0006345743,0.000072742536,0.00013473256,0.0001618352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020540801,0.00016123432,0.00016379674,0.0014204856,0.00022413219,0.00066187844,0.00015199302,0.00020159014,0.0012279885],"category_scores_gemma":[0.0013138321,0.00010086509,0.000105786574,0.0011541354,0.00033459233,0.0004443092,0.0005678808,0.00013142082,0.00015178576],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007187344,0.000027881766,0.99247897,0.000015156928,0.00003023508,0.00008134143,0.0002636214,0.0010245015,0.0026305772,0.00009432675,0.00007572555,0.0032057918],"study_design_scores_gemma":[0.00000166956,0.000018234055,0.99814355,0.0000031167701,0.0000043647074,0.000024630945,0.00032587335,0.0011576585,0.00020525993,0.000029821786,0.000083220664,0.0000025554782],"about_ca_topic_score_codex":0.011408229,"about_ca_topic_score_gemma":0.025007324,"teacher_disagreement_score":0.011408229,"about_ca_system_score_codex":0.00029234478,"about_ca_system_score_gemma":0.0002527129,"threshold_uncertainty_score":0.02268368},"labels":[],"label_agreement":null},{"id":"W3184851937","doi":"10.1029/2021gl094918","title":"Radar Observation of Extreme Vertical Drafts in the Polar Summer Mesosphere","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Agence Nationale de la Recherche; Deutsche Forschungsgemeinschaft","keywords":"Mesosphere; Geology; Polar; Radar; Environmental science; Atmospheric sciences; Meteorology; Stratosphere; Geography; Astronomy; Physics; Computer science; Telecommunications","score_opus":0.04623983312095312,"score_gpt":0.29966547495105433,"score_spread":0.2534256418301012,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3184851937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984499,0.00007515549,0.000554881,0.000016489486,0.000006162705,0.000003834774,0.00014076289,0.0000302582,0.00072242634],"genre_scores_gemma":[0.9992386,0.000032854143,0.00039067146,0.000008168463,0.000006209749,0.0000018149535,0.00019192742,0.0000028727266,0.00012689222],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999633,0.0000036550173,0.0000016155655,0.00000766733,0.000013285674,0.000010451213],"domain_scores_gemma":[0.999841,0.000020459862,0.00003846247,0.00001263661,0.00003185988,0.00005563864],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111495305,0.00014578177,0.00010079029,0.0003295898,0.00013540208,0.00021992256,0.00008522028,0.00016685232,0.00034183558],"category_scores_gemma":[0.00021243557,0.0000807874,0.00006233559,0.00020070274,0.00014827216,0.00014761701,0.00022972366,0.00021031017,0.00011605848],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003593328,0.00005832127,0.27117935,0.00003832068,0.000059258175,0.001094514,0.00053667184,0.00068640034,0.7049732,0.00018699204,0.00070814986,0.020119486],"study_design_scores_gemma":[0.000013061884,0.00012093414,0.98752743,0.000005318018,0.000010128879,0.00033058008,0.00015032681,0.0010868618,0.009872016,0.000053479307,0.00082368293,0.000006195445],"about_ca_topic_score_codex":0.0011462508,"about_ca_topic_score_gemma":0.0020789446,"teacher_disagreement_score":0.0011462508,"about_ca_system_score_codex":0.0000705276,"about_ca_system_score_gemma":0.000057174777,"threshold_uncertainty_score":0.0022791624},"labels":[],"label_agreement":null},{"id":"W3185163169","doi":"10.1029/2021gl094706","title":"Seismic Reflection and Electrical Resistivity Imaging Support Pre‐Quaternary Glaciation in the Rocky Mountains (Unaweep Canyon, Colorado)","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Science Foundation","keywords":"Geology; Quaternary; Glacial period; Paleontology; Canyon; Fluvial; Basement; Precambrian; Sedimentary rock; Geomorphology; Structural basin; Archaeology","score_opus":0.022688122665678594,"score_gpt":0.2960591990132927,"score_spread":0.2733710763476141,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3185163169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99809736,0.00008373898,0.00011936002,0.000038348517,0.0000015281308,0.000003159586,0.000162355,0.0000073714655,0.0014866911],"genre_scores_gemma":[0.9991254,0.00005854674,0.00021026525,0.000008378211,0.000002314056,0.0000024447131,0.00023923283,0.0000022583697,0.00035123806],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995553,0.0000040418013,0.0000021251115,0.000012690644,0.00000967422,0.000015966483],"domain_scores_gemma":[0.9998497,0.00001814077,0.000028980301,0.0000102885815,0.00007094729,0.000021957452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000093701754,0.00008024939,0.00007251934,0.0005036146,0.00038727192,0.0004554574,0.00014974299,0.00024653284,0.0008827956],"category_scores_gemma":[0.00028771875,0.0000807797,0.000031738018,0.00041986437,0.00027802886,0.00013975742,0.00025216507,0.00013338121,0.00015131611],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012314107,0.00006459201,0.94871175,0.000029559968,0.000030851043,0.0005082557,0.0016793725,0.00045581255,0.025743809,0.00015933267,0.000799783,0.021693751],"study_design_scores_gemma":[0.000002203156,0.00000763485,0.99765766,0.000007756678,0.0000059486465,0.00010950407,0.0007035669,0.0004404485,0.00047756435,0.000020681102,0.00056571135,0.0000013099223],"about_ca_topic_score_codex":0.102003135,"about_ca_topic_score_gemma":0.35311902,"teacher_disagreement_score":0.102003135,"about_ca_system_score_codex":0.00033238492,"about_ca_system_score_gemma":0.00038145843,"threshold_uncertainty_score":0.20281881},"labels":[],"label_agreement":null},{"id":"W3185548972","doi":"10.1029/2021gl095396","title":"On the Detection of COVID‐Driven Changes in Atmospheric Carbon Dioxide","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Nuclear Safety and Security Commission; Keck Institute for Space Studies; National Aeronautics and Space Administration; National Science Foundation","keywords":"Atmosphere (unit); Carbon dioxide; Carbon dioxide in Earth's atmosphere; Atmospheric carbon cycle; Carbon fibers; SIGNAL (programming language); Atmospheric dynamics","score_opus":0.01627410206372897,"score_gpt":0.2521713970317246,"score_spread":0.2358972949679956,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3185548972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977035,0.000053527518,0.0013587293,0.00011020927,0.000012258981,0.0000045131965,0.00024350839,0.00007607141,0.00043776887],"genre_scores_gemma":[0.9993086,0.0000111175395,0.00029279434,0.000023230794,0.0000061747555,0.000002240103,0.00031739153,0.000009536553,0.000028978542],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99923456,0.00028575747,0.00003787038,0.00025630262,0.00010036495,0.00008507674],"domain_scores_gemma":[0.9942069,0.003761785,0.0005632994,0.0006714769,0.00043250708,0.00036402658],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0031947023,0.0005866684,0.0006742191,0.00047593119,0.00041725888,0.0008951225,0.0006346835,0.00067146437,0.00074023893],"category_scores_gemma":[0.011925568,0.0005278654,0.00064438256,0.00026777294,0.0007077141,0.0008353585,0.001321364,0.0006817995,0.00011892863],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001324485,0.00039602348,0.69022894,0.00011060571,0.0010263387,0.00020695956,0.00013149757,0.26630616,0.018834632,0.0009338479,0.0013890626,0.019111402],"study_design_scores_gemma":[0.00007098877,0.0002946762,0.26495996,0.000012092944,0.00009359362,0.00007631752,0.0000771528,0.72812706,0.005119748,0.0007407244,0.00037769863,0.000049948307],"about_ca_topic_score_codex":0.0072285156,"about_ca_topic_score_gemma":0.0064759464,"teacher_disagreement_score":0.0072285156,"about_ca_system_score_codex":0.00046869516,"about_ca_system_score_gemma":0.0004080161,"threshold_uncertainty_score":0.016895413},"labels":[],"label_agreement":null},{"id":"W3186103167","doi":"10.1029/2021gl093919","title":"Catastrophic Drainage From the Northwestern Outlet of Glacial Lake Agassiz During the Younger Dryas","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"MacEwan University; University of Alberta; Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Government of Alberta; Univerzita Karlova v Praze","keywords":"Younger Dryas; Meltwater; Glacial lake; Geology; Glacial period; Oceanography; Flood myth; Physical geography; Climatology; Geomorphology; Archaeology; Geography","score_opus":0.026036389275964883,"score_gpt":0.2698640866025409,"score_spread":0.24382769732657603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3186103167","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947244,0.0000126589175,0.000104590166,0.00003298051,0.0000014333978,0.0000012822919,0.00008436732,0.000014495179,0.00027586156],"genre_scores_gemma":[0.99980384,0.000009778636,0.000064638356,0.0000032831824,0.0000011192634,7.837885e-7,0.0000758983,9.40844e-7,0.000039827206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994826,0.000006510693,0.000002750703,0.000014491931,0.000007702988,0.000020287123],"domain_scores_gemma":[0.9999149,0.000016220167,0.000030218791,0.0000061146557,0.000010319166,0.000022158734],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015838773,0.00022280966,0.0001615284,0.00040164773,0.00038599072,0.00069401774,0.00028802725,0.00031447783,0.0006219963],"category_scores_gemma":[0.00031151055,0.00013668412,0.00036941946,0.00031691664,0.00048265466,0.00026513296,0.0005552391,0.00022603078,0.00004041797],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004257763,0.00006854219,0.90028566,0.000041429423,0.00011690382,0.0005207812,0.00030576836,0.07907109,0.010687847,0.0012625415,0.0004345619,0.0067790733],"study_design_scores_gemma":[0.00006476145,0.00006930947,0.87082106,0.000018587834,0.000051709892,0.0000816592,0.00035637539,0.12596467,0.0014030392,0.00047177795,0.00067667064,0.000020478583],"about_ca_topic_score_codex":0.10501696,"about_ca_topic_score_gemma":0.16321449,"teacher_disagreement_score":0.10501696,"about_ca_system_score_codex":0.002122847,"about_ca_system_score_gemma":0.0008864968,"threshold_uncertainty_score":0.20881134},"labels":[],"label_agreement":null},{"id":"W3186429835","doi":"10.1029/2021gl094607","title":"Underwater Sound Levels in the Arctic: Filling Knowledge Gaps","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wildlife Conservation Society Canada; University of Victoria","funders":"","keywords":"Arctic; Underwater; Sound (geography); Oceanography; Climate change; Baseline (sea); The arctic; Sea ice; Soundscape; Environmental science; Arctic ice pack; Geology; Physical geography; Climatology; Geography","score_opus":0.06532336879742467,"score_gpt":0.3129844763099543,"score_spread":0.24766110751252962,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3186429835","genre_codex":"review","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.051723544,0.8696434,0.0042499923,0.0520076,0.003740439,0.000034914432,0.006124224,0.00008864081,0.012387228],"genre_scores_gemma":[0.44795862,0.5189344,0.0102393795,0.011716051,0.006424294,0.00012352064,0.0039718663,0.000043438464,0.0005884175],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9967501,0.0009273208,0.0007306514,0.0006628587,0.000676561,0.00025249284],"domain_scores_gemma":[0.9551349,0.027763488,0.0039236164,0.0016530381,0.00991742,0.0016074541],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010337315,0.00068650104,0.0016327889,0.005331123,0.00088273553,0.004306904,0.0019073507,0.0018487613,0.003138071],"category_scores_gemma":[0.028934363,0.00047997295,0.0007607619,0.0050085234,0.0023837823,0.005056593,0.0029471153,0.003387685,0.00056647713],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032506662,0.00022372245,0.08657556,0.024754563,0.0010885133,0.0005406115,0.0067251096,0.0030079319,0.00063382677,0.010450754,0.037507817,0.82816654],"study_design_scores_gemma":[0.000044757096,0.00039980802,0.31818387,0.112181574,0.002048895,0.0011845982,0.026713373,0.004756982,0.00097071164,0.07636587,0.4567853,0.00036427763],"about_ca_topic_score_codex":0.07428055,"about_ca_topic_score_gemma":0.05517789,"teacher_disagreement_score":0.07428055,"about_ca_system_score_codex":0.0027031102,"about_ca_system_score_gemma":0.0064191427,"threshold_uncertainty_score":0.14769638},"labels":[],"label_agreement":null},{"id":"W3186470940","doi":"10.1029/2021gl094987","title":"Topographic Roughness on Forested Hillslopes: A Theoretical Approach for Quantifying Hillslope Sediment Flux From Tree Throw","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Environmental Resilience Institute, Indiana University","keywords":"Geology; Flux (metallurgy); Dimensionless quantity; Tree (set theory); Sediment; Geomorphology; Hydrology (agriculture); Soil science; Geotechnical engineering; Mechanics; Mathematics","score_opus":0.03985239384463401,"score_gpt":0.3057434582576694,"score_spread":0.2658910644130354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3186470940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.82731605,0.00038729524,0.16765611,0.00024239252,0.000012315072,0.000029675773,0.00018166016,0.0001180508,0.0040563853],"genre_scores_gemma":[0.99471563,0.00009046999,0.005008918,0.00000863122,0.0000064600667,0.0000075971984,0.000023027984,0.0000056505523,0.00013375851],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990416,0.000027552536,0.000007169545,0.000023998426,0.000023579409,0.000013475744],"domain_scores_gemma":[0.99950886,0.00025562322,0.00012486105,0.000034728753,0.00005020681,0.000025741185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006086819,0.000275037,0.0001548264,0.0017559547,0.0002826788,0.0008346925,0.00034685046,0.00028903934,0.0006642314],"category_scores_gemma":[0.001446759,0.00014469051,0.00030499947,0.00059370615,0.0012352814,0.0007941857,0.0003716286,0.00024864057,0.00004165402],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008033546,0.000093604045,0.118936054,0.00016985684,0.00010165237,0.0005708801,0.00046941583,0.6334281,0.037575763,0.17868789,0.0007639915,0.02912252],"study_design_scores_gemma":[0.000008063482,0.000063544925,0.06864745,0.000039491817,0.000024125326,0.0002186444,0.00033653446,0.8879942,0.002866614,0.038937263,0.0008289642,0.00003515219],"about_ca_topic_score_codex":0.0056902464,"about_ca_topic_score_gemma":0.0037867937,"teacher_disagreement_score":0.0056902464,"about_ca_system_score_codex":0.0012731592,"about_ca_system_score_gemma":0.00031528057,"threshold_uncertainty_score":0.011314273},"labels":[],"label_agreement":null},{"id":"W3186973207","doi":"10.1029/2021gl095082","title":"How Does Coastal Gravel Get Sorted Under Stormy Longshore Transport?","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coastal and Marine Dynamics","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Azrieli Foundation; Israel Science Foundation; United States - Israel Binational Science Foundation; United States-Israel Binational Science Foundation; National Science Foundation","keywords":"Geology; Storm; Longshore drift; Sorting; Shore; Underwater; Sediment transport; Bathymetry; Oceanography; Geomorphology; Sediment","score_opus":0.02524181194950865,"score_gpt":0.25536908710817613,"score_spread":0.2301272751586675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3186973207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9949444,0.000024756673,0.0033247874,0.00010535256,0.0000044883623,0.0000018330617,0.00003804665,0.000017899356,0.0015384661],"genre_scores_gemma":[0.99939215,0.000015102439,0.00018950283,0.000007636308,0.0000013284539,5.8001217e-7,0.000013500015,0.0000025101644,0.00037762886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999516,0.0000035788705,0.0000026620191,0.000017309958,0.000007628002,0.00001720929],"domain_scores_gemma":[0.9998784,0.000017605862,0.000039981343,0.000014305878,0.000020356305,0.000029324461],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000892881,0.00009941905,0.0001687882,0.00024022702,0.00033617823,0.00081661355,0.00028532447,0.00032753588,0.0015174955],"category_scores_gemma":[0.00057163025,0.00012128752,0.00012806471,0.00021980244,0.00062422396,0.0006398915,0.00033145805,0.00015755609,0.0001810607],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004232612,0.00016653181,0.41969776,0.00012748543,0.00012162657,0.0014880704,0.0012714613,0.31851906,0.16198125,0.038759016,0.0019310706,0.055513453],"study_design_scores_gemma":[0.000015263024,0.00015665193,0.2818108,0.000021121567,0.000029008774,0.00034872416,0.002164884,0.6895925,0.009720184,0.014846764,0.00125204,0.00004206466],"about_ca_topic_score_codex":0.010321891,"about_ca_topic_score_gemma":0.013170142,"teacher_disagreement_score":0.010321891,"about_ca_system_score_codex":0.00060138747,"about_ca_system_score_gemma":0.0003085151,"threshold_uncertainty_score":0.020523608},"labels":[],"label_agreement":null},{"id":"W3187426502","doi":"10.1029/2021gl095075","title":"Coupling Between Lithosphere Removal and Mantle Flow in the Central Andes","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"ExxonMobil Research and Engineering Company; National Natural Science Foundation of China","keywords":"Lithosphere; Geology; Magmatism; Crust; Mantle (geology); Subduction; Geophysics; Lithospheric flexure; Seismology; Tectonics","score_opus":0.03658094016581815,"score_gpt":0.28593971049661465,"score_spread":0.2493587703307965,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3187426502","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99825686,0.000029370953,0.00016446953,0.000059749775,0.0000010622222,0.0000025543086,0.000029992401,0.000015316926,0.0014406482],"genre_scores_gemma":[0.99968493,0.000022483286,0.00005191304,0.0000061860005,0.0000014068333,0.0000014087088,0.000023431598,0.0000027071505,0.0002055728],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99992096,0.000014094978,0.0000048607876,0.000023218972,0.000009476521,0.000027267286],"domain_scores_gemma":[0.9999068,0.00002035867,0.000029371726,0.000009276061,0.000013959055,0.000020259195],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014951214,0.0002446733,0.00031956777,0.000567535,0.00044879256,0.0009594712,0.00037519977,0.00039324892,0.0018065752],"category_scores_gemma":[0.00055156706,0.00026320168,0.00034866226,0.00033249523,0.000595606,0.00036633192,0.0008327371,0.00022491506,0.00014357426],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000771969,0.00030656008,0.57946575,0.00015699574,0.0006296071,0.0012440592,0.001849464,0.27597713,0.09564611,0.015355729,0.00090827554,0.027688354],"study_design_scores_gemma":[0.00014210009,0.000078240926,0.7636584,0.000016771155,0.00009436676,0.00011126241,0.0007386317,0.22725466,0.0025821566,0.0036581962,0.001624343,0.00004088726],"about_ca_topic_score_codex":0.073028885,"about_ca_topic_score_gemma":0.05428614,"teacher_disagreement_score":0.073028885,"about_ca_system_score_codex":0.0015159183,"about_ca_system_score_gemma":0.0005932828,"threshold_uncertainty_score":0.14520764},"labels":[],"label_agreement":null},{"id":"W3188952517","doi":"10.1029/2021gl093805","title":"Measuring Atmospheric CO <sub>2</sub> Enhancements From the 2017 British Columbia Wildfires Using a Lidar","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Armstrong Flight Research Center; National Aeronautics and Space Administration","keywords":"Lidar; Environmental science; Remote sensing; Meteorology; Atmospheric sciences; Geology; Geography","score_opus":0.030231505165869466,"score_gpt":0.2571505662838602,"score_spread":0.2269190611179907,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3188952517","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99583167,0.000048580554,0.00036563302,0.00005908079,0.0000075652406,0.00001685097,0.00072945823,0.00007798166,0.002863058],"genre_scores_gemma":[0.9978275,0.00005636751,0.0006348952,0.000028366348,0.00000253763,0.0000099766785,0.00058768876,0.000008118961,0.00084464025],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989545,0.0000048420784,0.0000021488108,0.000022572163,0.000051583705,0.00002331924],"domain_scores_gemma":[0.9998733,0.000010567812,0.000007648456,0.000005515295,0.00008342835,0.000019569145],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012714496,0.0003345585,0.00013308178,0.00036702334,0.0009633876,0.0005406971,0.0003373279,0.00030514697,0.00078402093],"category_scores_gemma":[0.00018454932,0.00015987366,0.000093665476,0.00058332126,0.00018457837,0.00021268365,0.00023403874,0.0005375404,0.00016917137],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006449529,0.0004828051,0.6072427,0.00014596696,0.00017060124,0.00081781595,0.0011824153,0.013158651,0.28910813,0.00022672795,0.0064955703,0.080323726],"study_design_scores_gemma":[0.000056123325,0.00015514647,0.8972565,0.000030514278,0.000089443274,0.00014465075,0.0013979991,0.036351416,0.059298355,0.00008726373,0.00508462,0.00004798931],"about_ca_topic_score_codex":0.68120325,"about_ca_topic_score_gemma":0.8661957,"teacher_disagreement_score":0.31879675,"about_ca_system_score_codex":0.0021952353,"about_ca_system_score_gemma":0.001701904,"threshold_uncertainty_score":0.64134836},"labels":[],"label_agreement":null},{"id":"W3190628334","doi":"10.1029/2021gl094038","title":"Quantifying the Effect of Precipitation on Landslide Hazard in Urbanized and Non‐Urbanized Areas","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":74,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Artificial Intelligence in Medicine (Canada)","funders":"Furman University; Stanford University","keywords":"Landslide; Urbanization; Precipitation; Hazard; Bay; Environmental science; Climatology; Climate change; Hazard analysis; Physical geography; Geography; Geology; Meteorology; Oceanography; Seismology; Ecology","score_opus":0.021204376026928713,"score_gpt":0.3001831732671068,"score_spread":0.2789787972401781,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3190628334","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980007,0.000022039254,0.0010030519,0.000030935134,0.0000016772008,0.000003061089,0.0005570996,0.000009220296,0.00037212172],"genre_scores_gemma":[0.999355,0.000015592099,0.00017698696,0.0000057466623,0.0000020788077,0.000002095124,0.00035494022,0.000001503046,0.00008608685],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996871,0.00014962889,0.0000143285615,0.00007013822,0.000037524995,0.000041387353],"domain_scores_gemma":[0.9966355,0.0018340712,0.0009649804,0.00024318649,0.00017852224,0.00014371106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006372623,0.00015944465,0.00017004565,0.0004463247,0.00014395165,0.00040837153,0.00023388816,0.00017004451,0.0012498957],"category_scores_gemma":[0.0026862896,0.00012227354,0.00033765077,0.00064498413,0.00032308948,0.00026409302,0.0004097057,0.00034014354,0.00013734888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077259705,0.000033711247,0.9788503,0.000007774972,0.00015132834,0.000035512,0.00004015737,0.01736738,0.00071382814,0.00016126002,0.00014512675,0.0024163644],"study_design_scores_gemma":[0.000003032516,0.00005242839,0.98355305,0.000003236737,0.00003245799,0.000021181591,0.00013401944,0.015222187,0.0006048483,0.00016554305,0.000202746,0.0000053663125],"about_ca_topic_score_codex":0.01581857,"about_ca_topic_score_gemma":0.01823874,"teacher_disagreement_score":0.01581857,"about_ca_system_score_codex":0.00024333074,"about_ca_system_score_gemma":0.0002431721,"threshold_uncertainty_score":0.031452954},"labels":[],"label_agreement":null},{"id":"W3190639937","doi":"10.1029/2021gl095264","title":"Magnitude and Uncertainty of Nitrous Oxide Emissions From North America Based on Bottom‐Up and Top‐Down Approaches: Informing Future Research and National Inventories","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; National Natural Science Foundation of China; European Commission; National Oceanic and Atmospheric Administration; Sight Research UK; Carnegie Institution for Science; Japan Society for the Promotion of Science; Agence Nationale de la Recherche; National Aeronautics and Space Administration; National Science Foundation","keywords":"Greenhouse gas; Nitrous oxide; Environmental science; Agriculture; Atmospheric sciences; Emission inventory; Environmental protection; Meteorology; Geography; Oceanography; Chemistry; Geology; Air quality index","score_opus":0.03456920977525337,"score_gpt":0.2795471107837228,"score_spread":0.24497790100846942,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3190639937","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97377735,0.0026772055,0.01274138,0.00081190286,0.000050526887,0.000035165904,0.0048540197,0.00011305766,0.004939345],"genre_scores_gemma":[0.9880121,0.0010940316,0.0078049023,0.0001234791,0.000019453251,0.000028226843,0.0025837559,0.00002298703,0.00031105767],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99950504,0.000115015646,0.00004649752,0.00015727733,0.0001221776,0.00005401095],"domain_scores_gemma":[0.9992261,0.0002180259,0.00012904569,0.00008290702,0.0003144799,0.00002955312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015106975,0.0005769004,0.00030336707,0.0012189101,0.00036751686,0.0013588726,0.00033302087,0.00026789858,0.00036803397],"category_scores_gemma":[0.001977763,0.00026365276,0.00081831636,0.0014633072,0.00033125054,0.001281997,0.00067842094,0.0003473652,0.00006511063],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014197126,0.00006019158,0.83095056,0.00037433603,0.0010188511,0.00013538198,0.00059128186,0.083784565,0.010565529,0.0024287333,0.0019978788,0.067950696],"study_design_scores_gemma":[0.000016288954,0.000050804843,0.84166306,0.00030843363,0.00062517653,0.000049606944,0.0012737717,0.123442106,0.009588065,0.0075418805,0.015356279,0.0000845373],"about_ca_topic_score_codex":0.15707019,"about_ca_topic_score_gemma":0.16151652,"teacher_disagreement_score":0.15707019,"about_ca_system_score_codex":0.0016081937,"about_ca_system_score_gemma":0.0014490631,"threshold_uncertainty_score":0.3123119},"labels":[],"label_agreement":null},{"id":"W3191060824","doi":"10.1029/2021gl092948","title":"Holocene Hydroclimatic Reorganizations in Northwest Canada Inferred From Lacustrine Carbonate Oxygen Isotopes","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Authigenic; Holocene; Calcite; Geology; Stalagmite; Speleothem; Isotopes of oxygen; Ostracod; Precipitation; Carbonate; Glacial period; Paleoclimatology; Climatology; Climate change; Oceanography; Physical geography; Geochemistry; Cave; Geography; Archaeology; Sedimentary rock; Paleontology","score_opus":0.022783154258551236,"score_gpt":0.25793206419259,"score_spread":0.23514890993403878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3191060824","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99608445,0.00033541402,0.00007260558,0.0001083845,0.000003417256,0.000004505773,0.00143478,0.000011985308,0.0019444228],"genre_scores_gemma":[0.9981425,0.00020881703,0.000119333665,0.00001911625,0.0000012652789,0.0000020872126,0.0007275937,0.00000428051,0.0007749339],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990726,0.0000039250667,0.0000027893798,0.000023112874,0.000020967467,0.000041928157],"domain_scores_gemma":[0.99955004,0.000020736064,0.000053638916,0.000012602597,0.0002633227,0.00009963711],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017466405,0.00013837292,0.00013146683,0.0011805575,0.0015545454,0.00084319495,0.00032690357,0.00018571968,0.0014898919],"category_scores_gemma":[0.00048778366,0.00016349464,0.00012402829,0.001484439,0.00046477423,0.00025511,0.00033045752,0.000240381,0.00014790952],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000107846834,0.000012941538,0.9775783,0.000026075622,0.00004212285,0.00011738524,0.0014290313,0.00034823595,0.004122933,0.00032582175,0.0009461418,0.014943079],"study_design_scores_gemma":[0.0000013366769,0.0000022674258,0.99803454,0.0000070834394,0.000005414275,0.000014346818,0.00043520133,0.00017360784,0.00015672739,0.000017199443,0.0011490416,0.0000031942122],"about_ca_topic_score_codex":0.9856836,"about_ca_topic_score_gemma":0.99643683,"teacher_disagreement_score":0.01431638,"about_ca_system_score_codex":0.011533819,"about_ca_system_score_gemma":0.0073082247,"threshold_uncertainty_score":0.08368403},"labels":[],"label_agreement":null},{"id":"W3191737884","doi":"10.1029/2021gl093962","title":"“Tiny Wiggles” in the Late Miocene Red Clay Deposits in the North‐East of the Tibetan Plateau","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Magnetostratigraphy; Geology; Earth's magnetic field; Plateau (mathematics); Precession; Paleontology; Geomagnetic reversal; Aeolian processes; Sedimentary rock; Paleomagnetism; Geophysics; Physics; Magnetic field; Astronomy","score_opus":0.03933119395567247,"score_gpt":0.2821527689162485,"score_spread":0.24282157496057605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3191737884","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995926,0.00003611804,0.00009853685,0.0000076276638,8.215047e-7,0.0000016906217,0.000048038328,0.0000047589115,0.00020980058],"genre_scores_gemma":[0.99981695,0.000009942709,0.00005026819,0.0000017036431,0.000001033779,8.1626865e-7,0.00004945644,6.266175e-7,0.00006908206],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993706,0.000010272254,0.0000071309523,0.000021330612,0.000009678525,0.0000145137055],"domain_scores_gemma":[0.9997596,0.000029022107,0.0001073407,0.000018812854,0.000045448614,0.000039803534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026728166,0.00015471675,0.000101399644,0.0013036533,0.0003398191,0.0003065495,0.00019162086,0.00017016096,0.0005305371],"category_scores_gemma":[0.0003577428,0.000090138456,0.000101173144,0.0008962127,0.0003567398,0.00019834413,0.00022386842,0.000098004595,0.00006668898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009750102,0.0000147811115,0.977817,0.000029330335,0.000032140037,0.00027669067,0.0007631963,0.0005063101,0.0097074425,0.00012446094,0.00006466303,0.01056644],"study_design_scores_gemma":[0.0000018193382,0.000016928472,0.9988777,0.0000023852544,0.0000039939823,0.000044229404,0.0001387799,0.0005861951,0.00019135013,0.000018998555,0.0001159848,0.0000016464464],"about_ca_topic_score_codex":0.021209292,"about_ca_topic_score_gemma":0.04043303,"teacher_disagreement_score":0.021209292,"about_ca_system_score_codex":0.00031801895,"about_ca_system_score_gemma":0.00021255999,"threshold_uncertainty_score":0.042171717},"labels":[],"label_agreement":null},{"id":"W3192000635","doi":"10.1029/2021gl094695","title":"Mercury's Northern Rise Core‐Field Magnetic Anomaly","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"National Aeronautics and Space Administration","keywords":"Mercury (programming language); Geology; Geophysics; Magnetic anomaly; Anomaly (physics); Seismology; Geodesy; Physics; Condensed matter physics","score_opus":0.022720766870169423,"score_gpt":0.2942189658905876,"score_spread":0.27149819902041816,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192000635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822456,0.000036652436,0.00014400664,0.000021970112,0.000001582284,0.0000011696262,0.00017633683,0.000020614656,0.0013731614],"genre_scores_gemma":[0.9988913,0.00006120972,0.0003170403,0.000007154595,0.0000026746754,6.71012e-7,0.00030056245,0.000002746538,0.00041660413],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997115,0.000002032061,6.4618473e-7,0.000009797094,0.000010139716,0.000006268693],"domain_scores_gemma":[0.99995613,0.0000032781631,0.000013374733,0.0000040029527,0.000011118815,0.000012196127],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00003753054,0.000096875105,0.00009295853,0.00039151817,0.00019378863,0.00020312288,0.00006972973,0.00009915623,0.00046323173],"category_scores_gemma":[0.000092909526,0.00004695154,0.00007108919,0.0004895005,0.00012542133,0.000053379936,0.0001206363,0.00007463867,0.00013247947],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030856772,0.000038017744,0.42533004,0.00003704637,0.000051610474,0.00055095693,0.00051628496,0.0007220313,0.5338454,0.0007071071,0.0006595594,0.03723333],"study_design_scores_gemma":[0.000004527748,0.000038859165,0.9793355,0.0000020042519,0.000012889378,0.00029422075,0.00009415535,0.00051438535,0.018572042,0.00012259859,0.0010049072,0.000003936804],"about_ca_topic_score_codex":0.010627092,"about_ca_topic_score_gemma":0.014975877,"teacher_disagreement_score":0.010627092,"about_ca_system_score_codex":0.0002315166,"about_ca_system_score_gemma":0.00020117826,"threshold_uncertainty_score":0.021130443},"labels":[],"label_agreement":null},{"id":"W3192130624","doi":"10.1029/2021gl093875","title":"Continental‐Scale Geographic Trends in Barometric‐Pumping Efficiency Potential: A North American Case Study","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Pacific Northwest National Laboratory; Lawrence Livermore National Laboratory; Workforce Development for Teachers and Scientists; Los Alamos National Laboratory; National Nuclear Security Administration; Office of Science; Office of Defense Nuclear Nonproliferation; U.S. Department of Energy","keywords":"Longitude; Latitude; Elevation (ballistics); Environmental science; Range (aeronautics); Geographic coordinate system; Scale (ratio); Atmospheric pressure; Continental shelf; Potential temperature; Climatology; Atmospheric sciences; Geology; Oceanography; Geodesy; Geography; Physics","score_opus":0.014249789987370089,"score_gpt":0.28056008236639757,"score_spread":0.2663102923790275,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192130624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99793553,0.0000516803,0.00016841805,0.00006153744,0.0000011052026,0.000005295036,0.0008099095,0.000008140791,0.00095840544],"genre_scores_gemma":[0.998898,0.00006671294,0.00024824502,0.000010424787,0.0000016966126,0.0000059127083,0.00051134353,0.000002436802,0.00025514708],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99980646,0.00004438492,0.000010637621,0.000054390726,0.000041194682,0.000042880525],"domain_scores_gemma":[0.99886346,0.00027338267,0.00023686705,0.000072351926,0.00045308968,0.00010092313],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003594377,0.00016047235,0.00014148891,0.0012349667,0.0004803119,0.0007377836,0.00034062707,0.00022230337,0.0007921699],"category_scores_gemma":[0.0011178507,0.00013160855,0.00018905524,0.0037078783,0.00036912062,0.00039576867,0.00046077455,0.00028926207,0.00008625197],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000022581622,0.000027793569,0.9914288,0.000009444714,0.000040936742,0.00028834186,0.00034237574,0.0023583767,0.000334648,0.0001908588,0.000569443,0.004386348],"study_design_scores_gemma":[0.0000021123847,0.000007700109,0.99364,0.000004784404,0.0000152118255,0.000096286945,0.00095740845,0.004338143,0.000103302285,0.00007061851,0.0007570608,0.000007426665],"about_ca_topic_score_codex":0.58187526,"about_ca_topic_score_gemma":0.7160209,"teacher_disagreement_score":0.58187526,"about_ca_system_score_codex":0.0017610153,"about_ca_system_score_gemma":0.0008309658,"threshold_uncertainty_score":0.8411743},"labels":[],"label_agreement":null},{"id":"W3192671250","doi":"10.1029/2021gl093312","title":"Enigmatic Mid‐Proterozoic Orogens: Hot, Thin, and Low","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":72,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Proterozoic; Geology; Supercontinent; Archean; Rodinia; Earth science; Mountain formation; Metamorphic rock; Geologic record; Phanerozoic; Magmatism; Paleontology; Tectonics; Geophysics; Craton; Cenozoic; Structural basin","score_opus":0.027206138372915883,"score_gpt":0.25610377870064754,"score_spread":0.22889764032773166,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3192671250","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9844328,0.0033999353,0.0008121864,0.00097163627,0.000020832322,0.000006845755,0.00028953434,0.000025825435,0.010040288],"genre_scores_gemma":[0.998126,0.0009185385,0.00017345049,0.00008731109,0.000016343694,8.3748245e-7,0.00010361361,0.0000051599513,0.0005687087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989283,0.000012426805,0.0000066765656,0.00003483323,0.000023549388,0.000029643685],"domain_scores_gemma":[0.9996911,0.000032676337,0.0001247932,0.000036300098,0.000065315566,0.00004989356],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032465707,0.00016162761,0.00018377126,0.0011023186,0.00056859455,0.001079141,0.0002421414,0.00017918901,0.0015781771],"category_scores_gemma":[0.0005158148,0.000105741885,0.000062774336,0.0010119037,0.0018018632,0.00055017567,0.0006880889,0.00035289652,0.00019728582],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047322956,0.000028298478,0.8335914,0.00041842935,0.00018352961,0.0006442566,0.0058679814,0.0008449111,0.052959334,0.022930847,0.0017613893,0.080296434],"study_design_scores_gemma":[0.0000049849377,0.000023676714,0.96795636,0.00007131498,0.000047349928,0.00040195463,0.0048251697,0.00043534458,0.0030023397,0.004902644,0.018316645,0.000012135836],"about_ca_topic_score_codex":0.008947299,"about_ca_topic_score_gemma":0.015726935,"teacher_disagreement_score":0.008947299,"about_ca_system_score_codex":0.00064824225,"about_ca_system_score_gemma":0.00044450368,"threshold_uncertainty_score":0.017790496},"labels":[],"label_agreement":null},{"id":"W3193342613","doi":"10.1029/2021gl095099","title":"First Observations of a Transient Polynya in the Last Ice Area North of Ellesmere Island","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Arctic; Climatology; Geology; Arctic ice pack; Oceanography; The arctic; Sea ice; Cryosphere; Physical geography; Geography","score_opus":0.04158417782153212,"score_gpt":0.2583838039920769,"score_spread":0.21679962617054477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193342613","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99724615,0.00011455058,0.00011667885,0.000047625945,0.000007171595,0.0000118722555,0.00046269223,0.000013139258,0.0019801147],"genre_scores_gemma":[0.99806994,0.00010899658,0.00044726458,0.000045500237,0.000009038276,0.000014111886,0.0005784871,0.0000035735127,0.0007231404],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999517,0.000004980146,0.0000032195755,0.000014013917,0.000012532893,0.000013572603],"domain_scores_gemma":[0.99976426,0.00002828092,0.00004543045,0.00001940069,0.00007803595,0.00006458373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013940393,0.0001224503,0.000117578544,0.00036108968,0.00064961065,0.0003808527,0.0001659685,0.00030968705,0.00080608093],"category_scores_gemma":[0.0002753542,0.00012377097,0.00008444144,0.00031240666,0.00025262978,0.00018591972,0.00036970628,0.0003094474,0.00014781859],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001550244,0.0000698029,0.97398937,0.000033508124,0.00004119617,0.0007973689,0.0010454077,0.00019234238,0.01635903,0.00007525329,0.0009297952,0.0063119526],"study_design_scores_gemma":[0.0000024014766,0.000020901345,0.99812084,0.00000624523,0.000005969889,0.00007785182,0.00035458963,0.000112718975,0.00032992323,0.0000066049142,0.0009602889,0.0000015827202],"about_ca_topic_score_codex":0.061516453,"about_ca_topic_score_gemma":0.22431785,"teacher_disagreement_score":0.93848354,"about_ca_system_score_codex":0.0004337086,"about_ca_system_score_gemma":0.00032785142,"threshold_uncertainty_score":0.12231678},"labels":[],"label_agreement":null},{"id":"W3193474468","doi":"10.1029/2021gl094178","title":"Extreme High Greenland Blocking Index Leads to the Reversal of Davis and Nares Strait Net Transport Toward the Arctic Ocean","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; University of Manitoba; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Oceanography; Bay; Geology; Arctic; Greenland ice sheet; Thermohaline circulation; Climatology; Ice sheet","score_opus":0.034227694349476624,"score_gpt":0.2567796177224444,"score_spread":0.22255192337296778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3193474468","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99936515,0.000018177047,0.00001999969,0.000032961714,0.000004930708,0.0000011924648,0.00007747582,0.0000032091648,0.00047702025],"genre_scores_gemma":[0.9994628,0.000014406796,0.00002140737,0.00001789062,0.000001480335,9.726716e-7,0.000106841544,0.0000014492101,0.0003728726],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999584,0.0000045107745,0.0000016314491,0.0000116885485,0.0000054340476,0.000018281082],"domain_scores_gemma":[0.99982506,0.00001591252,0.000045367316,0.000008904214,0.000016106851,0.00008869022],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006967635,0.00012745315,0.00012941667,0.00019604333,0.00026422951,0.00037718168,0.00007234783,0.00014460817,0.0019256695],"category_scores_gemma":[0.0002411516,0.00005777009,0.00014599114,0.00013110004,0.0001660844,0.00005468332,0.00013939728,0.0002599873,0.0001550591],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052024605,0.000113393864,0.947398,0.0000090625035,0.00006595095,0.00089965196,0.00013747103,0.0003666929,0.044868413,0.00011700285,0.0011431559,0.0043609254],"study_design_scores_gemma":[0.000001952751,0.00002529308,0.9986633,0.0000018625464,0.0000066365014,0.000096641925,0.00010179124,0.00017169565,0.0007197335,0.0000142647195,0.00019529244,0.0000015590024],"about_ca_topic_score_codex":0.064490564,"about_ca_topic_score_gemma":0.096587665,"teacher_disagreement_score":0.064490564,"about_ca_system_score_codex":0.00053836056,"about_ca_system_score_gemma":0.0005433477,"threshold_uncertainty_score":0.12823033},"labels":[],"label_agreement":null},{"id":"W3194039805","doi":"10.1029/2021gl094085","title":"Statistical Study of Whistler‐Mode Waves and Expected Pitch Angle Diffusion Rates During Dispersionless Electron Injections","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsches Zentrum für Luft- und Raumfahrt; National Aeronautics and Space Administration","keywords":"Whistler; Physics; Pitch angle; Electron; Diffusion; Mode (computer interface); Geophysics; Geology; Computational physics; Quantum electrodynamics; Nuclear physics; Quantum mechanics","score_opus":0.012774123365572798,"score_gpt":0.30829758533106805,"score_spread":0.2955234619654952,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3194039805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99772483,0.000026657,0.0017025161,0.000015658607,0.0000023132243,0.0000047679328,0.00024743663,0.000020422634,0.0002553766],"genre_scores_gemma":[0.99938977,0.00001070252,0.00015967153,0.0000012760256,0.00000268149,0.0000032339328,0.0003217957,0.0000035518347,0.00010722508],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998167,0.000024383702,0.000013086565,0.00007858105,0.000033094944,0.000034090113],"domain_scores_gemma":[0.99635917,0.0019210239,0.0009861696,0.0002710886,0.00027663627,0.00018590185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000634548,0.00013313,0.00014254544,0.0006680691,0.00016652538,0.00037028422,0.0002205603,0.00020254731,0.0009882946],"category_scores_gemma":[0.0033274686,0.000103072234,0.00020526019,0.00039925665,0.00031488854,0.00041459664,0.00021292572,0.0002568122,0.00012132998],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027331966,0.000060122067,0.9414264,0.00003471713,0.00014066152,0.00034548718,0.00022784113,0.026916552,0.017263416,0.0016746995,0.0005775446,0.011059249],"study_design_scores_gemma":[0.000011801106,0.00011437899,0.8747508,0.000006298234,0.000035337827,0.00026985566,0.00018661079,0.11883077,0.004635158,0.0006274308,0.00050412165,0.000027448183],"about_ca_topic_score_codex":0.0016456806,"about_ca_topic_score_gemma":0.0013743595,"teacher_disagreement_score":0.0016456806,"about_ca_system_score_codex":0.00020777887,"about_ca_system_score_gemma":0.00010482409,"threshold_uncertainty_score":0.0033558607},"labels":[],"label_agreement":null},{"id":"W3195342402","doi":"10.1029/2021gl094020","title":"Electrical Conductivity of Aqueous NaCl at High Pressure and Low Temperature: Application to Deep Subsurface Oceans of Icy Moons","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Calcium Carbonate Crystallization and Inhibition","field":"Materials Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Foundation for Innovation","keywords":"Molality; Electrical resistivity and conductivity; Icy moon; Conductivity; Aqueous solution; Conductance; Limiting; Atmospheric temperature range; Analytical Chemistry (journal); Geology; Mineralogy; Materials science; Chemistry; Thermodynamics; Environmental chemistry; Physics; Condensed matter physics; Saturn","score_opus":0.014913028014395336,"score_gpt":0.28360604985583626,"score_spread":0.26869302184144095,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195342402","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907494,0.00003734384,0.00054409535,0.000032120242,0.000002023434,0.0000040114955,0.00005683443,0.000015910535,0.0002325933],"genre_scores_gemma":[0.99929786,0.000030496889,0.0005755509,0.000003351388,9.178373e-7,0.00000383536,0.000034455486,0.000002028469,0.000051508752],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999211,0.000012753988,0.000007706982,0.000016469461,0.000028627019,0.000013288751],"domain_scores_gemma":[0.99983346,0.00005886911,0.000024851197,0.000016406524,0.000049111797,0.000017257235],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012863835,0.00019357349,0.00023791956,0.00018154857,0.0001874214,0.00025812894,0.00022226182,0.0002179158,0.00038479688],"category_scores_gemma":[0.00037171948,0.00009705837,0.0001626404,0.00028236661,0.0003093194,0.00017178107,0.00026636687,0.00024199714,0.000047405036],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017781643,0.0000471578,0.007346907,0.0000877701,0.000012062964,0.00013309518,0.00013242492,0.017718993,0.97067463,0.00021276747,0.000057523503,0.0033988184],"study_design_scores_gemma":[0.000041320553,0.0005682915,0.0122176185,0.0000071637323,0.000016104186,0.00007003724,0.00018935447,0.09349432,0.8926314,0.00025717352,0.00048707458,0.000020278714],"about_ca_topic_score_codex":0.0029053797,"about_ca_topic_score_gemma":0.0013305531,"teacher_disagreement_score":0.0029053797,"about_ca_system_score_codex":0.00030985245,"about_ca_system_score_gemma":0.00016770822,"threshold_uncertainty_score":0.005776942},"labels":[],"label_agreement":null},{"id":"W3195808224","doi":"10.1029/2021gl094130","title":"Polar Amplification in Idealized Climates: The Role of Ice, Moisture, and Seasons","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":59,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canada Research Chairs; Compute Canada; National Science Foundation","keywords":"Environmental science; Ice-albedo feedback; Sea ice; Climatology; Albedo (alchemy); Atmospheric sciences; Sea ice thickness; Latent heat; Polar; Moisture; Cryosphere; Geology; Meteorology; Physics","score_opus":0.03016254274186945,"score_gpt":0.30946261390778274,"score_spread":0.27930007116591327,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3195808224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9778998,0.00016566414,0.01577488,0.00027618656,0.00003153586,0.00002181298,0.00025593335,0.000110634624,0.0054635713],"genre_scores_gemma":[0.99910444,0.000055526332,0.0005108395,0.000015843456,0.000008460221,0.000011578118,0.000045755063,0.000010226749,0.00023739463],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997489,0.000117401825,0.0000110371775,0.000037214755,0.000033531614,0.000051951723],"domain_scores_gemma":[0.9993259,0.0003340225,0.00011114144,0.000090362264,0.000065970125,0.00007260929],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054185174,0.00052932557,0.00050269,0.0003045021,0.0003233147,0.001003047,0.00049102586,0.0003167804,0.0012476655],"category_scores_gemma":[0.0020233295,0.00030244642,0.0004937803,0.00023313051,0.0009023473,0.0013117241,0.0010269481,0.0004234776,0.00011424521],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038723226,0.000060133803,0.009249536,0.000042054493,0.000056909113,0.00015959673,0.00008988959,0.9732425,0.006556596,0.008123869,0.00019543609,0.0018363016],"study_design_scores_gemma":[0.00006780731,0.00006682969,0.004296245,0.000006696631,0.00002705445,0.000031830543,0.00006379446,0.9870679,0.0010224056,0.0070347423,0.00028916568,0.00002566873],"about_ca_topic_score_codex":0.005832831,"about_ca_topic_score_gemma":0.0029895839,"teacher_disagreement_score":0.005832831,"about_ca_system_score_codex":0.0005170442,"about_ca_system_score_gemma":0.00059261336,"threshold_uncertainty_score":0.011597753},"labels":[],"label_agreement":null},{"id":"W3196909956","doi":"10.1029/2021gl094008","title":"Significant Contribution of Stratospheric Water Vapor to the Poleward Expansion of the Hadley Circulation in Autumn Under Greenhouse Warming","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fundamental Research Funds for the Central Universities; Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Hadley cell; Stratosphere; Atmospheric sciences; Environmental science; Water vapor; Climatology; Greenhouse gas; Polar vortex; Atmospheric circulation; Subtropics; General Circulation Model; Climate change; Geology; Physics; Meteorology","score_opus":0.0370007117592265,"score_gpt":0.2907379865835378,"score_spread":0.2537372748243113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3196909956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99939466,0.00004815871,0.0001763359,0.000017589193,0.0000068412833,0.0000016769666,0.00003831218,0.000016175914,0.00030019213],"genre_scores_gemma":[0.9998006,0.000011509579,0.00004259916,0.00000937396,0.0000023457308,0.0000013959523,0.000040701234,0.0000024502108,0.00008900715],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999709,0.000006055659,0.0000012983389,0.000009278902,0.0000039355723,0.000008548697],"domain_scores_gemma":[0.99989176,0.000024780462,0.000017878068,0.000012883169,0.0000134128295,0.000039177456],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000101450896,0.00014890208,0.00018440245,0.00011225904,0.00016951078,0.0002618603,0.0000984528,0.00017321995,0.0008090155],"category_scores_gemma":[0.00019236482,0.000080734564,0.0001359177,0.00007134074,0.00019160022,0.00015178663,0.00022452702,0.00024283267,0.00007333753],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00064297125,0.000067428155,0.096889235,0.000051541232,0.000072102164,0.00021943547,0.00011266071,0.0016933947,0.8945006,0.00023901665,0.00018529744,0.005326237],"study_design_scores_gemma":[0.00003498629,0.00022183977,0.960971,0.0000047752656,0.00002936839,0.00007976937,0.00010745286,0.004977511,0.032647975,0.00021705663,0.00069621054,0.000012055429],"about_ca_topic_score_codex":0.0020641517,"about_ca_topic_score_gemma":0.0020512422,"teacher_disagreement_score":0.0020641517,"about_ca_system_score_codex":0.00013775022,"about_ca_system_score_gemma":0.00013080909,"threshold_uncertainty_score":0.0041043162},"labels":[],"label_agreement":null},{"id":"W3197104079","doi":"10.1029/2020gl091919","title":"Sensitivity Analysis of the Maximum Entropy Production Method to Model Evaporation in Boreal and Temperate Forests","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec en Outaouais; Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; Université du Québec en Outaouais; National Aeronautics and Space Administration; National Science Foundation","keywords":"Environmental science; Temperate climate; Climate change; Atmospheric sciences; Boreal; Evaporation; Latent heat; Entropy production; Temperate forest; Sensitivity (control systems); Transpiration; Climatology; Meteorology; Ecology; Physics; Thermodynamics; Geology; Chemistry","score_opus":0.02070062416882866,"score_gpt":0.2996049289422551,"score_spread":0.2789043047734264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3197104079","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96712196,0.00025537968,0.030775484,0.00014588668,0.0000197646,0.000047557092,0.0002554808,0.00015242396,0.0012260997],"genre_scores_gemma":[0.9979311,0.000020708996,0.0018748877,0.000012379959,0.0000035529067,0.0000151787635,0.000069780705,0.000010258582,0.00006211505],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99884653,0.00086056476,0.000045898905,0.000091057256,0.000085761734,0.00007027896],"domain_scores_gemma":[0.9884421,0.010571668,0.0002925868,0.0002916708,0.00029464657,0.00010724883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0045709647,0.00076264195,0.0005760616,0.00074688974,0.0003976653,0.00067435246,0.00067559205,0.00082779274,0.000492904],"category_scores_gemma":[0.010194416,0.00040955283,0.00092534826,0.00044505653,0.00052362843,0.0007979688,0.00084207684,0.00075423386,0.00004441238],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006906501,0.000019865909,0.007163772,0.000019966783,0.00007659096,0.000030181707,0.000014233463,0.99053055,0.00055827433,0.00022744261,0.000043042004,0.0012470401],"study_design_scores_gemma":[0.000007310505,0.000053651063,0.0031341508,0.0000055207697,0.000013792458,0.000010805989,0.000012751875,0.9954666,0.0008432174,0.0003856014,0.000057087356,0.000009449975],"about_ca_topic_score_codex":0.011422339,"about_ca_topic_score_gemma":0.0036775495,"teacher_disagreement_score":0.011422339,"about_ca_system_score_codex":0.0007994313,"about_ca_system_score_gemma":0.00037386976,"threshold_uncertainty_score":0.024173856},"labels":[],"label_agreement":null},{"id":"W3197720282","doi":"10.1029/2021gl094889","title":"On the Stability of Talc in Subduction Zones: A Possible Control on the Maximum Depth of Decoupling Between the Subducting Plate and Mantle Wedge","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of British Columbia","funders":"","keywords":"Geology; Mantle wedge; Mantle (geology); Transition zone; Forearc; Subduction; Petrology; Slab; Geophysics; Forsterite; Enstatite; Geochemistry; Seismology; Tectonics","score_opus":0.05308831523838486,"score_gpt":0.27231898699221607,"score_spread":0.2192306717538312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3197720282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998895,0.00009976704,0.00037805343,0.000011742897,5.9586745e-7,0.000002190846,0.00006345535,0.0000075591,0.0005417052],"genre_scores_gemma":[0.9998722,0.000009466728,0.000052460015,0.000001788383,3.9016695e-7,6.9953785e-7,0.00002329147,0.0000012576836,0.00003843111],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999442,0.000007384915,0.00000412923,0.000017479635,0.000010431338,0.00001621138],"domain_scores_gemma":[0.99969566,0.00009213527,0.00006679997,0.000024646342,0.000046639456,0.0000740822],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019994863,0.00012597544,0.00013772579,0.0006262022,0.00022472149,0.0005758063,0.00029340698,0.0001515668,0.00096715876],"category_scores_gemma":[0.0005758824,0.00013228785,0.00008916252,0.00021104336,0.0005412403,0.00027609183,0.0004226094,0.00011831679,0.000118634925],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011049004,0.000023250228,0.08581751,0.000054551118,0.000030365656,0.00015858341,0.00030151787,0.001627407,0.90258044,0.0014928452,0.000053814583,0.006754823],"study_design_scores_gemma":[0.00005496511,0.0002087093,0.6074101,0.000012257169,0.000046041627,0.00020047196,0.00047603415,0.012287754,0.37733358,0.0010656297,0.00088286604,0.000021607158],"about_ca_topic_score_codex":0.0024899726,"about_ca_topic_score_gemma":0.001803362,"teacher_disagreement_score":0.0024899726,"about_ca_system_score_codex":0.00036627587,"about_ca_system_score_gemma":0.0001637733,"threshold_uncertainty_score":0.004951},"labels":[],"label_agreement":null},{"id":"W3199018952","doi":"10.1029/2021gl095312","title":"Coupled Impacts of Atmospheric Circulation and Sea‐Ice on Late Pleistocene Terrigenous Sediment Dynamics in the Subarctic Pacific Ocean","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"National Natural Science Foundation of China; Natural Environment Research Council; China Postdoctoral Science Foundation; Sight Research UK","keywords":"Subarctic climate; Geology; Oceanography; Terrigenous sediment; Sea ice; Climatology; Thermohaline circulation; Orbital forcing; Atmospheric circulation; Climate change; Glacial period; Arctic sea ice decline; Sedimentary rock; Drift ice; Cryosphere; Paleontology","score_opus":0.020620302457399275,"score_gpt":0.2676383021478498,"score_spread":0.24701799969045052,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3199018952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99964726,0.000025394562,0.000031113144,0.00002238563,0.000002108925,7.713388e-7,0.000097114644,0.000005489356,0.00016832541],"genre_scores_gemma":[0.99977344,0.000028796572,0.000034975892,0.00000775509,0.0000019771135,0.0000012489326,0.000077338605,0.0000023832397,0.00007213234],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993646,0.00001618885,0.0000056387153,0.000017936967,0.00000851363,0.000015296835],"domain_scores_gemma":[0.9998423,0.000041945026,0.000037009475,0.000014927404,0.000024900359,0.000038887116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000297144,0.00024687225,0.00021331769,0.00039472966,0.00029761207,0.0007999937,0.00014889427,0.00019772837,0.0010310988],"category_scores_gemma":[0.00059077685,0.00020022756,0.0003044272,0.00036569685,0.00032294905,0.00028025827,0.00053940865,0.0002217485,0.00009206365],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002355282,0.00007659786,0.9637158,0.00003035087,0.00044131815,0.00027417962,0.0002679974,0.014185954,0.014232176,0.0003239157,0.0002917508,0.0059242994],"study_design_scores_gemma":[0.0000097421025,0.000019892641,0.99243695,0.0000034893117,0.000048168782,0.000020449019,0.000119919714,0.006678074,0.0004328678,0.00008333533,0.00014141994,0.0000056863346],"about_ca_topic_score_codex":0.03160857,"about_ca_topic_score_gemma":0.035977498,"teacher_disagreement_score":0.03160857,"about_ca_system_score_codex":0.00080958114,"about_ca_system_score_gemma":0.00059213967,"threshold_uncertainty_score":0.06284922},"labels":[],"label_agreement":null},{"id":"W3200244765","doi":"10.1029/2021gl094776","title":"Saltwater Intrusion Intensifies Coastal Permafrost Thaw","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"U.S. Geological Survey; National Science Foundation","keywords":"Permafrost; Saltwater intrusion; Climate change; Environmental science; Global warming; Intrusion; Geology; Aquifer; Hydrology (agriculture); Oceanography; Groundwater; Geotechnical engineering","score_opus":0.07192432266908202,"score_gpt":0.3061424451567975,"score_spread":0.23421812248771548,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200244765","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966974,0.000026530108,0.0004604433,0.000101280915,0.0000076023225,0.000004388999,0.00015732567,0.000039305512,0.002505821],"genre_scores_gemma":[0.99963665,0.000017965927,0.000086031985,0.000014848665,0.0000016032429,0.0000022591953,0.00004719175,0.0000042067086,0.00018927733],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999418,0.000008769247,0.0000050278377,0.000018959341,0.0000069997864,0.000018401433],"domain_scores_gemma":[0.99990153,0.000026720456,0.000025110405,0.000009539355,0.00001226011,0.000024818355],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008068747,0.00022863482,0.00021846025,0.00017499595,0.0003190691,0.0007046507,0.0002959032,0.00043935076,0.0032609939],"category_scores_gemma":[0.00033161262,0.00013819727,0.00044068272,0.00016435949,0.00043510552,0.0004571436,0.0006772849,0.00032520198,0.00014862193],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030848524,0.0003682297,0.30922237,0.00016502877,0.00018411415,0.0009230696,0.0003033738,0.6104768,0.06197491,0.0045479145,0.0012828569,0.010242923],"study_design_scores_gemma":[0.00008260551,0.00015001769,0.13709573,0.000029005669,0.00007184958,0.00011685729,0.00045009988,0.8526787,0.006425353,0.0016092561,0.0012537694,0.000036752303],"about_ca_topic_score_codex":0.016958524,"about_ca_topic_score_gemma":0.012585157,"teacher_disagreement_score":0.016958524,"about_ca_system_score_codex":0.00069396675,"about_ca_system_score_gemma":0.0005130079,"threshold_uncertainty_score":0.03371966},"labels":[],"label_agreement":null},{"id":"W3200413132","doi":"10.1029/2021gl095200","title":"Fate of Fugitive Natural Gas in Heterogeneous Near‐Surface Sediments in a Region of Extensive Petroleum Resource Development","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Carleton University; University of British Columbia","funders":"Natural Resources Canada","keywords":"Fugitive emissions; Groundwater; Greenhouse gas; Natural gas; Environmental science; Geology; Atmosphere (unit); Aquifer; Petroleum; Fossil fuel; Hydrology (agriculture); Waste management; Geotechnical engineering; Oceanography","score_opus":0.015176503791703752,"score_gpt":0.2538712929274408,"score_spread":0.23869478913573705,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200413132","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999729,0.000019950461,0.000045942168,0.0000030239157,2.8253666e-7,0.0000015908738,0.0000911503,0.0000019079819,0.00010721628],"genre_scores_gemma":[0.99956185,0.000037590635,0.00015047326,0.000003235582,3.8922985e-7,0.0000018813968,0.0001183604,7.976978e-7,0.00012550029],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999515,0.00000272424,0.0000017556571,0.000015849299,0.000012838103,0.000015246775],"domain_scores_gemma":[0.9999156,0.0000063352945,0.000021414433,0.0000029172704,0.00003600708,0.000017700462],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000066748216,0.0002069812,0.00017593906,0.0004860348,0.0006168408,0.00040285586,0.00022755635,0.00018380859,0.00021836112],"category_scores_gemma":[0.00012578662,0.00009999837,0.00009065307,0.00054575945,0.00034868403,0.00021568272,0.00026177694,0.00014596288,0.00003684107],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032940943,0.000074347525,0.7623668,0.000054868804,0.00006816002,0.00039096078,0.001107517,0.0025130895,0.2244736,0.00015042981,0.00011325631,0.00835767],"study_design_scores_gemma":[0.000004612913,0.000071604,0.9866919,0.0000057954485,0.000014192832,0.000048123155,0.00093012676,0.0020823064,0.009650583,0.000029232326,0.00046397647,0.000007399595],"about_ca_topic_score_codex":0.49821907,"about_ca_topic_score_gemma":0.6134783,"teacher_disagreement_score":0.49821907,"about_ca_system_score_codex":0.0017527747,"about_ca_system_score_gemma":0.00089553377,"threshold_uncertainty_score":0.99063826},"labels":[],"label_agreement":null},{"id":"W3200801709","doi":"10.1029/2021gl094726","title":"Atmospheric Circulation Sensitivity to Changes in the Vertical Structure of Polar Warming","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Hadley cell; Environmental science; Atmospheric circulation; Atmospheric sciences; Climatology; Longwave; Polar; Northern Hemisphere; Extratropical cyclone; Troposphere; Forcing (mathematics); Radiative forcing; Climate change; Geology; Radiative transfer; General Circulation Model; Physics","score_opus":0.020632800994397054,"score_gpt":0.26821063711062676,"score_spread":0.24757783611622972,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200801709","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976802,0.000061048166,0.0007488207,0.00010534074,0.000016841326,0.00000561509,0.00019740034,0.00004278558,0.0011418867],"genre_scores_gemma":[0.9996542,0.000026686295,0.00009811475,0.000010216491,0.0000048252614,0.0000023027026,0.00011665447,0.000006274636,0.000080830316],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9997621,0.000105720246,0.000012387555,0.000049140664,0.000025954054,0.000044683853],"domain_scores_gemma":[0.99936265,0.0003381749,0.000075097676,0.000090223075,0.000067078276,0.00006680307],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005261417,0.0003953505,0.00031065848,0.00025682346,0.0002797868,0.0008038465,0.00029595007,0.00047553735,0.0013798992],"category_scores_gemma":[0.0018160865,0.00029123036,0.00068086834,0.00025329736,0.00040457386,0.00040053145,0.0007616302,0.0005494153,0.000085781234],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006061637,0.000149378,0.16290201,0.000079170575,0.00048140684,0.0002538017,0.00013702703,0.7879165,0.04018738,0.0020949836,0.00048103856,0.0047112303],"study_design_scores_gemma":[0.00016726958,0.0005743083,0.3389004,0.000023567824,0.00017781946,0.000107684704,0.00022699141,0.6473589,0.009958757,0.0014103099,0.0010127843,0.00008120953],"about_ca_topic_score_codex":0.011376984,"about_ca_topic_score_gemma":0.004735005,"teacher_disagreement_score":0.011376984,"about_ca_system_score_codex":0.00040618435,"about_ca_system_score_gemma":0.000261031,"threshold_uncertainty_score":0.022621512},"labels":[],"label_agreement":null},{"id":"W3200861724","doi":"10.1029/2021gl094762","title":"Isolated Cavities Dominate Greenland Ice Sheet Dynamic Response to Lake Drainage","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":31,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Sherbrooke","funders":"National Science Foundation","keywords":"Greenland ice sheet; Geology; Meltwater; Ice sheet; Glacier; Drainage; Dewatering; Geomorphology; Channelized; Hydrology (agriculture); Geotechnical engineering; Ecology","score_opus":0.025499635278443848,"score_gpt":0.2854040277574456,"score_spread":0.25990439247900177,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3200861724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994591,0.000026672054,0.000024138973,0.000010941661,5.8982914e-7,0.0000012719757,0.000076503384,0.000004588842,0.00039620663],"genre_scores_gemma":[0.99978095,0.000010647488,0.000011612794,0.000005821242,0.0000011593203,8.434331e-7,0.00006532568,0.0000016515492,0.000121894605],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999436,0.000003886486,0.0000022628071,0.000018903767,0.000005747278,0.000025550295],"domain_scores_gemma":[0.99982375,0.000026941625,0.000050908493,0.000012520203,0.000027972113,0.000057912166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009130417,0.00017529371,0.00021424003,0.0005619512,0.00021323249,0.00056894857,0.00013767209,0.00016640413,0.0021852446],"category_scores_gemma":[0.00031735294,0.000097841556,0.00012014953,0.0003094023,0.00035203868,0.00029017607,0.00043869184,0.000114760885,0.00017964082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027289783,0.000039214046,0.9218226,0.000033972774,0.000068271715,0.00025155756,0.0006726058,0.002224315,0.06267198,0.00028017117,0.00056398666,0.011098425],"study_design_scores_gemma":[0.0000015824177,0.000009043752,0.9987318,0.000001886499,0.000003589296,0.000011142628,0.00012677067,0.00073057716,0.00022047649,0.000032831686,0.00012852765,0.0000017040417],"about_ca_topic_score_codex":0.017810978,"about_ca_topic_score_gemma":0.04342444,"teacher_disagreement_score":0.017810978,"about_ca_system_score_codex":0.00053945725,"about_ca_system_score_gemma":0.00023749462,"threshold_uncertainty_score":0.035414577},"labels":[],"label_agreement":null},{"id":"W3201254245","doi":"10.1029/2021gl094777","title":"Role of Mixed‐Layer Instabilities in the Seasonal Evolution of Eddy Kinetic Energy Spectra in a Global Submesoscale Permitting Simulation","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Geostrophic wind; Enstrophy; Kinetic energy; Spectral line; Mixed layer; Power law; Turbulence; Physics; Flattening; Atmospheric sciences; Turbulence kinetic energy; Scaling; Climatology; Geology; Mechanics; Meteorology; Classical mechanics; Vorticity; Vortex","score_opus":0.016320623946222405,"score_gpt":0.26000219680932,"score_spread":0.2436815728630976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201254245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971744,0.000026585945,0.00097114453,0.00009300378,0.0000101647465,0.000011061754,0.0002203299,0.00009450568,0.0013988075],"genre_scores_gemma":[0.99917823,0.000012444598,0.00053573644,0.00001634762,0.0000018652759,0.000006604866,0.000120956596,0.000020290765,0.00010742826],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989486,0.000040745188,0.0000069071066,0.000018291255,0.000015190891,0.000024003308],"domain_scores_gemma":[0.99948514,0.00025327964,0.000059595634,0.000046196215,0.00005714593,0.000098563105],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057324854,0.00059449894,0.00041527973,0.0004042421,0.0004910223,0.00086218375,0.00050933,0.0007523599,0.0008830678],"category_scores_gemma":[0.001665166,0.00029147536,0.00052610185,0.00038803057,0.0004727404,0.0004566072,0.00047564774,0.0005234505,0.00007431992],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002849634,0.00020352288,0.049129974,0.000030266758,0.00010688837,0.00025504225,0.00007922586,0.93807465,0.0075305747,0.0010333059,0.00043141504,0.0028401352],"study_design_scores_gemma":[0.000037708123,0.00005363332,0.010425955,0.0000048632246,0.000017912083,0.000012166488,0.000037663056,0.9881741,0.0009023363,0.00016581277,0.00015449748,0.000013344151],"about_ca_topic_score_codex":0.027038885,"about_ca_topic_score_gemma":0.015663655,"teacher_disagreement_score":0.027038885,"about_ca_system_score_codex":0.0005486944,"about_ca_system_score_gemma":0.0007211555,"threshold_uncertainty_score":0.053762972},"labels":[],"label_agreement":null},{"id":"W3201526697","doi":"10.1029/2021gl094543","title":"Preservation and Destruction of Holocene Marine Terraces: The Effects of Episodic Versus Gradual Relative Sea Level Change","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Marsden Fund","keywords":"Holocene; Terrace (agriculture); Geology; Shore; Peninsula; Sea level; River terraces; Physical geography; Cliff; Oceanography; Period (music); Weathering; Paleontology; Geomorphology; Fluvial; Archaeology; Geography","score_opus":0.09902241022491431,"score_gpt":0.312363892327652,"score_spread":0.21334148210273768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201526697","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989574,0.000039227467,0.00032852244,0.000051697712,0.0000026760388,0.0000041382764,0.00011184674,0.0000099730505,0.00049452274],"genre_scores_gemma":[0.99970776,0.00002432818,0.00010755749,0.0000075796006,8.222029e-7,0.0000028663155,0.00006613318,0.0000029363232,0.00008009972],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998233,0.000056945548,0.000010530512,0.00004977795,0.000018011384,0.000041599764],"domain_scores_gemma":[0.9994935,0.00022241716,0.00009135629,0.00005166516,0.000039119226,0.000101946214],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068607304,0.00025557086,0.00027102255,0.00026260663,0.00032985825,0.0010417828,0.0005896169,0.0004878836,0.0019234163],"category_scores_gemma":[0.0018754606,0.0002329772,0.0006668793,0.00029008422,0.0007766825,0.00048981275,0.00041134216,0.00034000786,0.00011182549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050446973,0.00016547764,0.49785018,0.00007919921,0.00042178776,0.0003483642,0.00013831609,0.48172367,0.0102128945,0.0012257097,0.00043759926,0.0068923417],"study_design_scores_gemma":[0.00009705112,0.00041274366,0.4496992,0.000015670383,0.00012846116,0.00011094076,0.00046932042,0.54617876,0.0016249734,0.00067189033,0.0005604917,0.000030494106],"about_ca_topic_score_codex":0.056359418,"about_ca_topic_score_gemma":0.046858363,"teacher_disagreement_score":0.056359418,"about_ca_system_score_codex":0.0010326048,"about_ca_system_score_gemma":0.0005413443,"threshold_uncertainty_score":0.11206275},"labels":[],"label_agreement":null},{"id":"W3201655326","doi":"10.1029/2021gl094737","title":"Deep Learning‐Based Super‐Resolution Climate Simulator‐Emulator Framework for Urban Heat Studies","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; McGill University","funders":"","keywords":"Consistency (knowledge bases); Computer science; Climate model; Deep learning; Simulation; Artificial intelligence; Climate change","score_opus":0.04950995980503612,"score_gpt":0.3467903981514692,"score_spread":0.2972804383464331,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201655326","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.046813056,0.00017496373,0.94524235,0.00048036146,0.00007677996,0.000069153015,0.0005180145,0.0024206056,0.00420475],"genre_scores_gemma":[0.81812084,0.00015742071,0.17715237,0.00024082899,0.000045639,0.00019867718,0.0009883621,0.00038683446,0.0027090136],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983513,0.00006398059,0.0000061754236,0.00002591163,0.000045917746,0.000022890017],"domain_scores_gemma":[0.9996668,0.00015902033,0.000025784764,0.000037357873,0.000077228506,0.00003387805],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006950214,0.0005883362,0.00043804932,0.0002789954,0.0002033655,0.00059003936,0.0015621774,0.0007784231,0.0028562855],"category_scores_gemma":[0.0019659924,0.00032962405,0.000526315,0.00024883932,0.00044298422,0.00076663535,0.0010380059,0.0013387067,0.00042565627],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000012971517,0.000010114278,0.00030767242,0.000007920011,0.0000097507955,0.000013548528,0.0000057328098,0.9945529,0.00035291072,0.0020552694,0.0002670228,0.0024041568],"study_design_scores_gemma":[0.000001723603,0.0000022277911,0.000019846186,7.542117e-7,5.150262e-7,0.0000015214398,9.054918e-7,0.9992962,0.00010313986,0.0004491151,0.00012307937,8.756722e-7],"about_ca_topic_score_codex":0.012548754,"about_ca_topic_score_gemma":0.011400499,"teacher_disagreement_score":0.012548754,"about_ca_system_score_codex":0.0007800689,"about_ca_system_score_gemma":0.0012465287,"threshold_uncertainty_score":0.024951398},"labels":[],"label_agreement":null},{"id":"W3201861369","doi":"10.1029/2021gl095495","title":"Can Earth's Magnetotail Plasma Sheet Produce a Source of Relativistic Electrons for the Radiation Belts?","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Plasma sheet; Physics; Van Allen radiation belt; Magnetosphere; Electron; Plasma; Solar wind; Atomic physics; Radiation; Van Allen Probes; Geophysics; Computational physics; Astrophysics; Nuclear physics","score_opus":0.013419907928434992,"score_gpt":0.2673189942939234,"score_spread":0.2538990863654884,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201861369","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996378,0.0003699141,0.000523224,0.00027774385,0.00001287663,0.0000035545295,0.000046371944,0.00003291178,0.002355493],"genre_scores_gemma":[0.99941945,0.00011132572,0.00017716929,0.000039708073,0.000015848573,0.0000013149463,0.00003533488,0.0000031540314,0.00019666833],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999567,0.000006733405,0.0000021237322,0.000011239077,0.0000074332324,0.000015736829],"domain_scores_gemma":[0.9998049,0.000050334984,0.00007246668,0.000024923898,0.000017737397,0.000029600938],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025104362,0.00014272633,0.00019440602,0.00030603848,0.00021714675,0.0007298239,0.00025605012,0.00032885786,0.00092548446],"category_scores_gemma":[0.0005906941,0.00010191001,0.00013153102,0.0002197601,0.0004268873,0.00056589535,0.00037735488,0.00015211903,0.00020798817],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010402154,0.00007249675,0.67763823,0.00018486759,0.00012258264,0.0019360742,0.0014973053,0.0010604188,0.25759158,0.009397869,0.0008618842,0.0485965],"study_design_scores_gemma":[0.00004827667,0.00020055001,0.97820765,0.000017983504,0.00003137055,0.00058980915,0.0010843435,0.0013140661,0.010009295,0.0041766334,0.004303409,0.000016500262],"about_ca_topic_score_codex":0.0006223346,"about_ca_topic_score_gemma":0.00070959504,"teacher_disagreement_score":0.00092548446,"about_ca_system_score_codex":0.00020456054,"about_ca_system_score_gemma":0.00006613445,"threshold_uncertainty_score":0.003096044},"labels":[],"label_agreement":null},{"id":"W3201942753","doi":"10.1029/2021gl094621","title":"Hygroscopic Seeding Effects of Giant Aerosol Particles Simulated by the Lagrangian‐Particle‐Based Direct Numerical Simulation","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Particle Dynamics in Fluid Flows","field":"Engineering","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Center for Atmospheric Research","keywords":"Seeding; Supersaturation; Aerosol; Adiabatic process; Cloud condensation nuclei; Turbulence; Mechanics; Coalescence (physics); Particle (ecology); Condensation; Entrainment (biomusicology); Computer simulation; Atmospheric sciences; Meteorology; Physics; Thermodynamics; Geology","score_opus":0.021585894424540255,"score_gpt":0.3022488388067472,"score_spread":0.28066294438220696,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3201942753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9902547,0.00006335706,0.005757875,0.00006302045,0.000018275587,0.000035156536,0.000092108676,0.00011563929,0.003599909],"genre_scores_gemma":[0.9982439,0.000021324327,0.0014407681,0.000014856598,0.0000035012138,0.000012885817,0.000038355316,0.000010918034,0.00021343319],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999905,0.000026620766,0.0000041676167,0.0000134032625,0.000024471912,0.000026420808],"domain_scores_gemma":[0.99947244,0.0002922197,0.000060004575,0.000038471837,0.000066527224,0.000070396265],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028660995,0.00039546003,0.0004598386,0.00030223542,0.0003071624,0.0004239149,0.00065518596,0.0005759971,0.0008598443],"category_scores_gemma":[0.001194705,0.00020684036,0.0003910284,0.00020060131,0.0005104854,0.00028962275,0.00042107466,0.0003664718,0.000069822076],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001190285,0.00010118035,0.0045643523,0.00003441779,0.00003012076,0.00014896935,0.00005125087,0.9797595,0.012296392,0.0010896395,0.000118640004,0.0016864879],"study_design_scores_gemma":[0.000020803442,0.000024905868,0.00059813604,0.0000016121888,0.000003494644,0.0000067438223,0.0000056620174,0.9978124,0.001406869,0.000063155785,0.00005272462,0.0000034563488],"about_ca_topic_score_codex":0.016893756,"about_ca_topic_score_gemma":0.005921897,"teacher_disagreement_score":0.016893756,"about_ca_system_score_codex":0.0007658099,"about_ca_system_score_gemma":0.0007505514,"threshold_uncertainty_score":0.033590853},"labels":[],"label_agreement":null},{"id":"W3202239357","doi":"10.1029/2021gl095779","title":"A Tale of Two Radiation Belts: The Energy‐Dependence of Self‐Limiting Electron Space Radiation","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Canadian Space Agency; Public Works and Government Services Canada; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Electron; Physics; Van Allen radiation belt; Storm; Limiting; Flux (metallurgy); Geomagnetic storm; Radiation; Computational physics; Atmospheric sciences; Energy flux; Atomic physics; Magnetic field; Magnetosphere; Nuclear physics; Meteorology; Solar wind; Astronomy; Quantum mechanics; Materials science","score_opus":0.0086590605846114,"score_gpt":0.2734128040535465,"score_spread":0.2647537434689351,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202239357","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956643,0.00018938312,0.0017771024,0.000065192966,0.0000034385662,0.000004868125,0.00003661799,0.000038323647,0.0022206802],"genre_scores_gemma":[0.999521,0.000028008004,0.0002290915,0.0000118544385,0.0000028552581,0.0000029790615,0.000030065372,0.0000059291783,0.0001682353],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999379,0.000011345781,0.000002714183,0.000018824465,0.000011130802,0.000018132909],"domain_scores_gemma":[0.9996277,0.00011797646,0.00011881324,0.000049260223,0.000044931618,0.000041261384],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002565403,0.000093163435,0.00020935744,0.00062578166,0.00024271994,0.0006095753,0.00031249394,0.0002978082,0.0010580341],"category_scores_gemma":[0.0009217093,0.00014518666,0.00020749852,0.00024372849,0.0006025439,0.00058547547,0.00039221617,0.0002127731,0.00014027131],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016274519,0.00027161083,0.47430557,0.00015694434,0.00016343404,0.0011229754,0.0019532766,0.026090655,0.39864698,0.044377103,0.0016431453,0.049640954],"study_design_scores_gemma":[0.000057401,0.00030948114,0.8927316,0.00002548483,0.000034753895,0.0007679495,0.0008974592,0.068096735,0.019285183,0.014781714,0.0029603124,0.000051888448],"about_ca_topic_score_codex":0.0011665246,"about_ca_topic_score_gemma":0.00050339027,"teacher_disagreement_score":0.0011665246,"about_ca_system_score_codex":0.0003222401,"about_ca_system_score_gemma":0.00008234233,"threshold_uncertainty_score":0.0035395026},"labels":[],"label_agreement":null},{"id":"W3202362314","doi":"10.1029/2021gl095347","title":"Seismic Formation Fluid Pressure Observations Reveal High Anisotropy of Oceanic Crust","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ocean Networks Canada Society; Geological Survey of Canada","funders":"National Science Foundation","keywords":"Geology; Crust; Oceanic crust; Anisotropy; Geophysics; Igneous rock; Compressibility; Hydrothermal circulation; Lithosphere; Petrology; Seismology; Borehole; Seismic anisotropy; Mantle (geology); Geochemistry; Subduction; Tectonics; Geotechnical engineering; Mechanics","score_opus":0.05097705315586851,"score_gpt":0.27558613945293314,"score_spread":0.22460908629706464,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3202362314","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993599,0.000026512513,0.0001434983,0.000006776289,6.2816093e-7,6.7598063e-7,0.000060555412,0.00001213189,0.00038927616],"genre_scores_gemma":[0.9998092,0.000009397188,0.00007064088,0.0000013030756,7.6762035e-7,3.742189e-7,0.000051968633,0.0000012932358,0.000055079116],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994457,0.0000033846525,0.0000034603402,0.000016219486,0.000017546381,0.000014808361],"domain_scores_gemma":[0.99986064,0.000018012743,0.00005813088,0.0000150554215,0.000021919488,0.00002614458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009416664,0.00016712237,0.00010174629,0.0005122452,0.00016421599,0.00022715032,0.000116197894,0.00015307484,0.00064646784],"category_scores_gemma":[0.00031413743,0.0001650889,0.00008996036,0.00027597393,0.0003722716,0.0001632429,0.0003270856,0.00018870873,0.00012163707],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001620337,0.00002068086,0.41758624,0.00002965565,0.000028490636,0.0003250689,0.00083018903,0.00075910037,0.5706664,0.00015535472,0.0000814971,0.009355267],"study_design_scores_gemma":[0.0000022380705,0.000017848399,0.98642576,0.0000015563411,0.0000039232036,0.00012584886,0.0000765888,0.0007091347,0.01241127,0.000025318845,0.00019658392,0.000003986924],"about_ca_topic_score_codex":0.0041915164,"about_ca_topic_score_gemma":0.0044742892,"teacher_disagreement_score":0.0041915164,"about_ca_system_score_codex":0.00024471065,"about_ca_system_score_gemma":0.00009152716,"threshold_uncertainty_score":0.008334219},"labels":[],"label_agreement":null},{"id":"W3203102895","doi":"10.1029/2021gl094285","title":"Variability in Timing and Transport of Pleistocene Meltwater Recharge to Regional Aquifers","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Global Water Futures; Natural Sciences and Engineering Research Council of Canada","keywords":"Groundwater recharge; Meltwater; Geology; Structural basin; Aquifer; Depression-focused recharge; Pleistocene; Glacial period; Paleontology; Geomorphology; Groundwater; Hydrology (agriculture)","score_opus":0.06470638645214805,"score_gpt":0.3125639702881317,"score_spread":0.24785758383598366,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203102895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994636,0.000030137218,0.000035769415,0.000011423437,5.053064e-7,7.597123e-7,0.00019845393,0.0000040302352,0.00025527255],"genre_scores_gemma":[0.9995968,0.000024459145,0.000027156528,0.0000021093456,4.6212608e-7,6.880367e-7,0.00017456549,0.0000011453186,0.00017264168],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999405,0.0000067917,0.0000040265745,0.000019794748,0.00001297305,0.000015871208],"domain_scores_gemma":[0.9996501,0.000057756948,0.00008826112,0.000023631448,0.00013301712,0.000047153426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014348105,0.000074619034,0.000108404056,0.0007985537,0.0002546954,0.00046277425,0.00015445687,0.00010654748,0.0008980574],"category_scores_gemma":[0.0007103426,0.00009877185,0.00011310747,0.00076410413,0.00028781398,0.0001783871,0.00030852482,0.00011701861,0.00008649948],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054200715,0.000004375067,0.99399996,0.0000058307833,0.000034880664,0.000030476102,0.0003725838,0.00047198104,0.0019489978,0.000072858005,0.00011394524,0.002889925],"study_design_scores_gemma":[5.5474624e-7,0.0000019139045,0.9994199,0.0000014485566,0.0000019931904,0.0000057020834,0.00009315092,0.00020974313,0.00013064958,0.0000071608056,0.00012665238,0.0000010702481],"about_ca_topic_score_codex":0.47496265,"about_ca_topic_score_gemma":0.67138827,"teacher_disagreement_score":0.47496265,"about_ca_system_score_codex":0.0013841676,"about_ca_system_score_gemma":0.0008427041,"threshold_uncertainty_score":0.94439614},"labels":[],"label_agreement":null},{"id":"W3203637025","doi":"10.1029/2021gl095376","title":"Reevaluation of Total‐Column Ozone Trends and of the Effective Radiative Forcing of Ozone‐Depleting Substances","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Institute of Water and Atmospheric Research","keywords":"Ozone; Environmental science; Forcing (mathematics); Northern Hemisphere; Atmospheric sciences; Climatology; Radiative forcing; Ozone depletion; Ozone layer; Southern Hemisphere; Meteorology; Geology; Aerosol; Geography","score_opus":0.024084821900638792,"score_gpt":0.29151411479362477,"score_spread":0.267429292892986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203637025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649423,0.000053925134,0.0022697323,0.000039233728,0.0000037809932,0.0000033088577,0.00030733368,0.000041134557,0.0007873683],"genre_scores_gemma":[0.9977175,0.000029158682,0.0018643654,0.0000058992136,0.000002167531,0.0000023944997,0.00022928148,0.000009331584,0.00013996153],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988604,0.000036457244,0.0000057371235,0.000020401005,0.000037759037,0.000013591516],"domain_scores_gemma":[0.99941206,0.00023848175,0.00007745323,0.00009096503,0.00015445749,0.000026660933],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007558189,0.00020254152,0.00021375809,0.00038982285,0.00014113977,0.0004658796,0.00044255902,0.00019790095,0.0006930217],"category_scores_gemma":[0.0017626808,0.00011527714,0.00037809106,0.00050996983,0.00011419162,0.0003825597,0.00022043478,0.00032675805,0.000109387525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009301226,0.00018311881,0.5070171,0.00018775585,0.0006552124,0.0002762118,0.00024757764,0.3798238,0.033551868,0.0017726553,0.00071449357,0.074640065],"study_design_scores_gemma":[0.00004878088,0.00030992157,0.42656013,0.000023938275,0.00025379768,0.000108992404,0.00022443527,0.5463169,0.02357114,0.00045612166,0.0020977946,0.000027959179],"about_ca_topic_score_codex":0.03196456,"about_ca_topic_score_gemma":0.020634325,"teacher_disagreement_score":0.03196456,"about_ca_system_score_codex":0.00050982914,"about_ca_system_score_gemma":0.00033109265,"threshold_uncertainty_score":0.06355703},"labels":[],"label_agreement":null},{"id":"W3203923787","doi":"10.1029/2021gl094040","title":"Decadal to Centennial Timescale Mantle Viscosity Inferred From Modern Crustal Uplift Rates in Greenland","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Science Mission Directorate; Jet Propulsion Laboratory","keywords":"Geology; Centennial; Mantle (geology); Geophysics; History","score_opus":0.029953414179204708,"score_gpt":0.2945204347962906,"score_spread":0.26456702061708587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3203923787","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990202,0.000085566666,0.00017409715,0.00003466754,0.000001181008,8.083747e-7,0.00027733916,0.000010221274,0.00039590086],"genre_scores_gemma":[0.9996462,0.00002840388,0.00009188826,0.0000047110157,8.5809023e-7,4.9288855e-7,0.00017030827,0.000002103736,0.00005501313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999579,0.0000070877495,0.0000032382104,0.000014137475,0.0000052963783,0.000012363495],"domain_scores_gemma":[0.99980587,0.000036817535,0.000067160916,0.000027373833,0.00003236488,0.000030385003],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036063595,0.00016901674,0.00012348521,0.0012454399,0.00017919739,0.00048534683,0.00019988477,0.0001839448,0.0005793858],"category_scores_gemma":[0.0005525182,0.00011666475,0.00019296058,0.0006862754,0.0003123185,0.00049763237,0.00045617847,0.000180313,0.00009187563],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011797278,0.000023232633,0.9649886,0.000025681673,0.00012912367,0.0001835235,0.0005812713,0.008839842,0.01016367,0.0006645818,0.00024400554,0.014038544],"study_design_scores_gemma":[0.0000019253441,0.0000051076304,0.9961588,0.000004535751,0.000010012735,0.000014125569,0.000058392277,0.0031019538,0.00027200067,0.0001293625,0.0002405024,0.0000033285307],"about_ca_topic_score_codex":0.050332192,"about_ca_topic_score_gemma":0.07808501,"teacher_disagreement_score":0.050332192,"about_ca_system_score_codex":0.0010168232,"about_ca_system_score_gemma":0.00023222029,"threshold_uncertainty_score":0.10007846},"labels":[],"label_agreement":null},{"id":"W3204572865","doi":"10.1029/2021gl095882","title":"An Observational Constraint on Aviation‐Induced Cirrus From the COVID‐19‐Induced Flight Disruption","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Advanced Aircraft Design and Technologies","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Cirrus; Aviation; Environmental science; Radiative forcing; Climatology; Atmospheric sciences; Meteorology; Radiative transfer; Coronavirus disease 2019 (COVID-19); Satellite; Aeronautics; Geography; Physics; Aerospace engineering; Aerosol; Engineering; Geology; Medicine","score_opus":0.15602217845571906,"score_gpt":0.37374135924038704,"score_spread":0.21771918078466798,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204572865","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98195064,0.00044290014,0.002956176,0.00056513626,0.00006223421,0.000011096844,0.0038420174,0.000045633413,0.010124125],"genre_scores_gemma":[0.9973707,0.00008727773,0.0002802805,0.00008849681,0.000029633702,0.000005516611,0.0020069198,0.000011833155,0.000119430195],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995883,0.00008562128,0.000028249422,0.0001502464,0.0000635561,0.00008405856],"domain_scores_gemma":[0.99751353,0.0008214705,0.00078742503,0.0004093047,0.00028471305,0.0001835322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00078140106,0.0002614178,0.00022559546,0.00032652012,0.0005239482,0.0009453123,0.0003496297,0.00033866242,0.0024209965],"category_scores_gemma":[0.0035185285,0.000116550225,0.00031262357,0.0005318147,0.00051136635,0.0005672816,0.0006348757,0.0005632476,0.0002859688],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017104336,0.000057993682,0.9732607,0.00009281551,0.00016024012,0.00016036852,0.00023888073,0.004760938,0.0077738566,0.0030368252,0.0024722128,0.007814068],"study_design_scores_gemma":[0.000007317446,0.000018310362,0.9901833,0.000031784566,0.000038904214,0.0000713611,0.00018293093,0.0050892155,0.00077748013,0.0007757356,0.0028122703,0.00001142964],"about_ca_topic_score_codex":0.030227166,"about_ca_topic_score_gemma":0.03561966,"teacher_disagreement_score":0.030227166,"about_ca_system_score_codex":0.00039214361,"about_ca_system_score_gemma":0.0006092431,"threshold_uncertainty_score":0.060102403},"labels":[],"label_agreement":null},{"id":"W3204905838","doi":"10.1029/2021gl094572","title":"Mechanisms of Dune Growth and Decay in Rivers","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; BC Hydro (Canada)","funders":"Mitacs","keywords":"Geology; Hydrograph; Kinematics; Bedform; Flow (mathematics); Geomorphology; Sediment transport; Flux (metallurgy); Paleontology; Sediment; Mechanics; Physics; Ecology; Surface runoff","score_opus":0.01692711868769134,"score_gpt":0.26912926537339005,"score_spread":0.25220214668569874,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3204905838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99237823,0.0013053679,0.004596808,0.00008445423,0.0000061417127,0.000008639787,0.00006995202,0.00011248045,0.0014379699],"genre_scores_gemma":[0.99901736,0.00020322287,0.00043418116,0.000006260069,0.000002905353,0.0000048596985,0.00002423628,0.0000035431506,0.00030349937],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998417,0.000025960479,0.000013478089,0.000039421462,0.00002826526,0.000051170744],"domain_scores_gemma":[0.99943966,0.00014244266,0.00016034821,0.000047274105,0.00009838338,0.000111793655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039880894,0.00018254005,0.00028345684,0.00095208926,0.0003450196,0.0009890844,0.00028732567,0.00033646298,0.0006107818],"category_scores_gemma":[0.00071111077,0.00021119555,0.00021933769,0.00027117608,0.000545476,0.00048309052,0.00047744182,0.0002450485,0.00010463513],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009903008,0.00016858937,0.29008356,0.0005025527,0.00019077116,0.0015207384,0.0016385254,0.019633517,0.5579178,0.016539088,0.000884905,0.109929666],"study_design_scores_gemma":[0.000052593536,0.0004049211,0.8350441,0.00009398281,0.00008298511,0.0015130494,0.0016109722,0.09367661,0.052325618,0.01012049,0.0049700383,0.000104645915],"about_ca_topic_score_codex":0.00173993,"about_ca_topic_score_gemma":0.0011880508,"teacher_disagreement_score":0.00173993,"about_ca_system_score_codex":0.00048152189,"about_ca_system_score_gemma":0.00014017503,"threshold_uncertainty_score":0.0034936666},"labels":[],"label_agreement":null},{"id":"W3206564585","doi":"10.1029/2021gl094407","title":"Forecasting the Indian Ocean Dipole With Deep Learning Techniques","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":50,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"National Natural Science Foundation of China","keywords":"Convolutional neural network; Predictability; Deep learning; Computer science; Artificial intelligence; Anomaly (physics); Indian Ocean Dipole; Machine learning; Climatology; Sea surface temperature; Geology; Mathematics; Statistics","score_opus":0.023266788366429442,"score_gpt":0.2515311713689399,"score_spread":0.22826438300251042,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3206564585","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8959043,0.00036877274,0.09783651,0.0006624427,0.00009136021,0.000020262296,0.0004743972,0.000651887,0.003990125],"genre_scores_gemma":[0.9961098,0.00004357586,0.0033320514,0.000015641253,0.000010411255,0.0000036448441,0.00012555899,0.000005962066,0.0003532568],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993813,0.000012253007,0.0000042051006,0.000016168511,0.000013700004,0.00001555495],"domain_scores_gemma":[0.9997446,0.00010190504,0.00005072632,0.000016171953,0.00006878322,0.000017736058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029053484,0.00036999345,0.00022694965,0.00044509876,0.00012363496,0.0004066853,0.00028891503,0.00021630117,0.00057347177],"category_scores_gemma":[0.00094851194,0.00019288425,0.00029796443,0.0004283091,0.00017843643,0.00041507295,0.00031468298,0.00044262208,0.0000980836],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038325572,0.000027116035,0.014227387,0.000012706897,0.000025296484,0.000037523514,0.000008944061,0.9633001,0.0013100228,0.0005658716,0.00040411734,0.02004249],"study_design_scores_gemma":[9.1032746e-7,0.000002489714,0.0008800751,6.7544454e-7,0.0000013076426,9.038085e-7,0.0000019021189,0.9987425,0.0001768107,0.00015272635,0.000038698105,9.985184e-7],"about_ca_topic_score_codex":0.031099847,"about_ca_topic_score_gemma":0.020608876,"teacher_disagreement_score":0.031099847,"about_ca_system_score_codex":0.00072438037,"about_ca_system_score_gemma":0.00060262886,"threshold_uncertainty_score":0.061837673},"labels":[],"label_agreement":null},{"id":"W3207058704","doi":"10.1029/2021gl095699","title":"Tropical Cyclone Winds and Inflow Angle Asymmetry From SAR Imagery","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Tropical cyclone; Synthetic aperture radar; Inflow; Geology; Wind speed; Remote sensing; Eye; RADIUS; Radiometer; Cyclone (programming language); Meteorology; Maximum sustained wind; Microwave radiometer; Asymmetry; Environmental science; Geodesy; Wind direction; Climatology; Physics; Wind gradient","score_opus":0.026723674193257788,"score_gpt":0.27849538036607413,"score_spread":0.25177170617281636,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3207058704","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9820259,0.000042054005,0.016005842,0.000028457605,0.000007797034,0.000012018699,0.00035944756,0.00009324102,0.001425145],"genre_scores_gemma":[0.9982408,0.000029653756,0.0013518669,0.0000027675776,0.000002897441,0.0000029510736,0.00020712786,0.000005679529,0.00015625381],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999584,0.000008631905,0.00000331149,0.0000131176985,0.000010312,0.0000061786473],"domain_scores_gemma":[0.9998921,0.00002885654,0.000029997645,0.000016120162,0.000023479315,0.000009413754],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015175523,0.00031793074,0.00011800536,0.00034401388,0.000078217025,0.00034791237,0.00010335402,0.00011151934,0.00046465197],"category_scores_gemma":[0.00044248666,0.00013347599,0.0002158644,0.00022622828,0.00011933132,0.00025894854,0.00012207573,0.00012919387,0.00010115337],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018041117,0.000055907378,0.17304642,0.000037934096,0.00008011953,0.00017434846,0.000050287978,0.7636811,0.029660305,0.0011900389,0.0006169441,0.031226093],"study_design_scores_gemma":[0.0000076780025,0.000017778762,0.061417915,0.000004117785,0.000009529682,0.00004291992,0.000015154674,0.93663806,0.0014760094,0.00019318746,0.00017185333,0.000005782316],"about_ca_topic_score_codex":0.006393281,"about_ca_topic_score_gemma":0.0051140958,"teacher_disagreement_score":0.006393281,"about_ca_system_score_codex":0.00017120109,"about_ca_system_score_gemma":0.00016973964,"threshold_uncertainty_score":0.012712121},"labels":[],"label_agreement":null},{"id":"W3207317893","doi":"10.1029/2021gl093746","title":"Sweeping Effects Modify Taylor’s Frozen Turbulence Hypothesis for Scalars in the Roughness Sublayer","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Advection; Turbulence; Anemometer; Mechanics; Turbulence kinetic energy; Physics; Kinetic energy; Meteorology; Optics; Classical mechanics; Thermodynamics","score_opus":0.030069014061447623,"score_gpt":0.2788553469868748,"score_spread":0.24878633292542718,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3207317893","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96757674,0.00009871723,0.030483257,0.00008587226,0.000027907798,0.000014351598,0.000033505396,0.00007595696,0.0016037148],"genre_scores_gemma":[0.9991242,0.000016631006,0.00071096735,0.000007472514,0.000004654032,0.0000022302347,0.000010602741,0.0000034949528,0.00011984343],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998318,0.000016363276,0.000008087625,0.000051361745,0.000035591627,0.000056711473],"domain_scores_gemma":[0.99948114,0.00017505606,0.00009828824,0.00009340224,0.00009144512,0.00006069042],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037975202,0.00023387343,0.00024589454,0.00035495491,0.0002727375,0.00065199303,0.0005456177,0.00025771582,0.0005196899],"category_scores_gemma":[0.0011342701,0.00020789776,0.00030921295,0.00011625375,0.0010762454,0.000838674,0.0003973523,0.00035418032,0.00006313942],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013159444,0.0002691988,0.11150503,0.00015361627,0.00014247591,0.0031097515,0.001120006,0.1492822,0.5933682,0.084341146,0.0013089016,0.054083563],"study_design_scores_gemma":[0.000060863436,0.00041910974,0.12737519,0.000020193103,0.00003757961,0.00044872685,0.00047929768,0.8151929,0.033856723,0.021305718,0.00070862396,0.00009514132],"about_ca_topic_score_codex":0.0029052028,"about_ca_topic_score_gemma":0.0011014239,"teacher_disagreement_score":0.0029052028,"about_ca_system_score_codex":0.0003342808,"about_ca_system_score_gemma":0.00020209572,"threshold_uncertainty_score":0.005776584},"labels":[],"label_agreement":null},{"id":"W3208143668","doi":"10.1029/2021gl095909","title":"Contribution of Recycled Moisture to Precipitation: A Modified D‐Excess‐Based Model","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Youth Innovation Promotion Association; National Natural Science Foundation of China","keywords":"Precipitation; Transpiration; Evapotranspiration; Environmental science; Water vapor; Moisture; Atmospheric sciences; Climatology; Water cycle; Meteorology; Geology; Chemistry; Geography; Ecology","score_opus":0.0503888327702654,"score_gpt":0.3320954382859072,"score_spread":0.2817066055156418,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3208143668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8324288,0.0005618302,0.15084608,0.0006709733,0.00015956639,0.00008287192,0.001785312,0.00077794085,0.0126865655],"genre_scores_gemma":[0.9938366,0.00008875771,0.0041013393,0.000040543997,0.00001803587,0.000037778223,0.00026679385,0.0000366426,0.0015735134],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998983,0.000026682275,0.0000066499515,0.000037291342,0.000013337786,0.000017697437],"domain_scores_gemma":[0.9998049,0.00008198187,0.000021783566,0.00002183613,0.000047468646,0.000022020133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024926008,0.00053625007,0.00056958915,0.0004149337,0.00037581462,0.0007768565,0.0013866487,0.00093924336,0.0011508699],"category_scores_gemma":[0.000596679,0.00031364337,0.00069386134,0.0004847567,0.00038573286,0.0006837532,0.0005579293,0.000608071,0.0001539838],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002399576,0.000014344726,0.0014761629,0.000011018335,0.000020123034,0.00003360753,0.000006912697,0.9952962,0.0009363232,0.0005721602,0.00013252471,0.0014766712],"study_design_scores_gemma":[0.0000051541792,0.0000030329113,0.00024458024,8.152888e-7,0.000004182118,0.000002419337,0.0000012768164,0.99945515,0.00010010184,0.000105565996,0.00007502431,0.000002657525],"about_ca_topic_score_codex":0.03350982,"about_ca_topic_score_gemma":0.014421756,"teacher_disagreement_score":0.03350982,"about_ca_system_score_codex":0.00074268656,"about_ca_system_score_gemma":0.0009098268,"threshold_uncertainty_score":0.06662953},"labels":[],"label_agreement":null},{"id":"W3209244424","doi":"10.1029/2021gl095074","title":"From Seismic Quiescence to Surged Activity After Decades of Wastewater Disposal: A Case Study in Central‐West Alberta, Canada","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geoscience BC; University of Victoria; Geological Survey of Canada","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Devonian; Reef; Seismology; Hydraulic fracturing; Aquifer; Structural basin; Sedimentary rock; Sedimentary basin; Geochemistry; Geomorphology; Geotechnical engineering; Oceanography; Groundwater","score_opus":0.025502378531678215,"score_gpt":0.2771036802901066,"score_spread":0.25160130175842843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3209244424","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9945398,0.0003926438,0.00016648066,0.00049755134,0.000010137214,0.000047769114,0.0006139174,0.000012469176,0.0037191382],"genre_scores_gemma":[0.99681085,0.0003759645,0.00021457173,0.00013475957,0.00000613342,0.00000863082,0.0002989022,0.0000053850135,0.0021446955],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99954236,0.00003293667,0.000015420892,0.000044345998,0.00013607665,0.00022893542],"domain_scores_gemma":[0.9991185,0.000072049974,0.00009635111,0.00002028249,0.00038364567,0.00030912642],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032716047,0.00044301507,0.0002927696,0.0019261405,0.004621735,0.0013693783,0.0012794378,0.0009560306,0.0017488712],"category_scores_gemma":[0.00076162117,0.00028819923,0.00025857898,0.0037300347,0.0011826832,0.00026162874,0.0009334352,0.0007156501,0.00015873472],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034105405,0.00034723425,0.90805674,0.00019394222,0.000119169905,0.018875923,0.022247754,0.0018678873,0.0035117408,0.00082794734,0.004492022,0.03911864],"study_design_scores_gemma":[0.000020481353,0.00009108135,0.91542023,0.00009648811,0.000060966686,0.0015533286,0.0750317,0.0014895516,0.00044488013,0.00014616211,0.005592031,0.00005297499],"about_ca_topic_score_codex":0.9949274,"about_ca_topic_score_gemma":0.9985667,"teacher_disagreement_score":0.033939384,"about_ca_system_score_codex":0.033939384,"about_ca_system_score_gemma":0.034343503,"threshold_uncertainty_score":0.2462486},"labels":[],"label_agreement":null},{"id":"W3210995728","doi":"10.1029/2021gl096644","title":"Geoscientists, Who Have Documented the Rapid and Accelerating Climate Crisis for Decades, Are Now Pleading for Immediate Collective Action","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; University of Victoria","funders":"","keywords":"Pleading; Portfolio; Action (physics); Political science; Climate science; Key (lock); Climate change; Economics; Finance; Computer science; Geology; Law; Physics","score_opus":0.04004589373319127,"score_gpt":0.32074310763807695,"score_spread":0.28069721390488567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3210995728","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0007946457,0.011488765,0.0013451787,0.634175,0.3044655,0.000032657106,0.00021549457,0.00044721697,0.047035422],"genre_scores_gemma":[0.021494625,0.043904077,0.007835916,0.35099107,0.32602265,0.00008263907,0.0006926583,0.0011500949,0.24782617],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.99475926,0.0007408637,0.00036890974,0.00050700374,0.0030266135,0.000597356],"domain_scores_gemma":[0.94053614,0.014013384,0.0041566817,0.003728329,0.017309938,0.020255547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.010161726,0.0012013689,0.0010964522,0.003597173,0.0039005615,0.017934266,0.0015938962,0.010833027,0.06823856],"category_scores_gemma":[0.03270927,0.0006457077,0.00071674417,0.003798396,0.004519048,0.01321654,0.00648621,0.012644984,0.03884236],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000017206212,0.000016538503,0.00040719978,0.0001453863,0.000006874158,0.000102750884,0.00018250509,0.000042901374,0.00037601741,0.004276735,0.9641698,0.030256085],"study_design_scores_gemma":[0.000005431109,0.00000899509,0.00039347305,0.00008144607,0.000003830906,0.000056332938,0.0007015616,0.000031667492,0.0000775527,0.0042071887,0.99442333,0.000009256918],"about_ca_topic_score_codex":0.0016514097,"about_ca_topic_score_gemma":0.007726982,"teacher_disagreement_score":0.06823856,"about_ca_system_score_codex":0.001663662,"about_ca_system_score_gemma":0.0070781643,"threshold_uncertainty_score":0.22828072},"labels":[],"label_agreement":null},{"id":"W3211114642","doi":"10.1029/2021gl095432","title":"Space Weather Observations With InSight","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Institut de Physique du Globe de Paris; Centre National de la Recherche Scientifique; Eidgenössische Technische Hochschule Zürich; Centre National d’Etudes Spatiales; Branco Weiss Fellowship – Society in Science; Max-Planck-Gesellschaft; UK Space Agency; National Aeronautics and Space Administration","keywords":"Coronal mass ejection; Solar wind; Space weather; Mars Exploration Program; Physics; Magnetometer; Planet; Magnetic cloud; Interplanetary magnetic field; Magnetic field; Geophysics; Mercury's magnetic field; Astrobiology; Solar System; Astronomy; Atmospheric sciences","score_opus":0.060772764120792015,"score_gpt":0.29187331248744997,"score_spread":0.23110054836665794,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211114642","genre_codex":"dataset","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.16301808,0.0008538323,0.0040559755,0.000972695,0.0007131104,0.0003817234,0.6494199,0.0058108456,0.17477389],"genre_scores_gemma":[0.47343215,0.0007284601,0.01219227,0.00053097395,0.00047484375,0.00028252846,0.48067006,0.00055091846,0.031137852],"study_design_codex":"not_applicable","study_design_gemma":"observational","domain_scores_codex":[0.99963284,0.000028990073,0.00003559537,0.00009629449,0.0001458944,0.00006041981],"domain_scores_gemma":[0.99869746,0.00006782723,0.0004099089,0.0002088178,0.00042323914,0.00019283651],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000300321,0.00058224454,0.0002602894,0.0018352247,0.00027649247,0.0009386843,0.00034667656,0.00027690455,0.023962716],"category_scores_gemma":[0.0010560921,0.00015629605,0.00023356726,0.0025328756,0.000116677205,0.0006112721,0.00094184576,0.00063086214,0.008124359],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001023249,0.0002223905,0.3446426,0.0007207195,0.00024312446,0.0005238375,0.00064643455,0.0028064793,0.013520528,0.0031962588,0.4776647,0.15478966],"study_design_scores_gemma":[0.00012776817,0.00010248501,0.49018228,0.00019368039,0.000073318486,0.00019696789,0.00034206104,0.004135051,0.0035602814,0.0010171914,0.5000155,0.00005340972],"about_ca_topic_score_codex":0.0072695566,"about_ca_topic_score_gemma":0.01072809,"teacher_disagreement_score":0.023962716,"about_ca_system_score_codex":0.0002805122,"about_ca_system_score_gemma":0.00043646563,"threshold_uncertainty_score":0.08016324},"labels":[],"label_agreement":null},{"id":"W3211520754","doi":"10.1029/2021gl096488","title":"Multipoint Measurement of Fine‐Structured EMIC Waves by Arase, Van Allen Probe A, and Ground Stations","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Japan Society for the Promotion of Science","keywords":"Van Allen Probes; Physics; Emic and etic; Magnetosphere; Geophysics; Computational physics; Magnetometer; Magnetic field; Van Allen radiation belt","score_opus":0.020688654805723114,"score_gpt":0.27790779276320343,"score_spread":0.2572191379574803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3211520754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830186,0.000023180139,0.0008461922,0.000008254499,0.0000028192367,0.000006859882,0.00019026021,0.000018342036,0.0006021623],"genre_scores_gemma":[0.9984415,0.000015044022,0.0011209918,0.0000034149602,0.0000049823657,0.000007907949,0.00022335729,0.0000027490266,0.00017999782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986947,0.000023370707,0.000005370287,0.000041982865,0.00003867086,0.000021143052],"domain_scores_gemma":[0.999589,0.000106142164,0.00011129715,0.000044935365,0.000093847615,0.000054708944],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022606742,0.0002033335,0.00016134274,0.0011888132,0.00015722384,0.00018939534,0.00025435758,0.00022449384,0.00057596026],"category_scores_gemma":[0.0006100627,0.00014214774,0.000120928366,0.00061915343,0.00011002944,0.00028622575,0.0003917595,0.0002489855,0.00012185428],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039901223,0.00009778905,0.8400813,0.000028017486,0.00008328078,0.00017193165,0.00039621856,0.002848754,0.12703426,0.00016986087,0.00021821843,0.02847146],"study_design_scores_gemma":[0.000023826917,0.00017460904,0.9807469,0.000005576635,0.000032282675,0.00009791,0.00021223338,0.0086711785,0.00924669,0.000059955048,0.000716341,0.0000124488815],"about_ca_topic_score_codex":0.0026493792,"about_ca_topic_score_gemma":0.007284927,"teacher_disagreement_score":0.0026493792,"about_ca_system_score_codex":0.0001344504,"about_ca_system_score_gemma":0.000088793844,"threshold_uncertainty_score":0.005267918},"labels":[],"label_agreement":null},{"id":"W3212018187","doi":"10.1029/2021gl096049","title":"Significant Increase of Continental Freeboard During the Early Paleoproterozoic: Insights From Metasediment‐Derived Granites","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"National Natural Science Foundation of China","keywords":"Zircon; Continental crust; Geology; Geochemistry; Archean; Earth science; Supercontinent; Continental margin; Igneous rock; Lithosphere; Crust; Craton; Tectonics; Paleontology","score_opus":0.019766964272928313,"score_gpt":0.2293080662828535,"score_spread":0.20954110200992518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3212018187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988738,0.00027324943,0.000096164214,0.000021552973,0.0000019302033,0.0000019409927,0.00017798171,0.000005753533,0.00054779084],"genre_scores_gemma":[0.999099,0.00032516872,0.0001224565,0.000012104318,0.0000034446775,0.0000015423794,0.00019136441,0.0000058746396,0.00023904018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994946,0.000004117533,0.0000041708163,0.000020581561,0.00000694187,0.000014779017],"domain_scores_gemma":[0.99989974,0.000012015036,0.0000361987,0.000008911268,0.000021541271,0.000021500347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027381146,0.0003897476,0.00021800997,0.0013661315,0.00040293593,0.00091115496,0.0001704744,0.00023132862,0.0013708834],"category_scores_gemma":[0.00021428602,0.00018474634,0.00028338714,0.00091908587,0.0004502278,0.0003075061,0.0006338469,0.00022709403,0.00018031542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039930965,0.000023781166,0.8835255,0.00009468778,0.00018429216,0.00065752835,0.0013303806,0.00054909923,0.09989458,0.00027497712,0.0000918395,0.012974089],"study_design_scores_gemma":[0.0000048953816,0.000019063018,0.9972595,0.0000074732343,0.000025389896,0.00012268442,0.0002869176,0.00014524325,0.001468964,0.000041657237,0.0006144739,0.000003787413],"about_ca_topic_score_codex":0.01121211,"about_ca_topic_score_gemma":0.021792624,"teacher_disagreement_score":0.01121211,"about_ca_system_score_codex":0.00037606293,"about_ca_system_score_gemma":0.00026668957,"threshold_uncertainty_score":0.022293687},"labels":[],"label_agreement":null},{"id":"W3213260462","doi":"10.1029/2021gl095824","title":"Predictable Pattern of Precipitation Over Asian Summer Monsoon Regions","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"","keywords":"Predictability; Climatology; Precipitation; Monsoon; Environmental science; Indian Ocean Dipole; Empirical orthogonal functions; Bay; El Niño Southern Oscillation; East Asian Monsoon; Geology; Meteorology; Geography; Oceanography","score_opus":0.05379225129893989,"score_gpt":0.3233034434421485,"score_spread":0.2695111921432086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213260462","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984395,0.000044868495,0.0002722436,0.000034563367,0.0000041980297,0.0000018512534,0.0004540943,0.000018293045,0.0007304696],"genre_scores_gemma":[0.99946016,0.00001773967,0.000057791374,0.0000031791408,0.0000045774386,0.0000013143178,0.00038235067,0.0000020367506,0.00007087097],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999938,0.000009815267,0.000005320822,0.000017555556,0.000014290817,0.000014991495],"domain_scores_gemma":[0.99971706,0.00003898926,0.00008559892,0.000022427772,0.00008836364,0.000047590027],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020354183,0.00016965,0.0001163641,0.0004009903,0.00019082444,0.00030612922,0.0001373583,0.00008137541,0.00070282485],"category_scores_gemma":[0.00037820713,0.00007860052,0.00015031752,0.00047902938,0.00014063345,0.00013835997,0.0002051154,0.00014784002,0.00014290526],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036229685,0.000053299893,0.9509522,0.00006582104,0.00021306418,0.00042288276,0.00041481288,0.0111417435,0.015580085,0.000815388,0.0017427629,0.018235644],"study_design_scores_gemma":[0.000008301848,0.00003010605,0.9897753,0.000004203113,0.000020768251,0.000070897244,0.00014698252,0.008109935,0.0010847733,0.00017706933,0.00056443544,0.0000071754403],"about_ca_topic_score_codex":0.008223177,"about_ca_topic_score_gemma":0.009463798,"teacher_disagreement_score":0.008223177,"about_ca_system_score_codex":0.00022302583,"about_ca_system_score_gemma":0.00029231358,"threshold_uncertainty_score":0.016350627},"labels":[],"label_agreement":null},{"id":"W3213295897","doi":"10.1029/2021gl094985","title":"Future Changes in Snowpack, Snowmelt, and Runoff Potential Extremes Over North America","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":58,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Environmental Security Technology Certification Program; National Aeronautics and Space Administration; U.S. Department of Energy; U.S. Department of Defense","keywords":"Snowmelt; Snowpack; Snow; Precipitation; Environmental science; Climatology; Surface runoff; Water year; Climate change; Climate model; Physical geography; Drainage basin; Meteorology; Geography; Geology; Oceanography; Ecology","score_opus":0.0275658461702815,"score_gpt":0.26594246886802414,"score_spread":0.23837662269774265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3213295897","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966948,0.0002159119,0.00029644856,0.00040842113,0.000008388988,0.000002663376,0.001307425,0.000033021952,0.0010328199],"genre_scores_gemma":[0.9990175,0.00010853334,0.00019750815,0.000049222075,0.0000037491293,0.0000036435943,0.00049240363,0.000002917253,0.00012457823],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994576,0.000013355168,0.0000020642394,0.00001617647,0.000009708636,0.000012989806],"domain_scores_gemma":[0.99985385,0.000021548747,0.000031281503,0.000010090654,0.000055787754,0.000027471626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024456534,0.0001549444,0.00013139415,0.00022354082,0.00023893938,0.00041445554,0.00018274451,0.00025668074,0.0007696937],"category_scores_gemma":[0.00042370643,0.00008416602,0.00019745406,0.00047295087,0.0001354983,0.00036621073,0.00021775339,0.00020378671,0.00006651255],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000105296895,0.00005199125,0.93428755,0.000048493494,0.00018903926,0.00015828373,0.00022235641,0.041853506,0.0041096257,0.0005840546,0.0031422288,0.01524767],"study_design_scores_gemma":[0.000009123356,0.000017821589,0.9722797,0.000013758093,0.000031280848,0.00002920326,0.0002905277,0.0238889,0.00048557355,0.00035946927,0.0025846427,0.000009817016],"about_ca_topic_score_codex":0.15339546,"about_ca_topic_score_gemma":0.20614639,"teacher_disagreement_score":0.8466045,"about_ca_system_score_codex":0.0011377134,"about_ca_system_score_gemma":0.0006097317,"threshold_uncertainty_score":0.30500525},"labels":[],"label_agreement":null},{"id":"W3214968703","doi":"10.1029/2021gl095933","title":"Conjugate Observation of Magnetospheric Chorus Propagating to the Ionosphere by Ducting","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Nuclear Safety and Security Commission; Sight Research UK; European Space Agency; National Aeronautics and Space Administration; Natural Environment Research Council; University of Calgary; National Science Foundation","keywords":"Physics; Ionosphere; Chorus; Atmospheric duct; Magnetosphere; Geophysics; Electron precipitation; Van Allen radiation belt; Wave propagation; Computational physics; Whistler; Electron; Atmospheric sciences; Atmosphere (unit); Plasma; Meteorology; Optics","score_opus":0.021884918531066066,"score_gpt":0.2830307922184457,"score_spread":0.2611458736873796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3214968703","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920448,0.00008493811,0.0038567476,0.00005261589,0.000015633263,0.000010218584,0.00023399954,0.00015720043,0.0035438451],"genre_scores_gemma":[0.9986455,0.000025729572,0.00096788834,0.000009315781,0.0000039662473,0.000004019473,0.00009120099,0.000014323355,0.00023823271],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.999933,0.0000119555525,0.0000028290533,0.000021167194,0.000018274864,0.000012790402],"domain_scores_gemma":[0.9997155,0.000034750545,0.000089559726,0.000060665992,0.00005589282,0.00004363977],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013154722,0.0002037294,0.00013417989,0.000325016,0.0002564694,0.00044287698,0.00017370704,0.00017155192,0.0010880277],"category_scores_gemma":[0.00047752028,0.00015318245,0.00013484508,0.0002732703,0.00039312805,0.00028930508,0.0005673828,0.00044629173,0.0001591521],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074862706,0.00012475024,0.39706978,0.00015154365,0.00021942532,0.00072190433,0.00169194,0.0063381377,0.54952735,0.0034303472,0.0017430003,0.03823318],"study_design_scores_gemma":[0.000078198864,0.0004033177,0.79850644,0.000032518154,0.0001046131,0.00058356463,0.0007032792,0.033015024,0.1576619,0.0016704672,0.007160317,0.00008035834],"about_ca_topic_score_codex":0.002023296,"about_ca_topic_score_gemma":0.0020365054,"teacher_disagreement_score":0.002023296,"about_ca_system_score_codex":0.00016027997,"about_ca_system_score_gemma":0.00018235878,"threshold_uncertainty_score":0.0040230155},"labels":[],"label_agreement":null},{"id":"W3215686510","doi":"10.1029/2021gl095500","title":"Improving the Estimation of Human Climate Influence by Selecting Appropriate Forcing Simulations","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Pacific Institute for Climate Solutions; University of Victoria","funders":"","keywords":"Coupled model intercomparison project; Overfitting; Environmental science; Forcing (mathematics); Radiative forcing; Climatology; Climate model; Aerosol; Regression; Greenhouse gas; Meteorology; Climate change; Atmospheric sciences; Computer science; Statistics; Mathematics; Geography; Machine learning; Ecology","score_opus":0.030844431707337194,"score_gpt":0.3248455120739726,"score_spread":0.2940010803666354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3215686510","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90213853,0.00018088499,0.09075693,0.00046494158,0.00004049901,0.000041271443,0.0013701973,0.0006378396,0.004368947],"genre_scores_gemma":[0.9894421,0.000025904445,0.010041674,0.000029184543,0.0000077163895,0.000017503004,0.000294104,0.00002746051,0.00011437919],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996356,0.00023809531,0.000014928304,0.00005847171,0.000018647928,0.000034403718],"domain_scores_gemma":[0.99837863,0.0010804536,0.00012422459,0.00021886677,0.0001358174,0.00006203023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011929219,0.00039378274,0.00036044038,0.0004890812,0.00024348484,0.000523574,0.00055432296,0.0004894004,0.0015627705],"category_scores_gemma":[0.006609404,0.00030627375,0.00047049104,0.00046971222,0.00025405586,0.00055403274,0.0004183462,0.00042307333,0.00019010947],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006614599,0.000030318663,0.019343495,0.00002139941,0.0000570274,0.000025660394,0.000018016846,0.97121394,0.0006686281,0.000699376,0.00033308988,0.007522941],"study_design_scores_gemma":[0.000031891013,0.000016480231,0.006176154,0.000013117049,0.000015606265,0.000008489252,0.000019092931,0.9914145,0.0009019069,0.0009905921,0.00039948625,0.000012655331],"about_ca_topic_score_codex":0.015443065,"about_ca_topic_score_gemma":0.011188815,"teacher_disagreement_score":0.015443065,"about_ca_system_score_codex":0.00040269745,"about_ca_system_score_gemma":0.0008395447,"threshold_uncertainty_score":0.030706346},"labels":[],"label_agreement":null},{"id":"W3216068753","doi":"10.1029/2021gl096532","title":"Origin of Frequency‐Doubling and Shoulder‐Like Magnetic Pulsations in ULF Waves","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Physics; Monochromatic color; Geophysics; Amplitude; Magnetic field; Spacecraft; Azimuth; Computational physics; Optics; Astronomy","score_opus":0.027310085221978884,"score_gpt":0.31144028492854636,"score_spread":0.2841301997065675,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3216068753","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936598,0.00016035835,0.004286927,0.000055330915,0.000014804205,0.0000082126535,0.000072175164,0.00009127024,0.0016510837],"genre_scores_gemma":[0.9994199,0.000016021228,0.0004346414,0.0000048260863,0.0000050357626,0.0000027707858,0.000035232068,0.0000035795,0.00007808753],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997365,0.0000028651837,0.000001333306,0.000008161697,0.0000050369717,0.000008965888],"domain_scores_gemma":[0.99987674,0.00002830542,0.000041437466,0.00002094764,0.00001248206,0.000020046029],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007735436,0.00015521796,0.00016297384,0.0004970019,0.00018616239,0.000256738,0.00028404174,0.00034870347,0.00084656005],"category_scores_gemma":[0.00030338703,0.000117400064,0.00014039548,0.00027395898,0.00022192471,0.00018450798,0.00025818014,0.00025713388,0.00012798561],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009940708,0.00017508681,0.21695511,0.00024148585,0.00011774756,0.0032179265,0.0011002842,0.012840969,0.6613796,0.012069498,0.002026263,0.08888197],"study_design_scores_gemma":[0.0000762705,0.00029687048,0.82598597,0.000041521766,0.00005089644,0.0015661083,0.00028487746,0.11596577,0.045599714,0.0062278262,0.0038462954,0.000057965084],"about_ca_topic_score_codex":0.00065544894,"about_ca_topic_score_gemma":0.00035333566,"teacher_disagreement_score":0.00084656005,"about_ca_system_score_codex":0.0001711402,"about_ca_system_score_gemma":0.00003832555,"threshold_uncertainty_score":0.002832055},"labels":[],"label_agreement":null},{"id":"W3217421959","doi":"10.1029/2021gl095898","title":"Stratospheric Temperature and Ozone Anomalies Associated With the 2020 Australian New Year Fires","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Goddard Space Flight Center; Nuclear Safety and Security Commission; National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Polar vortex; Stratosphere; Ozone depletion; Atmospheric sciences; Polar; Southern Hemisphere; Ozone; Environmental science; Aerosol; Northern Hemisphere; Climatology; Middle latitudes; Breakup; Geology; Meteorology; Physics","score_opus":0.020201776557599065,"score_gpt":0.2537732392087844,"score_spread":0.23357146265118536,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W3217421959","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986565,0.00005816606,0.00002940937,0.000039088925,0.0000053381445,0.0000031974162,0.00041984118,0.000002280562,0.00078605406],"genre_scores_gemma":[0.99873465,0.000059272177,0.000042476746,0.000016853997,0.00000751068,0.0000047350295,0.0006398325,7.189286e-7,0.00049399846],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998528,0.000019209456,0.000009671196,0.00002733815,0.000053730633,0.00003724522],"domain_scores_gemma":[0.99956447,0.00003410102,0.0001668474,0.00002757687,0.00012920145,0.00007786069],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003455453,0.0001548602,0.00013764952,0.0007292548,0.0004090848,0.0004811055,0.00023017619,0.0003180344,0.0007798058],"category_scores_gemma":[0.0007109332,0.00012654696,0.00018723762,0.00060512795,0.00017684528,0.00025091678,0.0005047587,0.0002951515,0.00013053969],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000175954,0.00007164225,0.98657227,0.000034328692,0.000062498264,0.00015630535,0.0005642036,0.00066727534,0.004760911,0.0001120708,0.00078892766,0.006033714],"study_design_scores_gemma":[3.132632e-7,0.000007378322,0.9995461,0.000001659639,0.0000023018217,0.00001263416,0.000049338756,0.00013400042,0.00006557495,0.0000049328146,0.00017501737,7.884754e-7],"about_ca_topic_score_codex":0.080869064,"about_ca_topic_score_gemma":0.16856275,"teacher_disagreement_score":0.080869064,"about_ca_system_score_codex":0.0008642837,"about_ca_system_score_gemma":0.000289323,"threshold_uncertainty_score":0.16079676},"labels":[],"label_agreement":null},{"id":"W4200035836","doi":"10.1029/2021gl095908","title":"Iron‐Phosphorus Feedbacks Drive Multidecadal Oscillations in Baltic Sea Hypoxia","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Netherlands Earth System Science Centre; Ministerie van Onderwijs, Cultuur en Wetenschap; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Stockholms Universitet; Academy of Finland; H2020 European Research Council; Helsingin Yliopisto","keywords":"Hypoxia (environmental); Environmental science; Cycling; Brackish water; Phosphorus; Sedimentary rock; Climate change; Climatology; Oceanography; Sediment; Geology; Chemistry; Geomorphology; Salinity; Paleontology; Geography; Oxygen","score_opus":0.03042739166499127,"score_gpt":0.2973039122210417,"score_spread":0.26687652055605043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200035836","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989772,0.000042458058,0.0003573437,0.00010562968,0.000004877797,0.000002565498,0.00007710122,0.000026810541,0.00040603228],"genre_scores_gemma":[0.99976534,0.000022426268,0.00007601875,0.000010999351,0.0000018147987,0.0000027935678,0.00003955432,0.0000026213224,0.00007845922],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993026,0.000012838884,0.000007030849,0.00002582193,0.00000802883,0.000016012069],"domain_scores_gemma":[0.9998305,0.000036039328,0.00005350848,0.000015701085,0.000031823532,0.000032458618],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031246356,0.00018841961,0.000264775,0.0003250098,0.00037089805,0.000628915,0.00028363176,0.00045735255,0.0008739471],"category_scores_gemma":[0.00076327845,0.00027508603,0.00020136978,0.00023542072,0.00041433706,0.00046553422,0.0006559217,0.0002819217,0.00009862758],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035142453,0.00013937669,0.84199536,0.00008980412,0.0002969909,0.0007184487,0.0010937774,0.036857173,0.09823052,0.001793715,0.0011065216,0.017326955],"study_design_scores_gemma":[0.000021813174,0.00008172311,0.92997295,0.000009353998,0.000046219993,0.00006943394,0.00035440704,0.06549085,0.0016848354,0.0012761866,0.0009723884,0.00001986686],"about_ca_topic_score_codex":0.013860095,"about_ca_topic_score_gemma":0.017853562,"teacher_disagreement_score":0.013860095,"about_ca_system_score_codex":0.00061442977,"about_ca_system_score_gemma":0.00038075977,"threshold_uncertainty_score":0.027558863},"labels":[],"label_agreement":null},{"id":"W4200139025","doi":"10.1029/2021gl096437","title":"Nonlinear Enhancement of Radiative Absorption by Black Carbon in Response to Particle Mixing Structure","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":79,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada; Métis National Council","funders":"Natural Science Foundation of Zhejiang Province; National Natural Science Foundation of China","keywords":"Carbon black; Radiative transfer; Mixing (physics); Particle (ecology); Absorption (acoustics); Radiation; Materials science; Population; Carbon fibers; Molecular physics; Computational physics; Particle size; Physics; Optics; Chemistry; Composite material; Composite number; Quantum mechanics; Geology; Physical chemistry","score_opus":0.018249955341796867,"score_gpt":0.279334165134115,"score_spread":0.26108420979231817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200139025","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97053605,0.00018231907,0.02450626,0.000110550056,0.000027523753,0.000014019948,0.0001364101,0.00023534919,0.004251501],"genre_scores_gemma":[0.99823123,0.000044332453,0.0013710371,0.000010962497,0.0000025415059,0.0000033460365,0.000030686675,0.000013195959,0.0002927301],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994874,0.000007087583,0.0000011774747,0.000013046234,0.000017422297,0.000012572756],"domain_scores_gemma":[0.9998853,0.000050506715,0.000017560458,0.000010961265,0.000024698742,0.00001105048],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001414626,0.000297369,0.00010540665,0.00021222889,0.0001914167,0.00026385117,0.00026744764,0.0003246453,0.000877781],"category_scores_gemma":[0.00042195845,0.00014555288,0.0002640102,0.00015870445,0.00032359103,0.00029910402,0.00020476329,0.0002927509,0.00011839037],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000194954,0.00016105508,0.030946394,0.000106007996,0.00006232625,0.00033972578,0.00015522141,0.619716,0.32852694,0.0048722513,0.00066722225,0.014251857],"study_design_scores_gemma":[0.000004962961,0.000009747357,0.0044591897,0.0000017860867,0.0000031340878,0.000013955854,0.000007095026,0.9824347,0.01264973,0.00029402078,0.00011490447,0.0000067996075],"about_ca_topic_score_codex":0.009736522,"about_ca_topic_score_gemma":0.004405405,"teacher_disagreement_score":0.009736522,"about_ca_system_score_codex":0.0004632125,"about_ca_system_score_gemma":0.000330722,"threshold_uncertainty_score":0.019359648},"labels":[],"label_agreement":null},{"id":"W4200191074","doi":"10.1029/2021gl096583","title":"Unsteady Magnetopause Reconnection Under Quasi‐Steady Solar Wind Driving","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Air Force Research Laboratory; Air Force Office of Scientific Research; National Aeronautics and Space Administration; National Science Foundation","keywords":"Magnetopause; Magnetosheath; Physics; Magnetic reconnection; Solar wind; Geophysics; Magnetosphere; Amplitude; Electric field; Computational physics; Magnetic field","score_opus":0.02203525425322058,"score_gpt":0.2893230513509443,"score_spread":0.26728779709772377,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200191074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979596,0.000031929176,0.00061026466,0.000051311108,0.000009099952,0.000004061221,0.00006539624,0.00003360533,0.0012348642],"genre_scores_gemma":[0.9996623,0.00001766079,0.0001280105,0.0000068787094,0.000002084796,0.000002121421,0.000039733484,0.0000040205855,0.00013723441],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999523,0.000006677103,0.000002319749,0.000007552207,0.000009873956,0.000021279451],"domain_scores_gemma":[0.9998191,0.00005987616,0.000040654657,0.00001670728,0.000022387663,0.00004134587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012045479,0.00017814641,0.0002297239,0.00019285426,0.00025410068,0.0004319081,0.00026330331,0.00024909046,0.001217081],"category_scores_gemma":[0.00048840896,0.000106658066,0.00021700807,0.00018657181,0.00039322252,0.00033107845,0.00029931343,0.00020294226,0.00006949446],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005022429,0.00020081986,0.0273922,0.000067843735,0.00013223097,0.00088898995,0.00021972944,0.92974925,0.031206243,0.0031838515,0.0008933703,0.0055632046],"study_design_scores_gemma":[0.000046917747,0.00017472335,0.015105329,0.0000038638063,0.00001601422,0.0000555751,0.00015272203,0.98186076,0.0017307192,0.0005994005,0.00024167696,0.000012333126],"about_ca_topic_score_codex":0.010092935,"about_ca_topic_score_gemma":0.0070568956,"teacher_disagreement_score":0.010092935,"about_ca_system_score_codex":0.00042473496,"about_ca_system_score_gemma":0.00033129126,"threshold_uncertainty_score":0.020068407},"labels":[],"label_agreement":null},{"id":"W4200250447","doi":"10.1029/2021gl094036","title":"Coral Oxygen Isotopic Records Capture the 2015/2016 El Niño Event in the Central Equatorial Pacific","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coral and Marine Ecosystems Studies","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Georgia Institute of Technology; National Science Foundation","keywords":"Coral; Oceanography; Seawater; Sea surface temperature; Salinity; Temperature record; Geology; Isotopes of oxygen; δ18O; Climatology; Pacific ocean; Environmental science; Stable isotope ratio; Climate change","score_opus":0.024243356538313856,"score_gpt":0.29632620033637974,"score_spread":0.2720828437980659,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200250447","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819475,0.00003475335,0.000050928895,0.000017803355,0.0000039444994,0.000002879974,0.0005191922,0.00000500239,0.0011707348],"genre_scores_gemma":[0.99897647,0.000048550824,0.00012215352,0.00001097267,0.0000036961928,0.000004158933,0.0006098768,0.0000026062874,0.00022145995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.000005831243,0.000009239639,0.000024498459,0.000016115324,0.000017634506],"domain_scores_gemma":[0.99973506,0.0000144353835,0.00010899585,0.000028476874,0.00007235997,0.00004064159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019258285,0.00020003597,0.00012619545,0.00052890246,0.00035839394,0.00039567493,0.00018070456,0.00013459586,0.0007638089],"category_scores_gemma":[0.0004656938,0.000109047796,0.0001203743,0.0006466573,0.00016961328,0.00031848167,0.0006324596,0.0001494071,0.000100925885],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005035553,0.00001997528,0.9911411,0.000012150784,0.00003529259,0.0000310875,0.0001357393,0.00028046206,0.0033179661,0.000032738513,0.00022626379,0.0047167838],"study_design_scores_gemma":[0.000001769403,0.0000054608527,0.99896395,0.000003780761,0.000008447527,0.000013353079,0.0001492964,0.00021447812,0.00027525594,0.000010206049,0.00035231092,0.000001741579],"about_ca_topic_score_codex":0.029310733,"about_ca_topic_score_gemma":0.08493789,"teacher_disagreement_score":0.029310733,"about_ca_system_score_codex":0.00034968337,"about_ca_system_score_gemma":0.00036215014,"threshold_uncertainty_score":0.05828023},"labels":[],"label_agreement":null},{"id":"W4200454914","doi":"10.1029/2021gl093979","title":"Complex 3D Migration and Delayed Triggering of Hydraulic Fracturing‐Induced Seismicity: A Case Study Near Fox Creek, Alberta","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Induced seismicity; Geology; Hydrogeology; Hydraulic fracturing; Seismology; Poromechanics; Pore water pressure; Fault (geology); Natural hazard; Geotechnical engineering","score_opus":0.06524063724748795,"score_gpt":0.30958456258838823,"score_spread":0.24434392534090027,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200454914","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952897,0.00006763287,0.0008276301,0.00015301889,0.0000074302097,0.000037768066,0.0005033728,0.00005474518,0.003058707],"genre_scores_gemma":[0.997431,0.000055250926,0.0013863852,0.000013522414,0.0000022325614,0.0000059404874,0.00018918382,0.000006527386,0.0009100129],"study_design_codex":"observational","study_design_gemma":"case_report","domain_scores_codex":[0.9998919,0.00000873989,0.000004454203,0.0000156963,0.00004501783,0.00003425906],"domain_scores_gemma":[0.99985254,0.000035257875,0.000015535532,0.000013914014,0.00003857054,0.00004416133],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011145151,0.0003056903,0.00015372502,0.0008405533,0.0012568933,0.0009173803,0.00063025544,0.00063080864,0.0016862729],"category_scores_gemma":[0.00040161252,0.00017865775,0.00019401584,0.0012886573,0.00076478923,0.00019631401,0.0005147763,0.00034879107,0.00015014934],"study_design_candidate":"case_report","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006984505,0.0011003133,0.5846806,0.00033944388,0.0002023584,0.05186431,0.010447819,0.20411022,0.0444574,0.0039939797,0.0071395254,0.09096562],"study_design_scores_gemma":[0.00008055823,0.00016796791,0.7777948,0.00007159355,0.0000757683,0.0022566929,0.015290463,0.19107044,0.003948547,0.00094134075,0.008168007,0.00013380553],"about_ca_topic_score_codex":0.7497651,"about_ca_topic_score_gemma":0.92183673,"teacher_disagreement_score":0.2502349,"about_ca_system_score_codex":0.003143695,"about_ca_system_score_gemma":0.0030168104,"threshold_uncertainty_score":0.50341713},"labels":[],"label_agreement":null},{"id":"W4200493938","doi":"10.1029/2021gl096072","title":"3D Joint Inversion of Scanning Magnetic Microscopy Data","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mount Allison University","funders":"Norges Teknisk-Naturvitenskapelige Universitet","keywords":"Remanence; Natural remanent magnetization; Magnetization; Geology; Magnetometer; Magnetic anomaly; Rock magnetism; Mineralogy; Geophysics; Physics; Magnetic field","score_opus":0.08777300214363738,"score_gpt":0.34111151324456795,"score_spread":0.2533385111009306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200493938","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.2667834,0.000176888,0.7172241,0.00036309272,0.00013641902,0.00014911269,0.0028051923,0.00658579,0.005775979],"genre_scores_gemma":[0.70684916,0.00012751184,0.28722617,0.00009749132,0.000029466806,0.00013345297,0.003401263,0.0004948851,0.0016405684],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998091,0.000026073689,0.00001020668,0.000034451128,0.000086329084,0.000033876862],"domain_scores_gemma":[0.9994137,0.00017213235,0.00007190176,0.0001008615,0.00020849182,0.000032860808],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061332865,0.0007313769,0.0004326286,0.0015888747,0.00025173894,0.0011338827,0.0008011669,0.00066862174,0.0035401713],"category_scores_gemma":[0.0019272739,0.00046311627,0.00088705367,0.0009987268,0.00035017895,0.00062671,0.0007711492,0.0006521645,0.0010763495],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043114982,0.00025386584,0.01047873,0.00038451518,0.0002938297,0.0004817761,0.00032953467,0.5324557,0.20998664,0.005806651,0.005942297,0.23315527],"study_design_scores_gemma":[0.00001073652,0.000019473746,0.0017545762,0.0000057007474,0.000012733274,0.000056124867,0.00003840916,0.9807928,0.0138024315,0.0013194635,0.0021696137,0.000017884162],"about_ca_topic_score_codex":0.005348593,"about_ca_topic_score_gemma":0.0074416813,"teacher_disagreement_score":0.005348593,"about_ca_system_score_codex":0.00044263154,"about_ca_system_score_gemma":0.0011632583,"threshold_uncertainty_score":0.011843026},"labels":[],"label_agreement":null},{"id":"W4200522234","doi":"10.1029/2021gl093416","title":"Fluvial Organic Carbon Composition Regulated by Seasonal Variability in Lowland River Migration and Water Discharge","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Deutsche Forschungsgemeinschaft; Alexander von Humboldt-Stiftung","keywords":"Fluvial; Tributary; Overprinting; Biogeochemical cycle; Total organic carbon; Composition (language); Environmental science; Floodplain; Hydrology (agriculture); Biogeochemistry; Provenance; Channel (broadcasting); Oceanography; Geology; Environmental chemistry; Ecology; Geochemistry; Structural basin; Geomorphology; Geography; Chemistry","score_opus":0.009253429645552995,"score_gpt":0.22033683983871702,"score_spread":0.211083410193164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200522234","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999355,0.000023941642,0.00005846762,0.000013387512,0.0000011948033,0.0000013637888,0.00018214354,0.000003853045,0.00036063528],"genre_scores_gemma":[0.9995832,0.0000146106795,0.000038553015,0.000005432967,0.0000012388427,0.000002013888,0.00016783984,0.000002243002,0.00018491599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999341,0.000011669264,0.0000035447924,0.00002585273,0.000006853134,0.000018017416],"domain_scores_gemma":[0.9997317,0.000035561367,0.000111167596,0.000015333922,0.000056568388,0.000049606257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013343718,0.0000930355,0.00012388999,0.00031202505,0.00018966172,0.00042433187,0.000101945385,0.00010194626,0.0009892937],"category_scores_gemma":[0.0003730415,0.000083869025,0.00009716959,0.00031580552,0.0002052735,0.00014834909,0.00018309822,0.00009690116,0.00013363341],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008058218,0.00001778021,0.9892581,0.000008427678,0.000025317622,0.000038876093,0.00013003104,0.00018508405,0.0073565976,0.000039421102,0.00014203017,0.0027176822],"study_design_scores_gemma":[8.242747e-7,0.0000044990716,0.99965525,9.905191e-7,0.000001877493,0.0000054930138,0.00005509627,0.00014957861,0.00006407623,0.0000062501204,0.000055388868,6.975316e-7],"about_ca_topic_score_codex":0.027983919,"about_ca_topic_score_gemma":0.052498866,"teacher_disagreement_score":0.027983919,"about_ca_system_score_codex":0.00039026202,"about_ca_system_score_gemma":0.000254769,"threshold_uncertainty_score":0.05564207},"labels":[],"label_agreement":null},{"id":"W4200524423","doi":"10.1029/2021gl096244","title":"On the Limitations of Using Polarimetric Radar Sounding to Infer the Crystal Orientation Fabric of Ice Masses","year":2021,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Villum Fonden","keywords":"Geology; Depth sounding; Polarimetry; Glacier; Radar; Ice crystals; Orientation (vector space); Anisotropy; Geophysics; Geodesy; Geometry; Meteorology; Physics; Optics; Geomorphology; Computer science; Mathematics; Scattering","score_opus":0.15732434636240766,"score_gpt":0.3282659627422383,"score_spread":0.17094161637983063,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4200524423","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.34844974,0.0034739769,0.6331258,0.0033103744,0.0001845002,0.00010911485,0.0017683224,0.0012108597,0.008367323],"genre_scores_gemma":[0.9008587,0.0015258081,0.09553502,0.00038970218,0.00015409646,0.00008191419,0.00048772714,0.00011594509,0.0008510295],"study_design_codex":"design_other","study_design_gemma":"observational","domain_scores_codex":[0.9983511,0.0008441983,0.000085214175,0.0002422348,0.00042394781,0.00005337217],"domain_scores_gemma":[0.9830361,0.01148507,0.0007724404,0.0030924252,0.0014620544,0.0001519182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.007179373,0.0005170765,0.0004214807,0.0007893099,0.00035082735,0.0014739716,0.00093583873,0.00074318465,0.00085662596],"category_scores_gemma":[0.022062317,0.0003875657,0.0004019513,0.00078905874,0.00095376564,0.0018135726,0.0009077806,0.0007505779,0.0010186295],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006813577,0.00021068541,0.078625716,0.0008284246,0.00057014375,0.00024570877,0.0005769987,0.4000423,0.06719641,0.02001993,0.0041506127,0.42685172],"study_design_scores_gemma":[0.00004229897,0.00014222172,0.025113953,0.000173919,0.000086661414,0.0005256147,0.0002594469,0.9229109,0.016248126,0.02876308,0.0056376527,0.00009612159],"about_ca_topic_score_codex":0.0060984814,"about_ca_topic_score_gemma":0.004183221,"teacher_disagreement_score":0.007179373,"about_ca_system_score_codex":0.0003423737,"about_ca_system_score_gemma":0.0006176829,"threshold_uncertainty_score":0.037968636},"labels":[],"label_agreement":null},{"id":"W4205123983","doi":"10.1029/2021gl096346","title":"The Influence of Riparian Vegetation on the Sinuosity and Lateral Stability of Meandering Channels","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; University of British Columbia","funders":"National Natural Science Foundation of China","keywords":"Sinuosity; Meander (mathematics); Grassland; Riparian zone; Vegetation (pathology); Geology; Floodplain; Rainforest; Hydrology (agriculture); Riparian forest; Environmental science; Ecology; Geomorphology","score_opus":0.027646421829123594,"score_gpt":0.26910021815865187,"score_spread":0.2414537963295283,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205123983","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957865,0.00002981941,0.000047977774,0.000005114555,6.347832e-7,5.8640313e-7,0.00006571983,0.0000019069093,0.00026962097],"genre_scores_gemma":[0.99986553,0.000014148469,0.00002561385,0.0000018864984,0.0000010546953,4.7762376e-7,0.000045805384,0.0000010803216,0.000044318855],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998764,0.000042824922,0.000009037174,0.000029957548,0.000015501271,0.000026301868],"domain_scores_gemma":[0.9986745,0.00052368426,0.00036966655,0.00008064436,0.00014807016,0.00020342009],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026284682,0.00007409489,0.00009548874,0.00065554515,0.00019557285,0.00050343515,0.000114840586,0.00012130314,0.0013997749],"category_scores_gemma":[0.0011496986,0.00006906108,0.00013744635,0.00046602395,0.000343887,0.00021935398,0.0002753093,0.00009601539,0.00013498761],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042047584,0.00000488006,0.9963193,0.000005433073,0.000029812849,0.00004635135,0.00008756085,0.00021084031,0.0012185221,0.000031838503,0.000037610032,0.0019656846],"study_design_scores_gemma":[3.800392e-7,0.0000040994596,0.9996092,0.0000010569065,0.0000039760084,0.000017273645,0.00008133485,0.00019186261,0.00004131003,0.000012595412,0.000036067628,8.3365273e-7],"about_ca_topic_score_codex":0.0052291565,"about_ca_topic_score_gemma":0.01575421,"teacher_disagreement_score":0.0052291565,"about_ca_system_score_codex":0.00014039227,"about_ca_system_score_gemma":0.000131594,"threshold_uncertainty_score":0.010397434},"labels":[],"label_agreement":null},{"id":"W4205311639","doi":"10.1029/2021gl096501","title":"Retreat of Northern Hemisphere Marine‐Terminating Glaciers, 2000–2020","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":78,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"","keywords":"Surge; Glacier; Geology; Glacier morphology; Ice sheet; Ice stream; Northern Hemisphere; Physical geography; Ice calving; Greenland ice sheet; Oceanography; Ice caps; Cryosphere; Climatology; Sea ice; Geomorphology; Geography","score_opus":0.02740864317047976,"score_gpt":0.26660107296873486,"score_spread":0.2391924297982551,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205311639","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99428374,0.0005414249,0.00012721823,0.00012903087,0.000020589274,0.0000041259013,0.0027934946,0.000027854845,0.0020724586],"genre_scores_gemma":[0.99431497,0.00021120567,0.00013330346,0.000048034115,0.000013509796,0.000004270428,0.004518826,0.000006065324,0.0007498005],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986327,0.000010643685,0.000011945625,0.000038659593,0.00004148598,0.0000339968],"domain_scores_gemma":[0.9993111,0.000040724313,0.00026825094,0.00003495968,0.00023730566,0.00010765322],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056403864,0.00035311191,0.00014155085,0.0010687159,0.00023644355,0.00079282233,0.0002747712,0.0002867234,0.00092339265],"category_scores_gemma":[0.0012037967,0.00009932145,0.0002343842,0.0008894963,0.00025211892,0.0005904847,0.00041625358,0.00031928485,0.00030814647],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016218086,0.000025375404,0.98043174,0.00004287246,0.0000896416,0.00013890864,0.00027709742,0.0016611161,0.0014464787,0.0001399873,0.001883674,0.013700923],"study_design_scores_gemma":[0.0000028882123,0.000019338306,0.9966511,0.000013978962,0.000012331262,0.00008208147,0.00013216429,0.0006507753,0.00021345896,0.000026950987,0.0021912784,0.0000036160648],"about_ca_topic_score_codex":0.0658505,"about_ca_topic_score_gemma":0.08827449,"teacher_disagreement_score":0.0658505,"about_ca_system_score_codex":0.0010816122,"about_ca_system_score_gemma":0.0005831011,"threshold_uncertainty_score":0.13093442},"labels":[],"label_agreement":null},{"id":"W4205683175","doi":"10.1029/2021gl095579","title":"Using End‐Member Models to Estimate Seasonal Carbonate Chemistry and Acidification Sensitivity in Temperate Estuaries","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":24,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada; Simon Fraser University","funders":"Marine Environmental Observation Prediction and Response Network","keywords":"Alkalinity; Temperate climate; Carbonate; Total inorganic carbon; Productivity; Ocean acidification; Estuary; Environmental science; Carbon fibers; Calcium carbonate; Environmental chemistry; Oceanography; Chemistry; Carbon dioxide; Ecology; Geology; Seawater; Biology; Materials science","score_opus":0.0641331920956049,"score_gpt":0.32413910408400753,"score_spread":0.2600059119884026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205683175","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970548,0.000028743721,0.0019122382,0.000040608546,0.000006000217,0.0000055233804,0.00045392098,0.000084091356,0.00041417472],"genre_scores_gemma":[0.9984743,0.000012388565,0.0007660061,0.000014145581,0.0000025221252,0.0000071424815,0.0005937765,0.000010963368,0.00011878995],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99977726,0.0000643917,0.000021763362,0.00008240955,0.000019777688,0.000034354427],"domain_scores_gemma":[0.9989184,0.00044590683,0.00015116869,0.00017539553,0.00020257448,0.000106681466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012890238,0.0006303801,0.00037769065,0.00037896817,0.00041063127,0.0010311769,0.0008659431,0.0008553035,0.00056775595],"category_scores_gemma":[0.0021847882,0.0004396444,0.0010539708,0.00031486334,0.00030029152,0.0007143649,0.00081065646,0.00046784108,0.00012778683],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020491966,0.00009782432,0.28361654,0.000021701879,0.00038863043,0.00006465158,0.00007202246,0.71073496,0.0022429966,0.00023126714,0.00022624401,0.002098266],"study_design_scores_gemma":[0.00005506546,0.00007442417,0.102437556,0.0000102766535,0.00007056688,0.000022426973,0.000069665315,0.89522374,0.001315078,0.0003203159,0.00037038457,0.000030520237],"about_ca_topic_score_codex":0.06110694,"about_ca_topic_score_gemma":0.036270566,"teacher_disagreement_score":0.06110694,"about_ca_system_score_codex":0.0009381585,"about_ca_system_score_gemma":0.00060961256,"threshold_uncertainty_score":0.12150252},"labels":[],"label_agreement":null},{"id":"W4205776466","doi":"10.1029/2021gl095020","title":"Effects of Deep Circulation on CaCO<sub>3</sub> Dissolution and Accumulation in the Southwestern Atlantic Ocean","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Natural Science Foundation of China","keywords":"Thermohaline circulation; Oceanography; Geology; North Atlantic Deep Water; Seafloor spreading; Bottom water; Benthic zone; Deep sea; Carbonate; Ocean current; Circumpolar deep water; Water mass; Ocean chemistry; Oceanic basin; Shutdown of thermohaline circulation; Antarctic Bottom Water; Structural basin; Seawater; Paleontology; Chemistry","score_opus":0.026212330972625226,"score_gpt":0.27788430304868517,"score_spread":0.25167197207605996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205776466","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997445,0.000018793293,0.000017370248,0.00002062896,0.0000011652122,5.4543074e-7,0.00006617377,0.0000023475973,0.00012846082],"genre_scores_gemma":[0.99981266,0.0000204634,0.000021767331,0.000007886966,0.0000011643498,6.518131e-7,0.000065564425,0.0000011468384,0.00006870365],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999685,0.0000068716026,0.0000033096735,0.000007701601,0.0000046685273,0.000008967826],"domain_scores_gemma":[0.9998055,0.00004387276,0.000052409763,0.000017052222,0.000029534127,0.00005162951],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012141933,0.00015807888,0.00012770291,0.00019825961,0.0001769011,0.00026035367,0.000099656914,0.00015199954,0.00093111594],"category_scores_gemma":[0.0003686371,0.0001138892,0.00020398888,0.00018002113,0.0002191861,0.00018509652,0.0003559676,0.00016138892,0.00009026748],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051607424,0.000055713037,0.9338886,0.000035673143,0.0000714762,0.00017183521,0.00023780065,0.00302999,0.056470077,0.00015843341,0.00021217138,0.0051520835],"study_design_scores_gemma":[0.000007402992,0.000032429998,0.99665546,0.0000022612544,0.000010141704,0.000009471651,0.000082370796,0.0021925496,0.00085901323,0.00003017681,0.00011630742,0.0000024326534],"about_ca_topic_score_codex":0.0370741,"about_ca_topic_score_gemma":0.04035387,"teacher_disagreement_score":0.0370741,"about_ca_system_score_codex":0.0006685567,"about_ca_system_score_gemma":0.00029161712,"threshold_uncertainty_score":0.07371658},"labels":[],"label_agreement":null},{"id":"W4205812252","doi":"10.1029/2021gl096974","title":"Upper Plate Structure and Megathrust Properties in the Shumagin Gap Near the July 2020 M7.8 Simeonof Event","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Science Foundation","keywords":"Geology; Subduction; Seismology; Episodic tremor and slip; Slip (aerodynamics); Crust; Plate tectonics; Tectonics; Interplate earthquake; Convergent boundary; Induced seismicity; Geophysics; Oceanic crust","score_opus":0.03878019524748188,"score_gpt":0.26878755371604446,"score_spread":0.23000735846856257,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4205812252","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997352,0.000006846467,0.00006699458,0.000008844824,5.040366e-7,7.5384463e-7,0.000030542695,0.000004939633,0.00014550789],"genre_scores_gemma":[0.999819,0.000005887547,0.0000397815,0.0000018115587,5.6480167e-7,7.6430274e-7,0.000078478246,0.0000014702159,0.000052324718],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.000008520482,0.0000034887014,0.000015684604,0.0000071823524,0.000014749772],"domain_scores_gemma":[0.9998853,0.000018300014,0.00002573772,0.000012945566,0.000021870084,0.00003587588],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019573292,0.0002966266,0.0002945412,0.0004470812,0.0003405907,0.0006477624,0.00040359714,0.0006614209,0.0009739232],"category_scores_gemma":[0.00044792413,0.0002651451,0.00037729766,0.0002462648,0.00032924153,0.00034857105,0.00036920473,0.00019609867,0.00020724346],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020340054,0.0001293866,0.9109269,0.000023564822,0.000083998246,0.0002915488,0.00031275206,0.074798375,0.009292471,0.0004637002,0.00019604074,0.0032778839],"study_design_scores_gemma":[0.000017486944,0.000105689636,0.7364506,0.000010653273,0.000031860447,0.000071182156,0.000500979,0.261484,0.00093509245,0.0001934092,0.00018001333,0.00001911666],"about_ca_topic_score_codex":0.04411158,"about_ca_topic_score_gemma":0.041814525,"teacher_disagreement_score":0.04411158,"about_ca_system_score_codex":0.0007742274,"about_ca_system_score_gemma":0.00035252245,"threshold_uncertainty_score":0.087709665},"labels":[],"label_agreement":null},{"id":"W4206236386","doi":"10.1029/2021gl096842","title":"Urban Heat Islands Significantly Reduced by COVID‐19 Lockdown","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":67,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Megacity; Daytime; Urban heat island; Environmental science; Coronavirus disease 2019 (COVID-19); Climatology; Canopy; Atmospheric sciences; 2019-20 coronavirus outbreak; Severe acute respiratory syndrome coronavirus 2 (SARS-CoV-2); Urbanization; Meteorology; Geography; Geology; Medicine; Ecology","score_opus":0.028261373970156687,"score_gpt":0.2916992113745064,"score_spread":0.2634378374043497,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206236386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99739206,0.000085321946,0.00027204255,0.00007130581,0.00001296787,0.000010840363,0.00078052736,0.00003768131,0.0013372645],"genre_scores_gemma":[0.9989429,0.000030272997,0.00009484879,0.000023086313,0.0000051732695,0.000008321295,0.00062566454,0.000003735349,0.0002661506],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991786,0.000007379877,0.000004133053,0.000017484992,0.000012290503,0.000040835213],"domain_scores_gemma":[0.9998248,0.000010966289,0.000045541914,0.000015532494,0.000055121593,0.00004815477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000100421705,0.00019745744,0.00019092363,0.00028304098,0.00032798646,0.00039790702,0.00023323968,0.00017543048,0.0021211223],"category_scores_gemma":[0.00035510704,0.000066217064,0.00022281581,0.00042157708,0.00023044321,0.00024601835,0.00061368564,0.00025839685,0.00015911857],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042779272,0.0001135114,0.9327788,0.00011331963,0.00012599147,0.0004564663,0.00086123735,0.0028045475,0.019199122,0.00030518754,0.0033085316,0.03950554],"study_design_scores_gemma":[0.0000027148737,0.000033451863,0.9963805,0.000005429227,0.000014286727,0.000024025707,0.00055045105,0.0007598866,0.0009755448,0.000031411215,0.0012169455,0.000005446003],"about_ca_topic_score_codex":0.04777587,"about_ca_topic_score_gemma":0.061153125,"teacher_disagreement_score":0.04777587,"about_ca_system_score_codex":0.00060992,"about_ca_system_score_gemma":0.00047394264,"threshold_uncertainty_score":0.09499556},"labels":[],"label_agreement":null},{"id":"W4206377843","doi":"10.1029/2021gl095759","title":"Are Low‐Frequency Earthquake Moments Area‐ or Slip‐Limited? A Rock Record Examination","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Slip (aerodynamics); Seismology; Geology; Subduction; Moment magnitude scale; Fault plane; Fault (geology); Geometry; Tectonics; Physics; Mathematics","score_opus":0.06605891953492406,"score_gpt":0.28806635047954854,"score_spread":0.2220074309446245,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206377843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977708,0.000055679124,0.00026780882,0.000015317046,7.4229024e-7,0.0000044616527,0.00062069076,0.000012089172,0.001252472],"genre_scores_gemma":[0.9993443,0.000031046548,0.00011498552,0.0000029248804,0.000003597887,0.0000028871182,0.00033915718,0.0000027330382,0.00015839079],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99970907,0.000047563328,0.000048507998,0.00008756215,0.000064932115,0.000042320167],"domain_scores_gemma":[0.9943346,0.0015486188,0.0024805812,0.0007473114,0.00062095455,0.00026791397],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051289133,0.00012341906,0.00028332014,0.0023907607,0.0003075759,0.00067693193,0.00038433843,0.00018460547,0.002489686],"category_scores_gemma":[0.0047178944,0.00014711425,0.0001467448,0.0018527869,0.00060965726,0.00070840784,0.00046801544,0.00012352006,0.00040081047],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070335926,0.00001020653,0.9895874,0.00002115528,0.0000390896,0.00007618738,0.00018489051,0.00033964598,0.0026485343,0.00021610202,0.00008110831,0.006725289],"study_design_scores_gemma":[9.858722e-7,0.000019359639,0.998792,0.000002505482,0.000007924543,0.00006928611,0.000113792994,0.0005057035,0.00021839244,0.00006616599,0.00020127163,0.000002639335],"about_ca_topic_score_codex":0.005754749,"about_ca_topic_score_gemma":0.0128536755,"teacher_disagreement_score":0.005754749,"about_ca_system_score_codex":0.0003274547,"about_ca_system_score_gemma":0.00018461233,"threshold_uncertainty_score":0.0114424825},"labels":[],"label_agreement":null},{"id":"W4206464744","doi":"10.1029/2021gl096840","title":"Impacts of Sudden Stratospheric Warming on Extreme Cold Events in Early 2021: An Ensemble‐Based Sensitivity Analysis","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Key Research and Development Program of China; Xiamen University; China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Climatology; Geopotential height; Northern Hemisphere; Environmental science; Polar vortex; Troposphere; Sudden stratospheric warming; Atmospheric sciences; Forecast skill; Polar; Meteorology; Precipitation; Geology; Geography; Physics","score_opus":0.05711949465199758,"score_gpt":0.31463970808492264,"score_spread":0.2575202134329251,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4206464744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969024,0.00008931087,0.00095085485,0.000110995265,0.0000195358,0.000023578723,0.0012358527,0.000032727632,0.0006348906],"genre_scores_gemma":[0.998885,0.000028962364,0.0002602301,0.000018821833,0.0000048490183,0.000013841682,0.0006904706,0.0000030606766,0.000094802774],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994925,0.00025191993,0.000025814712,0.000081313505,0.000059970767,0.00008846351],"domain_scores_gemma":[0.99816066,0.0012682902,0.00011396133,0.00016039872,0.00020393333,0.000092741306],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0023408139,0.00090630486,0.0005635964,0.0006484969,0.0004463783,0.0008498427,0.0005364305,0.0008571922,0.0006895869],"category_scores_gemma":[0.0026750662,0.0003406425,0.0018444872,0.00052414974,0.00033015021,0.00061672705,0.00056657154,0.0009402018,0.00007446123],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003105122,0.00013190313,0.03842938,0.000032751945,0.0006412696,0.00017843768,0.000025793686,0.95515025,0.0024427252,0.00028276176,0.00035508542,0.0020191749],"study_design_scores_gemma":[0.000065345914,0.00042206526,0.091871776,0.000013387275,0.00026254784,0.00006274822,0.000089628455,0.90229845,0.0038640848,0.00045514046,0.0005186677,0.00007608975],"about_ca_topic_score_codex":0.042910457,"about_ca_topic_score_gemma":0.01656241,"teacher_disagreement_score":0.042910457,"about_ca_system_score_codex":0.0013179755,"about_ca_system_score_gemma":0.0006150262,"threshold_uncertainty_score":0.08532137},"labels":[],"label_agreement":null},{"id":"W4210278486","doi":"10.1029/2021gl094756","title":"ENSO‐Driven Fires Cause Large Interannual Variability in the Naturally Emitted, Ozone‐Depleting Trace Gas CH<sub>3</sub>Br","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Ozone; Trace gas; Environmental science; El Niño Southern Oscillation; Atmosphere (unit); Atmospheric sciences; Ozone depletion; Montreal Protocol; Biomass burning; Sea surface temperature; Climatology; Ozone layer; Stratosphere; Environmental chemistry; Chemistry; Meteorology; Geology; Aerosol; Geography","score_opus":0.012509445907622001,"score_gpt":0.25862015156080187,"score_spread":0.24611070565317986,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210278486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999014,0.000018248547,0.00016194175,0.000018035858,0.0000058673427,0.000001947011,0.00034763006,0.000021893955,0.00041044218],"genre_scores_gemma":[0.9993381,0.000016449096,0.000082493,0.000010586883,0.0000030447911,0.0000030939195,0.00040726078,0.0000047379267,0.00013410319],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999523,0.0000071588283,0.0000034687298,0.000015531365,0.000010798082,0.000010643354],"domain_scores_gemma":[0.99982375,0.000039596292,0.00006029233,0.000017499611,0.00002581354,0.000033056695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017474551,0.00015063648,0.00009824357,0.00013652456,0.0001551036,0.000238491,0.00009362297,0.00011623225,0.0006222934],"category_scores_gemma":[0.00033885278,0.00010753572,0.00018693222,0.00016024667,0.00013564024,0.00012246128,0.00018951547,0.00017231621,0.00010971198],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007993266,0.00024656556,0.8211712,0.000045924255,0.00029332092,0.00021226233,0.00014676867,0.016357865,0.14769733,0.00035321005,0.0015071583,0.01116913],"study_design_scores_gemma":[0.000018057583,0.00003520716,0.9869207,0.0000020483897,0.000014876601,0.000028878732,0.000051525327,0.0088382065,0.003609587,0.000085272244,0.00039037224,0.0000052365262],"about_ca_topic_score_codex":0.005994096,"about_ca_topic_score_gemma":0.007801314,"teacher_disagreement_score":0.005994096,"about_ca_system_score_codex":0.00024056694,"about_ca_system_score_gemma":0.00010630847,"threshold_uncertainty_score":0.011918366},"labels":[],"label_agreement":null},{"id":"W4210364008","doi":"10.1029/2021gl097373","title":"Potential Link Between Ice Nucleation and Climate Model Spread in Arctic Amplification","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Aeronautics and Space Administration","keywords":"Arctic; Atmospheric sciences; Environmental science; Climatology; Troposphere; The arctic; Coupled model intercomparison project; Climate model; Sea ice; Arctic ice pack; Climate change; Oceanography; Geology","score_opus":0.02953080276474012,"score_gpt":0.27636107364850493,"score_spread":0.2468302708837648,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4210364008","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958656,0.00011959927,0.0013596881,0.00015836263,0.000010096718,0.0000066772986,0.000339559,0.00005563485,0.0020848592],"genre_scores_gemma":[0.9997012,0.000015817264,0.00008837808,0.000008592303,0.000002428107,0.0000026033445,0.00010208202,0.000005395377,0.00007348711],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99981743,0.00006855534,0.000013086936,0.000051984724,0.000016732349,0.000032295353],"domain_scores_gemma":[0.99818677,0.0012216136,0.00018824836,0.00014393858,0.00015068559,0.00010882549],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010276047,0.00041471602,0.00025193102,0.00051847496,0.00034716306,0.00095226837,0.0005464952,0.0004171503,0.0016206407],"category_scores_gemma":[0.0037148793,0.00034322066,0.00054958,0.0003687028,0.00037958732,0.00072714,0.00078238756,0.0005591913,0.000099008554],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006114674,0.00014580773,0.3431853,0.000062471045,0.00035773675,0.00017581935,0.00014639823,0.63808864,0.0077226427,0.0027243977,0.000752283,0.0060270755],"study_design_scores_gemma":[0.000080924125,0.000063087995,0.13749334,0.00002018526,0.000077057746,0.00003464168,0.000103659404,0.8571152,0.0024814268,0.0018858421,0.000610153,0.00003451755],"about_ca_topic_score_codex":0.021164054,"about_ca_topic_score_gemma":0.011561086,"teacher_disagreement_score":0.021164054,"about_ca_system_score_codex":0.0007408236,"about_ca_system_score_gemma":0.00036241536,"threshold_uncertainty_score":0.042081714},"labels":[],"label_agreement":null},{"id":"W4212881428","doi":"10.1029/2021gl096885","title":"Multidecadal Trends in Organic Carbon Flux Through a Grassland River Network Shaped by Human Controls and Climatic Cycles","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; University of Lethbridge","keywords":"Environmental science; Grassland; Flux (metallurgy); Dissolved organic carbon; Carbon cycle; Seasonality; Pacific decadal oscillation; Climate change; Climatology; Hydrology (agriculture); El Niño Southern Oscillation; Ecosystem; Oceanography; Ecology; Geology","score_opus":0.024070831922983402,"score_gpt":0.27485499706705024,"score_spread":0.2507841651440668,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4212881428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953115,0.000020231122,0.000078142024,0.000013815743,8.0834394e-7,9.2715015e-7,0.00021974451,0.0000042555293,0.00013098113],"genre_scores_gemma":[0.99956924,0.000019955092,0.00008720342,0.0000060432935,0.00000125695,0.0000024112378,0.00022830012,0.000001218939,0.00008426307],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993074,0.00001582642,0.0000056035383,0.00002781626,0.0000074651134,0.000012532308],"domain_scores_gemma":[0.99968874,0.000060386956,0.00012784846,0.000026533531,0.000057242345,0.000039285023],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021613132,0.00006888869,0.00010683967,0.00047747503,0.00015372457,0.00038930756,0.00011070731,0.00020084804,0.00056774926],"category_scores_gemma":[0.0004234548,0.000066741915,0.00011834794,0.00055835355,0.00015572734,0.00026012716,0.00022036272,0.00012739617,0.00007389802],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008419924,0.000030954197,0.9902777,0.000013331278,0.00009092993,0.00004685294,0.00021975506,0.001020588,0.0034885455,0.000099729936,0.0002073832,0.0044198963],"study_design_scores_gemma":[0.0000012918874,0.000011520322,0.998544,0.0000016025156,0.0000074153368,0.000018247565,0.000112145266,0.0010259602,0.00008581674,0.00003051911,0.00015950689,0.000002078686],"about_ca_topic_score_codex":0.008031018,"about_ca_topic_score_gemma":0.012064698,"teacher_disagreement_score":0.008031018,"about_ca_system_score_codex":0.00023201536,"about_ca_system_score_gemma":0.000119430144,"threshold_uncertainty_score":0.015968502},"labels":[],"label_agreement":null},{"id":"W4213076607","doi":"10.1029/2021gl096716","title":"The 28 November 2020 Landslide, Tsunami, and Outburst Flood – A Hazard Cascade Associated With Rapid Deglaciation at Elliot Creek, British Columbia, Canada","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":90,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Vancouver Island University; Fisheries and Oceans Canada; Natural Resources Canada; Geoscience BC; Assembly of First Nations; 3v Geomatics (Canada); Simon Fraser University; Geological Survey of Canada; Tula Foundation; Ministry of Forests; University of Calgary; Saint Mary's University; BGC Engineering (Canada); University of Northern British Columbia","funders":"Hakai Institute; RES’EAU-WaterNET; Tula Foundation","keywords":"Debris; Geology; Landslide; Fjord; Glacier; Flood myth; Hydrology (agriculture); Plume; Sediment; Mudflow; Deglaciation; Oceanography; Glacial lake; Physical geography; Geomorphology; Archaeology; Geography; Holocene; Meteorology","score_opus":0.007858861007099208,"score_gpt":0.21287949726609706,"score_spread":0.20502063625899786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213076607","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98555064,0.000073040326,0.00057053776,0.0006794314,0.000029128814,0.000049814164,0.0030881218,0.00009788867,0.009861344],"genre_scores_gemma":[0.9952127,0.000061299404,0.00033926693,0.000058211997,0.0000053299027,0.000016294001,0.0010945061,0.000008612579,0.0032038686],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998436,0.000013536753,0.0000051243483,0.00002204227,0.00003367362,0.00008191228],"domain_scores_gemma":[0.9997367,0.000023958532,0.000028204457,0.000010423853,0.00007647386,0.00012413891],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019373118,0.0003749037,0.00023906516,0.00046371235,0.0015768177,0.0015054144,0.00087512535,0.00093124283,0.0051847524],"category_scores_gemma":[0.0006311971,0.00029245377,0.00028462836,0.0004993113,0.00074111734,0.00049799803,0.0007845818,0.00091624295,0.00029522777],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00039008193,0.00024056224,0.35865617,0.0000595469,0.00011736405,0.0015656408,0.0005202292,0.6059041,0.0020613843,0.0037924442,0.019164717,0.007527718],"study_design_scores_gemma":[0.00015800013,0.0001224209,0.28617775,0.000043546315,0.00006667624,0.0001378555,0.0024680602,0.7023743,0.000560204,0.0017447748,0.006069584,0.00007678173],"about_ca_topic_score_codex":0.9507134,"about_ca_topic_score_gemma":0.9736786,"teacher_disagreement_score":0.049286604,"about_ca_system_score_codex":0.014381396,"about_ca_system_score_gemma":0.008805301,"threshold_uncertainty_score":0.104344785},"labels":[],"label_agreement":null},{"id":"W4213169803","doi":"10.1029/2021gl096483","title":"Are Significant Tornadoes Occurring Later in the Year in Southern Ontario?","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"","keywords":"Tornado; Confidence interval; Climatology; Meteorology; Environmental science; Geography; Geology; Statistics; Mathematics","score_opus":0.06972649255025767,"score_gpt":0.2825179599013168,"score_spread":0.2127914673510591,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213169803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9840152,0.00032899843,0.00012179203,0.00064385746,0.000020588028,0.000008959623,0.010764142,0.000012783093,0.004083558],"genre_scores_gemma":[0.99572974,0.0002064721,0.000057556124,0.000043329703,0.000006207791,0.000004349184,0.0025714731,0.0000036904394,0.0013772699],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998092,0.0000067619785,0.000011248119,0.000043376884,0.000048580176,0.00008087192],"domain_scores_gemma":[0.99880075,0.000057136604,0.00041989118,0.000040861385,0.00044689127,0.00023437804],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016845041,0.00015835029,0.00021153089,0.0007840011,0.0010498086,0.0011140062,0.00047175863,0.0002389011,0.0030616785],"category_scores_gemma":[0.0013644607,0.00012847899,0.00028521102,0.001968643,0.00048578912,0.00035913818,0.00047856613,0.00031960555,0.0002121534],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047637073,0.0000055532864,0.99471104,0.000025294648,0.00004044661,0.000119086275,0.00053412415,0.00032246616,0.0002844723,0.000119405035,0.0016139448,0.0021765034],"study_design_scores_gemma":[0.0000022080637,0.0000041595677,0.99620515,0.000018460478,0.0000124154285,0.000019200384,0.0013640155,0.00024952402,0.00006019633,0.000026197626,0.0020333359,0.000005150267],"about_ca_topic_score_codex":0.991657,"about_ca_topic_score_gemma":0.9968591,"teacher_disagreement_score":0.0094770435,"about_ca_system_score_codex":0.0094770435,"about_ca_system_score_gemma":0.01186277,"threshold_uncertainty_score":0.06876111},"labels":[],"label_agreement":null},{"id":"W4213234955","doi":"10.1029/2021gl097024","title":"Secondary 12‐Day Planetary Wave in the Mesospheric Water Vapor During the 2016/2017 Unusual Canadian Stratospheric Warming","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Stratosphere; Polar vortex; Sudden stratospheric warming; Microwave Limb Sounder; Atmospheric sciences; Climatology; Water vapor; Mesosphere; Mesopause; Environmental science; Polar; Advection; Arctic; Baroclinity; Geology; Physics; Meteorology; Oceanography; Astronomy","score_opus":0.025488659121706884,"score_gpt":0.24089056621995475,"score_spread":0.21540190709824786,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213234955","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954847,0.00011665807,0.000113551476,0.00018964752,0.00004435334,0.00001224889,0.0008813867,0.000027890457,0.0031296317],"genre_scores_gemma":[0.9989605,0.00003880394,0.0000638011,0.000020019945,0.000010792073,0.0000027003714,0.0003763619,0.000004004707,0.00052306167],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989104,0.0000024485473,0.0000017891178,0.000015739035,0.00003965633,0.00004924816],"domain_scores_gemma":[0.9998073,0.0000074703803,0.000023701004,0.000008651071,0.00009251714,0.00006041301],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000107852844,0.00023842914,0.00016780308,0.00059737405,0.0012780421,0.00055572856,0.00024981707,0.00029241169,0.0012191115],"category_scores_gemma":[0.00027817494,0.00007697841,0.0001677946,0.0006094952,0.00041995905,0.00016820789,0.00045387723,0.00046319506,0.000097528566],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00078801624,0.000117973366,0.79889905,0.00017701338,0.00019404887,0.0032864194,0.003390132,0.002544375,0.13183138,0.0020954919,0.009790579,0.046885505],"study_design_scores_gemma":[0.000005210686,0.00001570921,0.9935946,0.0000066562225,0.000014419061,0.00006976516,0.0006478811,0.0006084768,0.0014669998,0.000053370557,0.0035060016,0.000010990427],"about_ca_topic_score_codex":0.78701967,"about_ca_topic_score_gemma":0.88836193,"teacher_disagreement_score":0.21298033,"about_ca_system_score_codex":0.0024603491,"about_ca_system_score_gemma":0.0037449223,"threshold_uncertainty_score":0.42846918},"labels":[],"label_agreement":null},{"id":"W4213251495","doi":"10.1029/2021gl095199","title":"The Effect of Correlated Permeability on Fluid‐Induced Seismicity","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"","keywords":"Induced seismicity; Geology; Permeability (electromagnetism); Seismology; Footprint; Seismic hazard; Basement; Scaling; Spatial variability; Porosity; Petrology; Geotechnical engineering; Geometry; Paleontology","score_opus":0.029396918995999808,"score_gpt":0.2841619573934513,"score_spread":0.25476503839745146,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213251495","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947508,0.000042851636,0.0044016084,0.000043175623,0.000004464885,0.000005125508,0.000090719084,0.000054864297,0.0006064391],"genre_scores_gemma":[0.9998977,0.0000054234106,0.000066632565,0.0000014483621,8.4127646e-7,6.0168054e-7,0.000011208144,0.0000022384286,0.000013919181],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99952936,0.00018885495,0.000028367242,0.00011918557,0.00006105508,0.000073248986],"domain_scores_gemma":[0.9869811,0.008493379,0.002537148,0.0010183493,0.0005463275,0.00042370876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.001173304,0.00031153878,0.00028561676,0.0006322803,0.00023256995,0.0006255893,0.00046087953,0.0003401424,0.0011330794],"category_scores_gemma":[0.016361702,0.00027653942,0.00023292833,0.0004378429,0.0012666936,0.0009982669,0.00074414205,0.00047906977,0.00009131027],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010208798,0.0003105831,0.38903034,0.00010864017,0.00029193392,0.0013693508,0.00021009913,0.5403765,0.04806771,0.0044528027,0.00041347247,0.0143477535],"study_design_scores_gemma":[0.00003296077,0.0002460385,0.41665012,0.000015998132,0.00007430871,0.0004085541,0.00014207115,0.5630662,0.015756056,0.0032946062,0.00025193836,0.000061277475],"about_ca_topic_score_codex":0.0033292247,"about_ca_topic_score_gemma":0.001434275,"teacher_disagreement_score":0.0033292247,"about_ca_system_score_codex":0.0006144213,"about_ca_system_score_gemma":0.0003736004,"threshold_uncertainty_score":0.006619692},"labels":[],"label_agreement":null},{"id":"W4213255831","doi":"10.1029/2021gl096088","title":"The Impact of Intermittency on Bed Load Sediment Transport","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aeolian processes and effects","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Army Research Laboratory; National Science Foundation","keywords":"Intermittency; Sediment transport; Entrainment (biomusicology); Sediment; Bed load; Geology; Environmental science; Hydrology (agriculture); Soil science; Mechanics; Geotechnical engineering; Turbulence; Geomorphology; Physics","score_opus":0.023541984041688592,"score_gpt":0.3052979250888191,"score_spread":0.2817559410471305,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213255831","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996051,0.000028082044,0.003329533,0.00005392408,0.000006861185,0.0000027420263,0.0000735785,0.000038926533,0.0004152692],"genre_scores_gemma":[0.99986553,0.000004509095,0.00008993645,0.0000021427793,0.0000016367362,8.130444e-7,0.000014000608,0.000002114235,0.000019317762],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99985516,0.000030715262,0.000010733134,0.000044448632,0.000029665336,0.000029239025],"domain_scores_gemma":[0.9985752,0.0008809886,0.00017911942,0.00014820702,0.000107629356,0.000108825174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042199146,0.00018435481,0.00024271508,0.0003758092,0.0002306516,0.0005512294,0.00020005218,0.00026034872,0.00072242215],"category_scores_gemma":[0.0027441685,0.00014795439,0.00015641339,0.00017305634,0.0005138245,0.00059356954,0.0003706266,0.0003002795,0.00005704124],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006956224,0.0003204574,0.27932325,0.00013267017,0.00014100691,0.0007821739,0.00018578001,0.45448256,0.23464933,0.008655108,0.00088935456,0.019742804],"study_design_scores_gemma":[0.00001726145,0.00021779073,0.09521628,0.00000822386,0.000017886834,0.000080140446,0.00005299042,0.88219947,0.018504553,0.0034861157,0.00016791665,0.00003135844],"about_ca_topic_score_codex":0.0028467688,"about_ca_topic_score_gemma":0.0013261625,"teacher_disagreement_score":0.0028467688,"about_ca_system_score_codex":0.0004751977,"about_ca_system_score_gemma":0.00023793975,"threshold_uncertainty_score":0.0056604147},"labels":[],"label_agreement":null},{"id":"W4213277952","doi":"10.1029/2021gl097353","title":"Effects of Improved Simulation of Precipitation on Evapotranspiration and Its Partitioning Over Land","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China; U.S. Department of Energy; Biological and Environmental Research; Office of Science; National Science Foundation","keywords":"Evapotranspiration; Environmental science; Atmospheric sciences; Precipitation; Water cycle; Transpiration; Evaporation; Canopy interception; Climatology; Meteorology; Soil water; Soil science; Geology; Throughfall; Geography","score_opus":0.014421981082612941,"score_gpt":0.2738809212673503,"score_spread":0.25945894018473736,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213277952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99395233,0.00007497788,0.004213078,0.00009978994,0.000024162622,0.000012105894,0.00027316474,0.00024173674,0.0011087096],"genre_scores_gemma":[0.99803513,0.000019274345,0.0017271695,0.000015798947,0.0000040432055,0.0000066073967,0.00010902616,0.000019028694,0.000064019674],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99976474,0.00009075109,0.000017043512,0.00005235567,0.000028095366,0.00004695267],"domain_scores_gemma":[0.99909043,0.0005201457,0.00009075366,0.00009327815,0.00012744883,0.00007799659],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006241231,0.00053269544,0.00040962154,0.00025135977,0.00023842257,0.0004797264,0.00061150343,0.0005342445,0.000740119],"category_scores_gemma":[0.0018640636,0.00021425373,0.0004289964,0.00034665506,0.0003149723,0.00042096328,0.00037353145,0.0004919244,0.00007974271],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020085133,0.00009293416,0.009323972,0.000021984091,0.000042839314,0.000032157244,0.000019565889,0.9826333,0.004279544,0.00021478221,0.00014447422,0.0029936011],"study_design_scores_gemma":[0.000030742714,0.000031967855,0.0023864242,0.0000022550776,0.000011424533,0.0000036282565,0.000006707815,0.9956189,0.0017785685,0.000049895454,0.00007415481,0.000005301786],"about_ca_topic_score_codex":0.024621358,"about_ca_topic_score_gemma":0.010048863,"teacher_disagreement_score":0.024621358,"about_ca_system_score_codex":0.0005629996,"about_ca_system_score_gemma":0.00062444917,"threshold_uncertainty_score":0.048956096},"labels":[],"label_agreement":null},{"id":"W4213360190","doi":"10.1029/2021gl096599","title":"Ice Sheet Surface and Subsurface Melt Water Discrimination Using Multi‐Frequency Microwave Radiometry","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":32,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Meltwater; Greenland ice sheet; Environmental science; Microwave; Geology; Ice sheet; Subsurface flow; Remote sensing; Climatology; Snow; Geomorphology; Groundwater","score_opus":0.07737959762095126,"score_gpt":0.3058378799226895,"score_spread":0.22845828230173826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4213360190","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.987362,0.00018017423,0.011148999,0.000025818159,0.0000062654417,0.0000079858055,0.00029788603,0.000116974574,0.0008538535],"genre_scores_gemma":[0.9932,0.00007673243,0.0062131374,0.000015172669,0.0000072349185,0.0000066037783,0.00025757318,0.000011989071,0.0002115533],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999511,0.000008515379,0.0000014150968,0.000020711057,0.0000089259465,0.000009297658],"domain_scores_gemma":[0.9999305,0.00001952029,0.00001690762,0.000008802848,0.000017706718,0.0000064869396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018190258,0.00027071728,0.00017161279,0.00044164978,0.00007510204,0.00032807278,0.00013917149,0.00012747163,0.00045598717],"category_scores_gemma":[0.00013914681,0.00010004005,0.00014398158,0.00030173876,0.00011191894,0.00030775688,0.00014333516,0.00015235186,0.0001225142],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003930644,0.0000707124,0.14904723,0.00007305669,0.00008785886,0.000069522896,0.0000856769,0.007387484,0.7867031,0.00020997,0.00028420196,0.055588186],"study_design_scores_gemma":[0.00005305615,0.00021920598,0.6737442,0.000021434249,0.00015504738,0.000108286156,0.00013944825,0.14691904,0.17593856,0.00046266842,0.002200118,0.000038898306],"about_ca_topic_score_codex":0.0028488543,"about_ca_topic_score_gemma":0.0062139058,"teacher_disagreement_score":0.0028488543,"about_ca_system_score_codex":0.00016705928,"about_ca_system_score_gemma":0.00011865959,"threshold_uncertainty_score":0.005664587},"labels":[],"label_agreement":null},{"id":"W4220658326","doi":"10.1029/2021gl096868","title":"Increased Variability of Biomass Burning Emissions in CMIP6 Amplifies Hydrologic Cycle in the CESM2 Large Ensemble","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Pacific Northwest National Laboratory; University of Victoria; National Center for Atmospheric Research; National Science Foundation","keywords":"Environmental science; Coupled model intercomparison project; Longwave; Atmospheric sciences; Climatology; Precipitation; Water cycle; Shortwave radiation; Shortwave; Biomass burning; Greenhouse gas; Climate model; Meteorology; Climate change; Radiative transfer; Aerosol; Geology","score_opus":0.017238093805122204,"score_gpt":0.273911407088647,"score_spread":0.2566733132835248,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220658326","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99561536,0.000046431156,0.00096566597,0.00028136483,0.000025803944,0.0000080104555,0.0012254489,0.00015074962,0.0016812548],"genre_scores_gemma":[0.9982816,0.000026313568,0.00038277707,0.000052159427,0.00001613945,0.00000868116,0.0009925164,0.000027970018,0.00021186832],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997925,0.00005358959,0.000012843654,0.00006696125,0.000029408617,0.000044655608],"domain_scores_gemma":[0.999464,0.00019077657,0.00005718905,0.00011228425,0.00009224076,0.00008355365],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009541797,0.00053858774,0.0003371848,0.00036131163,0.0003712019,0.00080970844,0.000532712,0.0005272007,0.0017834565],"category_scores_gemma":[0.0016227507,0.0002578987,0.0006929887,0.00054005894,0.0003357686,0.0008245203,0.000643443,0.0006824392,0.00016846953],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00086389243,0.00028926617,0.31458393,0.00008391363,0.00072963745,0.0005073607,0.00014174564,0.6342415,0.026145075,0.0023064576,0.0058480203,0.014259114],"study_design_scores_gemma":[0.00020464494,0.000092726674,0.25219774,0.000015896072,0.0001509009,0.0000645057,0.00010773617,0.7328999,0.010756349,0.00086772186,0.0025708403,0.000071132155],"about_ca_topic_score_codex":0.01788966,"about_ca_topic_score_gemma":0.01390536,"teacher_disagreement_score":0.01788966,"about_ca_system_score_codex":0.0006204714,"about_ca_system_score_gemma":0.00050080277,"threshold_uncertainty_score":0.03557104},"labels":[],"label_agreement":null},{"id":"W4220789544","doi":"10.1029/2021gl097614","title":"Elucidating Coastal Ocean Carbon Transport Processes: A Novel Approach Applied to the Northwest North Atlantic Shelf","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Dalhousie University","funders":"Natural Sciences and Engineering Research Council of Canada; Marine Environmental Observation Prediction and Response Network","keywords":"Oceanography; Biogeochemical cycle; Outgassing; Alkalinity; Latitude; Environmental science; Continental shelf; Geology; Climatology","score_opus":0.022873769722592,"score_gpt":0.22818292948751112,"score_spread":0.20530915976491912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220789544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9219143,0.0007216315,0.07213873,0.00023804893,0.000030002357,0.00006024614,0.0005564272,0.00013807007,0.0042024674],"genre_scores_gemma":[0.95493084,0.0005880221,0.043221235,0.000046996494,0.000023084871,0.000033329827,0.00016638935,0.000016206739,0.0009740163],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999752,0.0000034060663,0.000001633217,0.00001043576,0.0000045323245,0.0000047152816],"domain_scores_gemma":[0.9999528,0.000008333792,0.000011308595,0.0000074086665,0.000012159491,0.000007927778],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009177011,0.00030745685,0.00028359634,0.00047436226,0.00049745786,0.0009193895,0.00032425433,0.0003029246,0.00078064005],"category_scores_gemma":[0.00017411946,0.00015990797,0.00036254566,0.0006213857,0.0002818865,0.0003054858,0.0005640838,0.00023643747,0.00010716771],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021014592,0.0002343131,0.25853425,0.0002485661,0.0003454265,0.0011370818,0.00051627227,0.1481975,0.47684756,0.010830208,0.00054269674,0.10235594],"study_design_scores_gemma":[0.00003398877,0.00016026653,0.17139848,0.000028978411,0.00015682877,0.00023074946,0.0008136534,0.8061015,0.011112991,0.0064194957,0.0034860726,0.00005703323],"about_ca_topic_score_codex":0.046639882,"about_ca_topic_score_gemma":0.07522656,"teacher_disagreement_score":0.046639882,"about_ca_system_score_codex":0.0006010735,"about_ca_system_score_gemma":0.0008224561,"threshold_uncertainty_score":0.09273684},"labels":[],"label_agreement":null},{"id":"W4220845663","doi":"10.1029/2021gl096069","title":"Urban Water Storage Capacity Inferred From Observed Evapotranspiration Recession","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Research Foundation of Korea; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; Canada Foundation for Innovation; Academy of Finland; National Research Foundation Singapore; Deutsche Forschungsgemeinschaft","keywords":"Evapotranspiration; Water storage; Environmental science; Eddy covariance; Latent heat; Precipitation; Evaporation; Surface runoff; Sensible heat; Hydrology (agriculture); Atmospheric sciences; Ecosystem; Meteorology; Geology; Geography; Ecology; Geomorphology","score_opus":0.08017829622395693,"score_gpt":0.28021680233970203,"score_spread":0.20003850611574509,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220845663","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987785,0.000017245817,0.0005572577,0.0000046819587,4.4928265e-7,0.0000016458403,0.00036439687,0.000018959458,0.00025687896],"genre_scores_gemma":[0.9995975,0.000009274793,0.00014191,5.4394656e-7,4.323056e-7,0.0000018914955,0.00022541509,0.0000022148056,0.000020779018],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994445,0.000009361621,0.000005381092,0.000017016788,0.000009333611,0.000014532287],"domain_scores_gemma":[0.9996631,0.000119226985,0.0000891348,0.000053748678,0.000050492214,0.000024280529],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019795625,0.00025068579,0.00019986724,0.0008512756,0.00013433314,0.00038190253,0.00023675285,0.00015265156,0.00069385604],"category_scores_gemma":[0.0006671746,0.00018284001,0.00017962215,0.0008790486,0.0002336383,0.0004126545,0.00036854993,0.0001189233,0.00014642235],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040006667,0.000062027946,0.86968875,0.00007348944,0.00015064061,0.00012281662,0.00021159921,0.08780267,0.027567815,0.0005644901,0.0003647501,0.012990932],"study_design_scores_gemma":[0.000011800719,0.000028707282,0.8631308,0.000009828176,0.000030221569,0.000049741102,0.00015088219,0.12852879,0.0073702647,0.00035594957,0.00030687233,0.000026103751],"about_ca_topic_score_codex":0.007770743,"about_ca_topic_score_gemma":0.01006033,"teacher_disagreement_score":0.007770743,"about_ca_system_score_codex":0.0003028573,"about_ca_system_score_gemma":0.00016593037,"threshold_uncertainty_score":0.015451014},"labels":[],"label_agreement":null},{"id":"W4220852734","doi":"10.1029/2021gl097347","title":"Closing the Winter Gap—Year‐Round Measurements of Soil CO<sub>2</sub> Emission Sources in Arctic Tundra","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Mining Association of Canada","funders":"National Science Foundation","keywords":"Tundra; Permafrost; Environmental science; Arctic; Climate change; Soil carbon; Growing season; Atmospheric sciences; Atmosphere (unit); Carbon dioxide; Carbon fibers; Greenhouse gas; Chronosequence; Soil water; Climatology; Physical geography; Soil science; Agronomy; Ecology; Geology; Oceanography; Geography; Meteorology","score_opus":0.11706540369753211,"score_gpt":0.31539632895909486,"score_spread":0.19833092526156276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220852734","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986564,0.000061570034,0.00026417518,0.000016191536,0.0000030001756,0.0000013191227,0.00050479575,0.000013558655,0.0004790097],"genre_scores_gemma":[0.9991327,0.000028328981,0.00020593828,0.000017984325,0.000004130682,0.0000030265594,0.00047381007,0.0000044599565,0.00012956049],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999943,0.0000103788525,0.0000034455823,0.000020692176,0.000009798557,0.000012670628],"domain_scores_gemma":[0.999814,0.000025867726,0.00005018991,0.000020740708,0.00004946219,0.000039822826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018118162,0.00020138074,0.00017660263,0.00035883358,0.00037138845,0.000457234,0.0002227814,0.0002825096,0.0005207249],"category_scores_gemma":[0.00027828052,0.00011814543,0.00013400268,0.00035160064,0.00016165504,0.00025678868,0.00024660453,0.00021590412,0.0001359129],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036465493,0.000048247854,0.92884433,0.000025253454,0.000115409486,0.000100638805,0.00038172858,0.0008953584,0.059325762,0.00007978895,0.00031963675,0.009499248],"study_design_scores_gemma":[0.0000017883392,0.000014905535,0.997015,0.0000017989585,0.000008162731,0.00002742264,0.00007265081,0.0004833121,0.001985536,0.000017099943,0.00036998157,0.0000024495505],"about_ca_topic_score_codex":0.027106656,"about_ca_topic_score_gemma":0.05168022,"teacher_disagreement_score":0.027106656,"about_ca_system_score_codex":0.00038860345,"about_ca_system_score_gemma":0.00020292871,"threshold_uncertainty_score":0.05389774},"labels":[],"label_agreement":null},{"id":"W4220902169","doi":"10.1029/2021gl097491","title":"Baroclinic Control of Southern Ocean Eddy Upwelling Near Topography","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Baroclinity; Upwelling; Eddy; Geology; Mesoscale meteorology; Isopycnal; Climatology; Oceanography; Meteorology; Turbulence; Geography","score_opus":0.020202658057458623,"score_gpt":0.2575694972518816,"score_spread":0.23736683919442297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220902169","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974227,0.00004323152,0.00066291617,0.00005552832,0.000010193015,0.000002840563,0.000050939077,0.000038015194,0.0017136189],"genre_scores_gemma":[0.99978787,0.000016176507,0.000064976375,0.0000046596515,0.0000021171682,7.2529195e-7,0.000014614772,0.0000044142153,0.000104376624],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999722,0.000007641689,0.000001925716,0.000005421839,0.0000043645127,0.000008374235],"domain_scores_gemma":[0.9998642,0.000037430807,0.00002840566,0.000014399875,0.000020390524,0.00003516088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114652605,0.00017216231,0.00012799488,0.00014999707,0.00020140494,0.0005402162,0.00012503323,0.00015783067,0.0010890565],"category_scores_gemma":[0.00038536714,0.00015218982,0.00021160513,0.0000883945,0.0002774188,0.00027860995,0.00031396828,0.0002064341,0.000100086996],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004848726,0.00021914799,0.22380346,0.000091347865,0.00026785844,0.00043145582,0.00026918674,0.48333278,0.2695848,0.005592891,0.0012671931,0.014654986],"study_design_scores_gemma":[0.00009990824,0.000115339324,0.24352334,0.000011104516,0.000051836065,0.00003463296,0.000120627104,0.74807286,0.0060113664,0.0012882054,0.0006456177,0.000025197987],"about_ca_topic_score_codex":0.008520097,"about_ca_topic_score_gemma":0.0066626896,"teacher_disagreement_score":0.008520097,"about_ca_system_score_codex":0.00032973278,"about_ca_system_score_gemma":0.00035054085,"threshold_uncertainty_score":0.016941011},"labels":[],"label_agreement":null},{"id":"W4220942934","doi":"10.1029/2021gl096474","title":"Withdrawn: Similar Isotopic Biases of Plant Stem Bulk Water From Different Water Sources by Cryogenic Vacuum Distillation Demonstrated Through Rehydration Experiments","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Wilfrid Laurier University; McGill University","funders":"","keywords":"Distillation; Vacuum distillation; Environmental science; Chemistry; Chromatography","score_opus":0.04013772184392208,"score_gpt":0.2584879885405813,"score_spread":0.21835026669665922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220942934","genre_codex":"editorial","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.073061354,0.012177414,0.017698498,0.13293251,0.5665912,0.0007440497,0.11549151,0.0069218166,0.07438166],"genre_scores_gemma":[0.2425423,0.014449896,0.021785945,0.043465663,0.03532192,0.00078621367,0.105667464,0.0071981605,0.5287824],"study_design_codex":"not_applicable","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99708515,0.00013336517,0.00039610593,0.00018832828,0.002028597,0.00016850997],"domain_scores_gemma":[0.9785181,0.0024591482,0.0009041517,0.0012027388,0.016241064,0.0006747258],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0027581772,0.0007776909,0.0009834709,0.0016012281,0.0018497109,0.0022848055,0.001739159,0.002588266,0.06389278],"category_scores_gemma":[0.02167407,0.0003777551,0.0006886127,0.0026401873,0.00067365135,0.0018265,0.0013109053,0.0023047228,0.027500032],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013831941,0.0000807517,0.001547462,0.0013781183,0.00009823822,0.0015996097,0.00037378364,0.00016016996,0.06254103,0.003814582,0.84119827,0.08582477],"study_design_scores_gemma":[0.0002300263,0.00025137633,0.012482077,0.00022398421,0.00013194718,0.00075565337,0.00041482731,0.0006317901,0.050514467,0.0018478595,0.9323608,0.00015524644],"about_ca_topic_score_codex":0.006892281,"about_ca_topic_score_gemma":0.0073509286,"teacher_disagreement_score":0.06389278,"about_ca_system_score_codex":0.0020923864,"about_ca_system_score_gemma":0.0033189985,"threshold_uncertainty_score":0.21374267},"labels":[],"label_agreement":null},{"id":"W4220972324","doi":"10.1029/2022gl097984","title":"Supershear Rupture During the 2021 <i>M</i><sub>W</sub> 7.4 Maduo, China, Earthquake","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Natural Resources Canada","funders":"","keywords":"Seismology; Geology; Aftershock; Earthquake rupture; Seismometer; Geodetic datum; Fault (geology); Geodesy","score_opus":0.01784879896368408,"score_gpt":0.24070417003934333,"score_spread":0.22285537107565925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220972324","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997278,0.000013597156,0.000097874596,0.000010576588,0.0000010108321,0.0000011193416,0.000030611405,0.0000037819923,0.000113713686],"genre_scores_gemma":[0.9997545,0.000013218365,0.00006928068,0.0000033887275,0.0000025379234,0.0000012899798,0.00009363829,6.5542787e-7,0.000061450504],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999398,0.0000058171777,0.0000036385786,0.00001489328,0.000013588876,0.000022205235],"domain_scores_gemma":[0.9998652,0.000012106324,0.000051043076,0.000014208107,0.000018328095,0.000039095463],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012754324,0.00023302273,0.0002165738,0.00046769012,0.00032121508,0.00025184674,0.000242371,0.00020514865,0.00037809846],"category_scores_gemma":[0.00024882366,0.00018422425,0.00019240353,0.00031301007,0.00020245618,0.00024688497,0.0003638647,0.00013665832,0.00006198946],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031140415,0.000100723766,0.8882708,0.000078437755,0.00018581247,0.0012662981,0.0006095018,0.012437127,0.07053588,0.0003320499,0.00045380084,0.02541814],"study_design_scores_gemma":[0.00000783741,0.00005854951,0.984938,0.0000036921413,0.000046308614,0.00006821444,0.00019406686,0.012187532,0.0022153708,0.000044483622,0.00022698562,0.00000893606],"about_ca_topic_score_codex":0.012006139,"about_ca_topic_score_gemma":0.02419282,"teacher_disagreement_score":0.012006139,"about_ca_system_score_codex":0.0004101328,"about_ca_system_score_gemma":0.00027291334,"threshold_uncertainty_score":0.023872495},"labels":[],"label_agreement":null},{"id":"W4220977417","doi":"10.1029/2022gl098158","title":"Global Propagation of Ionospheric Disturbances Associated With the 2022 Tonga Volcanic Eruption","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":264,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Canadian Space Agency; Natural Environment Research Council; Sight Research UK","keywords":"Ionosphere; Geology; Volcano; Epicenter; Vulcanian eruption; Satellite; Global Positioning System; Seismology; Geophysics; Geodesy; Physics; Telecommunications","score_opus":0.01135392284469783,"score_gpt":0.2620723736408518,"score_spread":0.25071845079615396,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220977417","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99924845,0.000033589193,0.000111819914,0.000008084872,0.0000022196496,0.0000025423637,0.00027418297,0.000009182853,0.000309925],"genre_scores_gemma":[0.998987,0.00003247215,0.00014771702,0.000006189693,0.000003831206,0.000003500804,0.00064003543,0.0000022680968,0.00017697766],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994504,0.000005403346,0.000003629753,0.000015769216,0.000013973495,0.000016278644],"domain_scores_gemma":[0.9997212,0.000026750387,0.000121701254,0.000020971404,0.000051133848,0.000058215082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015373924,0.0001934447,0.00015441829,0.0005379025,0.0002053849,0.00037828452,0.00011491464,0.00016883152,0.0006613091],"category_scores_gemma":[0.00039570528,0.00008569726,0.0001392299,0.00067044224,0.00015857677,0.0001823075,0.000390438,0.0001508236,0.00011538206],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008547539,0.000014286796,0.9823646,0.000016417487,0.000059521735,0.00015160102,0.00033649208,0.0009669654,0.008912582,0.000027601098,0.00019855644,0.0068659275],"study_design_scores_gemma":[0.0000015004598,0.000016271293,0.9988502,0.0000014977492,0.000010656726,0.000028244342,0.000085627034,0.0004893259,0.00027082278,0.000004516208,0.00023919773,0.0000020646185],"about_ca_topic_score_codex":0.01834665,"about_ca_topic_score_gemma":0.028469216,"teacher_disagreement_score":0.01834665,"about_ca_system_score_codex":0.00037119095,"about_ca_system_score_gemma":0.0002516739,"threshold_uncertainty_score":0.03647971},"labels":[],"label_agreement":null},{"id":"W4220997579","doi":"10.1029/2021gl097154","title":"Extratropical Shortwave Cloud Feedbacks in the Context of the Global Circulation and Hydrological Cycle","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Pacific Northwest National Laboratory; Lawrence Livermore National Laboratory; University of Wyoming; Biological and Environmental Research; Natural Sciences and Engineering Research Council of Canada; National Oceanic and Atmospheric Administration; Nuclear Safety and Security Commission; Battelle; Office of Science; National Aeronautics and Space Administration; U.S. Department of Energy; Division of Earth Sciences; National Science Foundation","keywords":"Extratropical cyclone; Climatology; Context (archaeology); Shortwave; General Circulation Model; Environmental science; Water cycle; Cloud computing; Meteorology; Circulation (fluid dynamics); Geology; Climate change; Geography; Oceanography; Computer science; Radiative transfer; Physics","score_opus":0.01995985537436864,"score_gpt":0.2756739091265563,"score_spread":0.2557140537521877,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4220997579","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976301,0.00017798132,0.00013097475,0.00053716084,0.00001403158,0.0000024686512,0.00032353064,0.000017466746,0.0011662275],"genre_scores_gemma":[0.99970907,0.00006376512,0.00004743043,0.00003130774,0.000007681289,9.403503e-7,0.000065453176,0.0000039654424,0.00007044027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999001,0.000034281504,0.000005851666,0.000020243106,0.00001443259,0.000025124238],"domain_scores_gemma":[0.99963033,0.000117881405,0.0000649693,0.00003006605,0.00007430165,0.00008242534],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036029212,0.00017669324,0.00020303864,0.00038262733,0.00029514756,0.00071194005,0.00017502096,0.0002699474,0.0012532509],"category_scores_gemma":[0.0009717137,0.00012666623,0.00028665396,0.00043081533,0.00040129622,0.0005632481,0.00063868787,0.00034782628,0.000064938686],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027443393,0.00009052338,0.84856755,0.00011641104,0.00039104425,0.00053401955,0.0005645593,0.1088256,0.016785111,0.006230711,0.0029792646,0.014640664],"study_design_scores_gemma":[0.000025258638,0.00002506867,0.95127785,0.000014438913,0.000046926856,0.000027319722,0.00043178885,0.043778922,0.00077769335,0.0023232684,0.0012497054,0.00002172977],"about_ca_topic_score_codex":0.04752285,"about_ca_topic_score_gemma":0.071124025,"teacher_disagreement_score":0.04752285,"about_ca_system_score_codex":0.0009546143,"about_ca_system_score_gemma":0.0005775862,"threshold_uncertainty_score":0.094492435},"labels":[],"label_agreement":null},{"id":"W4221035301","doi":"10.1029/2021gl097526","title":"Standing Alfvén Waves Within Equatorial Plasma Bubbles","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Physics; Ionosphere; Geophysics; Plasma; Magnetic field; Electric field; Field line; Computational physics; Magnetometer; Standing wave; Spacecraft; Optics","score_opus":0.0243596595939877,"score_gpt":0.2910376713160007,"score_spread":0.266678011722013,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221035301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986528,0.000067937486,0.00069826544,0.000016104743,0.000002427507,0.0000016745669,0.00004909738,0.000016636704,0.00049496477],"genre_scores_gemma":[0.99962103,0.0000156754,0.00021072656,0.00000399359,0.0000031354416,0.0000017074891,0.000047081376,0.0000021182466,0.0000946366],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999671,0.0000033110894,0.000001537968,0.00000674168,0.00000914829,0.000012115343],"domain_scores_gemma":[0.9997515,0.00005845278,0.000082635415,0.000025751706,0.000038247654,0.000043423508],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000770986,0.00008785717,0.00009039445,0.00036008918,0.00018402813,0.00025772367,0.00014337986,0.00012600175,0.00083392934],"category_scores_gemma":[0.00030333063,0.00009382925,0.000056804136,0.00021232138,0.00028015007,0.0002711549,0.00034581867,0.00015670972,0.00008912494],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00062022946,0.000054240703,0.22697736,0.00007585471,0.00007355218,0.0011514081,0.001240656,0.0015162596,0.73712724,0.0015340127,0.00069984846,0.028929302],"study_design_scores_gemma":[0.000023505016,0.00017124212,0.9486518,0.000015603038,0.000024084482,0.0007223575,0.00073424465,0.008394739,0.03822308,0.0009295586,0.0020893419,0.000020415493],"about_ca_topic_score_codex":0.0007397643,"about_ca_topic_score_gemma":0.00062214956,"teacher_disagreement_score":0.00083392934,"about_ca_system_score_codex":0.000088299385,"about_ca_system_score_gemma":0.00004181477,"threshold_uncertainty_score":0.0027897954},"labels":[],"label_agreement":null},{"id":"W4221069593","doi":"10.1029/2021gl096076","title":"Distinct North American Cooling Signatures Following the Zonally Symmetric and Asymmetric Modes of Winter Stratospheric Variability","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Polar vortex; Stratosphere; Sudden stratospheric warming; Arctic oscillation; Vortex; Polar; Atmospheric sciences; Arctic; Climatology; Geology; Oscillation (cell signaling); Physics; Meteorology; Northern Hemisphere; Chemistry; Astronomy; Oceanography","score_opus":0.02242414930160834,"score_gpt":0.28187780789216005,"score_spread":0.2594536585905517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221069593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992906,0.000014509303,0.00011133164,0.000011614905,0.0000014598597,0.000001097758,0.00007462914,0.000012222963,0.000482627],"genre_scores_gemma":[0.9997025,0.0000095691075,0.00004010031,0.000002660894,9.717605e-7,0.0000013381385,0.00013220205,0.000004150093,0.00010641705],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997044,0.000006104344,8.5724616e-7,0.0000074234795,0.000004694458,0.00001050596],"domain_scores_gemma":[0.9999249,0.000016723458,0.000012011123,0.000011849324,0.000019466752,0.000015000136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000098927296,0.00016455627,0.00014936153,0.00021629705,0.00017525844,0.00029003003,0.0001045066,0.00012299129,0.0011025397],"category_scores_gemma":[0.00021219994,0.00012494052,0.0002112169,0.00015391216,0.00017742833,0.0001534731,0.00021602375,0.000120947974,0.00010684578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011023955,0.0001410787,0.6746713,0.000058976937,0.00039233043,0.0002839689,0.00054040883,0.046854824,0.25531268,0.0010213953,0.0014384628,0.01818227],"study_design_scores_gemma":[0.000023976894,0.000070509326,0.9674153,0.0000034748793,0.000040825926,0.000036061818,0.00012794965,0.027167305,0.0044646305,0.0001571753,0.00048148894,0.000011438633],"about_ca_topic_score_codex":0.017837983,"about_ca_topic_score_gemma":0.02699943,"teacher_disagreement_score":0.017837983,"about_ca_system_score_codex":0.00016939864,"about_ca_system_score_gemma":0.00019412946,"threshold_uncertainty_score":0.03546828},"labels":[],"label_agreement":null},{"id":"W4221107151","doi":"10.1029/2021gl097036","title":"The 2021 Western North American Heatwave and Its Subseasonal Predictions","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":111,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Anomaly (physics); Boreal; Environmental science; Range (aeronautics); Troposphere; El Niño Southern Oscillation; Magnitude (astronomy); Atmospheric sciences; Meteorology; Geography; Geology","score_opus":0.03530031002722574,"score_gpt":0.2974376140448716,"score_spread":0.2621373040176459,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4221107151","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9933444,0.00009716688,0.001306361,0.00029005436,0.00003532736,0.000009738353,0.001375692,0.0001294266,0.0034118607],"genre_scores_gemma":[0.9979063,0.00003971244,0.00048378296,0.000021831545,0.000011586267,0.000009131326,0.0010270431,0.000009306879,0.00049142976],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992883,0.000016926984,0.000003129941,0.000018655977,0.00001470705,0.000017776178],"domain_scores_gemma":[0.9998029,0.000044531378,0.000023418768,0.000019510317,0.00007261188,0.000037173522],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003748376,0.0004181678,0.00024290076,0.00015787085,0.00025874126,0.0005031164,0.00030773456,0.0003153927,0.0012387802],"category_scores_gemma":[0.0005849774,0.00014426674,0.00028300588,0.000249066,0.0001469264,0.00038574115,0.00024573164,0.00033718752,0.0002725927],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021903585,0.000093190785,0.07158778,0.00001822009,0.000080607606,0.000070738715,0.00003905386,0.9116775,0.0011242188,0.00062678836,0.0028843882,0.011578453],"study_design_scores_gemma":[0.00003176993,0.000041821848,0.030405125,0.0000053559643,0.000024082205,0.000009702088,0.00006678748,0.9673104,0.0006946998,0.00045050323,0.00095003116,0.000009627671],"about_ca_topic_score_codex":0.14777605,"about_ca_topic_score_gemma":0.13477132,"teacher_disagreement_score":0.85222393,"about_ca_system_score_codex":0.00096423796,"about_ca_system_score_gemma":0.0011516211,"threshold_uncertainty_score":0.29383183},"labels":[],"label_agreement":null},{"id":"W4223424848","doi":"10.1029/2021gl097659","title":"Effects of Subseasonal Variation in the East Asian Monsoon System on the Summertime Heat Wave in Western North America in 2021","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":48,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Postdoctoral Program for Innovative Talents","keywords":"Teleconnection; Climatology; Rossby wave; Anomaly (physics); East Asia; Geology; Monsoon; Siberian High; Jet stream; Environmental science; Atmospheric sciences; El Niño Southern Oscillation; Jet (fluid); Geography","score_opus":0.02843692306431578,"score_gpt":0.2596304386145701,"score_spread":0.2311935155502543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223424848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997099,0.000017602057,0.000024962086,0.000016643802,0.000003005805,0.0000011266513,0.00005781507,0.0000027571218,0.00016607343],"genre_scores_gemma":[0.99983335,0.000014688138,0.00001870668,0.0000045662528,0.0000016860514,0.0000013105835,0.00007599268,8.5239424e-7,0.000048709295],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999176,0.000024713463,0.000005720259,0.000016454022,0.000013708414,0.000021824973],"domain_scores_gemma":[0.9997019,0.00008143718,0.00006289971,0.00002067393,0.000052855754,0.00008011347],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002344394,0.0001524684,0.00012970935,0.00021272339,0.00025380187,0.00044439902,0.00010874302,0.00016341546,0.00056137226],"category_scores_gemma":[0.00070633186,0.00007231562,0.000156421,0.00029198016,0.00021229952,0.00017591323,0.00020283238,0.00018766103,0.000056707795],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032615196,0.000120756835,0.9768003,0.000016971764,0.00011128811,0.00030317903,0.00030363185,0.0046875435,0.009072838,0.00015619346,0.00043842613,0.007662629],"study_design_scores_gemma":[0.000002428993,0.000017797953,0.99676955,0.0000014079588,0.0000100312,0.000014564857,0.00021440942,0.0026490137,0.0001954146,0.000010703155,0.000112689246,0.0000021492879],"about_ca_topic_score_codex":0.06417602,"about_ca_topic_score_gemma":0.10413992,"teacher_disagreement_score":0.935824,"about_ca_system_score_codex":0.00042981564,"about_ca_system_score_gemma":0.00034829715,"threshold_uncertainty_score":0.12760496},"labels":[],"label_agreement":null},{"id":"W4223451023","doi":"10.1029/2022gl098951","title":"Complexity in the Evolution, Composition, and Spectroscopy of Brown Carbon in Aircraft Measurements of Wildfire Plumes","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; York University","funders":"National Oceanic and Atmospheric Administration; Natural Sciences and Engineering Research Council of Canada; Mitacs; National Aeronautics and Space Administration","keywords":"Plume; Absorption (acoustics); Environmental science; Carbon fibers; Atmospheric sciences; Aerosol; Absorption spectroscopy; Meteorology; Analytical Chemistry (journal); Environmental chemistry; Chemistry; Materials science; Geology; Physics; Optics","score_opus":0.05431207887533041,"score_gpt":0.28673676607435533,"score_spread":0.23242468719902493,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223451023","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998133,0.000047308302,0.0012856591,0.0000116127185,0.0000027062467,0.0000036885385,0.00008027309,0.000029718864,0.00040593243],"genre_scores_gemma":[0.99894875,0.00002154216,0.000798744,0.000011630979,0.0000018729535,0.0000027589138,0.00011230366,0.0000064624014,0.00009592696],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989486,0.000015165241,0.0000035123292,0.000032998854,0.000033837823,0.000019599862],"domain_scores_gemma":[0.99982363,0.000063997664,0.000026773649,0.000010060361,0.00005687149,0.000018629338],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036095633,0.00020525235,0.00009537653,0.00068723323,0.00024965135,0.00025550096,0.00017231423,0.0002294323,0.00033622858],"category_scores_gemma":[0.00038967983,0.00015506663,0.00019669079,0.00029632897,0.0002011633,0.00030488815,0.00013877051,0.00020561826,0.000053081963],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044646196,0.00012592762,0.36624542,0.000056279656,0.00012939896,0.00019576654,0.00059546717,0.003384369,0.61360645,0.00030567948,0.00025756608,0.014651286],"study_design_scores_gemma":[0.000009727023,0.00012751645,0.9177602,0.000008533137,0.0000550994,0.00019701169,0.00024955987,0.01775339,0.06308846,0.0001397499,0.0005917666,0.000019022822],"about_ca_topic_score_codex":0.007851899,"about_ca_topic_score_gemma":0.010077126,"teacher_disagreement_score":0.007851899,"about_ca_system_score_codex":0.0003019434,"about_ca_system_score_gemma":0.00010683142,"threshold_uncertainty_score":0.015612364},"labels":[],"label_agreement":null},{"id":"W4223569320","doi":"10.1029/2021gl097243","title":"Observation‐Based Estimates of Eulerian‐Mean Boundary Downwelling in the Western Subpolar North Atlantic","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Agence Nationale de la Recherche","keywords":"Downwelling; Geology; Hydrography; Continental shelf; Boundary current; Oceanography; Thermohaline circulation; Climatology; Upwelling; Argo; North Atlantic Deep Water; Geostrophic wind; Ocean current","score_opus":0.04023667734060096,"score_gpt":0.26833848429419743,"score_spread":0.22810180695359647,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4223569320","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99806505,0.000034414985,0.00031450237,0.000008990948,0.0000026956413,0.0000031357963,0.00092675275,0.000016417145,0.0006279891],"genre_scores_gemma":[0.99708146,0.000037755104,0.00064350595,0.000004910287,0.000003651118,0.000004884352,0.002041372,0.000004655084,0.0001777837],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993885,0.00001144464,0.000006128469,0.000021643056,0.000012714636,0.000009212889],"domain_scores_gemma":[0.9996823,0.00006593521,0.00010244923,0.00003150545,0.00007767851,0.00004011939],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002872835,0.00016457103,0.00013477103,0.00066493667,0.00017036943,0.00042967638,0.00011179105,0.00013902294,0.0009292999],"category_scores_gemma":[0.000618515,0.00012850399,0.00017853208,0.0004695497,0.00011215761,0.00035048203,0.00030223426,0.00010618963,0.00023416082],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000070735936,0.000027217196,0.9863544,0.000014882251,0.000049369544,0.000020701309,0.00012109787,0.002622451,0.0032631867,0.000047783156,0.0002652455,0.007142793],"study_design_scores_gemma":[0.0000034808058,0.0000060503985,0.99632484,0.0000041934477,0.000006756849,0.0000052191876,0.000055513556,0.0031623372,0.00020550018,0.000015445488,0.0002083527,0.0000024375072],"about_ca_topic_score_codex":0.0383372,"about_ca_topic_score_gemma":0.098689616,"teacher_disagreement_score":0.0383372,"about_ca_system_score_codex":0.0002813503,"about_ca_system_score_gemma":0.00020281535,"threshold_uncertainty_score":0.07622808},"labels":[],"label_agreement":null},{"id":"W4225163054","doi":"10.1029/2021gl096869","title":"Microphysical Characteristics of the Phase‐Locking VRW‐Induced Asymmetric Convection in the Outer Eyewall of Super Typhoon Lekima (2019)","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Graupel; Eye; Typhoon; Rainband; Convection; Tropical cyclone; Geology; Precipitation; Vortex; Atmospheric sciences; Meteorology; Climatology; Physics","score_opus":0.04119025583572221,"score_gpt":0.300520002352145,"score_spread":0.25932974651642277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225163054","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997788,0.000011951521,0.000022640237,0.0000042255338,7.8044894e-7,0.0000012108125,0.000084861684,0.0000022254071,0.00009315406],"genre_scores_gemma":[0.9996908,0.000009257586,0.000027051496,0.00000326631,0.0000019743723,0.0000020816888,0.00020498982,9.942435e-7,0.00005962023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999697,0.0000023059133,0.0000024411388,0.0000072543185,0.000004437344,0.000013903202],"domain_scores_gemma":[0.9998764,0.00001619495,0.000040941963,0.000007687427,0.00002027822,0.000038588496],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000072442206,0.00015864696,0.00014151292,0.0006027406,0.0002159173,0.00023583094,0.000092443785,0.00014969817,0.00046284415],"category_scores_gemma":[0.0001256871,0.00009090185,0.00017436784,0.00036995026,0.00016899935,0.00014593227,0.0002089353,0.00011611228,0.00007389992],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023816909,0.000046705103,0.90304375,0.000029192513,0.00006243822,0.00048588045,0.0003982529,0.0010140259,0.08988466,0.000070412854,0.00017569696,0.0045509436],"study_design_scores_gemma":[0.0000022241763,0.000011572404,0.9986457,9.660677e-7,0.0000045478123,0.000019299732,0.00006478083,0.00061593985,0.00057249545,0.0000048197826,0.00005566118,0.0000019402719],"about_ca_topic_score_codex":0.0109659415,"about_ca_topic_score_gemma":0.01663857,"teacher_disagreement_score":0.0109659415,"about_ca_system_score_codex":0.0002464137,"about_ca_system_score_gemma":0.00013931289,"threshold_uncertainty_score":0.021804214},"labels":[],"label_agreement":null},{"id":"W4225299090","doi":"10.1029/2022gl098541","title":"Identification of High δ<sup>18</sup>O Adakite‐Like Granites in SE Tibet: Implication for Diapiric Relamination of Subducted Sediments","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"","keywords":"Adakite; Geology; Subduction; Geochemistry; Crust; Continental crust; Oceanic crust; Sedimentary rock; Felsic; Earth science; Paleontology; Mafic; Tectonics","score_opus":0.031610267641898296,"score_gpt":0.28533205439383247,"score_spread":0.2537217867519342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225299090","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949217,0.000040041436,0.000040515864,0.000006674075,9.504305e-7,0.0000014512567,0.000031050815,0.000002753321,0.0003843228],"genre_scores_gemma":[0.9996865,0.00002580697,0.00007927953,0.000004305319,0.0000019049011,0.0000012343335,0.00006648977,0.0000012569369,0.0001331918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995315,0.0000049852424,0.000006684996,0.000015376307,0.000009109778,0.000010746211],"domain_scores_gemma":[0.9998627,0.000013929555,0.00006405151,0.00000969815,0.00002743694,0.000022318802],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001628988,0.00018943506,0.00012329931,0.0012404757,0.00043624168,0.00052371155,0.00019421481,0.00018473876,0.0011026915],"category_scores_gemma":[0.00017690346,0.000116735304,0.00009826661,0.0008002826,0.0005717708,0.00015682857,0.00038534714,0.00014411798,0.00014349146],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030117398,0.000024588791,0.8817957,0.000077606666,0.000042187094,0.00091303873,0.0012670886,0.00033850584,0.105834894,0.00020427689,0.000051791038,0.009149085],"study_design_scores_gemma":[0.0000058578407,0.00003217959,0.9973847,0.000004472943,0.000008867619,0.00029978534,0.0005287402,0.00015047495,0.0011393443,0.000057998546,0.00038515966,0.0000024877215],"about_ca_topic_score_codex":0.0054245815,"about_ca_topic_score_gemma":0.010186212,"teacher_disagreement_score":0.0054245815,"about_ca_system_score_codex":0.00022617738,"about_ca_system_score_gemma":0.00016678408,"threshold_uncertainty_score":0.0107860565},"labels":[],"label_agreement":null},{"id":"W4225303478","doi":"10.1029/2022gl098249","title":"Novel EMIC Wave Propagation Pathway Through Buchsbaum Resonance and Inter‐Hemispheric Wave Interference: Swarm Observations and Modeling","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Alberta","funders":"Canadian Space Agency; European Space Agency","keywords":"Emic and etic; Physics; Ionosphere; Van Allen Probes; Geophysics; Computational physics; Field line; Magnetosphere; Van Allen radiation belt; Wave propagation; Optics; Magnetic field; Quantum mechanics","score_opus":0.06542337780580039,"score_gpt":0.2863767041291838,"score_spread":0.22095332632338344,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225303478","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9756173,0.000085374944,0.019331176,0.0001071978,0.000008560923,0.000025412779,0.0002770499,0.00025215556,0.004295803],"genre_scores_gemma":[0.9976793,0.000033761364,0.0018086416,0.0000044610947,0.0000032868586,0.000009501086,0.00013309602,0.000018676492,0.00030938108],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999596,0.000008195557,0.0000019383865,0.000011791162,0.0000090643825,0.000009513352],"domain_scores_gemma":[0.9999306,0.000019914656,0.000016524622,0.000008919076,0.000010366576,0.0000135658465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001445974,0.0004037865,0.00017715446,0.0002998155,0.00025168518,0.00046913253,0.0004959017,0.0004317799,0.00083199464],"category_scores_gemma":[0.00025005607,0.00023363988,0.0004034373,0.00027143292,0.0003214485,0.00036966804,0.00022935707,0.00037777348,0.00010231838],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003228998,0.00017751168,0.1532135,0.00007238464,0.00010661762,0.000621241,0.00039614044,0.77489316,0.049719125,0.0038435715,0.0012898452,0.015344116],"study_design_scores_gemma":[0.00002532716,0.000018371018,0.021899449,0.0000030339522,0.000009779084,0.000030645457,0.000030747746,0.97616667,0.0012226473,0.00031667724,0.00026786438,0.000008703455],"about_ca_topic_score_codex":0.015582865,"about_ca_topic_score_gemma":0.010232257,"teacher_disagreement_score":0.015582865,"about_ca_system_score_codex":0.0005597939,"about_ca_system_score_gemma":0.00041189426,"threshold_uncertainty_score":0.030984342},"labels":[],"label_agreement":null},{"id":"W4225308706","doi":"10.1029/2021gl097191","title":"Cordilleran Ice Sheet Stability During the Last Deglaciation","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Tula Foundation; University of Northern British Columbia","funders":"Hakai Institute; National Geographic Society","keywords":"Deglaciation; Geology; Ice sheet; Oceanography; Antarctic ice sheet; Glacial period; Ice-sheet model; Physical geography; Cryosphere; Bedrock; Climatology; Ice shelf; Thinning; Sea ice; Geomorphology; Holocene; Geography","score_opus":0.03564418313519592,"score_gpt":0.27924029709094544,"score_spread":0.24359611395574954,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225308706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99612147,0.00032312612,0.000026737825,0.000068953384,0.00000504157,0.0000038694748,0.0010512025,0.000009291545,0.0023902045],"genre_scores_gemma":[0.99799216,0.00012975221,0.000053058484,0.000019611543,0.000006539017,0.000004181304,0.0010107844,0.000003337883,0.0007806023],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99983275,0.000015553607,0.000008932775,0.000049385533,0.000040094594,0.00005335533],"domain_scores_gemma":[0.9992275,0.00004312214,0.00020760525,0.000038558635,0.0003753739,0.00010779646],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000394648,0.0002773849,0.00019423537,0.0015804191,0.00089333666,0.0010950565,0.0003444878,0.00027689108,0.0015983043],"category_scores_gemma":[0.0011380066,0.00010215344,0.00012980883,0.0012505155,0.00037527774,0.00035042607,0.00063880166,0.0002185169,0.0002922392],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020725279,0.000017483077,0.98349416,0.000022363072,0.00005416441,0.00016619483,0.00078671676,0.00028566318,0.0013940872,0.00011214514,0.0006369605,0.012822911],"study_design_scores_gemma":[9.372003e-7,0.000005914285,0.9990758,0.000004187002,0.0000034825264,0.000016003863,0.000073644944,0.0000738225,0.00008170884,0.000006682521,0.00065653364,0.0000013685076],"about_ca_topic_score_codex":0.5728856,"about_ca_topic_score_gemma":0.72103417,"teacher_disagreement_score":0.5728856,"about_ca_system_score_codex":0.0035949755,"about_ca_system_score_gemma":0.0009770083,"threshold_uncertainty_score":0.8592596},"labels":[],"label_agreement":null},{"id":"W4225598432","doi":"10.1029/2021gl097595","title":"Increasing Multiyear Sea Ice Loss in the Beaufort Sea: A New Export Pathway for the Diminishing Multiyear Ice Cover of the Arctic Ocean","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Fisheries and Oceans Canada; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Meteorological and Oceanographic Society; Natural Environment Research Council; Canada Excellence Research Chairs, Government of Canada; Norges Forskningsråd; Sight Research UK","keywords":"Ocean gyre; Sea ice; Oceanography; Beaufort sea; Arctic sea ice decline; Arctic; Arctic ice pack; Beaufort scale; Climatology; Geology; Environmental science; Antarctic sea ice; Fishery","score_opus":0.03204652278216394,"score_gpt":0.27120759540094347,"score_spread":0.23916107261877953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225598432","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.982882,0.0010952043,0.0022325297,0.002866081,0.000063696025,0.00002040308,0.0014090543,0.000076235396,0.009354762],"genre_scores_gemma":[0.99586284,0.00034079913,0.00094327977,0.00019837191,0.000041280804,0.000007660251,0.0005913148,0.000026416537,0.0019878938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99977225,0.000033943365,0.000016874534,0.000064156426,0.000061190185,0.000051599298],"domain_scores_gemma":[0.9992613,0.00005848628,0.00033095322,0.00006696328,0.00018938191,0.00009292187],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005683705,0.00044591096,0.0002470903,0.00095928204,0.0007524936,0.0027493017,0.00054911635,0.000490584,0.0027425208],"category_scores_gemma":[0.0008479155,0.00017208191,0.00051820395,0.0009113763,0.00054504775,0.0014079671,0.0007495179,0.00058004697,0.00025305332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003087992,0.000054993343,0.92714113,0.00013610217,0.00020787986,0.00090309227,0.0011003028,0.00448879,0.011727539,0.0038117236,0.0034604508,0.04665912],"study_design_scores_gemma":[0.0000054802813,0.00004610248,0.983093,0.00003390952,0.00002952416,0.0003326604,0.0007096596,0.0041556642,0.0010983379,0.0008567638,0.009615319,0.000023576997],"about_ca_topic_score_codex":0.053259235,"about_ca_topic_score_gemma":0.067921154,"teacher_disagreement_score":0.053259235,"about_ca_system_score_codex":0.0015470078,"about_ca_system_score_gemma":0.001228817,"threshold_uncertainty_score":0.10589844},"labels":[],"label_agreement":null},{"id":"W4225660066","doi":"10.1029/2021gl096443","title":"Crustal Thickening of the Northern Central Andean Plateau Inferred From Trace Elements in Zircon","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Division of Earth Sciences; National Science Foundation","keywords":"Geology; Zircon; Neogene; Magmatism; Subduction; Thickening; Geochemistry; Cretaceous; Plateau (mathematics); Trace element; Paleontology; Tectonics; Structural basin","score_opus":0.02818411623953281,"score_gpt":0.25369914242604696,"score_spread":0.22551502618651414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4225660066","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980026,0.00032492742,0.00006907642,0.000016663587,0.0000016277457,0.0000023525533,0.00014182553,0.0000095047,0.0014312919],"genre_scores_gemma":[0.9994629,0.000120759585,0.0000681137,0.0000058559785,0.0000024938204,0.0000013668997,0.00014682255,0.0000017529895,0.00018987716],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999422,0.0000062232657,0.00000478631,0.000020349102,0.000011633833,0.000014799614],"domain_scores_gemma":[0.9998648,0.000016169422,0.000038828624,0.000011370059,0.000048413876,0.000020328054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029782043,0.00018398253,0.0001345358,0.0017634194,0.0003931661,0.0006389131,0.00015344135,0.00017169527,0.00088422763],"category_scores_gemma":[0.00037708445,0.00012432905,0.00013368923,0.0010507496,0.00033425025,0.00020229408,0.00041085776,0.000114185306,0.0001253906],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001491537,0.000014527573,0.9392119,0.000053021504,0.00008115125,0.0004763065,0.0012088706,0.00054367597,0.040548265,0.00020099767,0.00012739848,0.017384738],"study_design_scores_gemma":[0.0000018500816,0.000008637793,0.9984976,0.0000069584635,0.000008191273,0.000067741974,0.00021494976,0.00019326956,0.00052669906,0.000037564223,0.00043468073,0.0000018686453],"about_ca_topic_score_codex":0.04265087,"about_ca_topic_score_gemma":0.055745292,"teacher_disagreement_score":0.04265087,"about_ca_system_score_codex":0.00055619754,"about_ca_system_score_gemma":0.0002578928,"threshold_uncertainty_score":0.08480525},"labels":[],"label_agreement":null},{"id":"W4226173340","doi":"10.1029/2021gl097699","title":"The 2021 Pacific Northwest Heat Wave and Associated Blocking: Meteorology and the Role of an Upstream Cyclone as a Diabatic Source of Wave Activity","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":118,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Climatology; Cyclone (programming language); Cyclogenesis; Anticyclone; Diabatic; Atmospheric sciences; Troposphere; Tropical cyclone; Geology; Environmental science; Meteorology; Geography; Physics","score_opus":0.017144776566531347,"score_gpt":0.25665934680708125,"score_spread":0.2395145702405499,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226173340","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988563,0.000022604814,0.00009410825,0.00004308647,0.000002876803,0.000002333201,0.00017045274,0.0000036313377,0.0008046275],"genre_scores_gemma":[0.99956197,0.000025398715,0.00005913443,0.0000047633926,0.0000044703183,0.0000014294757,0.00019284539,0.0000010412557,0.00014887065],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99998045,0.000002758352,8.987586e-7,0.0000031946824,0.0000049662644,0.000007671967],"domain_scores_gemma":[0.99990976,0.000013677541,0.00002944052,0.0000055695373,0.000016130445,0.000025508598],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010611796,0.00010523672,0.00007880684,0.00016861256,0.0003000228,0.00044520738,0.00009990392,0.00014279467,0.0010845218],"category_scores_gemma":[0.00020924986,0.00005274072,0.000094963325,0.00016277474,0.00016935762,0.0001687924,0.00012988746,0.00022037972,0.00006570749],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028972604,0.00009599369,0.96663874,0.000020741905,0.00003524214,0.00029984745,0.00010044943,0.014527247,0.007587171,0.0014192889,0.0009834006,0.008002096],"study_design_scores_gemma":[0.000008897503,0.000028968572,0.97671574,0.0000045159723,0.000012930293,0.000040785864,0.00013276402,0.021219848,0.0010390913,0.00017627368,0.00061601115,0.0000041588887],"about_ca_topic_score_codex":0.03579245,"about_ca_topic_score_gemma":0.05272019,"teacher_disagreement_score":0.03579245,"about_ca_system_score_codex":0.00060382474,"about_ca_system_score_gemma":0.0003453954,"threshold_uncertainty_score":0.071168184},"labels":[],"label_agreement":null},{"id":"W4226176224","doi":"10.1029/2022gl098947","title":"Thank You to Our 2021 Peer Reviewers","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Environmental Engineering and Cultural Studies","field":"Computer Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Girton College, University of Cambridge","keywords":"Computer science; Peer review; Psychology; Information retrieval; World Wide Web; Biology","score_opus":0.03702850062822601,"score_gpt":0.3060681113854293,"score_spread":0.2690396107572033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4226176224","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0007034587,0.01365207,0.009623228,0.27771828,0.6715915,0.0014615312,0.0016016052,0.0041036885,0.019544676],"genre_scores_gemma":[0.008944841,0.020240612,0.033282287,0.24109513,0.42759413,0.005620221,0.0042760465,0.006992764,0.25195408],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.92933935,0.017250877,0.008204722,0.007326111,0.03499121,0.0028878185],"domain_scores_gemma":[0.3519075,0.02519429,0.01807457,0.016066374,0.54872674,0.040030643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.045435708,0.003259957,0.0045021563,0.007790658,0.0068719117,0.028849829,0.0047068065,0.011435661,0.11158197],"category_scores_gemma":[0.32434025,0.0020748156,0.0027432512,0.004882671,0.0035609608,0.010782843,0.006906071,0.012717737,0.23757412],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000020829495,0.000009852452,0.00014191448,0.0001472357,0.00000997754,0.00008070174,0.00009519768,0.000018221024,0.000099477875,0.00019839236,0.9804983,0.018679911],"study_design_scores_gemma":[0.000021600452,0.000017636721,0.00023637133,0.0002789396,0.000015718277,0.0003281334,0.00039240287,0.000087437795,0.00009477942,0.00071421335,0.99776685,0.000045870853],"about_ca_topic_score_codex":0.002494335,"about_ca_topic_score_gemma":0.0051205773,"teacher_disagreement_score":0.11158197,"about_ca_system_score_codex":0.0034205124,"about_ca_system_score_gemma":0.019376142,"threshold_uncertainty_score":0.37327886},"labels":[],"label_agreement":null},{"id":"W4229072242","doi":"10.1029/2021gl097623","title":"Southeastern Tibetan Plateau Growth Revealed by Inverse Analysis of Landscape Evolution Model","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Natural Science Foundation of China","keywords":"Plateau (mathematics); Cenozoic; Geology; Neogene; Fluvial; Paleogene; Paleontology; Erosion; Structural basin; Physical geography; Geomorphology; Geography","score_opus":0.028344172159971346,"score_gpt":0.2716851776110174,"score_spread":0.24334100545104606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229072242","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9772201,0.00008216822,0.016754813,0.00016869925,0.00001620476,0.000018827723,0.00043670795,0.0001866394,0.005115769],"genre_scores_gemma":[0.9956196,0.000040611507,0.0034719575,0.000017266097,0.000005323429,0.000026247379,0.00019294566,0.000025191115,0.0006007681],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999572,0.000012289122,0.000002247634,0.000012602406,0.0000054810184,0.000010203685],"domain_scores_gemma":[0.9998753,0.000055121538,0.000013815505,0.000014626843,0.000028481712,0.000012623614],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014397471,0.00032476513,0.00029268753,0.00039532824,0.00033161137,0.0005171583,0.0006373455,0.0006146497,0.0019430454],"category_scores_gemma":[0.0006613756,0.00024611878,0.0004965312,0.00035769638,0.0003153855,0.00023641989,0.00025940817,0.00036068304,0.00011545029],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000008823674,0.000012960477,0.0030127433,0.000008151619,0.00001263921,0.000044009616,0.000017956916,0.9944772,0.00073062425,0.0007179243,0.00008042805,0.00087655225],"study_design_scores_gemma":[0.0000044686876,0.0000025890367,0.00047392517,8.138077e-7,0.0000029438752,0.0000036685997,0.0000036414185,0.99928206,0.00004684308,0.00012181264,0.00005557578,0.0000017427452],"about_ca_topic_score_codex":0.04708426,"about_ca_topic_score_gemma":0.021117438,"teacher_disagreement_score":0.04708426,"about_ca_system_score_codex":0.0006784297,"about_ca_system_score_gemma":0.0007538685,"threshold_uncertainty_score":0.09362042},"labels":[],"label_agreement":null},{"id":"W4229440182","doi":"10.1029/2022gl098582","title":"Topographic Control on Ground Motions and Landslides From the 2015 Gorkha Earthquake","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":46,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration; UK Research and Innovation; National Science Foundation","keywords":"Landslide; Geology; Seismology; Terrain; Ridge; Landslide classification; Geomorphology; Cartography; Geography; Paleontology","score_opus":0.017936374977905827,"score_gpt":0.26735561391806967,"score_spread":0.24941923894016385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229440182","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994499,0.000010804036,0.00013076619,0.000012830282,8.0668804e-7,0.0000016066333,0.00004256436,0.000004996624,0.00034568118],"genre_scores_gemma":[0.9998565,0.0000061870205,0.000059094225,0.0000014666592,4.3093314e-7,0.0000012087696,0.000028486907,6.8812426e-7,0.000045832672],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999255,0.000017979313,0.000007640165,0.000015724576,0.000015192254,0.000018028708],"domain_scores_gemma":[0.99966097,0.00013678032,0.000101926256,0.000028737724,0.000038156937,0.000033504504],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018533616,0.00012227948,0.00017194315,0.00033869484,0.00027554642,0.00049627665,0.00016227017,0.00019718446,0.0010406123],"category_scores_gemma":[0.001053599,0.0001321585,0.00018397867,0.00030464146,0.00034942944,0.00024272944,0.00042158173,0.00020229469,0.0001181887],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022151375,0.0001594118,0.8809974,0.00009980436,0.00012039233,0.0004500854,0.0006369313,0.08201844,0.019652562,0.00083996623,0.00030829592,0.014495044],"study_design_scores_gemma":[0.000015315924,0.000078644254,0.9024955,0.000013392856,0.000030079345,0.00011401681,0.00048867153,0.09398692,0.002171952,0.00036567764,0.00021932383,0.000020525364],"about_ca_topic_score_codex":0.0093339905,"about_ca_topic_score_gemma":0.013285667,"teacher_disagreement_score":0.0093339905,"about_ca_system_score_codex":0.00037845096,"about_ca_system_score_gemma":0.00027387176,"threshold_uncertainty_score":0.018559337},"labels":[],"label_agreement":null},{"id":"W4229449457","doi":"10.1029/2022gl098511","title":"Rainbow of the Night: First Direct Observation of a SAR Arc Evolving Into STEVE","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Arc (geometry); Observatory; Geology; Plasma; Atmospheric sciences; Meteorology; Geophysics; Physics; Astrophysics","score_opus":0.01833187880891244,"score_gpt":0.2652688765862244,"score_spread":0.24693699777731196,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4229449457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99406224,0.00012005872,0.00041330844,0.00014402774,0.00003299978,0.000012837383,0.0004019125,0.000046395257,0.0047663976],"genre_scores_gemma":[0.9981147,0.00004163666,0.00057898636,0.00006172742,0.00001635299,0.0000034711163,0.00034009758,0.000010837649,0.0008322787],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999325,0.0000046352025,0.0000017664394,0.000021189886,0.0000216072,0.000018269437],"domain_scores_gemma":[0.9998634,0.000017429253,0.000015980915,0.00001608159,0.000036193793,0.000050853298],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001362912,0.00014032482,0.00021471691,0.00042712403,0.00067213277,0.0004827356,0.00022094717,0.00037104377,0.0010654371],"category_scores_gemma":[0.00027639364,0.00017670807,0.0001659834,0.0002346494,0.00031458458,0.00023695562,0.00050050474,0.00069580646,0.00029752954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010214254,0.00031507018,0.7079322,0.00012934365,0.00017993912,0.012619737,0.0056949835,0.0005784669,0.23342016,0.0006798387,0.006285409,0.031143427],"study_design_scores_gemma":[0.000011472375,0.00013300721,0.98463815,0.000021748478,0.000022770004,0.0017534005,0.001206472,0.0008556775,0.00431018,0.00009855201,0.00693528,0.000013267358],"about_ca_topic_score_codex":0.01204636,"about_ca_topic_score_gemma":0.044388,"teacher_disagreement_score":0.01204636,"about_ca_system_score_codex":0.00036457772,"about_ca_system_score_gemma":0.00023848303,"threshold_uncertainty_score":0.023952484},"labels":[],"label_agreement":null},{"id":"W4244658999","doi":"10.1029/2006gl026946","title":"Correction to “Recent changes in the fire regime across the North American boreal region‐Spatial and temporal patterns of burning across Canada and Alaska”","year":2006,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Boreal; Taiga; Climatology; Physical geography; Geography; Environmental science; Geology; Archaeology; Forestry","score_opus":0.011899096846876282,"score_gpt":0.2673427143453927,"score_spread":0.2554436174985164,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4244658999","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.00046367105,0.0011438802,0.0017124739,0.031112278,0.9562643,0.000020699981,0.0048356056,0.0007652886,0.003681664],"genre_scores_gemma":[0.058087904,0.011131617,0.017202746,0.055867415,0.38339546,0.00027535573,0.02799978,0.0048954985,0.44114423],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9961098,0.0004325467,0.00064161984,0.0005037455,0.0018984596,0.00041386782],"domain_scores_gemma":[0.9700631,0.003121662,0.0018968121,0.0018083883,0.021597574,0.0015123562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0029993837,0.002185834,0.0024054113,0.003084598,0.0035861863,0.0035286895,0.0044361507,0.00403433,0.09655187],"category_scores_gemma":[0.034690678,0.0014205736,0.0016776067,0.00386338,0.0015039794,0.002732892,0.0022565639,0.0075114374,0.03594974],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041029874,0.000006922749,0.00013466373,0.00012801964,0.000014421809,0.00010697451,0.00005018162,0.000079256286,0.00009396688,0.000545754,0.99363613,0.0051627136],"study_design_scores_gemma":[0.000052895077,0.000023011495,0.0028383054,0.00018347648,0.000039761057,0.00034038816,0.00013383814,0.00043035392,0.0005058051,0.0010169753,0.99438643,0.000048704835],"about_ca_topic_score_codex":0.05109848,"about_ca_topic_score_gemma":0.08149527,"teacher_disagreement_score":0.94890153,"about_ca_system_score_codex":0.0035376912,"about_ca_system_score_gemma":0.0060297316,"threshold_uncertainty_score":0.32299817},"labels":[],"label_agreement":null},{"id":"W4252925609","doi":"10.1029/2012gl053926","title":"Satellite constraints of Nitrogen Oxide (NOX) emissions from India based on OMI observations and WRF-Chem simulations","year":2012,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":47,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Dalhousie University; Department of Science and Technology, Ministry of Science and Technology, India; Indian Institute of Technology Madras; University Corporation for Atmospheric Research; National Science Foundation","keywords":"Ozone Monitoring Instrument; Emission inventory; NOx; Troposphere; Weather Research and Forecasting Model; Environmental science; Satellite; Nitrogen oxide; Atmospheric sciences; Meteorology; Atmospheric research; Tropospheric ozone; Climatology; Air quality index; Geography; Geology; Chemistry; Physics","score_opus":0.0559927826392532,"score_gpt":0.2946295883037136,"score_spread":0.2386368056644604,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4252925609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9813669,0.00006052959,0.007925064,0.000099058336,0.0000114289505,0.00003198379,0.004275717,0.00043230611,0.0057969703],"genre_scores_gemma":[0.9877687,0.000044491317,0.008338404,0.000028709757,0.000008684578,0.000034828772,0.0033101472,0.00011553692,0.0003504496],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998084,0.00003110564,0.000011208404,0.000050030445,0.000048079364,0.000051269762],"domain_scores_gemma":[0.99966705,0.00008231163,0.000054214743,0.00007607661,0.00008694298,0.000033362438],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003369046,0.0007098987,0.00048868114,0.0006363252,0.0005172892,0.00065519125,0.0011978624,0.00040021012,0.0010960266],"category_scores_gemma":[0.0009261793,0.00053586863,0.00097199925,0.0010698722,0.0003503606,0.00058209914,0.0006149937,0.00053298316,0.0002295809],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000092405986,0.00006454577,0.04632056,0.00004579836,0.00011306442,0.000089662506,0.00005913729,0.94299835,0.0047117705,0.00067428465,0.0005404849,0.0042899214],"study_design_scores_gemma":[0.00012921204,0.000038489874,0.08335529,0.00001738364,0.00010238294,0.000038230974,0.00007453832,0.9046154,0.009658937,0.000625118,0.0012828881,0.0000621893],"about_ca_topic_score_codex":0.1091484,"about_ca_topic_score_gemma":0.094598025,"teacher_disagreement_score":0.1091484,"about_ca_system_score_codex":0.0016233502,"about_ca_system_score_gemma":0.0013861813,"threshold_uncertainty_score":0.21702611},"labels":[],"label_agreement":null},{"id":"W4280496629","doi":"10.1029/2021gl097195","title":"Watching the Cryosphere Thaw: Seismic Monitoring of Permafrost Degradation Using Distributed Acoustic Sensing During a Controlled Heating Experiment","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BC Studies","funders":"Strategic Environmental Research and Development Program","keywords":"Permafrost; Geology; Seismometer; Passive seismic; Cryosphere; Environmental science; Climate change; Remote sensing; Seismology; Climatology; Oceanography","score_opus":0.0620239409680107,"score_gpt":0.3104343014230794,"score_spread":0.24841036045506867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280496629","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99844664,0.00000709086,0.0010284159,0.000013647215,0.000005043449,0.000021075406,0.00010488696,0.00002435772,0.00034881989],"genre_scores_gemma":[0.9987017,0.0000080032205,0.0009730369,0.000015196251,0.0000054753327,0.000034484783,0.00010214348,0.0000044914377,0.00015553039],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999132,0.000015149358,0.0000037493858,0.000024340097,0.000022852586,0.00002073553],"domain_scores_gemma":[0.99975795,0.000063587446,0.000038237213,0.000029743182,0.000047015084,0.00006354883],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000231307,0.00022868975,0.00016982495,0.00020198147,0.00036837236,0.00014864148,0.0002814874,0.0002748118,0.000804333],"category_scores_gemma":[0.00031115735,0.000089549874,0.00015435425,0.00011962093,0.00033467973,0.00014372864,0.00027021626,0.00037046394,0.00006262056],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019628403,0.00092199806,0.08480387,0.000047399488,0.00006314,0.0002012985,0.00052434916,0.0047422415,0.8906514,0.000104775754,0.0003439776,0.015632758],"study_design_scores_gemma":[0.00018297577,0.005935127,0.75833803,0.000012627651,0.00008256996,0.0001409362,0.0006464352,0.031541083,0.2014914,0.00019517739,0.0013938587,0.000039663777],"about_ca_topic_score_codex":0.0027892366,"about_ca_topic_score_gemma":0.006772949,"teacher_disagreement_score":0.0027892366,"about_ca_system_score_codex":0.00021972386,"about_ca_system_score_gemma":0.0002000413,"threshold_uncertainty_score":0.0055460334},"labels":[],"label_agreement":null},{"id":"W4280498689","doi":"10.1029/2021gl095748","title":"The Effect of Ocean Salinity on Climate and Its Implications for Earth's Habitability","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":71,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"National Aeronautics and Space Administration","keywords":"Oceanography; Environmental science; Climatology; Salinity; Habitability; Sea ice; Geology; Atmosphere (unit); Greenhouse gas; Early Earth; Climate change; Atmospheric sciences; Planet; Meteorology; Geography","score_opus":0.035737909154543536,"score_gpt":0.328265849547084,"score_spread":0.29252794039254043,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280498689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99526876,0.00011477845,0.00074911286,0.0003438464,0.000014273889,0.0000027462297,0.0002602512,0.000028095765,0.0032182613],"genre_scores_gemma":[0.9998258,0.000025606994,0.000035296052,0.000011141331,0.0000023065268,5.294656e-7,0.000033121516,0.000003618779,0.00006268132],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999144,0.000028214152,0.0000066147136,0.000017803914,0.000013360178,0.00001968747],"domain_scores_gemma":[0.9994235,0.00026913008,0.00009021239,0.000060524275,0.000060479444,0.000096113865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031205927,0.00018250577,0.00021779306,0.00030864688,0.0001823155,0.0008393755,0.00023287369,0.00040380092,0.0023273728],"category_scores_gemma":[0.0018186935,0.00013336277,0.00042145493,0.0002870746,0.000623873,0.00082081906,0.0008288587,0.00027646797,0.00019200878],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045376463,0.00007499919,0.72141856,0.00010357856,0.00025281517,0.0004696728,0.00014514216,0.21189578,0.041664653,0.008787582,0.0008401519,0.013893277],"study_design_scores_gemma":[0.00005161629,0.00014314456,0.81937414,0.000023780533,0.000061552084,0.00014016373,0.00032423515,0.16120832,0.004416264,0.013124127,0.0010714086,0.000061242106],"about_ca_topic_score_codex":0.005747426,"about_ca_topic_score_gemma":0.0024772577,"teacher_disagreement_score":0.005747426,"about_ca_system_score_codex":0.00038074324,"about_ca_system_score_gemma":0.00017104606,"threshold_uncertainty_score":0.011427939},"labels":[],"label_agreement":null},{"id":"W4280499099","doi":"10.1029/2022gl098485","title":"Variations in Vertical CO/CO<sub>2</sub> Profiles in the Martian Mesosphere and Lower Thermosphere Measured by the ExoMars TGO/NOMAD: Implications of Variations in Eddy Diffusion Coefficient","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Instituto de Astrofísica de Andalucía; Ministerio de Ciencia e Innovación; Canadian Space Agency; UK Space Agency; Belgian Federal Science Policy Office; Fonds De La Recherche Scientifique - FNRS; Japan Society for the Promotion of Science; Ministerio de Ciencia, Innovación y Universidades; National Aeronautics and Space Administration","keywords":"Eddy diffusion; Thermosphere; Martian; Atmospheric sciences; Mars Exploration Program; Southern Hemisphere; Mesosphere; Northern Hemisphere; Altitude (triangle); Latitude; Atmosphere of Mars; Diffusion; Geology; Nadir; Atmosphere (unit); Environmental science; Geophysics; Astrobiology; Physics; Climatology; Ionosphere; Geodesy; Stratosphere; Meteorology; Turbulence; Astronomy; Thermodynamics; Satellite","score_opus":0.021686618031827882,"score_gpt":0.27369731329913116,"score_spread":0.2520106952673033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280499099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993698,0.000016605358,0.00016271911,0.000010091186,8.789589e-7,0.0000011930379,0.00012742453,0.000011402742,0.00029998005],"genre_scores_gemma":[0.99971396,0.000007282904,0.000132575,0.0000027478616,7.681462e-7,9.627098e-7,0.000105938496,0.0000016143495,0.000034143774],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997604,0.0000028811978,0.00000130944,0.000007886171,0.00000581481,0.000006083404],"domain_scores_gemma":[0.9999434,0.000012598339,0.000012997161,0.0000044602475,0.000012154461,0.000014398351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008571001,0.00015972358,0.00007030158,0.00026624856,0.0001330021,0.0002272073,0.00011607341,0.0001838447,0.00033048936],"category_scores_gemma":[0.00017305254,0.000096567244,0.00011430436,0.00018773171,0.00011439466,0.00017258734,0.000104078164,0.00013346034,0.00007145757],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033816864,0.00005221671,0.8194015,0.000026343392,0.00008285093,0.00018540365,0.00021314182,0.004151653,0.1661319,0.00023249262,0.00022499256,0.008959415],"study_design_scores_gemma":[0.0000062123345,0.000013086829,0.9888474,0.000001749551,0.000009019226,0.000027659567,0.000040908923,0.005422364,0.0054251784,0.000021068072,0.00018185479,0.0000035498908],"about_ca_topic_score_codex":0.015198324,"about_ca_topic_score_gemma":0.01633618,"teacher_disagreement_score":0.015198324,"about_ca_system_score_codex":0.00025370147,"about_ca_system_score_gemma":0.000113053444,"threshold_uncertainty_score":0.030219734},"labels":[],"label_agreement":null},{"id":"W4280628596","doi":"10.1029/2022gl097978","title":"Nonlinear Wave Growth Analysis of Chorus Emissions Modulated by ULF Waves","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"China Postdoctoral Science Foundation","keywords":"Chorus; Physics; Substorm; Magnetosphere; Amplitude; Longitudinal wave; Nonlinear system; Geophysics; Computational physics; Magnetic field; Wave propagation; Optics","score_opus":0.01540600379445519,"score_gpt":0.2796030881105701,"score_spread":0.26419708431611494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280628596","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99374974,0.00009019753,0.0036352065,0.000028091168,0.0000033150866,0.00001008918,0.000106137355,0.000048204492,0.002329064],"genre_scores_gemma":[0.99885464,0.00003296352,0.00074338645,0.0000024251788,0.0000025617487,0.000005301434,0.00006923998,0.000007049954,0.00028226816],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994886,0.0000067240476,0.0000013624353,0.000010749651,0.000020700467,0.000011636053],"domain_scores_gemma":[0.9998229,0.0000631215,0.00004451605,0.000015223137,0.000033418208,0.000020904366],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000064876855,0.00015960832,0.00010650572,0.000731783,0.00015399628,0.00017819942,0.00017090504,0.00010165842,0.0008702269],"category_scores_gemma":[0.000284314,0.000096482196,0.00012548256,0.00032752776,0.00020956915,0.00017319698,0.00017520832,0.00020082179,0.000078464145],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043553484,0.000056558198,0.085890904,0.00011769196,0.000069893154,0.00090844184,0.00060403644,0.011753207,0.8716981,0.0029932258,0.0005040665,0.024968332],"study_design_scores_gemma":[0.000031974396,0.00012541568,0.5548807,0.000019482932,0.000035723668,0.00048262888,0.0003965479,0.3028343,0.1382167,0.0011237344,0.0018096814,0.000043077078],"about_ca_topic_score_codex":0.0043324027,"about_ca_topic_score_gemma":0.0031634474,"teacher_disagreement_score":0.0043324027,"about_ca_system_score_codex":0.0002458575,"about_ca_system_score_gemma":0.00007543062,"threshold_uncertainty_score":0.008614361},"labels":[],"label_agreement":null},{"id":"W4280640598","doi":"10.1029/2021gl097394","title":"Mechanism for the Uplift of Gongga Shan in the Southeastern Tibetan Plateau Constrained by 3D Magnetotelluric Data","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Magnetotellurics; Geology; Craton; Massif; Plateau (mathematics); Inversion (geology); Crust; Geomorphology; Electrical resistivity and conductivity; Tectonics; Seismology; Paleontology; Geophysics","score_opus":0.07343766844207361,"score_gpt":0.318446341471411,"score_spread":0.24500867302933738,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4280640598","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976101,0.00008111223,0.0011283329,0.00006997781,0.0000056566923,0.0000075186394,0.00021590687,0.00007171529,0.0008096755],"genre_scores_gemma":[0.9994351,0.000036688452,0.00025421553,0.000008013284,0.000003153359,0.0000035564567,0.00017137585,0.0000043325454,0.000083666135],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999907,0.000014845374,0.000008512162,0.000031741914,0.000016682206,0.000021295133],"domain_scores_gemma":[0.9998253,0.000025538258,0.000057853795,0.000024291858,0.000041258518,0.000025910931],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035134633,0.0003044658,0.00025600643,0.0013767069,0.0003538472,0.0007792135,0.00039663396,0.00029296475,0.0009609433],"category_scores_gemma":[0.0005920141,0.00026002177,0.00030523367,0.0011419985,0.00036224854,0.0003000574,0.00046929202,0.00017699761,0.000110585555],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014570203,0.000056994588,0.9203451,0.000062156345,0.00016891965,0.00091377593,0.00035879065,0.031513747,0.029311702,0.0014222345,0.00046060275,0.015240301],"study_design_scores_gemma":[0.000033580563,0.00002664245,0.9135573,0.000019463947,0.000050745573,0.00011368794,0.00024320061,0.083461635,0.0011459623,0.0007621359,0.0005606592,0.000025109071],"about_ca_topic_score_codex":0.01997961,"about_ca_topic_score_gemma":0.017230185,"teacher_disagreement_score":0.01997961,"about_ca_system_score_codex":0.0004974178,"about_ca_system_score_gemma":0.0005368597,"threshold_uncertainty_score":0.039726615},"labels":[],"label_agreement":null},{"id":"W4281253889","doi":"10.1029/2022gl099400","title":"A Deep Learning Approach to Extract Internal Tides Scattered by Geostrophic Turbulence","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Canadian Institute for Theoretical Astrophysics; University of Toronto; Autodesk (Canada)","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Agence Nationale de la Recherche","keywords":"Snapshot (computer storage); Turbulence; Geostrophic wind; Internal wave; Computer science; Data-driven; Generative grammar; Geology; Artificial intelligence; Meteorology; Physics; Oceanography","score_opus":0.020518496386747707,"score_gpt":0.25423212595399874,"score_spread":0.23371362956725103,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281253889","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.25729448,0.00031356857,0.7378948,0.0005411421,0.00006672638,0.00004207072,0.00028583166,0.0012209342,0.0023404397],"genre_scores_gemma":[0.92937833,0.00009702142,0.06716257,0.00013175144,0.000027560458,0.0000384343,0.00059426477,0.000060107453,0.0025099253],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991155,0.000019853162,0.000004553038,0.000024788798,0.000018445204,0.000020849631],"domain_scores_gemma":[0.99966896,0.00018335294,0.000037912258,0.000029301964,0.00005490169,0.000025616191],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047348344,0.0005906505,0.00029256588,0.000365536,0.00021927514,0.0003589128,0.0006812718,0.00054261094,0.0007574167],"category_scores_gemma":[0.0011964787,0.00035445695,0.0003959277,0.00033147956,0.000504924,0.0005016295,0.00086878863,0.0010215752,0.00018306784],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004129472,0.00004081109,0.001235459,0.000012626517,0.000033939614,0.000031304917,0.000020081363,0.96315855,0.0029676263,0.0016365707,0.0006062766,0.030215489],"study_design_scores_gemma":[9.327105e-7,0.0000039308816,0.00007757555,7.2919624e-7,9.170975e-7,0.0000013580335,0.0000010397995,0.99921167,0.0003477728,0.00031558244,0.000037631977,8.614899e-7],"about_ca_topic_score_codex":0.005382696,"about_ca_topic_score_gemma":0.007406911,"teacher_disagreement_score":0.005382696,"about_ca_system_score_codex":0.0005094614,"about_ca_system_score_gemma":0.0006233919,"threshold_uncertainty_score":0.010702729},"labels":[],"label_agreement":null},{"id":"W4281260407","doi":"10.1029/2022gl101452","title":"Computing the Ensemble Spread From Deterministic Weather Predictions Using Conditional Generative Adversarial Networks","year":2023,"lang":"en","type":"preprint","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Ensemble forecasting; Ensemble learning; Computer science; Statistical ensemble; Artificial intelligence; Machine learning; Canonical ensemble; Mathematics; Statistics; Monte Carlo method","score_opus":0.12958424667788232,"score_gpt":0.3373320464578761,"score_spread":0.2077477997799938,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281260407","genre_codex":"methods","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":"methods","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.36793563,0.00024100453,0.6269192,0.0006122584,0.00006437218,0.000027530235,0.00021299916,0.0009028457,0.0030841401],"genre_scores_gemma":[0.9816296,0.00004573908,0.017222779,0.000063142266,0.000020580232,0.00002174707,0.00015579334,0.00003779213,0.0008028526],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997861,0.00007150314,0.000009873198,0.000052232757,0.000045735218,0.000034574943],"domain_scores_gemma":[0.9977076,0.0017116752,0.00017769476,0.00013729208,0.00018275846,0.00008286159],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012192538,0.00061281445,0.0005984235,0.00049169094,0.0002684122,0.0006645851,0.0006564708,0.00079662894,0.0014698235],"category_scores_gemma":[0.0038155415,0.00045362505,0.0004202542,0.0003532082,0.0007510812,0.0010197646,0.0009073578,0.0012911434,0.00019921904],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000134348975,0.000005256106,0.00031225293,0.0000024605242,0.000007295878,0.0000059039658,0.0000038822645,0.9964665,0.00012762366,0.00083620654,0.000082315906,0.0021369436],"study_design_scores_gemma":[4.7360672e-7,0.0000012816658,0.000032688233,3.8763295e-7,4.940522e-7,4.5498297e-7,3.3877274e-7,0.999522,0.000057011024,0.00037719292,0.0000071306918,5.936847e-7],"about_ca_topic_score_codex":0.011200088,"about_ca_topic_score_gemma":0.008898628,"teacher_disagreement_score":0.011200088,"about_ca_system_score_codex":0.0009575266,"about_ca_system_score_gemma":0.00071760186,"threshold_uncertainty_score":0.022269845},"labels":[],"label_agreement":null},{"id":"W4281396306","doi":"10.1029/2021gl097389","title":"Detailed Seafloor Imagery of Turbidity Current Bedforms Reveals New Insight Into Fine‐Scale Near‐Bed Processes","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Geological Survey of Canada; Natural Resources Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Ministère de l'Économie, de l’Innovation et des Exportations du Québec; Université Laval","keywords":"Turbidity current; Bedform; Turbidite; Geology; Bathymetry; Current (fluid); Seafloor spreading; Geomorphology; Outcrop; Erosion; Flume; Flow (mathematics); Sedimentary depositional environment; Oceanography; Sediment transport; Sediment; Geometry; Structural basin","score_opus":0.042155027554723466,"score_gpt":0.2957816866847646,"score_spread":0.2536266591300412,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281396306","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9898679,0.000072298404,0.0032247668,0.000036492373,0.000004363217,0.000010769569,0.002545859,0.00022658276,0.0040110084],"genre_scores_gemma":[0.9910575,0.000080796155,0.004511967,0.000015776908,0.000006888485,0.000005507263,0.0030818952,0.000034682915,0.0012049268],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999678,0.0000026858213,0.00000121293,0.000008734404,0.000009707146,0.000009917937],"domain_scores_gemma":[0.99994254,0.0000064068877,0.000010442447,0.000010718095,0.000014949403,0.000014902955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000056460933,0.0001337679,0.0001209128,0.0007256109,0.00010385233,0.00031993203,0.00008868029,0.00010048617,0.0017797727],"category_scores_gemma":[0.00013195338,0.00009857783,0.000088851106,0.00040048602,0.00010610997,0.00017438663,0.0002741079,0.000101971345,0.00034567955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002776209,0.00018572844,0.46818346,0.000183744,0.00013448,0.00064119074,0.0013335351,0.015267527,0.31788552,0.0011924655,0.0050241007,0.18969058],"study_design_scores_gemma":[0.000006589343,0.000024760788,0.9771105,0.000011261319,0.000016792459,0.00014789059,0.0002585207,0.012775238,0.0054501332,0.00015100306,0.0040355283,0.00001191076],"about_ca_topic_score_codex":0.00737654,"about_ca_topic_score_gemma":0.026298957,"teacher_disagreement_score":0.00737654,"about_ca_system_score_codex":0.000094869385,"about_ca_system_score_gemma":0.0001746249,"threshold_uncertainty_score":0.014667213},"labels":[],"label_agreement":null},{"id":"W4281642889","doi":"10.1029/2022gl098062","title":"A Small CO<sub>2</sub> Leakage May Induce Seismicity on a Sub‐Seismic Fault in a Good‐Porosity Clastic Saline Aquifer","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":45,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Centennial College","funders":"","keywords":"Induced seismicity; Plume; Geology; Aquifer; Seismology; Fault (geology); Overpressure; Pore water pressure; Overburden; Petrology; Geotechnical engineering; Groundwater","score_opus":0.05224254457878158,"score_gpt":0.27903641660491996,"score_spread":0.22679387202613838,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281642889","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992878,0.000009442365,0.00035206063,0.000015122522,0.0000012255431,0.0000019041196,0.00004119216,0.000027182406,0.00026421642],"genre_scores_gemma":[0.99980897,0.0000043712225,0.000099933306,0.0000021287715,4.077333e-7,7.584912e-7,0.000025427098,0.0000015463617,0.00005655334],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.0000035846665,0.0000034324396,0.0000095642345,0.0000120715,0.00002097201],"domain_scores_gemma":[0.9998667,0.000023995743,0.00005329489,0.000013599927,0.000019487648,0.00002293396],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000860059,0.00013716512,0.00012408507,0.00019788907,0.00020175242,0.00027356253,0.00016994141,0.0002196273,0.0010421467],"category_scores_gemma":[0.00023995187,0.00008841861,0.00009177729,0.00018645248,0.00028473532,0.00023273852,0.00023795404,0.0001276424,0.00008343038],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008123244,0.00012684843,0.32514623,0.00009046172,0.00006016833,0.0020042697,0.00038271392,0.022019759,0.6293291,0.0005836903,0.0005628444,0.018881563],"study_design_scores_gemma":[0.000024226863,0.00043925134,0.76709193,0.000011153112,0.000050076247,0.0005645911,0.0006804215,0.073485896,0.15571372,0.00043414134,0.0014737807,0.000030753115],"about_ca_topic_score_codex":0.0037400739,"about_ca_topic_score_gemma":0.0054497784,"teacher_disagreement_score":0.0037400739,"about_ca_system_score_codex":0.0003329374,"about_ca_system_score_gemma":0.00021066499,"threshold_uncertainty_score":0.007436633},"labels":[],"label_agreement":null},{"id":"W4281705659","doi":"10.1029/2022gl098825","title":"Two Sources of Deep Decadal Variability in the Central Labrador Sea Open‐Ocean Convection Region","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Geology; Oceanography; Climatology; Thermohaline circulation; Ocean current; Deep convection; Convective mixing; Convection; Geography; Meteorology","score_opus":0.025225120184225923,"score_gpt":0.27602259973694426,"score_spread":0.25079747955271836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281705659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858934,0.00007587004,0.0005986874,0.000041485626,0.0000041203803,0.0000014357099,0.00032478874,0.000059880073,0.00030428352],"genre_scores_gemma":[0.9995536,0.000012055495,0.000093695395,0.000004967683,0.0000026140478,0.0000015394052,0.0002310694,0.000005901801,0.00009446882],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998982,0.000022681541,0.000007699797,0.00003679991,0.000010493295,0.000024097631],"domain_scores_gemma":[0.9995875,0.00009122262,0.00014092434,0.00006877122,0.000065775836,0.000045825498],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045079464,0.0001987917,0.00019360967,0.0005673116,0.00018281353,0.00059748656,0.00026319892,0.00016695196,0.0006613882],"category_scores_gemma":[0.0008555403,0.00012298556,0.00028878343,0.0004980222,0.00016790663,0.00020587545,0.00046554045,0.00025007682,0.00012505983],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024463283,0.00005253722,0.9459886,0.00002703327,0.0002733098,0.00014101317,0.00022785594,0.015368591,0.014607814,0.00048604075,0.00071053003,0.021871887],"study_design_scores_gemma":[0.000008320847,0.000018603761,0.9732684,0.000007724017,0.000033750923,0.00004514194,0.00007916977,0.02436188,0.0015031443,0.00013235676,0.00052759395,0.000014079492],"about_ca_topic_score_codex":0.0142081855,"about_ca_topic_score_gemma":0.015917284,"teacher_disagreement_score":0.0142081855,"about_ca_system_score_codex":0.00029211995,"about_ca_system_score_gemma":0.00017373785,"threshold_uncertainty_score":0.028250992},"labels":[],"label_agreement":null},{"id":"W4281716394","doi":"10.1029/2022gl097973","title":"Long‐Term Trends in pCO<sub>2</sub> in Lake Surface Water Following Rebrowning","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; Canadian Forest Service; Ministry of the Environment, Conservation and Parks; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Dissolved organic carbon; Boreal; Environmental science; Surface water; Acid deposition; Deposition (geology); Period (music); Hydrology (agriculture); Environmental chemistry; Oceanography; Ecology; Chemistry; Geology; Biology; Soil science; Sediment","score_opus":0.025107198270004547,"score_gpt":0.2603898632158272,"score_spread":0.23528266494582264,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281716394","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930954,0.00002505479,0.000026423035,0.00003292985,0.0000018556908,0.0000032337534,0.00028325766,0.000002428353,0.00031524186],"genre_scores_gemma":[0.99911815,0.000023653134,0.000028531507,0.000021965172,0.000002022017,0.0000039376278,0.00041479818,0.0000010211476,0.00038593725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990857,0.0000064511637,0.000004894825,0.00001898871,0.000029521203,0.000031584277],"domain_scores_gemma":[0.9994894,0.000025028012,0.00014084684,0.000017689374,0.0002270844,0.000099857076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001824621,0.00012863848,0.00021607011,0.00026477448,0.00061598595,0.00051209994,0.00015965308,0.00028417798,0.0008012544],"category_scores_gemma":[0.00045095352,0.000110298046,0.00018078678,0.00049021514,0.00042998348,0.00025013904,0.0003435934,0.000246246,0.0001393679],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029967964,0.00002973238,0.98398143,0.000012845772,0.000046562505,0.000100168945,0.0006252463,0.00017203066,0.012509996,0.000021018051,0.00027975574,0.0019215086],"study_design_scores_gemma":[7.109221e-7,0.000016069545,0.99937373,7.2813384e-7,0.0000037931197,0.000004847894,0.00015527062,0.00005651837,0.00024532113,0.0000030211925,0.00013889425,0.0000011620508],"about_ca_topic_score_codex":0.4343291,"about_ca_topic_score_gemma":0.6151474,"teacher_disagreement_score":0.4343291,"about_ca_system_score_codex":0.002256053,"about_ca_system_score_gemma":0.0011721981,"threshold_uncertainty_score":0.86360204},"labels":[],"label_agreement":null},{"id":"W4281727444","doi":"10.1029/2022gl098821","title":"Planet‐Wide Ozone Destruction in the Middle Atmosphere on Mars During Global Dust Storm","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Belgian Federal Science Policy Office","keywords":"Dust storm; Atmosphere (unit); Mars Exploration Program; Atmosphere of Mars; Storm; Atmospheric sciences; Occultation; Astrobiology; Water vapor; Orbiter; Environmental science; Martian; Trace gas; Middle latitudes; Ozone; Radio occultation; Geology; Meteorology; Ionosphere; Physics; Geophysics; Astronomy","score_opus":0.04197810303840156,"score_gpt":0.2743708152718672,"score_spread":0.23239271223346564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281727444","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99879265,0.000028492632,0.00021198748,0.000063578234,0.000007777449,0.0000048729157,0.00017890813,0.000033955603,0.00067782705],"genre_scores_gemma":[0.99957746,0.000015139664,0.00014132832,0.000012414606,0.0000025089068,0.000004015382,0.00013507574,0.0000059085537,0.00010604259],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99988973,0.00002329872,0.000004197829,0.000019485162,0.0000121104795,0.0000511333],"domain_scores_gemma":[0.9998332,0.000052551306,0.000024384197,0.00001647163,0.000018503695,0.00005475676],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002505398,0.0005424949,0.00048260586,0.00028492892,0.0005556928,0.00074152777,0.00052457786,0.0009594063,0.0013140717],"category_scores_gemma":[0.00042075125,0.00026688722,0.0008865441,0.00022438898,0.00041153686,0.00046224432,0.0005903184,0.00045757342,0.000094033116],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005591897,0.000267735,0.11443425,0.00004101618,0.0002454839,0.0005502254,0.0001519862,0.86908245,0.010864503,0.00076985004,0.00065907417,0.0023743159],"study_design_scores_gemma":[0.00029513147,0.00030069106,0.066415146,0.000009628263,0.00008261453,0.00005316672,0.00022539994,0.92808646,0.003360745,0.00039946675,0.0007405187,0.000031018943],"about_ca_topic_score_codex":0.03728198,"about_ca_topic_score_gemma":0.013643815,"teacher_disagreement_score":0.03728198,"about_ca_system_score_codex":0.0009790512,"about_ca_system_score_gemma":0.0004511506,"threshold_uncertainty_score":0.07413},"labels":[],"label_agreement":null},{"id":"W4281751372","doi":"10.1029/2021gl097492","title":"Biogeochemical Distinctiveness of Peatland Ponds, Thermokarst Waterbodies, and Lakes","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":39,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Université de Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Natural Environment Research Council; Sight Research UK","keywords":"Biogeochemical cycle; Thermokarst; Peat; Environmental science; Biogeochemistry; Ecosystem; Lake ecosystem; Dissolved organic carbon; Freshwater ecosystem; Carbon cycle; Ecology; Hydrology (agriculture); Environmental chemistry; Permafrost; Geology; Chemistry; Biology","score_opus":0.02173678172195421,"score_gpt":0.24414510793649874,"score_spread":0.22240832621454454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281751372","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999134,0.00005474848,0.00007076884,0.0000054963834,5.1289095e-7,0.0000023356934,0.00021760658,0.000003663148,0.0005110148],"genre_scores_gemma":[0.9995197,0.000034921988,0.000113641894,0.0000069075845,0.0000010399335,0.0000027726537,0.00024832445,0.000002486785,0.00007017986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99985254,0.000026019254,0.000017245256,0.00004849831,0.000027281678,0.000028400724],"domain_scores_gemma":[0.9995497,0.000078704936,0.00018229999,0.000046545294,0.000075213306,0.0000675169],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002297609,0.000120297074,0.00022855765,0.0015699166,0.0003173466,0.00075176725,0.00014334131,0.00012571456,0.00094807736],"category_scores_gemma":[0.00050939707,0.00010018507,0.00023244445,0.0013366452,0.00061355927,0.000352507,0.00067089696,0.00009488992,0.00010721055],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000085947664,0.000016081925,0.9780241,0.000054160937,0.00010601376,0.00006416099,0.0003740872,0.00034115236,0.013578117,0.00016460118,0.000059105,0.007132403],"study_design_scores_gemma":[0.0000018321911,0.00001102786,0.9988745,0.0000039045717,0.000012103906,0.000024026747,0.00018762967,0.00023227224,0.00042336504,0.00006338275,0.00016365931,0.0000024204674],"about_ca_topic_score_codex":0.010568204,"about_ca_topic_score_gemma":0.025906716,"teacher_disagreement_score":0.010568204,"about_ca_system_score_codex":0.0003910077,"about_ca_system_score_gemma":0.00032136883,"threshold_uncertainty_score":0.02101338},"labels":[],"label_agreement":null},{"id":"W4281781554","doi":"10.1029/2022gl098720","title":"Mixed Layer Depth Promotes Trophic Amplification on a Seasonal Scale","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"China Scholarship Council; Bundesministerium für Bildung und Forschung; University of Victoria","keywords":"Upwelling; Trophic level; Phytoplankton; Mixed layer; Environmental science; Zooplankton; Biogeochemical cycle; Productivity; Oceanography; Atmospheric sciences; Ecology; Biology; Nutrient; Geology","score_opus":0.05597350817326295,"score_gpt":0.273680203108409,"score_spread":0.21770669493514605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281781554","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986526,0.000045271914,0.00026012093,0.000038265083,0.0000033635736,0.0000019432148,0.00004331435,0.000016445087,0.0009386756],"genre_scores_gemma":[0.9997887,0.000012403383,0.000047721198,0.00000963316,9.094595e-7,6.4892583e-7,0.000010871325,0.0000019131614,0.0001271357],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996173,0.0000067654682,0.0000022974657,0.000008854754,0.0000072822636,0.00001309277],"domain_scores_gemma":[0.9997706,0.00007317246,0.00006251619,0.000021233502,0.000025570735,0.00004683131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010858439,0.00014924863,0.00010847138,0.00014541416,0.00014951485,0.00049947196,0.00011727364,0.00016342777,0.0029088184],"category_scores_gemma":[0.0005502391,0.000132397,0.00016967086,0.00008798242,0.00013616144,0.000256532,0.0004988884,0.00017474899,0.00015799419],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011448204,0.00041706642,0.4631852,0.000253748,0.00042541887,0.00070991006,0.0004449557,0.051459122,0.4419789,0.0025956312,0.0016340128,0.035751287],"study_design_scores_gemma":[0.0000359263,0.0003455284,0.9007135,0.000036471047,0.00012878593,0.00011355687,0.00034423824,0.08236079,0.012651529,0.0018345065,0.0014087404,0.000026489282],"about_ca_topic_score_codex":0.0029039613,"about_ca_topic_score_gemma":0.00422103,"teacher_disagreement_score":0.0029088184,"about_ca_system_score_codex":0.00029750427,"about_ca_system_score_gemma":0.00017506153,"threshold_uncertainty_score":0.009730995},"labels":[],"label_agreement":null},{"id":"W4281864981","doi":"10.1029/2021gl097618","title":"Krypton‐81 Dating Constrains Timing of Deep Groundwater Flow Activation","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Natural Science Foundation of China; Canadian Institute for Advanced Research; W. M. Keck Foundation","keywords":"Evaporite; Geology; Meteoric water; Groundwater recharge; Aquifer; Geochemistry; Groundwater; Denudation; Geomorphology; Paleontology; Structural basin; Tectonics","score_opus":0.055244376155943714,"score_gpt":0.304844053584271,"score_spread":0.2495996774283273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4281864981","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99733114,0.00013367557,0.0005520332,0.000013345107,0.000001525025,0.0000018298207,0.00014547189,0.000010850312,0.0018101489],"genre_scores_gemma":[0.9992574,0.000049483097,0.00020594591,0.0000037161585,8.875185e-7,0.0000013331187,0.00015001472,0.000004383543,0.00032688852],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993503,0.000005682168,0.000002756044,0.000029945535,0.000011027879,0.000015475682],"domain_scores_gemma":[0.9998567,0.000022308963,0.00003294656,0.000015283527,0.000060562983,0.000012228454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013392081,0.00009083998,0.00011219119,0.00041262954,0.0002642633,0.00041327256,0.00015970133,0.00021012417,0.0010613146],"category_scores_gemma":[0.00036079,0.00013598407,0.000047849135,0.0002685041,0.00022363738,0.00030635725,0.00026613715,0.00013677173,0.00017235219],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018924887,0.000016199614,0.69264823,0.000044729335,0.000029436673,0.00016279753,0.0005334633,0.0022067095,0.28205755,0.00090875285,0.0003845537,0.020818312],"study_design_scores_gemma":[0.0000036316155,0.000024659541,0.9787394,0.000008398048,0.000010661886,0.00011007199,0.00015552378,0.003134982,0.015084409,0.00011526505,0.0026070795,0.000005898596],"about_ca_topic_score_codex":0.03114131,"about_ca_topic_score_gemma":0.072212435,"teacher_disagreement_score":0.03114131,"about_ca_system_score_codex":0.0005117567,"about_ca_system_score_gemma":0.00023081308,"threshold_uncertainty_score":0.061920106},"labels":[],"label_agreement":null},{"id":"W4282964610","doi":"10.1029/2022gl097945","title":"Burn Severity in Canada's Mountain National Parks: Patterns, Drivers, and Predictions","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Banff Centre; Parks Canada; Canadian Forest Service; University of British Columbia; Natural Resources Canada","funders":"","keywords":"Vegetation (pathology); Environmental science; Physical geography; Fire regime; National park; Scale (ratio); Geography; Climatology; Ecology; Ecosystem; Geology; Archaeology; Medicine; Cartography","score_opus":0.011342563186224165,"score_gpt":0.24872888128895795,"score_spread":0.23738631810273378,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4282964610","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980824,0.00008572882,0.00018157171,0.00008432835,0.0000017769727,0.0000063580997,0.0009768286,0.000012991965,0.0005679925],"genre_scores_gemma":[0.9991098,0.00004797567,0.000106539424,0.000006191133,0.0000010164995,0.0000024822568,0.000539629,0.0000017971523,0.00018445299],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998461,0.000015180186,0.000005763903,0.000030391848,0.00003487421,0.000067697096],"domain_scores_gemma":[0.9993395,0.00011054232,0.00010340641,0.000024618326,0.00023570828,0.00018618109],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036044535,0.00025259508,0.00017816544,0.0007900824,0.000609702,0.00081175804,0.00047628113,0.0002272866,0.0013389451],"category_scores_gemma":[0.0009816305,0.00014036363,0.00034852137,0.0010202869,0.00028704776,0.00027804685,0.00035129022,0.0002932979,0.00010824664],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000033895416,0.00001802197,0.9901383,0.000010142795,0.000035255,0.000034763412,0.00011160454,0.0062121963,0.00015478095,0.00014828041,0.00047401423,0.0026287066],"study_design_scores_gemma":[0.0000023209068,0.0000052121886,0.984536,0.000008638533,0.000008271585,0.000014315372,0.0004256755,0.014578637,0.000047446953,0.00008177686,0.0002862673,0.000005332104],"about_ca_topic_score_codex":0.9549653,"about_ca_topic_score_gemma":0.9748463,"teacher_disagreement_score":0.045034707,"about_ca_system_score_codex":0.0067309034,"about_ca_system_score_gemma":0.005298453,"threshold_uncertainty_score":0.090599775},"labels":[],"label_agreement":null},{"id":"W4283123382","doi":"10.1029/2022gl098487","title":"Amplification of Plunging Flows in Bedrock Canyons","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Canadian Hydrographic Service; University of Ottawa; University of Victoria; Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; National Geographic Society","keywords":"Bedrock; Geology; Erosion; Canyon; River morphology; Flood myth; Hydraulics; Hydrology (agriculture); Geomorphology; Sediment transport; Discharge; Floodplain; Bed load; Sediment; Hydraulic jump; Overbank; Flow (mathematics); Fluvial; Mechanics; Geotechnical engineering; Drainage basin","score_opus":0.025903918566870573,"score_gpt":0.2936078957081492,"score_spread":0.26770397714127864,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283123382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926263,0.000023284463,0.0002254965,0.000009407459,9.481836e-7,0.0000017663573,0.000035951325,0.00002482742,0.00041559373],"genre_scores_gemma":[0.99960583,0.000012313353,0.00016292541,0.000004700589,8.7349355e-7,0.0000017821917,0.000049022525,0.0000029139535,0.00015965398],"study_design_codex":"observational","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992716,0.000010126805,0.000003337893,0.00002927523,0.000010181625,0.000019942392],"domain_scores_gemma":[0.999673,0.00011082245,0.00007041073,0.00002534008,0.00004865687,0.00007173868],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016710453,0.00019695896,0.00020264101,0.00068819145,0.00027433224,0.00052354904,0.00018650369,0.00022387931,0.0018024473],"category_scores_gemma":[0.0005819158,0.00022339252,0.00014267108,0.00035873867,0.00033363674,0.00022171321,0.0004960877,0.00024268871,0.0001504371],"study_design_candidate":"bench_or_experimental","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005540468,0.00012784834,0.80751234,0.00018361976,0.0001297781,0.0012312769,0.0017311373,0.014501388,0.119779594,0.002229651,0.0010057213,0.05101364],"study_design_scores_gemma":[0.000014955923,0.00008230654,0.9863685,0.000013377692,0.000021390095,0.00015791549,0.00032195164,0.009874342,0.001943527,0.00064192875,0.00054574735,0.0000141171595],"about_ca_topic_score_codex":0.0035456442,"about_ca_topic_score_gemma":0.005938935,"teacher_disagreement_score":0.0035456442,"about_ca_system_score_codex":0.0003754663,"about_ca_system_score_gemma":0.00020440182,"threshold_uncertainty_score":0.0070500374},"labels":[],"label_agreement":null},{"id":"W4283372564","doi":"10.1029/2022gl099140","title":"India (Tethyan Himalaya Series) in Central Myanmar: Implications for the Evolution of the Eastern Himalayan Syntaxis and the Sagaing Transform‐Fault System","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Deutsche Forschungsgemeinschaft","keywords":"Geology; Subduction; Fibrous joint; Tectonics; Ordovician; Ophiolite; Fault (geology); Plate tectonics; Seismology; Paleontology; Collision zone","score_opus":0.016909074399825485,"score_gpt":0.23755017452724406,"score_spread":0.22064110012741858,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283372564","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99884725,0.00011723232,0.000026665466,0.00006819514,0.0000010288883,0.000002758239,0.00009168043,0.0000035360194,0.00084161345],"genre_scores_gemma":[0.999668,0.0000613333,0.000035788846,0.000009131288,0.0000016843022,0.0000028072413,0.00007428241,0.000001424854,0.00014549312],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992406,0.000013329965,0.000005491023,0.000022872435,0.000007027138,0.000027187476],"domain_scores_gemma":[0.99987376,0.000014182494,0.00006202746,0.000011211576,0.000019042054,0.000019770468],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015222799,0.00014284806,0.0000971443,0.00079108094,0.0005222858,0.00056995923,0.00025607136,0.00015777079,0.001747127],"category_scores_gemma":[0.00033476207,0.00012596295,0.00013903872,0.0009771427,0.00043954054,0.00035025142,0.00069686864,0.00017975048,0.00016856528],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000110199355,0.000038582697,0.9485386,0.00008243025,0.000104135936,0.0012979019,0.006367952,0.0009146718,0.01698955,0.0014652234,0.00038214016,0.02370867],"study_design_scores_gemma":[0.0000023221369,0.000010916096,0.99802005,0.000008251972,0.000010132651,0.00012795789,0.0009658543,0.00017001889,0.00014663942,0.000036389378,0.0004991848,0.0000023692064],"about_ca_topic_score_codex":0.029825004,"about_ca_topic_score_gemma":0.060770962,"teacher_disagreement_score":0.029825004,"about_ca_system_score_codex":0.00066358317,"about_ca_system_score_gemma":0.0004361714,"threshold_uncertainty_score":0.059302807},"labels":[],"label_agreement":null},{"id":"W4283383689","doi":"10.1029/2022gl099230","title":"Rapid Growth of Outer Size of Tropical Cyclones: A New Perspective on Their Destructive Potential","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Fundamental Research Funds for the Central Universities; National Outstanding Youth Science Fund Project of National Natural Science Foundation of China; National Natural Science Foundation of China","keywords":"Tropical cyclone; RADIUS; Growth rate; Environmental science; Atmospheric sciences; Climatology; Meteorology; Physics; Geology; Mathematics; Computer science; Geometry","score_opus":0.02646447577729158,"score_gpt":0.27297104973298913,"score_spread":0.24650657395569756,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283383689","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96912247,0.003609402,0.008296219,0.00049865566,0.000059142018,0.00001887626,0.0006634918,0.000058303674,0.017673401],"genre_scores_gemma":[0.9977531,0.00068478385,0.0009070498,0.000026110329,0.000099432655,0.0000039969,0.000113251,0.000011090214,0.0004011451],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987316,0.000023457698,0.000009853082,0.000035794208,0.000029867108,0.000027732045],"domain_scores_gemma":[0.9980307,0.00064510346,0.0006183573,0.00012469375,0.0002683583,0.00031277887],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036665355,0.00028845185,0.00016183179,0.0021704321,0.0002986837,0.0010945915,0.00021183689,0.00019371364,0.0012477112],"category_scores_gemma":[0.0015350818,0.00009072321,0.00014925619,0.00085243303,0.0009967706,0.0012831155,0.00073140755,0.00046527627,0.00010492549],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034455117,0.000066478504,0.8351669,0.00028861198,0.00008138315,0.0011147243,0.0026649171,0.011213324,0.038890205,0.026757134,0.0015595033,0.081852354],"study_design_scores_gemma":[0.0000065986187,0.00015159955,0.9600775,0.00007646028,0.000043200635,0.0012525322,0.0019395732,0.012646286,0.003939246,0.010756952,0.009069636,0.000040477447],"about_ca_topic_score_codex":0.002643812,"about_ca_topic_score_gemma":0.0025023073,"teacher_disagreement_score":0.002643812,"about_ca_system_score_codex":0.00042089526,"about_ca_system_score_gemma":0.00015148328,"threshold_uncertainty_score":0.0052568913},"labels":[],"label_agreement":null},{"id":"W4283527791","doi":"10.1029/2022gl099371","title":"Annual Mean Arctic Amplification 1970–2020: Observed and Simulated by CMIP6 Climate Models","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":220,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Los Alamos National Laboratory; National Oceanic and Atmospheric Administration","keywords":"Climatology; Surface air temperature; Environmental science; Forcing (mathematics); Arctic; Climate change; Arctic oscillation; Climate model; The arctic; Atmospheric sciences; Geology; Oceanography","score_opus":0.04004774462901935,"score_gpt":0.26862159751591963,"score_spread":0.2285738528869003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4283527791","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.988861,0.00020009495,0.00052645046,0.00017429188,0.000031592266,0.0000081340495,0.007401675,0.00020510454,0.002591594],"genre_scores_gemma":[0.9944172,0.00008708245,0.0002770506,0.000021249205,0.000014800804,0.0000092438395,0.0049790316,0.00002240059,0.00017192852],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998603,0.000030329766,0.00000852886,0.00004318238,0.0000252885,0.000032313128],"domain_scores_gemma":[0.999629,0.000084059895,0.00007081105,0.000041382893,0.00010343203,0.00007128726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074931607,0.00082612573,0.00029780055,0.0007070323,0.00032926726,0.00069781987,0.00047608046,0.0007136675,0.0013576858],"category_scores_gemma":[0.0011404152,0.00030240373,0.00072162226,0.0011341311,0.00029538598,0.0005749045,0.0002787904,0.00045773527,0.0005107175],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007397887,0.00018787934,0.31400228,0.00014487017,0.00037306413,0.00026763577,0.00014156663,0.66322994,0.0025236176,0.0010520921,0.008983269,0.008353993],"study_design_scores_gemma":[0.00020325155,0.00012969735,0.3053634,0.00005503129,0.00014294314,0.00017075488,0.0001487437,0.6851324,0.0028487686,0.0008153302,0.0049093175,0.00008045086],"about_ca_topic_score_codex":0.05026975,"about_ca_topic_score_gemma":0.030693905,"teacher_disagreement_score":0.05026975,"about_ca_system_score_codex":0.0011513524,"about_ca_system_score_gemma":0.00051563955,"threshold_uncertainty_score":0.09995431},"labels":[],"label_agreement":null},{"id":"W4285800833","doi":"10.1029/2021gl097525","title":"The Influence of the Solid Earth on the Contribution of Marine Sections of the Antarctic Ice Sheet to Future Sea‐Level Change","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; National Science Foundation","keywords":"Geology; Antarctic ice sheet; Ice sheet; Solid earth; Climate change; Ice-sheet model; Climatology; Sea ice; Climate model; Oceanography; Geophysics; Arctic ice pack; Drift ice; Cryosphere","score_opus":0.04622259962121307,"score_gpt":0.2787721345653246,"score_spread":0.23254953494411157,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285800833","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968497,0.000053824533,0.0007832182,0.00023488257,0.000008800652,0.0000025225497,0.00030935678,0.000019400666,0.0017383416],"genre_scores_gemma":[0.999595,0.000047635294,0.00009828857,0.000011490829,0.000003208908,0.0000016660571,0.00010512573,0.0000051067723,0.00013249692],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998853,0.00004547891,0.000005798832,0.00001515408,0.000022601616,0.000025496449],"domain_scores_gemma":[0.9996032,0.00018507213,0.00005950362,0.000035124453,0.000057117595,0.000060052847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003829419,0.000419102,0.00015489387,0.00033100555,0.00034071214,0.000964407,0.000263154,0.00044669738,0.0014528455],"category_scores_gemma":[0.001320242,0.00027358366,0.00056104676,0.00029894296,0.00048203047,0.0005640228,0.000521821,0.00035824362,0.00015760644],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022420395,0.00004869367,0.22495063,0.000037881382,0.00022301081,0.00030125317,0.0000854488,0.75434786,0.008624005,0.0027238766,0.00056679983,0.007866258],"study_design_scores_gemma":[0.000041962325,0.00012270904,0.24020769,0.000023933273,0.00014477728,0.00011470587,0.00020374407,0.75178987,0.0034944369,0.0025488602,0.0012710977,0.00003616854],"about_ca_topic_score_codex":0.02137799,"about_ca_topic_score_gemma":0.01584786,"teacher_disagreement_score":0.02137799,"about_ca_system_score_codex":0.000708608,"about_ca_system_score_gemma":0.0006093709,"threshold_uncertainty_score":0.042507112},"labels":[],"label_agreement":null},{"id":"W4285802436","doi":"10.1029/2022gl098762","title":"Fugitive Gas Migration in the Vadose Zone at an Experimental Field Site in the Montney Shale Gas Region","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Guelph; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; H2020 European Research Council; Natural Resources Canada; British Columbia Oil and Gas Commission; Canada First Research Excellence Fund","keywords":"Vadose zone; Methane; Soil gas; Natural gas; Geology; Oil shale; Fugitive emissions; Biogeochemical cycle; Carbon dioxide; Environmental science; Fossil fuel; Natural gas field; Diamondoid; Petroleum; Carbon sequestration; Hydrology (agriculture); Soil science; Greenhouse gas; Environmental chemistry; Soil water; Oceanography; Geotechnical engineering; Chemistry; Paleontology","score_opus":0.03408164553017022,"score_gpt":0.29985999192900614,"score_spread":0.2657783463988359,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4285802436","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998597,0.0000021229268,0.00005952593,0.0000027600581,2.086102e-7,0.000005263573,0.000021664968,0.0000029379207,0.00004579847],"genre_scores_gemma":[0.99929845,0.000005808022,0.00046595256,0.000003914758,2.874854e-7,0.000014301644,0.000074625605,0.0000011310203,0.00013559811],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990225,0.000027975671,0.000003201234,0.000030019584,0.000013455634,0.000023050574],"domain_scores_gemma":[0.99979156,0.00006159829,0.000030141442,0.00002091711,0.000045876746,0.000049949467],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024942533,0.00024442057,0.00014486749,0.00025524772,0.0006062496,0.0002928801,0.0005500024,0.00033868774,0.00039968028],"category_scores_gemma":[0.00026577176,0.00012100715,0.00023041508,0.00023204587,0.0005212059,0.00020840703,0.00022539742,0.00024172182,0.000062123734],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0037331309,0.00321198,0.65985215,0.00007913823,0.000117849966,0.0012428262,0.0025497563,0.062498983,0.24850382,0.00092691445,0.00041982223,0.01686365],"study_design_scores_gemma":[0.0002794051,0.006225868,0.77035695,0.000013766434,0.00008060023,0.00023196344,0.0028140626,0.15481979,0.06350947,0.00039586044,0.0011974141,0.000074749325],"about_ca_topic_score_codex":0.16333883,"about_ca_topic_score_gemma":0.26350415,"teacher_disagreement_score":0.83666116,"about_ca_system_score_codex":0.0026803152,"about_ca_system_score_gemma":0.0010911027,"threshold_uncertainty_score":0.32477623},"labels":[],"label_agreement":null},{"id":"W4286214487","doi":"10.1029/2022gl098208","title":"Deep Geological Controls on Formation of the Highest‐Grade Uranium Deposits in the World: Magnetotelluric Imaging of Unconformity‐Related Systems From the Athabasca Basin, Canada","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Laurentian University; Geological Survey of Canada","funders":"","keywords":"Magnetotellurics; Geology; Uranium ore; Unconformity; Uranium; Structural basin; Geochemistry; Geothermal gradient; Radiogenic nuclide; Hydrothermal circulation; Source rock; Petrology; Rift; Magmatism; Geomorphology; Geophysics; Electrical resistivity and conductivity; Paleontology; Tectonics; Mantle (geology)","score_opus":0.018433159945983296,"score_gpt":0.24619705532689562,"score_spread":0.22776389538091232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286214487","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99641293,0.0001276493,0.00017392934,0.000073885,0.0000016773424,0.000005866416,0.0005976849,0.000016364293,0.002590092],"genre_scores_gemma":[0.9989686,0.00007322485,0.00023082693,0.000015805794,8.9192474e-7,0.000001942262,0.00020614396,0.000005132506,0.00049756083],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992764,0.000002588909,0.0000018202851,0.000013510792,0.000019714693,0.000034831482],"domain_scores_gemma":[0.99986947,0.0000063193315,0.000019293442,0.000004523848,0.00007372271,0.000026528738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008912452,0.0002101342,0.00014856058,0.0016145793,0.0012038448,0.0009125067,0.00037469756,0.00021772805,0.0010711857],"category_scores_gemma":[0.00022406723,0.00014802438,0.000089669935,0.001868584,0.0004992035,0.0002132522,0.00040620408,0.00019577678,0.00012236334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014911403,0.00004842506,0.8850241,0.000059585658,0.000089363064,0.0004464895,0.0029120187,0.0016425697,0.078031264,0.00094503973,0.0016905013,0.028961524],"study_design_scores_gemma":[0.0000027743538,0.0000028497554,0.9969994,0.0000067422166,0.0000074767595,0.00003610785,0.0007774963,0.00064613036,0.0008111806,0.000036258818,0.0006681505,0.0000054323195],"about_ca_topic_score_codex":0.93373615,"about_ca_topic_score_gemma":0.9780716,"teacher_disagreement_score":0.066263855,"about_ca_system_score_codex":0.0046291007,"about_ca_system_score_gemma":0.0026872186,"threshold_uncertainty_score":0.13330811},"labels":[],"label_agreement":null},{"id":"W4286501707","doi":"10.1029/2022gl100200","title":"On the Linearity of External Forcing Response in Solar Geoengineering Experiments","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Solar constant; Cloud forcing; Earth's energy budget; Forcing (mathematics); Atmospheric sciences; Shortwave; Radiative forcing; Environmental science; Radiative transfer; Energy balance; Physics; Solar irradiance; Meteorology; Radiation; Aerosol","score_opus":0.055027856481122565,"score_gpt":0.3154598970860439,"score_spread":0.2604320406049213,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286501707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98760533,0.00007617994,0.0044852816,0.00068944605,0.000019365663,0.00004401164,0.0005526335,0.00023374661,0.0062941816],"genre_scores_gemma":[0.9987224,0.000018286904,0.0004722043,0.000121801786,0.000004730783,0.000030658408,0.00025486609,0.000035025427,0.0003399944],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99941325,0.00030692425,0.000032892272,0.00011573598,0.000053630087,0.00007754837],"domain_scores_gemma":[0.99558544,0.0029773482,0.0003952345,0.00062681525,0.00024929005,0.0001659452],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0018241839,0.00029521258,0.00035344195,0.0003590473,0.00024289588,0.00068862474,0.0004860802,0.0006036898,0.0029488239],"category_scores_gemma":[0.009070063,0.00023198195,0.0006322451,0.0002178699,0.0009013914,0.0007926067,0.00090792077,0.0009357544,0.0003013136],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0021782464,0.000604432,0.20192632,0.00031853592,0.0005303798,0.00041415443,0.00054774166,0.6937906,0.057766166,0.021100309,0.0033564814,0.017466594],"study_design_scores_gemma":[0.00038491006,0.00058530964,0.21399423,0.000052370506,0.00008800631,0.0000975731,0.00039924355,0.7561375,0.015234831,0.011300655,0.0016377995,0.000087621665],"about_ca_topic_score_codex":0.0059408667,"about_ca_topic_score_gemma":0.0028442065,"teacher_disagreement_score":0.0059408667,"about_ca_system_score_codex":0.00061353296,"about_ca_system_score_gemma":0.00045962256,"threshold_uncertainty_score":0.011812568},"labels":[],"label_agreement":null},{"id":"W4286502892","doi":"10.1029/2022gl098364","title":"CMIP5 and CMIP6 Model Projection Comparison for Hydrological Impacts Over North America","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":69,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"École de Technologie Supérieure; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Agence Nationale de la Recherche","keywords":"Coupled model intercomparison project; Climatology; Precipitation; Environmental science; Climate model; Climate change; Meteorology; Geography; Geology","score_opus":0.04604784620578935,"score_gpt":0.3250753078186201,"score_spread":0.27902746161283076,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4286502892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9776924,0.00030017894,0.0034825883,0.00047162845,0.00005932639,0.00004011886,0.0107262945,0.00046344547,0.0067639756],"genre_scores_gemma":[0.9857633,0.00022504426,0.0042854077,0.000067284775,0.000021680045,0.00006657868,0.00890483,0.00007869523,0.000587233],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996666,0.00014979432,0.000019623063,0.00006634606,0.00006332216,0.000034371762],"domain_scores_gemma":[0.99918514,0.0002584762,0.0000774561,0.000088776935,0.00033261982,0.000057555328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015583897,0.00064823235,0.00034466403,0.000633002,0.00031122082,0.0007768062,0.00056875503,0.00047123613,0.002497324],"category_scores_gemma":[0.0022683374,0.0002578982,0.00065838237,0.0016255536,0.00017433659,0.00091671984,0.0004930832,0.00042540312,0.00032260315],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045614474,0.00013194598,0.07610719,0.0001222458,0.00051304273,0.00014975699,0.00012819195,0.8934166,0.0014330178,0.0015510791,0.006795328,0.019195493],"study_design_scores_gemma":[0.00018620609,0.00010233062,0.16338487,0.000056969802,0.00020076887,0.00008271613,0.00036116934,0.825653,0.001993898,0.0017318982,0.006153601,0.00009263767],"about_ca_topic_score_codex":0.059759784,"about_ca_topic_score_gemma":0.052990578,"teacher_disagreement_score":0.9402402,"about_ca_system_score_codex":0.0009842869,"about_ca_system_score_gemma":0.0008407748,"threshold_uncertainty_score":0.118823886},"labels":[],"label_agreement":null},{"id":"W4289687853","doi":"10.1029/2022gl098539","title":"Fine‐Scale Geothermal Heat Flow in Antarctica Can Increase Simulated Subglacial Melt Estimates","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":35,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Meltwater; Geology; Ice stream; Geothermal gradient; Geomorphology; Ice sheet; Ice shelf; Geothermal heating; Cryosphere; Climatology; Geothermal energy; Geophysics; Sea ice; Glacial period","score_opus":0.02760689557190803,"score_gpt":0.27491289982067524,"score_spread":0.2473060042487672,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289687853","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782664,0.000048915674,0.00039360308,0.000100146055,0.000012349634,0.0000051040665,0.00048615527,0.0000875167,0.0010395558],"genre_scores_gemma":[0.99945706,0.000022438539,0.00019130924,0.000017716724,0.0000033172182,0.000004593566,0.00017994428,0.000012826593,0.00011082736],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989843,0.000044218777,0.0000050156614,0.000019648121,0.000009034366,0.000023593086],"domain_scores_gemma":[0.99946505,0.00030794847,0.000052176412,0.000067530884,0.00004761893,0.000059636623],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003726315,0.0003852083,0.00026038272,0.00028402006,0.00024508892,0.0006622766,0.00046408296,0.00057205703,0.0016297742],"category_scores_gemma":[0.0011951699,0.00023361336,0.000508709,0.00031903415,0.00027790532,0.00037449703,0.00031538968,0.00032350156,0.00013822918],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024348749,0.00012753325,0.11083664,0.00004199841,0.00021370249,0.00008609217,0.00006032034,0.8778502,0.004306557,0.000334758,0.0009010968,0.004997612],"study_design_scores_gemma":[0.00013572935,0.000103046936,0.06868409,0.000014018666,0.00008429653,0.00001545236,0.00008649059,0.9269049,0.002657262,0.00032266031,0.0009682252,0.000023732753],"about_ca_topic_score_codex":0.031976223,"about_ca_topic_score_gemma":0.024548635,"teacher_disagreement_score":0.031976223,"about_ca_system_score_codex":0.00061759964,"about_ca_system_score_gemma":0.00047206698,"threshold_uncertainty_score":0.063580215},"labels":[],"label_agreement":null},{"id":"W4289704954","doi":"10.1029/2022gl099205","title":"Bores Observed During the Warm Season of 2015–2019 Over the Southern North China Plain","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"National Natural Science Foundation of China; State Key Laboratory of Severe Weather; National Science Foundation","keywords":"Mesoscale meteorology; Climatology; Geology; Convection; Southern china; Mesoscale convective system; Range (aeronautics); China; Meteorology; Geography","score_opus":0.0409945372521212,"score_gpt":0.26888099007216165,"score_spread":0.22788645282004044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289704954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99826545,0.000043526506,0.00008087306,0.00002762898,0.0000079833235,0.000005883929,0.0011168739,0.000014652663,0.0004370862],"genre_scores_gemma":[0.99843425,0.000028339971,0.00007427597,0.000010271998,0.000010373356,0.0000066057723,0.0012544709,0.0000017645765,0.00017954665],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991226,0.000007689726,0.000009764496,0.00002171418,0.000023871478,0.00002471491],"domain_scores_gemma":[0.9996377,0.000025540552,0.00013309377,0.000026090984,0.00007919466,0.000098225486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028577936,0.00016844865,0.0001583222,0.0006784281,0.000336402,0.00036564737,0.00018838783,0.0001530906,0.00067979074],"category_scores_gemma":[0.00042789875,0.000072466595,0.00019187336,0.0006189157,0.00022104368,0.00036549714,0.0005372595,0.0001763916,0.00010129362],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001364077,0.000039754796,0.9874264,0.000034220346,0.00005226262,0.00023489141,0.0006773995,0.00080737966,0.0037802998,0.00012701895,0.001219122,0.00546482],"study_design_scores_gemma":[0.0000015233211,0.000010656653,0.9988557,0.0000028334189,0.0000044314534,0.00002408128,0.00018542292,0.00039293207,0.00009840329,0.000010531404,0.00041069568,0.0000028689378],"about_ca_topic_score_codex":0.043181207,"about_ca_topic_score_gemma":0.082439624,"teacher_disagreement_score":0.043181207,"about_ca_system_score_codex":0.00045981712,"about_ca_system_score_gemma":0.00044798708,"threshold_uncertainty_score":0},"labels":[],"label_agreement":null},{"id":"W4289943346","doi":"10.1029/2022gl098776","title":"Seasonality of Continental Extratropical‐Cyclone Wind Speeds Over Northeastern North America","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"","keywords":"Extratropical cyclone; Climatology; Seasonality; Cyclone (programming language); Wind speed; Maximum sustained wind; Storm; Environmental science; Tropical cyclone; Geology; Atmospheric sciences; Meteorology; Wind profile power law; Oceanography; Geography; Wind gradient; Mathematics; Statistics","score_opus":0.029699553528070397,"score_gpt":0.27985054246971397,"score_spread":0.25015098894164356,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4289943346","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99839205,0.00008935873,0.00004159579,0.000018199953,0.0000040030045,0.0000020693412,0.0009590061,0.000005935871,0.00048772438],"genre_scores_gemma":[0.9982724,0.00008976045,0.00006940656,0.000008277037,0.0000051252523,0.0000041541034,0.0012439871,0.0000015410401,0.00030524645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999944,0.000008397719,0.0000051714105,0.000018268094,0.000014176241,0.0000101067135],"domain_scores_gemma":[0.9997131,0.000044189626,0.0000939956,0.000018093393,0.00008703251,0.00004359923],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013113541,0.00011320631,0.000108716275,0.0005149451,0.00015479981,0.0002581676,0.00008444603,0.00009067892,0.00085268734],"category_scores_gemma":[0.00034781417,0.00005801731,0.000100447265,0.0005738788,0.00009088296,0.00015969813,0.0001654392,0.0001082489,0.000086736705],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003263648,0.000013251492,0.99345946,0.000012283195,0.00004005728,0.00006236701,0.000095386,0.0008171011,0.001122131,0.000027929866,0.00051909284,0.0037983677],"study_design_scores_gemma":[8.3483764e-7,0.000004051476,0.9993311,0.0000020054958,0.0000030004537,0.000015886166,0.000054955628,0.00028284133,0.00005041824,0.0000037319392,0.00025020432,0.0000010825776],"about_ca_topic_score_codex":0.060986362,"about_ca_topic_score_gemma":0.20957085,"teacher_disagreement_score":0.93901366,"about_ca_system_score_codex":0.00034226195,"about_ca_system_score_gemma":0.00019846388,"threshold_uncertainty_score":0.12126279},"labels":[],"label_agreement":null},{"id":"W4291124519","doi":"10.1029/2022gl098063","title":"Neglected Spatiotemporal Variations of Model Biases in Ensemble‐Based Climate Projections","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Prince Edward Island; University of Regina","funders":"Western Economic Diversification Canada; Mitacs; Canada Research Chairs","keywords":"Probabilistic logic; Bayesian probability; Computer science; Robustness (evolution); Ensemble forecasting; Bayesian inference; Ensemble learning; Climate model; Artificial intelligence; Climate change; Geology","score_opus":0.10314817188839423,"score_gpt":0.3477377495266845,"score_spread":0.24458957763829028,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291124519","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.4004849,0.00022000131,0.5943479,0.00040677702,0.00005506315,0.000032284803,0.00036861876,0.0006023476,0.0034821217],"genre_scores_gemma":[0.9414101,0.00009019926,0.05774251,0.000034137185,0.000022804967,0.000025423826,0.0002457807,0.00006756489,0.00036142624],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99949384,0.00019833507,0.000025550835,0.00009089574,0.00015267692,0.00003880352],"domain_scores_gemma":[0.9988851,0.00041652704,0.00016050978,0.0001998693,0.00029468958,0.0000432973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0020301503,0.0004925806,0.00037148618,0.0006132796,0.0003597346,0.0006383118,0.00058744865,0.00047157967,0.0005865515],"category_scores_gemma":[0.005826176,0.00029815992,0.00048039912,0.0006783712,0.00027278118,0.001336173,0.00078484206,0.0007424148,0.0001453953],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005105056,0.000028808929,0.010888854,0.000029348288,0.00013039127,0.00004706623,0.000076427736,0.9078262,0.0060208337,0.007360365,0.0008155499,0.06672513],"study_design_scores_gemma":[0.0000036597307,0.000005251419,0.0028313778,0.0000040424156,0.000011570792,0.000010744879,0.000007954158,0.992249,0.0012546007,0.0032532616,0.00035743858,0.00001109408],"about_ca_topic_score_codex":0.012623178,"about_ca_topic_score_gemma":0.013411741,"teacher_disagreement_score":0.012623178,"about_ca_system_score_codex":0.00046238338,"about_ca_system_score_gemma":0.0010555463,"threshold_uncertainty_score":0.025099456},"labels":[],"label_agreement":null},{"id":"W4291165744","doi":"10.1029/2022gl099614","title":"Impact of Vertical Mixing Parameterizations on Internal Gravity Wave Spectra in Regional Ocean Models","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Stennis Space Center; Jet Propulsion Laboratory; Nuclear Safety and Security Commission; Office of Naval Research; Compute Canada; National Aeronautics and Space Administration; California Institute of Technology; University of Toronto; National Science Foundation","keywords":"Internal wave; Geology; Mixing (physics); Wavenumber; Gravity wave; Kinetic energy; Vertical mixing; Spectral line; Geophysics; Ridge; Ocean dynamics; Amplitude; Geodesy; Gravitational wave; Atmospheric sciences; Climatology; Physics; Ocean current; Oceanography; Classical mechanics; Optics","score_opus":0.05600506383657045,"score_gpt":0.30146618055534474,"score_spread":0.2454611167187743,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291165744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96994823,0.00028640195,0.021311814,0.0006562277,0.0000808068,0.0000651355,0.0006494911,0.0007975688,0.006204362],"genre_scores_gemma":[0.99322927,0.00007876339,0.0058051017,0.000097752185,0.000017345523,0.000034932447,0.00018780657,0.00013159968,0.0004174809],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9992335,0.0004324131,0.00004493403,0.000092397226,0.000089828005,0.00010695965],"domain_scores_gemma":[0.99703276,0.0017569006,0.00028929743,0.0003700418,0.0003624062,0.00018860183],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0021609962,0.0013462917,0.001014093,0.00047826488,0.0007659241,0.0016942419,0.001575599,0.0015441205,0.001198888],"category_scores_gemma":[0.008115737,0.0007962943,0.0010659193,0.0005102402,0.00086224824,0.0015100159,0.0013465874,0.0014581882,0.00022281136],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006590141,0.000039320654,0.0024979098,0.000009628408,0.00004813644,0.000023425622,0.000015846244,0.99500966,0.0009345654,0.00033160023,0.0000919863,0.00093198154],"study_design_scores_gemma":[0.000032359738,0.000030023602,0.00042704164,0.0000053642457,0.000020326555,0.000003482621,0.000012042718,0.9986094,0.0006236872,0.00013036883,0.00009592693,0.000009890786],"about_ca_topic_score_codex":0.06050906,"about_ca_topic_score_gemma":0.026698766,"teacher_disagreement_score":0.06050906,"about_ca_system_score_codex":0.001479461,"about_ca_system_score_gemma":0.0014117149,"threshold_uncertainty_score":0.120313704},"labels":[],"label_agreement":null},{"id":"W4291383506","doi":"10.1029/2022gl099481","title":"On the Potentials and Limitations of Attributing a Small‐Scale Climate Event","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos","funders":"","keywords":"Scale (ratio); Event (particle physics); Climatology; Environmental science; Geology; Geography; Cartography; Physics; Astrophysics","score_opus":0.10416163907664507,"score_gpt":0.3122678158895047,"score_spread":0.20810617681285964,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291383506","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9677297,0.0003438236,0.02767408,0.00065780844,0.00006769552,0.000020519476,0.00032094496,0.00010119613,0.0030841702],"genre_scores_gemma":[0.99766195,0.000057212383,0.0020531956,0.000019569134,0.00001500768,0.0000029345874,0.00007444749,0.000009588561,0.00010606926],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9992424,0.0003988721,0.000043951757,0.00014797448,0.00010430654,0.0000624722],"domain_scores_gemma":[0.98435414,0.012921899,0.0009751342,0.0009402284,0.0005660688,0.00024252557],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0033758504,0.00039630785,0.00027747592,0.0005133655,0.00045254207,0.0012603855,0.00069227646,0.00068316865,0.00094232947],"category_scores_gemma":[0.013321431,0.0001450624,0.00042252743,0.00038376526,0.0005650446,0.0013277069,0.00079200877,0.0006555682,0.00009472547],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005140393,0.00007547473,0.17992614,0.000106010455,0.00021277713,0.0002064387,0.0002520356,0.7821517,0.0027370588,0.0054692333,0.0006808155,0.027668362],"study_design_scores_gemma":[0.0000150031265,0.000101024685,0.04246883,0.000047301655,0.00007282992,0.00009300601,0.0002742958,0.94727606,0.0019389194,0.006979764,0.00069475546,0.00003813626],"about_ca_topic_score_codex":0.013761096,"about_ca_topic_score_gemma":0.010466863,"teacher_disagreement_score":0.013761096,"about_ca_system_score_codex":0.0004601098,"about_ca_system_score_gemma":0.0007579539,"threshold_uncertainty_score":0.027361989},"labels":[],"label_agreement":null},{"id":"W4291433219","doi":"10.1029/2022gl099250","title":"A Minimally Cemented Shallow Crust Beneath InSight","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Nuclear Safety and Security Commission; Canadian Institute for Advanced Research; National Aeronautics and Space Administration; Earth Sciences Division; Division of Earth Sciences; National Science Foundation","keywords":"Geology; Martian; Crust; Mars Exploration Program; Basalt; Mineral; Geochemistry; Cement; Petrology; Astrobiology; Materials science; Composite material","score_opus":0.046855181965154966,"score_gpt":0.2968179539921892,"score_spread":0.2499627720270342,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291433219","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.995799,0.00006213569,0.0011304192,0.00005056546,0.000003184657,0.0000043830482,0.00018491824,0.000113306785,0.0026520104],"genre_scores_gemma":[0.9992781,0.000019252577,0.00038348234,0.0000088559955,6.739853e-7,5.8680405e-7,0.000052807907,0.0000032856144,0.0002529349],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999291,0.0000029120451,0.0000036908439,0.00002266516,0.000021168706,0.000020457604],"domain_scores_gemma":[0.99986625,0.000016087357,0.000040662624,0.000016462434,0.000017378283,0.000043110627],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005143422,0.00025959796,0.00022401745,0.00042253322,0.00035137878,0.00066230504,0.00038746433,0.00042106264,0.0024524925],"category_scores_gemma":[0.00037576247,0.00028562546,0.00015528029,0.00030973786,0.00045780162,0.00040610615,0.0009280077,0.00030978658,0.00026379584],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074733736,0.00015973835,0.25880975,0.00024070962,0.00011481231,0.007094456,0.0012172974,0.033641607,0.65097404,0.0058660526,0.0007427184,0.04039157],"study_design_scores_gemma":[0.00007730289,0.00062617374,0.8582338,0.0001071286,0.00017208919,0.006137218,0.0016717461,0.066792026,0.05139759,0.005481377,0.0091476105,0.000155888],"about_ca_topic_score_codex":0.007181491,"about_ca_topic_score_gemma":0.004509078,"teacher_disagreement_score":0.007181491,"about_ca_system_score_codex":0.0004828831,"about_ca_system_score_gemma":0.00038002888,"threshold_uncertainty_score":0.014279366},"labels":[],"label_agreement":null},{"id":"W4291719075","doi":"10.1029/2022gl100152","title":"Cloud Feedback on Earth's Long‐Term Climate Simulated by a Near‐Global Cloud‐Permitting Model","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Cloud albedo; Cloud feedback; Cloud computing; Term (time); Environmental science; Atmospheric sciences; Cloud cover; Climate model; General Circulation Model; Shortwave; Convection; Albedo (alchemy); Climatology; Meteorology; Climate change; Geology; Climate sensitivity; Physics; Radiative transfer; Computer science; Astronomy","score_opus":0.04986357093920393,"score_gpt":0.30628373907853895,"score_spread":0.256420168139335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4291719075","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994189,0.00007470099,0.0015571408,0.00035253004,0.000029345316,0.000011249032,0.0006832334,0.00013180311,0.002970923],"genre_scores_gemma":[0.9986517,0.00004441953,0.0004781779,0.0000462388,0.000008498329,0.000010587402,0.00037435454,0.000017702447,0.00036849797],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991894,0.000024749017,0.0000039085576,0.000021925076,0.000008275789,0.00002217339],"domain_scores_gemma":[0.99972075,0.000104070146,0.000038258477,0.00002793029,0.00003876694,0.000070252376],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024800372,0.00056220277,0.0005327752,0.00028625276,0.00056568615,0.0008322257,0.0008239265,0.001314426,0.0016171841],"category_scores_gemma":[0.0007094033,0.00032924153,0.0007662493,0.00048561848,0.00060947164,0.0007703324,0.00050213275,0.00077532383,0.00014363794],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089050736,0.00005984676,0.0062152967,0.000014274297,0.00005220236,0.00008380466,0.000017384804,0.99079317,0.0011419296,0.0006644847,0.00030887828,0.00055959093],"study_design_scores_gemma":[0.00006002311,0.000033910794,0.0033506153,0.0000029164137,0.000022865199,0.0000083566265,0.000018680299,0.9958578,0.00019954462,0.00025884507,0.00017643927,0.00001003105],"about_ca_topic_score_codex":0.06714757,"about_ca_topic_score_gemma":0.023213381,"teacher_disagreement_score":0.06714757,"about_ca_system_score_codex":0.0010049327,"about_ca_system_score_gemma":0.00085054664,"threshold_uncertainty_score":0.13351345},"labels":[],"label_agreement":null},{"id":"W4292074780","doi":"10.1029/2022gl099655","title":"Quantifying the Size and Duration of a Microburst‐Producing Chorus Region on 5 December 2017","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Athabasca University; University of Calgary","funders":"National Aeronautics and Space Administration","keywords":"Chorus; Microburst; Duration (music); Environmental science; Meteorology; Atmospheric sciences; Geology; Climatology; Geography; Physics; Acoustics; Wind shear; Wind speed","score_opus":0.039436952819354526,"score_gpt":0.30738659629527515,"score_spread":0.26794964347592065,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292074780","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896444,0.00028768953,0.0012681872,0.00011923108,0.00002933711,0.000021954238,0.0033696506,0.00020600243,0.005053555],"genre_scores_gemma":[0.9904813,0.0001406661,0.0014438675,0.000031593554,0.000040774434,0.000020041813,0.0072189933,0.00004774162,0.00057506026],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986446,0.00001005867,0.00000527731,0.00003278486,0.0000438815,0.000043600547],"domain_scores_gemma":[0.99962676,0.000055121556,0.00009218331,0.000034600376,0.000089645095,0.00010169188],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002555582,0.00026083246,0.0002375449,0.0013260355,0.00041274694,0.0005110452,0.00025642343,0.0002814096,0.0012750244],"category_scores_gemma":[0.000796435,0.00013883707,0.0002568051,0.00064691104,0.00019279026,0.00037566523,0.00060509826,0.00031853298,0.00035141062],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004534864,0.00006206125,0.93028975,0.000103036335,0.00023022386,0.0005816453,0.0006023036,0.003912945,0.027832352,0.00062681106,0.0056074513,0.02969791],"study_design_scores_gemma":[0.000009420083,0.00001923413,0.9887207,0.000022837632,0.000026917134,0.00010654556,0.00018316381,0.004238678,0.0029744515,0.0000843744,0.0036039485,0.000009830458],"about_ca_topic_score_codex":0.016003266,"about_ca_topic_score_gemma":0.026397876,"teacher_disagreement_score":0.016003266,"about_ca_system_score_codex":0.00038692873,"about_ca_system_score_gemma":0.00023105726,"threshold_uncertainty_score":0.031820178},"labels":[],"label_agreement":null},{"id":"W4292674163","doi":"10.1029/2022gl098945","title":"Rheology of Naturally Deformed Antigorite Serpentinite: Strain and Strain‐Rate Dependence at Mantle‐Wedge Conditions","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"European Commission","keywords":"Geology; Rheology; Dislocation creep; Mantle (geology); Dissolution; Shear (geology); Shear zone; Strain rate; Slip (aerodynamics); Creep; Shear stress; Grain boundary; Differential stress; Mineralogy; Petrology; Deformation (meteorology); Geophysics; Materials science; Seismology; Microstructure; Composite material; Thermodynamics; Tectonics","score_opus":0.026553335538076043,"score_gpt":0.27362252037562607,"score_spread":0.24706918483755003,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4292674163","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994005,0.000030020434,0.000058057874,0.0000070842107,0.0000011268194,0.0000016820987,0.000092348004,0.000008733995,0.00040059225],"genre_scores_gemma":[0.9997975,0.000012693165,0.000031439504,0.0000018192118,6.6517197e-7,9.4644815e-7,0.00007650309,0.0000031045245,0.000075220974],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999577,0.000003965192,0.0000047603,0.00001429073,0.000010204556,0.000009080839],"domain_scores_gemma":[0.99982786,0.000024531382,0.0000435837,0.000018599667,0.000047674435,0.000037680722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008160402,0.00017338223,0.00014047409,0.00054310303,0.0001868326,0.00036520773,0.0001660844,0.00013803937,0.0009473487],"category_scores_gemma":[0.00033899577,0.00016058532,0.00009709911,0.0002130766,0.00033297515,0.0002005107,0.0001412658,0.00017730893,0.00014837201],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006207274,0.0000608507,0.20068726,0.00007312182,0.000049691993,0.0008499851,0.000564465,0.0023087235,0.7890785,0.00021038776,0.00017052203,0.005325794],"study_design_scores_gemma":[0.000013157799,0.000080988786,0.95439327,0.000004338775,0.000012217442,0.00037595694,0.00019923154,0.0058565564,0.038584523,0.00005073222,0.00041388682,0.000015212335],"about_ca_topic_score_codex":0.0050104028,"about_ca_topic_score_gemma":0.0045908405,"teacher_disagreement_score":0.0050104028,"about_ca_system_score_codex":0.00021789027,"about_ca_system_score_gemma":0.00009089735,"threshold_uncertainty_score":0.00996244},"labels":[],"label_agreement":null},{"id":"W4293213259","doi":"10.1029/2022gl099543","title":"West Antarctic Surface Climate Changes Since the Mid‐20th Century Driven by Anthropogenic Forcing","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Belgian Federal Science Policy Office; Fonds De La Recherche Scientifique - FNRS; Natural Environment Research Council; Sight Research UK","keywords":"Forcing (mathematics); Greenhouse gas; Environmental science; Climatology; Climate model; Climate change; Ozone depletion; Ozone layer; Radiative forcing; Atmospheric sciences; Proxy (statistics); Snow; Oceanography; Geology; Meteorology; Geography; Stratosphere","score_opus":0.03627941954902608,"score_gpt":0.2827154925357261,"score_spread":0.2464360729867,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293213259","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940877,0.0004654176,0.00025039236,0.00025627282,0.00003422727,0.0000037085788,0.0037223096,0.000025022084,0.0011549143],"genre_scores_gemma":[0.99664414,0.00039702686,0.00018910976,0.00007118381,0.000028206,0.0000071588092,0.0024264348,0.000008762779,0.00022799094],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998894,0.00002318536,0.000013594789,0.00003095327,0.000019300469,0.000023522305],"domain_scores_gemma":[0.99961793,0.000045536093,0.00013168932,0.000054968517,0.00010735773,0.000042476135],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00051161234,0.00032542218,0.00020830373,0.0006600265,0.00028709075,0.00095381384,0.00027078518,0.00042178872,0.0009723127],"category_scores_gemma":[0.0006745977,0.00012972209,0.00058420235,0.0013077005,0.00024037524,0.00042443,0.000495098,0.0003593125,0.0002594146],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029548572,0.00006487903,0.9619596,0.0001195439,0.00063846837,0.00041804244,0.00021883061,0.016943974,0.0054191067,0.0008938159,0.0018718673,0.011156392],"study_design_scores_gemma":[0.000009823046,0.000024925259,0.99193186,0.00001638645,0.00008687002,0.00008246507,0.00009086743,0.004584387,0.00069919083,0.00010338792,0.0023583046,0.000011586436],"about_ca_topic_score_codex":0.016790984,"about_ca_topic_score_gemma":0.017588135,"teacher_disagreement_score":0.016790984,"about_ca_system_score_codex":0.00063839235,"about_ca_system_score_gemma":0.0003896806,"threshold_uncertainty_score":0.03338653},"labels":[],"label_agreement":null},{"id":"W4293213379","doi":"10.1029/2022gl100158","title":"Seismic Evidence for a Weakened Thick Crust at the Beaufort Sea Continental Margin","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Ottawa; Geological Survey of Canada; Natural Resources Canada; McGill University","funders":"","keywords":"Geology; Crust; Subduction; Continental margin; Seismology; Continental crust; Oceanic crust; Convergent boundary; Sedimentary rock; Accretionary wedge; Mantle (geology); Paleontology; Tectonics","score_opus":0.06540731740024949,"score_gpt":0.30143789378675084,"score_spread":0.23603057638650135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293213379","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99365246,0.00012980783,0.0003088437,0.00007553874,0.000002870666,0.000004239859,0.00041908975,0.00005748345,0.0053497064],"genre_scores_gemma":[0.99929476,0.000023161918,0.00019700645,0.0000057935945,5.941495e-7,5.1806194e-7,0.00015765971,0.0000032995738,0.00031727637],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998342,0.000012027238,0.0000066657153,0.00003951941,0.00006854028,0.00003907915],"domain_scores_gemma":[0.99973875,0.00001842855,0.00006275409,0.000032647087,0.0001012581,0.000046037138],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014874995,0.0002000211,0.00014307612,0.0007627859,0.0007894751,0.00091988756,0.0005818409,0.0003262401,0.0023845274],"category_scores_gemma":[0.000695902,0.00017750954,0.00021432359,0.0007216632,0.00074917113,0.00016143525,0.00043172494,0.00016804821,0.0002257056],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016543451,0.000015094814,0.92433906,0.000044101,0.00010493368,0.00077619986,0.0008250942,0.019365977,0.029776517,0.0015568616,0.0010818733,0.021948898],"study_design_scores_gemma":[0.0000035125013,0.000009973383,0.9925161,0.000008528776,0.000008159849,0.00007655785,0.0002494571,0.005087049,0.0005897769,0.00006843231,0.0013734574,0.000009093096],"about_ca_topic_score_codex":0.8932735,"about_ca_topic_score_gemma":0.933321,"teacher_disagreement_score":0.8932735,"about_ca_system_score_codex":0.003517358,"about_ca_system_score_gemma":0.0024032327,"threshold_uncertainty_score":0.21471006},"labels":[],"label_agreement":null},{"id":"W4293213571","doi":"10.1029/2022gl100146","title":"Hidden Roughness of Subducting Seafloor and Implications for Megathrust Seismogenesis: Example From Northern Manila Trench","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"Youth Innovation Promotion Association of the Chinese Academy of Sciences; Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Seafloor spreading; Trench; Seismology; Subduction; Bathymetry; Seamount; Accretion (finance); Basement; Tectonics; Geophysics; Geochemistry; Oceanography","score_opus":0.07315823155903257,"score_gpt":0.29431640046450225,"score_spread":0.2211581689054697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293213571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987864,0.00006403928,0.00008066247,0.000024172494,0.0000015092514,0.0000038009036,0.000052374067,0.0000063645202,0.0009807466],"genre_scores_gemma":[0.99964404,0.000034147768,0.000080610254,0.000003219721,0.0000019407971,0.0000012565911,0.000030494071,0.0000013684519,0.00020296266],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992585,0.000010430092,0.0000037361053,0.000014739482,0.0000124510125,0.00003292936],"domain_scores_gemma":[0.99973255,0.00006345311,0.00006254078,0.00003287305,0.000053712032,0.00005474613],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015158053,0.00023785878,0.00021896469,0.0010917572,0.00071212905,0.0005554595,0.0003293966,0.00034803478,0.0015012809],"category_scores_gemma":[0.0004547349,0.00012109477,0.00016008203,0.0010360996,0.0006681484,0.00019589628,0.00054424437,0.00015365276,0.00016079216],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024085461,0.000066605644,0.9426069,0.00010613842,0.00006013234,0.020564117,0.004743971,0.003805214,0.010060721,0.00037667915,0.00029931962,0.01706925],"study_design_scores_gemma":[0.0000032396513,0.00004119918,0.9945005,0.000013029936,0.000013950035,0.0010836759,0.0022489151,0.0009994473,0.0004491846,0.00008946607,0.00054540945,0.000011847429],"about_ca_topic_score_codex":0.03922054,"about_ca_topic_score_gemma":0.09452725,"teacher_disagreement_score":0.03922054,"about_ca_system_score_codex":0.0005684071,"about_ca_system_score_gemma":0.00036639912,"threshold_uncertainty_score":0.07798451},"labels":[],"label_agreement":null},{"id":"W4293795928","doi":"10.1029/2022gl100449","title":"Ion Behavior at Shocklets: A Case Study of MMS Observations","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Whistler; Ion; Physics; Foreshock; Solar wind; Geophysics; Cyclotron; Space physics; Resonance (particle physics); Magnetosphere; Cyclotron resonance; Plasma; Atomic physics; Geology; Nuclear physics; Seismology","score_opus":0.04933453311491305,"score_gpt":0.32385295760654936,"score_spread":0.2745184244916363,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293795928","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99664116,0.00015891109,0.0012431742,0.00013775461,0.000009924898,0.000022774067,0.00035577986,0.000055355897,0.0013750726],"genre_scores_gemma":[0.997042,0.00014553335,0.0017722677,0.000029462213,0.00003126024,0.0000071842273,0.00038054757,0.000014872612,0.00057678134],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998267,0.000026710994,0.000014637087,0.000032528842,0.00006028078,0.000039092207],"domain_scores_gemma":[0.9995204,0.00013926548,0.000108239656,0.00007019946,0.00007883966,0.000083095394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039208998,0.00032802307,0.00023927151,0.0014552299,0.0007483731,0.0005526767,0.0005091934,0.0010321185,0.00075384293],"category_scores_gemma":[0.00075608835,0.00015048632,0.00036057184,0.001148564,0.00035641974,0.00034535886,0.0008869434,0.00038441335,0.00017922712],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006536367,0.0003093512,0.7645335,0.00018116127,0.00019779113,0.14697357,0.003547182,0.011347655,0.03696064,0.002022935,0.0034813134,0.029791232],"study_design_scores_gemma":[0.00008261748,0.0006138969,0.8583375,0.0000778165,0.00016094286,0.033629753,0.0066199936,0.067258626,0.014905032,0.0025129835,0.015703255,0.00009750336],"about_ca_topic_score_codex":0.003816678,"about_ca_topic_score_gemma":0.0052700657,"teacher_disagreement_score":0.003816678,"about_ca_system_score_codex":0.00035464403,"about_ca_system_score_gemma":0.00016975113,"threshold_uncertainty_score":0.007588923},"labels":[],"label_agreement":null},{"id":"W4293915783","doi":"10.1029/2022gl099133","title":"Irminger Sea Is the Center of Action for Subpolar AMOC Variability","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":64,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ocean gyre; Oceanography; Climatology; Geology; Thermohaline circulation; Zonal and meridional; Ocean current; Latitude; Environmental science; Subtropics","score_opus":0.07155018266062343,"score_gpt":0.3408261866638022,"score_spread":0.26927600400317875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4293915783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99019974,0.00023107868,0.0010003953,0.00029605316,0.0000252686,0.000005073538,0.00049997703,0.00007093434,0.007671313],"genre_scores_gemma":[0.9990393,0.00007195754,0.00026036863,0.000023151337,0.000017210767,0.000002485073,0.00020851927,0.000007944987,0.00036910182],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999368,0.0000069784687,0.0000031840984,0.000022470986,0.000011225421,0.00001932065],"domain_scores_gemma":[0.99978596,0.000014592029,0.00008930488,0.000022688515,0.000043197128,0.00004435575],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016492275,0.00015196882,0.00015679895,0.0003457224,0.0002736614,0.0005289312,0.00015553442,0.00010857579,0.0025308295],"category_scores_gemma":[0.000422153,0.00005958879,0.00020347215,0.00029363783,0.0002156708,0.00039821022,0.00059825496,0.0002557888,0.0003074164],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015401583,0.000034400724,0.89838624,0.0000811683,0.00019054253,0.00020640653,0.00067989324,0.0038732246,0.016473867,0.004112886,0.0038645514,0.071942806],"study_design_scores_gemma":[0.000004169986,0.000024159855,0.98815674,0.000023946206,0.000036839945,0.000037984657,0.000343511,0.0037834782,0.0011670945,0.0007632165,0.0056480668,0.000010845869],"about_ca_topic_score_codex":0.01525736,"about_ca_topic_score_gemma":0.01833014,"teacher_disagreement_score":0.01525736,"about_ca_system_score_codex":0.0003386251,"about_ca_system_score_gemma":0.00036010667,"threshold_uncertainty_score":0.030337095},"labels":[],"label_agreement":null},{"id":"W4294891614","doi":"10.1029/2022gl098842","title":"The Effect of Compression Induced Chorus Waves on 10–100 s eV Electron Precipitation","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Electron precipitation; Physics; Magnetosphere; Ionosphere; Geomagnetic storm; Chorus; Geophysics; Atmospheric sciences; Electron; Cutoff; Computational physics; Proton; Van Allen Probes; Pitch angle; Van Allen radiation belt; Plasma; Solar wind; Nuclear physics","score_opus":0.013587652793065268,"score_gpt":0.30450127028858875,"score_spread":0.29091361749552347,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294891614","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985482,0.000036224206,0.00020535098,0.000014752382,0.0000030188753,0.0000025330683,0.000041377752,0.0000127280255,0.001135824],"genre_scores_gemma":[0.999845,0.000011824493,0.000043619042,0.0000021866563,6.654047e-7,9.78676e-7,0.000028999104,0.0000025348295,0.00006408974],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999534,0.000005266597,0.0000014962781,0.000009357099,0.000012977202,0.000017487931],"domain_scores_gemma":[0.99987006,0.00005177826,0.000022311047,0.000013275254,0.000019021854,0.000023546787],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000073238916,0.00014933219,0.00011347045,0.0001523064,0.00022007881,0.00021565538,0.000120849414,0.00014167886,0.0012821087],"category_scores_gemma":[0.0003701965,0.00008257098,0.0001085437,0.00010295122,0.00022786792,0.0001504516,0.00025938195,0.00023755102,0.00009503526],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016846198,0.00014251599,0.15385853,0.00009736947,0.00008654325,0.00090445066,0.00024163727,0.014940021,0.80556494,0.0007741546,0.00059489784,0.021110319],"study_design_scores_gemma":[0.000060234895,0.00058464654,0.73469543,0.000013857038,0.000032441,0.00027540475,0.00035723613,0.039178293,0.2231425,0.00040607151,0.0012324464,0.000021436283],"about_ca_topic_score_codex":0.0026459806,"about_ca_topic_score_gemma":0.0021154769,"teacher_disagreement_score":0.0026459806,"about_ca_system_score_codex":0.0002014274,"about_ca_system_score_gemma":0.00011217696,"threshold_uncertainty_score":0.005261123},"labels":[],"label_agreement":null},{"id":"W4294891992","doi":"10.1029/2022gl097935","title":"Salt‐Fingering in Seasonally Ice‐Covered Lakes","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ecology and biodiversity studies","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Queen's University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Environmental science; Salt (chemistry); Salt water; Climatology; Oceanography; Hydrology (agriculture); Chemistry; Geotechnical engineering","score_opus":0.03233790217843773,"score_gpt":0.27678872373127617,"score_spread":0.24445082155283843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4294891992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996369,0.000023526169,0.0000704427,0.0000040077625,6.933082e-7,0.0000023301704,0.000043984368,0.0000037790528,0.00021433829],"genre_scores_gemma":[0.9995758,0.000019195182,0.00020503525,0.000008605985,8.4250195e-7,0.0000045427755,0.00007023904,0.000002019408,0.00011382833],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999577,0.0000047421486,0.0000033179965,0.000012006672,0.000010890492,0.000011424616],"domain_scores_gemma":[0.9997956,0.00003212233,0.00007781686,0.000009857543,0.000042259177,0.00004227824],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009437645,0.00013579412,0.00016645601,0.00029165743,0.00038049923,0.00028913165,0.00012836156,0.00014076612,0.00057991897],"category_scores_gemma":[0.0002404259,0.00012762318,0.00009119349,0.0001917786,0.0003822376,0.00024656105,0.00025870078,0.00013149278,0.000060052684],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00074518303,0.000101868485,0.27277157,0.00008588075,0.000052843883,0.0004603573,0.0007754503,0.0008762422,0.71708244,0.00012138183,0.0001619228,0.006764943],"study_design_scores_gemma":[0.0000065109916,0.00018545763,0.972904,0.000004673297,0.000012635616,0.00011101896,0.00034960965,0.0013493225,0.024719818,0.00006892621,0.00028090063,0.0000071286117],"about_ca_topic_score_codex":0.006069054,"about_ca_topic_score_gemma":0.014217119,"teacher_disagreement_score":0.006069054,"about_ca_system_score_codex":0.00031956687,"about_ca_system_score_gemma":0.00017498509,"threshold_uncertainty_score":0.012067497},"labels":[],"label_agreement":null},{"id":"W4295599243","doi":"10.1029/2022gl099578","title":"How Are Mixed‐Phase Clouds Mixed?","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":73,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Mixed phase; Phase (matter); Environmental science; Precipitation; Cascade; Atmospheric sciences; Meteorology; Physics; Chemistry","score_opus":0.03050027110425248,"score_gpt":0.2953650286793617,"score_spread":0.26486475757510924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295599243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9883031,0.0022762879,0.0033234647,0.00048361314,0.00004477442,0.000015589827,0.00027412988,0.000066305976,0.0052126762],"genre_scores_gemma":[0.99957997,0.000105597304,0.00012903094,0.000026502677,0.000017004664,0.0000011214936,0.00004297057,0.0000032957093,0.00009449861],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996283,0.00006794635,0.000018076973,0.00008766954,0.00008675094,0.00011115101],"domain_scores_gemma":[0.99881256,0.00033139254,0.0003827532,0.00011113478,0.00019874898,0.00016335429],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00044473293,0.00015587322,0.00029985438,0.0007578394,0.0004609953,0.0023096027,0.000428765,0.00046243297,0.0020939729],"category_scores_gemma":[0.0030165222,0.00016718835,0.00024219498,0.0007833988,0.0006653208,0.0015340245,0.0005113971,0.00023954133,0.00028924938],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011281733,0.00013216773,0.85293317,0.0002936408,0.000674227,0.002686831,0.0011257434,0.00835515,0.04430193,0.015782848,0.0016638407,0.070922226],"study_design_scores_gemma":[0.000081635604,0.00013347654,0.8477832,0.00014821853,0.0002968709,0.0041276766,0.004301556,0.054582253,0.018524522,0.053938683,0.015991962,0.00008994591],"about_ca_topic_score_codex":0.00319818,"about_ca_topic_score_gemma":0.0028543388,"teacher_disagreement_score":0.00319818,"about_ca_system_score_codex":0.00059770467,"about_ca_system_score_gemma":0.00019226123,"threshold_uncertainty_score":0.007005036},"labels":[],"label_agreement":null},{"id":"W4295599277","doi":"10.1029/2022gl099848","title":"Tropopause‐Level NO<sub>x</sub> in the Asian Summer Monsoon","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Tropopause; Climatology; East Asian Monsoon; Monsoon; Environmental science; Atmospheric sciences; Meteorology; Geology; Geography; Stratosphere","score_opus":0.05141558415421741,"score_gpt":0.2855426751567265,"score_spread":0.23412709100250909,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295599277","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999342,0.000050158134,0.000050051003,0.000032208074,0.0000023401042,6.5818034e-7,0.000094225696,0.000006346635,0.00042201974],"genre_scores_gemma":[0.99974006,0.000024279758,0.00002706052,0.0000078692865,0.0000027036722,7.8406964e-7,0.00009073086,0.0000015884187,0.00010489321],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996114,0.000007088523,0.0000024486583,0.000007898683,0.0000051017482,0.000016303238],"domain_scores_gemma":[0.99985385,0.00002521823,0.000040245923,0.000007434303,0.000023940825,0.00004925854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018649336,0.00013163818,0.00012634307,0.00021386126,0.00018653854,0.0003549285,0.00012224184,0.00014424721,0.00085025217],"category_scores_gemma":[0.00024050752,0.00012470283,0.00015211699,0.00024385052,0.00015242117,0.0002671459,0.00020285095,0.00014666967,0.00012962984],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061035104,0.000062643696,0.9510957,0.00004199238,0.00008992365,0.0004158202,0.00037105058,0.0038960006,0.035621103,0.00044246123,0.0007221762,0.0066306875],"study_design_scores_gemma":[0.000011629077,0.000027175505,0.9953166,0.000003464295,0.000014240854,0.000042381827,0.0001811703,0.003564134,0.0005667063,0.00007562529,0.00019351987,0.0000033127196],"about_ca_topic_score_codex":0.02613711,"about_ca_topic_score_gemma":0.03375331,"teacher_disagreement_score":0.02613711,"about_ca_system_score_codex":0.000286315,"about_ca_system_score_gemma":0.00031735597,"threshold_uncertainty_score":0.051969945},"labels":[],"label_agreement":null},{"id":"W4295884602","doi":"10.1029/2022gl099661","title":"The Relationship Between Kimberlitic Magmatism and Electrical Conductivity Anomalies in the Mantle","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysical and Geoelectrical Methods","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Australian Research Council; Macquarie University","keywords":"Kimberlite; Metasomatism; Geology; Geochemistry; Mantle (geology); Lithosphere; Magmatism; Archean; Craton; Terrane; Igneous rock; Earth science; Petrology; Paleontology; Tectonics","score_opus":0.08732589869882948,"score_gpt":0.3359648660553084,"score_spread":0.24863896735647892,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4295884602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993437,0.00003285904,0.00018036488,0.00000869507,3.42687e-7,8.136041e-7,0.00018354342,0.000006950519,0.00024263481],"genre_scores_gemma":[0.9997507,0.000013574508,0.00008672119,0.00000107164,3.7459512e-7,4.873914e-7,0.00010659119,0.0000015207303,0.000039006412],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996257,0.0000065665713,0.0000029848122,0.000014310753,0.000005403225,0.0000081523485],"domain_scores_gemma":[0.99982566,0.000064241656,0.00004637353,0.0000140945485,0.000030379028,0.000019303769],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012035938,0.00015284542,0.00008727908,0.0008789549,0.0001397449,0.00048213688,0.00011134561,0.0001289257,0.0005309193],"category_scores_gemma":[0.0005337407,0.000111333924,0.00010630857,0.0006236706,0.00016292537,0.0002491641,0.00019070822,0.00008763737,0.00008308961],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000052942465,0.000008136221,0.9837167,0.000010312451,0.000058959897,0.00005052109,0.00007148764,0.0036860975,0.008879845,0.000110521134,0.000037570913,0.0033169026],"study_design_scores_gemma":[0.0000025614722,0.0000063046145,0.98732203,0.000003667936,0.0000135663895,0.00004631692,0.00008071038,0.010881863,0.0013082945,0.000101754915,0.00022856308,0.0000042959064],"about_ca_topic_score_codex":0.02819024,"about_ca_topic_score_gemma":0.03391711,"teacher_disagreement_score":0.02819024,"about_ca_system_score_codex":0.0004888808,"about_ca_system_score_gemma":0.00015931882,"threshold_uncertainty_score":0.056052327},"labels":[],"label_agreement":null},{"id":"W4296049041","doi":"10.1029/2022gl100147","title":"Evaluating Global Atmospheric Inversions of Terrestrial Net Ecosystem Exchange CO<sub>2</sub> Over North America on Seasonal and Sub‐Continental Scales","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Pennsylvania State University; Nuclear Safety and Security Commission; University of Pennsylvania; Colorado State University; National Aeronautics and Space Administration","keywords":"Environmental science; Inversion (geology); Observatory; Satellite; Climatology; Ecosystem; Carbon flux; Atmospheric sciences; Global change; Climate change; Oceanography; Ecology; Geology","score_opus":0.022279604886319783,"score_gpt":0.28407883153987973,"score_spread":0.2617992266535599,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296049041","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99896395,0.000017232805,0.0003592312,0.0000288037,0.0000034668417,0.000004056652,0.00025921504,0.000041221367,0.00032287533],"genre_scores_gemma":[0.99860114,0.00001229774,0.00086629903,0.0000067132046,0.0000022916631,0.0000035990402,0.00045741178,0.0000077167915,0.0000424957],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998697,0.000042432977,0.000007437272,0.000038316542,0.000018190127,0.000023947827],"domain_scores_gemma":[0.99953544,0.00017425207,0.00007700994,0.000051650575,0.00011587063,0.0000458674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000680796,0.00044369488,0.0002101887,0.00032613528,0.0002313842,0.00038527552,0.00032723128,0.00028042612,0.000402468],"category_scores_gemma":[0.0014235922,0.0002109295,0.00032688922,0.0005945122,0.00025101227,0.00062234735,0.00029695028,0.00026012716,0.000050640414],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006208797,0.00027323814,0.64182174,0.000045288507,0.00041007125,0.00015023383,0.00024088024,0.3179456,0.013842645,0.00039706597,0.0010341874,0.0232182],"study_design_scores_gemma":[0.00014712583,0.00018458415,0.37444204,0.000013629194,0.00012473481,0.000036281144,0.00041944176,0.6173951,0.005915452,0.00036565753,0.00091778516,0.00003812194],"about_ca_topic_score_codex":0.082162365,"about_ca_topic_score_gemma":0.112928264,"teacher_disagreement_score":0.082162365,"about_ca_system_score_codex":0.00061987527,"about_ca_system_score_gemma":0.00058541156,"threshold_uncertainty_score":0.16336828},"labels":[],"label_agreement":null},{"id":"W4296185672","doi":"10.1029/2022gl100912","title":"A 2D Kaleidoscope of Electron Heat Fluxes Driven by Auroral Electron Precipitation","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Electron precipitation; Substorm; Electron; Precipitation; Ionosphere; Physics; Atmospheric sciences; Flux (metallurgy); Computational physics; Heat flux; Kinetic energy; Geophysics; Environmental science; Meteorology; Magnetosphere; Plasma; Materials science; Heat transfer; Mechanics; Nuclear physics","score_opus":0.00972580838995163,"score_gpt":0.2820890574062547,"score_spread":0.27236324901630304,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296185672","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.29277676,0.00018115882,0.64247674,0.00020153564,0.00025935748,0.00028794847,0.023249147,0.016874848,0.023692576],"genre_scores_gemma":[0.8153203,0.00017383562,0.17096733,0.00007291711,0.00005046338,0.00021342422,0.007841209,0.0011020551,0.00425851],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999366,0.0000069850726,0.0000044793564,0.00002115964,0.00002284959,0.000007863481],"domain_scores_gemma":[0.9998517,0.000035958867,0.000011909451,0.000032418473,0.00005296884,0.000015107785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016034037,0.00035160233,0.0002884791,0.00075631717,0.00030695455,0.00059837813,0.00037698649,0.0003087696,0.008670692],"category_scores_gemma":[0.00045446274,0.00025550922,0.00040384385,0.00055322004,0.00013369,0.0004035977,0.00034886342,0.00040797933,0.0009486285],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006585001,0.00024866022,0.04093554,0.000378904,0.0002546748,0.0011766098,0.00070201344,0.5358616,0.2302349,0.013625631,0.03626302,0.13965993],"study_design_scores_gemma":[0.000045605084,0.000022281087,0.0173843,0.000014368078,0.000012590002,0.000116129595,0.00006268367,0.9547826,0.012759524,0.0019824791,0.012777168,0.000040272644],"about_ca_topic_score_codex":0.0054683024,"about_ca_topic_score_gemma":0.0069381483,"teacher_disagreement_score":0.008670692,"about_ca_system_score_codex":0.00026928243,"about_ca_system_score_gemma":0.00034050725,"threshold_uncertainty_score":0.029006362},"labels":[],"label_agreement":null},{"id":"W4296203942","doi":"10.1029/2022gl099017","title":"Summer Midlatitude Stationary Wave Patterns Synchronize Northern Hemisphere Wildfire Occurrence","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Canadian Forest Service; Australian Research Council; National Center for Atmospheric Research; Institute for Basic Science; National Science Foundation; University of Cambridge; U.S. Forest Service","keywords":"Middle latitudes; Climatology; Northern Hemisphere; Atmospheric sciences; Troposphere; Environmental science; Atmospheric circulation; Latitude; Southern Hemisphere; Atmospheric wave; Rossby wave; Geology; Wave propagation; Gravity wave; Physics","score_opus":0.05367729346058218,"score_gpt":0.3076490307606144,"score_spread":0.2539717373000322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296203942","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99719304,0.000028142624,0.0008974231,0.000023564462,0.0000061735354,0.000003163187,0.0004929088,0.00004013132,0.0013155072],"genre_scores_gemma":[0.99939525,0.000010923987,0.0001635015,0.0000034563654,0.0000025792058,0.0000015311982,0.00029581404,0.0000043506443,0.00012261039],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999566,0.0000059390586,0.000002972157,0.000012534293,0.0000086862265,0.000013278504],"domain_scores_gemma":[0.99978465,0.0000389294,0.000070828835,0.000028292856,0.00004250595,0.00003474019],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013540375,0.00009123532,0.0001247918,0.00029009697,0.00013351966,0.00028591673,0.00010715791,0.000112795555,0.0019604045],"category_scores_gemma":[0.00062159216,0.00006308044,0.00015062686,0.00021277979,0.00009050304,0.00018812915,0.00018027071,0.00013762877,0.00017447927],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033751724,0.000102223086,0.8940615,0.000042322015,0.00014166835,0.00016983689,0.00028964714,0.045537658,0.02578761,0.0010346655,0.002602172,0.029893182],"study_design_scores_gemma":[0.000008472252,0.000023035613,0.96405023,0.0000039081165,0.0000102878685,0.000023316043,0.000068811,0.03419096,0.00078059355,0.00041881498,0.00041566632,0.0000057431134],"about_ca_topic_score_codex":0.007829053,"about_ca_topic_score_gemma":0.010653872,"teacher_disagreement_score":0.007829053,"about_ca_system_score_codex":0.00014924166,"about_ca_system_score_gemma":0.00014431709,"threshold_uncertainty_score":0.015566945},"labels":[],"label_agreement":null},{"id":"W4296208938","doi":"10.1029/2022gl099333","title":"Molecular Dynamics Simulation of Solar Wind Implantation in the Permanently Shadowed Regions on the Lunar Surface","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Solar wind; Astrobiology; Sputtering; Environmental science; Molecule; Materials science; Atmospheric sciences; Plasma; Physics; Nanotechnology; Thin film","score_opus":0.035905481442057734,"score_gpt":0.3054418790163044,"score_spread":0.26953639757424663,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296208938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9911628,0.00008600184,0.001706788,0.00026606364,0.00003575867,0.000029691608,0.0005012237,0.0000754282,0.0061362586],"genre_scores_gemma":[0.99700326,0.00006749058,0.0012203003,0.000066467124,0.000009046354,0.000043140622,0.00044756828,0.00003248918,0.0011102731],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998714,0.00002445042,0.0000036700424,0.000017214477,0.000028489478,0.00005481821],"domain_scores_gemma":[0.999514,0.00024568875,0.000044284512,0.0000305208,0.00008049645,0.00008497726],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002558288,0.0005723275,0.0009082075,0.0005299756,0.0009786792,0.0008806377,0.00089096115,0.0013992172,0.004023225],"category_scores_gemma":[0.0009997097,0.0004265416,0.0007780004,0.0006851005,0.0008310454,0.00061050855,0.0005573592,0.00095621235,0.00022673748],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018910642,0.00014804679,0.004526194,0.00003772298,0.000065033855,0.00023744267,0.00007897953,0.98863494,0.0027096914,0.0018831545,0.00041589013,0.0010737625],"study_design_scores_gemma":[0.000059211725,0.00006240028,0.0016251795,0.000004038322,0.000009846866,0.000009623022,0.000065224776,0.99732697,0.00038086477,0.00024242104,0.00020511157,0.0000090124295],"about_ca_topic_score_codex":0.023905091,"about_ca_topic_score_gemma":0.012241569,"teacher_disagreement_score":0.023905091,"about_ca_system_score_codex":0.0011255844,"about_ca_system_score_gemma":0.0011567665,"threshold_uncertainty_score":0.047531903},"labels":[],"label_agreement":null},{"id":"W4296335838","doi":"10.1029/2022gl099808","title":"The Influence of Transport Stage on Preserved Fluvial Cross Strata","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological formations and processes","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University; BC Hydro (Canada)","funders":"American Chemical Society; University of California; National Science Foundation","keywords":"Bedform; Fluvial; Geology; Stage (stratigraphy); Sediment transport; Flow (mathematics); Sediment; Geomorphology; Trough (economics); Sedimentary depositional environment; Paleontology; Geometry; Mathematics","score_opus":0.04691653195099677,"score_gpt":0.30927759145665734,"score_spread":0.2623610595056606,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296335838","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996898,0.000016633265,0.000095413794,0.0000010668822,5.6134274e-7,0.0000016940094,0.000054260927,0.0000024244468,0.00013808628],"genre_scores_gemma":[0.9995746,0.000009839531,0.0000907978,0.0000024651476,4.6312968e-7,0.000003288872,0.000078795514,0.000002935781,0.0002367874],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999399,0.000010672799,0.0000043080654,0.0000176143,0.000011962491,0.000015595499],"domain_scores_gemma":[0.99975544,0.000059407663,0.00004953784,0.000039324234,0.000041072388,0.000055174143],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000111925874,0.00015928084,0.00010423014,0.0002186311,0.00017769024,0.00030961502,0.00013182573,0.00013297916,0.0014116311],"category_scores_gemma":[0.00028923037,0.00013122398,0.00012921667,0.00012414259,0.00032677766,0.0002213081,0.0002567855,0.00025860858,0.000096848315],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011867281,0.0001156128,0.073993415,0.000028108007,0.000035029756,0.00006350993,0.00024553455,0.00068488263,0.9180332,0.00013160327,0.00004156765,0.0054408005],"study_design_scores_gemma":[0.000014727365,0.00067483145,0.8181321,0.000006506566,0.000031193715,0.00008027525,0.00016480635,0.0024184652,0.17802916,0.00007008198,0.0003671692,0.000010574372],"about_ca_topic_score_codex":0.002281917,"about_ca_topic_score_gemma":0.0032720754,"teacher_disagreement_score":0.002281917,"about_ca_system_score_codex":0.0002515837,"about_ca_system_score_gemma":0.00010013196,"threshold_uncertainty_score":0.004722357},"labels":[],"label_agreement":null},{"id":"W4296622905","doi":"10.1029/2022gl100014","title":"Geospace Concussion: Global Reversal of Ionospheric Vertical Plasma Drift in Response to a Sudden Commencement","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Aeronautics and Space Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Ionosphere; Geophysics; Physics; Interplanetary magnetic field; Interplanetary spaceflight; Geology; Plasma; Geodesy; Atmospheric sciences; Solar wind","score_opus":0.015111632676614318,"score_gpt":0.2994391822181251,"score_spread":0.2843275495415108,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4296622905","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99589866,0.000043521068,0.0006210432,0.00010920523,0.00002767457,0.000007198787,0.00052506715,0.00010475757,0.0026629458],"genre_scores_gemma":[0.99895215,0.000021434216,0.00021258218,0.000012624979,0.000006572855,0.0000020316966,0.0004985399,0.000007754079,0.0002862298],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99996173,0.0000039733204,0.0000019542013,0.000010656067,0.000011482346,0.000010246834],"domain_scores_gemma":[0.9999281,0.000010301191,0.000015827329,0.000010707939,0.000012835184,0.000022193712],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008557355,0.00024845623,0.00016268878,0.00023724316,0.00022810658,0.00039195784,0.00025383456,0.000289899,0.0019026108],"category_scores_gemma":[0.00024802214,0.00008863869,0.0002560865,0.00024173335,0.00022985689,0.00030250754,0.00045334297,0.00025132383,0.00013765608],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0018764341,0.0002957123,0.36146536,0.00019322743,0.00040142395,0.0031347373,0.00056709896,0.51004636,0.06490941,0.005250728,0.012354706,0.039504863],"study_design_scores_gemma":[0.00022711829,0.00040376236,0.39181143,0.000019025196,0.000074364994,0.00023378272,0.00053520844,0.5858358,0.013646437,0.00192328,0.0052337986,0.000055835993],"about_ca_topic_score_codex":0.014327371,"about_ca_topic_score_gemma":0.013744112,"teacher_disagreement_score":0.014327371,"about_ca_system_score_codex":0.00029181485,"about_ca_system_score_gemma":0.00029507017,"threshold_uncertainty_score":0.02848798},"labels":[],"label_agreement":null},{"id":"W4297341748","doi":"10.1029/2022gl100505","title":"Causes of Missing Snowmelt Following Drought","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":30,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Oak Ridge Institute for Science and Education; Simon Fraser University","keywords":"Snowmelt; Snowpack; Streamflow; Surface runoff; Evapotranspiration; Environmental science; Water year; Hydrology (agriculture); Precipitation; Snow; Meltwater; Subsurface flow; Climate change; Drainage basin; Climatology; Groundwater; Geology; Meteorology; Geography; Oceanography; Ecology","score_opus":0.060501755861400205,"score_gpt":0.30711663781641835,"score_spread":0.24661488195501813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4297341748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99714154,0.00018622552,0.00042914602,0.00072157325,0.00002203091,0.000007019496,0.00070833106,0.00003434178,0.00074977166],"genre_scores_gemma":[0.9997317,0.000022350743,0.000039077382,0.000016259191,0.000008562757,0.0000015436063,0.0001352923,0.0000025072222,0.00004261256],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99950993,0.00011300434,0.000050108036,0.00011272846,0.00009469416,0.00011950399],"domain_scores_gemma":[0.9960295,0.001051256,0.0015768643,0.00027348695,0.0005749748,0.0004940291],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013263772,0.00013796594,0.0003407984,0.00081276766,0.0006276399,0.00073213346,0.0005030197,0.00071852264,0.002323589],"category_scores_gemma":[0.005732999,0.00022513734,0.00035334376,0.0007380205,0.0004914054,0.000629257,0.00092511997,0.0007042415,0.00013784286],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001834409,0.000035596182,0.9855267,0.000038614646,0.000072092895,0.00038204447,0.00024189778,0.0050439155,0.00058828533,0.00050270837,0.001038824,0.006345924],"study_design_scores_gemma":[0.000018040846,0.00005403056,0.9715176,0.000030957326,0.00002885851,0.0003052635,0.0008431273,0.023526449,0.0004123493,0.0023009726,0.0009478423,0.000014482257],"about_ca_topic_score_codex":0.009695401,"about_ca_topic_score_gemma":0.01350022,"teacher_disagreement_score":0.009695401,"about_ca_system_score_codex":0.00089061534,"about_ca_system_score_gemma":0.00052180735,"threshold_uncertainty_score":0.01927793},"labels":[],"label_agreement":null},{"id":"W4302774290","doi":"10.1029/2022gl100202","title":"Using CMIP6 Models to Assess the Significance of the Observed Trend in the Atlantic Meridional Overturning Circulation","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Climatology; Coupled model intercomparison project; Climate model; Zonal and meridional; Environmental science; Series (stratigraphy); Climate system; Geology; Climate change; Atmospheric sciences; Oceanography","score_opus":0.266314838845753,"score_gpt":0.3509670925008105,"score_spread":0.08465225365505746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4302774290","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9920168,0.00008412787,0.0029680768,0.0002503504,0.000038057467,0.000017574994,0.0025616353,0.0003100565,0.0017533452],"genre_scores_gemma":[0.9937627,0.000071030954,0.0031077152,0.000036542548,0.000019525469,0.000026800168,0.0025080203,0.000076355456,0.0003912648],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999666,0.00015644242,0.000018952953,0.000072255534,0.00004090189,0.0000455514],"domain_scores_gemma":[0.99779737,0.0014041911,0.00018564663,0.0002120054,0.0002621595,0.00013857945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019017208,0.0008969637,0.00037628584,0.00055906497,0.0004613129,0.0008596211,0.0009182084,0.0008078099,0.0020405448],"category_scores_gemma":[0.0043055816,0.0003427449,0.0008064263,0.0010221462,0.00030032214,0.00082142773,0.00054132316,0.00094125455,0.00040708075],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004842287,0.00017041022,0.08419701,0.00006590934,0.0003534425,0.00010187048,0.000054339678,0.9048936,0.0014802398,0.0010621214,0.0017685369,0.0053683077],"study_design_scores_gemma":[0.000071771196,0.000071023234,0.020612415,0.000008288888,0.000045791985,0.000018123947,0.0000331894,0.977249,0.0010108055,0.0004262378,0.00043802016,0.000015194376],"about_ca_topic_score_codex":0.03903915,"about_ca_topic_score_gemma":0.020385401,"teacher_disagreement_score":0.03903915,"about_ca_system_score_codex":0.00076278986,"about_ca_system_score_gemma":0.00061048527,"threshold_uncertainty_score":0.077623785},"labels":[],"label_agreement":null},{"id":"W4306751384","doi":"10.1029/2022gl100136","title":"Freshwater Flux Variability Lengthens the Period of the Low‐Frequency AMOC Variability","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Lawrence Berkeley National Laboratory; Office of Science; National Natural Science Foundation of China; National Energy Research Scientific Computing Center; Polit National Laboratory for Marine Science and Technology; U.S. Department of Energy","keywords":"Anomaly (physics); Climatology; Forcing (mathematics); Flux (metallurgy); Salinity; Environmental science; Period (music); Geology; Madden–Julian oscillation; Lead (geology); Oceanography; Atmospheric sciences; Convection; Geography; Physics","score_opus":0.017007805627175195,"score_gpt":0.2419724292921513,"score_spread":0.2249646236649761,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4306751384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99945027,0.000013756109,0.00020131956,0.000012933085,0.0000037853658,0.0000024961232,0.000043799617,0.000010768623,0.0002609255],"genre_scores_gemma":[0.99974686,0.000008457413,0.00009120341,0.000011105849,0.000002771729,0.0000042872393,0.000040672,0.000003538948,0.00009105792],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99993014,0.000011213619,0.0000045271954,0.000025528518,0.00000881211,0.000019815245],"domain_scores_gemma":[0.9998087,0.000039157545,0.000041181967,0.000037505768,0.000015536778,0.00005785659],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013548952,0.00015529967,0.00018928394,0.00013094411,0.0001877387,0.00029119593,0.00009858019,0.00012690222,0.0006673832],"category_scores_gemma":[0.00039450527,0.00009610562,0.00021234526,0.00007622064,0.00020303264,0.00018675816,0.00036207886,0.00028842269,0.000063434716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017112879,0.00025193053,0.16349158,0.000045308305,0.00019355699,0.00012280807,0.00025165916,0.0033133333,0.81462854,0.00068184227,0.0002534874,0.01505474],"study_design_scores_gemma":[0.000049774317,0.0005049447,0.9624825,0.00000480397,0.00006614256,0.000044830245,0.00009519352,0.007629017,0.027726656,0.00021660376,0.0011661558,0.000013225332],"about_ca_topic_score_codex":0.0050224694,"about_ca_topic_score_gemma":0.0056950287,"teacher_disagreement_score":0.0050224694,"about_ca_system_score_codex":0.0003112888,"about_ca_system_score_gemma":0.0002670196,"threshold_uncertainty_score":0.00998646},"labels":[],"label_agreement":null},{"id":"W4307139384","doi":"10.1029/2022gl099393","title":"Multidecadal Variation in the Seasonal Predictability of Winter PNA and Its Sources","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Hohai University; Fundamental Research Funds for the Central Universities; National Science Foundation","keywords":"Predictability; Extratropical cyclone; Climatology; Teleconnection; El Niño Southern Oscillation; Environmental science; Seasonality; Southern oscillation; Geology; Mathematics; Ecology; Biology","score_opus":0.036237269331624515,"score_gpt":0.29912161248143265,"score_spread":0.26288434314980813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307139384","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9967269,0.00015335256,0.0008117504,0.00005774176,0.000020008776,0.0000018217685,0.0014423042,0.00004478636,0.00074141816],"genre_scores_gemma":[0.99849474,0.00005398956,0.00016104367,0.000006478725,0.0000105034205,0.000002796304,0.001102235,0.0000063931775,0.00016183859],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999471,0.000009514005,0.0000047814697,0.000018097797,0.000012198691,0.000008444664],"domain_scores_gemma":[0.99963856,0.00011489604,0.000075900236,0.000036631478,0.000089551475,0.00004452257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00034472384,0.00016318065,0.00014016916,0.0004486897,0.00014743739,0.0004959742,0.00010810532,0.00013233013,0.00079984847],"category_scores_gemma":[0.0006110473,0.000089760186,0.00023511586,0.0004434777,0.00008721992,0.00025019536,0.00027082235,0.00024511415,0.0001326657],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003338642,0.00008973364,0.9047274,0.000050239236,0.0005291583,0.00015283858,0.00014689066,0.0521873,0.010999179,0.0010337443,0.002690666,0.027058998],"study_design_scores_gemma":[0.000009825211,0.00003285002,0.9355283,0.000009892644,0.000047490714,0.000036388614,0.00005725459,0.061384235,0.001179337,0.00035304847,0.0013487235,0.000012668473],"about_ca_topic_score_codex":0.0072069108,"about_ca_topic_score_gemma":0.008002146,"teacher_disagreement_score":0.0072069108,"about_ca_system_score_codex":0.00018763026,"about_ca_system_score_gemma":0.00015257603,"threshold_uncertainty_score":0.01432991},"labels":[],"label_agreement":null},{"id":"W4307139954","doi":"10.1029/2022gl100835","title":"The Role of Wave Breaking in the Development and Subseasonal Forecasts of the February 2021 Great Plains Cold Air Outbreak","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Predictability; Climatology; Anticyclone; Environmental science; Cold wave; Range (aeronautics); Meteorology; Forecast skill; Outbreak; Extreme Cold; Event (particle physics); Geography; Geology","score_opus":0.0323535433438504,"score_gpt":0.26434713213771077,"score_spread":0.23199358879386037,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307139954","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978715,0.000038620023,0.00043213807,0.00021102023,0.000019059842,0.0000076772685,0.00025959243,0.00005081287,0.0011095646],"genre_scores_gemma":[0.9994399,0.000017462724,0.00019427024,0.00001043485,0.000008719209,0.000002792496,0.00022386527,0.000005285231,0.00009724054],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999007,0.00002914292,0.0000076945535,0.000023307599,0.000018054776,0.000021082702],"domain_scores_gemma":[0.99946135,0.00018951739,0.00010400614,0.00004466134,0.00009621886,0.000104148574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005739702,0.00032979317,0.0002020327,0.00034652487,0.00032114342,0.0010438015,0.00029602228,0.0005316201,0.00094165595],"category_scores_gemma":[0.0022369323,0.00018761719,0.00028833636,0.0002674239,0.00020303536,0.00049515493,0.00040712112,0.00060124596,0.00011565513],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002625994,0.00015321188,0.4162216,0.000018958235,0.00013793363,0.00021011378,0.00010978638,0.56564045,0.0034645097,0.0006702489,0.0019707715,0.011139804],"study_design_scores_gemma":[0.00004480016,0.000048213857,0.15363927,0.000009264382,0.000028288352,0.000015301035,0.00012650048,0.8446914,0.000643556,0.00028087714,0.00045641264,0.00001607603],"about_ca_topic_score_codex":0.08975815,"about_ca_topic_score_gemma":0.06542521,"teacher_disagreement_score":0.08975815,"about_ca_system_score_codex":0.0007257886,"about_ca_system_score_gemma":0.00066569407,"threshold_uncertainty_score":0.17847139},"labels":[],"label_agreement":null},{"id":"W4307564328","doi":"10.1029/2022gl099995","title":"Small Magnitude Events Highlight the Correlation Between Hydraulic Fracturing Injection Parameters, Geological Factors, and Earthquake Occurrence","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Deutsche Forschungsgemeinschaft","keywords":"Hydraulic fracturing; Geology; Seismology; Induced seismicity; Magnitude (astronomy); Structural basin; Maximum magnitude; Fault (geology); Earthquake prediction; Petroleum engineering; Paleontology","score_opus":0.06648559747517907,"score_gpt":0.2746445716022773,"score_spread":0.20815897412709822,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4307564328","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997212,0.000023419241,0.00037463443,0.000019066381,0.0000010929514,0.0000066979037,0.0010520016,0.000018997212,0.0012920359],"genre_scores_gemma":[0.9990233,0.000010868255,0.00017718996,0.0000025714564,6.3799814e-7,0.0000016191591,0.0004886587,0.000001734899,0.00029343384],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998698,0.00001751912,0.000013068515,0.00003177147,0.000033941724,0.000033741497],"domain_scores_gemma":[0.9988072,0.0003755296,0.0003364032,0.00009433599,0.0002724046,0.00011414351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016943821,0.0001436348,0.00012316581,0.0009756064,0.0003368057,0.0005342489,0.00014516574,0.00012379127,0.0020222082],"category_scores_gemma":[0.0018232855,0.0000656912,0.00007934926,0.001212712,0.00022323069,0.00017940786,0.00026070766,0.00016504247,0.00017445233],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002323562,0.0000075376834,0.99315006,0.0000048575926,0.0000121244175,0.000036537545,0.000079645964,0.0005332819,0.000923683,0.000037967893,0.00017074552,0.005020316],"study_design_scores_gemma":[3.6552217e-7,0.000003052024,0.9988483,0.0000011359166,0.000002498958,0.000012080513,0.000114217466,0.00074932084,0.000107145024,0.000013888484,0.00014680703,0.0000011176662],"about_ca_topic_score_codex":0.5034946,"about_ca_topic_score_gemma":0.8142572,"teacher_disagreement_score":0.5034946,"about_ca_system_score_codex":0.000779029,"about_ca_system_score_gemma":0.001013996,"threshold_uncertainty_score":0.9988588},"labels":[],"label_agreement":null},{"id":"W4308025962","doi":"10.1029/2022gl101472","title":"Abrupt Northern Baffin Bay Autumn Warming and Sea‐Ice Loss Since the Turn of the Twenty‐First Century","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; University of Toronto","funders":"","keywords":"Bay; Arctic ice pack; Sea ice; Oceanography; Geology; Arctic; Cryosphere; Climatology; Antarctic sea ice; Drift ice; Fast ice","score_opus":0.013835545627276619,"score_gpt":0.24041570445880164,"score_spread":0.22658015883152502,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308025962","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956145,0.00027539046,0.00003528835,0.0007495221,0.00002728985,0.0000024863132,0.0003997411,0.0000067463166,0.0028890553],"genre_scores_gemma":[0.9981998,0.00015203144,0.000035142035,0.00013899159,0.00002346718,0.0000035168505,0.00026645986,0.000001553424,0.0011789938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987483,0.000009775805,0.0000071726513,0.00003337529,0.000035774647,0.0000391074],"domain_scores_gemma":[0.999498,0.000025410947,0.0001725764,0.00002185015,0.00014417633,0.00013805466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002944059,0.00013890355,0.00012571587,0.00056557317,0.00072900334,0.0009833913,0.0002579619,0.00037555065,0.002484547],"category_scores_gemma":[0.00063418015,0.00008951606,0.00009359887,0.00045475634,0.00051911955,0.0003569645,0.000510597,0.00031097437,0.00023515242],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016757498,0.00004309958,0.97652286,0.000051023573,0.00004687047,0.00045704556,0.001313089,0.00020562089,0.004882783,0.00035476504,0.0027985636,0.013156651],"study_design_scores_gemma":[0.0000013796971,0.000007538126,0.9973477,0.0000063724247,0.0000031212544,0.00003368943,0.00025841978,0.00004629709,0.00013330401,0.000015253537,0.0021446985,0.0000021652404],"about_ca_topic_score_codex":0.1664833,"about_ca_topic_score_gemma":0.31795323,"teacher_disagreement_score":0.1664833,"about_ca_system_score_codex":0.0020719978,"about_ca_system_score_gemma":0.0011769101,"threshold_uncertainty_score":0.33102846},"labels":[],"label_agreement":null},{"id":"W4308029469","doi":"10.1029/2022gl100937","title":"Changes in Deep Ocean Contribute to a “See‐Sawing” Gulf Stream Path","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Gulf Stream; Empirical orthogonal functions; Geology; Seamount; Water mass; Satellite altimetry; Altimeter; Longitude; Oceanography; Geodesy; Zonal and meridional; Latitude; Climatology","score_opus":0.019566054627456038,"score_gpt":0.26085086144696223,"score_spread":0.2412848068195062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308029469","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987418,0.000022088097,0.00006478521,0.0001018271,0.0000063464895,0.0000023356495,0.00007172608,0.000004654155,0.0009844727],"genre_scores_gemma":[0.9995185,0.00003909126,0.00007225398,0.00001895491,0.000005888686,9.3213333e-7,0.000073636416,0.0000013473058,0.00026948086],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994993,0.000007106922,0.000004067834,0.000011053766,0.000015515781,0.0000123085265],"domain_scores_gemma":[0.99972147,0.000044034598,0.00010078283,0.00002136086,0.00006733135,0.000044953573],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017764213,0.000106484404,0.00008459845,0.0003421985,0.00023450734,0.00040598286,0.000085970394,0.00018178692,0.0017772018],"category_scores_gemma":[0.00071952405,0.00008195363,0.00012984152,0.00035339512,0.00029075844,0.00020709078,0.0004044167,0.00025357332,0.00010743548],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009549709,0.00003749823,0.9731322,0.000016787479,0.000027669903,0.00020290575,0.00040601534,0.0009429864,0.007684516,0.0004495031,0.0005240492,0.016480368],"study_design_scores_gemma":[0.0000017758736,0.000013023663,0.99835396,0.000003405334,0.0000047694875,0.00002614173,0.00017624034,0.00054932345,0.00022106459,0.00007395251,0.0005746414,0.0000017800107],"about_ca_topic_score_codex":0.014652567,"about_ca_topic_score_gemma":0.027051138,"teacher_disagreement_score":0.014652567,"about_ca_system_score_codex":0.0003607446,"about_ca_system_score_gemma":0.0003286723,"threshold_uncertainty_score":0.029134572},"labels":[],"label_agreement":null},{"id":"W4308149271","doi":"10.1029/2022gl100924","title":"An Interannual Drought Feedback Loop Affects the Surface Energy Balance and Cloud Properties","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Drought Analysis","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"","keywords":"Environmental science; Positive feedback; Climate model; Cloud feedback; Climate change; Groundwater; Climatology; Earth system science; Water balance; Atmosphere (unit); Feedback loop; Probabilistic logic; Negative feedback; Atmospheric sciences; Meteorology; Climate sensitivity; Geology; Computer science; Geography","score_opus":0.01610840386896859,"score_gpt":0.26270732029510574,"score_spread":0.24659891642613715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308149271","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99458545,0.00008399948,0.0037239213,0.00017230201,0.000017857321,0.0000034945954,0.00027044187,0.00009266726,0.0010497288],"genre_scores_gemma":[0.9997453,0.0000143366815,0.00012196027,0.000008392032,0.0000019929896,8.8313305e-7,0.000040274765,0.0000056523936,0.000061180835],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999151,0.000023156654,0.0000045533016,0.000027216598,0.000008895799,0.00002097087],"domain_scores_gemma":[0.9997067,0.00014358657,0.000052797866,0.000022786979,0.000037433227,0.000036706577],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031017937,0.00017307977,0.00018807912,0.00021971234,0.00018384942,0.0006811656,0.00021625005,0.0003699834,0.0017358721],"category_scores_gemma":[0.00095926237,0.0001427292,0.00023541399,0.00020411242,0.00018086367,0.00065736007,0.0003724562,0.0003286673,0.00009700212],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00067929534,0.00032067078,0.25608915,0.00010475561,0.0005272122,0.00049166917,0.0002079265,0.5901469,0.10188386,0.01237142,0.0030024927,0.034174677],"study_design_scores_gemma":[0.00005351887,0.000056732748,0.13943052,0.00000836339,0.00008456799,0.000054109005,0.00010218646,0.8497741,0.004546071,0.004789906,0.0010691778,0.00003076665],"about_ca_topic_score_codex":0.004423518,"about_ca_topic_score_gemma":0.0022300964,"teacher_disagreement_score":0.004423518,"about_ca_system_score_codex":0.0003951653,"about_ca_system_score_gemma":0.00028229342,"threshold_uncertainty_score":0.008795559},"labels":[],"label_agreement":null},{"id":"W4308149819","doi":"10.1029/2022gl100446","title":"Challenging Radiocarbon Chronostratigraphies in Central Arctic Ocean Sediment","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Holocene; Oceanography; Radiocarbon dating; Sediment; Arctic; Sedimentary rock; Glacial period; Winnowing; Paleontology; Archaeology","score_opus":0.027529165041937302,"score_gpt":0.2678522424993983,"score_spread":0.240323077457461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308149819","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951656,0.0010569176,0.0007233174,0.000030939234,0.00002989579,0.000006428442,0.000755951,0.000015518728,0.0022154788],"genre_scores_gemma":[0.99789196,0.00025023604,0.0008315999,0.000015502823,0.000009431685,0.0000061207206,0.00064666505,0.000008012486,0.00034049986],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995474,0.00011683228,0.000061199535,0.0001334549,0.00007302592,0.00006799621],"domain_scores_gemma":[0.9975515,0.0004569159,0.0007269327,0.00028433205,0.00089174364,0.000088590044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019217556,0.00024223563,0.00014218542,0.0035040015,0.00064543943,0.0011499226,0.00028867938,0.00017112339,0.0005485203],"category_scores_gemma":[0.0032215193,0.00016973625,0.00013802253,0.0038212133,0.00032289425,0.0003752933,0.0003456278,0.00018992393,0.00016890332],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016637481,0.000013429281,0.9522939,0.00008022498,0.00012423082,0.00023848187,0.0015069372,0.0014520821,0.0042283274,0.0006886062,0.0004774662,0.038729947],"study_design_scores_gemma":[0.0000014866379,0.000015369531,0.9944267,0.000035896617,0.00002303713,0.00009004232,0.0006176799,0.00071759964,0.0007521015,0.00009954988,0.003215252,0.0000052366254],"about_ca_topic_score_codex":0.1246177,"about_ca_topic_score_gemma":0.25648332,"teacher_disagreement_score":0.1246177,"about_ca_system_score_codex":0.000761844,"about_ca_system_score_gemma":0.00077909906,"threshold_uncertainty_score":0.24778467},"labels":[],"label_agreement":null},{"id":"W4308593435","doi":"10.1029/2022gl100276","title":"Depth‐Dependent Crustal Stress Rotation and Strength Variation in the Charlevoix Seismic Zone (CSZ), Québec, Canada","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Intraplate earthquake; Crust; Seismology; Induced seismicity; Tectonics; Clockwise; Cauchy stress tensor; Focal mechanism; Inversion (geology); Stress (linguistics); Geophysics; Geodesy; Rotation (mathematics); Geometry","score_opus":0.020651083827161597,"score_gpt":0.24596223423463545,"score_spread":0.22531115040747385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4308593435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9912401,0.00022389121,0.00018843214,0.00012910031,0.0000053403533,0.000014741617,0.0049714735,0.000035684192,0.0031913186],"genre_scores_gemma":[0.99603266,0.00008554028,0.00018550997,0.000024935647,0.0000017322525,0.000006341352,0.0021843673,0.0000067817714,0.001472087],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997894,0.000014662078,0.000008344009,0.000048305214,0.00006332227,0.00007596825],"domain_scores_gemma":[0.9989477,0.00007402918,0.00012032187,0.000037673268,0.00063566735,0.00018469941],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002798535,0.00028607706,0.00020365462,0.0012628813,0.0009572652,0.00086153625,0.0005929193,0.00022545827,0.0023373454],"category_scores_gemma":[0.00086459506,0.00015406222,0.00015897494,0.0018256154,0.00053635053,0.00020537237,0.0003664947,0.00027385767,0.00023350112],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016781302,0.00003863714,0.9717065,0.000038338945,0.00009819516,0.00011830983,0.00067102717,0.0028178259,0.004566082,0.00028550587,0.003386107,0.016105628],"study_design_scores_gemma":[0.0000056317463,0.000004513357,0.99762684,0.000007699455,0.000005946563,0.000009116623,0.00030396876,0.0010077449,0.0001552525,0.000009753734,0.0008578074,0.0000056991535],"about_ca_topic_score_codex":0.99618834,"about_ca_topic_score_gemma":0.9982344,"teacher_disagreement_score":0.017189795,"about_ca_system_score_codex":0.017189795,"about_ca_system_score_gemma":0.008953372,"threshold_uncertainty_score":0.12472129},"labels":[],"label_agreement":null},{"id":"W4309070484","doi":"10.1029/2022gl100703","title":"Increasing Drought Risks Over the Past Four Centuries Amidst Projected Flood Intensification in the Kabul River Basin (Afghanistan and Pakistan)—Evidence From Tree Rings","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"","keywords":"Flood myth; Monsoon; Structural basin; Precipitation; Drainage basin; Geography; Shadow (psychology); Water resource management; Physical geography; Environmental science; Climatology; Geology; Cartography; Archaeology; Meteorology; Geomorphology","score_opus":0.06981684730186953,"score_gpt":0.318438446665915,"score_spread":0.24862159936404543,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309070484","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992424,0.000023586626,0.00013551113,0.000031625485,0.0000018475018,9.2607564e-7,0.00028852248,0.000004523936,0.00027097098],"genre_scores_gemma":[0.9996536,0.00002355121,0.00006865631,0.0000040998293,0.0000021610806,0.0000012368663,0.00020926744,0.0000012222769,0.00003628645],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998516,0.000045396217,0.00001014131,0.000035702924,0.000017890652,0.000039273218],"domain_scores_gemma":[0.9994198,0.00014993211,0.00019686487,0.00007300315,0.00010279722,0.00005759328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054623035,0.00015207825,0.00010979058,0.00060581986,0.0003412511,0.00064335164,0.0002292917,0.00021395425,0.0012003079],"category_scores_gemma":[0.0010929779,0.00011100942,0.00016154117,0.00088053074,0.00031907915,0.00045679553,0.0003295455,0.00023332732,0.00018716049],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009222663,0.000021659333,0.9843858,0.00001425222,0.00010072415,0.00015718289,0.0004213543,0.005249258,0.0009357938,0.00021574448,0.00041613574,0.007989863],"study_design_scores_gemma":[0.0000042035867,0.000025290792,0.9928214,0.000008472129,0.000025151672,0.00008387929,0.0006152219,0.005333882,0.0002943905,0.00013905001,0.0006405079,0.000008601575],"about_ca_topic_score_codex":0.01290498,"about_ca_topic_score_gemma":0.019010471,"teacher_disagreement_score":0.01290498,"about_ca_system_score_codex":0.0003064782,"about_ca_system_score_gemma":0.00024711527,"threshold_uncertainty_score":0.02565974},"labels":[],"label_agreement":null},{"id":"W4309116386","doi":"10.1029/2022gl101027","title":"Relative Timing of the Ends of Hurricane Intensification and Contraction of the Radius of Maximum Wind in the North Atlantic and Eastern North Pacific","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"Fundamental Research Funds for the Central Universities; National Key Research and Development Program of China; China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Tropical cyclone; Intensity (physics); Climatology; Environmental science; RADIUS; Atlantic hurricane; Atmospheric sciences; Geology; Meteorology; Physics; Optics","score_opus":0.03615711617518479,"score_gpt":0.25974803616347353,"score_spread":0.22359091998828873,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309116386","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99879116,0.000059601523,0.00006811682,0.000018063125,0.0000027948727,0.0000019892977,0.00038312643,0.0000031540753,0.0006721588],"genre_scores_gemma":[0.99858284,0.000039874205,0.0000598359,0.0000063142643,0.0000057667035,0.0000032459434,0.0011022212,0.0000017742287,0.00019824633],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998259,0.00002383825,0.000018962568,0.000055149412,0.000038864157,0.00003730514],"domain_scores_gemma":[0.9984835,0.00032561677,0.00062418,0.00006319809,0.00027302338,0.0002305103],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004268104,0.00010112396,0.0001524056,0.00064830744,0.00021650587,0.0004665627,0.00010547402,0.00012734601,0.0009127363],"category_scores_gemma":[0.0016947759,0.00009158173,0.00015792038,0.00047471919,0.00017226281,0.00027743488,0.00041877272,0.00026581433,0.00013936525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006683922,0.000007185276,0.9969023,0.0000067753977,0.000029352866,0.000035741297,0.00011432657,0.0001977859,0.00063294027,0.000042446147,0.00014364702,0.001820617],"study_design_scores_gemma":[4.644759e-7,0.000005469021,0.9996123,0.0000015856444,0.0000019180152,0.00001152304,0.00008519068,0.00014727072,0.00003686103,0.0000044962794,0.000092172486,8.8793195e-7],"about_ca_topic_score_codex":0.012016948,"about_ca_topic_score_gemma":0.03000292,"teacher_disagreement_score":0.012016948,"about_ca_system_score_codex":0.00018690334,"about_ca_system_score_gemma":0.00022209021,"threshold_uncertainty_score":0.023894012},"labels":[],"label_agreement":null},{"id":"W4309189448","doi":"10.1029/2022gl100950","title":"Enhanced India‐Africa Carbon Uptake and Asia‐Pacific Carbon Release Associated With the 2019 Extreme Positive Indian Ocean Dipole","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Environment and Climate Change Canada","funders":"Nanjing University","keywords":"Indian Ocean Dipole; Carbon cycle; Environmental science; Biome; Primary production; Climatology; Indian ocean; Carbon fibers; Carbon flux; Atmospheric sciences; South asia; Productivity; Ecosystem; Oceanography; El Niño Southern Oscillation; Geology; Biology; Ecology; Materials science","score_opus":0.02165091371947054,"score_gpt":0.24434493697882617,"score_spread":0.22269402325935564,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309189448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99795306,0.000036978774,0.00031953378,0.00018973285,0.000019311874,0.0000036608253,0.000489682,0.000051659183,0.0009363833],"genre_scores_gemma":[0.9995678,0.00001638542,0.000071035465,0.000015465366,0.0000041693356,0.0000023942437,0.00025074402,0.0000045817405,0.00006745814],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99990404,0.000013287916,0.000007458225,0.000023559673,0.000018371386,0.000033268218],"domain_scores_gemma":[0.999826,0.00003559899,0.000043602282,0.000019702782,0.000038841783,0.000036290458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029517966,0.00028395103,0.0002294844,0.00022207943,0.00027058672,0.0005948557,0.00024663392,0.00035713284,0.0011431549],"category_scores_gemma":[0.00051786297,0.00013411543,0.0004600179,0.00037270892,0.00029319167,0.00033359445,0.00057080976,0.0004571026,0.00011495266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00096817064,0.00023991504,0.7818135,0.00014587361,0.00042660715,0.0014009216,0.00020052172,0.12404292,0.07231982,0.0018497952,0.0029532027,0.013638683],"study_design_scores_gemma":[0.000062413856,0.0001269381,0.87636477,0.000015601752,0.00009377055,0.00019967652,0.00037532405,0.10800337,0.011867355,0.00079072587,0.00205708,0.000043024404],"about_ca_topic_score_codex":0.019059023,"about_ca_topic_score_gemma":0.012572707,"teacher_disagreement_score":0.019059023,"about_ca_system_score_codex":0.00073370285,"about_ca_system_score_gemma":0.00047193922,"threshold_uncertainty_score":0.037896216},"labels":[],"label_agreement":null},{"id":"W4309627391","doi":"10.1029/2022gl099396","title":"Anthropogenic Contributions to the 2021 Pacific Northwest Heatwave","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":54,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Biological and Environmental Research; Environmental Resilience Institute, Indiana University; Office of Science; U.S. Department of Energy","keywords":"Hindcast; Climatology; Climate change; Environmental science; Global warming; Climate model; Causal inference; Oceanography; Geology; Econometrics; Mathematics","score_opus":0.02975301653096984,"score_gpt":0.324380217991281,"score_spread":0.29462720146031113,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4309627391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864325,0.00031313972,0.00200176,0.0015176538,0.00009221361,0.000012216288,0.0029418762,0.00015275233,0.00653586],"genre_scores_gemma":[0.9982863,0.00017990635,0.00024906424,0.00005235568,0.000026104408,0.0000071008526,0.0009163589,0.000014752298,0.00026816654],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983895,0.000039740276,0.000006645816,0.000036610458,0.00004249116,0.00003555999],"domain_scores_gemma":[0.99954116,0.00011640192,0.000081613616,0.000058140908,0.00012713272,0.00007561722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006877119,0.00036361592,0.00017760943,0.00027281605,0.0006054317,0.001002417,0.00038706098,0.0004894685,0.002267975],"category_scores_gemma":[0.0016041687,0.00016824077,0.00047927487,0.000686808,0.00040953857,0.000532104,0.0006405227,0.00077187375,0.00015637417],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022681459,0.0001130736,0.5674946,0.00015276011,0.00039393388,0.0003561225,0.0002857963,0.38315582,0.0034540072,0.00653523,0.008368928,0.029462926],"study_design_scores_gemma":[0.00005391524,0.00007500432,0.58009565,0.00008667261,0.000140136,0.00011987713,0.00084975106,0.39493483,0.0026289101,0.006728225,0.014228631,0.000058420945],"about_ca_topic_score_codex":0.13064377,"about_ca_topic_score_gemma":0.10102662,"teacher_disagreement_score":0.13064377,"about_ca_system_score_codex":0.0016623915,"about_ca_system_score_gemma":0.0013274532,"threshold_uncertainty_score":0.2597667},"labels":[],"label_agreement":null},{"id":"W4311446150","doi":"10.1029/2022gl100450","title":"Enhanced Mixing of Heat in the Arctic Ocean Halocline in Weakly Turbulent Conditions","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Helmholtz Association; Killam Trusts; Canada Research Chairs; Government of Canada; Marine Environmental Observation Prediction and Response Network; Alfred P. Sloan Foundation","keywords":"Halocline; Turbulence; Mixing (physics); Dissipation; Atmospheric sciences; Convection; Advection; Geology; Heat transfer; Thermal; Convective mixing; Mechanics; Geophysics; Thermodynamics; Physics; Oceanography","score_opus":0.02304965086622777,"score_gpt":0.2791613217345946,"score_spread":0.25611167086836684,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311446150","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993333,0.000057943074,0.00016618431,0.000012937037,0.0000036103656,0.000001585066,0.00002834421,0.000008720607,0.00038739815],"genre_scores_gemma":[0.9998241,0.000021552773,0.00005001549,0.0000034916554,0.0000036747579,0.0000012437005,0.000033071843,0.0000020165724,0.000060897033],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994004,0.000011886719,0.0000035634014,0.000009723648,0.000013537541,0.00002123548],"domain_scores_gemma":[0.999861,0.000019158551,0.000028445229,0.000009665937,0.000034903445,0.000046748082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015150741,0.00020387706,0.00021685894,0.00040355982,0.00041986778,0.00073158316,0.000110074565,0.00015660725,0.000492486],"category_scores_gemma":[0.00027548574,0.00017292472,0.0001960828,0.00016011394,0.00038977305,0.00019467776,0.00043521196,0.00021635255,0.000097035794],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00065469136,0.00005263988,0.068989955,0.000059052112,0.00006917,0.0003244486,0.00032648942,0.0032876905,0.92204565,0.0008751337,0.00013515282,0.0031800666],"study_design_scores_gemma":[0.00008351931,0.00030669168,0.865549,0.000016374861,0.00006828626,0.00025783578,0.00049509853,0.023728391,0.10776472,0.0007149371,0.00097447826,0.000040769683],"about_ca_topic_score_codex":0.003563061,"about_ca_topic_score_gemma":0.0026917462,"teacher_disagreement_score":0.003563061,"about_ca_system_score_codex":0.00032148958,"about_ca_system_score_gemma":0.0002620631,"threshold_uncertainty_score":0.007084608},"labels":[],"label_agreement":null},{"id":"W4311452550","doi":"10.1029/2022gl100747","title":"A Large New Crater Exposes the Limits of Water Ice on Mars","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":49,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Science and Technology Facilities Council; Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Impact crater; Martian; Mars Exploration Program; Geology; Water ice; Astrobiology; Latitude; Atmosphere of Mars; Planet; Cryosphere; Climatology; Atmospheric sciences; Sea ice; Geodesy","score_opus":0.05594736291368425,"score_gpt":0.3050985647432818,"score_spread":0.24915120182959755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311452550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.996714,0.000120681645,0.00013177266,0.000057419118,0.000005452306,0.0000049190116,0.00009733752,0.000018369323,0.0028500296],"genre_scores_gemma":[0.9994974,0.00003734884,0.0001537432,0.000008028271,0.000005376327,0.0000012214009,0.000054552223,0.0000017246374,0.00024057062],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999546,0.000003152649,0.0000013237202,0.000010860423,0.000015765034,0.000014325372],"domain_scores_gemma":[0.99984825,0.000024834342,0.000033971657,0.000014656902,0.000021518357,0.000056680234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000076803386,0.00011733594,0.00011474896,0.0006065689,0.0005368944,0.00039765242,0.00016605067,0.00015295565,0.001417595],"category_scores_gemma":[0.00019851745,0.000121743135,0.00013042708,0.00018124659,0.00040194477,0.00026881634,0.0008239312,0.00026181038,0.00011872183],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008922589,0.00009510399,0.7553678,0.00010313138,0.00011578443,0.008737835,0.004035168,0.0012792364,0.16184506,0.0018675046,0.0029903166,0.06267088],"study_design_scores_gemma":[0.0000079457795,0.000064920845,0.99024117,0.000017852875,0.000011545461,0.0012822053,0.0008544568,0.000490275,0.002332648,0.0001145644,0.0045757242,0.0000067277388],"about_ca_topic_score_codex":0.009341833,"about_ca_topic_score_gemma":0.028141312,"teacher_disagreement_score":0.009341833,"about_ca_system_score_codex":0.00034405998,"about_ca_system_score_gemma":0.00018289757,"threshold_uncertainty_score":0.018574893},"labels":[],"label_agreement":null},{"id":"W4311498965","doi":"10.1029/2022gl100739","title":"Inter‐Model Differences in Future Summer Onset Over the Northern High Latitudes","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministry of Science and ICT, South Korea; National Research Foundation of Korea; Korea Meteorological Administration; National Research Foundation","keywords":"Climatology; Albedo (alchemy); Latitude; Snow; Environmental science; Climate model; Snow cover; Global warming; Climate change; High latitude; General Circulation Model; Physical geography; Geography; Oceanography; Meteorology; Geology","score_opus":0.04933342045307453,"score_gpt":0.3035196128475759,"score_spread":0.25418619239450135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311498965","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99206924,0.00009625794,0.0037797801,0.00010702198,0.000019520992,0.0000060307,0.0012697636,0.00015752921,0.0024949166],"genre_scores_gemma":[0.99857616,0.00003114158,0.00036916177,0.0000102851045,0.0000027380804,0.00000417736,0.0006958975,0.000022976994,0.00028751543],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998512,0.00004464852,0.000009069375,0.00005092791,0.000019797362,0.000024344321],"domain_scores_gemma":[0.9996362,0.00016983101,0.000043195807,0.000042675667,0.00007492055,0.000033233497],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00082699367,0.0003450069,0.00022710896,0.00016200023,0.0002582789,0.000637869,0.0003875622,0.00021490721,0.0014027387],"category_scores_gemma":[0.00096957415,0.00020446596,0.00066462246,0.0002596826,0.00017978219,0.00035802615,0.00032132654,0.00039657613,0.00017447962],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021829283,0.00003699178,0.07642871,0.000027457832,0.0002995487,0.000044265547,0.00006087187,0.91470546,0.0029277941,0.00047354444,0.00072694634,0.00405018],"study_design_scores_gemma":[0.00007924196,0.0000958443,0.14535594,0.000019234893,0.00016867672,0.000039998074,0.00015291561,0.8482902,0.0033925278,0.0008155708,0.0015457285,0.000044218217],"about_ca_topic_score_codex":0.06189903,"about_ca_topic_score_gemma":0.06357662,"teacher_disagreement_score":0.06189903,"about_ca_system_score_codex":0.0006338415,"about_ca_system_score_gemma":0.0010231974,"threshold_uncertainty_score":0.12307751},"labels":[],"label_agreement":null},{"id":"W4311507207","doi":"10.1029/2022gl101097","title":"Paleolake Inlet Valley Formation: Factors Controlling Which Craters Breached on Early Mars","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; Canadian Institute for Advanced Research","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Impact crater; Mars Exploration Program; Geology; Martian; Inlet; Fluvial; Noachian; Geomorphology; Structural basin; Earth science; Hydrology (agriculture); Astrobiology; Geotechnical engineering","score_opus":0.04350046425881778,"score_gpt":0.28189134840450575,"score_spread":0.23839088414568796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311507207","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99976856,0.000022759286,0.000025273353,0.000005754548,2.182305e-7,0.0000011605193,0.000027495387,0.0000018959896,0.00014682909],"genre_scores_gemma":[0.9998704,0.000013739335,0.000032422606,0.0000017007877,5.454074e-7,5.7619405e-7,0.000026503096,9.3497704e-7,0.00005314283],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998615,0.000020226194,0.0000110074925,0.000047263442,0.000024228417,0.000035822068],"domain_scores_gemma":[0.9995121,0.00008750474,0.00021233835,0.000030281204,0.000058606667,0.00009919493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002002079,0.00012627177,0.00021588354,0.00070308306,0.0003851108,0.000891864,0.00020217262,0.00024075854,0.001438497],"category_scores_gemma":[0.00094807823,0.00015237393,0.00014675083,0.0005285693,0.00071108365,0.00028589767,0.00047468639,0.00018378842,0.000104847284],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084016116,0.0000119624865,0.98778486,0.000016407841,0.000021071664,0.00013158315,0.00052723085,0.0003271535,0.007870723,0.000093785406,0.000047541915,0.0030836496],"study_design_scores_gemma":[5.356335e-7,0.000009333488,0.9995442,0.0000017357274,0.0000018369284,0.000028455126,0.00016322998,0.00010215529,0.00009308444,0.000010451965,0.000044051943,8.9733817e-7],"about_ca_topic_score_codex":0.010461373,"about_ca_topic_score_gemma":0.026704084,"teacher_disagreement_score":0.010461373,"about_ca_system_score_codex":0.00038806055,"about_ca_system_score_gemma":0.00020543973,"threshold_uncertainty_score":0.020800948},"labels":[],"label_agreement":null},{"id":"W4311683731","doi":"10.1029/2022gl100559","title":"Recent Intensification (2004–2020) of Permafrost Mass‐Wasting in the Central Mackenzie Valley Foothills Is a Legacy of Past Forest Fire Disturbances","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of Northwest Territories; University of Alberta","funders":"Natural Sciences and Engineering Research Council of Canada; University of Alberta","keywords":"Permafrost; Mass wasting; Disturbance (geology); Geology; Foothills; Climate change; Landslide; Arctic; Physical geography; Terrain; Earth science; Hydrology (agriculture); Geomorphology; Ecology; Oceanography; Geography; Geotechnical engineering","score_opus":0.06021418268505394,"score_gpt":0.29191157057833705,"score_spread":0.23169738789328312,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4311683731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980932,0.00020736265,0.000041987416,0.0001211519,0.0000036385502,0.0000032964235,0.0006976566,0.000007452333,0.0008242887],"genre_scores_gemma":[0.9990758,0.000114734255,0.00009191687,0.000033218792,0.0000046442833,0.0000033500585,0.00044659933,0.0000013246902,0.00022833065],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998976,0.000008658529,0.000008695576,0.000030473488,0.000021445358,0.00003305888],"domain_scores_gemma":[0.99966156,0.000017082419,0.00016779747,0.000019811965,0.00007247399,0.000061319166],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022901727,0.00013150457,0.000120928366,0.0007986169,0.0005294891,0.0006942602,0.0003641569,0.00021529749,0.0013445856],"category_scores_gemma":[0.00045861138,0.000091233414,0.00016607046,0.0007958384,0.00032918408,0.0003342725,0.00038017816,0.0002469756,0.00010971261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000054389824,0.000018867093,0.9891065,0.000041246083,0.00005722843,0.00012149681,0.0003140287,0.00021988357,0.0019155254,0.00007456517,0.0004852291,0.00759114],"study_design_scores_gemma":[5.8928805e-7,0.0000044383087,0.99921465,0.000004286747,0.000004030307,0.000024947056,0.00017161491,0.00008993861,0.00006610378,0.0000063255425,0.00041182924,0.000001160413],"about_ca_topic_score_codex":0.37439263,"about_ca_topic_score_gemma":0.74135864,"teacher_disagreement_score":0.6256074,"about_ca_system_score_codex":0.002126022,"about_ca_system_score_gemma":0.0011364152,"threshold_uncertainty_score":0.74442685},"labels":[],"label_agreement":null},{"id":"W4312059783","doi":"10.1029/2022gl100919","title":"Significant Contribution of Paleogeography to Stratospheric Water Vapor Variations in the Past 250 Million Years","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fundamental Research Funds for the Central Universities; Canadian Space Agency; Peking University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Supercontinent; Geology; Climatology; Atmospheric sciences; Climate model; Environmental science; Water vapor; Climate change; Meteorology; Oceanography; Paleontology; Tectonics","score_opus":0.01859443305679486,"score_gpt":0.2581138497624183,"score_spread":0.23951941670562343,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312059783","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980342,0.00032505614,0.0004498271,0.00015553585,0.000011983074,0.0000016787358,0.00060400757,0.00003571226,0.00038185302],"genre_scores_gemma":[0.9993594,0.0001008164,0.00008451319,0.000014752743,0.0000047703093,0.0000013743967,0.00033297238,0.0000050544577,0.00009634236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993515,0.00001683886,0.00000427593,0.000022293018,0.0000066874263,0.000014710916],"domain_scores_gemma":[0.99982387,0.00006418962,0.00003910716,0.000024480245,0.000017932553,0.00003056146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026236186,0.00026035344,0.00034973086,0.00032591398,0.00029613267,0.0006917514,0.00026373196,0.0005233864,0.0012215989],"category_scores_gemma":[0.00075443654,0.0003051359,0.00062282087,0.00037386938,0.00026401045,0.0004451764,0.0004637533,0.0002799111,0.00008560064],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034751534,0.000065118,0.7945139,0.000080190526,0.0012871773,0.00048000718,0.000119320466,0.17666292,0.016237382,0.0012186739,0.0007925144,0.008195319],"study_design_scores_gemma":[0.000034455636,0.000056146706,0.8063536,0.000016633063,0.00024478123,0.00012399752,0.0000855164,0.1898519,0.0011685252,0.00063405896,0.0013881134,0.000042264586],"about_ca_topic_score_codex":0.022754794,"about_ca_topic_score_gemma":0.01515423,"teacher_disagreement_score":0.022754794,"about_ca_system_score_codex":0.00037329405,"about_ca_system_score_gemma":0.0003313614,"threshold_uncertainty_score":0.045244694},"labels":[],"label_agreement":null},{"id":"W4312126800","doi":"10.1029/2022gl101496","title":"Presence, Sources and Transport of Polycyclic Aromatic Hydrocarbons in the Arctic Ocean","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Toxic Organic Pollutants Impact","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"National Institutes of Health; National Institute of General Medical Sciences; National Natural Science Foundation of China","keywords":"Arctic; Biogeochemical cycle; Environmental science; Oceanography; Seawater; Archipelago; The arctic; Environmental chemistry; Particulates; Surface water; Geology; Chemistry; Environmental engineering","score_opus":0.01770066099832741,"score_gpt":0.26865286494402474,"score_spread":0.25095220394569734,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312126800","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999044,0.0001735069,0.0000879343,0.000008497939,0.0000025920663,0.0000016020815,0.00028534574,0.000002509553,0.0003940021],"genre_scores_gemma":[0.99841774,0.00034885737,0.000264508,0.000010794999,0.0000036048846,0.0000025926163,0.0004533278,0.000001782989,0.0004967866],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999877,0.0000106727175,0.0000061732912,0.000040433977,0.000038582446,0.00002708253],"domain_scores_gemma":[0.9998642,0.000014291711,0.000040203722,0.000005105663,0.00005642636,0.000019763738],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014936012,0.00024298877,0.00015378425,0.00055231544,0.000571099,0.0007179165,0.00010815563,0.00017815185,0.00024415832],"category_scores_gemma":[0.00013762011,0.00015816437,0.00016286182,0.00069238927,0.00021533383,0.00017897625,0.0003026065,0.00015411733,0.000100468445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026977662,0.000036944188,0.84183896,0.00007802713,0.000084867694,0.00019269972,0.0004837186,0.000829692,0.14652538,0.00011639178,0.000122827,0.009420687],"study_design_scores_gemma":[0.000003915586,0.000071433155,0.9830655,0.000015905911,0.00004371321,0.000092127004,0.00069990713,0.00091689016,0.0132685285,0.000034572706,0.0017792314,0.0000083989335],"about_ca_topic_score_codex":0.17935266,"about_ca_topic_score_gemma":0.18773402,"teacher_disagreement_score":0.17935266,"about_ca_system_score_codex":0.0008610799,"about_ca_system_score_gemma":0.0009330684,"threshold_uncertainty_score":0.3566174},"labels":[],"label_agreement":null},{"id":"W4312126895","doi":"10.1029/2022gl101197","title":"Sensitivity of the Tropical Dust Cycle to Glacial Abrupt Climate Changes","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Climatology; Radiative forcing; Forcing (mathematics); Stadial; Glacial period; Environmental science; Deposition (geology); Anomaly (physics); Mineral dust; Atmospheric sciences; Last Glacial Maximum; Climate change; Tropical Atlantic; Climate model; Geology; Radiative transfer; Oceanography; Sea surface temperature; Physics; Meteorology; Geomorphology; Sediment; Aerosol","score_opus":0.03227956479486689,"score_gpt":0.29422974920108236,"score_spread":0.2619501844062155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4312126895","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998563,0.000031993448,0.0003118746,0.00008419719,0.000009695617,0.0000058427654,0.0002384203,0.000032499687,0.00072254357],"genre_scores_gemma":[0.99974364,0.000018139574,0.00005522998,0.000014898584,0.0000019466593,0.0000024591868,0.000100780264,0.0000052904534,0.000057656463],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983084,0.00006505128,0.000011208261,0.000038822825,0.000015015269,0.000039091137],"domain_scores_gemma":[0.99943775,0.00031974618,0.00006067135,0.000053731797,0.00004443262,0.000083714716],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00045365724,0.0003210537,0.00032951974,0.0002981028,0.00031573357,0.0008978392,0.00033653033,0.00081282156,0.001610661],"category_scores_gemma":[0.0021700107,0.0002779737,0.0004924327,0.0003007101,0.00044211524,0.00036598215,0.00047164146,0.00047486267,0.000118349744],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038358322,0.00011172653,0.10776071,0.000053534375,0.00032509636,0.00028315175,0.00008247112,0.8787073,0.008416825,0.0009807852,0.0005941189,0.0023007642],"study_design_scores_gemma":[0.00020223919,0.00025801986,0.10056235,0.00001908113,0.00009265801,0.000090008456,0.00017942757,0.8927967,0.003916714,0.0011550253,0.0006802672,0.00004739979],"about_ca_topic_score_codex":0.016897256,"about_ca_topic_score_gemma":0.005909702,"teacher_disagreement_score":0.016897256,"about_ca_system_score_codex":0.0006972542,"about_ca_system_score_gemma":0.00035372257,"threshold_uncertainty_score":0.033597827},"labels":[],"label_agreement":null},{"id":"W4313332706","doi":"10.1029/2022gl098009","title":"Seasonal Acceleration of Petermann Glacier, Greenland, From Changes in Subglacial Hydrology","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Agence Nationale de la Recherche","keywords":"Glacier; Geology; Climatology; Future sea level; Greenland ice sheet; Ice sheet; Ice stream; Geomorphology; Hydrology (agriculture); Cryosphere; Sea ice","score_opus":0.05102182132757302,"score_gpt":0.2846707508389225,"score_spread":0.2336489295113495,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313332706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99926966,0.000017433927,0.00015645678,0.000029932919,0.0000021492933,0.0000018853149,0.00019131186,0.000023634286,0.00030753494],"genre_scores_gemma":[0.99970055,0.000010448766,0.000063240725,0.0000046039527,6.5094e-7,0.0000010385518,0.00015898277,0.0000032566159,0.00005732174],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999591,0.0000052851733,0.0000013816893,0.000015285048,0.000007854761,0.00001106164],"domain_scores_gemma":[0.9999044,0.00002135617,0.00002642006,0.000010760681,0.000013780009,0.000023219873],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000178424,0.00025794294,0.00012710386,0.00022041691,0.00017031842,0.00040526848,0.00020524413,0.00018324895,0.000577306],"category_scores_gemma":[0.0003264467,0.00009183534,0.00022739737,0.0002511188,0.0002201103,0.0002357644,0.00018963168,0.00016860355,0.00006379804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032323212,0.00008086415,0.7848021,0.00003989491,0.00018676954,0.0004105583,0.00022618499,0.1760858,0.025478106,0.0010339542,0.0015426103,0.009789946],"study_design_scores_gemma":[0.000014268082,0.000034658766,0.8487817,0.000004703831,0.000023718769,0.00004635538,0.00009432718,0.14805007,0.002077929,0.00031833982,0.00054209895,0.000011800353],"about_ca_topic_score_codex":0.07395211,"about_ca_topic_score_gemma":0.09124604,"teacher_disagreement_score":0.07395211,"about_ca_system_score_codex":0.0011589018,"about_ca_system_score_gemma":0.0006147537,"threshold_uncertainty_score":0.14704335},"labels":[],"label_agreement":null},{"id":"W4313418759","doi":"10.1029/2022gl101150","title":"High and Dry: Billion‐Year Trends in the Aridity of River‐Forming Climates on Mars","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"","keywords":"Mars Exploration Program; Arid; Aridity index; Climate change; Physical geography; Environmental science; Latitude; Geology; Climatology; Geography; Astrobiology; Oceanography","score_opus":0.04179525462287584,"score_gpt":0.29818480955815657,"score_spread":0.2563895549352807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313418759","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9958916,0.00024669126,0.00014180601,0.00018259812,0.0000051925963,0.000001271108,0.002859894,0.00002537321,0.00064560445],"genre_scores_gemma":[0.9980172,0.00008704651,0.00015173119,0.000023218567,0.000009329117,0.0000023867958,0.0016159428,0.000004938373,0.00008827474],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998503,0.000028262592,0.000013127593,0.000051940642,0.000032229957,0.000024242474],"domain_scores_gemma":[0.99911493,0.00011529894,0.0004008326,0.00008270867,0.00016507907,0.00012118389],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00035395316,0.00011166737,0.00017621071,0.0011611925,0.00025397932,0.0008523165,0.0002448271,0.00029543473,0.0009860336],"category_scores_gemma":[0.0010331509,0.00009125586,0.00013550761,0.0014410794,0.0002587188,0.00051999884,0.00057553913,0.00034687907,0.00015954838],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006754499,0.000012817083,0.9878934,0.000034147222,0.000086575776,0.00004144047,0.0003422558,0.00090213254,0.0019007631,0.00030043352,0.0010741407,0.0073443893],"study_design_scores_gemma":[9.677486e-7,0.000009983715,0.99788207,0.0000036958672,0.0000069419816,0.00003137008,0.00013511143,0.00045367892,0.00010839511,0.000058878006,0.0013059394,0.0000029297703],"about_ca_topic_score_codex":0.005032564,"about_ca_topic_score_gemma":0.007880915,"teacher_disagreement_score":0.005032564,"about_ca_system_score_codex":0.00023720699,"about_ca_system_score_gemma":0.000096799755,"threshold_uncertainty_score":0.010006547},"labels":[],"label_agreement":null},{"id":"W4313419015","doi":"10.1029/2022gl100405","title":"Evaluation of Paleomagnetic Bias in Ediacaran Global Paleogeographic Reconstructions","year":2022,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University; St. Francis Xavier University","funders":"Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Paleomagnetism; Geology; Tectonics; Plate tectonics; Precambrian; Paleontology; Seismology; Subduction","score_opus":0.08189526088295102,"score_gpt":0.30707680746554794,"score_spread":0.22518154658259693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313419015","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9926111,0.00017284948,0.0059441864,0.00006897143,0.0000041648796,0.000008721113,0.00026938098,0.00005447926,0.00086613034],"genre_scores_gemma":[0.9976826,0.000039369774,0.0019395751,0.000008808525,0.0000022178858,0.0000042206816,0.00027041824,0.000014135686,0.000038636284],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99694437,0.0018020135,0.00032184727,0.0004387571,0.0003571454,0.0001358636],"domain_scores_gemma":[0.9785417,0.014373755,0.0026407458,0.002214527,0.0020003333,0.0002290318],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.011952547,0.000340591,0.00043578612,0.0022693197,0.00037662478,0.0017157552,0.00053537264,0.00032767802,0.0008192382],"category_scores_gemma":[0.03879195,0.00021114643,0.00035187745,0.0031441539,0.00072993204,0.00082363875,0.0013320011,0.0002281266,0.000090425136],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014606409,0.000010443275,0.9602781,0.0000222321,0.00021352008,0.000057092864,0.000323695,0.026641676,0.0005493443,0.001124704,0.00011550874,0.010517673],"study_design_scores_gemma":[0.0000443919,0.00010675939,0.77268404,0.00010192553,0.0001918922,0.0002776143,0.0012904768,0.2158191,0.0033567618,0.0043592965,0.0017254939,0.00004219817],"about_ca_topic_score_codex":0.008980675,"about_ca_topic_score_gemma":0.009060216,"teacher_disagreement_score":0.011952547,"about_ca_system_score_codex":0.00078048237,"about_ca_system_score_gemma":0.0004829662,"threshold_uncertainty_score":0.06321186},"labels":[],"label_agreement":null},{"id":"W4313830822","doi":"10.1029/2022gl100247","title":"Understanding the History of Two Complex Ice Crystal Habits Deduced From a Holographic Imager","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"HORIZON EUROPE European Research Council; Swiss Polar Institute; Horizon 2020 Framework Programme; Deutsche Forschungsgemeinschaft; EEA Grants/Norway Grants; European Commission; EEA Grants; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Ice crystals; Atmospheric sciences; Aerosol; Radiative transfer; Precipitation; Materials science; Crystal (programming language); Arctic; Ice core; Arctic ice pack; Geology; Sea ice; Environmental science; Climatology; Meteorology; Optics; Physics; Oceanography","score_opus":0.14214586129878304,"score_gpt":0.3217222831446394,"score_spread":0.17957642184585637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313830822","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99403894,0.00008863341,0.002709977,0.0000111864765,0.0000047442613,0.000014594829,0.0007092783,0.000039741284,0.0023828812],"genre_scores_gemma":[0.99727976,0.000046865458,0.0019528486,0.000006336069,0.000004324534,0.0000049596347,0.00035466996,0.000008980892,0.00034125242],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999678,0.0000015797443,0.0000014349879,0.000009298957,0.00000844777,0.0000114550185],"domain_scores_gemma":[0.99984133,0.000042172247,0.000039295068,0.000017976068,0.00003071733,0.000028414603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0000618589,0.00009024441,0.000083467385,0.0005986408,0.00014548129,0.0004092531,0.0001218594,0.0001290556,0.0009476868],"category_scores_gemma":[0.00017612269,0.00010998496,0.00010132221,0.00027270423,0.00015835058,0.0002246028,0.00011911714,0.00014960399,0.00016409499],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022203318,0.000064753396,0.17577614,0.000070508286,0.000038765003,0.00027971345,0.0002749733,0.0025456278,0.797744,0.0005051748,0.00054813357,0.021930166],"study_design_scores_gemma":[0.0000069571715,0.000038393846,0.8997711,0.00000854165,0.000026830794,0.00020760822,0.00019941492,0.016411256,0.082132936,0.00014474078,0.0010380357,0.000014228652],"about_ca_topic_score_codex":0.005268756,"about_ca_topic_score_gemma":0.010470573,"teacher_disagreement_score":0.005268756,"about_ca_system_score_codex":0.00022947915,"about_ca_system_score_gemma":0.00014631041,"threshold_uncertainty_score":0.010476172},"labels":[],"label_agreement":null},{"id":"W4313839682","doi":"10.1029/2022gl100696","title":"Synoptic Variability in Satellite Altimeter‐Derived Radar Freeboard of Arctic Sea Ice","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":36,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Natural Environment Research Council; Met Office; Sight Research UK; Nuclear Safety and Security Commission; European Space Agency; National Aeronautics and Space Administration","keywords":"Freeboard; Snow; Radar altimeter; Radar; Satellite; Sea ice; Remote sensing; Altimeter; Geology; Meteorology; Arctic ice pack; Scatterometer; Environmental science; Climatology; Oceanography; Geomorphology; Wind speed; Geography; Aerospace engineering","score_opus":0.028712462043786524,"score_gpt":0.275694949440231,"score_spread":0.24698248739644446,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313839682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867517,0.00003287394,0.00035140387,0.000012880041,0.0000069632993,0.0000019476468,0.0005949458,0.000020051348,0.00030377728],"genre_scores_gemma":[0.99844885,0.000022496577,0.0002248415,0.00000833677,0.000005600557,0.000003922573,0.0011797807,0.0000055473515,0.00010052188],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998642,0.00003613188,0.000013161421,0.00004419673,0.00002560063,0.000016743956],"domain_scores_gemma":[0.9991504,0.0003139293,0.0001965417,0.00011034237,0.00017162203,0.000057201207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00068811834,0.00014709476,0.00011079728,0.00049623125,0.000113633185,0.0004267791,0.00015012285,0.0002196074,0.00054095924],"category_scores_gemma":[0.0010987887,0.00012139063,0.00018459737,0.00045719475,0.00016320618,0.00031790437,0.00020946148,0.0001298207,0.00014855334],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005509234,0.00012924682,0.95463103,0.00005430506,0.0002887647,0.00012213875,0.0002704866,0.012938113,0.015005523,0.0003692568,0.001411822,0.01422847],"study_design_scores_gemma":[0.000011101099,0.00004533079,0.9855655,0.000008525392,0.00002353817,0.00003595724,0.000076207696,0.012457679,0.0011845116,0.000056292654,0.0005280644,0.00000725487],"about_ca_topic_score_codex":0.0052143396,"about_ca_topic_score_gemma":0.006565994,"teacher_disagreement_score":0.0052143396,"about_ca_system_score_codex":0.0001883106,"about_ca_system_score_gemma":0.000116388524,"threshold_uncertainty_score":0.01036799},"labels":[],"label_agreement":null},{"id":"W4313839724","doi":"10.1029/2022gl100772","title":"New Detections of Feldspar‐Bearing Volcanic Rocks in the Walls of Valles Marineris, Mars","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Brock University","funders":"Agence Nationale de la Recherche","keywords":"Geology; Plagioclase; Geochemistry; Lava; Porphyritic; Volcanic rock; Crust; Basalt; Anorthosite; Igneous rock; Pluton; Mars Exploration Program; Outcrop; Petrology; Feldspar; Volcano; Quartz; Astrobiology; Paleontology","score_opus":0.04591552532247716,"score_gpt":0.3066580520942834,"score_spread":0.2607425267718062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313839724","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99858826,0.00020700048,0.00012415735,0.000013666866,0.0000029297362,0.0000021403114,0.00016200262,0.00002535172,0.0008743433],"genre_scores_gemma":[0.99947804,0.000040563657,0.00016893353,0.0000043513946,0.0000033652434,0.0000012189743,0.00014937721,0.0000023045884,0.00015181612],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998971,0.0000093532535,0.0000040281284,0.000038619117,0.000031476688,0.000019391688],"domain_scores_gemma":[0.9997435,0.0000402027,0.000087696455,0.000028018538,0.000041611565,0.00005899155],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016516606,0.00019061423,0.000115737,0.0013862494,0.0004235812,0.00048651223,0.00024913394,0.00028301697,0.0006933996],"category_scores_gemma":[0.00034435594,0.00017041346,0.00013685405,0.0003385178,0.00034486488,0.00017918799,0.00047390783,0.00015214238,0.00016176715],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011906842,0.000017432616,0.8252374,0.000044654487,0.000041999647,0.0006572542,0.0012128205,0.00015998405,0.15988979,0.00010631866,0.0002599689,0.01225332],"study_design_scores_gemma":[0.0000013005725,0.000016205788,0.99790585,0.000005781714,0.0000056384383,0.00019892583,0.00015818648,0.00010996409,0.0011144386,0.000013998082,0.00046773147,0.000001898674],"about_ca_topic_score_codex":0.006655558,"about_ca_topic_score_gemma":0.021360332,"teacher_disagreement_score":0.006655558,"about_ca_system_score_codex":0.00022982247,"about_ca_system_score_gemma":0.00011928923,"threshold_uncertainty_score":0.013233602},"labels":[],"label_agreement":null},{"id":"W4313839726","doi":"10.1029/2022gl101285","title":"How Is Time Distributed in a River Meander Belt?","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Laurentian University; Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"","keywords":"Meander (mathematics); Floodplain; Geology; Hydrology (agriculture); Channel (broadcasting); Geomorphology; Aggradation; Fluvial; Geometry; Geotechnical engineering; Structural basin; Geography","score_opus":0.02552323097429619,"score_gpt":0.28291828902940486,"score_spread":0.25739505805510865,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313839726","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971111,0.000055477576,0.0019555194,0.00008137879,0.0000025189845,0.000002316584,0.00004697973,0.0000144504,0.0007302822],"genre_scores_gemma":[0.99975497,0.000014928734,0.00013525882,0.0000034219186,0.0000017783096,0.0000013754994,0.000012276436,0.0000024565072,0.00007358306],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997725,0.000063464664,0.000014928128,0.00007566033,0.000028619626,0.000044849927],"domain_scores_gemma":[0.9974993,0.001124441,0.0006716147,0.00026058013,0.00022907268,0.0002150072],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008098064,0.00008000785,0.0002631771,0.0009152082,0.0002493288,0.0013269193,0.00040082636,0.00034950575,0.0019562468],"category_scores_gemma":[0.0063815354,0.00012403894,0.00022520217,0.00063132256,0.00090210536,0.0015224331,0.00039410513,0.00019164644,0.00012520635],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000581179,0.00008810052,0.8039911,0.000096597585,0.00016187514,0.00039296874,0.0018566787,0.102680996,0.020333596,0.030691924,0.0006099094,0.038515054],"study_design_scores_gemma":[0.00003555476,0.00019452522,0.7519956,0.000028021152,0.00006469932,0.00032504104,0.0021740359,0.21406436,0.0022932633,0.02707127,0.0017033658,0.000050227114],"about_ca_topic_score_codex":0.002656246,"about_ca_topic_score_gemma":0.0019107088,"teacher_disagreement_score":0.002656246,"about_ca_system_score_codex":0.0007887249,"about_ca_system_score_gemma":0.0002304588,"threshold_uncertainty_score":0.0065443516},"labels":[],"label_agreement":null},{"id":"W4313839805","doi":"10.1029/2022gl100836","title":"Increasing Precipitation Efficiency Amplifies Climate Sensitivity by Enhancing Tropical Circulation Slowdown and Eastern Pacific Warming Pattern","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lawrence Livermore National Laboratory; Horizon 2020 Framework Programme; National Oceanic and Atmospheric Administration; Deutsches Klimarechenzentrum; McGill University; Florida State University; Agence Nationale de la Recherche; National Science Foundation","keywords":"Coupled model intercomparison project; Environmental science; Precipitation; Climatology; Slowdown; Climate sensitivity; Climate model; Atmospheric sciences; Climate change; Greenhouse gas; Global warming; Walker circulation; Cloud feedback; Cloud cover; Meteorology; Cloud computing; Geology","score_opus":0.030457468589544564,"score_gpt":0.29537731805280126,"score_spread":0.2649198494632567,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4313839805","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992367,0.000018672032,0.00020314888,0.00003254877,0.0000013850089,0.000001381031,0.00006955342,0.000018073579,0.0004185872],"genre_scores_gemma":[0.9998049,0.000010542236,0.0000849866,0.000010012718,0.0000010090223,8.897078e-7,0.000033392855,0.0000032612043,0.000051175695],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999267,0.000020460542,0.0000044603435,0.000020591184,0.000008367747,0.000019542586],"domain_scores_gemma":[0.9997888,0.0000718323,0.0000448209,0.000036715683,0.000018532755,0.000039409566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016893778,0.00018820773,0.00016728435,0.0001588042,0.00009710772,0.00043700726,0.00019225958,0.00018697268,0.0010309956],"category_scores_gemma":[0.0006043965,0.00015462648,0.00024425748,0.00013127028,0.00024074408,0.00025738528,0.00032533656,0.0002115674,0.00005228143],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009044208,0.00028100522,0.49500248,0.00012857863,0.00075032405,0.00036734392,0.00016607334,0.19393171,0.2941085,0.0023714781,0.001192726,0.010795333],"study_design_scores_gemma":[0.00009033431,0.00017028123,0.80162096,0.000011352715,0.00021636889,0.000090584486,0.00015015404,0.17679396,0.018829258,0.0011065305,0.0009016394,0.000018671572],"about_ca_topic_score_codex":0.007425859,"about_ca_topic_score_gemma":0.007880188,"teacher_disagreement_score":0.007425859,"about_ca_system_score_codex":0.00030387423,"about_ca_system_score_gemma":0.00020884625,"threshold_uncertainty_score":0.014765263},"labels":[],"label_agreement":null},{"id":"W4317397272","doi":"10.1029/2022gl100028","title":"Pleistocene Accelerated Exhumation Within the Sumatran Fault: Implications for Late Cenozoic Evolution of Sumatra (Indonesia)","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geophysical Studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University; Simon Fraser University","funders":"National Natural Science Foundation of China","keywords":"Geology; Forearc; Cenozoic; Thermochronology; Fault (geology); Seismology; Sinistral and dextral; Paleontology; Late Miocene; Strike-slip tectonics; Subduction; Tectonics; Structural basin","score_opus":0.09755607653240211,"score_gpt":0.31907944385663506,"score_spread":0.22152336732423294,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317397272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99649185,0.00036046936,0.0001877331,0.00012557875,0.000010274232,0.0000044513,0.00018198458,0.000011761315,0.002625998],"genre_scores_gemma":[0.99898607,0.00022323245,0.00016029531,0.000019018926,0.0000041142494,0.0000034953894,0.00008535999,0.0000064413284,0.0005118635],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992347,0.000010046926,0.000009400001,0.000031150455,0.000011303228,0.000014530501],"domain_scores_gemma":[0.9998292,0.000016745924,0.00006583581,0.000015196949,0.000047075147,0.000026007556],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026889477,0.0003182088,0.00018721263,0.0008682379,0.000753449,0.00096183264,0.00022349884,0.00024859817,0.003241172],"category_scores_gemma":[0.00044422768,0.00020453265,0.00015909506,0.0009701562,0.00071298494,0.00066633325,0.0006927355,0.00046497388,0.000403007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035050453,0.00009987368,0.86372095,0.0003008108,0.00013605338,0.0024421532,0.005728392,0.0039355946,0.06571601,0.0013912534,0.00037334202,0.055805087],"study_design_scores_gemma":[0.0000045997285,0.00001913591,0.99605227,0.000021035456,0.00001728075,0.00026438388,0.00071935763,0.0005832106,0.00083503866,0.00014159468,0.0013356472,0.0000064103815],"about_ca_topic_score_codex":0.014390435,"about_ca_topic_score_gemma":0.026191412,"teacher_disagreement_score":0.014390435,"about_ca_system_score_codex":0.0011855012,"about_ca_system_score_gemma":0.0004457418,"threshold_uncertainty_score":0.028613329},"labels":[],"label_agreement":null},{"id":"W4317397790","doi":"10.1029/2022gl102183","title":"Revisiting the Mechanisms of ENSO Response to Tropical Volcanic Eruptions","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":25,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"National Supercomputer Centre, Linköpings Universitet; Natural Sciences and Engineering Research Council of Canada; Vetenskapsrådet; Fonds de recherche du Québec – Nature et technologies; National Science Council","keywords":"Volcano; Climatology; El Niño Southern Oscillation; Tropics; Radiative forcing; Geology; Vulcanian eruption; Forcing (mathematics); Southern oscillation; Atmospheric sciences; Global change; Tropical cyclone; Global cooling; Aerosol; Stratosphere; Environmental science; Earth science; Climate change; Meteorology; Oceanography; Geography; Seismology","score_opus":0.05874409434774558,"score_gpt":0.34109899321478915,"score_spread":0.28235489886704357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317397790","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99720156,0.000068480585,0.00059853285,0.00022471593,0.00002576532,0.000012849084,0.00019110556,0.00003514458,0.0016417702],"genre_scores_gemma":[0.9997069,0.000038161314,0.00009149832,0.000019122508,0.0000048728666,0.000004236019,0.00003519946,0.000005675787,0.00009429509],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985766,0.000057792968,0.0000093695435,0.000025836756,0.000011052092,0.000038219005],"domain_scores_gemma":[0.99948597,0.00030099848,0.00007472136,0.000043449294,0.000041841082,0.000053004234],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056479714,0.00043876647,0.00034315864,0.00030804952,0.0002949771,0.00085939874,0.00047023752,0.0006969988,0.0024724961],"category_scores_gemma":[0.0014984559,0.00029985924,0.00058660243,0.00020812705,0.00049563515,0.0007885841,0.0004962771,0.0005542646,0.0001239018],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035103512,0.00034514655,0.068765186,0.00011959901,0.00031832932,0.0003601742,0.00015534283,0.890388,0.02970005,0.005182442,0.00090646243,0.0034082888],"study_design_scores_gemma":[0.00016759157,0.00015911393,0.040474158,0.00001272105,0.00006748001,0.000040067727,0.00019146095,0.9521447,0.0038962548,0.0021227181,0.00069219567,0.000031573512],"about_ca_topic_score_codex":0.017199183,"about_ca_topic_score_gemma":0.0063610924,"teacher_disagreement_score":0.017199183,"about_ca_system_score_codex":0.0007281587,"about_ca_system_score_gemma":0.0007126188,"threshold_uncertainty_score":0.034198165},"labels":[],"label_agreement":null},{"id":"W4317606122","doi":"10.1029/2022gl102394","title":"Resonant Scattering of Radiation Belt Electrons at Saturn by Ion Cyclotron Waves","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Astro and Planetary Science","field":"Physics and Astronomy","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National Key Research and Development Program of China; Fundamental Research Funds for the Central Universities; Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Saturn; Physics; Electron; Van Allen radiation belt; Cyclotron; Scattering; Pitch angle; Atomic physics; Ion; Electron precipitation; Kinetic energy; Magnetosphere; Computational physics; Nuclear physics; Optics; Geophysics; Astrophysics; Plasma","score_opus":0.0175223761620388,"score_gpt":0.28700042693798394,"score_spread":0.26947805077594517,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4317606122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963813,0.000038549588,0.0024291067,0.000052513104,0.0000029238076,0.000004069825,0.000086877146,0.000024223886,0.0009803921],"genre_scores_gemma":[0.99948967,0.000020179432,0.00024939587,0.000005558656,0.0000013534315,0.0000025193938,0.0000730968,0.0000062858862,0.00015189724],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999442,0.000010114045,0.0000021755282,0.000017634497,0.000009924448,0.000016044469],"domain_scores_gemma":[0.9998859,0.000035953202,0.000024628875,0.000019228275,0.000021189504,0.000012955157],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029851092,0.0002241621,0.00017011423,0.00025018485,0.00030551784,0.00030174825,0.00039005966,0.00027473638,0.0007647692],"category_scores_gemma":[0.00060267857,0.00013714185,0.00028597264,0.00018772206,0.00022316878,0.00043098314,0.0002515393,0.00023329708,0.00009389961],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037071953,0.00008918472,0.35296187,0.00008381926,0.000141458,0.00044728635,0.00031050743,0.5640475,0.065870665,0.00658891,0.0006566309,0.008431472],"study_design_scores_gemma":[0.000023741482,0.000042833613,0.106110245,0.0000054667566,0.000015696442,0.00007073359,0.00010996202,0.88590205,0.006347854,0.0009284739,0.00042675025,0.00001616415],"about_ca_topic_score_codex":0.015630497,"about_ca_topic_score_gemma":0.008685648,"teacher_disagreement_score":0.015630497,"about_ca_system_score_codex":0.0009196575,"about_ca_system_score_gemma":0.00030640137,"threshold_uncertainty_score":0.031078994},"labels":[],"label_agreement":null},{"id":"W4318962809","doi":"10.1029/2022gl101220","title":"An Assessment of Vertical Carbon Flux Parameterizations Using Backscatter Data From BGC Argo","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Ocean Frontier Institute","keywords":"Argo; Environmental science; Flux (metallurgy); Proxy (statistics); Atmospheric sciences; Backscatter (email); Biogeochemical cycle; Meteorology; Geology; Climatology; Physics; Materials science; Computer science; Chemistry","score_opus":0.07576924217470359,"score_gpt":0.38192836036143174,"score_spread":0.30615911818672814,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4318962809","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99232084,0.00007564881,0.0046726377,0.00012518451,0.000016843833,0.000017426077,0.0013366836,0.00026485033,0.001169873],"genre_scores_gemma":[0.9954497,0.00002836479,0.0028992258,0.000029021745,0.000005464555,0.000010341008,0.0014941351,0.000032703265,0.000051011506],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99934095,0.00023650774,0.000052769898,0.0001502909,0.00012213111,0.0000972951],"domain_scores_gemma":[0.9983051,0.0007078323,0.00023333085,0.00031277898,0.00033988766,0.00010104117],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030220165,0.0010348142,0.00038590262,0.00079709635,0.00028852557,0.0009912107,0.00043232142,0.00097261573,0.00045092145],"category_scores_gemma":[0.003644267,0.00034923147,0.00084108167,0.0008206579,0.00034762904,0.0013624694,0.00039288227,0.00035623496,0.00018618794],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009982616,0.00023051997,0.42765418,0.00012493439,0.0005802929,0.00017503284,0.0001242788,0.5067452,0.0279857,0.0014226292,0.0013706038,0.032588337],"study_design_scores_gemma":[0.00013125458,0.00011363418,0.29776368,0.000035968696,0.00009721343,0.00005777651,0.00012024948,0.69262296,0.007367232,0.000587825,0.0010043557,0.0000978724],"about_ca_topic_score_codex":0.01910552,"about_ca_topic_score_gemma":0.010762756,"teacher_disagreement_score":0.01910552,"about_ca_system_score_codex":0.00071163545,"about_ca_system_score_gemma":0.00046813124,"threshold_uncertainty_score":0.037988663},"labels":[],"label_agreement":null},{"id":"W4319040595","doi":"10.1029/2022gl101978","title":"Tomographic Retrievals of Hunga Tonga‐Hunga Ha'apai Volcanic Aerosol","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":51,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Goddard Space Flight Center; National Aeronautics and Space Administration","keywords":"Aerosol; Volcano; Stratosphere; Lidar; Environmental science; Atmospheric sciences; Vulcanian eruption; Occultation; Extinction (optical mineralogy); Altitude (triangle); Optical depth; Sulfate aerosol; Remote sensing; Geology; Meteorology; Physics; Mineralogy; Astrophysics","score_opus":0.04215108963257834,"score_gpt":0.30025923179375547,"score_spread":0.2581081421611771,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319040595","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99677354,0.000084430474,0.0007644903,0.00003759185,0.000008566487,0.000011259919,0.0012879226,0.00009312407,0.0009390643],"genre_scores_gemma":[0.99708563,0.000039314185,0.0011665834,0.000008005524,0.0000056404806,0.0000073137207,0.0014806733,0.00001095492,0.00019593383],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999466,0.00000427161,0.0000029124628,0.000016622947,0.000014147484,0.000015470017],"domain_scores_gemma":[0.99988866,0.000014973723,0.000016869819,0.000014270106,0.00004437693,0.00002087713],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012822344,0.00029734607,0.00022133872,0.0007088863,0.00024700502,0.0004402108,0.0003247574,0.00030985332,0.0011318933],"category_scores_gemma":[0.0003712619,0.00020194046,0.0003420987,0.0009852735,0.00013492854,0.00029773414,0.00032481962,0.00021693979,0.00015966251],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010663964,0.00046330914,0.4455952,0.00039216317,0.00092867913,0.0017094094,0.0007345154,0.20734009,0.24500048,0.00081441965,0.0044466546,0.09150873],"study_design_scores_gemma":[0.00009830227,0.000053601594,0.6763805,0.000017204042,0.0001660919,0.00014285323,0.00021713885,0.30994534,0.010651354,0.00012943296,0.0021612498,0.000036925132],"about_ca_topic_score_codex":0.042962816,"about_ca_topic_score_gemma":0.03799569,"teacher_disagreement_score":0.042962816,"about_ca_system_score_codex":0.0006691273,"about_ca_system_score_gemma":0.00056887727,"threshold_uncertainty_score":0.085425496},"labels":[],"label_agreement":null},{"id":"W4319342138","doi":"10.1029/2022gl100958","title":"Everything Hits at Once: How Remote Rainfall Matters for the Prediction of the 2021 North American Heat Wave","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":41,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Helmholtz-Fonds; Deutsche Forschungsgemeinschaft","keywords":"Predictability; Extratropical cyclone; Heat wave; Climatology; Cascade; Limiting; Environmental science; Meteorology; Ridge; Numerical weather prediction; Climate change; Geology; Geography; Physics","score_opus":0.05517373891854656,"score_gpt":0.29422714954564355,"score_spread":0.239053410627097,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4319342138","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99635017,0.00019944424,0.00084074814,0.0013253209,0.00003270701,0.000004891678,0.00018933546,0.000031795553,0.0010256368],"genre_scores_gemma":[0.9996213,0.00004663603,0.0000810989,0.000032973843,0.000023228757,0.0000010308411,0.00010112055,0.0000045872625,0.00008800743],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997477,0.0001012592,0.000011522413,0.000078109035,0.000017800707,0.000043566408],"domain_scores_gemma":[0.9962037,0.0025645792,0.00044006444,0.00012822004,0.00018073957,0.00048260737],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012465388,0.00033247302,0.0003385617,0.00037288183,0.00049432606,0.0018895271,0.00044868904,0.0009783477,0.0023506372],"category_scores_gemma":[0.0073920824,0.0002685256,0.00050079223,0.00033827196,0.0006698681,0.0012498582,0.00068793935,0.00093084585,0.00026621198],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050413125,0.00020066422,0.7877364,0.000031156564,0.0002717948,0.00020170835,0.00014428156,0.19591191,0.0015178563,0.0015024348,0.0019222667,0.010055478],"study_design_scores_gemma":[0.00005244384,0.000106371255,0.34367663,0.000037448663,0.000099835575,0.00004193687,0.0003896162,0.65127283,0.00041758877,0.003315734,0.000548543,0.00004100907],"about_ca_topic_score_codex":0.02996739,"about_ca_topic_score_gemma":0.018283924,"teacher_disagreement_score":0.02996739,"about_ca_system_score_codex":0.00043339035,"about_ca_system_score_gemma":0.00072147994,"threshold_uncertainty_score":0.05958593},"labels":[],"label_agreement":null},{"id":"W4320914117","doi":"10.1029/2022gl102020","title":"A Positive Cooling Feedback for the Neoproterozoic Snowball Earth Initiation Due To Weakening of Ocean Ventilation","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"","keywords":"Deep sea; Snowball Earth; Glacial period; Ventilation (architecture); Geology; Ice age; Atmosphere (unit); Sea level; Environmental science; Atmospheric sciences; Climatology; Oceanography; Meteorology; Paleontology; Geography","score_opus":0.04941982836406995,"score_gpt":0.3146044499381828,"score_spread":0.2651846215741129,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4320914117","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9943652,0.00010081234,0.0017905236,0.00041611015,0.00004468391,0.000010563314,0.00039932312,0.00020969498,0.002663034],"genre_scores_gemma":[0.99930465,0.000036802627,0.00021890542,0.000050351366,0.000006610232,0.00000567412,0.00009477209,0.000025814192,0.00025648958],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999447,0.000009593687,0.0000029868288,0.000014917889,0.0000066707003,0.000021126441],"domain_scores_gemma":[0.9998671,0.0000312543,0.00001928968,0.0000122703095,0.000023405222,0.00004670799],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022673511,0.000465704,0.00037296326,0.0002984065,0.000384663,0.00055931206,0.00044628172,0.0006068641,0.006430189],"category_scores_gemma":[0.00078077655,0.00033543503,0.00058205536,0.00015054717,0.00040836222,0.0005104228,0.00078160287,0.00064240594,0.0002988076],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00093753816,0.0002495151,0.16064435,0.00048411524,0.00046234505,0.0014784139,0.00044493817,0.4484989,0.3559459,0.010651684,0.004501988,0.015700348],"study_design_scores_gemma":[0.00059202686,0.00035100576,0.27280638,0.0000540977,0.00020986282,0.0002086873,0.00030941266,0.6914375,0.023284238,0.0060659237,0.0045985417,0.00008231665],"about_ca_topic_score_codex":0.010084506,"about_ca_topic_score_gemma":0.0051677534,"teacher_disagreement_score":0.010084506,"about_ca_system_score_codex":0.0007045879,"about_ca_system_score_gemma":0.0005192462,"threshold_uncertainty_score":0.021511078},"labels":[],"label_agreement":null},{"id":"W4321018330","doi":"10.1029/2022gl101213","title":"Global Variability of Density Contrast Across the 660‐km Discontinuity","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"","keywords":"Jump; Geology; Mantle (geology); Discontinuity (linguistics); Subduction; Density contrast; Amplitude; Mantle convection; Classification of discontinuities; Geodesy; Geophysics; Seismology; Physics; Tectonics; Astrophysics; Optics","score_opus":0.028387482099605035,"score_gpt":0.31561072328622986,"score_spread":0.28722324118662484,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321018330","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992211,0.000021248727,0.00013310429,0.000006263788,9.544748e-7,7.4764347e-7,0.0001945317,0.000014199523,0.0004078151],"genre_scores_gemma":[0.9995073,0.000011905656,0.000092090144,0.0000016903002,0.0000013950065,7.068928e-7,0.00029872998,0.0000028790676,0.000083281615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995315,0.0000054751295,0.0000025273932,0.000015942023,0.0000102896665,0.000012719791],"domain_scores_gemma":[0.9998677,0.00002137613,0.000042560598,0.000013887961,0.000033532913,0.000020950289],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011675936,0.00014109336,0.000150292,0.00080615585,0.00012482762,0.0003314034,0.00011121986,0.00015338357,0.0009077832],"category_scores_gemma":[0.0003452945,0.0001149292,0.00012632427,0.0006406161,0.00018551103,0.00022495922,0.00035141213,0.00012126335,0.00023797447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002981361,0.000029279974,0.8926156,0.000033611617,0.000104803934,0.0001351819,0.00052143366,0.00268651,0.08854046,0.00028088264,0.0002728271,0.0144813],"study_design_scores_gemma":[0.0000021258002,0.000008071625,0.9981945,0.0000019085342,0.000006075753,0.000025039963,0.000059207763,0.0008582292,0.00062627473,0.000024534673,0.00019112208,0.000002925661],"about_ca_topic_score_codex":0.005340953,"about_ca_topic_score_gemma":0.0046311445,"teacher_disagreement_score":0.005340953,"about_ca_system_score_codex":0.00013735791,"about_ca_system_score_gemma":0.00006985331,"threshold_uncertainty_score":0.01061976},"labels":[],"label_agreement":null},{"id":"W4321479676","doi":"10.1029/2022gl101493","title":"Preconditioning of Summer Melt Ponds From Winter Sea Ice Surface Temperature","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":23,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft","keywords":"Snow; Melt pond; Sea ice; Climatology; Arctic; Environmental science; Atmospheric sciences; Snowmelt; Geology; Arctic ice pack; Sea surface temperature; Oceanography; Antarctic sea ice; Geomorphology","score_opus":0.02922000551559385,"score_gpt":0.2865981198203272,"score_spread":0.25737811430473334,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321479676","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99699247,0.00004767881,0.0020456156,0.000011963468,0.0000056185118,0.000004687151,0.00020433165,0.00011706261,0.00057055434],"genre_scores_gemma":[0.9991416,0.000013190848,0.00045656227,0.0000022339925,0.0000022981335,0.0000027959334,0.00024038753,0.000006633256,0.00013429654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.0000091682805,0.00000449766,0.000018610788,0.000010124977,0.000020194306],"domain_scores_gemma":[0.99978536,0.000051690156,0.00005948099,0.00002324591,0.000040936902,0.00003932222],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017587634,0.00016152178,0.00023601831,0.00033504976,0.00020788766,0.00035596863,0.00009400577,0.000121485115,0.0010950008],"category_scores_gemma":[0.0004898606,0.00010054041,0.00020176821,0.000267895,0.000114784525,0.00023472792,0.00021970145,0.00012734819,0.00021092025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012145822,0.00009399721,0.794678,0.00008676962,0.000068856585,0.00013311827,0.00021639522,0.016899904,0.115073025,0.00017807282,0.0011540477,0.07020331],"study_design_scores_gemma":[0.000011657592,0.00009797817,0.92732304,0.0000071018335,0.0000199993,0.00005188566,0.00007803496,0.057456248,0.01423644,0.00015614845,0.00055398623,0.000007456377],"about_ca_topic_score_codex":0.005197641,"about_ca_topic_score_gemma":0.008984299,"teacher_disagreement_score":0.005197641,"about_ca_system_score_codex":0.00021751954,"about_ca_system_score_gemma":0.00022781882,"threshold_uncertainty_score":0.01033479},"labels":[],"label_agreement":null},{"id":"W4321617968","doi":"10.1029/2022gl100948","title":"Northward Extent of Atmospheric Mercury Transboundary Transport to the Himalayas and Tibetan Plateau Region","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"","keywords":"Westerlies; Plateau (mathematics); Mercury (programming language); Monsoon; Geology; Atmospheric circulation; South asia; Physical geography; Pollution; Environmental science; Climatology; Geography","score_opus":0.04043676543532744,"score_gpt":0.3077703626704835,"score_spread":0.2673335972351561,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321617968","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99860436,0.00014317829,0.000047924885,0.000041028463,0.0000019823983,0.0000017915643,0.000100516816,0.000004388008,0.001054876],"genre_scores_gemma":[0.9994272,0.00008352333,0.000047128433,0.000011187518,0.0000038556245,0.0000017587457,0.000109338056,7.7777497e-7,0.00031533008],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.000014465045,0.0000049545283,0.000018942686,0.00001293733,0.000019667863],"domain_scores_gemma":[0.9998282,0.000021082422,0.000048389673,0.000008830737,0.000056445315,0.000036894602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015018757,0.00017829306,0.00010124765,0.0007471894,0.0005658897,0.0006725573,0.00011994658,0.00012805263,0.001121663],"category_scores_gemma":[0.00021024143,0.00007885938,0.00015203317,0.0011812717,0.00024962277,0.00023189459,0.00032219468,0.0001615615,0.00010081585],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010560544,0.000022029479,0.9775174,0.000047601014,0.00009760901,0.0005111952,0.0015061366,0.0004247498,0.009817065,0.00019894622,0.00018812834,0.009563587],"study_design_scores_gemma":[0.0000018303036,0.000009172551,0.99851006,0.000004803399,0.00001057085,0.000055812703,0.000677341,0.00020467526,0.00020540817,0.000027225724,0.00029077101,0.0000022813108],"about_ca_topic_score_codex":0.06849688,"about_ca_topic_score_gemma":0.08028634,"teacher_disagreement_score":0.06849688,"about_ca_system_score_codex":0.00047304467,"about_ca_system_score_gemma":0.00057473936,"threshold_uncertainty_score":0.13619637},"labels":[],"label_agreement":null},{"id":"W4321781533","doi":"10.1029/2022gl101985","title":"Low‐Altitude UAV Imaging Accurately Quantifies Eelgrass Wasting Disease From Alaska to California","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal plant biology","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Tula Foundation","funders":"Hakai Institute; Tula Foundation; Smithsonian Institution; National Science Foundation","keywords":"Seagrass; Altitude (triangle); Intertidal zone; Environmental science; Mass wasting; Habitat; Remote sensing; Geography; Physical geography; Ecology; Geology; Biology","score_opus":0.057592194152266254,"score_gpt":0.31254692965612396,"score_spread":0.2549547355038577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4321781533","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99893445,0.000054275955,0.00043698304,0.0000048932516,0.0000022662932,0.0000048197508,0.00012561721,0.000020826836,0.00041596705],"genre_scores_gemma":[0.9987733,0.00004677206,0.0008125305,0.0000067532137,0.0000011803389,0.0000032807116,0.00018926432,0.000002412884,0.00016458081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993193,0.000007917661,0.0000039889237,0.000026753884,0.000017163225,0.000012344347],"domain_scores_gemma":[0.999816,0.000035022607,0.00004595432,0.000011794081,0.000067425615,0.000023736839],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013560959,0.00016619117,0.00012673328,0.00043643007,0.00022974338,0.00041238967,0.00014066549,0.000113714705,0.00036333542],"category_scores_gemma":[0.00024842235,0.00009629918,0.00007821545,0.00023857241,0.00011286215,0.0001969586,0.00013209223,0.0001386836,0.00006225783],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013010867,0.00007053959,0.9234654,0.000043513628,0.00004180373,0.00007406811,0.00024296586,0.0018612901,0.05676061,0.000025192643,0.00022679522,0.01705775],"study_design_scores_gemma":[0.0000030422914,0.00005800161,0.98941576,0.000012591393,0.000029218352,0.00004886061,0.0004068651,0.0054032984,0.0043265135,0.000014434946,0.00027707225,0.00000432405],"about_ca_topic_score_codex":0.053498916,"about_ca_topic_score_gemma":0.12267565,"teacher_disagreement_score":0.053498916,"about_ca_system_score_codex":0.00032234492,"about_ca_system_score_gemma":0.0001698094,"threshold_uncertainty_score":0.10637504},"labels":[],"label_agreement":null},{"id":"W4322765699","doi":"10.1029/2022gl100563","title":"Large Contribution of Ozone‐Depleting Substances to Global and Arctic Warming in the Late 20th Century","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"International Institute for Applied Systems Analysis; Natural Environment Research Council; Sight Research UK; National Science Foundation","keywords":"Climatology; Global warming; Environmental science; Arctic; Radiative forcing; Climate change; Ozone depletion; Montreal Protocol; The arctic; Atmospheric sciences; Forcing (mathematics); Arctic geoengineering; Ozone layer; Arctic ice pack; Sea ice; Oceanography; Geology; Stratosphere","score_opus":0.022797494089140263,"score_gpt":0.2958268917577713,"score_spread":0.27302939766863105,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4322765699","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99347174,0.0016458024,0.0006600211,0.00067318685,0.000075987664,0.0000046943783,0.00079274055,0.000027641012,0.002648103],"genre_scores_gemma":[0.99845684,0.0005578445,0.00021817451,0.00007392347,0.00003126677,0.0000028347113,0.00032460384,0.000005810462,0.00032880594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999014,0.000019056024,0.0000067863325,0.000025292362,0.000018913572,0.0000285241],"domain_scores_gemma":[0.9998053,0.000027739658,0.000049834005,0.000018308481,0.00006130839,0.000037626116],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005989053,0.00020381216,0.0001775864,0.00050202775,0.0002731536,0.0007012209,0.00020317092,0.00038530419,0.0007526952],"category_scores_gemma":[0.00067419885,0.00012041276,0.0006064785,0.0004108644,0.00022301178,0.0003776199,0.0005611901,0.00034235936,0.000065925786],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00051054894,0.00007847354,0.8767249,0.0003400974,0.00093426916,0.0006118818,0.00040721474,0.048285466,0.03227487,0.0072697937,0.0019582298,0.030604217],"study_design_scores_gemma":[0.000015670992,0.00005680566,0.972736,0.00003878286,0.00015273232,0.00006922033,0.00013716255,0.012180576,0.004780486,0.0010555339,0.008754631,0.000022282044],"about_ca_topic_score_codex":0.05070842,"about_ca_topic_score_gemma":0.053449366,"teacher_disagreement_score":0.05070842,"about_ca_system_score_codex":0.0010862579,"about_ca_system_score_gemma":0.00085991854,"threshold_uncertainty_score":0.1008265},"labels":[],"label_agreement":null},{"id":"W4323352859","doi":"10.1029/2022gl101640","title":"A Storyline Approach to the June 2021 Northwestern North American Heatwave","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Climatology; Anomaly (physics); Anticyclone; Atmospheric circulation; Magnitude (astronomy); Environmental science; El Niño Southern Oscillation; Atmospheric sciences; Geology","score_opus":0.05243772935395535,"score_gpt":0.3095126977245385,"score_spread":0.25707496837058313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323352859","genre_codex":"other","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.22837466,0.005837867,0.14104806,0.043036774,0.0047823647,0.00054663187,0.051809154,0.0027989058,0.52176553],"genre_scores_gemma":[0.86803037,0.003551551,0.0714679,0.0013198745,0.0008983144,0.00044494818,0.013694641,0.00033986798,0.0402526],"study_design_codex":"not_applicable","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988174,0.00004518654,0.0000061207365,0.00002036084,0.000030460888,0.00001610887],"domain_scores_gemma":[0.9996749,0.000114610644,0.00005549931,0.000016886976,0.00008320078,0.00005487653],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042910824,0.00030354355,0.000094764495,0.0009968427,0.0009135407,0.002043347,0.00039897035,0.00054556486,0.015027617],"category_scores_gemma":[0.0013850597,0.0000974187,0.00017046838,0.0010563402,0.0002876439,0.0014057343,0.0006832207,0.0006879908,0.0009756288],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019011387,0.00011693603,0.03887981,0.0003650597,0.00007990803,0.0017519683,0.005593396,0.051372085,0.0023130416,0.23947345,0.44655305,0.21331124],"study_design_scores_gemma":[0.000024199098,0.00007860617,0.033196047,0.00024343801,0.000037874717,0.0002724479,0.0072872997,0.07048669,0.0012570729,0.07102898,0.8160292,0.000058168273],"about_ca_topic_score_codex":0.020655656,"about_ca_topic_score_gemma":0.043241553,"teacher_disagreement_score":0.020655656,"about_ca_system_score_codex":0.0009979741,"about_ca_system_score_gemma":0.0007022122,"threshold_uncertainty_score":0.050272346},"labels":[],"label_agreement":null},{"id":"W4323545133","doi":"10.1029/2022gl102027","title":"Global Asymmetries in the Influence of ENSO on Flood Risk Based on 1,600 Years of Hybrid Simulations","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Mitacs; Marine Environmental Observation Prediction and Response Network","keywords":"Predictability; Climatology; Teleconnection; Flood myth; El Niño Southern Oscillation; Environmental science; Observational study; Baseline (sea); Hazard; Geology; Geography; Statistics; Mathematics; Oceanography","score_opus":0.034429273236221504,"score_gpt":0.3261769537117391,"score_spread":0.2917476804755176,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323545133","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985133,0.000037933707,0.0006441578,0.000030416328,0.0000043242135,0.000002515951,0.00027873114,0.000022770459,0.0004658882],"genre_scores_gemma":[0.9994648,0.000010633275,0.00020310904,0.0000046526493,0.0000023367566,0.00000317995,0.00027159636,0.000004812423,0.00003490143],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997565,0.0000978859,0.000017461976,0.000067166824,0.0000223834,0.0000384885],"domain_scores_gemma":[0.99862945,0.00094487704,0.00013039171,0.0001269482,0.000088043715,0.00008026369],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010565998,0.0003650613,0.00038519656,0.00049578893,0.00015589775,0.00069066783,0.00034147242,0.00045729653,0.00087020616],"category_scores_gemma":[0.002538178,0.0001764037,0.0006156722,0.000397183,0.00029741268,0.00055852864,0.00042204597,0.00034167187,0.00006312756],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005060327,0.00009016045,0.10064826,0.000029983274,0.00045092223,0.00014374057,0.00005371183,0.8891754,0.0022603595,0.0007716545,0.00030847476,0.005561226],"study_design_scores_gemma":[0.00005891944,0.00011658408,0.08822349,0.000010099162,0.000121178906,0.00003416854,0.000073772884,0.9092725,0.0011402204,0.0006924953,0.00022847837,0.00002814281],"about_ca_topic_score_codex":0.008337198,"about_ca_topic_score_gemma":0.0049088723,"teacher_disagreement_score":0.008337198,"about_ca_system_score_codex":0.00044077894,"about_ca_system_score_gemma":0.00020187617,"threshold_uncertainty_score":0.016577363},"labels":[],"label_agreement":null},{"id":"W4323822301","doi":"10.1029/2022gl101054","title":"A 1000‐Year Record of Temperature From Isotopic Analysis of the Deep Critical Zone in Central China","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Global Institute for Water Security; University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Stalagmite; Paleoclimatology; Geology; Ice core; Soil water; Loess; Period (music); δ13C; Stable isotope ratio; Physical geography; Mineralogy; Hydrology (agriculture); Climatology; Holocene; Paleontology; Climate change; Soil science; Oceanography","score_opus":0.021045470126285996,"score_gpt":0.2947422127722568,"score_spread":0.2736967426459708,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4323822301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99957484,0.000028123188,0.000035581397,0.0000055229843,6.202825e-7,9.675679e-7,0.00019611095,0.0000027837548,0.00015546726],"genre_scores_gemma":[0.9994562,0.000023953362,0.000053116662,0.0000034078262,0.0000016099211,0.0000018549811,0.00034698585,9.81103e-7,0.00011183261],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995553,0.0000033119543,0.000003892894,0.000015686794,0.0000095119085,0.000011946419],"domain_scores_gemma":[0.9997329,0.000017696517,0.00007263,0.00002657948,0.00009623132,0.00005402028],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019188927,0.00017032119,0.00013652066,0.0014080261,0.00035516528,0.00025480567,0.00026095856,0.00014776982,0.0003313914],"category_scores_gemma":[0.0002491178,0.0001254602,0.00008567937,0.0010734827,0.00021536689,0.00020435722,0.0003094309,0.00009740997,0.0000678615],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000041648997,0.00001598924,0.97988224,0.00001775946,0.000036705962,0.00010820621,0.00037478397,0.00038311246,0.011887092,0.00008219139,0.00016593936,0.007004374],"study_design_scores_gemma":[0.0000010505296,0.000006001167,0.99915946,0.0000015142479,0.000004547796,0.000018536726,0.000051355797,0.00026569443,0.00028377076,0.000010614315,0.00019590871,0.0000015801044],"about_ca_topic_score_codex":0.058960117,"about_ca_topic_score_gemma":0.10682225,"teacher_disagreement_score":0.058960117,"about_ca_system_score_codex":0.0006504265,"about_ca_system_score_gemma":0.00038564723,"threshold_uncertainty_score":0.11723387},"labels":[],"label_agreement":null},{"id":"W4324348848","doi":"10.1029/2022gl101205","title":"New Insight Into the Transition From a SAR Arc to STEVE","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary","funders":"University of Calgary","keywords":"Ionosphere; Arc (geometry); Geology; Wavelength; Spectral line; Spectrograph; Physics; Emission spectrum; Astrophysics; Atmospheric sciences; Geophysics; Optics; Astronomy","score_opus":0.018337116249524183,"score_gpt":0.2866693351880327,"score_spread":0.26833221893850856,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4324348848","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99528766,0.000061595754,0.0017953153,0.000027720174,0.0000021177993,0.0000037008415,0.00007867922,0.000054310593,0.0026887413],"genre_scores_gemma":[0.9994504,0.000019375151,0.00022919747,0.000005852058,0.0000015206447,0.0000010011547,0.000050704282,0.000006489479,0.00023539721],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99997866,0.0000015397542,7.78219e-7,0.0000064647284,0.0000039077922,0.000008572234],"domain_scores_gemma":[0.9999279,0.000023076858,0.000016045706,0.000008227264,0.0000101020805,0.000014608652],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006115004,0.000099513716,0.00009091547,0.0003318957,0.00016014569,0.00032813224,0.0001411776,0.0001707666,0.002208728],"category_scores_gemma":[0.00019447239,0.00010870145,0.000108375636,0.00023732234,0.0002680626,0.00025069105,0.00021326625,0.0002537126,0.00015496921],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007592572,0.00011949777,0.47483552,0.00009185045,0.00006801237,0.001444956,0.0012941082,0.011194093,0.4772626,0.0064855474,0.0007701209,0.025674455],"study_design_scores_gemma":[0.000008323678,0.00008840165,0.9620954,0.0000102188105,0.000012773574,0.00052583625,0.00055689685,0.019035285,0.014016938,0.0013853398,0.0022534607,0.00001106355],"about_ca_topic_score_codex":0.0015612503,"about_ca_topic_score_gemma":0.0023226487,"teacher_disagreement_score":0.002208728,"about_ca_system_score_codex":0.0001761242,"about_ca_system_score_gemma":0.00009436025,"threshold_uncertainty_score":0.0073889494},"labels":[],"label_agreement":null},{"id":"W4327604749","doi":"10.1029/2022gl101857","title":"Drivers and Potential Consequences of Observed Extreme Hypoxia Along the Canadian Pacific Continental Shelf","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria; Fisheries and Oceans Canada; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Marine Environmental Observation Prediction and Response Network","keywords":"Oceanography; Continental shelf; Upwelling; Biogeochemical cycle; Hypoxia (environmental); Biogeochemistry; Oxygen minimum zone; Environmental science; Water column; Phytoplankton; Geology; Ecology; Oxygen; Nutrient; Biology; Chemistry","score_opus":0.0554639355261601,"score_gpt":0.24324843475984387,"score_spread":0.18778449923368376,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4327604749","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99738044,0.00015560973,0.00004518226,0.00031600278,0.000005978953,0.000006743494,0.0009571408,0.000004318533,0.0011285476],"genre_scores_gemma":[0.99949944,0.00008291997,0.000029527817,0.000021207894,0.0000026532541,0.0000022422066,0.00023755396,9.642304e-7,0.00012342545],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997073,0.000028356599,0.00001678425,0.00006319835,0.000078289035,0.00010605838],"domain_scores_gemma":[0.9985662,0.00012728178,0.00043091568,0.000040737952,0.00053327216,0.00030163745],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037258994,0.00016149743,0.00016673606,0.0008267703,0.0012118609,0.0011149617,0.000578361,0.00036130872,0.001322067],"category_scores_gemma":[0.0016252819,0.00019174807,0.00023969964,0.0017853744,0.0006654597,0.00033900756,0.0007720859,0.00043525992,0.000052743588],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000013042952,0.0000040252103,0.9983785,0.000005721436,0.000023951208,0.00003165053,0.00013351308,0.00016233943,0.00015837178,0.00007540741,0.0001963159,0.0008171386],"study_design_scores_gemma":[4.2905822e-7,0.000001322586,0.9993055,0.0000027890626,0.0000036290785,0.000009237211,0.00033833153,0.00014653786,0.00001210406,0.000018050068,0.00015996807,0.0000021019405],"about_ca_topic_score_codex":0.94563204,"about_ca_topic_score_gemma":0.9774914,"teacher_disagreement_score":0.05436796,"about_ca_system_score_codex":0.0066387514,"about_ca_system_score_gemma":0.0072168154,"threshold_uncertainty_score":0.10937625},"labels":[],"label_agreement":null},{"id":"W4327933932","doi":"10.1029/2022gl100610","title":"Abyssal Circulation From the Yap‐Mariana Junction to the Northern Philippine Basin","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"","keywords":"Geology; Oceanography; Ridge; Shutdown of thermohaline circulation; Deep sea; Structural basin; Abyssal zone; Ocean current; North Atlantic Deep Water; Biogeochemical cycle; Climatology; Thermohaline circulation; Paleontology","score_opus":0.03352554460639838,"score_gpt":0.26439262389521034,"score_spread":0.23086707928881195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4327933932","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969844,0.00009164245,0.00009278506,0.00010855776,0.0000070689316,0.000004432771,0.00066677696,0.000048617494,0.001995747],"genre_scores_gemma":[0.9988644,0.00008353228,0.00014039305,0.000010561046,0.000007218641,0.000005105571,0.0004464169,0.000004913933,0.00043744687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000052239475,0.0000027798312,0.0000152537405,0.000009932142,0.000009650278],"domain_scores_gemma":[0.99986947,0.0000111433055,0.00002893205,0.0000072851067,0.000050518578,0.000032554628],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000109322136,0.00030008145,0.00012317521,0.0005416896,0.00051308156,0.0006464266,0.00020692105,0.00018701903,0.0018268861],"category_scores_gemma":[0.00034209495,0.00012176217,0.00017556787,0.000779596,0.00017834424,0.00032922297,0.00065402465,0.00024079412,0.00018855873],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002485699,0.000083428524,0.9295692,0.00018673374,0.00024212504,0.0018559407,0.0028090933,0.0086849,0.020334633,0.00073538674,0.0030324613,0.032217402],"study_design_scores_gemma":[0.0000114563545,0.00002643717,0.99029,0.000016418328,0.000033381268,0.00008723272,0.00074250635,0.005539176,0.00077266485,0.00006728819,0.0024000937,0.000013249613],"about_ca_topic_score_codex":0.14861882,"about_ca_topic_score_gemma":0.103792325,"teacher_disagreement_score":0.14861882,"about_ca_system_score_codex":0.00067740143,"about_ca_system_score_gemma":0.00074527867,"threshold_uncertainty_score":0.2955075},"labels":[],"label_agreement":null},{"id":"W4327933956","doi":"10.1029/2022gl100951","title":"Impact of Thermally Forced Circulations on the Diurnal Cycle of Summer Precipitation Over the Southeastern Tibetan Plateau","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"","keywords":"Plateau (mathematics); Climatology; Midnight; Precipitation; Sunset; Diurnal cycle; Atmospheric circulation; Environmental science; Atmospheric sciences; Diurnal temperature variation; Geology; Meteorology; Geography","score_opus":0.07370585651666414,"score_gpt":0.3552450558418225,"score_spread":0.28153919932515836,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4327933956","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994599,0.000020304693,0.000066276,0.000031098418,0.000005314814,0.0000015120548,0.00013829423,0.000011053914,0.00026611725],"genre_scores_gemma":[0.99976176,0.000009045673,0.000025830877,0.000004974179,0.000004105473,0.0000018647835,0.00014443474,0.0000016570993,0.0000463604],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989057,0.00003619961,0.000009184225,0.000022509927,0.000014451873,0.00002711448],"domain_scores_gemma":[0.99970585,0.00007319969,0.00006127535,0.000028202456,0.00006156623,0.000069806076],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031104582,0.00019496122,0.00014051843,0.0003447173,0.00033431363,0.00063432194,0.00020435643,0.00019839463,0.0009797409],"category_scores_gemma":[0.0006933751,0.00011215482,0.0003128603,0.0003718924,0.0002542439,0.0002776146,0.00030492563,0.0002215564,0.00006659823],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023950191,0.00009190591,0.96742266,0.000025503248,0.000179494,0.00036191626,0.00023374023,0.016878763,0.0074985675,0.00031935098,0.00050963764,0.0062389695],"study_design_scores_gemma":[0.000022838318,0.000041416817,0.96713924,0.000006804293,0.000021181417,0.000032012158,0.0002646043,0.031802498,0.00032462878,0.000088521265,0.000246395,0.00000977017],"about_ca_topic_score_codex":0.04110799,"about_ca_topic_score_gemma":0.043682046,"teacher_disagreement_score":0.04110799,"about_ca_system_score_codex":0.00051719975,"about_ca_system_score_gemma":0.0005284459,"threshold_uncertainty_score":0.0817374},"labels":[],"label_agreement":null},{"id":"W4353085769","doi":"10.1029/2023gl102815","title":"A Robust Estimate of Continental‐Scale Terrestrial Carbon Sinks Using GOSAT XCO <sub>2</sub> Retrievals","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Environmental science; Biosphere; Carbon cycle; Scale (ratio); Satellite; Carbon fibers; Spatial variability; Carbon sink; Atmospheric sciences; Climatology; Ecosystem; Climate change; Geology; Statistics; Computer science; Mathematics; Geography; Oceanography; Ecology; Algorithm","score_opus":0.03826707007242088,"score_gpt":0.28643341920333565,"score_spread":0.24816634913091476,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4353085769","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.90798163,0.00061509706,0.08289808,0.0002828606,0.000033741377,0.000039009436,0.0038854985,0.0010428586,0.0032212099],"genre_scores_gemma":[0.9719267,0.0001713086,0.024075162,0.000036425456,0.00001983455,0.000018057153,0.0033594295,0.000094006704,0.0002991256],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99987006,0.00003133994,0.000006671335,0.000041830866,0.00003512582,0.000014910105],"domain_scores_gemma":[0.99974376,0.000071778995,0.000052352327,0.00005035058,0.00006660948,0.0000151575705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057478726,0.00063962414,0.00029660907,0.000940278,0.00021080303,0.00065177056,0.00029500015,0.0003472185,0.0005708106],"category_scores_gemma":[0.0014723102,0.00024108287,0.00041354293,0.00068719033,0.00025756424,0.00072414643,0.000479731,0.00031303783,0.00013545968],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003882196,0.00008139404,0.17615393,0.00017335187,0.0007456629,0.00009875079,0.00008320235,0.64396286,0.08796725,0.0043927114,0.002096145,0.08385656],"study_design_scores_gemma":[0.00005894522,0.000024698964,0.15377963,0.000023299295,0.00012726377,0.000024613186,0.000045580582,0.82396114,0.017481292,0.0022460972,0.0021577592,0.000069703216],"about_ca_topic_score_codex":0.025394697,"about_ca_topic_score_gemma":0.03173246,"teacher_disagreement_score":0.025394697,"about_ca_system_score_codex":0.0005371217,"about_ca_system_score_gemma":0.000851824,"threshold_uncertainty_score":0.050493777},"labels":[],"label_agreement":null},{"id":"W4360610011","doi":"10.1029/2023gl102940","title":"Disposal From In Situ Bitumen Recovery Induced the <i>M</i><sub><i>L</i></sub> 5.6 Peace River Earthquake","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada; University of Alberta","funders":"","keywords":"Geology; Asphalt; Seismology; Fault (geology); Tectonics; Geochemistry; Archaeology","score_opus":0.038698912940083305,"score_gpt":0.2696933580531697,"score_spread":0.23099444511308637,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4360610011","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998209,0.00001633374,0.00025939563,0.00002274,0.0000032982714,0.000004617788,0.00014544185,0.000021474556,0.0013176545],"genre_scores_gemma":[0.99957913,0.000012051619,0.00008226124,0.0000074948975,0.0000011267457,0.0000010201777,0.00010547232,0.0000023686796,0.0002091938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988246,0.0000091912125,0.0000075167736,0.00001443999,0.000050251205,0.000036095138],"domain_scores_gemma":[0.99975735,0.000029813365,0.00010279036,0.000022014847,0.000051969902,0.000036095444],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012090485,0.00016587453,0.00016418796,0.00033873104,0.00029963176,0.00035487927,0.00024849956,0.00022454328,0.001597392],"category_scores_gemma":[0.00034754802,0.0000705745,0.00013109866,0.00038192072,0.000293306,0.00017075926,0.0003047013,0.00022383747,0.00015669955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007905127,0.00023019254,0.7153894,0.00020137773,0.00008428814,0.0015000138,0.0005865089,0.0048485445,0.23729314,0.00043725775,0.0013103131,0.037328415],"study_design_scores_gemma":[0.000008985059,0.00017566248,0.94816434,0.000008540479,0.000021502727,0.00017678867,0.00047566628,0.001933789,0.04799023,0.00008334158,0.0009537043,0.0000075048133],"about_ca_topic_score_codex":0.008789243,"about_ca_topic_score_gemma":0.019377764,"teacher_disagreement_score":0.99121076,"about_ca_system_score_codex":0.0005732376,"about_ca_system_score_gemma":0.00029728425,"threshold_uncertainty_score":0.017476141},"labels":[],"label_agreement":null},{"id":"W4361204416","doi":"10.1029/2022gl102502","title":"Intermittent Generation of Internal Solitary‐Like Waves on the Northern Shelf of the South China Sea","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Internal tide; Geology; Oceanography; Forcing (mathematics); Seafloor spreading; Continental shelf; Internal wave; Climatology","score_opus":0.037754958424244436,"score_gpt":0.260044514201078,"score_spread":0.22228955577683357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361204416","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99978,0.000005696842,0.000045511995,0.0000064019623,8.1598944e-7,8.2908133e-7,0.000013879581,0.0000024632595,0.00014441863],"genre_scores_gemma":[0.9998872,0.0000044642693,0.00003077272,0.0000016638096,9.937951e-7,9.965255e-7,0.000026622376,4.0227042e-7,0.000046856698],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999646,0.0000033939227,0.0000027246708,0.000009679493,0.00001032533,0.000009205451],"domain_scores_gemma":[0.9998042,0.00002626989,0.000049252056,0.000018239309,0.000043014974,0.00005910201],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010391553,0.00016356105,0.00017631946,0.000432469,0.00032855105,0.00024231694,0.00016521772,0.00015856785,0.0005216206],"category_scores_gemma":[0.0002646231,0.00012144294,0.00015142784,0.0003132525,0.00041412853,0.00015353019,0.0003192806,0.000113848924,0.000053815515],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021397509,0.00007446583,0.9312396,0.000056666777,0.00009588559,0.00090336625,0.0005939485,0.0060973237,0.046941757,0.00032254535,0.0003848273,0.013075652],"study_design_scores_gemma":[0.0000089998075,0.000060704424,0.98715127,0.0000032899322,0.000017347484,0.000042146447,0.00020451065,0.011167591,0.0011422429,0.00007987883,0.00011559085,0.000006571214],"about_ca_topic_score_codex":0.01142374,"about_ca_topic_score_gemma":0.011786016,"teacher_disagreement_score":0.01142374,"about_ca_system_score_codex":0.0002911618,"about_ca_system_score_gemma":0.00028078514,"threshold_uncertainty_score":0.022714496},"labels":[],"label_agreement":null},{"id":"W4361216979","doi":"10.1029/2022gl102057","title":"A Note on the Timing and Nature of the Moho Geometry and Upper Mantle Structure Beneath Southern New England","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Waterloo; Geological Survey of Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Fibrous joint; Paleontology; Laurentia; Lithosphere; Terrane; Devonian; Paleozoic; Magmatism; Carboniferous; Seismology; Structural basin; Tectonics","score_opus":0.021082228630068978,"score_gpt":0.2681510312038259,"score_spread":0.2470688025737569,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361216979","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.981312,0.00072973844,0.00074481854,0.0013301272,0.000037883412,0.0000065493787,0.00076202414,0.000026700765,0.015050153],"genre_scores_gemma":[0.99602556,0.0002457539,0.0005334691,0.00015416094,0.000013146036,0.0000047135068,0.00012098062,0.0000066263374,0.002895498],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.0000038246276,0.0000044343615,0.000018921088,0.000007925841,0.000011440465],"domain_scores_gemma":[0.9997191,0.00006875805,0.000069183676,0.000033197386,0.0000805274,0.000029130932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021088708,0.00007062667,0.00011719996,0.00033287072,0.00046623326,0.0009953134,0.00018935,0.0002291549,0.0030985933],"category_scores_gemma":[0.00044492868,0.00010692987,0.000064610074,0.00028196818,0.00048559095,0.0005914433,0.0004986364,0.00034978523,0.00022997458],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042493799,0.000020261039,0.81065583,0.00022616547,0.000084245345,0.001825593,0.006020127,0.00068045367,0.09367752,0.0025077772,0.0037246977,0.08015237],"study_design_scores_gemma":[0.000003687832,0.000009755846,0.98834175,0.000023396942,0.00001333686,0.00027809967,0.0014325969,0.00017628488,0.0019947663,0.00020602618,0.0075105033,0.000009803785],"about_ca_topic_score_codex":0.14002372,"about_ca_topic_score_gemma":0.43133432,"teacher_disagreement_score":0.14002372,"about_ca_system_score_codex":0.0005880626,"about_ca_system_score_gemma":0.000356792,"threshold_uncertainty_score":0.27841735},"labels":[],"label_agreement":null},{"id":"W4361269099","doi":"10.1029/2023gl102762","title":"Influence of the Madden‐Julian Oscillation on Continental United States Hurricane Landfalls","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Office of Naval Research; Natural Sciences and Engineering Research Council of Canada; G. Unger Vetlesen Foundation; National Oceanic and Atmospheric Administration; Cooperative Institute for Research in Environmental Sciences; Mississippi State University","keywords":"Madden–Julian oscillation; Tropical cyclone; Climatology; Landfall; Convection; Southern Hemisphere; Oceanography; Indian ocean; Geology; Peninsula; Storm; Geography; Meteorology","score_opus":0.027988322994189643,"score_gpt":0.28946658213721643,"score_spread":0.2614782591430268,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4361269099","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968989,0.00021409639,0.000036857156,0.00025099653,0.000030328281,0.0000034781212,0.0006429109,0.0000066935086,0.0019157978],"genre_scores_gemma":[0.9992405,0.00010223008,0.000030222036,0.00003168949,0.000021803746,0.0000022980037,0.000396733,0.0000025512868,0.00017198242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997993,0.00004499049,0.000020144778,0.000035270325,0.000050698094,0.000049664523],"domain_scores_gemma":[0.9986297,0.00026672767,0.0005624488,0.000055813798,0.00025938617,0.00022592154],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003319751,0.0001317223,0.000181397,0.00060522195,0.00046490406,0.00082969473,0.00013876257,0.00018392007,0.0016820799],"category_scores_gemma":[0.0022027537,0.00006977788,0.00017425533,0.0007493283,0.00021239223,0.0003042859,0.0005978605,0.00029325148,0.00012874966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005552514,0.000014870405,0.99398994,0.000009999487,0.000038839687,0.00009460055,0.0001106655,0.00058122876,0.00036481654,0.000110926485,0.000916261,0.0037123223],"study_design_scores_gemma":[0.000001910526,0.0000105340805,0.9978935,0.000011244462,0.0000102884305,0.000020132975,0.00028384477,0.0008027613,0.000071390736,0.000023043396,0.0008690746,0.0000022656684],"about_ca_topic_score_codex":0.0473673,"about_ca_topic_score_gemma":0.11271844,"teacher_disagreement_score":0.0473673,"about_ca_system_score_codex":0.0005573424,"about_ca_system_score_gemma":0.0004442313,"threshold_uncertainty_score":0.09418321},"labels":[],"label_agreement":null},{"id":"W4362453547","doi":"10.1029/2022gl102216","title":"Estimating Arctic Ocean Acoustic Travel Times Using an Earth System Model","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Los Alamos National Laboratory; Office of Naval Research","keywords":"Arctic; Environmental science; The arctic; Range (aeronautics); Climate change; Meteorology; Geology; Climatology; Oceanography; Geography; Engineering","score_opus":0.05300715942117384,"score_gpt":0.29801975947788883,"score_spread":0.245012600056715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362453547","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.96495163,0.00010563892,0.02938362,0.00016785886,0.000044303582,0.00002059923,0.0018275926,0.0003656144,0.0031332558],"genre_scores_gemma":[0.990833,0.0000681517,0.007383686,0.000012362958,0.000009779131,0.000016589109,0.0011104079,0.000027172777,0.0005388539],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987173,0.00003635177,0.0000076629285,0.000035737437,0.000026222555,0.000022365155],"domain_scores_gemma":[0.99967086,0.00015246023,0.00003287804,0.0000247602,0.000086716085,0.000032318872],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037450367,0.0004832471,0.00034388585,0.00072078727,0.000498106,0.0009083694,0.00042358504,0.0005498218,0.0009717043],"category_scores_gemma":[0.0015731765,0.00036460135,0.0006134096,0.00067722745,0.0001802164,0.0006225108,0.00033675306,0.0004970204,0.00024244978],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036030964,0.000016848058,0.010889005,0.000009024353,0.000033980563,0.00002666242,0.00001746426,0.9853265,0.0004609068,0.00024903176,0.0001890525,0.002745434],"study_design_scores_gemma":[0.0000065515037,0.000009038687,0.002902842,0.0000027924702,0.000010264312,0.000003537957,0.000012508373,0.9966125,0.00016210096,0.000118060925,0.00015292446,0.000006792362],"about_ca_topic_score_codex":0.27450275,"about_ca_topic_score_gemma":0.118736535,"teacher_disagreement_score":0.27450275,"about_ca_system_score_codex":0.0010406942,"about_ca_system_score_gemma":0.0015027792,"threshold_uncertainty_score":0.54581},"labels":[],"label_agreement":null},{"id":"W4362720773","doi":"10.1029/2022gl101940","title":"Flexural Response to Erosional Unloading of Continental Margins: An Example From the Bering Sea, USA","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Geology; Canyon; Pleistocene; Continental margin; Paleontology; Erosion; Submarine canyon; Continental shelf; Passive margin; Quaternary; Unconformity; Geomorphology; Early Pleistocene; Sea level; Margin (machine learning); Oceanography; Tectonics; Rift","score_opus":0.09186585313348002,"score_gpt":0.3267457614297987,"score_spread":0.23487990829631872,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4362720773","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99808455,0.000058898717,0.000095838295,0.00007888618,0.0000030680862,0.0000031773397,0.00022638687,0.000012723304,0.0014364343],"genre_scores_gemma":[0.99889225,0.00008169188,0.00017468534,0.000018618732,0.0000019105094,0.0000021365818,0.00025902296,0.000004571933,0.00056508114],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994075,0.000015760788,0.0000036403799,0.000017990185,0.000009219525,0.000012671385],"domain_scores_gemma":[0.99973935,0.000075999735,0.000046271154,0.00001674723,0.00008352998,0.000038136426],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002493875,0.0002811784,0.00022006834,0.00041092353,0.00033189665,0.0006803397,0.00023251452,0.00031877297,0.001702353],"category_scores_gemma":[0.0006584555,0.00011468639,0.00028445365,0.00062929,0.00022976287,0.0003292688,0.00030051492,0.0002352587,0.00017339627],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021037184,0.000102520105,0.9164954,0.000048618836,0.00014821156,0.00092159584,0.00040122707,0.06427667,0.0025731877,0.0004585884,0.0016490236,0.012714725],"study_design_scores_gemma":[0.000025826585,0.00009582152,0.94198954,0.00002184818,0.00006112082,0.00008727179,0.000724999,0.054552868,0.00055790774,0.00025725248,0.0016070878,0.000018494007],"about_ca_topic_score_codex":0.17214559,"about_ca_topic_score_gemma":0.29243144,"teacher_disagreement_score":0.17214559,"about_ca_system_score_codex":0.00085164106,"about_ca_system_score_gemma":0.00043041818,"threshold_uncertainty_score":0.34228718},"labels":[],"label_agreement":null},{"id":"W4364374731","doi":"10.1029/2022gl100913","title":"Wood‐Based Carbon Storage in the Mackenzie River Delta: The World's Largest Mapped Riverine Wood Deposit","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Aurora Research Institute; University of Colorado Boulder; Sight Research UK; Colorado State University; National Science Foundation","keywords":"Delta; River delta; Permafrost; Carbon stock; Geology; Physical geography; Carbon fibers; Environmental science; Hydrology (agriculture); Arctic; Oceanography; Climate change; Geography","score_opus":0.06290308961621824,"score_gpt":0.3046552753239251,"score_spread":0.24175218570770687,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4364374731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9954751,0.00023248087,0.00025472467,0.00003594176,0.0000027665585,0.0000038155026,0.002352352,0.00003688878,0.0016060038],"genre_scores_gemma":[0.99821067,0.0000909415,0.00048251185,0.000010183891,0.0000026037826,0.0000034406398,0.00090500916,0.000006395023,0.00028833922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995327,0.000004021549,0.0000032779599,0.000019743195,0.00000836678,0.0000113484875],"domain_scores_gemma":[0.99985385,0.000015600968,0.000042936863,0.00001570858,0.000050964478,0.000020902538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011697521,0.00019696928,0.00011882638,0.0016534155,0.00029026848,0.000596991,0.0001578796,0.00012229453,0.0010572835],"category_scores_gemma":[0.00022140163,0.00011538887,0.00012858771,0.0014969191,0.0002531578,0.00033527214,0.0004319192,0.00013375502,0.00020033756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007699673,0.000022107572,0.96197027,0.00007151441,0.00008848276,0.00011982762,0.00046748447,0.001777784,0.0053044516,0.00025120552,0.0011834704,0.02866631],"study_design_scores_gemma":[0.000002180098,0.0000045492816,0.99566615,0.00002021447,0.000011625121,0.000039889528,0.00029233735,0.0015609341,0.0004588943,0.00007397284,0.00186265,0.000006562045],"about_ca_topic_score_codex":0.06675163,"about_ca_topic_score_gemma":0.15313622,"teacher_disagreement_score":0.9332484,"about_ca_system_score_codex":0.0003772137,"about_ca_system_score_gemma":0.00026270177,"threshold_uncertainty_score":0.13272619},"labels":[],"label_agreement":null},{"id":"W4365814560","doi":"10.1029/2022gl102377","title":"Biogeochemical River Runoff Drives Intense Coastal Arctic Ocean CO<sub>2</sub> Outgassing","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval; Makivik Corporation; University of Alberta","funders":"Japan Aerospace Exploration Agency; Earth Sciences Division; Horizon 2020 Framework Programme; Jet Propulsion Laboratory; Centre National de la Recherche Scientifique; European Commission; California Institute of Technology; National Aeronautics and Space Administration; National Science Foundation","keywords":"Biogeochemical cycle; Environmental science; Sink (geography); Arctic; Oceanography; Outgassing; Carbon sink; Permafrost; Climate change; Environmental chemistry; Geology; Chemistry","score_opus":0.023927312835681374,"score_gpt":0.26938767654614426,"score_spread":0.2454603637104629,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4365814560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904364,0.0000110188985,0.00018817866,0.000044798813,0.000002951504,0.0000018875147,0.0001472032,0.00001642306,0.0005438591],"genre_scores_gemma":[0.9996581,0.0000131603265,0.00010425157,0.000008676912,0.0000012757439,0.0000015024413,0.00008340173,0.0000038041048,0.00012567478],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999504,0.000011612969,0.0000032139608,0.000016361128,0.00000448988,0.000013900957],"domain_scores_gemma":[0.99991894,0.000018920127,0.00002162185,0.000007898637,0.000012056014,0.000020620482],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012658896,0.000284839,0.00020380983,0.00015193173,0.000311325,0.000775483,0.0003329012,0.00040232931,0.0011174909],"category_scores_gemma":[0.00028675428,0.0002525474,0.00045670688,0.00018404359,0.00033766334,0.00029743425,0.00030915637,0.00026027602,0.000077378485],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037205257,0.00016888071,0.3707402,0.00006383062,0.00021449743,0.00037286276,0.00016216101,0.5804312,0.041235425,0.0012047206,0.0010223829,0.004011787],"study_design_scores_gemma":[0.000057842786,0.00008907028,0.2630976,0.00000817158,0.000062708044,0.000049659633,0.00018049526,0.7311165,0.004208891,0.00040172838,0.00070001296,0.000027367594],"about_ca_topic_score_codex":0.10500608,"about_ca_topic_score_gemma":0.074342944,"teacher_disagreement_score":0.10500608,"about_ca_system_score_codex":0.0010503533,"about_ca_system_score_gemma":0.0007669178,"threshold_uncertainty_score":0.2087897},"labels":[],"label_agreement":null},{"id":"W4366827938","doi":"10.1029/2022gl102618","title":"Compensatory Effects Between CO<sub>2</sub>, Nitrogen Deposition, and Nitrogen Fertilization in Terrestrial Biosphere Models Without Nitrogen Compromise Projections of the Future Terrestrial Carbon Sink","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Nitrogen; Environmental science; Sink (geography); Cycling; Nitrogen cycle; Biosphere; Carbon sink; Carbon cycle; Global change; Carbon sequestration; Terrestrial ecosystem; Ecology; Ecosystem; Climate change; Chemistry; Geography; Biology; Forestry","score_opus":0.017463287831691685,"score_gpt":0.25930769705759127,"score_spread":0.2418444092258996,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4366827938","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98352724,0.00013673477,0.0075422586,0.00074512325,0.00006298728,0.00003120658,0.00071897765,0.00016426381,0.0070711407],"genre_scores_gemma":[0.9973574,0.000060876937,0.0016727466,0.0000930646,0.000011064144,0.000030243602,0.0001809627,0.00002720353,0.00056637847],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999723,0.00014582132,0.00001697278,0.000048417078,0.00002393774,0.000041817813],"domain_scores_gemma":[0.9991679,0.00044180488,0.00011019224,0.00005940946,0.000124689,0.000096053656],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012199647,0.00081247964,0.00072274305,0.00046402856,0.00043243956,0.0010368697,0.0010095701,0.0013597861,0.0015318904],"category_scores_gemma":[0.0026089624,0.00037885795,0.00076141,0.0005923835,0.00077708974,0.001025802,0.0007577351,0.0005479353,0.00012182269],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006310914,0.000020441443,0.004752327,0.000016667947,0.000059441518,0.000044442942,0.00001126189,0.9925216,0.0005724949,0.0012170888,0.00015263494,0.00056849385],"study_design_scores_gemma":[0.000042818963,0.000040496245,0.0015687157,0.00000687617,0.00003535253,0.000011498386,0.000032956705,0.99642307,0.00024638945,0.0013456785,0.0002336119,0.0000125027045],"about_ca_topic_score_codex":0.034573205,"about_ca_topic_score_gemma":0.025080979,"teacher_disagreement_score":0.034573205,"about_ca_system_score_codex":0.0012322548,"about_ca_system_score_gemma":0.0013761269,"threshold_uncertainty_score":0.068743944},"labels":[],"label_agreement":null},{"id":"W4367051827","doi":"10.1029/2023gl102763","title":"Episodic Magma Hammers for the 15 January 2022 Cataclysmic Eruption of Hunga Tonga‐Hunga Ha'apai","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Instituto Dom Luiz, Universidade de Lisboa; Natural Resources Canada; University of California, Santa Barbara; U.S. Naval Observatory; Lamont-Doherty Earth Observatory, Columbia University; U.S. Geological Survey; Eidgenössische Technische Hochschule Zürich; Universidad de Chile; Institut de Physique du Globe de Paris; Universidade de Lisboa; University of California, San Diego; University of Oregon; National Oceanic and Atmospheric Administration; University of Texas at Austin; Univerzita Karlova v Praze; Dublin Institute for Advanced Studies; California Institute of Technology; U.S. Department of Energy; National Science Foundation","keywords":"Geology; Magma; Volcano; Seismology; Plume; Geophysics; Meteorology; Physics","score_opus":0.058588516394545584,"score_gpt":0.3162117509459883,"score_spread":0.2576232345514427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367051827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985012,0.000034882214,0.00016048817,0.00009545644,0.0000058925075,0.00000815565,0.00038801343,0.00003137222,0.0007745758],"genre_scores_gemma":[0.99949896,0.00001595172,0.00007137593,0.0000062026943,0.0000044053504,0.0000041733647,0.00025144414,0.000002569961,0.00014483466],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994516,0.000005079684,0.0000043819573,0.000015159439,0.000012884091,0.000017284776],"domain_scores_gemma":[0.99982834,0.00003035562,0.000043266824,0.000017814747,0.000027792517,0.000052483334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021701014,0.00021105263,0.00020934128,0.00064122357,0.000469258,0.00048230487,0.00026227682,0.00061427435,0.0018291118],"category_scores_gemma":[0.0006193131,0.00016948167,0.0002563127,0.0006466786,0.0002786283,0.00035584497,0.00055901194,0.00030102933,0.00016640523],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035787365,0.000102390535,0.9304602,0.00013741711,0.0001960223,0.00365235,0.0023191485,0.01892009,0.017538013,0.0011035549,0.0024755166,0.022737445],"study_design_scores_gemma":[0.000008482948,0.000029992172,0.98531324,0.0000052339633,0.000020332463,0.00012469763,0.00038941522,0.012682112,0.0003912069,0.00012828814,0.00089642656,0.000010624172],"about_ca_topic_score_codex":0.030361256,"about_ca_topic_score_gemma":0.051553916,"teacher_disagreement_score":0.030361256,"about_ca_system_score_codex":0.0011048918,"about_ca_system_score_gemma":0.0004515701,"threshold_uncertainty_score":0.060369074},"labels":[],"label_agreement":null},{"id":"W4367595465","doi":"10.1029/2022gl101919","title":"How Fast or How Many? Sources of Intermittent Sediment Transport","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"BC Hydro (Canada); Simon Fraser University","funders":"DEVCOM Army Research Laboratory; National Aeronautics and Space Administration","keywords":"Intermittency; Flume; Flux (metallurgy); Sediment; Sediment transport; Grain size; Geology; Magnitude (astronomy); Soil science; Environmental science; Atmospheric sciences; Hydrology (agriculture); Geomorphology; Mechanics; Physics; Geotechnical engineering; Turbulence; Flow (mathematics); Materials science","score_opus":0.03422319247874587,"score_gpt":0.2849644287359618,"score_spread":0.2507412362572159,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367595465","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9612345,0.001252654,0.031314857,0.0017360266,0.00007978539,0.00001596717,0.000401389,0.00027759647,0.0036872064],"genre_scores_gemma":[0.99824655,0.00012890136,0.0011600031,0.000048255286,0.000040152725,0.000005210358,0.00007416463,0.000023727483,0.00027315624],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99968493,0.000052251584,0.000021045671,0.000110872614,0.000073487245,0.00005737477],"domain_scores_gemma":[0.9960687,0.0018353564,0.0010882043,0.00038312917,0.00041207144,0.00021250008],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007461726,0.00026088842,0.0005847589,0.0011254862,0.0005647641,0.0014181883,0.00054357096,0.00080463506,0.0017118949],"category_scores_gemma":[0.006742719,0.00043392842,0.0002831295,0.0011631913,0.0007535614,0.0016030739,0.00086255476,0.0005698283,0.00022104578],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007428766,0.00020492797,0.61140394,0.0005005564,0.0005937336,0.0023924317,0.0014712871,0.09652095,0.046519555,0.07373845,0.011378117,0.15453318],"study_design_scores_gemma":[0.00008136498,0.00010642855,0.3063285,0.0001813559,0.00030354346,0.0012327863,0.0013713643,0.48251045,0.010523328,0.18658876,0.01057924,0.00019290642],"about_ca_topic_score_codex":0.0030123533,"about_ca_topic_score_gemma":0.001980873,"teacher_disagreement_score":0.0030123533,"about_ca_system_score_codex":0.0007319347,"about_ca_system_score_gemma":0.00024393445,"threshold_uncertainty_score":0.0059896708},"labels":[],"label_agreement":null},{"id":"W4367627294","doi":"10.1029/2022gl102680","title":"The Potential Role of Modified Electron Acoustic Wave and Nonlinear Mode Coupling in Mono‐Energetic Aurora","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Natural Science Foundation of China","keywords":"Physics; Magnetosphere; Alfvén wave; Electron; Ionosphere; Kinetic energy; Computational physics; Mode coupling; Acceleration; Coupling (piping); Electric field; Electron precipitation; Geophysics; Mesoscale meteorology; Magnetic field; Classical mechanics; Magnetohydrodynamics; Optics; Meteorology; Quantum mechanics","score_opus":0.011730449353028942,"score_gpt":0.27671907697021214,"score_spread":0.2649886276171832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367627294","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98365825,0.00015717535,0.0068729403,0.00027157183,0.000043198335,0.000020975991,0.0001661232,0.00015566382,0.008654083],"genre_scores_gemma":[0.9989077,0.000041118303,0.00055061816,0.00002078223,0.000006543281,0.000009670904,0.00004547411,0.00002326807,0.00039491773],"study_design_codex":"simulation_or_modeling","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.9999182,0.000022413638,0.0000043922273,0.000010739382,0.00001565548,0.00002857375],"domain_scores_gemma":[0.99978894,0.00007036848,0.000034253997,0.000026176984,0.000029926376,0.00005037096],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024552605,0.00044733204,0.00045211025,0.00032190882,0.0005610933,0.0010580145,0.00059407606,0.00079920463,0.002242408],"category_scores_gemma":[0.0008836978,0.0003297183,0.00047996268,0.00026294132,0.00062759884,0.00078798016,0.00062223437,0.00042036638,0.00015738524],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016076062,0.000105519415,0.012116092,0.00006983525,0.00008325457,0.00040666363,0.0001620207,0.9684411,0.010595737,0.005068631,0.00038921417,0.0024010898],"study_design_scores_gemma":[0.000031281463,0.000026155118,0.0023979458,0.0000036613526,0.0000091462225,0.000020900541,0.00003579358,0.99618065,0.00050797325,0.0005476423,0.00022997228,0.000008894656],"about_ca_topic_score_codex":0.007970179,"about_ca_topic_score_gemma":0.0031836305,"teacher_disagreement_score":0.007970179,"about_ca_system_score_codex":0.00040587797,"about_ca_system_score_gemma":0.00059823727,"threshold_uncertainty_score":0.015847564},"labels":[],"label_agreement":null},{"id":"W4367856267","doi":"10.1029/2023gl103156","title":"Deep Hydraulically‐Active Fractures in Sensitive Clay Deposits: Implications for Groundwater Flow and Slope Stability","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Landslides and related hazards","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ministère des Transports; Université Laval","funders":"Ministry of Public Security of the People's Republic of China","keywords":"Geology; Groundwater flow; Piezometer; Groundwater; Hydrogeology; Landslide; Glacial period; Current (fluid); Flow (mathematics); Hydraulic head; Geomorphology; Geotechnical engineering; Hydrology (agriculture); Fracture (geology); Slope stability; Disturbance (geology); Geochemistry; Aquifer","score_opus":0.022024278885451568,"score_gpt":0.3063697025523906,"score_spread":0.28434542366693905,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4367856267","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9991302,0.000020773701,0.00035825255,0.000017887636,2.4765342e-7,0.0000030356402,0.00012172364,0.000004903508,0.00034304618],"genre_scores_gemma":[0.9998056,0.000009586454,0.00009720834,0.0000017998486,2.153762e-7,8.907009e-7,0.000027200696,4.0942066e-7,0.00005710111],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999293,0.00001331484,0.000003977912,0.00001563724,0.000014478257,0.000023432987],"domain_scores_gemma":[0.99952924,0.00013561921,0.000108854794,0.000020571246,0.00014354273,0.00006205898],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024354662,0.00011679209,0.000113592556,0.0007664644,0.00039210866,0.00056027644,0.0002413989,0.00025920323,0.0007054795],"category_scores_gemma":[0.0009010088,0.000116155694,0.00010657968,0.00073049567,0.0006566103,0.00021738974,0.00022346836,0.00012845486,0.00006674675],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005767227,0.000020217609,0.97485334,0.000020022184,0.000022033184,0.00016002012,0.0003313331,0.010854509,0.0065155406,0.00032623968,0.000079366335,0.006759721],"study_design_scores_gemma":[0.0000013435246,0.000012863533,0.99100566,0.0000047042954,0.000005315243,0.000041223688,0.00049226906,0.007691169,0.0004870899,0.00017988004,0.00007435827,0.000004208635],"about_ca_topic_score_codex":0.42274225,"about_ca_topic_score_gemma":0.52588004,"teacher_disagreement_score":0.42274225,"about_ca_system_score_codex":0.0019406629,"about_ca_system_score_gemma":0.00088144996,"threshold_uncertainty_score":0.84056324},"labels":[],"label_agreement":null},{"id":"W4368404917","doi":"10.1029/2023gl102745","title":"Stratospheric Gas‐Phase Production Alone Cannot Explain Observations of Atmospheric Perchlorate on Earth","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Chemical Analysis and Environmental Impact","field":"Environmental Science","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Toronto Metropolitan University","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Perchlorate; Deposition (geology); Environmental science; Atmospheric sciences; Aerosol; Flux (metallurgy); Atmospheric chemistry; Environmental chemistry; Chemistry; Geology; Ozone","score_opus":0.06348445710261949,"score_gpt":0.31613140386802924,"score_spread":0.2526469467654098,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4368404917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971354,0.00004589611,0.001436676,0.000103343395,0.000004516928,0.0000053712542,0.00020671981,0.00006886761,0.0009932923],"genre_scores_gemma":[0.9993563,0.00003582901,0.00037680398,0.000014203463,0.0000017642182,0.0000043459218,0.000107411346,0.000012024288,0.00009126355],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.0000164632,0.0000032595842,0.00001590733,0.000010694097,0.00001629559],"domain_scores_gemma":[0.9998641,0.00006482517,0.000019860096,0.00001552789,0.00002051336,0.000015130595],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018486034,0.00046913815,0.00025883847,0.00016530658,0.0002815062,0.00041268303,0.00054852734,0.00065992965,0.00073818583],"category_scores_gemma":[0.00036351557,0.00019823958,0.0005762384,0.0001994296,0.00031462507,0.00043499196,0.00025067554,0.00026054066,0.000102533755],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013869,0.00006893451,0.11337056,0.000052843287,0.0001625186,0.00014185903,0.000061960964,0.86121166,0.020358512,0.00093978527,0.00026201407,0.003230669],"study_design_scores_gemma":[0.000098666314,0.00011503513,0.04484079,0.000006473352,0.000053674597,0.000047011912,0.000070260634,0.9464311,0.0069743497,0.0007358963,0.0006086469,0.000017970167],"about_ca_topic_score_codex":0.045187112,"about_ca_topic_score_gemma":0.01989773,"teacher_disagreement_score":0.045187112,"about_ca_system_score_codex":0.0008742323,"about_ca_system_score_gemma":0.00069890043,"threshold_uncertainty_score":0.08984822},"labels":[],"label_agreement":null},{"id":"W4377086973","doi":"10.1029/2023gl102794","title":"Potential Role of Mid‐Latitude Seaway on Early Paleogene Atlantic Overturning Circulation","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Natural Science Foundation of China","keywords":"Paleogene; Shutdown of thermohaline circulation; Geology; Oceanography; Arctic; Thermohaline circulation; North Atlantic Deep Water; Latitude; Climatology; Ocean current; The arctic; Paleontology; Structural basin","score_opus":0.02713581822714431,"score_gpt":0.2819135469819263,"score_spread":0.254777728754782,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4377086973","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99325436,0.00008968795,0.0009651196,0.00032721812,0.000028498545,0.0000052170253,0.00035823573,0.000040149087,0.0049314597],"genre_scores_gemma":[0.999406,0.000046685476,0.00012639975,0.000017586453,0.0000031668076,0.0000019455376,0.00007262349,0.0000111427935,0.00031440996],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999355,0.0000205961,0.000003981397,0.000013645048,0.0000071556497,0.00001912741],"domain_scores_gemma":[0.9998287,0.000040803738,0.000021311547,0.000016042522,0.000025123403,0.00006788897],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024305157,0.00029559364,0.00031926262,0.0002694586,0.00057195313,0.0015314937,0.00050497765,0.0007223172,0.0043226806],"category_scores_gemma":[0.0009302562,0.00021818839,0.00049923157,0.0002396903,0.0006082791,0.00070356805,0.0007333031,0.00045846016,0.00023563135],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004729544,0.00014491593,0.15806475,0.000055640787,0.00014431421,0.0004517449,0.00021723918,0.8092316,0.008960836,0.015479625,0.0010884934,0.0056878747],"study_design_scores_gemma":[0.00016489066,0.00014201118,0.07708042,0.00003393372,0.00008163372,0.00007701694,0.0003802847,0.91551274,0.0014334978,0.00293348,0.0021204762,0.000039530496],"about_ca_topic_score_codex":0.05693589,"about_ca_topic_score_gemma":0.032827854,"teacher_disagreement_score":0.05693589,"about_ca_system_score_codex":0.0012019657,"about_ca_system_score_gemma":0.0010644712,"threshold_uncertainty_score":0.11320901},"labels":[],"label_agreement":null},{"id":"W4378071706","doi":"10.1029/2022gl101801","title":"Hydrologic Connectivity and Patch‐To‐Hillslope Scale Relations in Dryland Ecosystems","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"U.S. Forest Service; Oak Ridge Institute for Science and Education; Simon Fraser University; U.S. Department of Agriculture; U.S. Department of Energy; National Science Foundation","keywords":"Surface runoff; Hydrology (agriculture); Ecohydrology; Environmental science; Sink (geography); Geology; Storm; Soil science; Ecosystem; Geotechnical engineering; Ecology; Geography","score_opus":0.023174351409439353,"score_gpt":0.28701777154573693,"score_spread":0.2638434201362976,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378071706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996457,0.000015225913,0.00007568407,0.0000089183295,2.382943e-7,0.0000016405202,0.00005199265,0.0000034159957,0.000197211],"genre_scores_gemma":[0.99982846,0.000012244328,0.000051841922,0.0000032817545,6.828224e-7,0.000002137465,0.00005370607,0.0000012780791,0.000046241927],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994314,0.000013741632,0.000003847416,0.000020060863,0.0000055414307,0.000013706647],"domain_scores_gemma":[0.999385,0.00023909606,0.00018526973,0.00004322702,0.000043349384,0.00010407786],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021339805,0.000081697304,0.00016819971,0.0007402107,0.00023517753,0.00059478515,0.000118779244,0.00012856355,0.0013266817],"category_scores_gemma":[0.00081367086,0.00010921284,0.00010598396,0.00045212102,0.0006628487,0.0004673004,0.000362035,0.00016101157,0.000072503644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027651453,0.00008942404,0.9644283,0.00004550955,0.00013800916,0.00015227188,0.00076721824,0.0074468288,0.019039016,0.0012094834,0.00024249926,0.0061650067],"study_design_scores_gemma":[0.000006264375,0.000025351928,0.9969693,0.0000017325972,0.000006962525,0.000024550944,0.00017575319,0.0022072694,0.00014816567,0.00034699467,0.00008514412,0.000002620401],"about_ca_topic_score_codex":0.005537462,"about_ca_topic_score_gemma":0.010325974,"teacher_disagreement_score":0.005537462,"about_ca_system_score_codex":0.000468831,"about_ca_system_score_gemma":0.00012586186,"threshold_uncertainty_score":0.011010408},"labels":[],"label_agreement":null},{"id":"W4378233852","doi":"10.1029/2023gl103733","title":"Multi‐Scale Ionospheric Poynting Fluxes Using Ground and Space‐Based Observations","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Saskatchewan","funders":"European Space Agency","keywords":"Poynting vector; Ionosphere; Swarm behaviour; Geophysics; Electric field; Physics; Magnetosphere; Convection; Geology; Meteorology; Magnetic field; Computer science","score_opus":0.06723703649715516,"score_gpt":0.32659255714821533,"score_spread":0.25935552065106016,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378233852","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9979215,0.00002363292,0.0009883714,0.0000111333975,0.000004188959,0.000006109005,0.0002878321,0.00003437976,0.000722794],"genre_scores_gemma":[0.99796885,0.000017376497,0.0013457065,0.0000023386142,0.0000051088705,0.0000041405337,0.00047462358,0.0000072859325,0.00017455599],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999306,0.000011121543,0.0000033641,0.000025722396,0.000014247696,0.000014865204],"domain_scores_gemma":[0.9998436,0.00004804993,0.00003372324,0.000019571382,0.000021872278,0.000033093056],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017496324,0.00023520624,0.00014392941,0.00080668565,0.00018131106,0.00045623304,0.000112065994,0.00020894923,0.00064250786],"category_scores_gemma":[0.00038334823,0.00009666656,0.00019503226,0.00052747363,0.00011513213,0.00038814713,0.0002765613,0.0001689191,0.000095632895],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012908627,0.00022645138,0.7741972,0.00007567036,0.0002567952,0.00043590844,0.00046164723,0.038601905,0.10367508,0.0005670305,0.0008031308,0.07940834],"study_design_scores_gemma":[0.000031046045,0.000102148006,0.9376733,0.0000081202525,0.00003957395,0.00006353344,0.00012333474,0.05404408,0.0069570397,0.00015645355,0.0007877711,0.000013591111],"about_ca_topic_score_codex":0.0032442976,"about_ca_topic_score_gemma":0.005820227,"teacher_disagreement_score":0.0032442976,"about_ca_system_score_codex":0.00018851952,"about_ca_system_score_gemma":0.000095776355,"threshold_uncertainty_score":0.006450832},"labels":[],"label_agreement":null},{"id":"W4378831391","doi":"10.1029/2023gl102758","title":"What Is the Altitude of Thermal Equilibrium?","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Aeronautics and Space Administration; Canadian Space Agency; National Science Foundation","keywords":"Thermosphere; Altitude (triangle); Ionosphere; Atmospheric sciences; Physics; Incoherent scatter; Thermalisation; Atmosphere (unit); Exosphere; Thermal; Electron temperature; Ion; Atmospheric models; Computational physics; Electron; Environmental science; Geophysics; Atomic physics; Meteorology; Nuclear physics","score_opus":0.024008487393071168,"score_gpt":0.3105274276221676,"score_spread":0.28651894022909646,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4378831391","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.85349065,0.01766781,0.015161527,0.012065923,0.00055067,0.000033846994,0.0009175283,0.00013443972,0.09997761],"genre_scores_gemma":[0.9976897,0.0010077567,0.0003767157,0.00013487376,0.00012004412,0.0000033530257,0.00006237394,0.000015347265,0.0005898309],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995751,0.00013411466,0.000024788449,0.00008249061,0.00009061679,0.000092999995],"domain_scores_gemma":[0.9984738,0.00053491455,0.0004085076,0.00008548758,0.00029565295,0.00020162568],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007122749,0.00010601793,0.00030900343,0.00054099533,0.0005499848,0.002224227,0.00047271425,0.00038953553,0.004724659],"category_scores_gemma":[0.0040684063,0.00011167534,0.0001535315,0.0006871694,0.0014997863,0.0022190234,0.00065102434,0.0005409546,0.0006124726],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000659657,0.0001381976,0.46248752,0.0014260861,0.0003900283,0.0008793263,0.004567298,0.009711924,0.010264978,0.2976047,0.017363371,0.19450691],"study_design_scores_gemma":[0.00003912478,0.00017691142,0.7036259,0.00070873165,0.00011420287,0.0012116138,0.012949864,0.008362408,0.004930829,0.20362183,0.064152546,0.00010599606],"about_ca_topic_score_codex":0.0031743208,"about_ca_topic_score_gemma":0.0023651123,"teacher_disagreement_score":0.004724659,"about_ca_system_score_codex":0.0007559803,"about_ca_system_score_gemma":0.00036000664,"threshold_uncertainty_score":0.015805542},"labels":[],"label_agreement":null},{"id":"W4379231303","doi":"10.1029/2022gl102685","title":"Variability in Biomass Burning Emissions Weakens Aerosol Forcing Due To Nonlinear Aerosol‐Cloud Interactions","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; University of Victoria","keywords":"Aerosol; Forcing (mathematics); Radiative forcing; Environmental science; Atmospheric sciences; Climatology; Northern Hemisphere; Latitude; Cloud forcing; Biomass burning; Sulfate aerosol; Climate model; Middle latitudes; Meteorology; Climate change; Geography; Physics; Geology","score_opus":0.024637133999128848,"score_gpt":0.30685159738051737,"score_spread":0.2822144633813885,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4379231303","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9980617,0.000044939115,0.0008576266,0.00006575528,0.0000071995833,0.0000017830027,0.000085304106,0.00001805009,0.00085763884],"genre_scores_gemma":[0.99981624,0.000012259322,0.00007381052,0.000007855235,0.0000030163162,6.605148e-7,0.000041881023,0.0000030880287,0.000041228646],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998367,0.00003983072,0.000015778336,0.000032288277,0.000035472083,0.000039969756],"domain_scores_gemma":[0.9991623,0.00040288203,0.00018557254,0.000091445676,0.000095225856,0.000062672945],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00057496614,0.00024462014,0.00023462926,0.0002836315,0.00027447534,0.00043929968,0.00022456812,0.00022839343,0.0007471884],"category_scores_gemma":[0.0017296539,0.00017759045,0.0002652786,0.0002538718,0.00028951452,0.00027865724,0.00046656822,0.00035466603,0.00010060438],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005458561,0.00016264973,0.7381853,0.00008106821,0.00036224583,0.00050105806,0.00012900072,0.08980646,0.15448786,0.0011320156,0.0005228941,0.014083625],"study_design_scores_gemma":[0.00001692389,0.0000676571,0.86627984,0.000012594063,0.000063549654,0.00011242879,0.00008822407,0.12291912,0.009173616,0.00082980597,0.00041915104,0.0000170808],"about_ca_topic_score_codex":0.008208168,"about_ca_topic_score_gemma":0.0060533257,"teacher_disagreement_score":0.008208168,"about_ca_system_score_codex":0.0003581272,"about_ca_system_score_gemma":0.00029822704,"threshold_uncertainty_score":0.016320765},"labels":[],"label_agreement":null},{"id":"W4380683238","doi":"10.1029/2023gl103765","title":"Subglacial Freshwater Drainage Increases Simulated Basal Melt of the Totten Ice Shelf","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":38,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"","keywords":"Geology; Ice shelf; Glacier; Ice stream; Plume; Outflow; Geomorphology; Ice divide; Shelf ice; Melt pond; Oceanography; Cryosphere; Sea ice; Meteorology","score_opus":0.04073539847456354,"score_gpt":0.2852207931413769,"score_spread":0.24448539466681335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380683238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903893,0.000012859875,0.00013387612,0.000022922864,0.000004698367,0.0000031224768,0.00020640064,0.00002379127,0.00055355224],"genre_scores_gemma":[0.9995523,0.000010550062,0.00009810617,0.000008195095,0.0000011781398,0.0000053135727,0.000149005,0.0000052964924,0.00016999632],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999583,0.0000079905485,0.0000025938546,0.000010752459,0.0000048210295,0.000015538228],"domain_scores_gemma":[0.99985945,0.000060163293,0.000017449041,0.0000100876605,0.000017921173,0.000034968394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010591264,0.00034203116,0.0002358053,0.00018836357,0.00023038214,0.0005139516,0.00034705634,0.0005177379,0.0022322587],"category_scores_gemma":[0.0003438578,0.00022630572,0.0005240983,0.00019601156,0.0003140353,0.00023630225,0.0003251685,0.0003040362,0.00010626145],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036177694,0.00014083384,0.08345847,0.00004456088,0.000113850205,0.0001996581,0.00009302682,0.9045124,0.006921677,0.00037349173,0.00048624267,0.0032939776],"study_design_scores_gemma":[0.00017177411,0.000248106,0.061788592,0.000017037664,0.00006957232,0.00002702225,0.00014815637,0.93422,0.0026118616,0.00022705234,0.00044881398,0.000022054159],"about_ca_topic_score_codex":0.04614597,"about_ca_topic_score_gemma":0.029123873,"teacher_disagreement_score":0.04614597,"about_ca_system_score_codex":0.0006278235,"about_ca_system_score_gemma":0.0006059339,"threshold_uncertainty_score":0.091754735},"labels":[],"label_agreement":null},{"id":"W4380881222","doi":"10.1029/2023gl103713","title":"Ice Concentration Scaling Laws for Freshwater Lakes in Numerical Weather and Climate Prediction","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Rheology; Viscoelasticity; Scaling; Geology; Mechanics; Climatology; Geophysics; Meteorology; Environmental science; Atmospheric sciences; Physics; Mathematics; Thermodynamics; Geometry","score_opus":0.026535882135175402,"score_gpt":0.28201025711196476,"score_spread":0.2554743749767894,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380881222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.87914866,0.0004894395,0.11161845,0.00067890866,0.000047184738,0.00011345541,0.00035428876,0.0004749102,0.007074694],"genre_scores_gemma":[0.99339914,0.00009903823,0.005911092,0.00002928958,0.000011768491,0.00005130471,0.000076111784,0.000037897822,0.00038442167],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983907,0.000060600047,0.000017036962,0.00002796638,0.000034507073,0.000020706368],"domain_scores_gemma":[0.9979001,0.0013436301,0.00029057235,0.00013085348,0.00024854066,0.000086218104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013051535,0.00028497755,0.00027877468,0.000672998,0.00044465644,0.000713511,0.00047766647,0.00045861225,0.0011892602],"category_scores_gemma":[0.006141549,0.00025306104,0.00034216765,0.0003689658,0.00060324866,0.00089003675,0.00044916812,0.00042537844,0.00009402433],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000015308418,0.000031850606,0.0062501514,0.000018393608,0.000012849382,0.000055094668,0.000046693713,0.9806451,0.0009774208,0.0074054953,0.00036063715,0.0041810134],"study_design_scores_gemma":[0.0000035945063,0.0000054168795,0.00077850686,0.0000036263898,0.0000011753935,0.0000037295126,0.0000058498595,0.9978702,0.00013825702,0.0011113831,0.00007486848,0.0000033709796],"about_ca_topic_score_codex":0.010926218,"about_ca_topic_score_gemma":0.0070013683,"teacher_disagreement_score":0.010926218,"about_ca_system_score_codex":0.00079120044,"about_ca_system_score_gemma":0.00046697137,"threshold_uncertainty_score":0.021725237},"labels":[],"label_agreement":null},{"id":"W4380995754","doi":"10.1029/2023gl103969","title":"Stepwise Widening of the Central Andes—The Role of the Lower Crust","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Alliance de recherche numérique du Canada; Dalhousie University; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Geology; Crust; Lithosphere; Foreland basin; Plateau (mathematics); Front (military); Cenozoic; Deformation (meteorology); Seismology; Tectonics; Geophysics; Geomorphology","score_opus":0.02267315968980712,"score_gpt":0.24758830343050542,"score_spread":0.2249151437406983,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380995754","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9969009,0.00008546067,0.00045801883,0.00009105096,0.0000014517924,0.0000030035742,0.000031985248,0.000017460288,0.002410815],"genre_scores_gemma":[0.9997638,0.000030549367,0.000074159856,0.0000039897895,6.767236e-7,6.6701006e-7,0.000011319307,0.0000013504513,0.00011341832],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.000008188234,0.000002640122,0.000016540513,0.0000058980845,0.000013284315],"domain_scores_gemma":[0.9999106,0.000013281743,0.000024910443,0.000013018096,0.000015912032,0.000022341657],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014982054,0.00021092831,0.00025725624,0.00036988166,0.00043320842,0.0011265642,0.00032449063,0.00021708547,0.0013413356],"category_scores_gemma":[0.0003645859,0.00016850968,0.00024286323,0.00028592136,0.00060762523,0.00043906856,0.00075111986,0.00023997066,0.00011820504],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005262677,0.0001303122,0.52677065,0.00023443918,0.00027606776,0.001206362,0.0011361268,0.25059435,0.14771049,0.021236965,0.00064414635,0.049533818],"study_design_scores_gemma":[0.000094568335,0.00019452984,0.6584593,0.00005339672,0.00012431756,0.00030687923,0.0009115666,0.32168454,0.009418294,0.005870605,0.0028388458,0.000043186305],"about_ca_topic_score_codex":0.023613263,"about_ca_topic_score_gemma":0.013272945,"teacher_disagreement_score":0.023613263,"about_ca_system_score_codex":0.00076091965,"about_ca_system_score_gemma":0.00052831543,"threshold_uncertainty_score":0.04695165},"labels":[],"label_agreement":null},{"id":"W4380996482","doi":"10.1029/2023gl103904","title":"Snow Suppresses Seismic Signals From Steamboat Geyser","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismic Waves and Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"University of Utah; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Seismometer; Snow; Geology; Seismology; Broadband; National park; Volcano; Attenuation; Amplitude; Remote sensing; Geomorphology; Geography","score_opus":0.04967742008442607,"score_gpt":0.3004780735886753,"score_spread":0.25080065350424924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4380996482","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998926,0.000024155544,0.00024380676,0.00001971804,0.0000031200998,0.0000017233784,0.00022765288,0.000025355506,0.0005285267],"genre_scores_gemma":[0.9990988,0.0000209436,0.00019632718,0.000011925875,0.000003894224,0.0000017561484,0.0003458756,0.00000910465,0.0003114821],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999058,0.00001231477,0.0000037033558,0.000024805662,0.000026212721,0.00002707404],"domain_scores_gemma":[0.99975175,0.000049593393,0.00006873052,0.00002253524,0.00007308196,0.00003426828],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017605805,0.00017303704,0.00022730372,0.00044533578,0.0002485043,0.00034924544,0.0001704874,0.00019530265,0.00092583644],"category_scores_gemma":[0.0006841371,0.00013149077,0.00008877259,0.00044367628,0.00020187732,0.00025852106,0.00039216795,0.00014142093,0.00017259756],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005576924,0.000046821024,0.8366476,0.00006234167,0.00010636541,0.0004861875,0.0012386151,0.0023931533,0.13220772,0.00010279541,0.0016551465,0.02449555],"study_design_scores_gemma":[0.0000036225524,0.000017388898,0.9961196,0.0000034988545,0.000007356543,0.00003519921,0.0001409539,0.0015574627,0.0015938656,0.00002105173,0.0004976597,0.0000023481552],"about_ca_topic_score_codex":0.027962089,"about_ca_topic_score_gemma":0.079053946,"teacher_disagreement_score":0.027962089,"about_ca_system_score_codex":0.00028123605,"about_ca_system_score_gemma":0.00023801485,"threshold_uncertainty_score":0.055598676},"labels":[],"label_agreement":null},{"id":"W4381801886","doi":"10.1029/2022gl102145","title":"Subseasonal Predictions of Polar Low Activity Using a Hybrid Statistical‐Dynamical Approach","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Naval Research","keywords":"Predictability; Climatology; Environmental science; The arctic; Arctic; Polar; Forecast skill; Meteorology; Statistics; Mathematics; Geology; Oceanography; Geography; Physics","score_opus":0.03892419970372319,"score_gpt":0.2945261126023791,"score_spread":0.2556019128986559,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4381801886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9399433,0.00016829262,0.054695178,0.0003030969,0.00003950941,0.000021924483,0.00053543097,0.00027321043,0.0040200544],"genre_scores_gemma":[0.99662906,0.00002477774,0.00286498,0.00001520506,0.000018176132,0.000008705805,0.00016634077,0.000010465465,0.0002622411],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986815,0.000044901215,0.000008004968,0.000036566726,0.000022120792,0.000020236901],"domain_scores_gemma":[0.9994746,0.00025525005,0.00007700907,0.000034751214,0.00009303367,0.00006542335],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049116346,0.00041152077,0.0003053108,0.0008032229,0.00029508624,0.00093606877,0.0005024339,0.0003039939,0.00085863133],"category_scores_gemma":[0.0010748145,0.00026827378,0.0005412968,0.00040081068,0.0003071697,0.0005367975,0.0005615245,0.00034613066,0.00012180096],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0000534838,0.000035408393,0.015730247,0.000007877118,0.00006264373,0.000024049195,0.000012233758,0.97636414,0.0010291688,0.0006499044,0.00012976667,0.0059011355],"study_design_scores_gemma":[0.0000033516756,0.000008076233,0.0017805784,8.9159005e-7,0.0000035358642,0.0000016759392,0.000004870626,0.9979102,0.00007629346,0.00016790924,0.000039082184,0.0000034994691],"about_ca_topic_score_codex":0.039320666,"about_ca_topic_score_gemma":0.028084725,"teacher_disagreement_score":0.039320666,"about_ca_system_score_codex":0.0006240966,"about_ca_system_score_gemma":0.0007071509,"threshold_uncertainty_score":0.07818359},"labels":[],"label_agreement":null},{"id":"W4382046040","doi":"10.1029/2023gl103024","title":"Small, Coastal Temperate Rainforest Watersheds Dominate Dissolved Organic Carbon Transport to the Northeast Pacific Ocean","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Forests; University of Saskatchewan; University of Alberta; Vancouver Island University; Government of British Columbia; Tula Foundation; Simon Fraser University","funders":"Office of Experimental Program to Stimulate Competitive Research; Hakai Institute; Tula Foundation; University of Washington; National Science Foundation","keywords":"Environmental science; Rainforest; Dissolved organic carbon; Temperate climate; Oceanography; Drainage basin; Temperate rainforest; Precipitation; Total organic carbon; Ecosystem; Hydrology (agriculture); Geology; Ecology; Geography","score_opus":0.024906069641981176,"score_gpt":0.2337107940917731,"score_spread":0.20880472444979192,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382046040","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99874544,0.000052917203,0.00006249082,0.00001558858,6.961555e-7,0.0000026968821,0.0001316237,0.000008637036,0.000979836],"genre_scores_gemma":[0.9994419,0.000077149154,0.00009563371,0.000008712378,0.0000016449228,0.0000016184509,0.0001735957,0.0000025099232,0.00019717004],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.000003906363,0.0000041033,0.000025265104,0.000012671254,0.000015115329],"domain_scores_gemma":[0.99985766,0.000017608469,0.000046846555,0.000009325978,0.000033485856,0.000035081695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009208016,0.00015164689,0.00015915727,0.00029061546,0.0003672482,0.0006773553,0.00014458128,0.00007337117,0.001365316],"category_scores_gemma":[0.00031316528,0.00010295396,0.000087731925,0.00053722644,0.00022761211,0.00037198214,0.00039916992,0.00011623458,0.00012332352],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000035662888,0.000018754565,0.9785543,0.000027746752,0.000024020876,0.0002283179,0.00037661087,0.00029628986,0.012342292,0.00016171602,0.0002190577,0.007715234],"study_design_scores_gemma":[0.000003220827,0.0000081962935,0.99791723,0.0000065246413,0.000010138538,0.000072161136,0.00051004114,0.00048562224,0.000413954,0.00006018293,0.00051087816,0.0000018689598],"about_ca_topic_score_codex":0.060079478,"about_ca_topic_score_gemma":0.1024368,"teacher_disagreement_score":0.060079478,"about_ca_system_score_codex":0.00042446176,"about_ca_system_score_gemma":0.0004947735,"threshold_uncertainty_score":0.11945957},"labels":[],"label_agreement":null},{"id":"W4382314820","doi":"10.1029/2023gl104214","title":"Thank You to Our 2022 Peer Reviewers","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Scientific Computing and Data Management","field":"Decision Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Presentation (obstetrics); Rigour; Reading (process); Peer review; Library science; Quality (philosophy); Computer science; Engineering ethics; Political science; Data science; Public relations; Medicine; Engineering; Law","score_opus":0.3282845110858884,"score_gpt":0.5069510288248523,"score_spread":0.17866651773896391,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382314820","genre_codex":"editorial","genre_gemma":"other","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"other","genre_consensus":null,"domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0012439261,0.011811997,0.010632241,0.2982225,0.64011234,0.0019466731,0.0036148308,0.0053804866,0.027035072],"genre_scores_gemma":[0.017327173,0.015550326,0.03368836,0.20241101,0.36286616,0.0056981873,0.006897918,0.008196033,0.34736484],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.940071,0.01608429,0.007796278,0.0064204484,0.027177542,0.002450535],"domain_scores_gemma":[0.40941662,0.020627212,0.01493477,0.014079182,0.51111025,0.029832033],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.039962683,0.002635626,0.0036941166,0.007834655,0.0063335835,0.026293805,0.0039087497,0.00891909,0.14083095],"category_scores_gemma":[0.2742692,0.0016663579,0.0023009912,0.004164466,0.002494476,0.00819534,0.0062470497,0.008701367,0.22711417],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000021609698,0.000008183973,0.00018715471,0.0001316494,0.000009209213,0.000077163124,0.000075810625,0.00001926214,0.00009288301,0.00017187784,0.9810178,0.018187441],"study_design_scores_gemma":[0.000023290733,0.00001701184,0.0003352198,0.00027945935,0.000014492763,0.00026180746,0.00034715573,0.00012528569,0.00012550798,0.00064322405,0.99778026,0.00004727161],"about_ca_topic_score_codex":0.002878912,"about_ca_topic_score_gemma":0.0050527034,"teacher_disagreement_score":0.9600373,"about_ca_system_score_codex":0.0034803967,"about_ca_system_score_gemma":0.018271824,"threshold_uncertainty_score":0.47112644},"labels":[],"label_agreement":null},{"id":"W4382361514","doi":"10.1029/2022gl101974","title":"On the Remote Impacts of Mid‐Holocene Saharan Vegetation on South American Hydroclimate: A Modeling Intercomparison","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; St. Francis Xavier University; Université du Québec à Montréal","funders":"Natural Sciences and Engineering Research Council of Canada; Goddard Institute for Space Studies; Conselho Nacional de Desenvolvimento Científico e Tecnológico; National Aeronautics and Space Administration; Canada Research Chairs; Fundação de Amparo à Pesquisa do Estado de São Paulo; National Center for Atmospheric Research; National Science Foundation","keywords":"Holocene; Vegetation (pathology); Climatology; Climate model; Proxy (statistics); Precipitation; Monsoon; Climate change; Paleoclimatology; Physical geography; Environmental science; Greenhouse gas; General Circulation Model; Geology; Geography; Oceanography; Meteorology","score_opus":0.0732173469259211,"score_gpt":0.33491899165659794,"score_spread":0.2617016447306768,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382361514","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99804604,0.000047947677,0.0003866236,0.00013648644,0.0000059437193,0.000006946831,0.00028123255,0.000027678096,0.0010611808],"genre_scores_gemma":[0.9987073,0.00006384853,0.000680395,0.000039623133,0.0000056300123,0.00001672541,0.00026469378,0.00001445356,0.0002074287],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99984086,0.00008189471,0.000005865975,0.00003614951,0.00001129918,0.000023867906],"domain_scores_gemma":[0.9996394,0.00019422674,0.000034590255,0.000048835514,0.00004317836,0.000039877814],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00074582105,0.00055816147,0.00041213105,0.00024202067,0.00056994456,0.00082654075,0.0009037554,0.00073910586,0.0014483264],"category_scores_gemma":[0.00077641394,0.00032033125,0.00075231976,0.0005345861,0.0003096797,0.0006139787,0.00060039904,0.00043170457,0.00012599718],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006707294,0.00040587466,0.16443613,0.00009978472,0.0008231659,0.0003252222,0.0006882069,0.80724645,0.008505304,0.0022399516,0.0018022943,0.012756921],"study_design_scores_gemma":[0.00039416217,0.00019293568,0.118672565,0.000025012523,0.0004089211,0.000038586397,0.00059490465,0.87295645,0.0032257999,0.0011561693,0.0022743733,0.000060100316],"about_ca_topic_score_codex":0.08382807,"about_ca_topic_score_gemma":0.065639876,"teacher_disagreement_score":0.08382807,"about_ca_system_score_codex":0.00094597676,"about_ca_system_score_gemma":0.000979514,"threshold_uncertainty_score":0.16668028},"labels":[],"label_agreement":null},{"id":"W4382500856","doi":"10.1029/2023gl102894","title":"Anthropogenic Bromoform at the Extratropical Tropopause","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Saskatchewan","funders":"Natural Sciences and Engineering Research Council of Canada; European Centre for Medium-Range Weather Forecasts","keywords":"Bromoform; Atmospheric sciences; Environmental science; Stratosphere; Boreal; Northern Hemisphere; Extratropical cyclone; Tropopause; Bromine; Ozone depletion; Climatology; Annual cycle; Southern Hemisphere; Chemistry; Ecology; Geology","score_opus":0.04493995067023474,"score_gpt":0.3128564452791468,"score_spread":0.26791649460891204,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4382500856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9908785,0.00049882405,0.0005981668,0.00007761304,0.000015690715,0.000008625759,0.0040450934,0.00006824009,0.003809224],"genre_scores_gemma":[0.99665135,0.00031453586,0.0002877776,0.000040140243,0.000009156026,0.0000062614104,0.0021582767,0.000014120294,0.00051837007],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999441,0.0000048516326,0.0000018049939,0.000017619852,0.000014972213,0.000016603259],"domain_scores_gemma":[0.9999279,0.000007988644,0.000017792121,0.000008747893,0.000025339194,0.000012256739],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011229629,0.00034336874,0.00013247026,0.00036783723,0.00021416854,0.00035535154,0.00014527501,0.000104535706,0.0013206544],"category_scores_gemma":[0.000096057156,0.00008290116,0.00026684094,0.00033898995,0.00013730356,0.00022186992,0.0003274029,0.00014649218,0.00016100942],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046811742,0.000039324197,0.70554227,0.0002453245,0.00038097982,0.0004899827,0.0004308882,0.004461216,0.2618899,0.00029637173,0.0017291653,0.02402654],"study_design_scores_gemma":[0.0000042515308,0.000013286065,0.99239904,0.000005491028,0.000021008893,0.000037372014,0.0000840981,0.0006035885,0.0046109855,0.00003058884,0.0021856169,0.0000046201626],"about_ca_topic_score_codex":0.046834048,"about_ca_topic_score_gemma":0.05846519,"teacher_disagreement_score":0.046834048,"about_ca_system_score_codex":0.0005316548,"about_ca_system_score_gemma":0.00031482193,"threshold_uncertainty_score":0.0931229},"labels":[],"label_agreement":null},{"id":"W4383498761","doi":"10.1029/2023gl104362","title":"Pine Maximum Latewood Density in Semi‐Arid Northern China Records Hydroclimate Rather Than Temperature","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Institut National de la Recherche Scientifique","funders":"Vetenskapsrådet; China Meteorological Administration; National Natural Science Foundation of China; Riksbankens Jubileumsfond; Swedish Collegium for Advanced Study","keywords":"Dendrochronology; Climatology; Arid; Precipitation; Paleoclimatology; Environmental science; Proxy (statistics); Chronology; Aridity index; Climate change; Atmospheric sciences; Geology; Physical geography; Meteorology; Geography; Oceanography","score_opus":0.023813424952385812,"score_gpt":0.2780722596456134,"score_spread":0.2542588346932276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383498761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875295,0.00004130544,0.00016616909,0.000010866454,0.0000013733269,0.0000019183485,0.0007322986,0.000009339316,0.00028376622],"genre_scores_gemma":[0.9987716,0.000023524351,0.00011566476,0.0000056048843,0.000002290324,0.000003910154,0.0010044761,0.0000016239017,0.000071363116],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999187,0.000012146849,0.000005989363,0.000031642936,0.000013398488,0.00001818734],"domain_scores_gemma":[0.999726,0.000032626347,0.00008001094,0.000043055526,0.00006358147,0.000054690146],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003281926,0.00018762596,0.00017110317,0.00064276485,0.00024380935,0.00027130722,0.00020531089,0.00007926326,0.00046923273],"category_scores_gemma":[0.0003608065,0.00011969646,0.00014780716,0.0008271048,0.00018026022,0.00022311218,0.0002557471,0.00008498721,0.00008792825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000042626696,0.000016077782,0.9851318,0.000028200495,0.00004687287,0.00006395676,0.00021894569,0.0010294119,0.006775032,0.00006199989,0.00025023872,0.006334869],"study_design_scores_gemma":[0.0000012181554,0.000003957803,0.99843234,0.0000017079685,0.0000054877064,0.000016725719,0.000057517285,0.0009861697,0.0002753394,0.000012393373,0.00020483528,0.0000023052683],"about_ca_topic_score_codex":0.03629638,"about_ca_topic_score_gemma":0.07406565,"teacher_disagreement_score":0.03629638,"about_ca_system_score_codex":0.00038335225,"about_ca_system_score_gemma":0.0003302752,"threshold_uncertainty_score":0.0721702},"labels":[],"label_agreement":null},{"id":"W4383750284","doi":"10.1029/2023gl103723","title":"Diagnosing the Radiation Biases in Global Climate Models Using Radiative Kernels","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada","keywords":"Environmental science; Earth's energy budget; Climate model; Radiative transfer; Climatology; Troposphere; Atmosphere (unit); Radiation; Cloud cover; GCM transcription factors; Atmospheric sciences; Meteorology; General Circulation Model; Climate change; Cloud computing; Physics; Geology; Computer science","score_opus":0.1325424985244455,"score_gpt":0.3797278085544287,"score_spread":0.24718531002998323,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383750284","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870669,0.00007194149,0.011710887,0.00006194532,0.000015168402,0.000018207498,0.00014439577,0.00023050758,0.0006799575],"genre_scores_gemma":[0.99633265,0.000018790897,0.0034844885,0.00000925573,0.0000043491705,0.00000717887,0.00007653745,0.000019184408,0.000047500253],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994824,0.00021918816,0.000055330307,0.000086055144,0.00009172384,0.00006525512],"domain_scores_gemma":[0.99755824,0.0013351253,0.00037764816,0.0003495127,0.0002888736,0.00009051688],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002270891,0.000737222,0.00052821124,0.00072899944,0.00031352916,0.001073762,0.0006803086,0.00080830924,0.00030268816],"category_scores_gemma":[0.0072602513,0.00041275934,0.0007912819,0.00059197773,0.0005479648,0.0011368738,0.00091169635,0.00059668755,0.00006135536],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007295487,0.00006164938,0.04909055,0.000017692937,0.000120591794,0.000029949128,0.00004664229,0.94165516,0.0037268705,0.0008281614,0.000095176045,0.0042545884],"study_design_scores_gemma":[0.00001777081,0.000016255084,0.008091635,0.00000443606,0.000020881538,0.000007157386,0.000011174174,0.98955756,0.0017291409,0.00043899284,0.00009219467,0.000012766297],"about_ca_topic_score_codex":0.021283468,"about_ca_topic_score_gemma":0.009049956,"teacher_disagreement_score":0.021283468,"about_ca_system_score_codex":0.0010144752,"about_ca_system_score_gemma":0.0007467655,"threshold_uncertainty_score":0.04231918},"labels":[],"label_agreement":null},{"id":"W4383750304","doi":"10.1029/2023gl103415","title":"Nature and Origin of Magnetic Lineations Within Valdivia Bank: Ocean Plateau Formation by Complex Seafloor Spreading","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"National Natural Science Foundation of China; Natural Environment Research Council; Sight Research UK; U.S. Science Support Program, Lamont-Doherty Earth Observatory; National Science Foundation","keywords":"Geology; Seafloor spreading; Magnetic anomaly; Lineation; Paleomagnetism; Ridge; Paleontology; Hotspot (geology); Volcano; Lava; Volcanism; Plateau (mathematics); Sill; Geophysics; Rift; Mid-ocean ridge; Cretaceous; Tectonics; Petrology","score_opus":0.026376571479551948,"score_gpt":0.30935720065951583,"score_spread":0.28298062917996386,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4383750304","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992217,0.00006469042,0.000034970297,0.000009588176,7.135633e-7,0.0000016203705,0.00009250556,0.0000028995855,0.000571254],"genre_scores_gemma":[0.9996408,0.00002773639,0.000052234132,0.0000035581893,6.7716644e-7,0.0000014189462,0.00016836864,0.0000011621374,0.00010402313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999403,0.000007846789,0.000004621044,0.000024978603,0.00000676251,0.000015476116],"domain_scores_gemma":[0.999882,0.00001598022,0.000042860705,0.000008698062,0.000027285654,0.000023162203],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009926768,0.0001328856,0.00014966991,0.000845086,0.00023155414,0.0005911269,0.00019636398,0.00017299777,0.00078597065],"category_scores_gemma":[0.00032504048,0.00009300242,0.00009692501,0.00060837244,0.00039765073,0.00013393293,0.00044724214,0.00011767511,0.00012447544],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011743707,0.000010027136,0.94819903,0.000025657526,0.00003141249,0.000297732,0.000534711,0.000433468,0.043371025,0.00022861455,0.00007829093,0.0066724652],"study_design_scores_gemma":[0.0000031901554,0.000016310287,0.99832815,0.000005399921,0.000003923782,0.00008071547,0.00030657463,0.00022763145,0.0006176999,0.000047133977,0.0003612561,0.0000019628296],"about_ca_topic_score_codex":0.018781139,"about_ca_topic_score_gemma":0.017843883,"teacher_disagreement_score":0.018781139,"about_ca_system_score_codex":0.0006395025,"about_ca_system_score_gemma":0.00024482384,"threshold_uncertainty_score":0.03734362},"labels":[],"label_agreement":null},{"id":"W4384154750","doi":"10.1029/2022gl100366","title":"Inter‐Annual Variability in Atmospheric Transport Complicates Estimation of US Methane Emissions Trends","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Johns Hopkins University; National Science Foundation","keywords":"Methane; Environmental science; Methane emissions; Atmospheric methane; Atmospheric sciences; Satellite; Greenhouse gas; Climatology; Geology; Chemistry; Oceanography","score_opus":0.019178033034949665,"score_gpt":0.3010460441787074,"score_spread":0.2818680111437577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384154750","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9759498,0.0009459332,0.016066087,0.00066741934,0.00007280528,0.000018720531,0.002127457,0.00020245378,0.003949407],"genre_scores_gemma":[0.99785763,0.00017184272,0.0010857552,0.000048535458,0.000023069877,0.0000066593175,0.00066687673,0.000019248857,0.00012043508],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9994796,0.0001816245,0.00006672753,0.000126248,0.000085895015,0.00005988718],"domain_scores_gemma":[0.9982673,0.0007058655,0.00050436356,0.00026154387,0.00022519093,0.000035730587],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0017840024,0.00027564497,0.00020802942,0.00070859253,0.0003071085,0.000963573,0.00031136387,0.00027603286,0.000420934],"category_scores_gemma":[0.004300029,0.0002691392,0.0005976588,0.0012897453,0.00021914724,0.001242793,0.0005167735,0.0003491444,0.00014924821],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000043092066,0.00002357848,0.9502066,0.00004506063,0.00024713323,0.000052313088,0.00010550294,0.027347669,0.0017060781,0.00092884793,0.0008480113,0.018446214],"study_design_scores_gemma":[0.000004159983,0.000023244447,0.8693794,0.000049003003,0.00007477647,0.00007407875,0.00038029457,0.122098275,0.0014037199,0.0018213902,0.00467384,0.000017858443],"about_ca_topic_score_codex":0.044951096,"about_ca_topic_score_gemma":0.05511811,"teacher_disagreement_score":0.044951096,"about_ca_system_score_codex":0.00058616285,"about_ca_system_score_gemma":0.00062603905,"threshold_uncertainty_score":0.08937889},"labels":[],"label_agreement":null},{"id":"W4384299379","doi":"10.1029/2023gl104800","title":"Substorm Impact on Dayside Ionospheric Currents","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Goddard Space Flight Center; Università degli Studi dell'Aquila; Sveriges Geologiska Undersökning; Helmholtz-Zentrum Potsdam - Deutsches GeoForschungsZentrum GFZ; Universitetet i Tromsø; Trond Mohn stiftelse; Florida Institute of Technology; Alberta Agricultural Research Institute; Norges Forskningsråd; National Aeronautics and Space Administration","keywords":"Substorm; Ionosphere; Geophysics; Interplanetary magnetic field; Magnetopause; Physics; Magnetosphere; Solar wind; Current (fluid); Magnetic field","score_opus":0.028285215710030176,"score_gpt":0.3403849262629741,"score_spread":0.31209971055294394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384299379","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988005,0.000057589383,0.00017618318,0.000009582124,0.0000018847855,0.0000018602068,0.000120376666,0.000010679382,0.000821284],"genre_scores_gemma":[0.9997265,0.00002320713,0.00004012059,0.000002810934,0.000002647671,9.178466e-7,0.000113231115,0.0000034650898,0.000087148874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995184,0.000007798716,0.0000042394454,0.000009731259,0.000009617372,0.000016632961],"domain_scores_gemma":[0.9994885,0.00013147149,0.00016629827,0.00004288255,0.000093924755,0.00007687439],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001324498,0.00008820328,0.00018933971,0.00037696766,0.00014762941,0.00035599765,0.000080078455,0.000114600356,0.0015468885],"category_scores_gemma":[0.0005838959,0.000053605716,0.00012567548,0.00027058052,0.0001750455,0.00019901816,0.00028193998,0.00012613578,0.00015309075],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005417827,0.000031228057,0.81991285,0.000044979293,0.00006830072,0.0003231056,0.000440395,0.0014227966,0.16170628,0.0004156772,0.00030412505,0.014788431],"study_design_scores_gemma":[0.000002162774,0.000028618799,0.99622405,0.0000025258569,0.000009563332,0.00004898264,0.00006765318,0.00074606034,0.0025801419,0.000052137424,0.00023601056,0.0000020215894],"about_ca_topic_score_codex":0.0023268457,"about_ca_topic_score_gemma":0.002610767,"teacher_disagreement_score":0.0023268457,"about_ca_system_score_codex":0.00015508186,"about_ca_system_score_gemma":0.00009037764,"threshold_uncertainty_score":0.0051748753},"labels":[],"label_agreement":null},{"id":"W4384341521","doi":"10.1029/2023gl103970","title":"Post‐Sunset Field‐Line Resonances at Equatorial Latitudes Observed by Swarm","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Canadian Space Agency; European Space Agency","keywords":"Ionosphere; Sunset; Poynting vector; Field line; Physics; Geophysics; Conjugate points; Magnetic field; Harmonics; Latitude; Field (mathematics); Geology; Altitude (triangle); Magnetometer; Geodesy; Computational physics; Mathematics; Geometry; Optics","score_opus":0.034529152884392254,"score_gpt":0.31023100382844115,"score_spread":0.2757018509440489,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384341521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992428,0.00001914541,0.00013325224,0.0000040071795,0.0000016779563,0.000001110738,0.00007543434,0.0000068692684,0.00051577156],"genre_scores_gemma":[0.9996264,0.0000115534285,0.00008209991,0.000002244918,0.0000028602035,0.0000013917867,0.00015110843,0.0000020210439,0.000120309836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999708,0.0000042754264,0.0000016117549,0.000006863491,0.000007844904,0.000008526175],"domain_scores_gemma":[0.9998266,0.00003356167,0.00005861387,0.000017242555,0.000029629486,0.00003434394],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000084124214,0.00011950486,0.00010808088,0.00042662595,0.00018904136,0.0002000127,0.00008575792,0.00013657664,0.00090847805],"category_scores_gemma":[0.000254575,0.00007726633,0.00007171493,0.00023745545,0.00013743508,0.0001413465,0.00022010064,0.00011168398,0.00015327509],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005523782,0.000043323693,0.87552845,0.000040404695,0.000050745384,0.00046412877,0.0013508373,0.00050022325,0.10731971,0.000117534095,0.0003771167,0.0136550395],"study_design_scores_gemma":[0.0000041382427,0.00006367146,0.99748707,0.0000023746802,0.0000060943257,0.00008646833,0.00014890147,0.00032754187,0.0015036358,0.000012856415,0.00035539924,0.0000018411531],"about_ca_topic_score_codex":0.0015855756,"about_ca_topic_score_gemma":0.0032414757,"teacher_disagreement_score":0.0015855756,"about_ca_system_score_codex":0.00008872182,"about_ca_system_score_gemma":0.00004333656,"threshold_uncertainty_score":0.003152728},"labels":[],"label_agreement":null},{"id":"W4384698297","doi":"10.1029/2023gl103037","title":"Cold‐Season Methane Fluxes Simulated by GCP‐CH<sub>4</sub> Models","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal; Université du Québec à Montréal; Environment and Climate Change Canada","funders":"Bundesministerium für Bildung und Forschung; University of Birmingham; Environmental Restoration and Conservation Agency; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; Ministry of Education, Culture, Sports, Science and Technology; Ministry of the Environment, Government of Japan; National Science Foundation","keywords":"Environmental science; Methane; Atmospheric sciences; Snow; Greenhouse gas; Climatology; Climate model; Flux (metallurgy); Winter season; Wetland; Climate change; Meteorology; Geology; Chemistry; Ecology; Geography","score_opus":0.022297710547614966,"score_gpt":0.27122504664006747,"score_spread":0.2489273360924525,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384698297","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99658835,0.000027225828,0.0010010228,0.000067466746,0.000010943474,0.000008001441,0.0009186715,0.00017242043,0.001205873],"genre_scores_gemma":[0.9980338,0.00001993786,0.00075955037,0.000018946856,0.0000046977416,0.0000131716,0.0009038501,0.00003104877,0.00021501248],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998547,0.00004422949,0.000007333801,0.000041602536,0.000013616479,0.00003843392],"domain_scores_gemma":[0.9996008,0.00015793393,0.000047605103,0.00006784645,0.00006036783,0.0000654124],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043594485,0.0007570137,0.0004526931,0.000301597,0.00043025223,0.0006633644,0.0008798426,0.0007784609,0.0011683266],"category_scores_gemma":[0.00083410053,0.00043021757,0.00067755085,0.00045722767,0.00042939693,0.00068080577,0.00034256815,0.0006341049,0.00019191012],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003447904,0.00009019279,0.043774433,0.000022416893,0.00013562934,0.00006012044,0.000042882308,0.94845784,0.0040046466,0.00038303982,0.0006742134,0.002009839],"study_design_scores_gemma":[0.00009341097,0.000055111424,0.016010214,0.000004529485,0.000038625294,0.000010368825,0.000038360107,0.98065156,0.0024268127,0.00026803624,0.00038519813,0.000017756107],"about_ca_topic_score_codex":0.07656671,"about_ca_topic_score_gemma":0.04656354,"teacher_disagreement_score":0.07656671,"about_ca_system_score_codex":0.0010679206,"about_ca_system_score_gemma":0.0008046911,"threshold_uncertainty_score":0.15224206},"labels":[],"label_agreement":null},{"id":"W4384821886","doi":"10.1029/2022gl102633","title":"New Insights Into the Relationship Between Mass Eruption Rate and Volcanic Column Height Based On the IVESPA Data Set","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Environment Research Council; British Geological Survey; U.S. Geological Survey; Horizon 2020 Framework Programme; Agence Nationale de la Recherche; Sight Research UK","keywords":"Volcano; Explosive eruption; Geology; Empirical modelling; Wind speed; Range (aeronautics); Atmospheric sciences; Meteorology; Explosive material; Environmental science; Seismology; Computer science; Magma; Geography","score_opus":0.13281104844250632,"score_gpt":0.31382332488571174,"score_spread":0.18101227644320542,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384821886","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98719364,0.00013388826,0.003031273,0.00018059555,0.00000703168,0.000008056865,0.0074534584,0.00014012687,0.0018520181],"genre_scores_gemma":[0.9892225,0.000053206248,0.0016871983,0.000022185905,0.000009191378,0.0000040844025,0.008878561,0.000022923801,0.00010015943],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99962986,0.000094719515,0.000034772427,0.000115124276,0.0000831496,0.000042362193],"domain_scores_gemma":[0.99573934,0.002688288,0.00035833177,0.0007257191,0.00036278274,0.0001255943],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013991193,0.0002544806,0.00031465598,0.0013225701,0.00014865368,0.000987951,0.00041650265,0.00033377798,0.0007484829],"category_scores_gemma":[0.005636187,0.00019097317,0.0003618478,0.0011198124,0.00028887263,0.00095204613,0.0006502154,0.0007874187,0.00020976525],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012198709,0.000095280375,0.9206156,0.00006800127,0.00021833954,0.00016032286,0.00024326242,0.039160017,0.009944761,0.001350451,0.0023089342,0.025712969],"study_design_scores_gemma":[0.000009694189,0.000033797864,0.8843763,0.00002499989,0.000030465037,0.00011175692,0.00022517612,0.110598356,0.0014842603,0.00096005294,0.0021241235,0.000021016072],"about_ca_topic_score_codex":0.010942121,"about_ca_topic_score_gemma":0.016228871,"teacher_disagreement_score":0.010942121,"about_ca_system_score_codex":0.00025758217,"about_ca_system_score_gemma":0.0002552346,"threshold_uncertainty_score":0.021756887},"labels":[],"label_agreement":null},{"id":"W4384824000","doi":"10.1029/2022gl102466","title":"How Credibly Do CMIP6 Simulations Capture Historical Mean and Extreme Precipitation Changes?","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":44,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"HORIZON EUROPE Marie Sklodowska-Curie Actions; HORIZON EUROPE Framework Programme; Horizon 2020 Framework Programme; Generalitat de Catalunya; Agencia Estatal de Investigación; AXA Research Fund","keywords":"Precipitation; Coupled model intercomparison project; Climatology; Environmental science; Credibility; Climate model; Climate change; Meteorology; Geology; Geography; Oceanography","score_opus":0.10679650115932544,"score_gpt":0.3151744210250553,"score_spread":0.20837791986572984,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384824000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9574373,0.00073125254,0.025631847,0.0029004295,0.00025167316,0.000060177612,0.0034994932,0.00080431066,0.008683486],"genre_scores_gemma":[0.99538887,0.00010811634,0.0027202528,0.00026504946,0.000045345132,0.0000120181985,0.0011677712,0.00007539442,0.00021713602],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9988084,0.00047122416,0.000118654956,0.00033332745,0.0001339184,0.00013445933],"domain_scores_gemma":[0.9874303,0.00626175,0.0018434582,0.0024267207,0.0014309393,0.0006069681],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0052086245,0.00068884663,0.0005053809,0.00065726484,0.0003784755,0.0021249126,0.0011773563,0.0014531943,0.0020654732],"category_scores_gemma":[0.036933955,0.00047662423,0.0005135111,0.00086340914,0.0006187305,0.0037303574,0.00083812315,0.0011175328,0.00072130054],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033409608,0.00014196754,0.36961952,0.00015562327,0.00069416646,0.00016232417,0.00021869368,0.5937468,0.0027429103,0.002816966,0.0044234106,0.024943558],"study_design_scores_gemma":[0.00010750886,0.00007597363,0.10723135,0.0001489868,0.00009651987,0.00010406332,0.00021496043,0.8777733,0.0037036655,0.006559847,0.0039042358,0.00007969199],"about_ca_topic_score_codex":0.020426624,"about_ca_topic_score_gemma":0.013921193,"teacher_disagreement_score":0.020426624,"about_ca_system_score_codex":0.00066516455,"about_ca_system_score_gemma":0.0009218354,"threshold_uncertainty_score":0.0406155},"labels":[],"label_agreement":null},{"id":"W4384930450","doi":"10.1029/2023gl103402","title":"Restratification in Late Winter Lakes Induced by Cabbeling","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; Wilfrid Laurier University","funders":"Alliance de recherche numérique du Canada; Ontario Ministry of Research, Innovation and Science","keywords":"Stratification (seeds); Instability; Richardson number; Geology; Limiting; Turbulence; Mixing (physics); Stratified flow; Vertical mixing; Mechanics; Atmospheric sciences; Climatology; Physics","score_opus":0.06479651044345966,"score_gpt":0.3276070718816375,"score_spread":0.2628105614381778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384930450","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994373,0.000010929345,0.00018344248,0.000016215467,0.0000018527077,0.0000017904953,0.000011141145,0.000017604592,0.00031961434],"genre_scores_gemma":[0.99986637,0.0000040193627,0.000046436897,0.000004213148,5.457064e-7,0.0000010882807,0.000010882314,0.0000021287356,0.000064187014],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999559,0.000005311755,0.000002160959,0.0000061024684,0.000005403426,0.000025192774],"domain_scores_gemma":[0.9998903,0.000008685062,0.0000334957,0.0000070212946,0.000011528519,0.00004883911],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008423186,0.00016153009,0.000215184,0.00024335882,0.00049327477,0.0004990598,0.00018915116,0.00026575022,0.0006824092],"category_scores_gemma":[0.00028161437,0.00017101165,0.00021183971,0.000118049924,0.00037588752,0.00019360818,0.0005372098,0.0002562262,0.00008138713],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014489053,0.00028387105,0.21128756,0.00010638806,0.000120061944,0.0018636241,0.0013494603,0.0639322,0.7003968,0.0041340706,0.0010127383,0.014064345],"study_design_scores_gemma":[0.00014116935,0.0007299135,0.6814608,0.000026141039,0.00006819457,0.00045537355,0.0013922032,0.26175186,0.04777941,0.0030183396,0.0031057906,0.00007075171],"about_ca_topic_score_codex":0.010184692,"about_ca_topic_score_gemma":0.0092046065,"teacher_disagreement_score":0.010184692,"about_ca_system_score_codex":0.0007598157,"about_ca_system_score_gemma":0.00038253577,"threshold_uncertainty_score":0.020250857},"labels":[],"label_agreement":null},{"id":"W4384930560","doi":"10.1029/2023gl103538","title":"The Glacier‐Climate Interaction Over the Tibetan Plateau and Its Surroundings During the Last Glacial Maximum","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Peking University; National Natural Science Foundation of China","keywords":"Glacier; Westerlies; Geology; Plateau (mathematics); Precipitation; Glacial period; Climatology; Glacier mass balance; Climate change; Physical geography; Accumulation zone; Glacier morphology; Geomorphology; Cryosphere; Geography; Meteorology; Oceanography; Ice stream","score_opus":0.03152347070327464,"score_gpt":0.3046946596267516,"score_spread":0.2731711889234769,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4384930560","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990212,0.00003888643,0.000093676754,0.00004358514,0.000004967812,0.0000017926453,0.00010038209,0.000021577504,0.0006739608],"genre_scores_gemma":[0.9997298,0.000016535254,0.0000361979,0.0000062745357,0.0000036029805,0.0000016623441,0.00009908425,0.000004162224,0.00010277185],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999267,0.00002393079,0.000003441083,0.00001806365,0.0000067377764,0.00002107953],"domain_scores_gemma":[0.99989426,0.000026193076,0.00001750834,0.000010087916,0.00001604157,0.000035800185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002813806,0.00037008623,0.00029230857,0.00038953553,0.00048182698,0.00088866777,0.00038996522,0.00045895492,0.0016155834],"category_scores_gemma":[0.00041072795,0.00021823145,0.0004754907,0.00057548675,0.00035215885,0.0003504389,0.00038714512,0.00030021396,0.00011624135],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005233544,0.00025202223,0.46158475,0.00006385632,0.0005509118,0.0006602772,0.0002620994,0.5162994,0.00942184,0.0010511478,0.0010526972,0.00827763],"study_design_scores_gemma":[0.0001940755,0.00015530513,0.4128095,0.000022150205,0.00013550269,0.00008944103,0.000278453,0.5843388,0.00073118135,0.00046616627,0.0007481975,0.00003128885],"about_ca_topic_score_codex":0.074500635,"about_ca_topic_score_gemma":0.05378819,"teacher_disagreement_score":0.074500635,"about_ca_system_score_codex":0.0010430972,"about_ca_system_score_gemma":0.0007782139,"threshold_uncertainty_score":0.14813393},"labels":[],"label_agreement":null},{"id":"W4385250917","doi":"10.1029/2023gl104255","title":"Inferring Hillslope Groundwater Recharge Ratios From the Storage‐Discharge Relation","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Forest Service; Simon Fraser University","keywords":"Groundwater recharge; Hydrology (agriculture); Groundwater; Water storage; Geology; Depression-focused recharge; Groundwater discharge; Precipitation; Weathering; Environmental science; Streamflow; Aquifer; Geomorphology; Drainage basin; Geography; Meteorology; Geotechnical engineering","score_opus":0.04416054480502033,"score_gpt":0.2963574564746012,"score_spread":0.25219691166958086,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385250917","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956565,0.000048580532,0.003001933,0.000010831525,8.680351e-7,0.000005862957,0.0004928844,0.00009112612,0.00069140916],"genre_scores_gemma":[0.9985073,0.000025870582,0.0012205478,0.000002489726,9.686061e-7,0.0000023159043,0.00016165675,0.0000036741203,0.000075105134],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994576,0.000009601862,0.0000046373334,0.000018823825,0.000010227925,0.000010954758],"domain_scores_gemma":[0.9998561,0.000053751675,0.000042247913,0.0000145452295,0.000020578955,0.000012806884],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014388304,0.00013024129,0.00016007393,0.00078237336,0.00011038538,0.00037608392,0.00013911987,0.000097177006,0.00056613353],"category_scores_gemma":[0.0005681136,0.000107515625,0.000104632745,0.0005091606,0.00011140551,0.00029892244,0.00017074103,0.00007881856,0.00011986619],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012920292,0.000048824353,0.90095806,0.00003932564,0.00006409252,0.000078559264,0.00012520974,0.01585668,0.049026135,0.0002768632,0.00026885426,0.033128172],"study_design_scores_gemma":[0.000014820147,0.000052701023,0.8977427,0.0000061642268,0.000019323312,0.000055704157,0.00015505595,0.091136895,0.009928095,0.00046480977,0.00041004535,0.000013727524],"about_ca_topic_score_codex":0.01918365,"about_ca_topic_score_gemma":0.045278884,"teacher_disagreement_score":0.01918365,"about_ca_system_score_codex":0.00023957537,"about_ca_system_score_gemma":0.00028487731,"threshold_uncertainty_score":0.038143933},"labels":[],"label_agreement":null},{"id":"W4385283295","doi":"10.1029/2022gl102131","title":"Separating Hydraulic Fracturing Microseismicity From Induced Seismicity by Bayesian Inference of Non‐Linear Pressure Diffusivity","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Chevron (Canada); University of Calgary","funders":"","keywords":"Microseism; Induced seismicity; Hydraulic fracturing; Geology; Seismology; Quantile; Thermal diffusivity; Linear regression; Statistics; Mathematics; Geotechnical engineering; Physics","score_opus":0.020877928439250765,"score_gpt":0.30368245569266344,"score_spread":0.28280452725341265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385283295","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.26826343,0.000108311935,0.73012465,0.00020482042,0.0000063649773,0.000023305043,0.00016322982,0.00018987631,0.0009160263],"genre_scores_gemma":[0.9630198,0.000060617967,0.036137078,0.000022593353,0.000011374701,0.000018966415,0.00020504779,0.000028154644,0.00049637875],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996222,0.0001787849,0.000022110247,0.000079922414,0.000055215427,0.00004172166],"domain_scores_gemma":[0.99688345,0.0024182096,0.00032857028,0.00012476678,0.00017057841,0.00007440104],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0019699128,0.00034332895,0.0003778331,0.00057993334,0.00019572135,0.000537521,0.0006012637,0.0004586518,0.0007537481],"category_scores_gemma":[0.006995162,0.00036602508,0.0004268727,0.00031013764,0.00052964606,0.0007925082,0.0005843404,0.00060164725,0.00012389707],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013367798,0.00007317442,0.017518274,0.000055906465,0.00007426717,0.000090739784,0.000072857525,0.92353696,0.0054858713,0.009654245,0.00034599617,0.042958017],"study_design_scores_gemma":[0.0000034067687,0.000007875171,0.0020090155,0.000003771291,0.000004052156,0.0000066761754,0.0000057307952,0.99503064,0.0007165234,0.002141441,0.000065133514,0.0000057264137],"about_ca_topic_score_codex":0.0067556007,"about_ca_topic_score_gemma":0.0072769183,"teacher_disagreement_score":0.0067556007,"about_ca_system_score_codex":0.00044074262,"about_ca_system_score_gemma":0.00071166287,"threshold_uncertainty_score":0.013432562},"labels":[],"label_agreement":null},{"id":"W4385457854","doi":"10.1029/2023gl103326","title":"Stability Dependence of the Turbulent Dissipation Rate in the Convective Atmospheric Boundary Layer","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"National Key Research and Development Program of China; China Meteorological Administration; National Natural Science Foundation of China","keywords":"Dissipation; Turbulence; Convection; Scaling; Physics; Mechanics; Convective Boundary Layer; Boundary layer; Turbulence kinetic energy; Isotropy; Planetary boundary layer; Eddy; Large eddy simulation; Statistical physics; Classical mechanics; Meteorology; Thermodynamics; Geometry; Optics; Mathematics","score_opus":0.057505425327141556,"score_gpt":0.32154897206260186,"score_spread":0.2640435467354603,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385457854","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9845084,0.00012552687,0.0136250155,0.000077132536,0.000013439478,0.000007092556,0.00010230697,0.000075168704,0.0014659102],"genre_scores_gemma":[0.999567,0.000014554925,0.00033060517,0.0000024614314,0.000002088948,0.0000023937755,0.000026775277,0.000004960023,0.000049035538],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999249,0.000015735546,0.0000052225632,0.00002318614,0.000018406194,0.000012565396],"domain_scores_gemma":[0.9996068,0.00018099052,0.00008602253,0.000052721298,0.000053049025,0.000020511152],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029498525,0.00025263845,0.000108734836,0.00022666095,0.00016493502,0.0004195761,0.00024762636,0.00021974315,0.00022267291],"category_scores_gemma":[0.0014317278,0.00013871402,0.0002837708,0.00011956665,0.00028172607,0.00036703225,0.00026841246,0.00029867148,0.00007062466],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025474542,0.00010390669,0.071742095,0.00006976151,0.000100868514,0.00015747528,0.00017653947,0.80669045,0.09294251,0.0108134365,0.0005400011,0.01640814],"study_design_scores_gemma":[0.000004752642,0.000024972363,0.014399866,0.0000041368453,0.0000065983145,0.000013066595,0.0000071355676,0.9793941,0.0051254723,0.00092371803,0.00008729655,0.00000888029],"about_ca_topic_score_codex":0.0027540699,"about_ca_topic_score_gemma":0.0010449607,"teacher_disagreement_score":0.0027540699,"about_ca_system_score_codex":0.00033928448,"about_ca_system_score_gemma":0.00017993173,"threshold_uncertainty_score":0.005476117},"labels":[],"label_agreement":null},{"id":"W4385496227","doi":"10.1029/2023gl104100","title":"An Observational Study of Short‐Cycle Lightning Outbreaks in the Inner Core of Typhoon Hato (2017) Before Landfall","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Education and Child Care","funders":"State Key Laboratory of Severe Weather; National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Graupel; Typhoon; Lightning (connector); Eye; Inner core; Rainband; Landfall; Meteorology; Rossby wave; Convection; Atmospheric sciences; Tropical cyclone; Climatology; Environmental science; Geology; Geophysics; Physics; Power (physics)","score_opus":0.19086657384394198,"score_gpt":0.37882634131186466,"score_spread":0.18795976746792267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385496227","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99970824,0.000014829589,0.000030481928,0.000006509987,0.0000020307557,0.000002193301,0.00012980895,0.0000020416012,0.00010382478],"genre_scores_gemma":[0.99943346,0.00001878295,0.000039257917,0.0000049148193,0.00000550482,0.0000028702798,0.00042650496,8.769551e-7,0.00006785812],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999423,0.000004776543,0.0000048579764,0.000015135935,0.000011012036,0.00002195302],"domain_scores_gemma":[0.9997087,0.000028945804,0.00009313386,0.00002339656,0.000056890123,0.000088977664],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012861162,0.00017361483,0.00020102333,0.00060687575,0.00038401468,0.0002675971,0.00014773307,0.00022622095,0.00044815004],"category_scores_gemma":[0.00026858575,0.00009107912,0.0001599101,0.00045329696,0.00021398178,0.0002720996,0.0003577699,0.00015421565,0.000071982],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012921957,0.00005711527,0.98411363,0.00002409669,0.00004409243,0.000486463,0.0004891505,0.00047626346,0.010111758,0.000062354884,0.00036470883,0.0036410708],"study_design_scores_gemma":[0.0000040262835,0.000027151444,0.99805045,0.0000034465338,0.000010389997,0.00003762242,0.00033059446,0.00087040453,0.0004135474,0.000010665196,0.00023878818,0.00000291486],"about_ca_topic_score_codex":0.024808263,"about_ca_topic_score_gemma":0.04461544,"teacher_disagreement_score":0.024808263,"about_ca_system_score_codex":0.00039188782,"about_ca_system_score_gemma":0.00035754862,"threshold_uncertainty_score":0.04932773},"labels":[],"label_agreement":null},{"id":"W4385568678","doi":"10.1029/2023gl103995","title":"Glacial Isostatic Adjustment Modulates Lateral Migration Rate and Morphology of the Red River (North Dakota, USA and Manitoba, Canada)","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Tributary; Geology; Meander (mathematics); Glacial period; Floodplain; Geomorphology; Erosion; Shear stress; Hydrology (agriculture); Channel (broadcasting); River morphology; Bank erosion; Physical geography; Geotechnical engineering; Geography; Sediment","score_opus":0.018929042415591464,"score_gpt":0.243730296756802,"score_spread":0.22480125434121054,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385568678","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990833,0.000053499967,0.00003553471,0.000039142495,0.0000017010915,0.0000026141786,0.000200758,0.0000045367974,0.0005789908],"genre_scores_gemma":[0.99932575,0.000050729832,0.00007935242,0.000023797782,7.111273e-7,0.0000027815593,0.00018825964,0.0000031986983,0.0003254479],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999027,0.000015637035,0.0000043840196,0.000031136355,0.000020219815,0.000025863214],"domain_scores_gemma":[0.9993988,0.000051385792,0.000109015,0.000028420207,0.00028374506,0.00012859312],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019371454,0.00014928848,0.00016916668,0.00063158583,0.000795747,0.00076170464,0.00035772898,0.00015710651,0.001026368],"category_scores_gemma":[0.00065181067,0.0001521891,0.00013228091,0.00088508654,0.0006803073,0.00014682402,0.00042127378,0.00022040431,0.00013364767],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006148793,0.000022849556,0.9861822,0.000013988529,0.00005662735,0.000059474805,0.0007920428,0.00042643794,0.007760881,0.00010446201,0.00045089,0.0040686666],"study_design_scores_gemma":[0.000001291615,0.0000030723093,0.99918777,0.0000026741632,0.000004304152,0.000007639313,0.00036135633,0.0001804415,0.00008336893,0.000006727534,0.00015884668,0.0000023842024],"about_ca_topic_score_codex":0.90603375,"about_ca_topic_score_gemma":0.9716123,"teacher_disagreement_score":0.093966246,"about_ca_system_score_codex":0.003919289,"about_ca_system_score_gemma":0.003920441,"threshold_uncertainty_score":0.18903923},"labels":[],"label_agreement":null},{"id":"W4385582237","doi":"10.1029/2023gl104787","title":"Dynamic Rupture Process of the 2023 <i>Mw</i> 7.8 Kahramanmaraş Earthquake (SE Türkiye): Variable Rupture Speed and Implications for Seismic Hazard","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":84,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Seismology; Geology; Seismic hazard; Waveform; Fault (geology); Earthquake rupture; Engineering; Aerospace engineering","score_opus":0.03046785237440454,"score_gpt":0.3058243447439334,"score_spread":0.27535649236952886,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385582237","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99907434,0.000014352195,0.0002799144,0.000027448952,0.000003972418,0.0000030435087,0.000102383994,0.000013871332,0.00048071015],"genre_scores_gemma":[0.9997652,0.0000068261943,0.00008043595,0.0000032715911,9.752912e-7,0.000003064186,0.00007560735,0.000001986312,0.0000626698],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999403,0.000010241602,0.0000034146242,0.000012944363,0.0000065149266,0.00002650874],"domain_scores_gemma":[0.99989545,0.000027850103,0.000026689402,0.000010787422,0.000018636507,0.000020643136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017672728,0.00038957412,0.00028288935,0.0003250479,0.00032496924,0.0005955146,0.0005950122,0.0006722778,0.0011386306],"category_scores_gemma":[0.00046060217,0.00021658701,0.00048051728,0.0003192791,0.00030034364,0.00033867708,0.00030735103,0.0003243805,0.0001328946],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025129833,0.00014057022,0.09002687,0.000030949523,0.00012814527,0.0009001484,0.00009074191,0.89102733,0.012094832,0.00086419645,0.00043611604,0.0040087886],"study_design_scores_gemma":[0.000045751538,0.00015349632,0.05428505,0.0000067859637,0.000051099094,0.00011674589,0.00016497239,0.94240266,0.0022287953,0.00023023064,0.0002868066,0.000027574542],"about_ca_topic_score_codex":0.028816631,"about_ca_topic_score_gemma":0.013224066,"teacher_disagreement_score":0.028816631,"about_ca_system_score_codex":0.00071264536,"about_ca_system_score_gemma":0.00046350865,"threshold_uncertainty_score":0.057297826},"labels":[],"label_agreement":null},{"id":"W4385582980","doi":"10.1029/2023gl104642","title":"Impacts of Evaporation‐Induced Groundwater Upwelling on Mixing Dynamics in Shallow Wetlands","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Watershed Management Studies","field":"Environmental Science","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"National Science Foundation","keywords":"Biogeochemical cycle; Upwelling; Groundwater; Wetland; Evaporation; Geology; Mixing (physics); Surface water; Hydrology (agriculture); Groundwater flow; Environmental science; Soil science; Oceanography; Aquifer; Environmental chemistry; Ecology; Chemistry; Environmental engineering","score_opus":0.04066502778328413,"score_gpt":0.3128272799396908,"score_spread":0.27216225215640666,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385582980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923944,0.0000152012,0.00041509132,0.000023481003,0.0000019490278,0.0000030575347,0.000027276521,0.000008624876,0.00026587388],"genre_scores_gemma":[0.99982554,0.000011332925,0.000098481454,0.0000037888713,5.613526e-7,0.0000021318624,0.000010021895,0.0000016651355,0.000046443016],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999193,0.00002126187,0.0000060858097,0.000010229244,0.0000074569803,0.00003562249],"domain_scores_gemma":[0.9998097,0.00009791585,0.000029727082,0.00001198218,0.000017321703,0.00003348789],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002014057,0.00025957,0.00032969884,0.00023785651,0.00036082955,0.000494777,0.0002098997,0.0003710657,0.0006586855],"category_scores_gemma":[0.00064412743,0.00016875056,0.00047821843,0.00019562842,0.0004084113,0.00044237069,0.000538251,0.00028794407,0.000030864005],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029256192,0.00020316626,0.04813504,0.000063320695,0.000101460406,0.00044140665,0.00010465326,0.88815296,0.05644911,0.0013258646,0.0001392376,0.004591201],"study_design_scores_gemma":[0.00009245972,0.00019091017,0.032449525,0.0000070183887,0.000039080936,0.000029117113,0.00013515036,0.9609892,0.0053245504,0.00059630675,0.000120971,0.000025719593],"about_ca_topic_score_codex":0.017812379,"about_ca_topic_score_gemma":0.010268181,"teacher_disagreement_score":0.017812379,"about_ca_system_score_codex":0.0006772091,"about_ca_system_score_gemma":0.0006111865,"threshold_uncertainty_score":0.035417378},"labels":[],"label_agreement":null},{"id":"W4385658220","doi":"10.1029/2023gl103742","title":"Stratospheric Ozone Loss Enhances Summer Precipitation Over the Southern Slope of the Tibetan Plateau","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Canadian Space Agency; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Plateau (mathematics); Precipitation; Climatology; Environmental science; Atmospheric sciences; Stratosphere; Troposphere; Geology; Meteorology; Geography","score_opus":0.04309931919011565,"score_gpt":0.3132099303369917,"score_spread":0.270110611146876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385658220","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99948055,0.00003515268,0.00005190381,0.00003360542,0.0000016504579,0.0000010153775,0.000062654835,0.0000059724825,0.00032748078],"genre_scores_gemma":[0.9998356,0.000018306522,0.0000149934485,0.00000445481,0.0000013807811,8.013831e-7,0.000053074884,4.9072764e-7,0.00007083278],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997354,0.000005224427,0.0000015353855,0.000005403191,0.000004177238,0.000010142139],"domain_scores_gemma":[0.9999392,0.000009297228,0.000015332105,0.000004471093,0.000010709874,0.000020931295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010101496,0.00012214127,0.000109696084,0.00019286474,0.00024124335,0.00036951283,0.00014853437,0.00012570388,0.0009919958],"category_scores_gemma":[0.00016501713,0.0000579698,0.00015998728,0.0002794943,0.00012055695,0.00017986003,0.00022131951,0.00014219411,0.000048162357],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026606067,0.00013324663,0.92797345,0.000069885486,0.00017220175,0.00048402426,0.00028722268,0.01092514,0.047968816,0.0003734894,0.00056752627,0.01077903],"study_design_scores_gemma":[0.000011417874,0.000032761476,0.99174833,0.0000032180387,0.000019385023,0.000021265323,0.0002320848,0.0068839486,0.0007188418,0.00008976838,0.00023602418,0.000002944826],"about_ca_topic_score_codex":0.029453915,"about_ca_topic_score_gemma":0.022682467,"teacher_disagreement_score":0.029453915,"about_ca_system_score_codex":0.00030034478,"about_ca_system_score_gemma":0.0003281482,"threshold_uncertainty_score":0.0585649},"labels":[],"label_agreement":null},{"id":"W4385658282","doi":"10.1029/2023gl104661","title":"Contrasting Trends and Drivers of Global Surface and Canopy Urban Heat Islands","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Urban Heat Island Mitigation","field":"Environmental Science","cited_by":57,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Pacific Northwest National Laboratory; Biological and Environmental Research; Office of Science; National Natural Science Foundation of China; Battelle; U.S. Department of Energy","keywords":"Daytime; Environmental science; Urban heat island; Global warming; Climatology; Surface air temperature; Climate change; Canopy; Urban climate; Urbanization; Atmospheric sciences; Geography; Meteorology; Physical geography; Precipitation; Geology; Oceanography; Economics","score_opus":0.022450065315697796,"score_gpt":0.29171516414109183,"score_spread":0.269265098825394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4385658282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.997468,0.00016445918,0.00028632287,0.00008983921,0.000004726166,0.0000033719932,0.0007398024,0.00001202253,0.0012314201],"genre_scores_gemma":[0.99950993,0.000048973157,0.00006080027,0.000005951234,0.0000035357077,0.0000015306993,0.00029611358,0.0000021324013,0.000071045775],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998938,0.000017944893,0.000008099836,0.000032380445,0.000022668315,0.000025113179],"domain_scores_gemma":[0.9996099,0.00005753297,0.00016371965,0.000036802354,0.00009196338,0.000040121227],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020735375,0.000105836916,0.000113683156,0.00056373415,0.00009083349,0.00046094763,0.00012638367,0.00009192672,0.0009929872],"category_scores_gemma":[0.00051030854,0.00006713116,0.0002085255,0.0009284083,0.0002443325,0.0003120587,0.00048255987,0.0001829757,0.00009444758],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000040819414,0.000009249955,0.9874895,0.000038355578,0.000086441236,0.000037470643,0.00036168564,0.00061289733,0.0017971362,0.00055501424,0.00042742593,0.008544004],"study_design_scores_gemma":[4.6375936e-7,0.0000071519808,0.998792,0.0000049947353,0.000008002433,0.000012389044,0.0002981509,0.0003957319,0.00012044363,0.000066964705,0.00029167952,0.0000019521833],"about_ca_topic_score_codex":0.01589502,"about_ca_topic_score_gemma":0.024460956,"teacher_disagreement_score":0.01589502,"about_ca_system_score_codex":0.00022058091,"about_ca_system_score_gemma":0.0001972655,"threshold_uncertainty_score":0.031605005},"labels":[],"label_agreement":null},{"id":"W4386000668","doi":"10.1029/2023gl103953","title":"Fire Characteristics and Hydrologic Connectivity Influence Short‐Term Responses of North Temperate Lakes to Wildfire","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université de Montréal","funders":"National Science Foundation","keywords":"Environmental science; Water quality; Watershed; Hydrology (agriculture); Temperate climate; Chlorophyll a; Phosphorus; Shore; Ecology; Oceanography; Geology; Biology","score_opus":0.02305479963303802,"score_gpt":0.29119731402086557,"score_spread":0.26814251438782755,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386000668","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99983156,0.000026798998,0.000018264838,0.00000664282,7.114757e-7,0.0000011544041,0.000036711754,7.541115e-7,0.000077297605],"genre_scores_gemma":[0.9997975,0.0000177327,0.00002324167,0.0000071184145,0.0000015792131,0.0000025457657,0.00006269521,7.8736235e-7,0.000086922075],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986994,0.00004260695,0.00001002667,0.00003222936,0.000016077325,0.000029151974],"domain_scores_gemma":[0.99919754,0.00017815914,0.00029160458,0.000039176328,0.00009789015,0.00019563409],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003573968,0.00011898886,0.00014559411,0.00026572717,0.0002478399,0.00043617468,0.00015876425,0.00022223129,0.0009215978],"category_scores_gemma":[0.0012724312,0.00012898276,0.00016947021,0.00022493563,0.00023397738,0.00030754364,0.00027703817,0.00017023756,0.00008102658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00022761645,0.000051665782,0.9939031,0.000007468332,0.000061114384,0.000032576965,0.00016494276,0.00014330093,0.0037687118,0.000010949402,0.00005982485,0.0015687497],"study_design_scores_gemma":[7.226976e-7,0.00002296784,0.99965596,8.3255156e-7,0.0000044415565,0.000007068709,0.00007914929,0.00011964245,0.000080592006,0.000004832233,0.00002313924,6.4187276e-7],"about_ca_topic_score_codex":0.016415546,"about_ca_topic_score_gemma":0.050686885,"teacher_disagreement_score":0.016415546,"about_ca_system_score_codex":0.00038708662,"about_ca_system_score_gemma":0.00021073714,"threshold_uncertainty_score":0.03263998},"labels":[],"label_agreement":null},{"id":"W4386022122","doi":"10.1029/2023gl104549","title":"Winter Arctic Outflow Winds Cause Upper Ocean Cooling and Reoxygenation in a Temperate Canadian Fjord","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Government of British Columbia; University of Victoria; Vancouver Island University; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Hakai Institute","keywords":"Outflow; Oceanography; Inlet; Arctic; Fjord; Environmental science; Temperate climate; Climatology; Atmospheric sciences; Geology; Ecology","score_opus":0.027657786009501487,"score_gpt":0.2740999281438534,"score_spread":0.24644214213435195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386022122","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99894243,0.000025591276,0.000024999934,0.000046992685,0.0000031509871,0.0000029998046,0.00031437384,0.000009383912,0.00063005416],"genre_scores_gemma":[0.99918395,0.000030296216,0.000049141858,0.000015905442,0.0000010318857,0.0000016465759,0.0002654535,0.0000025813574,0.00045004886],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998765,0.000005083105,0.000004434299,0.000023036862,0.000025300633,0.00006568007],"domain_scores_gemma":[0.9997918,0.0000129695745,0.000025192796,0.000009635936,0.00008935422,0.000071033835],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001365424,0.0003241298,0.00021390448,0.0004688956,0.002297632,0.0008692502,0.0005357055,0.00037902757,0.0015018407],"category_scores_gemma":[0.0003648576,0.00022561394,0.00043560876,0.0006157737,0.00049354497,0.00016603261,0.00041078214,0.00029925435,0.00012787581],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029661827,0.00009527566,0.9740141,0.000029027964,0.00010206031,0.0007081505,0.0006051742,0.0079506785,0.008469205,0.00023300381,0.0017656325,0.0057310793],"study_design_scores_gemma":[0.000012610433,0.000012178575,0.9937453,0.000005788981,0.000022929078,0.000037279202,0.00060181244,0.004568558,0.00030310624,0.000031141877,0.0006489076,0.000010299543],"about_ca_topic_score_codex":0.9908065,"about_ca_topic_score_gemma":0.9919876,"teacher_disagreement_score":0.0128772445,"about_ca_system_score_codex":0.0128772445,"about_ca_system_score_gemma":0.007921942,"threshold_uncertainty_score":0.09343135},"labels":[],"label_agreement":null},{"id":"W4386067374","doi":"10.1029/2023gl104769","title":"Martian Bow Shock Oscillations Driven by Solar Wind Variations: Simultaneous Observations From Tianwen‐1 and MAVEN","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"University of Science and Technology of China; National Natural Science Foundation of China; Tencent","keywords":"Martian; Bow shock (aerodynamics); Solar wind; Magnetosphere; Magnetopause; Shock (circulatory); Physics; Geophysics; Dynamic pressure; Magnetosphere of Jupiter; Atmospheric sciences; Shock wave; Environmental science; Mars Exploration Program; Astrobiology; Mechanics; Plasma","score_opus":0.04231370433322292,"score_gpt":0.28654783798045813,"score_spread":0.2442341336472352,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386067374","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99841964,0.000071917915,0.00028305294,0.00002042269,0.000006425507,0.0000062837753,0.0004579167,0.000023219338,0.00071103266],"genre_scores_gemma":[0.9981242,0.000054424825,0.0005160843,0.000015179877,0.000010596646,0.000012245112,0.0009953389,0.000015565547,0.00025635373],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991286,0.000009501475,0.0000053124486,0.000022900225,0.000025712105,0.000023640318],"domain_scores_gemma":[0.99980253,0.00002235205,0.00005002758,0.000030475967,0.00004130845,0.000053278156],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014899852,0.00031795862,0.00046926067,0.000818181,0.00039722238,0.00046477118,0.00044723423,0.00040616767,0.00043134546],"category_scores_gemma":[0.0003271361,0.00020811336,0.00034933968,0.0011534365,0.0001928322,0.00030160276,0.00068019255,0.00032999256,0.00013293288],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00076535536,0.00012552342,0.74280375,0.00010668621,0.0005387624,0.0023893362,0.0017941492,0.003996283,0.22496137,0.00027916074,0.0014370889,0.020802595],"study_design_scores_gemma":[0.00001782197,0.000046366906,0.9902774,0.0000059072827,0.000070468785,0.00023381399,0.00031368167,0.0030720907,0.0045126243,0.000053070362,0.0013806669,0.000016065731],"about_ca_topic_score_codex":0.008768144,"about_ca_topic_score_gemma":0.02413551,"teacher_disagreement_score":0.008768144,"about_ca_system_score_codex":0.00024639632,"about_ca_system_score_gemma":0.00020018307,"threshold_uncertainty_score":0.01743424},"labels":[],"label_agreement":null},{"id":"W4386068184","doi":"10.1029/2023gl103996","title":"Plateau Formation Controlled by Lithospheric Foundering Under a Weak Crust","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Geology; Foreland basin; Lithosphere; Crust; Plateau (mathematics); Subsidence; Tectonics; Lithospheric flexure; Continental crust; Seismology; Structural basin; Paleontology","score_opus":0.03952130991115895,"score_gpt":0.27559795113626673,"score_spread":0.23607664122510777,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386068184","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976029,0.000033280092,0.0007459524,0.000045722823,0.000003129189,0.00000340446,0.00002449781,0.000018827113,0.0015223627],"genre_scores_gemma":[0.99979,0.000011968067,0.0000707534,0.0000025601353,8.0985984e-7,0.000001178102,0.000008070961,0.0000015993043,0.000113079455],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999273,0.000015929363,0.0000044255166,0.000017833236,0.000004921414,0.000029631281],"domain_scores_gemma":[0.9997702,0.000039323615,0.00006897061,0.00003154099,0.000017332952,0.000072570954],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021411853,0.00023901206,0.00034424863,0.00025882685,0.0005207319,0.0010759266,0.0005293112,0.00041795734,0.0016914811],"category_scores_gemma":[0.0006005747,0.0003009955,0.0004915691,0.00022724998,0.0010414544,0.0004692081,0.00070299936,0.0002894491,0.00011923396],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040310892,0.00016178784,0.17914899,0.00013951054,0.00016648523,0.0016286304,0.000467524,0.74853164,0.05053626,0.012692312,0.00034386275,0.0057798717],"study_design_scores_gemma":[0.00017032927,0.00023936444,0.15830477,0.000018794928,0.00006794706,0.00028342966,0.0003457012,0.8316433,0.0021976181,0.0061450195,0.0005475168,0.00003611802],"about_ca_topic_score_codex":0.008461999,"about_ca_topic_score_gemma":0.004647862,"teacher_disagreement_score":0.008461999,"about_ca_system_score_codex":0.0007613864,"about_ca_system_score_gemma":0.0006297925,"threshold_uncertainty_score":0.016825497},"labels":[],"label_agreement":null},{"id":"W4386308278","doi":"10.1029/2023gl103909","title":"Using Deep Learning for Flexible and Scalable Earthquake Forecasting","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; National Science Foundation","keywords":"Benchmark (surveying); Scalability; Earthquake prediction; Aftershock; Computer science; Data set; Earthquake simulation; Set (abstract data type); Scale (ratio); Artificial neural network; Seismology; Data mining; Machine learning; Artificial intelligence; Geology; Geography; Cartography; Database","score_opus":0.14191344088159213,"score_gpt":0.33394648219165884,"score_spread":0.1920330413100667,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386308278","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.3158456,0.00069017854,0.6703923,0.0012401339,0.00014296884,0.0000565727,0.0008667369,0.0064971712,0.0042683487],"genre_scores_gemma":[0.9113617,0.00014871957,0.08591078,0.00011891316,0.000043740198,0.00004012563,0.00078159827,0.00008003974,0.0015143754],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998369,0.000034274923,0.000012154557,0.000045927944,0.00004067322,0.000030058989],"domain_scores_gemma":[0.99939275,0.0002691975,0.000060304224,0.00011150826,0.00013101385,0.00003521431],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006329586,0.0006163383,0.00045862468,0.000426881,0.0002260836,0.00063774927,0.0009864367,0.00061037444,0.0014244105],"category_scores_gemma":[0.0021430575,0.00042219582,0.00029083996,0.0005410384,0.00035171647,0.0011929452,0.00092700816,0.0010297205,0.00046778866],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007216987,0.000051902844,0.0017234378,0.000022532959,0.000032941938,0.00003949675,0.000018505294,0.9196242,0.0037340196,0.0014055991,0.0018716592,0.07140354],"study_design_scores_gemma":[0.0000016526903,0.0000029593505,0.00004330041,5.8285406e-7,7.312036e-7,9.805678e-7,0.0000011995576,0.99918836,0.00024899066,0.00045224442,0.000058212358,7.838657e-7],"about_ca_topic_score_codex":0.016387591,"about_ca_topic_score_gemma":0.018575111,"teacher_disagreement_score":0.016387591,"about_ca_system_score_codex":0.0007199113,"about_ca_system_score_gemma":0.0008366128,"threshold_uncertainty_score":0.03258437},"labels":[],"label_agreement":null},{"id":"W4386495717","doi":"10.1029/2023gl104095","title":"Closing Greenland's Mass Balance: Frontal Ablation of Every Greenlandic Glacier From 2000 to 2020","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Lethbridge; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; University of Ottawa","keywords":"Glacier mass balance; Glacier; Greenland ice sheet; Ablation zone; Ablation; Geology; Climatology; Ice stream; Tidewater glacier cycle; Glacier ice accumulation; Physical geography; Oceanography; Cryosphere; Geomorphology; Sea ice; Geography; Medicine; Ice calving","score_opus":0.03717243733427427,"score_gpt":0.28464766439044514,"score_spread":0.24747522705617087,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386495717","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99227166,0.00042107017,0.00043883608,0.00020485342,0.000015648531,0.0000033964543,0.0027458337,0.000043716795,0.003854971],"genre_scores_gemma":[0.9972121,0.00013352634,0.00023220258,0.000060842587,0.0000067250107,0.0000030371027,0.0017333449,0.000010130273,0.00060808717],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999392,0.0000064812143,0.0000035887922,0.000014445382,0.000018896599,0.000017380511],"domain_scores_gemma":[0.9998516,0.00001621662,0.000048092035,0.000012625589,0.000049495335,0.000022011503],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025000054,0.00031217505,0.00013366132,0.0005282865,0.0001912753,0.00063101575,0.00018577618,0.00017079117,0.00092676486],"category_scores_gemma":[0.00037321966,0.00006841073,0.00026983445,0.00059768726,0.00019607623,0.0004883005,0.00032199168,0.0001914742,0.00016628086],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020328577,0.000030965217,0.9400428,0.00006461564,0.00018545744,0.00019816068,0.00030406358,0.013321812,0.00573564,0.0008014226,0.00313654,0.03597534],"study_design_scores_gemma":[0.000003978552,0.000016001364,0.99112916,0.000019231547,0.000026001131,0.00005090056,0.00012464199,0.003599494,0.00074336026,0.00024357796,0.0040386897,0.0000050616386],"about_ca_topic_score_codex":0.06972567,"about_ca_topic_score_gemma":0.10295555,"teacher_disagreement_score":0.06972567,"about_ca_system_score_codex":0.0011405352,"about_ca_system_score_gemma":0.00063947414,"threshold_uncertainty_score":0.13863963},"labels":[],"label_agreement":null},{"id":"W4386554130","doi":"10.1029/2023gl103341","title":"Winter Mixed Layer Restratification Induced by Vertical Eddy Buoyancy Flux in the Labrador Sea","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Alberta","funders":"Fundamental Research Funds for the Central Universities; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China","keywords":"Buoyancy; Geology; Eddy; Convection; Mixed layer; Mesoscale meteorology; Frontogenesis; Deep convection; Neutral buoyancy; Climatology; Atmospheric sciences; Geophysics; Mechanics; Turbulence; Physics","score_opus":0.046774871973178436,"score_gpt":0.2986115044764341,"score_spread":0.25183663250325566,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386554130","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877733,0.000018988567,0.00027602617,0.000048914673,0.0000050051613,0.0000021595938,0.00015480357,0.000079261765,0.00063756836],"genre_scores_gemma":[0.99961805,0.000009563563,0.0000884488,0.000009958303,0.0000015184505,0.0000025459472,0.00012051347,0.000011022858,0.00013825491],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991953,0.000015718544,0.0000055141404,0.000016380309,0.000008089376,0.000034793087],"domain_scores_gemma":[0.99986434,0.000025521651,0.000030545856,0.000021961378,0.000018640974,0.000039028262],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000161871,0.00046570937,0.0004164512,0.00030915605,0.00033340082,0.00088458316,0.0004111181,0.00047492195,0.00076241815],"category_scores_gemma":[0.00042519215,0.0002592786,0.0005567354,0.00022913195,0.00035452525,0.00039317767,0.00043347196,0.00037961552,0.00015105317],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010230739,0.00029049424,0.2375619,0.0000663541,0.00027782924,0.0006199578,0.00021034946,0.6858288,0.06202627,0.0012762118,0.0015510618,0.009267664],"study_design_scores_gemma":[0.00016073829,0.00015112774,0.17193115,0.000012935968,0.000066450906,0.00005338462,0.00010707397,0.8202135,0.0064131534,0.00032476624,0.00052431686,0.000041446605],"about_ca_topic_score_codex":0.07186375,"about_ca_topic_score_gemma":0.030822152,"teacher_disagreement_score":0.9281362,"about_ca_system_score_codex":0.0011761647,"about_ca_system_score_gemma":0.00047646023,"threshold_uncertainty_score":0.14289087},"labels":[],"label_agreement":null},{"id":"W4386794748","doi":"10.1029/2023gl103519","title":"Electron Precipitation Observed by ELFIN Using Proton Precipitation as a Proxy for Electromagnetic Ion Cyclotron (EMIC) Waves","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":55,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration; Canadian Space Agency; University of Alberta; National Science Foundation","keywords":"Electron precipitation; Van Allen radiation belt; Van Allen Probes; Emic and etic; Cyclotron; Physics; Precipitation; Proton; Pitch angle; Polar; Atmospheric sciences; Electron; Ion; Geophysics; Computational physics; Magnetosphere; Nuclear physics; Astronomy; Meteorology; Plasma","score_opus":0.029360886416487035,"score_gpt":0.3198712014267518,"score_spread":0.29051031501026475,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386794748","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9870433,0.00007811565,0.0013873334,0.00007199687,0.00001239872,0.00001941906,0.004756339,0.00037607978,0.0062551047],"genre_scores_gemma":[0.9950492,0.00003103508,0.0013402828,0.00005032497,0.000009318439,0.00001512604,0.00305002,0.000043267148,0.00041132333],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991906,0.0000065583754,0.0000030186784,0.00002410641,0.000025253834,0.000022020968],"domain_scores_gemma":[0.99982136,0.000024463707,0.000053743246,0.000024322871,0.000048175916,0.000028003837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022750838,0.00031490356,0.00018479215,0.0006840882,0.00026701883,0.00033816136,0.00023174452,0.000181384,0.0021539142],"category_scores_gemma":[0.00030146964,0.00010874126,0.00015578556,0.0006065854,0.00020329666,0.00037528938,0.00035870585,0.0002688343,0.00027286314],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.001038154,0.00020698154,0.8059421,0.000090273614,0.0002000788,0.00037738902,0.0002291566,0.008369002,0.15113233,0.00048564255,0.005727225,0.026201645],"study_design_scores_gemma":[0.000040186093,0.000097266355,0.960062,0.000012004682,0.000029999243,0.00022463051,0.00011054881,0.009613142,0.026311016,0.0002263856,0.0032584467,0.000014256946],"about_ca_topic_score_codex":0.003141111,"about_ca_topic_score_gemma":0.005904155,"teacher_disagreement_score":0.003141111,"about_ca_system_score_codex":0.0003235333,"about_ca_system_score_gemma":0.00011775941,"threshold_uncertainty_score":0.007205546},"labels":[],"label_agreement":null},{"id":"W4386927461","doi":"10.1029/2023gl103994","title":"Thermal Conductivity of Hydrogen at High Pressure and High Temperature: Implications to Giant Planets","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Academia Sinica; Natural Sciences and Engineering Research Council of Canada; National Science and Technology Council","keywords":"Thermal conductivity; Planet; Hydrogen; Thermodynamics; Thermal; Materials science; Crystallization; Physics; Analytical Chemistry (journal); Chemistry; Astrophysics","score_opus":0.029937452325776527,"score_gpt":0.277511227766691,"score_spread":0.2475737754409145,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386927461","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9896923,0.0016282777,0.0044984994,0.0006734631,0.000032930122,0.0000037160255,0.0001388662,0.00016200106,0.0031700123],"genre_scores_gemma":[0.9995633,0.00017095853,0.00015017818,0.0000137305315,0.000007301785,0.0000016882522,0.00002263933,0.000005480552,0.00006476526],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99995685,0.0000055800606,0.0000014049177,0.000014572327,0.000011522043,0.000009991631],"domain_scores_gemma":[0.9999275,0.000026888256,0.000019025723,0.00000789402,0.000009923317,0.000008736668],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000087673296,0.00023185147,0.00014927653,0.00017759859,0.00021530775,0.0003392877,0.0002760239,0.00037506782,0.0005853784],"category_scores_gemma":[0.00032918472,0.00014393518,0.000101106605,0.00023725946,0.0007849419,0.0006595379,0.00042131657,0.00039666763,0.000093595474],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00029937417,0.00008930986,0.0494275,0.00036963105,0.000063133346,0.0017417052,0.0005104743,0.06528834,0.8452545,0.01645937,0.0023954078,0.01810132],"study_design_scores_gemma":[0.00005935358,0.00031268445,0.1725313,0.00007288274,0.000050046594,0.0012818882,0.0013611634,0.37590963,0.3451496,0.09445547,0.008673654,0.00014235738],"about_ca_topic_score_codex":0.0005900065,"about_ca_topic_score_gemma":0.00021190253,"teacher_disagreement_score":0.0005900065,"about_ca_system_score_codex":0.00023187691,"about_ca_system_score_gemma":0.00008477967,"threshold_uncertainty_score":0.0019583106},"labels":[],"label_agreement":null},{"id":"W4386967342","doi":"10.1029/2023gl104171","title":"Predicting Tropical Cyclone‐Induced Sea Surface Temperature Responses Using Machine Learning","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou); National Social Science Fund of China; Natural Science Foundation of Guangdong Province","keywords":"Tropical cyclone; Sea surface temperature; Environmental science; Intensity (physics); Climatology; Storm; Wind speed; Meteorology; Atmospheric sciences; Geology; Geography","score_opus":0.06269969315870133,"score_gpt":0.3227638230737218,"score_spread":0.2600641299150205,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4386967342","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.6605651,0.00022896682,0.33632493,0.0002060502,0.000058031397,0.000049141294,0.000373326,0.00071885943,0.0014757172],"genre_scores_gemma":[0.98491836,0.000038634964,0.014420815,0.000018597499,0.000013778728,0.000028339926,0.00018268437,0.00000856139,0.0003701612],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998964,0.000045224107,0.0000044503763,0.000022378334,0.000013066519,0.000018399141],"domain_scores_gemma":[0.99956304,0.00028833197,0.000036577014,0.00002270525,0.000072488685,0.000016829461],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006432873,0.00036001246,0.00037277397,0.000317682,0.00020996736,0.00030803896,0.00031203308,0.0003848633,0.00069388875],"category_scores_gemma":[0.0010028897,0.00016576861,0.00043382106,0.00021067043,0.00016468563,0.00028734677,0.00015508644,0.00033700082,0.00014543122],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00004356837,0.00005837781,0.006218213,0.000009600768,0.000028967017,0.000013082457,0.000005013868,0.9822041,0.0006467577,0.00018236795,0.00018699346,0.010403011],"study_design_scores_gemma":[0.0000015000737,0.0000057052453,0.0003191389,5.205627e-7,0.0000012723557,0.0000010661672,6.633083e-7,0.9995345,0.00007067152,0.000052045798,0.000012242071,6.678525e-7],"about_ca_topic_score_codex":0.013107571,"about_ca_topic_score_gemma":0.008507168,"teacher_disagreement_score":0.013107571,"about_ca_system_score_codex":0.0002984483,"about_ca_system_score_gemma":0.0005764925,"threshold_uncertainty_score":0.026062548},"labels":[],"label_agreement":null},{"id":"W4387048282","doi":"10.1029/2023gl105472","title":"On the Influence of Hydroxyl Radical Changes and Ocean Sinks on Estimated HCFC and HFC Emissions and Banks","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Aeronautics and Space Administration; National Science Foundation","keywords":"Montreal Protocol; Greenhouse gas; Environmental science; Chlorofluorocarbon; Halocarbon; Atmospheric sciences; Atmosphere (unit); Seawater; Hydroxyl radical; Greenhouse effect; Global warming; Environmental chemistry; Climate change; Climatology; Meteorology; Oceanography; Chemistry; Ozone layer; Radical; Stratosphere; Geology","score_opus":0.03813750124515672,"score_gpt":0.29646511624527344,"score_spread":0.2583276150001167,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387048282","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99183613,0.000248828,0.0033969993,0.00022576781,0.000030620336,0.0000136769295,0.0017854451,0.000112585614,0.0023498998],"genre_scores_gemma":[0.9982736,0.00005367965,0.00069127936,0.000028157701,0.000003513577,0.000005087071,0.0006905638,0.000019171875,0.00023477747],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.999752,0.00007680693,0.000019228597,0.000077305536,0.000040951974,0.000033773544],"domain_scores_gemma":[0.99875677,0.00078939536,0.00012725873,0.00010464873,0.0001814819,0.000040456525],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00097485294,0.0004835397,0.00018497319,0.00035398555,0.0002585755,0.0007638042,0.00045343116,0.0005552756,0.0012047729],"category_scores_gemma":[0.0033310952,0.00023585318,0.0007654403,0.00027349577,0.000281139,0.0008179862,0.00048373447,0.00038972366,0.00017552887],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006682609,0.0001034113,0.43102145,0.00016767887,0.0005323155,0.00023768307,0.00008449551,0.5265278,0.023402637,0.0012238709,0.0012719124,0.014758396],"study_design_scores_gemma":[0.00011560369,0.000107763946,0.29698408,0.000049515067,0.0001945164,0.000065621585,0.00017886788,0.67427707,0.025171313,0.0009492705,0.0018275869,0.0000788381],"about_ca_topic_score_codex":0.061496396,"about_ca_topic_score_gemma":0.033711515,"teacher_disagreement_score":0.061496396,"about_ca_system_score_codex":0.00071824196,"about_ca_system_score_gemma":0.0005727712,"threshold_uncertainty_score":0.1222769},"labels":[],"label_agreement":null},{"id":"W4387168891","doi":"10.1029/2023gl105225","title":"Exploring the AMOC Connectivity Between the RAPID and OSNAP Lines With a Model‐Based Data Set","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Xiamen University","keywords":"Ekman transport; Climatology; Isopycnal; Oceanography; Adiabatic process; Geology; Forcing (mathematics); Shutdown of thermohaline circulation; Mode water; Thermohaline circulation; Environmental science; North Atlantic Deep Water; Physics; Subtropics","score_opus":0.2428419069472255,"score_gpt":0.3227515119363239,"score_spread":0.07990960498909841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387168891","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9952624,0.00002456732,0.0006925053,0.000043838732,0.0000057816296,0.0000075374305,0.0033520514,0.00004878429,0.000562527],"genre_scores_gemma":[0.99199706,0.000017836175,0.0009205984,0.000010240089,0.0000051139423,0.000011352694,0.006934163,0.00000821765,0.000095427524],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997718,0.00006282623,0.000015777223,0.00008863332,0.000029810868,0.000031220523],"domain_scores_gemma":[0.9995167,0.00013783426,0.000101394166,0.000112885224,0.00008764095,0.000043488853],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056665804,0.0002489632,0.00023796267,0.00055595,0.00025207663,0.0005877152,0.00051005563,0.00031880275,0.00075816235],"category_scores_gemma":[0.0010343624,0.00018531356,0.00051011035,0.00074351724,0.00020591413,0.00053254166,0.0004802105,0.0003108244,0.000117338735],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030248,0.00023894777,0.75567394,0.00006349426,0.00048536784,0.00013714394,0.00013947964,0.22131719,0.004101457,0.00086257706,0.0021024547,0.014575498],"study_design_scores_gemma":[0.00007054137,0.00009181939,0.56249183,0.000015382655,0.00008406662,0.000045269608,0.0002326193,0.43315703,0.0013422078,0.0003728513,0.0020660772,0.00003040713],"about_ca_topic_score_codex":0.06394532,"about_ca_topic_score_gemma":0.11825186,"teacher_disagreement_score":0.06394532,"about_ca_system_score_codex":0.0005974145,"about_ca_system_score_gemma":0.000655483,"threshold_uncertainty_score":0.12714624},"labels":[],"label_agreement":null},{"id":"W4387170945","doi":"10.1029/2023gl105205","title":"Drought and Waterlogging Stress Regimes in Northern Peatlands Detected Through Satellite Retrieved Solar‐Induced Chlorophyll Fluorescence","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Fonds Wetenschappelijk Onderzoek; Vlaamse regering; Vlaams Supercomputer Centrum","keywords":"Peat; Environmental science; Waterlogging (archaeology); Water table; Chlorophyll fluorescence; Vegetation (pathology); Primary production; Ecosystem respiration; Atmospheric sciences; Climate change; Transpiration; Hydrology (agriculture); Ecosystem; Wetland; Photosynthesis; Geology; Ecology; Groundwater; Chemistry; Oceanography","score_opus":0.027349816363287798,"score_gpt":0.2821702864121719,"score_spread":0.2548204700488841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387170945","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99986374,0.000009827024,0.000048080237,0.0000015415784,2.8949077e-7,5.782667e-7,0.00003418069,0.0000017444681,0.000040038827],"genre_scores_gemma":[0.9998313,0.000007821818,0.0000696547,0.0000012515326,6.3030177e-7,0.000001570675,0.00005628713,5.6804765e-7,0.000030844865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993706,0.000014219525,0.0000048338825,0.000018755765,0.000008670828,0.000016370228],"domain_scores_gemma":[0.9997882,0.00005396451,0.00006329345,0.000017149438,0.000027622424,0.00004970112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030766884,0.00014619857,0.00024286279,0.0003652648,0.00018238225,0.00027488283,0.00011120809,0.00019132637,0.0003280919],"category_scores_gemma":[0.00037881985,0.000105873456,0.0001645111,0.0003021922,0.0002524576,0.0002794895,0.00021563216,0.00010078183,0.000051779054],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024017146,0.00006196602,0.95492995,0.000022736882,0.00006225555,0.00015890737,0.0003458032,0.001989399,0.037598237,0.00004184649,0.0000350427,0.004513712],"study_design_scores_gemma":[0.0000013666979,0.000021230417,0.99818295,0.000001292771,0.000004669729,0.000028301216,0.00010004071,0.0011499252,0.00046675993,0.000012387974,0.000028749608,0.0000023122282],"about_ca_topic_score_codex":0.018545631,"about_ca_topic_score_gemma":0.025369937,"teacher_disagreement_score":0.018545631,"about_ca_system_score_codex":0.00034835062,"about_ca_system_score_gemma":0.00021254417,"threshold_uncertainty_score":0.036875367},"labels":[],"label_agreement":null},{"id":"W4387186382","doi":"10.1029/2023gl103943","title":"Use of Shallow Ice Core Measurements to Evaluate and Constrain 1980–1990 Global Reanalyses of Ice Sheet Precipitation Rates","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"U.S. Department of Energy","keywords":"Ice sheet; Ice core; Climatology; Precipitation; Greenland ice sheet; Firn; Ice-sheet model; Future sea level; Antarctic ice sheet; Geology; Environmental science; Atmospheric sciences; Ice stream; Sea ice; Cryosphere; Meteorology; Snow; Oceanography; Geography; Geomorphology","score_opus":0.26720178621274177,"score_gpt":0.3877804489495801,"score_spread":0.12057866273683832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387186382","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977912,0.00005908492,0.0006313535,0.000013872912,0.0000021464984,0.000007985651,0.0005428347,0.0000146045695,0.0009369192],"genre_scores_gemma":[0.9974842,0.00004593871,0.0012627316,0.000012554094,0.0000024108708,0.000009107916,0.0010418693,0.0000032177472,0.00013793874],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999845,0.000043847267,0.000015787258,0.000039477723,0.00003618871,0.000019597259],"domain_scores_gemma":[0.99935704,0.00014633371,0.00013166499,0.00010052776,0.00020980717,0.000054636035],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006947314,0.00023025059,0.00010510916,0.00059383153,0.00019409339,0.00027082028,0.00012779231,0.0001269458,0.0002363464],"category_scores_gemma":[0.0012861455,0.00011581195,0.00013620767,0.00054699864,0.00015988799,0.00029432535,0.00027357115,0.00012023504,0.00008835253],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010780038,0.000054755335,0.96856403,0.00001392942,0.000095514944,0.000021722955,0.00013715983,0.0055314014,0.007942245,0.00010784346,0.0002702137,0.017153384],"study_design_scores_gemma":[0.000011650981,0.000031947155,0.9901598,0.0000049867404,0.00002447337,0.000012190878,0.00004907277,0.0072077843,0.0019002871,0.00005645268,0.000537361,0.0000039534298],"about_ca_topic_score_codex":0.06399388,"about_ca_topic_score_gemma":0.14257546,"teacher_disagreement_score":0.06399388,"about_ca_system_score_codex":0.00069923856,"about_ca_system_score_gemma":0.0005823047,"threshold_uncertainty_score":0.12724274},"labels":[],"label_agreement":null},{"id":"W4387307939","doi":"10.1029/2023gl104732","title":"Dissolved Organic Radiocarbon in the West Indian Ocean","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa","funders":"Canada Research Chairs; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Dissolved organic carbon; Radiocarbon dating; Seawater; Oceanography; Particulate organic carbon; Deep water; Total organic carbon; Deep sea; Surface water; Deep ocean water; Dissolution; Water column; Geology; Indian ocean; Carbon fibers; Environmental science; Carbon cycle; Environmental chemistry; Chemistry; Ecosystem; Phytoplankton; Ecology; Environmental engineering","score_opus":0.02651193581280458,"score_gpt":0.2628311360903581,"score_spread":0.2363192002775535,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387307939","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948454,0.0004497556,0.0001622301,0.00005085593,0.000017012135,0.0000054408697,0.0014552715,0.000018279366,0.0029958151],"genre_scores_gemma":[0.9974577,0.00037466187,0.00025931932,0.000046014127,0.000009410225,0.00000776761,0.00085921126,0.000005817294,0.000980157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989855,0.000009653412,0.000009470744,0.000030668944,0.000026245649,0.00002548259],"domain_scores_gemma":[0.9996307,0.000039798288,0.00012423056,0.00002625634,0.00014571333,0.000033164168],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011236367,0.00021116335,0.00010631933,0.0010680921,0.00034347546,0.0006079635,0.00021387714,0.00008490176,0.00076220563],"category_scores_gemma":[0.00033447912,0.00011473463,0.00010599135,0.001360593,0.0001900839,0.00021715503,0.00030960797,0.00020273028,0.00022735096],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012360894,0.000021525006,0.9546753,0.00006795391,0.00005121922,0.00031224088,0.00053293526,0.00017233896,0.024634795,0.00008196345,0.00028615122,0.01904001],"study_design_scores_gemma":[0.0000013306401,0.000016983,0.9963385,0.0000065910954,0.000015578442,0.00010307633,0.00034628288,0.00007142252,0.0015010759,0.000011571881,0.0015826151,0.000004860785],"about_ca_topic_score_codex":0.09187432,"about_ca_topic_score_gemma":0.12029613,"teacher_disagreement_score":0.09187432,"about_ca_system_score_codex":0.0003653564,"about_ca_system_score_gemma":0.00041542386,"threshold_uncertainty_score":0.18267906},"labels":[],"label_agreement":null},{"id":"W4387576398","doi":"10.1029/2023gl104991","title":"Systematic Occurrence Cycle of Typical RH‐Profiles During the MJO: Evidence for Ubiquitous Pre‐Moistening","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Space Agency; Environment and Climate Change Canada; Natural Environment Research Council; Sight Research UK","keywords":"Madden–Julian oscillation; Troposphere; Climatology; Environmental science; Atmospheric Infrared Sounder; Relative humidity; Precipitation; Atmospheric sciences; Convection; Climate model; Meteorology; Geology; Climate change; Geography; Oceanography","score_opus":0.09025446572788069,"score_gpt":0.369013014527078,"score_spread":0.2787585487991973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387576398","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988834,0.000030887644,0.0002856263,0.000012650974,0.0000025063182,0.0000026738435,0.00037259798,0.00002142383,0.00038818642],"genre_scores_gemma":[0.9995635,0.000008017111,0.00009955619,0.0000026628927,0.0000022347674,0.0000018055531,0.000292345,0.000002689853,0.000027160519],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999923,0.000014466821,0.000008312144,0.00002564025,0.000013385391,0.00001521305],"domain_scores_gemma":[0.9994773,0.00013657377,0.0001728728,0.000079199024,0.000060493432,0.00007352511],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023772115,0.000088163,0.00014276676,0.00045723334,0.00018168952,0.00029022532,0.00014608807,0.00016479699,0.0005632256],"category_scores_gemma":[0.00080314366,0.000092783535,0.00016053388,0.0004254506,0.00020848852,0.0001789631,0.00023952399,0.00013640939,0.00010578284],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000143301,0.00003594674,0.97723275,0.000018124403,0.00006353742,0.00006217186,0.0001051647,0.0016972723,0.015146215,0.0001539787,0.0002726878,0.0050688176],"study_design_scores_gemma":[0.0000024227015,0.000016861366,0.99578285,0.0000014446787,0.000007623038,0.000039016573,0.00002345228,0.0029217885,0.00093605,0.000033668726,0.00023211802,0.0000027786373],"about_ca_topic_score_codex":0.0035689028,"about_ca_topic_score_gemma":0.004712844,"teacher_disagreement_score":0.0035689028,"about_ca_system_score_codex":0.00014268755,"about_ca_system_score_gemma":0.00010870321,"threshold_uncertainty_score":0.0070962906},"labels":[],"label_agreement":null},{"id":"W4387704616","doi":"10.1029/2023gl104314","title":"Effect of Regional Marine Cloud Brightening Interventions on Climate Tipping Elements","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate Change and Geoengineering","field":"Environmental Science","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Defense Advanced Research Projects Agency","keywords":"Tipping point (physics); Environmental science; Greenhouse gas; Climate change; Psychological intervention; Climate model; Climatology; Global warming; Natural resource economics; Environmental resource management; Meteorology; Atmospheric sciences; Economics; Geography; Oceanography; Geology","score_opus":0.06495758230833729,"score_gpt":0.3640216899132401,"score_spread":0.29906410760490276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387704616","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978144,0.000087295986,0.00037450253,0.00014374555,0.000015619386,0.00006410326,0.0001798189,0.000030569372,0.0012900367],"genre_scores_gemma":[0.9991128,0.000040696745,0.00038992515,0.00008144959,0.000003904386,0.000058095262,0.00006678267,0.0000038143123,0.00024251558],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9994068,0.0003225481,0.000018554176,0.00010420726,0.000044689026,0.00010321859],"domain_scores_gemma":[0.99819213,0.0006713804,0.0004931433,0.0002206606,0.00014951006,0.00027330837],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00096439145,0.0003192456,0.00038222247,0.00016492762,0.00038737734,0.0004592135,0.00070916704,0.0005363244,0.0036381017],"category_scores_gemma":[0.003179434,0.000106226085,0.0005108524,0.0002279983,0.0005504374,0.00031809596,0.00083941955,0.00061489723,0.0001919341],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.046304327,0.032049775,0.22365466,0.0021588237,0.002846885,0.00094894256,0.0017837646,0.28615472,0.22821695,0.008015289,0.006686311,0.16117957],"study_design_scores_gemma":[0.0038412695,0.055854887,0.78967243,0.00016535225,0.00116623,0.000100546524,0.0031813798,0.07496274,0.056554437,0.0058282395,0.008508894,0.00016365215],"about_ca_topic_score_codex":0.018337073,"about_ca_topic_score_gemma":0.024484072,"teacher_disagreement_score":0.018337073,"about_ca_system_score_codex":0.0010692995,"about_ca_system_score_gemma":0.0010708139,"threshold_uncertainty_score":0.036460698},"labels":[],"label_agreement":null},{"id":"W4387730493","doi":"10.1029/2023gl105156","title":"Seasonal Changes in Atmospheric Heat Transport to the Arctic Under Increased CO<sub>2</sub>","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Environmental science; Arctic; Climatology; Arctic sea ice decline; Global warming; Sea ice; Arctic ice pack; Atmospheric sciences; Seasonality; Forcing (mathematics); Arctic geoengineering; Climate change; Oceanography; Sea ice thickness; Geology; Ecology","score_opus":0.038502699302819736,"score_gpt":0.2954761258328761,"score_spread":0.25697342653005634,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387730493","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9966126,0.00008667609,0.0010147342,0.00013662735,0.000043986714,0.000004069652,0.00063556765,0.0000774719,0.0013882638],"genre_scores_gemma":[0.99928254,0.00004945768,0.0001378673,0.000018891194,0.0000062211298,0.000003982502,0.00030093204,0.000011644146,0.00018842355],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999434,0.000011052671,0.000003234447,0.00001676065,0.000006881405,0.000018654966],"domain_scores_gemma":[0.99989116,0.000028471652,0.000020466898,0.000011999452,0.00002711646,0.000020742054],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017937877,0.0003650777,0.00023118706,0.0001823042,0.00025234642,0.00056263455,0.0002723932,0.00031918625,0.001230241],"category_scores_gemma":[0.00029034266,0.00016620099,0.00058458385,0.00025810188,0.00028685958,0.00029169358,0.00023891454,0.00043354143,0.00012273215],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000634477,0.00018156327,0.13547882,0.00010415369,0.000510543,0.00025669023,0.0000864154,0.8054964,0.04753669,0.0016501329,0.0021334859,0.0059306147],"study_design_scores_gemma":[0.0000845629,0.0001668346,0.23047566,0.000024413832,0.00016118925,0.000062200845,0.00018094221,0.75819784,0.008364813,0.00079393707,0.0014348265,0.00005278022],"about_ca_topic_score_codex":0.053695608,"about_ca_topic_score_gemma":0.02681574,"teacher_disagreement_score":0.053695608,"about_ca_system_score_codex":0.0006727159,"about_ca_system_score_gemma":0.00057449454,"threshold_uncertainty_score":0.106766164},"labels":[],"label_agreement":null},{"id":"W4387735316","doi":"10.1029/2023gl104461","title":"Retrieval of Snow Depth on Arctic Sea Ice From Surface‐Based, Polarimetric, Dual‐Frequency Radar Altimetry","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Manitoba","funders":"HORIZON EUROPE European Research Council; Natural Environment Research Council; Swiss Polar Institute; Deutsche Forschungsgemeinschaft; Sight Research UK; European Space Agency; National Science Foundation","keywords":"Snow; Geology; Sea ice; Remote sensing; Altimeter; Polarimetry; Sea ice thickness; Radar; Arctic; Arctic ice pack; Geodesy; Climatology; Oceanography; Geomorphology","score_opus":0.03903547408894607,"score_gpt":0.29227084020105226,"score_spread":0.2532353661121062,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4387735316","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.989627,0.0001312918,0.008760687,0.000020930518,0.0000121496705,0.000009800165,0.000356618,0.00009272157,0.0009888734],"genre_scores_gemma":[0.9883299,0.00009811501,0.010662398,0.000013281551,0.00001075018,0.000007053294,0.00053037645,0.000011972443,0.0003362998],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99992,0.000022262171,0.0000035303574,0.00001708434,0.000024302177,0.00001276836],"domain_scores_gemma":[0.9998342,0.000033566983,0.000027026777,0.000018904724,0.000068278736,0.000017928087],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027494915,0.00035069362,0.00025093497,0.0006277945,0.00011919316,0.00048785828,0.00016066022,0.00015661829,0.00028011136],"category_scores_gemma":[0.00042917285,0.00019287264,0.0002210266,0.0003694181,0.00010652848,0.00034008047,0.00033721633,0.00014427857,0.00020677569],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0016219834,0.00016713837,0.21423729,0.00022069525,0.00028148023,0.00015373151,0.00023455358,0.0593276,0.57541674,0.0004383983,0.00095811544,0.14694224],"study_design_scores_gemma":[0.00018190553,0.0005101579,0.41248515,0.00004139819,0.00022504728,0.0001603279,0.00018756837,0.46466523,0.11875199,0.00047327008,0.002257476,0.00006047218],"about_ca_topic_score_codex":0.0027135296,"about_ca_topic_score_gemma":0.004911671,"teacher_disagreement_score":0.0027135296,"about_ca_system_score_codex":0.00022107128,"about_ca_system_score_gemma":0.00025464612,"threshold_uncertainty_score":0.0053954124},"labels":[],"label_agreement":null},{"id":"W4388015486","doi":"10.1029/2023gl105112","title":"A Dissection of the Inter‐Model Spread of the Aerosol Direct Radiative Effect in CMIP6 Models","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aerosol; Radiative transfer; Environmental science; Anomaly (physics); Atmospheric sciences; Shortwave; Climate model; Albedo (alchemy); Climatology; Meteorology; Climate change; Physics; Geology","score_opus":0.023721630216569763,"score_gpt":0.29285273189948524,"score_spread":0.2691311016829155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388015486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99239784,0.00016838996,0.0044277525,0.00016655408,0.00001342004,0.000015643704,0.00044633137,0.00019773014,0.0021663855],"genre_scores_gemma":[0.9987562,0.00003109902,0.00074750383,0.000011944809,0.0000054381408,0.0000060603984,0.00030634852,0.00003750675,0.00009792888],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99948174,0.0002132516,0.000033676653,0.00014554163,0.00007398044,0.0000518278],"domain_scores_gemma":[0.997264,0.0016309862,0.0002306802,0.0004479437,0.00033866783,0.00008772583],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0030272477,0.00065609417,0.00029313547,0.00092957716,0.00028905005,0.00073073624,0.0006944031,0.00058898504,0.00082193234],"category_scores_gemma":[0.005770628,0.0004067809,0.0010301248,0.0006736549,0.0003354179,0.0008911084,0.000634666,0.00057161634,0.00013783129],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003428472,0.00012010898,0.2262932,0.00005860794,0.0009376788,0.00021328915,0.00016872594,0.74157095,0.011637627,0.0024723033,0.0010056869,0.015178978],"study_design_scores_gemma":[0.00005007078,0.000076145436,0.1284284,0.000018730632,0.00014448226,0.00004737953,0.000091399794,0.8652818,0.0043508927,0.0007435476,0.0007300004,0.00003706505],"about_ca_topic_score_codex":0.015937105,"about_ca_topic_score_gemma":0.00694041,"teacher_disagreement_score":0.015937105,"about_ca_system_score_codex":0.00047993934,"about_ca_system_score_gemma":0.00032506435,"threshold_uncertainty_score":0.03168863},"labels":[],"label_agreement":null},{"id":"W4388088994","doi":"10.1029/2023gl105344","title":"Steady‐State Bedrock Channel Width","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Simon Fraser University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Bedrock; Bed load; Geology; Scaling; Sediment; Hydrology (agriculture); Geomorphology; Erosion; Flux (metallurgy); Channel (broadcasting); Drainage basin; Sediment transport; Grain size; Steady state (chemistry); Geotechnical engineering; Geometry","score_opus":0.034619371968980184,"score_gpt":0.30295786809007297,"score_spread":0.2683384961210928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388088994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.91960126,0.00011214071,0.06899349,0.00016084478,0.000017110515,0.000019795747,0.00049255876,0.00022083911,0.010382039],"genre_scores_gemma":[0.9970107,0.00003715153,0.0014568188,0.000014185999,0.0000020277096,0.000016864135,0.00013547191,0.00001620132,0.0013105462],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991655,0.000012512998,0.000003986451,0.000034054203,0.000012031326,0.000020887272],"domain_scores_gemma":[0.9997588,0.00008714113,0.000045580357,0.00003437765,0.000053524753,0.000020719064],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023129111,0.0001860623,0.0002022856,0.00021072206,0.00019354191,0.00075639284,0.0006232588,0.00042382436,0.0018226693],"category_scores_gemma":[0.0010473591,0.00023641787,0.00042987592,0.00019507857,0.0004319608,0.00076632196,0.0002659738,0.0002675494,0.00025142854],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002904368,0.000029869614,0.013265349,0.000017972818,0.000021746591,0.000051757594,0.00005357276,0.97005165,0.0037559266,0.00850845,0.00032159782,0.0038930993],"study_design_scores_gemma":[0.000010450613,0.000033057368,0.005513374,0.000008748135,0.000012765636,0.000028926264,0.000040034218,0.9879985,0.0011927846,0.004643967,0.00050446833,0.000012961942],"about_ca_topic_score_codex":0.007138834,"about_ca_topic_score_gemma":0.00482601,"teacher_disagreement_score":0.007138834,"about_ca_system_score_codex":0.0007256666,"about_ca_system_score_gemma":0.00053413404,"threshold_uncertainty_score":0.014194608},"labels":[],"label_agreement":null},{"id":"W4388232102","doi":"10.1029/2023gl105132","title":"An Explanation for the Metric Dependence of the Midlatitude Jet‐Waviness Change in Response to Polar Warming","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":28,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Middle latitudes; Waviness; Climatology; Jet (fluid); Atmospheric sciences; Amplitude; Geology; Polar; Environmental science; Physics; Mechanics; Optics; Materials science","score_opus":0.0646679634191937,"score_gpt":0.3395010865716701,"score_spread":0.27483312315247643,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388232102","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939464,0.000073098156,0.0031849304,0.00029565056,0.000017584864,0.000015852835,0.00027703645,0.000077263314,0.002112326],"genre_scores_gemma":[0.9994997,0.000010309453,0.00032553155,0.000024786175,0.0000024192143,0.000005385202,0.00006310242,0.0000094466195,0.000059371007],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998142,0.000072958945,0.000016089665,0.00003628186,0.000016711389,0.00004379167],"domain_scores_gemma":[0.99914575,0.0003453009,0.00014046821,0.0001920731,0.00009824945,0.00007816965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00054622,0.00030169848,0.00030343243,0.00040852322,0.00028145523,0.00064293854,0.00048653447,0.00040774237,0.001990061],"category_scores_gemma":[0.0031068055,0.00019039208,0.00051156967,0.00022876434,0.000510516,0.00048723043,0.0005936818,0.00043918975,0.00012830575],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00082113856,0.000321482,0.26674196,0.0002541019,0.00039773874,0.00043739434,0.0004997056,0.5780317,0.12690648,0.011225153,0.0022487666,0.012114388],"study_design_scores_gemma":[0.00009149434,0.00025095293,0.28297004,0.000022185362,0.000059200753,0.00011437175,0.00035578784,0.69816315,0.010374972,0.006646944,0.00090689916,0.000044082502],"about_ca_topic_score_codex":0.0049920445,"about_ca_topic_score_gemma":0.003861791,"teacher_disagreement_score":0.0049920445,"about_ca_system_score_codex":0.00044797873,"about_ca_system_score_gemma":0.00023860106,"threshold_uncertainty_score":0.0099259615},"labels":[],"label_agreement":null},{"id":"W4388283545","doi":"10.1029/2023gl106073","title":"It's Not Easy Being Green: Kinetic Modeling of the Emission Spectrum Observed in STEVE's Picket Fence","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Electric field; Electron precipitation; Physics; Fence (mathematics); Kinetic energy; Electron; Spectral line; Ionosphere; Atmosphere (unit); Line (geometry); Picketing; Atmospheric sciences; Computational physics; Atomic physics; Environmental science; Magnetic field; Meteorology; Geophysics; Magnetosphere; Classical mechanics; Quantum mechanics","score_opus":0.04056407115722502,"score_gpt":0.2927529805503898,"score_spread":0.25218890939316474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388283545","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.994023,0.000011992176,0.0037718636,0.000043562435,0.0000035019946,0.0000035210294,0.00002954962,0.000036806705,0.0020761776],"genre_scores_gemma":[0.99948716,0.0000062046324,0.00021341999,0.000003684227,6.0653576e-7,0.0000017025096,0.000013106341,0.000007663701,0.00026637054],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999788,0.0000035364385,3.6760676e-7,0.0000047078665,0.0000035955154,0.000008998408],"domain_scores_gemma":[0.99993527,0.000019226529,0.000010947949,0.0000068902405,0.0000086085965,0.000019050782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008975805,0.00021409524,0.00019079843,0.0001859527,0.0003548546,0.00035365432,0.00046146507,0.00031656332,0.001234227],"category_scores_gemma":[0.0002965949,0.00011230712,0.00024490716,0.00012057373,0.0003623487,0.00035486775,0.00022507421,0.00021583351,0.00006899604],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044335375,0.000116290576,0.033181187,0.000029460738,0.00006219875,0.00065745803,0.00023934299,0.90041536,0.049395066,0.011025728,0.0006125483,0.0038220375],"study_design_scores_gemma":[0.000032177784,0.000032785752,0.008508651,0.0000019260674,0.0000054835236,0.00004062501,0.00009625358,0.9862775,0.0031695233,0.0015977914,0.00022780013,0.000009469404],"about_ca_topic_score_codex":0.008308193,"about_ca_topic_score_gemma":0.004467858,"teacher_disagreement_score":0.008308193,"about_ca_system_score_codex":0.00048229934,"about_ca_system_score_gemma":0.00018869092,"threshold_uncertainty_score":0.016519666},"labels":[],"label_agreement":null},{"id":"W4388538312","doi":"10.1029/2023gl105392","title":"Intense Energetic Electron Precipitation Caused by the Self‐Limiting of Space Radiation","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Thunder Bay Regional Research Institute; University of Alberta","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Public Works and Government Services Canada; Nuclear Safety and Security Commission; Sight Research UK; National Aeronautics and Space Administration","keywords":"Electron precipitation; Van Allen radiation belt; Electron; Precipitation; Limiting; Atmospheric sciences; Physics; Geomagnetic storm; Flux (metallurgy); Storm; Atmosphere (unit); Earth's magnetic field; Magnetosphere; Geophysics; Environmental science; Chemistry; Magnetic field; Meteorology; Nuclear physics; Plasma","score_opus":0.011970396816971821,"score_gpt":0.2789361599800179,"score_spread":0.2669657631630461,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388538312","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994642,0.000033673525,0.00023337598,0.0000040827836,9.2271927e-7,0.0000019254462,0.000030146033,0.000007917649,0.00022358968],"genre_scores_gemma":[0.9997942,0.000015997695,0.00008352826,0.0000028413249,0.0000021233304,0.000001449699,0.000055356173,0.0000017848138,0.00004283917],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993896,0.000006095211,0.000003751031,0.000018688575,0.000015690615,0.000016825725],"domain_scores_gemma":[0.99974555,0.0000419141,0.00011953797,0.000026753769,0.000033913722,0.000032335007],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015285007,0.00012162316,0.0002588718,0.00045365075,0.00025106443,0.00032547183,0.00018069628,0.00014750488,0.0004204732],"category_scores_gemma":[0.0003217134,0.00009835099,0.00015243991,0.00024507233,0.00029720747,0.0002105331,0.00039504305,0.00016633146,0.00006095506],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045249384,0.00009673886,0.77645195,0.000045510496,0.00017425057,0.00054020557,0.00028504131,0.0059584114,0.20525283,0.00030603283,0.0002645753,0.0101719415],"study_design_scores_gemma":[0.000008790168,0.00009156728,0.9751472,0.0000030807907,0.000020496369,0.00024693806,0.00009491002,0.007891831,0.016072305,0.00013667434,0.00027966857,0.000006634035],"about_ca_topic_score_codex":0.0012388291,"about_ca_topic_score_gemma":0.0013028552,"teacher_disagreement_score":0.0012388291,"about_ca_system_score_codex":0.00019862801,"about_ca_system_score_gemma":0.00009201635,"threshold_uncertainty_score":0.0024632215},"labels":[],"label_agreement":null},{"id":"W4388851347","doi":"10.1029/2023gl103096","title":"Arctic Tropospheric Ozone Trends","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Centre National d’Etudes Spatiales; Agence Nationale de la Recherche; Natural Environment Research Council; Sight Research UK","keywords":"Environmental science; Troposphere; Climatology; The arctic; Ozone; Tropospheric ozone; Arctic; Atmospheric sciences; Meteorology; Oceanography; Geography; Geology","score_opus":0.037936611756251855,"score_gpt":0.2942679173715187,"score_spread":0.25633130561526685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388851347","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.902483,0.0019712085,0.003235025,0.00035476996,0.00015550363,0.000023083834,0.0743915,0.00045237635,0.016933654],"genre_scores_gemma":[0.980213,0.0007337601,0.0013297892,0.00004451586,0.000020937354,0.00001885686,0.016219681,0.000028328455,0.001391169],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998853,0.00001390663,0.00000999814,0.00004456513,0.000028690223,0.000017509805],"domain_scores_gemma":[0.9997948,0.000026105787,0.00004181894,0.000018540502,0.00010246574,0.000016299047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003303177,0.00029655138,0.00014472473,0.0006223236,0.00030259666,0.0006632171,0.00014164699,0.00017670654,0.0015105889],"category_scores_gemma":[0.00045936875,0.00009569784,0.00040695816,0.00084900006,0.00004781629,0.00028726461,0.00031972743,0.00020631013,0.00029951954],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028645527,0.000059103688,0.840893,0.00044231865,0.0007533492,0.00013298824,0.00037914608,0.08599713,0.0066030356,0.0020029875,0.013455159,0.048995387],"study_design_scores_gemma":[0.00002680677,0.000077011755,0.91923124,0.0001080348,0.00025014495,0.00007062919,0.00026118816,0.0361107,0.0046302336,0.0006770261,0.03852735,0.000029673127],"about_ca_topic_score_codex":0.08589418,"about_ca_topic_score_gemma":0.08839784,"teacher_disagreement_score":0.08589418,"about_ca_system_score_codex":0.0007117206,"about_ca_system_score_gemma":0.0005691341,"threshold_uncertainty_score":0.1707884},"labels":[],"label_agreement":null},{"id":"W4388934599","doi":"10.1029/2023gl106178","title":"Multi‐Decadal Record of Sensible‐Heat Polynya Variability From Satellite Optical and Thermal Imagery at Pine Island Glacier, West Antarctica","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Sciences and Engineering Research Council of Canada; Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Geology; Glacier; Climatology; Oceanography; Satellite; Satellite imagery; Ice shelf; Sea ice; Cryosphere; Geomorphology","score_opus":0.04092669018004446,"score_gpt":0.2844566499227412,"score_spread":0.24352995974269676,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388934599","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99554056,0.00012604627,0.000085362444,0.000044325046,0.000007781213,0.0000066160082,0.0032829784,0.000021796577,0.0008845598],"genre_scores_gemma":[0.9954586,0.00013809926,0.00039590802,0.000031810512,0.00001844858,0.000014751617,0.003552998,0.0000069218077,0.0003826297],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995506,0.0000065614017,0.0000037966875,0.000013285425,0.0000107188425,0.000010542513],"domain_scores_gemma":[0.9997179,0.00003671266,0.00008037363,0.00003110763,0.00006837472,0.000065480854],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021190174,0.00017894451,0.00010896401,0.0008675337,0.0003470421,0.00040769338,0.00015459361,0.00018393376,0.00077910174],"category_scores_gemma":[0.0003209108,0.00011602893,0.00012010383,0.0007180394,0.00017638216,0.0002650915,0.00036668306,0.00021219792,0.00011990713],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011351765,0.00005521766,0.9749645,0.000058062084,0.0001269675,0.00016644642,0.00047872888,0.0010156876,0.0073062973,0.000057366433,0.0021435139,0.013513635],"study_design_scores_gemma":[0.0000021727872,0.000004948451,0.99902344,0.0000048957227,0.000009540599,0.0000194654,0.000063026346,0.00027971712,0.00014807686,0.000006048796,0.0004369738,0.0000017209302],"about_ca_topic_score_codex":0.05559281,"about_ca_topic_score_gemma":0.1692265,"teacher_disagreement_score":0.05559281,"about_ca_system_score_codex":0.0003499882,"about_ca_system_score_gemma":0.00029361487,"threshold_uncertainty_score":0.11053842},"labels":[],"label_agreement":null},{"id":"W4388965198","doi":"10.1029/2023gl105307","title":"The Role of Small to Moderate Volcanic Eruptions in the Early 19th Century Climate","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"HORIZON EUROPE European Research Council; Bundesministerium für Bildung und Forschung; Deutsche Forschungsgemeinschaft; Deutsches Klimarechenzentrum","keywords":"Volcano; Climatology; Global cooling; Geology; Forcing (mathematics); Ice core; Solar irradiance; Environmental science; Atmospheric sciences; Climate change; Earth science; Seismology; Oceanography","score_opus":0.04288312749644517,"score_gpt":0.3070259916033837,"score_spread":0.2641428641069385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388965198","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978775,0.00008371638,0.0006910087,0.00014945009,0.000014080144,0.000004297774,0.00032202658,0.000023150847,0.00083479594],"genre_scores_gemma":[0.99961,0.000040001916,0.00014590693,0.000012062559,0.0000047925473,0.0000025537104,0.00011222313,0.000007803534,0.00006466275],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998803,0.000042270494,0.0000068280933,0.000034157532,0.00001032836,0.000026037527],"domain_scores_gemma":[0.99976,0.00009994661,0.00003220787,0.00003542744,0.000024592562,0.000047933238],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047970813,0.0003216588,0.00028260527,0.0003213339,0.0003290316,0.00078292115,0.00043342158,0.00060460967,0.0014871915],"category_scores_gemma":[0.0010623534,0.00023858766,0.00054333813,0.00033870098,0.0004228308,0.00050766004,0.000469296,0.00046384058,0.00008992588],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024879797,0.00016982996,0.3490756,0.00006606789,0.00041046855,0.0003852253,0.00017239107,0.6266397,0.011673617,0.0030889793,0.00081685296,0.0072524934],"study_design_scores_gemma":[0.00008188613,0.00009148745,0.36657003,0.000025259109,0.000105998944,0.000086262036,0.00016089242,0.62558776,0.0027760416,0.0023637086,0.002112435,0.000038137314],"about_ca_topic_score_codex":0.03010209,"about_ca_topic_score_gemma":0.026061254,"teacher_disagreement_score":0.03010209,"about_ca_system_score_codex":0.00095820735,"about_ca_system_score_gemma":0.0005132102,"threshold_uncertainty_score":0.059853792},"labels":[],"label_agreement":null},{"id":"W4388977925","doi":"10.1029/2023gl105723","title":"Time Resolved Reflectivity Measurements of Convective Clouds","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Science Mission Directorate; Langley Research Center; National Aeronautics and Space Administration; California Institute of Technology; Jet Propulsion Laboratory; U.S. Department of Energy; National Science Foundation","keywords":"Convection; Radar; Remote sensing; Doppler effect; Sampling (signal processing); Doppler radar; Geology; Environmental science; Meteorology; Physics; Optics; Computer science; Astronomy","score_opus":0.14718289561732417,"score_gpt":0.34731079236376566,"score_spread":0.2001278967464415,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4388977925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974311,0.000045337267,0.0017905264,0.000009192126,0.0000036016588,0.000002796369,0.000108659755,0.000032531592,0.0005761511],"genre_scores_gemma":[0.999132,0.000013699055,0.00067664817,0.000003116701,0.0000018194074,0.0000013050573,0.00009210536,0.0000022150202,0.00007714951],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99992716,0.0000098896335,0.0000032076332,0.000020982528,0.000021642803,0.000017083044],"domain_scores_gemma":[0.9998851,0.000022173208,0.000024169078,0.000016366692,0.00003415558,0.000017974846],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015918458,0.000106625026,0.00010987154,0.00032801335,0.00013278275,0.00020702444,0.00016356261,0.00014276839,0.00027453736],"category_scores_gemma":[0.00038294736,0.000078976635,0.00007242722,0.00019542503,0.00008774725,0.00019739928,0.0001787392,0.00019868503,0.00009408281],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007445266,0.00025717294,0.23379081,0.00004211394,0.000094386225,0.000185007,0.0003551919,0.020683859,0.69404703,0.0007665453,0.0008263721,0.04820685],"study_design_scores_gemma":[0.00006760325,0.0005767128,0.6115903,0.0000144440555,0.00007335262,0.00029913953,0.0002585728,0.19506063,0.18963821,0.00041502473,0.0019629495,0.00004306326],"about_ca_topic_score_codex":0.0019355594,"about_ca_topic_score_gemma":0.002019651,"teacher_disagreement_score":0.0019355594,"about_ca_system_score_codex":0.00017102715,"about_ca_system_score_gemma":0.000090960566,"threshold_uncertainty_score":0.0038485527},"labels":[],"label_agreement":null},{"id":"W4389142251","doi":"10.1029/2023gl105469","title":"Statistical Properties of the Distribution and Generation of Kinetic‐Scale Flux Ropes in the Terrestrial Dayside Magnetosheath","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Science Foundation of Shandong Province; Vetenskapsrådet; China Postdoctoral Science Foundation; Swedish National Space Agency; National Natural Science Foundation of China","keywords":"Magnetosheath; Magnetopause; Physics; Solar wind; Magnetic reconnection; Geophysics; Magnetosphere; Flux (metallurgy); Bow shock (aerodynamics); Magnetic flux; Atmospheric sciences; Computational physics; Magnetic field; Shock wave; Mechanics","score_opus":0.03432242260578348,"score_gpt":0.28103645290515306,"score_spread":0.24671403029936959,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389142251","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99881506,0.000035745015,0.0007348729,0.000012876908,0.0000016779933,0.000002377642,0.00015316861,0.000014089624,0.00023021198],"genre_scores_gemma":[0.9996947,0.0000092430655,0.00007627668,0.0000010971237,0.0000027888852,0.00000194191,0.00016672217,0.0000022807176,0.000045053574],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985945,0.00002243747,0.000008533075,0.000052041276,0.000027955379,0.000029516712],"domain_scores_gemma":[0.99824095,0.0007013043,0.0005767881,0.00014592042,0.00015240948,0.00018253921],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043137363,0.0001206455,0.0001620829,0.0011430891,0.0002368646,0.0003469973,0.00018038781,0.00022137903,0.000921668],"category_scores_gemma":[0.0019278426,0.00010848938,0.00021778558,0.0005817736,0.0004046224,0.00039051543,0.0003141482,0.00017517073,0.00008249032],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027196752,0.000037804904,0.9516888,0.00004176787,0.00016104877,0.0004654089,0.00023887945,0.018648524,0.017258726,0.0021571403,0.0005171955,0.008512577],"study_design_scores_gemma":[0.000009149283,0.00006809401,0.95328647,0.0000043742443,0.000024947129,0.00022058563,0.00021303997,0.043306638,0.0016934815,0.0007722764,0.000378442,0.000022562563],"about_ca_topic_score_codex":0.0008179141,"about_ca_topic_score_gemma":0.00053195516,"teacher_disagreement_score":0.0011430891,"about_ca_system_score_codex":0.00016855501,"about_ca_system_score_gemma":0.0000718043,"threshold_uncertainty_score":0.0030832887},"labels":[],"label_agreement":null},{"id":"W4389167952","doi":"10.1029/2023gl106715","title":"Van Allen Probes Observations of a Three‐Dimensional Field Line Resonance at a Plasmaspheric Plume","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University; Thunder Bay Regional Research Institute","funders":"Science and Technology Facilities Council; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Magnetosphere; Physics; Plume; Field line; Geophysics; Plasmasphere; Alfvén wave; Computational physics; Van Allen Probes; Earth's magnetic field; Magnetohydrodynamic drive; Plasma; Geomagnetic storm; Van Allen radiation belt; Magnetohydrodynamics; Magnetic field; Meteorology","score_opus":0.04044586481982916,"score_gpt":0.29248236068267186,"score_spread":0.2520364958628427,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389167952","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99756,0.00002767322,0.0007218771,0.000037137135,0.0000033253957,0.0000058722844,0.00018661201,0.000045543,0.0014119453],"genre_scores_gemma":[0.9985347,0.000014344291,0.0010415884,0.000013361351,0.0000030101296,0.0000043692958,0.00015672072,0.0000066669886,0.00022535973],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999578,0.0000051843854,9.643986e-7,0.000009347615,0.00001429598,0.0000124467915],"domain_scores_gemma":[0.99989367,0.000030855317,0.000023988749,0.000009037795,0.00001869486,0.000023705357],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008105478,0.00010901057,0.00008514669,0.00048279107,0.0002362205,0.00022840647,0.00022669228,0.00023147334,0.0005186254],"category_scores_gemma":[0.00017504433,0.000102108825,0.000101152305,0.00024684894,0.00012665887,0.000187158,0.000276671,0.00025578,0.00007301653],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00040157273,0.000086596265,0.12253145,0.000032504086,0.000060197744,0.0008446979,0.0009803855,0.0049503893,0.8535819,0.00079435535,0.0008887005,0.014847181],"study_design_scores_gemma":[0.00006897495,0.00038651488,0.89788216,0.000023045402,0.000047960344,0.0007273923,0.0010184912,0.039169516,0.054957714,0.00074581953,0.004912523,0.000059933678],"about_ca_topic_score_codex":0.005849498,"about_ca_topic_score_gemma":0.009109814,"teacher_disagreement_score":0.005849498,"about_ca_system_score_codex":0.00015965794,"about_ca_system_score_gemma":0.00009206699,"threshold_uncertainty_score":0.011630952},"labels":[],"label_agreement":null},{"id":"W4389274624","doi":"10.1029/2023gl104790","title":"Gravitational Constraints on the Earth's Inner Core Differential Rotation","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"European Research Council; Université de Strasbourg; Centre National d’Etudes Spatiales; Centre National de la Recherche Scientifique; Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada; Natural Sciences and Engineering Research Council of Canada; European Commission","keywords":"Inner core; Amplitude; Physics; Differential rotation; Earth's rotation; Gravitation; Geodesy; Rotation (mathematics); Gravitational field; Mantle (geology); Geology; Geophysics; Geometry; Classical mechanics; Optics; Astrophysics; Mathematics","score_opus":0.0964814914532164,"score_gpt":0.31096610240059575,"score_spread":0.21448461094737936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389274624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98968387,0.00036742323,0.0017207729,0.00014883431,0.0000127962685,0.0000035537037,0.00058822375,0.00008030847,0.007394191],"genre_scores_gemma":[0.99939823,0.000047745158,0.00014328514,0.0000135371765,0.000006609162,8.332709e-7,0.0002524722,0.00000886644,0.0001284597],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991274,0.000013194233,0.000004894953,0.000023751452,0.00001759512,0.000027817987],"domain_scores_gemma":[0.99948055,0.000119837714,0.000120424746,0.00009042668,0.00011047245,0.000078255674],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000316643,0.00039983983,0.0002394379,0.00079958024,0.00030795,0.00071521645,0.00024129904,0.00034267578,0.0015107774],"category_scores_gemma":[0.0019685568,0.00021384636,0.00019680991,0.0005832887,0.0005068301,0.00046823657,0.0006592938,0.00032449834,0.00029757264],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006847239,0.000081779624,0.72929764,0.00013926129,0.00015260723,0.0005661207,0.00039488025,0.10574166,0.09645156,0.019925011,0.0039363033,0.042628445],"study_design_scores_gemma":[0.000023152113,0.00004428013,0.93978256,0.000025358531,0.000022713126,0.0000926908,0.00008904191,0.049859956,0.0038103408,0.003305694,0.0029129265,0.00003126816],"about_ca_topic_score_codex":0.017106896,"about_ca_topic_score_gemma":0.016078431,"teacher_disagreement_score":0.017106896,"about_ca_system_score_codex":0.0006061678,"about_ca_system_score_gemma":0.000292663,"threshold_uncertainty_score":0.034014642},"labels":[],"label_agreement":null},{"id":"W4389374435","doi":"10.1029/2023gl105972","title":"Paleozoic Decollement Displaced the Surface Trace of Iapetus Ocean Closure in Northern Appalachians","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Laurentia; Geology; Terrane; Gondwana; Paleozoic; Crust; Paleontology; Décollement; Geophysics; Earth science; Tectonics","score_opus":0.024718333634490018,"score_gpt":0.26743160722078835,"score_spread":0.24271327358629832,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389374435","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99857104,0.000033591914,0.000026057874,0.000016862072,9.0849915e-7,0.0000010900847,0.00014935997,0.0000031279512,0.0011979429],"genre_scores_gemma":[0.99947494,0.000024271443,0.000027451055,0.000005277362,6.54685e-7,0.000001255874,0.00013121856,0.0000012909308,0.00033374658],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999417,0.0000044543995,0.0000021248045,0.000018841132,0.00001113111,0.000021732903],"domain_scores_gemma":[0.99980146,0.000021677944,0.000044161006,0.00001251312,0.00008195383,0.000038122722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008716912,0.00012832973,0.00010351726,0.00073438947,0.0006888036,0.00061920483,0.00021867885,0.00015888222,0.0022333027],"category_scores_gemma":[0.00040200475,0.000101994774,0.00007427834,0.0008696959,0.00048129953,0.00020863212,0.00046045578,0.0002142674,0.00019870604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000084548185,0.00000982056,0.97958916,0.0000146669045,0.00001744441,0.00022776016,0.0018802396,0.00016859887,0.008234653,0.00013869492,0.00021402007,0.0094203735],"study_design_scores_gemma":[4.2847176e-7,0.000002304357,0.9991604,0.0000025327338,0.000001312411,0.000017986109,0.000481485,0.000047711907,0.00009120225,0.000004549496,0.00018942493,8.134339e-7],"about_ca_topic_score_codex":0.62537026,"about_ca_topic_score_gemma":0.78269565,"teacher_disagreement_score":0.62537026,"about_ca_system_score_codex":0.0012883487,"about_ca_system_score_gemma":0.00077784323,"threshold_uncertainty_score":0.753672},"labels":[],"label_agreement":null},{"id":"W4389639503","doi":"10.1029/2023gl104977","title":"Characterization of the Spatial Distribution of the Thermodynamic Phase Within Mixed‐Phase Clouds Using Satellite Observations","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Mixed phase; Ice crystals; Phase (matter); Mixing (physics); Satellite; Spatial distribution; Liquid water content; Environmental science; Atmospheric sciences; Materials science; Geology; Meteorology; Cloud computing; Remote sensing; Physics","score_opus":0.058271964237146145,"score_gpt":0.3056442373749536,"score_spread":0.24737227313780746,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389639503","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99879277,0.000022832683,0.0006078113,0.0000073519363,7.436544e-7,0.0000033263757,0.00031518703,0.000013635031,0.00023629935],"genre_scores_gemma":[0.9992372,0.000010417682,0.0003748858,0.0000011158312,0.0000015724146,0.000002153411,0.00034577938,0.0000020226319,0.000024893669],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992514,0.000012930288,0.000005221793,0.000023028735,0.000017706336,0.000015853959],"domain_scores_gemma":[0.9996239,0.000121958474,0.000081578895,0.00003457963,0.000098792494,0.000039085768],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002743966,0.00018340732,0.0001678823,0.0007210256,0.00015475319,0.00040102736,0.00023329174,0.0001895572,0.0003634267],"category_scores_gemma":[0.0006181202,0.00015068734,0.00022479628,0.00062843144,0.00013502559,0.00041095627,0.00019496403,0.00012657653,0.00010869306],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024229544,0.000072357965,0.94255304,0.000030425208,0.00009972085,0.000068475856,0.00014109105,0.02242178,0.026276987,0.00026553654,0.000107108375,0.0077211796],"study_design_scores_gemma":[0.0000179937,0.000047351336,0.8404556,0.000009172543,0.00003475638,0.00004346815,0.00010748779,0.15315038,0.005747281,0.000114631825,0.00026087134,0.000011038073],"about_ca_topic_score_codex":0.018892795,"about_ca_topic_score_gemma":0.017721003,"teacher_disagreement_score":0.018892795,"about_ca_system_score_codex":0.00031122795,"about_ca_system_score_gemma":0.00019620378,"threshold_uncertainty_score":0.03756565},"labels":[],"label_agreement":null},{"id":"W4389677404","doi":"10.1029/2023gl105100","title":"Exploration of Thermal Bridging Through Shrub Branches in Alpine Snow","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université Laval","funders":"European Research Council; Natural Sciences and Engineering Research Council of Canada; Labex; Agence Nationale de la Recherche; European Commission","keywords":"Tundra; Snow; Shrub; Atmospheric sciences; Permafrost; Environmental science; Arctic; Liquid water; Snowmelt; Physical geography; Geology; Geomorphology; Earth science; Ecology; Geography","score_opus":0.16127678276547738,"score_gpt":0.34461405761479674,"score_spread":0.18333727484931936,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389677404","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988398,0.000047587684,0.00047644883,0.0000080958225,9.3540575e-7,0.0000023523028,0.00005832328,0.000016476853,0.00054997747],"genre_scores_gemma":[0.99958843,0.000022340486,0.0002851834,0.0000022300967,8.506905e-7,0.0000018481135,0.000046770518,0.000002677178,0.000049661812],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99997187,0.000004815076,9.928855e-7,0.0000094911675,0.000004503141,0.000008346558],"domain_scores_gemma":[0.9999331,0.000022760754,0.000015850897,0.0000057467637,0.000009196483,0.000013315895],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000094343515,0.00020699108,0.00022123978,0.00031686045,0.0002796145,0.00042357598,0.00021979699,0.0002193839,0.00095666846],"category_scores_gemma":[0.00013978289,0.00016663912,0.00019315128,0.00027491245,0.00028507106,0.00027250408,0.00021582117,0.000140132,0.00008371106],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000640704,0.00033320935,0.3149556,0.00026034127,0.00018707712,0.0008991175,0.00059136463,0.34618008,0.30433762,0.0014415848,0.00032557963,0.029847657],"study_design_scores_gemma":[0.00004910302,0.0002547413,0.2726953,0.000028772647,0.000047568046,0.00015047147,0.00049191137,0.7033268,0.020605773,0.0011975691,0.0011209183,0.000031051128],"about_ca_topic_score_codex":0.004458574,"about_ca_topic_score_gemma":0.005683457,"teacher_disagreement_score":0.004458574,"about_ca_system_score_codex":0.00024335696,"about_ca_system_score_gemma":0.00017312319,"threshold_uncertainty_score":0.008865237},"labels":[],"label_agreement":null},{"id":"W4389774986","doi":"10.1029/2023gl105964","title":"Unprecedented Human‐Perceived Heat Stress in 2021 Summer Over Western North America: Increasing Intensity and Frequency in a Warming Climate","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Relative humidity; Environmental science; Air temperature; Climate change; Humidity; Atmospheric sciences; Apparent temperature; Climatology; Heat stress; Intensity (physics); Percentile; Meteorology; Geography; Geology; Ecology; Physics; Biology","score_opus":0.0506124102765331,"score_gpt":0.3310404231043864,"score_spread":0.28042801282785335,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389774986","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99586594,0.00027930998,0.00022242236,0.0006484679,0.000015957741,0.000007326576,0.0015735073,0.000019112764,0.0013679287],"genre_scores_gemma":[0.99869174,0.000109581095,0.0001227833,0.000067926136,0.000012097745,0.000008098359,0.00078539544,0.000002101008,0.00020023732],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991596,0.000013497099,0.0000030500173,0.000025460322,0.00001728737,0.000024734949],"domain_scores_gemma":[0.9998752,0.000012736654,0.000029350665,0.000007426752,0.00003946435,0.00003588325],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025801896,0.00019934044,0.00013122185,0.00023755396,0.000390732,0.000603764,0.00025637232,0.0004075875,0.0013056477],"category_scores_gemma":[0.00033497822,0.00011203597,0.00021661406,0.0006702071,0.00024533065,0.00037666716,0.00043031867,0.00033105165,0.00009631765],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015833814,0.000068826565,0.96850204,0.000111489506,0.0001387811,0.00015996382,0.0012377267,0.007542974,0.0034767734,0.00053569244,0.005271824,0.012795556],"study_design_scores_gemma":[0.000003062964,0.000010106225,0.99464095,0.000009612035,0.000008869018,0.00001328902,0.00067012233,0.0031562764,0.00008450371,0.00011132141,0.0012862269,0.0000056429126],"about_ca_topic_score_codex":0.4385911,"about_ca_topic_score_gemma":0.5307666,"teacher_disagreement_score":0.5614089,"about_ca_system_score_codex":0.0014076608,"about_ca_system_score_gemma":0.0009183629,"threshold_uncertainty_score":0.8720764},"labels":[],"label_agreement":null},{"id":"W4389829632","doi":"10.1029/2023gl105200","title":"Historical Shifts in Seasonality and Timing of Extreme Precipitation","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"HORIZON EUROPE Framework Programme; European Commission","keywords":"Climatology; Precipitation; Seasonality; Flash flood; Climate change; Natural hazard; Environmental science; Geography; Meteorology; Ecology; Flood myth; Geology; Biology","score_opus":0.1356808995031217,"score_gpt":0.34093619030811045,"score_spread":0.20525529080498875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389829632","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9977818,0.000104151004,0.0003844596,0.000013922775,0.0000043421705,0.0000013121007,0.0011735928,0.0000105683785,0.00052577263],"genre_scores_gemma":[0.9989497,0.000032999713,0.000111936155,0.0000017785592,0.0000031393001,0.0000012878429,0.0008364584,0.0000013901017,0.00006138124],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999006,0.000019109128,0.000011538945,0.000031811986,0.000022642476,0.000014253138],"domain_scores_gemma":[0.9996189,0.000087262655,0.00014216459,0.000038901493,0.000077703364,0.000035056735],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038450168,0.00008700344,0.00009245675,0.0007168914,0.00009264464,0.00025042685,0.00007823523,0.00010593526,0.0005871718],"category_scores_gemma":[0.000781164,0.000049320006,0.0001495729,0.0008239967,0.00012028423,0.00021845358,0.00017567085,0.00012130696,0.00013733814],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007181013,0.000011066006,0.980057,0.000028216456,0.000112352165,0.00007516262,0.0001435917,0.0058549554,0.0023182463,0.0002567028,0.00047917114,0.010591713],"study_design_scores_gemma":[8.50039e-7,0.000017723643,0.9966562,0.0000031812,0.000007832424,0.000065508,0.000044669127,0.0021886113,0.0002976518,0.00006733282,0.00064733706,0.0000031807454],"about_ca_topic_score_codex":0.0017361945,"about_ca_topic_score_gemma":0.002556289,"teacher_disagreement_score":0.0017361945,"about_ca_system_score_codex":0.00012393584,"about_ca_system_score_gemma":0.000051131985,"threshold_uncertainty_score":0.0034522414},"labels":[],"label_agreement":null},{"id":"W4389977483","doi":"10.1029/2023gl106492","title":"Reduced Deep Convection and Bottom Water Formation Due To Antarctic Meltwater in a Multi‐Model Ensemble","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":27,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; University of Victoria","funders":"Goddard Institute for Space Studies; Munich-Centre for Advanced Photonics; Australian Research Council; University of Otago; Nederlandse Organisatie voor Wetenschappelijk Onderzoek; National Natural Science Foundation of China; Antarctica New Zealand; National Aeronautics and Space Administration","keywords":"Meltwater; Climatology; Geology; Climate model; Antarctic Bottom Water; Convection; Antarctic ice sheet; Downscaling; Sea ice; Environmental science; Cryosphere; Climate change; Oceanography; Meteorology; Thermohaline circulation; Glacier; Geomorphology","score_opus":0.060176936913677766,"score_gpt":0.3210187710938016,"score_spread":0.26084183418012385,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4389977483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971629,0.00007583301,0.0013054836,0.00013347965,0.000027190494,0.0000055348314,0.00057559507,0.000104193256,0.0006096798],"genre_scores_gemma":[0.9984301,0.00004172985,0.00056293193,0.000032871478,0.000016561795,0.00001088448,0.0007324323,0.000022233919,0.00015031251],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99983597,0.000047129237,0.000011738658,0.000045017074,0.000021634227,0.000038517668],"domain_scores_gemma":[0.9995478,0.00012987504,0.00007062242,0.000103305334,0.000065390464,0.0000829826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007294842,0.0006873024,0.0006226084,0.00036827475,0.00047600784,0.0008590742,0.00084248336,0.0008744398,0.0008482913],"category_scores_gemma":[0.00092908216,0.00041319692,0.0014811575,0.0003935739,0.00044332747,0.0007561193,0.0007429725,0.0007682384,0.00010531823],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024855402,0.00011353756,0.045836255,0.000029150655,0.00074335875,0.000111854424,0.000042071086,0.9431997,0.0054179872,0.00044093505,0.0008187563,0.0029978193],"study_design_scores_gemma":[0.000050904433,0.00006308691,0.018826978,0.0000047703475,0.00011173986,0.000016298609,0.000022148124,0.9790683,0.0012731553,0.00023047182,0.00030907107,0.00002310877],"about_ca_topic_score_codex":0.02600943,"about_ca_topic_score_gemma":0.013074237,"teacher_disagreement_score":0.02600943,"about_ca_system_score_codex":0.00066272303,"about_ca_system_score_gemma":0.0007317087,"threshold_uncertainty_score":0.05171609},"labels":[],"label_agreement":null},{"id":"W4390024488","doi":"10.1029/2023gl105865","title":"The 3‐Week‐Long Transport History and Deep Tropical Origin of the 2021 Extreme Heat Wave in the Pacific Northwest","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Austrian Science Fund","keywords":"Heat wave; Climatology; Latent heat; Advection; Environmental science; Sensible heat; Extreme heat; Diabatic; Precipitation; Atmospheric sciences; Air mass (solar energy); Meteorology; Geology; Climate change; Geography; Oceanography; Physics","score_opus":0.07071187233245646,"score_gpt":0.2766655848304062,"score_spread":0.20595371249794975,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390024488","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989831,0.000053600306,0.000052653293,0.00004359042,0.0000039236015,0.000002162405,0.00046417938,0.000003602182,0.00039314356],"genre_scores_gemma":[0.99902666,0.00005626474,0.00005313101,0.00000871666,0.0000057152984,0.0000039065076,0.00071120716,0.0000019117324,0.00013255943],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999435,0.0000067134774,0.0000029270695,0.0000140862385,0.000013081423,0.000019652829],"domain_scores_gemma":[0.9997334,0.000032319935,0.00007977016,0.000016819316,0.00006717571,0.000070475784],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021439166,0.00013676535,0.00012978629,0.00033747664,0.00040883722,0.0004953121,0.00016019013,0.00023193154,0.0007130376],"category_scores_gemma":[0.00042104337,0.000095652045,0.00016037446,0.00051997375,0.0001842088,0.00024402473,0.00033294436,0.00030852744,0.00013650452],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010003784,0.000033497487,0.9896521,0.000011578852,0.000035258498,0.0001305205,0.0003138231,0.00062132446,0.0027631675,0.000075306125,0.00046480715,0.0057986206],"study_design_scores_gemma":[9.1537845e-7,0.000006251665,0.99917126,0.00000283256,0.0000029047642,0.00001288945,0.00013035015,0.00034123694,0.00009493138,0.000008692972,0.00022622522,0.0000016592886],"about_ca_topic_score_codex":0.11982436,"about_ca_topic_score_gemma":0.12423004,"teacher_disagreement_score":0.11982436,"about_ca_system_score_codex":0.0006487809,"about_ca_system_score_gemma":0.00039070664,"threshold_uncertainty_score":0.23825377},"labels":[],"label_agreement":null},{"id":"W4390090491","doi":"10.1029/2023gl106496","title":"Evaluating Methane Emissions From Decommissioned Unconventional Petroleum Wells in British Columbia, Canada","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ministry of Forests; Government of British Columbia","funders":"British Columbia Oil and Gas Commission","keywords":"Soil water; Methane; Environmental science; Greenhouse gas; Natural gas; Soil gas; Petroleum; Geology; Fossil fuel; Unconventional oil; Earth science; Geochemistry; Hydrology (agriculture); Environmental chemistry; Mining engineering; Soil science; Oceanography; Geotechnical engineering; Waste management; Oil shale; Ecology; Chemistry; Paleontology","score_opus":0.03093122669278486,"score_gpt":0.31024400254617185,"score_spread":0.279312775853387,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390090491","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951422,0.00021227691,0.00032304283,0.00006866562,0.0000047310014,0.00004702296,0.001301142,0.000021897718,0.0028790229],"genre_scores_gemma":[0.99683726,0.00025599467,0.00044203486,0.000039079685,0.0000011343227,0.000013984026,0.0006690428,0.000006811729,0.0017346378],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99960965,0.00001997576,0.000011650069,0.000055307275,0.0001920289,0.00011148993],"domain_scores_gemma":[0.9992256,0.000049874605,0.000063216416,0.000015601994,0.00056807563,0.0000775699],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024154279,0.000655407,0.00025085793,0.00090347993,0.0018816484,0.0010849884,0.0007405035,0.00040910018,0.0010208494],"category_scores_gemma":[0.00048605754,0.00027725167,0.00021954523,0.0019625318,0.0005144395,0.00036213236,0.00045126738,0.00046702343,0.00010645029],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007118098,0.0002836305,0.89865303,0.000255721,0.00020199183,0.0016618556,0.0015136153,0.015346283,0.044761173,0.00043157596,0.0020534473,0.034125816],"study_design_scores_gemma":[0.000042487944,0.0002172193,0.9489719,0.000079747064,0.00009961256,0.00018522819,0.006934088,0.015436495,0.021037687,0.00012809144,0.0067998734,0.00006746239],"about_ca_topic_score_codex":0.9917464,"about_ca_topic_score_gemma":0.9965174,"teacher_disagreement_score":0.023396472,"about_ca_system_score_codex":0.023396472,"about_ca_system_score_gemma":0.013249671,"threshold_uncertainty_score":0.16975409},"labels":[],"label_agreement":null},{"id":"W4390236827","doi":"10.1029/2023gl104928","title":"The Capability of Deep Learning Model to Predict Ozone Across Continents in China, the United States and Europe","year":2023,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"University of Science and Technology of China; National Natural Science Foundation of China; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"China; Ozone; Climatology; Environmental science; Atmospheric sciences; Deep learning; Meteorology; Geology; Geography; Computer science; Artificial intelligence","score_opus":0.025721146159594362,"score_gpt":0.29272511603727397,"score_spread":0.2670039698776796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390236827","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9940334,0.00013813254,0.0038202046,0.00033754786,0.00002966643,0.000008829263,0.00045326547,0.00020802443,0.00097095146],"genre_scores_gemma":[0.9982827,0.000026379905,0.00095456396,0.000039570874,0.0000047492863,0.000003683256,0.00046723947,0.000006937474,0.00021434328],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998217,0.000043637207,0.000012179935,0.000060339204,0.00002424539,0.000037978996],"domain_scores_gemma":[0.99951804,0.00017117902,0.000050540282,0.000059425398,0.00014223826,0.00005858472],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0013948027,0.00070410565,0.00033225247,0.0004572257,0.00029832116,0.0006450056,0.0005893478,0.0005652283,0.00059756485],"category_scores_gemma":[0.0016244929,0.00026660317,0.00061027874,0.00037284291,0.0003929658,0.00073349423,0.00063284644,0.00051490776,0.00012293184],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011660562,0.00008899495,0.072026335,0.000016064228,0.00012969352,0.000044499404,0.000021612288,0.9150946,0.0013204701,0.00023943407,0.000674444,0.0102271605],"study_design_scores_gemma":[0.000014964806,0.000018505276,0.007353593,0.0000030031683,0.000013792564,0.0000026911625,0.000015713957,0.9914561,0.0007378091,0.00024333438,0.00013480854,0.000005786749],"about_ca_topic_score_codex":0.120363116,"about_ca_topic_score_gemma":0.061531007,"teacher_disagreement_score":0.120363116,"about_ca_system_score_codex":0.0013199075,"about_ca_system_score_gemma":0.001322642,"threshold_uncertainty_score":0.23932505},"labels":[],"label_agreement":null},{"id":"W4390544528","doi":"10.1029/2023gl105893","title":"Morphometry of Tidal Meander Cutoffs Indicates Similarity to Fluvial Morphodynamics","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Okanagan University College; University of British Columbia, Okanagan Campus; University of British Columbia","funders":"Ministero dell’Istruzione, dell’Università e della Ricerca; China Scholarship Council; Università degli Studi di Padova; Natural Sciences and Engineering Research Council of Canada; European Commission; Dipartimenti di Eccellenza","keywords":"Meander (mathematics); Beach morphodynamics; Fluvial; Geology; Wetland; Channel (broadcasting); Ephemeral key; Oceanography; Geomorphology; Ecology; Sediment transport; Sediment; Geometry","score_opus":0.021624437455553737,"score_gpt":0.30441495198503166,"score_spread":0.2827905145294779,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390544528","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995865,0.0000061418586,0.00011791401,0.0000019549848,3.5169248e-7,0.0000011430449,0.00004286157,0.0000050376834,0.00023807182],"genre_scores_gemma":[0.99978215,0.000002613085,0.00008425418,0.0000012884847,3.8815378e-7,0.0000015235042,0.00005820059,0.0000013042586,0.00006835825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992275,0.000013241169,0.00000613003,0.00002291841,0.000012638463,0.0000224181],"domain_scores_gemma":[0.9991774,0.0002033543,0.00031621516,0.000074577714,0.000090005095,0.00013831211],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014896896,0.0000834447,0.00013324672,0.0009991426,0.00022318366,0.000527212,0.00012285814,0.00015085137,0.0015042789],"category_scores_gemma":[0.00089812715,0.000076912744,0.00008555845,0.00047046592,0.00040165253,0.00024699184,0.00034217534,0.00013497655,0.00015695841],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000055423392,0.000014263147,0.987703,0.0000045328857,0.000011596364,0.00005220806,0.00027584343,0.0001431648,0.008779468,0.00008433595,0.000054600987,0.0028214583],"study_design_scores_gemma":[4.88152e-7,0.0000120195045,0.99936384,7.221103e-7,0.0000011846444,0.000044808345,0.00014344057,0.00024483932,0.000121998055,0.000029666342,0.000035848072,0.0000011602741],"about_ca_topic_score_codex":0.0030459317,"about_ca_topic_score_gemma":0.0071244603,"teacher_disagreement_score":0.0030459317,"about_ca_system_score_codex":0.0001623624,"about_ca_system_score_gemma":0.00009619135,"threshold_uncertainty_score":0.006056428},"labels":[],"label_agreement":null},{"id":"W4390589148","doi":"10.1029/2023gl106433","title":"The Cause of Negative CO <sub>2</sub> Forcing at the Top‐Of‐Atmosphere: The Role of Stratospheric Versus Tropospheric Temperature Inversions","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; McGill University; National Oceanic and Atmospheric Administration; U.S. Department of Commerce","keywords":"Forcing (mathematics); Atmospheric sciences; Stratosphere; Climatology; Cloud forcing; Environmental science; Radiative forcing; Atmosphere (unit); Troposphere; The arctic; Climate change; Geology; Meteorology; Physics","score_opus":0.010598235803057979,"score_gpt":0.2561825896659493,"score_spread":0.24558435386289135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390589148","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9973055,0.00022796585,0.00033285478,0.00019479959,0.000012793282,0.0000021992976,0.00008661467,0.000021838217,0.0018153968],"genre_scores_gemma":[0.99980766,0.0000463012,0.000039913823,0.000011602212,0.0000063319226,4.5057845e-7,0.000020491047,0.0000034957195,0.00006371535],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999548,0.0000063831512,0.0000017233348,0.000009711586,0.000006588513,0.000020831156],"domain_scores_gemma":[0.9998486,0.000039466006,0.000041511288,0.00001226835,0.000022318123,0.00003582082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012447721,0.00025428922,0.00022013782,0.00026296012,0.00025437507,0.00048427863,0.00018632771,0.00037288415,0.001060508],"category_scores_gemma":[0.00026356304,0.00013211402,0.00017906706,0.00015224367,0.0004617663,0.00025501102,0.00029809398,0.00026321146,0.00015362626],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055395224,0.000076528304,0.3668485,0.00014852402,0.0001573938,0.0013053939,0.00017549106,0.0066272826,0.60916257,0.0025574889,0.001045458,0.011341453],"study_design_scores_gemma":[0.000026198255,0.000063491054,0.9449006,0.000009807458,0.00007553748,0.0003444571,0.00024975138,0.016902577,0.034940854,0.0015722672,0.00089148164,0.000023122062],"about_ca_topic_score_codex":0.0034539173,"about_ca_topic_score_gemma":0.0023415845,"teacher_disagreement_score":0.0034539173,"about_ca_system_score_codex":0.00019311186,"about_ca_system_score_gemma":0.00019069567,"threshold_uncertainty_score":0.0068675876},"labels":[],"label_agreement":null},{"id":"W4390827241","doi":"10.1029/2023gl105581","title":"Pollen in Polar Ice Implies Eastern Canadian Forest Dynamics Diverged From Climate After European Settlement","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Science Foundation","keywords":"Biome; Pollen; Taiga; Climate change; Vegetation (pathology); Boreal; Physical geography; Geography; Ecology; Ice core; Climatology; Ice age; Geology; Ecosystem; Forestry; Biology; Glacial period; Paleontology","score_opus":0.02002591808856986,"score_gpt":0.26730463723829745,"score_spread":0.2472787191497276,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390827241","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964271,0.00018577026,0.000052616284,0.00006325598,0.000003691024,0.0000015561095,0.0006857443,0.000003281231,0.0025770022],"genre_scores_gemma":[0.9991072,0.00008053394,0.00004271854,0.000012530969,0.0000014681664,7.978264e-7,0.0002954139,0.0000014846398,0.00045788608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.0000034320014,0.0000018527047,0.000017311411,0.000009729416,0.000028534125],"domain_scores_gemma":[0.99974567,0.000023121442,0.000038175567,0.000012113897,0.00013544188,0.000045560115],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019064912,0.00013001285,0.000088408655,0.0005767585,0.0009860543,0.00074824755,0.00021813242,0.00012122763,0.0014097857],"category_scores_gemma":[0.0004878973,0.00006888205,0.00010174241,0.00076938316,0.00042528333,0.00020427832,0.00028988213,0.00021440741,0.00008009778],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012582836,0.000008219191,0.9869594,0.000016093145,0.000043010194,0.00008981156,0.00072034803,0.0006377264,0.002265066,0.00061855227,0.0005182261,0.007997619],"study_design_scores_gemma":[0.0000012213318,0.000002204357,0.99836916,0.000004457615,0.000005336598,0.000014040487,0.00025038936,0.0001327779,0.00013411339,0.000031368607,0.0010533269,0.0000016744729],"about_ca_topic_score_codex":0.90221167,"about_ca_topic_score_gemma":0.9648013,"teacher_disagreement_score":0.097788334,"about_ca_system_score_codex":0.0042261938,"about_ca_system_score_gemma":0.002895229,"threshold_uncertainty_score":0.19672841},"labels":[],"label_agreement":null},{"id":"W4390839013","doi":"10.1029/2023gl104851","title":"Vertical Land Motion Due To Present‐Day Ice Loss From Greenland's and Canada's Peripheral Glaciers","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Vetenskapsrådet; Sun Yat-sen University; Fundamental Research Funds for the Central Universities; Villum Fonden","keywords":"Glacier; Geology; Greenland ice sheet; Climatology; Ice core; Ice sheet; Ice caps; Future sea level; Groenlandia; Motion (physics); Physical geography; Glaciology; Cryosphere; Geodesy; Ice stream; Geomorphology; Seismology; Sea ice; Geography; Tectonics","score_opus":0.023635915298993386,"score_gpt":0.2615687463386243,"score_spread":0.23793283103963092,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4390839013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9978756,0.000071763585,0.000023766239,0.000059571656,0.0000032309676,0.0000024674414,0.00086027157,0.0000055785667,0.0010976918],"genre_scores_gemma":[0.9986041,0.00005067522,0.000029434512,0.000015160955,0.000001608271,0.0000011337754,0.0009564977,0.0000019757183,0.0003394188],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986887,0.000008454906,0.0000045391007,0.000019866575,0.000040433686,0.000057836733],"domain_scores_gemma":[0.99960786,0.000031397703,0.000055159424,0.000015903634,0.00016756411,0.00012211224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001840585,0.00023635317,0.00016066985,0.000790477,0.0006758448,0.00060128834,0.00032857174,0.00017752511,0.0012796591],"category_scores_gemma":[0.00060108386,0.00010962894,0.00018641604,0.0013876198,0.00037201372,0.00019647692,0.00044878677,0.00019063368,0.000111287656],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016832454,0.000022252692,0.9862721,0.000019372343,0.00006519468,0.00013004681,0.00025835406,0.0022952743,0.0019553036,0.00013959466,0.0011327529,0.0075415163],"study_design_scores_gemma":[0.000002305449,0.0000031060538,0.99883157,0.0000039821484,0.0000064013443,0.000009948761,0.00019552924,0.0006040784,0.000097180615,0.000011902339,0.00023158567,0.0000024447306],"about_ca_topic_score_codex":0.9504584,"about_ca_topic_score_gemma":0.97360826,"teacher_disagreement_score":0.049541593,"about_ca_system_score_codex":0.006041305,"about_ca_system_score_gemma":0.0035056532,"threshold_uncertainty_score":0.099666655},"labels":[],"label_agreement":null},{"id":"W4391026640","doi":"10.1029/2023gl106654","title":"Large Igneous Province Emplacement Triggered an Oxygenation Event at ∼1.4 Ga: Evidence From Mercury and Paleo‐Productivity Proxies","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Natural Science Foundation of China","keywords":"Geology; Proterozoic; Weathering; Pyrite; Igneous rock; Trace element; Total organic carbon; Geochemistry; Paleontology; Environmental chemistry; Chemistry; Tectonics","score_opus":0.044784185240658234,"score_gpt":0.3176602720797964,"score_spread":0.27287608683913817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391026640","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990502,0.00009660507,0.00009636336,0.000021336036,0.0000026918456,0.0000019820486,0.0001142436,0.0000120088125,0.0006045086],"genre_scores_gemma":[0.9995449,0.000043706954,0.0000732358,0.000007834506,0.0000023791708,0.0000014318758,0.00010462718,0.0000033806002,0.00021842976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994326,0.0000033764302,0.000003347472,0.000024293935,0.000011627955,0.000014100051],"domain_scores_gemma":[0.999864,0.000013675246,0.000046881625,0.000010533482,0.000041170348,0.000023846073],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017050724,0.00021593996,0.00017258867,0.0007980555,0.00051758764,0.00042919436,0.0002203936,0.00024288017,0.0011446615],"category_scores_gemma":[0.00025857677,0.00016450608,0.00013851997,0.0005136825,0.00041162517,0.00023776967,0.00046049833,0.00020409044,0.00013928369],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010442523,0.000016871149,0.90912884,0.00004449082,0.00006568698,0.00051878975,0.0006929319,0.0003911449,0.08267792,0.00017775278,0.00013277274,0.006048366],"study_design_scores_gemma":[0.0000021354538,0.0000102095455,0.99747986,0.0000027373683,0.000011861071,0.000050265462,0.00014061567,0.00027031067,0.0016345114,0.000023802942,0.00037129567,0.0000022575202],"about_ca_topic_score_codex":0.023685347,"about_ca_topic_score_gemma":0.03429316,"teacher_disagreement_score":0.023685347,"about_ca_system_score_codex":0.0005610719,"about_ca_system_score_gemma":0.00031582417,"threshold_uncertainty_score":0.04709494},"labels":[],"label_agreement":null},{"id":"W4391027489","doi":"10.1029/2023gl105324","title":"Land and Atmosphere Precursors to Fuel Loading, Wildfire Ignition and Post‐Fire Recovery","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":19,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"United Nations University Institute for Water, Environment, and Health; McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; California Institute of Technology; Jet Propulsion Laboratory; Massachusetts Institute of Technology; National Aeronautics and Space Administration","keywords":"Environmental science; Dryness; Vegetation (pathology); Water content; Atmosphere (unit); Moisture; Fire regime; Ignition system; Atmospheric sciences; Meteorology; Ecology; Geology; Ecosystem; Geography","score_opus":0.011307127076122582,"score_gpt":0.2644586433759252,"score_spread":0.2531515162998026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391027489","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99949515,0.000025063959,0.0000874051,0.000018494897,0.0000014580003,0.0000012130608,0.000121073106,0.0000055581877,0.00024459514],"genre_scores_gemma":[0.99976605,0.000011415206,0.000035710287,0.0000033418999,0.0000016444145,0.0000010010948,0.00010806181,0.0000011646431,0.000071645394],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.0000067625156,0.0000031550903,0.000011931525,0.000008099539,0.000015758595],"domain_scores_gemma":[0.99944,0.00014392303,0.0002139783,0.000039007013,0.000055154524,0.000107886655],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021172117,0.00012709199,0.0001611077,0.00031841337,0.00016146187,0.00044784017,0.00014975699,0.00018187588,0.0019347748],"category_scores_gemma":[0.000931092,0.0000977882,0.00013262079,0.00031305247,0.00016676389,0.00026873586,0.00034051243,0.0003015501,0.00013632148],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019625186,0.00010463921,0.9865145,0.000011091313,0.000035569086,0.00008016176,0.00010263194,0.0017874374,0.004655207,0.00015240547,0.00015168104,0.0062083364],"study_design_scores_gemma":[0.0000010878381,0.000014045011,0.9978911,0.0000014630087,0.0000036841473,0.000014581122,0.00006583597,0.0016635783,0.0002318434,0.00006431376,0.000046744077,0.0000017702137],"about_ca_topic_score_codex":0.012996216,"about_ca_topic_score_gemma":0.022850472,"teacher_disagreement_score":0.012996216,"about_ca_system_score_codex":0.00020929636,"about_ca_system_score_gemma":0.00019688482,"threshold_uncertainty_score":0.025841177},"labels":[],"label_agreement":null},{"id":"W4391035137","doi":"10.1029/2023gl106646","title":"Apatite Textures, Elemental and Isotopic Compositions Unmask the Homogenizing Process in Silicic Magma Chambers","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Institute of Geochemistry, Chinese Academy of Sciences; Guangzhou Institute of Geochemistry, Chinese Academy of Sciences; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou); National Natural Science Foundation of China","keywords":"Silicic; Pluton; Geology; Magma chamber; Magma; Geochemistry; Apatite; Igneous differentiation; Texture (cosmology); Homogeneous; Fractional crystallization (geology); Crystallization; Precipitation; Mineralogy; Igneous rock; Volcano; Chemistry; Paleontology","score_opus":0.021307003062268813,"score_gpt":0.28644658389774547,"score_spread":0.2651395808354767,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391035137","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993093,0.00005864039,0.00022624245,0.0000047965004,0.000001005518,0.0000018500799,0.00003599987,0.000006314707,0.00035592492],"genre_scores_gemma":[0.9995635,0.000024194924,0.00017407707,0.0000032506496,0.000001336547,0.00000119432,0.0000418054,0.00000294973,0.00018766262],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999447,0.0000025664772,0.0000048211573,0.000024731675,0.000012972362,0.0000102082195],"domain_scores_gemma":[0.99992454,0.0000109223965,0.000021489666,0.000012229797,0.000017623575,0.000013162843],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000078784295,0.0001718186,0.00017550828,0.0005844588,0.00024226311,0.00035990166,0.00015442492,0.00017081821,0.0006479958],"category_scores_gemma":[0.00013697677,0.00016883844,0.00013917482,0.00035536662,0.00039708192,0.00028718493,0.0002495533,0.00013744216,0.00009003141],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008693734,0.0000052570617,0.065669805,0.000028945073,0.000016433638,0.00016179807,0.00019621382,0.00014966559,0.9302615,0.00011674479,0.000015719104,0.0032909275],"study_design_scores_gemma":[0.0000104740075,0.000056326375,0.83289236,0.0000042723677,0.000027477921,0.0005473668,0.00039598407,0.0014036987,0.16333784,0.00022419031,0.0010901417,0.000009892627],"about_ca_topic_score_codex":0.002399689,"about_ca_topic_score_gemma":0.0032262802,"teacher_disagreement_score":0.002399689,"about_ca_system_score_codex":0.00022568667,"about_ca_system_score_gemma":0.00018266246,"threshold_uncertainty_score":0.0047714114},"labels":[],"label_agreement":null},{"id":"W4391109076","doi":"10.1029/2023gl105452","title":"Syn‐Drift Plate Tectonics","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"The Scarborough Hospital; University of Toronto","funders":"Alliance de recherche numérique du Canada","keywords":"Subduction; Geology; Plate tectonics; Lithosphere; Convergent boundary; Seismology; Tectonics; Pacific Plate; Oceanic crust; North American Plate; Eurasian Plate; Slab; Geodynamics; Geophysics; Pacific ocean; Oceanography","score_opus":0.031622635293163795,"score_gpt":0.27916891254476445,"score_spread":0.24754627725160067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391109076","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8147766,0.004039561,0.0105753355,0.0012229476,0.00014664633,0.00007169417,0.001621215,0.00013719757,0.16740885],"genre_scores_gemma":[0.98640025,0.0016059552,0.0013607142,0.00008482024,0.000031375406,0.000015035776,0.00058981153,0.000012771705,0.009899308],"study_design_codex":"observational","study_design_gemma":"theoretical_or_conceptual","domain_scores_codex":[0.99989986,0.000010514028,0.000008027186,0.000025868889,0.000039480456,0.000016328502],"domain_scores_gemma":[0.9998123,0.000013407747,0.00006912069,0.000023405368,0.000066695146,0.0000150288015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021772683,0.00029712447,0.00011637698,0.00081860495,0.00036145202,0.0007090998,0.00021221593,0.00017140395,0.0037639707],"category_scores_gemma":[0.0004093204,0.00008125281,0.000120791694,0.0011970556,0.0007027123,0.00045427715,0.00059362076,0.00033925552,0.00043793244],"study_design_candidate":"theoretical_or_conceptual","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026265378,0.000053587162,0.560439,0.0005834718,0.00017927407,0.0009162701,0.002270216,0.022463098,0.022888295,0.16804105,0.0067537553,0.2151494],"study_design_scores_gemma":[0.000030772873,0.00011396583,0.8628805,0.00013152134,0.00007085665,0.0011266533,0.0016061394,0.017708305,0.0056444816,0.035748288,0.074906625,0.00003178055],"about_ca_topic_score_codex":0.0126339095,"about_ca_topic_score_gemma":0.011031421,"teacher_disagreement_score":0.0126339095,"about_ca_system_score_codex":0.0008038683,"about_ca_system_score_gemma":0.0007561414,"threshold_uncertainty_score":0.025120735},"labels":[],"label_agreement":null},{"id":"W4391448910","doi":"10.1029/2023gl105914","title":"Growth Increments of Coralline Red Alga <i>Clathromorphum Compactum</i> Capture Sea‐Ice Variability Links to Arctic and Atlantic Multidecadal Oscillations (1805–2015)","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Toronto; College of Family Physicians of Canada; Memorial University of Newfoundland","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto; Deutsche Forschungsgemeinschaft","keywords":"Atlantic multidecadal oscillation; Oceanography; Sea ice; North Atlantic oscillation; Climatology; Arctic ice pack; Geology; Arctic; Arctic sea ice decline; Arctic oscillation; Ice core; Pacific decadal oscillation; Environmental science; Antarctic sea ice; Sea surface temperature; The arctic","score_opus":0.02484523214537275,"score_gpt":0.2901330683718996,"score_spread":0.26528783622652685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391448910","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948086,0.00018119719,0.00014565658,0.000031179214,0.00000543229,0.0000024419396,0.002214226,0.000019674462,0.0025916712],"genre_scores_gemma":[0.99797016,0.00006439717,0.00014679284,0.000014006449,0.0000039737124,0.0000023472153,0.0013896603,0.0000050930867,0.00040348325],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999417,0.0000031182665,0.0000034168443,0.000022459806,0.000012122988,0.000017045752],"domain_scores_gemma":[0.99960357,0.000022295893,0.00014845944,0.00003059876,0.00013985285,0.000055228615],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017528786,0.00012250473,0.00009075081,0.0008924459,0.00034804622,0.00047671737,0.00020661151,0.00011887534,0.0015217338],"category_scores_gemma":[0.00043184758,0.000082960636,0.00015297461,0.0008344181,0.00016446876,0.00022378327,0.00038187773,0.00013394264,0.00024855667],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000062411935,0.000010263228,0.9814022,0.000027967233,0.000051609928,0.000029551937,0.00021473787,0.00035744277,0.0068300683,0.00013547289,0.000935959,0.009942369],"study_design_scores_gemma":[3.8660647e-7,0.0000017648767,0.99915755,0.0000024247024,0.0000029958587,0.000008291988,0.00005223508,0.00011234428,0.00014954864,0.0000059115605,0.00050545356,0.0000010303294],"about_ca_topic_score_codex":0.20673324,"about_ca_topic_score_gemma":0.40627882,"teacher_disagreement_score":0.20673324,"about_ca_system_score_codex":0.00079280953,"about_ca_system_score_gemma":0.00042174893,"threshold_uncertainty_score":0.4110598},"labels":[],"label_agreement":null},{"id":"W4391449074","doi":"10.1029/2023gl105605","title":"Constraining Projected Changes in Rare Intense Precipitation Events Across Global Land Regions","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":20,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria; Environment and Climate Change Canada","funders":"National Natural Science Foundation of China","keywords":"Precipitation; Climatology; Environmental science; Constraint (computer-aided design); Climate model; Global warming; Climate change; Greenhouse gas; Atmospheric sciences; Meteorology; Geography; Ecology; Geology; Mathematics","score_opus":0.07497729002466133,"score_gpt":0.3777293620307661,"score_spread":0.30275207200610477,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391449074","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9710107,0.00008930664,0.023581633,0.0003001518,0.000020130408,0.000025303378,0.00252209,0.00014813755,0.002302571],"genre_scores_gemma":[0.99601823,0.00003477948,0.0028123534,0.000021143682,0.0000057756115,0.00002019038,0.0009842915,0.000014065455,0.00008920843],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9996257,0.00017904573,0.000017867174,0.000103166,0.000035895857,0.000038400132],"domain_scores_gemma":[0.998738,0.0006652257,0.0002097672,0.0001592764,0.00015562121,0.00007211779],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0015563901,0.00042039723,0.00028166405,0.00036769733,0.00023926288,0.0007074273,0.0005075284,0.00041594636,0.0011015707],"category_scores_gemma":[0.003891631,0.00030658106,0.00048098285,0.0005228417,0.00027294562,0.0007530966,0.000638344,0.0006567558,0.00015136028],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000047119243,0.000023223192,0.02496909,0.000016287391,0.000060345796,0.000021615473,0.00002069013,0.9701086,0.0006996197,0.00067386444,0.00021967795,0.003139751],"study_design_scores_gemma":[0.000034244527,0.000052240375,0.05821936,0.000023608685,0.000033043187,0.000018938857,0.00006269802,0.93548167,0.002098854,0.0027646967,0.0011757695,0.000034820303],"about_ca_topic_score_codex":0.022524158,"about_ca_topic_score_gemma":0.024085263,"teacher_disagreement_score":0.022524158,"about_ca_system_score_codex":0.00068543584,"about_ca_system_score_gemma":0.00081142277,"threshold_uncertainty_score":0.044786096},"labels":[],"label_agreement":null},{"id":"W4391611031","doi":"10.1029/2023gl106095","title":"Capturing the Relative‐Humidity‐Sensitive Gas–Particle Partitioning of Organic Aerosols in a 2D Volatility Basis Set","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Alfred P. Sloan Foundation; Environment and Climate Change Canada; U.S. Department of Energy","keywords":"Volatility (finance); Relative humidity; Environmental science; Aerosol; Atmospheric sciences; Particle (ecology); Humidity; Meteorology; Geology; Physics; Econometrics; Mathematics; Oceanography","score_opus":0.04033008702640944,"score_gpt":0.2856200289980487,"score_spread":0.24528994197163928,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391611031","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8072741,0.00022304582,0.18395396,0.00027340214,0.000053293217,0.00006145963,0.0008408386,0.00039177804,0.0069281594],"genre_scores_gemma":[0.98156595,0.00010746875,0.016570095,0.00005665685,0.00001547998,0.000052153733,0.0004009777,0.00004983678,0.0011814137],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99990714,0.000032911918,0.000003843306,0.000008518732,0.000028333396,0.000019202515],"domain_scores_gemma":[0.99977475,0.000102585705,0.000021226364,0.00003765882,0.000035399902,0.000028359973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003005516,0.00042825725,0.00036388915,0.0002480633,0.00023423096,0.0005341725,0.0006587298,0.0005519628,0.0011282015],"category_scores_gemma":[0.0005940967,0.00025262256,0.00054807134,0.00029483877,0.00032257487,0.0004438319,0.00035341486,0.0004946964,0.00018463944],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000036159192,0.00004314436,0.0013073332,0.0000282301,0.000022299246,0.000031990083,0.000013173554,0.9872153,0.004959038,0.003610308,0.0001802191,0.0025528932],"study_design_scores_gemma":[0.0000028829268,0.0000046617774,0.00019280681,0.0000010269789,0.0000010303487,0.0000024344934,0.0000020209834,0.9990409,0.00038445843,0.00029561215,0.00006988603,0.0000022001134],"about_ca_topic_score_codex":0.011147341,"about_ca_topic_score_gemma":0.0057434733,"teacher_disagreement_score":0.011147341,"about_ca_system_score_codex":0.0003519902,"about_ca_system_score_gemma":0.00066743407,"threshold_uncertainty_score":0.02216494},"labels":[],"label_agreement":null},{"id":"W4391611562","doi":"10.1029/2023gl106694","title":"Climate Variability Leads to Multiple Oxygenation Episodes Across the Great Oxidation Event","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Glacial period; Climate change; Sedimentary rock; Geology; Paleoclimatology; Atmospheric sciences; Geologic record; Ice core; Climatology; Environmental science; Paleontology; Oceanography","score_opus":0.037448934234616774,"score_gpt":0.34075528881798683,"score_spread":0.3033063545833701,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391611562","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997092,0.000010452045,0.00004918246,0.000036808677,0.0000012363432,7.011348e-7,0.000046952304,0.0000056016347,0.00013993528],"genre_scores_gemma":[0.9998579,0.0000071408813,0.000019943522,0.0000048473203,0.0000011035374,6.41525e-7,0.00006958743,0.0000010339919,0.000037841608],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999192,0.000021655433,0.0000034476366,0.00002753732,0.000007754942,0.000020423133],"domain_scores_gemma":[0.9995609,0.00015361681,0.00012738389,0.000036506575,0.0000370022,0.00008454119],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027830998,0.000107861175,0.00015638625,0.0002604674,0.0002265391,0.00044528994,0.0001612411,0.00027694152,0.0009471604],"category_scores_gemma":[0.0009792388,0.00014948107,0.00023867616,0.00026999376,0.00025079673,0.00016150267,0.000489961,0.00027424254,0.00006871411],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00045359225,0.00007999746,0.97239774,0.000014496911,0.00018022755,0.00023867439,0.00032502398,0.0095855715,0.0107696215,0.00043547637,0.0004553897,0.0050641773],"study_design_scores_gemma":[0.000008922481,0.000031964093,0.989447,0.000002031745,0.000019335337,0.000028092934,0.00012836768,0.009641599,0.0003162403,0.00023386715,0.00013662518,0.0000059901217],"about_ca_topic_score_codex":0.0077509186,"about_ca_topic_score_gemma":0.010183357,"teacher_disagreement_score":0.0077509186,"about_ca_system_score_codex":0.0002999287,"about_ca_system_score_gemma":0.00013734403,"threshold_uncertainty_score":0.015411615},"labels":[],"label_agreement":null},{"id":"W4391749222","doi":"10.1029/2023gl107512","title":"Marine Aluminum Phosphate–Sulfate Authigenesis as a Phosphorus Sink During Mid‐Proterozoic Oxygenation","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fundamental Research Funds for the Central Universities; China University of Geosciences; China University of Geosciences, Beijing; National Natural Science Foundation of China","keywords":"Authigenic; Proterozoic; Geology; Diagenesis; Sink (geography); Geochemistry; Sulfate; Phosphorus; Biogeochemical cycle; Phosphate; White Phosphorus; Environmental chemistry; Paleontology; Chemistry; Tectonics","score_opus":0.024115369741840257,"score_gpt":0.2796198643001519,"score_spread":0.25550449455831165,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391749222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997341,0.000033067667,0.00003433555,0.000009936112,5.444802e-7,0.000001012332,0.00002635605,0.0000040827567,0.00015653846],"genre_scores_gemma":[0.99973196,0.000028402066,0.000042684882,0.00000382447,9.653409e-7,9.334934e-7,0.000046398516,0.0000010090025,0.00014385679],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999689,0.000002473976,0.0000020294863,0.0000090324775,0.000007165634,0.000010419147],"domain_scores_gemma":[0.9999372,0.0000061380515,0.000019329576,0.0000035114465,0.0000187531,0.000015183553],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012658087,0.00017116092,0.00018780638,0.00062715006,0.00046270018,0.0003487334,0.00019115607,0.00021693979,0.00049068197],"category_scores_gemma":[0.00013886119,0.00017802924,0.000081088336,0.00030720836,0.000297848,0.0002775746,0.0003429428,0.00014517877,0.00009488313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00028576024,0.000021755952,0.4986789,0.00006233586,0.000030138764,0.00067537866,0.0007780648,0.0007423822,0.49174067,0.00035825573,0.00008009741,0.0065462976],"study_design_scores_gemma":[0.000004895735,0.000040633837,0.98934656,0.000003227497,0.0000071706295,0.00011426916,0.000284107,0.00069865957,0.008953211,0.000088582485,0.0004548609,0.0000037447514],"about_ca_topic_score_codex":0.011740716,"about_ca_topic_score_gemma":0.018342301,"teacher_disagreement_score":0.011740716,"about_ca_system_score_codex":0.0006094629,"about_ca_system_score_gemma":0.00037739825,"threshold_uncertainty_score":0.023344755},"labels":[],"label_agreement":null},{"id":"W4391754907","doi":"10.1029/2023gl107273","title":"Airborne Observations Constrain Heterogeneous Nitrogen and Halogen Chemistry on Tropospheric and Stratospheric Biomass Burning Aerosol","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Aerosol; Troposphere; Biomass burning; Environmental science; Atmospheric sciences; Atmospheric chemistry; Stratosphere; Nitrogen; Halogen; Astrobiology; Environmental chemistry; Climatology; Meteorology; Chemistry; Ozone; Geology; Physics","score_opus":0.031617401770976536,"score_gpt":0.2648076411141347,"score_spread":0.23319023934315813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4391754907","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996327,0.000013304976,0.00009459096,0.0000019671327,4.296058e-7,0.0000019003821,0.000073125746,0.0000035799476,0.00017843419],"genre_scores_gemma":[0.9996661,0.0000119546075,0.00013309921,0.000003500335,8.73193e-7,0.0000017318399,0.0001489485,0.0000015850435,0.000032223892],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992883,0.000008055379,0.0000021211672,0.000027908036,0.000017332792,0.000015798734],"domain_scores_gemma":[0.99991727,0.000025684598,0.000016546888,0.000009618634,0.00001584306,0.00001496112],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017775684,0.00036243576,0.00012558563,0.00027847665,0.00025270807,0.0002773175,0.0001872719,0.00020036985,0.0003423486],"category_scores_gemma":[0.00017351023,0.00017907149,0.00013287104,0.00017981681,0.00019103508,0.00021461479,0.0001959839,0.00015022236,0.000059661685],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032597655,0.00014853159,0.67960197,0.000029857954,0.00010908564,0.00008548213,0.00021302499,0.005083681,0.3062805,0.00012121326,0.00010294232,0.007897685],"study_design_scores_gemma":[0.00002222277,0.000080587735,0.9728046,0.0000036018232,0.000026975958,0.000023225828,0.00009331025,0.009947387,0.016700462,0.000054832195,0.0002367363,0.000006074493],"about_ca_topic_score_codex":0.033731263,"about_ca_topic_score_gemma":0.048259214,"teacher_disagreement_score":0.033731263,"about_ca_system_score_codex":0.00043833716,"about_ca_system_score_gemma":0.0001610309,"threshold_uncertainty_score":0.06706983},"labels":[],"label_agreement":null},{"id":"W4392015049","doi":"10.1029/2023gl106416","title":"Basin‐Wide Shift in Bowhead Whale Migration in the Pacific Arctic","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine animal studies overview","field":"Environmental Science","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Marine Fisheries Service; Office of Polar Programs; Office of Naval Research; Office of Science; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Oceanography; Whale; Arctic; Beaufort sea; Beaufort scale; Geology; Canada Basin; The arctic; Overwintering; Geography; Fishery; Ecology","score_opus":0.03676739240902505,"score_gpt":0.3095685967508568,"score_spread":0.27280120434183175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392015049","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983016,0.00022581631,0.000047636084,0.00011315269,0.000015691194,0.0000013028017,0.00024187149,0.0000045216075,0.0010483077],"genre_scores_gemma":[0.9991135,0.00024181367,0.000058108275,0.00004097382,0.000010053215,0.0000023026296,0.00025047618,0.0000017878392,0.00028097117],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998883,0.00002093043,0.000007507447,0.000034275152,0.000019846035,0.000029171226],"domain_scores_gemma":[0.9996425,0.000043809792,0.000080509795,0.000021554837,0.00013285081,0.00007872815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00042382188,0.00007958113,0.000113230824,0.00076310284,0.00044612182,0.0006504116,0.00014490465,0.00023180155,0.0008593799],"category_scores_gemma":[0.00044269484,0.000080003585,0.00014947908,0.0010494551,0.00028939365,0.0002725909,0.0003419024,0.00018603534,0.00009347417],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000077497796,0.000014241979,0.9871547,0.000025193776,0.00005905271,0.00009875519,0.000703974,0.00021940867,0.0013606035,0.000076224016,0.0005142318,0.009696117],"study_design_scores_gemma":[4.86007e-7,0.000007925551,0.99878854,0.0000060688835,0.0000057828784,0.000016779319,0.0005371085,0.000050733273,0.000035013487,0.000009118408,0.00054101454,0.0000014139046],"about_ca_topic_score_codex":0.08801998,"about_ca_topic_score_gemma":0.19267054,"teacher_disagreement_score":0.08801998,"about_ca_system_score_codex":0.0004971623,"about_ca_system_score_gemma":0.0006388966,"threshold_uncertainty_score":0.17501527},"labels":[],"label_agreement":null},{"id":"W4392135463","doi":"10.1029/2023gl107261","title":"Arctic Sea Ice Topography Information From RADARSAT Constellation Mission (RCM) Synthetic Aperture Radar (SAR) Backscatter","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Sea ice; Geology; Remote sensing; Synthetic aperture radar; Backscatter (email); Arctic; Sea ice concentration; Sea ice thickness; Satellite; Arctic ice pack; Surface roughness; Altimeter; Geodesy; Climatology; Oceanography; Computer science","score_opus":0.015284957784010286,"score_gpt":0.25117110037901275,"score_spread":0.23588614259500246,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392135463","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9830119,0.00012470987,0.00461016,0.000060980266,0.000010389988,0.000026224858,0.007551319,0.00017848743,0.004425711],"genre_scores_gemma":[0.9932842,0.000060830094,0.0017340808,0.000012610811,0.0000038265466,0.0000066697603,0.0043406365,0.000012547398,0.0005445226],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000011245493,0.000005898567,0.000025269515,0.00004564086,0.00002356564],"domain_scores_gemma":[0.99977237,0.000039996667,0.000039242703,0.00003251721,0.00010262138,0.000013312979],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020499087,0.00023435627,0.00017594745,0.0006162097,0.0002156305,0.00040745075,0.00021137566,0.00013083853,0.0012324237],"category_scores_gemma":[0.00087049394,0.00011815647,0.0002636892,0.00064620236,0.00011875592,0.00023261673,0.000169761,0.00010635613,0.00028098654],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001304062,0.0000613956,0.7232992,0.00006248306,0.000116704214,0.0001138556,0.000077038996,0.2187966,0.009417208,0.00088409294,0.00336758,0.043673486],"study_design_scores_gemma":[0.000011968317,0.000028429182,0.7616002,0.000017969673,0.000027063492,0.00005322883,0.00008045281,0.2332108,0.0025896945,0.00025893646,0.0021019147,0.000019393085],"about_ca_topic_score_codex":0.3617334,"about_ca_topic_score_gemma":0.43489012,"teacher_disagreement_score":0.3617334,"about_ca_system_score_codex":0.0014237779,"about_ca_system_score_gemma":0.0009859331,"threshold_uncertainty_score":0.7192558},"labels":[],"label_agreement":null},{"id":"W4392287761","doi":"10.1029/2023gl105039","title":"Real‐Time Water Levels Using GNSS‐IR: A Potential Tool for Flood Monitoring","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Flood Risk Assessment and Management","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada; Université du Québec à Montréal; McGill University; Université Laval","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"GNSS applications; Reflectometry; Environmental science; Remote sensing; Water level; Satellite system; Flood myth; Global Positioning System; Satellite; Computer science; Geology; Telecommunications","score_opus":0.0425793173312811,"score_gpt":0.3442487983259741,"score_spread":0.301669480994693,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392287761","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7604572,0.0012166802,0.2086939,0.0016938966,0.00031456724,0.00010069597,0.0028756117,0.005247822,0.019399712],"genre_scores_gemma":[0.90031284,0.00027290764,0.095800415,0.00019570997,0.0001045186,0.00004578411,0.0005706084,0.00010640455,0.0025908141],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987316,0.000040864124,0.000005034267,0.000028852637,0.000039529772,0.000012528861],"domain_scores_gemma":[0.99981874,0.000040487495,0.000046700523,0.000029229319,0.000046165118,0.000018698129],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029801897,0.00040164316,0.00019594411,0.0006384605,0.0001259758,0.0004183815,0.00039555068,0.00046875124,0.0016979243],"category_scores_gemma":[0.00046783124,0.00015890553,0.00014461906,0.00071017345,0.0002516624,0.0005903789,0.00038117726,0.00036251283,0.00048751917],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006269522,0.0002447502,0.07226739,0.00023022167,0.0001027416,0.00017219028,0.00019963377,0.023481045,0.52834374,0.001571738,0.0060175452,0.36674213],"study_design_scores_gemma":[0.00028251845,0.0013731688,0.2883474,0.00015125859,0.00031453854,0.0006040776,0.00058810855,0.32318294,0.34195697,0.008239692,0.034674127,0.00028526183],"about_ca_topic_score_codex":0.0012030636,"about_ca_topic_score_gemma":0.0021171435,"teacher_disagreement_score":0.0016979243,"about_ca_system_score_codex":0.00018511398,"about_ca_system_score_gemma":0.00013224182,"threshold_uncertainty_score":0.005680144},"labels":[],"label_agreement":null},{"id":"W4392356801","doi":"10.1029/2023gl106300","title":"Multi‐Decadal Coastal Acidification in the Northern Gulf of Mexico Driven by Climate Change and Eutrophication","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"National Centers for Coastal Ocean Science; National Natural Science Foundation of China; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Eutrophication; Oceanography; Climate change; Ocean acidification; Environmental science; Climatology; Geology; Ecology; Nutrient","score_opus":0.048460756716293206,"score_gpt":0.3050279663152686,"score_spread":0.2565672095989754,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392356801","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99867815,0.00015278526,0.000077156394,0.00012902694,0.000009913414,0.0000016492525,0.00070088916,0.000008754775,0.00024162857],"genre_scores_gemma":[0.9991266,0.0001077493,0.00009632957,0.00002138503,0.000007171454,0.0000042115043,0.0005028803,0.0000014106706,0.00013235644],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999628,0.0000046829573,0.0000037659277,0.000013431524,0.0000049531272,0.000010285723],"domain_scores_gemma":[0.99978906,0.000018703924,0.00010348856,0.000010691011,0.000041934876,0.00003615709],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022847184,0.00013194582,0.00012631487,0.00048767228,0.00024819627,0.00031803167,0.00011977103,0.00024418553,0.00084677787],"category_scores_gemma":[0.00036203174,0.000062251354,0.00016865821,0.00047522693,0.00011642615,0.00020752543,0.0004484374,0.00020269319,0.00004865042],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019713122,0.000028711062,0.98565304,0.000043863896,0.00014710997,0.00021861993,0.00020555468,0.0017603324,0.0044217017,0.00007265939,0.0008640449,0.0063872193],"study_design_scores_gemma":[0.0000019278664,0.000007603242,0.9990107,0.0000036271153,0.000011522531,0.000019453164,0.00010091587,0.0003968455,0.00010531376,0.000015700287,0.00032440035,0.0000020231457],"about_ca_topic_score_codex":0.04297507,"about_ca_topic_score_gemma":0.061442256,"teacher_disagreement_score":0.04297507,"about_ca_system_score_codex":0.000592477,"about_ca_system_score_gemma":0.00024494034,"threshold_uncertainty_score":0.085449874},"labels":[],"label_agreement":null},{"id":"W4392374035","doi":"10.1029/2023gl106584","title":"Quantifying the Relative Contributions of the Global Oceans to ENSO Predictability With Deep Learning","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"National Natural Science Foundation of China","keywords":"Predictability; El Niño Southern Oscillation; Climatology; Oceanography; Environmental science; Geology; Mathematics; Statistics","score_opus":0.024049961475143242,"score_gpt":0.2987827506265248,"score_spread":0.27473278915138155,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392374035","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.71971214,0.0003381808,0.2763856,0.00044576288,0.00004042057,0.000019751898,0.0003637149,0.000351693,0.002342643],"genre_scores_gemma":[0.9874653,0.00006005419,0.011904358,0.000032001575,0.000022769189,0.000010745315,0.00018007387,0.000012893099,0.00031183157],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998004,0.00006027885,0.000009879547,0.000039981347,0.000051354255,0.000038141738],"domain_scores_gemma":[0.9992888,0.00040332248,0.00010937735,0.000061480125,0.00009683331,0.00004014477],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008625958,0.00048388136,0.00024160661,0.0006146008,0.00020007392,0.0006378152,0.00023442732,0.0002773865,0.0004891101],"category_scores_gemma":[0.0026195976,0.00016331451,0.00023547527,0.00057921384,0.0003884364,0.00092426135,0.00087572384,0.0004701994,0.00005841898],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013003194,0.000077763005,0.056042533,0.000028453846,0.00014934491,0.00003625563,0.000033015094,0.8275194,0.0067584193,0.0038758942,0.0007162966,0.10463268],"study_design_scores_gemma":[0.0000016938737,0.000010029024,0.004945731,0.0000017121042,0.000005538142,0.0000024537578,0.000004336854,0.99298453,0.00064656796,0.0013184496,0.000075088894,0.0000038667176],"about_ca_topic_score_codex":0.0047013275,"about_ca_topic_score_gemma":0.0073970985,"teacher_disagreement_score":0.0047013275,"about_ca_system_score_codex":0.00044148325,"about_ca_system_score_gemma":0.00061088713,"threshold_uncertainty_score":0.009347916},"labels":[],"label_agreement":null},{"id":"W4392457742","doi":"10.1029/2023gl107085","title":"Localized Magnetopause Erosion at Geosynchronous Orbit by Reconnection","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Aeronautics and Space Administration","keywords":"Magnetopause; Geosynchronous orbit; Magnetic reconnection; Geophysics; Orbit (dynamics); Physics; Magnetosphere; Magnetosheath; Astrobiology; Environmental science; Astronomy; Aerospace engineering; Plasma; Satellite","score_opus":0.0132862767939184,"score_gpt":0.28068048599217627,"score_spread":0.26739420919825785,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392457742","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875116,0.0000661937,0.00012769262,0.000009777045,0.0000025667946,0.0000019878773,0.00011289142,0.000023388533,0.0009042509],"genre_scores_gemma":[0.99953365,0.000025006859,0.000093851464,0.0000073460947,0.000003423198,0.0000013224793,0.00020050058,0.000002671079,0.00013231089],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995947,0.0000039322113,0.0000014710046,0.000011281934,0.000012671827,0.000011269074],"domain_scores_gemma":[0.99992716,0.000008777218,0.000030715746,0.000007464617,0.000010593346,0.000015226684],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00005711402,0.00015420199,0.00018296261,0.00045949442,0.00019783493,0.00022565956,0.00012690174,0.00020682398,0.00078833796],"category_scores_gemma":[0.00010915183,0.00009536125,0.000098694094,0.0003070813,0.0001336422,0.00014409049,0.00022384067,0.00019122243,0.00013459368],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00073212443,0.00009171664,0.6737849,0.000072362425,0.00014861605,0.001076818,0.0006855003,0.0018266623,0.30177256,0.00023139066,0.0010556033,0.018521782],"study_design_scores_gemma":[0.000013198948,0.000051546715,0.99512637,0.0000039171555,0.000010313129,0.00013344659,0.000099274126,0.00071613974,0.003254794,0.000036597758,0.0005511428,0.0000032857129],"about_ca_topic_score_codex":0.0020784324,"about_ca_topic_score_gemma":0.005669424,"teacher_disagreement_score":0.0020784324,"about_ca_system_score_codex":0.0001772614,"about_ca_system_score_gemma":0.00007027122,"threshold_uncertainty_score":0.0041326284},"labels":[],"label_agreement":null},{"id":"W4392881671","doi":"10.1029/2023gl107622","title":"Moisture Sources and Pathways of Annual Maximum Precipitation in the Lancang‐Mekong River Basin","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science, Technology and Innovation Commission of Shenzhen Municipality; Natural Science Foundation of Jiangsu Province","keywords":"Precipitation; Environmental science; Climatology; Evapotranspiration; Moisture; Equator; Bay; Structural basin; Tropical cyclone; Atmospheric sciences; Oceanography; Geology; Geography; Meteorology; Latitude","score_opus":0.03003968700153083,"score_gpt":0.2886714449166743,"score_spread":0.2586317579151435,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392881671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993406,0.000026545926,0.00007348049,0.000036776375,7.480553e-7,0.0000021245096,0.00020991518,0.000007681278,0.00030210754],"genre_scores_gemma":[0.9997278,0.00001459207,0.00004566004,0.0000019408467,3.6680996e-7,0.000001522428,0.000091519425,9.405849e-7,0.00011568477],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996483,0.000007578853,0.0000026303055,0.000008315124,0.0000048453335,0.000011703894],"domain_scores_gemma":[0.9998816,0.00002465838,0.000037381156,0.000005867724,0.000027079686,0.000023304354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008154289,0.00012636042,0.00008425869,0.0004397773,0.00029634306,0.0004331791,0.00019702979,0.000113975235,0.00077133405],"category_scores_gemma":[0.000286106,0.00014394849,0.00014602693,0.0005424067,0.0001493648,0.00019902157,0.00029215976,0.00012302355,0.00005257516],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012885453,0.000041541058,0.9551708,0.000042408567,0.000079638405,0.00048801722,0.00061602704,0.02794085,0.004725697,0.00074483285,0.00058023434,0.009440994],"study_design_scores_gemma":[0.000020467593,0.000020846155,0.9211003,0.000017203289,0.0000284978,0.000076380966,0.0008803993,0.07562151,0.0007572014,0.0002444326,0.0012141299,0.00001861244],"about_ca_topic_score_codex":0.20822296,"about_ca_topic_score_gemma":0.20353739,"teacher_disagreement_score":0.20822296,"about_ca_system_score_codex":0.0008064854,"about_ca_system_score_gemma":0.0006424265,"threshold_uncertainty_score":0.4140219},"labels":[],"label_agreement":null},{"id":"W4392882757","doi":"10.1029/2023gl106985","title":"Regime Shifts in Lake Oxygen and Temperature in the Rapidly Warming High Arctic","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Marine and coastal ecosystems","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; Université Laval; Center for Northern Studies; Makivik Corporation","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Permafrost; Environmental science; Cryosphere; Ice-albedo feedback; Glacier; Climatology; Arctic; Atmospheric sciences; Global warming; Biogeochemical cycle; Sea ice; Climate change; Stratification (seeds); Forcing (mathematics); Oceanography; Geology; Physical geography; Sea ice thickness; Ecology; Geography","score_opus":0.017974676058005633,"score_gpt":0.25517265711850035,"score_spread":0.23719798106049472,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4392882757","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99974245,0.000022962317,0.000033302516,0.0000107078995,8.2572194e-7,4.2152033e-7,0.000032409585,0.0000012913662,0.0001556546],"genre_scores_gemma":[0.9998684,0.00001285713,0.00003198954,0.0000069478774,0.0000011147911,8.031783e-7,0.000029923844,5.5073497e-7,0.00004739973],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999596,0.0000083859895,0.0000025752977,0.000009345688,0.000008135433,0.000011972096],"domain_scores_gemma":[0.99986935,0.000024922107,0.00004917041,0.0000064419105,0.000027559934,0.000022482547],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018943436,0.00006344343,0.00012027895,0.00023903324,0.0003289767,0.00038284005,0.00007757464,0.00014150118,0.0003201673],"category_scores_gemma":[0.0002720848,0.000081631966,0.00007386364,0.0003105134,0.0002174878,0.00017124646,0.00020457887,0.00016671207,0.000055122015],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020103129,0.000045302815,0.96037513,0.000016581585,0.000052625808,0.00009800678,0.00055517664,0.00068069453,0.033644315,0.00013190882,0.00014387158,0.0040553664],"study_design_scores_gemma":[0.0000014058966,0.000015985477,0.99855644,0.0000013302044,0.0000048860006,0.000026474427,0.00019797773,0.00043187395,0.00061409385,0.000037027537,0.000110774075,0.0000016825674],"about_ca_topic_score_codex":0.013351015,"about_ca_topic_score_gemma":0.027504344,"teacher_disagreement_score":0.013351015,"about_ca_system_score_codex":0.00038752676,"about_ca_system_score_gemma":0.00020985288,"threshold_uncertainty_score":0.026546597},"labels":[],"label_agreement":null},{"id":"W4393021980","doi":"10.1029/2023gl107777","title":"Responses of Atlantic Water Inflow Through Fram Strait to Arctic Storms","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada","keywords":"Inflow; Oceanography; Storm; Climatology; Geology; Arctic; The arctic; Environmental science","score_opus":0.03169992166322976,"score_gpt":0.30178489672891123,"score_spread":0.27008497506568147,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393021980","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986891,0.000024397092,0.00014710805,0.00005522142,0.000017624408,0.000004167053,0.00034407235,0.00003054197,0.0006878206],"genre_scores_gemma":[0.999074,0.000030084326,0.00008551539,0.000020788466,0.0000039145207,0.000004019925,0.00045222262,0.00000807511,0.0003213699],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99984527,0.000030355322,0.000013006363,0.000036221103,0.000016323344,0.00005879731],"domain_scores_gemma":[0.99957603,0.0001916103,0.00006795692,0.000023815799,0.00006886442,0.000071805705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002992806,0.00046035703,0.00039048732,0.0003921857,0.0004006363,0.0008790495,0.00024580947,0.0006437046,0.0015660997],"category_scores_gemma":[0.0012232815,0.00028406692,0.000588705,0.00031716086,0.0002377037,0.0003278677,0.00044502516,0.0004998497,0.00020307928],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010938039,0.0002716058,0.43427157,0.0000774621,0.00037000704,0.0005865214,0.00022677374,0.5342759,0.021474134,0.00041817434,0.001719523,0.0052145408],"study_design_scores_gemma":[0.00013572109,0.00042403932,0.43593258,0.00003523385,0.00012747447,0.000080587815,0.00048463975,0.55465704,0.006491508,0.0002943381,0.0012701085,0.00006657445],"about_ca_topic_score_codex":0.05506613,"about_ca_topic_score_gemma":0.044320792,"teacher_disagreement_score":0.05506613,"about_ca_system_score_codex":0.0009809779,"about_ca_system_score_gemma":0.00062447804,"threshold_uncertainty_score":0.10949123},"labels":[],"label_agreement":null},{"id":"W4393046774","doi":"10.1029/2023gl106788","title":"Magnetic Field Signatures of Craters on Mars","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Impact crater; Geology; Geophysics; Astrobiology; Field (mathematics); Earth science; Seismology; Physics","score_opus":0.0248225256064387,"score_gpt":0.3014245355286965,"score_spread":0.2766020099222578,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393046774","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947184,0.000050786868,0.000033333345,0.000005373504,9.0439255e-7,0.0000014094015,0.00007366733,0.000005783811,0.00035680193],"genre_scores_gemma":[0.9997311,0.000022758195,0.00007063072,0.0000026063512,0.0000031703098,7.4328767e-7,0.00008668857,0.0000012407454,0.000081037615],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995244,0.000004453224,0.0000029474686,0.000013151615,0.000012735196,0.000014181837],"domain_scores_gemma":[0.99964607,0.000043066953,0.00015348448,0.00002165976,0.000076942255,0.000058688634],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000064396685,0.0001414491,0.00014432013,0.0014272314,0.00017343348,0.00025354963,0.00010321761,0.00013659474,0.00094978436],"category_scores_gemma":[0.0003521857,0.000067001965,0.00007408203,0.00052879535,0.00020147274,0.00010191272,0.00022843873,0.00010107748,0.00010088827],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005160376,0.000035288114,0.79483813,0.0000729735,0.000071309456,0.00061481056,0.0005607211,0.000335098,0.18122172,0.00012026225,0.00029347328,0.021320151],"study_design_scores_gemma":[0.0000019903262,0.000027245624,0.9982912,0.0000027725703,0.000004650879,0.00017812387,0.000067835404,0.00009819454,0.0011222305,0.000011615257,0.00019204008,0.0000020914213],"about_ca_topic_score_codex":0.0024169795,"about_ca_topic_score_gemma":0.0030359772,"teacher_disagreement_score":0.0024169795,"about_ca_system_score_codex":0.00012949036,"about_ca_system_score_gemma":0.00004741236,"threshold_uncertainty_score":0.0048058033},"labels":[],"label_agreement":null},{"id":"W4393337803","doi":"10.1029/2023gl105578","title":"Shaking up Assumptions: Earthquakes Have Rarely Triggered Andean Glacier Lake Outburst Floods","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; Nuclear Safety and Security Commission; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Glacier; Geology; Permafrost; Natural hazard; Climate change; Climatology; Hazard; Physical geography; Oceanography; Geomorphology; Geography","score_opus":0.08210189380457344,"score_gpt":0.32896117414311576,"score_spread":0.24685928033854232,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393337803","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8149603,0.0019904983,0.0663918,0.024097767,0.000837479,0.00014204741,0.004451881,0.00033577648,0.08679253],"genre_scores_gemma":[0.9951611,0.0002849418,0.0013745294,0.0010930648,0.00020492433,0.000030075927,0.00064732,0.000022630993,0.0011814218],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9964515,0.0010293374,0.00035485372,0.0010050825,0.0006524093,0.00050688424],"domain_scores_gemma":[0.93689954,0.04072621,0.010646173,0.006869394,0.0037207406,0.0011379956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009670818,0.00037059764,0.00068700896,0.0018444896,0.0018774495,0.0022700464,0.002072118,0.0013520985,0.011402482],"category_scores_gemma":[0.08992883,0.00022834919,0.0005086285,0.001407768,0.0030621528,0.0043882867,0.0018267957,0.0016380098,0.0020077254],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0027386975,0.00021174512,0.68025756,0.0007924129,0.00052166777,0.003431727,0.005663673,0.025060108,0.003393817,0.12713754,0.03263304,0.11815796],"study_design_scores_gemma":[0.00031238422,0.0006186577,0.48104054,0.0012666134,0.00053284044,0.0047099884,0.016033046,0.14312072,0.011521732,0.29426682,0.046319313,0.0002572133],"about_ca_topic_score_codex":0.010874899,"about_ca_topic_score_gemma":0.007972944,"teacher_disagreement_score":0.011402482,"about_ca_system_score_codex":0.001718469,"about_ca_system_score_gemma":0.00078809354,"threshold_uncertainty_score":0.05114484},"labels":[],"label_agreement":null},{"id":"W4393481345","doi":"10.1029/2023gl105762","title":"Chemistry Contribution to Stratospheric Ozone Depletion After the Unprecedented Water‐Rich Hunga Tonga Eruption","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":18,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Climate Program Office; National Aeronautics and Space Administration; Canadian Space Agency; National Oceanic and Atmospheric Administration; National Center for Atmospheric Research; National Science Foundation","keywords":"Ozone depletion; Ozone; Sulfate aerosol; Stratosphere; Atmospheric sciences; Ozone layer; Plume; Aerosol; Atmospheric chemistry; Climatology; Sulfate; Volcano; Water vapor; Middle latitudes; Southern Hemisphere; Northern Hemisphere; Environmental science; Latitude; Chemistry; Geology; Meteorology; Geography","score_opus":0.015602981280544815,"score_gpt":0.275594605427156,"score_spread":0.2599916241466112,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393481345","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993734,0.00004141712,0.000103183644,0.000056246707,0.000005692071,0.000002402645,0.00012658007,0.000012614593,0.00027838442],"genre_scores_gemma":[0.99976164,0.00002026292,0.00003152818,0.000005431538,0.0000012241683,0.0000013617567,0.00008753336,0.0000016348969,0.00008934138],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999634,0.000008154363,0.0000015754059,0.000008208127,0.000004606323,0.000014076943],"domain_scores_gemma":[0.9999447,0.000011572548,0.000011387484,0.000005223474,0.00000919359,0.000017833088],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001500221,0.0002689968,0.00020443185,0.00015527436,0.00035106405,0.0004906639,0.00020231647,0.00034308224,0.0010040896],"category_scores_gemma":[0.00022508562,0.00019554955,0.0003817358,0.00018414838,0.00023600683,0.00027382138,0.0003418009,0.00025680533,0.000071365364],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000786639,0.0002847619,0.5579408,0.00012173987,0.00048536365,0.0014954574,0.00030325798,0.33721933,0.09184743,0.0011493878,0.0011589363,0.007206936],"study_design_scores_gemma":[0.00012709163,0.00022767736,0.6239872,0.0000063488205,0.00018110142,0.00010994973,0.00023966267,0.3629618,0.010438387,0.00038971403,0.0012985092,0.00003256226],"about_ca_topic_score_codex":0.044041403,"about_ca_topic_score_gemma":0.026463656,"teacher_disagreement_score":0.044041403,"about_ca_system_score_codex":0.0013279053,"about_ca_system_score_gemma":0.00053195946,"threshold_uncertainty_score":0.08757007},"labels":[],"label_agreement":null},{"id":"W4393935248","doi":"10.1029/2023gl106926","title":"Influence of Lowering Soot‐Water Contact Angle on Ice Nucleation of Ozone‐Aged Soot","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Impact","funders":"China Scholarship Council; Eidgenössische Technische Hochschule Zürich","keywords":"Soot; Ice nucleus; Ozone; Nucleation; Contact angle; Atmospheric sciences; Materials science; Environmental science; Meteorology; Geology; Chemistry; Thermodynamics; Physics; Physical chemistry; Composite material; Combustion","score_opus":0.021947526380611076,"score_gpt":0.27472234681795416,"score_spread":0.25277482043734306,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4393935248","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995552,0.00007255409,0.000113400594,0.0000036217898,0.0000043718137,0.0000035551677,0.00008445351,0.0000033700926,0.00015960631],"genre_scores_gemma":[0.9995926,0.00006602788,0.000112301044,0.000006643089,0.0000012560638,0.000002936825,0.000060349717,0.0000033471727,0.00015439084],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999162,0.000009146123,0.0000045828956,0.000019628618,0.000018526614,0.000032067463],"domain_scores_gemma":[0.99988604,0.000036022433,0.000023563158,0.000009056284,0.00002291097,0.000022388094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000114139686,0.0002316597,0.0002002539,0.0000953346,0.00014955692,0.00023815992,0.00012695245,0.00016130276,0.000862293],"category_scores_gemma":[0.00018273649,0.00010199711,0.00017303572,0.00007427798,0.00018095871,0.00013490462,0.000116954245,0.00020963309,0.000077682125],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027852258,0.000013120996,0.0010137042,0.000019599996,0.000009581261,0.00002898253,0.000024047671,0.00013461385,0.99806875,0.000010485391,0.000008524822,0.0003899927],"study_design_scores_gemma":[0.000006355803,0.00032576828,0.018584095,0.00000289067,0.00001552028,0.00002247128,0.00006355691,0.000791509,0.979965,0.000013997663,0.00020443083,0.000004424587],"about_ca_topic_score_codex":0.002720473,"about_ca_topic_score_gemma":0.0023203392,"teacher_disagreement_score":0.002720473,"about_ca_system_score_codex":0.00016263232,"about_ca_system_score_gemma":0.00012276621,"threshold_uncertainty_score":0.0054093003},"labels":[],"label_agreement":null},{"id":"W4394678521","doi":"10.1029/2023gl106639","title":"Model Biases in the Atmosphere‐Ocean Partitioning of Poleward Heat Transport Are Persistent Across Three CMIP Generations","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Teachers College; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Atmosphere (unit); Environmental science; Climatology; Atmospheric sciences; Geology; Meteorology; Geography","score_opus":0.11967629594941881,"score_gpt":0.34485844544277316,"score_spread":0.22518214949335436,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394678521","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99779594,0.00006450614,0.0004652817,0.00011268733,0.00001075492,0.0000036781123,0.0008468873,0.0000764852,0.0006237324],"genre_scores_gemma":[0.99897385,0.00003318741,0.00018792413,0.000024562189,0.000002666906,0.000005197552,0.00067675044,0.00001675437,0.00007914237],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99982786,0.0000481987,0.0000111732115,0.000059735296,0.00001859672,0.000034320765],"domain_scores_gemma":[0.99948573,0.00019766594,0.00008423177,0.00012486696,0.0000566545,0.000050902592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000941451,0.0004700468,0.00029660706,0.0002258746,0.0002949501,0.00075401895,0.00043939662,0.0004165799,0.0012560711],"category_scores_gemma":[0.0016903752,0.00030845273,0.0006996922,0.0003695928,0.0002629318,0.0004518041,0.00048712132,0.00043344346,0.00021610185],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009881798,0.00015108673,0.7324943,0.00009838294,0.0011746807,0.00015205245,0.00028644328,0.21998063,0.024326166,0.0011446308,0.0034397037,0.015763832],"study_design_scores_gemma":[0.00017862461,0.00011714711,0.7939418,0.000026362688,0.00031630654,0.00007586197,0.00016247058,0.19461143,0.0076857843,0.0012705714,0.0015477207,0.000065883374],"about_ca_topic_score_codex":0.022661045,"about_ca_topic_score_gemma":0.01963564,"teacher_disagreement_score":0.022661045,"about_ca_system_score_codex":0.0005838811,"about_ca_system_score_gemma":0.00045441615,"threshold_uncertainty_score":0.04505825},"labels":[],"label_agreement":null},{"id":"W4394678763","doi":"10.1029/2023gl107477","title":"Radiation, Air Temperature, and Soil Water Availability Drive Tree Water Deficit Across Temporal Scales in Canada's Western Boreal Forest","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Trent University; Global Institute for Water Security; Wilfrid Laurier University; University of Saskatchewan; Université de Montréal; Université du Québec à Montréal","funders":"Fonds de recherche du Québec – Nature et technologies; Canada First Research Excellence Fund; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Canada Foundation for Innovation","keywords":"Environmental science; Taiga; Boreal; Soil water; Air temperature; Atmospheric sciences; Climatology; Hydrology (agriculture); Forestry; Geography; Soil science; Geology","score_opus":0.008714942829796998,"score_gpt":0.2443998909830061,"score_spread":0.23568494815320912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394678763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923325,0.000050592713,0.000057307894,0.00003113222,9.2443827e-7,0.000002030676,0.00026789054,0.0000047684885,0.00035212524],"genre_scores_gemma":[0.99956006,0.000027235074,0.000050797888,0.0000072515118,4.249628e-7,0.0000015706622,0.00015600705,0.0000013621939,0.00019516567],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993944,0.0000045932716,0.0000025153,0.000015493602,0.000011713971,0.000026234036],"domain_scores_gemma":[0.99971956,0.00003968668,0.00005152066,0.000009327188,0.00010268498,0.000077147706],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012723422,0.00010687767,0.00012938915,0.0004008363,0.0006088873,0.0005415265,0.0002451955,0.00014726767,0.0010067117],"category_scores_gemma":[0.00042465827,0.00011017684,0.00012411927,0.0006515529,0.00033854265,0.0001535933,0.00026852483,0.00016968316,0.00006430691],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000088894,0.00002447195,0.9882045,0.000014025023,0.000037263635,0.000058956957,0.00044539117,0.0010035193,0.005643432,0.0001694147,0.0004329801,0.0038771098],"study_design_scores_gemma":[0.0000012813211,0.0000023980683,0.998691,0.0000017517391,0.00000562339,0.0000073613455,0.00025624628,0.0007922182,0.0000752186,0.000019825882,0.00014497811,0.0000020625362],"about_ca_topic_score_codex":0.95837396,"about_ca_topic_score_gemma":0.98080736,"teacher_disagreement_score":0.041626036,"about_ca_system_score_codex":0.0032833263,"about_ca_system_score_gemma":0.0031294478,"threshold_uncertainty_score":0.08374232},"labels":[],"label_agreement":null},{"id":"W4394691650","doi":"10.1029/2024gl108715","title":"Continental Crust Rejuvenation Across the Paleo‐Mesoarchean Transition Resulted From Elevated Mantle Geotherms","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Postdoctoral Research Foundation of China; National Natural Science Foundation of China; Natural Environment Research Council; Sight Research UK","keywords":"Zircon; Geology; Geochemistry; Mantle (geology); Continental crust; Crust; Underplating; Petrogenesis; Transition zone; Radiogenic nuclide; Plate tectonics; Petrology; Rejuvenation; Earth science; Subduction; Tectonics; Paleontology","score_opus":0.02923362609844251,"score_gpt":0.2866435462737422,"score_spread":0.25740992017529973,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394691650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999008,0.00013895455,0.00011406394,0.000031666743,0.0000018497726,0.0000022755999,0.00011544658,0.000007987235,0.00057978154],"genre_scores_gemma":[0.99967575,0.000047344976,0.000039952618,0.000007889278,0.0000012089281,0.0000010863396,0.000054636315,0.0000025879087,0.00016953431],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992573,0.0000072927946,0.000005147605,0.000027375809,0.000013179652,0.000021280222],"domain_scores_gemma":[0.9998872,0.000012757218,0.000031539388,0.000022581042,0.00002454735,0.000021298487],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024410011,0.00025775906,0.00019841846,0.00068585336,0.00050235156,0.00054489507,0.00019066913,0.00021788217,0.0020327633],"category_scores_gemma":[0.00030121105,0.000112078276,0.00023418762,0.00066116225,0.0006503459,0.0002997812,0.00062141713,0.00027256098,0.00017636955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046782815,0.000017814838,0.8238435,0.00007750696,0.00026619917,0.00060058123,0.0009231471,0.001567632,0.1454833,0.00084401306,0.00018774447,0.025720749],"study_design_scores_gemma":[0.0000023130526,0.000018537672,0.9964489,0.000002703351,0.000014352302,0.000087481174,0.0002469171,0.00015836263,0.0025464934,0.00007691145,0.00039470528,0.0000022412526],"about_ca_topic_score_codex":0.0106560495,"about_ca_topic_score_gemma":0.016639218,"teacher_disagreement_score":0.0106560495,"about_ca_system_score_codex":0.00071520277,"about_ca_system_score_gemma":0.00035876347,"threshold_uncertainty_score":0.02118808},"labels":[],"label_agreement":null},{"id":"W4394760671","doi":"10.1029/2024gl108459","title":"Insights Into Changing Interglacial Conditions in Subarctic Canada From MIS 11 Through MIS 5e From Seasonally Resolved Speleothem Records","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Parks Canada","funders":"National Science Foundation","keywords":"Speleothem; Interglacial; Subarctic climate; Northern Hemisphere; Climatology; Precipitation; Paleoclimatology; Ice core; Geology; Latitude; Climate change; Physical geography; Environmental science; Oceanography; Glacial period; Cave; Geography; Paleontology; Meteorology","score_opus":0.02748504475879963,"score_gpt":0.28515846053258037,"score_spread":0.2576734157737807,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394760671","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9960555,0.0002717765,0.0001892199,0.00006063586,0.0000042140755,0.000003631451,0.0017813884,0.000012645392,0.0016210015],"genre_scores_gemma":[0.9982894,0.00015252957,0.00028160255,0.000021667176,0.0000014958949,0.0000019711401,0.0008994132,0.0000052846017,0.00034655782],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999113,0.000007108478,0.000004833656,0.000024090365,0.000019555093,0.000033066623],"domain_scores_gemma":[0.9996675,0.0000326661,0.000057911675,0.000018099247,0.00016771095,0.000056127617],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022754658,0.00018683741,0.00013279454,0.0010380198,0.00071929954,0.00069336686,0.00021456936,0.00012515753,0.00094111776],"category_scores_gemma":[0.00053200003,0.00010913081,0.00014391253,0.0012796103,0.00025935724,0.00019023566,0.0002954395,0.00014639721,0.000085795626],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048773833,0.000006930014,0.9830634,0.000024342036,0.000060731458,0.000056487897,0.00052894186,0.00050942856,0.0057224524,0.00016094682,0.00051907694,0.009298415],"study_design_scores_gemma":[4.518645e-7,0.000001157762,0.9989058,0.000004584032,0.0000057598113,0.000007762316,0.00024276243,0.0001631402,0.00015797121,0.000010856484,0.0004981791,0.0000015115264],"about_ca_topic_score_codex":0.898794,"about_ca_topic_score_gemma":0.9739309,"teacher_disagreement_score":0.101206005,"about_ca_system_score_codex":0.0032028165,"about_ca_system_score_gemma":0.003460022,"threshold_uncertainty_score":0.20360398},"labels":[],"label_agreement":null},{"id":"W4394846092","doi":"10.1029/2023gl107357","title":"Geologic Provinces Beneath the Greenland Ice Sheet Constrained by Geophysical Data Synthesis","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"NASA Headquarters; Goddard Space Flight Center; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geology; Subaerial; Glacier; Glaciology; Ice sheet; Greenland ice sheet; Geophysics; Geomorphology; Ice stream; Groenlandia; Ice caps; Paleontology; Cryosphere; Oceanography; Tectonics; Volcanism; Sea ice","score_opus":0.06616172074966366,"score_gpt":0.29877452195865245,"score_spread":0.2326128012089888,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394846092","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9648727,0.0011993612,0.0019157471,0.00021915864,0.000011310637,0.00003329242,0.024793876,0.00014642379,0.0068081864],"genre_scores_gemma":[0.9837393,0.00034668457,0.0026624217,0.00003721318,0.0000046622376,0.000021899252,0.012829729,0.000022192287,0.00033572593],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99968123,0.000063401036,0.00004503192,0.00010096203,0.000050345127,0.000059112386],"domain_scores_gemma":[0.9991398,0.0002540384,0.0001518881,0.00016371853,0.00024503432,0.000045580207],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00056914386,0.0002664075,0.0002898089,0.0027452845,0.00020988891,0.0012250043,0.00023034612,0.000110026915,0.0009657347],"category_scores_gemma":[0.0017845988,0.00013238363,0.00025509106,0.003926656,0.00030574744,0.00027607998,0.0006499181,0.00013876773,0.00015821369],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001728028,0.000023584082,0.86474246,0.00033200893,0.00044697206,0.00031793592,0.00082223286,0.034127213,0.009640658,0.002325988,0.0031264906,0.08392174],"study_design_scores_gemma":[0.000016735135,0.000009133345,0.97300816,0.00011774812,0.00012262541,0.000028246777,0.00086292566,0.010776504,0.001539418,0.000871494,0.0126323495,0.000014635463],"about_ca_topic_score_codex":0.21207084,"about_ca_topic_score_gemma":0.3498816,"teacher_disagreement_score":0.21207084,"about_ca_system_score_codex":0.0014091281,"about_ca_system_score_gemma":0.002595885,"threshold_uncertainty_score":0.42167288},"labels":[],"label_agreement":null},{"id":"W4394855019","doi":"10.1029/2024gl108490","title":"Secondary Ice Production Improves Simulations of Freezing Rain","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal; Polytechnique Montréal; Environment and Climate Change Canada","funders":"Environment and Climate Change Canada","keywords":"Precipitation; Environmental science; Freezing rain; Hard rime; Winter storm; Snow; Storm; Climatology; Precipitation types; Graupel; Atmospheric sciences; Meteorology; Geology; Physics","score_opus":0.04951357411770672,"score_gpt":0.30927697686691114,"score_spread":0.2597634027492044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394855019","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98214,0.00015589173,0.008451549,0.00020937594,0.000076197175,0.000038648373,0.0006270944,0.00056559435,0.0077356333],"genre_scores_gemma":[0.9979201,0.000039096583,0.0014460132,0.000013153254,0.000008492873,0.000007581525,0.00018372033,0.00003439909,0.0003474384],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998925,0.000020806967,0.000005213129,0.00002385958,0.000020045045,0.00003762416],"domain_scores_gemma":[0.99963355,0.000109505076,0.000044836765,0.000036668134,0.00008167161,0.00009384965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027110448,0.0006720158,0.0005025072,0.00029074293,0.0004015086,0.0006905938,0.0006417374,0.00048792435,0.001500732],"category_scores_gemma":[0.0009680548,0.00026526948,0.0004930858,0.0002169516,0.0003083857,0.00041468418,0.0005623976,0.0005060744,0.00014181524],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000089464644,0.0000661011,0.006324373,0.000018003315,0.000025664656,0.000040775434,0.000019341425,0.98611337,0.0030909325,0.00042429293,0.00041173914,0.0033758935],"study_design_scores_gemma":[0.000014459404,0.00002339326,0.001142704,0.0000020170185,0.000004859895,0.0000026706807,0.0000036912836,0.99790657,0.00066222396,0.00007909998,0.00015599352,0.0000023857506],"about_ca_topic_score_codex":0.08651723,"about_ca_topic_score_gemma":0.039818253,"teacher_disagreement_score":0.08651723,"about_ca_system_score_codex":0.00084107165,"about_ca_system_score_gemma":0.001474527,"threshold_uncertainty_score":0.17202723},"labels":[],"label_agreement":null},{"id":"W4394927211","doi":"10.1029/2023gl106486","title":"Mapping Potential Timing of Ice Algal Blooms From Satellite","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Université Laval; Makivik Corporation; University of Manitoba","funders":"Nuclear Safety and Security Commission; Met Office; Natural Environment Research Council; Sight Research UK; National Aeronautics and Space Administration","keywords":"Sea ice; Cryosphere; Oceanography; Arctic ice pack; Bloom; Environmental science; Arctic; Algal bloom; Snow; Climatology; Drift ice; Geology; Phytoplankton; Ecology; Geomorphology","score_opus":0.02968761332190503,"score_gpt":0.27452439406556894,"score_spread":0.2448367807436639,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394927211","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99381447,0.00012870629,0.0005351579,0.000022162265,0.000006607574,0.000007721222,0.0028902646,0.000030062598,0.002564867],"genre_scores_gemma":[0.9943264,0.00011627901,0.0015392636,0.000011730051,0.000007557357,0.000012029346,0.0031285298,0.0000059572812,0.0008521733],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995816,0.000004656345,0.0000024457804,0.000013101117,0.000012043444,0.000009545237],"domain_scores_gemma":[0.99971837,0.000038813236,0.00008749301,0.000015493973,0.00009740493,0.000042458287],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017795779,0.000116233576,0.00007557879,0.0010574572,0.00016158787,0.00027901694,0.00010498824,0.00013567349,0.0011858682],"category_scores_gemma":[0.00036604895,0.0000730033,0.00011731233,0.0007679193,0.00007394087,0.00019096732,0.00021837797,0.00010711817,0.00024504194],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019985411,0.000031395546,0.95772624,0.00005114101,0.000059422,0.0000956971,0.00025688906,0.0030352455,0.015223178,0.00020810791,0.0009950503,0.022117784],"study_design_scores_gemma":[0.0000046083633,0.000035222303,0.99264103,0.000016048134,0.000017921471,0.000047817623,0.00019618352,0.0030991684,0.0020036814,0.00005296493,0.0018810803,0.0000042469096],"about_ca_topic_score_codex":0.014407361,"about_ca_topic_score_gemma":0.04345759,"teacher_disagreement_score":0.014407361,"about_ca_system_score_codex":0.00027410034,"about_ca_system_score_gemma":0.00018643471,"threshold_uncertainty_score":0.028647006},"labels":[],"label_agreement":null},{"id":"W4394970540","doi":"10.1029/2024gl108176","title":"Regional Responses of Vegetation Productivity to the Two Phases of ENSO","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":13,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Inversa Systems (Canada)","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"El Niño Southern Oscillation; Productivity; Vegetation (pathology); Environmental science; Climatology; Geology; Physical geography; Geography; Economics","score_opus":0.03643091700429482,"score_gpt":0.3249737663075633,"score_spread":0.28854284930326846,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4394970540","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995134,0.000026015936,0.00013576925,0.000013155736,0.0000022917889,0.0000016605409,0.000114044175,0.0000094589195,0.00018424774],"genre_scores_gemma":[0.99980277,0.00000875471,0.000028698525,0.0000026287807,0.00000116292,0.0000016555828,0.00011144959,0.0000021328874,0.000040811243],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991095,0.000017950457,0.0000046183095,0.000031649,0.000008256867,0.000026578004],"domain_scores_gemma":[0.9995999,0.000121460514,0.00007344645,0.000039685863,0.000076942815,0.00008863279],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030456713,0.00019773497,0.00018975849,0.00029017744,0.000120726625,0.00037175915,0.00015015836,0.00020867924,0.00055312546],"category_scores_gemma":[0.00089966366,0.00014750502,0.00026143546,0.00019902879,0.00020136978,0.0002514235,0.0004370764,0.00022068419,0.00010083508],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0014494032,0.00017581286,0.7580818,0.000064565465,0.0005466695,0.00029396344,0.00033857257,0.06368407,0.16081089,0.00062558235,0.00063842564,0.013290203],"study_design_scores_gemma":[0.000018059232,0.00006606895,0.9704917,0.0000031600634,0.000033667024,0.000036506826,0.00014424622,0.026137073,0.0026950066,0.00013720154,0.00022590224,0.000011337883],"about_ca_topic_score_codex":0.004713602,"about_ca_topic_score_gemma":0.0031111196,"teacher_disagreement_score":0.004713602,"about_ca_system_score_codex":0.0002795516,"about_ca_system_score_gemma":0.00012945592,"threshold_uncertainty_score":0.009372294},"labels":[],"label_agreement":null},{"id":"W4395002395","doi":"10.1029/2024gl108457","title":"The Irminger Gyre as a Key Driver of the Subpolar North Atlantic Overturning","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; Sight Research UK","keywords":"Ocean gyre; Oceanography; Thermohaline circulation; Key (lock); Geology; Climatology; Environmental science; Fishery; Biology; Subtropics; Ecology","score_opus":0.02601346860901917,"score_gpt":0.2914503657499271,"score_spread":0.26543689714090796,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395002395","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99680233,0.0001070535,0.0003701507,0.0002811273,0.000013990232,0.000002834906,0.00032515565,0.000035268844,0.002062143],"genre_scores_gemma":[0.9993525,0.00004311857,0.000103531405,0.000023497458,0.000012038515,0.0000013259773,0.00017993404,0.0000052666755,0.00027875003],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999269,0.00001193732,0.0000033832084,0.000027882394,0.000009073669,0.000020797364],"domain_scores_gemma":[0.99980265,0.000023835084,0.000076179866,0.00001598639,0.00003309972,0.000048288122],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020266342,0.00017182679,0.0001576589,0.0002831379,0.00019630746,0.00063334726,0.00014748042,0.0001750163,0.0019332966],"category_scores_gemma":[0.00045835724,0.000073307885,0.0002114982,0.00030582206,0.00015992763,0.00033504877,0.0003793927,0.0003002692,0.00021392731],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008074726,0.000038033264,0.96215326,0.000028003935,0.00011759599,0.00017735225,0.00033115735,0.00716283,0.00829202,0.0013490266,0.002129777,0.01814021],"study_design_scores_gemma":[0.0000053055537,0.000014077296,0.9855494,0.000012232176,0.000029112252,0.000015695434,0.00018544722,0.011826838,0.0003522069,0.00043026006,0.0015718235,0.0000076155193],"about_ca_topic_score_codex":0.03077809,"about_ca_topic_score_gemma":0.036261503,"teacher_disagreement_score":0.03077809,"about_ca_system_score_codex":0.00035386713,"about_ca_system_score_gemma":0.00029998276,"threshold_uncertainty_score":0.061197877},"labels":[],"label_agreement":null},{"id":"W4395031360","doi":"10.1029/2023gl105617","title":"Statistical Analysis of Whistler Precursors Upstream of Foreshock Transient Shocks: MMS Observations","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Whistler; Foreshock; Physics; Geophysics; Computational physics; Solar wind; Shock (circulatory); Polarization (electrochemistry); Shock wave; Plasma; Aftershock; Mechanics; Geology; Seismology; Nuclear physics","score_opus":0.029801326794726683,"score_gpt":0.3167304620825249,"score_spread":0.28692913528779823,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4395031360","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998382,0.000019477535,0.0010255424,0.000011735827,0.0000034144832,0.000004211393,0.00028651062,0.000032279848,0.00023484549],"genre_scores_gemma":[0.99876773,0.000012052521,0.00050471415,0.0000021967385,0.0000075089233,0.0000042888482,0.0005935783,0.0000050710423,0.00010291783],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988425,0.000018851337,0.000007987824,0.000033415447,0.000030912575,0.000024631463],"domain_scores_gemma":[0.9990608,0.00025876,0.0003432344,0.00009617709,0.00011932288,0.00012167782],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003351961,0.00013598848,0.00013744137,0.00093700795,0.00017711883,0.00024358004,0.00013822931,0.00013197087,0.0005384252],"category_scores_gemma":[0.0010597273,0.00009681259,0.000188789,0.0006114394,0.000118908436,0.00014539668,0.00026001458,0.00018543816,0.00008480328],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004443911,0.00003736804,0.92633784,0.000031503136,0.00010282413,0.0004094405,0.00022136507,0.0054018497,0.0386905,0.00063804747,0.0005058522,0.027178943],"study_design_scores_gemma":[0.0000036864722,0.000042159634,0.9892727,0.0000025840686,0.000013879562,0.000059313144,0.00007954761,0.008147629,0.0019570736,0.00006756162,0.00034710672,0.000006721377],"about_ca_topic_score_codex":0.0021415795,"about_ca_topic_score_gemma":0.00247397,"teacher_disagreement_score":0.0021415795,"about_ca_system_score_codex":0.00011299901,"about_ca_system_score_gemma":0.000163129,"threshold_uncertainty_score":0.004258275},"labels":[],"label_agreement":null},{"id":"W4396583643","doi":"10.1029/2024gl109159","title":"Atlantic Meridional Overturning Circulation Influence on the Annual Mean Intertropical Convergence Zone Location in the Miocene","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Purdue University; National Science Foundation","keywords":"Intertropical Convergence Zone; Geology; Climatology; Circulation (fluid dynamics); Zonal and meridional; Convergence zone; Shutdown of thermohaline circulation; Walker circulation; Oceanography; Thermohaline circulation; Geography; North Atlantic Deep Water; Meteorology; El Niño Southern Oscillation; Precipitation","score_opus":0.03203433582581375,"score_gpt":0.297507253560848,"score_spread":0.26547291773503423,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396583643","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99904174,0.00007290751,0.000029936853,0.0000358985,0.000002776497,0.0000010897272,0.00013974971,0.0000028700088,0.00067296217],"genre_scores_gemma":[0.9997656,0.000024471301,0.000020415673,0.0000048428715,0.0000017021134,8.0521005e-7,0.000083289,0.0000015083457,0.00009752246],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999163,0.000015942196,0.0000038135772,0.00002244108,0.000011039772,0.000030365472],"domain_scores_gemma":[0.9996922,0.000055801294,0.00006774984,0.000028009701,0.00007189999,0.00008438176],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026475987,0.00014055676,0.00014649944,0.00038030016,0.00034684467,0.0006157409,0.00020058929,0.0001548732,0.0014993807],"category_scores_gemma":[0.0008333789,0.000083663974,0.00019805614,0.00034275078,0.0002694843,0.00020138612,0.00035938667,0.00020524647,0.000116158575],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008262146,0.00001151816,0.99353915,0.0000073561164,0.0000631918,0.000056704812,0.00022901715,0.00029996043,0.0024691066,0.00014853055,0.0001875601,0.0029052375],"study_design_scores_gemma":[6.486925e-7,0.0000026120947,0.99962926,0.000001220571,0.000004709372,0.000003480975,0.000060024922,0.00014824382,0.00003430204,0.0000065624795,0.000108212735,6.362536e-7],"about_ca_topic_score_codex":0.16945156,"about_ca_topic_score_gemma":0.256729,"teacher_disagreement_score":0.16945156,"about_ca_system_score_codex":0.0007061495,"about_ca_system_score_gemma":0.0005417048,"threshold_uncertainty_score":0.3369305},"labels":[],"label_agreement":null},{"id":"W4396665080","doi":"10.1029/2024gl109626","title":"Thank You to Our 2023 Peer Reviewers","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Scientific Computing and Data Management","field":"Decision Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Office National de l’Eau et des Milieux Aquatiques; Curtin University of Technology","keywords":"Peer review; Environmental science; Geology; Psychology; Political science","score_opus":0.2948532722307753,"score_gpt":0.5085376973850151,"score_spread":0.2136844251542398,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396665080","genre_codex":"editorial","genre_gemma":"editorial","domain_codex":null,"domain_gemma":"evaluation","model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"editorial","genre_consensus":"editorial","domain_candidate":"evaluation","domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0013164795,0.012213951,0.01146917,0.30563962,0.628507,0.002122845,0.0038983054,0.005715519,0.02911711],"genre_scores_gemma":[0.018257936,0.016219703,0.0381719,0.20154414,0.34310555,0.0057482487,0.007331012,0.008598384,0.36102313],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9363067,0.01719746,0.008584604,0.006541144,0.028820243,0.0025497621],"domain_scores_gemma":[0.39993188,0.020851955,0.014976187,0.01470627,0.5196614,0.029872293],"candidate_categories":["metaresearch"],"consensus_categories":[],"category_scores_codex":[0.042325847,0.002575156,0.003681315,0.008038764,0.006289622,0.026959574,0.004001344,0.008837045,0.14445636],"category_scores_gemma":[0.28421253,0.0016666118,0.002403716,0.004466991,0.0025461065,0.0080272965,0.0063146697,0.008587405,0.231821],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00002185848,0.000008181863,0.00019644864,0.00013121669,0.000009510337,0.00007477178,0.00007576175,0.000020000265,0.00009031826,0.00018037768,0.9802152,0.01897643],"study_design_scores_gemma":[0.000023280976,0.000016636926,0.00033786078,0.0002896341,0.000015101605,0.0002485114,0.00033997107,0.0001312947,0.00012833916,0.00069472386,0.9977276,0.000047074816],"about_ca_topic_score_codex":0.002989446,"about_ca_topic_score_gemma":0.00533042,"teacher_disagreement_score":0.95767415,"about_ca_system_score_codex":0.0036164653,"about_ca_system_score_gemma":0.019570807,"threshold_uncertainty_score":0.48325467},"labels":[],"label_agreement":null},{"id":"W4396760413","doi":"10.1029/2024gl109022","title":"Emerging Influence of Enhanced Greenland Melting on Boundary Currents and Deep Convection Regimes in the Labrador and Irminger Seas","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological Studies and Exploration","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Deutsche Forschungsgemeinschaft","keywords":"Geology; Boundary current; Convection; Oceanography; Deep convection; Current (fluid); Geophysics; Climatology; Ocean current; Mechanics; Physics","score_opus":0.028820756363825382,"score_gpt":0.29599844472566705,"score_spread":0.2671776883618417,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396760413","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947864,0.0000098171595,0.000021367487,0.00002424798,9.271518e-7,0.0000010605273,0.000103434715,0.000007818373,0.00035275694],"genre_scores_gemma":[0.99966514,0.000010252923,0.000044825956,0.000010479431,0.0000012899221,0.0000013141675,0.00015886937,0.0000037540506,0.000104002844],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998883,0.00002906099,0.000007216523,0.000024863893,0.000010005649,0.000040446048],"domain_scores_gemma":[0.99981064,0.0000424187,0.000039923685,0.000026141177,0.000025507581,0.000055427605],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00030218385,0.00034125926,0.00027158333,0.00035269104,0.00026654292,0.00079016405,0.00027513166,0.00038688665,0.0012957501],"category_scores_gemma":[0.00058589416,0.00015363167,0.00060245,0.00029862905,0.00036577357,0.00043448264,0.0005401228,0.00024922114,0.00014372356],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009833785,0.00023147596,0.8200338,0.000060037753,0.00043732644,0.0008445798,0.00047236998,0.12915772,0.03275948,0.0010561335,0.0008474807,0.013116322],"study_design_scores_gemma":[0.000077504505,0.0001461929,0.9265254,0.000017410553,0.00009595615,0.00003717026,0.00041334116,0.068870045,0.0030861592,0.00018659506,0.00051501836,0.000029216368],"about_ca_topic_score_codex":0.07928797,"about_ca_topic_score_gemma":0.06517845,"teacher_disagreement_score":0.07928797,"about_ca_system_score_codex":0.001103301,"about_ca_system_score_gemma":0.0004960858,"threshold_uncertainty_score":0.15765291},"labels":[],"label_agreement":null},{"id":"W4396857047","doi":"10.1029/2023gl107780","title":"Top of the Atmosphere Shortwave Arctic Cloud Feedbacks: A Comparison of Diagnostic Methods","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies","keywords":"Shortwave; Atmosphere (unit); Environmental science; Cloud computing; Arctic; The arctic; Meteorology; Atmospheric sciences; Shortwave radiation; Climatology; Astrobiology; Geology; Oceanography; Geography; Radiative transfer; Computer science; Physics; Radiation","score_opus":0.03318716214228209,"score_gpt":0.3709249011622266,"score_spread":0.3377377390199445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396857047","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8540431,0.0020901319,0.12939136,0.00047517402,0.00018796069,0.000365083,0.003788893,0.0039251316,0.00573324],"genre_scores_gemma":[0.9519408,0.0002585669,0.045954306,0.000053050207,0.000029182835,0.00007641911,0.0011641617,0.00020707479,0.00031647398],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99871945,0.00048872933,0.00015570961,0.00020673135,0.00031414305,0.00011521946],"domain_scores_gemma":[0.9933901,0.0038682607,0.000797434,0.00042782232,0.0012860436,0.00023031965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0041919923,0.00085501175,0.00040431437,0.003930724,0.00037466592,0.0013799762,0.0010254288,0.0006684567,0.0016182038],"category_scores_gemma":[0.0116808275,0.00032416225,0.0006744251,0.0012569765,0.00022221243,0.0011104706,0.0011193388,0.0005511356,0.00028272488],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.005815923,0.00085918774,0.43699643,0.0010032362,0.0014605996,0.00031374773,0.0008307203,0.16421653,0.02879642,0.005623444,0.003933367,0.35015032],"study_design_scores_gemma":[0.0002066874,0.00018373625,0.061055407,0.00012294269,0.0001425279,0.00011240852,0.00034536023,0.923914,0.010702609,0.0016720197,0.0014427077,0.00009949947],"about_ca_topic_score_codex":0.012553961,"about_ca_topic_score_gemma":0.008144449,"teacher_disagreement_score":0.012553961,"about_ca_system_score_codex":0.000998363,"about_ca_system_score_gemma":0.00086807867,"threshold_uncertainty_score":0.02496177},"labels":[],"label_agreement":null},{"id":"W4396872006","doi":"10.1029/2023gl106685","title":"Interactions Between Anthropogenic Greenhouse‐Gas and Aerosol Emissions Will Shape Extreme Precipitations Over the Qinghai‐Tibet Plateau","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Regina","funders":"National Natural Science Foundation of China","keywords":"Greenhouse gas; Plateau (mathematics); Environmental science; Aerosol; Atmospheric sciences; Earth science; Geology; Meteorology; Geography; Oceanography","score_opus":0.07420002630688605,"score_gpt":0.35138684035187057,"score_spread":0.2771868140449845,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396872006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987093,0.000026081843,0.00058980903,0.000037722588,0.0000025639322,0.0000022389731,0.00018983065,0.00001358228,0.00042867905],"genre_scores_gemma":[0.9996606,0.000007509933,0.00012062174,0.0000043523555,0.0000031485229,0.0000018851784,0.00015074584,0.0000020095158,0.00004922085],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998733,0.000047397116,0.000006278717,0.00003256444,0.0000130221415,0.000027436761],"domain_scores_gemma":[0.99982697,0.00005584662,0.00003707988,0.000013125133,0.000034135686,0.000032965727],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00048587707,0.00021619293,0.00014722133,0.00042964297,0.00027387333,0.00052061054,0.00023410592,0.00016901159,0.00066490466],"category_scores_gemma":[0.00041238317,0.0001134738,0.0003852489,0.00056671526,0.0002460911,0.0002294765,0.00030515774,0.00015803397,0.00005297638],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00008449997,0.000027580916,0.96625227,0.000018380773,0.00019458498,0.00011723572,0.00012478963,0.01699216,0.0088217445,0.00031807096,0.00019957118,0.006849121],"study_design_scores_gemma":[0.000008800924,0.000015110153,0.96844953,0.0000028412207,0.000022654964,0.000017085737,0.00011380843,0.03076943,0.0003013167,0.00013390856,0.00015905629,0.000006521755],"about_ca_topic_score_codex":0.02874819,"about_ca_topic_score_gemma":0.024319172,"teacher_disagreement_score":0.02874819,"about_ca_system_score_codex":0.0003680091,"about_ca_system_score_gemma":0.00035239913,"threshold_uncertainty_score":0.05716169},"labels":[],"label_agreement":null},{"id":"W4396917556","doi":"10.1029/2024gl108494","title":"Interpreting the Seasonality of Atmospheric Methane","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":26,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Seasonality; Methane; Atmospheric methane; Environmental science; Climatology; Atmospheric sciences; Meteorology; Geography; Geology; Chemistry; Statistics; Mathematics","score_opus":0.017483836759129658,"score_gpt":0.29543276919136,"score_spread":0.27794893243223034,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4396917556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951389,0.00013413001,0.0012997945,0.00014666242,0.000028192744,0.00000516168,0.0014851999,0.00010931899,0.0016526075],"genre_scores_gemma":[0.9984864,0.000035900557,0.00052561186,0.000012959202,0.0000127187695,0.000002814253,0.00079300936,0.000015709284,0.00011487411],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993217,0.000013006538,0.0000038842186,0.000027647568,0.000009203994,0.000014098281],"domain_scores_gemma":[0.99984694,0.000042379277,0.000031625157,0.00002255396,0.000035197172,0.000021363867],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029205004,0.0001738265,0.00012007246,0.00051898346,0.00019480311,0.00043026192,0.00017335742,0.00020446013,0.00064877194],"category_scores_gemma":[0.0006596602,0.00013026985,0.00016922978,0.00046534877,0.00009927363,0.00031891646,0.00028225142,0.00016971795,0.00012753486],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002236912,0.000050073926,0.92230153,0.000054374486,0.00014928797,0.00022736318,0.00032190527,0.020644397,0.02951853,0.0006811716,0.0024716232,0.02335605],"study_design_scores_gemma":[0.000010398098,0.000022214383,0.9351055,0.000012139391,0.000042737258,0.00005560048,0.00023102135,0.05662193,0.0036595287,0.0004765661,0.003745499,0.000016923197],"about_ca_topic_score_codex":0.014000348,"about_ca_topic_score_gemma":0.018183796,"teacher_disagreement_score":0.014000348,"about_ca_system_score_codex":0.00028268958,"about_ca_system_score_gemma":0.00019234593,"threshold_uncertainty_score":0.027837753},"labels":[],"label_agreement":null},{"id":"W4397016814","doi":"10.1029/2024gl109028","title":"The Beginning of a Wilson Cycle in an Accretionary Orogen: The Mongol–Okhotsk Ocean Opened Assisted by a Devonian Mantle Plume","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Chinese Academy of Sciences; National Natural Science Foundation of China","keywords":"Geology; Plume; Devonian; Mantle (geology); Mantle plume; Geophysics; Seismology; Paleontology; Tectonics; Lithosphere; Meteorology; Physics","score_opus":0.026351251343365047,"score_gpt":0.28513609338255047,"score_spread":0.25878484203918545,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4397016814","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988463,0.00006310226,0.00007097729,0.000043937638,0.0000024047258,0.0000018450162,0.000021413109,0.0000036771137,0.00094643154],"genre_scores_gemma":[0.9996221,0.000029848534,0.00008180023,0.000010375086,0.0000019443335,0.0000010972094,0.000023555322,0.000001505959,0.00022783173],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999324,0.000008583282,0.0000046348664,0.000014123261,0.000013479209,0.000026754456],"domain_scores_gemma":[0.9998275,0.000023368433,0.000056012854,0.0000143125735,0.00003540315,0.00004331815],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020164147,0.000117469615,0.0001780182,0.0005274347,0.0009473049,0.0007411195,0.0002290804,0.0002744497,0.001274971],"category_scores_gemma":[0.0003524398,0.00016051612,0.00012271694,0.00041663347,0.0009147702,0.00037855777,0.0009479139,0.00030344923,0.000099038014],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00047485207,0.000053740372,0.8726012,0.0001032806,0.000107606225,0.003941235,0.0066528996,0.0014024979,0.09458911,0.004457112,0.0003192297,0.015297117],"study_design_scores_gemma":[0.000016764723,0.0000632155,0.9882681,0.000021302425,0.000029834015,0.00034507195,0.0036153956,0.0016206309,0.00284196,0.00055892253,0.0026034894,0.00001531254],"about_ca_topic_score_codex":0.022092124,"about_ca_topic_score_gemma":0.030459158,"teacher_disagreement_score":0.022092124,"about_ca_system_score_codex":0.0009840549,"about_ca_system_score_gemma":0.0005595269,"threshold_uncertainty_score":0.043927073},"labels":[],"label_agreement":null},{"id":"W4397033804","doi":"10.1029/2024gl108396","title":"Biodiversity and Wetting of Climate Alleviate Vegetation Vulnerability Under Compound Drought‐Hot Extremes","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":37,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Science Foundation of Jiangsu Province; National Natural Science Foundation of China","keywords":"Vegetation (pathology); Biodiversity; Environmental science; Vulnerability (computing); Climate change; Climatology; Physical geography; Geography; Geology; Ecology; Oceanography; Biology","score_opus":0.03168834403539429,"score_gpt":0.2877607049839696,"score_spread":0.25607236094857533,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4397033804","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99792564,0.000020940728,0.0013525271,0.000028935818,0.0000017805507,0.000002043328,0.00008123357,0.000011787969,0.00057503366],"genre_scores_gemma":[0.9997819,0.000007350695,0.00009685939,0.0000025874062,8.22332e-7,0.0000011889312,0.000030421968,0.0000017350577,0.00007713052],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999882,0.000030400126,0.0000054801308,0.000027080032,0.000011956927,0.000043082084],"domain_scores_gemma":[0.9996866,0.000099745135,0.000091842645,0.000023344961,0.000023487524,0.00007503231],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032462212,0.00021326116,0.00023838687,0.00027185507,0.00021809456,0.00066921714,0.00023725518,0.00025612974,0.001528339],"category_scores_gemma":[0.00083557976,0.00012466311,0.0002904282,0.00024498612,0.00033606592,0.0005426076,0.0006596731,0.00020290994,0.00010260369],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035890326,0.00015186096,0.56658274,0.000070351205,0.00031545732,0.00031418406,0.00023437882,0.40041214,0.016578365,0.0033499512,0.0006024426,0.011029222],"study_design_scores_gemma":[0.000011420448,0.00011797865,0.46139622,0.000011595406,0.0000447144,0.000106763466,0.00045584983,0.532216,0.0013432889,0.0038292238,0.00044542263,0.000021510848],"about_ca_topic_score_codex":0.005562479,"about_ca_topic_score_gemma":0.0071268217,"teacher_disagreement_score":0.005562479,"about_ca_system_score_codex":0.00039462114,"about_ca_system_score_gemma":0.00025673973,"threshold_uncertainty_score":0.011060238},"labels":[],"label_agreement":null},{"id":"W4398205071","doi":"10.1029/2024gl109000","title":"Red Line Diffuse‐Like Aurora Driven by Time Domain Structures Associated With Braking Magnetotail Flow Bursts","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Division of Atmospheric and Geospace Sciences; National Aeronautics and Space Administration","keywords":"Line (geometry); Flow (mathematics); Physics; Time domain; Geophysics; Geodesy; Computer science; Geology; Mechanics; Geometry; Mathematics","score_opus":0.008514851459001223,"score_gpt":0.2550773687692752,"score_spread":0.246562517310274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398205071","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99499977,0.00003349154,0.0028972325,0.000045417233,0.0000120367795,0.000009369981,0.00013860995,0.00015355532,0.0017106377],"genre_scores_gemma":[0.99943894,0.000011000302,0.00030172808,0.0000056233844,0.000004440867,0.0000025548566,0.000046741006,0.000007974929,0.00018099569],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999771,0.0000038352737,0.0000011050836,0.000006456074,0.000003676747,0.000007862862],"domain_scores_gemma":[0.9999325,0.000013147479,0.000020223812,0.000009338031,0.000008224086,0.000016535783],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000065679116,0.00021294624,0.00011670147,0.00013406313,0.0001346621,0.00029822532,0.00022990859,0.0002133539,0.0011341149],"category_scores_gemma":[0.00021988041,0.00010230356,0.00024738567,0.00009852089,0.00020948565,0.00019615851,0.00021753841,0.00025711404,0.00009733811],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007622958,0.00030844068,0.21892455,0.00012515369,0.00023201489,0.0021177025,0.00031107763,0.5763616,0.17207313,0.006788637,0.0026157943,0.019379528],"study_design_scores_gemma":[0.00007989286,0.00008802264,0.10907162,0.0000063100565,0.000022351602,0.0002013387,0.000058467922,0.8819828,0.0065126545,0.00079942367,0.001161761,0.00001532732],"about_ca_topic_score_codex":0.002909499,"about_ca_topic_score_gemma":0.0022230367,"teacher_disagreement_score":0.002909499,"about_ca_system_score_codex":0.0002470533,"about_ca_system_score_gemma":0.00011454322,"threshold_uncertainty_score":0.0057851076},"labels":[],"label_agreement":null},{"id":"W4398222301","doi":"10.1029/2023gl107718","title":"M‐ENIAC: A Physics‐Informed Machine Learning Recreation of the First Successful Numerical Weather Forecasts","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"","keywords":"Numerical weather prediction; Meteorology; Weather prediction; Recreation; Computer science; Environmental science; Physics; Political science","score_opus":0.04493113546220205,"score_gpt":0.2966460502263002,"score_spread":0.25171491476409813,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398222301","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.49525544,0.00058471237,0.38866958,0.0052099694,0.0021960963,0.0001429588,0.0028979392,0.0065155737,0.09852777],"genre_scores_gemma":[0.8819358,0.00016467583,0.11031982,0.00043146798,0.00011837379,0.00009678577,0.0010425565,0.0005443531,0.005346158],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999816,0.00005762287,0.000008173003,0.000027065595,0.00006586459,0.00002517532],"domain_scores_gemma":[0.9990934,0.00041930145,0.00005762149,0.00021513486,0.00014877901,0.00006581321],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007067093,0.0002841555,0.0003596554,0.0003348677,0.0004336807,0.00076124235,0.0009182846,0.0008808567,0.004333376],"category_scores_gemma":[0.0035376207,0.0001833463,0.00032850564,0.00037045986,0.0008733681,0.0008919274,0.00086842815,0.0013967421,0.00045141025],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000109569104,0.000082646555,0.0017155862,0.000058857397,0.000030036943,0.0001423687,0.00014833115,0.93981063,0.0016516957,0.033103492,0.008323441,0.014823265],"study_design_scores_gemma":[0.000022969027,0.000015559104,0.00023836075,0.000009629878,0.000002807577,0.000013893115,0.00001770954,0.99025095,0.0007479796,0.0056401864,0.003031883,0.000007996716],"about_ca_topic_score_codex":0.00679675,"about_ca_topic_score_gemma":0.006243629,"teacher_disagreement_score":0.00679675,"about_ca_system_score_codex":0.0005512228,"about_ca_system_score_gemma":0.00090588053,"threshold_uncertainty_score":0.014496565},"labels":[],"label_agreement":null},{"id":"W4398781976","doi":"10.1029/2023gl107386","title":"Reconstructing Glacier Surge Kinematics Using a Numerical Ice‐Flow Model Applied to the Dusty Glacier, St. Elias Mountains, Canada","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Lethbridge; Simon Fraser University","funders":"","keywords":"Surge; Glacier; Geology; Ice stream; Glacier ice accumulation; Kinematics; Tidewater glacier cycle; Geomorphology; Geodesy; Oceanography; Cryosphere; Sea ice; Physics; Ice calving","score_opus":0.060973897696520146,"score_gpt":0.29218171019715883,"score_spread":0.23120781250063868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4398781976","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9957883,0.000037135364,0.0021480343,0.00007109928,0.0000059611198,0.000020591524,0.00046118934,0.00015065879,0.0013171947],"genre_scores_gemma":[0.9976432,0.0000325771,0.0015411503,0.00000880204,0.0000025762092,0.000008554114,0.0003623327,0.000012203011,0.00038865564],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999411,0.0000058010696,0.000002606665,0.000017672879,0.000012781019,0.000020071422],"domain_scores_gemma":[0.9998259,0.000036649875,0.00002518508,0.000017493809,0.000055346576,0.00003949403],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020556769,0.0005569198,0.00030211068,0.00049756933,0.00078146067,0.0007946214,0.00093580567,0.0005304089,0.0007984833],"category_scores_gemma":[0.00070154335,0.00034853362,0.0004635323,0.00048758398,0.0006001733,0.00023053792,0.00032135658,0.00042805172,0.00010507258],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038278034,0.000035227782,0.020056574,0.000008544454,0.000024405737,0.00004689091,0.000045898,0.9759719,0.0010718211,0.00019535887,0.0001887906,0.0023163639],"study_design_scores_gemma":[0.000021250522,0.0000066304483,0.0075762807,0.0000026689977,0.000005573662,0.0000052897944,0.00002826851,0.9920075,0.00021273487,0.000035538244,0.00009318059,0.0000051786624],"about_ca_topic_score_codex":0.90332246,"about_ca_topic_score_gemma":0.82542366,"teacher_disagreement_score":0.09667754,"about_ca_system_score_codex":0.0059076343,"about_ca_system_score_gemma":0.007865785,"threshold_uncertainty_score":0.19449377},"labels":[],"label_agreement":null},{"id":"W4399256691","doi":"10.1029/2024gl108499","title":"South Asian Summer Monsoon Precipitation Is Sensitive to Southern Hemisphere Subtropical Radiation Changes","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Natural Sciences and Engineering Research Council of Canada; Defense Advanced Research Projects Agency; Amazon Web Services; Amazon","keywords":"Subtropics; Climatology; Precipitation; Southern Hemisphere; Monsoon; Subtropical ridge; Environmental science; Northern Hemisphere; South asia; Atmospheric sciences; Geology; Geography; Meteorology; History","score_opus":0.04164788009736815,"score_gpt":0.3147446219438213,"score_spread":0.27309674184645316,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399256691","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982339,0.000035134755,0.00025812775,0.00009764831,0.000006755234,0.000004344246,0.0002813043,0.000040250787,0.0010424068],"genre_scores_gemma":[0.99944144,0.000028756498,0.0001092256,0.00002332277,0.0000039945635,0.0000030092795,0.00027298706,0.0000114315535,0.0001058567],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99979585,0.0000758051,0.000013741614,0.000048589907,0.000028664572,0.00003733527],"domain_scores_gemma":[0.99922717,0.00031333815,0.00014340441,0.000099573575,0.0001234315,0.00009310249],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005741012,0.00041861247,0.0003963424,0.00026794072,0.0003369854,0.0007725117,0.00042124387,0.0004931542,0.0016477056],"category_scores_gemma":[0.0024730265,0.00028012122,0.000644013,0.000575306,0.0002922475,0.0005248201,0.00046189636,0.00047222225,0.00020170645],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042537085,0.00016007334,0.4469895,0.00008289762,0.0005650068,0.00029788932,0.00018516048,0.5299623,0.013150386,0.0006854839,0.0014599557,0.006036057],"study_design_scores_gemma":[0.0001881415,0.00018883267,0.2908728,0.000018376471,0.00017007742,0.00008717984,0.00025454658,0.70070225,0.005318433,0.0009437879,0.001207243,0.000048331316],"about_ca_topic_score_codex":0.050341133,"about_ca_topic_score_gemma":0.027876535,"teacher_disagreement_score":0.050341133,"about_ca_system_score_codex":0.0004911815,"about_ca_system_score_gemma":0.00058546575,"threshold_uncertainty_score":0.100096226},"labels":[],"label_agreement":null},{"id":"W4399588642","doi":"10.1029/2024gl109541","title":"CFC‐12 Emissions in China Inferred From Observation and Inverse Modeling","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Nuclear Safety and Security Commission; National Natural Science Foundation of China; National Key Research and Development Program of China; Massachusetts Institute of Technology; National Aeronautics and Space Administration","keywords":"Greenhouse gas; China; Environmental science; Inversion (geology); Montreal Protocol; Atmospheric sciences; Climatology; Ozone; Emission inventory; Atmospheric research; Meteorology; Ozone layer; Geography; Air quality index; Geology; Oceanography","score_opus":0.06408398431920247,"score_gpt":0.3033411328412252,"score_spread":0.23925714852202273,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399588642","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99736744,0.000065333006,0.0015080974,0.000034153247,0.0000030418837,0.000006126739,0.0004611467,0.000052514373,0.0005020597],"genre_scores_gemma":[0.9982999,0.000059070466,0.0009034752,0.0000072284734,0.0000025313373,0.0000058836945,0.0005770438,0.0000053321583,0.00013959521],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998223,0.000023267885,0.000008406922,0.0000618706,0.000037518723,0.000046544843],"domain_scores_gemma":[0.99985945,0.000028342585,0.000025513471,0.00002240963,0.00005047295,0.0000138539435],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005968064,0.0006501507,0.00033811654,0.0009629719,0.00038167412,0.00047389066,0.00040905768,0.0003669546,0.00033684104],"category_scores_gemma":[0.00037347132,0.0002596232,0.00074721756,0.0013236773,0.00029860626,0.0004544461,0.00039016362,0.00020022926,0.00006871135],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019106743,0.00016290674,0.6514198,0.0001341891,0.000348117,0.00036960526,0.00029617216,0.28652006,0.025724007,0.0009645597,0.0011752378,0.032694265],"study_design_scores_gemma":[0.000042949938,0.000032479424,0.53955525,0.000015254248,0.00012887287,0.00003353492,0.00012436442,0.4539374,0.0045915293,0.00034103895,0.0011436209,0.00005363298],"about_ca_topic_score_codex":0.21754172,"about_ca_topic_score_gemma":0.15524834,"teacher_disagreement_score":0.21754172,"about_ca_system_score_codex":0.0013827902,"about_ca_system_score_gemma":0.0016471862,"threshold_uncertainty_score":0.43255097},"labels":[],"label_agreement":null},{"id":"W4399667899","doi":"10.1029/2023gl107158","title":"More Frequent Spaceborne Sampling of X <sub>CO2</sub> Improves Detectability of Carbon Cycle Seasonal Transitions in Arctic‐Boreal Ecosystems","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Arctic; Environmental science; Sampling (signal processing); Satellite; Boreal; Atmospheric sciences; Carbon cycle; Ecosystem; Climatology; Flux (metallurgy); Greenhouse gas; Carbon flux; Remote sensing; Oceanography; Geology; Detector; Computer science; Ecology; Physics; Astronomy","score_opus":0.014401389893389441,"score_gpt":0.2663686126611877,"score_spread":0.25196722276779826,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399667899","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976126,0.000018349345,0.0017435403,0.00003934997,0.0000036085996,0.000003911786,0.00005027335,0.000054216955,0.0004740939],"genre_scores_gemma":[0.9976266,0.000011876739,0.0022056904,0.000013027089,0.0000018987583,0.0000023588548,0.000058387708,0.000006517282,0.00007363616],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99992895,0.000019780442,0.0000026187554,0.000020440248,0.000011709313,0.000016544242],"domain_scores_gemma":[0.9997478,0.00013603714,0.00003685963,0.000026361287,0.000031588086,0.000021360485],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00049139385,0.00031931195,0.0002274622,0.00016557478,0.00027208924,0.00035762668,0.00028234778,0.0002866903,0.0009548418],"category_scores_gemma":[0.0006991649,0.00012659318,0.000256566,0.0002485472,0.00031340902,0.0006660298,0.00025443183,0.00026281577,0.00008076521],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008905748,0.0004990377,0.14537352,0.000070647766,0.00015233905,0.00010279504,0.00009163083,0.75173914,0.070733525,0.0006591417,0.00057595986,0.0291117],"study_design_scores_gemma":[0.000081946426,0.00023362182,0.044909913,0.000004694064,0.00003513019,0.000027216676,0.00005995986,0.9423751,0.011781744,0.0002283663,0.0002484779,0.000013757258],"about_ca_topic_score_codex":0.023537256,"about_ca_topic_score_gemma":0.028203396,"teacher_disagreement_score":0.023537256,"about_ca_system_score_codex":0.00036353013,"about_ca_system_score_gemma":0.00031920636,"threshold_uncertainty_score":0.046800494},"labels":[],"label_agreement":null},{"id":"W4399669900","doi":"10.1029/2024gl109664","title":"Investigating Catchment‐Scale Daily Snow Depths of CMIP6 in Canada","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"National Research Council Canada; Concordia University; University of Calgary","funders":"Global Water Futures; National Research Council Canada; Natural Sciences and Engineering Research Council of Canada; Killam Trusts; Grantová Agentura České Republiky","keywords":"Snow; Scale (ratio); Geology; Drainage basin; Climatology; Environmental science; Hydrology (agriculture); Physical geography; Geomorphology; Geography; Cartography","score_opus":0.03961134689297843,"score_gpt":0.2791262743993746,"score_spread":0.23951492750639616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399669900","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9910014,0.00011693765,0.0005645268,0.000277891,0.00001094954,0.0000204594,0.0047285967,0.00016522635,0.0031139597],"genre_scores_gemma":[0.99696666,0.00005846483,0.0005298299,0.000035748377,0.000002146423,0.000006500709,0.0020394335,0.00001717023,0.0003441152],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998273,0.00001386164,0.0000059335466,0.00004190074,0.000047634327,0.00006327155],"domain_scores_gemma":[0.9995401,0.00005546463,0.000032211046,0.000028574388,0.00026618378,0.00007755592],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0004877623,0.0004695694,0.00018964923,0.00047998186,0.0008668057,0.00088160654,0.00096868403,0.0004795664,0.0012575944],"category_scores_gemma":[0.0013673343,0.00018974202,0.00044570782,0.0011379112,0.00041875735,0.00045738003,0.0004823412,0.00040309652,0.0001373604],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033791925,0.000137893,0.5569937,0.00013651336,0.00027209084,0.00023792691,0.00063898775,0.40551823,0.0039918195,0.0021602446,0.008472643,0.021102088],"study_design_scores_gemma":[0.00008384355,0.00003434451,0.4710782,0.00005847761,0.00007945616,0.000049418282,0.000996893,0.51597464,0.0031035198,0.0005158188,0.007951969,0.00007341062],"about_ca_topic_score_codex":0.9821348,"about_ca_topic_score_gemma":0.9775038,"teacher_disagreement_score":0.017865181,"about_ca_system_score_codex":0.0129901925,"about_ca_system_score_gemma":0.009979282,"threshold_uncertainty_score":0.09425086},"labels":[],"label_agreement":null},{"id":"W4399780519","doi":"10.1029/2024gl109173","title":"Quantifying Seepage‐Face Evaporation and Its Effects on Groundwater Flow and Solute Transport in Small‐Slope Tidal Flat","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater flow and contamination studies","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Shenzhen Science and Technology Innovation Program; Shenzhen Graduate School, Peking University; Southern University of Science and Technology; National Natural Science Foundation of China","keywords":"Groundwater; Groundwater flow; Evaporation; Geology; Flow (mathematics); Hydrology (agriculture); Environmental science; Soil science; Geotechnical engineering; Aquifer; Mechanics; Meteorology","score_opus":0.044120832667303225,"score_gpt":0.2979928417666235,"score_spread":0.2538720090993203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399780519","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992494,0.000013117063,0.0005426998,0.000003858094,6.196715e-7,0.0000036469887,0.000036925114,0.0000081749495,0.00014147663],"genre_scores_gemma":[0.99964523,0.000017714383,0.00026380978,0.000002073014,4.639635e-7,0.0000021654773,0.00003079342,0.0000011122053,0.000036557143],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993455,0.000011594891,0.000004208664,0.00001536828,0.0000148550735,0.000019385645],"domain_scores_gemma":[0.99986446,0.00005759506,0.000032105218,0.000009605504,0.000017855957,0.000018368924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000140103,0.0002369109,0.0002284581,0.00036637782,0.0002363187,0.0003817116,0.00018158545,0.0002824665,0.0003753506],"category_scores_gemma":[0.00038124065,0.00013777321,0.00028514984,0.00043926743,0.000310127,0.00041472728,0.00030273577,0.00016007134,0.000042245763],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00044830955,0.00034469957,0.48354867,0.00011435191,0.00013850153,0.00067661353,0.00016948942,0.30158004,0.19275741,0.0008721419,0.00016183902,0.019187957],"study_design_scores_gemma":[0.000028034881,0.000190281,0.48476127,0.000006618943,0.000041952142,0.0000759272,0.00018712653,0.48962352,0.024398163,0.0004835268,0.00017063138,0.000033007786],"about_ca_topic_score_codex":0.013498537,"about_ca_topic_score_gemma":0.0128360335,"teacher_disagreement_score":0.013498537,"about_ca_system_score_codex":0.0004850314,"about_ca_system_score_gemma":0.000317487,"threshold_uncertainty_score":0.026839972},"labels":[],"label_agreement":null},{"id":"W4399859946","doi":"10.1029/2024gl108578","title":"On the Duration of Tropical Cyclone Rapid Intensification","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"Hohai University","keywords":"Tropical cyclone; Environmental science; Meteorology; Climatology; Duration (music); Intensity (physics); Atmospheric sciences; Geography; Physics; Geology","score_opus":0.04956982469873088,"score_gpt":0.29904666493477583,"score_spread":0.24947684023604494,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399859946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99479914,0.00028757748,0.00054850196,0.000068343754,0.000016764705,0.000008952533,0.0005817485,0.000016966562,0.0036720037],"genre_scores_gemma":[0.9994106,0.00006890295,0.00007763563,0.000008366173,0.000011693515,0.0000034105967,0.0002873345,0.0000018954283,0.00013019166],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998714,0.000013925533,0.000009702805,0.000039562852,0.00003653805,0.000028868219],"domain_scores_gemma":[0.99876463,0.00039048147,0.00042019287,0.000050483988,0.00022796239,0.00014627876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003554,0.00013449015,0.00013484071,0.0004969287,0.00018631118,0.00042160143,0.0001281506,0.00020367249,0.0015152292],"category_scores_gemma":[0.0016548794,0.00008087504,0.00009691263,0.00030396608,0.00015277897,0.0002971219,0.00033119463,0.00034215298,0.00017377149],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004849242,0.000069221634,0.9435185,0.000119379314,0.00011774145,0.00030268205,0.00031685343,0.016825873,0.00799887,0.0009338089,0.0010561253,0.028256046],"study_design_scores_gemma":[0.0000050116314,0.000068596695,0.9894057,0.00003020243,0.000021106804,0.000054957694,0.00022797413,0.00800052,0.0008735013,0.00014214175,0.0011615288,0.0000088184825],"about_ca_topic_score_codex":0.00566034,"about_ca_topic_score_gemma":0.0067928885,"teacher_disagreement_score":0.00566034,"about_ca_system_score_codex":0.00029539052,"about_ca_system_score_gemma":0.00018410028,"threshold_uncertainty_score":0.011254787},"labels":[],"label_agreement":null},{"id":"W4399982222","doi":"10.1029/2023gl105660","title":"Evolution of Energetic Proton Parallel Pressure Anisotropy at Geosynchronous Altitudes: Potential Role in Triggering Substorm Expansion Phase Onset","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science and Technology Facilities Council; Canadian Space Agency; Natural Environment Research Council; Sight Research UK","keywords":"Substorm; Geosynchronous orbit; Proton; Anisotropy; Geophysics; Phase (matter); Physics; Atmospheric sciences; Magnetosphere; Geology; Nuclear physics; Astronomy; Plasma; Optics","score_opus":0.00916793462896525,"score_gpt":0.2843103038482955,"score_spread":0.2751423692193302,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4399982222","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9970716,0.00010410834,0.00074366096,0.000053952055,0.0000059690074,0.000005412323,0.0004704831,0.000040277682,0.0015044822],"genre_scores_gemma":[0.99949276,0.000026050977,0.00014076957,0.000006456493,0.0000052128044,0.000002318327,0.00023578265,0.0000043537125,0.00008631857],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999504,0.0000062296826,0.0000032018766,0.000014366027,0.000009782215,0.000015993191],"domain_scores_gemma":[0.9997111,0.000042506148,0.00011489835,0.000022459746,0.000056615634,0.00005244956],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023230555,0.00014717107,0.00016552284,0.000638181,0.0002521824,0.00053816615,0.00012921814,0.00019045835,0.0014301552],"category_scores_gemma":[0.0006230168,0.00008353291,0.00015935558,0.000501995,0.00020358298,0.00037687927,0.00038332448,0.00022084966,0.00016917071],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00027321387,0.000036812817,0.93061376,0.000045559707,0.00007922184,0.00035598513,0.0002931034,0.0021476073,0.05412445,0.0012335501,0.0007253794,0.010071366],"study_design_scores_gemma":[0.000004294531,0.000017290959,0.9949503,0.000004404834,0.000013480064,0.000034886285,0.00007358317,0.0027121706,0.0015751213,0.00015232488,0.00045869997,0.0000034951272],"about_ca_topic_score_codex":0.0069737253,"about_ca_topic_score_gemma":0.0063389754,"teacher_disagreement_score":0.0069737253,"about_ca_system_score_codex":0.00028844114,"about_ca_system_score_gemma":0.00015444259,"threshold_uncertainty_score":0.013866246},"labels":[],"label_agreement":null},{"id":"W4400089821","doi":"10.1029/2024gl108444","title":"Intensification of Mid‐Latitude Cyclone by Aerosol‐Radiation Interaction Increases Transport of Canadian Wildfire Smoke to Northeastern US","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Environmental science; Smoke; Radiative forcing; Cyclone (programming language); Atmospheric sciences; Climatology; Aerosol; Atmosphere (unit); Forcing (mathematics); Middle latitudes; Meteorology; Geology; Geography","score_opus":0.01929415816301767,"score_gpt":0.27939351835202203,"score_spread":0.26009936018900437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400089821","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99678135,0.00018749686,0.00008425064,0.00028081486,0.000013243234,0.0000044374,0.0010020079,0.000014578941,0.0016318581],"genre_scores_gemma":[0.9986883,0.00009980949,0.000045725363,0.00003920957,0.0000035374164,0.0000014238674,0.00037696637,0.0000026854611,0.00074236194],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998987,0.000007743077,0.0000028683314,0.00002544716,0.000022755738,0.000042461936],"domain_scores_gemma":[0.9996308,0.00003104565,0.00006311058,0.000016257289,0.00014644292,0.0001122136],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014688045,0.00018835459,0.00015964486,0.00040391236,0.0007171545,0.0006992582,0.00031790498,0.0001987434,0.003599443],"category_scores_gemma":[0.00055907806,0.00008976464,0.00034898665,0.0004912873,0.00015871458,0.00019312017,0.000401593,0.0003465726,0.000106364954],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000112804504,0.000030763338,0.9886778,0.00001787223,0.000082028375,0.000113273556,0.00017393914,0.0006388111,0.0021078829,0.00018433288,0.001564912,0.006295446],"study_design_scores_gemma":[0.0000020938978,0.0000064589167,0.99810165,0.000004237,0.000019607241,0.000014152539,0.00028402935,0.00075754855,0.00018603401,0.000024239018,0.0005961943,0.0000037569973],"about_ca_topic_score_codex":0.96516734,"about_ca_topic_score_gemma":0.9738952,"teacher_disagreement_score":0.034832656,"about_ca_system_score_codex":0.0043080887,"about_ca_system_score_gemma":0.006617941,"threshold_uncertainty_score":0.07007551},"labels":[],"label_agreement":null},{"id":"W4400111872","doi":"10.1029/2023gl107675","title":"Atmospheric Escape From Earth and Mars: Response to Solar and Solar Wind Drivers of Oxygen Escape","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Solar and Space Plasma Dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Canadian Space Agency; National Research Council Canada; NASA Headquarters; National Aeronautics and Space Administration","keywords":"Mars Exploration Program; Astrobiology; Environmental science; Solar wind; Atmospheric sciences; Atmospheric escape; Atmosphere of Mars; Martian; Geology; Physics","score_opus":0.010966386218534028,"score_gpt":0.268414239481195,"score_spread":0.257447853262661,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400111872","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99918646,0.000026344274,0.00005186479,0.00004160694,0.0000019728343,0.0000019585088,0.00019556066,0.000005216438,0.00048894016],"genre_scores_gemma":[0.99935895,0.000015411873,0.00002405342,0.000008813041,0.000003128569,0.0000019748582,0.00034928333,0.0000041582525,0.00023421625],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998896,0.000023710802,0.00000582962,0.000032079857,0.000019590489,0.000029239252],"domain_scores_gemma":[0.99891126,0.00039162656,0.0003285552,0.000049165097,0.000116518204,0.00020289436],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00027394306,0.00014239438,0.00024397633,0.0003425995,0.0002078599,0.0006795216,0.00019327343,0.00026050862,0.002612461],"category_scores_gemma":[0.0016889964,0.00009475862,0.00026217033,0.00034367657,0.00012106926,0.0002852241,0.00058667257,0.00031830408,0.00024646067],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041559234,0.000061022165,0.9868841,0.000017790197,0.00011914712,0.000093723116,0.00023005293,0.0014214538,0.006990335,0.0001411652,0.0003727794,0.0032528387],"study_design_scores_gemma":[0.0000028543245,0.000029696745,0.99816376,0.0000015920743,0.0000065418567,0.000020513191,0.00014427582,0.0012197951,0.00015412927,0.000045331602,0.00020858126,0.000002993761],"about_ca_topic_score_codex":0.0038884215,"about_ca_topic_score_gemma":0.0033775286,"teacher_disagreement_score":0.0038884215,"about_ca_system_score_codex":0.00014607399,"about_ca_system_score_gemma":0.00008286078,"threshold_uncertainty_score":0.008739591},"labels":[],"label_agreement":null},{"id":"W4400283785","doi":"10.1029/2024gl109326","title":"Picky Eaters: Carbon Isotopic Evidence for the Uniform Bioavailability of Riverine Dissolved Organic Matter to a Model Marine Microorganism","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Microbial Community Ecology and Physiology","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Ottawa; McGill University","funders":"Canada Research Chairs","keywords":"Dissolved organic carbon; Environmental chemistry; Bioavailability; Environmental science; Organic matter; Carbon cycle; Biogeochemistry; Total organic carbon; Chemistry; Ecology; Biology; Ecosystem","score_opus":0.055876606935847305,"score_gpt":0.33188794262301247,"score_spread":0.2760113356871652,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400283785","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99908173,0.000092809714,0.00042989597,0.0000125984825,0.000001929289,0.0000032636412,0.0001426084,0.000006706579,0.00022843918],"genre_scores_gemma":[0.9975852,0.00009147748,0.0012012103,0.000029171446,0.000001983297,0.000008974635,0.00030421157,0.0000057873185,0.0007719189],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99988663,0.000015717398,0.000008289749,0.0000477109,0.000023713761,0.00001792188],"domain_scores_gemma":[0.99980694,0.00003052625,0.000059367227,0.000026850012,0.00004443814,0.000031901058],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014214679,0.00020840703,0.00013297572,0.00027566546,0.00027393104,0.00032952536,0.00015796149,0.00028331773,0.0006579602],"category_scores_gemma":[0.00022675694,0.0001329737,0.0001141165,0.00018449916,0.00020089919,0.0001499749,0.000269352,0.00019385792,0.000114233975],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000111058645,0.000023762874,0.010123565,0.000014198772,0.000008579741,0.00004913101,0.00004246075,0.000052771647,0.9886367,0.000038475868,0.000020163863,0.0008791233],"study_design_scores_gemma":[0.0000125975885,0.00043599904,0.2594572,0.000009016081,0.000036835023,0.0003312207,0.00032669195,0.0021854492,0.73573136,0.00012277158,0.0013361911,0.000014655021],"about_ca_topic_score_codex":0.0038828864,"about_ca_topic_score_gemma":0.005328661,"teacher_disagreement_score":0.0038828864,"about_ca_system_score_codex":0.00016732344,"about_ca_system_score_gemma":0.00009166857,"threshold_uncertainty_score":0.0077205896},"labels":[],"label_agreement":null},{"id":"W4400368544","doi":"10.1029/2023gl106847","title":"The Role of Continental Alkaline Magmatism in Mantle Carbon Outflux Constrained by a Machine Learning Analysis of Zircon","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Queen's University","funders":"Fundamental Research Funds for the Central Universities; National Natural Science Foundation of China","keywords":"Magmatism; Geology; Zircon; Geochemistry; Mantle (geology); Earth science; Paleontology","score_opus":0.010228318338553066,"score_gpt":0.2481295053569018,"score_spread":0.23790118701834875,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400368544","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9927644,0.00011845367,0.0063054184,0.0000319159,0.0000043983177,0.0000032996022,0.0002625592,0.000060126855,0.000449324],"genre_scores_gemma":[0.99788576,0.00002793558,0.0016901504,0.0000039756696,0.0000038887915,0.0000015572717,0.00026723935,0.0000054544957,0.00011392266],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999052,0.000015740761,0.000007733874,0.00003767207,0.000013992554,0.000019623425],"domain_scores_gemma":[0.99971765,0.00009872829,0.000076551354,0.00003797113,0.000050950784,0.000018158955],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005093429,0.00032879485,0.0002504125,0.001102181,0.00023762985,0.0005920731,0.00023737192,0.00024874826,0.0005880923],"category_scores_gemma":[0.0007819932,0.00010343024,0.00045120265,0.0006647612,0.00019195276,0.00024538493,0.0003413209,0.00018902152,0.00016890703],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003215179,0.00009054466,0.7495966,0.000063757725,0.00029312292,0.00017654225,0.000097829405,0.043785334,0.14060703,0.0008130657,0.000334736,0.063819855],"study_design_scores_gemma":[0.000013682265,0.00007340583,0.5835638,0.000008734331,0.000089121946,0.0001223023,0.000082849736,0.39159676,0.022795245,0.00070855033,0.00092540437,0.000020130048],"about_ca_topic_score_codex":0.0036166732,"about_ca_topic_score_gemma":0.0044970117,"teacher_disagreement_score":0.0036166732,"about_ca_system_score_codex":0.00028065802,"about_ca_system_score_gemma":0.00019812185,"threshold_uncertainty_score":0.007191241},"labels":[],"label_agreement":null},{"id":"W4400884224","doi":"10.1029/2024gl109061","title":"Influence of Western Pacific Madden–Julian Oscillation on New York City's Record‐Breaking Air Pollution in Early June 2023","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Madden–Julian oscillation; Teleconnection; Climatology; Anomaly (physics); Environmental science; Smoke; Pollution; Oceanography; El Niño Southern Oscillation; Geology; Meteorology; Convection; Geography","score_opus":0.046564336233199284,"score_gpt":0.3082322247797051,"score_spread":0.2616678885465058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400884224","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9951729,0.00011221834,0.00006075472,0.0006653338,0.000047790818,0.0000075877124,0.0023831928,0.000014499071,0.0015357523],"genre_scores_gemma":[0.9977946,0.00008880706,0.00006104656,0.00006120885,0.000022336215,0.0000062468457,0.001508283,0.0000043617792,0.00045301035],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992,0.0000107519645,0.0000061735627,0.000017725453,0.000022326572,0.000023003857],"domain_scores_gemma":[0.9992836,0.00009248517,0.00017602312,0.000033656946,0.00022944612,0.00018481015],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025232142,0.00020723081,0.00017545692,0.00033219645,0.0006823614,0.0010629076,0.00029243788,0.000462968,0.0018404751],"category_scores_gemma":[0.0010740075,0.000112028916,0.00022198692,0.00055984536,0.0001848311,0.00031363918,0.0004764895,0.00059604325,0.00019040298],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015349984,0.000059295893,0.9890793,0.00001777188,0.00007106278,0.00019691921,0.0002123579,0.0019859099,0.0010603648,0.00014186927,0.0037602303,0.0032614595],"study_design_scores_gemma":[0.000004904064,0.000011781495,0.99382555,0.000009888879,0.000015600774,0.000013945048,0.00031300017,0.0043611187,0.00017404028,0.000019378884,0.0012446737,0.000006137287],"about_ca_topic_score_codex":0.64785177,"about_ca_topic_score_gemma":0.7743752,"teacher_disagreement_score":0.64785177,"about_ca_system_score_codex":0.002361481,"about_ca_system_score_gemma":0.0017273955,"threshold_uncertainty_score":0.70844424},"labels":[],"label_agreement":null},{"id":"W4400902982","doi":"10.1029/2024gl109758","title":"Seismic Azimuthal Anisotropy Beneath the Alaska Subduction Zone","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Division of Earth Sciences; Jackson School of Geosciences,University of Texas at Austin","keywords":"Subduction; Geology; Forearc; Trench; Seismology; Slab; Anisotropy; Seismic anisotropy; Oceanic crust; Geophysics; Mantle (geology); Tectonics","score_opus":0.02716272558627448,"score_gpt":0.281999108938103,"score_spread":0.2548363833518285,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4400902982","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99836487,0.000085827116,0.00026520932,0.000012582434,0.0000032044213,0.0000014474222,0.0007074451,0.00003985246,0.0005195563],"genre_scores_gemma":[0.9985172,0.00005094642,0.0002815433,0.0000022584697,0.0000019904674,0.0000012558259,0.0010016424,0.0000029599078,0.00014025967],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999254,0.000008942203,0.0000084358835,0.000028693014,0.00001636248,0.000012228547],"domain_scores_gemma":[0.9998223,0.000019772788,0.000044579152,0.000026661093,0.000052343057,0.00003431622],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023163891,0.00028439699,0.00018430718,0.0008556805,0.00023316186,0.0004243299,0.00016116686,0.00019504825,0.00078675937],"category_scores_gemma":[0.00053416,0.00018707699,0.00022928798,0.00057500514,0.00015094245,0.00029758655,0.00042784942,0.00018534111,0.00024081454],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00020560807,0.000039027993,0.9476522,0.000036964215,0.00013980594,0.00013267828,0.00033333883,0.021969922,0.013955997,0.00014935256,0.0003422074,0.01504288],"study_design_scores_gemma":[0.000009444198,0.000019841942,0.972389,0.000015419193,0.000038307084,0.0000522331,0.00022867892,0.024906646,0.0014948894,0.00008249141,0.00074962917,0.000013452362],"about_ca_topic_score_codex":0.043918442,"about_ca_topic_score_gemma":0.06156921,"teacher_disagreement_score":0.043918442,"about_ca_system_score_codex":0.00024813638,"about_ca_system_score_gemma":0.00032408437,"threshold_uncertainty_score":0.08732557},"labels":[],"label_agreement":null},{"id":"W4401113089","doi":"10.1029/2023gl106689","title":"Freshwater Biogeochemical Hotspots: High Primary Production and Ecosystem Respiration in Shallow Waterbodies","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Aquatic Ecosystems and Phytoplankton Dynamics","field":"Environmental Science","cited_by":21,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ducks Unlimited Canada","funders":"California Department of Fish and Wildlife; Institute for Wetland and Waterfowl Research, Ducks Unlimited Canada; Marine Institute; Washington Department of Fish and Wildlife; St. Olaf College; Just Beginnings Collaborative; Middlebury College; Global Lake Ecological Observatory Network; Augsburg University; National Science Foundation; Macalester College; University of Minnesota; U.S. Department of Energy; U.S. Geological Survey; Ducks Unlimited Canada; Biological and Environmental Research; Professional Beauty Association","keywords":"Biogeochemical cycle; Environmental science; Ecosystem; Primary production; Freshwater ecosystem; Respiration; Oceanography; Biogeochemistry; Ecology; Geology; Biology","score_opus":0.017409584981270206,"score_gpt":0.2588548885421753,"score_spread":0.2414453035609051,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401113089","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9998036,0.0000109928615,0.000055580877,0.0000026045623,1.4032341e-7,6.640028e-7,0.000036511818,0.0000022074025,0.00008776832],"genre_scores_gemma":[0.9998888,0.000005519832,0.000037328133,0.0000019038135,3.418265e-7,6.748256e-7,0.00003774841,6.83819e-7,0.000026957461],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999236,0.00001454538,0.0000073541137,0.000022121681,0.000013736399,0.00001862328],"domain_scores_gemma":[0.999653,0.00006209388,0.00016166823,0.000023570723,0.00003392666,0.00006572459],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001731932,0.00012371798,0.00023866977,0.00074381876,0.0002989461,0.0004687135,0.00013267898,0.00017145902,0.0006273294],"category_scores_gemma":[0.00039717052,0.00013094099,0.00015509606,0.00073589187,0.00043823267,0.00029212216,0.0005523136,0.00008080751,0.000058959562],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000050481158,0.00000871322,0.9891192,0.000011825909,0.00003132044,0.00007836561,0.00018083067,0.00025424018,0.0080380915,0.00003088009,0.000028872239,0.0021671627],"study_design_scores_gemma":[5.5137394e-7,0.0000047017697,0.9996424,7.590877e-7,0.0000027435067,0.000015047557,0.000061582585,0.00013208824,0.00010228728,0.00001746438,0.000019453126,9.4769126e-7],"about_ca_topic_score_codex":0.010493002,"about_ca_topic_score_gemma":0.02170603,"teacher_disagreement_score":0.010493002,"about_ca_system_score_codex":0.00031617997,"about_ca_system_score_gemma":0.0001617471,"threshold_uncertainty_score":0.02086389},"labels":[],"label_agreement":null},{"id":"W4401224245","doi":"10.1029/2024gl109308","title":"Pressure Dependence of Permeability in Cracked Rocks: Experimental Evidence of Non‐Linear Pore‐Pressure Gradients From Local Measurements","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Institut national des sciences de l'Univers; Centre National de la Recherche Scientifique; China Scholarship Council","keywords":"Geology; Permeability (electromagnetism); Pore water pressure; Fluid dynamics; Brittleness; Linearity; Mineralogy; Materials science; Geotechnical engineering; Mechanics; Composite material; Chemistry","score_opus":0.0765959401472368,"score_gpt":0.33700452324149693,"score_spread":0.2604085830942601,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401224245","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99295276,0.0001204861,0.0063735475,0.000015258529,0.0000019521901,0.000007969179,0.00009101509,0.000049358354,0.0003877118],"genre_scores_gemma":[0.99903655,0.000031222506,0.0008385184,0.0000027631904,6.622089e-7,0.0000044190333,0.000027023301,0.0000053728645,0.000053323773],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99978393,0.000022622873,0.000014949812,0.00005233506,0.00009569773,0.0000305633],"domain_scores_gemma":[0.9991455,0.00040484552,0.00016057643,0.00012401782,0.000119774355,0.000045272493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025122342,0.00016066252,0.00019149028,0.0003102867,0.00017782005,0.00023471472,0.0003578951,0.00027575353,0.00084136904],"category_scores_gemma":[0.0010893258,0.00024992594,0.00007365551,0.00022063937,0.0006473137,0.00046030106,0.00036516905,0.00052102905,0.000094360876],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005640364,0.000016148173,0.0024467097,0.00003871098,0.000005110339,0.00004495737,0.000065902175,0.0005741776,0.99492353,0.000060151975,0.00001227308,0.0017559616],"study_design_scores_gemma":[0.000009848281,0.00015782965,0.048517015,0.0000057654825,0.000009397905,0.00016650591,0.00006737514,0.011846706,0.9389114,0.00011503561,0.00018101836,0.000012029024],"about_ca_topic_score_codex":0.0005748585,"about_ca_topic_score_gemma":0.00076591864,"teacher_disagreement_score":0.00084136904,"about_ca_system_score_codex":0.00012130696,"about_ca_system_score_gemma":0.000075461125,"threshold_uncertainty_score":0.0028147101},"labels":[],"label_agreement":null},{"id":"W4401224797","doi":"10.1029/2023gl107474","title":"Large Isotopic Shift in Volcanic Plume CO <sub>2</sub> Prior to a Basaltic Paroxysmal Explosion","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Ministero dell'Università e della Ricerca; Ministero dell’Istruzione, dell’Università e della Ricerca","keywords":"Volcano; Plume; Magma; Geology; Basalt; Geochemistry; Carbon dioxide; Isotopic signature; Earth science; Isotope; Chemistry; Meteorology","score_opus":0.026423200012431054,"score_gpt":0.27670027973598244,"score_spread":0.2502770797235514,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401224797","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99901557,0.000053783624,0.00010212969,0.000024391407,0.00000623454,0.0000015765279,0.00021830139,0.000013499318,0.00056451204],"genre_scores_gemma":[0.9992901,0.0000242764,0.00008111503,0.000016812435,0.0000047502126,0.000002008587,0.0003311294,0.0000064628216,0.000243203],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999523,0.000003047174,0.0000016048263,0.000016893546,0.000011941632,0.00001427126],"domain_scores_gemma":[0.9998735,0.000016488575,0.000030748008,0.000007424587,0.000042871587,0.000028874669],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008030191,0.00016661163,0.00017802873,0.0005426994,0.0003153891,0.00040068556,0.00018502945,0.00031580703,0.0012330802],"category_scores_gemma":[0.00023601021,0.000117960364,0.00008823836,0.00029612138,0.0002444807,0.00016857896,0.00021851253,0.00027455387,0.00020110882],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008060228,0.000071467635,0.4453364,0.000033314715,0.000049934817,0.0008470978,0.00043525707,0.00028508905,0.54450047,0.000092869406,0.00038673618,0.007155316],"study_design_scores_gemma":[0.000002209998,0.000045165787,0.98553187,0.0000027417996,0.000008207296,0.00012760187,0.00015773793,0.00035580824,0.013298494,0.00002341906,0.00044205843,0.0000046569844],"about_ca_topic_score_codex":0.007861079,"about_ca_topic_score_gemma":0.015478303,"teacher_disagreement_score":0.007861079,"about_ca_system_score_codex":0.00032664312,"about_ca_system_score_gemma":0.00013437055,"threshold_uncertainty_score":0.015630662},"labels":[],"label_agreement":null},{"id":"W4401276624","doi":"10.1029/2024gl109756","title":"Solar Wind Drivers of Auroral Omega Bands","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Solar wind; Magnetosphere; Ionosphere; Omega; Ring current; Physics; Geophysics; Mesoscale meteorology; Earth's magnetic field; Geomagnetic storm; Geology; Astrophysics; Magnetic field; Meteorology","score_opus":0.015530390814315505,"score_gpt":0.2911955205237056,"score_spread":0.2756651297093901,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401276624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99861276,0.000037543734,0.00008009841,0.000010967545,0.0000025932463,0.0000026163736,0.0003671608,0.000006034437,0.00088016293],"genre_scores_gemma":[0.9992403,0.000034531626,0.000057410376,0.000003569888,0.000006546689,0.0000018747332,0.0004933359,0.0000025605584,0.00015984358],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993503,0.000006410366,0.000004900938,0.000019009578,0.000015790938,0.000018869634],"domain_scores_gemma":[0.9995425,0.00006763732,0.00021805584,0.000036342222,0.00006928277,0.00006626131],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013231776,0.000091783775,0.00013881749,0.00060946145,0.00016729312,0.00048098262,0.000084918436,0.000098248725,0.0012127854],"category_scores_gemma":[0.0004925404,0.00007782523,0.00012887016,0.00051255996,0.00014297315,0.00022046253,0.00037593034,0.00014811671,0.0001476245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011444637,0.000015715852,0.9885062,0.000013058829,0.00002890323,0.00013408673,0.0001710737,0.00026962688,0.006006913,0.00012705543,0.00029182184,0.0043211738],"study_design_scores_gemma":[6.464335e-7,0.000004346371,0.999474,0.0000015130973,0.0000026775808,0.000022531985,0.000045170527,0.00016311987,0.000105771855,0.000013254375,0.00016614085,8.6496334e-7],"about_ca_topic_score_codex":0.0030720823,"about_ca_topic_score_gemma":0.0060039023,"teacher_disagreement_score":0.0030720823,"about_ca_system_score_codex":0.00016882428,"about_ca_system_score_gemma":0.000100933976,"threshold_uncertainty_score":0.006108403},"labels":[],"label_agreement":null},{"id":"W4401368546","doi":"10.1029/2024gl109369","title":"Reactive Nitrogen Partitioning Enhances the Contribution of Canadian Wildfire Plumes to US Ozone Air Quality","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":14,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Office of Experimental Program to Stimulate Competitive Research; National Oceanic and Atmospheric Administration; National Science Foundation","keywords":"Ozone; Air quality index; Environmental science; Reactive nitrogen; Atmospheric sciences; Nitrogen; Nitrogen oxides; Meteorology; Nitrogen dioxide; Climatology; Geology; Chemistry; Geography; Waste management","score_opus":0.02122069489574297,"score_gpt":0.3099313993926752,"score_spread":0.28871070449693226,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401368546","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9984127,0.00003584799,0.0005222878,0.00003299585,0.0000042977713,0.0000060053867,0.00019258125,0.000038262497,0.00075510715],"genre_scores_gemma":[0.99935883,0.00002183484,0.0002659797,0.000010500145,7.629149e-7,0.0000015243209,0.00018679774,0.000004907512,0.0001489405],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99986815,0.000010057336,0.0000040133214,0.000040148283,0.000029674266,0.00004785301],"domain_scores_gemma":[0.9999163,0.00001253496,0.000010861416,0.0000074514637,0.000034241082,0.000018623037],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021448632,0.0005082001,0.00018239461,0.0002632564,0.00067960325,0.000597632,0.00047335072,0.0002369301,0.0006960141],"category_scores_gemma":[0.00032885282,0.00020710341,0.00042622574,0.00027453448,0.00028574368,0.00033495203,0.00038980372,0.00032208933,0.00004509265],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006383755,0.00029451135,0.5363175,0.00007027514,0.0004272671,0.0002186868,0.0002049611,0.3587718,0.080487914,0.0013040433,0.0016611298,0.019603483],"study_design_scores_gemma":[0.000075247524,0.00011083625,0.50832456,0.000010246832,0.00013321512,0.000047390582,0.0003077743,0.469871,0.019177942,0.00043823567,0.0014540508,0.000049468028],"about_ca_topic_score_codex":0.851844,"about_ca_topic_score_gemma":0.8529551,"teacher_disagreement_score":0.14815599,"about_ca_system_score_codex":0.0035680619,"about_ca_system_score_gemma":0.0026025034,"threshold_uncertainty_score":0.29805696},"labels":[],"label_agreement":null},{"id":"W4401646871","doi":"10.1029/2024gl110317","title":"Future Changes in the Winter Beaufort High Under Warming Climate Scenarios","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Fisheries and Oceans Canada; Dalhousie University","keywords":"Beaufort sea; Environmental science; Climatology; Beaufort scale; Climate change; Global warming; Warming up; Climate simulation; Climate model; Oceanography; Geology; Sea ice","score_opus":0.05880560728233291,"score_gpt":0.3167688425327207,"score_spread":0.2579632352503878,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401646871","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9938305,0.00018198245,0.0005205511,0.00036334258,0.00003971117,0.0000038767794,0.0015150137,0.00005079068,0.0034942916],"genre_scores_gemma":[0.9988135,0.00004689136,0.0001765247,0.000030159234,0.0000131225,0.0000027998306,0.00072058005,0.000004991624,0.00019151672],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998319,0.00004613549,0.000008477062,0.000026085401,0.00003083876,0.000056504985],"domain_scores_gemma":[0.999706,0.00003994316,0.00008766749,0.000019981266,0.00008756571,0.00005875465],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005052138,0.00026366307,0.00018597947,0.00041161614,0.00031431508,0.0011067447,0.00027131496,0.0005723651,0.0012176863],"category_scores_gemma":[0.0006869749,0.00007778472,0.00040016315,0.00048697295,0.00025180713,0.0003463609,0.0002614467,0.00024270004,0.00017085372],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011030961,0.00012486223,0.83066165,0.00012322502,0.00056375837,0.0016105312,0.00044641085,0.11615301,0.015963994,0.005400204,0.0049739643,0.022875268],"study_design_scores_gemma":[0.00003891079,0.0001746099,0.9323798,0.000024483783,0.00008586527,0.00026347287,0.0005946114,0.05311601,0.0023534724,0.0018813377,0.009039201,0.00004807349],"about_ca_topic_score_codex":0.022347169,"about_ca_topic_score_gemma":0.019349977,"teacher_disagreement_score":0.022347169,"about_ca_system_score_codex":0.00087791524,"about_ca_system_score_gemma":0.00031345442,"threshold_uncertainty_score":0.04443419},"labels":[],"label_agreement":null},{"id":"W4401687735","doi":"10.1029/2024gl109469","title":"Forest‐Wide Growth Rates Stabilize After Experiencing Accelerated Temperature Changes Near an Alaskan Glacier","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Royal Bank of Canada; National Science Foundation","keywords":"Glacier; Geology; Physical geography; Environmental science; Earth science; Geomorphology; Geography","score_opus":0.041068013705052975,"score_gpt":0.3157464137184149,"score_spread":0.2746784000133619,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401687735","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997497,0.000008007715,0.000030378254,0.000005890722,0.0000013188956,0.0000011595638,0.000039433624,0.0000034254208,0.00016065927],"genre_scores_gemma":[0.99977773,0.0000066385683,0.00003995593,0.00000714428,8.928106e-7,0.000002226345,0.000058803773,9.564594e-7,0.0001057464],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996173,0.000008491861,0.0000024763426,0.000011728608,0.000006002075,0.000009632842],"domain_scores_gemma":[0.9998301,0.000033946784,0.000037454272,0.000023555123,0.000031859716,0.000043038373],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020319571,0.00011736033,0.0001316619,0.00013577948,0.00032501694,0.00031182612,0.00010789512,0.00016495075,0.0008722658],"category_scores_gemma":[0.0002800948,0.00006524545,0.00010392317,0.00007504684,0.00022616705,0.00012573782,0.00019843323,0.0002641789,0.00008414427],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0019439847,0.00050898624,0.6128757,0.000056697674,0.00017012408,0.00040140154,0.0009891962,0.0076733534,0.3633794,0.00031792838,0.00061244407,0.011070804],"study_design_scores_gemma":[0.0000127773765,0.0002904736,0.98926187,0.0000037108086,0.000019285812,0.000047060268,0.00042989233,0.002815329,0.0066948608,0.000117027754,0.00029937798,0.000008309784],"about_ca_topic_score_codex":0.009409185,"about_ca_topic_score_gemma":0.021062093,"teacher_disagreement_score":0.009409185,"about_ca_system_score_codex":0.00034383536,"about_ca_system_score_gemma":0.00016866368,"threshold_uncertainty_score":0.018708825},"labels":[],"label_agreement":null},{"id":"W4401927868","doi":"10.1029/2024gl108622","title":"Traveling Light: Arctic Coastal Erosion Releases Mostly Matrix Free, Unprotected Organic Carbon","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Natural Resources Canada","funders":"Nederlandse Organisatie voor Wetenschappelijk Onderzoek","keywords":"Coastal erosion; Arctic; Erosion; Environmental science; Carbon fibers; Oceanography; The arctic; Total organic carbon; Matrix (chemical analysis); Geology; Environmental chemistry; Materials science; Geomorphology; Chemistry","score_opus":0.04216984487879478,"score_gpt":0.2939772791614072,"score_spread":0.25180743428261243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4401927868","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9931172,0.00013440204,0.00021384149,0.000108840024,0.000011724045,0.00000525818,0.00028020635,0.00002079222,0.006107687],"genre_scores_gemma":[0.99700755,0.00015034963,0.00024786196,0.00007191585,0.000008834742,0.0000026506377,0.0002126162,0.000008319117,0.0022900125],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998888,0.0000075471767,0.000004056684,0.000026389178,0.000032058637,0.000041207895],"domain_scores_gemma":[0.9997241,0.000027858025,0.000060191185,0.000026164653,0.000103810395,0.000057848818],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001816057,0.00020167415,0.0001289653,0.00033593667,0.0011152937,0.0011067226,0.00022897973,0.00022653156,0.0037633698],"category_scores_gemma":[0.00029216954,0.00007199175,0.000110725785,0.00051858614,0.00042782593,0.00029215,0.00037608287,0.00021238455,0.00039271245],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00089651364,0.00010580666,0.73625994,0.0001713041,0.000090972055,0.0013162536,0.0011513701,0.0013736516,0.16248238,0.001091251,0.003802137,0.09125836],"study_design_scores_gemma":[0.000008643778,0.00007140815,0.98238117,0.000024584035,0.000023268038,0.00022192644,0.0021182115,0.00038827362,0.008764869,0.00015598207,0.0058313296,0.000010288918],"about_ca_topic_score_codex":0.12846285,"about_ca_topic_score_gemma":0.27330974,"teacher_disagreement_score":0.12846285,"about_ca_system_score_codex":0.0012984748,"about_ca_system_score_gemma":0.0010590001,"threshold_uncertainty_score":0.25543022},"labels":[],"label_agreement":null},{"id":"W4402087609","doi":"10.1029/2024gl110069","title":"Synergistic Forcing of the Troposphere and Stratosphere on Explosively Developing Cyclones Over the North Pacific During Cold Season","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Queen's University; China Meteorological Administration; National Natural Science Foundation of China; Sight Research UK; Government of Jiangsu Province; University of Bern; Massachusetts Institute of Technology","keywords":"Stratosphere; Troposphere; Climatology; Forcing (mathematics); Environmental science; Atmospheric sciences; Cyclone (programming language); Meteorology; Geology; Geography","score_opus":0.02756750950010104,"score_gpt":0.2739195475393739,"score_spread":0.24635203803927289,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402087609","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993043,0.000021106873,0.000045377816,0.000016554086,0.0000021816859,0.0000017913826,0.00009768621,0.0000061090977,0.0005049222],"genre_scores_gemma":[0.99980396,0.00002119286,0.00003380272,0.000003990087,0.000003079421,0.0000016759263,0.00007784311,0.0000011095382,0.000053268937],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999521,0.000007128843,0.0000031063014,0.000010063189,0.000008656202,0.000018940595],"domain_scores_gemma":[0.9998667,0.000020830594,0.00003531912,0.000009616855,0.000022192224,0.000045388766],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011302671,0.00022915947,0.00017881267,0.00046860002,0.00036220727,0.0003264507,0.00011403264,0.0001372647,0.0008928027],"category_scores_gemma":[0.0002429413,0.00013287306,0.00022467587,0.000296349,0.00022655983,0.00019721755,0.00056586217,0.00017876578,0.000051223782],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004815965,0.00010037175,0.9135503,0.00006001307,0.00022565755,0.0011776054,0.00036128334,0.015329544,0.056067128,0.00054093625,0.00075114454,0.011354471],"study_design_scores_gemma":[0.0000126544965,0.00002981285,0.99381304,0.0000048988186,0.00003149807,0.000045803696,0.00016744646,0.004588847,0.0009663685,0.000073070994,0.00026099637,0.000005581623],"about_ca_topic_score_codex":0.018228382,"about_ca_topic_score_gemma":0.025737012,"teacher_disagreement_score":0.018228382,"about_ca_system_score_codex":0.00033799137,"about_ca_system_score_gemma":0.0003143837,"threshold_uncertainty_score":0.03624457},"labels":[],"label_agreement":null},{"id":"W4402131555","doi":"10.1029/2024gl109109","title":"Autogenic Formation of Bimodal Grain Size Distributions in Rivers and Its Contribution to Gravel‐Sand Transitions","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrology and Sediment Transport Processes","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia; Simon Fraser University","funders":"University of Illinois System; China Association for Science and Technology; National Natural Science Foundation of China; California Institute of Technology","keywords":"Grain size; Geology; Geomorphology","score_opus":0.016161291877610357,"score_gpt":0.28707468287750276,"score_spread":0.2709133909998924,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402131555","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99709916,0.0000137145635,0.0023661607,0.000017528384,0.0000010098216,0.0000016961078,0.000022110396,0.000034499957,0.00044422332],"genre_scores_gemma":[0.99983394,0.0000025051697,0.000089964225,0.0000017377048,3.1204274e-7,7.60038e-7,0.0000071645436,0.0000028758145,0.00006070229],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999391,0.000009860378,0.0000029358712,0.00001986704,0.000007675031,0.000020560808],"domain_scores_gemma":[0.9996152,0.00013811732,0.000099314966,0.000044874014,0.000028899767,0.0000735288],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017646527,0.00012863001,0.00015751705,0.00036970942,0.00025521926,0.00050534675,0.00020984927,0.00026504954,0.00078302785],"category_scores_gemma":[0.00076272845,0.00019253528,0.00018866878,0.0001421014,0.0005564051,0.00026422224,0.00048066062,0.00023644084,0.000057706104],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003897034,0.0002114487,0.47156888,0.00007438733,0.00010528079,0.0013487133,0.0006592527,0.3213806,0.17230791,0.014095002,0.000576186,0.017282622],"study_design_scores_gemma":[0.000018445098,0.000077297744,0.30131733,0.000007476647,0.00002669039,0.00026411243,0.0002487072,0.68041235,0.010082421,0.0070887567,0.00041671755,0.000039747672],"about_ca_topic_score_codex":0.0031941435,"about_ca_topic_score_gemma":0.0029752504,"teacher_disagreement_score":0.0031941435,"about_ca_system_score_codex":0.00050556136,"about_ca_system_score_gemma":0.00021125376,"threshold_uncertainty_score":0.0063511133},"labels":[],"label_agreement":null},{"id":"W4402314459","doi":"10.1029/2023gl108039","title":"Internal‐Wave Dissipation Mechanisms and Vertical Structure in a High‐Resolution Regional Ocean Model","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Office of Naval Research; Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration; National Science Foundation","keywords":"Dissipation; Geology; Internal wave; High resolution; Geophysics; Internal tide; Seismology; Geodesy; Remote sensing; Physics; Oceanography","score_opus":0.024847659737841702,"score_gpt":0.26382144791530454,"score_spread":0.23897378817746284,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402314459","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9729831,0.00014492785,0.021974666,0.00032080078,0.000021447717,0.000019766932,0.000655063,0.00055434107,0.0033258344],"genre_scores_gemma":[0.9912431,0.00006689313,0.007510877,0.000023765882,0.000007587228,0.000024008266,0.00045100474,0.00005407756,0.0006186666],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985385,0.000044783264,0.000009168853,0.00004820041,0.000021955117,0.000022061864],"domain_scores_gemma":[0.9996489,0.00010431495,0.00006535257,0.00007123886,0.000068239264,0.0000419626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005618264,0.00052257534,0.0005928506,0.00031702602,0.0003545374,0.0010956691,0.0012983432,0.000912939,0.00072052865],"category_scores_gemma":[0.0011998244,0.0005030241,0.00075525447,0.00046771643,0.0005447408,0.00090743863,0.00060259417,0.0006069853,0.00018839787],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000048063444,0.000022642113,0.0032367732,0.0000073439583,0.00004315111,0.00002855489,0.000015041759,0.993769,0.0013072452,0.0005079117,0.00012146405,0.0008928179],"study_design_scores_gemma":[0.000017833334,0.000017278744,0.0009138677,0.0000014311738,0.000011984889,0.0000030984013,0.000004546964,0.99868053,0.00015110688,0.00011998814,0.00007307993,0.000005178939],"about_ca_topic_score_codex":0.051785205,"about_ca_topic_score_gemma":0.022548635,"teacher_disagreement_score":0.051785205,"about_ca_system_score_codex":0.0011670903,"about_ca_system_score_gemma":0.0010139225,"threshold_uncertainty_score":0.10296756},"labels":[],"label_agreement":null},{"id":"W4402350272","doi":"10.1029/2024gl110986","title":"Quantum Calculation of the Vibrational Excitation of Nitrogen Molecules by Fast Ions: Can It Contribute to STEVE Formation?","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atomic and Molecular Physics","field":"Physics and Astronomy","cited_by":10,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Canadian Space Agency","keywords":"Excitation; Ion; Quantum; Molecule; Nitrogen; Atomic physics; Physics; Chemical physics; Quantum mechanics","score_opus":0.01769067231208513,"score_gpt":0.30778427523797663,"score_spread":0.2900936029258915,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402350272","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8852466,0.00040573525,0.0822984,0.00052768184,0.0000938326,0.00007367253,0.00014395357,0.00023162476,0.030978508],"genre_scores_gemma":[0.9956371,0.00011763511,0.0031656306,0.000043127628,0.000008775792,0.000024665633,0.000028227525,0.00004701307,0.0009279299],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998691,0.000045402558,0.0000031241477,0.000009857026,0.000033893433,0.000038635975],"domain_scores_gemma":[0.99957746,0.00020723636,0.00004954882,0.000061029325,0.000061368824,0.00004336741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005821554,0.0003626905,0.00042556034,0.0003466235,0.0006686654,0.00044531474,0.0008791303,0.00067461986,0.0024181458],"category_scores_gemma":[0.001282179,0.00024036955,0.0004467819,0.0002833234,0.0007568305,0.00054222345,0.0005769328,0.0004797086,0.00015381534],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023403985,0.00014457825,0.006260418,0.00021952987,0.00006455256,0.0005349174,0.00027845553,0.8652055,0.016561506,0.1002942,0.0009632059,0.009239028],"study_design_scores_gemma":[0.000016552913,0.000019879168,0.0012386243,0.00000759616,0.0000069647535,0.000020279891,0.000041064413,0.9922604,0.0014372823,0.0047086375,0.00023253905,0.000010190701],"about_ca_topic_score_codex":0.0054272986,"about_ca_topic_score_gemma":0.0035562012,"teacher_disagreement_score":0.0054272986,"about_ca_system_score_codex":0.00059471565,"about_ca_system_score_gemma":0.00067637634,"threshold_uncertainty_score":0.010791421},"labels":[],"label_agreement":null},{"id":"W4402506396","doi":"10.1029/2024gl109441","title":"Plasma Structure Decay Rates in the Equatorial Ionosphere Are Strongly Coupled by Turbulence","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University; University of Saskatchewan","funders":"","keywords":"Sunset; Ionosphere; Scintillation; Physics; Turbulence; Amplitude; Plasma; Satellite; Computational physics; Space weather; Atmospheric sciences; Meteorology; Geophysics; Astronomy; Optics; Nuclear physics","score_opus":0.012918393450232319,"score_gpt":0.2883736348693375,"score_spread":0.27545524141910516,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402506396","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992193,0.000022786018,0.00034199585,0.000012253801,0.000001197817,0.0000022309066,0.000047384543,0.000011446836,0.00034141302],"genre_scores_gemma":[0.9998425,0.0000072598727,0.000048227223,0.0000020170246,0.0000011382037,0.0000012359409,0.000050612027,0.0000028633083,0.000044157936],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998857,0.000020562085,0.000008775464,0.000031458352,0.000023081715,0.000030349545],"domain_scores_gemma":[0.9984816,0.0006334821,0.0004546488,0.00017136082,0.00014735546,0.000111510446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003763314,0.00011396297,0.00018749076,0.0005101096,0.00016790743,0.00051761104,0.00011456419,0.00020024722,0.00057068764],"category_scores_gemma":[0.0029030873,0.00018714159,0.00014668437,0.00032225242,0.00027776705,0.00029878708,0.0002675282,0.00026346228,0.000119240336],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006560671,0.000070878996,0.9227754,0.000029904177,0.000095211624,0.00020623395,0.00034901625,0.008097574,0.057267066,0.0007435689,0.0003077484,0.009401308],"study_design_scores_gemma":[0.000008290144,0.00006085422,0.9832411,0.000002608475,0.000013541892,0.00007225797,0.00007791929,0.014291746,0.0019378989,0.00016875296,0.00011313968,0.000011796623],"about_ca_topic_score_codex":0.0025461123,"about_ca_topic_score_gemma":0.0017156098,"teacher_disagreement_score":0.0025461123,"about_ca_system_score_codex":0.00020039601,"about_ca_system_score_gemma":0.00011209302,"threshold_uncertainty_score":0.0050626397},"labels":[],"label_agreement":null},{"id":"W4402551624","doi":"10.1029/2024gl110691","title":"Inland Summer Speedup at Zachariæ Isstrøm, Northeast Greenland, Driven by Subglacial Hydrology","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Carlsbergfondet","keywords":"Geology; Hydrology (agriculture); Speedup; Physical geography; Geomorphology; Geography","score_opus":0.033315524031653505,"score_gpt":0.29817560585744834,"score_spread":0.26486008182579485,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402551624","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99921954,0.000020000269,0.000040740822,0.00003726446,0.00000217442,0.0000011974026,0.00027471315,0.000012758722,0.00039162117],"genre_scores_gemma":[0.9994709,0.000018745159,0.000051580006,0.000009116054,0.0000016119666,0.0000012475762,0.0003104893,0.000004484159,0.00013180525],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999274,0.0000065983177,0.0000036747624,0.000022509232,0.00001149065,0.000028353728],"domain_scores_gemma":[0.9998721,0.000013961686,0.00003758943,0.000009814583,0.000021715337,0.000044867826],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022141701,0.00021689989,0.0001923399,0.00048211042,0.0003192669,0.0007039721,0.00023762416,0.00021379357,0.0011603346],"category_scores_gemma":[0.00034872923,0.00011288076,0.00019058061,0.00041867496,0.00038860601,0.0003364777,0.00047653855,0.00019546472,0.00012217808],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002065935,0.00006491354,0.97170246,0.000026832182,0.000054172266,0.00041002373,0.00067573023,0.012762162,0.006015405,0.0002842826,0.0012005703,0.0065967613],"study_design_scores_gemma":[0.0000055902315,0.000011845427,0.9925949,0.0000073895003,0.000006817545,0.000022918373,0.00039668457,0.0061660474,0.00021068352,0.00006164453,0.00051218754,0.0000033898484],"about_ca_topic_score_codex":0.13620298,"about_ca_topic_score_gemma":0.25121078,"teacher_disagreement_score":0.13620298,"about_ca_system_score_codex":0.001454943,"about_ca_system_score_gemma":0.00089474814,"threshold_uncertainty_score":0.27082038},"labels":[],"label_agreement":null},{"id":"W4402556746","doi":"10.1029/2024gl111737","title":"Humid, Warm and Treed Ecosystems Show Longer Time‐Lag of Vegetation Response to Climate","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ecology and Vegetation Dynamics Studies","field":"Environmental Science","cited_by":17,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Lag; Environmental science; Vegetation (pathology); Ecosystem; Arid; Climate change; Precipitation; Climatology; Time lag; Terrestrial ecosystem; Atmospheric sciences; Ecology; Geography; Geology; Meteorology","score_opus":0.017744567577034583,"score_gpt":0.3028707793694572,"score_spread":0.28512621179242265,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402556746","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99830234,0.000055623048,0.0008577356,0.0000093804665,0.0000023199646,0.0000017948834,0.0002945199,0.00001971714,0.00045661273],"genre_scores_gemma":[0.9994697,0.000017431295,0.00018988171,0.0000042250736,0.000001062043,0.0000019119054,0.00020246545,0.000003299144,0.00011006984],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999573,0.0000061413602,0.0000034298262,0.000013959628,0.000007184608,0.000011982395],"domain_scores_gemma":[0.9996412,0.00012336351,0.00012226828,0.000024001725,0.00003203835,0.00005713518],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015792144,0.00011338057,0.0001290508,0.0004995262,0.0001205519,0.00038795092,0.00007547552,0.00012030051,0.0017870639],"category_scores_gemma":[0.0003965686,0.00006971204,0.00014291509,0.0003803168,0.00011723261,0.00023900226,0.00021345055,0.00015941699,0.00021899829],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037514276,0.0000641919,0.90749425,0.00007324537,0.00015911789,0.00014725026,0.00023573359,0.0068634255,0.07126446,0.0003906761,0.00028417518,0.012648331],"study_design_scores_gemma":[0.0000017741147,0.000020805186,0.9955786,0.000002094307,0.000007527633,0.000048832986,0.00008404039,0.0024650462,0.0014151513,0.00011923641,0.00025353566,0.0000033845126],"about_ca_topic_score_codex":0.0020938942,"about_ca_topic_score_gemma":0.0026419533,"teacher_disagreement_score":0.0020938942,"about_ca_system_score_codex":0.00012193995,"about_ca_system_score_gemma":0.00009156566,"threshold_uncertainty_score":0.005978346},"labels":[],"label_agreement":null},{"id":"W4402673308","doi":"10.1029/2024gl109457","title":"First High‐Precision U–Pb CA–ID–TIMS Age of the Chuanlinggou Formation, North China Craton: Implications for Global Correlations of Black Shales and the Statherian/Calymmian Boundary","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Craton; Geology; China; Geochemistry; Boundary (topology); Geophysics; Earth science; Mineralogy; Seismology; Geography; Archaeology; Tectonics","score_opus":0.021883258102258645,"score_gpt":0.2702726332089838,"score_spread":0.24838937510672518,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402673308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99812704,0.00019552217,0.00026432687,0.00003400548,0.0000041540657,0.0000032765386,0.00020750896,0.0000126480745,0.0011515034],"genre_scores_gemma":[0.9992737,0.000042400283,0.00019676179,0.000008654174,0.0000025097952,0.0000033444746,0.00017593597,0.000003609121,0.0002929925],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992025,0.000006907717,0.0000059312806,0.000027886486,0.000020797563,0.000018195418],"domain_scores_gemma":[0.9997689,0.000016526488,0.00005769043,0.000024968796,0.00010488303,0.000027016484],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003239012,0.00024731326,0.00018367071,0.0013783613,0.0007400894,0.0004935493,0.00022182739,0.00022704748,0.00093885284],"category_scores_gemma":[0.0003751202,0.00018056695,0.00013701244,0.001113785,0.0004877699,0.00025371503,0.0006267205,0.00018733619,0.00011913611],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014708325,0.000020818827,0.9209821,0.0000899565,0.00010835438,0.00023121666,0.0016771719,0.0013988608,0.04910007,0.0006664039,0.0004635734,0.025114493],"study_design_scores_gemma":[0.0000047315284,0.000012488549,0.99607736,0.000008597025,0.000027416872,0.000033550776,0.00020638746,0.00097307784,0.0011548434,0.00005590807,0.0014416743,0.0000040676678],"about_ca_topic_score_codex":0.09805982,"about_ca_topic_score_gemma":0.23397504,"teacher_disagreement_score":0.09805982,"about_ca_system_score_codex":0.0011012957,"about_ca_system_score_gemma":0.00089414645,"threshold_uncertainty_score":0.19497812},"labels":[],"label_agreement":null},{"id":"W4402900238","doi":"10.1029/2024gl111677","title":"The High Latitude Ionospheric Response to the Major May 2024 Geomagnetic Storm: A Synoptic View","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":83,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Office of Naval Research; Natural Environment Research Council; Office of Nuclear Energy; School of Global Policy and Strategy, University of California, San Diego; Sight Research UK; General Dynamics; Leverhulme Trust; Symposium Mammographicum; Massachusetts Institute of Technology; National Science Foundation","keywords":"Ionosonde; Ionosphere; Geomagnetic storm; Geology; Geophysics; Atmospheric sciences; Interplanetary scintillation; Storm; F region; Incoherent scatter; Scintillation; Substorm; Earth's magnetic field; Physics; Solar wind; Magnetosphere; Plasma; Coronal mass ejection; Electron density; Magnetic field","score_opus":0.012223921948132892,"score_gpt":0.28819329404555305,"score_spread":0.2759693720974202,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4402900238","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98545897,0.0005082283,0.00021206847,0.0003883027,0.00009563571,0.000016549751,0.0016508925,0.000047900856,0.011621525],"genre_scores_gemma":[0.9969553,0.00021597513,0.00013971479,0.00005899428,0.00013328882,0.000009527916,0.0011262058,0.000007050412,0.0013538742],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999465,0.000007243158,0.000006299696,0.0000097897355,0.000015619073,0.000014567201],"domain_scores_gemma":[0.999742,0.000032991888,0.00008913282,0.0000138141895,0.000066208646,0.000055784065],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022939382,0.00017580089,0.00012776612,0.0013028032,0.00043017312,0.001042973,0.00014034261,0.00026243116,0.0022748066],"category_scores_gemma":[0.00038228373,0.00008332765,0.00011720891,0.00080043933,0.00022327561,0.0003211633,0.00046068276,0.00015923074,0.00023053333],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010795172,0.000112541915,0.9033173,0.00027759108,0.00017305117,0.0014779854,0.001723189,0.0041410387,0.039273117,0.002071929,0.011034275,0.035318512],"study_design_scores_gemma":[0.000007644971,0.00010850893,0.98834246,0.000016945187,0.000024207182,0.00010655814,0.00060084753,0.0009405549,0.0008546308,0.00013897562,0.00884877,0.0000098997],"about_ca_topic_score_codex":0.017818704,"about_ca_topic_score_gemma":0.03200457,"teacher_disagreement_score":0.017818704,"about_ca_system_score_codex":0.0007060062,"about_ca_system_score_gemma":0.00037945437,"threshold_uncertainty_score":0.035429955},"labels":[],"label_agreement":null},{"id":"W4403180467","doi":"10.1029/2024gl110456","title":"Tracking the Filling, Outburst Flood and Resulting Subglacial Water Channel From a Large Canadian Arctic Subglacial Lake","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; University of Waterloo; University of Ottawa","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Polar Knowledge Canada","keywords":"Geology; Flood myth; Arctic; Channel (broadcasting); Tracking (education); Geomorphology; The arctic; Oceanography; Geography","score_opus":0.042265525704557494,"score_gpt":0.27091311047147304,"score_spread":0.22864758476691555,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403180467","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99837106,0.000018064708,0.00016189186,0.00003270678,0.0000015710816,0.000007680995,0.0007926909,0.000029603963,0.0005847428],"genre_scores_gemma":[0.9975165,0.00002653242,0.00070453226,0.000010655353,9.820989e-7,0.0000059103395,0.001247868,0.000005912363,0.00048109985],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998921,0.000005616001,0.0000018746792,0.000020980033,0.000034971104,0.000044439003],"domain_scores_gemma":[0.9997595,0.00002024536,0.000022969893,0.00001175741,0.000102862665,0.000082611965],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017105111,0.00023884507,0.0001701746,0.00065112795,0.0013508673,0.0006067236,0.00038698385,0.00024309238,0.0006396397],"category_scores_gemma":[0.0003950715,0.00013456891,0.00016287815,0.000903313,0.00030550093,0.00019373266,0.00043748476,0.00023018167,0.000099028475],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023014205,0.00011407404,0.94726247,0.00003409364,0.00008511164,0.0003923613,0.0019793373,0.009167476,0.012206502,0.00042118315,0.002924699,0.0251826],"study_design_scores_gemma":[0.000010754383,0.00002934856,0.96650374,0.000008040845,0.000023036959,0.00003645875,0.0012457476,0.028207654,0.0014136661,0.00005631724,0.0024497123,0.000015527468],"about_ca_topic_score_codex":0.9535268,"about_ca_topic_score_gemma":0.98780036,"teacher_disagreement_score":0.046473205,"about_ca_system_score_codex":0.005709306,"about_ca_system_score_gemma":0.0047306046,"threshold_uncertainty_score":0.09349376},"labels":[],"label_agreement":null},{"id":"W4403208976","doi":"10.1029/2024gl110568","title":"Unexpected STEVE Observations at High Latitude During Quiet Geomagnetic Conditions","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Mount Royal University; University of Calgary","funders":"Air Force Office of Scientific Research; Departamento de Investigaciones Científicas y Tecnológicas, Universidad de Santiago de Chile; Canadian Space Agency; Agencia Nacional de Investigación y Desarrollo; National Aeronautics and Space Administration","keywords":"Substorm; Latitude; Geology; Ionosphere; Magnetosphere; Earth's magnetic field; Geomagnetic latitude; Middle latitudes; Geophysics; High latitude; Satellite; Low latitude; Atmospheric sciences; Geodesy; Physics; Astronomy; Plasma; Magnetic field","score_opus":0.021590690093283994,"score_gpt":0.29312556862470535,"score_spread":0.27153487853142133,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403208976","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99640983,0.00006172227,0.00040475366,0.00004132625,0.000012407893,0.0000051437846,0.00020911542,0.000037529964,0.002818258],"genre_scores_gemma":[0.9994103,0.000022503427,0.00015358823,0.000015468415,0.000008932152,0.000001771097,0.00012744185,0.000005143666,0.0002548318],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999938,0.000004457009,0.000002119929,0.000011795981,0.000017341747,0.000026334214],"domain_scores_gemma":[0.9998466,0.00002637687,0.000030716757,0.000020931531,0.00003256829,0.000042776257],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010974347,0.000105680905,0.00017088614,0.00030886062,0.0004185267,0.00038167267,0.00012591814,0.00029964262,0.00062466995],"category_scores_gemma":[0.00028476707,0.00009095501,0.00009339603,0.00021856691,0.000218348,0.00019263188,0.00041986778,0.00032116944,0.00014716898],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00095864595,0.0001310431,0.61673474,0.00010255553,0.00011712689,0.006280173,0.0029943292,0.000820495,0.34168816,0.0006242018,0.0024226024,0.02712599],"study_design_scores_gemma":[0.000007945128,0.00008079314,0.98936707,0.000011438312,0.000014776661,0.0009876158,0.00063111633,0.00048792316,0.0060947635,0.000079183854,0.0022292773,0.000008013829],"about_ca_topic_score_codex":0.0036387052,"about_ca_topic_score_gemma":0.013169898,"teacher_disagreement_score":0.0036387052,"about_ca_system_score_codex":0.00013809111,"about_ca_system_score_gemma":0.00010871409,"threshold_uncertainty_score":0.00723505},"labels":[],"label_agreement":null},{"id":"W4403558078","doi":"10.1029/2024gl109865","title":"Magnitude Clustering During Stick‐Slip Dynamics on Laboratory Faults","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hotchkiss Brain Institute; University of Calgary","funders":"Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Alberta Innovates; National Science Foundation","keywords":"Magnitude (astronomy); Cluster analysis; Slip (aerodynamics); Geology; Seismology; Statistics; Mathematics; Physics; Engineering; Aerospace engineering","score_opus":0.02669168726084268,"score_gpt":0.2900839262587189,"score_spread":0.2633922389978762,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403558078","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960476,0.000013399276,0.00021112665,0.00000218203,6.8491426e-7,0.0000021294775,0.000047381993,0.000008634647,0.00010980299],"genre_scores_gemma":[0.9998323,0.00000475591,0.000067117166,8.110156e-7,9.785944e-7,0.0000020167386,0.000053687636,0.0000013098661,0.00003697622],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9998704,0.000011498689,0.000009355555,0.000037500067,0.000045393135,0.000025900215],"domain_scores_gemma":[0.9995877,0.00007713716,0.0001623489,0.00004781085,0.000061807084,0.00006315916],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012993465,0.00011366071,0.00025975195,0.0007159382,0.00018076316,0.0002496185,0.0001623333,0.00014079486,0.0008671609],"category_scores_gemma":[0.0005272545,0.0001152022,0.000118164695,0.0003414374,0.00032501353,0.0001641914,0.0003143031,0.00015063002,0.00010033296],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0012149271,0.0001432287,0.25307235,0.00007448578,0.000110095556,0.0003199373,0.00051467516,0.004570723,0.7238681,0.00017479931,0.00019844642,0.015738295],"study_design_scores_gemma":[0.0000071497175,0.00025905704,0.95060134,0.0000027266144,0.000014983684,0.000102585596,0.00018370734,0.007332351,0.041216165,0.000060331357,0.00020642365,0.000013164647],"about_ca_topic_score_codex":0.0013898661,"about_ca_topic_score_gemma":0.0013331661,"teacher_disagreement_score":0.0013898661,"about_ca_system_score_codex":0.00021777063,"about_ca_system_score_gemma":0.00006766138,"threshold_uncertainty_score":0.002900958},"labels":[],"label_agreement":null},{"id":"W4403810751","doi":"10.1029/2024gl110791","title":"Centennial‐Scale Variability of the Atlantic Meridional Overturning Circulation in CMIP6 Models Shaped by Arctic–North Atlantic Interactions and Sea Ice Biases","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Horizon 2020 Framework Programme","keywords":"Climatology; Centennial; Geology; Thermohaline circulation; Shutdown of thermohaline circulation; Oceanography; North Atlantic Deep Water; Geography","score_opus":0.04479766687865497,"score_gpt":0.30006953471619957,"score_spread":0.25527186783754463,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403810751","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9974712,0.000054438984,0.0008999904,0.00009503305,0.000015204112,0.0000044947947,0.00044712672,0.00007968072,0.0009327826],"genre_scores_gemma":[0.9992907,0.000030106296,0.00024055458,0.000014256487,0.0000044117596,0.000005944841,0.00024753535,0.00002055763,0.00014590958],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986005,0.000054213575,0.000008755946,0.000034011897,0.000011071762,0.000031889336],"domain_scores_gemma":[0.99937516,0.0002807613,0.00009783457,0.000090172245,0.00007535208,0.00008080969],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00081000826,0.00066273625,0.00033177357,0.0004685185,0.00037725255,0.00093338854,0.0008247771,0.0006405227,0.001278109],"category_scores_gemma":[0.001315057,0.000305762,0.0008090309,0.000475657,0.00041223163,0.0004908733,0.0005297513,0.0006812127,0.00017628836],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023717224,0.00011947432,0.06642212,0.000037026668,0.00030226703,0.00012012738,0.00007252153,0.92505586,0.0033650068,0.0008774433,0.0009624375,0.0024284779],"study_design_scores_gemma":[0.00004723161,0.00006435026,0.024581082,0.000010021992,0.00005619612,0.00003021664,0.00006667017,0.9735189,0.00085097173,0.0004649459,0.00028953492,0.000019910536],"about_ca_topic_score_codex":0.022169394,"about_ca_topic_score_gemma":0.014259047,"teacher_disagreement_score":0.022169394,"about_ca_system_score_codex":0.0006895863,"about_ca_system_score_gemma":0.0005011394,"threshold_uncertainty_score":0.044080675},"labels":[],"label_agreement":null},{"id":"W4403900919","doi":"10.1029/2024gl111071","title":"Optimising Interannual Sea Ice Thickness Variability Retrieved From CryoSat‐2","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Horizon 2020 Framework Programme; Natural Environment Research Council; Sight Research UK; European Space Agency","keywords":"Geology; Climatology; Sea ice; Environmental science; Geodesy","score_opus":0.026353865382571635,"score_gpt":0.290021371673085,"score_spread":0.2636675062905134,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403900919","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98654085,0.000090538,0.011490616,0.00003764993,0.000015276744,0.000012071364,0.00076874334,0.0003456605,0.0006985228],"genre_scores_gemma":[0.9846252,0.00004615681,0.012775438,0.000019686679,0.00001154509,0.000013194317,0.0021849757,0.00007936274,0.0002443328],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999841,0.000033386987,0.000009654624,0.00005832014,0.000028093087,0.000029566963],"domain_scores_gemma":[0.9995783,0.00012830737,0.00007317981,0.000056095585,0.00013649302,0.000027654973],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006910283,0.00056911266,0.0003824618,0.00068707345,0.00015339718,0.00071119,0.00032567795,0.0003045021,0.00053322123],"category_scores_gemma":[0.001380886,0.0002494503,0.00030927753,0.0006488542,0.000102852115,0.0005339963,0.00025388246,0.00022535337,0.00036203896],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015441402,0.00045406452,0.22319323,0.00017167162,0.0004569117,0.00019078943,0.00023802013,0.34841442,0.18087223,0.00020091061,0.0024026115,0.24186102],"study_design_scores_gemma":[0.000070092225,0.00019757124,0.23143382,0.000017127339,0.0001184465,0.000055298642,0.00009729735,0.7247994,0.042018563,0.00014046514,0.0010086958,0.00004326686],"about_ca_topic_score_codex":0.008546715,"about_ca_topic_score_gemma":0.009584379,"teacher_disagreement_score":0.008546715,"about_ca_system_score_codex":0.0002631999,"about_ca_system_score_gemma":0.00035013203,"threshold_uncertainty_score":0.01699394},"labels":[],"label_agreement":null},{"id":"W4403907448","doi":"10.1029/2024gl112412","title":"Projected Changes of the Warm Arctic‐Cold North American Pattern","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Climatology; Arctic; The arctic; Geology; Environmental science; Oceanography","score_opus":0.04284618856172545,"score_gpt":0.3096800136580646,"score_spread":0.26683382509633913,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403907448","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9864857,0.00013338686,0.0012313308,0.0008520808,0.000045006323,0.000009571421,0.0037495208,0.00010093941,0.007392301],"genre_scores_gemma":[0.99714226,0.00008889045,0.0005748497,0.00005453616,0.000006752894,0.000007974995,0.0011200649,0.000007955745,0.0009965645],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99994004,0.000009747378,0.000002727024,0.000015021321,0.000013338954,0.00001908677],"domain_scores_gemma":[0.999864,0.000005797127,0.000021729144,0.000008399948,0.00006378169,0.000036350448],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000214588,0.00021419286,0.00009359361,0.00027158772,0.0003437087,0.00060203875,0.00020924788,0.00029308547,0.002430603],"category_scores_gemma":[0.000385889,0.00009184296,0.0002671999,0.000467868,0.00012419195,0.0001942602,0.00029398713,0.00021758674,0.00023122606],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006762938,0.00018975713,0.7454044,0.00012012807,0.000389527,0.00034641486,0.00029514462,0.16599718,0.015299967,0.007882918,0.014841552,0.04855671],"study_design_scores_gemma":[0.00006582185,0.0000687793,0.8760189,0.000019430272,0.00009417617,0.00008799742,0.0003404079,0.10221872,0.0021915354,0.0017867364,0.017074892,0.00003263574],"about_ca_topic_score_codex":0.21420401,"about_ca_topic_score_gemma":0.23475339,"teacher_disagreement_score":0.21420401,"about_ca_system_score_codex":0.001398892,"about_ca_system_score_gemma":0.0011560698,"threshold_uncertainty_score":0.4259144},"labels":[],"label_agreement":null},{"id":"W4403980707","doi":"10.1029/2024gl109746","title":"Opposite Trends in the Northern Hemisphere Stratosphere Between Mid‐Winter and Early Spring Linked to Surface Temperature Anomalies","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Stratosphere; Polar vortex; Northern Hemisphere; Troposphere; Climatology; Atmospheric sciences; Sudden stratospheric warming; Southern Hemisphere; Polar; Anomaly (physics); Geology; Polar night; Environmental science; Vortex; Meteorology; Geography; Physics","score_opus":0.032114294831824215,"score_gpt":0.30239801776939224,"score_spread":0.270283722937568,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4403980707","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9989611,0.000067695066,0.000034993063,0.000042291405,0.0000051814013,0.0000011831148,0.00039943977,0.0000057450325,0.00048226732],"genre_scores_gemma":[0.9991898,0.00002693931,0.000028474755,0.000009544991,0.0000047832377,0.0000015311082,0.0005083977,0.0000014251586,0.00022913421],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999367,0.000010421753,0.0000045794295,0.000017465156,0.000011251506,0.000019639918],"domain_scores_gemma":[0.9996215,0.00006832992,0.00012244919,0.000020124648,0.000069011534,0.00009851753],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020312112,0.00011918997,0.000110153094,0.0005135586,0.00017458179,0.00044840618,0.00012489835,0.00019215,0.0014655838],"category_scores_gemma":[0.00040132512,0.00008233738,0.0001799983,0.00036434407,0.00016021138,0.00016085505,0.00015189001,0.00014327558,0.00021651266],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016093296,0.000022064129,0.9925079,0.000009363528,0.000056368044,0.000076671786,0.00022730106,0.00014898737,0.0045365687,0.000088945584,0.0002799247,0.00188502],"study_design_scores_gemma":[9.636378e-7,0.000008495299,0.9996351,9.0285795e-7,0.000004281407,0.000013671306,0.000049606995,0.00008378661,0.000094254865,0.000009711981,0.00009859049,6.5820075e-7],"about_ca_topic_score_codex":0.015012921,"about_ca_topic_score_gemma":0.028593494,"teacher_disagreement_score":0.015012921,"about_ca_system_score_codex":0.00023096298,"about_ca_system_score_gemma":0.00023644221,"threshold_uncertainty_score":0.029851079},"labels":[],"label_agreement":null},{"id":"W4404195115","doi":"10.1029/2024gl109393","title":"Sodium Enrichment of Mercury's Subsurface Through Diffusion","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Centre National d’Etudes Spatiales; Agence Nationale de la Recherche","keywords":"Mercury (programming language); Sodium; Diffusion; Environmental science; Geology; Environmental chemistry; Mineralogy; Astrobiology; Materials science; Chemistry; Physics; Thermodynamics; Metallurgy","score_opus":0.03751861238979377,"score_gpt":0.3199287553627199,"score_spread":0.28241014297292616,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404195115","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99712914,0.00016121608,0.0018518044,0.00006761056,0.0000036257015,0.0000031165494,0.0000680864,0.000034226203,0.00068105076],"genre_scores_gemma":[0.99899596,0.00010620643,0.00050421164,0.0000049857695,0.00000117253,0.0000016491559,0.000023927516,0.000003822263,0.0003580144],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999651,0.0000030601316,9.0219703e-7,0.000012075522,0.0000071747077,0.0000117087975],"domain_scores_gemma":[0.9999684,0.000010406313,0.0000071254385,0.0000024370274,0.000007942402,0.000003598562],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000064292624,0.0001922737,0.0001712556,0.00015898314,0.00019749661,0.00022767288,0.00020925267,0.00016164627,0.00063654606],"category_scores_gemma":[0.000116982126,0.00012424988,0.00020124733,0.00012623277,0.00020035572,0.00029624335,0.00027741957,0.00017205959,0.00008224533],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013140537,0.0000144129035,0.0062909774,0.0000809122,0.000017784005,0.00006658926,0.00008494832,0.0038130605,0.98498005,0.0012027862,0.00010365985,0.0032134075],"study_design_scores_gemma":[0.000059702863,0.00027150867,0.017334837,0.000011299869,0.00003328769,0.00016728362,0.00022729622,0.123464495,0.854275,0.0014000917,0.0027237397,0.000031489297],"about_ca_topic_score_codex":0.009531408,"about_ca_topic_score_gemma":0.0055085844,"teacher_disagreement_score":0.009531408,"about_ca_system_score_codex":0.00052694575,"about_ca_system_score_gemma":0.00022674308,"threshold_uncertainty_score":0.018951833},"labels":[],"label_agreement":null},{"id":"W4404205635","doi":"10.1029/2024gl110318","title":"Turbulent Vertical Velocities in Labrador Sea Convection","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Horizon 2020 Framework Programme; Natural Environment Research Council; European Commission; Sight Research UK","keywords":"Geology; Turbulence; Convection; Geophysics; Deep convection; Climatology; Geodesy; Meteorology; Geography","score_opus":0.023648147993794964,"score_gpt":0.2747692603715395,"score_spread":0.25112111237774454,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404205635","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986563,0.00013803065,0.00022463826,0.000019552579,0.0000052378905,0.0000022187255,0.00025946705,0.00003477721,0.0006598747],"genre_scores_gemma":[0.9993364,0.000035905974,0.00011461599,0.0000046368104,0.0000023365699,0.0000018627213,0.00031891017,0.000007363244,0.0001778737],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984825,0.000017732991,0.000013815723,0.00003389758,0.000027794582,0.000058474496],"domain_scores_gemma":[0.9997452,0.00004801378,0.00009619975,0.000019787974,0.000043082357,0.000047844296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002646231,0.0003843036,0.00020191004,0.0010635656,0.00021657193,0.0009732595,0.00022930875,0.00026866002,0.00073280325],"category_scores_gemma":[0.00084985036,0.00018989659,0.00024295934,0.0008100874,0.0003377435,0.0003446685,0.0005020239,0.00018286111,0.00033605951],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010496236,0.00013060204,0.8612239,0.00012497518,0.00015354554,0.00035357007,0.0008625355,0.027596988,0.0676019,0.0015509725,0.0012640789,0.038087428],"study_design_scores_gemma":[0.00005170302,0.00014647114,0.96750253,0.00003486654,0.000024820705,0.00007455161,0.00029536616,0.02142605,0.00835665,0.00032059068,0.0017164277,0.000049889743],"about_ca_topic_score_codex":0.034310255,"about_ca_topic_score_gemma":0.01834187,"teacher_disagreement_score":0.034310255,"about_ca_system_score_codex":0.0008535519,"about_ca_system_score_gemma":0.0003991383,"threshold_uncertainty_score":0.06822109},"labels":[],"label_agreement":null},{"id":"W4404248453","doi":"10.1029/2024gl110614","title":"Past Groundwater Drought in the North American Cordillera","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tree-ring climate responses","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Simon Fraser University","funders":"","keywords":"Groundwater; Geology; Hydrology (agriculture); Earth science; Climatology; Physical geography; Geography; Geotechnical engineering","score_opus":0.03460573928446011,"score_gpt":0.2990674683517284,"score_spread":0.26446172906726834,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404248453","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99930024,0.00005849085,0.000012968144,0.000031029846,8.918278e-7,0.0000010994365,0.00018257544,0.0000028060344,0.0004100208],"genre_scores_gemma":[0.9996,0.00004318897,0.000031259577,0.000009693088,0.0000012447281,0.000001529763,0.00018360923,5.314675e-7,0.00012910308],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999907,0.000011463676,0.0000043676087,0.000025391495,0.00002182243,0.000029881367],"domain_scores_gemma":[0.9996362,0.000031722935,0.000084625644,0.000016896356,0.00016774904,0.00006276261],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015213121,0.00008140195,0.00011341225,0.0007682373,0.000630314,0.00051460136,0.00018104399,0.00015635866,0.0007779488],"category_scores_gemma":[0.0005716643,0.000048743113,0.000048409584,0.0011806255,0.00023957812,0.00014871803,0.00027392662,0.00013725697,0.000060680217],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000056846984,0.00001754125,0.9867356,0.000012926622,0.000023204762,0.00011141453,0.0005698026,0.00045119185,0.0016952377,0.0000895444,0.00037199302,0.009864875],"study_design_scores_gemma":[0.0000013730777,0.000005427076,0.9987431,0.0000033179479,0.000003686273,0.00001626131,0.00027771897,0.00029259492,0.00010755007,0.000013317486,0.00053409045,0.0000014599814],"about_ca_topic_score_codex":0.6100126,"about_ca_topic_score_gemma":0.81491256,"teacher_disagreement_score":0.6100126,"about_ca_system_score_codex":0.0031622162,"about_ca_system_score_gemma":0.0009704327,"threshold_uncertainty_score":0.78456825},"labels":[],"label_agreement":null},{"id":"W4404326039","doi":"10.1029/2024gl111364","title":"Baffin Bay Ice Export and Production From Sentinel‐1, the RADARSAT Constellation Mission, and CryoSat‐2: 2016–2022","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba; University of Toronto; Environment and Climate Change Canada","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Constellation; Bay; Geology; Production (economics); Remote sensing; Oceanography; Environmental science; Astronomy; Physics","score_opus":0.021469134955762782,"score_gpt":0.2655731976657065,"score_spread":0.2441040627099437,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404326039","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9872127,0.00030537375,0.0003288296,0.00013750406,0.000018308712,0.00000853063,0.009583799,0.000030586445,0.0023742355],"genre_scores_gemma":[0.9793224,0.00026191032,0.00044894507,0.000054424014,0.00001786372,0.0000135750015,0.017699908,0.000011919339,0.0021690952],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998487,0.000008278492,0.0000105487425,0.000041683423,0.000066650966,0.000024022422],"domain_scores_gemma":[0.9995783,0.000030313895,0.00011282437,0.000020158852,0.00019705972,0.00006129594],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033263216,0.00042856883,0.00017347415,0.0009018467,0.00026021223,0.00081584824,0.00026602604,0.000251165,0.001304657],"category_scores_gemma":[0.00070885057,0.00014328076,0.00032066827,0.00088313216,0.00020827056,0.0005967962,0.0003995868,0.00023039641,0.0003050527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001393087,0.000024203073,0.9781302,0.000060281884,0.000118511074,0.00013217071,0.00012709278,0.0056462227,0.0028264183,0.00010052332,0.0028670097,0.00982808],"study_design_scores_gemma":[0.0000072782545,0.000011440402,0.99139166,0.000020835623,0.000019111529,0.000037703692,0.00012762769,0.003966644,0.00067357224,0.000022904895,0.003711664,0.0000094642855],"about_ca_topic_score_codex":0.3626223,"about_ca_topic_score_gemma":0.40883464,"teacher_disagreement_score":0.63737774,"about_ca_system_score_codex":0.0020617181,"about_ca_system_score_gemma":0.0011666885,"threshold_uncertainty_score":0.7210232},"labels":[],"label_agreement":null},{"id":"W4404361281","doi":"10.1029/2024gl112470","title":"Recent Decreases in the Growth Rate of Atmospheric HCFC‐22 Column Derived From the Ground‐Based FTIR Harmonized Retrievals at 16 NDACC Sites","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; Environment and Climate Change Canada; Antarctica New Zealand; Ministry of Business, Innovation and Employment; Naturvårdsverket; Nagoya University; National Institute of Water and Atmospheric Research","keywords":"Environmental science; Atmospheric sciences; Column (typography); Fourier transform infrared spectroscopy; Atmospheric chemistry; Remote sensing; Geodesy; Meteorology; Geology; Mathematics; Ozone; Physics; Optics","score_opus":0.02734218738187287,"score_gpt":0.27398378590204614,"score_spread":0.24664159852017326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404361281","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98492485,0.00025314902,0.0023186072,0.00010332953,0.000026369502,0.000020225065,0.010072651,0.00038466946,0.0018961054],"genre_scores_gemma":[0.971429,0.00014378807,0.0053547337,0.000049526094,0.000017547902,0.00003245424,0.022333303,0.00008727253,0.0005524137],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997186,0.000022035583,0.000016729675,0.00010259473,0.00010237316,0.000037637317],"domain_scores_gemma":[0.9993718,0.000065283566,0.00010609815,0.00010745656,0.00031456057,0.000034831486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00072737905,0.0006449193,0.0002929815,0.00097373436,0.0003208334,0.00046303592,0.0005303141,0.00048704678,0.0005193665],"category_scores_gemma":[0.00077467976,0.00024312458,0.0005732933,0.0016419252,0.00023674245,0.0006867785,0.0003918729,0.00030016413,0.0002702392],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0007897124,0.00026650837,0.703049,0.00043256476,0.00077299867,0.0004999821,0.00041718894,0.086204566,0.10494111,0.0004175459,0.0096673835,0.09254138],"study_design_scores_gemma":[0.00004616661,0.000062263054,0.88027346,0.00001917229,0.00019386367,0.00016455569,0.000114391565,0.06745459,0.04234865,0.00009118377,0.009159594,0.00007210637],"about_ca_topic_score_codex":0.06270655,"about_ca_topic_score_gemma":0.057748634,"teacher_disagreement_score":0.06270655,"about_ca_system_score_codex":0.0010775303,"about_ca_system_score_gemma":0.00045680444,"threshold_uncertainty_score":0.12468314},"labels":[],"label_agreement":null},{"id":"W4404361428","doi":"10.1029/2024gl110348","title":"Influence of Foehn‐Like Winds on Near‐Surface Temperature at Jang Bogo Station, Terra Nova Bay, East Antarctica","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Research Foundation of Korea; Ministry of Oceans and Fisheries; Korea Polar Research Institute; National Research Foundation","keywords":"Bay; Nova (rocket); Geology; Oceanography; Climatology; Nova scotia; Meteorology; Geography","score_opus":0.03553110433279917,"score_gpt":0.2947563454727253,"score_spread":0.2592252411399261,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404361428","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.998793,0.00006723571,0.000013354412,0.00004024588,0.000009138865,0.0000026386958,0.0004997242,0.000003179971,0.0005714232],"genre_scores_gemma":[0.9985819,0.00008923374,0.000052888303,0.000021499754,0.000010544665,0.000004902509,0.0008389001,0.0000021345782,0.00039807393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998821,0.000023824046,0.000008586125,0.000023044637,0.000030498339,0.000031884232],"domain_scores_gemma":[0.9997011,0.000035573437,0.00008011753,0.000022663624,0.000058691978,0.00010190663],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020556063,0.00019913622,0.00020359385,0.00038151044,0.00053097797,0.00061992963,0.00018621974,0.00022920055,0.00088558206],"category_scores_gemma":[0.0003571335,0.000099607234,0.00022012793,0.00045608083,0.0002484413,0.00020947406,0.00039508054,0.0002568771,0.0001704263],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015907858,0.000033338605,0.9931416,0.000025645399,0.000078216166,0.0002435775,0.00029318914,0.00042530365,0.0026136723,0.000028700617,0.00040833667,0.0025494064],"study_design_scores_gemma":[0.0000017854934,0.000008378306,0.9994168,0.0000024094427,0.0000045722495,0.000013664542,0.00016777942,0.00012166188,0.000046831392,0.000002846861,0.00021224319,0.0000011503664],"about_ca_topic_score_codex":0.0942507,"about_ca_topic_score_gemma":0.14597987,"teacher_disagreement_score":0.0942507,"about_ca_system_score_codex":0.00065310684,"about_ca_system_score_gemma":0.0005596752,"threshold_uncertainty_score":0.18740422},"labels":[],"label_agreement":null},{"id":"W4404644187","doi":"10.1029/2024gl110588","title":"Exploring Thermospheric Disturbance Patterns Through Space‐Borne Accelerometer Measurement Errors: A Weighted Accelerometer 1B Dataset of GRACE C","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Accelerometer; Disturbance (geology); Remote sensing; Environmental science; Space (punctuation); Geodesy; Thermosphere; Observational error; Meteorology; Computer science; Atmospheric sciences; Geology; Mathematics; Statistics; Geophysics; Ionosphere; Physics","score_opus":0.23766942292629825,"score_gpt":0.3201778711518156,"score_spread":0.08250844822551737,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404644187","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9303845,0.00017689753,0.0050478536,0.0003620287,0.00009450628,0.00005073006,0.061145037,0.000808495,0.0019299127],"genre_scores_gemma":[0.8461952,0.00010285448,0.008043353,0.000105412146,0.0000929695,0.00009694811,0.14419049,0.0001752949,0.0009975027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9995621,0.00008993076,0.00003206507,0.00010909585,0.00012724247,0.000079527344],"domain_scores_gemma":[0.9989104,0.00013831143,0.00020249096,0.00030442694,0.00031851744,0.00012584851],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00061031565,0.0005461627,0.00043785066,0.001072486,0.00036920686,0.00051798316,0.00055489386,0.0005636963,0.0008932393],"category_scores_gemma":[0.0015181322,0.00018849869,0.00048657026,0.0013833415,0.00036212805,0.0002967219,0.0007565139,0.0006375563,0.00074211595],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0017625884,0.0014824432,0.6497154,0.00052221055,0.0011199687,0.0010380549,0.0008896648,0.07704274,0.05683439,0.0033132571,0.101407304,0.104872],"study_design_scores_gemma":[0.0001363214,0.00015673926,0.91396976,0.00004701644,0.00006563167,0.00020455291,0.00027500832,0.06197332,0.0040938375,0.00075032713,0.018238075,0.000089393405],"about_ca_topic_score_codex":0.023293639,"about_ca_topic_score_gemma":0.040781807,"teacher_disagreement_score":0.023293639,"about_ca_system_score_codex":0.00028821928,"about_ca_system_score_gemma":0.00061134703,"threshold_uncertainty_score":0.046316147},"labels":[],"label_agreement":null},{"id":"W4404651090","doi":"10.1029/2024gl110058","title":"Localization and Delocalization During Seismic Slip","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Division of Earth Sciences","keywords":"Geology; Seismology; Slip (aerodynamics); Geophysics; Engineering; Aerospace engineering","score_opus":0.02703587810722408,"score_gpt":0.2782699477206469,"score_spread":0.2512340696134228,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404651090","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99659723,0.00014405504,0.0025623317,0.000018135452,0.0000026620385,0.0000043073705,0.0000971882,0.000031554737,0.00054253463],"genre_scores_gemma":[0.9992366,0.000029560506,0.0004686577,0.0000055930304,0.0000019383044,0.000002587389,0.00008809177,0.000007618972,0.00015940654],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99986744,0.000018609984,0.000009306708,0.000046929785,0.000029886713,0.000027775453],"domain_scores_gemma":[0.99859804,0.00028896434,0.000566439,0.00012749965,0.00029223895,0.00012681959],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003552938,0.00011074415,0.00015048444,0.00080357306,0.00015114681,0.00041920747,0.00021177366,0.00011481091,0.0009081084],"category_scores_gemma":[0.0018386968,0.00018440069,0.00006383145,0.00039389502,0.0003200144,0.00044124428,0.00055768073,0.00021821939,0.00014701665],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011569539,0.000051405586,0.35253203,0.00015672369,0.00008849334,0.00028750178,0.0019197024,0.004121334,0.57887053,0.0010717108,0.00035098096,0.05939263],"study_design_scores_gemma":[0.000013041113,0.00014278339,0.93824244,0.000021565313,0.000027534465,0.00032520553,0.0007112937,0.014853682,0.043459427,0.00083714863,0.0013361837,0.00002960656],"about_ca_topic_score_codex":0.0017903604,"about_ca_topic_score_gemma":0.002404718,"teacher_disagreement_score":0.0017903604,"about_ca_system_score_codex":0.0003087826,"about_ca_system_score_gemma":0.00011557994,"threshold_uncertainty_score":0.0035598278},"labels":[],"label_agreement":null},{"id":"W4404665411","doi":"10.1029/2024gl110312","title":"Forest Areas in China Are Recovering Since the 21st Century","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Land Use and Ecosystem Services","field":"Environmental Science","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China","keywords":"China; Geology; Environmental science; Climatology; Earth science; Geography; Physical geography; Archaeology","score_opus":0.0175600474897978,"score_gpt":0.26743292610284103,"score_spread":0.24987287861304322,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404665411","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99002224,0.0012220105,0.00026890627,0.00081160787,0.000032851596,0.000013567759,0.0018255883,0.00004101882,0.0057621473],"genre_scores_gemma":[0.9972529,0.00045500917,0.00017795965,0.00012209463,0.000022382776,0.000005080832,0.0012362642,0.000003025784,0.00072532584],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99984646,0.000011194965,0.000014721118,0.000033252916,0.000044255754,0.000050129736],"domain_scores_gemma":[0.99962914,0.0000168277,0.0001222612,0.000025576455,0.0001428002,0.000063455016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00039384866,0.00018633144,0.00012535759,0.0008817956,0.0003490131,0.0005617437,0.00024703448,0.00017543985,0.0016395093],"category_scores_gemma":[0.00056914875,0.000051833005,0.00022486103,0.0018030326,0.00025086178,0.0005974906,0.00042794645,0.00018212594,0.00014835899],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000038265927,0.000019305926,0.92875755,0.00012309705,0.000066710425,0.000304669,0.0008605209,0.0010254199,0.002130728,0.0013139007,0.0031978555,0.062162],"study_design_scores_gemma":[0.0000010448144,0.000008128581,0.9942299,0.0000074741656,0.000008276248,0.000052719617,0.00020657794,0.00032270633,0.00013539498,0.0001047787,0.004919654,0.0000033352185],"about_ca_topic_score_codex":0.04385628,"about_ca_topic_score_gemma":0.05711225,"teacher_disagreement_score":0.04385628,"about_ca_system_score_codex":0.000742683,"about_ca_system_score_gemma":0.0010132871,"threshold_uncertainty_score":0.08720201},"labels":[],"label_agreement":null},{"id":"W4404691701","doi":"10.1029/2024gl111242","title":"Heat Fluxes in a Glacial Fjord: The Role of Buoyancy‐Driven Circulation and Offshore Forcing","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta; Carleton University; University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; University of British Columbia; Killam Trusts; Polar Knowledge Canada; Canada Foundation for Innovation; Ontario Research Foundation","keywords":"Fjord; Buoyancy; Geology; Forcing (mathematics); Submarine pipeline; Glacial period; Circulation (fluid dynamics); Oceanography; Climatology; Geomorphology; Mechanics","score_opus":0.015271387612566002,"score_gpt":0.27729346083762424,"score_spread":0.2620220732250582,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404691701","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9988556,0.00002439327,0.00033558652,0.00006299689,0.000007570691,0.00000401063,0.00008119297,0.000020587597,0.00060793303],"genre_scores_gemma":[0.99954444,0.000012709184,0.00019631063,0.000011058919,0.0000023817715,0.0000033772312,0.000060108156,0.0000040154446,0.00016548601],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991393,0.000023572176,0.0000066545786,0.000014435047,0.000009854094,0.000031518037],"domain_scores_gemma":[0.99974364,0.00009721613,0.000039216022,0.000022671982,0.000029780564,0.00006742421],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028153195,0.00040328578,0.00039593168,0.00035038913,0.00066164543,0.000893561,0.0005290035,0.0008796385,0.0009414805],"category_scores_gemma":[0.0009602916,0.0002971542,0.0005317661,0.00029911887,0.0008543855,0.0003889218,0.0005230211,0.00043474152,0.00007357317],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023837708,0.00013934931,0.06665375,0.000023773018,0.00009739754,0.00031371915,0.00007470448,0.92492557,0.004965486,0.00076423166,0.00026634076,0.0015372409],"study_design_scores_gemma":[0.000112509304,0.00011405003,0.031784542,0.000009831263,0.000032330383,0.000026078653,0.00009063745,0.96645164,0.0008823923,0.00025428846,0.0002218409,0.000019860114],"about_ca_topic_score_codex":0.070917346,"about_ca_topic_score_gemma":0.037650775,"teacher_disagreement_score":0.070917346,"about_ca_system_score_codex":0.0011836168,"about_ca_system_score_gemma":0.0010747254,"threshold_uncertainty_score":0.14100909},"labels":[],"label_agreement":null},{"id":"W4404712706","doi":"10.1029/2024gl111481","title":"Early Season 2023 Wildfires Generated Record‐Breaking Surface Ozone Anomalies Across the U.S. Upper Midwest","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":29,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"NOAA Research; National Oceanic and Atmospheric Administration","keywords":"Ozone; Environmental science; Atmospheric sciences; Climatology; Ozone depletion; Climate change; Geology; Meteorology; Geography; Oceanography","score_opus":0.029935088562599153,"score_gpt":0.2927110918226035,"score_spread":0.2627760032600044,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404712706","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9956215,0.00007660392,0.00007839593,0.00019559836,0.000009103715,0.000006580972,0.0025002495,0.000019611398,0.001492335],"genre_scores_gemma":[0.9976139,0.000061902196,0.00009068523,0.0000729533,0.0000053169156,0.0000051169304,0.0015399099,0.0000036601361,0.00060652825],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.000009046536,0.0000053453214,0.00003186966,0.000022988112,0.00003457364],"domain_scores_gemma":[0.99966455,0.000022764169,0.000064631444,0.000020606156,0.00015212782,0.00007537692],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020996977,0.000165384,0.00011831883,0.0003476521,0.0005924877,0.000692784,0.00028252145,0.00024724466,0.0013967089],"category_scores_gemma":[0.00044207243,0.00010642207,0.0001508216,0.0004899806,0.00011654578,0.00023689531,0.0004130668,0.0003840392,0.00020717786],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001630125,0.00009141043,0.97760665,0.000016517888,0.000060690894,0.00017485705,0.00037617318,0.00058555725,0.0044922554,0.0000902479,0.003952039,0.012390616],"study_design_scores_gemma":[0.0000036945596,0.000019604273,0.99673873,0.0000085668735,0.000015707576,0.00002546182,0.0005392852,0.00072609173,0.00065306923,0.00003301695,0.0012329706,0.0000036619297],"about_ca_topic_score_codex":0.40451646,"about_ca_topic_score_gemma":0.56059885,"teacher_disagreement_score":0.40451646,"about_ca_system_score_codex":0.0010619558,"about_ca_system_score_gemma":0.0011622687,"threshold_uncertainty_score":0.8043238},"labels":[],"label_agreement":null},{"id":"W4404799131","doi":"10.1029/2024gl111113","title":"Amapari Marker Band, Gale Crater, Mars: Event Horizon With Highest Bedrock Iron and Zinc Concentrations Detected by <i>Curiosity's</i> Alpha Particle X‐Ray Spectrometer","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":15,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph; University of New Brunswick","funders":"Canadian Space Agency; California Institute of Technology","keywords":"Impact crater; Mars Exploration Program; Alpha particle; Zinc; Geology; Alpha (finance); Event (particle physics); Bedrock; Event horizon; Particle (ecology); Astrobiology; Physics; Astrophysics; Materials science; Nuclear physics; Geomorphology; Metallurgy; Political science","score_opus":0.013278720487330977,"score_gpt":0.258793510836091,"score_spread":0.24551479034876,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404799131","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99704474,0.00013621591,0.00008947726,0.000059518818,0.000006190805,0.000004449618,0.0008221963,0.0000355316,0.0018017706],"genre_scores_gemma":[0.9980661,0.000068259265,0.0003436858,0.000026333868,0.0000062552353,0.0000042034653,0.00073933206,0.000007919162,0.0007378128],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999572,0.0000032933203,0.0000020733623,0.0000128657675,0.000011554067,0.00001305995],"domain_scores_gemma":[0.9999019,0.000009381564,0.000037490667,0.0000071131576,0.000017929438,0.00002613185],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000058801947,0.00024363463,0.0001404252,0.0010694696,0.00052232813,0.0005684521,0.00023166831,0.00033721083,0.0017085106],"category_scores_gemma":[0.00015519443,0.00014151508,0.000106325206,0.00064162305,0.00032699518,0.00018491023,0.0004378813,0.00021974836,0.00029391484],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00042431362,0.000050307415,0.9153563,0.000077371034,0.00013455903,0.0016402622,0.000992396,0.0004845153,0.061371565,0.00021164362,0.0026057027,0.016650997],"study_design_scores_gemma":[0.0000032436812,0.00001676184,0.9973628,0.0000037642724,0.0000047277454,0.00026877708,0.00022039529,0.00007843641,0.00087510154,0.00001764443,0.0011462207,0.00000208958],"about_ca_topic_score_codex":0.012511013,"about_ca_topic_score_gemma":0.023905551,"teacher_disagreement_score":0.012511013,"about_ca_system_score_codex":0.00022556467,"about_ca_system_score_gemma":0.00013519889,"threshold_uncertainty_score":0.024876356},"labels":[],"label_agreement":null},{"id":"W4404862339","doi":"10.1029/2024gl111183","title":"Iridescence Reveals the Formation and Growth of Ice Aerosols in Martian Noctilucent Clouds","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Agencia Estatal de Investigación; Ministerio de Ciencia e Innovación; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Martian; Astrobiology; Iridescence; Atmospheric sciences; Geology; Mars Exploration Program; Physics; Optics","score_opus":0.03427623246278379,"score_gpt":0.2990854638893292,"score_spread":0.26480923142654544,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4404862339","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986842,0.00008131316,0.00014833237,0.000009486135,0.0000022053368,0.0000027902543,0.0000691916,0.000014631826,0.000987801],"genre_scores_gemma":[0.9990582,0.00004103944,0.00029661498,0.000010960933,0.0000044838466,0.0000023881303,0.00016578831,0.000005114154,0.00041530727],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999788,0.0000012140808,6.067485e-7,0.0000045287375,0.000006919099,0.000007995141],"domain_scores_gemma":[0.99994814,0.0000068082686,0.000012670041,0.0000032160813,0.000011463809,0.000017764929],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00004918891,0.000117962605,0.00006254226,0.00046339512,0.0002092862,0.00016858667,0.00008479551,0.00015212307,0.0007961436],"category_scores_gemma":[0.000079332756,0.00007145233,0.00007498261,0.00013633267,0.00010287026,0.000103412385,0.00012888502,0.00014091615,0.00011502535],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003657142,0.000063860294,0.11450768,0.000025636013,0.000019969382,0.0009738694,0.00030659593,0.00028015743,0.87355727,0.000105282095,0.00038067557,0.009413171],"study_design_scores_gemma":[0.0000058291803,0.000101883175,0.9533418,0.0000041162934,0.000006586996,0.0007706996,0.00016665005,0.0013943434,0.043166623,0.000039801875,0.000997317,0.0000043787304],"about_ca_topic_score_codex":0.0037089493,"about_ca_topic_score_gemma":0.004627627,"teacher_disagreement_score":0.0037089493,"about_ca_system_score_codex":0.00016312153,"about_ca_system_score_gemma":0.000048149548,"threshold_uncertainty_score":0.0073747635},"labels":[],"label_agreement":null},{"id":"W4405008350","doi":"10.1029/2024gl112155","title":"No Temporal Change Seen in High‐Frequency Waves Scattered Near the Core‐Mantle Boundary","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Institute of Geology and Geophysics, Chinese Academy of Sciences; National Science Foundation","keywords":"Mantle (geology); Geology; Core–mantle boundary; Geophysics; Cosmic microwave background; Scattering; Observable; Diffraction; Seismology; Inner core; Seismic wave; Travel time; Core (optical fiber); Physics; Optics; Anisotropy","score_opus":0.0580636621930575,"score_gpt":0.30142733782046144,"score_spread":0.24336367562740394,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405008350","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99825424,0.000051679206,0.00027762196,0.000014048822,0.0000035308615,0.0000021277162,0.0001044871,0.000010629475,0.0012814671],"genre_scores_gemma":[0.9994041,0.000020323223,0.00011230429,0.000008638366,0.0000027301173,0.0000022478073,0.00014901657,0.0000024317112,0.00029827838],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999453,0.0000045572406,0.000002662985,0.0000145763415,0.00001925735,0.000013699607],"domain_scores_gemma":[0.9996835,0.000050543826,0.00008041879,0.000038581857,0.000090174086,0.00005676859],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010185705,0.00007251789,0.00010738397,0.00037763937,0.00022242949,0.00027936455,0.0001455494,0.00021759835,0.0014843569],"category_scores_gemma":[0.00061740424,0.000093124705,0.00004848198,0.00027842302,0.00026003394,0.00018969082,0.00032987053,0.00022472662,0.00022998052],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053890224,0.00010740828,0.61668813,0.00006283128,0.00006480387,0.0006363648,0.0010854631,0.0006987091,0.3547019,0.0004251219,0.000654863,0.024335487],"study_design_scores_gemma":[0.0000034416141,0.00004792961,0.99263716,0.0000045637744,0.000004582921,0.00017757031,0.00020748594,0.00030092505,0.005992513,0.00003326592,0.0005878782,0.000002688996],"about_ca_topic_score_codex":0.0038629894,"about_ca_topic_score_gemma":0.0065438855,"teacher_disagreement_score":0.0038629894,"about_ca_system_score_codex":0.00014252396,"about_ca_system_score_gemma":0.00008932693,"threshold_uncertainty_score":0.007681012},"labels":[],"label_agreement":null},{"id":"W4405240483","doi":"10.1029/2024gl113002","title":"Comparing Point Source CO <sub>2</sub> Emission Rate Estimates From Near‐Simultaneous OCO‐3 and EMIT Observations","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto; Environment and Climate Change Canada","funders":"Nuclear Safety and Security Commission; California Institute of Technology; Jet Propulsion Laboratory; National Aeronautics and Space Administration","keywords":"Point source; Environmental science; Mineralogy; Materials science; Geology; Physics; Optics","score_opus":0.025778859959669193,"score_gpt":0.27093812972319303,"score_spread":0.24515926976352384,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405240483","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99380374,0.00008334338,0.00399855,0.00003218221,0.000010574076,0.000010243078,0.0008733332,0.00009995807,0.0010881175],"genre_scores_gemma":[0.99628663,0.000032290256,0.0021493777,0.00001660357,0.0000063572793,0.000007846907,0.001336605,0.000016146412,0.0001480258],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999729,0.00002214458,0.0000110917845,0.00009888018,0.00009111405,0.0000477723],"domain_scores_gemma":[0.9996227,0.000080567734,0.00008330585,0.000054844106,0.0001284894,0.000030064186],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00047450294,0.00045449263,0.00025772466,0.0006860442,0.0002587055,0.00041478797,0.000381657,0.0004174433,0.0005145128],"category_scores_gemma":[0.00069361506,0.00018144578,0.00045504447,0.00082838105,0.0002294555,0.0005431895,0.00045852154,0.00024563514,0.00016654888],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031911806,0.0001366937,0.8711184,0.00007551983,0.0003878514,0.0001337607,0.00014198845,0.051265765,0.041082196,0.00037476906,0.0009246107,0.034039315],"study_design_scores_gemma":[0.000034904173,0.00005564059,0.89609253,0.000013239061,0.00012357975,0.0000899181,0.00014711947,0.08668601,0.014894961,0.00027026454,0.0015553599,0.0000365522],"about_ca_topic_score_codex":0.025837686,"about_ca_topic_score_gemma":0.04884835,"teacher_disagreement_score":0.025837686,"about_ca_system_score_codex":0.0004568826,"about_ca_system_score_gemma":0.00036735783,"threshold_uncertainty_score":0.051374614},"labels":[],"label_agreement":null},{"id":"W4405279925","doi":"10.1029/2024gl112308","title":"Skillful Prediction of Indian Monsoon Intraseasonal Precipitation Using Central Indian Ocean Mode and Machine Learning","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"National Key Research and Development Program of China; Directorate for Engineering; National Natural Science Foundation of China","keywords":"Climatology; Indian ocean; Precipitation; Monsoon; Geology; Mode (computer interface); Madden–Julian oscillation; Monsoon of South Asia; Oceanography; Meteorology; Geography; Convection; Computer science","score_opus":0.033260829235952145,"score_gpt":0.30056832707014,"score_spread":0.26730749783418783,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405279925","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86074823,0.00012236614,0.13465765,0.00031342017,0.00006195953,0.000020399646,0.00013001656,0.0007975706,0.0031483865],"genre_scores_gemma":[0.993775,0.000013298727,0.0059497575,0.000013689715,0.000009411127,0.0000034334555,0.00004008495,0.000010589532,0.00018485133],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991083,0.000028140152,0.000004886315,0.00002134401,0.000017915532,0.000016908576],"domain_scores_gemma":[0.9991738,0.00044023638,0.0001176881,0.0000872694,0.00011876382,0.000062264924],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005527689,0.00034984044,0.00023182342,0.00025243714,0.00014720786,0.0004301202,0.00029506316,0.00020801158,0.00040848544],"category_scores_gemma":[0.0022812919,0.00013109653,0.00021281955,0.00022794808,0.00021327926,0.00031039855,0.00047438627,0.0005284817,0.00009586453],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017716583,0.00008451557,0.03963925,0.00002338784,0.000079532954,0.000071201895,0.0000339349,0.8969959,0.013776935,0.001913953,0.0006996614,0.046504583],"study_design_scores_gemma":[0.000002233371,0.000006357308,0.0023598156,8.753483e-7,0.0000018595688,0.000002317628,0.000001808168,0.9964869,0.00079966214,0.00029247286,0.000043211763,0.0000025395145],"about_ca_topic_score_codex":0.00892519,"about_ca_topic_score_gemma":0.006589391,"teacher_disagreement_score":0.00892519,"about_ca_system_score_codex":0.00026099465,"about_ca_system_score_gemma":0.00060115603,"threshold_uncertainty_score":0.017746508},"labels":[],"label_agreement":null},{"id":"W4405880863","doi":"10.1029/2024gl111386","title":"Antarctic Wide Subglacial Hydrology Modeling","year":2024,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo","funders":"Australian Research Council; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Discovery Eye Foundation","keywords":"Meltwater; Geology; Glacier; Ice sheet; Cryosphere; Ice stream; Ice divide; Hydrology (agriculture); Geomorphology; Drainage system (geomorphology); Antarctic ice sheet; Ice shelf; Shelf ice; Oceanography; Drainage; Sea ice","score_opus":0.057117325913946575,"score_gpt":0.30343138625707955,"score_spread":0.24631406034313297,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4405880863","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97253317,0.00017604067,0.0071225627,0.00034840984,0.000042279626,0.00003649434,0.0072603975,0.00043015095,0.012050377],"genre_scores_gemma":[0.99065864,0.00020941939,0.0029099002,0.00007116111,0.000017503779,0.000067931745,0.0026058578,0.00009159419,0.0033680105],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999232,0.000023257853,0.0000039328634,0.000023274184,0.000009794822,0.000016499731],"domain_scores_gemma":[0.99982053,0.00006559847,0.000021667527,0.000028862238,0.00003784496,0.000025486095],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017149386,0.00052023306,0.00040589174,0.00033875395,0.00039746155,0.0007707495,0.000931976,0.0006910145,0.005505179],"category_scores_gemma":[0.00045857247,0.00036068063,0.0008091484,0.000699065,0.00028087696,0.00048081437,0.00038986953,0.00057082716,0.00055839744],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00003195823,0.00001956308,0.005590868,0.000012573055,0.000040597657,0.00004102027,0.00002562243,0.99055594,0.0004937066,0.0006629927,0.0007224003,0.0018027641],"study_design_scores_gemma":[0.00004470654,0.000018496401,0.005255026,0.0000044164017,0.00002145264,0.0000140405555,0.000037526454,0.9919281,0.00031718874,0.0006643912,0.0016844186,0.000010276631],"about_ca_topic_score_codex":0.07942046,"about_ca_topic_score_gemma":0.057086717,"teacher_disagreement_score":0.07942046,"about_ca_system_score_codex":0.0010171003,"about_ca_system_score_gemma":0.0012707398,"threshold_uncertainty_score":0.15791637},"labels":[],"label_agreement":null},{"id":"W4406481946","doi":"10.1029/2023gl108081","title":"Regional Hotspots of Change in Northern High Latitudes Informed by Observations From Space","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"NASA Earth Science Technology Office; Generalitat de Catalunya; Gordon and Betty Moore Foundation","keywords":"Latitude; Climatology; Climate change; Space (punctuation); Geology; Geography; Environmental science; Oceanography; Geodesy; Computer science","score_opus":0.1591465261010567,"score_gpt":0.3384106730381162,"score_spread":0.17926414693705953,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406481946","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99719393,0.00009617735,0.0005460618,0.000014748401,0.0000032488126,0.0000038370795,0.0011350674,0.000037989335,0.0009689854],"genre_scores_gemma":[0.99890983,0.00001909269,0.00039535476,0.000002851945,0.000003551619,0.0000026026757,0.0005840098,0.0000032187158,0.000079495236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998847,0.000032740907,0.0000099703875,0.000036319667,0.000016600246,0.000019669636],"domain_scores_gemma":[0.9992919,0.00018743618,0.00026378897,0.00008030063,0.00011125218,0.00006538825],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005261856,0.00011995446,0.00015602847,0.0011307503,0.00018150236,0.0005807171,0.00011102701,0.00011892069,0.0011648152],"category_scores_gemma":[0.0008183312,0.00006603917,0.00015974078,0.000991495,0.00015757639,0.0002617722,0.0003076759,0.00012289154,0.00020538039],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011423335,0.000008936813,0.9880156,0.00001871468,0.000053916498,0.000045161276,0.00029874712,0.001799635,0.0029970487,0.00009731782,0.00027716366,0.0062735337],"study_design_scores_gemma":[0.0000012826811,0.0000074677587,0.9973693,0.00000398045,0.000009873634,0.00001793612,0.00017967526,0.0019022275,0.00023557853,0.000050203504,0.00021960073,0.0000029318694],"about_ca_topic_score_codex":0.011155659,"about_ca_topic_score_gemma":0.020124372,"teacher_disagreement_score":0.011155659,"about_ca_system_score_codex":0.00016018402,"about_ca_system_score_gemma":0.00011761453,"threshold_uncertainty_score":0.022181451},"labels":[],"label_agreement":null},{"id":"W4406531128","doi":"10.1029/2024gl110679","title":"Peat Depth and Carbon Storage of the Hudson Bay Lowlands, Canada","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Ministry of Natural Resources and Forestry; University of Toronto; Canadian Forest Service; Toronto Metropolitan University; World Wildlife Fund Canada; Natural Resources Canada; Ontario Forest Research Institute; McMaster University","funders":"Natural Sciences and Engineering Research Council of Canada; Environment and Climate Change Canada; Canada Research Chairs; Parks Canada; Ontario Ministry of Natural Resources and Forestry; World Wildlife Fund","keywords":"Peat; Bay; Carbon fibers; Oceanography; Geology; Environmental science; Blue carbon; Earth science; Physical geography; Carbon sequestration; Geography; Carbon dioxide; Archaeology; Ecology","score_opus":0.010536015372564557,"score_gpt":0.2551385690460941,"score_spread":0.24460255367352957,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406531128","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9963559,0.0002476829,0.000064506174,0.000066423076,0.0000039599927,0.0000047559356,0.0022578225,0.0000098211185,0.0009893009],"genre_scores_gemma":[0.99867153,0.0000849007,0.00009728809,0.000013589671,0.000001275427,0.0000027966817,0.0005794072,0.0000020254197,0.0005471454],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999057,0.000006553517,0.000005864034,0.000021571992,0.000030749965,0.000029551626],"domain_scores_gemma":[0.99940956,0.000040547962,0.00009317705,0.000016208507,0.00031628288,0.00012420354],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015954548,0.00015610362,0.00016084139,0.0010010698,0.0006128863,0.00072903244,0.0002893909,0.00010421353,0.0015031305],"category_scores_gemma":[0.00059974816,0.0001064978,0.000115927185,0.0014056902,0.00032458064,0.00022529795,0.00035847438,0.0001505858,0.00013977542],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006297111,0.000017212948,0.99002504,0.000030432722,0.0000459872,0.000091329224,0.00032646823,0.00045490987,0.0010424422,0.00012405572,0.0007527673,0.0070264563],"study_design_scores_gemma":[0.0000025901154,0.0000032944588,0.9985777,0.000012116015,0.0000057310867,0.00001073747,0.00044950005,0.00035063195,0.000108453605,0.000019023391,0.00045719172,0.000003033244],"about_ca_topic_score_codex":0.98067904,"about_ca_topic_score_gemma":0.9924338,"teacher_disagreement_score":0.019320965,"about_ca_system_score_codex":0.008056891,"about_ca_system_score_gemma":0.0052927467,"threshold_uncertainty_score":0.058457136},"labels":[],"label_agreement":null},{"id":"W4406667363","doi":"10.1029/2024gl110803","title":"Temperature Anomalies During Late Boreal Winters With and Without Sudden Stratospheric Warming","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Väisälän Rahasto; Lapin Rahasto; Suomen Kulttuurirahasto; Suomalainen Tiedeakatemia; Academy of Finland","keywords":"Climatology; Boreal; Sudden stratospheric warming; Environmental science; Atmospheric sciences; Stratosphere; Global warming; Climate change; Polar vortex; Geology; Oceanography","score_opus":0.014367888277428702,"score_gpt":0.27923472347216566,"score_spread":0.26486683519473697,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406667363","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99875474,0.000039287715,0.00008298496,0.000031546115,0.000019046336,0.0000024417839,0.00052002893,0.000017291188,0.0005325015],"genre_scores_gemma":[0.99916935,0.000012094762,0.000047382673,0.0000065706045,0.000011754707,0.000002016228,0.0006833541,0.0000020240805,0.00006535337],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99988973,0.00001874177,0.000009846875,0.000028652668,0.000023459028,0.000029508545],"domain_scores_gemma":[0.9996525,0.00006952538,0.00010117118,0.000026648484,0.000065138316,0.00008502082],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00029461985,0.00032174346,0.00024624975,0.0004025996,0.0003844388,0.00060472783,0.00019720233,0.00032539334,0.000712755],"category_scores_gemma":[0.0005421583,0.00008367761,0.00029770518,0.00030816437,0.00024737598,0.0002844287,0.00024318878,0.00022115897,0.00011752709],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006917429,0.00010860187,0.9833339,0.000020562318,0.00012929078,0.00019282303,0.00013367916,0.0035284911,0.0069183363,0.00014084933,0.00088602764,0.0039157327],"study_design_scores_gemma":[0.0000073834317,0.000052084335,0.99766135,0.0000016206848,0.00000961388,0.000032046974,0.000062836305,0.0017257425,0.00020785828,0.000026087397,0.00021027235,0.0000030659023],"about_ca_topic_score_codex":0.019388115,"about_ca_topic_score_gemma":0.029650988,"teacher_disagreement_score":0.019388115,"about_ca_system_score_codex":0.0003406834,"about_ca_system_score_gemma":0.00021671344,"threshold_uncertainty_score":0.038550496},"labels":[],"label_agreement":null},{"id":"W4406763136","doi":"10.1029/2024gl111961","title":"Exploring Causal Relationships and Adjustment Timescales of Aerosol‐Cloud Interactions in Geostationary Satellite Observations and CAM6 Using Wavelet Phase Coherence Analysis","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric aerosols and clouds","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"Office of Science; National Oceanic and Atmospheric Administration; U.S. Department of Energy","keywords":"Liquid water path; Environmental science; Cloud top; Atmospheric sciences; Entrainment (biomusicology); Satellite; Meteorology; Context (archaeology); Lag; Cloud computing; Geostationary orbit; Coherence (philosophical gambling strategy); Daytime; Geostationary Operational Environmental Satellite; Aerosol; Mathematics; Physics; Statistics; Computer science; Geology","score_opus":0.18038537988592715,"score_gpt":0.36202176586446366,"score_spread":0.1816363859785365,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406763136","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99787426,0.00007446654,0.00112398,0.00006398421,0.000008138955,0.00000569686,0.0003166873,0.000022254075,0.00051050214],"genre_scores_gemma":[0.9992575,0.000018094152,0.00040605405,0.000007712009,0.000007079834,0.0000037643194,0.00024904707,0.0000044637136,0.000046337373],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99987364,0.00003197915,0.0000102966615,0.0000355233,0.00002296336,0.00002557298],"domain_scores_gemma":[0.99914455,0.00043770627,0.00020635437,0.000067794215,0.0000832425,0.00006020806],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006907149,0.00018598922,0.00012204314,0.0006173977,0.00021869491,0.00047877053,0.00018324022,0.00029231387,0.0007993524],"category_scores_gemma":[0.0024755653,0.0001685579,0.0002495973,0.00069342897,0.00018066615,0.00040710598,0.0004200305,0.00030968853,0.00007328852],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00037750186,0.00011378068,0.938022,0.00006182033,0.00024705287,0.0002429459,0.00033094612,0.014280528,0.0235589,0.0014391879,0.00073047605,0.020594792],"study_design_scores_gemma":[0.000018225626,0.000022672188,0.9513379,0.000007922754,0.00002403886,0.000023047744,0.00006892726,0.04638379,0.0013061976,0.00034023175,0.00045613348,0.000010963679],"about_ca_topic_score_codex":0.012319466,"about_ca_topic_score_gemma":0.011808513,"teacher_disagreement_score":0.012319466,"about_ca_system_score_codex":0.0002319145,"about_ca_system_score_gemma":0.00023844394,"threshold_uncertainty_score":0.024495542},"labels":[],"label_agreement":null},{"id":"W4406763202","doi":"10.1029/2024gl113290","title":"Coherence‐Based Characterization of a Long‐Period Monochromatic Seismic Signal","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Seismology and Earthquake Studies","field":"Computer Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Japan Society for the Promotion of Science","keywords":"Coherence (philosophical gambling strategy); Monochromatic color; Seismology; SIGNAL (programming language); Period (music); Geology; Geophysics; Physics; Geodesy; Optics; Acoustics; Computer science","score_opus":0.03255362750405953,"score_gpt":0.3124655239139068,"score_spread":0.27991189640984726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406763202","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.8921106,0.0005057645,0.10138538,0.00014574341,0.000025441635,0.00002874646,0.0014281637,0.000249101,0.0041210935],"genre_scores_gemma":[0.9817052,0.00015349765,0.016869556,0.000024160054,0.000023431536,0.00001154751,0.0007671868,0.000020793628,0.00042472794],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99989533,0.000009381297,0.0000048574143,0.000026855307,0.000034975652,0.000028585226],"domain_scores_gemma":[0.99964285,0.000088387584,0.00009916902,0.0000409838,0.000093461815,0.00003515316],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016300446,0.00028810225,0.00017670993,0.0014105721,0.00016656175,0.00041351788,0.00020887454,0.00022341018,0.0013151404],"category_scores_gemma":[0.0006391652,0.00009786638,0.00012087776,0.0012996081,0.00022748845,0.0003693628,0.0003521382,0.00017933619,0.00018796205],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00055471755,0.00013672924,0.061393037,0.00025862348,0.00014286353,0.0007703096,0.00032046484,0.03574562,0.7004712,0.004613924,0.0019746448,0.19361787],"study_design_scores_gemma":[0.000037086927,0.00034359732,0.46058688,0.000033239623,0.000111617395,0.00075085566,0.00037938243,0.46194717,0.06790291,0.0030452579,0.004796678,0.00006534721],"about_ca_topic_score_codex":0.0038990371,"about_ca_topic_score_gemma":0.0067261397,"teacher_disagreement_score":0.0038990371,"about_ca_system_score_codex":0.00023478745,"about_ca_system_score_gemma":0.00029254137,"threshold_uncertainty_score":0.007752657},"labels":[],"label_agreement":null},{"id":"W4406805096","doi":"10.1029/2024gl113112","title":"Mercury Isotopes Track the Causes of Carbon Perturbations in the Early Permian Ocean and Continent","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada","funders":"National Natural Science Foundation of China","keywords":"Mercury (programming language); Isotope; Isotopes of carbon; Geology; Permian; Environmental science; Oceanography; Earth science; Paleontology; Nuclear physics","score_opus":0.030330367145376937,"score_gpt":0.31780625236211313,"score_spread":0.28747588521673617,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406805096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99874026,0.00011812775,0.00015040567,0.000055148827,0.0000033916328,0.000001053873,0.000097728596,0.00001090972,0.00082308217],"genre_scores_gemma":[0.9996778,0.000046443503,0.00007193331,0.000012994911,0.0000025233526,6.715781e-7,0.00004961176,0.000002773497,0.00013522219],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999578,0.0000058212063,0.0000019714673,0.000014022867,0.000009132384,0.000011124868],"domain_scores_gemma":[0.9999244,0.00000857217,0.000023905031,0.0000066341745,0.00001974319,0.000016589574],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018588798,0.00016224927,0.00010586701,0.00053990714,0.00027868222,0.00030879877,0.000157851,0.00018634424,0.00085581833],"category_scores_gemma":[0.00022438492,0.00008900621,0.00008846347,0.00049748964,0.00032371195,0.00022671369,0.00031765108,0.00015103574,0.00008270787],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00019186507,0.000022979837,0.8904637,0.00002937168,0.00009275724,0.00012764038,0.0003515593,0.0008707369,0.08985547,0.00032903525,0.00017929455,0.017485572],"study_design_scores_gemma":[0.0000023879843,0.000018421273,0.9952998,0.000002220319,0.000011453288,0.000025172483,0.00014567235,0.000813196,0.0029164595,0.0001424759,0.00062006264,0.0000026244693],"about_ca_topic_score_codex":0.009855703,"about_ca_topic_score_gemma":0.011956438,"teacher_disagreement_score":0.009855703,"about_ca_system_score_codex":0.0003799778,"about_ca_system_score_gemma":0.00024494383,"threshold_uncertainty_score":0.019596696},"labels":[],"label_agreement":null},{"id":"W4406806556","doi":"10.1029/2024gl111269","title":"Evidence of Unusually Strong Equatorial Ionization Anomaly at Three Local Time Sectors During the Mother's Day Geomagnetic Storm On 10–11 May 2024","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":34,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Agência Espacial Brasileira; Conselho Nacional de Desenvolvimento Científico e Tecnológico; Ministério da Ciência, Tecnologia e Inovação; Nuclear Safety and Security Commission; National Atmospheric Research Laboratory; Fundação de Amparo à Pesquisa do Estado de São Paulo; National Aeronautics and Space Administration; National Science Foundation","keywords":"Geomagnetic storm; Anomaly (physics); Storm; Geology; Geophysics; Earth's magnetic field; Ionization; Atmospheric sciences; Ionosphere; Climatology; Physics; Oceanography; Ion; Magnetic field","score_opus":0.01554940690945055,"score_gpt":0.27884842356194,"score_spread":0.26329901665248945,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406806556","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999052,0.000019136003,0.00006876828,0.000013314949,0.000004081629,0.000001909507,0.000087798755,0.0000063068774,0.00074677455],"genre_scores_gemma":[0.9995276,0.000013158797,0.000075460375,0.0000064010355,0.000004418309,0.000001556106,0.00013790978,0.000001483744,0.00023201905],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999535,0.0000043111118,0.0000020329653,0.000009775549,0.00001388975,0.000016438049],"domain_scores_gemma":[0.9998889,0.000011355043,0.00003802859,0.000009589181,0.000019900783,0.00003223722],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009159186,0.0001214551,0.00017894058,0.0003523528,0.0004057892,0.0002846604,0.00012300642,0.00021333907,0.0009772717],"category_scores_gemma":[0.0001455175,0.000087529035,0.000105348074,0.00022101079,0.00020060784,0.00011643859,0.00033148463,0.00023050782,0.00013734089],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00072348147,0.00009924555,0.7762435,0.000043846583,0.00007924386,0.002793794,0.0010165933,0.0005303325,0.20518176,0.00018952394,0.00074419397,0.01235449],"study_design_scores_gemma":[0.0000030498663,0.00004483644,0.9968959,0.0000017306597,0.000006193217,0.000121855075,0.00019918766,0.0001840929,0.0021876893,0.000011312214,0.000341331,0.0000028041754],"about_ca_topic_score_codex":0.006096071,"about_ca_topic_score_gemma":0.013831937,"teacher_disagreement_score":0.006096071,"about_ca_system_score_codex":0.00022888085,"about_ca_system_score_gemma":0.00012972098,"threshold_uncertainty_score":0.012121141},"labels":[],"label_agreement":null},{"id":"W4406823299","doi":"10.1029/2024gl110601","title":"The Metabolic Balance of Lake Superior's Mixed Layer","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fish Ecology and Management Studies","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ministry of Natural Resources and Forestry; Trent University","funders":"Directorate for Engineering; U.S. Environmental Protection Agency","keywords":"Balance (ability); Mixed layer; Layer (electronics); Water balance; Geology; Environmental science; Climatology; Biology; Chemistry; Geotechnical engineering","score_opus":0.018229522437290244,"score_gpt":0.2931788051960979,"score_spread":0.27494928275880764,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4406823299","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994362,0.000017204964,0.00012612483,0.000007887253,6.0958166e-7,9.856061e-7,0.0001498122,0.000006383845,0.00025487054],"genre_scores_gemma":[0.99959606,0.000007172088,0.00015766831,0.0000023672428,3.9643456e-7,0.0000010921573,0.00015217876,0.0000011653616,0.000081939725],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997234,0.0000032655041,0.0000021544138,0.000008219739,0.000007892116,0.000006153172],"domain_scores_gemma":[0.99994254,0.000009168503,0.000016579277,0.0000033741135,0.000016803433,0.00001148861],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000127048,0.00017744608,0.00011004665,0.00025534316,0.0002737825,0.00044626178,0.000113004724,0.00016235544,0.00065868866],"category_scores_gemma":[0.00024037894,0.00012402,0.00016609073,0.00028076372,0.00014693537,0.0002752067,0.0002637297,0.000098547105,0.0000656259],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00024447415,0.000029164712,0.85335696,0.00007069734,0.0001486445,0.00015468484,0.0004191546,0.0388416,0.09598702,0.00040393556,0.00041380792,0.009929866],"study_design_scores_gemma":[0.000013372659,0.000046126814,0.9110154,0.000007408207,0.00003367219,0.00002978364,0.00017686277,0.081108086,0.0068519358,0.00016547073,0.0005393468,0.000012433109],"about_ca_topic_score_codex":0.060565833,"about_ca_topic_score_gemma":0.05793955,"teacher_disagreement_score":0.9394342,"about_ca_system_score_codex":0.0007803749,"about_ca_system_score_gemma":0.00042598243,"threshold_uncertainty_score":0.120426595},"labels":[],"label_agreement":null},{"id":"W4407057994","doi":"10.1029/2024gl110453","title":"Double Reflections in Polarized Radar Data Reveal Ice Fabric in the North East Greenland Ice Stream","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Manitoba","funders":"Danmarks Frie Forskningsfond; Novo Nordisk; Novo Nordisk Fonden; Canada Excellence Research Chairs, Government of Canada","keywords":"Geology; Anisotropy; Ice stream; Birefringence; Ice crystals; Radar; Orientation (vector space); Antarctic sea ice; Arctic ice pack; Sea ice; Geodesy; Remote sensing; Climatology; Meteorology; Cryosphere; Optics; Geometry; Physics","score_opus":0.10416135844956347,"score_gpt":0.3439414228410432,"score_spread":0.2397800643914797,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407057994","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993556,0.000024060726,0.0001035414,0.00000721261,0.0000016474651,0.0000016936884,0.00015728126,0.0000061081823,0.00034280503],"genre_scores_gemma":[0.9992173,0.000032755455,0.00027648875,0.0000091772,0.0000030443362,0.0000023899004,0.00029140018,0.000003851225,0.00016358186],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993503,0.000007173138,0.000002974855,0.000014519684,0.00001809791,0.000022193102],"domain_scores_gemma":[0.99979585,0.00003028154,0.000056971745,0.000016150323,0.00006781712,0.000032939493],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015224004,0.00014710303,0.00015070588,0.000969473,0.00023171931,0.00036729322,0.000094964234,0.00011900531,0.0004813725],"category_scores_gemma":[0.00023731445,0.00009656631,0.000078868405,0.000617738,0.00025147147,0.00013673979,0.00017452768,0.00011158954,0.0001569608],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0002554018,0.000059821254,0.8295165,0.00003600089,0.000046413137,0.00042499305,0.0007707776,0.0008966695,0.15002191,0.000106140884,0.0005405619,0.017324785],"study_design_scores_gemma":[0.0000025966526,0.000010083132,0.99703825,0.0000027370438,0.0000060910725,0.000068633664,0.00019801673,0.0006480918,0.0017669965,0.000011992827,0.00024409237,0.000002346518],"about_ca_topic_score_codex":0.026187802,"about_ca_topic_score_gemma":0.06488293,"teacher_disagreement_score":0.026187802,"about_ca_system_score_codex":0.0002842387,"about_ca_system_score_gemma":0.00024288223,"threshold_uncertainty_score":0.052070737},"labels":[],"label_agreement":null},{"id":"W4407175013","doi":"10.1029/2024gl113926","title":"Mars' Hemispheric Magnetic Field From a Full‐Sphere Dynamo","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung; National Aeronautics and Space Administration","keywords":"Dynamo; Mars Exploration Program; Dynamo theory; Geophysics; Mercury's magnetic field; Physics; Magnetic field; Field (mathematics); Geology; Astrobiology; Geodesy; Astronomy; Earth's magnetic field; L-shell; Mathematics","score_opus":0.014696279962007544,"score_gpt":0.2817359242497186,"score_spread":0.26703964428771104,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407175013","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99214077,0.00006473898,0.00090787775,0.00031014998,0.000021921256,0.000011376591,0.0004385789,0.00011422114,0.0059904074],"genre_scores_gemma":[0.9991135,0.000031977645,0.0002567023,0.000030297171,0.0000073526,0.000007378041,0.00019886497,0.00002660482,0.00032732714],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99991906,0.000022024917,0.00000292666,0.000014580562,0.000014047861,0.00002733248],"domain_scores_gemma":[0.9997203,0.00008101333,0.00003386203,0.000035026867,0.00004130631,0.000088442495],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000214805,0.0004135514,0.0005308722,0.0002597819,0.00057363167,0.00067013816,0.0006641346,0.0009087385,0.0027477227],"category_scores_gemma":[0.0007916793,0.00025174543,0.0005486081,0.0003194069,0.00073568575,0.000512636,0.0005473259,0.0005693956,0.00018992611],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032569328,0.000128716,0.008035822,0.000046797624,0.000096372205,0.00037734935,0.000114392016,0.9787419,0.006427645,0.0028191428,0.0013457872,0.0015403004],"study_design_scores_gemma":[0.00021399085,0.00009376103,0.008101073,0.000006548625,0.000029068067,0.000049330058,0.00008282909,0.9888947,0.0010094172,0.0008338775,0.0006658676,0.000019585592],"about_ca_topic_score_codex":0.015704004,"about_ca_topic_score_gemma":0.005532336,"teacher_disagreement_score":0.015704004,"about_ca_system_score_codex":0.0008581987,"about_ca_system_score_gemma":0.0006640121,"threshold_uncertainty_score":0.031225204},"labels":[],"label_agreement":null},{"id":"W4407346972","doi":"10.1029/2024gl112900","title":"Identifying Typical Relativistic Electron Pitch Angle Distributions: Evolution During Geomagnetic Storms","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Science and Technology Facilities Council; Natural Environment Research Council; Sight Research UK","keywords":"Geomagnetic storm; Pitch angle; Geophysics; Ionosphere; Storm; Earth's magnetic field; Electron; Geology; Physics; Van Allen radiation belt; Geomagnetic secular variation; Atmospheric sciences; Computational physics; Magnetosphere; Meteorology; Nuclear physics; Magnetic field; Plasma","score_opus":0.011302437207458018,"score_gpt":0.293931399149786,"score_spread":0.282628961942328,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407346972","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976788,0.000039572325,0.001278414,0.000020021393,0.0000028213894,0.0000044973426,0.0004317354,0.000057775193,0.00048629488],"genre_scores_gemma":[0.99808025,0.000016988366,0.00090752635,0.0000035104586,0.0000029554792,0.0000033787576,0.0008694851,0.000007450204,0.000108516346],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99991417,0.000012494986,0.000005391459,0.000035725323,0.000015339341,0.000016865375],"domain_scores_gemma":[0.9993812,0.0002204169,0.00016286099,0.00007025222,0.00011041871,0.000054830016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00031666266,0.00013552001,0.00013537523,0.00088195904,0.00019696947,0.00042337755,0.00023203349,0.00016150344,0.00043645708],"category_scores_gemma":[0.001031715,0.00008729206,0.00013169041,0.0005490941,0.00013097908,0.00027226828,0.00022740517,0.00020122585,0.00016158154],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009719301,0.000031021675,0.9600254,0.00001670904,0.000047040947,0.00010471704,0.00022532567,0.007320907,0.0122623285,0.0002411543,0.00062781293,0.019000396],"study_design_scores_gemma":[0.0000066786747,0.000025622789,0.9581303,0.000005430102,0.0000123112895,0.000109673885,0.00016517092,0.037868626,0.0024785837,0.00015729306,0.0010321294,0.00000823251],"about_ca_topic_score_codex":0.007939849,"about_ca_topic_score_gemma":0.012089589,"teacher_disagreement_score":0.007939849,"about_ca_system_score_codex":0.00019853788,"about_ca_system_score_gemma":0.00014730528,"threshold_uncertainty_score":0.015787244},"labels":[],"label_agreement":null},{"id":"W4407351441","doi":"10.1029/2024gl111670","title":"Poloidal Field Line Resonances Driven by a Fast Wave","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Magnetic confinement fusion research","field":"Physics and Astronomy","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"Natural Environment Research Council; Science and Technology Facilities Council; Canadian Space Agency; National Natural Science Foundation of China; National Aeronautics and Space Administration","keywords":"Field (mathematics); Physics; Line (geometry); Geophysics; Field line; Quantum electrodynamics; Computational physics; Geology; Plasma; Nuclear physics; Mathematics","score_opus":0.01956960682611851,"score_gpt":0.32268131974934056,"score_spread":0.30311171292322203,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407351441","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.98309165,0.000037002384,0.0049786028,0.00018995216,0.00003323661,0.000020426434,0.00012336562,0.000125682,0.011400016],"genre_scores_gemma":[0.9984407,0.000012829616,0.0008046084,0.000027931981,0.000003039876,0.0000139388,0.00004404954,0.00001913004,0.00063378096],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999318,0.000012829503,0.0000018969865,0.000008010472,0.000013981547,0.000031501473],"domain_scores_gemma":[0.99971145,0.00012993088,0.00004124588,0.000023674833,0.000037539943,0.000056087167],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001612983,0.00023780164,0.00039077742,0.00019783228,0.00053110096,0.00073051243,0.00051204895,0.00075469544,0.0030084162],"category_scores_gemma":[0.00076369935,0.0001783218,0.0003173602,0.00024265677,0.00074518594,0.00041697678,0.0005042732,0.00052227435,0.00017400693],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00021318911,0.00010992491,0.0025717956,0.00004055722,0.000043001957,0.000303357,0.00019468059,0.98016375,0.007749112,0.006418685,0.0006563281,0.001535611],"study_design_scores_gemma":[0.00003308062,0.00002626075,0.0005392646,0.0000032838634,0.000004877442,0.000010030736,0.000053317846,0.9976641,0.0008286115,0.00063033437,0.00020119411,0.0000056862823],"about_ca_topic_score_codex":0.011899954,"about_ca_topic_score_gemma":0.004676144,"teacher_disagreement_score":0.011899954,"about_ca_system_score_codex":0.00064284814,"about_ca_system_score_gemma":0.00053732324,"threshold_uncertainty_score":0.023661375},"labels":[],"label_agreement":null},{"id":"W4407388877","doi":"10.1029/2024gl111669","title":"Disentangling Ecological Restoration's Impact on Terrestrial Water Storage","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":22,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Guelph","funders":"Guangdong Academy of Sciences; Chinese Academy of Sciences; National Natural Science Foundation of China; CERN","keywords":"Environmental science; Water storage; Restoration ecology; Terrestrial ecosystem; Ecology; Environmental resource management; Ecosystem; Oceanography; Geology; Biology","score_opus":0.05298468263910218,"score_gpt":0.32746425956848224,"score_spread":0.2744795769293801,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407388877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9986008,0.000051259038,0.00055043487,0.000070255766,0.0000024412493,0.000004671644,0.00014403524,0.000017296192,0.00055876997],"genre_scores_gemma":[0.9998394,0.000014274275,0.00007053652,0.0000037522068,7.793627e-7,0.0000010451965,0.000031300446,0.0000013648794,0.000037508453],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99981934,0.000053078682,0.000015006708,0.000030258148,0.000032980755,0.000049315502],"domain_scores_gemma":[0.9995603,0.00009562424,0.0001275972,0.000059388367,0.00008389651,0.000073115014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009562015,0.00029473673,0.00024017206,0.0008286798,0.0002473739,0.00064267725,0.00035991194,0.0002278351,0.0008641239],"category_scores_gemma":[0.0011225846,0.000112498754,0.0004951816,0.0007931787,0.0006732502,0.00072025164,0.00067901995,0.00019610689,0.00006825135],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025334745,0.00009794979,0.9040063,0.00007422973,0.00024521135,0.00038704075,0.00022616828,0.065797925,0.00926699,0.0016831567,0.00040121248,0.017560448],"study_design_scores_gemma":[0.0000071968234,0.00007311262,0.89900756,0.000010177994,0.000055094075,0.00005304108,0.0006091223,0.09702762,0.0015226505,0.0009591556,0.0006597133,0.000015526013],"about_ca_topic_score_codex":0.036323614,"about_ca_topic_score_gemma":0.046997752,"teacher_disagreement_score":0.036323614,"about_ca_system_score_codex":0.001239401,"about_ca_system_score_gemma":0.0008669189,"threshold_uncertainty_score":0.07222438},"labels":[],"label_agreement":null},{"id":"W4407409908","doi":"10.1029/2024gl112485","title":"Quantitative Estimates of Younger Dryas Freshening From Lipid δ <sup>2</sup> H Analysis in the Beaufort Sea","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"China Scholarship Council","keywords":"Younger Dryas; Beaufort sea; Geology; Oceanography; Climate change; Sea ice","score_opus":0.028461835947731117,"score_gpt":0.3169731857427346,"score_spread":0.2885113497950035,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407409908","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99848866,0.00014428452,0.0001161045,0.000012821426,0.0000017589634,0.0000033934994,0.0005778356,0.000008284405,0.000646841],"genre_scores_gemma":[0.9985323,0.00008658461,0.00030927843,0.000015983262,0.0000027532124,0.0000033956871,0.0006797404,0.0000033460276,0.0003666085],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999925,0.0000045003376,0.000004276152,0.000021059263,0.000026206602,0.000018913728],"domain_scores_gemma":[0.99976987,0.0000199686,0.000086614906,0.0000126323375,0.00007597233,0.000034940327],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014494639,0.0002384171,0.00012712665,0.0011552854,0.0005251792,0.0004436082,0.00020535651,0.00018014992,0.00076594093],"category_scores_gemma":[0.00027141118,0.00013170372,0.0002150794,0.0009363563,0.0003098241,0.00021725277,0.0003149393,0.00019271272,0.00013585381],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00036967863,0.0000117048585,0.7730537,0.000037416026,0.00009244557,0.00025175654,0.00054705504,0.0007509503,0.21365702,0.00008934005,0.00017452892,0.010964425],"study_design_scores_gemma":[8.6100226e-7,0.000008881247,0.99741447,8.4039016e-7,0.0000034357554,0.000018403036,0.00007982343,0.0000994872,0.002111035,0.000005144205,0.00025515814,0.0000023915543],"about_ca_topic_score_codex":0.2472458,"about_ca_topic_score_gemma":0.45549545,"teacher_disagreement_score":0.2472458,"about_ca_system_score_codex":0.0012376774,"about_ca_system_score_gemma":0.00038855415,"threshold_uncertainty_score":0.49161333},"labels":[],"label_agreement":null},{"id":"W4407429931","doi":"10.1029/2024gl113892","title":"The Widely Increasing Sensitivity of Vegetation Productivity to Phenology in Northern Middle and High Latitudes","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Remote Sensing in Agriculture","field":"Environmental Science","cited_by":11,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Natural Science Foundation of Hunan Province; National Natural Science Foundation of China","keywords":"Latitude; Phenology; Vegetation (pathology); High latitude; Climatology; Productivity; Environmental science; Physical geography; Geology; Atmospheric sciences; Geography; Ecology; Geodesy","score_opus":0.018219819159552085,"score_gpt":0.2720787713585588,"score_spread":0.2538589521990067,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407429931","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9981337,0.00032325927,0.000333292,0.00007787317,0.000005721244,0.0000015084968,0.00022460404,0.000014752434,0.00088521704],"genre_scores_gemma":[0.9996511,0.00005941557,0.00007191726,0.000017133745,0.0000049374744,9.967749e-7,0.000109804925,0.0000021491219,0.00008255245],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998016,0.00004812358,0.000011328127,0.00007326593,0.000029164552,0.000036494373],"domain_scores_gemma":[0.99916947,0.0002539292,0.00029258808,0.000077759156,0.00012206147,0.00008429044],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005065027,0.00012236334,0.00017915758,0.0004007975,0.00018772992,0.00061365875,0.00010177919,0.00013542273,0.0007940472],"category_scores_gemma":[0.0009215416,0.00009081954,0.00022023123,0.0004960839,0.00021993199,0.0002337486,0.0002774542,0.00019228854,0.00012353409],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000060198363,0.000007693195,0.98422396,0.000030371973,0.00009673841,0.000057822075,0.00026122757,0.0005582147,0.007946927,0.00009447259,0.00016878237,0.0064935824],"study_design_scores_gemma":[5.21261e-7,0.000005251492,0.99944264,0.0000017664058,0.000004557922,0.00001398048,0.000058508333,0.00016951759,0.00011133435,0.000022291857,0.00016862738,0.0000010599259],"about_ca_topic_score_codex":0.015188386,"about_ca_topic_score_gemma":0.020921724,"teacher_disagreement_score":0.015188386,"about_ca_system_score_codex":0.00020329106,"about_ca_system_score_gemma":0.00015599902,"threshold_uncertainty_score":0.030200005},"labels":[],"label_agreement":null},{"id":"W4407642486","doi":"10.1029/2024gl113786","title":"Climate Warming and Deglaciation Drive New Peat Formation in the Southern Alps, Aotearoa/New Zealand","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Environment Research Council; Leverhulme Trust","keywords":"Peat; Climate change; Global warming; Deglaciation; Boreal; Physical geography; Geology; Climatology; Environmental science; Earth science; Glacial period; Ecology; Oceanography; Geography; Geomorphology","score_opus":0.0170443977673589,"score_gpt":0.28443031925406514,"score_spread":0.26738592148670626,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407642486","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993248,0.000058787617,0.000022882172,0.000018836117,7.099564e-7,0.000002088904,0.00006474721,0.0000021429157,0.00050499005],"genre_scores_gemma":[0.9997274,0.00004942641,0.000042511263,0.0000037527382,8.242886e-7,0.0000018064435,0.00004460048,0.0000010683509,0.00012857199],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.000005004308,0.0000044165054,0.00001764745,0.000013249801,0.000022343726],"domain_scores_gemma":[0.99969065,0.000026660076,0.00014507839,0.000011295177,0.00005808077,0.00006836295],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020614771,0.00010826243,0.0001298285,0.000716173,0.0005036226,0.00065617834,0.00017807729,0.000155405,0.0013641833],"category_scores_gemma":[0.0004208036,0.00011587337,0.0001824555,0.0005313534,0.0005243754,0.00028781258,0.0003824027,0.00021358024,0.00012514261],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001314766,0.000035693687,0.9706643,0.00005144432,0.00004636955,0.00035760368,0.0017142205,0.000320967,0.018152121,0.00013600776,0.00015289079,0.008236914],"study_design_scores_gemma":[0.0000013869247,0.000005046947,0.99950695,0.00000275784,0.0000024803937,0.000016236636,0.00023155472,0.0000586053,0.000046337227,0.000009354179,0.00011839364,9.946675e-7],"about_ca_topic_score_codex":0.22525795,"about_ca_topic_score_gemma":0.41719848,"teacher_disagreement_score":0.22525795,"about_ca_system_score_codex":0.0009973159,"about_ca_system_score_gemma":0.0006563003,"threshold_uncertainty_score":0.44789356},"labels":[],"label_agreement":null},{"id":"W4407857523","doi":"10.1029/2024gl112584","title":"Record Early Sea Ice Loss in Southeastern Hudson Bay in Spring 2024","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geology and Paleoclimatology Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Manitoba","funders":"HORIZON EUROPE European Research Council; Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Bay; Spring (device); Oceanography; Geology; Sea ice; Environmental science; Climatology","score_opus":0.028864651735953255,"score_gpt":0.3010164685290847,"score_spread":0.27215181679313144,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4407857523","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99687564,0.00010316691,0.000041379415,0.000047240646,0.000013906789,0.0000063550046,0.001837751,0.000013137583,0.0010613725],"genre_scores_gemma":[0.99543285,0.000099506055,0.00012270799,0.000042423857,0.000008934917,0.000011576699,0.003082732,0.0000036087938,0.0011956966],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999113,0.0000055034093,0.000009695459,0.000016718033,0.000026142763,0.00003070445],"domain_scores_gemma":[0.9995552,0.000025299569,0.0001187259,0.000019938416,0.0001759231,0.00010497507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022916298,0.00024330032,0.00018811249,0.0011635543,0.0005709295,0.00063381187,0.00029010166,0.000240211,0.0012540078],"category_scores_gemma":[0.00045054423,0.0001348272,0.00014650307,0.0009885804,0.00021907745,0.00026461374,0.000546315,0.00019060732,0.00037824825],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006027725,0.000013434636,0.995408,0.000010984811,0.000012344949,0.00011860146,0.00021378437,0.00006016405,0.0007834706,0.0000124655735,0.00069290877,0.0026134597],"study_design_scores_gemma":[0.0000012323806,0.00000765665,0.99896383,0.0000036684667,0.000003478817,0.000022735741,0.0002833309,0.000083170155,0.00014318462,0.0000034319846,0.00048299262,0.0000012403963],"about_ca_topic_score_codex":0.40312612,"about_ca_topic_score_gemma":0.60311586,"teacher_disagreement_score":0.5968739,"about_ca_system_score_codex":0.0015449933,"about_ca_system_score_gemma":0.0014164338,"threshold_uncertainty_score":0.8015593},"labels":[],"label_agreement":null},{"id":"W4408308308","doi":"10.1029/2024gl113522","title":"Natural Soils‐Based Oxidation Mitigates Methane Leakage From Integrity Compromised Legacy Wells","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"BC Oil and Gas Research and Innovation Society","keywords":"Methane; Soil water; Leakage (economics); Natural (archaeology); Environmental science; Geology; Anaerobic oxidation of methane; Natural gas; Soil science; Waste management; Chemistry; Engineering","score_opus":0.024404684965892605,"score_gpt":0.3067849479174164,"score_spread":0.2823802629515238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408308308","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99822634,0.00022989251,0.00053536217,0.000048718557,0.000005262578,0.000011909396,0.00007717336,0.00003305595,0.0008323912],"genre_scores_gemma":[0.9987888,0.00015909687,0.00044084003,0.000023723036,0.0000014036272,0.0000040312298,0.00005470118,0.0000030749159,0.0005243154],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9999224,0.000007240725,0.0000020392827,0.000013562942,0.000018845567,0.000035956233],"domain_scores_gemma":[0.99992573,0.0000054613006,0.000019486792,0.000005032645,0.00002104137,0.000023251083],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000081072874,0.00017939074,0.0001420273,0.00016620591,0.00031053854,0.0005179881,0.00021916103,0.0001590867,0.00080400624],"category_scores_gemma":[0.00013842451,0.000058301328,0.00010914225,0.00013381575,0.00024714592,0.00021117662,0.00034042288,0.00021244836,0.000095756266],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00071744435,0.00028679293,0.0225621,0.00023321838,0.000049230686,0.00015243096,0.00016088055,0.002872776,0.9409729,0.00025870494,0.00067666156,0.031056782],"study_design_scores_gemma":[0.000055440752,0.0025254006,0.25431955,0.000074985874,0.00011982868,0.0001520563,0.0019494435,0.010971415,0.7145384,0.0005005152,0.014753591,0.000039311428],"about_ca_topic_score_codex":0.036303315,"about_ca_topic_score_gemma":0.1220469,"teacher_disagreement_score":0.036303315,"about_ca_system_score_codex":0.00076470175,"about_ca_system_score_gemma":0.0010006698,"threshold_uncertainty_score":0.072184026},"labels":[],"label_agreement":null},{"id":"W4408320323","doi":"10.1029/2024gl114492","title":"Increased Atmospheric Aridity and Reduced Precipitation Drive the 2023 Extreme Wildfire Season in Canada","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":12,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Environmental science; Precipitation; Atmospheric sciences; Arid; Climatology; Meteorology; Geology; Geography","score_opus":0.014056359206982654,"score_gpt":0.2516607586643532,"score_spread":0.23760439945737058,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408320323","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9950237,0.00021393817,0.00025483366,0.00040380086,0.0000074404193,0.00000519929,0.0018499636,0.000024025092,0.0022170176],"genre_scores_gemma":[0.9987915,0.000120363766,0.00018249347,0.00007257047,0.0000025624443,0.0000015056537,0.00045584425,0.000003854855,0.00036931393],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998858,0.0000049902774,0.000003113528,0.000019053146,0.000033938868,0.00005303191],"domain_scores_gemma":[0.9996289,0.000024316518,0.000060092545,0.000012617314,0.00017440636,0.00009957932],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019975255,0.00016071567,0.00013136194,0.0004219311,0.0016194191,0.00084354175,0.00032142582,0.00023244026,0.0014109213],"category_scores_gemma":[0.00048590722,0.0001010801,0.00022634199,0.00091956294,0.00039357576,0.00018558835,0.00036189542,0.00051225204,0.00009621007],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007461229,0.000035751396,0.97050977,0.00002741738,0.00007503652,0.00013482585,0.00044464262,0.0027977384,0.0020561693,0.0003714182,0.0032071245,0.020265525],"study_design_scores_gemma":[0.0000025312004,0.00000452785,0.99376935,0.0000125441675,0.000012539694,0.0000257897,0.0009209529,0.0029463705,0.00027302068,0.00011300901,0.0019106925,0.000008565441],"about_ca_topic_score_codex":0.988226,"about_ca_topic_score_gemma":0.9957748,"teacher_disagreement_score":0.0117740035,"about_ca_system_score_codex":0.008318827,"about_ca_system_score_gemma":0.009721128,"threshold_uncertainty_score":0.06035757},"labels":[],"label_agreement":null},{"id":"W4408342802","doi":"10.1029/2025gl114621","title":"Conditions for the Kelvin‐Helmholtz Instability in the Polar Ionosphere","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Nuclear Safety and Security Commission; National Aeronautics and Space Administration","keywords":"Ionosphere; Polar; Instability; Geophysics; Physics; Geology; Geodesy; Astronomy; Mechanics","score_opus":0.019525033491945076,"score_gpt":0.3256021742408229,"score_spread":0.3060771407488778,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408342802","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9907526,0.00009188101,0.0044209347,0.00014083364,0.00001799649,0.000030168789,0.0001328522,0.000080151134,0.0043327473],"genre_scores_gemma":[0.9992607,0.000020295787,0.00040040622,0.000012402969,0.0000031167315,0.000013123531,0.000042316035,0.000009943831,0.00023768756],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99991524,0.000015204738,0.000004251392,0.000009864912,0.000015478343,0.0000399407],"domain_scores_gemma":[0.9996437,0.00014974775,0.00007813369,0.000018010793,0.000055910663,0.00005444253],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022849534,0.00024247872,0.00021223677,0.0004301887,0.00068901177,0.0007747267,0.00021830949,0.00041605977,0.0020376823],"category_scores_gemma":[0.0017229962,0.00019031839,0.0003495767,0.00016441278,0.00063748733,0.00044274595,0.00036841625,0.00038813511,0.00019315827],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00038666808,0.00015952038,0.031238541,0.0000754719,0.000052821808,0.00060372835,0.00028840924,0.90489984,0.043089136,0.013918419,0.0012296487,0.004057775],"study_design_scores_gemma":[0.00010002589,0.00011225362,0.012849166,0.000016876296,0.000011745238,0.00006695201,0.00021515654,0.976695,0.006625232,0.0028618749,0.0004191722,0.000026578133],"about_ca_topic_score_codex":0.010883992,"about_ca_topic_score_gemma":0.0032927776,"teacher_disagreement_score":0.010883992,"about_ca_system_score_codex":0.0007913954,"about_ca_system_score_gemma":0.00082943076,"threshold_uncertainty_score":0.021641254},"labels":[],"label_agreement":null},{"id":"W4408485392","doi":"10.1029/2025gl114954","title":"Quantifying the Effects of Solar Wind Fluctuations on the Solar Wind‐Magnetosphere Interaction","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Lakehead University","funders":"","keywords":"Solar wind; Magnetosphere; Atmospheric sciences; Environmental science; Magnetopause; Polar wind; Solar physics; Physics; Meteorology; Geophysics; Astrobiology; Astronomy; Plasma","score_opus":0.020172514750281118,"score_gpt":0.3094355886412519,"score_spread":0.28926307389097083,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408485392","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99638546,0.000056021287,0.0015139856,0.000113260045,0.0000134119655,0.00000527492,0.00017592471,0.00007560801,0.0016611055],"genre_scores_gemma":[0.999546,0.00001435715,0.00024466502,0.000012494685,0.0000034680345,0.0000026010844,0.000080560625,0.000012346469,0.00008357238],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99993956,0.000020443116,0.0000026578293,0.000012685214,0.000006383766,0.000018225675],"domain_scores_gemma":[0.99975294,0.00013684378,0.000024745448,0.00002412662,0.000018285886,0.00004302865],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023863635,0.0003677725,0.00039641227,0.00018613735,0.0003081861,0.0005741204,0.00035023352,0.00046387175,0.0013173618],"category_scores_gemma":[0.00068873604,0.00023227386,0.00052471884,0.0002414438,0.00032503027,0.0004956373,0.00045703157,0.00049922586,0.000118931224],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030237387,0.00012137888,0.045852195,0.000041982275,0.0002713154,0.0002219342,0.00008122395,0.93881327,0.0082122395,0.0015084324,0.0007531322,0.0038205287],"study_design_scores_gemma":[0.00010492479,0.000106524276,0.026903419,0.000003900958,0.000050486553,0.000023381182,0.000051354815,0.9703774,0.001372425,0.000624935,0.00036241833,0.000018893641],"about_ca_topic_score_codex":0.012031364,"about_ca_topic_score_gemma":0.007247824,"teacher_disagreement_score":0.012031364,"about_ca_system_score_codex":0.00046075895,"about_ca_system_score_gemma":0.0002796089,"threshold_uncertainty_score":0.023922682},"labels":[],"label_agreement":null},{"id":"W4408934213","doi":"10.1029/2024gl110244","title":"Deformation Controlled Fluid Mass‐Transfer Processes in Ancient Orogens","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Simon Fraser University","funders":"Canada First Research Excellence Fund","keywords":"Geology; Deformation (meteorology); Geophysics; Mass transfer; Earth science; Mechanics; Physics; Oceanography","score_opus":0.01982422131091373,"score_gpt":0.25953234769709943,"score_spread":0.23970812638618572,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408934213","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99849296,0.00005442458,0.0003684227,0.000025762642,8.4511123e-7,0.0000041228323,0.00003778941,0.000012157091,0.001003594],"genre_scores_gemma":[0.99953747,0.000052328745,0.00016300626,0.00000409066,0.0000010598869,0.0000017829402,0.000023713415,0.000002888318,0.00021360442],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988973,0.000009073842,0.0000071849995,0.00003620331,0.000026215324,0.000031609237],"domain_scores_gemma":[0.9999063,0.000014194051,0.000034519104,0.000012463385,0.000022846021,0.000009544425],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000146298,0.0002382526,0.00030200472,0.0010122041,0.0006657356,0.0007975305,0.00041259907,0.00028031654,0.0012730731],"category_scores_gemma":[0.0005612719,0.0001862746,0.00012174616,0.0011660208,0.0019766404,0.0004448858,0.0007805296,0.000250934,0.00013607487],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000638827,0.00009079756,0.5321917,0.00038194444,0.00010941931,0.002132793,0.006899486,0.020676801,0.3876687,0.011615985,0.00018018977,0.03741343],"study_design_scores_gemma":[0.000028634311,0.00008575105,0.9484169,0.000029612314,0.000056662313,0.00058459776,0.004093563,0.015641334,0.025159733,0.002181215,0.0036836814,0.000038220154],"about_ca_topic_score_codex":0.052426875,"about_ca_topic_score_gemma":0.050564267,"teacher_disagreement_score":0.052426875,"about_ca_system_score_codex":0.001680569,"about_ca_system_score_gemma":0.0008782458,"threshold_uncertainty_score":0.10424346},"labels":[],"label_agreement":null},{"id":"W4408998812","doi":"10.1029/2024gl113022","title":"Rapid Changes in Retrogressive Thaw Slump Dynamics in the Russian High Arctic Based on Very High‐Resolution Remote Sensing","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":16,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"","keywords":"Slump; Arctic; Remote sensing; Geology; High resolution; Environmental science; The arctic; Earth science; Oceanography; Geography","score_opus":0.036855691415785576,"score_gpt":0.2879989776823449,"score_spread":0.2511432862665593,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4408998812","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99911517,0.000054632914,0.00019956123,0.000008662842,0.000002444208,0.0000022371312,0.0002738621,0.000008514356,0.000334845],"genre_scores_gemma":[0.9994042,0.00003096053,0.00020193984,0.0000024750987,0.0000015529964,0.0000015441282,0.00028907985,0.0000013555156,0.00006694176],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998684,0.00002314162,0.000012087328,0.000031033782,0.000032046275,0.000033302804],"domain_scores_gemma":[0.9997303,0.000037568978,0.00008037808,0.00002633394,0.00009315559,0.00003223414],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043095805,0.00016771286,0.00016069192,0.00091030326,0.00029418367,0.00044457146,0.00015410998,0.00014870003,0.00031060015],"category_scores_gemma":[0.00039704482,0.000103621554,0.0003075008,0.00065753143,0.00019464028,0.00023277491,0.00034373,0.00012310663,0.00007465861],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011044464,0.000018564677,0.9827368,0.00003352191,0.00010326234,0.00010801158,0.0003092358,0.0023763299,0.006381146,0.00006641074,0.00015660492,0.007599652],"study_design_scores_gemma":[0.0000013176683,0.000012242265,0.9970055,0.0000052312575,0.00001626927,0.000029541263,0.00023411233,0.0020595826,0.0004237301,0.00001041708,0.00019854725,0.0000034398895],"about_ca_topic_score_codex":0.05004086,"about_ca_topic_score_gemma":0.07699859,"teacher_disagreement_score":0.05004086,"about_ca_system_score_codex":0.00032721786,"about_ca_system_score_gemma":0.00037914267,"threshold_uncertainty_score":0.099499226},"labels":[],"label_agreement":null},{"id":"W4409149874","doi":"10.1029/2024gl114444","title":"Crustal Magnetization Source Depths North of the Caloris Basin, Mercury","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Sciences and Engineering Research Council of Canada; National Aeronautics and Space Administration","keywords":"Geology; Mercury (programming language); Magnetization; Structural basin; Geophysics; Seismology; Earth science; Paleontology; Magnetic field; Physics","score_opus":0.017745960025177653,"score_gpt":0.27364098893419975,"score_spread":0.2558950289090221,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409149874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9948369,0.000099698416,0.00016203173,0.000033851877,0.0000014286259,0.0000032515454,0.0011151269,0.00008032926,0.00366738],"genre_scores_gemma":[0.9986105,0.00004446512,0.00018889848,0.0000056751664,0.0000020799473,0.000002216714,0.0006728208,0.000012984678,0.00046032443],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99996364,0.0000013372173,0.0000013101456,0.00001333413,0.000010455663,0.000009865586],"domain_scores_gemma":[0.99989367,0.000019440857,0.000024547413,0.000011220409,0.000028052293,0.000023052246],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006623904,0.00023041423,0.00018152122,0.0014577105,0.00033664648,0.00035930992,0.00019210126,0.00021582117,0.0031627975],"category_scores_gemma":[0.00030795732,0.00017058058,0.00013844168,0.0008083986,0.00016019549,0.00022742728,0.00058839255,0.00016062576,0.00042756723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00030341698,0.000031844516,0.85022044,0.0001367995,0.00017075428,0.00043319174,0.0013415248,0.0038795876,0.10537944,0.00063185144,0.0011071723,0.036363974],"study_design_scores_gemma":[0.0000047938784,0.000009139191,0.99512357,0.0000057184243,0.000012834566,0.00006178249,0.00011461055,0.00079081766,0.0030217508,0.000084589476,0.00076551485,0.0000048806037],"about_ca_topic_score_codex":0.024470894,"about_ca_topic_score_gemma":0.03608778,"teacher_disagreement_score":0.024470894,"about_ca_system_score_codex":0.00044194201,"about_ca_system_score_gemma":0.00024629553,"threshold_uncertainty_score":0.04865694},"labels":[],"label_agreement":null},{"id":"W4409167971","doi":"10.1029/2025gl115257","title":"The Sudden Stratospheric Warming Events in the Antarctic in 2024","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":9,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada; Dalhousie University","funders":"China Scholarship Council; Dalhousie University; National Natural Science Foundation of China","keywords":"Sudden stratospheric warming; Environmental science; Climatology; Atmospheric sciences; Astrobiology; Stratosphere; Geology; Meteorology; Polar vortex; Physics","score_opus":0.0236819372831787,"score_gpt":0.3022197159531949,"score_spread":0.2785377786700162,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409167971","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99476033,0.00024171761,0.00008508115,0.00031013988,0.00008146607,0.000009536941,0.0016512488,0.000012565325,0.00284793],"genre_scores_gemma":[0.997042,0.00010642585,0.00008686904,0.000101902086,0.000043626165,0.00001062159,0.0018976033,0.0000021922403,0.00070876884],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999374,0.000008970164,0.0000042872916,0.000007195697,0.000014595952,0.00002754641],"domain_scores_gemma":[0.9998678,0.000011224228,0.000041697065,0.000007612263,0.000038266437,0.000033341174],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001674741,0.00020828308,0.0000984914,0.00047361094,0.0003762792,0.00044128892,0.00013350362,0.00031829436,0.0011017255],"category_scores_gemma":[0.00030029868,0.000059482565,0.00014750025,0.00044956928,0.00014675362,0.00018367369,0.00034488164,0.00022340636,0.00022730025],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052479294,0.000058833266,0.9683349,0.0000649666,0.000083464685,0.001090999,0.00044874818,0.00075843564,0.008064909,0.0003957278,0.0050050286,0.015169198],"study_design_scores_gemma":[0.0000050516173,0.00004867147,0.9938105,0.0000084914545,0.00001526734,0.00014142792,0.00043772339,0.00041497435,0.00079251034,0.000083303414,0.004237197,0.0000047921117],"about_ca_topic_score_codex":0.019188106,"about_ca_topic_score_gemma":0.042495508,"teacher_disagreement_score":0.019188106,"about_ca_system_score_codex":0.0005627206,"about_ca_system_score_gemma":0.0005198977,"threshold_uncertainty_score":0.038152814},"labels":[],"label_agreement":null},{"id":"W4409329775","doi":"10.1029/2024gl113789","title":"Mixing Accounts for More Than Half of Biogeochemical Changes Along Mode Water Ventilation Pathways","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Natural Environment Research Council; Natural Sciences and Engineering Research Council of Canada; Nuclear Safety and Security Commission; Earth Sciences Division; Sight Research UK; National Aeronautics and Space Administration; National Science Foundation","keywords":"Biogeochemical cycle; Mixing (physics); Environmental science; Atmospheric sciences; Vertical mixing; Geology; Physics; Chemistry; Environmental chemistry","score_opus":0.02139838957761887,"score_gpt":0.28691790599780853,"score_spread":0.26551951642018967,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409329775","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9891067,0.00088856614,0.006720628,0.00016582072,0.00002616828,0.000022758803,0.00062587095,0.0002904095,0.002153082],"genre_scores_gemma":[0.99803334,0.00022791456,0.00076797843,0.000028171926,0.000012430575,0.000009582584,0.00041982054,0.000050878378,0.00044979583],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998301,0.000015082137,0.000015836453,0.00006971595,0.000029559144,0.000039666505],"domain_scores_gemma":[0.99969244,0.000104875005,0.000084071165,0.00004584469,0.000040783783,0.000032078486],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00036189577,0.0007132446,0.00048216325,0.00088357524,0.0003842765,0.000700844,0.00032772706,0.00039951407,0.002321269],"category_scores_gemma":[0.001380621,0.0003714221,0.001001659,0.00065924256,0.0002633262,0.00077843235,0.00062976487,0.00027369245,0.00038916807],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026336592,0.000045640038,0.7343412,0.00018753129,0.00046590008,0.00026929844,0.00020322578,0.011030696,0.20167057,0.0010570594,0.0005892063,0.04987628],"study_design_scores_gemma":[0.000019499532,0.000045438926,0.9212567,0.000021668326,0.00015002221,0.00015152637,0.00011079639,0.06108172,0.013168073,0.0014078042,0.0025492832,0.000037435937],"about_ca_topic_score_codex":0.015199037,"about_ca_topic_score_gemma":0.0099886,"teacher_disagreement_score":0.015199037,"about_ca_system_score_codex":0.0005190814,"about_ca_system_score_gemma":0.00049805234,"threshold_uncertainty_score":0.030221105},"labels":[],"label_agreement":null},{"id":"W4409440993","doi":"10.1029/2024gl112229","title":"Channel Steepness Biases and Nonsteady Erosion in Landscapes Evolving Under Cyclical Climate","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Soil erosion and sediment transport","field":"Agricultural and Biological Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Erosion; Environmental science; Channel (broadcasting); Climatology; Climate change; Hydrology (agriculture); Geology; Oceanography; Geomorphology; Geotechnical engineering; Computer science","score_opus":0.05193026954060288,"score_gpt":0.312412634521989,"score_spread":0.2604823649813861,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409440993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996207,0.0000063979273,0.0002189335,0.0000044816156,3.3911007e-7,5.8533266e-7,0.000025422383,0.0000033285237,0.00011971514],"genre_scores_gemma":[0.9999012,0.0000027248332,0.000050602874,0.0000015648892,3.1860063e-7,3.80815e-7,0.000025584515,0.0000014628064,0.000016244976],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998312,0.0000660582,0.000011674452,0.000044777556,0.000017979812,0.000028257578],"domain_scores_gemma":[0.998596,0.0008887872,0.00021198114,0.00017405575,0.00007538501,0.000053742635],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008807733,0.000083220286,0.00015068734,0.0005937639,0.00021038418,0.00069457944,0.00013988848,0.00019302774,0.00072452263],"category_scores_gemma":[0.0032816727,0.000104521656,0.00016897323,0.00048341113,0.00045831964,0.00040850864,0.00029463193,0.0001412289,0.00006295382],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017106422,0.00003037775,0.96728957,0.000013588892,0.00008204942,0.000087518754,0.00029317584,0.01679801,0.007898314,0.0005360456,0.00009025316,0.0067100017],"study_design_scores_gemma":[0.0000026125265,0.000013035429,0.9756596,0.0000025719887,0.000009083654,0.00005336779,0.00011565443,0.023058195,0.0005696844,0.00043247765,0.000077196244,0.0000064794917],"about_ca_topic_score_codex":0.0063477517,"about_ca_topic_score_gemma":0.010703186,"teacher_disagreement_score":0.0063477517,"about_ca_system_score_codex":0.0003734606,"about_ca_system_score_gemma":0.00013611185,"threshold_uncertainty_score":0.012621582},"labels":[],"label_agreement":null},{"id":"W4409480440","doi":"10.1029/2025gl115547","title":"Spatial Distribution of Ion Cyclotron Waves at Io","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"National Key Research and Development Program of China; Chinese Academy of Sciences; Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; Tencent","keywords":"Cyclotron; Ion; Spatial distribution; Geology; Physics; Geophysics; Atmospheric sciences; Remote sensing","score_opus":0.010026815070783252,"score_gpt":0.2826367391405272,"score_spread":0.272609924069744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409480440","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99819165,0.00004465393,0.00020290274,0.000013254082,0.0000023533426,0.0000028528314,0.00031639432,0.000011432338,0.001214504],"genre_scores_gemma":[0.9987526,0.00003429242,0.0001448306,0.0000068701893,0.0000048728507,0.000003371863,0.00076209893,0.0000045627135,0.0002865962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999366,0.0000035897756,0.000003150831,0.000018993807,0.00001672316,0.000021087702],"domain_scores_gemma":[0.9996056,0.000060065362,0.00012455782,0.00002363779,0.000097110045,0.00008906331],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000098526056,0.0001668447,0.0001856186,0.0010725571,0.00021217365,0.00034755317,0.00017113514,0.00018159929,0.0008042391],"category_scores_gemma":[0.00043307053,0.00007443596,0.00012182047,0.0006052788,0.00021073272,0.00025147243,0.0004298511,0.00020597283,0.00014187447],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00026834712,0.000032771437,0.9141859,0.000038446153,0.00007512661,0.00028930887,0.00048061842,0.0014916259,0.0669886,0.00020998948,0.0006276707,0.015311555],"study_design_scores_gemma":[0.0000022608024,0.000019326617,0.9977514,0.0000038746757,0.000007912128,0.00007124217,0.00015230787,0.00080365886,0.0008103016,0.000026073807,0.00034741277,0.0000041290727],"about_ca_topic_score_codex":0.0074965474,"about_ca_topic_score_gemma":0.012192852,"teacher_disagreement_score":0.0074965474,"about_ca_system_score_codex":0.00025042446,"about_ca_system_score_gemma":0.00010391276,"threshold_uncertainty_score":0.01490581},"labels":[],"label_agreement":null},{"id":"W4409645333","doi":"10.1029/2024gl113139","title":"Controls of Slab Subduction and Tearing on the Magmatism of Wrangell Volcanoes in South‐Central Alaska","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Massachusetts Green High Performance Computing Center; National Science Foundation","keywords":"Geology; Subduction; Magmatism; Tearing; Seismology; Slab; Volcano; Geochemistry; Geophysics; Tectonics","score_opus":0.019224820573638765,"score_gpt":0.246551736444518,"score_spread":0.22732691587087922,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409645333","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99946827,0.000016916249,0.00014872389,0.000012728519,0.0000011435638,9.644119e-7,0.00007407595,0.000008417596,0.00026866078],"genre_scores_gemma":[0.9997732,0.000010882244,0.00006412713,0.0000011559088,4.938193e-7,6.46915e-7,0.00006753772,0.0000014714951,0.00008039334],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999143,0.000017174661,0.0000066469443,0.000029319779,0.000013187686,0.00001929164],"domain_scores_gemma":[0.9998654,0.000024243582,0.000032630058,0.000014912666,0.000033550237,0.000029268758],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018653214,0.00020195587,0.00020757453,0.00029242897,0.00036359284,0.00063943694,0.00022729396,0.00018970494,0.00060566945],"category_scores_gemma":[0.00047433923,0.00016764682,0.00028211664,0.00021120258,0.000278049,0.00028439346,0.00037986157,0.00017039297,0.00009314477],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017788829,0.000043600172,0.9213151,0.000020796046,0.0001109306,0.00029575202,0.00055272516,0.054575503,0.017455734,0.00036897397,0.00015429003,0.0049286224],"study_design_scores_gemma":[0.000012437707,0.000029726987,0.94645333,0.0000070797996,0.000028320008,0.000047078076,0.00076750014,0.05079433,0.0012155662,0.00020266256,0.00042519314,0.00001669369],"about_ca_topic_score_codex":0.19834141,"about_ca_topic_score_gemma":0.20965885,"teacher_disagreement_score":0.19834141,"about_ca_system_score_codex":0.0010392042,"about_ca_system_score_gemma":0.00073260354,"threshold_uncertainty_score":0.3943739},"labels":[],"label_agreement":null},{"id":"W4409770967","doi":"10.1029/2025gl115446","title":"Downdip Variations in Megathrust Seismogenic Behavior in the Japan Trench Subduction Zone Affected by Mantle Wedge Serpentinite","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada; Natural Resources Canada","funders":"","keywords":"Subduction; Geology; Trench; Mantle wedge; Wedge (geometry); Seismology; Mantle (geology); Geochemistry; Tectonics; Materials science; Layer (electronics)","score_opus":0.026082513553771242,"score_gpt":0.2926193668716989,"score_spread":0.2665368533179277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409770967","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997403,0.000025899117,0.00002965039,0.000005104091,5.3989515e-7,8.713071e-7,0.000043070027,0.0000030444019,0.000151452],"genre_scores_gemma":[0.9998691,0.000012878738,0.000015976555,0.0000018602374,6.285014e-7,5.660449e-7,0.000046875026,7.837985e-7,0.000051335162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999211,0.0000063770703,0.00000812239,0.000025098136,0.000011269501,0.000027956943],"domain_scores_gemma":[0.99978155,0.000015334263,0.00008198073,0.000018332683,0.00004500458,0.00005773282],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010986965,0.00022342999,0.00020772974,0.0011236083,0.00027001795,0.0004244021,0.00020692933,0.00019194308,0.0008334138],"category_scores_gemma":[0.00033141224,0.00015807706,0.00014731666,0.00060621236,0.000355116,0.00025295274,0.00049828173,0.00013205457,0.00013467597],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00013473186,0.000013830134,0.980316,0.000017983633,0.000040099007,0.00043289296,0.0007732693,0.0006163844,0.01447483,0.000050412065,0.000050921397,0.003078651],"study_design_scores_gemma":[0.0000012915427,0.000007990428,0.9992872,0.0000014211687,0.0000045328793,0.00003636823,0.00021838697,0.00020947162,0.00017902437,0.000007926069,0.00004486006,0.00000149792],"about_ca_topic_score_codex":0.01586548,"about_ca_topic_score_gemma":0.022255182,"teacher_disagreement_score":0.01586548,"about_ca_system_score_codex":0.0003445052,"about_ca_system_score_gemma":0.00014823567,"threshold_uncertainty_score":0.031546235},"labels":[],"label_agreement":null},{"id":"W4409904659","doi":"10.1029/2025gl114775","title":"On Risk of Rain on Snow Over High‐Latitude Coastal Areas in North America","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Division of Information and Intelligent Systems; Legislative-Citizen Commission on Minnesota Resources; National Science Foundation","keywords":"Snow; Climatology; Latitude; Environmental science; High latitude; Physical geography; Geology; Oceanography; Meteorology; Geography","score_opus":0.024221809003121045,"score_gpt":0.28711327517135904,"score_spread":0.262891466168238,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409904659","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99846613,0.00006140415,0.000033959754,0.00017797881,0.0000026715568,0.0000028855964,0.00045133673,0.0000043892082,0.0007994228],"genre_scores_gemma":[0.99954456,0.00006198433,0.000026729645,0.000019981775,0.0000030429787,0.000002191884,0.00021661064,8.783165e-7,0.0001238834],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99987495,0.000030987263,0.000009508764,0.00002759983,0.000021824102,0.000035120633],"domain_scores_gemma":[0.9992231,0.00014132564,0.00030334078,0.000031281215,0.00012493516,0.00017589702],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024181818,0.00012781925,0.0001282045,0.00036988975,0.00035392292,0.00063563243,0.00022576521,0.0003105948,0.0021395057],"category_scores_gemma":[0.001042382,0.00011025293,0.00018472661,0.000499526,0.00020554417,0.00038855438,0.0005522236,0.00023108016,0.00013892156],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000031037856,0.000015721542,0.9965191,0.0000067351,0.000028718607,0.00007526317,0.00007571838,0.0013999542,0.000104883125,0.000070442606,0.00036867528,0.0013038602],"study_design_scores_gemma":[0.000003913343,0.000014726861,0.9959351,0.000009506127,0.000010577328,0.000039611245,0.0006251316,0.002900313,0.00003812789,0.000116197414,0.00030381756,0.0000030345705],"about_ca_topic_score_codex":0.09502484,"about_ca_topic_score_gemma":0.19515947,"teacher_disagreement_score":0.9049752,"about_ca_system_score_codex":0.0007274609,"about_ca_system_score_gemma":0.0005368789,"threshold_uncertainty_score":0.18894345},"labels":[],"label_agreement":null},{"id":"W4409968534","doi":"10.1029/2025gl116574","title":"Frequent Millennial‐Scale Oceanic Redox Oscillations Recorded by Negative Pyrite Δ<sup>33</sup>S: Implications for Phanerozoic Extinctions","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Methane Hydrates and Related Phenomena","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"National Natural Science Foundation of China; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Phanerozoic; Pyrite; Geology; Redox; Extinction event; Paleontology; Scale (ratio); Earth science; Oceanography; Cenozoic; Mineralogy; Physics; Chemistry; Structural basin","score_opus":0.022465181653806184,"score_gpt":0.3090290255328283,"score_spread":0.2865638438790221,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4409968534","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9992236,0.0000757766,0.00018723006,0.000038446786,0.0000027852884,0.000001294299,0.000069593574,0.000006925244,0.00039438426],"genre_scores_gemma":[0.9998541,0.000025286727,0.000044042034,0.000008609614,0.000002191925,8.8480994e-7,0.000029761222,0.0000011390911,0.000034047687],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995124,0.0000077765635,0.0000037312861,0.00001651239,0.000008293336,0.00001238274],"domain_scores_gemma":[0.9997981,0.00003288922,0.00008412689,0.000014897051,0.000037663438,0.000032278902],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002931173,0.00017034814,0.00013236092,0.00032128947,0.0003282073,0.00039680133,0.00019293076,0.00018902747,0.0007299898],"category_scores_gemma":[0.00047218712,0.0000901615,0.00009107408,0.00024962943,0.0005065944,0.0002711546,0.0004299093,0.00025300097,0.000067642024],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018328242,0.00001603252,0.901922,0.000039854265,0.000049143517,0.00017478825,0.00051951315,0.00037882716,0.08859186,0.00031091948,0.00011009542,0.0077036507],"study_design_scores_gemma":[0.0000014849712,0.000015952433,0.99716717,0.0000025536433,0.000006157906,0.000043928372,0.00016656364,0.0002432211,0.0019932988,0.00007430647,0.00028286697,0.0000024478459],"about_ca_topic_score_codex":0.0045744246,"about_ca_topic_score_gemma":0.005540128,"teacher_disagreement_score":0.0045744246,"about_ca_system_score_codex":0.00029538994,"about_ca_system_score_gemma":0.00018394954,"threshold_uncertainty_score":0.009095609},"labels":[],"label_agreement":null},{"id":"W4410057878","doi":"10.1029/2024gl114185","title":"A First Look at River Discharge Estimation From SWOT Satellite Observations","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Flood Risk Assessment and Management","field":"Environmental Science","cited_by":42,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Jet Propulsion Laboratory; California Institute of Technology","keywords":"SWOT analysis; Satellite; Estimation; Environmental science; Meteorology; Discharge; Remote sensing; Geology; Geography; Cartography; Business; Engineering; Aerospace engineering; Drainage basin","score_opus":0.032336793441029174,"score_gpt":0.30827324159439357,"score_spread":0.2759364481533644,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410057878","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.97682095,0.0007910822,0.008457308,0.00052123074,0.00005862778,0.000039423714,0.0060350304,0.00018567391,0.007090705],"genre_scores_gemma":[0.9833363,0.000343498,0.0065926183,0.000116019444,0.000038115228,0.000011998408,0.008046736,0.000044351396,0.0014703071],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99947757,0.00011069822,0.000045626064,0.000092014896,0.00022588985,0.000048195965],"domain_scores_gemma":[0.9975763,0.0006714129,0.00030790074,0.0001833319,0.001164025,0.000097120705],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0011469158,0.00034100102,0.0002609678,0.00098208,0.00023635026,0.0009575671,0.00021286178,0.00032836507,0.0019819236],"category_scores_gemma":[0.004138181,0.00013271756,0.00028990424,0.0012639241,0.00018886822,0.0012396844,0.0006476303,0.0003696324,0.000589837],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031242814,0.000097822194,0.8891877,0.00022170038,0.0002249461,0.00035726224,0.0003382623,0.011747264,0.01082409,0.0005463181,0.0048927288,0.08124951],"study_design_scores_gemma":[0.00001153379,0.0001873572,0.96623224,0.00006152825,0.00005164632,0.00018017073,0.0005323247,0.019062107,0.0059525534,0.00039332945,0.0073032295,0.00003195528],"about_ca_topic_score_codex":0.012730538,"about_ca_topic_score_gemma":0.023039933,"teacher_disagreement_score":0.012730538,"about_ca_system_score_codex":0.00041122158,"about_ca_system_score_gemma":0.00036244924,"threshold_uncertainty_score":0.0253129},"labels":[],"label_agreement":null},{"id":"W4410135874","doi":"10.1029/2024gl112717","title":"Climate‐Dependency of Impact of Increased Carbon Dioxide on African Monsoon Rainfall: Insights From Model Simulations","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Université du Québec à Montréal","funders":"Deutsches Klimarechenzentrum","keywords":"Monsoon; Climatology; Environmental science; Dependency (UML); Climate model; Carbon dioxide; Climate change; Carbon dioxide in Earth's atmosphere; Atmospheric sciences; Geology; Oceanography; Ecology","score_opus":0.03346859266364448,"score_gpt":0.3288719601082313,"score_spread":0.2954033674445868,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410135874","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964133,0.00010558047,0.0004180004,0.00019054537,0.000010331608,0.000011848501,0.0005525183,0.000037807527,0.002260109],"genre_scores_gemma":[0.999318,0.00007842831,0.00021706977,0.00001810904,0.000004904542,0.0000104291,0.00019385254,0.000011771062,0.00014744824],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99980396,0.0000795733,0.000012094702,0.000032457327,0.000017528078,0.000054511373],"domain_scores_gemma":[0.9991973,0.0005255187,0.00007930023,0.00005111329,0.000071388764,0.000075351454],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0007782703,0.00066251337,0.000691359,0.00053130527,0.00054729433,0.0010661214,0.00078505377,0.001482534,0.0023770176],"category_scores_gemma":[0.0020921372,0.00043185786,0.0009623184,0.00074901915,0.000624876,0.0008486252,0.00052884646,0.0007892547,0.00017896344],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018038462,0.0001390186,0.021110334,0.000060142516,0.00014014526,0.0001597164,0.000042969703,0.9738106,0.0017763546,0.0009805763,0.00034745253,0.0012523485],"study_design_scores_gemma":[0.000121694255,0.000095292555,0.012356883,0.000012415691,0.00005024707,0.000021962082,0.00007764811,0.9858657,0.0006796448,0.00040911694,0.00028745795,0.000021851856],"about_ca_topic_score_codex":0.045621198,"about_ca_topic_score_gemma":0.022555357,"teacher_disagreement_score":0.045621198,"about_ca_system_score_codex":0.000970514,"about_ca_system_score_gemma":0.00094599347,"threshold_uncertainty_score":0.090711296},"labels":[],"label_agreement":null},{"id":"W4410302279","doi":"10.1029/2024gl112434","title":"Properties of New Flows Indicate that Martian Gullies Form via CO<sub>2</sub> Frost‐Fluidization Processes","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"National Aeronautics and Space Administration","keywords":"Martian; Fluidization; Frost (temperature); Astrobiology; Geology; Environmental science; Atmospheric sciences; Mars Exploration Program; Meteorology; Thermodynamics; Geomorphology; Physics; Fluidized bed","score_opus":0.03964340411968201,"score_gpt":0.2781335516940626,"score_spread":0.2384901475743806,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410302279","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982217,0.000093809824,0.00025191053,0.000014258004,0.0000040026457,0.0000046122527,0.00025277399,0.000047262045,0.001109655],"genre_scores_gemma":[0.999185,0.000024855315,0.00025833695,0.0000074044397,0.0000034677016,0.0000021374974,0.00027834228,0.000005425088,0.00023500234],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999614,0.0000016142303,0.0000017742517,0.0000140988805,0.0000076913075,0.0000133158],"domain_scores_gemma":[0.9998286,0.000024356425,0.00006435995,0.000009511843,0.00003917618,0.000033976045],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006938395,0.00019015367,0.00013054155,0.00089488283,0.0002751403,0.00047150708,0.000112441274,0.0001980465,0.0022405814],"category_scores_gemma":[0.00020269936,0.000123436,0.00010864156,0.00036635585,0.0002553127,0.00030348945,0.00013815392,0.00016435917,0.00022458933],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005799354,0.000079547426,0.482228,0.00006239826,0.00005404329,0.00050653797,0.0004098734,0.00092062866,0.49779806,0.0005046417,0.0008728598,0.01598342],"study_design_scores_gemma":[0.000006751735,0.00004261315,0.97600275,0.0000035678054,0.000011895918,0.00014845307,0.00012478905,0.0030768597,0.019531537,0.00006599022,0.0009769814,0.000007726587],"about_ca_topic_score_codex":0.0065605934,"about_ca_topic_score_gemma":0.007782929,"teacher_disagreement_score":0.0065605934,"about_ca_system_score_codex":0.00028555034,"about_ca_system_score_gemma":0.000068034824,"threshold_uncertainty_score":0.013044834},"labels":[],"label_agreement":null},{"id":"W4410302336","doi":"10.1029/2025gl114690","title":"Impact of Cold Tongue Bias on Indian Ocean Dipole Prediction Skills","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Northern British Columbia","funders":"National Key Research and Development Program of China; National Natural Science Foundation of China","keywords":"Dipole; Climatology; Geology; Indian ocean; Environmental science; Oceanography; Physics","score_opus":0.019187158572587487,"score_gpt":0.29870746568263196,"score_spread":0.2795203071100445,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410302336","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9935441,0.00011087197,0.002853599,0.0002898662,0.000030433148,0.000008273467,0.00047170563,0.00013599147,0.0025551056],"genre_scores_gemma":[0.99911505,0.000022084365,0.0003340909,0.000026750131,0.00000837945,0.0000019939323,0.00032437392,0.000015796568,0.0001516626],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993525,0.00022316382,0.000047492165,0.00017282696,0.000094676165,0.00010925005],"domain_scores_gemma":[0.9945528,0.003351651,0.0005859316,0.0006088746,0.0005342465,0.00036655352],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026017185,0.00041552723,0.00034494905,0.0005035952,0.00033925002,0.0014586847,0.000596745,0.00040618106,0.0018369281],"category_scores_gemma":[0.012127662,0.00025722437,0.0005489196,0.00039514157,0.00047410617,0.0011903045,0.0012753031,0.00071837544,0.00031136238],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033136987,0.00007418915,0.7764154,0.000043139076,0.0003144584,0.00016516977,0.00029132015,0.19723317,0.0021404142,0.00092173286,0.0017416095,0.02032802],"study_design_scores_gemma":[0.0000791688,0.00010697041,0.3629523,0.00005115164,0.00009425442,0.00008340165,0.00054156047,0.6291323,0.002722088,0.0024825702,0.0016829106,0.00007130993],"about_ca_topic_score_codex":0.023456993,"about_ca_topic_score_gemma":0.019603081,"teacher_disagreement_score":0.023456993,"about_ca_system_score_codex":0.0005117491,"about_ca_system_score_gemma":0.00084438646,"threshold_uncertainty_score":0.046640933},"labels":[],"label_agreement":null},{"id":"W4410496243","doi":"10.1029/2024gl114207","title":"A Unique Mechanism of Ozone Surges Jointly Triggered by Deep Stratospheric Intrusions and the Tibetan Plateau Topographic Forcing","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":6,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Key Research and Development Program of China; Natural Science Foundation of Anhui Province; Nanjing University of Information Science and Technology; National Natural Science Foundation of China","keywords":"Plateau (mathematics); Forcing (mathematics); Geology; Mechanism (biology); Climatology; Ozone; Surge; Environmental science; Meteorology; Geomorphology; Geography","score_opus":0.01340684699959077,"score_gpt":0.2560770179938156,"score_spread":0.24267017099422483,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410496243","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99750704,0.000117069205,0.000963664,0.000066849534,0.0000135624105,0.0000054461943,0.000063671345,0.000059296905,0.0012035064],"genre_scores_gemma":[0.9996731,0.00002723457,0.00012375973,0.000005957902,0.00000566303,0.0000016402726,0.0000317965,0.0000010474192,0.00012973249],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999672,0.0000032084197,0.0000014418019,0.000006663227,0.0000049103264,0.000016568243],"domain_scores_gemma":[0.99993706,0.0000069232333,0.000018832332,0.000007136579,0.000009840508,0.000020194993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00010858118,0.00015345584,0.00013552803,0.00028882225,0.00028361773,0.00030067685,0.00017622247,0.00021022317,0.0009525896],"category_scores_gemma":[0.00011460823,0.00011481912,0.00020133791,0.00021187363,0.00019600202,0.00018565648,0.0003238024,0.00015036712,0.00007416608],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035328645,0.00009090008,0.41837502,0.00014443132,0.0001562405,0.0053256718,0.00045809572,0.013141727,0.5383229,0.0034849236,0.0011319567,0.019014822],"study_design_scores_gemma":[0.000049085767,0.00022950277,0.90162957,0.000016316337,0.000071131566,0.0008678554,0.00071402855,0.077324726,0.015082081,0.0021092538,0.0018725549,0.0000339105],"about_ca_topic_score_codex":0.0037393493,"about_ca_topic_score_gemma":0.0036056857,"teacher_disagreement_score":0.0037393493,"about_ca_system_score_codex":0.00018305809,"about_ca_system_score_gemma":0.00020319782,"threshold_uncertainty_score":0.0074352026},"labels":[],"label_agreement":null},{"id":"W4410496309","doi":"10.1029/2024gl112591","title":"Clustering to Characterize Extreme Marine Conditions for the Benthic Region of the Northeastern Pacific Continental Margin","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ocean Acidification Effects and Responses","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Hewlett-Packard (Canada); Fisheries and Oceans Canada","funders":"","keywords":"Environmental science; Benthic zone; Oceanography; Continental margin; Predictability; Climatology; Geology","score_opus":0.050284564504104116,"score_gpt":0.2891216604860947,"score_spread":0.2388370959819906,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410496309","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99089664,0.000038194372,0.0077141263,0.000030341895,0.0000031050959,0.000029128772,0.00056177686,0.000061957406,0.0006648499],"genre_scores_gemma":[0.9933295,0.000012699902,0.005474157,0.0000046972978,0.0000023651683,0.000016164364,0.00096497574,0.000009221374,0.00018628938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998599,0.000033126344,0.000011384737,0.000049356928,0.00002575062,0.000020380403],"domain_scores_gemma":[0.9996414,0.00007188228,0.00009427838,0.000057983052,0.000096178934,0.000038277667],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038770356,0.00021815032,0.00017813775,0.000990558,0.00036574516,0.00049883535,0.0002732255,0.00021378297,0.0005267258],"category_scores_gemma":[0.0010528674,0.00011834545,0.0004319645,0.0006429747,0.00017015058,0.00018682372,0.00042342054,0.00019586342,0.00007094596],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000295516,0.00014894192,0.66086483,0.000062745145,0.0007255449,0.00009019788,0.00043747088,0.28292188,0.011601038,0.0015300807,0.0017600846,0.039561704],"study_design_scores_gemma":[0.000014862318,0.000041829026,0.5704541,0.000010330783,0.000038949915,0.000041482774,0.00023992344,0.42647386,0.001122281,0.00090067834,0.0006360625,0.000025543879],"about_ca_topic_score_codex":0.03624194,"about_ca_topic_score_gemma":0.039206225,"teacher_disagreement_score":0.03624194,"about_ca_system_score_codex":0.00065954076,"about_ca_system_score_gemma":0.00048395956,"threshold_uncertainty_score":0.072062016},"labels":[],"label_agreement":null},{"id":"W4410601014","doi":"10.1029/2024gl113734","title":"Robustness and Mechanisms of the Atmospheric Response Over the Southern Ocean to Idealized Freshwater Input Around Antarctica","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Key Research and Development Program of China; Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)","keywords":"Robustness (evolution); Geology; Oceanography; Climatology; Environmental science; Meteorology; Geography","score_opus":0.009579974455847169,"score_gpt":0.2537330272938264,"score_spread":0.24415305283797925,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410601014","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99775285,0.000045670684,0.0008188069,0.00019668015,0.000011192414,0.000008218893,0.00024052501,0.000076908385,0.0008492694],"genre_scores_gemma":[0.99977,0.000014395991,0.000069665904,0.000009892691,0.0000031190573,0.0000033504111,0.00008027632,0.0000053654726,0.00004396112],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999813,0.00006674044,0.00001336884,0.00004313679,0.000016938926,0.000046909645],"domain_scores_gemma":[0.99924016,0.0003524843,0.00016162304,0.00010797994,0.00006787425,0.000069900976],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006266204,0.00046165907,0.0003547942,0.0003535879,0.0003399231,0.00062702934,0.0005084337,0.0005590519,0.0008710141],"category_scores_gemma":[0.0023701694,0.00038657198,0.00069116463,0.0002128157,0.0006498379,0.00042239594,0.0006318029,0.00039165665,0.00007672513],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00053289504,0.00008579747,0.06562899,0.00007174953,0.00032143673,0.00025626193,0.000116014126,0.89438635,0.033031315,0.0023642576,0.0005268069,0.0026780176],"study_design_scores_gemma":[0.00011536869,0.00015876984,0.09125424,0.000014880657,0.00007124013,0.000044421282,0.00011573599,0.9030902,0.0029903252,0.0018151732,0.0002806489,0.000048936632],"about_ca_topic_score_codex":0.014654901,"about_ca_topic_score_gemma":0.0041955705,"teacher_disagreement_score":0.014654901,"about_ca_system_score_codex":0.0006062577,"about_ca_system_score_gemma":0.00043226726,"threshold_uncertainty_score":0.02913922},"labels":[],"label_agreement":null},{"id":"W4410714053","doi":"10.1029/2025gl115606","title":"Coastal Erosion as a Major Sediment Source in the Inner Gulf of Thailand: Implications for Carbon Dynamics in Tropical Coastal Ocean Systems","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Coastal wetland ecosystem dynamics","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Cégep de Rimouski; Université du Québec à Rimouski","funders":"Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research; Deutsche Forschungsgemeinschaft","keywords":"Oceanography; Sediment; Erosion; Coastal erosion; Geology; Tropical cyclone; Environmental science; Tropical marine climate; Climatology; Hydrology (agriculture); Geomorphology; Meteorology; Geography; Shore","score_opus":0.013077691946330459,"score_gpt":0.2797518575596532,"score_spread":0.26667416561332274,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410714053","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99894446,0.00024026586,0.00006869009,0.000101898,0.0000019498577,0.0000022134009,0.00018625398,0.000004237675,0.000450115],"genre_scores_gemma":[0.9994869,0.00024653785,0.00005647908,0.000011466731,0.0000027042536,0.0000017714203,0.0000875968,0.0000014402192,0.00010506946],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999223,0.000018974542,0.000010373907,0.000014928741,0.000011296092,0.000022070362],"domain_scores_gemma":[0.99947244,0.00007016242,0.00021640155,0.000013176832,0.00009894044,0.00012902741],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025426206,0.00027616264,0.00014892564,0.00094601285,0.00044757302,0.0011303675,0.00015291611,0.00020610428,0.0011374485],"category_scores_gemma":[0.00039855792,0.00013926376,0.00020346383,0.0018331192,0.00044170616,0.00050881883,0.0005966108,0.0002232573,0.00007892153],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007913792,0.000016790516,0.98866117,0.00006727579,0.000053415395,0.0007233101,0.0005719721,0.0015855065,0.0022762213,0.00011623593,0.00013625811,0.005712716],"study_design_scores_gemma":[0.0000031761658,0.000017655777,0.99528766,0.00002237419,0.000023894416,0.00015710256,0.0017385905,0.0020947927,0.00021537383,0.00010253106,0.00032895192,0.000007918473],"about_ca_topic_score_codex":0.04675005,"about_ca_topic_score_gemma":0.046714816,"teacher_disagreement_score":0.04675005,"about_ca_system_score_codex":0.00059449463,"about_ca_system_score_gemma":0.00060936913,"threshold_uncertainty_score":0.09295583},"labels":[],"label_agreement":null},{"id":"W4410755731","doi":"10.1029/2025gl114831","title":"Large Decreases in Sea Ice Strength and Pressure Along Major Arctic Shipping Routes Projected for the Next Two Decades","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Environment and Climate Change Canada; York University","funders":"National Oceanic and Atmospheric Administration; Met Office","keywords":"Arctic; Sea ice; Geology; Climatology; The arctic; Arctic ice pack; Environmental science; Oceanography; Physical geography; Meteorology; Geography","score_opus":0.0288318678689691,"score_gpt":0.30600548779369685,"score_spread":0.2771736199247278,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410755731","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99301213,0.00027572725,0.0012029348,0.00030696124,0.000037865288,0.0000048269676,0.0038389775,0.00004591332,0.0012746799],"genre_scores_gemma":[0.9949005,0.0003236226,0.00057474343,0.000047296333,0.000016154916,0.000012101021,0.0035346411,0.000009462253,0.00058144453],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999137,0.000014243297,0.0000064348096,0.00002457297,0.000020822772,0.000020167596],"domain_scores_gemma":[0.999681,0.000033003376,0.00011583082,0.000023419952,0.00010390942,0.000042876334],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00038381884,0.00034733737,0.00013974463,0.00030037083,0.00018245462,0.00057666475,0.00020581893,0.00038181024,0.0012437116],"category_scores_gemma":[0.000762497,0.00011240954,0.00051873224,0.0005532757,0.00013321954,0.00047748638,0.00034875784,0.00043476725,0.00031686045],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003523573,0.00007506564,0.9156192,0.00012136553,0.00036509923,0.00031495077,0.00013799814,0.051660866,0.005363569,0.000906539,0.0027908138,0.022292271],"study_design_scores_gemma":[0.000014932405,0.00013286155,0.9555917,0.000043105865,0.00011508203,0.0001868076,0.00034369534,0.03462519,0.0025475163,0.00047125592,0.0058991266,0.000028711713],"about_ca_topic_score_codex":0.0209934,"about_ca_topic_score_gemma":0.018285647,"teacher_disagreement_score":0.0209934,"about_ca_system_score_codex":0.00045045343,"about_ca_system_score_gemma":0.00047114675,"threshold_uncertainty_score":0.041742444},"labels":[],"label_agreement":null},{"id":"W4410894856","doi":"10.1029/2025gl115483","title":"Field‐Aligned Proton Beams Upstream of the Martian Bow Shock: First Observations","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Centre National d’Etudes Spatiales","keywords":"Martian; Bow shock (aerodynamics); Bow wave; Upstream (networking); Proton; Physics; Field (mathematics); Shock (circulatory); Solar wind; Geophysics; Shock wave; Astrobiology; Mars Exploration Program; Geology; Astronomy; Environmental science; Nuclear physics; Mechanics; Plasma","score_opus":0.034009483405569994,"score_gpt":0.29670634555605724,"score_spread":0.26269686215048726,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4410894856","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99512804,0.00035241255,0.0008761908,0.000045979,0.000012872257,0.000020563726,0.0004455579,0.00006490079,0.0030534137],"genre_scores_gemma":[0.9970175,0.00016019224,0.0014510211,0.00003622388,0.000022721979,0.000012541557,0.0004640153,0.000009082513,0.00082658516],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99993837,0.000007197227,0.0000016279816,0.000011777854,0.00002266602,0.000018353105],"domain_scores_gemma":[0.9997737,0.00004119985,0.000038861872,0.000027737142,0.00007340123,0.00004510606],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017422043,0.00021559146,0.00021771624,0.0004980139,0.00042114372,0.00038376564,0.00019171809,0.00037984378,0.0015088689],"category_scores_gemma":[0.00029668174,0.00019259921,0.00015553828,0.00035863882,0.00016543493,0.00021049996,0.0003515445,0.00041908864,0.00030912925],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0023051132,0.00016168946,0.40412146,0.00026156884,0.00020782444,0.0034028823,0.0015839691,0.0009488076,0.537489,0.0009543864,0.0021787253,0.046384588],"study_design_scores_gemma":[0.00004318652,0.000584286,0.94810194,0.00003827924,0.000055498404,0.0013053674,0.00038812697,0.0010061417,0.03742863,0.00015530897,0.010875028,0.000018171966],"about_ca_topic_score_codex":0.0023293842,"about_ca_topic_score_gemma":0.0037044112,"teacher_disagreement_score":0.0023293842,"about_ca_system_score_codex":0.0002050716,"about_ca_system_score_gemma":0.00018175434,"threshold_uncertainty_score":0.0050476193},"labels":[],"label_agreement":null},{"id":"W4411132078","doi":"10.1029/2025gl115634","title":"Comment on “Revealing the Cape Verde Hotspot Track Across the Great Lakes” by Tao et al.","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"Directorate for Engineering; Natural Sciences and Engineering Research Council of Canada; Discovery Eye Foundation","keywords":"Hotspot (geology); Geology; Cape verde; Lithosphere; Geodynamics; Mesozoic; Paleontology; Mantle plume; Structural basin; Tectonics; Glacial period; Earth science; Seismology","score_opus":0.030460328908950042,"score_gpt":0.308231425418162,"score_spread":0.27777109650921195,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411132078","genre_codex":"commentary","genre_gemma":"commentary","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"commentary","genre_consensus":"commentary","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.0005456191,0.0010676073,0.00020066713,0.9265947,0.06939643,0.000029068131,0.0005201331,0.00013168999,0.0015141373],"genre_scores_gemma":[0.0029122238,0.00073005276,0.00020057133,0.95113474,0.040011108,0.00006870792,0.000113025446,0.0000534091,0.0047760988],"study_design_codex":"not_applicable","study_design_gemma":"not_applicable","domain_scores_codex":[0.9975103,0.00042180176,0.00036073354,0.0005510687,0.0008077656,0.0003482624],"domain_scores_gemma":[0.9915671,0.004044833,0.0006453809,0.0004537562,0.0023088318,0.0009800695],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.003999108,0.0011736321,0.0011337294,0.0011122858,0.0034874107,0.0030564799,0.0034221383,0.03184093,0.009028544],"category_scores_gemma":[0.025030963,0.00084908993,0.0010496511,0.0010380618,0.003681567,0.0041074613,0.0022834255,0.029129753,0.0074278167],"study_design_candidate":"not_applicable","study_design_consensus":"not_applicable","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000027209731,0.0000073082388,0.0002905562,0.000039518745,0.000005016292,0.00015101164,0.000109570545,0.000021454538,0.00009282545,0.00044824206,0.9972728,0.0015344147],"study_design_scores_gemma":[0.000068592606,0.00003514802,0.0027838764,0.00028092833,0.000019398332,0.0005692408,0.0007453678,0.00026279417,0.000536121,0.002617257,0.99200153,0.00007976719],"about_ca_topic_score_codex":0.030993598,"about_ca_topic_score_gemma":0.028630825,"teacher_disagreement_score":0.03184093,"about_ca_system_score_codex":0.0028491279,"about_ca_system_score_gemma":0.0046290853,"threshold_uncertainty_score":0.061626434},"labels":[],"label_agreement":null},{"id":"W4411132375","doi":"10.1029/2025gl114815","title":"Aerosol and Meteorological Influences on Mixed‐Phase Stratiform Clouds at North Slope of Alaska","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"","keywords":"Arctic; Liquid water path; Environmental science; Aerosol; Atmospheric sciences; The arctic; Liquid water content; Cloud computing; Climatology; Meteorology; Geology; Geography; Oceanography","score_opus":0.029323853779231697,"score_gpt":0.29991527472111884,"score_spread":0.27059142094188715,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411132375","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9995937,0.000018289948,0.000029661875,0.0000056707568,0.0000018893177,5.556295e-7,0.00016520952,0.0000026953242,0.00018242488],"genre_scores_gemma":[0.9997104,0.000014227492,0.000027379836,0.0000013725776,0.0000012187669,7.665664e-7,0.00017449228,7.6334055e-7,0.00006937157],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999436,0.000007798399,0.0000058698347,0.000017834955,0.000012219421,0.000012658703],"domain_scores_gemma":[0.9997303,0.000073534175,0.000047100217,0.000020794307,0.00007285326,0.000055439537],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00021613213,0.00016687666,0.00016164719,0.00035446355,0.00040750435,0.0005474292,0.00018301305,0.0002040916,0.00064376293],"category_scores_gemma":[0.0003781201,0.00011690764,0.00020674316,0.00025420415,0.00017135787,0.00029801612,0.00036287206,0.00017577826,0.00009564794],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017666069,0.000051378353,0.987523,0.000013652797,0.00006124971,0.00013164603,0.00019048856,0.0043288684,0.0054984554,0.000084027975,0.00009662674,0.0018439611],"study_design_scores_gemma":[0.0000034060677,0.000022072889,0.99435353,0.0000061362384,0.000018037372,0.000024276496,0.0003236903,0.004148275,0.00084652245,0.000042061627,0.00020695424,0.000004990592],"about_ca_topic_score_codex":0.119432494,"about_ca_topic_score_gemma":0.12783031,"teacher_disagreement_score":0.119432494,"about_ca_system_score_codex":0.0005629285,"about_ca_system_score_gemma":0.00042429226,"threshold_uncertainty_score":0.23747468},"labels":[],"label_agreement":null},{"id":"W4411176038","doi":"10.1029/2024gl113365","title":"Characteristics of Ice Nucleating Particles From the Long‐Range Transport of Saharan Dust","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"National Research Council Canada","funders":"National Research Council Canada; U.S. Department of Energy; National Science Foundation","keywords":"Range (aeronautics); Ice nucleus; Mineral dust; Geology; Atmospheric sciences; Environmental science; Nucleation; Meteorology; Aerosol; Materials science; Geography; Physics; Composite material","score_opus":0.028244712444421758,"score_gpt":0.2694395138163419,"score_spread":0.24119480137192015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411176038","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99903667,0.00009208929,0.00015834143,0.0000059568974,0.0000051472675,0.0000029036612,0.00016904826,0.0000045231204,0.0005253193],"genre_scores_gemma":[0.9991242,0.00004644152,0.0001288976,0.0000081338785,0.000007970388,0.0000046032733,0.0004158438,0.0000052838436,0.00025861213],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995434,0.000004543534,0.0000034758827,0.0000122848805,0.000013268689,0.000012148649],"domain_scores_gemma":[0.9998629,0.000027887894,0.000027013148,0.0000056490817,0.00004550761,0.000030915395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000116883115,0.00020168336,0.00012204149,0.0004643726,0.00028061628,0.00039290512,0.00015181326,0.00016725199,0.00087825576],"category_scores_gemma":[0.00019816718,0.00009350868,0.0001357787,0.0002394217,0.00010247081,0.00018038093,0.00014557273,0.00013691698,0.00022079723],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005395337,0.00008824241,0.6186095,0.00006543158,0.000118322525,0.00069301255,0.00044130447,0.0006370242,0.36798206,0.00017925406,0.00029547798,0.010350865],"study_design_scores_gemma":[0.000006371321,0.00008689031,0.978218,0.000004973298,0.000015174062,0.00019479971,0.00023719053,0.000987973,0.019596742,0.000038575105,0.0006070265,0.0000062373606],"about_ca_topic_score_codex":0.004071553,"about_ca_topic_score_gemma":0.0031878278,"teacher_disagreement_score":0.004071553,"about_ca_system_score_codex":0.00022339763,"about_ca_system_score_gemma":0.00007859617,"threshold_uncertainty_score":0.008095741},"labels":[],"label_agreement":null},{"id":"W4411242052","doi":"10.1029/2025gl116516","title":"Streamer‐Like Red Line Diffuse Auroras Driven by Time Domain Structures Associated With Electron Injection and Braking Ion Flows","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Air Force Office of Scientific Research; Division of Atmospheric and Geospace Sciences; Canadian Space Agency; National Aeronautics and Space Administration","keywords":"Ion; Electron; Line (geometry); Physics; Time domain; Van Allen radiation belt; Computational physics; Domain (mathematical analysis); Geophysics; Environmental science; Atomic physics; Magnetosphere; Plasma; Computer science; Nuclear physics; Geometry; Mathematics","score_opus":0.005191885078138193,"score_gpt":0.2530823204122413,"score_spread":0.24789043533410313,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411242052","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.991256,0.00005505821,0.0063330866,0.000039875307,0.000008446092,0.000009950021,0.00008481102,0.00014135662,0.0020715103],"genre_scores_gemma":[0.9989127,0.0000168869,0.0007188968,0.000005990006,0.000005375775,0.0000021837009,0.000037496888,0.000007089307,0.00029341475],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999851,0.000002370261,6.3201435e-7,0.00000412553,0.000003330982,0.0000045179213],"domain_scores_gemma":[0.99991155,0.000015896863,0.00003434312,0.000010946049,0.000011765009,0.000015456379],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000048956612,0.00015110648,0.00009554211,0.00015038575,0.00010816874,0.0002442652,0.00012572415,0.00012588309,0.000979083],"category_scores_gemma":[0.00017951377,0.00007546761,0.00012439795,0.00010263823,0.00018797569,0.00014776095,0.0001746767,0.00023908657,0.000072931354],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00090285874,0.00027097028,0.177115,0.00013911873,0.00021995738,0.0026566752,0.000628859,0.08923323,0.6729879,0.011704822,0.0029398024,0.041200846],"study_design_scores_gemma":[0.000085363885,0.00018611735,0.41658726,0.000013297764,0.000037634927,0.00062204676,0.00021575027,0.54075974,0.03532544,0.003464124,0.0026638366,0.000039433464],"about_ca_topic_score_codex":0.0006725973,"about_ca_topic_score_gemma":0.0006949261,"teacher_disagreement_score":0.000979083,"about_ca_system_score_codex":0.00013232899,"about_ca_system_score_gemma":0.000059096285,"threshold_uncertainty_score":0.0032753944},"labels":[],"label_agreement":null},{"id":"W4411308966","doi":"10.1029/2025gl114768","title":"Geostationary Satellites Total Ozone Observations: First Results on Ground‐Based Networks Validation Efforts for TEMPO and GEMS","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Geostationary orbit; Environmental science; Satellite; Meteorology; Geostationary Operational Environmental Satellite; Ozone Monitoring Instrument; Remote sensing; Troposphere; Ozone; Geography; Physics","score_opus":0.044383055192128096,"score_gpt":0.2941327220667286,"score_spread":0.24974966687460048,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411308966","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9691436,0.00018987469,0.007882012,0.00022695548,0.00007721926,0.00024601954,0.016025538,0.0004814739,0.0057273335],"genre_scores_gemma":[0.9185666,0.0001409208,0.020919928,0.000095458876,0.000039600218,0.00019009592,0.05868826,0.00015015197,0.0012089629],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99846786,0.0004978004,0.00010131491,0.0003178569,0.00049845414,0.00011671722],"domain_scores_gemma":[0.9961146,0.0007352074,0.00048751832,0.00117399,0.0012747467,0.00021391084],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.005040256,0.0006576361,0.00026869052,0.0006987253,0.0005216112,0.0007069023,0.0010616871,0.00057938165,0.0005764884],"category_scores_gemma":[0.0071534864,0.00019025852,0.00044414282,0.00096779654,0.0003172758,0.0009789215,0.00088771444,0.0005199354,0.00028176315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022972436,0.0021767274,0.672936,0.00032857308,0.0009830428,0.00034799948,0.0009116882,0.12971288,0.031347964,0.00434162,0.01792813,0.13668813],"study_design_scores_gemma":[0.0005504496,0.00071445305,0.80773985,0.00011885614,0.0002352961,0.00013152763,0.00050748093,0.15335685,0.01853095,0.00093789335,0.017095268,0.00008119519],"about_ca_topic_score_codex":0.04344126,"about_ca_topic_score_gemma":0.045808848,"teacher_disagreement_score":0.04344126,"about_ca_system_score_codex":0.0008553801,"about_ca_system_score_gemma":0.0006399906,"threshold_uncertainty_score":0.086376846},"labels":[],"label_agreement":null},{"id":"W4411341472","doi":"10.1029/2025gl114870","title":"Detectable Anthropogenic Influence in Mean Precipitation of China","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Pacific Institute for Climate Solutions; University of Victoria","funders":"China Meteorological Administration; National Natural Science Foundation of China","keywords":"Precipitation; Environmental science; Climatology; China; Atmospheric sciences; Geology; Meteorology; Geography","score_opus":0.02150096400552354,"score_gpt":0.32476710315936275,"score_spread":0.3032661391538392,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411341472","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99923384,0.000034342305,0.00016271745,0.000023364872,0.0000015561963,8.3386595e-7,0.00023810154,0.000011610635,0.00029366504],"genre_scores_gemma":[0.9997631,0.000011438711,0.000043987573,0.0000022655745,0.0000014862323,6.204129e-7,0.00015644002,6.585287e-7,0.000020081941],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99989176,0.000020008418,0.000009088583,0.000034034976,0.000024246741,0.0000208719],"domain_scores_gemma":[0.9994803,0.00010968665,0.00018322657,0.00007228305,0.00009973891,0.000054772212],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003323637,0.00016130798,0.00014300206,0.00048277446,0.00015710515,0.0003536415,0.00014944615,0.00009016364,0.00043052345],"category_scores_gemma":[0.00083568454,0.00009107417,0.0001627437,0.0008119406,0.00026203287,0.00017867512,0.00030534223,0.000103782935,0.00003345439],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006421543,0.000010047856,0.985276,0.000020919317,0.00005668862,0.00006957886,0.00009515021,0.004506482,0.003521151,0.00028790257,0.00016756686,0.0059244013],"study_design_scores_gemma":[0.0000021871892,0.000008745911,0.9954318,0.0000020450188,0.000007528196,0.000013531007,0.000032770862,0.0038515665,0.00038549307,0.000076080396,0.00018537544,0.0000030442952],"about_ca_topic_score_codex":0.016146151,"about_ca_topic_score_gemma":0.017932035,"teacher_disagreement_score":0.016146151,"about_ca_system_score_codex":0.00041213378,"about_ca_system_score_gemma":0.00046678956,"threshold_uncertainty_score":0.032104373},"labels":[],"label_agreement":null},{"id":"W4411419497","doi":"10.1029/2024gl114583","title":"Multidirectional Dune Dynamics Under Seasonal Winds on Mars","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"York University","funders":"Natural Sciences and Engineering Research Council of Canada","keywords":"Aeolian processes; Geology; Global wind patterns; Mars Exploration Program; Prevailing winds; Atmospheric sciences; Climatology; Geomorphology; Oceanography; Astrobiology","score_opus":0.02580603409698457,"score_gpt":0.3128731526606915,"score_spread":0.2870671185637069,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411419497","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994825,0.00002403369,0.000046378093,0.0000070587057,9.14033e-7,0.0000014830688,0.00017680472,0.0000063797465,0.00025438037],"genre_scores_gemma":[0.9995328,0.000024806224,0.00013680714,0.0000033044853,0.0000016501822,0.00000253837,0.00019194861,0.0000024307192,0.00010366865],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999312,0.000011370684,0.0000029695373,0.00002243876,0.000013606824,0.00001839003],"domain_scores_gemma":[0.99988866,0.00001682793,0.000035279965,0.000012295208,0.000022406562,0.000024542564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011731994,0.00013831303,0.00013594271,0.0008031214,0.00037024735,0.0005115221,0.0001275424,0.00018133354,0.0008307533],"category_scores_gemma":[0.00023335534,0.000089064284,0.00013950112,0.0004831821,0.00014837427,0.00022349646,0.0004238235,0.00012641972,0.0001220968],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009538631,0.000021899928,0.9723947,0.000024370262,0.00006399514,0.00026554862,0.0008152124,0.0017154047,0.010224318,0.00009331115,0.00035760336,0.013928158],"study_design_scores_gemma":[0.0000011884447,0.00001683377,0.9976673,0.000004163266,0.000007588023,0.000064420004,0.0003627413,0.0011440235,0.00019288981,0.000018425826,0.00051739713,0.0000030089263],"about_ca_topic_score_codex":0.005720144,"about_ca_topic_score_gemma":0.0110328775,"teacher_disagreement_score":0.005720144,"about_ca_system_score_codex":0.00019746687,"about_ca_system_score_gemma":0.00009060061,"threshold_uncertainty_score":0.011373699},"labels":[],"label_agreement":null},{"id":"W4411454993","doi":"10.1029/2025gl116307","title":"Fingerprints of AMOC Decline Are Sensitive to External and Mechanistic Forcing","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Ministero dell'Università e della Ricerca; National Science Foundation","keywords":"Forcing (mathematics); Climatology; Buoyancy; Environmental science; Climate model; Geology; Sea surface temperature; Climate change; Atmospheric sciences; Oceanography; Physics; Mechanics","score_opus":0.03194879758233629,"score_gpt":0.3278406267824928,"score_spread":0.29589182920015655,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411454993","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9975376,0.00003410055,0.0012001077,0.00003527548,0.000005706018,0.000006527436,0.00019280736,0.0000681774,0.0009197088],"genre_scores_gemma":[0.9996069,0.000010757254,0.00012688707,0.000008619848,0.000002310165,0.000003224878,0.00017658879,0.000010806568,0.000053934094],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9997875,0.00004634325,0.00002049503,0.00006880775,0.000029756717,0.00004708962],"domain_scores_gemma":[0.9984459,0.00062294287,0.00026286885,0.000332176,0.00015033827,0.00018570016],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0008519175,0.00022222157,0.00032780517,0.0004954547,0.00022689125,0.00086592743,0.00024192885,0.0002477142,0.0011043088],"category_scores_gemma":[0.0047256257,0.00019706757,0.00039953578,0.0002879718,0.00038363467,0.00066792144,0.0007377692,0.00043707792,0.000120287325],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00052842963,0.00014855588,0.8297751,0.00009376577,0.0003786831,0.00026219082,0.00025488957,0.10095172,0.049701676,0.0015440673,0.0007062995,0.015654694],"study_design_scores_gemma":[0.000025390302,0.000168591,0.77871776,0.000015767631,0.00005592207,0.000098294375,0.0001696707,0.21155983,0.007440113,0.0010165196,0.0006973197,0.000034751356],"about_ca_topic_score_codex":0.002498864,"about_ca_topic_score_gemma":0.0015620631,"teacher_disagreement_score":0.002498864,"about_ca_system_score_codex":0.00023716401,"about_ca_system_score_gemma":0.0001825404,"threshold_uncertainty_score":0.004968643},"labels":[],"label_agreement":null},{"id":"W4411456877","doi":"10.1029/2024gl114184","title":"Depositional Controls on ∆′ <sup>17</sup> O Signatures of Sedimentary Sulfate","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Paleontology and Stratigraphy of Fossils","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University","funders":"Natural Sciences and Engineering Research Council of Canada; Canadian Institute for Advanced Research; National Science Foundation","keywords":"Sedimentary depositional environment; Sulfate; Geology; Sedimentary rock; Proterozoic; Carbonate; Geochemistry; Paleontology; Structural basin; Chemistry","score_opus":0.01920769514711672,"score_gpt":0.2864143993025444,"score_spread":0.2672067041554277,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411456877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99882334,0.00007507405,0.00011572129,0.00001200959,0.0000013285654,0.0000013088851,0.000103220824,0.0000062312424,0.00086168095],"genre_scores_gemma":[0.99960846,0.00004879271,0.00006620998,0.000007593555,0.0000010150002,0.0000011898182,0.00007830056,0.0000052483774,0.00018316638],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9999099,0.000013873205,0.000007643443,0.000033968405,0.000016469876,0.00001824872],"domain_scores_gemma":[0.99981004,0.00004905106,0.00005875718,0.000026164756,0.000029916506,0.0000260351],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00025191423,0.0001772354,0.0001381027,0.00048142852,0.0002523847,0.00047474744,0.00019997475,0.00015428376,0.001076774],"category_scores_gemma":[0.00038478055,0.00017801668,0.00011114765,0.00034971457,0.00060197903,0.00023562234,0.00044444497,0.00013890104,0.00013606228],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00050836464,0.000028196122,0.3564927,0.00007302019,0.00009000689,0.00036203675,0.0007106242,0.0007637042,0.6296404,0.0009947759,0.00016698586,0.010169165],"study_design_scores_gemma":[0.0000041655194,0.000035609417,0.9891366,0.0000042587467,0.000013796746,0.000062753825,0.00019648472,0.00018329834,0.009645815,0.00014372605,0.00056938815,0.0000041863723],"about_ca_topic_score_codex":0.004847666,"about_ca_topic_score_gemma":0.009113405,"teacher_disagreement_score":0.004847666,"about_ca_system_score_codex":0.00026303786,"about_ca_system_score_gemma":0.00019951824,"threshold_uncertainty_score":0.0096389055},"labels":[],"label_agreement":null},{"id":"W4411624877","doi":"10.1029/2025gl115235","title":"Glaciers in Western Canada‐Conterminous US and Switzerland Experience Unprecedented Mass Loss Over the Last Four Years (2021–2024)","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Northern British Columbia; Environment and Climate Change Canada; Geological Survey of Canada; Natural Resources Canada","funders":"Global Water Futures; Hakai Institute; Natural Sciences and Engineering Research Council of Canada; U.S. Geological Survey; Directorate for Engineering; Austrian Science Fund; Tula Foundation","keywords":"Glacier; Physical geography; Climatology; Geology; Geography","score_opus":0.023299559070976045,"score_gpt":0.275432176800581,"score_spread":0.252132617729605,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411624877","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9944278,0.00046161524,0.00012228006,0.00030013738,0.000020035672,0.00000436866,0.0022876733,0.0000429024,0.002333224],"genre_scores_gemma":[0.99692863,0.00021920392,0.00006491135,0.000043002052,0.000008198019,0.0000027335943,0.0021423975,0.0000048484467,0.00058616576],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998989,0.0000048614265,0.0000033027084,0.000014821799,0.000031072457,0.000046958885],"domain_scores_gemma":[0.99977285,0.000009689208,0.00008080484,0.000011081392,0.00008559374,0.00004000847],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019683337,0.00033553242,0.00012967645,0.0006684813,0.0006149483,0.0008745514,0.00025430668,0.00034445545,0.0017160551],"category_scores_gemma":[0.00038611642,0.00008112306,0.0002152037,0.0008845469,0.00032391725,0.00046442568,0.0004662686,0.00026893042,0.0003158877],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017440433,0.000025074889,0.972672,0.000040617277,0.00012608885,0.0002749203,0.00036157775,0.0023589188,0.0022237063,0.00021880941,0.0042775422,0.01724648],"study_design_scores_gemma":[0.0000036231843,0.000015918722,0.9953133,0.000012574565,0.000019374052,0.00006862039,0.00044613794,0.0010289513,0.00029214067,0.00006126107,0.0027311933,0.000006851384],"about_ca_topic_score_codex":0.50156826,"about_ca_topic_score_gemma":0.6189815,"teacher_disagreement_score":0.49843174,"about_ca_system_score_codex":0.0019599698,"about_ca_system_score_gemma":0.0010240898,"threshold_uncertainty_score":0.9972976},"labels":[],"label_agreement":null},{"id":"W4411649892","doi":"10.1029/2024gl113849","title":"Large Size of Two 19th‐Century Chile‐Peru Earthquakes Inferred From Trans‐Pacific Tsunami Records","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria; Geological Survey of Canada","funders":"Fondo de Financiamiento de Centros de Investigación en Áreas Prioritarias; Fondo Nacional de Desarrollo Científico y Tecnológico; Agencia Nacional de Investigación y Desarrollo","keywords":"Geology; Seismology","score_opus":0.022085294022705,"score_gpt":0.29096716591570587,"score_spread":0.2688818718930009,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411649892","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99826765,0.000081558304,0.00012939339,0.00005438092,0.0000017872491,0.000002651706,0.0003611131,0.0000071981026,0.0010942352],"genre_scores_gemma":[0.9993754,0.00007197776,0.000091909016,0.0000042716456,0.0000050617837,0.0000039981983,0.00033420188,0.000001770088,0.000111493995],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999229,0.000023925611,0.000007814048,0.000019345307,0.00001556795,0.000010375951],"domain_scores_gemma":[0.99904484,0.00023027681,0.00035521737,0.00010104693,0.00018055803,0.00008805446],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00032936898,0.00013405994,0.00009583629,0.0011357729,0.00022981239,0.00049557706,0.00019647804,0.0001668563,0.0013748647],"category_scores_gemma":[0.0020923791,0.00012630428,0.00012586833,0.0007947319,0.00026599053,0.0004101514,0.00081904815,0.0002482017,0.00024682423],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006606481,0.000015164547,0.98443246,0.000033823664,0.000087593624,0.00031808484,0.0010981503,0.00073348597,0.0034579043,0.00020300315,0.000353902,0.009200279],"study_design_scores_gemma":[0.0000031126679,0.000008339668,0.9982311,0.000010079534,0.000009859799,0.000078916346,0.00027671945,0.0004885355,0.00023417534,0.000045355766,0.00060910627,0.0000046921687],"about_ca_topic_score_codex":0.005396673,"about_ca_topic_score_gemma":0.008461466,"teacher_disagreement_score":0.005396673,"about_ca_system_score_codex":0.00028634802,"about_ca_system_score_gemma":0.00015217792,"threshold_uncertainty_score":0.010730505},"labels":[],"label_agreement":null},{"id":"W4411785593","doi":"10.1029/2025gl114941","title":"Causal Directions Matter: How Environmental Factors Drive Convective Cloud Detrainment Heights","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Workforce Development for Teachers and Scientists; U.S. Department of Energy","keywords":"Environmental science; Cloud computing; Atmospheric sciences; Convection; Meteorology; Physics; Computer science","score_opus":0.028106722175285672,"score_gpt":0.26956479285578894,"score_spread":0.24145807068050326,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411785593","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9515021,0.00041759814,0.044265855,0.001096958,0.00004530796,0.000036515703,0.000873019,0.00011970962,0.0016429782],"genre_scores_gemma":[0.99842215,0.000042724278,0.0012225066,0.000030656618,0.000009067456,0.000004366858,0.00012812536,0.0000066625507,0.00013376272],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9990702,0.0005207476,0.00004277485,0.00021633343,0.000059823382,0.00009017362],"domain_scores_gemma":[0.98640513,0.011466798,0.0010188749,0.0006027755,0.00026027003,0.0002461458],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0026897206,0.00026434442,0.00025300556,0.0005420754,0.0003271299,0.0010157548,0.00036913238,0.00042935312,0.0025664663],"category_scores_gemma":[0.016539125,0.00025398852,0.0006504469,0.0005270065,0.0005214906,0.0007589358,0.00060205016,0.00076183234,0.00014137724],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00033383662,0.00011681632,0.9199729,0.000088934205,0.0006379576,0.00023895844,0.00039037567,0.03912402,0.0027258203,0.010602696,0.0006798923,0.025087856],"study_design_scores_gemma":[0.000065578715,0.00015152516,0.6238695,0.00007393724,0.00044558707,0.00014479413,0.00077853067,0.3167583,0.0023542575,0.052928984,0.002370207,0.00005878264],"about_ca_topic_score_codex":0.010734135,"about_ca_topic_score_gemma":0.010538957,"teacher_disagreement_score":0.010734135,"about_ca_system_score_codex":0.00034426045,"about_ca_system_score_gemma":0.0007150757,"threshold_uncertainty_score":0.02134335},"labels":[],"label_agreement":null},{"id":"W4411785888","doi":"10.1029/2025gl115919","title":"Low Heat Flow in the Anhydros Basin, Aegean Sea, Recorded by Deep Subsurface Temperatures","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydrocarbon exploration and reservoir analysis","field":"Engineering","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"U.S. Science Support Program, Lamont-Doherty Earth Observatory; Grantová Agentura České Republiky; United States Science Support Program; Canadian Institute for Advanced Research; Adolph C. and Mary Sprague Miller Institute for Basic Research in Science, University of California Berkeley","keywords":"Heat flow; Geology; Structural basin; Oceanography; Climatology; Meteorology; Geomorphology; Geography","score_opus":0.011475912414057082,"score_gpt":0.2692832315313388,"score_spread":0.2578073191172817,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411785888","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99896467,0.000050492457,0.000025631318,0.00000945058,0.0000019579657,0.0000011613703,0.00022216514,0.000002502099,0.0007220733],"genre_scores_gemma":[0.9994548,0.000055436733,0.00007973212,0.0000053933836,0.0000024737399,0.0000016955131,0.000264279,8.6033975e-7,0.00013531701],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999961,0.000003685204,0.0000051340294,0.000013708618,0.000007753395,0.00000868166],"domain_scores_gemma":[0.99993813,0.000007036673,0.00002272573,0.000004852899,0.00001701139,0.000010219296],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009342009,0.00020532383,0.00014285556,0.00055390655,0.00023179979,0.00030272568,0.000081164995,0.00013601546,0.00055076805],"category_scores_gemma":[0.00014448108,0.00011511138,0.000086495194,0.00043164488,0.00034401324,0.00025959496,0.00021718154,0.00011695435,0.00011354621],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017781413,0.000026266334,0.9668142,0.00005119162,0.00004463859,0.00028030705,0.0004987516,0.0006610284,0.02188347,0.00015151977,0.00023696378,0.009173838],"study_design_scores_gemma":[0.000005933214,0.000031839798,0.9977996,0.0000070549363,0.000009634214,0.00007014152,0.000282048,0.00031118921,0.0008618993,0.00002455176,0.0005932648,0.0000028017753],"about_ca_topic_score_codex":0.021747552,"about_ca_topic_score_gemma":0.030675085,"teacher_disagreement_score":0.021747552,"about_ca_system_score_codex":0.0005189407,"about_ca_system_score_gemma":0.00032097538,"threshold_uncertainty_score":0.043241978},"labels":[],"label_agreement":null},{"id":"W4411808940","doi":"10.1029/2025gl114864","title":"Scale Dependent Relationships Between Precipitation and Atmospheric Source Nitrate: Insights From the Yarlung Tsangpo River Basin","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Groundwater and Isotope Geochemistry","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Natural Science Foundation of Gansu Province; National Natural Science Foundation of China","keywords":"Precipitation; Environmental science; Scale (ratio); Climatology; Drainage basin; Nitrate; Structural basin; Atmospheric sciences; Hydrology (agriculture); Geology; Meteorology; Geography; Geomorphology","score_opus":0.024353876102105602,"score_gpt":0.2536197601071166,"score_spread":0.22926588400501102,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411808940","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999446,0.000021604948,0.00007418798,0.00002393334,7.5004874e-7,0.0000018969981,0.00007935235,0.0000031527318,0.00034903485],"genre_scores_gemma":[0.99976236,0.000031486466,0.000075586366,0.0000054254383,0.0000017178677,0.0000021664996,0.000077584555,0.0000013488947,0.00004240273],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999536,0.000013247363,0.0000039716438,0.000011869866,0.000006896876,0.0000104039855],"domain_scores_gemma":[0.9998691,0.000045269346,0.000029038296,0.000008725416,0.00002765922,0.000020129555],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018024494,0.00013402237,0.00017874874,0.0005657648,0.0002963524,0.00036757955,0.00021917692,0.00018560162,0.000580231],"category_scores_gemma":[0.00041760312,0.000111645,0.00021645198,0.001096425,0.00025147866,0.00027970917,0.00032601063,0.00017323927,0.00004685403],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000082981314,0.000054291966,0.96993726,0.00005450867,0.000089718545,0.000558761,0.0010487316,0.0050870725,0.009876654,0.0002735618,0.0002165908,0.012719937],"study_design_scores_gemma":[0.000006502019,0.0000128726115,0.98733205,0.0000065335335,0.000017046286,0.000036902267,0.00066742377,0.01123915,0.00021010576,0.00016768338,0.00029736437,0.0000063880116],"about_ca_topic_score_codex":0.040998325,"about_ca_topic_score_gemma":0.06194809,"teacher_disagreement_score":0.040998325,"about_ca_system_score_codex":0.0003352258,"about_ca_system_score_gemma":0.00039084858,"threshold_uncertainty_score":0.081519425},"labels":[],"label_agreement":null},{"id":"W4411880621","doi":"10.1029/2025gl116467","title":"Statistical Distribution of Dawnside Auroral Polarization Streams","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Science and Technology Facilities Council; Science Mission Directorate; National Aeronautics and Space Administration; Canadian Space Agency; UK Space Agency; National Science Foundation","keywords":"STREAMS; Polarization (electrochemistry); Geology; Geophysics; Induced polarization; Statistical analysis; Remote sensing; Environmental science; Physics; Computer science; Statistics","score_opus":0.011122494568995262,"score_gpt":0.3026009365882606,"score_spread":0.2914784420192653,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4411880621","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99730057,0.000041734744,0.0013756315,0.00002941426,0.000005737387,0.000005296943,0.0007091271,0.000033353394,0.0004990498],"genre_scores_gemma":[0.99886924,0.000011707841,0.000107053296,0.0000021365915,0.0000053987633,0.0000030594495,0.00091668195,0.00000386758,0.00008101347],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9996119,0.00006801876,0.00003139382,0.00015970398,0.000071853494,0.00005721366],"domain_scores_gemma":[0.9942205,0.0029169722,0.0012303112,0.0006130777,0.00064213335,0.00037702336],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009071036,0.000116227806,0.00020953799,0.0010075945,0.00022448077,0.0005861028,0.00023021834,0.00023253157,0.001262342],"category_scores_gemma":[0.0050497483,0.00010565158,0.00022847879,0.0007020165,0.0005307442,0.00044036022,0.00034505955,0.00025471288,0.00020247376],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017951641,0.000041375566,0.97172594,0.000031813248,0.00010759306,0.00016702335,0.00021104568,0.010601514,0.0060566426,0.0012272933,0.00075937656,0.00889086],"study_design_scores_gemma":[0.000010687143,0.00014799507,0.93176585,0.000007885076,0.000044324526,0.00035692143,0.00032417863,0.06296231,0.0022963444,0.0010020249,0.0010433684,0.00003811383],"about_ca_topic_score_codex":0.0013079154,"about_ca_topic_score_gemma":0.0009790946,"teacher_disagreement_score":0.0013079154,"about_ca_system_score_codex":0.00022406958,"about_ca_system_score_gemma":0.00016771303,"threshold_uncertainty_score":0.00479728},"labels":[],"label_agreement":null},{"id":"W4412090266","doi":"10.1029/2024gl112870","title":"Ku‐ and Ka‐Band Polarimetric Radar Waveforms and Snow Depth Estimation Over Multi‐Year Antarctic Sea Ice in the Weddell Sea","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary; University of Manitoba","funders":"International Space Science Institute; Natural Environment Research Council; European Space Agency","keywords":"Geology; Sea ice; Polarimetry; Snow; Remote sensing; Radar; Sea ice thickness; Cryosphere; Climatology; Geomorphology; Scattering","score_opus":0.019815938755917088,"score_gpt":0.28415259596343456,"score_spread":0.2643366572075175,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412090266","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994777,0.000036043966,0.00015357471,0.000006092655,0.0000030998751,0.0000016192963,0.000092998824,0.0000041064873,0.00022480547],"genre_scores_gemma":[0.99931335,0.00003104168,0.00033131277,0.0000043476084,0.000002607845,0.0000015588364,0.00015602808,0.0000012991616,0.00015845402],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99995625,0.0000076049173,0.000004175071,0.000011071391,0.000007669667,0.0000133108315],"domain_scores_gemma":[0.99982196,0.000034918365,0.000043782322,0.000013994818,0.000054288754,0.00003118305],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00022643934,0.00017378457,0.00009292892,0.0007024796,0.00013986354,0.00035929587,0.000112477836,0.00013864182,0.00035751148],"category_scores_gemma":[0.00028310873,0.00008588534,0.000094990864,0.00030555218,0.00009565168,0.00026071735,0.00023826394,0.000087585315,0.00010142275],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000224078,0.00004593682,0.9486931,0.00002927132,0.000047299465,0.00020347681,0.00028894746,0.0021675006,0.025181003,0.000053948697,0.00023704424,0.022828411],"study_design_scores_gemma":[0.000005333304,0.000057597375,0.9903612,0.000009854303,0.000018446555,0.00007976762,0.00038231682,0.005520818,0.003210193,0.000019134755,0.00033104626,0.000004321039],"about_ca_topic_score_codex":0.007051101,"about_ca_topic_score_gemma":0.020864047,"teacher_disagreement_score":0.007051101,"about_ca_system_score_codex":0.0001848614,"about_ca_system_score_gemma":0.00014463601,"threshold_uncertainty_score":0.014020145},"labels":[],"label_agreement":null},{"id":"W4412146682","doi":"10.1029/2024gl114388","title":"Capillary‐Driven Transport and Precipitation of Salt in Heterogeneous Structures During Carbon Sequestration","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"CO2 Sequestration and Geologic Interactions","field":"Environmental Science","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Alberta","funders":"National Natural Science Foundation of China","keywords":"Carbon sequestration; Precipitation; Carbon fibers; Environmental science; Capillary action; Geology; Earth science; Atmospheric sciences; Carbon dioxide; Materials science; Chemistry; Meteorology","score_opus":0.01704866213566389,"score_gpt":0.3081331573928492,"score_spread":0.29108449525718527,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412146682","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994854,0.000013770505,0.0003098909,0.000008113564,0.0000011051903,0.000003825769,0.000018779088,0.000008074198,0.00015099664],"genre_scores_gemma":[0.9997209,0.000009621203,0.00016391328,0.0000027358885,5.1121197e-7,0.0000027555327,0.000014906715,0.0000016190602,0.00008313735],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99992716,0.000007837861,0.0000029546607,0.000018627821,0.000017696058,0.000025797333],"domain_scores_gemma":[0.999876,0.000037676466,0.000026116673,0.0000056404397,0.000028763267,0.000025808566],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014497072,0.00016260364,0.00017977328,0.00013385825,0.00025918568,0.00038998123,0.0001733399,0.00018370031,0.000371921],"category_scores_gemma":[0.00023949315,0.00012322384,0.000093776835,0.00009507451,0.0005221128,0.00027596945,0.00023897902,0.00025863692,0.00003841846],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012431896,0.000043277294,0.0041855685,0.000013668365,0.0000061169417,0.000087753986,0.00004881814,0.001697714,0.9923861,0.00014577045,0.000040626383,0.001220119],"study_design_scores_gemma":[0.000029398801,0.0003152012,0.027118273,0.000003610179,0.000008291095,0.00006214432,0.00014139134,0.030507933,0.94143313,0.00011322391,0.0002539579,0.000013486632],"about_ca_topic_score_codex":0.0035454808,"about_ca_topic_score_gemma":0.0043170014,"teacher_disagreement_score":0.0035454808,"about_ca_system_score_codex":0.0003865685,"about_ca_system_score_gemma":0.0003215288,"threshold_uncertainty_score":0.0070497394},"labels":[],"label_agreement":null},{"id":"W4412450397","doi":"10.1029/2025gl116050","title":"Large Surface‐Rupturing Earthquakes and a &gt;12 kyr, Open Interseismic Interval on the Tintina Fault, Yukon","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"earthquake and tectonic studies","field":"Earth and Planetary Sciences","cited_by":5,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; Natural Resources Canada; University of Alberta; University of Victoria","funders":"Canada Foundation for Innovation; Polar Knowledge Canada; University of Victoria; British Columbia Knowledge Development Fund; Natural Sciences and Engineering Research Council of Canada; Yukon Foundation","keywords":"Geology; Seismology; Fault (geology); Interval (graph theory)","score_opus":0.04721395939675155,"score_gpt":0.3122501077528456,"score_spread":0.26503614835609407,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412450397","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9994361,0.000039740673,0.000026283797,0.000008965787,0.0000010318992,0.0000018881084,0.00007330168,0.0000022863114,0.00041027702],"genre_scores_gemma":[0.99962795,0.000024517332,0.00002840274,0.0000049976575,6.2101685e-7,0.0000012009416,0.00014115643,6.416809e-7,0.0001705735],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999198,0.0000048509596,0.000006525912,0.000019822714,0.000017345896,0.000031560547],"domain_scores_gemma":[0.999701,0.00001929617,0.00006644244,0.000017399718,0.000102279424,0.00009355866],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009579471,0.00015871853,0.00014993288,0.0006555939,0.0007726262,0.00046481457,0.0002470234,0.00021438676,0.00087214855],"category_scores_gemma":[0.0003545962,0.00011548189,0.00010509131,0.0007862464,0.0005239949,0.00015823996,0.0005261605,0.00015968064,0.00010155166],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00007127937,0.00001779634,0.9859584,0.00001999103,0.000036495316,0.00053808675,0.0010320374,0.00015952725,0.006259564,0.000078456906,0.0001227404,0.005705652],"study_design_scores_gemma":[0.0000013814172,0.00000928565,0.9991788,0.000002256871,0.0000045756965,0.000066831046,0.0004540318,0.000047755213,0.00005968895,0.000009989256,0.00016398214,0.00000134417],"about_ca_topic_score_codex":0.43041706,"about_ca_topic_score_gemma":0.7363477,"teacher_disagreement_score":0.56958294,"about_ca_system_score_codex":0.0018524561,"about_ca_system_score_gemma":0.0013391089,"threshold_uncertainty_score":0.8558235},"labels":[],"label_agreement":null},{"id":"W4412514426","doi":"10.1029/2025gl115788","title":"Hourly Sulfur Dioxide Observations Over North America: First Retrieval Results From TEMPO","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"National Aeronautics and Space Administration","keywords":"Sulfur dioxide; Environmental science; Sulfur; Climatology; Meteorology; Geology; Chemistry; Geography; Inorganic chemistry","score_opus":0.03819492319155159,"score_gpt":0.27814985259266484,"score_spread":0.23995492940111324,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412514426","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9939452,0.00017593926,0.0009579204,0.00010967753,0.000024578787,0.000016910597,0.0020951268,0.00028889542,0.002385849],"genre_scores_gemma":[0.98887,0.00014673932,0.004746306,0.00005079132,0.000059171565,0.000017524475,0.0051111174,0.00005667743,0.0009416224],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989605,0.000008957022,0.000004651378,0.000028641758,0.000037368936,0.000024262225],"domain_scores_gemma":[0.9997807,0.000025612264,0.000029364437,0.00003422518,0.000092115515,0.00003804363],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00023434017,0.00039871468,0.00036639356,0.00058913155,0.0003683641,0.00046131003,0.0003269216,0.0003657087,0.0011168906],"category_scores_gemma":[0.0004049176,0.00021322905,0.0002838,0.00073452387,0.00018534252,0.00040262647,0.00045293482,0.00032097232,0.00020895181],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0015825152,0.0006387077,0.43673906,0.0003396822,0.00067344244,0.0013838208,0.0011408995,0.022326576,0.40444818,0.0005376548,0.008342163,0.12184718],"study_design_scores_gemma":[0.00022434442,0.00028365068,0.92515093,0.000027199305,0.0002082296,0.00019079524,0.00043545204,0.036055554,0.025058083,0.00022911726,0.012059315,0.000077465134],"about_ca_topic_score_codex":0.022839045,"about_ca_topic_score_gemma":0.064337894,"teacher_disagreement_score":0.022839045,"about_ca_system_score_codex":0.00032715578,"about_ca_system_score_gemma":0.0003426712,"threshold_uncertainty_score":0.045412183},"labels":[],"label_agreement":null},{"id":"W4412577602","doi":"10.1029/2025gl116548","title":"The Spatiotemporal Dynamics of Heatwaves and Cold‐Spells in Earth's Largest Freshwater Systems","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"National Science Foundation","keywords":"Climatology; Environmental science; Earth system science; Meteorology; Geology; Atmospheric sciences; Oceanography; Geography","score_opus":0.019968585707034085,"score_gpt":0.2886798251730169,"score_spread":0.2687112394659828,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412577602","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9993612,0.000032228876,0.000098935096,0.000031871572,0.0000010559634,8.4846937e-7,0.00024882908,0.000005752466,0.00021930145],"genre_scores_gemma":[0.9996493,0.00002337338,0.000038111866,0.000003872118,0.000001569377,0.0000013019467,0.00022562484,9.279692e-7,0.000055984554],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996066,0.0000082040115,0.0000034121224,0.000010817282,0.0000066529096,0.000010172114],"domain_scores_gemma":[0.9998031,0.00004564006,0.00007123952,0.000016771282,0.00002663047,0.00003666079],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016832823,0.000088698136,0.000109541375,0.00031288716,0.00019713613,0.0004605328,0.000093380186,0.0001652776,0.0007015982],"category_scores_gemma":[0.00051766506,0.00010380016,0.00019887096,0.00047388978,0.00023344347,0.0002662714,0.00037179832,0.00011545492,0.000069396716],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006531416,0.000019993004,0.9794763,0.00001984491,0.000109353925,0.000065021006,0.00018392659,0.0123936115,0.0030198328,0.00027179896,0.00048134112,0.003893799],"study_design_scores_gemma":[0.0000035335654,0.000014603264,0.9920614,0.0000031035738,0.000011588337,0.000016298887,0.000104472616,0.0072023063,0.00015704661,0.00009729137,0.0003247447,0.0000036512024],"about_ca_topic_score_codex":0.029777056,"about_ca_topic_score_gemma":0.04235635,"teacher_disagreement_score":0.029777056,"about_ca_system_score_codex":0.0003478183,"about_ca_system_score_gemma":0.00018858786,"threshold_uncertainty_score":0.05920744},"labels":[],"label_agreement":null},{"id":"W4412577909","doi":"10.1029/2025gl115080","title":"Coupling Between Methylmercury and Carbon‐Gases Across Boreal Rivers of Québec, Canada","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Mercury impact and mitigation studies","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université du Québec à Montréal; Université de Montréal; McGill University; Université du Québec","funders":"Natural Sciences and Engineering Research Council of Canada; Groupe de recherche interuniversitaire en limnologie; Svenska Forskningsrådet Formas","keywords":"Boreal; Methylmercury; Coupling (piping); Environmental science; Carbon fibers; Atmospheric sciences; Oceanography; Climatology; Astrobiology; Earth science; Physics; Geology; Materials science; Chemistry; Environmental chemistry; Paleontology","score_opus":0.030526474430826556,"score_gpt":0.33610529428583863,"score_spread":0.30557881985501206,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412577909","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9936473,0.000305818,0.00028401686,0.00011719932,0.000003588851,0.00001709758,0.003215702,0.000024480434,0.0023849704],"genre_scores_gemma":[0.9976089,0.00011115785,0.0003066738,0.000043793698,0.0000014665128,0.000009859951,0.00096934143,0.0000053444373,0.0009434551],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997756,0.000024486742,0.000010018861,0.000079723875,0.000049681585,0.000060464467],"domain_scores_gemma":[0.99931157,0.0000613755,0.00009123718,0.000020783695,0.0004482521,0.00006672395],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024027009,0.00022782337,0.00021341901,0.00089449337,0.0012197735,0.0008974201,0.00045033445,0.00024131837,0.0014130407],"category_scores_gemma":[0.00063697295,0.00014928778,0.00022592371,0.002172762,0.0004346527,0.00020769211,0.0003109391,0.00018558143,0.000108734006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00009684876,0.000017402634,0.9840395,0.000037493064,0.00012489955,0.000101139696,0.00072096195,0.0009838183,0.00394138,0.00013518288,0.0007718655,0.009029579],"study_design_scores_gemma":[0.0000017007429,0.000004208729,0.99865,0.0000062587815,0.000011061421,0.000010836659,0.00032687993,0.00025657247,0.00015483625,0.000010811926,0.0005622087,0.0000045502093],"about_ca_topic_score_codex":0.9909622,"about_ca_topic_score_gemma":0.99593204,"teacher_disagreement_score":0.0117589375,"about_ca_system_score_codex":0.0117589375,"about_ca_system_score_gemma":0.0068769553,"threshold_uncertainty_score":0.08531749},"labels":[],"label_agreement":null},{"id":"W4412739353","doi":"10.1029/2025gl115872","title":"Tropical Cyclone Center Estimates Purely From FY‐3E WindRAD Measurements in the Dawn‐Dusk Orbit","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Bedford Institute of Oceanography; Fisheries and Oceans Canada","funders":"Canadian Space Agency; Dalhousie University; Natural Science Foundation of Zhejiang Province; China Meteorological Administration; National Natural Science Foundation of China","keywords":"Dusk; Tropical cyclone; Meteorology; Center (category theory); Environmental science; Climatology; Orbit (dynamics); Geodesy; Geology; Geography; Physics; Astronomy; Aerospace engineering","score_opus":0.06301977958564628,"score_gpt":0.32160975832481664,"score_spread":0.25858997873917033,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412739353","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99153966,0.00010017895,0.0059324666,0.000024486564,0.0000125054285,0.000011725779,0.0013102877,0.00019131388,0.0008773497],"genre_scores_gemma":[0.9956339,0.000038079044,0.0021445598,0.0000072983653,0.0000057649763,0.0000059941694,0.0020077447,0.00001617534,0.00014040242],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9997801,0.00004025048,0.00001771248,0.00007557409,0.00004712674,0.000039237693],"domain_scores_gemma":[0.9996562,0.00006974545,0.00008051773,0.000079016725,0.000080081234,0.000034428584],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00043671433,0.00044175246,0.0004687653,0.00079776277,0.00023384689,0.0006459561,0.00024132528,0.0002876047,0.00053672714],"category_scores_gemma":[0.0010828607,0.00029327915,0.00046942622,0.0006637157,0.00017245262,0.0005178146,0.00045169584,0.00028212307,0.00025526696],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004659236,0.00017343127,0.5066975,0.00009096855,0.00035685426,0.000115909424,0.00011930082,0.4290439,0.012762754,0.00047325855,0.0021922374,0.04750805],"study_design_scores_gemma":[0.000090660695,0.000069405854,0.43072703,0.00003501958,0.00007625708,0.000055777673,0.00011470427,0.5619747,0.0052809753,0.00022540122,0.0013006055,0.000049418828],"about_ca_topic_score_codex":0.063695796,"about_ca_topic_score_gemma":0.06218859,"teacher_disagreement_score":0.063695796,"about_ca_system_score_codex":0.00047202155,"about_ca_system_score_gemma":0.0008116768,"threshold_uncertainty_score":0.1266501},"labels":[],"label_agreement":null},{"id":"W4412748858","doi":"10.1029/2025gl117160","title":"Anomalous Vertical Structure of Tropospheric Ozone Due To Stratospheric Intrusions and Convective Transport","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Convection; Troposphere; Atmospheric sciences; Stratosphere; Environmental science; Ozone layer; Geology; Ozone; Climatology; Meteorology; Physics","score_opus":0.010915866720220399,"score_gpt":0.26309241750720463,"score_spread":0.25217655078698425,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4412748858","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9997292,0.000021173155,0.000071223185,0.000006280016,0.0000013486647,7.612743e-7,0.000050339717,0.000006449723,0.00011325876],"genre_scores_gemma":[0.9998703,0.000008036515,0.000029128698,0.0000016452087,0.0000017271592,5.1721764e-7,0.0000670207,6.9861113e-7,0.00002093654],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999486,0.0000048774577,0.0000036824779,0.000011893466,0.000011302423,0.000019560188],"domain_scores_gemma":[0.9997898,0.000026722693,0.000092503346,0.000019272651,0.000027817536,0.00004402224],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00012879423,0.00013799843,0.00012626094,0.0006495035,0.00020527958,0.00028507214,0.00013818173,0.00015971855,0.00034058793],"category_scores_gemma":[0.00024936063,0.00012738888,0.00014712197,0.00042377505,0.00022174596,0.00015459405,0.0002688471,0.00016258967,0.00004994162],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017745983,0.000040557497,0.88135666,0.000016737069,0.00009320066,0.00027636232,0.00024321876,0.0011785999,0.111530714,0.0001579047,0.00013495977,0.00479358],"study_design_scores_gemma":[0.0000018539669,0.000015467393,0.9975399,9.584072e-7,0.0000068614613,0.000035316894,0.00004342354,0.0012257878,0.0010506663,0.0000266313,0.000051128412,0.000001968314],"about_ca_topic_score_codex":0.007927907,"about_ca_topic_score_gemma":0.007688088,"teacher_disagreement_score":0.007927907,"about_ca_system_score_codex":0.0002779774,"about_ca_system_score_gemma":0.00014491448,"threshold_uncertainty_score":0.015763521},"labels":[],"label_agreement":null},{"id":"W4413214623","doi":"10.1029/2025gl115559","title":"Climate‐Dependent Hydrogen Isotopic Offset of Stem Water and Its Effect on Quantification of Plant Water Sources","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Plant Water Relations and Carbon Dynamics","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"National Key Research and Development Program of China; China Postdoctoral Science Foundation; National Natural Science Foundation of China","keywords":"Environmental science; Soil water; Precipitation; Loess plateau; Hydrology (agriculture); Stable isotope ratio; Water content; Atmospheric sciences; Soil science; Geology","score_opus":0.015770894831348355,"score_gpt":0.2600044865011368,"score_spread":0.24423359166978842,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413214623","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9971317,0.00008957573,0.0020791362,0.000008874149,0.000002488393,0.0000031958057,0.00015877066,0.000016026674,0.0005101602],"genre_scores_gemma":[0.9989355,0.000025967714,0.00083097315,0.000008563137,0.0000015446777,0.000004045688,0.00011806467,0.0000045807024,0.000070731236],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998115,0.000054070497,0.0000082387105,0.000063143,0.000044030752,0.000019184607],"domain_scores_gemma":[0.99963546,0.00014654237,0.00008466998,0.00003360771,0.0000752878,0.000024361269],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006000169,0.00018517983,0.0001727207,0.00047081657,0.0001808366,0.00028125456,0.00016923832,0.00013991183,0.0003543899],"category_scores_gemma":[0.0006057947,0.00013461948,0.00010165425,0.00051606516,0.00024402194,0.000323002,0.0002936902,0.00013485459,0.000053987966],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018330563,0.000018148521,0.8708742,0.000042459284,0.00008252727,0.00004335688,0.00018208411,0.0012783428,0.114580736,0.00011439599,0.000067397086,0.012533013],"study_design_scores_gemma":[0.000003675286,0.000027253775,0.9748103,0.000003225421,0.00002182274,0.000034463734,0.00008127633,0.006213401,0.018427348,0.000099043216,0.0002715968,0.000006636096],"about_ca_topic_score_codex":0.0032194164,"about_ca_topic_score_gemma":0.008222492,"teacher_disagreement_score":0.0032194164,"about_ca_system_score_codex":0.00014736192,"about_ca_system_score_gemma":0.00010239862,"threshold_uncertainty_score":0.00640136},"labels":[],"label_agreement":null},{"id":"W4413301550","doi":"10.1029/2025gl116833","title":"Threshold Domain Sizes for Multifractality in Sea Ice Deformation","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Horizon 2020 Framework Programme; Academy of Finland","keywords":"Geology; Sea ice; Domain (mathematical analysis); Geophysics; Climatology; Mathematics","score_opus":0.024841231373913874,"score_gpt":0.3036153494857689,"score_spread":0.27877411811185504,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413301550","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9791236,0.00008298451,0.019834105,0.00011555326,0.000005121103,0.000010190748,0.00008768196,0.00007142294,0.0006694423],"genre_scores_gemma":[0.9990619,0.0000060900857,0.0008745311,0.0000030179467,0.0000019929555,0.0000033112801,0.000024054252,0.0000046260375,0.000020490726],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.9997769,0.000056884346,0.000015076733,0.00004910841,0.00006391539,0.000038068672],"domain_scores_gemma":[0.9923793,0.0049336646,0.001216485,0.0006009889,0.00044867536,0.0004208958],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0009773611,0.00012432679,0.00015345993,0.00111396,0.00025568492,0.00066281395,0.00024670118,0.00025604086,0.00097467744],"category_scores_gemma":[0.0074517294,0.000116221396,0.00019726493,0.00028913247,0.0008596527,0.0006484514,0.0003662151,0.0004321865,0.000053252013],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0009795883,0.00043590623,0.29353192,0.00024569605,0.00015682995,0.000702089,0.0018572324,0.2556225,0.31855792,0.0681881,0.0020282737,0.057693936],"study_design_scores_gemma":[0.000026982885,0.00010782608,0.37831703,0.00002902504,0.000019235695,0.0002706484,0.00030793317,0.5759518,0.02438021,0.020051185,0.000470146,0.00006800169],"about_ca_topic_score_codex":0.0011758024,"about_ca_topic_score_gemma":0.00078741903,"teacher_disagreement_score":0.0011758024,"about_ca_system_score_codex":0.0004864946,"about_ca_system_score_gemma":0.00019992614,"threshold_uncertainty_score":0.005168855},"labels":[],"label_agreement":null},{"id":"W4413302705","doi":"10.1029/2025gl115936","title":"Windstorm Extremes in a Warmer World: Raising the Bar for Destruction","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos","funders":"Realdania","keywords":"Raising (metalworking); Bar (unit); Environmental science; Climatology; Meteorology; Geology; Geography; Engineering","score_opus":0.07898956996225495,"score_gpt":0.3378797625864459,"score_spread":0.258890192624191,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413302705","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9964587,0.00012562981,0.0008806279,0.0005753732,0.000021527374,0.000002359457,0.0001017845,0.00002520011,0.0018088613],"genre_scores_gemma":[0.9996153,0.00006190949,0.00017785888,0.000026624453,0.000008502166,8.777673e-7,0.000025062433,0.0000027484027,0.00008118803],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9999349,0.000024577426,0.000002846938,0.000013475953,0.000008354316,0.000015883066],"domain_scores_gemma":[0.9997969,0.00006270832,0.00006394294,0.000025277806,0.000017011193,0.00003400239],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019924088,0.00016041835,0.00021761724,0.00022350266,0.00024304831,0.0012869978,0.00016723348,0.00047628794,0.0014015243],"category_scores_gemma":[0.0010015144,0.00010748108,0.000254977,0.00024418646,0.00035930407,0.0010757897,0.00069471425,0.00044501646,0.00007912642],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00061413564,0.00027029778,0.6059866,0.00015262318,0.00046640175,0.00105026,0.0007037283,0.32947066,0.009284503,0.013512203,0.005487687,0.033000886],"study_design_scores_gemma":[0.000098972676,0.00020770023,0.62596506,0.00007134135,0.00015737327,0.0002447755,0.0028761548,0.34457886,0.002518401,0.017831767,0.0053756866,0.00007384418],"about_ca_topic_score_codex":0.006211677,"about_ca_topic_score_gemma":0.0062864902,"teacher_disagreement_score":0.006211677,"about_ca_system_score_codex":0.00023632727,"about_ca_system_score_gemma":0.00018105969,"threshold_uncertainty_score":0.012351036},"labels":[],"label_agreement":null},{"id":"W4413743681","doi":"10.1029/2024gl110661","title":"Tropical Cyclone Multi‐Level Wind‐Speed Structure Reconstruction From Sparse Dropsonde Data Via Adversarial Learning","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Fisheries and Oceans Canada","funders":"National Key Research and Development Program of China; Shanghai Jiao Tong University; National Natural Science Foundation of China","keywords":"Tropical cyclone; Dropsonde; Meteorology; Cyclone (programming language); Environmental science; Wind speed; Remote sensing; Computer science; Geology; Climatology; Geography","score_opus":0.07080107629921885,"score_gpt":0.315471643823963,"score_spread":0.24467056752474414,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413743681","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.35066715,0.00015757099,0.6454373,0.000559598,0.00004872773,0.00004182967,0.0002839635,0.00054105424,0.0022627036],"genre_scores_gemma":[0.98047537,0.000042003583,0.018342415,0.00006501518,0.000020135309,0.000018371667,0.00024222945,0.000019445139,0.00077502185],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99985874,0.000047062487,0.000006015599,0.000033420172,0.000029903927,0.000024833558],"domain_scores_gemma":[0.99900717,0.0006677899,0.00011021223,0.00008332604,0.000080086655,0.00005155755],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000654049,0.00050704874,0.00036022224,0.00025932977,0.00016215075,0.00037026533,0.00053478946,0.000464096,0.00061230536],"category_scores_gemma":[0.0023245201,0.00029791472,0.00034302994,0.00020354262,0.00056654756,0.00047386967,0.0006942979,0.0009794394,0.00010716199],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000023633882,0.000010114927,0.0009941822,0.0000065252157,0.000008359355,0.000018242168,0.000007677534,0.99251986,0.00053476845,0.00083512726,0.00020392021,0.0048375744],"study_design_scores_gemma":[9.5228836e-7,0.0000025214379,0.00007104464,5.531642e-7,4.6067137e-7,0.0000011555813,8.679454e-7,0.9995339,0.000106142885,0.0002642419,0.000017436923,5.880339e-7],"about_ca_topic_score_codex":0.0063353125,"about_ca_topic_score_gemma":0.0058584693,"teacher_disagreement_score":0.0063353125,"about_ca_system_score_codex":0.0004454706,"about_ca_system_score_gemma":0.00048539473,"threshold_uncertainty_score":0.012596905},"labels":[],"label_agreement":null},{"id":"W4413806573","doi":"10.1029/2025gl117200","title":"1.38 Ga Four‐Layer Tuff Marker Horizon in North China black Shales as a Chronostratigraphic Boundary for the Pre‐Ediacaran Geological Timescale","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Carleton University; University of Toronto","funders":"Chinese Academy of Geological Sciences; National Natural Science Foundation of China","keywords":"Geology; Geochronology; Craton; Horizon; Supercontinent; Sequence (biology); Phanerozoic; Paleontology; Volcano; Rodinia; Geochemistry; Tectonics; Cenozoic; Structural basin","score_opus":0.02451464154572818,"score_gpt":0.272710298731333,"score_spread":0.24819565718560482,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413806573","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.999124,0.000058482034,0.00009041494,0.0000070689375,0.0000016119175,0.0000019377203,0.00009784674,0.0000076905335,0.000610875],"genre_scores_gemma":[0.9993426,0.000032739328,0.0001267372,0.0000031363475,0.0000011848349,0.0000022295865,0.0001681445,0.0000020040088,0.00032114773],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999733,0.0000022559186,0.0000021089168,0.000009579608,0.000005140569,0.0000075415405],"domain_scores_gemma":[0.99990046,0.0000075754533,0.000033438526,0.000006972993,0.000035840585,0.000015606904],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000119508404,0.00014380636,0.00009033869,0.0011924186,0.0003838055,0.000279485,0.000125379,0.00013250248,0.0009929044],"category_scores_gemma":[0.00019287596,0.00008879689,0.00007974933,0.0006013391,0.00023575853,0.00015271721,0.00023074397,0.000086700646,0.00011244396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00017511567,0.000021745385,0.93194234,0.000046820656,0.000039337785,0.00049476477,0.0013019011,0.0012842063,0.041572664,0.00054405344,0.00022038937,0.022356553],"study_design_scores_gemma":[0.0000026271618,0.00001109618,0.9976693,0.0000059603744,0.000008678101,0.000053015425,0.00012687854,0.00063131854,0.0008354046,0.000033033564,0.0006208872,0.0000017199733],"about_ca_topic_score_codex":0.045697212,"about_ca_topic_score_gemma":0.0692604,"teacher_disagreement_score":0.045697212,"about_ca_system_score_codex":0.0006366143,"about_ca_system_score_gemma":0.00030207468,"threshold_uncertainty_score":0.09086245},"labels":[],"label_agreement":null},{"id":"W4413907501","doi":"10.1029/2025gl116170","title":"Earth Wind‐Driven Formation of Hematite on the Lunar Surface","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Macau University of Science and Technology; Fundo para o Desenvolvimento das Ciências e da Tecnologia; National Natural Science Foundation of China","keywords":"Astrobiology; Hematite; Earth (classical element); Geology; Earth surface; Geophysics; Earth science; Mineralogy; Physics; Astronomy","score_opus":0.035355486836596416,"score_gpt":0.29841711974899454,"score_spread":0.26306163291239815,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413907501","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9987268,0.00010990698,0.00041541582,0.000012155255,0.0000034292862,0.000004767362,0.0000899911,0.00001588948,0.0006215438],"genre_scores_gemma":[0.9989261,0.00004629935,0.00017006778,0.000009844998,0.0000010335121,0.00000296707,0.000104671555,0.000006424127,0.0007325911],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996746,0.0000040625782,8.320981e-7,0.000008253979,0.0000095183,0.000009872711],"domain_scores_gemma":[0.9999486,0.000013737868,0.0000097837265,0.0000044325175,0.000013913082,0.000009503736],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00007376319,0.0001464204,0.00011870079,0.00009814908,0.00012719953,0.00019930223,0.00011264753,0.00015078363,0.001499702],"category_scores_gemma":[0.00008379212,0.00007373359,0.000083646184,0.00007456953,0.00013978795,0.00008562815,0.00013740009,0.00018135342,0.00017274311],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015710124,0.000014851318,0.0020753813,0.00002170876,0.000005146368,0.00003006407,0.000019416228,0.0002069848,0.9962859,0.00004303622,0.00004423091,0.0010962375],"study_design_scores_gemma":[0.00002040188,0.00043295696,0.06615552,0.0000066090456,0.000011165371,0.00006926581,0.00014391723,0.0023057843,0.92948866,0.00010087827,0.0012578827,0.000006901699],"about_ca_topic_score_codex":0.0008591167,"about_ca_topic_score_gemma":0.0011622299,"teacher_disagreement_score":0.001499702,"about_ca_system_score_codex":0.00011824912,"about_ca_system_score_gemma":0.0000749658,"threshold_uncertainty_score":0.005017042},"labels":[],"label_agreement":null},{"id":"W4413956408","doi":"10.1029/2025gl116914","title":"Water Budgets Control the Resilience of Large‐Scale Ecological Restoration","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ecosystem dynamics and resilience","field":"Environmental Science","cited_by":7,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia, Okanagan Campus; Kelowna General Hospital","funders":"Fundamental Research Funds for the Central Universities; National Key Research and Development Program of China; National Forestry and Grassland Administration; National Natural Science Foundation of China","keywords":"Resilience (materials science); Environmental science; Scale (ratio); Restoration ecology; Ecology; Environmental resource management; Geography; Biology","score_opus":0.008204276357897795,"score_gpt":0.28014342886513355,"score_spread":0.27193915250723577,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413956408","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9932181,0.00009540303,0.001886172,0.00033591752,0.0000069254747,0.000009995849,0.00011025387,0.000038600094,0.0042986637],"genre_scores_gemma":[0.9998129,0.0000135811415,0.00005503731,0.000007139852,7.214179e-7,0.0000013932017,0.000011782184,0.0000017234124,0.00009571263],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999863,0.00002673987,0.00000695305,0.000026014492,0.000012372111,0.000064862455],"domain_scores_gemma":[0.9995807,0.00006336547,0.00012239246,0.000045382963,0.00006147581,0.00012671988],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00053570117,0.00019138548,0.00012958993,0.00052375847,0.00045937332,0.0007566531,0.00037562978,0.00021555179,0.0021335424],"category_scores_gemma":[0.0012800595,0.00011746032,0.0001905272,0.00035036894,0.00092504063,0.0010671513,0.0010171483,0.00022181787,0.00010263961],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00032857805,0.00016797306,0.6334938,0.00016577785,0.00027679524,0.0007205443,0.0012998836,0.19986053,0.0434906,0.048880257,0.0039088735,0.067406334],"study_design_scores_gemma":[0.000020588253,0.00014227955,0.7857799,0.00006411023,0.00006997753,0.00016121616,0.003169782,0.15674752,0.004505263,0.04022376,0.009064959,0.000050704875],"about_ca_topic_score_codex":0.014631981,"about_ca_topic_score_gemma":0.018352961,"teacher_disagreement_score":0.014631981,"about_ca_system_score_codex":0.001468912,"about_ca_system_score_gemma":0.0009425073,"threshold_uncertainty_score":0.029093623},"labels":[],"label_agreement":null},{"id":"W4413991276","doi":"10.1029/2025gl115773","title":"Lithospheric Structures of Marginal Sea Basins in and Around the Philippine Sea Plate Shaped by Eastward Mantle Flow","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Victoria","funders":"Nutrition Obesity Research Center, University of North Carolina","keywords":"Geology; Lithosphere; Mantle (geology); Heat flow; Seismology; Geophysics; Oceanography; Tectonics; Thermal; Meteorology","score_opus":0.016462482745516333,"score_gpt":0.2661167450585255,"score_spread":0.24965426231300916,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4413991276","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99960405,0.000032571512,0.000040573297,0.000010432027,4.2526042e-7,7.3812794e-7,0.000045417237,0.0000051095267,0.00026061866],"genre_scores_gemma":[0.9998754,0.000016485366,0.000025166975,0.0000017270197,5.712769e-7,6.6230996e-7,0.00004084972,0.0000012797735,0.000037758313],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999664,0.000005564193,0.0000024632677,0.000009148572,0.0000051466163,0.000011252838],"domain_scores_gemma":[0.9998697,0.000016500026,0.00004687729,0.000009546623,0.000027489334,0.000029828434],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008508639,0.00022849186,0.00013644452,0.00080963515,0.00026280474,0.00038348074,0.00014261872,0.00011638386,0.0010610032],"category_scores_gemma":[0.00028156792,0.00014821618,0.00015332273,0.00051935384,0.00033983839,0.00024070896,0.00044477894,0.00013235927,0.00010801804],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015158005,0.000015553047,0.9591624,0.000039739545,0.00007735332,0.00038880168,0.0017201432,0.0016330268,0.028444786,0.00025272247,0.00013753811,0.007976263],"study_design_scores_gemma":[0.000002069991,0.0000071892177,0.9985008,0.0000024468736,0.000007711963,0.000030833355,0.00034992857,0.00063703174,0.00032079555,0.00004073583,0.00009754113,0.0000030062122],"about_ca_topic_score_codex":0.014518145,"about_ca_topic_score_gemma":0.0149263535,"teacher_disagreement_score":0.014518145,"about_ca_system_score_codex":0.00020574436,"about_ca_system_score_gemma":0.00021360873,"threshold_uncertainty_score":0.028867245},"labels":[],"label_agreement":null},{"id":"W4414000571","doi":"10.1029/2025gl116416","title":"A Diachronic Assessment of Advances in Seasonal Forecasting: Evolution of the APCC Multi‐Model Ensemble Prediction System Over the Last Two Decades","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Korea Meteorological Administration; Rural Development Administration; Environment and Climate Change Canada; National Aeronautics and Space Administration","keywords":"Climatology; Environmental science; Meteorology; Geology; Geography","score_opus":0.03553021830839668,"score_gpt":0.3407611482241819,"score_spread":0.3052309299157852,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414000571","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.94980085,0.0050778408,0.025273247,0.0039550336,0.00042959373,0.000049089642,0.0035643147,0.00041537549,0.011434734],"genre_scores_gemma":[0.9868557,0.0008710601,0.009311404,0.00016611304,0.00008306139,0.000019448446,0.0022122639,0.00004810219,0.00043277896],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99875677,0.00039777913,0.00012514748,0.00026774823,0.00034886636,0.00010369788],"domain_scores_gemma":[0.9939666,0.0017884996,0.00087985286,0.0007991045,0.0021907224,0.00037517337],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.009048921,0.00045076138,0.00033912732,0.0010738514,0.00036375268,0.0017055505,0.0005854384,0.0006739955,0.00074852497],"category_scores_gemma":[0.013496422,0.00015868145,0.0003798255,0.0016254305,0.0003173572,0.0018518216,0.0012375296,0.0012226315,0.00019026795],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006648411,0.00026561128,0.46597123,0.0002738407,0.00063620775,0.0001848321,0.0005018671,0.27998015,0.0058758655,0.00814239,0.009297085,0.22820601],"study_design_scores_gemma":[0.000034415632,0.0003256386,0.2778464,0.00016411391,0.00016237186,0.00012013473,0.00038075206,0.6909162,0.005327644,0.0033718091,0.021257358,0.00009329106],"about_ca_topic_score_codex":0.0094183,"about_ca_topic_score_gemma":0.008337737,"teacher_disagreement_score":0.0094183,"about_ca_system_score_codex":0.00077356736,"about_ca_system_score_gemma":0.001100548,"threshold_uncertainty_score":0.047855854},"labels":[],"label_agreement":null},{"id":"W4414019882","doi":"10.1029/2025gl116477","title":"On the Spatial Relationship Between the Aurora and Relativistic Electron Precipitation During a Storm‐Time Substorm","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"Saint Petersburg State University","keywords":"Substorm; Electron precipitation; Storm; Precipitation; Geophysics; Geomagnetic storm; Atmospheric sciences; Physics; Electron; Geology; Meteorology; Magnetosphere; Solar wind; Plasma; Quantum mechanics","score_opus":0.016239286397160275,"score_gpt":0.2844787815471904,"score_spread":0.26823949515003015,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414019882","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990859,0.000037071062,0.00009802523,0.000016028527,0.0000019005096,0.0000017989407,0.00018244961,0.0000040374157,0.00057278253],"genre_scores_gemma":[0.999637,0.000018324507,0.00005889724,0.0000026421724,0.000004834469,0.0000014962353,0.00019250998,0.0000013304772,0.000082873594],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999114,0.000017196164,0.0000070332644,0.000023499799,0.000013199752,0.000027594442],"domain_scores_gemma":[0.9991842,0.00024039182,0.00030785543,0.00004618644,0.0001335468,0.00008782661],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020063002,0.00007951825,0.000116990384,0.0007996838,0.0003404503,0.00045287327,0.00012435549,0.00011949404,0.0011758897],"category_scores_gemma":[0.0009074446,0.0000547756,0.00010734117,0.0007753958,0.00022005868,0.00019070986,0.00037495664,0.00012127596,0.00014334527],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00005410931,0.000009023423,0.9951971,0.000005404441,0.000020567704,0.00007814206,0.0001961539,0.00018610181,0.0019036127,0.000087226086,0.00009755274,0.0021650926],"study_design_scores_gemma":[8.5787536e-7,0.000007649113,0.99927574,0.0000018211848,0.000004817013,0.000028729171,0.00017636183,0.00024289935,0.000094444265,0.000013106667,0.00015272762,8.3662127e-7],"about_ca_topic_score_codex":0.013180469,"about_ca_topic_score_gemma":0.021750739,"teacher_disagreement_score":0.013180469,"about_ca_system_score_codex":0.00019363237,"about_ca_system_score_gemma":0.0001689961,"threshold_uncertainty_score":0.026207507},"labels":[],"label_agreement":null},{"id":"W4414139992","doi":"10.1029/2025gl117794","title":"Increasing Contribution of Condensable Particulate Matter From Stationary Combustion Sources Under Strict Control Standards in China","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Ministry of Science and Technology of the People's Republic of China; National Natural Science Foundation of China","keywords":"Particulates; Combustion; Emission standard; Air pollution; Major stationary source; Coal combustion products; Pollution; Emission inventory","score_opus":0.011287137322493276,"score_gpt":0.2740767828374068,"score_spread":0.2627896455149135,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414139992","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99782604,0.0001322931,0.0008858308,0.00003203344,0.000004160483,0.000012281985,0.00041386587,0.00001833646,0.00067515566],"genre_scores_gemma":[0.998353,0.00013261984,0.0004144977,0.000021436605,0.00000696258,0.000007727186,0.00073529023,0.0000040293744,0.0003244386],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99956626,0.000039361246,0.000036925267,0.000096878306,0.00019031398,0.00007023462],"domain_scores_gemma":[0.9994578,0.00004683515,0.00013885718,0.000035081517,0.00028888122,0.000032531603],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0006712241,0.00048809737,0.00026203037,0.0018038636,0.0003886757,0.0007266783,0.00030257364,0.00024870152,0.0004971474],"category_scores_gemma":[0.00045879764,0.00017022117,0.00039755044,0.0019583036,0.00024927958,0.00050225126,0.0004779791,0.00016989817,0.00008328762],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000148174,0.00006345588,0.9206383,0.00019618939,0.00018881011,0.00043571266,0.00042940964,0.007923057,0.031958405,0.00052724907,0.0005340884,0.036957145],"study_design_scores_gemma":[0.0000049899622,0.00005572014,0.98418856,0.000010539076,0.000049574162,0.00004969989,0.00018985568,0.007657743,0.0063733975,0.00013068515,0.0012760167,0.000013234668],"about_ca_topic_score_codex":0.063888505,"about_ca_topic_score_gemma":0.06683333,"teacher_disagreement_score":0.063888505,"about_ca_system_score_codex":0.0012214826,"about_ca_system_score_gemma":0.000986997,"threshold_uncertainty_score":0.12703323},"labels":[],"label_agreement":null},{"id":"W4414181794","doi":"10.1029/2024gl113940","title":"Yucatan Hurricane Activity Highlights Common Era Tropical Cyclone Dipole","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McMaster University","funders":"University of Texas at Austin; Geological Society of America; National Centers for Environmental Information; National Science Foundation","keywords":"Intertropical Convergence Zone; Tropical cyclone; Yucatan peninsula; Atlantic hurricane; Latitude; Proxy (statistics); Northern Hemisphere; Climate change","score_opus":0.025052307221447176,"score_gpt":0.3103152094032489,"score_spread":0.2852629021818017,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414181794","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9877913,0.00033293024,0.00043623056,0.00006690093,0.000010321358,0.0000040313153,0.005623264,0.00007642768,0.0056585646],"genre_scores_gemma":[0.99500495,0.00020248196,0.00032235603,0.00001316498,0.0000051108495,0.0000032633193,0.003797996,0.000017497476,0.00063316873],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995863,0.0000052457467,0.0000049252494,0.000014207687,0.0000075646963,0.000009562982],"domain_scores_gemma":[0.9997129,0.000045878907,0.000074620606,0.000031399504,0.00010712726,0.000028078293],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008605676,0.00009376834,0.00007629518,0.0009894619,0.0001938572,0.00067575334,0.00008624868,0.00008457271,0.002622446],"category_scores_gemma":[0.00043778846,0.00007513327,0.00007725919,0.0012792776,0.00014500211,0.00027749204,0.00046084743,0.00013977861,0.00029073906],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000067795125,0.000009045015,0.9603605,0.00008462325,0.00007278511,0.00016351929,0.0005652539,0.0033467596,0.003946953,0.0004491055,0.0034681025,0.027465675],"study_design_scores_gemma":[0.0000015944238,0.000002941518,0.9946784,0.000014745159,0.0000068416743,0.000050893486,0.00027800695,0.0012778164,0.00034020393,0.00006102816,0.0032838394,0.000003713466],"about_ca_topic_score_codex":0.07722365,"about_ca_topic_score_gemma":0.21440889,"teacher_disagreement_score":0.07722365,"about_ca_system_score_codex":0.0003613483,"about_ca_system_score_gemma":0.00033725429,"threshold_uncertainty_score":0.15354836},"labels":[],"label_agreement":null},{"id":"W4414279840","doi":"10.1029/2025gl119254","title":"Four-dimensional generalization of ensemble singular vector: Formulation and experiments with the Lorenz 96 model","year":2025,"lang":"en","type":"preprint","venue":"Geophysical Research Letters","topic":"Control Systems and Identification","field":"Engineering","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Japan Society for the Promotion of Science; National Central University; Research Organization of Information and Systems","keywords":"Generalization; Sensitivity (control systems); Measure (data warehouse); Singular value; Simple (philosophy)","score_opus":0.042707243687067985,"score_gpt":0.29660465164309785,"score_spread":0.2538974079560299,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414279840","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.86623824,0.0002724537,0.12601969,0.00047660046,0.0000960447,0.000052997337,0.00022979428,0.00045293148,0.0061612194],"genre_scores_gemma":[0.99209493,0.00004984642,0.007184857,0.000018815155,0.000009745398,0.000013940772,0.00008308938,0.000019642774,0.00052511215],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999635,0.00019561616,0.000016931548,0.00003950679,0.000084416206,0.000028605185],"domain_scores_gemma":[0.99873954,0.0007001272,0.000102581085,0.00020660364,0.00017040403,0.0000807047],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0012160989,0.0005091082,0.00053843885,0.00041219767,0.00029855475,0.00059786875,0.0004028161,0.00050377235,0.00081545423],"category_scores_gemma":[0.002623107,0.00014129732,0.00042421682,0.00031432317,0.0005432144,0.00082513015,0.0008083555,0.0010184054,0.000088036315],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00015232936,0.00010127118,0.001219115,0.000041778425,0.00005475715,0.000080246056,0.00006811408,0.9726273,0.005435891,0.008430135,0.00069097144,0.011098062],"study_design_scores_gemma":[0.0000037635343,0.00002990417,0.00015437533,0.0000010475725,0.00000181672,0.0000051813636,0.0000062845834,0.99769515,0.00060675264,0.0014038143,0.00008661662,0.0000052613022],"about_ca_topic_score_codex":0.00739075,"about_ca_topic_score_gemma":0.0028681227,"teacher_disagreement_score":0.00739075,"about_ca_system_score_codex":0.00038946778,"about_ca_system_score_gemma":0.00032573257,"threshold_uncertainty_score":0.014695466},"labels":[],"label_agreement":null},{"id":"W4414308843","doi":"10.1029/2025gl115839","title":"Influence of Large‐Scale Teleconnection Patterns on Hailstorm Severity in Alberta","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Environment and Climate Change Canada; Western University","funders":"Natural Sciences and Engineering Research Council of Canada; Institute for Catastrophic Loss Reduction","keywords":"Teleconnection; Arctic; Intensity (physics); The arctic; Climate change","score_opus":0.022298165994522015,"score_gpt":0.29485329108370323,"score_spread":0.2725551250891812,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414308843","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9985103,0.00004273828,0.00011616726,0.000049951293,0.0000023128919,0.0000033118831,0.00043186962,0.000008405383,0.00083501596],"genre_scores_gemma":[0.99929845,0.000034459223,0.00007749185,0.000010233486,8.9776626e-7,0.0000013883821,0.00028317486,0.000001842914,0.0002919847],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998566,0.000017878787,0.0000063044126,0.000024487583,0.00004213374,0.000052605887],"domain_scores_gemma":[0.9994821,0.00008506926,0.00008882364,0.000020357904,0.00021443512,0.0001092959],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00026453933,0.0001947004,0.00011206054,0.0005961143,0.00043636205,0.0007354249,0.00031720652,0.0001229805,0.00090935914],"category_scores_gemma":[0.0009194879,0.000081622784,0.0001544102,0.00088755967,0.00036146372,0.00015768611,0.00038285795,0.00018681177,0.00005245402],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0001367636,0.000030241232,0.98335004,0.00001065899,0.00005479067,0.00011936483,0.0002525568,0.0057078116,0.0024832718,0.00021817278,0.00054250535,0.007093829],"study_design_scores_gemma":[0.0000042680517,0.000007148944,0.9947299,0.0000034347427,0.000010485033,0.000012396842,0.00041158838,0.004129545,0.00020677607,0.00003550544,0.0004438252,0.000005095534],"about_ca_topic_score_codex":0.95940155,"about_ca_topic_score_gemma":0.97451186,"teacher_disagreement_score":0.040598452,"about_ca_system_score_codex":0.006319591,"about_ca_system_score_gemma":0.0051151947,"threshold_uncertainty_score":0.08167505},"labels":[],"label_agreement":null},{"id":"W4414361680","doi":"10.1029/2025gl116984","title":"Representing the Teleconnection Between the Jet Stream and Extreme Cold Air Outbreaks Over North America","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"EIT Climate-KIC; RES’EAU-WaterNET; European Commission; Natural Sciences and Engineering Research Council of Canada; Horizon 2020 Framework Programme; Vetenskapsrådet; Natural Environment Research Council","keywords":"Jet stream; Teleconnection; Jet (fluid); Atmospheric circulation; Extreme weather; STREAMS; Extreme value theory; Climate model","score_opus":0.04014775599240811,"score_gpt":0.3015987694629612,"score_spread":0.2614510134705531,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414361680","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99800354,0.000028766435,0.0014003767,0.00003747513,0.0000034712098,0.0000034181337,0.00018917801,0.00003115116,0.00030271293],"genre_scores_gemma":[0.99837494,0.00002173263,0.0013063308,0.000005187496,0.000004512342,0.0000036575598,0.00020873982,0.000003889451,0.00007093073],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.999944,0.00001713285,0.000003696979,0.000015037463,0.000008433465,0.000011695059],"domain_scores_gemma":[0.99960035,0.00020308196,0.00009919035,0.00002356604,0.00004310915,0.000030798175],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019818213,0.00013548616,0.00011351547,0.0006713044,0.00018496631,0.0005319516,0.00014542956,0.00015425625,0.0006177939],"category_scores_gemma":[0.0010352969,0.00008558709,0.0001484473,0.0007368111,0.00018031782,0.0003434637,0.00027801876,0.00018641354,0.000037187452],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00046020746,0.000112586014,0.748784,0.000053649503,0.00022775622,0.00034689234,0.00054229674,0.17501752,0.016775867,0.000896816,0.0011215542,0.055660766],"study_design_scores_gemma":[0.000018308167,0.000035311965,0.73740566,0.0000088930565,0.000034803383,0.00004287353,0.00045323503,0.25984204,0.0010783991,0.00056475843,0.0005028889,0.000012805414],"about_ca_topic_score_codex":0.033135675,"about_ca_topic_score_gemma":0.0665859,"teacher_disagreement_score":0.033135675,"about_ca_system_score_codex":0.00035046798,"about_ca_system_score_gemma":0.0002801351,"threshold_uncertainty_score":0.0658856},"labels":[],"label_agreement":null},{"id":"W4414402763","doi":"10.1029/2025gl117126","title":"Interplay of Loading and Adsorption Controls Elastic Deformation of Clastic and Crystalline Rocks","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Hydraulic Fracturing and Reservoir Analysis","field":"Engineering","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Western University","funders":"Ministry of Business, Innovation and Employment; National Natural Science Foundation of China; China Coal Technology Engineering Group","keywords":"Softening; Stiffening; Stiffness; Moisture; Elasticity (physics); Adsorption; Overburden; Elastic modulus","score_opus":0.008570142882022097,"score_gpt":0.27229036140381585,"score_spread":0.2637202185217937,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414402763","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99967074,0.000015094279,0.00008201426,0.000004146844,4.906888e-7,0.0000015651867,0.000029249333,0.0000047286862,0.00019198222],"genre_scores_gemma":[0.9998673,0.00000878304,0.00003476358,0.0000024797646,4.030442e-7,0.0000013508024,0.000019767192,0.0000016045766,0.00006366747],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.99987686,0.000009838545,0.0000075318576,0.000023888308,0.000035820365,0.000045982106],"domain_scores_gemma":[0.9998505,0.00004273414,0.000033514498,0.000015137058,0.000024465166,0.000033688564],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008676243,0.00013220249,0.00017043036,0.0002539149,0.00021268385,0.00034828088,0.00017579872,0.00016971957,0.0012175947],"category_scores_gemma":[0.0003046833,0.00018120078,0.00009365244,0.00017112485,0.00042193494,0.00020333196,0.00030875226,0.00014404819,0.00011772909],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014287616,0.000022714818,0.010331262,0.000023536568,0.000008977311,0.000039549966,0.000060305054,0.00050341256,0.98702013,0.000043291442,0.000018957904,0.0017851338],"study_design_scores_gemma":[0.000014951802,0.0002166276,0.47470242,0.000004509031,0.000016028984,0.00013267291,0.00038542785,0.011553869,0.5124543,0.00013043589,0.00036859422,0.000020189525],"about_ca_topic_score_codex":0.0029750466,"about_ca_topic_score_gemma":0.0048578344,"teacher_disagreement_score":0.0029750466,"about_ca_system_score_codex":0.00022605837,"about_ca_system_score_gemma":0.00018523457,"threshold_uncertainty_score":0.005915463},"labels":[],"label_agreement":null},{"id":"W4414561433","doi":"10.1029/2025gl114672","title":"Characterizing the Interannual Variability of North Atlantic Subpolar Overturning","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":8,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Bedford Institute of Oceanography; Memorial University of Newfoundland; Fisheries and Oceans Canada","funders":"National Science Foundation","keywords":"Boundary current; Thermohaline circulation; Structural basin; North Atlantic Deep Water; Zonal and meridional; Atlantic hurricane; Shutdown of thermohaline circulation; General Circulation Model","score_opus":0.03279754585974636,"score_gpt":0.28897703278974485,"score_spread":0.2561794869299985,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414561433","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982998,0.00003333527,0.00048169162,0.000022414011,0.0000042282413,0.0000019838944,0.0006128696,0.000026965336,0.0005167021],"genre_scores_gemma":[0.998887,0.000019543279,0.00015345732,0.0000044312715,0.000003967763,0.0000016961118,0.0008151778,0.000004493557,0.00011029918],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999548,0.0000068959894,0.000003069898,0.000015073922,0.000008485682,0.00001168386],"domain_scores_gemma":[0.99980456,0.00004492268,0.000059831113,0.000023259929,0.000037741127,0.00002962626],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020530482,0.00012624793,0.00011857996,0.00049624377,0.00008447543,0.00032611354,0.00012052592,0.000110396526,0.00068217446],"category_scores_gemma":[0.00047855012,0.000063565516,0.00013139489,0.00039790096,0.00008265702,0.00018164796,0.00017062173,0.00013971918,0.00011683085],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00011064952,0.000058762882,0.9452414,0.00002041171,0.00012342044,0.00006394388,0.00008100697,0.02338837,0.009365152,0.0002891481,0.00094789383,0.020309875],"study_design_scores_gemma":[0.000003816969,0.000014230723,0.96809274,0.0000035993635,0.000011583086,0.000012884828,0.000031788382,0.030369548,0.00086775736,0.00007139254,0.0005157092,0.0000049133982],"about_ca_topic_score_codex":0.014712858,"about_ca_topic_score_gemma":0.020825613,"teacher_disagreement_score":0.014712858,"about_ca_system_score_codex":0.0001821652,"about_ca_system_score_gemma":0.00014871903,"threshold_uncertainty_score":0.029254436},"labels":[],"label_agreement":null},{"id":"W4414593292","doi":"10.1029/2025gl119595","title":"Bayesian Estimates of Ice Optical Properties for Lake Ice Modeling","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Arctic and Antarctic ice dynamics","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Trent University; York University","funders":"Canadian Union of Public Employees, Local 3903; Ministero dell'Università e della Ricerca; Limnological Institute, Siberian Branch of Russian Academy of Science; Svenska Forskningsrådet Formas; Global Institute for Water Security, University of Saskatchewan; Dipartimenti di Eccellenza; Kungl. Skogs- och Lantbruksakademien; University of Saskatchewan; Vetenskapsrådet; Siberian Branch, Russian Academy of Sciences; National Science Foundation; Natural Sciences and Engineering Research Council of Canada; National Academy of Sciences of Armenia","keywords":"Snow cover; Snow; Sea ice; Irradiance; Cryosphere; Energy budget; Thermal; Arctic ice pack","score_opus":0.03796897792979919,"score_gpt":0.2928630108960901,"score_spread":0.25489403296629093,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414593292","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.42257544,0.00030957352,0.5740131,0.00020408639,0.0000121961875,0.00007073596,0.0010840627,0.00038757094,0.0013432507],"genre_scores_gemma":[0.91743577,0.00012674878,0.07998621,0.000053164942,0.00002681623,0.00012730408,0.0016870877,0.00008497419,0.0004718986],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9993438,0.0003688188,0.000041866424,0.00012607854,0.000069726855,0.000049727325],"domain_scores_gemma":[0.99625164,0.002623883,0.00049124693,0.0002135717,0.00032521476,0.00009457233],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0032571754,0.0005016558,0.0006202349,0.0013735913,0.00047551538,0.0010417044,0.0008984058,0.0005380648,0.0012363708],"category_scores_gemma":[0.013718056,0.0009104299,0.00079330447,0.0008480476,0.0005381089,0.0013221671,0.00095832424,0.00094218715,0.00027083347],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000059854294,0.000053417578,0.027749294,0.000026545775,0.00012133848,0.000023145114,0.000100258025,0.9454405,0.0011956398,0.0049950485,0.00045443323,0.019780459],"study_design_scores_gemma":[0.000007136107,0.0000058605656,0.0041384976,0.000010248277,0.00000689943,0.0000050248736,0.000010389254,0.9905281,0.00017174744,0.0049311086,0.0001745208,0.000010443792],"about_ca_topic_score_codex":0.017693957,"about_ca_topic_score_gemma":0.016785765,"teacher_disagreement_score":0.017693957,"about_ca_system_score_codex":0.0010268614,"about_ca_system_score_gemma":0.00095557445,"threshold_uncertainty_score":0.03518194},"labels":[],"label_agreement":null},{"id":"W4414661319","doi":"10.1029/2025gl116714","title":"The Remarkable 2024 North Atlantic Mid‐Season Hurricane Lull","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Tropical and Extratropical Cyclones Research","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Ouranos","funders":"Biological and Environmental Research; National Oceanic and Atmospheric Administration; G. Unger Vetlesen Foundation; U.S. Department of Energy; Office of Science; National Science Foundation","keywords":"Atlantic hurricane; Tropical cyclone; Tropical wave; Storm; Tropical Atlantic; Latitude; Tropical cyclone scales; Tropical cyclone rainfall forecasting","score_opus":0.021017213845929868,"score_gpt":0.28424252175083825,"score_spread":0.2632253079049084,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414661319","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9222498,0.0011825955,0.0005284402,0.010681762,0.0012992546,0.00002859891,0.0036939501,0.00021311776,0.06012245],"genre_scores_gemma":[0.98857063,0.0002900086,0.00013074181,0.0014843894,0.00047925772,0.000010594989,0.0021086473,0.000017667724,0.0069079027],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999074,0.000008269162,0.0000050993776,0.000011590693,0.000038080718,0.000029624221],"domain_scores_gemma":[0.999801,0.000013595195,0.000050898547,0.000011137569,0.000075675474,0.00004777474],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00017435754,0.00014165157,0.000110177054,0.0002486842,0.0005954005,0.0006829974,0.00010802411,0.0003168094,0.0034462842],"category_scores_gemma":[0.00039493162,0.0000588626,0.00006941803,0.00019281675,0.00015882147,0.00025098308,0.00045393824,0.0004807956,0.0008744981],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008989257,0.00013115528,0.6218749,0.00018643038,0.00012459107,0.0032673855,0.001467789,0.0017419358,0.028741354,0.0027554398,0.2409024,0.09790771],"study_design_scores_gemma":[0.00002129438,0.00010100081,0.88199997,0.000035867863,0.000019591651,0.00043412266,0.0016598534,0.0016284771,0.0020355626,0.00041088663,0.11163144,0.000021837315],"about_ca_topic_score_codex":0.021840157,"about_ca_topic_score_gemma":0.080083966,"teacher_disagreement_score":0.021840157,"about_ca_system_score_codex":0.00079314876,"about_ca_system_score_gemma":0.00038126917,"threshold_uncertainty_score":0.043426037},"labels":[],"label_agreement":null},{"id":"W4414768015","doi":"10.1029/2025gl119220","title":"Formation and Arrest of a Surface Density Front via Strain‐Driven Frontogenesis","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"High-pressure geophysics and materials","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"Natural Sciences and Engineering Research Council of Canada; University of Toronto","keywords":"Frontogenesis; Front (military); Mixed layer; Layer (electronics); Surface (topology); Biogeochemical cycle","score_opus":0.021344891904081016,"score_gpt":0.2699559622696808,"score_spread":0.24861107036559982,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414768015","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968335,0.000011410752,0.0013601474,0.00004136985,0.000007180287,0.000011106441,0.000048662732,0.000042105657,0.0016446715],"genre_scores_gemma":[0.99947697,0.0000076036285,0.00025112662,0.0000066549446,0.0000015389098,0.0000036279223,0.000024409286,0.0000052792107,0.00022277566],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9999528,0.0000073595693,0.0000020120672,0.0000051669654,0.0000074593854,0.000025121106],"domain_scores_gemma":[0.9998323,0.000037175505,0.000030055466,0.000015578404,0.000019263583,0.000065553206],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015910885,0.0002537893,0.00023163606,0.00026513828,0.0004021667,0.0007782043,0.00033579898,0.00031466407,0.0016426313],"category_scores_gemma":[0.0006368676,0.0001794205,0.00036474285,0.00010067981,0.0005783723,0.00032497203,0.00043934744,0.00042386254,0.00010256006],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000559353,0.00029451604,0.034456037,0.000048718557,0.000084022526,0.00060355384,0.00024143132,0.9020151,0.048736133,0.007112826,0.00068161235,0.0051666955],"study_design_scores_gemma":[0.00007648265,0.00007773028,0.00685912,0.000004614178,0.000010864069,0.000021945647,0.000048331625,0.98977613,0.0024043312,0.00052196416,0.00019046999,0.000008021563],"about_ca_topic_score_codex":0.014691287,"about_ca_topic_score_gemma":0.006523884,"teacher_disagreement_score":0.014691287,"about_ca_system_score_codex":0.00080360944,"about_ca_system_score_gemma":0.00068074086,"threshold_uncertainty_score":0.02921158},"labels":[],"label_agreement":null},{"id":"W4414824737","doi":"10.1029/2025gl115332","title":"Ice Sheets Without Dynamic Topography","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Cryospheric studies and observations","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Discovery Eye Foundation","keywords":"Ice sheet; Ice divide; Antarctic ice sheet; Ice shelf; Ice stream; Antarctic sea ice; Dynamic equilibrium; Ice-sheet model; Ocean surface topography","score_opus":0.02677337383483638,"score_gpt":0.3079516602177099,"score_spread":0.28117828638287357,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414824737","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99530053,0.000056411187,0.0015515407,0.000058446218,0.000015821972,0.0000072074977,0.0006446604,0.000041559357,0.0023238482],"genre_scores_gemma":[0.9982705,0.000056117053,0.0005816471,0.000024759307,0.000007327763,0.000006465347,0.0006675967,0.000016678636,0.00036881448],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9998529,0.0000256545,0.000008588773,0.000045484943,0.000020048228,0.000047392576],"domain_scores_gemma":[0.99978644,0.00003927942,0.000038391845,0.00005602423,0.00004075538,0.000039156075],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00015353442,0.00045367132,0.00059863256,0.00027243627,0.00029104494,0.0008696085,0.00046425776,0.00028798607,0.002158346],"category_scores_gemma":[0.00060869433,0.00028131114,0.0007176084,0.00039025026,0.0006502873,0.0006817475,0.0003317641,0.0002891821,0.0001694135],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00016499971,0.00007075783,0.046708956,0.00004586677,0.0002578846,0.00013075101,0.000032055214,0.9413963,0.005450285,0.002324233,0.0004374637,0.0029805347],"study_design_scores_gemma":[0.00022201726,0.00018595917,0.12964445,0.000027525335,0.00024848088,0.00013474339,0.00016947366,0.8578424,0.0028187432,0.0058369525,0.0028190336,0.00005028558],"about_ca_topic_score_codex":0.048150577,"about_ca_topic_score_gemma":0.03450154,"teacher_disagreement_score":0.048150577,"about_ca_system_score_codex":0.0007703585,"about_ca_system_score_gemma":0.0008623727,"threshold_uncertainty_score":0.09574062},"labels":[],"label_agreement":null},{"id":"W4414842024","doi":"10.1029/2025gl116647","title":"Seismic Evidence for Widespread Active Magmatism in Eastern Marie Byrd Land, Antarctica","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geological and Geochemical Analysis","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"National Science Foundation","keywords":"Volcano; Induced seismicity; Magmatism; Tectonics; Mount; Volcanology; Antarctic ice sheet","score_opus":0.05544028778178037,"score_gpt":0.3259787980605443,"score_spread":0.27053851027876397,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414842024","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99588,0.00035004126,0.000042971078,0.00010548221,0.000008597928,0.000009356527,0.00064809655,0.000009352976,0.0029461351],"genre_scores_gemma":[0.9981852,0.00030257466,0.00013380664,0.000047084282,0.00002038974,0.000008944887,0.0006647571,0.0000043979826,0.000632841],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998648,0.00001917579,0.000010939965,0.000019601683,0.000039871404,0.000045507524],"domain_scores_gemma":[0.99945444,0.00005164496,0.0002336944,0.000060487142,0.00008862438,0.00011119221],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00024175938,0.0003065191,0.0002191324,0.0018648666,0.00087407365,0.0006606297,0.00032424816,0.00037590237,0.0014641687],"category_scores_gemma":[0.0004899835,0.00017146181,0.00020459565,0.0018213132,0.0005485506,0.00027731038,0.000902899,0.00018543816,0.0004113386],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00012809,0.000017790124,0.97187096,0.0000948419,0.000056692934,0.0012618396,0.002173645,0.00019482689,0.014820356,0.000082038445,0.0010527491,0.008246186],"study_design_scores_gemma":[0.000002805306,0.000015357864,0.99700576,0.000013797576,0.000009899012,0.00018505708,0.0005952617,0.000052756055,0.00021345227,0.0000103639395,0.0018931555,0.000002377635],"about_ca_topic_score_codex":0.07943157,"about_ca_topic_score_gemma":0.1685116,"teacher_disagreement_score":0.07943157,"about_ca_system_score_codex":0.0007366819,"about_ca_system_score_gemma":0.0007357611,"threshold_uncertainty_score":0.15793842},"labels":[],"label_agreement":null},{"id":"W4414950457","doi":"10.1029/2025gl117477","title":"Reducing Uncertainty in Climate Projections for the Mid and High Latitudes of the Northern Hemisphere","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Northern Hemisphere; Latitude; Precipitation; Climate model; Arctic; Global warming; Climate change; Climate extremes; Sea ice; Temperate climate","score_opus":0.032029388607093166,"score_gpt":0.3172371991497109,"score_spread":0.28520781054261773,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414950457","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.81030303,0.0003884755,0.17527913,0.0013291982,0.00008136667,0.00005011053,0.0018999219,0.00034502448,0.010323773],"genre_scores_gemma":[0.98339313,0.00006300957,0.015592395,0.00006478091,0.00002656231,0.00002014195,0.0004991625,0.000026370357,0.0003143636],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9991653,0.0005405677,0.00002811279,0.00011429458,0.00009184834,0.00005992598],"domain_scores_gemma":[0.997468,0.0015683597,0.0003321996,0.00026295445,0.00027000447,0.00009849147],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.002602132,0.00050212414,0.00045119022,0.0005466583,0.00039558197,0.0012627394,0.0005651725,0.00053290953,0.0014543649],"category_scores_gemma":[0.0072636097,0.00028112612,0.00059938815,0.00067697,0.00031161957,0.000879659,0.0011543933,0.00083516346,0.00011448042],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00006691386,0.000025806892,0.0045362148,0.000021573966,0.00009544286,0.000036581212,0.000032533673,0.97951335,0.00046591565,0.0029375898,0.000652982,0.011615052],"study_design_scores_gemma":[0.000026947802,0.000033623357,0.0060062916,0.000018089622,0.00004197516,0.000014277027,0.000054411037,0.98169094,0.0007070722,0.0104329465,0.0009510841,0.000022410548],"about_ca_topic_score_codex":0.017560191,"about_ca_topic_score_gemma":0.01779131,"teacher_disagreement_score":0.017560191,"about_ca_system_score_codex":0.0006147244,"about_ca_system_score_gemma":0.0013260735,"threshold_uncertainty_score":0.034915924},"labels":[],"label_agreement":null},{"id":"W4414950498","doi":"10.1029/2025gl118344","title":"Large Carbon Losses From Burned Permafrost Peatlands During Post‐Fire Succession","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Peatlands and Wetlands Ecology","field":"Environmental Science","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Geological Survey of Canada; McGill University; University of British Columbia; Wildlife Conservation Society Canada; Center for Northern Studies; Government of Alberta; Université de Montréal; University of Alberta","funders":"Global Water Futures; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Government of Canada","keywords":"Permafrost; Peat; Boreal; Carbon sink; Thermokarst; Sink (geography); Eddy covariance; Taiga; Carbon dioxide","score_opus":0.011288574035842765,"score_gpt":0.2862487051265278,"score_spread":0.274960131090685,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414950498","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99953926,0.000042307485,0.000060032853,0.000006725089,8.770604e-7,0.0000014556555,0.00014104755,0.0000044372655,0.00020390362],"genre_scores_gemma":[0.9996201,0.000021073409,0.00005721036,0.000004497781,8.410574e-7,0.0000018085747,0.00015783188,0.000001361725,0.00013524081],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999218,0.0000058895002,0.0000040401233,0.00001744121,0.00002170242,0.000029082787],"domain_scores_gemma":[0.999767,0.00002482065,0.00007773816,0.000015802323,0.00006238828,0.000052391602],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00019700086,0.00020721937,0.0001645726,0.0004245674,0.00056911947,0.0005128999,0.00026597784,0.00025787065,0.00056107214],"category_scores_gemma":[0.00042277298,0.00010927617,0.00014943717,0.000347418,0.00032854822,0.0002457628,0.00021971087,0.00019653125,0.000092258495],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0004901376,0.000044573222,0.9623485,0.000030966115,0.0000735729,0.00032516045,0.00031362302,0.0017859155,0.02539319,0.000057296555,0.00014162464,0.008995413],"study_design_scores_gemma":[8.943212e-7,0.000008498194,0.9987872,0.0000014696486,0.0000032096284,0.000040824412,0.000066424764,0.0003399354,0.00065414247,0.000010694732,0.00008525108,0.0000015197212],"about_ca_topic_score_codex":0.15769903,"about_ca_topic_score_gemma":0.2986632,"teacher_disagreement_score":0.15769903,"about_ca_system_score_codex":0.0014845359,"about_ca_system_score_gemma":0.0005814354,"threshold_uncertainty_score":0.31356227},"labels":[],"label_agreement":null},{"id":"W4414950542","doi":"10.1029/2025gl117454","title":"How Ice Composition Controls Radiatively Driven Convection Under Lake Ice","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of British Columbia","funders":"Wisconsin Alumni Research Foundation","keywords":"Convection; Water column; Radiative forcing; Stratification (seeds); Forcing (mathematics); Attenuation; Sea ice growth processes","score_opus":0.02283828401750862,"score_gpt":0.27486056670096515,"score_spread":0.2520222826834565,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414950542","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99925464,0.0000171707,0.0002605723,0.000027278107,0.0000028789,0.0000015998219,0.00002829674,0.0000074320733,0.00040015086],"genre_scores_gemma":[0.9998305,0.000012916862,0.00006252197,0.000004189422,8.082653e-7,0.000001224951,0.000023556951,0.000002953147,0.00006130883],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99994564,0.000007909506,0.0000030568517,0.000009931838,0.0000067534725,0.000026625125],"domain_scores_gemma":[0.9998864,0.00003118494,0.000026746746,0.000008202683,0.000015740554,0.0000318281],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00009602529,0.00022963979,0.0001980786,0.00010768975,0.00031873802,0.00075562164,0.00022218066,0.00022019069,0.000722291],"category_scores_gemma":[0.00041997945,0.0002335519,0.00021576727,0.00009075427,0.0004362851,0.00042815844,0.00043225347,0.0002839264,0.000082283615],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0006705013,0.00019254634,0.06275458,0.000078358964,0.00010147814,0.00021662505,0.00028635294,0.40661418,0.5225487,0.0030677402,0.00034696868,0.0031220126],"study_design_scores_gemma":[0.00011423181,0.0001681841,0.055670764,0.0000089809755,0.000043497985,0.000030038023,0.00019583477,0.8958057,0.0465598,0.0009764194,0.0003842213,0.000042304648],"about_ca_topic_score_codex":0.011321315,"about_ca_topic_score_gemma":0.0066844495,"teacher_disagreement_score":0.011321315,"about_ca_system_score_codex":0.00066229014,"about_ca_system_score_gemma":0.0005904259,"threshold_uncertainty_score":0.022510827},"labels":[],"label_agreement":null},{"id":"W4414976321","doi":"10.1029/2025gl116236","title":"Delayed Pantropical Carbon Sink Recovery Due To Asynchronous Post‐El Niño Photosynthesis and Respiration Trajectories","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Inversa Systems (Canada); University of Toronto","funders":"National Key Research and Development Program of China; Nanjing University; Southwest University; Lunds Universitet; National Natural Science Foundation of China","keywords":"Pantropical; Ecosystem; Carbon cycle; Primary production; Respiration; Carbon sink; Photosynthesis; Sink (geography); Ecosystem respiration","score_opus":0.009280881057884046,"score_gpt":0.25300539674528666,"score_spread":0.2437245156874026,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414976321","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9982822,0.00009025154,0.0005016363,0.00013451852,0.000009069455,0.000002795634,0.00021796956,0.00003751552,0.00072416273],"genre_scores_gemma":[0.9997191,0.000018640594,0.000048646172,0.000012513617,0.0000022542786,0.0000013013201,0.00012989147,0.0000032842443,0.00006429549],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989855,0.000013325292,0.0000066804387,0.000038158763,0.000010738044,0.000032567998],"domain_scores_gemma":[0.99978346,0.000045120785,0.00008051838,0.000024314853,0.000037289545,0.000029210507],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002860018,0.00018475602,0.00014484124,0.0002603882,0.0002457094,0.00039413106,0.00018144975,0.00020650339,0.001851922],"category_scores_gemma":[0.00070153363,0.00013383923,0.0002121251,0.0002528534,0.0002715217,0.00040790523,0.0003874235,0.00025331933,0.00014479955],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00043271008,0.000041793046,0.9510418,0.00007789851,0.000146179,0.0003673997,0.00034431802,0.00862269,0.02354485,0.00085856585,0.00092597026,0.013595911],"study_design_scores_gemma":[0.0000078552275,0.00001360805,0.9892118,0.000007225327,0.000015447891,0.000044566343,0.00010144543,0.009266562,0.000586271,0.00017030863,0.00056871586,0.000006175772],"about_ca_topic_score_codex":0.018818742,"about_ca_topic_score_gemma":0.020766087,"teacher_disagreement_score":0.018818742,"about_ca_system_score_codex":0.0004038248,"about_ca_system_score_gemma":0.0003539577,"threshold_uncertainty_score":0.037418425},"labels":[],"label_agreement":null},{"id":"W4414987208","doi":"10.1029/2025gl119790","title":"Microbial Controls on Dissolved Organic Nitrogen Cycling During Long‐Term Degradation Experiments","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Wastewater Treatment and Nitrogen Removal","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université Laval; Université de Moncton; McGill University; Bureau de Coopération Interuniversitaire","funders":"Fonds de recherche du Québec – Nature et technologies; McGill Space Institute; Natural Sciences and Engineering Research Council of Canada; McGill University","keywords":"Dissolved organic carbon; Degradation (telecommunications); Nitrogen; Cycling; Microbial biodegradation; Carbon fibers; Total organic carbon","score_opus":0.022478114297857333,"score_gpt":0.2992605005363054,"score_spread":0.27678238623844803,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4414987208","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99802244,0.00019747447,0.00072851504,0.000024737035,0.000010154227,0.000029092062,0.00040743774,0.000018165458,0.0005620612],"genre_scores_gemma":[0.99494296,0.00023999864,0.0026392792,0.00004634257,0.00000925945,0.00011030482,0.0007940235,0.000019227753,0.0011986585],"study_design_codex":"bench_or_experimental","study_design_gemma":"bench_or_experimental","domain_scores_codex":[0.9994543,0.00010559218,0.00004760929,0.00017220963,0.0001230904,0.00009713582],"domain_scores_gemma":[0.9993487,0.00018617552,0.00011480523,0.000081198894,0.00020305757,0.000066043445],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005099081,0.00043022272,0.00044240864,0.00015844317,0.00030095156,0.0005455209,0.00026447602,0.00033493797,0.00046510153],"category_scores_gemma":[0.0008338491,0.00014400067,0.00025060406,0.00026151276,0.00024180088,0.00031272133,0.0004334668,0.00038665935,0.00015366318],"study_design_candidate":"bench_or_experimental","study_design_consensus":"bench_or_experimental","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00031390443,0.00005307919,0.0017498111,0.00003529452,0.000009108507,0.000021257416,0.00004918629,0.000113608665,0.99609727,0.0000196728,0.000019166473,0.0015185126],"study_design_scores_gemma":[0.000020799462,0.0012450956,0.019287376,0.000012724633,0.00003399091,0.000057537316,0.0001532173,0.0014593846,0.976388,0.00007162307,0.0012539908,0.000016224223],"about_ca_topic_score_codex":0.00364259,"about_ca_topic_score_gemma":0.005203685,"teacher_disagreement_score":0.00364259,"about_ca_system_score_codex":0.00046102607,"about_ca_system_score_gemma":0.00030361244,"threshold_uncertainty_score":0.007242799},"labels":[],"label_agreement":null},{"id":"W4415047105","doi":"10.1029/2025gl117469","title":"Direct Radiation Belt Injections and Their Auroral Counterparts","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Calgary","funders":"","keywords":"Mesoscale meteorology; Van Allen radiation belt; Radiation; Earth's magnetic field; Electron; Geomagnetic storm; Relativistic particle","score_opus":0.010496343361467148,"score_gpt":0.28730608945951996,"score_spread":0.2768097460980528,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415047105","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99518675,0.00012531051,0.0016432711,0.000034433913,0.0000038262165,0.000018883115,0.00011513185,0.000049325856,0.0028231472],"genre_scores_gemma":[0.9993862,0.000033883596,0.0003555662,0.0000037088691,0.0000046730224,0.000003042842,0.000045869867,0.0000029775722,0.0001640922],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998715,0.000026224998,0.0000086006385,0.000031429063,0.000034102777,0.000028165867],"domain_scores_gemma":[0.99951875,0.00015290658,0.00019558839,0.000054073742,0.000031278592,0.00004732833],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00018300311,0.00024962064,0.00019941058,0.00041745542,0.000248192,0.00066740834,0.00028948276,0.00038227494,0.0013571235],"category_scores_gemma":[0.00075459044,0.00013575502,0.00027597157,0.00033550317,0.0003798494,0.0002944716,0.0005527644,0.0002425735,0.00009949028],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00094563153,0.0003080743,0.84178764,0.00018930412,0.00029815506,0.018914308,0.0012939255,0.060981993,0.033225603,0.008904748,0.0008869287,0.03226383],"study_design_scores_gemma":[0.00016631446,0.00070280913,0.7883129,0.000059434584,0.00017797359,0.008772758,0.0014564614,0.1713595,0.015377764,0.005162329,0.008396594,0.00005512581],"about_ca_topic_score_codex":0.0023541567,"about_ca_topic_score_gemma":0.0021372174,"teacher_disagreement_score":0.0023541567,"about_ca_system_score_codex":0.00028892414,"about_ca_system_score_gemma":0.000116004034,"threshold_uncertainty_score":0.004680872},"labels":[],"label_agreement":null},{"id":"W4415173095","doi":"10.1029/2025gl118709","title":"Chemical Heating as a Feedback Mechanism in the Mesopause Region","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of New Brunswick","funders":"Leibniz-Gemeinschaft","keywords":"Mesopause; Exothermic reaction; Thermal; Mechanism (biology); Chemical reaction; Nonlinear system","score_opus":0.016753421099267175,"score_gpt":0.30047435033967906,"score_spread":0.28372092924041187,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415173095","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9607721,0.00017026556,0.022647934,0.0003780862,0.00006361989,0.000021630596,0.00010175489,0.0007379407,0.015106625],"genre_scores_gemma":[0.99885786,0.000014998683,0.00043673743,0.000014016782,0.000003609791,0.000003948317,0.000008623211,0.000012378594,0.00064786494],"study_design_codex":"bench_or_experimental","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.99996185,0.000003569731,8.901106e-7,0.0000085224165,0.0000098829705,0.000015349451],"domain_scores_gemma":[0.9999144,0.00003247593,0.00001621609,0.000006440849,0.000013689245,0.000016729538],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00008485982,0.00023540319,0.0002471313,0.00015327698,0.0003403328,0.0003635932,0.00030770552,0.00023809883,0.0029842188],"category_scores_gemma":[0.00024526494,0.00016222545,0.00021934396,0.00007015278,0.00043851393,0.00042942763,0.00043308845,0.00033005138,0.00023810385],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041207758,0.00009941986,0.0060282303,0.00011644229,0.000050723276,0.00086839433,0.00016752281,0.24634254,0.7171381,0.016132545,0.0012889128,0.011355101],"study_design_scores_gemma":[0.00008551557,0.0001770275,0.012314888,0.000008668345,0.000023622855,0.00016984838,0.00006987563,0.9046064,0.075106345,0.0051482436,0.0022539806,0.000035637175],"about_ca_topic_score_codex":0.0052968278,"about_ca_topic_score_gemma":0.0036700827,"teacher_disagreement_score":0.0052968278,"about_ca_system_score_codex":0.0005900928,"about_ca_system_score_gemma":0.00035801213,"threshold_uncertainty_score":0.010531962},"labels":[],"label_agreement":null},{"id":"W4415173650","doi":"10.1029/2025gl116033","title":"Summertime Diurnal Variability of Formaldehyde Over the Contiguous United States: Constraints From Pandonia Global Network","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Nuclear Safety and Security Commission; Office of Experimental Program to Stimulate Competitive Research; Langley Research Center; National Aeronautics and Space Administration","keywords":"Troposphere; Diurnal cycle; Diurnal temperature variation; Planetary boundary layer; Ozone Monitoring Instrument; Geostationary orbit; Satellite; Formaldehyde; Tropospheric ozone","score_opus":0.017705802692549608,"score_gpt":0.27909569748840674,"score_spread":0.2613898947958571,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415173650","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9959246,0.000060220023,0.00014224197,0.000050275376,0.00000476239,0.0000048764055,0.0029802676,0.000026082347,0.0008066918],"genre_scores_gemma":[0.9958637,0.000041147123,0.00022651647,0.00001400652,0.0000033724566,0.0000052839664,0.0037208884,0.000004409096,0.00012067889],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9998771,0.00003154641,0.000010809984,0.00003669526,0.000019225943,0.000024594201],"domain_scores_gemma":[0.999731,0.000059506012,0.0000651466,0.000037658,0.00007223819,0.00003437643],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00028753642,0.00022639876,0.0001694009,0.00057249254,0.00031169088,0.0005620107,0.00019402713,0.000170328,0.0005846747],"category_scores_gemma":[0.00059551856,0.00012344978,0.00022489362,0.0008291771,0.00014180144,0.00030475273,0.0004282911,0.00013500436,0.00008843396],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00010174175,0.000047923422,0.9823736,0.000026727614,0.00012665214,0.00011670112,0.00011902599,0.005961704,0.0033819752,0.00011727413,0.00116265,0.006464078],"study_design_scores_gemma":[0.0000032078792,0.000010013478,0.99169195,0.0000055192036,0.000024832521,0.000021189639,0.000152355,0.007029938,0.00036671312,0.000023821423,0.0006654485,0.000004995161],"about_ca_topic_score_codex":0.19574322,"about_ca_topic_score_gemma":0.31256875,"teacher_disagreement_score":0.19574322,"about_ca_system_score_codex":0.00059195544,"about_ca_system_score_gemma":0.00038524228,"threshold_uncertainty_score":0.38920772},"labels":[],"label_agreement":null},{"id":"W4415243022","doi":"10.1029/2025gl118662","title":"Prevailing Climate Patterns for Concurrent High Temperature and Low Precipitation Days in Canada","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate variability and models","field":"Environmental Science","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"University of Calgary; University of Manitoba","funders":"Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs","keywords":"Precipitation; Climate extremes; Climate change; Arctic; The arctic; Period (music)","score_opus":0.01950664667635862,"score_gpt":0.29710783184011447,"score_spread":0.27760118516375587,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415243022","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9968374,0.00014455564,0.00010929034,0.0000987227,0.000003674477,0.000004426584,0.0016071982,0.000008260267,0.0011863842],"genre_scores_gemma":[0.99933547,0.00007165149,0.00005790729,0.000009239234,0.0000011044946,0.0000014092791,0.0003587721,0.0000016168348,0.00016281566],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99988806,0.000008820844,0.000005870987,0.00002790541,0.000025895066,0.000043534892],"domain_scores_gemma":[0.9994301,0.000055083336,0.000099920304,0.00001716114,0.00026552827,0.0001321014],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00016915669,0.00013934146,0.00011727486,0.0007286223,0.0009740281,0.0008300664,0.00028296164,0.00012171063,0.0014275876],"category_scores_gemma":[0.000742969,0.000089483714,0.00019889636,0.0015600697,0.00037498094,0.00017629794,0.00042103312,0.00022842675,0.00007329117],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.000037274527,0.000007673803,0.99483734,0.000009302082,0.00003298349,0.00004808383,0.0002875803,0.0004998207,0.0005871222,0.00013603207,0.00040927756,0.0031075454],"study_design_scores_gemma":[0.0000010379405,0.0000024392825,0.9985911,0.000003319706,0.000006301407,0.000013449298,0.00053032214,0.0004197941,0.00005538323,0.000015984922,0.00035730115,0.000003514852],"about_ca_topic_score_codex":0.9837325,"about_ca_topic_score_gemma":0.99292904,"teacher_disagreement_score":0.016267478,"about_ca_system_score_codex":0.00707868,"about_ca_system_score_gemma":0.00958547,"threshold_uncertainty_score":0.051359653},"labels":[],"label_agreement":null},{"id":"W4415243025","doi":"10.1029/2025gl117816","title":"Limits to the Practical Predictability of Convective‐Scale Forecast Systems With World‐Class Data Assimilation","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Meteorological Phenomena and Simulations","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Natural Sciences and Engineering Research Council of Canada; Alliance de recherche numérique du Canada","keywords":"Data assimilation; Predictability; Radar; Forecast verification; Limiting; Forecast skill; Forecast error; Numerical weather prediction","score_opus":0.12170633114323755,"score_gpt":0.356730601871835,"score_spread":0.23502427072859744,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415243025","genre_codex":"methods","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.45634446,0.0026066909,0.5051668,0.012158512,0.00038479964,0.00016035757,0.00071173883,0.0013999747,0.021066634],"genre_scores_gemma":[0.98530674,0.00019957645,0.013764827,0.00012665759,0.00008822667,0.000040594547,0.00015453194,0.000032214153,0.00028671554],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9974815,0.0012894784,0.00019065273,0.0003204543,0.00051005353,0.00020796197],"domain_scores_gemma":[0.957796,0.036159206,0.0011703335,0.0028794224,0.0016515895,0.00034344927],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0106364265,0.00051707105,0.0008329882,0.00042880318,0.00083196093,0.0023160593,0.0008874214,0.001138873,0.0009372436],"category_scores_gemma":[0.06197101,0.0005441477,0.00041384794,0.0005451028,0.0016706071,0.003952517,0.0017524117,0.0017925431,0.00023905741],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0003716031,0.000062088904,0.01418609,0.00010586718,0.000109640736,0.00007291141,0.00017441151,0.91388214,0.002166623,0.03296674,0.0017813853,0.03412048],"study_design_scores_gemma":[0.00001030845,0.000018159844,0.00096996373,0.000013119485,0.000005724235,0.000011286559,0.000022836079,0.98743886,0.0005790079,0.010647484,0.0002742098,0.000008966425],"about_ca_topic_score_codex":0.013448941,"about_ca_topic_score_gemma":0.006197972,"teacher_disagreement_score":0.013448941,"about_ca_system_score_codex":0.0010526818,"about_ca_system_score_gemma":0.0014292403,"threshold_uncertainty_score":0.056251526},"labels":[],"label_agreement":null},{"id":"W4415438460","doi":"10.1029/2025gl119977","title":"The Life Cycle of a Stratospheric Smoke Plume as Seen From EarthCARE—Tracking a Plume From Canada to Europe","year":2025,"lang":"en","type":"preprint","venue":"Geophysical Research Letters","topic":"Atmospheric and Environmental Gas Dynamics","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"European Space Agency; National Aeronautics and Space Administration","keywords":"Plume; Smoke; Lidar; Aerosol; Tracking (education); Atmosphere (unit)","score_opus":0.01849467426380737,"score_gpt":0.26731110404696085,"score_spread":0.24881642978315346,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415438460","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9976804,0.0000667673,0.00012608878,0.00004101236,0.000003068488,0.000008862866,0.00057929487,0.000024232857,0.0014702836],"genre_scores_gemma":[0.9977457,0.000041902924,0.0003226794,0.00001700309,0.0000010819244,0.0000026691912,0.0010666166,0.000004397346,0.0007977938],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992526,0.0000031131935,0.0000016049512,0.000010863668,0.000035226323,0.000023877845],"domain_scores_gemma":[0.9997907,0.000016019532,0.000015975716,0.000008842524,0.00012389333,0.00004446294],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00013081919,0.00017408394,0.00012481655,0.0008166023,0.00064382737,0.000589447,0.0002565868,0.0002939325,0.0006342859],"category_scores_gemma":[0.00021116676,0.00007720469,0.00016227234,0.00071842776,0.00024901875,0.00021053528,0.0003519061,0.00018208739,0.00008397313],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":true,"about_ca_topic_consensus":true,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00041606027,0.00014586424,0.8875907,0.000044757104,0.00008548403,0.0009581472,0.0018569926,0.005517546,0.06291662,0.0008589239,0.0024295235,0.037179537],"study_design_scores_gemma":[0.000009145513,0.00006414309,0.980923,0.000014392028,0.000017718558,0.000101012825,0.0011632538,0.0067157117,0.0068066847,0.000066322944,0.004098236,0.00002038225],"about_ca_topic_score_codex":0.8395595,"about_ca_topic_score_gemma":0.85750484,"teacher_disagreement_score":0.1604405,"about_ca_system_score_codex":0.0032170177,"about_ca_system_score_gemma":0.0020070672,"threshold_uncertainty_score":0.3227707},"labels":[],"label_agreement":null},{"id":"W4415617604","doi":"10.1029/2025gl117683","title":"Extreme Magnetopause Deformation Induced by High‐Speed Jet From Foreshock Transient","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Ionosphere and magnetosphere dynamics","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Saskatchewan","funders":"Canadian Space Agency; National Science Foundation","keywords":"Magnetosheath; Magnetopause; Magnetosphere; Solar wind; Foreshock; Interplanetary magnetic field; Bow shock (aerodynamics); Convection; Jet (fluid)","score_opus":0.019976861707582734,"score_gpt":0.2731567958693125,"score_spread":0.2531799341617298,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415617604","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99918896,0.00004264575,0.00018070829,0.0000073257734,0.0000047515987,0.0000023033065,0.00012560275,0.0000182973,0.0004294282],"genre_scores_gemma":[0.9995573,0.00001942985,0.00012370328,0.0000036424908,0.0000036700442,0.0000011120524,0.00018303914,0.0000018587779,0.000106121995],"study_design_codex":"bench_or_experimental","study_design_gemma":"observational","domain_scores_codex":[0.99995756,0.0000018288955,0.0000011809453,0.00001019969,0.0000102903,0.00001893575],"domain_scores_gemma":[0.99992037,0.000006392032,0.000034220102,0.000007596374,0.000009060735,0.000022315107],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00006834214,0.00017249063,0.00013297066,0.00033035234,0.00023463975,0.00025624695,0.00009691705,0.00015315866,0.00073339214],"category_scores_gemma":[0.00009514234,0.00007407398,0.00012669075,0.00024437023,0.00012873518,0.00015257747,0.00029297036,0.00018525365,0.00006776081],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0013711351,0.000072675924,0.40574774,0.000104931554,0.0001535717,0.0028463912,0.0005860258,0.0032875957,0.5651265,0.00031495336,0.00077108,0.019617375],"study_design_scores_gemma":[0.000012833039,0.00008479433,0.9841561,0.0000051623497,0.000022023745,0.00023583896,0.00020087542,0.0017777027,0.012722091,0.00006541339,0.0007073492,0.000009798418],"about_ca_topic_score_codex":0.0034052671,"about_ca_topic_score_gemma":0.006395507,"teacher_disagreement_score":0.0034052671,"about_ca_system_score_codex":0.0001764491,"about_ca_system_score_gemma":0.00012908304,"threshold_uncertainty_score":0.006770909},"labels":[],"label_agreement":null},{"id":"W4415762744","doi":"10.1029/2025gl117360","title":"Diurnal Variations in Background and Urban NO <sub>2</sub> Estimated From TEMPO","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Marshall Space Flight Center; National Aeronautics and Space Administration","keywords":"Noon; Diurnal temperature variation; Morning; Troposphere; Diurnal cycle; Plume; Seasonality","score_opus":0.03358788210618997,"score_gpt":0.29071274487244125,"score_spread":0.2571248627662513,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4415762744","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9983606,0.000025599918,0.000930096,0.0000033975905,0.000002603183,0.000003695126,0.00029358306,0.000035973444,0.00034440082],"genre_scores_gemma":[0.9976428,0.000025511057,0.0013148303,0.0000030516799,0.0000049364826,0.000008457606,0.0007617971,0.000011585218,0.00022696768],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.999941,0.000008259493,0.0000028161821,0.000018504774,0.000020054124,0.00000930198],"domain_scores_gemma":[0.9998784,0.00002805355,0.000029482839,0.000010917143,0.000034905617,0.000018289993],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011000582,0.00018631367,0.00014397128,0.00044725894,0.000091545146,0.00022434813,0.000111279056,0.00011956014,0.00048441504],"category_scores_gemma":[0.0003406048,0.00008385886,0.00007929176,0.00034787008,0.00006139978,0.00012591227,0.00015711953,0.000113649985,0.0001271315],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0011676088,0.00013304375,0.6956494,0.0000973469,0.000120752804,0.0002368601,0.0003787834,0.010277942,0.24121918,0.00013281326,0.00055917806,0.050027005],"study_design_scores_gemma":[0.0000069034027,0.00006912616,0.9685081,0.0000035213732,0.000020803354,0.000067871944,0.000103551094,0.014796573,0.015817713,0.000047021993,0.00054807524,0.000010710641],"about_ca_topic_score_codex":0.0018161624,"about_ca_topic_score_gemma":0.004507209,"teacher_disagreement_score":0.0018161624,"about_ca_system_score_codex":0.0000817354,"about_ca_system_score_gemma":0.000049646642,"threshold_uncertainty_score":0.0036111474},"labels":[],"label_agreement":null},{"id":"W4416087796","doi":"10.1029/2025gl118367","title":"Winter Methane Fluxes Over Boreal and Arctic Environments","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Université de Montréal; Université du Québec à Trois-Rivières; Center for Northern Studies; Cégep de Sherbrooke","funders":"European Research Council; Natural Sciences and Engineering Research Council of Canada; Fonds de recherche du Québec; Bundesministerium für Bildung und Forschung; Polar Knowledge Canada","keywords":"Boreal; Tundra; Taiga; Snowpack; Wetland; Boreal ecosystem; Arctic; Snow; Carbon cycle; Subarctic climate","score_opus":0.04138382523299923,"score_gpt":0.31020465234388334,"score_spread":0.2688208271108841,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416087796","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99947876,0.000029784316,0.000031111995,0.000003693399,0.0000011738823,6.944802e-7,0.0002553865,0.0000045056536,0.00019482123],"genre_scores_gemma":[0.999388,0.00002265806,0.000087043714,0.000003079426,0.0000013111008,0.0000014308483,0.0004459767,0.0000014180234,0.000049106962],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99993587,0.000008045823,0.000003496538,0.000018893275,0.000014233048,0.000019519073],"domain_scores_gemma":[0.9999001,0.000016672357,0.000023475071,0.000005634146,0.00002988954,0.000024149625],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0001685571,0.00031978538,0.00017209732,0.00033979642,0.0005146266,0.00047281003,0.000160413,0.000156905,0.00038568067],"category_scores_gemma":[0.00018017982,0.00009610498,0.00019488522,0.00041500173,0.00017673368,0.00023799035,0.00020849548,0.0001138132,0.000044165474],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0010227395,0.00006487219,0.95564896,0.00005012686,0.00013534962,0.0001567598,0.00038517217,0.0043835756,0.030136073,0.00010389221,0.00021288997,0.007699526],"study_design_scores_gemma":[0.0000066893194,0.000030596206,0.99712855,0.000002528333,0.000018520037,0.00003916006,0.00020743387,0.0014714344,0.0008566066,0.000021594953,0.0002119595,0.0000048679617],"about_ca_topic_score_codex":0.21067779,"about_ca_topic_score_gemma":0.30943894,"teacher_disagreement_score":0.21067779,"about_ca_system_score_codex":0.0007963004,"about_ca_system_score_gemma":0.00048483707,"threshold_uncertainty_score":0.41890305},"labels":[],"label_agreement":null},{"id":"W4416134236","doi":"10.1029/2025gl117957","title":"Mean Kinetic Energy and Its Projected Changes Dominate Over Eddy Kinetic Energy in the Arctic Ocean","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":3,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"McGill University","funders":"Fonds de recherche du Québec – Nature et technologies; Natural Sciences and Engineering Research Council of Canada; Canada Research Chairs; Agence Nationale de la Recherche","keywords":"Baroclinity; Kinetic energy; Arctic; Sea ice; Forcing (mathematics); Sea ice thickness; Arctic ice pack; Ocean current; The arctic","score_opus":0.01638517626150995,"score_gpt":0.2575041420800347,"score_spread":0.24111896581852474,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416134236","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99887174,0.00005599534,0.0003263323,0.000076164266,0.0000070563638,8.89454e-7,0.00015237191,0.000011995212,0.00049748935],"genre_scores_gemma":[0.99962115,0.000032020907,0.00014541791,0.0000060193333,0.0000029297448,0.0000012096716,0.00010690618,0.0000031362433,0.0000811067],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99992216,0.000020160016,0.000005439943,0.000017405493,0.000014361525,0.000020518073],"domain_scores_gemma":[0.99981815,0.000058878817,0.000031349795,0.000016162225,0.000045122866,0.000030372106],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0003743712,0.00021467579,0.00021672086,0.0002016707,0.00030715507,0.000876056,0.00019517141,0.0002767496,0.0005768893],"category_scores_gemma":[0.00073769985,0.00019242043,0.00042539,0.0002768845,0.0002561539,0.00048657233,0.00028881122,0.0003220221,0.00006867644],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00056931743,0.00015002622,0.6742186,0.000058888094,0.0003694354,0.0002111365,0.00014265394,0.295868,0.014924484,0.0025932651,0.0008974824,0.00999677],"study_design_scores_gemma":[0.00003780415,0.00009993007,0.5932814,0.000020532563,0.00007725119,0.000086612505,0.00029936424,0.4006678,0.0031366386,0.0012840064,0.0009690714,0.000039598242],"about_ca_topic_score_codex":0.033005588,"about_ca_topic_score_gemma":0.03265015,"teacher_disagreement_score":0.033005588,"about_ca_system_score_codex":0.00064900046,"about_ca_system_score_gemma":0.0005565894,"threshold_uncertainty_score":0.06562698},"labels":[],"label_agreement":null},{"id":"W4416380006","doi":"10.1029/2025gl118603","title":"Soluble Iron in Source‐Based Anthropogenic PM <sub>2.5</sub> Predominantly From Steel Industry and Residential Combustion in China","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"Ministry of Science and Technology of the People's Republic of China; Fudan University; National Natural Science Foundation of China; Shanghai Normal University; Dalian University of Technology; Lanzhou University","keywords":"Combustion; Particulates; Plume; Solubility; Flue-gas desulfurization; Flue gas; Aerosol; Oxy-fuel; Flue","score_opus":0.015845833138956683,"score_gpt":0.2683053250643479,"score_spread":0.2524594919253912,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416380006","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9996942,0.000027208562,0.00005953839,0.000008282031,6.240521e-7,0.0000017429685,0.00008836028,0.0000025569109,0.00011745969],"genre_scores_gemma":[0.9995857,0.00002911924,0.000049918897,0.0000050473304,0.000001990527,0.0000018447838,0.00023825992,0.000001138276,0.00008697139],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99989617,0.000008161274,0.000008234507,0.000034166416,0.000029600535,0.00002371729],"domain_scores_gemma":[0.9999194,0.000010565921,0.000021927364,0.0000070623973,0.000028468032,0.000012471134],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00020170664,0.000409743,0.00024603057,0.0007594936,0.00044637048,0.0004095124,0.00027377805,0.00027549625,0.0003321065],"category_scores_gemma":[0.00014383915,0.00023448656,0.0003731334,0.000570936,0.00026438577,0.00034139754,0.0003153906,0.00009648146,0.000056874494],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00018880035,0.000082285995,0.9344604,0.00012339416,0.0001621214,0.00047893048,0.00042741295,0.0066563464,0.04717833,0.00019485372,0.00029708867,0.00975003],"study_design_scores_gemma":[0.000009414973,0.000022564847,0.98949695,0.000003419161,0.000033250173,0.00003983003,0.00018104867,0.0070384815,0.0028896686,0.00004321567,0.00023524415,0.0000069308135],"about_ca_topic_score_codex":0.083702385,"about_ca_topic_score_gemma":0.095012,"teacher_disagreement_score":0.083702385,"about_ca_system_score_codex":0.00089411077,"about_ca_system_score_gemma":0.000526669,"threshold_uncertainty_score":0.16643035},"labels":[],"label_agreement":null},{"id":"W4416380479","doi":"10.1029/2025gl118495","title":"Seasonal Freezing Enhances Groundwater–Lake Connectivity and Nutrient Delivery in Saline Basins","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Dalhousie University","funders":"","keywords":"Biogeochemical cycle; Groundwater; Salinity; Hydrology (agriculture); Nutrient; Hydrogeology; Saline water; Evaporation","score_opus":0.04420076802867654,"score_gpt":0.2999535938757404,"score_spread":0.2557528258470638,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416380479","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99961,0.0000073802153,0.00019658188,0.000011377366,6.068302e-7,9.98997e-7,0.00001818797,0.0000055381265,0.00014945537],"genre_scores_gemma":[0.9999286,0.0000052344903,0.000032527474,0.0000020096252,2.1792599e-7,4.7029474e-7,0.000011525586,7.91105e-7,0.000018610162],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999696,0.0000052342752,0.0000019795089,0.000007036653,0.000002799967,0.000013315427],"domain_scores_gemma":[0.9999403,0.000014962063,0.000014020187,0.000004773765,0.000008030849,0.000017985578],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00011353213,0.00016946616,0.00019259332,0.00019691014,0.00028218012,0.00039687718,0.00024889177,0.0001640878,0.00092931057],"category_scores_gemma":[0.00026631026,0.0001368414,0.00023374616,0.00014392655,0.00040258828,0.00036949274,0.00036418313,0.00013497283,0.000028373624],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00035438887,0.00020942872,0.52876693,0.00008997733,0.0001944105,0.0004988513,0.000393966,0.31850004,0.13894625,0.0025606952,0.00033039105,0.009154692],"study_design_scores_gemma":[0.00009325683,0.00023747832,0.4857936,0.000010948794,0.00009901279,0.000089748384,0.0004467538,0.5025555,0.007913873,0.0022947513,0.00043513556,0.000029885972],"about_ca_topic_score_codex":0.0241162,"about_ca_topic_score_gemma":0.018328128,"teacher_disagreement_score":0.0241162,"about_ca_system_score_codex":0.00063794653,"about_ca_system_score_gemma":0.00046607704,"threshold_uncertainty_score":0.04795164},"labels":[],"label_agreement":null},{"id":"W4416409888","doi":"10.1029/2025gl118580","title":"Plausibility Criteria for GRACE‐Derived Groundwater Storage Changes From Aquifers Globally","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geophysics and Gravity Measurements","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"","funders":"Lembaga Pengelola Dana Pendidikan; Canadian Institute for Advanced Research","keywords":"Aquifer; Groundwater; Hydrology (agriculture); Residual; Structural basin; Gravimetry; Water storage; Climate change; Sustainability","score_opus":0.07502173953798898,"score_gpt":0.3341835694679714,"score_spread":0.25916182992998243,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416409888","genre_codex":"empirical","genre_gemma":"methods","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"methods","genre_consensus":null,"domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9679672,0.00024917137,0.028212337,0.00044919123,0.000015284646,0.00004118252,0.0007505082,0.0001567475,0.0021585538],"genre_scores_gemma":[0.99813735,0.000017245566,0.0013297502,0.0000149327925,0.000010345803,0.000009515225,0.0004319303,0.000010911798,0.00003801578],"study_design_codex":"observational","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9950664,0.0022481529,0.00050576567,0.001056527,0.00082046713,0.00030258173],"domain_scores_gemma":[0.9223069,0.06433329,0.0047112526,0.0054528774,0.002288467,0.00090729876],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.016163675,0.00067659945,0.0007367184,0.002783812,0.000886029,0.002853207,0.0014151023,0.0011100527,0.0018334516],"category_scores_gemma":[0.10102369,0.00046838165,0.0011871567,0.0014864986,0.0016955587,0.0022385975,0.0025518418,0.0008311587,0.00015126707],"study_design_candidate":"simulation_or_modeling","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0022386836,0.000104858416,0.66721207,0.00016609477,0.0009459793,0.0013988791,0.0008611508,0.27982447,0.0051608714,0.017534379,0.0008727662,0.023679791],"study_design_scores_gemma":[0.00022529376,0.00026807774,0.18645252,0.000117455085,0.0003952739,0.00066599,0.00094332686,0.75586414,0.0050928774,0.048359938,0.0014885215,0.00012654223],"about_ca_topic_score_codex":0.00437713,"about_ca_topic_score_gemma":0.002124481,"teacher_disagreement_score":0.016163675,"about_ca_system_score_codex":0.0008237247,"about_ca_system_score_gemma":0.00060401415,"threshold_uncertainty_score":0.08548272},"labels":[],"label_agreement":null},{"id":"W4416593254","doi":"10.1029/2025gl118651","title":"Ozone Trends in the Upper Troposphere‐Lower Stratosphere Using Equivalent Latitude‐Potential Temperature Coordinates","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric Ozone and Climate","field":"Earth and Planetary Sciences","cited_by":2,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"","keywords":"Stratosphere; Troposphere; Ozone; Ozone depletion; Atmospheric dynamics; Consistency (knowledge bases); Polar; Latitude","score_opus":0.024517274586637994,"score_gpt":0.3093796054756734,"score_spread":0.2848623308890354,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416593254","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9924034,0.00011723426,0.0026124008,0.000056955232,0.000005172608,0.000002971467,0.0031956732,0.0000623892,0.0015437262],"genre_scores_gemma":[0.9973531,0.00004429421,0.00110381,0.000005354238,0.0000038379626,0.0000024694964,0.0013523938,0.000009929024,0.0001248158],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.9999167,0.000031441003,0.000005629942,0.000021435728,0.000015076007,0.000009847687],"domain_scores_gemma":[0.99978036,0.00007738274,0.000055365806,0.000036105193,0.000041391962,0.000009396881],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0002271146,0.0001458392,0.000096169526,0.0006419861,0.00008700867,0.0004998168,0.0001271783,0.000084364896,0.0008506329],"category_scores_gemma":[0.00070367666,0.00005628922,0.00025688272,0.0010416762,0.000105666906,0.00025875974,0.00024389422,0.00013104592,0.00015869658],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00023817111,0.000044973196,0.83797354,0.00010751831,0.0004894614,0.00015857296,0.00035300694,0.09665369,0.017995317,0.004307185,0.002041208,0.039637286],"study_design_scores_gemma":[0.000011899019,0.000042792435,0.9216418,0.000013789395,0.000091140646,0.000044576856,0.00017338294,0.07083613,0.003956548,0.00054953573,0.0026218733,0.000016463846],"about_ca_topic_score_codex":0.019412145,"about_ca_topic_score_gemma":0.016451016,"teacher_disagreement_score":0.019412145,"about_ca_system_score_codex":0.0001649105,"about_ca_system_score_gemma":0.00011144864,"threshold_uncertainty_score":0.03859836},"labels":[],"label_agreement":null},{"id":"W4416965570","doi":"10.1029/2025gl120749","title":"Tropical Cyclones Drive Enhanced Inorganic Iodine in the Mid‐Latitude Upper Troposphere","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"European Centre for Medium-Range Weather Forecasts; Deutsche Forschungsgemeinschaft","keywords":"Troposphere; Iodine; Stratosphere; Atmosphere (unit); Halogen; Tropical cyclone","score_opus":0.014027731094418874,"score_gpt":0.274455350807609,"score_spread":0.2604276197131902,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4416965570","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9990295,0.000042396918,0.000044175205,0.0000273313,0.0000061168607,0.0000031485129,0.00024098603,0.00000887738,0.0005975957],"genre_scores_gemma":[0.9995291,0.000026203845,0.00003468851,0.00001586902,0.0000059689346,0.0000018222391,0.00021163862,0.0000022736667,0.0001724748],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99995244,0.000004917813,0.0000024614649,0.0000140045095,0.0000075296116,0.000018636894],"domain_scores_gemma":[0.9998865,0.000010667263,0.000042611802,0.0000071657064,0.000017641905,0.00003539785],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000067448855,0.00018542701,0.00011353625,0.00021975947,0.00018797925,0.00042849797,0.000077056335,0.000130025,0.0012433953],"category_scores_gemma":[0.00011446362,0.00009693729,0.00014039334,0.00015322774,0.00010729655,0.00012612712,0.0002457408,0.00016835552,0.00016368445],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025480438,0.00007035016,0.90721464,0.00003271474,0.000090722475,0.000249051,0.0002708628,0.00039567988,0.0856189,0.00017176317,0.0008064255,0.0048239757],"study_design_scores_gemma":[0.0000033453728,0.000018970475,0.99855214,0.0000022273364,0.000007798339,0.000014692992,0.00009046364,0.00024221312,0.00083302666,0.000013764091,0.00021952069,0.0000017459122],"about_ca_topic_score_codex":0.011041626,"about_ca_topic_score_gemma":0.011740257,"teacher_disagreement_score":0.011041626,"about_ca_system_score_codex":0.00020145446,"about_ca_system_score_gemma":0.00017704218,"threshold_uncertainty_score":0.021954715},"labels":[],"label_agreement":null},{"id":"W4417100829","doi":"10.1029/2025gl118030","title":"A &gt;70‐Myr‐Long Geomagnetic Field Reversal Hyperactivity Across the Ediacaran‐Cambrian Transition","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Geomagnetism and Paleomagnetism Studies","field":"Biochemistry, Genetics and Molecular Biology","cited_by":4,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":true,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"Western University","funders":"Natural Sciences and Engineering Research Council of Canada; National Natural Science Foundation of China; National Key Research and Development Program of China; National Science and Technology Major Project; Yale University","keywords":"Earth's magnetic field; Geomagnetic reversal; Dynamo theory; Magnetostratigraphy; Paleomagnetism; Secular variation","score_opus":0.013672464911090322,"score_gpt":0.3088362830885183,"score_spread":0.295163818177428,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417100829","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99723744,0.00031503374,0.00022888853,0.00006329644,0.0000030688666,0.0000045759266,0.00041440292,0.000026079819,0.0017071973],"genre_scores_gemma":[0.9993487,0.000074496944,0.00007061366,0.000017523871,0.0000021892738,0.0000016978573,0.00017392251,0.0000022395393,0.00030867264],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994695,0.0000029795524,0.0000023711336,0.000016894131,0.000009377004,0.000021328462],"domain_scores_gemma":[0.99986315,0.000010535704,0.000045644974,0.000009006013,0.00004046544,0.000031256328],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00014166521,0.0001199484,0.00016762078,0.00059695856,0.0004780459,0.0005193707,0.00015197709,0.00015177418,0.0012636008],"category_scores_gemma":[0.00026222557,0.000073458126,0.000075706186,0.00061064877,0.0004357425,0.000102255086,0.00030850776,0.00021867843,0.00016438174],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00025760767,0.00002521039,0.84203756,0.000074258955,0.000085532854,0.000369215,0.0012255183,0.0007685879,0.12356845,0.00086491177,0.00084497203,0.029878153],"study_design_scores_gemma":[8.910099e-7,0.000006788891,0.9982362,0.0000023634564,0.000003973085,0.00003322318,0.000085864114,0.00006111517,0.0007817723,0.000014408491,0.00077233097,0.0000011401179],"about_ca_topic_score_codex":0.13263603,"about_ca_topic_score_gemma":0.18871644,"teacher_disagreement_score":0.13263603,"about_ca_system_score_codex":0.0014922234,"about_ca_system_score_gemma":0.00057746226,"threshold_uncertainty_score":0.26372796},"labels":[],"label_agreement":null},{"id":"W4417432000","doi":"10.1029/2025gl118112","title":"Mercury's Hollows: A Potential Signature of Sulfur Exosphere‐Subsurface Transport","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Planetary Science and Exploration","field":"Physics and Astronomy","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Memorial University of Newfoundland","funders":"Centre National d’Etudes Spatiales; Agence Nationale de la Recherche","keywords":"Sulfur; Diffusion; Mercury (programming language); Sulfur cycle; Porosity; Pore water pressure; Porous medium","score_opus":0.016390098275245363,"score_gpt":0.281750387766158,"score_spread":0.26536028949091267,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417432000","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99785763,0.00003587251,0.0010309108,0.00006447716,0.0000025417228,0.0000021607145,0.00018410961,0.000102579,0.00071984273],"genre_scores_gemma":[0.9996973,0.000008950256,0.00018099224,0.000003014773,6.377008e-7,5.377528e-7,0.000043701282,0.0000066015696,0.0000584042],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99997556,0.0000028674797,7.6694386e-7,0.000007403425,0.0000040822715,0.000009450513],"domain_scores_gemma":[0.9999213,0.000013085301,0.00001764491,0.000009635603,0.0000143559255,0.000024006094],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.000068101035,0.0002448516,0.00020834625,0.0002924471,0.0002510094,0.00040151054,0.0003071741,0.00040710016,0.0012696523],"category_scores_gemma":[0.00018671808,0.00019647092,0.00026310282,0.000339545,0.000363294,0.00031248678,0.000488364,0.00022752532,0.000087119006],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0008363892,0.00012978548,0.55809563,0.00011087671,0.00018207614,0.0011428754,0.0004311084,0.18248759,0.24012172,0.004815413,0.0013337341,0.010312783],"study_design_scores_gemma":[0.000071852875,0.00013705132,0.37684548,0.000015197791,0.000044788914,0.00023555248,0.00037553583,0.598998,0.019109095,0.0028760496,0.0012508947,0.00004059444],"about_ca_topic_score_codex":0.018199114,"about_ca_topic_score_gemma":0.009585108,"teacher_disagreement_score":0.018199114,"about_ca_system_score_codex":0.0005089379,"about_ca_system_score_gemma":0.00027776946,"threshold_uncertainty_score":0.036186397},"labels":[],"label_agreement":null},{"id":"W4417496988","doi":"10.1029/2025gl116414","title":"Quantification of Scales Not Constrained by Observation Using Ensembles","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Oceanographic and Atmospheric Processes","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"Environment and Climate Change Canada","funders":"","keywords":"Data assimilation; Ensemble average; Limit (mathematics); Satellite; Ensemble forecasting; Scale (ratio); Filter (signal processing); Ensemble Kalman filter","score_opus":0.05998904667503522,"score_gpt":0.3124598348839499,"score_spread":0.25247078820891466,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417496988","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.7892474,0.00018292887,0.20784079,0.00015118837,0.000030178675,0.000018428898,0.000209653,0.00027017843,0.0020491919],"genre_scores_gemma":[0.989815,0.00004008186,0.009859766,0.00001427923,0.000017897328,0.000012602471,0.000114715884,0.000030190495,0.00009547922],"study_design_codex":"simulation_or_modeling","study_design_gemma":"simulation_or_modeling","domain_scores_codex":[0.9995877,0.0000989411,0.000029793471,0.00012143703,0.00011672427,0.00004536459],"domain_scores_gemma":[0.9947202,0.0027320231,0.0010081127,0.0010322063,0.00033912397,0.0001682922],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0010259921,0.00039448348,0.00039889754,0.0004755888,0.00036620846,0.00093918515,0.0004131993,0.0004511029,0.00057479437],"category_scores_gemma":[0.0063778865,0.00035930975,0.00037400023,0.00048118073,0.0004728808,0.0018084197,0.0011996872,0.00094436575,0.000065514854],"study_design_candidate":"simulation_or_modeling","study_design_consensus":"simulation_or_modeling","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00034763524,0.00017084359,0.09548105,0.000099937126,0.00034539078,0.0002532274,0.0003753403,0.75986564,0.053385027,0.01738277,0.00073279155,0.07156039],"study_design_scores_gemma":[0.000007936355,0.0000298902,0.030307222,0.000018125727,0.00003685826,0.000023790173,0.00003165446,0.9568096,0.005535561,0.006646722,0.0005186234,0.00003412084],"about_ca_topic_score_codex":0.0039941785,"about_ca_topic_score_gemma":0.0029912898,"teacher_disagreement_score":0.0039941785,"about_ca_system_score_codex":0.0004096395,"about_ca_system_score_gemma":0.00045814883,"threshold_uncertainty_score":0.007941842},"labels":[],"label_agreement":null},{"id":"W4417525729","doi":"10.1029/2025gl118618","title":"Ocean Outgassing of Methyl Chloroform as an Underestimated Source of Emission","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Atmospheric chemistry and aerosols","field":"Earth and Planetary Sciences","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":false,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":true,"ca_institutions":"","funders":"Natural Environment Research Council; National Aeronautics and Space Administration; National Science Foundation","keywords":"Outgassing; Sink (geography); TRACER; Chloroform; Carbon dioxide; Atmospheric chemistry; Atmosphere (unit)","score_opus":0.03355995244835034,"score_gpt":0.3257025703410334,"score_spread":0.29214261789268303,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W4417525729","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99296874,0.0003181772,0.001810746,0.00031317442,0.000052443018,0.000010065314,0.0018591502,0.00019475896,0.00247274],"genre_scores_gemma":[0.99771464,0.00014930192,0.00062125805,0.0000559108,0.000008022409,0.0000053268172,0.0010524918,0.000041931362,0.00035104866],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.99988365,0.000022391969,0.00000779843,0.00004284562,0.000017987682,0.000025380807],"domain_scores_gemma":[0.99973077,0.0000700119,0.00004483035,0.000044246666,0.00007229917,0.000037825466],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00033029186,0.0005528616,0.00035544013,0.00035530463,0.00030021454,0.0009748102,0.0004581214,0.0009902272,0.0017554725],"category_scores_gemma":[0.0009789263,0.00032996017,0.0011647353,0.0005613666,0.0003189964,0.0009241694,0.0005416679,0.0005086549,0.0002687023],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.0005312962,0.00010050995,0.4198315,0.00027676887,0.00048801457,0.0004411856,0.00015386243,0.5363037,0.026654681,0.0016176652,0.001968537,0.011632224],"study_design_scores_gemma":[0.00022706222,0.00015790791,0.3175019,0.00011755116,0.00031008432,0.00011519861,0.00032389924,0.6609934,0.01214968,0.0014259337,0.0065386216,0.00013880862],"about_ca_topic_score_codex":0.061356317,"about_ca_topic_score_gemma":0.030544953,"teacher_disagreement_score":0.061356317,"about_ca_system_score_codex":0.001111611,"about_ca_system_score_gemma":0.00096840714,"threshold_uncertainty_score":0.12199837},"labels":[],"label_agreement":null},{"id":"W7116749051","doi":"10.1029/2025gl117623","title":"Reversal Trends in Shallow‐Soil Temperature Over the Qinghai‐Tibet Plateau During 1950–2014","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Climate change and permafrost","field":"Earth and Planetary Sciences","cited_by":1,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Waterloo; University of Regina","funders":"National Natural Science Foundation of China","keywords":"Plateau (mathematics); Greenhouse gas; Dominance (genetics); Global warming; Climate change; Thermal; Greenhouse effect","score_opus":0.03082134016909293,"score_gpt":0.3050254455601014,"score_spread":0.2742041053910085,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116749051","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.99877375,0.00010474077,0.00012967698,0.00005815159,0.0000053547824,0.0000023883113,0.0003693456,0.000007873213,0.00054870424],"genre_scores_gemma":[0.9994797,0.000030763196,0.000035502937,0.000009869778,0.000006051287,0.0000021412336,0.0002619864,0.0000010232136,0.00017285836],"study_design_codex":"observational","study_design_gemma":"observational","domain_scores_codex":[0.99994075,0.000009188155,0.0000052210626,0.000017374372,0.000010458695,0.00001689008],"domain_scores_gemma":[0.99978954,0.00001970584,0.000058449376,0.000011836924,0.000064868946,0.00005569024],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.00037474008,0.0001670182,0.00012623517,0.00070694607,0.00033533064,0.0003719802,0.00019246501,0.00014737273,0.0011790594],"category_scores_gemma":[0.00028163183,0.00007772488,0.00019592281,0.0008864901,0.00035066568,0.0002323461,0.00027581427,0.00016616454,0.000073445655],"study_design_candidate":"observational","study_design_consensus":"observational","about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00014196867,0.000023778392,0.9705015,0.00008105092,0.00017389089,0.00022834477,0.00081212557,0.0022389998,0.010930288,0.0004806422,0.00070549233,0.01368193],"study_design_scores_gemma":[0.0000023701296,0.000013050091,0.9986203,0.0000035888233,0.000010833164,0.000015093481,0.000101693506,0.00069465744,0.00015090783,0.000026086956,0.0003580325,0.000003391135],"about_ca_topic_score_codex":0.044865403,"about_ca_topic_score_gemma":0.050804038,"teacher_disagreement_score":0.044865403,"about_ca_system_score_codex":0.0007005739,"about_ca_system_score_gemma":0.0005037572,"threshold_uncertainty_score":0.08920848},"labels":[],"label_agreement":null},{"id":"W7116786096","doi":"10.1029/2025gl117400","title":"Constraining African Fire CO <sub>2</sub> Emissions During 2015–2016 Using Satellite XCO <sub>2</sub> Retrievals","year":2025,"lang":"en","type":"article","venue":"Geophysical Research Letters","topic":"Fire effects on ecosystems","field":"Environmental Science","cited_by":0,"is_retracted":false,"has_abstract":true,"route_ca_aff":true,"route_ca_fund":false,"route_ca_venue":false,"route_about_ca":false,"ca_institutions":"University of Toronto","funders":"National Natural Science Foundation of China","keywords":"Inversion (geology); Satellite; Ecosystem; Earth system science; Carbon flux; Carbon cycle; Climate change","score_opus":0.022395645553289815,"score_gpt":0.3031997066405741,"score_spread":0.2808040610872843,"validation_status":"score_only:v0-immature-baseline","prediction":{"id":"W7116786096","genre_codex":"empirical","genre_gemma":"empirical","domain_codex":null,"domain_gemma":null,"model_version":"metacan-v3-hybrid-931329e0061c","genre_candidate":"empirical","genre_consensus":"empirical","domain_candidate":null,"domain_consensus":null,"prediction_status":"machine_predicted_unvalidated","genre_scores_codex":[0.9947976,0.000095500276,0.0028856013,0.00010318698,0.000013580104,0.000012747475,0.0007665606,0.00013062877,0.0011945803],"genre_scores_gemma":[0.9966967,0.000040860166,0.0024669403,0.000012508404,0.000007659174,0.000005685451,0.00062601996,0.000020195464,0.00012348284],"study_design_codex":"simulation_or_modeling","study_design_gemma":"observational","domain_scores_codex":[0.9998884,0.000025823952,0.0000063056473,0.0000315532,0.000017163493,0.000030759376],"domain_scores_gemma":[0.99981254,0.00004927262,0.00003559505,0.000033997472,0.00004607159,0.000022478182],"candidate_categories":[],"consensus_categories":[],"category_scores_codex":[0.0005728585,0.00057680963,0.00026105886,0.00044211734,0.00040129467,0.0005921729,0.00038477505,0.00047563706,0.00085599243],"category_scores_gemma":[0.00097345194,0.00025965142,0.00050689024,0.00060754584,0.00036595823,0.00061995594,0.00047036863,0.00047963613,0.00013767013],"study_design_candidate":"observational","study_design_consensus":null,"about_ca_topic_candidate":false,"about_ca_topic_consensus":false,"about_ca_system_candidate":false,"about_ca_system_consensus":false,"study_design_scores_codex":[0.00060335035,0.00018267754,0.17003141,0.0001020407,0.00034660054,0.00021493985,0.00016066259,0.7681451,0.023756308,0.0012078532,0.0011996727,0.03404948],"study_design_scores_gemma":[0.000116478266,0.00004764211,0.07547441,0.000031624277,0.00009688884,0.000031399486,0.00011978732,0.91013896,0.011849919,0.0005411737,0.0015104742,0.00004129144],"about_ca_topic_score_codex":0.06676982,"about_ca_topic_score_gemma":0.07089566,"teacher_disagreement_score":0.06676982,"about_ca_system_score_codex":0.0006612792,"about_ca_system_score_gemma":0.0011899791,"threshold_uncertainty_score":0.13276237},"labels":[],"label_agreement":null}]}